﻿PT	AU	BA	BE	GP	AF	BF	CA	TI	SO	SE	BS	LA	DT	CT	CY	CL	SP	HO	DE	ID	AB	C1	C3	RP	EM	RI	OI	FU	FP	FX	CR	NR	TC	Z9	U1	U2	PU	PI	PA	SN	EI	BN	J9	JI	PD	PY	VL	IS	PN	SU	SI	MA	BP	EP	AR	DI	DL	D2	EA	PG	WC	WE	SC	GA	PM	OA	HC	HP	DA	UT
J	Li, H; Miao, JL; Cui, FX; Li, GY				Li, Hao; Miao, Jinlai; Cui, Fengxia; Li, Guangyou			SURFACTANT PROMOTION OF THE INHIBITORY EFFECTS OF CUPRIC GLUTAMATE ON THE DINOFLAGELLATE <i>ALEXANDRIUM</i>	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium sp; LC3; cupric glutamate; cupric sulfate; extinguishment; hexadecyltrimethyleamine bromide; TEM; ultrastructure	INDUCED OXIDATIVE STRESS; HARMFUL ALGAL BLOOMS; COPPER; CELLS; ACCUMULATION; ANTIOXIDANTS; MITIGATION; RESPONSES; MEMBRANE; CYSTEINE	We studied cupric glutamate as a novel algicide for marine harmful algae and hexadecyltrimethyleamine bromide (HDTMAB) as an accelerant. Cupric glutamate had an excellent ability to inhibit the growth of Alexandrium sp. LC3, but the inhibition efficiency did not increase with higher cupric glutamate concentration. The studies on the inhibition ofAlexandrium sp. LC3 by cupric sulfate or cupric glutamate showed that cupric glutamate had a higher inhibition rate than cupric sulfate (P < 0.05). HDTMAB could significantly enhance the inhibition by cupric glutamate (P < 0.05). Ultrastructural changes of Alexandrium sp. LC3 under cupric sulfate, cupric glutamate, and cupric glutamate-HDTMAB combined treatment were studied with TEM. Under these stresses, the integrity of the cell plasma membranes (cell plasma membrane, chloroplast and mitochondria membranes) was destroyed. The degree of damage under cupric glutamate-HDTMAB combined treatment was more severe than under the other stresses. These results indicated that mechanistically cupric glutamate inhibits algal growth by destroying the cell membranes, and that HDTMAB promotes this process, which induced mass extravasation of intracellular components and more copper ion entry into the plasma.	[Li, Hao; Miao, Jinlai] SOA, Key Lab Marine Biol Act Subst, Qingdao 266061, Peoples R China; [Cui, Fengxia] China Natl Res Inst Food & Fermentat Ind, Beijing 100027, Peoples R China; [Li, Guangyou] SOA, Key Lab Marine Biol Act Subst, Qingdao 266061, Peoples R China		Miao, JL (通讯作者)，SOA, Key Lab Marine Biol Act Subst, Qingdao 266061, Peoples R China.	miaojinlai@163.com						Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; Andrade LR, 2004, ECOTOX ENVIRON SAFE, V58, P117, DOI 10.1016/S0147-6513(03)00106-4; Baek SH, 2003, J MICROBIOL BIOTECHN, V13, P651; Banat IM, 2000, APPL MICROBIOL BIOT, V53, P495, DOI 10.1007/s002530051648; Bustamante J, 2003, HARMFUL ALGAE, V2, P207, DOI 10.1016/S1568-9883(03)00022-2; [曹西华 Cao Xihua], 2003, [海洋与湖沼, Oceanologia et Limnologia Sinica], V34, P201; Demidchik V, 2001, PLANTA, V212, P583, DOI 10.1007/s004250000422; Ferrier M, 2002, J APPL MICROBIOL, V92, P706, DOI 10.1046/j.1365-2672.2002.01576.x; FOYER CH, 1994, PHYSIOL PLANTARUM, V92, P696, DOI 10.1111/j.1399-3054.1994.tb03042.x; Glahn RP, 1997, J NUTR, V127, P642, DOI 10.1093/jn/127.4.642; Glover CN, 2003, BBA-BIOMEMBRANES, V1614, P211, DOI 10.1016/S0005-2736(03)00178-0; Glover RE, 1999, FEMS MICROBIOL LETT, V177, P57; Gryzunov YA, 2003, ARCH BIOCHEM BIOPHYS, V413, P53, DOI 10.1016/S0003-9861(03)00091-2; Hansen G, 2003, HARMFUL ALGAE, V2, P317, DOI 10.1016/S1568-9883(03)00060-X; Hayashi M, 2006, EXP ANIM TOKYO, V55, P419, DOI 10.1538/expanim.55.419; KANG ZY, 1996, J HARBIN U SCI TECHN, V20, P110; Lee J, 2000, GENE, V254, P87, DOI 10.1016/S0378-1119(00)00287-0; Li H, 2006, J ENVIRON SCI, V18, P1152, DOI 10.1016/S1001-0742(06)60054-5; Luo LiXin Luo LiXin, 1998, Chinese Journal of Applied Ecology, V9, P95; MASUDA K, 1993, AQUACULTURE, V117, P287, DOI 10.1016/0044-8486(93)90326-T; NELSON EW, 1991, FEED MANAGEMENT, V42, P6; Nguyen-Ngoc L, 2004, HARMFUL ALGAE, V3, P117, DOI 10.1016/S1568-9883(03)00062-3; Nishikawa K, 2003, FEMS MICROBIOL ECOL, V44, P253, DOI 10.1016/S0168-6496(03)00049-7; Qin CQ, 2004, INT J BIOL MACROMOL, V34, P121, DOI 10.1016/j.ijbiomac.2004.03.009; Salama AAK, 2003, J DAIRY RES, V70, P9, DOI 10.1017/S0022029902005708; SCHWARTZMAN RA, 1993, ENDOCR REV, V14, P133, DOI 10.1210/er.14.2.133; Sengco MR, 2001, MAR ECOL PROG SER, V210, P41, DOI 10.3354/meps210041; Srivastava S, 2006, AQUAT TOXICOL, V80, P405, DOI 10.1016/j.aquatox.2006.10.006; Stitham J, 2006, J BIOL CHEM, V281, P37227, DOI 10.1074/jbc.M604042200; Sun XX, 2004, J EXP MAR BIOL ECOL, V304, P35, DOI 10.1016/j.jembe.2003.11.020; Sun XX, 2004, MAR POLLUT BULL, V48, P937, DOI 10.1016/j.marpolbul.2003.11.021; Tarhanen S, 1998, ANN BOT-LONDON, V82, P735, DOI 10.1006/anbo.1998.0734; Tashjian DH, 2006, ENVIRON TOXICOL CHEM, V25, P2618, DOI 10.1897/05-572R.1; Tripathi BN, 2004, PLANTA, V219, P397, DOI 10.1007/s00425-004-1237-2; VERWEIJ W, 1992, CHEM SPEC BIOAVAILAB, V4, P43, DOI 10.1080/09542299.1992.11083177; WONG SL, 1994, J APPL PHYCOL, V6, P405, DOI 10.1007/BF02182157; Yu ZM, 1999, CHINESE SCI BULL, V44, P617, DOI 10.1007/BF03182721	37	3	3	1	11	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	DEC	2008	44	6					1364	1371		10.1111/j.1529-8817.2008.00591.x	http://dx.doi.org/10.1111/j.1529-8817.2008.00591.x			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	378OQ	27039850	Bronze			2025-03-11	WOS:000261334200002
J	Escalera, L; Reguera, B				Escalera, Laura; Reguera, Beatriz			PLANOZYGOTE DIVISION AND OTHER OBSERVATIONS ON THE SEXUAL CYCLE OF SEVERAL SPECIES OF <i>DINOPHYSIS</i> (DINOPHYCEAE, DINOPHYSIALES)	JOURNAL OF PHYCOLOGY			English	Article						Dinophysis; harmful algal blooms; planozygote division; sexual cycle	LIFE-CYCLE; DINOFLAGELLATE; CULTURE; REPRODUCTION; ACUMINATA	A life-cycle model has been proposed for Dinophysis, but several transitions between stages of this cycle needed more detailed description. In this study, the steps from mating gamete pairs, cell fusion, nuclear fusion, and the fate of planozygotes were tracked and described from incubations of different sexual-cycle stages of D. acuminata Clap. et J. Lachm., D. cf. ovum F. Schutt, and D. acuta Ehrenb. There were several pathways for depauperating division and formation of small and intermediate cells; observed mating tubes that connect mating gamete pairs were more delicate than the feeding tube described in D. acuminata; nuclear fusion occurs following cell fusion. Planozygotes were able to divide and produce several vegetative cells 2-3 weeks after incubation. New pathways were added to the revised sexual life-cycle model of Dinophysis spp. It is hypothesized that planozygotes are the main diploid sexual stage that may be involved in overwintering and seeding strategies. The importance of planozygote division, without further maturation into a resting cyst, as an adaptive strategy for holoplanktonic organisms is discussed.	[Escalera, Laura; Reguera, Beatriz] Ctr Oceanog Vigo, IEO, Vigo 36200, Spain	Spanish Institute of Oceanography	Escalera, L (通讯作者)，Ctr Oceanog Vigo, IEO, Aptdo 1552, Vigo 36200, Spain.	laura.escalera@vi.ieo.es	Reguera, Beatriz/AAG-8273-2020; Escalera, Laura/S-2836-2018	Escalera, Laura/0000-0003-0938-4250; Reguera, Beatriz/0000-0003-4582-9798				Balech E, 2002, FLORACIONES ALGALES, P123; BHAUD Y, 1988, J CELL SCI, V89, P197; Delgado M., 1996, HARMFUL TOXIC ALGAL, P261; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; FRANCO M, 2006, REV GALEGA EC, V15, P1; GARCES E, 2002, RES ENCLOSED SEAS, V12; GENTIEN P, 2004, 11 INT C HARMF ALG I, P121; Giacobbe MG, 1997, J PHYCOL, V33, P73, DOI 10.1111/j.0022-3646.1997.00073.x; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Hajdu S, 2006, AFR J MAR SCI, V28, P289, DOI 10.2989/18142320609504164; Figueroa RI, 2006, J PHYCOL, V42, P1028, DOI 10.1111/j.1529-8817.2006.00262.x; KOFOID CHARLES ATWOOD, 1928, MEM MUS COMP ZOOL HARVARD COLLEGE, V51, P1; Koike K, 2006, J PHYCOL, V42, P1247, DOI 10.1111/j.1529-8817.2006.00288.x; LOVEGROVE T., 1960, JOUR CONSEIL PERM INTERNATL EXPLOR MER, V25, P279; MACKENZIE L, 1992, J PHYCOL, V28, P399, DOI 10.1111/j.0022-3646.1992.00399.x; MOITA MT, 1993, DEV MAR BIO, V3, P153; Olenina I., 2006, HELCOM BALTIC SEA EN, V106; Park MG, 2006, AQUAT MICROB ECOL, V45, P101, DOI 10.3354/ame045101; Parrow MW, 2004, J PHYCOL, V40, P664, DOI 10.1111/j.1529-8817.2004.03202.x; Pfiester L.A., 1984, P181; REGUERA B, 1995, J PLANKTON RES, V17, P999, DOI 10.1093/plankt/17.5.999; Reguera B, 2001, J PHYCOL, V37, P318, DOI 10.1046/j.1529-8817.2001.037002318.x; Reguera B., 2003, THESIS U BARCELONA S; REGUERA B, 1990, CM1990L14 INT COUNC; Reguera B, 2007, J PHYCOL, V43, P1083, DOI 10.1111/j.1529-8817.2007.00399.x; SCHNEPF E, 1988, BOT ACTA, V101, P196, DOI 10.1111/j.1438-8677.1988.tb00033.x; SCHNEPF E, 1984, NATURWISSENSCHAFTEN, V71, P218, DOI 10.1007/BF00490442; SOURNIA A., 1986, ATLAS PHYTOPLANCTON, VI; Uchida Takuji, 1999, Bulletin of Fisheries and Environment of Inland Sea, V1, P163; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Van de Hoek C., 1995, Algae; an Introduction Phycology; Von Stosch HA., 1973, Br Phycol J, V8, P105; VONSTOSCH HA, 1965, NATURWISSENSCHAFTEN, V52, P12	35	30	32	1	20	WILEY-BLACKWELL PUBLISHING, INC	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0022-3646			J PHYCOL	J. Phycol.	DEC	2008	44	6					1425	1436		10.1111/j.1529-8817.2008.00610.x	http://dx.doi.org/10.1111/j.1529-8817.2008.00610.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	378OQ	27039857				2025-03-11	WOS:000261334200009
J	Harzhauser, M; Kern, A; Soliman, A; Minati, K; Piller, WE; Danielopol, DL; Zuschin, M				Harzhauser, Mathias; Kern, Andrea; Soliman, Ali; Minati, Klaus; Piller, Werner E.; Danielopol, Dan L.; Zuschin, Martin			Centennial- to decadal scale environmental shifts in and around Lake Pannon (Vienna Basin) related to a major Late Miocene lake level rise	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pannonian; Dinoflagellates; Palynology; Climate; Impagidinium; Loxoconcha	WALLED DINOFLAGELLATE CYSTS; QUANTITATIVE-ANALYSIS; CLIMATIC CYCLES; POLLEN RECORD; EVOLUTION; MIDDLE; NEOGENE; EUROPE; GRADIENTS; SEDIMENTS	A detailed ultra-high-resolution analysis of a 37-cm-long core of Upper Miocene lake sediments of the long-lived Lake Pannon has been performed. Despite a general stable climate at c. 11-9 Ma, several high-frequency oscillations of the paleoenvironments and depositional environments are revealed by the analysis over a short time span of less than 1000 years. Shifts of the lake level, associated with one major 3rd order flooding are reflected by all organisms by a cascade of environmental changes on a decadal scale. Within a few decades, the pollen record documents shifting vegetation zones due to the landward migration of the coast; the dino-flagellate assemblages switch towards "offshore-type" due to the increasing distance to the shore; the benthos is affected by low oxygen conditions due to the deepening. This general trend is interrupted by smaller scale cycles, which lack this tight interconnection. Especially, the pollen data document a clear cyclicity that is expressed by iterative low pollen concentration events. These "negative" cycles are partly reflected by dino-flagellate blooms suggesting a common trigger-mechanism and a connection between terrestrial environments and surface waters of Lake Pannon. The benthic fauna of the core, however, does not reflect these surface water cycles. This forcing mechanism is not understood yet but periodic climatic fluctuations are favoured as hypothesis instead of further lake level changes. Short phases of low precipitation, reducing pollen production and suppressing effective transport by local streams, might be a plausible mechanism. This study is the first hint towards solar activity related high-frequency climate changes during the Vallesian (Late Miocene) around Lake Pannon and should encourage further ultra-high-resolution analyses in the area. (C) 2008 Elsevier B.V. All rights reserved.	[Harzhauser, Mathias] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1010 Vienna, Austria; [Kern, Andrea; Zuschin, Martin] Univ Vienna, Dept Paleontol, A-1090 Vienna, Austria; [Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Minati, Klaus; Danielopol, Dan L.] Austrian Acad Sci, Commiss Stratig & Palaeontol Res Austria, A-8010 Graz, Austria	University of Vienna; University of Graz; Egyptian Knowledge Bank (EKB); Tanta University; Austrian Academy of Sciences	Harzhauser, M (通讯作者)，Nat Hist Museum Vienna, Geol Paleontol Dept, Burgring 7, A-1010 Vienna, Austria.	mathias.harzhauser@nhm-wien.ac.at	Soliman, Ali/R-1583-2018; Kern, Andrea K./V-5078-2017; Zuschin, Martin/M-9951-2016	Harzhauser, Mathias/0000-0002-4471-6655; Kern, Andrea K./0000-0002-9343-0696; Soliman, Ali/0000-0001-7366-4607; Zuschin, Martin/0000-0002-5235-0198; Piller, Werner E./0000-0003-2808-4720	FWF [P18519-B17, P17738-B03]; NECLIME project; Oskar and Friederike Ermann Fonds; Austrian Academy of Science (Commission for the Stratigraphical and Palaeontological Research of Austria)	FWF(Austrian Science Fund (FWF)); NECLIME project; Oskar and Friederike Ermann Fonds; Austrian Academy of Science (Commission for the Stratigraphical and Palaeontological Research of Austria)	The studies were supported by FWF-grants P18519-B17 and FWF P17738-B03 and contribute to the NECLIME project. Palynological analyses were financed by the Oskar and Friederike Ermann Fonds and by the Austrian Academy of Science (Commission for the Stratigraphical and Palaeontological Research of Austria). One of us (D.L.D.) is much indebted to his colleagues M. Gross (Graz), R. Olteanu (Bucharest), R. Pipik (Banska Bistrica), R. Ross (Ithaka, NY) and Dave Strayer (Millbrook, NY) for fruitful discussion on topics related to the systematics and the ecology of ostracods and J. Knoblechner (Mondsee), A. Stracke (Graz) and R. Buttinger (Vienna) for their technical assistance in the field and/or laboratory.We thank Gonzalo Jimenez-Moreno and Wei-Ming Wang for their intense reviews and helpful suggestions.	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Paleoclimatol. Paleoecol.	DEC 1	2008	270	1-2					102	115		10.1016/j.palaeo.2008.09.003	http://dx.doi.org/10.1016/j.palaeo.2008.09.003			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	386AD	21179376	Green Accepted			2025-03-11	WOS:000261853800009
J	Radi, T; de Vernal, A				Radi, Taoufik; de Vernal, Anne			Last glacial maximum (LGM) primary productivity in the northern North Atlantic Ocean	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST ASSEMBLAGES; OVERTURNING CIRCULATION; BENTHIC FORAMINIFERA; ATMOSPHERIC PCO2; LATE QUATERNARY; HIGH-LATITUDES; CLIMATE-CHANGE; LABRADOR SEA; RECONSTRUCTION	To reconstruct oceanic primary productivity in the northern North Atlantic Ocean during the last glacial maximum (LGM), we have applied the modern analogue technique to dinocyst assemblages using it Northern Hemisphere database that includes 1171 reference sites. The reconstructions were made in LGM sediments (21 +/- 2 kit) of a set of 62 cores collected from 36 degrees N to 75 degrees N. Here, we present the compilation of reconstructed seasonal and annual productivity during the LGM. Results Show lower mean annual productivity during the LGM than at present in the northern North Atlantic. At most high-latitude locations, LGM productivity has been estimated at <200 gC m(-2) a(-1), with extremely low values (<100 gC m(-2) a(-1)) in the Labrador Sea, Baffin Bay, and along the margins of Greenland. Such low values might be the result of reduced Atlantic Meridional Overturning Circulation and stratified water that characterized the glacial episode of the North Atlantic Ocean.	[Radi, Taoufik; de Vernal, Anne] Univ Quebec, Ctr Rech Geochim & Geodynam GEOTOP UQAM & McGill, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Radi, T (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam GEOTOP UQAM & McGill, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	radi.taoufik@courrier.uqam.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Science and Engineering Research Council of Canada (NSERC); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	This work is a contribution to the Polar Climate Stability Network (PCSN) supported by the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS). The authors also acknowledge support from the Natural Science and Engineering Research Council of Canada (NSERC) and the Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT). The authors thank Francesca Sangiorgi and Fabienne Marret for their review of the manuscript.	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J. Earth Sci.	NOV	2008	45	11					1299	1316		10.1139/E08-059	http://dx.doi.org/10.1139/E08-059			18	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	442NF					2025-03-11	WOS:000265847200009
J	Ledu, D; Rochon, A; de Vernal, A; St-Onge, G				Ledu, David; Rochon, Andre; de Vernal, Anne; St-Onge, Guillaume			Palynological evidence of Holocene climate change in the eastern Arctic: a possible shift in the Arctic oscillation at the millennial time scale	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; BARENTS SEA; BAFFIN-BAY; FRESH-WATER; ICE-SHEET; VARIABILITY; RECONSTRUCTION; ISLAND	Dinocyst assemblages and the physical properties of two sediment cores collected in the easternmost part of the main axis of the Northwest Passage, Canadian Arctic Ocean (cores 2004-804-009 BC and 2004-804-009 PC, 74 degrees 11.2'N, 81 degrees 11.7'W) were used to reconstruct changes in sea-surface conditions and to characterize changes in the depositional environment. Core 2004-804-009 PC spans the last 12 180 calibrated (cal) years BP, with sedimentation rates ranging from 45 to 122 cm/ka. Quantitative estimates of sea-surface parameters reveal relatively large hydrographic variability at millennial time scale. Before 11 000 cal years BP, Our records suggest terrigenous inputs related to the last deglaciation. Between 11 000 and 9600 cal years BP, harsh conditions prevailed with August sea-surface temperatures <2 degrees C and the dominance of heterotrophic taxa. This episode was followed by a gradual increase in the relative abundance of phototrophic taxa and the establishment of milder condition with sea-surface temperature (SST) reaching similar to 2 degrees C similar to 8300 cal years BP, possibly related to increased exchange between the Arctic Ocean and the North Atlantic Ocean. From 6000 cal years BP to the late Holocene, climate variability Could be the results of changes in the synoptic-scale atmospheric pattern such as the Arctic oscillation.	[Ledu, David; Rochon, Andre; St-Onge, Guillaume] ISMER, Rimouski, PQ G5L 3A1, Canada; [Ledu, David; Rochon, Andre; de Vernal, Anne; St-Onge, Guillaume] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Ledu, D (通讯作者)，ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	david.ledu@uqar.qc.ca	St-Onge, Guillaume/E-4828-2014; Ledu, David/X-4166-2019; de Vernal, Anne/D-5602-2013	St-Onge, Guillaume/0000-0001-6958-4217; de Vernal, Anne/0000-0001-5656-724X; Ledu, David/0000-0001-5313-7068	ArcticNet Networks of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC); Canadian Foundation for Climate and Atmospheric Science	ArcticNet Networks of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canadian Foundation for Climate and Atmospheric Science	This work was funded by the ArcticNet Networks of Centres of Excellence and the Natural Science and Engineering Research Council of Canada (NSERC). This is a contribution to the ArcticNet project 1.6, the Polar Climate Stability Network supported by the Canadian Foundation for Climate and Atmospheric Science, and the NSERC International Polar Year project, Natural climate variability and forcings in Canadian Arctic and Arctic Ocean - Special Research Opportunity - International Polar Year. We wish to thank the officers and crew of the CCGS Amundsen for their help and support during sampling. We also wish to express our gratitude to the following people who helped during the collection and analyse of the samples: Robbie Bennett, Bedford Institute of Oceanography; Trecia Schell, Dalhousie University; and Pierre Simard, Universite du Quebec a Rimouski, Quebec. Thanks are due to Bassam Ghaleb and Jean-Francois Helie (GEOTOP at UQAM) for geochemical and isotope analyses. We are grateful to the two reviewers. Alwynne B. Beaudoin (Archeological Survey, Provincial Museum of Alberta) and Svend Funder (Geological Museum, University of Copenhagen) for their comments, which helped to improve the manuscript.	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J. Earth Sci.	NOV	2008	45	11					1363	1375		10.1139/E08-043	http://dx.doi.org/10.1139/E08-043			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	442NF					2025-03-11	WOS:000265847200013
J	McKay, JL; de Vernal, A; Hillaire-Marcel, C; Not, C; Polyak, L; Darby, D				McKay, J. L.; de Vernal, A.; Hillaire-Marcel, C.; Not, C.; Polyak, L.; Darby, D.			Holocene fluctuations in Arctic sea-ice cover: dinocyst-based reconstructions for the eastern Chukchi Sea	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; LAST GLACIAL MAXIMUM; NORTH-ATLANTIC; SURFACE CONDITIONS; MARINE ENVIRONMENTS; HIGH-LATITUDES; NORWEGIAN SEA; LEVEL CHANGE; BARENTS SEA; CLIMATE	Cores from site HLY0501-05 on the Alaskan margin in the eastern Chukchi Sea were analyzed for their geochemical (organic carbon, delta C-13(org), C-org/N, and CaCO3) and palynological (dinocyst, pollen, and spores) content to document oceanographic changes during the Holocene. The chronology of the cores was established from Pb-210 dating of near-surface sediments and C-14 dating of bivalve shells. The sediments span the last 9000 years, possibly more, but with a gap between the base of the trigger core and top of the piston core. Sedimentation rates are very high (similar to 156 cm/ka), allowing analyses with a decadal to centennial resolution. The data suggest a shift front a dominantly terrigenous to marine input from the early to late Holocene. Dinocyst assemblages are characterized by relatively high concentrations (6007200 cysts/cm(3)) and high species diversity, allowing the use of the modern analogue technique for the reconstruction of sea-ice cover, summer temperature, and salinity. Results indicate a decrease in sea-ice cover and a corresponding, albeit much smaller, increase in summer sea-surface temperature over the past 9000 years. Superimposed on these long-term trends are millennial-scale fluctuations characterized by periods of low sea-ice and high sea-surface temperature and salinity that appear quasi-cyclic with a frequency of about one every 2500-3000 years. The results of this Study clearly show that sea-ice cover in the western Arctic Ocean has varied throughout the Holocene. More importantly, there have been times when sea-ice cover was less extensive than at the end of the 20th century.	[McKay, J. L.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA; [de Vernal, A.; Hillaire-Marcel, C.; Not, C.] Univ Quebec, Ctr GEOTOP UQAM McGill, Montreal, PQ H3C 3P8, Canada; [Polyak, L.] Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA; [Darby, D.] Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	Oregon State University; University of Quebec; University of Quebec Montreal; University System of Ohio; Ohio State University; Old Dominion University	McKay, JL (通讯作者)，Oregon State Univ, Coll Ocean & Atmospher Sci, 104 COAS Admin Bldg, Corvallis, OR 97331 USA.	mckay_jen@yahoo.ca	Darby, Dennis/A-9219-2010; Hillaire-Marcel, Claude/H-1441-2012; Not, Christelle/A-7082-2011; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	de Vernal, Anne/0000-0001-5656-724X; Not, Christelle/0000-0002-1386-6079; Hillaire-Marcel, Claude/0000-0002-3733-4632	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Sciences and Engineering Research Council (NSERC) of Canada; Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec; US National Science Foundation (NSF) [OPP-9817051/98170540]	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); US National Science Foundation (NSF)(National Science Foundation (NSF))	The authors would like to thank two anonymous reviewers for their constructive comments as well as the editorial staff at CJES. This study is a contribution to the Polar Climate Stability Network (PCSN) supported by the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS). Complementary support was provided by the Natural Sciences and Engineering Research Council (NSERC) of Canada and the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec. The HOTRAX 2005 coring expeditions was supported by a US National Science Foundation (NSF) award to D. Darby and L. Polyak (OPP-9817051/98170540). This paper is dedicated to the memory of Maxime Paiement.	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J	Solignac, S; Grelaud, M; de Vernal, A; Giraudeau, J; Moros, M; McCave, IN; Hoogakker, B				Solignac, Sandrine; Grelaud, Michael; de Vernal, Anne; Giraudeau, Jacques; Moros, Matthias; McCave, I. Nicholas; Hoogakker, Babette			Reorganization of the upper ocean circulation in the mid-Holocene in the northeastern Atlantic	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; SEA-SURFACE CONDITIONS; NORWEGIAN-GREENLAND SEA; NORDIC SEAS; LATE QUATERNARY; TEMPORAL VARIABILITY; SUBPOLAR GYRE; DEEP-OCEAN; DATA-BASE	A micropaleontological investigation was conducted on two sediment cores from the Reykjanes Ridge (RR; core LO09-14; 59 degrees 12.30'N, 31 degrees 05.94'W) and the Faroe-Shetland Channel (FSC; core HM03-133-25; 60 degrees 06.55'N, 06 degrees 04.18'W) to document hydrographical changes of the North Atlantic Current (NAC) during the Holocene. Dinocyst and coccolith assemblages were analyzed, and quantitative reconstructions of sea surface temperatures (SSTs) and sea surface salinities (SSSs) were conducted based on dinocyst assemblages. Both proxies suggest a major reorganization Of Surface circulation patterns in the northeastern North Atlantic between 7 and 5.4 ka BP. At both sites, SSSs before 6.5-7 ka BP were lower than during the mid-late Holocene, Suggesting dispersal of meltwater through the NAC. Long term trends of SSTs, however, show higher than present summer SSTs on the RR from 9.3 to similar to 6 ka BP, and lower than present SSTs in the FSC until ca. 5.4 ka BP. The contrasted SST trends at the two sites suggest that decreasing Summer insolation was not the only forcing behind hydrographical changes in the region. Decoupling of the NAC and the Slope Current (SC), which both influence the FSC, is proposed as a possible mechanism. We hypothesize that a strong NAC during the early to middle Holocene resulted in a SST increase on the RR and decrease in the FSC. Inversely, a weaker NAC after 5-6 ka BP, leading to decreased SSTs on the RR, would have enhanced the relative contribution of the warmer, saltier SC in the FSC, thus resulting in a regional SST and SSS increase.	[Solignac, Sandrine; de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Grelaud, Michael] CEREGE, F-13545 Aix En Provence, France; [Giraudeau, Jacques] Univ Bordeaux 1, CNRS, UMR 5805, F-33405 Talence, France; [Moros, Matthias] Bjerknes Ctr Climate Res, N-5007 Bergen, Norway; [Moros, Matthias] Inst Ostseeforsch, Warnemunde, Germany; [McCave, I. Nicholas; Hoogakker, Babette] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England	University of Quebec; University of Quebec Montreal; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Bjerknes Centre for Climate Research; Leibniz Institut fur Ostseeforschung Warnemunde; University of Cambridge	Solignac, S (通讯作者)，Univ Quebec, Geotop, CP 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	solignac.sandrine@courrier.uqam.ca	McCave, I./O-3992-2018; Grelaud, Michael/I-4189-2015; Giraudeau, Jacques/AAF-5764-2019; de Vernal, Anne/D-5602-2013	Giraudeau, Jacques/0000-0002-5069-4667; Hoogakker, Babette/0000-0002-8171-9679; Grelaud, Michael/0000-0001-8649-9743; Solignac, Sandrine/0000-0003-3373-6922; de Vernal, Anne/0000-0001-5656-724X	Canadian Foundation of Climate and Atmospheric Science (CFCAS); Natural Sciences and Engineering Research Council of Canada (NSERC); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT); French Institut National des Sciences de l'Univers/Conseil National de la Recherche Scientifique (INSU/CNRS); French Agence Nationale de la Recherche	Canadian Foundation of Climate and Atmospheric Science (CFCAS); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); French Institut National des Sciences de l'Univers/Conseil National de la Recherche Scientifique (INSU/CNRS)(Centre National de la Recherche Scientifique (CNRS)); French Agence Nationale de la Recherche(Agence Nationale de la Recherche (ANR))	This study is a contribution of the Polar Climate Stability Network (PCNS) supported by the Canadian Foundation of Climate and Atmospheric Science (CFCAS). The authors also acknowledge financial support from the Natural Sciences and Engineering Research Council of Canada (NSERC), the Fonds quebecois de la recherche sur la nature et les technologies (FQRNT), the French Institut National des Sciences de l'Univers/Conseil National de la Recherche Scientifique (INSU/CNRS) (Project "TARDHOL") and the French Agence Nationale de la Recherche (ANR Project "PICC"). Thanks are due to the two anonymous reviewers and Associate Editor Peter Hollings for their comments on the manuscript.	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J	Novichkova, EA; Polyakova, EI				Novichkova, E. A.; Polyakova, E. I.			Hydrological changes in the White Sea during the historical period inferred from analysis of dinocysts	DOKLADY EARTH SCIENCES			English	Article							DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS		[Novichkova, E. A.] Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia; [Polyakova, E. I.] Moscow MV Lomonosov State Univ, Dept Geog, Moscow, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; Lomonosov Moscow State University	Novichkova, EA (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol, Nakhimovskii Pr 36, Moscow 117997, Russia.		Novichkova, Ekaterina/AAC-4726-2019; Polyakova, Yelena/L-8889-2015; Novichkova, Ekaterina/B-5807-2017	Novichkova, Ekaterina/0000-0001-5687-1719	Russian Foundation for Basic Research [06-05-65267, 06-05-64815]; Program No. 17 of Basic Research [4.4]; Earth Sciences Branch of the Russian Academy of Sciences [OSL-06-16];  [NSh-2236.2006.5]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Program No. 17 of Basic Research; Earth Sciences Branch of the Russian Academy of Sciences(Russian Academy of Sciences); 	We are grateful to Academician A.P. Lisitsyn and V.P. Shevchenko for donated materials for this study thank R.A. Aliev, an employee of the Research Institute of Nuclear Physics of Moscow State University for determination of sedimentation rates at sampling sites using the <SUP>210</SUP>Pb and <SUP>137</SUP>Cs method and calculations of the presumed age of sediments. We are grateful also to the crew of the R/V Professor Shtokman and V.N. Churun, a worker of the Shmidt Laboratory (Arctic and Antarctic Research Institute, St. Petersburg) for vacuum drying of samples. This work was supported by the Russian Foundation for Basic Research (project nos. 06-05-65267 and 06-05-64815), grant NSh-2236.2006.5, Project No. 4.4 of Program No. 17 of Basic Research (Presidium of the Russian Academy of Sciences), grant OSL-06-16, Project "Nanoparticles in Outer and Inner Spheres of the Earth" of the Earth Sciences Branch of the Russian Academy of Sciences.	Aliev RA, 2006, RADIOCHEMISTRY+, V48, P620, DOI 10.1134/S1066362206060166; BERGER VY, 1955, WHITE SEA BIOL RES 1, P7; Golovnina EA, 2005, DOKL EARTH SCI, V400, P136; GRIBBIN J, 1980, CLIMATIC CHANGES; ILINA LV, 2003, PHYTOPLANKTON WHITE; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; LISITSYN AP, 2003, TOPICAL PROBLEMS OCE, P554; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; Mudie PJ, 2001, J QUATERNARY SCI, V16, P595, DOI 10.1002/jqs.660; Nevesskii E. N., 1977, White Sea. Sedimentogenesis and Development History in the Holocene; Novichkova EA, 2007, OCEANOLOGY+, V47, P660, DOI 10.1134/S0001437007050086; PANTYULIN AN, 2003, OCEANOLOGY S1, V43, P1; Polyakova EI, 2003, OCEANOLOGY+, V43, pS144; ZAKHAROV VF, 1981, ICES ARCTIC REGION R	15	2	2	1	4	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1028-334X	1531-8354		DOKL EARTH SCI	Dokl. Earth Sci.	NOV	2008	423	1					1290	1293		10.1134/S1028334X08080242	http://dx.doi.org/10.1134/S1028334X08080242			4	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	376LW					2025-03-11	WOS:000261186100024
J	Povilauskas, L; Barreda, V; Marenssi, S				Povilauskas, Leticia; Barreda, Viviana; Marenssi, Sergio			Pollen and spores of the La Irene Formation (Maastrichtian), Southwestern Santa Cruz Province: First results	GEOBIOS			Spanish	Article						Santa Cruz Province; Palynology; Maastrichtian; La Irene Formation	ANGIOSPERM DIVERSIFICATION; SEYMOUR-ISLAND; PALYNOLOGY	Palynological assemblages are reported for the first time for the La Irene Formation, southwestern Santa Cruz Province, Argentina. This unit represents the sedimentation during a regressive period from transitional or delta-plain to fluvial environments. Palynological assemblages are scarce and moderately well preserved. They mainly consist of continental elements (wood remains, cuticles, spores and pollen grains) with scarse marine palynomorphs (dinoflagellate cysts). The spore-pollen assemblages are dominated by fern spores, followed by angiosperm and gymnosperm pollen grains. Bryophyte spores and fungal remains are also present. Among ferns, Cyatheaceae and spores of Laevigatosporites, of uncertain affinity, are dominant. Of the angiosperm pollen, those of Chloranthaceae (Clavatipollenites sp.) and Arecaceae (Arecipites spp., Longapertites sp., Spinizonocolpites hialinus Archangelsky and Zamaloa) are the most abundant. Pollen of Liliaceae (Liliacidites spp.), Proteaceae (Proteacidites sp., Peninsulapollis gillii (Cookson) Dettmann and Jarzen, Retidiporites camachoii Archangelsky) and Ericaceae (Ericipites scabratus Harris) are also present. Gymnosperm pollen is represented by Podocarpaceae (Podocarpidites spp.) and Ephedraceae (Equisetosporites sp.). These palynological suites would represent a fern-angiosperm dominated coastal vegetation, developed under warm and at least locally humid climatic conditions. La Irene Formation is considered Maastrichtian in age based on stratigraphic evidence, which is, in turn consistent with the ages suggested by the species ranges and the similarities observed with others previously described assemblages. This is the southernmost record of Spinizonocolpites, similar to the extant mangrove palm Nypa. (C) 2008 Elsevier Masson SAS. All rights reserved.	[Povilauskas, Leticia; Barreda, Viviana] Consejo Nacl Invest Cient & Tecn, Div Paleobot, Museo Argentino Ciencias Nat Bernardino Rivadavia, RA-1248 Buenos Aires, DF, Argentina; [Marenssi, Sergio] Univ Buenos Aires, Inst Antartico Argentino, Buenos Aires, DF, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); University of Buenos Aires; Instituto Antartico Argentino	Povilauskas, L (通讯作者)，Consejo Nacl Invest Cient & Tecn, Div Paleobot, Museo Argentino Ciencias Nat Bernardino Rivadavia, Av Angel Gallardo 470,C1405DJR, RA-1248 Buenos Aires, DF, Argentina.	lepovilauskas@macn.gov.ar		Povilauskas, Leticia/0000-0002-5241-0883; Barreda, Viviana Dora/0000-0002-1560-1277				Arbe H.A., 1984, ACT 9 C GEOL ARG SAN, V5, P7; Arbe H.A., 1987, Boletin de Informaciones Petroleras, V9, P91; ARCHANGELSKY S, 1973, Ameghiniana, V10, P339; Archangelsky S., 1986, Ameghiniana, V23, P35; Askin R.A., 1989, Specical Publications of the Geological Society of London, V147, P107; ASKIN RA, 1990, REV PALAEOBOT PALYNO, V65, P105, DOI 10.1016/0034-6667(90)90061-M; ASKIN RA, 1990, MICROPALEONTOLOGY, V36, P141, DOI 10.2307/1485498; Baldoni A.M., 1986, Boletin del IG-USP, Serie Cientifica, V17, P89; Baldoni Alicia M., 1992, Palynology, V16, P117; Baldoni Alicia M., 1993, Palynology, V17, P241; Brasil do, B TEC PETROBRAS, V17, P263; CRANE PR, 1989, SCIENCE, V246, P675, DOI 10.1126/science.246.4930.675; Dettmann M.E., 1987, BRIT ANTARCTIC SURVE, V77, P13; Dettmann M E., 1988, Memoir Assoc Australas Palaeontol, V5, P217; Friis EM, 2006, PALAEOGEOGR PALAEOCL, V232, P251, DOI 10.1016/j.palaeo.2005.07.006; GERMERAAD JH, 1968, REV PALAEOBOT PALYNO, V6, P189, DOI 10.1016/0034-6667(68)90051-1; Harris WK., 1965, Palaeontographica B, V115, P75; Herngreen GFW., 1996, PALYNOLOGY PRINCIPLE, V3, P1157; Kraemer P.E., 1997, Revista de la Asociacion Geologica Argentina, V52, P333; LIDGARD S, 1990, PALEOBIOLOGY, V16, P77, DOI 10.1017/S009483730000974X; Macellari C.E., 1989, J S AM EARTH SCI, V2, P223; Marenssi S, 2004, CRETACEOUS RES, V25, P907, DOI 10.1016/j.cretres.2004.08.004; MILDENHALL DC, 1977, NEW ZEAL J GEOL GEOP, V20, P655, DOI 10.1080/00288306.1977.10430726; Papu O.H., 1989, Ameghiniana, V25, P193; Papú OH, 2002, AMEGHINIANA, V39, P415; Quattrocchio, 1997, REV ESP MICROPALEONT, V29, P115; Raine J.I., 1984, Rep NZ Geol Surv, V109, P1; Ruiz L.C., 1997, REV ESP MICROPALEONT, V29, P13; STOVER L E, 1973, Proceedings of the Royal Society of Victoria, V85, P237; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]	35	23	28	0	4	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	ISSY-LES-MOULINEAUX	65 RUE CAMILLE DESMOULINS, CS50083, 92442 ISSY-LES-MOULINEAUX, FRANCE	0016-6995	1777-5728		GEOBIOS-LYON	Geobios	NOV-DEC	2008	41	6					819	831		10.1016/j.geobios.2008.07.002	http://dx.doi.org/10.1016/j.geobios.2008.07.002			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	386GY		Green Published			2025-03-11	WOS:000261871500009
J	Ghasemi-Nejad, E; Head, MJ; Zamani, M				Ghasemi-Nejad, Ebrahim; Head, Martin J.; Zamani, Maryam			Dinoflagellate cysts from the Upper Triassic (Norian) of northeastern Iran	JOURNAL OF MICROPALAEONTOLOGY			English	Article						dinoflagellate; Miankuhi; Aghdarband; Triassic; Iran	SVERDRUPIELLA; STRATIGRAPHY; ALPS	Upper Triassic (Norian) strata of the Miankuhi Formation in northeastern Iran have been studied palynologically, revealing a diverse but poorly preserved association of dinoflagellate cysts. Based on representatives of the genera Hebecysta, Heibergella, Rhaetogonyaulax and Sverdrupiella, the strata are assigned to the middle of the Hebecysta balmei Zone with an inferred age of early Late Norian. The association shows similarities with assemblages from Australia, New Zealand, Indonesia, Northwest Europe, arctic Canada and Alaska, indicating an interconnection of warm Tethyan waters during the Late Triassic. The occurrence of Sverdrupiella species in the clastic. near-shore marine deposits of Miankuhi, and their presence in similar sedimentary facies world-wide, indicate that this genus was well adapted to clastic shallow-marine environments. J. Micropalaeontol. 27(2): 125-134, November 2008.	[Ghasemi-Nejad, Ebrahim; Zamani, Maryam] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	University of Tehran; Brock University	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Fac Sci, Dept Geol, Enghelab Ave, Tehran, Iran.	eghasemi@khayam.ut.ac.ir; mjhead@brocku.ca	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068				Alavi M, 1997, GEOL SOC AM BULL, V109, P1563, DOI 10.1130/0016-7606(1997)109<1563:TTAARO>2.3.CO;2; [Anonymous], 1989, Tectonic Evolution of the Tethyan Region; [Anonymous], GEOLOGIC TIME SCALE; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 1975, Geosci. Man, DOI DOI 10.1080/00721395.1975.9989758; [Anonymous], 1984, Neues Jahrbuch fur Geologie und Palaontologie-Abhandlungen; [Anonymous], NEUES JB GEOLOGIE PA; [Anonymous], 1996, Palynology: principles and applications; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Baud Aymon, 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P111; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BOERSMA M, 1991, ABH GEOL B A, V38, P223; Brinkhuis H., 2006, ADV COURSE JURASSIC; BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; Davoudzadeh M., 1981, Neues Jahrbuch Geologie und Palaontologie, V3, P180; Detterman R.L., 1970, Proceedings of the geological seminar on the North Slope of Alaska: Pacific Section AAPG, P1; Donofrio Donato A., 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P205; Eftekharnezhad J., 1991, Abhandlungen der Geologischen Bundesanstalt, V38, P89; Ghasemi-Nejad E, 2004, REV PALAEOBOT PALYNO, V132, P207, DOI 10.1016/j.revpalbo.2004.07.001; HELBY R, 1988, NEW ZEAL J BOT, V26, P117, DOI 10.1080/0028825X.1988.10410104; HELBY R, 1987, AUST J EARTH SCI, V34, P151, DOI 10.1080/08120098708729399; Hochuli PA, 2000, ECLOGAE GEOL HELV, V93, P429; KRYSTANTOLLMANN E, 1991, ABHANDLUNGEN GEOLOGI, V38, P195; Krystyn Leopold, 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P139; Kuerschner WM, 2007, PALAEOGEOGR PALAEOCL, V244, P257, DOI 10.1016/j.palaeo.2006.06.031; Morbey S.J., 1978, Palinologia numero extraordinario, V1, P355; Oberhauser Rudolf, 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P201; OSULLIVAN T, 1985, IND PETR ASS P 14 AN; Palliani RB, 2006, LETHAIA, V39, P305, DOI 10.1080/00241160600847538; Ruttner A.W, 1991, ABHANDLUNGEN GEOL BU, V38, P7; RUTTNER AW, 1993, GEOL RUNDSCH, V82, P110, DOI 10.1007/BF00563274; RUTTNER AW, 1988, 2 MIN S IR KER MIN M, P183; Ruttner AW, 1983, GEOLOGICAL SURVEY IR, V51, P451; Schmidt K., 1984, NEUES JB GEOLOGIE PA, V168, P173; Schonlaub Hans Peter, 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P81; Seyed-Emami K., 1971, GEOL SURV IRAN REPOR, V20, P41; Siblik Milos, 1991, Abhandlungen der Geologischen Bundesanstalt (Vienna), V38, P165; SOFFEL H, 1975, J GEOPHYS-Z GEOPHYS, V41, P541; SOFFEL H, 1980, J GEOMAGNETISM S, V111, P117; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P143; TRAVERSE A, 1972, GEOSCIENCE MAN, V4, P87; WENSINK H, 1983, EARTH PLANET SC LETT, V63, P325, DOI 10.1016/0012-821X(83)90045-6; WENSINK H, 1982, J GEOPHYSICS, V51, P21; WIGGINS V D, 1973, Micropaleontology (New York), V19, P1, DOI 10.2307/1484961; WIGGINS VD, 1976, 9 ANN M AM ASS STRAT; WILSON GJ, 1986, NZ GEOLOGICAL SOC NE, V71, P48	46	12	12	0	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	NOV	2008	27		2				125	134		10.1144/jm.27.2.125	http://dx.doi.org/10.1144/jm.27.2.125			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	474QC		hybrid			2025-03-11	WOS:000268298000005
J	Liu, GX; Pei, GF; Hu, ZY				Liu, Guo-Xiang; Pei, Guo-Feng; Hu, Zheng-Yu			<i>Peridiniopsis niei</i> sp nov (Dinophyceae), a new species of freshwater red tide dinoflagellates from China	NOVA HEDWIGIA			English	Article							LAKE KINNERET; PERIDINIALES; PHYTOPLANKTON; PENARDII	A new freshwater phototrophic species of the dinoflagellate genus Peridiniopsis, P. niei sp. nov., is described based on morphology. The new species appeared during spring with densities up to 1.48 x 10(7) cells L(-1) in some tributaries and gullies of Three Gorge Reservoir and Lake Donghu, China, forming red tides. Peridiniopsis niei is a cyst-producing freshwater dinoflagellate that belongs to the group Penardii. The plate tabulation is po+x+4 '+0a+6 ''+5c+5s+5 '''+2 '''' and the plate pattern is symmetric. The cells of P. niei are pentagonal in ventral view, the epitheca is larger than the hypotheca, making up about 2/3 the length of the cell. Plate 3 ' is hexangular. The closest species to P. niei is P. penardii (Lemmermann) Bourrelly, but cells of the former are pentagonal, very compressed dorsoventrally, and the hypotheca is truncated with one transparent, robust spine on each antapical plate.	[Liu, Guo-Xiang; Hu, Zheng-Yu] Chinese Acad Sci, Inst Hydrobiol, State Key Lab Freshwater Ecol & Biotechnol China, Wuhan 430072, Peoples R China; [Pei, Guo-Feng] S Cent Univ Nationalities, Coll Life Sci, Wuhan 430074, Peoples R China	Chinese Academy of Sciences; Institute of Hydrobiology, CAS; South Central Minzu University	Liu, GX (通讯作者)，Chinese Acad Sci, Inst Hydrobiol, State Key Lab Freshwater Ecol & Biotechnol China, Wuhan 430072, Peoples R China.	liugx@ihb.ac.cn	Liu, Guoxiang/L-7413-2019	Liu, Guoxiang/0000-0001-8565-2363	National Natural Science Foundation of China [30470140]; Key Project of the Chinese Academy of Sciences [KSCX2-YW-Z-039]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Key Project of the Chinese Academy of Sciences(Chinese Academy of Sciences)	This work was supported by the National Natural Science Foundation of China (No. 30470140), the Key Project of the Chinese Academy of Sciences (Grant No. KSCX2-YW-Z-039).	BERMAN T, 1992, AQUAT SCI, V54, P104, DOI 10.1007/BF00880278; Boltovskoy A, 1999, GRANA, V38, P98, DOI 10.1080/713786927; BOURRELLY P, 1968, Protistologica, V4, P5; Bourrelly P, 1970, ALGUES EAU DOUCE INI, VIII; Calado AJ, 2002, PHYCOLOGIA, V41, P567, DOI 10.2216/i0031-8884-41-6-567.1; Chinese Environmental Protection Bureau, 1989, MON AN METH WAT SEW; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; HORNE AJ, 1971, LIMNOL OCEANOGR, V16, P684, DOI 10.4319/lo.1971.16.4.0684; IMAMURA K, 1990, RED TIDE ORGANISMS J, P134; ITO T, 1979, B PLANKTON SOC JPN, V26, P113; JAVORNIC.P, 1971, J PHYCOL, V7, P303, DOI 10.1111/j.0022-3646.1971.00303.x; Leitao Maria, 2001, Archiv fuer Hydrobiologie Supplement, V138, P1; LIU JK, 1995, ECOLOGICAL STUDIES L, V2; LIU JK, 1990, ECOLOGICAL STUDIES L, V1; Meyer B, 1997, NOVA HEDWIGIA, V65, P365; Popovsky J., 1990, SUSSWASSERFLORA MITT, V6, P1; Rodriguez Sylvaine, 1999, Archiv fuer Hydrobiologie Supplement, V130, P15; SAKO Y, 1987, B JPN SOC SCI FISH, V53, P473; Takano Y, 2008, PHYCOLOGIA, V47, P41, DOI 10.2216/07-36.1; Ten-Hage L, 2007, NOVA HEDWIGIA, V85, P259, DOI 10.1127/0029-5035/2007/0085-0259; Trigueros JM, 2000, PHYCOLOGIA, V39, P126, DOI 10.2216/i0031-8884-39-2-126.1; Xie P, 2001, ScientificWorldJournal, V1, P337; Zohary T, 2004, FRESHWATER BIOL, V49, P1355, DOI 10.1111/j.1365-2427.2004.01271.x	23	21	28	1	14	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0029-5035			NOVA HEDWIGIA	Nova Hedwigia	NOV	2008	87	3-4					487	499		10.1127/0029-5035/2008/0087-0487	http://dx.doi.org/10.1127/0029-5035/2008/0087-0487			13	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	385OG					2025-03-11	WOS:000261822900011
J	Elbrächter, M; Gottschling, M; Hildebrand-Habel, T; Keupp, H; Kohring, R; Lewis, J; Meier, KJS; Montresor, M; Streng, M; Versteegh, GJM; Willems, H; Zonneveld, K				Elbraechter, Malte; Gottschling, Marc; Hildebrand-Habel, Tania; Keupp, Helmut; Kohring, Rolf; Lewis, Jane; Meier, K. J. Sebastian; Montresor, Marina; Streng, Michael; Versteegh, Gerard J. M.; Willems, Helmut; Zonneveld, Karin			Establishing an Agenda for Calcareous Dinoflagellate Research (Thoracosphaeraceae, Dinophyceae) including a nomenclatural synopsis of generic names	TAXON			English	Article						calcareous dinophytes; checklist; Thoracosphaeraceae	SOUTH ATLANTIC-OCEAN; SURFACE SEDIMENTS; LIFE-CYCLE; SCRIPPSIELLA-TROCHOIDEA; CYST PRODUCTION; PHYLOGENY; CALCIODINELLOIDEAE; NOV; PERIDINIALES; ASSOCIATIONS	Calcareous dinoflagellates are considered to be a monophyletic group of peridinoid taxa that have the potential to produce calcified exoskeletal structures during the life cycle, or that derive from such forms. Frequently, these calcareous bodies are excellently preserved in the fossil record and have received increased attention during the past three decades with regard to their use in biostratigraphy, climate and environmental reconstruction. Fossil and extant taxa have been classified in various, partly concurring, systematic concepts, using character complexes of the theca, cyst wall ultrastructure and archaeopyle/operculum morphology. The significance of such character complexes is briefly discussed in the light of molecular data that have been accumulated during the past decade. Over the years, the number of published taxonomic names has increased partly due to nomenclatural changes. We propose that the entirely of calcareous dinoflagellates, and non-calcareous relatives derived from them, is accommodated in a single family of the order Peridiniates, the Thoracosphaeraceae, combining the former segregate taxonomic units Calciodinelloideae, a subfamily within Peridiniaceae, and Thoracosphaerales, a separate dinoflagellate order. As a result of a meeting of calcareous dinoflagellate specialists. we outline major subjects that are in need of re-investigation and -evaluation (an Agenda for Calcareous Dinoflagellate Research). In order to contribute to a consistent and stable nomenclature and taxonomy of calcareous dinoflagellates, we list 97 published generic names assigned to known calcareous dinoflagellates in a nomenclatural synopis, with species names indicating their types and information on type locality and stratigraphy. We evaluate the status of these names-whether validly published and, if so, whether legitimate-a crucial first step for any revisionary work in the future.	[Elbraechter, Malte] Deutsch Zentrum Marine Diversitatsforsch, Forschungsinst Senckenberg, Wattenmeerstn Sylt, D-25991 List Auf Sylt, Germany; [Gottschling, Marc; Keupp, Helmut; Kohring, Rolf] Univ Munich, D-80638 Munich, Germany; [Hildebrand-Habel, Tania] Univ Stavanger, Fac Sci & Technol, N-4036 Stavanger, Norway; [Lewis, Jane] Univ Westminster, Sch Biosci, London W1W 6UW, England; [Meier, K. J. Sebastian] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany; [Montresor, Marina] Stn Zool A Dohrn, I-80121 Naples, Italy; [Streng, Michael] Uppsala Univ, Dept Earth Sci Palaeobiol, S-75236 Uppsala, Sweden; [Versteegh, Gerard J. M.] Univ Hamburg, Inst Biogeochem & Marine Chem, D-20146 Hamburg, Germany; [Willems, Helmut; Zonneveld, Karin] Univ Bremen, Fachbereich Geowissensch Hist Geol & Palaontol, D-28334 Bremen, Germany	Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Munich; Universitetet i Stavanger; University of Westminster; University of Kiel; Stazione Zoologica Anton Dohrn; Uppsala University; University of Hamburg; University of Bremen	Elbrächter, M (通讯作者)，Deutsch Zentrum Marine Diversitatsforsch, Forschungsinst Senckenberg, Wattenmeerstn Sylt, Hafenstr 43, D-25991 List Auf Sylt, Germany.	melbraechter@awi-bremerhaven.de	Hildebrand-Habel, Tania/F-3590-2011; Gottschling, Marc/K-2186-2014; Meier, K. J. Sebastian/H-7914-2014; Versteegh, Gerard J.M./H-2119-2011	Meier, K. J. 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F., 2005, Palaeontologische Zeitschrift, V79, P61	89	65	67	0	12	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0040-0262	1996-8175		TAXON	Taxon	NOV	2008	57	4					1289	1303		10.1002/tax.574019	http://dx.doi.org/10.1002/tax.574019			15	Plant Sciences; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Evolutionary Biology	377WO					2025-03-11	WOS:000261283000019
J	Figueroa, RI; Garcés, E; Massana, R; Camp, J				Figueroa, Rosa Isabel; Garces, Esther; Massana, Ramon; Camp, Jordi			Description, host-specificity, and strain selectivity of the dinoflagellate parasite <i>Parvilucifera sinerae</i> sp nov (Perkinsozoa)	PROTIST			English	Article						dinoflagellates; Parvilucifera; parasites; perkinsids; toxic phytoplankton	AMOEBOPHRYA-CERATII; CHESAPEAKE BAY; ULTRASTRUCTURE; DINOPHYCEAE; INFECTION; ALVEOLATA; POSITION; HISTORY; PROBES	A new species of parasite, Parvilucifera sinerae sp. nov., isolated from a bloom of the toxic dinoflagellate Alexandrium minutum in the harbor of Arenys de Mar (Mediterranean Sea, Spain), is described. This species is morphologically, behaviourally, and genetically (18S rDNA sequence) different from Parvilucifera infectans, until now the only species of the genus Parvilucifera to be genetically analyzed. Sequence analysis of the 18S ribosomal DNA supported P. sinerae as a new species placed within the Perkinsozoa and close to P. infectans. Data on the seasonal occurrence of P. sinerae, its infective rates in natural and laboratory cultures, and intra-species strain-specific resistance are presented. Life-cycle studies in field samples showed that the dinoflagellate resting zygote (resting cyst) was resistant to infection, but the mobile zygote (planozygote) or pellicle stage (temporary cyst) became infected. The effects of light and salinity levels on the growth of P. sinerae were examined, and the results showed that low salinity levels promote both sporangial germination and higher rates of infection. Our findings on this newly described parasite point to a complex host-parasite interaction and provide valuable information that leads to a reconsideration of the biological strategy to control dinoflagellate blooms by means of intentional parasitic infections. (C) 2008 Elsevier GmbH. All rights reserved.	[Figueroa, Rosa Isabel; Garces, Esther; Massana, Ramon; Camp, Jordi] CSIC, ICM, E-08003 Barcelona, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Figueroa, RI (通讯作者)，CSIC, ICM, Pg Maritim Barceloneta 37-49, E-08003 Barcelona, Spain.	figueroa@icm.csic.es; esther@icm.csic.es	Massana, Ramon/F-4205-2016; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015	Garces, Esther/0000-0002-2712-501X; Figueroa, Rosa/0000-0001-9944-7993; Massana, Ramon/0000-0001-9172-5418; Camp, Jordi/0000-0002-5202-9783	EU Project SEED [GOCE-CT-2005-003875]; Spanish Ministry of Education and Science [I3P, Ramon y Cajal]	EU Project SEED; Spanish Ministry of Education and Science(Spanish Government)	This research was funded by the EU Project SEED (GOCE-CT-2005-003875). R.I. Figueroa work is supported by a I3P contract and E. Garces' work is supported by a Ramon y Cajal grant, both from the Spanish Ministry of Education and Science. We thank J.M. Fortuno for his technical assistance during SEM analyses; M. Alcaraz, who suggested the name of the species; S. Fraga and M. Mas, for helping with the Latin etymology, and S. Fraga, L. Cros, and N. Sampedro for providing the cultures. We also thank R. Logares for his help with the phylogenetic analyses.	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J	Spilling, K; Lindström, M				Spilling, Kristian; Lindstrom, Magnus			Phytoplankton life cycle transformations lead to species-specific effects on sediment processes in the Baltic Sea	CONTINENTAL SHELF RESEARCH			English	Article						Baltic Sea; Phosphorus cycling; Phytoplankton; Sedimentation; Resting stages	SCRIPPSIELLA-HANGOEI DINOPHYCEAE; ANAEROBIC AMMONIUM OXIDATION; DISSOLVED ORGANIC-MATTER; FLUIDIZED-BED REACTOR; GREEN ALGAL CELLS; SPRING-BLOOM; MICROBIAL DECOMPOSITION; RESTING CYSTS; DINOFLAGELLATE; WATER	In order to study the sediment response to different addition of organic matter, we added cultures of the dinoflagellates Scrippsiella hangoei and Woloszynskia halophila and the diatom Pauliella taeniata to aquaria containing natural sediment. The biomass added was 1550-3260 mg C m(-2), and in the control, no biomass was added (n = 3). Oxygen profiles at the sediment-water interface and inorganic nutrients in the near bottom water were determined once a week. In the additions of P. taeniata and W halophila the sediment quickly became anoxic. and subsequently there was a flux of > 1 mmol PO43- m(-2) d(-1) out of the sediment in these treatments. The majority of the released P came from P stored in the sediment and not from the organic phosphorus added. The result was very different for the S. hangoei addition. This species underwent a life cycle change to form temporary cysts. During this process there was a net uptake of nutrients. After the formation of cysts the concentration of inorganic nutrient was similar to that of the control. Cysts generally survive for long periods in the sediment (months to years) before germinating, but can also be permanently buried in the sediment. The novel idea presented here is that the phytoplankton composition may directly affect sediment processes such as oxygen consumption and phosphorus release, through species-specific life cycle changes and yields of resting stages produced prior to sedimentation. This can be an important aspect of nutrient cycling in eutrophic waters, like the Baltic Sea, where there is large year-to-year difference in the amount of resting stages settling at the sea floor, mainly due to differences in abundance of diatoms and dinoflagellates during the spring bloom. If yields of resting stages change, e.g. due to changes in the phytoplankton community, it may lead to alterations in the biogeochemical cycling of nutrients. (C) 2008 Elsevier Ltd. All rights reserved.	[Spilling, Kristian] Finnish Environm Inst, FIN-00251 Helsinki, Finland; [Spilling, Kristian; Lindstrom, Magnus] Univ Helsinki, Tvarminne Zool Stn, FIN-10900 Hango, Finland	Finnish Environment Institute; University of Helsinki	Spilling, K (通讯作者)，Finnish Environm Inst, POB 140, FIN-00251 Helsinki, Finland.	kristian.spilling@ymparisto.fi	Spilling, Kristian/L-7932-2014	Spilling, Kristian/0000-0002-8390-8270	Finnish Academy [111336]; Walter and Andre de Nottbeck Foundation; Academy of Finland (AKA) [111336] Funding Source: Academy of Finland (AKA)	Finnish Academy(Research Council of Finland); Walter and Andre de Nottbeck Foundation; Academy of Finland (AKA)(Research Council of Finland)	This study was funded by Finnish Academy (Project 111336) and Walter and Andre de Nottbeck Foundation. We would like to acknowledge the staff at Tvarminne Zoological Station, University of Helsinki for help and support during this project, in particular Elina Salminen and Mervi Sjoblom for measuring nutrient concentrations and Antti Nevalainen for operating the mass spectrometer. We would also like to thank Jouni Lehtoranta for vibrant discussions about the important topic of sediment remineralization.	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Shelf Res.	OCT 15	2008	28	17					2488	2495		10.1016/j.csr.2008.07.004	http://dx.doi.org/10.1016/j.csr.2008.07.004			8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	363AX					2025-03-11	WOS:000260239400011
J	Alves-De-Souza, C; Varela, D; Navarrete, F; Fernández, P; Leal, P				Alves-De-Souza, Catharina; Varela, Daniel; Navarrete, Florencia; Fernandez, Pamela; Leal, Pablo			Distribution, abundance and diversity of modern dinoflagellate cyst assemblages from southern Chile (43-54° S)	BOTANICA MARINA			English	Article						Alexandrium catenella; inshore seas; dinoflagellate cysts; recent sediments; southern Chile	RECENT MARINE-SEDIMENTS; TAMARENSE LEBOUR BALECH; ENVIRONMENTAL-FACTORS; SURFACE SEDIMENTS; COASTAL WATERS; RESTING CYSTS; WEST-COAST; ALEXANDRIUM; PHYTOPLANKTON; PATAGONIA	The distribution, abundance and diversity of modern dinoflagellate cyst assemblages were investigated in sediments from the inshore seas of southern Chile (43 degrees 08'-54 degrees 55' S) at eight sites from April 2004 to January 2005. A total of 24 cyst types were recorded, of which 12 and five were identified at the species and genus levels, respectively. Dinoflagellate cysts were recorded from all sampling sites, but they differed in total abundance (15-270 cysts ml(-1)) and diversity index (H' 0.88-2.40). Heterotrophic dinoflagellate cysts assigned to heterotrophic species were the most abundant trophic form, with 418 cysts ml(-1), representing 55% of the total cyst abundance. Cluster analysis based on the abundance of dinoflagellate cyst species indicated that sampling sites were segregated into three groups likely to be related to the proportion of autotrophic vs. heterotrophic species cysts and the total abundance of cysts at each site. Distinctive cyst species composition differences among sampling sites may allow inferences about local nutrient and feeding dynamics within the water column.	[Alves-De-Souza, Catharina] Univ Austral Chile, Inst Biol Marina Dr Jurgen Winter, Valdivia, Chile; [Alves-De-Souza, Catharina; Varela, Daniel; Navarrete, Florencia; Fernandez, Pamela; Leal, Pablo] Univ Los Lagos, Ctr I Mar, Puerto Montt, Chile	Universidad Austral de Chile; Universidad de Los Lagos	Alves-De-Souza, C (通讯作者)，Univ Austral Chile, Inst Biol Marina Dr Jurgen Winter, POB 567,Campus Isla Teja, Valdivia, Chile.	catharinaalves@uach.cl	Alves-de-Souza, Catharina/G-3286-2014; Leal, Pablo/N-3927-2019; Varela, Daniel/D-9484-2013; Fernandez, Pamela/AAX-1676-2021; Leal, Pablo/H-6355-2013; Fernandez, Pamela Andrea/K-2021-2014; Varela, Daniel/D-7908-2013	Leal, Pablo/0000-0002-7616-1850; Alves-de-Souza, Catharina/0000-0001-9577-8090; Fernandez, Pamela Andrea/0000-0003-3122-0084; Varela, Daniel/0000-0003-4603-4970	FDI-Corfo [CT03MR-02]	FDI-Corfo	We would like to thank the Instituto de Fomento Pesquero (IFOP) of Punta Arenas for helping with sediment sampling at the site in the Magallanes Region. We are also grateful to Dr. Marina Montresor, who confirmed the taxonomic identification of some dinoflagellate cysts, and Dr. Jose Luis Iriarte, who read and commented on the manuscript and financially supported the translation into English. Finally, we are grateful to Julie Koester and two anonymous reviewers whose suggestions greatly improved the paper. This study was funded by project FDI-Corfo CT03MR-02.	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Marina	OCT	2008	51	5					399	410		10.1515/BOT.2008.052	http://dx.doi.org/10.1515/BOT.2008.052			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	367WG					2025-03-11	WOS:000260582700007
J	Götz, AE; Feist-Burkhardt, S; Ruckwied, K				Goetz, Annette E.; Feist-Burkhardt, Susanne; Ruckwied, Katrin			Palynofacies and sea-level changes in the Upper Cretaceous of the Vocontian Basin, southeast France	CRETACEOUS RESEARCH			English	Article; Proceedings Paper	7th International Symposium on Cretaceous	SEP 05-09, 2005	Neuchatel, SWITZERLAND			Upper Cretaceous; southeastern France; Vocontian Basin; Palynofacies; Sea-level changes; Sequence stratigraphy	SEDIMENTARY ORGANIC-MATTER; SEQUENCE STRATIGRAPHY; CARBONATES	Upper Cretaceous platform carbonates of the Vocontian Basin (southeastern France) have been investigated in a cross-section from the proximal deposits exposed in the lower Rhone Valley to the distal part of the basin in the Southern Subalpine Ranges north of Nice. The stratigraphic interval studied in detail spans the uppermost Turonian and Coniacian. Palynofacies patterns were used to detect eustatic signals at a third-order scale and are the tool for correlation of proximal and distal platform deposits. The organic constituents observed in the studied samples have been grouped into a continental fraction, including higher plant debris (phytoclasts) and sporomorphs, and a marine fraction with dinoflagellate cysts, acritarchs, prasinophytes, and foraminiferal test linings. The main factors influencing the stratigraphic and spatial distribution of land-derived, allochthonous, and marine, relatively autochthonous, organic particles are the proximity of land, the organic productivity, the degree of biodegradation and the hydrodynamic conditions of the depositional system. Palynofacies parameters used for the sequence stratigraphic interpretation are: (1) the ratio of continental to marine constituents (CONT/MAR ratio); (2) the ratio of opaque to translucent phytoclasts (OP/TR ratio); (3) the phytoclast particle size and shape; and (4) the relative proportion and species diversity of marine plankton. Ternary diagrams illustrating significant proximality changes were used to decipher transgressive-regressive trends within the succession. High amounts of translucent phytoclasts and decreasing values of the CONT/MAR ratio occur during the phase of relative sea-level rise in the upper Turonian. The stratigraphic interval of maximum flooding around the Turonian/Coniacian boundary is marked by the highest abundance and species diversity of clinoflagellate cysts, and by high percentages of opaque, equidimensional particles within the phytoclast group. The OP/TR ratio is still high within the lower Coniacian representing the early highstand deposits, whereas the relative abundance of marine constituents is again decreasing. Sedimentary organic matter of the upper Coniacian is dominated by large, blade-shaped, mainly opaque phytoclasts, which are a characteristic palynofacies signature of late highstand deposits. The present study demonstrates the high potential of palynofacies analysis in high-resolution stratigraphy and correlation of sedimentary series of shallow epeiric seas. (C) 2008 Elsevier Ltd. All rights reserved.	[Goetz, Annette E.] Tech Univ Darmstadt, Inst Appl Geosci, D-64287 Darmstadt, Germany; [Feist-Burkhardt, Susanne] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Ruckwied, Katrin] Shell Int Explorat & Prod BV, NL-2288 GS Rijswijk, Netherlands	Technical University of Darmstadt; Natural History Museum London; Royal Dutch Shell	Götz, AE (通讯作者)，Tech Univ Darmstadt, Inst Appl Geosci, Schnittspahnstr 9, D-64287 Darmstadt, Germany.	goetz@energycenter.tu-darmstadt.de	Götz, Annette/AAJ-5873-2020; Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242; Gotz, Annette E./0000-0002-7467-3617				[Anonymous], 2007, Paleopalynology; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1982, J. 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Res.	OCT-DEC	2008	29	5-6					1047	1057		10.1016/j.cretres.2008.05.029	http://dx.doi.org/10.1016/j.cretres.2008.05.029			11	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	370KP					2025-03-11	WOS:000260761400027
J	Touzet, N; Franco, JM; Raine, R				Touzet, Nicolas; Franco, Jose M.; Raine, Robin			Morphogenetic diversity and biotoxin composition of <i>Alexandrium</i> (Dinophyceae) in Irish coastal waters	HARMFUL ALGAE			English	Article						Alexandrium HAB; PSP toxins; rDNA; resting cysts; spirolides	PARALYTIC SHELLFISH TOXINS; HARMFUL ALGAL BLOOMS; SPIROLIDE MARINE TOXINS; DINOFLAGELLATE CYSTS; MINUTUM DINOPHYCEAE; SPECIES COMPLEX; PHYLOGENETIC ANALYSIS; SEQUENCE COMPARISONS; NATURAL-POPULATIONS; PIGMENT COMPOSITION	The diversity of Alexandrium spp. in Irish coastal waters was investigated through the morphological examination of resting cysts and vegetative cells, the determination of PSP toxin and spirolide profiles and the sequence analysis of rDNA genes. Six morphospecies were characterised: A. tamarense, A. minutum, A. ostenfeldii, A. peruvianum, A tamutum and A andersoni. Both PSP toxin producing and nontoxic strains of A. tamarense and A. minutum were observed. The average toxicities of toxic strains for both cultured species were respectively 11.3 (8.6 S.D.) and 2.3 (0.5 S.D.) pg STX equiv. cell(-1). Alexandrium ostenfeldii and A. peruvianum did not synthesise PSP toxins but HPLC-MS analysis of two strains showed distinct spirolide profiles. A cyst-derived culture of A. peruvianum from Lough Swilly mainly produced spirolides 13 desmethyl-C and 13 desmethyl-D whereas one of A. ostenfeldii, from Bantry Bay, produced spirolides C and D. Species identification was confirmed through the analyses of SSU, ITS1-5.8S-ITS2 and LSU rDNA genes. Some nucleotide variability was observed among clones of toxic strains of A. tamarense, which all clustered within the North American clade. However, rDNA sequencing did not allow discrimination between the toxic and non-toxic forms of A. minutum. Phylogenetic analysis also permitted the differentiation of A. ostenfeldii from A. peruvianum. Resting cysts of PSP toxin producing Alexandrium species were found in Cork Harbour and Belfast Lough, locations where shellfish contamination events have occurred in the past, highlighting the potential for the initiation of harmful blooms from cyst beds. The finding of supposedly non-toxic and biotoxin-producing Alexandrium species near aquaculture production sites will necessitate the use of reliable discriminative methods in phytoplankton monitoring. (C) 2008 Elsevier B.V. All rights reserved.	[Touzet, Nicolas; Raine, Robin] Natl Univ Ireland Univ Coll Galway, Martin Ryan Inst, Galway, Ireland; [Franco, Jose M.] UA Fitoplancton Tox, CSIC IEO, Vigo, Spain	Ollscoil na Gaillimhe-University of Galway; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM)	Touzet, N (通讯作者)，Natl Univ Ireland Univ Coll Galway, Martin Ryan Inst, Galway, Ireland.	nicolas.touzet@nuigalway.ie		touzet, nicolas/0000-0002-8524-9184	Higher Education Authority of Ireland (Department of Education and Science) (PRTLI Cycle III); EC 6th Framework Programme [GOCE-CT-2005-003375]	Higher Education Authority of Ireland (Department of Education and Science) (PRTLI Cycle III); EC 6th Framework Programme(European Union (EU))	The authors wish to thank the captain and crew of the RV Celtic Voyager, Glenn Nolan, Tara Chamberlain and Aoife Ni Rathaille for assistance in field sampling. We are grateful to Pilar Riobo Agulla and Beatriz Paz Pino (IEO, Vigo) for assistance with toxin analysis. 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J	Persson, A; Smith, BC; Wikfors, GH; Alix, JH				Persson, Agneta; Smith, Barry C.; Wikfors, Gary H.; Alix, Jennifer H.			Dinoflagellate gamete formation and environmental cues: Observations, theory, and synthesis	HARMFUL ALGAE			English	Article						bloom; cyst; dinollagellate; gamete; mating; red tide	GYMNODINIUM-CATENATUM; GONYAULAX-TAMARENSIS; VERTICAL MIGRATION; ENCYSTMENT; LACHRYMOSA; EXPRESSION; CULTURE; CYSTS	For some species of cyst-producing dinoflagellates, the sexual life cycle is well studied in laboratory cultures. Dinoflagellate blooms in stratified waters, vertical migration of vegetative cells, and the accumulation of populations within thin layers are well-documented phenomena in nature. We propose a conceptual model that places these phenomena in a functional, ecological context: vegetative cells of a dinoflagellate population display vertical migration, but at the end of the bloom, environmental or internal cues shift the cell cycle to gamete formation. Then the vertical migrations cease, and cells accumulate in a layer at the pycnocline where gametes fuse to form zygotes, which then sink to the sediment as resting cysts. We support this conceptual model with experimental and environmental evidence. (C) 2008 Elsevier B.V. All rights reserved.	[Persson, Agneta; Smith, Barry C.; Wikfors, Gary H.; Alix, Jennifer H.] Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Natl Ocean & Atmospher Adm, Milford, MA USA	National Oceanic Atmospheric Admin (NOAA) - USA	Smith, BC (通讯作者)，Univ Gothenburg, Dept Marine Ecol, Box 461, SE-40530 Gothenburg, Sweden.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514	National Oceanic and Atmospheric Administration, National Marine Fisheries Service Laboratory in Milford, Connecticut; Magnus Bergvalls foundation; Oscar and Lili Lamm's Foundation	National Oceanic and Atmospheric Administration, National Marine Fisheries Service Laboratory in Milford, Connecticut(National Oceanic Atmospheric Admin (NOAA) - USA); Magnus Bergvalls foundation; Oscar and Lili Lamm's Foundation	Most of the research was performed while Dr. Agneta Persson held a National Research Council research associate ship award at the National Oceanic and Atmospheric Administration, National Marine Fisheries Service Laboratory in Milford, Connecticut. The recent experiments were financed by a travel grant from Magnus Bergvalls foundation, and continued research in the subject by Oscar and Lili Lamm's Foundation for Scientific Research.[SS]	ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Anderson DM, 1998, SOURCE POPULATION DY; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BALDWIN J D, 1970, Primates, V11, P317, DOI 10.1007/BF01730636; Dale B., 1983, P69; De Kievit TR, 2001, APPL ENVIRON MICROB, V67, P1865, DOI 10.1128/AEM.67.4.1865-1873.2001; DELGADO M, 1998, HARMFUL ALGAE, P160; Doblin MA, 2006, HARMFUL ALGAE, V5, P665, DOI 10.1016/j.hal.2006.02.002; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; Hardman AM, 1998, ANTON LEEUW INT J G, V74, P199, DOI 10.1023/A:1001178702503; Harris G.P., 1986, PHYTOPLANKTON ECOLOG; Lewis J., 2001, lifehab life histories of microalgal species causing harmful blooms, P49; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; PROBERT L, 2001, LIFEHAB LIFE HIST MI, P57; RASMUSSEN J, 1989, J PLANKTON RES, V11, P747, DOI 10.1093/plankt/11.4.747; Rasmussen TB, 2005, J BACTERIOL, V187, P1799, DOI 10.1128/JB.187.5.1799-1814.2005; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Smith BC, 2005, J APPL PHYCOL, V17, P317, DOI 10.1007/s10811-005-4944-6; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Vogel S., 1994, LifeinMovingFluids: ThePhysicalBiologyofFlowRevisedandExpandedSecondEdition; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	25	27	31	2	17	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	OCT	2008	7	6					798	801		10.1016/j.hal.2008.04.002	http://dx.doi.org/10.1016/j.hal.2008.04.002			4	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	352RO					2025-03-11	WOS:000259515300009
J	Frommlet, JC; Iglesias-Rodriguez, MD				Frommlet, Joerg C.; Iglesias-Rodriguez, M. Debora			Microsatellite genotyping of single cells of the dinoflagellate species <i>Lingulodinium polyedrum</i> (Dinophyceae):: A novel approach for marine microbial population genetic studies	JOURNAL OF PHYCOLOGY			English	Article						dinoflagellate; genetic diversity; Lingulodinium polyedrum; microsatellites; phytoplankton; single-cell PCR	PCR AMPLIFICATION; SPRING BLOOM; GENOME SIZE; MARKERS; DIVERSITY; DNA; CYSTS; LOCI; DIFFERENTIATION; EXTRACTION	In recent years, two new approaches have been introduced in genetic studies of phytoplankton species. One is the application of highly polymorphic microsatellite markers, which allow detailed population genetic studies; the other is the development of methods that enable the direct genetic characterization of single cells as an alternative to clonal cultures. The aim of this study was to combine these two approaches in a method that would allow microsatellite genotyping of single phytoplankton cells, providing a novel tool for high-resolution population genetic studies. The dinoflagellate species Lingulodinium polyedrum (F. Stein) J. D. Dodge was selected as a model organism to develop this novel approach. The method we describe here is based on several key developments: (i) a simple and efficient DNA extraction method for single cells, (ii) the characterization of microsatellite markers for L. polyedrum, (iii) a protocol for the species identification of single cells through the analysis of partial rRNA gene sequences, and (iv) a two-step multiplex PCR protocol for the simultaneous amplification of microsatellite markers and partial rRNA gene sequences from single cells. Our protocol allowed the amplification of up to six microsatellite loci together with either the complete ITS1-5.8S-ITS2 region or a partial 18S region of the ribosomal gene of L. polyedrum from single motile cells and resting cysts. This article describes and evaluates the developed approach and discusses its significance for population genetic studies of L. polyedrum and other phytoplankton species.	[Frommlet, Joerg C.; Iglesias-Rodriguez, M. Debora] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	University of Southampton; NERC National Oceanography Centre	Iglesias-Rodriguez, MD (通讯作者)，Univ Southampton, Natl Oceanog Ctr, Waterfront Campus,European Way, Southampton SO14 3ZH, Hants, England.	dir@noc.soton.ac.uk	Frommlet, Joerg/AAD-1722-2020	Frommlet, Joerg/0000-0001-7399-3021	University of Southampton; Office of Naval Research [NOOO14-04-1-4019]; World Universities Network	University of Southampton; Office of Naval Research(United States Department of DefenseUnited States NavyOffice of Naval Research); World Universities Network	We would like to thank Peter Franks, Marcela Trevino Santa Cruz, Andrew Taylor, Leena Palekar, and Xavier Mayali for their support during sampling activities in Southern California. Additional samples from California and Sweden were kindly provided by Peter von Dassow and Marianne Ellegard, respectively. Further, we would like to thank Mark Dixon for access to genotyping facilities, as well as Mike Zubkov, Duncan Purdie, and two anonymous referees for valuable comments on the manuscript. This research was supported by the University of Southampton, a grant from the Office of Naval Research (NOOO14-04-1-4019) to M. D. I.-R., and a Student Travel Award by the World Universities Network to J.C.F.	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Phycol.	OCT	2008	44	5					1116	1125		10.1111/j.1529-8817.2008.00566.x	http://dx.doi.org/10.1111/j.1529-8817.2008.00566.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	357SN	27041708	Bronze			2025-03-11	WOS:000259866800003
J	Morgenroth, P; Rahardjo, AT; Maryunani, KA				Morgenroth, Peter; Rahardjo, A. T.; Maryunani, K. Anwar			Dinoflagellate cysts from Miocene outcrops on Java Island, Indonesia	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			English	Article						dinoflagellate cysts; Dilabidium nov gen.; Javadinium nov gen.; Miocene; Indonesia		As part of a study on the stratigraphic distribution of dinoflagellate cysts in the Tertiary of Indonesia three Miocene surface sections have been investigated in West- and Central Java. The sections are exposed in rivers and are easily accessible during the dry season. The sections cover possibly Lower Miocene, confirmed Middle Miocene and Upper Miocene strata and almost all samples collected contain abundant dinoflagellate cysts. 29 species are described, of which 15 are new from the genera Achomosphaera, Dilabidinium, Edwardsiella, Hystrichosphaeropsis, Javadinium, Lejeunecysta, Operculodinium, Spiniferites and, possibly, Baltisphaeridium and Erymnodinium. The new genera Dilabidinium and Javadinium are established. The study has also resulted in the identification of stratigraphically important species which can be used for correlations of Miocene sediments in the area.	[Rahardjo, A. T.; Maryunani, K. Anwar] Inst Technol Bandung, Dept Geol, Bandung 40132, Indonesia	Institute Technology of Bandung	Morgenroth, P (通讯作者)，Trienendorfer Str 100, D-58300 Wetter, Germany.	pawmorg@yahoo.com; anwar@gc.itb.ac.id			Lembaga Ilmu Pengetahuan Indonesia (Indonesian Institute of Sciences), Jakarta	Lembaga Ilmu Pengetahuan Indonesia (Indonesian Institute of Sciences), Jakarta	Peter MORGENROTH would like to take this opportunity to thank Lembaga Ilmu Pengetahuan Indonesia (Indonesian Institute of Sciences), Jakarta, for supporting this study.	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A. S., 1959, Geological Magazine, V96, P329; SARJEANT W A S, 1970, Grana, V10, P74; STOVER LE, 1978, GEOSCIENCE SERIES, V15; Strauss Christoph, 1992, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V73, P159; VANDENBRINK H, 2001, BERITA SEDIMENTOLOGI, V16; VERSTEEGH GJM, 1995, REV PALAEOBOT PALYNO, V85, P213, DOI 10.1016/0034-6667(94)00127-6; WALL D., 1967, PALAEONTOLOGY, V10, P95; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; Williams G., 1975, OFFSHORE GEOLOGY E C, V2, P107; Williams G.L., 1985, P847; WILLIAMS GL, 1978, AM ASS STRATIGR PALY, V2; WILLIAMS GL, 1966, B BRIT MUS NAT HI S2; WRENN JH, 1988, GEOL SOC AM MEM, V169	51	2	2	0	5	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	2194-900X	2509-839X		PALAEONTOGR ABT B	Palaeontogr. Abt. B-Palaophytol.	OCT	2008	278	4-6					111	137		10.1127/palb/278/2008/111	http://dx.doi.org/10.1127/palb/278/2008/111			27	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	363CP					2025-03-11	WOS:000260243800002
J	Vilanova, I; Guerstein, GR; Akselman, R; Prieto, AR				Vilanova, Isabel; Guerstein, G. Raquel; Akselman, Rut; Prieto, Aldo. R.			Mid- to Late Holocene organic-walled dinoflagellate cysts from the northern Argentine shelf	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Holocene; dinoflagellate cysts; northern Argentine inner shelf; sea-level; coastal evolution; palaeoenvironments	SEA-LEVEL FLUCTUATIONS; BAHIA-BLANCA ESTUARY; CONTINENTAL-SHELF; BUENOS-AIRES; PLATA RIVER; EVOLUTION; SEDIMENTS; REGIMES; COAST	A Mid- to Late Holocene dinocyst record from the northern inner shelf of Argentina is described. It is analyzed with respect to the distribution of modern dinocysts, other Holocene records from the Buenos Aires province and the biogeographic distribution of planktonic dinocysts and their motile equivalents. Between ca. 5360 and 3300 C-14 yr BP the low diversity and abundance of the cyst assemblages can be related to a restricted littoral subtidal environments. After ca. 3300 C-14 yr BP a major change is characterized by an increase in dinocyst abundance, indicating a normal inner neritic environment. The dominance of Operculodindium centrocarpum at some levels suggests some influence of continental shelf waters whereas the higher abundances of dinocysts from heterotrophic taxa e.g. Protoperidinium stellatum, Votadinium calvum, V. spinosurn in other levels reflects a more inshore-coastal water influence with increased nutrient availability. Both assemblages are consistent with the present day transitional coastal-neritic conditions, suggesting that they were established after ca. 3300 C-14 yr. These inferences supplement those based on other proxies, reflecting sea-level decrease and the coastal geomorphological evolution post ca. 5360 C-14 yr BP. (C) 2008 Elsevier B.V. All rights reserved.	[Vilanova, Isabel; Prieto, Aldo. R.] Univ Nacl Mar Plata, Lab Paleoecol & Palinol, RA-7600 Mar Del Plata, Argentina; [Vilanova, Isabel; Guerstein, G. Raquel; Prieto, Aldo. R.] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina; [Guerstein, G. Raquel] Univ Nacl Sur, INGEOSUR, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Akselman, Rut] Inst Nacl Invest & Desarrollo Pesquero, INIDEP, RA-7600 Mar Del Plata, Argentina	National University of Mar del Plata; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); National Fisheries Research & Development Institute (INIDEP)	Vilanova, I (通讯作者)，Univ Nacl Mar Plata, Lab Paleoecol & Palinol, Funes 3250, RA-7600 Mar Del Plata, Argentina.	ivilanov@mdp.edu.ar		vilanova, isabel/0000-0002-8327-5207	CONICET [PIP 6416]; Agencia Nacional de Investigacion Cientifica y Tecnologica [PICT 26057]; Universidad Nacional del Sur [PGI 24/H079]; Universidad Nacional de Mar del Plata [Exa 349/06]	CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Agencia Nacional de Investigacion Cientifica y Tecnologica; Universidad Nacional del Sur; Universidad Nacional de Mar del Plata(National University of La Plata)	We are most grateful to Dr. Rex Harland for going through the material, making exhaustive revision of the language and helpful suggestions. We would like to thank Karin Zonneveld and to an anonymous reviewer for their useful comments, and to Raul Guerrero for providing the oceanographic data. This research was financed by CONICET PIP 6416, Agencia Nacional de Investigacion Cientifica y Tecnologica PICT 26057, Universidad Nacional del Sur PGI 24/H079 and Universidad Nacional de Mar del Plata Exa 349/06.	AKSELMAN R, 1987, Boletim do Instituto Oceanografico, V35, P17; Akselman R., 1998, HARMFUL ALGAE, P122; AKSELMAN R, 1999, LIBRO RESUMENES AMPL, V1, P323; [Anonymous], 1999, 14 C GEOL ARG OCT 19; BALECH E, 1988, PUBLICACION ESPECIAL, V1; Borel CM, 2006, AMEGHINIANA, V43, P399; BOREL CM, 2006, GEOACTA, V31, P23; Borromei AM, 2007, AMEGHINIANA, V44, P161; CAPITANIO F, 1988, SEM CURS OC BIOL FCE; Carreto J.I., 1985, P147; Carreto J. 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De. la Asoc. oN. Geol. ogica Argent., V56, P51; Violante RA, 2004, QUATERN INT, V114, P167, DOI 10.1016/S1040-6182(03)00036-3; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	49	9	9	0	4	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	OCT	2008	152	1-2					11	20		10.1016/j.revpalbo.2008.03.006	http://dx.doi.org/10.1016/j.revpalbo.2008.03.006			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	373AE					2025-03-11	WOS:000260942600002
J	Kodrans-Nsiah, M; de Lange, GJ; Zonneveld, KAF				Kodrans-Nsiah, Monika; de Lange, Gert J.; Zonneveld, Karin A. F.			A natural exposure experiment on short-term species-selective aerobic degradation of dinoflagellate cysts	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; organic matter; oxygen; taphonomy	ORGANIC-CARBON ACCUMULATION; SEA-SURFACE CONDITIONS; EASTERN MEDITERRANEAN SAPROPELS; BENGUELA UPWELLING SYSTEM; MARINE-SEDIMENTS; NORTHERN BELGIUM; SOUTH ATLANTIC; ANOXIC BASINS; S1 SAPROPEL; ARABIAN SEA	Although studies have shown that organic-walled dinoflagellate cysts (dinocysts) can undergo species-selective aerobic degradation, the alteration rate of this process is not known. Here we provide data on the decay rates of dinocyst from a degradation experiment in which sediment samples of Holocene age from (a) anoxic Namibian shelf and (b) anoxic part of the eastern Mediterranean S1 sapropel have been exposed to oxic and anoxic conditions in natural environments. The two types of sediment were stored in bags composed of a dialyse membrane that allows oxygen penetration but prevents bacterial exchange. Sediment bags were placed in open containers connected to sediment traps and moored for 15 months in anoxic brines and oxic intermediate waters of the Urania and Bannock Basins areas. Within the short experimental time (15 months), exposure to oxygenated waters resulted in a 24% to 57% reduction in concentration of cysts attributable to Brigantedinium spp. and Echinidinium granulatum. Other taxa such as Spiniferites spp., Lingulodinium machaerophorum and Echinidinium spp. appear to be less sensitive. A slight increase in cyst concentration is observed for Nematosphaeropsis labyrinthus, Echinidinium aculeatum, Operculodinium israelianum, and Impagidinium aculeatum, indicating that these cyst species are more resistant to aerobic degradation. Exposure to anoxic conditions has not lead to detectable differences between initial and exposed composition and concentration. Our study is the first to document that species-selective degradation of dinocysts in oxygenated natural environments is a rapid process that changes considerably dinocyst concentrations and assemblages. (C) 2008 Elsevier B.V. All rights reserved.	[Kodrans-Nsiah, Monika; Zonneveld, Karin A. F.] Fachbereich 5 Geowissensch, D-28334 Bremen, Germany; [de Lange, Gert J.] Fac Geosci, Dept Earth Sci Geochem, NL-3584 CD Utrecht, Netherlands	University of Bremen	Kodrans-Nsiah, M (通讯作者)，Fachbereich 5 Geowissensch, Postfach 330440, D-28334 Bremen, Germany.	mknsiah@uni-bremen.de	De Lange, Gert/B-9639-2014	De Lange, Gert/0000-0002-9420-3022	German Science Foundation (DFG) [EUROPROX]	German Science Foundation (DFG)(German Research Foundation (DFG))	This study was carried out as part of the German Science Foundation (DFG) grant EUROPROX.	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Palaeobot. Palynology	OCT	2008	152	1-2					32	39		10.1016/j.revpalbo.2008.04.002	http://dx.doi.org/10.1016/j.revpalbo.2008.04.002			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	373AE					2025-03-11	WOS:000260942600004
J	Aleksandrova, GN; Zaporozhets, NI				Aleksandrova, G. N.; Zaporozhets, N. I.			Palynological characteristics of Upper Cretaceous and Paleogene deposits on the West of the Sambian Peninsula (Kaliningrad region), Part 2	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Campanian; Maastrichtian; Paleocene; Eocene; biostratigraphy; dinocysts; spores and pollen	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; NORTH-SEA; DINOCYST ZONATION; EOCENE; STRATIGRAPHY; ASSEMBLAGES; BASIN; URALS	The results of studying dinocysts in the Upper Cretaceous-Lower Paleogene succession of the Kaliningrad region are considered. Distinguished in the succession are seven biostratigraphic units in the rank of the Palaeohystrichophora infusorioides, Chatangiella vnigrii, Cerodinium diebelii, Alisocysta margarita, Deflandrea oebisfeldensis, Areosphaeridium diktyoplokum, and Rhombodinium perforatum beds and one Charlesdowniea clathrata angulosa Zone. The Lyubavas Formation has not been distinguished on the west of the Sambian Peninsula. Ages of the Sambia, Alka, and Prussian formations are verified.	[Aleksandrova, G. N.; Zaporozhets, N. I.] Russian Acad Sci, Inst Geol, Moscow V71, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Aleksandrova, GN (通讯作者)，Russian Acad Sci, Inst Geol, Moscow V71, Russia.		Galina, Aleksandrova/AAW-8215-2020		Russian Foundation for basic Research [05-05-64910, NSh-1615-2003.5]	Russian Foundation for basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	We are grateful to N. P. Lukashina and A. D. Krylov (Institute of Oceanology RAS, Atlantic Division, Kaliningrad) who kindly donated samples for this study. Determination of nannofossils from Borehole 1P by O. B. Dmitrenko (Institute of Oceanology RAS, Moscow) is highly appreciated. We also thank M. A. Akhmetiev, V. N. Beniamovski, and A. I. Yakovleva (GIN RAS) for fruitful discussion of our results and manuscript. Advices and comments of reviewers N. K. Lebedeva and V. A. Zakharov were very valuable. The work was supported by the Russian Foundation for basic Research, project 05-05-64910 and grant NSh-1615-2003.5.	Akhmetiev M.A., 2003, Byulleten' Moskovskogo Obshchestva Ispytatelei Prirody Otdel Geologicheskii, V78, P40; ANDREEVAGRIGORO.AS, 1991, THESIS KIEV; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; BaltaKis V. I., 1966, T INSITITUTA GEOLOGI, V3, P277; BERGGREN WA, 1954, SEPM SPEC PUBL, V54, P1; Blow W.H., 1969, Proceedings of the International Conference on Planktonic Microfossils, V1, P199; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Chateauneuf J.-J., 1978, Bull. Bur. Rech. Geol. Min. 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Geol., P30; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; Kothe A., 1990, GEOL JB A, V118, P3; Lebedeva NK, 2005, STRATIGR GEO CORREL+, V13, P310; Luterbacher HP., 2004, GEOLOGIC TIME SCALE, P384; Marinov V.A., 2002, Byulleten' Moskovskogo Obshchestva Ispytatelei Prirody Otdel Geologicheskii, V77, P26; Martini E., 1971, P 2 PLANKT C ROM 197, P739; MUDGE DC, 1994, MAR PETROL GEOL, V11, P166, DOI 10.1016/0264-8172(94)90093-0; NIKOLAEVA IA, 2006, ZONAL STRATIGRAPHY P, P172; Ogg J.G., 2004, GEOLOGIC TIME SCALE, P344; Olfer'ev AG, 2003, STRATIGR GEO CORREL+, V11, P172; Olfer'ev AG, 2002, STRATIGR GEO CORREL+, V10, P270; Oreshkina TV, 2004, NEUES JAHRB GEOL P-A, V234, P201; ORLOV YA, 1963, FUNDAMENTALS PALEONT; Perch-Nielsen K., 1985, P329; Powell A.J., 1992, P155; Prince IM, 1999, REV PALAEOBOT PALYNO, V105, P143, DOI 10.1016/S0034-6667(98)00077-3; Robaszynski F., 1985, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V9, P1; Robaszynski F., 1984, Revue de Micropaleontologie, V26, P145; Schioler P, 1997, MAR MICROPALEONTOL, V31, P65, DOI 10.1016/S0377-8398(96)00058-8; SCHIOLER P, 1993, REV PALAEOBOT PALYNO, V78, P321, DOI 10.1016/0034-6667(93)90070-B; Schulz M.G., 1979, GEOLOGISCHES JB A, V47, P1; SISSINGH W, 1977, Geologie en Mijnbouw, V56, P37; Slimani Hamid, 2001, Geologica et Palaeontologica, V35, P161; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; Strelnikova N.I., 1978, P57; STRELNIKOVA NI, 1992, PALEOGENE DIATOMACEO; VASILEVA O. N., 1990, Palynology and stratigraphy of marine sediments of the Paleogene of the Southern Trans-Urals; VASILEVA ON, 2004, EZHEGODNIK 2004, P14; VASILEVA ON, 2000, EZHEGODNIK 1999, P11; Wind F., 1979, Deep drilling results in the Atlantic Ocean: continental margins and paleoenvironment, P123; WIND FH, 1983, INITIAL REP DEEP SEA, V71, P551; YAKOVLEVA AI, 2003, REV PALAEOBOT PALYNO, V123, P185; Zaporozhets N. I., 1993, STRATIGR GEOL CORREL, V1, P117; Zaporozhets NI, 1999, STRATIGR GEOL CORREL, V7, P161; Zaporozhets NI, 2001, STRATIGR GEO CORREL+, V9, P603; ZAPOROZHETS NI, 1998, GEOLOGIC BIOTIC EV 2, P23	52	43	52	0	9	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0869-5938			STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	OCT	2008	16	5					528	539		10.1134/S0869593808050067	http://dx.doi.org/10.1134/S0869593808050067			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	356HQ					2025-03-11	WOS:000259769700006
J	Kuz'mina, OB; Volkova, BS				Kuz'mina, O. B.; Volkova, B. S.			Palynostratigraphy of Oligocene-Miocene continental deposits in Southwestern Siberia	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						pollen; spores; dinocysts; Oligocene; Miocene; West Siberia; palynostratigraphy	PALEOGENE; MARINE	Data on spores, pollen, and dinoflagellate cysts studied in composite section of Oligocene-Miocene deposits in southern part of West Siberia are presented. Eleven biostratigraphic units distinguished in the section are ranked as palynozones and beds with palynological assemblages. Palynological data substantiate age of deposits and specify ranges and boundaries of palynozones. Based on dinocyst assemblages first studied in sediments of the Zhuravka and Abrosimovo horizons (upper Oligocene, lower Miocene), the Pseudokomewuia Beds are included into local stratigraphic scheme. According to results of comparative analysis, similar and distinctive features of Oligocene-Miocene dinocyst assemblages from West Siberia, China and North America are elucidated. Based on palynological data, the local stratigraphic scheme of higher resolution is suggested for subdivision of Oligocene and Miocene deposits in southern part of West Siberia (Baraba and Kulunda lithofacies regions).	[Kuz'mina, O. B.; Volkova, B. S.] Russian Acad Sci, Inst Oil & Gas Geol & Geophys, Siberian Branch, Novosibirsk, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences	Kuz'mina, OB (通讯作者)，Russian Acad Sci, Inst Oil & Gas Geol & Geophys, Siberian Branch, Novosibirsk, Russia.		Kuzmina, Olga/I-9547-2018		Russian Foundation for Basic Research [08-05-00344-a]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	We are grateful to G.N. Aleksandrova, from the Laboratory of Paleofloristics, GIN RAS, for valuable recommendations and assistance during preparation of manuscript. The work was supported by the Russian Foundation for Basic Research, project no. 08-05-00344-a.	Akhmet'ev MA, 2004, STRATIGR GEO CORREL+, V12, P58; Akhmet'ev MA, 2001, STRATIGR GEO CORREL+, V9, P373; [Anonymous], 2001, UNIFIED REGIONAL STR; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BENIAMOVSKI VN, 2002, B MOSK O VA ISPYT PR, V77, P28; Boitsova E.P., 1973, MARINE CONTINENTAL P, P78; BOITSOVA EP, 1966, P 2 INT PAL C METH P, P236; BOITSOVA EP, 1973, PALINOLOGIYA KAINOFI, P42; BOITSOVA EP, 1968, T VSEGEI, V143, P37; DARGEVICH VA, 1969, GEOLOGY PLACERS SO W, P32; [Гнибиденко З.Н. Gnibidenko Z.N.], 2006, [Геология и геофизика, Geologiya i geofizika], V47, P762; Grichuk VP., 1948, ANAL FOSSIL POLLEN S; HE C, 1980, NANJ I GEOL PAL AC S, P11; ILENOK LL, 1989, CENOZOIC SIBERIA NE, P75; KRASHENINNIKOV VA, 1996, GEOLOGIC BIOTIC EV 1; KULKOVA IA, 1998, MIKROFOSSILII STRATI, P25; KULKOVA IA, 1994, STRATIGR GEOL CORREL, V2, P302; Kuz'mina OB, 2004, DOKL EARTH SCI, V394, P14; Kuz'mina OB, 2003, GEOL GEOFIZ, V44, P348; Kuzmina, 2001, NOVOSTI PALEONTOLOGI, P135; KUZMINA OB, 2008, NOVOSTI PAL IN PRESS; NIKITIN VP, 1999, THESIS NITS OIGGIM S; NIKITIN VP, 2006, PALEOCARPOLOGY PALEO; Panova L.A., 1971, CENOZOIC FLORAS SIBE, P40; Panova L.A., 1990, PRACTICAL PALYNOSTRA; PANOVA LA, 1967, THESIS VSEGEL LENING; VASILEVA ON, 1990, THESIS IGIG URO AN S; Volkova VS, 2005, GEOL GEOFIZ, V46, P60; Volkova VS, 2002, GEOL GEOFIZ, V43, P1017	29	12	12	0	2	PLEIADES PUBLISHING INC	MOSCOW	PLEIADES PUBLISHING INC, MOSCOW, 00000, RUSSIA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	OCT	2008	16	5					540	552		10.1134/S0869593808050079	http://dx.doi.org/10.1134/S0869593808050079			13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	356HQ					2025-03-11	WOS:000259769700007
J	Picot, L; Becker, D; Cavin, L; Pirkenseer, C; Lapaire, F; Rauber, G; Hochuli, PA; Spezzaferri, S; Berger, JP				Picot, Laurent; Becker, Damien; Cavin, Lionel; Pirkenseer, Claudius; Lapaire, Frederic; Rauber, Gaetan; Hochuli, Peter A.; Spezzaferri, Silvia; Berger, Jean-Pierre			Sedimentology and paleontology of Rupelian coast paleoenvironments in the Swiss Jura Molasse	SWISS JOURNAL OF GEOSCIENCES			French	Article; Proceedings Paper	Conference on Modern Methods in Structural Geology and Tectonics held in honor of Martin Burkhard	MAY 11-13, 2007	Neuchatel, SWITZERLAND			foraminiferes; ostracodes; poissons; Rupelien; UMM rhenane; Molasse du Jura	UPPER RHINE GRABEN; MAINZ BASIN; PALEOGEOGRAPHY; OLIGOMIOCENE; TERTIARY; EXAMPLE; MIOCENE; EOCENE; SOUTH; URG	Aim. To analyse the marine influences of the Rhenish sea in the distal part of the Swiss Molasse Basin (Jura Molasse) during the Early Oligocene, in order to reconstruct the palaeoenvironmental and the palaeogeographical evolution. Location and geological setting. In the Jura Molasse, the Rhenish sea deposits are mainly preserved in three sedimentary basins: Laufen, Delemont and Ajoie. They belong to the following stratigraphical groups of the Jura Molasse: Conglomerats de Porrentruy, Septarienton and Meeressand. Methods. The sedimentological series have been studied in detail for stratigraphy, sedimentology and palaeontology. Three stratigraphical columns are proposed for the Laufen, Delemont and Ajoie basins, corresponding to the southern extension of Rhenish sea in the Swiss Jura. Various fossil groups including foraminifers, ostracods, fishes, dinoflagellate cysts, spores and pollens were studied in terms of taxonomy, biostratigraphy and palaeoecology. These studies lead to reconstruct Oligocene palaeoenvironments and their evolution during the time interval NP21 to base NP25 (corresponding to 34.4-25.0 My). Results. Although three transgression-regression cycles are known in the Rhine Graben, only the first two cycles are recorded in the Ajoie basin and only one in the Delemont and the Laufen basins. New biostratigraphical data allow the dating of the different marine incursions in the Swiss Jura basins. In Ajoie basin, the first recorded transgression corresponds to the biozones top NP21 to base NP22. The second one, the global Rupelian transgression, synchronically invaded the whole northern Swiss Jura area at the top part of NP22-base NP23. The regression is clearly diachronous, occuring during the top part of NP23, in two directions, westward and northward. In the Ajoie basin, the Rhenish sea remained until NP24 to base NP25. Main conclusions. The palaeobathymetrical estimations of the global Rupelian transgression based on ostracods, foraminifers and fishes correspond to the interval 0-50 m. During the considered time interval of this study (34.4-25.0 My), fossil assemblages can be very different, showing a high degree of endemism (especially for ostracods). New palaeogeographical data suggest a possible connection between the south of the Rhine Graben and the Bresse Graben, and show local drainage directions of fluviatile systems. In the Jura, there is no evidence for a third transgression.	[Picot, Laurent; Becker, Damien; Rauber, Gaetan] Republ & Canton Jura, Off Culture, Sect Archeol & Paleontol, CH-2900 Porrentury, Switzerland; [Cavin, Lionel] Museum Hist Nat, CH-1211 Geneva 6, Switzerland; [Pirkenseer, Claudius; Spezzaferri, Silvia; Berger, Jean-Pierre] Univ Fribourg, Dept Geosci Geol & Paleontol, CH-1700 Fribourg, Switzerland; [Lapaire, Frederic] Republ & Canton Jura, Off Eaux & Protect Nat, CH-2882 St Ursanne, Switzerland; [Hochuli, Peter A.] Univ Zurich, Inst Palaeontol, CH-8006 Zurich, Switzerland; [Hochuli, Peter A.] Univ Zurich, Museum Palaeontol, CH-8006 Zurich, Switzerland	University of Fribourg; University of Zurich; University of Zurich	Becker, D (通讯作者)，Republ & Canton Jura, Off Culture, Sect Archeol & Paleontol, CH-2900 Porrentury, Switzerland.	damien.becker@palaeojura.ch	Cavin, Lionel/AAZ-8120-2021; PICOT, Laurent/N-6179-2014					[Anonymous], 2005, INT J EARTH SCI, DOI DOI 10.1007/s00531-005-0479-y; [Anonymous], GEOLOGIE MEDITERRANE; [Anonymous], ABHANDLUNGEN GEOLOGI; [Anonymous], GEOLOGCIA CARPATHICA; [Anonymous], 1980, Geology of Switzer- land, a Guide Book: Schweiz Geologica Kommis- sione; [Anonymous], SPECIAL PUBLICATION; [Anonymous], 1980, Geology of Switzer- land, a Guide Book: Schweiz Geologica Kommis- sione; [Anonymous], 1984, PAL ONTOL KURSB; Athersuch J., 1989, SYNOPSES BRIT FAUNA, V43, DOI [10.1017/s0025315400059178, DOI 10.1017/S0025315400059178]; Becker D, 2004, COUR FOR SEKENBG, V249, P1; Becker D, 2002, GEOBIOS-LYON, V35, P89, DOI 10.1016/S0016-6995(02)00012-8; Becker D., 2003, GEOFOCUS, V9, P1; Becker Damien, 2004, Revue de Paleobiologie Volume Special, V9, P179; Berger J.P., 1996, Neues Jahrbuch Geol. 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Geosci.	SEP	2008	101	2					483	513		10.1007/s00015-008-1275-z	http://dx.doi.org/10.1007/s00015-008-1275-z			31	Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	357BI		Bronze			2025-03-11	WOS:000259820900018
J	González, C; Dupont, LM; Mertens, K; Wefer, G				Gonzalez, Catalina; Dupont, Lydie M.; Mertens, Kenneth; Wefer, Gerold			Reconstructing marine productivity of the Cariaco Basin during marine isotope stages 3 and 4 using organic-walled dinoflagellate cysts	PALEOCEANOGRAPHY			English	Article							INTERTROPICAL CONVERGENCE ZONE; RAPID CLIMATE CHANGES; NORTH-ATLANTIC; TROPICAL ATLANTIC; VEGETATION RESPONSE; SURFACE SEDIMENTS; CARIBBEAN SEA; EL-NINO; VARIABILITY; CYCLE	An organic-walled dinoflagellate cyst analysis was carried out on sediment core MD03-2622, retrieved from the Cariaco Basin. The core comprises the 73-30 ka interval. Down core changes in cyst abundance, accumulation rate, and composition of cyst assemblages were used to identify climatic and oceanographic changes at orbital and millennial time scales in this near-equatorial seasonal upwelling area. Throughout the sequence, dinoflagellate cyst assemblages were dominated by heterotrophic dinocysts (mainly Brigantedinium spp.), with the exception of four autotrophic-dominated (mainly Spiniferites ramosus) intervals around 58, 53, 46, and 37 ka. At orbital time scales, changes in the dinoflagellate productivity seem to follow low-latitude insolation, with the highest productivities coinciding with maximum February insolation (47-38 ka). At millennial scales, cyst accumulation rates appeared to coincide with Dansgaard-Oeschger (D-O) variability, with significant increments occurring during warm interstadials. The opposite was true during stadials. Short periods of high nutrient availability and stratified conditions followed Heinrich events H4, H5, H5a, and H6 and concurred with enhanced river runoff. Spectral analyses confirm the existence of these and other higher-frequency periodicities and support the idea of a tightly coupled terrestrial/marine and tropical/high-latitude climate system during the last glacial period.	[Gonzalez, Catalina; Dupont, Lydie M.; Wefer, Gerold] Univ Bremen, MARUM, D-28369 Bremen, Germany; [Mertens, Kenneth] Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, B-9000 Ghent, Belgium	University of Bremen; Ghent University	González, C (通讯作者)，Univ Bremen, MARUM, Leobener Str, D-28369 Bremen, Germany.	catalina@uni-bremen.de; dupont@uni-bremen.de; kenneth.mertens@ugent.be; gwefer@marum.de	Mertens, Kenneth/AAO-9566-2020; Arango, Catalina/D-2308-2011; Wefer, Gerold/S-2291-2016; Mertens, Kenneth/C-3386-2015	Wefer, Gerold/0000-0002-6803-2020; Dupont, Lydie/0000-0001-9531-6793; Mertens, Kenneth/0000-0003-2005-9483; Gonzalez Arango, Catalina/0000-0003-1709-4405	European Union Programme of High Level Scholarships for Latin America [E04D047330CO]; Deutsche Akademische Austausch Dienst (DAAD)	European Union Programme of High Level Scholarships for Latin America(European Union (EU)); Deutsche Akademische Austausch Dienst (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD))	The authors thank Gerald Haug and Larry Peterson for providing the sediment samples and for their valuable comments on an early version of the manuscript. Karin Zonneveld is gratefully acknowledged for the training she provided on dinoflagellate identification and ecology during the early stage of this project. We are grateful to G. Dickens, H. Brinkhuis, U. Martens, and an anonymous reviewer for their constructive criticism and valuable suggestions. This work was supported by the Programme Al beta an - the European Union Programme of High Level Scholarships for Latin America (scholarship E04D047330CO) and the Deutsche Akademische Austausch Dienst (DAAD). Data are available in Pangaea (http://www.pangaea.de). This is MARUM publication MARUM0589.	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J	Murgese, DS; De Deckker, P; Spooner, MI; Young, M				Murgese, Davide S.; De Deckker, Patrick; Spooner, Michelle I.; Young, Martin			A 35,000 year record of changes in the eastern Indian Ocean offshore Sumatra	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						last glacial maximum; deep chlorophyll maximum; barrier layer; Java upwelling system; monsoon; organic carbon; foraminifera; dinoflagellates	WALLED DINOFLAGELLATE CYSTS; SEA BENTHIC FORAMINIFERA; LAST GLACIAL MAXIMUM; WESTERN EQUATORIAL PACIFIC; SOUTH CHINA SEA; PLANKTONIC-FORAMINIFERA; SURFACE SEDIMENTS; LATE PLEISTOCENE; HIGH-PRODUCTIVITY; MARINE-SEDIMENTS	We have examined the upper 276 cm of deep-sea core BAR9403 taken at a water depth of 2034 m offshore the southern portion of Sumatra in the eastern Indian Ocean using several micropalaeontological proxies. Faunal counts and stable isotopes of oxygen and carbon of planktic and benthic foraminifers, as well as floral counts of dinoflagellates were obtained to reconstruct conditions in the oceans over the last 35,000 years. At times, we found that when benthic foraminifers indicate high organic content values at the bottom of the ocean this is not paralleled by high productivity signals at the sea surface, but instead must relate to changes in bottom-water circulation as a result of slower water circulation. The marine isotopic stages [MIS] 3-1 are clearly differentiated by benthic and foraminiferal assemblages as well as dinoflagellates and their cysts. MIS 3 is characterised by a much sharper [than today] thermocline that was closer to the sea surface and by the absence of a low-salinity 'barrier layer' which today results from high monsoonal rains. The absence of the latter persisted during the last glacial period [MIS 2] when bottom circulation must have been reduced and high percentages of organic matter occurred on the sea floor combined with low dissolved-oxygen levels. The deglaciation is marked by a change in salinity at the sea surface as seen by the dinoflagellates and planktic foraminifers and progressive alteration of the thermocline was detected by foraminifers suggesting a less productive deep chlorophyll maximum in contrast with MIS 3 and 2. Monsoonal activity commenced around 15,000 cal years ago and was well established 2000 years later. The Holocene is marked by a significant increase in river discharge to the ocean, pulsed by the delivery of organic matter to the sea floor, despite overall oligotrophic conditions at and near the sea surface induced by a permanent low-salinity cap. We did not identify obvious and persistent upwelling conditions offshore Sumatra for the last 35,000 years. (C) 2008 Elsevier B.V. All rights reserved.	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WOCE Newsl, V24, P25; YAN XH, 1992, SCIENCE, V258, P1643, DOI 10.1126/science.258.5088.1643; Yokoyama Y, 2000, NATURE, V406, P713, DOI 10.1038/35021035; Yokoyama Y, 2001, PALAEOGEOGR PALAEOCL, V165, P281, DOI 10.1016/S0031-0182(00)00164-4; YOUNG MD, 2006, DISTRIBUTION ORGANIC; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1; Zonneveld KAF, 2000, DEEP-SEA RES PT II, V47, P2229, DOI 10.1016/S0967-0645(00)00023-0	98	20	22	1	17	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	AUG 11	2008	265	3-4					195	213		10.1016/j.palaeo.2008.06.001	http://dx.doi.org/10.1016/j.palaeo.2008.06.001			19	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	342YC					2025-03-11	WOS:000258818500003
J	Gedl, P; Garecka, M				Gedl, Przemyslaw; Garecka, Malgorzata			Middle-Late Eocene phytoplankton from marl intraclasts (Podhale Paleogene, Inner Carpathians, Poland): biostratigraphic and paleoenvironmental implications	GEOLOGICA CARPATHICA			English	Article						Eocene; Carpathians; Poland; Central Carpathian Paleogene; Podhale Basin; paleogeography; biostratigraphy; calcareous nannoplankton; dinoflagellate cysts	CALCAREOUS NANNOPLANKTON; OLIGOCENE TRANSITION; DINOFLAGELLATE CYSTS; MAGURA NAPPE; ZONATION; FOLUSZ; BASIN	Organic-walled dinoflagellate cysts and calcareous nannoplankton are described from marly intraclasts found in submarine slump deposits within the Lower Oligocene Szaflary Beds exposed in the Lesnica Stream. Their Middle and Late Eocene age implies that the investigated deposits are coeval with the basal deposits of the Podhale Paleogene succession. These Middle and Upper Eocene marl intraclasts were eroded and transported into the flysch basin during the Early Oligocene. They represent the sediments deposited in the northern part of the Podhale Basin that is not exposed in recent times. Paleoenvironmental analysis of microfossils suggests sea-level oscillations during late Middle-Late Eocene (Bartonian-Priabonian) with its maximum during the earliest Late Eocene (earliest Priabonian). A drop of sea surface temperature during Late Eocene is also suggested on the basis of high-latitude microfossil occurrence.	[Gedl, Przemyslaw] Polish Acad Sci, Cracow Res Ctr, Inst Geol Sci, PL-31002 Krakow, Poland; [Garecka, Malgorzata] Polish Geol Inst, Carpathian Branch, PL-31560 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Geological Institute - National Research Institute	Gedl, P (通讯作者)，Polish Acad Sci, Cracow Res Ctr, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl; malgorzata.garecka@pgi.gov.pl	Garecka, Małgorzata/X-1531-2018					Alexandrowicz S. 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Carpath.	AUG	2008	59	4					319	331						13	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	346ZQ					2025-03-11	WOS:000259108500004
J	Figueroa, RI; Bravo, I; Garcés, E				Figueroa, Rosa Isabel; Bravo, Isabel; Garces, Esther			The significance of sexual versus asexual cyst formation in the life cycle of the noxious dinoflagellate <i>Alexandrium peruvianum</i>	HARMFUL ALGAE			English	Article						Alexandrium peruvianum; cysts; nitrates; phosphates; sexuality; life cycle	SP-NOV DINOPHYCEAE; GYMNODINIUM-CATENATUM; GONYAULAX-TAMARENSIS; RESTING CYSTS; MATING-TYPE; REPRODUCTION; TAYLORI; ENCYSTMENT; TAMUTUM	Alexandrium peruvianum (Balech et Mendiola) is a noxious phototrophic marine dinoflagellate. During the life cycle of this species, two kinds of cysts are produced: resting cysts, which are long-lasting and double-walled, and temporary cysts, which are short-lasting and thin-walled. In addition, short-lasting, but resting-like cysts can also be formed. Although it is crucial to identify sexual events in a dinoflagellate population, sexual and asexual cysts are morphologically very similar in this species. Therefore, we studied the complete life cycle and the nature of the cyst-like stages formed after individual isolation of specimens and crossing of clonal cultures established from germination of wild resting cysts. Asexual division in A. peruvianum takes place either in the motile stage by sharing of the theca (desmoschisis), or inside a vegetative cyst (temporary cyst), from which two, or at times four or six naked daughter cells can originate. The daughter cells completely synthesize new cell walls (eleutheroschisis). Sexuality was confirmed by the presence of fusing gamete pairs and longitudinally biflagellated planozygotes after out-crossing of compatible clonal strains. However, the clonal cultures had low levels of self-compatibility, since a flow cytometry analysis showed that synchronized self-crosses produced few zygotes (< 5%). After isolation of individual cells, it was proved that the fate of the planozygotes depended on the nutritional status of the isolation media. Most of the planozygotes isolated to replete medium (L1) divided, whereas in medium lacking nitrates (L-N) or phosphates (L-P) they formed temporary, thin-walled cysts. Temporary cysts formed in L1 were always uninucleated and gave rise to one cell, while those formed in L-N or L-P produced 1-6 small cells. In addition, resting cysts were formed in culture, but never after individual planozygote isolation. Resting cysts were uninucleated and needed maturation time before entering dormancy. The resting cysts were considered sexual products, since longitudinally biflagellate germlings were liberated after germination in all cases studied. Mature resting cysts (52.3 +/- 3.0 mu m) had a dormancy period of 1-3 months, whereas temporary asexual cysts (32.5 +/- 5.4 mu m) germinated in less than 7 days. (c) 2008 Elsevier B.V. All rights reserved.	[Figueroa, Rosa Isabel; Garces, Esther] CSIC, Inst Ciencias Mar, Barcelona, Spain; [Bravo, Isabel] Inst Espanol Oceanografia, Vigo 36200, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，CSIC, Inst Ciencias Mar, Barcelona, Spain.	figueroa@icm.csic.es	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011	Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X; Garces, Esther/0000-0002-2712-501X				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], IOC TAXONOMIC REFERE; [Anonymous], 1997, ADV MAR BIOL; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; FIGUEROA RI, 2005, THESIS LUND U LUND; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; Franco J. 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J	Roth, PB; Twiner, MJ; Mikulski, CM; Barnhorst, AB; Doucette, GJ				Roth, Patricia B.; Twiner, Michael J.; Mikulski, Christina M.; Barnhorst, Amanda B.; Doucette, Gregory J.			Comparative analysis of two algicidal bacteria active against the red tide dinoflagellate <i>Karenia brevis</i>	HARMFUL ALGAE			English	Article						algicidal bacteria; cyst formation; Cytophaga; dinoflagellate; Flavobacteriaceae; harmful algal bloom; Karenia brevis	MARINE BACTERIUM; FAMILY FLAVOBACTERIACEAE; HARMFUL MICROALGAE; GYMNODINIUM-BREVE; SP-NOV.; GROWTH; SEA; JAPAN; PHYTOPLANKTON; COMMUNITIES	The red tide dinoflagellate Karenia brevis blooms annually along the eastern Gulf of Mexico, USA, and is often linked to significant economic losses through massive fish kills, shellfish harvest closures, and the potential threat to humans of neurotoxic shellfish poisonings as well as exposure to aerosolized toxin. As part of an effort to enhance the strategies employed to manage and mitigate these events and their adverse effects, several approaches are being investigated for controlling blooms. Previous studies have established the presence of algicidal bacteria lethal to K. brevis in these waters, and we aim to characterize bacterial-algal interactions, evaluate their role as natural regulators of K. brevis blooms, and ultimately assess possible management applications. Herein, the algicidal activity of a newly isolated Cytophaga/Flavobacterium/Bacteroidetes (CFB)-bacterium, strain S03, and a previously described CFB-bacterium, strain 41-DBG2, was evaluated against various harmful algal bloom (HAB) and non-HAB species (23 total), including multiple clones of K. brevis, to evaluate algal target specificity. Strains S03 and 41-DBG2, which employ direct and indirect modes of algicidal lysis, respectively, killed similar to 20% and similar to 40% of the bacteria-containing isolates tested. Interestingly, no bacteria-free algal cultures were resistant to algicidal attack, whereas susceptibility varied occasionally among bacteria-containing isolates of a single algal taxon originating from either the same or different geographic location. The dynamics of K. brevis culture death appeared to differ according to whether the algicidal bacterium did or did not require direct contact with algal cells, with the former most rapidly affecting K. brevis morphology and causing cell lysis. Both bacterial strains promoted the formation of a small number of cyst-like structures in the K. brevis cultures, possibly analogous to temporary cysts formed by other dinoflagellates exposed to certain types of stress. Results were also consistent with earlier work demonstrating that bacterial assemblages from certain cultures can confer resistance to attack by algicidal bacteria, again indicating the complexity and importance of microbial interactions, and the need to consider carefully the potential for using such bacteria in management activities. Published by Elsevier B.V.	[Roth, Patricia B.; Twiner, Michael J.; Mikulski, Christina M.; Barnhorst, Amanda B.; Doucette, Gregory J.] NOAA, Natl Ocean Serv, Marine Biotoxins Program, Charleston, SC 29412 USA; [Roth, Patricia B.] Coll Charleston, Grice Marine Biol Lab, Grad Program Marine Biol, Charleston, SC 29412 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; College of Charleston	Doucette, GJ (通讯作者)，NOAA, Natl Ocean Serv, Marine Biotoxins Program, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	greg.doucette@noaa.gov	Doucette, Gregory/M-3283-2013					Agogué H, 2005, APPL ENVIRON MICROB, V71, P5282, DOI 10.1128/AEM.71.9.5282-5289.2005; ALTSCHUL SF, 1990, J MOL BIOL, V215, P403, DOI 10.1016/S0022-2836(05)80360-2; ANDERSON DM, 2001, TECHNICAL SERIES IOC, V59, P174; Azam F, 1998, SCIENCE, V280, P694, DOI 10.1126/science.280.5364.694; Castberg T, 2001, MAR ECOL PROG SER, V221, P39, DOI 10.3354/meps221039; Copley J, 2002, NATURE, V415, P572, DOI 10.1038/415572a; DAVIS CC, 1948, BOT GAZ, V109, P358, DOI 10.1086/335488; Doucette G.J., 1998, NATO ASI Series Series G Ecological Sciences, V41, P619; Doucette GJ, 1999, J PHYCOL, V35, P1447, DOI 10.1046/j.1529-8817.1999.3561447.x; Doucette Gregory J., 1995, Natural Toxins, V3, P65, DOI 10.1002/nt.2620030202; Fandino LB, 2001, AQUAT MICROB ECOL, V23, P119, DOI 10.3354/ame023119; FUKAMI K, 1992, NIPPON SUISAN GAKK, V58, P1073; Fukami K, 1997, HYDROBIOLOGIA, V358, P185, DOI 10.1023/A:1003139402315; Fukuyo Y., 2002, HARMFUL ALGAL BLOOMS, P7; Glöckner FO, 1999, APPL ENVIRON MICROB, V65, P3721; Guillard RRL., 1975, CULTURE MARINE INVER, P29, DOI [10.1007/978-1-4615-8714-93, DOI 10.1007/978-1-4615-8714-93, 10.1007/978-1-4615-8714-9_3]; Hare CE, 2005, HARMFUL ALGAE, V4, P221, DOI 10.1016/j.hal.2004.03.001; HAYGOOD MG, 1985, J BACTERIOL, V162, P209, DOI 10.1128/JB.162.1.209-216.1985; HENNES KP, 1995, APPL ENVIRON MICROB, V61, P3623, DOI 10.1128/AEM.61.10.3623-3627.1995; Hold GL, 2001, FEMS MICROBIOL ECOL, V37, P161, DOI 10.1111/j.1574-6941.2001.tb00864.x; IMAI I, 1995, FISHERIES SCI, V61, P628, DOI 10.2331/fishsci.61.628; IMAI I, 1993, MAR BIOL, V116, P527, DOI 10.1007/BF00355470; Imai Ichiro, 1998, Phycological Research, V46, P139, DOI 10.1111/j.1440-1835.1998.tb00106.x; Kang YH, 2005, J APPL MICROBIOL, V98, P1030, DOI 10.1111/j.1365-2672.2005.02533.x; Khan ST, 2006, INT J SYST EVOL MICR, V56, P323, DOI 10.1099/ijs.0.63841-0; Kim HG, 2006, ECOL STU AN, V189, P327, DOI 10.1007/978-3-540-32210-8_25; Kitaguchi H, 2001, PHYCOLOGIA, V40, P275, DOI 10.2216/i0031-8884-40-3-275.1; Kodama M, 2006, ECOL STU AN, V189, P243, DOI 10.1007/978-3-540-32210-8_19; Kondo R, 1999, FISHERIES SCI, V65, P432, DOI 10.2331/fishsci.65.432; Lane D. 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J	Ichinomiya, M; Nakamachi, M; Fukuchi, M; Taniguchi, A				Ichinomiya, Mutsuo; Nakamachi, Miwa; Fukuchi, Mitsuo; Taniguchi, Akira			Population dynamics of an ice-associated diatom, <i>Thalassiosira australis</i> Peragallo, under fast ice near Syowa Station, East Antarctica, during austral summer	POLAR BIOLOGY			English	Article						Thalassiosira australis; auxospore; resting spore; Antarctica; seed population	ARCTIC SEA-ICE; MARINE DIATOM; WEDDELL SEA; ELLIS FJORD; ROSS SEA; CHAETOCEROS-PSEUDOCURVISETUS; PHYTOPLANKTON SUCCESSION; MICROBIAL COMMUNITY; PLANKTONIC DIATOMS; CELL ENLARGEMENT	A clear shift from vegetative cells to auxospores and resting spores in Thalassiosira australis was observed in the water column and sinking fluxes under the fast ice near Syowa Station in the austral summer of 2005/2006. This is the first report of the auxosporulation by T. australis in situ. Resting spores were also observed in the sediment even before new spore formation, suggesting that T. australis can overwinter in the sediment. Heterotrophic dinoflagellates ingested and digested vegetative cells and auxospores but did not digest resting spores, suggesting a high tolerance of resting spores to grazing by heterotrophic dinoflagellates. We discuss the possible life history and overwintering strategy that T. australis uses in an Antarctic coastal area to cope with the unpredictable timing of sea ice growth and decay.	[Ichinomiya, Mutsuo] Lab Aquat Sci & Consultant Co Ltd, Ota Ku, Tokyo 1450064, Japan; [Nakamachi, Miwa] Tohoku Natl Fisheries Res Inst, Shiogama, Miyagi 9850001, Japan; [Fukuchi, Mitsuo] Natl Inst Polar Res, Tokyo, Kaga 1738515, Japan; [Taniguchi, Akira] Tokyo Univ Agr, Abashiri, Hokkaido 0992493, Japan	Japan Fisheries Research & Education Agency (FRA); Research Organization of Information & Systems (ROIS); National Institute of Polar Research (NIPR) - Japan; Tokyo University of Agriculture	Ichinomiya, M (通讯作者)，Lab Aquat Sci & Consultant Co Ltd, Ota Ku, Meishin BLDG,Kamiikedai 1-14-1, Tokyo 1450064, Japan.	ichinomiya@lasc.co.jp						Archer SD, 1996, MAR ECOL PROG SER, V139, P239, DOI 10.3354/meps139239; Assmy P, 2006, J PHYCOL, V42, P1002, DOI 10.1111/j.1529-8817.2006.00260.x; BERKMAN PA, 1986, POLAR BIOL, V6, P1, DOI 10.1007/BF00446234; Chepurnov VA, 2006, J PHYCOL, V42, P845, DOI 10.1111/j.1529-8817.2006.00244.x; Clarke A, 1996, LIMNOL OCEANOGR, V41, P1281, DOI 10.4319/lo.1996.41.6.1281; CRAWFORD RM, 1995, LIMNOL OCEANOGR, V40, P200, DOI 10.4319/lo.1995.40.1.0200; Drebes G., 1977, BIOL DIATOMS, P250; Enomoto H., 2002, POLAR METOROL GLACIO, V16, P1; FRYXELL GA, 1989, POLAR BIOL, V10, P1; FRYXELL GA, 1990, PHYCOLOGIA, V29, P27, DOI 10.2216/i0031-8884-29-1-27.1; GALLAGHER JC, 1983, J PHYCOL, V19, P539, DOI 10.1111/j.0022-3646.1983.00539.x; Garrison D.L., 1984, Marine Plankton Life Cycles Strategies, P1; Garrison DL, 2005, MAR ECOL PROG SER, V300, P39, DOI 10.3354/meps300039; Gran H.H., 1912, DEPTHS OCEAN, P307; Hargraves P., 1983, SURVIVAL STRATEGIES, P49; ICHINOMIYA M, 2008, POLAR SCI IN PRESS; Ichinomiya M, 2007, POLAR BIOL, V30, P1285, DOI 10.1007/s00300-007-0289-8; Ishikawa, 2001, POLAR BIOSCI, V14, P10; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; IWANAMI K, 1986, MEM NATL I POLAR RES, V40, P1; JEWSON DH, 1992, J PHYCOL, V28, P856, DOI 10.1111/j.0022-3646.1992.00856.x; JOHANSEN JR, 1985, PHYCOLOGIA, V24, P155, DOI 10.2216/i0031-8884-24-2-155.1; Kuwata A, 2005, J EXP MAR BIOL ECOL, V322, P143, DOI 10.1016/j.jembe.2005.02.013; KUWATA A, 1990, MAR BIOL, V107, P503, DOI 10.1007/BF01313435; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; Masqué P, 2007, DEEP-SEA RES PT I, V54, P1289, DOI 10.1016/j.dsr.2007.04.016; McMinn A, 1999, POLAR BIOL, V21, P220, DOI 10.1007/s003000050356; McMinn A, 1996, POLAR BIOL, V16, P301, DOI 10.1007/s003000050057; McMinn A, 2000, J PLANKTON RES, V22, P287, DOI 10.1093/plankt/22.2.287; MCMINN A, 1995, POLAR BIOL, V15, P269; MCMINN A, 1993, J PLANKTON RES, V15, P925, DOI 10.1093/plankt/15.8.925; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Moro I, 2000, MAR ECOL-P S Z N I, V21, P233, DOI 10.1046/j.1439-0485.2000.00706.x; Nagai S, 1995, PHYCOLOGIA, V34, P533, DOI 10.2216/i0031-8884-34-6-533.1; Otsuki Akihisa S., 2006, Antarctic Record, V50, P231; Palmisano A.C., 1993, P167; Palmisano A.C., 1985, P131; PFIRMAN SL, 1995, SCI TOTAL ENVIRON, V159, P129, DOI 10.1016/0048-9697(95)04174-Y; Roberts D, 2007, POLAR BIOL, V30, P143, DOI 10.1007/s00300-006-0169-7; Ryan KG, 2006, ANTARCT SCI, V18, P583, DOI 10.1017/S0954102006000629; SAITO R, 1998, ANTARCT REC, V42, P252; SCHAREK R, 1994, DEEP-SEA RES PT I, V41, P1231, DOI 10.1016/0967-0637(94)90042-6; Schmid AMM, 2001, EUR J PHYCOL, V36, P307, DOI 10.1080/09670260110001735468; Scott F.J., 2005, Antarctic Marine Protists, P13, DOI DOI 10.1017/S0954102005242906; Stoecker DK, 1998, J PHYCOL, V34, P60, DOI 10.1046/j.1529-8817.1998.340060.x; Swadling KM, 2004, LIMNOL OCEANOGR, V49, P644, DOI 10.4319/lo.2004.49.3.0644; SYVERTSEN EE, 1985, POLAR BIOL, V4, P113, DOI 10.1007/BF00442909; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; von Stosch H.A., 1982, BACILLARIA, V5, P127; WAITE A, 1992, MAR ECOL PROG SER, V87, P113, DOI 10.3354/meps087113	50	4	4	1	15	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	0722-4060			POLAR BIOL	Polar Biol.	AUG	2008	31	9					1051	1058		10.1007/s00300-008-0444-x	http://dx.doi.org/10.1007/s00300-008-0444-x			8	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	332CI					2025-03-11	WOS:000258059000005
J	Van Nieuwenhove, N; Bauch, HA				Van Nieuwenhove, Nicolas; Bauch, Henning A.			Last interglacial (MIS 5e) surface water conditions at the Voring Plateau (Norwegian Sea), based on dinoflagellate cysts	POLAR RESEARCH			English	Article						Dinoflagellate cysts; Holocene; last interglacial; marine isotope stage 5e; transfer functions	EEMIAN HYDROGRAPHIC CONDITIONS; NORTHERN NORTH-ATLANTIC; NORDIC SEAS; HIGH-RESOLUTION; MARINE ENVIRONMENTS; BALTIC SEA; RECONSTRUCTION; HOLOCENE; CLIMATE; SEDIMENTS	Sediments from the last interglacial, marine isotope stage 5e (MIS 5e), have been studied for their dinoflagellate cyst content in a core retrieved from the Voring Plateau, Norwegian Sea. Qualitative and quantitative analyses of the data, and comparison with the surface sample and published Holocene data from the core, reveal distinct differences in hydrological surface conditions between the late Holocene and MIS 5e. A higher number of co-dominant, subordinate species in the last interglacial samples suggests there was a more pronounced seasonality of the surface water at this time. This is supported by the significant presence of Bitectatodinium tepikiense, a species that was virtually absent from the area for most of the Holocene. The seasonality signal is further substantiated by transfer-function reconstructions, which also indicates a stronger stratification of the upper water column during MIS 5e. Moreover, the assemblage data clearly show that optimal, fully marine interglacial conditions prevailed only late in MIS 5e (between ca. 117.5 and 116.5 Kya), which is in contrast with the climatic optimum early in the Holocene. Stable oxygen isotope values from planktic foraminifera for this MIS 5e optimum are comparable with the average Holocene values, but are generally ca. 0.3 parts per thousand higher than those of the earlier part of the last interglacial (sensu stricto). These higher delta O-18 values are likely to be the result of the enhanced and prolonged influence of Saalian deglacial meltwater, thus corroborating the existence of a quite differently structured sea surface, as suggested by the dinocyst data.	[Van Nieuwenhove, Nicolas; Bauch, Henning A.] Univ Kiel, Leibniz Inst Marine Sci, DE-24148 Kiel, Germany; [Bauch, Henning A.] Mainz Acad Sci Human & Literature, DE-55131 Mainz, Germany	University of Kiel; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Van Nieuwenhove, N (通讯作者)，Univ Kiel, Leibniz Inst Marine Sci, Wischhofstr 1-3, DE-24148 Kiel, Germany.	nvannieuwenhove@ifm-geomar.de	Van Nieuwenhove, Nicolas/IAQ-1532-2023	Van Nieuwenhove, Nicolas/0000-0001-6369-2751				Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; [Anonymous], 1971, POLLEN SPORES; Bauch HA, 1999, PALAEOGEOGR PALAEOCL, V145, P95, DOI 10.1016/S0031-0182(98)00104-7; Bauch HA, 1996, QUATERNARY RES, V46, P260, DOI 10.1006/qres.1996.0065; Bauch HA, 2000, PALEOCEANOGRAPHY, V15, P76, DOI 10.1029/1998PA000343; Bauch HA, 2001, QUATERNARY SCI REV, V20, P659, DOI 10.1016/S0277-3791(00)00098-6; Bauch HA, 2008, POLAR RES, V27, P135, DOI 10.1111/j.1751-8369.2008.00059.x; Bauch HA, 2007, PALEOCEANOGRAPHY, V22, DOI 10.1029/2005PA001252; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Beets DJ, 2006, QUATERNARY SCI REV, V25, P876, DOI 10.1016/j.quascirev.2005.10.001; BERGER AL, 1978, J ATMOS SCI, V35, P2362, DOI [10.1175/1520-0469(1978)035<2362:LTVODI>2.0.CO;2, 10.1016/0033-5894(78)90064-9]; Boyer T.P., 2006, NOAA Atlas NESDIS 60, P1; Brauer A, 2007, P NATL ACAD SCI USA, V104, P450, DOI 10.1073/pnas.0603321104; Calvo E, 2002, QUATERNARY SCI REV, V21, P1385, DOI 10.1016/S0277-3791(01)00096-8; Cheddadi R, 1998, PALAEOGEOGR PALAEOCL, V143, P73, DOI 10.1016/S0031-0182(98)00067-4; CHEN JH, 1991, GEOL SOC AM BULL, V103, P82, DOI 10.1130/0016-7606(1991)103<0082:PCOTLI>2.3.CO;2; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Eriksson B, 1999, BOREAS, V28, P274; Eynaud F, 2004, REV PALAEOBOT PALYNO, V128, P55, DOI 10.1016/S0034-6667(03)00112-X; Eynaud F, 2000, MAR MICROPALEONTOL, V40, P9, DOI 10.1016/S0377-8398(99)00045-6; EYNAUD F, 1999, THESIS U BORDEAUX 1; Fronval T, 1997, PALEOCEANOGRAPHY, V12, P443, DOI 10.1029/97PA00322; GERLACH SA, 1986, BERICTE SONDERFORSCH, V4; Goñi MFS, 1999, EARTH PLANET SC LETT, V171, P123; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; Grosfjeld K, 2006, BOREAS, V35, P493, DOI 10.1080/03009480600781917; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; GUIOT J, 1993, PALAEOGEOGR PALAEOCL, V103, P73, DOI 10.1016/0031-0182(93)90053-L; Haake F.-W., 1992, P235; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head MJ, 2007, GEOL MAG, V144, P987, DOI 10.1017/S0016756807003780; Head MJ, 2005, QUATERN INT, V130, P3, DOI 10.1016/j.quaint.2004.04.027; HOPKINS TS, 1991, EARTH-SCI REV, V30, P175, DOI 10.1016/0012-8252(91)90001-V; Kandiano ES, 2004, PALAEOGEOGR PALAEOCL, V204, P145, DOI 10.1016/S0031-0182(03)00728-4; KOC N, 1993, QUATERNARY SCI REV, V12, P115, DOI 10.1016/0277-3791(93)90012-B; Kukla G, 2004, GLOBAL PLANET CHANGE, V40, P27, DOI 10.1016/S0921-8181(03)00096-1; Laskar J, 2004, ASTRON ASTROPHYS, V428, P261, DOI 10.1051/0004-6361:20041335; MANGERUD J, 1979, NATURE, V277, P189, DOI 10.1038/277189a0; Mangerud J., 1989, QUATERN INT, V3-4, P1, DOI [10.1016/1040-6182(89) 90067-0., DOI 10.1016/1040-6182(89)90067-0]; Marret F, 2004, REV PALAEOBOT PALYNO, V128, P35, DOI 10.1016/S0034-6667(03)00111-8; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Martens R., 1987, The Sport Psychologist, V1, P29, DOI [DOI 10.1123/TSP.1.1.29, 10.1123/tsp.1.1.29]; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen J, 2001, GLOBAL PLANET CHANGE, V31, P65, DOI 10.1016/S0921-8181(01)00113-8; Matthiessen J, 2001, J QUATERNARY SCI, V16, P727, DOI 10.1002/jqs.656; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; Mayewski PA, 2004, QUATERNARY RES, V62, P243, DOI 10.1016/j.yqres.2004.07.001; McCulloch MT, 2000, CHEM GEOL, V169, P107, DOI 10.1016/S0009-2541(00)00260-6; OVERPECK JT, 1985, QUATERNARY RES, V23, P87, DOI 10.1016/0033-5894(85)90074-2; Paillard D., 1996, Eos Trans. 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AUG	2008	27	2					175	186		10.1111/j.1751-8369.2008.00062.x	http://dx.doi.org/10.1111/j.1751-8369.2008.00062.x			12	Ecology; Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Oceanography	327VY		Bronze			2025-03-11	WOS:000257757800008
J	Meckler, AN; Schubert, CJ; Hochuli, PA; Plessen, B; Birgel, D; Flower, BP; Hinrichs, KU; Haug, GH				Meckler, A. N.; Schubert, C. J.; Hochuli, P. A.; Plessen, B.; Birgel, D.; Flower, B. P.; Hinrichs, K. -U.; Haug, G. H.			Glacial to Holocene terrigenous organic matter input to sediments from Orca Basin, Gulf of Mexico - A combined optical and biomarker approach	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						deglaciation; organic matter source; kerogen; bulk parameters; meltwater	LAURENTIDE ICE-SHEET; CARBON ISOTOPIC COMPOSITION; YOUNGER DRYAS; NORTHERN GULF; LAST DEGLACIATION; ATCHAFALAYA RIVER; SURFACE SEDIMENTS; AGE CALIBRATION; MELTWATER; MARINE	In this study we assessed changes in the contribution of terrigenous organic matter (OM) to the Gulf of Mexico over the course of the last deglaciation (the last 25 kyr). To this end, we combined optical kerogen analyses with bulk sedimentary, biomarker, and compound-specific Carbon isotope analyses. Samples were obtained from core MD02-2550 from Orca Basin (2249 in water depth at 26 degrees 56.77N, 91 degrees 20.74W) with temporal resolution ranging from multi-decadal to millennial-scale, depending on the proxy. All proxies confirmed larger terrigenous input during glacial times compared to the Holocene. In addition, the kerogen analyses suggest that much of the glacial OM is reworked (at least 50% of spores and pollen grains and 40% of dinoflagellate cysts). The Holocene sediments, in contrast, contain mainly marine OM, which is exceptionally well preserved. During the deglaciation, terrigenous input Was generally high due to large meltwater fluxes, whereby discrepancies between different proxies call for additional influences, Such as the change in distance to the river mouth, local productivity changes, and hydrodynamic particle sorting. It is possible that kerogen particles and the terrigenous biomarkers studied here represent distinct pools of land-derived OM with inputs varying independently. (C) 2008 Elsevier B.V. All rights reserved.	[Meckler, A. N.; Haug, G. H.] ETH, Inst Geol, CH-8092 Zurich, Switzerland; [Schubert, C. J.] EAWAG, CH-6047 Kastanienbaum, Switzerland; [Hochuli, P. A.] Univ Zurich, Inst Paleontol, CH-8006 Zurich, Switzerland; [Plessen, B.] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany; [Birgel, D.; Hinrichs, K. -U.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; [Haug, G. H.] Univ Potsdam, DFG Leibniz Ctr Surface Proc & Climate Studies, D-14476 Potsdam, Germany	Swiss Federal Institutes of Technology Domain; ETH Zurich; Swiss Federal Institutes of Technology Domain; Swiss Federal Institute of Aquatic Science & Technology (EAWAG); University of Zurich; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; University of Bremen; University of Potsdam	Meckler, AN (通讯作者)，CALTECH, Div Geol & Planetary Sci, MC 100-23,1200 E,Calif Blvd, Pasadena, CA 91125 USA.	ameckler@gps.caltech.edu	Meckler, Anna/AAC-2490-2020; Schubert, Carsten/GQQ-1673-2022; Hinrichs, Kai-Uwe/C-7675-2009	Meckler, Anna Nele/0000-0002-7225-8276; Schroder, Birgit/0000-0003-4807-6357; Schubert, Carsten J./0000-0003-1668-5967; Hinrichs, Kai-Uwe/0000-0002-0739-9291	Swiss National Science Foundation; EAWAG; Geoforschungszentrum Potsdam, Bremen University; Comer Science and Education Foundation	Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); EAWAG; Geoforschungszentrum Potsdam, Bremen University; Comer Science and Education Foundation	We Would like to thank Laurent Labeyrie, Viviane Bout-Roumazeilles, Yvon Balut, and the crew of R/V Marion Dufresne for a Successful cruise in the Gulf of Mexico. Hsin-Chi Lan is thanked for preparing the samples dated at ETH. Hans Thierstein provided expertise on nannofossil assemblages. P. Meier, U. Kegel, G. Schettler, and O. Scheidegger are gratefully acknowledged for their help with sample preparation and measurements. Julius Lipp assisted with lipid extractions and Heather Hill provided helpful comments on an earlier version of this manuscript. We furthermore thank Phil Meyers and an anonymous reviewer for their constructive comments. This work was funded by the Swiss National Science Foundation, with additional financial Support provided by EAWAG, Geoforschungszentrum Potsdam, Bremen University, and the Comer Science and Education Foundation.	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Sci. Lett.	JUL 30	2008	272	1-2					251	263		10.1016/j.epsl.2008.04.046	http://dx.doi.org/10.1016/j.epsl.2008.04.046			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	347DD		Green Accepted			2025-03-11	WOS:000259119900025
J	He, RY; McGillicuddy, DJ; Keafer, BA; Anderson, DM				He, Ruoying; McGillicuddy, Dennis J., Jr.; Keafer, Bruce A.; Anderson, Donald M.			Historic 2005 toxic bloom of <i>Alexandrium fundyense</i> in the western Gulf of Maine:: 2.: Coupled biophysical numerical modeling	JOURNAL OF GEOPHYSICAL RESEARCH-OCEANS			English	Article							PHYSICAL-BIOLOGICAL MODEL; RED TIDE DINOFLAGELLATE; VERTICAL MIGRATION; HUMIC SUBSTANCES; OCEANIC MODEL; CIRCULATION; SURFACE; POPULATIONS; MECHANISMS; COORDINATE	A coupled physical/biological modeling system was used to hindcast a massive Alexandrium fundyense bloom that occurred in the western Gulf of Maine in 2005 and to investigate the relative importance of factors governing the bloom's initiation and development. The coupled system consists of a state-of-the-art, free-surface primitive equation Regional Ocean Modeling System (ROMS) tailored for the Gulf of Maine (GOM) using a multinested configuration, and a population dynamics model for A. fundyense. The system was forced by realistic momentum and buoyancy fluxes, tides, river runoff, observed A. fundyense benthic cyst abundance, and climatological nutrient fields. Extensive comparisons were made between simulated ( both physical and biological) fields and in situ observations, revealing that the hindcast model is capable of reproducing the temporal evolution and spatial distribution of the 2005 bloom. Sensitivity experiments were then performed to distinguish the roles of three major factors hypothesized to contribute to the bloom: (1) the high abundance of cysts in western GOM sediments; (2) strong ` northeaster' storms with prevailing downwelling- favorable winds; and (3) a large amount of fresh water input due to abundant rainfall and heavy snowmelt. Model results suggest the following. (1) The high abundance of cysts in western GOM was the primary factor of the 2005 bloom. (2) Wind- forcing was an important regulator, as episodic bursts of northeast winds caused onshore advection of offshore populations. These downwelling favorable winds accelerated the alongshore flow, resulting in transport of high cell concentrations into Massachusetts Bay. A large regional bloom would still have happened, however, even with normal or typical winds for that period. (3) Anomalously high river runoff in 2005 resulted in stronger buoyant plumes/currents, which facilitated the transport of cell population to the western GOM. While affecting nearshore cell abundance in Massachusetts Bay, the buoyant plumes were confined near to the coast, and had limited impact on the gulf- wide bloom distribution.	[He, Ruoying] N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Raleigh, NC 27695 USA; [Keafer, Bruce A.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [McGillicuddy, Dennis J., Jr.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA	North Carolina State University; Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution	He, RY (通讯作者)，N Carolina State Univ, Dept Marine Earth & Atmospher Sci, Box 8208, Raleigh, NC 27695 USA.	rhe@ncsu.edu	; He, Ruoying/C-5598-2015	McGillicuddy, Dennis/0000-0002-1437-2425; He, Ruoying/0000-0001-6158-2292	Division Of Ocean Sciences; Directorate For Geosciences [0911031] Funding Source: National Science Foundation	Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))		Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Dinniman MS, 2003, DEEP-SEA RES PT II, V50, P3103, DOI 10.1016/j.dsr2.2003.07.011; DURBIN EG, 1992, LIMNOL OCEANOGR, V37, P361, DOI 10.4319/lo.1992.37.2.0361; Fairall CW, 2003, J CLIMATE, V16, P571, DOI 10.1175/1520-0442(2003)016<0571:BPOASF>2.0.CO;2; Flather R. 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Res.-Oceans	JUL 26	2008	113	C7							C07040	10.1029/2007JC004602	http://dx.doi.org/10.1029/2007JC004602			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	331GG		Green Accepted, Green Submitted, Bronze, Green Published			2025-03-11	WOS:000258000100004
J	Donders, TH; Gorissen, PM; Sangiorgi, F; Cremer, H; Wagner-Cremer, F; McGee, V				Donders, Timme H.; Gorissen, P. Martijn; Sangiorgi, Francesca; Cremer, Holger; Wagner-Cremer, Friederike; McGee, Vicky			Three-hundred-year hydrological changes in a subtropical estuary, Rookery Bay (Florida): Human impact versus natural variability	GEOCHEMISTRY GEOPHYSICS GEOSYSTEMS			English	Article						runoff; Florida; microfossils; hurricane; human impact; El Nino-southern oscillation	RADIOCARBON AGE CALIBRATION; CLIMATE VARIABILITY; MARINE-SEDIMENTS; EL-NINO; RECORD; IRRADIANCE; CARBONATE; SALINITY; IGNITION; HOLOCENE	The coastal wetland ecosystems in Florida are highly sensitive to changes in freshwater budget, which is driven by regional sea surface temperature, tropical storm activity, and the El Nino-Southern Oscillation (ENSO). Although studying Florida wetlands is pivotal to the understanding of these interacting climate systems, wetland dynamics have been severely altered by recent land use and drainage activities. To gather insights into the natural variability of the coastal ecosystems in Florida versus the effects of anthropogenic impact in the area, we present a 300-year record of changes in the hydrological cycle from a shallow subtropical estuary (Rookery Bay) on the western shelf of Florida, Gulf of Mexico. Palynological (pollen and organic-walled dinoflagellate cysts), diatom, and sedimentological analyses of a sediment core reveal significant changes in past runoff and wetland development. The onset and development of human impact in Florida are evident from high influx of Ambrosia pollen at about A. D. 1900, indicative of land clearance and disturbed conditions. To date, this is the southernmost record of Ambrosia increase related to human impact in the United States. Wetland drainage and deforestation since A. D. 1900 are evident from the reduced freshwater wetland and pine vegetation, and lower abundances of phytoplankton species indicative of lagoonal and brackish conditions. High runoff after A. D. 1900 relates to increased erosion and may correspondingly reflect higher impact from hurricane landfalls in SW Florida. Several phases with high siliciclastic input and greater wetland pollen abundance occur that predate the human impact period. These phases are interpreted as periods with higher runoff and are likely related to regional longer-term climate variability.	[Donders, Timme H.; Gorissen, P. Martijn; Sangiorgi, Francesca; Wagner-Cremer, Friederike] Univ Utrecht, Fac Sci, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Gorissen, P. Martijn; Cremer, Holger] Natl Geol Survey, Netherlands Org Appl Sci Res, TNO, NL-3584 CB Utrecht, Netherlands; [McGee, Vicky] Rookery Bay Natl Estuarine Res Reserve, Florida Dept Environm Protect, Naples, FL 34113 USA	Utrecht University; Netherlands Organization Applied Science Research	Donders, TH (通讯作者)，Univ Utrecht, Fac Sci, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	t.h.donders@uu.nl	Donders, Timme/J-5044-2012; Wagner-Cremer, Friederike/B-4225-2009	Sangiorgi, Francesca/0000-0003-4233-6154; Wagner-Cremer, Friederike/0000-0002-8119-3558; Donders, Timme/0000-0003-4698-3463				Alexander T.R., 1974, Environments of South Florida: present and past, P61; Bard E, 2000, TELLUS B, V52, P985, DOI 10.1034/j.1600-0889.2000.d01-7.x; BAZZAZ FA, 1974, ECOLOGY, V55, P112, DOI 10.2307/1934623; Brewster-Wingard GL, 1999, ESTUARIES, V22, P369, DOI 10.2307/1353205; Burns L.A., 1984, Cypress Swamps, P318; Cahoon D.R., 1997, Mangroves and Salt Marshes, V1, P173, DOI [10.1023/A:1009904816246, DOI 10.1023/A:1009904816246]; Cremer H, 2007, CARIBB J SCI, V43, P23; Cronin TM, 2002, CLIM RES, V19, P233, DOI 10.3354/cr019233; D'Arrigo R, 2005, GEOPHYS RES LETT, V32, DOI 10.1029/2004GL022055; DEAN WE, 1974, J SEDIMENT PETROL, V44, P242; Donders TH, 2005, QUATERNARY RES, V64, P333, DOI 10.1016/j.yqres.2005.08.016; Donders TH, 2005, P NATL ACAD SCI USA, V102, P10904, DOI 10.1073/pnas.0505015102; Donders TH, 2004, RADIOCARBON, V46, P455, DOI 10.1017/S003382220003976X; Donders TH, 2008, QUATERNARY SCI REV, V27, P571, DOI 10.1016/j.quascirev.2007.11.010; Doyle T.W., 1995, J COASTAL RES, V21, P159; Duever M.J., 1986, BIG CYPRESS NATL PRE; Fensome R.A., 2004, The Lentin and Williams Index of Fossil Dinoflagellates; Fourqurean JW, 1999, ESTUARIES, V22, P345, DOI 10.2307/1353203; GRIMM EC, 1993, SCIENCE, V261, P198, DOI 10.1126/science.261.5118.198; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Grimm EC, 2006, QUATERNARY SCI REV, V25, P2197, DOI 10.1016/j.quascirev.2006.04.008; Heiri O, 2001, J PALEOLIMNOL, V25, P101, DOI 10.1023/A:1008119611481; Hine AC, 2003, MAR GEOL, V200, P1, DOI 10.1016/S0025-3227(03)00161-0; HOOGHIEMSTRA H, 1988, PHILOS T ROY SOC B, V318, P431, DOI 10.1098/rstb.1988.0018; Hughen KA, 2004, RADIOCARBON, V46, P1059, DOI 10.1017/S0033822200033002; JARRELL JD, 1992, NHC46 NOAA NWS; Lean J, 2000, GEOPHYS RES LETT, V27, P2425, DOI 10.1029/2000GL000043; Light Stephen S., 1994, P47; Lund DC, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001218; Lund DC, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2004PA001008; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MORTON JF, 1978, ECON BOT, V32, P353, DOI 10.1007/BF02907927; Myers R.L., 1990, P150; Nyberg J, 2007, NATURE, V447, P698, DOI 10.1038/nature05895; Reimer PJ, 2004, RADIOCARBON, V46, P1029, DOI 10.1017/S0033822200032999; Reimer PJ, 2004, RADIOCARBON, V46, P1299; Richey JN, 2007, GEOLOGY, V35, P423, DOI 10.1130/G23507A.1; Rochon A., 1999, Distribution of recent dinoflagellate cysts in surface sediments from the North Atlantic Ocean and adjacent seas in relation to sea-surface parameters; Shirley MA, 2003, NOAACSC20414CD; Sklar FH, 2005, FRONT ECOL ENVIRON, V3, P161, DOI 10.2307/3868544; Snyder George H., 1994, P85; STUIVER M, 1993, RADIOCARBON, V35, P215, DOI 10.1017/S0033822200013904; STUIVER M, 1993, RADIOCARBON, V35, P1, DOI 10.1017/S0033822200013874; Stuiver M., 2006, CALIB Radiocarbon Calibration; Surge DM, 2003, ESTUAR COAST SHELF S, V57, P737, DOI 10.1016/S0272-7714(02)00370-0; Surge DM, 2002, ESTUARIES, V25, P393, DOI 10.1007/BF02695982; Swart PK, 1999, ESTUARIES, V22, P384, DOI 10.2307/1353206; Tomlinson P. B., 2016, The botany of mangroves; Van Campo E, 2004, MAR GEOL, V208, P315, DOI 10.1016/j.margeo.2004.04.014; Vega AJ, 1998, CLIMATE RES, V10, P115, DOI 10.3354/cr010115; Wanless Harold R., 1994, P199; Willard D.A., 2001, PALEOECOLOGY S FLORI, V361, P41; Willard DA, 2003, HOLOCENE, V13, P201, DOI 10.1191/0959683603hl607rp; Willard DA, 2001, REV PALAEOBOT PALYNO, V113, P213, DOI 10.1016/S0034-6667(00)00042-7; Willard Debra A., 2004, Palynology, V28, P175, DOI 10.2113/28.1.175; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Xu YP, 2007, ESTUAR COAST SHELF S, V73, P201, DOI 10.1016/j.ecss.2007.01.002	57	15	20	0	2	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA		1525-2027		GEOCHEM GEOPHY GEOSY	Geochem. Geophys. Geosyst.	JUL 10	2008	9								Q07V06	10.1029/2008GC001980	http://dx.doi.org/10.1029/2008GC001980			15	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	327OC					2025-03-11	WOS:000257737400002
J	Okolodkov, YB				Okolodkov, Yuri B.			<i>Protoperidinium</i> bergh (Dinophyceae) of the National Park Sistema Arrecifal Veracruzano, Gulf of Mexico, with a key for identification	ACTA BOTANICA MEXICANA			English	Article						dinoflagellates; Gulf of Mexico; key for identification; Protoperidinium; taxonomy	HETEROTROPHIC DINOFLAGELLATE GENUS; SEQUENCES; SEDIMENTS; CYSTS; OCEAN	The morphology of 46 species of Protoperidinium was studied based on 510 phytoplankton net samples taken from May 2005 through February 2007 at 7 stations in the northwestern part of the National Park Sistema Arrecifal Veracruzano, southern Gulf of Mexico. Forty-three species are represented by vegetative cells and three species only by cysts (P. oblongum, P. cf. stellatum and P. subinerme). Descriptions with an emphasis on the first apical and the second intercalary plates and synonymy are given for each species. Cell size variation, the mean and the standard deviation of three or four measurements are given for most species. The hypothecal pore in the first postcingular plate, a stable taxonomic feature, was observed only in P. solidicorne, P. pellucidum, P. ovum, P. sp. E meta-hexa and P. cf. hirobis; the position of the pore is also a conservative characteristic. Twenty-five species are provided with affinities and taxonomic, nomenclatural or biogeographic comments. A dichotomous key for identification of all the species found is presented, and species are illustrated with light microscope photographs. A new combination is proposed: Protoperidinium persicum (J. Schill.) Okolodkov comb. nov. Fifteen species are new records for the Gulf of Mexico, and about 25 species for the state of Veracruz.	Univ Veracruzana, Ctr Ecol & Pesquerias, Boca Del Rio 94290, Veracruz, Mexico	Universidad Veracruzana	Okolodkov, YB (通讯作者)，Univ Veracruzana, Ctr Ecol & Pesquerias, Calle Hidalgo 617,Col Rio Jamapa, Boca Del Rio 94290, Veracruz, Mexico.	yuriokolodkov@yahoo.com						Abe T. 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J	Garrido, S; Rosa, R; Ben-Hamadou, R; Cunha, ME; Chícharo, MA; van der Lingen, CD				Garrido, Susana; Rosa, Rui; Ben-Hamadou, Radhouan; Cunha, Maria Emilia; Chicharo, Maria Alexandra; van der Lingen, Carl D.			Spatio-temporal variability in fatty acid trophic biomarkers in stomach contents and muscle of Iberian sardine (<i>Sardina pilchardus</i>) and its relationship with spawning	MARINE BIOLOGY			English	Article							GALICIA NW SPAIN; NORTHEASTERN ATLANTIC; SPECIES VARIABILITY; LIPID-COMPOSITION; EGG-PRODUCTION; TELEOST FISH; PLANKTON; INVERTEBRATES; SEASON; GULF	Temporal variation in the fatty acid (FA) composition of stomach contents of Iberian sardines was compared to the relative contribution to dietary carbon made by different prey types for fish from two areas off Portugal. The effect of the FA content of the diet on sardine muscle FA composition was also studied, aiming at (1) analysing if FA biomarkers can be used as a complementary technique for the study of sardine diet and (2) to relate spatial and temporal variations of prey FA content with sardine condition and reproduction. Significant spatial differences in the FA composition of sardine diet occurred with concentrations of n-3 polyunsaturated FA, namely eicosapentaenoic acid [EPA, 20:5n-3] and linolenic acid 18:3n-3, being significantly higher in the diet of sardines from the west coast, whilst the diet of sardines from the south coast was richer in monounsaturated fatty acids (MUFA), namely the carnivory biomarker oleic acid 18:1n-9. These results are in agreement with the higher contribution made by diatoms and dinoflagellates to the diet of sardines off the west coast. Spatial variation in sardine dietary FA was also detected in their muscle composition, specifically for EPA, and the eicosapentaenoic/docosahexaenoic acid and (n-3)/(n-6) ratios, which were higher in sardines from the west coast. No difference in FA composition was detected between sexes, and the seasonal variability in sardine total FA concentration was primarily related to the seasonality of spawning. Sardines accumulate high concentrations of FAs during the resting stage of reproduction when the feeding intensity is similar or lower to that observed during the spawning season. Additionally, sardines show a high selective retention of MUFA and polyunsaturated FA (PUFA) throughout the year except at the beginning of the spawning season, when these FAs are largely invested in the formation of the gonads. Therefore, temporal and regional differences of prey environments are strong enough to be reflected in fish body composition, namely on the accumulation of essential FAs, which can have a strong impact on reproduction success for this species.	[Ben-Hamadou, Radhouan; Chicharo, Maria Alexandra] Univ Algarve, EcoReach Res Grp, FCMA, CCMAR, P-8005139 Faro, Portugal; [Cunha, Maria Emilia] CRIP Sul, INIAP IPIMAR, P-8700305 Olhao, Portugal; [van der Lingen, Carl D.] Marine & Coastal Management, ZA-8012 Cape Town, South Africa; [Garrido, Susana; Rosa, Rui] INIAP IPIMAR, P-1449006 Lisbon, Portugal	Universidade do Algarve	Garrido, S (通讯作者)，INIAP IPIMAR, Ave Brasilia, P-1449006 Lisbon, Portugal.	garridosus@gmail.com	Teodosio, Maria/B-5077-2013; Rosa, Rui/A-4580-2009; Garrido, Susana/F-7151-2011; Ben-Hamadou, Radhouan/F-8192-2011	Teodosio, Maria/0000-0002-0939-9885; Rosa, Rui/0000-0003-2801-5178; Garrido, Susana/0000-0001-6360-2883; Ben-Hamadou, Radhouan/0000-0003-2686-5822				[Anonymous], FISH NUTR; Bandarra NM, 1997, J FOOD SCI, V62, P40, DOI 10.1111/j.1365-2621.1997.tb04364.x; BARBOSA A, 2006, THESIS U ALGARVE ALG; Bell MV, 1996, MAR ECOL PROG SER, V134, P315, DOI 10.3354/meps134315; Bode A, 2003, ICES J MAR SCI, V60, P11, DOI 10.1006/jmsc.2002.1326; Budge SM, 2002, CAN J FISH AQUAT SCI, V59, P886, DOI 10.1139/F02-062; Carrera P, 2003, SCI MAR, V67, P245, DOI 10.3989/scimar.2003.67s1245; Coombs SH, 2006, J MAR BIOL ASSOC UK, V86, P1245, DOI 10.1017/S0025315406014251; Dalsgaard J, 2003, ADV MAR BIOL, V46, P225, DOI 10.1016/S0065-2881(03)46005-7; Dwyer KS, 2003, MAR BIOL, V143, P659, DOI 10.1007/s00227-003-1101-0; FIUZA AFD, 1982, OCEANOL ACTA, V5, P31; Gámez-Meza N, 1999, LIPIDS, V34, P639, DOI 10.1007/s11745-999-0409-1; Ganias K, 2003, MAR BIOL, V142, P1169, DOI 10.1007/s00227-003-1028-5; Garrido S, 2008, MAR ECOL PROG SER, V354, P245, DOI 10.3354/meps07201; Garrido S, 2007, COMP BIOCHEM PHYS B, V148, P398, DOI 10.1016/j.cbpb.2007.07.008; Garrido S, 2007, MAR ECOL PROG SER, V330, P189, DOI 10.3354/meps330189; Gurr MI., 1991, Lipid Biochemistry: An Introduction, V4th; HUNTER JR, 1981, FISH B-NOAA, V79, P215; *ICES, 2000, ICES CM, V5, P546; Iverson SJ, 2002, MAR ECOL PROG SER, V241, P161, DOI 10.3354/meps241161; Lee RF, 2006, MAR ECOL PROG SER, V307, P273, DOI 10.3354/meps307273; LEGENDRE L., 1983, NUMERICAL ECOLOGY; LINKO RR, 1985, COMP BIOCHEM PHYS B, V82, P699, DOI 10.1016/0305-0491(85)90511-5; Marshall CT, 1999, NATURE, V402, P288, DOI 10.1038/46272; Morimoto H, 1996, SURVIVAL STRATEGIES IN EARLY LIFE STAGES OF MARINE RESOURCES, P3; MORIMOTO H, 1991, ICES CM, V19; NEDENSKOV KJ, 2007, J SCI FOOD AGR; Parrish CC, 1998, ORG GEOCHEM, V29, P1531, DOI 10.1016/S0146-6380(98)00176-4; Peliz AJ, 1999, INT J REMOTE SENS, V20, P1363, DOI 10.1080/014311699212786; Pinto J. d. S., 1957, Proceedings Fisheries Council for the Mediterranean FAO, V4, P393; R Core Team, 2019, R: A language and environment for statistical computing; Reuss N, 2002, MAR BIOL, V141, P423, DOI 10.1007/s00227-002-0841-6; Ribeiro AC, 2005, J MARINE SYST, V53, P87, DOI 10.1016/j.jmarsys.2004.05.031; Riveiro I, 2004, MAR ECOL PROG SER, V274, P225, DOI 10.3354/meps274225; Rosa R, 2007, MAR BIOL, V151, P935, DOI 10.1007/s00227-006-0535-6; Sargent J., 1989, FISH NUTR, P153, DOI 10.1016/B978-012319652-1/50005-7; SARGENT JR, 1988, HYDROBIOLOGIA, V167, P101, DOI 10.1007/BF00026297; Shirai N, 2002, COMP BIOCHEM PHYS B, V131, P387, DOI 10.1016/S1096-4959(01)00507-3; Silva A, 2006, ICES J MAR SCI, V63, P663, DOI 10.1016/j.icesjms.2006.01.005; Silva A, 2003, ICES J MAR SCI, V60, P1352, DOI 10.1016/S1054-3139(03)00141-3; Somarakis S, 2006, FISH OCEANOGR, V15, P281, DOI 10.1111/j.1365-2419.2005.00387.x; Tocher DR, 2003, REV FISH SCI, V11, P107, DOI 10.1080/713610925; Uysal K, 2005, ECOL FOOD NUTR, V44, P23, DOI 10.1080/03670240590904308; Wedemeyer G.J.C.H., 1996, Physiology of Fish in Intensive Culture Systems, P232; Wiegand MD, 1996, REV FISH BIOL FISHER, V6, P259, DOI 10.1007/BF00122583	45	48	53	0	36	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	0025-3162			MAR BIOL	Mar. Biol.	JUL	2008	154	6					1053	1065		10.1007/s00227-008-0999-7	http://dx.doi.org/10.1007/s00227-008-0999-7			13	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	313RB					2025-03-11	WOS:000256756600011
J	Rochon, A; Eynaud, F; de Vernal, A				Rochon, Andre; Eynaud, Frederique; de Vernal, Anne			Dinocysts as tracers of hydrographical conditions and productivity along the ocean margins: Introduction	MARINE MICROPALEONTOLOGY			English	Editorial Material						dinocyst; North Atlantic Ocean; quaternary; Beaufort Sea; Pacific Ocean; transfer functions; primary productivity; climate change; preservation; upwelling	DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE CONDITIONS; LATE QUATERNARY; NORTH-ATLANTIC; SEDIMENTS	Quaternary organic- and calcitic-walled dinoflagellate cysts have received considerable attention within the last two decades due to their potential as tracers of sea surface parameters (temperature, salinity, sea ice cover, productivity). Despite uncertainties about taxonomical identity and limitations due to taphonomical processes, dinoflagellate cysts provide extremely useful and unique information on marine environments of the past. This is illustrated in the present special issue, which contains a selection of papers dealing with various approaches for reconstructing oceanographic parameters such as productivity, sea-ice cover, salinity, temperature, seasonality, and stratification in the upper water mass. All papers use organic-walled dinoflagellate cysts as their main proxy, but most combine the dinocyst information with results from complementary proxies, including benthic foraminifers, coccoliths, pollen, and stable isotopes in carbonates or organic matter. In all contributions, the approaches are based upon rigorous statistical treatment. (C) 2008 Elsevier B.V. All rights reserved.	[Rochon, Andre] ISMER UQAR, Rimouski, PQ G5L 3A1, Canada; [Eynaud, Frederique] Univ Bordeaux 1, CNRS, UMR 5805, EPOC, F-33405 Talence, France; [de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; Universite du Quebec a Rimouski; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; University of Quebec; University of Quebec Montreal	Rochon, A (通讯作者)，ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	andre_rochon@uqar.qc.ca	; de Vernal, Anne/D-5602-2013	Eynaud, Frederique/0000-0003-1283-7425; de Vernal, Anne/0000-0001-5656-724X				Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; DE VERNAL A, 1992, GEOLOGY, V20, P527, DOI 10.1130/0091-7613(1992)020<0527:QAOCDI>2.3.CO;2; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Rochon Andre, 1999, AASP Contributions Series, V35, P1; TRAVERSE A., 2007, Paleopalynology, Topics in Geobiology, P497, DOI [10.1007/978-1-4020-5610-9_17, DOI 10.1007/978-1-4020-5610-9_17]; Turon J.L., 1984, MEM I GEOL BASSIN AQ, V17, P1; WILLIAMS KM, 1990, CAN J EARTH SCI, V27, P1487, DOI 10.1139/e90-158; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	16	11	13	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	JUL	2008	68	1-2					1	5		10.1016/j.marmicro.2008.04.001	http://dx.doi.org/10.1016/j.marmicro.2008.04.001			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700001
J	Richefol, T; Rochon, A; Blasco, S; Scott, DB; Schell, TM; Bennett, RJ				Richefol, Thomas; Rochon, Andre; Blasco, Steve; Scott, Dave B.; Schell, Trecia M.; Bennett, Robbie J.			Evolution of paleo sea-surface conditions over the last 600 years in the Mackenzie Trough, Beaufort Sea (Canada)	MARINE MICROPALEONTOLOGY			English	Article						Arctic; dinoflagellate cysts; Beaufort Sea; Mackenzie Shelf; Amundsen Gulf; Mackenzie Trough; palynology; climate change; sea-ice cover; global warming	WALLED DINOFLAGELLATE CYSTS; HIGH-LATITUDE; LATE QUATERNARY; BAFFIN-ISLAND; ARCTIC LAKE; SEDIMENTS; SHELF; PHYTOPLANKTON; RECORD; BASIN	In order to document long-term climate trends and predict future climate change for the Arctic, we need to look at the geological record to establish the link between historical and pre-industrial sea-surface parameters. Dinoflagellate cysts (dinocysts) are used as proxy indicators of sea-surface parameters (temperature, salinity, sea-ice cover, primary productivity) jointly with transfer functions and a modern dinocyst reference database, to reconstruct the evolution of sea-surface conditions at decadal and multi-decadal timescales. Here we present the fossil dinocyst assemblages established from three sediment cores collected along an inshore-offshore transect in the Mackenzie Trough during the 2004 CASES (Canadian Arctic Shelf Exchange Study) cruise. The chronology of each core was determined using Pb-210 activity and AMS-C-14 measurements in core 912A. Sediment cores 912A, 909B and 906B cover the last 600,200 and 100 years respectively. Palynomorph influxes increase from the bottom to the top of each core, illustrating an increasing productivity over the last similar to 600 years until similar to 1850 AD, when we observe a decrease of productivity until today. We determined a succession of two assemblages over the last similar to 600 years. Assemblage 1, at the base of each core, is mostly composed of dinocysts from heterotrophic taxa. The modern assemblage (Assemblage II at the top of each core) is mostly composed of dinocysts from autotrophic taxa. Quantitative reconstructions of sea-surface parameters reveal a sharp increase in summer (August) temperature (similar to 2 to 5 degrees C) throughout the study area from similar to 1400 AD until similar to 1800-1850 AD, after which the increase (between similar to 0.5 and 1.0 degrees C) is much slower until modern times. (c) 2008 Elsevier B.V. All rights reserved.	[Richefol, Thomas; Rochon, Andre] UQAR ISMER, Rimouski, PQ G5L 3A1, Canada; [Blasco, Steve; Bennett, Robbie J.] Bedford Inst Oceanog, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; [Scott, Dave B.; Schell, Trecia M.] Dalhousie Univ, Ctr Environm & Marine Geol, Halifax, NS B3H 3J5, Canada	University of Quebec; Universite du Quebec a Rimouski; Bedford Institute of Oceanography; Natural Resources Canada; Dalhousie University	Richefol, T (通讯作者)，UQAR ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	thomas.richerol@uqar.qc.ca	RICHEROL, Thomas/G-4598-2017	RICHEROL, Thomas/0000-0001-5295-0022	Natural Sciences and Engineering Research Council (NSERC); Canadian Foundation for Innovation; FQRNT Funds of Quebec	Natural Sciences and Engineering Research Council (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canadian Foundation for Innovation(Canada Foundation for Innovation); FQRNT Funds of Quebec(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	This work is a contribution to the Canadian Arctic Shelf Exchange Study (CASES) program and was funded by the Natural Sciences and Engineering Research Council (NSERC) of Canada, and the Canadian Foundation for Innovation. Thomas Richerol was funded through the FQRNT Funds of Quebec. We are also grateful to the Quebec-Ocean group. We wish to thank the officers and crew of the CCGS Amundsen for their help and support during sampling. We also wish to express our gratitude to the following people who have helped during the collection and analyses of the surface samples and cores (Kate Jarrett, Bedford Institute of Oceanography; Dominique Hamel, Ursule Boyer-Villemaire, Hubert Gagne, Gervais Ouellet and Sylvain Leblanc, UQAR-ISMER; Maryse Henry and Bassam Ghaleb, UQAM-GEOTOP). We are also acknowledging Joel Guiot and Simon Brewer (CNRS-France) for the technical help on the use of the reconstruction software R. Finally we are grateful to two anonymous reviewers for their critical comments, which helped improve the manuscript.	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Micropaleontol.	JUL	2008	68	1-2					6	20		10.1016/j.marmicro.2008.03.003	http://dx.doi.org/10.1016/j.marmicro.2008.03.003			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700002
J	Pospelova, V; de Vernal, A; Pedersen, TF				Pospelova, Vera; de Vernal, Anne; Pedersen, Thomas F.			Distribution of dinoflagellate cysts in surface sediments from the northeastern Pacific Ocean (43-25°N) in relation to sea-surface temperature, salinity, productivity and coastal upwelling	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; northeastern Pacific; climate; productivity; paleoproductivity; upwelling; diversity; toxic species; HABs	LATITUDE MARINE ENVIRONMENTS; NORTHWESTERN INDIAN-OCEAN; NORTH PACIFIC; ESTUARINE SEDIMENTS; BRITISH-COLUMBIA; ADJACENT SEAS; ASSEMBLAGES; ATLANTIC; WATER; GULF	Fifty-six surface sediment samples from the northeastern Pacific (43-25 degrees N) were investigated in order to examine the spatial distribution of modern organic-walled dinoflagellate cysts in relation to hydrological conditions and marine productivity. The analyzed dinoflagellate cyst assemblages are diverse, and include over 60 taxa. Multivariate statistical analysis (CCA) of dinoflagellate cysts and environmental variables identifies annual productivity and sea-surface temperature as main factors affecting dinoflagellate cyst distribution in the region. In the Studied area, marine productivity is greatly influenced by the strength of the coastal upwelling. Cyst assemblages from the coastal sites associated with active upwelling are characterized by the dominance of heterotrophic taxa, particularly Brigantedinium spp., Echinidinium spp. and cysts of Protoperidinium americanum. Taxa associated with low productivity offshore sites arc Impagidinium spp., Nematosphaeropsis labyrinthus, Pyxidinopsis reticulata and Operculodinium centrocarpum. Dinoflagellate cyst species associated with warmer waters are Lingulodinium machaerophorum, Spiniferites mirabilis, S. ramosus, S. delicatus/bulloideus, Bitectatodinium spongium and Polykrikos cf. kofoidii, while those from cooler environments include Selenopemphix nephroiodes, Trinovantedinium variable and cysts of Pentapharsodinium dalei. Combining the present cyst dataset with other published cyst data from the Northeastern Pacific, we have compiled a "NE Pacific 188" database. This database can be used as a basis for the quantitative reconstruct ions of (palco)temperature and productivity in the Northeastern Pacific. (c) 2008 Elsevier B. V. All rights reserved.	[Pospelova, Vera; Pedersen, Thomas F.] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; [de Vernal, Anne] Univ Quebec, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Victoria; University of Quebec; University of Quebec Montreal	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, Petch 168,POB 3055 STN CSC, Victoria, BC V8W 3P6, Canada.	vpospe@uvic.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Pospelova, Vera/0000-0003-4049-8133	Fonds pour la Formation de Chercheurs et d'aide a la Recherche du Quebec (FCAR); Natural Sciences and Engineering Research Council of Canada (NSERC)	Fonds pour la Formation de Chercheurs et d'aide a la Recherche du Quebec (FCAR); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was funded by the Fonds pour la Formation de Chercheurs et d'aide a la Recherche du Quebec (FCAR) through a grant to VP and the Natural Sciences and Engineering Research Council of Canada (NSERC) through grants to VP, AdV, and TFP. Complementary support provided to ADV and TFP by the Canadian foundation for climate and atmospheric sciences (CFCAS) is also acknowledged.	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Micropaleontol.	JUL	2008	68	1-2					21	48		10.1016/j.marmicro.2008.01.008	http://dx.doi.org/10.1016/j.marmicro.2008.01.008			28	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700003
J	Vásquez-Bedoya, LF; Radi, T; Ruiz-Fernández, AC; de Vernal, A; Machain-Castillo, ML; Kielt, JF; Hillaire-Marcel, C				Vasquez-Bedoya, L. F.; Radi, T.; Ruiz-Fernandez, A. C.; de Vernal, A.; Machain-Castillo, M. L.; Kielt, J. F.; Hillaire-Marcel, C.			Organic-walled dinoflagellate cysts and benthic foraminifera in coastal sediments of the last century from the Gulf of Tehuantepec, South Pacific Coast of Mexico	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; Pb-210; Cs-137; benthic foraminifera; Pacific coast; eutrophication; upwelling; Gulf of Tehuantepec	SEA-SURFACE CONDITIONS; ESTUARINE SEDIMENTS; BRITISH-COLUMBIA; NORTH-ATLANTIC; HIGH-LATITUDES; OXYGEN; EUTROPHICATION; INDICATORS; OCEAN; ASSEMBLAGES	Qualitative and quantitative analysis of recent organic-walled dinoflagellate cysts (dinocysts) was performed on surface sediment samples and a core from the continental shelf of the Gulf of Tehuantepec, Mexico, in order to document the spatial distribution of dinocyst assemblages in relation to upwelling and primary productivity, and to assess the environmental history of the last century. The analyses of surface sediment samples show a close relation between dinocyst assemblages and productivity on a regional scale. Polysphaeridium zoharyi and heterotrophic taxa (notably Brigantedinium spp.) dominate in the high productivity zone, whereas Spiniferites delicatus and other phototrophic taxa are more abundant in the lower productivity zone. Sediment in an eighteen cm long gravity core (dated using Pb-210 and Cs-137) provided a record of the last century at annual to decadal resolution, thus yielding a unique opportunity to examine variations in dinocyst assemblages associated with environmental changes. Cyst concentrations in the core range between 477 and 2300 cysts g(-1), giving cyst fluxes between 68 and 494 Cysts cm(-2) yr(-1). Twenty-three phototrophic and heterotrophic cyst taxa were identified. Brigantedinium spp., P zoharyi and Bitectatodinium spongium are dominant, and are associated with the seasonal upwelling that characterizes the area. Cysts of potentially toxic species such as P. zoharyi (the cyst of Pyrodinium bahamense var. compressum and/or bahamense) occur throughout the core. Despite slight variations in relative abundances of the taxa in the assemblages, there is no evidence for eutrophication following industrial development of the adjacent coastal zone. Core samples were also analyzed for benthic foraminiferal content in order to determine possible effects of high, upwelling-induced productivity on bottom water oxygenation. The benthic foraminiferal assemblages are dominated by Hanzawaia concentrica (over 50%), with less abundant Uvigerina excellens, Cancris spp, Planulina ornata, Quinqueloculina lamarckiana, Epistominella sandiegoensis, Nonionella basispinata, Cassidulina modeloensis and Textularia foliacea. The benthic foraminiferal assemblages are characteristic of oxygen concentrations above 1 ml l(-1), indicating that possible changes in productivity did not significantly affect bottom water oxygen concentrations over the last 100 years. (c) 2008 Elsevier B.V. All rights reserved.	[Vasquez-Bedoya, L. F.; Ruiz-Fernandez, A. C.; Machain-Castillo, M. L.] Univ Nacl Autonoma Mexico, Mazatian 82040, Sin, Mexico; [Radi, T.; de Vernal, A.; Kielt, J. F.; Hillaire-Marcel, C.] Univ Quebec, Ctr Rech Geochim & Geodynam GETOP, Montreal, PQ H3C 3P8, Canada	Universidad Nacional Autonoma de Mexico; University of Quebec; University of Quebec Montreal	Ruiz-Fernández, AC (通讯作者)，Univ Nacl Autonoma Mexico, Calz Joel Montes Camarena S-N, Mazatian 82040, Sin, Mexico.	caro@ola.icmyl.unam.mx	Ruiz-Fernández, Ana Carolina/ABG-6985-2020; Hillaire-Marcel, Claude/H-1441-2012; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249; de Vernal, Anne/0000-0001-5656-724X; MACHAIN-CASTILLO, MARIA LUISA/0000-0002-4973-4967; Hillaire-Marcel, Claude/0000-0002-3733-4632	National Council of Science and Technology from Mexico (CONACyT) [45841-F]; UNAM-Direccion General de Estudios de Postgrado; Laboratory of Micropaleontology at (GEOTOP); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)	National Council of Science and Technology from Mexico (CONACyT)(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); UNAM-Direccion General de Estudios de Postgrado; Laboratory of Micropaleontology at (GEOTOP); Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	This research was partially funded by grant 45841-F from the National Council of Science and Technology from Mexico (CONACyT). The scholarships for LFVB were provided by UNAM-Direccion General de Estudios de Postgrado and the Laboratory of Micropaleontology at (GEOTOP). Mobility support to ACRF was provided by the UNAM-CIC International Academic Exchange Program, the Geochemistry and Geodynamics Research Centre GEOTOP and the bilateral Mexico-Quebec program for Scientific and Technological Cooperation 2007-2009 (Ministere des Relations Internationales du Quebec-Secretaria cle Relaciones Exteriores de Mexico). Thanks are due to M. Henry, M.C. Ramirez-Jauregui, G. Ramirez-Resendiz, H. Bojorquez-Leyva, L.H. Perez-Bernal, V. Montes-Montes and G. Gonzalez-Chavez for their technical assistance; as well to the crew of O/V El Puma for their help in the field. Analytical work was supported by infrastructure grants to GEOTOP by the Fonds Quebecois de Recherche sur la Nature et les Technologies (FQRNT). The authors gratefully acknowledge the constructive reviews of Francesca Sangiorgi and Marit-Solveig Seidenkrantz.	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Micropaleontol.	JUL	2008	68	1-2					49	65		10.1016/j.marmicro.2008.03.002	http://dx.doi.org/10.1016/j.marmicro.2008.03.002			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700004
J	Seidenkrantz, MS; Roncaglia, L; Fischel, A; Heilmann-Clausen, C; Kuijpers, A; Moros, M				Seidenkrantz, Marit-Solveig; Roncaglia, Lucia; Fischel, Andrea; Heilmann-Clausen, Claus; Kuijpers, Antoon; Moros, Matthias			Variable North Atlantic climate seesaw patterns documented by a late Holocene marine record from Disko Bugt, West Greenland	MARINE MICROPALEONTOLOGY			English	Review						West Greenland; Disko Bugt; Late Holocene; climate seesaw; palaeoceanography; dinoflagellates	WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; SOUTHERN GREENLAND; IGALIKU-FJORD; BAFFIN-BAY; RADIOCARBON CALIBRATION; PALYNOFACIES ANALYSIS; HYDROGRAPHIC CHANGES; MID-HOLOCENE; SEDIMENTS	The reconstruction of past sea-surface conditions in the Labrador Sea is essential for understanding climate fluctuations in the North Atlantic region. We here study late Holocene sea-surface conditions off West Greenland in order to elucidate the possible relationship between a North Atlantic seesaw and centennial to millennial-scale climate fluctuations in the Labrador Sea region. For that purpose we have studied the particulate organic matter (especially dinoflagellate cysts and acritarchs) from two marine sediment cores from Disko Bugt, central West Greenland. Our data show significant variations in sea-surface temperature and sea-ice cover during the last ca. 3200 years. After a cooling at ca. 2.9 ka cal. BP, presumably related to the Neoglacial cooling seen in large parts of the Northern Hemisphere, the area was Subjected to significant variability both in the entrainment of Atlantic Water (West Greenland Current water) and in atmospheric temperatures. From 2.0-1.5 ka cal. BP corresponding to the later part of the 'Roman Warm Period', the area experienced a return to a stronger influx of Atlantic water and an increased fresh-water influx from land probably related to increased precipitation or to melt-water outflow front the nearby inland ice. The 'Dark Ages' (1.5-1.3 ka cal. BP) were characterised by an only minor cooling of the surface waters. However, as seen in other records from the Labrador Sea region, the beginning of the 'Medieval Warm Period' (1.3-0.9 ka cal. BP) signified a severe cooling presumably due to a significant reduction in Atlantic water entrainment. The cold conditions continued through the 'Little Ice Age' (after 0.9 ka cal. BP) although the area seems to have experienced a minor decrease in sea-ice cover until 0.5 ka cal. B.P., after which sea-ice cover may again have increased. The period of 'Modern Warming' is not represented in Our data. Our study shows that a North Atlantic Oscillation-type pattern played a significant role in the late Holocene centennial to millennial-scale climate fluctuations in the Labrador Sea region. However, this cannot explain the full complexity of the climate signal. The fact that a simple pattern of 'cold' versus 'warm' climate scenario does not exist demonstrates that it will hardly be feasible to select the correct 'baseline' data set when modelling future climate development. (c) 2008 Elsevier B.V. All rights reserved.	[Seidenkrantz, Marit-Solveig; Fischel, Andrea; Heilmann-Clausen, Claus] Univ Aarhus, Dept Earth Sci, DK-8000 Aarhus, Denmark; [Roncaglia, Lucia] GNS Sci, Lower Hutt, New Zealand; [Kuijpers, Antoon] Geol Surv Denmark & Greenland GEUS, DK-1350 Copenhagen, Denmark; [Moros, Matthias] Balt Sea Res Inst, D-18119 Rostock, Germany; [Moros, Matthias] Bjerknes Ctr Climate Res, N-5007 Bergen, Norway	Aarhus University; GNS Science - New Zealand; Geological Survey Of Denmark & Greenland; Bjerknes Centre for Climate Research	Seidenkrantz, MS (通讯作者)，Univ Aarhus, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus, Denmark.	mss@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; Seidenkrantz, Marit-Solveig/A-3451-2012	Seidenkrantz, Marit-Solveig/0000-0002-1973-5969	Carlsberg Foundation, Copenhagen; Danish Natural Science Research Council [9802945, 9901443, 21-04-0336]; European Union 'PACLIVA' [EVR1-2002-000413]; Department of Earth Sciences, University of Aarhus; GEUS	Carlsberg Foundation, Copenhagen(Carlsberg Foundation); Danish Natural Science Research Council(Danish Natural Science Research Council); European Union 'PACLIVA'(European Union (EU)); Department of Earth Sciences, University of Aarhus; GEUS	We would like to sincerely thank Jesper Olsen, Department of Earth Sciences, University of Aarhus, Denmark, for his help in constructing the age models for the two cores. <SUP>14</SUP>C datings were carried out at the Leibniz-Labor, Christian Albrechts Universitat, Germany, the Poznan Radiocarbon Laboratory, Foundation of the Adam Mickiewicz University, Poland, the AMS laboratory, University of Aarhus, Denmark and the Center for Accelerator Mass Spectrometry, Lawrence Livermore National Laboratory, California, USA. Palynomorph samples were prepared at the Geological Survey of Denmark and Greenland (GEUS). We are grateful to the master and crew of R/V Dana for ship operations during the cruise in summer 2000, and we would also like to express Our thanks to Jack Schilling, Royal Netherlands Institute for Sea Research, and John Boserup (GEUS), who provided indispensable help with coring during the cruise. We Would also like to acknowledge reviewer's comment by Elisabeth Levac and an unnamed reviewer. Part of the work was carried out as a Bachelor thesis by A. Fischel (Fischel, 2006). This research was funded by the Carlsberg Foundation, Copenhagen (grant to L. Roncaglia), the Danish Natural Science Research Council (Danish Research Agency grants 9802945 and 990 1443 to A. Kuijpers, and grant no. 21-04-0336 to A. Kuijpers and M.-S. Seidenkrantz), the European Union 'PACLIVA' (GEUS Contract EVR1-2002-000413). the Department of Earth Sciences, University of Aarhus, and GEUS.	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J	Radi, T; de Vernal, A				Radi, Taoufik; de Vernal, Anne			Dinocysts as proxy of primary productivity in mid-high latitudes of the Northern Hemisphere	MARINE MICROPALEONTOLOGY			English	Review						dinoflagellate cysts; paleoproductivity; quantitative reconstruction; Northern Hemisphere	DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE CONDITIONS; OCEANIC PRIMARY PRODUCTION; CANONICAL CORRESPONDENCE-ANALYSIS; SATELLITE RADIOMETER DATA; EQUATORIAL INDIAN-OCEAN; LAST CLIMATIC CYCLE; NW ARABIAN SEA; LABRADOR SEA; BIOLOGICAL PRODUCTIVITY	In order to explore the potential of dinocyst assemblages in marine sediment as a proxy for primary productivity, we analyzed a reference "modern" database including 1171 sites from the North Atlantic Ocean (n = 483), the Arctic Ocean (n = 401) and the North Pacific Ocean (n = 287). We compiled two sets of primary productivity data derived from satellite observations: (1) The dataset from the Coastal Zone Color Scanner (CZCS) program applied to observations from 1978 to 1989 and (2) the data set from the MODerate resolution Imaging Spectroradiometer (MODIS) program using observations from 2002 to 2005. We performed canonical correspondence analysis (CCA) on a data matrix that included 62 dinocyst taxa and eight sea-surface parameters (winter and summer salinity, winter and summer temperature, sea-ice cover, summer, winter and annual primary productivity). CCA results show that primary productivity is a determinant parameter of dinocyst assemblages (including both phototrophic and heterotrophic taxa) in the North Atlantic, North Pacific, and at hemispheric scale. In the North Pacific, the relationship between productivity and dinocyst assemblages is particularly strong. We tested the modern analogue technique to reconstruct productivity using the North Atlantic, North Pacific, Arctic and hemispheric dinocyst data sets. With the exception of the Arctic Ocean alone, which is characterized by overall low productivity, productivity Can be estimated with an accuracy (Root Mean Square Error = RMSE) of +/- 11-25%. The best performance is obtained for reconstruction of winter productivity from the MODIS data. It is noteworthy that the RMSE for all estimated productivity parameters is narrower than the mean differences between productivity data derived from the MODIS and CZCS data sets. Therefore, we conclude that dinocysts can be used to reconstruct productivity with an accuracy equivalent to that of primary productivity estimated from satellite observations. Application of the approach in a sedimentary core from the northwest North Atlantic (core HU 91-045-094) revealed large amplitude variations of productivity over the last 25,000 years. The use of both MODIS and CZCS datasets indicate generally low productivity during the glacial stage, the Younger Dryas and Heinrich events, with annual productivity of less than 100 gC m(-2). The reconstructions also suggest higher productivity during the early Holocene, especially based on the MODIS data that suggest annual values of up to 350 gC m(-2). (C) 2008 Elsevier B.V. All rights reserved.	[Radi, Taoufik; de Vernal, Anne] Univ Quebec, Ctr Rech Geodynam GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Radi, T (通讯作者)，Univ Quebec, Ctr Rech Geodynam GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	radi.taoufik@courrier.uqam.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X	Canadian Foundation for Climate and Atmospheric Sciences; Natural Sciences and Engineering Research Council (NSERC) of Canada; Fonds de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec	Canadian Foundation for Climate and Atmospheric Sciences; Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	We thank L. Levesque for technical computer assistance in downloading and compiling the estimates of MODIS ocean productivity. We are grateful to the NASA Goddard Earth Sciences Distributed Active Archive Center (GES DAAC) for making CZCS and MODIS data available to the user community. This study is a contribution to the Polar Climate Stability Network supported by the Canadian Foundation for Climate and Atmospheric Sciences. Financial support from the Natural Sciences and Engineering Research Council (NSERC) of Canada and from the Fonds de la Recherche sur la Nature et les Technologies (FQRNT) of Quebec is also acknowledged. We are grateful to the reviewers of the Journal and to Thomas Pedersen and Laurent Londeix for their constructive comments on the original manuscript.	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Micropaleontol.	JUL	2008	68	1-2					84	114		10.1016/j.marmicro.2008.01.012	http://dx.doi.org/10.1016/j.marmicro.2008.01.012			31	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700006
J	Solignac, S; de Vernal, A; Giraudeau, J				Solignac, Sandrine; de Vernal, Anne; Giraudeau, Jacques			Comparison of coccolith and dinocyst assemblages in the northern North Atlantic: How well do they relate with surface hydrography?	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cyst; coccolith; North Atlantic; distribution; hydrography; multivariate analysis	NORWEGIAN-GREENLAND SEA; SCALE PHYSICAL CONTROLS; DINOFLAGELLATE CYSTS; NORDIC SEAS; PHYTOPLANKTON GROWTH; LIVING COMMUNITIES; HIGH-LATITUDES; IRMINGER SEA; CIRCULATION; PRODUCTIVITY	Coccolith and dinoflagellate cyst (or dinocyst) population counts were compiled from existing Surface sediment databases as well as new counts in order to establish an 87-sample database for which assemblages of both microfossil groups are known. This database allowed a direct comparison of the distribution of coccolith and dinocyst assemblages in the subtropical to subpolar North Atlantic. In addition, the relationship between these assemblages and sea Surface environmental parameters was addressed, in order to identify possible differences in the ecology of the two plankton groups. The comparison highlights all excellent correspondence between dinocyst assemblages, coccolith assemblages and the distribution of the Surface water masses represented in Our database, notably in the subtropical and temperate domains. In the subpolar domain, coccolith assemblages arc much less diversified than dinocyst assemblages in terms of species. As a result, the discrimination between the subpolar water masses based oil coccolith assemblages is not as clear as in the subtropical/temperate regions, whereas dinocyst assemblages show a distribution pattern closely related with surface hydrography. Canonical correspondence analyses performed oil coccolith and dinocyst assemblages show that sea surface temperature is the primary environmental parameter influencing the distribution of both groups. Dinocyst assemblages also seem to respond to the distance to the coast, and may therefore bring additional information compared with coccolith assemblages. Other significant environmental factors include sea surface salinity and productivity, but their relative importance changes depending on the inclusion of samples from extreme environmental settings in the database. Results suggest that the complexity of the interrelationships between the various environmental parameters makes it difficult to adequately bring to light all the different environments and their associated coccolith/dinocyst assemblages in multivariate analyses. However, each surface water mass represented ill Our database is characterized by a unique combination of environmental parameters as well as by distinct associations of coccolith and dinocyst assemblages, thus showing that these microfossil groups closely relate to sea Surface conditions, including temperature, salinity and productivity. (C) 2008 Elsevier B. V. All rights reserved.	[Solignac, Sandrine; de Vernal, Anne] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; [Giraudeau, Jacques] Univ Bordeaux 1, CNRS, UMR Environm & Paleoenvironm Ocean 5805, F-33405 Talence, France	University of Quebec; University of Quebec Montreal; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS)	Solignac, S (通讯作者)，Univ Quebec, GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	Solignac.sandrine@courrier.uqam.ca; anne.devernal@uqam.ca; j.giraudeau@epoc.u-bordeaux1.fr	Giraudeau, Jacques/AAF-5764-2019; de Vernal, Anne/D-5602-2013	Solignac, Sandrine/0000-0003-3373-6922; de Vernal, Anne/0000-0001-5656-724X; Giraudeau, Jacques/0000-0002-5069-4667	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Sciences and Engineering Research Council (NSERC) of Canada; Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	The authors want to thank Fabienne Marret, Department of Geography, University of Liverpool, and Karen Luise Knudsen, Geologisk Institut, Aarhus Universitet, for access to surface samples from the Celtic Sea and Icelandic shelf, as well as Harald Andruleit, Bundesanstalt fur Geowissenschaften und Rohstoffe, Federal Institute for Geosciences and Natural Resources, Hannover, for sharing coccolith data from the Nordic Seas with Linda Levesque (formerly at GEOTOP, Universite du Quebec a Montreal). Special thanks to Bianca Frechette, GEOTOP, Universite du Quebec Montreal, for her help in the interpretation of the statistical analyses, and to Fabienne Marret and an anonymous reviewer for their helpful comments. This study is a contribution to the Polar Climate Stability Network, supported by the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS). Support from the Natural Sciences and Engineering Research Council (NSERC) of Canada and the Fonds quebecois de la recherche sur la nature et les technologies (FQRNT) is acknowledged. This is GEOTOP publication 2008-0016.	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Micropaleontol.	JUL	2008	68	1-2					115	135		10.1016/j.marmicro.2008.01.001	http://dx.doi.org/10.1016/j.marmicro.2008.01.001			21	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700007
J	Penaud, A; Eynaud, F; Turon, JL; Zaragosi, S; Marret, F; Bourillet, JF				Penaud, A.; Eynaud, F.; Turon, J. L.; Zaragosi, S.; Marret, F.; Bourillet, J. F.			Interglacial variability (MIS 5 and MIS 7) and dinoflagellate cyst assemblages in the Bay of Biscay (North Atlantic)	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; foraminifera; Celtic-Armorican margin; Marine Isotope Stages (MIS) 5 and 7; Interglacial Complexes; climatic optima	LAST EUROPEAN DEGLACIATION; SEA-SURFACE CONDITIONS; ARMORICAN MARGIN BAY; BENTHIC FORAMINIFERA; KOLJO FJORD; SEDIMENTS; CLIMATE; RECORD; OCEAN; TEMPERATURE	The interglacial periods of the late Quaternary are frequently investigated as they constitute potential analogues for our modem climate and may shed light on the key questions of natural climate variability and future developments. The aim of this work is to reconstruct the paleoenvironmental history of Marine Isotope Stages (MIS) 5 and 7 in deep-sea sediments of the northern Bay of Biscay (North East Atlantic Ocean). On the basis of a multiproxy compilation, including analysis of dinoflagellate cyst assemblages, we discuss the nature of the paleoenvironmental and paleoclimate changes that took place in this region. Recurrent successions Of Species marking the beginning and the Termination of the Interglacial Complexes (MIS 5 and MIS 7) revealed a coherent scheme of water mass migration during these key transitional periods. Moreover, our data extend knowledge about the ecology of several dinoflagellate taxa. In particular, we discuss the ecology of Spiniferites septentrionalis and note that this species can be used as a biostratigraphical tracer in North Atlantic Quaternary sediments, until a major event of iceberg calving occurred during MIS 6. dated to around 150 ka BP. The dinocyst Spinferites mirabilis appears to be an important proxy for recognizing warm intervals within Interglacial Complexes. During MIS 5e, the Last Interglacial, this species is represented by the highest percentages ever recorded in sediments from the North Atlantic region. Peak occurrence of this species during MIS 7 indicates that substage MIS 7c, the second warm interval of the Penultimate Interglacial, represents the climatic optimum during the MIS 7 Interglacial Complex. (C) 2008 Elsevier B.V. All rights reserved.	[Penaud, A.; Eynaud, F.; Turon, J. L.; Zaragosi, S.] Univ Bordeaux 1, CNRS, UMR 5805, EPOC, F-33405 Talence, France; [Marret, F.] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Bourillet, J. F.] IFREMER, Dept Marine Geosci, Lab Environm Sedimentaires, F-29280 Plouzane, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; University of Liverpool; Universite Paris Cite; Ifremer	Penaud, A (通讯作者)，Univ Bordeaux 1, CNRS, UMR 5805, EPOC, Ave Fac, F-33405 Talence, France.	a.penaud@epoc.u-bordeaux1.fr	ZARAGOSI, Sébastien/JXL-2488-2024; Bourillet, Jean-Francois/O-9761-2017; Penaud, Aurelie/F-2485-2011	BOURILLET, Jean-Francois/0000-0002-6982-592X; Marret-Davies, Fabienne/0000-0003-4244-0437; Eynaud, Frederique/0000-0003-1283-7425; Zaragosi, Sebastien/0000-0002-1456-8129; Penaud, Aurelie/0000-0003-3578-4549	French CNRS; ANR PICC	French CNRS(Centre National de la Recherche Scientifique (CNRS)); ANR PICC(Agence Nationale de la Recherche (ANR))	Thanks to IPEV, the captain and the crew of the Marion Dufresne, and the scientific team of the SEDICAR cruise. We wish to thank Mr. Y. Balut for his assistance at sea and M. Castera, M. Georget and O. Ther for invaluable technical assistance at the laboratory. We gratefully acknowledge the reviewers, in particular Kari Grosfield whose comments permit to greatly improve this manuscript. Finally, we gratefully acknowledge Frank Oldfield for the English revision. Part of this study was supported by the French CNRS and the French contract of the ANR PICC. This is an U.M.R./EPOC C.N.R.S. 5805 contribution No 1675.	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Micropaleontol.	JUL	2008	68	1-2					136	155		10.1016/j.marmicro.2008.01.007	http://dx.doi.org/10.1016/j.marmicro.2008.01.007			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ		Green Published			2025-03-11	WOS:000259053700008
J	Ribeiro, S; Amorim, A				Ribeiro, Sofia; Amorim, Ana			Environmental drivers of temporal succession in recent dinoflagellate cyst assemblages from a coastal site in the North-East Atlantic (Lisbon Bay, Portugal)	MARINE MICROPALEONTOLOGY			English	Article						Gymnodinium catenatum; Lingulodinium polyedrum; dinoflagellate cyst signals; runoff; upwelling; water stability	SURFACE SEDIMENTS; GYMNODINIUM-CATENATUM; SODIUM POLYTUNGSTATE; SEASONAL OCCURRENCE; ONAGAWA BAY; DINOPHYCEAE; PHYTOPLANKTON; SCRIPPSIELLA; BLOOM; ISLANDINIUM	Temporal changes in the community structure of recent dinoflagellate cyst assemblages of Lisbon Bay (Iberian upwelling system) were investigated between 2000 and 2005. The assemblages were diverse and characterized by high inter-annual variability, rather than a clear seasonal pattern. In order to identify the main environmental drivers of community changes, several regional (river runoff, rainfall, upwelling, radiation, daylength) and in situ (sea surface temperature, salinity, bottom and Surface chlorophyll a concentration) environmental parameters were tested. Multivariate statistical analysis allowed the identification of water stability as the main environmental gradient influencing, the community composition, with river runoff in the preceding rain season and upwelling being the two drivers of stratification and turbulence, respectively. Both these processes can be described as nutrient enrichment processes, but the cyst signal indicates that the two mechanisms select for different functional groups. The main upwelling cyst signal is characterised by the dominance of heterotrophic species (Protoperidinioid species) and presence of the autotrophic chain-forming Gymnodinium catenatum, while the river runoff Cyst signal is characterised by dominance of autotrophs forming calcareous cysts, mainly Scrippsiella spp. Lingulodinium polyedrum is suggested to be indicative of upwelling conditions in the region but reflecting an ecological niche different from the more classical heterotrophic assemblage and G. catenatum. Our results reinforce the applicability of dinoflagellate cysts as environmental tracers in the warm-temperate region of the NE Atlantic, and contribute to the development of palaeoenvironmental cyst-based signals. (C) 2008 Elsevier B.V All rights reserved.	[Ribeiro, Sofia; Amorim, Ana] Univ Lisbon, Fac Ciencias, Inst Oceanog, P-1749016 Lisbon, Portugal	Universidade de Lisboa	Amorim, A (通讯作者)，Univ Lisbon, Fac Ciencias, Inst Oceanog, Campo Grande, P-1749016 Lisbon, Portugal.	sribeiro@fc.ul.pt; ajamorim@fc.ul.pt	Amorim, Ana/B-2117-2012; Ribeiro, Sofia/AAZ-2782-2021; Amorim, Ana/AAA-2615-2020; Ribeiro, Sofia/G-9213-2018	Amorim, Ana/0000-0002-9612-4280; Ribeiro, Sofia/0000-0003-0672-9161	Portuguese Foundation for Science and Technology [PDCTE/CTA/50386/2003, POCTI/CLI/58348/2004, SFRH/BD/30847/20061]; Fundação para a Ciência e a Tecnologia [PDCTE/CTA/50386/2003] Funding Source: FCT	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	This work has been developed within projects PROFIT - "Interdisciplinary study of processes underlying the phytoplankton dynamics in the Portuguese upwelling system" - (PDCTE/CTA/50386/2003) and PORTCOAST - "Present and future Portuguese coastal climate and its impacts on the biological communities" - (POCTI/CLI/58348/2004), funded by the Portuguese Foundation for Science and Technology. The authors would like to thank Teresa Moita and Sofia Palma, from IPIMAR, for kindly making available environmental data used in this study. Lino Costa is greatly acknowledged for advices regarding statistical analyses, and Vera Veloso for the help with sampling and slide preparation. Thanks are also due to two anonymous reviewers, for constructive comments that helped improve this manuscript. Sofia Ribeiro holds a PhD scholarship from the Portuguese Foundation for Science and Technology (SFRH/BD/30847/20061).	AMBAR I, 1994, SECOND INTERNATIONAL CONFERENCE ON AIR-SEA INTERACTION AND ON METEOROLOGY AND OCEANOGRAPHY OF THE COASTAL ZONE, P286; Amorim A, 2006, AFR J MAR SCI, V28, P193, DOI 10.2989/18142320609504146; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; Amorim A., 2004, Harmful Algae 2002, P89; Amorim A., 2001, Harmful Algal Blooms 2000, P133; AMORIM A, 2001, THESIS U LISBON PORT; Amorim A., 1998, Harmful Algae. 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F., 1988, CANOCO REFERENCE MAN; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wang ZH, 2004, PHYCOL RES, V52, P387, DOI 10.1111/j.1440-183.2004.00356.x; WOOSTER WS, 1976, J MAR RES, V34, P131; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X	67	40	44	0	15	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	JUL	2008	68	1-2					156	178		10.1016/j.marmicro.2008.01.013	http://dx.doi.org/10.1016/j.marmicro.2008.01.013			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700009
J	Zonneveld, KAF; Versteegh, G; Kodrans-Nsiah, M				Zonneveld, Karin A. F.; Versteegh, Gerard; Kodrans-Nsiah, Monika			Preservation and organic chemistry of Late Cenozoic organic-walled dinoflagellate cysts: A review	MARINE MICROPALEONTOLOGY			English	Review						dinoflagellate cyst; selective preservation; proxy; macromolecular chemistry; diagenesis; ocean ventilation	SEA-SURFACE CONDITIONS; CELL-WALL; MARINE-SEDIMENTS; SELECTIVE PRESERVATION; RESISTANT BIOPOLYMER; CHEMICAL-COMPOSITION; SPATIAL-DISTRIBUTION; ATMOSPHERIC CO2; LOW-TEMPERATURE; MATTER	Within the last decade considerable information has become available on the effects of early diagenesis on the taphonomy of organic-walled dinoflagellate cysts. Here, we review the information currently available on this topic. After discussing organic matter degradation in general, an overview on the effects of different laboratory treatments on the dinoflagellate cyst association is given. Hereafter, the rates and amount of species-selective degradation in modern and fossil natural environments are discussed. it appears that the availability of oxygen in the sediments is the most important diagenetic variable. Some of the modern dinoflagellate cyst species survive thousands of years in well oxygenated sediments and are as such among the most refractory types of organic matter. Most (but not all) of these refractory species are phototrophic gonyaulacoids. However, the refractory cysts form only a part of the modern gonyaulacoid or phototrophic cyst producing taxa. The modem species most vulnerable to degradation are often produced by heterotrophic peridinioids. Again, these Vulnerable species form only a part of the heterotrophic species and species with a peridinioid plate configuration. To get insight in the intrinsic properties of the cysts bringing about the selective preservation, we continue with reviewing the understanding of algal cell walls and dinoflagellate cyst walls at the molecular level. The review documents that cysts of Mesozoic age have different preservation characteristics than Late Cenozoic to Modern species. We propose that over long periods, taphonomic processes on a molecular level substantially change the cyst wall macromolecular structure and herewith cyst degradability. Having described the impact of selective preservation on the dinoflagellate cyst assemblages, we continue summarising the methods presently available for the recognition of and correction for this diagenetic overprint. Subsequently, we take advantage of the selective preservation by using it for reconstructing past export production. Since the rates of dinoflagellate cyst degradation are strongly related to the bottom water oxygen concentration, this opens the way for a new proxy to reconstruct deep-ocean oxygen concentrations. The importance of the rate of deep-ocean ventilation within the marine global carbon cycle and its relationship with climate change, make this use of selective dinoflagellate cyst preservation an important though unexpected application. (C) 2008 Elsevier B.V. All rights reserved.	[Zonneveld, Karin A. F.; Kodrans-Nsiah, Monika] Univ Bremen, Inst Hist Geol, D-2800 Bremen 33, Germany; [Versteegh, Gerard] Univ Hamburg, Fac Geosci, Inst Biogeochem & Marine Chem, D-20146 Hamburg, Germany	University of Bremen; University of Hamburg	Zonneveld, KAF (通讯作者)，Univ Bremen, Inst Hist Geol, D-2800 Bremen 33, Germany.	zonnev@micropal.uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	GJMV [MI157-20/1,2]; MNK (EUROPROX)	GJMV; MNK (EUROPROX)	We thank the reviewers for their constructive and detailed comments and for critically reading the manuscript. We thank Anne de Vernal for inviting us to contribute to this special issue. We thank the German Science Foundation for financial support to GJMV (grant MI157-20/1,2) and MNK (EUROPROX). This work is carried out as pat of MARUM Bereich B MARUM Nr. 0587.	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Micropaleontol.	JUL	2008	68	1-2					179	197		10.1016/j.marmicro.2008.01.015	http://dx.doi.org/10.1016/j.marmicro.2008.01.015			19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700010
J	Marret, F; Scourse, J; Kennedy, H; Ufkes, E; Jansen, JHF				Marret, Fabienne; Scourse, James; Kennedy, Hilary; Ufkes, Els; Jansen, J. H. Fred			Marine production in the Congo-influenced SE Atlantic over the past 30,000 years: A novel dinoflagellate-cyst based transfer function approach	MARINE MICROPALEONTOLOGY			English	Review						equatorial Africa; South Atlantic; palaeoproductivity; dinocysts; pollen; delta C-13; foraminifera; LGM; Holocene	EAST EQUATORIAL ATLANTIC; OCEANIC PRIMARY PRODUCTION; SURFACE SEDIMENTS; SOUTH-ATLANTIC; BENGUELA CURRENT; CLIMATE CHANGES; ZAIRE RIVER; PALAEOCEANOGRAPHIC CHANGES; LAST DEGLACIATION; OPAL PHYTOLITHS	The sediments front the Congo deep-sea fan contain valuable information about past environmental conditions of the cast equatorial Atlantic during the transition from the Last Glacial Maximum (LGM) to present-day climatic conditions. The high-resolution marine (organic-walled dinoflagellate cysts = dinocysts) and terrestrial (pollen) palynological records from two cores off equatorial West Africa, covering the last 30,000 years, document three major phases in surface productivity. (1) During the LGM relative sea level was low, nutrient enrichment due to seasonal coastal upwelling prevailed off the Congo mouth and high aridity prevailed in the catchment area. (2) At around 15.2 cal ka BP, monsoonal precipitation strengthened over the Congo Basin, generating high river discharges, river-induced upwelling, and increased nutrient flux to the ocean. In parallel, erosion of shelf sediments during shelf transgression further enhanced nutrient flux. (3) At around 9-8 cal ka BP, rainforest vegetation inhibited soil erosion, depleted nutrient Supply, and restricted marine productivity 10 its modern levels. The study presents the application of modern analogues and a dinocyst transfer function to the reconstruction of primary palaeoproductivity (PP) in a region of freshwater influence. A database of recent dinocyst assemblages comprising of 208 sites in the equatorial Atlantic enabled the reconstruction of sea-surface annual PP 1.3 times higher during the LGM and also during the deglaciation, between 15.2 and 13.2 cal ka BP. The reconstruction is independent of, and thus provides corroboration for, other biological and geochemical proxies. (C) 2009 Elsevier B. V. All rights reserved.	[Marret, Fabienne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Scourse, James; Kennedy, Hilary] Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales; [Ufkes, Els] Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Paleoclimatol & Geomorphol, NL-1081 HV Amsterdam, Netherlands; [Jansen, J. H. Fred] Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands	University of Liverpool; Bangor University; Vrije Universiteit Amsterdam; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Marret, F (通讯作者)，Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk; j.scourse@bangor.ac.uk; oss054@bangor.ac.uk; ufke@geo.vu.nl; jansen@nioz.nl	Kennedy, Hilary/M-5574-2014	Ufkes, E./0000-0003-3257-0203; Marret-Davies, Fabienne/0000-0003-4244-0437	UK Natural Environment Research Council Small Research [GR9/02631]; Leverhuline Trust [F/00174/E]	UK Natural Environment Research Council Small Research(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Leverhuline Trust(Leverhulme Trust)	This work was supported by a UK Natural Environment Research Council Small Research Grant (GR9/02631) and a major grant from the Leverhuline Trust (F/00174/E) both of which are gratefully acknowledged. We thank Klaas van der Borg (Utrecht) and Hans van de Plicht (Groningen) for the radiocarbon data, Anne de Vernal (Montreal) for useful discussion, and Maryse Henry (Montreal) for assisting with the modern environmental dataset as well Brian Long (Bangor) for helping with the preparation of the pollen samples. We are grateful to Lydie Dupont for her constructive comments on an earlier version of the manuscript and to Lucy Edwards and anonymous reviewer for their critical comments that helped to improve this paper. This is in part a contribution within the framework of the Netherlands-Bremen Oceanographic Cooperation (NEBROC).	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Micropaleontol.	JUL	2008	68	1-2					198	222		10.1016/j.marmicro.2008.01.004	http://dx.doi.org/10.1016/j.marmicro.2008.01.004			25	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346FJ					2025-03-11	WOS:000259053700011
J	Nye, E; Feist-Burkhardt, S; Horne, DJ; Ross, AJ; Whittaker, JE				Nye, Eleanor; Feist-Burkhardt, Susanne; Horne, David J.; Ross, Andrew J.; Whittaker, John E.			The palaeoenvironment associated with a partial <i>Iguanodon</i> skeleton from the Upper Weald Clay (Barremian, Early Cretaceous) at Smokejacks Brickworks (Ockley, Surrey, UK), based on palynomorphs and ostracods	CRETACEOUS RESEARCH			English	Article						lower Cretaceous; Wealden; England; palynology; ostracods; megaspores; Iguanodon; palaeoenvironment; palaeoclimate; preservation	SOUTHERN ENGLAND; PURBECK-WEALDEN; DINOSAURS; SEDIMENTS; FACIES; PLANT; BIOSTRATIGRAPHY; REPRODUCTION; CLIMATES; BELGIUM	In 2001 a partial skeleton of an Iguanodon was discovered in the Upper Weald Clay (Barremian, Early Cretaceous) at Smokejacks Brickworks near Ockley, Surrey, UK. When the dinosaur was excavated, a detailed stratigraphic section was logged and 25 samples taken for palynological and micropalaeontological (ostracod and megaspore) analysis, including a detailed sample set of the dinosaur bed itself. Qualitative and quantitative analysis of the palynoflora revealed rich and well-preserved non-marine assemblages of pollen and spores, including early angiosperms, and freshwater green algae. Four types of angiosperm pollen are described and assigned to the genus Retimonocolpites Pierce, 196 1, but left in open nomenclature. Some marine elements such as dinoflagellate cysts are identified as the result of reworking of Middle and Upper Jurassic sediments. The pollen/spore assemblages depict a vegetational change from principally gymnosperm-dominated assemblages at the base to principally pteridophyte-dominated assemblages at the top of the section. The dinosaur bed shows a pteridophyte-dominated assemblage, with a significantly high amount of the freshwater green alga Scenedesmus novilunaris He Cheng-quan et al., 1992. Samples close to the dinosaur bed yielded the first useful ostracod finds from Smokejacks Brickworks: well-preserved assemblages containing Cypridea clavata (Anderson, 1939), Damonella cf. pygmaea (Anderson, 1941), Stenestroemia cf. cressida Anderson, 1971 and Stenestroemia sp. A, and fragments and damaged valves of a thin-shelled ostracod, possibly belonging to Mantelliana Anderson, 1966. Those identified as Cypridea clavata show a wide range of morphological variety and in opposition to Anderson's (1967, 1985) taxonomic scheme, which would assign them to up to five different taxa, they are considered to be intraspecific variants of a single species. The possibilities and limitations of age determination of the Wealden sediments using palynomorphs and ostracods are discussed; distinct forms of early angiosperm, pollen, together with the ostracod fauna, are consistent with an early Barremian age. Pollen and spores are discussed in terms of their parent plants and the reconstruction of vegetation and palaeoclimate. Palynology and ostracods give evidence for temporary freshwater conditions at the time when the Iguanodon died and the carcase was buried. (C) 2008 The Natural History Museum. Published by Elsevier Ltd. All rights reserved.	[Nye, Eleanor; Feist-Burkhardt, Susanne; Ross, Andrew J.; Whittaker, John E.] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Horne, David J.] Nat Hist Museum, Dept Zool, London SW7 5BD, England; [Horne, David J.] Univ London, Dept Geog, London E1 4NS, England	Natural History Museum London; Natural History Museum London; University of London	Feist-Burkhardt, S (通讯作者)，Nat Hist Museum, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.	s.feist-burkhardt@nhm.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242; Horne, David J./0000-0002-2148-437X				ALLEN P, 1981, J GEOL SOC LONDON, V138, P375, DOI 10.1144/gsjgs.138.4.0375; Allen P, 1998, P GEOLOGIST ASSOC, V109, P197, DOI 10.1016/S0016-7878(98)80066-7; ALLEN P, 1975, Proceedings of the Geologists' Association, V86, P389; ALLEN P, 1990, P GEOLOGISTS ASS, V1989, P529; ANDERSON F. 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Res.	JUN	2008	29	3					417	444		10.1016/j.cretres.2008.01.004	http://dx.doi.org/10.1016/j.cretres.2008.01.004			28	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	326ZX					2025-03-11	WOS:000257699500004
J	Bravo, I; Vila, M; Masó, M; Figueroa, RI; Ramilo, I				Bravo, Isabel; Vila, Magda; Maso, Mercedes; Figueroa, Rosa Isabel; Ramilo, Isabel			<i>Alexandrium catenella</i> and <i>Alexandrium minutum</i> blooms in the, Mediterranean Sea:: Toward the identification of ecological niches	HARMFUL ALGAE			English	Article						Alexandrium catenella; Alexandrium minutum; dinoflagellate cysts; dinoflagellate blooms; Mediterranean Sea	DINOFLAGELLATE ALEXANDRIUM; WATERS; FRANCE	Annual recurrent blooms of the toxic dinoflagellates Alexandrium catenella and Alexandrium minutum were detected from 2000 to 2003 in harbours along the Catalan coast. The interrelation study between the occurrence of the blooms and specific external conditions at the study sites demonstrated that different factors are required for the bloom of each Alexandrium species. Concentrations higher than 105 cells 1(-1) of A. catenella were only detected in Tarragona harbour. These blooms were associated with water surface temperature between 21 and 25 degrees C and salinities of around 34 psu or higher than 37 psu. A. minutum appeared widely spread along the Catalan coast, though the most intensive and recurrent blooms of this species were observed in Arenys de Mar harbour. Concentrations of millions of cells per litre of A. minutum were associated with water temperatures below 14 degrees C and salinities of around 34-36 psu. A. minutum cell densities showed a positive significant correlation with NO3 but a negative correlation with NH4. On the other hand, A. catenella blooms dominated when both NO3 and NH4 levels were high. The prevailing inorganic nitrogen form (NO3 vs. NH4) could explain why these two species rarely coincide in the same harbours. Accumulation of cysts in the sediment was found to be an important potential factor for the recurrence of these spocies. The 4.3 x 10(3) A. catenella Cysts cm(-3) of wet sediment in Tarragona harbour and the 3.02 x 10(3) A. minutum Cysts cm(-3) of wet sediment in Vilanova harbour were the highest concentrations observed from the cyst study. Confined waters such as harbours play an important role as reservoirs for the accumulation of cysts and vegetative cells, which contributes to the expansion of these dinoflagellates in the region. However, the particular environmental conditions are also decisive factors of bloom intensity. (C) 2007 Elsevier B.V. All rights reserved.	[Bravo, Isabel; Figueroa, Rosa Isabel; Ramilo, Isabel] IEO, Vigo 36200, Spain; [Vila, Magda; Maso, Mercedes] CSIC, Inst Ciencias Mar, E-08003 Barcelona, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Bravo, I (通讯作者)，IEO, Aptado 1552, Vigo 36200, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Vila, Magda/B-2447-2014; Figueroa, Rosa/M-7598-2015	Vila, Magda/0000-0002-6855-841X; Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X				Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; [Anonymous], 2003, BOCCONEA; [Anonymous], 1996, HARMFUL TOXIC ALGAL; Balech E., 1995, Sherkin Island Marine Station. 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J	Siringan, FP; Azanza, RV; Macalalad, NJH; Zamora, PB; Maria, MYYS				Siringan, Femando P.; Azanza, Rhodora V.; Macalalad, Neil John H.; Zamora, Peter B.; Maria, Ma. Yvainnc Y. Sta.			Temporal changes in the cyst densities of <i>Pyrodinium bahamense</i> var. <i>compressum</i> and other dinoflagellates in Manila Bay, Philippines	HARMFUL ALGAE			English	Article						climate; dinollagellate cyst; harmful algal blooms; Manila Bay; Pyrodinium bahamense var. compressum; toxic dinoflagellate	HARMFUL ALGAL BLOOMS; EUTROPHICATION; RECORDS	Temporal variation in the type and abundance of dinoflagellate cysts in Manila Bay, Philippines, is established using Pb-210-dated sediment cores. At least 17 dinoflagellate cyst species, including those of the toxic species, Pyrodinium bahamense var. compressum, were identified. P. bahamense may have been present in the area since at least the 1920s. Total cyst density has increased beginning about 1988 to 1998 coinciding with records of P. bahamense blooms in the area. Heterotrophs have always dominated the cysts assemblage. These changes in the dinoflagellate record and the P. bahamense blooms in recent years may have been induced by the interplay of warmer temperatures, high rainfall leading to higher river discharge and less turbulent waters due to passage of few tropical cyclones. (C) 2008 Elsevier B.V. All rights reserved.	[Siringan, Femando P.; Azanza, Rhodora V.; Zamora, Peter B.; Maria, Ma. Yvainnc Y. Sta.] Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines; [Siringan, Femando P.; Macalalad, Neil John H.; Zamora, Peter B.; Maria, Ma. Yvainnc Y. Sta.] Univ Philippines, Natl Inst Geol Sci, Quezon City 1101, Philippines	University of the Philippines System; University of the Philippines Diliman; University of the Philippines System; University of the Philippines Diliman	Siringan, FP (通讯作者)，Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines.	fpsiringan@upmsi.ph	Azanza, Rhodora/HGU-5811-2022; Zamora, Peter/N-6568-2019					Anderson D.M., 1984, Seafood toxins, P125; [Anonymous], 1996, HARMFUL TOXIC ALGAL; Azanza R., 1997, SCI DILIMAN, V9, P1; Azanza RV, 2004, PHYCOL RES, V52, P376; Azanza RV, 2001, J SHELLFISH RES, V20, P1251; Azanza RV, 1998, J SHELLFISH RES, V17, P1619; AZANZA RV, 2007, 3 JOINT SEM JSPS MUL; Bajarias FA., 1996, HARMFUL TOXIC ALGAL, P49; Burkholder JM, 2006, ECOL STU AN, V189, P53, DOI 10.1007/978-3-540-32210-8_5; Corrales R.A., 1995, P573; Dale B., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; *EMB, 1992, MAN BAY MON PR UNPUB; Furio E. F., 1996, HARMFUL TOXIC ALGAL, P185; Hansen PJ, 2004, MAR ECOL PROG SER, V275, P79, DOI 10.3354/meps275079; *IRI LDEO CLIM DAT, KAPL IND NIN 3 4 186; *IRI LDEO CLIM DAT, HIST RAINF AIR TEMP; Jacinto GS, 2006, ENVIRONMENT IN ASIA PACIFIC HARBOURS, P293, DOI 10.1007/1-4020-3655-8_18; *JOINT TYPH WARN C, TROP CYCL TRACKS W N; MACLOUF J, 1989, PHARMACOL RES, V21, P1, DOI 10.1016/1043-6618(89)90115-1; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MATSUOKA K, 2000, TECHN GUID MOD DIN C; Mudie PJ, 2002, PALAEOGEOGR PALAEOCL, V180, P159, DOI 10.1016/S0031-0182(01)00427-8; *PAGASA, 1949, HIST ANN PREC DAT PO; Phlips EJ, 2006, MAR ECOL PROG SER, V322, P99, DOI 10.3354/meps322099; Phlips EJ, 2004, HARMFUL ALGAE, V3, P39, DOI 10.1016/j.hal.2003.08.003; REIGMAN R, 1996, PHYSL ECOLOGY HARMFU, P475; SELIGER HH, 1989, ICLARM CONT, V21, P53; SIRINGAN NP, 1997, SCI DILIMAN, V9, P29; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1132, DOI 10.4319/lo.1997.42.5_part_2.1132; SMITH DW, 1908, PHILOS J SCI, P187; Sombrito EZ, 2004, J ENVIRON RADIOACTIV, V76, P177, DOI 10.1016/j.jenvrad.2004.03.025; SOMBRITO EZ, 2001, PHILIPP NUCL J, V13, P1; USUP G, 1998, PHYSL ECOLOGY HARMFU, P81; Villanoy CL, 2006, HARMFUL ALGAE, V5, P156, DOI 10.1016/j.hal.2005.07.001; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; YNIGUEZ AT, 2000, HAB 2000 C TASM AUST; INT GLOB OC SERVSEA	39	25	28	1	13	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JUN	2008	7	4					523	531		10.1016/j.hal.2007.11.003	http://dx.doi.org/10.1016/j.hal.2007.11.003			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	311CS					2025-03-11	WOS:000256578400015
J	Lee, FWF; Ho, KC; Lo, SCL				Lee, Fred Wang-Fat; Ho, Kin Chung; Lo, Samuel Chun-Lap			Rapid identification of dinoflagellates using protein profiling with matrix-assisted laser desorption/ionization mass spectrometry	HARMFUL ALGAE			English	Article						dinoflagellates; harmful algal blooms (HABs); identification; MALDI; protein profiling	DISTRIBUTED ALEXANDRIUM DINOPHYCEAE; INTERNAL TRANSCRIBED SPACER; DESORPTION-IONIZATION-TIME; RIBOSOMAL-RNA GENES; BACILLUS SPORES; WHOLE CELLS; BACTERIA; MALDI; FRAGMENT; CULTURE	The occurrence of harmful algal blooms (HABs) or red tides is an important and expanding threat to human health, fishery resources, and the tourism industries. Toxic species post an additional treat of intoxication when consumed either in seafood or directly swallowed. Rapid and accurate identification of the HAB species is critical for minimizing or controlling the damage. We report the use of protein/peptide mass fingerprint profiles obtained with matrix-assisted laser desorption ionization time-of-flight (MALDI-TOF) mass spectrometry (MS) for the identification of dinoflagellates, common causative agents of HABs. The method is simple, fast and reproducible. The peptide mass fingerprint spectral patterns are unique for different dinoflagellate species and are easily distinguishable by visual inspection. In addition to the whole mass spectra, several specific biomarkers were identified from the mass spectra of different species. These biomarker ions and the mass spectral patterns form an unambiguous basis for species discrimination. (C) 2007 Elsevier B.V. All rights reserved.	[Lee, Fred Wang-Fat; Lo, Samuel Chun-Lap] Hong Kong Polytech Univ, Dept Appl Biol & Chem Technol, Hong Kong, Hong Kong, Peoples R China; [Ho, Kin Chung] Open Univ Hong Kong, Fac Sci & Technol, Hong Kong, Hong Kong, Peoples R China; [Lo, Samuel Chun-Lap] State Key Lab Tradit Chinese Med & Mol Pharmacol, Shenzhen, Peoples R China	Hong Kong Polytechnic University; Hong Kong Metropolitan University	Lo, SCL (通讯作者)，Hong Kong Polytech Univ, Dept Appl Biol & Chem Technol, Hong Kong, Hong Kong, Peoples R China.	bcsamlo@inet.polyu.edu.hk		Lee, Wang-Fat/0000-0001-9665-1163; Lo, Samuel Chun-lap/0000-0003-1134-7299				ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Amiri-Eliasi BJ, 2001, ANAL CHEM, V73, P5228, DOI 10.1021/ac010651t; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; Dickinson DN, 2004, APPL ENVIRON MICROB, V70, P475, DOI 10.1128/AEM.70.1.475-482.2004; Donohue MJ, 2006, J MICROBIOL METH, V65, P380, DOI 10.1016/j.mimet.2005.08.005; Evason DJ, 2000, RAPID COMMUN MASS SP, V14, P669, DOI 10.1002/(SICI)1097-0231(20000430)14:8<669::AID-RCM932>3.3.CO;2-Z; Fenselau C, 2001, MASS SPECTROM REV, V20, P157, DOI 10.1002/mas.10004; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hathout Y, 1999, APPL ENVIRON MICROB, V65, P4313; Jarman KH, 1999, RAPID COMMUN MASS SP, V13, P1586, DOI 10.1002/(SICI)1097-0231(19990815)13:15<1586::AID-RCM680>3.0.CO;2-2; Jarman KH, 2000, ANAL CHEM, V72, P1217, DOI 10.1021/ac990832j; KELLER MD, 1987, J PHYCOL, V23, P633; Krishnamurthy T, 1996, RAPID COMMUN MASS SP, V10, P1992, DOI 10.1002/(SICI)1097-0231(199612)10:15<1992::AID-RCM789>3.0.CO;2-V; Krishnamurthy T, 1996, RAPID COMMUN MASS SP, V10, P883, DOI 10.1002/(SICI)1097-0231(19960610)10:8<883::AID-RCM594>3.3.CO;2-M; Li TY, 2000, RAPID COMMUN MASS SP, V14, P2393, DOI 10.1002/1097-0231(20001230)14:24<2393::AID-RCM178>3.0.CO;2-9; Magnuson ML, 2000, APPL ENVIRON MICROB, V66, P4720, DOI 10.1128/AEM.66.11.4720-4724.2000; PREMAZZI G, 1993, MICROPHYTE TOXIN MAN; Ryzhov V, 2000, APPL ENVIRON MICROB, V66, P3828, DOI 10.1128/AEM.66.9.3828-3834.2000; Ryzhov V, 2001, ANAL CHEM, V73, P746, DOI 10.1021/ac0008791; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SCHOLIN CA, 1993, J PHYCOL, V29, P209, DOI 10.1111/j.0022-3646.1993.00209.x; SCHOLIN CA, 1994, J PHYCOL, V30, P744, DOI 10.1111/j.0022-3646.1994.00744.x; SCHOLIN CA, 1995, J PHYCOL, V30, P321; STEIDINGER KA, 1990, TOXIC MARINE PHYTOPLANKTON, P522; Taylor F.J. R., 1984, SEAFOOD TOXINS, P77; Valentine N, 2005, APPL ENVIRON MICROB, V71, P58, DOI 10.1128/AEM.71.1.58-64.2005; Welham KJ, 2000, RAPID COMMUN MASS SP, V14, P307, DOI 10.1002/(SICI)1097-0231(20000315)14:5<307::AID-RCM823>3.0.CO;2-3; Winkler MA, 1999, ANAL CHEM, V71, P3416, DOI 10.1021/ac990135r; YAO Z, 2001, P 49 ANN C AM SOC MA	30	14	14	1	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JUN	2008	7	4					551	559		10.1016/j.hal.2007.12.001	http://dx.doi.org/10.1016/j.hal.2007.12.001			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	311CS					2025-03-11	WOS:000256578400018
J	Shikata, T; Nagasoe, S; Matsubara, T; Yamasaki, Y; Shimasaki, Y; Oshima, Y; Uchida, T; Jenkinson, IR; Honjo, T				Shikata, Tomoyuki; Nagasoe, Sou; Matsubara, Tadashi; Yamasaki, Yasuhiro; Shimasaki, Yohei; Oshima, Yuji; Uchida, Takuji; Jenkinson, Ian R.; Honjo, Tsuneo			Encystment and excystment of <i>Gyrodinium instriatum</i> Freudenthal et Lee	JOURNAL OF OCEANOGRAPHY			English	Article						encystment; excystment; dinoflagellate; Gyrodinium instriatum; cyst; nutrient; temperature	DINOFLAGELLATE GYMNODINIUM-CATENATUM; RAPHIDOPHYTE HETEROSIGMA-AKASHIWO; SEXUAL REPRODUCTION; CYST FORMATION; GONYAULAX-TAMARENSIS; RESTING CYSTS; LIFE-CYCLE; BALTIC SEA; DINOPHYCEAE; GERMINATION	In the present study, we have investigated the conditions influencing encystment and excystment in the dinoflagellate Gyrodinium instriatum under laboratory conditions. We incubated G. instriatum in modified whole SWM-3 culture medium and in ver- sions of modified SWM-3 from which NO(3)(-), PO(4)(3-), NO(3)(-) + PO(4)(3-), or Si had been omitted and observed encystment. Percentage encystment was high in the media without N and without P, while the percentage encystment in the medium lacking both N and P was highest. Moreover, to investigate N or P concentration which induced the encystment, Gyrodinium instriatum was also incubated in media with different concentrations of inorganic N and P; the concentrations of NO(2)(-) + NO(3)(-) and PO(4)(3-) were measured over time. The precursors of cysts appeared within 2 or 3 days of a decrease in NO(2)(-) + NO(3)(-) or PO(4)(3-) concentration to values lower than 1 mu M or 0.2 mu M, respectively. When cysts produced in the laboratory were incubated, we observed excystment after 8-37 days, without a mandatory period of darkness or low temperature. We incubated cysts collected from nature at different temperatures or in the dark or light and observed excystments. Natural cysts excysted at temperatures from 10 to 30 degrees C, in both light and dark, but excystment was delayed at low temperatures. These studies indicate that G. instriatum encysts in low N or P concentration and excysts over a wide temperature range, regardless of light conditions, after short dormancy periods.	[Shikata, Tomoyuki; Matsubara, Tadashi; Yamasaki, Yasuhiro; Shimasaki, Yohei; Oshima, Yuji; Honjo, Tsuneo] Kyushu Univ, Grad Sch Bioresource & Bioenvironm Sci, Dept Biosci & Biotechnol, Lab Marine Environm Sci, Fukuoka 8128581, Japan; [Nagasoe, Sou; Uchida, Takuji] Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Hiroshima 7390452, Japan; [Jenkinson, Ian R.] Agcy Conseil & Rech Oceanog, F-19320 La Roche Canillac, France	Kyushu University; Japan Fisheries Research & Education Agency (FRA)	Shikata, T (通讯作者)，Kyushu Univ, Grad Sch Bioresource & Bioenvironm Sci, Dept Biosci & Biotechnol, Lab Marine Environm Sci, Fukuoka 8128581, Japan.	shikata@agr.kyushu-u.ac.jp	Oshima, Yuji/C-7701-2011	xiong zhi, da dao/0000-0002-7682-9611				ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Azanza RV, 2004, PHYCOL RES, V52, P376; BINDER BJ, 1987, J PHYCOL, V23, P99; Blackburn S., 2005, Algal Culturing Techniques, P399; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CUSHING DH, 1994, J PLANKTON RES, V16, P291, DOI 10.1093/plankt/16.3.291; ENDO T, 1984, Bulletin of Plankton Society of Japan, V31, P23; Engel M, 2004, J PLANKTON RES, V26, P1083, DOI 10.1093/plankt/fbh099; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Itakura S, 1996, J PLANKTON RES, V18, P1975, DOI 10.1093/plankt/18.10.1975; ITOH K, 1987, JAPAN FISHERIES RESO, P122; JIMENEZ R, 1993, DEV MAR BIO, V3, P257; Joyce LB, 2006, AFR J MAR SCI, V28, P295, DOI 10.2989/18142320609504165; Kamiyama T, 1996, J PLANKTON RES, V18, P2313, DOI 10.1093/plankt/18.12.2313; Katajisto T, 1996, HYDROBIOLOGIA, V320, P153, DOI 10.1007/BF00016816; KOJIMA N, 1992, REV PALAEOBOT PALYNO, V74, P239, DOI 10.1016/0034-6667(92)90009-6; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Nagai Satoshi, 2004, Plankton Biology and Ecology, V51, P103; Nagasoe S, 2006, HARMFUL ALGAE, V5, P20, DOI 10.1016/j.hal.2005.06.001; NAGASOE S, 2006, THESIS KYUSHU U FUKU; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; PFIESTER LA, 1976, J PHYCOL, V12, P234; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; SAKO Y, 1984, B JPN SOC SCI FISH, V50, P743; SAKO Y, 1987, B JPN SOC SCI FISH, V53, P473; Shikata T, 2007, HARMFUL ALGAE, V6, P700, DOI 10.1016/j.hal.2007.02.008; Strickland J.D. H., 1968, A Practical Handbook of Seawater Analysis, V2nd; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; WALKER LM, 1979, J PHYCOL, V15, P312; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; Yamasaki Y, 2007, MAR ECOL PROG SER, V339, P83, DOI 10.3354/meps339083; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131	45	13	17	1	21	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0916-8370			J OCEANOGR	J. Oceanogr.	JUN	2008	64	3					355	365		10.1007/s10872-008-0028-y	http://dx.doi.org/10.1007/s10872-008-0028-y			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	292FQ					2025-03-11	WOS:000255252300002
J	Munnecke, A; Servais, T				Munnecke, Axel; Servais, Thomas			Palaeozoic calcareous plankton: evidence from the Silurian of Gotland	LETHAIA			English	Article; Proceedings Paper	Conference on Changing Palaeogeographical and Palaeobiogeographical Patterns in the Ordovician and Silurian	AUG 30-SEP 01, 2006	Univ Glasgow, Glasgow, SCOTLAND		Univ Glasgow	calcispheres; Gotland; Palaeozoic; plankton; Silurian	EVOLUTION; SWEDEN; HISTORY; PHYTOPLANKTON; NANNOFOSSILS; LIMESTONES; CARBONATES; ISOTOPES; FACIES	In order to investigate whether or not equivalents to modern calcareous plankton existed in Palaeozoic times, extremely well-preserved successions have to be investigated. The Silurian strata on Gotland (Sweden) are exceptionally well preserved because they have not experienced deep burial conditions and tectonic stress, due to their position on the stable Baltic Shield. Scanning electron microscope investigations of polished, slightly etched rock surfaces revealed the presence of a variety of calcareous micro- and nannofossils. Among these organisms, many can be termed 'calcispheres' (60-100 mu m in diameter), whereas others due to their size range (nannofossils) are informally termed herein as 'nannospheres' (10-25 mu m in diameter). The systematic attribution of these fossils is unknown (incertae sedis). Mesozoic calcispheres are usually attributed to calcareous cysts of dinoflagellates following comparisons of ultrastructure with modern species. The abundance of different calcispheres in the Silurian sediments of Gotland and the observation that many of the calcareous microfossils occur in distinctly different facies as well as their spherical shape indicate that they probably belong to calcareous micro- and nannoplankton. We therefore conclude that calcareous plankton most probably existed already during the Palaeozoic, but can only be observed under conditions of exceptional preservation.	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J	Glibert, PM; Azanza, R; Burford, M; Furuya, K; Abal, E; Al-Azri, A; Al-Yamani, F; Andersen, P; Anderson, DM; Beardall, J; Berg, GM; Brand, L; Bronk, D; Brookes, J; Burkholder, JM; Cembella, A; Cochlan, WP; Collier, JL; Collos, Y; Diaz, R; Doblin, M; Drennen, T; Dyhrman, S; Fukuyo, Y; Furnas, M; Galloway, J; Granéli, E; Ha, DV; Hallegraeff, G; Harrison, J; Harrison, PJ; Heil, CA; Heimann, K; Howarth, R; Jauzein, C; Kana, AA; Kana, TM; Kim, H; Kudela, R; Legrand, C; Mallin, M; Mulholland, M; Murray, S; O'Neil, J; Pitcher, G; Qi, YZ; Rabalais, N; Raine, R; Seitzinger, S; Salomon, PS; Solomon, C; Stoecker, DK; Usup, G; Wilson, J; Yin, KD; Zhou, MJ; Zhu, MY				Glibert, Patricia M.; Azanza, Rhodora; Burford, Michele; Furuya, Ken; Abal, Eva; Al-Azri, Adnan; Al-Yamani, Faiza; Andersen, Per; Anderson, Donald M.; Beardall, John; Berg, G. Mine; Brand, Larry; Bronk, Deborah; Brookes, Justin; Burkholder, Joann M.; Cembella, Allan; Cochlan, William P.; Collier, Jackie L.; Collos, Yves; Diaz, Robert; Doblin, Martina; Drennen, Thomas; Dyhrman, Sonya; Fukuyo, Yasuwo; Furnas, Miles; Galloway, James; Graneli, Edna; Ha, Dao Viet; Hallegraeff, Gustaaf; Harrison, John; Harrison, Paul J.; Heil, Cynthia A.; Heimann, Kirsten; Howarth, Robert; Jauzein, Cecile; Kana, Austin A.; Kana, Todd M.; Kim, Hakgyoon; Kudela, Raphael; Legrand, Catherine; Mallin, Michael; Mulholland, Margaret; Murray, Shauna; O'Neil, Judith; Pitcher, Grant; Qi, Yuzao; Rabalais, Nancy; Raine, Robin; Seitzinger, Sybil; Salomon, Paulo S.; Solomon, Caroline; Stoecker, Diane K.; Usup, Gires; Wilson, Joanne; Yin, Kedong; Zhou, Mingjiang; Zhu, Mingyuan			Ocean urea fertilization for carbon credits poses high ecological risks	MARINE POLLUTION BULLETIN			English	Editorial Material						urea dumping; ocean fertilization; carbon credits; Sulu Sea; carbon sequestration; harmful algae; toxic dinoflagellates; cyanobacteria; hypoxia	DISSOLVED ORGANIC NITROGEN; AUREOCOCCUS-ANOPHAGEFFERENS; IRON FERTILIZATION; ALGAL BLOOM; CORAL-REEFS; MARINE; TRICHODESMIUM; GROWTH; SEA; CYANOBACTERIUM	The proposed plan for enrichment of the Sulu Sea, Philippines, a region of rich marine biodiversity, with thousands of tonnes of urea in order to stimulate algal blooms and sequester carbon is flawed for multiple reasons. Urea is preferentially used as a nitrogen source by some cyanobacteria and dinoflagellates, many of which are neutrally or positively buoyant. Biological pumps to the deep sea are classically leaky, and the inefficient burial of new biomass makes the estimation of a net loss of carbon from the atmosphere questionable at best. The potential for growth of toxic dinoflagellates is also high, as many grow well on urea and some even increase their toxicity when grown on urea. Many toxic dinoflagellates form cysts which can settle to the sediment and germinate in subsequent years, forming new blooms even without further fertilization. If large-scale blooms do occur, it is likely that they will contribute to hypoxia in the bottom waters upon decomposition. Lastly, urea production requires fossil fuel usage, further limiting the potential for net carbon sequestration. The environmental and economic impacts are potentially great and need to be rigorously assessed. (C) 2008 Elsevier Ltd. All rights reserved.	[Glibert, Patricia M.; Kana, Todd M.; O'Neil, Judith; Stoecker, Diane K.] Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA; [Azanza, Rhodora] Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines; [Burford, Michele; Yin, Kedong] Griffith Univ, Australian Rivers Inst, Brisbane, Qld 4111, Australia; [Furuya, Ken] Univ Tokyo, Dept Aquat Biosci, Tokyo 1138657, Japan; [Abal, Eva] SE Queensland Healthy Waterways Partnership, Brisbane, Qld 4001, Australia; [Al-Azri, Adnan] Sultan Quboos Univ, Dept Marine Sci & Fisheries, Muscat, Oman; [Al-Yamani, Faiza] Kuwait Inst Sci Res, Safat 13109, Kuwait; [Andersen, Per] Orbicon AS, DK-8260 Vibyj, Denmark; [Anderson, Donald M.; Dyhrman, Sonya] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Beardall, John; Dyhrman, Sonya] Monash Univ, Sch Biol Sci, Clayton, Vic 3800, Australia; [Berg, G. Mine] Stanford Univ, Dept Geophys, Stanford, CA 94305 USA; [Brand, Larry] Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine Biol & Fisheries, Miami, FL 33149 USA; [Bronk, Deborah; Diaz, Robert] Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA; [Brookes, Justin] Univ Adelaide, Water Res Cluster, Adelaide, SA 5005, Australia; [Burkholder, Joann M.] N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27695 USA; [Cembella, Allan] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Cochlan, William P.] San Francisco State Univ, Romberg Tiburon Ctr Environm Studies, San Francisco, CA 94920 USA; [Collier, Jackie L.] SUNY Stony Brook, Marine Sci Res Ctr, Stony Brook, NY 11794 USA; [Collos, Yves; Jauzein, Cecile] Univ Montpellier 2, IFREMER, CNRS, Lab Ecosyst Lagunaires UMR 5119, F-34095 Montpellier 5, France; [Doblin, Martina] Univ Technol Sydney, Dept Environm Sci, Sydney, NSW 2007, Australia; [Drennen, Thomas; Kana, Austin A.] Hobart & William Smith Coll, Dept Econ, Geneva, NY 14456 USA; [Drennen, Thomas; Kana, Austin A.] Hobart & William Smith Coll, Dept Environm Studies, Geneva, NY 14456 USA; [Fukuyo, Yasuwo] Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, Tokyo 1138657, Japan; [Furnas, Miles] Australian Inst Marine Sci, Water Qual & Ecosyst Hlth Team, Townsville, Qld 4810, Australia; [Galloway, James] Univ Virginia, Dept Environm Sci, Charlottesville, VA 22903 USA; [Graneli, Edna; Legrand, Catherine; Solomon, Caroline] Univ Kalmar, Dept Marine Sci, Kalmar 39182, Sweden; [Ha, Dao Viet] Inst Oceanog, Nhatrang City, Vietnam; [Hallegraeff, Gustaaf] Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia; [Harrison, John] Washington State Univ, Sch Earth & Environm Sci, Vancouver, WA 98686 USA; [Harrison, Paul J.] Hong Kong Univ Sci & Technol, Atmospher Marine & Coastal Environm Program, Kowloon, Hong Kong, Peoples R China; [Heil, Cynthia A.] Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, St Petersburg, FL 33701 USA; [Heimann, Kirsten] James Cook Univ, Sch Marine & Trop Biol, Townsville, Qld 4811, Australia; [Howarth, Robert] Cornell Univ, Dept Ecol & Evolutionary Biol, Ithaca, NY 14853 USA; [Kim, Hakgyoon] Pukyong Natl Univ, Dept Ocean Sci, Pusan, South Korea; [Kudela, Raphael] Univ Calif Santa Cruz, Ocean Sci & Inst Marine Sci, Santa Cruz, CA 95064 USA; [Mallin, Michael] Univ N Carolina Wilmington, Ctr Marine Sci, Wilmington, NC 28409 USA; [Mulholland, Margaret] Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA; [Murray, Shauna] Univ Sydney, Sch Biol Sci, Sydney, NSW 2006, Australia; [Pitcher, Grant] Marine & Coastal Management, Cape Town, South Africa; [Qi, Yuzao] Jinan Univ, Res Ctr Harmful Algae & Aquat Environm, Guangzhou 510632, Guangdong, Peoples R China; [Rabalais, Nancy] Louisiana Univ Marine Consortium, Chauvin, LA 70344 USA; [Raine, Robin] Natl Univ Ireland, Martin Ryan Inst, Galway, Ireland; [Seitzinger, Sybil] State Univ New Jersey, NOAA CMER, Inst Marine & Coastal Sci, New Brunswick, NJ 08901 USA; [Solomon, Caroline] Gallaudet Univ, Dept Biol, Washington, DC 20002 USA; [Usup, Gires] Univ Kebangsaan Malaysia, Fac Sci & Technol, Bangi 43600, Selangor, Malaysia; [Wilson, Joanne] Nature Conservancy, Coral Triangle Ctr, Sanur 80228, Bali, Indonesia; [Zhou, Mingjiang] Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China; [Zhu, Mingyuan] First Inst Oceanog, Qingdao 266071, Peoples R China	University System of Maryland; University of Maryland Center for Environmental Science; University of the Philippines System; University of the Philippines Diliman; Griffith University; University of Tokyo; Healthy Waterways; Kuwait Institute for Scientific Research; Woods Hole Oceanographic Institution; Monash University; Stanford University; University of Miami; William & Mary; Virginia Institute of Marine Science; University of Adelaide; North Carolina State University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; California State University System; San Francisco State University; State University of New York (SUNY) System; Stony Brook University; Centre National de la Recherche Scientifique (CNRS); Ifremer; Universite de Montpellier; University of Technology Sydney; University of Tokyo; Australian Institute of Marine Science; University of Virginia; Linnaeus University; University of Kalmar; University of Tasmania; Washington State University; Hong Kong University of Science & Technology; Florida Fish & Wildlife Conservation Commission; James Cook University; Cornell University; Pukyong National University; University of California System; University of California Santa Cruz; University of North Carolina; University of North Carolina Wilmington; Old Dominion University; University of Sydney; Jinan University; Ollscoil na Gaillimhe-University of Galway; National Oceanic Atmospheric Admin (NOAA) - USA; Rutgers University System; Rutgers University New Brunswick; Universiti Kebangsaan Malaysia; The Nature Conservancy Indonesia; Nature Conservancy; Chinese Academy of Sciences; Institute of Oceanology, CAS; First Institute of Oceanography, Ministry of Natural Resources	Glibert, PM (通讯作者)，Univ Maryland, Ctr Environm Sci, Horn Point Lab, POB 775, Cambridge, MD 21613 USA.	glibert@hpl.umces.edu; rhodaazanza@yahoo.com; m.burford@griffith.edu.au; furuya@fs.a.u-tokyo.ac.jp; e.abal@uq.edu.au; adnazri@squ.edu.om; fyamani@safat.kisr.edu.kw; pea@orbicon.dk; danderson@whoi.edu; john.beardall@sci.monash.edu.au; mineberg@stanford.edu; lbrand@rsmas.miami.edu; bronk@vims.edu; justin.brookes@adelaide.edu.au; jburk@ncsu.edu; Allan.Cembella@awi.de; cochlan@sfsu.edu; jcollier@notes.cc.sunysb.edu; Yves.Collos@univ-montp2.fr; diaz@vims.edu; Martina.Doblin@uts.edu.au; drennen@hws.edu; sdyhrman@whoi.edu; ufukuyo@mail.ecc.u-tokyo.ac.jp; m.furnas@aims.gov.au; jng@virginia.edu; edna.graneli@hik.se; tmmp_vno-cean@ng.vnn.vn; Hallegraeff@utas.ed; harrisoj@vancouver.wsu.edu; harrison@ust.hk; Cindy.Heil@MyFWC.com; rsten.Heimann@jcu.edu.au; rwh2@cornell.edu; cjauzein@univ-montp2.fr; austin.kana@hws.edu; kana@hpi.umces.edu; hgkim7592@yahoo.com.kr; kudela@ucsc.edu; catherine.legrand@hik.se; mallinm@uncw.edu; mmulholl@odu.edu; smurray@bio.usyd.edu.au; joneil@hpl.umces.edu; Gpitcher@deat.gov.za; tql@jnu.edu.cn; nrabalais@lumcon.edu; robin.raine@nuigalway.ie; sybil@marine.rutgers.edu; paulo.salomon@hik.se; caroline.solomon@gallaudet.edu; stoecker@hpl.umces.edu; giresusup@yahoo.com; jowilson67@gmail.com; k.yin@griffith.edu.au; mjzhou@ms.qdio.ac.cm; zhumingyuan@fio.org.cn	Galloway, James/C-2769-2013; Murray, Shauna/JAN-6668-2023; stoecker, diane/F-9341-2013; Graneli, Edna/F-5936-2015; Beardall, John/L-5262-2019; Kana, Austin/AAD-5417-2019; Ha, Dao Viet/JMQ-4044-2023; Brookes, Justin/G-4270-2013; Collier, Jackie/AFF-7928-2022; Rabalais, Nancy/GQA-6087-2022; Mingyuan, Zhu/H-6247-2013; Salomon, Paulo/D-3310-2011; Azanza, Rhodora/HGU-5811-2022; Yin, Kedong/B-9773-2009; Heimann, Kirsten/M-4814-2019; Heimann, Kirsten/N-1512-2013; Doblin, Martina/E-8719-2013; Beardall, John/A-1250-2008; Hallegraeff, Gustaaf/C-8351-2013; Glibert, Patricia/G-1026-2013; Mulholland, Margaret/E-8480-2011; Burford, Michele/A-3138-2012; Murray, Shauna A/K-5781-2015; Harrison, John/F-2280-2011; O'Neil, Judith M./F-9024-2013	Heimann, Kirsten/0000-0003-2691-9659; Collier, Jackie/0000-0001-8774-5715; Howarth, Robert/0000-0001-9531-4288; Doblin, Martina/0000-0001-8750-3433; Beardall, John/0000-0001-7684-446X; Hallegraeff, Gustaaf/0000-0001-8464-7343; Jauzein, Cecile/0000-0001-6291-6821; Glibert, Patricia/0000-0001-5690-1674; Galloway, James/0000-0001-7676-8698; Solomon, Caroline/0000-0002-5083-4041; Brookes, JUSTIN/0000-0001-8408-9142; Mulholland, Margaret/0000-0001-8819-189X; Burford, Michele/0000-0002-1076-6144; Murray, Shauna A/0000-0001-7096-1307; Rabalais, Nancy N./0000-0002-1514-837X; Harrison, John/0000-0002-0677-5478; furuya, ken/0000-0002-3507-5489; Cembella, Allan/0000-0002-1297-2240; O'Neil, Judith M./0000-0002-7697-5299				Anderson D.M., 2004, Oceanus, V43, P1; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 2003, MANUAL HARMFUL MARIN, P165; ANING J, 2007, INQUIRER        1110; AZAM F, 1983, MAR ECOL PROG SER, V10, P257, DOI 10.3354/meps010257; 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JUN	2008	56	6					1049	1056		10.1016/j.marpolbul.2008.03.010	http://dx.doi.org/10.1016/j.marpolbul.2008.03.010			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	322LU	18439628	Green Accepted, Green Submitted			2025-03-11	WOS:000257377400014
J	Wijnker, E; Bor, TJ; Wesselingh, FP; Munsterman, DK; Brinkhuis, H; Burger, AW; Vonhof, HB; Post, K; Hoedemakers, K; Janse, AC; Taverne, N				Wijnker, E.; Bor, T. J.; Wesselingh, F. P.; Munsterman, D. K.; Brinkhuis, H.; Burger, A. W.; Vonhof, H. B.; Post, K.; Hoedemakers, K.; Janse, A. C.; Taverne, N.			Neogene stratigraphy of the Langenboom locality (Noord-Brabant, the Netherlands)	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						Breda Formation; mill; Miocene; North Sea Basin; Oosterhout Formation; Pliocene	NORTH-SEA BASIN; DINOFLAGELLATE CYST; UPPER MIOCENE; PLIOCENE; BELGIUM; PLEISTOCENE; AGE	The locality of Langenboom (eastern Noord-Brabant, the Netherlands), also known as Mill, is famous for its Neogene molluscs, shark teeth, teleost remains, birds and marine mammals. The stratigraphic context of the fossils, which have been collected from sand suppletions, was hitherto poorly understood. Here we report on a section which has been sampled by divers in the adjacent flooded sandpit 'De Kuilen' from which the Langenboom sands have been extracted. The studied section covers part of the marine Miocene Breda Formation and Pliocene Oosterhout Formation, and is topped by fluvial Quaternary deposits of presumably the Beegden Formation. The Breda Formation (15 - 18 m below lake surface) in this section is, based on organic walled dinoflagellate cysts, of an early-middle Tortonian age. The Oosterhout Formation (7 - 15 m below lake surface) comprises two depositional sequences, the lower of which (12 - 15 m below lake surface) presumably is the source of most Langenboom fossils. Combined dinoflagellate cyst and benthic mollusc indicators point to an early Zanclean - early Piacenzian age for this lower cycle. Its basal transgressive lag and (to lesser extent) top comprise reworked Tortonian taxa as well. Dinoflagellate cysts and a single benthic mollusc point to a Piacenzian age for the upper Oosterhout Formation sequence (7 - 12 m below lake surface).	[Wijnker, E.] Univ Wageningen & Res Ctr, Genet Lab, NL-6703 BD Wageningen, Netherlands; [Wesselingh, F. P.] Naturalis, NL-2300 RA Leiden, Netherlands; [Munsterman, D. K.] TNO B&O Natl Geol Survey, NL-3508 TA Utrecht, Netherlands; [Brinkhuis, H.] Univ Utrecht, Palaeobot & Palynol Lab, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; [Vonhof, H. B.] Vrije Univ Amsterdam, Fac Earth & Life Sci, NL-1081 EH Amsterdam, Netherlands; [Post, K.] Nat Museum Rotterdam, NL-3001 KL Rotterdam, Netherlands	Wageningen University & Research; Naturalis Biodiversity Center; Netherlands Organization Applied Science Research; Utrecht University; Vrije Universiteit Amsterdam	Wijnker, E (通讯作者)，Univ Wageningen & Res Ctr, Genet Lab, Arboretumlaan 4, NL-6703 BD Wageningen, Netherlands.	erik.wijnker@wur.nl	Brinkhuis, Henk/B-4223-2009; Wijnker, Erik/H-4816-2011; Wesselingh, Frank/C-1367-2018	Wesselingh, Frank/0000-0003-3655-0701; Vonhof, Hubert/0000-0002-0897-8244; Brinkhuis, Henk/0000-0003-0253-6610				ADAMS CG, 1977, NATURE, V269, P383, DOI 10.1038/269383a0; AHRENS H, 2003, KIES MASTODONT ANANC; AHRENS H, 2004, VIER NIEUWE FOSSIELE; Ahrens Hansjorg, 2005, Cranium, V22, P41; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; BURGER AW, 2006, MOLLUSKEN GROEVE KUI; Cadee M.C., 1988, Afzettingen Werkgroep voor Tertiaire en Kwartaire Geologie, V9, P3; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; De Schepper S., 2006, THESIS U CAMBRIDGE; De Vos J., 2006, CAINOZOIC RES, V5, P107; Doppert J.W. 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J. Geosci.	JUN	2008	87	2					165	180		10.1017/S0016774600023209	http://dx.doi.org/10.1017/S0016774600023209			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	316LJ		Bronze			2025-03-11	WOS:000256950800003
J	Heilmann-Clausen, C; Abrahamsen, N; Larsen, M; Piasecki, S; Stemmerik, L				Heilmann-Clausen, Claus; Abrahamsen, Niels; Larsen, Michael; Piasecki, Stefan; Stemmerik, Lars			Age of the youngest Paleogene flood basalts in East Greenland	NEWSLETTERS ON STRATIGRAPHY			English	Article						Eocene; flood basalts; Greenland; stratigraphy; dinoflagellate cysts	TERTIARY BASALTS; BIOSTRATIGRAPHY; INDICATORS; VOLCANISM; MARGIN	Intra-basaltic sediments 50 m below the top of the Paleogene lava succession at Kap Dalton, East Greenland, contain dinoflagellate cysts of late Ypresian-earliest Lutetian age, while sediments immediately above the lavas contain an assemblage of early Lutetian age. Combined with paleomagnetic results, this constrains the termination of the East Greenland Paleogene Igneous Province to the Early-Middle Eocene transition (nannoplankton chronozones NP13-NP14/earliest NP15). This is 6-8 Ma younger than according to previous biostratigraphic age assignments. The new data show that flood basalt volcanism occurred simultaneously with major intrusions occurring further to the south. This corroborates previous assumptions of an important melting event much younger than the continental break-up.	[Heilmann-Clausen, Claus; Abrahamsen, Niels] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Larsen, Michael; Piasecki, Stefan; Stemmerik, Lars] Geol Surg Denmark & Greenland, DK-1350 Copenhagen K, Denmark	Aarhus University; Geological Survey Of Denmark & Greenland	Heilmann-Clausen, C (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	claus.heilmann@geo.au.dk; abraham@geo.au.dk; sp@geus.dk; micla@dongenergy.dk; ls@geo.ku.dk	Abrahamsen, Niels/A-3553-2012; Heilmann-Clausen, Claus/A-4848-2012; Stemmerik, Lars/A-9217-2013	Stemmerik, Lars/0000-0002-8374-6400				[Anonymous], MICROPALAEONTOLOGICA; [Anonymous], 1980, PALAEONTOLOGY; Bernstein S, 1998, EARTH PLANET SC LETT, V160, P845, DOI 10.1016/S0012-821X(98)00132-0; Boulter M.C., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P663, DOI 10.2973/odp.proc.sr.104.192.1989; Brinkhuis H, 2006, NATURE, V441, P606, DOI 10.1038/nature04692; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak J., 1980, PALAEONTOLOGICAL ASS, V24, P1; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; COLLINSON ME, 1985, J GEOL SOC LONDON, V142, P375, DOI 10.1144/gsjgs.142.2.0375; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; de Coninck J., 1977, Mededelingen Rijks Geologische Dienst, V28, P33; Eaton GL., 1976, B BRIT MUS NAT HIST, V26; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; FOWLER K, 1975, Palaeontology (Oxford), V18, P483; Hansen H, 2002, GEOL SOC SPEC PUBL, V197, P183, DOI 10.1144/GSL.SP.2002.197.01.08; Heilmann-Clausen C., 1989, Geol. 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R., 1947, MEDD GRONLAND, V134, P1	41	6	6	0	4	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0078-0421			NEWSL STRATIGR	Newsl. Stratigr.	JUN	2008	43	1					55	63		10.1127/0078-0421/2008/0043-0055	http://dx.doi.org/10.1127/0078-0421/2008/0043-0055			9	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	331HT					2025-03-11	WOS:000258004000008
J	Piot, A; Rochon, A; Stora, G; Desrosiers, G				Piot, Adeline; Rochon, Andre; Stora, Georges; Desrosiers, Gaston			Experimental study on the influence of bioturbation performed by <i>Nephtys caeca</i> (Fabricius) and <i>Nereis virens</i> (Sars) annelidae on the distribution of dinoflagellate cysts in the sediment	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Review						bioturbation; dinoflagellate cysts; Nephtys caeca; Nereis virens; optical reworking coefficient	MACOMA-BALTHICA COMMUNITY; RESTING CYSTS; GONYAULAX-TAMARENSIS; DEPOSIT-FEEDERS; SPRING BLOOM; IN-SITU; GERMINATION; TEMPERATURE; ESTUARINE; REWORKING	Dinoflagellates include noxious microalgae responsible for the formation of toxic red tides and the poisoning of molluscs and crustaceans, resulting in important economic losses. As a consequence, the life cycle of these algae has been extensively studied, but the dormancy phase (cyst) in the sediment record is little known. In the intertidal zone, bioturbation, an important biological process resulting from the activities of benthic fauna, significantly influences the movement of particles in the sediments. Laboratory experiments have allowed comparing and quantifying the movements of fluorescent microspheres resulting from the activity of two polychaetes annelidae, Nereis virens and Nephtys caeca. The particles, which simulate 45 mu m diameter dinoflagellate cysts, are deposited in flat aquaria at the surface or deep in the sediment. Photographs of the aquaria were taken at regular intervals, to observe, in a non-destructive manner, the movement of the particles and to calculate, using adapted software, the optical reworking coefficient (ORC) over time. A difference appears between the movements of the particles generated by both species of polychaetes. Nereis virens create "permanent" galleries that carry the microspheres deeply in the sediment during the digging, bioirrigation and feeding, and Nephtys caeca homogenize the particles in the first centimetres of sediment during its erratic movements. The study shows that the bioturbation generated by these organisms can modify the distribution of the 45 mu m diameter dinoflagellate cysts in the sedimentary column, burying them or raising them back to the water-sediment interface. (C) 2008 Elsevier B.V. All rights reserved.	[Piot, Adeline; Rochon, Andre; Desrosiers, Gaston] UQAR ISMER, Rimouski, PQ G5L 3A1, Canada; [Stora, Georges] LMGEM, F-13288 Marseille, France	University of Quebec; Universite du Quebec a Rimouski	Piot, A (通讯作者)，UQAR ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	adeline.piot@uqar.qc.ca						Aller R. 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Exp. Mar. Biol. Ecol.	MAY 9	2008	359	2					92	101		10.1016/j.jembe.2008.02.023	http://dx.doi.org/10.1016/j.jembe.2008.02.023			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	313MA					2025-03-11	WOS:000256743500002
J	Louwye, S; Foubert, A; Mertens, K; Van Rooij, D				Louwye, Stephen; Foubert, Anneleen; Mertens, Kenneth; Van Rooij, David		IODP Expedition 307 Sci Party	Integrated stratigraphy and palaeoecology of the lower and Middle Miocene of the Porcupine Basin	GEOLOGICAL MAGAZINE			English	Article						Porcupine Basin; dinoflagellate cysts; magnetostratigraphy; palaeoenvironment; Miocene; IODP Expedition 307	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; WATER CORAL BANKS; NORTHERN BELGIUM; SEA-LEVEL; ATLANTIC; PLIOCENE; ASSEMBLAGES; PROGRAM; CLIMATE; OCEAN	A high-resolution palynological analysis and a detailed palaeomagnetic study of a marine sequence recovered during IODP Expedition Leg 307 in the Porcupine Basin southwest of Ireland provide new insights into the regional depositional history and palaeoenvironmental evolution during Early Neogene times. The Hole 1318B studied was drilled on the upper slope of the continental margin in a water depth of 409 in, upslope from a province of carbonate mounds (the Belgica mound province). The diverse and well-preserved dinoflagellate cyst associations consist typically of deep neritic and oceanic species, mixed with a neritic component transported from the shelf, reflecting the deep depositional setting at the continental margin. The palaeomagnetic record together with the ranges of key dinoflagellate cyst species constrain the age of the studied sequence between 16.7 Ma and 12.01 Ma, that is, between the late Burdigalian and late Serravallian. The distinct unconformity terminating the Miocene sequence correlates to the global sequence boundary Ser4/Tor1 dated at 10.5 Ma, and represents, according to previous extensive seismic studies, a basin-wide erosional event. The overlying sediments are of Middle Pleistocene or younger age. Downslope from IODP Site 1318, carbonate mounds root on the erosional surface. The dinoflagellate cyst associations from the Porcupine Basin distinctly mirror the global cooling phase following the Middle Miocene Climatic Optimum. Cooling phase NIB, a short-lived glaciation, is particularly well expressed and here dated at 13.6 Ma. The palynomorph record furthermore indicates a reduction of the productivity and an increase of oceanic oligotrophic species after 14 Ma, suggesting a reduction or perhaps even a shutdown of the upwelling.	[Louwye, Stephen; Mertens, Kenneth] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Foubert, Anneleen; Van Rooij, David] Univ Ghent, Renard Ctr Marine Geol, B-9000 Ghent, Belgium	Ghent University; Ghent University	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	Stephen.Louwye@UGent.be	Mertens, Kenneth/AAO-9566-2020; Van Rooij, David/A-7938-2014; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015; Foubert, Anneleen/F-7245-2019	Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483; Foubert, Anneleen/0000-0002-9011-9683				Abels HA, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2004PA001129; [Anonymous], PROFONDEURS MER; [Anonymous], OCEAN BIOCOENOSIS SE; Boessenkool KP, 2001, GLOBAL PLANET CHANGE, V30, P33, DOI 10.1016/S0921-8181(01)00075-3; Böhme M, 2003, PALAEOGEOGR PALAEOCL, V195, P389, DOI 10.1016/S0031-0182(03)00367-5; BROWN S, 1985, INITIAL REP DEEP SEA, V80, P643; Cortese G, 2004, EARTH PLANET SC LETT, V224, P509, DOI 10.1016/j.epsl.2004.05.035; COSTA LI, 1979, INITIAL REPORTS DEEP, P513; DALE AL, 1996, PALYNOLOGY PRINCIPLE, V3, P1249; Dale B, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P207; De Mol B, 2002, MAR GEOL, V188, P193, DOI 10.1016/S0025-3227(02)00281-5; De Verteuil L., 1996, P OCEAN DRILLING PRO, V150, P439; de Verteuil Laurent, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P129; DEGRACIANSKY PC, 1985, INITIAL REPORTS DEEP, V80, P33; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; EDWARDS LE, 1984, INITIAL REP DEEP SEA, V81, P581; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; FERLMAN TG, 2006, P INTEGRATED OCEAN D, V307, P1; Florindo F, 2003, GEOCHEM GEOPHY GEOSY, V4, DOI 10.1029/2003GC000516; Foubert A, 2005, ERLANGEN EARTH C SER, P403, DOI 10.1007/3-540-27673-4_20; Gradstein F. 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Mag.	MAY	2008	145	3					321	344		10.1017/S0016756807004244	http://dx.doi.org/10.1017/S0016756807004244			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	305JZ					2025-03-11	WOS:000256175900002
J	Guerstein, GR; Guler, MV; Williams, GL; Fensome, RA; Chiesa, JO				Guerstein, G. R.; Guler, M. V.; Williams, G. L.; Fensome, R. A.; Chiesa, J. O.			Middle Palaeogene dinoflagellate cysts from Tierra del Fuego, Argentina: biostratigraphy and palaeoenvironments	JOURNAL OF MICROPALAEONTOLOGY			English	Article						Dinoflagellates; Palaeogene; biostratigraphy; palaeoenvironments; Argentina	LATE EOCENE; SCOTIA SEA; STRATIGRAPHY; EVOLUTION; ANTARCTICA; GLACIATION	Palynological data from four surface sections in northern Tierra del Fuego, southern Argentina, provide a biostratigraphical and palaeoenvironmental framework for the lower member of the La Despedida Formation and the Cabo Pena Formation in their type areas. Selected dinoflagellate cyst (dinocyst) events indicate that the age of the lower member of the La Despedida Formation is Middle Eocene and that of the Cabo Pena Formation is Late Eocene-earliest Oligocene. The age assigned to the La Despedida Formation agrees with determinations based on calcareous microfossils, but there is a potential discrepancy regarding the Cabo Pena Formation. According to recent stratigraphic studies, the Cabo Domingo Group, which includes the Cabo Pena Formation, is Late Eocene-Miocene in age. The palynomorph assemblages from the lower member of the La Despedida Formation contain the endemic 'Transantarctic Flora', which reflects marginal marine conditions. The maximum abundance of Enneadocysta spp. reflects more open-sea conditions and a warming event during the late Middle Eocene. The lower part of the Cabo Pena Formation has a high ratio of dinocysts to sporomorphs and an abundance of Nematosphaeropsis lemniscata, Reticulatosphaera actinocoronata and Impagidinium spp., suggesting an oceanic to outer neritic environment. Abundant Gelatia inflata and protoperidiniacean cysts indicate cool surface waters rich in dissolved nutrients. These cold-water markers may reflect the development of the Antarctic Circumpolar Current, an important event in the transition from a greenhouse to an icehouse climate mode. Toward the top of the sections, the lower ratios of dinocysts to sporomorphs, as well as the composition of the dinocyst assemblages, reflect a neritic rather than an oceanic setting. This palynological change may be due to eustatic sea-level lowering caused by cooling during the latest Eocene-earliest Oligocene. A new species, Spiniferites scalenus, is described and the new combination Lingulodinium echinatum proposed; an emendation for the latter species is also proposed.	[Guerstein, G. R.; Guler, M. V.] Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, INGEOSUR, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Williams, G. L.; Fensome, R. A.] Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; [Chiesa, J. O.] Univ Nacl San Luis, Dept Geol, RA-5700 San Luis, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Universidad Nacional de San Luis	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, INGEOSUR, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	gmguerst@criba.edu.ar						[Anonymous], NOVA HEDWIGIA; ARCHANGELSKY S, 1969, Ameghiniana, V6, P181; Barker PF, 2001, EARTH-SCI REV, V55, P1, DOI 10.1016/S0012-8252(01)00055-1; Biddle K., 1986, Assoc. 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Micropalaentol.	MAY	2008	27		1				75	94		10.1144/jm.27.1.75	http://dx.doi.org/10.1144/jm.27.1.75			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	313KJ		hybrid			2025-03-11	WOS:000256739200006
J	Prince, IA; Jarvis, I; Pearce, MA; Tocher, BA				Prince, Iain A.; Jarvis, Ian; Pearce, Martin A.; Tocher, Bruce A.			Dinoflagellate cyst biostratigraphy of the Coniacian-Santonian (Upper Cretaceous): New data from the English Chalk	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						dinoflagellate cysts; Upper Cretaceous; biostratigraphy; chalk; Coniacian; Santonian	CARBON-ISOTOPE STRATIGRAPHY; JAMES-ROSS-ISLAND; SOUTHERN ENGLAND; SEA-LEVEL; GLOBAL CORRELATION; TURONIAN BOUNDARY; NORTHERN GERMANY; LITHOSTRATIGRAPHY; PALYNOLOGY; DELTA-C-13	Results are presented here for the first chalk-based, high-resolution quantitative study of organic-walled dinoflagellate cysts (dinocysts) from the entire Coniacian-Santonian Chalk successions in east Kent and on the Isle of Wight. The lithostratigraphy and dinocyst records (137 taxa) of seven sections are presented, and the stratigraphic ranges of taxa are constrained relative to stage and zonal boundaries, located using extensive macrofossil data. Results are integrated with a previous complementary study of the Isle of Wight Santonian to test and refine existing dinocyst bioevent schemes. Sixteen dinocyst events are proposed as a sequence of biostratigraphic datum levels for the lower Coniacian to uppermost Santonian which, based on average sedimentation rates, represent an average temporal resolution of around 360 kyr. The event stratigraphy forms a basis for the first high-resolution correlation study of quantitative dinocyst data from the Upper Cretaceous of NW Europe. A new genus Culversphaera Prince, Jarvis, Pearce et Tocher gen. nov. is proposed with the new combination Culversphaera velata Prince, Jarvis, Pearce et Tocher gen. et comb. nov. Five new species: Ellipsodinium membraniferum Prince, Jarvis, Pearce et Tocher sp. nov., Senoniasphaera macroreticulata Prince, Jarvis, Pearce et Tocher sp. nov., Senoniasphaera whitenessii Prince, Jarvis, Pearce et Tocher sp. nov., Xenascus spinatus Prince, Jarvis, Pearce et Tocher sp. nov. and X yunii sp. nov, and the new subspecies S. protrusa congrensa Prince, Jarvis, Pearce et Tocher subsp. nov. are described. (c) 2008 Elsevier B.V All rights reserved.	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J	Nikitenko, BL; Pestchevitskaya, EB; Lebedeva, NK; Ilyina, VI				Nikitenko, Boris L.; Pestchevitskaya, Ekaterina B.; Lebedeva, Natalia K.; Ilyina, Vlpa I.			Micropalaeontological and palynological analyses across the Jurassic-Cretaceous boundary on Nordvik Peninsula, Northeast Siberia	NEWSLETTERS ON STRATIGRAPHY			English	Article							DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY; SECTIONS; RUSSIA; BASIN	Results are presented of a high-resolution study of foraminifers, ostracods and marine palynomorphs from the continuous succession of Middle Volgian - Lower Valanginian (Upper Jurassic to Lower Cretaceous) deposits of the Nordvik section (NE Siberia). Six foraminiferal and six dinoflagellate cyst (dinocyst) zones and subzones have been identified. Volgian foraminiferal assemblages (Dorothia tortuosa JF51 zone and Ammodiscus veteranus, Evolutinella emeljanzevi JF52 zone) may be regarded as correlative markers for Arctic regions as they are also observed in Barents Sea shelf sediments and different regions of Siberia. Marine palynomorph assemblages provide a reliable correlation with northern areas of Western Europe and Canada at three stratigraphic levels: (a) the base of the Upper Volgian, (b) the middle of the Berriasian and (c) the lowermost Valanginian. The stratigraphic position of foraminiferal and dinocyst zones has been analyzed taking into consideration two alternative horizons for the Jurassic-Cretaceous boundary (A - base of the Upper Volgian, B - base of the Boreal Berriasian). Remarkable changes in foraminiferal assemblages and the first occurences of stratigraphically important taxa occur at the base of the Gaudryina gerkei, Ammobaculites gerkei KF 1 zone, slightly higher than horizon B. The base of the Ammodiscus veteranus, Evolutinella emeljanzevi JF52 zone (slightly below horizon A) is marked by a significant turnover of the characteristic species and dominant taxa. The strongest changes in dinocyst assemblages occur near the base of the Paragonyaulacysta ?borealis, Dingodinium ?spinosum zone (horizon A). The analysis of published macrofauna data and new microfossil information indicates palaeoenvironments ranging from the middle sublittoral to the lower sublittoral.	[Nikitenko, Boris L.; Pestchevitskaya, Ekaterina B.; Lebedeva, Natalia K.; Ilyina, Vlpa I.] Russian Acad Sci, Inst Petr Geol & Geophys, Siberan Branch, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Nikitenko, BL (通讯作者)，Russian Acad Sci, Inst Petr Geol & Geophys, Siberan Branch, Koptyug 3, Novosibirsk 630090, Russia.	NikitenkoBL@ipgg.nsc.ru	Nikitenko, Boris/S-9028-2017; Natalia, Lebedeva/T-6040-2017	Pestchevitskaya, Ekaterina/0000-0001-8174-0737; Natalia, Lebedeva/0000-0002-7192-8303				AARHUS N, 1986, NORSK GEOL TIDSSKR, V66, P17; ARHUS N, 1990, POLAR RES, V8, P165, DOI 10.1111/j.1751-8369.1990.tb00383.x; Basov V.A., 1989, YARUSNYE ZONALNYE SH, P60; BASOV VA, 1991, PRAKTICHESKOE RUKOVO, P210; BASOV VA, 1972, GRANITSA YURY MELA B, P233; BASOV VA, 1970, INFORMATCYONNY B NII, V29, P14; BOGOLEPOV KV, 1983, PALEOGEOGRAPHYA SEVE; BOGOMOLOV YI, 1989, POLYPTYKHITY BIOSTRA; Brideaux W.W., 1976, B GEOLOGICAL SURVEY, V259, P3; Bujak P.J., 1978, GEOLOGICAL SURVEY CA, V297, P1; Cariou E., 1997, Biostratigraphie du Jurassique ouest-europeen et mediterraneen: Zonations paralleles et distribution des invertebres et microfossiles; DAIN LG, 1972, FORAMINIFERY VERKHNE; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; DAVEY RJ, 1982, SPECIAL PUBLICATIO B, V6, P5; DAVIES EH, 1983, B GEOLOGICAL SURVEY, V359, P3; Duxbury S, 1999, GEOL SOC SPEC PUBL, V152, P23, DOI 10.1144/GSL.SP.1999.152.01.03; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Fedorova V.A., 1993, Phanerozoic Stratigraphy of Petroleum Bearing Regions of Russia. 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Inst., P172; Fensome R.A., 1993, Micropaleontology Press Special Paper; FENSOME RA, 2004, LENTIN WILIAMS INDEX; Fisher M.J., 1980, P 4 INT PAL C LUCKN, V2, P313; GOLBERT AV, 1981, OPORNYI RAZREZ NEOKO, V1, P5; GRIGELIS AA, 1982, BIOSTRATIGRAFIA VERK; HAKANSSON E, 1981, Bulletin of the Geological Society of Denmark, V30, P11; HOEDEMAEKER PJ, 1990, GRANITCA YURY MELA, P22; Ilyina V.I., 1988, Palynology in the USSR, P103; Ilyina V.I., 1985, PALINOLOGIYA YURY SI; Jeletzky J.A, 1984, GEOLOGICAL ASS CANAD, V27, P175; Kaplan M.E., 1973, GEOLOGY GEOPHYS, V3, P58; KAPLAN ME, 1973, DOKL AKAD NAUK SSSR+, V209, P691; KRYMHOLTS GY, 1982, ZONY YURSKOY SISTEMY; KRYMHOLTS GY, 1988, GEOLOGICAL SOC AM SP, V223, P5; Lebedeva N.K, 1998, RUSS GEOL GEOPHYS+, V39, P810; Lebedeva NK, 1999, GRANA, V38, P134, DOI 10.1080/00173139908559222; LEBEDEVA NK, 1996, AKTUALNYE VOPROSY GE, P250; MCINTYRE DJ, 1980, GEOL SURV CAN B, V320, P57; PESTCHEVITSKAYA EB, 2000, RUSSIAN GEOLOGY GEOP, V41, P1585; PESTCHEVITSKAYA EB, 2006, PALAEONTOL J S5, V40, pS429; PESTCHEVITSKAYA EB, 2005, SOVREMENNYE PROBLEMY, P245; Pocock S.A.J., 1980, P 4 INT PALYNOLOGICA, V2, P377; Powell A.J., 1992, STRATIGRAPHIC INDEX; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; RAWSON PF, 1982, AAPG BULL, V66, P2628; RAWSON PF, 1990, GRANITCA YURY MELA, P48; REMANE J, 1986, Acta Geologica Hungarica, V29, P15; REMANE J, 1990, GRANITCA YURY MELA, P7; RIDING JB, 1999, AASP CONTRIBUTION SE, V36; Saks V.N., 1963, STRATIGRAFIYA YURSKO; Saks V.N., 1972, GRANITSA YURY MELA B; SAKS VN, 1958, INFORMATCYONNY B NII, V2, P22; SAKS VN, 1976, STRATIGRAFIA YURSKOI; SAKS VN, 1969, OPORNYI RAZREZ VERHN; Sey I. I., 1997, STRATIGR GEOL CORREL, V5, P42; Sey LI, 1999, PALAEOGEOGR PALAEOCL, V150, P49, DOI 10.1016/S0031-0182(99)00007-3; SHAROVSKAYA NV, 1961, RESHENIYA TRUDY MEZH, P171; SHULGINA NI, 1994, CRETACEOUS RES, V15, P1, DOI 10.1006/cres.1994.1001; SHULGINA NI, 1984, POGRANICHNYE YARUSY, P67; SHURYGIN BN, 2000, STRATIGRAPHIYA NEFTE; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; van Helden B.G.T., 1986, Palynology, V10, P181; WIGGINS VD, 1969, MICROPALEONTOLOGY, V15, P3; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zakharov V.A., 1974, PALEOBIOGEOGRAFIYA S, P127; Zakharov VA, 2003, STRATIGR GEO CORREL+, V11, P585; ZAKHAROV VA, 1996, GEOLOGIYA PROBLEMY P, V1, P75; ZAKHAROV VA, 1983, PALEOBIOGEOGRAFIYA B, P56; ZAKHAROV VA, 1997, RUSSIAN GEOLOGY GEOP, V5, P965; ZAKHAROV VA, 1987, CRETACEOUS RES, V19, P35; ZEISS A, 1986, Acta Geologica Hungarica, V29, P27	70	33	40	0	2	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0078-0421			NEWSL STRATIGR	Newsl. Stratigr.	APR 30	2008	42	3					181	222		10.1127/0078-0421/2008/0042-0181	http://dx.doi.org/10.1127/0078-0421/2008/0042-0181			42	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	301TC					2025-03-11	WOS:000255917500002
J	Palci, A; Jurkovsek, B; Kolar-Jurkovsek, T; Caldwell, MW				Palci, Alessandro; Jurkovsek, Bogdan; Kolar-Jurkovsek, Tea; Caldwell, Michael W.			New palaeoenvironmental model for the Komen (Slovenia) Cenomanian (Upper Cretaceous) fossil <i>lagerstitte</i>	CRETACEOUS RESEARCH			English	Article						fossil lagerstatte; Komen limestone; palaeoenvironment; Cenomanian	CALCAREOUS DINOFLAGELLATE CYSTS; CARBONATE FACIES; SEA-LEVEL; PALEOCEANOGRAPHY; RECONSTRUCTION; PALEOECOLOGY; STRATIGRAPHY; RUDISTS; CROATIA; BASIN	Three sections which crop out near Tomacevica (2 km east of Komen), Slovenia, were measured and described. Thirty-seven rock samples were collected for thin section analysis. A database on all the fossils from the Komen area was compiled from collections of the Museo Civico di Storia Naturale in Trieste, Italy, the Museo Geologico Paleontologico G. Capellini in Bologna, Italy, and the Slovenian Museum of Natural History in Ljubljana, Slovenia. The data collected on the stratigraphy, sedimentology and palaeontology of the Komen platy limestones were used to build a new depositional model for the area. This Dew hypothesis is proposed in place of the "lagoonal model", too often invoked in the past in order to explain the occurrence of dark platy limestones occurring worldwide in platform settings. Given the absence of any evidence in support of a true "lagoonal system" in the examined area (e.g. channel fills, herring bone cross stratification, sand bars or bioherms delimiting the area of interest) the latter has been examined in search of an alternative sedimentological model. New data regarding facies succession and faunal composition have been gathered. The typical facies succession of the Komen Limestone comprises: (a) flat pebble breccias that grade up-section into packstones and wackestones containing progressively rarer, and smaller, flat micritic intraclasts; (b) well bedded to platy limestones; and (c) stromatolitic limestones. All of these lithologies contain scattered chert nodules and sheets. The available evidence suggests that the depositional environment of the Komen Limestone was in an intraplatform basin, in the proximity of an exposed area (tidal flat plus probably other supratidal environments populated by conifers and where karstification could occur). The bottom water conditions were periodically dysoxic to anoxic, and the stacking of different facies was due to a combination of small scale sea-level fluctuations and local subsidence of the area. (c) 2007 Elsevier Ltd. All rights reserved.	[Palci, Alessandro] Univ Modena & Reggio Emilia, Dipartimento Museo Paleobiol & Orto Bot, I-41100 Modena, Italy; [Jurkovsek, Bogdan; Kolar-Jurkovsek, Tea] Geol Zavod Slovenije, SI-1000 Ljubljana, Slovenia; [Caldwell, Michael W.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E9, Canada; [Caldwell, Michael W.] Univ Alberta, Dept Biol Sci, Edmonton, AB T6G 2E9, Canada	Universita di Modena e Reggio Emilia; University of Alberta; University of Alberta	Palci, A (通讯作者)，Univ Modena & Reggio Emilia, Dipartimento Museo Paleobiol & Orto Bot, Via Univ N 4, I-41100 Modena, Italy.	apalci@unimore.it	Palci, Alessandro/HJX-9568-2023; Caldwell, Michael/A-2622-2014	Palci, Alessandro/0000-0002-9312-0559; Caldwell, Michael/0000-0002-2377-3925				[Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; [Anonymous], ATTI MUSEO CIVICO ST; [Anonymous], 1999, ESTUD MUS CIENC NAT; BARDACK D, 1965, U KANSAS PALEONTOLOG, V10, P1; BLOT J, 1987, ATT MUS CIV STOR NAT; BOSELLINI A, 1989, ROCCE SUCCESSIONI SE; Buser S, 1968, Osnovna geoloska karta SFRJ 1: 100.000, list Postojna=Basic geological map SFRJ 1: 100.000, sheet Postojna; BUSER S, 1983, TOLMAC LISTA GORICA; Calligaris R., 1988, Atti del Museo Civico di Storia Naturale di Trieste, V41, P85; Cati A., 1987, Mem. 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Res.	APR	2008	29	2					316	328		10.1016/j.cretres.2007.05.003	http://dx.doi.org/10.1016/j.cretres.2007.05.003			13	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	293WW					2025-03-11	WOS:000255367100009
J	Slimani, H; Louwye, S; Toufiq, A; Verniers, J; De Coninck, J				Slimani, Hamid; Louwye, Stephen; Toufiq, Abdelkabir; Verniers, Jacques; De Coninck, Jan			New dinoflagellate cyst species from Cretaceous/Palaeogene boundary deposits at Ouled haddou, south-eastern rif, morocco	CRETACEOUS RESEARCH			English	Article						Cretaceous/Palaeogene boundary; dinollagellate cysts; stratigraphy; Ouled haddon section; south-eastern Rif; northern Morocco	NORTHERN APENNINES; EOCENE; BIOSTRATIGRAPHY; PALEOCENE; ZONATION; ENGLAND; COMPLEX; GENUS	A palynological investigation of the recently described and foraminifera-dated Ouled Haddou section (south-eastern Rif Corridor) in northern Morocco yielded eight new dinoflagellate cyst species within a rich and well-preserved assemblage as follows: Batiacasphaera rifensis, Cerodinium mediterraneum, Damassadinium? spinosum, Eisenackia nisounensis, Impagidiniun? maghribensis, Lejeunecysta izerzenensis, Pterodinium cretaceum and Ynezidinium tazaensis. They are described because they are likely to be important for recognition of the Cretaceous/Palaeogene boundary elsewhere in Morocco and at other locations. (c) 2007 Elsevier Ltd. All rights reserved.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Dept Geol, Rabat 10106, Morocco; [Louwye, Stephen; Verniers, Jacques; De Coninck, Jan] Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium; [Toufiq, Abdelkabir] Univ Chouaib Doukkali, Fac Sci, Lab Geosci & Environm Tech, El Jadida 24000, Morocco	Mohammed V University in Rabat; Ghent University; Chouaib Doukkali University of El Jadida	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Dept Geol, Ave Ibn Batouta,BP 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Verniers, Jacques/B-8024-2009; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Verniers, Jacques/0000-0002-2939-7684; Slimani, Hamid/0000-0001-6392-1913				[Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; [Anonymous], MEMOIRS; [Anonymous], 1831, SYMBOLAE PHYSICAE AN; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Bujak J.P., 1980, SPEC PAP PALAEONTOL, V24, P100; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; Cookson I. 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Res.	APR	2008	29	2					329	344		10.1016/j.cretres.2007.06.003	http://dx.doi.org/10.1016/j.cretres.2007.06.003			16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	293WW					2025-03-11	WOS:000255367100010
J	Matsuoka, K; Iwataki, M; Kawami, H				Matsuoka, Kazumi; Iwataki, Mitsunori; Kawami, Hisae			Morphology and taxonomy of chain-forming species of the genus <i>Cochlodinium</i> (Dinophyceae)	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; Cochlodinium heterolobatum; Cochlodinium catenatum; Cochlodinium convolutum; dinoflagellate; morphology; taxonomy; HAB	POLYKRIKOIDES GYMNODINIALES; COSTA-RICA; RED TIDE; DINOFLAGELLATE; BLOOMS; COAST; CALIFORNIA; CYSTS; USA	The morphology of an unarmored chain-forming harmful dinnoflagellate Cochlodinium polykrikoides and its similar species such as Cochlodinium catenatum, Cochlodinium fulvescens, and Cochlodinium convolutum was carefully observed, emphasizing the single cell stage for clarifying taxonomically important morphological features. To differentiate C. polykrikoides from C. convolutum, the shape and the position of the nucleus are useful characters. C. polykrikoides also differs from C. fulvescens in being smaller in size, possessing many rod-shaped chloroplasts and having the sulcus running just below the cingulum on the dorsal surface. Careful observation of the ichnotype of C. catenatum suggests that C. catenatum sensu Kofoid and Swezy collected from off La Jolla, CA, USA, is not identical to C. catenatum sensu Okamura and is probably a different species, in having no chloroplasts and a nucleus positioned at the center of the cell. In addition, C. polykrikoides has many morphological features in common with C. catenatum sensu Okamura except for slightly elongate cells and is probably a junior synonym of this species. (C) 2008 Elsevier B.V. All rights reserved.	[Matsuoka, Kazumi; Iwataki, Mitsunori] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Kawami, Hisae] Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan	Nagasaki University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@net.nagasaki-u.ac.jp	Iwataki, Mitsunori/H-9640-2019	Iwataki, Mitsunori/0000-0002-5844-2800				ALTAMIRANO RC, 2004, HARMFUL ALGAE 2002, P344; [Anonymous], WORKSH RED TID MON A; Anton A, 2008, HARMFUL ALGAE, V7, P331, DOI 10.1016/j.hal.2007.12.013; Azanza R.V., 2005, Harmful Algae News, V29, P13; AZANZA RV, 2006, P WORKSH REC PROGR R, P27; Bhat SR, 2004, CURR SCI INDIA, V87, P1079; Curtiss CC, 2008, HARMFUL ALGAE, V7, P337, DOI 10.1016/j.hal.2007.12.012; Gárate-Lizárraga I, 2004, REV BIOL TROP, V52, P51; Garate-Lizarraga I., 2000, Harmful Algae News, V21, P7; Gobler CJ, 2008, HARMFUL ALGAE, V7, P293, DOI 10.1016/j.hal.2007.12.006; GUZMAN HM, 1990, MAR ECOL PROG SER, V60, P299, DOI 10.3354/meps060299; HARGRAVES PE, 1981, REV BIOL TROP, V29, P31; Hirasaka K., 1922, ZOOL MAG, V34, P740; Ho M.-S., 1979, P409; Iwataki M, 2008, HARMFUL ALGAE, V7, P271, DOI 10.1016/j.hal.2007.12.003; Iwataki M, 2007, PHYCOL RES, V55, P231, DOI 10.1111/j.1440-1835.2007.00466.x; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; KIM HG, 1998, HARMFUL ALGAL BLOOMS, P20; Kofoid C. A., 1921, Memoirs of the University of California, V5, P1; Kudela RM, 2008, HARMFUL ALGAE, V7, P278, DOI 10.1016/j.hal.2007.12.016; KUDELA RM, 2006, P WORKSH REC PROGR R, P51; KUMADA K, 1980, YATSUSHIRO KAIIKI TA, P125; LU SL, 1999, J JIAOZUO I TECHNOL, V18, P1; MARGALEF RAMON, 1961, INVEST PESQUERA, V18, P33; Matsuoka Kazumi, 2004, Bulletin of Plankton Society of Japan, V51, P38; Morales-Blake Alejandro, 2001, Harmful Algae News, V22, P6; NAKAZAWA K, 1911, ZOOL MAG DOUBTSUGAKU, V272, P304; Nuzzi Robert, 2004, Harmful Algae News, V27, P10; Okamura K., 1916, SUISAN KOUSHU SIKENJ, V12, P26; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; Rosales-Loessener F, 1996, HARMFUL TOXIC ALGAL, P193; SILVA ESTELA DE SOUSA, 1967, J PROTOZOOL, V14, P745, DOI 10.1111/j.1550-7408.1967.tb02072.x; Vargas-Montero M., 2004, Harmful Algae News, V26, P7; YAMATOGI T, 2003, B NAGASAKI PREF I FI, V28, P21; Yuki K., 1989, P451; Zingone A, 2006, HARMFUL ALGAE, V5, P321, DOI 10.1016/j.hal.2005.09.002	36	55	67	2	14	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	APR	2008	7	3					261	270		10.1016/j.hal.2007.12.002	http://dx.doi.org/10.1016/j.hal.2007.12.002			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	278TC		Green Submitted			2025-03-11	WOS:000254308200002
J	Tomas, CR; Smayda, TJ				Tomas, Carmelo R.; Smayda, Theodore J.			Red tide blooms of <i>Cochlodinium polykrikoides</i> in a coastal cove	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; harmful bloom; Narragansett Bay region	DINOFLAGELLATE; GROWTH; DINOPHYCEAE; GYMNODINIALES; WATERS; CYCLE	Successive blooms of the dinoflagellate Cochlodinium polykrikoides occurred in Pettaquamscutt Cove, RI, persisting from September through December 1980 and again from April through October 1981. Cell densities varied from <100 cells L-1 at the onset of the bloom and reached a maximum density exceeding 3.4 x 10(6) cells L-1 during the summer of 1981. The bloom was mainly restricted to the mid to inner region of this shallow cove with greatest concentrations localized in surface waters of the southwestern region during summer/fall periods of both years. Highly motile cells consisting of single, double and multiple cell zooids were found as chains of 4 and 8 cells restricted to the late August/September periods. The highest cell densities occurred during periods when annual temperatures were between 19 and 28 degrees C and salinities between 25 and 30. A major nutrient source for the cove was Crying Brook, located at the innermost region at the head of the cove. Inorganic nitrogen (NH3 and NO2 + NO3) from the brook was continually detectable throughout the study with maximum values of 57.5 and 82.5 mu mol L-1, respectively. Phosphate (PO4-P) was always present in the source waters and rarely <0.5 mu mol L-1; silicate always exceeded 30 mu mol L-1 with maximum concentrations reaching 226 mu mol L-1. Chlorophyll a and ATP concentfations during the blooms varied directly with cell densities. Maximum Chi a levels were 218 mg m(-3) and ATP-carbon was >20 g C m(-3). Primary production by the dinoflagellate-dominated community during the bloom varied between 4.3 and 0.07 g C m(-3) d(-1). Percent carbon turnover calculated from primary production values and ATP-carbon varied from 6 to 129% d(-1). The dinotlagellates dominated the entire summer period; other flagellates and diatoms were present in lesser amounts. A combination of low washout rate due to the cove dynamics, active growth, and life cycles involving cysts allowed C. polykrikoides to maintain recurrent bloom populations in this area. (C) 2007 Elsevier B.V. All rights reserved.	[Tomas, Carmelo R.] Univ N Carolina, Ctr Marine Sci, Wilmington, NC 28409 USA; [Smayda, Theodore J.] Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA	University of North Carolina; University of North Carolina Wilmington; University of Rhode Island	Tomas, CR (通讯作者)，Univ N Carolina, Ctr Marine Sci, 5600 Marvin K Moss Lane, Wilmington, NC 28409 USA.	tomasc@uncw.edu						BURKHOLD.PR, 1967, B MAR SCI, V17, P1; CHEER S, 1974, ANAL BIOCHEM, V60, P102, DOI 10.1016/0003-2697(74)90134-1; EPPLEY RW, 1971, LIMNOL OCEANOGR, V16, P741, DOI 10.4319/lo.1971.16.5.0741; ESILVA ES, 1967, J PROTOZOOL, V14, P745; Furnas MJ, 1989, MARINE NATURE, V2, P79; Furnas MJ, 1990, MARINE NATURE, V3, P9; Gaines A. 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J	Pielou, EC				Pielou, E. C.			Plankton, from the last ice age to the year 3007	ICES JOURNAL OF MARINE SCIENCE			English	Article; Proceedings Paper	4th International Zooplankton Production Symposium	MAY 28-JUN 01, 2007	Hiroshima, JAPAN			Canada; ice age; palaeoecology; plankton; time-series; trends	ABRUPT CLIMATE CHANGES; OCEAN; MACKENZIE; BIOMASS; FUTURE; HOLE; SEA	Climate forcing of the environment and biota has been happening since time immemorial, human forcing only for the past 200 years or so. This paper considers, first, climatic changes over the past 30 000 years, as indicated by plankton and their effects on plankton. Only fossilizable plankton can be observed: principally foraminifera, radiolaria, and pteropods in the zooplankton, and their food, principally coccolithophores, diatoms, and dinoflagellate cysts, in the phytoplankton. The soft-bodied zooplankton species-especially copepods-that lived with them can only be inferred. Large, abrupt climate changes took place, aided by positive feedback. Second, this paper attempts to predict how human forcing in the form of anthropogenic climate change is likely to affect marine ecosystems in the future. Past predictions have underestimated the speed at which warming is actually happening: positive feedback has been unexpectedly strong. Thus, the melting of snow and ice, by reducing the earth's albedo, has increased the amount of solar energy absorbed. Also, warming of the surface (water and land) has caused outgassing of methane from buried clathrates (hydrates), and methane is a strong greenhouse gas. Currently, predictions emphasize one or the other of two contrasted alternatives: abrupt cooling caused by a shutdown of the thermohaline circulation (the "ocean conveyor") or abrupt warming caused by copious outgassing of methane. Both arguments (the former from oceanographers and the latter from geophysicists) are equally persuasive, and I have chosen to explore the methane alternative, because I am familiar with an area (the Beaufort Sea and Mackenzie Delta) where outgassing has recently (2007) been detected and is happening now: in the Arctic Ocean and the Canadian Arctic Archipelago, where disappearance of the ice will affect currents, temperature, thermocline, salinity, upwelling, and nutrients, with consequent effects on the zooplankton.			Pielou, EC (通讯作者)，335 Pritchard Rd, Comox, BC V9M 2Y8, Canada.	piefouec@uniserve.com						Alley R.B., 2000, The two-mile time machine; Alley RB, 2000, P NATL ACAD SCI USA, V97, P1331, DOI 10.1073/pnas.97.4.1331; [Anonymous], 1991, ICE AGE RETURN LIFE, DOI DOI 10.7208/CHICAGO/9780226668093.001.0001; [Anonymous], 1983, Special Paper 26; BECKER L, EOS T AM GEOPHYS UNI, P88; Bishop JKB, 2002, SCIENCE, V298, P817, DOI 10.1126/science.1074961; BLASCO SM, 2006, P ANN M ATL GEOSC SO; Broecker W.S., 1999, GSA Today, V9, P1; Broecker WS, 2003, SCIENCE, V300, P1519, DOI 10.1126/science.1083797; CLAYTON L, 1983, CLACIAL LAKE AGASSIZ, P291; DALLIMORE SR, 1995, GEOLOGY, V23, P527, DOI 10.1130/0091-7613(1995)023<0527:IGHFAD>2.3.CO;2; Fabry VJ, 2008, ICES J MAR SCI, V65, P414, DOI 10.1093/icesjms/fsn048; Gradinger R, 1999, DEEP-SEA RES PT II, V46, P1457, DOI 10.1016/S0967-0645(99)00030-2; Grousset FE, 2001, PALEOCEANOGRAPHY, V16, P240, DOI 10.1029/2000PA000559; Hemming SR, 2004, REV GEOPHYS, V42, DOI 10.1029/2003RG000128; Hendy IL, 2000, PALEOCEANOGRAPHY, V15, P30, DOI 10.1029/1999PA000413; Hooff RC, 2006, LIMNOL OCEANOGR, V51, P2607, DOI 10.4319/lo.2006.51.6.2607; Hughen KA, 1996, NATURE, V380, P51, DOI 10.1038/380051a0; Keigwin LD, 2006, GEOLOGY, V34, P861, DOI 10.1130/G22712.1; Kennett JP, 2000, SCIENCE, V288, P128, DOI 10.1126/science.288.5463.128; KENNETT JP, 2007, EOS T AM GEOPHYS UN, V88, P23; LORIUS C, 1990, NATURE, V347, P139, DOI 10.1038/347139a0; MACKAY JR, 1988, ARCTIC, V41, P267; MACKAY JR, 1994, CANADA TERRA, V106, P1; MATSCH CL, 1983, GEOLOGICAL ASS CANAD, V26, P231; Paull CK, 2007, GEOPHYS RES LETT, V34, DOI 10.1029/2006GL028331; Pickard G.L., 1990, Descriptive Physical Oceanography, V5th; Stocker TF, 1999, INT J EARTH SCI, V88, P365, DOI 10.1007/s005310050271; Wadhams P, 2004, OCEANOGR MAR BIOL, V42, P1	29	3	3	0	22	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	1054-3139	1095-9289		ICES J MAR SCI	ICES J. Mar. Sci.	APR	2008	65	3					296	301		10.1093/icesjms/fsn008	http://dx.doi.org/10.1093/icesjms/fsn008			6	Fisheries; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Fisheries; Marine & Freshwater Biology; Oceanography	304SU		Bronze			2025-03-11	WOS:000256130200003
J	Chu, G; Sun, Q; Rioual, P; Boltovskoy, A; Liu, Q; Sun, P; Han, J; Liu, J				Chu, Guoqiang; Sun, Qing; Rioual, Patrick; Boltovskoy, Andres; Liu, Qiang; Sun, Peiqi; Han, Jintai; Liu, Jiaqi			Dinocyst microlaminations and freshwater "red tides" recorded in Lake Xiaolongwan, northeastern China	JOURNAL OF PALEOLIMNOLOGY			English	Article						dinocyst microlamination; sediment trap; dinocyst flux; radiometric dating; red tide history	DINOFLAGELLATE CYST ASSEMBLAGES; SEXUAL REPRODUCTION; PERIDINIUM-CINCTUM; VARVED SEDIMENTS; ENCLOSURE EXPERIMENTS; ENVIRONMENTAL-FACTORS; LAMINATED SEDIMENTS; SPECIES COMPOSITION; JILIN PROVINCE; DINOPHYCEAE	We reported a special type of lamination formed in the sediments of Lake Xiaolongwan, northeastern China. The lamination consists of light- and brown-colored laminate couplets in the thin sections. The brown-colored layer is composed mainly of dinoflagellate cysts. The grey-colored layer consists of other organic and siliceous matter (plant detritus, diatoms, chrysophyte cysts) and clastics. Preliminary sediment trap results show that a distinct peak of dinocyst flux occurred in November. The dinocyst flux maximum also corresponds to the peaks of diatom flux and chrysophyte stomatocyst flux. These suggest that "red tide blooms" occur in this freshwater lake. We speculate that the dinocyst flux maximum could be related to autumn overturn due to increased nutrients, and the availability of cysts for germination from the lake bottom. Additionally, it may also reflect increasing dissolved organic matter after leaf fall. An independent chronology derived from Cs-137 and (210) Pb shows a good agreement with counted laminations. From the sediment trap data and the independent chronology data, the dinocyst microlaminae appear to be annually laminated, and probably could be called dinocyst varves. Although vegetative (thecate stage) cells of Peridinium volzii and Ceratium furcoides are found in the water samples, it is not possible to relate the dinocysts to these two dinoflagellate species. Based on morphological and ecological analyses, we suggested that they have affinities with species of Peridinium (sensu lato), most probably to P. inconspicuum. Detailed investigations should be carried out to understand the red tide history in this freshwater lake. Annually laminated dinocyst microlayers in freshwater and marine sediments not only provide an uncommon archive for understanding the history of red tides and harmful algal blooms, and why and how certain species periodically bloom over several thousands years, but also provide important records of paleoenvironmental and paleoclimatic changes at seasonal to annual resolution.	[Chu, Guoqiang; Rioual, Patrick; Liu, Qiang; Han, Jintai; Liu, Jiaqi] Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China; [Sun, Qing] Natl Res Ctr Geoanal, Beijing, Peoples R China; [Boltovskoy, Andres] Museo La Plata, Dept Cientifico Ficol, RA-1900 La Plata, Argentina; [Sun, Peiqi] Longwan Natl Nat Protect Bur, Huinan 135102, Jilin, Peoples R China	Chinese Academy of Sciences; Institute of Geology & Geophysics, CAS; National University of La Plata; Museo La Plata	Chu, G (通讯作者)，Chinese Acad Sci, Inst Geol & Geophys, Beijing 100029, Peoples R China.	chuguoqiang@mail.igcas.ac.cn	Rioual, Patrick/H-5140-2018	Rioual, Patrick/0000-0001-9491-9197				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON RY, 1988, PALAEOGEOGR PALAEOCL, V62, P215, DOI 10.1016/0031-0182(88)90055-7; APPLEBY PG, 1986, HYDROBIOLOGIA, V143, P21, DOI 10.1007/BF00026640; BATTARBEE R.W., 2003, Handbook of Holocene Palaeoecology and Palaeohyrology, P527, DOI DOI 10.1127/NOVA_HEDWIGIA/2015/0263; 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Paleolimn.	APR	2008	39	3					319	333		10.1007/s10933-007-9106-1	http://dx.doi.org/10.1007/s10933-007-9106-1			15	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	277TL					2025-03-11	WOS:000254237500003
J	Gottschling, M; Renner, SS; Meier, KJS; Willems, H; Keupp, H				Gottschling, Marc; Renner, Susanne S.; Meier, K. J. Sebastian; Willems, Helmut; Keupp, Helmut			Timing deep divergence events in calcareous dinoflagellates	JOURNAL OF PHYCOLOGY			English	Article						calcareous nannoplankton; dinoflagellates; K/T boundary; micropaleontology; molecular clock; time estimate	SOUTH ATLANTIC-OCEAN; RIBOSOMAL-RNA; MOLECULAR PHYLOGENY; SCRIPPSIELLA-TROCHOIDEA; EQUATORIAL ATLANTIC; MEDITERRANEAN-SEA; CYST PRODUCTION; FOSSIL RECORD; DINOPHYCEAE; EVOLUTION	Based on morphological and molecular data, calcareous dinoflagellates (Thoracosphaeraceae, Peridiniales) are a monophyletic group comprising the three major clades Ensiculifera/Pentapharsodinium, Thoracosphaera/Pfiesteria, and Scrippsiella sensu lato. We used stratigraphically well-documented first occurrences of particular archeopyle types to constrain relaxed Bayesian molecular clocks applied to nuclear rRNA sequences of 18 representatives of the three main clades. By comparing divergence estimates obtained in differently calibrated clocks with first stratigraphic occurrences of taxa not themselves used as constraints, we identified plausible divergence times for several subclades of calcareous dinoflagellates. The initial diversification of extant calcareous dinoflagellates probably took place in the Late Jurassic, with the three main clades all established by the Cretaceous. The two mesoepicystal operculum types observed in calcareous dinoflagellates probably evolved independently from simple apical archeopyles. Based on our taxon sample, the K/T boundary had relatively little effect on the diversity of the group, with several lineages dating to before 65 mya (million years ago). The first stratigraphic occurrences of key taxa, such as Thoracosphaera and Calciodinellum (not themselves used as constraints), are in agreement with the molecular time estimates. Conflicts that involve "Calciodinellum" levantinum, Leonella, Pentapharsodinium, Pernambugia, and the Scrippsiella trochoidea species complex may be due to inaccurate assignment of fossils because of high morphological homoplasy and insufficient knowledge of the extant diversity of calcareous dinoflagellates.	[Gottschling, Marc; Keupp, Helmut] Free Univ Berlin, Fachrichtung Palaontol, Inst Geol Wissensch, D-12249 Berlin, Germany; [Renner, Susanne S.] Univ Munich, D-80638 Munich, Germany; [Meier, K. J. Sebastian] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany; [Willems, Helmut] Univ Bremen, Fachbereich Geowissensch Hist Geol & Palaontol, D-28359 Bremen, Germany	Free University of Berlin; University of Munich; University of Kiel; University of Bremen	Keupp, H (通讯作者)，Charite Univ Med Berlin, Haut Tumor Ctr Charite, Dermatol Klin, Berlin, Germany.	keupp@zedat.fu-berlin.de	Gottschling, Marc/K-2186-2014; Renner, Susanne/J-8895-2014; Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. 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F., 2005, Palaeontologische Zeitschrift, V79, P61; Zugel Peter, 1994, Courier Forschungsinstitut Senckenberg, V176, P1	83	21	23	1	12	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	APR	2008	44	2					429	438		10.1111/j.1529-8817.2008.00479.x	http://dx.doi.org/10.1111/j.1529-8817.2008.00479.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	288MU	27041198				2025-03-11	WOS:000254991300017
J	Gu, HF; Sun, J; Kooistra, WHCF; Zeng, RY				Gu, Haifeng; Sun, Jun; Kooistra, Wiebe H. C. F.; Zeng, Runying			Phylogenetic position and morphology of thecae and cysts of <i>Scrippsiella</i> (Dinophyceae) species in the East China Sea	JOURNAL OF PHYCOLOGY			English	Article						cysts; dinoflagellate; East China Sea; ITS; S. precaria; S. rotunda; S. trochoidea; Scrippsiella donghaienis	RECENT MARINE-SEDIMENTS; SP-NOV DINOPHYCEAE; DINOFLAGELLATE CYSTS; TROCHOIDEA DINOPHYCEAE; ALEXANDRIUM-TAMARENSE; CALCAREOUS CYSTS; RESTING CYSTS; PERIDINIALES; COAST; CALCIODINELLOIDEAE	Resting cysts of the marine phytoplanktonic dinoflagellate Scrippsiella spp. are encountered in coastal habitats and shallow seas all over the world. Identification of Scrippsiella species requires information on cyst morphology because the plate pattern of the flagellated cell is conserved. Cysts from sediments of the East China Sea were identified based on traits from both the cysts and the thecal patterns of germinated cells. Calcareous cysts belonged predominantly to S. trochoidea (F. Stein) A. R. Loebl., S. rotunda J. Lewis, and S. precaria Montresor et Zingone. The former two species also produced smooth and noncalcified cysts in the field. A new species, S. donghaienis H. Gu sp. nov, was obtained from six noncalcified cysts with organic spines. These cysts are spherical, full of pale white and greenish granules with a mesoepicystal archeopyle. The vegetative cells consist of a conical epitheca and a round hypotheca with a plate formula of po, x, 4', 3a, 7 '', 6c (5c + t), 6 s, 5''', 2'''' and are morphologically indistinguishable from S. trochoidea. Results of internal transcribed spacer (ITS) sequence comparisons revealed that S. donghaienis was distinct from the S. trochoidea complex and appeared nested within the Calciodinellum/Calcigonellum clade. Culture experiments showed that the presence of a red body in the cyst and the shape of the archeopyle were constant within cell lines from one generation to the next, while the morphological features of the cyst wall, such as calcification and spine shape, appeared to be phenotypically plastic.	[Gu, Haifeng; Zeng, Runying] Third Inst Oceanog, Xiamen 361005, Peoples R China; [Sun, Jun] Chinese Acad Sci, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Kooistra, Wiebe H. C. F.] Stn Zool A Dohrn, I-80121 Naples, Italy	Third Institute of Oceanography, Ministry of Natural Resources; Chinese Academy of Sciences; Stazione Zoologica Anton Dohrn	Gu, HF (通讯作者)，Third Inst Oceanog, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	Sun, Jun/A-5254-2009; Gu, Haifeng/ADN-4528-2022	Sun, Jun/0000-0001-7369-7871; Kooistra, Wiebe/0000-0002-8641-9739; Gu, Haifeng/0000-0002-2350-9171				[Anonymous], SEAL SEQUENCE ALIGNM; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; BINDER BJ, 1987, J PHYCOL, V23, P99; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Cho HJ, 2003, BOT MAR, V46, P332, DOI 10.1515/BOT.2003.030; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; GAO XP, 1989, PHYCOLOGIA, V28, P342; Gayoso AM, 2006, HARMFUL ALGAE, V5, P233, DOI 10.1016/j.hal.2004.12.010; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Gomez Fernando, 2005, Acta Botanica Croatica, V64, P129; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Gottschling M, 2005, EUR J PHYCOL, V40, P207, DOI 10.1080/09670260500109046; Gu HF, 2003, ACTA OCEANOL SIN, V22, P407; GUILLARD RRL, 1962, GRAN CAN J MICROBIOL, V8, P229; HALLEGRAEFF GM, 1992, MAR POLLUT BULL, V25, P186, DOI 10.1016/0025-326X(92)90223-S; Head MJ, 2006, J PALEONTOL, V80, P1, DOI 10.1666/0022-3360(2006)080[0001:TCOTCD]2.0.CO;2; HILLIS DM, 1992, J HERED, V83, P189, DOI 10.1093/oxfordjournals.jhered.a111190; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; ISHIKAWA A, 1993, B PLANKTON SOC JPN, V440, P1; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; JANOFSKE D, 2000, BER FB GEOWISS U BRE, V152, P93; Keupp H., 1991, P267; KOBAYASHI S, 1995, J PHYCOL, V31, P147, DOI 10.1111/j.0022-3646.1995.00147.x; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Kremp A, 2005, J PHYCOL, V41, P629, DOI 10.1111/j.1529-8817.2005.00070.x; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Litaker RW, 2007, J PHYCOL, V43, P344, DOI 10.1111/j.1529-8817.2007.00320.x; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 2003, PHYCOLOGIA, V42, P56, DOI 10.2216/i0031-8884-42-1-56.1; MONTRESOR M, 1988, PHYCOLOGIA, V27, P387, DOI 10.2216/i0031-8884-27-3-387.1; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MORITZ C, 1994, TRENDS ECOL EVOL, V9, P373, DOI 10.1016/0169-5347(94)90057-4; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; SWOFFORD DL, 2002, PAUP PHYLOGENETIC AN	45	30	34	3	24	BLACKWELL PUBLISHING	OXFORD	9600 GARSINGTON RD, OXFORD OX4 2DQ, OXON, ENGLAND	0022-3646			J PHYCOL	J. Phycol.	APR	2008	44	2					478	494		10.1111/j.1529-8817.2008.00478.x	http://dx.doi.org/10.1111/j.1529-8817.2008.00478.x			17	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	288MU	27041202				2025-03-11	WOS:000254991300021
J	Lignum, J; Jarvis, I; Pearce, MA				Lignum, John; Jarvis, Ian; Pearce, Martin A.			A critical assessment of standard processing methods for the preparation of palynological samples	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynological preparation; dinoflagellate cysts; Lycopodium spores; sieve mesh; processing technique	WALLED DINOFLAGELLATE CYSTS; POLLEN	Standard processing techniques for the isolation of organic walled dinoflagellate cysts from geological samples are examined, with particular attention to the size and type of sieve mesh used. Variations within the 'standard' processing techniques used by different laboratories are identified, and an assessment of the retention capacities of meshes of different sizes and different materials is carried out. Some dinoflagellate cysts and large numbers of Lycopodium spores, used for the calculations of absolute abundance data, were found to pass through 20 mu m meshes. This is due to a combination of factors including: the diagonal aperture diameter of a 20 mu m mesh measuring over 28 gm; the three-dimensional properties of different mesh weaves (nylon and polyester); and the non-spherical shape of the particles. Experiments demonstrate that the maximum mesh size that should be used in palynological processing is 15 gin. Nylon mesh is more practical to use than polyester as processing time is reduced, but nylon is degraded by contact with acid solutions. Meshes with apertures < 15 mu m may be used, though this may be impractical for large samples containing significant quantities of fine siliciclastic or organic material. (c) 2007 Elsevier B.V. All rights reserved.	[Lignum, John; Jarvis, Ian] Kingston Univ London, Ctr Earth & Environm Sci Res, Sch Earth Sci & Geog, Kingston upon Thames KT1 2EE, Surrey, England; [Pearce, Martin A.] StatoilHydro, N-4035 Stavanger, Norway	Kingston University; Equinor	Lignum, J (通讯作者)，Kingston Univ London, Ctr Earth & Environm Sci Res, Sch Earth Sci & Geog, Penrhyn Rd, Kingston upon Thames KT1 2EE, Surrey, England.	j.lignum@kingston.ac.uk; i.jarvis@kingston.ac.uk; mpear@StatoilHydro.com	; Jarvis, Ian/A-1637-2008	Pearce, Martin/0000-0001-7856-1076; Jarvis, Ian/0000-0003-3184-3097				[Anonymous], 2007, Paleopalynology; BASINGER JF, 1984, SCIENCE, V224, P511, DOI 10.1126/science.224.4648.511; Batten D.J., 1983, NPD B, V2, P35; BENNINGHOFF W. S., 1962, POLLEN ET SPORES, V4, P332; COMELL WC, 1997, REV PALAEOBOT PALYNO, V98, P153; Davis M.B., 1965, HDB PALEONTOLOGICAL, P674; DAVIS MB, 1966, ECOLOGY, V47, P310, DOI 10.2307/1933780; Doher L.I., 1980, US GEOLOGICAL SURVEY, V830, P1, DOI 10.3133/cir830; ERDTMAN G., 1933, SVENSK BOT TIDSKR, V27, P347; Eshet Y, 1996, REV PALAEOBOT PALYNO, V94, P101, DOI 10.1016/S0034-6667(96)00008-5; Gray J., 1965, Handbook of paleontological techniques, P530; JORGENSEN S, 1967, NEW PHYTOL, V66, P489, DOI 10.1111/j.1469-8137.1967.tb06028.x; Pearce MA, 2003, MAR MICROPALEONTOL, V47, P271, DOI 10.1016/S0377-8398(02)00132-9; Pross J, 2006, J SEDIMENT RES, V76, P524, DOI 10.2110/jsr.2006.031; Pross J, 2001, PALAEOGEOGR PALAEOCL, V166, P369, DOI 10.1016/S0031-0182(00)00219-4; Riding JB, 2006, PALYNOLOGY, V30, P69, DOI 10.2113/gspalynol.30.1.69; Riding James B., 2004, Revista Brasileira de Paleontologia, V7, P13; Schrank E, 2003, REV PALAEOBOT PALYNO, V123, P199, DOI 10.1016/S0034-6667(02)00228-2; SCHRANK E, 1988, REV PALAEOBOT PALYNO, V56, P123, DOI 10.1016/0034-6667(88)90078-4; SCHULZE F, 2006, BERLINER KONIGLICHEN, V21, P676; Scourse J, 2005, QUATERNARY RES, V64, P57, DOI 10.1016/j.yqres.2005.03.002; STOCKMARR J, 2001, POLLEN SPORES, V13, P615; Stockmarr J., 1973, Danmarks Geologiske Undersogelse, P87; Tocher Bruce A., 1994, Revue de Micropaleontologie, V37, P223; Van Mourik CA, 2001, GEOL SOC SPEC PUBL, V183, P225, DOI 10.1144/GSL.SP.2001.183.01.11; VIDAL G, 1988, Palynology, V12, P215; VONPOST L, 1916, GEOL FOR STOCKG FORH, V38, P434; Wendler J, 2002, PALAEOGEOGR PALAEOCL, V179, P19, DOI 10.1016/S0031-0182(01)00366-2; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1	29	32	33	1	9	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	2008	149	3-4					133	149		10.1016/j.revpalbo.2007.11.004	http://dx.doi.org/10.1016/j.revpalbo.2007.11.004			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	295IL					2025-03-11	WOS:000255468100004
J	Lebedeva, NK				Lebedeva, N. K.			Biofacies analysis of Upper Cretaceous deposits in the Ust-Yenisei region: Implications of palynomorphs	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						dinocysts; acritarchs; prasinophytes; Upper Cretaceous; Ust-Yenisei region	SEA-LEVEL CHANGE; DINOFLAGELLATE CYSTS; TERTIARY BOUNDARY; WESTERN INTERIOR; SEDIMENTS; STRATIGRAPHY; ASSEMBLAGES; NETHERLANDS; ACRITARCHS; MORPHOLOGY	The results of palynomorph biofacies analysis in the Upper Cretaceous deposits of the Ust-Yenisei region are presented. The established facies confinement and indicative features of separate palynomorph groups are used, along with identified dinocyst morphotypes and taxa, in paleogeographic reconstructions. Seven palynomorph associations characterizing continental, coastal-marine, shallow-and deep-water facies are distinguished based on quantitative proportions between morphological groupings and individual taxa. As boundaries between distinguishable biostratigraphic and facies subdivisions do not coincide, dinocysts were likely insignificantly dependent in distribution on facies in the West Siberian epicontinental basin at least. On the other hand, distribution trends of particular dinocyst morphotypes and other microphytofossils are correlative with transgressive-regressive cycles and can be used for reconstruction of paleoenvironments.	Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Lebedeva, NK (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia.		Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303				BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 1983, SURVIVAL STRATEGIES; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DAVEY R.J., 1971, P 2 PLANKTONIC C, VI., P331; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; Downie C., 1971, Geoscience Man, V3, P29; Elsik W.C., 1977, Palynology, V1, P95; ESHET Y, 1994, MAR MICROPALEONTOL, V23, P231, DOI 10.1016/0377-8398(94)90014-0; FECHNER GG, 1996, GEOWISS ABH REICHE E, V18, P77; FENSOME RA, 1990, AASP CONTRIB SER; Firth JV, 1998, MAR MICROPALEONTOL, V34, P1, DOI 10.1016/S0377-8398(97)00046-7; Goodman D.K., 1987, Botanical Monographs (Oxford), V21, P649; HABIB D, 1989, PALAEOGEOGR PALAEOCL, V74, P23, DOI 10.1016/0031-0182(89)90018-7; HABIB D, 1992, GEOLOGY, V20, P165, DOI 10.1130/0091-7613(1992)020<0165:DACNRT>2.3.CO;2; HARKER SD, 1990, PALAEONTOGRAPHICA, V219; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; HARLAND R, 1988, PALAEONTOLOGY, V33, P877; Harris AJ, 2003, MAR MICROPALEONTOL, V48, P127, DOI 10.1016/S0377-8398(03)00002-1; HARRISON PJ, 1977, MAR BIOL, V43, P19, DOI 10.1007/BF00392568; Head MJ., 1992, NEOGENE QUATERNARY D; Herngreen G. 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W., 1998, MEDED NED INST TOEG, V61, P3; HINGA KR, 1992, MAR ECOL PROG SER, V86, P181, DOI 10.3354/meps086181; HULBURT EM, 1963, J MAR RES, V21, P81; HULTBERG SU, 1986, MICROPALEONTOLOGY, V32, P316, DOI 10.2307/1485725; ILINA VI, 1985, PALYNOLOGY JURASSIC; KHLONOVA AF, 1988, MIKROFITOFOSSILII ST, P7; Lebedeva NK, 2003, GEOL GEOFIZ, V44, P769; LEBEDEVA NK, 2001, APPENDIX GEOL GEOFIZ, V42, P125; LEBEDEVA NK, 2002, P 3 INT C ENV MICR P, P132; Li H, 1996, PALAIOS, V11, P15, DOI 10.2307/3515113; LIENGJARERN M, 1980, Palaeontology (Oxford), V23, P475; MAC ARTHUR ROBERT H., 1967; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MARSHALL KL, 1988, REV PALAEOBOT PALYNO, V54, P85, DOI 10.1016/0034-6667(88)90006-1; MAY F E, 1980, Palaeontographica Abteilung B Palaeophytologie, V172, P10; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; PARTRIDGE AD, 1976, J APEA, P73; Pearce MA, 2003, MAR MICROPALEONTOL, V47, P271, DOI 10.1016/S0377-8398(02)00132-9; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; PRAUSS M, 1989, NEUES JB GEOLOGIE PA, V11, P671; RICHARDSON JB, 1984, P 27 IGC STRAT NAUK; Sahagian D, 1996, AAPG BULL, V80, P1433; SARJEANT WAS, 1987, MICROPALEONTOLOGY, V33, P1, DOI 10.2307/1485525; Schioler P, 1997, MAR MICROPALEONTOL, V31, P65, DOI 10.1016/S0377-8398(96)00058-8; Schrank E, 2003, REV PALAEOBOT PALYNO, V123, P199, DOI 10.1016/S0034-6667(02)00228-2; SHAKHMUNDES VA, 1973, MIKROFOSSILII DREVNE, P50; TAPPAN H, 1989, PALEOBIOLOGY PLANT P; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; VOZZHENNIKOVA TF, 1965, INTRO RES FOSSIL PER; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; Wheeler J.W., 1990, Modern Geology, V14, P267; WILLIAMS GL, 1975, PAP GEOL SURV CAN, V2, P1075; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; YOO KI, 1991, MAR POLLUT BULL, V23, P185, DOI 10.1016/0025-326X(91)90672-F; Zakharov VA, 2003, GEOL GEOFIZ, V44, P1093; ZAKHAROV VA, 1991, GEOL GEOFIZ, V8, P9; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1; ZVEREV KV, 1999, CANDIDATES DISSERTAT	62	10	10	0	0	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0869-5938			STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	APR	2008	16	2					182	197		10.1134/S0869593808020068	http://dx.doi.org/10.1134/S0869593808020068			16	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	297BH					2025-03-11	WOS:000255590300006
J	Akkiraz, MS; Kayseri, MS; Akgün, F				Akkiraz, Mehmet Serkan; Kayseri, Mine Sezguel; Akgun, Funda			Palaeoecology of coal-bearing eocene sediments in central Anatolia (Turkey) based on quantitative palynological data	TURKISH JOURNAL OF EARTH SCIENCES			English	Review						Middle-Late Eocene; mangrove; palaeoenvironment; palaeoclimate; central Anatolia	MIDDLE EOCENE; CLIMATE; EVOLUTION; BASIN	In this study, the lignite-bearing Yoncali formation between Yozgat and Sorgun, in central Anatolia has been palynologically examined. Based on 37 outcrop samples, quantitative palynological studies recognized 64 genera and 136 palynoflora species in the palynological assemblage, which indicated a Middle-?Late Eocene age. This paper also presents a quantitative palaeovegetation and palaeodimate reconstruction for the Middle-?Upper Eocene coal occurrences of Central Anatolia on the basis of palynomorph assemblages. The diversified floral and ecological characteristics of the pollen taxa indicates that the Middle-?Upper Eocene formations in central Anatolia were characterized by the presence of a complex mangrove swamp with contributions by Nypa, Pelliciera, Avicennia, Diporites tszkaszentgydrgyi and dinoflagellate cysts which reflect warm climatic conditions. Behind the mangrove zone, pollen of Restionaceae, Ephedraceae, Mauritia, Proxapertites (Araceae) and Longapertites (Arecaceae) as well as the fern Acrostichum aureum occur. Lowland-riparian and montane elements are characterized by the dominance of Myricaceae, Symplocaceae, Icacinaceae, Quercus, Pinus and Castanea. Swamp-freshwater elements are represented by Sparganjaceae, Nymphaceae, Taxodjaceae, Cupressaceae and Nyssa as well as fern spores such as Osmundaceae and Gleicheniaceae. The calculations were performed with the help of the 'Coexistence Approach' method to climatically evaluate palynoflora from the Yozgat-Sorgun area. The obtained results have been compared to data derived from the application of the Coexistence Approach to other, already published Central Anatolian palynofloras of the same age. The results of the climatic inferences suggest that the palaeoclimatic conditions were in the megathermal zone (mean annual temperature of 24.8-25 degrees C), megatherm/mesotherm intermediate zone (mean annual temperature of 23.1-24.8 degrees C near the coast) whereas mesothermic (mean annual temperature of 16.5-23.1 degrees C) conditions prevailed in the montane region. Likewise, the results of mean annual range of temperatures indicate the influence of the Indian ocean, which enabled the development of the mangroves.	[Akkiraz, Mehmet Serkan; Kayseri, Mine Sezguel; Akgun, Funda] Dokuz Eylul Univ, Dept Geol Engn, TR-35160 Izmir, Turkey	Dokuz Eylul University	Akkiraz, MS (通讯作者)，Dokuz Eylul Univ, Dept Geol Engn, TR-35160 Izmir, Turkey.	serkan.akkiraz@deu.edu.tr	Akgün, Funda/AAC-2859-2020; akkiraz, mehmet/ADP-2366-2022; Kayseri Ozer, Mine Sezgul/KIJ-4911-2024	Akgun, Funda/0000-0002-6028-6704; Kayseri Ozer, Mine Sezgul/0000-0003-2712-2457				Akgun F, 2002, [古生物学报, Acta Palaeontologica Sinica], V41, P576; AKGUN F, 2002, TURKISH J EARTH SCI, V11, P1; Akkiraz MS, 2006, TURK J EARTH SCI, V15, P155; AKYOL E, 1978, JEOLOJI MUHENDISLIGI, V6, P31; AKYOL E, 1980, MINERAL RES EXPLORAT, V91, P39; ALEKSANDROVA AN, 1987, INT GEOL REV, V29, P503; ALLEN LO, 1988, GEOLOGISCHES JB A, V100, P288; [Anonymous], USGS PROFESSIONAL PA; [Anonymous], TEMPERATURE PARAMETE; [Anonymous], 1988, Geologisches Jahrbuch Reihe A; BARUTOGLU OH, 1953, UNPUB REPORT CELTEK; BIRGILI S, 1975, 5621 MIN RES EXPL I; Blasco F., 1977, Ecosystems of the World 1: Wet Coastal Ecosystems, P241; 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J., 1962, Blumea, V11, P235; VONDERBRELIE G, 1988, GEOLOGISCHES JB, V100, P288; WESTGATE JW, 1990, PALAEOGEOGR PALAEOCL, V78, P163, DOI 10.1016/0031-0182(90)90210-X; Wolfe J.A., 1992, Eocene-Oligocene Climatic and Biotic Evolution, P421, DOI DOI 10.1515/9781400862924.421/HTML; WOLFE JA, 1978, AM SCI, V66, P694; Wolfe JA., 1982, Climate in Earth History, P154; WRENN JH, 1986, CONTRIBUTIONS SERIES, V17, P169; YASAMANOV NA, 1982, IZVESTIYA AN SSSR G, V10, P106; Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	112	43	47	0	14	Tubitak Scientific & Technological Research Council Turkey	ANKARA	ATATURK BULVARI NO 221, KAVAKLIDERE, TR-06100 ANKARA, TURKIYE	1300-0985			TURK J EARTH SCI	Turk. J. Earth Sci.	APR-JUN	2008	17	2					317	360						44	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	281TP					2025-03-11	WOS:000254522100006
J	Barocio-León, OA; Millan-Núñez, R; Santamaría-del-Angel, E; Gonzalez-Silvera, A; Trees, CC; Orellana-Cepeda, E				Barocio-Leon, Oscar A.; Millan-Nunez, Roberto; Santamaria-del-Angel, Eduardo; Gonzalez-Silvera, Adriana; Trees, Charles C.; Orellana-Cepeda, Elizabeth			Bio-optical characteristics of a phytoplankton bloom event off Baja California Peninsula (30-31°N)	CONTINENTAL SHELF RESEARCH			English	Article						phytoplankton; absorption coefficient; pigments; HPLC; dinoflagellate cyst; Pseudo-nitzschia; Mexico; California Current (30-31 degrees N)	ABSORPTION-COEFFICIENTS; MARINE-PHYTOPLANKTON; RED TIDE; LIGHT-ABSORPTION; CHLOROPHYLL-A; VARIABILITY; PIGMENTS; WATERS; SYSTEM	A phytoplankton bloom was detected in the Southern California Current System, off the Baja California Peninsula (Mexico) on June 2003 with chlorophyll-a concentration (TChla) of 10.13 mg m(-3). Two stations (D1 and D2) were sampled on June 24, and D2 was resampled 6 days later; chlorophyll-a concentration had decreased by about one half. LAC MODIS-Chla images were obtained and showed the spread of the bloom on the day after sampling. The phytoplankton community consisted primarily of dinoflagellate temporary cysts, mainly at the surface and at 5 m in station D1. Two Pseudo-nitzschia species (P. australis, P. seriata) were also very abundant. Samples from the bloom had a specific phytoplankton absorption coefficient (a*(ph)(lambda)) lower than the rest of the samples. Values varied from 0.0186 to 0.0455 m(2) mg(-1) for a*(ph)(440) and from 0.0092 to 0.0294 m(2) mg(-1) for a*(ph) (675), with ratios a*(ph)(440): a*(ph)(675) ranging from 0.99 to 2.20. These low ratios were associated with the combined effect of packaging, and with the relatively high ratios of fucoxanthin, peridinin, diadinoxanthin and chlorophyll-c2 to TChla. Samples from the surface and 5 m depth at station D1 had higher ratios of Perid:TChla (0.12-0.32) than the rest of the samples, suggesting that cysts have similar Perid:TChla as free-living dinoflagellates. An unusual absorption spectrum with a broad maximum around 480-500 nm was associated with the high proportion of cysts and diatoms. The slope of the spectra between 443 and 488 nm was a good index to differentiate bloom samples containing high proportions of dinoflagellate temporary cysts. Further investigation of the absorption properties of dinoflagellate cysts is needed in order to detect these waters by remote sensing. Although much work is still necessary to understand and explain the bio-optical properties of a bloom, the present study is the first assessment off the Baja California coast to simultaneously consider aspects such as absorption properties, pigment composition and to include a spatial evaluation of the extension of a bloom with satellite images. (C) 2007 Elsevier Ltd. All rights reserved.	[Barocio-Leon, Oscar A.; Millan-Nunez, Roberto; Santamaria-del-Angel, Eduardo; Gonzalez-Silvera, Adriana; Orellana-Cepeda, Elizabeth] Univ Autonoma Baja California, Fac Ciencias Marinas, Ensenada 22830, Baja California, Mexico; [Trees, Charles C.] NATO, Undersea Res Ctr, I-19138 La Spezia, Italy	Universidad Autonoma de Baja California; NATO (North Atlantic Treaty Organisation)	Gonzalez-Silvera, A (通讯作者)，Univ Autonoma Baja California, Fac Ciencias Marinas, Km 103 Carretera Tijuana Ensenada, Ensenada 22830, Baja California, Mexico.	oscar_barocio@yahoo.com.mx; rmillan@uabc.mx; santamaria@uabc.mx; agglez@uabc.mx; trees@nurc.nato.int; orellana@uabc.mx	; Santamaria-del-Angel, Eduardo/S-1630-2017; Gonzalez-Silvera, Adriana/F-7923-2018	Barocio Leon, Oscar Alcides/0000-0003-1433-2164; Santamaria-del-Angel, Eduardo/0000-0002-1882-7714; Gonzalez-Silvera, Adriana/0000-0001-7817-5343				Aguirre-Hernández E, 2004, DEEP-SEA RES PT II, V51, P799, DOI 10.1016/j.dsr2.2004.05.015; Alvain S, 2005, DEEP-SEA RES PT I, V52, P1989, DOI 10.1016/j.dsr.2005.06.015; Andersen P., 2003, Manual on harmful marine microalgae. Monographs on oceanographic methodology, P99; Barocio-León OA, 2006, J OCEANOGR, V62, P873, DOI 10.1007/s10872-006-0105-z; BAROCIOLEON O, 2006, THESIS U BAJA CALIFO; Bjornland T., 1997, PHYTOPLANKTON PIGMEN, P578; Bricaud A, 2004, J GEOPHYS RES-OCEANS, V109, DOI 10.1029/2004JC002419; BRICAUD A, 1995, J GEOPHYS RES-OCEANS, V100, P13321, DOI 10.1029/95JC00463; Carder KL, 1999, J GEOPHYS RES-OCEANS, V104, P5403, DOI 10.1029/1998JC900082; DUYSENS LNM, 1956, BIOCHIM BIOPHYS ACTA, V19, P1; Falkowski P.G., 1997, AQUATIC PHOTOSYNTHES, P375; Fujiki T, 2002, J PLANKTON RES, V24, P859, DOI 10.1093/plankt/24.9.859; Goericke R, 2004, CAL COOP OCEAN FISH, V45, P27; Hallegraeff G.M., 2003, MANUAL HARMFUL MARIN, P25, DOI DOI 10.25607/OBP-1370; Hasle Grethe R., 1997, P5, DOI 10.1016/B978-012693018-4/50004-5; Horner RA, 1997, LIMNOL OCEANOGR, V42, P1076, DOI 10.4319/lo.1997.42.5_part_2.1076; Johnsen G, 1996, SCI MAR, V60, P47; Kahru M, 1998, J GEOPHYS RES-OCEANS, V103, P21601, DOI 10.1029/98JC01945; KISHINO M, 1985, B MAR SCI, V37, P634; Kudela Raphael, 2005, Oceanography, V18, P184; Mackey MD, 1996, MAR ECOL PROG SER, V144, P265, DOI 10.3354/meps144265; MATSUOKA K, 2000, WESTPACHABWESTPAC10C; Millán-Núñez E, 2004, DEEP-SEA RES PT II, V51, P817, DOI 10.1016/j.dsr2.2004.05.023; Mitchell B.G., 2003, OCEAN OPT PROTOC SAT, V4, P39; Moisan TA, 1999, LIMNOL OCEANOGR, V44, P247, DOI 10.4319/lo.1999.44.2.0247; MOREL A, 1981, DEEP-SEA RES, V28, P1375, DOI 10.1016/0198-0149(81)90039-X; Morel A, 2001, J GEOPHYS RES-OCEANS, V106, P7163, DOI 10.1029/2000JC000319; ORELLANACEPEDA E, 13 INT MAT RES C CAN; ORELLANACEPEDA E, 2004, DYNAMICS PSEUDO NITZ; Peña-Manjarrez JL, 2005, CONT SHELF RES, V25, P1375, DOI 10.1016/j.csr.2005.02.002; Pitcher GC, 1998, MAR ECOL PROG SER, V172, P253, DOI 10.3354/meps172253; QUILLIAM MA, 2003, P 8 CAN WORKSH HARMF, V2498; SATHYENDRANATH S, 1987, LIMNOL OCEANOGR, V32, P403, DOI 10.4319/lo.1987.32.2.0403; Sosik HM, 1995, DEEP-SEA RES PT I, V42, P1717, DOI 10.1016/0967-0637(95)00081-G; Trees CC, 2000, LIMNOL OCEANOGR, V45, P1130, DOI 10.4319/lo.2000.45.5.1130; Utermohl H, 1958, LIMNOLOGIE, V9, P1; VALENZUELA E, 2005, 12 C NAC CIENC TECN; WRIGHT SW, 1991, MAR ECOL PROG SER, V77, P183, DOI 10.3354/meps077183	38	10	16	0	9	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0278-4343	1873-6955		CONT SHELF RES	Cont. Shelf Res.	MAR 30	2008	28	4-5					672	681		10.1016/j.csr.2007.12.002	http://dx.doi.org/10.1016/j.csr.2007.12.002			10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	291XV					2025-03-11	WOS:000255231600013
J	van der Meer, MTJ; Sangiorgi, F; Baas, M; Brinkhuis, H; Damste, JSS; Schouten, S				van der Meer, Marcel T. J.; Sangiorgi, Francesca; Baas, Marianne; Brinkhuis, Henk; Damste, Jaap S. Sinninghe; Schouten, Stefan			Molecular isotopic and dinoflagellate evidence for Late Holocene freshening of the Black Sea	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						paleosalinity; compound-specific hydrogen isotopes; alkenones; organic-walled dinotlagellate cysts; Black Sea	SURFACE CONDITIONS; EMILIANIA-HUXLEYI; GROWTH-RATE; RECORD; CYSTS; ASSEMBLAGES; ALKENONES; IDENTIFICATION; CALIBRATION; INDICATORS	The Black Sea is the world's largest anoxic basin with oxygen-free conditions below water depths of approximately 100 m resulting from strong density stratification. The salinity of its surface water likely varied substantially over time due to variations in freshwater input from large rivers and in the saline bottom water of Mediterranean origin coming across the shallow sill of the Bosporus. However, long-term reconstructions of surface water salinities are lacking. The invasion of the coccolithophorid Emiliania huxleyi in the Black Sea at approximately 2720 a, responsible for a marked change in sediment composition (lithology), has been commonly attributed to salinity levels rising above 11. We analyzed the delta D values of long-chain alkenones produced by haptophyte algae, mainly E. huxleyi, in a core from the eastern basin of the Black Sea to reconstruct past variations in sea surface salinities, and combined this with relative salinity changes generated from organic-walled dinoflagellate cyst (dinocyst) distributions from the same core. Combined results indicate a substantial freshening of Black Sea surface waters in the last 3000 years, suggesting that sea surface salinity was substantially higher than the present-day salinity of approximately 18 at the time E. huxleyi invaded the Black Sea. (C) 2007 Elsevier B.V. All rights reserved.	[van der Meer, Marcel T. J.; Baas, Marianne; Damste, Jaap S. Sinninghe; Schouten, Stefan] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands; [Sangiorgi, Francesca; Brinkhuis, Henk] Univ Utrecht, Fac Sci, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; [Damste, Jaap S. Sinninghe] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Utrecht University	van der Meer, MTJ (通讯作者)，NIOZ Royal Netherlands Inst Sea Res, POB 59, NL-1790 AB Den Burg, Netherlands.	mvdmeer@nioz.nl	Schouten, Stefan/P-4380-2016; Brinkhuis, Henk/B-4223-2009; Sinninghe Damste, Jaap/F-6128-2011; van der Meer, Marcel/L-3450-2013	Sinninghe Damste, Jaap/0000-0002-8683-1854; van der Meer, Marcel/0000-0001-6454-1752; Brinkhuis, Henk/0000-0003-0253-6610; Sangiorgi, Francesca/0000-0003-4233-6154				Arthur MA, 1998, PALEOCEANOGRAPHY, V13, P395, DOI 10.1029/98PA01161; Benthien A, 2007, GEOCHIM COSMOCHIM AC, V71, P1528, DOI 10.1016/j.gca.2006.12.015; BRASSELL SC, 1986, NATURE, V320, P129, DOI 10.1038/320129a0; BUKRY D, 1970, NATURE, V226, P156, DOI 10.1038/226156a0; Bukry D., 1974, AAPG Memoir, V20, P353; CHRISTOVA R, 2003, OCEANOLOGIA, V4, P36; Coolen MJL, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001188; DAMSTE JSS, 1993, NATURE, V362, P827, DOI 10.1038/362827a0; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DEGENS ET, 1972, CHEM GEOL, V10, P1, DOI 10.1016/0009-2541(72)90073-3; Englebrecht AC, 2005, GEOCHIM COSMOCHIM AC, V69, P4253, DOI 10.1016/j.gca.2005.04.011; Fensome RA, 2004, CONTRIBUTIONS SERIES, V42; FREEMAN KH, 1994, ORG GEOCHEM, V21, P629, DOI 10.1016/0146-6380(94)90009-4; Hay BJ, 1988, PALEOCEANOGRAPHY, V3, P491, DOI 10.1029/PA003i004p00491; Head MJ, 2006, J PALEONTOL, V80, P1, DOI 10.1666/0022-3360(2006)080[0001:TCOTCD]2.0.CO;2; Hopmans EC, 2005, ORG GEOCHEM, V36, P485, DOI 10.1016/j.orggeochem.2004.10.001; JAOSHVILI S, 2002, RIVERS BLACK SEA EUR; JONES GA, 1994, DEEP-SEA RES PT I, V41, P531, DOI 10.1016/0967-0637(94)90094-9; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; LAWS EA, 1995, GEOCHIM COSMOCHIM AC, V59, P1131, DOI 10.1016/0016-7037(95)00030-4; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MARRETT F, 2007, BLACK SEA QUAT INT, V167, P19; Morzadec-Kerfourn MT, 2005, QUATERN INT, V133, P137, DOI 10.1016/j.quaint.2004.10.006; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; Muller PJ, 1998, GEOCHIM COSMOCHIM AC, V62, P1757, DOI 10.1016/S0016-7037(98)00097-0; MURRAY JW, 1991, DEEP-SEA RES, V38, pS663, DOI 10.1016/S0198-0149(10)80003-2; Oguz T, 2006, J MARINE SYST, V59, P173, DOI 10.1016/j.jmarsys.2005.08.002; Paul H.A., 2002, Application of novel stable isotope methods to reconstruct paleoenvironments: Compound specific hydrogen isotopes and pore-water oxygen isotopes; Peyron O, 2001, J QUATERNARY SCI, V16, P699, DOI 10.1002/jqs.651; Popp BN, 1998, GEOCHIM COSMOCHIM AC, V62, P69, DOI 10.1016/S0016-7037(97)00333-5; PRAHL FG, 1987, NATURE, V330, P367, DOI 10.1038/330367a0; Prahl FG, 2006, GEOCHIM COSMOCHIM AC, V70, P2856, DOI 10.1016/j.gca.2006.03.009; Reichart GJ, 2003, MAR MICROPALEONTOL, V49, P303, DOI 10.1016/S0377-8398(03)00050-1; REPETA DJ, 1989, NATURE, V342, P69, DOI 10.1038/342069a0; REPETA DJ, 1993, GEOCHIM COSMOCHIM AC, V57, P4337, DOI 10.1016/0016-7037(93)90334-S; Sangiorgi F, 2004, ESTUAR COAST SHELF S, V60, P69, DOI 10.1016/j.ecss.2003.12.001; Schouten S, 1998, GEOCHIM COSMOCHIM AC, V62, P1397, DOI 10.1016/S0016-7037(98)00076-3; Schouten S, 2006, BIOGEOSCIENCES, V3, P113, DOI 10.5194/bg-3-113-2006; van der Meer MTJ, 2007, EARTH PLANET SC LETT, V262, P594, DOI 10.1016/j.epsl.2007.08.014; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Wall D., 1973, Geoscience Man, V7, P95; Xu L, 2001, ORG GEOCHEM, V32, P633, DOI 10.1016/S0146-6380(01)00019-5	43	92	97	1	25	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0012-821X	1385-013X		EARTH PLANET SC LETT	Earth Planet. Sci. Lett.	MAR 30	2008	267	3-4					426	434		10.1016/j.epsl.2007.12.001	http://dx.doi.org/10.1016/j.epsl.2007.12.001			9	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	283WN					2025-03-11	WOS:000254667300003
J	Sangiorgi, F; van Soelen, EE; Spofforth, DJA; Pälike, H; Stickley, CE; St John, K; Koç, N; Schouten, S; Damsté, JSS; Brinkhuis, H				Sangiorgi, Francesca; van Soelen, Els E.; Spofforth, David J. A.; Palike, Heiko; Stickley, Catherine E.; St. John, Kristen; Koc, Nalan; Schouten, Stefan; Damste, Jaap S. Sinninghe; Brinkhuis, Henk			Cyclicity in the middle Eocene central Arctic Ocean sediment record:: Orbital forcing and environmental response	PALEOCEANOGRAPHY			English	Article							SINGULAR-SPECTRUM ANALYSIS; DINOFLAGELLATE CYSTS; ICE; CLIMATE; CIRCULATION; MIOCENE; POLLEN; LIPIDS; SEAS	Continuous X-ray fluorescence scanning of middle Eocene (similar to 46 Ma) core M0002A-55X (similar to 236-241 m composite depth), recovered during Integrated Ocean Drilling Program Expedition 302, revealed a strong cyclical signal in some major and trace geochemical elements. We performed a multiproxy study of the same core, which included organic geochemical, sedimentological, and biological parameters, and integrated our results with available geochemical and physical properties data. The target was to look for cyclicity in the several proxies, investigate their frequency, and understand the environmental response to the potential forcing. Results indicate that a higher terrigenous component corresponds to lower organic carbon concentration, smaller contributions by angiosperm pollen and spores, organic-walled dinoflagellate cysts, and chrysophyte cysts (lower productivity, shorter growing season for flowering plants, and lower stratification) but higher contributions by bisaccate pollen and diatoms (drier conditions on land, more marine conditions) and higher terrigenous sand (ice-rafted debris (IRD)). Our investigation shows that physical proxy parameters hold cyclicity with periods of about 50 and 100 cm and that these frequency components are compatible with a Milankovitch-type orbital forcing, representing precession and obliquity, respectively. The longer 100 cm cyclicity is also present in the biological (pollen, dinoflagellate cysts, and siliceous microfossils) and in the sedimentological (IRD) proxies. The environmental signal derived from the integrated multiproxy analysis suggests that in an enclosed Arctic Ocean at time of ice (sea ice and glacial ice) initiation the biological proxies responded more strongly to growing season length/darkness, whereas the terrigenous components, directly driven by sea ice and/or glacial ice formation and extent, responded more directly to seasonal insolation.	[Sangiorgi, Francesca; van Soelen, Els E.; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Sangiorgi, Francesca; Schouten, Stefan; Damste, Jaap S. Sinninghe] Royal Netherlands Inst Sea Res, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Texel, Netherlands; [Spofforth, David J. A.; Palike, Heiko] Univ Southampton, Sch Ocean & Earth Sci, Southampton SO17 3ZH, Hants, England; [Stickley, Catherine E.; Koc, Nalan] Norwegian Polar Res Inst, Polar Environm Ctr, N-9296 Tromso, Norway; [St. John, Kristen] James Madison Univ, Dept Geol & Environm Sci, Harrisonburg, VA 22807 USA; [Koc, Nalan] Univ Tromso, Dept Geol, Tromso, Norway	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Southampton; NERC National Oceanography Centre; Norwegian Polar Institute; James Madison University; UiT The Arctic University of Tromso	Sangiorgi, F (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	f.sangiorgi@uu.nl	Schouten, Stefan/P-4380-2016; Brinkhuis, Henk/B-4223-2009; Sinninghe Damste, Jaap/F-6128-2011; Palike, Heiko/A-6560-2008	Brinkhuis, Henk/0000-0003-0253-6610; Sangiorgi, Francesca/0000-0003-4233-6154; Sinninghe Damste, Jaap/0000-0002-8683-1854; Palike, Heiko/0000-0003-3386-0923; St. John, Kristen/0000-0001-7045-7485	NERC [NE/D000343/1] Funding Source: UKRI; STFC [PP/D002176/1] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); STFC(UK Research & Innovation (UKRI)Science & Technology Facilities Council (STFC))		AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; Backman J, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001476; Battarbee R.W., 2001, TRACKING ENV CHANGES, P155, DOI DOI 10.1007/0-306-47668-1_8; BATTARBEE RW, 1982, LIMNOL OCEANOGR, V27, P184, DOI 10.4319/lo.1982.27.1.0184; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H, 2006, NATURE, V441, P606, DOI 10.1038/nature04692; CHEDDADI R, 1995, PALEOCEANOGRAPHY, V10, P291, DOI 10.1029/94PA02672; Darby DA, 2006, PROG OCEANOGR, V71, P129, DOI 10.1016/j.pocean.2006.09.009; Eldrett JS, 2007, NATURE, V446, P176, DOI 10.1038/nature05591; *EXP 302 SCI, 2006, P INT OC DRILL PROGR, V302, DOI DOI 10.2204/I0DP.PR0C.302.104.2006; Fensome R.A., 2004, The Lentin and Williams Index of Fossil Dinoflagellates; Flannery P.B., 1992, NUMERICAL RECIPES FO; GREENWOOD DR, 1995, GEOLOGY, V23, P1044, DOI 10.1130/0091-7613(1995)023<1044:ECCALT>2.3.CO;2; HAYS JD, 1976, SCIENCE, V194, P1121, DOI 10.1126/science.194.4270.1121; HOOGHIEMSTRA H, 1988, PHILOS T ROY SOC B, V318, P431, DOI 10.1098/rstb.1988.0018; HOOGHIEMSTRA H, 1989, NATO ADV SCI I C-MAT, V282, P733; Hopmans EC, 2004, EARTH PLANET SC LETT, V224, P107, DOI 10.1016/j.epsl.2004.05.012; Hopmans EC, 2000, RAPID COMMUN MASS SP, V14, P585, DOI 10.1002/(SICI)1097-0231(20000415)14:7<585::AID-RCM913>3.0.CO;2-N; Jackson CS, 2003, CLIM DYNAM, V21, P539, DOI 10.1007/s00382-003-0351-3; Jahren AH, 2003, GEOLOGY, V31, P463, DOI 10.1130/0091-7613(2003)031<0463:HEFTME>2.0.CO;2; Jakobsson M, 2007, NATURE, V447, P986, DOI 10.1038/nature05924; Jansen JHF, 1998, MAR GEOL, V151, P143, DOI 10.1016/S0025-3227(98)00074-7; Jiang N, 1995, CLIM DYNAM, V12, P101, DOI 10.1007/BF00223723; Jin MB, 2007, GEOPHYS RES LETT, V34, DOI 10.1029/2006GL028849; Lammers RB, 2001, J GEOPHYS RES-ATMOS, V106, P3321, DOI 10.1029/2000JD900444; Laskar J, 2004, ASTRON ASTROPHYS, V428, P261, DOI 10.1051/0004-6361:20041335; Lowenstein TK, 2006, SCIENCE, V313, P1928, DOI 10.1126/science.1129555; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Meincke J, 1997, ICES J MAR SCI, V54, P283, DOI 10.1006/jmsc.1997.0229; Miller KG, 2005, SCIENCE, V310, P1293, DOI 10.1126/science.1116412; Moran K, 2006, NATURE, V441, P601, DOI 10.1038/nature04800; Paillard D., 1996, Eos Trans. 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J	D'Costa, PM; Anil, AC; Patil, JS; Hegde, S; D'Silva, MS; Chourasia, M				D'Costa, Priya M.; Anil, Arga Chandrashekar; Patil, Jagadish S.; Hegde, Sahana; D'Silva, Maria Sharnina; Chourasia, Moji			Dinoflagellates in a mesotrophic, tropical environment influenced by monsoon	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						dinoflagellates; seasonal cycling; heterotrophy; monsoon; tropical environment	RECENT MARINE-SEDIMENTS; HARMFUL ALGAL BLOOMS; COASTAL WATERS; RESTING CYSTS; DINOPHYSIS; EUTROPHICATION; PHYTOPLANKTON; GERMINATION; ALEXANDRIUM; TURBULENCE	The changes in dinoflagellate community structure in both - the water column and sediment in a mesotrophic, tropical port environment were investigated in this study. Since the South West Monsoon (SWM) is the main source of climatic variation, observations were made during two consecutive post-monsoon periods (2001 and 2002) and the intervening pre-monsoon period (2002). The pre-monsoon period supported a more diverse dinoflagellate community in the water column compared to both post-monsoon periods. Heterotrophic dinoflagellates were abundant in the water column as well as sediment. A seasonal cycling between vegetative and resting cysts of autotrophic and heterotrophic dinoflagellates governed by the environmental characteristics of the study area was observed. Temperature, salinity and suspended particulate matter were the main factors affecting dinoflagellate community structure in both the water column and sediment. The dominant dinoflagellates in the water column differed during both post-monsoon periods that followed two dissimilar monsoon events. Prorocentroids and gonyaulacoids dominated the water column subsequent to the 2001 SWM, whereas dinophysoids and unidentified tiny dinoflagellates dominated during the next post-monsoon period. The 2001 SWM started in May, peaked during June-July and reduced gradually to end in October. The 2002 SWM was erratic; it started late (in June) and ended earlier (in September). These observations highlight the potential of the SWM to influence the community structure of dinoflagellates in tropical waters and points to the importance of long-term studies to discern robust variations in dinoflagellate communities in response to fluctuating monsoon regimes. (c) 2007 Elsevier Ltd. All rights reserved.	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J	Peng, SE; Luo, YJ; Huang, HJ; Lee, IT; Hou, LS; Chen, WNU; Fang, LS; Chen, CS				Peng, S. -E.; Luo, Y. -J.; Huang, H. -J.; Lee, I. -T.; Hou, L. -S.; Chen, W. -N. U.; Fang, L. -S.; Chen, C. -S.			Isolation of tissue layers in hermatypic corals by <i>N</i>-acetylcysteine:: morphological and proteomic examinations	CORAL REEFS			English	Article						epidermis; gastrodermis; proteomics; endosymbiosis; Symbiodinium	ACETYL-L-CYSTEINE; MUCOLYTIC AGENT; HYDRA; REDUCTION; SYMBIOSIS; ENDODERM; MESOGLEA; PROTEIN	Corals are diploblastic in body pattern and include two tissue layers, the epidermis and gastrodermis, interconnected by an acellular matrix mesoglea. During development, cells in these tissue layers differentiate morphologically and functionally. In most hermatypic corals, the gastrodermis further develops an ability to associate with microalgae dinoflagellates. This endosymbiosis occurs inside specific host gastrodermal cells, and its mechanism still remains unclear notwithstanding decades of research. The delay in progress is partly due to the difficulty in separating the gastrodermis and its symbionts from the epidermis for detailed cellular and biochemical investigations. The present study reports a simple method to separate these two tissue layers in hermatypic corals using the reducing agent, N-acetylcysteine (NAC). Efficient tissue and proteomic isolations are demonstrated by microscopy and two-dimensional SDS polyacrylamide gel electrophoresis (2D SDS-PAGE). The NAC treatment was able to separate tissue layers without inducing protein degradation. Furthermore, the sensitivity of protein detection greatly increases in the isolated tissue layers. The application of the present technique provides future research on endosymbiosis and coral development with a tool for higher accuracy and sensitivity.	[Peng, S. -E.; Luo, Y. -J.; Huang, H. -J.; Lee, I. -T.; Hou, L. -S.; Chen, C. -S.] Nat Dong Hwa Univ, Inst Marine Biotechnol, Pingtung 944, Taiwan; [Chen, C. -S.] Nat Museum Marine Biol & Aquarium, Pingtung 944, Taiwan; [Chen, W. -N. U.] I Sou Univ, Dept Biotechnol, Kaohsiung, Taiwan; [Hou, L. -S.] Cheng Shiu Univ, Niao Song, Taiwan	National Museum of Marine Biology & Aquarium; I Shou University; Cheng Shiu University	Chen, CS (通讯作者)，Nat Dong Hwa Univ, Inst Marine Biotechnol, 2 Houwan Rd, Pingtung 944, Taiwan.	cchen@nmmba.gov.tw	Luo, Yi-Jyun/G-8020-2012	Luo, Yi-Jyun/0000-0002-3418-3146				Barneah O, 2006, MAR BIOTECHNOL, V8, P11, DOI 10.1007/s10126-004-5120-8; BERKING S, 2007, J THEOR BIOL; Chen CS, 2005, PROTOPLASMA, V226, P175, DOI 10.1007/s00709-005-0116-4; Deboer ML, 2007, COMP BIOCHEM PHYS D, V2, P63, DOI 10.1016/j.cbd.2006.11.003; EPP L, 1986, J MORPHOL, V189, P271, DOI 10.1002/jmor.1051890306; EPP LG, 1979, T AM MICROSC SOC, V98, P392, DOI 10.2307/3225724; Hackett JD, 2004, AM J BOT, V91, P1523, DOI 10.3732/ajb.91.10.1523; HAYNES J, 1963, SCIENCE, V142, P1481, DOI 10.1126/science.142.3598.1481; HEMMRICH G, 2006, MOL PHYLOGENET EVOL; Kishimoto Y, 1996, J CELL SCI, V109, P763; Matsuyama T, 2006, J CONTROL RELEASE, V115, P183, DOI 10.1016/j.jconrel.2006.08.004; MILLER HR, 1986, J CLIN MICROBIOL, V24, P470, DOI 10.1128/JCM.24.3.470-471.1986; NORRIS BJ, 1994, PLANT MOL BIOL, V24, P673, DOI 10.1007/BF00023563; Richier S, 2005, J EXP BIOL, V208, P277, DOI 10.1242/jeb.01368; Richier S, 2003, BBA-GEN SUBJECTS, V1621, P84, DOI 10.1016/S0304-4165(03)00049-7; Rinkevich B, 2005, MAR BIOTECHNOL, V7, P429, DOI 10.1007/s10126-004-0108-y; Salih A, 2000, NATURE, V408, P850, DOI 10.1038/35048564; SARRAS MP, 1991, DEV BIOL, V148, P481, DOI 10.1016/0012-1606(91)90266-6; SHEFFNER AL, 1963, ANN NY ACAD SCI, V106, P298; Stambler N, 2005, CORAL REEFS, V24, P1, DOI 10.1007/s00338-004-0452-4; TRENCH RK, 1993, ENDOCYTOBIOSIS CELL, V9, P135; VERCAUTEREN FG, 2006, AMINO ACIDS; Weis VM, 1996, J EXP BIOL, V199, P883	23	27	27	1	17	SPRINGER	NEW YORK	233 SPRING STREET, NEW YORK, NY 10013 USA	0722-4028			CORAL REEFS	Coral Reefs	MAR	2008	27	1					133	142		10.1007/s00338-007-0300-4	http://dx.doi.org/10.1007/s00338-007-0300-4			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	256ZA					2025-03-11	WOS:000252767200018
J	Coccioni, R; Marsili, A; Montanari, A; Bellanca, A; Neri, R; Bice, DM; Brinkhuis, H; Church, N; Macalady, A; McDaniel, A; Deino, A; Lirer, F; Sprovieri, M; Maiorano, P; Monechi, S; Nini, C; Nocchi, M; Pross, J; Rochette, P; Sagnotti, L; Tateo, F; Touchard, Y; Van Simaeys, S; Williams, GL				Coccioni, Rodolfo; Marsili, Andrea; Montanari, Alessandro; Bellanca, Adriana; Neri, Rodolfo; Bice, David M.; Brinkhuis, Henk; Church, Nathan; Macalady, Alison; McDaniel, Aaron; Deino, Alain; Lirer, Fabrizio; Sprovieri, Mario; Maiorano, Patrizia; Monechi, Simonetta; Nini, Claudio; Nocchi, Marisa; Pross, Joerg; Rochette, Pierre; Sagnotti, Leonardo; Tateo, Fabio; Touchard, Yannick; Van Simaeys, Stefaan; Williams, Graham L.			Integrated stratigraphy of the Oligocene pelagic sequence in the Umbria-Marche basin (northeastern Apennines, Italy): A potential Global Stratotype Section and Point (GSSP) for the Rupelian/Chattian boundary	GEOLOGICAL SOCIETY OF AMERICA BULLETIN			English	Article						integrated stratigraphy; Oligocene; Rupelian/Chattian boundary; Umbria-Marche; Apennines; central Italy	PLANKTONIC FORAMINIFERAL BIOSTRATIGRAPHY; WESTERN NORTH-ATLANTIC; CALCAREOUS NANNOFOSSILS; DINOFLAGELLATE CYSTS; STRONTIUM ISOTOPES; SOUTH-ATLANTIC; TIME-SCALE; EOCENE; GUBBIO; REGION	The Oligocene represents an important time period from a wide range of perspectives and includes significant climatic and eustatic variations. The pelagic succession of the Umbria-Marche Apennines (central Italy) includes a complete and continuous sequence of marly limestones and marls, with volcaniclastic layers that enable us to construct an integrated stratigraphic framework for this time period. We present here a synthesis of detailed biostratigraphic, magnetostratigraphic, and chemostratigraphic studies, along with geochronologic results from several biotite-rich volcaniclastic layers, which provide the means for an accurate and precise radiometric calibration of the Oligocene time scale. From this study, the interpolated ages for the Rupelian/Chattian stage boundary, located in the upper half of Chron 10n at meter level 188 in the Monte Cagnero section, and corresponding to the O4/O5 planktonic foraminiferal zonal boundary, are 28.36 Ma (paleomagnetic interpolation), 28.27 +/- 0.1 Ma (direct radioisotopic dating), and 27.99 Ma (astrochronological interpolation). These ages appear to be slightly younger than those reported in recent chronostratigraphic time scale compilations. The Monte Cagnero section is a potential candidate for defining the Chattian Global Stratotype Section and Point (GSSP) and some reliable criteria are here proposed for marking the Rupelian/Chattian boundary according to International Union of Geological Sciences (IUGS) recommendations.	[Coccioni, Rodolfo; Marsili, Andrea] Univ Urbino, Ist Geol, I-61029 Urbino, Italy; [Coccioni, Rodolfo; Marsili, Andrea] Univ Urbino, Ctr Gepbiol, I-61029 Urbino, Italy; [Montanari, Alessandro; Bice, David M.] Osservatorio Geol Coldigioco, I-62020 Frontale Di Apiro, Italy; [Montanari, Alessandro; Church, Nathan; Macalady, Alison; McDaniel, Aaron] Carleton Coll, Dept Geol, Northfield, MN 55057 USA; [Bellanca, Adriana; Neri, Rodolfo] Dipartimento Chim Fis Terra Applicaz Georisorse &, I-90123 Palermo, Italy; [Bice, David M.] Penn State Univ, Dept Geosci, University Pk, PA 16802 USA; [Brinkhuis, Henk] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Deino, Alain] Berkeley Geochronol Ctr, Berkeley, CA 94709 USA; [Lirer, Fabrizio; Sprovieri, Mario] CNR, IAMC, I-80123 Naples, Italy; [Maiorano, Patrizia] Univ Bari, Dipartimento Geol & Geofis, I-70125 Bari, Italy; [Monechi, Simonetta] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy; [Nini, Claudio] Ente Nazl Idrocarburi ENI SpA, Explorat, Explorat & Prod Div, I-20097 San Donato Milanese, Italy; [Nocchi, Marisa] Piazza Univ, Dipartimento Sci Terra, I-06100 Perugia, Italy; [Pross, Joerg] Goethe Univ Frankfurt, Inst Geowissensch, D-60054 Frankfurt, Germany; [Rochette, Pierre; Touchard, Yannick] Univ Aix Marseille 3, CNRS, UMR 6635, CEREGE Europole Arbois, F-13545 Aix En Provence 4, France; [Sagnotti, Leonardo] Ist Nazl Geofis & Vulcanol, I-00143 Rome, Italy; [Tateo, Fabio] CNR, Ist Geosci & Georisorse, Dipartimento Geol Paleontol & Geofis, I-35137 Padua, Italy; [Van Simaeys, Stefaan] Katholieke Univ Leuven, B-3000 Louvain, Belgium; [Williams, Graham L.] Geol Survey Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada	University of Urbino; University of Urbino; Carleton College; Pennsylvania Commonwealth System of Higher Education (PCSHE); Pennsylvania State University; Pennsylvania State University - University Park; Utrecht University; Berkeley Geochronolgy Center; Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Universita degli Studi di Bari Aldo Moro; University of Florence; Eni SpA; Goethe University Frankfurt; Aix-Marseille Universite; Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Istituto Nazionale Geofisica e Vulcanologia (INGV); Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); KU Leuven; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Coccioni, R (通讯作者)，Univ Urbino, Ist Geol, Campus Sci, I-61029 Urbino, Italy.	cron@info-net.it	Sagnotti, Leonardo/AFM-3916-2022; monechi, simonetta/AAN-6148-2020; Sprovieri, Mario/AAY-1021-2020; Brinkhuis, Henk/B-4223-2009; Lirer, Fabrizio/N-5306-2015; Rochette, Pierre/O-4612-2019; Tateo, Fabio/ABA-4862-2021	SPROVIERI, MARIO/0000-0002-7192-5014; COCCIONI, Rodolfo/0000-0003-2333-4030; Church, Nathan/0000-0001-5426-6224; Rochette, Pierre/0000-0002-7362-0660; Sagnotti, Leonardo/0000-0003-3944-201X; Maiorano, Patrizia/0000-0003-4917-1786; Brinkhuis, Henk/0000-0003-0253-6610	Directorate For Geosciences; Division Of Earth Sciences [0732473] Funding Source: National Science Foundation	Directorate For Geosciences; Division Of Earth Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))		[Anonymous], INT SUBCOMMISSION PA; BAUMANN P, 1969, Eclogae Geologicae Helvetiae, V62, P303; Berggren W. 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J	Tang, YZ; Egerton, TA; Kong, L; Marshall, HG				Tang, Ying Zhong; Egerton, Todd A.; Kong, Lesheng; Marshall, Harold G.			Morphological variation and phylogenetic analysis of the dinoflagellate <i>Gymnodinium aureolum</i> from a tributary of Chesapeake Bay	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Chesapeake Bay; dinoflagellate; Gymnodinium aureolum; Gymnodinium maguelonnense; LSU rDNA sequence; morphological variation	SP-NOV GYMNODINIALES; GYRODINIUM-AUREOLUM; DINOPHYCEAE; ULTRASTRUCTURE; KARENIA; GENERA; INFERENCE; TASMANIA; MRBAYES; CYSTS	Cultures of four strains of the dinoflagellate Gymnodinium aureolum (Hulburt) G. Hansen were established from the Elizabeth River, a tidal tributary of the Chesapeake Bay, USA. Light microscopy, scanning electron microscopy, nuclear-encoded large sub-unit rDNA sequencing, and culturing observations were conducted to further characterize this species. Observations of morphology included: a multiple structured apical groove; a peduncle located between the emerging points of the two flagella; pentagonal and hexagonal vesicles on the amphiesma; production and germination of resting cysts; variation in the location of the nucleus within the center of the cell; a longitudinal ventral concavity; and considerable variation in cell width/length and overall cell size. A fish bioassay using juvenile sheepshead minnows detected no ichthyotoxicity from any of the strains over a 48-h period. Molecular analysis confirmed the dinoflagellate was conspecific with G. aureolum strains from around the world, and formed a cluster along with several other Gymnodinium species. Morphological evidence suggests that further research is necessary to examine the relationship between G. aureolum and a possibly closely related species Gymnodinium maguelonnense.	[Egerton, Todd A.; Marshall, Harold G.] Old Dominion Univ, Dept Biol Sci, Norfolk, VA 23529 USA; [Tang, Ying Zhong] SUNY Stony Brook, Marine Sci Res Ctr, Stony Brook, NY 11794 USA; [Kong, Lesheng] Natl Univ Singapore, Computat Biol Grp, Temasek Life Sci Lab, Singapore 117604, Singapore	Old Dominion University; State University of New York (SUNY) System; Stony Brook University; National University of Singapore	Egerton, TA (通讯作者)，Old Dominion Univ, Dept Biol Sci, Norfolk, VA 23529 USA.	tegerton@odu.edu	; Kong, Lesheng/O-8933-2015	Egerton, Todd/0000-0002-0341-7915; Kong, Lesheng/0000-0002-9225-3421				[Anonymous], 2004, Modeltest v2; ARZUL G, 1994, WATER RES, V28, P961, DOI 10.1016/0043-1354(94)90105-8; Bergholtz T, 2006, J PHYCOL, V42, P170, DOI 10.1111/j.1529-8817.2006.00172.x; Biecheler B., 1939, Bulletin de la Societe Zoologique de France, V64, P12; Biecheler B., 1952, Bull. Biol. Fr. 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J	De Schepper, S; Head, MJ				De Schepper, Stijn; Head, Martin J.			New dinoflagellate cyst and acritarch taxa from the Pliocene and Pleistocene of the eastern North Atlantic (DSDP Site 610)	JOURNAL OF SYSTEMATIC PALAEONTOLOGY			English	Article						taxonomy; palynology; marine; Quaternary; neogene	HEMISPHERE GLACIATIONS; SEA	A palynotogical study of Pliocene and Pleistocene deposits from DSDP Hole 610A in the eastern North Atlantic has revealed the presence of several new organic-walled dinoflagellate cyst taxa. Impagidinium cantabrigiense sp. nov. first appeared in the latest Pliocene, within an interval characterised by a paucity of new dinoflagellate cyst species. Operculodinium? eirikianum var. crebrum var. nov. is mostly restricted to a narrow interval near the Mammoth Subchron within the Pliocene (Piacenzian Stage) and may be a morphological adaptation to the changing climate at that time. An unusual morphotype of Melitasphaeridium choanophorum (Deflandre & Cookson, 1955) Harland & Hill, 1979 characterised by a perforated cyst wall is also documented. In addition, the stratigraphic utility of small acritarchs in the late Cenozoic of the northern North Atlantic region is emphasised and three stratigraphically restricted acritarchs Cymatiosphaera latisepta sp. nov., Lavradosphaera crista gen. et sp. nov. and Lavradosphaera lucifer gen. et sp. nov. are formally described.	[De Schepper, Stijn] Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	University of Cambridge; Brock University	De Schepper, S (通讯作者)，Univ Bremen, Geowissensch, Fachbereich 5, Postfach 330 440, D-28334 Bremen, Germany.	sdeschepper@uni-bremen.de; mjhead@brocku.ca	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914				ANSTEY CA, 1992, THESIS U TORONTO TOR, V105; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; CLEMENT BM, 1989, P OC DRILL PROGR SCI, P583; CLEMENT BM, 1987, DEEP SEA DRILLING PR, P635; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; Deflandre G., 1954, COMPTE RENDU SOMMAIR, P257; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DESCHEPPER S, 2006, THESIS U CAMBRIDGE C, P6; Fensome R.A., 1993, Micropaleontology Press Special Paper; HARLAND R, 1979, REV PALAEOBOT PALYNO, V28, P37, DOI 10.1016/0034-6667(79)90023-X; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P423, DOI 10.2973/odp.proc.sr.105.135.1989; Head M. 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Syst. Palaeontol.	MAR	2008	6	1					101	117		10.1017/S1477201907002167	http://dx.doi.org/10.1017/S1477201907002167			17	Evolutionary Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology; Paleontology	271KZ					2025-03-11	WOS:000253788600004
J	Qin, JA; Wu, GX; Zheng, HB; Zhou, Q				Qin, Jungan; Wu, Guoxuan; Zheng, Hongbo; Zhou, Qi			The palynology of the first hard clay layer (late Pleistocene) from the Yangtze delta, China	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Yangtze delta; First Hard Clay Layer; Last Glacial Maximum; palynomorphs	LAST GLACIAL MAXIMUM; SEA-LEVEL RISE; PEDIASTRUM; VEGETATION; SEDIMENTS; RECORDS	This paper reports on palynomorphs of environmentally diagnostic significance that were recovered from the First Hard Clay Layer, a widely distributed stratigraphic unit of late Pleistocene age in the Yangtze delta and adjacent areas in China. The palynomorphs represent the Last Glacial Maximum (LGM) and provide the first palynological evidence for reconstructing the sedimentary environment. The high abundance of the algal palynomorph Concentricystes indicates that the Hard Clay Layer is a freshwater deposit. Dinoflagellate cysts occur in low abundance suggesting that the area had minor marine influence. Spore and pollen assemblages show that the regional upland vegetation of the Yangtze delta and adjacent areas was a broadleaved and coniferous mixed forest with meadows present in the riverine wetlands and on the floodplains. The forest taxa are indicative of a temperate climate and show that the LGM was not a continuously cold and dry period, but was punctuated by relatively warm and relatively wet periods. The palynomorph assemblages indicate that the First Hard Clay Layer in the Yangtze delta and adjacent areas is of lacustrine-fluvial origin, rather than aeolian origin as some researchers have suggested. (c) 2007 Elsevier B.V. All rights reserved.	[Qin, Jungan; Zhou, Qi] Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China; [Qin, Jungan; Wu, Guoxuan; Zheng, Hongbo] Tongji Univ, Coll Environm Sci & Engn, Shanghai 200092, Peoples R China	Tongji University; Tongji University	Qin, JA (通讯作者)，Tongji Univ, State Key Lab Marine Geol, Shanghai 200092, Peoples R China.	qinjungan@163.com	Zheng, Hongbo/LNP-2343-2024; zhou, qi/JEF-7253-2023					*AC SIN, 1985, PHYS GEOGR CHIN; An ZS., 1990, LOESS QUATERNARY G 2, P1; [Anonymous], 1980, VEGETATION CHINA; Bing Deng, 1999, MARINE GEOLOGY QUATE, V19, P29; CAI YL, 1913, J LAKE SCI, V13, P118; Chen Q.Q., 1998, SCI GEOGRAPHICA SINI, V18, P53; Chen Q.X., 1998, CHINESE SCI BULL, V43, P2557; CHEN ZY, 1993, MAR GEOL, V112, P13, DOI 10.1016/0025-3227(93)90158-R; Chen ZY, 1999, ENVIRON GEOL, V37, P333, DOI 10.1007/s002540050392; DAVIS CA, 1916, NATL ACAD SCI US AM, V11, P114; EVITT W, 1963, AM J SCI, V261, P890, DOI 10.2475/ajs.261.9.890; Geng X.S., 1981, Acta Oceanol. Sin., V3, P114; GRENFELL HR, 1995, REV PALAEOBOT PALYNO, V84, P201, DOI 10.1016/0034-6667(94)00134-6; Jiang D., 1991, CLIMATE YANGTZE DELT, P42; Li C.X., 1986, Chin. Sci. Bull., V31, P1650; Li CX, 2001, MAR GEOL, V173, P97, DOI 10.1016/S0025-3227(00)00169-9; LI CX, 1998, STRATIGRAPHY LATE QU; LIU BZ, 1995, MARINE GEOLOGY QUATE, V15, P17; MIN QB, 1979, J TONGJI U, V7, P109; Moore P.D., 1991, POLLEN ANAL; NIELSEN H, 1992, REV PALAEOBOT PALYNO, V74, P55, DOI 10.1016/0034-6667(92)90138-7; ROCHON A, 1999, DISTRIBUTION RECENT, P12; Shi Y., 1997, J. Glaciol. Geocryol, V19, P97; STANLEY DJ, 1994, SCIENCE, V265, P228, DOI 10.1126/science.265.5169.228; Stanley DJ, 1996, GEOLOGY, V24, P1083, DOI 10.1130/0091-7613(1996)024<1083:NSDAAF>2.3.CO;2; SUN SC, 1987, SCI CHINA SER B, V2, P1329; Sun XJ, 2000, ACTA BOT SIN, V42, P1201; Sun XJ, 1999, MAR GEOL, V156, P211, DOI 10.1016/S0025-3227(98)00180-7; Tang L.Y., 1994, ACTA OCEANOL SIN, V16, P78; WANG K, 1986, ACTA OCEANOL SIN, V5, P257; Wang K.F., 1983, ACTA PALAEONTOL SIN, V22, P468; Wang K.F., 1982, J Geogr, V37, P261; WANG KF, 1979, J TONGJI U, V7, P57; WANG KF, 1981, CHINESE SCI BULL, V26, P540; Wu J.M., 1988, SE CULTURES, P16; Xue XX, 2000, CHINESE SCI BULL, V45, P853, DOI 10.1007/BF02887417; Yan Q.S., 1987, Acta Oceanol. Sin., V9, P744; Yang H.R., 1984, OCEANOL LIMNOL SINIC, V15, P1; Yao T.D., 1999, SCI CHIN D, V29, P175; Yi S, 2003, QUATERNARY SCI REV, V22, P1501, DOI 10.1016/S0277-3791(03)00080-5; YU HJ, 1995, ADV EARTH SCI, V10, P531; ZHENG XM, 1999, AEOLIAN LOESS DEPOSI; Zhu Y., 1981, CHINESE SCI BULL, V26, P1195	43	25	33	2	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	2008	149	1-2					63	72		10.1016/j.revpalbo.2007.10.003	http://dx.doi.org/10.1016/j.revpalbo.2007.10.003			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	276ST					2025-03-11	WOS:000254163500006
J	Sangiorgi, F; Brumsack, HJ; Willard, DA; Schouten, S; Stickley, CE; O'Regan, M; Reichart, GJ; Damste, JSS; Brinkhuis, H				Sangiorgi, Francesca; Brumsack, Hans-Juergen; Willard, Debra A.; Schouten, Stefan; Stickley, Catherine E.; O'Regan, Matthew; Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Brinkhuis, Henk			A 26 million year gap in the central Arctic record at the greenhouse-icehouse transition: Looking for clues	PALEOCEANOGRAPHY			English	Article							ORGANIC-MATTER; SEDIMENTS; CALIBRATION; CLIMATES; MARGINS; LIPIDS; UPLIFT; SEA	The Cenozoic record of the Lomonosov Ridge (central Arctic Ocean) recovered during Integrated Ocean Drilling Program (IODP) Expedition 302 revealed an unexpected 26 Ma hiatus, separating middle Eocene (similar to 44.4 Ma) from lower Miocene sediments (similar to 18.2 Ma). To elucidate the nature of this unconformity, we performed a multiproxy palynological (dinoflagellate cysts, pollen, and spores), micropaleontological (siliceous microfossils), inorganic, and organic (Tetra Ether Index of lipids with 86 carbon atoms (TEX86) and Branched and Isoprenoid Tetraether (BIT)) geochemical analysis of the sediments from similar to 5 m below to similar to 7 m above the hiatus. Four main paleoenvironmental phases (A-D) are recognized in the sediments encompassing the unconformity, two below (A-B) and two above (C-D): (A) Below the hiatus, proxies show relatively warm temperatures, with Sea Surface Temperatures (TEX86-derived SSTs) of about 8 degrees C and high fresh to brackish water influence. (B) Approaching the hiatus, proxies indicate a cooling trend (TEX86-derived SSTs of similar to 5 degrees C), increased freshwater influence, and progressive shoaling of the Lomonosov Ridge drilling site, located close to or at sea level. (C) The interval directly above the unconformity contains sparse reworked Cretaceous to Oligocene dinoflagellate cysts. Sediments were deposited in a relatively shallow, restricted marine environment. Proxies show the simultaneous influence of both fresh and marine waters, with alternating oxic and anoxic conditions. Pollen indicates a relatively cold climate. Intriguingly, TEX86-derived SSTs are unexpectedly high, similar to 15-19 degrees C. Such warm surface waters may be partially explained by the ingression of warmer North Atlantic waters after the opening of the Fram Strait during the early Miocene. (D) Sediments of the uppermost interval indicate a phase of extreme oxic conditions, and a well-ventilated environment, which occurred after the complete opening of the Fram Strait. Importantly, and in contrast with classical postrifting thermal subsidence models for passive margins, our data suggest that sediment erosion and/or nondeposition that generated the hiatus was likely due to a progressive shoaling of the Lomonosov Ridge. A shallow water setting both before and after the hiatus suggests that the Lomonosov Ridge remained at or near sea level for the duration of the gap in the sedimentary record. Interacting sea level changes and/or tectonic activity (possibly uplift) must be invoked as possible causes for such a long hiatus.	[Sangiorgi, Francesca; Brinkhuis, Henk] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Sangiorgi, Francesca; Schouten, Stefan; Damste, Jaap S. Sinninghe] Royal Netherlands Inst Sea Res NIOZ, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Texel, Netherlands; [Brumsack, Hans-Juergen] Carl von Ossietzky Univ Oldenburg, Inst Chem & Biol Marine Environm ICBM, D-26111 Oldenburg, Germany; [Stickley, Catherine E.] Polar Environm Ctr, Norwegian Polar Inst, N-9296 Tromso, Norway; [O'Regan, Matthew] Univ Rhode Isl, Grad Sch Oceanog, Narragansett, RI 02882 USA; [Reichart, Gert-Jan; Damste, Jaap S. Sinninghe] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Willard, Debra A.] US Geol Survey, Reston, VA 20192 USA	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Carl von Ossietzky Universitat Oldenburg; Norwegian Polar Institute; University of Rhode Island; Utrecht University; United States Department of the Interior; United States Geological Survey	Sangiorgi, F (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		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J	Van Nieuwenhove, N; Bauch, HA; Matthiessen, J				Van Nieuwenhove, Nicolas; Bauch, Henning A.; Matthiessen, Jens			Last interglacial surface water conditions in the eastern Nordic Seas inferred from dinocyst and foraminiferal assemblages	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; planktic foraminifers; Nordic Seas; last interglacial; marine oxygen isotope stage 5e	DINOFLAGELLATE CYST ASSEMBLAGES; NORTHWEST NORTH-ATLANTIC; ABRUPT CLIMATE-CHANGE; NORWEGIAN SEA; THERMOHALINE CIRCULATION; LATE QUATERNARY; ADJACENT SEAS; RAPID CHANGES; BALTIC SEA; ICE COVER	Marine sediments from the Voring Plateau (Norwegian Sea) have been studied for their dinoflagellate cyst (dinocyst) and foraminiferal content in order to reconstruct sea-surface conditions in the eastern Norwegian Sea during Marine Isotope Stage (MIS) 5e. In combination with stable oxygen isotope and ice rafted detritus (IRD) data, the variations in foraminiferal and dinocyst assemblage composition reflect a stepwise transition from the final phase of deglaciation (Termination II) into typical interglacial conditions. This stepwise change is repeated subsequently during the cooling conditions of glacial inception towards MIS 5d. The interval studied is characterized by relatively high abundances of Bitectatodinium tepikiense, in comparison to present-day values in the area, indicating a larger seasonal temperature amplitude with enhanced surface water stratification during MIS 5e. The important occurrence of the warm-temperate dinocyst Spiniferites mirabilis s.l. concurrent with subpolar foraminifers Turborotalita quinqueloba, Globigerina bulloides, and Globigerinita glutinata reveals that most pronounced interglacial marine conditions prevailed in the area just prior to the transition towards MIS 5d. The late stratigraphic position of this phase in the interglacial is verified by comparison with dinocyst data from south of Iceland, manifesting its over-regional implication. Besides the good agreement in dinocyst and foraminiferal assemblage changes, the variations in and between both fossil assemblages also point to the existence of some significant surface water variability in the eastern Norwegian Sea during MIS 5e. (c) 2007 Elsevier B.V. All rights reserved.	[Van Nieuwenhove, Nicolas; Bauch, Henning A.] IFM Geomar Leibniz Inst Marine Sci, D-24148 Kiel, Germany; [Bauch, Henning A.] Mainz Acad Sci Humanities & Literature, D-55131 Mainz, Germany; [Matthiessen, Jens] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Van Nieuwenhove, N (通讯作者)，IFM Geomar Leibniz Inst Marine Sci, Wischhofstr 1-3, D-24148 Kiel, Germany.	nvannieuwenhove@ifm-geomar.de	Van Nieuwenhove, Nicolas/IAQ-1532-2023	Matthiessen, Jens/0000-0002-6952-2494; Van Nieuwenhove, Nicolas/0000-0001-6369-2751				Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; ANDERSSON C, 2003, PALEOCEANOGRAPHY, V18, DOI DOI 10.1029/200PA000654; [Anonymous], [No title captured]; [Anonymous], 1971, POLLEN SPORES; Bauch HA, 1999, PALAEOGEOGR PALAEOCL, V145, P95, DOI 10.1016/S0031-0182(98)00104-7; Bauch HA, 1996, QUATERNARY RES, V46, P260, DOI 10.1006/qres.1996.0065; Bauch HA, 2000, PALEOCEANOGRAPHY, V15, P76, DOI 10.1029/1998PA000343; Bauch HA, 2001, QUATERNARY SCI REV, V20, P659, DOI 10.1016/S0277-3791(00)00098-6; Bauch Henning A., 1997, Grzybowski Foundation Special Publication, V5, P83; BAUMANN KH, 1995, QUATERNARY RES, V43, P185, DOI 10.1006/qres.1995.1019; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Be A.W.H., 1977, P1; Be A. 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Micropaleontol.	FEB 20	2008	66	3-4					247	263		10.1016/j.marmicro.2007.10.004	http://dx.doi.org/10.1016/j.marmicro.2007.10.004			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	276IH					2025-03-11	WOS:000254134000007
J	Sluijs, A; Röhl, U; Schouten, S; Brumsack, HJ; Sangiorgi, F; Damsté, JSS; Brinkhuis, H				Sluijs, Appy; Roehl, Ursula; Schouten, Stefan; Brumsack, Hans-J.; Sangiorgi, Francesca; Damste, Jaap S. Sinninghe; Brinkhuis, Henk			Arctic late Paleocene-early Eocene paleoenvironments with special emphasis on the Paleocene-Eocene thermal maximum (Lomonosov Ridge, Integrated Ocean Drilling Program Expedition 302)	PALEOCEANOGRAPHY			English	Review							ATMOSPHERIC CARBON-DIOXIDE; SEA-SURFACE CONDITIONS; ORGANIC-CARBON; DINOFLAGELLATE CYSTS; ISOTOPE EXCURSION; METHANE HYDRATE; RICH SEDIMENTS; NORTH-ATLANTIC; MARINE; CLIMATE	We reconstruct the latest Paleocene and early Eocene (similar to 57-50 Ma) environmental trends in the Arctic Ocean and focus on the Paleocene-Eocene thermal maximum (PETM) (similar to 55 Ma), using strata recovered from the Lomonosov Ridge by the Integrated Ocean Drilling Program Expedition 302. The Lomonosov Ridge was still partially subaerial during the latest Paleocene and earliest Eocene and gradually subsided during the early Eocene. Organic dinoflagellate cyst (dinocyst) assemblages point to brackish and productive surface waters throughout the latest Paleocene and early Eocene. Dinocyst assemblages are cosmopolitan during this time interval, suggesting warm conditions, which is corroborated by TEX86'-reconstructed temperatures of 15 degrees-18 degrees C. Inorganic geochemistry generally reflects reducing conditions within the sediment and euxinic conditions during the upper lower Eocene. Spectral analysis reveals that the cyclicity, recorded in X-ray fluorescence scanning Fe data from close to Eocene thermal maximum 2 (similar to 53 Ma, presence confirmed by dinocyst stratigraphy), is related to precession. Within the lower part of the PETM, proxy records indicate enhanced weathering, runoff, anoxia, and productivity along with sea level rise. On the basis of total organic carbon content and variations in sediment accumulation rates, excess organic carbon burial in the Arctic Ocean appears to have contributed significantly to the sequestration of injected carbon during the PETM.	[Sluijs, Appy; Sangiorgi, Francesca; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Brumsack, Hans-J.] Carl von Ossietzky Univ Oldenburg, Inst Biol Chem & Marine Environm, D-26111 Oldenburg, Germany; [Roehl, Ursula] Univ Bremen, Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Schouten, Stefan] Royal Netherlands Inst Sea Res, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Netherlands; [Damste, Jaap S. Sinninghe] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; Carl von Ossietzky Universitat Oldenburg; University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		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J	Taylor, FJR; Hoppenrath, M; Saldarriaga, JF				Taylor, F. J. R.; Hoppenrath, Mona; Saldarriaga, Juan F.			Dinoflagellate diversity and distribution	BIODIVERSITY AND CONSERVATION			English	Article						alveolate; dinoflagellates; dinokaryon; dinophyceae; distribution; fossil; morphospecies; resting cyst	CATENELLA SPECIES COMPLEX; TOXIC DINOFLAGELLATE; PHYLOGENY; SEQUENCES; BIOGEOGRAPHY; EUKARYOTES; MORPHOLOGY; EVOLUTION; TRANSPORT; EMPHASIS	Dinoflagellates are common to abundant in both marine and freshwater environments. They are particularly diverse in the marine plankton where some cause "red tides" and other harmful blooms. More than 2,000 extant species have been described, only half of which are photosynthetic. They include autotrophs, mixotrophs and grazers. They are biochemically diverse, varying in photosynthetic pigments and toxin production ability. Some are important sources of bioluminescence in the ocean. They can host intracellular symbionts or be endosymbionts themselves. Most of the photosynthetic "zooxanthellae" of invertebrate hosts are mutualistic dinoflagellate symbionts, including all those essential to reef-building corals. Roughly 5% are parasitic on aquatic organisms. The fossil record, consisting of more than 2,500 species, shows a rapid radiation of cysts, starting in the Triassic, peaking in the Cretaceous, and declining throughout the Cenozoic. Marine species with a benthic, dormant cyst stage are confined to the continental shelf and fossil cysts can be used as markers of ancient coastlines. Northern and southern hemispheres contain virtually identical communities within similar latitudes, separated by a belt of circumtropical species. A few endemics are present in tropical and polar waters. Some benthic dinoflagellates are exclusively tropical, including a distinct phycophilic community, some of which are responsible for ciguatera fish poisoning. In lakes chemical and grazing effects can be important. Predatory dinoflagellates co-occur with their prey, often diatoms.	[Taylor, F. J. R.; Hoppenrath, Mona; Saldarriaga, Juan F.] Univ British Columbia, Dept Bot, Vancouver, BC V6T 1Z4, Canada; [Taylor, F. J. 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Conserv.	FEB	2008	17	2					407	418		10.1007/s10531-007-9258-3	http://dx.doi.org/10.1007/s10531-007-9258-3			12	Biodiversity Conservation; Ecology; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	255WR					2025-03-11	WOS:000252689400013
J	Leander, BS; Hoppenrath, M				Leander, Brian S.; Hoppenrath, Mona			Ultrastructure of a novel tube-forming, intracellular parasite of dinoflagellates:: <i>Parvilucifera prorocentri</i> sp nov (Alveolata, Myzozoa)	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						Colpodella; group I alveolates; Parvilucifera; Perkinsus; Syndinium; ultrastructure	GENETIC DIVERSITY; FINE-STRUCTURE; N-SP; PHYLOGENETIC POSITION; EVOLUTIONARY HISTORY; MICROBIAL EUKARYOTES; PERKINSUS-MARINUS; SYNDINIUM SP; FLAGELLATE; APICOMPLEXA	We have characterized the intracellular development and ultrastructure of a novel parasite that infected the marine benthic dinoflagellate Prorocentrum fukuyoi. The parasite possessed a combination of features described for perkinsids and syndineans, and also possessed novel characters associated with its parasitic life cycle. Reniform zoospores, about 4 mu m long, possessed a transverse flagellum, alveoli, a refractile body, a mitochondrion with tubular cristae, a syndinean-like nucleus with condensed chromatin, micronemes, bipartite trichocysts with square profiles (absent in perkinsids) and oblong microbodies. Like Parvilucifera, the zoospores also possessed a shorter posterior flagellum, a heteromorphic pair of central microtubules in the anterior axoneme and a reduced pseudoconoid positioned directly above an orthogonal pair of basal bodies. Early developmental stages consisted of a sporangium about 5-15 mu m in diam that contained spherical bodies and amorphous spaces. The undifferentiated sporangium increased to about 20-25 mu m in diam before being enveloped by a wall with a convoluted mid-layer. The sporangium differentiated into an unordered mass of zoospores that escaped from the cyst through a pronounced germ tube about 4-5 mu m in diam and 10-15 mu m long. Weakly developed germ tubes have been described in Perkinsus but are absent altogether in Parvilucifera and syndineans. Comparison of these data with other myzozoans led us to classify the parasite as Parvilucifera prorocentri sp. nov., Myzozoa. Although we were hesitant to erect a new genus name in the absence of molecular sequence data, our ultrastructural data strongly indicated that this parasite is most closely related to perkinsids and syndineans, and represents an intriguing candidate for the cellular identity of a major subclade of Group I alveolates. (C) 2007 Elsevier GmbH. All rights reserved.	[Leander, Brian S.] Univ British Columbia, Dept Bot, Canadian Inst Adv Res, Program Integrated Microbial Biodivers, Vancouver, BC V6T 1Z4, Canada; Univ British Columbia, Dept Zool, Canadian Inst Adv Res, Program Integrated Microbial Biodivers, Vancouver, BC V6T 1Z4, Canada	University of British Columbia; Canadian Institute for Advanced Research (CIFAR); Canadian Institute for Advanced Research (CIFAR); University of British Columbia	Leander, BS (通讯作者)，Univ British Columbia, Dept Bot, Canadian Inst Adv Res, Program Integrated Microbial Biodivers, Vancouver, BC V6T 1Z4, Canada.	bleander@interchange.ubc.ca						Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; AZEVEDO C, 1989, J PARASITOL, V75, P627, DOI 10.2307/3282915; AZEVEDO C, 1990, PARASITOLOGY, V100, P351, DOI 10.1017/S0031182000078616; Blackbourn J, 1998, CAN J ZOOL, V76, P942, DOI 10.1139/cjz-76-5-942; BRUGEROLLE G, 1979, PROTISTOLOGICA, V15, P183; Brugerolle G, 2003, EUR J PROTISTOL, V39, P101, DOI 10.1078/0932-4739-00910; Brugerolle G, 2002, EUR J PROTISTOL, V37, P379, DOI 10.1078/0932-4739-00837; Cachon J., 1987, The Biology of Dinoflagellates, P571; Cavalier-Smith T, 2004, EUR J PROTISTOL, V40, P185, DOI 10.1016/j.ejop.2004.01.002; Chatton E, 1936, CR HEBD ACAD SCI, V203, P573; Chatton E., 1934, CR Acad Sci Paris, V199, P252; Coats DW, 1999, J EUKARYOT MICROBIOL, V46, P402, DOI 10.1111/j.1550-7408.1999.tb04620.x; Díez B, 2001, APPL ENVIRON MICROB, V67, P2932, DOI 10.1128/AEM.67.7.2932-2941.2001; DODGE J D, 1971, Protistologica, V7, P399; DODGE J D, 1971, Protistologica, V7, P295; Dolven JK, 2007, PROTIST, V158, P65, DOI 10.1016/j.protis.2006.07.004; Dungan CF, 2006, J EUKARYOT MICROBIOL, V53, P316, DOI 10.1111/j.1550-7408.2006.00120.x; Fernández I, 1999, EUR J PROTISTOL, V35, P255, DOI 10.1016/S0932-4739(99)80002-9; Fernández I, 1999, EUR J PROTISTOL, V35, P55, DOI 10.1016/S0932-4739(99)80022-4; FRITZ L, 1992, J PHYCOL, V28, P312, DOI 10.1111/j.0022-3646.1992.00312.x; Groisillier A, 2006, AQUAT MICROB ECOL, V42, P277, DOI 10.3354/ame042277; GUNDERSON JH, 2002, CHESAPEAKE BAY J EUK, V49, P469; Harada A, 2007, PROTIST, V158, P337, DOI 10.1016/j.protis.2007.03.005; HOLLANDE A, 1974, Protistologica, V10, P413; Hoppenrath M, 2006, J EUKARYOT MICROBIOL, V53, P327, DOI 10.1111/j.1550-7408.2006.00110.x; Kuvardina ON, 2002, J EUKARYOT MICROBIOL, V49, P498, DOI 10.1111/j.1550-7408.2002.tb00235.x; Leander BS, 2004, J PHYCOL, V40, P341, DOI 10.1111/j.1529-8817.2004.03129.x; Leander BS, 2003, J EUKARYOT MICROBIOL, V50, P334, DOI 10.1111/j.1550-7408.2003.tb00145.x; Leander BS, 2003, TRENDS ECOL EVOL, V18, P395, DOI 10.1016/S0169-5347(03)00152-6; LESTER RJG, 1981, J INVERTEBR PATHOL, V37, P181, DOI 10.1016/0022-2011(81)90073-2; López-García P, 2001, NATURE, V409, P603, DOI 10.1038/35054537; MANIER J-F, 1971, Protistologica, V7, P213; Maranda L, 2001, J PHYCOL, V37, P245, DOI 10.1046/j.1529-8817.2001.037002245.x; MIGNOT J P, 1975, Protistologica, V11, P429; Moon-van der Staay SY, 2001, NATURE, V409, P607, DOI 10.1038/35054541; Moreira D, 2002, TRENDS MICROBIOL, V10, P31, DOI 10.1016/S0966-842X(01)02257-0; Murray S, 2007, PHYCOL RES, V55, P91, DOI 10.1111/j.1440-1835.2007.00452.x; Myl'nikov AP, 2000, ZOOL ZH, V79, P261; MYLNIKOV AP, 1991, ZOOL ZH, V70, P5; MYLNIKOV AP, 1998, SANKPTERSBURG, V3, P55; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; Park MG, 2004, J EUKARYOT MICROBIOL, V51, P145, DOI 10.1111/j.1550-7408.2004.tb00539.x; PERKINS FO, 1976, J PARASITOL, V62, P959, DOI 10.2307/3279192; Perkins FO, 1996, J SHELLFISH RES, V15, P67; RIS H, 1974, J CELL BIOL, V60, P702, DOI 10.1083/jcb.60.3.702; Saldarriaga JF, 2004, EUR J PROTISTOL, V40, P85, DOI 10.1016/j.ejop.2003.11.003; Saldarriaga JF, 2003, INT J SYST EVOL MICR, V53, P355, DOI 10.1099/ijs.0.02328-0; Siddall Mark E., 2001, American Museum Novitates, V3314, P1, DOI 10.1206/0003-0082(2001)314<0001:MDOTPP>2.0.CO;2; Siddall ME, 1997, PARASITOLOGY, V115, P165, DOI 10.1017/S0031182097001157; Simpson AGB, 1996, SYST PARASITOL, V33, P187, DOI 10.1007/BF01531200; Skovgaard A, 2005, PROTIST, V156, P413, DOI 10.1016/j.protis.2005.08.002; SOYER MO, 1974, VIE MILIEU A BIOL MA, V24, P191; Takishita K, 2007, PROTIST, V158, P51, DOI 10.1016/j.protis.2006.07.003; Uhlig G., 1964, Helgolander Wissenschaftliche Meeresuntersuchungen, V11, P178, DOI 10.1007/BF01612370; Worden AZ, 2006, AQUAT MICROB ECOL, V43, P165, DOI 10.3354/ame043165	55	48	51	0	14	ELSEVIER GMBH, URBAN & FISCHER VERLAG	JENA	OFFICE JENA, P O BOX 100537, 07705 JENA, GERMANY	0932-4739			EUR J PROTISTOL	Eur. J. Protistol.	FEB	2008	44	1					55	70		10.1016/j.ejop.2007.08.004	http://dx.doi.org/10.1016/j.ejop.2007.08.004			16	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	276BR	17936600				2025-03-11	WOS:000254116700006
J	Shiraishi, T; Hiroishi, S; Taino, S; Ishikawa, T; Hayashi, Y; Sakamoto, S; Yamaguchi, M; Imai, I				Shiraishi, Tomotaka; Hiroishi, Shingo; Taino, Seiya; Ishikawa, Tetsu; Hayashi, Yoshihiro; Sakamoto, Setsuko; Yamaguchi, Mineo; Imai, Ichiro			Identification of overwintering vegetative cells of the bivalve-killing dinoflagellate <i>Heterocapsa circularisquama</i> in Uranouchi Inlet, Kochi Prefecture, Japan	FISHERIES SCIENCE			English	Article						body scale; Heterocapsa circularisquama; indirect fluorescent antibody technique; overwintering; population dynamics; temperature; temporary cyst; vegetative cell	CHATTONELLA-VERRUCULOSA RAPHIDOPHYCEAE; HARMFUL DINOFLAGELLATE; CULTURE; GROWTH; DINOPHYCEAE	Red tides of Heterocapsa circularisquama have led to serious damage of bivalve aquacultures in western coastal areas of Japan. To understand the whole picture regarding the ecology of this species, it is essential to clarify its overwintering mechanisms. In this study, the population dynamics of H. circularisquama were investigated from February 2004 to November 2005, and overwintering cells were identified for the first time in water columns of Uranouchi Inlet, Kochi Prefecture, Japan. Heterocapsa circularisquama cells were detected by the indirect fluorescent antibody technique using monoclonal antibodies that specifically recognize and react to this species. Vegetative cells were almost always detected from the first observation in February 2004 to November 2005 with temperatures of 10.5-30.6 degrees C. During the period from winter to spring, this species survived in areas with a temperature higher than 10 degrees C. The overwintering cells of H. circularisquama were isolated in March 2004, and identification was made via observation of the morphology and body scales of the cultured cells. These overwintering cells were identified as H. circularisquama and reacted to the monoclonal antibody. These results indicate that H. circularisquama can overwinter and survive throughout the year in a vegetative cell state in Uranouchi Inlet.	[Shiraishi, Tomotaka; Imai, Ichiro] Kyoto Univ, Lab Marine Environm Microbiol, Div Appl Biosci, Grad Sch Agr,Sakyo Ku, Kyoto 6068502, Japan; [Hiroishi, Shingo] Fukui Prefectural Univ, Fac Biotechnol, Dept Marine Biosci, Microbiol Lab, Fukui 9170003, Japan; [Taino, Seiya; Ishikawa, Tetsu; Hayashi, Yoshihiro] Kochi Prefectural Fisheries Expt Stn, Kochi 7850167, Japan; [Sakamoto, Setsuko; Yamaguchi, Mineo] Natl Res Inst Fisheries & Environm Inland Sea, Red Tide Expt Div, Fisheries Res Agcy, Hiroshima 7390452, Japan	Kyoto University; Fukui Prefectural University; Japan Fisheries Research & Education Agency (FRA)	Imai, I (通讯作者)，Kyoto Univ, Lab Marine Environm Microbiol, Div Appl Biosci, Grad Sch Agr,Sakyo Ku, Kyoto 6068502, Japan.	imai1ro@kais.kyoto-u.ac.jp						CHEN LCM, 1969, J PHYCOL, V5, P211, DOI 10.1111/j.1529-8817.1969.tb02605.x; Hiroishi S, 2002, FISHERIES SCI, V68, P627, DOI 10.2331/fishsci.68.sup1_627; HONJO T, 1990, TOXIC MARINE PHYTOPLANKTON, P165; HONJO T, 1999, B PLANKTON SOC JPN, V46, P180; Honjo T, 1998, HARMFUL ALGAE, P224; Horiguchi Takeo, 1995, Phycological Research, V43, P129, DOI 10.1111/j.1440-1835.1995.tb00016.x; IMADA N, 2001, HARMFUL ALGAL BLOOMS, P474; Imai I, 1996, FISHERIES SCI, V62, P834, DOI 10.2331/fishsci.62.834; IMAI I, 1987, MAR BIOL, V94, P287, DOI 10.1007/BF00392942; IMAI I, 1988, Bulletin of Plankton Society of Japan, V35, P35; IMAI I, 1989, MAR BIOL, V103, P235, DOI 10.1007/BF00543353; IMAI I, 1993, NIPPON SUISAN GAKK, V59, P1169; Imai Ichiro, 2006, Plankton & Benthos Research, V1, P71; Itakura S., 1990, B NANSEI NATL FISH R, V23, P27; Iwataki M, 2004, PHYCOLOGIA, V43, P394, DOI 10.2216/i0031-8884-43-4-394.1; Matsuyama Y, 2001, J SHELLFISH RES, V20, P1269; MATSUYAMA Y, 2001, HARMFUL ALGAL BLOOMS, P411; Matsuyama Yukihiko, 2003, Bulletin of Fisheries Research Agency, V7, P24; Nakanishi Katsuyuki, 1999, Bulletin of Plankton Society of Japan, V46, P161; NAKATA K, 1987, Bulletin of Plankton Society of Japan, V34, P199; Shiraishi Tomotaka, 2007, Plankton & Benthos Research, V2, P49, DOI 10.3800/pbr.2.49; Tamai K., 1999, BULL PLANKTON SOC JP, V46, P153; TERADA K, 1987, Bulletin of Plankton Society of Japan, V34, P201; Yamaguchi M, 1997, J PLANKTON RES, V19, P1167, DOI 10.1093/plankt/19.8.1167; Yamatogi T, 2005, NIPPON SUISAN GAKK, V71, P746, DOI 10.2331/suisan.71.746; Yoshida Takashi, 2001, Phycological Research, V49, P13; YOSHIMATSU S, 1987, Bulletin of Plankton Society of Japan, V34, P25	27	1	3	1	5	BLACKWELL PUBLISHING	OXFORD	9600 GARSINGTON RD, OXFORD OX4 2DQ, OXON, ENGLAND	0919-9268			FISHERIES SCI	Fish. Sci.	FEB	2008	74	1					128	136		10.1111/j.1444-2906.2007.01502.x	http://dx.doi.org/10.1111/j.1444-2906.2007.01502.x			9	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	258VP					2025-03-11	WOS:000252897900016
J	Lee, YJ; Choi, JK; Kim, EK; Youn, SH; Yang, EJ				Lee, Young-Ju; Choi, Joong-Ki; Kim, Eun-Ki; Youn, Seok-Hyun; Yang, Eun-Jin			Field experiments on mitigation of harmful algal blooms using a Sophorolipid-Yellow clay mixture and effects on marine plankton	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; harmful algal blooms; mitigation; sophorolipid; yellow clay	RED-TIDE; DINOFLAGELLATE; CYSTS; DINOPHYCEAE; LOESS	This study examined a new method of mitigating harmful algal blooms (HABs) by combining biosurfactant sophorolipid and yellow clay. To investigate the effects and practicability of this HAB mitigation method, field experiments were carried out during a Cochlodinium bloom near Miruk Island, South Korea, in August 2002. Field experiments examined the effects of sophorolipid and yellow clay on Cochlodinium bloom mitigation and on marine plankton such as bacteriaplankton, heterotrophic protists, and zooplankton. A mixture of 5 mg l(-1) sophorolipid and 1 g l(-1) yellow clay was sprayed directly on the sea surface and its effect was compared with that of 10 g l(-1) of yellow clay applied under similar conditions. The sophorolipid-yellow clay mixture more efficiently mitigated the Cochlodinium bloom (95% removal efficiency after 30 min) than yellow clay alone (79% after 30 min). Further, no variation in bacterial abundance occurred 30 min after spraying the sophorolipid-yellow clay mixture. After 30 min, heterotrophic protist abundance at the surface decreased 21 and 41 %, respectively, following the sophorolipid-yellow clay mixture and yellow clay treatments. Zooplankton decreased by 38% 15 min after spraying the mixture and 67% 30 min after spraying the yellow clay. These results indicate that the mixture of sophorolipid and yellow clay had a less adverse effect on bacteriaplankton, heterotrophic protists, and zooplankton than the yellow clay, suggesting that the sophorolipid-yellow clay mixture can mitigate HABs efficiently with fewer negative effects on the pelagic ecosystem. (c) 2007 Elsevier B.V. All rights reserved.	[Lee, Young-Ju; Choi, Joong-Ki] Inha Univ, Dept Oceanog, Inchon 402751, South Korea; [Kim, Eun-Ki] Inha Univ, Dept Biol Engn, Inchon 402751, South Korea; [Youn, Seok-Hyun] E Sea Fisheries Res Inst, Kangnung 210861, South Korea; [Yang, Eun-Jin] KORDI, Marine Environm Res Dept, Seoul 425600, South Korea	Inha University; Inha University; Korea Institute of Ocean Science & Technology (KIOST)	Choi, JK (通讯作者)，Inha Univ, Dept Oceanog, 253 Yonghyun Dong, Inchon 402751, South Korea.	jkchoi@inha.ae.kr		Yang, Eun Jin/0000-0002-8639-5968	National Research Foundation of Korea [과C6A2604] Funding Source: Korea Institute of Science & Technology Information (KISTI), National Science & Technology Information Service (NTIS)	National Research Foundation of Korea(National Research Foundation of Korea)		ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BAE HM, 2000, P AUT M KOR FISH SOC, P143; Baek SH, 2003, J MICROBIOL BIOTECHN, V13, P651; Chen CZS, 2002, BIOMATERIALS, V23, P3359, DOI 10.1016/S0142-9612(02)00036-4; Choi Hee Gu, 1998, Journal of the Korean Fisheries Society, V31, P109; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; Jeong HJ, 1999, MAR ECOL PROG SER, V176, P263, DOI 10.3354/meps176263; Jeong HJ, 2002, PHYCOLOGIA, V41, P643, DOI 10.2216/i0031-8884-41-6-643.1; Jeong HJ, 2001, J EUKARYOT MICROBIOL, V48, P298, DOI 10.1111/j.1550-7408.2001.tb00318.x; Jeong Seong-Youn, 2000, Journal of the Korean Fisheries Society, V33, P339; JUNG KS, 2000, THESI CHOSUN U GWANG; Kang S.J., 2001, J KOREA TECHNOL SOC, V9, P11; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kim Sung-Jae, 1999, Journal of the Korean Fisheries Society, V32, P706; KIM WK, 1992, THESIS INHA U; Lee S.W. R., 2002, P ASME INT MECH ENG, P1; Lee SM, 1998, MICROSCALE THERM ENG, V2, P31; *NAT FISH RES DEV, 1998, RED TID KOR; Park JG, 2001, PHYCOLOGIA, V40, P292, DOI 10.2216/i0031-8884-40-3-292.1; Park Young-Tae, 1998, Journal of the Korean Fisheries Society, V31, P767; Park Young-Tae, 1998, Journal of the Korean Fisheries Society, V31, P920; PARSONS TR, 1987, MANUAL CHEM BIOL MET; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; Shumway SE, 2003, AQUAC RES, V34, P1391, DOI 10.1111/j.1365-2109.2003.00958.x; SOURNIA A, 1991, J PLANKTON RES, V13, P1093, DOI 10.1093/plankt/13.5.1093; Sun XX, 2004, HYDROBIOLOGIA, V519, P153, DOI 10.1023/B:HYDR.0000026502.05971.bf; Sun XX, 2004, J EXP MAR BIOL ECOL, V304, P35, DOI 10.1016/j.jembe.2003.11.020; Sun XX, 2004, MAR POLLUT BULL, V48, P937, DOI 10.1016/j.marpolbul.2003.11.021; Sun XX, 2004, MAR POLLUT BULL, V48, P863, DOI 10.1016/j.marpolbul.2003.11.002	30	97	111	4	49	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	FEB	2008	7	2					154	162		10.1016/j.hal.2007.06.004	http://dx.doi.org/10.1016/j.hal.2007.06.004			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	257IU					2025-03-11	WOS:000252793200004
J	Fauchot, J; Saucier, FJ; Levasseur, M; Roy, S; Zakardjian, B				Fauchot, Juliette; Saucier, Franqois J.; Levasseur, Maurice; Roy, Suzanne; Zakardjian, Bruno			Wind-driven river plume dynamics and toxic <i>Alexandrium tamarense</i> blooms in the St. Lawrence estuary (Canada):: A modeling study	HARMFUL ALGAE			English	Article						Alexandrium tamarense; coupled physical-biological model; harmful algal blooms; river plume dynamics; St. Lawrence estuary	SEA-ICE; GROWTH; GULF; DINOPHYCEAE; VARIABILITY; MESOSCALE; BAY	In the lower St. Lawrence estuary (LSLE, eastern Canada), blooms of the toxic dinoflagellate Alexandrium tamarense are a recurrent phenomenon, resulting in paralytic shellfish poisoning outbreaks every summer. A first coupled physical-biological model of A. tamarense blooms was developed for this system in order to explore the interactions between cyst germination, cellular growth and water circulation and to identify the effect of physical processes on bloom development and transport across the estuary. The simulated summer (1998) was characterized by an A. tamarense red tide with concentrations reaching 2.3 x 10(6) cells L-1 along the south shore of the LSLE. The biological model was built with previously observed A. tamarense cyst distribution, cyst germination rate and timing, and A. tamarense growth limitation by temperature and salinity. The coupled model successfully reproduced the timing of the A. tamarense bloom in 1998, its coincidence with the combined plumes from the Manicouagan and Aux-Outardes (M-O) rivers on the north shore of the estuary, and the temporal variations in the north-south gradients in cell concentrations. The simulation results reveal that the interaction between cyst germination and the estuarine circulation generates a preferential inoculation of the surface waters of the M-O river plume with newly germinated cells which could partly explain the coincidence of the blooms with the freshwater plume. Furthermore, the results suggest that the spatio-temporal evolution of the bloom is dominated by alternating periods of retention and advection of the M-O plume: east or northeast winds favor the retention of the plume close to the north shore while west or north-west winds result in its advection toward the south shore. The response of the simulated freshwater plume to fluctuating wind forcing controls the delivery of the A. tamarense bloom from the northern part of the estuary to the south shore. In addition, our results suggest that a long residence time of the M-O plume and associated A. tamarense population in the LSLE during the summer 1998 contributed to the development of the red tide. We thus hypothesize that the wind-driven dynamics of the M-O plume could partly determine the success of A. tamarense blooms in the LSLE by influencing the residence time of the blooms and water column stability, which in turn affects A. tamarense vertical migrations and growth. (c) 2007 Elsevier B.V. All rights reserved.	[Levasseur, Maurice] Univ Laval, Dept Biol, Ste Foy, PQ G1K 7P4, Canada; [Fauchot, Juliette; Saucier, Franqois J.; Roy, Suzanne; Zakardjian, Bruno] Univ Quebec Rimouski, Inst Sci Mer Rimouski, Rimouski, PQ G5L 1C9, Canada; [Fauchot, Juliette] Fisheries & Oceans Canada, Maurice Lamontagne Inst, Mont Joli, PQ G5H 3Z4, Canada	Laval University; University of Quebec; Universite du Quebec a Rimouski; Fisheries & Oceans Canada	Levasseur, M (通讯作者)，Univ Laval, Dept Biol, Ste Foy, PQ G1K 7P4, Canada.	Maurice.Levasseur@bio.ulaval.ca	Fauchot, Juliette/HHS-0759-2022; Zakardjian, Bruno/AAL-9123-2021	Zakardjian, Bruno/0000-0002-6667-3086				Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; Blasco D, 2003, SCI MAR, V67, P261, DOI 10.3989/scimar.2003.67n3261; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; Cembella A.D., 1989, P81; Eilertsen H.C., 1998, HARMFUL ALGAE, P196; ELSABH MI, 1979, NAT CAN, V106, P55; Fauchot J, 2005, MAR ECOL PROG SER, V296, P241, DOI 10.3354/meps296241; Fauchot J, 2005, J PHYCOL, V41, P263, DOI 10.1111/j.1529-8817.2005.03092.x; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; Gagnon R, 2005, J PHYCOL, V41, P489, DOI 10.1111/j.1529-8817.2005.00077.x; Hunke EC, 1997, J PHYS OCEANOGR, V27, P1849, DOI 10.1175/1520-0485(1997)027<1849:AEVPMF>2.0.CO;2; Ingram R.G., 1990, Oceanography of a Large-scale Estuarine System: the St. Lawrence. 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J	Kennedy, EM; Alloway, BV; Mildenhall, DC; Cochran, U; Pillans, B				Kennedy, Elizabeth M.; Alloway, Brent V.; Mildenhall, Dallas C.; Cochran, Ursula; Pillans, Brad			An integrated terrestrial paleoenvironmental record from the Mid-Pleistocene transition, eastern North Island, New Zealand	QUATERNARY INTERNATIONAL			English	Article							TAUPO VOLCANIC ZONE; RHYOLITIC ERUPTIONS; DISTAL RECORD; PLEISTOCENE; AUCKLAND; PLIOCENE; TEPHRA; CHRONOLOGY; TELEOSTEI; HISTORY	A tephra-bearing lake sequence from near Ormond, New Zealand, provided the opportunity to conduct a multi-proxy paleoenvironmental analysis within the Mid-Pleistocene time period. A 10.5-m-thick section was measured and analysed for pollen, spores, diatoms, macrofossils, and tephra geochemistry. Palynological assemblages in the lower 4 m of the section indicate an ameliorating temperate climate and increased humidity. The upper 6.5 m is dominated by diatomite that did not yield sufficient palynomorphs for study. The source vegetation was distal lowland mixed broadleaf podocarp forest, swamp forest from ca. 2.5-4.0 m, and proximal scrubland with sporadic forest encroachment. Abundant freshwater algae in the samples suggest that any brackish influence in the lower part of the section was minor. Marine dinoflagellates found in the basal pollen samples could be mostly recycled. Diatomite samples were overwhelmingly dominated by a freshwater but mildly salt-tolerant diatom. We interpret the section as representing a shallow coastal lowland lake that intermittently had access to the sea. The chronology of the section is based on a single glass-ITPFT age of 0.62 +/- 0.09 Ma from a tephra interbed (T8) in the lower part of the section. In addition, the lowermost tephra in the sequence (T1) is geochemically correlated to AT-485, preserved in the marine record east of New Zealand, with an astronomically tuned age of 0.7163 Ma. This chronology places the basal portion of the Ormond section within the Brunhes normal Chron with sequence deposition occurring during either the OIS 18/17 or 16/15 transitions. However, paleomagnetic data indicate a clear reverse polarity from an equivalent stratigraphic position and at this stage it is difficult to reconcile this age discrepancy. (c) 2007 Elsevier Ltd and INQUA. All rights reserved.	[Kennedy, Elizabeth M.; Alloway, Brent V.; Mildenhall, Dallas C.; Cochran, Ursula] GNS Sci, Lower Hutt, New Zealand; [Pillans, Brad] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia	GNS Science - New Zealand; Australian National University	Kennedy, EM (通讯作者)，GNS Sci, POB 30-368, Lower Hutt, New Zealand.	E.Kennedy@gns.cri.nz; B.Alloway@gns.cri.nz; D.Mildenhall@gns.cri.nz; U.Cochran@gns.cri.nz; Brad.Pillans@anu.edu.au		Cochran, Ursula/0000-0001-8002-4958; Kennedy, Elizabeth/0000-0002-1989-779X; Pillans, Bradley/0000-0002-8373-635X				Alloway B, 2004, NEW ZEAL J GEOL GEOP, V47, P447, DOI 10.1080/00288306.2004.9515070; Alloway BV, 2005, QUATERNARY SCI REV, V24, P1601, DOI 10.1016/j.quascirev.2004.07.026; Balestrieri ML, 1998, SOLID EARTH, V10, P287; Batten DJ., 1996, Palynology: principles and applications, P191; Byrami ML, 2005, GEOL SOC SPEC PUBL, V247, P183, DOI 10.1144/GSL.SP.2005.247.01.10; BYRAMI ML, 2003, THESIS U AUCKLAND; Carter L, 2003, GEOLOGY, V31, P493, DOI 10.1130/0091-7613(2003)031<0493:DOOVZA>2.0.CO;2; CHARLESTON G, 1999, THESIS U AUCKLAND; COLEMAN JL, 1999, THESIS U AUCKLAND; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; HARPER MA, 1986, NEW ZEAL J MAR FRESH, V20, P107, DOI 10.1080/00288330.1986.9516135; Harwood David M., 1999, P436; HEAD M, 2005, GEOLOGICAL SOC LONDO, V247; Henderson J., 1920, NZ GEOLOGICAL SURVEY, V21; HILL H, 1888, TNZ I, V20, P293; Hill H, 1889, T NZ I, V21, P318; HOUGHTON BF, 1995, GEOLOGY, V23, P13, DOI 10.1130/0091-7613(1995)023<0013:CADOAL>2.3.CO;2; KENNEDY E, 2004, 200413 I GEOL NUCL S; KENNEDY EM, 2004, INT ORG PAL C 21 26, P63; KIRSCHVINK JL, 1980, GEOPHYS J ROY ASTR S, V62, P699, DOI 10.1111/j.1365-246X.1980.tb02601.x; LEMAITRE RW, 1984, AUST J EARTH SCI, V31, P243, DOI 10.1080/08120098408729295; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; McDowall RM, 2006, J ROY SOC NEW ZEAL, V36, P97, DOI 10.1080/03014223.2006.9517803; McDowall RM, 2006, J ROY SOC NEW ZEAL, V36, P27, DOI 10.1080/03014223.2006.9517797; McQUEEN D. 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FEB	2008	178						146	166		10.1016/j.quaint.2007.02.011	http://dx.doi.org/10.1016/j.quaint.2007.02.011			21	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	292ZP					2025-03-11	WOS:000255304900014
J	Howe, JA; Shimmield, TM; Harland, R				Howe, John A.; Shimmield, Tracy M.; Harland, Rex			Late Quaternary contourites and glaciomarine sedimentation in the Fram Strait	SEDIMENTOLOGY			English	Article						contourite; dinoflagellate; Fram Strait; ice-rafted debris; Last Glacial Maximum; Late Quaternary; turbidite; West Spitsbergen Current	SEA-ICE SHEET; NORTH-ATLANTIC; ARCTIC-OCEAN; CONTINENTAL-MARGIN; GLACIAL HISTORY; ROCKALL TROUGH; NORDIC SEAS; DEEP-SEA; SPITSBERGEN; WATER	Two sites in the eastern Fram Strait, the Vestnesa Ridge and the Yermak Plateau, have been surveyed and sampled providing a depositional record over the last glacial-interglacial cycle. The Fram Strait is the only deep-water connection from the Arctic Ocean to the North Atlantic and contains a marine sediment record of both high latitude thermohaline flow and ice sheet interaction. On the Vestnesa Ridge, the western Svalbard margin, a sediment drift was identified in 1226 m of water. Gravity and multicores from the crest of the drift recovered turbidites and contourites. C-14 dating indicates an age range of 8287 to 26 900 years BP (Early Holocene to Late Weichselian). The Yermak Plateau is characterized by slope sediments in 961 m of water. Gravity and multicores recovered contourites and hemipelagites. C-14 ages were between 8615 and 46 437 years BP (Early Holocene to mid-Weichselian). Downcore dinoflagellate cyst analyses from both sites provide a record of changing surface water conditions since the mid-Weichselian, suggesting variable sea ice extent, productivity and polynyas present even during the Last Glacial Maximum. Four layers of ice-rafted debris were also identified and correlated within the cores. These events occurred ca at 9, 24 to 25, 26 to 27 and 43 ka, asynchronous with Heinrich layers in the wider north-east Atlantic and here interpreted as reflecting instability in the Svalbard/Barents Ice sheet and the northward advection of warm Atlantic water during the Late Weichselian. The activity of the ancestral West Spitsbergen Current is interpreted using mean sortable silt records from the cores. On the Vestnesa Ridge drift the modern mass accumulation rate, calculated using excess Pb-210, is 0.076 g cm(-2) year(-1). On the Yermak Plateau slope the modern mass accumulation rate is 0.053 g cm(-2) year(-1).	[Howe, John A.; Shimmield, Tracy M.] Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA37 1QA, Argyll, Scotland; [Harland, Rex] DinoData Serv, Nottingham NG13 8AH, England	University of the Highlands & Islands	Howe, JA (通讯作者)，Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA37 1QA, Argyll, Scotland.	jaho@sams.ac.uk	Shimmield, Tracy/B-4483-2010		NERC [dml010002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		AAGAARD K, 1987, J GEOPHYS RES-OCEANS, V92, P3778, DOI 10.1029/JC092iC04p03778; Andersen ES, 1996, MAR GEOL, V133, P123, DOI 10.1016/0025-3227(96)00022-9; Bianchi GG, 1999, NATURE, V397, P515, DOI 10.1038/17362; Birgel D, 2004, QUATERNARY SCI REV, V23, P29, DOI 10.1016/j.quascirev.2003.10.001; BIRGEL D, 2003, ORGANIC CARBON CYCLE, P29; BOND G, 1992, NATURE, V360, P245, DOI 10.1038/360245a0; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Dowdeswell JA, 1999, NATURE, V400, P348, DOI 10.1038/22510; EIKEN O, 1993, SEDIMENT GEOL, V82, P15, DOI 10.1016/0037-0738(93)90110-Q; Ellison CRW, 2006, SCIENCE, V312, P1929, DOI 10.1126/science.1127213; Elverhoi A., 1983, POLAR RES-SWEDEN, V1, P1, DOI [DOI 10.1111/J.1751-8369.1983.TB00697.X, DOI 10.3402/POLAR.V1I2.6978]; Fahrbach E, 2001, POLAR RES, V20, P217, DOI 10.1111/j.1751-8369.2001.tb00059.x; Faugères JC, 2002, MAR GEOL, V182, P279, DOI 10.1016/S0025-3227(01)00242-0; FOHRMANN H, 1995, NO N ATLANTIC CHANGI, P135; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Grobe H., 1987, Polarforschung, V57, P123; Hald M, 2004, QUATERNARY SCI REV, V23, P2075, DOI 10.1016/j.quascirev.2004.08.006; HARLAND R, 1989, J GEOL SOC LONDON, V146, P945, DOI 10.1144/gsjgs.146.6.0945; Hass HC, 2002, POLAR RES, V21, P299, DOI 10.1111/j.1751-8369.2002.tb00084.x; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HEBBELN D, 1991, NATURE, V350, P409, DOI 10.1038/350409a0; Hebbeln D, 1998, QUATERNARY SCI REV, V17, P125, DOI 10.1016/S0277-3791(97)00067-X; HEBBELN D, 1994, NATURE, V370, P357, DOI 10.1038/370357a0; HEIN FJ, 1990, MAR GEOL, V93, P243, DOI 10.1016/0025-3227(90)90086-Y; HEINRICH H, 1988, QUATERNARY RES, V29, P142, DOI 10.1016/0033-5894(88)90057-9; Howe J.A., 2002, Geological Soc Lond Memoirs, Geological Society, V22, P65, DOI [DOI 10.1144/GSL.MEM.2002.022.01, DOI 10.1144/GSL.MEM.2002.022.01.06]; Howe JA, 1996, SEDIMENTOLOGY, V43, P219, DOI 10.1046/j.1365-3091.1996.d01-1.x; HOWE JA, 1994, PALEOCEANOGRAPHY, V9, P989, DOI 10.1029/94PA01440; JANSEN E, 1996, P ODP, P5; Knies J, 1999, GEO-MAR LETT, V18, P195, DOI 10.1007/s003670050068; Koç N, 2002, POLAR RES, V21, P307, DOI 10.1111/j.1751-8369.2002.tb00085.x; Kristoffersen Y, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2003PA000985; KRISTOFFERSEN Y, 1990, NATO ADV SCI I C-MAT, V308, P63; Lambeck K, 2000, EARTH PLANET SC LETT, V181, P513, DOI 10.1016/S0012-821X(00)00223-5; Landvik JY, 2005, BOREAS, V34, P7, DOI 10.1080/03009480510012809; Lowe DR, 2000, SEDIMENTOLOGY, V47, P31, DOI 10.1046/j.1365-3091.2000.00276.x; MANGERUD J, 1975, QUATERNARY RES, V5, P263, DOI 10.1016/0033-5894(75)90028-9; Mangerud J, 1998, QUATERNARY SCI REV, V17, P11, DOI 10.1016/S0277-3791(97)00069-3; Masson DG, 2002, MAR GEOL, V192, P215, DOI 10.1016/S0025-3227(02)00556-X; Matthiessen J, 2001, GLOBAL PLANET CHANGE, V31, P65, DOI 10.1016/S0921-8181(01)00113-8; MCCAVE IN, 1995, PALEOCEANOGRAPHY, V10, P593, DOI 10.1029/94PA03039; Michels K.H., 2002, DEEPWATER CONTOURITE, V22, P305, DOI [DOI 10.1144/GSL.MEM.2002.022.01.22, 10.1144/gsl.mem.2002.022.01, DOI 10.1144/GSL.MEM.2002.022.01]; Moran K, 2006, NATURE, V441, P601, DOI 10.1038/nature04800; Mori Y.H., 2002, P 4 INT C GAS HYDR Y, P222; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; Nost OA, 2003, J MAR RES, V61, P175, DOI 10.1357/002224003322005069; O Cofaigh C, 2004, MAR GEOL, V207, P39, DOI 10.1015/j.margeo.2004.02.009; Pudsey C. 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J	Ivanova, D; Kolodziej, B; Koleva-Rekalova, E; Roniewicz, E				Ivanova, Daria; Kolodziej, Boguslaw; Koleva-Rekalova, Elena; Roniewicz, Ewa			OXFORDIAN TO VALANGINIAN PALAEOENVIRONMENTAL EVOLUTION ON THE WESTERN MOESIAN CARBONATE PLATFORM: A CASE STUDY FROM SW BULGARIA	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Review						Oxfordian-Valanginian; biostratigraphy; carbonate sedimentology; reefs; Moesian Platform; Lyubash unit; Bulgaria	CORAL-MICROBIALITE REEFS; FLORIGEMMA-BANK; PATCH REEF; NW GERMANY; NORTHERN; EXAMPLE; EUROPE; BALKANIDES; DEPOSITS; MODELS	Three sections (Rebro, Lyalintsi and Velinovo) of the Upper Jurassic-Lower Cretaceous carbonate sequences from the Lyubash unit (Srednogorie, Balkanides, SW Bulgaria) have been studied for elucidation of biostratigraphy and palaeoenvironmental evolution. Palaeontological studies of foraminifera, supplemented by studies of calcareous dinoflagellate cysts and corals, enabled the determination of the Oxfordian-Valanginian age of the analysed sequences. They were deposited on the Drago man Block (western part of the Moesian Platform), and during Mid-Late Cretaceous included to the Srednogorie. A possible Middle to Late Callovian age of the lowermost part (overlying the Bajocian-Lower Bathonian Polaten Formation) of the studied sections assumed till now has not been confirmed by the present studies. Eleven facies have been distinguished and attributed to depositional environments. Marine sedimentation on a homoclinal ramp started in the Oxfordian and till the Early Kimmeridgian - in all three sections - was dominated by fine-grained peloidal-bioclastic wackestones to grainstones. Since the Late Kimmeridgian, when a rimmed platform established, facies pattern underwent differentiation into (i) the inner plat form (lagoon and tidal flat facies) - only in Velinovo, (ii) reef and peri-reef facies/bioclastic shoals - mainly in Lyalintsi, and (iii) plat form slope - mainly in Rebro. Sedimentation generally displays a shallowing-upward trend. Two stages in evolution of the rimmed platform are postulated. The mobile stage lasting till the Tithonian/Berriasian boundary was followed by a more stable stage in the Berriasian to Valanginian time. Reefs are developed mainly as coral-microbial biostromes, lower coral bioherms or coral thickets, in the environment of moderate energy and sedimentation. They contain highly diversified corals (72 species). Microbialites contributed to the reef framework, but they never dominated. Locally, microencrusters and cement crusts formed important part of reefal framework. During the mobile stage of the platform evolution a relative sea-level rise interrupted reef development, as evidenced by intercalations of limestones with Saccocoma. During the second stage high carbonate production and/or regressive eustatic events, not balanced by subsidence, decreased accommodation space, limiting reef growth and enhancing carbonate export to distal parts of the platform.	[Ivanova, Daria; Koleva-Rekalova, Elena] Bulgarian Acad Sci, Inst Geol, Acad G Bonchev Str,Bl 24, BU-1113 Sofia, Bulgaria; [Kolodziej, Boguslaw] Jagiellonian Univ, Inst Geol Sci, PL-30063 Krakow, Poland; [Roniewicz, Ewa] Polish Acad Sci, Inst Palaeobiol, PL-00818 Warsaw, Poland	Bulgarian Academy of Sciences; Jagiellonian University; Polish Academy of Sciences	Ivanova, D (通讯作者)，Bulgarian Acad Sci, Inst Geol, Acad G Bonchev Str,Bl 24, BU-1113 Sofia, Bulgaria.	dariaiv@geology.bas.bg; boguslaw.kolodziej@uj.edu.pl; e_koleva@geology.bas.bg; eron@twarda.pan.pl	Ivanova, Daria/B-8443-2013	Kolodziej, Boguslaw/0000-0002-9838-3411	Mesozoic Correlations of the Moesian Platform [72/95-96]; Peri-Tethyan Programme; Bulgarian Academy of Sciences; Polish Academy of Sciences; Bulgarian National Fund "Scientific Research" [NZ-1516/2005]	Mesozoic Correlations of the Moesian Platform; Peri-Tethyan Programme; Bulgarian Academy of Sciences; Polish Academy of Sciences; Bulgarian National Fund "Scientific Research"	This work was financially supported by the project 72/95-96 Mesozoic Correlations of the Moesian Platform funded by the Peri-Tethyan Programme, and was under taken in the framework of the project Integrated paleontological, stratigraphical and sedimentological study of the Upper Jurassic-Lower Cretaceous carbonate platforms from Western Bulgaria and Southern Poland funded by the Bulgarian Academy of Sciences and the Polish Academy of Sciences. The paper is also a contribution to the project NZ-1516/2005 of the Bulgarian National Fund "Scientific Research", as well to DS research studies of the Jagiellonian University. The authors are very grateful to Prof. P. Tchoumatchenco (Geological Institute, Bulgarian Academy of Sciences), who has initiated the collaboration between Bulgarian and Polish specialists in 2001, for the field trips and for his kind advice on the regional geology. Special thanks to Dr. V. Zlatarski (Bris-tol, RI, USA), who organized the first fieldtrip in 1981 and helped during coral sampling. We thank Prof. I. Bucur (Cluj-Napoca, Romania) for the determination of Dasycladales algae. Comments and suggestions of the referees Prof. I. Bucur and Dr. J. Szulc (Krakow), as well as editorial work of Dr. M. Gradzinski (Krakow) are greatly appreciated.	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Balc., V30, P59; ZLATARSKI G, 1885, PERIODICAL J BULGARI, V16, P1	106	43	44	0	12	POLISH GEOLOGICAL SOC	KRAKOW	UL. OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. Pol.		2008	78	2					65	90						26	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	399XT					2025-03-11	WOS:000262833300001
J	Guéguen, M; Lassus, P; Laabir, M; Bardouil, M; Baron, R; Sechet, V; Truquet, P; Amzil, Z; Barillé, L				Gueguen, Marielle; Lassus, Patrick; Laabir, Mohamed; Bardouil, MicheLe; Baron, Regis; Sechet, Veronique; Truquet, Philippe; Amzil, Zouher; Barille, Laurent			Gut passage times in two bivalve molluscs fed toxic microalgae:: <i>Alexandrium minutum</i>, <i>A-catenella</i> and <i>Pseudo-nitzschia calliantha</i>	AQUATIC LIVING RESOURCES			English	Article						Crassostrea gigas; Mytilus edulis; gut passage; uptake; toxic phytoplankton; risk assessment	OYSTER CRASSOSTREA-GIGAS; DINOFLAGELLATE CYSTS; VIABILITY; PHYTOPLANKTON; DINOPHYCEAE; INGESTION; SHELLFISH; SURVIVAL; PACIFIC; ORIGIN	The occurrence of new phytoplankton species in a coastal area may be explained by the import of shellfish containing whole live algal cells in their digestive tracts. Indeed, shellfish containing toxic algal cells can induce both primary contaminations in safe areas ( initially free from toxic microalgae), and secondary contaminations of other shellfish growing in the same area via the faeces of the imported animals. To mitigate this problem, shellfish need to be placed in a separate holding tank and their intestinal content purged. For a deeper understanding of the risks associated with transferring contaminated shellfish, oysters ( Crassostrea gigas) and mussels ( Mytilus edulis) were purposely fed either Alexandrium minutum or A. catenella ( Dinophyceae) or Pseudo- nitzschia calliantha ( Bacillariophyceae) toxic algae for 2 h. They were then transferred into individual tanks where they were continuously fed with a non- toxic alga, Tetraselmis suecica. Biodeposit production, faeces composition, and filtration rates were monitored for the shellfish over a 6- h period. The effect of temperature differences and different initial toxic algae concentrations were compared. This study revealed a relationship between temperature and cell lysis in the oyster digestive tract. It also indicated that toxic algae concentration did not seem to influence gut passage time in oysters, while a significant effect was observed in mussels, and confirmed the existence of a difference between oyster and mussel feeding patterns.	[Gueguen, Marielle; Lassus, Patrick; Bardouil, MicheLe; Sechet, Veronique; Truquet, Philippe; Amzil, Zouher] IFREMER, Lab Phycotoxines, F-44311 Nantes, France; [Laabir, Mohamed] Univ Montpellier 2, CNRS, UMR UM2 5119, Lab Ecosyst Lagunaires, F-34095 Montpellier, France; [Baron, Regis] IFREMER, Dept STAM, F-44311 Nantes, France; [Barille, Laurent] Lab Ecophysiol Marine Integree EA 2663, F-44322 Nantes 3, France	Ifremer; Centre National de la Recherche Scientifique (CNRS); Universite de Montpellier; Ifremer	Guéguen, M (通讯作者)，IFREMER, Lab Phycotoxines, BP 21105, F-44311 Nantes, France.	Marielle.Gueguen@ifremer.fr		sechet, veronique/0000-0002-7085-3215; Baron, Regis/0000-0002-0350-6838; Barille, Laurent/0000-0001-5138-2684				Amzil Z, 2001, TOXICON, V39, P1245, DOI 10.1016/S0041-0101(01)00096-4; [Anonymous], HARMFUL ALGAL BLOOMS; BARDOUIL M, 1993, J SHELLFISH RES, V12, P417; Barillé L, 2000, DIATOM RES, V15, P11; Bauder AG, 2000, J SHELLFISH RES, V19, P321; BOUCAUD C, 1983, ACTES C, V1, P75; Boyce SJ, 2000, J FISH BIOL, V57, P908, DOI 10.1006/jfbi.2000.1357; BRICELJ VM, 1993, DEV MAR BIO, V3, P371; Burkholder JM, 2007, HARMFUL ALGAE, V6, P486, DOI 10.1016/j.hal.2006.11.006; CARRIKER MR, 1992, J SHELLFISH RES, V2, P507; Cognie B, 2001, ESTUARIES, V24, P126, DOI 10.2307/1352819; DUKEMA R, 1995, PURIFICATION COQUILL, P355; Kikuchi T., 1996, HARMFUL TOXIC ALGAL, P413; Laabir M, 1999, J SHELLFISH RES, V18, P217; Laabir M, 2007, AQUAT LIVING RESOUR, V20, P51, DOI 10.1051/alr:2007015; Lassus P, 1988, AQUAT LIVING RESOUR, V1, P155, DOI 10.1051/alr:1988017; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; MANN DG, 2002, EC RES ENCLOSED SEAS, V12, P13; MARCAILLOU C, 2001, HARMFUL ALGAL BLOOMS, P356; Montresor M, 2003, J EXP MAR BIOL ECOL, V287, P209, DOI 10.1016/S0022-0981(02)00549-X; Nehring S, 1998, ARCH FISH MAR RES, V46, P181; PENRY DL, 1987, AM NAT, V129, P69, DOI 10.1086/284623; REID PC, 1987, J PLANKTON RES, V9, P249, DOI 10.1093/plankt/9.1.249; SCARRATT AM, 1993, J SHELLFISH RES, V12, P383; SCHET V, 2003, MOLLUSCAN SHELLFISH, P135; Soletchnik P, 1996, AQUAT LIVING RESOUR, V9, P65, DOI 10.1051/alr:1996009; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; van den Bergh JCJM, 2002, MAR POLICY, V26, P59, DOI 10.1016/S0308-597X(01)00032-X	28	10	12	0	32	EDP SCIENCES S A	LES ULIS CEDEX A	17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A, FRANCE	0990-7440			AQUAT LIVING RESOUR	Aquat. Living Resour.	JAN-MAR	2008	21	1					21	29		10.1051/alr:2008018	http://dx.doi.org/10.1051/alr:2008018			9	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	283YI		Bronze, Green Submitted			2025-03-11	WOS:000254672000003
J	Figueroa, RI; Bravo, I; Ramilo, I; Pazos, Y; Moroño, A				Figueroa, Rosa Isabel; Bravo, Isabel; Ramilo, Isabel; Pazos, Yolanda; Morono, Angeles			New life-cycle stages of <i>Gymnodinium catenatum</i> (Dinophyceae):: laboratory and field observations	AQUATIC MICROBIAL ECOLOGY			English	Article						dinophyceae; encystment; life-cycle stages; Gymnodinium catenatum; Galician rias	SEXUAL REPRODUCTION; GONYAULAX-TAMARENSIS; NOLLERI DINOPHYCEAE; POLEWARD CURRENT; RESTING CYSTS; DINOFLAGELLATE; CULTURE; SPAIN; COAST; VIGO	The chain-forming dinoflagellate Gymnodinium catenatum is responsible for outbreaks of paralytic shellfish poisoning (PSP); however, the relative importance of benthic-planktonic life-cycle transitions in the appearance of blooms of this species needs to be clarified. By coupling field and laboratory experiments, the present study is the first to analyze the dynamics of vegetative cells and sexual stages during a bloom of G. catenatum. In natural samples, the sexual stages of G. catenatum were associated with several different cellular behaviors and morphologies. This confirmed laboratory evidence for the reversibility of the species' sexual processes and for the ability of zygotes to either bypass or shorten the route to resting-cyst formation. Moreover, chains of up to 4 viable cysts with differing morphologies occurred and these have never been reported previously for this species. At least two of the cysts had reticulated surfaces, a feature related to sexual reproduction in previous studies; this observations suggests the involvement of sexual processes in mechanisms that cannot be explained by any known life cycle route depicted for this species. Morphological variability and abundance of the sexual stages during the bloom indicated the complexity of the G. catenatum sexual cycle and the important role of sexual reproduction in the ecological succession of this species. However, the lack of a dormancy period in the sexual resting stage (evidenced by the large number of germinated cysts in sediments sampled 3 mo after the bloom) indicated that the advection of offshore populations shoreward, rather than 'seed beds', is the main mechanism explaining G. catenatum bloom formation in the Galician rias.	[Figueroa, Rosa Isabel] CSIC, Inst Ciencias Mar, E-08003 Barcelona, Spain; [Bravo, Isabel; Ramilo, Isabel] Inst Oceanog Vigo, Vigo 36200, Spain; [Pazos, Yolanda; Morono, Angeles] Inst Tecnolox Control Med Marino Galicia, Vilaxoan 36611, Pontevedra, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，CSIC, Inst Ciencias Mar, E-08003 Barcelona, Spain.	figueroa@cmima.csic.es	Bravo, Isabel/D-3147-2012; Morono, Alejandro/H-2100-2016; Figueroa, Rosa/M-7598-2015	Bravo, Isabel/0000-0003-3764-745X; Morono, Angeles/0009-0003-2568-2570; Figueroa, Rosa/0000-0001-9944-7993				ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J PHYCOL, V21, P200; Beam C. 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Microb. Ecol.		2008	52	1					13	23		10.3354/ame01206	http://dx.doi.org/10.3354/ame01206			11	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	335ZS		Green Submitted, Bronze			2025-03-11	WOS:000258334700002
S	de Vernal, A; Hillaire-Marcel, C; Solignac, S; Radi, T; Rochon, A		DeWeaver, ET; Bitz, CM; Tremblay, LB		de Vernal, Anne; Hillaire-Marcel, Claude; Solignac, Sandrine; Radi, Taoufik; Rochon, Andre			Reconstructing Sea Ice Conditions in the Arctic and Sub-Arctic Prior to Human Observations	ARCTIC SEA ICE DECLINE: OBSERVATIONS, PROJECTIONS, MECHANISMS, AND IMPLICATIONS	Geophysical Monograph Book Series		English	Article; Book Chapter							WALLED DINOFLAGELLATE CYSTS; LAST GLACIAL MAXIMUM; NORTHWEST NORTH-ATLANTIC; SOUTHERN-OCEAN SEDIMENTS; MAJOR DIATOM TAXA; SURFACE CONDITIONS; HOLOCENE PALEOCEANOGRAPHY; HIGH-LATITUDES; BAFFIN-BAY; PLANKTIC FORAMINIFERS	Sea ice is a sensitive parameter characterized by a high variability in space and time that can be reconstructed from paleoclimatological archives. The most direct indication of past sea ice cover is found in marine sediments, which contain various tracers or proxies of environments characterized by sea ice. They include sedimentary tracers of particles entrained and dispersed by sea ice, biogenic remains associated with production under/within sea ice or with ice-free conditions, in addition to geochemical and isotopic tracers of brine formation linked to sea ice growth. Reconstructing the extent of past sea ice is, however, difficult because proxies are only indirectly related to sea ice and require the use of transfer functions having inherent uncertainties. In particular, we have to assume a correspondence between sea ice cover values from modern observations and the sea ice proxies from surface sediment samples, which is a source of bias since the time intervals represented by modern observations (here 1954-2000) and surface sediments (10(0)-10(3) years) are not equivalent. Moreover, suitable sedimentary sequences for reconstructing sea ice are rare, making the spatial resolution of reconstructions very patchy. Nevertheless, although fragmentary in time and space and despite uncertainties, available reconstructions reveal very large amplitude changes of sea ice in response to natural forcing during the recent geological past. For example, during the early Holocene, about 8000 years ago, data from dinocyst assemblages suggest reduced sea ice cover as compared to present in some subarctic basins (Labrador Sea, Baffin Bay, and Hudson Bay), whereas enhanced sea ice cover is reconstructed along the eastern Greenland margin and in the western Arctic, showing a pattern not unlike the dipole anomaly that was observed during the 20th century.	[de Vernal, Anne; Hillaire-Marcel, Claude; Solignac, Sandrine; Radi, Taoufik] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Rochon, Andre] Univ Quebec, Geotop, Rimouski, PQ G5L 3A1, Canada; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; University of Quebec; University of Quebec	de Vernal, A (通讯作者)，Univ Quebec, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	Hillaire-Marcel, Claude/H-1441-2012; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	Solignac, Sandrine/0000-0003-3373-6922; Hillaire-Marcel, Claude/0000-0002-3733-4632				AAGAARD K, 1981, DEEP-SEA RES, V28, P251, DOI 10.1016/0198-0149(81)90066-2; AKSU AE, 1988, CAN J EARTH SCI, V25, P701, DOI 10.1139/e88-066; Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; Andreev AA, 2000, J PALEOLIMNOL, V24, P81, DOI 10.1023/A:1008121917521; Andrews JT, 2007, J SEDIMENT RES, V77, P469, DOI 10.2110/jsr.2007.045; Armand LK, 2005, PALAEOGEOGR PALAEOCL, V223, P93, DOI 10.1016/j.palaeo.2005.02.015; Arzel O, 2006, OCEAN MODEL, V12, P401, DOI 10.1016/j.ocemod.2005.08.002; BARRY RG, 1993, REV GEOPHYS, V31, P397, DOI 10.1029/93RG01998; Bauch D, 1997, EARTH PLANET SC LETT, V146, P47, DOI 10.1016/S0012-821X(96)00211-7; Bauch HA, 2000, INT J EARTH SCI, V89, P569, DOI 10.1007/s005310000122; BEDARD P, 1981, NATURE, V293, P287, DOI 10.1038/293287a0; Belt ST, 2007, ORG GEOCHEM, V38, P16, DOI 10.1016/j.orggeochem.2006.09.013; BERGER AL, 1978, J ATMOS SCI, V35, P2362, DOI [10.1175/1520-0469(1978)035<2362:LTVODI>2.0.CO;2, 10.1016/0033-5894(78)90064-9]; Bigg GR, 2000, J GEOPHYS RES-OCEANS, V105, P8527, DOI 10.1029/2000JC900005; BILODEAU G, 1990, CAN J EARTH SCI, V27, P946, DOI 10.1139/e90-098; Bischof JF, 1997, SCIENCE, V277, P74, DOI 10.1126/science.277.5322.74; Bond G, 2001, SCIENCE, V294, P2130, DOI 10.1126/science.1065680; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; Carmack EC, 2000, NATO SCI S PRT 2 ENV, V70, P91; Crosta X, 1998, PALEOCEANOGRAPHY, V13, P284, DOI 10.1029/98PA00339; Crosta X, 2004, MAR MICROPALEONTOL, V50, P209, DOI 10.1016/S0377-8398(03)00072-0; Crosta X, 2005, PALAEOGEOGR PALAEOCL, V223, P66, DOI 10.1016/j.palaeo.2005.03.028; Darby D.A., 2001, Eos Trans. 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E., 1983, Atmosphere-Ocean, V21, P229, DOI 10.1080/07055900.1983.9649166; Walsh JE, 2001, ANN GLACIOL, V33, P444, DOI 10.3189/172756401781818671; Watanabe E, 2006, GEOPHYS RES LETT, V33, DOI 10.1029/2006GL028112; Wu BY, 2006, J CLIMATE, V19, P210, DOI 10.1175/JCLI3619.1; Yi DR, 1999, ATMOS OCEAN, V37, P389, DOI 10.1080/07055900.1999.9649633; Zonneveld KAF, 2008, MAR MICROPALEONTOL, V68, P179, DOI 10.1016/j.marmicro.2008.01.015	106	33	37	0	6	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0065-8448		978-0-87590-445-0	GEOPHYS MONOGR SER			2008	180						27	45		10.1029/180GM04	http://dx.doi.org/10.1029/180GM04	10.1029/GM180		19	Geochemistry & Geophysics; Environmental Sciences; Meteorology & Atmospheric Sciences	Book Citation Index– Science (BKCI-S)	Geochemistry & Geophysics; Environmental Sciences & Ecology; Meteorology & Atmospheric Sciences	BKA21					2025-03-11	WOS:000267579700003
J	Skupien, P; Mohamed, O				Skupien, Petr; Mohamed, Omar			Campanian to Maastrichtian palynofacies and dinoflagellate cysts of the Silesian Unit, Outer Western Carpathians, Czech Republic	BULLETIN OF GEOSCIENCES			English	Article						Silesian Unit; Cretaceous; Campanian; Maastrichtian; dinoflagellate cysts; palynofacies; Carpathians	NORTHERN APENNINES; ZONATION	Dinoflagellate cysts are reported from 20 Upper Cretaceous claystone samples from the Godula and Istebna formations of the Silesian unit. Age-assessment of the sediments based on 150 species suggests a Late Campanian to probably earliest Maastrichtian age for the middle and upper part of the Godula Formation and a Early Maastrichtian age for the basal part of the Istebna Formation. Key biotic events are especially the first occurrence datums of Areoligera senonensis, Cerodinium diebelii, Palaeocystodinium golzowense and Trithyrodinium evittii, and the last occurrence datums of Odontochitina, Palaeohystrichophora infusorioides, Raeteiaedinium truncigerum, Trihyrodinium suspectum and Xenascus ceratioides. Palynofacies analysis shows deposition in an offshore marine environment subjected to influxes of terrestrial material. Organic matter is dominated by phytoclasts and contains very little amorphous organic material. The succession is also characterized by a low percentage of dinoflagellate cysts and a very low percentage of spores and pollen grains. The presence of thermophilitic dinoflagellate cysts points to a warm- temperate to subtropical climate during Late Campanian to Early Maastrichtian.	[Skupien, Petr] Tech Univ Ostrava, Inst Geol Engn, CZ-70833 Ostrava, Czech Republic; [Mohamed, Omar] Elminia Univ, Fac Sci, Dept Geol, Elminia, Egypt	Technical University of Ostrava; Egyptian Knowledge Bank (EKB); Minia University	Skupien, P (通讯作者)，Tech Univ Ostrava, Inst Geol Engn, 17 Listopadu 15, CZ-70833 Ostrava, Czech Republic.	petr.skupien@vsb.cz; omaraosman@yahoo.com	Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X	Czech [205/05/0917]	Czech(Czech Republic Government)	This research was supported by the Czech Grant Agency No. 205/05/0917 "Upper Cretaceous oceanic red beds in the Czech part of the Outer Western Carpathians; biostratigraphy, sedimentology and geochemistry". We would like to thank Susanne Feist-Burkhardt, Mohamed Ismail Ibrahim, and an anonymous reviewer for reading the manuscript; their critical remarks significantly improved the manuscript.	[Anonymous], 1996, Palynology: principles and applications; ANTONESCU E, 2001, CAMPANIAN MAASTRICHT, P253; Batten D., 1996, PALYNOLOGY PRINCIPLE, P1011; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Costa L.I., 1992, P99; Elias M., 2000, GEOLOGICKE VYZKUMY M, V1999, P64; Fauconnier D., 2004, Les dinoflagelles fossile. Guide pratique de determination. Les genres a processus et a archeopyle apical; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; GEDL P, 2004, CAMPANIAN MAASTRICHT, P257; Hanzlikova E., 1972, Rozpravy ustred Ust geol, V39, P1; Hanzlikova E., 1972, Vestnik Ustred Ust Geol, V47, P69; HANZLIKOVA E, 1973, Sbornik Geologickych Ved Rada P Paleontologie, V15, P119; Hoek RP, 1996, MICROPALEONTOLOGY, V42, P125, DOI 10.2307/1485866; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; Lemanska Anna, 2005, Slovak Geological Magazine, V11, P45; LISTER J K, 1988, Palaeontographica Abteilung B Palaeophytologie, V210, P9; MATEJKA A, 1949, SBORNIK STATNIHO GEO, V16, P643; Mencik E., 1983, GEOLOGY MORAVSKOSLEZ; PICHA EJ, 2006, AAPG MEMOIR, V84, P49; Robaszynski F., 1985, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V9, P1; Roncaglia L, 1997, NEWSL STRATIGR, V35, P29; Roncaglia L, 2002, CRETACEOUS RES, V23, P65, DOI 10.1006/cres.2002.0298; Roth Z., 1980, ZAPADNI KARPATY TERC; Skupien P, 2003, T VSB TU OSTRAVA MIN, V8, P107; SKUPIEN P, SEPM SPECIA IN PRESS; Skupien P., 2003, T VSB TU OSTRAVA MIN, V8, P64; Smelror M., 1989, Palynology, V13, P121; Torricelli S, 2003, RIV ITAL PALEONTOL S, V109, P499, DOI 10.13130/2039-4942/5519; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; YPES O, 2001, PALYNOLOGY, V25, P217, DOI DOI 10.2113/0250217	31	33	36	0	4	CZECH GEOLOGICAL SURVEY	PRAGUE	KLAROV 131/3, PRAGUE, CZECH REPUBLIC	1214-1119			B GEOSCI	Bull. Geosci.		2008	83	2					207	224		10.3140/bull.geosci.2008.02.207	http://dx.doi.org/10.3140/bull.geosci.2008.02.207			18	Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	360XP		Bronze			2025-03-11	WOS:000260091800006
J	Louwye, S; Laga, P				Louwye, Stephen; Laga, Pieter			Dinoflagellate cyst stratigraphy and palaeoenvironment of the marginal marine Middle and Upper Miocene of the eastern Campine area, northern Belgium (southern North Sea Basin)	GEOLOGICAL JOURNAL			English	Article						dinoflagellate cysts; Miocene; southern North Sea Basin; Belgium; Bolderberg formation; Diest formation	DEPOSITIONAL HISTORY; DIEST FORMATION; BIOSTRATIGRAPHY; PLIOCENE; NETHERLANDS; PALYNOLOGY	A stratigraphical and palaeoenvironmental analysis with organic-walled palynomorphs of the Bolderberg and Diest formations provides new insights in the depositional history during Miocene times at the southern border of the North Sea Basin. The Neogene transgression invaded Belgium from a north-northwestern direction and fully marine sediments were deposited in the northern part of Belgium. The age and the palaeoenvironment of the deposits at the very border of the southern North Sea Basin remained till a few decades ago incomplete. The recovered dinoflagellate cysts, acritarchs and green algae from the Bolderberg Formation in the Wijshagen Borehole indicate a marginal marine depositional environment during late Burdigalian and Langhian times in the eastern Campine area, in contrast to the deeper marine conditions prevailing to the north-northwest. The relative dating of the Bolderberg Formation confirms that maximum flooding occurred during Langhian to early Serravallian times. Deposition apparently took place during the Middle Miocene Climatic Optimum, and ended when the climatic deterioration set in at around 14 Ma. A hiatus spanning ca. 2 Ma separates the Middle Miocene Bolderberg Formation from the Upper Miocene Diest Formation in the eastern Campine area at the border of the North Sea Basin. Copyright (C) 2007 John Wiley & Sons, Ltd.	[Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Laga, Pieter] Royal Inst Nat Sci, Geol Survey Belgium, Brussels, Belgium	Ghent University; Royal Belgian Institute of Natural Sciences	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S9, B-9000 Ghent, Belgium.	stephen.louwye@ugent.be	Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				Brenner W.W., 2001, BALTICA, V14, P40; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Drugg W.S., 1967, Tulane Studies in Geology, V5, P181; Elsik W.C., 1977, Palynology, V1, P95; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Head MJ, 1999, J PALEONTOL, V73, P1; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; Head MJ, 2005, QUATERN INT, V130, P3, DOI 10.1016/j.quaint.2004.04.027; Hooyberghs H.J.F., 1983, Aardkundige Mededelingen, V2, P1; HOOYBERGHS H. J. F., 1988, GEOLOGISCHES JB A, VA100, P190; KURITA H, 1994, REV PALAEOBOT PALYNO, V84, P129, DOI 10.1016/0034-6667(94)90047-7; Louwye S, 2000, GEOL MAG, V137, P381, DOI 10.1017/S0016756800004258; Louwye S, 2005, GEOL J, V40, P441, DOI 10.1002/gj.1021; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Louwye S, 2002, GEOL J, V37, P55, DOI 10.1002/gj.900; Louwye S, 1999, REV PALAEOBOT PALYNO, V107, P109, DOI 10.1016/S0034-6667(99)00012-3; Louwye S, 1999, GEOL MIJNBOUW, V78, P31, DOI 10.1023/A:1003793300214; MARTINI E, 1973, NEUES JB GEOLOGIE PA, V9, P555; Miller KG, 1998, REV GEOPHYS, V36, P569, DOI 10.1029/98RG01624; MILLER KG, 1991, J GEOPHYS RES-SOLID, V96, P6829, DOI 10.1029/90JB02015; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Schioler P, 1997, MAR MICROPALEONTOL, V31, P65, DOI 10.1016/S0377-8398(96)00058-8; Shevenell AE, 2004, SCIENCE, V305, P1766, DOI 10.1126/science.1100061; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	27	40	41	0	8	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0072-1050			GEOL J	Geol. J.	JAN	2008	43	1					75	94		10.1002/gj.1103	http://dx.doi.org/10.1002/gj.1103			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	254QQ					2025-03-11	WOS:000252603500005
J	Dybkjær, K; Piasecki, S				Dybkjaer, Karen; Piasecki, Stefan			A new Neogene biostratigraphy for Denmark	GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN			English	Article							DINOFLAGELLATE CYST STRATIGRAPHY; NORTH-SEA BASIN; UPPERMOST OLIGOCENE; LOWER MIOCENE; JYLLAND; SECTION	In Denmark most of the water used in private households, in the industry and for irrigation in agriculture comes from subsurface aquifers. Some of the most important aquifers in Jylland, western Denmark, are sand layers deposited from 23 to 15 Ma ago, in the Early Neogene (Early to Middle Miocene). About 23 Ma ago, in the Early Miocene, the coastline ran NW-SE across present-day Jylland (Rasmussen 2004). Global climatic variations led to major sea-level changes (Zachos et al. 2001), which in combination with increased sediment transport from the north (the present Norway) resulted in deposition of several huge, fluvio-deltaic sand systems intercalated with marine clay (e. g. Rasmussen 1961; Rasmussen 2004; Rasmussen & Dybkjaer 2005). The Geological Survey of Denmark and Greenland (GEUS) and the regional Environment Centres (the former counties (amter)) in Jylland are working in close cooperation to study the Early Neogene succession; the main purposes are: (1) to find new aquifers, (2) to map the extent of known aquifers and clarify their mutual relationships, in order to evaluate the size of the water resources and optimise production, and (3) to protect the aquifers from pollution due to leaching from the surface. In order to map the complex sedimentary succession, it has been necessary to combine several geological disciplines, including seismic interpretation, sedimentology, correlation of geophysical logs, and biostratigraphy (e. g. Dybkjaer 2004; Rasmussen 2004; Rasmussen et al. 2004; Piasecki 2005; Rasmussen & Dybkjaer 2005; Dybkjaer & Rasmussen 2007). This article shows some results of a detailed dinoflagellate cyst stratigraphy, which is based on an extensive database (Fig. 1). We present here for the first time a dinoflagellate cyst zonation for the complete Neogene succession in the Danish area.	[Dybkjaer, Karen; Piasecki, Stefan] Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Dybkjær, K (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018		Danish Environment Centres	Danish Environment Centres	The Danish Environment Centres and the former counties are thanked for their cooperation and financial support.	[Anonymous], 2004, GEOL SURV DEN GREENL; DE VERTEUIL L., 1996, MICROPALEONTOLOGY S, V42; Dybkjaer K, 2000, B GEOL SOC DENMARK, V47, P87; Dybkjaer K, 2007, J MICROPALAEONTOL, V26, P1, DOI 10.1144/jm.26.1.1; Dybkjær K, 2004, REV PALAEOBOT PALYNO, V131, P201, DOI 10.1016/j.revpalbo.2004.03.006; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; GRANDSTEIN FM, 2004, GEOLOGICAL TIME SCAL; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Kothe A., 2003, REV PALEOBIOL, V22, P895; Larsen G, 1959, DANMARKS GEOLOGISKE, V82; Louwye S, 1999, GEOL MIJNBOUW, V78, P31, DOI 10.1023/A:1003793300214; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Piasecki S., 2005, Palaeontos, V7, P29; Rasmussen ES, 2006, B GEOL SOC DENMARK, V53, P23; Rasmussen ES, 2004, B GEOL SOC DENMARK, V51, P89; Rasmussen ES, 2005, SEDIMENTOLOGY, V52, P25, DOI 10.1111/j.1365-3091.2004.00681.x; RASMUSSEN ES, 2005, 200533 DANM GRONL GE; RASMUSSEN LB, 1961, DANMARKS GEOLOGISKE, V4; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	20	19	23	0	5	GEOLOGICAL SURVEY DENMARK & GREENLAND	COPENHAGEN K	OSTER VOLDGADE 10, COPENHAGEN K, DK-1350, DENMARK	1604-8156			GEOL SURV DEN GREENL	Geol. Surv. Den. Greenl. Bull.		2008		15					29	32						4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	354UM					2025-03-11	WOS:000259664500007
C	Tiffany, MA; Wolny, J; Garrett, I; Steidinger, K; Hurlbert, SH		Hoover, RB; Levin, GV; Rozanov, AY; Davies, PCW		Tiffany, Mary Ann; Wolny, Jennifer; Garrett, Iatthew; Steidinger, Karen; Hurlbert, Stuart H.			Dramatic blooms of <i>Prymnevium</i> sp and <i>Alexandrium margalefii</i> in the Salton Sea, California	INSTRUMENTS, METHODS, AND MISSIONS FOR ASTROBIOLOGY XI	Proceedings of SPIE		English	Proceedings Paper	Conference on Instruments, Methods, and Missions for Astrobiology XI	AUG 12-14, 2008	San Diego, CA	SPIE		Bioluminescence; dinoflagellates; foam; phytoplankton; salt take; cysts; allelopathy	DINOFLAGELLATE GENUS ALEXANDRIUM; PRYMNESIUM-PARVUM; COASTAL WATERS; MICROECOSYSTEMS; DINOPHYCEAE; SALINITY; TOXICITY; CYSTS	In early 2006, unusual algal blooms of two species occurred in the Salton Sea, a large salt lake in southern California. In mid-January local residents reported bioluminescence in the Sea. Starting in February, large rafts of long-lasting foam, also bioluminescent, were observed as well. Microscopy investigations on water and sediment samples collected in March showed the marine dinoflagellate, Alexandrium margalefii, and the prymnesiophyte, Prymnesium sp., both previously unreported in the Salton Sea, to be abundant. Bioluminescence and foam production continued through March. Other dinoflagellate species, recorded during earlier studies, were rare or not detected during these blooms. Despite the fact that many Alexandrium species are known paralytic shellfish poison (PSP) producers, preliminary saxitoxin tests on this population of A. margalefii were negative. Previous reports on A. margalefii do not mention bioluminescence. It appears that the foam was caused by the Prymnesium sp. bloom, probably via protein-rich exudates and lysis of other algal cells, and its glow was due to entrained A. margalefii. This is the first report of A. margalefii in U.S. waters and the first report of it in a lake.	[Tiffany, Mary Ann; Hurlbert, Stuart H.] San Diego State Univ, Dept Biol, San Diego, CA 92182 USA; [Wolny, Jennifer; Garrett, Iatthew; Steidinger, Karen] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, St Petersburg, FL 33701 USA; [Wolny, Jennifer; Garrett, Iatthew; Steidinger, Karen] Florida Inst Oceanog, St Petersburg, FL 33701 USA	California State University System; San Diego State University; Florida Fish & Wildlife Conservation Commission	Tiffany, MA (通讯作者)，San Diego State Univ, Dept Biol, San Diego, CA 92182 USA.			Wolny, Jennifer L./0000-0002-3556-5015	NASA Earth System Science Fellowship Program [NNG05GB55H]	NASA Earth System Science Fellowship Program	We thank Brian Brinegar for logistical support and Jay Abbott for assistance with the STX assays, Kevin Marty of the Imperial Valley Press and Norm Niver for providing photographs of the Salton Sea, and four anonymous reviewers for helpful suggestions on the manuscript. This work was supported in part by the NASA Earth System Science Fellowship Program under grant no. NNG05GB55H to M. A. Tiffany.	ABRAHAMS MV, 1993, ECOLOGY, V74, P258, DOI 10.2307/1939521; Andersen R. A., 2005, Algal culturing techniques, P83; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON TW, 2007, LAKE RESERV IN PRESS; [Anonymous], PHYSL ECOLOGY HARMFU; [Anonymous], CALIFORNIA DEP FISH; Badylak S, 2004, PHYCOLOGIA, V43, P653, DOI 10.2216/i0031-8884-43-6-653.1; BALECH E, 1994, T AM MICROSC SOC, V113, P216, DOI 10.2307/3226651; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; Band-Schmidt CJ, 2003, PHYCOLOGIA, V42, P261, DOI 10.2216/i0031-8884-42-3-261.1; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Carmichael Wayne W, 2006, Saline Syst, V2, P5, DOI 10.1186/1746-1448-2-5; CASKEY LL, 2007, LAKE RESERV IN PRESS; ch2m, 2018, SALTON SEA HYDROLOGY; Costa-Pierce BA, 1997, TILAPIA AQUACULTURE IN THE AMERICAS, VOLUME ONE, P1; Fistarol GO, 2003, MAR ECOL PROG SER, V255, P115, DOI 10.3354/meps255115; FISTAROL GO, 2004, AQUAT MICROB ECOL, V35, P5; González MR, 1998, HYDROBIOLOGIA, V381, P105, DOI 10.1023/A:1003227624686; GONZALEZ MR, 1997, THESIS CTR INVESTIGA; Granéli E, 2006, ECOL STU AN, V189, P189, DOI 10.1007/978-3-540-32210-8_15; Granéli E, 2003, HARMFUL ALGAE, V2, P135, DOI 10.1016/S1568-9883(03)00006-4; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; Hart CM, 1998, HYDROBIOLOGIA, V381, P129, DOI 10.1023/A:1003490215005; HURLBERT AH, 2007, LAKE RESERV IN PRESS; Jehl JR, 2002, HYDROBIOLOGIA, V473, P245, DOI 10.1023/A:1016514725025; Kempton Jason W., 2002, Harmful Algae, V1, P383, DOI 10.1016/S1568-9883(02)00051-3; Lange CB, 2002, HYDROBIOLOGIA, V473, P179, DOI 10.1023/A:1016550205461; Liu LY, 2004, P NATL ACAD SCI USA, V101, P16555, DOI 10.1073/pnas.0407597101; MacKenzie L, 2004, HARMFUL ALGAE, V3, P71, DOI 10.1016/j.hal.2003.09.001; MAURER F, 1906, HDB VERGLEICHENDEN 1, V3, P1; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; Oh C.O., 2005, T32001168 PWD RP TEX; Reifel KM, 2001, HYDROBIOLOGIA, V466, P177, DOI 10.1023/A:1014551804059; Reifel KM, 2007, HYDROBIOLOGIA, V576, P167, DOI 10.1007/s10750-006-0300-3; RHODES K, 1992, SOUTHWEST NAT, V37, P178, DOI 10.2307/3671666; Richardson K, 1997, ADV MAR BIOL, V31, P301, DOI 10.1016/S0065-2881(08)60225-4; RIEDEL R, 2001, REV FISH SCI, V10, P77; Roelke DL, 2007, AQUAT MICROB ECOL, V46, P125, DOI 10.3354/ame046125; SAGER DR, 2007, T32001404 PWD RP; SCHLICHTING HAROLD E., 1960, TRANS AMER MICROSC SOC, V79, P160, DOI 10.2307/3224082; Selina M.S., 2005, RUSSIAN J MARINE BIO, V31, P187, DOI DOI 10.1007/S11179-005-0066-X; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Sullivan JM, 2003, J PHYCOL, V39, P83, DOI 10.1046/j.1529-8817.2003.02094.x; Sweeney B. M., 1987, BIOL DINOFLAGELLATES, P269; Thornton DCO, 1999, ETHOL ECOL EVOL, V11, P179, DOI 10.1080/08927014.1999.9522835; Throndsen Jahn, 1997, P591, DOI 10.1016/B978-012693018-4/50007-0; TIFFANY MA, LAKE RESERV IN PRESS; Tillmann U, 2007, J PLANKTON RES, V29, P527, DOI 10.1093/plankt/fbm034; TOMAS C, 2004, HARMFUL ALGAE 2002, P369; WALKER BW, 1961, CALIF DEP FISH GAME, V113, P1; Watts JM, 2001, HYDROBIOLOGIA, V466, P159, DOI 10.1023/A:1014599719989; 2006, EUROPEAN J PHYCOLOGY, V41, P293	52	0	0	0	8	SPIE-INT SOC OPTICAL ENGINEERING	BELLINGHAM	1000 20TH ST, PO BOX 10, BELLINGHAM, WA 98227-0010 USA	0277-786X	1996-756X	978-0-8194-7317-2	PROC SPIE			2008	7097								70970T	10.1117/12.800919	http://dx.doi.org/10.1117/12.800919			14	Astronomy & Astrophysics; Instruments & Instrumentation; Optics	Conference Proceedings Citation Index - Science (CPCI-S)	Astronomy & Astrophysics; Instruments & Instrumentation; Optics	BIS82					2025-03-11	WOS:000262473900023
J	Aligizaki, K; Nikolaidis, G				Aligizaki, Katerina; Nikolaidis, Georgios			Morphological identification of two tropical dinoflagellates of the genera <i>Gambierdiscus</i> and <i>Sinophysis</i> in the Mediterranean Sea	JOURNAL OF BIOLOGICAL RESEARCH-THESSALONIKI			English	Article						Gambierdiscus; ciguatera; Mediterranean; benthic dinoflagellates; Sinophysis canaliculata	SP-NOV; BENTHIC DINOFLAGELLATE; COOLIA DINOPHYCEAE; CIGUATERA; OSTREOPSIS; TOXICITY; DINOPHYSIALES; MACROALGAE; ISLANDS; SAUPE	Gambierdiscus cells were found on macroalgae samples ( Padina pavonica, Corallina elongata, Jania sp. and Cystoseira sp.) collected from 11 sites in Crete Island in summer and autumn months of the years 2003, 2004, 2005 and 2007. The presence of the genus Gambierdiscus in Crete since 2003 constituted the earliest record of this genus in the Mediterranean Sea. The epiphytic dinoflagellate community comprised the genera Gambierdiscus, Ostreopsis, Coolia, Prorocentrum, Amphidinium and the non- photosynthetic benthic species Sinophysis canaliculata. The last species was also recorded for the first time in the Mediterranean Sea in the present study. Furthermore, diatoms of the genera Coscinodiscus, Licmophora and Striatella were observed as well. Sinophysis canaliculata cells fitted in the earlier descriptions of the species bearing the characteristic hole on the left lateral hypothecal plate. Gambierdiscus cells from both field samples and cultures were round to ellipsoid in shape ( dorsoventral diameter / transdiameter ratio, DV/ W: 1.02 +/- 0.06) and anterior- posteriorly compressed ( AP < 45 mu m), while field specimens ( DV: 57.12- 76.16 mu m, W: 52.36- 78.54 Im) were found to be smaller than those grown in culture conditions ( DV: 69.02- 84.49 mu m, W: 69.02- 85.68 mu m). Specific discriminative characteristics of Gambierdiscus specimens examined in this study, such as the thecal surface pattern and the posterior plate ( 1p), fitted well with those of the " G. toxicus type"; nevertheless, our specimens were not assigned to a species due to inconsistencies revealed lately regarding the identity of the type species.	[Aligizaki, Katerina; Nikolaidis, Georgios] Aristotle Univ Thessaloniki, Fac Sci, Sch Biol, Dept Bot, Thessaloniki 54124, Greece	Aristotle University of Thessaloniki	Aligizaki, K (通讯作者)，Aristotle Univ Thessaloniki, Fac Sci, Sch Biol, Dept Bot, Thessaloniki 54124, Greece.	aligiza@bio.auth.gr						ADACHI R, 1979, B JPN SOC SCI FISH, V45, P67; Aligizaki K., 2008, Harmful Algae News, V36, P6; ALIGIZAKI K, 2006, 12 INT C HARMF ALG C, P123; Aligizaki K, 2006, HARMFUL ALGAE, V5, P717, DOI 10.1016/j.hal.2006.02.005; [Anonymous], 12 INT C HARMF ALG C; [Anonymous], 2006, ACTA BOT MEX, DOI DOI 10.21829/ABM74.2006.1008; [Anonymous], 2005, Algal Culturing Techniques; BESADA EG, 1982, B MAR SCI, V32, P723; Bianchi CN, 2007, HYDROBIOLOGIA, V580, P7, DOI 10.1007/s10750-006-0469-5; Bustillos-Guzmn J., 1998, Harmful Algae, P372; Carlson RD., 1984, Seafood Toxins, P271; CHEVALDONNE P, 1990, J FISH BIOL, V37, P503, DOI 10.1111/j.1095-8649.1990.tb05883.x; Chinain M, 1999, MAR BIOL, V135, P259, DOI 10.1007/s002270050623; Chinain M, 1999, J PHYCOL, V35, P1282, DOI 10.1046/j.1529-8817.1999.3561282.x; de Haro L, 2006, CLIN TOXICOL, V44, P185, DOI 10.1080/15563650500514590; DURANDCLEMENT M, 1986, TOXICON, V24, P1153, DOI 10.1016/0041-0101(86)90141-8; Faust MA, 1995, J PHYCOL, V31, P996, DOI 10.1111/j.0022-3646.1995.00996.x; Fraga S, 2007, 4 EUR PHYC C OV, P41; Fraga S., 2004, 11 INT C HARMF ALG C, P115; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1981, B JPN SOC SCI FISH, V47, P967; GLAZIOU P, 1994, TOXICON, V32, P863, DOI 10.1016/0041-0101(94)90365-4; Hallegraeff G.M., 2003, Manual on Harmful Marine Algae; Herzberg A., 1973, Aquaculture, V2, P89, DOI 10.1016/0044-8486(73)90127-0; Holmes MJ, 1998, J PHYCOL, V34, P661, DOI 10.1046/j.1529-8817.1998.340661.x; Hoppenrath M, 2000, EUR J PHYCOL, V35, P153, DOI 10.1080/09670260010001735741; Lehane L, 2000, INT J FOOD MICROBIOL, V61, P91, DOI 10.1016/S0168-1605(00)00382-2; Lewis RJ, 2001, TOXICON, V39, P97, DOI 10.1016/S0041-0101(00)00161-6; Mohammad-Noor N, 2004, NORD J BOT, V24, P629, DOI 10.1111/j.1756-1051.2004.tb01938.x; Monti M, 2007, MAR POLLUT BULL, V54, P598, DOI 10.1016/j.marpolbul.2007.01.013; Occhipinti-Ambrogi A, 2007, MAR POLLUT BULL, V55, P342, DOI 10.1016/j.marpolbul.2006.11.014; Parsons ML, 2007, HARMFUL ALGAE, V6, P658, DOI 10.1016/j.hal.2007.01.001; Penna A, 2005, J PHYCOL, V41, P212, DOI 10.1111/j.1529-8817.2005.04011.x; Pérez-Arellano JL, 2005, EMERG INFECT DIS, V11, P1981, DOI 10.3201/eid1112.050393; Quod JP, 1999, PHYCOLOGIA, V38, P87, DOI 10.2216/i0031-8884-38-2-87.1; Richlen M L., 2008, Harmful Algae; Salat J., 2002, Tracking longterm hydrological change in the Mediterranean Sea, VVolume 16; Selina M, 2004, PHYCOL RES, V52, P149, DOI 10.1111/j.1440-183.2004.00336.x; SPANIER E, 1989, J FISH BIOL, V34, P635, DOI 10.1111/j.1095-8649.1989.tb03342.x; TESTER P, 2006, 12 INT C HARMF ALG C, P290; TOSTESON TR, 1989, APPL ENVIRON MICROB, V55, P137, DOI 10.1128/AEM.55.1.137-141.1989; Turki S, 2005, CAH BIOL MAR, V46, P29; Turquet J., 2001, HARMFUL ALGAL BLOOMS, P50; Utermohl H., 1953, SIL Commun. 19531996, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Vila M, 2001, AQUAT MICROB ECOL, V26, P51, DOI 10.3354/ame026051; YASUMOTO T, 1977, B JPN SOC SCI FISH, V43, P1021, DOI 10.2331/suisan.43.1021	46	80	86	1	24	ARISTOTLE UNIV THESSALONIKI	THESSALONIKI	ADMIN BLDG, 6TH FLOOR, THESSALONIKI, GR-540 06, GREECE	1790-045X			J BIOL RES-THESSALON	J. Biol. Res.		2008	9						75	82						8	Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics	329US					2025-03-11	WOS:000257896700009
S	Barreda, V; Guler, V; Palazzesi, L		Rabassa, J		Barreda, Viviana; Guler, Veronica; Palazzesi, Luis			Late Miocene Continental and Marine Palynological Assemblages from Patagonia	LATE CENOZOIC OF PATAGONIA AND TIERRA DEL FUEGO	Developments in Quaternary Science		English	Article; Book Chapter							SANTA-CRUZ PROVINCE; DINOFLAGELLATE CYSTS; COLORADO BASIN; CHUBUT PROVINCE; BIOSTRATIGRAPHY; BOREHOLE; AREA; AGE		[Barreda, Viviana; Palazzesi, Luis] Consejo Nacl Invest Cient & Tecn, Div Paleobot, Museo Argentino Ciencias Nat B Rivadavia, RA-1033 Buenos Aires, DF, Argentina; [Guler, Veronica] Univ Nacl Sur, CONICET, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Barreda, V (通讯作者)，Consejo Nacl Invest Cient & Tecn, Div Paleobot, Museo Argentino Ciencias Nat B Rivadavia, Av A Gallardo 470 C1405DJR, RA-1033 Buenos Aires, DF, Argentina.			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J	Persson, A; Smith, BC; Dixon, MS; Wikfors, GH				Persson, Agneta; Smith, Barry C.; Dixon, Mark S.; Wikfors, Gary H.			The Eastern mudsnail, <i>Ilyanassa obsoleta</i>, actively forages for, consumes, and digests cysts of the dinoflagellate, <i>Scrippsiella lachrymosa</i>	MALACOLOGIA			English	Article						deposit feeding; dinoflagellate resting stages; cyst ecology	DEPOSIT-FEEDERS; RESTING CYSTS	The Eastern mudsnail, Ilyanassa obsoleta, was attracted to, consumed, and digested resting cysts of the dinoflagellate Scrippsiella lachrymosa when cysts were presented in grazing experiments. Twenty snails were observed individually for one hour in petri dishes divided into four parts wherein cysts were present in one quadrant, sediment particles of the same size range were in another quadrant, and two quadrants were free of particles. Actively foraging snails were nearly twice as likely to be found in quadrants containing S. lachrymosa cysts as in the other quadrants until cysts were consumed. Microscope observations of fecal pellets from snails feeding on cysts revealed digestive destruction of the cysts. These findings indicate that deposit-feeding grazers can actively seek dinoflagellate cysts as a food item, thereby influencing distribution of cysts and subsequent germination of dinoflagellate vegetative cells.	[Persson, Agneta; Smith, Barry C.; Dixon, Mark S.; Wikfors, Gary H.] NE Fisheries Sci Ctr, Milford Lab, Natl Marine Fisheries Serv, Natl Ocean & Atmospher Adm, Milford, CT 06460 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Smith, BC (通讯作者)，NE Fisheries Sci Ctr, Milford Lab, Natl Marine Fisheries Serv, Natl Ocean & Atmospher Adm, Milford, CT 06460 USA.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514				[Anonymous], 1989, Ecology of Soil Seed Banks; BIANCHI TS, 1981, J MAR RES, V39, P547; Dale B., 1983, P69; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kremp A, 2003, MAR ECOL PROG SER, V263, P65, DOI 10.3354/meps263065; LEWIS CM, 1979, BIOL DINOFLAGELLATES, P235; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; REID PC, 1987, J PLANKTON RES, V9, P249, DOI 10.1093/plankt/9.1.249; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53; Underwood AJ., 1996, Experiments in Ecology: Their Logical Design and Interpretation Using Analysis of Variance	13	7	7	0	2	INST MALACOL	ANN ARBOR	2415 SOUTH CIRCLE DR, ANN ARBOR, MI 48103 USA	0076-2997			MALACOLOGIA	Malacologia		2008	50	1-2					341	345		10.4002/0076-2997-50.1-2.341	http://dx.doi.org/10.4002/0076-2997-50.1-2.341			5	Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Zoology	314KD					2025-03-11	WOS:000256807400012
J	Hégaret, H; Shumway, SE; Wikfors, GH; Pate, S; Burkholder, JM				Hegaret, Helene; Shumway, Sandra E.; Wikfors, Gary H.; Pate, Susan; Burkholder, Joann M.			Potential transport of harmful algae via relocation of bivalve molluscs	MARINE ECOLOGY PROGRESS SERIES			English	Article						bivalve mollusc; harmful algal bloom; toxic algae; transport; clam s; scallop; oyster	OYSTER CRASSOSTREA-GIGAS; ALEXANDRIUM-CATENELLA; GUT PASSAGE; DINOFLAGELLATE CYSTS; MYTILUS-EDULIS; DINOPHYCEAE; BLOOMS; INGESTION; VIABILITY; VIRGINICA	Aquaculture and restoration activities with bivalve molluscs often involve moving individuals from one body of water to another. Our study tests the hypothesis that harmful algae ingested by source populations of shellfish can be introduced into new environments by means of these shellfish relocations. Cultures of several harmful algal strains, including Prorocentrum minimum, Alexandrium fundyense, Heterosigma akashiwo, Aureococcus anophagefferens, Karenia mikimotoi and Alexandrium monflatum, were fed to various species of bivalve molluscs, Crassostrea virginica, Argopecten irradians irradians, Mercenaria mercenaria, Mytilus edulis, Mya arenaria, Venerupis philippinarum and Perna viridis, to assess the ability of the algal cells to pass intact though the digestive tracts of the shellfish and subsequently multiply in number. Ten individuals of each shellfish species were exposed for 2 d to it simulated harmful algal bloom at a natural bloom concentration. The shellfish were removed after exposure, and maintained for 2 further days in ultra-filtered seawater. Biodeposits (feces) were collected after 24 and 48 additional hours, and observed under light microscopy for the presence or absence of intact, potentially viable algal cells or temporary cysts. Subsamples of biodeposits were transferred into both algal culture medium and filtered seawater and monitored for algal growth. Intact cells of most harmful algal species tested were seen in biodeposits. Generally, harmful algae from the biodeposits collected in the first 24 h after transfer re-established growing populations, but algae could less often be recovered from the biodeposits collected after 48 h. These data provide evidence that transplanted bivalve molluscs may be vectors for the transport of harmful algae and that a short holding period in water without algae may mitigate this risk. Further, preliminary results indicate that emersion may also serve to mitigate the risk of transport.	[Hegaret, Helene; Shumway, Sandra E.] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; [Wikfors, Gary H.] NOAA, NE Fisheries Sci Ctr, Natl Marine Fisheries Serv, Milford, CT 06460 USA; [Pate, Susan; Burkholder, Joann M.] N Carolina State Univ, CAAE, Raleigh, NC 27695 USA	University of Connecticut; National Oceanic Atmospheric Admin (NOAA) - USA; North Carolina State University	Shumway, SE (通讯作者)，Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA.	sandra.shumway@uconn.edu	Hegaret, Helene/B-7206-2008	Hegaret, Helene/0000-0003-4639-9013				BARDOUIL M, 1993, J SHELLFISH RES, V12, P417; Bauder AG, 2000, J SHELLFISH RES, V19, P321; BRICELJ VM, 1993, DEV MAR BIO, V3, P371; Burkholder JM, 1998, ECOL APPL, V8, pS37; Carriker Melbourne R., 1992, Journal of Shellfish Research, V11, P507; FOGG GE, 1983, BOT MAR, V26, P3, DOI 10.1515/botm.1983.26.1.3; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Harper FM, 2002, J SHELLFISH RES, V21, P471; Hégaret H, 2005, HARMFUL ALGAE, V4, P201, DOI 10.1016/j.hal.2003.12.005; Hsia M.H., 2005, HARMFUL ALGAE, V4, P287; Laabir M, 1999, J SHELLFISH RES, V18, P217; Laabir M, 2007, AQUAT LIVING RESOUR, V20, P51, DOI 10.1051/alr:2007015; Landsberg JH, 2002, REV FISH SCI, V10, P113, DOI 10.1080/20026491051695; Li SC, 2001, MAR BIOL, V139, P617, DOI 10.1007/s002270100613; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; Matsuyama Y, 1999, FISHERIES SCI, V65, P248, DOI 10.2331/fishsci.65.248; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; Nuzzi R., 1989, Novel Phytoplankton blooms, V35, P117; OLSON AM, 2001, MARKETING SHIPPING L, P243; OWEN K C, 1982, Florida Scientist, V45, P227; PATE S, 2006, THESIS N CAROLINA ST; Penna A, 2005, MAR BIOL, V148, P13, DOI 10.1007/s00227-005-0067-5; PERRY HM, 1979, GULF RES REP, V6, P313; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Powell EN, 2004, J SHELLFISH RES, V23, P803; Rensel JE., 2003, Manual on harmful marine algae, P693; Ruesink JL, 2005, ANNU REV ECOL EVOL S, V36, P643, DOI 10.1146/annurev.ecolsys.36.102003.152638; Ruiz GM, 2000, ANNU REV ECOL SYST, V31, P481, DOI 10.1146/annurev.ecolsys.31.1.481; Ruiz GM, 2000, NATURE, V408, P49, DOI 10.1038/35040695; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Shumway SE, 2006, HARMFUL ALGAE, V5, P442, DOI 10.1016/j.hal.2006.04.013; SILVERT WL, 1995, CAN J FISH AQUAT SCI, V52, P521, DOI 10.1139/f95-053; Springer JJ, 2002, MAR ECOL PROG SER, V245, P1, DOI 10.3354/meps245001; Ukeles R., 1973, Handbook of Phycological Methods, P233; van den Bergh JCJM, 2002, MAR POLICY, V26, P59, DOI 10.1016/S0308-597X(01)00032-X; Vila M, 2001, MAR ECOL PROG SER, V222, P73, DOI 10.3354/meps222073; Ward JE, 2004, J EXP MAR BIOL ECOL, V300, P83, DOI 10.1016/j.jembe.2004.03.002	40	65	71	1	33	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2008	361						169	179		10.3354/meps07375	http://dx.doi.org/10.3354/meps07375			11	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	322ZM		Bronze			2025-03-11	WOS:000257413800016
J	Crespo, BG; Teixeira, IG; Figueiras, FG; Castro, CG				Crespo, B. G.; Teixeira, I. G.; Figueiras, F. G.; Castro, C. G.			Microplankton composition off NW Iberia at the end of the upwelling season: source areas of harmful dinoflagellate blooms	MARINE ECOLOGY PROGRESS SERIES			English	Article						harmful dinoflagellates; coastal upwelling; Iberian poleward current; subsurface chlorophyll maximum; NW Iberia; rias baixas	RIA-DE-VIGO; POLEWARD CURRENT; RED TIDES; SPAIN; SYSTEM; COAST; GULF; FLOW; CIRCULATION; ATLANTIC	The Rias Baixas of Galicia are 4 bays on the NW Iberia Peninsula that experience harmful dinoflagellate blooms toward the end of the upwelling season, in late summer to early autumn. In order to identify the source areas of initial bloom populations, we studied the hydrographic regime and the microplankton composition in the NW Iberian margin at the end of summer 1991. Three distinctive oceanographic features were recognised as possible sources of initial populations: (1) the onset of a northward stream, the Iberian Poleward Current (IPC), which can transport seed populations to the region; (2) a subsurface chlorophyll maximum (SCM); and (3) weak upwelling at the coast, which can promote the growth of dinoflagellates. While the SCM held populations of the small dinoflagellates Heterocapsa niei and Prorocentrum minimum, larger dinoflagellates Prorocentrum micans, Dinophysis acuminata, Gymnodinium catenatum and the raphidophycean Heterosigma akashiwo, which habitually form blooms in the Rias Baixas, were only found in upwelled coastal waters, mostly off the Rias. These species occurred with a microplankton assemblage composed of other large dinoflagellates and diatoms, which is characteristic of the final summer upwelling events in the Rias. It is hypothesised that the Rias Baixas can be both the source and the target of harmful dinoflagellate blooms. Summer upwelling, through cyst resuspension and subsequent germination in the nearby stratified waters, would provide the initial populations. Downwelling, which promotes the accumulation of dinoflagellates in the interior of the Rias, would ensure blooms and hence replenish the sediments with new cysts.	[Crespo, B. G.; Teixeira, I. G.; Figueiras, F. G.; Castro, C. G.] CSIC, Inst Invest Marinas, Vigo 36208, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM)	Crespo, BG (通讯作者)，CSIC, Inst Invest Marinas, Eduardo Cabello 6, Vigo 36208, Spain.	bibiana@iim.csic.es	G. Teixeira, Isabel/S-6222-2016; G Figueiras, Francisco/A-5034-2008	G. Teixeira, Isabel/0000-0002-3279-754X; G Figueiras, Francisco/0000-0003-1810-4935; Castro, Carmen G./0000-0001-7415-078X				Alvarez-Salgado XA, 2003, PROG OCEANOGR, V56, P281, DOI 10.1016/S0079-6611(03)00007-7; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; BJORNSEN PK, 1991, MAR ECOL PROG SER, V73, P263, DOI 10.3354/meps073263; Castro CG, 1997, J MAR RES, V55, P321, DOI 10.1357/0022240973224436; Crespo BG, 2007, HARMFUL ALGAE, V6, P686, DOI 10.1016/j.hal.2007.02.007; Crespo BG, 2006, HARMFUL ALGAE, V5, P770, DOI 10.1016/j.hal.2006.03.006; Fermin EG, 1996, J PHYCOL, V32, P212, DOI 10.1111/j.0022-3646.1996.00212.x; FIGUEIRAS FG, 1993, DEV MAR BIO, V3, P239; Figueiras FG, 2002, HYDROBIOLOGIA, V484, P121, DOI 10.1023/A:1021309222459; FIGUEIRAS FG, 1994, J PLANKTON RES, V16, P857, DOI 10.1093/plankt/16.7.857; FRAGA S, 1988, ESTUAR COAST SHELF S, V27, P349, DOI 10.1016/0272-7714(88)90093-5; FROUIN R, 1990, J GEOPHYS RES-OCEANS, V95, P679, DOI 10.1029/JC095iC01p00679; Hansen HP., 1983, Automated Chemical Analysis. 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Ecol.-Prog. Ser.		2008	355						31	43		10.3354/meps07261	http://dx.doi.org/10.3354/meps07261			13	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	280NH		Green Submitted, Bronze			2025-03-11	WOS:000254433000004
J	Gedl, P				Gedl, Przemyslaw			Dinoflagellate cysts from Callovian of Lukow (Poland) - a re-examination	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article						dinoflagellate cysts; Jurassic; Callovian; Lukow; Poland; palaeogeography; biostratigraphy		More than 110 dinoflagellate cyst taxa have been found in the Callovian (Middle Jurassic) fossiliferous concretion and mudstone samples from Lukow, eastern Poland. Their assemblages are dominated by proximal species with apical archaeopyle (Lithodinia jurassica, Senstusidinium spp., Batiacasphaera spp., Escharisphaeridia spp.). The Lukow assemblage may be correlated with the Upper Callovian Wanaea thysanota Interval Biozone established in the British Isles. This is based on the co-occurrence of Trichodinium scarbourghense, Clathroctenocystis asaphes and Durotrigia filapicata. Diversity of the dinoflagellate cyst assemblage indicates optimal living conditions for dinoflagellates whereas dominance of land-derived phytoclasts and sporomorphs suggests a near-shore sedimentary setting. Presence of some endemic Boreal species, Ctenidodinium thulium and Valvaeodinium groenlandicum, points to influences from northern areas.	Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						[Anonymous], 1996, Palynology: principles and applications; Bailey D.A., 1991, Journal of Micropalaeontology, V9, P245; BAILEY D A, 1990, Palynology, V14, P135; BANDEL K, 1988, CEPHALOPODS PRESENT, P303; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; BIRKENMAJER K, 2007, STUDIA GEOLOGICA POL, V127, P49; BRAND U, 1986, J PALEONTOL, V60, P293, DOI 10.1017/S002233600002182X; BRINKMANN R., 1927, SCHRIFTEN PHYS OKON GES KONIGSBERG, V65, P49; Cookson I. C., 1962, Proceedings of the Royal Society of Victoria, V75, P269; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; DAVIES E. 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A. S, 1968, R MICROPALEONTOL, V10, P221; Schroeder Michael, 1995, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V238, P1; SIEMIRADZKI J, 1923, GEOLOGIA ZIEM POLSKI, V1, P223; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; SMELROR M, 1993, PALAEOGEOGR PALAEOCL, V102, P121, DOI 10.1016/0031-0182(93)90009-8; STUPNICKA T, 1979, SPRAWOZDAIA POSIEDZE, V21, P187; STUPNICKA T, 1979, SPRAWOZDAIA POSIEDZE, V22, P193; STUPNICKA T, 1974, ACTA PALAEONTOLOGICA, V19, P179; Tarkowski R., 1987, MINERALOGIA POLONICA, V18, P19; TARKOWSKI R, 1989, SPRAWOZDANIA POSIEDZ, V31, P94; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V28; WOOLLAM R, 1983, I GEOL SCI REP, V83, P1	69	6	6	0	3	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.		2008	247	2					209	269		10.1127/0077-7749/2008/0247-0209	http://dx.doi.org/10.1127/0077-7749/2008/0247-0209			61	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	281LU					2025-03-11	WOS:000254499900007
J	Pestchevitskaya, EB				Pestchevitskaya, Ekatarina B.			Lower Cretaceous palynostratigraphy and dinoflagellate cyst palaeoecology in the Siberian palaeobasin	NORWEGIAN JOURNAL OF GEOLOGY			English	Article							BIOSTRATIGRAPHY; NORTH; SECTION	Palynological analysis of Lower Cretaceous (Berriasian-Barremian) sections from North Siberia allows definition of detailed dinocyst and spore-pollen zonations, which are calibrated against the established ammonite biostratigraphic schemes of Siberia. Most of the boundaries of the palynological zones are reliable correlative markers, which also can be recognized elsewhere in East and West Siberia (the spore-pollen zonation) and in NW Europe, Canada and Siberia (the dinocyst zonation). Changes in the microphytoplankton associations reflect both trends related to the dynamic evolution of the Siberian palaeobasin and trends of the dinocyst evolution. Results from the present study suggest that the diversity and the abundance of the Siberian microphytoplankton associations to a large extent were determined by sea water temperature and nutrients.	Inst Petr Geol & Geophys SB RAS, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Pestchevitskaya, EB (通讯作者)，Inst Petr Geol & Geophys SB RAS, Av Prof Koptyug 3, Novosibirsk 630090, Russia.	PeschevickayaEB@ipgg.nsc.ru		Pestchevitskaya, Ekaterina/0000-0001-8174-0737	Russian Fund of Basic Research [09-05-00645]	Russian Fund of Basic Research(Russian Foundation for Basic Research (RFBR))	Financial support of Russian Fund of Basic Research, grant No 09-05-00645.	AARHUS N, 1986, NORSK GEOL TIDSSKR, V66, P17; AARHUS N, 1990, POLAR RES, V8, P165; BARABOSHKIN EY, 2007, PROLIVY SEVERNOGO PO, P1; BOGOMOLOV YI, 1989, POLYPTICHITY AMMONIT, P1; Costa L.I., 1992, P99; Davey R.J., 1982, Danmarks Geologiske Undersogelse Serie B, P1; DAVIES E. H., 1983, GEOL SURV CAN B, V359, P1; DAVIES EH, 1982, P 3 N AM PAL CONV, V1, P125; Duxbury S, 2001, NEUES JAHRB GEOL P-A, V219, P95, DOI 10.1127/njgpa/219/2001/95; Fisher M.J., 1980, P 4 INT PAL C LUCKN, V2, P313; GOLBERT AV, 1987, OSNOVY REGIOLALNOJ P, P1; HAKANSSON E, 1981, Bulletin of the Geological Society of Denmark, V30, P11; Konovalova G.V., 1998, P1; KORT VG, 1969, MIKROFLORA MIKROFAUN, P1; Lebedeva NK, 2008, STRATIGR GEO CORREL+, V16, P182, DOI 10.1134/S0869593808020068; Lebedeva NK, 1999, GRANA, V38, P134, DOI 10.1080/00173139908559222; Leerveld H., 1995, LPP Contribution Series, V2, P1; MCINTYRE DJ, 1980, GEOL SURV CAN B, V320, P57; NORRIS G, 1970, REV PALAEOBOT PALYNO, V10, P131, DOI 10.1016/0034-6667(70)90016-3; Pestchevitskaya EB, 2007, STRATIGR GEO CORREL+, V15, P577, DOI 10.1134/S0869593807060020; Pestchevitskaya EB, 2007, RUSS GEOL GEOPHYS+, V48, P941, DOI 10.1016/j.rgg.2007.10.004; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Robin South G., 1987, INTRO PHYCOLOGY, P1; Smelror M, 1998, POLAR RES, V17, P181, DOI 10.1111/j.1751-8369.1998.tb00271.x; Smelror M., 2005, NORGES GEOLOGISKE UN, V443, P61; VANHELDEN BGT, 1986, PALYNOLOGY, V10, P81; VINOGRADOV ME, 2004, NOVYE IDEI OKEANOLOG, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D, 1969, P N AM PAL CONV G, P844; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zakharov V.A., 1974, PALEOBIOGEOGRAFIYA S, P127; Zakharov V.A., 1997, RUSS GEOL GEOPHYS+, V38, P965; ZAKHAROV VA, 1983, PALEOBIOGEOGRAFIYA B, P56; ZAKHAROV VA, 1999, RUSSIAN GEOLOGY GEOP, V40, P1117	35	9	12	0	1	GEOLOGICAL SOC NORWAY	TRONDHEIM	C/O NGU, 7491 TRONDHEIM, NORWAY	0029-196X			NORW J GEOL	Norw. J. Geol.		2008	88	4					279	286						8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	435OG					2025-03-11	WOS:000265352600008
J	Kennaway, GM; Eaton, GL; Feist-Burkhardt, S				Kennaway, Gabrielle M.; Eaton, Geoffrey L.; Feist-Burkhardt, Susanne			A DETAILED PROTOCOL FOR THE PREPARATION AND ORIENTATION OF SINGLE FOSSIL DINOFLAGELLATE CYSTS FOR TRANSMISSION ELECTRON MICROSCOPY	PALYNOLOGY			English	Article						encapsulation; orientation; transmission electron microscopy; dinoflagellate cysts; wall structure		The relationship between wall layers in dinoflagellate cysts was investigated with transmission electron microscopy. A simple method is described in which small cysts (<100 mu m) were identified. isolated, and encapsulated in colored agarose. The individual cysts, now visible to the naked eye, were easy to track throughout the multi-step protocol. The routine TEM protocol for biological material was modified and simplified for dinoflagellate cysts, and is described in detail, This method ensures that all saniples can be retained, an important consideration when working with rare or unique specimens. Specimens of Hystrichosphaeropsis Deflandre 1935 were orientated for sectioning relative to the natural plane of settlement of the cyst. Serial sections demonstrated that the relationship between the endophragm and periphragm is complex and irregular. Interpretation of micrographs and some common misinterpretations of artifacts are illustrated and discussed. The protocol is presented in detail and illustrated so that an inexperienced person, with the assistance of an electron microscopy unit. could successfully carry out the procedure. The technique has been used with minor adaptations to prepare a range of biological materials and palynomorph specimens for transmission electron microscopy.	[Kennaway, Gabrielle M.] Nat Hist Museum, Dept Mineral, Electron Microscopy & Mineral Anal Div, London SW7 5BD, England; [Eaton, Geoffrey L.; Feist-Burkhardt, Susanne] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England	Natural History Museum London; Natural History Museum London	Kennaway, GM (通讯作者)，Nat Hist Museum, Dept Mineral, Electron Microscopy & Mineral Anal Div, Cromwell Rd, London SW7 5BD, England.	Gabrielle.Kennaway@nhm.ac.uk; geoffeaton1@aol.com; S.Feist-Burkhardt@nhm.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242				[Anonymous], 1968, PALAEONTOGRAPHICA B; BENEDEK P N, 1981, Palaeontographica Abteilung B Palaeophytologie, V180, P39; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BOZZOLA JJ, 1992, ELECT MICROSCOPY PRI, P67; Eaton G.L., 1984, Journal of Micropalaeontology, V3, P53; Glauert A.M., 1998, PRACT MET E, V17; Javaux EJ, 2004, GEOBIOLOGY, V2, P121, DOI 10.1111/j.1472-4677.2004.00027.x; JUX U, 1980, Palaeontographica Abteilung B Palaeophytologie, V174, P1; Jux U., 1976, Palaeontographica Abteilung B Palaeophytologie, V155, P149; Jux U., 1971, Palaeontogr. Abt. B, V132, P165; Jux U., 1971, Palaeontographica Abt., VB136, P115; JUX U, 1965, PALAEONTOGR ABT B, V115, P107; Jux U., 1968, Palaeontographica Abt, v, VB124, P112; JUX U, 1968, PALAEONTOGR ABT B, V123, P147; Kennaway Gabrielle M., 2004, Systematic and Applied Acarology, V9, P3; Kennaway GM, 2004, PHYCOLOGIA, V43, P353; Lewis J, 2001, PHYCOLOGIA, V40, P280, DOI 10.2216/i0031-8884-40-3-280.1; Norris G., 1984, Palaeontographica Abteilung B Palaeophytologie, V190, P158; PEARCE MA, 2000, THESIS KINGSTON U UK; PEAT CJ, 1981, J MICROSC-OXFORD, V122, P287, DOI 10.1111/j.1365-2818.1981.tb01268.x; REYNOLDS ES, 1963, J CELL BIOL, V17, P208, DOI 10.1083/jcb.17.1.208; SPURR AR, 1969, J ULTRA MOL STRUCT R, V26, P31, DOI 10.1016/S0022-5320(69)90033-1; Talyzina NM, 2000, REV PALAEOBOT PALYNO, V112, P1, DOI 10.1016/S0034-6667(00)00032-4	23	3	3	0	6	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2008	32						1	15		10.2113/gspalynol.32.1.1	http://dx.doi.org/10.2113/gspalynol.32.1.1			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600001
J	Smelror, M; Key, RM; Smith, RA; Njange, F				Smelror, Morten; Key, Roger M.; Smith, Richard A.; Njange, Fernando			LATE JURASSIC AND CRETACEOUS PALYNOSTRATIGRAPHY OF THE ONSHORE ROVUMA BASIN, NORTHERN MOZAMBIQUE	PALYNOLOGY			English	Article						palynomorphs; biostratigraphy; Mesozoic; Mozambique		Late Jurassic and Cretaceous palynomorph assemblages were recovered from the Macomia, Pemba, and Mifume formations front the onshore Rovuma Basin. northern Mozambique. These assemblages provide new evidence for in Aptian-Albian age for the Macomia Formation and the Upper member of Pemba Formation, and confirm that these two stratigraphic units are coeval and laterally continuous. The lower member of the Pemba Formation contains Kimmeridgian-Tithonian palynomorphs, thus documenting for the first time the existence of Upper Jurassic strata north of Nacala in the onshore Rovuma Basin. The rich and diverse dinoflagellate cyst assemblage recovered from the Mifume Formation is of late Campanian age. This indicates an early Late Cretaceous hiatus between the sandstones of Pemba Formation, and the marls of the overlying Mifume Formation. The hiatus corresponds to a break in sedimentation prior to a rapid. global marine transgression, recognised in the Rovuma and Mozambique basins, during the middle Campanian, associated with the onset of Gondwana fragmentation. Earlier, Late Jurassic faulting produced local half-grabens filled with continental debris, for example the N'Gapa Formation of northern Mozambique.	[Smelror, Morten] Geol Survey Norway, NO-7491 Trondheim, Norway; [Key, Roger M.; Smith, Richard A.] British Geol Survey, Edinburgh EH9 3LA, Midlothian, Scotland; [Njange, Fernando] Direccao Natl Geol, Pemba, Mozambique	Geological Survey of Norway; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Smelror, M (通讯作者)，Geol Survey Norway, Leiv Eirikssons Vei 39, NO-7491 Trondheim, Norway.	Morten.Smelror@ngu.no						AITKEN WG, 1961, GEOLOGICAL SURVEY TA, V31; [Anonymous], 1973, Sedimentary basins of the African coasts; CIVITELLI G, 1988, J AFR EARTH SCI, V7, P629, DOI 10.1016/0899-5362(88)90113-3; Costa L.I., 1992, P99; COSTER PW, 1989, J PETROL GEOL, V12, P205, DOI 10.1111/j.1747-5457.1989.tb00233.x; DANIELS CH, 1977, GEOLOGISCHES JB, V26, P167; FLORES GM, 1960, RECONNAISSANCE UNPUB; FORSTER R, 1975, PALAEOGEOGR PALAEOCL, V17, P267, DOI 10.1016/0031-0182(75)90002-4; Gradstein F., 2004, A Geological Time Scale; Groschke Manfred, 1995, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V16, P645; Hancox PJ, 2002, J AFR EARTH SCI, V34, P291, DOI 10.1016/S0899-5362(02)00028-3; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Key RM, 2008, S AFR J GEOL, V111, P89, DOI 10.2113/gssajg.111.1.89; KEY RM, 2006, C AFR GEOL 21 MAP JU, P232; PINNA P, 1995, J AFR EARTH SCI, V21, P477, DOI 10.1016/0899-5362(95)00077-7; SALMAN G, 1995, SEDIMENT GEOL, V96, P7, DOI 10.1016/0037-0738(95)00125-R; Schrank E, 2005, PALYNOLOGY, V29, P49, DOI 10.2113/29.1.49; Schrank Eckart, 1999, Mitteilungen aus dem Museum fuer Naturkunde in Berlin Geowissenschaftliche Reihe, V2, P171; SMELROR M, 2006, C AFR GEOL 21 MAP JU, P248; SMELROR M, 2006, GEOEXPRO, V3, P14	20	17	18	0	10	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2008	32						63	76		10.1080/01916122.2008.9989650	http://dx.doi.org/10.1080/01916122.2008.9989650			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR		Green Accepted			2025-03-11	WOS:000207494600005
J	Eisawi, A; Schrank, E				Eisawi, Ali; Schrank, Eckart			UPPER CRETACEOUS TO NEOGENE PALYNOLOGY OF THE MELUT BASIN, SOUTHEAST SUDAN	PALYNOLOGY			English	Article						Upper Cretaceous; Paleogene; Neogene; pollen; spores; biostratigraphy; paleoecology; Melut Basin; Sudan		The palynology of the Upper Cretaceous to Neogene non-marine Succession in the Melut Basin, southeast Sudan was investigated. The palynomorphsare overwhelmingly of terrestrial origin, but rare brackish water dinoflagellate cysts and scolecodonts were encountered from the Lower Miocene and Oligocene-Miocene. Mangrove pollen, which is common in coeval West African coastal basins, is rare and inconsistent. Examples are Spinizonocolpites(Nypa) from the Campanian-Maastrichtian to Eocene and Rhizophoraceae (Zonocostites romonae) from the Neogene. Based on the stratigraphic distribution Of Selected pollen and Spores from four exploration wells, eight informal palynozones from the Campanian to the Neogene are proposed. The zones. in stratigraphically ascending order, are as follows: Assemblage Zone 1, Campanian (lower Melut Formation) Assemblage Zone 11, (middle Melut Formation): Assemblage Zone III, Maastrichtian (upper Melut Formation) Assemblage Zone IV, Palcocene (Yale Formation) Assemblage Zone V, Eocene (upper Yale and Adar formations); Assemblage Zone VI, Oligocene-Early Miocene (Jimidi and lower Miadol formations): Assemblage Zone VII, Early Miocene (uppermost Miadol and lowermost Daga formations)-. and Assemblage Zone VIII, Late Miocene-Pliocene (Daga Formation). The ages are based on stratigraphic positions and a series of first downhole appearances of key species Such as Foveotricolpites cf. giganteus (Zone I), Auriculiidites reticulatus (Zone II), Ariadnaesporites spinosus (Zone III), Periretisyncolpites giganteus (Zone IV), Retistephanocolpites williamsii (Zone V), Cricotriporites camerounensis (Zone VI), Peifotricolpites digitatus (Zone VII),and Peregrinipollis nigericus (Zone VIII). Palynofacies investigations indicated differences between the Late Cretaceous and Paleogene-Neoggene paleoenvironments of the sections Studied. The coexistence of structured organic palynodebris with pteridophyte spores. including those of water ferns (Ariadnaespwrites), in the Upper Cretaceous strata suggests swampy conditions within a predominantly fluvial setting.The frequent occurrence of Palinae pollen indicates warm, humid conditions during the Late Cretaceous, although seasonal or hinterland aridity is suggested because of the occurrence of ephedroid pollen. Late Paleogene and Neogene assemblages are characterized by amorphous organic matter, fern spores, freshwater algae, and Gramineae pollen. Deposition in lacustrine habitats under warm, humid conditions is inferred. The occurrence of Gramineae pollen, mainly in the Neogene, indicates the development of grassy areas in it seasonally dry climate. A short marine incursion may have taken place during the Oligocene-Miocene, due to the rare occurrence of brackish water dinoflagellate cysts and scolecodonts.	[Eisawi, Ali] Al Neelain Univ, Fac Sci & Technol, Sch Appl Earth Sci, Khartoum, Sudan; [Schrank, Eckart] Tech Univ Berlin, Inst Angew Geowissensch, D-10587 Berlin, Germany	Technical University of Berlin	Eisawi, A (通讯作者)，Al Neelain Univ, Fac Sci & Technol, Sch Appl Earth Sci, POB 12702, Khartoum, Sudan.	eisawia@yahoo.com; e.schrank@tu-berlin.de						ADEGOKE O S, 1978, Revista Espanola de Micropaleontologia, V10, P267; Akkiraz MS, 2005, GEOBIOS-LYON, V38, P283, DOI 10.1016/j.geobios.2003.11.010; [Anonymous], REV ESPANOLA MICROPA; Awad, 1994, BERLINER GEOWISSENSC, V161; BAKR IM, 1995, THESIS U KHARTOUM SU; BEILSTEIN U, 1994, GEOLOGISCHES I U KOE, V95; Clarke R.T., 1968, Grana Palynologica, V8, P210; COUPER R.A., 1958, PALAEONTOGRAPHICA, V103, P75; Edet J.J., 1992, Revista Espanola de Micropaleontologia, V24, P3; EISAWI AAM, 2007, THESIS TU BERLIN; GERMERAAD JH, 1968, REV PALAEOBOT PALYNO, V6, P189, DOI 10.1016/0034-6667(68)90051-1; Guinet P, 1975, BOISSIERA, V24, P21; GUZMAN AEG, 1967, PALYNOLOGY STUDY UPP; HALL JW, 1975, AM J BOT, V62, P359, DOI 10.2307/2442089; Herngreen GFW., 1996, PALYNOLOGY PRINCIPLE, V3, P1157; Jansonius J, 1987, GENERA FILE FOSSIL S; Jaramillo Carlos A., 2001, Palaeontographica Abteilung B Palaeophytologie, V258, P87; Jardine S., 1965, M M BUR RECH G OL MI, V32, P187; Kaska H.V., 1989, PALYNOLOGY, V13, P79, DOI [10.1080/01916122.1989.9989356, DOI 10.1080/01916122.1989.9989356]; Lawal O., 1986, Review de Micro. 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K., 1999, Palynology, V23, P197; Mahmoud MS, 2003, J AFR EARTH SCI, V36, P135, DOI 10.1016/S0899-5362(03)00047-2; MBEDE EI, 1987, J AFR EARTH SCI, V6, P313, DOI 10.1016/0899-5362(87)90074-1; *RRI, 1991, GEOL PETR POT SO CEN, V1; SAH SCD, 1967, MUSEE ROYAL AFRIQUE, V57; SALARD-CHEBOLDAEFF M., 1978, POLLEN SPORES, V20, P215; SALARDCHEBOLDAEFF M, 1979, REV PALAEOBOT PALYNO, V28, P365, DOI 10.1016/0034-6667(79)90032-0; SALARDCHEBOLDAEFF M, 1990, J AFR EARTH SCI, V11, P1, DOI 10.1016/0899-5362(90)90072-M; Schrank E., 1987, BERLINER GEOWISS ABH, V75, P249, DOI DOI 10.1016/0195-6671(92)90040-W; Schrank Eckart, 1994, Palaeontographica Abteilung B Palaeophytologie, V231, P63; SCHULL TJ, 1988, AAPG BULL, V72, P1128; Stead DT, 2005, MICROPAL SOC SPEC PU, P161; Sultan I.Z., 1986, Revue de Micropaleontologie, V28, P213; Takahashi J., 1989, Bulletin of the Faculty of Liberal Arts, Nagasaki University, Natural Science, V29, P181; Torricelli Stefano, 2001, Palynology, V25, P29, DOI 10.2113/0250029; Utescher T, 2007, PALAEOGEOGR PALAEOCL, V247, P243, DOI 10.1016/j.palaeo.2006.10.022; van HOEKEN KLINKENBERG P. M. J., 1964, POLLEN SPORES, V6, P209; Wilkinson G.C., 1980, PALAEONTOGR ABT B, V175, P27	39	40	49	1	10	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						101	129						29	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600008
J	Louwye, S; Mertens, KN; Vercauteren, D				Louwye, Stephen; Mertens, Kenneth Neil; Vercauteren, Dries			NEW DINOFLAGELLATE CYSTS FROM THE MIOCENE OF THE PORCUPINE BASIN, OFFSHORE SOUTHWEST IRELAND	PALYNOLOGY			English	Article						dinoflagellate cysts; biostratigraphy; taxonomy; offshore Ireland; eastern North Atlantic; Miocene	NORTHERN BELGIUM; ATLANTIC; PLIOCENE; MOUND	Four new dinoflagellate cyst species from the Lower and Middle Miocene strata of the Porcupine Basin, offshore southwest Ireland. are formally described. Batiacasphaera edwardsiae sp. nov. was previously described under open nomenclature from the Miocene of the adjacent Rockall Plateau. Lejeunecysta challengerensis sp. nov. is recorded sporadically from the Burdigalian and Serravallian. Selenopemphix porcupensis sp. nov. and Trinovantedinium henrietii sp. nov. are large-sized dinoflagellate cysts with maximum dimensions of approximately 100 mu m. Selenopemphix porcupensis sp. nov. is recorded in the uppermost Burdigalian and Langhian, and Trinovantedinium henrietii sp. nov. is present in the Langhian and lowermost Batiacasphaera edwardsiae sp. nov. is possibly biostratigraphically significant for the Middle Miocene.	[Louwye, Stephen; Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Vercauteren, Dries] Univ Ghent, Lab Gen Biochem & Phys Pharm, B-9000 Ghent, Belgium	Ghent University; Ghent University	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	stephen.louwye@UGent.be	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Mertens, Kenneth/0000-0003-2005-9483; Louwye, Stephen/0000-0003-4814-4313				Böhme M, 2003, PALAEOGEOGR PALAEOCL, V195, P389, DOI 10.1016/S0031-0182(03)00367-5; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; DE VERTEUIL L., 1996, MICROPALEONTOLOGY S, V42; DEMOL B, 2002, MAR GEOL, V88, P193; EDWARDS LE, 1984, INITIAL REP DEEP SEA, V81, P581; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FERDELMAN TG, 2006, P IODP, V307, DOI DOI 10.2204/IODP.PROC.307.105.2006; Kano A, 2007, GEOLOGY, V35, P1051, DOI 10.1130/G23917A.1; Lourens L.J., 2004, GEOLOGICAL TIME SCAL, P409, DOI 10.1017/CBO9780511536045; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Louwye S, 2007, GEOL MAG, V144, P33, DOI 10.1017/S0016756806002627; McDonnell A, 2001, GEOL SOC SPEC PUBL, V188, P323, DOI 10.1144/GSL.SP.2001.188.01.19; PEARSON I, 1986, SPEC PUBL GEOL SOC L, V21, P79; Stoker MS, 2001, GEOL SOC SPEC PUBL, V188, P411, DOI 10.1144/GSL.SP.2001.188.01.26; STOKER MS, 2003, MAR PETROL GEOL, V22, P965; Van Rooij D, 2007, GEOL SOC SPEC PUBL, V276, P225, DOI 10.1144/GSL.SP.2007.276.01.11; Van Rooij D, 2003, MAR GEOL, V195, P31, DOI 10.1016/S0025-3227(02)00681-3; Versteegh GJM, 1996, GLOBAL PLANET CHANGE, V11, P155, DOI 10.1016/0921-8181(95)00054-2; Warny SA, 2002, MICROPALEONTOLOGY, V48, P257, DOI 10.2113/48.3.257; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	21	4	4	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2008	32						131	142						12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600009
J	Garzon, SL; Torres-Torres, V; Jaramillo, C				Garzon, S. L.; Torres-Torres, V; Jaramillo, C.			EARLY OLIGOCENE-EARLY MIOCENE DINOFLAGELLATE CYSTS FROM ARROYO ALFEREZ SECTION, CARMEN DE BOLIVAR, COLOMBIA	PALYNOLOGY			English	Meeting Abstract									[Garzon, S. L.] Univ Ind Santander, Santander, Colombia; [Jaramillo, C.] Smithsonian Trop Res Inst, Balboa, Panama	Universidad Industrial de Santander; Smithsonian Institution; Smithsonian Tropical Research Institute									0	0	0	0	1	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						260	260						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600026
J	Louwye, S; Foubert, A; Mertens, K; Van Rooij, D				Louwye, S.; Foubert, A.; Mertens, K.; Van Rooij, D.		IODP Expedition 307 Sci Party	DINOFLAGELLATE CYST STRATIGRAPHY AND PALAEOECOLOGY OF THE LOWER AND MIDDLE MIOCENE OF PORCUPINE BASIN, SOUTHWEST OF IRELAND	PALYNOLOGY			English	Meeting Abstract									[Louwye, S.; Foubert, A.; Mertens, K.; Van Rooij, D.] Univ Ghent, Renard Ctr Marine Geol, Res Unit Palaeontol, Ghent, Belgium	Ghent University			Mertens, Kenneth/AAO-9566-2020; Van Rooij, David/A-7938-2014; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483					0	0	0	0	5	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						263	263						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600038
J	McCarthy, FMG; Gregg, HA; Head, MJ; Shaw, JC				McCarthy, F. M. G.; Gregg, H. A.; Head, M. J.; Shaw, J. C.			DISTINGUISHING THE IMPACT OF EUROPEAN AND WENDAT (FIRST NATIONS) SETTLEMENT ON SEVERN SOUND, GEORGIAN BAY (NORTH AMERICAN GREAT LAKES) USING RESTING CYSTS OF FRESHWATER DINOFLAGELLATES	PALYNOLOGY			English	Meeting Abstract									[McCarthy, F. M. G.; Head, M. J.; Shaw, J. C.] Brock Univ, St Catharines, ON L2S 3A1, Canada	Brock University									0	0	0	0	0	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						264	264						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600040
J	Michoux, D				Michoux, D.			DINOFLAGELLATE CYST ASSEMBLAGES FROM THE PALEOGENE OF TIERRA DEL FUEGO, ARGENTINA	PALYNOLOGY			English	Meeting Abstract																		OLIVERO, 1999, AAPG B, V832; OLIVERO, 2001, REV ASOCIATION GEOLO, V572	2	0	0	0	0	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						265	265						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600042
J	Paez, M; Head, MJ; McCarthy, FMG; Westphal, RMH				Paez, M.; Head, M. J.; McCarthy, F. M. G.; Westphal, RCom-Marum H.			PRELIMINARY DINOFLAGELLATE CYST BIOSTRATIGRAPHY OF A NEOGENE SUBTROPICAL CARBONATE PLATFORM: ODP HOLE 1007C, BAHAMAS	PALYNOLOGY			English	Meeting Abstract									[Paez, M.; Head, M. J.; McCarthy, F. M. G.] Brock Univ, St Catharines, ON L2S 3A1, Canada; [Westphal, RCom-Marum H.] Univ Bremen, D-2800 Bremen 33, Germany	Brock University; University of Bremen									0	0	0	0	0	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						266	267						2	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600047
J	Pavlishina, P				Pavlishina, P.			UPPER JURASSIC-LOWER CRETACEOUS DINOFLAGELLATE CYST BIOSTRATIGRAPHY, PALYNOFACIES AND PALEOENVIRONMENTAL INTERPRETATIONS IN THE AREA OF LAKE HAZEN, ELLESMERE ISLAND, CANADIAN ARCTIC	PALYNOLOGY			English	Meeting Abstract									[Pavlishina, P.] Univ Sofia, Dept Geol & Paleontol, Sofia, Bulgaria	University of Sofia			Pavlishina, Polina/AAL-5710-2021						0	0	0	0	3	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2008	32						267	267						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	V10WR					2025-03-11	WOS:000207494600050
J	Moestrup, O; Hansen, G; Daugbjerg, N				Moestrup, Ojvind; Hansen, Gert; Daugbjerg, Niels			Studies on woloszynskioid dinoflageflates III:: on the ultrastructure and phylogeny of <i>Borghiella dodgei</i> gen. et sp nov., a cold-water species from Lake Tovel, N. Italy, and on <i>B-tenuissima</i> comb. nov (syn. <i>Woloszynskia tenuissima</i>)	PHYCOLOGIA			English	Article						freshwater; dinoflagellates; ultrastructure; taxonomy; phylogeny	FLAGELLAR APPARATUS; DINOPHYCEAE; DNA; ARCHITECTURE; MORPHOLOGY; POLARELLA; NETWORK; GROWTH; LIGHT	Using ultrastructure and nuclear-encoded large subunit (LSU) rDNA sequences, the woloszynskioid dinoflagellates have been shown recently to form a polyphyletic assemblage. The first group comprises the family Tovelliaceae, with the genera Tovellia and Jadwigia. The present manuscript describes the second group, comprising Borghiella dodgei gen. et sp. nov. from the Italian Alps. The new genus differs in a number of ultrastructural features, of which the most important are the structure of the eyespot (type B sensu Moestrup & Daugbjerg) and the structure of the apical part of the cell. The resting cyst is smooth, in contrast to the cysts of other woloszynskioids such as Tovellia and some species of Woloszynskia. The new species has been previously confused with Tovellia sanguinea, which was responsible for colouring the water of Lake Tovel, in the Italian Alps, blood-red up to 1964. However, B. dodgei may form brown, never truly red blooms as in the case of T. sanguinea. The transverse flagellum of Borghiella carries, in addition to thin hairs found also in other dinoflagellates, a row of shorter, thicker hairs resembling the curly hairs on the homologous, anterior flagellum of the perkinsid Parvilucifera but apparently not observed in any other dinoflagellates. Woloszynskia tenuissima, a well-known cold-water dinoflagellate, has been re-examined using material isolated from Greenland. Based on partial LSU rDNA sequencing it is shown to be related to R dodgei (sequence divergence only 1.1%) and is transferred to this genus as B. tenuissima comb. nov. We agree with the observations of von Stosch that the cysts of this species are spherical and smooth, in contrast to what was mentioned in the original description by Woloszynska.	[Moestrup, Ojvind; Hansen, Gert; Daugbjerg, Niels] Univ Copenhagen, Psychol Sect, Inst Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark	University of Copenhagen	Moestrup, O (通讯作者)，Univ Copenhagen, Psychol Sect, Inst Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	moestrup@bi.ku.dk	Daugbjerg, Niels/D-3521-2014; Hansen, Gert/P-3328-2014	Daugbjerg, Niels/0000-0002-0397-3073; Moestrup, Ojvind/0000-0003-0965-8645; Hansen, Gert/0000-0002-5751-8316				Andersen RA, 1997, J PHYCOL, V33, P1, DOI 10.1111/j.0022-3646.1997.00001.x; Bergholtz T, 2006, J PHYCOL, V42, P170, DOI 10.1111/j.1529-8817.2006.00172.x; Biecheler B, 1934, CR SOC BIOL, V115, P1039; Biecheler B., 1952, Bull. Biol. Fr. 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Zbl, V14, P390; LAUTERBORN R, 1899, Z WISSENSCHAFTLICHEN, V656, P369; LENAERS G, 1989, J MOL EVOL, V29, P40, DOI 10.1007/BF02106180; Lindberg K, 2005, PHYCOLOGIA, V44, P416, DOI 10.2216/0031-8884(2005)44[416:SOWDIW]2.0.CO;2; Lindemann E., 1929, Archiv fuer Protistenkunde Jena, V68, P1; LINDEMANN E, 1925, EINFACHSTE LEBENSFOR, V5, P144; Loeblich A.R., 1966, STUD TROP OCEANOGR, V3, P1; LOEBLICH AR, 1979, J MAR BIOL ASSOC UK, V59, P195, DOI 10.1017/S0025315400046270; Logares R, 2007, MICROB ECOL, V53, P549, DOI 10.1007/s00248-006-9088-y; MADDISON DR, 2003, MACCLADE, V4; Matvilenko O.M., 1977, Vyznachnyk Prisnovodnykh Vodoroste! Ukrains'koi RSR, V3, P1; McNeill J., 2006, V146, P1; Moestrup O, 2006, EUR J PHYCOL, V41, P47, DOI 10.1080/09670260600556682; Moestrup O, 2000, SYST ASSOC SPEC VOL, V59, P69; Moestrup O, 2007, UNRAVELLING ALGAE PR, P215; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; Nunn GB, 1996, J MOL EVOL, V42, P211, DOI 10.1007/BF02198847; Nygaard G., 1949, Biologiske Skrifter Copenhagen, V7, P1; Palliani RB, 2003, GRANA, V42, P108, DOI 10.1080/00173130310012495; PFIESTER LA, 1980, T AM MICROSC SOC, V99, P213, DOI 10.2307/3225709; POPOVSKY J., 1990, Susswasserflora von Mitteleuropa, P272; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; ROBERTS KR, 1988, J PHYCOL, V24, P544, DOI 10.1111/j.1529-8817.1988.tb00104.x; Roberts KR, 1995, J PHYCOL, V31, P948, DOI 10.1111/j.0022-3646.1995.00948.x; SCHILLER J., 1926, ARCH PROTISTENK, V56, P1; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SUCHLANDT O., 1916, Ber. Deutsch. Bot. Ges, V34, P242; Swofford DL., 1998, PHYLOGENETIC ANAL US; TAMURA K, 1993, MOL BIOL EVOL, V10, P512, DOI 10.1093/oxfordjournals.molbev.a040023; THOMPSON JD, 1995, NAT MED, V1, P277, DOI 10.1038/nm0395-277; Thompson R.H., 1947, FRESH WATER DINOFLAG; Von Stosch HA., 1973, Br Phycol J, V8, P105; WILCOX LW, 1989, J PHYCOL, V25, P785, DOI 10.1111/j.0022-3646.1989.00785.x; Wilgenbusch JC., 2004, AWTY: A system for graphical exploration of MCMC convergence in Bayesian phylogenetic inference, DOI DOI 10.1214/20-BA1221; WOIOSZYNSKA J, 1917, B ACAD SCI CRACOVI B, V1, P114	62	59	63	0	7	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	JAN	2008	47	1					54	78		10.2216/07-32.1	http://dx.doi.org/10.2216/07-32.1			25	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	250GU					2025-03-11	WOS:000252288800007
J	Konovalova, GV				Konovalova, G. V.			Parasitic dinoflagellates and ellobiopsids (Ellobiopsidae) of the coastal waters of the sea of Japan	RUSSIAN JOURNAL OF MARINE BIOLOGY			English	Article						parasitic dinoflagellates; ellobiopsidae; sea of Japan	DISSODINIUM; DINOPHYTA; CYSTS	Five species of parasitic dinoflagellates of the genera Protoodinium, Paulsenella, Duboscquella, Syndinium, and Dissodinium and two species of ellobiopsids of the genus Ellobiopsis are described. Figures and distribution data are provided. All species, except for Dissodinium pseudolunula Swift ex Elbrachter et Drebes, are first records for the Russia Far-Eastern seas.	Russian Acad Sci, Inst Marine Biol, Far E Div, Vladivostok 690041, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Konovalova, GV (通讯作者)，Russian Acad Sci, Inst Marine Biol, Far E Div, Vladivostok 690041, Russia.	vpois@imb.dvo.ru						AKSELMAN R, 1989, Physis Seccion A los Oceanos y sus Organismos, V47, P43; BOSCHMA H, 1956, CONS INT EXPLOR MER, P1; Bridgeman TB, 2000, CAN J FISH AQUAT SCI, V57, P1539, DOI 10.1139/cjfas-57-8-1539; Cachon J., 1987, Botanical Monographs (Oxford), V21, P571; Caullery M., 1910, B SCI FR BELG, V44, P201; Chatton E., 1920, Archives de Zoologie Experimentale Paris, V59; Chatton E., 1952, TRAITE ZOOL, P309; Dogel V.A., 1981, Zoologiya bespozvonochnykh: uchebnik dlya universitetov (Zoology of Invertebrates: Textbook for the Universities); DREBES G, 1984, HELGOLANDER MEERESUN, V37, P603; DREBES G, 1981, BRIT PHYCOL J, V16, P207, DOI 10.1080/00071618100650211; Drebes G., 1974, MARINE PHYTOPLANKTON; ELBRACHTER M, 1978, HELGOLAND WISS MEER, V31, P347, DOI 10.1007/BF02189487; ELBRACHTER M, 1988, JAHRESBER BIOL ANST, P130; Fensome R.A., 1993, Micropaleontology Press Special Paper; Jepps MW, 1937, Q J MICROSC SCI, V79, P589; JOHN AWG, 1983, BRIT PHYCOL J, V18, P61, DOI 10.1080/00071618300650071; Kiselev I.A., 1950, PANTSIRNYE ZHGUTIKON; Konovalova G.V, 1998, DINOFLAGELLYATY DINO; Ohtsuka Susumu, 2000, Bulletin of Plankton Society of Japan, V47, P1; Popovski J., 1990, SUSSWASSERFLORA MITT, V6, P243; SCHILLER J, 1933, RABENHORSTS KRYPTO 3, V10; Schtt F., 1895, ERG PLANKTON EXP, V4, P1, DOI [10.5962/bhl.title.2167, DOI 10.3390/IJERPH10105146]; Shields Jeffrey D., 1994, Annual Review of Fish Diseases, V4, P241, DOI 10.1016/0959-8030(94)90031-0; SHIPUNOV AB, 2002, SYSTEMA NATURAE ELEC, P13; SMAYDA TJ, 1992, NATURE, V358, P374, DOI 10.1038/358374a0; SOURNIA A., 1986, ATLAS PHYTOPLANCTON, VI; Taylor FJR, 2004, PHYCOL RES, V52, P308, DOI 10.1111/j.1440-1835.2004.tb00341.x	27	9	11	0	13	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1063-0740	1608-3377		RUSS J MAR BIOL+	Russ. J. Mar. Biol.	JAN	2008	34	1					28	37		10.1134/S1063074008010045	http://dx.doi.org/10.1134/S1063074008010045			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	309JK					2025-03-11	WOS:000256456300004
J	De Schepper, S; Head, MJ				De Schepper, Stijn; Head, Martin J.			Age calibration of dinoflagellate cyst and acritarch events in the Pliocene-Pleistocene of the eastern North Atlantic (DSDP Hole 610A)	STRATIGRAPHY			English	Article							EEMIAN HYDROGRAPHIC CONDITIONS; MID-PLIOCENE; BALTIC SEA; RETICULOFENESTRA; BIOSTRATIGRAPHY; INTENSIFICATION; EXTINCTION; BELGIUM; ISOTOPE; MIOCENE	An independently calibrated record of dinoflagellate cyst and acritarch events is presented for the Early Pliocene through Middle Pleistocene (ca. 4.0-0.5 Ma) of eastern North Atlantic Deep Sea Drilling Project (DSDP) Hole 610A. A new age model is established for this hole and tied to marine isotope stratigraphy and magnetostratigraphy back to 3.6 Ma. New data on the range of the calcareous nannofossil Reticulofenestra pseudoumbilicus indicate that the base of this hole is about 1.0 Myr younger than previously thought. A diverse dinoflagellate cyst and acritarch record allows the significant highest and/or lowest occurrences of 19 dinoflagellate cyst and seven acritarch taxa to be recognised in Hole 610A and calibrated to the latest astronomically-tuned Neogene time scale (ATNTS 2004) via our new age model. Comparing records across the North Atlantic and Mediterranean reveals near- synchronous highest occurrences of the dinoflagellate cysts Ataxiodinium confusum (2.63-2.65 Ma), Invertocysta lacrymosa (2.72-2.74 Ma in the eastern and central North Atlantic and Mediterranean) and Impagidinium solidum (ca. 3.15-3.17 Ma), and the acritarch Leiosphaeridia rockhallensis (ca. 3.83-3.88 Ma). Highest occurrences of the dinoflagellate cyst Batiacasphaera minuta/micropapillata (3.83-ca. 3.7 Ma) and acritarch Cymatiosphaera latisepta (2.49-2.63 Ma) also provide useful markers for correlation. A precise stratigraphy for Hole 610A allows us to evaluate the impact of paleoceanographic and climatic events on the dinoflagellate cyst record. Climatic and oceanographic reorganizations associated with the onset of Northern Hemisphere glaciation appear responsible for the disappearance of many species between 2.8 and 2.6 Ma. The lowest occurrence of Impagidinium cantabrigiense (1.86 Ma) in the Olduvai Subchron is one of the few good biostratigraphic markers for the uppermost Gelasian in Hole 610A.	[Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [De Schepper, Stijn] Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England	Brock University; University of Cambridge	De Schepper, S (通讯作者)，Univ Bremen, Fachbereich 5,Postfach 330 440, D-28334 Bremen, Germany.	smad2@cantab.net; mjhead@brocku.ca	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914				[Anonymous], NEOGENE QUATERNARY D; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P729; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; Barron John A., 1993, P155; Bartoli G, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001185; Bartoli G, 2005, EARTH PLANET SC LETT, V237, P33, DOI 10.1016/j.epsl.2005.06.020; Berggren W.A., 1985, The chronology of the geological record, V10, P211, DOI DOI 10.1144/GSLMEM.1985.010.01.18; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Chapman MR, 1997, PALAEOGEOGR PALAEOCL, V134, P109, DOI 10.1016/S0031-0182(97)00035-7; Chapman MR, 1998, MAR MICROPALEONTOL, V33, P203, DOI 10.1016/S0377-8398(97)00041-8; Clement B., 1989, P ODP SCI RESULTS, V105, P583; CLEMENT BM, 1987, INITIAL REP DEEP SEA, V94, P635; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; De Schepper S, 2008, J SYST PALAEONTOL, V6, P101, DOI 10.1017/S1477201907002167; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; DESCHEPPER S, 2006, THESIS U CAMBRIDGE C, V327, P6; DESCHEPPER S, GEOLOGICAL IN PRESS; DEVERNAL A, 1947, P OC DRILL PROGR SCI, V105, P401; DICKSON RR, 1987, INITIAL REP DEEP SEA, V94, P1061; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; ELLETT DJ, 1986, P ROY SOC EDINB B, V88, P61, DOI 10.1017/S0269727000004474; Fensome RA, 2004, CONTRIBUTIONS SERIES, V42; Gibbs SJ, 2005, PALAEOGEOGR PALAEOCL, V217, P155, DOI 10.1016/j.palaeo.2004.11.005; Hansen B, 2000, PROG OCEANOGR, V45, P109, DOI 10.1016/S0079-6611(99)00052-X; HARLAND R, 1948, DEEP SEA DRILLING PR, V48, P531; Hassold NJC, 2006, PALAEOGEOGR PALAEOCL, V236, P290, DOI 10.1016/j.palaeo.2005.11.011; Haug GH, 1998, NATURE, V393, P673, DOI 10.1038/31447; HEAD M. 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J	Sluijs, A; Brinkhuis, H; Schouten, S; Bohaty, SM; John, CM; Zachos, JC; Reichart, GJ; Damsté, JSS; Crouch, EM; Dickens, GR				Sluijs, Appy; Brinkhuis, Henk; Schouten, Stefan; Bohaty, Steven M.; John, Cedric M.; Zachos, James C.; Reichart, Gert-Jan; Damste, Jaap S. Sinninghe; Crouch, Erica M.; Dickens, Gerald R.			Environmental precursors to rapid light carbon injection at the Palaeocene/Eocene boundary	NATURE			English	Article							EOCENE THERMAL MAXIMUM; METHANE HYDRATE; LATE PALEOCENE; ISOTOPE EXCURSION; MEMBRANE-LIPIDS; TEMPERATURES; MARINE; OCEAN; GAS; DISSOCIATION	The start of the Palaeocene/Eocene thermal maximum - a period of exceptional global warming about 55 million years ago - is marked by a prominent negative carbon isotope excursion that reflects a massive input of C-13-depleted (`light') carbon to the ocean - atmosphere system(1). It is often assumed(2) that this carbon injection initiated the rapid increase in global surface temperatures and environmental change that characterize the climate perturbation(3-7), but the exact sequence of events remains uncertain. Here we present chemical and biotic records of environmental change across the Palaeocene/Eocene boundary from two sediment sections in New Jersey that have high sediment accumulation rates. We show that the onsets of environmental change ( as recorded by the abundant occurrence ('acme') of the dinoflagellate cyst Apectodinium) and of surface- ocean warming ( as evidenced by the palaeothermometer TEX86) preceded the light carbon injection by several thousand years. The onset of the Apectodinium acme also precedes the carbon isotope excursion in sections from the southwest Pacific Ocean(8) and the North Sea, indicating that the early onset of environmental change was not confined to the New Jersey shelf. The lag of similar to 3,000 years between the onset of warming in New Jersey shelf waters and the carbon isotope excursion is consistent with the hypothesis that bottom water warming caused the injection of C-13-depleted carbon by triggering the dissociation of submarine methane hydrates(1,9,10), but the cause of the early warming remains uncertain.	Univ Utrecht, Palaeobot & Palynol Lab, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; Netherlands Inst Sea Res, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Netherlands; Univ Calif Santa Cruz, Dept Earth Sci, Santa Cruz, CA 95060 USA; Rice Univ, Dept Earth Sci, Houston, TX 77005 USA	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of California System; University of California Santa Cruz; Rice University	Sluijs, A (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Inst Environm Biol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	A.Sluijs@uu.nl	Crouch, Erica/C-2820-2013; Dickens, Gerald/G-1222-2011; Brinkhuis, Henk/B-4223-2009; John, Cedric/B-3292-2008; Schouten, Stefan/P-4380-2016; Sluijs, Appy/B-3726-2009; Zachos, James/A-7674-2008; Sinninghe Damste, Jaap/F-6128-2011; Reichart, Gert-Jan/N-6308-2018	Sluijs, Appy/0000-0003-2382-0215; Brinkhuis, Henk/0000-0003-0253-6610; John, Cedric/0000-0001-9711-1548; Zachos, James/0000-0001-8439-1886; Sinninghe Damste, Jaap/0000-0002-8683-1854; Reichart, Gert-Jan/0000-0002-7256-2243; Dickens, Gerald/0000-0003-2869-4860				Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Cramer BS, 1999, B SOC GEOL FR, V170, P883; Cramer BS, 2005, PALAEOGEOGR PALAEOCL, V224, P144, DOI 10.1016/j.palaeo.2005.03.040; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; Dickens GR, 2003, EARTH PLANET SC LETT, V213, P169, DOI 10.1016/S0012-821X(03)00325-X; DICKENS GR, 1995, PALEOCEANOGRAPHY, V10, P965, DOI 10.1029/95PA02087; Higgins JA, 2006, EARTH PLANET SC LETT, V245, P523, DOI 10.1016/j.epsl.2006.03.009; KENNETT JP, 1991, NATURE, V353, P225, DOI 10.1038/353225a0; KOCH PL, 1992, NATURE, V358, P319, DOI 10.1038/358319a0; KVENVOLDEN KA, 1988, CHEM GEOL, V71, P41, DOI 10.1016/0009-2541(88)90104-0; Lourens LJ, 2005, NATURE, V435, P1083, DOI 10.1038/nature03814; MACDONALD GJ, 1990, CLIMATIC CHANGE, V16, P247, DOI 10.1007/BF00144504; Milkov AV, 2004, EARTH-SCI REV, V66, P183, DOI 10.1016/j.earscirev.2003.11.002; Pagani M, 2006, SCIENCE, V314, P1556, DOI 10.1126/science.1136110; Schouten S, 2003, GEOLOGY, V31, P1069, DOI 10.1130/G19876.1; Schouten S, 2002, EARTH PLANET SC LETT, V204, P265, DOI 10.1016/S0012-821X(02)00979-2; Sluijs A, 2007, DEEP-TIME PERSPECTIVES ON CLIMATE CHANGE: MARRYING THE SIGNAL FROM COMPUTER MODELS AND BIOLOGICAL PROXIES, P323; Sluijs A, 2006, NATURE, V441, P610, DOI 10.1038/nature04668; STOLL HM, 2005, PALEOCEANOGRAPHY, V20; Storey M, 2007, SCIENCE, V316, P587, DOI 10.1126/science.1135274; Svensen H, 2004, NATURE, V429, P542, DOI 10.1038/nature02566; Thomas DJ, 2002, GEOLOGY, V30, P1067, DOI 10.1130/0091-7613(2002)030<1067:WTFFTF>2.0.CO;2; Thomas E., 1996, Geological Society Special Publication, V101, P401, DOI 10.1144/GSL.SP.1996.101.01.20; Tripati A, 2005, SCIENCE, V308, P1894, DOI 10.1126/science.1109202; WUCHTER C, 2004, PALEOCEANOGRAPHY, V19; Xu WY, 2001, J GEOPHYS RES-SOL EA, V106, P26413, DOI 10.1029/2001JB000420; Zachos JC, 2006, GEOLOGY, V34, P737, DOI 10.1130/G22522.1; Zachos JC, 2007, PHILOS T R SOC A, V365, P1829, DOI 10.1098/rsta.2007.2045; Zachos JC, 2005, SCIENCE, V308, P1611, DOI 10.1126/science.1109004; Zachos JC, 2003, SCIENCE, V302, P1551, DOI 10.1126/science.1090110	30	275	314	2	94	NATURE PUBLISHING GROUP	LONDON	MACMILLAN BUILDING, 4 CRINAN ST, LONDON N1 9XW, ENGLAND	0028-0836			NATURE	Nature	DEC 20	2007	450	7173					1218	U5		10.1038/nature06400	http://dx.doi.org/10.1038/nature06400			5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	243HA	18097406				2025-03-11	WOS:000251786200047
J	Finkel, ZV; Sebbo, J; Feist-Burkhardt, S; Irwin, AJ; Katz, ME; Schofield, OME; Young, JR; Falkowski, PG				Finkel, Z. V.; Sebbo, J.; Feist-Burkhardt, S.; Irwin, A. J.; Katz, M. E.; Schofield, O. M. E.; Young, J. R.; Falkowski, P. G.			A universal driver of macroevolutionary change in the size of marine phytoplankton over the Cenozoic	PROCEEDINGS OF THE NATIONAL ACADEMY OF SCIENCES OF THE UNITED STATES OF AMERICA			English	Article						cell size; climate change; dinoflagellates; evolution; food webs	GROWTH-RATES; FOOD WEBS; BODY-SIZE; FEEDING-BEHAVIOR; EVOLUTION; PLANKTON; CLIMATE; ZOOPLANKTON; ASSEMBLAGES; DIATOMS	The size structure of phytoplankton assemblages strongly influences energy transfer through the food web and carbon cycling in the ocean. We determined the macroevolutionary trajectory in the median size of dinoflagellate cysts to compare with the macroevolutionary size change in other plankton groups. We found the median size of the dinoflagellate cysts generally decreases through the Cenozoic. Diatoms exhibit an extremely similar pattern in their median size over time, even though species diversity of the two groups has opposing trends, indicating that the macroevolutionary size change is an active response to selection pressure rather than a passive response to changes in diversity. The changes in the median size of dinoflagellate cysts are highly correlated with both deep ocean temperatures and the thermal gradient between the surface and deep waters, indicating the magnitude and frequency of nutrient availability may have acted as a selective factor in the macroevolution of cell size in the plankton. Our results suggest that climate, because it affects stratification in the ocean, is a universal abiotic driver that has been responsible for macroevolutionary changes in the size structure of marine planktonic communities over the past 65 million years of Earth's history.	[Finkel, Z. V.] Mt Allison Univ, Environm Sci Program, Sackville, NB E4L 1A7, Canada; [Irwin, A. J.] Mt Allison Univ, Dept Math & Comp Sci, Sackville, NB E4L 1A7, Canada; [Sebbo, J.; Schofield, O. M. E.; Falkowski, P. G.] Rutgers State Univ, Inst Marine & Coastal Sci, New Brunswick, NJ 08901 USA; [Feist-Burkhardt, S.; Young, J. R.] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Katz, M. E.; Falkowski, P. G.] Rutgers State Univ, Dept Earth & Planetary Sci, Piscataway, NJ 08854 USA; [Katz, M. E.] Rensselaer Polytech Inst, Troy, NY 12180 USA	Mount Allison University; Mount Allison University; Rutgers University System; Rutgers University New Brunswick; Natural History Museum London; Rutgers University System; Rutgers University New Brunswick; Rensselaer Polytechnic Institute	Finkel, ZV (通讯作者)，Mt Allison Univ, Environm Sci Program, Sackville, NB E4L 1A7, Canada.	zfinkel@mta.ca; falko@marine.rutgers.edu	Irwin, Andrew/B-2245-2008; Feist-Burkhardt, Susanne/B-1522-2009; Finkel, Zoe/B-9626-2008; Schofield, Oscar/H-4169-2018	Young, Jeremy/0000-0001-9320-9804; Irwin, Andrew/0000-0001-7784-2319; Finkel, Zoe/0000-0003-4212-3917; Schofield, Oscar/0000-0003-2359-4131; Feist-Burkhardt, Susanne/0000-0001-6019-6242				ANDERSON DM, 1985, J PHYCOL, V21, P200; [Anonymous], 1995, Publ. Society for Sedimentary Geology. III. 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Natl. Acad. Sci. U. S. A.	DEC 18	2007	104	51					20416	20420		10.1073/pnas.0709381104	http://dx.doi.org/10.1073/pnas.0709381104			5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	244SG	18077334	Green Published, Green Accepted			2025-03-11	WOS:000251885000048
J	Mayali, X; Franks, PJS; Azam, F				Mayali, Xavier; Franks, Peter J. S.; Azam, Farooq			Bacterial induction of temporary cyst formation by the dinoflagellate <i>Lingulodinium polyedrum</i>	AQUATIC MICROBIAL ECOLOGY			English	Article						ecdysis; cyst; bacteria; dinoflagellate; bloom; algicidal	ALGICIDAL BACTERIA; MARINE BACTERIUM; LIFE-HISTORY; DINOPHYCEAE; PHYTOPLANKTON; GROWTH; IDENTIFICATION; GYMNODINIUM; ENCYSTMENT; CELLS	We report the isolation of 3 novel bacterial strains from the Bacteroidetes group capable of inducing temporary cyst formation by ecdysis in the bloom-forming dinoflagellate Lingulodinium polyedrum. Phylogenetic analysis of 16S rRNA revealed that 2 of these strains are most closely related to previously identified algicidal bacteria, indicating potentially similar mechanisms of interaction. Long-term (2 wk) co-incubations of algae and bacteria under a 12:12 h light:dark cycle resulted in decreased algal cell abundances (compared to bacteria-free controls) followed by temporary cyst formation. Short-term incubations in continuous light resulted in no apparent effects of the bacteria over 2 d, but incubations in continuous darkness resulted in algal ecdysis after 24 h followed by significant decreases in total algal cell abundances after 52 h compared to controls without algicidal bacteria. We also showed that ecdysis resulted in the removal of bacteria attached to the surface of the algal cells, demonstrating a potentially direct benefit to the algae if the bacteria are harmful. We further suggest that negative interactions of bacteria on phytoplankton may be enhanced in the absence of light.	[Mayali, Xavier; Franks, Peter J. S.; Azam, Farooq] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA	University of California System; University of California San Diego; Scripps Institution of Oceanography	Mayali, X (通讯作者)，Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA.	xmayali@ucsd.edu	Mayali, Xavier/JBJ-2272-2023; Azam, Farooq/A-2306-2012	Mayali, Xavier/0000-0002-2170-0773				Adachi M, 2002, AQUAT MICROB ECOL, V26, P223, DOI 10.3354/ame026223; AMANN RI, 1995, MICROBIOL REV, V59, P143, DOI 10.1128/MMBR.59.1.143-169.1995; AZAM F, 1991, NATO ASI SERIES G, V27, P213; Azam F., 1984, Flows of energy and materials in marine ecosystems, P345, DOI 10.1007/978-1-4757-0387-0_14; Bernard L, 2000, AQUAT MICROB ECOL, V23, P1, DOI 10.3354/ame023001; Bidle KD, 1999, NATURE, V397, P508, DOI 10.1038/17351; BOWEN JD, 1993, LIMNOL OCEANOGR, V38, P36, DOI 10.4319/lo.1993.38.1.0036; Brussaard CPD, 1998, AQUAT MICROB ECOL, V14, P271, DOI 10.3354/ame014271; CARON DA, 1988, HYDROBIOLOGIA, V159, P27, DOI 10.1007/BF00007365; Cembella AD, 2003, PHYCOLOGIA, V42, P420, DOI 10.2216/i0031-8884-42-4-420.1; Doucette GJ, 1999, J PHYCOL, V35, P1447, DOI 10.1046/j.1529-8817.1999.3561447.x; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Fandino LB, 2001, AQUAT MICROB ECOL, V23, P119, DOI 10.3354/ame023119; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Ferrier M, 2002, J APPL MICROBIOL, V92, P706, DOI 10.1046/j.1365-2672.2002.01576.x; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Fistarol GO, 2004, ENVIRON MICROBIOL, V6, P791, DOI 10.1111/j.1462-2920.2004.00609.x; Franklin DJ, 2006, EUR J PHYCOL, V41, P1, DOI 10.1080/09670260500505433; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 2007, AQUAT MICROB ECOL, V46, P55, DOI 10.3354/ame046055; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Giovannoni S., 1991, NUCL ACID TECHNIQUES, P177; Guillard R. 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Microb. Ecol.	DEC 12	2007	50	1					51	62		10.3354/ame01143	http://dx.doi.org/10.3354/ame01143			12	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	252WR		Bronze			2025-03-11	WOS:000252478500005
J	Esper, O; Zonneveld, KAF				Esper, Oliver; Zonneveld, Karin A. F.			The potential of organic-walled dinoflagellate cysts for the reconstruction of past sea-surface conditions in the Southern Ocean	MARINE MICROPALEONTOLOGY			English	Article						Southern Ocean; Modern Analogue Technique; palaeotemperatures; Late Quaternary; dinoflagellates	EASTERN ATLANTIC SECTOR; NORTHERN NORTH-ATLANTIC; LAST GLACIAL MAXIMUM; THERMOHALINE CIRCULATION; FALKLAND TROUGH; INDIAN SECTOR; ICE EXTENT; SEDIMENTS; TEMPERATURES; ASSEMBLAGES	In this study we investigate the potential of organic-walled dinoflagellate cysts (dinocysts) as tools for quantifying past sea-surface temperatures (SST) in the Southern Ocean. For this purpose, a dinocyst reference dataset has been formed, based on 138 surface sediment samples from different circum-Antarctic environments. The dinocyst assemblages of these samples are composed of phototrophic (gonyaulacoid) and heterotrophic (protoperidinioid) species that provide a broad spectrum of palaeoenvironmental information. The relationship between the environmental parameters in the upper water column and the dinocyst distribution patterns of individual species has been established using the statistical method of Canonical Correspondence Analysis (CCA). Among the variables tested, summer SST appeared to correspond to the maximum variance represented in the dataset. To establish quantitative summer SST reconstructions, a Modem Analogue Technique (MAT) has been performed on data from three Late Quaternary dinocyst records recovered from locations adjacent to prominent oceanic fronts in the Atlantic sector of the Southern Ocean. These dinocyst time series exhibit periodic changes in the dinocyst assemblage during the last two glacial/ interglacial-cycles. During glacial conditions the relative abundance of protoperidinioid cysts was highest, whereas interglacial conditions are characterised by generally lower cyst concentrations and increased relative abundance of gonyaulacoid cysts. The MAT palaeotemperature estimates show trends in summer SST changes following the global oxygen isotope signal and a strong correlation with past temperatures of the last 140 000 years based on other proxies. However, by comparing the dinocyst results to quantitative estimates of summer SSTs based on diatoms, radiolarians and foraminifer-derived stable isotope records it can be shown that in several core intervals the dinocyst-based summer SSTs appeared to be extremely high. In these intervals the dinocyst record seems to be highly influenced by selective degradation, leading to unusual temperature ranges and to unrealistic palaeotemperatures. We used the selective degradation index (kt-index) to determine those intervals that have been biased by selective degradation in order to correct the palaeotemperature estimates. We show that after correction the dinocyst based SSTs correspond reasonably well with other palaeotemperature estimates for this region, supporting the great potential of dinoflagellate cysts as a basis for quantitative palaeoenvironmental studies. (c) 2007 Elsevier B.V. All rights reserved.	[Esper, Oliver] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany; [Zonneveld, Karin A. F.] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Bremen	Esper, O (通讯作者)，Alfred Wegener Inst Polar & Marine Res, PF 120161, D-27515 Bremerhaven, Germany.	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TERBRAAK CJF, 1998, CANOCO, V4; Versteegh GJM, 2004, PHYCOL RES, V52, P325, DOI 10.1111/j.1440-1835.2004.tb00342.x; Versteegh GJM, 2002, GEOLOGY, V30, P615, DOI 10.1130/0091-7613(2002)030<0615:UOSDTS>2.0.CO;2; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817; Zielinski U, 1998, PALEOCEANOGRAPHY, V13, P365, DOI 10.1029/98PA01320; Zielinski U, 1997, PALAEOGEOGR PALAEOCL, V129, P213, DOI 10.1016/S0031-0182(96)00130-7; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1; Zonneveld KAF, 2007, MAR GEOL, V237, P109, DOI 10.1016/j.margeo.2006.10.023	76	45	47	0	11	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	DEC 5	2007	65	3-4					185	212		10.1016/j.marmicro.2007.07.002	http://dx.doi.org/10.1016/j.marmicro.2007.07.002			28	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	243GH					2025-03-11	WOS:000251783000004
J	Hasegawa, Y; Martin, JL; Giewat, MW; Rooney-Varga, JN				Hasegawa, Yuko; Martin, Jennifer L.; Giewat, Michael W.; Rooney-Varga, Juliette N.			Microbial community diversity in the phycosphere of natural populations of the toxic alga, <i>Alexandrium fundyense</i>	ENVIRONMENTAL MICROBIOLOGY			English	Article							CYST FORMATION; HIROSHIMA BAY; PHYLOGENETIC DIVERSITY; SEQUENCE-ANALYSIS; NORTH-ATLANTIC; MARINE WATERS; WESTERN GULF; BACTERIA; BLOOM; DIMETHYLSULFONIOPROPIONATE	The dinoflagellate Alexandrium fundyense is the major causative organism of paralytic shellfish poisoning in the Gulf of Maine. While laboratory studies have shown that A. fundyense population dynamics can be affected dramatically by co-occurring bacteria, little is known about these interactions in nature. Because A. fundyense is typically a minor Gulf of Maine phytoplankton community member, analyses of the bulk community cannot be used to address bacterium-A. fundyense associations. Therefore, an immunomagnetic bead method was used to selectively capture A. fundyense cells, and the bacteria attached to them, from complex natural samples. Bulk particle-associated and free-living bacterial communities were collected simultaneously. DNA was extracted from all sample types and subjected to 16S rRNA gene fragment amplification, denaturing gradient gel electrophoresis (DGGE) and sequence analysis. Ordination analysis of DGGE profiles confirmed that A. fundyense-associated bacteria community profiles were distinct from bulk bacterial community profiles, indicating selection of specific phylotypes in the A. fundyense phycosphere. Phylogenetic analyses confirmed that Alexandrium-associates were distinct from bulk particle-associated bacteria and that they included a greater prevalence and broader diversity of Gammaproteobacteria than previously thought to be associated with toxic algae. Phylogenetic groups known to be associated with dinoflagellates were also found, including members of the families Alteromonadaceae, Pseudoalteromonadaceae, Rhodobacteraceae and Flavobacteraceae.	Univ Massachusetts, Lowell, MA 01854 USA; Fisheries & Oceans Canada, St Andrews, NB, Canada	University of Massachusetts System; University of Massachusetts Lowell; Fisheries & Oceans Canada	Rooney-Varga, JN (通讯作者)，Univ Massachusetts, Lowell, MA 01854 USA.	Juliette_RooneyVarga@uml.edu	Martin, Jennifer/G-5217-2011	Rooney-Varga, Juliette/0000-0001-7102-6919; Hasegawa, Yuko/0000-0002-1328-276X				Adachi M, 2003, APPL ENVIRON MICROB, V69, P6560, DOI 10.1128/AEM.69.11.6560-6568.2003; Adachi M, 2002, AQUAT MICROB ECOL, V26, P223, DOI 10.3354/ame026223; Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Aguilera A, 1996, MAR ECOL PROG SER, V143, P255, DOI 10.3354/meps143255; ALTSCHUL SF, 1990, J MOL BIOL, V215, P403, DOI 10.1016/S0022-2836(05)80360-2; AMANN RI, 1990, APPL ENVIRON MICROB, V56, P1919, DOI 10.1128/AEM.56.6.1919-1925.1990; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; [Anonymous], FISH BOARD RES CAN; Buchan A, 2000, APPL ENVIRON MICROB, V66, P4662, DOI 10.1128/AEM.66.11.4662-4672.2000; Cole JR, 2007, NUCLEIC ACIDS RES, V35, pD169, DOI 10.1093/nar/gkl889; Dang HY, 2002, APPL ENVIRON MICROB, V68, P496, DOI 10.1128/AEM.68.2.496-504.2002; Dang HY, 2000, APPL ENVIRON MICROB, V66, P467, DOI 10.1128/AEM.66.2.467-475.2000; DELONG EF, 1993, LIMNOL OCEANOGR, V38, P924, DOI 10.4319/lo.1993.38.5.0924; Doucette G.J., 1998, PHYSL ECOLOGY HARMFU, P619; Fandino LB, 2001, AQUAT MICROB ECOL, V23, P119, DOI 10.3354/ame023119; Ferrier M, 2002, J APPL MICROBIOL, V92, P706, DOI 10.1046/j.1365-2672.2002.01576.x; González JM, 1999, APPL ENVIRON MICROB, V65, P3810; Green DH, 2004, FEMS MICROBIOL ECOL, V47, P345, DOI 10.1016/S0168-6496(03)00298-8; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hold GL, 2001, FEMS MICROBIOL ECOL, V37, P161, DOI 10.1111/j.1574-6941.2001.tb00864.x; Hold GL, 2001, FEMS MICROBIOL ECOL, V36, P223, DOI 10.1111/j.1574-6941.2001.tb00843.x; IMAI I, 1993, MAR BIOL, V116, P527, DOI 10.1007/BF00355470; JAMIESON GS, 1983, CAN J FISH AQUAT SCI, V40, P313, DOI 10.1139/f83-046; Jasti S, 2005, APPL ENVIRON MICROB, V71, P3483, DOI 10.1128/AEM.71.7.3483-3494.2005; Kiene RP, 1999, APPL ENVIRON MICROB, V65, P4549; LANE DJ, 1985, P NATL ACAD SCI USA, V82, P6955, DOI 10.1073/pnas.82.20.6955; Liao WR, 2003, J IND MICROBIOL BIOT, V30, P433, DOI 10.1007/s10295-003-0068-7; Love RC, 2005, DEEP-SEA RES PT II, V52, P2450, DOI 10.1016/j.dsr2.2005.06.030; Lovejoy C, 1998, APPL ENVIRON MICROB, V64, P2806; Ludwig W, 2004, NUCLEIC ACIDS RES, V32, P1363, DOI 10.1093/nar/gkh293; Malin G, 1997, J PHYCOL, V33, P889, DOI 10.1111/j.0022-3646.1997.00889.x; Malmstrom RR, 2004, LIMNOL OCEANOGR, V49, P597, DOI 10.4319/lo.2004.49.2.0597; Martin J. 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Microbiol.	DEC	2007	9	12					3108	3121		10.1111/j.1462-2920.2007.01421.x	http://dx.doi.org/10.1111/j.1462-2920.2007.01421.x			14	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	228VS	17991038				2025-03-11	WOS:000250761300018
J	Prasad, V; Garg, R; Singh, V; Thakur, B				Prasad, Vandana; Garg, Rahul; Singh, Vartika; Thakur, Biswajit			Organic matter distribution pattern in Arabian Sea: Palynofacies analysis from the surface sediments off Karwar coast (west coast of India)	INDIAN JOURNAL OF MARINE SCIENCES			English	Article						palynofacies; primary productivity; oxygen minima zone; Karwar coast; Arabian Sea; west coast of India; organic matter; sediments; amorphous organic matter	CARBON	Central Arabian Sea region, situated off the Karwar coast, is characterized by intense mid depth (similar to 120-1200 m) oxygen minima zone and shows preservation and accumulation of relatively high organic matter content. Palynofacies analysis was carried out with a view to understand the organic matter production, preservation and degradation in the surface sediments of Arabian Sea from 15 m-2750 m depth-off Karwar [14.47-14.40 degrees N -70.77-74.25 degrees E transect]. Palynofacies analysis, which involves qualitative and quantitative estimation of terrestrial and marine organic matter is a useful tool to decipher and assess paleoenvironmental changes in various water depth zones from shelf-slope region off the Karwar coast. There is a marked change in the palynofacies characteristics of the organic matter recovered from various depth zones. High SW monsoonal activity over Karwar coast results in increased runoff and nutrient loading in the coastal waters. This enhances primary productivity in the inner shelf region. Organic walled dinoflagellate cysts as important constituent of primary productivity, predominate under such conditions, being converted into Amorphous organic matter (AOM) as a result of degradation under low oxygen environment. Hence, in the present study high AOM is used as proxy for the low oxygen content at sediment-water interface. It also provides evidence of high primary productivity in the photic zone. Study further reveals that terrestrially derived charcoal and woody plant tissue resistant to degradation, are transported to continental slope regions at greater depths. Occurrence of a large proportion of well preserved labile organic matter (exoskeleton fragments of planktonic crustaceans) and AOM in the mid-outer slope surface sediments indicate enhanced primary productivity and high rate of burial efficiency making these areas, characteristic of low oxygen. The study shows that the Karwar coast margin is highly productive as a result of runoff related nutrient loading and is the primary cause for oxygen minima conditions.	[Prasad, Vandana; Garg, Rahul; Singh, Vartika; Thakur, Biswajit] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Prasad, V (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	vanprasad@yahoo.co.uk	PRASAD, VANDANA/KUF-4093-2024					[Anonymous], 1984, MARINE GEOLOGY OCEAN; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1982, J. Micropal., V1, P107; Emerson S, 1988, PALEOCEANOGRAPHY, V3, P621, DOI 10.1029/PA003i005p00621; HENRICHS SM, 1987, GEOMICROBIOL J, V5, P191, DOI 10.1080/01490458709385971; Inthorn M, 2006, GEOLOGY, V34, P205, DOI 10.1130/G22153.1; Mishra AK, 2004, CURR SCI INDIA, V87, P475; MURTHY MR, 1987, GEOL SURV PUB ARABIA, V24, P173; MURTY PSN, 1969, P NAT I SC IND, V35, P385; NAQVI SWA, 1987, J MAR RES, V45, P1049, DOI 10.1357/002224087788327118; PAROPKARI AL, 1992, MAR GEOL, V107, P213, DOI 10.1016/0025-3227(92)90168-H; Roncaglia L, 2004, MAR MICROPALEONTOL, V50, P21, DOI 10.1016/S0377-8398(03)00065-3; Roncaglia L, 2006, FACIES, V52, P19, DOI 10.1007/s10347-005-0028-y; RYTHER JH, 1965, DEEP SEA RES OCEANOG, V12, P91; Schulte S, 1999, EARTH PLANET SC LETT, V173, P205, DOI 10.1016/S0012-821X(99)00232-0; STEFFEN D, 1993, B CENT RECH EXPL, V17, P235; THIEDE J, 1977, EARTH PLANET SC LETT, V33, P301, DOI 10.1016/0012-821X(77)90082-6; Traverse A., 2005, SEDIMENTATION ORGANI, P544; Tyson RV, 2000, GEOLOGY, V28, P569, DOI 10.1130/0091-7613(2000)28<569:PPODFS>2.0.CO;2; Tyson RV., 1995, SEDIMENTARY ORGANIC, P615, DOI [DOI 10.1007/978-94-011-0739-6, 10.1007/978-94-011-0739-6]; VANWAVEREN I, 1994, PALAEOGEOGR PALAEOCL, V112, P85, DOI 10.1016/0031-0182(94)90135-X; WHELAN JK, 1992, PRODUCTIVITY ACCUMUL, P533; WISEMAN JDH, 1940, J M EXPEDITION, P3; WYRTKI K, 1971, P531	24	11	11	0	7	NATL INST SCIENCE COMMUNICATION-NISCAIR	NEW DELHI	DR K S KRISHNAN MARG, PUSA CAMPUS, NEW DELHI 110 012, INDIA	0379-5136	0975-1033		INDIAN J MAR SCI	Indian J. Mar. Sci.	DEC	2007	36	4					399	406						8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	265LD					2025-03-11	WOS:000253359500015
J	Leroy, SAG; Marret, F; Gibert, E; Chalié, F; Reyss, JL; Arpe, K				Leroy, S. A. G.; Marret, F.; Gibert, E.; Chalie, F.; Reyss, J. -L.; Arpe, K.			River inflow and salinity changes in the Caspian Sea during the last 5500 years	QUATERNARY SCIENCE REVIEWS			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; BLACK-SEA; ARAL SEA; MARINE-SEDIMENTS; STABLE-ISOTOPE; LEVEL CHANGES; MARMARA SEA; HOLOCENE; POLLEN; LAKE	Pollen, spores and dinoflagellate cysts have been analysed on three sediment cores (1.8-1.4m-long) taken from the south and middle basins of the Caspian Sea. A chronology available for one of the cores is based on calibrated radiocarbon dates (ca 5.5-0.8 cal. ka BP). The pollen and spores assemblages indicate fluctuations between steppe and desert. In addition there are some outstanding zones with a bias introduced by strong river inflow. The dinocyst assemblages change between slightly brackish (abundance of Pyxidinopsis psilata and Spiniferites cruciformis) and more brackish (dominance of Impagidinium caspienense) conditions. During the second part of the Holocene, important flow modifications of the Uzboy River and the Volga River as well as salinity changes of the Caspian Sea, causing sea-level fluctuations, have been reconstructed. A major change is suggested at ca 4 cal. ka BP with the end of a high level phase in the south basin. Amongst other hypotheses, this could be caused by the end of a late and abundant flow of the Uzboy River (now defunct), carrying to the Caspian Sea either meltwater from higher latitudes or water from the Amu-Daria. A similar, later clear phase of water inflow has also been observed from 2.1 to 1.7 cal. ka BP in the south basin and probably also in the north of the middle basin. (c) 2007 Elsevier Ltd. All rights reserved.	Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Marret, F.] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Gibert, E.] Univ Paris 11, CNRS, UPS, UMR8148 IDES, F-91405 Orsay, France; [Chalie, F.] CNRS UPCAM, UMR 6635, CEREGE, IRD, F-13545 Aix En Provence, France; [Reyss, J. -L.] CEA, CNRS, Lab Sci Climat Environm, F-91198 Gif Sur Yvette, France; [Arpe, K.] Max Planck Inst Meteorol, Hamburg, Germany	Brunel University; University of Liverpool; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; Universite de Toulouse; Universite Toulouse III - Paul Sabatier; Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CEA; Max Planck Society	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk; 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Sci. Rev.	DEC	2007	26	25-28					3359	3383		10.1016/j.quascirev.2007.09.012	http://dx.doi.org/10.1016/j.quascirev.2007.09.012			25	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	256UT					2025-03-11	WOS:000252756100027
J	Stock, CA; McGillicuddy, DJ; Anderson, DM; Solow, AR; Signell, RP				Stock, Charles A.; McGillicuddy, Dennis J., Jr.; Anderson, Donald M.; Solow, Andrew R.; Signell, Richard P.			Blooms of the toxic dinoflagellate <i>Alexandrium fundyense</i> in the western Gulf of Maine in 1993 and 1994:: A comparative modeling study	CONTINENTAL SHELF RESEARCH			English	Article						red tides; algal blooms; harmful algal blooms; modeling; paralytic shellfish poisoning	GONYAULAX-TAMARENSIS; MARINE-PHYTOPLANKTON; COASTAL CURRENT; INTERANNUAL VARIABILITY; GROWTH; CIRCULATION; TRANSPORT; SALINITY; DYNAMICS; OCEAN	Blooms of the toxic dinoflagellate Alexandrium fundyense commonly occur in the western Gulf of Maine but the amount of toxin observed in coastal shellfish is highly variable. In this study, a coupled physical-biological model is used to investigate the dynamics underlying the observed A. fundyense abundance and shellfish toxicity in 1993 (a high toxicity year) and 1994 (low toxicity year). The physical model simulates the spring circulation, while the biological model estimates the germination and population dynamics of A. fundyense based on laboratory and field data. The model captures the large-scale aspects of the initiation and development of A. fundyense blooms during both years, but small-scale patchiness and the dynamics of bloom termination remain problematic. In both cases, the germination of resting cysts accounts for the magnitude of A. fundyense populations early in the spring. Simulations with low net A. fundyense growth rates capture the mean observed concentration during the bloom peak, which is of similar magnitude during both years. There is little evidence that large-scale changes in biological dynamics between 1993 and 1994 were a primary driver of the differences in shellfish toxicity. Results instead suggest that the persistent southwesterly flow of the western Maine Coastal Current led to A. fundyense populations of similar alongshore extent by late May of both years. This period coincides with peak cell abundance in the region. Variations in wind forcing (downwelling favorable in 1993, upwelling favorable in 1994) and subsequent cell transport (inshore in 1993, offshore in 1994) in early June then provides a plausible explanation for the dramatic mid-June differences in shellfish toxicity throughout the western Gulf of Maine. (c) 2007 Elsevier Ltd. All rights reserved.	Woods Hole Oceanog Inst, Woods Hole, MA 02540 USA; Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; US Geol Survey, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; United States Department of the Interior; United States Geological Survey	Stock, CA (通讯作者)，Princeton Univ Forrestal Campus, NOAA, Geophys Fluid Dynam Lab, 201 Forrestal Rd, Princeton, NJ 08540 USA.	cstock@alum.mit.edu; dmcgillicuddy@whoi.edu; danderson@whoi.edu; asolow@whoi.edu; rsignell@usgs.gov	Stock, Charles/H-1281-2012	McGillicuddy, Dennis/0000-0002-1437-2425; Stock, Charles/0000-0001-9549-8013; Signell, Richard/0000-0003-0682-9613				Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; [Anonymous], MEMOIRES SOC ROYALE, DOI DOI 10.1093/plankt/fbi019; BAUERFEIND E, 1986, MAR BIOL, V93, P323, DOI 10.1007/BF00401099; Bigelow H.B., 1927, FISH B-NOAA, V40, P511; Blumberg A.F., 1987, Three Dimensional Ocean Models, P1; BROOKS DA, 1985, J GEOPHYS RES-OCEANS, V90, P4687, DOI 10.1029/JC090iC03p04687; CARPENTER E J, 1971, Ecology (Washington D C), V52, P183, DOI 10.2307/1934753; Chai F, 2002, DEEP-SEA RES PT II, V49, P2713, DOI 10.1016/S0967-0645(02)00055-3; Denman KL, 1999, DEEP-SEA RES PT II, V46, P2877, DOI 10.1016/S0967-0645(99)00087-9; DROOP MR, 1983, BOT MAR, V26, P99, DOI 10.1515/botm.1983.26.3.99; EPPLEY RW, 1969, LIMNOL OCEANOGR, V14, P912, DOI 10.4319/lo.1969.14.6.0912; EPPLEY RW, 1969, J PHYCOL, V5, P365; Etheridge SM, 2005, DEEP-SEA RES PT II, V52, P2491, DOI 10.1016/j.dsr2.2005.06.026; Fong DA, 1997, J MARINE SYST, V12, P69, DOI 10.1016/S0924-7963(96)00089-9; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; FUNG IY, 1984, REV GEOPHYS, V22, P177, DOI 10.1029/RG022i002p00177; Garside C, 1996, ESTUAR COAST SHELF S, V42, P617, DOI 10.1006/ecss.1996.0040; Geyer W.R., 1992, Physical Oceanographic Invertigation of Massachusetts and Cape Cod Bays; Geyer WR, 2004, CONT SHELF RES, V24, P1339, DOI 10.1016/j.csr.2004.04.001; KAMYKOWSKI D, 1992, MAR BIOL, V113, P319; Keafer BA, 2005, DEEP-SEA RES PT II, V52, P2674, DOI 10.1016/j.dsr2.2005.06.016; Kelly JR, 1997, MAR ECOL PROG SER, V148, P155, DOI 10.3354/meps148155; KUHL M, 1994, LIMNOL OCEANOGR, V39, P1368; LANGDON C, 1987, J PLANKTON RES, V9, P459, DOI 10.1093/plankt/9.3.459; Large W.G., 1981, J PHYS OCEANOGR, V11, P329; LARGE WG, 1982, J PHYS OCEANOGR, V12, P464, DOI 10.1175/1520-0485(1982)012<0464:SALHFM>2.0.CO;2; Liebig J., 1845, Chemistry and its Applications to Agriculture and Physiology; Lomas MW, 2000, J PHYCOL, V36, P903, DOI 10.1046/j.1529-8817.2000.99029.x; Luerssen RM, 2005, DEEP-SEA RES PT II, V52, P2656, DOI 10.1016/j.dsr2.2005.06.025; Luettich R. 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J	Bernaola, G; Monechi, S				Bernaola, Gilen; Monechi, Simonetta			Calcareous nannofossil extinction and survivorship across the Cretaceous-Paleogene boundary at Walvis Ridge (ODP Hole 1262C, South Atlantic Ocean)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	Symposium on Mass Extinctions and Other Large Ecosystem Perturbations/K/T Boundary Events held at the 32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			calcareous nannofossils; Cretaceous/Paleogene boundary; Walvis Ridge; extinction; paleoecology	TERTIARY BOUNDARY; K/T BOUNDARY; NANNOPLANKTON PRODUCTIVITY; END; BIOSTRATIGRAPHY; GEULHEMMERBERG; COCCOSPHERES; TRANSITION; SUCCESSION; SEQUENCES	Site 1262 in the South Atlantic Ocean has provided a stratigraphically continuous deep Cretaceous/Paleogene boundary sequence. High resolution calcareous nannofossil quantitative analyses were carried out across the K/P boundary, and provided a remarkable record of the abrupt and catastrophic extinction. The calcareous nannofossil assemblages are abundant and well preserved allowing to obtain a precise bioevent sequence and to document in detail the survivors and victims and the subsequent recovery across the K/P boundary. Late Maastrichtian diversity and absolute abundance is high and no decrease towards the boundary has been observed. The relative abundance of Cretaceous species does not suffer important changes during the latest Maastrichtian. However, the increase in abundance of cool-water taxa, paralleled with a decrease of warm water taxa in the uppermost 2 cm of the Maastrichtian, revealed a pulse of surface water cooling. The K/P boundary is marked by an important decrease in calcareous nannofossil absolute abundance, the increase of Cretaceous-persistent species such as Cyclagelosphaera reinhardtii together with the dinoflagellate cysts of Thoracosphaera operculata and the appearance of the new-Paleocene taxa Cyclagelosphaera alta and Biantholithus sparsus. These events are followed by the successive relative abundance increases of other Cretaceous survivors as Zeugrhabdotus sigmoides, Markalius inversus and Biscutum recognized as r-selected taxa, adapted to eutrophic and cold water environments. In the early Danian several first occurrences of small new-Paleocene species have been observed: calcareous nannoplankton evolutionary attempts to colonize vacant niches left by the extinct Cretaceous species. Only some forms succeed and become ancestors to the Cenozoic assemblages-the other disappear in few kiloyear. The presence of a reworking/mixing interval above the K/P boundary hampered to unequivocally interpret if the few Cretaceous-vanishing taxa may have survived for a very short time after the K/P extinction. (c) 2007 Elsevier B.V. All rights reserved.	Univ Basque Country, Dept Estratigrafia & Paleontol, E-48080 Bilbao, Spain; Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy	University of Basque Country; University of Florence	Bernaola, G (通讯作者)，Univ Basque Country, Dept Estratigrafia & Paleontol, Apt 644, E-48080 Bilbao, Spain.	gilen.bernaola@ehu.es; monechi@unifi.it	Bernaola, Gilen/AAA-6959-2019; monechi, simonetta/AAN-6148-2020	BERNAOLA BILBAO, GILEN/0000-0003-1095-0854				Aguado Roque, 2005, Journal of Iberian Geology, V31, P9; ALCALAHERRERA JA, 1992, MAR MICROPALEONTOL, V20, P77, DOI 10.1016/0377-8398(92)90010-H; ALCALAHERRERA JA, 1990, ABSTR PROG GEOL SOC, V22, P279; ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; ALVAREZ W, 1984, SCIENCE, V223, P1183, DOI 10.1126/science.223.4641.1183; [Anonymous], 1980, CRETACEOUS RES; [Anonymous], REV ESPANOLA PALEONT; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], SEPM SPECIAL PUBLICA; [Anonymous], P ODP SCI RES; BERNAOLA G, 2002, THESIS U PAIS VASCO; Bown P, 2005, GEOLOGY, V33, P653, DOI 10.1130/G21566.1; Bown P.R., 1998, BRIT MICROPALAEONTOL; Burnett J.A., 1998, P132; CARATINI C, 1960, THESIS U ALGER; CLEMENS WA, 1981, PALEOBIOLOGY, V7, P293, DOI 10.1017/S0094837300004589; COURTILLOT V, 1988, NATURE, V333, P843, DOI 10.1038/333843a0; EHRENDORFER T, 1992, SCI RESULTS P OCEA 2, V120, P451; Erba E., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V129, P189; ESHET Y, 1992, MAR MICROPALEONTOL, V18, P199, DOI 10.1016/0377-8398(92)90013-A; Eshet Y, 1996, MAR MICROPALEONTOL, V29, P37, DOI 10.1016/0377-8398(96)00006-0; Gardin S, 2002, PALAEOGEOGR PALAEOCL, V178, P211, DOI 10.1016/S0031-0182(01)00397-2; Gardin S, 1998, B SOC GEOL FR, V169, P709; Gartner S., 1996, P27; GARTNER S, 1994, NEW DEV REG K T EV O, V825, P40; Gorostidi A., 1991, Revista Espanola de Paleontologia, V6, P89; Gorostidi Amalia, 1995, Revista Espanola de Paleontologia, P153; Grun W., 1975, Eclogae Geologicae Helvetiae, V68, P147; HALLAM A, 1990, TECTONOPHYSICS, V171, P347, DOI 10.1016/0040-1951(90)90109-L; HALLAM A, 1987, SCIENCE, V238, P1237, DOI 10.1126/science.238.4831.1237; HARRIES PJ, 1995, BIOTIC REC AFTER EXT, V102, P41; HAY WILLIAM W., 1967, J PALEONTOL, V41, P1505; Henriksson AS, 1996, CRETACEOUS RES, V17, P451, DOI 10.1006/cres.1996.0028; JIANG MJ, 1986, MICROPALEONTOLOGY, V32, P232, DOI 10.2307/1485619; Keller G, 2004, METEORIT PLANET SCI, V39, P1127, DOI 10.1111/j.1945-5100.2004.tb01133.x; KILHAM P, 1980, STUDIES ECOLOGY, V7, P493; Lamolda MA, 2005, PALAEOGEOGR PALAEOCL, V224, P27, DOI 10.1016/j.palaeo.2005.03.030; Lees JA, 2002, CRETACEOUS RES, V23, P537, DOI 10.1006/cres.2003.1021; MAGARITZ M, 1985, NEWSL STRATIGR, V15, P100; Mai H, 1999, MAR MICROPALEONTOL, V36, P1, DOI 10.1016/S0377-8398(98)00023-1; Mai H, 1997, MICROPALEONTOLOGY, V43, P281, DOI 10.2307/1485829; Mai H, 2003, MICROPALEONTOLOGY, V49, P189, DOI 10.2113/49.2.189; MCLEAN DM, 1985, CRETACEOUS RES, V6, P235, DOI 10.1016/0195-6671(85)90048-5; MCLEAN DM, 1982, SYLLOGEUS, V39, P143; Minoletti F, 2005, PALAEOGEOGR PALAEOCL, V216, P119, DOI 10.1016/j.palaeo.2004.10.006; MONECHI S, 1985, INITIAL REP DEEP SEA, V86, P787; MONECHI S, UNPUB HIGH STRESS PA; MOORE TC, 1984, INITIAL REP DEEP SEA, V74, P873; Mortimer C.P., 1987, Abhandlungen der Geologischen Bundesanstalt (Vienna), V39, P143; Mutterlose J., 1996, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V77, P291; OFFICER CB, 1983, SCIENCE, V219, P1383, DOI 10.1126/science.219.4591.1383; OFFICER CB, 1985, SCIENCE, V227, P1161, DOI 10.1126/science.227.4691.1161; OFFICER CB, 1987, NATURE, V326, P143, DOI 10.1038/326143a0; OKADA H, 1980, MAR MICROPALEONTOL, V5, P1; Perch-Nielsen K., 1979, INTERNATIONAL UNION OF GEOLOGICAL SCIENCES SERIES A, V6, P223; PERCH-NIELSEN K, 1973, Bulletin of the Geological Society of Denmark, V22, P306; Perch-Nielsen K., 1979, P120; Perch-Nielsen K., 1985, P329; Perch-Nielsen K., 1969, B GEOL SOC DENMARK, V19, P51; Perch-Nielsen K., 1981, CAH MICROPALEONTOL, V3, P25; Perch-Nielsen K.J. 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Paleoclimatol. Paleoecol.	NOV 2	2007	255	1-2					132	156		10.1016/j.palaeo.2007.02.045	http://dx.doi.org/10.1016/j.palaeo.2007.02.045			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	230TH					2025-03-11	WOS:000250898300010
J	Gu, HF; Wang, Y				Gu Hai-Feng; Wang Yan			The first record of <i>Ensiculifera</i> Balech and <i>Fragilidium</i> Balech (Dinophyceae) from Chinese coast	ACTA PHYTOTAXONOMICA SINICA			Chinese	Article						Ensiculifera; Fragilidium; Fragilidium mexicanum; dinoflagellate; cyst; China sea	DINOFLAGELLATE CYSTS; SEDIMENTS; CALCIODINELLOIDEAE; STRATEGIES; PHYLOGENY; GENERA	Resting cysts and vegetative cells of Ensiculifera Balech and Fragilidium Balech have never been reported in China Sea. Such kinds of cysts were collected in the East China Sea and were allowed to germinate. The cyst of Ensiculifera sp. is spherical with a diameter of 22 mu m. The cyst consists of two layers and is full of greenish granules, with a bright red body inside. The cyst wall is covered with short organic spines (2 mu m long). The cell of Ensiculifera sp. comprises a conical epitheca and a rounded hypotheca, with the dimension of 17.7 mu m long and 12.5 mu m wide on the average. The plate pattern is po, x, 4', 3a, 7 '', 5c, 4s, 5'''P, 2''''. The cysts of Fragilidium mexicanum Balech are spherical with the diameter ranging from 54-60 mu m. They are full of pale white granules and brown protoplasm, with a bright yellow body present. The archeopyle is spherical. The cells of F mexicanum are 45.3 mu m long and 42.8 mu m wide, with the plate formula of po, 5', 7 '', 10c, 7s, 7''' 2'''', 1P. The cyst of Fragilidium sp. is also spherical with a diameter of 45 mu m, which is similar to that of F. mexicanum except that the yellow body is not present. The cells of Fragilidium sp. are 41.6 pin long and 35.3 mu m wide with the plate formula of po, 5', 7 '', 7''', 2'''', 1P. The Internal Transcribed Spacers (ITS) of Ensiculifera sp. and the small subunit (18S) rDNA of Fragilidium spp. were amplified and sequenced. Their phylogenetic positions agree with the morphological taxonomy.	Ocean Univ China, Coll Marine Biol, Qingdao 266003, Peoples R China; Third Inst Oceanog, Dept Geol & Environm, Xiamen 361005, Peoples R China; Jinan Univ, Coll Sci & Engn, Dept Environm Engn, Guangzhou 510632, Peoples R China	Ocean University of China; Third Institute of Oceanography, Ministry of Natural Resources; Jinan University	Gu, HF (通讯作者)，Ocean Univ China, Coll Marine Biol, Qingdao 266003, Peoples R China.	haifenggu@yahoo.com	Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171				ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; BALECH E, 1990, HELGOLANDER MEERESUN, V44, P387, DOI 10.1007/BF02365475; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; BALECH E., 1988, SERIES ZOOLOGICA, V58, P479; BLANCO J, 1989, Scientia Marina, V53, P785; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Cox E. 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Sin.	NOV	2007	45	6					828	840		10.1360/aps07001	http://dx.doi.org/10.1360/aps07001			13	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	238RH					2025-03-11	WOS:000251464700008
J	Peyrot, D; Rodríguez-López, JP; Lassaletta, L; Meléndez, N; Barrón, E				Peyrot, Daniel; Pedro Rodriguez-Lopez, Juan; Lassaletta, Luis; Melendez, Nieves; Barron, Eduardo			Contributions to the palaeoenvironmental knowledge of the Escucha Formation in the Lower Cretaceous Oliete Sub-basin, Teruel, Spain	COMPTES RENDUS PALEVOL			English	Article; Proceedings Paper	International Seminar on Palaeobotany and Evolution of the Plants World	MAY 23-25, 2007	Coll France, Paris, FRANCE		Coll France	palynology; palaeoecology; Upper Aptian-Lower Albian; Oliete Sub-Basin; Spain	ATMOSPHERIC CO2; ANGIOSPERM; POLLEN; MODEL	The Oliete Sub-basin is located in the link zone between the Iberian and the Catalonian Coastal Ranges (Teruel Province, Spain). The palynological samples have been collected in the Upper Aptian-lower Albian rocks of the Escucha Formation, which present an organic-rich sedimentary succession deposited in a variety of continental and coastal environments. Four detailed sections have been studied in order to establish the stratigraphical framework to perform the palynological study. The rocks of these sections contained abundant and well-diversified palynomorph assemblages. Their study allowed the identification of 78 taxa or taxonomic groups (dinoflagellate cysts, acritarchs, phycomes of prasinophytes, algae, bryophytes, lycophytes, pteridophytes, gymnosperms, and primitive angiosperms). The quantitative percentual and the multivariate analysis performed upon the supplied palynological data supports the hypothesis of subtropical palaeoenvironments controlled by non-uniform conditions. The assemblages are comprised of parautochthonous and allochthonous elements, which reflect the existence of coniferous forests and wetlands.	[Peyrot, Daniel] Fac Ciencias Geol, Inst Geol Econ UCM CSIC, Dept Paleontol, Madrid 28040, Spain; [Peyrot, Daniel] Univ Montpellier 2, ISE Montpellier, Lab Paleoenvironm, F-34095 Montpellier 5, France; [Pedro Rodriguez-Lopez, Juan; Melendez, Nieves] Fac Ciencias Geol, Inst Geol Econ UCM CSIC, Dept Estratigrafia, Madrid 28040, Spain; [Lassaletta, Luis] Fac Ciencias Biol UCM, Dept Interuniv Ecol, Madrid 28040, Spain; [Barron, Eduardo] IGME, Museo Geominero, Madrid 28003, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE); Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE)	Peyrot, D (通讯作者)，Fac Ciencias Geol, Inst Geol Econ UCM CSIC, Dept Paleontol, JOse Antonio Novais 2, Madrid 28040, Spain.	danip@geo.ucm.es	peyrot, Daniel/AAI-6091-2020; Barrón, Eduardo/L-4726-2014; Lassaletta, Luis/D-3894-2009	Barron, Eduardo/0000-0003-4979-1117; Lassaletta, Luis/0000-0001-9428-2149; peyrot, Daniel/0000-0002-3897-6733; melendez, nieves/0000-0002-9476-740X				Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; AGUILAR M.J., 1971, ESTUDIOS GEOL GICOS, V27, P497; ALVIN KL, 1982, REV PALAEOBOT PALYNO, V37, P71, DOI 10.1016/0034-6667(82)90038-0; [Anonymous], 1994, SEDIMENTATION ORGANI; Balme Basil E., 1995, Review of Palaeobotany and Palynology, V87, P81, DOI 10.1016/0034-6667(95)93235-X; BARRON EJ, 1995, PALEOCEANOGRAPHY, V10, P953, DOI 10.1029/95PA01624; Batten DJ, 1997, REV PALAEOBOT PALYNO, V99, P25, DOI 10.1016/S0034-6667(97)00036-5; Behrensmeyer Anna K., 1992, P15; Benzecri J.P., 1973, L'analyse des donnees, V2, P1; Berner RA, 2001, AM J SCI, V301, P182, DOI 10.2475/ajs.301.2.182; Cervera A., 1976, Tecniterrae, V14, P25; Clarke LJ, 1999, GEOLOGY, V27, P699, DOI 10.1130/0091-7613(1999)027<0699:NOIEFL>2.3.CO;2; Coiffard C, 2006, ANN BOT-LONDON, V98, P495, DOI 10.1093/aob/mcl125; COURTINAT B, 1984, REV PALAEOBOT PALYNO, V41, P39, DOI 10.1016/0034-6667(84)90042-3; Crane P.R., 1987, The origins of angiosperms and their biological consequences, P107; CRANE PR, 1989, SCIENCE, V246, P675, DOI 10.1126/science.246.4930.675; Diéguez C, 2000, PALAEONTOLOGY, V43, P1113, DOI 10.1111/1475-4983.00163; Doyle JA, 1999, PALAEOECO A, V26, P3; Feild TS, 2004, PALEOBIOLOGY, V30, P82, DOI 10.1666/0094-8373(2004)030<0082:DADANI>2.0.CO;2; Fluteau F, 2007, PALAEOGEOGR PALAEOCL, V247, P357, DOI 10.1016/j.palaeo.2006.11.016; Friis EM, 2006, PALAEOGEOGR PALAEOCL, V232, P251, DOI 10.1016/j.palaeo.2005.07.006; Friis EM, 2000, GRANA, V39, P226, DOI 10.1080/00173130052017262; Hallam A., 1992, PHANEROZOIC SEA LEVE; Hammer O, 2006, PALEONTOLOGICAL DATA ANALYSIS, P1; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; HARRIS TM, 1983, BOT J LINN SOC, V86, P149, DOI 10.1111/j.1095-8339.1983.tb00722.x; Herngreen GF., 1996, Palynology: Principles and Applications, V3, P1157; Hesse M, 2007, PLANT SYST EVOL, V263, P93, DOI 10.1007/s00606-006-0468-z; Hubbard RNLB, 1997, PALAEONTOLOGY, V40, P43; HUBER BT, 1995, GEOL SOC AM BULL, V107, P1164, DOI 10.1130/0016-7606(1995)107<1164:MLCCOT>2.3.CO;2; Lupia R, 1999, PALEOBIOLOGY, V25, P305, DOI 10.1017/S009483730002131X; McCune B., 2006, PC ORD MULTIVARIATE; MEDUS J, 1977, REV PALAEOBOT PALYNO, V24, P141, DOI 10.1016/0034-6667(77)90009-4; MELENDEZ A, 2000, LAKE BASINS SPACE TI, V46, P279; Mohr B.A.R., 1989, Berliner Geowissenschaftliche Abhandlungen. 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J	Courtinat, B; Pittet, B; Mattioli, E; Rio, M				Courtinat, Bernard; Pittet, Bernard; Mattioli, Ernantiela; Rio, Michel			Marine microplankton and calcareous nannofossil palaeoecology of the Toarcian stratotype	GEOBIOS			English	Article						dinoflagellate cysts; acritarchs; Calcareous nannofossils; palaeoenvironments; Toarcian; stratotype; Europe	NANNOPLANKTON PRODUCTIVITY; SOUTHERN GERMANY; ANOXIC EVENT; PHYTOPLANKTON; BASIN; DEPOSITION; SEDIMENTS; FRANCE; NORTH	In the Bifrons to Aalensis Ammonite Zones of the Wines section (Toarcian stratotype), woody phytoclasts, nonsaccate pollen grains, and marine assemblages (dinoflagellate cysts, acritarchs, and foraminiferal linings) dominate the palynofacies. The dinoflagellate cyst assemblage is cosmopolitan with minor Boreal influences, characterized by relatively high quantities of Micrhystridium, Baltisphaeridium, Mendicodinium spinosum, Nannoceratopsis, and the Parvocysta suite, dominating in turn the marine assemblages. Marine assemblage compositions, both dinoflagellate cysts and acritarchs, and calcareous nannofossil abundances are different in marl and limestone lithotypes of the Wines section. Calcareous nannofossils are generally more abundant in marls than in limestones, they display however a cyclic pattern of semiquantitative abundances in phase with lithological cycles. Although a diagenetic overprint cannot be completely excluded to explain such a difference, it seems likely that these dissimilarities are in part primary, the results of variations in terms of proximality-distality, and climatic fluctuations. A mean duration of 117.6 Kyr per marl-limestone alternation, and the stacking of four mad-limestone alternations for 470.6 Kyr, suggest a control by the Earth's two orbital eccentricity cycles. It is likely that the pal aeoenvi ron mental conditions, which influenced the formation of marl-limestone alternations, also controlled the variations in marine phytoplankton assemblages. (c) 2007 Published by Elsevier Masson SAS.	[Courtinat, Bernard; Pittet, Bernard; Mattioli, Ernantiela; Rio, Michel] Univ Lyon 1, CNRS, PEPS, UMR 5125, F-69622 Villeurbanne, France	Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS)	Courtinat, B (通讯作者)，Univ Lyon 1, CNRS, PEPS, UMR 5125, Campus Doua,Batiment Geode, F-69622 Villeurbanne, France.	bernard.courtinat@univ-lyon1.fr	Pittet, Bernard/B-9664-2012; Mattioli, Emanuela/D-7951-2012					[Anonymous], RIV ITAL PALEONTOL S, DOI DOI 10.13130/2039-4942/8959; BACELLE L, 1965, 9 SCI GEOLOGICHE PAL, V1, P59; Baldanza Angela, 1996, Palaeopelagos, V5, P161; BASSOULLET JP, ATLAS TECHYS PALEOEN; BERGER A, 1988, REV GEOPHYS, V26, P624, DOI 10.1029/RG026i004p00624; BIGNOT G, 2001, INTRO MICROPALEONTO; Claps M., 1995, Memorie di Scienze Geologiche Padova, V47, P179; CUBAYNES R, 1994, STRATA, V24, P1; CUBAYNES R, 1987, JURASSIQUE QUERCY ST, V7, P1; DAVIES E H, 1985, Palynology, V9, P105; de Vains G., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P451; DORHOFER G, 1980, LIFE SCI MISCELLANEO, P1; Erkmen U., 1980, Geobios (Villeurbanne), V13, P45, DOI 10.1016/S0016-6995(80)80014-3; Evitt W.R., 1985, SPOROPOLLENIN DINOFL, P1; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; FENCHEL TM, 1970, MAR BIOL, V7, P255, DOI 10.1007/BF00367496; Galbrun Bruno, 1994, Geobios Memoire Special (Villeurbanne), V17, P575; GARDEN G, 1991, Society for Neuroscience Abstracts, V17, P229; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; HALLAM A, 1969, Palaeontology (Oxford), V12, P1; Hallock P, 1987, PALEOCEANOGRAPHY, V2, P457, DOI 10.1029/PA002i005p00457; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; LISTER J K, 1988, Palaeontographica Abteilung B Palaeophytologie, V210, P9; Mattioli E, 2004, J GEOL SOC LONDON, V161, P685, DOI 10.1144/0016-764903-074; Mattioli E, 2002, MAR MICROPALEONTOL, V45, P175, DOI 10.1016/S0377-8398(02)00039-7; Mattioli E, 1997, PALAEOGEOGR PALAEOCL, V130, P113, DOI 10.1016/S0031-0182(96)00127-7; NOEL D, 1994, RIV ITAL PALEONTOL S, V99, P515; Olivier N, 2004, PALAEOGEOGR PALAEOCL, V212, P233, DOI 10.1016/j.palaeo.2004.06.003; Palliani RB, 1998, PALAEOGEOGR PALAEOCL, V142, P33, DOI 10.1016/S0031-0182(97)00152-1; Palliani RB, 1997, B CENT RECH EXPL, V21, P107; Palliani RB, 1999, MICROPALEONTOLOGY, V45, P201, DOI 10.2307/1486113; Palliani RB, 1999, MAR MICROPALEONTOL, V37, P101, DOI 10.1016/S0377-8398(99)00017-1; Palliani RB, 2000, P YORKS GEOL SOC, V53, P1, DOI 10.1144/pygs.53.1.1; PALLIANI RB, 1993, PALEOPELAGOS, V3, P129; PALLIANI RB, 2002, MAR MICROPALEONTOL, V885, P1; Pittet B, 2002, PALAEOGEOGR PALAEOCL, V179, P71, DOI 10.1016/S0031-0182(01)00409-6; Pittet B, 2000, J SEDIMENT RES, V70, P392, DOI 10.1306/2DC40918-0E47-11D7-8643000102C1865D; POULSEN NE, 1996, CONTRIBUTIONS SERIES, V31, P1; Reboulet S, 2003, PALAEOGEOGR PALAEOCL, V201, P113, DOI 10.1016/S0031-0182(03)00541-8; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding J.B., 1984, Proceedings of the Yorkshire Geological Society, V45, P109; Riding James B., 1991, Palynology, V15, P115; Riding JB, 1996, B SOC GEOL FR, V167, P3; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; ROTH PH, 1984, INITIAL REP DEEP SEA, V75, P651; SAJEANT WAS, 1974, FOSSIL LIVING DINOFL; Shannon C.E., 1964, MATH THEORY COMMUNIC; Silva IP, 1989, TERRA NOVA, V1, P443, DOI 10.1111/j.1365-3121.1989.tb00407.x; THIERSTEIN HR, 1991, MAR GEOL, V9, P1; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Tyson R.V., 1987, Marine petroleum source rocks, V26, P47, DOI 10.1144/GSL.SP.1987.026.01.03; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; WATKINS DK, 1989, PALAEOGEOGR PALAEOCL, V74, P75, DOI 10.1016/0031-0182(89)90020-5; Winter Amos, 1994, P161; WOOLLAM R, 1983, 832 I GEOL SCI REP, P1; [No title captured]	57	5	5	0	5	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS	23 RUE LINOIS, 75724 PARIS, FRANCE	0016-6995			GEOBIOS-LYON	Geobios	NOV-DEC	2007	40	6					785	800		10.1016/j.geobios.2007.01.005	http://dx.doi.org/10.1016/j.geobios.2007.01.005			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	248XH					2025-03-11	WOS:000252190000008
J	Head, MJ				Head, Martin J.			Last Interglacial (Eemian) hydrographic conditions in the southwestern Baltic Sea based on dinoflagellate cysts from Ristinge Klint, Denmark	GEOLOGICAL MAGAZINE			English	Article						dinoflagellate cysts; Eemian; Last Interglacial; quaternary; Baltic sea	NORTHERN NORTH-ATLANTIC; RECENT SEDIMENTS; RESTING CYSTS; POLLEN STRATIGRAPHY; MOLLUSK FAUNAS; CLIMATE; QUATERNARY; MOMMARK; WESTERN; MORPHOLOGY	A dinoflagellate cyst record with strong Mediterranean/Lusitanian affinities is described from marine deposits of Eemian age (Last Interglacial; Late Pleistocene) at Ristinge Klint, Denmark, revealing new information about the hydrographic evolution of the southwestern Baltic Sea. A revised correlation of the pollen record at Ristinge Klint with that of the annually laminated site at Bispingen in northern Germany provides temporal control. Approximately the first quarter of Eemian time is represented. A marine ingression into a lake took place during the Quercus rise, about 300 years into the interglacial, and is marked by low (< c. 3 psu) salinities at the base of the Cyprina Clay that increased progressively. An abrupt and significant rise in the inflow of warm, saline waters from the North Sea occurred at about 750 years into the interglacial (the Corylus rise), and at about 1900 years into the interglacial, strongly stratified waters developed. Higher in the Cyprina Clay and continuing to its top, at nearly 3000 years into the interglacial, more open-marine waters are indicated, although fully marine conditions were not reached. The dinoflagellate record throughout the Cyprina Clay at Ristinge Klint is therefore one of increasing marine influence. Summer sea-surface temperatures approached, and may have exceeded, 26-28 degrees C during early Eemian time, indicating temperatures at least 5 degrees C warmer than at present. These warm conditions persisted to the top of the record at Ristinge Klint. No evidence exists at Ristinge Klint for the influence of Arctic watermasses, and the paucity of cold-water species throughout the section reflects mild winter temperatures in the southwestern Baltic Sea. The new species Spiniferites ristingensis is formally described, and the name Operculodinium centrocarpum var. cezare de Vernal, Goyette & Rodrigues, 1989 is validated.	[Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University	Head, MJ (通讯作者)，Brock Univ, Dept Earth Sci, 500 Glenridge Ave, St Catharines, ON L2S 3A1, Canada.	mjhead@brocku.ca						Aalbersberg G, 1998, J QUATERNARY SCI, V13, P367, DOI 10.1002/(SICI)1099-1417(1998090)13:5<367::AID-JQS400>3.0.CO;2-I; Andersen S. 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J	Pitcher, GC; Cembella, AD; Joyce, LB; Larsen, J; Probyn, TA; Sebastián, CR				Pitcher, G. C.; Cembella, A. D.; Joyce, L. B.; Larsen, J.; Probyn, T. A.; Sebastian, C. Ruiz			The dinoflagellate <i>Alexandrium minutum</i> in Cape Town harbour (South Africa):: Bloom characteristics, phylogenetic analysis and toxin composition	HARMFUL ALGAE			English	Article						Alexandrium minutum; harbour bloom; phylogenetics; cysts; toxins	ISOTOPE-DILUTION MODELS; ENVIRONMENTAL-FACTORS; GONYAULAX-TAMARENSIS; CYST PRODUCTION; DINOPHYCEAE; NITROGEN; PHOSPHORUS; AMMONIUM; GROWTH; ENCYSTMENT	A novel bloom of Alexandrium minutum occurred in an inner basin of the Cape Town harbour from November 2003 to February 2004. Cellular concentrations reached a maximum of 1.4 x 10(8) cells l(-1) during the mid-December period with corresponding chlorophyll a concentrations of 243 mg m(-3). Primary productivity measurements conducted during the latter part of the bloom revealed a maximum assimilation number of 11.17 mg C mg Chl a(-1) h(-1) during the middle of the day. Productivity during this post-peak period was sustained largely by the reduced nitrogen species NH4 and urea (96%) as measured using N-15 tracer techniques. The large subunit ribosomal DNA sequence of A. minutum isolates from Cape Town harbour was identical to conspecifics collected in Western Europe and in Australia. The composition of tetrahydropurine neurotoxins associated with paralytic shellfish poisoning (PSP) was limited to gonyautoxins (GTX1-GTX4). This profile combined with evidence of a low toxin cell quota (1.5 fmol GTX cell(-1)) supports a close association of this taxon with other members of the A. minutum species complex, particularly from Europe. Toxin analysis from black mussels collected during this bloom indicated that the accumulated PSP toxins originated from A. minutum and not from Alexandrium catenella as is most often the case along the South African coast. (C) 2007 Elsevier B.V. All rights reserved.	Marine & Coastal Management, Cape Town, South Africa; Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; Inst Bot, DK-1353 Copenhagen, Denmark; Univ Cape Town, Dept Zool, ZA-7701 Rondebosch, South Africa	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Cape Town	Pitcher, GC (通讯作者)，Marine & Coastal Management, Private Bag X2, Cape Town, South Africa.	gpitcher@deat.gov.za						Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson P., 2003, Monographs on Oceanographic Methodology, V11, P99; BALECH E, 1989, PHYCOLOGIA, V28, P206, DOI 10.2216/i0031-8884-28-2-206.1; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLACKBURN TH, 1979, APPL ENVIRON MICROB, V37, P760, DOI 10.1128/AEM.37.4.760-765.1979; CAPERON J, 1979, MAR BIOL, V54, P33, DOI 10.1007/BF00387049; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; CEMBELLA AD, 1993, J SHELLFISH RES, V12, P389; Chang FH, 1997, NEW ZEAL J MAR FRESH, V31, P1, DOI 10.1080/00288330.1997.9516740; Chang FH, 1997, TOXICON, V35, P393, DOI 10.1016/S0041-0101(96)00168-7; DELGADO M, 1990, Scientia Marina, V54, P1; Diener M, 2006, EUR FOOD RES TECHNOL, V224, P147, DOI 10.1007/s00217-006-0302-4; Erard-Le Denn E, 2000, ESTUAR COAST SHELF S, V50, P109, DOI 10.1006/ecss.1999.0537; FRANCO JM, 1994, J APPL PHYCOL, V6, P275, DOI 10.1007/BF02181938; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Giacobbe MG, 1996, ESTUAR COAST SHELF S, V42, P539, DOI 10.1006/ecss.1996.0035; GLIBERT PM, 1982, LIMNOL OCEANOGR, V27, P639; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Guindon S, 2003, SYST BIOL, V52, P696, DOI 10.1080/10635150390235520; Halim Y., 1960, Vie et Milieu, V11, P102; HALLEGRAEFF GM, 1988, J PLANKTON RES, V10, P533, DOI 10.1093/plankt/10.3.533; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; Hansen G, 2003, HARMFUL ALGAE, V2, P317, DOI 10.1016/S1568-9883(03)00060-X; Hasle G.R., 1978, PHYTOPLANKTON MANUAL, P88; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; KNAUER GA, 1979, DEEP-SEA RES, V26, P97, DOI 10.1016/0198-0149(79)90089-X; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; LAWS E, 1984, LIMNOL OCEANOGR, V29, P379, DOI 10.4319/lo.1984.29.2.0379; Lilly EL, 2005, HARMFUL ALGAE, V4, P1004, DOI 10.1016/j.hal.2005.02.001; Maguer JF, 2004, LIMNOL OCEANOGR, V49, P1108, DOI 10.4319/lo.2004.49.4.1108; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Mitchell-Innes BA, 2000, S AFR J MARINE SCI, V22, P273, DOI 10.2989/025776100784125762; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Pitcher GC, 2000, S AFR J MARINE SCI, V22, P255, DOI 10.2989/025776100784125681; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Probert I, 2002, CRYPTOGAMIE ALGOL, V23, P343; PROBYN TA, 1987, MAR ECOL PROG SER, V37, P53, DOI 10.3354/meps037053; Quilliam MA., 2001, Mycotoxins and Phycotoxins in Perspective at the Turn of the Century, P383; Sapeika N., 1948, South African Medical Journal, V22, P337; Sebastián CR, 2005, PHYCOLOGIA, V44, P49, DOI 10.2216/0031-8884(2005)44[49:PAOTAD]2.0.CO;2; Sebastián CR, 2001, MOL ECOL NOTES, V1, P329; Swofford D., 2002, PAUP PHYLOGENETIC AN; Taylor F.J.R., 1995, Manual on Harmful Marine Microalgae, P283; Thompson JD, 1997, NUCLEIC ACIDS RES, V25, P4876, DOI 10.1093/nar/25.24.4876; Usup G, 2002, HARMFUL ALGAE, V1, P265, DOI [10.1016/S1568-9883(02)00044-6, 10.1016/S1568-9883(02)00003-3]; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175	55	50	52	0	18	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	NOV	2007	6	6					823	836		10.1016/j.hal.2007.04.008	http://dx.doi.org/10.1016/j.hal.2007.04.008			14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	238TN					2025-03-11	WOS:000251470600007
J	Genovesi, B; Mouillot, D; Vaquer, A; Laabir, M; Pastoureaud, A				Genovesi, B.; Mouillot, D.; Vaquer, A.; Laabir, M.; Pastoureaud, A.			Towards an optimal sampling strategy for <i>Alexandrium catenella</i> (Dinophyceae) benthic resting cysts	HARMFUL ALGAE			English	Article						Alexandrium catenella; toxic dinoflagellate; resting cyst; optimum sample size; spatial distribution; vertical profiles	DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; DISPERSION STATISTICS; ENVIRONMENTAL-FACTORS; MARINE-SEDIMENTS; WEST-COAST; BAY; BLOOM; GERMINATION; DYNAMICS	The study proposes methodological developments to optimize sampling strategy of resting cysts of Alexandrium catenella to estimate their abundance with a predefined error. This work also aims to provide information on spatial distribution of resting cysts in sediments. The distribution mode of A. catenella resting cysts related to the abundance variability was studied through sediment cores sampling on four different spatial scales and using Ludox CLX gradient density method. The quantification method underestimates by a factor of 2 the resting cysts abundance in one gram of sediment. Application of Taylor's power law allowed us to define a compromise between sampling effort and abundance estimation error. In the case of A. catenella resting cysts from Thau lagoon, the optimal sampling strategy consists of sampling 10 stations on a surface of 2 km(2) for a given coefficient of variability (C) of 15%, sampling 3 sediment cores at each station (C = 30%) and counting only one replicate by core (C = 18%). Results related to the application of Taylor's power law are closely dependent on resting cyst density and aggregation in a given sediment. In our area, A. catenella resting cysts are mainly observed in the upper 3 cm of sediment. Horizontally, their heterogeneity is lower on 10 cm(2) surface and tends to stabilize itself beyond a surface of 10 m(2). Each author has to carry out this pre-sampling effort for his own resting cysts-fonning species, in his own area, in order to increase accuracy of resting cyst mapping. (C) 2007 Elsevier B.V. All rights reserved.	Univ Montpellier 2, CNRS, IFREMER, UMR 5119,UM2, F-34095 Montpellier, France; IFREMER, LER LR, F-34203 Sete, France	Ifremer; Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Ifremer	Genovesi, B (通讯作者)，Univ Montpellier 2, CNRS, IFREMER, UMR 5119,UM2, F-34095 Montpellier, France.	genovesi@univ-montp2.fr	Mouillot, David/HCH-5670-2022					AN KH, 1992, BOT MAR, V35, P61, DOI 10.1515/botm.1992.35.1.61; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; [Anonymous], 1996, HARMFUL TOXIC ALGAL; [Anonymous], DEEP SEA RES 2; [Anonymous], HARMFUL ALGAE 2002; BLANCHARD GF, 1990, MAR ECOL PROG SER, V68, P101, DOI 10.3354/meps068101; Blanco J, 1986, OCEANOGRAPHY WASHING, V3, P181; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Dale B., 1983, P69; Erard-Le Denn E., 1995, HARMFUL MARINE ALGAL, P257; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; François F, 1999, CR ACAD SCI III-VIE, V322, P339, DOI 10.1016/S0764-4469(99)80070-5; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Giangrande A, 2002, J SEA RES, V47, P97, DOI 10.1016/S1385-1101(01)00103-4; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HO CC, 1993, ENVIRON ENTOMOL, V22, P21, DOI 10.1093/ee/22.1.21; Irwin A, 2003, HARMFUL ALGAE, V2, P61, DOI 10.1016/S1568-9883(02)00084-7; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; KARANDINOS MG, 1976, B ENTOMOL SOC AM, V22, P21; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; Marret F, 2003, MAR MICROPALEONTOL, V47, P101, DOI 10.1016/S0377-8398(02)00095-6; Matsuoka K, 2003, J PLANKTON RES, V25, P1461, DOI 10.1093/plankt/fbg111; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Mizushima K, 2004, PHYCOL RES, V52, P408, DOI 10.1111/j.1440-183.2004.00358.x; Mouillot D, 1999, MAR ECOL-P S Z N I, V20, P19, DOI 10.1046/j.1439-0485.1999.00064.x; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; SCHWINGHAMER P, 1991, LIMNOL OCEANOGR, V36, P588, DOI 10.4319/lo.1991.36.3.0588; Siegel S.John C.N., 1988, Nonparametric Statistics for the Behavioral Sciences, V2nd, P399; TAYLOR LR, 1961, NATURE, V189, P732, DOI 10.1038/189732a0; TAYLOR LR, 1984, ANNU REV ENTOMOL, V29, P321, DOI 10.1146/annurev.en.29.010184.001541; THISTLEWOOD HMA, 1989, ENVIRON ENTOMOL, V18, P398, DOI 10.1093/ee/18.3.398; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; Wang ZH, 2004, PHYCOL RES, V52, P387, DOI 10.1111/j.1440-183.2004.00356.x; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; Wang ZH, 2004, MAR ECOL-P S Z N I, V25, P289, DOI 10.1111/j.1439-0485.2004.00035.x; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	47	14	14	1	21	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	NOV	2007	6	6					837	848		10.1016/j.hal.2007.04.007	http://dx.doi.org/10.1016/j.hal.2007.04.007			12	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	238TN		Bronze, Green Published			2025-03-11	WOS:000251470600008
J	Mouradian, M; Panetta, RJ; de Vernal, A; Gélinas, Y				Mouradian, Maggy; Panetta, Robert J.; de Vernal, Anne; Gelinas, Yves			Dinosterols or dinocysts to estimate dinoflagellate contributions to marine sedimentary organic matter?	LIMNOLOGY AND OCEANOGRAPHY			English	Article							STEROLS; PRESERVATION; BIOMARKERS	Dinosterol (4 alpha,23,24-trimethyl-5 alpha-cholest-22E-en-3 beta-ol) is frequently used as an alternative to dinoflagellate cyst (dinocyst) counting in paleoceanography to assess dinoflagellate inputs to marine sediments. However, recent studies have shown poor correlation between these two proxies in continental-margin sediments. We reevaluated the relationship and expanded it to include a suite of biogeochemical transformation products of the parent dinosterol (dinosterone, dinostanone, and dinostanol). These dinoflagellate-specific 4 alpha,23,24-trimethyl steroidal species (Sigma(dinosterol)) are compared to dinocyst counts in sediments from the western Mexican margin (375-3,500 m). Samples were taken from subsurface (3-6 cm) and down core (16-27 cm) to reflect widely contrasting organic carbon content and redox conditions. A strong correlation was found between the sum of all dinoflagellate-derived sterols, Sigma(dinosterols), and total dinocyst counts, highlighting the importance of including diagenetic alteration products of the parent molecule when exploiting organic biomarkers in paleoceanographic studies. In low-energy environments and for well-preserved samples, such as those studied in this work, both methods provide robust, internally consistent data, suggesting that when diagenetic transformation products of dinosterol are taken into account, gas chromatography and optical microscopy could be used interchangeably to estimate dinoflagellate inputs to marine sediments.	Concordia Univ, Dept Chem & Biochem, Geotop, Montreal, PQ H4B 1R6, Canada; Univ Quebec, Dept Sci Terre, Geotop, Montreal, PQ H3C 3P8, Canada	Concordia University - Canada; University of Quebec; University of Quebec Montreal	Gélinas, Y (通讯作者)，Concordia Univ, Dept Chem & Biochem, Geotop, 7141 Sherbrooke St W, Montreal, PQ H4B 1R6, Canada.	ygelinas@alcor.concordia.ca	Gelinas, Yves/K-4019-2013; de Vernal, Anne/D-5602-2013	Gelinas, Yves/0000-0001-5751-8378; de Vernal, Anne/0000-0001-5656-724X				[Anonymous], 1993, ORG GEOCHEM, DOI DOI 10.1007/978-1-4615-2890-6_6; Arzayus KM, 2005, GEOCHIM COSMOCHIM AC, V69, P455, DOI 10.1016/j.gca.2004.06.029; Brassell S.C., 1993, ORG GEOCHEM, P699; Canuel EA, 1996, GEOCHIM COSMOCHIM AC, V60, P1793, DOI 10.1016/0016-7037(96)00045-2; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Dickens AF, 2006, GEOCHIM COSMOCHIM AC, V70, P666, DOI 10.1016/j.gca.2005.10.024; DJERASSI C, 1981, PURE APPL CHEM, V53, P873, DOI 10.1351/pac198153040873; Gélinas Y, 2001, SCIENCE, V294, P145, DOI 10.1126/science.1062363; Hartnett HE, 1998, NATURE, V391, P572, DOI 10.1038/35351; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hedges JI, 2000, ORG GEOCHEM, V31, P945, DOI 10.1016/S0146-6380(00)00096-6; Hudson ED, 2001, MAR CHEM, V76, P253, DOI 10.1016/S0304-4203(01)00066-4; Jones GJ., 1994, Chemical Methods in Prokaryotic Systematics, P163; KEIL RG, 1994, NATURE, V370, P549, DOI 10.1038/370549a0; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Leblond JD, 2002, J PHYCOL, V38, P670, DOI 10.1046/j.1529-8817.2002.01181.x; Li W, 1995, BIOGEOCHEMISTRY, V31, P139, DOI 10.1007/BF00004046; Marret F, 2003, MAR MICROPALEONTOL, V47, P101, DOI 10.1016/S0377-8398(02)00095-6; Mollenhauer G, 2006, DEEP-SEA RES PT I, V53, P1224, DOI 10.1016/j.dsr.2006.05.005; Nash D, 2005, WATER RES, V39, P2964, DOI 10.1016/j.watres.2005.04.063; Rochon A., 1999, SPECIAL CONTRIBUTION, V35; Sangiorgi F, 2005, ESTUAR COAST SHELF S, V64, P395, DOI 10.1016/j.ecss.2005.03.005; Sikes EL, 2005, DEEP-SEA RES PT I, V52, P721, DOI 10.1016/j.dsr.2004.12.003; Smallwood BJ, 2000, DEEP-SEA RES PT II, V47, P353, DOI 10.1016/S0967-0645(99)00110-1; Stickley CE, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2004PA001022; Sun MY, 1998, ORG GEOCHEM, V28, P773, DOI 10.1016/S0146-6380(98)00043-6; VOLKMAN JK, 1986, ORG GEOCHEM, V9, P83, DOI 10.1016/0146-6380(86)90089-6; Volkman JK, 2005, ORG GEOCHEM, V36, P139, DOI 10.1016/j.orggeochem.2004.06.013; Volkman JK, 1998, ORG GEOCHEM, V29, P1163, DOI 10.1016/S0146-6380(98)00062-X; VOLKMAN JK, 1993, ORG GEOCHEM, V20, P7, DOI 10.1016/0146-6380(93)90076-N; Volkman JK, 1999, PHYTOCHEMISTRY, V52, P659, DOI 10.1016/S0031-9422(99)00251-4; WAKEHAM SG, 1989, NATURE, V342, P787, DOI 10.1038/342787a0; WITHERS N, 1987, BIOL DINOFLAGELLATES, V32, P316; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	34	16	20	1	12	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0024-3590	1939-5590		LIMNOL OCEANOGR	Limnol. Oceanogr.	NOV	2007	52	6					2569	2581		10.4319/lo.2007.52.6.2569	http://dx.doi.org/10.4319/lo.2007.52.6.2569			13	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	233ZG		Bronze			2025-03-11	WOS:000251129700022
J	Bockelmann, FD; Zonneveld, KAF; Schmidt, M				Bockelmann, Frank-D.; Zonneveld, Karin A. F.; Schmidt, Martin			Assessing environmental control on dinoflagellate cyst distribution in surface sediments of the Benguela upwelling region (eastern South Atlantic)	LIMNOLOGY AND OCEANOGRAPHY			English	Article							ORGANIC-MATTER; RED TIDE; DEEP-SEA; PRESERVATION; OCEAN; PRODUCTIVITY; SYSTEM; NORTH; ASSEMBLAGES; POPULATIONS	Organic-walled dinoflagellate cyst assemblages in surface sediments of the Benguela Current Upwelling System (eastern South Atlantic) show geographic patterns that cannot entirely originate from cyst production or transport. Aimed at answering how far these variations are due to taphonomic control, this study investigated a possible correlation with the changes in bottom-water oxygen concentrations typifying this region. Based on 36 samples, multivariate statistics were used to analyze community variability with respect to bottom-water oxygen concentration, temperature, salinity, nutrient content, chlorophyll a (Chl a) concentration, the organic carbon content of surface sediments, and a measure of water column stratification. Determined relationships to salinity, nutrient supply, nutrition, and environmental steadiness point out the requirements for dinoflagellate cyst production, while cross-shelf transport processes could have introduced variability prior to burial of cysts in surface sediments. The offshore decrease in the relative abundance of protoperidinacean cyst types was consistent with their lower preservation potential under oxygenated conditions and coincided with a change in assemblage composition toward oxidation resistant species. On elimination of covariation, bottom-water oxygenation was significantly related to this pattern and determined together with seasonal salinity, Chl a, and annual phosphate concentration, the parameter combination best explaining community variability. These results suggest that postdepositional degradation of peridinioid dinoflagellate cysts would partly explain the onshore-offshore gradient in species distributions and could be responsible for more variability in assemblage compositions than is presently acknowledged.	Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; Baltic Sea Res Inst Warnemunde, D-18119 Rostock, Germany	University of Bremen; Leibniz Institut fur Ostseeforschung Warnemunde	Bockelmann, FD (通讯作者)，Univ Bremen, Dept Geosci, PO Box 330440, D-28334 Bremen, Germany.	frankd@rcom-bremen.de		Bockelmann, Frank-Detlef/0000-0003-4900-6780				BAILEY GW, 1991, GEOL SOC SPEC PUBL, P171, DOI 10.1144/GSL.SP.1991.058.01.12; BREMNER JM, 1981, THESIS U CAPE TOWN; Calvert S.E., 1983, Coastal Upwelling: its Sedimentary Record (Pt. 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Oceanogr.	NOV	2007	52	6					2582	2594		10.4319/lo.2007.52.6.2582	http://dx.doi.org/10.4319/lo.2007.52.6.2582			13	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	233ZG		Bronze			2025-03-11	WOS:000251129700023
J	Attaran-Fariman, G; de Salas, MF; Negri, AP; Bolch, CJS				Attaran-Fariman, Gilan; de Salas, Miguel F.; Negri, Andrew P.; Bolch, Christopher J. S.			Morphology and phylogeny of <i>Gymnodinium trapeziforme</i> sp nov (Dinophyceae):: a new dinoflagellate from the southeast coast of Iran that forms microreticulate resting cysts	PHYCOLOGIA			English	Article						dinollagellate; gymnodinium; systematics; taxonomy; DNA; LSU-rDNA; microreticulate; resting cyst; Iran; Oman sea	RECENT MARINE-SEDIMENTS; CATENATUM-LIKE CYSTS; COMB. NOV; ULTRASTRUCTURE; TASMANIA; REPRODUCTION; AUREOLUM; WATERS; BASIN; SEA	A new gymnodinioid dinoflagellate, Gymnodinium trapeziforme sp. nov. is described from laboratory cultures established by germination of microreticulate resting cysts collected along the southeast coast of Iran bordering the northern Oman Sea. The vegetative cells are small, biconical to ovoid, with a horseshoe-shaped apical groove that encircles the apex in an anticlockwise direction. Cells have a large tear-shaped nucleus positioned in the right side of the cell that extends from the epicone to the hypocone. Cells of G. trapeziforme can be clearly differentiated from the three other microreticulate cyst-forming gymnodinioids, Gymnodinium catenatum, Gymnodinium nolleri, and Gymnodinium microreticulatum by the shape and position of the nucleus. Cultures established from resting cysts do not produce detectable saxitoxin. The resting cysts of G. trapeziforme are unique in being cubic-trapezoidal in shape with a cyst wall colour that is pale purple-brown, most similar in colour to cysts of G. microreticulatum Botch & Hallegraeff. Comparisons of partial large subunit ribosomal RNA gene sequences demonstrate that G. trapeziforme is allied with, but distinct from (> 12.4%, sequence divergence) the other microreticulate cyst-forming gymnodinioid species.	Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia; Australian Inst Marine Sci, Townsville, Qld, Australia	University of Tasmania; University of Tasmania; Australian Institute of Marine Science	Attaran-Fariman, G (通讯作者)，Offshore Fisheries Res Ctr, Shilat Sq, Chabahar 99717, Iran.	gilanattaran@ifro.ir	Attaran Fariman, Gilan/ABC-4059-2021; Bolch, Christopher/J-7619-2014; Negri, Andrew/G-9909-2017	Negri, Andrew/0000-0003-1388-7395				Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1988, J PHYCOL, V24, P255; [Anonymous], 2002, PHYLOGENETIC ANAL US; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BOLCH CJ, 1998, HARMFUL MICROALGAE, P283; Bolch CJS, 2004, EUR J PHYCOL, V39, P351, DOI 10.1080/09670260410001728098; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRAVO I, 1986, Investigacion Pesquera (Barcelona), V50, P313; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; De Salas ME, 2004, PHYCOLOGIA, V43, P624, DOI 10.2216/i0031-8884-43-5-624.1; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Hall TA., 1999, NUCL ACIDS S SERIES, V41, P95, DOI [DOI 10.1021/BK-1999-0734.CH008, DOI 10.14344/IOC.ML.11.1]; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; Hansen G, 2000, PHYCOLOGIA, V39, P365, DOI 10.2216/i0031-8884-39-5-365.1; Hansen G, 2001, J PHYCOL, V37, P612, DOI 10.1046/j.1529-8817.2001.037004612.x; Hansen G, 2007, PHYCOL RES, V55, P25, DOI 10.1111/j.1440-1835.2006.00442.x; Honsell G, 2004, BOT MAR, V47, P152, DOI 10.1515/BOT.2004.016; Jeanmougin F, 1998, TRENDS BIOCHEM SCI, V23, P403, DOI 10.1016/S0968-0004(98)01285-7; MARCHANT HJ, 1983, J MICROSC-OXFORD, V131, P127, DOI 10.1111/j.1365-2818.1983.tb04239.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; NATION JL, 1983, STAIN TECHNOL, V58, P347, DOI 10.3109/10520298309066811; NEGR AP, 1995, ALATHYRIA CONDOLA TO, V7, P325; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; NEHRING S, 1995, J PLANKTON RES, V17, P85, DOI 10.1093/plankt/17.1.85; OSHIMA Y, 1993, DEV MAR BIO, V3, P907; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; REES AJJ, 1991, PHYCOLOGIA, V30, P90, DOI 10.2216/i0031-8884-30-1-90.1; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; TANGEN K, 1977, SARSIA, V63, P123, DOI 10.1080/00364827.1977.10411330; Targarona J, 1999, GRANA, V38, P170; VINCENT B, 2003, GROWTH STIMULATION G; Zonneveld KAF, 2000, DEEP-SEA RES PT II, V47, P2229, DOI 10.1016/S0967-0645(00)00023-0; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	44	30	31	0	14	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	NOV	2007	46	6					644	656		10.2216/07-05.1	http://dx.doi.org/10.2216/07-05.1			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	227ZD					2025-03-11	WOS:000250695600005
J	Dechraoui, MYB; Wang, ZH; Ramsdell, JS				Dechraoui, Marie-Yasmine Bottein; Wang, Zhihong; Ramsdell, John S.			Intrinsic potency of synthetically prepared brevetoxin cysteine metabolites BTX-B2 and desoxyBTX-B2	TOXICON			English	Article						brevetoxin; marine toxins; Karenia brevis; neurotoxic shellfish poisoning; voltage-gated sodium channel; cytotoxicity assay; radioimmunoassay; receptor-binding assay	OYSTER CRASSOSTREA-VIRGINICA; SENSITIVE SODIUM-CHANNELS; KARENIA-BREVIS CULTURES; RED-TIDE; PTYCHODISCUS-BREVIS; NEW-ZEALAND; AUSTROVENUS-STUTCHBURYI; CONTROLLED EXPOSURES; GREENSHELL MUSSELS; PERNA-CANALICULUS	In mammals and shellfish, brevetoxins produced by the dinoflagellate Karenia brevis are rapidly metabolized to cysteine conjugates. These metabolites identified by mass spectrometry are produced in abundance in mammals and are potentially major bioactive products for intoxication. They are also abundant metabolites in shellfish where they are, in contrast to mammals, retained for prolonged periods, posing a potential threat to shellfish consumers. In this work, we analyze the intrinsic potency of the semi-synthetic cysteine brevetoxin sulfoxide (BTX-B2) and the cysteine brevetoxin (desoxyBTX-B2), each confirmed for purity by LC-MS and NMR techniques, on receptor site 5 of the voltage-gated sodium channels (VGSCs) in brain, heart and skeletal muscle. We show that both brevetoxin conjugates compete with the tritiated reduced parent brevetoxin ([H-3]PbTx-3) in rat brain membrane preparations and in HEK cells expressing skeletal muscle or cardiac VGSC, albeit, with 8-16-fold lower affinity than the PbTx-3. On neuroblastoma cell assays we show a 3-fold reduction in cytotoxic potency for BTX-B2 relative to PbTx-3, and an 8-fold reduction for desoxyBTX-B2. In conclusion, the major transformation product of brevetoxin observed in diverse species through cysteine adduction and oxidation leads to metabolites with reduced potency on brain, skeletal muscle and heart cells. (c) 2007 Elsevier Ltd. All rights reserved.	NOAA, Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxins Program, Charleston, SC 29412 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA	Ramsdell, JS (通讯作者)，NOAA, Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxins Program, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	john.ramsdell@noaa.gov	Bottein, Marie-Yasmine/J-8851-2018	Dechraoui Bottein, Marie-Yasmine/0000-0002-6468-7222				Abraham A, 2006, TOXICON, V48, P104, DOI 10.1016/j.toxicon.2006.04.015; BADEN DG, 1982, TOXICON, V20, P457, DOI 10.1016/0041-0101(82)90009-5; BADEN DG, 1988, TOXICON, V26, P97, DOI 10.1016/0041-0101(88)90141-9; Bourdelais AJ, 2004, CELL MOL NEUROBIOL, V24, P553, DOI 10.1023/B:CEMN.0000023629.81595.09; CATTERALL WA, 1981, MOL PHARMACOL, V19, P345; Cheng YS, 2005, ENVIRON SCI TECHNOL, V39, P3443, DOI 10.1021/es048680j; DAVIS CC, 1948, BOT GAZ, V109, P358, DOI 10.1086/335488; Dechraoui MYB, 2006, TOXICON, V48, P702, DOI 10.1016/j.toxicon.2006.07.032; Dechraoui MYB, 2005, TOXICON, V46, P261, DOI 10.1016/j.toxicon.2005.04.006; Dechraoui MYB, 2003, TOXICON, V41, P919, DOI 10.1016/S0041-0101(03)00088-6; Dickey R, 1999, NAT TOXINS, V7, P157, DOI 10.1002/(SICI)1522-7189(199907/08)7:4<157::AID-NT52>3.3.CO;2-R; Flewelling LJ, 2005, NATURE, V435, P755, DOI 10.1038/nature435755a; GAWLEY RE, 1995, CHEM BIOL, V2, P533, DOI 10.1016/1074-5521(95)90187-6; Goldin AL, 2000, NEURON, V28, P365, DOI 10.1016/S0896-6273(00)00116-1; HUANG JMC, 1984, J PHARMACOL EXP THER, V229, P615; Ishida H, 2004, TOXICON, V43, P701, DOI 10.1016/j.toxicon.2004.03.002; ISHIDA H, 1995, TETRAHEDRON LETT, V36, P725, DOI 10.1016/0040-4039(94)02326-7; LIN YY, 1981, J AM CHEM SOC, V103, P6773, DOI 10.1021/ja00412a053; MANGER RL, 1993, ANAL BIOCHEM, V214, P190, DOI 10.1006/abio.1993.1476; Maucher JM, 2007, ENVIRON SCI TECHNOL, V41, P563, DOI 10.1021/es0612605; McFARREN E. 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J	Saito, K; Drgon, T; Krupatkina, DN; Drgonova, J; Terlizzi, DE; Mercer, N; Vasta, GR				Saito, Keiko; Drgon, Tomas; Krupatkina, Danara N.; Drgonova, Jana; Terlizzi, Daniel E.; Mercer, Natalia; Vasta, Gerardo R.			Effect of biotic and abiotic factors on in vitro proliferation, encystment, and excystment of <i>Pfiesteria piscicida</i>	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							DINOFLAGELLATE HETEROCAPSA-CIRCULARISQUAMA; PHOSPHORUS-LIMITED CULTURES; TOXIC DINOFLAGELLATE; GONYAULAX-TAMARENSIS; CYST GERMINATION; GROWTH-RATES; LIFE-CYCLE; ENVIRONMENTAL EXPOSURE; FORMING DINOFLAGELLATE; ICHTHYOCIDAL ACTIVITY	Pfiesteria spp. are mixotrophic armored dinoflagellates populating the Atlantic coastal waters of the United States. They have been a focus of intense research due to their reported association with several fish mortality events. We have now used a clonal culture of Pfiesteria piscicida and several new environmental isolates to describe growth characteristics, feeding, and factors contributing to the encystment and germination of the organism in both laboratory and environmental samples. We also discuss applied methods of detection of the different morphological forms of Pfiesteria in environmental samples. In summary, Pfiesteria, when grown with its algal prey, Rhodomonas sp., presents a typical growth curve with lag, exponential, and stationary phases, followed by encystment. The doubling time in exponential phase is about 12. h. The profiles of proliferation under a standard light cycle and in the dark were similar, although the peak cell densities were markedly lower when cells were grown in the dark. The addition of urea, chicken manure, and soil extracts did not enhance Pfiesteria proliferation, but crude unfiltered spent aquarium water did. Under conditions of food deprivation or cold (4 degrees C), Pfiesteria readily formed harvestable cysts that were further analyzed by PCR and scanning electron microscopy. The germination of Pfiesteria cysts in environmental sediment was enhanced by the presence of live fish: dinospores could be detected 13 to 15 days earlier and reached 5- to 10-times-higher peak cell densities with live fish than with artificial seawater or f/2 medium alone. The addition of ammonia, urea, nitrate, phosphate, or surprisingly, spent fish aquarium water had no effect.	Univ Maryland, Ctr Marine Biotechnol, Inst Biotechnol, Baltimore, MD 21202 USA; NIH, Natl Inst Drug Abuse, Baltimore, MD 21224 USA; Univ Nacl La Plata, Fac Ciencias Exactas, Catedra Inmunol, La Plata, Argentina	University System of Maryland; University of Maryland Baltimore; National Institutes of Health (NIH) - USA; NIH National Institute on Drug Abuse (NIDA); NIH National Institute on Aging (NIA); National University of La Plata	Vasta, GR (通讯作者)，Univ Maryland, Ctr Marine Biotechnol, Inst Biotechnol, 701 E Pratt St, Baltimore, MD 21202 USA.	vasta@umbi.umd.edu	Vasta, Gerardo/LXU-3978-2024; Drgonova, Jana/B-2903-2008	Drgonova, Jana/0000-0002-4623-8466				ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; Anderson T. 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A., 1999, Virginia Journal of Science, V50, P325; Saito K, 2002, APPL ENVIRON MICROB, V68, P5394, DOI 10.1128/AEM.68.11.5394-5407.2002; STEIDINGER KA, 1975, ENVIRON LETT, V9, P129, DOI 10.1080/00139307509435842; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Vogelbein WK, 2002, NATURE, V418, P967, DOI 10.1038/nature01008; Yamaguchi M, 2001, PHYCOLOGIA, V40, P313, DOI 10.2216/i0031-8884-40-3-313.1; Yamaguchi M, 1999, FISHERIES SCI, V65, P367, DOI 10.2331/fishsci.65.367; Zhang H, 2002, APPL ENVIRON MICROB, V68, P989, DOI 10.1128/AEM.68.2.989-994.2002	68	6	8	0	12	AMER SOC MICROBIOLOGY	WASHINGTON	1752 N ST NW, WASHINGTON, DC 20036-2904 USA	0099-2240			APPL ENVIRON MICROB	Appl. Environ. Microbiol.	OCT	2007	73	20					6410	6420		10.1128/AEM.01229-07	http://dx.doi.org/10.1128/AEM.01229-07			11	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	221SU	17704277	Green Published			2025-03-11	WOS:000250248400011
J	Ki, JS; Han, MS				ki, Jang-Seu; Han, Myung-Soo			Rapid molecular identification of the harmful freshwater dinoflagellate <i>Peridinium</i> in various life stages using genus-specific single-cell PCR	JOURNAL OF APPLIED PHYCOLOGY			English	Article						dinoflagellate cyst; planozygote; rDNA	DINOPHYCEAE; CYSTS	Cysts of the freshwater dinoflagellate Peridinium are typically different from vegetative cells in shape and remain largely undescribed. Molecular discrimination of such cysts would be useful to a number of research disciplines. A reliable method for the amplification of ribosomal DNA (rDNA) from Peridinium at different life stages is described. This genotyping strategy relies on whole cell PCR using Peridinium-specific primers designed from available 18S rDNA sequences. Here, we demonstrate the effectiveness of Peridinium-specific PCR for the rapid molecular identification of Peridinium cells in various life stages such as vegetative, planozygote, hypnozygote and cyst.	Hong Kong Univ Sci & Technol, Dept Biol, Kowloon, Hong Kong, Peoples R China; Hanyang Univ, Coll Nat Sci, Dept Life Sci, Seoul 133791, South Korea	Hong Kong University of Science & Technology; Hanyang University	Ki, JS (通讯作者)，Hong Kong Univ Sci & Technol, Dept Biol, Clear Water Bay, Kowloon, Hong Kong, Peoples R China.	kijs@hanyang.ac.kr						Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; Coyne KJ, 2005, J EUKARYOT MICROBIOL, V52, P90, DOI 10.1111/j.1550-7408.2005.05202001.x; Kawabata Z, 1995, HYDROBIOLOGIA, V312, P115, DOI 10.1007/BF00020767; Ki JS, 2004, MAR BIOTECHNOL, V6, P587, DOI 10.1007/s10126-004-1700-x; Ki JS, 2005, J APPL PHYCOL, V17, P147, DOI 10.1007/s10811-005-7211-y; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Rengefors K, 2001, LIMNOL OCEANOGR, V46, P1990, DOI 10.4319/lo.2001.46.8.1990	7	11	11	1	10	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-8971	1573-5176		J APPL PHYCOL	J. Appl. Phycol.	OCT	2007	19	5					467	470		10.1007/s10811-007-9157-8	http://dx.doi.org/10.1007/s10811-007-9157-8			4	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	206TJ					2025-03-11	WOS:000249205500010
J	Ajuzie, CC				Ajuzie, C. C.			Palatability and fatality of the dinoflagellate <i>Prorocentrum lima</i> to <i>Artemia salina</i>	JOURNAL OF APPLIED PHYCOLOGY			English	Article						artemia; cell-free culture medium; nauplii survivorship; Prorocentrum lima	GRAZING RESPONSES; COPEPODS; TOXICITY; ZOOPLANKTON; DINOPHYCEAE; SURVIVAL; MEDIA; ACID; FISH	Prorocentrum lima is a toxic alga that produces both intra-cellular and extra-cellular toxins, including okadaic acid (OA) and dinophysistoxins (DTXs). Nauplii of the brine shrimp Artemia salina were exposed to both the cell and cell-free culture medium of P. lima in order to test the hypotheses that the extra-cellular medium is toxic to brine shrimp and that the P. lima cell is palatable but fatal to it. Artemia cysts incubated in the cell-free medium hatched, but mortalities were recorded for nauplii that hatched in, and metanuaplii exposed to, test solutions (autoclaved filtered seawater + cell-free medium) that contained at least 50% of the cell-free medium. Animals exposed to cells of P. lima readily fed on the cells. Some, especially among the Day 1 nauplii, ingested only one cell before dying, while others ingested more than one cell, up to six cells in the case of Day 3 nauplii, before dying. Day 3 nauplii were readily and heavily impacted by the P. lima cells. Survival analysis was used to evaluate survivorship of Day 1 to Day 3 nauplii exposed to cells of P. lima. Estimates were made of tD50s for the different age groups. Comparisons of the tD50s showed that the tD50s for Day 1 and Day 2 nauplii did not vary significantly, but they each varied significantly from the tD50 for the Day 3 nauplii. The possible ecological implications of the findings are discussed.	Univ Libre Bruxelles, Lab Oceanog Biol & Aquacultures, B-1050 Brussels, Belgium	Universite Libre de Bruxelles	Ajuzie, CC (通讯作者)，Univ Libre Bruxelles, Lab Oceanog Biol & Aquacultures, CP 160-19,Av Roosevelt 50, B-1050 Brussels, Belgium.	cajuzie@ulb.ac.be						Ajuzie C.C., 2002, THESIS U LIBRE BRUXE; Bagoien E., 1996, HARMFUL TOXIC ALGAL, P385; Barbier M, 1999, PHYCOLOGIA, V38, P41, DOI 10.2216/i0031-8884-38-1-41.1; Boyer G.L., 1985, P407; Bravo I, 2001, TOXICON, V39, P1537, DOI 10.1016/S0041-0101(01)00126-X; FIEDLER PC, 1982, LIMNOL OCEANOGR, V27, P961, DOI 10.4319/lo.1982.27.5.0961; Foden J, 2005, HARMFUL ALGAE, V4, P1063, DOI 10.1016/j.hal.2005.03.004; GILL CW, 1987, LIMNOL OCEANOGR, V27, P961; HARRINGTON DP, 1982, BIOMETRIKA, V69, P553, DOI 10.2307/2335991; HUNTLEY M, 1986, MAR ECOL PROG SER, V28, P105, DOI 10.3354/meps028105; IVES JD, 1987, J EXP MAR BIOL ECOL, V112, P131, DOI 10.1016/0022-0981(87)90113-4; KELLER MD, 1987, J PHYCOL, V23, P633; KELLY AM, 1992, ENVIRON BIOL FISH, V33, P275, DOI 10.1007/BF00005871; LANDAU M, 1985, CRUSTACEANA, V49, P318, DOI 10.1163/156854085X00657; Lush G.J., 1996, HARMFUL TOXIC ALGAL, P389; MAESTRINI SY, 1996, HARMFUL TOXIC ALGAL, P397; MASSELIN P, 1991, P S MAR BIOT CNEVA M, P93; PILLET S, 1995, P 6 INT C TOX MAR PH, P487; Prince EK, 2006, OECOLOGIA, V147, P479, DOI 10.1007/s00442-005-0274-2; QUILLIAM MA, 1995, IOC MANUALS GUIDES, V33, P95; ROBINEAU B, 1991, MAR BIOL, V108, P293, DOI 10.1007/BF01344344; Tang KW, 2001, MAR ECOL PROG SER, V209, P197, DOI 10.3354/meps209197; Teegarden G. J., 1996, HARMFUL TOXIC ALGAL, P393; UYE S, 1990, MAR ECOL PROG SER, V59, P97, DOI 10.3354/meps059097; Vismara R, 2003, J APPL PHYCOL, V15, P75, DOI 10.1023/A:1022942705496; White A.W., 1989, P395; WHITE AW, 1981, LIMNOL OCEANOGR, V26, P103, DOI 10.4319/lo.1981.26.1.0103; [No title captured], DOI DOI 10.1016/J.JASMS.2007.11.001; [No title captured]	29	26	27	1	23	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-8971			J APPL PHYCOL	J. Appl. Phycol.	OCT	2007	19	5					513	519		10.1007/s10811-007-9164-9	http://dx.doi.org/10.1007/s10811-007-9164-9			7	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	206TJ					2025-03-11	WOS:000249205500017
J	Bison, KM; Versteegh, GJM; Hilgen, FJ; Willems, H				Bison, Katarzyna-Maria; Versteegh, Gerard J. M.; Hilgen, Frits J.; Willems, Helmut			Calcareous dinoflagellate turnover in relation to the Messinian salinity crisis in the eastern Mediterranean Pissouri Basin, Cyprus	JOURNAL OF MICROPALAEONTOLOGY			English	Article						Messinian; calcareous dinoflagellates; Mediterranean; Pliocene; Miocene	EQUATORIAL ATLANTIC-OCEAN; UPPER WATER COLUMN; SURFACE SEDIMENTS; THORACOSPHAERA-HEIMII; SPATIAL-DISTRIBUTION; QUATERNARY EASTERN; POTENTIAL USE; LATE MIOCENE; LAGO-MARE; CYSTS	The extent to which the Messinian salinity crisis modified the initially Tethyan, eastern Mediterranean phytoplankton community has been investigated by monitoring the fate of calcareous dinoflagellate cyst assemblages prior to, during and after the salinity crisis in the Pissouri section (Cyprus). A rich, but low diversity open oceanic assemblage, dominated by Calciodinellum albatrosianum, is found in the upper Tortonian and lower Messinian. The upper Messinian (pre-evaporitic) sediments yield only few cysts but the assemblage is much more diverse and reflects unstable more neritic conditions (Bicarinellum tricarinelloides), fluvial influence (Leonella granifera) and varying, temporally increased salinities (Pernambugia tuberosa), probably related to the increasingly restricted environment. The basal Pliocene sediments reflect the return to normal marine conditions; the dinoflagellate assemblage is rich in cysts and again has a low diversity. However, in contrast to the C albatrosianum-dominated upper Tortonian and pre-evaporitic Messinian sediments, L. granifera clearly dominates the basal Pliocene association just after the replenishment of the Mediterranean basin. Apart from this shift in dominance, the onset of the Pliocene is furthermore marked by the first appearance of Calciodinellum elongatum, which must have immigrated from the Atlantic Ocean. Lebessphaera urania, a postulated remnant of the Tethyan Ocean survived the salinity crisis, possibly in as yet unidentified marine refuges in the Mediterranean itself. Although the environmental changes caused by the Messinian salinity crisis did not lead to an extinction of calcareous dinoflagellate species of the Pissouri Basin, it resulted in a significant change in the assemblages and contributed to a more modern character of the Pliocene dinoflagellate association in the eastern Mediterranean.	Univ Bremen, Div Palaeontol, D-28334 Bremen, Germany; Univ Hamburg, Inst Biogeochem & Meereschem, D-20146 Hamburg, Germany; Univ Utrecht, Fac Earth Sci, NL-3594 Utrecht, Netherlands	University of Bremen; University of Hamburg; Utrecht University	Bison, KM (通讯作者)，Univ Bremen, Div Palaeontol, FB 5,Geowissensch,Postfach 330440, D-28334 Bremen, Germany.	kbison@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				[Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Bianchi CN, 2000, MAR POLLUT BULL, V40, P367, DOI 10.1016/S0025-326X(00)00027-8; Blanc PL, 2002, GEODIN ACTA, V15, P303, DOI 10.1016/S0985-3111(02)01095-1; BOUCHET P, 1992, DEEP-SEA RES, V39, P169, DOI 10.1016/0198-0149(92)90103-Z; Bouillon J, 2004, SCI MAR, V68, P5, DOI 10.3989/scimar.2004.68s25; Butler RWH, 1999, J GEOL SOC LONDON, V156, P827, DOI 10.1144/gsjgs.156.4.0827; Carnevale G, 2006, J GEOL SOC LONDON, V163, P75, DOI 10.1144/0016-764904-158; Castradori Davide, 1998, Proceedings of the Ocean Drilling Program Scientific Results, V160, P113; 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Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	87	3	4	0	9	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	OCT	2007	26		2				103	116		10.1144/jm.26.2.103	http://dx.doi.org/10.1144/jm.26.2.103			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	231YZ		hybrid			2025-03-11	WOS:000250986400002
J	Figueroa, RI; Garcés, E; Bravo, I				Figueroa, Rosa Isabel; Garces, Esther; Bravo, Isabel			Comparative study of the life cycles of <i>Alexandrium tamutum</i> and <i>Alexandrium minutum</i> (Gonyaulacales, Dinophyceae) in culture	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium minutum; Alexandrium tamutum; cysts; dinoflagellates; encystment; excystment; flow cytometry; nitrogen; phosphorus; sexual reproduction	GYMNODINIUM-NOLLERI DINOPHYCEAE; SEXUAL REPRODUCTION; TAYLORI DINOPHYCEAE; DINOFLAGELLATE; TAMARENSIS; CATENELLA; ENCYSTMENT; CYST; EXCYSTMENT; MORPHOLOGY	The microalgal genus Alexandrium includes species known to produce paralytic shellfish poisoning (PSP). Due to the importance of discriminating between HAB-forming species, we compared the undescribed life-cycle pattern of Alexandrium tamutum Montresor, Beran et U. John and of its toxic relative Alexandrium minutum Halim. Sexual stages, asexual and sexual division, mating type, and nuclear morphology were studied in both species. Sexual cysts are known to be morphologically identical. However, the relative size of the U-shaped nucleus may be used to differentiate between the cysts of these species since DNA packaging in the resting cysts was lower in A. tamutum than in A. minutum, species in which the planozygote nucleus was reduced to half its volume prior to encystment. The dormancy period of the cysts was < 20 d for A. tamutum, but longer than 1 month for A. minutum. In both species, cyst appearance needed to be explained by the existence of more than two sexual types (+/-), which indicates a complex heterothallic mating type. However, planozygotes of both species may divide instead of encysting. This characteristic was used for nutritional and heritage studies. Isolated planozygotes of both species encysted in larger percentages in medium deficient in both nitrates and phosphates (L/15) than in medium without phosphates added (L-P), a medium in which most planozygotes neither divide nor encyst. Parental strains of A. minutum with and without the ventral pore formed planozygotes and, later, offspring with the ventral pore, although apparently smaller than usual. A synchronization-flow cytometry method for discriminating diploids formed by sexual fusion (planozygotes) from cells with 2C DNA content resulting from self-duplication of DNA (dividing cells) was described. The results indicated that the maximum percentage of A. minutum planozygotes (20%) was achieved only 3 to 5 d after crossing the parental strains, and that light might not be needed for the sexual fusion and formation of planozygotes.	Inst Oceanog Vigo, Vigo 36200, Spain; IRTA, San Carlos de la Rapita, Spain	Spanish Institute of Oceanography; IRTA	Figueroa, RI (通讯作者)，Inst Oceanog Vigo, Cabo Estai Canido, Vigo 36200, Spain.	figueroa@icm.csic.es	Bravo, Isabel/D-3147-2012; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015	Garces, Esther/0000-0002-2712-501X; Bravo, Isabel/0000-0003-3764-745X; Figueroa, Rosa/0000-0001-9944-7993				ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; [Anonymous], 1996, Harmful and Toxic Algal Blooms; [Anonymous], IOC TAXONOMIC REFERE; Balech E., 1995, Sherkin Island Marine Station. 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Phycol.	OCT	2007	43	5					1039	1053		10.1111/j.1529-8817.2007.00393.x	http://dx.doi.org/10.1111/j.1529-8817.2007.00393.x			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	215RT					2025-03-11	WOS:000249827400017
J	Sabot, HK				Sabot, H. K.			Significant dinoflagellate cyst biohorizons in the upper cretaceous-palaeocene succession of the Khasi Hills, Meghalaya	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Editorial Material											Sabot, HK (通讯作者)，AMD Complex, Hyderabad 500016, Andhra Pradesh, India.	sabothk_60@yahoo.co.in							0	0	0	0	1	GEOLOGICAL SOC INDIA	BANGALORE	#64 12TH CROSS, BASAPPA LAYOUT P B 1922, GAVIPURAM PO, BANGALORE 560019, INDIA	0016-7622			J GEOL SOC INDIA	J. Geol. Soc. India	OCT	2007	70	4					676	677						2	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	259KL					2025-03-11	WOS:000252938100016
J	Subrahmanyam, AV; Nayak, S				Subrahmanyam, A. V.; Nayak, S.			Significant dinoflagellate cyst biohorizons in the upper cretaceous-palaeocene succession of the Khasi Hills, Meghalaya	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Editorial Material							NORTHEASTERN INDIA		[Subrahmanyam, A. V.; Nayak, S.] AMD ER DAE, Hyderabad 500016, Andhra Pradesh, India	Atomic Minerals Directorate for Exploration & Research (AMD)	Subrahmanyam, AV (通讯作者)，AMD ER DAE, Hyderabad 500016, Andhra Pradesh, India.							Ali M.A., 1982, REC GEOL SURV INDIA, V112, P17; [Anonymous], 1975, Sedimentation models and quantitative stratigraphy Developments in Sedimentology; [Anonymous], 1962, Bulletin of the Geological Mining and Metallurgical Society of India, V25, P1; BAKSI AK, 1995, CHEM GEOL, V121, P73, DOI 10.1016/0009-2541(94)00124-Q; BALASUNDARAM, 1972, REC GEOL SURV INDIA, V104, P1; Bhattacharya A., 1987, Three Decades of Developments in Palaeontology and Stratigraphy in India, 1 (Precambrian to Mesozoic), V11, P367; CHAKRABORTY A, 1972, QUAT J GEOL MIN META, V44, P107; DASGUPTA AB, 2000, GEOLOGY ASSAM GEOL S; GARG R, 1995, CURR SCI, V66, P1012; GRANSTEIN F, 2004, GEOLOGICAL TIME SCAL, P847; HABIB D, 1977, STRATIGRAPHIC MICROP; JAIN KP, 1975, PALEOBOTANIST, V22, P1; Kak SN, 2002, J GEOL SOC INDIA, V60, P151; Kar RK, 2006, J GEOL SOC INDIA, V67, P180; NANDI B, 1990, REV PALAEOBOT PALYNO, V65, P119, DOI 10.1016/0034-6667(90)90063-O; PANDEY J, 1973, P 2 IND COLL MICR ST, P77; Poornachandra Rao G. V. S., 1993, GONDWANA GEOLOGICAL, P163; RADHA DR, 1998, J GEOL SOC INDIA, V60, P151; RAO GVS, 2000, MEM GEOL SOC INDIA, V46, P355; SABOT HK, 2001, REPORT SOME ASPECTS; Sen DB., 2002, EXPLOR RES ATOM MINE, V14, P29; Williams G.L., 1985, P847	22	0	0	0	3	GEOLOGICAL SOC INDIA	BANGALORE	#64 12TH CROSS, BASAPPA LAYOUT P B 1922, GAVIPURAM PO, BANGALORE 560019, INDIA	0016-7622			J GEOL SOC INDIA	J. Geol. Soc. India	OCT	2007	70	4					678	678						1	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	259KL					2025-03-11	WOS:000252938100017
J	Novichkova, EA; Polyakova, EI				Novichkova, E. A.; Polyakova, E. I.			Dinoflagellate cysts in the surface sediments of the White Sea	OCEANOLOGY			English	Article							ARCTIC-OCEAN; ASSEMBLAGES; INDICATORS; NUTRIENTS; ATLANTIC; LAPTEV; WATER	Dinoflagellate cysts were studied in 42 samples from the surface sediments of the White Sea. The total concentration of dinocysts varies from single cysts to 25000 cyst/g of dry sediments, which reflects the biological productivity in the White Sea waters and the regional particular features of the sedimentation processes. The highest concentrations are observed in silts; they are related to the regions of propagation of the highly productive Barents Sea waters in the White Sea. Generally, the spatial distribution of dinocysts species in the surface sediments corresponds to the distribution of the major types of water masses in the White Sea. The cysts of the relatively warm-water species (Operculodinium centrocarpum, Spiniferites sp.) of North Atlantic origin that dominate in the sediments indicate an intensive intrusion of the Barents Sea water masses to the White Sea along with hydrological dwelling conditions in the White Sea favorable for the development of these species during their vegetation period. The cold-water dinocyst assemblage (Islandinium minutum, Polykrikos sp.) is rather strictly confined to the inner parts of shallow-water bays, firstly, those adjacent to the Onega and Severnaya Dvina river mouths.	[Novichkova, E. A.] Russian Acad Sci, Shirshov Inst Oceanol, Moscow, Russia; [Polyakova, E. I.] Moscow MV Lomonosov State Univ, Fac Geog, Moscow, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; Lomonosov Moscow State University	Novichkova, EA (通讯作者)，Russian Acad Sci, Shirshov Inst Oceanol, Moscow, Russia.	enovichkova@mail.ru	Polyakova, Yelena/L-8889-2015; Novichkova, Ekaterina/AAC-4726-2019; Novichkova, Ekaterina/B-5807-2017	Novichkova, Ekaterina/0000-0001-5687-1719				[Anonymous], 1999, LAND OCEAN SYSTEMS S; [Anonymous], POLAR OCEANS THEIR R, DOI DOI 10.1029/GM085P0005; [Anonymous], 1971, POLLEN SPORES; BARSS MS, 1973, PALYNOLOGY NANNOFOSS; Berger V., 2001, White Sea. Ecology and Environment; Berger V. Ya., 2000, Berichte zur Polarforschung, P3; Bobrov Yu. A., 1995, WHITE SEA BIOL RES 1, P92; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Dobrovol'skii A.D., 1982, The USSR Seas; DODGE JD, 1994, REV PALAEOBOT PALYNO, V84, P169, DOI 10.1016/0034-6667(94)90049-3; Fedorova VD., 2003, PHYTOPLANKTON WHITE; GLUKHOVSKOI BK, 1991, SEAS USSR HYDROMETEO; Gordeev VV, 1996, AM J SCI, V296, P664, DOI 10.2475/ajs.296.6.664; ILYASH LV, 1999, VESTNIK MOSK UN TA S, V16, P24; KISELEV IA, 1957, MATER KOMPLEKSNOMU I, P282; KONIOVALOVA GV, 1998, DINOFLAGELLATES DINO; KOSHECHKIN BI, 1976, NATURE ECONOMY N, P3; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; KUZNETSOV LL, 2003, PHYTOCOENOSES BARENT; LISITSYN AP, 2003, URGENT PROBLEMS OCEA, P554; LISITZIN AP, 1994, OKEANOLOGIYA+, V34, P735; MAKSIMOVA MP, 1978, OKEANOLOGIYA+, V18, P58; MAKSIMOVA MP, SEAS USSR HYDROMETEO, V2, P8; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie PJ, 2001, J QUATERNARY SCI, V16, P595, DOI 10.1002/jqs.660; NALETOVA IA, 1994, MULTIDISCIPLINARY ST, P76; Nevesskii E. N., 1977, White Sea. Sedimentogenesis and Development History in the Holocene; Okolodkov YU.B., 2000, THESIS; Pantyulin AN, 2003, OCEANOLOGY+, V43, pS1; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Polyakova EI, 2003, OCEANOLOGY+, V43, pS144; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rat'kova T. N., 2000, BER POLARFORSCHUNG, V359, P97; RATKOVA TM, 2000, BERICHTE POLARFORSCH, V359, P23; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; SCHCHERBAKOV FA, 2001, GEOECOLOGY SHELF COA; Semina G. I., 1983, EKOLOGIYA FIZIOLOGIY, P3; Semina HJ, 1997, ADV MAR BIOL, V32, P527; SERGEEVA OM, 1972, PHYTOPLANKTON STUDIE, P82; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; Zhitina L. S., 1990, BIOL MONITORING PRIB, V41-49; 1995, WHITE SEA BIOL RESOU	47	13	13	0	5	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370			OCEANOLOGY+	Oceanology	OCT	2007	47	5					660	670		10.1134/S0001437007050086	http://dx.doi.org/10.1134/S0001437007050086			11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	245XD					2025-03-11	WOS:000251971200008
J	Akgün, F; Kayseri, MS; Akkiraz, MS				Akgun, Funda; Kayseri, Mine Sezgul; Akkiraz, Mehmet Serkan			Palaeoclimatic evolution and vegetational changes during the Late Oligocene-Miocene period in Western and Central Anatolia (Turkey)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						palaeoctimate; palaeovegetation; palynoflora; coexistence approach; Turkey	NEOGENE DEPOSITS; BORATE DEPOSITS; BASIN; LIGNITE	Neogene basins are widespread in Turkey and contain important lignite deposits. In this study, we reconstruct quantitatively the Late Oligocene-Miocene climate evolution in western and central Anatolia by applying the Coexistence Approach to the palynofloras obtained from the published literatures and ongoing studies. The Coexistence Approach results show that sedimentation occurred mainly under warm subtropical climatic conditions during the Chattian and Aquitanian period in western Anatolia (16.5-21.3 degrees C mean annual temperature (MAT) and 5.5-13.3 degrees C mean temperature of coldest month (CMT)). Rare occurrences of dinoflagellate cysts in the Chattian and Aquitanian indicates a marine influence. After the regression of the sea during the Burdigalian period, climate becomes cooler due to a decrease of the Palacotropical/Arctotertiary-ratio during the latest Burdigalian-Langhian. Vegetation developed under terrestrial conditions, which had started in the Burdigalian time in western and central Anatolia and continued to the early-middle Serravallian period. The climate was subtropical in western and central Anatolia during the early-late Serravalian (17.2 to 20.8 degrees C for MAT and 9.6 to 13.1 degrees C for CMT). Besides, increase of the CMT and MAT values in western and central Anatolia supports the latest Chattian-earliest Aquitanian warming and Middle Miocene climatic optimum being also globally observed. Warm temperate climatic conditions are observed in the Late Miocene. During the early-middle Tortonian, the values are 15.6 to 20.8 degrees C for the MAT, 5.5 to 13.3 degrees C for the CMT and 823 and 1520 mm for the mean annual precipitation (MAP). They had experienced dry seasons due to lower boundary of MAP lying at 823 mm during the middle-late Tortonian. The palaeotopography of central Anatolia was higher, compared to that of western Anatolia during the Middle-Late Miocene as indicated by a rich species diversification in mountain forests. This study provides the first quantitative model for Late Oligocene-Miocene palaeoclimatic evolution in western and central Anatolia. (C) 2007 Published by Elsevier B.V.	Dokuz Eylul Univ, Dept Geol Engn, TR-35100 Bornova, Turkey	Dokuz Eylul University	Akgün, F (通讯作者)，Dokuz Eylul Univ, Dept Geol Engn, TR-35100 Bornova, Turkey.	funda.akgun@deu.edu.tr; sezgul.kayseri@ogr.deu.edu.tr; serkan.akkiraz@deu.edu.tr	Akgün, Funda/AAC-2859-2020; akkiraz, mehmet/ADP-2366-2022; Kayseri Ozer, Mine Sezgul/KIJ-4911-2024	Kayseri Ozer, Mine Sezgul/0000-0003-2712-2457; Akgun, Funda/0000-0002-6028-6704				AKGUN F, 1987, Turkiye Jeoloji Kurumu Bulteni, V30, P35; Akgün F, 1999, GEOBIOS-LYON, V32, P367, DOI 10.1016/S0016-6995(99)80013-8; Akgün F, 2001, GEODIN ACTA, V14, P71, DOI 10.1016/S0985-3111(00)01054-8; AKGUN F, 1986, Turkiye Jeoloji Kurumu Bulteni, V29, P13; Akgun F., 1995, Turkiye Petrol Jeologlari Dernegi Bulteni, V6, P51; Akgun F, 2004, NECLIME ANN M ISL CR, P7; AKGUN F, 2002, TURKISH J EARTH SCI, V11, P1; Akgun Funda, 2000, Turkish Journal of Earth Sciences, V9, P57; AKYOL E, 1990, MADEN TETKIK ARAMA D, V11, P165; [Anonymous], 1993, Bull. Geol. Soc. 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Paleoclimatol. Paleoecol.	SEP 14	2007	253	1-2					56	+		10.1016/j.palaeo.2007.03.034	http://dx.doi.org/10.1016/j.palaeo.2007.03.034			33	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	218DM					2025-03-11	WOS:000249996200005
J	Iakovleva, AI; Heilmann-Clausen, C				Iakovleva, Alina I.; Heilmann-Clausen, Claus			<i>Wilsonidium pechoricum</i> new species -: A new dinoflagellate species with unusual asymmetry from the Paleocene/Eocene transition	JOURNAL OF PALEONTOLOGY			English	Article							THERMAL MAXIMUM; PALEOGENE; KAZAKSTAN; CYSTS	Fossil dinoflagellates, when asymmetrical, almost always have features such as antapical horns on the right side reduced relative to features on the left side. A new species here described, Wilsonidium pechoricum, is therefore unusual in having a reduced left antapical horn. W. pechoricum seems to have originated in the northern Tethys in the latest Palcocene. It subsequently spread northwards and became widely distributed in the Peri-Tethys and parts of the Arctic region during the short interval known as the Initial Eocene Thermal Maximum (IETM). The new species was probably favored by extraordinary paleoecological conditions (high sea-surface temperatures and probably also high nutrient levels) prevailing in neritic waters of the IETM; a time during which aberrant morphotypes were also recorded among other planktonic protists. The apparent absence of W pechoricum from the North Atlantic region suggests that the Turgay Strait may have functioned as a waterway between the Arctic and Peri-Tethys during the IETM. W. pechoricum is the oldest species of the genus Wilsollidium and possibly descended from the genus Apectodinium. Its early appearance points to a Late Paleocene radiation of the Wetzelielloideae before the well-known Early Eocene radiation in the subfamily, and its morphology is in accordance with a monophyletic origin of the group.	Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; Russian Acad Sci, Inst Geol, Moscow 109017, Russia	Aarhus University; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences	Iakovleva, AI (通讯作者)，Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark.	iakovl@yahoo.com; claus.heilmann@geo.au.dk	IAKOVLEVA, ALINA/ABH-9243-2020; Heilmann-Clausen, Claus/A-4848-2012					AKHMETEV MA, 1996, ISKOPAEMYE ORGANIZMY, P55; Alberti G., 1961, Palaeontographica, V116, P1; AUBRY MP, 2003, CAUSES CONSEQUENCES, P551; AUBRY MP, 2000, UPPER PALEOCENE LOWE, V122, P15; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Baschli O., 1885, WISSENSCHAFTLICH DAR, P865; Berggren WA, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P1; BERGH R. 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Paleontol.	SEP	2007	81	5					1020	1030		10.1666/pleo05-120.1	http://dx.doi.org/10.1666/pleo05-120.1			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	210NP					2025-03-11	WOS:000249463200015
J	Park, TG; Bolch, CS; Hallegraeff, GM				Park, Tae-Gyu; Bolch, Christopherj. S.; Hallegraeff, Gustaaf M.			Larval <i>Crassostrea</i> bivalve and <i>Artemia</i> brine shrimp bioassays to assess toxicity and micropredation by the heterotrophic dinoflagellates <i>Cryptoperidiniopsis brodyi</i> and <i>Pfiesteria piscicida</i> from Australian waters	JOURNAL OF PLANKTON RESEARCH			English	Article							ESTUARINE DINOFLAGELLATE; LIFE-CYCLE; PROTOGONYAULAX-TAMARENSIS; INVERTEBRATE LARVAE; ATLANTIC MENHADEN; FISH BIOASSAY; DINOPHYCEAE; BEHAVIOR; SHUMWAYAE; PREY	The capability of the heterotrophic Australian marine dinoflagellates Cryptoperidiniopsis brodyi and Pfiesteria piscicida to impact on larval Pacific oyster (Crassostrea gigas) and brine shrimp) (Artemia salina) nauplii was investigated. An attractant response of the heterotrophs toward actively swarming Artemia was not observed and no mortality occurred. In contrast, the dinoflagellates became active and exhibited attacking) behavior toward planktonic oyster larvae (below 1 mm size) within a few seconds. The oyster larvae survived 2500 cells mL(-1) for 2 days, but mortality increased to 82-88% by day 12. Aqueous dinoflagellate cell extracts collected from. the bioassay that induced oyster kills were tested in a further larval bivalve bioassay but no mortality was observed. Oyster over 2 mm in size survived the physical attack by the heterotrophs and remained alive during the bioassay period. Changes in zoospore and cyst abundances in the presence of oyster larvae were also documented. More actively swarming zoospores and 2.5-fold higher cell numbers were produced in the presence of oysters compared to control cultures. These results indicate that mortalities of the planktonic larvae can be induced by micro-predatory feeding behavior of C. brodyi and P. piscicida.	Univ Tasmania, Dept Plant Sci, Hobart, Tas 7001, Australia; Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia	University of Tasmania; University of Tasmania	Hallegraeff, GM (通讯作者)，Univ Tasmania, Dept Plant Sci, Private Bag 55, Hobart, Tas 7001, Australia.	hallegraeff@utas.edu	Bolch, Christopher/J-7619-2014; Hallegraeff, Gustaaf/C-8351-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343				Alavi M, 2001, ENVIRON MICROBIOL, V3, P380, DOI 10.1046/j.1462-2920.2001.00207.x; Alavi MR, 2004, MICROBIAL ECOL, V47, P48, DOI 10.1007/s00248-003-1018-7; BEAN B, 1979, J CELL BIOL, V83, P351; Berry JP, 2002, P NATL ACAD SCI USA, V99, P10970, DOI 10.1073/pnas.172221699; Blaise C, 1998, MICROSCALE TESTING IN AQUATIC TOXICOLOGY, P1; Blazer V.S., 2000, MAR ENVIRON RES, V50, P487; Blazer VS, 1999, J AQUAT ANIM HEALTH, V11, P340, DOI 10.1577/1548-8667(1999)011<0340:AAACOU>2.0.CO;2; Bougrier S, 2003, AQUAT LIVING RESOUR, V16, P347, DOI 10.1016/S0990-7440(03)00080-9; BRICELJ VM, 1991, MAR ECOL PROG SER, V74, P33, DOI 10.3354/meps074033; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P667, DOI 10.2307/3454912; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P745, DOI 10.2307/3454922; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; BURKHOLDER JM, 1995, ARCH PROTISTENKD, V145, P177, DOI 10.1016/S0003-9365(11)80314-3; BURKHOLDER JM, 2005, P NATL ACAD SCI USA, V99, P10970; BURTON DT, 1990, B ENVIRON CONTAM TOX, V44, P776, DOI 10.1007/BF01701802; Buskey EJ, 1997, MAR ECOL PROG SER, V153, P77, DOI 10.3354/meps153077; Cancellieri PJ, 2001, J EXP MAR BIOL ECOL, V264, P29, DOI 10.1016/S0022-0981(01)00299-4; Coats DW, 2002, J PHYCOL, V38, P417, DOI 10.1046/j.1529-8817.2002.03832.x; DRGON T, 2005, APPL ENVIRON MICROB, V67, P191; GAINEY LF, 1988, COMP BIOCHEM PHYS C, V91, P159, DOI 10.1016/0742-8413(88)90182-X; Hauser D. 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Plankton Res.	SEP	2007	29	9					791	801		10.1093/plankt/fbm060	http://dx.doi.org/10.1093/plankt/fbm060			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	213IH		Bronze			2025-03-11	WOS:000249659600006
J	Orlova, TY; Selina, MS; Lilly, EL; Kulis, DM; Anderson, DM				Orlova, Tatiana Y.; Selina, Marina S.; Lilly, Emily L.; Kulis, David M.; Anderson, Donald M.			Morphogenetic and toxin composition variability of <i>Alexandrium tamarense</i> (Dinophyceae) from the east coast of Russia	PHYCOLOGIA			English	Article						Alexandrium tamarense; distribution; far eastern seas of Russia; LSU rRNA; morphology; PSP; toxicity	DINOFLAGELLATE PROTOGONYAULAX-TAMARENSIS; NORTH-AMERICAN; SPECIES COMPLEX; RED TIDE; POPULATIONS; GONYAULAX; WATERS; MORPHOLOGY; STRAINS	Twenty-seven clones were established from elongate Alexandrium sp. cysts collected in six regions along the Russian Pacific coast. All isolates were identified as Alexandrium tamarense via detailed epifluoresence microscopy of thecal plates. Morphological differences of both cultured and wild cells from the study regions mainly occurred in the shape of the cell (length/width ratio), degree of development of the sulcal list, and the shape of the posterior sulcal (S.p.) and second antapical (2) plates. Cells were divided into two cell types: 'short' (isodiametrical or wide) and 'tall'. Each cell type exhibits specific features of tabulation, mainly the shape of the S.p. and 2 plates and was dominant in each particular region of the study. The short type, with a wide S.p. and reduced length in the dorsoventral 2 plates, was characteristic of A. tamarense from Primorye and southern Sakhalin Island. The tall cells, i.e., with cell length exceeding width, and having and elongate S.p. and dorsoventrally elongate 2 plates, prevailed in Avachinskaya Guba Inlet and in the Bering Sea. The differences reported here between the two types are within the range of morphological variability of A. tamarense sensu Balech, 1995. The D1-D2 fragment of the large subunit nuclear ribosomal DNA was analyzed for 24 clones. Alexandrium tamarense from the Russian Pacific coast compose three genetically distinct populations that correspond to the Japanese temperate Asian, eastern North American, and western North American ribotypes of the 'tamarensis' complex. The presence and distribution of eastern and western North American ribotypes along the Russian Pacific coast suggest that dispersion to the temperate Asian region occurred long ago via natural cur-rents and processes, and not through human-mediated introductions, as has been proposed. No strict correlation was observed between different morphological types of cells and ribotypes. High-performance liquid chromatography toxin analyses showed that all isolates were toxic and demonstrated variability in toxin content and composition among different populations. These data document the significant and previously uncharacterized risk of shellfish contamination with paralytic shellfish poisoning toxins from blooms of A. tamarense in Russian marine waters.	Russian Acad Sci, Far E Branch, AV Zhirmunsky Inst Marine Biol, Vladivostok 690041, Russia; Harvard Univ, Dept Organism & Evolut Biol, Cambridge, MA 02360 USA; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences; Harvard University; Woods Hole Oceanographic Institution	Orlova, TY (通讯作者)，Russian Acad Sci, Far E Branch, AV Zhirmunsky Inst Marine Biol, Vladivostok 690041, Russia.	torlova@imb.dvo.ru	Selina, Marina/AAM-6847-2021; Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967				Anderson D.M., 1989, P11; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Balech E., 1985, P33; Balech E., 1995, Sherkin Island Marine Station; BOYER GL, 1987, MAR BIOL, V96, P123, DOI 10.1007/BF00394845; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; CEMBELLA AD, 1988, BOT MAR, V31, P39, DOI 10.1515/botm.1988.31.1.39; Delgado M, 1997, J PLANKTON RES, V19, P749, DOI 10.1093/plankt/19.6.749; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1985, B MAR SCI, V37, P529; FUKUYO Y, 1985, TOXIC DINOFLAGELLATE, P51; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hall S., 1982, THESIS U ALASKA; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; Hansen G, 2003, HARMFUL ALGAE, V2, P317, DOI 10.1016/S1568-9883(03)00060-X; KIM CH, 1993, NIPPON SUISAN GAKK, V59, P641, DOI 10.2331/suisan.59.641; Kim Keun-Yong, 2002, Algae, V17, P11; KISSELEV IA, 1959, ISSLEDOVANIYA DALNEV, V6, P58; KONOVALOVA G V, 1989, Botanicheskii Zhurnal (St. Petersburg), V74, P1401; KONOVALOVA G V, 1991, Botanicheskii Zhurnal (St. Petersburg), V76, P79; Konovalova G.V., 1993, Harmful Algae News, V4, P2; Konovalova G. 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S., 2001, Botanicheskii Zhurnal (St. Petersburg), V86, P22; SELINA MS, 2005, RUSSIAN J MARINE BIO, V3, P187; Taylor F.J. R., 1984, SEAFOOD TOXINS, P77; TAYLOR FJR, 1975, ENVIRON LETT, V9, P103, DOI 10.1080/00139307509435840; Yoshida Makoto, 2000, Bulletin of Plankton Society of Japan, V47, P34	49	43	49	0	21	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	SEP	2007	46	5					534	548		10.2216/06-17.1	http://dx.doi.org/10.2216/06-17.1			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	208XX					2025-03-11	WOS:000249353600005
J	Attaran-Fariman, G; Bolch, CJS				Attaran-Fariman, Gilan; Bolch, Christopher J. S.			<i>Scrippsiella irregularis</i> sp nov (Dinophyceae), a new dinoflagellate from the southeast coast of Iran	PHYCOLOGIA			English	Article						Scrippsiella; resting cyst; DNA; phylogeny; rDNA-ITS; Iran; Oman sea	RECENT MARINE-SEDIMENTS; CYSTS; PERIDINIALES; TROCHOIDEA; MORPHOLOGY; DIVERSITY; TASMANIA; ECOLOGY	A new species of Scrippsiella is described by light and electron microscopy from laboratory cultures established from resting cysts collected from the southeast coast of Iran. Comparative morphological analyses and sequencing of the rDNA-ITS and 5.8S rDNA show that the new species, Scrippsiella irregularis sp. nov., is allied to but distinct from Scrippsiella precaria and S. ramonii. Vegetative cells of the new species are similar in size, shape, and plate tabulation to S. precaria; however, the cingulum is equatorially placed, the nucleus is in the hypocone, and the second anterior intercalary plate is larger and rounded rather than diamond-shaped. The resting cysts isolated from sediments and produced in laboratory cultures are spherical to ovoid with numerous pointed to slightly capitate calcareous processes.	Univ Tasmania, Sch Aquaculture, Launceston, Tasmania 7250, Australia	University of Tasmania	Attaran-Fariman, G (通讯作者)，Univ Tasmania, Sch Aquaculture, Locked Bag 1370, Launceston, Tasmania 7250, Australia.	gilanattaran@ifro.ir	Bolch, Christopher/J-7619-2014; Attaran Fariman, Gilan/ABC-4059-2021					ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; [Anonymous], 2002, PHYLOGENETIC ANAL US; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BOLCH CJ, 1998, HARMFUL MICROALGAE, P283; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1992, DINOFLAGELLATE CONTR, P1; Faust MA, 1998, PHYCOLOGIA, V37, P47, DOI 10.2216/i0031-8884-37-1-47.1; Faust MA, 1996, J PHYCOL, V32, P669, DOI 10.1111/j.0022-3646.1996.00669.x; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Fensome R. A., 1993, CLASSIFICATION LIVIN; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Gottschling M, 2005, EUR J PHYCOL, V40, P207, DOI 10.1080/09670260500109046; Hall TA., 1999, NUCL ACIDS S SERIES, V41, P95, DOI [DOI 10.1021/BK-1999-0734.CH008, DOI 10.14344/IOC.ML.11.1]; HILLIS DM, 1992, J HERED, V83, P189, DOI 10.1093/oxfordjournals.jhered.a111190; HONSELL G, 1991, BOT MAR, V34, P167, DOI 10.1515/botm.1991.34.3.167; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; Jeanmougin F, 1998, TRENDS BIOCHEM SCI, V23, P403, DOI 10.1016/S0968-0004(98)01285-7; KOBAYASHI S, 1995, J PHYCOL, V31, P147, DOI 10.1111/j.0022-3646.1995.00147.x; Kremp A, 2005, J PHYCOL, V41, P629, DOI 10.1111/j.1529-8817.2005.00070.x; LARSEN J, 1995, PHYCOLOGIA, V34, P135, DOI 10.2216/i0031-8884-34-2-135.1; MARCHANT HJ, 1983, J MICROSC-OXFORD, V131, P127, DOI 10.1111/j.1365-2818.1983.tb04239.x; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 2003, PHYCOLOGIA, V42, P56, DOI 10.2216/i0031-8884-42-1-56.1; MONTRESOR M, 1988, PHYCOLOGIA, V27, P387, DOI 10.2216/i0031-8884-27-3-387.1; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; NATION JL, 1983, STAIN TECHNOL, V58, P347, DOI 10.3109/10520298309066811; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7	30	17	20	0	1	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	SEP	2007	46	5					572	582		10.2216/07-02.1	http://dx.doi.org/10.2216/07-02.1			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	208XX					2025-03-11	WOS:000249353600008
J	Gussone, N; Zonneveld, K; Kuhnert, H				Gussone, N.; Zonneveld, K.; Kuhnert, H.			Trace element and Ca isotope ratios in calcareous dinoflagellate cysts of <i>Thoracosphaera heimii</i>	GEOCHIMICA ET COSMOCHIMICA ACTA			English	Meeting Abstract	17th Annual V M Goldschmidt Conference	AUG, 2007	Cologne, GERMANY				FRACTIONATION		Univ Bremen, D-28159 Bremen, Germany; Univ Munster, Inst Mineral, D-48149 Munster, Germany; RCOM, D-28159 Bremen, Germany	University of Bremen; University of Munster		nikolaus.gussone@uni-muenster.de; zonnev@uni-bremen.de; hkuhnert@uni-bremen.de						Böhm F, 2006, GEOCHIM COSMOCHIM AC, V70, P4452, DOI 10.1016/j.gca.2006.06.1546; Gussone N, 2006, GEOLOGY, V34, P625, DOI 10.1130/G22733.1; Hildebrand-Habel T, 2000, INT J EARTH SCI, V88, P694, DOI 10.1007/s005310050298; ZONNEVELD, IN PRESS MARINE MICR; Zonneveld K, 2004, MAR MICROPALEONTOL, V50, P307, DOI 10.1016/S0377-8398(03)00097-5	5	0	0	0	5	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0016-7037			GEOCHIM COSMOCHIM AC	Geochim. Cosmochim. Acta	AUG	2007	71	15		S			A364	A364						1	Geochemistry & Geophysics	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	200VC					2025-03-11	WOS:000248789900738
J	Bolch, CJS; de Salas, MF				Bolch, Christopher J. S.; de Salas, Miguel F.			A review of the molecular evidence for ballast water introduction of the toxic dinoflagellates <i>Gymnodinium catenatum</i> and the <i>Alexandrium</i> "<i>tamarensis</i> complex" to Australasia	HARMFUL ALGAE			English	Review						harmful algae; dinoflagellate; Alexandrium; Gymnodinium catenatum; ballast water; RAPD-PCR; rDNA; ITS; single nucleotide; polymorphism; global dispersal; evolution; palaeogeography	RECENT MARINE-SEDIMENTS; GENUS ALEXANDRIUM; RESTING CYSTS; MICRORETICULATE CYST; SEQUENCE COMPARISONS; DINOPHYCEAE STRAINS; SURFACE SEDIMENTS; WESTERN PACIFIC; GENETIC-MARKERS; COASTAL WATERS	The potential of ballast water to act as a major introduction vector for toxic dinoflagellates and other phytoplankton is beyond doubt; however, evidence that links the suspected introduced species with a source population is less convincing, especially without supporting historical and biochemical data, or consideration of palaeobiogeographical scenarios that may explain current species distributions. This paper presents new molecular data based on LSU-rDNA and rDNA-ITS sequences that demonstrate an unequivocal and recent link between Temperate Asian and Australasian populations of the toxic dinoflagellates Gymnodinium catenatum and toxic strains of the Alcxandrium "tamarensis complex". We integrate our data with supporting evidence from historical distribution records, sediment dating studies, toxin profiles, mating studies and previous molecular studies. We contrast the observed patterns of genetic and biochemical variation with those expected from various palaeobiogeographical scenarios explaining the evolution and natural dispersal of both species. While definitive proof is impossible, the total evidence indicates that these toxic dinoflagellates were introduced to Australasia during the past 100 years, most probably via ballast water from bulk-cargo shipping from Japan and/or south-east Asia. (C) 2007 Elsevier B.V. All rights reserved.	Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	University of Tasmania; University of Tasmania	Bolch, CJS (通讯作者)，Univ Tasmania, Sch Aquaculture, Locked Bag 1370, Launceston, Tas 7250, Australia.	chris.bolch@utas.edu.au	Bolch, Christopher/J-7619-2014					ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; Amorim A, 2006, AFR J MAR SCI, V28, P193, DOI 10.2989/18142320609504146; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; [Anonymous], 2004, Modeltest v2; ANTON A, 1996, NATO ASI WORKSH PHYS, P1996; BALECH E., 1964, BOL INST BIOL MAR MAR DEL PLATA, V4, P1; Band-Schmidt C, 2006, J PHYCOL, V42, P757, DOI 10.1111/j.1529-8817.2006.00234.x; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; BOLCH CJ, 1998, HARMFUL MICROALGAE, P283; Bolch CJS, 1999, J PHYCOL, V35, P356, DOI 10.1046/j.1529-8817.1999.3520356.x; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; CARRADA GC, 1991, J PLANKTON RES, V13, P229, DOI 10.1093/plankt/13.1.229; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Coleman AW, 2000, PROTIST, V151, P1, DOI 10.1078/1434-4610-00002; DALE B, 1993, DEV MAR BIO, V3, P47; DESALAS MF, 2001, HARMFUL ALGAL BLOOMS, P214; Doblin MA, 2004, APPL ENVIRON MICROB, V70, P6495, DOI 10.1128/AEM.70.11.6495-6500.2004; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; ESTRADA M, 1984, INVEST PESQ, V48, P31; Fabry S, 1999, J MOL EVOL, V48, P94, DOI 10.1007/PL00006449; Finlay BJ, 2002, SCIENCE, V296, P1061, DOI 10.1126/science.1070710; Forbes E., 2001, P 15 DIAT S, P509; Franca S., 1989, P93; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1993, DEV MAR BIO, V3, P875; Giannakourou A, 2005, CONT SHELF RES, V25, P2585, DOI 10.1016/j.csr.2005.08.003; Godhe Anna, 1996, Harmful Algae News, V15, P1; Gomez Fernando, 2001, Harmful Algae News, V22, P1; Graham Herbert W, 1943, TRANS AMER MICROSC SOC, V62, P259, DOI 10.2307/3223028; Green DH, 2004, FEMS MICROBIOL ECOL, V47, P345, DOI 10.1016/S0168-6496(03)00298-8; HADA Y, 1967, B SUZUGAMINE WOMENS, V13, P1; Hallegraeff G., 1988, Australian Fisheries, V47, P32; Hallegraeff G, 2006, ECOL STU AN, V189, P379, DOI 10.1007/978-3-540-32210-8_29; Hallegraeff G., 1986, Australian Fisheries, V45, P15; Hallegraeff G.M., 1989, P77; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1988, J PLANKTON RES, V10, P533, DOI 10.1093/plankt/10.3.533; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Higman WA, 2001, PHYCOLOGIA, V40, P256, DOI 10.2216/i0031-8884-40-3-256.1; Holmes MJ, 2002, J PHYCOL, V38, P96, DOI 10.1046/j.1529-8817.2002.01153.x; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; Irwin A, 2003, HARMFUL ALGAE, V2, P61, DOI 10.1016/S1568-9883(02)00084-7; John U, 2003, MOL BIOL EVOL, V20, P1015, DOI 10.1093/molbev/msg105; LABARBERASANCHEZ A, 1993, DEV MAR BIO, V3, P281; Le Messurier D. 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J. F., 1954, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V5, P171	114	125	139	2	72	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	AUG	2007	6	4					465	485		10.1016/j.hal.2006.12.008	http://dx.doi.org/10.1016/j.hal.2006.12.008			21	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	167WO		Green Accepted			2025-03-11	WOS:000246483400002
J	Burkholder, JM; Hallegraeff, GM; Melia, G; Cohen, A; Bowers, HA; Oldach, DW; Parrow, MW; Sullivan, MJ; Zimba, PV; Allen, EH; Kinder, CA; Mallin, MA				Burkholder, JoAnn M.; Hallegraeff, Gustaaf M.; Melia, Gregory; Cohen, Andrew; Bowers, Holly A.; Oldach, David W.; Parrow, Matthew W.; Sullivan, Michael J.; Zimba, Paul V.; Allen, Elle H.; Kinder, Carol A.; Mallin, Michael A.			Phytoplankton and bacterial assemblages in ballast water of US military ships as a function of port of origin, voyage time, and ocean exchange practices	HARMFUL ALGAE			English	Review						bacteria; ballast water exchange; harmful algae; phytoplankton; ship; transport	RIBOSOMAL-RNA GENES; 18S RDNA SEQUENCES; PCR AMPLIFICATION; PFIESTERIA-PISCICIDA; DINOFLAGELLATE CYSTS; MARINE COMMUNITIES; PSEUDOMONAS-PUTIDA; ESCHERICHIA-COLI; GLOBAL TRANSPORT; RAPID DETECTION	We characterized the physical/chemical conditions and the algal and bacterial assemblages in ballast water from 62 ballast tanks aboard 28 ships operated by the U.S. Military Sealift Command and the Maritime Administration, sampled at 9 ports on the U.S. West Coast and 4 ports on the U.S. East Coast. The ballast tank waters had been held for 2-176 days, and 90% of the tanks had undergone ballast exchange with open ocean waters. Phytoplankton abundance was highly variable (grand mean for all tanks, 3.21 x 10(4) viable cells m(-3); median, 7.9 x 10(3) cells m(-3)) and was unrelated to physical/chemical parameters, except for a positive relationship between centric diatom abundance and nitrate concentration. A total of 100 phytoplankton species were identified from the ballast tanks, including 23 potentially harmful taxa (e.g. Chaetoceros concavicornis, Dinophysis acuminata, Gambierdiscus toxicus, Heterosigma akashiwo, Karlodinium veneficum, Prorocentrunt minimum, Pseudo-nitzschia multiseries). Assemblages were dominated by chain-forming diatoms and dinoflagellates, and viable organisms comprised about half of the total cells. Species richness was higher in ballast tanks with coastal water, and in tanks containing Atlantic or Pacific Ocean source waters rather than Indian Ocean water. Total and viable phytoplankton numbers decreased with age of water in the tanks. Diversity also generally decreased with water age, and tanks with ballast water age >33 days did not produce culturable phytoplankton. Abundance was significantly higher in tanks with recently added coastal water than in tanks without coastal sources, but highly variable in waters held less than 30 days. Bacterial abundance was significantly lower in ballast tanks with Atlantic than Pacific Ocean source water, but otherwise was surprisingly consistent among ballast tanks (overall mean across all tanks, 3.13 +/- 1.27 x 10(11) cells m(-3); median, 2.79 x 10(11) cells m(-3)) and was unrelated to vessel type, exchange status, age of water, environmental conditions measured, or phytoplankton abundance. At least one of four pathogenic eubacteria (Listeria monocytogenes, Escherichia coli, Mycobacterium spp., Pseudomonas aeruginosa) was detected in 48% of the ballast tanks, but toxigenic strains of Vibrio cholerae were not detected. For ships with tanks of similar ballasting history, the largest source of variation in phytoplankton and bacteria abundance was among ships; for ships with tanks of differing ballasting histories, and for all ships/tanks considered collectively, the largest source of variation was within ships. Significant differences in phytoplankton abundance, but not bacterial abundance, sometimes occurred between paired tanks with similar ballasting history; hence, for regulatory purposes phytoplankton abundance cannot be estimated from single tanks only. Most tanks (94%) had adequate records to determine the source locations and age of the ballast water and, as mentioned, 90% had had ballast exchange with open-ocean waters. Although additional data are needed from sediments that can accumulate at the bottom of ballast tanks, the data from this water-column study indicate that in general, U.S. Department of Defense (DoD) ships are well managed to minimize the risk for introduction of harmful microbiota. Nevertheless, abundances of viable phytoplankton with maximum dimension >50 Rm exceeded proposed International Maritime Organization standards in 47% of the ballast tanks sampled. The data sugget that further treatment technologies and/or alternative management strategies will be necessary to enable DoD vessels to comply with proposed standards. (C) 2007 Elsevier B.V. All rights reserved.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7000, Australia; San Francisco Estuary Inst, Richmond, CA 94804 USA; Univ Maryland, Sch Med, Inst Human Virol, Baltimore, MD 21201 USA; Florida State Univ, Coastal & Marine Lab, St Teresa, FL USA; USDA ARS, Catfish Genet Res Unit, Stoneville, MS 38776 USA; Univ N Carolina, Ctr Marine Sci, Wilmington, NC 28409 USA; Univ N Carolina, Dept Biol, Charlotte, NC 28223 USA	North Carolina State University; University of Tasmania; University System of Maryland; University of Maryland Baltimore; State University System of Florida; Florida State University; United States Department of Agriculture (USDA); University of North Carolina; University of North Carolina Wilmington; University of North Carolina; University of North Carolina Charlotte	Burkholder, JM (通讯作者)，N Carolina State Univ, Ctr Appl Aquat Ecol, 4700 Hillsborough St, Raleigh, NC 27606 USA.	joann_burkholder@ncsu.edu	Zimba, Paul/O-2778-2013; Sullivan, Michael/B-5459-2012; Parrow, Matthew/HMO-6676-2023; Hallegraeff, Gustaaf/C-8351-2013	Parrow, Matthew/0000-0002-3197-2510; zimba, paul/0000-0001-6541-2055; Hallegraeff, Gustaaf/0000-0001-8464-7343				Altschul SF, 1997, NUCLEIC ACIDS RES, V25, P3389, DOI 10.1093/nar/25.17.3389; Amann R, 2000, SYST APPL MICROBIOL, V23, P1; AMANN RI, 1995, MICROBIOL REV, V59, P143, DOI 10.1128/MMBR.59.1.143-169.1995; ANAISSIE E, 1987, AM J MED, V82, P1191, DOI 10.1016/0002-9343(87)90223-3; Becker S, 2000, APPL ENVIRON MICROB, V66, P4945, DOI 10.1128/AEM.66.11.4945-4953.2000; BEJ AK, 1994, APPL ENVIRON MICROB, V60, P368, DOI 10.1128/AEM.60.1.368-373.1994; Bergholtz T, 2006, J PHYCOL, V42, P170, DOI 10.1111/j.1529-8817.2006.00172.x; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Bowers HA, 2006, J PHYCOL, V42, P1333, DOI 10.1111/j.1529-8817.2006.00285.x; Burkholder JM, 2006, AFR J MAR SCI, V28, P177, DOI 10.2989/18142320609504143; BURKHOLDER J M, 1989, Archiv fuer Hydrobiologie Supplement, V83, P1; Button DK, 2001, APPL ENVIRON MICROB, V67, P1636, DOI 10.1128/AEM.67.4.1636-1645.2001; Campbell MS, 2003, APPL ENVIRON MICROB, V69, P7137, DOI 10.1128/AEM.69.12.7137-7144.2003; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; CHAN AT, 1980, J PHYCOL, V16, P428, DOI 10.1111/j.1529-8817.1980.tb03056.x; Chandler DP, 1997, MOL ECOL, V6, P475, DOI 10.1046/j.1365-294X.1997.00205.x; Cohen AN, 1998, SCIENCE, V279, P555, DOI 10.1126/science.279.5350.555; Coles SL, 1999, MAR BIOL, V135, P147, DOI 10.1007/s002270050612; Dawson SC, 2002, P NATL ACAD SCI USA, V99, P8324, DOI 10.1073/pnas.062169599; Dickman M, 1999, MAR ECOL PROG SER, V176, P253, DOI 10.3354/meps176253; Díez B, 2001, APPL ENVIRON MICROB, V67, P2932, DOI 10.1128/AEM.67.7.2932-2941.2001; Doblin MA, 2006, MAR POLLUT BULL, V52, P259, DOI 10.1016/j.marpolbul.2005.12.014; Drake LA, 2002, MAR ECOL PROG SER, V233, P13, DOI 10.3354/meps233013; Drancourt M, 2000, J CLIN MICROBIOL, V38, P3623, DOI 10.1128/JCM.38.10.3623-3630.2000; FARRELLY V, 1995, APPL ENVIRON MICROB, V61, P2798, DOI 10.1128/AEM.61.7.2798-2801.1995; Figueras MJ, 2000, INT J SYST EVOL MICR, V50, P2069, DOI 10.1099/00207713-50-6-2069; FORBES E, 1998, P 15 DIAT S, P00509; Foulds IV, 2002, J APPL MICROBIOL, V93, P825, DOI 10.1046/j.1365-2672.2002.01772.x; Fuse H, 2003, BIOSCI BIOTECH BIOCH, V67, P1121, DOI 10.1271/bbb.67.1121; Gasol JM, 2000, SCI MAR, V64, P197, DOI 10.3989/scimar.2000.64n2197; Gollasch S., 2003, Biological Invasions, V5, P365, DOI 10.1023/B:BINV.0000005569.81791.25; Guillard RRL., 1975, CULTURE MARINE INVER, P29, DOI [10.1007/978-1-4615-8714-93, DOI 10.1007/978-1-4615-8714-93, 10.1007/978-1-4615-8714-9_3]; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Hansen MC, 1998, FEMS MICROBIOL ECOL, V26, P141, DOI 10.1016/S0168-6496(98)00031-2; HOLLAND PM, 1991, P NATL ACAD SCI USA, V88, P7276, DOI 10.1073/pnas.88.16.7276; Huber T, 2004, BIOINFORMATICS, V20, P2317, DOI 10.1093/bioinformatics/bth226; Kim SH, 2003, J FOOD PROTECT, V66, P1385, DOI 10.4315/0362-028X-66.8.1385; Kong RYC, 2002, WATER RES, V36, P2802, DOI 10.1016/S0043-1354(01)00503-6; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; López-García P, 2001, NATURE, V409, P603, DOI 10.1038/35054537; LUDWIG W, 1994, APPL ENVIRON MICROB, V60, P3236, DOI 10.1128/AEM.60.9.3236-3244.1994; LUND J. 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J	Doblin, MA; Coyne, KJ; Rinta-Kanto, JM; Wilhelm, SW; Dobbs, FC				Doblin, Martina A.; Coyne, Kathryn J.; Rinta-Kanto, Johanna M.; Wilhelm, Steven W.; Dobbs, Fred C.			Dynamics and short-term survival of toxic cyanobacteria species in ballast water from NOBOB vessels transiting the Great Lakes - implications for HAB invasions	HARMFUL ALGAE			English	Article						ballast-water; molecular probes; viability; toxic cyanobacteria	REAL-TIME PCR; 16S RIBOSOMAL-RNA; PFIESTERIA-PISCICIDA; DINOFLAGELLATE CYSTS; CENTRAL CALIFORNIA; DNA EXTRACTION; SHIPS; TRANSPORT; MICROCYSTIS; BLOOM	We measured the presence, viability and potential toxicity of cyanobacteria in ships' ballast tanks during three domestic voyages through the North American Great Lakes. Using molecular methods, the toxin-producing forms of Microcystis and Anabaena were monitored in ballast water after ships' ballast tanks were filled at their first port of call, and at subsequent ports as ships transited the Great Lakes. Microcystis was detected in ballast water at intermediate and final ports of call in all three experiments, but the presence of Anabaena was more variable, suggesting low abundance or patchy distribution in ballast tanks. Both species were detected in ballast water up to I I days old. Detection of the microcystin synthetase gene, incyE, in ballast tanks indicated entrained cells were capable of producing microcystin, and further analyses of RNA indicated the toxin was being expressed by Microcystis, even after I I days in dark transit. These data demonstrate within-basin transport and delivery of planktonic harmful algal bloom (HAB) species to distant ports in the world's largest freshwater reservoir, with potential implications for drinking water quality. These implications are discussed with respect to management of microbial invasions and the fate of introduced phytoplankton in their receiving environment. (C) 2007 Elsevier B.V. All rights reserved.	Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA; Univ Delaware, Grad Coll Marine Studies, Lewes, DE 19958 USA; Univ Tennessee, Dept Microbiol, Knoxville, TN 37996 USA; Univ Technol Sydney, Dept Environm Sci, Inst Water & Environm Resource Management, Sydney, NSW 2007, Australia	Old Dominion University; University of Delaware; University of Tennessee System; University of Tennessee Knoxville; University of Technology Sydney	Doblin, MA (通讯作者)，Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA.	martina.doblin@uts.edu.au	Wilhelm, Steven/B-8963-2008; Doblin, Martina/E-8719-2013	Wilhelm, Steven/0000-0001-6283-8077; Rinta-Kanto, Johanna/0000-0002-5824-0897; Doblin, Martina/0000-0001-8750-3433; Coyne, Kathryn/0000-0001-8846-531X				Bailey SA, 2005, DIVERS DISTRIB, V11, P453, DOI 10.1111/j.1366-9516.2005.00150.x; Baker JA, 2002, APPL ENVIRON MICROB, V68, P6070, DOI 10.1128/AEM.68.12.6070-6076.2002; Boström KH, 2004, LIMNOL OCEANOGR-METH, V2, P365, DOI 10.4319/lom.2004.2.365; Brittain SM, 2000, J GREAT LAKES RES, V26, P241, DOI 10.1016/S0380-1330(00)70690-3; Carmichael WW, 2001, HUM ECOL RISK ASSESS, V7, P1393, DOI 10.1080/20018091095087; CHOMCZYNSKI P, 1987, ANAL BIOCHEM, V162, P156, DOI 10.1006/abio.1987.9999; Coyne KJ, 2005, LIMNOL OCEANOGR-METH, V3, P381, DOI 10.4319/lom.2005.3.381; Coyne KJ, 2004, APPL ENVIRON MICROB, V70, P5298, DOI 10.1128/AEM.70.9.5298-5304.2004; Coyne KJ, 2001, AQUAT MICROB ECOL, V24, P275, DOI 10.3354/ame024275; Dempster EL., 1999, BIOTECHNIQUES, V27, P66; Doblin M.A., 2004, Harmful Algae 2002, P317; Doblin MA, 2006, MAR POLLUT BULL, V52, P259, DOI 10.1016/j.marpolbul.2005.12.014; Doblin MA, 2004, APPL ENVIRON MICROB, V70, P6495, DOI 10.1128/AEM.70.11.6495-6500.2004; Drake LA, 2002, MAR ECOL PROG SER, V233, P13, DOI 10.3354/meps233013; Elton CS, 1958, ECOLOGY INVASIONS; Forsberg R., 2005, P 28 ANN M ADH SOC, P92; Galil BS, 1997, EUR J PROTISTOL, V33, P244, DOI 10.1016/S0932-4739(97)80002-8; GOLLASCH S, 1998, 5064 ICES COOP RES; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Hasle Grethe R., 1997, P5, DOI 10.1016/B978-012693018-4/50004-5; Hosoi-Tanabe S, 2005, MAR BIOTECHNOL, V7, P506, DOI 10.1007/s10126-004-4128-4; Johengen T, 2005, ASSESSMENT TRANSOCEA; Kaebernick M, 2002, APPL ENVIRON MICROB, V68, P449, DOI 10.1128/AEM.68.2.449-455.2002; Kaebernick M, 2001, FEMS MICROBIOL ECOL, V35, P1, DOI 10.1111/j.1574-6941.2001.tb00782.x; Kolar CS, 2001, TRENDS ECOL EVOL, V16, P199, DOI 10.1016/S0169-5347(01)02101-2; LEE SH, 1994, LIMNOL OCEANOGR, V39, P869, DOI 10.4319/lo.1994.39.4.0869; McCarthy Heather P., 2000, Biological Invasions, V2, P321, DOI 10.1023/A:1011418432256; MILLER AW, 2005, WORKSH EV BALL WAT T; MILLS EL, 1993, J GREAT LAKES RES, V19, P1, DOI 10.1016/S0380-1330(93)71197-1; Mitrovic SM, 2005, MAR ENVIRON RES, V60, P397, DOI 10.1016/j.marenvres.2005.01.001; MUYZER G, 1993, APPL ENVIRON MICROB, V59, P695, DOI 10.1128/AEM.59.3.695-700.1993; Ouellette AJA, 2003, FRONT ECOL ENVIRON, V1, P359, DOI 10.1890/1540-9295(2003)001[0359:TCTEMT]2.0.CO;2; Parsons T.R., 1992, MANUAL CHEM BIOL MET; PATIL J, 2004, PORT HASTINGS NATL D; POULSEN LK, 1993, APPL ENVIRON MICROB, V59, P1354, DOI 10.1128/AEM.59.5.1354-1360.1993; Rinta-Kanto JM, 2005, ENVIRON SCI TECHNOL, V39, P4198, DOI 10.1021/es048249u; Rublee PA, 2005, J EUKARYOT MICROBIOL, V52, P83, DOI 10.1111/j.1550-7408.2005.05202007.x; Ruiz GM, 2005, BIOL STUDY CONTAINER; Ruiz Gregory M., 2003, P459; Scholin CA, 2000, NATURE, V403, P80, DOI 10.1038/47481; Scholin CA, 1999, J PHYCOL, V35, P1356, DOI 10.1046/j.1529-8817.1999.3561356.x; Shumway Sandra E., 1993, Reviews in Fisheries Science, V1, P121; Stults JR, 2001, APPL ENVIRON MICROB, V67, P2781, DOI 10.1128/AEM.67.6.2781-2789.2001; TEBBE CC, 1993, APPL ENVIRON MICROB, V59, P2657, DOI 10.1128/AEM.59.8.2657-2665.1993; Vaitomaa J, 2003, APPL ENVIRON MICROB, V69, P7289, DOI 10.1128/AEM.69.12.7289-7297.2003; Wasson K, 2005, BIOL INVASIONS, V7, P935, DOI 10.1007/s10530-004-2995-2; Wiedner C, 2003, APPL ENVIRON MICROB, V69, P1475, DOI 10.1128/AEM.69.3.1475-1481.2003; Williamson M, 1966, BIOL INVASIONS; Wilson IG, 1997, APPL ENVIRON MICROB, V63, P3741, DOI 10.1128/AEM.63.10.3741-3751.1997; Wyatt T., 2002, CIESM Workshop Monographs, V20, P41; ZHANG X, 1999, P IEEE VEH TECHN C, V1, P243	54	43	51	0	38	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	AUG	2007	6	4					519	530		10.1016/j.hal.2006.05.007	http://dx.doi.org/10.1016/j.hal.2006.05.007			12	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	167WO					2025-03-11	WOS:000246483400004
J	Gregg, MD; Hallegraeff, GM				Gregg, Matthew D.; Hallegraeff, Gustaaf M.			Efficacy of three commercially available ballast water biocides against vegetative microalgae, dinoflagellate cysts and bacteria	HARMFUL ALGAE			English	Article						bacteria; ballast water treatment; chemical biocides; dinollagellate cysts	VIBRIO-CHOLERAE; SHIPS; TRANSPORT; VIABILITY; SURVIVAL	One proposed solution to the problem of ball ast-mediated aquatic invasions involves chemically treating ballast water to kill key target organisms. Here, we examine the efficacy of three commercially available ballast water biocides using vegetative microalgae, dinoflagellate resting cysts and bacteria as test organisms. Chemicals tested were the ballast water biocides SeaKleen (R) and Peraclean (R) Ocean, and the chlorine dioxide biocide Vibre (R). Results demonstrate that the applicability of each of the three chemical biocides as a routine ballast water treatment is limited by factors such as cost, biological effectiveness and possible residual toxicity of the discharged ballast water (assessed on the basis of impact on motility of vegetative marine microalgae). Of the three biocides tested, Peraclean (R) Ocean appears to hold the most potential; however its effectiveness in shipboard trials is yet to be proven. Peraclean (R) Ocean was biodegradable within 2-6 weeks (initial concentration of 200 ppm), could effectively inactivate resting cysts of the marine dinoflagellates Gymnodinium catenatuni, Alexandrium catenella and Protoceratium reticulatum at 400 ppm, could control bacterial growth of Escherichia coli, Staphylococcus aureus, Listeria innocua and Vibrio alginolyticus at 125-250 ppm, and could eliminate vegetative dinoflagellate cells at a concentration of 100 ppm. SeaKleen (R) eliminated vegetative microalgae at 2 ppm and could control resting cysts of the dinoflagellates G. catenatum and P. reticulatum at a concentration of 6 and 10 ppm, respectively, when exposed for a period of 2 weeks. SeaKleen (R) did not inactivate resting cysts of A. catenella at a concentration of 10 ppm and was found to degrade at a rate that could result in the discharge of residual toxic water into the marine environment. Together with the poor bactericidal properties of SeaKleen (R) (100-200 ppm required), this may limit the use of this biocide as a routine treatment option. Vibrex (R) is not a suitable ballast water treatment option due to the need for hydrochloric acid as an activator, however it was found to be the most effective against bacteria (complete inhibition at 15 ppm) indicating that onboard chlorine dioxide generators may provide an effective bacterial treatment option. The performance of these biocides was adversely influenced by a variety of factors including low water temperatures (6 degrees C compared to 17 degrees C, light versus dark conditions, and the presence of humus-rich seawater and ballast water sediments. (C) 2007 Elsevier B.V. All rights reserved.	Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	University of Tasmania	Hallegraeff, GM (通讯作者)，Univ Tasmania, Sch Plant Sci, Private Bag 55, Hobart, Tas 7001, Australia.	Hallegraeff@utas.edu.au	Hallegraeff, Gustaaf/C-8351-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343				[Anonymous], AUSTR PILOT PROJECT; [Anonymous], 1994, J MAR ENV ENG; Binet MT, 2006, MAR ENVIRON RES, V62, P247, DOI 10.1016/j.marenvres.2006.03.011; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Bolch C.J., 1993, Journal of Marine Environmental Engineering: 1993, P23; Cangelosi A, 2002, INVASIVE AQUATIC SPECIES OF EUROPE: DISTRIBUTION, IMPACTS AND MANAGEMENT, P511; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; Chu KH, 1997, HYDROBIOLOGIA, V352, P201, DOI 10.1023/A:1003067105577; *EC, 2003, EC BALL TREATM SYST; *ENV SOUNDN WORK G, 2004, ENV SOUNDN WORK GROU; FUCHS R, 2001, PERACLEAN OCEAN POTE; Galil BS, 2002, INVASIVE AQUATIC SPECIES OF EUROPE: DISTRIBUTION, IMPACTS AND MANAGEMENT, P508; Galil BS, 1997, EUR J PROTISTOL, V33, P244, DOI 10.1016/S0932-4739(97)80002-8; Guillard RRL., 1975, CULTURE MARINE INVER, P29, DOI [10.1007/978-1-4615-8714-93, DOI 10.1007/978-1-4615-8714-93, 10.1007/978-1-4615-8714-9_3]; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Hallegraeff Gustaaf M., 1997, Aquatic Ecology, V31, P47, DOI 10.1023/A:1009972931195; HERWIG RP, 2004, U WASHINGTON RES SEA; HUQ A, 1983, APPL ENVIRON MICROB, V45, P275, DOI 10.1128/AEM.45.1.275-283.1983; ICHIKAWA S, 1992, NIPPON SUISAN GAKK, V58, P2229; IVANOV V, 2003, E AS SEAS C 2003 THE; Junli Huang, 1997, Water Research, V31, P455, DOI 10.1016/S0043-1354(96)00276-X; KIM YM, 2002, EFFECT CHLORINE DIOX; McCarthy HP, 2000, BIOL INVASIONS, V2, P221; MCCARTHY SA, 1994, APPL ENVIRON MICROB, V60, P2597, DOI 10.1128/AEM.60.7.2597-2601.1994; Mocé-Llivina L, 2003, APPL ENVIRON MICROB, V69, P1452, DOI 10.1128/AEM.69.3.1452-1456.2003; Montani S., 1995, J. 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J	Smayda, TJ				Smayda, Theodore J.			Reflections on the ballast water dispersal - harmful algal bloom paradigm	HARMFUL ALGAE			English	Review						ballast water; harmful algal blooms	DINOFLAGELLATE GYMNODINIUM-CATENATUM; ALEXANDRIUM-TAMARENSE DINOPHYCEAE; LONG-TERM PERSPECTIVE; MARINE-PHYTOPLANKTON; NORTH-ATLANTIC; BROWN TIDE; ECOLOGY; CYST; RAPHIDOPHYCEAE; CATENELLA	The ballast water dispersal-HAB paradigm, increasingly invoked circumstantially to explain puzzling and unaccountable HAB species outbreaks when lacking the multiple tests of confirmation recommended by Bolch and de Salas (2007), is evaluated. The types and examples of natural dispersions and taxon cycles are compared to exotic species bloom behavior linked to ballast water vectoring. The regional spreading, bloom behavior and disjunct distributions of the brown tide pelagophyte Aureococcus anophagefferens and the toxic dinoflagellate Gymnodinium cetenatum, attributed to ballast water vectoring, are used as representative examples to evaluate the general application of the ballast water-HAB paradigm and associated interpretative problems. Human-aided emigration has a seeding and colonization ecology that differs from bloom ecology. For self-sustaining blooms to occur, these two ecologies must be accommodated by habitat growth conditions. The three stages that a non-native species must pass through (pioneering, persistence, community entry) to achieve colonization, community maintenance, and to bloom, and the niche-related factors and role of habitat disturbance are discussed. The relevance of cryptic occurrences, cyst deposits, dormancy periods and bloom rhythms of HAB species to their blooms attributed to ballast water-assisted introductions is also sketched. The different forms of HAB species rarity, their impact on the ballast water dispersal-HAB paradigm, and the dispersion and blooms of specialist and generalist HAB species are discussed. The remarkable novel and, often, monospecific blooms of dinoflagellate HAB species are being paralleled by similar eruptive bloom behavior cutting across phylogenetic lines, and being found also in raphidophytes, haptophytes, diatoms, silicoflagellates, etc. These blooms cannot be explained only as seeding events. An ecological release of 'old barriers' appears to be occurring generally at coastal bloom sites, i.e. something significant is happening ecologically and embedded within the ballast water-HAB paradigm. There may be a relationship between Life Form type [Smayda, T.J., Reynolds, C.S., 2001. Community assembly in marine phytoplankton: application of recent models to harmful dinoflagellate blooms. J. Plankton Res. 23, 447-461] and mode of expatriation; HAB dinoflagellate species commonly reported to produce ballast water-assisted toxic blooms invariably are members of cyst-producing Life Forms IV, V, VI. Ballast water vectoring of Life Forms I, II, III is rarely reported, even though many produce cysts, and where their novel introductions do occur they are more likely to be ichthyotoxic, and vectored in shellfish stock consignments. The relevance of, and need to distinguish between morphospecies and their geographic/ribotype clades are discussed based on the Alexandrium tamarense/catenella/fundyense complex. Morphospecies-level ballast water dispersions are probably minor compared to the dispersal of the different ribotypes (toxic/non-toxic clades) making up HAB morphospecies; the redistribution and admixture of genotypes should be the focus. Ballast water-assisted expatriations impact the global occurrence of HABs through the direct transfer of previously absent species or introduction of genetic strains from the donor habitat that are ecologically favored over resident strains. The hybridization of species may be of potentially greater impact, resulting from the (1) mating of individuals from the donor and recipient habitats, or (2) through the interbreeding of strains introduced from to different donor sites into the recipient site, and whose progeny have greater ecological fitness than indigenous strains. Exceptional ecological changes of some sort appear to be occurring globally which, in combination with the genetically altered ecophysiological behavior of HAB species linked to ballast water dispersion and admixture, underpins the global HAB phenomenon. The impact of ballast water and shellfish transplantation on HABs and phytoplankton community ecology, generally, is considerably greater than the current focus on HAB species distributions, vectoring, and blooms. The methodological, investigative and conceptual potential of the ballast water-HAB paradigm should be exploited by developing a GEOHAB type intiative to advance quantification of global HAB ecology. (C) 2007 Elsevier B.V. All rights reserved.	Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA	University of Rhode Island	Smayda, TJ (通讯作者)，Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA.	tsmayda@gso.uri.edu						Allen W E, 1933, Science, V78, P12, DOI 10.1126/science.78.2010.12; Allen W. 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J	Hernández-Becerril, DU; Alonso-Rodríguez, R; Alvarez-Góngora, C; Barón-Campis, SA; Ceballos-Corona, G; Herrera-Silveira, J; Del Castillo, MEM; Juárez-Ruíz, N; Merino-Virgilio, F; Morales-Blake, A; Ochoa, JL; Orellana-Cepeda, E; Ramírez-Camarena, C; Rodríguez-Salvadoro, R				Hernandez-Becerril, David U.; Alonso-Rodriguez, Rosalba; Alvarez-Gongora, Cynthia; Baron-Campis, Sofia A.; Ceballos-Corona, Gerardo; Herrera-Silveira, Jorge; Del Castillo, Maria E. Meave; Juarez-Ruiz, Norma; Merino-Virgilio, Fanny; Morales-Blake, Alejandro; Ochoa, Jose L.; Orellana-Cepeda, Elizabeth; Ramirez-Camarena, Casimiro; Rodriguez-Salvadoro, Raciel			Toxic and harmful marine phytoplankton and microalgae (HABs) in Mexican Coasts	JOURNAL OF ENVIRONMENTAL SCIENCE AND HEALTH PART A-TOXIC/HAZARDOUS SUBSTANCES & ENVIRONMENTAL ENGINEERING			English	Review						biotoxins; harmful algal blooms; marine phytoplankton; Mexican coasts; microalgae	PSEUDO-NITZSCHIA; ALGAL BLOOMS; PYRODINIUM-BAHAMENSE; DINOFLAGELLATE CYSTS; DOMOIC ACID; 1ST RECORD; RED TIDE; BACILLARIOPHYCEAE; SHELLFISH; TRANSPORT	Harmful Algal Blooms (HABs) are becoming an increasing problem to human health and environment (including effects on natural and cultured resources, tourism and ecosystems) all over the world. In Mexico a number of human fatalities and important economic losses have occurred in the last 30 years because of these events. There are about 70 species of planktonic and non-planktonic microalgae considered harmful in Mexican coasts. The most important toxin-producing species are the dinoflagellates Gymnodinium catenatuni and Pyrodinium bahamense var. compressum, in the Mexican Pacific, and Karenia brevis in the Gulf of Mexico, and consequently the poisonings documented in Mexico are Paralytic Shellfish Poisoning (PSP) and Neurotoxic Shellfish Poisoning (NSP). Although there is evidence that Amnesic Shellfish Poisoning (ASP), Diarrhetic Shellfish Poisoning (DSP) and Ciguatera Fish Poisoning (CFP) also occur in Mexico, these problems are reported less frequently. The type of phytoplankton and epiphytic microalgae, their toxins and harmful effects as well as current methodology used to study these phenomena are presented in this paper. As an experienced group of workers, we include descriptions of monitoring and mitigation programs, our proposals for collaborative projects and perspectives on future research.	Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Apdo Postal 70-305, Mexico City, DF, Mexico; Cambiar Unit Acad Mazatlan, Inst Ciencias Mar & Limnol, Mazatlan, Mexico; Unidad Merida, Ctr Invest & Estudios Avanzados, Merida, Mexico; SAGARPA, Inst Nacl Pesca, Mexico City, DF, Mexico; Univ Michoacana, Fac Biol, Morelia, Michoacan, Mexico; Univ Autonoma Metropolitana Iztapalapa, Dept Hydrobiol, Mexico City 09340, DF, Mexico; Univ Colima, Fac Ciencias Marinas, Manzanillo, Colima, Mexico; Ctr Invest Biol Noroeste, La Paz, Mexico; Univ Autonoma Baja California, Fac Ciencias Marinas, Ensenada, Baja California, Mexico; CETMAR, Puerto Madero, Chiapas, Mexico	Universidad Nacional Autonoma de Mexico; Universidad Michoacana de San Nicolas de Hidalgo; Universidad Autonoma Metropolitana - Mexico; Universidad de Colima; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Telefonica SA; Universidad Autonoma de Baja California	Hernández-Becerril, DU (通讯作者)，Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Apdo Postal 70-305, Mexico City, DF, Mexico.	dhernand@mar.icmyl.unam.mx	Ochoa, Jose/KDP-2447-2024; Alonso-Rodriguez, Rosalba/U-9896-2017	Alonso-Rodriguez, Rosalba/0000-0001-7716-3869				AGUIRREGOMEZ R, 1999, GEOFISICA INT, V38, P63; Alonso-Rodríguez R, 2000, MAR POLLUT BULL, V40, P331, DOI 10.1016/S0025-326X(99)00225-8; Alonso-Rodríguez R, 2003, AQUACULTURE, V219, P317, DOI 10.1016/S0044-8486(02)00509-4; ALONSORODRIGUEZ R, 2004, FITOPLANCTON LARVICU; Alvarez-Góngora C, 2006, MAR POLLUT BULL, V52, P48, DOI 10.1016/j.marpolbul.2005.08.006; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 2001, TECHNICAL SERIES ASI, V59; [Anonymous], 2004, HARMFUL ALGAE; Band-Schmidt CJ, 2004, HYDROBIOLOGIA, V515, P79, DOI 10.1023/B:HYDR.0000027320.00977.8b; Barón-Campis Sofía A., 2005, Hidrobiológica, V15, P73; BATES SS, 1989, CAN J FISH AQUAT SCI, V46, P1203, DOI 10.1139/f89-156; Bustillos-Guzmán J, 2004, REV BIOL TROP, V52, P17; Capone DG, 2005, ASM NEWS, V71, P179; Ceballos-Corona J. 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Environ. Sci. Health Part A-Toxic/Hazard. Subst. Environ. Eng.	AUG	2007	42	10					1349	1363		10.1080/10934520701480219	http://dx.doi.org/10.1080/10934520701480219			15	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	206IG	17680474				2025-03-11	WOS:000249176500003
J	Hégaret, H; Wikfors, GH; Shumway, SE				Hegaret, Helene; Wikfors, Gary H.; Shumway, Sandra E.			Diverse feeding responses of five species of bivalve mollusc when exposed to three species of harmful algae	JOURNAL OF SHELLFISH RESEARCH			English	Article						filtration; clearance; biodeposits; bivalve mollusc; mussels; oysters; clams; scallops; harmful algal bloom; HAB; toxic algae; Alexandrium fundyense; Heterosigma akashiwo; Prorocentrum minimum; Argopecten irradians; Crassostrea virginica; Merceneria mercenaria; Mya arenaria; Mytilus edulis	DINOFLAGELLATE PROROCENTRUM-MINIMUM; CRASSOSTREA-GIGAS THUNBERG; PROTOGONYAULAX-TAMARENSIS; HETEROSIGMA-AKASHIWO; MYTILUS-GALLOPROVINCIALIS; PARTICLE SELECTION; CULTURED STRAIN; EASTERN OYSTERS; CONCANAVALIN-A; FLOW-CYTOMETRY	Shell closure and restriction of filtration are behavioral responses by which bivalve molluscs can limit exposure of soft tissues to noxious or toxic agents, including harmful microalgae. In this study, we assessed the clearance rates of five species of bivalve mollusc-the northern bay scallop Argopecten irradians irradians, the eastern oyster Crassostrea virginica, the northern quahog Mercenaria mercennaria, the softshell clarn Mya arenaria, and the blue mussel Mytilus edulis-exposed for one hour to each of three harmful-algal strains: Prorocentrum minimum. Alexandrium fundyense, and Heterosigma akashiwo. Clearance rates of harmful-algal cells were compared with clearance rates of a benign microalga, Rhodomonas sp., and to a Mix of each harmful alga with Rhodomonas sp. Qualitative observations of valve closure and production of biodeposits were also assessed during the exposure experiments. Feces and pseudofeces were collected and observed with light and fluorescence microscopy for the presence or absence of intact, potentially-viable algal cells or temporary cysts. Results increase our understanding of the high variation between the different bivalve/harmful alga pairs. Responses of bivalve species to the different harmful algae were species-specific. but ill most cases indicated a preferential retention of harmful algal cells, probably based upon different characteristics of the algae. Each shellfish species also reacted differently to the harmful-algal exposures; several remained open; whereas, others, such as oysters exposed to the toxic raphiclophyte Heterosigma akashiwo, closed shells partially or totally. Similarly, production of feces and pseudofeces varied appreciably between the different bivalve/alga pairs; with the exception of softshell clams Mya arenaria, intact cells of most harmful-algal species tested were seen in biodeposits of the other four bivalve species. These results extend our understanding of the high species specificity in the interactions between harmful algae and bivalve molluscs and confirm that generalizations about feeding responses of bivalves to harmful algae cannot easily be made. In most cases. however. there was at least some ingestion of the harmful algae leading to exposure of soft tissues to the algal cells.	Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford, CT 06460 USA	University of Connecticut; National Oceanic Atmospheric Admin (NOAA) - USA	Shumway, SE (通讯作者)，Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA.	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SANDRA E. SHUMWAY, UNIV CONNECTICUT, 1080 SHENNECOSSETT RD, GROTON, CT 06340 USA	0730-8000	1943-6319		J SHELLFISH RES	J. Shellfish Res.	AUG	2007	26	2					549	559		10.2983/0730-8000(2007)26[549:DFROFS]2.0.CO;2	http://dx.doi.org/10.2983/0730-8000(2007)26[549:DFROFS]2.0.CO;2			11	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	208JA					2025-03-11	WOS:000249314400029
J	Daneshian, J; Sarkar, S; Sharma, V				Daneshian, J.; Sarkar, S.; Sharma, V.			Miocene palynoflora from Inglis Island, Andaman Sea and its palaeoecological implication	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						palynoflora; late Early Miocene-Early Middle Miocene; palacoecology; Inglis Island; Andaman Sea	RADIOLARIAN; BIOSTRATIGRAPHY	A rich palynofloral assemblage has been recorded for the first time from a stratigraphic section of the Inglis Formation at Inglis Island, Andaman Sea, India. Forty-six genera and fifty-eight species belonging to different botanical groups viz., dinoflagellate cysts, fungal remains, pteridophytic spores, and gymnospermous and angiospermous pollen have been recognized. Geological ranges of some stratigraphically important palynotaxa suggest late Early Mioceneearly Middle Miocene age to the assemblage. The recorded palynofloral assemblage is also closely comparable to that recorded from late Early Miocene-Early Middle Miocene sediments of South India. The palynoflora has been compared with the modem equivalents and it indicates a warm humid climate with high degree of rainfall during the deposition of the sequence in the area of investigation.	Teacher Training Univ, Dept Geol, Tehran, Iran; Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India; Univ Delhi, Dept Geol, Delhi 110007, India	Shahid Rajaee Teacher Training University (SRTTU); Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); University of Delhi	Daneshian, J (通讯作者)，Teacher Training Univ, Dept Geol, 49 Mofatteh Ave, Tehran, Iran.	jdaneshian@yahoo.co.uk						[Anonymous], 1994, Journal of Palaeosciences, DOI DOI 10.54991/JOP.1993.1147; [Anonymous], 1996, GEOPHYTOLOGY; BANERJEE D., 1966, POLLEN SPORES, V8, P205; BANERJEE D, 1964, B GEOL MIN METAL SOC, V29, P1; BERGGREN WA, 1995, SEPM SPEC PUBL, V54, P212; CROIZAT L, 1958, PHYTOGEOGRAPHY GEOLO, V1; Good R., 1953, The Geography of the Flowering Plants; Kar R.K., 1990, J PALAEOSCI, V38, P229; KARUNAKARAN C, 1964, P 22 INT GEOL C NEW, V4, P507; Maithani A., 1992, B OIL NAT GAS COMM, V29, P19; MANDAL J, 1994, GEOPHYTOLOGY, V2, P209; Mathur K., 1981, Geosci. J., V2, P31; Mathur YK, 1980, GEOSCI J, V1, P51; PANDE J, 1972, P 2 IND C MICR STRAT, P66; Ramanujam C.G.K., 1991, J PALAEONTOL SOC IND, V36, P51; Ramanujam C.K., 1984, J PALYNOL, V20, P58; Ramanujam CGK, 1987, JOUR PALAEONT SOC IN, V32, P25; Rao M.R., 1990, PROC SYMPVISTAS INDI, V38, P243; RAO MR, 1978, PALAEBOTANIST, V25, P397; RAO MR, 1995, PALAEBOT PALYNOL, V86, P325; References KarunakaranC. Ray., 1968, J GEOL SOC INDIA, V9, P32, DOI DOI 10.17491/JGSI/1968/090104; Sah S.C.D., 1967, ANN MUS E ROYAL AFRI, V57, P1; SAH SCD, 1968, PALEOBOTANIST, V16, P177; Sarkar S., 1990, PALEOBOTANIST, V38, P319; SHARMA V, 1993, J GEOL SOC INDIA, V42, P154; SHARMA V, 1989, J GEOL SOC INDIA, V34, P76; SHARMA V, 2003, PROC 8 INT C PACIFIC, P126; SINGH HP, 1987, PALEOBOTANIST, V35, P331; SRINIVASAN M. S., 1976, P 6 IND C MICR STRAT, P328; SRINIVASAN MS, 1983, J GEOL SOC INDIA, V24, P1; Thanikaimoni G., 1984, Selected Tertiary Angiosperm Pollen from India and Their Relationship with African Tertiary Pollen, V19, P1; Tyron RM., 1982, Ferns and Allied Plants: With Special Reference to Tropical America; WEI K-Y, 1984, Revista Espanola de Micropaleontologia, V16, P345; Willis J.C., 1966, A Dictionary of Flowering Plants and Ferns	34	0	0	0	1	GEOLOGICAL SOC INDIA	BANGALORE	#64 12TH CROSS, BASAPPA LAYOUT P B 1922, GAVIPURAM PO, BANGALORE 560019, INDIA	0016-7622			J GEOL SOC INDIA	J. Geol. Soc. India	JUL	2007	70	1					147	157						11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	211XO					2025-03-11	WOS:000249556800016
J	Rintala, JM; Spilling, K; Blomster, J				Rintala, Janne-Markus; Spilling, Kristian; Blomster, Jaanika			Temporary cyst enables long-term dark survival of <i>Scrippsiella hangoei</i> (Dinophyceae)	MARINE BIOLOGY			English	Article							RED-TIDE DINOFLAGELLATE; ALEXANDRIUM-TAYLORI DINOPHYCEAE; SEA-ICE; HETEROCAPSA-CIRCULARISQUAMA; GONYAULAX-EXCAVATA; LIFE-HISTORY; BALTIC SEA; DYNAMICS; RATES; NOV	We examined the dark survival strategy of the cold-water dinoflagellate Scrippsiella hangoei from the Baltic Sea. Cultures of S. hangoei were placed in dark and light and we followed the morphological developmentand, determined respiration rate and activity of extracellular leucine aminopeptidase (LAP). S. hangoei had LAP activity in the light, but not in the dark, suggesting that the degradation and use of organic substrates is not part of the dark survival strategy. After prolonged time in darkness (> 5 days), S. hangoei started to shed flagella and theca, and produced a previously undescribed temporary cyst. The transformation from vegetative cell into the temporary cyst initially increased respiration rate tenfold, but after the transformation the respiration rate decreased to almost undetectable levels. The presented temporary cyst enables survival through long periods in dark by reducing the respiration rate.	Finnish Environm Inst, FIN-00251 Helsinki, Finland; Finnish Inst Marine Res, FIN-00561 Helsinki, Finland; Univ Helsinki, Dept Biol & Environm Sci, FIN-00014 Helsinki, Finland	Finnish Environment Institute; University of Helsinki	Spilling, K (通讯作者)，Finnish Environm Inst, Mechelininkatu 34A, FIN-00251 Helsinki, Finland.	kristian.spilling@ymparisto.fi	; Spilling, Kristian/L-7932-2014	Blomster, Jaanika/0000-0003-1347-7919; Rintala, Janne-Markus/0000-0002-3514-6582; Spilling, Kristian/0000-0002-8390-8270				ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; Carlsson P., 1998, NATO ASI Series Series G Ecological Sciences, V41, P509; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; delGiorgio PA, 1997, NATURE, V385, P148, DOI 10.1038/385148a0; Ehn J, 2004, J GEOPHYS RES-OCEANS, V109, DOI 10.1029/2003JC002042; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Grenfell T.C., 1977, J GLACIOL, V18, P445, DOI [10.3189/S0022143000021122, DOI 10.3189/S0022143000021122, DOI 10.1017/S0022143000021122]; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; HANSEN G, 1995, SCANNING S97, V17; Ikavalko J, 1997, EUR J PROTISTOL, V33, P229; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; KITA T, 1985, B MAR SCI, V37, P643; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Kremp A, 2005, J PHYCOL, V41, P629, DOI 10.1111/j.1529-8817.2005.00070.x; LARSEN J, 1995, PHYCOLOGIA, V34, P135, DOI 10.2216/i0031-8884-34-2-135.1; Legrand C, 1998, AQUAT MICROB ECOL, V16, P81, DOI 10.3354/ame016081; Nagasaki K, 2000, NIPPON SUISAN GAKK, V66, P666; Olli K, 2004, MAR BIOL, V145, P1, DOI 10.1007/s00227-004-1295-9; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Rintala JM, 2006, HYDROBIOLOGIA, V554, P11, DOI 10.1007/s10750-005-1002-y; Sarath G., 1989, Proteolytic Enzymes: A Practical Approach, P25, DOI [10.1016/0968-0004(85)90125-2, DOI 10.1016/0968-0004(85)90125-2]; SCAVIA D, 1987, LIMNOL OCEANOGR, V32, P1017, DOI 10.4319/lo.1987.32.5.1017; SOMVILLE M, 1983, LIMNOL OCEANOGR, V28, P190, DOI 10.4319/lo.1983.28.1.0190; Spilling K., 2007, THESIS, V31, P1; Stoecker D, 2005, AQUAT MICROB ECOL, V40, P151, DOI 10.3354/ame040151; Stoecker DK, 2003, AQUAT MICROB ECOL, V30, P175, DOI 10.3354/ame030175; Tarutani K, 2001, AQUAT MICROB ECOL, V23, P103, DOI 10.3354/ame023103; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P398; WILLIAMS PJL, 1982, LIMNOL OCEANOGR, V27, P576, DOI 10.4319/lo.1982.27.3.0576; Xiao Yong-zhi, 2001, Marine Sciences (Beijing), V25, P50	32	27	31	0	18	SPRINGER	NEW YORK	233 SPRING STREET, NEW YORK, NY 10013 USA	0025-3162			MAR BIOL	Mar. Biol.	JUL	2007	152	1					57	62		10.1007/s00227-007-0652-x	http://dx.doi.org/10.1007/s00227-007-0652-x			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	181YG					2025-03-11	WOS:000247471700006
J	Harada, A; Ohtsuka, S; Horiguchi, T				Harada, Ai; Ohtsuka, Susumu; Horiguchi, Takeo			Species of the parasitic genus <i>Duboscquella</i> are members of the enigmatic Marine Alveolate Group I	PROTIST			English	Article						alveolate; Duboscquella; environmental clone; Favella ehrenbergii; Marine Alveolate Group I; parasitic dinoflagellate	LOBSTER NEPHROPS-NORVEGICUS; HOST EUTINTINNUS-PECTINIS; GENETIC DIVERSITY; N-SP; DINOFLAGELLATE; DINOPHYCEAE; EUKARYOTES; INFECTION; CACHONI; BAY	Small subunit ribosomal RNA gene sequences of Duboscquella spp. infecting the tintinnid ciliate, Favella ehrenbergii, were determined. Two parasites were sampled from different localities. They are morphologically similar to each other and both resemble D. aspida. Nevertheless, two distinct sequences (7.6% divergence) were obtained from them. Phylogenetic trees inferred from maximum likelihood and maximum parsimony revealed that these two Duboscquella spp. sequences are enclosed in an environmental clade named Marine Alveolate Group 1. This clade consists of a large number of picoplanktonic organisms known only from environmental samples from various parts of the ocean worldwide, and which therefore lack clear characterization and identification. Here, we provide morphological and genetic characterization of these two Duboscquella genotypes included in this enigmatic clade. Duboscquella spp. produce a large number of small flagellated spores as dispersal agents and the presence of such small cells partially explains why the organisms related to these parasites have been detected within environmental genetic libraries, built from picoplanktonic size fractions of environmental samples. The huge diversity of the Marine Alveolate Group I and the finding that parasites from different marine protists belong to this lineage suggest that parasitism is a widespread and ecologically relevant phenomenon in the marine environment. (c) 2007 Elsevier GmbH. All rights reserved.	Hokkaido Univ, Grad Sch Sci, Div Biol Sci, Sapporo, Hokkaido 0600810, Japan; Hiroshima Univ, Grad Sch Biosphere Sci, Setouchi Field Sci Ctr, Takehara Marine Sci Stn, Hiroshima 7250024, Japan; Hokkaido Univ, Fac Sci, Dept Nat Hist Sci, Sapporo, Hokkaido 0600810, Japan	Hokkaido University; Hiroshima University; Hokkaido University	Horiguchi, T (通讯作者)，Hokkaido Univ, Grad Sch Sci, Div Biol Sci, Sapporo, Hokkaido 0600810, Japan.	horig@sci.hokudai.ac.jp	Horiguchi, Takeo/D-7612-2012; Ohtsuka, Susumu/U-8166-2017	Ohtsuka, Susumu/0000-0001-6018-7442				Appleton PL, 1996, PARASITOL RES, V82, P279, DOI 10.1007/s004360050113; Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; Cachon J., 1987, The Biology of Dinoflagellates, P571; CACHON J, 1964, ANN SCI NAT ZOOL, V12, P1; Chatton E., 1920, Archives de Zoologie Experimentale Paris, V59; Chatton E., 1952, TRAITE ZOOL, P309; COATS DW, 1988, J PROTOZOOL, V35, P607, DOI 10.1111/j.1550-7408.1988.tb04159.x; COATS DW, 1989, MAR BIOL, V101, P401, DOI 10.1007/BF00428137; Díez B, 2001, APPL ENVIRON MICROB, V67, P2932, DOI 10.1128/AEM.67.7.2932-2941.2001; Dolven JK, 2007, PROTIST, V158, P65, DOI 10.1016/j.protis.2006.07.004; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Fensome R.A., 1993, CLASSIFICATION FOSSI; FIELD RH, 1992, DIS AQUAT ORGAN, V13, P1, DOI 10.3354/dao013001; FRITZ L, 1992, J PHYCOL, V28, P312, DOI 10.1111/j.0022-3646.1992.00312.x; Groisillier A, 2006, AQUAT MICROB ECOL, V42, P277, DOI 10.3354/ame042277; Horiguchi T, 2000, J PHYCOL, V36, P960, DOI 10.1046/j.1529-8817.2000.00007.x; HUDSON DA, 1994, DIS AQUAT ORGAN, V19, P109, DOI 10.3354/dao019109; Jeon SO, 2006, APPL ENVIRON MICROB, V72, P6578, DOI 10.1128/AEM.00787-06; Johansson M, 2004, J PLANKTON RES, V26, P67, DOI 10.1093/plankt/fbg115; López-García P, 2001, NATURE, V409, P603, DOI 10.1038/35054537; López-García P, 2003, P NATL ACAD SCI USA, V100, P697, DOI 10.1073/pnas.0235779100; Massana R, 2004, FEMS MICROBIOL ECOL, V50, P231, DOI 10.1016/j.femsec.2004.07.001; Nakayama Takeshi, 1996, Phycological Research, V44, P47, DOI 10.1111/j.1440-1835.1996.tb00037.x; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; RAUSCH H, 1989, J MOL EVOL, V29, P255, DOI 10.1007/BF02100209; RIS H, 1974, J CELL BIOL, V60, P702, DOI 10.1083/jcb.60.3.702; Saldarriaga JF, 2004, EUR J PROTISTOL, V40, P85, DOI 10.1016/j.ejop.2003.11.003; Skovgaard A, 2005, PROTIST, V156, P413, DOI 10.1016/j.protis.2005.08.002; Stentiford GD, 2002, J INVERTEBR PATHOL, V79, P179, DOI 10.1016/S0022-2011(02)00028-9; Stoeck T, 2006, PROTIST, V157, P31, DOI 10.1016/j.protis.2005.10.004; SWOFFORD DL, 2002, PAUP PHYLOGENETIC AN; Takano Y, 2006, J PHYCOL, V42, P251, DOI 10.1111/j.1529-8817.2006.00177.x; Takano Y, 2004, PHYCOL RES, V52, P107, DOI 10.1111/j.1440-183.2004.00332.x; VANDERSTAAY SYM, 2001, NATURE, V401, P607	34	72	82	0	9	ELSEVIER GMBH, URBAN & FISCHER VERLAG	JENA	OFFICE JENA, P O BOX 100537, 07705 JENA, GERMANY	1434-4610			PROTIST	Protist	JUL	2007	158	3					337	347		10.1016/j.protis.2007.03.005	http://dx.doi.org/10.1016/j.protis.2007.03.005			11	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	194GU	17560828	Green Submitted			2025-03-11	WOS:000248333500005
J	Mahmoud, MS; Deaf, AS				Mahmoud, Magdy S.; Deaf, Amr S.			Cretaceous palynology (spores, pollen and dinoflagellate cysts) of the Siqeifa 1-X borehole, northern Egypt	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article							STRATIGRAPHY; MIDDLE	Diverse and well preserved palynofloras were recognized in the Lower Cretaceous succession penetrated by well Siqeifa 1-X in northern Egypt. Dinoflagellate cysts such as Subtilisphaera senegalensis was regarded, with the spores Impardecispora apiverrucata and Aequitriradites spinulosus, as important Berriasian to Barremian species. Afropollis operculatuslzonatus pollen and spores such as Balmeisporites holodictyus, Trilobosporites laevigatus and Duplexisporites generalis are diagnostic of Aptian. The lowest occurrences of the pollen Afropollis jardinus, the spore Crybelosporites pannuceus and elaterates such as Elaterosporites klaszii, Elaterocolpites castelainii and Elateroplicites africaensis characterize the Albian/lower Cenomanian interval. The palynofloras enabled the recognition of five spore-pollen and four dinoflagellate zones, which are correlated with regional records, mainly from Egypt and Libya. The vertical distribution of terrestrial and marine palynomorphs, along with palynodebris, reflects two regressive marginal marine cycles during Berriasian-Barremian and Albian-lower Cenomanian times whereas the Aptian witnessed a transgressive open marine (inner shelf) environment. A warm humid palacoclimate was inferred during deposition of the investigated succession of the borehole, in contrast to the known warm and to semi-arid climate, suggested for the Northern Gondwana Realm during Early Cretaceous times. This is probably due to the palaeogeographic position of Egypt during Early Cretaceous times or, to a local reason. Palynofloras from Siqeifa 1 -X borehole, with Afropollis pollen and claterates, are of North African aspect and share the broad characteristics of the "Albian-Cenomanian Elaterates Province" of Herngreen et al. (1996). Abundance of spores and araucariacean pollen are transitional features between those in North Gondwana and Southern Laurasia but, unlikely, typical transitional assemblages contain bisaccates conifers and have Gleicheniaceae spores.	Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt; Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	Egyptian Knowledge Bank (EKB); Assiut University; NERC National Oceanography Centre; University of Southampton	Mahmoud, MS (通讯作者)，Assiut Univ, Dept Geol, Fac Sci, Assiut 71516, Egypt.	magdysm@yahoo.com; deaf@noc.soton.ac.uk	Mahmoud, Magdy/ABD-1262-2020; Deaf, Amr/AAF-6269-2020	Deaf, Amr/0000-0002-5073-7911				ANANYORKE R, 1978, GEOLOGICAL ASS CANAD, V18, P473; [Anonymous], FIN REP COMP LOG SIQ; ARCHANGELSKY S, 1967, Review of Palaeobotany and Palynology, V5, P179, DOI 10.1016/0034-6667(67)90221-7; ARCHANGELSKY S, 1967, Review of Palaeobotany and Palynology, V1, P211, DOI 10.1016/0034-6667(67)90123-6; Awad M.Z., 1994, Berliner geowissenschaftlische Abhandlungen A, V161, P1; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BESEMS RE, 1982, P K NED AKAD B PHYS, V85, P1; BRENNER G.J., 1968, POLLEN SPORES, V10, P341; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; DELIMA MR, 1983, REV BRASILEIRA GEOCI, V13, P223; Dino R, 1999, REV PALAEOBOT PALYNO, V105, P201, DOI 10.1016/S0034-6667(98)00076-1; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; EL Beialy SY, 1994, QATAR U SCI J, V14, P148; Ela N.M. 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Pal, V29, P61; Mahmoud M.S., 2002, Revista Espanola de Micropaleontologia, V34, P129; Mahmoud M.S., 1999, 1 INT C GEOL AFR, V1, P1; MAHMOUD MS, 1994, N JB GEOL PALAONT, V3, P155; MAHMOUD MS, 2003, 3 INT C GEOL AFR, V2, P409; OMRAN AM, 1990, REV PALAEOBOT PALYNO, V66, P293, DOI 10.1016/0034-6667(90)90044-J; Parrish JT., 1987, ORIGINS ANGIOSPERMS, P51; Penny J., 1986, SP PAP PALAEONTOL, V35, P121; Penny J. H., 1988, J MICROPALAEONTOL, V7, P201, DOI DOI 10.1144/JM.7.2.201; PENNY J H J, 1991, Palaeontographica Abteilung B Palaeophytologie, V222, P31; Ravn R.L., 1998, TAXON ELECT INTERNET; Reyre Y., 1973, M M MUS NAT DHIST NA, V27, P1; SAAD S I, 1976, Pollen et Spores, V18, P407; SAAD S I, 1978, Pollen et Spores, V20, P261; Schrank E, 1998, J AFR EARTH SCI, V26, P167, DOI 10.1016/S0899-5362(98)00004-9; SCHRANK E, 1984, N JB GEOL PALAONT MH, P95; SCHRANK E., 1990, Berliner geowissenschaftliche Abhandlungen. Abteilung A, V120, P149; Schrank E., 1996, INPROCEEDINGS 9 INT, P201; Schrank E., 1995, BERLINER GEOWISSENSC, V177, P1; Schrank E., 1987, BERLINER GEOWISS ABH, V75, P249, DOI DOI 10.1016/0195-6671(92)90040-W; Thusu B., 1988, SUBSURFACE PALYNOSTR, P171; TREVISAN L, 1980, Pollen et Spores, V22, P85; Uwins F.J.R., 1988, SUBSURFACEPALYNOSTRA, P215; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817	51	39	41	0	3	UNIV STUDI MILANO	MILANO	C/O RIVISTA ITALIANA PALEONTOLOGIA STRATIGRAFIA, VIA MANGIAGALLI, 34, 20133 MILANO, ITALY	0035-6883	2039-4942		RIV ITAL PALEONTOL S	Riv. Ital. Paleontol. Stratigr.	JUL	2007	113	2					203	221		10.13130/2039-4942/5871	http://dx.doi.org/10.13130/2039-4942/5871			19	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	197XA					2025-03-11	WOS:000248588800004
J	Borel, CM				Borel, C. Marcela			Non siliceous algae and acritarchs from the Holocene coastal deposits at the La Ballenera Creek, Buenos Aires, Argentina	AMEGHINIANA			Spanish	Article						palynology; algae; acritarchs; holocene; Buenos Aires; Argentina	QUEQUEN-GRANDE RIVER; TAGELUS-PLEBEIUS LIGHTFOOT; 1786 MOLLUSCA; PROVINCE; BIVALVIA	NON SILICEOUS ALGAE AND ACRITARCHS FROM THE HOLOCENE COASTAL DEPOSITS AT THE LA BALLENERA CREEK, BUENOS AIRES, ARGENTINA. The palynological analysis of the Holocene sequence that crops out at arroyo La Ballenera (38 degrees 19' S; 57 degrees 57' W), southeastern littoral of Buenos Aires province, allows the establishment of three zones (LB-1, LB-2, LB-3) and two subzones (LB-3a and b). This analysis is based on non-pollen aquatic palynomorphs: algae (Chlorophyta, Cyanophyta and Dinoflagellata), invertebrate remains and acritarchs. The chlorophycean algae consist of colonies of Botryococcus braunii Kutzing, zygospores of Zygnemataceae (Mougeotia sp., Spirogyra sp. I and Spirogyra sp. 2) and phycomas of Prasinophyceae. Cyanophycean sheets of Gloeotrichia sp. are rare. The assemblages also contain non-marine dinoflagellate cysts of affinity with a peridinioid genus. The acritarchs are represented by Cobricosphaeridium spp. (probably copepod or anostracod eggs), Micrhystridium sp. and other species defined under an open nomenclature. Between 6,790 - 6,300 C-14 yr. B.P., these palynomorphs show the beginning of marine influence in the site and reveal a marsh enviromnent in close relation with shallow freshwater habitats. Between 6,300 C-14 - ca. 5,600 C-14 yr. B.P. the presence of dinocysts of Peridinioideae, Gloeotrichia and Botryococcus indicate the development of a marginal brackish water body, oligotrophic to mesotrophic, of low energy, with a considerable freshwater influence. From 5,600 C-14 yr. B.P. to 4,700 C-14 yr. B.P. the algae and acritarchs reflect an increase of salinity, related with a major marine influence. After ca. 4,700 C-14 yr. B.P. Cobricosphaeridium is present along with Botryococcus and other acritarchs, indicating a coastal, unstable water body of lower salinity than the aforementioned zone.	Inst Argentino Oceanog, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Borel, CM (通讯作者)，Inst Argentino Oceanog, Complejo CRIBABB Camino La Carrindanga 7-5Km,CC 8, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	mabore1@criba.edu.ar		Borel, C. Marcela/0000-0001-5772-4534				[Anonymous], PALYNOLOGICAL TECHNI; Batten DJ., 1996, Palynology: principles and applications, P191; BOLTOVSKOY A, 1976, Physis Seccion B las Aguas Continentales y sus Organismos, V35, P147; BOLTOVSKOY A, 1989, NOVA HEDWIGIA, V49, P369; BOLTOVSKOY A, 1973, Physis Seccion B las Aguas Continentales y sus Organismos, V32, P331; BOLTOVSKOY A, 1975, Physis Seccion B las Aguas Continentales y sus Organismos, V34, P73; Boltovskoy A., 1973, Revista Esp Micropaleont, V5, P81; Borel CM, 2003, AMEGHINIANA, V40, P531; BOREL CM, 2003, THESIS U NACL SUR; Burgos J.J., 1951, Meteoros, V1, P3; COHEN RG, 1995, ECOSISTEMAS AGUAS CO, V2; Daugbjerg Niels, 2000, Phycological Research, V48, P199, DOI 10.1111/j.1440-1835.2000.tb00216.x; De Francesco CG, 2001, AMEGHINIANA, V38, P467; De Francesco CG, 1999, AMEGHINIANA, V36, P297; Espinosa M, 2003, J PALEOLIMNOL, V29, P49, DOI 10.1023/A:1022873131949; Faegri Knut., TXB POLLEN ANAL; Golfieri GA, 1998, AMEGHINIANA, V35, P255; Gómez EA, 2005, J S AM EARTH SCI, V20, P139, DOI 10.1016/j.jsames.2005.06.01; Grill S.C., 1995, POLEN, V7, P41; GRIMM E., 1991, TILIA SOFTWARE; GUARRERA S A, 1968, REVISTA DEL MUSEO DE LA PLATA SECCION BOTANICA, V10, P223; GUYYOHLSON D, 1996, PALYNOLOGY PRINCIPLE, V1, P181; Head M.J., 2003, J PALEONTOL, V77, P963; HOFFMEYER MS, 1997, CAPITULO 3  BIOL I A; Isla F.I., 2001, Revista Brasileira de Geomorfologia, V2, P73, DOI [10.20502/rbg.v2i1.9, DOI 10.20502/rbg.v2i1.9]; ISLA FI, 1998, ACT 7 REUN ARG SED S, P24; PALS JP, 1980, REV PALAEOBOT PALYNO, V30, P371, DOI 10.1016/0034-6667(80)90020-2; PARKE M, 1964, J MAR BIOL ASSOC UK, V44, P499, DOI 10.1017/S0025315400024954; STUTZ S., 2000, Historia de la vegetacion del litoral bonaerense durante el ultimo ciclo transgresivo-regresivo del Holoceno; STUTZ S, 2002, 8 C ARG PAL BIOESTR, P55; Stutz S., 1999, ASOCIACION PALEONTOL, V6, P65; Van Geel B., 1996, M. PACT, V50, P399; van Geel B., 2001, TRACKING ENV CHANGE, P99, DOI DOI 10.1007/0-306-47668-1_6; Vilanova I, 2006, J QUATERNARY SCI, V21, P227, DOI 10.1002/jqs.953	34	18	18	0	2	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	JUN 30	2007	44	2					359	366						8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	212IV					2025-03-11	WOS:000249590800008
J	Zonneveld, KAF; Mackensen, A; Baumann, KH				Zonneveld, Karin A. F.; Mackensen, Andreas; Baumann, Karl-Heinz			Stable oxygen isotopes of <i>Thoracosphaera heimii</i> (Dinophyceae) in relationship to temperature;: a culture experiment	MARINE MICROPALEONTOLOGY			English	Article						oxygen isotopes; calcareous dinoflagellate cysts; temperature; culture	SEAWATER CARBONATE CONCENTRATION; DIEL VERTICAL MIGRATION; BIOLOGICAL CARBONATES; MARINE DINOFLAGELLATE; COCCOLITH CARBONATE; INORGANIC CARBON; PHOTOSYNTHESIS; DISEQUILIBRIUM; EQUILIBRIUM; SEDIMENTS	To establish a relationship between temperature and the stable oxygen isotopic composition (delta O-18) of vegetative cysts of the photosynthetic calcareous dinoflagellate cyst Thoracosphaera heindi, two unicellular cultures of T heiniii have been cultured under different temperatures by using a temperature gradient box. There is a clear relationship between temperature variance and the isotopic composition of T heimii cysts according to the relationship: T(degrees C)=-6.827 (delta O-18(c)-delta O-18(w))-3.906 (R=0.921), with c = calcite and w = water. Within this paper we are the first to discuss the possible vital effects that might cause an offset between the temperature-isotope relationship found for T heiniii calcite and that of equilibrium inorganic calcite precipitation. No indication for strong kinetic effects as result of fast calcite precipitation can be found. We observed a positive relationship between delta O-18(c)-delta O-18(w) and ambient mediumwater pH. We speculate that this might be the result of the presence of external carbonate anhydrase, which is common in photosynthetic dinoflagellates. The efficiency of this enzyme increases rapidly between pH 7.5 to 9, which could result in an increase in CO2 uptake relative to HCO3- with increasing pH. We furthermore discuss the possibility of T hehnii using respirative 3 carbon at least as part of its carbon source for calcite precipitation, which can be based on the light values of 61110,480, and delta C-13(C)-delta C-13(DIC) (DIC = dissolved inorganic carbon) found in this and previous studies on the isotopic composition of calcareous dinoflagellates. The results of this study as well as the broad geographic distribution of T heindi, its stable position within the water column, its presence in the geological record since the Late Cretaceous and its resistance against dissolution compared to other plankton groups underlines the potential for a wide usability of the oxygen isotope composition of T heimii as palaeotemperature proxy for the deeper parts of the photic zone. (C) 2007 Elsevier B.V. All rights reserved.	Univ Bremen, Geowissensch FB 5, D-27334 Bremen, Germany; Alfred Wegener Inst Polar & Marine Res, D-2850 Bremerhaven, Germany	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Zonneveld, KAF (通讯作者)，Univ Bremen, Geowissensch FB 5, Postfach 330440, D-27334 Bremen, Germany.	zonnev@uni-bremen.de	Mackensen, Andreas/J-8600-2013	Mackensen, Andreas/0000-0002-5024-4455				Adkins JF, 2003, GEOCHIM COSMOCHIM AC, V67, P1129, DOI 10.1016/S0016-7037(02)01203-6; ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; Baumann KH, 2004, SOUTH ATLANTIC IN THE LATE QUATERNARY: RECONSTRUCTION OF MATERIAL BUDGETS AND CURRENT SYSTEMS, P81; Bemis BE, 1998, PALEOCEANOGRAPHY, V13, P150, DOI 10.1029/98PA00070; BermanFrank I, 1995, J PHYCOL, V31, P906, DOI 10.1111/j.0022-3646.1995.00906.x; Bijma J., 1999, USES PROXIES PALEOCE, P489, DOI DOI 10.1007/978-3-642-58646-0_20; Dason JS, 2004, J PHYCOL, V40, P285, DOI 10.1111/j.1529-8817.2004.03123.x; DUDLEY WC, 1986, MAR MICROPALEONTOL, V10, P1, DOI 10.1016/0377-8398(86)90021-6; DUDLEY WC, 1980, NATURE, V285, P222, DOI 10.1038/285222a0; Fisher G., 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic, P1; Friedrich O, 2003, MICROPALEONTOLOGY, V49, P375, DOI 10.1661/0026-2803(2003)049[0375:SIIFTC]2.0.CO;2; GAO XP, 1989, BRIT PHYCOL J, V24, P153; Giordano M, 2005, ANNU REV PLANT BIOL, V56, P99, DOI 10.1146/annurev.arplant.56.032604.144052; Grice K, 1998, PALEOCEANOGRAPHY, V13, P686, DOI 10.1029/98PA01871; Hildebrand-Habel T, 2000, INT J EARTH SCI, V88, P694, DOI 10.1007/s005310050298; Hut G., 1987, CONSULTANTS GROUP M, P1; INOUYE I, 1983, S AFR J BOT, V2, P63, DOI 10.1016/S0022-4618(16)30147-4; Kamykowski D, 1998, J PLANKTON RES, V20, P1781, DOI 10.1093/plankt/20.9.1781; Karwath B, 2000, INT J EARTH SCI, V88, P668, DOI 10.1007/s005310050296; Karwath B, 2000, MAR MICROPALEONTOL, V39, P43, DOI 10.1016/S0377-8398(00)00013-X; Karwath B, 2000, BERICHTE FACHBEREICH, V152, P1; Kim ST, 1997, GEOCHIM COSMOCHIM AC, V61, P3461, DOI 10.1016/S0016-7037(97)00169-5; King AL, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2002PA000839; Langer G, 2006, LIMNOL OCEANOGR, V51, P310, DOI 10.4319/lo.2006.51.1.0310; LIEBERMAN OS, 1994, J PHYCOL, V30, P964, DOI 10.1111/j.0022-3646.1994.00964.x; MCCONNAUGHEY T, 1989, GEOCHIM COSMOCHIM AC, V53, P151, DOI 10.1016/0016-7037(89)90282-2; McConnaughey TA, 2003, CORAL REEFS, V22, P316, DOI 10.1007/s00338-003-0325-2; McConnaughey TA, 1997, GEOCHIM COSMOCHIM AC, V61, P611, DOI 10.1016/S0016-7037(96)00361-4; Nimer NA, 1997, J PHYCOL, V33, P625, DOI 10.1111/j.0022-3646.1997.00625.x; Nimer NA, 1999, PLANT PHYSIOL, V120, P105, DOI 10.1104/pp.120.1.105; PAULL CK, 1994, DEEP-SEA RES PT I, V41, P223, DOI 10.1016/0967-0637(94)90034-5; ROMANEK CS, 1992, GEOCHIM COSMOCHIM AC, V56, P419, DOI 10.1016/0016-7037(92)90142-6; Rost B, 2006, PLANT CELL ENVIRON, V29, P810, DOI 10.1111/j.1365-3040.2005.01450.x; Spero HJ, 1996, MAR MICROPALEONTOL, V28, P231, DOI 10.1016/0377-8398(96)00003-5; Spero HJ, 1997, NATURE, V390, P497, DOI 10.1038/37333; Stoll HM, 2001, GEOCHEM GEOPHY GEOSY, V2, DOI 10.1029/2000GC000144; Stoll HM, 2004, COCCOLITHOPHORES: FROM MOLECULAR PROCESSES TO GLOBAL IMPACT, P529; Stoll HM, 2002, MAR MICROPALEONTOL, V46, P209, DOI 10.1016/S0377-8398(02)00040-3; Stoll HM, 2002, PHILOS T R SOC A, V360, P719, DOI 10.1098/rsta.2001.0966; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7; Young JR, 1999, J STRUCT BIOL, V126, P195, DOI 10.1006/jsbi.1999.4132; Zeebe RE, 1999, GEOCHIM COSMOCHIM AC, V63, P2001, DOI 10.1016/S0016-7037(99)00091-5; Zeebe RE, 2001, PALAEOGEOGR PALAEOCL, V170, P49, DOI 10.1016/S0031-0182(01)00226-7; Ziveri P, 2003, EARTH PLANET SC LETT, V210, P137, DOI 10.1016/S0012-821X(03)00101-8; Zonneveld K, 2004, MAR MICROPALEONTOL, V50, P307, DOI 10.1016/S0377-8398(03)00097-5	46	15	15	0	9	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	JUN 25	2007	64	1-2					80	90		10.1016/j.marmicro.2007.03.002	http://dx.doi.org/10.1016/j.marmicro.2007.03.002			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	185VA					2025-03-11	WOS:000247737300006
J	Holzwarth, U; Esper, O; Zonneveld, K				Holzwarth, Ulrike; Esper, Oliver; Zonneveld, Karin			Distribution of organic-walled dinoflagellate cysts in shelf surface sediments of the Benguela upwelling system in relationship to environmental conditions	MARINE MICROPALEONTOLOGY			English	Review						organic-walled dinoflagellate cysts; upwelling; Benguela system; productivity; chlorophyll-alpha; river mouths	SOUTH ATLANTIC-OCEAN; HYDROGRAPHIC CONDITIONS; SPATIAL-DISTRIBUTION; CONTINENTAL-MARGIN; NEPHELOID LAYERS; NORTH-ATLANTIC; TOKYO-BAY; SEA; ASSEMBLAGES; PRESERVATION	To obtain insight in the relationship between the spatial distribution of organic-walled dinoflagellate cysts (dinocysts) and local environmental conditions, fifty-eight surface sediment samples from the coastal shelf off SW Africa were investigated on their dinocyst content with special focus oil the two main river systems and the active upwelling that characterise this region. To avoid possible overprint by species-selective preservation, samples have been selected mainly from shelf sites where high sedimentation rates and/or low bottom water oxygen concentrations prevail. Multivariate ordination analyses have been carried out to investigate the relationship between the distribution patterns of individual species to environmental parameters of the upper water column and sediment transport processes. The main oceanographical variables at the surface (temperature, salinity, nutrients chlorophyll-a) in the region show onshoreoffshore gradients. This pattern is reflected in the dinocyst associations with high relative abundances of heterotrophic dinocyst species in neritic regions characterised by high chlorophyll-aand low salinity conditions in surface waters. Phototrophic dinocyst species, notably Operculodinium centrocarpum, dominate in the more oceanic area. Differences in the distribution of phototrophic dinocyst species can be related to sea surface salinity and sea surface temperature gradients and to a lesser extent to chlorophyll-a concentrations. Apart from longitudinal gradients the dinocyst distribution clearly reflects regional environmental features. Six groups of species can be distinguished, characteristic for (1) coastal regions (cysts of Polykrikos kofoidii and Selenopemphix quanta), (2) the vicinity of active upwelling (Brigantedinium spp., Echinidinium aculeatum, Echinidinium spp. and Echinidinium transparantinn), (3) river mouths (Lejeunecysta oliva, cysts of Protoperidinium americanum, Selenopemphix nephroides and Votadinium calvum), (4) slope and open ocean sediments (Dalella chathamense, Impagidinium patulum and operculodinium centrocarpum, (5) the southern Benguela region (south of 24 degrees S) (Spiniferites ramosus) and (6) the northern Benguela region (north of 24 degrees S) (Nematosphaeropsis labyrinthus and Pyxidinopsis reticulata). No indication of overprint of the palaeo-ecological signal by lateral transport of allochthonous species could be observed. (C) 2007 Elsevier B.V. All rights reserved.	Univ Bremen, Res Ctr Ocean Margins, D-28334 Bremen, Germany	University of Bremen	Holzwarth, U (通讯作者)，Univ Bremen, Res Ctr Ocean Margins, POB 330440, D-28334 Bremen, Germany.	holzwarth@rcom-bremen.de		Esper, Oliver/0000-0002-4342-3471				AGENBAG JJ, 1988, S AFR J MARINE SCI, V6, P119, DOI 10.2989/025776188784480726; ALLDREDGE AL, 1995, DEEP-SEA RES PT II, V42, P1, DOI 10.1016/0967-0645(95)90003-9; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; BACON MP, 1989, EARTH PLANET SC LETT, V92, P157, DOI 10.1016/0012-821X(89)90043-5; BARANGE M, 1992, CONT SHELF RES, V12, P1027, DOI 10.1016/0278-4343(92)90014-B; BARANGE M, 1992, S AFR J MARINE SCI, V12, P3; BERGER WH, 1982, OCEANOL ACTA, V5, P249; Biebow N., 1996, DINOFLAGELLATENZYSTE; BIRCH GF, 1975, B JOINT GELOGICAL SU, V6; BOCKELMANN FD, 2007, THESIS DEP GEOSCIENC; BREMNER JM, 1981, B JOINT GELOGICAL SU, V10; CHAPMAN P, 1985, OCEANOGR MAR BIOL, V23, P183; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DALE B, 2002, PALAEOGEOGR PALAEOCL, V2893, P1; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DAVEY RJ, 1970, P 2 PLANKT C ROM, V1, P331; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DEVERNAL A, 1991, CANADIAN J FISHERIES, V113, P198; DINGLE RV, 1993, S AFR J MARINE SCI, V13, P33, DOI 10.2989/025776193784287220; Duncombe Rae CM, 2005, AFR J MAR SCI, V27, P617; EDWARDS LE, 1992, NEOGENE QUATERNARY D; Esper O, 2004, GLOBAL PLANET CHANGE, V41, P31, DOI 10.1016/j.gloplacha.2003.10.002; Fensome R.A., 1993, CLASSIFICATION LIVIN, V7; Fensome R. 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Micropaleontol.	JUN 25	2007	64	1-2					91	119		10.1016/j.marmicro.2007.04.001	http://dx.doi.org/10.1016/j.marmicro.2007.04.001			29	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	185VA					2025-03-11	WOS:000247737300007
J	Richter, D; Vink, A; Zonneveld, KAF; Kuhlmann, H; Willems, H				Richter, Dorit; Vink, Annemiek; Zonneveld, Karin A. F.; Kuhlmann, Holger; Willems, Helmut			Calcareous dinoflagellate cyst distributions in surface sediments from upwelling areas off NW Africa, and their relationships with environmental parameters of the upper water column	MARINE MICROPALEONTOLOGY			English	Article						calcareous dinoflagellate cysts; surface sediments; NW Africa; accumulation rates; statistical analyses; ecology	ATLANTIC-OCEAN; THORACOSPHAERA-HEIMII; NORTHWEST AFRICA; CANARY-ISLANDS; SPATIAL AUTOCORRELATION; POTENTIAL USE; TEMPERATURE; SEA; DISSOLUTION; RECONSTRUCTION	Only very few studies have focussed on the spatial distribution and ecology of calcareous dinoflagellate cysts (dinocysts) in upwelling areas. Here, distributions of individual calcareous dinocyst species in surface sediment samples from the coastal upwelling zone off NW Africa and their relationships with known environmental parameters of the (sub-)surface waters have been analysed in order to enhance our knowledge on their modem distribution patterns and to determine the ecological significance and palaeoenvironmental reconstruction potential of each calcareous dinocyst species within this exemplary high-productivity region. in addition to calculating relative cyst abundances, well-constrained sedimentation rates have allowed the calculation of dinocyst accumulation rates (Cysts cm(-2) ka(-1)) for most of the surface sample positions, thus providing a much more accurate estimation of actual calcareous dinocyst production in the upper water column than could be warranted in similar studies so far. Distinct differences in the geographic distribution patterns of nine species were observed. In general, high accumulation rates of calcareous dinocysts were found around and south of 29 degrees N and offshore the westernmost Canary Island La Palma, with slightly lower accumulation rates in the upwelling-influenced areas off Cape Yubi and in the upwelling filament area off Cape Ghir. Multivariate ordination techniques were applied in order to compare the cyst accumulation rates of individual species with physical parameters (temperature, salinity, density, mixed layer depth) and the trophic state (nitrate, phosphate and chlorophyll concentrations) of the overlying (sub-)surface waters. All species were found to relate significantly to one or more of the environmental parameters, partly confirming previous results on cyst ecology but also providing new information which will be useful for future palaeoenvironmental reconstructions within upwelling areas. (c) 2007 Elsevier B.V All rights reserved.	Univ Bremen, Fachbereich Geowissenschaften 5, D-28334 Bremen, Germany; Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany	University of Bremen	Richter, D (通讯作者)，Univ Bremen, Fachbereich Geowissenschaften 5, Postfach 330440, D-28334 Bremen, Germany.	siggel@rcom-bremen.de	; Vink, Annemiek/GXG-6435-2022	Kuhlmann, Holger/0000-0001-8932-7031; Vink, Annemiek/0000-0002-5178-9721				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Barton E., 1998, The Sea: The Global Coastal Ocean. 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F., 2005, Palaeontologische Zeitschrift, V79, P61	62	17	17	0	9	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	JUN 13	2007	63	3-4					201	228		10.1016/j.marmicro.2006.12.002	http://dx.doi.org/10.1016/j.marmicro.2006.12.002			28	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	178PK					2025-03-11	WOS:000247232400006
J	Wheeler, K; Shields, JD; Taylor, DM				Wheeler, Kersten; Shields, Jeffrey D.; Taylor, David M.			Pathology of <i>Hematodinium</i> infections in snow crabs (<i>Chionoecetes opilio</i>) from Newfoundland, Canada	JOURNAL OF INVERTEBRATE PATHOLOGY			English	Article						bitter crab disease; bitter crab syndrome; sporulation; gills; hepatopancreas; fishery; disease; crab	LOBSTER NEPHROPS-NORVEGICUS; PARASITIC DINOFLAGELLATE; NORWAY LOBSTER; CALLINECTES-SAPIDUS; BLUE CRABS; DISEASE; PEREZI; PREVALENCE; MORTALITY; SP.	Bitter crab disease (BCD) of snow crabs, Chionoecetes opilio, is caused by a parasitic dinoflagellate, Hematodinium sp. The disease has shown an alarming increase in prevalence in the commercial fishery in eastern and northeastern areas of Newfoundland and Labrador since it was first recorded there in the early 1990s. We documented histopathological alterations to the tissues in snow crabs with heavy infections of Honatodinium sp. and during sporulation of the parasite. Pressure necrosis was evident in the spongy connective tissues of the hepatopancreas and the blood vessels in most organs. In heavy infections, little remained of the spongy connective tissues around the hepatopancreas. Damage to the gills varied; in some cases it was severe, particularly during sporulation, involving apparent thinning of the cuticle, loss of epithelial cells, and fusion of the membranous layers of adjacent gill lamellae. Affected lamellae exhibited varying degrees of distention with a loss of trabecular cells, heitiocyte infiltrations, and swelling or "clubbing" along the distal margins. Large numbers of zoospores were located along the distal margins of affected lamellae suggesting that sporulation may cause a lysis or bursting of the thin lamellar cuticle, releasing spores. Pressure necrosis, due to the build up of high densities of parasites, was the primary histopathological alteration in most tissues. Hematodinium infections in the snow crab are chronic, long-term infections that end in host death, during sporulation of the parasite. (c) 2007 Elsevier Inc. All rights reserved.	Coll William & Mary, Sch Marine Sci, Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA; Fisheries & Oceans Canada, St John, NF A1C 5X1, Canada	William & Mary; Virginia Institute of Marine Science; Fisheries & Oceans Canada	Shields, JD (通讯作者)，Coll William & Mary, Sch Marine Sci, Virginia Inst Marine Sci, 1208 Greate Rd, Gloucester Point, VA 23062 USA.	jeff@vims.edu		Shields, Jeffrey D./0000-0002-2658-4572				Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; Dawe EG, 2002, LOW WAKE FI, V19, P385; *DEP FISH OC, 2006, SPEC QUOT REP SNOW C; Factor JR, 2005, J SHELLFISH RES, V24, P713; FIELD RH, 1995, DIS AQUAT ORGAN, V22, P115, DOI 10.3354/dao022115; FIELD RH, 1992, DIS AQUAT ORGAN, V13, P1, DOI 10.3354/dao013001; Hébert M, 2002, CRUSTACEANA, V75, P671, DOI 10.1163/156854002760202679; HUDSON DA, 1994, DIS AQUAT ORGAN, V19, P109, DOI 10.3354/dao019109; Johnson PT., 1980, HISTOLOGY BLUE CRAB; Luna LG., 1968, MANUAL HISTOLOGIC ST, P258, DOI DOI 10.1038/OBY.20230; MESSICK GA, 1994, DIS AQUAT ORGAN, V19, P77, DOI 10.3354/dao019077; MEYERS TR, 1987, DIS AQUAT ORGAN, V3, P195, DOI 10.3354/dao003195; Pestal GP, 2003, DIS AQUAT ORGAN, V53, P67, DOI 10.3354/dao053067; Sheppard M, 2003, J SHELLFISH RES, V22, P873; Shields JD, 2005, DIS AQUAT ORGAN, V64, P253, DOI 10.3354/dao064253; Shields JD, 2003, B MAR SCI, V72, P519; Shields JD, 2000, FISH B-NOAA, V98, P139; SHIELDS JD, EPIDEMIOLOGICAL DETE; Stentiford GD, 2000, DIS AQUAT ORGAN, V42, P133, DOI 10.3354/dao042133; Stentiford GD, 2005, DIS AQUAT ORGAN, V66, P47, DOI 10.3354/dao066047; Stentiford GD, 2005, J INVERTEBR PATHOL, V88, P136, DOI 10.1016/j.jip.2005.01.006; Stentiford GD, 2002, J INVERTEBR PATHOL, V79, P179, DOI 10.1016/S0022-2011(02)00028-9; Stentiford GD, 2001, GEN COMP ENDOCR, V121, P13, DOI 10.1006/gcen.2000.7575; Taylor AC, 1996, J EXP MAR BIOL ECOL, V207, P217, DOI 10.1016/S0022-0981(96)02649-4; Taylor D.M., 1989, North American Journal of Fisheries Management, V9, P504, DOI 10.1577/1548-8675(1989)009<0504:SHISCC>2.3.CO;2; TAYLOR DM, 1995, J INVERTEBR PATHOL, V65, P283, DOI 10.1006/jipa.1995.1043	26	35	40	1	16	ACADEMIC PRESS INC ELSEVIER SCIENCE	SAN DIEGO	525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA	0022-2011	1096-0805		J INVERTEBR PATHOL	J. Invertebr. Pathol.	JUN	2007	95	2					93	100		10.1016/j.jip.2007.01.002	http://dx.doi.org/10.1016/j.jip.2007.01.002			8	Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Zoology	177LA	17336326				2025-03-11	WOS:000247153400004
J	Tillmann, U; John, U; Cembella, A				Tillmann, Urban; John, Uwe; Cembella, Allan			On the allelochemical potency of the marine dinoflagellate <i>Alexandrium ostenfeldii</i> against heterotrophic and autotrophic protists	JOURNAL OF PLANKTON RESEARCH			English	Article							PRYMNESIUM-PARVUM; CYST FORMATION; LIFE-HISTORY; FOOD UPTAKE; PHYTOPLANKTON; GROWTH; DINOPHYCEAE; ALLELOPATHY; HAPTOPHYTE; TAMARENSE	Three strains of the marine dinoflagellate Alexandrium ostenfeldii of different geographic origin were tested for their short-term deleterious effects on a diversity of marine protists. All A. ostenfeldii strains were capable of eliciting an apparent allelochernical response, but the various protistan target species were differentially affected. Protists that were negatively affected by exposure to cells of A. ostenfeldii and associated extracellular metabolites comprised both autotrophs (Rhodomonas sp., Dunaliella salina, Thalassiosira weissflogii) and heterotrophs (Oxyrrhis marina, Amphidinium crassum, Rimostrombidium caudatum). Observed effects included immobilisation (e.g. of O. marina), morphological changes (e.g. in D. salina) and/or aberrant behaviour (e.g. of R. caudatum), mainly as preliminary stages of cell lysis. Immobilization and lytic effects against O. marina were strongly dependent on A. ostenfeldii cell concentrations. Effects also differed substantially among strains and different batch cultures of the same strain. Values of EC50, defined as the A. ostenfeldii cell concentration causing lysis of 50% of O. marina cells, ranged from 0.3 to 1.9 x 10(3) mL(-1), depending on the A. ostenfeldii strain. The autotrophic dinoflagellate Scrippsiella trchoidea reacted to exposure to A. ostenfeldii cells by formation of temporay (ecdysal) cysts, whereas, in contrast, the flagellates Emaliania huxleyi and Prymnesium parvum and the ciliate Strombidium sp. were relatively refractory or even unaffected. As long as cells did not lyse, the fluorescence field of target autotrophs, estimated by pulse-amplitude modulation fluorometry, did not significantly change during the first 3 h of incubation, suggesting that allelochemicals produced by A. ostenfeldii caused no shortterm negative effects oil the photosynthetic apparatus. Overall, the allelochemical responses of target species showed no obvious relationship to cell quota or extracellular concentrations of either toxic inacrog,clic innues (spirolides) or letralydropurine neuroloxins (saxitoxill and analogues) produced by various strains of A. ostenfeldii. Instead, the poteng of A. osteifieldii, eliciting immobilization and lytic speries-specific responses in potential piedato?s and competitors, is consistent with the existence of all alleloclienzical meckam m unrelated to the bioactiviy of known phycoloxins of the genus A lexandrium.	Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Tillmann, U (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Am Handelshafen 12, D-27570 Bremerhaven, Germany.	utillmann@awi-bremerhaven.de	John, Uwe/S-3009-2016	John, Uwe/0000-0002-1297-4086				ALLDREDGE AL, 1987, SCIENCE, V235, P689, DOI 10.1126/science.235.4789.689; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Arzul G, 1999, J EXP MAR BIOL ECOL, V232, P285, DOI 10.1016/S0022-0981(98)00120-8; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLANCO J, 1988, AQUACULTURE, V68, P289, DOI 10.1016/0044-8486(88)90242-6; BUSKEY EJ, 1988, B MAR SCI, V43, P783; Carlsson P, 1998, AQUAT MICROB ECOL, V16, P65, DOI 10.3354/ame016065; Cembella A.D., 1998, Physiological Ecology of Harmful Algal Blooms, P381; Cembella AD, 2000, PHYCOLOGIA, V39, P67, DOI 10.2216/i0031-8884-39-1-67.1; Cembella AD, 1999, NAT TOXINS, V7, P197, DOI 10.1002/1522-7189(200009/10)7:5<197::AID-NT62>3.3.CO;2-8; Cembella AD, 2003, PHYCOLOGIA, V42, P420, DOI 10.2216/i0031-8884-42-4-420.1; Ceniceros HD, 2002, COMMUN PURE APPL ANA, V1, P1; DAHL E, 1989, NOVEL PHYTOPLANKTON, P383; Doucette G.J., 1998, PHYSL ECOLOGY HARMFU, P619; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Fenchel T, 1999, PROTIST, V150, P325, DOI 10.1016/S1434-4610(99)70033-7; Fistarol GO, 2004, ENVIRON MICROBIOL, V6, P791, DOI 10.1111/j.1462-2920.2004.00609.x; Fistarol GO, 2004, AQUAT MICROB ECOL, V35, P45, DOI 10.3354/ame035045; Gentien P., 1998, Physiological Ecology of Harmful Algal Blooms, P155; GLEASON FK, 1986, FEMS MICROBIOL LETT, V33, P85; Granéli E, 2006, ECOL STU AN, V189, P189, DOI 10.1007/978-3-540-32210-8_15; Granéli E, 2003, HARMFUL ALGAE, V2, P135, DOI 10.1016/S1568-9883(03)00006-4; Granéli E, 2003, MAR ECOL PROG SER, V254, P49, DOI 10.3354/meps254049; Gribble KE, 2005, DEEP-SEA RES PT II, V52, P2745, DOI 10.1016/j.dsr2.2005.06.018; HANSEN PJ, 1992, J PHYCOL, V28, P597, DOI 10.1111/j.0022-3646.1992.00597.x; HANSEN PJ, 1989, MAR ECOL PROG SER, V53, P105, DOI 10.3354/meps053105; HEWLETT PS, 1979, INTRO INTERPRETATION, P12; HU TM, 1995, J CHEM SOC CHEM COMM, P2159, DOI 10.1039/c39950002159; Jacobson DM, 1996, J PHYCOL, V32, P279, DOI 10.1111/j.0022-3646.1996.00279.x; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; John EH, 1999, MAR BIOL, V133, P11, DOI 10.1007/s002270050437; John U, 2003, EUR J PHYCOL, V38, P25, DOI 10.1080/0967026031000096227; John Uwe, 2002, Harmful Algae, V1, P45, DOI 10.1016/S1568-9883(02)00005-7; Juneau P, 2005, PHOTOCHEM PHOTOBIOL, V81, P649, DOI 10.1562/2005-01-13-RA-414.1; KELLER MD, 1987, J PHYCOL, V23, P633; KONOVALOVA GV, 1993, DEV MAR BIO, V3, P275; Legrand C, 2003, PHYCOLOGIA, V42, P406, DOI 10.2216/i0031-8884-42-4-406.1; Legrand C, 1998, AQUAT MICROB ECOL, V16, P81, DOI 10.3354/ame016081; Mackenzie L, 1996, PHYCOLOGIA, V35, P148, DOI 10.2216/i0031-8884-35-2-148.1; MacKinnon SL, 2006, J NAT PROD, V69, P983, DOI 10.1021/np050220w; Maclean C, 2003, BOT MAR, V46, P466, DOI 10.1515/BOT.2003.048; Matsuoka K, 2000, PHYCOLOGIA, V39, P82, DOI 10.2216/i0031-8884-39-1-82.1; McClintock J.B., 2001, MARINE CHEM ECOLOGY; MITCHELL JG, 1985, NATURE, V316, P58, DOI 10.1038/316058a0; Ogata T, 1996, HARMFUL TOXIC ALGAL, P343; Paulsen O., 1904, MEDD KOMM HAVUNDERS, V1, P1; Pedersen MF, 2003, MAR ECOL PROG SER, V260, P33, DOI 10.3354/meps260033; Richard D., 2001, 9 INT C HARMFUL MICR, P383; Richardson K, 1997, ADV MAR BIOL, V31, P301, DOI 10.1016/S0065-2881(08)60225-4; Rines JEB, 2002, MAR ECOL PROG SER, V225, P123, DOI 10.3354/meps225123; Schmidt LE, 2001, MAR ECOL PROG SER, V216, P67, DOI 10.3354/meps216067; Schmitter R.E., 1979, P123; SCHREIBER U, 1986, PHOTOSYNTH RES, V10, P51, DOI 10.1007/BF00024185; Skovgaard A, 2003, LIMNOL OCEANOGR, V48, P1161, DOI 10.4319/lo.2003.48.3.1161; Skovgaard A, 2003, AQUAT MICROB ECOL, V31, P259, DOI 10.3354/ame031259; Sukenik A, 2002, LIMNOL OCEANOGR, V47, P1656, DOI 10.4319/lo.2002.47.6.1656; Taylor F.J.R., 1998, NATO ASI Series Series G Ecological Sciences, V41, P3; TAYLOR JFR, 1987, BIOL DINOFLAGELLATES; Tillmann U, 2003, AQUAT MICROB ECOL, V32, P73, DOI 10.3354/ame032073; Tillmann U, 1998, AQUAT MICROB ECOL, V14, P155, DOI 10.3354/ame014155; Tillmann U, 2002, MAR ECOL PROG SER, V230, P47, DOI 10.3354/meps230047; Toth GB, 2004, P ROY SOC B-BIOL SCI, V271, P733, DOI 10.1098/rspb.2003.2654; Vardi A, 2002, CURR BIOL, V12, P1767, DOI 10.1016/S0960-9822(02)01217-4; von Elert E, 1997, LIMNOL OCEANOGR, V42, P1796, DOI 10.4319/lo.1997.42.8.1796; Wolfe GV, 2000, BIOL BULL-US, V198, P225, DOI 10.2307/1542526	65	118	129	3	38	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	JUN	2007	29	6					527	543		10.1093/plankt/fbm034	http://dx.doi.org/10.1093/plankt/fbm034			17	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	186MH		Bronze			2025-03-11	WOS:000247782300005
J	Willman, S; Moczydlowska, M				Willman, Sebastian; Moczydlowska, Malgorzata			Wall ultrastructure of an Ediacaran acritarch from the Officer Basin, Australia	LETHAIA			English	Article						acritarchs; Australia; Ediacaran; neoproterozoic; Officer Basin; phytoplankton; protists; TEM; wall ultrastructure	RESISTANT BIO-POLYMER; CELL-WALL; OUTER WALLS; BIOLOGICAL AFFINITIES; BOTRYOCOCCUS-BRAUNII; CHLOROPHYTA; CHLOROCOCCALES; SPECTROSCOPY; MICROALGAE; MICROSCOPY	Well-preserved organic-walled microfossils referred to as acritarchs occur abundantly in Ediacaran deposits in the Officer Basin in Australia. The assemblages are taxonomically diverse, change over short stratigraphical intervals and are largely facies independent across marine basins. Affinities of this informal group of fossils to modern biota are poorly recognized or unknown, with the exception of only a few taxa. Morphological studies by use of transmitted light microscopy, geochemical analyses and other lines of evidence, suggest that some Precambrian acritarchs are related to algae (including prasinophytes, chlorophytes, and perhaps also dinoflagellates). Limitations in magnification and resolution using transmitted light microscopy may be relevant when assessing relationships to modern taxa. Scanning electron microscopy reveals details of morphology, microstructure and wall surface microelements, whereas transmission electron microscopy provides high-resolution images of the cell wall ultrastructure. In the light of previous ultrastructural studies it can be concluded that the division of acritarchs into leiospheres (unornamented) and acanthomorphs (ornamented) is entirely artificial and has no phylogenetic meaning. Examination of Gyalosphaeridium pulchrum using transmission electron microscopy reveals a vesicle wall with four distinct layers. This multilayered wall ultrastructure is broadly shared by a range of morphologically diverse acritarchs as well as some extant microalgae. The chemically resistant biopolymers forming the comparatively thick cell, together with the overall morphology support the interpretation of the microfossil as being in the resting stage in the life cycle. The set of features, morphological and ultrastructural, suggests closer relationship to green algae than dinoflagellates.	Uppsala Univ, Dept Earth Sci, SE-75236 Uppsala, Sweden	Uppsala University	Willman, S (通讯作者)，Uppsala Univ, Dept Earth Sci, Villavagen 16, SE-75236 Uppsala, Sweden.	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J	Mudie, PJ; Marret, F; Aksu, AE; Hiscott, RN; Gillespie, H				Mudie, P. J.; Marret, F.; Aksu, A. E.; Hiscott, R. N.; Gillespie, H.			Palynological evidence for climatic change, anthropogenic activity and outflow of Black Sea water during late Pleistocene and Holocene: Centennial- to decadal-scale records from the Black and Marmara Seas	QUATERNARY INTERNATIONAL			English	Article							LATE QUATERNARY CORES; DINOFLAGELLATE CYSTS; ENVIRONMENTAL-CHANGES; AEGEAN SEA; SEDIMENTS; POLLEN; ASSEMBLAGES; RATIOS; IMPACT; SOUTH	Previous marine palynology studies of pollen and dinoflagellate cysts (dinocysts) in the Black Sea-Mediterranean corridor were made on short cores, allowing only millennial-century scale reconstruction of past climates. We now describe pollen accumulation rates for 5 cores with eleven C-14 ages over 30,000 years, and new decadal-scale data for a Holocene core with fourteen 14 C ages. Pollen influxes show Pinus-Abies-Quercus forest-steppe and deteriorating climate from 29.8-24 kyr BP, then colder, drier pre- and post-LGM conditions, with Artemisia, Cheno-Ams and Ephedra that lasted through the Bolling interstade. Deciduous oak returns by the Younger Dryas, and rapidly expands, followed by Pistacia by 9.3 kyr BP. Foraminiferal delta O-18 shows 4 degrees C cooler than present late glacial summers and rapid Holocene warming. By 9 BP, influxes from Quercus cerris, Tilia, Fagus, Castanea, Ulmus, shade ferns, aquatics, swamp plants and 6180 indicate warm winters (5 degrees C or more) and year-round precipitation (> 600-1000 mm), not the dry conditions that would be required for Black Sea drawdown. There is mid-Holocene expansion of Carpinus, evergreen Quercus and Pistacia. Walnut, olive and cereal pollen suggest early cultivation attempts, but no sustained farming before 4.5 kyr BP. Dinocyst assemblages show major changes traceable throughout the Corridor. Variability in process length marks low diversity (N = 13) Pleniglacial-early Holocene Spiniferites cruciformis assemblages, suggesting fluctuating salinity like the modern Caspian Sea, with brackish to saline conditions (similar to 5-16 parts per thousand). Distributions of euryhaline cysts Spiniferites mirabilis and Spiniferites bentorii show the Aegean and Marmara Seas were connected by similar to 11 kyr BP and linked to Black Sea by 9.3 kyr BP. There is no palynological evidence of either freshwater (salinity < 3 parts per thousand) for farming on the southwest shelf or of catastrophic marine flooding. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.	Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada; Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Liverpool; Memorial University Newfoundland	Mudie, PJ (通讯作者)，Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada.	pmudie@nrcan.gc.ca; f.marret@liv.ac.uk; aaksu@esd.mun.ca; hiscott@esd.mun.ca; gillespie@esd.mun.ca		Marret-Davies, Fabienne/0000-0003-4244-0437				Abrajano T, 2002, MAR GEOL, V190, P151, DOI 10.1016/S0025-3227(02)00346-8; Aksu AE, 2002, MAR GEOL, V190, P119, DOI 10.1016/S0025-3227(02)00345-6; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; Aksu AE, 1999, MAR GEOL, V153, P303, DOI 10.1016/S0025-3227(98)00077-2; [Anonymous], NOAHS FLOOD NEW SCI; [Anonymous], 2007, Paleopalynology; ATANASSOVA ID, 1995, ENVIRON POLLUT, V87, P17, DOI 10.1016/S0269-7491(99)80003-7; Atanassova J, 2005, HOLOCENE, V15, P576, DOI 10.1191/0959683605hl832rp; BOTTEMA S, 1995, PALEOHISTORIA, V17, P53; BOZILOVA E, 1996, PALAEOECOLOGICAL EVE, P701; Caner H, 2002, MAR GEOL, V190, P35, DOI 10.1016/S0025-3227(02)00341-9; CORDOVA C, 2006, UNPUB QUATERNARY INT; Doonan O., 2004, SINOP LANDSCAPES EXP; DUMAN M, 1994, GEO-MAR LETT, V14, P272, DOI 10.1007/BF01274063; Filipova-Marinova M., 2004, Journal of Environment, Micropaleontology, Microbiology, and Meiobenthology, V1, P135; FILIPOVAMARINOV.M, 2006, BRIT ARCHAEOLOGICAL, V3, P1; FILOPOVAMARINOV.M, 2002, PHYTOLOGIA BALCANICA, V8, P133; FILOPOVAMARINOV.M, 2003, DOBRUDUZA, V21, P279; FLIPOVAMARINOVA M, 2003, PHYTOLOGIA BALCANICA, V9, P275; Hiscott RN, 2002, MAR GEOL, V190, P95, DOI 10.1016/S0025-3227(02)00344-4; HISCOTT RN, 2006, BLACK SEA FLOOD QUES; Hooghiemstra H, 2006, QUATERN INT, V148, P29, DOI 10.1016/j.quaint.2005.11.005; Hopkins Jennifer A., 2002, Palynology, V26, P167, DOI 10.2113/0260167; HSICOTT RN, 2006, QUATERNARY INT   NOV; Jorgensen DG, 2003, GLOBAL PLANET CHANGE, V35, P37, DOI 10.1016/S0921-8181(02)00090-5; KORENEVA EV, 1975, INIT REP DSDP, V42, P951; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Lamb AL, 2006, EARTH-SCI REV, V75, P29, DOI 10.1016/j.earscirev.2005.10.003; Leroy S, 2002, MAR GEOL, V190, P531, DOI 10.1016/S0025-3227(02)00361-4; Leroy SAG, 2006, QUATERN INT, V150, P1, DOI 10.1016/j.quaint.2006.01.003; LEROY SAG, 2004, FIELD C IGCP490 ICSU; Marret F, 2004, REV PALAEOBOT PALYNO, V129, P1, DOI 10.1016/j.revpalbo.2003.10.002; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MARRET F, 2007, IN PRESS QUATERNARY; Marret F., 1993, PALYNOSCIENCES, V2, P267; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; McCarthy FMG, 1998, PALAEOGEOGR PALAEOCL, V138, P187, DOI 10.1016/S0031-0182(97)00135-1; Mudie Peta J., 2006, Transactions of the Royal Society of South Africa, V61, P139; Mudie PJ, 2004, REV PALAEOBOT PALYNO, V128, P143, DOI 10.1016/S0034-6667(03)00117-9; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; Mudie PJ, 2002, MAR GEOL, V190, P233, DOI 10.1016/S0025-3227(02)00349-3; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; RAVAZZI C, 2006, QUATERN INT, V140, P37; Roberts Neil., 1998, HOLOCENE ENV HIST; Ross D.A., 1974, The Black Sea - Geology, Chemistry and Biology, V20, P183; RossignolStrick M, 1995, QUATERNARY SCI REV, V14, P893, DOI 10.1016/0277-3791(95)00070-4; Ryan WBF, 2003, ANNU REV EARTH PL SC, V31, P525, DOI 10.1146/annurev.earth.31.100901.141249; Sorrel P, 2006, PALAEOGEOGR PALAEOCL, V234, P304, DOI 10.1016/j.palaeo.2005.10.012; Traverse A., 1978, Initial Reports of the Deep Sea Drilling Project, V42B, P993; van Zeist W., 1982, PALAEOCLIMATES PALAE, V2, P277; Wall D., 1973, Geoscience Man, V7, P95; WALL D, 1974, BLACK SEA GEOLOGY CH, V20, P354; Wick L, 2003, HOLOCENE, V13, P665, DOI 10.1191/0959683603hl653rp	53	78	81	0	17	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1040-6182	1873-4553		QUATERN INT	Quat. Int.	JUN	2007	167						73	90		10.1016/j.quaint.2006.11.009	http://dx.doi.org/10.1016/j.quaint.2006.11.009			18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	191PF					2025-03-11	WOS:000248142700009
J	Zonneveld, KAF; Susek, E				Zonneveld, Karin A. F.; Susek, Ewa			Effects of temperature, light and salinity on cyst production and morphology of <i>Tuberculodinium vancampoae</i> (the resting cyst of <i>Pyrophacus steinii</i>)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate; cyst; morphology; temperature; salinity; light; culture; Tuberculodinium vancampoae	DINOFLAGELLATE CYST; BALTIC SEA; RECENT SEDIMENTS; LIFE-CYCLE; DINOPHYCEAE; ASSEMBLAGES; ABUNDANCE; MARMARA; DENMARK; MARINE	Cyst forming dinoflagellates are useful in reconstructing past environments. For accuracy it is essential to know how environmental parameters such as salinity, temperature and light influence dinoflagellate cyst production and morphology. Here the effect of variation in these parameters on production and morphology of Tuberculodinium vancampoae (the resting stage of Pyrophacus steinii) is detailed. Encystment of T vancampoae has been observed in all studied culture-experiments although only a few cysts are being formed at the limits of the temperature and salinity ranges (16.5 degrees C, 34.8 degrees C and 20, 45 psu) with highest cyst production at 27 degrees C and 35 psu. Temperature clearly affects cyst morphology; cysts formed in cultures grown at 16.5 degrees C and 34.8 degrees C possess small, flattened processes. These cysts are not completely absent in cultures grown at intermediate temperatures but form only a minor part of the association. In previous studies, salinity has been found to influence the cyst morphology of several dinoflagellate species but this seems not to be the case for T vancampoae. In this study there was no morphological variation related to salinity. High cyst production was observed in cultures grown under moderate to strong illumination but variation in illumination did not lead to morphological change. Our findings correspond to field observations where T. vancampoae has been observed in surface sediments of the sub-tropical to tropical regions characterised by mean sea surface temperatures between 12.7 degrees C and 29.5 degrees C, and sea surface salinities between 16.9 and 36.6 psu. In contrast to previous suggestions, T vancampoae appears to be heterothallic rather than homothallic. (c) 2006 Elsevier B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Zonneveld, KAF (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de						Adl SM, 2005, J EUKARYOT MICROBIOL, V52, P399, DOI 10.1111/j.1550-7408.2005.00053.x; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; Brenner W.W., 2001, BALTICA, V14, P40; Brenner Wolfram, 2002, Meyniana, V54, P17; Brenner WW, 2005, PALAEOGEOGR PALAEOCL, V220, P227, DOI 10.1016/j.palaeo.2004.12.010; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dawson E.Y., 1966, Marine Botany: An Introduction; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Dybkjær K, 2004, PALAEOGEOGR PALAEOCL, V206, P41, DOI 10.1016/j.palaeo.2003.12.021; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Evitt W. 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Palaeobot. Palynology	JUN	2007	145	1-2					77	88		10.1016/j.revpalbo.2006.09.001	http://dx.doi.org/10.1016/j.revpalbo.2006.09.001			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	179LL					2025-03-11	WOS:000247291000004
J	Kim, BH; Park, MH; Hwang, SJ; Han, MS				Kim, Baik-Ho; Park, Myung-Hwan; Hwang, Soon-Jin; Han, Myung-Soo			Excystment patterns of the freshwater dinoflagellate <i>Peridinium bipes</i> (Dinophyceae) in Juam Reservoir, Korea	AQUATIC MICROBIAL ECOLOGY			English	Article						cyst germination; dinoflagellates; environment; freshwater red-tide; Peridinium bipes	ALEXANDRIUM-TAMARENSE DINOPHYCEAE; GONYAULAX-TAMARENSIS; CYST GERMINATION; RESTING CYSTS; RED TIDES; LAKE; TEMPERATURE; ENCYSTMENT; DORMANCY	We examined seasonal variations in vegetative populations and cyst germination of the dinoflagellate Peridinium bipes Stein in reservoir water samples collected from August 2003 to March 2005, a period that included a sudden bloom of this species (September 2003 to March 2004). Monthly variations in cyst abundance and germination were tracked, and the effects of environmental factors (water temperature, pH, light and nutrients) on cyst germination were measured in the laboratory under ambient field conditions. During the bloom period, the cyst abundance of P. bipes in sediment samples fluctuated from 4 to 427 cells g(-1) (wet weight), and did not show season-dependent variation. During the same period, the number of vegetative cells of P. bipes in water samples varied from 0 to 9.79 x 10(2) ml(-1). Laboratory experiments revealed a maximum germination rate at 15.6 degrees C, and effective germination was observed at the naturally occurring pH values of 6 to 8, but not at pH 9. Cysts obtained from samples collected at higher temperatures (over 15 degrees C) germinated more quickly than those seeded at lower temperatures, while cysts collected in fall and early winter had a higher cumulative excystment rate than those collected in spring and summer, suggesting that cysts deposited at higher temperatures may act as a seed population for the winter blooms. These findings collectively indicate that germination of R bipes was mainly affected by water temperature and light intensity, and not nutrient levels and pH, and further show that the bloom of P. bipes observed in Juam Reservoir was likely promoted by the presence of sufficient nutrients, relatively high excystment rates and active growth occurring under low temperature conditions.	Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; Konkuk Univ, Dept Environm Sci, Seoul 143701, South Korea	Hanyang University; Konkuk University	Han, MS (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	hanms@hanyang.ac.kr	Hwang, Sunjin/AAK-7149-2020; Kim, Baik-Ho/D-9356-2011	Hwang, Soon-Jin/0000-0001-7083-5036				Abe T.H., 1981, UNFINISHED MONOGRAPH; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson Donald M., 2000, Protist, V151, P97, DOI 10.1078/1434-4610-00010; [Anonymous], 1992, STANDARD METHODS EXA; BEAKES GW, 1988, CAN J BOT, V66, P1054, DOI 10.1139/b88-151; BINDER BJ, 1986, NATURE, V322, P659, DOI 10.1038/322659a0; BINDER BJ, 1987, J PHYCOL, V23, P99; BURKHOLDER JM, 1995, ARCH PROTISTENKD, V145, P177, DOI 10.1016/S0003-9365(11)80314-3; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Dale B., 1983, P69; ELSTER HJ, 1968, BINNENGEWASSER EINZE; Fryxell G.A., 1983, SURVIVAL STRATEGIES; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; HOLM S, 1979, SCAND J STAT, V6, P65; KEATING KI, 1977, SCIENCE, V196, P885, DOI 10.1126/science.196.4292.885; KIDA K, 1989, Journal of the Faculty of Science Shinshu University, V24, P13; Kim BH, 2005, ARCH HYDROBIOL, V163, P49, DOI 10.1127/0003-9136/2005/0163-0049; KIM BH, 1996, THESIS CHONNAM U; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kishimoto Naoyuki, 2001, Limnology, V2, P101, DOI 10.1007/s102010170005; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Lee Ki-Ho, 2005, Korean Journal of Limnology, V38, P249; Matsuoka K., 1989, P461; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; Park Ho-Dong, 1992, Journal of the Faculty of Science Shinshu University, V27, P87; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Pollingher U., 1975, Verhandlungen Int Verein Theor Angew Limnol, V19, P1370; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; SAKO Y, 1987, B JPN SOC SCI FISH, V53, P473; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; STEIN F, 1883, ORG INFUSIONSTIERE E, V3; Sukenik A, 2002, LIMNOL OCEANOGR, V47, P1656, DOI 10.4319/lo.2002.47.6.1656; UCHIDA A, 1988, NIPPON SUISAN GAKK, V54, P1941; Vardi A, 2002, CURR BIOL, V12, P1767, DOI 10.1016/S0960-9822(02)01217-4; Wu JT, 1998, CURR MICROBIOL, V37, P257; Yacobi YZ, 2003, FRESHWATER BIOL, V48, P1850, DOI 10.1046/j.1365-2427.2003.01135.x	40	6	7	2	16	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055			AQUAT MICROB ECOL	Aquat. Microb. Ecol.	MAY 30	2007	47	3					213	221		10.3354/ame047213	http://dx.doi.org/10.3354/ame047213			9	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	182IW		Bronze			2025-03-11	WOS:000247499300001
J	Strom, SL; Wolfe, GV; Bright, KJ				Strom, Suzanne L.; Wolfe, Gordon V.; Bright, Kelley J.			Responses of marine planktonic protists to amino acids:: feeding inhibition and swimming behavior in the ciliate <i>Favella</i> sp.	AQUATIC MICROBIAL ECOLOGY			English	Article						chemical ecology; signaling; ingestion; swimming behavior; ciliate; dinoflagellate	LIQUID-CHROMATOGRAPHIC DETERMINATION; DISSOLVED FREE; CHEMOSENSORY RESPONSES; CHEMICAL IDENTITY; SEA; DIMETHYLSULFONIOPROPIONATE; CHEMORECEPTION; PHYTOPLANKTON; PARAMECIUM; CHEMOTAXIS	Feeding rates of the tintinnid Favella sp. on the dinoflagellate Heterocapsa triquetra were inhibited by a number of dissolved free amino acids (DFAAs), with inhibition inversely proportional to the size of the amino acid side chain. The most inhibitory compounds (valine, cysteine, proline, alanine, and serine) reduced feeding to < 20 % of the control rate at a concentration of 20 mu M. Inhibition was dose-dependent, with a threshold of ca. 200 nM for proline, and did not depend on ciliate feeding history (well-fed versus starved). Inhibition occurred rapidly (<5 min after exposure) and was partially reversible upon removal of DFAAs. Detailed analysis of swimming did not reveal consistent changes in Favella sp. behavior upon exposure to inhibitory amino acids. In contrast to Favella sp., the heterotrophic dinoflagellate Gyrodinium dominans showed no feeding response to 20 mu M DFAAs, while the tintinnid Coxliella sp. exhibited reduced feeding (to approximately 50 % of control rates) in response to a subset of the amino acids active in Favella sp. Our findings, along with the prevalence of some inhibitory compounds at nM concentrations in natural waters, point to a signaling function for these amino acids. Feeding deterrence in Favella sp. is, however, contrary to the typical attractant or stimulatory role of DFAAs, which has been documented for organisms ranging from bacteria to metazoans. The information content of the signal remains unclear but may be related to detection of prey quality during suspension feeding by Favella sp.	Western Washington Univ, Shannon Point Marine Ctr, Anacortes, WA 98221 USA; Calif State Univ Los Angeles, Dept Biol Sci, Chico, CA 95929 USA	Western Washington University; California State University System; California State University Los Angeles	Strom, SL (通讯作者)，Western Washington Univ, Shannon Point Marine Ctr, 1900 Shannon Point Rd, Anacortes, WA 98221 USA.	stroms@cc.wwu.edu						ANDERSSON A, 1985, MAR ECOL PROG SER, V23, P99, DOI 10.3354/meps023099; BILLEN G, 1980, ESTUAR COAST MAR SCI, V11, P279, DOI 10.1016/S0302-3524(80)80084-3; BIRWE H, 1991, CLIN CHIM ACTA, V199, P33, DOI 10.1016/0009-8981(91)90006-X; Boettcher AA, 1998, BIOL BULL, V194, P132, DOI 10.2307/1543043; BUSKEY EJ, 1988, B MAR SCI, V43, P783; BUSKEY EJ, 1989, J EXP MAR BIOL ECOL, V132, P1, DOI 10.1016/0022-0981(89)90173-1; Carr WES, 1996, BIOL BULL, V190, P149, DOI 10.2307/1542535; CRAWFORD CC, 1974, ECOLOGY, V55, P551, DOI 10.2307/1935146; CRONKITE DL, 1993, J EUKAROYOT MICROBIO, V407, P796; CSONKA LN, 1991, ANNU REV MICROBIOL, V45, P569, DOI 10.1146/annurev.mi.45.100191.003033; 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Microb. Ecol.	MAY 16	2007	47	2					107	121		10.3354/ame047107	http://dx.doi.org/10.3354/ame047107			15	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	176II		Bronze			2025-03-11	WOS:000247077800001
J	Touzet, N; Franco, JM; Raine, R				Touzet, Nicolas; Franco, Jose M.; Raine, Robin			Characterization of nontoxic and toxin-producing strains of <i>Alexandrium minutum</i> (Dinophyceae) in Irish coastal waters	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							PARALYTIC SHELLFISH TOXINS; SP-NOV DINOPHYCEAE; GYMNODINIUM-CATENATUM; CATENELLA DINOPHYCEAE; PHYLOGENETIC ANALYSIS; SPECIES COMPLEX; RIBOSOMAL DNA; DINOFLAGELLATE; TAMARENSE; PHYTOPLANKTON	A comparative analysis of the morphology, toxin composition, and ribosomal DNA (rDNA) sequences was performed on a suite of clonal cultures of the potentially toxic dinoflagellate Alexandrium minutum Halim. These were established from resting cysts or vegetative cells isolated from sediment and water samples taken from the south and west coasts of Ireland. Results revealed that strains were indistinguishable, both morphologically and through the sequencing of the D1-D2 domain of the large subunit and the ITS1-5.8S-ITS2 regions of the rDNA. High-performance liquid chromatography fluorescence detection analysis, however, showed that only strains derived from retentive inlets on the southern Irish coast synthesized paralytic shellfish poisoning (PSP) toxins (GTX2 and GTX3), whereas all strains of A. minutum isolated from the west coast were nontoxic. Toxin analysis of net hauls, taken when A. minutum vegetative cells were in the water column, revealed no PSP toxins in samples from Killary Harbor (western coast), whereas GTX2 and GTX3 were detected in samples from Cork Harbor (southern coast). These results confirm the identity of A. minutum as the most probable causative organism for historical occurrences of contamination of shellfish with PSP toxins in Cork Harbor. Finally, random amplification of polymorphic DNA was carried out to determine the degree of polymorphism among strains. The analysis showed that all toxic strains from Cork Harbor clustered together and that a separate cluster grouped all nontoxic strains from the western coast.	Natl Univ Ireland Univ Coll Galway, Martin Ryan Inst, Galway, Ireland; Inst Espanol Oceanog, Vigo, Spain	Ollscoil na Gaillimhe-University of Galway; Spanish Institute of Oceanography	Touzet, N (通讯作者)，Natl Univ Ireland Univ Coll Galway, Martin Ryan Inst, Galway, Ireland.	nicolas.touzet@nuigalway.ie		touzet, nicolas/0000-0002-8524-9184				Adachi M, 1997, FISHERIES SCI, V63, P701, DOI 10.2331/fishsci.63.701; Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; Anderson DM, 1999, J PHYCOL, V35, P870, DOI 10.1046/j.1529-8817.1999.3540870.x; [Anonymous], HARMFUL ALGAE; BALECH E, 1989, PHYCOLOGIA, V28, P206, DOI 10.2216/i0031-8884-28-2-206.1; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Biegala IC, 2002, J PHYCOL, V38, P404, DOI 10.1046/j.1529-8817.2002.01045.x; Boelens R.G.V., 1999, IRELANDS MARINE COAS; Bolch CJS, 1999, J PHYCOL, V35, P356, DOI 10.1046/j.1529-8817.1999.3520356.x; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; Bornet B, 2005, J PHYCOL, V41, P704, DOI 10.1111/j.1529-8817.2005.00073.x; CAMINOORDAS M, 2004, J PLANKTON RES, V26, P341; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; Chang FH, 1997, TOXICON, V35, P393, DOI 10.1016/S0041-0101(96)00168-7; Dantzer WR, 1997, J APPL MICROBIOL, V83, P464, DOI 10.1046/j.1365-2672.1997.00246.x; FRANCO JM, 1993, CHROMATOGRAPHIA, V35, P613, DOI 10.1007/BF02267925; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Gallacher S, 1997, APPL ENVIRON MICROB, V63, P239, DOI 10.1128/AEM.63.1.239-245.1997; Galluzzi L, 2004, APPL ENVIRON MICROB, V70, P1199, DOI 10.1128/AEM.70.2.1199-1206.2004; Godhe A, 2001, MAR BIOTECHNOL, V3, P152, DOI 10.1007/s101260000052; Guillard R. 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Environ. Microbiol.	MAY	2007	73	10					3333	3342		10.1128/AEM.02161-06	http://dx.doi.org/10.1128/AEM.02161-06			10	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	170RA	17337562	Green Published			2025-03-11	WOS:000246680500026
J	Kobiyama, A; Ikeda, Y; Koike, K; Ogata, T				Kobiyama, Atsushi; Ikeda, Yoshifumi; Koike, Kazuhiko; Ogata, Takehiko			Isolation of a differentially expressed gene in separate mating types of the dinoflagellate <i>Alexandrium tamarense</i>	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Alexandrium tamarense; life cycle; mating type; sexual reproduction; subtractive hybridization	STRIGOSUM-LITTORALE COMPLEX; SEQUENCE TAG ANALYSIS; SACCHAROMYCES-CEREVISIAE; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; CYST FORMATION; CHLAMYDOMONAS-REINHARDTII; FACTOR PHEROMONE; LIFE-CYCLE; IDENTIFICATION	In this study, subtractive PCR was used to isolate a gene that is differentially expressed in the different mating-type cells of Alexandriton tamarense. After three rounds of subtractive PCR using cDNAs synthesized from mRNA of different matingtype cells, amplified PCR products were subcloned into a plasmid vector for construction of subtractive libraries. The dependence on mating type for different levels of accumulated mRNA in randomly selected library clones was confirmed by cDNA membrane array, amplified cDNA Southern blot and RNA dot blot analyses using DIG-labelled probes. One gene, AT4-3, showed a strong and mating-type-specific signal. As a result of sequencing of the complete nucleotide sequence of AT4-3, it was predicted that this gene encodes a protein with 131 amino acid residues. BLAST homology searches of nucleotide and deduced amino acid sequences showed no similarity to any known genes or proteins. The predicted amino acid sequence of AT4-3 has a presumptive N-terminal signal peptide for extracellular secretion, an N-linked glycosylation site and eight cysteine residues in half of the C-terminus. Although the function of this gene is unknown, these results provide the first evidence of intracellular variation between cells of different mating types in dinoflagellates.	Kitasato Univ, Sch Fisheries Sci, Ofunato, Iwate 0220101, Japan	Kitasato University	Kobiyama, A (通讯作者)，Kitasato Univ, Sch Fisheries Sci, Ofunato, Iwate 0220101, Japan.	kobiyama@kitasato-u.ac.jp	Koike, Kazuhiko/A-3392-2019					Anderson D.M., 1998, Physiological Ecology of Harmful Algal Blooms; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Armbrust EV, 1999, APPL ENVIRON MICROB, V65, P3121; Bazan JF, 1997, NATURE, V385, P640, DOI 10.1038/385640a0; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; CHURCH GM, 1984, P NATL ACAD SCI-BIOL, V81, P1991, DOI 10.1073/pnas.81.7.1991; COE JGS, 1994, MOL GEN GENET, V244, P661, DOI 10.1007/BF00282757; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Endo B, 1997, J PLANT RES, V110, P463, DOI 10.1007/BF02506807; Ezer N, 2003, ENDOCRINOLOGY, V144, P975, DOI 10.1210/en.2002-220705; Ferris PJ, 2005, PLANT CELL, V17, P597, DOI 10.1105/tpc.104.028035; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Gast RJ, 2003, BIOL BULL-US, V204, P210, DOI 10.2307/1543561; Gurvitz A, 1997, J BIOL CHEM, V272, P22140, DOI 10.1074/jbc.272.35.22140; Hackett JD, 2005, BMC GENOMICS, V6, DOI 10.1186/1471-2164-6-80; Hoover DM, 2000, J BIOL CHEM, V275, P23187, DOI 10.1074/jbc.M002584200; Hosoi-Tanabe S, 2005, FEMS MICROBIOL LETT, V251, P161, DOI 10.1016/j.femsle.2005.07.046; IWASAKI H, 1961, BIOL BULL-US, V121, P173, DOI 10.2307/1539469; KINOSHITA T, 1992, P NATL ACAD SCI USA, V89, P4693, DOI 10.1073/pnas.89.10.4693; KOZAK M, 1981, NUCLEIC ACIDS RES, V9, P5233, DOI 10.1093/nar/9.20.5233; Kurvari V, 1998, J CELL BIOL, V143, P1971, DOI 10.1083/jcb.143.7.1971; MICELI C, 1989, P NATL ACAD SCI USA, V86, P3016, DOI 10.1073/pnas.86.9.3016; MICHAELIS S, 1988, MOL CELL BIOL, V8, P1309, DOI 10.1128/MCB.8.3.1309; Nishiyama R, 2002, P NATL ACAD SCI USA, V99, P5925, DOI 10.1073/pnas.082120199; NOJIRI T, 1995, PLANT CELL PHYSIOL, V36, P79; Ryang SH, 2002, BIOCHEM BIOPH RES CO, V299, P352, DOI 10.1016/S0006-291X(02)02639-6; SAWAYAMA S, 1993, J PHYCOL, V29, P189, DOI 10.1111/j.0022-3646.1993.00189.x; SAWAYAMA S, 1993, NIPPON SUISAN GAKK, V59, P291; SEKIMOTO H, 1990, PLANTA, V182, P348, DOI 10.1007/BF02411384; Sekimoto H, 1998, PLANT CELL PHYSIOL, V39, P1169, DOI 10.1093/oxfordjournals.pcp.a029317; SINGH A, 1983, NUCLEIC ACIDS RES, V11, P4049, DOI 10.1093/nar/11.12.4049; Skibbe DS, 2006, BIOINFORMATICS, V22, P1863, DOI 10.1093/bioinformatics/btl270; Tanikawa N, 2004, PHOTOCHEM PHOTOBIOL, V80, P31, DOI 10.1562/2004-03-12-RA-110.1; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131	36	6	6	0	8	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0967-0262			EUR J PHYCOL	Eur. J. Phycol.	MAY	2007	42	2					183	190		10.1080/09670260601092364	http://dx.doi.org/10.1080/09670260601092364			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	179CB					2025-03-11	WOS:000247265800006
J	Londeix, L; Benzakour, M; Suc, JP; Turon, JL				Londeix, Laurent; Benzakour, Mohamed; Suc, Jean-Pierre; Turon, Jean-Louis			Messinian palaeoenvironments and hydrology in Sicily (Italy): The dinoflagellate cyst record	GEOBIOS			English	Review						Messinian; Late Tortonian; early Zanclean; sicily; dinoflagellate cysts; palaeoenvironment; palaeohydrology; sea-surface temperature reconstruction	MIOCENE PLIOCENE BOUNDARY; SEA-SURFACE CONDITIONS; TRIPOLI FORMATION; SALINITY CRISIS; MEDITERRANEAN PLIOCENE; ENVIRONMENTAL-CHANGES; UPPERMOST OLIGOCENE; REFERENCE SECTION; STABLE-ISOTOPE; NORTH-ATLANTIC	Hydrological conditions prevailing before, during and after the Messinian salinity crisis in Sicily have been approached using dinoflagellate cyst records. The synthetic sequence considered is based on five classical sections from the Caltanissetta Basin. Our interpretations are based on the recognition of autochthonous, allochthonous and reworked population among the dinocyst assemblages. For the first time, sea-surface temperatures and seasonal salinity contrasts were tentatively reconstructed using a "Mutual Climatic Range Method". Sicilian late Tortonian deposits correspond to marine environment with significant terrestrial inputs favourable to eutrophic dinocyst species. Immediately after the beginning of the Messinian Stage, euryhaline assemblages took place, followed by meso-hyperhaline taxa, within a general trend to shallowing. At the end of the Tripoli diatomitic Formation, environment appears confined, with regular oceanic inflows. Such marine inflows remain persistent during the deposition of the salt Member, witnessing the probable persistence of nearby normal marine sea-surface water conditions in the Mediterranean Sea but with possible reduced hydrological circulation and/or low nutrient component. Such inflows are slightly decreasing up to the top of the Sicilian Upper Evaporites. At the same time, river inputs appear weak during the salt deposition, as the consequence of a rather dry climatic context. As shown by reworking activity, terrestrial inputs increase progressively from the base of the Upper Evaporites. During the Lago Mare period, while climate remains rather dry (absence of freshwater algae inputs, very low amount in trees requiring humid conditions), local deposition environment is confined with mesohaline to hypohaline sea-surface waters, in a context with relatively high seasonal sea-surface salinity contrast (up to 6%o). The very high reworking observed in the Arenazzolo silts. in addition to slightly increasing water depth, led us to consider the presence of a discontinuity between the Lago Mare and the Arenazzolo Frns. We consider the Arenazzolo Formation as a transgressive facies following a deep downcutting period. The Arenazzolo Formation presents a two-step development. The first one, correlative with the presence of a G.etrusca (a species with Paratethyan affinities), corresponds to a relative high-stand sea-level with oceanic influxes, low seasonal sea-surface salinity contrast and probable more humid context, as revealed by the important freshwater algal inputs. During the second step, salinity becomes much more variable, with a clear increase of seasonal sea-surface salinity contrast. a possible slight mean sea-surface temperature increase (only few degrees) and a clear weakening of the river inputs. Taking the proposed 9 Zanclean position of the Arenazzolo Fm. into consideration, we state that mean sea-surface temperature did not change significantly from the base of the Messinian to the earliest Zanclean. At 5.33 Ma, the suddenly achieved flooding restored a fair, deep oceanic environment characterized, at the beginning, by a clear mean sea-surface temperature cooling (up to 6-7 degrees C) and a nutrient depletion, associated with the basins starvation. Sea-surface salinities were normal, with very low seasonal contrast. Hydrodynamics then nutrient supply became then quite normal from c.a. 5.08 Ma. The status of the Sicilian Caltanissetta. Basin as a marginal basin although fastly deepening and the stratigraphical location of the Messinian discontinuity at the base of the Arenazzolo is the scenrio that best matches our dinocyst record. (C) 2007 Elsevier Masson SAS. All rights reserved.	Univ Bordeaux 1, CNRS, UMR 5805, Dept Geol & Oceanog, F-33405 Talence, France; Univ Mohammed 5, Fac Sci, Dept Sci Terre, Rabat, Morocco; Univ Lyon 1, CNRS, UMR 5125, PEPS, F-69622 Villeurbanne, France	Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Mohammed V University in Rabat; Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS)	Londeix, L (通讯作者)，Univ Bordeaux 1, CNRS, UMR 5805, Dept Geol & Oceanog, 1 Ave Fac, F-33405 Talence, France.	l.londeix@epoc.u-bordeauxl.fr						ABIDI N, 1997, THESIS U PIERRE ET M; [Anonymous], NEWSL STRATIGR; [Anonymous], 1980, PALEOBIOLOGY PLANT P; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Atkinson T.C., 1986, P851; BARRIENTOS POO, 1979, BIBLIOTHECA PHYCOLOG, V48, P1; Bellanca A, 2001, SEDIMENT GEOL, V140, P87, DOI 10.1016/S0037-0738(00)00173-1; BENSON RH, 1976, PALAEOGEOGR PALAEOCL, V20, P147, DOI 10.1016/0031-0182(76)90028-6; Benson RH, 1991, PALEOCEANOGRAPHY, V6, P165, DOI 10.1029/90PA00756; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; BERTINI A, 1998, RAPPORT BOTANISK SER, P5; Blanc-Valleron MM, 2002, PALAEOGEOGR PALAEOCL, V185, P255, DOI 10.1016/S0031-0182(02)00302-4; BOISSEAU T, 1990, B CENT RECH EXPL, V14, P541; BRADFORD M R, 1977, Grana, V16, P45; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRINKHUIS H, 1992, THESIS U UTRECHT; BROCQUET P, 1984, REVUE GEOLOGIE DYNAM, V25, P75; Brolsma M.J., 1976, Memorie della Societa Geologica Italiana, V16, P153; BROLSMA MJ, 1978, UTRECHT MICROPALEONT, V17, P10; BUTLER RWH, 1995, GEOL SOC AM BULL, V107, P425, DOI 10.1130/0016-7606(1995)107<0425:TASSIM>2.3.CO;2; Butler RWH, 1999, J GEOL SOC LONDON, V156, P827, DOI 10.1144/gsjgs.156.4.0827; CATALANO R, 1979, SCOGLIERE EVAPORITI, V18, P1; CATALANO R, 1978, MESSINIAN REEFS W CE; Cita M., 1978, Init. 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J	Popescu, SM; Melinte, MC; Suc, JP; Clauzon, G; Quillévéré, F; Süto-Szentai, M				Popescu, Speranta-Maria; Melinte, Mihaela-Carmen; Suc, Jean-Pierre; Clauzon, Georges; Quillevere, Frederic; Suto-Szentai, Maria			Earliest Zanclean age for the Colombacci and uppermost Di Tetto formations of the "Latest Messinian" northern Apennines:: New palaeoenvironmental data from the Maccarone section (Marche province, Italy)	GEOBIOS			English	Article						Zanclean transgression; calcareous nannofossils; marine dinoflagellate cysts; Lago Mare	SALINITY CRISIS; LAGO-MARE; MEDITERRANEAN-SEA; LATE NEOGENE; MARGIN; SEDIMENTS; GULF; PERSPECTIVES; EVAPORITES; CARBONATES	The occurrence of planktonic foraminifers in the latest Messinian deposits (uppermost Di Tetto Formation and Colombacci Formation) of the Marche Province (Apennine foredeep, Italy) has stimulated a debate since the 1970s. An earlier palynological study of the entire Maccarone section revealed a pronounced. and a sudden increasing frequency of saccate pollen grains which indicates more distal conditions, and thus a transgression. At first attributed to tectonic activity, this transgression is now interpreted as representing the Zanclean marine transgression after the discovery of Ceratolithus acutus, the calcareous nannofossil marker of the earliest Zanclean in the Mediterranean Sea. Evidence from marine dinoflagellate cysts and planktonic foraminifers supports this result. The Colombacci Formation and uppermost part of the Di Tetto Formation (i.e. the entire p-ev2 stratigraphic unit) belong to the earliest Zanclean. The so-called Lago Mare no longer has a regional chronostratigraphic sense, and should be understood as the invasion of Paratethyan Organisms via surface waters owing to a connection at high sea-level between the Aegean Sea and the Eastern Paratethys (Dacic Basin). A new robust environmental reconstruction of the northern Apennine foredeep is proposed, which respectively considers the effects of tectonics and Mediterranean eustasy. (C) 2007 Elsevier Masson SAS. All rights reserved.	Univ Lyon 1, CNRS, UMR 515, PEPS, F-69622 Villeurbanne, France; Natl Inst Marine Geol & Geoecol, Bucharest 024053, Romania; Univ Paul Cezanne, CNRS, UMR 6635, CEREGE, F-13545 Aix En Provence 04, France; Nat Hist Collect Komlo, H-7300 Komlo, Hungary	Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Aix-Marseille Universite; Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD)	Popescu, SM (通讯作者)，Univ Lyon 1, CNRS, UMR 515, PEPS, Campus Doua,Batiment Geode, F-69622 Villeurbanne, France.	popescu@univ-lvon1.fr	Mihaela, mihaela/AAF-5894-2021; Quillévéré, Frédéric/C-8317-2012	Popescu, Speranta- Maria/0000-0001-5345-395X; Quillevere, Frederic/0000-0002-6248-0447; Melinte-Dobrinescu, Mihaela Carmen/0000-0003-4716-6844				[Anonymous], MEM SOC GEOL ITAL SC; [Anonymous], MEM SOC GEOL ITAL; Backman Jan, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V154, P83; 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SAVOYE B, 1991, MAR GEOL, V97, P279, DOI 10.1016/0025-3227(91)90121-J; Selli R., 1973, MESSINIAN EVENTS MED, P150; Siesser William G., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V161, P223; Sorrel P, 2006, PALAEOGEOGR PALAEOCL, V234, P304, DOI 10.1016/j.palaeo.2005.10.012; Van Couvering JA, 2000, EPISODES, V23, P179; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962	68	41	42	0	4	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	ISSY-LES-MOULINEAUX	65 RUE CAMILLE DESMOULINS, CS50083, 92442 ISSY-LES-MOULINEAUX, FRANCE	0016-6995	1777-5728		GEOBIOS-LYON	Geobios	MAY-JUN	2007	40	3					359	373		10.1016/j.geobios.2006.11.005	http://dx.doi.org/10.1016/j.geobios.2006.11.005			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	185SI					2025-03-11	WOS:000247730300011
J	Warrington, G				Warrington, G.			Palynomorphs from the Penarth group (Rhaetian, Late triassic) at outcrop in north-west Lincolnshire, England	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article								Palynomorphs have previously been documented from only two sections of the Penarth Group in Lincolnshire, in the Blyborough and Tetney Lock boreholes. These records are now augmented by the first from the group at crop in that county, from temporary exposures near Scotter and between Kettlethorpe and Thorney, north-west Lincolnshire. By comparison with those from the Blyborough and Tetney Lock sections and other records nearby in Yorkshire and Nottinghamshire, an assemblage from near Scotter is considered to be from a level low in the Westbury Formation, and those from a site between Kettlethorpe and Thorney to be from higher levels in the Penarth Group, within the Cotham Member of the Lilstock Formation. The assemblages include spores, pollen and organic-walled microplankton that are indicative of a Rhaetian (late Late Triassic) age. The organic-walled microplankton include acritarchs and dinoflagellate cysts, indicating a marine depositional environment.										[Anonymous], 1938, BRIT RHAETIC FLORA; Balchin D. A, 1970, Q. Jl geol. Soc. Lond., V126, P91; Berridge N. G., 1994, MEMOIR BRIT GEOLOGIC; Berridge N.G., 1999, MEMOIR BRIT GEOLOGIC, V127, P1; BURTON FM, 1867, Q J GEOL SOC LOND, V23, P315; BURTON FM, 1867, 6 M BRIT ASS ADV SCI, P51; Gaunt G.D., 1992, Memoir of the British Geological Survey, Sheets 80 and 89 (England and Wales); GAUNT GD, 1980, REPORT I GEOLOGICAL, P79; GEIGER ME, 1968, PHILOS T R SOC B, V254, P1, DOI 10.1098/rstb.1968.0012; GOZZARD JR, 1975, MINERAL ASSESSMENT R, V17; GOZZARD JR, 1978, MINERAL ASSESSMENT R, V33; Hounslow MW, 2004, PALAEOGEOGR PALAEOCL, V213, P331, DOI 10.1016/j.palaeo.2004.07.018; HOWARD AS, IN PRESS MEMOIR BRIT; JAMES JWC, 1976, MINERAL ASSESSMENT R, V22; Kent P. E., 1968, P174; KENT P. E., 1953, PROC YORKSHIRE GEOL SCO, V29, P117; Kent P. E., 1970, Mercian Geol., V3, P361; Kent P.E., 1980, BRIT REGIONAL GEOLOG; KENT PE, 1943, T LINCOLNSHIRE NATUR, V10, P130; KENT PE, 1970, T LINCOLNSHIRE NATUR, V17, pR1; LEES M, 1946, Q J GEOL SOC LOND, V101, P255; Lott G. K., 1988, P YORKS GEOL SOC, V47, P139, DOI [10.1144/pygs.47.2.139, DOI 10.1144/PYGS.47.2.139]; LOVELL JH, 1976, REPORT I GEOLOGICAL, V19; LOVELL JH, 1977, MINERAL ASSESSMENT R, V29; POWER EA, 1992, SEDIMENT TOXICITY AS, V1, P1; SMITH G, 1973, MEMOIR BRIT GEOLOGIC; SOLLAS IBJ, 1901, Q J GEOL SOC LOND, V57, P307; SWIFT A, 1995, P GEOLOGIST ASSOC, V106, P247, DOI 10.1016/S0016-7878(08)80236-2; SWINNERTON HH, 1949, LINCOLNSHIRE NATURAL; Sykes JH., 1974, Mercian Geologist, V5, P39; Sykes JH., 1977, Mercian Geologist, V6, P197; USSHER WAE, 1890, MEMOIR BRIT GEOLOGIC; USSHER WAE, 1888, MEMOIR BRIT GEOLOGIC; Warrington G., 1981, P61; WARRINGTON G, 1979, PALYNOLOGY REPORT TR; WARRINGTON G, 1978, PALYNOLOGY REPORT RH; WILSON E, 1882, Q J GEOL SOC LOND, V38, P451; WOODWARD HB, 1803, JURASSIC ROCKS BRITI; 1973, SCIENCE, V74	39	2	2	0	3	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0044-0604			P YORKS GEOL SOC	Proc. Yorks. Geol. Soc.	MAY	2007	56		3				209	214		10.1144/pygs.56.3.209	http://dx.doi.org/10.1144/pygs.56.3.209			6	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	182JA					2025-03-11	WOS:000247499700003
J	Tang, YZ; Dobbs, FC				Tang, Ying Zhong; Dobbs, Fred C.			Green autofluorescence in dinoflagellates, diatoms, and other microalgae and its implications for vital staining and morphological studies	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							FLOW-CYTOMETRY; GYMNODINIUM-SANGUINEUM; AMPHIDINIUM-CARTERAE; CHESAPEAKE BAY; AMOEBOPHRYA SP; PHYTOPLANKTON; CYSTS; MAINE; CELLS; GULF	Green autofluorescence (GAF) has been described in the short flagellum of golden and brown algae, the stigma of Euglenophyceae, and cytoplasm of different life stages of dinoflagellates and is considered by some researchers a valuable taxonomic feature for dinoflagellates. In addition, green fluorescence staining has been widely proposed or adopted to measure cell viability (or physiological state) in areas such as apoptosis of phytoplankton, pollutant stresses on algae, metabolic activity of algae, and testing treatment technologies for ships' ballast water. This paper reports our epifluorescence microscopic observations and quantitative spectrometric measurements of GAIT in a broad phylogenetic range of microalgae. Our results demonstrate GAIT is a common feature of dinoflagellates, diatoms, green algae, cyanobacteria, and raphidophytes, occurs in the cytoplasm and particularly in eyespots, accumulation bodies, spines, and aerotopes, and is caused by molecules other than chlorophyll. GAF intensity increased with time after cell death or fixation and with excitation by blue or UV light and was affected by pH. GAF of microalgae may be only of limited value in taxonomy. It can be strong enough to interfere with the results of green fluorescence staining, particularly when stained samples are observed microscopically. GAF is useful, however, for microscopic study of algal morphology, especially to visualize cellular components such as eyespots, nucleus, aerotopes, spines, and chloroplasts. Furthermore, GAF can be used to visualize and enumerate dinoflagellate cysts in marine and estuarine sediments in the context of anticipating and monitoring harmful algal blooms and in tracking potentially harmful dinoflagellates transported in ships' ballast tanks.	Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	Old Dominion University	Tang, YZ (通讯作者)，Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, 4600 Elkhorn Ave, Norfolk, VA 23529 USA.	ytang@odu.edu			PHS HHS [NA04OAR4170146] Funding Source: Medline	PHS HHS(United States Department of Health & Human ServicesUnited States Public Health Service)		Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; BERGLUND DL, 1988, CYTOMETRY, V9, P150, DOI 10.1002/cyto.990090209; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CARPENTER EJ, 1991, MAR BIOL, V108, P145, DOI 10.1007/BF01313482; COATS DW, 1994, J EUKARYOT MICROBIOL, V41, P586, DOI 10.1111/j.1550-7408.1994.tb01520.x; COLEMAN AW, 1988, J PHYCOL, V24, P118; Doblin MA, 1999, J EXP MAR BIOL ECOL, V236, P33, DOI 10.1016/S0022-0981(98)00193-2; DORSEY J, 1989, CYTOMETRY, V10, P622, DOI 10.1002/cyto.990100518; ELBRACHTER M, 1994, REV PALAEOBOT PALYNO, V84, P101, DOI 10.1016/0034-6667(94)90043-4; Franklin DJ, 2004, P ROY SOC B-BIOL SCI, V271, P2099, DOI 10.1098/rspb.2004.2810; Fujita S, 2005, EUR J PHYCOL, V40, P159, DOI 10.1080/09670260500063193; Grégori G, 2001, CYTOMETRY, V44, P247, DOI 10.1002/1097-0320(20010701)44:3<247::AID-CYTO1117>3.0.CO;2-Z; Johnson MD, 2003, LIMNOL OCEANOGR, V48, P238, DOI 10.4319/lo.2003.48.1.0238; Kamiyama T, 2000, MAR ECOL PROG SER, V197, P299, DOI 10.3354/meps197299; KAWAI H, 1988, J PHYCOL, V24, P114; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Lage OM, 2001, CYTOMETRY, V44, P226, DOI 10.1002/1097-0320(20010701)44:3<226::AID-CYTO1115>3.0.CO;2-9; LESSARD EJ, 1986, J PLANKTON RES, V8, P1209, DOI 10.1093/plankt/8.6.1209; Li AS, 1996, AQUAT MICROB ECOL, V10, P139, DOI 10.3354/ame010139; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; Park MG, 2004, J EUKARYOT MICROBIOL, V51, P145, DOI 10.1111/j.1550-7408.2004.tb00539.x; Pouneva Irina, 1997, Bulgarian Journal of Plant Physiology, V23, P67; Salomon PS, 2003, AQUAT MICROB ECOL, V33, P163, DOI 10.3354/ame033163; SHAPIRO LP, 1989, J PHYCOL, V25, P189, DOI 10.1111/j.0022-3646.1989.00189.x; Tang YZ, 2007, J PHYCOL, V43, P65, DOI 10.1111/j.1529-8817.2006.00306.x; Veal DA, 2000, J IMMUNOL METHODS, V243, P191, DOI 10.1016/S0022-1759(00)00234-9; Veldhuis MJW, 1997, J PHYCOL, V33, P527, DOI 10.1111/j.0022-3646.1997.00527.x; Veldhuis MJW, 2001, EUR J PHYCOL, V36, P167, DOI 10.1017/S0967026201003110; Vives-Rego J, 2000, FEMS MICROBIOL REV, V24, P429, DOI 10.1016/S0168-6445(00)00033-4; Yamasaki T, 2001, NDT&E INT, V34, P207, DOI 10.1016/S0963-8695(00)00060-8; Yih W, 2000, J EUKARYOT MICROBIOL, V47, P504, DOI 10.1111/j.1550-7408.2000.tb00082.x	34	80	87	1	79	AMER SOC MICROBIOLOGY	WASHINGTON	1752 N ST NW, WASHINGTON, DC 20036-2904 USA	0099-2240			APPL ENVIRON MICROB	Appl. Environ. Microbiol.	APR	2007	73	7					2306	2313		10.1128/AEM.01741-06	http://dx.doi.org/10.1128/AEM.01741-06			8	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	155KM	17277199	Green Published			2025-03-11	WOS:000245576300033
J	Zhu, YH; He, CQ				Zhu, Youhua; He, Chengquan			Middle Jurassic to Early Cretaceous dinoflagellate assemblage zones in eastern Heilongjiang Province, northeast China	CRETACEOUS RESEARCH			English	Article						dinoflagellate cysts; assemblage zone; Jurassic; Early Cretaceous; Heilongjiang Province; northeast China		A Jurassic-Cretaceous marine dinoflagellate cyst biostratigraphic sequence is established for the first time in eastern Heilongjiang Province, northeast China; based on 20 years of data accumulation. This consists of eight assemblage zones (AZs, including three peak zones), of which four are of Callovian-Valanginian age in the Suibin area and four are of early Cretaceous age in the Jixi Basin (including one that is also present in, and coeval with, deposits of Berriasian-Valanginian age in the Suibin area). They are, in ascending order: 1, the Pareodinia ceratophora-Nannoceratopsis pellucida AZ, Suibin Formation; 2, the Gonyaulacysta jurassica AZ (peak zone) in the lower part of the Dongrong Formation; 3, the Amphorula delicata AZ in the upper part of the Dongrong Formation; 4, the marine Oligosphaeridium pulcherrimum AZ (peak zone) in the uppermost Dongrong Formation, Suibin area; 5, the coeval slightly brackish Vesperopsis didaoensis-Lagenorhytis granorugosa AZ in the Didao Formation, Jixi Basin; 6, the marine Odontochitina operculata-Muderongia tetracantha AZ in the lower part of the Chengzihe Formation; 7, the marine Canningia reticulata AZ in the upper part of the Chengzihe Formation; and 8, the Cribroperidinium? parorthoceras AZ (peak zone) in the lower part of the Muling Formation. (C) 2006 Elsevier Ltd. All rights reserved.	Chinese Acad Sci, Inst Geol & Palaeontol, Nanjing 210008, Peoples R China	Chinese Academy of Sciences	Zhu, YH (通讯作者)，Chinese Acad Sci, Inst Geol & Palaeontol, Nanjing 210008, Peoples R China.	yhzhu@nigpas.ac.cn						[Anonymous], 1996, Palynology: principles and applications; Chen J.-h., 1992, Acta Palaeontologica Sinica, V31, P163; Cheng Jin-Hui, 2001, Acta Palaeontologica Sinica, V40, P127; Futakami Masao, 1995, Journal of the Geological Society of Japan, V101, P79; He Cheng-Quan, 2003, Acta Palaeontologica Sinica, V42, P328; He Cheng-Quan, 1997, Acta Micropalaeontologica Sinica, V14, P21; He Cheng-Quan, 2000, Acta Palaeontologica Sinica, V39, P46; He Cheng-Quan, 1999, Acta Palaeontologica Sinica, V38, P183; Kelly Simon R.A., 1994, Acta Palaeontologica Sinica, V33, P509; Sha JG, 2002, J ASIAN EARTH SCI, V20, P141, DOI 10.1016/S1367-9120(01)00035-9; SUN XK, 1992, ACTA PALAEONTOLOGICA, V31, P188; Wan C., 2000, SELECTED PAPERS PALY, P83; Wang Y. G, 1983, FOSSILS MIDDLE UPPER, P100; WILLIAMS GL, 1985, CAMBRIDGE EARTH SCI, P847; WILLIS S, 1993, S ATL QUART, V92, P1; YU JX, 1982, SHENYANG I GEOLOGY M, V5, P227	16	12	13	0	2	ACADEMIC PRESS LTD ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	APR	2007	28	2					327	332		10.1016/j.cretres.2006.10.001	http://dx.doi.org/10.1016/j.cretres.2006.10.001			6	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	171VE					2025-03-11	WOS:000246762700022
J	Yang, XJ; Li, WB; Batten, DJ				Yang, Xiaoju; Li, Wenben; Batten, David J.			Biostratigraphic and palaeoenvironmental implications of an Early Cretaceous miospore assemblage from the Muling Formation, Jixi Basin, northeast China	CRETACEOUS RESEARCH			English	Article						miospores; Early Cretaceous; Muling Formation; Heilongjiang; China	EASTERN HEILONGJIANG; LONGZHAOGOU; AGE	In the Jixi Basin, eastern Heilongjiang Province, China, the lower part of the Lower Cretaceous succession consists of coal-bearing strata including the Muling Formation, which, in addition to plant megafossils, yields abundant spores and pollen grains and a few dinoflagellate cysts. The spore-pollen assemblage consists of more than 42 species belonging to 34 genera. Most of these are derived from pteridophytes and gymnosperms. The association of Aequitriradites echinatus, Cicatricosisporites australiensis, C. imbricatus, C. mediostriatus, C. undosus, Contignisporites glebulentus, Crybelosporites punctatus, Foranminisporis asymmetricus, Gleicheniidites laetus, Impardecispora purverulenta, Kuylisporites lunaris, Pilosisporites trichopapillosus and Triporoletes singularis suggests that the formation is unlikely to be older than late Hauterivian and younger than Aptian, with emphasis placed on the Barremian-early Aptian. The composition of the dinoflagellate cyst and plant megafossil assemblages is consistent with this determination. Based on palynofloral content, a comparison between the miospores recovered and the spores and pollen produced by extant plant taxa, the associated plant megafossils, and the sedimentary facies that characterize the Muling Formation, it is concluded that the source vegetation was dominated by ferns and that the climate was wet subtropical but seasonally dry. (C) 2007 Elsevier Ltd. All rights reserved.	Chinese Acad Sci, Inst Geol & Palaeontol, Nanjing 210008, Peoples R China; Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England	Chinese Academy of Sciences; University of Manchester	Yang, XJ (通讯作者)，Chinese Acad Sci, Inst Geol & Palaeontol, Nanjing 210008, Peoples R China.	xjyang@nigpas.ac.cn	Xiaoju, Yang/J-4785-2013					AHNERT E, 1925, B GEOLOGICAL SOC CHI, V4, P95; Batten D.J., 1983, NPD B, V2, P35; BATTEN DJ, 1975, P GEOLOGISTS ASS, V85, P435; *BUR GEOL MIN RES, 1997, STRAT LITH HEIL PROV, P198; CHEN GY, 1959, GEOLOGICAL REV, V19, P216; Gu Z, 1962, The Jurassic and Cretaceous of China; He Cheng-Quan, 2000, Acta Palaeontologica Sinica, V39, P46; He Cheng-Quan, 1999, Acta Palaeontologica Sinica, V38, P183; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; JU RH, 1982, CHINESE ACAD GEOLOGI, V5, P1; LI W, 1992, ACTA PALAEONTOL SIN, V31, P178; Oishi Saburo, 1938, JOUR FAC SCI HOKKAIDO IMP UNIV SER 4 GEOL AND MIN, V4, P57; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Pu R. G., 1982, B SHENYANG I GEOL MI, V5, P383; Sha J.G., 2000, P 3 NAT STRAT C CHIN, P265; SHA JG, 1994, NEWSL STRATIGR, V31, P101; Sha JG, 2002, J ASIAN EARTH SCI, V20, P141, DOI 10.1016/S1367-9120(01)00035-9; SHA JG, 1991, ACTA GEOL SINICA, V4, P376; SHI TM, 1960, ACTA GEOL SINICA, V40, P187; SUN G, 1993, SCI CHINA SER B, V36, P249; Sun G., 1999, COAL GEOLOGY EXPLORA, V27, P1; SUN G, 1997, ACTA PALAEONTOL SIN, V36, P135; Sun Ge, 1996, PALEOBOTANIST, V45, P393; Taylor T.N., 1993, BIOL EVOLUTION FOSSI, DOI 10.2307/1223352; Tyron RM., 1982, Ferns and Allied Plants: With Special Reference to Tropical America; Vakhrameev V.A., 1991, JURASSIC CRETACEOUS; Wan C., 2000, SELECTED PAPERS PALY, P83; WANG HS, 1929, B GEOLOGICAL SURVEY, V13, P25; Working Group of ``Regional Stratigraphic Chart of Heilongjiang Province'', 1979, REG STRAT CHARTS NE; Wu Zhang, 1980, PALEONTOLOGICAL ATLA, P222; [杨小菊 Yang Xiaoju], 2003, [古生物学报, Acta Palaeontologica Sinica], V42, P561; Yang XJ, 2003, CHINESE SCI BULL, V48, P2480; Yang XJ, 2003, CRETACEOUS RES, V24, P653, DOI 10.1016/j.cretres.2003.07.003; Zhang CB, 1965, MEMOIRS NANJING I GE, V4, P163; Zheng S.L., 1982, Bull. Shenyang Inst. Geol. Miner. Resour., V5, P277; ZHOU ZY, 1980, B NANJING I GEOL PAL, V1, P56	36	17	22	0	8	ACADEMIC PRESS LTD ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	APR	2007	28	2					339	347		10.1016/j.cretres.2006.07.008	http://dx.doi.org/10.1016/j.cretres.2006.07.008			9	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	171VE					2025-03-11	WOS:000246762700024
J	Ishikawa, A; Hattori, M; Imai, I				Ishikawa, Akira; Hattori, Mayuko; Imai, Ichiro			Development of the "plankton emergence trap/chamber (PET Chamber)", a new sampling device to collect in situ germinating cells from cysts of microalgae in surface sediments of coastal waters	HARMFUL ALGAE			English	Article						cyst; device; in situ germination; microalgae; plankton emergence trap/chamber	FLAGELLATE HETEROSIGMA-AKASHIWO; SETO INLAND SEA; HIROSHIMA BAY; POPULATION-DYNAMICS; BOTTOM SEDIMENTS; NORTHEAST JAPAN; ONAGAWA BAY; EGGS; RAPHIDOPHYCEAE; ABUNDANCE	A simple device was developed to collect germinating cells from settled cysts of microalgae on the sea bottom. This new device - the plankton emergence trap chamber (PET Chamber) - made of a clear acrylic plastic, consists of a top cylinder and a base plate attached to a bottom cylinder. After plugging the bottom cylinder with sediment collected from in situ sea bottom and filling the top cylinder with filtered seawater, the PET Chamber attached to a platform specially made for submerging the chambers is placed on the seafloor. An adequate area of the lateral side of the top cylinder is opened and covered by a plankton net (10 mu m mesh) to allow a water exchange between the inside and outside the cylinder. Thus, the PET Chamber can replicate in situ environments, such as temperature, irradiance and dissolved oxygen. Using the PET Chamber, we have succeeded in collecting germinating cells and estimating the germination flux (cells m(-2) day(-1)) of two dinoflagellates, Alexandrium catenella and Scrippsiella spp., in Ago Bay, Japan. Mircoscopic observations on the samples collected from July to October 2003 revealed fluxes of 124-2022 and 622-3732 cells m(-2) day(-1) in A. catenella and Scrippsiella spp., respectively. The data indicate that the new device can detect variations in the number of germinating cells of dinoflagellates. Its sampling ability, coupled with simplicity in deployment and retrieval procedures, can allow one to monitor the in situ emergence from/on the surface sediments of various organisms, that possess resting stages during their life histories, in various coastal waters. (C) 2006 Elsevier B.V. All rights reserved.	Mie Univ, Fac Bioresources, Tsu, Mie 5148507, Japan; Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Kyoto 6068502, Japan	Mie University; Kyoto University	Ishikawa, A (通讯作者)，Mie Univ, Fac Bioresources, 1577 Kurima Machiya, Tsu, Mie 5148507, Japan.	ishikawa@bio.mie-u.ac.jp						ANDRERSON DM, 1987, OCEANOGR, V32, P340; Dale B., 1983, P69; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Hasle G.R., 1978, PHYTOPLANKTON MANUAL, P88; Imai I, 1999, MAR BIOL, V133, P755, DOI 10.1007/s002270050517; IMAI I, 1987, MAR BIOL, V94, P287, DOI 10.1007/BF00392942; IMAI I, 1988, Bulletin of Plankton Society of Japan, V35, P35; IMAI I, 1993, NIPPON SUISAN GAKK, V59, P1669; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; ISHIKAWA A, 1995, J PLANKTON RES, V17, P647, DOI 10.1093/plankt/17.3.647; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; Kamiyama T, 1996, J PLANKTON RES, V18, P1253, DOI 10.1093/plankt/18.7.1253; KASAHARA S, 1974, MAR BIOL, V26, P167, DOI 10.1007/BF00388886; KIM YO, 1995, AQUAT MICROB ECOL, V9, P149, DOI 10.3354/ame009149; MARCUS NH, 1984, MAR ECOL PROG SER, V15, P47, DOI 10.3354/meps015047; ONBE T, 1985, MAR BIOL, V87, P83, DOI 10.1007/BF00397009; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Yokoyama Hisashi, 1997, Benthos Research, V52, P119	19	12	17	1	13	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	APR	2007	6	3					301	307		10.1016/j.hal.2006.04.005	http://dx.doi.org/10.1016/j.hal.2006.04.005			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	160BZ					2025-03-11	WOS:000245913100001
J	Kamikawa, R; Nagai, S; Hosoi-Tanabe, S; Itakura, S; Yamaguchi, M; Uchida, Y; Baba, T; Sako, Y				Kamikawa, Ryoma; Nagai, Satoshi; Hosoi-Tanabe, Shoko; Itakura, Shigeru; Yamaguchi, Mineo; Uchida, Yoshitaka; Baba, Toshinori; Sako, Yoshihiko			Application of real-time PCR assay for detection and quantification of <i>Alexandrium tamarense</i> and <i>Alexandrium catenella</i> cysts from marine sediments	HARMFUL ALGAE			English	Article						A. tamarense; A. catenella; cyst; dinoflagellate; paralytic shellfish poisoning (PSP); real-time PCR	RESTING CYSTS; GONYAULAX-TAMARENSIS; DINOFLAGELLATE; DINOPHYCEAE; IDENTIFICATION; HYBRIDIZATION; BLOOMS; PROBES	The dinoflagellates Alexandrium tamarense (Lebor) Balech and Alexandrium catenella (Whedon and Kofoid) Balech (Dinophyceae) are believed to be the main species responsible for paralytic shellfish poisoning (PSP) all over the world. It is necessary to identify A. tamarense and A. catenella cysts and to monitor their distribution in sediment in order to minimize the damages caused by PSP to the economy and food quality because cysts are the seed population for blooms caused by motile vegetative cells. In this study, we developed an efficient DNA extraction method from the natural cysts present in marine sediments after they were size fractionated with a plankton net (mesh size of 20-150 mu m). The 10-3000 cysts were added to the sediments collected from the Ariake Sea, and for which the primuline-staining method did not reveal any cysts. DNA was then extracted from each sample, and linear standard curves for A. tamarense and A. catenella cysts were obtained from the correlation between the Ct values by real-time PCR and the log of the initial densities of cysts. We monitored the A. tamarense and A. catenella cyst densities in the environmental samples. This assay was demonstrated to be a powerful tool for the identification, detection, and quantification of the cysts of the toxic dinoflagellates. (C) 2007 Elsevier B.V. All rights reserved.	Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Lab Marine Microbiol, Kyoto 6068502, Japan; Natl Res Inst Fisheries & Environm Isl Sea, Harmful Algal Bloom Div, Hiroshima 7390452, Japan; Kobe Univ, Res Ctr Inland Seas, Environm Biochem Grp, Kobe, Hyogo 6580022, Japan; Yamaguchi Prefectural Fisheries Res Ctr, Inland Sea Res Div, Yamaguchi 7540893, Japan	Kyoto University; Japan Fisheries Research & Education Agency (FRA); Kobe University	Kamikawa, R (通讯作者)，Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Lab Marine Microbiol, Kyoto 6068502, Japan.	kami-88@kais.kyoto-u.ac.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063				Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.x; ADACHI M, 1993, NIPPON SUISAN GAKK, V59, P1171; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Dale B., 1979, P443; FUKUYO Y, 1985, B MAR SCI, V37, P529; Galluzzi L, 2004, APPL ENVIRON MICROB, V70, P1199, DOI 10.1128/AEM.70.2.1199-1206.2004; Godhe Anna, 2002, Harmful Algae, V1, P361, DOI 10.1016/S1568-9883(02)00053-7; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; HALLEGRAEFF GM, 1990, TOXIC MARINE PHYTOPLANKTON, P475; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hosoi-Tanabe S, 2005, MAR BIOTECHNOL, V7, P506, DOI 10.1007/s10126-004-4128-4; Kamikawa R, 2005, FISHERIES SCI, V71, P987, DOI 10.1111/j.1444-2906.2005.01055.x; Matsuoka K., 1989, P461; Sako Y, 2004, J PHYCOL, V40, P598, DOI 10.1111/j.1529-8817.2004.03035.x; SAKO Y, 1995, KAIYO, V27, P628; SCHWINGHAMER P, 1991, LIMNOL OCEANOGR, V36, P588, DOI 10.4319/lo.1991.36.3.0588; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Yamaguchi M, 2002, FISHERIES SCI, V68, P1012, DOI 10.1046/j.1444-2906.2002.00526.x; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Zhou ZH, 1999, NEW PHYTOL, V144, P55, DOI 10.1046/j.1469-8137.1999.00504.x	24	54	58	1	27	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	APR	2007	6	3					413	420		10.1016/j.hal.2006.12.004	http://dx.doi.org/10.1016/j.hal.2006.12.004			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	160BZ					2025-03-11	WOS:000245913100012
J	Dybkjaer, K; Rasmussen, ES				Dybkjaer, Karen; Rasmussen, Erik Skovbjerg			Organic-walled dinoflagellate cyst stratigraphy in an expanded Oligocene-Miocene boundary section in the eastern North Sea Basin (Frida-1 Well, Denmark) and correlation from basinal to marginal areas	JOURNAL OF MICROPALAEONTOLOGY			English	Article						North Sea; Oligocene-Miocene; organic-walled dinoflagellate cysts; sequence stratigraphy; Mi-1 glaciation event	UPPERMOST OLIGOCENE; SEQUENCE STRATIGRAPHY; SUCCESSION; BIOSTRATIGRAPHY; CLIMATE; JYLLAND; HISTORY; MIDDLE; DEPOSITS; BELGIUM	The organic-walled dinoflagellate cyst (dinocyst) assemblages in an unusually thick (>800m) Oligocene-Miocene boundary succession from the eastern North Sea Basin (the Frida-1 Well) were studied. Six successive dinocyst assemblages are described: the Wetzeliella gochtii Assemblage (early Chattian), the Distatodinhan biffii Assemblage (Chattian), the Deflandrea phosphoritica Assemblage (latest Chattian), the Holnotryblium spp. Assemblage (early Aquitanian), the Caligodinium amiculum Assemblage (Aquitanian) and the Cordosphaeridium cantharellus Assemblage (latest Aquitanian to early Burdigalian). The dinocyst assemblages are compared with informal dinocyst zonations proposed for the southern North Sea Basin (Germany, Belgium and the Netherlands). A correlation of the expanded basinal succession in Frida-1 with the marginal marine succession found onshore Jylland, based on the dinocyst stratigraphy combined with well logs and seismic data, is proposed. This correlation confirms earlier proposed datings of the onshore deposits and the presence of several hiati. Furthermore, the correlation made it possible to subdivide the succession in Frida-1 into the sequences A-C, as defined onshore. The Mi-1 glaciation event and thus the Oligocene Miocene boundary are proposed to correlate to the boundary between sequences A and B.	GEUS, Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland	Dybkjaer, K (通讯作者)，GEUS, Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	kd@geus.dk; esr@geus.dk	Dybkjær, Karen/G-5223-2018					Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; BUCHARDT B, 1978, NATURE, V275, P121, DOI 10.1038/275121a0; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Coccioni R., 1997, Developments in Palaeontology and Stratigraphy, V15, P279; COSTA LI, 1980, 5 INT PAL C CAMBR, P92; DALE B, 1996, PALYNOLOGY PRINCIPLE, P1749; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P263, DOI 10.2307/1485875; Downie C., 1971, Geoscience Man, V3, P29; Dybkjaer K, 2000, B GEOL SOC DENMARK, V47, P87; Dybkjær K, 2004, REV PALAEOBOT PALYNO, V131, P201, DOI 10.1016/j.revpalbo.2004.03.006; Dybkjær K, 2004, PALAEOGEOGR PALAEOCL, V206, P41, DOI 10.1016/j.palaeo.2003.12.021; Flower B.J., 1997, PROC OCEAN DRILL SCI, V154, P451; Friis H, 1998, SEDIMENT GEOL, V117, P221, DOI 10.1016/S0037-0738(98)00013-X; Gerlach E., 1961, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V112, P143; GRADSTEIN FM, 1992, MICROPALEONTOLOGY, V38, P101, DOI 10.2307/1485991; Hansen J.P.V., 2004, GEOLOGICAL SOC MEMOI, V29, P83; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; Heilmann-Clausen C., 1989, Geol. 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Micropalaentol.	APR	2007	26		1				1	17		10.1144/jm.26.1.1	http://dx.doi.org/10.1144/jm.26.1.1			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	173HS		hybrid			2025-03-11	WOS:000246864700001
J	Feist-Burkhardt, S				Feist-Burkhardt, Susanne			Comments on the spelling of 'archaeopyle', the germination aperture in dinoflagellate cysts	JOURNAL OF MICROPALAEONTOLOGY			English	Article									British Museum Nat Hist, Dept Palaeontol, London SW7 5BD, England	British Museum of Natural History	Feist-Burkhardt, S (通讯作者)，British Museum Nat Hist, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.	S.Feist-Burkhardt@nhm.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242				[Anonymous], 1980, Special Papers in Palaeontology; Brown R.W., 1979, COMPOSITION SCI WORD; BUJAK JP, 1983, MODERN FOSSIL PERIDI, V13; Evitt W. R., 1961, Micropaleontology, V7, P385, DOI 10.2307/1484378; Fensome R.A., 1993, Micropaleontology Press Special Paper; Stearn WilliamT., 1983, BOT LATIN HIST GRAMM, V3rd; Williams G.L., 2000, CONTRIBUTION SERIES, V37, P370	7	0	0	1	3	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	APR	2007	26		1				39	40		10.1144/jm.26.1.39	http://dx.doi.org/10.1144/jm.26.1.39			2	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	173HS		hybrid			2025-03-11	WOS:000246864700003
J	Oboh-Ikuenobe, FE; Benson, DG; Scott, RW; Holbrook, JM; Evetts, MJ; Erbacher, J				Oboh-Ikuenobe, Francisca E.; Benson, Don G.; Scott, Robert W.; Holbrook, John M.; Evetts, Mike J.; Erbacher, Jochen			Re-evaluation of the Alblan-Cenomanian boundary in the US Western Interior based on dinoflagellate cysts	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	11th International Palynological Congress	JUL 04-09, 2004	Granada, SPAIN	CIMP		Late Albian; Early Cenomanian; dinollagellate cysts; US Western Interior; graphic correlation	BASIN	The position of the Albian-Cenomanian boundary in the U.S. Western Interior Basin has been the subject of debate because the anunonites and foraminifers that define the boundary are endemic. Traditionally, the boundary, as defined in Europe by planktonic foraminifers and ammonites, is correlated with the last occurrence of the ammonite genus, Neogastroplites [Reeside, J.B., Cobban, W.A., 1960. Studies of the Mowry Shale (Cretaceous) and contemporary formations in the United States and Canada. U.S. Geological Survey Professional Paper 355, 126 pp]. More recently, the boundary was correlated with the first occurrence of Metengonoceras teigenensis [Cobban, W.A., 1951. Colorado shale of central and northwestern Montana and equivalent rocks of Black Hills. American Association of Petroleum Geologists Bulletin 35, 2170-2198]. These ammonites are associated with bentonites, the ages of which have been extrapolated to the type region of France to date the base of the Cenomanian from the Western Interior Basin. However, since cosmopolitan dinoflagellates are common to this region and the European reference sections where the boundary is defined, they can be used to reevaluate the position of the Albian-wCenomanian boundary in the Western Interior Basin. In our study, 224 samples from 29 outcrop sections in Montana, Wyoming, Colorado. Oklahoma and New Mexico were analyzed for dinoflagellate cysts, as well as other palynomorphs, foraminifers, bivalves and ammonites; these fossils were used for graphic correlation. The recovery and preservation of the dinoflagellate cysts varied from poor to good, and diversity varied from low to moderate. Typical Late Albian to Early Cenomanian taxa, including (Ovoidinium verrucosum, Ovoidinium scabrosum and Palaeoltystrichophora infusorioides, dominate the assemblages; however, dinoflagellate ranges in the five sections in which the neogastroplitid zones are defined (Arrow Creek, Ayers Ranch, Belt Butte, Geyser, Teigen) suggest correlation with the uppermost Albian. Dinoflagellate ranges were confirmed in additional Montana, Wyoming and northern Colorado sections by a few diagnostic taxa (Aptea polymorpha, Apteodinium grande, Batioladinium jaegeri. Lixadinium propatulum, Chichaouadinium vestitum), and they were graphically correlated with published European ranges. The result is that the Albian-Cenomanian boundary correlates with the 97 million year old Clay Spur Bentonite. (c) 2006 Elsevier B.V. All rights reserved.	Univ Missouri, Dept Geol Sci & Engn, Rolla, MO 65409 USA; Irf Grp Inc, Fayetteville, TX 78940 USA; Precis Stratig Associates, Cleveland, OK 74020 USA; Univ Tulsa, Cleveland, OK 74020 USA; Univ Texas, Dept Earth & Environm Sci, Arlington, TX 76019 USA; Fed Inst Geosci & Nat Resources, D-30655 Hannover, Germany	University of Missouri System; Missouri University of Science & Technology; University of Tulsa; University of Texas System; University of Texas Arlington	Oboh-Ikuenobe, FE (通讯作者)，Univ Missouri, Dept Geol Sci & Engn, Rolla, MO 65409 USA.	ikuenobe@umr.edu; dbenson308@earthlink.net; rwscott@ix.netcom.com; holbrook@uta.edu; evettmj@concentric.net; j.erbacher@bgr.de	Scott, Robert/A-8742-2011	Erbacher, Jochen/0000-0003-2793-0307; Oboh-Ikuenobe, Francisca/0000-0002-2223-9691				[Anonymous], 9210 GEOL SURV CAN; [Anonymous], 2004, The Mountain Geologist; [Anonymous], 2007, Paleopalynology; Bhattacharya JP, 2001, AAPG BULL, V85, P261; Breton G., 2002, B TRIMESTRIEL SOC GE, V87, P5; BRINKHUIS H, 2004, JURASSIC CRETACEOUS; Carney JL., 1995, SEPM SPECIAL PUBLICA, P23, DOI DOI 10.2110/PEC.95.53.0023; Cobban W.A., 1991, U S Geological Survey Bulletin, pB1; Cobban W.A., 1972, STRATIGRAPHY AMMONIT, P108; Cobban W.A., 1993, EVOLUTION W INTERIOR, V39, P435; COBBAN WA, 1951, AAPG BULL, V35, P2170; COBBAN WA, 1953, 243D US GEOL SURV PR, P45; COBBAN WA, 1984, 1271 US GEOL SURV; COBBAN WA, 1989, US GEOLOGICAL SURVEY, V1787, pL1; COBBAN WA, 1990, 1917B US GEOL SURV B; DOLSON J, 1991, AAPG BULL, V75, P409; EICHER DL, 1960, YALE U B, V15; EICHER DON L., 1965, J PALEONTOL, V39, P875; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Fiet N, 2001, CRETACEOUS RES, V22, P63, DOI 10.1006/cres.2000.0237; Gale AS, 1996, CRETACEOUS RES, V17, P515, DOI 10.1006/cres.1996.0032; Gradstein F., 2004, A Geological Time Scale; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; HOLBROOK JM, 1992, GEOL SOC AM BULL, V104, P802, DOI 10.1130/0016-7606(1992)104<0802:DHOLCS>2.3.CO;2; Kauffman E.G., 1984, JURASSIC CRETACEOUS, V27, P273; Kauffman E.G., 1993, Evolution of the Western Interior Basin, P397; KAUFFMAN EG, 1977, GEOLOGICAL SOC AM ME, V149; KENNEDY WJ, 1988, GEOLOGICAL SOC SPECI, V39; LIPPS JH, 1994, FOSSIL PROKARYOTES P; MAUGHAN EK, 1993, ENERGY MINERAL RESOU, P3; Nichols D. J., 1994, MESOZOIC SYSTEMS ROC, P503; Obradovich J.D., 1993, EVOLUTION W INTERIOR, V39, P379; Obradovich J.D., 1975, Geological Association of Canada Special Paper, V13, P31; Obradovich JD, 2002, P JPN ACAD B-PHYS, V78, P149, DOI 10.2183/pjab.78.149; OBRADOVICH JD, 1996, GEOL SOC AM ANN A, V66; PORTER KW, 1999, MONTANA BUREAU MINES, V307; PORTER KW, 1993, ENERGY MINERAL RESOU, P45; PORTER KW, 1999, GEOLOGICAL MAP LEWIS, V308; PORTER KW, 1997, 6 OUTCROP SECTIONS M, V3; REESIDE JB, 1960, 355 US GEOL SURV PRO; Scott R.W., 2001, New Mexico Geological Society Field Conference Guidebook, V52, P221; Scott R.W., 1998, STRATIGRAPHY PALEOEN, V6, P11; Scott R.W., 1994, Unconformity-related hydrocarbons in sedimentary sequences, P89; Scott R. W., 2000, SEPM SPEC PUBL, V69, P77; SCOTT RW, 2003, SEPM FDN SPECIAL PUB, V1, P277; SHAW AB, 1964, TIME STRATIGRAPHYS; TILLMAN RW, 1994, AM ASS PETR GEOL ANN; VERDIER JP, 1975, REV MICROPALEONTOL, V25, P231; WILLIAMS G D, 1975, P1; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1	52	20	24	0	4	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	2007	144	1-2					77	97		10.1016/j.revpalbo.2005.09.008	http://dx.doi.org/10.1016/j.revpalbo.2005.09.008			21	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	154JC					2025-03-11	WOS:000245502000006
J	Borromei, AM; Quattrocchio, M				Borromei, Ana M.; Quattrocchio, Mirta			Holocene sea-level change inferred from palynological data in the Beagle Channel, southern Tierra del Fuego, Argentina	AMEGHINIANA			English	Article						palynology; paleoenvironment; Holocene transgression; Bahia Lapataia; Beagle Channel; Tierra del Fuego; Argentina	DINOFLAGELLATE CYST ASSEMBLAGES; QUATERNARY; AMERICA; NORWAY	An early-middle Holocene section in Bahia Lapataia (54 degrees 50'S, 68 degrees 34' W), Beagle Channel, Tierra del Fuego, Argentina has been examined taking into account its sporomorphs and organic-walled microplankton. The palynological assemblage suggests nearshore environments. Two relatively higher sea levels were identified by the increased abundance of organic-walled dinoflagellate cysts (Brigantedinium spp., Selenopemphix sp., Operculodinium centrocarpum sensu Wall and Dale, Spiniferites spp.), the acritarch Halodinium sp. and zoomorph remains (test linings of foraminifera and copepod egg-envelopes). The littoral vegetation at the time of the marine incursion was mainly arboreal, as can be seen in the pollen records by significant increase in Nothofagus dombeyi type frequencies, while a forest-steppe vegetational pattern developed regionally. After comparison with another nearby fossil marine terrace, the palynological analysis has demonstrated that these terraces represent the same transgressive-regressive event. The relative altitudinal differences between these terraces in the area may be the result of seismotectonic activity during the Holocene.	Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cientif & Tecn, RA-8000 Bahia Blanca, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Borromei, AM (通讯作者)，Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cientif & Tecn, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	borromei@criba.edu.ar; mquattro@ctiba.edu.ar						ALBERO M, 1987, QUATERNARY S AM ANTA, V5, P59; ANGIOLINI FE, 1984, SEM SIT INV CULT IND, P101; [Anonymous], 1986, INT S SEA LEV CHANG; [Anonymous], 2000, Gottinger Arbeiten Zur Geologie Und Palaontologie; [Anonymous], CLIMATE CENTRAL S AM; Batten D., 1996, Palynology: principles and applications, P1011; BOESSENKOOL KP, 2001, PALEOBOTANY PALYNOLO, V15, P1; BORRELLO AV, 1969, ANALES DIRECCION NAC; BORROMEI A, 1997, 6 C AS BRAS EST CUAT, P317; Borromei A.M., 2001, Revista Espanola de Micropaleontologia, V33, P61; CORONATO A, IN PRESS GEOSUR; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; GORDILLO S, 1993, QUATERNARY SCI REV, V12, P889, DOI 10.1016/0277-3791(93)90027-J; GORDILLO S, 1992, PALAEOGEOGR PALAEOCL, V99, P41, DOI 10.1016/0031-0182(92)90006-Q; Grill S., 2002, Revista Espanola de Micropaleontologia, V34, P145; GRIMM E., 1991, TILIA SOFTWARE; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; HEUSSER CJ, 1989, QUATERNARY RES, V31, P396, DOI 10.1016/0033-5894(89)90047-1; Heusser CJ, 1998, PALAEOGEOGR PALAEOCL, V141, P277, DOI 10.1016/S0031-0182(98)00053-4; HEUSSER L E, 1984, Palynology, V8, P225; ISLA FI, 1989, QUATERNARY SCI REV, V8, P359, DOI 10.1016/0277-3791(89)90036-X; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Moore D.M., 1983, Flora of Tierra del Fuego; Morner N. A., 1991, B IG USP SPECIAL PUB, V8, P133; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; PALS JP, 1980, REV PALAEOBOT PALYNO, V30, P371, DOI 10.1016/0034-6667(80)90020-2; PISANO VE, 1977, AN I PATAGONIA, V8, P121; PORTER SC, 1984, QUATERNARY RES, V22, P59, DOI 10.1016/0033-5894(84)90006-1; Rabassa J, 2000, QUATERN INT, V68, P217, DOI 10.1016/S1040-6182(00)00046-X; RABASSA J, 1989, Q S AM ANTARCT PENIN, V7, P327; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rostami K, 2000, QUATERNARY SCI REV, V19, P1495, DOI 10.1016/S0277-3791(00)00075-5; Stanley E.A., 1966, Marine Geology, V4, P397, DOI DOI 10.1016/0025-3227; STOCKMARR J, 1971, Pollen et Spores, V13, P615; Urien C.M., 1966, 3 JORNADAS GEOLOGICA, V2, P35; van Waveren I.M., 1994, Scripta Geologica, V105, P27	41	25	26	0	3	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	MAR 30	2007	44	1					161	171						11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	180CA					2025-03-11	WOS:000247336300011
J	Radi, T; Pospelova, V; de Vernal, A; Barrie, JV				Radi, Taoufik; Pospelova, Vera; de Vernal, Anne; Barrie, J. Vaughn			Dinoflagellate cysts as indicators of water quality and productivity in British Columbia estuarine environments	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; estuaries; British Columbia; productivity; sea-surface temperature; sea-surface salinity; nutrients	JUAN-DE-FUCA; OCEANIC PRIMARY PRODUCTION; SURFACE SEDIMENTS; VANCOUVER-ISLAND; HYDROGRAPHIC CONDITIONS; SPATIAL-DISTRIBUTION; NUTRIENT SOURCES; EFFINGHAM INLET; YOKOHAMA-PORT; INDIAN-OCEAN	Palynological analyses of 60 surface sediment samples from estuarine environments near Vancouver Island, including the Georgia Strait (GS), the Effingham (EFF) and the Seymour-Belize (SB) Inlets were performed in order to document the distribution of dinoflagellate cyst assemblages and their relationship to hydrographic conditions, productivity and nutrient concentrations. We tested transfer functions using the analogue method, and suggest that dinoflagellate cyst assemblages can be used to reconstruct primary productivity, temperature and salinity. The EFF and SB Inlets are characterized by a dominance of autotrophic taxa, particularly Operculodinium centrocarpum, whereas the Protoperidinoid and gymnodinial heterotrophic taxa such as Quinquecuspis concreta and Brigantedinium spp. dominate the assemblages of the GS. Multivariate analysis shows that this distribution is closely linked to primary productivity, sea-surface temperature (SST) and spring silica concentration. The abundance of autotrophic taxa in the EFF and SB Inlets is associated with high primary productivity and low summer SST, indicating summer upwelling of coastal British Columbia, whereas the heterotrophic taxa that characterizes the GS assemblages are related to low productivity, high summer SST and high silica concentration during spring. Multivariate analysis shows that the most important environmental parameters related to dinocyst distribution in the restricted embayment of the GS, are distance to the shore, distance to Vancouver Harbor, spring sea surface salinity (SSS), spring phosphate concentration and spring productivity. The autotrophic taxa are generally more common in coastal and shallow waters, but Spiniferites ramosus and Pentapharsodinium dalei show an opposite correlation to spring productivity and salinity. P dalei is particularly abundant around Vancouver Harbor, near highly urbanized shores and within the Fraser River plume, where salinity is low and spring productivity and continental runoff are high. S. ramosus shows its highest abundance on the western coast of GS. Protoperidinioid and gymnodinial cysts characterize distal zones within the central and southern GS that are associated with a mixture of brackish waters coming from the Fraser River and deep upwelling waters entering the GS via Juan de Fuca Strait. The relationship between dinoflagellate cyst assemblages and primary productivity in these estuarine systems differs from that in oceanic and outer neritic zones, where the abundance of heterotrophic taxa is commonly associated with upwelling and high productivity. (c) 2006 Elsevier B.V. All rights reserved.	Univ Quebec, Ctr Rech Geochim & Geodynam, UQAM, GEOTOP, Montreal, PQ H3C 3P8, Canada; Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; Geol Survey Canada, Inst Ocean Sci, Sidney, BC V8L 4B2, Canada	University of Quebec; University of Quebec Montreal; University of Victoria; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Radi, T (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam, UQAM, GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	radi.taoufik@courrier.uqam.ca; vpospe@uvic.ca; devernal.anne@uqam.ca; barrie@pgc.nrcan.gc.ca	; de Vernal, Anne/D-5602-2013	Pospelova, Vera/0000-0003-4049-8133; de Vernal, Anne/0000-0001-5656-724X				Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P43, DOI 10.1029/95GB02831; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; BARKER ML, 1974, WATER RESOURCES RELA, V56; Beamish RJ, 1999, CAN J FISH AQUAT SCI, V56, P506, DOI 10.1139/cjfas-56-3-506; BEAMISH RJ, 1993, CAN J FISH AQUAT SCI, V50, P1002, DOI 10.1139/f93-116; Boyer T., 2002, World Ocean Atlas 2001, Volume 2: Salinity, V2; Bricker S.B., 1999, NOAA NATL OCEAN SERV; Conkright M., 2002, NUTRIENTS; Conkright M E., 2002, World ocean database 2001, V1; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A., 1999, CAHIERS GEOTOP, V3; EFRON B, 1983, AM STAT, V37, P36, DOI 10.2307/2685844; EVOY RW, 1993, GEO-MAR LETT, V13, P212, DOI 10.1007/BF01207750; GAINES G, 1986, BIOL DINOFLAGELLATES, P224; Guiot J., 1996, Dendrochronologia, V14, P295; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HARRISON PJ, 1983, CAN J FISH AQUAT SCI, V40, P1064, DOI 10.1139/f83-129; HARRISON PJ, 1948, REV MARINE ENV BIOTA, P138; Hart BS, 1998, J SEDIMENT RES, V68, P556, DOI 10.2110/jsr.68.556; Head MJ, 2002, J MICROPALAEONTOL, V21, P169, DOI 10.1144/jm.21.2.169; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Johannessen SC, 2003, ESTUAR COAST SHELF S, V56, P845, DOI 10.1016/S0272-7714(02)00303-7; Jongman R.H.G., 1995, Data Analysis in Community and Landscape Ecology; KEY BH, 1989, 891 ENV CAN; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; LEBLOND PH, 1983, CAN J FISH AQUAT SCI, V40, P1033, DOI 10.1139/f83-128; LEBLOND PH, 1991, ATMOS OCEAN, V29, P288, DOI 10.1080/07055900.1991.9649406; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; Li M, 2000, ESTUAR COAST SHELF S, V50, P467, DOI 10.1006/ecss.2000.0593; Mackas DL, 1997, ESTUAR COAST SHELF S, V44, P1, DOI 10.1006/ecss.1996.0110; Mackas DL, 2001, CAN J FISH AQUAT SCI, V58, P685, DOI 10.1139/cjfas-58-4-685; Mantua NJ, 1997, B AM METEOROL SOC, V78, P1069, DOI 10.1175/1520-0477(1997)078<1069:APICOW>2.0.CO;2; Marinone SG, 1996, ESTUAR COAST SHELF S, V43, P183, DOI 10.1006/ecss.1996.0064; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Masson D, 2000, J MAR RES, V58, P439, DOI 10.1357/002224000321511106; Masson D, 2006, ATMOS OCEAN, V44, P1, DOI 10.3137/ao.440101; Masson D, 2002, ESTUAR COAST SHELF S, V54, P115, DOI 10.1006/ecss.2001.0833; Matsuoka K, 2000, MICROPALEONTOLOGY, V46, P360; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K., 1987, Bull. 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Micropaleontol.	MAR 16	2007	62	4					269	297		10.1016/j.marmicro.2006.09.002	http://dx.doi.org/10.1016/j.marmicro.2006.09.002			29	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	146YB					2025-03-11	WOS:000244969500004
J	Zonneveld, KAF; Bockelmann, F; Holzwarth, U				Zonneveld, Karin A. F.; Bockelmann, Frank; Holzwarth, Ulrike			Selective preservation of organic-walled dinoflagellate cysts as a tool to quantify past net primary production and bottom water oxygen concentrations	MARINE GEOLOGY			English	Article						dinoflagellate cysts; early diagenesis; organic matter; preservation; oxygen	BENGUELA UPWELLING SYSTEM; DIEL VERTICAL MIGRATION; SHORT-TERM VARIABILITY; SURFACE SEDIMENTS; ATMOSPHERIC CO2; ANCHOR STATION; PHYTOPLANKTON; OCEAN; NORTH; SCRIPPSIELLA	To understand the role of the ocean within the global carbon cycle, detailed information is required on key-processes within the marine carbon cycle; bio-production in the upper ocean, export of the produced material to the deep ocean and the storage of carbon in oceanic sediments. Quantification of these processes requires the separation of signals of net primary production and the rate of organic matter decay as reflected in fossil sediments. This study examines the large differences in degradation rates of organic-walled dinoflagellate cyst species to separate these degradation and productivity signals. For this, accumulation rates of cyst species known to be resistant (R-cysts) or sensitive (S-cysts) to aerobic degradation of 62 sites are compared to mean annual chlorophyll-a, sea-surface temperature, sea-surface salinity, nitrate and phosphate concentrations of the upper waters and deepwater oxygen concentrations. Furthermore, the degradation of sensitive cysts, as expressed by the degradation constant k and reaction time t, has been related to bottom water [O-2]. The studied sediments were taken from the Arabian Sea, north-western African Margin (North Atlantic), western-equatorial Atlantic Ocean/Caraibic, south-western African margin (South Atlantic) and Southern Ocean (Atlantic sector). Significant relationships are observed between (a) accumulation rates of R-cysts and upper water chlorophyll-a concentrations, (b) accumulation rates of S-cysts and bottom water [O-2] and (c) degradation rates of S-cysts (kt) and bottom water [O-2]. Relationships that are extremely weak or are clearly insignificant on all confidence intervals are between (1) S-cyst accumulation rates and chlorophyll-a concentrations, sea-surface temperature (SST), sea-surface salinity (SSS), phosphate concentrations (P) and nitrate concentrations (N), (2) between R-cyst accumulation rates and bottom water [O-2], SST, SSS, P and N, and between (3) kt and water depth. Co-variance is present between the parameters N and P, N, P and chlorophyll-a, oxygen and water depth. Correcting for this co-variance does not influence the significance of the relationship given above. The possible applicability of dinoflagellate cyst degradation to estimate past net primary production and deep ocean ventilation is discussed. (c) 2007 Published by Elsevier B.V.	Fachbereich 5 Geowissensch, D-28334 Bremen, Germany	University of Bremen	Zonneveld, KAF (通讯作者)，Fachbereich 5 Geowissensch, Postfach 330440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de		Bockelmann, Frank-Detlef/0000-0003-4900-6780				ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; [Anonymous], 1987, DATA ANAL COMMUNITY; [Anonymous], CANOCO; Behrenfeld MJ, 2005, GLOBAL BIOGEOCHEM CY, V19, DOI 10.1029/2004GB002299; BOCKELMANN FD, UNPUB QUAT SCI REV; Campbell J, 2002, GLOBAL BIOGEOCHEM CY, V16, DOI 10.1029/2001GB001444; Cao MK, 2005, TELLUS B, V57, P210, DOI 10.1111/j.1600-0889.2005.00146.x; COWIE GL, 1995, GEOCHIM COSMOCHIM AC, V59, P33, DOI 10.1016/0016-7037(94)00329-K; Dale A.L., 1992, DINOFLAGELLATE CONTR, V5, P45; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; de Lange G., 1998, PROC OCEAN DRILL SCI, P573, DOI DOI 10.2973/ODP.PROC.SR.157.143.1998; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; DELEEUW JW, 2006, PLANT ECOL, DOI DOI 10.1007/S11258-005-9027; Derenne S, 2001, SOIL SCI, V166, P833, DOI 10.1097/00010694-200111000-00008; DEVERNAL A, 2001, J QUATERNARY SCI, V126, P681; ELBRACHTER M, 1994, REV PALAEOBOT PALYNO, V84, P101, DOI 10.1016/0034-6667(94)90043-4; Francois R, 1997, NATURE, V389, P929, DOI 10.1038/40073; Franke C, 2004, PHYS EARTH PLANET IN, V147, P285, DOI 10.1016/j.pepi.2004.07.004; Gibson CH, 2000, DYNAM ATMOS OCEANS, V31, P295, DOI 10.1016/S0377-0265(99)00038-X; Gibson CH, 1995, J GEOPHYS RES-OCEANS, V100, P24841, DOI 10.1029/95JC02256; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Guerra-García JM, 2005, ENVIRON POLLUT, V135, P281, DOI 10.1016/j.envpol.2004.10.004; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Hartnett HE, 1998, NATURE, V391, P572, DOI 10.1038/35351; Hedges J.I., 1993, TOPICS GEOBIOLOGY, P237; Hedges JI, 1999, AM J SCI, V299, P529, DOI 10.2475/ajs.299.7-9.529; HEMSLEY AR, 1994, PUBL NERC, V94, P15; Hopkins Jennifer A., 2002, Palynology, V26, P167, DOI 10.2113/0260167; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Ivanochko TS, 2004, QUATERNARY SCI REV, V23, P467, DOI 10.1016/j.quascirev.2003.06.006; IVANOVA EM, 2000, THESIS VU AMSTERDAM, P1; Jorge RMF, 1999, APPL MICROBIOL BIOT, V52, P174; Jorgensen B.B., 2000, MARINE GEOCHEMISTRY, P173, DOI DOI 10.1007/3-540-32144-6_5; Kamykowski D, 1998, J PLANKTON RES, V20, P1781, DOI 10.1093/plankt/20.9.1781; Keil RG, 2004, MAR CHEM, V92, P157, DOI 10.1016/j.marchem.2004.06.024; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kuhlmann H, 2004, MAR GEOL, V207, P209, DOI 10.1016/j.margeo.2004.03.017; LIEBERMAN OS, 1994, J PHYCOL, V30, P964, DOI 10.1111/j.0022-3646.1994.00964.x; LONGHURST A, 1995, J PLANKTON RES, V17, P1245, DOI 10.1093/plankt/17.6.1245; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Marret F., 1993, PALYNOSCIENCES, V2, P267; MATEAR RJ, 2003, GLOB BIOGEOCHEM CYCL, V4; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Mayer LM, 2004, MAR CHEM, V92, P135, DOI 10.1016/j.marchem.2004.06.022; McManus JF, 2004, NATURE, V428, P834, DOI 10.1038/nature02494; MIDDELBURG JJ, 1989, GEOCHIM COSMOCHIM AC, V53, P1577, DOI 10.1016/0016-7037(89)90239-1; MITCHELLINNES BA, 1991, PROG OCEANOGR, V28, P65, DOI 10.1016/0079-6611(91)90021-D; Mollenhauer G., 2002, Univ. 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Geol.	MAR 13	2007	237	3-4					109	126		10.1016/j.margeo.2006.10.023	http://dx.doi.org/10.1016/j.margeo.2006.10.023			18	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	144UX					2025-03-11	WOS:000244822900001
J	Zhu, YH; Qi, YP; Zhang, BG; Yang, HR; He, CQ; Wang, SH; Zhou, W; Zhu, Q; Li, Z				Zhu, Youhua; Qi, Yuping; Zhang, Binggao; Yang, Hengren; He, Chengquan; Wang, Shihu; Zhou, Wen; Zhu, Qiang; Li, Zheng			Revision of the age of the Qom Formation in the Central Iran Basin, Iran	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						the Qom Formation; Eocene; Kashan block; Central Iran Basin; Iran		The Qom Formation in the Central Iran Basin contains not only relatively abundant calcareous nannofossils and a small number of dinoflagellate cysts, but also a number of stratigraphically significant benthonic foraminifers and ostracods. Calcareous nannofossils reported for the first time from this formation include Coccolithus pelagicus, Cyclicargolithus abisectus, C. floridanus, Dictyococcites bisectus, D. scrippsae, Helicosphaera euphratis, Ericsonia fenestratus, Pontosphaera sp., Reticulofenestra dictyoda, R. minuta and Sphenolithus moriformis. Dinoflagellates include Homotryblium plectilum, Hystrichokolpoma rigaudiae, Operculodinium centrocarpum, Palaeocystodinium golzowense, Spiniferites pseudofurcatus and Thalassiphora pelagica. Benthonic foraminifers include Assilina aff. spira, Discocyclina sp., Neodiscocyclina cf. barkeri, Nummulites aff. variolarius, Operculina sp. and Orbitolites sp. Among the ostracods recovered are Alocopocythere dhansariensis, Asymmetricythere samalutensis, Bairdia montiformis, Cytherella jonesiana, Cytheretta virgulata, Cytheridea cf. bundensis, C. cf. scruposa, C. sp., Eopaijenborchella sp., Hermanites cf. grafica, Krithe oryza, K cf. pernoides, Loxoconcha sp., Paracypris sp., Propontocypris zongbuensis, P. sp. and Xestoleberis sp. This assemblage indicates that the Qom Formation is Eocene in age instead of Middle-Late Oligocene to Early Miocene as previously determined. (c) 2006 Elsevier Ltd. All rights reserved.	Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China; Dept Iran Explorat Project Shengli Petr Adm, Dongying 257015, Peoples R China	Chinese Academy of Sciences	Zhu, YH (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China.	yhzhu@nigpas.ac.cn; ypqi@nigpas.ac.cn						BOWN PR, 1998, CALCAREOUS NANNOFOSS, P266; Bramlette M. N., 1967, Tulane Studies in Geology, V5, P93; Bujak J., 1980, PALAEONTOLOGICAL ASS, V24, P1; Bukry D, 1971, Tulane Stud Geol Paleont, V8, P123; Drugg W.S., 1967, Tulane Studies in Geology, V5, P181; HE C-Q, 1990, Acta Micropalaeontologica Sinica, V7, P403; HE CQ, 1991, LATE CRETACEOUS EARL, P8; He Y., 1976, PALAEONTOLOGY, P1; Hottinger L., 1960, Schweizerische Palaeontologische Abhandlungen, V75-76, P1; HUANG BL, 1975, PALAEONTOLOGY, V1, P317; NEALE JW, 1985, PALAEONTOLOGY, V28, P355; Perch-Nielsen K., 1985, P329; Stocklin J., 1991, Report No. 18, P40; STOVER LE, 1996, MESOZOIC TERTIARY DI, P641; WILLIS S, 1993, S ATL QUART, V92, P1; ZHONG SL, 1992, CALCAREOUS NANNOFOSS, P61	16	16	16	0	4	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1367-9120	1878-5786		J ASIAN EARTH SCI	J. Asian Earth Sci.	MAR 1	2007	29	5-6					715	721		10.1016/j.jseaes.2006.04.012	http://dx.doi.org/10.1016/j.jseaes.2006.04.012			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	155GA					2025-03-11	WOS:000245564700011
J	Yu, SY; Berglund, BE				Yu, Shi-Yong; Berglund, Bjorn E.			A dinoflagellate cyst record of Holocene climate and hydrological changes along the southeastern Swedish Baltic coast	QUATERNARY RESEARCH			English	Article						Holocene; Baltic Sea; dinollagellate cysts; littorina transgression; climate changes; North Atlantic storminess	NORTH-ATLANTIC OSCILLATION; SEA-LEVEL; ATMOSPHERIC CIRCULATION; OXYGEN CONCENTRATIONS; SEDIMENT CORE; SCALE; VARIABILITY; HISTORY; OCEAN; YR	A high-resolution, well-dated dinoflagellate cyst record from a lagoon of the southeastern Swedish Baltic Sea reveals climate and hydrological changes during the Holocene. Marine dinoflagellate cysts occurred initially at about 8600 cal yr BP, indicating the onset of the Littorina transgression in the southeastern Swedish lowland associated with global sea level rise, and thus the opening of the Danish straits. Both the species diversity and the total accumulation rates of dinoflagellate cysts continued to increase by 7000 cal yr BP and then decreased progressively. This pattern reveals the first-order change in local sea level as a function of ice-volume-equivalent sea level rise versus isostatic land uplift. Superimposed upon this local sea level trend, well-defined fluctuations of the total accumulation rates of dinoflagellate cysts occurred on quasi] 1000- and 500-yr frequency bands particularly between 7500 and 4000 cal yr BP, when the connection between the Baltic basin and the North Atlantic was broader. A close correlation of the total accumulation rates of dinoflagellate cysts with GISP2 ice core sea-salt ions suggests that fluctuations of Baltic surface conditions during the middle Holocene might have been regulated by quasi-periodic variations of the prevailing southwesterly winds, most likely through a system similar to the dipole oscillation of the modem North Atlantic atmosphere. (c) 2007 University of Washington. All rights reserved.	Univ Minnesota, Large Lakes Observ, Duluth, MN 55812 USA; Lund Univ, Dept Geol Quaternary Sci, GeoBiosphere Sci Ctr, SE-22362 Lund, Sweden	University of Minnesota System; University of Minnesota Duluth; Large Lakes Observatory; Lund University	Yu, SY (通讯作者)，Univ Minnesota, Large Lakes Observ, 2205 E 5th St, Duluth, MN 55812 USA.	syu@d.umn.edu						Andersson HC, 2002, TELLUS A, V54, P76, DOI 10.1034/j.1600-0870.2002.00288.x; Andrén E, 2000, BOREAS, V29, P233; Andrén E, 2000, HOLOCENE, V10, P687, DOI 10.1191/09596830094944; Andrews JT, 2003, EARTH PLANET SC LETT, V210, P453, DOI [10.1016/S0012-821X(03)00139-0, 10.1016/S0012-821X(03)-00139-0]; Andrews JT, 2003, HOLOCENE, V13, P625, DOI 10.1191/0959683603hl651ft; [Anonymous], 2001, Baltica; BERGLUND B E, 1971, Geologiska Foreningens i Stockholm Forhandlingar, V93, P625; Berglund BE, 2005, QUATERN INT, V130, P111, DOI 10.1016/j.quaint.2004.04.036; BJORCK S, 1995, QUATERN INT, V27, P19, DOI 10.1016/1040-6182(94)00057-C; Bond G, 2001, SCIENCE, V294, P2130, DOI 10.1126/science.1065680; 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Wilson P, 2002, SCOT J GEOL, V38, P5, DOI 10.1144/sjg38010005; Winsor P, 2001, CLIM RES, V18, P5, DOI 10.3354/cr018005; Woolf D.K., 2003, GLOBAL ATMOSPHERE OC, V9, P145, DOI DOI 10.1080/10236730310001633803; Yu SY, 2005, HOLOCENE, V15, P278, DOI 10.1191/0959683605hl792rp; Yu SY, 2003, GEOL SOC AM BULL, V115, P1404, DOI 10.1130/B25217.1; Zorita E, 2000, CLIMATE RES, V14, P25, DOI 10.3354/cr014025	76	20	21	0	5	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0033-5894	1096-0287		QUATERNARY RES	Quat. Res.	MAR	2007	67	2					215	224		10.1016/j.yqres.2006.12.004	http://dx.doi.org/10.1016/j.yqres.2006.12.004			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	142AO					2025-03-11	WOS:000244621000004
J	Wright, DA; Dawson, R; Cutler, SJ; Cutler, HG; Orano-Dawson, CE; Graneli, E				Wright, D. A.; Dawson, R.; Cutler, S. J.; Cutler, H. G.; Orano-Dawson, C. E.; Graneli, E.			Naphthoquinones as broad spectrum biocides for treatment of ship's ballast water: Toxicity to phytoplankton and bacteria	WATER RESEARCH			English	Article						ballast water; naphthoquinones; phytoplankton; bacteria; menadione	CYTOTOXICITY	Current UN International Maritime Organization legislation mandates the phased introduction of ballast water treatment technologies capable of complying with rigorous standards related to removal of waterborne organisms. Doubts concerning mechanical treatments at very high ballasting rates have renewed interest in chemical treatment for very large vessels. High removal rates for biota require broad spectrum biocides that are safe to transport and handle and pose no corrosion problems for ships' structure. The current study focuses on the naphthoquinone group of compounds and extends a previously reported set of screening bioassays with an investigation of the toxicity of four naphthoquinones to select protists and prokaryotes, representative of typical ballast water organisms. Vegetative dinoflagellate cysts exposed to 2.0 mg/L of the naphthoquinones juglone, plumbagin, menadione and naphthazarin showed varying degrees of chloroplast destruction, with menadione demonstrating the most potency. Laboratory and mesocosm exposures of various phytoplankton genera to menadione showed toxicity at 1.0 mg/L. Juglone demonstrated the most bactericidal activity as judged by a Deltatox assay (Vibrio fischeri) and by acridine orange counts of natural bacterial populations. (c) 2007 Elsevier Ltd. All rights reserved.	Univ Maryland, Chesapeake Biol Lab, Ctr Environm Sci, Solomons, MD 20688 USA; Mercer Univ, Sch Pharm, Nat Prod Discovery Grp, Atlanta, GA 30341 USA; Maryland Dept Nat Resources, Annapolis, MD 21401 USA; Univ Kalmar, Inst Marine Sci, Kalmar, Sweden	University System of Maryland; University of Maryland Center for Environmental Science; Mercer University; Linnaeus University; University of Kalmar	Wright, DA (通讯作者)，Univ Maryland, Chesapeake Biol Lab, Ctr Environm Sci, Solomons, MD 20688 USA.	wright@cbl.umces.edu	Graneli, Edna/F-5936-2015					HOBBIE JE, 1977, APPL ENVIRON MICROB, V33, P1225, DOI 10.1128/AEM.33.5.1225-1228.1977; KONEMANN H, 1981, TOXICOLOGY, V19, P209, DOI 10.1016/0300-483X(81)90130-X; OBRIEN PJ, 1991, CHEM-BIOL INTERACT, V80, P1, DOI 10.1016/0009-2797(91)90029-7; OLLINGER K, 1991, J BIOL CHEM, V266, P21496; Salmon-Chemin L, 2001, J MED CHEM, V44, P548, DOI 10.1021/jm001079l; Sano LL, 2004, J GREAT LAKES RES, V30, P201, DOI 10.1016/S0380-1330(04)70340-8; WRIGHT DA, 2007, IN PRESS ENV TECHNOL	7	38	43	1	41	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0043-1354			WATER RES	Water Res.	MAR	2007	41	6					1294	1302		10.1016/j.watres.2006.11.051	http://dx.doi.org/10.1016/j.watres.2006.11.051			9	Engineering, Environmental; Environmental Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Water Resources	149UD	17270232				2025-03-11	WOS:000245171400016
J	Vardi, A; Eisenstadt, D; Murik, O; Berman-Frank, I; Zohary, T; Levine, A; Kaplan, A				Vardi, Assaf; Eisenstadt, Doron; Murik, Omer; Berman-Frank, Ilana; Zohary, Tamar; Levine, Alex; Kaplan, Aaron			Synchronization of cell death in a dinoflagellate population is mediated by an excreted thiol protease	ENVIRONMENTAL MICROBIOLOGY			English	Article							PERIDINIUM-GATUNENSE; CYSTEINE PROTEASES; PHYTOPLANKTON; APOPTOSIS; CYANOBACTERIUM; MECHANISMS; RESISTANCE; EVOLUTION; VIRUSES; STRESS	Regulated programmed cell death (PCD) processes have been documented in several phytoplankton species and are hypothesized to play a role in population dynamics. However, the mechanisms leading to the coordinated collapse of phytoplankton blooms are poorly understood. We showed that the collapse of the annual bloom of Peridinium gatunense, an abundant dinoflagellate in Lake Kinneret, Israel, is initiated by CO2 limitation followed by oxidative stress that triggers a PCD-like cascade. We provide evidences that a protease excreted by senescing P. gatunense cells sensitizes younger cells to oxidative stress and may consequently trigger synchronized cell death of the population. Ageing of the P. gatunense cultures was characterized by a remarkable rise in DNA fragmentation and enhanced sensitivity to H2O2. Exposure of logarithmic phase (young) cultures to conditioning media from stationary phase (old) cells sensitized them to H2O2 and led to premature massive cell death. We detected the induction of specific extracellular protease activity, leupeptin-sensitive, in ageing cultures and in lake waters during the succession of the P. gatunense bloom. Partial purification of the conditioned media revealed that this protease activity is responsible for the higher susceptibility of young cells to oxidative stress. Inhibition of the protease activity lowered the sensitivity to oxidative stress, whereas application of papain to logarithmic phase P. gatunense cultures mimicked the effect of the spent media and enhanced cell death. We propose a novel mechanistic framework by which a population of unicellular phytoplankton orchestrates a coordinated response to stress, thereby determine the fate of its individuals.	Hebrew Univ Jerusalem, Dept Plant & Environm Sci, IL-91904 Jerusalem, Israel; Bar Ilan Univ, Fac Life Sci, IL-52900 Ramat Gan, Israel; Israel Oceanog & Limnol Res, Yigal Allon Limnol Lab, IL-14950 Midgal, Israel	Hebrew University of Jerusalem; Bar Ilan University; Israel Oceanographic & Limnological Research Institute	Kaplan, A (通讯作者)，Hebrew Univ Jerusalem, Dept Plant & Environm Sci, IL-91904 Jerusalem, Israel.	aaronka@vms.huji.ac.il	Kaplan, Aaron/GLN-5655-2022; Murik, Omer/O-7894-2019	Berman-Frank, Ilana/0000-0003-3497-1844; Kaplan, Aaron/0000-0002-0815-5731; Vardi, Assaf/0000-0002-7079-0234				Agustí S, 1998, LIMNOL OCEANOGR, V43, P1836; Alster A, 2006, FRESHWATER BIOL, V51, P1219, DOI 10.1111/j.1365-2427.2006.01543.x; Ameisen JC, 1996, SCIENCE, V272, P1278, DOI 10.1126/science.272.5266.1278; AMEISEN JC, 1995, CELL DEATH DIFFER, V2, P285; Beckman KB, 1998, PHYSIOL REV, V78, P547, DOI 10.1152/physrev.1998.78.2.547; Berges JA, 1998, LIMNOL OCEANOGR, V43, P129, DOI 10.4319/lo.1998.43.1.0129; Berman T, 1998, J PLANKTON RES, V20, P709, DOI 10.1093/plankt/20.4.709; Berman-Frank I, 2004, LIMNOL OCEANOGR, V49, P997, DOI 10.4319/lo.2004.49.4.0997; Butow BJ, 1996, PLANT PHYSIOL, V111, P85; Butow BJ, 1997, J PHYCOL, V33, P780, DOI 10.1111/j.0022-3646.1997.00780.x; Chung CC, 2005, APPL ENVIRON MICROB, V71, P8744, DOI 10.1128/AEM.71.12.8744-8751.2005; Coffeen WC, 2004, PLANT CELL, V16, P857, DOI 10.1105/tpc.017947; Falkowski PG, 2004, SCIENCE, V305, P354, DOI 10.1126/science.1095964; Foyer CH, 1997, PHYSIOL PLANTARUM, V100, P241, DOI 10.1034/j.1399-3054.1997.1000205.x; Franklin DJ, 2004, P ROY SOC B-BIOL SCI, V271, P2099, DOI 10.1098/rspb.2004.2810; Fröhlich KU, 2000, FEBS LETT, V473, P6, DOI 10.1016/S0014-5793(00)01474-5; Fuhrman JA, 1999, NATURE, V399, P541, DOI 10.1038/21119; Groover A, 1997, PROTOPLASMA, V196, P197, DOI 10.1007/BF01279568; Krüger J, 2002, SCIENCE, V296, P744, DOI 10.1126/science.1069288; Lee SO, 2000, APPL ENVIRON MICROB, V66, P4334, DOI 10.1128/AEM.66.10.4334-4339.2000; LINDSTROM K, 1984, J PHYCOL, V20, P212, DOI 10.1111/j.0022-3646.1984.00212.x; Madeo F, 2002, MOL CELL, V9, P911, DOI 10.1016/S1097-2765(02)00501-4; Moharikar S, 2006, J PHYCOL, V42, P423, DOI 10.1111/j.1529-8817.2006.00207.x; Nyström T, 2002, CURR OPIN MICROBIOL, V5, P596, DOI 10.1016/S1369-5274(02)00367-3; Otto HH, 1997, CHEM REV, V97, P133, DOI 10.1021/cr950025u; POLLINGHER U, 1991, ARCH HYDROBIOL, V120, P267; Sawada MT, 1997, BIOCHEM BIOPH RES CO, V236, P40, DOI 10.1006/bbrc.1997.6900; Segovia M, 2003, PLANT PHYSIOL, V132, P99, DOI 10.1104/pp.102.017129; Smirnoff N, 1998, CURR OPIN BIOTECH, V9, P214, DOI 10.1016/S0958-1669(98)80118-3; Stoecker DK, 2003, AQUAT MICROB ECOL, V30, P175, DOI 10.3354/ame030175; SUTTLE CA, 1990, NATURE, V347, P467, DOI 10.1038/347467a0; Takai T, 2002, FEBS LETT, V531, P265, DOI 10.1016/S0014-5793(02)03534-2; Tao Y, 2003, PLANT CELL, V15, P317, DOI 10.1105/tpc.007591; Tchernov D, 2004, P NATL ACAD SCI USA, V101, P13531, DOI 10.1073/pnas.0402907101; Uren AG, 2000, MOL CELL, V6, P961, DOI 10.1016/S1097-2765(05)00086-9; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; van der Hoorn RAL, 2004, PLANT PHYSIOL, V135, P1170, DOI 10.1104/pp.104.041467; Vardi A, 2002, CURR BIOL, V12, P1767, DOI 10.1016/S0960-9822(02)01217-4; Vardi A, 2006, PLOS BIOL, V4, P411, DOI 10.1371/journal.pbio.0040060; Vardi A, 1999, CURR BIOL, V9, P1061, DOI 10.1016/S0960-9822(99)80459-X	40	59	73	0	35	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1462-2912	1462-2920		ENVIRON MICROBIOL	Environ. Microbiol.	FEB	2007	9	2					360	369		10.1111/j.1462-2920.2006.01146.x	http://dx.doi.org/10.1111/j.1462-2920.2006.01146.x			10	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	124OF	17222134				2025-03-11	WOS:000243376800008
J	Soma, Y; Tani, Y; Soma, M; Mitake, H; Kurihara, R; Hashomoto, S; Watanabe, T; Nakamura, T				Soma, Yuko; Tani, Yukinori; Soma, Mitsuyuki; Mitake, Hideo; Kurihara, Ryo; Hashomoto, Shinya; Watanabe, Takahiro; Nakamura, Toshio			Sedimentary steryl chlorin esters (SCEs) and other photosynthetic pigments as indicators of paleolimnological change over the last 28,000 years from the Buguldeika saddle of Lake Baikal	JOURNAL OF PALEOLIMNOLOGY			English	Article						Phytoplankton; Lake Baikal; Sediment; Photosynthetic pigments; Steryl chlorin esters; Sterols	SOUTHERN BASIN; STEROLS; MARINE; CORE; BACILLARIOPHYTA; 75-DEGREES-W; 15-DEGREES-S; BACTERIA; MARKERS; SPAIN	Detailed depth profiles of photosynthetic pigments in a sediment core (G-12) collected at the BDP93 site, the Buguldeika saddle, of south Lake Baikal, along with depth profiles of total organic carbon (TOC) and biogenic silica, were studied to elucidate the temporal changes of phytoplankton assemblages in the lake during the past 28 kyr. In addition to the quantification of carotenoids by high-performance liquid chromatography with photodiode-array detection (HPLC-PDA), steryl chlorin esters (SCEs) were analyzed by HPLC-PDA, HPLC-mass spectrometry (LC-MS) and sterols in SCEs by gas chromatography-mass spectrometry (GC-MS) to enrich the taxonomical information on the phytoplankton composition. Allochthonous input of organic matter from the Selenga River resulted in the higher TOC contents in core G-12 than in a previously reported core (G-6) collected at another site from the southern basin. The poorer correlation in core G-12 than in G-6 between TOC and chlorophyll-a-originating pigments, which are indicative of autochthonous production, also indicated a significant allochthonous input at the site. The abundance of lutein among the carotenoids detected, and the good correlation of total chlorophyll a and b shows that green algae represented a significant portion of the phytoplankton, accompanying the diatoms at the G-12 site, after the last glacial period. The presence of cryptomonads and cyanobacteria were confirmed from marker carotenoids in the sediment core. GC-MS analysis of sterols in SCEs detected marker sterols of diatoms, green algae, chrysophytes and dinoflagellates. The depth profiles of the measured indicators gave consistent features for temporal changes in phytoplankton assemblage at the G-12 site of Lake Baikal after the last glacial maximum. Notably, the profile of a chrysophyte-specific sterol in SCEs was consistent with the reported distribution of chrysophyte cysts during the Holocene. The presence of phytoplankton, such as green algae, diatoms and chrysophytes, in Lake Baikal during the late last glacial period was indicated by the analysis of sterols in SCEs. Sedimentary carotenoids and sterols in SCEs were found to give complementary information about phytoplankton composition. These molecular indicators allow us to reconstruct past lake phytoplankton assemblages responding to environmental changes with a time resolution as high as age-depth relationship in sediments attainable at present.	Univ Shizuoka, Inst Environm Sci, Shizuoka 4228526, Japan; Nagoya Univ, Ctr Chronol Res, Chikusa Ku, Nagoya, Aichi 4648602, Japan	University of Shizuoka; Nagoya University	Soma, Y (通讯作者)，Univ Shizuoka, Inst Environm Sci, 52-1 Yada, Shizuoka 4228526, Japan.	yukosoma@s03.itscom.net	Tani, Yukinori/ADC-9546-2022					BARRETT SM, 1995, J PHYCOL, V31, P360, DOI 10.1111/j.0022-3646.1995.00360.x; Bjornland T., 1997, PHYTOPLANKTON PIGMEN, P578; Bradbury J. 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Paleolimn.	FEB	2007	37	2					163	175		10.1007/s10933-006-9011-z	http://dx.doi.org/10.1007/s10933-006-9011-z			13	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	127WQ					2025-03-11	WOS:000243617400001
J	Nagai, S; Lian, C; Yamaguchi, S; Hamaguchi, M; Matsuyama, Y; Itakura, S; Shimada, H; Kaga, S; Yamauchi, H; Sonda, Y; Nishikawa, T; Kim, CH; Hogetsu, T				Nagai, Satoshi; Lian, Chunlan; Yamaguchi, Sanae; Hamaguchi, Masami; Matsuyama, Yukihiko; Itakura, Shigeru; Shimada, Hiroshi; Kaga, Shinnosuke; Yamauchi, Hiroyuki; Sonda, Yoshiko; Nishikawa, Tetsuya; Kim, Chang-Hoon; Hogetsu, Taizo			Microsatellite markers reveal population genetic structure of the toxic dinoflagellate <i>Alexandrium tamarense</i> (Dinophyceae) in Japanese coastal waters	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium tamarense; dinoflagellate; Dinophyceae; gene flow; genetic distance; genetic structure; human-assisted dispersal; microsatellite; paralytic shellfish poisoning; population differentiation	SHIPS BALLAST WATER; SP-NOV DINOPHYCEAE; SIMPLE SEQUENCES; CYST FORMATION; HIROSHIMA-BAY; DIATOM; DNA; DIVERSITY; CATENELLA; DIFFERENTIATION	This is the first report to explore the fine-scale diversity, population genetic structure, and biogeography of a typical planktonic microbe in Japanese and Korean coastal waters and also to try to detect the impact of natural and human-assisted dispersals on the genetic structure and gene flow in a toxic dinoflagellate species. Here we present the genetic analysis of Alexandrium tamarense (Lebour) Balech populations from 10 sites along the Japanese and Korean coasts. We used nine microsatellite loci, which varied widely in number of alleles and gene diversity across populations. The analysis revealed that Nei's genetic distance correlated significantly with geographic distance in pair-wise comparisons, and that there was genetic differentiation in about half of 45 pair-wise populations. These results clearly indicate genetic isolation among populations according to geographic distance and restricted gene flow via natural dispersal through tidal currents among the populations. On the other hand, high P-values in Fisher's combined test were detected in five pair-wise populations, suggesting similar genetic structure and a close genetic relationship between the populations. These findings suggest that the genetic structure of Japanese A. tamarense populations has been disturbed, possibly by human-assisted dispersal, which has resulted in gene flow between geographically separated populations.	Natl Res Inst Fisheries & Environm Inland Sea, Hatsukaichi, Hiroshima 7390452, Japan; Univ Tokyo, Asian Nat Environm Sci Ctr, Tokyo 1880002, Japan; Hokkaido Cent Fisheries Expt Stn, Div Oceanog, Yoichi, Hokkaido 0468555, Japan; Iwate Fisheries Technol Ctr, Kamaishi, Iwate 0260001, Japan; Miyagi Prefecture Fisheries Res & Dev Ctr, Ishinomaki, Miyagi 9862135, Japan; Aichi Fisheries Res Inst, Gamagorishi, Aichi 4430021, Japan; Hyogo Prefectural Technol Ctr Agr Forestry & Fish, Akashi, Hyogo 6740093, Japan; Pukyong Natl Univ, Fisheries Sci & Technol Ctr, Pusan 608737, South Korea; Univ Tokyo, Dept Forest Sci, Grad Sch Agr & Life Sci, Bunkyo Ku, Tokyo 1138657, Japan	Japan Fisheries Research & Education Agency (FRA); University of Tokyo; Pukyong National University; University of Tokyo	Nagai, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Maruishi 2-17-5, Hatsukaichi, Hiroshima 7390452, Japan.	snagai@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Matsuyama, Yukihiko/0000-0002-2775-1723; Nagai, Satoshi/0000-0001-7510-0063				ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; 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Phycol.	FEB	2007	43	1					43	54		10.1111/j.1529-8817.2006.00304.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00304.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	133HP					2025-03-11	WOS:000244004300005
J	Tang, YZ; Dobbs, FC				Tang, Ying Zhong; Dobbs, Fred C.			Green autofluorescence of dinoflagellate cysts can be used instead of primuline staining for cyst visualization and enumeration in sediments	JOURNAL OF PHYCOLOGY			English	Article						dinoflagellate cyst; green autofluorescence; Gymnodinium catenatum; primuline staining; Scrippsiella trochoidea	RESTING CYSTS; ALEXANDRIUM; GULF; DINOPHYCEAE; GERMINATION; ABUNDANCE	Primuline staining is widely used to visualize and enumerate dinoflagellate cysts in marine sediments. In staining cysts of Gymnodinium catenatum H. W. Graham, Scrippsiella trochoidea (F. Stein) A. R. Loebl., and cysts from estuarine sediments, we found their green fluorescence after primuline treatment to be seemingly no different from the green autofluorescence (GAF) inherent in vegetative cells and cysts of dinoflagellates fixed in formaldehyde. Although primuline subsequently proved to enhance green fluorescence of both species quantitatively, we nonetheless recommend taking advantage of dinoflagellates' GAF to detect and count their cysts in sediments. Doing so will reduce the time, chemical consumption, and possible loss of cells involved in the primuline-staining procedure.	Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	Old Dominion University	Tang, YZ (通讯作者)，Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, 5600 Eikhorn Ave, Norfolk, VA 23529 USA.	ytang@odu.edu						Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 2003, MANUAL HARMFUL MARIN, P165; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Doblin MA, 1999, J EXP MAR BIOL ECOL, V236, P33, DOI 10.1016/S0022-0981(98)00193-2; ELBRACHTER M, 1994, REV PALAEOBOT PALYNO, V84, P101, DOI 10.1016/0034-6667(94)90043-4; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Matsuoka K, 2000, TECHNICAL GUIDE MODE, P5; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Yih W, 2000, J EUKARYOT MICROBIOL, V47, P504, DOI 10.1111/j.1550-7408.2000.tb00082.x	15	4	4	3	16	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2007	43	1					65	68		10.1111/j.1529-8817.2006.00306.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00306.x			4	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	133HP					2025-03-11	WOS:000244004300007
J	Wang, ZH; Qi, YZ; Yang, YF				Wang, Zhao-Hui; Qi, Yu-Zao; Yang, Yu-Feng			Cyst formation:: an important mechanism for the termination of <i>Scrippsiella trochoidea</i> (Dinophyceae) bloom	JOURNAL OF PLANKTON RESEARCH			English	Article							NORTHERN BALTIC SEA; SOUTH CHINA SEA; RESTING CYSTS; DINOFLAGELLATE CYSTS; SPRING-BLOOM; POPULATION-DYNAMICS; SURFACE SEDIMENTS; ONAGAWA BAY; DAYA BAY; GERMINATION	A sediment trap study was conducted at Daya Bay, South China Sea, to investigate the relationships between encystment and population dynamics of Scrippsiella trochoidea from December 1999 to January 2001. A dense bloom of S. trochoidea occurred during the study period from August to September 2000, with the maximum cell number of 3.18 x 10(4) cells mL(-1). Two morphotypes of cysts, one with a thick calcareous wall (calcified cyst) and another without the obvious calcareous cover (non-calcified cyst), were observed during this investigation. The morphological and excystment characteristics of these two cyst types were studied as well. Mass encystments of S. trochoidea, with the maximum of 3.05 x 10(5) cysts m(-2) d(-1) for calcified cyst, and 1.54 x 10(7) cysts m(-2) d(-1) for non-calcified cyst, coincided with the maximum abundance of the vegetative cells. Encystment caused the transfer of a total of 2.24-4.49 x 10(8) cells m(-2) vegetative cells from the water column to the sea bottom during the bloom and resulted in a considerable loss of the bloom population. High assemblages of cysts of S. trochoidea were detected in the surface sediments as well. This rich 'seed bed' in the surface sediments caused by the high efficiency of encystment after blooms acting as a benthic reservoir for future vegetative population, together with the short dormant period (15-26 days) and high germination rate (50-90%), may explain the repeated occurrence of S. trochoidea blooms in Daya Bay.	Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China	Chinese Academy of Sciences; Jinan University	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn	Yang, Yufeng/ABS-0346-2022					Adachi R., 1972, Journal Fac Fish prefect Univ Mie, V9, P9; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1998, US LIMNOLOGY OCEANOG, V42, P1009; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; BRACKBURN SI, 1989, J PHYCOL, V25, P577; [曹宇 Cao Yu], 2006, [生态科学, Ecologic Science], V25, P17; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Dale B., 1983, P69; [邓光 Deng Guang], 2004, [武汉植物学研究, Journal of Wuhan Botanical Research], V22, P129; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; Fryxell G.A., 1983, Survival Strategies of the algae, P1; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; HUANG NM, 1999, RAD PROTECTION B, V19, P12; ISHIKAWA A, 1994, MAR BIOL, V119, P39, DOI 10.1007/BF00350104; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; MATSUOKA K, 1995, FOSSILS, V59, P31; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; Park J.S., 1989, P37; Pati AC, 1999, MAR BIOL, V134, P419, DOI 10.1007/s002270050558; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1977, J PHYCOL, V13, P234; Qi YZ, 2004, HYDROBIOLOGIA, V512, P209, DOI 10.1023/B:HYDR.0000020329.06666.8c; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; *SOA, 2004, B OC DIS CHIN; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; Wang ZH, 2004, MAR ECOL-P S Z N I, V25, P289, DOI 10.1111/j.1439-0485.2004.00035.x; Wang ZH, 2006, J MARINE SYST, V62, P85, DOI 10.1016/j.jmarsys.2006.04.008; [徐宁 Xu Ning], 2004, [海洋环境科学, Marine Environmental Science], V23, P36	45	74	89	1	31	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	FEB	2007	29	2					209	218		10.1093/plankt/fbm008	http://dx.doi.org/10.1093/plankt/fbm008			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	152IB					2025-03-11	WOS:000245354200010
J	Garcés, E; Vila, M; Reñé, A; Alonso-Sáez, L; Anglès, S; Lugliè, A; Masó, M; Gasol, JM				Garces, Esther; Vila, Magda; Rene, Albert; Alonso-Saez, Laura; Angles, Silvia; Luglie, Antonella; Maso, Mercedes; Gasol, Josep M.			Natural bacterioplankton assemblage composition during blooms of <i>Alexandrium</i> spp. (Dinophyceae) in NW Mediterranean coastal waters	AQUATIC MICROBIAL ECOLOGY			English	Article						FISH; dinoflagellates; HAB; Alexandrium; Roseobacter; Alteromonas	PARALYTIC SHELLFISH TOXINS; PELAGIC MARINE-BACTERIA; OLIGONUCLEOTIDE PROBES; PHYLOGENETIC DIVERSITY; COMMUNITY COMPOSITION; DINOFLAGELLATE BLOOM; FUNCTIONAL DIVERSITY; POPULATION-DYNAMICS; ALGICIDAL BACTERIA; CYST FORMATION	We characterised the spatial and temporal variation in the bacterioplankton assemblage composition during bloom events of different Alexandrium species (Dinophyceae) in the littoral of the NW Mediterranean Sea by means of catalysed reporter deposition fluorescence in situ hybridisation with oligonucleotide probes (CARD-FISH). We studied several Alexandrium blooms through their seasonal development (at La Fosca beach) or in their spatial variability (in Arenys Harbour and Olbia Bay), and we complemented these observations by describing the composition of the bacterial assemblage associated with cultures of Alexandrium species isolated from the same sites. Our studies on natural bacterioplankton assemblages identified the Bacteroidetes lineage and the Alphaproteobacteria as the dominating components during the studied blooms of Alexandrium. Alphaproteobacteria dominated in the La Fosca and Olbia blooms, while bacteria belonging to the Bacteroidetes were abundant in the development phase of the La Fosca beach bloom and in the winter Arenys bloom. Gammaproteobacteria contributed in low proportions without significant changes through the different bloom phases at La Fosca beach and in Olbia Bay, but were more abundant in Arenys Harbour. While the absolute bacterial abundances in the spatial study of Olbia Bay covaried with the Alexandrium densities, there were no spatial changes in the bacterioplankton assemblage composition. Alteromonas-like organisms were never an important fraction of the assemblage, but Roseobacter dominated Alphaproteobacteria in Arenys Harbour. Furthermore, the bacterioplankton assemblages associated with Alexandrium spp. cultures were very different from the natural bacterial assemblages during blooms of the same species. We conclude that the presence of a given harmful algal bloom species during a bloom will not always necessarily be accompanied by the same bacterial assemblage structure, and studies done with dinoflagellate cultures may only reflect the bacteria capable of growing under laboratory conditions, with little resemblance to what occurs under natural conditions.	CSIC, CMIMA, Inst Ciencies Mar, Dept Biol marina & Oceanog, Barcelona 08003, Spain; IRTA, San Carlos de la Rapita, Spain; Univ Sassari, Dipartimento Bot Ecol Vegetale, I-07100 Sassari, Italy	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); IRTA; University of Sassari	Garcés, E (通讯作者)，CSIC, CMIMA, Inst Ciencies Mar, Dept Biol marina & Oceanog, Pg Maritim Barcelona 37-49, Barcelona 08003, Spain.	esther@icm.csic.es	Alonso-Saez, Laura/M-2744-2014; Garces, Esther/C-5701-2011; Rene, Albert/D-4560-2012; Gasol, Josep M/B-1709-2008; Vila, Magda/B-2447-2014; Luglie, Antonella/M-4321-2015; Angles, Silvia/B-9469-2011	Garces, Esther/0000-0002-2712-501X; Alonso-Saez, Laura/0000-0003-1757-4767; Rene, Albert/0000-0002-0488-3539; Gasol, Josep M/0000-0001-5238-2387; Vila, Magda/0000-0002-6855-841X; Luglie, Antonella/0000-0001-6382-4208; Angles, Silvia/0000-0003-0529-7504				Adachi M, 2003, APPL ENVIRON MICROB, V69, P6560, DOI 10.1128/AEM.69.11.6560-6568.2003; Adachi M, 2002, AQUAT MICROB ECOL, V26, P223, DOI 10.3354/ame026223; Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Alavi M, 2001, ENVIRON MICROBIOL, V3, P380, DOI 10.1046/j.1462-2920.2001.00207.x; ALONSOSAEZ L, 2007, IN PRESS FEMS MICROB; Alverca E, 2002, EUR J PHYCOL, V37, P523, DOI 10.1017/S0967026202003955; AMANN RI, 1990, J BACTERIOL, V172, P762, DOI 10.1128/jb.172.2.762-770.1990; Amaro AM, 2005, J EUKARYOT MICROBIOL, V52, P191, DOI 10.1111/j.1550-7408.2005.00031.x; [Anonymous], 2003, BOCCONEA; [Anonymous], 1995, MANUAL HARMFUL MARIN; BABINCHAK JA, 1998, HARMFUL ALGAE, P410; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Biegala IC, 2002, J PHYCOL, V38, P404, DOI 10.1046/j.1529-8817.2002.01045.x; Böckelmann U, 2000, FEMS MICROBIOL ECOL, V33, P157, DOI 10.1016/S0168-6496(00)00056-8; Brinkmeyer R, 2000, EUR J PHYCOL, V35, P315, DOI 10.1080/09670260010001735921; BUCK JD, 1989, ESTUAR COAST SHELF S, V29, P317, DOI 10.1016/0272-7714(89)90031-0; Castle D, 2004, LIMNOL OCEANOGR-METH, V2, P303, DOI 10.4319/lom.2004.2.303; COLE JJ, 1982, ANNU REV ECOL SYST, V13, P291, DOI 10.1146/annurev.es.13.110182.001451; Córdova JL, 2002, J PLANKTON RES, V24, P1, DOI 10.1093/plankt/24.1.1; Daims H, 1999, SYST APPL MICROBIOL, V22, P434, DOI 10.1016/S0723-2020(99)80053-8; DELONG EF, 1993, LIMNOL OCEANOGR, V38, P924, DOI 10.4319/lo.1993.38.5.0924; Doucette G.J., 1995, P33; Doucette GJ, 1999, J PHYCOL, V35, P1447, DOI 10.1046/j.1529-8817.1999.3561447.x; DOUCETTE GJ, 1998, PHYSL ECOLOGY HARMFU, P29; Doucette Gregory J., 1995, Natural Toxins, V3, P65, DOI 10.1002/nt.2620030202; Duarte CM, 1999, PROG OCEANOGR, V44, P245, DOI 10.1016/S0079-6611(99)00028-2; Eilers H, 2000, APPL ENVIRON MICROB, V66, P4634, DOI 10.1128/AEM.66.11.4634-4640.2000; Eilers H, 2001, APPL ENVIRON MICROB, V67, P5134, DOI 10.1128/AEM.67.11.5134-5142.2001; Fandino LB, 2001, AQUAT MICROB ECOL, V23, P119, DOI 10.3354/ame023119; Fandino LB, 2005, AQUAT MICROB ECOL, V40, P251, DOI 10.3354/ame040251; Ferrier M, 2002, J APPL MICROBIOL, V92, P706, DOI 10.1046/j.1365-2672.2002.01576.x; FRANCA S, 1996, HARMFUL TOXIC ALGAL, P347; Franca Susana, 1995, P45; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKAMI K, 1991, NIPPON SUISAN GAKK, V57, P2321; Gallacher S, 1997, APPL ENVIRON MICROB, V63, P239, DOI 10.1128/AEM.63.1.239-245.1997; Garcés E, 2005, MAR ECOL PROG SER, V301, P67, DOI 10.3354/meps301067; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Gasol JM, 2005, HARMFUL ALGAE, V4, P771, DOI 10.1016/j.hal.2004.12.007; Gasol JM, 2000, FEMS MICROBIOL ECOL, V31, P99, DOI 10.1016/S0168-6496(99)00090-2; Glöckner FO, 1999, APPL ENVIRON MICROB, V65, P3721; Gonzalez JM, 1997, APPL ENVIRON MICROB, V63, P4237; Graneli E.Turner., 2006, ECOLOGY HARMFUL ALGA, V189; Grasshoff K., 1983, Methods of sea-water analysis; Green DH, 2004, FEMS MICROBIOL ECOL, V47, P345, DOI 10.1016/S0168-6496(03)00298-8; Groben R, 2000, MICROBIAL ECOL, V39, P186; Grossart HP, 2005, ENVIRON MICROBIOL, V7, P860, DOI 10.1111/j.1462-2920.2005.00759.x; Guillard R. 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Microb. Ecol.	JAN 19	2007	46	1					55	70		10.3354/ame046055	http://dx.doi.org/10.3354/ame046055			16	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	136AE		Green Submitted, Bronze			2025-03-11	WOS:000244194200005
J	Gedl, P				Gedl, Przemyslaw			EARLY JURASSIC DINOFLAGELLATE CYSTS FROM THE KRAKOW-SILESIA MONOCLINE, SOUTHERN POLAND: A RECORD FROM THE BLANOWICE FORMATION AT MRZYGLOD	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						dinocysts; palynofacies; Lower Jurassic; Poland; biostratigraphy; palaeoenvironment		A 3-m thick section of the Blanowice Formation exposed in an abandoned clay-pit at Mrzyglod (Krakow-Silesia Monocline, southern Poland) yielded rich palynological material. Be sides dominating land-derived phytoclasts and sporomorphs organic-walled dinoflagellate cysts (dinocysts) occur. Presence of Luehndea spinosa allows considering time of deposition of studied deposits as Late Pliensbachian-earliest Toarcian. Quantitative fluctuations of main groups of palynofacies elements suggest variable sedimentological conditions of deposition within the southern part of the Polish epicontinental basin. Dominance of large-sized cuticle remains and lack of dinocysts occurs in sediments deposited in continental conditions. Occurrence of dinocysts and other aquatic palynomorphs takes place in sediments that have originated during marine ingression.	Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl						[Anonymous], 1962, PRACE I GEOLOGICZNEG; [Anonymous], 1980, PALEOBIOLOGY PLANT P; [Anonymous], I GEOLOGICZNY PRACE; Barski Marcin, 2002, Przeglad Geologiczny, V50, P411; DADLEZ R, 1976, GEOLOGY POLAND 2, V1, P199; Dadlez R., 1962, KWARTALNIK GEOLOGICZ, V6, P447; DADLEZ R, 1978, KWARTALNIK GEOLOGICZ, V22, P773; Dadlez R., 1972, KWARTALNIK GEOL, V16, P620; Dadlez R., 2000, Geological map of Poland without Cenozoic deposits, scale 1:1 000 000; DECZKOWSKI Z, 1997, EPICONTINENTAL PERMI, V153; Deczkowski Z., 1962, KWARTALNIK GEOLOGICZ, V6, P50; EVITT WILLIAM R., 1961, MICROPALEONTOLOGY, V7, P305, DOI 10.2307/1484365; FENSOME RA, 1979, GRONLANDS GEOLOGISKE, V132, P1; GEDL P, 2003, TOMY JURAJSKIE S, V1; Gocht H., 1964, Neues Jahrb. Geol. Palaontol. Abh., V119, P113; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; JURKIEWICZOWA I, 1967, I GEOLOGICZNY B, V200, P5; KOPIK J, 1967, I GEOLOGICZNY B, V189, P135; KOPIK J, 1964, I GEOLOGICZNY B, V189, P43; Kopik J., 1967, I GEOLOGICZNY B, V209, P5; Kopik Janusz, 1998, Biuletyn Panstwowego Instytutu Geologicznego, V378, P67; Marcinkiewicz T., 1960, KWARTALNIK GEOLOGICZ, V4, P386; Morgenroth P., 1970, Neues Jb. Geol. Palaont. Abh., V136, P345; MOSSOCZY Z, 1949, PANSTWOWY I GEOLOGIC, V54, P20; Mossoczy Z., 1961, KWARTALNIK GEOLOGICZ, V5, P81; Palliani RB, 1997, B CENT RECH EXPL, V21, P107; PIENKOWSKI G, 1997, EPICONTINENTAL PERMI, V153, P217; Pienkowski G., 2004, Polish Geological Institute Special Papers, V12, P1; Pienkowski G., 1988, PRZEGLAD GEOLOGICZNY, V36, P449; POULSEN NE, 1992, REV PALAEOBOT PALYNO, V75, P33, DOI 10.1016/0034-6667(92)90148-A; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; PRAUSS M, 1989, NEUES JB GEOL PAL, P671; Riding J.B., 1992, P7; Riding J.B., 1982, Journal of Micropalaeontology, V1, P13; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding J.B., 1984, Proceedings of the Yorkshire Geological Society, V45, P109; Riding J.B., 1983, GLOUCESTERSHIRE ENGL, V9, P111; Riding James B., 1991, Palynology, V15, P115; ROGALSKA M, 1976, I GEOLOGICZNY PRACA, V78, P1; ROGALSKA M, 1954, I GEOL WARSZ B, V89, P1; Rozycki S., 1953, I GEOLOGICZNY PRACE, V17, P1; RUTKOWSKI F, 1923, SPRAWOZDANIA PANTWOW, V2, P117; Tyson R.V., 1987, Marine petroleum source rocks, V26, P47, DOI 10.1144/GSL.SP.1987.026.01.03; Wille W., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V164, P74; Wille W., 1979, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V158, P221; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V28, P1; ZNOSKO J, 1959, KWARTALNIK GEOLOGICZ, V3, P501; Znosko J., 1955, I GEOLOGICZNY, V14, P1	48	5	6	0	0	POLISH GEOLOGICAL SOC	KRAKOW	UL. OLEANDRY 2A, KRAKOW, POLAND	0208-9068			ANN SOC GEOL POL	Ann. Soc. Geol. Pol.		2007	77	2					147	159						13	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	365LT					2025-03-11	WOS:000260408800006
J	Laabir, M; Amzil, Z; Lassus, P; Masseret, E; Tapilatu, Y; De Vargas, R; Grzebyk, D				Laabir, Mohamed; Amzil, Zouher; Lassus, Patrick; Masseret, Estelle; Tapilatu, Yosmina; De Vargas, Romain; Grzebyk, Daniel			Viability, growth and toxicity of <i>Alexandrium catenella</i> and <i>Alexandrium minutum</i> (Dinophyceae) following ingestion and gut passage in the oyster <i>Crassostrea gigas</i>	AQUATIC LIVING RESOURCES			English	Article; Proceedings Paper	Conference on New Developments in Coastal Environment Research	JUN 26-28, 2006	IFREMER Ctr Campus, Nantes, FRANCE		IFREMER Ctr Campus	Alexandrium catenella; Alexandrium minutum; cysts; oysters; paralytic shellfish poisoning	POPULATION-DYNAMICS; BIVALVE MOLLUSKS; SURVIVAL; PACIFIC; TOXINS; CYSTS; CELLS	Adult oysters Crassostrea gigas were experimentally fed with Alexandrium catenella and Alexandrium minutum which are responsible for recurrent toxic blooms in French coastal waters. C. gigas produced faeces and pseudofaeces containing intact and viable temporary pellicular cysts of these two Paralytic toxin producing species. When incubated in favourable conditions, these pellicular cysts were able to germinate at high rates (between 74 and 94%) and the resulting vegetative cells divided with growth rates close to the non-ingested cells (control). The toxin profile of the vegetative cells originated from the germinated temporary cysts was analyzed by liquid chromatography/ fluorescence detection. Total toxin content of newly germinated cells was lower than that of cultured cells. Besides, cell contents of C2, B1, B2 and dcGTX3 toxins featured some changes. Our results suggest that the increased spreading of toxic dinoflagellates through the transfer of shellfish from contaminated towards pristine coastal areas cannot be ruled out. We also suggest that pellicular cysts and newly germinated cells could represent a potential way for the transfer of paralytic toxins toward the higher trophic levels.	Univ Montpellier 2, Lab Ecosyst Lagunaires, UMR 5119, CNRS, F-34095 Montpellier, France; IFREMER, Ctr Nantes, Lab Phycotoxines, F-44311 Nantes, France	Centre National de la Recherche Scientifique (CNRS); Universite de Montpellier; Ifremer; Nantes Universite	Laabir, M (通讯作者)，Univ Montpellier 2, Lab Ecosyst Lagunaires, UMR 5119, CNRS, Case 093,Pl Eugene Bataillon, F-34095 Montpellier, France.	laabir@univ-montp2.fr	Tapilatu, Yosmina/O-7296-2018; Grzebyk, Daniel/A-9286-2009	Tapilatu, Yosmina/0000-0002-9310-6175; Masseret, Estelle/0000-0001-6856-8637; Grzebyk, Daniel/0000-0002-1130-7724				Bardouil M, 1996, OCEANOL ACTA, V19, P177; Bauder AG, 2000, J SHELLFISH RES, V19, P321; Béchemin C, 1999, AQUAT MICROB ECOL, V20, P157, DOI 10.3354/ame020157; BRICELJ VM, 1993, DEV MAR BIO, V3, P371; Carriker Melbourne R., 1992, Journal of Shellfish Research, V11, P507; COUGHLAN J, 1969, MAR BIOL, V2, P356, DOI 10.1007/BF00355716; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HARRISON PJ, 1980, J PHYCOL, V16, P28, DOI 10.1111/j.1529-8817.1980.tb00724.x; IMADA N, 2001, HARMFUL ALGAL BLOOMS, P474; Laabir M, 1999, J SHELLFISH RES, V18, P217; Lassus P, 2004, AQUAT LIVING RESOUR, V17, P207, DOI 10.1051/alr:2004012; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; MARASOVIC I, 1993, DEV MAR BIO, V3, P139; Masselin P., 2001, Harmful Algal Blooms, P26; Negri A P., 2001, Harmful Algal Blooms 2000, P210; OSHIMA Y, 1995, J AOAC INT, V78, P528; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; SCARRATT AM, 1993, J SHELLFISH RES, V12, P383; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; SHUMWAY SE, 1987, AQUAT TOXICOL, V10, P9, DOI 10.1016/0166-445X(87)90024-5; Siu GKY, 1997, HYDROBIOLOGIA, V352, P117, DOI 10.1023/A:1003042431985; Springer JJ, 2002, MAR ECOL PROG SER, V245, P1, DOI 10.3354/meps245001; Sullivan JM, 2003, HARMFUL ALGAE, V2, P183, DOI 10.1016/S1568-9883(03)00039-8; van den Bergh JCJM, 2002, MAR POLICY, V26, P59, DOI 10.1016/S0308-597X(01)00032-X	26	42	44	2	40	EDP SCIENCES S A	LES ULIS CEDEX A	17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A, FRANCE	0990-7440			AQUAT LIVING RESOUR	Aquat. Living Resour.	JAN-MAR	2007	20	1					51	57		10.1051/alr:2007015	http://dx.doi.org/10.1051/alr:2007015			7	Fisheries; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	169CS		Green Submitted, Bronze			2025-03-11	WOS:000246570900006
J	Bolli, L; Llaveria, G; Garcés, E; Guadayol, O; van Lenning, K; Peters, F; Berdalet, E				Bolli, L.; Llaveria, G.; Garces, E.; Guadayol, O.; van Lenning, K.; Peters, F.; Berdalet, E.			Modulation of ecdysal cyst and toxin dynamics of two <i>Alexandrium</i> (Dinophyceae) species under small-scale turbulence	BIOGEOSCIENCES			English	Article							POPULATION-GROWTH; NET GROWTH; DINOFLAGELLATE; PLANKTON; PHYTOPLANKTON; ENVIRONMENTS; CATENELLA; COMMUNITY; MODELS; RATES	Some dinoflagellate species have shown different physiological responses to certain turbulent conditions. Here we investigate how two levels of turbulent kinetic energy dissipation rates (epsilon = 0.4 and 27 cm(2) s(-3)) affect the PSP toxins and ecdysal cyst dynamics of two bloom forming species, Alexandrium minutum and A. catenella. The most striking responses were observed at the high epsilon generated by an orbital shaker. In the cultures of the two species shaken for more than 4 days, the cellular GTX(1+4) toxin contents were significantly lower than in the still control cultures. In A. minutum this trend was also observed in the C(1+2) toxin content. For the two species, inhibition of ecdysal cyst production occurred during the period of exposure of the cultures to stirring (4 or more days) at any time during their growth curve. Recovery of cyst abundances was always observed when turbulence stopped. When shaking persisted for more than 4 days, the net growth rate significantly decreased in A. minutum (from 0.25 +/- 0.01 day(-1) to 0.19 +/- 0.02 day(-1)) and the final cell numbers were lower (ca. 55.4%) than in the still control cultures. In A. catenella, the net growth rate was not markedly modified by turbulence although under long exposure to shaking, the cultures entered earlier in the stationary phase and the final cell numbers were significantly lower (ca. 23%) than in the control flasks. The described responses were not observed in the experiments performed at the low turbulence intensities with an orbital grid system, where the population development was favoured. In those conditions, cells appeared to escape from the zone of the influence of the grids and concentrated in calmer thin layers either at the top or at the bottom of the containers. This ecophysiological study provides new evidences about the sensitivity to high levels of small-scale turbulence by two life cycle related processes, toxin production and encystment, in dinoflagellates. This can contribute to the understanding of the dynamics of those organisms in nature.	CSIC, Inst Ciencies Mar, E-08003 Barcelona, Catalunya, Spain; IRTA, Ctra Poble Nou, Catalunya, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); IRTA	Berdalet, E (通讯作者)，CSIC, Inst Ciencies Mar, Passeig Maritim 37-49, E-08003 Barcelona, Catalunya, Spain.	berdalet@icm.csic.es	Peters, Francesc/A-6364-2009; Guadayol, Oscar/N-2940-2013; Garces, Esther/C-5701-2011; BERDALET, ELISA/K-6956-2014	Peters, Francesc/0000-0001-9405-4306; Guadayol, Oscar/0000-0001-9552-1041; Garces, Esther/0000-0002-2712-501X; BERDALET, ELISA/0000-0003-1123-9706				ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; BERDALET E, 1992, J PHYCOL, V28, P267, DOI 10.1111/j.0022-3646.1992.00267.x; Berdalet E., 1993, TOXIC PHYTOPLANKTON; BERDALET E, 2007, IN PRESS J PHYCOL, V43; BERDALET E, 2005, ALGAL CULTURES ANALO; Berman T, 1998, J PLANKTON RES, V20, P709, DOI 10.1093/plankt/20.4.709; DELGADO M, 1990, Scientia Marina, V54, P1; Dolan JR, 2003, AQUAT MICROB ECOL, V31, P183, DOI 10.3354/ame031183; ESTRADA M, 1979, LIMNOL OCEANOGR, V24, P1065, DOI 10.4319/lo.1979.24.6.1065; FIGUEROA RI, 2007, IN PRESS J PHYCOL, V43; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; GARCES E, 2002, LIFE HIST MICROALGAL; GRANATA TC, 1991, PROG OCEANOGR, V26, P243, DOI 10.1016/0079-6611(91)90003-5; Guadayol O, 2006, SCI MAR, V70, P9, DOI 10.3989/scimar.2006.70n19; Guillard R. R., 1975, Culture of Marine Invertebrate Animals, P2960; Guillard RL, 1973, CULTURE METHODS GROW; Halim Y., 1960, Vie et Milieu, V11, P102; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Havskum H, 2006, AQUAT MICROB ECOL, V42, P55, DOI 10.3354/ame042055; Havskum H, 2005, LIMNOL OCEANOGR, V50, P1543, DOI 10.4319/lo.2005.50.5.1543; Havskum H, 2003, OPHELIA, V57, P125, DOI 10.1080/00785236.2003.10409509; HONSELL G, 1995, HARMFUL TOXIC ALGAL; Juhl AR, 2001, LIMNOL OCEANOGR, V46, P758, DOI 10.4319/lo.2001.46.4.0758; KIORBOE T, 1995, MAR ECOL PROG SER, V122, P135, DOI 10.3354/meps122135; Latasa M, 2001, CHROMATOGRAPHIA, V53, P385, DOI 10.1007/BF02491072; MACKENZIE BR, 1993, MAR ECOL PROG SER, V94, P207, DOI 10.3354/meps094207; MARGALEF R, 1979, TOXIC DINOFLAGELLATE; Motulsky HJ., 2003, PRISM 4 STAT GUIDE S; Oshima Y., 1995, IOC MANUALS GUIDES, P81; PETERS F, 1994, MAR ECOL PROG SER, V115, P299, DOI 10.3354/meps115299; Peters F, 2000, MAR ECOL PROG SER, V205, P291, DOI 10.3354/meps205291; Peters F, 1997, SCI MAR, V61, P205; Petersen JE, 1998, MAR ECOL PROG SER, V171, P23, DOI 10.3354/meps171023; POLLINGHER U, 1981, BRIT PHYCOL J, V16, P281, DOI 10.1080/00071618100650301; Smayda TJ, 2001, J PLANKTON RES, V23, P447, DOI 10.1093/plankt/23.5.447; Smith BC, 2005, J APPL PHYCOL, V17, P317, DOI 10.1007/s10811-005-4944-6; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53; Stiansen JE, 2001, SCI MAR, V65, P151, DOI 10.3989/scimar.2001.65n2151; Sullivan JM, 2003, HARMFUL ALGAE, V2, P183, DOI 10.1016/S1568-9883(03)00039-8; Sullivan JM, 2003, J PHYCOL, V39, P83, DOI 10.1046/j.1529-8817.2003.02094.x; Thomas William H., 1997, Progress in Phycological Research, V12, P283; Tynan CT, 1993, THESIS U CALIFORNIA; Utermohl H., 1953, SIL Commun. 19531996, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Vila M, 2001, MAR ECOL PROG SER, V222, P73, DOI 10.3354/meps222073; Vila M, 2001, J PLANKTON RES, V23, P497, DOI 10.1093/plankt/23.5.497; WYATT T, 1973, NATURE, V244, P238, DOI 10.1038/244238a0; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; Yeung PKK, 2003, PROTOPLASMA, V220, P173, DOI 10.1007/s00709-002-0039-2; YOSHIMATSU S, 1984, Bulletin of Plankton Society of Japan, V31, P107	49	20	20	1	22	EUROPEAN  GEOSCIENCES UNION	KATLENBURG-LINDAU	MAX-PLANCK-STR 13, 37191 KATLENBURG-LINDAU, GERMANY	1726-4170			BIOGEOSCIENCES	Biogeosciences		2007	4	4					559	567		10.5194/bg-4-559-2007	http://dx.doi.org/10.5194/bg-4-559-2007			9	Ecology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	204LY		Green Submitted, gold			2025-03-11	WOS:000249046600008
J	Barreda, V; Palazzesi, L				Barreda, Viviana; Palazzesi, Luis			Patagonian vegetation turnovers during the Paleogene-early Neogene: Origin of arid-adapted floras	BOTANICAL REVIEW			English	Review							TIERRA-DEL-FUEGO; SANTA-CRUZ PROVINCE; COLORADO BASIN; DINOFLAGELLATE CYSTS; CHUBUT PROVINCE; PLANT DIVERSITY; MIOCENE; EOCENE; BIOSTRATIGRAPHY; PALYNOSTRATIGRAPHY	The structure of the living Patagonian flora, dominated by the steppe, is a direct consequence of past climatic and tectonic events. These arid-adapted communities were widespread during the Late Neogene, but their origin in Patagonia can be traced back to the Paleogene. Vegetational trends throughout Paleocene-Miocene time are based on available paleobotanical and palynological information. Four major supported stages in vegetation turnovers are recognized: (1) Paleocene and Early Eocene floras were rainforest-dominated, including many angiosperms with warm-temperate affinities (e.g., palms, Juglandaceae, Casuarinaceae). However, mainly in the Early Eocene, some geographic areas influenced by warm but drier conditions are suggested by the occurrence of certain taxa (e.g., Anacardiaceae). These areas containing arid-adapted floras would have arisen in Patagonian inland regions, in a generally wet continent. (2) The Middle Eocene-Early Oligocene interval was distinguished by the invasion of Nothofagus forests. Progressive replacements of megathermal communities by meso- and microthermal rainforest are documented. Nothofagus forest expansion suggests a marked cooling trend at this time, although some megathermal elements (Aquifoliaceae Ilex, Tiliaceae-Bombacaceae, Sapindaceae) were still present at the beginning of this period. Arid-loving taxa have not been recorded in abundance. (3) Late Oligocene-Early Miocene floras were characterized by the occurrence of shrubby-herbaceous elements belonging to Asteraceae, Chenopodiaceae, Ephedraceae, Convolvulaceae, Fabaceae, and Poaceae. They began to give a modern appearance to plant communities. Xerophytic formations would have occupied coastal salt marshes and pockets in inland areas. Megathermal angiosperms of the Rubiaceae, Combretaceae, Sapindaceae, Chloranthaceae, and Arecaceae occurred mainly during the Late Oligocene. Forests of Nothofagaceae, Podocarpaceae, and Araucariaceae are still documented in extra-Andean Patagonia; however, a contrast between coastal and inland environments may have developed, particularly in the Miocene. (4) Middle-Late Miocene records show an increasing diversity and abundance of xerophytic-adapted taxa, including Asteraceae, Chenopodiaceae, and Convolvulaceae Cressa/Wilsonia. Expansion of these xerophytic taxa, coupled with extinctions of megathermal/nonseasonal elements, would have been associated with both tectonic and climatic forcing factors, led to the development of aridity and extreme seasonality. These arid-adapted Late Miocene floras are closely related to modern communities, with steppe widespread across extra-Andean Patagonia and forest restricted to the western humid upland regions.	Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat, Div Paleobot, Buenos Aires, DF, Argentina	Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Barreda, V (通讯作者)，Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat, Div Paleobot, Av Angel Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina.			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Rev.	JAN-MAR	2007	73	1					31	50		10.1663/0006-8101(2007)73[31:PVTDTP]2.0.CO;2	http://dx.doi.org/10.1663/0006-8101(2007)73[31:PVTDTP]2.0.CO;2			20	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	155NA					2025-03-11	WOS:000245582900002
J	Cremer, H; Sangiorgi, F; Wagner-Cremer, F; McGee, V; Visscher, H				Cremer, Holger; Sangiorgi, Francesca; Wagner-Cremer, Friederike; McGee, Vicki; Visscher, Henk			Diatoms (Bacillariophyceae) and dinoflagellate cysts (Dinophyceae) from Rookery Bay, Florida, USA	CARIBBEAN JOURNAL OF SCIENCE			English	Article						diatoms; dinoflagellate cysts; floristics; taxonomy; Florida	INDIAN RIVER LAGOON; MARINE DIATOMS; PUERTO-RICO; SUBORDER RAPHIDINEAE; MORPHOLOGY; TAXONOMY; GENERA; SEA; SEDIMENTS; BIDDULPHIINEAE	This paper is a report on the diatoms and dinoflagellate cysts identified in a sediment core and a water sample recovered from Rookery Bay, a subtropical estuarine system located on the west coast of Florida. Eighty-eight diatom taxa representing 48 genera, many of which have been rarely observed, and 14 dinoflagellate cyst genera with 20 taxa were identified in Rookery Bay. All taxa are briefly annotated and documented by light micrographs. The most common diatom taxa in the surface sediment sample are Amphicocconeis disculoides, Chaetoceros resting spores, Cyclotella litoralis, Cyinatosira belgica, Neodelphineis pelagica, Paralia sulcata, and Pleurosigina rhombeum. The most abundant dinoflagellate cyst taxa in the surface sample include Brigantedinium spp., Lingulodinium machaerophorum, Polyspheridium zoharyi, Spiniferites bentorii, and Spiniferites ramosus.	Inst Geog Survey, Netherlands Org Appl SCi Res TNO, NL-3584 CB Utrecht, Netherlands; Univ Utrecht, Fac Sci, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; Rookery Bay Natl Estuarine Res Reserve, Florida Dept Environm Protect, Naples, FL 34113 USA	Netherlands Organization Applied Science Research; Utrecht University	Cremer, H (通讯作者)，Inst Geog Survey, Netherlands Org Appl SCi Res TNO, Princetonlaan 6, NL-3584 CB Utrecht, Netherlands.	holger.cremer@tno.nl	; Wagner-Cremer, Friederike/B-4225-2009; Lotter, Andre F./C-3477-2008	Visscher, Henk/0000-0002-9276-0220; Sangiorgi, Francesca/0000-0003-4233-6154; Wagner-Cremer, Friederike/0000-0002-8119-3558; Lotter, Andre F./0000-0002-2954-8809				Andrews G.W., 1984, P 7 INT DIAT S PHIL, P225; [Anonymous], SUSSWASSERFLORA MITT; [Anonymous], 1874, Atlas der Diatomaceen-kunde; [Anonymous], P 6 S REC FOSS DIAT; [Anonymous], INT REV GESAMTEN HYD, DOI DOI 10.1111/j.1529-8817.2006.00291.x; [Anonymous], SUSSWASSERFLORA MITT; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Badylak S, 2004, J PLANKTON RES, V26, P1229, DOI 10.1093/plankt/fbh114; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BREWSTERWINGARD GL, 1998, 98122 US GEOL SURV, P1; BREWSTERWINGARD GL, 1997, 97460 US GEOL SURV, P1; Cooper Sherri Rumer, 1995, Diatom Research, V10, P39; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; de Stefano M, 2003, EUR J PHYCOL, V38, P361, DOI 10.1080/09670260310001612646; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1987, CAN J EARTH SCI, V24, P1886, DOI 10.1139/e87-178; DEFELICE DR, 1978, J PHYCOL, V14, P25, DOI 10.1111/j.1529-8817.1978.tb00627.x; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FENSOME RA, 2004, CONTR SERIES, V42, P909; Foged N., 1984, BIBLIOTHECA DIATOMOL, V5, P1; Foged N., 1975, BIBLIOTHECA PHYCOLOG, V16, P1; FRYXELL GA, 1972, J PHYCOL, V8, P297, DOI 10.1111/j.1529-8817.1972.tb04044.x; GIFFEN MH, 1975, BOT MAR, V18, P71, DOI 10.1515/botm.1975.18.2.71; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HASLE G R, 1979, Bacillaria, V2, P85; Hasle GR, 2001, DIATOM RES, V16, P1; Hasle Grethe R., 1996, P5, DOI 10.1016/B978-012693015-3/50005-X; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; HENDEY NL, 1964, INTRO ACCOUNT SAMM 5; Hustedt F, 1959, L RABENHORSTS KRYPTO, V7, P1; Hustedt F., 1930, L. 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J	Filipova-Marinova, M				Filipova-Marinova, M.			Palynological evidence of vegetation dynamic and human impact along the southern Bulgarian black sea coast	COMPTES RENDUS DE L ACADEMIE BULGARE DES SCIENCES			English	Article						pollen and spores; dinoflagellate cysts; non-pollen palynomorphs; Holocene; archaeology; lithology		A new 190 cm long sediment core taken from Quadrant "I" of the submerged prehistoric settlement in the Bay of Sozopol at the Bulgarian Black Sea coast was analysed for pollen and spores, dinoflagellate cysts and non-pollen palynomorphs. Three local pollen assemblage zones based on AP/NAP ratio were distinguished. A detailed reconstruction of the past vegetation reveals the extent of anthropogenic influence in the area. The available AMS radiocarbon dating of the lowest layer shows that the palaeoecological record starts at ca. 5170 +/- 30 years BP. Complex palynological, archaeological and sedimentological data confirm the existence of settlement and anthropogenic activities during the Final Stage of the Late Eneolithic and the second phase of Early Bronze Age. The interruption of human occupation between these two archaeological cultural stages appeared during the Transitional Period that lasted about 600 years. It was connected with the rise of sea level or land subsidence suggested by the increase of euryhaline marine dinoflagellate cysts.	Nat Hist Museum, Varna 9000, Bulgaria		Filipova-Marinova, M (通讯作者)，Nat Hist Museum, 41 Maria Louisa Blvd, Varna 9000, Bulgaria.	marianafilipova@yahoo.com		Filipova-Marinova, Mariana/0000-0002-0786-9476				Angelova H., 2003, THRACIA PONTICA, V6, P9; [Anonymous], 1996, EURASIA ANTIQUA; BEHRE KE, 1990, NACHRICHTEN NIEDERSA, V59, P141; BOTTEMA S, 1980, ACTA BOT NEERL, V29, P343, DOI 10.1111/j.1438-8677.1980.tb01240.x; BOTTEMA S, 1990, IMPACT ANCIENT MAN L, P231; Bozilova E., 1992, Vegetation History and Archaebotany, V1, P19; Chepalyga A, 2002, Dynamics of Terrestrial Landscape Components and Inner Marine Basins of Northern Eurasia during the Last 130.000, P170; Draganov V., 1995, MONOGRAPHS WORLD ARC, V22, P225; DRAGANOV V, 1998, J H GAUL MEMORIAM, P203; Faegri K., 1989, J BIOGEOGR, V4th; Filipova M, 1989, Bulletin du Musee National de Varna, V25, P177; Filipova-Marinova M., 2003, Aspects of Palynology and Palaeoecology, P213; Filipova-Marinova Mariana, 2002, Phytologia Balcanica, V8, P133; Kuniholm P.I., 2007, BLACK SEA FLOOD QUES, P483, DOI [10.1007/978-1-4020-5302-3_20, DOI 10.1007/978-1-4020-5302-3_20]; Preisinger A., 2004, Izvestia na Narodnia muzey-Varna, V36-37, P9; Todorova H., 1986, Eneolithic in Bulgaria: Vth millennia BC; Todorova H., 2002, DURANKULAK, P17; VAJSOV I, 2002, DURANKULAK, V2, P159; Van Geel B., 1998, A Study of Non-pollen Objects in Pollen Slides (the types as described by Dr Bas Van Geel and colleagues)	19	0	0	0	3	PUBL HOUSE BULGARIAN ACAD SCI	SOFIA	ACADEMICIAN G BONCEV ST, 1113 SOFIA, BULGARIA	1310-1331			CR ACAD BULG SCI	C. R. Acad. Bulg. Sci.		2007	60	6					669	680						12	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	189IQ					2025-03-11	WOS:000247983000012
B	Sluijs, A; Bowen, GJ; Brinkhuis, H; Lourens, LJ; Thomas, E		Williams, M; Haywood, AM; Gregory, FJ; Schmidt, DN		Sluijs, A.; Bowen, G. J.; Brinkhuis, H.; Lourens, L. J.; Thomas, E.			The Palaeocene-Eocene Thermal Maximum super greenhouse: biotic and geochemical signatures, age models and mechanisms of global change	DEEP-TIME PERSPECTIVES ON CLIMATE CHANGE: MARRYING THE SIGNAL FROM COMPUTER MODELS AND BIOLOGICAL PROXIES			English	Article; Book Chapter							CARBON-ISOTOPE STRATIGRAPHY; DINOFLAGELLATE CYSTS; METHANE HYDRATE; CLIMATE-CHANGE; NORTH-AMERICA; OXYGEN-ISOTOPE; BIGHORN BASIN; SEA-LEVEL; MAUD RISE; PALAEOCENE/EOCENE BOUNDARY	The Palaeocene-Eocene Thermal Maximum (PETM), a geologically brief episode of global warming associated with the Palaeocene-Eocene boundary, has been studied extensively since its discovery in 1991. The PETM is characterized by a globally quasi-uniform 5-8 degrees C warming and large changes in ocean chemistry and biotic response. The warming is associated with a negative carbon isotope excursion (CIE), reflecting geologically rapid input of large amounts of isotopically light CO2 and/or CH4 into the exogenic (ocean-atmosphere) carbon pool. The biotic response on land and in the oceans was heterogeneous in nature and severity, including radiations, extinctions and migrations. Recently, several events that appear similar to the PETM in nature, but of smaller magnitude, were identified to have occurred in the late Palaeocene through early Eocene, with their timing possibly modulated by orbital forcing. Although debate continues on the carbon source, the mechanisms that caused the input, the mechanisms of carbon sequestration, and the duration and pacing of the event, the research carried out over the last 15 years has provided new constraints and spawned new research directions that will lead to improved understanding of PETM carbon cycle and climate change.	[Sluijs, A.; Brinkhuis, H.] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Bowen, G. J.] Purdue Univ, W Lafayette, IN 47907 USA; [Lourens, L. J.] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3584 CD Utrecht, Netherlands; [Thomas, E.] Yale Univ, Dept Geol & Geophys, Ctr Study Global Change, New Haven, CT 06520 USA; [Thomas, E.] Wesleyan Univ, Dept Earth & Environm Sci, Middletown, CT USA	Utrecht University; Purdue University System; Purdue University; Utrecht University; Yale University; Wesleyan University	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	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Meteorology & Atmospheric Sciences; Paleontology	Book Citation Index– Science (BKCI-S)	Geology; Meteorology & Atmospheric Sciences; Paleontology	BQD44					2025-03-11	WOS:000280735300015
J	Meier, KJS; Young, JR; Kirsch, M; Feist-Burkhardt, S				Meier, K. J. Sebastian; Young, Jeremy R.; Kirsch, Monika; Feist-Burkhardt, Susanne			Evolution of different life-cycle strategies in oceanic calcareous dinoflagellates	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						calcareous dinoflagellates; Calciodinellum levantinum; confocal laser scanning microscopy; cultures; evolution; Leonella granifera; life-cycle; Thoracosphaera heimii	PFIESTERIA-PISCICIDA; SCRIPPSIELLA-HANGOEI; SURFACE SEDIMENTS; CYST PRODUCTION; DINOPHYCEAE; ENCYSTMENT; CULTURE; NOV; CALCIODINELLOIDEAE; TEMPERATURE	The formation of non-motile resting cysts within the dinoflagellate life-cycle has long been considered to be unsuitable for open oceanic environments, because a considerable part of a population might be lost due to sinking. An alternative life-cycle with the production of vegetative calcareous cells as the dominant life-cycle stage was reported for the oceanic calcareous dinoflagellate Thoracosphaera heimii, and earlier observations suggested that other oceanic calcareous dinoflagellates might have similar life-cycles. In order to test this hypothesis, we investigated the life-cycle of three oceanic calcareous dinoflagellates, Thoracosphaera heimii, Leonella granifera and Calciodinellum levantinum in culture and determined relative ploidy levels with confocal laser scanning microscopy. Whereas C. levantinum forms calcareous resting cysts within the diploid sexual life-cycle phase, T. heimii and L. granifera form vegetative calcareous cells within the haploid asexual phase. By comparison with recently published molecular phylogenies, we conclude that C. levantinum is part of a group of mainly neritic species, from which oceanic species evolved repeatedly. The life-cycle of C. levantinum is basically identical to that of its neritic relatives. A reduced dormancy period is interpreted as an adaptation to the oceanic environment. By contrast, T. heimii and L. granifera are part of a clade of dinoflagellates in which the haploid vegetative life- cycle phase has diversified and enabled their members to access new habitats. While the primary calcification during the diploid phase was lost in this group, calcification was regained secondarily in the haploid vegetative life- cycle phase in T. heimii and L. granifera. Therefore the vegetative calcareous cells are not homologous with the calcareous resting cysts formed in other calcareous dinoflagellates, which may also be expressed in different biomineralization modes.	Nat Hist Museum, London SW7 5BD, England; Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	Natural History Museum London; University of Bremen	Meier, KJS (通讯作者)，Europole Mediterraneen Arbois, CEREGE, BP 80, F-13545 Aix En Provence 04, France.	meier@cerege.fr	Feist-Burkhardt, Susanne/B-1522-2009; Meier, K. J. Sebastian/H-7914-2014	Young, Jeremy/0000-0001-9320-9804; Meier, K. J. 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J. Phycol.		2007	42	1					81	89		10.1080/09670260600937833	http://dx.doi.org/10.1080/09670260600937833			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	150TO		Bronze			2025-03-11	WOS:000245242200006
J	Van Simaeys, S; De Man, E; Vandenberghe, N				Van Simaeys, Stefaan; De Man, Ellen; Vandenberghe, Noel			Re-assessment of the new geological map of Belgium: Earliest oligocene dinoflagellate cyst-based ages in the Leuven area (sheet 24 Aarschot)	GEOLOGICA BELGICA			English	Article						Oligocene; dinoflagellate cysts; biostratigraphy; Tongrian; Belgium	NORTH-SEA BASIN	The dinoflagellate cyst (dinocyst) assemblages of two samples from a temporary outcrop in the vicinity of Haacht (Leuven) have been analysed. The co-occurrence of Areosphaeridium diktyoplokum, Cerebrocysta bartonensis, Glaphyrocysta semitecta, Rombodinium perforatum and Thalassiphora reticulata allows correlation with the North Sea Oligocene-1 zone. As a consequence, the considered unit has a latest Eocene to earliest Oligocene age, equivalent to the age of the marine Tongrian. Comparison of the studied area with the recent 1: 5 0 000 geological map (sheet 24 Aarschot) shows that the current lithostratigraphic interpretation of the analysed section, i.e. the Middle Eocene Maldegem Formation, can no longer be uphold.	Univ Louvain, B-3000 Louvain, Belgium; Inst Royal Sci Nat Belgique, B-1000 Brussels, Belgium		Van Simaeys, S (通讯作者)，Univ Louvain, Redlingenstr 16, B-3000 Louvain, Belgium.							De Coninck J., 1999, B SOC BELG GEOL, V105, P171; De Coninck Jan, 1995, Mededelingen Rijks Geologische Dienst, V53, P65; De Man E, 2004, NETH J GEOSCI, V83, P193, DOI 10.1017/S0016774600020266; DECONINCK J, 2001, GEOLOGICAL SURVEY BE, V294, P1; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Kothe A., 1990, GEOL JB A, V118, P3; Laga Pieter, 2001, Geologica Belgica, V4, P135; Saeys R, 2004, NETH J GEOSCI, V83, P179, DOI 10.1017/S0016774600020242; STEURBAUT E, 1986, MEDEDELINGEN WERKGRO, V23, P49; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; Van Simaeys S, 2005, REV PALAEOBOT PALYNO, V134, P105, DOI 10.1016/j.revpalbo.2004.12.003; Vandenberghe N, 2004, NETH J GEOSCI, V83, P155, DOI 10.1017/S0016774600020229; Vandenberghe Noel, 2003, P419; VANSIMAEYS SV, 2004, THESIS KATHOLIEKE U	14	4	4	0	5	GEOLOGICA BELGICA	BRUSSELS	JENNER STREET 13, BRUSSELS, BELGIUM	1374-8505			GEOL BELG	Geol. Belg.		2007	10	1-2					39	46						8	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	167LM					2025-03-11	WOS:000246453200003
J	Louwye, S; De Schepper, S; Laga, P; Vandenberghe, N				Louwye, Stephen; De Schepper, Stijn; Laga, Pieter; Vandenberghe, Noel			The Upper Miocene of the southern North Sea Basin (northern Belgium): a palaeoenvironmental and stratigraphical reconstruction using dinoflagellate cysts	GEOLOGICAL MAGAZINE			English	Article						palynology; dinoflagellates; Miocene; North Sea	MESSINIAN SALINITY CRISIS; PLIOCENE; ATLANTIC; PALEOECOLOGY; POLYKRIKOS; ZONATION	Organic-walled palynomorph assemblages from the Kasterlee Formation in northern Belgium provide new insights into the Late Miocene depositional history and palaeoenvironments of the southernmost North Sea Basin. Ranges of key dinoflagellate cysts constrain the unit between 7.5 and 5.32 Ma, that is, a latest Tortonian to Messinian age. The palynomorph assemblage is characterized, amongst others, by Geonettia clineae, an opportunistic species that thrives in mesotrophic, coastal embayments with a low sediment influx. This environmental setting is corroborated by the notable presence of Gramocysta verricula, a species with preference for shallow marine environments. The occurrence of species of the fresh water green alga Pediastrum indicates manifest river discharge in a near-shore environment or embayment. The coastal depositional environment mirrored by the palynomorphs of the Kasterlee Formation succeeds the distinct transgressive and fully marine environments of the underlying Diest Formation in the Campine area. The results from the palynological study, combined with lithological and geophysical data, show that both Upper Miocene formations are two distinct depositional cycles separated by an erosional or regressive phase. The upper boundary of the Kasterlee Formation is correlated with the Me2 sequence boundary at 5.73 Ma. The Kasterlee Formation is herein formally moved from the Lower Pliocene series to the Upper Miocene series. The coastal environment, probably characterized by a shoaling phase, recorded at the border of the southern North Sea Basin, matches the global record of regressive phases in Messinian sedimentary sequences, which are linked to cooling and increasing global ice volume.	Univ Ghent, Paleontol Res Unit, B-9000 Ghent, Belgium; Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; Royal Belgian Inst Nat Sci, Geol Survey Belgium, B-1000 Brussels, Belgium; Katholieke Univ Leuven, B-3000 Louvain, Belgium	Ghent University; University of Cambridge; Royal Belgian Institute of Natural Sciences; KU Leuven	Louwye, S (通讯作者)，Univ Ghent, Paleontol Res Unit, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	stephen.louwye@UGent.be	De Schepper, Stijn/A-2836-2011; Louwye, Stephen/D-3856-2012	De Schepper, Stijn/0000-0002-6934-0914; Louwye, Stephen/0000-0003-4814-4313				ADAMS CG, 1977, NATURE, V269, P383, DOI 10.1038/269383a0; AHARON P, 1993, GEOLOGY, V21, P771, DOI 10.1130/0091-7613(1993)021<0771:SLEITS>2.3.CO;2; BERGGREN WA, 1995, GEOCHRONOLOGY TIME S, P29; Blow W. 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Mag.	JAN	2007	144	1					33	52		10.1017/S0016756806002627	http://dx.doi.org/10.1017/S0016756806002627			20	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	138WY					2025-03-11	WOS:000244395200003
J	Schioler, P; Andsbjerg, J; Clausen, OR; Dam, G; Dybkjaer, K; Hamberg, L; Heilmann-Clausen, C; Johannessen, EP; Kristensen, LE; Prince, I; Rasmussen, JA				Schioler, P.; Andsbjerg, J.; Clausen, O. R.; Dam, G.; Dybkjaer, K.; Hamberg, L.; Heilmann-Clausen, C.; Johannessen, E. P.; Kristensen, L. E.; Prince, I.; Rasmussen, J. A.			Lithostratigraphy of the palaeogene-lower neogene succession of the Danish North Sea	GEOLOGICAL SURVEY OF DENMARK AND GREENLAND BULLETIN			English	Review						lithostratigraphy; biostratigraphy; North Sea Basin; palaeogene; neogene	FORAMINIFERAL BIOSTRATIGRAPHY; SEQUENCE STRATIGRAPHY; DINOFLAGELLATE CYSTS; UPPERMOST OLIGOCENE; MIOCENE SUCCESSION; SELANDIAN BOUNDARY; EOCENE; BASIN; TRANSITION; ORIGIN	As a result of a lithological, sedimentological and biostratigraphic study of well sections from the Danish sector of the North Sea, including some recently drilled exploration wells on the Ringkobing-Fyn High, the lithostratigraphic framework for the siliciclastic Palaeogene to Lower Neogene sediments of the Danish sector of the North Sea is revised. The sediment package from the top of the Chalk Group to the base of the Nordland Group is subdivided into seven formations containing eleven new members. The existing Vale, Lista, Sele, Fur, Balder, Horda and Lark Formations of previously published lithostratigraphic schemes are adequate for a subdivision of the Danish sector at formation level. Bor is a new sandstone member of the Vale Formation. The Lista Formation is subdivided into three new mudstone members: Vile, Ve and Bue, and three new sandstone members: Tyr, Idun and Rind. Kolga is a new sandstone member of the Sele Formation. Hefring is a new sandstone member of the Horda Formation. Freja and Dufa are two new sandstone members of the Lark Formation. Danish reference sections are established for the formations, and the descriptions of their lithology, biostratigraphy, age and palaeoenvironmental setting are updated.	[Schioler, P.; Andsbjerg, J.; Dybkjaer, K.; Kristensen, L. E.] Geol Survey Greenland, DK-1350 Copenhagen, Denmark; [Clausen, O. R.; Heilmann-Clausen, C.] Univ Aarhus, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Dam, G.; Hamberg, L.] DONG Energy, DK-2970 Horsholm, Denmark; [Johannessen, E. P.; Prince, I.] Statoil Norway, N-4035 Stavanger, Norway; [Rasmussen, J. A.] Univ Copenhagen, Geol Museum, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland; Aarhus University; Orsted; Equinor; University of Copenhagen	Schioler, P (通讯作者)，Geol Survey Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	p.schioler@gns.cri.nz	Clausen, Ole/A-5290-2012; Dybkjær, Karen/G-5223-2018; Dam, Gregers/G-4548-2018; Heilmann-Clausen, Claus/A-4848-2012; Rasmussen, Jan Audun/Q-7472-2018	Rasmussen, Jan Audun/0000-0003-0520-9148				Ahmadi Z.M., 2003, MILLENNIUM ATLAS PET, P235; [Anonymous], TERTIARY RES; [Anonymous], DANMARKS GEOLOGISK A; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1988, Geol. 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Surv. Den. Greenl. Bull.		2007		12					5	77						73	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	242AS					2025-03-11	WOS:000251697500001
J	Kim, CJ; Kim, HG; Kim, CH; Oh, HM				Kim, Choong-Jae; Kim, Hak-Gyoon; Kim, Chang-Hoon; Oh, Hee-Mock			Life cycle of the ichthyotoxic dinoflagellate <i>Cochlodinium polykrikoides</i> in Korean coastal waters	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; armored type; unarmored type; resting cyst		Since 1995, blooms of the harmful dinoflagellate, Cochlodinium polykrikoides, have caused considerable mortality of aquatic organisms and economic loss in Korea. However, little is known about the life cycle of the species, except for the planktonic vegetative stage; therefore, the aim of this paper was to elucidate the life cycle of C polykrikoides. Its life cycle has two morphologically different stages: an armored and an unarmored vegetative stage. Armored vegetative cells were found in seawater samples collected in late-November and developed into four-cell chained, unarmored vegetative cells under laboratory culture. In samples collected in late-May, both the armored and unarmored types (vegetative swimming stage) occurred; the former easily developed into an unarmored vegetative cell type, suggesting that the armoured-unarmored transition occurs as early as May. A presumptive resting cyst, round but folded at one side, was produced from armored type cells in laboratory conditions. It was also collected from natural bottom sediments, which suggests it is the dormant resting cyst of C. polykrikoides. (c) 2006 Elsevier B.V. All rights reserved.	Environm Biotechnol Res Ctr, KRIBB, Taejon 305333, South Korea; Pukyong Natl Univ, Dept Oceanog, Pusan 606737, South Korea; Pukyong Natl Univ, Dept Aquaculture, Pusan 606737, South Korea	Korea Research Institute of Bioscience & Biotechnology (KRIBB); Pukyong National University; Pukyong National University	Oh, HM (通讯作者)，Environm Biotechnol Res Ctr, KRIBB, Taejon 305333, South Korea.	heemock@kribb.re.kr		Oh, Hee-Mock/0000-0002-2151-3687				Cho ES, 2004, J PLANKTON RES, V26, P175, DOI 10.1093/plankt/fbh022; Cho Eun Seob, 2000, Journal of Fisheries Science and Technology, V3, P83; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Jeong Seong-Youn, 2000, Journal of the Korean Fisheries Society, V33, P331; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kim Hak Gyoon, 1999, Bulletin of National Fisheries Research and Development Institute, V57, P119; Kim Hak Gyoon, 1997, Ocean Research (Seoul), V19, P185; Kim Hak-Gyoon, 2001, Journal of the Korean Fisheries Society, V34, P691; KIM HG, 1998, XUNTA GALICIA INTERG, P227; Kim Hyung Chul, 2001, Journal of the Korean Fisheries Society, V34, P445; KIM SJ, 2003, J KOREAN FISH SOC, V36, P716; Lim W A, 2004, THESIS PUSAN NATL U; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Na G.-H., 1996, J. Aquacult., V9, P239; NFRDI, 2004, HARMF ALG BLOOMS KOR; Park Young-Tae, 1998, Journal of the Korean Fisheries Society, V31, P767; Park Young-Tae, 1998, Journal of the Korean Fisheries Society, V31, P920; YOUNG YJ, 1998, B KOREAN FISH SOC, V31, P695; Yu ZM, 1999, CHINESE SCI BULL, V44, P617, DOI 10.1007/BF03182721	19	62	70	0	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	JAN	2007	6	1					104	111		10.1016/j.hal.2006.07.004	http://dx.doi.org/10.1016/j.hal.2006.07.004			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	131CR					2025-03-11	WOS:000243846200009
J	Tiffany, MA; Wolny, J; Garrett, M; Steidinger, K; Hurlbert, SH				Tiffany, Mary Ann; Wolny, Jennifer; Garrett, Matthew; Steidinger, Karen; Hurlbert, Stuart H.			Dramatic blooms of <i>Prymnesium</i> sp (Prymnesiophyceae) and <i>Alexandrium margalefii</i> (Dinophyceae) in the Salton Sea, California	LAKE AND RESERVOIR MANAGEMENT			English	Article						bioluminescence; dinoflagellates; foam; phytoplankton; salt lake; cysts; allelopathy	DINOFLAGELLATE GENUS ALEXANDRIUM; POPULATION-DYNAMICS; RECENT SEDIMENTS; COASTAL WATERS; GROWTH-RATE; FISH; PARVUM; CYSTS; MICROECOSYSTEMS; SALINITY	In early 2006, unusual algal blooms of two species occurred in the Salton Sea, a large salt lake in southern California. In mid-January local residents reported bioluminescence in the Sea. Starting in February, large rafts of long-lasting foam, also bioluminescent, were observed as well. Microscopy investigations on water and sediment samples collected in March showed the marine dinoflagellate, Alexandrium margalefii, and the prymnesiophyte, Prymnesium sp., both previously unreported in the Salton Sea, to be abundant. Bioluminescence and foam production continued through March. Other dinoflagellate species, recorded during earlier studies, were rare or not detected during these blooms. Despite the fact that many Alexandrium species are known paralytic shellfish poison (PSP) producers, preliminary saxitoxin tests on this population of A. margalefii were negative. Previous reports on A. margalefii do not mention bioluminescence. It appears that the foam was caused by the Prymnesium sp. bloom, probably via protein-rich exudates and lysis of other algal cells, and its glow was due to entrained A. margalefii. This is the first report of A. margalefii in U.S. waters and the first report of it in a lake.	[Tiffany, Mary Ann; Hurlbert, Stuart H.] San Diego State Univ, Dept Biol, San Diego, CA 92182 USA; [Tiffany, Mary Ann; Hurlbert, Stuart H.] San Diego State Univ, Ctr Inland Waters, San Diego, CA 92182 USA; [Wolny, Jennifer; Garrett, Matthew] Fish & Wildlife Res Inst, Florida Fish & Wildlife Conservat Commiss, St Petersburg, FL 33701 USA; [Wolny, Jennifer; Garrett, Matthew; Steidinger, Karen] Florida Inst Oceanog, St Petersburg, FL 33701 USA	California State University System; San Diego State University; California State University System; San Diego State University; Florida Fish & Wildlife Conservation Commission	Tiffany, MA (通讯作者)，San Diego State Univ, Dept Biol, San Diego, CA 92182 USA.	mtiffany@sunstroke.sdsu.edu		Wolny, Jennifer L./0000-0002-3556-5015				ABRAHAMS MV, 1993, ECOLOGY, V74, P258, DOI 10.2307/1939521; Andersen R. 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M., 1987, BIOL DINOFLAGELLATES, P269; Thornton DCO, 1999, ETHOL ECOL EVOL, V11, P179, DOI 10.1080/08927014.1999.9522835; Throndsen Jahn, 1997, P591, DOI 10.1016/B978-012693018-4/50007-0; Tiffany MA, 2007, LAKE RESERV MANAGE, V23, P582, DOI 10.1080/07438140709354039; Tillmann U, 2007, J PLANKTON RES, V29, P527, DOI 10.1093/plankt/fbm034; TOMAS C, 2004, HARMFUL ALGAE 2002, P369; WALKER BW, 1961, CALIF DEP FISH GAME, V113, P1; Watts JM, 2001, HYDROBIOLOGIA, V466, P159, DOI 10.1023/A:1014599719989	52	2	3	1	16	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	1040-2381	2151-5530		LAKE RESERV MANAGE	Lake Reserv. Manag.		2007	23	5					620	629		10.1080/07438140709354041	http://dx.doi.org/10.1080/07438140709354041			10	Limnology; Marine & Freshwater Biology; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Water Resources	V06EV		Bronze			2025-03-11	WOS:000207177800010
J	Bati, Z; Sancay, RH				Bati, Zuhtu; Sancay, Recep Hayrettin			Palynostratigraphy of Rupelian sediments in the Mus Basin, Eastern Anatolia, Turkey	MICROPALEONTOLOGY			English	Article							OLIGOCENE; BIOSTRATIGRAPHY; STRATIGRAPHY	Biostratigraphically important dinoflagellate, acritarch, and pollen events calibrated by planktonic foraminifers and calcareous nannoplankton are here documented for the first time in the Rupelian sediments of the Mus Basin, Eastern Anatolia. The LAD of Ascostomocystis potane in coincidence with the FAD of Globorotalia opima opima in the "late" Rupelian, the FAD of Wetzeliella gochtii in the "middle" Rupelian, the LAD of Wetzeliella gochtii in the "latest" Rupelian, and the FADs of Compositae (tubuliflorae type), Monoporopollenites gramineoides and Umbelliferae at the base of Rupelian should be of particular importance for regional correlations. In addition to the Rupelian acritarch Ascostomocystis potane, diverse dinoflagellate cysts such as Achillodinium biformoides, Wetzeliella gochtii, Membranophoridium aspinatum, Distatodinium biffii, Enneaedocysta pectiniformis complex, Deflandrea spp., Glaphyrocysta group, and terrestrial palynomorphs including Compositae (tubuliflorae type), Slowakipollenites hipophaeoides, Mediocolpopollis compactus Monoporopollenites gramineoides, Umbelliferae, Periporopollenites multiporatus, Ephedripites sp., Cicatricosisporites sp., Lusatisporites perinatus, Cingulatisporites spp. and Saxosporis sp. comprise the main palynological elements of the Rupelian deposits. Combined information from all three disciplines (terrestrial/marine palynomorphs and sedimentary organic matter, nannoplankton, and foraminifers) suggests that Rupelian sedimentation in the studied sections was characterized by an initial fresh water phase and continued with deposition in shallow to deep marine environments. Although the marine Eocene-Oligocene transition has not been observed in the studied sections, the presence of transitional marine Upper Eocene and Lower Oligocene successions in the northern regions (Cat, SW of Erzurum) as documented by Sancay (2005) suggests that the boundary between the Upper Eocene and Lower Oligocene sediments could have been comformable in some localities of the Mus Basin. However, this argument still needs to be tested where the appropriate lithologies, with recoverable microfossils, are present in the transitional interval in the basin.	[Bati, Zuhtu; Sancay, Recep Hayrettin] Turkish Petr Corp, Res Ctr, Ankara, Turkey	Ministry of Energy & Natural Resources - Turkey; Turkish Petroleum Corporation (TPAO)	Bati, Z (通讯作者)，Turkish Petr Corp, Res Ctr, Ankara, Turkey.	bati@petro.tpao.gov.tr; hsancay@petrol.tpao.gov.tr						AKGUN F, 1986, Turkiye Jeoloji Kurumu Bulteni, V29, P13; AKGUN F, 2004, CARDAK TOKCA BURDUR; Akkiraz M.S., 2000, THESIS DOKUZ EYLUL U; ALLEN CR, 1969, 32 GEOL PLAN SCI DIV; [Anonymous], 1987, B GEOLOGICAL SOC TUR; Arpat E., 1972, Bull. Miner. Res. Explor. Inst. 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Jahrb., V111, P1; Islam M.A., 1983, Revue de Micropaleontologie, V25, P231; Klumpp B., 1953, Palaeontographica A, V103, P377; Kothe A., 1990, GEOL JB A, V118, P3; KRUTZSCH W, 1970, LIEFERUNG, V7; Martini E., 1971, P 2 PLANKT C ROM 197, P739; Morgenroth P., 1968, Geologisches Jahrbuch, V86, P533; MORGENROTH P., 1966, PALAEONTOGRAPHICA, V119, P1; Powell A.J., 1986, Contribution Series, V17, P83; Powell A.J., 1986, AASP CONTRIB SERIES, V17, P105; Pross J, 2001, NEUES JAHRB GEOL P-A, V219, P207, DOI 10.1127/njgpa/219/2001/207; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; Rossignol M, 1962, POLLEN SPORES, V3, P303; Sancay RH, 2006, TURK J EARTH SCI, V15, P259; SANCAY RH, 2005, THESIS MIDDLE E TECH; SARJEANT W A S, 1981, Meyniana, V33, P97; SARJEANT W A S, 1970, Grana, V10, P74; Seng├Ar A.M.C., 1979, J GEOL SOC LONDON, V136, P269, DOI [10.1144/gsjgs.136.3.0269, DOI 10.1144/GSJGS.136.3.0269]; SENGOR AMC, 1979, TECTONOPHYSICS, V55, P361, DOI 10.1016/0040-1951(79)90184-7; Steininger FF, 1997, EPISODES, V20, P23; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	65	16	18	0	1	MICROPALEONTOLOGY PRESS	NEW YORK	256 FIFTH AVE, NEW YORK, NY 10001 USA	0026-2803			MICROPALEONTOLOGY	Micropaleontology		2007	53	4					249	283		10.2113/gsmicropal.53.4.249	http://dx.doi.org/10.2113/gsmicropal.53.4.249			35	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	242SF					2025-03-11	WOS:000251745300001
J	Sajjadi, F; Hashemi, H; Dehbozorgi, A				Sajjadi, Freshteh; Hashemi, Hossein; Dehbozorgi, Afsaneh			Middle Jurassic palynomorphs of the Kashafrud formation, Koppeh Dagh Basin, Northeastern Iran	MICROPALEONTOLOGY			English	Article								Diverse and moderately well-preserved palynofloras occur in Middle Jurassic sediments of the Kashafrud Formation at the Senjedak section, southeast of Mashhad, northeastern Iran. Trilete and monolete spores and pollen dominate the assemblages, whereas dinoflagellate cysts, foraminiferal test linings, and fungal spores are minor components. Forty-seven species of spores (30 genera) and 15 species of pollen (eight genera) are identified. Representatives of Dictiophyllidites and Klukisporites are particularly abundant. Based on the stratigraphic distribution of miospores, three distinctive strati graphically successive palynofloras informally termed in ascending order, Assemblages A, B, and C are identified within the Kashafrud Formation. These are compared with palynozones known from Iran and elsewhere. Based on the presence of certain miospore species, the Kashafrud palynofloras are collectively dated as Middle Jurassic (Bajocian-Bathonian), thus corroborating the faunal (ammonoid) evidence. The appearance of a key miospore species, Contignisporites burgeri, within the succession has been used to attribute a late Bajocian age and early Bathonian age to the lower and upper parts of the studied interval, respectively. Inferred natural relationships of the miospores imply derivation from a diverse parental flora of Pterophyta and gymnosperms, such as Coniferophyta, Cycadophyta, and Ginkgophyta, growing under warm, humid conditions during the Bajocian-Bathonian. The associated marine fauna (ammonites), marine palynomorphs (proximate dinoflagellate cysts, and acritarchs such as Micrhystridium), and foraminiferal test linings, along with terrestrial palynomorphs (spores and pollen) collectively indicate an open marine, nearshore depositional setting for the Kashafrud Formation at the section studied.	[Sajjadi, Freshteh; Dehbozorgi, Afsaneh] Univ Tehran, Coll Sci, Sch Geol, Tehran, Iran; [Hashemi, Hossein] Tarbiat Moallem Univ, Sch Appl Sci, Fac Sci & Res, Dept Geol, Tehran 15614, Iran	University of Tehran; Kharazmi University	Sajjadi, F (通讯作者)，Univ Tehran, Coll Sci, Sch Geol, Enghelab Ave, Tehran, Iran.	sajjadi@khayam.ut.ac.ir; hashemi@saba.tmu.ac.ir; dehbozorgi@khayam.ut.ac.ir						ABBINK OA, 1998, LAB PALEOBOTANY PALY, V8; ACHILLES H, 1984, Palaeontographica Abteilung B Palaeophytologie, V194, P14; [Anonymous], 1975, Palaeontographica B; [Anonymous], 1993, LANDSCAPE ECOLOGY ST, DOI DOI 10.1007/978-94-011-2318-1_2; [Anonymous], 1977, Palaeontographica B; [Anonymous], 1996, Palynology: principles and applications; BALME BE, 1995, REV PALAEOBOT PALYNO, V87, P85; BALME BE, 1957, COMMONWEALTH SCI IND; Batten D.J., 1996, Palynology: principles and applications, V2, P795; Batten D. 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J	Versteegh, GJM; Blokker, P; Marshall, C; Pross, J				Versteegh, Gerard J. M.; Blokker, Peter; Marshall, Craig; Pross, Joerg			Macromolecular composition of the dinoflagellate cyst <i>Thalassiphora pelagica</i> (Oligocene, SW Germany)	ORGANIC GEOCHEMISTRY			English	Article							ALIPHATIC POLYMER; LOW-TEMPERATURE; FATTY-ACIDS; PYROLYSIS; PRESERVATION; SULFUR; ORIGIN; LIPIDS; POLYSULFIDES; PRECURSORS	Origin, composition and fate of organic particles in marine sediments are to a large extent unknown. Here we contribute to resolving this lack of information by reporting on the structural characterization (FTIR micro-spectroscopy, py/GC/MS and TMAH assisted thermochemolysis GC/MS) of hand-picked Thalassiphora pelagica dinoflagellate cysts (Oligocene). The cyst wall macromolecule is relatively condensed. It is composed of a mixture of aliphatic moieties with the linear carbon units having an average chain length of similar to 12 carbon atoms. In the pyrolysate this is reflected in aliphatic series of alkanes and alkenes (both <C-23), alkan-2-ones (<C-16) and alkylbenzenes (<C-20) and a high abundance of alkylated indenes and naphthalenes (both <C-13). The relatively strong aromatic signature of the pyrolysate supports a relatively extensive cross-linking between the aliphatic moieties, which is very unlike the highly aliphatic resistant biopolymer walls of Chlorophyta and Eustigmatophyta but agrees with the sparse information on organic-walled cysts of other Dinophyta. Thermochemolysis further supports the above and further indicates that carboxylic acids have been added to the macromolecule post-mortem. Additional series of alkylated thiophenes and benzothiophenes present in the pyrolysate and thermochemolysate are considered to result from early sulphurisation of the cysts in the anoxic to suboxic setting of the depositional environment. (c) 2007 Elsevier Ltd. All rights reserved.	Univ Hamburg, Fac Geogsci, Inst Biochem & Marine Chem, D-20146 Hamburg, Germany; Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Syst Ecol, Inst Ecol Sci, NL-1081 HV Amsterdam, Netherlands; Univ Sydney, Sch Chem, Vibrat Spect Facil, Sydney, NSW 2006, Australia; Goethe Univ Frankfurt, Inst Geosci, D-60054 Frankfurt, Germany	University of Hamburg; Vrije Universiteit Amsterdam; University of Sydney; Goethe University Frankfurt	Versteegh, GJM (通讯作者)，Univ Hamburg, Fac Geogsci, Inst Biochem & Marine Chem, Bunde Str 55, D-20146 Hamburg, Germany.	fgfa008@uni-hamburg.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				Allard B, 1998, ORG GEOCHEM, V28, P543, DOI 10.1016/S0146-6380(98)00012-6; BRIGGS DEG, 1995, LETHAIA, V28, P15, DOI 10.1111/j.1502-3931.1995.tb01589.x; CHUECAS L, 1969, J MAR BIOL ASSOC UK, V49, P97, DOI 10.1017/S0025315400046439; CONESA JA, 1994, ENERG FUEL, V8, P1238, DOI 10.1021/ef00048a012; Damste J.S. 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Geochem.		2007	38	10					1643	1656		10.1016/j.orggeochem.2007.06.007	http://dx.doi.org/10.1016/j.orggeochem.2007.06.007			14	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	230UR					2025-03-11	WOS:000250902000004
J	Riboulleau, A; Schnyder, J; Riquier, L; Lefebvre, V; Baudin, F; Deconinck, JF				Riboulleau, Armelle; Schnyder, Johann; Riquier, Laurent; Lefebvre, Vincent; Baudin, Francois; Deconinck, Jean-Francois			Environmental change during the Early Cretaceous in the Purbeck-type Durlston Bay section (Dorset, Southern England): A biomarker approach	ORGANIC GEOCHEMISTRY			English	Article							BRANCHED ALIPHATIC ALKANES; GEOCHEMICAL SIGNIFICANCE; MOLECULAR INDICATORS; DINOFLAGELLATE CYSTS; CYANOBACTERIAL MATS; BIOLOGICAL MARKERS; SEDIMENTARY RECORD; PLANT BIOMARKERS; CLAY MINERALOGY; CARBON-ATOMS	The Purbeck-type section (Durlston Bay, Dorset, UK) exhibits littoral lagoonal to lacustrine facies. It shows a gradual climatic/environmental change from semi-arid conditions associated with evaporites at the Jurassic-Cretaceous transition, to a more humid climate at the end of the Berriasian. Though generally organic-poor (total organic carbon, TOC, <1.3%), the Durlston Bay section shows an orgarlic-rich episode (TOC up to 8.5%) located at the transition from evaporitic to more humid facies. A biomarker study was performed in order to determine the origin of the organic matter (OM) in the section and see if changes in organic sources accompanied the general environmental change. The distribution of alkanes, hopanes and steranes indicates that the origin of the OM is mainly algal/bacterial and only changed moderately with the climatic evolution. The saline and anoxic bottom water conditions indicated for most of the samples point to the recurrence of salinity stratification within the basin. A high contribution of odd numbered C-23-C-31 n-alkanes from algaenan-containing freshwater algae, in particular Botryococcus, is noted for all the samples, despite the low abundance of these organisms in the corresponding palynofacies. This prominence probably results from the high resistance to degradation and the selective preservation of Botryococcus-related lipids. The subtle balance of aridity and freshwater inputs favoured both an abundance of Botryococcus and the development of anoxia, leading to the enhanced preservation of OM during the intermediate climatic episode, while the conditions were less favourable during the semi-arid and more humid episodes. (C) 2007 Elsevier Ltd. All rights reserved.	Univ Lille 1, PBDS, UMR 8110, F-59655 Villeneuve Dascq, France; Univ Paris 06, CNRS, UMR Tecton 7072, F-75252 Paris 05, France; Univ Bourgogne, CNRS, UMR Biogeosci 5561, F-21000 Dijon, France	Universite de Lille; Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Universite de Bourgogne; Centre National de la Recherche Scientifique (CNRS)	Riboulleau, A (通讯作者)，Univ Lyon 1, UMR PaleoEnvironm & PaleobioSphere 5125, UFR Sci Terre, Campus La Doua,2 Rue Dubois,Bat Geode, F-69622 Villeurbanne, France.	armelle.riboulleau@univ-lille1.fr	Lefebvre, Vincent/F-4900-2013; Schnyder, Johann/IQV-5253-2023; Baudin, Francois/ITU-7485-2023; Riquier, Laurent/AAZ-4381-2020; Riboulleau, Armelle/G-4719-2012; RIQUIER, Laurent/C-5286-2008	/0000-0002-8317-6567; Riboulleau, Armelle/0000-0002-2717-8330; RIQUIER, Laurent/0000-0001-5510-2061; Baudin, Francois/0000-0003-3180-459X				Albro P.W., 1976, Chemistry and Biochemistry of Natural Waxes, P419; Allard B, 2000, PHYTOCHEMISTRY, V54, P369, DOI 10.1016/S0031-9422(00)00135-7; 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Geochem.		2007	38	11					1804	1823		10.1016/j.orggeochem.2007.07.006	http://dx.doi.org/10.1016/j.orggeochem.2007.07.006			20	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	238KM					2025-03-11	WOS:000251446500002
J	Riding, JB; Kyffin-Hughes, JE; Owens, B				Riding, James B.; Kyffin-Hughes, Jane E.; Owens, Bernard			An effective palynological preparation procedure using hydrogen peroxide	PALYNOLOGY			English	Article						palynomorph preparation techniques; hydrogen peroxide; Carboniferous; Jurassic; Paleogene; Quaternary; Antarctica; UK; USA	POLLEN ASSEMBLAGES; SEYMOUR-ISLAND; STRATIGRAPHY; SPORE	Most pre-Quaternary palynology samples are currently prepared by demineralization of the sediment/sedimentary rock matrix using hydrochloric and hydrofluoric acids (HCl and HF respectively). If a consistently effective alternative to this procedure can be developed, palynological processing will be made significantly less hazardous to both laboratory personnel, and to the wider environment. Furthermore, most non-acid processing methods are normally quicker and cheaper than matrix dissolution using acid. Some authors have previously used hydrogen peroxide (H2O2) to extract palynomorphs by the physico-chemical disaggregation of the clay fraction. However, H2O2 is a powerful oxidizing agent and hence can potentially destroy sedimentary organic material, including palynomorphs. A new method using hot H2O2, where exposure of the sample material to the H2O2 is minimized, has been developed. Crushed sample material in a suitable vessel is placed on a hot plate for one minute, treated with 15-30% H2O2 for 10 minutes, then the residue is diluted with cold distilled water. Disaggregated sample material tends to float, and is decanted into a large vessel containing distilled water to further dilute the H2O2. If any undisaggregated sample remains, the procedure is repeated several times if necessary. Relatively indurated sedimentary lithotypes normally require several treatments. The reason for this stepwise treatment is that the organic material is not exposed to H2O2 for sustained periods, thereby reducing the possibility of palynomorph damage/degradation due to oxidation. When the sample matrix has been fully disaggregated, the residue can be further processed as appropriate. In this study, eight samples of Carboniferous, Jurassic, Paleogene, and Quaternary age were prepared quantitatively using the new H2O2 method. These were all prepared using 30% H2O2. For comparison, they were also prepared quantitatively using HCl/HF and/or sodium hexametaphosphate [(NaPO3)(6)]. Quantitative preparations allow the concentration of palynomorphs extracted to be determined, and therefore the effectiveness of the techniques used can be compared objectively. The palynomorph residues derived from these three techniques varied markedly. The H2O2 method does not consistently disaggregate all the sample material, particularly the older and more indurated lithotypes. Some evidence of oxidation effects was observed. Two samples of Mississippian mudstone from the U.S.A. were prepared using H2O2 and (NaPO3)(6). Both methods produced abundant miospores, however the H2O2 procedure yielded far higher palynomorph concentrations than the (NaPO3)(6) technique. Minor degradation of palynomorphs in the H2O2 preparation was noted. The H2O2 and HCl/HF methods were compared directly on a palynomorph-rich sample of Upper Carboniferous mudstone from offshore Scotland. Both preparations produced abundant miospores. The HCl/HF method had significantly higher recovery levels than the H2O2 procedure. It appears that the H202 method simultaneously macerates the matrix, and oxidizes any amorphous organic material (AOM) present. In this sample, the HCl/HF residue was relatively rich in AOM. By contrast, the H202 preparation is virtually clear of this phytoclast type, which partially obscures palynomorphs. Two samples of the Middle Jurassic Grantham Formation of eastern England were processed using H(2)O(2)and HCl/HF. The two methods produced abundant palynofloras of similar palynomorph concentrations. Two dinoflagellate cyst acmes within the Danian (Paleogene) part of the Lopez de Bertodano Formation of Seymour Island, Antarctica were also tested using H2O2, (NaPO3)(6), and HCl/HF. The H2O2 preparation completely destroyed the dominant taxon, Palaeoperidinium pyrophorum, in one sample. By contrast, the (NaPO3)(6) and HCl/HF preparations produced abundant, fully representative palynofloras. In the other sample, the acme of Spinidinium spp. is completely unaffected by the H2O2 preparation procedure. The final sample of this study is an unconsolidated clay of Late Pleistocene age from offshore Scotland. Both the H2O2 and HCl/HF preparations proved similar in both taxonomic content and overall palynomorph yield. The new method of preparation using hot H2O2 has proved to be extremely effective. In particular, it appears to be superior to the (NaPO3)(6) procedure for indurated lithotypes. However care should be taken because H2O2 can destroy certain dinoflagellate cysts and kerogen macerals which are especially susceptible to oxidation. Further development work, and more comparative testing of the H2O2, (NaPO3)(6), and HCl/HF procedures, should be undertaken.	[Riding, James B.; Kyffin-Hughes, Jane E.; Owens, Bernard] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk			NERC [bgs010024] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], MEMOIR BRIT GEOLOGIC; [Anonymous], 1980, PALAEONTOLOGY; [Anonymous], 2007, Paleopalynology; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R.A., 1988, Geology and Paleontology of Seymour Island Antarctic Peninsula, V169, P155, DOI [10.1130/MEM169-p155, DOI 10.1130/MEM169-P155, 10.1130/mem169-p155]; ASKIN RA, 1990, REV PALAEOBOT PALYNO, V65, P105, DOI 10.1016/0034-6667(90)90061-M; ASKIN RA, 1990, MICROPALEONTOLOGY, V36, P141, DOI 10.2307/1485498; Batten D.J., 1999, FOSSIL PLANTS SPORES, P15; Brown CA., 1960, Palynological Techniques; Clayton G, 1998, J MICROPALAEONTOL, V17, P183, DOI 10.1144/jm.17.2.183; CLAYTON G, 1977, MEDEDELINGEN RIJKS G; Coleman U., 1987, COUR FORSCH I SENCKE, V98, P75; COLLINSON ME, 1978, ANN BOT-LONDON, V42, P233, DOI 10.1093/oxfordjournals.aob.a085445; Crame JA, 2004, CRETACEOUS RES, V25, P411, DOI 10.1016/j.cretres.2004.02.002; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DODSWORTH P, 1995, J MICROPALAEONTOL, V14, P6, DOI 10.1144/jm.14.1.6; Eshet Y, 1996, REV PALAEOBOT PALYNO, V94, P101, DOI 10.1016/S0034-6667(96)00008-5; Evitt William R., 1998, Palynology, V22, P1; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FUNKHOUSER JOHN W., 1959, MICROPALEONTOLOGY, V5, P369, DOI 10.2307/1484431; Gelsthorpe DN, 2002, J MICROPALAEONTOL, V21, P81, DOI 10.1144/jm.21.1.81; Gray J., 1965, Handbook of paleontological techniques, P530; Harland R., 1992, P253; HARLAND R, 1989, J GEOLOGICAL SOC, V25, P113; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hopkins Jennifer A., 2002, Palynology, V26, P167, DOI 10.2113/0260167; Hughes NF., 1964, COMPTES RENDUS, V3, P1095; Hyde JE, 1915, J GEOL, V23, P655, DOI 10.1086/622282; *I GEOL SCI, 1975, 757 I GEOL SCI; Jenkins W. A. M., 1967, Palaeontology, V10, P436; Leschik G., 1956, PALAEONTOGRAPHICA, V100, P122; MOLYNEUX S.G., 1984, Journal of Micropalaeontology, V3, P41; Owens B., 1978, 7820 I GEOL SCI; PEARSON T., 1999, Fossil Plants and Spores: Modern Techniques, P20; PHIPPS D, 1984, PAPERS DEP GEOLOGY U, V11; PIRRIE D, 1992, ANTARCT SCI, V4, P259, DOI 10.1017/S0954102092000427; Powell A.J., 1992, P155; Riding J.B., 1992, WH92307R BRIT GEOL S; Riding JB, 2006, PALYNOLOGY, V30, P69, DOI 10.2113/gspalynol.30.1.69; Riding James B., 2004, Revista Brasileira de Paleontologia, V7, P13; Riding JB, 2006, J MICROPALAEONTOL, V25, P35, DOI 10.1144/jm.25.1.35; Riding James B., 1991, Palynology, V15, P115; RIDING JB, 1992, NEWSL STRATIGR, V26, P19; RIDING JB, 2000, CR0008 BRIT GEOL SUR; Smith A.H.V., 1967, SP PAP PALAEONTOL, V1, P1; SRIVASTAVA SK, 1987, GEOBIOS-LYON, V20, P5, DOI 10.1016/S0016-6995(87)80057-8; Stoker M.S., 1993, UK OFFSHORE REGIONAL; THORN VC, 2007, ONL P 10 INT S ANT E; Williams G, 2005, MICROPALEAEONTOLOGIC, P219; Winslow M.R., 1962, 364 US GEOL SURV, V364, P27; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; [No title captured]	53	13	14	0	21	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2007	31						19	36		10.2113/gspalynol.31.1.19	http://dx.doi.org/10.2113/gspalynol.31.1.19			18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	252GN		Green Accepted			2025-03-11	WOS:000252435100006
J	Mao, SZ; Li, H; Qin, XD; Wu, GX; Harland, R				Mao, Shaozhi; Li, He; Qin, Xiaodan; Wu, Guoxuan; Harland, Rex			Dinoflagellate cysts and environmental evolution of the oligocene to lower miocene at site 1148, odp leg 184, south china sea	PALYNOLOGY			English	Article						dinoflagellate cysts; paleoenvironments; Oligocene; Miocene; basin development; South China Sea; ODP leg 184	ATLANTIC-OCEAN; ADJACENT SEAS; SEDIMENTS; NORTH; RECORDS	The Oligocene to Lower Miocene of Site 1148, Ocean Drilling Program (ODP) Leg 184 was investigated palynologically to explore environmental change within the newly formed rifted South China Sea. The basin first developed 32.8 Ma ago during an initial rifting phase, and before sea floor spreading. Palynomorph Assemblage A contains abundant coastal and neritic dinoflagellate cysts (for example, Lingulodinium and Spiniferites) and a small number of oceanic Impagidinium species, together with abundant pollen, spores, and terrigenous phytoplankton. Offshore transportation induced by basement subsidence played an important role in the makeup of this assemblage. Paleoenvironments during the earliest Oligocene include shallow shelf, shelf/slope boundary, and mid slope regimes. The latter is indicated by the intermittent and rare occurrences of Impagidinium. Later, in the Early Oligocene to earliest Late Oligocene, there was a deepening of the basin with increasing influence of lower slope environments, indicated by increasing abundances of Impagidinium. A barren zone corresponding to a period of sea floor spreading during the latest Oligocene to the earliest Miocene effectively separates assemblages A and B. The Early Miocene environment deepened to a lower slope (>1500 m) regime, indicated by Assemblage B with consistent Impagidinium. This regime was relatively stable with much less terrigenous input, indicated by the rare occurrence of pollen and spores, and the absence of terrigenous phytoplankton.	[Mao, Shaozhi; Li, He; Qin, Xiaodan] China Univ Geosci, Beijing 100083, Peoples R China; [Wu, Guoxuan] Tongji Univ, Shanghai 200092, Peoples R China	China University of Geosciences; Tongji University	Mao, SZ (通讯作者)，China Univ Geosci, Beijing 100083, Peoples R China.	rex.harland@ntlworld.com		LI, JIE/0009-0001-1924-0210				[Anonymous], 1980, Special Papers in Palaeontology; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Downie C., 1971, Geoscience Man, V3, P29; Eaton GL, 2001, NEUES JAHRB GEOL P-A, V219, P171, DOI 10.1127/njgpa/219/2001/171; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Kothe A., 1990, GEOL JB A, V118, P3; Li XH, 2003, EARTH PLANET SC LETT, V211, P207, DOI 10.1016/S0012-821X(03)00229-2; MAO SZ, 2004, P OCEAN DRILLING PRO; Oboh-Ikuenobe Francisca E., 1999, Palynology, V23, P87; Pross J, 2001, PALAEOGEOGR PALAEOCL, V166, P369, DOI 10.1016/S0031-0182(00)00219-4; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; [Wang P. Shipboard Scientific Party Shipboard Scientific Party], 2000, P ODP INITIAL, V184, P1, DOI [10.2973/odp.proc.ir.184.2000, DOI 10.2973/ODP.PROC.IR.184.2000, DOI 10.2973/ODP.PROC.IR.184.107.2000]; Wang PX, 2003, CHINESE SCI BULL, V48, P2549, DOI 10.1360/03wd0156; Wang PX, 2003, CHINESE SCI BULL, V48, P2524, DOI 10.1007/BF03037016; WILLIAMS GL, 1977, MAR MICROPALEONTOL, V2, P223, DOI 10.1016/0377-8398(77)90012-3; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169	24	3	5	0	15	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2007	31						37	52		10.2113/gspalynol.31.1.37	http://dx.doi.org/10.2113/gspalynol.31.1.37			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	252GN					2025-03-11	WOS:000252435100007
J	Antolinez-Delgado, H; Oboh-Ikuenobe, FE				Antolinez-Delgado, Hernan; Oboh-Ikuenobe, Francisca E.			New species of dinoflagellate cysts from the paleocene of the Anambra Basin, southeast Nigeria	PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Paleogene; Nigeria		Six new species of dinoflagellate cysts and one new combination from the Paleocene to ?lowermost Eocene succession in the Alo-1 well, southeast Nigeria, are proposed herein. The new species are Achomosphaera quadrata, Diphyes bifidum, Ifecysta fusiforma, Ifecysta heterospinosa, Palaeocystodinium rafii, and Wilsonidium stellatum. Furthermore, Fibrocysta lappacea (Drugg 1970) Stover & Evitt 1978 is transferred to Ifecysta, and the diagnosis of Ifecysta is emended.	[Antolinez-Delgado, Hernan; Oboh-Ikuenobe, Francisca E.] Missouri Univ Sci & Technol, Rolla, MO 65409 USA	University of Missouri System; Missouri University of Science & Technology	Oboh-Ikuenobe, FE (通讯作者)，Missouri Univ Sci & Technol, Rolla, MO 65409 USA.	ikuenobe@umr.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691				[Anonymous], 2007, Paleopalynology; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Antolinez H, 2006, PALYNOLOGY, V30, P213; ANTOLINEZ HJ, 2006, THESIS U MISSOURIROL; BERGGREN WA, 1960, INT GEOL C COP, V21, P41; Drugg W.S., 1970, P N AM PAL CONV CH G, P809; DUCHENE REJ, 1988, NOUVELLE SERIE, V2, P147; DUCHENE RJ, 1985, CAHIERS MICROPALEONT, P5; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FENSOME RA, 1993, 7 MICR PRESS, V7; Oboh-Ikuenobe FE, 2005, J AFR EARTH SCI, V41, P79, DOI 10.1016/j.jafrearsci.2005.02.002; Reyment R.A., 1965, ASPECTS GEOLOGY NIGE; *SHELL PETR, 1976, UNPUB PREL LITH BIOS; STOVER LE, 1978, GEOLOGICAL SCI; Williams GL, 2000, AM ASS STRATIGRAPHIC; WILSON GRAEME J., 1967, N Z J BOT, V5, P469	16	15	18	0	0	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2007	31						53	62		10.2113/gspalynol.31.1.53	http://dx.doi.org/10.2113/gspalynol.31.1.53			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	252GN					2025-03-11	WOS:000252435100008
J	Lenz, OK; Wilde, V; Riegel, W; Heinrichs, T				Lenz, Olaf K.; Wilde, Volker; Riegel, Walter; Heinrichs, Till			Distribution and paleoecologic significance of the freshwater dinoflagellate cyst <i>Messelodinium thielepfeifferae</i> gen. et sp nov from the Middle Eocene of Lake Messel, Germany	PALYNOLOGY			English	Article						middle Eocene; Germany; maar lake; freshwater dinoflagellate cysts; taxonomy; systematics; paleoecology	SEDIMENTS	An exploration well drilled at the Middle Eocene fossil site of Messel, near Darmstadt, Germany proved that the famous Messel oil shale was deposited in a maar lake. During a quantitative palynological investigation of the entire succession of lake sediments, a monospecific population of dinoflagellate cysts was encountered. Based on transmitted light and scanning electron microscope (SEM) studies, they are assigned to the new peridinioid taxon Messelodinium thielepfeifferae gen. et sp. nov. because they are acavate and lack distinct apical or antapical horns. The dinoflagellate cysts exhibit considerable intraspecific variation in surface ornamentation. Messelodinium thielepfeifferae gen. et sp. nov. is abundant in sediments of the early holomictic stage of Lake Messel, but generally is reduced in frequency in the oil shale which represents the meromictic stage. These dinoflagellate cysts appear in peak abundances in mass flow and debris flow deposits in which material from the lake shore was transported downslope to the basin center. Thus, major concentrations of Messelodinium thielepfeifferae gen. et sp. nov. occurred in nearshore environments either due to primary population density of the parent motile stage, or due to secondary cyst accumulation by wind and wave action. The dinoflagellate cysts are notably absent in the uppermost 25 m of the core, where Botryococcus dominates. This shift in algal populations is interpreted as a response to changes in the chemistry of the water body.	[Lenz, Olaf K.; Riegel, Walter; Heinrichs, Till] Univ Gottingen, Geowissensch Zentrum Gottingen, Abt Geobiol, D-37077 Gottingen, Germany; [Lenz, Olaf K.; Wilde, Volker] Forschungsinst Senckenberg, Sekt Palaobot, D-60325 Frankfurt, Germany	University of Gottingen; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN)	Lenz, OK (通讯作者)，Univ Gottingen, Geowissensch Zentrum Gottingen, Abt Geobiol, Goldschmidtstr 3, D-37077 Gottingen, Germany.	olenz@gwdg.de		Lenz, Olaf K./0000-0002-0958-7982				[Anonymous], 1983, Wetzel; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; De Dekker P., 1988, Lacustrine Petroleun Source Rocks. Geological Society Special Publication, V40, P45; Felder M., 2004, COURIER FORSCHUNGSIN, V252, P151; Felder M., 2001, GEOL JB HESSEN, V128, P29; Goth K., 1990, COURIER FORSCHUNGSIN, V131, P1; Harms FJ, 2003, NAT MUS, V133, P140; Harms FJ, 1999, KARTE VERBREITUNG ME; Kaiser M. L., 1974, GEOLOGISCHES JB A, V25, P85; Köhler J, 2000, REV PALAEOBOT PALYNO, V112, P39, DOI 10.1016/S0034-6667(00)00034-8; Krutzsch W, 1962, HALLESCHES JB MITTEL, V4, P40; Krutzsch W, 1990, ACTA U CAROL GEOLOGI, V4, P345; Lenz OK, 2007, REV PALAEOBOT PALYNO, V145, P217, DOI 10.1016/j.revpalbo.2006.11.001; Liebig Karin, 1998, Kaupia Darmstaedter Beitraege zur Naturgeschichte, V7, P1; Liebig V., 2001, KAUPIA, V11, P3; LORENZ V, 2000, TERRA NOSTRA, P284; Mertz D.F., 2005, COUR FORSCH I SENCKE, V255, P67; Michaelis W., 1988, COUR FORSCH I SENCKE, V107, P89; Nickel B., 1996, MAINZER NATURWISS AR, V18, P1; Pollingher U., 1987, Botanical Monographs (Oxford), V21, P502; Richter G, 2005, PALAEOGEOGR PALAEOCL, V223, P147, DOI 10.1016/j.palaeo.2005.04.002; Richter G., 2004, NAT MUS, V134, P129; Schulz R., 2002, Z ANGEW GEOL, V48, P9; THIELE-PFEIFFER H, 1988, Palaeontographica Abteilung B Palaeophytologie, V211, P1	24	16	21	0	6	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2007	31						119	134		10.2113/gspalynol.31.1.119	http://dx.doi.org/10.2113/gspalynol.31.1.119			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	252GN					2025-03-11	WOS:000252435100013
J	Lucas-Clark, J				Lucas-Clark, Joyce			<i>Litosphaeridium</i> too:: Two new dinoflagellate cyst species from the Cretaceous of California	PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Cretaceous; California	FRANCISCAN	The 'Middle' Cretaceous of the Northern California Coast Ranges has yielded unusually well-preserved specimens of Litosphaeridium, some of which (Litosphaeridium arundum, Litosphaeridium bacar, Litosphaeridium conispinum, and Litosphaeridium siphoniphorum subsp. glabrum) have been analyzed in detail previously. Two other species, which were discovered later, are Litosphaeridium adnatum sp. nov. and Litosphaeridium gaponoffiae sp. nov. Litospheridium adnatum sp. nov. is most similar to Litosphaeridium siphoniphorum, but has an adnate operculum, sulcal processes, a more elongate central body, and less of the central body is covered by processes. The other, Litosphaeridium gaponoffiae sp. nov., is most similar to Litosphaeridium arundum and Litospheridium fucosum, but has goblet-shaped processes, a free operculum, a more spherical central body, and its cingular processes are not reduced as they are in Litospheridium arundum. The two species are from the late Albian based on the associated dinoflagellate cysts.	Clark Geol Serv, Fremont, CA 94536 USA		Lucas-Clark, J (通讯作者)，Clark Geol Serv, 1023 Old Canyon Rd, Fremont, CA 94536 USA.	jluclark@comcast.net						[Anonymous], 1985, SPOROPOLLENIN DINOFL; Bailey E.H., 1964, FRANCISCAN RELATED R; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BERKLAND JO, 1973, GEOL SOC AM BULL, V84, P2389, DOI 10.1130/0016-7606(1973)84<2389:RVOSOC>2.0.CO;2; BERKLAND JO, 1972, AM ASSOC PETR GEOL B, V56, P2295; BERKLAND JO, 1972, P 24 INT GEOL C, V3, P99; BLAKE MC, 1981, GEOTECTONIC DEV CALI, V1, P307; BLAKE MC, 1984, PACIFIC SECTION SOC, V43, P221; BLAKE MC, 1985, EARTH SCI SERIES, V1, P159; BLAKE MC, 1978, PAC COAST PALEOGEOGR, V2, P397; BROWN RD, 1964, US GEOLOGICAL SURVEY, V4750, P7; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; GUCWA PR, 1975, GEOLOGY, V3, P105, DOI 10.1130/0091-7613(1975)3<105:MTLCSM>2.0.CO;2; LUCAS-CLARK J, 1984, Palynology, V8, P165; LUCASCLARK J, 1986, PACIFIC SECTION SOC, P223; MCLAUGHLIN RJ, 1983, AM GEOPHYS UNION T, V64, P868; SWE W, 1970, GEOLOGICAL SOC AM B, V81, P125	18	3	3	0	0	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2007	31						205	217		10.2113/gspalynol.31.1.205	http://dx.doi.org/10.2113/gspalynol.31.1.205			13	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	252GN					2025-03-11	WOS:000252435100017
J	Roberts, D; Craven, M; Cai, MH; Allison, I; Nash, G				Roberts, D.; Craven, M.; Cai, Minghong; Allison, I.; Nash, G.			Protists in the marine ice of the Amery Ice Shelf, East Antarctica	POLAR BIOLOGY			English	Article							SOUTHERN-OCEAN SEDIMENTS; WATER-COLUMN ASSEMBLAGES; MAJOR DIATOM TAXA; SEA-ICE; SURFACE SEDIMENTS; MASS-BALANCE; WEDDELL SEA; BENEATH; PHYTOPLANKTON; BIOGEOGRAPHY	Samples of marine ice were collected from the Amery Ice Shelf, a large embayed ice shelf in East Antarctica, during the Austral summer of 2001-2002. The samples came from a site -90 km from the iceberg calving front of the shelf, where the ice is 479 m thick and the lower 203 m is composed of accreted marine ice. Protists identified within the marine ice layer of the Amery Ice Shelf include diatoms, chrysophytes, silicoflagellates and dinoflagellates. The numerical dominance of sea ice indicator diatoms such as Fragilariopsis curta, Fragilariopsis cylindrus, Fragilariopsis rhombica and Chaetoceros resting spores, and the presence of cold open water diatoms such as Fragilariopsis kerguelensis and species of Thalassiosira suggest the protist composition of the Amery marine ice is attributable to seeding from melting pack and/or fast ice protist communities in the highly productive waters of Prydz Bay to the north.	Antarctic Climate & Ecosyst Cooperat Res Ctr, Hobart, Tas 7001, Australia; Australian Antarctic Div, Kingston, Tas 7050, Australia; Polar Res Inst China, Shanghai 200129, Peoples R China	Antarctic Climate & Ecosystems Cooperative Research Centre (ACE CRC); Australian Antarctic Division; Polar Research Institute of China	Craven, M (通讯作者)，Antarctic Climate & Ecosyst Cooperat Res Ctr, Private Bag 80, Hobart, Tas 7001, Australia.	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JAN	2007	30	2					143	153		10.1007/s00300-006-0169-7	http://dx.doi.org/10.1007/s00300-006-0169-7			11	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	114TJ					2025-03-11	WOS:000242688200003
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J	Köthe, A				Koethe, Angelika			Cenozoic biostratigraphy from the German North Sea sector (G-11-1 borehole, dinoflagellate cysts, calcareous nannoplankton)	ZEITSCHRIFT DER DEUTSCHEN GESELLSCHAFT FUR GEOWISSENSCHAFTEN			English	Article						Neogene; Paleogene; biostratigraphy; dinoflagellate cysts; calcareous nannoplankton; log correlation; seismic sequence; North Sea Basin; German North Sea sector	LOWER MIOCENE; STRATIGRAPHY; BASIN; OLIGOCENE; TERTIARY; BOUNDARY; DEPOSITS; BELGIUM; EOCENE; MARGIN	Ditch cuttings from Neogene and Paleogene sequences of the G-11-1 borehole from the German North Sea were analysed for dinoflagellate cysts and calcareous nannoplankton. The record displays several time gaps (Late Thanetian to Middle Y presian, Bartonian to Middle Priabonian, earliest Oligocene, within the Middle Rupelian, Chattian to earliest Aquitanian, Middle Burdigalian and Late Tortonian to Early Zanclean), which were detected biostratigraphically by the absence of zones and by graphic correlation of this borehole with a biostratigraphic standard for North Germany (time-depth correlation). These time gaps can be traced for at least 30 kilometres in seismic lines. There is apparently no hiatus around the Cretaceous/Paleogene boundary because the youngest Maastrichtian calcareous nannoplankton zone (CC26) and the oldest Paleocene dinoflagellate cyst zone (D I) were determined. One of the most prominent seismic features in the Cenozoic sequences of the North Sea Basin is the Mid-Miocene Unconformity (MMU). The age of the MMU in the G-11-1 borehole can be narrowed as Early Miocene (dinoflagellate cyst zone DN2 for sediments below the MMU) to Middle Miocene (dinoflagellate cyst zone DN5, calcareous nannoplankton zone NN5 for sediments above the MMU). A gamma ray log correlation with the Wursterheide borehole, which lies about 190 km southeast, refines the downlap age to the latest Early Miocene (latest part of dinoflagellate cyst zone DN3) - slightly older than previously known. The MMU probably coincides with a hiatus or a condensed section which comprises the largest part of dinoflagellate cyst zone DN3. Below the MMU, the sedimentary pattern is strongly influenced by numerous time gaps (erosions or condensed sections), whereas above the MMU prograding deltas are the main features. The compacted sedimentation rate at the G-11-1 location amounts to 97 m/Ma for sediments above the MMU and to 21 m/Ma for Cenozoic sediments below the MMU. Biostratigraphic data based on dinoflagellate cysts and calcareous nannoplankton are published for the first time for Cenozoic sediments from the German North Sea sector and for Pliocene sediments from Germany.	Fed Inst Geosci & Nat Resources, D-30655 Hannover, Germany		Köthe, A (通讯作者)，Fed Inst Geosci & Nat Resources, Stilleweg 2, D-30655 Hannover, Germany.	angelika.koethe@bgr.de						Andruleit Harald, 2000, Journal of Nannoplankton Research, V22, P201; [Anonymous], 1987, SCIENCE, DOI DOI 10.1126/SCIENCE.235.4793.1156; [Anonymous], 1988, Geol. 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Dtsch. Ges. Geowiss.		2007	158	2					287	327		10.1127/1860-1804/2007/0158-0287	http://dx.doi.org/10.1127/1860-1804/2007/0158-0287			41	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	288OB					2025-03-11	WOS:000254994600011
J	Rasmussen, ES; Dybkjaer, K; Piasecki, S				Rasmussen, Erik S.; Dybkjaer, Karen; Piasecki, Stefan			Neogene fluvial and nearshore marine deposits of the Salten section, central Jylland, Denmark	BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK			English	Article						sedimentary facies; stratigraphy; dinoflagellate cysts; Denmark; Miocene	OLIGOCENE LOWER MIOCENE; SEA-LEVEL CHANGES; UPPERMOST OLIGOCENE; NORTH-SEA; DINOFLAGELLATE CYSTS; STRATIGRAPHY; SUCCESSION; EVOLUTION; SYSTEMS; BASIN		Geoctr Copenhagen, Geol Survey Denmark & Greeland, Copenhagen, Denmark	Geological Survey Of Denmark & Greenland	Rasmussen, ES (通讯作者)，Geoctr Copenhagen, Geol Survey Denmark & Greeland, Oster Voldgade 10, Copenhagen, Denmark.	esr@geus.dk	Dybkjær, Karen/G-5223-2018					[Anonymous], 2004, GEOL SURV DEN GREENL; [Anonymous], 9210 GEOL SURV CAN; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BUCHARDT B, 1978, NATURE, V275, P121, DOI 10.1038/275121a0; CHRISTENSEN NS, 2004, THESIS U COPENHAGEN; Coccioni R., 1997, Developments in Palaeontology and Stratigraphy, V15, P279; DYBKJAER K, 2005, 20056 DANM GRONL GEO; DYBKJAER K, 2004, 200439 DENM GRONL GE; DYBKJAER K, 2001, 2001104 DANM GRONL G; DYBKJAER K, 2003, 200328 DANM GRONL GE; Dybkjaer K, 2000, B GEOL SOC DENMARK, V47, P87; DYBKJAR K., 2005, P 6 PETR GEOL C LOND, P1347, DOI DOI 10.1144/0061347; Dybkjær K, 2004, REV PALAEOBOT PALYNO, V131, P201, DOI 10.1016/j.revpalbo.2004.03.006; Dybkjær K, 2004, PALAEOGEOGR PALAEOCL, V206, P41, DOI 10.1016/j.palaeo.2003.12.021; ELLIOT T, 1974, SEDIMENTOLOGY, P611; Friis H, 1998, SEDIMENT GEOL, V117, P221, DOI 10.1016/S0037-0738(98)00013-X; FRIIS H, 1976, B GEOL SOC DEN, V25, P99; HANSEN HCS, 1993, P 2 S MAR GEOL GEOL, P39; HANSEN JO, 1985, THESIS U AARHUS; HANSEN JPV, 2004, THESIS U AARHUS; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; Hartz N., 1909, BIDRAG DANMARKS TERT, V20; Japsen P, 2002, MAR GEOL, V186, P571, DOI 10.1016/S0025-3227(02)00208-6; JAPSEN P, 1993, AAPG BULL, V77, P194; JESSE J, 1995, GEOLOGISK TIDSSKRIFT, V2, P95; JORDAN DW, 1992, AAPG BULL, V76, P1601; KOCH BE, 1989, GEOL SURVEY DENMAR A, V22; LARSEN G, 1994, MELLEMSTE JYLLAND GE; Larsen G, 1959, DANMARKS GEOLOGISKE, V82; Loseth H., 2005, GEOLOGICAL SOC LONDO, P845, DOI DOI 10.1144/0060845; Lotsch D., 1968, GRUNDRISS GEOLOGIE D, V1, P356; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; Martinsen O.J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European Basins, P91; MIALL AD, 1996, GEOLGOY FLUVIAL DEPO; Nio S.-D., 1991, CLASTIC TIDAL SEDIME, V16, P3; Piasecki S., 2005, Palaeontos, V7, P29; PIASECKI S, 2002, 200218 DANM GRONL GE; Plint AG, 2003, SEDIMENTOLOGY, V50, P1147, DOI 10.1111/j.1365-3091.2003.00599.x; Pross J, 2002, MAR MICROPALEONTOL, V45, P1, DOI 10.1016/S0377-8398(01)00046-9; RADWANSKI A, 1975, Bulletin of the Geological Society of Denmark, V24, P229; Rasmussen E.S., 2005, PALEONTOS, V7, P5; Rasmussen ES, 2004, B GEOL SOC DENMARK, V51, P89; Rasmussen ES, 2004, GLOBAL PLANET CHANGE, V41, P15, DOI 10.1016/j.gloplacha.2003.08.004; Rasmussen ES, 2005, SEDIMENTOLOGY, V52, P25, DOI 10.1111/j.1365-3091.2004.00681.x; Sorgenfrei T, 1958, MOLLUSCAN ASSEMBLAGE; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; WEIBEL R, 2003, B GEOLOGICAL SOC DEN, V50, P141; WILLIAMS GL, 2004, P OC DRILL PROGR SCI, V189; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Ziegler P.A., 1990, Geological Atlas of Western and Central Europe: The Hague	50	13	14	0	4	GEOLOGICAL SOC DENMARK	COPENHAGEN	OSTER VOLDGADE 5-7, DK-1350 COPENHAGEN, DENMARK	2245-7070			B GEOL SOC DENMARK	Bull. Geol. Soc. Den.	DEC	2006	53						23	37						15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	141AS					2025-03-11	WOS:000244549100002
J	Wagreich, M; Pavlishina, P; Malata, E				Wagreich, Michael; Pavlishina, Polina; Malata, Ewa			Biostratigraphy of the lower red shale interval in the Rhenodanubian Flysch Zone of Austria	CRETACEOUS RESEARCH			English	Article						Rhenodanubian Flysch Zone; Albian; Cenomanian; Dinoflagellates; Foraminifera; nannofossils	MONT RISOU; BIOZONATION	In the Rhenodanubian Flysch Zone of Austria, between the Aptian-Albian "Gault Flysch" and the Cenomanian-Turonian Reiselsberg Formation, an interval with predominant red shales ("Untere Bunte Schiefer") occurs. In the Oberaschau section near Attersee (Upper Austria) a ca. 18-m-thick interval of alternating red and grey shales and marlstones with minor sandstones is present. Thin sandstone intercalations are interpreted as distal turbidites. Dinoflagellate cyst assemblages indicate the Litosphaeridium siphoniphorum Zone. The concurrent presence of Litosphaeridium siphoniphorum and Ovoidinium verrucosum in all samples allows a correlation to the lower part of this zone, thus defining a Late Albian-Early Cenomanian age. Based on foraminifera, the red beds can be assigned to the topmost Rotalipora appenninica Zone and the Rotalipora globotruncanoides Zone due to the presence of small morphotypes of the index taxa. Nannofossils indicate standard zones CC9/UC0 throughout the red interval, defined by the first occurrence of Eiffellithus turriseiffelii, and UC1 above the red shales. Based on these multistratigraphic data, a latest Albian-Early Cenomanian age can be inferred. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Vienna, Dept Geol Sci, A-1090 Vienna, Austria; Univ Sofia, Dept Geol & Paleontol, Sofia 1000, Bulgaria; Jagiellonian Univ, Inst Geol Sci, Krakow, Poland	University of Vienna; University of Sofia; Jagiellonian University	Wagreich, M (通讯作者)，Univ Vienna, Dept Geol Sci, Waehringer Guertel 18, A-1090 Vienna, Austria.	michael.wagreich@univie.ac.at	Pavlishina, Polina/AAL-5710-2021; Wagreich, Michael/D-2279-2013	Pavlishina, Polina/0000-0002-1172-9142; Wagreich, Michael/0000-0002-8828-0857; Malata, Ewa/0000-0003-4900-0186				[Anonymous], 1996, Palynology: principles and applications; BAK K, 1998, STUD GEOL POL, V111, P7; BAK K, 2000, P 5 INT WORKSH AGGL, V7, P15; Bralower T.J., 1995, Geochronology Time Scales and Global Stratigraphic Correlation, P65; Burnett J.A., 1998, Calcareous Nannofossil Biostratigraphy, P132; Caron M., 1985, P17; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Egger H, 2002, SEDIMENT GEOL, V152, P247, DOI 10.1016/S0037-0738(02)00072-6; Egger H, 1992, Z DTSCH GEOL GES, V143, P51; Egger Hans, 1993, Zitteliana, V20, P59; Faupl P., 2000, Mitteilungen der O sterreichischen Geologischen Gesellschaft, V92, P79; Fiet N, 2001, CRETACEOUS RES, V22, P63, DOI 10.1006/cres.2000.0237; Foucher J.-C., 1979, Palaeontographica Abteilung B Palaeophytologie, V169, P78; FOUCHER J.C., 1983, CAHIERS MICROPAL ONT, V4, P23; Gale AS, 1996, CRETACEOUS RES, V17, P515, DOI 10.1006/cres.1996.0032; GASINSKI MA, 1983, CRETACEOUS RES, V4, P221, DOI 10.1016/0195-6671(83)90038-1; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Gradstein FM, 2004, EPISODES, V27, P83, DOI 10.18814/epiiugs/2004/v27i2/002; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Herngreen G.F.W., 1978, Palinologia, P273; Hu XM, 2005, CRETACEOUS RES, V26, P3, DOI 10.1016/j.cretres.2004.11.011; HU XM, 2003, IGCP 463 IGCP 494 WO, P8; Jeremiah J, 1996, J MICROPALAEONTOL, V15, P97, DOI 10.1144/jm.15.2.97; Kennedy WJ, 2004, EPISODES, V27, P21, DOI 10.18814/epiiugs/2004/v27i1/003; Kirsch Karl-Heinz, 2003, Zitteliana Reihe A, V43, P143; Leereveld H., 1995, LPP CONTRIBUTION SER, V2; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; Mattern F., 1999, Zeitschrift der Deutschen Geologischen Gesellschaft, V150, P89; Miles G.A., 1980, Initial Reports of the Deep Sea Drilling Project, V51-53, P791; MILES GA, 1980, INITIAL REPORTS DEEP, V53, P791; MILES GA, 1980, INITIAL REPORTS DEEP, V52, P791; Perch-Nielsen K., 1985, P329; Premoli Silva I., 2004, INT SCH PLANKT FOR 3; PREY SIEGMUND, 1950, JAHRB GEOL BUNDESANSTALT, V94, P93; Prokoph Andreas, 1997, Freiberger Forschungshefte Reihe C, V468, P259; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; Robaszynski F, 1995, B SOC GEOL FR, V166, P681; Robaszynski F., 1979, Cahiers de Micropaleontologie; SILVA IP, 2002, INT SCH PLANKT FOR 1; Stampfli G.M., 2002, J VIRTUAL EXPLORER, V7, P75, DOI DOI 10.1016/S0012-821X; TESTOLIN R, 1992, ACTA HORTIC, V313, P99, DOI 10.17660/ActaHortic.1992.313.11; WILLIAMS GL, 2004, P ODP SCI RESULTS, V189; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Wortmann UG, 2001, TECTONICS, V20, P134, DOI 10.1029/2000TC900029; Wortmann UG, 2004, EARTH PLANET SC LETT, V220, P69, DOI 10.1016/S0012-821X(04)00031-7	45	13	15	0	5	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2006	27	6					743	753		10.1016/j.cretres.2006.01.002	http://dx.doi.org/10.1016/j.cretres.2006.01.002			11	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	115DC					2025-03-11	WOS:000242714000004
J	Oosting, AM; Leereveld, H; Dickens, GR; Henderson, RA; Brinkhuis, H				Oosting, A. M.; Leereveld, H.; Dickens, G. R.; Henderson, R. A.; Brinkhuis, H.			Correlation of Barremian-Aptian (mid-Cretaceous) dinoflagellate cyst assemblages between the Tethyan and Austral realms	CRETACEOUS RESEARCH			English	Article						Middle Cretaceous; Barremian; Aptian; palynology; organic-walled dinoflagellate cysts; carbon isotopes; OAE; Australia	APTICORE SOUTHERN ALPS; STRATIGRAPHY; SEDIMENTS; CARBON; SECTION; RECORD; NORTH; OCEAN	Quantified organic-walled dinoflagellate cyst (dinocyst) assemblages are presented for two sedimentary successions deposited in neritic environments of the Tethys Ocean during the Barremian and Aptian in an attempt to reconcile established dinocyst biostratigraphic schemes for Tethyan and Austral regions. One section is at Angles, southeast France (the Barremian stratotype section); the other is at Deep Sea Drilling Project Site 263, Off northwest Australia. We also construct a carbon isotope record for Site 263 Using bulk organic carbon. Both sections contain abundant, well-preserved dinocyst assemblages. These are diverse, with 89 taxa identified at Angles and 103 taxa identified at Site 263. Of these, more than 93% are cosmopolitan. When combined with other work at Angles and Site 263, we found that nine dinocysts have their first occurrence (FO) or last occurrence (LO) at both locations. These dinocyst events are, in alphabetical order: LO of Cassiculosphaeridia magna, FO of Criboperidinium? tenuiceras, LO of Kleithriaphaeridium fasciatum, LO of Muderongia staurota, FO of Odontochitina operculata, LO of Phoberocysta neocomica, FO of Prolixosphaeridium parvispinum, FO of Pseudoceratium retusum var. securigerum, and FO of Tehamadinium sousense. Although these events support a Barrermian-Aptian age for both sections, their stratigraphic order is not the same in the sections. The delta C-13(org) record at Site 263 displays a characteristic series of changes that have also been recorded in other carbon isotope curves spanning the Late Barremian-Early Aptian. Such independent dating (along with ammonite zones at Angles) suggests that three of the nine dinocyst events are approximately isochronous at Angles and Site 263: the LO of K. fasciatum in the mid Barremian, the FO of P. retusum var. securigerum and the FO of C.? tenuiceras in the earliest Aptian; the other six dinocyst events are diachronous. Dinocyst assemblages at Site 263 can be loosely placed within existing Australian zonation schemes, providing much-needed calibration. Our data suggest that the Muderongia testudinaria Zone ends in sediments of mid Barremian age, the succeeding Muderongia australis Zone extends into the Early Aptian, and the younger Odontochitina operculata Zone begins in Early Aptian deposits. The boundary between the M. australis and O. operculata zones, and the Ovoidinium cinctum (as Ascodinium) Subzone, positioned at the top of the M. australis Zone when present, could not be recognized incontrovertibly. Interestingly, however, this horizon broadly correlates with the onset and extent of the Selli Event, a time of major biogeochemical change. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; James Cook Univ N Queensland, Sch Earth Sci, Townsville, Qld 4811, Australia	Utrecht University; James Cook University	Oosting, AM (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Buchapestlaan, NL-3584 CD Utrecht, Netherlands.	oostinga@rpsgroup.com	Dickens, Gerald/G-1222-2011; Brinkhuis, Henk/B-4223-2009	Dickens, Gerald/0000-0003-2869-4860; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], MEMOIRS; BACKHOUSE J., 1988, BULLETIN, V135, P1; BIRKELUND T, 1984, Bulletin of the Geological Society of Denmark, V33, P3; Bralower RJ, 1999, J FORAMIN RES, V29, P418; BREHERET JG, 1994, SP PUB EAPG, P295; Brenner W., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P511, DOI 10.2973/odp.proc.sr.122.158.1992; Busnardo R., 1965, Mem Bur Rech Geol Minier, V34, P101; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; CROUCH EM, 2003, PALAEOGEOGR PALAEOCL, V107, P121; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; de Gea GA, 2003, PALAEOGEOGR PALAEOCL, V200, P207, DOI 10.1016/S0031-0182(03)00451-6; Decima F.P., 1974, Initial Rep Deep Sea Drilling Project, V27, P589; DELANOY G, 1997, SCI TERRE PLANETES, V325, P689; Delanoy Gerard, 1995, Memorie Descrittive della Carta Geologica d'Italia, V51, P65; Dickens GR, 2000, B SOC GEOL FR, V171, P37; DUCHENE RJ, 1986, CAHIERS MICROPALEONT, P5; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Erba E, 1999, J FORAMIN RES, V29, P371; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Gradstein FM, 2004, EPISODES, V27, P83, DOI 10.18814/epiiugs/2004/v27i2/002; Gröcke DR, 1999, GEOLOGY, V27, P155, DOI 10.1130/0091-7613(1999)027<0155:CICOLC>2.3.CO;2; Habib D., 1987, Initial Reports of the Deep Sea Drilling Project, V93, P751; HARDENBOL J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European basins, V60, P1, DOI DOI 10.2110/PEC.98.02; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Hay W.W., 1999, Evolution of the Cretaceous Ocean-Climate System. 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Res.	DEC	2006	27	6					792	813		10.1016/j.cretres.2006.03.012	http://dx.doi.org/10.1016/j.cretres.2006.03.012			22	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	115DC					2025-03-11	WOS:000242714000009
J	Ghasemi-Nejad, E; Hobbi, MH; Schioler, P				Ghasemi-Nejad, Ebrahim; Hobbi, Mohammad Hadi; Schioler, Paul			Dinoflagellate and foraminiferal biostratigraphy of the Gurpi Formation (upper Santonian-upper Maastrichtian), Zagros Mountains, Iran	CRETACEOUS RESEARCH			English	Article						Upper Cretaceous; Paleocene; dinoflagellate cysts; Zagros Mountains; Iran	PALYNOFACIES; CARBONATES; PIRIPAUAN; SEDIMENTS; NORTH; FIELD	A rich dinoflagellate cyst assemblage has been recovered from an outcrop of the Gurpi Formation, the hydrocarbon source rock in the South Iranian Basin. Key dinoflagellates recorded in the section studied provide a means of correlation with zonation schemes for Australasia and north-west Europe. These include Eucladinium kaikourense, Nelsoniella aceras, Odontochitina spp., Cannosphaeropsis itinensis, Palaeocystodinium denticulatum and Dinogymnium spp. The assemblage points to a late Santonian-late Maastrichtian age for the Gurpi Formation. Dinoflagellate and planktonic foraminiferal evidence indicates the presence of a hiatus spanning the uppermost Maastrichtian to at least the lowermost Danian at the base of a glaucony-rich layer separating the Gurpi Formation from the overlying Pabdeh Formation. Palynofacies and lithofacies profiles suggest that the sediments were deposited in an open, relatively deep marine outer ramp environment belonging to ramp facies 8 and 9. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran; Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark	University of Tehran; Geological Survey Of Denmark & Greenland	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Dept Geol, Fac Sci, Tehran, Iran.	eghasemi@khayam.ut.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068				Ala M. A., 1980, Journal of Petroleum Geology, V3, P61; [Anonymous], DANMARKS GEOLOGISK A; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 2007, Paleopalynology; Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Caron M., 1985, P17; Crampton J, 2000, NEW ZEAL J GEOL GEOP, V43, P309, DOI 10.1080/00288306.2000.9514890; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; GHASEMINEJAD E, 1999, SCHWEIZERISCHE PALAE, V119; GORIN GE, 1991, PALAEOGEOGR PALAEOCL, V85, P303, DOI 10.1016/0031-0182(91)90164-M; HUBER BT, 1992, PALAEOGEOGR PALAEOCL, V92, P325, DOI 10.1016/0031-0182(92)90090-R; James G.A., 1965, American Association of Petroleum Geologists Bulletin, V49, P2182, DOI DOI 10.1306/A663388A-16C0-11D7-8645000102C1865D; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; MOTIEI H, 2003, GEOLOGICAL SURVEY IR, V84; Olsson R.K., 1999, Smithsonian Contributions to Paleobiology, V85, P1, DOI [10.5479/si.00810266.85.1, DOI 10.5479/SI.00810266.85.1]; Pedley H.M., 1998, GEOL SOC SPEC PUBL, V149, P163; Powell A.J., 1992, P155; Robaszynski F, 1995, B SOC GEOL FR, V166, P681; Roncaglia L, 1997, REV PALAEOBOT PALYNO, V97, P177, DOI 10.1016/S0034-6667(96)00070-X; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; SAMPO M., 1969, INT SEDIMENTARY PETR, V12; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; SCHIOLER P, 1993, REV PALAEOBOT PALYNO, V78, P321, DOI 10.1016/0034-6667(93)90070-B; Setudehnia A., 1978, Journal of Petroleum Geology, V1, P3; STEFFEN D, 1993, B CENT RECH EXPL, V17, P235; TESTOLIN R, 1992, ACTA HORTIC, V313, P99, DOI 10.17660/ActaHortic.1992.313.11; Tyson R.V., 1987, Marine petroleum source rocks, V26, P47, DOI 10.1144/GSL.SP.1987.026.01.03; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; VANDERZWAN CJ, 1990, REV PALAEOBOT PALYNO, V62, P157, DOI 10.1016/0034-6667(90)90021-A; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; WRIGHT VP, 1998, GEOLOGICAL SOC LONDO, V149, P163; ZAHIRI AH, 1982, TECHNICAL NOTES NATL, V226	36	35	35	0	3	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2006	27	6					828	835		10.1016/j.cretres.2006.03.013	http://dx.doi.org/10.1016/j.cretres.2006.03.013			8	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	115DC					2025-03-11	WOS:000242714000011
J	Prauss, ML				Prauss, Michael L.			The Cenomanian/Turonian Boundary Event (CTBE) at Wunstorf, north-west Germany, as reflected by marine palynology	CRETACEOUS RESEARCH			English	Article						Cenomanian/Turonian Boundary Event; marine palynology; dinoflagellate cysts; prasinophytes; water masses; palaeoceanography; North-West Germany	SEA-LEVEL CHANGES; DINOFLAGELLATE CYSTS; TURONIAN BOUNDARY; ANOXIC EVENT; CALCAREOUS NANNOFOSSIL; VOCONTIAN BASIN; ADJACENT SEAS; PLENUS MARLS; STRATIGRAPHY; ENGLAND	The Cenomanian/Turonian Boundary Event (CTBE) at Wunstorf, north-west Germany, has been analysed palynologically by high resolution sampling to reconstruct changes in relative sea-level and water mass character within photic zone waters. Based on changes in the ratio of terrigenous sporomorphs to marine palynomorphs (t/m index), the distribution of the organic-walled algal taxa as well as of selected dinocyst taxa and groups the section can largely be subdivided into pre-"plenus-bed" and post-"plenus-bed" intervals, reflecting different stages of third-order relative sea-level cycles and/or changes in water mass influence in the photic zone. Accordingly, the pre-"plenus-bed" interval is placed in a transgressive systems tract starting at the "facies change" event (C. guerangerilM. geslinianum ammonite Zone boundary) with the maximum flooding surface at the top of the "Chondrites II" bed (top of R. cushmani Biozone). A highstand systems tract is suggested from the base of the "plenus-bed" up the base of the "fish-shale" event. Within the "fish-shale" event interval, a transgressive systems tract is suggested to start at the base of the thin, grey-green marly interbed. The Cenomanian/Turonian boundary proper, as defined by the first occurrence of Mytiloidcs spp., as well as the lowermost Turomian are located within the initial phase of a transgressive systems tract. With respect to water mass characteristics within photic-zone waters, the pre-"plenus-bed" interval is predominantly characterized by warm water masses that changed gradually towards the deposition of the "Chondrites II" bed, where a strong influence of cool and/or salinity-reduced waters is indicated by various palynological proxies. Within the post- "plenus-bed" interval a mixture and/or alternation of warmer and cooler waters is indicated, with the warmer water influence increasing gradually towards and within the Lower Turonian stage. The increased proportions of prasinophytes within the "Chondrites II" bed and parts of the "fish-shale" interval may indicate availability of reduced nitrogen chemospecies, especially ammonium, within photic-zone waters as a function of a vertical expansion of the oceanic O-2-minimum zone. (c) 2006 Elsevier Ltd. All rights reserved.	Free Univ Berlin, Sect Paleontol, Inst Geosci, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Free Univ Berlin, Sect Paleontol, Inst Geosci, Malteser Str 74-100, D-12249 Berlin, Germany.	mprauss@zedat.fu-berlin.de						ALAMERI TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103, DOI 10.1016/0031-0182(83)90007-X; [Anonymous], 1965, Southeastern Geology; [Anonymous], 1988, Am Assoc Petrol Geol Mem; [Anonymous], MATH THEORY COMMUNIC; [Anonymous], 1980, PALEOBIOLOGY PLANT P; [Anonymous], 1985, SPOROPOLLENIN DINOFL; ARTHUR MA, 1988, NATURE, V335, P714, DOI 10.1038/335714a0; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Carey S.W., 1961, GEOL ARCTIC, V2, P865, DOI DOI 10.3138/J.CTVFRXK58.12; Clarke R. F. 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J., 1998, BOCHUMER GEOLOGISCHE, V48, P62; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	82	45	49	0	8	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2006	27	6					872	886		10.1016/j.cretres.2006.04.004	http://dx.doi.org/10.1016/j.cretres.2006.04.004			15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	115DC					2025-03-11	WOS:000242714000015
J	Willumsen, PS				Willumsen, Pi Suhr			<i>Palynodinium minus</i> sp nov., a new dinoflagellate cyst from the Cretaceous-Paleogene transition in New Zealand;: its significance and palaeoecology	CRETACEOUS RESEARCH			English	Article						Cretaceous-Paleogene transition; New Zealand; dinoflagellate cysts; Palynodinium; biostratigraphy; palaeoenvironment	MID-WAIPARA RIVER; TERTIARY BOUNDARY; NORTH CANTERBURY; SECTION; BIOSTRATIGRAPHY; PALYNOLOGY	This is the first record of a representative of the organic-walled dinoflagellate cyst genus Palynodinium from the New Zealand region. Previously, Palynodinium grallator has been reported from two sites in offshore Tasmania during Ocean Drilling Program, Leg 189. The new species Palynodinium minus is found consistently in latest Maastrichtian? and earliest Danian strata (latest Haumurian-earliest Teurian) in two sections located along the mid-Waipara and Grey rivers, North Canterbury, South Island. It occurs in a narrow stratigraphic interval at the Cretaceous-Paleogene transition and is potentially a stratigraphically important index species in the region. Its range coincides with that of the global earliest Danian index fossil Carpatella cornuta and a basal Danian acme interval of Trithyrodinium evittii, and is correlated to ca. 65.5-65.2 Ma. Its highest occurrence is at the base of an acme interval of Palaeoperidinium pyrophorum. It has only been recorded from sections composed of siliciclastic shelf sediments, suggesting that it might have had a palaeoecological preference for relatively near-shore environments. (c) 2006 Elsevier Ltd. All rights reserved.	Victoria Univ Wellington, Dept Earth Sci, Wellington, New Zealand	Victoria University Wellington	Willumsen, PS (通讯作者)，Univ Oslo, Dept Geosci, POB 1047, NO-0316 Oslo, Norway.	pi.willumsen@geo.uio.no						[Anonymous], 1989, NZ GEOL SURV REC; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], P 2 PLANKT C ROM 197; [Anonymous], THESIS VICTORIA U WE; [Anonymous], NZ GEOLOGICAL SURVEY; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Benson D.G. Jr., 1976, Tulane Stud Geol Paleont, V12, P169; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BRINKHUIS H, 1998, MEDEDELINGEN NEDERLA, V61, P12; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; BROOKS RR, 1986, NEW ZEAL J GEOL GEOP, V29, P1; Brown G. 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Surv. Rec, V20, P8; WILSON GJ, 1982, UNPUB NZ GEOLOGICAL; Wilson GJ., 1974, THESIS U NOTTINGHAM	66	23	25	0	6	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2006	27	6					954	963		10.1016/j.cretres.2006.06.002	http://dx.doi.org/10.1016/j.cretres.2006.06.002			10	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	115DC					2025-03-11	WOS:000242714000021
J	Persson, A; Smith, BC; Wikfors, GH; Quilliam, M				Persson, Agneta; Smith, Barry C.; Wikfors, Gary H.; Quilliam, Michael			Grazing on toxic <i>Alexandrium fundyense</i> resting cysts and vegetative cells by the eastern oyster (<i>Crassostrea virginica</i>)	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Crassostrea virginica; cyst; dinoflagellate; grazing; oyster; PSP; toxic	DINOFLAGELLATE GONYAULAX-TAMARENSIS	In laboratory experiments, oysters (Crassostrea virginica) were fed Alexandrium fundyense (strain C13501) vegetative cells or resting cysts (from strains CB501 and GMT25) produced from laboratory cultures. The toxicity per cyst was 1.7 pg STXequiv/cyst and for vegetative cells 3.9 pg STXequiv/cell. The toxic, resting cysts and vegetative cells were removed from suspension in the experimental containers within about 4 It. Oysters fed toxic vegetative cells digested 72% of cells ingested, and 28% survived gut passage by forming temporary cysts. Toxin levels of oysters fed vegetative cells averaged 27 mu g STXequiv/100 g meat. Resting cysts added to the experimental containers adhered to the walls so that only 40% of the cysts added were available to the oysters during the experiment. Of the cysts that were ingested, approximately 59% were digested, and oysters accumulated toxins (an average of 1.2 mu g STXequiv/100 g meat), showing that consumption of resting cysts can cause toxicity in oysters. Direct consumption of resting cysts, thus, may explain shellfish toxicity in areas without known blooms, but with toxic resting cysts in the sediment. These results suggest a possible role of toxic cysts in mediating time-lags between surface blooms and appearance of toxicity in benthic grazers, and the possible role of benthic grazers in controlling seed populations, except in anoxic areas, which can serve as cyst "refuges" from grazing mortality. (c) 2006 Elsevier B.V. All rights reserved.	NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA; Natl Res Council Canada, Inst Marine Biosci, Halifax, NS B3H 3Z1, Canada	National Oceanic Atmospheric Admin (NOAA) - USA; National Research Council Canada; International Business Machines (IBM); IBM Canada	Smith, BC (通讯作者)，NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT 06460 USA.	agnetapersson77@telia.com; barry.smith@noaa.gov; gary.wikfors@noaa.gov; Michael.Quilliam@nrc-cnrc.gc.ca		Quilliam, Michael/0000-0002-2670-4220; Persson, Agneta/0000-0003-0202-6514				Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BARDOUIL M, 1993, J SHELLFISH RES, V12, P417; BLOGOSLAWSKI W J, 1988, Journal of Shellfish Research, V7, P702; BOLCH CJ, 2001, LIFEHAB LIFE HIST MI, P37; BRAVO I, 1998, HARMFUL ALGAE, P356; Bricelj V. Monica, 1998, Reviews in Fisheries Science, V6, P315, DOI 10.1080/10641269891314294; BRICELJ VM, 1993, DEV MAR BIO, V3, P371; Carreto J.I., 1998, HARMFUL ALGAE, P131; CEMBELLA AD, 1990, TOXIC MARINE PHYTOPLANKTON, P333; DENN EE, 1993, TOXIC PHYTOPLANKTON, P109; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Harper FM, 2002, J SHELLFISH RES, V21, P471; Hurst J.W., 1985, P427; KENNEDY VS, 1996, E OYSTER CRASSOSTREA, P237; Laabir M, 1999, J SHELLFISH RES, V18, P217; LAROCQUE R, 1990, TOXIC MARINE PHYTOPLANKTON, P368; LIRDWITAYAPRASIT T, 1990, TOXIC MARINE PHYTOPLANKTON, P294; Martin J.L., 1998, HARMFUL ALGAE, P233; OSHIMA Y, 1992, TOXICON, V30, P1539, DOI 10.1016/0041-0101(92)90025-Z; Oshima Y., 1995, MANUAL HARMFUL MARIN, P81; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; SCHWINGHAMER P, 1994, AQUACULTURE, V122, P171, DOI 10.1016/0044-8486(94)90508-8; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53; Tsujino M, 2004, J EXP MAR BIOL ECOL, V303, P1, DOI 10.1016/j.jembe.2003.10.018; TURGEON J, 1990, TOXIC MARINE PHYTOPLANKTON, P238; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Yentsch C.M., 1979, P127	31	45	51	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	DEC	2006	5	6					678	684		10.1016/j.hal.2006.02.004	http://dx.doi.org/10.1016/j.hal.2006.02.004			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	109IM					2025-03-11	WOS:000242301400006
J	Aligizaki, K; Nikolaidis, G				Aligizaki, Katerina; Nikolaidis, Georgios			The presence of the potentially toxic genera <i>Ostreopsis</i> and <i>Coolia</i> (Dinophyceae) in the north Aegean sea, Greece	HARMFUL ALGAE			English	Article						dinoflagellates; Coolia; east Mediterranean; harmful algae; North Aegean Sea; Ostreopsis	SP-NOV DINOPHYCEAE; DINOFLAGELLATES DINOPHYCEAE; MONOTIS DINOPHYCEAE; OVATA DINOPHYCEAE; PALYTOXIN ANALOGS; LIFE-HISTORY; CIGUATERA; TEMPERATURE; MORPHOLOGY; GROWTH	The examination of macrophyte, water and sediment samples, collected at depths less than 1.5 m from 50 different sites along the North Aegean coasts, has revealed, for the first time in Greek coastal waters, the presence of two Ostreopsis species (O. ovata and O. cf. siamensis) and Coolia monotis in the majority of the sampling sites (94% and 100%, respectively). Other epiphytic dinoflagellates of the genera Prorocentrum and Amphidinium and diatoms were accompanying species in this epiphytic community. Morphometric features, plate formula and thecal ornamentation were used for species identification. O. ovata cells were smaller in dorsoventral (DV) diameter and width (W) (26.18-61.88 mu m and 13.09-47.60 mu m, respectively) in comparison with O. cf. siamensis (35.70-65.45 mu m and 23.80-49.98 mu m, respectively). In contrast, the anterioposterior (AP) diameter of O. cf. siamensis was smaller (14.28-26.18 mu m) resulting in DV/AP approximate to 3, whereas the above ratio for O. ovata was less than 2 (AP ranging between 14.28-35.70 mu m). Moreover, the theca of O. ovata cells was ornamented with scattered pores, which fluctuated in a wider range (0.07-0.32 mu m) than those of O. cf. siamensis (0.23-0.29 mu m). Coolia monotis cells were almost round with average DV diameter 26.88 mu m, AP 25.66 mu m and width 26.76 mu m. Small and large cells were recorded in both field and culture populations of Ostreopsis spp. and C. monotis, while hyaline cysts were observed for O. ovata. The presence of O. ovata and O. cf. siamensis exhibited a clear seasonal pattern dominating (maximum abundance up to 4.05 x 10(5) cells gr(-1) fwm) the period from midsummer to late autumn in years 2003 and 2004, while C. monotis was found also in winter and spring months. (c) 2006 Elsevier B.V. All rights reserved.	Aristotle Univ Thessaloniki, Sch Biol, Dept Bot, GR-54124 Thessaloniki, Greece	Aristotle University of Thessaloniki	Nikolaidis, G (通讯作者)，Aristotle Univ Thessaloniki, Sch Biol, Dept Bot, POB 109, GR-54124 Thessaloniki, Greece.	nikola@bio.auth.gr						[Anonymous], HARMFUL ALGAL BLOOMS; [Anonymous], 2003, Biol Ambient, DOI DOI 10.1021/AC060250J; Bagnis R., 1985, P177; Balech E., 1956, Rev. 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J	Navarro, JM; Muñoz, MG; Contreras, AM				Navarro, J. M.; Munoz, M. G.; Contreras, A. M.			Temperature as a factor regulating growth and toxin content in the dinofiagellate <i>Alexandrium catenella</i>	HARMFUL ALGAE			English	Article						Alexandrium catenella; dinoflagellate; temperature; growth rates; toxin content; PSP; HABs	CYST FORMATION; DINOFLAGELLATE; DINOPHYCEAE; POPULATION; TAMARENSE	Controlled laboratory culture of Alexandrium catenella was used to determine the effects of a range of temperatures between 10 and 16 degrees C on the growth and saxitoxin content of this dinoflagellate, using strain ACC02 isolated from seawater at Aysen, XI Region, Southern Chile. Cell cultures were made using L1 culture medium at 30 parts per thousand salinity, and a photon flux density of 59.53 mu mol m(2) s(-1). The results showed that the duration of the exponential growth phase was determined by the experimental temperature, with maximum cell concentrations obtained at 12 degrees C; significantly lower cell concentrations and growth rates were obtained at 16 degrees C. Cell dry weight and chlorophyll a values followed cell growth trends. The toxicity of A. catenella was variable at all the experimental temperatures, with a tendency towards having an inverse relation to temperature, with the highest values occurring at 10 degrees C and the lowest at 16 degrees C. The optimal range of temperature for the growth of the Chilean strain of A. catenella differed from rates reported for this species isolated at other latitudes, and was correlated with natural temperature conditions predominant in the environment from which it was isolated. The inverse relation of toxicity with temperature in the laboratory was broadly reflected in observations on the toxicity of this dinoflagellate in the field, and coincided with results from the literature. (c) 2006 Elsevier B.V. All rights reserved.	Univ Austral Chile, Inst Biol Marina Dr Jurgen Winter, Valdivia, Chile	Universidad Austral de Chile	Navarro, JM (通讯作者)，Univ Austral Chile, Inst Biol Marina Dr Jurgen Winter, Casilla 567, Valdivia, Chile.	jnavarro@uach.cl	Navarro, Jorge M./B-7928-2008	Navarro, Jorge M./0000-0001-9920-190X				ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1993, HDB PHYCOLOGICAL MET; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; CLEMENT A, 2002, ANAL MAREA ROJA ARCH; Falkowski P.G., 1980, Primary Productivity in the Sea, P99, DOI DOI 10.1357/002224083788520199; Falkowski P.G., 1997, AQUATIC PHOTOSYNTHES, P375; GAVIN K, 1997, HYDROBIOLOGIA, V352, P117; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Ichimi K, 2002, J EXP MAR BIOL ECOL, V273, P51, DOI 10.1016/S0022-0981(02)00137-5; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Juhl AR, 2005, HARMFUL ALGAE, V4, P287, DOI 10.1016/j.hal.2004.05.003; Lim PT, 2005, TOXICON, V45, P699, DOI 10.1016/j.toxicon.2005.01.007; MacKenzie L, 2004, HARMFUL ALGAE, V3, P71, DOI 10.1016/j.hal.2003.09.001; Matsuda A., 1996, Harmful and Toxic Algal Blooms, P305; Molinet C, 2003, REV CHIL HIST NAT, V76, P681; Navarro Jorge M., 1994, Revista de Biologia Marina, V29, P57; Parker NS, 2002, J APPL PHYCOL, V14, P313, DOI 10.1023/A:1022170330857; RAMUS J, 1990, HYDROBIOLOGIA, V204, P65, DOI 10.1007/BF00040216; Reguera B., 2002, Floraciones Algales Nocivas en el Cono Sur Americano, P21; SECHET V, 2003, MOLLUSCAN SHELFISH S; Siu GKY, 1997, HYDROBIOLOGIA, V352, P117, DOI 10.1023/A:1003042431985; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Vélez P, 2001, TOXICON, V39, P929, DOI 10.1016/S0041-0101(00)00230-0; YENTSCH CS, 1963, DEEP-SEA RES, V10, P221, DOI 10.1016/0011-7471(63)90358-9; Zar J.H, 1999, BIOSTAT ANAL, V4th	27	92	102	5	33	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	DEC	2006	5	6					762	769		10.1016/j.hal.2006.04.001	http://dx.doi.org/10.1016/j.hal.2006.04.001			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	109IM					2025-03-11	WOS:000242301400014
J	Koike, K; Nishiyama, A; Saitoh, K; Imai, K; Koike, K; Kobiyama, A; Ogata, T				Koike, Kazuhiko; Nishiyama, Asami; Saitoh, Kazuya; Imai, Keisuke; Koike, Kanae; Kobiyama, Atsushi; Ogata, Takehiko			Mechanism of gamete fusion in <i>Dinophysis fortii</i> (Dinophyceae, Dinophyta):: Light microscopic and ultrastructural observations	JOURNAL OF PHYCOLOGY			English	Article						cell fusion; Dinophysis fortii; life cycle; TEM; ultrastructure	SEXUAL REPRODUCTION; LIFE-CYCLE; SEDIMENTS; CYSTS	A variety of studies have examined the sexual life cycle of species belonging to the genus Dinophysis Ehrenberg. Here, we used TEM to investigate the mechanism of cellular fusion during the sexual life cycle in Dinophysis fortii Pavillard. We observed that fusion always occurred between a normal-sized cell and a small cell following attachment of their ventral margins. After cell attachment, the small cell moved toward the epitheca of the normal-sized cell, and the cingular and sulcal lists of the small cell shrunk or were almost lost. The epitheca of the normal-sized cell then opened between the cingulum plates and the upper cingular list, after which the small cell was gradually engulfed. This is the first ultrastructural observation in a dinoflagellate of a larger cell opening its epitheca to engulf the smaller gamete. In another case, the normal-sized cell did not open the epitheca, the cell wall of the attached small cell underwent extensive extracellular digestion, and the cytoplasm appeared to flow into the normal-sized cell via the periflagellar area. Inflow of the nucleus was not observed in this case, suggesting that it represented a failure of sexual fusion. In both cases, membranous separations between the cytoplasm of the two cells were not observed. At the beginning of the fusion process, the nucleus of the small cell was substantially deformed. The plano-zygote, formed upon completion of sexual fusion, sometimes had two longitudinal flagella, but was identical to a normal vegetative cell in its cellular shape, as already mentioned by previous authors.	Kitasato Univ, Sch Fisheries Sci, Ofunato, Iwate 0220101, Japan	Kitasato University	Koike, K (通讯作者)，Kitasato Univ, Sch Fisheries Sci, Ofunato, Iwate 0220101, Japan.	k.koike@kitasato-u.ac.jp	Koike, Kazuhiko/A-3392-2019	Kazuhiko, Koike/0000-0001-5380-5839				BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Delgado M., 1996, HARMFUL TOXIC ALGAL, P261; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Giacobbe MG, 1997, J PHYCOL, V33, P73, DOI 10.1111/j.0022-3646.1997.00073.x; IWASAKI H, 1961, BIOL BULL-US, V121, P173, DOI 10.2307/1539469; JACOBSON DM, 1994, PHYCOLOGIA, V33, P97, DOI 10.2216/i0031-8884-33-2-97.1; Jorgensen E., 1923, REP DAN OCEANOGR EXP, V2, P1; Koike K, 2005, PROTIST, V156, P225, DOI 10.1016/j.protis.2005.04.002; Koike Kazuhiko, 2000, Phycological Research, V48, P121, DOI 10.1111/j.1440-1835.2000.tb00206.x; LARRAZABAL ME, 1990, CRYPTOGAMIE ALGOL, V11, P171; MACKENZIE L, 1992, J PHYCOL, V28, P399, DOI 10.1111/j.0022-3646.1992.00399.x; MCLACHLAN JL, 1993, DEV MAR BIO, V3, P143; MOITA MT, 1993, DEV MAR BIO, V3, P153; Pfiester L.A., 1984, P181; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; RAO DVS, 1995, AQUAT MICROB ECOL, V9, P199, DOI 10.3354/ame009199; REGUERA B, 1995, J PLANKTON RES, V17, P999, DOI 10.1093/plankt/17.5.999; Reguera B, 2003, MAR ECOL PROG SER, V249, P117, DOI 10.3354/meps249117; Reguera B, 2001, J PHYCOL, V37, P318, DOI 10.1046/j.1529-8817.2001.037002318.x; Reguera B, 1990, DISTRIBUTION DINOPHY, V14; SOURNIA A., 1986, ATLAS PHYTOPLANCTON, VI; Stosch H.A., 1964, Helgolander Wissenschaftliche Meeresuntersuchungen, V10, P140; Uchida Takuji, 1999, Bulletin of Fisheries and Environment of Inland Sea, V1, P163; von Stosch H.A., 1965, NATURWISSENSCHAFTEN, V52, P112; Von Stosch HA., 1973, Br Phycol J, V8, P105	27	13	15	0	8	WILEY-BLACKWELL	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	DEC	2006	42	6					1247	1256		10.1111/j.1529-8817.2006.00288.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00288.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	116WR					2025-03-11	WOS:000242835000011
J	Palliani, RB; Buratti, N				Palliani, Raffaella Bucefalo; Buratti, Nicoletta			High diversity dinoflagellate cyst assemblages from the Late Triassic of southern England: new information on early dinoflagellate evolution and palaeogeography	LETHAIA			English	Article						dinoflagellate cysts; Late Triassic; palaeogeography	PALYNOLOGY; BASE	Abundant and diverse dinoflagellate cyst assemblages from the Rhaetian of southern England are characterized by the occurrence of a new species of Rhaetogonyaulax, some undescribed taxa and numerous forms with Arctic and Australasian affinities. The dinoflagellate cyst assemblages permit a discussion of the palaeogeographic distribution of dinoflagellate cysts in the Late Triassic. The hypothesis on a Late Triassic migration event of organic walled microplankton from higher latitudes to the Boreal domain is presented.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy	University of Perugia	Palliani, RB (通讯作者)，Univ Perugia, Dept Earth Sci, Piazza Univ 1, I-06100 Perugia, Italy.	Rbucefa@tin.it; stradott@unipg.it						BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; FEISTBURKHARDT S, 2002, IPC 2002 GEOLOGICAL, V68, P208; Felix C.J., 1978, Palinologia, P225; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; FISHER M J, 1979, Palynology, V3, P265; FISHER MJ, 1981, REV PALAEOBOT PALYNO, V34, P129, DOI 10.1016/0034-6667(81)90070-1; FISHER MJ, 1972, MERCIAN GEOLOGIST, V7, P101; Ghasemi-Nejad E, 2004, REV PALAEOBOT PALYNO, V132, P207, DOI 10.1016/j.revpalbo.2004.07.001; HARLAND R, 1975, Palaeontology (Oxford), V18, P847; HELBY R, 1988, NEW ZEAL J BOT, V26, P117, DOI 10.1080/0028825X.1988.10410104; HELBY R, 1987, AUST J EARTH SCI, V34, P151, DOI 10.1080/08120098708729399; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Heunisch Carmen, 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P87; Hochuli PA, 2000, ECLOGAE GEOL HELV, V93, P429; HOCHULI PA, 1998, SEPM SPECIAL PUBLICA, V60, P780; Ivimey-Cook Hugh C., 1999, Palaeontological Association Field Guides to Fossils, V9, P83; Kristan-Tollmann E., 1981, Mitteilungen der Oesterreichischen Geologischen Gesellschaft, V74-75, P129; Lindström S, 2002, REV PALAEOBOT PALYNO, V120, P247, DOI 10.1016/S0034-6667(02)00079-9; MACQUAKER JHS, 1994, ZOOL J LINN SOC-LOND, V112, P285, DOI 10.1006/zjls.1994.1043; Martini R, 2004, PALAEOGEOGR PALAEOCL, V206, P75, DOI 10.1016/j.palaeo.2003.12.020; MAYALL MJ, 1981, GEOL MAG, V118, P377, DOI 10.1017/S0016756800032246; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; Moldowan JM, 1996, GEOLOGY, V24, P159; Morbey J., 1975, Palaeontographica B, V152, P1; Morbey S.J., 1978, CONTINENTAL SHELF I, V100, P47; MORBEY SJ, 1974, REV PALAEOBOT PALYNO, V17, P161, DOI 10.1016/0034-6667(74)90097-9; ORBELL G., 1973, Bulletin of the Geological Survey of Great Britain, V44, P1; OSULLIVAN T, 1985, P IND PETR ASS 14 AN; Powell A.J., 1992, P1; SARJEANT WA, 1963, NATURE, V199, P353, DOI 10.1038/199353a0; SARJEANT WAS, 1966, GEOLOGY S, V3, P107; STORRS GW, 1994, ZOOL J LINN SOC-LOND, V112, P217, DOI 10.1006/zjls.1994.1041; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P101; Warrington G., 1984, Proceedings of the Ussher Society, V6, P100; WARRINGTON G, 1994, GEOL MAG, V131, P191, DOI 10.1017/S0016756800010724; WARRINGTON G, 1985, MEMOIRS BRIT GEOLOGI, P84; WARRINGTON G, 1977, B GEOLOGICAL SURVEY, V57, P40; Warrington G., 1978, V68, P22; WARRINGTON G, 1983, MEMOIR I GEOLOGICAL, V131, P61; WARRINGTON G, 1990, CAHIERS U CATHOLIQUE, V3, P207; WARRINGTON G, 1981, BRIT MICROPALAEONTOL, P61; Warrington G., 1977, P USSHER SOC, V4, P76; WIGGINS V D, 1973, Micropaleontology (New York), V19, P1, DOI 10.2307/1484961; Williams G.L., 1977, Oceanic Micropalaeontology, V2, P1231; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; WOOLLAM R, 1983, I GEOL SCI REP, V83, P1; ZIEGLER PA, 1982, GEOL RUNDSCH, V71, P147	47	13	13	0	2	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0024-1164	1502-3931		LETHAIA	Lethaia	DEC	2006	39	4					305	312		10.1080/00241160600847538	http://dx.doi.org/10.1080/00241160600847538			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	111SE					2025-03-11	WOS:000242474000003
J	Klyuvitkina, TS; Bauch, HA				Klyuvitkina, T. S.; Bauch, H. A.			Hydrological changes in the Laptev Sea during the Holocene inferred from the studies of aquatic palynomorphs	OCEANOLOGY			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; ARCTIC-OCEAN; FRESH-WATER; HISTORY; SEDIMENTS; CLIMATE; ICE	Based on the study of aquatic palynomorph assemblages in two Holocene sediment cores obtained from the eastern Laptev Sea shelf, the main stages in the postglacial transgression are reconstructed for the last 11.3 ky. During that period, the inner shelf of the Laptev Sea ( sea depth of 51 m) was already flooded representing an area of intense freshwater sedimentation in the immediate proximity from the river mouth in the period of 11.3 to 10.3 ky B. P. Approximately 1.0 - 1.5 ky later, the inner shelf ( sea depth of 32 m) was flooded, although it remained under the influence of the river runoff up to 7.4 ky B. P. The period of 10.3 - 7.4 ky B. P. was marked by the dominant dinoflagellate cysts Operculodinium centrocarpum among the aquatic palynomorphs, the appearance of more thermophilic dinoflagellate species, and elevated values of the AH ratio, which indicates an enhanced influx of relatively warm North Atlantic waters to the Laptev Sea shelf. The environment close to the present- day one became dominant on the outer and inner shelf of the Laptev Sea approximately 8.6 and 7.4 ky B. P., respectively.	Moscow MV Lomonosov State Univ, Fac Geog, Moscow, Russia; Mainz Acad Sci Humanities & Literature, Kiel, Germany	Lomonosov Moscow State University	Klyuvitkina, TS (通讯作者)，Moscow MV Lomonosov State Univ, Fac Geog, Moscow, Russia.	t.klyuvitkina@mail.ru	Klyuvitkina, Tatyana/L-8843-2015					AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; [Anonymous], 1999, LAND OCEAN SYSTEM SI; [Anonymous], 1999, LAND OCEAN SYSTEMS S; [Anonymous], EARTHS CRYOSPHERE; BARSS MS, 1973, PALYNOLOGY NANOFOSSI; Bauch HA, 2001, GLOBAL PLANET CHANGE, V31, P125, DOI 10.1016/S0921-8181(01)00116-3; Bauch HA, 1999, BOREAS, V28, P194, DOI 10.1111/j.1502-3885.1999.tb00214.x; BAUCH HA, 2003, PALEOOCEANOGRAPHY, V2, P1; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Cremer H, 1998, BERICHTE POLARFORSCH, V260, P1; DALE B, 1996, PRINCIPALS APPL NEW, P1149; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Dmitrenko I.A., 1999, P 15 INT C PORT OC E, V1, P311; Dobrovol'skii A.D., 1982, The USSR Seas; Gordeev VV, 1996, AM J SCI, V296, P664, DOI 10.2475/ajs.296.6.664; Gordeev VV, 2000, NATO SCI S PRT 2 ENV, V70, P297; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; GUKOV AY, 1999, ECOSYSTEM SIBERIAN P; Holmes M.L., 1974, MARINE GEOLOGY OCEAN, P211, DOI DOI 10.1007/978-3-642-87411-6_9; HOLMES ML, 1967, THESIS U WASHINGTON; Ivanov V, 1999, Land-Ocean Systems in the Siberian Arctic, P239, DOI DOI 10.1007/978-3-642-60134-7_22; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Kassens H., 1998, EOS T AM GEOPHYS UN, V79, P317, DOI [10.1029/98EO00234, DOI 10.1029/98EO00234]; Kleiber HP, 2001, GLOBAL PLANET CHANGE, V31, P105, DOI 10.1016/S0921-8181(01)00115-1; KLYUVITKINA TS, 2003, GEOLOGY SEAS OCEANS, V1, P98; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; LISITZIN AP, 1994, OKEANOLOGIYA+, V34, P735; MacDonald GM, 2000, QUATERNARY RES, V53, P302, DOI 10.1006/qres.1999.2123; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie PJ, 2001, J QUATERNARY SCI, V16, P595, DOI 10.1002/jqs.660; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; Mueller-Lupp T, 2000, INT J EARTH SCI, V89, P563, DOI 10.1007/s005310000128; Okolodkov Yu B, 2000, THESIS ST PETERSBURG; Pavlidis Yu.A., 1992, SHELF WORLD OCEAN LA; Pfirman SL, 1997, J GEOPHYS RES-OCEANS, V102, P12575, DOI 10.1029/96JC03980; Pisaric MFJ, 2001, QUATERNARY SCI REV, V20, P235, DOI 10.1016/S0277-3791(00)00120-7; Polyakova YI, 2005, GLOBAL PLANET CHANGE, V48, P208, DOI 10.1016/j.gloplacha.2004.12.014; POLYAKOVA YI, 2000, DOKL EARTH SCI, V2, P315; POLYAKOVA YI, 1999, TERRA NOSTRA, P11; Proshutinsky AY, 1997, J GEOPHYS RES-OCEANS, V102, P12493, DOI 10.1029/97JC00738; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; ROMANOVSKII NN, 2001, POLARFORSCHUNG, P237; SEMENOV YI, 1971, MAR GEOL, P42; Sher AV, 2005, QUATERNARY SCI REV, V24, P533, DOI 10.1016/j.quascirev.2004.09.007; STEPANOVA AY, 2004, THESIS MOSCOW; Stockmarr J., 1971, POLLEN SPORES, V13, P616; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Svendsen JI, 2004, QUATERNARY SCI REV, V23, P1229, DOI 10.1016/j.quascirev.2003.12.008; Timokhov L.A., 1994, REPORTS POLAR RES, P15; ZAKHAROV VF, 1996, ARCTIC ICE CLIMATIC; ZAKHAROV VF, 1966, OKEANOLOGIYA, V6, P1014; ZAKHAROV VF, 1981, ARCTIC ICE PRESENT D	56	8	10	0	1	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370	1531-8508		OCEANOLOGY+	Oceanology	DEC	2006	46	6					859	868		10.1134/S0001437006060117	http://dx.doi.org/10.1134/S0001437006060117			10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	156MJ					2025-03-11	WOS:000245652500011
J	Genovesi-Giunti, B; Laabir, M; Vaquer, A				Genovesi-Giunti, B.; Laabir, M.; Vaquer, A.			The benthic resting cyst: A key actor in harmful dinoflagellate blooms - A review	VIE ET MILIEU-LIFE AND ENVIRONMENT			English	Review						seeding; bioturbation; maturation; distribution mode; density; sediment; germination; recruitment; suspended cyst; geographic strain	ALEXANDRIUM-TAMARENSE DINOPHYCEAE; GONYAULAX-TAMARENSIS; SURFACE SEDIMENTS; ALGAL BLOOMS; TOXIC DINOFLAGELLATE; ENVIRONMENTAL-FACTORS; SCRIPPSIELLA-HANGOEI; MARINE-SEDIMENTS; LIFE-HISTORY; INLAND SEA	Resting cysts (RC) constitute a coupling between benthic and pelagic stages and influence the bloom development in a number of bloom forming dinoflagellate species. Encystment capability coupled with high vegetative cell density (> one million cells 1(-1)) contribute to the formation of an accumulation zone: '' the cyst bank '', which is directly linked to the success of bloom initiation and its recurrence. The survival time of benthic RCs (few weeks to their viability which could be negatively affected by predation, and their mandaseveral years), mandatory dormancy period (few days to several months) are variable and influence the seeding potential of the population significantly. Excystment rate, mainly controlled by temperature and oxygen level, and the germling cells' viability determine the inoculum size. Many biological processes in RCs have been shown to be controlled by endogenous and environmental factors, and vary between species and within the same species as a function of geographic strains.	Univ Montpellier 2, CNRS, UMR 5119, Lab Ecosyst Lagunaires, F-34095 Montpellier 05, France	Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS)	Genovesi-Giunti, B (通讯作者)，Univ Montpellier 2, CNRS, UMR 5119, Lab Ecosyst Lagunaires, Case Courrier 093,Pl Eugene Bataillon, F-34095 Montpellier 05, France.	genovesi@univ-montp2.fr						Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; 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J	Carvalho, MD; Mendonca, JG; Menezes, TR				Carvalho, Marcelo de Araujo; Mendonca Filho, Jodo Graciano; Menezes, Taissa Rego			Palynofacies and sequence stratigraphy of the Aptian-Albian of the Sergipe Basin, Brazil	SEDIMENTARY GEOLOGY			English	Article						palynofacies; sequence stratigraphy; Aptian-Albian; Sergipe Basin; Brazil	SEDIMENTARY ORGANIC-MATTER; SE FRANCE; MARGINAL BASINS; CARBONATES; ATLANTIC; FACIES; FIELD	In order to place information from palynofacies variations in a sequence stratigraphic context, palynofacies analyses for wells GTP-17-SE and GTP-24-SE from the Sergipe Basin, was integrated with sequence stratigraphy. Previous works assigned the succession to two second-order sequences, K50 and K60, the last being subdivided into systems tracts KM1 and KM2 (third-order sequences). By combining lithofacies data and gamma-ray logs from the studied wells with palynofacies and paleoecological data, the succession was subdivided into third-order sequences and correlated with the integrated sequence stratigraphic framework. The K50 sequence shows a slightly transgressive upward trend. The sequence boundaries of K50 are marked by major peaks in abundance of phytoplankton and amorphous organic matter and in the gamma-ray. KM 1 sequence starts below of the boundary between Muribeca and Riachuelo Formations. This sequence was subdivided into three parasequences. The first transgressive systems tract is supported by a marked increase in Palynological Marine Index and amorphous organic matter values, and the phytoclast relative abundance shows a progressive decrease. The upper boundaries are marked by maximum flooding surface characterized by high abundances of dinoflagellate cysts. The boundaries are also marked by an abrupt decrease of phytoclasts, which is best observed in well GTP-24-SE. The highstand systems tract is characterized by an increase in amount of phytoclast particles, a clear decrease in amorphous organic matter percentage values and moderate values that tend to increase upwards of the Palynological Marine Index. The upper boundary of this sequence is marked by a peak of dinoflagellate cysts indicating the transgressive surface. In well GTP-24-SE, the boundary is placed at the base of an abrupt lithological change, from calcilutites to dark shales. The second transgressive systems tract is based on a marked increase in Palynological Marine Index and amorphous organic matter percentage values, together with the clear decrease in phytoclast particles. These are observed clearly in well GTP-24-SE, especially the decrease of phytoclasts. The top of these parasequences is distinguished on the basis of the peaks of Palynological Marine Index indicating the maximum flooding surface. In well GTP-24-SE, the lowest abundances of the phytoclast group are recorded at the maximum flooding surface. The KM2 sequence interpreted previously as a highstand systems tract is confirmed herein, on the basis of palynofacies. (c) 2006 Elsevier B.V. All rights reserved.	UFRJ, Dept Geol & Paleontol, Museu Nacl, DLab Palinol Aplicada, BR-22040040 Sao Cristovao, RJ, Brazil; UFRJ, IGEO, Dept Geol, BR-21949900 Rio De Janeiro, Brazil; UFRJ, Fdn Coppetec, RJ Organ Petrog Lab, PETROBRA,CENPES, BR-21949900 Rio De Janeiro, Brazil	Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro; Universidade Federal do Rio de Janeiro	Carvalho, MD (通讯作者)，UFRJ, Dept Geol & Paleontol, Museu Nacl, DLab Palinol Aplicada, RJ Quinta Boa Vista S-N, BR-22040040 Sao Cristovao, RJ, Brazil.	mcarvalho@mn.ufrj.br	Carvalho, Marcelo/G-8463-2015; Mendonca Filho, Joao Graciano/C-2098-2013	Mendonca Filho, Joao Graciano/0000-0001-8997-0270				[Anonymous], 1993, SPECIAL PUBL INT ASS; [Anonymous], 1966, TXB POLLEN ANAL; [Anonymous], 1977, J. 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Geol.	NOV 15	2006	192	1-2					57	74		10.1016/j.sedgeo.2006.03.017	http://dx.doi.org/10.1016/j.sedgeo.2006.03.017			18	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	108ZQ					2025-03-11	WOS:000242278100003
J	Lindström, S; Erlström, M				Lindstrom, S.; Erlstrom, M.			The late Rhaetian transgression in southern Sweden:: Regional (and global) recognition and relation to the Triassic-Jurassic boundary	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; palynology; flooding events; sea-level changes; Rhaetian; Triassic-Jurassic boundary	ATLANTIC MAGMATIC PROVINCE; TECTONIC EVOLUTION; TORNQUIST ZONE; FACIES CHANGES; EXTINCTION; SCANIA; BASIN; STRATIGRAPHY; TERRESTRIAL; SUCCESSION	Palynological investigations of Rhaetian outcrops and drillcores in combination with subsurface data from wells in Scania, southern Sweden, have revealed the presence of marine dinoflagellate cysts in sedimentary strata that were previously considered to have been deposited in a mainly terrestrial environment. Two distinct dinocyst events are identified. One older event where persistent, rare to common occurrences of Rhaetogonyaulax rhaetica and Lunnomidinium scaniense indicates deposition in shallow marine and marginal marine environments. This Lunnomidinium interval is preceded and succeeded by assemblages with rare to common R. rhaetica, and can be correlated with the mid to late Rhaetian R. rhaetica Zone. It is associated with spore/pollen assemblages of the mid Rhaetian Rhaetipollis-Limbosporites Zone. The younger event, the R. rhaetica maximum interval, is characterised by mass-occurrence of R. rhaetica, with less common or absent Dapcodinium priscum, in association with a dark grey to black mudstone/shale. The introduction of D. priscum in association with the over-whelming abundance of R. rhaetica allows correlation with the transition between the R. rhaetica Zone and the succeeding D. priscum Zone, and signals fully marine conditions. The R. rhaetica maximum interval is associated with spore/pollen assemblages of the late Rhaetian Ricciisporites-Polypodiisporites Zone, and is in Sweden succeeded both lithostratigraphically and palynostratigraphically by the T-J transition. The R. rhaetica maximum interval corresponds to a late Rhaetian maximum flooding event that took place in a shallow, gently sloping embayment that covered the Danish Basin area during the Late Triassic-Early Jurassic. This maximum flooding event can be recognised in late Rhaetian strata from different parts of the Northern Hemisphere. It is an important temporal constraint on the T-J boundary as it is associated with the disappearance of Triassic marine faunas, appears to coincide with the onset of the main pulse of CAMP volcanism, immediately precedes the initial carbon isotope excursion and the global sea-level drop that characterises the T-J transition, (c) 2006 Elsevier B.V. All rights reserved.	Lund Univ, Dept Geol, GeoBiosphere Sci Ctr, SE-22362 Lund, Sweden; Geol Survey Sweden, SE-22350 Lund, Sweden	Lund University	Lindström, S (通讯作者)，Lund Univ, Dept Geol, GeoBiosphere Sci Ctr, Solvegatan 12, SE-22362 Lund, Sweden.	sofie.lindstrom@geol.lu.se; mikael.erlstrorn@sgu.se	Lindström, Sofie/G-5481-2018	Lindstrom, Malin Sofie/0000-0001-8278-1055				Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; Ahlberg A, 2002, TERRA NOVA, V14, P241, DOI 10.1046/j.1365-3121.2002.00416.x; [Anonymous], SVERIGES GEOLOGISK C; [Anonymous], 1994, LUND PUBLICATIONS GE; [Anonymous], SVERIGES GEOLOGISKA; [Anonymous], LUNDS U ARSSKRIFT N; [Anonymous], 1996, Palynology: principles and applications; ARNDORFF L, 1994, LUND PUBLICATIONS GE, V116, P1; Backhouse J., 2002, SEDIMENTARY BASINS W, V3, P13; BALME BE, 1995, REV PALAEOBOT PALYNO, V87, P85; Batten D., 1994, Cahiers de Micropaleontologie, V9, P21; BOLAU E, 1963, STENKOL LERA, V3; CLEMMENSSON G, 1958, STENKOL LERA, V2; Courtinat B, 2002, GEOBIOS-LYON, V35, P429, DOI 10.1016/S0016-6995(02)00038-4; DYBKJAER K., 1988, DANMARKS GEOLOGISKE, V21, P1; Dybkjaer K., 1991, DANMARKS GEOLOGISK A, V30, P1; Erlstrom M, 1997, TECTONOPHYSICS, V271, P191, DOI 10.1016/S0040-1951(96)00247-8; Galli MT, 2005, PALAEOGEOGR PALAEOCL, V216, P203, DOI 10.1016/j.palaeo.2004.11.009; Gierlinski Gerard, 1994, Ichnos, V3, P99; Grice K, 2005, ORG GEOCHEM, V36, P1347, DOI 10.1016/j.orggeochem.2005.06.003; GRIGELIS A, 1999, SVERIGES GEOLOGISK C, V89; Guex J, 2004, EARTH PLANET SC LETT, V225, P29, DOI 10.1016/j.epsl.2004.06.006; GUYOHLSON D, 1981, GEOL FOREN STOCK FOR, V103, P233, DOI 10.1080/11035898109454520; Haas J, 2004, SEDIMENT GEOL, V168, P19, DOI 10.1016/j.sedgeo.2004.03.002; Hallam A, 2000, SEDIMENT GEOL, V137, P101, DOI 10.1016/S0037-0738(00)00155-X; Hames WE, 2000, GEOLOGY, V28, P859, DOI 10.1130/0091-7613(2000)028<0859:NEFGIE>2.3.CO;2; Hesselbo SP, 2004, J GEOL SOC LONDON, V161, P365, DOI 10.1144/0016-764903-033; Hesselbo SP, 2002, GEOLOGY, V30, P251, DOI 10.1130/0091-7613(2002)030<0251:TAMEAT>2.0.CO;2; Hounslow MW, 2004, PALAEOGEOGR PALAEOCL, V213, P331, DOI 10.1016/j.palaeo.2004.07.018; Hubbard RNLB, 2000, PALAIOS, V15, P120, DOI 10.2307/3515498; Kelber KP, 1998, REV PALAEOBOT PALYNO, V100, P1, DOI 10.1016/S0034-6667(97)00061-4; Knight KB, 2004, EARTH PLANET SC LETT, V228, P143, DOI 10.1016/j.epsl.2004.09.022; Koppelhus E.B., 1996, American Association of Stratigraphic Palynologists Foundation, V2, P779; LIBORIUSSEN J, 1987, TECTONOPHYSICS, V137, P21, DOI 10.1016/0040-1951(87)90310-6; Lindström S, 2002, REV PALAEOBOT PALYNO, V120, P247, DOI 10.1016/S0034-6667(02)00079-9; Lott G. 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NOV 14	2006	241	3-4					339	372		10.1016/j.palaeo.2006.04.006	http://dx.doi.org/10.1016/j.palaeo.2006.04.006			34	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	109JO					2025-03-11	WOS:000242304300001
J	Bravo, I; Garcés, E; Diogène, J; Fraga, S; Sampedro, N; Figueroa, RI				Bravo, I.; Garces, E.; Diogene, J.; Fraga, S.; Sampedro, N.; Figueroa, R., I			Resting cysts of the toxigenic dinoflagellate genus <i>Alexandrium</i> in recent sediments from the Western Mediterranean coast, including the first description of cysts of <i>A. kutnerae</i> and <i>A. peruvianum</i> (vol 41, pg 293, 2006)	EUROPEAN JOURNAL OF PHYCOLOGY			English	Correction													Bravo, Isabel/D-3147-2012; Fraga, Santiago/AAA-3760-2020; SAMPEDRO, NAGORE/I-1767-2015; Fraga, Santiago/C-8641-2012; Diogene, Jorge/AAB-8667-2019; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011	SAMPEDRO, NAGORE/0000-0002-0829-5152; Fraga, Santiago/0000-0003-3917-9960; Bravo, Isabel/0000-0003-3764-745X; Diogene, Jorge/0000-0002-6567-6891; Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X				Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360	1	1	1	1	8	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0967-0262			EUR J PHYCOL	Eur. J. Phycol.	NOV	2006	41	4					449	450		10.1080/09670260601093594	http://dx.doi.org/10.1080/09670260601093594			2	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	131AO		Bronze			2025-03-11	WOS:000243840500008
J	Scourse, J; Sejrup, HP; Jones, PD				Scourse, James; Sejrup, Hans Petter; Jones, Phil D.		HOLSMEER project participants	Late Holocene oceanographic and climate change from the western European margin: the results of the HOLSMEER project	HOLOCENE			English	Editorial Material						Holocene; palaeoclimate; marine; thermohaline circulation; sea level; Arctica islandica; transfer function; HOLSMEER project; North Atlantic Ocean; western European margin	SEA-SURFACE TEMPERATURES; NORTH-ATLANTIC; RIVER DISCHARGE; GERMAN BIGHT; SHELF; ASSEMBLAGES; SALINITY; ISOTOPES; ICELAND; RECORD	The underlying aim of the HOLSMEER project has been to improve our understanding of natural climate variability through the search for, interpretation and quantification of, climatic variability in very high-resolution shallow marine records from Atlantic Europe covering the last 2000 years. This has been achieved through detailed analyses of a series of coastal and shallow marine sites spanning the Atlantic seaboard from Iberia to western Norway, and extending across to Iceland. HOLSMEER partners have documented pronounced instability in the thermohaline circulation (THC) during the period immediately prior to the recent significant anthropogenic impact on the environment. For the first time we have been able to document that these changes in the coastal ocean are correlated with significant changes in terrestrial palaeoclimate proxies, notably during the last 1000 years. The notable changes are the significance of warm sea surface temperatures (SST) associated with active THC between AD 700 and 1000, a transition phase to much colder SST and reduced THC between AD 1000 and AD 1300, colder SST through to AD 1900 followed by an active re-establishment of warm surface water circulation during the twentieth century These switch-like reorganizations of the climate system have influenced the entire seaboard from western Iberia to western Norway, and have forced changes in ocean productivity, iceberg frequency and sea ice coverage. These changes have also directly influenced sea level through steric effects. The project has also resulted in significant advances in the establishment of new palaeoclimate proxies, including transfer functions related to benthic foraminifera, diatoms and dinoflagellate cysts. Annual growth band series from fossil specimens of the long-lived bivalve mollusc Arctica islandica from the northern North Sea have been successfully cross-matched, and independently verified by radiocarbon dating, to provide the longest Arctica chronology, and the first floating chronology constructed entirely from marine fossils.	Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales; Univ Bergen, Dept Earth Sci, N-5007 Bergen, Norway; Univ E Anglia, Climat Res Unit, Norwich NR4 7TJ, Norfolk, England	University of Bergen; University of East Anglia	Scourse, J (通讯作者)，Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales.	j.scourse@bangor.ac.uk	Jones, Philip/C-8718-2009	Jones, Philip/0000-0001-5032-5493				Andersson C, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2001PA000654; Austin WEN, 2006, HOLOCENE, V16, P937, DOI 10.1177/0959683606hl985rp; Eiríksson J, 2006, HOLOCENE, V16, P1017, DOI 10.1177/0959683606hl991rp; Gehrels WR, 2006, HOLOCENE, V16, P949, DOI 10.1177/0959683606hl986rp; Gyllencreutz R, 2006, HOLOCENE, V16, P975, DOI 10.1177/0959683606hl988rp; Hebbeln D, 2006, HOLOCENE, V16, P987, DOI 10.1177/0959683606hl989rp; Jiang H, 2001, MAR MICROPALEONTOL, V41, P73, DOI 10.1016/S0377-8398(00)00053-0; Jiang H, 2002, HOLOCENE, V12, P137, DOI 10.1191/0959683602h1529rp; Jones P.D., 2001, History and Climate: Memories of the Future?; Knudsen KL, 2004, QUATERNARY SCI REV, V23, P2231, DOI 10.1016/j.quascirev.2004.08.012; Lebreiro SM, 2006, HOLOCENE, V16, P1003, DOI 10.1177/0959683606hl990rp; Marret F, 2004, REV PALAEOBOT PALYNO, V128, P35, DOI 10.1016/S0034-6667(03)00111-8; Moros M, 2004, QUATERNARY SCI REV, V23, P2113, DOI 10.1016/j.quascirev.2004.08.003; Scheurle C, 2003, GEO-MAR LETT, V23, P130, DOI 10.1007/s00367-003-0133-2; Scheurle C, 2005, HOLOCENE, V15, P429, DOI 10.1191/0959683605hl802rp; Scourse J, 2006, HOLOCENE, V16, P967, DOI 10.1177/0959683606hl987rp; Scourse JD, 2004, HOLOCENE, V14, P747, DOI 10.1191/0959683604hl753rp; Sejrup HP, 2004, MAR MICROPALEONTOL, V53, P197, DOI 10.1016/j.marmicro.2004.05.009	18	4	5	0	12	SAGE PUBLICATIONS LTD	LONDON	1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND	0959-6836	1477-0911		HOLOCENE	Holocene	NOV	2006	16	7					931	935		10.1177/0959683606hl984ed	http://dx.doi.org/10.1177/0959683606hl984ed			5	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	118JS					2025-03-11	WOS:000242939200001
J	Atta-Peters, D; Salami, MB				Atta-Peters, D.; Salami, M. B.			Aptian-Maastrichtian palynomorphs from the offshore Tano Basin, western Ghana	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						miospores; dinollagellate cysts; cretaceous; palaeoenvironment; Ghana	PALYNOLOGY; POLLEN	Cretaceous dinoflagellate cysts and miospores have been recovered from the Tano 1-1 and 1S-3AX wells, offshore of western Ghana. Based on marker palynomorphs (Afropollis jardinus, Elaterosporites klaszii, Elaterocolpites castelainii, Sofreipites legouxae, Reyrea polymorphus, Cyclonephelium vannophorum) an Aptian-early Cenomanian age has been assigned to sediments from the well Tano 1-1. The taxa Auriculiidites reticulatus, Spinizonotriletes echinatus, Buttinia andreevi, Longapertites spp., Echitriporites trianguliformis, Dinogymnium spp., Trichodinium castanea, Andalusiella spp., which are elements typical of Campanian-Maastrichtian sediments have been recognized in the sediments from 1S-3AX. Palaeoenvironmental interpretation based on identified palynomorphs in the light of their ecological preferences and also on the relative proportions of palynomorph groups, indicate that the Aptian-lower Cenomanian sediments were deposited in a marginal marine environment with vegetation on wetlands, under a relatively dry climate. The Campanian-Maastrichtian sediments suggest a fluctuation between marginal to open marine (inner shelf) conditions. The sediments have characteristic elements indicative of the Albian-Cenomanian "Elaterate Province", and the late Cretaceous "Senonian Palmae Province", which supports a warm tropical climate. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Ghana, Dept Geol, Accra, Ghana; Obafemi Awolowo Univ, Dept Geol, Ife, Osun State, Nigeria	University of Ghana; Obafemi Awolowo University	Atta-Peters, D (通讯作者)，Univ Ghana, Dept Geol, POB LG 58, Accra, Ghana.	dattapeters@yahoo.com		Atta-Peters, David/0000-0002-1072-4040				[Anonymous], 1996, Palynology: principles and applications; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; Batten D.J., 1985, J MICROPALAEONTOL, V4, P131; Boltenhagen E, 1977, MICROPLANCTON CRETAC; BRENNER G.J., 1968, POLLEN SPORES, V10, P341; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; BUJAK JP, 1977, GEOLOICAL SURVEY CAN, V297, P19; COSTA LI, 1999, BRIT MICROPALEONTOLO, P99; COX LR, 1952, GOLD COAST GEOLOGICA, V17, P68; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; Digbehi Z.B., 1996, GEOLOGIE MEDITERRANE, V23, P155; DIMTER A, 1990, PALAEOGEOGR PALAEOCL, V80, P173, DOI 10.1016/0031-0182(90)90131-P; Dino R, 1999, REV PALAEOBOT PALYNO, V105, P201, DOI 10.1016/S0034-6667(98)00076-1; Downie C., 1971, Geoscience Man, V3, P29; Doyle J.A., 1977, Bull. 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Earth Sci.	NOV	2006	46	4					379	394		10.1016/j.jafrearsci.2006.07.002	http://dx.doi.org/10.1016/j.jafrearsci.2006.07.002			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	112EH					2025-03-11	WOS:000242507800006
J	Jiménez-Moreno, G; Head, MJ; Harzhauser, M				Jimenez-Moreno, Gonzalo; Head, Martin J.; Harzhauser, Mathias			Early and Middle Miocene dinoflagellate cyst stratigraphy of the Central Paratethys, Central Europe	JOURNAL OF MICROPALAEONTOLOGY			English	Article						dinoflagellate cysts; palaeoenvironments; Miocene; Paratethys	NORTHERN BELGIUM; OLIGOCENE; BIOSTRATIGRAPHY; EVOLUTION; DINOPHYCEAE; CIRCULATION; BOREHOLE; TERTIARY; BASIN; CORE	Marine organic-walled dinoflagellate cysts have been studied from the Early and Middle Miocene of the Central Paratethys in Austria (Vienna and eastern Alpine Foreland basins) and Hungary (Pannonian Basin), and compared with assemblages of similar age from the Atlantic Ocean and Mediterranean Sea. The presence of a diverse flora of 71 taxa, including such biostratigraphical markers as Apteodinium spiridoides, Cerebrocysta poulsenii, Cordosphaeridium cantharellus, Cribroperidinium tenuitabulatum, Exochosphaeridium insigne, Glaphyrocysta reticulosa s.l., Habibacysta tectata, Labyrinthodinium truncatum subsp. truncatum, Palaeocystodinium miocaenicum, and Unipontidinium aquaeductus, has allowed the establishment of five biozones that characterize the Ottnangian, Badenian and Sarmatian local stages (collectively equivalent to the mid-Burdigalian, upper Langhian and Serravallian stages). This is the first study to demonstrate the applicability of dinoflagellate cysts for detailed stratigraphic correlation and palaeoenvironmental interpretation in the Early and Middle Miocene of the Central Paratethys area.	Univ Lyon 1, CNRS, UMR 5125, Lab Paleoenvironm & Paleobiosphere, F-69622 Villeurbanne, France; Univ Granada, Dept Estratig & Paleontol, Granada 18002, Spain; Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; Museum Nat Hist, A-1010 Vienna, Austria	Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; University of Granada; University of Cambridge	Jiménez-Moreno, G (通讯作者)，Univ New Mexico, Dept Earth & Planetary Sci, Northrop Hall, Albuquerque, NM 87131 USA.	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J	Zavattieri, AM; Prámparo, MB				Zavattieri, Ana M.; Pramparo, Mercedes B.			Freshwater algae from the Upper Triassic Cuyana Basin of Argentina:: Palaeoenvironmental implications	PALAEONTOLOGY			English	Review						Chlorophycean algae; Upper Triassic; Cuyana Basin; Argentina; palaeoenvironments; palynofacies	WESTERN-AUSTRALIA; CACHEUTA HILL; ZYGNEMATACEAE; PALYNOLOGY; POTRERILLOS; ACRITARCHS; ZYGOSPORES; PROVINCE; MENDOZA	Diverse freshwater aquatic palynomorphs are present among rich terrestrial palynofloras from the upper part of the Potrerillos and Cacheuta formations outcropping in the Cuyana Basin at the southern extremity of the Precordillera of Argentina. The Potrerillos/Cacheuta sequence includes fluvial, deltaic and lacustrine facies deposited in the early Late Triassic fault-bounded syn-rift Cacheuta hemigraben. The phytoplankton described and illustrated consist of representatives of colonial chlorococcalean algae belonging to the Hydrodictyaceae (Plaesiodictyon) and Botryococcaceae (Botryococcus), a diverse group of Zygnemataceae zygospores, a freshwater dinoflagellate cyst (Bosedinia) and acritarchs (sphaeromorphs). Zygnematacean zygospores are represented by species of Gelasinicysta?, Lecaniella, Mougeotia, Ovoidites, Peltacystia and Schizocystia. Of these, Gelasinicysta? cuyanensis sp. nov. is newly described. Quantitative analysis of the palynofloras permits interpretation of changes in the local vegetation and phytoplankton communities controlled by changes in environmental setting. Two algal associations are recognized as belonging to different stages in the evolution of the basin. Diverse zygnematacean assemblages along with hydrodictyacean, botryococcacean and leiosphere/sphaeromorph algae are common in fluvial-deltaic environments of the upper part of the Potrerillos Formation and the lowermost part of the Cacheuta Formation. Higher in the sections (in the Cacheuta Formation) Botryococcus dominates, in association with amorphous kerogen, representing deposition in a relatively deep, quiet-water, lacustrine environment where anoxic conditions prevailed. In the Cacheuta hemigraben the lacustrine shales have average TOC values of 4 per cent (locally reaching 20 per cent), with some terrigenous components (Type II/III kerogen), but dominant amorphous, algal-like, organic matter (Type I/II kerogen). Oils derived from these source rocks are predominantly waxy.	Consejo Nacl Invest Cient & Tecn, CRICYT, IANIGLA, Unidad Palaeopalinol, RA-5500 Mendoza, Argentina	University Nacional Cuyo Mendoza; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); CRICYT	Zavattieri, AM (通讯作者)，Consejo Nacl Invest Cient & Tecn, CRICYT, IANIGLA, Unidad Palaeopalinol, CC 131, RA-5500 Mendoza, Argentina.	amz@lab.cricyt.edu.ar; mprampar@lab.cricyt.edu.ar						AGARDH CA, SYSTEMA ALGARUM LUND; [Anonymous], PALYNOLOGY PRINCIPLE; [Anonymous], 1931, JPN J GEOL GEOGR; [Anonymous], REV PALAEOBOTANY PAL; [Anonymous], 1980, PALEOBIOLOGY PLANT P; Artabe A. E., 2001, SISTEMA TRIASICO ARG; BACKHOUSE J, 1991, REV PALAEOBOT PALYNO, V67, P237, DOI 10.1016/0034-6667(91)90046-6; BALME BE, 1966, J ROYAL SOC W AUSTR, V19, P26; Batten D., 1996, PALYNOLOGY PRINCIPLE, P1011; BATTEN DJ, 1980, P 4 INT PAL C LUCKN, V2, P589; Bharadwaj D. 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J	Matsuoka, K; Kawami, H; Fujii, R; Iwataki, M				Matsuoka, Kazumi; Kawami, Hisae; Fujii, Rika; Iwataki, Mitsunori			Further examination of the cyst-theca relationship of <i>Protoperidinium thulesense</i> (Peridiniales, Dinophyceae) and the phylogenetic significance of round brown	PHYCOLOGIA			English	Article						archeopyle; cyst; dinoflagellate; dinophyceae; diplopsalid; phylogeny; round brown cyst; Protoperidinium; P. thulesense (Balech) Balech; SSU rDNA	RIBOSOMAL-RNA GENE	The heterotrophic armored dinollagellate Protoperidinium thulesense has an unusual combination of morphological characters, i.e. the thecal plate arrangement of the motile cell resembles a typical Protoperidinium, whereas the shape and archeopyle of the cyst are like the diplopsalids. We have re-examined the cyst-motile relationship of P. thulesense by cyst incubation and thecal plate analysis together with a molecular phylogenetic study based on small subunit (SSU) rDNA sequences. Five isolates of P. thulesense, including motile cells and cysts, and three Protoperidinium and three diplopsalid species were examined by using the single cell PCR method. The thecal plate arrangement of the motile cells isolated from field samples and those germinated from cysts were identical. The plate formula was: Po, X, 3 ', 3a, 7 '', 3c+t, 4s, 5 ''', 2 ''''. The cysts of P. thulesense were round and brown with a theropylic archeopyle, and rather similar to the diplopsalid species, Diplopsalis lenticula, D. lebourae, Gotoius abei and others. SSU rDNA sequence analysis reveals P. thulesense is closely related to the subgenus Protoperidinium, especially species of the section Conica, and distant from the diplopsalid species. The phylogenetic and taxonomic significances of Protoperidinium and diplopsalid round brown cysts with a theropylic archeopyle are discussed.	Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan	Nagasaki University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp	Iwataki, Mitsunori/H-9640-2019	Iwataki, Mitsunori/0000-0002-5844-2800				Abe T.H., 1981, SETO MARINE BIOL LAB, V6, P1, DOI DOI 10.5134/176462; AKSELMAN R, 1987, Boletim do Instituto Oceanografico, V35, P17; [Anonymous], 1988, PUBLICACIONES ESPECI; [Anonymous], 1919, MUSEE ROYAL HIST NAT; [Anonymous], 1935, HVALRADETS SKRIFTER; [Anonymous], 1958, PHYSIS; Balech E., 1973, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V3, P347; Balech E., 1956, Rev. Algol, V2, P29; BLANCO J, 1989, Scientia Marina, V53, P797; Dale B., 1983, P69; Dodge D.J., 1985, Atlas of Dinoflagellates; Dodge DJ, 1982, MARINE DINOFLAGELLAT; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; HALLEGRAEFF GM, 1988, J PLANKTON RES, V10, P533, DOI 10.1093/plankt/10.3.533; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Hermosilla J., 1969, Neotropica, V15, P9; JOrgensen E, 1912, SVENSKA HYDROGRAFISK, V4, P1; Kim SH, 2004, J MICROBIOL BIOTECHN, V14, P959; LEWIS J, 1990, BRIT PHYCOL J, V25, P339, DOI 10.1080/00071619000650381; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Matsuoka K., 1989, P461; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; MATSUOKA K, 1982, REV PALAEOBOT PALYNO, V38, P109, DOI 10.1016/0034-6667(82)90052-5; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Nakayama Takeshi, 1996, Phycological Research, V44, P47, DOI 10.1111/j.1440-1835.1996.tb00037.x; PAULSEN OVE, 1930, TRAB INST ESPANOL OCEANOGR, VNo. 4., P1; POPOVSKY J., 1990, Susswasserflora von Mitteleuropa, P272; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; RAUSCH H, 1989, J MOL EVOL, V29, P255, DOI 10.1007/BF02100209; Saldarriaga JF, 2004, EUR J PROTISTOL, V40, P85, DOI 10.1016/j.ejop.2003.11.003; Swofford D., 1993, PAUP: Phylogenetic Analysis Using Parsimony; Takano Y, 2004, PHYCOL RES, V52, P107, DOI 10.1111/j.1440-183.2004.00332.x; Watanabe MM., 2000, NIES COLLECTION LIST; Woloszynska J., 1928, ARCH HYDROBIOLOGIE I, V3, P153; Yamaguchi A, 2005, PHYCOL RES, V53, P30; ZONNEVELD KAF, 1994, PHYCOLOGIA, V33, P39	38	30	35	1	10	ALLEN PRESS INC	LAWRENCE	810 E 10TH ST, LAWRENCE, KS 66044 USA	0031-8884			PHYCOLOGIA	Phycologia	NOV	2006	45	6					632	641		10.2216/05-42.1	http://dx.doi.org/10.2216/05-42.1			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	104QG					2025-03-11	WOS:000241973000004
J	Mailliot, S; Mattioli, E; Guex, J; Pittet, B				Mailliot, Samuel; Mattioli, Emanuela; Guex, Jean; Pittet, Bernard			The Early Toarcian anoxia, a synchronous event in the Western Tethys? An approach by quantitative biochronology (Unitary Associations), applied on calcareous nannofossils	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						anoxic event; Early Toarcian; quantitative biochronology; calcareous nannofossils	CALIBRATION; BIOSTRATIGRAPHY; PHYTOPLANKTON; EUROPE; SEDIMENTARY; EVOLUTION; AMMONITES; SECTIONS	During the Early Toarcian, major paleoenvironnemental and paleoceanographical changes occurred, leading to an oceanic anoxic event (OAE) and to a perturbation of the carbon isotope cycle. Although the standard biochronology of the Lower Jurassic is essentially based upon ammonites, in recent years biostratigraphy based on calcareous nannofossils and dinoflagellate cysts is increasingly used to date Jurassic rocks. However, the precise dating and correlation of the Early Toarcian OAE, and of the associated delta C-13 anomaly in different settings of the western Tethys, are still partly problematic, and it is still unclear whether these events are synchronous or not. In order to allow more accurate correlations of the organic rich levels recorded in the Lower Toarcian OAE, this account proposes a new biozonation based on a quantitative biochronology approach, the Unitary Associations (UA), applied to calcareous nannofossils. This study represents the first attempt to apply the UA method to Jurassic nannofossils. The study incorporates eighteen sections distributed across western Tethys and ranging from the Pliensbachian to Aalenian, comprising 1220 samples and 72 calcareous nannofossil taxa. The BioGraph [Savary, J., Guex, J., 1999. Discrete biochronological scales and unitary associations: description of the Biograph Computer program. Memoires de Geologie de Lausanne 34, 282 pp] and UA-Graph (Copyright Hammer O., Guex and Savary, 2002) softwares provide a discrete biochronological framework based upon multi-taxa concurrent range zones in the different sections. The optimized dataset generates nine UAs using the co-occurrences of 56 taxa. These UAs are grouped into six Unitary Association Zones (UA-Z), which constitute a robust biostratigraphic synthesis of all the observed or deduced biostratigraphic relationships between the analysed taxa. The UA zonation proposed here is compared to "classic" calcareous nannofossil biozonations, which are commonly used for the southern and the northern sides of Tethys. The biostratigraphic resolution of the UA-Zones varies from one nannofossil subzone or part of it to several subzones, and can be related to the pattern of calcareous nannoplankton originations and extinctions during the studied time interval. The Late Pliensbachian - Early Toarcian interval (corresponding to the UA-Z II) represents a major step in the Jurassic nannoplankton radiation. The recognized UA-Zones are also compared to the carbon isotopic negative excursion and TOC maximum in five sections of central Italy, Germany and England, with the aim of providing a more reliable correlation tool for the Early Toarcian OAE, and of the associated isotopic anomaly, between the southern and northern part of western Tethys. The results of this work show that the TOC maximum and delta C-13 negative excursion correspond to the upper part of the UA-Z II (i.e., UA 3) in the sections analysed. This suggests that the Early Toarcian OAE was a synchronous event within the western Tethys. (c) 2006 Elsevier B.V. All rights reserved.	Univ Lyon 1, CNRS, UMR 5125, Lab PEPS,UFR Sci Terre, F-69622 Villeurbanne, France; Univ Lausanne, UNIL, BFSH2, CH-1015 Lausanne, Switzerland	Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); University of Lausanne	Mailliot, S (通讯作者)，Univ Lyon 1, CNRS, UMR 5125, Lab PEPS,UFR Sci Terre, 2 Rue Dubois, F-69622 Villeurbanne, France.	Samuel.Mailliot@univ-lyon1.fr	Pittet, Bernard/B-9664-2012; Mattioli, Emanuela/D-7951-2012	Mattioli, Emanuela/0000-0003-0990-1641				[Anonymous], 1992, BENTHIC LIFE EARLY T; BARTOLINI A, 2002, GEN FIELD TRIP GUIDE, P96; BASSOULLET JP, 1993, ATLAS TETHYS PALEOEN; BASSOULLET JP, 1994, GEOBIOS MEMORIE SPEC, V7, P645; BAUDIN F, 1989, THESIS U P M CURIE P; Baumgartner P. 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Sc. Geol. Padova, V43, P41; Reale V., 1989, MEM DESCR CARTE GEOL, V39, P80; Riegraf W., 1985, TUBINGERMIKROPALAONT, V3, P1; Röhl HJ, 2001, PALAEOGEOGR PALAEOCL, V169, P271, DOI 10.1016/S0031-0182(01)00224-3; ROOD A P, 1973, Eclogae Geologicae Helvetiae, V66, P365; Roth PH, 1987, PALEOCEANOGRAPHY, V2, P601, DOI 10.1029/PA002i006p00601; ROTH PH, 1989, PALAEOGEOGR PALAEOCL, V74, P111, DOI 10.1016/0031-0182(89)90022-9; Sandoval J, 2001, PALAIOS, V16, P311, DOI 10.2307/3515574; SAVARY J, 1991, Bulletin de la Societe Vaudoise des Sciences Naturelles, V80, P317; SAVARY J, 1999, MEMORIES GEOLOGIE LA, V34; VENTURI F, 1999, BIOEVENTS INTEGRATE, V3, P89; [No title captured]	90	60	62	0	14	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	OCT 19	2006	240	3-4					562	586		10.1016/j.palaeo.2006.02.016	http://dx.doi.org/10.1016/j.palaeo.2006.02.016			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	097FB					2025-03-11	WOS:000241431200012
J	Tardio, M; Sangiorgi, F; Brinkhuis, H; Filippi, ML; Cantonati, M; Lotter, AF				Tardio, Massimiliano; Sangiorgi, Francesca; Brinkhuis, Henk; Filippi, Maria Letizia; Cantonati, Marco; Lotter, Andre F.			Peridinioid dinoflagellate cysts in a Holocene high-mountain lake deposit in Italy	JOURNAL OF PALEOLIMNOLOGY			English	Article						peridinioid dinoflagellate cysts; freshwater; lake sediments; central-eastern Alps; holocene	SEDIMENTS; GERMANY; USA	This paper documents the discovery of peridinioid organic walled dinoflagellate cysts in Holocene sediments of the freshwater, low-alkalinity, high mountain Lake Nero di Cornisello (Adamello mountain range, Trentino, Italy). Among the three main cyst morphotypes found in the samples, the dominant one is acavate, with a smooth and light brown colored wall, with a clear conical shape, elongated with a pointy to rounded end in the antapical-ventral part, with the epicyst broader than the hypocyst and displays a typical peridinioid archeopyle. Comparison with data available in literature, besides pointing out the general scarcity of observations on dinocysts in lakes sediments, suggested a strong morphological similarity with the marine genus Brigantedinium. This finding pinpoints the need for more detailed studies on cysts in freshwater environments offering a new tool for paleoenvironmental interpretations.	Museo Tridentino Sci Nat, Limnol & Phycol Sect, I-38100 Trento, Italy; Univ Pisa, Dept Biol, I-56126 Pisa, Italy; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Museo Tridentino Sci Nat, Geol Sect, I-38100 Trento, Italy	University of Pisa; Utrecht University	Tardio, M (通讯作者)，Museo Tridentino Sci Nat, Limnol & Phycol Sect, Via Calepina 14, I-38100 Trento, Italy.	tardio@mtsn.tn.it	Brinkhuis, Henk/B-4223-2009; Cantonati, Marco/G-4278-2018; Lotter, Andre F./C-3477-2008	Lotter, Andre F./0000-0002-2954-8809; Sangiorgi, Francesca/0000-0003-4233-6154; Cantonati, Marco/0000-0003-0179-3842; Brinkhuis, Henk/0000-0003-0253-6610				ACETI A, 2005, OP SCI C GLOB CHANG; BATTEN D J, 1988, Cretaceous Research, V9, P337, DOI 10.1016/0195-6671(88)90007-9; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; Callegari E., 2002, Mem Sci Geol, V54, P19; CANTONATI M, 2002, LAGHI PARCO NATURALE, V14, P1; EVITT WR, 1985, REV PALAEOBOT PALYNO, V45, P35, DOI 10.1016/0034-6667(85)90064-8; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Findlay DL, 1998, J PALEOLIMNOL, V19, P41, DOI 10.1023/A:1007906611087; Köhler J, 2000, REV PALAEOBOT PALYNO, V112, P39, DOI 10.1016/S0034-6667(00)00034-8; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Marret F, 2004, REV PALAEOBOT PALYNO, V129, P1, DOI 10.1016/j.revpalbo.2003.10.002; Mudie PJ, 2004, REV PALAEOBOT PALYNO, V128, P143, DOI 10.1016/S0034-6667(03)00117-9; NORRIS G, 1970, REV PALAEOBOT PALYNO, V10, P131, DOI 10.1016/0034-6667(70)90016-3; TARDIO M, 2006, IN PRESS HYDROBIOLOG; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; ZIPPI P, 1990, TECHNOLOGY TRANSFER, V1, P393	16	10	10	0	6	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-2728			J PALEOLIMNOL	J. Paleolimn.	OCT	2006	36	3					315	318		10.1007/s10933-006-9001-1	http://dx.doi.org/10.1007/s10933-006-9001-1			4	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	092QR					2025-03-11	WOS:000241112900006
J	Figueroa, RI; Bravo, I; Garcés, E				Isabel Figueroa, Rosa; Bravo, Isabel; Garces, Esther			Multiple routes of sexuality in <i>Alexandrium taylori</i> (Dinophyceae) in culture	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium taylori; Dinophyceae; encystment; flow cytometry; gametes; life cycle; nitrates; nutritional effects; phosphate	DINOFLAGELLATE GYMNODINIUM-CATENATUM; CINCTUM-F-OVOPLANUM; LIFE-CYCLE; CELL-CYCLE; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; REPRODUCTION; CYSTS; HISTORY; ENCYSTMENT	Alexandrium taylori Balech is a cyst-forming dinoflagellate species responsible for recurrent blooms in Mediterranean coastal waters. The nuclear development of the cells during the sexual cycle and the effect of different external nitrate and phosphate levels were studied. Nuclear fusion of gametes occurred 6-12 h after the complete cytoplasmic fusion. The U-shaped nuclei fused through the end of one nucleus and the mid-area of the other. The mobile and biflagellated zygote had a large, U-shaped nucleus and may follow three different fates: direct division, short-term encystment (ecdysal), and long-term encystment (resting). Ecdysal cysts may divide in > 24-96 h into two, four, six, or eight cells before germinating. Meiosis presumably occurred in three locations: in the planozygote, within the ecdysal cyst, and in the planomeiocyte (germling) liberated either from ecdysal or resting cysts. The effects of nutrients on these routes were studied in individually isolated sexual stages. (1) Direct divisions occurred mainly under replete conditions (L1), whereas no direct planozygote divisions were recorded in media with no phosphate added (L-P). (2) Short-term encystment was larger in media lacking phosphate (L-P and L/30) than in medium with no nitrate added (L-N) or under replete conditions (L1). (3) Long-term encystment was only observed in medium with no nitrate added (L-N). The long-lived resting cyst, not previously described for this species, had a clear double wall, an irregular shape, a flat morphology, and a middle orange spot. No cysts germinated in 1-2 months, whereas 86% of the cysts germinated 2-3 months after being formed. A flow cytometry analysis showed that sexual induction and zygote formation were very fast and highly common processes, zygotes being nearly half of the population at days 3 and 5 after the induction of sexuality in the cultures.	Inst Oceanog Vigo, Vigo 36200, Spain; CSIC, Inst Ciencias Mar, Barcelona, Spain; IRTA, Ctr Aquicultura, St Charles Rapita 43540, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); IRTA	Figueroa, RI (通讯作者)，Inst Oceanog Vigo, Cabo Estai Canido, Vigo 36200, Spain.	rosabel.figueroa@vi.ieo.es	Bravo, Isabel/D-3147-2012; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015	Garces, Esther/0000-0002-2712-501X; Bravo, Isabel/0000-0003-3764-745X; Figueroa, Rosa/0000-0001-9944-7993				ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Basterretxea G, 2005, ESTUAR COAST SHELF S, V62, P1, DOI 10.1016/j.ecss.2004.07.008; BERNSTEIN H, 1983, BIOSCIENCE, V33, P326, DOI 10.2307/1309320; BHAUD Y, 1988, J CELL SCI, V89, P197; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BRAVO I, 2006, IN PRESS EUR J PHYCO; CETTA CM, 1990, J EXP MAR BIOL ECOL, V135, P69, DOI 10.1016/0022-0981(90)90199-M; COOPER S, 1987, BIOESSAYS, V7, P220, DOI 10.1002/bies.950070507; Cooper S, 1998, FASEB J, V12, P367, DOI 10.1096/fasebj.12.3.367; Dale B., 1983, P69; Emura A, 2004, HARMFUL ALGAE, V3, P29, DOI 10.1016/j.hal.2003.08.004; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; Fukuyo Y., 2003, RED TIDES, P61; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Garces Esther, 2000, Harmful Algae News, V20, P10; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; GIACOBBE MG, 2006, IN PRESS HYDROBIOLOG; Goodenough U.W., 1985, MBL (Marine Biology Laboratory) Lectures in Biology, V7, P123; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; HAMILTON WD, 1980, OIKOS, V35, P282, DOI 10.2307/3544435; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kwok ACM, 2003, PLANT PHYSIOL, V131, P1681, DOI 10.1104/pp.102.018945; LEGALL Y, 1993, PROTOPLASMA, V173, P123; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Lim PT, 2005, HARMFUL ALGAE, V4, P391, DOI 10.1016/j.hal.2004.07.001; LIVELY CM, 1987, NATURE, V328, P519, DOI 10.1038/328519a0; LIVELY CM, 1989, EVOLUTION, V43, P1663, DOI [10.2307/2409382, 10.1111/j.1558-5646.1989.tb02616.x]; LOMBARD EH, 1971, J PHYCOL, V7, P188, DOI 10.1111/j.1529-8817.1971.tb01500.x; MANSINGH A, 1971, CAN ENTOMOL, V103, P983, DOI 10.4039/Ent103983-7; Parrow Matthew, 2002, Harmful Algae, V1, P5, DOI 10.1016/S1568-9883(02)00009-4; Parrow MW, 2004, J PHYCOL, V40, P664, DOI 10.1111/j.1529-8817.2004.03202.x; Parrow MW, 2003, J PHYCOL, V39, P678, DOI 10.1046/j.1529-8817.2003.02146.x; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; PFIESTER LA, 1989, INT REV CYTOL, V114, P249; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; SPECTOR DL, 1981, AM J BOT, V68, P34, DOI 10.2307/2442989; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P24; UCHIDA T, 1991, NIPPON SUISAN GAKK, V57, P1215, DOI 10.2331/suisan.57.1215; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; VAULOT D, 1986, EXP CELL RES, V167, P38, DOI 10.1016/0014-4827(86)90202-8; Von Stosch HA., 1973, Br Phycol J, V8, P105; VONSTOSCH HA, 1972, SOC BOT FR MEMOIRES, P201; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	56	72	76	0	14	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	OCT	2006	42	5					1028	1039		10.1111/j.1529-8817.2006.00262.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00262.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	086GS					2025-03-11	WOS:000240662400007
J	Narsimha, K				Narsimha, K.			A record of late Jurassic dinoflagellate cysts from Ariyalur-Pondicherry sub-basin of Cauvery Basin, Tamil Nadu	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						dinoflagellates; Jurassic-Cretaceous; biostratigraphy; marine transgressions; Cauvery Basin; Tamil Nadu		A detailed study was carried out on dinoflagellate cyst taxa in the interval between 4995 m and 4725 in in Andimadam Formation (Pre-Albian) of well Komarakshi # A of Artyalur-Pondicherry sub-basin in the Cauvery Basin. The study recognises five dinoflagellate cyst biozones, ranging from Late Jurassic to Early Cretaceous (Early Oxfordian & older - Aptian) age. The stratigraphic order of these biozones are: Sentusidinium rioultii - Polystephanephorus calathus Interval zone, Polystephanephorus calathus - Wanaea clathrata Interval zone, Wanaea clathrata - Gochteodinia mutabilis Interval zone, Gochteodinia mutabilis - Egniontodinium torynum Interval zone and Odontochitina operculata - Pseudoceratium pelliferum Assemblage zone. The presence of dinoflagellate cysts throughout the study interval suggests that the marine influence was prevalent through Late Jurassic (Early Oxfordian) to Early Cretaceous (Aptian) period. The record of Late Jurassic dinoflagellate cysts in the well Komarakshi # A, amply suggests that the marine incursion had taken place during Early Oxfordian in the Cauvery Basin. This also leads to the hypothesis that the rifting of Gondwanaland and opening up of Indian Ocean might have begun during Late Jurassic (Early Oxfordian) period, which led to the first marine transgression into the basin.	Oil & Nat Gas Corp Ltd, Geol Lab, RGL, Bombay 410221, Maharashtra, India	Oil & Natural Gas Corporation	Narsimha, K (通讯作者)，Oil & Nat Gas Corp Ltd, Geol Lab, RGL, ONGC Complex,Phase 1, Bombay 410221, Maharashtra, India.	narasimha_kanchi@yahoo.co.in						Aswal H.S., 1999, ONGC B, V36, P45; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; MEHROTRA NC, 1986, GEOBIOS-LYON, V19, P705, DOI 10.1016/S0016-6995(86)80105-X; Mehrotra NC, 2002, MEM GEOL SOC INDIA; PANDEY J, 1991, STANDARD LAB TECHNIQ, P83; PRASAD B, 1995, GEOSCI J, V16; Rangaraju M. K., 1993, P 2 SEM PETR BAS IND, V1, P371; Smelror M., 1989, Palynology, V13, P121; Stover LE, 1978, ANAL PREPLEISTOCENE; VENKATACHALA BS, 1971, PALYNOLOGICAL ZONATI, P172; WILLIAMS GL, 1985, LANKTON STRATIGRAPHY, P847; WILLIAMS GL, 1993, GEOL SURV CANADA; WILSON GJ, 1980, NZ GEOL SURV	14	1	2	0	0	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	OCT	2006	68	4					597	604						8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	118CX					2025-03-11	WOS:000242920800007
J	Binet, MT; Stauber, JL				Binet, M. T.; Stauber, J. L.			Rapid flow cytometric method for the assessment of toxic dinoflagellate cyst viability	MARINE ENVIRONMENTAL RESEARCH			English	Article						ballast water; dinoflagellate cyst; alexandrium catenella; flow cytometry; viability	SHIPS BALLAST WATER; SYTOX GREEN; MARINE; TRANSPORT; BIOASSAY; SPORES	The inadvertent transfer and dispersal of non-indigenous marine species via shipping ballast water is of increasing environmental concern. Despite a major global effort to develop new ballast water treatment technologies, their acceptance has been hampered by the lack of suitable indicator species for assessing treatment effectiveness. Resistant dinoflagellate cysts are one proposed test organism, however their use has been limited due to difficulties in assessing their viability after treatment. The paper describes the development of a rapid method to determine the viability of cysts of the dinoflagellate Alexandrium catenella using staining with SYTOX (R) Green and flow-cytometric analysis. The viability of A. catenella cysts was inversely proportional to their ability to take up the stain. There was excellent agreement between cysts measured as viable/non-viable using flow cytometry and cyst viability determined in standard long-term germination tests. Advantages of the flow-cytometric method include high test precision and rapid testing times of < 2 days, compared to > 4 weeks using existing germination methods. Crown Copyright (c) 2006 Published by Elsevier Ltd. All rights reserved.	CSIRO Energy Technol, Ctr Environm Contaminants Res, Sydney, NSW 2234, Australia	Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Binet, MT (通讯作者)，CSIRO Energy Technol, Ctr Environm Contaminants Res, Private Mail Bag 7, Sydney, NSW 2234, Australia.	monique.binet@csiro.au	Stauber, Jenny/G-8418-2011; Binet, Monique/F-2996-2011	Stauber, Jenny/0000-0002-1231-3173; Binet, Monique/0000-0003-3502-9025				Adams MS, 2004, ENVIRON TOXICOL CHEM, V23, P1957, DOI 10.1897/03-232; ANDERSON AB, 2004, P 2 INT BALL WAT TRE; Anderson D. M., 1995, MANUAL HARMFUL MARIN, V33, P229; ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Bax N, 2003, MAR POLICY, V27, P313, DOI 10.1016/S0308-597X(03)00041-1; Bolch C.J., 1993, Journal of Marine Environmental Engineering: 1993, P23; Endresen O, 2004, MAR POLLUT BULL, V48, P615, DOI 10.1016/j.marpolbul.2004.01.016; Franklin NM, 2001, ARCH ENVIRON CON TOX, V40, P469; Franklin NM, 2001, ENVIRON TOXICOL CHEM, V20, P160, DOI [10.1897/1551-5028(2001)020<0160:DOFCBA>2.0.CO;2, 10.1002/etc.5620200118]; Gill MS, 2003, FREE RADICAL BIO MED, V35, P558, DOI 10.1016/S0891-5849(03)00328-9; Green LC, 2000, J CLIN MICROBIOL, V38, P3811, DOI 10.1128/JCM.38.10.3811-3814.2000; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; HALLEGRAEFF GM, 1997, EQUATIC ECOLOGY, V31, P47; *IMO, 2005, INT CONV CONTR MAN B; *INT MAR ORG, 2002, GLOB BALL WAT MAN PR; Joachimsthal EL, 2004, MAR POLLUT BULL, V49, P334, DOI 10.1016/j.marpolbul.2004.02.036; Joachimsthal EL, 2003, MAR POLLUT BULL, V46, P308, DOI 10.1016/S0025-326X(02)00401-0; Langsrud S, 1996, J APPL BACTERIOL, V81, P411; LOEBLICH AR, 1968, LIPIDS, V3, P5, DOI 10.1007/BF02530961; MATHEICKAL JT, 2004, P 2 INT BALL WAT TRE; Montani S., 1995, J. Mar. Biotechnol, V2, P179; MOUNTFORT D, 2004, P 2 INT BALL WAT TRA; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Pughuic D., 2001, TROPICAL COASTS, V8, P42; Roth BL, 1997, APPL ENVIRON MICROB, V63, P2421, DOI 10.1128/AEM.63.6.2421-2431.1997; Simpson SL, 2003, ENVIRON TOXICOL CHEM, V22, P2073, DOI 10.1897/02-418; Stauber JL, 2002, TRENDS BIOTECHNOL, V20, P141, DOI 10.1016/S0167-7799(01)01924-2; STEVENS TG, 2004, P 2 INT BALL WAT TRE; VALENTINE JP, 1996, THESIS U TASMANIA HO; Veldhuis MJW, 1997, J PHYCOL, V33, P527, DOI 10.1111/j.0022-3646.1997.00527.x; Waite TD, 2002, MAR TECHNOL SOC J, V36, P29, DOI 10.4031/002533202787914070	34	17	23	2	26	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0141-1136	1879-0291		MAR ENVIRON RES	Mar. Environ. Res.	OCT	2006	62	4					247	260		10.1016/j.marenvres.2006.03.011	http://dx.doi.org/10.1016/j.marenvres.2006.03.011			14	Environmental Sciences; Marine & Freshwater Biology; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Toxicology	091WB	16740303				2025-03-11	WOS:000241057900001
J	Weller, AF; Harris, AJ; Ware, JA				Weller, Andrew F.; Harris, Anthony J.; Ware, J. Andrew			Artificial neural networks as potential classification tools for dinoflagellate cyst images: A case using the self-organizing map clustering algorithm	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; palynofacies; image analysis; cluster; artificial neural network; self-organizing map	PATTERN-RECOGNITION; IDENTIFICATION; POLLEN; AUTOMATION; PALYNOLOGY; PROSPECTS; SYSTEM	Automated palynological analysis has been previously proposed but proved difficult to achieve. Here, the first instance of dinoflagellate cyst (dinocyst) image clustering from palynological samples based on morphological and textural image analysis (IA) features is presented. Dinocyst-dominated example images (including acritarchs and other algae) were acquired from Cretaceous, Paleogene and Holocene samples. IA features that cover a broad array of measurements are used, including morphological, Fourier and textural descriptors, as well as geometric moments and color. To determine clusters, unsupervised self-organized maps (a genre of artificial neural networks) were used. Self-organized maps (SOMs) can determine their own classification of data in cases where no knowledge of the true class of each data point exists. Using a SOM five major clusters can be identified including clusters of freshwater alga, proximate dinocysts, proximate dinocysts with long horns, proximochorate dinocysts and chorate dinocysts. Minor variations can also be identified based on red, green and blue color, textural variations, and dinocyst process length in the form of morphological (shape) descriptors. These major and minor clusters demonstrate the open-ended capability of the system to be a wider palynological identification tool. The advantages of automation in palynology are articulated and the hurdles yet to overcome discussed. These advantages include freeing humans from 'routine identification' so that more emphasis can be placed upon distinguishing the rarer ('unknown') particles and placing them in a descriptive context. Challenges yet to conquer include distinguishing between images of closely related morphologies and/or textures. It is envisaged that technological and computational developments will quickly facilitate such further developments. (c) 2006 Elsevier B.V. All rights reserved.	ETH, Inst Geol, Dept Earth Sci, CH-8092 Zurich, Switzerland; Univ Glamorgan, Sch Appl Sci, Pontypridd CF37 1DL, M Glam, Wales; Univ Glamorgan, Sch Comp, Pontypridd CF37 1DL, M Glam, Wales	Swiss Federal Institutes of Technology Domain; ETH Zurich; University of South Wales; University of South Wales	Weller, AF (通讯作者)，ETH, Inst Geol, Dept Earth Sci, CH-8092 Zurich, Switzerland.	weller@erdw.ethz.ch; ajharri1@glam.ac.uk; jaware@glam.ac.uk						BALFOORT HW, 1992, J PLANKTON RES, V14, P575, DOI 10.1093/plankt/14.4.575; Batten D., 1996, Palynology: principles and applications, P1011; BOLLMANN J, 2004, IMAGE ANAL SEDIMENTS, P110; BOULTER MC, 1999, SEDIMENTATION ORGANI, P199; Chang HC, 2002, COMPUT GEOSCI-UK, V28, P223, DOI 10.1016/S0098-3004(01)00067-X; Culverhouse PF, 1996, MAR ECOL PROG SER, V139, P281, DOI 10.3354/meps139281; Culverhouse PF, 2002, SEA TECHNOL, V43, P39; DABROS MJ, 1986, CURRENT RES A, V86, P107; Evitt W.R., 1985, Sporopollen in Dinoflagellate Cysts: Their Morphology and Interpretation; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Flenley J, 2003, QUATERN INT, V105, P77, DOI 10.1016/S1040-6182(02)00153-2; France I, 2000, QUATERNARY SCI REV, V19, P537, DOI 10.1016/S0277-3791(99)00021-9; Gaston KJ, 2004, PHILOS T R SOC B, V359, P655, DOI 10.1098/rstb.2003.1442; Kartalopoulos S.V., 1996, Understanding Neural Networks and Fuzzy Logic: Basic Concepts and Applications; Kohonen T, 2012, SELF ORG ASS MEMORY; Kropp J, 1997, ECOL MODEL, V103, P151, DOI 10.1016/S0304-3800(97)00083-5; Leong FJW, 2003, ADV ANAT PATHOL, V10, P88, DOI 10.1097/00125480-200303000-00003; Leong FJWM, 2001, J PATHOL, V195, P508, DOI 10.1002/path.972; Li P, 2004, J QUATERNARY SCI, V19, P755, DOI 10.1002/jqs.874; Lorente M.A., 1990, MEDEDELINGEN RIJKS G, V45, P103; *MVTEC GMBH, 2004, HALCON; Pech-Pacheco JL, 1998, MAR BIOL, V132, P357, DOI 10.1007/s002270050402; *SPSS INC, 2004, ANSWERTREE; Stillman EC, 1996, QUATERNARY SCI REV, V15, P1, DOI 10.1016/0277-3791(95)00076-3; Truquet P, 1996, AQUAT LIVING RESOUR, V9, P273, DOI 10.1051/alr:1996031; Tyson R. V., 1995, Sedimentary Organic Matter, DOI [10.1007/978-94-011-0739-6_20, DOI 10.1007/978-94-011-0739-6_20]; TYSON RV, 1990, MEDEDELINGEN RIJKS G, V45, P139; Ujiié Y, 2001, ORG GEOCHEM, V32, P127, DOI 10.1016/S0146-6380(00)00146-7; Weller AF, 2005, COMPUT GEOSCI-UK, V31, P1213, DOI 10.1016/j.cageo.2005.03.011; WELLER AF, UNPUB MATH GEOLOGY; WELLER AF, 2004, THESIS U GLAMORGAN U; WELLER AF, IN PRESS COMPUTERS G; WILKINS MF, 1994, BINARY-COMPUT MICROB, V6, P64; Yule B, 1998, ORG GEOCHEM, V28, P139, DOI 10.1016/S0146-6380(97)00125-3; Zhang WQ, 2004, J WUHAN UNIV TECHNOL, V19, P8	35	11	15	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	OCT	2006	141	3-4					287	302		10.1016/j.revpalbo.2006.06.001	http://dx.doi.org/10.1016/j.revpalbo.2006.06.001			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	094BP					2025-03-11	WOS:000241214400005
J	Panera, JPP; Angelozzi, GN				Perez Panera, Juan Pablo; Noemi Angelozzi, Gladys			Late Cretaceous - Tertiary calcareous nannofossils from the BBIII A x-1 (Bahia Blanca) borehole, Colorado Basin, Argentina	AMEGHINIANA			Spanish	Article						calcareous nannofossils; Late Cretaceous; tertiary; biostratigraphy; Colorado Basin; Argentina	DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY; OCEAN	A quantitative biostratigraphic study based on calcareous nannofossils, using cutting samples from the BB III A x-1 (Bahia Blanca) borehole placed in the western area of the Colorado Basin, off shore, is presented. According to the marker species, the stratigraphic column was divided in nine sections included in the Miocene, Oligocene, middle-late Eocene, early Paleocene, and late Campanian-Maastrichtian. The study has shown a rich nannoflora with species cited for the first time in the Colorado Basin. Early Danian, late Campanian and Maastrichtian biozones and a well defined Cretaceous-Tertiary boundary were recognized.	Univ Nacl La Plata, Fac Ciencias Nat & Museo, Div Paleozool Invertebrados, RA-1900 La Plata, Argentina; GEMA SRL, Serv Bioestratigraf, RA-1888 Buenos Aires, DF, Argentina	National University of La Plata; Museo La Plata	Panera, JPP (通讯作者)，Univ Nacl La Plata, Fac Ciencias Nat & Museo, Div Paleozool Invertebrados, Paseo Bosque S-N, RA-1900 La Plata, Argentina.	perezpanera@ciudad.com.ar; gema@infovia.com.ar	Perez Panera, Juan/HSI-3366-2023					[Anonymous], CREATACEOUS TERTARY; [Anonymous], 2003, STUD GEOPHYS GEOD; BECKER D, 1980, 1 C LATINOAMERICANO, V2, P315; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bramlette M. N., 1967, Tulane Studies in Geology, V5, P93; BRAMLETTE M. N., 1961, MICROPALEONTOLOGY, V7, P129, DOI 10.2307/1484276; Bramlette M.N., 1954, Jour. Pal, V28, P385; Burnett J. A., 1999, Calcareous Nannofossil Biostratigraphy, P132; Caramés A, 2000, AMEGHINIANA, V37, P387; Concheyro Andrea, 1997, Palaeopelagos, V6, P281; FRYKLUND B, 1996, 13 C GEOL ARG 3 C EX, P135; Guerstein GR, 2000, AMEGHINIANA, V37, P81; Guerstein GR, 2001, AMEGHINIANA, V38, P299; Guler MV, 2002, AMEGHINIANA, V39, P103; Hay W.W., 1977, P1055; HAY WILLIAM W., 1967, J PALEONTOL, V41, P1505; MALUMIAN N, 1970, Ameghiniana, V7, P173; MALUMIAN N, 1996, GEOLOGIA RECURSOS NA, P73; Moshkovitz S., 1976, B GEOL SURV ISRAEL, V69, P1; Perch-Nielsen K., 1985, P427; Perch-Nielsen K., 1985, P329; Perch-Nielsen K., 1983, S CRETACEOUS STAGE B, P152; Pospichal J.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P613, DOI 10.2973/odp.proc.sr.113.205.1990; Quattrocchio ME, 1999, AMEGHINIANA, V36, P37; Ronchi D. I., 1994, B INFORM PETROLERAS, V39, P65; Roth P.H., 1978, Initial Reports of the Deep Sea Drilling Project, V44, P731; SISSINGH W, 1977, Geologie en Mijnbouw, V56, P37; VAROL O, 1999, CALCAREOUS NANNOFOSS, P225; WIND FH, 1983, INITIAL REP DEEP SEA, V71, P551; WIND FH, 1975, ANTARCT J US, V10, P265; WISE S, 1976, INITIAL REPORTS DEEP, V36, P269; Young J.R., 1999, CALCAREOUS NANNOFOSS, P225; YRIGOYEN MR, 1999, ANALES, V29, P645; [No title captured]	34	8	8	0	0	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	SEP 30	2006	43	3					557	565						9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	109BR					2025-03-11	WOS:000242283400004
J	Kuhlmann, G; Langereis, C; Munsterman, D; van Leeuwen, RJ; Verreussel, R; Meulenkamp, J; Wong, T				Kuhlmann, Gesa; Langereis, Cor; Munsterman, Dirk; van Leeuwen, Robert Jan; Verreussel, Roel; Meulenkamp, Johan; Wong, Theo			Chronostratigraphy of late Neogene sediments in the southern North Sea Basin and paleoenvironmental interpretations	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						North Sea; neogene; paleoenvironment; paleomagnetism; biostratigraphy; chronostratigraphy; X-event	DINOFLAGELLATE CYST; SEQUENCE STRATIGRAPHY; MAGNETIC-ANOMALIES; ATLANTIC; HISTORY; QUATERNARY; OCEAN; DEPOSITS; MARGIN; UPLIFT	A chronostratigraphic framework has been established for Upper Neogene sediments from the northern Netherlands offshore sector, southern North Sea. Data of dinoflagellate cysts, pollen and foraminifers from eight boreholes are integrated and the resulting biostratigraphic events are connected to an additionally retrieved paleomagnetic record. The sedimentary succession comprises at the base Late to Middle Miocene sediments and spans the Piacenzian to Gelasian stages, from 3.6 to 1.8 Ma, including the paleomagnetic Gauss-Matuyama boundary and the Olduvai subchron. Sedimentation rates vary between 30 cm/kyr in the lower part of the succession and reach up to 84 cm/kyr in the upper part. These rates are high enough to record short paleomagnetic events and for the first time the presence of the so-called X-event has been recorded and dated at around 2.44 Main a sedimentary setting. The name `North Sea event' is proposed here. The paleoclimatic and paleoenvironmental information pictures the onset of Northern Hemisphere Glaciation and the subsequent intensification of glacial conditions with its impact on the North Sea sea region. The paleoenvironmental changes are characterised by a stepwise development and five successive intervals are distinguished. During the first interval, a warm climate and an open marine setting prevailed. The second interval is characterised by dominantly cold climatic conditions with occasional warmer periods. During the third interval, the environment became restricted marine and a stable freshwater layering occurred, which facilitated the development of sea-ice in the shallow sea. Within the fourth interval, extreme cold (arctic) conditions were predominant, and shallowing continued. The fifth interval shows fluvial to deltaic, paralic conditions. From then on, facies differences from the nearby delta system overruled the basin-wide signals at the studied location. (c) 2006 Elsevier B.V. All rights reserved.	Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; Natl Geol Survey Netherlands, TNO, NITG, NL-3584 CB Utrecht, Netherlands	Utrecht University; Netherlands Organization Applied Science Research	Langereis, C (通讯作者)，Univ Utrecht, Dept Earth Sci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	langer@geo.uu.nl		Langereis, Cor/0000-0001-9232-2178				[Anonymous], GEOLOGISCHES JB A; [Anonymous], 1990, AAPG AAPG METHODS EX; [Anonymous], 2003, The Millenium Atlas: petroleum geology of the central and northern North Sea; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Barthès V, 1999, EARTH PLANET SC LETT, V165, P97, DOI 10.1016/S0012-821X(98)00214-3; BAUMANN KH, 1999, P OC DRILL PROGR, P179; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BIJLSMA S, 1981, GEOL MIJNBOUW, V60, P337; BLAKELY RJ, 1972, J GEOPHYS RES, V77, P7065, DOI 10.1029/JB077i035p07065; BURGER AW, 2002, FORSCHUNGSBOHRUNG NI, V152, P141; CAMERON TDJ, 1993, MAR PETROL GEOL, V10, P591, DOI 10.1016/0264-8172(93)90061-V; 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Paleoclimatol. Paleoecol.	SEP 25	2006	239	3-4					426	455		10.1016/j.palaeo.2006.02.004	http://dx.doi.org/10.1016/j.palaeo.2006.02.004			30	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	091RY					2025-03-11	WOS:000241047200011
J	Friedrich, O; Meier, KJS				Friedrich, Oliver; Meier, K. J. Sebastian			Suitability of stable oxygen and carbon isotopes of calcareous dinoflagellate cysts for paleoclimatic studies: Evidence from the Campanian/Maastrichtian cooling phase	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						ocean drilling program; calcareous dinoflagellate cysts; Maastrichtian; Campanian; stable isotopes	WESTERN TROPICAL ATLANTIC; DIEL VERTICAL MIGRATION; UPPER WATER COLUMN; SURFACE SEDIMENTS; THORACOSPHAERA-HEIMII; BIOLOGICAL CARBONATES; QUATERNARY EASTERN; CLIMATIC-CHANGE; POTENTIAL USE; BOTTOM-WATER	In order to determine the possible usefulness of stable isotope measurements on calcareous dinoflagellate cysts for paleoceanographic and paleoclimatic studies, we have produced oxygen and carbon isotope records of the species Pirumella krasheninnikovii (Bolli, H.M., 1974. Jurassic and Cretaceous Calcisphaerulidae from DSDP Leg 27, eastern Indian Ocean. Initial Reports of the Deep Sea Drilling Project 27, 843-907.) for the latest Campanian to earliest Maastrichtian (similar to 73-68 Ma) of high-latitude Ocean Drilling Program Hole 690C in the southern South Atlantic (eastern Weddell Sea). Foraminiferal stable isotope values characterize this time interval as a phase of continuous cooling, superimposed by a short-term, strong cooling event between 71 and 70 Ma that was detected at various sites in the mid to high latitudes. This event is interpreted to reflect short-term surface-water cooling, leading to changes in the mode and direction of deep-water formation and possibly the growth of continental ice sheets. Our delta O-18 values of calcareous cysts verify this event as well as the general cooling of surface waters during the latest Campanian and early Maastrichtian. Prior to this cooling event, between similar to 72 and 71 Ma, a negative excursion in accompanying delta C-13 records of planktic and benthic foraminifera was observed. This negative excursion and the subsequent positive one were proposed to reflect sea-level fluctuations, changes in productivity, and/or changes in the ratio of organic to inorganic carbon input to the ocean. The delta C-13 values of calcareous cysts show the positive excursion between 71 and 70 Ma, but don't show the expected negative excursion before. In addition, they yield extremely light carbon isotope values that probably resulted from photosynthetic processes. As the stable oxygen isotope data of the calcareous dinoflagellate species P. krasheninnikovii show isotopic shifts comparable to planktic foraminifera from the same locality and from various other sites in the Pacific and South Atlantic oceans, we suggest that calcareous cyst oxygen isotopes can provide information for paleoceanographic reconstructions of sea-surface water temperatures and paleoceanographic changes. However, the application of carbon isotope data from cysts of P. krasheninnikovii appears to be questionable, and investigations of different species are needed to further evaluate the reconstruction potential based on stable isotopes and to assess species-specific vital effects. (c) 2006 Elsevier B.V. All rights reserved.	Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany; Nat Hist Museum, London SW7 5BD, England	Natural History Museum London	Friedrich, O (通讯作者)，Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany.	oliver.friedrich@bgr.de	Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. 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J	Thibodeau, B; de Vernal, A; Mucci, A				Thibodeau, Benoit; de Vernal, Anne; Mucci, Alfonso			Recent eutrophication and consequent hypoxia in the bottom waters of the Lower St. Lawrence Estuary: Micropaleontological and geochemical evidence	MARINE GEOLOGY			English	Article						Lower St. Lawrence Estuary; eutrophication; hypoxia; dinoflagellate cysts; benthic foraminifera; geochemistry	BENTHIC FORAMINIFERAL ASSEMBLAGE; SURFACE OCEAN PRODUCTIVITY; DINOFLAGELLATE CYSTS; CHESAPEAKE BAY; CONTINENTAL-SHELF; MODERN SEDIMENTS; ORGANIC-MATTER; ATLANTIC; MARINE; OXYGEN	Micropaleontological and gechemical analyses were carried out on two sediment box cores (AH00-2220 and CR02-23) recovered in the Lower St. Lawrence Estuary (LSLE) in order to document recent temporal variations of primary productivity and carbon fluxes to the bottom waters. These reveal a ten-fold increase in the accumulation rate of dinoflagellate cysts and benthic foraminifera in the sediment over the last four decades which can be interpreted as a recent increase in pelagic and benthic production. Furthermore, the appearance of the benthic foraminiferal species Brizalina subaenariensis and Bulimina exilis, which are tolerant of low oxygen concentrations and high organic,fluxes, in the upper 20 cm of the cores, may reflect significant changes in bottom water conditions over the last 40 yrs. Variations in the microfossil abundances in core AH00-2220 are strongly correlated with an increase in organic carbon (OC) content (from 1.1 to 1.6%) and to a shift in the isotopic signature of the latter (delta C-13(ORG) from -24.8 to -24.0 parts per thousand). Similarly, a concomitant decrease in the C-ORG:N ratio (from 15 to 12), an increase in organic carbon content (from 1.3 to 1.9%) and an increase in delta C-13(ORG) (from -24.5 to -23.5 parts per thousand) were observed in core CR02-23, all of which suggest an enhanced accumulation of marine over terrestrial OC in the LSLE. Our results imply that a significant increase in marine productivity in the LSLE occurred since the 1960's. (c) 2006 Elsevier B.V. All rights reserved.	Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; McGill Univ, Dept Earth & Planetary Sci, Montreal, PQ H3A 2A7, Canada	University of Quebec; University of Quebec Montreal	Thibodeau, B (通讯作者)，Univ Quebec, GEOTOP, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.	thibodeau.benoit@courrier.uqam.ca	Thibodeau, Benoit/B-5629-2008; de Vernal, Anne/D-5602-2013	Thibodeau, Benoit/0000-0003-0422-2308; Mucci, Alfonso/0000-0001-9155-6319; de Vernal, Anne/0000-0001-5656-724X				Altenbach A.V., 1988, REV PALEOBIOLOGIE, V2, P719; ALTENBACH AV, 1992, MAR MICROPALEONTOL, V19, P119, DOI 10.1016/0377-8398(92)90024-E; [Anonymous], 2001, WORLD OC ATL; BENOIT P, IN PRESS MARINE CHEM; Bernhard JM, 1997, J FORAMIN RES, V27, P301, DOI 10.2113/gsjfr.27.4.301; Bourgault D, 1999, ATMOS OCEAN, V37, P201; Bratton JF, 2003, GEOCHIM COSMOCHIM AC, V67, P3385, DOI 10.1016/S0016-7037(03)00131-5; Brüchert V, 2000, MAR GEOL, V163, P27, DOI 10.1016/S0025-3227(99)00099-7; Cloern JE, 2001, MAR ECOL PROG SER, V210, P223, DOI 10.3354/meps210223; Colman SM, 2003, GEOLOGY, V31, P71, DOI 10.1130/0091-7613(2003)031<0071:AICISA>2.0.CO;2; COPLEN TB, 1995, NATURE, V375, P285, DOI 10.1038/375285a0; CORLISS BH, 1988, GEOLOGY, V16, P716, DOI 10.1130/0091-7613(1988)016<0716:MPONSD>2.3.CO;2; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1992, GEOLOGY, V20, P527, DOI 10.1130/0091-7613(1992)020<0527:QAOCDI>2.3.CO;2; de Vernal A., 1987, POLLEN SPORES, V29, P291; DESCHAMPS P, 1997, THESIS U QUEBEC MONT; DEVERNAL A, 1999, TECHNIQUES PREPARATI; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Diaz RJ, 1995, OCEANOGR MAR BIOL, V33, P245; Dickie L.M., 1983, ECOSYSTEMS WORLD, V26, P403; EDENBORN HM, 1986, SEDIMENTOLOGY, V33, P147, DOI 10.1111/j.1365-3091.1986.tb00750.x; El-Sabh M.I., 1990, Coastal and Estuarine Studies, V39; FLYNN WW, 1968, ANAL CHIM ACTA, V43, P221, DOI 10.1016/S0003-2670(00)89210-7; Gilbert D, 2005, LIMNOL OCEANOGR, V50, P1654, DOI 10.4319/lo.2005.50.5.1654; GIROUX L, 1990, THESIS U QUEBEC MONT; GOODAY AJ, 1988, NATURE, V332, P70, DOI 10.1038/332070a0; GOODAY AJ, 1994, PALAIOS, V9, P14, DOI 10.2307/3515075; GOODAY AJ, 1986, DEEP-SEA RES, V33, P1345, DOI 10.1016/0198-0149(86)90040-3; Gray JS, 2002, MAR ECOL PROG SER, V238, P249, DOI 10.3354/meps238249; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JENNANE A, 1992, THESIS U QUEBEC MONT, P85; Jouanneau JM, 1999, CR ACAD SCI II A, V329, P265, DOI 10.1016/S1251-8050(99)80245-6; KAIHO K, 1994, GEOLOGY, V22, P719, DOI 10.1130/0091-7613(1994)022<0719:BFDOIA>2.3.CO;2; Karlsen AW, 2000, ESTUARIES, V23, P488, DOI 10.2307/1353141; Leduc J, 2002, PALAEOGEOGR PALAEOCL, V180, P207, DOI 10.1016/S0031-0182(01)00429-1; Lee J.J., 1974, FORAMINIFERA, V1, P207; Livingston RobertJ., 2000, CRC MAR SCI; Loubere P, 1999, GLOBAL BIOGEOCHEM CY, V13, P115, DOI 10.1029/1998GB900001; Loubere P, 1991, PALEOCEANOGRAPHY, V6, P193, DOI 10.1029/90PA02612; MACKENSEN A, 1993, MAR MICROPALEONTOL, V22, P33, DOI 10.1016/0377-8398(93)90003-G; MATTHEWS J, 1969, NEW PHYTOL, V68, P161, DOI 10.1111/j.1469-8137.1969.tb06429.x; McKay JL, 2004, QUATERNARY SCI REV, V23, P261, DOI 10.1016/j.quascirev.2003.07.004; MEYERS PA, 1994, CHEM GEOL, V114, P289, DOI 10.1016/0009-2541(94)90059-0; MOOK WG, 1975, ESTUAR COAST MAR SCI, V3, P325, DOI 10.1016/0302-3524(75)90032-8; Osterman LE, 2003, ESTUAR COAST SHELF S, V58, P17, DOI 10.1016/S0272-7714(02)00352-9; PARSON TR, 1984, BIOL OCEANIC PROCESS; PEDERSEN TF, 1983, GEOLOGY, V11, P16, DOI 10.1130/0091-7613(1983)11<16:IPITEE>2.0.CO;2; PETRIE B, 1996, CAN TECH REP HYDROGR, V78; Platon E, 2005, MAR MICROPALEONTOL, V54, P263, DOI 10.1016/j.marmicro.2004.12.004; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Rabalais NN, 2001, J ENVIRON QUAL, V30, P320, DOI 10.2134/jeq2001.302320x; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Rochon A, 1999, AM ASS STRATIGR PALY, V35; Rodrigues C. 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J	Parrow, MW; Elbrächter, M; Krause, MK; Burkholder, JM; Deamer, NJ; Htyte, N; Allen, EH				Parrow, M. W.; Elbraechter, M.; Krause, M. K.; Burkholder, J. M.; Deamer, N. J.; Htyte, N.; Allen, E. H.			The taxonomy and growth of a <i>Crypthecodinium</i> species (Dinophyceae) isolated from a brackish-water fish aquarium	AFRICAN JOURNAL OF MARINE SCIENCE			English	Article; Proceedings Paper	11th International Conference on Harmful Algae	NOV 15-19, 2004	Cape Town, SOUTH AFRICA			Crypthecodinium; dinoflagellate; phylogeny; small sub-unit rDNA; taxonomy; theca	ALGA PORPHYRIDIUM SP; CELL-CYCLE; COHNII; COMPLEX; MEMBERS	An unidentified heterotrophic dinoflagellate found growing in abundance in a brackish-water fish aquarium was isolated and serially cultivated using a fish cell line as the food source. Prominent characteristics of this dinoflagellate included a cingulum that did not fully encircle the motile cell, cell division in non-motile cysts, and a theca composed of thin but structured plates. Morphological analysis of flagellate cells by scanning electron microscopy revealed a Kofoid thecal plate tabulation of 4', 4a, 4", 'X', 5 or 6c, ?s, 5"', 1p, 1'''', most consistent with the original description of Crypthecodinium setense Biecheler. This Crypthecodinium species exhibited a high maximum division rate (3.2 divisions day(-1)) and cell yield (> 10(6) cells ml(-1)) when fed cultured fish cells. Small sub-unit rDNA phylogenetic analyses supported relatedness with a previously studied Crypthecodinium-like dinoflagellate, but a significant difference in aligned gene sequences was found. This study provides the first clear demonstration of the plate tabulation of a Crypthecodinium species since the original description over 60 years ago, allowing the original morphological conception of Crypthecodinium to be linked with molecular phylogenetic information.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA; Deutsch Zentrum Marine Biodiversitatsforsch, Forschungsinst Senckenberg, D-25992 List Auf Sylt, Germany; 114 Hofstra Univ, Dept Biol, Hempstead, NY 11549 USA	North Carolina State University; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Hofstra University	Parrow, MW (通讯作者)，N Carolina State Univ, Ctr Appl Aquat Ecol, 620 Hutton St,Suite 104, Raleigh, NC 27606 USA.	mwparrow@email.uncc.edu	Parrow, Matthew/HMO-6676-2023	Allen, Elle/0009-0001-3560-1768; Parrow, Matthew/0000-0002-3197-2510				[Anonymous], ACTA SOC BOT POL; BARLOW SB, 1986, J HISTOCHEM CYTOCHEM, V34, P1021, DOI 10.1177/34.8.3016072; Beam C.A., 1984, P263; BEAM CA, 1977, J PROTOZOOL, V24, P532, DOI 10.1111/j.1550-7408.1977.tb01007.x; BEAM CA, 1993, J EUKARYOT MICROBIOL, V40, P660, DOI 10.1111/j.1550-7408.1993.tb06124.x; BEAM CA, 1982, J PROTOZOOL, V29, P8, DOI 10.1111/j.1550-7408.1982.tb02874.x; BHAUD Y, 1994, J EUKARYOT MICROBIOL, V41, P519, DOI 10.1111/j.1550-7408.1994.tb06052.x; Bhaud Y, 2000, J CELL SCI, V113, P1231; Biecheler B., 1938, Bulletin de la Societe Zoologique de France, V63, P9; Biecheler B., 1952, Bull. Biol. Fr. Belg., V36, P1; CHATTON E, 1952, B SOC ZOOLOGIQUE FRA, P309; Chatton E., 1952, TRAITE ZOOL, P309; Elbrächter M, 2001, NEUES JAHRB GEOL P-A, V219, P221, DOI 10.1127/njgpa/219/2001/221; FENSOME RA, 1993, MICROPALENOTOLOGY SP, V7; GAJADHAR AA, 1991, MOL BIOCHEM PARASIT, V45, P147, DOI 10.1016/0166-6851(91)90036-6; JAVORNICKY PAVEL, 1962, PRESLIA [PRAHA], V34, P98; Kumar S, 2004, BRIEF BIOINFORM, V5, P150, DOI 10.1093/bib/5.2.150; Lam CMC, 2001, J PHYCOL, V37, P79, DOI 10.1046/j.1529-8817.2001.037001079.x; Murray S, 2005, PROTIST, V156, P269, DOI 10.1016/j.protis.2005.05.003; Parrow MW, 2005, AQUAT MICROB ECOL, V39, P97, DOI 10.3354/ame039097; PERRET E, 1993, J CELL SCI, V104, P639; Saldarriaga JF, 2004, EUR J PROTISTOL, V40, P85, DOI 10.1016/j.ejop.2003.11.003; Saldarriaga JF, 2001, J MOL EVOL, V53, P204, DOI 10.1007/s002390010210; STEIN F, 1883, ORGANISUMS INFUSIONS; TUTTLE R C, 1975, Phycologia, V14, P1, DOI 10.2216/i0031-8884-14-1-1.1; Ucko M, 1997, EUR J PHYCOL, V32, P133; UCKO M, 1989, APPL ENVIRON MICROB, V55, P2990, DOI 10.1128/AEM.55.11.2990-2994.1989	27	9	14	1	14	NATL INQUIRY SERVICES CENTRE PTY LTD	GRAHAMSTOWN	19 WORCESTER STREET, PO BOX 377, GRAHAMSTOWN 6140, SOUTH AFRICA	1814-232X			AFR J MAR SCI	Afr. J. Mar. Sci.	SEP	2006	28	2					185	191		10.2989/18142320609504145	http://dx.doi.org/10.2989/18142320609504145			7	Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	091TA					2025-03-11	WOS:000241050000003
J	Amorim, A; Dale, B				Amorim, A.; Dale, B.			Historical cyst record as evidence for the recent introduction of the dinoflagellate <i>Gymnodinium catenatum</i> in the north-eastern Atlantic	AFRICAN JOURNAL OF MARINE SCIENCE			English	Article; Proceedings Paper	11th International Conference on Harmful Algae	NOV 15-19, 2004	Cape Town, SOUTH AFRICA			ballast water introduction; cysts; eutrophication; Gymnodinium catenatum		The geographical origin of the warm-temperate paralytic shellfish poison producer Gymnodinium catenatum Graham is still under debate. It was first reported in the north-eastern Atlantic in 1976, from the Galician rias (North-West Iberia). Since then, and until 1995, recurrent blooms were recorded, with north-south progression of the affected areas, eventually affecting the whole West and South Atlantic coasts of Iberia and the Moroccan coast. This study presents results obtained from cyst analyses of a (210)Pb-dated box core and a (14)C-dated piston core, collected off Iberia, covering the last 2 000 years. They indicate that G catenatum is not endemic to the area but has been introduced around the beginning of the last century, coinciding with another major environmental change, possibly related to cultural eutrophication.	Univ Lisbon, Fac Ciencias, Inst Oceanog, P-1749016 Lisbon, Portugal; Univ Oslo, Dept Geosci, N-0316 Oslo, Norway	Universidade de Lisboa; University of Oslo	Amorim, A (通讯作者)，Univ Lisbon, Fac Ciencias, Inst Oceanog, P-1749016 Lisbon, Portugal.	ajamorim@fc.ul.pt	Amorim, Ana/AAA-2615-2020	Amorim, Ana/0000-0002-9612-4280				Abrantes F, 2005, QUATERNARY SCI REV, V24, P2477, DOI 10.1016/j.quascirev.2004.04.009; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1988, J PHYCOL, V24, P255; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Dale B, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P207; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; ESTRADA M, 1984, INVEST PESQ, V48, P31; Franca S., 1989, P93; Graham Herbert W, 1943, TRANS AMER MICROSC SOC, V62, P259, DOI 10.2307/3223028; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; Irwin A, 2003, HARMFUL ALGAE, V2, P61, DOI 10.1016/S1568-9883(02)00084-7; JOULEI LT, 1998, HARMFUL ALGAE XUNTA, P66; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; MCMINN A, 2001, HARMFUL ALGAL BLOOMS, P477; Moita M.T., 2001, Harmful Algal Blooms 2000, P169; MOITA MT, 1993, DEV MAR BIO, V3, P299; Moita MT., 1998, Harmful Algae, P118; Mudie PJ, 2002, PALAEOGEOGR PALAEOCL, V180, P159, DOI 10.1016/S0031-0182(01)00427-8	20	31	34	1	11	NATL INQUIRY SERVICES CENTRE PTY LTD	GRAHAMSTOWN	19 WORCESTER STREET, PO BOX 377, GRAHAMSTOWN 6140, SOUTH AFRICA	1814-232X			AFR J MAR SCI	Afr. J. Mar. Sci.	SEP	2006	28	2					193	197		10.2989/18142320609504146	http://dx.doi.org/10.2989/18142320609504146			5	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	091TA					2025-03-11	WOS:000241050000004
J	Joyce, LB; Pitcher, GC				Joyce, L. B.; Pitcher, G. C.			Cysts of <i>Alexandrium catenella</i> on the west coast of South Africa:: distribution and characteristics of germination	AFRICAN JOURNAL OF MARINE SCIENCE			English	Article; Proceedings Paper	11th International Conference on Harmful Algae	NOV 15-19, 2004	Cape Town, SOUTH AFRICA			Alexandrium catenella; cysts; southern Benguela	GONYAULAX-TAMARENSIS; RESTING CYSTS; DINOPHYCEAE; SCRIPPSIELLA; TEMPERATURE; DARKNESS	Cysts of the toxic dinoflagellate Alexandrium catenella (Whedon and Kofoid) Balech were found in the sediments of the southern Namaqua shelf, on the west coast of South Africa, with a maximum recorded abundance of 238 cysts ml(-1) wet sediment. Experimental results indicate a short dormancy period of 15-18 days, suggesting that the cyst population does not necessarily serve as an overwintering strategy, but may rather permit rapid cycling between benthic and planktonic stages. Cysts were isolated monthly from sediments and incubated in the laboratory. Cyst germination ranged between 20% and 88% and did not show a clear seasonal pattern. The rate of germination was examined as a function of temperature and light. Cysts germinated within the temperature range 4 degrees-22 degrees C, but germination was highest at 10 degrees C under both light and dark conditions. Although cysts germinated in the dark, germination in the light was higher and required a shorter period of incubation.	Marine & Coastal Management, Dept Environm Affairs & Tourism, ZA-8012 Cape Town, South Africa; Univ Cape Town, Dept Oceanog, ZA-7701 Rondebosch, South Africa	University of Cape Town	Pitcher, GC (通讯作者)，Marine & Coastal Management, Dept Environm Affairs & Tourism, Private Bag X2, ZA-8012 Cape Town, South Africa.	gpitcher@deat.gov.za						ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; BINDER BJ, 1987, J PHYCOL, V23, P99; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CANNON JA, 1993, DEV MAR BIO, V3, P103; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Pitcher GC, 2001, J SHELLFISH RES, V20, P895; Pitcher GC, 2000, S AFR J MARINE SCI, V22, P255, DOI 10.2989/025776100784125681; Pitcher GC, 1998, MAR ECOL PROG SER, V172, P253, DOI 10.3354/meps172253; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x	18	16	17	1	10	NATL INQUIRY SERVICES CENTRE PTY LTD	GRAHAMSTOWN	19 WORCESTER STREET, PO BOX 377, GRAHAMSTOWN 6140, SOUTH AFRICA	1814-232X	1814-2338		AFR J MAR SCI	Afr. J. Mar. Sci.	SEP	2006	28	2					295	298		10.2989/18142320609504165	http://dx.doi.org/10.2989/18142320609504165			4	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	091TA					2025-03-11	WOS:000241050000023
J	Juliano, VB; T Garcia, VM				Juliano, V. B.; T Garcia, V. M.			Cysts of potentially harmful dinoflagellates, with emphasis on the genus <i>Alexandrium</i>, in Sepetiba Bay (Brazil) during a port survey of GloBallast	AFRICAN JOURNAL OF MARINE SCIENCE			English	Article; Proceedings Paper	11th International Conference on Harmful Algae	NOV 15-19, 2004	Cape Town, SOUTH AFRICA			Alexandrium; ballast water; dinoflagellate cysts; Sepetiba Bay	TRANSPORT	Sepetiba Bay in south-eastern Brazil has been selected as a pilot demonstration site within the Global Ballast Water Management Programme (GloBallast; IMO/PNUD/ GEF). As part of the port baseline survey, a series of 43 sediment cores was taken in triplicate in the bay in November 2001, by SCUBA divers, using PVC tubes. The top 60mm of each core was processed for dinoflagellate cyst analysis. Cysts of the potentially toxic Alexandrium cf. minutum were identified in 41% of the samples, but the highest density (22 cysts cm(-3)) was found in the port area, at the Iron Ore Terminal. Other Alexandrium-type cysts were observed in 37% of the samples and their highest density (26 cysts cm(-3)) was also associated with the port area. These results indicate that the northern area of the bay is unsuitable for the intake by ships of ballast water. This investigation highlights the importance of cyst surveys to the management of ballasting and deballasting in port areas.	Museu Ciencias Nat, Fundacao Zoobot Rio Grande Do Sul, BR-90690000 Rio Grande Do Sul, Brazil; Fundacao Univ Fed Rio Grande, Dept Oceanog, BR-96201900 Rio Grande RS, Brazil	Universidade Federal do Rio Grande	Juliano, VB (通讯作者)，Museu Ciencias Nat, Fundacao Zoobot Rio Grande Do Sul, Rua Dr Salvador Franca 1427,Jardim Bot, BR-90690000 Rio Grande Do Sul, Brazil.	vivijuliano@hotmail.com	Tavano, Virginia/C-5241-2013	Tavano, Virginia/0000-0003-0039-8111				Balech E, 2002, FLORACIONES ALGALES, P123; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; FORBES JR, 1999, RED TIDE NEWSLETTER, V3, P2; GRINDLEY J R, 1968, South African Journal of Science, V64, P420; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEWITT CL, 2001, 22 CSRIO MAR RES CTR; JULIANO VB, 2003, THESIS FUNDACAO U FE; Landsberg JH, 2002, REV FISH SCI, V10, P113, DOI 10.1080/20026491051695; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATSUOKA K, 2000, WESTPACHABWESPAC10C; MATSUYAMA Y, 1995, PARAPLEGIA, V33, P381, DOI 10.1038/sc.1995.87; MOESTRUP O., 2004, IOC TAXONOMIC REFERE; Orozco F.E., 1989, P309; Persich GR, 2006, HARMFUL ALGAE, V5, P36, DOI 10.1016/j.hal.2005.04.002; PERSICH GR, 2003, ALANTICA RIO GRANDE, V25, P122; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1	19	5	5	1	8	NATL INQUIRY SERVICES CENTRE PTY LTD	GRAHAMSTOWN	19 WORCESTER STREET, PO BOX 377, GRAHAMSTOWN 6140, SOUTH AFRICA	1814-232X	1814-2338		AFR J MAR SCI	Afr. J. Mar. Sci.	SEP	2006	28	2					299	303		10.2989/18142320609504166	http://dx.doi.org/10.2989/18142320609504166			5	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	091TA					2025-03-11	WOS:000241050000024
J	Larsson, LM; Vajda, V; Rasmussen, ES				Larsson, Linda M.; Vajda, Vivi; Rasmussen, Erik S.			Early Miocene pollen and spores from western Jylland, Denmark - environmental and climatic implications	GFF			English	Article						Sonder Vium; Miocene; Denmark; palynology; paleoclimate; Taxodiaceae; Cupressaceae; swamp forest	UPPERMOST OLIGOCENE; STYRIAN BASIN; STRATIGRAPHY; PALYNOLOGY; PALYNOFACIES; PETROGRAPHY; SUCCESSION; VEGETATION; AUSTRIA; MODEL	A palynological analysis of a Lower Miocene cored section from Sonder Vium in western Jylland, Denmark, provides new data regarding the vegetation and climate during the earliest Neogene. Most samples yielded well-preserved palynomorphs. Terrestrial pollen and spores dominate, with lesser proportions of dinoflagellates. A fluvial input into the marine setting is corroborated by the presence of freshwater algae, indicating, an inner-neritic setting. A level containing comparatively abundant dinoflagellate cysts probably represents a transgressional event. The late Aquitanian age of the sequence as suggested by previous studies is supported by the composition of the palynoflora, e.g., by the presence of Ephedripites, Platycarya, and the relatively frequent occurrence of Engelhardtia. The pollen record is dominated by Taxodiaceae-Cupressaceae suggesting that swamp forests dominated the onshore region, which is consistent with previous results from central and northern Europe. Besides Taxodium, the swamp forest also contained angiosperm taxa such as Myricaceae, Nyssa, Betula, and Alnus. Elevated or better drained hinterland areas hosted a diverse mesophytic forest, with a ground cover of reeds, sedges and pteridophytes. Abundant pollen taxa derived from mesophytic forests indicates the presence of evergreen conifers, such as Pinus, Sequoia and Sciadopitys, and deciduous angiosperms, including Fagus and Quercus. A decrease in relative abundances of thermophilous elements such as Arecaceae (palms), Ilex, Mastixiaceae and Engelhardtia, in the middle part of the studied succession indicates a possible correlation to the late Aquitanian climatic deterioration. The composition of the palynological assemblages including widely distributed Taxodium swamps, suggests a warm, frost-free temperate climate during the Aquitanian in Denmark.	Lund Univ, Dept Geol, GeoBiosphere Sci Ctr, SE-22362 Lund, Sweden; Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen, Denmark	Lund University; Geological Survey Of Denmark & Greenland	Larsson, LM (通讯作者)，Lund Univ, Dept Geol, GeoBiosphere Sci Ctr, Solvegatan 12, SE-22362 Lund, Sweden.	linda.larsson@geol.lu.se	Vajda, Vivi/N-7693-2018	Vajda, Vivi/0000-0003-2987-5559				[Anonymous], 2007, Paleopalynology; Ashraf A. R., 1996, Palaeontographica Abteilung B Palaeophytologie, V241, P1; Ashraf A. 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J	Bowers, HA; Trice, TM; Magnien, RE; Goshorn, DM; Michael, B; Schaefer, EF; Rublee, PA; Oldach, DW				Bowers, Holly A.; Trice, T. Mark; Magnien, Robert E.; Goshorn, David M.; Michael, Bruce; Schaefer, Eric F.; Rublee, Parke A.; Oldach, David W.			Detection of <i>Pfiesteria</i> spp. by PCR in surface sediments collected from Chesapeake Bay tributaries (Maryland)	HARMFUL ALGAE			English	Article						PCR; Pfiesteria; sediment; Chesapeake Bay	PISCICIDA; DNA; AMPLIFICATION; POLYMERASE; DISCOVERY; IMPACTS; ASSAYS; GENE	In 1997 blooms of Pfiesteria piscicida occurred in association with fish kills and human health problems in tributaries of the Chesapeake Bay (Maryland) and the scientific and media response resulted in large economic losses in seafood sales and tourism. These events prompted the Maryland Department of Natural Resources (MDNR) to begin monitoring for Pfiesteria spp. in water column samples. Real-time PCR assays targeted to the 18S rRNA gene were developed by our laboratories and utilized in conjunction with traditional microscopy and fish kill bioassays for detection of these organisms in estuarine water samples. This monitoring strategy aided in determining temporal and spatial distribution of motile forms of Pfiesteria spp. (i.e. zoospores), but did not assess resting stages of the dinoflagellates' life cycle. To address this area, a 3-year study was designed using real-time PCR assays for analysis of surface sediment samples collected from several Chesapeake Bay tributaries. These samples were tested with the real-time PCR assays previously developed by our laboratories. The data reported herein suggest a strong positive association between presence of Pfiesteria spp. in the sediment and water column, based on long-term water column monitoring data. P. piscicida is detected more commonly in Maryland's estuarine waters than Pfiesteria shumwayae and sediment 'cyst beds' may exist for these organisms. (c) 2006 Published by Elsevier B.V.	Univ Maryland, Sch Med, Inst Human Virol, Baltimore, MD 21201 USA; Maryland Dept Nat Resources, Annapolis, MD 21401 USA; Univ N Carolina, Dept Biol, Greensboro, NC 27402 USA	University System of Maryland; University of Maryland Baltimore; University of North Carolina; University of North Carolina Greensboro	Oldach, DW (通讯作者)，Univ Maryland, Sch Med, Inst Human Virol, Room N557,725 W Lombard St, Baltimore, MD 21201 USA.	oldach@umbi.umd.edu						Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 1997, J ENVIRON QUAL, V26, P1451, DOI 10.2134/jeq1997.00472425002600060003x; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; GLIBERT PM, 2004, P 10 INT C HARM ALG, P74; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; HOLLAND PM, 1991, P NATL ACAD SCI USA, V88, P7276, DOI 10.1073/pnas.88.16.7276; Jakobsen KS, 2002, P ROY SOC B-BIOL SCI, V269, P211, DOI 10.1098/rspb.2001.1852; Joachimsthal EL, 2003, MAR POLLUT BULL, V46, P308, DOI 10.1016/S0025-326X(02)00401-0; Kreader CA, 1996, APPL ENVIRON MICROB, V62, P1102, DOI 10.1128/AEM.62.3.1102-1106.1996; Lewis PN, 2003, MAR POLLUT BULL, V46, P213, DOI 10.1016/S0025-326X(02)00364-8; LIPTON DW, 1998, P C EC POL OPT NUTR, P35; Magnien RE, 2001, ENVIRON HEALTH PERSP, V109, P711, DOI 10.2307/3454918; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; Saito K, 2002, APPL ENVIRON MICROB, V68, P5394, DOI 10.1128/AEM.68.11.5394-5407.2002; SCHAEFER EF, 1997, THESIS U N CAROLINA; SMALLA K, 1993, J APPL BACTERIOL, V74, P78, DOI 10.1111/j.1365-2672.1993.tb02999.x; Smol JP, 2000, J PHYCOL, V36, P986, DOI 10.1046/j.1529-8817.2000.00049.x; Stults JR, 2001, APPL ENVIRON MICROB, V67, P2781, DOI 10.1128/AEM.67.6.2781-2789.2001; Wittwer CT, 1997, BIOTECHNIQUES, V22, P130, DOI 10.2144/97221bi01; Zhang H, 2002, APPL ENVIRON MICROB, V68, P989, DOI 10.1128/AEM.68.2.989-994.2002	25	20	22	1	13	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	SEP	2006	5	4					342	351		10.1016/j.hal.2005.09.005	http://dx.doi.org/10.1016/j.hal.2005.09.005			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	077KI					2025-03-11	WOS:000240027800002
J	Coyne, KJ; Hare, CE; Popels, LC; Hutchins, DA; Cary, SC				Coyne, Kathryn J.; Hare, Clinton E.; Popels, Linda C.; Hutchins, David A.; Cary, S. Craig			Distribution of <i>Pfiesteria piscicida</i> cyst populations in sediments of the Delaware Inland Bays, USA	HARMFUL ALGAE			English	Article						cyst; Delaware Inland Bays; dinoflagellate; PCR; Pfiesteria; sediments	REAL-TIME PCR; ALGA AUREOCOCCUS-ANOPHAGEFFERENS; DINOFLAGELLATE CYSTS; GONYAULAX-TAMARENSIS; MOLECULAR TECHNIQUES; COMMUNITY STRUCTURE; SPRING BLOOM; GERMINATION; ASSAYS; DNA	The toxic dinoflagellate, Pfiesteria piscicida, is a common constituent of the phytoplankton community in the Delaware Inland Bays, USA. In this study, molecular methods were used to investigate the distributions of benthic stages (cysts) of P piscicida in sediment cores from the Delaware Inland Bays. Cores from 35 sites were partitioned into nephloid and anoxic layers and analyzed for P piscicida by nested amplification of the 18S rDNA gene using P. piscicida-specific primers. The presence of inhibitory substances in the PCR reaction was evaluated by inclusion of an exogenous control DNA in the extraction buffer, thus eliminating samples that may yield false-negative results. Our results indicate a patchy distribution of R piscicida in sediments of the Delaware Inland Bays, with distinct differences between each of the three bays. Overall, P. piscicida was found more frequently in sediments from Rehoboth Bay compared to Indian River and Little Assawoman Bays. These differences suggest (i) that populations of P. piscicida may be more widely distributed in Rehoboth Bay, (ii) that populations of P. piscicida may have been introduced to Rehoboth Bay at an earlier time, (iii) that past blooms of P. piscicida in Rehoboth Bay estuaries may have seeded the sediments with higher numbers of cysts, and/or (iv) that Rehoboth Bay sediments may be more resistant to clearing due to storm turbulence. (c) 2006 Elsevier B.V. All rights reserved.	Univ Delaware, Coll Marine Studies, Lewes, DE 19958 USA; Univ Waikato, Sch Sci & Engn, Hamilton, New Zealand	University of Delaware; University of Waikato	Coyne, KJ (通讯作者)，Univ Delaware, Coll Marine Studies, 70 Pilottown Rd, Lewes, DE 19958 USA.	kcoyne@udel.edu	; Hutchins, David/D-3301-2013	Cary, Stephen/0000-0002-2876-2387; Coyne, Kathryn/0000-0001-8846-531X; Hutchins, David/0000-0002-6637-756X				Anderson D.M., 1985, P219; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; Caron DA, 1999, HYDROBIOLOGIA, V401, P215, DOI 10.1023/A:1003721923719; Coyne KJ, 2005, LIMNOL OCEANOGR-METH, V3, P381, DOI 10.4319/lom.2005.3.381; Coyne KJ, 2005, J EUKARYOT MICROBIOL, V52, P90, DOI 10.1111/j.1550-7408.2005.05202001.x; Coyne KJ, 2001, AQUAT MICROB ECOL, V24, P275, DOI 10.3354/ame024275; Dale B., 1983, P69; Dempster EL., 1999, BIOTECHNIQUES, V27, P66; Díez B, 2001, APPL ENVIRON MICROB, V67, P2942, DOI 10.1128/AEM.67.7.2942-2951.2001; Doblin M.A., 2004, Harmful Algae 2002, P317; Doblin MA, 2004, APPL ENVIRON MICROB, V70, P6495, DOI 10.1128/AEM.70.11.6495-6500.2004; Godhe Anna, 2002, Harmful Algae, V1, P361, DOI 10.1016/S1568-9883(02)00053-7; Handy SM, 2005, AQUAT MICROB ECOL, V40, P121, DOI 10.3354/ame040121; Hare CE, 2005, HARMFUL ALGAE, V4, P221, DOI 10.1016/j.hal.2004.03.001; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; *HORS WITT INC, 1998, ASS NITR LOAD DEL IN; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; LU X, 1994, ESTUAR COAST SHELF S, V39, P353, DOI 10.1006/ecss.1994.1069; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; MEDLIN L, 1988, GENE, V71, P491, DOI 10.1016/0378-1119(88)90066-2; Miserez R, 1997, MOL CELL PROBE, V11, P103, DOI 10.1006/mcpr.1996.0088; Popels LC, 2003, LIMNOL OCEANOGR-METH, V1, P92, DOI 10.4319/lom.2003.1.92; Price KS, 1998, ENVIRON MONIT ASSESS, V51, P285, DOI 10.1023/A:1005951706152; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rozan TF, 2002, LIMNOL OCEANOGR, V47, P1346, DOI 10.4319/lo.2002.47.5.1346; Rublee PA, 2005, J EUKARYOT MICROBIOL, V52, P83, DOI 10.1111/j.1550-7408.2005.05202007.x; Saito K, 2002, APPL ENVIRON MICROB, V68, P5394, DOI 10.1128/AEM.68.11.5394-5407.2002; Scholin C.A., 1998, PHYSL ECOLOGY HARMFU, P337; STEIDINGER KA, 1975, ENVIRON LETT, V9, P129, DOI 10.1080/00139307509435842; Stoecker DK, 2000, AQUAT MICROB ECOL, V22, P261, DOI 10.3354/ame022261; Taillefert M, 2002, ANAL TRACE ELEMENTAL, P247; TEBBE CC, 1993, APPL ENVIRON MICROB, V59, P2657, DOI 10.1128/AEM.59.8.2657-2665.1993; Theron J, 2000, CRIT REV MICROBIOL, V26, P37, DOI 10.1080/10408410091154174; WESTON RF, 1983, CHARACTERIZATION INL; WONG KC, 1987, J PHYS OCEANOGR, V17, P413, DOI 10.1175/1520-0485(1987)017<0413:TASVID>2.0.CO;2; WONG KC, 1991, J GEOPHYS RES-OCEANS, V96, P8797, DOI 10.1029/90JC02471; Zhang H, 2005, APPL ENVIRON MICROB, V71, P7053, DOI 10.1128/AEM.71.11.7053-7063.2005	52	14	21	1	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	SEP	2006	5	4					363	373		10.1016/j.hal.2005.07.008	http://dx.doi.org/10.1016/j.hal.2005.07.008			11	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	077KI					2025-03-11	WOS:000240027800004
J	Shumway, SE; Burkholder, JM; Springer, J				Shumway, Sandra E.; Burkholder, JoAnn M.; Springer, Jeffrey			Effects of the estuarine dinoflagellate <i>Pfiesteria shumwayae</i> (Dinophyceae) on survival and grazing activity of several shellfish species	HARMFUL ALGAE			English	Article						Argopecten irradians; Crassostrea virginica; cyst; dinoflagellate; grazing; Geukensia demissa; Mercenaria mercenaria; Perna viridis; Pfiesteria shumwayae; shellfish; toxigenic	TOXIC PFIESTERIA; HETEROCAPSA-CIRCULARISQUAMA; PROTOGONYAULAX-TAMARENSIS; PARASITIC DINOFLAGELLATE; DOMINANCE HIERARCHIES; FISH BIOASSAY; CRAB DISEASE; GUT PASSAGE; PHYTOPLANKTON; PISCICIDA	A series of experiments was conducted to examine effects of four strains of the estuarine dinoflagellate, Pfiesteria shumwayae, on the behavior and survival of larval and adult shellfish (bay scallop, Argopecten irradians; eastern oyster, Crassostrea virginica; northern quahogs, Mercenaria mercenaria; green mussels, Perna viridis [adults only]). In separate trials with larvae of A. irradians, C. virginica, and M. mercenaria, an aggressive predatory response of three strains of algal- and fish-fed P. shumwayae was observed (exception, algal-fed strain 1024C). Larval mortality resulted primarily from damage inflicted by physical attack of the flagellated cells, and secondarily from Pfiesteria toxin, as demonstrated in larval C virginica exposed to P shumwayae with versus without direct physical contact. Survival of adult shellfish and grazing activity depended upon the species and the cell density, strain, and nutritional history of P. shumwayae. No mortality of the four shellfish species was noted after 24 h of exposure to algal- or fish-fed P. shumwayae (strains 1024C, 1048C, and CCMP2089) in separate trials at <= 5 x 10(3) cells ml(-1), whereas higher densities of fish-fed, but not algal-fed, populations (> 7-8 x 10(3) cells ml(-1)) induced low (<= 15%) but significant mortality. Adults of all four shellfish species sustained > 90% mortality when exposed to fish-fed strain 270A1 (8 x 10(3) cells ml(-1)). In contrast, adult M. mercenaria and P viridis exposed to a similar density of fish-fed strain 2172C sustained < 15% mortality, and there was no mortality of A. irradians and C. virginica exposed to that strain. In mouse bioassays with tissue homogenates (adductor muscle, mantle, and whole animals) of A. irradians and M. mercenaria that had been exposed to R shumwayae (three strains, separate trials), mice experienced several minutes of disorientation followed by recovery. Mice injected with tissue extracts from control animals fed cryptomonads showed no response. Grazing rates of adult shellfish on P. shumwayae (mean cell length +/- 1 standard error [S.E.], 9 +/- 1 mu m) generally were significantly lower when fed fish-fed (toxic) populations than when fed populations that previously had been maintained on algal prey, and grazing rates were highest with the nontoxic cryptomonad, Storeatula major (cell length 7 +/- 1 mu m). Abundant cysts of P. shumwayae were found in fecal strands of all shellfish species tested, and <= 45% of the feces produced viable flagellated cells when placed into favorable culture conditions. These findings were supported by a field study wherein fecal strands collected from field-collected adult shellfish (C virginica, M. mercenaria, and ribbed mussels, Geukensia demissa) were confirmed to contain cysts of P. shumwayae, and these cysts produced fish-killing flagellated populations in standardized fish bioassays. Thus, predatory feeding by flagellated cells of R shumwayae can adversely affect survival of larval bivalve molluscs, and grazing can be depressed when adult shellfish are fed P. shumwayae. The data suggest that R shumwayae could affect recruitment of larval shellfish in estuaries and aquaculture facilities; shellfish can be adversely affected via reduced filtration rates; and adult shellfish may be vectors of toxic P shumwayae when shellfish are transported from one geographic location to another. (c) 2006 Elsevier B.V. All rights reserved.	Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA	University of Connecticut; North Carolina State University	Shumway, SE (通讯作者)，Univ Connecticut, Dept Marine Sci, 1080 Shennescossett Rd, Groton, CT 06340 USA.	sandra.shumway@uconn.edu						[Anonymous], PHILLIPP J BIOL; Bauder AG, 2000, J SHELLFISH RES, V19, P321; Berry JP, 2002, P NATL ACAD SCI USA, V99, P10970, DOI 10.1073/pnas.172221699; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Brand A.R., 1991, Developments in Aquaculture and Fisheries Science, V21, P517; BRICELJ VM, 1991, MAR ECOL PROG SER, V74, P33, DOI 10.3354/meps074033; Burkholder J, 2004, P NATL ACAD SCI USA, V101, P9291, DOI 10.1073/pnas.0306842101; Burkholder JM, 2005, P NATL ACAD SCI USA, V102, P3471, DOI 10.1073/pnas.0500168102; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P667, DOI 10.2307/3454912; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P745, DOI 10.2307/3454922; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; Burkholder JM, 1998, ECOL APPL, V8, pS37; BURKHOLDER JM, 1992, LIMNOL OCEANOGR, V37, P974, DOI 10.4319/lo.1992.37.5.0974; Burkholder JM, 2006, LIMNOL OCEANOGR, V51, P463, DOI 10.4319/lo.2006.51.1_part_2.0463; Cancellieri PJ, 2001, J EXP MAR BIOL ECOL, V264, P29, DOI 10.1016/S0022-0981(01)00299-4; CARRIKER MR, 1951, ECOL MONOGR, V21, P19, DOI 10.2307/1948644; CASTAGNA M, 1973, Malacologia, V12, P47; CUKER BE, 1990, LIMNOL OCEANOGR, V35, P830, DOI 10.4319/lo.1990.35.4.0830; de Bravo MIS, 1998, REV BIOL TROP, V46, P121; Eckman JE, 1996, J EXP MAR BIOL ECOL, V200, P207, DOI 10.1016/S0022-0981(96)02644-5; Eversole AG, 2001, DEV AQUAC FISH SCI, V31, P221; Fielding A., 1987, An underwater guide to Hawai'i; GAINEY L F JR, 1988, Journal of Shellfish Research, V7, P623; GAINEY LF, 1991, BIOL BULL, V181, P298, DOI 10.2307/1542101; GAINEY LF, 1988, COMP BIOCHEM PHYS C, V91, P159, DOI 10.1016/0742-8413(88)90182-X; Glasgow HB, 2001, ENVIRON HEALTH PERSP, V109, P715, DOI 10.2307/3454919; Gordon A. 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J	Lin, SJ; Zhang, H; Hou, Y; Miranda, L; Bhattacharya, D				Lin, Senjie; Zhang, Huan; Hou, Yubo; Miranda, Lilibeth; Bhattacharya, Debashish			Development of a dinoflagellate-oriented PCR primer set leads to detection of picoplanktonic dinoflagellates from long island sound	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							DINOPHYCEAE; SEQUENCES; GENOME; CYST	We developed dinoflagellate-specific 18S rRNA gene primers. PCR amplification using these oligonucleotides for a picoplanktonic DNA sample from Long Island Sound yielded 24 clones, and all but one of these clones were dinoflagellates primarily belonging to undescribed and Amoebophrya-like lineages. These results highlight the need for a systematic investigation of picodinoflagellate diversity in both coastal and oceanic ecosystems.	Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA; Univ Iowa, Dept Sci Biol, Iowa City, IA 52242 USA; Univ Iowa, Roy J Carver Ctr Comparat Genom, Iowa City, IA 52242 USA	University of Connecticut; University of Iowa; University of Iowa	Lin, SJ (通讯作者)，Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA.	senjie.lin@uconn.edu	Lin, Senjie/A-7466-2011					BERHEY C, 2004, BMC BIOL, V2, P13; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; de Salas MF, 2003, J PHYCOL, V39, P1233, DOI 10.1111/j.0022-3646.2003.03-019.x; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; Guindon S, 2003, SYST BIOL, V52, P696, DOI 10.1080/10635150390235520; Hackett JD, 2005, BMC GENOMICS, V6, DOI 10.1186/1471-2164-6-80; Hackett JD, 2004, AM J BOT, V91, P1523, DOI 10.3732/ajb.91.10.1523; Huber T, 2004, BIOINFORMATICS, V20, P2317, DOI 10.1093/bioinformatics/bth226; Hugenholtz P, 2003, INT J SYST EVOL MICR, V53, P289, DOI 10.1099/ijs.0.02441-0; Jeong HJ, 2005, J EUKARYOT MICROBIOL, V52, P382, DOI 10.1111/j.1550-7408.2005.00051.x; KIMURA M, 1980, J MOL EVOL, V16, P111, DOI 10.1007/BF01731581; LaJeunesse TC, 2005, J PHYCOL, V41, P880, DOI 10.1111/j.0022-3646.2005.04231.x; López-García P, 2001, NATURE, V409, P603, DOI 10.1038/35054537; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; Moon-van der Staay SY, 2001, NATURE, V409, P607, DOI 10.1038/35054541; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Saldarriaga JF, 2003, INT J SYST EVOL MICR, V53, P355, DOI 10.1099/ijs.0.02328-0; Saunders GW, 1997, PLANT SYST EVOL, P237; Smith GA, 2004, REV PALAEOBOT PALYNO, V128, P355, DOI 10.1016/S0034-6667(03)00155-6; TAYLOR FJR, 1987, BIOL DINOFLAGELLATES, P143; Wright ADG, 2002, EUR J PROTISTOL, V37, P375, DOI 10.1078/0932-4739-00858; Zhang H, 2005, APPL ENVIRON MICROB, V71, P7053, DOI 10.1128/AEM.71.11.7053-7063.2005; Zhang H, 2005, J PHYCOL, V41, P411, DOI 10.1111/j.1529-8817.2005.04168.x	23	56	60	3	25	AMER SOC MICROBIOLOGY	WASHINGTON	1752 N ST NW, WASHINGTON, DC 20036-2904 USA	0099-2240	1098-5336		APPL ENVIRON MICROB	Appl. Environ. Microbiol.	AUG	2006	72	8					5626	5630		10.1128/AEM.00586-06	http://dx.doi.org/10.1128/AEM.00586-06			5	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	073ZC	16885319	Green Published			2025-03-11	WOS:000239780400062
J	Grosfjeld, K; Funder, S; Seidenkrantz, MS; Glaister, C				Grosfjeld, Kari; Funder, Svend; Seidenkrantz, Marit-Solveig; Glaister, Chris			Last interglacial marine environments in the White Sea region, northwestern Russia	BOREAS			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; SURFACE CONDITIONS; BARENTS SEA; BENTHIC FORAMINIFERA; ARKHANGELSK REGION; LATE QUATERNARY; ARCTIC-OCEAN; KOLJO FJORD; ICE-SHEET; NORTH	Marine sediments from river sections in the Mezen River drainage, northwest Russia, have been analysed for dinoflagellate cysts, foraminifers and molluscs. The sediments were dated by pollen analysis and by reference to the local sea-level history, and are Late Saalian to late Eemian ( c. 133 to 119.5 kyr in age). The Late Saalian deglaciation was characterized by Arctic conditions, but a few centuries into the Eemian the Gulf Stream system carried warm Atlantic water into the region. At 129.8 kyr BP there was a marked increase in the influx of Atlantic water, and the advection of warm Atlantic water was stronger and probably penetrated further eastwards than at present. The molluscs, dinoflagellate cysts and foraminifers reflect conditions warmer than present and that the optimum temperature occurred at the time of the early Eemian global sea-level rise. Around 128 kyr BP, the eustatic sea-level rise was curbed by isostatic rebound and accompanying regression and constriction of marine passages to the White Sea. Local, low-saline, stratified basins developed and characterized the next five to six millennia.	Geol Survey Norway, NO-7491 Trondheim, Norway; Univ Copenhagen, Geol Museum, DK-1350 Copenhagen K, Denmark; Univ Aarhus, Dept Earth Sci, DK-8000 Aarhus C, Denmark; Westlakes Sci Consulting, Moor Row CA24 3LN, Cumbria, England	Geological Survey of Norway; University of Copenhagen; Aarhus University	Grosfjeld, K (通讯作者)，Geol Survey Norway, NO-7491 Trondheim, Norway.	Kari.Grosfjeld@ngu.no	Seidenkrantz, Marit-Solveig/A-3451-2012	Seidenkrantz, Marit-Solveig/0000-0002-1973-5969				Bauch HA, 1999, PALAEOGEOGR PALAEOCL, V145, P95, DOI 10.1016/S0031-0182(98)00104-7; Berger V., 2001, White Sea. 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I., 1994, THESIS U TROMSO NORW, P61; Svendsen JI, 2004, QUATERNARY SCI REV, V23, P1229, DOI 10.1016/j.quascirev.2003.12.008; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Walton W.R., 1964, Approaches to Paleoecology, V151-237, P151; Wollenburg JE, 1998, MAR MICROPALEONTOL, V34, P153, DOI 10.1016/S0377-8398(98)00007-3; ZAGWIJN WH, 1983, GEOL MIJNBOUW, V62, P437; Zagwijn WH, 1996, QUATERNARY SCI REV, V15, P451, DOI 10.1016/0277-3791(96)00011-X; Zenkevitch L., 1963, BIOL SEAS USSR	77	47	50	0	9	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0300-9483	1502-3885		BOREAS	Boreas	AUG	2006	35	3					493	520		10.1080/03009480600781917	http://dx.doi.org/10.1080/03009480600781917			28	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	065WY					2025-03-11	WOS:000239192000006
J	Bravo, I; Garcés, E; Diogène, J; Fraga, S; Sampedro, N; Figueroa, RI				Bravo, Isabel; Garces, Esther; Diogene, Jorge; Fraga, Santiago; Sampedro, Nagore; Figueroa, Rosa I.			Resting cysts of the toxigenic dinofiagellate genus <i>Alexandrium</i> in recent sediments from the Western Mediterranean coast, including the first description of cysts of <i>A-kutnerae</i> and <i>A-peruvianum</i>	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Alexandrium; dinoflagellate cysts; Mediterranean sea	GONYAULAX-EXCAVATA; DINOPHYCEAE; MINUTUM; CATENELLA; TAMARENSIS; MORPHOLOGY; SEQUENCE; STRAIN; BLOOMS; WATERS	Cyst studies carried out in 2002-2003 on Mediterranean Sea sediment from seven different sites along the Catalan and Balearic coasts (Western Mediterranean) revealed a higher diversity of Alexandrium species in the region than was previously known. The cysts of eight species of the toxigenic, marine dinoflagellate genus Alexandrium are described, and some, such as A. kutnerae, A. margalefi, A. peruvianum and A. pseudogoniaulax, are reported from the area for the first time. This is also the first record of resting cysts of A. taylori in Mediterranean sediment, and the first description known to date of resting cysts for A. kutnerae and A. peruvianum. All the cysts were characterized by a smooth wall except for the paratabulated cyst of A. pseudogoniaulax, and most of them had a prominent yellow/orange accumulation body. Nevertheless, we have also detected an unparatabulated cyst of A. pseudogoniaulax, both from the sediment and in cultures. The cyst of A. kutnerae had a roughly cylindrical shape with rounded ends which makes it impossible to distinguish from resting cysts of A. tamarense and A. catenella, while the flattened round cysts of A. peruvianum were very similar to those of A. taylori. The cyst concentration data revealed A. catenella and A. minutum to be the most abundant cysts in the region, and they were detected in semi-enclosed waters, such as harbours. This highlights the importance of water exchange in the accumulation of cyst beds of these species, which has already been reported in the region by other authors for A. minutum. This paper contributes to the biogeographic distribution of some Alexandrium species, such as A. kutneare, A. margalefi, A. peruvianum and A. pseudogoniaulax, which have been reported only infrequently in a global context.	IEO, Vigo 36200, Spain; Inst Ciencias Mar, E-08003 Barcelona, Spain; Inst Recerca & Tecnol Agroalimentaria, Tarragona 43540, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); IRTA	Bravo, I (通讯作者)，IEO, Aptado 1552, Vigo 36200, Spain.	isabel.bravo@vi.ieo.es	Fraga, Santiago/AAA-3760-2020; Bravo, Isabel/D-3147-2012; Diogene, Jorge/AAB-8667-2019; Fraga, Santiago/C-8641-2012; Garces, Esther/C-5701-2011; SAMPEDRO, NAGORE/I-1767-2015; Figueroa, Rosa/M-7598-2015	Bravo, Isabel/0000-0003-3764-745X; Diogene, Jorge/0000-0002-6567-6891; Fraga, Santiago/0000-0003-3917-9960; Garces, Esther/0000-0002-2712-501X; SAMPEDRO, NAGORE/0000-0002-0829-5152; Figueroa, Rosa/0000-0001-9944-7993				Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Basterretxea G, 2005, ESTUAR COAST SHELF S, V62, P1, DOI 10.1016/j.ecss.2004.07.008; BELIN C, 1993, DEV MAR BIO, V3, P469; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; DELGADO M, 1990, Scientia Marina, V54, P1; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; FONT J., 1988, OCEANOL ACTA, VS-9, P51; Forteza V., 1998, HARMFUL ALGAE P 8 IN, P58; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1985, B MAR SCI, V37, P529; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; GENOVESIGIUNTI B, 2005, ASLO SUMM M 2005 JUN, P19; GIACOBBE MG, 1994, CRYPTOGAMIE ALGOL, V15, P47; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Giacobbe MG, 1996, ESTUAR COAST SHELF S, V42, P539, DOI 10.1006/ecss.1996.0035; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Halim Y., 1960, Vie et Milieu, V11, P102; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; HONSELL G, 1992, SCIENCE OF THE TOTAL ENVIRONMENT, SUPPLEMENT 1992, P107; Ismael AA, 2003, OCEANOLOGIA, V45, P721; John U, 2003, MOL BIOL EVOL, V20, P1015, DOI 10.1093/molbev/msg105; KEFI ODY, 2001, OCEANOL ACTA, V24, P17; KORAY T, 1988, Revue Internationale d'Oceanographie Medicale, V91-92, P25; Leaw CP, 2005, PHYCOLOGIA, V44, P550, DOI 10.2216/0031-8884(2005)44[550:PAOASA]2.0.CO;2; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; Luglie A., 2002, HARMFUL ALGAE, P329; MONTAGNA AA, 1995, CHEMTECH, V25, P44; PENNA A, 2000, HARMFUL ALGAL BLOOMS, P218; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; Turki S., 2005, Harmful Algae News, V28, P1; Vila M, 2005, HARMFUL ALGAE, V4, P673, DOI 10.1016/j.hal.2004.07.006; Vila M, 2001, J PLANKTON RES, V23, P497, DOI 10.1093/plankt/23.5.497; Vila Magda, 2004, Rapport du Congress de la CIESM, V37, P455	40	80	81	0	15	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0967-0262			EUR J PHYCOL	Eur. J. Phycol.	AUG	2006	41	3					293	302		10.1080/09670260600810360	http://dx.doi.org/10.1080/09670260600810360			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	087PU		Bronze			2025-03-11	WOS:000240755200003
J	Band-Schmidt, C; Bustillos-Guzmán, J; Morquecho, L; Gárate-Lizárraga, I; Alonso-Rodríguez, R; Reyes-Salinas, A; Erler, K; Luckas, B				Band-Schmidt, Christine; Bustillos-Guzman, Jose; Morquecho, Lourdes; Garate-Lizarraga, Ismael; Alonso-Rodriguez, Rosalba; Reyes-Salinas, Amada; Erler, Katrin; Luckas, Bernd			Variations of PSP toxin profiles during different growth phases in <i>Gymnodinium catenatum</i> (Dinophyceae) strains isolated from three locations in the Gulf of California, Mexico	JOURNAL OF PHYCOLOGY			English	Article						chain length; dinoflagellate; growth rate; Gulf of California; Gymnodinium catenatum; paralytic shellfish toxins	BAHIA-CONCEPCION; SHELLFISH; ALEXANDRIUM; PHYTOPLANKTON; TEMPERATURE; SALINITY; GRAHAM; SEDIMENTS; TOXICITY; COAST	In vitro experiments were performed with Gymnodinium catenatum Graham strains isolated from three locations in the Gulf of California to determine the variability in toxicity and toxin profiles. Strains were cultivated in GSe at 20 degrees C +/- 1 degrees C, 150 mu mol photons(.)m(-2.)s(-1) (12:12 light:dark cycle), and harvested during different growth phases. Growth rates were higher than in previous studies, varying between 0.70 and 0.82 day(-1). The highest cell yields were reached at 16 and 19 days, with maximum densities between 1090 and 3393 cells(.)mL(-1). Bahia de La Paz (BAPAZ) and Bahia de Mazatlan (BAMAZ) were the most toxic (101 pg STXeq.cell(-1)), whereas strains from Bahia Concepcion (BACO) were the least toxic (13 pg STXeq(.)cell(-1)). A strain isolated from cyst germination was one of the least toxic strains. No significant changes in toxin content with culture age were observed (0.2 and 0.6 pmol paralytic shellfish poisoning.cell(-1)). All strains contained neosaxitoxin (NEOSTX), decarbamoyl-saxitoxin (dcSTX), decarbamoyl-gonyautoxin-2,-3, (dcGTX2-3), N-sulfo-carbamoylsaxitoxin (B1), N-sulfo-carbamoylneosaxitoxin (B2), and N-sulfo-carbamoylgonyautoxin-2,-3 (C1-2). Bahia Concepcion strains had the highest content of C1; BAPAZ and BAMAZ strains had a higher percentage of NEOSTX. Differences in toxin composition with culture age were observed only in BAMAZ and BAPAZ strains. Cultures with a higher percentage of long chains had more NEOSTX, while those with a higher proportion of short chains had a lower content of NEOSTX. Gulf of California strains are characterized by a high proportion of NEOSTX, and seem to have evolved particular physiological responses to their environment that are reflected in the toxin profile, suggesting different populations.	IPN, Ctr Interdisciplinario Ciencias Marinas, Dept Plancton & Ecol Marina, La Paz 23000, Mexico; Ctr Inves Biol Noroeste, La Paz 23000, Mexico; Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Unidad Acad Mazatlan, Mazatlan 8200, Mexico	Instituto Politecnico Nacional - Mexico; Universidad Nacional Autonoma de Mexico	Band-Schmidt, C (通讯作者)，IPN, Ctr Interdisciplinario Ciencias Marinas, Dept Plancton & Ecol Marina, AP 592, La Paz 23000, Mexico.	cbands@ipn.mx	Morquecho, Lourdes/JPY-0626-2023; Gárate-Lizárraga, Ismael/GRS-5815-2022; Alonso-Rodriguez, Rosalba/U-9896-2017	Alonso-Rodriguez, Rosalba/0000-0001-7716-3869; Band-Schmidt, Christine Johanna/0000-0002-8251-9820; Morquecho, Lourdes/0000-0003-2963-8836; Garate-Lizarraga, Ismael/0000-0002-3835-183X				ALONSORODRIGUEZ R, 2004, 13 REUN NAC SOC MEX, P54; ANDERSON DM, 1990, TOXIC MARINE PHYTOPLANKTON, P41; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1989, TOXICON, V27, P665, DOI 10.1016/0041-0101(89)90017-2; [Anonymous], 2006, ACTA BOT MEX, DOI DOI 10.21829/ABM74.2006.1008; [Anonymous], HARMFUL TOXIC ALGAL; Band-Schmidt CJ, 2004, J PLANKTON RES, V26, P1459, DOI 10.1093/plankt/fbh133; Band-Schmidt CJ, 2005, HARMFUL ALGAE, V4, P21, DOI 10.1016/j.hal.2003.10.004; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BOLCH CJ, 2001, LIFEHAB LIFE HIST MI, P37; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Bustillos-Guzmán J, 2000, J EXP MAR BIOL ECOL, V249, P77, DOI 10.1016/S0022-0981(00)00188-X; BYRNE JV, 1960, GEOL SOC AM BULL, V71, P983, DOI 10.1130/0016-7606(1960)71[983:SOTGOC]2.0.CO;2; CAMINOORDAS M, 2004, J PLANKTON RES, V26, P341; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; Cortes-Altamirano R, 1999, CIENC MAR, V7, P50; Cortes-Altamirano R, 1997, CIENC MAR, V15, P31; Cortes-Altamirano Roberto, 1995, Revista Latinoamericana de Microbiologia, V37, P343; Doblin MA, 1999, J PLANKTON RES, V21, P1153, DOI 10.1093/plankt/21.6.1153; Doblin MA, 2000, J PLANKTON RES, V22, P421, DOI 10.1093/plankt/22.3.421; ESTRADA M, 1984, INVEST PESQ, V48, P31; Flynn KJ, 1996, J PLANKTON RES, V18, P2093, DOI 10.1093/plankt/18.11.2093; Franca S., 1989, P93; FUKUYO Y, 1993, DEV MAR BIO, V3, P875; Garate Lizarraga I., 2003, Acta Botanica Mexicana, P1; Gárate-Lizárraga I, 2005, MAR POLLUT BULL, V50, P211, DOI 10.1016/j.marpolbul.2004.11.034; Gárate-Lizárraga I, 2004, REV BIOL TROP, V52, P133; Garate-Lizarraga Ismael, 2001, Oceanides, V16, P127; GARATELIZARRAGA I, 2004, MAR POLL B, V48, P378, DOI DOI 10.1016/J.MARP0LBUL.2003.10.032; GARATELIZARRAGA I, 2006, IN PRESS MAR POLL B; Gilbert JY, 1943, J MAR RES, V5, P89; GILMARTIN M, 1978, ESTUAR COAST MAR SCI, V7, P29, DOI 10.1016/0302-3524(78)90055-5; Gomez Fernando, 2003, Acta Botanica Croatica, V62, P65; GONGORAGONZALEZ D, 2001, THESIS U AUTONOMA BA; Graham Herbert W, 1943, TRANS AMER MICROSC SOC, V62, P259, DOI 10.2307/3223028; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; Hallegraeff G.M., 1989, P77; Holmes MJ, 2002, J PHYCOL, V38, P96, DOI 10.1046/j.1529-8817.2002.01153.x; Hummert C, 1997, CHROMATOGRAPHIA, V45, P312, DOI 10.1007/BF02505576; Ikeda T., 1989, P411; La Barbara-Sanchez A, 2001, J SHELLFISH RES, V20, P1257; Landsberg JH, 2002, REV FISH SCI, V10, P113, DOI 10.1080/20026491051695; Leal Sylvia, 2003, Revista de Investigaciones Marinas, V24, P155; Lechuga-Devéze CH, 2001, REV BIOL TROP, V49, P525; López-Cortés David J., 2003, Hidrobiológica, V13, P195; MACKENZIE L, 2001, GYMNODINIUM CATENATU; Manrique F.A., 1997, HIDROBIOLOGICA, V7, P81; Matsuoka K., 2000, GUIA TECNICA ESTUDIO; Mee L.D., 1985, TROP OCEAN ATMOS NEW, V31, P9; MEE LD, 1986, MAR ENVIRON RES, V19, P77, DOI 10.1016/0141-1136(86)90040-1; Morquecho L, 2004, BOT MAR, V47, P313, DOI 10.1515/BOT.2004.037; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; Negri A, 2003, CHEM RES TOXICOL, V16, P1029, DOI 10.1021/tx034037j; Negri A P., 2001, Harmful Algal Blooms 2000, P210; OLIVEIRAPROENZA LA, 2001, REV ATL RIO GRANDE, V23, P59; OSHIMA Y, 1993, DEV MAR BIO, V3, P907; OSHIMA Y, 1993, MAR BIOL, V116, P471, DOI 10.1007/BF00350064; Páez-Osuna F, 2003, MAR POLLUT BULL, V46, P806, DOI 10.1016/S0025-326X(03)00107-3; Park TG, 2004, PHYCOL RES, V52, P300; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; REGUERA B, 1990, TOXIC MARINE PHYTOPLANKTON, P316; RIEGMAN R, 1998, PHYSL ECOLOGY HARMFU, P475; RODEN GI, 1959, J MAR RES, V18, P10; RODEN GUNNAR I., 1958, PACIFIC SCI, V12, P21; RONSONPAULIN JA, 1999, CIENC MAR, V9, P40; ROUND F. E., 1967, J EXP MAR BIOL ECOL, V1, P76, DOI 10.1016/0022-0981(67)90008-1; Taleb H, 2001, TOXICON, V39, P1855, DOI 10.1016/S0041-0101(01)00167-2; Throndsen J., 1978, Preservation and storage, P69, DOI DOI 10.1111/J.0022-3646.1975.00142.X; Van Andel T., 1964, Marine geology of the Gulf of California, P216; VARGASMONTERO M, 2002, REV COSTARRIC CIENC, V23, P115; WHITE AW, 1986, TOXICON, V24, P605, DOI 10.1016/0041-0101(86)90181-9; Yamamoto T, 2002, FISHERIES SCI, V68, P356, DOI 10.1046/j.1444-2906.2002.00433.x; Yu RC, 1998, CHROMATOGRAPHIA, V48, P671, DOI 10.1007/BF02467597	74	39	39	0	26	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	AUG	2006	42	4					757	768		10.1111/j.1529-8817.2006.00234.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00234.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	066VR					2025-03-11	WOS:000239258900002
J	Pertola, S; Faust, MA; Kuosa, H				Pertola, Sari; Faust, Maria A.; Kuosa, Harri			Survey on germination and species composition of dinoflagellates from ballast tanks and recent sediments in ports on the South Coast of Finland, North-Eastern Baltic Sea	MARINE POLLUTION BULLETIN			English	Article						ballast water; Baltic Sea; dinoflagellate cyst; germination; Gulf of Finland; recent sediments in ports	PROROCENTRUM-MINIMUM DINOPHYCEAE; MARINE DINOFLAGELLATE; ALEXANDRIUM-TAMARENSE; RESTING CYSTS; HIROSHIMA BAY; TOXIN CONTENT; GROWTH; SALINITY; MORPHOLOGY; PLANKTON	Cyst beds in ships and ports in Finland have previously been unstudied. Therefore, sediments from ships' ballast water tanks and four Finnish ports were sampled for dinoflagellate cysts and other phytoplankton. Untreated sediments were incubated at 10 degrees C and 20 degrees C in the local 6 psu salinity for 1, 4 and 7 days, and vegetative cells were examined with light and scanning electron microscope. Sediments were inhabited by various dinoflagellates, diatoms, chlorophytes, cyanophytes and small flagellates. Germinated dinoflagellates were found in 90% of ballast tanks and in all ports. Gymnodiniales spp. and Heterocapsa rotundata formed a major proportion of the proliferating dinoflagellate cells. One species, Peridinium quinquecorne, not previously reported from the Baltic Sea, was identified with SEM. The study emphasises that ships are potential transport vehicles for dinoflagellate cysts even in the low salinity Finnish waters, and small-sized dinoflagellates should be focused upon in ballast water studies. (c) 2005 Elsevier Ltd. All rights reserved.	Finnish Inst Marine Res, Dept Biol Res, FI-00561 Helsinki, Finland; US Natl Herbarium, Dept Bot, Smithsonian Inst, Suitland, MD 20746 USA; Univ Helsinki, Tvarminne Zool Stn, FI-10900 Hango, Finland	Smithsonian Institution; University of Helsinki	Pertola, S (通讯作者)，Finnish Inst Marine Res, Dept Biol Res, POB 2, FI-00561 Helsinki, Finland.	sari.pertola@fimr.fi		Kuosa, Harri/0000-0002-9641-9054				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; [Anonymous], [No title captured]; [Anonymous], VTT PUBLICATIONS; [Anonymous], OCEAN CHALLENGE; AUTIO R, 1990, 19871989 PELAG; BARONCAMPIS SA, 2003, DINO7 7 INT C MOD FO, P24; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; CANNON JA, 1993, DEV MAR BIO, V3, P741; Dale B., 1983, P69; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Deeds Jonathan R., 2002, Harmful Algae, V1, P169, DOI 10.1016/S1568-9883(02)00027-6; DEMADARIAGA I, 1989, BOT MAR, V32, P159, DOI 10.1515/botm.1989.32.2.159; Dodge J.D., 1982, P1; Estrada M., 1998, Physiological Ecology of Harmful Algal Blooms, P601; Faust MA, 1998, J PHYCOL, V34, P173, DOI 10.1046/j.1529-8817.1998.340173.x; Finni T, 2001, AMBIO, V30, P172, DOI 10.1579/0044-7447-30.4.172; Grzebyk D, 2003, J PLANKTON RES, V25, P1185, DOI 10.1093/plankt/fbg088; Grzebyk D, 1996, J PLANKTON RES, V18, P1837, DOI 10.1093/plankt/18.10.1837; Guillard R. 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Pollut. Bull.	AUG	2006	52	8					900	911		10.1016/j.marpolbul.2005.11.028	http://dx.doi.org/10.1016/j.marpolbul.2005.11.028			12	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	086SN	16442131				2025-03-11	WOS:000240693400017
J	Ellegaard, M; Clarke, AL; Reuss, N; Drew, S; Weckström, K; Juggins, S; Anderson, NJ; Conley, DJ				Ellegaard, Marianne; Clarke, Annemarie L.; Reuss, Nina; Drew, Simon; Weckstrom, Kaarina; Juggins, Stephen; Anderson, N. John; Conley, Daniel J.			Multi-proxy evidence of long-term changes in ecosystem structure in a Danish marine estuary, linked to increased nutrient loading	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						anoxia; eutrophication; diatoms; dinoflagellate cysts; pigments; palaeoecology	DINOFLAGELLATE CYSTS; TOKYO-BAY; COASTAL WATERS; ORGANIC-MATTER; YOKOHAMA-PORT; LAND-USE; EUTROPHICATION; SEDIMENTS; FJORD; RECONSTRUCTION	This paper presents a study of changes in eutrophication over the past 100 years in a fertile estuary. The Danish estuary Mariager Fjord is a long, narrow sill-fjord with a permanently anoxic basin. In 1997 anoxia spread from the basin to the entire inner estuary, killing almost all eukaryotes and prompting debate on the causes. This paper reports a multi-proxy survey of Pb-210-dated sediment cores from the anoxic basin. Analyses of diatoms, dinoflagellates, pigments and geochemical proxies were used to determine changes in ecosystem structure over the past 100 years. The aim was to establish 'base-line conditions', for management purposes, of the biological structure prior to 1900, and to examine possible causes of changes observed. Geochemical proxies total nitrogen (TN), total carbon (TC) and biogenic silica (BSi) were consistently high throughout the sediment record. Increased concentrations of pigments and natural isotopes (delta C-13, delta N-15) suggested increasing production and nutrient loading. The main changes in the biological proxies occurred between 1915 and the 1940s, and indicated that the estuary has been somewhat eutrophic since 1900, but that the eutrophication process increased over the past 100 years. A reconstruction of TN concentration by a diatom-based transfer function supports this interpretation, with inferred TN ca. 1900 around 60 mu mol l(-1), and an increase in TN concentration over the past century to ca. 130 mu mol l(-1) by 1995. Inferred TN decreased to ca. 100 mu mol l(-1) by 2001, similar to present day monitoring data. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Copenhagen, Dept Phycol, Inst Biol, DK-1353 Copenhagen K, Denmark; Natl Environm Res Inst, Dept Marine Ecol, DK-4000 Roskilde, Denmark; Newcastle Univ, Sch Geog Polit & Sociol, Newcastle Upon Tyne NE1 7RU, Tyne & Wear, England; Dept Biol & Environm Sci, FIN-00014 Helsinki, Finland; Loughborough Univ Technol, Dept Geog, Loughborough LE11 3TU, Leics, England; Univ Aarhus, Dept Marine Ecol, DK-8200 Aarhus, Denmark	University of Copenhagen; Aarhus University; Danish National Environmental Research Institute; Newcastle University - UK; Loughborough University; Aarhus University	Ellegaard, M (通讯作者)，Univ Copenhagen, Dept Phycol, Inst Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	me@bi.ku.dk; anc@dmu.dk; nina.reuss@geol.lu.se; kaarina.weckstrom@helsinki.fi; stephen.juggins@newcastle.ac.uk; n.j.anderson@lboro.ac.uk; dco@dmu.dk	Ellegaard, Marianne/H-6748-2014; Juggins, Steve/D-1653-2010	Ellegaard, Marianne/0000-0002-6032-3376; Juggins, Steve/0000-0003-4466-424X; Conley, Daniel Joseph/0000-0001-9668-9284				ANDERSEN F, 1998, MARIAGER FJORD UDVIK; Andersen JH, 2004, MAR POLLUT BULL, V49, P283, DOI 10.1016/j.marpolbul.2004.04.014; Andrén E, 1999, ESTUAR COAST SHELF S, V48, P665, DOI 10.1006/ecss.1999.0480; [Anonymous], 2000, Official Journal L, V327/1, 22.12, P1; Appleby PG, 2002, DEV PALEOENVIRON RES, V1, P171; APPLEBY PG, 1986, HYDROBIOLOGIA, V143, P21, DOI 10.1007/BF00026640; Bennett KD, 1996, NEW PHYTOL, V132, P155, DOI 10.1111/j.1469-8137.1996.tb04521.x; Birks HJB, 1992, HOLOCENE, V2, P1, DOI 10.1177/095968369200200101; Birks H.J.B., 1995, STAT MODELING QUATER, P161; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bradshaw EG, 2005, HOLOCENE, V15, P1152, DOI 10.1191/0959683605hl887rp; Chen NH, 2001, ORG GEOCHEM, V32, P543, DOI 10.1016/S0146-6380(00)00194-7; Chmura GL, 2004, SCI TOTAL ENVIRON, V320, P225, DOI 10.1016/j.scitotenv.2003.08.003; Clarke A, 2003, MAR POLLUT BULL, V46, P1615, DOI 10.1016/S0025-326X(03)00375-8; Clarke AL, 2006, LIMNOL OCEANOGR, V51, P385, DOI 10.4319/lo.2006.51.1_part_2.0385; CLARKE AL, 2001, THESIS NEWCASTLE U; Conley D. 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J. F., 1995, P91; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Weckström K, 2004, AMBIO, V33, P324, DOI 10.1639/0044-7447(2004)033[0324:QBNCIC]2.0.CO;2; Wester R C, 2000, Int J Occup Environ Health, V6, P122; WIGGERS L, 2002, MARIAGER FJORD TILFO; WRIGHT SW, 1991, MAR ECOL PROG SER, V77, P183, DOI 10.3354/meps077183; Zimmerman AR, 2000, MAR CHEM, V69, P117, DOI 10.1016/S0304-4203(99)00100-0	54	53	60	0	34	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0272-7714	1096-0015		ESTUAR COAST SHELF S	Estuar. Coast. Shelf Sci.	JUL	2006	68	3-4					567	578		10.1016/j.ecss.2006.03.013	http://dx.doi.org/10.1016/j.ecss.2006.03.013			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	061KQ					2025-03-11	WOS:000238871700020
J	Alster, A; Dubinsky, Z; Zohary, T				Alster, A; Dubinsky, Z; Zohary, T			Encystment of <i>Peridinium gatunense</i>:: occurrence, favourable environmental conditions and its role in the dinoflagellate life cycle in a subtropical lake	FRESHWATER BIOLOGY			English	Article						cyst formation; environmental factors; Lake Kinneret; resting stage	KINNERET; DINOPHYCEAE; CULTURE; BLOOM; PHYTOPLANKTON; TEMPERATURE; CINCTUM; GROWTH; WESTII; ISRAEL	1. The abundance of cysts of the bloom-forming dinoflagellate Peridinium gatunense in the sediments of Lake Kinneret and the effects of environmental conditions on encystment were studied in relation to bloom dynamics. Peak cyst formation coincided with the highest growth rate of the population, prior to bloom peak. 2. Peridinium cysts were counted in water and sediment corer samples from 2000 to 2003 and in archived sediment trap samples collected during 1993-94. The cyst data were examined in relation to ambient temperature and nutrient records, and revealed no direct correlation. 3. In laboratory encystment experiments with Peridinium cells collected from the lake, 0.2-3% of the vegetative cells encysted. Temperature, light and cell density had no significant effect on the percentage of encystment. 4. Cysts were always present in the lake sediments but their abundance in 'non Peridinium' years was much lower than after a massive bloom. Vegetative cells were always present in the water column after the collapse of the annual dinoflagellate bloom, potentially serving as the inoculum for the next bloom. We propose that the hardy cysts serve as an emergency 'gene bank' to initiate population build up following catastrophic die outs.	Israel Oceanog & Limnol Res, Kinneret Limnol Lab, IL-14950 Migdal, Israel; Bar Ilan Univ, Dept Life Sci, Ramat Gan, Israel	Israel Oceanographic & Limnological Research Institute; Bar Ilan University	Alster, A (通讯作者)，Israel Oceanog & Limnol Res, Kinneret Limnol Lab, POB 447, IL-14950 Migdal, Israel.	alster@gmail.com						ALSTER A, 2006, IN PRESS VERHANDLUNG, V29; ALSTER A, 2006, IN PRESS HYDROBIOLOG; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BAN S, 1992, J CRUSTACEAN BIOL, V12, P51, DOI 10.2307/1548718; BERMAN T, 1995, LIMNOL OCEANOGR, V40, P1064, DOI 10.4319/lo.1995.40.6.1064; BERMAN T, 1984, VERHANDLUNGEN INT VE, V22, P2850; BERMANFRANK I, 1994, LIMNOL OCEANOGR, V39, P1822, DOI 10.4319/lo.1994.39.8.1822; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Dale B., 1983, P69; Eren J., 1969, VERH INT VEREIN LIMN, V17, P1013; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; KADOT AH, 1984, MEMOIRS COLL AGR, V123, P27; LUND J. W. G., 1958, HYDROBIOLOGIA, V11, P143, DOI 10.1007/BF00007865; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Pollingher U., 1988, P134; POLLINGHER U, 1981, Journal of Plankton Research, V3, P93, DOI 10.1093/plankt/3.1.93; POLLINGHER U, 1991, ARCH HYDROBIOL, V120, P267; POLLINGHER U, 1976, J PHYCOL, V12, P162, DOI 10.1111/j.1529-8817.1976.tb00494.x; POLLINGHER U, 1978, LAKE KINNERET, P271; RAHAT M, 1968, ISRAEL J BOT, V17, P200; Reynolds C.S., 1984, ECOLOGY FRESHWATER P; SAKO Y, 1986, L NIHON BISEIBUTSU S, V1, P19; Tessenow U., 1977, Archiv fur Hydrobiologie, V48, P438; Zohary T, 2004, FRESHWATER BIOL, V49, P1355, DOI 10.1111/j.1365-2427.2004.01271.x; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175	29	10	14	1	15	BLACKWELL PUBLISHING	OXFORD	9600 GARSINGTON RD, OXFORD OX4 2DQ, OXON, ENGLAND	0046-5070			FRESHWATER BIOL	Freshw. Biol.	JUL	2006	51	7					1219	1228		10.1111/j.1365-2427.2006.01543.x	http://dx.doi.org/10.1111/j.1365-2427.2006.01543.x			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	051UC					2025-03-11	WOS:000238185600003
J	Spilling, K; Kremp, A; Tamelander, T				Spilling, Kristian; Kremp, Anke; Tamelander, Tobias			Vertical distribution and cyst production of <i>Peridiniella catenata</i> (Dinophyceae) during a spring bloom in the Baltic Sea	JOURNAL OF PLANKTON RESEARCH			English	Article							PLANKTONIC FOOD-WEB; SCRIPPSIELLA-HANGOEI; MIGRATION; PHYTOPLANKTON; MICROORGANISMS; SEDIMENTATION; GERMINATION; DYNAMICS; SIZE	Vertical distribution and cyst production of the chain-forming, spring dinoflagellate Peridiniella catenata were studied throughout the spring season of 2000 in the coastal Guy of Finland. Numbers of cells were monitored in the water column, and cyst sedimentation was recorded using multiple sediment traps moored at three discrete depths. At the onset of the spring bloom, most of the population was situated in the euphotic zone. When the bloom progressed, the population was more evenly dispersed throughout the water column. Coinciding with the decline of the spring bloom, after nitrogen depletion, a general reduction of cell size of P. catenata and a break-up of chains were observed. Resting cysts started to appear shortly after the peak of the bloom, in sedimentation traps moored at 30 and 40 in depth. Cysts were only retrieved from the uppermost sediment trap on three of the six sampling occasions, constituting only a small proportion of all cysts produced by P. catenata during spring. Our results suggest that cyst production of this vertically migrating organism takes place to a large extent in deep water layers and emphasizes the necessity of whole water column monitoring in studies aiming to understand in situ life-cycle transformations of vertically migrating dinoflagellates.	Finnish Environm Inst, FIN-00251 Helsinki, Finland; Univ Helsinki, Tvarminne Zool Stn, FIN-10900 Hango, Finland; Finnish Inst Marine Res, FIN-00561 Helsinki, Finland	Finnish Environment Institute; University of Helsinki	Spilling, K (通讯作者)，Finnish Environm Inst, POB 140, FIN-00251 Helsinki, Finland.	kristian.spilling@ymparisto.fi	Kremp, Anke/I-8139-2013; Spilling, Kristian/L-7932-2014	Spilling, Kristian/0000-0002-8390-8270				[Anonymous], 1998, PHYSL ECOLOGY HARMFU; [Anonymous], ACTA BOT FENN; Ault TR, 2000, OECOLOGIA, V125, P466, DOI 10.1007/s004420000472; Beckmann A, 2004, OCEAN DYNAM, V54, P581, DOI 10.1007/s10236-004-0103-x; EDLER L, 1979, BALT MAR BIOL, V5, P9; EPPLEY RW, 1968, J PHYCOL, V4, P333, DOI 10.1111/j.1529-8817.1968.tb04704.x; Flaim G, 2003, HYDROBIOLOGIA, V502, P357, DOI 10.1023/B:HYDR.0000004293.59239.6f; Fraga S., 1989, P281; Fryxell G.A., 1983, SURVIVAL STRATEGIES; Grasshof K., 1983, Methods of seawater analysis, V3rd; HAAPALA J, 1994, ESTUAR COAST SHELF S, V38, P507, DOI 10.1006/ecss.1994.1035; Heiskanen A S., 1998, Monographs of the Boreal Environment Research, V8, P1; HEISKANEN AS, 1994, ARCH HYDROBIOL, V131, P175; HEISKANEN AS, 1995, MAR ECOL PROG SER, V122, P45, DOI 10.3354/meps122045; Höglander H, 2004, MAR ECOL PROG SER, V283, P15, DOI 10.3354/meps283015; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; JONES RI, 1988, HYDROBIOLOGIA, V161, P75, DOI 10.1007/BF00044102; Kamykowski D, 1997, LIMNOL OCEANOGR, V42, P1189, DOI 10.4319/lo.1997.42.5_part_2.1189; Kim S, 2004, J PHYCOL, V40, P815, DOI 10.1111/j.1529-8817.2004.04002.x; Kononen K., 1984, Limnologica, V15, P605; Kremp A, 2000, PHYCOLOGIA, V39, P183, DOI 10.2216/i0031-8884-39-3-183.1; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kremp A, 2005, J PHYCOL, V41, P629, DOI 10.1111/j.1529-8817.2005.00070.x; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; Kuuppo P, 1998, ESTUAR COAST SHELF S, V46, P65, DOI 10.1006/ecss.1997.0258; LARSSON U, 1986, CONTR ASKO LAB U STO, V30, P1; Leynaert A, 2004, LIMNOL OCEANOGR, V49, P1134; LIGNELL R, 1993, MAR ECOL PROG SER, V94, P239, DOI 10.3354/meps094239; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MULLERHAECKEL A, 1981, SARSIA, V66, P267; Niemi A, 1973, Acta Botanica Fennica, V100, P1; Olli K, 1997, HYDROBIOLOGIA, V363, P179, DOI 10.1023/A:1003186024477; PASSOW U, 1991, MAR BIOL, V110, P455, DOI 10.1007/BF01344364; RAVEN JA, 1984, NEW PHYTOL, V98, P259, DOI 10.1111/j.1469-8137.1984.tb02736.x; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Sullivan JM, 2003, J PHYCOL, V39, P83, DOI 10.1046/j.1529-8817.2003.02094.x; Tamelander T, 2004, J MARINE SYST, V52, P217, DOI 10.1016/j.jmarsys.2004.02.001; TAMMINEN T, 1995, MAR ECOL PROG SER, V120, P123, DOI 10.3354/meps120123; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; VONBODUNGEN B, 1981, KIELER MEERESFORSCH, V5, P49; Wasmund N, 1998, J PLANKTON RES, V20, P1099, DOI 10.1093/plankt/20.6.1099	41	14	15	0	11	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	JUL	2006	28	7					659	665		10.1093/plankt/fbi149	http://dx.doi.org/10.1093/plankt/fbi149			7	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	062MO					2025-03-11	WOS:000238949400004
J	Telford, RJ				Telford, Richard J.			Limitations of dinoflagellate cyst transfer functions	QUATERNARY SCIENCE REVIEWS			English	Article							SEA-SURFACE TEMPERATURES; PARTIAL LEAST-SQUARES; NORTH-ATLANTIC; PLANKTONIC-FORAMINIFERA; RECONSTRUCTION; PALEOECOLOGY; ASSEMBLAGES; CALIBRATION; PACIFIC; RECORD	Organic-walled dinoflagellate cysts have become an important proxy for reconstructing Quaternary sea-surface conditions, with transfer functions generating quantitative estimates of summer and winter sea-surface temperatures, salinity, and ice cover. I critically reassess these transfer functions and argue that the uncertainty of the summer temperature and ice cover transfer functions has been substantially underestimated because the strong spatial structure in the data set has been ignored, and that there is little evidence that either winter sea-surface temperature or salinity can be independently reconstructed. (c) 2006 Elsevier Ltd. All rights reserved.	Bjerknes Ctr Climate Res, N-5007 Bergen, Norway; Univ Bergen, EECRG, Dept Biol, N-5007 Bergen, Norway	Bjerknes Centre for Climate Research; University of Bergen	Telford, RJ (通讯作者)，Bjerknes Ctr Climate Res, Allegaten 55, N-5007 Bergen, Norway.	Richard.Telford@bjerknes.uib.no	Telford, Richard/AAD-2249-2019; Telford, Richard/C-1668-2008	Telford, Richard/0000-0001-9826-3076				Birks CJA, 2002, BOREAS, V31, P323; Birks H.J.B., 1990, The Surface Waters Acidification Programme, P301; BIRKS HJB, 1995, TECH GUIDE QUAT RES, V5, P116; BORCARD D, 1992, ECOLOGY, V73, P1045, DOI 10.2307/1940179; Brooks SJ, 2001, QUATERNARY SCI REV, V20, P1723, DOI 10.1016/S0277-3791(01)00038-5; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; DUPLESSY JC, 1991, OCEANOL ACTA, V14, P311; Elderfield H, 2000, NATURE, V405, P442, DOI 10.1038/35013033; Fortin M-J., 2000, B ECOL SOC AM, V81, P201; Heiri O, 2001, J PALEOLIMNOL, V26, P343, DOI 10.1023/A:1017568913302; Hillaire-Marcel C, 2001, NATURE, V410, P1073, DOI 10.1038/35074059; Jackson ST, 2004, ANNU REV EARTH PL SC, V32, P495, DOI 10.1146/annurev.earth.32.101802.120435; Kim JH, 2004, QUATERNARY SCI REV, V23, P2141, DOI 10.1016/j.quascirev.2004.08.010; Kucera M, 2005, QUATERNARY SCI REV, V24, P951, DOI 10.1016/j.quascirev.2004.07.014; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; MANIGHETTI B, 1995, PALEOCEANOGRAPHY, V10, P611, DOI 10.1029/94PA03059; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Melnikov IA, 2002, DEEP-SEA RES PT I, V49, P1623, DOI 10.1016/S0967-0637(02)00042-0; Pflaumann U, 1996, PALEOCEANOGRAPHY, V11, P15, DOI 10.1029/95PA01743; Prell WL., 1985, STABILITY LOW LATITU; Risebrobakken B, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2002PA000764; Telford RJ, 2005, QUATERNARY SCI REV, V24, P2173, DOI 10.1016/j.quascirev.2005.05.001; Ter Braak C. J. F., 1988, Classification and Related Methods of Data Analysis. Proceedings of the First Conference of the International Federation of Classification Societies (IFCS), P551; TERBRAAK CJF, 1995, CHEMOMETR INTELL LAB, V28, P165, DOI 10.1016/0169-7439(95)00002-E; TERBRAAK CJF, 1993, HYDROBIOLOGIA, V269, P485, DOI 10.1007/BF00028046; WHITE AW, 1978, J PHYCOL, V14, P475; Woodward F. I., 1987, CLIMATE PLANT DISTRI	31	41	43	0	6	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0277-3791			QUATERNARY SCI REV	Quat. Sci. Rev.	JUL	2006	25	13-14					1375	1382		10.1016/j.quascirev.2006.02.012	http://dx.doi.org/10.1016/j.quascirev.2006.02.012			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	076EO					2025-03-11	WOS:000239940000002
J	Borel, CM; Gómez, EA				Borel, C. Marcela; Gomez, Eduardo A.			Palynology from the Holocene of Canal del Medio, Bahia Blanca estuary, Buenos Aires, Argentina	AMEGHINIANA			Spanish	Article						palynology; Algae; acritarchs; pollen; Holocene; Buenos Aires; Argentina	LA PLATA RIVER; DINOFLAGELLATE-CYSTS; SEA; ACRITARCHS; SEDIMENTS; MARINE; NORTH	Holocene palynological samples from the Canal del Medio (38 degrees 49 degrees S; 62 degrees 17' W), Bahia Blanca inner estuary, south of Buenos Aires province, contain pollen, spores, remains of algae (Dinoflagellata, Chlorophyta and Cyanophyta) and acritarchs. The pollen spectra are dominated by Chenopodiineae and Poaceae, along with Asteraceae and Ephedra. The dinophycean algae are represented by cysts of estuarine dinoflagellates of the order Gonyaulacales (Operculodinium centrocarpum (Deflandre and Cookson) Wall, Spiniferites bulloideus (Deflandre and Cookson) Sarjeant, S. sp. cf. S. pachydermis (Rossignol) Reid, S. bentorii (Rossignol) Wall and Dale and S. ramosus (Ehrenberg) Loeblich and Loeblich). The chlorophycean algae consist of cenobia of Pediastrum boryanum (Turpin) Meneghini and colonies of Botryococcus braunii Kutzing. The assemblages also contain sheets of Gloeotrichia sp. The acritarchs are represented by Micrhystridium sp., Cymatiosphaera sp., Halodinium minus Bujak, Acritarch sp. F, Acritarch sp. G and Acritarch sp. H. Three palynological zones are distinguished in the sequence. The lowermost zone, dated in 3,500 C-14 yr B.P., represents an ancient tidal plain in close relation with a channel of turbid water and variable energy. The intermediate zone suggests better conditions for the development of autotrophic dinoflagellates, in a restricted estuarine environment. For the top zone, the low frequencies of dinocysts and acritarchs indicate similar conditions to those currently present in the inner Bahia Blanca estuary. Along the profile, the pollen reflects the development in the surrounding areas of halophytic communities, with the presence of xerophytic woodland. The characteristics of these deposits indicate that ca. 3,500 C-14 yr B.P., the mean sea level was located at a similar position than the current one.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Inst Argentino Oceanog, Consejo Nacl Invest Cient & Tecn, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Univ Tecnol Nacl, Fac Reg Bahia Blanca, RA-8000 Bahia Blanca, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Borel, CM (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	maborel@criba.edu.ar; gmgomez@criba.edu.ar	Gomez, Eduardo/Q-9020-2019	Borel, C. 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J	Hense, I; Beckmann, A				Hense, Inga; Beckmann, Aike			Towards a model of cyanobacteria life cycle -: effects of growing and resting stages on bloom formation of N<sub>2</sub>-fixing species	ECOLOGICAL MODELLING			English	Article						akinetes; cyanobacteria; heterocysts; internal quotas; life cycle; model	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; NITROGEN-FIXATION; BALTIC SEA; EUTROPHICATION MODEL; POPULATION-DYNAMICS; HIROSHIMA BAY; WATER COLUMN; RECRUITMENT; GROWTH; DIFFERENTIATION	Cyanobacteria blooms are a common phenomenon in aquatic environments but although considerable effort has been devoted to study various aspects of bloom formation, the processes involved are still not fully understood. Most of the factors that have been investigated can be categorised as external (e.g. N/P-ratio, temperature), whereas internal factors on the generation of cyanobacteria blooms through their distinctive life cycle have not yet been sufficiently considered. To fill this gap and to investigate the dynamics of cyanobacteria life cycles, a numerical model has been developed. The model assumes that the life cycle is governed by the internal energy and nitrogen quotas of the cells, and discriminates four different stages: vegetative cells, vegetative cells with heterocysts, akinetes and recruiting cells (including germinates). The seasonal succession of life stages is simulated in a one-dimensional framework, and a typical bloom is successfully simulated with a set of plausible parameters. Observed interannual variations in the relative proportions of different life cycle stages can be explained as the direct result of life cycle dynamics. The results show that life cycle simulations are feasible and can be used to test hypotheses and to determine sensitivities regarding the role of cyanobacteria life cycles in marine and limnic environments. Our study indicates that prediction of cyanobacteria blooms has to be based on a detailed knowledge of all stages of the life cycle.	Univ Helsinki, Div Geophys, Dept Phys Sci, FIN-00014 Helsinki, Finland; Finnish Environm Inst, Helsinki 00251, Finland	University of Helsinki; Finnish Environment Institute	Hense, I (通讯作者)，Univ Helsinki, Div Geophys, Dept Phys Sci, POB 64, FIN-00014 Helsinki, Finland.	ihense@iki.fi						Adams DG, 1999, NEW PHYTOL, V144, P3, DOI 10.1046/j.1469-8137.1999.00505.x; Arhonditsis GB, 2005, ECOL MODEL, V187, P140, DOI 10.1016/j.ecolmodel.2005.01.040; Arhonditsis GB, 2005, ECOL MODEL, V187, P179, DOI 10.1016/j.ecolmodel.2005.01.039; Baird ME, 2004, J MARINE SYST, V50, P199, DOI 10.1016/j.jmarsys.2004.02.002; BARBIERO RP, 1993, ARCH HYDROBIOL, V127, P87; BARBIERO RP, 1992, FRESHWATER BIOL, V27, P249, DOI 10.1111/j.1365-2427.1992.tb00537.x; Beckmann A, 2004, OCEAN DYNAM, V54, P581, DOI 10.1007/s10236-004-0103-x; Codd GA, 1999, EUR J PHYCOL, V34, P405, DOI 10.1017/S0967026299002255; DAMERVAL T, 1991, PLANT CELL, V3, P191; Downing JA, 2001, CAN J FISH AQUAT SCI, V58, P1905, DOI 10.1139/cjfas-58-10-1905; DROOP MR, 1973, J PHYCOL, V9, P264; EPPLEY RW, 1972, FISH B-NOAA, V70, P1063; Fennel W, 2001, J PLANKTON RES, V23, P1217, DOI 10.1093/plankt/23.11.1217; Ferber LR, 2004, FRESHWATER BIOL, V49, P690, DOI 10.1111/j.1365-2427.2004.01218.x; Fogg G.E., 1973, BLUE GREEN ALGAE; Geider RJ, 1998, LIMNOL OCEANOGR, V43, P679, DOI 10.4319/lo.1998.43.4.0679; Howarth RW, 1999, BIOGEOCHEMISTRY, V46, P203; HOWARTH RW, 1988, LIMNOL OCEANOGR, V33, P688, DOI 10.4319/lo.1988.33.4_part_2.0688; HUBER AL, 1984, APPL ENVIRON MICROB, V47, P234, DOI 10.1128/AEM.47.2.234-238.1984; HUBER AL, 1985, HYDROBIOLOGIA, V123, P145, DOI 10.1007/BF00018976; Janowitz GS, 1999, ECOL MODEL, V118, P237, DOI 10.1016/S0304-3800(99)00037-X; Kahru M, 2000, MAR ECOL PROG SER, V207, P13, DOI 10.3354/meps207013; KAHRU M, 1994, AMBIO, V23, P469; Karl D, 1997, NATURE, V388, P533, DOI 10.1038/41474; KARLSSON I, 1999, ALGOLOGICAL STUDIES, V94, P175; Karlsson-Elfgren I, 2004, FRESHWATER BIOL, V49, P265, DOI 10.1111/j.1365-2427.2004.01182.x; Karlsson-Elfgren I, 2003, J PHYCOL, V39, P1050, DOI 10.1111/j.0022-3646.2003.03-030.x; Kovács AW, 2003, HYDROBIOLOGIA, V506, P181, DOI 10.1023/B:HYDR.0000008614.76166.28; LaRoche J, 2005, J SEA RES, V53, P67, DOI 10.1016/j.seares.2004.05.005; Larsson U, 2001, LIMNOL OCEANOGR, V46, P811, DOI 10.4319/lo.2001.46.4.0811; Lehtimaki J, 1997, APPL ENVIRON MICROB, V63, P1647, DOI 10.1128/AEM.63.5.1647-1656.1997; Meeks JC, 2002, MICROBIOL MOL BIOL R, V66, P94, DOI 10.1128/MMBR.66.1.94-121.2002; Miller CB, 1998, FISH OCEANOGR, V7, P219, DOI 10.1046/j.1365-2419.1998.00072.x; Mulholland MR, 2002, MAR ECOL PROG SER, V239, P45, DOI 10.3354/meps239045; Neumann T, 2002, GLOBAL BIOGEOCHEM CY, V16, DOI 10.1029/2001GB001450; OLIVER RL, 1994, J PHYCOL, V30, P161, DOI 10.1111/j.0022-3646.1994.00161.x; Rengefors K, 2004, AQUAT MICROB ECOL, V36, P213, DOI 10.3354/ame036213; ROBARTS RD, 1987, NEW ZEAL J MAR FRESH, V21, P391, DOI 10.1080/00288330.1987.9516235; Robson BJ, 2004, ECOL MODEL, V174, P203, DOI 10.1016/j.ecolmodel.2004.01.006; ROUHIAINEN L, 1995, J BACTERIOL, V177, P6021, DOI 10.1128/jb.177.20.6021-6026.1995; Sellner KG, 2003, J IND MICROBIOL BIOT, V30, P383, DOI 10.1007/s10295-003-0074-9; Smith A.J., 1982, The Biology of Cyanobacteria, P47; Ståhl-Delbanco A, 2003, J PLANKTON RES, V25, P1099, DOI 10.1093/plankt/25.9.1099; Stephens N, 2003, NEW PHYTOL, V160, P545, DOI 10.1046/j.1469-8137.2003.00901.x; SUTHERLAND JM, 1979, J GEN MICROBIOL, V115, P273, DOI 10.1099/00221287-115-2-273; Trimbee A., 1988, Verh. 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J	Bertini, A				Bertini, Adele			The Northern Apennines palynological record as a contribute for the reconstruction of the Messinian palaeoenvironments	SEDIMENTARY GEOLOGY			English	Review						pollen; dinoflagellate cysts; palaeoclimate; palaeoenvironments; stratigraphical correlations; Messinian; northern Apennines; Italy	STABLE-ISOTOPE STRATIGRAPHY; SALINITY CRISIS; DINOFLAGELLATE CYSTS; UPPER MIOCENE; SE SPAIN; TRIPOLI FORMATION; BASIN; PLIOCENE; SECTION; EVAPORITES	The Messinian stage has long been associated with an overall warm and dry climate whereas recent researches indicate either a warm and humid or a cool and dry climate. The integrated stratigraphic record of vegetation and climatic changes from Northern Apennines sites provides the solution to this apparent contradiction. Its integration with the updated geological and sedimentological studies provides additional data for the reconstruction of the depositional palaeoenvirontnents in both marginal and deeper sub-basins of the Apennines foredeep. The onset of the Mediterranean salinity crisis (MSC) is recorded in the Gessoso-Solfifera of the Vena del Gesso (marginal sub-basin). Cyclical humid conditions, corresponding to precession minima, developed during the deposition of the shales interbedded with the gypsum (5.9 to 5.6 Ma); some cooler events took also place under the effects of global (glacial stadials) and regional factors (Apennines uplift). At present no major changes from moist to dry conditions are attested to just before the salinity crisis, as well as in Sicily. So climate did not play a major role in the onset of the MSC despite the favourable context provided by inferred thermo-xeric conditions in southern Italy. A drier episode indicated by the expansion of the open vegetation including the northward migration of Lygeum postdates the onset of the salinity crisis of about 400 kyr, in the lower post-evaporitic deposits of Maccarone (deeper sub-basin). It falls within a period of global warming whereas at a regional scale it could correlate p.p. to the evaporite deposition in deeper basins and to hiatuses in the marginal basins of Sicily and of the western sector of Northern Apennines. Its sudden end, about 100 kyr later, in coincidence with a significant increase of Pinaceae, indicates a turnover in the terrestrial setting not linked to major climate changes but possibly to a complex interaction between other palaeoenvironmental factors (e.g., tectonics and eustatisin). In contrast organic-walled dinoflagellate cysts exclude significant modifications in aquatic settings (insaturation of either open marine or brackish conditions). In the latter, a later change is marked by the arrival of Impagidinium (?) sp. l., a species here referred instead to Caspidinium rugosum, about 7 m below the first colombaccio. This occurrence together with the spread of Pediastrum indicates a freshwater dilution i.e. the "Lago-Marc" event during wetter climatic conditions on the adjacent landmass (increase of Tsuga and Cedrus). The successive arrival and/or ;dominance of other "Paratethyan" taxa such as I. (?) sp. 2, l. (?) sp. 3 and Galeacysta etrusca indicate highly variable water environments (marine vs. continental water inputs) during the deposition of the uppermost post-evaporitic deposits. The Lago-Mare is stratigraphically sandwiched between an ash layer (130 m below) dated at 5.5 Ma and the beginning of the Pliocene where a peak of Impagidinium patulum marks the onset of open marine conditions. The dominant humid, subtropical to warm temperate climate indicates differences in both temperature and moisture values with respect to the coeval southern sections, revealing climatic gradients within the Mediterranean, at least from the Messinian. No dramatic vegetation and climate changes have been recorded during the MSC; major changes occurred later as indicated by the palynological record from 2.6 Ma. This palynostratigraphic record is a good reference for more recent models of the development of the MSC and for establishing time-relationshis between the Apennine and Sicilian successions. (c) 2006 Elsevier B.V. All rights reserved.	Univ Florence, Dept Earth Sci, I-50121 Florence, Italy	University of Florence	Bertini, A (通讯作者)，Univ Florence, Dept Earth Sci, Via La Pira 4, I-50121 Florence, Italy.	abertini@geo.unifi.it	Bertini, Adele/KFQ-7894-2024	BERTINI, Adele/0000-0002-9332-6725				Aguirre J, 2004, SEDIMENT GEOL, V168, P71, DOI 10.1016/j.sedgeo.2004.03.004; [Anonymous], MESSINIAN EVENTS MED; [Anonymous], [No title captured]; [Anonymous], MEM SOC GEOL ITAL; Bassetti M., 1994, MEM SOC GEOL ITAL, V48, P275; Bassetti M.A, 2000, MEMORIE SCI GEOLOGIC, V52, P319; Bassetti MA, 2004, SEDIMENT GEOL, V172, P1, DOI 10.1016/j.sedgeo.2004.07.004; Bassetti MA, 2003, PALAEOGEOGR PALAEOCL, V198, P335, DOI 10.1016/S0031-0182(03)00475-9; BENSON RH, 1991, CARBONATE EVAPORITE, V6, P127, DOI 10.1007/BF03174420; BENVENUTI M, 2000, SEDIMENTARY TECTONIC; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; Bertini A, 2001, GEOBIOS-LYON, V34, P253, DOI 10.1016/S0016-6995(01)80074-7; Bertini A, 1997, CR ACAD SCI II A, V324, P763; 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J	Boeckel, B; Baumann, KH; Henrich, R; Kinkel, H				Boeckel, Babette; Baumann, Karl-Heinz; Henrich, Ruediger; Kinkel, Hanno			Coccolith distribution patterns in South Atlantic and Southern Ocean surface sediments in relation to environmental gradients	DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS			English	Review						coccoliths; distribution; ecology; statistics; surface sediments; South Atlantic; Southern Ocean (Atlantic sector)	CALCAREOUS DINOFLAGELLATE CYSTS; EXPORT PRODUCTION; LATE QUATERNARY; UPWELLING SYSTEM; PHYTOPLANKTON; VARIABILITY; CIRCULATION; CARBONATE; DYNAMICS; NORTHERN	In this study, the coccolith compositions of 213 surface sediment samples from the South Atlantic and Southern Ocean were analysed with respect to the environmental parameters of the overlying surface waters. From this data set, the abundance patterns of the main species and their ecological affinities were ascertained. In general, Emiliania huxleyi is the most abundant species of the recent coccolith assemblages in the study region. However, the lower photic zone taxa, composed of Florisphaera profunda and Gladiolithus flabellatus often dominate the assemblages between 20 degrees N and 30 degrees S. If E huxleyi is excluded, Calcidiscus leptoporus and F. profunda become the most abundant species, each dominating discrete oceanographic regimes. While F. profunda is very abundant in the sediments underneath warmer, stratified surface waters with a deep nutricline, Calcidiscus leptoporus is encountered in high-productivity environments. Furthermore, the results of a canonical correspondence analysis reveal affinities of Gephyrocapsa spp., Helicosphaera spp. and Coccolithus pelagicus for intermediate to higher nutrient conditions in a well-mixed upper water column. In contrast, Gladiolithus flabellatus seems to be associated with high temperatures and salinities under low-nutrient conditions. Based on the relative abundances of Calcidiscus leptoporus, F. profunda, Gladiolithus flabellatus, Helicosphaera spp., Umbilicosphaera foliosa, Umbilicosphaera sibogae and a group of subordinate subtropical species, six surface sediment assemblages have been identified, which reflect the distribution and characteristics of the overlying surface waters. Their distribution appears to be mainly a function of the relative position of the nutricline and thermocline in the overlying photic zone. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Bremen, Fac 05, D-28334 Bremen, Germany; Univ Kiel, Inst Geosci, D-24098 Kiel, Germany	University of Bremen; University of Kiel	Boeckel, B (通讯作者)，Univ Bremen, Fac 05, POB 33 04 40, D-28334 Bremen, Germany.	bboeckel@uni-bremen.de						Andruleit H, 1996, MICROPALEONTOLOGY, V42, P403, DOI 10.2307/1485964; Andruleit H, 2002, MAR GEOL, V3132, P1; [Anonymous], USE PROXIES PALEOCEA, DOI DOI 10.1007/978-3-642-58646-0_12; [Anonymous], J GEOPHYS RES; Asmus T, 1999, MAR GEOL, V159, P63, DOI 10.1016/S0025-3227(98)00199-6; Baumann K.-H., 2000, J NANNOPLANKTON RES, V22, P82; Baumann Karl-Heinz, 2000, Journal of Nannoplankton Research, V22, P185; Baumann KH, 2000, DEEP-SEA RES PT II, V47, P1743, DOI 10.1016/S0967-0645(00)00005-9; Benthien A, 2000, DEEP-SEA RES PT I, V47, P2369, DOI 10.1016/S0967-0637(00)00030-3; Berger W.H., 1976, Treatise on Chemical Oceanography, V5, P265; BERGER WH, 2002, P ODP SCI RES, V175; Bickert T, 1996, SOUTH ATLANTIC, P599; BICKERT T, 1992, BERICHTE FACHBEREICH, V27; BISCAYE PE, 1976, J GEOPHYS RES-OC ATM, V81, P2595, DOI 10.1029/JC081i015p02595; 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Part I-Oceanogr. Res. Pap.	JUN	2006	53	6					1073	1099		10.1016/j.dsr.2005.11.006	http://dx.doi.org/10.1016/j.dsr.2005.11.006			27	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	070OS					2025-03-11	WOS:000239533000009
J	Gestal, C; Novoa, B; Posada, D; Figueras, A; Azevedo, C				Gestal, Camino; Novoa, Beatriz; Posada, David; Figueras, Antonio; Azevedo, Carlos			<i>Perkinsoide chabelardi</i> n. gen., a protozoan parasite with an intermediate evolutionary position:: possible cause of the decrease of sardine fisheries?	ENVIRONMENTAL MICROBIOLOGY			English	Article							EGGS; APICOMPLEXA; PHYLOGENIES; PILCHARDUS; ALGORITHM; MODEL	Phenotypic scrutiny on the life cycle of lcthyodinium chabelardi (Perkinsoide chabelardi n. gen.) based on ultrastructural techniques, and molecular phylogenetic analysis of RNA gene sequences, were carried out in order to elucidate the taxonomic position of this parasite. The absence of plastid, presence of trichocysts, and chromosomes or chromatin condensed and low in number, suggested that this protozoan could be considered a dinoflagellate syndinial parasite. However, the life cycle, schizogonic divisions and structure of schizonts inside the host, the nuclei without the typical dinoflagellate appearance, presence of rhoptrias-like structures, a possible pseudoconoid, and the biflagellated spore, resembled those of the genus Perkinsus. Phylogenetic analysis of genes transcribing for the RNA forming the small subunit and the large subunit suggests that this parasite has an ambiguous evolutionary position within the group formed by dinoflagellates, perkinsids and syndinials. Because of differences with dinoflagellates and similarities with perkinsids, we propose to change the generic name to P chabelardi n. gen. High stationary infection prevalence on Sardina pilchardus eggs was observed. This protozoan parasite caused the death of all the infected sardine eggs, and therefore a high impact in the recruitment of this fishery in the Atlantic coast is expected.	CSIC, Inst Invest Marinas, Vigo, Spain; Univ Porto, ICBAS, Inst Biomed Sci, Dept Cell Biol, P-4099003 Oporto, Portugal; Univ Porto, Lab Protoparasitol, Ctr Marine & Environm Res, CIIMAR, P-4099003 Oporto, Portugal; Univ Vigo, Dept Bioquim Genet & Immunol, Vigo 36310, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Universidade do Porto; Universidade do Porto; Universidade de Vigo	Novoa, B (通讯作者)，CSIC, Inst Invest Marinas, Eduardo Cabello 6, Vigo, Spain.	virus@iim.csic.es	Figueras, Antonio/AAB-8921-2019; Novoa, Beatriz/K-3785-2014; Gestal, Camino/F-5062-2016; Posada, David/C-4502-2008; Figueras, Antonio/B-5133-2015	Gestal, Camino/0000-0003-1931-9567; Azevedo, Carlos/0000-0003-0424-1488; Novoa, Beatriz/0000-0003-4888-8419; Posada, David/0000-0003-1407-3406; Figueras, Antonio/0000-0002-0617-0030				AZEVEDO C, 1989, J PARASITOL, V75, P627, DOI 10.2307/3282915; Brugerolle G, 2002, EUR J PROTISTOL, V38, P113, DOI 10.1078/0932-4739-00864; Carrera P, 2003, SCI MAR, V67, P245, DOI 10.3989/scimar.2003.67s1245; CAVALIERSMITH T, 1993, MICROBIOL REV, V57, P953, DOI 10.1128/MMBR.57.4.953-994.1993; Chavez FP, 2003, SCIENCE, V299, P217, DOI 10.1126/science.1075880; Chicharo MA, 1998, MAR ECOL PROG SER, V164, P273, DOI 10.3354/meps164273; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Gascuel O, 1997, MOL BIOL EVOL, V14, P685, DOI 10.1093/oxfordjournals.molbev.a025808; GOGGIN CL, 1993, MOL BIOCHEM PARASIT, V60, P65, DOI 10.1016/0166-6851(93)90029-W; Guindon S, 2003, SYST BIOL, V52, P696, DOI 10.1080/10635150390235520; HOLLANDE A, 1952, CR HEBD ACAD SCI, V235, P976; HOLLANDE A, 1974, Protistologica, V10, P413; HOLLANDE A, 1953, STA AQUAT PECHES CEU, V4, P321; *ICES, 2002, AD HOC WORK GROUP EV; Leander BS, 2004, J PHYCOL, V40, P341, DOI 10.1111/j.1529-8817.2004.03129.x; MANIER J-F, 1971, Protistologica, V7, P213; MARQUES V, 2003, I NACL INVEST AGRAR, V10, P1; Matsuoka M, 1996, FISHERIES SCI, V62, P855, DOI 10.2331/fishsci.62.855; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; Nunn GB, 1996, J MOL EVOL, V42, P211, DOI 10.1007/BF02198847; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Reece KS, 1997, J PARASITOL, V83, P417, DOI 10.2307/3284403; Saldarriaga JF, 2003, INT J SYST EVOL MICR, V53, P355, DOI 10.1099/ijs.0.02328-0; SCHOLIN CA, 1994, J PHYCOL, V30, P744, DOI 10.1111/j.0022-3646.1994.00744.x; Siddall ME, 1997, PARASITOLOGY, V115, P165, DOI 10.1017/S0031182097001157; SMITH PE, 1989, FISH B-NOAA, V87, P497; SOYER MO, 1974, MILIEU, V24, P191; Stratoudakis Y, 2000, J FISH BIOL, V57, P476, DOI 10.1111/j.1095-8649.2000.tb02186.x; Tenter AM, 2002, INT J PARASITOL, V32, P595, DOI 10.1016/S0020-7519(02)00021-8; Thompson JD, 1997, NUCLEIC ACIDS RES, V25, P4876, DOI 10.1093/nar/25.24.4876	30	26	28	0	9	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1462-2912	1462-2920		ENVIRON MICROBIOL	Environ. Microbiol.	JUN	2006	8	6					1105	1114		10.1111/j.1462-2920.2006.01008.x	http://dx.doi.org/10.1111/j.1462-2920.2006.01008.x			10	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	048LV	16689731	Bronze			2025-03-11	WOS:000237949500016
J	Seo, KS; Fritz, L				Seo, Kyung Suk; Fritz, Lawrence			Karyology of a marine non-motile dinoflagellate, <i>Pyrocystis lunula</i>	HYDROBIOLOGIA			English	Article						chromosome; DNA content; karyology; Pyrocystis lunula; ultrastructure	DIVISION BEHAVIOR; CHROMOSOMES; EVOLUTION; ORGANIZATION; NUCLEAR; ULTRASTRUCTURE; MORPHOLOGY; NOCTILUCA; FEATURES; PROTEIN	Dinoflagellates have a unique and interesting intracellular architecture such as permanently condensed chromosomes throughout the cell cycle. However the study of dinoflagellate chromosomes is not amendable because of the unusually higher number of chromosomes and problems in sample preparation. The species of Pyrocystis spend most of their life cycle as vegetative cyst forms and have been used as experimental organisms for bioluminescence and circadian rhythms. Here, we documented the content of DNA in different life stages and the chromosome karyology in a marine non-motile dinoflagellate Pyrocystis lunula, through light and fluorescent microscopy, serial ultra-thin sectioning, and three dimension (3D) modeling. The DNA content doubles during DNA synthesis and in the end of the cell division two separate daughter cells have the approximately same fluorescent values for the mother cells. Using serial ultra-thin sectioning and 3D modeling, we report the first ultrastructural karyogram. The cells chosen were at the end of karyokinesis. A total of 98 chromosomes were counted and assigned to 49 pairs. In this species, DNA synthesis appears to occur before, or during asexual division and P. lunula lives a diplontic life cycle.	Natl Fisheries Res & Dev Inst, Marine Harmful Organisms Res Team, Pusan 619902, South Korea; Univ New England, Dept Biol Sci, Biddeford, ME USA	University of New England - Maine	Seo, KS (通讯作者)，Natl Fisheries Res & Dev Inst, Marine Harmful Organisms Res Team, 408-1 Sirang Ri, Pusan 619902, South Korea.	dino_seo@hanmail.net						AUSTIN AP, 1959, STAIN TECHNOL, V34, P69, DOI 10.3109/10520295909114651; Bhaud Y, 2000, J CELL SCI, V113, P1231; Bhaud Y, 1999, J EUKARYOT MICROBIOL, V46, P259, DOI 10.1111/j.1550-7408.1999.tb05123.x; Bouligand Y, 2001, BIOCHIMIE, V83, P187, DOI 10.1016/S0300-9084(00)01211-6; COSTAS E, 1989, CYTOLOGIA, V54, P539, DOI 10.1508/cytologia.54.539; COSTAS E, 1987, CHROMOSOMA, V95, P435, DOI 10.1007/BF00333995; Costas E, 2005, CYTOGENET GENOME RES, V109, P268, DOI 10.1159/000082409; DODGE JD, 1985, INT REV CYTOL, V94, P5, DOI 10.1016/S0074-7696(08)60390-3; EBERSOLD WT, 1967, SCIENCE, V157, P447, DOI 10.1126/science.157.3787.447; ELBRACHTER M, 1987, BOT MAR, V30, P233, DOI 10.1515/botm.1987.30.3.233; Fensome R.A., 1993, Micropaleontology Press Special Paper; Harris E. H., 1989, CHLAMYDOMONAS SOURCE, P575; HERZOG M, 1984, ORIGINS LIFE EVOL B, V13, P205, DOI 10.1007/BF00927172; HERZOG M, 1983, EUR J CELL BIOL, V30, P33; HERZOG M, 1981, EUR J CELL BIOL, V23, P295; HOLT JR, 1982, AM J BOT, V32, P249; Hughes JS, 1999, AM NAT, V154, P306, DOI 10.1086/303241; KELLENBERGER E, 1992, J MICROSC-OXFORD, V168, P181, DOI 10.1111/j.1365-2818.1992.tb03260.x; LAESPINA SDD, 2005, EUROPEAN J CELL BIOL, V84, P137; LEADBEATER B, 1967, ARCH MIKROBIOL, V57, P239, DOI 10.1007/BF00405950; LONG A, 1995, THEOR POPUL BIOL, V47, P18, DOI 10.1006/tpbi.1995.1002; Michel LS, 1996, BIOL CELL, V87, P149, DOI 10.1016/S0248-4900(97)89272-6; Okamoto OK, 2003, J PHYCOL, V39, P519, DOI 10.1046/j.1529-8817.2003.02170.x; RILL RL, 1989, CHROMOSOMA, V98, P280, DOI 10.1007/BF00327314; RIZZO PJ, 1991, J PROTOZOOL, V38, P246, DOI 10.1111/j.1550-7408.1991.tb04437.x; Rizzo PJ, 2003, CELL RES, V13, P215, DOI 10.1038/sj.cr.7290166; Seo K.S., 2000, ALGAE, V15, P137; Seo KS, 2000, MAR BIOL, V137, P589, DOI 10.1007/s002270000374; Seo KS, 2000, J PHYCOL, V36, P351, DOI 10.1046/j.1529-8817.2000.99196.x; SIGEE DC, 1986, ADV BOT RES, V12, P205, DOI 10.1016/S0065-2296(08)60195-0; Soyer-Gobillard M O, 1999, Int Microbiol, V2, P93; SoyerGobillard MO, 1996, ZOOL STUD, V35, P78; SOYERGOBILLARD MO, 1990, J CELL BIOL, V111, P293, DOI 10.1083/jcb.111.2.293; SUNDBERG WJ, 1976, STAIN TECHNOL, V51, P103, DOI 10.3109/10520297609116679; SWIFT E, 1971, J PHYCOL, V7, P89, DOI 10.1111/j.1529-8817.1971.tb01486.x; Wargo MJ, 2000, J PHYCOL, V36, P584, DOI 10.1046/j.1529-8817.2000.99122.x; Zhang ZD, 2002, MOL BIOL EVOL, V19, P489, DOI 10.1093/oxfordjournals.molbev.a004104; Zhang ZD, 1999, NATURE, V400, P155, DOI 10.1038/22099	38	5	5	0	7	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0018-8158	1573-5117		HYDROBIOLOGIA	Hydrobiologia	JUN	2006	563						289	296		10.1007/s10750-006-0017-3	http://dx.doi.org/10.1007/s10750-006-0017-3			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	042TJ					2025-03-11	WOS:000237552100024
J	Grigorszky, I; Kiss, KT; Béres, V; Bácsi, I; M-Hamvas, M; Máthé, C; Vasas, G; Padisák, J; Borics, G; Gligora, M; Borbély, G				Grigorszky, Istvan; Kiss, Kevi T.; Beres, Viktoria; Bacsi, Istvan; M-Hamvas, Marta; Mathe, Csaba; Vasas, Gabor; Padisak, Judit; Borics, Gabor; Gligora, Marija; Borbely, Gyoergy			The effects of temperature, nitrogen, and phosphorus on the encystment of <i>Peridinium cinctum</i>, Stein (Dinophyta)	HYDROBIOLOGIA			English	Article						encystment; Peridinium cinctum; temperature; N and P starvation	DINOFLAGELLATE GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; CYST FORMATION; SKELETONEMA-COSTATUM; OCEANIC DIATOM; LAKE TOVEL; CULTURE; GROWTH; GERMINATION; EXCYSTMENT	For avoiding the unfavorable environmental conditions several aquatic microorganisms are capable of forming specialized resistance cells like akinets, hypnospores, statospores, etc. Recognition of the important role of cysts in the life cycles of dinoflagellates increased the need to study their role in the ecology of phytoplanktons, and this, combined with the knowledge of chemical and biological characteristics of the water, may lead to a better understanding of the spatial and temporal dynamics of dinoflagellates. This paper reports on the effects of temperature, nitrogen, and phosphorus on the percentage of encystment of the dinoflagellate Peridinum cinctum Stein. The phosphorus content of the medium affected encystment only at the highest temperature applied (22 degrees C). Nitrogen content and temperature were the most important factors controlling the encystment.	Univ Debrecen, Dept Bot, H-4010 Debrecen, Hungary; Hungarian Acad Sci, Hungarian Danube Res Stn, Inst Ecol & Bot, H-2131 God, Hungary; Univ Veszprem, Dept Limnol, H-8200 Veszprem, Hungary; Environm Protect Inspectorate Trans Tiszanian Reg, H-4025 Debrecen, Hungary; Univ Zagreb, Fac Sci, Dept Biol, Zagreb 10000, Croatia	University of Debrecen; HUN-REN; HUN-REN Centre for Ecological Research; Danube Research Institute; Hungarian Academy of Sciences; Institute of Ecology & Botany - HAS; University of Pannonia; University of Zagreb	Grigorszky, I (通讯作者)，Univ Debrecen, Dept Bot, POB 14, H-4010 Debrecen, Hungary.	gege@tigris.klte.hu	B-Beres, Viktoria/AAI-2055-2019; Udovič, Marija/IZE-0991-2023; Bácsi, István/ACX-9726-2022; István, Grigorszky/Q-2245-2019; Vasas, Gabor/E-7627-2010; Padisak, Judit/B-4514-2008	Gligora Udovic, Marija/0000-0002-1982-2528; Bacsi, Istvan/0000-0002-3916-8623; B-Beres, Viktoria/0000-0002-9632-2703				ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BARRY C, 2004, J APPL PHYCOL, V16, P401; BINDER BJ, 1987, J PHYCOL, V23, P99; Cantonati Marco, 2003, Journal of Limnology, V62, P79; CAREFOOT JR, 1968, J PHYCOL, V4, P129, DOI 10.1111/j.1529-8817.1968.tb04686.x; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Dale B., 1983, P69; DEMANCHE JM, 1979, MAR BIOL, V53, P323, DOI 10.1007/BF00391615; DORTCH Q, 1984, MAR BIOL, V81, P237, DOI 10.1007/BF00393218; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Edmonson W.T., 1972, AM SOC LIM OCEANOG S, V1, P172; ENDO T, 1984, Bulletin of Plankton Society of Japan, V31, P23; EPPLEY RW, 1974, J PHYCOL, V10, P15, DOI 10.1111/j.1529-8817.1974.tb02671.x; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; Flaim G, 2004, PHYCOLOGIA, V43, P737, DOI 10.2216/i0031-8884-43-6-737.1; Flaim G, 2003, HYDROBIOLOGIA, V502, P357, DOI 10.1023/B:HYDR.0000004293.59239.6f; FLEMING RH, 1940, PROCESS PACIFIC SCI, V3, P526; Grigorszky I, 2003, HYDROBIOLOGIA, V506, P203, DOI 10.1023/B:HYDR.0000008552.60232.68; Grigorszky I, 2003, HYDROBIOLOGIA, V506, P209, DOI 10.1023/B:HYDR.0000008632.57769.19; Grigorszky I, 2000, INT VER THEOR ANGEW, V27, P152; HICKEL B, 1988, HYDROBIOLOGIA, V161, P41, DOI 10.1007/BF00044098; Huppert A, 2002, AM NAT, V159, P156, DOI 10.1086/324789; Karlsson I, 2003, HYDROBIOLOGIA, V506, P189, DOI 10.1023/B:HYDR.0000008570.03256.00; KARLSSON I, 1999, ALGOLOGICAL STUDIES, V94, P175; KARSSONELFGREN I, 2003, J PHYCOL, V39, P1050; KETCHUM BH, 1939, J CELL PHYSL, P373; KIDA K, 1989, Journal of the Faculty of Science Shinshu University, V24, P13; Lawton L., 1999, Toxic cyanobacteria in water: A guide to their public health consequences, monitoring and management; Moore D, 2003, HYDROBIOLOGIA, V506, P175, DOI 10.1023/B:HYDR.0000008536.01716.1a; Olli K, 2004, MAR ECOL PROG SER, V273, P43, DOI 10.3354/meps273043; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; Park Ho-Dong, 1992, Journal of the Faculty of Science Shinshu University, V27, P87; PERRY MJ, 1976, LIMNOL OCEANOGR, V21, P88, DOI 10.4319/lo.1976.21.1.0088; PFIESTER LA, 1976, J PHYCOL, V12, P234; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; PFIESTER LA, 1977, J PHYCOL, V13, P62; POLLINGHER U, 1986, GROWTH REPROD STRATE, P134; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rodhe W., 1948, SYMB BOT UPSAL, V10, P1; SAKO Y, 1985, B JPN SOC SCI FISH, V51, P267; SAKO Y, 1984, B JPN SOC SCI FISH, V50, P743; SAKO Y, 1987, B JPN SOC SCI FISH, V53, P473; SAKSHAUG E, 1977, J EXP MAR BIOL ECOL, V29, P1, DOI 10.1016/0022-0981(77)90118-6; SCHINDLER DW, 1971, J FISH RES BOARD CAN, V28, P295, DOI 10.1139/f71-039; SERRUYA C, 1975, J PHYCOL, V11, P155, DOI 10.1111/j.1529-8817.1975.tb02764.x; SHAFIK HM, 1997, ANN LIMNOLOGY, V33, P1389; SPOEHR HA, 1949, PLANT PHYSIOL, V24, P120, DOI 10.1104/pp.24.1.120; Susek E, 2005, PHYCOL RES, V53, P97, DOI 10.1111/j.1440-183.2005.00377.x; Vollenweider R.A., 1970, SCI FUNDAMENTALS EUT; Von Stosch HA., 1973, Br Phycol J, V8, P105; WATANABE MM, 1982, RES REP NATL I ENV S, V30, P27; WYNNE D, 1981, HYDROBIOLOGIA, V83, P93, DOI 10.1007/BF02187154; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175	56	31	42	4	43	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0018-8158	1573-5117		HYDROBIOLOGIA	Hydrobiologia	JUN	2006	563						527	535		10.1007/s10750-006-0037-z	http://dx.doi.org/10.1007/s10750-006-0037-z			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	042TJ					2025-03-11	WOS:000237552100042
J	Garg, R; Khowaja-Ateequzzaman; Prasad, V				Garg, Rahul; Khowaja-Ateequzzaman; Prasad, Vandana			Significant dinoflagellate cyst biohorizons in the Upper Cretaceous-Palaeocene succession of the Khasi Hills, Meghalaya	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						dinoflagellate cysts; biostratigraphy; biohorizons; Upper Cretaceous-Palaeocene; Khasi Hills; Meghalaya	TERTIARY BOUNDARY; INDIA	The Upper Cretaceous-Palaeocene rocks of the Khasi Hills, Meghalaya have yielded rich dinoflagellate cysts assemblages recovered from the Mahadeo Formation, the Langpar Formation, lower part of the Therria Formation and lower part of the Sylhet Limestone Formation. Occurrence of several globally recognized marker dinoflagellate cyst taxa, having well-established First Appearance Datum (FAD) and Last Appearance Datum (LAD), is noted in these assemblages. A succession of cosmopolitan dinoflagellate cyst biohorizons (based on comparisons with global records) are summarized, highlighting their potential in precise age determination and demarcation of time boundaries within Late Campanian-Late Thanetian interval. The dinoflagellate cyst evidence demonstrates that the succession is not older than Late Campanian in age.	Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Garg, R (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	rahul_bsip@yahoo.com	PRASAD, VANDANA/KUF-4093-2024					[Anonymous], 1962, Bulletin of the Geological Mining and Metallurgical Society of India, V25, P1; [Anonymous], 1989, PALAEOBOTANIST; BALASUNDARAM, 1972, REC GEOL SURV INDIA, V104, P1; BHANDARI N, 1987, CURR SCI INDIA, V56, P1003; Bhattacharya A., 1981, Journal of the Palaeontological Society of India, V26, P26; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; CHAKRABORTY A, 1972, QUAT J GEOL MIN META, V44, P107; DUTTA S K, 1980, Biological Memoirs, V5, P56; Dutta S.K., 1970, PALAEONTOGRAPH ABTEI, V11, P1; Garg R, 1995, CURR SCI INDIA, V69, P1012; GARG R, 1996, GOLD JUB C PHYS BIOL, P34; GARG R, 2002, NAT C BIOD PAST PRES, P89; Garg R., 2000, PALAEOBOTANIST, V49, P461; GARG R, 1993, 5TH DINO5 INT C MOD, P43; Ghosh A.M.N., 1940, Rec Geol Surv India, V75, P1; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; Hardenbol J., 1998, SEPM SPECIAL PUBLICA, V60, P763, DOI DOI 10.2110/PEC.98.02.0003; JAIN KP, 1975, PALEOBOTANIST, V22, P1; Jauhri A.K., 1994, Bollettino della Societa Paleontologica Italiana Special Volume, V2, P157; Jauhri A.K., 1998, Journal of the Palaeontological Society of India, V43, P73; Jauhri A.K., 1996, Contributions to XV Indian Colloquium on Micropalaeontology and Stratigraphy, P209; KAR R K, 1986, Palaeontographica Abteilung B Palaeophytologie, V202, P83; KAR R K, 1986, Pollen et Spores, V28, P177; KUMAR A, 2001, P 9 INT PAL C HOUST, P149; MATHUR L.P., 1964, 22 SESSION, P1; Medlicott H. B., 1869, MEMOIRS GEOLOGICAL S, V7, P151; MEHROTRA NC, 2002, MEM GEOL SOC INDIA, V48, P161; MURTHY M. V. N., 1976, Records of the Geological Survey of India, V107, P80; MURTY KN, 1983, PETROLEUM ASIA J, V1, P1; NAGAPPA YEDATORE, 1959, MICROPALEONTOLOGY, V5, P145, DOI 10.2307/1484208; NANDI B, 1990, REV PALAEOBOT PALYNO, V65, P119, DOI 10.1016/0034-6667(90)90063-O; NANDI B, 1984, EVOLUTIONARY BOT BIO, P521; OLDHAM T, 1858, MEM GEOL SURV INDIA, V1, P99; PANDEY J, 1973, P 2 IND COLL MICR ST, P77; Pandey J., 1981, P 7 IND C MICR STRAT, P70; PANDEY J., 1981, Jour. Palaeont. Soc, V25, P53; Powell A.J., 1992, STRATIGRAPHIC INDEX; Raja Rao CS, 1982, B GEOL SURV INDIA SE, V45, P1; SAH SCD, 1977, J GEOL SOC INDIA, V18, P445; SAH SCD, 1967, PALEOBOTANIST, V16, P177; SAH SCD, 1988, GEOL SURV IND SPEC P, V11, P17; Serra-Kiel J, 1998, B SOC GEOL FR, V169, P281; STOVER LE, 1996, AM ASS STRATIGRAPHIC, V2, P641; Tripathi SKM., 1984, PALYNOSTRATIGRAPHICA, P316; WILLIS S, 1993, S ATL QUART, V92, P1; WILSON GF, 1953, WORLDS OILFIELDS E H, V6, P119	46	16	19	0	1	GEOLOGICAL SOC INDIA	BANGALORE	#64 12TH CROSS, BASAPPA LAYOUT P B 1922, GAVIPURAM PO, BANGALORE 560019, INDIA	0016-7622			J GEOL SOC INDIA	J. Geol. Soc. India	JUN	2006	67	6					737	747						11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	124UE					2025-03-11	WOS:000243394600005
J	Leroy, SAG; Marret, F; Giralt, S; Bulatov, SA				Leroy, S. A. G.; Marret, F.; Giralt, S.; Bulatov, S. A.			Natural and anthropogenic rapid changes in the Kara-Bogaz Gol over the last two centuries reconstructed from palynological analyses and a comparison to instrumental records	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY				LAKE ISSYK-KUL; DINOFLAGELLATE CYSTS; CASPIAN SEA; POLLEN; SEDIMENTS; DYNAMICS; REGION; SYSTEM	Palynological analyses (pollen and dinocysts) of a sediment core taken in the Kara-Bogaz Gol have been used to reconstruct rapid and catastrophic environmental changes over the last two centuries (chronology based on (210)Pb). A natural cyclicity (65 years) of water level changes in the Caspian Sea (CS) and in the Kara-Bogaz Gol (KBG) and anthropogenic factors (building of a dam separating the CS and the KBG waters) combine to induce rapid changes in water levels of the KBG, in the salinity of its waters and in vegetation cover of its surroundings. The impact of low water levels on the dinocysts is marked by a lower diversity and the survival of two species that are typical of the KBG, the Caspian Sea species present in the KBG having disappeared. During periods of higher water levels (AD 1871-1878), the lake is surrounded by a steppe-like vegetation dominated by Artemisia; whereas during periods of low water levels (AD 1878-1913 and AD 1955-1998), the emerged shore are colonised by Chenopodiaceae. The period of AD 1913-1955 corresponding to decreasing water levels has an extremely low pollen concentration and a maximum of reworking of arboreal taxa. During the last low-level period, humans responded by abandoning the shores of the bay. What happened to the KBG can be used as an example of what may happen in the future for the Aral Sea. A problem of reworking of Tertiary dinocysts into modern deposits has been detected owing to the knowledge of the modern dinoflagellate assemblages recently made available through a water survey. A comparison to modern surface pollen samples from Central Asia (Anzali, Caspian Sea south and central basins, Aral Sea, Lake Balkhash, Lake Issyk-Kul and the Chinese Tien-Shan range) allows us to establish the potential reworking of at least five arboreal pollen taxa possibly by run-off and dust storms. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.	Brunel Univ, Dept Geog & Earth Sci, Uxbridge UB8 3PH, Middx, England; Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; CSIC, Inst Earth Sci Jaume Almera, E-08028 Barcelona, Spain; Minist Agr Russian Fed, Dept Fishing Policy, Moscow, Russia	Brunel University; Brunel University; University of Liverpool; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Geociencias Barcelona (GEO3BCN)	Leroy, SAG (通讯作者)，Brunel Univ, Dept Geog & Earth Sci, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk	Leroy, Suzanne/D-3996-2009; Giralt, Santiago/AAA-8585-2020; Bulatov, Stanislav/AAA-1892-2020; Giralt, Santiago/G-4823-2011	Bulatov, Stanislav/0000-0001-9257-4754; Marret-Davies, Fabienne/0000-0003-4244-0437; Giralt, Santiago/0000-0001-8570-7838				[Anonymous], 1949, DIATOM ANAL; [Anonymous], 1983, Quat. Sci. 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Int.	JUN	2006	150						52	70		10.1016/j.quaint.2006.01.007	http://dx.doi.org/10.1016/j.quaint.2006.01.007			19	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	054VC		Green Submitted			2025-03-11	WOS:000238405700007
J	Marret, F; Maley, J; Scourse, J				Marret, Fabienne; Maley, Jean; Scourse, James			Climatic instability in west equatorial Africa during the Mid- and Late Holocene	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY				ENVIRONMENTAL-CHANGES; DIATOM RECORD; RAIN-FOREST; DINOFLAGELLATE CYSTS; HYDROLOGICAL CHANGES; VEGETATION HISTORY; LAST DEGLACIATION; MARINE-SEDIMENTS; POLLEN EVIDENCE; ZAIRE RIVER	Millennial-scale climatic variations have punctuated the Holocene characterised by abrupt changes from warm to cool or wetter to drier conditions. Amongst these climatic events, there is increased evidence for an abrupt multicentennial shift of climatic conditions around 3.8/3.7 kyr BP (4.1 cal. kyr BP) in mid- to low-latitude regions which had a profound impact on landscape and population migration. In the Mediterranean region, subtropical, tropical and equatorial Africa, a number of continental proxies (lake-levels, pollen sequences, stable isotopes) record this abrupt change towards drier conditions. However, regionalism in climatic conditions is reflected in the vegetation records, possibly in relation to orographic conditions and the influence of sea-surface conditions. Hitherto there have been very few marine sequences that record this particular climatic shift at high-resolution. We present here new data from the Congo deep-sea fan containing integrated marine and terrestrial proxies. Around 5-4 cal. kyr BP, shifts in surface conditions off the Congo River mouth are observed, with possible establishment of seasonal coastal upwelling, and lower sea-surface temperatures. In parallel, pollen data indicate fluctuations of herbaceous, afromontane taxa and charred grass cuticles, suggesting more open vegetation in the lowland regions and an increase in cloud forest and/or afromontane vegetation at higher altitudes within the Congolese region. (c) 2006 Elsevier Ltd and INQUA. All rights reserved.	Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; Univ Montpellier 2, CNRS, Paleotrop & Dept Paleoenvironm & Palynol, IRD,ISEM, F-34095 Montpellier 05, France; Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales	University of Liverpool; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier	Marret, F (通讯作者)，Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk		Marret-Davies, Fabienne/0000-0003-4244-0437				Abbott MB, 2003, PALAEOGEOGR PALAEOCL, V194, P123, DOI 10.1016/S0031-0182(03)00274-8; [Anonymous], VEGETATION HIST ARCH; [Anonymous], TROPICAL RAIN FOREST; Baker PA, 2001, NATURE, V409, P698, DOI 10.1038/35055524; Bar-Matthews M, 1999, EARTH PLANET SC LETT, V166, P85, DOI 10.1016/S0012-821X(98)00275-1; Barker PA, 2001, PALAEOECO A, V27, P77; Behling H, 2001, PALAEOGEOGR PALAEOCL, V173, P87, DOI 10.1016/S0031-0182(01)00321-2; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; 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Int.	JUN	2006	150						71	81		10.1016/j.quaint.2006.01.008	http://dx.doi.org/10.1016/j.quaint.2006.01.008			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	054VC					2025-03-11	WOS:000238405700008
J	Giunta, S; Negri, A; Maffioli, P; Sangiorgi, F; Capotondi, L; Morigi, C; Principato, MS; Corselli, C				Giunta, Simona; Negri, Alessandra; Maffioli, Paola; Sangiorgi, Francesca; Capotondi, Lucilla; Morigi, Caterina; Principato, Maria Speranza; Corselli, Cesare			Phytoplankton dynamics in the eastern Mediterranean sea during marine isotopic stage 5e	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			Eemian; sapropel; calcareous nannoplankton; diatoms; dinoflagellate cysts; eastern Mediterranean sea	DINOFLAGELLATE CYST ASSEMBLAGES; SOUTHERN ADRIATIC SEA; EMILIANIA-HUXLEYI; SAPROPEL S5; IONIAN SEA; LAST DEGLACIATION; CIRCULATION; EUTROPHICATION; RECONSTRUCTION; PRODUCTIVITY	Calcareous nannoplankton, diatoms and organic-walled dinoflagellate cysts from seven eastern Mediterranean sediment cores were investigated to clarify the climatic and paleoceanographic conditions that influenced the deposition of sapropel S5 during Marine Isotopic Stage 5e. Warming of surface waters during S5 deposition is indicated by the high abundance of the calcareous nannofossil "small" Gephyrocapsa group, the presence of the dinoflagellate species Spiniferites mirabilis, Spiniferites pachydermus, Lingulodinium machaerophorum and Polysphaeridium zoharyi, and the tropical-subtropical diatom Pseudosolenia calearavis, Chaetoceros resting spores, Rhizosolenids and Thalassionema group. Increased productivity accompanied S5 deposition as evidenced by a general decrease in abundance of calcareous nannofossil superficial species and a coeval increase of dinocysts and diatoms. The productivity increase is further supported by an increase of the deep dwelling calcareous nannofossil species Florisphaera profunda. Stratification of near-surface waters is recorded by the presence of the dinocyst species L. machaerophorum and P zoharyi together with the co-occurrence of the diatom Chaetoceros resting-spore group, Thalassionema frauenfieldii, and Thalassionema nitzschioides var. parva, which reflect transport of neritic waters off-shore, and by the presence of some freshwater and transport-related diatom taxa (Cyclotella, Diatomella and Diploneis). Gradual shoaling of the nutricline and a gradual weakening of water stratification at the end of S5 deposition is indicated by an increase in the deep dwelling calcareous nannoplankton species Gladiolithus flabellatus, which suggests a less-deep niche compared to the deeper dwelling F profunda. Time transgressive variations in the distribution of the calcareous nannofossil Emiliana huxleyi and changes in the abundances of Gephyrocapsa oceanica, small Gephyrocapsa, G. flabellatus, and of the dinocysts R zoharyi and L. machaerophorum lead to paleocirculation considerations, as they always reflect the main current path. Moreover, the occurrence of upwelling-related diatom and dinocyst taxa, such as Chaetoceros resting spores and S. pachydermus, suggests the presence of a former gyre structure south of Crete that was active during S5 time. (c) 2005 Elsevier B.V. All rights reserved.	Univ Politecn Marche, Dipartimento Sci Mare, I-60131 Ancona, Italy; Univ Milan, Dipartimento Sci Geol & Geotecnol, I-20126 Milan, Italy; Univ Bologna, Ctr Interdip Ric Sci Ambientali, I-48100 Ravenna, Italy; CNR, ISMAR Ist Sci Marine, I-40129 Bologna, Italy	Marche Polytechnic University; University of Milan; University of Bologna; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR)	Giunta, S (通讯作者)，Univ Politecn Marche, Dipartimento Sci Mare, Via Brecce Bianche, I-60131 Ancona, Italy.	s.giunta@univpm.it	Negri, Alessandra/D-4085-2011; Corselli, Cesare/E-9970-2011; CNR, Ismar/P-1247-2014; Capotondi, Lucilla/C-8874-2015; Morigi, Caterina/L-3883-2016	Sangiorgi, Francesca/0000-0003-4233-6154; Negri, Alessandra/0000-0002-8133-3936; CNR, Ismar/0000-0001-5351-1486; Capotondi, Lucilla/0000-0003-3282-7910; Morigi, Caterina/0000-0003-1340-9932				AKSNES DL, 1994, SARSIA, V79, P291, DOI 10.1080/00364827.1994.10413561; [Anonymous], UTRECHT MICROPALEONT; Bar-Matthews M, 2000, CHEM GEOL, V169, P145, DOI 10.1016/S0009-2541(99)00232-6; Baumann Karl-Heinz, 1998, Journal of Nannoplankton Research, V20, P75; Beaufort L, 1996, QUATERN INT, V31, P13, DOI 10.1016/1040-6182(95)00017-D; Cane T, 2002, PALAEOGEOGR PALAEOCL, V183, P87, DOI 10.1016/S0031-0182(01)00461-8; CASTRADORI D, 1993, PALEOCEANOGRAPHY, V8, P459, DOI 10.1029/93PA00756; Corselli C, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2000PA000536; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; EGGE JK, 1994, SARSIA, V79, P333, DOI 10.1080/00364827.1994.10413565; Emeis KC, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2000PA000617; Flores JA, 1997, MAR MICROPALEONTOL, V29, P351, DOI 10.1016/S0377-8398(96)00029-1; Gaines G., 1987, The Biology of Dinoflagellates, P224; Giunta S, 2003, PALAEOGEOGR PALAEOCL, V190, P39, DOI 10.1016/S0031-0182(02)00598-9; Hallegraeff G.M., 1986, DIATOM RES, V1, P57, DOI [10.1080/0269249X.1986.9704958, DOI 10.1080/0269249X.1986.9704958]; HASLE GR, 1997, IDENTIFYING MARINE P, P858; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Jorissen FJ, 1999, MAR GEOL, V153, P91, DOI 10.1016/S0025-3227(98)00088-7; Kallel N, 2000, PALAEOGEOGR PALAEOCL, V157, P45, DOI 10.1016/S0031-0182(99)00149-2; Kemp A.E. 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Paleoclimatol. Paleoecol.	MAY 29	2006	235	1-3					28	47		10.1016/j.palaeo.2005.09.022	http://dx.doi.org/10.1016/j.palaeo.2005.09.022			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	049LW					2025-03-11	WOS:000238018900003
J	Heimhofer, U; Hochuli, PA; Herrle, JO; Weissert, H				Heimhofer, Ulrich; Hochuli, Peter A.; Herrle, Jens O.; Weissert, Helmut			Contrasting origins of Early Cretaceous black shales in the Vocontian basin: Evidence from palynological and calcareous nannofossil records	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			OAE; black shale; Cretaceous; palynomorphs; dinoflagellate cysts; calcareous nannofossils	ORGANIC-CARBON BURIAL; OCEANIC ANOXIC EVENT; SE FRANCE; LIVELLO SELLI; SOUTHERN ALPS; PRODUCTIVITY; STRATIGRAPHY; SEDIMENTS; CO2; SWITZERLAND	Detailed records of spore-pollen assemblages, particulate organic matter (OM), dinoflagellate cysts and calcareous nannofossils provide new insights into the palaeoclimatic and palacoceanographic conditions during formation of Early Cretaceous black shales in the Vocontian basin (southeastern France). The early Aptian Niveau Goguel, which corresponds to the OAE1a, and the regionally distributed late Aptian Niveau Jacob have been studied with regard to changes in terrestrial vegetation patterns, terrigenous inputs and palaeofertility conditions. Palynological results from both black shale intervals exhibit a rich and stable floral pattern, dominated by various ferns, different types of cycads, bennettites as well as by several conifer families. Dinoflagellate cyst assemblages and the calcareous nannofossil-based nutrient index show no prominent changes in surface water productivity across the two studied intervals in the Vocontian basin. Significant variations are observed in terrestrial detrital input indicated by changes in absolute abundances of marine and terrestrial palynomorphs. According to our results, the laminated, OM-rich horizons of the Niveau Goguel interval reflect deposition during times of reduced siliciclastic input. Episodes of pronounced condensation were accompanied by anoxic conditions preventing degradation of the predominantly marine-derived OM. In contrast, the Niveau Jacob is characterised by a strong increase in terrestrial palynomorphs, most probably reflecting an abrupt increase in riverine runoff. The enhanced terrestrial OM input may have triggered oxygen-depletion in bottom waters, resulting in turn in increased OM preservation. Our results highlight the variety of processes that controlled the accumulation of OM in the Vocontian basin and they illustrate that enhanced surface water productivity is not an indispensable prerequisite for the formation of mid-Cretaceous black shales. (c) 2005 Elsevier B.V. All rights reserved.	ETH, Inst Geol, CH-8092 Zurich, Switzerland; Univ Zurich, Inst Paleontol, CH-8006 Zurich, Switzerland	Swiss Federal Institutes of Technology Domain; ETH Zurich; University of Zurich	Heimhofer, U (通讯作者)，Univ Oxford, Dept Earth Sci, Oxford OX1 3RPR, England.	uli.heimhofer@earth.ox.ac.uk; peter.hochuli@erdw.ethz.ch; Jens.Herrle@soc.soton.ac.uk; heimi@erdw.ethz.ch	Herrle, Jens/B-9088-2008					Abbink O.A., 1998, Palynological investigations in the Jurassic of the North Sea region; [Anonymous], 1995, P OCEAN DRILLING PRO; [Anonymous], 1980, CRETACEOUS RES; [Anonymous], PUBL SOC GEOL NORD; [Anonymous], 2007, Paleopalynology; [Anonymous], 1996, Palynology: principles and applications; Arnaud H., 1993, Geol Alpine, Ser Spec Colloq Excur, V3, P3; Arthur M.A., 1987, MARINE PETROLEUM SOU, V26, P401, DOI DOI 10.1144/GSL.SP.1987.026.01.25; ARTHUR MA, 1990, NATO ADV SCI I C-MAT, V304, P75; ARTHUR MA, 1988, NATURE, V335, P714, DOI 10.1038/335714a0; BARRON EJ, 1983, EARTH-SCI REV, V19, P305, DOI 10.1016/0012-8252(83)90001-6; Baudin F, 1998, CRETACEOUS RES, V19, P701, DOI 10.1006/cres.1998.0126; Beck CB, 1988, Origin and evolution of gymnosperms, P382; Beerling DJ, 2002, ANNU REV EARTH PL SC, V30, P527, DOI 10.1146/annurev.earth.30.091201.141413; Bellanca A, 2002, PALAEOGEOGR PALAEOCL, V185, P175, DOI 10.1016/S0031-0182(02)00299-7; BERNER RA, 1994, AM J SCI, V294, P56, DOI 10.2475/ajs.294.1.56; BOWN PR, 1999, BR MICROPALAEONTOL S, P16; Bralower RJ, 1999, J FORAMIN RES, V29, P418; BRALOWER TJ, 1984, GEOLOGY, V12, P614, DOI 10.1130/0091-7613(1984)12<614:LPASDC>2.0.CO;2; BRALOWER TJ, 1994, PALAIOS, V9, P335, DOI 10.2307/3515055; BREHERET J-G, 1983, Bulletin du Museum National d'Histoire Naturelle Section C Sciences de la Terre Paleontologie Geologie Mineralogie, V5, P113; BREHERET JG, 1994, SP PUB EAPG, P295; Brenner G.J., 1976, ORIGIN EARLY EVOLUTI, P23; CHUMAKOV NM, 1995, STRATIGR GEOL CORREL, V3, P241; Coccioni R., 1993, PALAEOPELAGOS, V3, P195; Erba E, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2003PA000884; ERBA E, 1994, PALEOCEANOGRAPHY, V9, P483, DOI 10.1029/94PA00258; ERBA E, 1991, Rivista Italiana di Paleontologia e Stratigrafia, V97, P455; ERBA E, 1989, MESOZOIC CENOZOIC ST, P146; Erbacher J, 1996, GEOLOGY, V24, P499, DOI 10.1130/0091-7613(1996)024<0499:EPORAO>2.3.CO;2; Erbacher J, 1998, CRETACEOUS RES, V19, P805, DOI 10.1006/cres.1998.0134; Erbacher J, 2001, NATURE, V409, P325, DOI 10.1038/35053041; Flandrin J., 1963, B SERV CARTE GEOL FR, V272, P815; Freeman KH, 1992, GLOBAL BIOGEOCHEM CY, V6, P185, DOI 10.1029/92GB00190; Friedrich O, 2003, MAR MICROPALEONTOL, V49, P65, DOI 10.1016/S0377-8398(03)00029-X; Geisen M, 1999, MICROPALEONTOLOGY, V45, P437, DOI 10.2307/1486125; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Habib D., 1982, NATURE ORIGIN CRETAC, P113; HALLAM A, 1985, J GEOL SOC LONDON, V142, P433, DOI 10.1144/gsjgs.142.3.0433; Hay WW, 1999, GEOL S AM S, P1; Heimhofer U, 2004, EARTH PLANET SC LETT, V223, P303, DOI 10.1016/j.epsl.2004.04.037; Herrle JO, 2004, EARTH PLANET SC LETT, V218, P149, DOI 10.1016/S0012-821X(03)00646-0; Herrle JO, 2003, TERRA NOVA, V15, P14, DOI 10.1046/j.1365-3121.2003.00448.x; Herrle JO, 2003, CRETACEOUS RES, V24, P1, DOI 10.1016/S0195-6671(03)00023-5; Herrle JO, 2003, PALAEOGEOGR PALAEOCL, V190, P399, DOI 10.1016/S0031-0182(02)00616-8; HEUSSER L, 1977, QUATERNARY RES, V7, P45, DOI 10.1016/0033-5894(77)90013-8; HOCHULI PA, 1981, REV PALAEOBOT PALYNO, V35, P337, DOI 10.1016/0034-6667(81)90116-0; Hochuli PA, 1999, GEOLOGY, V27, P657, DOI 10.1130/0091-7613(1999)027<0657:EOHPAC>2.3.CO;2; HUBER BT, 1995, GEOL SOC AM BULL, V107, P1164, DOI 10.1130/0016-7606(1995)107<1164:MLCCOT>2.3.CO;2; Jenkyns HC, 2004, NATURE, V432, P888, DOI 10.1038/nature03143; JENKYNS HC, 1999, ZBL GEOL PALAONTOL, V1997, P143; Kuypers MMM, 2004, GEOLOGY, V32, P853, DOI 10.1130/G20458.1; Kuypers MMM, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2000PA000569; Larson RL, 1999, PALEOCEANOGRAPHY, V14, P663, DOI 10.1029/1999PA900040; Leckie RM, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2001PA000623; Lister J.K., 1988, PALAEONTOGRAPHICA SE, V210, P9; Luciani V, 2001, GEOL MAG, V138, P277, DOI 10.1017/S0016756801005301; Masure E., 1998, GEOLOGIE MEDITERRANE, V25, P263; Menegatti AP, 1998, PALEOCEANOGRAPHY, V13, P530, DOI 10.1029/98PA01793; Mohr B.A.R., 1989, Berliner Geowissenschaftliche Abhandlungen. 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Paleoclimatol. Paleoecol.	MAY 29	2006	235	1-3					93	109		10.1016/j.palaeo.2005.09.025	http://dx.doi.org/10.1016/j.palaeo.2005.09.025			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	049LW					2025-03-11	WOS:000238018900006
J	Sangiorgi, F; Dinelli, E; Maffioli, P; Capotondi, L; Giunta, S; Morigi, C; Principato, MS; Negri, A; Emeis, KC; Corselli, C				Sangiorgi, Francesca; Dinelli, Enrico; Maffioli, Paola; Capotondi, Lucilla; Giunta, Simona; Morigi, Caterina; Principato, Maria Speranza; Negri, Alessandra; Emeis, Kay-Christian; Corselli, Cesare			Geochemical and micropaleontological characterisation of a Mediterranean sapropel S5: A case study from core BAN89GCO9 (south of Crete)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			multiproxy approach; sapropel S5; sediment provenance; micropaleontology; Mediterranean Sea	DEEP-SEA; SURFACE SEDIMENTS; PLANKTIC FORAMINIFERS; SEASONAL SUCCESSION; MARINE-SEDIMENTS; AFRICAN MONSOON; LEVANTINE BASIN; ORGANIC-MATTER; BLACK SHALES; ISOTOPE DATA	Several geochemical and micropaleontological proxies were studied in a well developed sapropel S5 from a core collected south of Crete to investigate the causes and the mechanisms of its deposition, to reconstruct the paleoenvironmental and paleoceanographical conditions at time of its formation and to detect the roles played by productivity and anoxia. The geochemical proxies are also used to unravel the sediment provenance and therefore to help tracing water circulation patterns and freshwater sources. The multiproxy approach reveals that the sapropel layer has high internal variability and five different depositional phases can be identified, four within the visible sapropel layer. An increase in temperature and the development of a Deep Chlorophyll Maximum characterise the onset of the sapropel (phase 1), with enhanced productivity being favoured by local riverine input, not clearly ascribable to Nile river freshwater discharge, and by the shoaling of the pyenocline/nutricline. Surface water stratification and productivity develop, together with strong seafloor dysoxia/anoxia. Phase 2 is characterised by lower stratification, slightly lower temperature and/or higher seasonal contrast, and still high productivity. Phase 3 records high productivity, high temperature and high stratification, probably more sustained by the Nile input. A sudden partial reoxygenation takes place at the end of this phase, changing the main features of the sapropel. In the fourth phase, productivity starts to decrease, water stratification seems to be partially broken down and sediment oxygenation increases. A transitional phase (phase 5) occurs between the end of the visible sapropel and the normal pelagic post-sapropel sedimentation, where productivity is still high and oxygenation improves compared to the visible sapropel layer. The massive occurrence of Polysphaeridium zoharyi, cyst of a red tide forming dinoflagellate, also characterises this phase. The geochemical proxies indicate that pre-sapropel and post-sapropel sediments are quite different from each other, and the provenance shifts from a more mixed to a more markedly southern origin of sediments. (c) 2005 Elsevier B.V. All rights reserved.	Univ Utrecht, Dept Biol, Lab Palaeobot, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Dept Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, I-48100 Ravenna, Italy; Univ Milan, Dipartimento Sci Geol & Geotecnol, I-20126 Milan, Italy; CNR, Ist Sci Marine, I-40129 Bologna, Italy; Univ Politecn Marche, Dipartimento Sci Mare, I-60131 Ancona, Italy; Univ Hamburg, Inst Biogeochem & Meereschem, D-20146 Hamburg, Germany	Utrecht University; Utrecht University; University of Bologna; University of Milan; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Marche Polytechnic University; University of Hamburg	Sangiorgi, F (通讯作者)，Univ Utrecht, Dept Biol, Lab Palaeobot, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	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Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	105	23	23	0	11	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAY 29	2006	235	1-3					192	207		10.1016/j.palaeo.2005.09.029	http://dx.doi.org/10.1016/j.palaeo.2005.09.029			16	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	049LW					2025-03-11	WOS:000238018900011
J	Guasti, E; Speijer, RP; Brinkhuis, H; Smit, J; Steurbaut, E				Guasti, Elisa; Speijer, Robert P.; Brinkhuis, Henk; Smit, Jan; Steurbaut, Etienne			Paleoenvironmental change at the Danian-Selandian transition in Tunisia: Foraminifera, organic-walled dinoflagellate cyst and calcareous nannofossil records	MARINE MICROPALEONTOLOGY			English	Article						Danian-Selandian transition; planktic foraminifera; organic-walled dinoflagellate cysts; Tunisia; calcareous nannofossils; paleoenvironment; Paleocene; stratigraphy	CRETACEOUS-TERTIARY BOUNDARY; PALEOCENE PLANKTIC FORAMINIFERA; SEA-LEVEL; EL-KEF; ISOTOPE STRATIGRAPHY; THERMAL MAXIMUM; AIN-SETTARA; PALEOGENE; ASSEMBLAGES; SECTION	In the present study, we document paleoenvironmental change across the Danian-Selandian transition (planktic foraminiferal interval P2-P3b; calcareous nannofossil Zone NP4, Subzones NTp6-NTp8A; 61-59N[a) in NW Tunisia. Diversifications of Paleogene planktic foraminifera with the evolution of the muricate and photosymbiotic lineages Morozovella, Acarinina and Igorina and of the biostratigraphically important nannofossils genus Fasciculithus are recorded within this interval. The present study aims to understand early Paleogene environmental changes in the southern Tethys, by analyzing the evolution of surface-water and-to a lesser extent-seafloor conditions. Three localities were investigated: Ain Settara, Elles and El Kef, all representing outer neritic deposition in the same basin, the Tunisian Trough. Paleoenvironmental changes are explored by combining planktic foraminiferal, organic dinocyst and calcareous nannofossils assemblages and several proxy parameters (planktic/benthic ratio, numbers of planktic foraminifera per gram, peridinioid/gonyaulacoid ratio; terrestrial/marine palynomorph ratio). In addition, also some geochemical parameters (calcite content and stable isotopes) are examined. Our records indicate that the environment evolved from an initially oligotrophic, open marine, deep outer neritic setting in P2-P3a towards a shallower and nutrient-rich setting from the base of Subzone P3b. This change is seen in the foraminiferal assemblages, with the substitution of Praemurica by Morozovella among the planktic foraminifera and an upward decrease in deeper benthic taxa. Also the organic-dinocyst assemblages show a peak of peridinioid cysts (Cerodinium and Lejeunecysta). Associated to these dinocyst assemblages, the lowest occurrence of Apectodinium is recorded, which seem to have evolved in this region, possibly in response to enhanced nutrient levels on the shelf. Additionally, a distinct change in calcareous nannofossil assemblages is also described, marked by the lowest appearance of Chiasmolithus edentulus, the lowest consistent occurrence of Fasciculithus and a slight increase in near-shore taxa (essentially Pontosphaera). This project provides an accurate understanding of paleoenvironmental change across the Danian-Selandian transition in Tunisia. Especially, integrating different proxies demonstrates a paleobathymetric shallowing from the Danian to the Selandian, associated to increase surface paleoproductivity. Furthermore, the results are compared with those from other localities along the Southern Tethyan margin (Egypt and Jordan) and a more regional paleoclimatic/paleoceanographic perturbation in the Southern Tethys is suggested. (c) 2006 Elsevier B.V. All rights reserved.	Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; Katholieke Univ Leuven, Dept Geog & Geol, B-3001 Heverlee, Belgium; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Vrije Univ Amsterdam, Fac Earth & Life Sci, Dept Sedimentol, NL-1081 HV Amsterdam, Netherlands; Inst Royal Sci Nat Belgique, B-1000 Brussels, Belgium	University of Bremen; KU Leuven; Utrecht University; Vrije Universiteit Amsterdam	Guasti, E (通讯作者)，Fugro Robertson Ltd, Strat Grp, Llandudno LL30 1SA, England.	elisa.guasti@fugro-robertson.com; robert.speijer@geo.kuleuven.be; H.Brinkhuis@bio.uu.nl; smit@geo.vu.nl; etienne.steurbaut@naturalsciences.be	Speijer, Robert/H-5073-2016; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610; Speijer, Robert/0000-0002-5873-7203				Adatte T, 2002, PALAEOGEOGR PALAEOCL, V178, P165, DOI 10.1016/S0031-0182(01)00395-9; [Anonymous], 1986, SEDIMENTARY ENV FACI; [Anonymous], CREATACEOUS TERTARY; [Anonymous], PALAEOCLIMATOLOGY PA; Arenillas I., 1995, Geogaceta, V17, P23; ARENILLAS I, 1996, TOMO EXTRAORDINARIO, V125, P272; AUBERT J, 1976, CEN RECH PAU SNPA B, V10, P379; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Berggren WA, 2000, PALAEOGEOGR PALAEOCL, V159, P1, DOI 10.1016/S0031-0182(00)00031-6; Berggren WA, 1997, MICROPALEONTOLOGY, V43, P1, DOI 10.2307/1485988; Berggren WA, 1994, GFF, V116, P44, DOI 10.1080/11035899409546145; BOBIER C, 1991, EUROPEAN GEOTRAVERSE, P371; Boersma A, 1989, PALEOCEANOGRAPHY, V4, P271, DOI 10.1029/PA004i003p00271; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brinkhuis H., 2003, P OCEAN DRILLING PRO, V189; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; Burollet P.F., 1956, Ann. 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Micropaleontol.	MAY 24	2006	59	3-4					210	229		10.1016/j.marmicro.2006.02.008	http://dx.doi.org/10.1016/j.marmicro.2006.02.008			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	046MN		Green Published			2025-03-11	WOS:000237815800006
J	Sorrel, P; Popescu, SM; Head, MJ; Suc, JP; Klotz, S; Oberhänsli, H				Sorrel, P.; Popescu, S. -M.; Head, M. J.; Suc, J. P.; Klotz, S.; Oberhaensli, H.			Hydrographic development of the Aral Sea during the last 2000 years based on a quantitative analysis of dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Aral Sea hydrology; Late Holocene; dinoflagellate cysts; lake level changes; glacial meltwater discharge; Mediterranean low-pressure system	RECENT SEDIMENTS; CLIMATE-CHANGE; WATER; ASSEMBLAGES; INDICATORS; PALEOCLIMATE; EVOLUTION; ATLANTIC; RECORD; ALGAE	The Aral Sea Basin is a critical area for studying the influence of climate and anthropogenic impact on the development of hydrographic conditions in an endorheic basin. We present organic-walled dinoflagellate cyst analyses with a sampling resolution of 15 to 20 years from a core retrieved at Chemyshov Bay in the NW Large Aral Sea (Kazakhstan). Cysts are present throughout, but species richness is low (seven taxa). The dominant morphotypes are Lingulodinium machaerophorum with varied process length and Impagidinium caspienense, a species recently described from the Caspian Sea. Subordinate species are Caspidinium rugosum, Romanodinium areolatum, Spiniferites cruciformis, cysts of Pentapharsodinium dalei, and round brownish protoperidiniacean cysts. The chlorococcalean algae Botryococcus and Pediastrum are taken to represent freshwater inflow into the Aral Sea. The data are used to reconstruct salinity as expressed in lake level changes during the past 2000 years. We quantify and date for the first time prominent salinity variations from the northern part of the Large Aral Sea. During high lake levels, I caspienense, representing brackish conditions with salinities of about 10-15 g kg(-1) or less, prevails. Assemblages dominated by L. machaerophorum document lake lowstands during approximately 0-425 AD (or 100? BC-425 AD), 920-1230 AD, 1500 AD, 1600-1650 AD, 1800 AD and since the 1960s. Because salinity in the Aral Sea is mostly controlled by meltwater discharges from the Syr Darya and Amu Darya rivers, we interpret changes in salinity levels as a proxy for temperature fluctuations in the Tien Shan Mountains that control snow melt. Significant erosion of marine Palaeogene and Neogene deposits in the hinterland, evidenced between 1230 AD and 1400 AD, is regarded as sheet-wash from shore. This is controlled by the low pressure system that develops over the Eastern Mediterranean and brings moist air to the Middle East and Central Asia during late spring and summer. We propose that the recorded environmental changes are related primarily to climate, but perhaps to a lesser extent by humancontrolled irrigation activities. Our results documenting climate change in western Central Asia are fairly consistent with reports elsewhere from Central Asia. (c) 2006 Elsevier B.V. All rights reserved.	Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany; Univ Lyon 1, UMR 5125, CNRS, Lab PaleoEnvirom & Paleobiosphere, F-69622 Villeurbanne, France; Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; Univ Tubingen, Inst Geowissensch, D-72070 Tubingen, Germany	Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences; Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); University of Cambridge; Eberhard Karls University of Tubingen	Sorrel, P (通讯作者)，Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany.	psorrel@gfz-potsdam.de	SORREL, Philippe/D-2696-2012					AKSU AE, 1995, MAR GEOL, V123, P33, DOI 10.1016/0025-3227(95)80003-T; AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; ALE B, 1993, NATO ASI SER, V1, P521; ALESHINSKAYA ZV, 1996, ARAL SEA KAZAKHSTAN, P108; [Anonymous], PALEOKLIMATY OLEDENE; [Anonymous], 1999, LAND OCEAN SYSTEMS S; [Anonymous], TIEN SHAN JUNIPER FO; BALTES N, 1971, REV PALAEOBOT PALYNO, V11, P125, DOI 10.1016/0034-6667(71)90023-6; Bao Y, 2003, QUATERNARY SCI REV, V22, P2335, DOI 10.1016/S0277-3791(03)00132-X; BARIENTOS OOP, 1979, BIBLIOTHECA PHYCOLOG, V48, P1; BARTHOLD W, 1910, QUELLEN FORSCHUNGEN, V2; Batten D.J., 1996, Palynology: principles and applications, P205; Bold H.C., 1985, Introduction to the algae, V2nd; Boomer I, 2000, QUATERNARY SCI REV, V19, P1259, DOI 10.1016/S0277-3791(00)00002-0; Boomer I., 2003, BRIDGING GAP TRENDS, P153, DOI DOI 10.1017/S1089332600002199; Boroffka N.G., 2005, Mitigation and Adaptation Strategies for Global Change, V10, P71, DOI DOI 10.1007/S11027-005-7831-1; BOROFFKA NGO, IN PRESS GEOARCHAEOL; Bortnik VN, 1990, ARAL SEA, V7; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Bradley R, 2000, SCIENCE, V288, P1353, DOI 10.1126/science.288.5470.1353; Brenner W.W., 2001, BALTICA, V14, P40; BRODSKAYA IG, 1952, T IN TA GEOL NAUK AN, V115; BRYSON RA, 1996, NATO ASI SERIES 1, V49, P465; CLEVE PT, 1900, HANDLINGAR, V32, P1; Cour P., 1974, POLLEN SPORES, V23, P247; Crowley TJ, 2000, SCIENCE, V289, P270, DOI 10.1126/science.289.5477.270; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Esper J, 2002, HOLOCENE, V12, P267, DOI 10.1191/0959683602hl543rp; Farinacci A., 1971, P 2 PLANKT C ROM 197, P1; Friedrich J, 2004, J MARINE SYST, V47, P77, DOI 10.1016/j.jmarsys.2003.12.010; Gundersen N., 1988, THESIS U OSLO; Hallett RI, 1999, THESIS U WESTMINSTER; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Head MJ, 2005, QUATERN INT, V130, P3, DOI 10.1016/j.quaint.2004.04.027; HEIM C, 2005, THESIS A WEGENER I B; HENSEN V, 1987, BERICHTE KOMMISSION, V5, P107; ISSAR AS, 1990, ISRAEL J EARTH SCI, V40, P219; Kloosterboer-van Hoeve ML, 2001, PALAEOGEOGR PALAEOCL, V173, P61, DOI 10.1016/S0031-0182(01)00314-5; Kokinos John P., 1995, Palynology, V19, P143; KOTLYAKOV VM, 1991, MT RES DEV, V11, P1, DOI 10.2307/3673523; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; Landmann G, 1996, PALAEOGEOGR PALAEOCL, V122, P107, DOI 10.1016/0031-0182(95)00101-8; Leegaard C., 1920, Act Soc Sc Fenn Helsingfors, V48, P1; LEMCKE G, 1996, NATO ASI SERIES 1, V449, P653; Letolle R., 1993, Aral; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; LIOUBIMTSEVA E, 2002, PHYS GEOGRAPHY NO EU; Maev E.G., 1999, Water Resources, V26, P187; Marret F, 2004, REV PALAEOBOT PALYNO, V129, P1, DOI 10.1016/j.revpalbo.2003.10.002; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; Meunier A., 1910, Microplankton Des Mers De Barents Et de Kara. 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J	Pospelova, V; Pedersen, TF; de Vernal, A				Pospelova, Vera; Pedersen, Thomas F.; de Vernal, Anne			Dinoflagellate cysts as indicators of climatic and oceanographic changes during the past 40 kyr in the Santa Barbara Basin, southern California	PALEOCEANOGRAPHY			English	Article							SEA-SURFACE CONDITIONS; LATE QUATERNARY; CURRENT SYSTEM; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; NORTH; ASSEMBLAGES; PRESERVATION; RECONSTRUCTION; MASSACHUSETTS	The dinoflagellate cyst record from Ocean Drilling Program Hole 893A, Santa Barbara Basin, southern California, is examined at millennial-scale resolution for the past similar to 40 kyr. Changes in cyst abundance, composition of cyst assemblages, and their diversity reflect major shifts in climate and ocean circulation in the region over this time interval. Throughout the sequence, dinoflagellate cyst assemblages are dominated by heterotrophic dinoflagellates. Brigantedinium spp. and other upwelling-related taxa such as Echinidinium and Protoperidinium americanum are abundant, indicating the continued influence of coastal upwelling on the basin during the late Quaternary. A significant increase in cyst accumulation rates is seen during the Holocene and, to a lesser extent, during shorter warming events such as Bolling/Allerod and Dansgaard-Oeschger interstadials, implying enhanced marine productivity during these periods. Cyst diversity is high during the Holocene. An increase in abundance of cysts produced by autotrophic dinoflagellates in the late Holocene suggests enhanced input of warm, nutrient-rich waters. In contrast, cyst assemblages from the Last Glacial Maximum exhibit a relatively low diversity and an increase in the cysts of heterotrophic dinoflagellates, in particular Selenopemphix nephroides. The presence of this taxon in association with Brigantedinium spp. implies substantial cooling of surface waters in the Santa Barbara Basin at that time.	Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Victoria; University of Quebec; University of Quebec Montreal	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, Petch 168,POB 3055 STN CSC, Victoria, BC V8W 3P6, Canada.	vpospe@uvic.ca	; de Vernal, Anne/D-5602-2013	Pospelova, Vera/0000-0003-4049-8133; de Vernal, Anne/0000-0001-5656-724X				[Anonymous], 1998, Sea; Behl R.J., 1995, PROC ODP, V146, P295; Behl RJ, 1996, NATURE, V379, P243, DOI 10.1038/379243a0; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 1997, PALEOCEANOGRAPHY, V12, P821, DOI 10.1029/97PA02167; Doose H, 1997, PALEOCEANOGRAPHY, V12, P615, DOI 10.1029/97PA00821; Emery KO., 1960, SEA OFF SO CALIFORNI, DOI [10.5962/bhl.title.39476, DOI 10.5962/BHL.TITLE.39476]; Gardner J., 1995, Proceedings of the Ocean Drilling Program, Scientific Results, V146, P103; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hendy IL, 2000, PALEOCEANOGRAPHY, V15, P30, DOI 10.1029/1999PA000413; Hendy IL, 1999, GEOLOGY, V27, P291, DOI 10.1130/0091-7613(1999)027<0291:LQNPSW>2.3.CO;2; Hendy IL, 2002, QUATERNARY SCI REV, V21, P1167, DOI 10.1016/S0277-3791(01)00138-X; Herbert T.D., 1995, Proceedings of the Ocean Drilling Program. 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J	Foissner, W				Foissner, Wilhelm			Biogeography and dispersal of micro-organisms: A review emphasizing protists	ACTA PROTOZOOLOGICA			English	Review						cryptogam spores; cyst viability; flagship species; Gondwana; human dispersal; Laurasia; local vs. global diversity; protozoa; undersampling	SOIL CILIATES PROTOZOA; 23S RIBOSOMAL-RNA; PAPUA-NEW-GUINEA; EUKARYOTIC DIVERSITY; CILIOPHORA DIVERSITY; MOLECULAR PHYLOGENY; COMMUNITY STRUCTURE; DEEP-SEA; NOV-SPEC; N. SP.	This review summarizes data on the biogeography and dispersal of bacteria, microfungi and selected protists, such as dinoflagellates, chrysophytes, testate amoebae, and ciliates. Furthermore, it introduces the restricted distribution and dispersal of mosses, ferns and macrofungi as arguments into the discussion on the postulated cosmopolitism and ubiquity of protists. Estimation of diversity and distribution of micro-organisms is greatly disturbed by undersampling, the scarcity of taxonomists, and the frequency of misidentifications. Thus, probably more than 50% of the actual diversity has not yet been described in many protist groups. Notwithstanding, it has been shown that a restricted geographic distribution of micro-organisms occurs in limnetic, marine, terrestrial, and fossil ecosystems. Similar as, in cryptogams and macrofungi about, 30% of the extant supragenefic taxa, described and undescribed, might be morphological and/or genetic and/or molecular endemics. At the present state of knowledge, micro-organism endemicity can be proved/disproved mainly by flagship species, excluding sites (e.g., university ponds) prone to be contaminated by invaders. In future, genetic and molecular data will be increasingly helpful. The wide distribution of many micro-organisms has been attributed to their small size and their astronomical numbers. However, this interpretation is flawed by data from macrofungi, mosses and ferns, many of which occupy distinct areas, in spite of their minute and abundant means of dispersal (spores). Thus, I suggest historic events (split of Pangaea etc.), limited cyst viability and, especially, time as major factors for dispersal and provinciality of micro-organisms. Furthermore, the true number of species and their distribution can hardly be estimated by theories and statistics but require reliable investigations on the number of morphospecies in representative ecosystems. Generally, the doubts on Beijerinck's famous metaphor "in micro-organisms everything is everywhere" can be focussed on a simple question: If the world is teeming with cosmopolitan unicells, where is everybody?	Salzburg Univ, FB Organ Biol, A-5020 Salzburg, Austria	Salzburg University	Foissner, W (通讯作者)，Salzburg Univ, FB Organ Biol, Hellbrunnerstr 34, A-5020 Salzburg, Austria.	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MAY	2006	45	2					111	136						26	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	044MD					2025-03-11	WOS:000237675700001
J	Solignac, S; Giraudeau, J; de Vernal, A				Solignac, S; Giraudeau, J; de Vernal, A			Holocene sea surface conditions in the western North Atlantic: Spatial and temporal heterogeneities	PALEOCEANOGRAPHY			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; EAST GREENLAND; MARINE ENVIRONMENTS; FJORD GLACIATIONS; SCALE VARIABILITY; LATE QUATERNARY; IRD-DEPOSITION; ICELAND MARGIN; ICE; CLIMATE	Holocene records of sea surface conditions in the western Nordic seas were obtained from quantitative reconstructions based on dinoflagellate cyst assemblages. Two sediment cores from the east Greenland and the north Iceland shelves provide a detailed account of the long- and short-term dynamics of the opposing flows of Arctic versus Atlantic waters. Both marker species and quantitative reconstructions depict an overall trend toward warmer winter temperatures, saltier surface waters, and decreased sea ice extent. The latter is supported by a close relationship between relative abundances of an Atlantic dinocyst species, Nematosphaeropsis labyrinthus, and ice-rafted debris (IRD) records. We propose that the late Holocene increased IRD delivery in the Denmark Strait region was primarily induced by a combination of less extensive sea ice cover under increased Atlantic water inflow and sustained iceberg calving tied to the readvance of the Greenland ice sheet. Our records thus suggest diminishing polar water supplies throughout the Holocene, although the timing of regime changes differs between the western and eastern sides of the Denmark Strait. Finally, comparison of our records with a core from southern Greenland points to very heterogeneous sea surface conditions in the western North Atlantic, which could be explained by the decoupled dynamics of the two Irminger Current branches. Similarities between the southern Greenland marine record and a continental record nearby suggest a close coupling with atmospheric processes, reminiscent of a North Atlantic Oscillation-like climate pattern.	Univ Quebec, GEOTOP, Ctr Rech Geochim Isotop & Geochronol, Montreal, PQ H3C 3P8, Canada; Univ Bordeaux 1, CNRS, UMR 5805, F-33405 Talence, France	University of Quebec; University of Quebec Montreal; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Univ Quebec, GEOTOP, Ctr Rech Geochim Isotop & Geochronol, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	solignac.sandrine@courrier.uqam.ca; j.giraudeau@epoc.u-bordeaux1.fr; devernal.anne@uqam.ca	Giraudeau, Jacques/AAF-5764-2019; de Vernal, Anne/D-5602-2013	Giraudeau, Jacques/0000-0002-5069-4667; de Vernal, Anne/0000-0001-5656-724X; Solignac, Sandrine/0000-0003-3373-6922				Alley RB, 1999, GEOPH MONOG SERIES, V112, P301; Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; Andresen CS, 2005, MAR GEOL, V214, P323, DOI 10.1016/j.margeo.2004.11.010; Andresen CS, 2004, J QUATERNARY SCI, V19, P783, DOI 10.1002/jqs.886; 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J	Gayoso, AM; Fulco, VK				Gayoso, AM; Fulco, VK			Occurrence patterns of <i>Alexandrium tamarense</i> (Lebour) Balech populations in the Golfo Nuevo (Patagonia, Argentina), with observations on ventral pore occurrence in natural and cultured cells	HARMFUL ALGAE			English	Article						Alexandrium; Argentina; harmful algae blooms; Patagonia	DINOFLAGELLATE; PHYTOPLANKTON; WATERS; SEA	Phytoplankton composition and abundance in the Golfo Nuevo, Argentina, have been studied from 1995 to 2001 along with water-temperature, salinity, nutrient and chlorophyll a concentrations. The pattern of seasonal phytoplankton distribution has shown recurrent blooms of Alexandrium tamarense during late winter and spring characterized by strong interannual fluctuations in magnitude. During October and December 2000, a large number of dead penguins (Spheniscus magellanicus) and other marine birds were found along the shore of Chubut. Coincident with those episodes of bird mortality, a bloom of A. tamarense occurred from October through December 2000. The spatial distribution of A. tamarense was patchy and the population density increased near the coast (maximum 22 x 10 3 cells L-1 in the surface layer). A. tamarense cysts were observed in bottom sediments, and increased in abundance from coastal stations (0-5 cysts cm(-3) of sediment) to the offshore, deeper areas (100300 cysts cm(-3)). Multiple regression analysis Suggests that variations in irradiance may be the major source of temporal variability of A. tamarense in Golfo Nuevo. The relationship of A. tainarense cell abundance and that of the dominant phytoplankton species during the spring was investigated using Pearson correlation. A. tamarense cell abundance was significantly correlated with cell abundances of the dinoflagellates Scrippsiello trochoidea and Prorocentrum micons and negatively correlated with phytoflagellates. The morphological variability of A. tainarense from field populations and in clones grown under different conditions was examined. There was great variability in the presence/absence of the ventral pore (an important character used to distinguish species of Alexandrium). (c) 2005 Published by Elsevier B.V.	Consejo Nacl Invest Cient & Tecn, Ctr Nacl Patagonico, RA-9120 Puerto Madryn, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Centro Nacional Patagonico (CENPAT)	Consejo Nacl Invest Cient & Tecn, Ctr Nacl Patagonico, B Brown S-N, RA-9120 Puerto Madryn, Argentina.	fitoplan@cenpat.edu.ar						ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BALECH E., 1977, HIDROBIOLOGIA, V5, P115; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; Carreto J. I, 1998, HARMFUL ALGAE, P135; Carreto J.I., 1998, HARMFUL ALGAE, P131; CARRETO JI, 1986, J PLANKTON RES, V8, P15, DOI 10.1093/plankt/8.1.15; CARRETO JI, 1993, DEV MAR BIO, V3, P377; CLEMENT A, 1993, DEV MAR BIO, V3, P223; ESTEVES JL, 1992, HYDROBIOLOGIA, V242, P115, DOI 10.1007/BF00018067; FUKUYO Y, 1985, B MAR SCI, V37, P529; FULCO VK, IN PRESS P 10 INT C; Gayoso AM, 2001, J PLANKTON RES, V23, P463, DOI 10.1093/plankt/23.5.463; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; HODKISS IJ, 2001, HARMFUL ALGAL BLOOMS, P454; Lechuga-Devéze CH, 1998, B MAR SCI, V63, P503; LORENZEN CJ, 1967, LIMNOL OCEANOGR, V12, P343, DOI 10.4319/lo.1967.12.2.0343; Mendez S.M., 1996, HARMFUL TOXIC ALGAL, P113; Mouzo F.H., 1978, Acta Oceanografica Argentina, V2, P69; MUNOZ-S P, 1986, Revista de Biologia Marina, V22, P141; MUNOZ-S P, 1983, Revista de Biologia Marina, V19, P63; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; QUINTANA F, 2001, UNPUB CAUSA MORTANDA, P1; Rivas A.L., 1989, Geofisica Internacional, V28, P3, DOI DOI 10.22201/IGEOF.00167169P.1989.28.1.1014; RIVAS AL, 1990, OCEANOL ACTA, V13, P15; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; Shumway SE, 2003, HARMFUL ALGAE, V2, P1, DOI 10.1016/S1568-9883(03)00002-7; Smayda TJ, 2000, S AFR J MARINE SCI, V22, P219, DOI 10.2989/025776100784125816; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Sokal R.R., 1981, BIOMETRY, V2nd, P859; SOLIS M, 1998, THESIS INT I INFRAST; STEINDINGER KA, 1996, IDENTIFYING MARINE D, P553; Strickland J.D.H., 1972, A Practical Handbook of Seawater Analysis, Vsecond, P310, DOI [10.25607/OBP-1791, DOI 10.25607/OBP-1791]	33	47	49	1	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	APR	2006	5	3					233	241		10.1016/j.hal.2004.12.010	http://dx.doi.org/10.1016/j.hal.2004.12.010			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	029ZV					2025-03-11	WOS:000236603800001
J	Prámparo, MB; Papú, OH				Pramparo, Mercedes B.; Papu, Oscar H.			Late Maastrichtian dinoflagellate cysts from the Cerro Butalo section, southern Mendoza province, Argentina	JOURNAL OF MICROPALAEONTOLOGY			English	Article						Late Maastrichtian; dinoflagellate cysts; biostratigraphy; Southern Mendoza; Argentina	PALYNOLOGY	The Late Cretaceous Atlantic transgression in southern South America is recorded in western Argentina in the upper part of the Malargue Group. The Cerro Butalo section outcrops in the south of Mendoza Province and comprises sediments attributable to the Jaguel and Roca formations. Well-preserved palynological associations were recovered from this section. Only the marine associations - dinoflagellate cysts, acritarchs and green algae - are considered in this article. A Late Maastrichtian age is suggested for the Roca and Jaguel formations based on the presence of Deflandrea galeata and Disphaerogena carposphaeropsis in the lower part of the section and Glaphyrocysta petforata in the upper part of the section and the absence of any Danian cosmopolitan markers. Variations in dinoflagellate cyst species diversity throughout the section permit recognition of two intervals that are probably related to different palaeoenvironmental conditions connected with episodes of sea-level fluctuation.	Consejo Nacl Invest Cient & Tecn, Unidad Paleopalinol, Inst Argentino Nivologia Glaciol & Ciencias Ambie, IANIGLA,CRICYT, RA-5500 Mendoza, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); CRICYT; University Nacional Cuyo Mendoza	Prámparo, MB (通讯作者)，Consejo Nacl Invest Cient & Tecn, Unidad Paleopalinol, Inst Argentino Nivologia Glaciol & Ciencias Ambie, IANIGLA,CRICYT, CC 131, RA-5500 Mendoza, Argentina.	mprampar@lab.cricyt.edu.ar; opapu@hotmail.com						Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1996, GRONLANDS GEOLOGISKE; ARAI M, 1994, 3 S CRET BRAS UNESP, P59; Benson D.G. Jr., 1976, Tulane Stud Geol Paleont, V12, P169; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; BRINKHUIS H, 1988, REV PALAEOBOT PALYNO, V56, P5, DOI 10.1016/0034-6667(88)90071-1; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; Cookson I. 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Micropalaentol.	APR	2006	25		1				23	33		10.1144/jm.25.1.23	http://dx.doi.org/10.1144/jm.25.1.23			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	052WQ		hybrid			2025-03-11	WOS:000238265000003
J	Riding, JB; Wilkinson, IP; Jones, LD; Freeborough, K				Riding, James B.; Wilkinson, Ian P.; Jones, Lee D.; Freeborough, Katy			The occurrence of dinoflagellate cysts in calcareous/siliceous microfossil preparations from the Eocene of southeast England	JOURNAL OF MICROPALAEONTOLOGY			English	Article									British Geol Survey, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; ipw@bgs.ac.uk; ldjon@bgs.ac.uk; kayo@bgs.ac.uk						[Anonymous], 1996, Palynology: principles and applications; Costa L.I., 1992, P99; DAVEY RJ, 1966, STUDIES MESOZOIC S 3, P3; EAGAR SH, 1963, NATURE, V198, P81, DOI 10.1038/198081a0; GEORGE W, 1978, TERTIARY RES, V2, P5; KING C, 1983, REPORT I GEOLOGICAL, V82, P40; Riding James B., 2004, Revista Brasileira de Paleontologia, V7, P13; Wilken M, 2004, BMC PUBLIC HEALTH, V4, DOI 10.1186/1471-2458-4-4; WILKINSON IPO, 2004, IR04093; WILLIAMS GL, 1966, BRIT MUSEUM B, V3, P20	10	5	5	0	0	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	APR	2006	25		1				35	36		10.1144/jm.25.1.35	http://dx.doi.org/10.1144/jm.25.1.35			2	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	052WQ		hybrid			2025-03-11	WOS:000238265000004
J	Figueroa, RI; Rengefors, K; Bravo, I				Figueroa, RI; Rengefors, K; Bravo, I			Effects of parental factors and meiosis on sexual offspring of <i>Gymnodinium nolleri</i> (dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						AFLPs; dinophyceae; encystment; gametes; Gymnodinium nolleri; life-cycle; nitrates; nutritional effects; phosphates; principal component analysis reproduction	MICRORETICULATE DINOFLAGELLATE CYSTS; SP. INED. DINOPHYCEAE; LIFE-CYCLE EVENTS; GONYAULAX-TAMARENSIS; CATENATUM DINOPHYCEAE; ALEXANDRIUM-CATENELLA; POPULATION-DYNAMICS; REPRODUCTION; ENCYSTMENT; CULTURE	Clonal strains of the dinoflagellate Gymnodinium nolleri Ellegaard and Moestrup were intercrossed to determine if cyst-related traits are genetically regulated and to clarify unknown aspects in the sexuality of this species. The objectives were to determine whether the parental identity influenced the physiological and morphological aspects of the cyst offspring, and to describe and compare nuclear development and cell division of encysting and non-encysting zygotes. Variables characteristic of each parental cross (difference in growth rates among parents, cyst production (CP), and genetic distance (GD) among parents assessed via an amplified fragment length analysis analysis) were studied to seek for possible relationships of the parental crosses with some characteristics of the cyst offspring (cyst size, length of dormancy period, germination success, and germling viability (V)). A principal component analysis using these variables showed three main results: (1) the dormancy period of cysts responded to a simple pattern of inheritance, (2) the larger the GD between parents, the smaller the CP, and progeny V, and (3) the size of cysts was influenced by both CP and the parental strain identity. A stable inheritance of the short dormancy period (14.6 +/- 5.5 days), dominant over medium (31.0 +/- 8.5 days) and long periods (52.7 +/- 9.2 days), was confirmed through two subsequent generations of cysts. The regulation of the sexual processes by a multiple loci system is discussed based on the pattern of inheritance of the dormancy period and the number of sexual recombination events recorded within cultures with self-CP capability. Fusion of the gamete nuclei happened 0-48 h after the total cytoplasmic fusion. The nucleus of the zygote was bilobed and had thick and distinct chromosomes. Similar processes of nuclear and cell division occurred in the non-encysting or encysting planozygote, and were characterized by the loss of the chromosomal structure, an apparent increase of the DNA content, and the formation of thinner chromosomes.	Inst Oceanog Vigo, Vigo 36200, Spain; Lund Univ, Ekol Inst, S-22362 Lund, Sweden	Spanish Institute of Oceanography; Lund University	Inst Oceanog Vigo, Cao Estai Canido, Vigo 36200, Spain.	Rosabel.figueroa@vi.ieo.es	Rengefors, Karin/K-5873-2019; Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015	Bravo, Isabel/0000-0003-3764-745X; Figueroa, Rosa/0000-0001-9944-7993; Rengefors, Karin/0000-0001-6297-9734				AN KH, 1992, BOT MAR, V35, P61, DOI 10.1515/botm.1992.35.1.61; ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson DM, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1997, ADV MAR BIOL; Beam C. 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Phycol.	APR	2006	42	2					350	362		10.1111/j.1529-8817.2006.00191.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00191.x			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	029GO					2025-03-11	WOS:000236549100009
J	Kremp, A; Parrow, MW				Kremp, A; Parrow, MW			Evidence for asexual resting cysts in the life cycle of the marine peridinoid dinoflagellate, <i>Scrippsiella hangoei</i>	JOURNAL OF PHYCOLOGY			English	Article						Baltic Sea; dinoflagellate; DNA content; dormancy; flow cytometry resting cyst; Scrippsiella hangoei	GONYAULAX-POLYEDRA STEIN; RELATIVE PLOIDY LEVELS; SEXUAL REPRODUCTION; DNA-CONTENT; GYMNODINIUM-CATENATUM; POPULATION-DYNAMICS; PLANKTONIC DIATOMS; CELL-CYCLE; DINOPHYCEAE; ENCYSTMENT	Scrippsiella hangoei (Schiller) Larsen is a peridinoid dinoflagellate that grows during winter and spring in the Baltic Sea. In culture this species formed round, smooth cysts when strains were mixed, indicating heterothallic sexuality and hypnozygote production. However, cysts of the same morphology were also formed in clonal strains exposed to slightly elevated temperature. To better understand the role of cysts in the life cycle of S. hangoei, cyst formation and dormancy were examined in culture experiments and the cellular DNA content of flagellate cells and cysts was compared in clonal and mixed strains using flow cytometry. S. hangoei exhibited a high rate of cyst formation in culture. Cysts produced in both clonal and mixed strain cultures were thick-walled and underwent a dormancy period of 4 months before germinating. The S. hangoei flagellate cell population DNA distributions consisted of 1C, intermediate, and 2C DNA, indicative of respective eukaryotic cell cycle phases G1, S, and G2M. The majority (> 95%) of cysts had a measured DNA content equivalent to the lower 1C DNA value, indicating a haploid nuclear phase and an asexual mode of cyst formation. A small percentage (< 5%) of cysts produced in the mixed strain culture had 2C DNA, and thus could have been diploid zygotes. These findings represent the first measurements of dinoflagellate resting cyst DNA content, and provide the first quantitative evidence for dinoflagellate asexual resting cysts. Asexual resting cysts may be a more common feature of dinoflagellate life cycles than previously thought.	Univ Helsinki, Tvarminne Zool Stn, Helsinki 10900, Finland; N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA	University of Helsinki; North Carolina State University	Univ Helsinki, Tvarminne Zool Stn, Helsinki 10900, Finland.	anke.kremp@ymparisto.fi	Kremp, Anke/I-8139-2013; Parrow, Matthew/HMO-6676-2023	Parrow, Matthew/0000-0002-3197-2510				ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Bewley J. D., 1982, Physiology and biochemistry of seeds in relation to germination. Vol.2. 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Phycol.	APR	2006	42	2					400	409		10.1111/j.1529-8817.2006.00205.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00205.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	029GO					2025-03-11	WOS:000236549100013
J	Calado, AJ; Craveiro, SC; Daugbjerg, N; Moestrup, O				Calado, AJ; Craveiro, SC; Daugbjerg, N; Moestrup, O			Ultrastructure and LSU rDNA-based phylogeny of <i>Esoptrodinium gemma</i> (Dinophyceae), with notes on feeding behavior and the description of the flagellar base area of a planozygote	JOURNAL OF PHYCOLOGY			English	Article						Bernardinium bernardinense; Dinophyceae; Esoptrodinium gemma; eyespot; flagellar apparatus; LSU rDNA; phagotrophy; phylogeny; planozygote; ultrastructure	ELECTRON-MICROSCOPIC OBSERVATIONS; FRESH-WATER; MARINE DINOFLAGELLATE; GYMNODINIUM; APPARATUS; PERIDINIOPSIS; LIGHT; DNA; ARCHITECTURE; AMPHIDINIUM	A small, freshwater dinoflagellate with an incomplete cingulum, identified as Esoptrodinium gemma Javornicky (=Bernardinium bernardinense sensu auctt. non sensu Chodat), was maintained in mixed culture and examined using light and serial section TEM. Vegetative flagellate cells, large cells with two longitudinal flagella (planozygotes), and cysts were examined. The cells displayed a red eyespot near the base of the longitudinal flagellum, made of two or three layers of pigment globules not bounded by a membrane. Yellow-green, band-shaped chloroplasts, bounded by three membranes and containing lamella with three thylakoids, were present in both flagellate cells and cysts. Most cells had food vacuoles, containing phagotrophically ingested chlamydomonads or chlorelloid green algae; ingestion occurred through the ventral area, involving a thin pseudopod apparently driven by the peduncle. The pusule was tubular, with numerous diverticula in its distal portion, and opened into the longitudinal flagellar canal. Three roots were associated with each pair of flagellar bases, both in vegetative cells and in a planozygote. The longitudinal microtubular root bifurcated around the longitudinal basal body. The planozygote contained a single peduncle and associated structures, and a single transverse flagellar canal with the two converging transverse flagella. Using two ciliates as outgroup species, phylogenetic analyses based on maximum parsimony, neighbor-joining and posterior probability (Bayesian analysis) supported a clade comprising Esoptrodinium, Tovellia, and Jadwigia.	Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; Univ Copenhagen, Inst Biol, Dept Phycol, DK-1353 Copenhagen K, Denmark	Universidade de Aveiro; University of Copenhagen	Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal.	acalado@bio.ua.pt	Calado, Sandra Carla/A-6791-2016; Calado, Antonio Jose/D-6263-2015; Daugbjerg, Niels/D-3521-2014	Calado, Sandra Carla/0000-0002-2738-7626; Calado, Antonio Jose/0000-0002-9711-0593; Daugbjerg, Niels/0000-0002-0397-3073; Moestrup, Ojvind/0000-0003-0965-8645				[Anonymous], B SOC BOT GENEVE 2; [Anonymous], 1982, J PHYCOL; [Anonymous], 1984, J PROTOZOOL; [Anonymous], 1917, Bulletin International de l'Academie des Sciences de Cracovie, Classe des Sciences Mathematiques et Naturelles, serie B: Sciences Naturelles; [Anonymous], 2002, SYSTEMATIC BIOL; Calado AJ, 1997, PHYCOLOGIA, V36, P47, DOI 10.2216/i0031-8884-36-1-47.1; Calado AJ, 2005, PHYCOLOGIA, V44, P112, DOI 10.2216/0031-8884(2005)44[112:OTFDPI]2.0.CO;2; Calado AJ, 2002, PHYCOLOGIA, V41, P567, DOI 10.2216/i0031-8884-41-6-567.1; Calado AJ, 1999, EUR J PHYCOL, V34, P179, DOI 10.1080/09670269910001736232; Calado AJ, 1998, J PHYCOL, V34, P536, DOI 10.1046/j.1529-8817.1998.340536.x; CHODAT R., 1924, Bull. 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Phycol.	APR	2006	42	2					434	452		10.1111/j.1529-8817.2006.00195.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00195.x			19	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	029GO		Bronze			2025-03-11	WOS:000236549100017
J	Barrón, E; Gómez, JJ; Goy, A; Pieren, AP				Barrón, E; Gómez, JJ; Goy, A; Pieren, AP			The Triassic-Jurassic boundary in Asturias (northern Spain):: Palynological characterisation and facies	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Triassic-Jurassic; biostratigraphy; palynology; climate change	SEA-LEVEL CHANGE; RHAETIAN STAGE; EXTINCTION; BIOSTRATIGRAPHY; STRATIGRAPHY; TERRESTRIAL; MICROFLORA; DISCOVERY; SEQUENCES; AMMONITE	A palynological, biostratigraphic, sedimentological and sequence stratigraphy study of the Triassic-Jurassic transition in Asturias (northern Spain) was performed by logging and sampling the cores of two boreholes, the Cantavieyo and Vilorteo boreholes. Four lithological units were differentiated and correlated. The lower unit, composed of mudstones and evaporites deposited in coastal lake to subaerial sabkha and distal alluvial environments, correlated in part with the Upper Triassic Keuper facies present ill most of western Europe. The middle unit of well bedded carbonates corresponds to the Solis Member of the Gijon Formation. This unit was deposited on a shallow, subtidal to inter- and supratidal carbonate platform influenced by storms and with interbedded distal fan-delta facies. The Triassic-Jurassic boundary has been located within the carbonates of the Solis Member, which contain a Hettangian ammonite, Caloceras pirondii (Reynes), in tempestitic carbonates attributed to the upper part of this unit. The upper unit, the Barzana Member, is composed of mudstones, evaporites and carbonates, respectively, deposited in distal alluvial environments, in supratidal sabkha environments, and on a shallow subtidal to intertidal platform. Overlying the upper unit, or as a time equivalent of the Barzana Member, the Fabares Member is composed of a carbonate breccia with a lutitic matrix, interpreted as formed by the dissolution of the evaporites of the Barzana Member and the collapse of the originally interbedded carbonates and mudstones. A total of 49 palynomorph taxa have been recorded: 20 spore taxa, 24 pollen taxa, 1 acritarch, 2 prasinophytes, and 2 dinoflagellate cysts. Three palynological assemblages (PA) have been distinguished. PA1, which is typically Rhaetian, corresponds to the Rhaetipollis germanicus Zone. PA2 can be Rhaetian and/or Hettangian in age. PA3, which is Hettangian in age, partly corresponds to the Kraeuselisporites reissingeri Zone. These zones have been correlated with similar zones in northwestern Europe. Palaeoecological analysis of the palynomorph assemblages indicates marked palaeofloral renewal, from diversified, Late Triassic xerophilous plants to an impoverished palaeofloral community at the Triassic-Jurassic transition. The latter was composed of a poorly diversified group of conifers and ferns. The and climate of the Late Triassic was followed by a short, humid event at the beginning of the Hettangian, during which the renewal and important recovery of vascular cryptogams and conifers occurred. The later predominance of xerophilous species in the Hettangian indicates a recovery of and climatic conditions. After the turnover at the end of the Triassic, and especially during the Hettangian, the recovery of new species is well marked. Of a total of 21 palynomorphs, 7 species did not surpass the base of the Triassic-Jurassic transition, 6 species appeared in this transition, and 22 species appeared in the Hettangian, marking an outstanding phase of recovery for the plants that generated the studied palynomorphs. (c) 2006 Elsevier B.V. All rights reserved.	Univ Complutense, Dept Estratig & UEI Correlac Estratigraf, Fac Ciencias Geol, E-28040 Madrid, Spain; Univ Complutense, Inst Geol Econ, CSIC, E-28040 Madrid, Spain; Univ Complutense, Dept Palaeontol & UEI Paleontol, Fac Ciencias Geol, Inst Geol Econ,CSIC, E-28040 Madrid, Spain	Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE); Complutense University of Madrid; Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE)	Univ Complutense, Dept Estratig & UEI Correlac Estratigraf, Fac Ciencias Geol, E-28040 Madrid, Spain.	jgomez@geo.ucm.es	Barrón, Eduardo/L-4726-2014; Pieren Pidal, Agustin Pedro/A-5610-2016	Goy, Antonio/0000-0002-2331-9765; Barron, Eduardo/0000-0003-4979-1117; Pieren Pidal, Agustin Pedro/0000-0001-8783-2368				Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; Adloff M.C., 1974, Comunicacoes Servicos Geologicos Portugal, VLVIII, P91; Adloff M. 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A., 2002, Review of Palaeobotany and Palynology, V119, P113, DOI 10.1016/S0034-6667(01)00132-4; VEGA LCS, 1969, SEMIN ESTRATIGR, V4, P41; VISSCHER H, 1981, REV PALAEOBOT PALYNO, V34, P115, DOI 10.1016/0034-6667(81)90069-5; Ward PD, 2001, SCIENCE, V292, P1148, DOI 10.1126/science.1058574; WARREN JK, 1985, AAPG BULL, V69, P1013; Warrington G., 1975, Bulletin geol Surv Gt Br, VNo. 50,1975, P37; WARRINGTON G, 1994, GEOL MAG, V131, P191, DOI 10.1017/S0016756800010724; WEEMS RE, 1992, PALAEOGEOGR PALAEOCL, V94, P1, DOI 10.1016/0031-0182(92)90111-H	107	62	68	0	18	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	2006	138	3-4					187	208		10.1016/j.revpalbo.2006.01.002	http://dx.doi.org/10.1016/j.revpalbo.2006.01.002			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	040SR		Green Accepted			2025-03-11	WOS:000237401200003
J	Torricelli, S				Torricelli, Stefano			Dinoflagellate cyst stratigraphy of the Scisti a Fucoidi formation (early cretaceous) from Piobbico, central Italy: Calibrated events for the Albian of the tethyan realm	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						biostratigraphy; dinoflagellate cysts; early cretaceous; albian; tethyan realm; central Italy	SITE-545	Rich and well preserved organic-walled dinoflagellate cyst assemblages recovered from the Scisti a Fucoidi Formation at Piobbico, central Italy are presented. Distributions of 83 taxa, plotted against the independent stratigraphic framework established from planktonic foraminifers and nannofossils, are compared with ranges documented in the literature in order to identify and calibrate reference horizons for the Albian dinoflagellate cyst stratigraphy of the Tethyan Realm. The following events have been selected: the lowest occurrences of Kleithriasphaeridium atlasiense and Tehamadinium coummia at the Aptian/Albian boundary, of Leberidocysta defloccata in the Lower Albian, of Adnatosphaeridium tutulosum, Litosphaeridium arundum and Ovoidinium sp. A sensu Davey (1979) in the Middle Albian, of Dapsilidinium? pumilum, Litospbaeridium conispinum, Tehamadinium mazaganense and Hapsocysta dictyota in the Upper Albian; the highest consistent occurrences of Hapsocysta peridictya in the Lower Albian, of Codoniella psygma and Damassadinium chibane in the Middle Albian, of Tebamadinium sousense in the Upper Albian.	ENI SpA, Explorat & Prod Div, I-20097 San Donato Milanese, Italy	Eni SpA	Torricelli, S (通讯作者)，ENI SpA, Explorat & Prod Div, Via Emilia 1, I-20097 San Donato Milanese, Italy.	stefano.torricelli@agip.it						[Anonymous], 1996, Palynology: principles and applications; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BRINKHUIS H, 2004, JURASSIC CRETACEOUS; Coccioni R., 1987, BOLLETTINO SOCIET GE, V106, P183; Cookson I. C., 1962, Micropaleontology, V8, P485, DOI 10.2307/1484681; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Davey R.J., 1971, VERHANDEL KONINKL NE, V26, P1; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; ERBA E, 1988, Rivista Italiana di Paleontologia e Stratigrafia, V94, P249; ERBA E, 1986, THESIS U MILANO; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fiet N, 2001, CRETACEOUS RES, V22, P63, DOI 10.1006/cres.2000.0237; Hardenbol J., 1998, MESOZOIC CENOZOIC SE, V60, DOI [10.2110/pec.98.02.0003, DOI 10.2110/PEC.98.02.0003]; Kennedy WJ, 2000, CRETACEOUS RES, V21, P591, DOI 10.1006/cres.2000.0223; KUPEUPLE PA, 1979, INIT REPTS DEEP SEA, V48, P451; LECKIE RM, 1984, INITIAL REP DEEP SEA, V79, P579; MACHOUR L, 1988, THESIS U PROVENCE; MASURE E, 1984, B SOC GEOL FR, V26, P93; MASURE E, 1988, ODP SCI RES, V101, P121; Nohr-Hansen Henrik, 1993, Gronlands Geologiske Undersogelse Bulletin, V166, P1; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; *SHIPB SCI PART, 2002, P ODP IN REPTS, P198; Silva IP, 1999, GEOL S AM S, P301; TESTOLIN R, 1992, ACTA HORTIC, V313, P99, DOI 10.17660/ActaHortic.1992.313.11; TORNAGHI M E, 1989, Rivista Italiana di Paleontologia e Stratigrafia, V95, P223; Torricelli S, 2001, RIV ITAL PALEONTOL S, V107, P79, DOI 10.13130/2039-4942/5425; Torricelli S, 2000, REV PALAEOBOT PALYNO, V108, P213, DOI 10.1016/S0034-6667(99)00041-X; WEZEL CF, 1985, GIORN GEOL, V47, P281; WILLIAMS GL, 2004, P ODP SCI RES LEG 18; WILLIAMS GL, 1998, AM ASS STRAT PALYNOL, V34	33	7	9	0	2	UNIV STUDI MILANO	MILANO	C/O RIVISTA ITALIANA PALEONTOLOGIA STRATIGRAFIA, VIA MANGIAGALLI, 34, 20133 MILANO, ITALY	0035-6883	2039-4942		RIV ITAL PALEONTOL S	Riv. Ital. Paleontol. Stratigr.	APR	2006	112	1					95	111						17	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	047NR					2025-03-11	WOS:000237886500006
J	Lambert, O; Louwye, S				Lambert, O; Louwye, S			<i>Archaeoziphius microglenoideus</i>, a new primitive beaked whale (Mammalia, Cetacea, Odontoceti) from the Middle Miocene of Belgium	JOURNAL OF VERTEBRATE PALEONTOLOGY			English	Article							DINOFLAGELLATE CYST; NORTHERN BELGIUM; PLIOCENE	Three partial skulls of odontocetes from the Miocene of Antwerp and Kessel, northern Belgium (southern North Sea Basin) are described here as a new genus and species of beaked whale (Ziphiidae), Archaeoziphius microglenoideus. This small new whale is one of the most archaic beaked whales, because of its low vertex, thin and laterally directed premaxillary crests, low contact between the supraoccipital and the frontals on the vertex, and its free atlas. It is also characterized by the strong transverse compression of the frontals on the vertex and a reduced glenoid surface on the squamosal; the two last characters might be considered as derived. Nasals wider than the frontals on the vertex might group A. microglenoideus with the extant larger genera Berardius and Tasmacetus; the nodular frontals and the premaxillary crests are more similar to the condition in Berardius. A sediment sample from the cetacean-bearing strata at Kessel is dated with dinoflagellate cysts as middle Miocene, tentatively late Langhian to early Serravallian, i.e.. from ca. 15 Ma to ca. 13.2 Ma. Archaeoziphius microglenoideus is therefore the oldest reported beaked whale known bycranial material.	Inst Royal Sci Nat Belgique, Dept Paleontol, B-1000 Brussels, Belgium; Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium	Ghent University	Inst Royal Sci Nat Belgique, Dept Paleontol, Rue Vautier 29, B-1000 Brussels, Belgium.	Olivier.Lambert@naturalsciences.be; stephen.louwye@rug.ac.be	Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Lambert, Olivier/0000-0003-0740-5791				Abel O., 1905, Memoires du Musee royal d'histoire naturelle de Belgique, V3, P1; Abel O., 1901, M M MUS R HIST NAT B, V1, P1; Abele S, 2000, EUR J ORG CHEM, V2000, P1; Bianucci Giovanni, 1997, Palaeontographia Italica, V84, P163; Bianucci Giovanni, 1992, Bollettino della Societa Paleontologica Italiana, V31, P261; Brisson M.J., 1762, QUADRUPEDUM SCILICET; Dalebout ML, 1998, MOL ECOL, V7, P687, DOI 10.1046/j.1365-294x.1998.00380.x; Dalebout ML, 2002, MAR MAMMAL SCI, V18, P577, DOI 10.1111/j.1748-7692.2002.tb01061.x; de Muizom C., 1991, B MUS NATL HIST NAT, V3-4, P279; de Muizon C., 1985, Travaux de l'Institut Francais d'Etudes Andines, V27, P1; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; DEBUS BAL, 1868, B ACAD ROYALE SCI BE, V25, P621; DEMUIZON C, 1983, CR ACAD SCI II, V297, P85; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Duvernoy G, 1851, Annales des Sciences Naturelles, Paris, Serie 3, Zoologie, V15, P52; FLOWER W.H., 1867, The Transactions of the Zoological Society of London, V6, P87, DOI DOI 10.1111/J.1096-3642.1867.TB00572.X; Fordyce R. Ewan, 1994, Proceedings of the San Diego Society of Natural History, V29, P147; FORDYCE RE, 1994, ANNU REV EARTH PL SC, V22, P419, DOI 10.1146/annurev.ea.22.050194.002223; Fordyce RE, 2002, ANTARCT SCI, V14, P37, DOI 10.1017/S0954102002000561; Fordyce RE, 2002, SM C PALEOB, P185; FRASER F. C., 1960, BULL BRIT MUS [NAT HIST] ZOOL, V7, P1; Geisler Jonathan H., 2003, Journal of Mammalian Evolution, V10, P23, DOI 10.1023/A:1025552007291; Gray J.E., 1850, CATALOGUE SPECIMEN 1; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; Heyning J E., 1989, Contrib. Sci. Nat. Hist. Museum Los Angeles Cty, V405, P1; Heyning John E., 1996, Contributions in Science (Los Angeles), V464, P1; HUYGHEBAERT B, 1979, MEDEDELINGEN WERKGRO, V16, P59; Louwye S, 2001, GEOBIOS-LYON, V34, P121; Louwye S, 2000, GEOL MAG, V137, P381, DOI 10.1017/S0016756800004258; MISONNE XAVIER, 1958, BULL INST ROY SCI NAT BELGIQUE, V34, P1; MOORE J C, 1968, Fieldiana Zoology, V53, P209; Muizom C., 1987, AM MUS NOVIT, V2904, P1; ROSS G J B, 1984, Annals of the Cape Provincial Museums Natural History, V15, P173; RUTOT A, 1909, B SOC GEOLOGIQUE BEL, V23, P387; STRAUSS C, 2001, EOLOGISCHES JB A, V111, P395; TAVERNIER R, 1963, MEM SOC BELG GEOL PA, V8, P7; van Helden AL, 2002, MAR MAMMAL SCI, V18, P609; Williams Graham L., 1998, AASP Contributions Series, V34, P1	38	34	38	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0272-4634	1937-2809		J VERTEBR PALEONTOL	J. Vertebr. Paleontol.	MAR 30	2006	26	1					182	191		10.1671/0272-4634(2006)26[182:AMANPB]2.0.CO;2	http://dx.doi.org/10.1671/0272-4634(2006)26[182:AMANPB]2.0.CO;2			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	030FB					2025-03-11	WOS:000236618500018
J	Kawamura, H; Holbourn, A; Kuhnt, W				Kawamura, H; Holbourn, A; Kuhnt, W			Climate variability and land-ocean interactions in the Indo Pacific Warm Pool: A 460-ka palynological and organic geochemical record from the Timor Sea	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; pollen; Timor Sea; Australian Monsoon; late pleistocene	WALLED DINOFLAGELLATE CYSTS; LAST GLACIAL MAXIMUM; INDIAN-OCEAN; WEST-JAVA; QUATERNARY; VEGETATION; NORTHERN; LEVEL; THROUGHFLOW; AUSTRALIA	Climatic conditions in the western Timor Sea and the adjacent northwestern part of Australia are reconstructed for the last 460 ka, based oil geochemical and palynological proxy records of paleoproductivity and land vegetation (precipitation) from IMAGES Core MD01-2378. Reduced precipitation and elevated productivity characterize glacial stages, whereas enhanced precipitation and reduced productivity are typical of interglacial stages. A long-term reduction in precipitation over the last 320 ka occurred in two steps at approximately 300 ka and 180 ka BP that are clearly recognizable in the pollen record. Variations in paleoproductivity and paleoclimate in the Timor Sea and adjacent landmasses appear to be driven by similar mechanisms that are related to the precession-control led Australian monsoon system. (c) 2005 Elsevier B.V All rights reserved.	Hokkaido Univ, Grad Sch Sci, COE Neosci Nat Hist, Sapporo, Hokkaido 0600810, Japan; Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany	Hokkaido University; University of Kiel	Hokkaido Univ, Grad Sch Sci, COE Neosci Nat Hist, N10 W8, Sapporo, Hokkaido 0600810, Japan.	hkawamura@nature.sci.hokudai.ac.jp		Holbourn, Ann/0000-0002-3167-0862				BARMAWIDJAJA BM, 1993, PALAEOGEOGR PALAEOCL, V101, P147, DOI 10.1016/0031-0182(93)90157-E; Beaufort L, 2001, SCIENCE, V293, P2440, DOI 10.1126/science.293.5539.2440; Beaufort L, 2003, MAR GEOL, V201, P53, DOI 10.1016/S0025-3227(03)00208-1; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; Bowler JM, 2001, QUATERN INT, V83-5, P63, DOI 10.1016/S1040-6182(01)00031-3; Bray NA, 1997, GEOPHYS RES LETT, V24, P2569, DOI 10.1029/97GL51793; Chen RF, 2000, ORG GEOCHEM, V31, P1755, DOI 10.1016/S0146-6380(00)00075-9; Chivas AR, 2001, QUATERN INT, V83-5, P19, DOI 10.1016/S1040-6182(01)00029-5; CLARKE AJ, 1994, J PHYS OCEANOGR, V24, P1224, DOI 10.1175/1520-0485(1994)024<1224:ISLITN>2.0.CO;2; Clement AC, 1999, GEOPH MONOG SERIES, V112, P363; Dai A, 2000, GEOPHYS RES LETT, V27, P1283, DOI 10.1029/1999GL011140; De Deckker P, 2003, GLOBAL PLANET CHANGE, V35, P25, DOI 10.1016/S0921-8181(02)00089-9; Gagan MK, 2004, QUATERN INT, V118, P127, DOI 10.1016/S1040-6182(03)00134-4; Godfred-Spenning CR, 2002, INT J CLIMATOL, V22, P509, DOI 10.1002/joc.710; Hantoro WS, 1997, QUATERN INT, V37, P73, DOI 10.1016/1040-6182(96)00010-9; HANTORO WS, 1995, QUATERN INT, V30, P129; Harris PG, 1996, NATURE, V383, P63, DOI 10.1038/383063a0; HESSE PP, 1994, QUATERNARY SCI REV, V13, P257, DOI 10.1016/0277-3791(94)90029-9; Hesse PP, 2003, QUATERNARY SCI REV, V22, P2007, DOI 10.1016/S0277-3791(03)00164-1; Holbourn A, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2004PA001094; Hope G, 2004, QUATERN INT, V118, P103, DOI 10.1016/S1040-6182(03)00133-2; JANSEN JHF, 1986, SCIENCE, V232, P619, DOI 10.1126/science.232.4750.619; Kershaw A., 1993, Proceedings of the Ocean Drilling Program, Scientific Results, V133, P107, DOI [10.2973/odp.proc.sr.133.221.1993, DOI 10.2973/0DP.PR0C.SR.133.221.1993]; Kershaw AP, 2003, MAR GEOL, V201, P81, DOI 10.1016/S0025-3227(03)00210-X; Koutavas A, 2002, SCIENCE, V297, P226, DOI 10.1126/science.1072376; Liu ZH, 2004, NATURE, V427, P720, DOI 10.1038/nature02338; Manins P., 2001, Atmosphere. 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Micropaleontol.	MAR 22	2006	59	1					1	14		10.1016/j.marmicro.2005.09.001	http://dx.doi.org/10.1016/j.marmicro.2005.09.001			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	028QZ					2025-03-11	WOS:000236504600001
J	Torricelli, S; Knezaurek, G; Biffi, U				Torricelli, S; Knezaurek, G; Biffi, U			Sequence biostratigraphy and paleo environmental reconstruction in the Early Eocene Figols Group of the Tremp-Graus Basin (south-central Pyrenees, Spain)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; foraminifers; paleoecology; sequence stratigraphy; Early Eocene; Spanish Pyrenees	WALLED DINOFLAGELLATE CYSTS; LARGER FORAMINIFERA; SURFACE SEDIMENTS; ATLANTIC; MIDDLE; ASSEMBLAGES; INDICATORS; MIOCENE; PALYNOFACIES; DINOCYST	The dinoflagellate cyst, palynofacies and foraminiferal records from the Early Eocene Figols Group of the Spanish Pyrenees exhibit major changes associated with relative sea-level fluctuations and variations in efficiency of the fluvial systems. The mixed siliciclastic-carbonate marine succession exposed in the Merli-Esdolomada area was deposited on the shelf in a tectonically active basin, under oxic conditions, in shallow to moderately deep marine waters (close to the lower boundary of the photic zone) influenced by river discharge from adjacent emerged lands. Sedimentary cycles are mainly recorded by fine-grained deposits. The paleoenvironmental interpretation of palynological and calcareous microfaunal records allows the definition of depositional sequences and enables to trace basinward surfaces identified in more proximal settings by means of sedimentological facies analysis. At the same time, the solid regional stratigraphic framework already available for the Figols Group allows new insights on the paleoecology of extinct taxa. The Merli-Esdolomada section (ME) spans two 3rd order sequences. The upper sequence reflects more marginal marine conditions than the lower one, thus pointing to an overall shallowing trend with time. In the lower sequence the maximum flooding interval is characterised by a rich and diverse microfauna, highest relative abundances of marine phytoplankton and typically neritic dinoflagellate cyst (dinocyst) assemblages dominated by Spiniferites and Cordosphaeridium. The final phase of the highstand systems tract, in proximity of the main sequence boundary, is characterised by a decrease in abundance and diversity of dinocysts, with the dominance of the lagoonal genus Polysphaeridium, and by decreased microfaunal diversity (discorbids, miliolids, larger foraminifers). Palynological records permit the reconstruction of activation and deactivation phases of the fluvial systems, variations in runoff from the hinterland, nutrient delivery to the sea and productivity in surface waters of the Tremp-Graus Basin. The overall abundance of Spiniferites and the scarcity of peridinioid cysts, Lingulodinium, Pediastrum and Botryococcus algae are interpreted to indicate oligotrophic conditions during the deposition of the investigated succession. Recurrent intervals where the temporary disappearance of Spiniferites corresponds to highest relative abundances of Operculodinium and herbaceous debris are the main evidence for river plumes and denote periods of enhanced fluvial discharge reflecting a Milankovitch-type cyclicity. The Rotalia group, which shows abundance peaks of Cuvillierina spp. in the shallower intervals, is often associated with these episodes, thus suggesting for this taxon more tolerance to turbidity than larger foraminifera. Within the maximum flooding zone, a Thalassiphora patula acme corresponding to the local disappearance of Homotryblium is deemed to record the distal expression of a fluvial activation which triggered water salinity stratification. Despite broad morphological similarities, Homotriblium exhibits more cosmopolitan preferences than Polysphaeridium, which is instead confirmed as a lagoonal euryhaline taxon. The increase of Spinizonocolpites pollen toward the top of the Figols Group records the northwestward migration of Nypa mangrove-palms from southern Europe during the mid Early Eocene. (c) 2005 Elsevier B.V. All rights reserved.	ENI SpA, Explorat & Prod Div, I-20097 San Donato Milanese, Italy	Eni SpA	ENI SpA, Explorat & Prod Div, Via Emilia 1, I-20097 San Donato Milanese, Italy.	stefano.torricelli@agip.it						[Anonymous], 1993, SPECIAL PUBL INT ASS; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: principles and applications, P205; Batten DJ., 1996, Palynology: principles and applications, P191; Below Raimond, 1997, Palaeontographica Abteilung B Palaeophytologie, V242, P1; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Berggren WA, 1997, MICROPALEONTOLOGY, V43, P1, DOI 10.2307/1485988; BILLMAN H, 1980, Schweizerische Palaeontologische Abhandlungen, V101, P71; Boersema A., 1980, INTRO MARINE MICROPA, P19; Boersma A., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V115, P315, DOI 10.2973/odp.proc.sr.115.146.1990; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; CARMINATTI M, 1992, THESIS PARMA U ITALY; Caro Y., 1973, Revista Esp Micropaleont, V5, P329; CAUS E, 1984, 1 C ESP GEOL MADR SP, P399; Collins M. 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Paleoclimatol. Paleoecol.	MAR 8	2006	232	1					1	35		10.1016/j.palaeo.2005.08.009	http://dx.doi.org/10.1016/j.palaeo.2005.08.009			35	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	026KD					2025-03-11	WOS:000236336900001
J	Roncaglia, L; Kuijpers, A				Roncaglia, L; Kuijpers, A			Revision of the palynofacies model of Tyson (1993) based on recent high-latitude sediments from the North Atlantic	FACIES			English	Article						palynology; depositional facies; North Atlantic; quaternary; holocene	WALLED DINOFLAGELLATE CYSTS; LATE QUATERNARY; SURFACE SEDIMENTS; AGE CALIBRATION; ORGANIC FACIES; ICELAND BASIN; NORDIC SEAS; C-14 DATA; GREENLAND; PRODUCTIVITY	This study presents data on the distribution of the palynofacies assemblages during the last 1500 years in sediments from Greenland and Faroe Islands fjords and North Atlantic deep-water sites. The sediments studied consist of olive grey to brown muddy silt occasionally mottled and faintly laminated. The chronology is based on Pb-210 and Cs-137 measurements and Accelerator Mass Spectrometry C-14 dating of shells and plant remains. As a result, the distribution of particulate organic matter at the high latitudes is controlled by the distance from the shore and water depth. Changes in water depth do not affect the assemblages near the shore. In order to provide a tool using palynofacies analysis for assessing high-latitude depositional settings, we propose to revise the palynological model of Tyson (1993). The revised model is a ternary plot of the relative amount of (1) amorphous organic material, (2) phytoclasts +sporomorphs, and (3) foraminifera + dinoflagellates +acritarchs +other marine algae in the sediment. Based on the integration of quantitative palynofacies analysis and environmental data, the revised model has the potential for discriminating spatial and redox status differences and providing information about terrestrial/fresh water influx at the high latitudes.	Danish Oil & Nat Gas AS, DK-2970 Horsholm, Denmark; Geol Survey Denmark & Greenland, Dept Quaternary Geol, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Danish Oil & Nat Gas AS, Agern Alle 24-26, DK-2970 Horsholm, Denmark.	luro@dong.dk						Andersen MS, 2000, GLOBAL PLANET CHANGE, V24, P239, DOI 10.1016/S0921-8181(00)00011-4; ANDERSEN OGN, 1981, ANN CYCEL TEMPERATUR, V5; [Anonymous], 1996, Am. Assoc. Strat. Palynol; [Anonymous], GEOLOGICAL SOC SPECI; [Anonymous], 2007, Paleopalynology; [Anonymous], FISKIRANNSOKNIR; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1982, J. Micropal., V1, P107; Bennike Ole, 1998, Frodskaparrit, V46, P267; BERTHELSEN C, 1990, KALALLIT NUNAAT GREE; Bianchi GG, 2000, MAR GEOL, V165, P137, DOI 10.1016/S0025-3227(99)00139-5; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; Buch E., 2000, Scientific report, V12, P1; Cuomo, 1996, PALYNOLOGY PRINCIPLE, V3, P1085; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; ENELL M, 1996, ENVIRON POLLUT, V93, P105; FARR KM, 1989, BRIT MICROPALAEONTOL, P265; Fogelqvist E, 2003, DEEP-SEA RES PT I, V50, P73, DOI 10.1016/S0967-0637(02)00131-0; Gilbert R, 1998, MAR GEOL, V147, P63, DOI 10.1016/S0025-3227(98)00008-5; HABIB D, 1982, MICROPALEONTOLGY, V28, P353; Hansen B, 2000, PROG OCEANOGR, V45, P109, DOI 10.1016/S0079-6611(99)00052-X; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HERMAN Y, 1972, ACTA U OULUENSIS A, V1, P357; HORSTED SA, 1956, MEDDEL DANMARKS FISK, V1, P61; Jones SE, 1998, CONT SHELF RES, V18, P1283, DOI 10.1016/S0278-4343(98)00044-2; JUUL M, 1992, THESIS U AARHUS DENM; Kuijpers A, 2001, GEO-MAR LETT, V20, P149; Kuijpers A., 2001, GEOL GREENLAND SURV, V189, P41; LARSEN B, 1991, MAR MAL FAER 19 25 J, V3, P1; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; Mustafa AA, 2002, J PETROL GEOL, V25, P351, DOI 10.1111/j.1747-5457.2002.tb00013.x; Nielsen N., 2001, DANISH J GEOGRAPHY, V101, P155; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Rasmussen TL, 2002, MAR GEOL, V188, P165, DOI 10.1016/S0025-3227(02)00280-3; Roncaglia L, 2004, MAR MICROPALEONTOL, V50, P21, DOI 10.1016/S0377-8398(03)00065-3; Schrank E, 1984, BERL GEO ABH, V50, P189; STUIVER M, 1977, RADIOCARBON, V19, P355, DOI 10.1017/S0033822200003672; STUIVER M, 1993, RADIOCARBON, V35, P215, DOI 10.1017/S0033822200013904; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Taylor J, 2000, MAR GEOL, V168, P1, DOI 10.1016/S0025-3227(00)00055-4; Traverse A., 1994, Sedimentation of Organic Particles; Tribovillard N, 2001, MAR PETROL GEOL, V18, P371, DOI 10.1016/S0264-8172(01)00006-X; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; Tyson RV, 2000, GEOLOGY, V28, P569, DOI 10.1130/0091-7613(2000)28<569:PPODFS>2.0.CO;2; VANAKEN HM, 1995, DEEP-SEA RES PT I, V42, P165, DOI 10.1016/0967-0637(94)00042-Q; VANAKEN HM, 1996, PROGR OCEANOGR, V38, P29; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817; WILLIAMS KM, 1995, ARCTIC ALPINE RES, V27, P352, DOI 10.2307/1552028; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; WRITE WR, 1970, SERIAL ATLAS MARINE, V19; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	56	31	33	1	3	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	0172-9179	1612-4820		FACIES	Facies	MAR	2006	52	1					19	39		10.1007/s10347-005-0028-y	http://dx.doi.org/10.1007/s10347-005-0028-y			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	021BC					2025-03-11	WOS:000235956400002
J	Courtinat, B				Courtinat, B			Palynostratigraphy of the Callovian-Oxfordian (Jurassic) of the Terres noires, southeast France	GEOBIOS			French	Article						dinoflagellate cysts; Jurassic; Callovian; Oxfordian; biostratigraphy; systematics		The Terre noires are monotonous sedimentary deposits comprising thick, dark marls and thin carbonaceous layers. They constitute a lithostratigraphical group known in the major part of the SE French Basin. In the East of this basin this group, dated from late Bajocian to mid Oxfordian, is well developed; on the other hand on the West, it is reduced until it disappears locally on the border of the Massif Central. In the East, the succession is precisely dated by ammonites, whereas in the west, ammonites are not consistently present, and do not permit the same precision. Analysis of dinoflagellate cyst assemblages, at the Callovian-Oxfordian boundary, show that it is possible to correlate the eastern to the western succession. Two marker species allow the correlation of four outcrop sections. The first index, Wanaea fimbriata, is well known-, its first appearance datum is exactly at the Callovian-Oxfordian limit in the Boreal and Mediterranean realms. It is the index taxon of the palynological parazone Wfi. The second index, Stephanelytron ceto, an endemic taxon in the SE French, has its last appearance datum within the Scarburghense horizon, the second subzone of the oldest zone of the Oxfordian (Mariae zone). The first section studied was sampled in the east part of the basin (Hautes Alpes department). It corresponds to the maxima of marine deposits and is used as the palynostratigraphical reference. The three other sections analyzed, sampled in the west part of the basin (Ardeche department) where marine deposits are more condensed, are correlated and dated due to dinoflagellate cyst markers observed in the reference section. These results indicate that dinoflagellate cysts are a reliable correlation tool. Batiacasphaera rugosa (Courtinat, 1980) nov. comb is proposed. (c) 2006 Elsevier SAS. Tous droits reserves.	Univ Lyon 1, Unite Format & Rech Sci Terre, F-69622 Villeurbanne, France	Universite Claude Bernard Lyon 1	Courtinat, B (通讯作者)，Univ Lyon 1, Unite Format & Rech Sci Terre, Batiment Geode,2,Rue Raphael Dubois, F-69622 Villeurbanne, France.	bernard.courtinat@univ-lyon1.fr						ARKELL WJ, 1946, GEOL SOC AM BULL, V57, P1, DOI 10.1130/0016-7606(1946)57[1:SOTEJ]2.0.CO;2; ARTRU P, 1972, THESIS U CLAUDE BERN; ARTU P, 1966, B SOC GEOLOGIQUE FRA, V8, P413; Bourseau J-P., 1977, NOUV ARCH MUS HIST N, V15, P1; BRENNER W., 1988, Tubinger Mikropalaontologische Mitteilungen, V6, P1; COLLIGNO.M, 1970, CR ACAD SCI D NAT, V270, P261; Courtinat B, 2003, B SOC GEOL FR, V174, P595, DOI 10.2113/174.6.595; Courtinat B, 1999, J MICROPALAEONTOL, V18, P169, DOI 10.1144/jm.18.2.169; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; COURTINAT B, 1980, DOCUMENTS LABORATOIR, V78, P1; DAVIES E. H., 1983, GEOL SURV CAN B, V359, P1; Debrand-Passard S., 1984, MEMOIRES BUREAU RECH, V125, P1; DEFLANDRE G, 1938, CR HEBD ACAD SCI, V206, P687; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Fauconnier D, 1996, MAR PETROL GEOL, V13, P707, DOI 10.1016/0264-8172(95)00024-0; FORTWENGLER D, 1994, 3 INT S JUR STRAT PO, V17, P203; *GROUP FRANC ET JU, 1971, COMPTE RENDU SOMMAIR, V2, P1; *GROUP FRANC ET JU, 2000, LIVRET GUIDE EXCURSI, P1; Groupe Francais d'Etude du Jurassique, 1997, BULL CENT RECH ELF E, V17, P1; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Haug E., 1891, B SERVICE CARTE GEOL, V3, P1; HERNGREEN GRW, 2000, TNO, V63, P1; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; LHAMYANI B, 1985, THESIS U CLAUDE BERN; MARCHAND D., 1979, COMPTES RENDUS SOMMA, V3, P122; Mennessier G., 1959, MEMOIRES SOC GEOLOGI, VXXXVIII, P1; ODIN GS, 1990, GEOCHRONIQUE, V35, P12; POULSEN N.E., 1996, American Association of Stratigraphic Palynologists, Contribution Series, V31, P1; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Riding J.B., 1992, P7; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; RIDING J B, 1984, Palynology, V8, P195; RILEY L A, 1982, Palynology, V6, P193; Smelror M., 1989, Palynology, V13, P121; Williams Graham L., 1998, AASP Contributions Series, V34, P1	35	3	5	0	2	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS	23 RUE LINOIS, 75724 PARIS, FRANCE	0016-6995			GEOBIOS-LYON	Geobios	MAR-APR	2006	39	2					201	213		10.1016/j.geobios.2004.11.001	http://dx.doi.org/10.1016/j.geobios.2004.11.001			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	032IW					2025-03-11	WOS:000236769100003
J	Villanoy, CL; Azanza, RV; Alternerano, A; Casil, AL				Villanoy, CL; Azanza, RV; Alternerano, A; Casil, AL			Attempts to model the bloom dynamics of Pyrodinium, a tropical toxic dinoflagellate	HARMFUL ALGAE			English	Article						Pyrodinium blooms; toxic algal blooms; harmful algal blooms; phytoplankton bloom model	MANILA BAY; RED TIDE; PHYTOPLANKTON; PHILIPPINES; VIGO; RIA	For the first time, several models have been used to aid in the understanding of the bloom dynamics of Pyrodinium bahamense var. compressum, the major causal organism of toxic algal blooms in Manila Bay and several areas in the tropical world. The complex life cycle of Pyrodinium includes the formation of cysts that settle at the sediments, which can serve as the inoculum for the next bloom. The seasonal variation of temperature and salinity reflects the combined effects of convection and water column stability, which can control vertical movement of plankton and other parameters essential to its growth. The significance of wind forcing appears to be related to the potential to resuspend cysts. In the absence of wind, tidal currents in the inner part of the bay may be too weak to induce resuspension. The addition of wind results in a significant increase in bottom current velocity. Off Cavite at the southeast, bottom velocity is enhanced by orbital motion due to waves, one of the reasons why sediments off this area are dominated by sandy material. The strong vertical mixing of the water column at depths of less than 10 m may influence nutrient and consequently, plankton populations. The wave field during the southwest monsoon indicates that its contribution to the bottom velocity dominates in this area of the bay. Bloom simulations using combined bio-physical parameters show that direction of advection is almost always along wind direction. The dispersal distances increases if the Pyrodinium cells are found higher in the water column. For cells originating from southeastern (Cavite) sources, the direction of transport is slightly towards the north. In either case, the formation of cysts after a bloom is adjacent to the northern area (Pampanga) for blooms originating from the western side (Bataan) and along the eastern side (Paranaque-Manila) for blooms originating from the southeastern side (Cavite). Comparison with a few records of bloom occurrences in Manila Bay shows some consistent features. Reports of these blooms also showed that they occurred almost always during spring tides. There appears to be two main systems for bloom formation: one fed by cyst beds in the west (Bataan) which is advected along the west-northwest coast (Bataan-Bulacan) while the other one is fed by the southeast (Cavite) cyst beds that dominates in the east-southeast (Paranaque-Cavite) area. (c) 2005 Elsevier B.V. All rights reserved.	Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines	University of the Philippines System; University of the Philippines Diliman	Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines.	cesarv@upmsi.ph	Azanza, Rhodora/HGU-5811-2022					[Anonymous], 1996, HARMFUL TOXIC ALGAL; Azanza R., 1997, SCI DILIMAN, V9, P1; Azanza RV, 2004, PHYCOL RES, V52, P376; Azanza RV, 2001, J SHELLFISH RES, V20, P1251; BAJARIAS FFA, 1995, INT SEM MAR FISH ENV, P139; Blumberg A.F., 1987, Three Dimensional Ocean Models, P1; FIGUEIRAS FG, 1991, J PLANKTON RES, V13, P589, DOI 10.1093/plankt/13.3.589; FRAGA S, 1988, ESTUAR COAST SHELF S, V27, P349, DOI 10.1016/0272-7714(88)90093-5; Franks P.J.S, 1997, OCEAN RES, V19, P153; Franks PJS, 1997, LIMNOL OCEANOGR, V42, P1273, DOI 10.4319/lo.1997.42.5_part_2.1273; Franks PJS, 2002, J OCEANOGR, V58, P379, DOI 10.1023/A:1015874028196; HOLTHUIJSEN L.H., 1993, Proceedings of the 2nd International Symposium of Ocean Wave Measurement and Analysis (New Orleans), P630; IWATA Y, 1989, RED TIDES BIOL ENV S, P45; JOHNSON BH, 1999, ESTIMATING DREDGING; Kishi M.J., 1989, P177; Lucas LV, 1998, J MAR RES, V56, P375, DOI 10.1357/002224098321822357; RIS RC, 1997, 8 INT BIENN C PHYS E, P139; STEIDINGER KS, 1983, PROGR PHYCOLOGICAL R, P147; Uchiyama M., 1989, P173; VIERA ME, 1993, ESTUARINE COASTAL SH, V36, P15; Villanoy C. L, 1996, HARMFUL TOXIC ALGAL, P189; WYATT T, 1973, NATURE, V244, P238, DOI 10.1038/244238a0; WYATT T, 1975, ENVIRON LETT, V9, P214; Yamamoto T, 2002, HARMFUL ALGAE, V1, P301, DOI 10.1016/S1568-9883(02)00029-X; Yanagi T., 1989, P149; YANAGI T, 1995, J MARINE SYST, V6, P269, DOI 10.1016/0924-7963(94)00027-9	26	36	42	0	20	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAR	2006	5	2					156	183		10.1016/j.hal.2005.07.001	http://dx.doi.org/10.1016/j.hal.2005.07.001			28	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	014TH					2025-03-11	WOS:000235502500006
J	Meijer, T; Cleveringa, P; Munsterman, DK; Verreussel, RMCH				Meijer, T; Cleveringa, P; Munsterman, DK; Verreussel, RMCH			The Early Pleistocene Praetiglian and Ludhamian pollen stages in the North Sea Basin and their relationship to the marine isotope record	JOURNAL OF QUATERNARY SCIENCE			English	Article						Early Pleistocene; Praetiglian; Ludhamian; land-sea correlation; Impagidinium multiplexum; Megayoldia thraciaeformis	QUATERNARY	In this paper, the Currently accepted correlation of the Early Pleistocene Ludhamian stage of England with the Tiglian-A sub-stage of the Netherlands is challenged. Recent investigations of Early Pleistocene marine North Sea deposits from a borehole near Noordwijk (the Netherlands) yielded evidence from molluscs, dinoflagellate cysts and sporomorphs for an alternation of warm-temperate and arctic intervals within the Praetiglian and Tiglian stages. Marine equivalents of the terrestrial-based pollen sub-stages Tiglian A and B have been recognised in the upper part of the sequence. A Praetiglian age can be assigned to the lower part of the sequence on the basis of mollusc Journal of Quaternary Science analysis. Within the Praetiglian, an alternation of warm and cold phases has been recognised from both the dinoflagellate cyst and molluscan records. Three cold phases within the Praetiglian are tentatively correlated with marine isotope stages (MIS) 96-100. The Molluscan assemblages provide evidence for climate forcing of the sea level: highest sea levels are reached in the warm-temperate intervals. Within the Praetiglian, an interval with an acme zone of the dinoflagellate cyst Impagidinium multiplexum, is correlated with the Ludhamian and tentatively linked to MIS 97 and/or MIS 96. The cold molluscan assemblages from the Noordwijk borehole include an acme zone of Megayoldia thraciaeformis, the first and Only Occurrence of this North Pacific bivalve in the North Sea Basin. Copyright (c) 2006 John Wiley & Sons, Ltd.	Naturalis, Dept Cainozoic Mollusca, NL-2300 RA Leiden, Netherlands; TNO, NITG, Natl Geol Survey Netherlands, Utrecht, Netherlands	Naturalis Biodiversity Center; Netherlands Organization Applied Science Research	Meijer, T (通讯作者)，Naturalis, Dept Cainozoic Mollusca, POB 9517, NL-2300 RA Leiden, Netherlands.	meijert@naturalis.nl						DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FUNNELL BM, 1998, DAWN QUATERNARY, V60, P227; Funnell Brian M., 1995, Geological Society Special Publication, V96, P3, DOI 10.1144/GSL.SP.1995.096.01.02; Gibbard PL, 2005, BOREAS, V34, P1, DOI 10.1080/03009480510012854; GIBBARD PL, 1991, QUATERNARY SCI REV, V10, P23, DOI 10.1016/0277-3791(91)90029-T; HARMER F W., 1896, Quarterly Journal of the Geological Society, V52, P748, DOI DOI 10.1144/GSL.JGS.1896.052.01-04.45; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; JANSE AC, 2003, CAINOZOIC RES, V2, P139; Meijer T., 1986, 9 INT MAL C ED, P53; Pillans B, 2004, QUATERNARY SCI REV, V23, P2271, DOI 10.1016/j.quascirev.2004.07.006; Pillans B, 2004, EPISODES, V27, P127, DOI 10.18814/epiiugs/2004/v27i2/008; Spaink G., 1975, TOELICHTING BIJ GEOL, P118; van Leeuwen RJW, 2000, GEOL MIJNBOUW-N J G, V79, P161; VANDERVLERK IM, 1953, VERHANDELINGEN KONIN, V20, P1; Westerhoff W. E., 1998, MEDEDELINGEN NEDERLA, V60, P35; Zagwijn W.H., 1975, GEOLOGICAL J, V6, P137; ZAGWIJN WH, 1992, QUATERNARY SCI REV, V11, P583, DOI 10.1016/0277-3791(92)90015-Z; ZAGWIJN WH, 1960, MEDEDELINGEN GEOLOGI; Zagwijn WH., 1957, Geol. Mijnbouw, V19, P233; Zagwijn WH., 1963, MEDED GEOL STICHTING, V16, P49	22	13	15	0	4	JOHN WILEY & SONS LTD	CHICHESTER	THE ATRIUM, SOUTHERN GATE, CHICHESTER PO19 8SQ, W SUSSEX, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	MAR	2006	21	3					307	310		10.1002/jqs.956	http://dx.doi.org/10.1002/jqs.956			4	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	027HI					2025-03-11	WOS:000236405400007
J	Anderson, DM; Rengefors, K				Anderson, DM; Rengefors, K			Community assembly and seasonal succession of marine dinoflagellates in a temperate estuary: The importance of life cycle events	LIMNOLOGY AND OCEANOGRAPHY			English	Article							NORTHERN BALTIC SEA; GONYAULAX-TAMARENSIS; GYRODINIUM-UNCATENUM; SCRIPPSIELLA-HANGOEI; CYST FORMATION; RESTING CYSTS; DINOPHYCEAE; GERMINATION; BLOOMS; ALEXANDRIUM	Dinoflagellate successional strategies and community structure were investigated in Perch Pond, a temperate estuary on the North American east coast by field surveys as well as laboratory investigations on growth rates, cyst maturation period, and cyst germination temperature thresholds. The dominant species were those predicted by the Smayda and Reynolds Rules of Assembly life form model. Three successional strategies were characterized: (1) holoplanktonic, (2) meroplanktonic (i.e., germinated from cysts), and (3) introduced by advection. The seasonal succession of the meroplanktonic dinoflagellates that were studied reflects the differential lengths of their mandatory dormancy periods as well as differences in their temperature thresholds or "windows" for germination. The holoplanktonic species present at low densities year-round in Perch Pond had a wide temperature tolerance for growth and thus did not need a cyst stage to survive seasonal extremes. Another non-cyst-forming species relied solely on advection to inoculate the salt pond; thus, blooms in successive years would be expected to be more stochastic in nature than for the other two strategies. The timing of cyst formation and population decline for meroplanktonic species corresponded on several occasions to an increase in grazers, suggesting that grazing might have contributed to bloom decline from cyst formation. This timing also suggests the possibility of encystment as a predator avoidance strategy. We suggest that seasonal succession of cyst-forming dinoflagellates is not stochastic. Instead, the appearance of these species in the plankton is predictable on the basis of measurable physiological responses to both endogenous and exogenous factors that they experience during dormancy and quiescence.	Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; Lund Univ, Dept Ecol, S-22241 Lund, Sweden	Woods Hole Oceanographic Institution; Lund University	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.		Rengefors, Karin/K-5873-2019	Rengefors, Karin/0000-0001-6297-9734				Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; ANDERSON DM, 1987, BIOL BULL, V172, P89, DOI 10.2307/1541609; [Anonymous], PHYSL ECOLOGY HARMFU; BINDER BJ, 1987, J PHYCOL, V23, P99; Boero F, 1996, MAR ECOL-P S Z N I, V17, P237, DOI 10.1111/j.1439-0485.1996.tb00505.x; BRAARUD T, 1951, MAT NATURV KLASSE, V2, P1; BRAND L E, 1981, Journal of Plankton Research, V3, P193, DOI 10.1093/plankt/3.2.193; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Dale B., 1983, P69; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; GARCON VC, 1986, ESTUARIES, V9, P179, DOI 10.2307/1352129; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HANSSON LA, 1995, J PHYCOL, V31, P540, DOI 10.1111/j.1529-8817.1995.tb02547.x; Huber G., 1922, Z BOTANIK, V14, P337; Huisman J, 2001, AM NAT, V157, P488, DOI 10.1086/319929; Jacobson D.M., 1987, The ecology and feeding biology of thecate heterotrophic dinoflagellates, DOI DOI 10.1575/1912/3937; Kokinos John P., 1995, Palynology, V19, P143; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Matsuoka K., 2003, Monographs on Oceanographic Methodology, V11, P563; MATSUOKA K, 1988, Japanese Journal of Phycology, V36, P311; MCQUOID MR, 1995, J PHYCOL, V31, P44, DOI 10.1111/j.0022-3646.1995.00044.x; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Reynolds C.S., 1988, P388; Smayda T.J., 1980, PHYSIOLOGICAL ECOLOG, P493; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Smayda TJ, 2001, J PLANKTON RES, V23, P447, DOI 10.1093/plankt/23.5.447; SOMMER U, 1986, ARCH HYDROBIOL, V106, P433; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; TURNER J T, 1983, Marine Ecology, V4, P359, DOI 10.1111/j.1439-0485.1983.tb00119.x; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wall D., 1971, Geoscience Man, V3, P1; WALL D., 1967, PALAEONTOLOGY, V10, P95; WATANABE MM, 1982, 30 NAT JAP I ENV STU; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; YAMOCHI S, 1986, Journal of the Oceanographical Society of Japan, V42, P266, DOI 10.1007/BF02114525	51	64	70	1	30	AMER SOC LIMNOLOGY OCEANOGRAPHY	WACO	5400 BOSQUE BLVD, STE 680, WACO, TX 76710-4446 USA	0024-3590			LIMNOL OCEANOGR	Limnol. Oceanogr.	MAR	2006	51	2					860	873		10.4319/lo.2006.51.2.0860	http://dx.doi.org/10.4319/lo.2006.51.2.0860			14	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	026MS		Bronze			2025-03-11	WOS:000236343600007
J	Doblin, MA; Dobbs, FC				Doblin, MA; Dobbs, FC			Setting a size-exclusion limit to remove toxic dinoflagellate cysts from ships' ballast water	MARINE POLLUTION BULLETIN			English	Article						ballast-water treatment; biological invasions; shipping; toxic dinoflagellate cysts	TANK SEDIMENTS; MICROORGANISMS; DINOPHYCEAE; TRANSPORT; INVASION	Dinoflagellate cysts are well-recognized biological constituents of ships' ballast tanks. They are present in ballast water, sediments and residual water in drained tanks, and in biofilms formed on interior tank Surfaces. Therefore, cysts have the potential to be released during ballast discharge. The International Maritime Organization's (IMO) Ballast Water Management Convention (promulgated February 2004) stipulates a performance standard (Annex, Regulation D2) requiring discharged ballast water contain < 10 viable organisms between 10 and 50 mu m per ml and < 10 viable organisms >= 50 mu m per m(3). The proposed size limit has potential to exclude both the smallest toxic and the largest toxic and non-toxic dinoflagellate (and other microalgal) cysts from discharged ballast water. Despite the appropriateness of size cutoffs however, ballast water containing predominantly small cysts (< 50 mu m) could be deemed in compliance with the performance standard, even without treatment, while ballast water having the same concentration of larger cysts (> 50 mu m) could require a multiple-log reduction in abundance before its permissible discharge. Also of concern, it remains uncertain whether ballast-water treatment can remove sufficient organisms, including dinoflagellate cysts. to meet the performance standard. (c) 2006 Elsevier Ltd. All rights reserved.	Univ Technol Sydney, Dept Environm Sci, Inst Water & Environm Resource Management, Sydney, NSW 2007, Australia; Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	University of Technology Sydney; Old Dominion University	Univ Technol Sydney, Dept Environm Sci, Inst Water & Environm Resource Management, POB 123 Broadway, Sydney, NSW 2007, Australia.	martina.doblin@uts.edu.au	Doblin, Martina/E-8719-2013	Doblin, Martina/0000-0001-8750-3433				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 2000, WHOI200011 US WOODS; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; Bolch C.J., 1993, Journal of Marine Environmental Engineering: 1993, P23; Bolch CJS, 1997, PHYCOLOGIA, V36, P6, DOI 10.2216/i0031-8884-36-1-6.1; Cangelosi A, 2002, INVASIVE AQUATIC SPECIES OF EUROPE: DISTRIBUTION, IMPACTS AND MANAGEMENT, P511; Coats DW, 2002, J PHYCOL, V38, P417, DOI 10.1046/j.1529-8817.2002.03832.x; Dale B., 1983, P69; Dobbs FC, 2005, ENVIRON SCI TECHNOL, V39, p259A, DOI 10.1021/es053300v; Drake LA, 2005, BIOL INVASIONS, V7, P969, DOI 10.1007/s10530-004-3001-8; Drake Lisa A., 2001, Biological Invasions, V3, P193, DOI 10.1023/A:1014561102724; Galil BS, 1997, EUR J PROTISTOL, V33, P244, DOI 10.1016/S0932-4739(97)80002-8; Gosselin Serge, 1995, P591; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hallegraeff Gustaaf M., 1997, Aquatic Ecology, V31, P47, DOI 10.1023/A:1009972931195; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Johengen T, 2005, ASSESSMENT TRANSOCEA; JONSSON S, 2005, THESIS U KALMAR SWED; MACDONALD EM, 1998, HARMFUL ALGAE, P220; McCollin T.A., 2000, Marine bioinvasions: Proceedings of the First National Conference, P282; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; MOEMCKE D, 1999, ECOPORTS MONOGRAPHS, V18; Montani S., 1995, J. Mar. Biotechnol, V2, P179; Murphy K, 2004, MAR POLLUT BULL, V48, P711, DOI 10.1016/j.marpolbul.2003.10.015; Oemcke D., 2003, Journal of Marine Environmental Engineering, V7, P47; Oemcke DJ, 2005, WATER RES, V39, P5119, DOI 10.1016/j.watres.2005.09.024; Parsons MG, 2000, MAR TECHNOL SNAME N, V37, P129; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; Verling E, 2005, P ROY SOC B-BIOL SCI, V272, P1249, DOI 10.1098/rspb.2005.3090	32	20	21	2	17	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	MAR	2006	52	3					259	263		10.1016/j.marpolbul.2005.12.014	http://dx.doi.org/10.1016/j.marpolbul.2005.12.014			5	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	027UT	16480748				2025-03-11	WOS:000236441800014
J	Kuhmann, G; Langereis, CG; Munsterman, D; van Leeuwen, RJ; Verreussel, R; Meutenkamp, JE; Wong, TE				Kuhmann, G; Langereis, CG; Munsterman, D; van Leeuwen, RJ; Verreussel, R; Meutenkamp, JE; Wong, TE			Integrated chronostratigraphy of the Ptiocene-Pleistocene interval and its relation to the regional stratigraphical stages in the southern North Sea region	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						North Sea; dinoflagellate cysts; foraminifers; pollen; Pliocene; Pleistocene; regional stratigraphy; chronostratigraphy	EASTERN ENGLAND; PLIOCENE; NETHERLANDS; BASIN; AGE; ASSEMBLAGES; QUATERNARY; TIMESCALE; BOREHOLE; ATLANTIC	Time-stratigraphic interpretations of Late Pliocene to Early Pleistocene sediments from onshore locations and from marginal marine settings of the North Sea Basin often refer to the subdivision of the Dutch and British 'Quaternary' regional stratigraphic stages. Since age control for these stages and their stage boundaries are based on relative dating methods, in this study pollen, dinoflagellate cysts and foraminiferal assemblages were investigated to correlate the regional stratigraphic stages independently to the global chronostratigraphy and the paleomagnetic timescale. The data were obtained from eight boreholes located in the depocentre setting of the Late Pliocene North Sea Basin comprising a 1000 m thick sedimentary succession. The British Gedgravian and Waltonian stages, the Dutch Reuverian to Brunssumian as well as published foraminiferal zones (NSB 14, FB and the lower part of the FA2 zone) fall within the Zanclean and Piacenzian. The lower boundaries of the Pre-Ludhamian and Pretiglian stages and of the NSB 14 to 15 zones are close to the paleomagnetic Gauss-Matuyama boundary. The Pre-Ludhamian, Ludhamian, Thurnian and the Pretiglian, Tiglian A and Tiglian B stages presumably cover the marine isotope stages 103 to 95. It is proposed that the Ludhamian, Thurnian and the Tiglian A were short lasting, warm, periods during which sea level highstand facilitated sedimentary deposition at the marginal areas of the North Sea Basin. The lower boundary of the paleomagnetic Olduvai subchron is situated in the Tiglian C1-4b stage while the TC4c stage is found within the Olduvai subchron. Foraminiferal NSB 15 and NSB 16 zone as well as the upper part of the FA2 and FA1 zone fall within the Gelasian and cover the Matuyama chron as well as the lower part of the Olduvai subchron. Comparison with formerly dated North Sea sediments shows a good agreement between foraminiferal zonations on a broader scale but significant differences in absolute ages occur. Strontium isotope values indicate approximately I Ma younger ages as expected from our chronostratigraphic model. This discrepancy is explained by the dominance of freshwater from river discharge contributing high amounts of eroded material to the basin, leading to an increase of the Sr-87/Sr-86 ratio in the shelf-sea water.	Univ Utrecht, Fac Earth Sci, NL-3584 CD Utrecht, Netherlands; Natl Geol Survey Netherlands, TNO Built Environm & Geosci, NL-3584 CB Utrecht, Netherlands	Utrecht University; Netherlands Organization Applied Science Research	Univ Utrecht, Fac Earth Sci, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	langer@geo.uu.nl						AGUIRRE E, 1985, EPISODES, V8, P116, DOI 10.18814/epiiugs/1985/v8i2/009; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BECK RB, 1972, GEOL MAG, V109, P137, DOI 10.1017/S0016756800039522; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; BIJLSMA S, 1981, GEOL MIJNBOUW, V60, P337; BOENIGK W, 1979, N JB GEOL PALAONT MH, V9, P513; CAMERON TDJ, 1984, GEOL MAG, V121, P85, DOI 10.1017/S0016756800028053; CANDE SC, 1995, J GEOPHYS RES-SOL EA, V100, P6093, DOI 10.1029/94JB03098; DEJONG J, 1988, PHILOS T ROY SOC B, V318, P603, DOI 10.1098/rstb.1988.0025; Doppert J.W.C., 1980, MEDEDELINGEN RIJKS G, V32, P255; Eidvin T, 1999, NORSK GEOL TIDSSKR, V79, P97, DOI 10.1080/002919699433843; FARRELL JW, 1995, GEOLOGY, V23, P403, DOI 10.1130/0091-7613(1995)023<0403:ICRCOL>2.3.CO;2; FUNNEL B, 1996, ISLAND BRITAIN QUATE, V96, P3; GIBBARD PL, 1991, QUATERNARY SCI REV, V10, P23, DOI 10.1016/0277-3791(91)90029-T; Glennie K.W., 1990, INTRO PETROLEUM GEOL, V3rd; Gradstein F, 1996, NORSK GEOL TIDSSKR, V76, P3; Gradstein F., 2004, A Geological Time Scale; HALLAM DF, 1994, EARTH PLANET SC LETT, V121, P71, DOI 10.1016/0012-821X(94)90032-9; HARLAND R, 1991, GEOL MAG, V128, P647, DOI 10.1017/S0016756800019749; Harland R., 1992, P253; HARLAND R, 1979, 48 US GOV PRINT OFF, P531; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 1998, GEOL MAG, V135, P803, DOI 10.1017/S0016756898001745; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; Huuse M, 2002, B GEOL SOC DENMARK, V49, P145; Kasse C, 1996, GEOL MIJNBOUW, V75, P19; King C., 1989, P418; KING C, 1983, REPORT I GEOLOGICAL, V82, P1; Konradi PB, 1996, GEOL SOC SPEC PUBL, V117, P15, DOI 10.1144/GSL.SP.1996.117.01.02; Kuhlmann G., 2004, THESIS UTRECHT U; LAURSEN GV, 1995, THESIS U AARHUS; Lourens LJ, 1996, PALEOCEANOGRAPHY, V11, P391, DOI 10.1029/96PA01125; MATTIESSEN J, 1996, P OC DRILL PROG SCI, P243; Mauz B, 1998, QUATERNARY SCI REV, V17, P357, DOI 10.1016/S0277-3791(97)00054-1; McArthur JM, 2001, J GEOL, V109, P155, DOI 10.1086/319243; MUDIE PJ, 1989, P OC DRILL PROGR COL; OAKLEY KP, 1949, P INT GEOL C 18 SESS, V86, P18; PALMER MR, 1989, EARTH PLANET SC LETT, V92, P11, DOI 10.1016/0012-821X(89)90017-4; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Smelror Morton, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P83; Sorensen JC, 1997, MAR PETROL GEOL, V14, P99, DOI 10.1016/S0264-8172(96)00052-9; URBAN B, 1978, Geologie en Mijnbouw, V57, P401; Van Adrichem Boogaert H.A., 1997, MEDEDELINGEN RIJKS G, V50, P1; Van den Berg MW, 2001, RIVER BASIN SEDIMENT SYSTEMS: ARCHIVES OF ENVIRONMENTAL CHANGE, P45; Van der Vlerk IM, 1950, NEDERLAND IJSTIJDVAK; VANMONTFRANS HM, 1971, EARTH PLANET SC LETT, V11, P226, DOI 10.1016/0012-821X(71)90168-3; VANVOORTHUYSEN JH, 1972, GEOL MIJNBOUW, V51, P627; Versteegh GJM, 1997, MAR MICROPALEONTOL, V30, P319, DOI 10.1016/S0377-8398(96)00052-7; VERSTEEGH GJM, 1995, THESIS U UTRECHT WAG; Vinken, 1988, 124 INT GEOL CORR PR; WEAVER PPE, 1987, INITIAL REP DEEP SEA, V94, P815; WEAVER PPE, 1986, MAR MICROPALEONTOL, V10, P295, DOI 10.1016/0377-8398(86)90033-2; WEST R. G., 1961, PROC ROY SOC SER B BIOL SCI, V155, P437; Westerhoff Wim E., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P35; Zagwijn W.H., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P19; Zagwijn W.H., 1974, Geologie en Mijnbouw, V53, P369; ZAGWIJN WH, 1992, QUATERNARY SCI REV, V11, P583, DOI 10.1016/0277-3791(92)90015-Z; ZAGWIJN WH, 1985, GEOL MIJNBOUW, V64, P17; ZAGWIJN WH, 1960, MEDEDELINGEN GEOLOGI, V5; Zagwijn WH., 1957, Geol. Mijnbouw, V19, P233; Zagwijn WH., 1963, MEDED GEOL STICHTING, V16, P49; ZAGWIJN WH, 1978, GEOL MIJNBOUW, V57, P577; ZALASIEWICZ JA, 1991, PHILOS T R SOC B, V333, P81, DOI 10.1098/rstb.1991.0061; ZIEGLER P, 1990, GEOLOGICAL ATLAS WE	67	0	0	0	4	CAMBRIDGE UNIV PRESS	CAMBRIDGE	EDINBURGH BLDG, SHAFTESBURY RD, CB2 8RU CAMBRIDGE, ENGLAND	0016-7746	1573-9708		NETH J GEOSCI	Neth. J. Geosci.	MAR	2006	85	1					19	35						17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	032XX					2025-03-11	WOS:000236811100002
J	Yamatogi, T; Sakaguchi, M; Iwataki, M; Matsuoka, K				Yamatogi, T; Sakaguchi, M; Iwataki, M; Matsuoka, K			Effects of temperature and salinity on the growth of four harmful red tide flagellates occurring in Isahaya Bay in Ariake Sound, Japan	NIPPON SUISAN GAKKAISHI			Japanese	Article							HETEROSIGMA-AKASHIWO; RAPHIDOPHYCEAE; CYSTS	Three harmful red tide causative raphidophytes Chattonella antiqua (Hada) Ono, Chattonella marina (Subrahmanyan) Hara et Chihara and Heterosigma akashiwo Hada, and a dinoflagellate Cochlodinium polykrikoides Margalef were isolated from Isahaya. Bay, Japan in 2003-2004. The growth characteristics of these four clonal cultures were examined in 60 different combinations of temperature (10-32.5 degrees C) and salinity (16-36) under a light intensity of 80 mu mol/m(2)/s. C. antiqua reproduced at 15-32.5 degrees C and 16-36 PSU, and the maximum growth rate was 0.99 day(-1) at 30 degrees C and 32 PSU. C. marina reproduced at 12.5-32.5 degrees C and 16-36 PSU. The maximum growth rate was 0.83 day(-1), which was obtained at 30 degrees C and 24 PSU. H. akashiwo reproduced at 10-32.5 degrees C and 16-36 PSU. The maximum growth rate was 1.14 day(-1) at 25 degrees C and 24 PSU. C. polykrikoides reproduced at 10-32.5 degrees C and 1636 PSU. The maximum growth rate was 0.56 day(-1) at 27.5 degrees C and 32 PSU. Four red tide flagellates examined in this study appeared to be euryhaline. The optimum temperatures for maximum growth were different in each species and these conditions clearly corresponded with recent red tide occurrences in Isahaya Bay. Compared with growth conditions previously reported, four isolates from Isahaya Bay are likely to tolerate relatively higher temperature.	Nagasaki Prefectural Inst Fisheries, Nagasaki 8512213, Japan; Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan	Nagasaki University	Yamatogi, T (通讯作者)，Nagasaki Prefectural Inst Fisheries, Nagasaki 8512213, Japan.	yamatogi@marinelabo.nagasaki.nagasaki.jp	Iwataki, Mitsunori/H-9640-2019	Iwataki, Mitsunori/0000-0002-5844-2800				Imai I, 1999, MAR BIOL, V133, P755, DOI 10.1007/s002270050517; IMAI I, 1993, NIPPON SUISAN GAKK, V59, P1669; Kim BG, 2004, MOL BIOTECHNOL, V26, P1, DOI 10.1385/MB:26:1:1; Kim D, 2004, J PLANKTON RES, V26, P967, DOI 10.1093/plankt/fbh085; NAKAMURA Y, 1983, Journal of the Oceanographical Society of Japan, V39, P110, DOI 10.1007/BF02070796; WATANABE M M, 1982, Japanese Journal of Phycology, V30, P279	6	33	34	1	13	JAPANESE SOC FISHERIES SCIENCE	TOKYO	C/O TOKYO UNIV FISHERIES, KONAN 4, MINATO, TOKYO, 108-8477, JAPAN	0021-5392			NIPPON SUISAN GAKK	Nippon Suisan Gakkaishi	MAR	2006	72	2					160	168		10.2331/suisan.72.160	http://dx.doi.org/10.2331/suisan.72.160			9	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	041DI		Bronze			2025-03-11	WOS:000237433100002
J	Suto, I				Suto, I			The explosive diversification of the diatom genus <i>Chaetoceros</i> across the Eocene/Oligocene and Oligocene/Miocene boundaries in the Norwegian Sea	MARINE MICROPALEONTOLOGY			English	Article						diatom resting spore events; Eocene/Oligocene; Oligocene/Miocene; Norwegian Sea; DSDP Site 338	MARINE PLANKTONIC DIATOM; RESTING SPORE FORMATION; STRATIGRAPHIC SIGNIFICANCE; SURFACE SEDIMENTS; SOUTHERN-OCEAN; MIOCENE; PHYTOPLANKTON; BACILLARIOPHYCEAE; PSEUDOCURVISETUS; CIRCULATION	Eocene to middle Miocene stratigraphic changes in species richness, abundance and valve size of Chaetoceros resting spores in the Norwegian Sea (DSDP Site 338) were investigated in order to understand past productivity and paleoenvironmental changes in upwelling regions. As a result, drastic resting spore events were recognized in a similar to 6 myr interval across the Eocene/Oligocene boundary (EO Event), the Oligocene/Miocene boundary (OM Event) and in the early middle Miocene (emM Event). The EO Event was characterized by explosive diversification at both the morpho-generic and specific levels, an increase in abundance, and a decrease in valve size from the upper Eocene through the lowest Oligocene. The OM Event was defined by a two-fold increase in species richness. During the emM Event spore abundance decreased rapidly, and species richness and valve size decreased gradually. These changes may indicate changes in the nutrient supply, especially in upwelling regions. The increased species richness suggests a change from a stable water column with a constant nutrient supply in the Eocene to an unstable one with a sporadic nutrient supply by increased vertical mixing in the Oligocene, based on evaluation of the ecologic differences between dinoflagellate cysts and Chaetoceros resting spores. The role of main primary producer might have switched from dinoflagellates and/or nannoplankton in the Eocene to diatoms, especially Choetoceros, in the Oligocene in the Norwegian Sea. Increased resting spore species richness during the OM Event may show that environmental changes such as global cooling and nutrient mixing led to a diversification of the spore producing genus Chaetoceros. The emM Event might have been affected by changes in paleoceanographic conditions, perhaps a decrease in nutrient supply. This study presents the first paleoceanographic analysis using not only the total resting spore abundance but also the abundances of individual species, and establishes the value of spore taxonomy and diatom analysis including spores. (c) 2005 Elsevier B.V. All rights reserved.	Natl Sci Museum, Dept Geol, Shinjuku Ku, Tokyo 1690073, Japan	National Museum of Nature and Science	Suto, I (通讯作者)，Natl Sci Museum, Dept Geol, Shinjuku Ku, Hyakunin Cho 3-23-1, Tokyo 1690073, Japan.	sutoitsu@kahaku.go.jp						ABRANTES F, 1988, MAR GEOL, V85, P15, DOI 10.1016/0025-3227(88)90082-5; ABRANTES F, 1991, MAR MICROPALEONTOL, V17, P285, DOI 10.1016/0377-8398(91)90017-Z; AKIBA F, 1986, INITIAL REP DEEP SEA, V87, P393; [Anonymous], 1863, Verhandlungen der kaiserlich-koniglichen zoologisch-botanischen Gesellschaft in Wien; [Anonymous], PALAOOKOLOGISCHE BIO; [Anonymous], J PALEONTOLOGICAL SO; Bailey J.W., 1856, Am. J. Sci. 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J	Coolen, MJL; Boere, A; Abbas, B; Baas, M; Wakeham, SG; Damsté, JSS				Coolen, MJL; Boere, A; Abbas, B; Baas, M; Wakeham, SG; Damsté, JSS			Ancient DNA derived from alkenone-biosynthesizing haptophytes and other algae in Holocene sediments from the Black Sea	PALEOCEANOGRAPHY			English	Article							ORGANIC-CARBON ACCUMULATION; LONG-CHAIN ALKENONES; DINOFLAGELLATE CYSTS; STEROL COMPOSITION; FATTY-ACID; TEMPERATURE; RECORDS; ASSEMBLAGES; POPULATIONS; ADSORPTION	[1] Holocene sea surface temperatures (SST) of the Black Sea have been reconstructed using sedimentary C-37 unsaturated alkenones assumed to be derived from the coccolithophorid haptophyte Emiliania huxleyi, whose fossil coccoliths are an important constituent of the unit I sediments. However, alkenones can also be biosynthesized by haptophyte species that do not produce microscopic recognizable coccoliths. A species-specific identification of haptophytes is important in such U-37(K')-based past SST reconstructions since different species have different alkenone-SST calibrations. We showed that 18S rDNA of E. huxleyi made up only a very small percentage ( less than 0.8%) of the total eukaryotic 18S rDNA within the up to 3600-year-old fossil record obtained from the depocenter (> 2000 m) of the Black Sea. The predominant fossil 18S rDNA was derived from dinoflagellates ( Gymnodinium spp.), which are predominant members of the summer phytoplankton bloom in the modern Black Sea. Using a polymerase chain reaction/denaturing gradient gel electrophoresis method selective for haptophytes, we recovered substantial numbers of a preserved 458-base-pair (bp)-long 18S rDNA fragment of E. huxleyi from the Holocene Black Sea sediments. Additional fossil haptophyte sequences were not detected, indicating that the E. huxleyi alkenone-SST calibration can be applied for at least the last similar to 3600 years. The ancient E. huxleyi DNA was well protected against degradation since the DNA/alkenone ratio did not significantly decrease throughout the whole sediment core and 20% of similar to 2700-year-old fossil E. huxleyi DNA was still up to 23,000 base pairs long. We showed that fossil DNA offers great potential to study the Holocene paleoecology and paleoenvironment of anoxic deep-sea settings in unprecedented detail.	Royal Netherlands Inst Sea Res, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Netherlands; Skidaway Inst Oceanog, Savannah, GA 31411 USA	Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University System of Georgia; University of Georgia; Skidaway Institute of Oceanography	Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, 360 Woods Hole Rd, Woods Hole, MA 02543 USA.	mcoolen@whoi.edu	Coolen, Marco/B-8263-2015; Sinninghe Damste, Jaap/F-6128-2011	Coolen, Marco/0000-0002-0417-920X; Sinninghe Damste, Jaap/0000-0002-8683-1854				Arthur MA, 1998, PALEOCEANOGRAPHY, V13, P395, DOI 10.1029/98PA01161; ARTHUR MA, 1994, GLOBAL BIOGEOCHEM CY, V8, P195, DOI 10.1029/94GB00297; Bendle J, 2004, GEOCHEM GEOPHY GEOSY, V5, DOI 10.1029/2004GC000741; Benson DA, 2004, NUCLEIC ACIDS RES, V32, pD23, DOI 10.1093/nar/gkh045; BOON JJ, 1979, NATURE, V277, P125, DOI 10.1038/277125a0; Brassell S.C., 1993, ORG GEOCHEM, P699; BRASSELL SC, 1986, NATURE, V320, P129, DOI 10.1038/320129a0; Calvert SE, 1998, GEOLOGY, V26, P107, DOI 10.1130/0091-7613(1998)026<0107:OCAITH>2.3.CO;2; CALVERT SE, 1987, GEOLOGY, V15, P918, DOI 10.1130/0091-7613(1987)15<918:CARATO>2.0.CO;2; Conte MH, 2001, GEOCHIM COSMOCHIM AC, V65, P4275, DOI 10.1016/S0016-7037(01)00718-9; Coolen MJL, 2006, NATO SCI S SS IV EAR, V64, P41; Coolen MJL, 1998, APPL ENVIRON MICROB, V64, P4513; Coolen MJL, 2004, EARTH PLANET SC LETT, V223, P225, DOI 10.1016/j.epsl.2004.04.014; Díez B, 2001, APPL ENVIRON MICROB, V67, P2942, DOI 10.1128/AEM.67.7.2942-2951.2001; Eker-Develi E, 2003, J MARINE SYST, V39, P203, DOI 10.1016/S0924-7963(03)00031-9; Goni MA, 2004, GLOBAL BIOGEOCHEM CY, V18, DOI 10.1029/2003GB002132; Hay BJ, 1988, PALEOCEANOGRAPHY, V3, P491, DOI 10.1029/PA003i004p00491; HAY BJ, 1991, DEEP-SEA RES, V38, pS1211; Hoehler TM, 2005, ASTROBIOLOGY, V5, P95, DOI 10.1089/ast.2005.5.95; Hurt RA, 2001, APPL ENVIRON MICROB, V67, P4495, DOI 10.1128/AEM.67.10.4495-4503.2001; Inagaki F, 2005, ASTROBIOLOGY, V5, P141, DOI 10.1089/ast.2005.5.141; JONES GA, 1994, DEEP-SEA RES PT I, V41, P531, DOI 10.1016/0967-0637(94)90094-9; KHANNA M, 1992, APPL ENVIRON MICROB, V58, P1930, DOI 10.1128/AEM.58.6.1930-1939.1992; LORENZ MG, 1987, APPL ENVIRON MICROB, V53, P2948, DOI 10.1128/AEM.53.12.2948-2952.1987; Ludwig W, 2004, NUCLEIC ACIDS RES, V32, P1363, DOI 10.1093/nar/gkh293; Mansour MP, 2003, PHYTOCHEMISTRY, V63, P145, DOI 10.1016/S0031-9422(03)00052-9; Mansour MP, 1999, J PHYCOL, V35, P710, DOI 10.1046/j.1529-8817.1999.3540710.x; MARLOWE IT, 1990, CHEM GEOL, V88, P349, DOI 10.1016/0009-2541(90)90098-R; MARLOWE IT, 1984, BRIT PHYCOL J, V19, P203, DOI 10.1080/00071618400650221; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; MUYZER G, 1993, APPL ENVIRON MICROB, V59, P695, DOI 10.1128/AEM.59.3.695-700.1993; PAGET E, 1992, FEMS MICROBIOL LETT, V97, P31, DOI 10.1111/j.1574-6968.1992.tb05435.x; PFENNIG N., 1989, Autotrophic bacteria, P97; PRAHL FG, 1987, NATURE, V330, P367, DOI 10.1038/330367a0; Rontani JF, 2004, PHYTOCHEMISTRY, V65, P117, DOI 10.1016/j.phytochem.2003.09.021; Rosell-Melé A, 1998, PALEOCEANOGRAPHY, V13, P694, DOI 10.1029/98PA02355; Ross D.A., 1974, The Black Sea - Geology, Chemistry and Biology, V20, P183; Sachs JP, 2000, GEOCHEM GEOPHY GEOSY, V1; Savin MC, 2004, MICROBIAL ECOL, V48, P51, DOI 10.1007/s00248-003-1033-8; Sikes EL, 2005, DEEP-SEA RES PT I, V52, P721, DOI 10.1016/j.dsr.2004.12.003; VANOS BJH, 1994, PALEOCEANOGRAPHY, V9, P601, DOI 10.1029/94PA00597; Versteegh GJM, 2001, ORG GEOCHEM, V32, P785, DOI 10.1016/S0146-6380(01)00041-9; Villanueva J, 2002, ORG GEOCHEM, V33, P897, DOI 10.1016/S0146-6380(02)00067-0; VOLKMAN JK, 1995, GEOCHIM COSMOCHIM AC, V59, P513, DOI 10.1016/0016-7037(95)00325-T; VOLKMAN JK, 1980, PHYTOCHEMISTRY, V19, P2619, DOI 10.1016/S0031-9422(00)83930-8; Wilkin RT, 1997, EARTH PLANET SC LETT, V148, P517, DOI 10.1016/S0012-821X(97)00053-8; Xu L, 2001, ORG GEOCHEM, V32, P633, DOI 10.1016/S0146-6380(01)00019-5	48	65	68	2	27	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0883-8305	1944-9186		PALEOCEANOGRAPHY	Paleoceanography	FEB 18	2006	21	1							PA1005	10.1029/2005PA001188	http://dx.doi.org/10.1029/2005PA001188			17	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	017EY		Green Published, Bronze			2025-03-11	WOS:000235678100002
J	Harland, R; Nordberg, K; Filipsson, HL				Harland, R; Nordberg, K; Filipsson, HL			Dinoflagellate cysts and hydrographical change in Gullmar Fjord, west coast of Sweden	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						dinoflagellate cysts; Eutrophication; North Atlantic oscillation; coastal upwelling; Gullmar Fjord; West coast of Sweden	NORTH-ATLANTIC OSCILLATION; MARINE BENTHIC HYPOXIA; ENVIRONMENTAL-FACTORS; KOLJO-FJORD; GONYAULAX-TAMARENSIS; SURFACE SEDIMENTS; YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION; ASSEMBLAGES	This high-resolution study of the latest Holocene dinoflagellate cyst record from Gullmar Fjord, on the west coast of Sweden, provides evidence for the recognition of two major dinoflagellate communities within the fjord over the last 85 years. These communities may have their origins with the history of cultural eutrophication within the region, but are more likely to be associated with the wider phenomenon of the North Atlantic Oscillation and/or the complex hydrographical response of the fjord to various changing climatic environments between 1915 and 1999. The changing dinoflagellate cyst populations are compared in detail with the many hydrographical parameters available from this well studied fjord with its long instrumental records. Indeed the dinoflagellate cysts fail to demonstrate a convincing ongoing eutrophication record for the fjord but do show a major change in the cyst assemblages at about 1969/1970 at a time when the NAO was changing from a negative phase to the present-day positive phase. Gullmar Fjord is important in the history of dinoflagellate cyst studies, being the site of the 1954 study by Erdtman in which viable cysts, produced within the phytoplankton, were first documented within the water column. (c) 2005 Elsevier B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Gothenburg, Dept Oceanog, Ctr Earth Sci, S-40530 Gothenburg, Sweden; Univ Bremen, DE-28334 Bremen, Germany	University of Gothenburg; University of Bremen	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.	rex.harland@ntlworld.com	Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Nordberg, Kjell/0000-0003-0085-4607				Ameborg L, 2004, CONT SHELF RES, V24, P443; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Aure J, 1996, ICES J MAR SCI, V53, P589, DOI 10.1006/jmsc.1996.0080; BADEN SP, 1990, AMBIO, V19, P113; Beaugrand G, 2002, SCIENCE, V296, P1692, DOI 10.1126/science.1071329; Björk G, 2003, CONT SHELF RES, V23, P1143, DOI 10.1016/S0278-4343(03)00081-5; Chen DL, 1999, TELLUS A, V51, P505, DOI 10.1034/j.1600-0870.1999.t01-4-00004.x; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B, 1985, NORSK GEOL TIDSSKR, V65, P97; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Diaz RJ, 1995, OCEANOGR MAR BIOL, V33, P245; ENGSTROM SG, 1970, LYSEKIL, V77, P1; Erdtman G., 1954, Botaniska Notiser, V2, P103; Filipsson HL, 2004, ESTUARIES, V27, P867, DOI 10.1007/BF02912048; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Gustafsson B, 1999, CONT SHELF RES, V19, P1021, DOI 10.1016/S0278-4343(99)00008-4; GUSTAFSSON M, 1996, J SEA RES, V35, P39; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; HARLAND R, 1989, J GEOL SOC LONDON, V146, P951; HURRELL JW, 1995, SCIENCE, V269, P676, DOI 10.1126/science.269.5224.676; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Lindahl O, 1998, ICES J MAR SCI, V55, P723, DOI 10.1006/jmsc.1998.0379; Lindahl O., 2003, ICES MAR SCI S, V219, P387; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; McQuoid MR, 2003, ESTUAR COAST SHELF S, V56, P339, DOI 10.1016/S0272-7714(02)00187-7; NIXON SW, 1995, OPHELIA, V41, P199, DOI 10.1080/00785236.1995.10422044; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Nordberg K, 2000, J MARINE SYST, V23, P303, DOI 10.1016/S0924-7963(99)00067-6; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Powell A.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V112, P297, DOI 10.2973/odp.proc.sr.112.196.1990; Reid P.C., 1974, Nova Hedwigia, V25, P579; Reynolds C.S., 1988, P388; Rochon Andre, 1999, AASP Contributions Series, V35, P1; ROSENBERG R, 1990, MAR POLLUT BULL, V21, P335, DOI 10.1016/0025-326X(90)90794-9; Rosenow J, 2001, ORYX, V35, P1; RYDBERG L, 1975, REPORT, V10, P1; Sangiorgi F, 2004, ESTUAR COAST SHELF S, V60, P69, DOI 10.1016/j.ecss.2003.12.001; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Smayda TJ, 2001, J PLANKTON RES, V23, P447, DOI 10.1093/plankt/23.5.447; Svansson A, 1984, I HYDROGR RES SER, V23, P1; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P1; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	63	57	58	0	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0048-9697			SCI TOTAL ENVIRON	Sci. Total Environ.	FEB 15	2006	355	1-3					204	231		10.1016/j.scitotenv.2005.02.030	http://dx.doi.org/10.1016/j.scitotenv.2005.02.030			28	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	014VM	15950265				2025-03-11	WOS:000235508500019
J	Prebble, JG; Raine, JI; Barrett, PJ; Hannah, MJ				Prebble, JG; Raine, JI; Barrett, PJ; Hannah, MJ			Vegetation and climate from two Oligocene glacioeustatic sedimentary cycles (31 and 24 Ma) cored by the Cape Roberts Project, Victoria Land Basin, Antarctica	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			Antarctica; Oligocene; miospores; paleobotany; paleoenvironment	PLIOCENE SIRIUS GROUP; TRANSANTARCTIC MOUNTAINS; ICE-SHEET; CHRONOLOGY; TRANSITION; GLACIATION; EOCENE; MARGIN; LEAVES; SEA	The Cape Roberts Project recovered over 1500 m of coastal glaciomarine sediments of Oligocene and Early Miocene age off the Ross Sea margin of Antarctica. The strata are characterised by cyclic repetition of facies in a glaciomarine setting, and are interpreted to be a record of glacial-interglacial episodes involving significant changes ill eustatic sea level oil Milankovitch frequencies. We have Undertaken a detailed Study of pollen and spores (miospores) from an Early Oligocene (31 Ma), and a Late Oligocene (24 Ma) cycle. Although miospores are sparse in the core, averaging only similar to 1 grain per grain of sediment processed, over 1200 Cenozoic miospores were recovered for this study. Previous studies of miospores from Ross Sea sediments have encountered problems differentiating between reworked and in Situ palynomorphs. Here, only samples containing a low relative abundance of all Eocene dinoflagellate cyst assemblage (the Transantarctic Flora) have been used to infer the contemporaneous Oligocene miospore flora. The flora of the Early Oligocene cycle is dominated by three species of Nothofagidites, and four types of Podocarpidites. The assemblage from the Upper Oligocene cycle is also dominated by Nothofagidites and Podocarpidites, bill with the addition of two distinctive taxa, in angiosperm pollen and a bryophyte spore. Notwithstanding these additions, there is a slight decrease in floral diversity between the two cycles. While this study confirms that some floristic changes did occur between Early and Late Oligocene time oil the Victoria Land coast, the present data suggest that the Changes were not extensive. It is likely that the vegetation of both cycles was a low diversity scrub of low stature, consisting of mainly Nothofagus, podocarps, and bryophytes. Modern analogues suggest that this vegetation was growing ill a climate significantly warmer (Mean Summer Monthly Temperature 4-12 degrees C) than is found on the present day Victoria Land (MSMT -5 degrees C), although colder that the temperate climate suggested by the diverse flora found in Ross Sea sediments of Eocene age. (c) 2005 Elsevier B.V. All rights reserved.	Victoria Univ Wellington, Sch Earth Sci, Wellington, New Zealand; Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand	Victoria University Wellington; GNS Science - New Zealand; Victoria University Wellington	Victoria Univ Wellington, Sch Earth Sci, POB 600, Wellington, New Zealand.	joseph_prebble@URSCorp.com	Raine, James/D-5124-2009; Hannah, Michael/H-1083-2015	Hannah, Michael/0000-0002-2275-0086; Raine, James Ian/0000-0001-5294-2102; Prebble, Joseph/0000-0002-7268-4187				[Anonymous], 1991, SPORE ATLAS NZ FERNS; [Anonymous], 2001, TERRA ANTARTICA; [Anonymous], 2001, Terra Antartica, V8, P615; [Anonymous], 1976, TUATARA; [Anonymous], 1996, ECOLOGY BIOGEOGRAPHY; Ashworth AC, 2004, PALAEOGEOGR PALAEOCL, V213, P65, DOI 10.1016/j.palaeo.2004.07.002; Askin R A., 2000, Terra Antarctica, V7, P493; Askin R A., 1986, Antarctic Journal of the United States, V21, P34; Askin R A., 2000, AGU Ant Res Ser, V76, P161, DOI DOI 10.1029/AR076P0161; BERGGREN WA, 1995, GEOCHRONOLOGY TIME S, P130; Billups K, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2000PA000567; Bold H.C., 1987, Morphology of Plants and Fungi; Brownsey P.J., 1989, New Zealand ferns and allied plants; CANTRILL DJ, 2001, TERRA ANTARTICA, V8, P401; *CAP ROB SCI TEAM, 1998, TERRA ANTARTICA, V5; COOKSON ISABEL C, 1954, AUSTRALIAN JOUR BOT, V2, P197, DOI 10.1071/BT9540197; Couper R. 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Paleoclimatol. Paleoecol.	FEB 9	2006	231	1-2					41	57		10.1016/j.palaeo.2005.07.025	http://dx.doi.org/10.1016/j.palaeo.2005.07.025			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	019PT					2025-03-11	WOS:000235849900004
J	Prebble, JG; Hannah, MJ; Barrett, PJ				Prebble, JG; Hannah, MJ; Barrett, PJ			Changing Oligocene climate recorded by palynomorphs from two glacio-eustatic sedimentary cycles, Cape Roberts Project, Victoria Land Basin, Antarctica	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			Antarctica; Oligocene; palynomorphs; marine environment; paleoenvironment; marine palynomorphs	DINOFLAGELLATE CYSTS; SEA; CHRONOLOGY; EOCENE	Two marine palynomorph assemblages recovered from two glacio-eustatic sedimentary cycles from the Cape Roberts Project (CRP), which recovered over 1500 m of Oligocene and Miocene strata from the western margin of the Victoria Land Basin, are investigated. We present results from one cycle dated as early Oligocene and the other dated as late Oligocene. Modest numbers of marine palynomorphs were recovered, with an average abundance of 56 specimens per gram. The assemblages recovered from both cycles are broadly similar, and dominated by acritarchs and the phycoma of prasinophyte algae. These include Leiosphaeridia sp. 2, Leiosphaeridia sp. 3, and the prasinophyte alga, Cymatiosphaera sp. 2. In detail, however, the lower Oligocene assemblage is different from that of the upper Oligocene. The lower Oligocene cycle includes Impagidinium cf. dispertium and Impagidinium cf elegans. Cymatiosphaera sp. 6 and Pyxidinopsis sp. are abundant. The upper Oligocene cycle is characterized by an absence of Cymatiosphaera (?) invaganata, Cymatiosphaera sp. 8, and Pterospemella sp. A. It has very low numbers of Acritarch sp. b, Impagidinium and Pyxidinopsis. It contains Tasmanites sp. and Brigantedinium pynei, and it has higher abundances of Lejeunecysta sp. 1 and Sigmopollis than the lower Oligocene cycle. The environmental interpretations of the CRP core from other workers using sedimentological and paleontological indicators are used to infer environmental conditions that are likely to have influenced the marine palynomorph assemblages. Paleontological and sedimentological analysis suggests that both cycles were deposited in cold conditions, with sea ice and melt water influence, although the upper Oligocene assemblage is inferred to have existed in colder marine conditions, with more prolonged sea ice cover and less associated fresh water input than the assemblage of early Oligocene times. The application of modem analogues for some of the marine palynomorph taxa identified suggest the presence of sea ice, and occasionally lowered salinity in both cycles. This is broadly consistent with the findings of the other paleoenvironmental studies on the CRP cores. (c) 2005 Elsevier B.V. All rights reserved.	Victoria Univ Wellington, Sch Earth Sci, Wellington, New Zealand; Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand	Victoria University Wellington; Victoria University Wellington	Prebble, JG (通讯作者)，Victoria Univ Wellington, Sch Earth Sci, Wellington, New Zealand.	Joseph_Prebble@URSCorp.com	Hannah, Michael/H-1083-2015	Hannah, Michael/0000-0002-2275-0086; Prebble, Joseph/0000-0002-7268-4187				[Anonymous], 2001, TERRA ANTARTICA; [Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1998, Terra Antartica, V5, P1; [Anonymous], TERRA ANTARTICA; [Anonymous], 2000, TERRA ANTARTICA; [Anonymous], TERRA ANTARTICA; [Anonymous], 1980, PALEOBIOLOGY PLANT P; Askin R A., 2000, Terra Antarctica, V7, P493; Atkins C., 2001, Terra Antarct, V8, P263; Barrett P.J., 2001, TERRA ANTARTICA, V8, P245; Davey F.J., 2001, EOS T AM GEOPHYS UN, V82, P585, DOI [10.1029/01EO00339, DOI 10.1029/01E000339]; Dingle R.V., 2001, TERRA ANTARTICA, V8, P369; Dingle RV., 2000, TERRA ANTARCT, V7, P479; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Ehrmann W., 2001, Terra Antartica, V8, P533; Ehrmann W., 2000, TERRA ANTART, V7, P575; Fielding C.R., 2001, Terra Antarctica, V8, P217; Florindo F, 2005, GLOBAL PLANET CHANGE, V45, P207, DOI 10.1016/j.gloplacha.2004.09.009; GALEOTTI MB, 2000, TERRA ANTARTICA, V7, P473; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; Hall K., 2001, TERRA ANTARCT, V8, P275; Hanna B, 2000, Aust J Holist Nurs, V7, P4; Hannah M. 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M., 2000, Terra Antartica, V7, P339; Watkins DK., 2001, TERRA ANTARTICA, V8, P339; WATKINS DK, 2000, TERRA ANTARTICA, V7, P443; Wilson GS, 1998, GEOL SOC AM BULL, V110, P35, DOI 10.1130/0016-7606(1998)110<0035:MCOTEO>2.3.CO;2; Wilson GS., 2000, Terra Antartica, V7, P647; Wrenn J H., 1998, Terra Antarctica, V5, P553; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	59	9	12	0	3	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	FEB 9	2006	231	1-2					58	70		10.1016/j.palaeo.2005.07.026	http://dx.doi.org/10.1016/j.palaeo.2005.07.026			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	019PT		Green Published			2025-03-11	WOS:000235849900005
J	Hannah, MJ				Hannah, MJ			The palynology of ODP site 1165, Prydz Bay, East Antarctica: A record of Miocene glacial advance and retreat	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	32nd International Geological Congress	AUG 20-28, 2004	Florence, ITALY			Prydz Bay; Leg 188; site 1165; palynology; Miocene ice shelf fluctuations		ODP Site 1165 recovered around 1000 m of Early to Late Miocene mixed hemi-pelagic sediments from the Wild Drift, offshore Prydz Bay. Samples from between the bottom of the hole and I 10 m below sea floor yielded distinctive palynomorph assemblages, ranging in age from 22.2 Ma at the base to 8 Ma at 110 mbsf. Many assemblages contain large numbers of reworked terrestrial pollen and spores varying in age from Devonian to Early Eocene. In situ palynomorph assemblages are dominated by the acritarch Leiosphaeridia. Other components of the assemblages are dinoflagellate cysts, prasinophyte algae and acanthomorph acritarchs. Comparison with modem Arctic assemblages suggests that the presence of these forms implies significant fresh water input, resulting in complex, stratified water masses unlike the situation in Prydz Bay today. Based on the palynomorph assemblages, which are alternately dominated by glacially derived reworked terrestrial miospores and in situ leiospheres typical of ice edges, the interval between the bottom of the hole and 310 mbsf (22.2-15 Ma) can be divided into three intervals. Samples from the base of each interval are dominated by high percentages of reworked terrestrial miospores and are interpreted as representing a period of time dominated by increased glacial flow down the Lambert Glacier and an expanded Amery Ice Shelf. Samples from the upper part of each interval are characterised by low percentages of reworked terrestrial miospores and generally high percentages of leiospheres. This is thought to represent a period of time of low glacial flow and retreat of the Amery Ice Shelf At the same time an increase in the minor components of the marine palynomorph assemblage is recorded, possibly in response to an overall climatic amelioration onto which the three glacial cycles are superimposed. Overlaying these glacial cycles, between 310 and 99.1 mbsf (15-8 Ma), the assemblages are completely dominated by reworked material, including an Eocene dinoflagellate assemblage previously recoded on the continental shelf in ODP drill-hole 1166. Leiospheres or other in situ marine palynomorphs are either absent or only make up a very small percentage of the assemblage. This is interpreted as representing an interval where the climatic amelioration recorded during the underlying three cycles has been sharply reversed and the Amery Ice Shelf has expanded to the point where it is grounded across the continental shelf, eroding the Eocene material present there. The age of this climatic reversal (15 Ma) coincides with the well-known shift in the oxygen isotope curve thought to be associated with the development of permanent ice sheets on Antarctica. (c) 2005 Elsevier B.V. All rights reserved.	Victoria Univ Wellington, Antarctic Res Ctr, Sch Earth Sci, Wellington, New Zealand	Victoria University Wellington	Hannah, MJ (通讯作者)，Victoria Univ Wellington, Antarctic Res Ctr, Sch Earth Sci, POB 600, Wellington, New Zealand.	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Paleoclimatol. Paleoecol.	FEB 9	2006	231	1-2					120	133		10.1016/j.palaeo.2005.07.029	http://dx.doi.org/10.1016/j.palaeo.2005.07.029			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	019PT					2025-03-11	WOS:000235849900009
J	Moestrup, O; Hansen, G; Daugbjerg, N; Flaim, G; D'Andrea, M				Moestrup, O; Hansen, G; Daugbjerg, N; Flaim, G; D'Andrea, M			Studies on woloszynskioid dinoflagellates II:: On <i>Tovellia sanguinea</i> sp nov., the dinoflagellate responsible for the reddening of Lake Tovel, N. Italy	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						dinophyceae; freshwater phytoplankton; Glenodinium sanguineum; red tide; Tovellia; LSU rDNA; phylogeny	AMPHIDINIUM DINOPHYCEAE; GLENODINIUM-SANGUINEUM; COMB. NOV; GEN. NOV; ULTRASTRUCTURE; PERIDINIOPSIS; TRICHOCYSTS; MORPHOLOGY; PHYLOGENY; CYSTS	The organism responsible for the former annual reddening of Lake Tovel in the Italian Alps (up to 1964) has been identified and studied in detail. Considerable confusion exists regarding the identity of this organism, and the detailed description by Baldi in 1941 is now believed to be based on more than one organism. Baldi's red and green forms appear to be two different organisms, both of which have now been isolated into unialgal culture and studied using light microscopy, electron microscopy, and sequencing of the large subunit of ribosomal DNA (LSU rDNA). The organism has been found in three lakes in the area, but only in Lake Tovel have conditions allowed for reddening of the water during summer. The name of the organism believed to be the cause of the reddening, Glenodinium sanguineum Marchesoni, used in numerous publications, is an illegitimate homonym of G. sanguineum H. J. Carter, and the organism is described here as a new species, Tovellia sanguinea sp. nov., the seventh species of the newly described genus Tovellia. T. sanguinea is closely related to the other red-coloured species of Tovellia, Tovellia coronata ( previously known as Woloszynskia coronata) but differs in several morphological features, notably the chloroplast arrangement, and in LSU rDNA sequence divergence (11-12%). Cells preserved from Lake Tovel during a reddening phenomenon in 1938 have been re-examined by scanning electron microscopy and agree morphologically with the new isolates. Tovellia sanguinea is a species of oligotrophic or mesotrophic-oligotrophic cold-water lakes, in which the average summer temperature does not exceed 15 degrees C. It occurs on both calcareous ( as in Lake Tovel) and non-calcareous substrata (as in the other two lakes).	Inst Biol, Dept Phycol, DK-1353 Copenhagen K, Denmark; Ist Agrario, I-38010 San Michele All Adige, TN, Italy	Fondazione Edmund Mach	Inst Biol, Dept Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	moestrup@bi.ku.dk	Flaim, Giovanna/AAD-5013-2020; Hansen, Gert/P-3328-2014; Flaim, Giovanna/C-7622-2016; Daugbjerg, Niels/D-3521-2014	Hansen, Gert/0000-0002-5751-8316; Moestrup, Ojvind/0000-0003-0965-8645; Flaim, Giovanna/0000-0002-1753-5605; Daugbjerg, Niels/0000-0002-0397-3073				Andersen RA, 1997, J PHYCOL, V33, P1, DOI 10.1111/j.0022-3646.1997.00001.x; [Anonymous], 1996, ZOOL ANZ; Baldi E., 1938, Studi Trentini Trento, V19, P245; Baldi E., 1941, Memorie del Museo di Storia Naturale della Venezia Tridentina, V6, P1; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; BOUCK GB, 1966, PROTOPLASMA, V61, P205, DOI 10.1007/BF01247920; Calado AJ, 1997, PHYCOLOGIA, V36, P47, DOI 10.2216/i0031-8884-36-1-47.1; Calado AJ, 2002, PHYCOLOGIA, V41, P567, DOI 10.2216/i0031-8884-41-6-567.1; Calado AJ, 1999, EUR J PHYCOL, V34, P179, DOI 10.1080/09670269910001736232; Calado AJ, 1998, J PHYCOL, V34, P536, DOI 10.1046/j.1529-8817.1998.340536.x; CARTER HJ, 1858, ANN MAG NAT HIST, V3, P258; Cavalca L, 2001, ANN MICROBIOL, V51, P159; CHRISTEN H. 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J. Phycol.	FEB	2006	41	1					47	65		10.1080/09670260600556682	http://dx.doi.org/10.1080/09670260600556682			19	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	037RN					2025-03-11	WOS:000237164700005
J	Figueroa, RI; Bravo, I; Garcés, E; Ramilo, I				Figueroa, RI; Bravo, I; Garcés, E; Ramilo, I			Nuclear features and effect of nutrients on <i>Gymnodinium catenatum</i> (Dinophyceae) sexual stages	JOURNAL OF PHYCOLOGY			English	Article						Dinophyceae; encystment; gametes; Gymnodinium catenatum; life cycle; nitrate; nutritional effects; phosphate; reproduction	DINOFLAGELLATE GONYAULAX-TAMARENSIS; CYST FORMATION; MATING-TYPE; LIFE-CYCLE; REPRODUCTION; ENCYSTMENT; TEMPERATURE; GERMINATION; EXCYSTMENT; DIVISION	Gymnodinium catenatum Graham is an unarmored, cyst-forming dinoflagellate species responsible for outbreaks of paralytic shellfish poisoning. The nuclear development of the cells during the sexual cycle and the effect of different nitrate and phosphate external levels on sexual stages were studied. Nuclear fusion of gametes occurred before or at the same time as cytoplasmic fusion. During this process, either both nuclei migrated to a central area in the sulcal region, or only one of them migrated to the other nucleus. The motile and longitudinally biflagellated zygote presented a large, pear-shaped nucleus, and either divided or encysted. Planozygotes and germlings underwent similar division processes, which suggested an uncoordinated meiosis in both encysting and non-encysting zygotes. Encystment in culture was greater under low nitrate and phosphate limitation (L/15) than when only one or neither of these nutrients were added (L-N, L-P, and -N-P). However, planozygotes individually monitored achieved the maximum encystment (40%) in a medium with no phosphate or nitrate added (-N-P), while most of them divided (70%-90%) in replete (L1) or half-replete (L-N and L-P) media. Low levels of nitrate in the medium of cyst formation promoted a deficient development of the cyst wall. On the other hand, low phosphate levels in the medium of germination prevented both planozygote and germling division and lowered the final germination frequencies of cysts. The minimum dormancy, with an average value of 13.7 +/- 5.5 days, was not affected by any of the nutritional conditions studied.	Inst Oceanog Vigo, Vigo 36200, Spain; Inst Ciencias Mar, CSIC, E-08039 Barcelona, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Inst Oceanog Vigo, Cabo Estai Canido, Vigo 36200, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015	Garces, Esther/0000-0002-2712-501X; Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X				AN KH, 1992, BOT MAR, V35, P61, DOI 10.1515/botm.1992.35.1.61; Anderson D.M., 1998, PHYSL ECOLOGY HARMFU, P19; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Beam C. 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Phycol.	FEB	2006	42	1					67	77		10.1111/j.1529-8817.2006.00181.x	http://dx.doi.org/10.1111/j.1529-8817.2006.00181.x			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	010TJ					2025-03-11	WOS:000235220500008
J	Fujii, R; Matsuoka, K				Fujii, R; Matsuoka, K			Seasonal change of dinoflagellates cyst flux collected in a sediment trap in Omura Bay, West Japan	JOURNAL OF PLANKTON RESEARCH			English	Article							DINOPHYCEAE; SCRIPPSIELLA; DYNAMICS; GROWTH; BLOOM; RATES	Sediment trap samples were harvested bimonthly from 1998 to 2000 and examined to better understand the species composition and seasonal variation of dinoflagellate cyst flux in Omura Bay in Japan. Samples' living cyst flux clearly showed seasonal variation with the higher flux number between autumn and winter. In total, 43 different cyst taxa were recorded, and these were composed of two different ecological groups. The first group included Protoperidinium compressum and Protoperidinium subinerme, which increased every autumn to winter. The second group included Gonyaulax spp. and Pheopolykrikos hartmannii and was trapped throughout the year. These two groups manifested the different flux patterns and were, respectively, heterotrophic and autotrophic in nutrition. In the heterotrophic group, protoperidinioid cysts were dominant. Vegetative cells of protoperidinioid are known to feed mainly diatoms. Sample diatom flux also increased from autumn to winter. Therefore, the increase of protoperidinioid cysts in autumn to winter was observed to correlate with diatom blooms. In contrast, the autotrophic group mostly consisted of Gonyaulacoid cysts and were generally observed throughout the year, although occurrence varied between species most likely responding to favorable environmental conditions. The results indicate that cyst production is closely related to different nutritional modes.	Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8512213, Japan	Nagasaki University; Nagasaki University	Nagasaki Univ, Inst E China Sea Res, 1551-7 Tairo Cho, Nagasaki 8512213, Japan.	kazu-mtk@net.nagasaki-u.ac.jp						Anderson DM., 1995, IOC MAN GUIDES, V33, P229; CARRADA G C, 1980, Marine Ecology, V1, P105, DOI 10.1111/j.1439-0485.1980.tb00213.x; DALE B, 1985, NORSK GEOL TIDSSKR, V65, P97; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; GAINES G, 1984, J PLANKTON RES, V6, P1057, DOI 10.1093/plankt/6.6.1057; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Goodman D.K., 1987, Botanical Monographs (Oxford), V21, P649; HANSEN PJ, 1992, MAR BIOL, V114, P327, DOI 10.1007/BF00349535; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HEINRICH A. K., 1962, JOUR CONSEIL PERM INTERNATL EXPLOR MER, V27, P15; IIZUKA S, 1985, COASTAL OCEANOGRAPHY, P879; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JACOBSON DM, 1993, J PLANKTON RES, V15, P723, DOI 10.1093/plankt/15.7.723; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; KATO M, 2000, THESIS TOKYO METROPO; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; KOBAYASHI S, 1986, Bulletin of Plankton Society of Japan, V33, P81; KOBAYASHI S, 1982, THESIS NAGASAKI U NA; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matsuoka K., 1989, P461; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MATSUOKA K, 1989, KAIYO MONTHLY, V21, P232; Matsuoka K., 2000, TECHNICAL GUIDE MODE; MATSUOKA K, 1995, TRANSITION ORGANISMS, V116, P45; MATSUOKA K, 1982, FUNDAMENTAL STUDIES, P197; Matsuoka Kazumi, 1992, Quaternary Research (Tokyo), V31, P147; Mizushima K, 2004, PHYCOL RES, V52, P408, DOI 10.1111/j.1440-183.2004.00358.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Poole R.W., 1974, INTRO QUANTITATIVE E; Shannon C.E., 1964, MATH THEORY COMMUNIC; SHIMIZU M, 2001, THESIS NAGASAKI U NA; SMITH GH, 1955, CRYPTOGENIC BOT, V1; *SOC WELF HUM SERV, 1999, RES WAT AN PUBL TRAC; *SOC WELF HUM SERV, 2000, RES WAT AN PUBL TRAC; *SOC WELF HUM SERV, 2001, RES WAT AN PUBL TRAC; SOMMER U, 1993, HYDROBIOLOGIA, V249, P1, DOI 10.1007/BF00008837; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; SOURNIA A, 1969, MAR BIOL, V3, P287, DOI 10.1007/BF00698859; Wendler I, 2002, MAR MICROPALEONTOL, V46, P1, DOI 10.1016/S0377-8398(02)00049-X; WIILIAMS GL, 1998, SPECIAL CONTRIBUTION, V34	43	39	45	0	11	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	FEB	2006	28	2					131	147		10.1093/plankt/fbi106	http://dx.doi.org/10.1093/plankt/fbi106			17	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	020QD		Bronze			2025-03-11	WOS:000235923900002
J	Riding, JB; Zijlstra, G				Riding, James B.; Zijlstra, Gea			<i>Belowicysta</i> nom. nov., a new name for the Jurassic dinoflagellate cyst <i>Belowia</i> Riding & Helby, 2001	ALCHERINGA			English	Article								The Jurassic dinoflagellate cyst genus Belowia Riding & Helby, 2001 is a junior homonym of Belowia Moquin-Tandon, 1849, a genus of the Chenopodiaceae. The new generic name Belowicysta is proposed here to replace Belowia Riding & Helby, 2001.	British Geol Survey, Nottingham NG12 5GG, England; Utrecht Univ Branch, Natl Herbarium Nederland, NL-3584 CS Utrecht, Netherlands	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Utrecht University	Riding, JB (通讯作者)，British Geol Survey, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk; g.zijlstra@bio.uu.nl						Foster C, 2001, MEMOIR ASS AUSTRALAS, V24, pi; HASIBUAN F, 1990, THESIS U AUCKLAND NZ; HELBY R, 1988, 7 INT PALYN C BRISB, P69; MOQUINTANDON CHB, 1849, PRODROMUS SYSTEMATIS, V13, P41; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P177	5	0	0	0	0	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0311-5518	1752-0754		ALCHERINGA	Alcheringa		2006	30	2					313	314		10.1080/03115510608619319	http://dx.doi.org/10.1080/03115510608619319			2	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	101KU		Green Submitted			2025-03-11	WOS:000241740500008
J	Bialkowski, A; Châteauneuf, JJ; Cojan, I; Bauer, H				Bialkowski, Anne; Chateauneuf, Jean-Jacoues; Cojan, Isabelle; Bauer, Hugues			Integrated stratigraphy and paleoenvironmental reconstruction of the Miocene series of the Chateauredon Dome, S.E. France	ECLOGAE GEOLOGICAE HELVETIAE			English	Article						palynology; paleoenvironment; carbon and oxygen stable isotopes; Miocene; France	CARBON-ISOTOPE STRATIGRAPHY; PROJECT LEG 90; MIDDLE MIOCENE; MAGNETOSTRATIGRAPHIC CALIBRATION; SOUTHWEST PACIFIC; HAUTE-PROVENCE; WESTERN-EUROPE; STABLE CARBON; SE FRANCE; NEOGENE	This study presents the results of a palynological analysis (dinocysts, spores and pollen) that are discussed with those obtained from stable isotopes geo-chemistry (delta C-13 and delta O-18) on Miocene coastal and continental deposits in the southern area of the Digne Valensole Basin. Palynology study has been conducted on dark levels while isotopic analysis was performed on paleosol carbonate nodules. Stratigraphic attributions based on palynology are restricted to dinoflagellate cysts associations as spore and pollen assemblages are scarcely identified. They confirm the stratigraphy based on the micromammal fossil sites and propose an Aquitanian to early Serravallian age. From a selection of ODP-DSDP sites, the marine delta C-13 chemostratigraphy shows several characteristic isotopic intervals. These were also identified on the continental signal from the paleosets. Stratigrapbic interpretation from the isotopic continental signal is in good agreement with both palynological data and micromammal sites attributions. It can offer a high resolution correlation, a few 100 kyr when paleosols are frequent and delta C-13 fluctuations significant. The method puts also in evidence hiatuses (during middle Aquitanian and late Burdigalian) and precise the age of formations interbedded between micromammal sites. Regarding paleoenvironmental reconstruction, the palynological study is more efficient than isotopic data and shows a flora evolution from mesothermic riparian and coastal vegetation during Aquitanian/Burdigalian to herbaceous and more open vegetation during the Langhian period in association to a drier and warmer climate. This study brings also new insights on paleogeographic reconstructions. The studied area was located close to the sea coast during the lower Miocene. Marine incursions occurred during the middle Aquitanian and from late Burdigalian to early Serravallian. These are characterized by tidal facies as well as dinoflagellate cysts and benthic foraminifera occurrences. These marine incursions, better recorded in the eastern part of the Chateauredon Dome, argued for a northern or a southern connection with the Miocene sea in relation to the foreland basin geodynamic evolution.	Ecole Mines, CGES Sedimentol, F-77300 Fontainebleau, France	Universite PSL; MINES ParisTech	Bialkowski, A (通讯作者)，Ecole Mines, CGES Sedimentol, 35 Rue St Honore, F-77300 Fontainebleau, France.	anne.bialkowski@wanadoo.fr; chateauboy@wanadoo.fr; isabelle.cojan@ensmp.fr; hugues.bauer@ensmp.fr	BAUER, HUGUES/AAK-6418-2021	BAUER, HUGUES/0000-0002-0895-6512				AGUILAR JP, 1982, CR ACAD SCI II, V294, P49; Aguilar JP, 1996, NEWSL STRATIGR, V34, P177; AGUILAR JP, 1981, THESIS U LANGUEDOC M; AGUILAR JP, 1999, NOUVEAUX CRICETIDES, V253, P1; AGUILAR JP, 2003, MAMMIFERES MIOCENE I, P1; Agustí J, 2001, EARTH-SCI REV, V52, P247, DOI 10.1016/S0012-8252(00)00025-8; [Anonymous], 1990, NATO S EUR NEOG MAMM; Barrera Enriqueta C, 1993, P OCEAN DRILLING PRO, P269, DOI DOI 10.2973/ODP.PROC.SR.130.022.1993; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BESSEDIK M, 1985, COUPLE RECIF MANGROV, P20; Bessedik M., 1985, THESIS U SCI TECHNIQ; BESSON D, 2005, THESIS ECOLE NATL S; BESSON D, 2002, NEOGENE BASSIN AVANT; BIALKOSKI A, 2004, 46 EC MIN PAR; BLOW WH, 1969, B LEIDEN, V1, P199; BRINKHUIS H, 1992, THESIS UTRECHT U; BURBANK DW, 1992, ECLOGAE GEOL HELV, V85, P399; CALLEC Y, 2001, 43 EC MIN PAR, V1; Cerling T.E., 1999, Palaeoweathering, palaeosurfaces and related continental deposits: International Association of Sedimentologists Special Publication, P43, DOI DOI 10.1002/9781444304190.CH2; Cerling T.E., 1993, CLIMATE CHANGE CONTI, DOI DOI 10.1029/GM078P0217; CERLING TE, 1984, EARTH PLANET SC LETT, V71, P229, DOI 10.1016/0012-821X(84)90089-X; Cerling TE, 1997, NATURE, V389, P153, DOI 10.1038/38229; CHATEAUNEUF J.J., 1995, GEOL FR, V2, P43; Châteauneuf JJ, 2006, CR GEOSCI, V338, P197, DOI 10.1016/j.crte.2005.10.004; Cojan I, 2000, GEOLOGY, V28, P259, DOI 10.1130/0091-7613(2000)028<0259:SCISOT>2.3.CO;2; Corfield R.M., 1993, Proceedings of the Ocean Drilling Program, 130 Scientific Results Ocean Drilling Program, P307, DOI DOI 10.2973/ODP.PROC.SR.130.026.1993; Couëffé R, 2003, ECLOGAE GEOL HELV, V96, P197, DOI 10.1007/s00015-003-1090-5; Crumeyrolle P., 1991, International Association Sedimentologists Special Publication, V12, P373, DOI [DOI 10.1002/9781444303896.CH20, 10.1002/9781444303896.ch20]; DEBRANDKPASSART S, 1984, MEMOIRE BRGM FRANCE, V125; DEBRANDPASSART S, 1984, MEMOIRE BRGM FRANCE, V126; Demarcq G., 1984, Synthse gologique du Sud-Est de la France : Stratigraphie et palogographie, V125, pp. 503; FLOWER BP, 1993, PALEOCEANOGRAPHY, V8, P811, DOI 10.1029/93PA02196; FLOWER BP, 1997, P ODP SCI RESULTS, V154, P269; HUGUENEY YM, 1992, PALEONTOLOGIA, V1, P24; HUGUENEY YM, 1992, PALEONTOLOGIA, V1, P123; Jiménez-Moreno G, 2005, PALAEOGEOGR PALAEOCL, V216, P73, DOI 10.1016/j.palaeo.2004.10.007; Kempf O., 1997, MEM TRAV EPHE I MONT, P547; KENNETT JP, 1986, INITIAL REP DEEP SEA, V90, P1383, DOI 10.2973/dsdp.proc.90.1986; KENNETT JP, 1986, 90 DSDP, V90; KOCH PL, 1992, NATURE, V358, P319, DOI 10.1038/358319a0; Lalai D., 1986, Palaeovertebrata (Montpellier), V16, P77; LOHMAN WH, 1986, INITIAL REP DEEP SEA, V90, P763; Lopez S, 2000, CR ACAD SCI II A, V330, P837, DOI 10.1016/S1251-8050(00)00224-X; MARTIN P, 1986, PSYCHOPHARMACOLOGY, V90, P90; MEIN P, 1984, CHAPITRE NEOGENE SYN, V125, P477; MILLER KG, 1985, GEOPHYS MONOGR SER, V32, P469, DOI DOI 10.1029/GM032P0469; MONTENAT C, 2001, GEOLOGIE FRANCE, V3, P3; Schlunegger F, 1996, ECLOGAE GEOL HELV, V89, P753; Sen S, 1997, PALAEOGEOGR PALAEOCL, V133, P181, DOI 10.1016/S0031-0182(97)00079-5; SPENCERCERVATO C, 1999, CENOZOIC DEEP SEA MI, V2; Steininger F.F., 1996, The Evolution of Western Eurasian Neogene Mammal Faunas, P7; STEININGER FF, 1990, NATO ASI SER A, V180, P15; Thome M., 1989, IN PRESS, V2, P281; VINCENT E, 1985, AM GEOPHYS UNION MON, V32, P455, DOI DOI 10.1029/GM032P0455; Woodruff F., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V115, P519, DOI 10.2973/odp.proc.sr.115.147.1990; Wright JD, 1992, PALEOCEANOGRAPHY, V7, P357, DOI 10.1029/92PA00760; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zachos JC, 2001, SCIENCE, V292, P274, DOI 10.1126/science.1058288	58	9	9	0	13	BIRKHAUSER VERLAG AG	BASEL	VIADUKSTRASSE 40-44, PO BOX 133, CH-4010 BASEL, SWITZERLAND	0012-9402			ECLOGAE GEOL HELV	Eclogae Geol. Helv.		2006	99	1					1	15		10.1007/s00015-006-1176-y	http://dx.doi.org/10.1007/s00015-006-1176-y			15	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	070IE		Bronze			2025-03-11	WOS:000239514300001
J	Nagasoe, S; Kim, DI; Shimasaki, Y; Oshima, Y; Yamaguchi, M; Honjo, T				Nagasoe, S; Kim, DI; Shimasaki, Y; Oshima, Y; Yamaguchi, M; Honjo, T			Effects of temperature, salinity and irradiance on the growth of the red tide dinoflagellate <i>Gyrodinium instriatum</i> Freudenthal et Lee	HARMFUL ALGAE			English	Article						Gyrodinium instriatum; temperature; salinity; irradiance; growth rate	DINOPHYCEAE; RAPHIDOPHYCEAE; PHYTOPLANKTON; CYST	The effects of temperature, salinity and irradiance on the growth of the red tide dinoflagellate Gyrodinium instriatum Freudenthal et Lee were examined in the laboratory. Exposed to 45 different combinations of temperature (10-30 degrees C) and salinity (0-40) under saturating irradiance, G. instriatum exhibited its maximum growth rate of 0.7 divisions/day at a combination of 25 degrees C and a salinity of 30. Optimum growth rates (>0.5 divisions/day) were observed at temperatures ranging from 20 to 30 degrees C and at salinities from 10 to 35. The organism could not grow at <= 10 degrees C. In addition, G. instriatum burst at a salinity of 0 at all temperatures, but grew at a salinity of 5 at temperatures between 20 and 25 degrees C. It is noteworthy that G. instriatum is a euryhaline organism that can live under extremely low salinity. Factorial analysis revealed that the contributions of temperature and salinity to its growth of the organism were almost equal. The irradiance at the light compensation point (I(o)) was 10.6 mu mol/(m(2) s) and the saturated irradiance for growth (I(s)) was 70 mu mol(m(2) s), which was lower than I(s) for several other harmful dinoflagellates (90-110 mu mol/(m(2) s)). (C) 2005 Elsevier B.V. All rights reserved.	Kyushu Univ, Div Bioresource & Bioenvironm Sci, Lab Fisheries Environm Sci, Fukuoka 8128581, Japan; Yosu Natl Univ, Div Ocean Syst, Dept Ocean Environm Syst Program, Yosu 550749, Jeon Num, South Korea; Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Blooms Div, Hiroshima 7390452, Japan	Kyushu University; Chonnam National University; Japan Fisheries Research & Education Agency (FRA)	Nagasoe, S (通讯作者)，Kyushu Univ, Div Bioresource & Bioenvironm Sci, Lab Fisheries Environm Sci, Fukuoka 8128581, Japan.	nagasoe@ag.kyushu-u.ac.jp	Oshima, Yuji/C-7701-2011	xiong zhi, da dao/0000-0002-7682-9611				Alverca E, 2002, EUR J PHYCOL, V37, P523, DOI 10.1017/S0967026202003955; Andersen RA, 1997, J PHYCOL, V33, P1, DOI 10.1111/j.0022-3646.1997.00001.x; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; FUKUYO Y, 1982, FUNDAMENTAL STUDIES, P205; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; Itoh K., 1987, GUIDE STUDIES RED TI, P122; Jacobson DM, 1996, J PHYCOL, V32, P279, DOI 10.1111/j.0022-3646.1996.00279.x; JIMENEZ R, 1993, DEV MAR BIO, V3, P257; Kim DI, 2004, J PLANKTON RES, V26, P61, DOI 10.1093/plankt/fbh001; KOJIMA N, 1992, REV PALAEOBOT PALYNO, V74, P239, DOI 10.1016/0034-6667(92)90009-6; LEDERMAN TC, 1981, BOT MAR, V24, P125, DOI 10.1515/botm.1981.24.3.125; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; SCHNEPF E, 1992, EUR J PROTISTOL, V28, P3, DOI 10.1016/S0932-4739(11)80315-9; SILVA ES, 1995, PHYCOLOGIA, V34, P396, DOI 10.2216/i0031-8884-34-5-396.1; SILVA ES, 1982, P 5 INT IUPAC S MYC, P216; Silva ES., 1982, MAR PHARM SCI, V2, P269, DOI [10.1515/9783110837506-015, DOI 10.1515/9783110837506-015]; Skovgaard A, 2000, J PHYCOL, V36, P1069, DOI 10.1046/j.1529-8817.2000.00009.x; TODA S, 1995, INT C EC SYST ENH TE, V1, P53; TORIUMI S, 1980, SYNOPSIS RED TIDE OR, P84; Uchida T, 1997, J PLANKTON RES, V19, P603, DOI 10.1093/plankt/19.5.603; UCHIDA T, 1995, MAR ECOL PROG SER, V118, P301, DOI 10.3354/meps118301; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Yamaguchi M, 1997, J PLANKTON RES, V19, P1167, DOI 10.1093/plankt/19.8.1167; YAMAGUCHI M, 1989, NIPPON SUISAN GAKK, V55, P2029; YAMAGUCHI M, 1991, NIPPON SUISAN GAKK, V57, P1277; Yamamoto Tamiji, 1997, Japanese Journal of Phycology, V45, P95	26	51	60	1	43	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	JAN	2006	5	1					20	25		10.1016/j.hal.2005.06.001	http://dx.doi.org/10.1016/j.hal.2005.06.001			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	004EA					2025-03-11	WOS:000234733600003
C	Alster, A; Zohary, T; Dubinsky, Z		Jones, J		Alster, Alla; Zohary, Tamar; Dubinsky, Zvy			<i>Peridinium gatunense</i> cyst type, abundance and germination in Lake Kinneret	International Association of Theoretical and Applied Limnology, Vol 29, Pt 4, Proceedings	INTERNATIONAL ASSOCIATION OF THEORETICAL AND APPLIED LIMNOLOGY - PROCEEDINGS		English	Proceedings Paper	29th Congress of the International-Association-of-Theoretical-and-Applied-Limnology	AUG 08-14, 2004	Lahti, FINLAND	Int Assoc Theoret & Appl Limnol		dinoflagellate; resting stage; cyst; excystation	SUBTROPICAL LAKE; DINOFLAGELLATE		Israel Oceanog & Limnol Res, Kinneret Limnol Lab, IL-14950 Migdal, Israel	Israel Oceanographic & Limnological Research Institute	Alster, A (通讯作者)，Israel Oceanog & Limnol Res, Kinneret Limnol Lab, POB 447, IL-14950 Migdal, Israel.							Alster A, 2006, FRESHWATER BIOL, V51, P1219, DOI 10.1111/j.1365-2427.2006.01543.x; Dale B., 1983, P69; GAMILEL H, 1985, SCAN ELECT MICROS, V4, P1649; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; Kadota H., 1984, MEM COLL AGR KYOTO U, V123, P27; POLLINGHER U, 1991, ARCH HYDROBIOL, V120, P267; POLLINGHER U, 1978, LAKE KINNERET, P271	8	3	3	0	1	E SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG	STUTTGART	JOHANNESTRASSE 3, W-7000 STUTTGART, GERMANY	0368-0770		3-510-54068-9	INT VER THEOR ANGEW			2006	29		4				2083	2086						4	Limnology; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	BFN29					2025-03-11	WOS:000243245800080
J	Head, MJ; Lewis, J; De Vernal, A				Head, MJ; Lewis, J; De Vernal, A			The cyst of the calcareous dinoflagellate <i>Scrippsiella trifida</i>:: Resolving the fossil record of its organic wall with that of <i>Alexandrium tamarense</i>	JOURNAL OF PALEONTOLOGY			English	Review							SEA-SURFACE CONDITIONS; LATITUDE MARINE ENVIRONMENTS; DINOPHYCEAE RESTING CYSTS; NORTHERN NORTH-ATLANTIC; GONYAULAX-EXCAVATA; GENUS ALEXANDRIUM; NOV DINOPHYCEAE; ICE COVER; COMB-NOV; SEDIMENTS	Scrippsiella trifida Lewis, 1991 ex Head, 1996 is a nontoxic marine calciodinelloidean dinoflagellate whose resting cyst has a distinctive wall containing large, erect, trifurcate, recurving calcareous processes that separate two organic layers. We show that the organic wall layers of living, Scrippsiella trifida cysts are resistant to acetolysis and can therefore potentially fossilize, and we report on abundant Scrippsiella trifida cysts from latest Pleistocene and early Holocene marine sediments off eastern Canada, representing the first confirmed fossil discovery of this species in the North Atlantic. A reappraisal of late Quaternary palynological records now shows that the organic remains of Scrippsiella trifida cysts have been widely misidentified as cysts of Alexandrium tamarense (Lebour. 1925) Balech, 1985, a goniodomacean (and hence noncalcareous) dinoflagellate and major cause of paralytic shellfish poisoning in humans. The morphology of these two cyst types is contrasted, and the modern and fossil distribution of Scrippsiella trifida cysts in sediments of the North Atlantic and adjacent areas is now clarified. It is apparent from this distribution that Scrippsiella trifida favors neritic environments characterized by cool winters and relatively warm (14 degrees-25 degrees C) Summers. Extremely high fluxes of S. trifida cysts in nearshore areas off Nova Scotia and southern Greenland during deglaciation and early postglacial time (14-7 ka) have no modern analog but may signal a reduction in salinity caused by meltwater discharge. fit general, the organic walls of calcareous dinoflagellate cysts are more common components of palynological assemblages than hitherto realized.	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; Univ Westminster, Sch Biosci, London W1W 6UW, England; Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	Brock University; University of Cambridge; University of Westminster; University of Quebec; University of Quebec Montreal	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	mjhead@brocku.ca; lewisjm@westminster.ac.uk; devernal.anne@uqam.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; [Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; [Anonymous], 1978, DEEP SEA DRILL PROJ; [Anonymous], 1996, IDENTIFYING MARINE D; Balech E., 1985, P33; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; 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J	Shaked, Y; de Vargas, C				Shaked, Yonathan; de Vargas, Colomban			Pelagic photosymbiosis: rDNA assessment of diversity and evolution of dinoilagellate symbionts and planktonic foraminiferal hosts	MARINE ECOLOGY PROGRESS SERIES			English	Article						symbiosis; planktonic foraminifer; dinoflagellate; open ocean; suessiales	MOLECULAR PHYLOGENY; DINOFLAGELLATE CYST; RIBOSOMAL-RNA; SYMBIODINIUM; ECOLOGY; CORALS; ZOOXANTHELLAE; DIVERSIFICATION; BIOSTRATIGRAPHY; ENDOSYMBIONTS	We present large subunit (LSU) and internal transcribed spacer (ITS) rDNA based phylogenies of symbiotic dinoflagellates retrieved from single-cell planktonic foraminifera collected around the world. All modern foraminiferal species involved in such symbiosis are included in our analyses. The pelagic symbiotic dinoflagellates form a monophyletic group sister to the Symbiodinium species complex found in coastal-benthic environments. The pelagic symbionts are descendants of free-living species and, together with the coastal-benthic Symbiodinium spp., they originated from the early Mesozoic suessiacean family represented by the extant Polarella glacialis. Out of hundreds of single planktonic foraminifera examined, 21 unique pelagic symbiont ribotypes were recognized, which could be divided into 2 main clades and 4 genetic subgroups, We observed an absence of specificity between the symbiont genetic types and the host genetic and morphological species. A few foraminifera even harbored dinoflagellates of more than one genetic subgroup. This genetic flexibility may be constrained by the fast life cycles of pelagic single-cell hosts, which acquire symbionts de novo from the ambient water at each generation. The obligatory transitional free-living stage of pelagic symbionts prior to acquisition by foraminiferal hosts may also explain their significantly lower rates of DNA substitution in comparison to their coastal-benthic relatives. We propose that the open ocean ecosystem has maintained photosymbioses involving a relatively low genetic diversity, but an extreme flexibility in the relationships between both partners, which also preserved their ancestral ability for independent life.	Rutgers State Univ, Inst Marine & Coastal Sci, New Brunswick, NJ 08901 USA; CNRS, UMR 7144, Biol Stn, F-29682 Roscoff, France	Rutgers University System; Rutgers University New Brunswick; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE)	de Vargas, C (通讯作者)，Rutgers State Univ, Inst Marine & Coastal Sci, 71 Dudley Rd, New Brunswick, NJ 08901 USA.	vargas@sb-roscoff.fr						Baker AC, 2001, NATURE, V411, P765, DOI 10.1038/35081151; Baker AC, 2003, ANNU REV ECOL EVOL S, V34, P661, DOI 10.1146/annurev.ecolsys.34.011802.132417; Baker AC, 2004, NATURE, V430, P741, DOI 10.1038/430741a; Berggren WA, 1997, MICROPALEONTOLOGY, V43, P1, DOI 10.2307/1485988; BIJMA J, 1990, J FORAMIN RES, V20, P117, DOI 10.2113/gsjfr.20.2.117; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; Buddemeier R. 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Ecol.-Prog. Ser.		2006	325						59	71		10.3354/meps325059	http://dx.doi.org/10.3354/meps325059			13	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	116LZ		Bronze			2025-03-11	WOS:000242805700005
J	Peperzak, L				Peperzak, L			Modelling vegetative growth, gamete production and encystment of dinoflagellates in batch culture	MARINE ECOLOGY PROGRESS SERIES			English	Article						dinoflagellate; vegetative growth; sexual cycle; gametes; cysts; model	DNA-SYNTHESIS CYCLES; ALEXANDRIUM-TAYLORI DINOPHYCEAE; SEXUAL REPRODUCTION; LIFE-CYCLE; RATES; POPULATIONS; HISTORY	An intriguing case of encystment of the dinoflagellate Scrippsiella lachrymosa in culture has recently been presented: cyst concentrations still increased after the abundance of the vegetative cells had decreased to very low numbers. To account for this apparent time lag, and using a model with an encystment rate equation in which vegetative growth and encystment rates were coupled, the calculated growth and encystment rates had to be 8 to 12 d(-1), values which were considered 'not biologically meaningful'. Here a new model of dinoflagellate growth and encystment is presented in which the mitotic cycle (vegetative growth) is coupled quantitatively to the sexual cycle (cyst formation) by having 4 gametes emanate from 1 vegetative cell, but without directly coupling the rates of vegetative growth and encystment. Calibrated on literature data of S. lachrymosa cultured in f/4 medium, this model satisfactorily describes motile cell (vegetative cells and gametes) and cyst development with correlations between log-transformed model and experimental data of r(2) = 0.80 (motile cells) and r(2) = 0.94 (cysts) and with typical maximum rates in the exponential growth phase of mu(cell) = 0.55 d(-1) (gross vegetative cell rate), mu(gamete+cell) = 0.38 d(-1) (net motile cell growth rate), epsilon = 0.42 d(-1) (encystment rate). All these rates declined in the stationary growth phase. Sample sonication is suggested as the cause for low motile cell concentrations in the original experiment when cyst production was high. Inorganic carbon limitation due to low inorganic carbon to nitrogen concentrations in the growth media is probably the reason why cysts in f/4 medium stopped making calcite covers in later stages of the experiment and why cyst yield in f/2 medium was not double the yield in f/4. A new method for measuring in situ encystment rates of dinoflagellate populations with a phased sexual cycle is proposed.	Koninklijk Nederlands Inst Onderzoek Zee, NL-1790 AB Den Burg, Netherlands; Rijksinst Kust Zee, NL-4330 EA Middelburg, Netherlands		Peperzak, L (通讯作者)，Koninklijk Nederlands Inst Onderzoek Zee, POB 59, NL-1790 AB Den Burg, Netherlands.	louis.peperzak@nioz.nl	Peperzak, Louis/A-2295-2009	Peperzak, Louis/0000-0003-0691-2521				ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; ANTIA AN, 1990, MAR ECOL PROG SER, V63, P273, DOI 10.3354/meps063273; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; CARPENTER EJ, 1988, MAR ECOL PROG SER, V43, P105, DOI 10.3354/meps043105; CETTA CM, 1990, J EXP MAR BIOL ECOL, V135, P69, DOI 10.1016/0022-0981(90)90199-M; CHANG J, 1990, MAR ECOL PROG SER, V65, P293, DOI 10.3354/meps065293; CHANG J, 1991, MAR ECOL PROG SER, V78, P115, DOI 10.3354/meps078115; CHANG J, 1988, MAR ECOL PROG SER, V44, P287, DOI 10.3354/meps044287; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Dale B., 1983, P69; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; GAO XP, 1989, PHYCOLOGIA, V28, P342; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garces E, 2002, LIFEHAB LIFE HIST MI; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; LEWIS J, 2002, LIFEHAB LIFE HIST MI, P49; MCDUFF RE, 1982, LIMNOL OCEANOGR, V27, P783, DOI 10.4319/lo.1982.27.4.0783; Olli K, 2004, MAR ECOL PROG SER, V273, P43, DOI 10.3354/meps273043; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; OLLI K, 2002, LIFEHAB LIFE HIST MI, P53; Peperzak L, 2000, J PLANKTON RES, V22, P2181, DOI 10.1093/plankt/22.12.2181; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; Pollingher U., 1988, P134; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; SMAYDA TJ, 1978, PHYOPLANKTON MANUAL, V6, P273; Stumm W., 2012, AQUATIC CHEM CHEM EQ; TOMAS CR, 1989, RED TIDES BIOL ENV S; van den Hoek C., 1995, Algae. An introduction to phycology; Von Stosch HA., 1973, Br Phycol J, V8, P105	31	9	9	0	4	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2006	306						143	152		10.3354/meps306143	http://dx.doi.org/10.3354/meps306143			10	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	014YQ		Bronze			2025-03-11	WOS:000235518100013
J	Streng, M; Hildebrand-Habel, T; Meier, KJS; Fensome, RA				Streng, Michael; Hildebrand-Habel, Tania; Meier, K. J. Sebastian; Fensome, Robert A.			Clarification of the systematic position of two calcareous dinoflagellate taxa belonging to the genus <i>Calciodinellum</i> (Dinophyceae, Peridiniales)	MICROPALEONTOLOGY			English	Article							CYSTS; ASSOCIATIONS; SEA		Uppsala Univ, Dept Geosci, S-75236 Uppsala, Sweden; Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada	Uppsala University; University of Oslo; Natural History Museum London; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Streng, M (通讯作者)，Uppsala Univ, Dept Geosci, Villavagen 16, S-75236 Uppsala, Sweden.	michael.streng@geo.uu.se	Hildebrand-Habel, Tania/F-3590-2011; Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. Sebastian/0000-0002-3918-4092				Bukry D., 1969, Tulane Studies in Geology, V7, P131; BUTSCHLI O, 1885, KLASSEN ORDNUNGEN TH, V1, P865; DEFLANDRE G, 1947, CR HEBD ACAD SCI, V224, P1781; Deflandre G., 1949, BOTANISTE, V34, P191; EHRENBERG CG, 1931, SYMBOLAE PHYS ICONES; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FENSOME RA, 2004, AASP CONTRIBUTION SE, V42; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Greuter W., 2000, International Code of Botanical Nomenclature (St Louis Code). Regnum Vegetabile, V138; HAECKEL F, 1894, SYSTEMATISCHE PHYLOG, V1; Hildebrand-Habel T, 1999, REV PALAEOBOT PALYNO, V106, P57, DOI 10.1016/S0034-6667(98)00079-7; Hildebrand-Habel T, 2003, PALAEOGEOGR PALAEOCL, V197, P293, DOI 10.1016/S0031-0182(03)00470-X; Kamptner E., 1963, Annalen des Naturhistorischen Museums in Wien, V66, P139; KARWATH B, 2000, BERICHTE FACHBEREICH, V152; Keupp H., 1989, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V106, P207; Keupp H., 1991, P267; KOHRING R, 1993, BERLINER GEOWISSENSC, V6; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; Pascher A., 1914, Berlin Ber D bot Ges, V32; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Streng M, 2002, J PALEONTOL, V76, P397, DOI 10.1666/0022-3360(2002)076<0397:ROTGSK>2.0.CO;2; Streng Michael, 2004, Journal of Nannoplankton Research, V26, P13; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2	23	2	3	0	0	MICROPALEONTOLOGY PRESS	NEW YORK	AMER MUSEUM NAT HISTORY 79TH ST AT CENTRAL PARK WEST, NEW YORK, NY 10024 USA	0026-2803			MICROPALEONTOLOGY	Micropaleontology		2006	52	2					189	192		10.2113/gsmicropal.52.2.189	http://dx.doi.org/10.2113/gsmicropal.52.2.189			4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	065QR					2025-03-11	WOS:000239174900004
J	Fensome, RA; Guerstein, GR; Williams, GL				Fensome, Robert A.; Guerstein, G. Raquel; Williams, Graham L.			New insights on the Paleogene dinoflagellate cyst genera <i>Enneadocysta</i> and <i>Licracysta</i> gen. nov based on material from offshore eastern Canada and southern Argentina	MICROPALEONTOLOGY			English	Article								Enneadocysta is a biostratigraphically important Paleogene dinoflagellate cyst genus. Its original interpretation as a partiform gonyaulacoid (thus belonging to the gonyaulacalean suborder Cladopyxiineae) was based on the presence of two antapical processes. Another Paleogene genus, Areosphaeridium, is similar, at least superficially, to Enneadocysta, but has a single antapical process, placing it in the sexiform gonyaulacalean suborder Gonyaulacineae. The morphology of a new species of Enneadocysta from offshore eastern Canada, Enneadocysta magna, shows that the two antapical processes of the genus (unlike processes reflecting other plate series) are penitabular, not mesotabular, and indicates that the genus is gonyaulacinean, not cladopyxiinean. This new interpretation, as well as new material from southern Argentina, confirms the generic assignment of the Southern Hemisphere species Enneadocysta dictyostila (emended) and a new species, Enneadocysta brevistila. A new genus and species, Licracysta corymbus, from offshore eastern Canada is intermediate in morphology between Enneadocysta and Cleislosphaeridium and strongly suggests an assignment for all three genera to the gonyaulacinean family Areoligeraceae. The new combination Licracysta? semicirculata is questionably proposed, and the descriptive terms licrate, dolabrate, entire clypeate, ragged clypeate. intratabular, mesotabular, obtabular, contabular and nontabular are either proposed as new or reviewed.	Geol Survey Canada, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; Univ Nacl Sur, Lab Palinol, Dept Geol, RA-8000 Bahia Blanca, Argentina	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Fensome, RA (通讯作者)，Geol Survey Canada, Nat Resources Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	rfensome@nrcan.gc.ca						[Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1971, P 2 PLANKT C; [Anonymous], 1885, HG BRONNS KLASSEN OR; ARCHANGELSKY S, 1969, Ameghiniana, V6, P181; ARCHANGELSKY S, 1969, AMEGHINIANA, V5, P406; Archangelsky S., 1971, Revista del Museo de la Plata, Seccion Paleontologia, V36, P1; Brinkhuis H., 2003, P OCEAN DRILLING PRO; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; BUJAK JP, 1976, MAR MICROPALEONTOL, V1, P101, DOI 10.1016/0377-8398(76)90007-4; COCOZZA CD, 1992, ANTARCT SCI, V4, P355, DOI 10.1017/S0954102092000506; Cookson I. C., 1965, Proceedings of the Royal Society of Victoria, V79, P119; COOKSON ISABEL C., 1967, MICROPALEONTOLOGY [NEW YORK], V13, P204, DOI 10.2307/1484671; Cranwell L.M, 1964, Grana Palynol., V5, P397; Davey JJ., 1966, B BR MUS NAT HIS G, P157; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; Eaton GL, 2001, NEUES JAHRB GEOL P-A, V219, P171, DOI 10.1127/njgpa/219/2001/171; EHRENBERG C.G., 1838, KONIGLICH AKAD WISSE, V1, P109; Eisenack A., 1972, Katalog der Fossilen Dinoflagellaten, Hystrichospharen und Verwandten Mikrofossilien, VII; EISENACK A., 1963, NEUES JB F R GEOLOGI, V118, P260; Evitt W. R, 1977, Papers Geological Survey Canada, V76, P1; Evitt W. R., 1961, Micropaleontology, V7, P385, DOI 10.2307/1484378; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P298, DOI 10.1073/pnas.49.3.298; EVITT WR, 1985, SPOROPOLLENIN DINOFA; EVITT WR, 1972, GEOSCIENCE MAN, V4, P130; FASOLA A, 1969, Ameghiniana, V6, P3; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; FENSOME RA, 2001, MRESGPAL102001RAF; Gerlach E., 1961, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V112, P143; GOODMAN DK, 1983, INITIAL REP DEEP SEA, V71, P859; Guerstein GR, 1998, PALAEONTOLOGY, V41, P23; ISLAM M A, 1983, Palynology, V7, P71; Klumpp B., 1953, Palaeontographica A, V103, P377; Lejeune-Carpentier M., 1938, Annales de la Societe gdologique de Belgique, V62, pB163; Levy Richard H., 2000, Antarctic Research Series, V76, P183; Menendez C. A., 1965, Ameghiniana, V4, P7; Morgenroth P., 1966, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V127, P1; Olivero EB, 1999, AAPG BULL, V83, P295; Pascher A., 1914, Berlin Ber D bot Ges, V32; Pothe de Baldis E.D., 1966, AMEGHINIANA, V4, P219; Röhl U, 2004, GEOPH MONOG SERIES, V151, P127; SARJEANT W A S, 1981, Meyniana, V33, P97; SARJEANT WAS, 1982, CAN J BOT, V60, P922, DOI 10.1139/b82-119; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; VONSTEIN FR, 1883, ORGANISMUS INFUSION; Williams G.L., 2000, CONTRIBUTION SERIES, V37, P370; Williams GL., 2005, GEOLOGICAL SURVEY CA; WILSON GRAEME J., 1967, NZ J BOT, V5, P57	51	16	16	0	0	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2006	52	5					385	410		10.2113/gsmicropal.52.5.385	http://dx.doi.org/10.2113/gsmicropal.52.5.385			26	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	141TS		Green Published			2025-03-11	WOS:000244602300001
J	Sancay, RH; Bati, Z; Edwards, LE; Ertug, KI				Hayrettin Sancay, R.; Bati, Zuhtu; Edwards, Lucy E.; Ertug, Kaya I.			A new species of <i>Pentadinium</i> from eastern Anatolia, Turkey, <i>Pentadinium galileoi</i>	MICROPALEONTOLOGY			English	Article								The new gonyaulacoid dinoflagellate Pentadinium galileoi Sancay et al., sp. nov. from the Oligocene-Lower Miocene sediments of Eastern Anatolia has been identified. It is spherical, chordate with prominant discoidal cingulum and distally furcate apical, sulcal, and antapical processes. It has a type P (3 '') archeopyle, and periarcheopyle is larger than endoarcheopyle. Tabulation is distinct and it has a formula of 1pr, 3-4', 6 '',6c, 6''', 1p, 1''''. Wall structure is granular in intraplate areas, and it has gonal spines at apex, posterior intercalary, and antapex. Processes at gonal positions may be on a variably developed antapical 'skirt' formed by extended septa (2-3 pm), minute bifurcate spines intergonally and along cingulum at plate intersections. Periphragm and endophragm appressed except at cingular area and at septa. The size of the cysts ranges between 73-89 mu m with an avarage of 84 mu m.	Turkish Petr Corp, Res Ctr, Ankara, Turkey; US Geol Survey, Reston, VA 22092 USA	Ministry of Energy & Natural Resources - Turkey; Turkish Petroleum Corporation (TPAO); United States Department of the Interior; United States Geological Survey	Sancay, RH (通讯作者)，Turkish Petr Corp, Res Ctr, Ankara, Turkey.	hsancay@petrol.tpao.gov.tr; bati@petrol.tpao.gov.tr; leedwards@usgs.gov; kertug@petrol.tpao.gov.tr						Allen CR, 1969, ACTIVE FAULTING NO T, V32s; Alptekin O, 1973, THESIS NEW MEXICO I; Arpat E., 1972, Bull. Miner. Res. Expl., V78, P44; BATI Z, UNPUB MICROPALEONTOL; BUTSCHLI O, BRONNS KLASSEN ORDUN, P865; EDWARDS L E, 1982, Palynology, V6, P105; Fensome R.A., 1993, Micropaleontology Press Special Paper; Gerlach E., 1961, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V112, P143; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; MCKENZIE D, 1976, EARTH PLANET SC LETT, V29, P189, DOI 10.1016/0012-821X(76)90038-8; Pascher A., 1914, Berlin Ber D bot Ges, V32; Sancay RH, 2006, TURK J EARTH SCI, V15, P259; SANCAY RH, 2005, THESIS MIDDLE E TECH; Seng├Ar A.M.C., 1979, J GEOL SOC LONDON, V136, P269, DOI [10.1144/gsjgs.136.3.0269, DOI 10.1144/GSJGS.136.3.0269]; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; Strauss Christoph, 1992, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V73, P159; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; TCHALENKO JS, 1977, REV GEOGR PHYS GEOL, V19, P189; von Benedek P.N., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V162, P265	19	4	4	0	1	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2006	52	6					537	543		10.2113/gsmicropal.52.6.537	http://dx.doi.org/10.2113/gsmicropal.52.6.537			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	165OG					2025-03-11	WOS:000246314200003
J	Backhouse, J				Backhouse, John			Albian (Lower Cretaceous) dinoflagellate cyst biostratigraphy of the lower Gearle Siltstone, Southern Carnarvon Basin, Western Australia	PALYNOLOGY			English	Article						Lower Cretaceous; Albian; dinoflagellate cysts; biostratigraphy; paleoecology; Western Australia		Rich and diverse assemblages of dinoflagellate cysts were recovered from the Gearle Siltstone in the Boologooro-1 stratigraphic well, Southern Carnarvon Basin, Western Australia. The cored interval through the Winning Group is proposed as a reference interval for the Canninginopsis denticulata, Endoceratium ludbrookiae, Dioxya armata and Xenascus asperatus dinoflagellate cyst zones of the Australian dinoflagellate cyst zonal scheme. The ranges of sixty-three dinoflagellate cyst species are documented in detail over this interval. Apart from the bioevents that define the widely-used dinoflagellate cyst subzones, the highest occurrences of Endoceratium turneri, Craspedodinium indistinctum and Litosphaeridium arundum, and the lowest occurrences of Nematosphaeropsis densiradiata, Canninginopsis denticulata, Leberidocysta chlamydata, Aptea? sp. cf. Aptea polymorpha, Litosphaeridium siphoniphorum, Balcattia cirribarbata and Stephodinium australicum are recognized as potential biostratigraphic datums in the Southern Camarvon Basin. Species diversity increased in the highest Canninginopsis denticulata Zone at approximately the horizon where Diconodinium spp. become dominant. Foraminiferal data indicate the interval from 361.15 m to 312.12 m is marginally inner neritic and corresponds with an interval of abundant Diconodinium spp., and fewer Spiniferites spp. Diversity increased in the Xenascus asperatus Zone with an increase in Spiniferites spp., and a shift to middle neritic paleobathymetry. The age of the top of the Xenascus asperatus Zone is constrained by calcareous nannofossils and dinoflagellate cyst correlations to the latest Albian, or possibly the early Cenomanian. The age of the base of the Canninginopsis denticulata Zone is constrained by dinoflagellate cyst and foraminiferal data to the early Albian, above the earliest Albian. One new species, Chlamydophorella haigii, is erected and aspects of several other dinoflagellate cyst taxa are reviewed.	Univ Western Australia, Sch Earth & Geog Sci, Crawley, WA 6009, Australia	University of Western Australia	Backhouse, J (通讯作者)，Univ Western Australia, Sch Earth & Geog Sci, 35 Stirling Highway, Crawley, WA 6009, Australia.	jbackhou@segs.uwa.edu.au						BURGER D, 1980, B BUREAU MINERAL RES, V189; Burger D., 1989, AUSTR PHANEROZOIC TI; Cookson I. C., 1962, Micropaleontology, V8, P485, DOI 10.2307/1484681; COOKSON I C, 1968, Journal of the Royal Society of Western Australia, V51, P110; Cookson I. C., 1962, Proceedings of the Royal Society of Victoria, V75, P269; COOKSON I C, 1982, Palaeontographica Abteilung B Palaeophytologie, V184, P23; COOKSON I C, 1970, Proceedings of the Royal Society of Victoria, V83, P137; Cookson I. C., 1961, PALAEONTOLOGY, V3, P485; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; COOKSON IC, 1979, NEUES JB GEOLOGIE PA, P77; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; COOKSON ISABEL C., 1962, JOUR ROY SOC WESTERN AUSTRALIA, V45, P97; Costa L. I., 1992, BRIT MICROPALAEONTOL, P99; DAVEY RJ, 1971, VERHANDELINGEN KONIN, V26; DAVEY RJ, 1999, MEMOIR GEOLOGICAL SU, V17; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Eisenack A., 1960, P R SOC VIC, V72, P1; Fiet N, 2001, CRETACEOUS RES, V22, P63, DOI 10.1006/cres.2000.0237; Foster C, 2001, MEMOIR ASS AUSTRALAS, V24, pi; Haig D.W., 2004, Record 2004/4; Haig DW, 1996, ALCHERINGA, V20, P41, DOI 10.1080/03115519608619222; Hardenbol J., 1998, SEPM SPECIAL PUBLICA; Helby R., 2004, GEOSCIENCE AUSTR PUB; HELBY R, 1974, UNPUB PALYNOLOGICAL; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Helenes Javier, 1997, Palynology, V21, P173; HOCKING RM, 1987, B GEOLOGICAL SURVEY, V133; Morgan R., 1977, Palynology, V1, P123; MORGAN R, 1980, MEMOIR GEOLOGICAL SU, V18; MORGAN R, 1980, 4 INT PAL C LUCKN, V2, P409; MORGAN R, 1977, Q NOTES GEOLOGICAL S, V28, P10; MORGAN R, 1975, J PROC R SOC N S W, V108, P157; NORVICK MS, 1975, B BUREAU MINERAL RES, V151; PLAYFORD PE, 1975, MEMOIR GEOLOGICAL SU, V2, P223; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P225; Riding JB, 2002, CRETACEOUS RES, V23, P739, DOI 10.1006/cres.2002.1024; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P101; Tocher BA, 1996, J MICROPALAEONTOL, V15, P55, DOI 10.1144/jm.15.1.55; [No title captured]	39	18	20	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2006	30						43	68		10.2113/gspalynol.30.1.43	http://dx.doi.org/10.2113/gspalynol.30.1.43			26	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400003
J	Riding, JB; Kyffin-Hughes, JE				Riding, James B.; Kyffin-Hughes, Jane E.			Further testing of a non-acid palynological preparation procedure	PALYNOLOGY			English	Article						palynomorphs; preparation techniques; Ordovician; Carboniferous; Jurassic; Paleogene; UK	DINOFLAGELLATE CYSTS; MIDDLE; PALYNOMORPHS	The extraction of palynomorphs from sedimentary rocks and unconsolidated sediments has traditionally used hydrochloric acid (HCl) and hydrofluoric acid (HF) to remove the matrix by dissolution. The use of these, and other, acids in palynological preparation requires significant laboratory infrastructure, and may produce hazardous and potentially environmentally damaging waste. An effective technique of palynomorph preparation using sodium hexametaphosphate [(NaPO3)(6)] was recently developed. This technique was initially demonstrated on a suite of samples of Early Jurassic to Quaternary age. In this study, non-acid preparation techniques were tested on 11 samples of Ordovician, Carboniferous, Jurassic and Paleogene age from the UK. In four of the six case studies described herein, the rock was prepared quantitatively using both the traditional mineral acid technique and the (NaPO3)(6) procedure. In the Carboniferous case study, the two samples were prepared quantitatively using HCl/HF, (NaPO3)(6), and hydrogen peroxide (H2O2). In the quantitative preparations, the concentrations of palynomorphs can be directly compared. Two non-quantitative case studies were undertaken using (NaPO3)(6) only, in order to demonstrate that this method is of practical utility. The (NaPO3)(6) and H2O2 methods generally proved to be as effective as the mineral acid procedure. However the results from the three Paleozoic samples proved somewhat variable. The Early Ordovician sample 1 did not break down in (NaPO3)(6), and consequently the palynomorph yield from this sample was extremely poor, compared to the acid preparation. Two Lower Carboniferous samples were prepared using all three methods. In sample 2, all the methods were effective, although the H2O2 technique proved less effective than those using mineral acids and (NaPO3)(6). In this sample, both the non-acid methods produced palynomorph assemblages cleaner of extraneous woody material than the residue produced by the acid digestion method. By contrast, in Carboniferous sample 3, the acid preparation was far better than those from the two non-acid preparations. It appears that mudrocks which are relatively indurated are not consistently disaggregated using (NaPO3)(6) and/or (HO2)-O-2. It may be possible to adapt these non-acid techniques so that they are more efficient on these relatively hard lithotypes. The samples would need to be softened prior to treatment with (NaPO3)(6) and/or H2O2,. Even on relatively hard lithotypes, some palynomorphs were extracted using (NaPO3)(6) and H2O2. This confirms that non-acid methods can be used on harder rocks if a preliminary age assessment is required and/or the full laboratory facilities are unavailable. The (NaPO3)(6) technique proved extremely effective in the two quantitative Jurassic case studies. These were on the Oxford Clay and Kimmeridge Clay formations (Callovian-Oxfordian and Kimmeridgian respectively). In samples 4, 6 and 7, both methods gave similar palynomorph yields. However in sample 5 from the Oxford Clay Formation, the acid preparation proved less palynologically productive than the material prepared using (NaPO3)(6). Palynomorph diversity was also higher in Oxford Clay Formation samples 4 and 5, prepared with (NaPO3)(6). In samples 6 and 7 from the Kimmeridge Clay Formation, the palynomorph diversity, preservation and yield were closely comparable. However, the HCl/HF preparations proved extremely rich in amorphous organic material as compared to the (NaPO3)(6) slides. It therefore appears that (NaPO3)(6) is effective at disaggregating amorphorgen in addition to clay minerals. This means that this reagent may be used as an alternative to nitric acid (HNO3) and other strong oxidizing agents for cleaning organic residues of amorphous organic material. More studies should be done using (NaPO3)6 to prove its effectiveness in dispersing amorphogen. The two non-quantitative case studies prepared only using (NaPO3)(6) were also successful. Three samples (8-10) of Early, Mid and Late Jurassic age and sample 11 of Paleogene age all produced abundant, well-preserved and diverse palynofloras. This indicates that the (NaPO3)(6) procedure can prepare palynomorph assemblages from Mesozoic and Cenozoic mudrocks as effectively as the HCl/HF procedure.	British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; jeky@bgs.ac.uk						[Anonymous], 334G US GEOL SURV PR; Barss M. S., 1973, 7326 GEOL SURV CAN; BRADSHAW MJ, 1982, GEOL MAG, V119, P113, DOI 10.1017/S0016756800025826; Bujak J. P, 1980, DINOFLAGELLATE CYSTS; CLAYTON G, 1977, CARBONIFEROUS MIOSPO; Cox B.M., 1981, Report of the Institute of Geological Sciences, V80/4; Downie C., 1958, Proceedings of the Yorkshire Geological Society, V31, P331; EATON G L, 1976, Bulletin of the British Museum (Natural History) Geology, V26, P227; FENSOME RA, 2004, CONTRIBUTIONS AM ASS, V42; FENSOME RA, 1990, CONTRIBUTIONS AM ASS, V25; FENTON J P G, 1987, Pollen et Spores, V29, P427; Fisher O, 1862, Q J GEOL SOC LOND, V18, P65, DOI 10.1144/GSL.JGS.1862.018.01-02.18; Fortey R.A., 2000, 24 GEOL SOC LOND; Gelsthorpe DN, 2002, J MICROPALAEONTOL, V21, P81, DOI 10.1144/jm.21.1.81; Green OR., 2001, MANUAL PRACTICAL LAB, P288; Green OR., 2001, MANUAL PRACTICAL LAB, P256; Herngreen G F W, 1983, NPD B, V2, P13; Hopkins Jennifer A., 2002, Palynology, V26, P167, DOI 10.2113/0260167; Palliani Raffaella Bucefalo, 2003, Palynology, V27, P179, DOI 10.2113/27.1.179; Palliani RB, 2002, MAR MICROPALEONTOL, V46, P223; PHIPPS D, 1984, 11 U QUEENSL DEP GEO; Powell A.J., 1992, P155; Prigmore J.K., 1999, GEOLOGICAL CONSERVAT, V18, P97; RASUL S M, 1974, Palaeontology (Oxford), V17, P41; RASUL S M, 1976, Micropaleontology (New York), V22, P479, DOI 10.2307/1485175; RASUL S M, 1979, Palynology, V3, P53; Riding J.B., 1992, P7; Riding J.B., 1983, Journal of Micropalaeontology, V2, P47; Riding J.B., 1982, Journal of Micropalaeontology, V1, P13; RIDING J B, 1988, Palynology, V12, P65; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding J.B., 1999, AM ASS STRATIGRAPHIC, V36; Riding JB, 2005, PALYNOLOGY, V29, P87, DOI 10.2113/29.1.87; Riding James B., 2004, Revista Brasileira de Paleontologia, V7, P13; Riding JB, 2006, J MICROPALAEONTOL, V25, P35, DOI 10.1144/jm.25.1.35; Riding James B., 1991, Palynology, V15, P115; Riding JB, 1997, SCOT J GEOL, V33, P59, DOI 10.1144/sjg33010059; RIDING JB, 1985, REV PALAEOBOT PALYNO, V45, P149, DOI 10.1016/0034-6667(85)90068-5; RIDING JB, 2005, IR0502 BRIT GEOL SUR; Stephenson M, 2002, SCOT J GEOL, V38, P93, DOI 10.1144/sjg38020093; Williams G, 2005, MICROPALEAEONTOLOGIC, P219; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; [No title captured]	43	24	24	0	9	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2006	30						69	87		10.2113/gspalynol.30.1.69	http://dx.doi.org/10.2113/gspalynol.30.1.69			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400004
J	Warny, S; Wrenn, JH; Bart, PJ; Askin, R				Warny, Sophie; Wrenn, John H.; Bart, Philip J.; Askin, Rosemary			Palynology of the NBP03-01A transect in the Northern Basin, Western Ross Sea, Antarctica: A Late Pliocene record	PALYNOLOGY			English	Article						paleoecology; biostratigraphy; Antarctica; Ross Sea; Northern Basin; Neogene	TRANSANTARCTIC MOUNTAINS; DINOFLAGELLATE CYSTS; SIRIUS GROUP; NOTHOFAGUS; LEAVES; SEDIMENTS; NEOGENE; OCEAN	Fifty-seven samples taken from ten piston cores collected along a transect off the continental margin of the Northern Basin, Ross Sea, Antarctica were analyzed for palynomorphs. Moderately diverse assemblages of marine microplankton and terrestrial palynomorphs were recovered. The palynomorph assemblages have been subdivided into two main groups: the in-situ flora (including acritarchs, dinoflagellate cysts, leiospheres and prasinophyte algae mainly composed of cymatiosphaerids), and the reworked flora (including dinoflagellate cysts, pollen and spores). The leiospheres are the most abundant palynomorphs. This prominence in the relative abundance of leiospheres has been reported as typical of assemblages found today at the limit between seasonal and pack ice in the Arctic. In-situ dinoflagellate cysts are sparse. They are mainly represented by Lejeunecysta, which, based on species similarities to those from Cape Roberts, are believed to be of Oligocene to Pliocene age. All other dinoflagellate cysts recovered are the result of reworking from Eocene to Oligocene sediments. Reworked spores and pollen comprise the second most abundant group. They are of moderate diversity and include an Eocene or older assemblage of Nothofagidites, Podocarpaceae and Proteaceae. Other taxa are representative of warmer rainforest vegetation, with Oligocene and Neogene taxa that include representatives of woodland to herbaceous/low shrubby tundra vegetation growing in colder subpolar climates. These assemblages indicate either different periods of deposition or reworking from diverse sources. Through seismic correlation and diatom analysis, the sediments are believed to be Late Pliocene in age. On this basis, it is postulated that the major glacial advance, RSU 2 of Brancolini et al. (1995) or Unconformity 10 (U 10) of Bart et al. (2000), occurred before 2.3 Ma, which is the oldest age of in-situ species recovered in units above U 10. As both terrestrial and marine reworked taxa include assemblages of Eocene to Oligocene age, it is assumed that those reworked components were yielded from a single source; most probably Eocene to Oligocene shallow marine strata eroded and transported from the area of Ross Island to the shelf margin through ice streams located in the Drygalsky and Joides basins.	Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University	Warny, S (通讯作者)，Louisiana State Univ, Museum Nat Sci, 119 Foster Hall, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X				[Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Askin R A., 2000, Terra Antarctica, V7, P493; Askin R.A., 1992, ANTARCTIC PALEOENVIR, P61; Askin R A., 2000, AGU Ant Res Ser, V76, P161, DOI DOI 10.1029/AR076P0161; BARROW CJ, 1983, BRIT ANTARCTIC SURVE, V58, P15; Bart PJ, 2000, MAR GEOL, V166, P31, DOI 10.1016/S0025-3227(00)00006-2; Boros A., 1993, An atlas of recent European Bryophyte spores; Brancolini G., 1995, GEOLOGY SEISMIC STRA, P209; Fensome RA, 2004, CONTRIBUTIONS SERIES, V42; Fleming RF, 1996, MAR MICROPALEONTOL, V27, P227, DOI 10.1016/0377-8398(95)00062-3; Francis JE, 1996, PALAIOS, V11, P389, DOI 10.2307/3515248; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; HAMILTON WB, 1972, US GEOLOGICAL SURVEY; Hannah M J., 1998, Terra Antarctica, V5, P527; Hannah MJ, 2006, PALAEOGEOGR PALAEOCL, V231, P120, DOI 10.1016/j.palaeo.2005.07.029; HANNAH MJ, 2000, 1999 VICT U WELL SCH, P59; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Hayes D.E., 1975, INITIAL REPORTS DEEP, V28, P919, DOI DOI 10.2973/DSDP.PROC.28.136.1975; Hill RS, 1996, REV PALAEOBOT PALYNO, V94, P11, DOI 10.1016/S0034-6667(96)00003-6; HILL RS, 1993, ANTAR RES S, V60, P67; Ishman Scott E., 1992, Antarctic Research Series, V56, P327; Kemp E.M., 1975, Initial Rep Deep Sea Drilling Project, V28, P599, DOI 10.2973/dsdp.proc.28.116.1975; Levy Richard H., 2000, Antarctic Research Series, V76, P183; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; Mildenhall D.C., 1984, NZ GEOLOGICAL SURVEY, V51; Mudie P.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P587, DOI 10.2973/odp.proc.sr.104.174.1989; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; MUDIE PJ, 1986, GEOL ASS CAN ANN M P, V11, P105; Piasecki S, 2003, MAR PETROL GEOL, V20, P1075, DOI 10.1016/S0264-8172(02)00089-2; POSPELOVA V, 2002, GEOL SOC AM ANN M AB, V34, P384; Raine J.I., 2001, TERRA ANTARTICA, V7, P389; Raine J.I., 1998, Terra Antarctica, V5, P539; Savage M.L., 1983, ANTARCTIC EARTH SCI, P555; Troedson AL, 2002, J SEDIMENT RES, V72, P510, DOI 10.1306/110601720510; TRUSWELL EM, 1984, MAR GEOL, V59, P187, DOI 10.1016/0025-3227(84)90093-8; Warny SA, 2003, PALAEOGEOGR PALAEOCL, V202, P59, DOI 10.1016/S0031-0182(03)00615-1; WILSON G J, 1968, New Zealand Journal of Marine and Freshwater Research, V2, P381; Wrenn J H., 1998, Terra Antarctica, V5, P553; WRENN JH, 2001, AM ASS STRAT PAL 34	41	19	23	0	5	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2006	30						151	182						32	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400009
J	Lucas-Clark, J				Lucas-Clark, Joyce			Small peridinioid dinoflagellate cysts from the Paleocene of South Carolina, USA	PALYNOLOGY			English	Article						dinoflagellate cysts; Paleocene; South Carolina; taxonomy; biostratigraphy	CRETACEOUS-TERTIARY BOUNDARY; STRATIGRAPHY; ASSEMBLAGES; PALYNOLOGY; OLIGOCENE; GEORGIA; ISLAND	Small peridinioid dinoflagellate cysts are abundant in Paleocene strata underlying the Savannah River Site and surrounding area of South Carolina, U.S.A. They are thin-walled and light colored, have one apical and two antapical horns, and show a high degree of intraspecific variability. They occur in low diversity assemblages. The samples in this study are from three lithostratigraphic units, the lower Ellenton, upper Ellenton, and Snapp formations. Some of the species are useful stratigraphic markers in the Paleocene strata of this area. Paleoenvironments include upper delta plain, lower delta plain, and shallow clastic shelf; some may represent fresh or brackish water environments. All species studied belong to the family Peridiniaceae and are assigned to eight genera. These are Alterbidinium, Arvalidinium, Deflandrea, ?Isabelidinium, Phthanoperidinium, Senegalinium, Spinidinium, and Vozzhennikovia. The seven new species described here are Alterbidinium ellentonense, Arvalidinium cristatum, Deflandrea lucyedwardsiae, Phthanoperidinium paleocenicum, Senegalinium pallidum, Senegalinium simplex, and Spinidinium bellum.	Clark Geol Serv, Fremont, CA 94536 USA		Lucas-Clark, J (通讯作者)，Clark Geol Serv, 1023 Old Canyon Rd, Fremont, CA 94536 USA.	jluclark@comcast.net						AADLAND RK, 1995, 5 STAT S CAR DEP NAT; [Anonymous], 1978, ANALYSES PREPLEISTOC; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; ASKIN RA, 1991, J S AM EARTH SCI, V4, P99, DOI 10.1016/0895-9811(91)90021-C; BENEDEK PN, 1974, NEUES JB GEOLOGIE PA, P385; Benson D.G. Jr., 1976, Tulane Stud Geol Paleont, V12, P169; BRIDEAUX WW, 1976, 761B GEOL SURV CAN, P251; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; CHAROLLAIS J, 1975, Geologie Alpine, V51, P25; *CLARK GEOL SERV, 1986, UNPUB; COCOZZA CD, 1992, ANTARCT SCI, V4, P355, DOI 10.1017/S0954102092000506; Cookson I. C., 1965, Proceedings of the Royal Society of Victoria, V79, P139; Cookson I.C., 1967, Proceeding of the Royal Society of Victoria, V80, P131; De Coninck J., 1980, Bull. Soc. Belge Geolog., V89, P201; De Coninck J., 1990, B SOC BELG GEOL, V97, P287; DECONINCK J, 1986, 224 SERV GEOL BELG; DRUGG W.S., 1967, PALAEONTOGRAPHICA B, V120, P1; Drugg W. S., 1975, AM ASS STRATIGRAPHIC, V4, P73; DUCHENE RJ, 1987, CAHIERS MICROPALEONT, V2, P148; Edwards L. E, 2001, Professional Paper 1603; Edwards L.E., 1997, 97145 US GEOL SURV; Edwards LE, 1998, T AM PHILOS SOC, V88, P28, DOI 10.2307/1006669; EDWARDS LE, 1980, FIELD TRIP GUIDEBOOK, V2, P385; EDWARDS LE, 2002, 4 BALD HEAD ISL C CO, V16; EDWARDS LE, 1984, AM ASS STRATIGR 1017, P137; EDWARDS LE, 1989, GEOLOGY PALEONTOLOGY, pC1; Edwards Lucy E., 2001, U S Geological Survey Professional Paper, V1603, pG1; ELBEIALY SY, 1990, J AFR EARTH SCI, V11, P291, DOI 10.1016/0899-5362(90)90007-2; Fallaw W.C., 1995, Southeastern Geology, V35, P21; Falls W.F., 1997, SOUTHEAST GEOL, V36, P153; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FIRTH J V, 1987, Palynology, V11, P199; FIRTH JV, 1993, REV PALAEOBOT PALYNO, V79, P179, DOI 10.1016/0034-6667(93)90022-M; Firth JV, 1998, MAR MICROPALEONTOL, V34, P1, DOI 10.1016/S0377-8398(97)00046-7; GAMERRO J C, 1981, Revista Espanola de Micropaleontologia, V13, P119; GRUASCAVAGNETTO C, 1972, REV MICROPALEONTOL, V15, P63; HARGROVE DC, 1977, SEDIMENT GEOL, V108, P121; HEILMANNCLAUSEN C, 1985, DANMARKS GEOLOGISKE, V7; HUDDLESTUN PF, 1996, GEORGIA GEOLOGIC SUR, V95; KOTHE A, 1991, GEOLOGISCHES JB A, V1, P3; KURITA H, 1994, REV PALAEOBOT PALYNO, V84, P129, DOI 10.1016/0034-6667(94)90047-7; Kurita H., 1994, Geological Survey of Canada Bulletin, V479, P67; Kurita Hiroshi, 1995, Palynology, V19, P119; Lentin J.K., 1989, American Association of Stratigraphic Palynologists, Contributions Series, V20; LENTIN JK, 1976, BR7516 BEDF I OC; LENTIN JK, 1977, BIR778 BEDF I OC; LENTIN JK, 1990, AM ASS STRATIGRAPHIC, V23; LUCASCLARK J, 1988, SIGNIFICANCE DISTRIB, V33; MARKHEINECKE U, 1992, PALAEONTOGR ABT B, V227, P1; May F. E, 1980, PALAEONTOGR ABT B, V172, P1; MAY FE, 1971, THESIS STANFORD U CA; Mohr B.A.R., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P595, DOI 10.2973/odp.proc.sr.113.140.1990; MOSHKOVITZ S, 1993, MICROPALEONTOLOGY, V39, P167, DOI 10.2307/1485838; OLTZ JR D. F., 1969, PALAEONTOGRAPHICA  B, V128, P90; Powell A.J., 1992, BRIT MICROPALAEONTOL; Prevot L, 1979, SCI GEOLOGIQUES B, V32, DOI DOI 10.3406/SGEOL.1979.1556; PROWELL DC, 1985, US GEOLOGICAL SURV A, V160, P63; Quattrocchio ME, 2003, AMEGHINIANA, V40, P129; SIPLE GE, 1967, 1841 US GEOL SURV; SLOAN E, 1908, B STATE COMMISSION C, V2; STANLEY EDWARD A., 1965, BULL AMER PALEONTOL, V49, P179; STONE J F, 1973, Bulletins of American Paleontology, V64, P1; Stover LE., 1973, SPECIAL PUBLICATIONS, V4, P167; Van Pelt RS, 2000, T GEOBIOL, V15, P407; VANPELT RS, 2001, P 9 INT PAL C HOUST, P161; WHITNEY BL, 1984, CRETACEOUS TERTIARY, P123; Williams G.L., 1985, P847; Williams G.L., 1975, GEOL SURV CAN BULL, V236, P1; Wilson G.J., 1988, NZ GEOLOGICAL SURVEY, V57; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321; Zaitzeff J.B, 1970, GSA SPEC PAP, V127, P341	72	9	10	0	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2006	30						183	210		10.2113/gspalynol.30.1.183	http://dx.doi.org/10.2113/gspalynol.30.1.183			28	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400010
J	Antolinez, H; Oboh-Ikuenobe, FE				Antolinez, Herman; Oboh-Ikuenobe, Francisca E.			Refinement of Early Paleogene biostratigraphy in West Africa using dinoflagellate cysts from Nigeria and ODP Hole 959D (Leg 159)	PALYNOLOGY			English	Meeting Abstract									Univ Missouri, Dept Geol Sci & Engn, Rolla, MO 65409 USA	University of Missouri System; Missouri University of Science & Technology									0	3	5	0	1	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2006	30						213	213						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400012
J	Flores-Trujillo, J; Helenes, J				Flores-Trujillo, Juan; Helenes, Javier			Dinoflagellate cysts in marine laminated sediments from Pescadero Basin, south Gulf of California - Preliminary results	PALYNOLOGY			English	Meeting Abstract									CICESE, Geol Dept, Ensenada 22800, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada			Escamilla, Javier/J-5033-2016						0	0	0	0	2	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2006	30						217	217						1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	125BB					2025-03-11	WOS:000243415400022
J	Vajda, V; Wigforss-Lange, J				Vajda, Vivi; Wigforss-Lange, Jane			The Jurassic-Cretaceous transition of Southern Sweden - palynological and sedimentological interpretation	PROGRESS IN NATURAL SCIENCE			English	Article; Proceedings Paper	International Symposium on the Jurassic Boundary Events/1st Annual Meeting of the International Geoscience Program IGCP 506	NOV 01-04, 2005	Nanjing, PEOPLES R CHINA	UNESCO IUGS Int Geosci Program, Natl Nat Sci Fdn China, Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig		palynology; tsunami; Jurassic; Cretaceous; Sweden	TSUNAMI DEPOSIT; NORTHERN FRANCE; CHINA; PALYNOFLORAS; PALYNOMORPHS; FORAMINIFERA; BOULONNAIS; CONIACIAN; BOUNDARY; SCANIA	Palynological studies on the Vitaback Clay help resolve the position of the Jurassic-Cretaceous boundary in southern Sweden. Well-preserved assemblages of terrestrial pollen and spores, together with abundant algae (Botrycoccus), and for the first time, dinoflagellates have been identified in the Vitaback Clay. A Berriasian age is corroborated for the Vitaback Clay based on the palynological data; the Jurassic-Cretaceous boundary being placed around the contact of this unit with the underlying "Nytorp Sand". The terrestrial vegetation was dominated by coniferous forest with an understorey of ferns in a warm, temperate climate. The palynoflora shows compositional similarities to the Northern Chinese Floral Province and especially the Jehol Group. The majority of the Vitaback Clay represents a moderate-to low-energy paralic succession. However, the basal part of the unit incorporates anomalously coarse material of mixed terrestrial and marine origin. This sedimentary package is herein interpreted to represent tsunami deposits and is similar to coeval tsunami-related deposits in France.	Lund Univ, GeoBiosphere Sci Ctr, S-22362 Lund, Sweden	Lund University	Vajda, V (通讯作者)，Lund Univ, GeoBiosphere Sci Ctr, Solvegatan 12, S-22362 Lund, Sweden.	Vivi.Vajda@geol.lu.se	Vajda, Vivi/N-7693-2018					Balme Basil E., 1995, Review of Palaeobotany and Palynology, V87, P81, DOI 10.1016/0034-6667(95)93235-X; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; Batten DJ, 1997, REV PALAEOBOT PALYNO, V99, P25, DOI 10.1016/S0034-6667(97)00036-5; Beck CB, 1988, Origin and evolution of gymnosperms, P382; CHEN PJ, 2003, CRETACEOUS BIOSTRATI, P465; Deconinck JF, 2000, CR ACAD SCI II A, V330, P527, DOI 10.1016/S1251-8050(00)00169-5; Dorhofer G., 1977, NEUES JB GEOLOGIE PA, V153, P50; Dypvik H, 1996, GEOLOGY, V24, P779, DOI 10.1130/0091-7613(1996)024<0779:MLSAIC>2.3.CO;2; Erlstorm M., 1991, Sveriges Geologiska Undersokning Serie Ca, V78, P1; Guy-Ohlson Dorothy, 1994, Geobios Memoire Special (Villeurbanne), V17, P275; GUYOHLSON D, 1982, SVERIGES GEOLOGISKA, V52, P45; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P1; Herngreen GF., 1996, Palynology: Principles and Applications, V3, P1157; Larsson K, 2000, NEUES JAHRB GEOL P-A, V216, P277; LI WB, 1994, CRETACEOUS RES, V15, P333, DOI 10.1006/cres.1994.1021; NORLING E, 1981, GEOL FOREN STOCK FOR, V103, P253, DOI 10.1080/11035898109454522; NORLING E, 1987, TECTONOPHYSICS, V137, P7, DOI 10.1016/0040-1951(87)90309-X; NORRIS G., 1969, PALAEONTOLOGY, V12, P574; Rees J, 2002, T ROY SOC EDIN-EARTH, V93, P59, DOI 10.1017/S0263593300000328; Saiki K, 2003, J ASIAN EARTH SCI, V21, P813, DOI 10.1016/S1367-9120(02)00107-4; Schnyder J, 2005, SEDIMENT GEOL, V177, P209, DOI 10.1016/j.sedgeo.2005.02.008; Sha JG, 2003, CRETACEOUS RES, V24, P715, DOI 10.1016/j.cretres.2003.07.006; SHAOZHI M, 1990, REV PALAEOBOT PALYNO, V65, P115; Smelror M, 2002, GEOLOGICAL AND BIOLOGICAL EFFECTS OF IMPACT EVENTS, P69; Synolakis CE., 1995, EOS Trans AGU, V76, P257, DOI DOI 10.1029/95EO00150; Vajda V, 2001, ACTA PALAEONTOL POL, V46, P403; VAJDA V, 1998, THESIS LUND PUBLICAT; Vajda-Santivanez V, 1999, GFF, V121, P281, DOI 10.1080/11035899901214281	28	8	8	0	7	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	1002-0071			PROG NAT SCI	Prog. Nat. Sci.		2006	16				SI		31	38						8	Materials Science, Multidisciplinary; Multidisciplinary Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Materials Science; Science & Technology - Other Topics	077MT					2025-03-11	WOS:000240034200005
J	Cheng, JH; He, CQ				Cheng Jinhui; He Chengquan			Middle-Late Jurassic marine dinoflagellate cysts from the eastern Qiangtang Basin in the Qinghai-Tibet Plateau, China	PROGRESS IN NATURAL SCIENCE			English	Article; Proceedings Paper	International Symposium on the Jurassic Boundary Events/1st Annual Meeting of the International Geoscience Program IGCP 506	NOV 01-04, 2005	Nanjing, PEOPLES R CHINA	UNESCO IUGS Int Geosci Program, Natl Nat Sci Fdn China, Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig			TOARCIAN	Dinoflagellate cysts from two Middle-Late Jurassic sections in the Wenquan and Yanshiping regions of the Qiangtang Basin comprise 24 genera and 36 species including one new taxon of the genus Tenua. Based on their stratigraphic distribution, six assemblage zones are recognized in ascending order as follows: 1) Tubotuberella egemenii Zone, probably Callovian, in the mid-upper part of the Xiali Formation; 2) Pareodinia ceratophora Zone, probably Oxfordian, in the lower part of the Suowa Formation; 3) Batiacasphaera floralis Zone, probably Oxfordian, in the middle part of the Suowa Formation; 4) Amphorula metaelliptica Zone, probably Early Kimmeridgian, in the upper part of the Suowa Formation; 5) Alisocysta spp. Zone, probably Early Kimmeridgian, in the base of the Xueshan Formation; 6) Tenua wenquanensis sp. nov. -Dichadogonyaulax schizoblata Zone, probably Late Kimmeridgian-Tithonian, in the lower part of the Xueshan Formation. Based on our analysis the Jurassic-Cretaceous Boundary in the Wenquan section is placed higher than previously.	Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China	Chinese Academy of Sciences	Cheng, JH (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China.	cheng_jin_hui@yahoo.com.cn						[Anonymous], 2005, Micropalaeontology of the Qiangtang Basin; [Anonymous], GEOLOGICAL SURVEY CA; [Anonymous], STRATIGRAPHY QINGHAI; BEJU D., 1971, Annales Instituti Geologici Publici Hungarici, V54, P275; Brenner W., 1988, MORPHOLOGIE OKOLOGIE, V6, P1; Bucefalo Palliani R., 1994, PALEOPELAGOS, V4, P129; BUJAK JP, 1977, STRATIGRAPHIC MICROP, P321; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; COURTINAT B, 1980, DOCUMENTS LABORATOIR, V78, P1; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; DAVIES E H, 1985, Palynology, V9, P105; DAVIES E. H., 1983, GEOL SURV CAN B, V359, P1; Deflandre G., 1938, TRAVAUX STATION ZOOL, V13, P147; DODEKOVA L, 1992, Geologica Balcanica, V22, P33; DODEKOVA L, 1990, Geologica Balcanica, V20, P3; Dodekova L., 1969, Bulgarska Akademiya na Naukite, Izvestiya na Geologicheskiya Institut, Seriya Paleontologiya, v, V18, p, P13; DOWNIE CHARLES, 1957, QUART JOUR GEOL SOC LONDON, V112, P413; DUPIN F, 1968, NOUVELLES ESPECES DI, V1, P1; DURR G, 1988, TUBINGER MIKROPALAON, V5, P1; Erkmen U., 1980, Geobios (Villeurbanne), V13, P45, DOI 10.1016/S0016-6995(80)80014-3; Fensome R.A., 1979, Gronlands Geologiske Undersogelse Bulletin, V132, P1, DOI [10.34194/bullggu.v132.6674, DOI 10.34194/BULLGGU.V132.6674]; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; GITMEZ G.U., 1970, B BRIT MUS NAT HIST, V18, P231; HABIB D, 1983, INITIAL REP DEEP SEA, V76, P623; Habib D., 1972, Initial Rep Deep Sea Drilling Project, V11, P367; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; He Cheng-Quan, 1997, Acta Micropalaeontologica Sinica, V14, P21; He Cheng-Quan, 2000, Acta Palaeontologica Sinica, V39, P46; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P1; JIANG Q, 1992, REV PALAEOBOT PALYNO, V74, P77, DOI 10.1016/0034-6667(92)90139-8; JIANG ZT, 1983, SOME PROBLEMS JURASS, V3, P87; JOHNSON C D, 1973, Bulletin of Canadian Petroleum Geology, V21, P178; Klement K. W., 1960, Palaeontographica, VA114, P1; Li Y, 2000, P 3 NAT STRAT C CHIN, P397; Mao Shaozhi, 2000, Geoscience, V14, P115; Monteil E., 1992, Revue de Paleobiologie, V11, P273; MONTEIL E, 1990, B CENT RECH EXPL, V14, P597; Monteil E., 1992, Revue de Paleobiologie, V11, P299; Nejad Ebrahim Ghasemi, 1999, Schweizerische Palaeontologische Abhandlungen, V119, P1; Palliani RB, 1998, PALAEOGEOGR PALAEOCL, V142, P33, DOI 10.1016/S0031-0182(97)00152-1; Palliani RB, 1998, J MICROPALAEONTOL, V17, P153, DOI 10.1144/jm.17.2.153; POCOCK SAJ, 1972, GEOLOGICAL SOC DENMA, V21, P346; Quattrocchio M., 1983, Revista de la Asociacion Geologica Argentina, V38, P34; RIDING JB, 1985, REV PALAEOBOT PALYNO, V45, P149, DOI 10.1016/0034-6667(85)90068-5; RIDING JB, 1992, STRATIGRAPHIC INDEX, P1; RILEY L A, 1982, Palynology, V6, P193; SARJEANT W, 1978, MISCELLANEOUS PUBLIC, V78, P1; Sarjeant W.A.S., 1974, P1; Sarjeant W. A. S., 1962, Micropaleontology, V8, P255, DOI 10.2307/1484746; SARJEANT W. A. 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S., 1960, GEOL MAG, V97, P137; SARJEANT WAS, 1961, PALAEONTOLOGY, V4, P80; Smelror M., 1989, Palynology, V13, P121; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; STOVER LE, 1996, AM ASS STRATIGRAPHIC, V2, P641; Sun C, 1997, MULTIPLE CLASSIFICAT, P1; Sun D., 2000, STRATIGRAPHICAL STUD, P283; Sun X.-k., 1992, Acta Palaeontologica Sinica, V31, P190; VALENSI LIONEL, 1953, MEM SOC GEOL FRANCE, V68, P1; [王康明 Wang Kangming], 2002, [地质通报, Geological Bulletin of China], V21, P421; Wang S.E., 2000, Stratigraphic Code of China-Jurassic System, P1; WANG SE, 1985, JURASSIC SYSTEM CHIN, P1; Williams G.L., 1985, PLANKTON STRATIGRAPH, V2, P847; Williams G.L., 1977, Oceanic Micropalaeontology, V2, P1231; WILLIS S, 1993, S ATL QUART, V92, P1; WOOLLAM R, 1983, REPORT I GEOLOGICAL, V2, P1; ZOTTO M, 1987, MICROPALEONTOLOGY, V33, P193, DOI 10.2307/1485637	68	12	15	0	5	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	1002-0071			PROG NAT SCI	Prog. Nat. Sci.		2006	16				SI		274	283						10	Materials Science, Multidisciplinary; Multidisciplinary Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Materials Science; Science & Technology - Other Topics	077MT					2025-03-11	WOS:000240034200025
J	Sha, JG; Chen, SW; Cai, HW; Jiang, BY; Yao, XG; Pan, YH; Wang, JP; Zhu, YH; He, CQ				Sha Jingeng; Chen Siwei; Cai Huawei; Jiang Baoyu; Yao Xiaogang; Pan Yanhong; Wang Jianpo; Zhu Youhua; He Chengquan			Jurassic-Cretaceous boundary in Northeastern China: placement based on buchiid bivalves and dinoflagellate cysts	PROGRESS IN NATURAL SCIENCE-MATERIALS INTERNATIONAL			English	Article; Proceedings Paper	International Symposium on the Jurassic Boundary Events/1st Annual Meeting of the International Geoscience Program IGCP 506	NOV 01-04, 2005	Nanjing, PEOPLES R CHINA	UNESCO IUGS Int Geosci Program, Natl Nat Sci Fdn China, Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig		marine; Jurassic-Cretaceous boundary; buchiid bivalves; dinoflagellate cysts; northeastern China	GEOLOGIC TIME-SCALE; EASTERN HEILONGJIANG	Global environments changed greatly during the Late Jurassic and Early Cretaceous, particularly during the Jurassic-Cretaceous boundary interval. Separation of the world into Tethyan, Boreal and other biogeographic realms complicates international correlation, and even the pelagic ammonites cannot play their characteristic role of principle correlation criteria. In the Boreal and North Pacific realms, the Late Jurassic and Cretaceous buchiid bivalve zones have very good calibration to Boreal ammonite zones, which, in turn, have approximate correlations to Tethyan ammonite zones. Therefore, buchiid bivalves provide a means to identify Upper Jurassic-Lower Cretaceous stages and the Jurassic-Cretaceous boundary interval. The base of the Buchia unschensis Zone is roughly coincident with the Boreal ammonite Craspedites exoticus subzone, Upper Volgian Craspedites okensis Zone, which in turn closely corresponds to the base of the Tethyan ammonite basal Berriasian Berriasella jacobi Zone. The top of the underlying Buchia russiensis Zone approximately coincides with that of the uppermost Middle Volgian, Boreal ammonite Epivirgatites variabilis Zone, which approximately corresponds to the Tethyan ammonite Durangites Zone of uppermost Tithonian. Buchia and dinoflagellate cyst assemblages from two regions in eastern Heilongiiang of northeastern China indicate the presence of the Jurassic-Cretaceous boundary interval. The Dong'anzhen Formation of Dong' an, Raohe County contains Middle Volgian-Lower Valanginian Buchia assemblages and the Jurassic-Cretaceous boundary is tentatively assigned to either the base of the Buchia fischeriana-Buchia unschensis assemblage or between the Buchia fischeriana-Buchia unschensis and Buchia russiensis-Buchia fischeriana assemblages. The Dongrong Formation from boreholes at Suibin, Suibin County, yields uppermost Oxfordian to basal Berriasian Buchia assemblages and Oxfordian-Barremian dinoflagellate cyst assemblages. Here, the Jurassic-Cretaceous boundary interval is probably between the Buchia cf. mosquensis-Buchia cf. rugosa assemblage (including Buchia ex gr. russiensis and Buchia ex gr. taimyrensis) and the overlying non-Buchia-bearing deposits.	Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, LPS, Nanjing 210008, Peoples R China	Chinese Academy of Sciences	Sha, JG (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, LPS, Nanjing 210008, Peoples R China.	jgsha@nigpas.ac.cn	jiang, johnson/KDP-0686-2024					*110 EXPL TEAM, 1992, ACTA PALAEONTOL SIN, V31, P129; [Anonymous], JURASSIC DENMARK GRE; [Anonymous], 2000, Stratigraphic Studies in China (1979-1999) (in Chinese); CASEY R, 1977, CORRELATION JURASSIC, V7, P14; CASEY R., 1973, BOREAL LOWER CRETACE, P193; CHEN JH, 1992, ACTA PALAEONTOLOGICA, V31, P161; Gradstein FM, 2004, EPISODES, V27, P83, DOI 10.18814/epiiugs/2004/v27i2/002; Gradstein FM., 2004, GEOLOGIC TIME SCALE, P20; GU ZW, 1992, LOWER CRETACEOUS BIV, P301; He Cheng-Quan, 2003, Acta Palaeontologica Sinica, V42, P328; HUANG GJ, 1990, MARINE JURASSIC JIXI, V2, P14; JU RH, 1982, CHINESE ACAD GEOLOGI, V5, P1; Kelly S.R.A., 1990, I GEOLOGY GEOPHYS T, V699, P129; LI ZS, 1982, B SHENYANG I GEOLOGY, V5, P73; Ogg J.G., 2004, GEOLOGIC TIME SCALE, P344; Ogg JG, 2004, LETHAIA, V37, P183, DOI 10.1080/00241160410006492; Powell A.J., 1992, STRATIGRAPHIC INDEX, P290; Sha J.-g., 1992, Journal of Stratigraphy, V16, P41; Sha J.-G., 1994, BERINGERIA, V12, P3; Sha JG, 2003, CRETACEOUS RES, V24, P715, DOI 10.1016/j.cretres.2003.07.006; SHA JG, 1994, NEWSL STRATIGR, V31, P101; SHA JG, 1993, GEOL MAG, V130, P533, DOI 10.1017/S0016756800020586; Sha Jin-geng, 2005, Journal of Stratigraphy, V29, P124; Sha Jin-geng, 2002, Dixue Qianyuan, V9, P95; Sha Jingeng, 1992, Geological Review (Beijing), V38, P131; Sun D., 2000, STRATIGRAPHICAL STUD, P283; Sun X.-k., 1992, Acta Palaeontologica Sinica, V31, P190; SURLYK F, 1982, PALAEONTOLOGY, V25, P727; Yu Jingxian, 1982, CHIN ACAD GEOL SCI S, V5, P227; ZAKHAROV V A, 1987, Cretaceous Research, V8, P141, DOI 10.1016/0195-6671(87)90018-8; ZAKHAROV VA, 1981, NORSK GEOL TIDSSKR, V61, P261; Zakharov VA., 1981, Trudy Instituta Geologii i Geofiziki, Akademija Nauk SSR, Sibirskoe Otdelenie, V458, P1; Zakharov Viktor A., 1996, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V66, P7	33	14	23	0	3	ELSEVIER SCIENCE INC	NEW YORK	360 PARK AVE SOUTH, NEW YORK, NY 10010-1710 USA	1002-0071	1745-5391		PROG NAT SCI-MATER	Prog. Nat. Sci.		2006	16				SI		39	49						11	Materials Science, Multidisciplinary; Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Materials Science; Science & Technology - Other Topics	077MT					2025-03-11	WOS:000240034200006
J	Radwan, FFY; Ramsdell, JS				Radwan, FFY; Ramsdell, JS			Characterization of <i>in vitro</i> oxidative and conjugative metabolic pathways for brevetoxin (PbTx-2)	TOXICOLOGICAL SCIENCES			English	Article						Karenia brevis; red tide bloom; brevetoxin metabolism; in vitro; cytochrome P450; CYP; conjugation	SENSITIVE SODIUM-CHANNELS; RED TIDE; RAT HEPATOCYTES; NEW-ZEALAND; GYMNODINIUM; CYTOCHROME-P450; ELIMINATION; ENZYMES; TOXINS; BETA	Brevetoxins are potent marine toxins produced by the dinoflagellate Karenia brevis, the causative organism of Florida red tides. An in vitro metabolism of PbTx-2 was performed using purified cDNA-expressed rat liver cytochrome P-450 (CYP) enzymes and freshly isolated rat hepatocytes. The metabolic activities of six CYP enzymes, CYP1A2, CYP2A2, CYP2C11, CYP2D1, CYP2E1, and CYP3A1, were examined by incubation with PbTx-2 for up to 4 h in the presence of a NADPH-generating system. Further identification of the metabolites produced by CYP1A2 and CYP3A1 was preformed using high performance liquid chromatography-mass spectrometry (LC/MS). Both CYP1A2 and CYP3A1 metabolized PbTx-2 to PbTx-3 (MH+: m/z 897), PbTx-9 (MH+: m/z 899), and a newly recorded diol brevetoxin-2 metabolite (MH+: m/z 929). CYP3A1 also produced a considerably higher amount of BTX-B5 (MH+: m/z 911). Subsequent incubation of PbTx-2 with rat hepatocytes produced additional phase 1 metabolites of MH+: m/z 911, 913, 915, 917, and 931, indicating a CYP-catalyzed epoxidation at H-ring (C-27,C-28-double bond) and a subsequent A-ring hydrolysis of PbTx-2 metabolic products. A conjugation metabolism was identified by the production of a glutathione-brevetoxin conjugate (MH+: m/z 1222) and a cysteine-brevetoxin conjugate (MH+: m/z 1018). Structures of the new metabolites are postulated, and a likely CYP-catalyzed metabolism pathway of PbTx-2 metabolism are discussed.	NOAA, Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Coastal Res Branch,Marine Biotoxins Program, Charleston, SC 29412 USA; S Valley Univ, Fac Sci, Sohag, Egypt	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; Egyptian Knowledge Bank (EKB); South Valley University Egypt	NOAA, Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Coastal Res Branch,Marine Biotoxins Program, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	john.ramsdell@noaa.gov						Baden DG, 2005, ENVIRON HEALTH PERSP, V113, P621, DOI 10.1289/ehp.7499; DAVIS CC, 1948, BOT GAZ, V109, P358, DOI 10.1086/335488; Dickey R, 1999, NAT TOXINS, V7, P157, DOI 10.1002/(SICI)1522-7189(199907/08)7:4<157::AID-NT52>3.3.CO;2-R; DONATO MT, 1993, ANAL BIOCHEM, V213, P29, DOI 10.1006/abio.1993.1381; Flewelling LJ, 2005, NATURE, V435, P755, DOI 10.1038/nature435755a; Ishida H, 2004, TETRAHEDRON LETT, V45, P29, DOI 10.1016/j.tetlet.2003.10.124; Jeglitsch G, 1998, J PHARMACOL EXP THER, V284, P516; KENNEDY CJ, 1992, AQUAT TOXICOL, V22, P3, DOI 10.1016/0166-445X(92)90032-I; LIN YY, 1981, J AM CHEM SOC, V103, P6773, DOI 10.1021/ja00412a053; McFARREN E. F., 1965, TOXICON, V3, P111, DOI 10.1016/0041-0101(65)90005-X; MCQUEEN CA, 1993, METHODS TOXICOLOGY, V1, P255; Nozawa A, 2003, TOXICON, V42, P91, DOI 10.1016/S0041-0101(03)00123-5; PIERCE RH, 1986, TOXICON, V24, P955, DOI 10.1016/0041-0101(86)90001-2; Plakas SM, 2002, TOXICON, V40, P721, DOI 10.1016/S0041-0101(01)00267-7; POLI MA, 1990, TOXICON, V28, P903, DOI 10.1016/0041-0101(90)90020-8; POLI MA, 1986, MOL PHARMACOL, V30, P129; Purkerson SL, 1999, NEUROTOXICOLOGY, V20, P909; Quick J.A. Jr., 1974, P85; Radwan FFY, 2005, TOXICOL SCI, V85, P839, DOI 10.1093/toxsci/kfi138; SHIMIZU Y, 1986, J AM CHEM SOC, V108, P514, DOI 10.1021/ja00263a031; SONDERFAN AJ, 1987, ARCH BIOCHEM BIOPHYS, V255, P27, DOI 10.1016/0003-9861(87)90291-8; Wang ZH, 2004, TOXICON, V43, P455, DOI 10.1016/j.toxicon.2004.02.017; WASHBURN BS, 1994, TOXICON, V32, P799, DOI 10.1016/0041-0101(94)90005-1; Washburn BS, 1996, AQUAT TOXICOL, V35, P1, DOI 10.1016/0166-445X(95)00050-E; WOODCOCK AH, 1948, J MAR RES, V7, P56; Woofter RT, 2005, ENVIRON HEALTH PERSP, V113, P11, DOI 10.1289/ehp.7274; WORTELBOER HM, 1990, BIOCHEM PHARMACOL, V40, P2525, DOI 10.1016/0006-2952(90)90095-3	27	34	41	0	15	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	1096-6080	1096-0929		TOXICOL SCI	Toxicol. Sci.	JAN	2006	89	1					57	65		10.1093/toxsci/kfj013	http://dx.doi.org/10.1093/toxsci/kfj013			9	Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Toxicology	993XN	16221966	Green Submitted, Bronze			2025-03-11	WOS:000233991000006
J	Akkiraz, MS; Akgün, F; Örçen, S; Bruch, AA; Mosbrugger, V				Akkiraz, Mehmet Serkan; Akgun, Funda; Orcen, Sefer; Bruch, Angela Anneliese; Mosbrugger, Volker			Stratigraphic and palaeoenvironmental significance of Bartonian-Priabonian (Middle-Late Eocene) microfossils from the Bascesme formation, Denizli province, western Anatolia	TURKISH JOURNAL OF EARTH SCIENCES			English	Review						Middle-Late Eocene; mangrove; western Anatolia; benthic foraminifer; palynomorph; palaeoenvironment; palaeoclimate	SOUTHERN MENDERES MASSIF; EARLY OLIGOCENE; TERTIARY; TURKEY; BASIN; EVOLUTION; PALYNOLOGY; EXTENSION; PALEOECOLOGY; PALYNOMORPHS	This study explains the stratigraphical and palaeoenvironmental significance of Bartonian - Priabonian ( Middle - Late Eocene) fossils, the fauna and flora obtained from the Bascesme formation of the Cardak - Tokca basin ( western Anatolia). The studied sequence is an outcrop from the Bascesme formation, deposited in a shallow-marine to coastal environment without stratigraphic breaks. Forty genera and 58 species have been recognized in the palynological assemblage of the Bascesme formation. A well-preserved diverse palynomorph and foraminiferal assemblages yield the Middle - Late Eocene age for the Bascesme formation. In western Anatolia, mangrove elements Nypa and Pelliciera have been first recorded in this study. The pollen of Mauritia and Acrostichum occur in the back-mangrove environment. Lowland - Riparian and montane elements are characterized by dominance of Myricaceae, Betulaceae, Engelhardia, Fagaceae, Myrtaceae, Anacardiaceae and Taxodiaceae, Pinus, Abies, Picea, Cathaya, Quercus and Castanea, respectively. Fresh-water elements are represented by Sparganiaceae, Pediastrum sp. and Aglaoreidia cyclops. The palynological data for samples taken from the lower part of the section of the Bascesme formation indicate a back-mangrove environment. The presence of poorly preserved dinoflagellate cysts suggest that sedimentation occurred in a mangrove environment in the upper part of the section. The well-preserved foraminiferal data, along with corals, bivalves and gastropods, indicate that sedimentation ceased in the shallow-marine environment. In this paper, terrestrial climatic conditions of the Bascesme formation are also discussed on the basis of the coexistence approach.	Dokuz Eylul Univ, Mukendislik Fak, TR-35100 Izmir, Turkey; Yuzuncu Yil Univ, Muhendisklik Mimarlik Fak, TR-65080 Van, Turkey; Inst & Museum Geol & Palaeontol, D-72076 Tubingen, Germany	Dokuz Eylul University; Yuzuncu Yil University; Eberhard Karls University of Tubingen	Akkiraz, MS (通讯作者)，Dokuz Eylul Univ, Mukendislik Fak, TR-35100 Izmir, Turkey.	serkan.akkiraz@deu.edu.tr	akkiraz, mehmet/ADP-2366-2022; Akgün, Funda/AAC-2859-2020; Mosbrugger, Volker/A-5469-2009	Akgun, Funda/0000-0002-6028-6704				Akgun F, 2002, [古生物学报, Acta Palaeontologica Sinica], V41, P576; AKGUN F, 2002, TURKISH J EARTH SCI, V11, P1; Akkiraz MS, 2005, GEOBIOS-LYON, V38, P283, DOI 10.1016/j.geobios.2003.11.010; AKYOL E, 1978, JEOLOJI MUHENDISLIGI, V6, P31; AKYOL E, 1980, MINERAL RES EXPLORAT, V91, P39; ALEKSANDROVA AN, 1987, INT GEOL REV, V29, P503; [Anonymous], USGS PROFESSIONAL PA; [Anonymous], 2002, Turkish Journal of Earth Science; [Anonymous], 1988, Geologisches Jahrbuch Reihe A; Blasco F., 1977, Ecosystems of the World 1: Wet Coastal Ecosystems, P241; Bolotnikova M.D., 1979, Spore-Pollen Complexes of Tertiary Sediments of the Western Coast of the Sea of Japan; BOZKURT E, 1994, J GEOL SOC LONDON, V151, P213, DOI 10.1144/gsjgs.151.2.0213; Bozkurt E, 1999, GEODIN ACTA, V12, P25, DOI 10.1016/S0985-3111(99)80021-7; BUCHARDT B, 1978, NATURE, V275, P121, DOI 10.1038/275121a0; Cavagnetto C, 1996, REV PALAEOBOT PALYNO, V92, P281, DOI 10.1016/0034-6667(95)00096-8; Cavagnetto Carla, 1995, Palaeontographica Abteilung B Palaeophytologie, V236, P147; Chapman V.J., 1976, Mangrove Vegetation; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Collins AS, 1998, J GEOL SOC LONDON, V155, P759, DOI 10.1144/gsjgs.155.5.0759; Collins AS, 1999, GEOL J, V34, P107; Collins AS, 1997, GEOLOGY, V25, P255, DOI 10.1130/0091-7613(1997)025<0255:LMSTAE>2.3.CO;2; COLLINS J P, 1977, Brenesia, V10, P17; Dilcher D.L., 1973, Vegetation and vegetational history of northern Latin America, P39; EDIGER VS, 1990, REV PALAEOBOT PALYNO, V62, P97, DOI 10.1016/0034-6667(90)90019-F; El Beialy SY, 1998, REV PALAEOBOT PALYNO, V102, P249, DOI 10.1016/S0034-6667(98)00019-0; Elsik W.C., 1974, Palaeontographica Abt B, V149, P90; FECHNER GG, 1988, PALAEOGEOGR PALAEOCL, V65, P73, DOI 10.1016/0031-0182(88)90113-7; FOWLER K, 1971, Pollen et Spores, V13, P135; Frederiksen N., 1988, United States Geological Survey Professional Paper 1448, V1448, P1; Frederiksen N., 1973, Tulane Studies in Geology and Paleontology, V10, P65; Frederiksen N.O., 1985, AM ASS STRATIGRAPHIC, V19, P1; FREDERIKSEN NO, 1980, J PALEONTOL, V54, P728; Frederiksen Norman O., 2002, Palynology, V26, P59, DOI 10.2113/0260059; Frederiksen Norman O., 1994, Palynology, V18, P91; FUCHS HP, 1970, ACTA BOT NEERL, V19, P884, DOI 10.1111/j.1438-8677.1970.tb00192.x; GERMERAAD JH, 1968, REV PALAEOBOT PALYNO, V6, P189, DOI 10.1016/0034-6667(68)90051-1; GOKTAS F, 1989, 8701 MTA; Gonzalez-Guzman A., 1967, PALYNOLOGICAL STUDY; GRAHAM A, 1995, BIOTROPICA, V27, P20, DOI 10.2307/2388899; GRAHAM A, 1977, BIOTROPICA, V9, P48, DOI 10.2307/2387858; GRAY J, 1960, SCIENCE, V132, P808, DOI 10.1126/science.132.3430.808; GREENWOOD DR, 1995, GEOLOGY, V23, P1044, DOI 10.1130/0091-7613(1995)023<1044:ECCALT>2.3.CO;2; GRUASCAVAGNETTO C, 1977, THESIS U PM CURIE 6; GUASCAVAGNETTO C, 1978, MEMOIRE SOC GEOLOGIQ, V131, P1; HASELDONCKX P, 1972, Geologie en Mijnbouw, V51, P645; Hochuli P.A., 1978, Beitrrage Palaontologie Osterreich, V4, P1; Hochuli P.A., 1984, Paleobiologie continentale, V14, P301; JIMENEZ JA, 1984, BIOTROPICA, V16, P304, DOI 10.2307/2387939; Kar, 1984, I FR PONDICHERRY TRA, V19, P1; KEDVES M, 1970, Pollen et Spores, V12, P83; KEDVES M, 1969, POLLEN SPORES, V11, P385; Kedves M., 1982, PALAEONTOGR ABT B, V182, P87; Kedves M., 1986, STUDIA BIOL HUNGARIC, V21, P1; Koçyigit A, 2005, GEODIN ACTA, V18, P167, DOI 10.3166/ga.18.167-208; Konak N., 1987, Bull.Min.Res.Expl.Inst. 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Meded, V30, P183; Westaway R, 2005, GEODIN ACTA, V18, P209, DOI 10.3166/ga.18.209-238; WESTGATE JW, 1990, PALAEOGEOGR PALAEOCL, V78, P163, DOI 10.1016/0031-0182(90)90210-X; Wolfe J.A., 1979, Termperature parameters of humid to mesic forests of eastern Aisia and their relation to forests of other regions of the Northern Hemisphere and Australia, V1106, P1, DOI DOI 10.3133/PP1106; Wolfe J.A., 1992, Eocene-Oligocene Climatic and Biotic Evolution, P421, DOI DOI 10.1515/9781400862924.421/HTML; WOLFE JA, 1978, AM SCI, V66, P694; YALCINKAYA S, 1986, 7898 MTA; YASAMANOV NA, 1982, IZVESTIYA AN SSSR G, V10, P106	105	33	36	0	7	Tubitak Scientific & Technological Research Council Turkey	ANKARA	ATATURK BULVARI NO 221, KAVAKLIDERE, TR-06100 ANKARA, TURKIYE	1300-0985			TURK J EARTH SCI	Turk. J. Earth Sci.		2006	15	2					155	180						26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	062VT					2025-03-11	WOS:000238974200003
J	Sancay, RH; Bati, Z; Isik, U; Kirici, S; Akça, N				Sancay, Recep Hayrettin; Bati, Zuehtue; Isik, Ugras; Kirici, Sabri; Akca, Nihal			Palynomorph, foraminifera, and calcareous nannoplankton biostratigraphy of Oligo-Miocene sediments in the Mus Basin, Eastern Anatolia, Turkey	TURKISH JOURNAL OF EARTH SCIENCES			English	Review						Oligocene; Miocene; Eastern Anatolia; palynomorphs; planktonic foraminifera; benthic foraminifera; nannoplankton; palaeoenvironment; palaeoclimate	DINOFLAGELLATE CYSTS; SEA-LEVEL; OLIGOCENE; MIOCENE; RECONSTRUCTIONS; STRATIGRAPHY; PALYNOLOGY; EVOLUTION; WESTERN; MODEL	Oligo-Miocene sediments have not been adequately studied biostratigraphically, and a detailed biochronostratigraphic framework has not yet been established in Eastern Anatolian basins. Palynomorphs have therefore been correlated with the biozonations of marine dinoflagellates, planktonic foraminifera and calcareous nannoplankton of similar latitudes in combined samples from the Ebulbahar and Keleresdere measured stratigraphic sections, which are located in the northeastern part of Mus. Palynological (dinoflagellate), foraminiferal micropalaentological, and nannopalaeontological events, correlatable with worldwide defined biozonations, have been documented from uppermost Rupelian to Upper Miocene-Pliocene sediments. First occurrences (FOs) and and last occurrences (LOs) of selected dinoflagellates are important in establishing the biostratigraphic framework. The LO of Wetzeliella gochtii in the latest Rupelian, the LO of Deflandrea phosphoritica in the latest Chattian, peak occurrences of Chiropteridium spp. in the early and late Aquitanian, the FO of Hystrichosphaeropsis obscura, followed by the FO of Membranilarnacea? picena in the late Aquitanian are of particular significance for regional correlations. Based on established marine zonations and the presence of characteristic Oligocene taxa such as Slowakipollenites hipophaeoides and Mediocolpopollis compactus, stratigraphic ranges of relatively less known pollen taxa in the region, especially those of Compositae ( tubuliflorae-type), Umbelliferae, Gramineae, considered to have their first occurrences at the beginning of Neogene in earlier studies, have been calibrated. In the light of this study, the Late Oligocene-Early Miocene zonation of some palynomorphs should be emended and the stratigraphic ranges of the Compositae (tubuliflorae-type), Umbelliferae, Gramineae pollen should be extended into the Chattian and even the Rupelian in this region. As far as depositional conditions are concerned, palynomorph and organic facies properties indicate deposition under brackish water, shallow ( restricted) and relatively deeper marine conditions related to fluctuating sea level during the Oligocene and Early Miocene. Shallowing-upwards deposition during the Late Oligocene was followed by restricted marine and brackish conditions at the Oligocene-Miocene boundary and in the early Aquitanian. Relatively deeper conditions in the late Aquitanian continued as extensive reef accumulations due to shallowing in the early Burdigalian. Finally, after the last deepening event at the end of Burdigalian and ? early Langian, completely terrestrial (lacustrine and fluvial) deposition predominated in the Mus Basin due to withdrawal of the sea. Terrestrial palynomorphs reflect temperate to subtropical climates in which mean annual temperatures vary between 15.6 and 21.3 degrees C, and mean temperatures of the coldest month (CMT) were between 5.0 and 13.3 degrees C.	Turkish Petr Corp TPAO, Res Ctr, TR-06100 Ankara, Turkey	Turkish Petroleum Corporation (TPAO); Ministry of Energy & Natural Resources - Turkey	Sancay, RH (通讯作者)，Turkish Petr Corp TPAO, Res Ctr, TR-06100 Ankara, Turkey.	hsancay@petrol.tpao.gov.tr						Akay E, 1989, B MINERAL RES EXPLOR, V109, P59; AKGUN F, 1986, Turkiye Jeoloji Kurumu Bulteni, V29, P13; Akgun F., 1995, Turkiye Petrol Jeologlari Dernegi Bulteni, V6, P51; AKGUN F, 2004, CARDAKTOKCA BURDUR I; AKGUN F, 1992, B TURKISH ASS PETROL, V4, P129; Akkiraz M.S., 2000, THESIS DOKUZ EYLUL U; Akkiraz MS, 2005, GEOBIOS-LYON, V38, P283, DOI 10.1016/j.geobios.2003.11.010; ALLEN CR, 1969, 32 CALTECH GEOL PLAN; ANGLADA R, 1971, CR ACAD SCI D NAT, V272, P1067; [Anonymous], 1990, N JB GEOL PALAONT AB; [Anonymous], 1965, Bull. Miner. Res. Explor; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; [Anonymous], 1987, B GEOLOGICAL SOC TUR; Arpat E., 1972, Bull. Miner. Res. 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J. Earth Sci.		2006	15	3					259	319						61	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	129TP					2025-03-11	WOS:000243753300002
J	de Vernal, A; Hillaire-Marcel, C; Darby, DA				de Vernal, A; Hillaire-Marcel, C; Darby, DA			Variability of sea ice cover in the Chukchi Sea (western Arctic Ocean) during the Holocene	PALEOCEANOGRAPHY			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; BERING LAND-BRIDGE; RADIOCARBON AGE CALIBRATION; NORTHERN NORTH-ATLANTIC; LAST GLACIAL MAXIMUM; SURFACE CONDITIONS; CLIMATE-CHANGE; NEOGLOBOQUADRINA-PACHYDERMA; NORTHWESTERN ALASKA; RIVER DISCHARGE	[1] Dinocysts from cores collected in the Chukchi Sea from the shelf edge to the lower slope were used to reconstruct changes in sea surface conditions and sea ice cover using modern analogue techniques. Holocene sequences have been recovered in a down-slope core (B15: 2135 m, 75 degrees 44'N, sedimentation rate of similar to 1 cm kyr(-1)) and in a shelf core (P1: 201 m, 73 degrees 41'N, sedimentation rate of similar to 22 cm kyr(-1)). The shelf record spanning about 8000 years suggests high-frequency centennial oscillations of sea surface conditions and a significant reduction of the sea ice at circa 6000 and 2500 calendar (cal) years B. P. The condensed offshore record (B15) reveals an early postglacial optimum with minimum sea ice cover prior to 12,000 cal years B. P., which corresponds to a terrestrial climate optimum in Bering Sea area. Dinocyst data indicate extensive sea ice cover (> 10 months yr(-1)) from 12,000 to 6000 cal years B. P. followed by a general trend of decreasing sea ice and increasing sea surface salinity conditions, superimposed on large-amplitude millennial-scale oscillations. In contrast, delta O-18 data in mesopelagic foraminifers (Neogloboquadrina pachyderma) and benthic foraminifers (Cibicides wuellerstorfi) reveal maximum subsurface temperature and thus maximum inflow of the North Atlantic water around 8000 cal years B. P., followed by a trend toward cooling of the subsurface to bottom water masses. Sea-surface to subsurface conditions estimated from dinocysts and delta O-18 data in foraminifers thus suggest a decoupling between the surface water layer and the intermediate North Atlantic water mass with the existence of a sharp halocline and a reverse thermocline, especially before 6000 years B. P. The overall data and sea ice reconstructions from core B15 are consistent with strong sea ice convergence in the western Arctic during the early Holocene as suggested on the basis of climate model experiments including sea ice dynamics, matching a higher inflow rate of North Atlantic Water.	Univ Quebec, Ctr Rech Geochim & Geodynam, Montreal, PQ H3C 3P8, Canada; Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	University of Quebec; University of Quebec Montreal; Old Dominion University	Univ Quebec, Ctr Rech Geochim & Geodynam, CP 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	Darby, Dennis/A-9219-2010; Hillaire-Marcel, Claude/H-1441-2012; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	de Vernal, Anne/0000-0001-5656-724X; Hillaire-Marcel, Claude/0000-0002-3733-4632				AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; Ager TA, 2003, QUATERNARY RES, V60, P19, DOI 10.1016/S0033-5894(03)00068-1; Andersen C, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2002PA000873; ANDERSON PM, 1988, QUATERNARY RES, V29, P263, DOI 10.1016/0033-5894(88)90035-X; Andreev AA, 2000, J PALEOLIMNOL, V24, P81, DOI 10.1023/A:1008121917521; Andreev AA, 2001, QUATERNARY SCI REV, V20, P259, DOI 10.1016/S0277-3791(00)00118-9; [Anonymous], 2006, LIMNOL OCEANOGR; Backman J, 2004, QUATERNARY SCI REV, V23, P1435, DOI 10.1016/j.quascirev.2003.12.005; BARRY RG, 1993, REV GEOPHYS, V31, P397, DOI 10.1029/93RG01998; Bauch D, 2003, NATURE, V424, P299, DOI 10.1038/nature01778; Bauch HA, 2001, GLOBAL PLANET CHANGE, V31, P125, DOI 10.1016/S0921-8181(01)00116-3; Bigelow NH, 2003, J GEOPHYS RES-ATMOS, V108, DOI 10.1029/2002JD002558; Bigg GR, 2000, J GEOPHYS RES-OCEANS, V105, P8527, DOI 10.1029/2000JC900005; BLAKE W, 1987, 877 GEOL SURV CAN; Carmack EC, 2000, NATO SCI S PRT 2 ENV, V70, P91; Comiso JC, 2002, ANN GLACIOL, V34, P420, DOI 10.3189/172756402781818067; CRONIN TM, 1995, PALEOCEANOGRAPHY, V10, P259, DOI 10.1029/94PA03149; Darby D.A., 2001, Eos Trans. 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J	Giannakourou, A; Orlova, TY; Assimakopoulou, G; Pagou, K				Giannakourou, A; Orlova, TY; Assimakopoulou, G; Pagou, K			Dinoflagellate cysts in recent marine sediments from Thermaikos Gulf, Greece: Effects of resuspension events on vertical cyst distribution	CONTINENTAL SHELF RESEARCH			English	Article						dinoflagellate cysts; bottom sediments; resuspension; phytoplankton blooms; Thermaikos Gulf; Eastern Mediterranean	SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; NORTHWESTERN AEGEAN SEA; RESTING STAGES; BALTIC SEA; ALEXANDRIUM-TAMARENSE; GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; DIAPAUSE EGGS; COPEPOD EGGS; GERMINATION	A qualitative and semi-quantitative study of recent dinoflagellate cysts has been undertaken in the NW part of Aegean Sea, Thermaikos Gulf (Eastern Mediteranean), before (September 2001), during (October 2001) and after 120 days (February 2002) of intensive trawling activities. This is the first survey of recent dinoflagellate cysts from Greek marine coastal environments. Sediment samples were collected with a corer and the vertical distribution of the cysts was studied at five different layers, from 0 to 10 cm. Dinoflagellate cysts were both abundant and diverse. Cysts were found over the whole sampling area and periods, with concentrations ranging between 247-3202 cysts cm(-3). Thirty-six cyst types were encountered, of which 32 were identified to species level, representing 12 genera. It seems that significant local resuspension, related to the onset of the trawling period and stirring up of the sediment,. contributed to mixing of the upper layers, resulting to more homogenous cyst profiles in the sediment. Viable cysts constituted 16-60% of the total cyst abundance. The abundance peaks of viable cysts within the subsurface sediment layers, observed during the undisturbed period, disappeared during October. In February, the reduction of cyst concentration was associated to a loss of viable cysts, whilst the ratio of viable/empty cysts ranged between 0.30 and 0.67. The abundance of the different dinoflagellate species, in their active form, was monitored in order to detect any relationship between the concentration of cysts in the top 10 cm of sediment and blooms of algae in the water column. Cysts of potentially toxic species, causing Paralitic Shellfish Poisoning (PSP), such as Alexandrium cf. tamarense, A. cf. affine, A. cf. minutum, as well as Gymnodinium catenatum, were detected in the cyst survey. (c) 2005 Elsevier Ltd. All rights reserved.	Hellen Ctr Marine Res, Inst Oceanog, Anavyssos 19013, Attiki, Greece; Russian Acad Sci, Far E Branch, Inst Marine Biol, Vladivostok 690041, Russia	Hellenic Centre for Marine Research; Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Hellen Ctr Marine Res, Inst Oceanog, POB 72, Anavyssos 19013, Attiki, Greece.	agiannak@ath.hcmr.gr	; Orlova, Tatiana/AAU-8448-2020	Pagou, Kalliopi/0000-0002-7601-296X; Orlova, Tatiana/0000-0002-5246-6967; Giannakourou, Antonia/0000-0003-3897-0339				ANAGNOSTOU C, 1997, WATER POLLUTION, V4, P269; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], EUROPEAN WATER MANAG; BALOPOULOS ET, 1993, J ENVIRON SCI HEAL A, V28, P1311, DOI 10.1080/10934529309375944; BARNETT PRO, 1984, OCEANOL ACTA, V7, P399; Belmonte G, 1997, HYDROBIOLOGIA, V355, P159, DOI 10.1023/A:1003071205424; Belmonte G, 1995, OLSEN INT S, P53; BINDER BJ, 1987, J PHYCOL, V23, P99; BLANCO J, 1988, Investigacion Pesquera (Barcelona), V52, P335; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; Dale B., 1983, P69; Dale B., 1979, P443; DALE B, 1994, NATO ASI SER, V1, P521; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; Friligos N, 1997, FRESEN ENVIRON BULL, V6, P27; Giangrande A, 2002, J SEA RES, V47, P97, DOI 10.1016/S1385-1101(01)00103-4; GLIBERT PM, 2003, EU US SCI INITIATIVE; Gotsis-Skretas O., 1990, Thalassographica, V13, P1; GRANELI E, 1998, 3 EUR MAR SCI TECHN, V1, P99; Head M.J., 1996, Palynology: Principles and Applications, P1197; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Karageorgis AP, 2005, REG ENVIRON CHANGE, V5, P138, DOI 10.1007/s10113-004-0078-7; Karageorgis AP, 2001, CONT SHELF RES, V21, P2141, DOI 10.1016/S0278-4343(01)00048-6; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; KREMP A, 1999, MAR BIOL, V4, P711; LINDLEY JA, 1990, MAR BIOL, V104, P209, DOI 10.1007/BF01313260; LYKOUSIS V, 1989, MAR GEOL, V87, P15, DOI 10.1016/0025-3227(89)90142-4; MARCUS NH, 1992, MAR BIOL, V114, P249, DOI 10.1007/BF00349526; Marcus NH, 1998, LIMNOL OCEANOGR, V43, P763, DOI 10.4319/lo.1998.43.5.0763; MARCUS NH, 1989, MAR BIOL, V100, P319, DOI 10.1007/BF00391146; MARCUS NH, 1986, J EXP MAR BIOL ECOL, V99, P247, DOI 10.1016/0022-0981(86)90226-1; MARCUS NH, 1984, MAR ECOL PROG SER, V15, P47, DOI 10.3354/meps015047; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Moncheva S, 2001, ESTUAR COAST SHELF S, V53, P281, DOI 10.1006/ecss.2001.0767; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; PAGOU K, 2003, MONITORING MARINE EN, P111; Pati AC, 1999, MAR BIOL, V134, P419, DOI 10.1007/s002270050558; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; Rubino F, 2000, MAR ECOL-P S Z N I, V21, P263, DOI 10.1046/j.1439-0485.2000.00725.x; Rubino F., 1998, BIOL MAR MEDIT, V5, P253; Stergiou K.I., 1997, Oceanography and Marine Biology an Annual Review, V35, P415	51	58	63	0	27	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0278-4343	1873-6955		CONT SHELF RES	Cont. Shelf Res.	DEC	2005	25	19-20					2585	2596		10.1016/j.csr.2005.08.003	http://dx.doi.org/10.1016/j.csr.2005.08.003			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	994ZT					2025-03-11	WOS:000234070400017
J	Yi, S; Batten, DJ; Lee, SJ				Yi, S; Batten, DJ; Lee, SJ			Provenance of recycled palynomorph assemblages recovered from surficial glaciomarine sediments in Bransfield Strait, offshore Antarctic Peninsula	CRETACEOUS RESEARCH			English	Article						palynofloras; recycling; Bransfield Strait; Antarctic Peninsula	LATE CRETACEOUS STRATIGRAPHY; DINOFLAGELLATE CYSTS; EAST ANTARCTICA; SEYMOUR-ISLAND; ICE SHELF; BASIN; PALYNOLOGY; VEGETATION; EVOLUTION; HOLOCENE	Glaciomarine surficial sediments in cores taken from Bransfield Strait, adjacent to the Antarctic Peninsula, have yielded abundant recycled and contemporaneous (Pleistocene-Holocene) palynomorphs. The former are derived principally from Late Cretaceous-Palaeogene sediments and provide information on glaciomarine depositional conditions and sediment source areas. The composition of the assemblages suggests that they reflect vegetation that was endemic to the Weddellian Biogeographic Province, which includes what is now Seymour Island, James Ross Island and other parts of the Antarctic Peninsula region. The sediments concerned are considered to have accumulated as a result of ice-rafting and discharge of subglacial meltwater. (c) 2005 Elsevier Ltd. All rights reserved.	Korea Inst Geosci & Mineral Resources, Quaternary Environm Res Grp, Geol & Environm Hazards Div, Taejon 305350, South Korea; Univ Manchester, Sch Earth Atmospher & Environm Sci, Manchester M13 9PL, Lancs, England; Univ Wales, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales; Kyungpook Natl Univ, Dept Geol, Taegu 702701, South Korea	Korea Institute of Geoscience & Mineral Resources (KIGAM); University of Manchester; Aberystwyth University; Kyungpook National University (KNU)	Korea Inst Geosci & Mineral Resources, Quaternary Environm Res Grp, Geol & Environm Hazards Div, 30 Gajeong Dong, Taejon 305350, South Korea.	shyi@kigam.re.kr; david.batten@manchester.ac.uk	Yi, Sangheon/D-4780-2011					[Anonymous], GEOLOGY ANTARCTICA; [Anonymous], 1991, GEOLOGICAL EVOLUTION; [Anonymous], KEY ENV; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R.A., 1983, Antarctic Journal of the United States, V18, P63; Askin R.A., 1988, Geological Society of America Memoir, V169, P155; Askin R.A., 1989, Specical Publications of the Geological Society of London, V147, P107; Askin R.A., 1997, The Antarctic Region: Geological Evolution Proceedings, P993; Askin R.A., 1992, ANTARCTIC PALEOENVIR, P61; ASKIN RA, 1990, REV PALAEOBOT PALYNO, V65, P105, DOI 10.1016/0034-6667(90)90061-M; ASKIN RA, 1990, MICROPALEONTOLOGY, V36, P141, DOI 10.2307/1485498; Bahk JJ, 2003, GEOSCI J, V7, P135, DOI 10.1007/BF02910216; Baldoni Alicia M., 1993, Palynology, V17, P241; BARKER PF, 1982, J GEOL SOC LONDON, V139, P787, DOI 10.1144/gsjgs.139.6.0787; Barton C, 1965, British Antarctic Survey Sci. 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Res.	DEC	2005	26	6					906	919		10.1016/j.cretres.2005.06.004	http://dx.doi.org/10.1016/j.cretres.2005.06.004			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	996IX					2025-03-11	WOS:000234168700008
J	van de Schootbrugge, B; Bailey, TR; Rosenthal, Y; Katz, ME; Wright, JD; Miller, KG; Feist-Burkhardt, S; Falkowski, PG				van de Schootbrugge, B; Bailey, TR; Rosenthal, Y; Katz, ME; Wright, JD; Miller, KG; Feist-Burkhardt, S; Falkowski, PG			Early Jurassic climate change and the radiation of organic-walled phytoplankton in the Tethys Ocean	PALEOBIOLOGY			English	Review							ROCK-EVAL PYROLYSIS; CARBON-ISOTOPE STRATIGRAPHY; TOARCIAN ANOXIC EVENT; SEA-LEVEL; DINOFLAGELLATE CYSTS; BASIN; SEDIMENTARY; PLATFORM; FRANCE; MATTER	During the Early Jurassic, cyst-forming dinoflagellates began a long-term radiation that would portend ecological importance of these taxa in the pelagic plankton community throughout the rest of the Mesozoic era. The factors that contributed to the evolutionary success of dinoflagellates are poorly understood. Here we examine the relationship between oceanographic and climatic conditions during the Hettangian-Toarcian interval in relation to the radiation of dinoflagellates and other organic-walled phytoplankton taxa in the Tethys Ocean. Our analysis is based on two data sets. The first includes delta(13)Ccarb, delta(13)Corg, total organic carbon (TOC), and quantitative palynological observations derived from the Mochras Core (Wales, U.K.), which spans the complete Early Jurassic. The second is a coupled Mg/Ca and delta(18)O record derived from analyses of belemnite calcite obtained from three sections in northern Spain, covering the upper Sinemurian to Toarcian. From these two data sets we reconstructed the influence of sea level, trophism, temperature, and salinity on dinoflagellate cyst abundance and diversity in northwest Europe. Our results suggest that organic-walled phytoplankton (acritarchs, prasinophytes, and dinoflagellates) diversity increased through the Early Jurassic. The radiation coincides with a long-term eustatic rise and overall increase in the areal extent of continental shelves, a factor critical to cyst germination. On Shorter timescales, we observed short bursts of dinoflagellate diversification during the late Sinemurian and late Pliensbachian. The former diversification is consistent with the opening of the Hispanic Corridor during the late Sinemurian, which apparently allowed the pioneer dinoflagellate, Liasi-dium variabile, to invade the Tethys from the Paleo-Pacific. A true radiation pulse during the late Pliensbachian, with predominantly cold-water taxa, occurred during sea level fall, suggesting that climate change was critical to setting the evolutionary tempo. Our belemnite delta(18)O and Mg/Ca data indicate that late Pliensbachian water masses cooled (DeltaT approximate to -6degreesC) and became more saline (DeltaS approximate to +2 psu). Cooling episodes during generally warm and humid Early Jurassic climate conditions would have produced stronger winter monsoon northeast trade winds, resulting in hydrographic instability, increased vertical mixing, and ventilation of bottom waters. During the late Pliensbachian, dinoflagellates replaced green algae, including prasinophytes and acritarchs, as primary producers. By producing benthic resting cysts, dinoflagellates; may have been better adapted to oxidized ocean regimes. This hypothesis is supported by palynogical data from the early Toarcian ocean anoxic event, which was marked by highly stratified anoxic bottom water overlain by low-salinity, warm surface waters. These conditions were advantageous to green algae, while cyst-producing dinoflagellates temporarily disappeared. Our results suggest that the rise in dinoflagellate diversity later in the Jurassic appears to correspond to deep water ventilation as a result of the opening of the Atlantic seaway, conditions that appear to have simultaneously led to a loss of prasinophyte dominance in the global oceans.	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Geol. Sci.; [No title captured]	106	154	161	1	46	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0094-8373	1938-5331		PALEOBIOLOGY	Paleobiology	WIN	2005	31	1					73	97		10.1666/0094-8373(2005)031<0073:EJCCAT>2.0.CO;2	http://dx.doi.org/10.1666/0094-8373(2005)031<0073:EJCCAT>2.0.CO;2			25	Biodiversity Conservation; Ecology; Evolutionary Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology; Evolutionary Biology; Paleontology	887NT					2025-03-11	WOS:000226313500006
J	Oemcke, DJ; van Leeuwen, J				Oemcke, DJ; van Leeuwen, J			Ozonation of the marine dinoflagellate alga <i>Amphidinium</i> sp -: implications for ballast water disinfection	WATER RESEARCH			English	Article						ozonation; seawater; ballast water; disinfection; algae	BROMATE FORMATION; OZONE; BROMIDE	Ozone has been investigated for its potential to remove marine dinoflagellate algae from ships' ballast water. Dinoflagellate algae, Amphidinium sp. isolated froth the Great Barrier Reef, Townsville, Australia were used as indicators since these produce a type of cyst that is difficult to inactivate, but are relatively easy to culture. The ozonation experiments have demonstrated a high ozone demand for inactivation of the algal cultures, which increases as the culture ages. The main ozone demand in seawater is due to its reaction with bromide to form bromine compounds. The non-bromide ozone demand has been estimated by measuring the residuals produced after various doses of ozone. The Amphidinium sp. show an unexpected response to both ozonation and bromination, with an instantaneous inactivation of the organisms for all doses that produced an oxidant residual in the seawater, followed by an effect of the disinfection residual. The standard design procedure of comparing Ct will not be effective for predicting the response of the organism to varying dose, C, and contact tithe, t, and a plot of ozone produced oxidant residual against organism inactivation for various contact times is proposed for design purposes. High doses of ozone (5-11 mg/L) and up to 6 h of residual contact were required for a 4-log inactivation of the Amphidinium sp. Ozonation is likely to be a difficult technology to implement for organisms with this ozone requirement in combination with characteristics of ballast tanks, which contain areas of sediments high in detritus and areas of corrosion. (c) 2005 Elsevier Ltd. All rights reserved.	Provisor Pty Ltd, Glen Osmond, SA 5064, Australia; Iowa State Univ, Dept Civil Construct & Environm Engn, Ames, IA 50011 USA	Iowa State University	Provisor Pty Ltd, POB 243, Glen Osmond, SA 5064, Australia.	darren@provisor.com.au; leeuwen@iastate.edu						[Anonymous], 1992, STAND METH EX WAT WA; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Bolch C.J., 1993, Journal of Marine Environmental Engineering: 1993, P23; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; DEMAN JC, 1977, EUR J APPL MICROBIOL, V4, P307; HALLEGRAEFF GM, 1992, MAR POLLUT BULL, V25, P186, DOI 10.1016/0025-326X(92)90223-S; Hallegraeff Gustaaf M., 1997, Aquatic Ecology, V31, P47, DOI 10.1023/A:1009972931195; HOIGNE J, 1983, WATER RES, V17, P185, DOI 10.1016/0043-1354(83)90099-4; MCCARTHY SA, 1994, APPL ENVIRON MICROB, V60, P2597, DOI 10.1128/AEM.60.7.2597-2601.1994; Millero F.J., 1996, Chemical Oceanography, P469, DOI DOI 10.1016/S0144-8609(03)00061-X; OEMCKE, 1999, THESIS J COOK U; Oemcke D, 2004, OZONE-SCI ENG, V26, P389, DOI 10.1080/01919510490482241; Oemcke D., 1998, 23 CRC REEF RES; OEMCKE DJ, 1998, PORTS CORPORATION QU; Pilson MEQ., 1998, An Introduction to the Chemistry of the Sea, P431; Ribera M.A., 1995, PROGR PHYCOLOGICAL R, V11, P217; RICHARDSON LB, 1981, WATER RES, V15, P1067, DOI 10.1016/0043-1354(81)90074-9; STAEHELIN J, 1984, J PHYS CHEM-US, V88, P5999, DOI 10.1021/j150668a051; von Gunten U, 2003, WATER RES, V37, P1469, DOI 10.1016/S0043-1354(02)00458-X; VONGUNTEN U, 1994, ENVIRON SCI TECHNOL, V28, P1234, DOI 10.1021/es00056a009; *WEF, 1996, WAST DIS MAN PRACT F	21	49	55	2	40	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0043-1354			WATER RES	Water Res.	DEC	2005	39	20					5119	5125		10.1016/j.watres.2005.09.024	http://dx.doi.org/10.1016/j.watres.2005.09.024			7	Engineering, Environmental; Environmental Sciences; Water Resources	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology; Water Resources	000EB	16289281				2025-03-11	WOS:000234442600027
J	Drake, LA; Meyer, AE; Forsberg, RL; Baier, RE; Doblin, MA; Heinemann, S; Johnson, WP; Koch, M; Rublee, PA; Dobbs, FC				Drake, LA; Meyer, AE; Forsberg, RL; Baier, RE; Doblin, MA; Heinemann, S; Johnson, WP; Koch, M; Rublee, PA; Dobbs, FC			Potential invasion of microorganisms and pathogens via 'interior hull fouling': biofilms inside ballast water tanks	BIOLOGICAL INVASIONS			English	Article						bacteria; ballast water; Chesapeake Bay; Great Lakes; management; policy; virus	DINOFLAGELLATE CYSTS; SHIPS; TRANSPORT; IDENTIFICATION; BACTERIA	Surfaces submerged in an aquatic milieu are covered to some degree with biofilms - organic matrices that can contain bacteria, microalgae, and protozoans, sometimes including disease-causing forms. One unquantified risk of aquatic biological invasions is the potential for biofilms within ships' ballast water tanks to harbor pathogens, and, in turn, seed other waters. To begin to evaluate this vector, we collected biofilm samples from tanks' surfaces and deployed controlled-surface sampling units within tanks. We then measured a variety of microbial metrics within the biofilms to test the hypotheses that pathogens are present in biofilms and that biofilms have higher microbial densities compared to ballast water. Field experiments and sampling of coastwise and oceangoing ships arriving at ports in Chesapeake Bay and the North American Great Lakes showed the presence of abundant microorganisms, including pathogens, in biofilms. These results suggest that ballast-tank biofilms represent an additional risk of microbial invasion, provided they release cells into the water or they are sloughed off during normal ballasting operations.	Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA; Univ Buffalo, Ind Univ Ctr Biosurfaces, Buffalo, NY 14214 USA; Univ Utah, Dept Geol & Geophys, Salt Lake City, UT 84112 USA; Univ N Carolina, Dept Biol, Greensboro, NC 27402 USA	Old Dominion University; State University of New York (SUNY) System; University at Buffalo, SUNY; Utah System of Higher Education; University of Utah; University of North Carolina; University of North Carolina Greensboro	US Coast Guard Acad, Dept Sci, Marine Sci Sect, 27 Mohegan Ave, New London, CT 06320 USA.	lisa.a.drake@uscg.mil	Johnson, William/G-7733-2011; Doblin, Martina/E-8719-2013	Johnson, William/0000-0003-3126-3877; Doblin, Martina/0000-0001-8750-3433				Ali A, 2002, APPL ENVIRON MICROB, V68, P5773, DOI 10.1128/AEM.68.11.5773-5778.2002; AMANN RI, 1995, MICROBIOL REV, V59, P143, DOI 10.1128/MMBR.59.1.143-169.1995; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; [Anonymous], P 6 INT C MAR CORR F; *AUSTR QUAR INSP S, 2001, AQIS APPR BALL WAT M; Baier RE., 1984, MARINE BIODETERIORAT, P57; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; Carman KR, 1997, MICROSC RES TECHNIQ, V37, P116, DOI 10.1002/(SICI)1097-0029(19970415)37:2<116::AID-JEMT2>3.0.CO;2-M; Choopun N, 2002, APPL ENVIRON MICROB, V68, P995, DOI 10.1128/AEM.68.2.995-998.2002; CONOVER WJ, 1981, AM STAT, V35, P124, DOI 10.2307/2683975; Costerton JW, 1999, SCIENCE, V284, P1318, DOI 10.1126/science.284.5418.1318; DECHO AW, 1990, OCEANOGR MAR BIOL, V28, P73; Decho AW, 2000, CONT SHELF RES, V20, P1257, DOI 10.1016/S0278-4343(00)00022-4; DOBLIN MA, IN PRESS P 10 INT C; DOBLIN MA, 2003, 3 INT C MAR BIOINV L; Drake LA, 2002, MAR ECOL PROG SER, V233, P13, DOI 10.3354/meps233013; Drake Lisa A., 2001, Biological Invasions, V3, P193, DOI 10.1023/A:1014561102724; FORSBERG R, 2002, P 45 C GREAT LAK RES, P41; FORSBERG RL, 2003, THESIS STATE U NEW Y; Guillard R. 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Invasions	NOV	2005	7	6					969	982		10.1007/s10530-004-3001-8	http://dx.doi.org/10.1007/s10530-004-3001-8			14	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	980RI					2025-03-11	WOS:000233035500008
J	Patil, JG; Gunasekera, RM; Deagle, BE; Bax, NJ; Blackburn, SI				Patil, JG; Gunasekera, RM; Deagle, BE; Bax, NJ; Blackburn, SI			Development and evaluation of a PCR based assay for detection of the toxic dinoflagellate, <i>Gymnodinium catenatum</i> (Graham) in ballast water and environmental samples	BIOLOGICAL INVASIONS			English	Article						cyst; dinoflagellate; Gymnodinium catenatum; introduced pest; PCR detection	PFIESTERIA-PISCICIDA; PACIFIC COAST; IDENTIFICATION; STRAINS; PROBES	Gymnodinium catenatum is a bloom forming dinoflagellate that has been known to cause paralytic shellfish poisoning (PSP) in humans. It is being reported with increased frequency around the world, with ballast water transport implicated as a primary vector that may have contributed to its global spread. Major limitations to monitoring and management of its spread are the inability for early, rapid, and accurate detection of G. catenatum in plankton samples. This study explored the feasibility of developing a PCR-based method for specific detection of G. catenatumin cultures and heterogeneous ballast water and environmental samples. Sequence comparison of the large sub unit (LSU) ribosomal DNA locus of several strains and species of dinoflagellates allowed the design of G. catenatum specific PCR primers that are flanked by conserved regions. Assay specificity was validated through screening a range of dinoflagellate cultures, including the morphologically similar and taxonomically closely related species G. nolleri. Amplification of the diagnostic PCR product from all the strains of G. catenatum but not from other species of dinoflagellates tested imply the species specificity of the assay. Sensitivity of the assay to detect cysts in ballast water samples was established by simulated spiked experiments. The assay could detect G. catenatum in all 'blank' plankton samples that were spiked with five or more cysts. The assay was used to test environmental samples collected from the Derwent river estuary, Tasmania. Based on the results we conclude that the assay may be utilized in large scale screening of environmental and ballast water samples.	CSIRO Marine Res, Hobart, Tas 7001, Australia	Commonwealth Scientific & Industrial Research Organisation (CSIRO)	CSIRO Marine Res, GPO Box 1538, Hobart, Tas 7001, Australia.	jawahar.patil@csiro.au	Bax, Nicholas/A-2321-2012; Patil, Jawahar/B-9527-2012; Blackburn, Susan/M-9955-2013; Deagle, Bruce/A-9854-2008; Gunasekera, Rasanthi/A-2318-2012	Patil, Jawahar G/0000-0002-2154-4627; Deagle, Bruce/0000-0001-7651-3687; Gunasekera, Rasanthi/0000-0003-1990-2752				Abath FGC, 2002, BIOTECHNIQUES, V33, P1210, DOI 10.2144/02336bm05; [Anonymous], MAR BIOINV P 1 NAT C; BAX N, 2002, IUCN OCCASSIONAL PAP, V27, P26; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; Bolch CJS, 1999, J PHYCOL, V35, P356, DOI 10.1046/j.1529-8817.1999.3520356.x; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Carlton JT, 1996, ECOLOGY, V77, P1653, DOI 10.2307/2265767; Cohen AN, 1998, SCIENCE, V279, P555, DOI 10.1126/science.279.5350.555; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Deagle BE, 2003, MAR FRESHWATER RES, V54, P709, DOI 10.1071/MF03031; Doblin MA, 2000, J PLANKTON RES, V22, P421, DOI 10.1093/plankt/22.3.421; Drake LA, 2002, MAR ECOL PROG SER, V233, P13, DOI 10.3354/meps233013; Echelle AA, 1997, CONSERV BIOL, V11, P153, DOI 10.1046/j.1523-1739.1997.95427.x; ESTRADA M, 1984, INVEST PESQ, V48, P31; GELLER JB, 1994, MAR BIOL, V119, P243, DOI 10.1007/BF00349563; Godhe A, 2001, MAR BIOTECHNOL, V3, P152, DOI 10.1007/s101260000052; Graham Herbert W, 1943, TRANS AMER MICROSC SOC, V62, P259, DOI 10.2307/3223028; Haley ST, 1999, BIOTECHNIQUES, V26, P88, DOI 10.2144/99261st01; Hallegraeff G., 1986, Australian Fisheries, V45, P15; Hallegraeff G.M., 1989, P77; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hayes KR, 2003, MAR POLLUT BULL, V46, P91, DOI 10.1016/S0025-326X(02)00321-1; Hewitt C.L., 1999, 20 CSIRO MAR RES; Hill RS, 2001, MAR BIOL, V139, P279; LOEBLICH AR, 1975, J PHYCOL, V11, P80, DOI 10.1111/j.1529-8817.1975.tb02752.x; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; MEE LD, 1986, MAR ENVIRON RES, V19, P77, DOI 10.1016/0141-1136(86)90040-1; Miserez R, 1997, MOL CELL PROBE, V11, P103, DOI 10.1006/mcpr.1996.0088; Morgan TS, 2001, MAR BIOL, V139, P967; OLSON RR, 1991, NATURE, V351, P357, DOI 10.1038/351357b0; Rublee PA, 2001, ENVIRON HEALTH PERSP, V109, P765, DOI 10.2307/3454924; RYCHLIK W, 1996, OLIGO VER 5 0 MACINT; Saito K, 2002, APPL ENVIRON MICROB, V68, P5394, DOI 10.1128/AEM.68.11.5394-5407.2002; Saunders GW, 1997, PLANT SYST EVOL, P237; Schaffelke B, 2002, MAR POLLUT BULL, V44, P204, DOI 10.1016/S0025-326X(01)00202-8; Scholin CA, 1999, J PHYCOL, V35, P1356, DOI 10.1046/j.1529-8817.1999.3561356.x; Thompson JD, 1997, NUCLEIC ACIDS RES, V25, P4876, DOI 10.1093/nar/25.24.4876; Wuyts J, 2001, NUCLEIC ACIDS RES, V29, P175, DOI 10.1093/nar/29.1.175	41	24	29	2	29	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	1387-3547	1573-1464		BIOL INVASIONS	Biol. Invasions	NOV	2005	7	6					983	994		10.1007/s10530-004-3119-8	http://dx.doi.org/10.1007/s10530-004-3119-8			12	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	980RI					2025-03-11	WOS:000233035500009
J	Wilmsen, M; Niebuhr, B; Hiss, M				Wilmsen, M; Niebuhr, B; Hiss, M			The Cenomanian of northern Germany: facies analysis of a transgressive biosedimentary system	FACIES			English	Article						Cretaceous; Cenomanian; northern Germany; facies analysis; nearshore-to-open shelf; palaeoceanography	CALCAREOUS DINOFLAGELLATE CYSTS; SEQUENCE STRATIGRAPHY; LOWER SAXONY; TIME-SCALE; SEA; RECONSTRUCTION; PALEOCEANOGRAPHY; PHYTOPLANKTON; RESUSPENSION; SEDIMENTS	A facies analysis of the epicontinental marine Cenomanian sediments of northern Germany shows the presence of 17 facies types (FTs, including several sub-types) which can be assigned to three facies associations: 1) an inner shelf facies association (FT 1-8) with high amounts of terrigenous material and/or high-energy depositional features, 2) a middle shelf facies association (FT 915) of predominantly calcareous sediments with moderate amounts of generally fine siliciclastics, and 3) an outer shelf facies association (FT 16-17) of low-energy, fine-grained, pure limestones. These three facies associations roughly correspond to the well-known lithological units of the Cenomanian of northern Germany, i.e., the Essen Greensand/Cenomanian Marls complex, the Planer Limestones, and the Poor rhotomagense Limestones. The sediments were deposited on a northward-dipping homoclinal ramp with more-or-less shoreline-parallel facies belts. The sediment composition on this ramp-like shelf was a function of the varying importance of three different sediment sources: 1) terrigenous input from the south (Rhenobohemia), generally fining/decreasing in a proximal-distal (i.e., S-N) direction; 2) production of skeletal grains, mainly by macrobenthic organisms; and 3) settling of planktic carbonate (mainly calcispheres and calcareous nannofossils). In response to decreasing water energy with increasing water depth, the seaward decreasing terrigenous influence, and increasing planktic carbonate production, increasingly finer and more calcareous sediments were deposited in a proximal-distal transect. This rather straightforward picture was slightly modified by highest carbonate accumulation rates (planktic and benthic) on the middle shelf, forming a mid-shelf depocenter (fossiliferous, calcisphere-rich Planer Limestones). Time-transgressive, southward-directed onlap of this biosedimentary system during the Cenomanian caused a significant retreat of the coastline towards the south and a retrogradational stacking of facies belts, explaining the broadly similar facies development and lithology of Cenomanian successions across northern Germany. The boundaries of the lithological units, however, tend to be considerably diachronous in a distal-proximal transect. In the late Middle and early Late Cenomanian, a final drowning and facies levelling ("oceanization") is indicated by the widespread deposition of uniform calcareous nannofossil mudstones (Poor rhotomagense Limestones).	Univ Wurzburg, Inst Palaontol, D-97070 Wurzburg, Germany; Geol Dienst NRW Landesbetrieb, D-47803 Krefeld, Germany	University of Wurzburg	Univ Wurzburg, Inst Palaontol, Pleicherwall 1, D-97070 Wurzburg, Germany.	m.wilmsen@mail.uni-wuerzburg.de						[Anonymous], 1995, Geologie im Munsterland; [Anonymous], 1995, TERRA NOSTRA; [Anonymous], 1984, SCHRIFTENREIHE ERDWI; [Anonymous], GEOLOGISCHES JB A; [Anonymous], Z DTSCH GEOLOGISCHEN; Baldschuhn R., 1991, Generation, accumulation and production of Europe- hydrocarbons, P149; Bartling R., 1920, Z DT GEOL GES, V72, P161; BECKER BF, 1982, MUNSTERSCHE FORSCH G, V57, P137; Biju-DuvAl B., 2000, ATLAS PERI TETHYS PA; Brasier M.D., 1995, Geological Society Special Publication, V83, P113, DOI 10.1144/GSL.SP.1995.083.01.07; Carter D. 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J	Lilly, EL; Halanych, KM; Anderson, DM				Lilly, EL; Halanych, KM; Anderson, DM			Phylogeny, biogeography, and species boundaries within the <i>Alexandrium minutum</i> group	HARMFUL ALGAE			English	Article						Alexandrium; Andersonii; Angustitabulatum; biogeography; Insuetum; Lusitanicum; Minutum; morphology; phylogeny; taxonomy; Tamutum	DINOFLAGELLATE CYSTS; TOXIN COMPOSITION; GENETIC-MARKERS; NORTH-AMERICAN; DINOPHYCEAE; IDENTIFICATION; CATENELLA; STRAIN; REGION; HALIM	The geographic range and bloom frequency of the toxic dinoflagellate Alexandrium minutum and other members of the A. minutum group have been increasing over the past few decades. Some of these species are responsible for paralytic shellfish poisoning (PSP) outbreaks throughout the world. The origins of new toxic populations found in previously unaffected areas are typically not known due to a lack of reliable plankton records with sound species identifications and to the lack of a global genetic database. This paper provides the first comprehensive study of minutum-group morphology and phylogeny on a global scale, including 45 isolates from northern Europe, the Mediterranean, Asia, Australia and New Zealand. Neither the morphospecies Alexandrium lusitanicum nor A. angustitabulatum was recoverable morphologically, due to large variation within and among all minutum-group clonal strains in characters previously used to distinguish these species: the length: width of the anterior sulcal plate, shape of the V plate, connection between the V plate and the apical pore complex, and the presence of a ventral pore. DNA sequence data from the D1 to D2 region of the LSU rDNA also fail to recognize these species. Therefore, we recommend that all isolates previously designated as A. lusitanicum or A. angustitabulatum be redesignated as A. minutum. A. tamutum, A. insuetum, and A. andersonii are clearly different from A. minutum on the basis of both genetic and morphological data. A. minutum strains from Europe and Australia are closely related to one another, which may indicate an introduction from Europe to Australia given the long history of PSP in Europe and its recent occurrence in Australia. A minutum from New Zealand and Taiwan form a separate phylogenetic group. Most strains of A. minutum fit into one of these two groups, although there are a few outlying strains that merit further study and may represent new species. The results of this paper have greatly improved our ability to track the spread of A. minutum species and to understand the evolutionary relationships within the A. minutum group by correcting inaccurate taxonomy and providing a global genetic database. (c) 2005 Elsevier B.V All rights reserved.	Harvard Univ, Dept Organism & Evolutionary Biol, Biol Labs 4079, Cambridge, MA 02138 USA; Auburn Univ, Auburn, AL 36849 USA; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Harvard University; Auburn University System; Auburn University; Woods Hole Oceanographic Institution	Harvard Univ, Dept Organism & Evolutionary Biol, Biol Labs 4079, 16 Divin Ave, Cambridge, MA 02138 USA.	elilly@oeb.harvard.edu	anderson, david/E-6416-2011; Halanych, Kenneth/A-9480-2009	Halanych, Kenneth/0000-0002-8658-9674				Anderson D.M., 1989, P11; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], RED TIDE NEWSL; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Béchemin C, 1999, AQUAT MICROB ECOL, V20, P157, DOI 10.3354/ame020157; BELIN C, 1993, DEV MAR BIO, V3, P469; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; Chang FH, 1999, NEW ZEAL J MAR FRESH, V33, P533, DOI 10.1080/00288330.1999.9516898; Chang FH, 1997, TOXICON, V35, P393, DOI 10.1016/S0041-0101(96)00168-7; DESALAS MF, 2001, HARMFUL ALGAL BLOOMS, P214; Elbrächter M, 1998, HELGOLANDER MEERESUN, V52, P235, DOI 10.1007/BF02908899; Franco J.M., 1995, P53; FRANCO JM, 1994, J APPL PHYCOL, V6, P275, DOI 10.1007/BF02181938; Giacobbe MG, 1996, ESTUAR COAST SHELF S, V42, P539, DOI 10.1006/ecss.1996.0035; GIBSON T, 1994, CLUSTAL 10 IMPROVED; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Godhe A, 2001, MAR BIOTECHNOL, V3, P152, DOI 10.1007/s101260000052; Guillou L, 2002, PROTIST, V153, P223, DOI 10.1078/1434-4610-00100; Halim Y., 1960, Vie et Milieu, V11, P102; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1988, J PLANKTON RES, V10, P533, DOI 10.1093/plankt/10.3.533; Hansen G, 2003, HARMFUL ALGAE, V2, P317, DOI 10.1016/S1568-9883(03)00060-X; HONSELL G, 1993, DEV MAR BIO, V3, P127; Hwang DF, 1999, FISHERIES SCI, V65, P171, DOI 10.2331/fishsci.65.171; ISHIDA Y, 1993, DEV MAR BIO, V3, P881; Kim Keun-Yong, 2002, Algae, V17, P11; Lilly E.L., 2003, Phylogeny and biogeography of the toxic dinoflagellate Alexandrium; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; MACKENZIE L, 1997, NEW ZEAL J MAR FRESH, V41, P403; Mackenzie L, 1996, PHYCOLOGIA, V35, P148, DOI 10.2216/i0031-8884-35-2-148.1; Maddison DR., 2000, MACCLADE 4 ANAL PHYL; Martins CA, 2004, TOXICON, V43, P195, DOI 10.1016/j.toxicon.2003.11.023; Medlin LK, 1998, EUR J PROTISTOL, V34, P329, DOI 10.1016/S0932-4739(98)80060-6; MENDOZA H, 1995, J EXP MAR BIOL ECOL, V186, P103, DOI 10.1016/0022-0981(94)00160-F; Montpetit MJ, 2003, COMPUT NETW, V42, P1, DOI 10.1016/S1389-1286(03)00216-0; Montresor M, 2004, J PHYCOL, V40, P398, DOI 10.1111/j.1529-8817.2004.03060.x; MONTRESOR M, 1990, TOXIC MARINE PHYTOPLANKTON, P82; NASCIMENTO SM, IN PRESS J PHYCOL; Nehring S, 1998, ARCH FISH MAR RES, V46, P181; OSHIMA Y, 1989, NIPPON SUISAN GAKK, V55, P925, DOI 10.2331/suisan.55.925; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; SAKO Y, 1992, BIOSCI BIOTECH BIOCH, V56, P692, DOI 10.1271/bbb.56.692; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SCHOLIN CA, 1994, J PHYCOL, V30, P744, DOI 10.1111/j.0022-3646.1994.00744.x; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SCHOLIN CA, 1998, PHYSL ECOLOGY HARMFU, P13; Shimodaira H, 1999, MOL BIOL EVOL, V16, P1114, DOI 10.1093/oxfordjournals.molbev.a026201; Spalter RA, 1997, BIOCHEM SYST ECOL, V25, P231, DOI 10.1016/S0305-1978(96)00111-1; Swofford D., 2002, PAUP PHYLOGENETIC AN; TAMURA K, 1993, MOL BIOL EVOL, V10, P512, DOI 10.1093/oxfordjournals.molbev.a040023; Taylor F.J.R., 2003, Monographs on Oceanographic Methodology, V11, P389; Taylor F.J.R., 1995, Manual on Harmful Marine Microalgae, P283; TAYLOR FJR, 1993, DEV MAR BIO, V3, P81; Usup G, 2002, HARMFUL ALGAE, V1, P265, DOI [10.1016/S1568-9883(02)00044-6, 10.1016/S1568-9883(02)00003-3]; Vila M, 2001, MAR ECOL PROG SER, V222, P73, DOI 10.3354/meps222073; ZARDOYA R, 1995, J MOL EVOL, V41, P637	59	83	87	2	29	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	NOV	2005	4	6					1004	1020		10.1016/j.hal.2005.02.001	http://dx.doi.org/10.1016/j.hal.2005.02.001			17	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	984SZ					2025-03-11	WOS:000233325900005
J	Kolár, J; Machácková, I				Kolár, J; Machácková, I			Melatonin in higher plants:: occurrence and possible functions	JOURNAL OF PINEAL RESEARCH			English	Review						antioxidant; circadian rhythms; higher plants; melatonin; melatonin determination; photoperiodism; reactive oxygen species	HYPERICUM-PERFORATUM L.; IN-VITRO; IMMUNOAFFINITY CHROMATOGRAPHY; CHENOPODIUM-RUBRUM; MASS-SPECTROMETRY; OXIDATIVE STRESS; PINEAL-GLAND; NEUROHORMONE MELATONIN; ANTIOXIDANT ENZYMES; GONYAULAX-POLYEDRA	Melatonin may be ubiquitous in the plant kingdom. This review considers the evaluation of methods of melatonin determination in plant material and possible melatonin functions in plants. Concerning the determination methods, the only reliable techniques are liquid chromatography - mass spectrometry or gas chromatography - mass spectrometry after some purification steps of the extract. Melatonin was shown to delay flower induction in some photoperiodic plants and in the dinoflagellate Lingulodinium it replaces, in part, the requirement of darkness for cyst formation. Melatonin may also have a function as an antioxidant and it may possess some auxin-like effects. Finally, it may act as a signal for interaction of plants with herbivores and pests. Further research is needed to clarify these potential functions.	Acad Sci Czech Republ, Inst Expt Bot, CR-16502 Prague, Czech Republic	Czech Academy of Sciences; Institute of Experimental Botany of the Czech Academy of Sciences	Acad Sci Czech Republ, Inst Expt Bot, Rozvojova 135, CR-16502 Prague, Czech Republic.	machackova@ueb.cas.cz						Acuna Castroviejo Dario, 2002, Curr Top Med Chem, V2, P133; [Anonymous], THESIS CHARLES U PRA; [Anonymous], CURR MED CHEM; [Anonymous], CELL BIOL PROBLEMS C; [Anonymous], 1997, THESIS U CALIFORNIA; Antolin I, 1996, FASEB J, V10, P882, DOI 10.1096/fasebj.10.8.8666165; Antolin Isaac, 1997, P86; Antón-Tay F, 1998, J PINEAL RES, V24, P35, DOI 10.1111/j.1600-079X.1998.tb00363.x; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; BALZER I, 1998, WORKSH EUR SOC CHRON; BANERJEE S, 1973, EXP CELL RES, V78, P314, DOI 10.1016/0014-4827(73)90074-8; BARTNESS TJ, 1989, EXPERIENTIA, V45, P939, DOI 10.1007/BF01953051; Baydas G, 2002, NEUROSCI LETT, V323, P195, DOI 10.1016/S0304-3940(02)00144-1; BENITEZKING G, 1993, EXPERIENTIA, V49, P635; BenitezKing G, 1996, BBA-GEN SUBJECTS, V1290, P191, DOI 10.1016/0304-4165(96)00025-6; BENITEZKING G, 1993, LIFE SCI, V53, P201, DOI 10.1016/0024-3205(93)90670-X; Blask DE, 2004, CARCINOGENESIS, V25, P951, DOI 10.1093/carcin/bgh090; BRAINARD GC, 1982, NEUROENDOCRINOLOGY, V35, P342, DOI 10.1159/000123405; Brusco LI, 1998, J PINEAL RES, V25, P260, DOI 10.1111/j.1600-079X.1998.tb00396.x; Burkhardt S, 2001, J AGR FOOD CHEM, V49, P4898, DOI 10.1021/jf010321+; CASSONE VM, 1990, TRENDS NEUROSCI, V13, P457, DOI 10.1016/0166-2236(90)90099-V; Chen GF, 2003, LIFE SCI, V73, P19, DOI 10.1016/S0024-3205(03)00252-2; CUMMING BG, 1985, CRC HDB FLOWERING, P196; DUBBELS R, 1995, J PINEAL RES, V18, P28, DOI 10.1111/j.1600-079X.1995.tb00136.x; EDMONDS K, 2000, 7 M SOC RES BIOL RHY; FINOCCHIARO L, 1988, J NEUROCHEM, V50, P382, DOI 10.1111/j.1471-4159.1988.tb02923.x; FLETCHER RA, 1997, 5 CAN PIN MEL S GUEL; Fu I, 1998, J PHARMACEUT BIOMED, V18, P347, DOI 10.1016/S0731-7085(98)00048-X; Fuhrberg B, 1996, PLANTA, V200, P125; Gitto E, 2001, PEDIATR RES, V50, P756, DOI 10.1203/00006450-200112000-00021; Gitto E, 2001, INTENS CARE MED, V27, P1116, DOI 10.1007/s001340100977; Goldman BD, 2001, J BIOL RHYTHM, V16, P283, DOI 10.1177/074873001129001980; Hardeland R, 1999, REPROD NUTR DEV, V39, P399, DOI 10.1051/rnd:19990311; HARDELAND R, 1993, NEUROSCI BIOBEHAV R, V17, P347, DOI 10.1016/S0149-7634(05)80016-8; Hardeland R, 2003, J PINEAL RES, V34, P233, DOI 10.1034/j.1600-079X.2003.00040.x; HARDELAND R, 1994, CELL BIOL PROBLEMS C, P136; Hardeland R., 1996, Trends in Comparative Biochemistry and Physiology, V2, P25; HARDELAND R, 2000, MELATONIN 4 DECADES, P387; HATTORI A, 1995, BIOCHEM MOL BIOL INT, V35, P627; Hernández-Ruiz J, 2004, PLANTA, V220, P140, DOI 10.1007/s00425-004-1317-3; JACKSON WT, 1969, J CELL SCI, V5, P745; Jou MJ, 2004, J PINEAL RES, V37, P55, DOI 10.1111/j.1600-079X.2004.00140.x; KATEKAR GF, 1979, PHYTOCHEMISTRY, V18, P223, DOI 10.1016/0031-9422(79)80059-X; Kolar J, 1997, PHYTOCHEMISTRY, V44, P1407, DOI 10.1016/S0031-9422(96)00568-7; Kolár J, 2003, PHYSIOL PLANTARUM, V118, P605, DOI 10.1034/j.1399-3054.2003.00114.x; KOLAR J, 1996, THESIS CHARLES U PRA; León J, 2005, J PINEAL RES, V38, P1, DOI 10.1111/j.1600-079X.2004.00181.x; LERNER AB, 1958, J AM CHEM SOC, V80, P2587, DOI 10.1021/ja01543a060; LEWY AJ, 1978, SCIENCE, V201, P741, DOI 10.1126/science.675255; LEWY AJ, 2000, MELATONIN 4 DECADES, P425; López-Burillo S, 2003, J PINEAL RES, V34, P269, DOI 10.1034/j.1600-079X.2003.00041.x; LUNING K, 2000, 2 WORKSH EUR SOC CHR; Mahal HS, 1999, FREE RADICAL BIO MED, V26, P557, DOI 10.1016/S0891-5849(98)00226-3; Manchester LC, 2000, LIFE SCI, V67, P3023, DOI 10.1016/S0024-3205(00)00896-1; Marshall KA, 1996, FREE RADICAL BIO MED, V21, P307, DOI 10.1016/0891-5849(96)00046-9; Martín M, 2000, FASEB J, V14, P1677; Martin M., 2001, Int. 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Pineal Res.	NOV	2005	39	4					333	341		10.1111/j.1600-079X.2005.00276.x	http://dx.doi.org/10.1111/j.1600-079X.2005.00276.x			9	Endocrinology & Metabolism; Neurosciences; Physiology	Science Citation Index Expanded (SCI-EXPANDED)	Endocrinology & Metabolism; Neurosciences & Neurology; Physiology	971MV	16207287	Bronze			2025-03-11	WOS:000232389300001
J	Figueroa, RI; Bravo, I; Garcés, E				Figueroa, RI; Bravo, I; Garcés, E			Effects of nutritional factors and different parental crosses on the encystment and excystment of <i>Alexandrium catenella</i> (Dinophyceae) in culture	PHYCOLOGIA			English	Article							DINOFLAGELLATE GONYAULAX-TAMARENSIS; RED-TIDE DINOFLAGELLATE; SEXUAL REPRODUCTION; RESTING CYSTS; LIFE-CYCLE; GYMNODINIUM-CATENATUM; POPULATION-DYNAMICS; GERMINATION; TEMPERATURE; EXCAVATA	Alexandrium catenella is a cyst-forming dinoflagellate causative of paralytic shellfish poisoning. Strain and nutritional factors affecting cyst formation and germination in this species were studied in cultures of several clonal crosses. Sexual reproduction was monitored and the effect of nutrients on sexual stages was proved because planozygotes isolated in medium with no phosphates added encysted in lower percentages than those placed in media with no nitrates added or in replete conditions, where the highest encystment was achieved. However, other unknown factors prevented encystment, because, even in replete conditions, some planozygotes were unable to encyst. Dormancy period of cysts ranged from 5 to 65 days at 24 degrees C. A progressive germination inside this time interval was recorded for cysts from all six clonal crosses employed, and therefore, identified as a species characteristic. This gadual germination was modulated by nutrient levels in both encystment and excystment media: (1) cysts formed in conditions where nitrates and phosphates were added needed more time to excyst than those from media lacking one of these nutrients and (2) cysts from any encystment treatment germinated faster, and in higher percentages in poor external conditions compared to those placed in replete L I medium. More than 90% of the cysts isolated to seawater germinated in less than 20 days, whereas those isolated to L I medium had not begun to excyst, and, after 60 days, the percentage of germinated cysts in replete conditions remained below 40%. However, ultimate germination frequencies and postmeiotic viability of cysts might depend on genetic characteristics because cysts from the clonal crosses of A. catenella employed showed significant differences. Ecdysal cysts were mainly observed under the treatments in which the smallest number of resting cysts were produced. In 65% of the cases germination of these cysts under replete conditions occurred within 15 days.	Inst Oceanog Vigo, Vigo 36200, Spain; CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Inst Oceanog Vigo, Cabo Estai Canido, Vigo 36200, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011	Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X; Bravo, Isabel/0000-0003-3764-745X				Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; AN KH, 1992, BOT MAR, V35, P61, DOI 10.1515/botm.1992.35.1.61; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CANNON JA, 1993, DEV MAR BIO, V3, P103; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Huber G., 1923, FLORA JENA, V116, P114; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Nagai Satoshi, 2004, Plankton Biology and Ecology, V51, P103; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; SAMPEDRO N, 2004, 8 REUN IB FIT TOX BI, P29; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; TAKEUCHI T, 1995, 7 C TOX PHYT SEND JA; UCHIDA T, 1991, NIPPON SUISAN GAKK, V57, P1215, DOI 10.2331/suisan.57.1215; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Vila M, 2001, MAR ECOL PROG SER, V222, P73, DOI 10.3354/meps222073; WALKER LM, 1979, J PHYCOL, V15, P312; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; YOSHIMATSU S, 1984, Bulletin of Plankton Society of Japan, V31, P107	41	67	77	2	38	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	NOV	2005	44	6					658	670		10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2	http://dx.doi.org/10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2			13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	981XD					2025-03-11	WOS:000233120400009
J	Riding, JB				Riding, JB			<i>Fostericysta</i> Riding nom. nov (Division <i>Dinoflagellata</i>)	TAXON			English	Editorial Material						Australia; dinoflagellate cysts; Iridaceae; Jurassic; taxonomy		The Jurassic dinoflagellate cyst genus Fosteria Riding & Helby 2001 is a later (junior) homonym of Fosteria Molseed 1968, a genus of the Iridaceae. The generic name Fostericysta is proposed here to replace Fosteria Riding & Helby 2001.	British Geol Survey, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	British Geol Survey, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk						FOSTER CB, 2001, AUSTRALASIAN PALAEON, V24, pR1; MOLSEED E, 1968, BRITTONIA, V20, P232, DOI 10.2307/2805447; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P111	3	1	1	1	2	INT ASSOC PLANT TAXONOMY-IAPT	BRATISLAVA	C/O INST BOTANY, SLOVAK ACAD SCIENCES DUBRAVSKA CESTA 9, SK-845 23 BRATISLAVA, SLOVAKIA	0040-0262	1996-8175		TAXON	Taxon	NOV	2005	54	4					1091	1091		10.2307/25065498	http://dx.doi.org/10.2307/25065498			1	Plant Sciences; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Evolutionary Biology	005HG					2025-03-11	WOS:000234812600027
J	Mudie, PJ; Rochon, A; Levac, E				Mudie, Peta J.; Rochon, Andre; Levac, Elisabeth			Decadal-scale sea ice changes in the Canadian Arctic and their impacts on humans during the past 4,000 years	ENVIRONMENTAL ARCHAEOLOGY			English	Article						ARCTIC ARCHAEOLOGY; GREENLAND; PALAEOCLIMATE; P ALAEOESKIMO; PALYNOLOGY; SEA ICE	ENVIRONMENTAL-CHANGE; SURFACE CONDITIONS; NORTH-ATLANTIC; BAFFIN-BAY; GREENLAND; ARCHIPELAGO; VARIABILITY; RECORD; OSCILLATIONS; ASSEMBLAGES	Climate warming of >1.5 degrees C over three decades has diminished Arctic sea ice and forced drastic changes on Inuit people of the Canadian Arctic. Discontinuities in archaeological records also suggest that climatic changes may have caused site abandonment and life style shifts in Paleo- and Neo-eskimo societies. We therefore examine the decadal-scale palaeoclimatic changes recorded by quantitative palynological data in marine records from Coburg Polynya, near Palaeo- and Neo-eskimo settlements on the North Devon Lowlands, and from the North Water Polynya between Canada and Northwest Greenland. Palaeotransfer functions from dinoflagellate cyst assemblages provide quantitative estimates of changes in sea surface temperature (SST) and sea ice cover (SIC) with the accuracy of historical measurements. Both sites record temperature variations of 2-4 degrees C corresponding to changes in hunting modes and occupation-abandonment cycles on Devon and Ellesmere Islands. Our data show that from similar to 6500 to 2600 BP, there were large oscillations in summer SST from 2-4 degrees C cooler than present to 6 degrees C warmer and SIC ranged from 2 months more sea ice to 4 months more open water. The warmer interval corresponds to the period of pre-Dorset cultures that hunted muskox and caribou. Subsequent marine-based Dorset and Neo-eskimo cultures correspond to progressively cooler intervals with expanded sea ice cover. The warming took similar to 50-100 years and lasted similar to 300 years before replacement by colder intervals lasting similar to 200-500 years. These climate oscillations are more rapid than the archaeological cultural changes, but are of similar length to successive Palaeoeskimo occupations in the Nares Strait region.	[Mudie, Peta J.] Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 1V5, Canada; [Levac, Elisabeth] St Francis Xavier Univ, Dept Earth Sci, Antigonish, NS B2G 2W5, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Quebec; Saint Francis Xavier University - Canada	Mudie, PJ (通讯作者)，Geol Survey Canada Atlantic, Nat Resources Canada, Box 1006, Dartmouth, NS B2Y 4A2, Canada.	mudiep@ns.sympatico.ca						Alt BT., 1985, The Franklin era in Canadian Arctic history, 1845 - 1859, P69; ANDREWS JT, 1991, CONT SHELF RES, V11, P791, DOI 10.1016/0278-4343(91)90080-P; Appelt M., 1998, MAN CULTURE ENV ANCI, P136; Bard E-., 1987, CLIM DYNAM, V1, P101; Barlow LK, 2001, CLIMATIC CHANGE, V48, P101, DOI 10.1023/A:1005629914868; BARRY RG, 1977, ARCTIC ALPINE RES, V9, P193, DOI 10.2307/1550581; Beattie Owen., 1988, FROZEN TIME; Bischof J., 2000, S-P BKS ENVIRONM SCI; Blake W., 1975, Geografiska Annaler, V57A, P1; Buckland PC, 1996, ANTIQUITY, V70, P88, DOI 10.1017/S0003598X00082910; Chapman MR, 1998, PALEOCEANOGRAPHY, V13, P311, DOI 10.1029/98PA01067; CHAPMAN WL, 1993, B AM METEOROL SOC, V74, P33, DOI 10.1175/1520-0477(1993)074<0033:RVOSIA>2.0.CO;2; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Douglas MSV, 2004, P NATL ACAD SCI USA, V101, P1613, DOI 10.1073/pnas.0307570100; Doyle A., 2003, REUTERS NEWS    1211; Dyke AS, 1997, ARCTIC, V50, P1; Dyke AS, 1996, ARCTIC, V49, P235; Dyke AS, 1996, GEOGR PHYS QUATERN, V50, P125, DOI 10.7202/033087ar; Dyke AS, 1999, ARCTIC, V52, P160; Furgal C.M., 2002, EARTH IS FASTER NOW, P267; Gadsby P., 2004, DISCOVER MAGAZIN JAN; Grumet NS, 2001, CLIMATIC CHANGE, V49, P129, DOI 10.1023/A:1010794528219; HELMER JW, 1992, J FIELD ARCHAEOL, V19, P291, DOI 10.1179/009346992791548888; HELMER JW, 1991, ARCTIC, V44, P301; Houghton JT, 2001, CLIMATE CHANGE 2001: THE SCIENTIFIC BASIS, P1; JACOBS JD, 1979, ARCTIC, V32, P345; Jennings AE, 2001, CLIMATIC CHANGE, V48, P83, DOI 10.1023/A:1005658620319; JOHANNESSEN OM, 1995, NATURE, V376, P126, DOI 10.1038/376126a0; Johannessen OM, 1999, SCIENCE, V286, P1937, DOI 10.1126/science.286.5446.1937; Koch L., 1945, E GREENLAND ICE; Krupnik I., 2002, EARTH IS FASTER NOW; Lamoureux SF, 2004, QUATERNARY RES, V61, P134, DOI 10.1016/j.yqres.2003.11.003; Levac E, 2001, J QUATERNARY SCI, V16, P353, DOI 10.1002/jqs.614; Lubbock B., 1937, ARCTIC WHALERS; Lynnerup N, 2004, POLAR REC, V40, P107, DOI 10.1017/S0032247402002875; MacLean B., 1984, GEOLOGICAL SURVEY CA, V84, P359; Maxwell MoreauS., 1976, E ARCTIC PREHISTORY, P1; Maxwell MoreauS., 1985, PREHISTORY E ARCTIC; McGhee Robert., 1976, Eastern Arctic Prehistory: Paleoeskimo Problems, P15; McGhee Robert., 1996, ANCIENT PEOPLE ARCTI; Mobjerg T., 1998, MAN CULTURE ENV ANCI, V4, P98; Mudie P. 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Archaeol.	OCT	2005	10	2					113	126		10.1179/env.2005.10.2.113	http://dx.doi.org/10.1179/env.2005.10.2.113			14	Archaeology; Environmental Sciences; Geosciences, Multidisciplinary	Arts &amp; Humanities Citation Index (A&amp;HCI)	Archaeology; Environmental Sciences & Ecology; Geology	V28AR					2025-03-11	WOS:000208654200001
J	Hosoi-Tanabe, S; Tomishima, S; Nagai, S; Sako, Y				Hosoi-Tanabe, S; Tomishima, S; Nagai, S; Sako, Y			Identification of a gene induced in conjugation-promoted cells of toxic marine dinoflagellates <i>Alexandrium tamarense</i> and <i>Alexandrium catenella</i> using differential display analysis	FEMS MICROBIOLOGY LETTERS			English	Article						toxic dinoflagellate; Alexandrium; paralytic shellfish poisoning; encystment; differential display; sporulation-specific gene	GONYAULAX-TAMARENSIS; SACCHAROMYCES-CEREVISIAE; TRANSCRIPTION; DINOPHYCEAE; SPORULATION; BLOOMS	Marine dinoflagellates Alexandrium tamarense and Alexandrium catenella produce toxins that cause paralytic shellfish poisoning (PSP). A detailed mechanism of encystment is necessary for a better understanding of bloom dynamics and the toxic effect of these organisms. In this study, a cDNA that was up-regulated in conjugation-promoted cells at encystment was identified using differential display. It encoded a polypeptide of 195 amino acids with a molecular weight of 20,900 Da. The deduced amino acid sequence of this cDNA showed 62% similarity with the polypeptide encoded by SPS19, a gene that is activated specifically during spore maturation and spore wall formation in Saccharomyces cerevisiae. Therefore, the cDNA obtained was termed an SPS19 homolog in this study. The expression levels of the SPS19 homolog were highest immediately after the promotion of conjugation and decreased sequentially later, a pattern similar to that of SPS19 in the sporulation of S. cerevisiae in terms of the time of induction and the duration of expression. These similarities between the SPS19 homolog and SPS19 suggested that the putative function of the SPS19 homolog might be an involvement in encystment. RT-PCR showed that the expression of the SPS19 homolog was highest in conjugation-promoted cells but low in vegetative cells. The SPS19 homolog was believed to be expressed constantly in order for cells to respond rapidly to environmental changes and ensure encystment. Characterization of the identified gene might help in understanding the mechanism of encystment. (c) 2005 Federation of European Microbiological Societies. Published by Elsevier B.V. All rights reserved.	Shiga Univ Med Sci, Sch Environm Sci, Dept Ecosyst Studies, Shiga 5228533, Japan; Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Lab Marine Microbiol, Kyoto 6068502, Japan; Fisheries Res Agcy Japan, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Toxic Phytoplankton Sect, Hiroshima 7390452, Japan	Shiga University of Medical Science; Kyoto University; Japan Fisheries Research & Education Agency (FRA)	Shiga Univ Med Sci, Sch Environm Sci, Dept Ecosyst Studies, 2500 Hassaka Cho, Shiga 5228533, Japan.	syonatsu@ses.usp.ac.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Carginale V, 2004, GENE, V332, P29, DOI 10.1016/j.gene.2004.02.030; COE JGS, 1994, MOL GEN GENET, V244, P661, DOI 10.1007/BF00282757; DICKINSON JR, 1988, MICROBIOL SCI, V5, P121; Diener LC, 2004, ENVIRON TOXICOL, V19, P179, DOI 10.1002/tox.20010; Dong JZ, 2004, PLANTA, V218, P483, DOI 10.1007/s00425-003-1124-2; GUILLARD RRL, 1962, GRAN CAN J MICROBIOL, V8, P229; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Hosoi-Tanabe S, 2005, HARMFUL ALGAE, V4, P319, DOI 10.1016/j.hal.2004.04.002; Kim H, 2002, EUKARYOT CELL, V1, P987, DOI 10.1128/EC.1.6.987-999.2002; KURJAN J, 1993, ANNU REV GENET, V27, P147; LAW DT, 1998, MOL CELL BIOL, V8, P912; NAGAI S, 2004, JAPAN PLANKTON BIOL, V51, P103; SHIMIZU Y, 1993, CHEM REV, V93, P1685, DOI 10.1021/cr00021a002; Shumway Sandra E., 1994, Natural Toxins, V2, P236, DOI 10.1002/nt.2620020413; Taroncher-Oldenburg G, 2000, APPL ENVIRON MICROB, V66, P2105, DOI 10.1128/AEM.66.5.2105-2112.2000; Tillett D, 2000, J PHYCOL, V36, P251, DOI 10.1046/j.1529-8817.2000.99079.x; Waters AP, 1997, J BIOL CHEM, V272, P3583, DOI 10.1074/jbc.272.6.3583	22	10	10	0	2	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0378-1097	1574-6968		FEMS MICROBIOL LETT	FEMS Microbiol. Lett.	OCT 1	2005	251	1					161	168		10.1016/j.femsle.2005.07.046	http://dx.doi.org/10.1016/j.femsle.2005.07.046			8	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	968WQ	16140475				2025-03-11	WOS:000232194100023
J	Kamikawa, R; Hosoi-Tanabe, S; Nagai, S; Itakura, S; Sako, Y				Kamikawa, R; Hosoi-Tanabe, S; Nagai, S; Itakura, S; Sako, Y			Development of a quantification assay for the cysts of the toxic dinoflagellate <i>Alexandrium tamarense</i> using real-time polymerase chain reaction	FISHERIES SCIENCE			English	Article						Alexandrium tamarense; cyst; dinoflagellate; paralytic shellfish poisoning (PSP); real-time PCR		The cysts of toxic dinoflagellate Alexandrium tamarense are the seed population for the bloom responsible for paralytic shellfish poisoning (PSP). However, it is impossible to identify the Alexandrium spp. cyst on the basis of morphological features. In this study, we prepared A. tamarense cysts by sexual conjugation in laboratory conditions and developed an efficient DNA extraction method for polymerase chain reaction (PCR) assay. Using the A. tamarense cysts, we established the identification and quantification method showing the species specificity and the high sensistivity for A. tamarense cysts using real-time PCR. This assay was also able to detect and quantify the A. tamarense cysts accurately when mixed with excess cysts of A. catenella (Whedon and Kofoid) Balech prepared by conjugation experiment.	Kyoto Univ, Lab Marine Microbiol, Div Appl Biosci, Grad Sch Agr, Kyoto 6068502, Japan; Univ Shiga Prefecture, Sch Environm Sci, Dept Ecosyst Studies, Shiga 5228533, Japan; Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Hiroshima 7390452, Japan	Kyoto University; University Shiga Prefecture; Japan Fisheries Research & Education Agency (FRA)	Kyoto Univ, Lab Marine Microbiol, Div Appl Biosci, Grad Sch Agr, Kyoto 6068502, Japan.	kami_88@kais.kyoto-u.ac.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063				Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.x; ADACHI M, 1993, NIPPON SUISAN GAKK, V59, P1171; Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Catterall WA, 2000, NEURON, V26, P13, DOI 10.1016/S0896-6273(00)81133-2; Cembella A.D., 1985, P55; DALL B, 1979, TOXIC DINOFLAGELLATE, P443; FUKUYO Y, 1985, B MAR SCI, V37, P529; Galluzzi L, 2004, APPL ENVIRON MICROB, V70, P1199, DOI 10.1128/AEM.70.2.1199-1206.2004; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; Hosoi-Tanabe S, 2005, HARMFUL ALGAE, V4, P319, DOI 10.1016/j.hal.2004.04.002; HOSOITANABE S, 2003, THESIS KYOTO U KYOTO; Matsuoka K., 1989, P461; PORTER RD, 1988, METHOD ENZYMOL, V167, P703; Sako Y, 2004, J PHYCOL, V40, P598, DOI 10.1111/j.1529-8817.2004.03035.x; SAKO Y, 1995, KAIYO, V27, P628; SCHWINGHAMER P, 1991, LIMNOL OCEANOGR, V36, P588, DOI 10.4319/lo.1991.36.3.0588; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Yamaguchi M, 2002, FISHERIES SCI, V68, P1012, DOI 10.1046/j.1444-2906.2002.00526.x; Yamasaki T, 2001, NDT&E INT, V34, P207, DOI 10.1016/S0963-8695(00)00060-8; Zhou ZH, 1999, NEW PHYTOL, V144, P55, DOI 10.1046/j.1469-8137.1999.00504.x	24	27	31	1	10	SPRINGER JAPAN KK	TOKYO	CHIYODA FIRST BLDG EAST, 3-8-1 NISHI-KANDA, CHIYODA-KU, TOKYO, 101-0065, JAPAN	0919-9268	1444-2906		FISHERIES SCI	Fish. Sci.	OCT	2005	71	5					987	991		10.1111/j.1444-2906.2005.01055.x	http://dx.doi.org/10.1111/j.1444-2906.2005.01055.x			5	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	980XL					2025-03-11	WOS:000233051400005
J	Clauzon, G; Suc, JP; Popescu, SM; Marunteanu, M; Rubino, JL; Marinescu, F; Melinte, MC				Clauzon, G; Suc, JP; Popescu, SM; Marunteanu, M; Rubino, JL; Marinescu, F; Melinte, MC			Influence of Mediterranean sea-level changes on the Dacic Basin (Eastern Paratethys) during the late Neogene: The Mediterranean Lago Mare facies deciphered	BASIN RESEARCH			English	Review							MESSINIAN EROSIONAL SURFACE; MIOCENE LAKE PANNON; CENTRAL APENNINES; CANYON PROVENCE; SALINITY CRISIS; STRATIGRAPHY; CHRONOLOGY; EVOLUTION; PLIOCENE; WESTERN	A recently published scenario viewing the Messinian salinity crisis as two evaporitic steps rather than one has led to a search for new indices of the crisis in the Eastern Paratethys. Fluvial processes characterized the southwestern Dacic Basin (Southern Romania, i.e. the Carpathian foredeep) whereas brackish sediments were continuously deposited in its northern part. This is consistent with previously evidenced responses of the Black Sea to the Messinian salinity crisis. High sea-level exchanges between the Mediterranean Sea and Eastern Paratethys are considered to have occurred just before and just after desiccation of the Mediterranean. This accounts for two successive Mediterranean nannoplankton-dinocyst influxes into the Eastern Paratethys that, respectively, belong to zones NN 11 and NN 12. Meanwhile, two separate events that gave rise to Lago Mare facies (with Paratethyan Congeria, ostracods and/or dinoflagellate cysts) arose in the Mediterranean Basin in response to these high sea-level exchanges and located 5.52 and 5.33 Ma (isotopic stages TG 11 and TG 5, respectively), i.e. just before and just after the almost complete desiccation of the Mediterranean). These Lago Mare facies formed independently of lakes with ostracods of the Cyprideis group that developed in the central basins during the final stages of desiccation. The gateway faciliting these water exchanges is not completely identified. A proto-Bosphorus strait seems unlikely. A plausible alternative route extends from the northern part of the Thessaloniki region up to the Dacic Basin and through Macedonia and the Sofia Basin. The expression 'Lago Mare' is chronostratigraphically ambiguous and should be discontinued for this purpose, although it might remain useful as a palaeoenvironmental term.	Univ Lyon 1, CNRS, UMR 5125, Lab PaleoEnvironm & PaleobioSphere, F-69622 Villeurbanne, France; Univ Paul Cezanne, Europole Arbois, CEREGE, CNRS,UMR 6635, Aix En Provence, France; Geol Inst Romania, Bucharest, Romania; CSTTF, TOTAL, TG ISS, Pau, France; Natl Inst Marine Geol & Geoecol, Bucharest, Romania	Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Geological Institute of Romania; Total SA; National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar)	Univ Lyon 1, CNRS, UMR 5125, Lab PaleoEnvironm & PaleobioSphere, 27-43 Blvd 11 Novembre, F-69622 Villeurbanne, France.	jean-pierre.suc@univ-lyon1.fr	Mihaela, mihaela/AAF-5894-2021	Popescu, Speranta- Maria/0000-0001-5345-395X; Melinte-Dobrinescu, Mihaela Carmen/0000-0003-4716-6844				ALERIA, 1980, GEOLOGIE MEDITERRANE, V7, P5; Almera J., 1894, MEM R ACAD CIENC ART, P1; [Anonymous], ROMANIAN J STRATIGRA; [Anonymous], 1998, ROM J STRATIGR; [Anonymous], 1974, FOSSIL LIVING DINOFL; [Anonymous], MEM SOC GEOL ITAL; Archambault-Guezou J., 1976, Bulletin de la Societe Geologique de France, V18, P1267; Archambault-Guezou J., 1979, ANN GEOL PAYS HELL, V1, P27; Backman Jan, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V154, P83; Ballesio R., 1972, Docum Lab Geol Fac Sci Lyon, V53, P1; BARBER PM, 1981, MAR GEOL, V44, P253, DOI 10.1016/0025-3227(81)90053-0; Bassetti M., 1994, MEM SOC GEOL ITAL, V48, P275; Benson R.H., 1978, Initial Reports of the Deep Sea Drilling Project, V42, P1039; BENSON RH, 1976, PALAEOGEOGR PALAEOCL, V20, P147, DOI 10.1016/0031-0182(76)90028-6; Berggren W.A., 1995, SPEC PUBL SOC EC PAL, V54, P141; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; Bertini A., 1995, ROM J STRATIGR S7, V76, P141; BERTINI A, 1992, THESIS U FLORENCE; Bertoldi G, 2002, J HIGH ENERGY PHYS; BIZON JJ, 1978, B MUS NATN HIST NA 3, V518, P123; BLANCVALLERON MM, 1998, P OCEAN DRILLING PRO, V160, P437; Bonaduce G., 1999, SOC GEOL ITAL MEM, V54, P83; BOSSIO A, 1978, MESSINIAN SEMINAR, V4, P88; BOSSIO A, 1981, 9 C SOC PAL IT, P199; Brolsma M.J., 1976, Memorie della Societa Geologica Italiana, V16, P153; Busson G, 1990, GEOLOGIE FRANCE, V3-4, P3; BUTLER RWH, 1995, GEOL SOC AM BULL, V107, P425, DOI 10.1130/0016-7606(1995)107<0425:TASSIM>2.3.CO;2; Carbonnel G., 1979, Revue de Micropaleontologie, V21, P106; CARBONNEL P, 1980, GEOL MEDIT, V7, P19; Carloni G.C., 1974, Giornale di Geolozia, V39, P363; CASTRADORI D, 1998, P OCEAN DRILL PROG S, V180, P113; Cavallo O., 1988, Rivista Piemontese di Storia Naturale, V9, P43; CHUMAKOV I, 1973, INITIAL REPORTS DEEP, V13, P1241, DOI DOI 10.2973/DSDP.PR0C.13.144-2.1973; Cipollari P, 1999, PALAEOGEOGR PALAEOCL, V151, P149, DOI 10.1016/S0031-0182(99)00026-7; Cita M., 1978, Init. 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SEP	2005	17	3					437	462		10.1111/j.1365-2117.2005.00269.x	http://dx.doi.org/10.1111/j.1365-2117.2005.00269.x			26	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	960RL					2025-03-11	WOS:000231610800007
J	Louwye, S				Louwye, S			The Early and Middle Miocene transgression at the southern border of the North Sea Basin (northern Belgium)	GEOLOGICAL JOURNAL			English	Article						dinoflagellate cysts; Miocene; southern North Sea Basin; Belgium	OLIGOCENE; STRATIGRAPHY; DENMARK; MARGIN	The Lower-Middle Miocene Berchem Formation of northern Belgium is an essentially sandy sequence with a varying glauconite content and often abundant shelly intervals. The formation was deposited in a shallow marine environment and rests unconformably on stiff Rupelian clays or Chattian sands. The lithological recognition of the four members (Edegem Sands, Kiel Sands, Antwerpen Sands and Zonderschot Sands members) of the Berchem Formation solely based on lithological criteria proved to be difficult, especially in boreholes. The geometry of the Formation in the subsurface of northern Belgium remained largely unknown. Diverse and well preserved dinoflagellate cyst associations have been recovered from the four members in seven boreholes and two outcrops, and allow a refinement of the biostratigraphy of these deposits. A Miocene biozonation defined in mid-latitude shallow marine deposits in the Atlantic Coastal Plain of the USA (Salisbury Embayment, Maryland) is readily applicable to this material, and has led to a detailed stratigraphic assessment of each member. Three detailed profiles depicting the distribution of the biozones in the subsurface of northern Belgium allow the reconstruction of the geometry and depositional history of the Berchem Formation. The oldest Miocene deposits are of early Burdigalian age and they testify to a transgression, which invaded Belgium from a north-northwestem direction. The maximum flooding took place during early Serravallian times. The upper boundary of the formation is a major erosional surface of late Serravallian or (slightly) younger age. Copyright (c) 2005 John Wiley & Sons, Ltd.	Univ Ghent, Palaeontol Res Unit, Krijgslaan 281 S8, B-9000 Ghent, Belgium	Ghent University	Univ Ghent, Palaeontol Res Unit, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	stephen.louwye@ugent.be	Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				[Anonymous], 1988, GEOLOGISCHES JB A; Bastin A., 1966, INGENIEURSBLAD, V35, P547; Berggren W.A., 1995, SEPM SPEC PUBL, V54, P29, DOI [10.7916/D8XD1B1H, DOI 10.7916/D8XD1B1H]; Blow W. 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SEP	2005	40	4					441	456		10.1002/gj.1021	http://dx.doi.org/10.1002/gj.1021			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	969CL					2025-03-11	WOS:000232210900003
J	Van Simaeys, S; Brinkhuis, H; Pross, J; Williams, GL; Zachos, JC				Van Simaeys, S; Brinkhuis, H; Pross, J; Williams, GL; Zachos, JC			Arctic dinoflagellate migrations mark the strongest Oligocene glaciations	GEOLOGY			English	Article						Oligocene; dinoflagellate cysts; migration; global atmospheric cooling; sea-level change; Rupelian-Chattian boundary	CALIBRATION; BOUNDARY; TRANSITION; RECORDS; REGION; CYSTS	Here we report on mid-Oligocene globally synchronous Arctic dinotlagellate migration events, calibrated against chron C9n. We show that sudden appearances and marked abundance increases of the Arctic taxon Svalbardella at lower and middle latitudes coincide with the Oi-2b benthic delta(18)O glacial episode, dated as ca. 27.1 Ma. These unprecedented migrations are taken to indicate anomalously strong surface-water cooling during Oi-2b time, in turn associated with strong concomitant Antarctic ice-sheet growth and sea-level lowering. We estimate the duration of these unique Svalbardella migrations and the associated episode of profound cooling as similar to 500 k.y. Our records suggest a close link between this distinct Oligocene glaciation episode, strong sea-level fall, and the classic lower-upper Oligocene, or Rupelian-Chattian, boundary, dating this boundary as ca. 27.1 Ma.	Univ Louvain, B-3000 Louvain, Belgium; Univ Utrecht, Palaeobot & Palynol Lab, Dept Palaeoecol, NL-3584 CD Utrecht, Netherlands; Univ Frankfurt, Inst Geol & Palaeontol, D-60054 Frankfurt, Germany; Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; Univ Calif Santa Cruz, Dept Earth Sci, Santa Cruz, CA 95064 USA	Utrecht University; Goethe University Frankfurt; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of California System; University of California Santa Cruz	Van Simaeys, S (通讯作者)，Univ Louvain, Redingenstr 16, B-3000 Louvain, Belgium.	stefaan.vansimaeys@geo.kuleuven.ac.be	Brinkhuis, Henk/B-4223-2009; Zachos, James/A-7674-2008	Zachos, James/0000-0001-8439-1886; Brinkhuis, Henk/0000-0003-0253-6610				Berggren W.A., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P551, DOI 10.2973/odp.proc.sr.120.151.1992; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; DeConto RM, 2003, NATURE, V421, P245, DOI 10.1038/nature01290; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; FENSOME RA, 1996, PALYNOLOGY PRINCIPLE, P107; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P515, DOI 10.2973/odp.proc.sr.105.178.1989; Kennett J.P., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P865, DOI 10.2973/odp.proc.sr.113.188.1990; LECKIE M, 1993, P OCEAN DRILLING PRO, V130, P113; MARRET F, 2003, REV PALAEOBOTANY PAL, V125; Miller KG, 1998, REV GEOPHYS, V36, P569, DOI 10.1029/98RG01624; MILLER KG, 1991, J GEOPHYS RES-SOLID, V96, P6829, DOI 10.1029/90JB02015; MONTANARI A, 1991, NEWSL STRATIGR, V23, P151; Pekar SF, 2002, GEOLOGY, V30, P903, DOI 10.1130/0091-7613(2002)030<0903:CBEEFB>2.0.CO;2; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Prothero D.R., 2003, GREENHOUSE ICEHOUSE; SILVA IP, 1988, EOCENE OLIGOCENE BOU, P137; STICKLEY CE, 2004, P OC DRILL PROGR SCI, V189; Stott L.D., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P549, DOI 10.2973/odp.proc.sr.113.121.1990; Van Simaeys S, 2004, NETH J GEOSCI, V83, P241, DOI 10.1017/S0016774600020308; Van Simaeys S, 2004, PALAEOGEOGR PALAEOCL, V208, P31, DOI 10.1016/j.palaeo.2004.02.029; Wade BS, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2004PA001042; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zachos JC, 1996, PALEOCEANOGRAPHY, V11, P251, DOI 10.1029/96PA00571; ZACHOS JC, 1993, J GEOL, V101, P191, DOI 10.1086/648216; ZACHOS JC, 1994, PALEOCEANOGRAPHY, V9, P353, DOI 10.1029/93PA03266	29	37	39	0	4	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0016-8505			GEOLOGY	Geology	SEP	2005	33	9					709	712		10.1130/G21634.1	http://dx.doi.org/10.1130/G21634.1			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	960JF					2025-03-11	WOS:000231585800005
J	Polyakova, YI; Bauch, HA; Klyuvitkina, TS				Polyakova, YI; Bauch, HA; Klyuvitkina, TS			Early to middle Holocene changes in Laptev Sea water masses deduced from diatom and aquatic palynomorph assemblages	GLOBAL AND PLANETARY CHANGE			English	Article						Arctic Siberia; Holocene river runoff; diatoms; aquatic palynomorphs; land-ocean interaction	DINOFLAGELLATE CYST ASSEMBLAGES; ARCTIC-OCEAN; FRESH-WATER; KARA SEAS; SHELF; ICE; SEDIMENTS; SIBERIA; NORTH; CIRCULATION	On the basis of diatom and aquatic palynomorph assemblages in sediment cores obtained from the eastern Laptev Sea shelf, major phases of environmental change associated with the last postglacial global sea-level rise can be recognized for the time since 11.3 calendar years BP (cal. ka). Until 11 cal. ka, the outer Laptev Sea shelf (>= 51 m paleodepth) was inundated and paleoenvironmental conditions were characterized by increased precipitation of river-loaded matter, primarily diatom plankton, in a river-proximal environment where reconstructed surface water salinities, using freshwater diatoms as proxy, remained below 9. The time interval 10.7-9.2 cal. ka was marked by a predominance of the dinoflagellate cyst Operculodinium centrocarpum as well as by the appearance of relatively warm-water indicative species in the outer Laptev Sea, probably due to enhanced influence of Atlantic Water at the continental margin. Because a continuously rising sea level resulted in an increasing distance between the investigated site and the southward retreating coastline, surface-water salinities on the outer shelf approached modem values of about 15-16 around 8.6 cal. ka. On the inner Laptev Sea shelf, modem-like environmental conditions were reached about I to 1.5 ky later, around 7.4 cal. ka, emphasizing the overwhelming influence of the global transgression on the Holocene evolution of Arctic shelf water masses. (c) 2005 Elsevier B.V All rights reserved.	Moscow MV Lomonosov State Univ, Dept Geog, Moscow 119899, Russia; IFM, GEOMAR, Mainz Acad Sci Humanities & Literature, D-24148 Kiel, Germany	Lomonosov Moscow State University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Moscow MV Lomonosov State Univ, Dept Geog, Vorobievy Gory, Moscow 119899, Russia.	yi@polyakova.geogr.msu.su	Polyakova, Yelena/L-8889-2015; Klyuvitkina, Tatyana/L-8843-2015					AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; [Anonymous], PALEOCEANOGRAPHY; [Anonymous], 1999, LAND OCEAN SYSTEMS S; [Anonymous], EARTHS CRYOSPHERE; [Anonymous], 1971, POLLEN SPORES; BATTARBE.RW, 1973, LIMNOL OCEANOGR, V18, P647, DOI 10.4319/lo.1973.18.4.0647; BAUCH D, 1995, PROG OCEANOGR, V35, P53, DOI 10.1016/0079-6611(95)00005-2; Bauch H.A., 2000, EOS T, V81, P233, DOI [10.1029/00EO00162, DOI 10.1029/00EO00162]; Bauch HA, 2001, GLOBAL PLANET CHANGE, V31, P125, DOI 10.1016/S0921-8181(01)00116-3; Bauch HA, 2000, INT J EARTH SCI, V89, P569, DOI 10.1007/s005310000122; Bauch HA, 2001, QUATERNARY RES, V55, P344, DOI 10.1006/qres.2000.2223; Bauch HA, 1999, BOREAS, V28, P194, DOI 10.1111/j.1502-3885.1999.tb00214.x; Cremer H, 1999, MAR MICROPALEONTOL, V38, P39, DOI 10.1016/S0377-8398(99)00037-7; Cremer H., 1999, Land-Ocean Systems in the Siberian Arctic, P533; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Dethleff D, 1998, COLD REG SCI TECHNOL, V27, P225, DOI 10.1016/S0165-232X(98)00005-6; Dmitrenko I.A., 1999, P 15 INT C PORT OC E, V1, P311; Fensome R.A., 1993, Micropaleontology Press Special Paper; Gordeev VV, 1996, AM J SCI, V296, P664, DOI 10.2475/ajs.296.6.664; Gordeev VV, 2000, NATO SCI S PRT 2 ENV, V70, P297; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; IVANOV II, 1995, RUSSIAN GERMAN COOPE, V176, P142; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Kassens H., 1998, EOS T AM GEOPHYS UN, V79, P317, DOI [10.1029/98EO00234, DOI 10.1029/98EO00234]; Kleiber H.P., 1999, LAND OCEAN SYSTEMS S, P657; Kleiber HP, 2000, INT J EARTH SCI, V89, P605, DOI 10.1007/s005310000130; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Lisitsyn A.P., 1995, Oceanol. 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Planet. Change	SEP	2005	48	1-3					208	222		10.1016/j.gloplacha.2004.12.014	http://dx.doi.org/10.1016/j.gloplacha.2004.12.014			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	966IJ					2025-03-11	WOS:000232013000013
J	Samant, B; Sakurkar, CV; Kundal, P; Mohabey, DM				Samant, B; Sakurkar, CV; Kundal, P; Mohabey, DM			Maastrichtian dinoflagellates and palynomorphs from subsurface Deccan inter-trap sediments, Khandala-Ashta area, Wardha District, Maharashtra	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						dinoflagellates; inter-trappeans; Wardha district; Maharashtra	INTERTRAPPEAN BEDS; TERTIARY BOUNDARY; AGE IMPLICATIONS; LAMETA FORMATION; ANDHRA-PRADESH; INDIA; ANJAR; VERTEBRATE; GUJARAT	A 164 m thick Deccan volcano sedimentary sequence comprising five flows, separated by four inter-trap beds and overlying the Lameta Formation, has been encountered in borehole KA-1, drilled by the Directorate of Geology and Mining (DGM) for the coal exploration in Khandala-Ashta area of Wardha District, Maharashtra. Of these, the intertrap between the two lowermost flows has yielded a rich spore-pollen assemblage that is dominated by angiosperms and pteridophytes. The presence of palynotaxa such as Azolla cretacea, Ariadnaesporites sp., Gabonisporis vigourouxii, Triporoletes reticulatus and Aquilapollenites bengalensis, suggests a Late Cretaceous (Maastrichtian) age for the sediments. The palynomorphs are associated with a rich dinoflagellate assemblage mostly comprising of Palaeoperidinium and Selenopemphix. The study indicates that the changing climatic and depositional scenario owing to Deccan volcanic eruption has possibly offered the suitable ecological niche for the first appearance of dinoflagellates and gradual domination of the angiosperm flora in the non-marine ecosystem during Late Cretaceous in India.	Nagpur Univ, Postgrad Dept Geol, Nagpur 440001, Maharashtra, India; Geol Survey India, Palaeontol Div, Nagpur 440006, Maharashtra, India	Rashtrasant Tukadoji Maharaj Nagpur University; Geological Survey India	Nagpur Univ, Postgrad Dept Geol, Nagpur 440001, Maharashtra, India.	tvandana@sify.com	Samant, Bandana/JFJ-4995-2023					AMBWANI K, 1981, PALAEOBOT, V11, P13; [Anonymous], 1993, PALAEOGEOGR PALAEOCL; BAJPAI S, 1993, CURR SCI INDIA, V64, P42; BANDE MB, 1990, PALEOBOTANIST, V38, P196; BHATIA SB, 1990, P IGCP 216 245 SEM C, P47; BROOKFIELD M E, 1987, Cretaceous Research, V8, P1, DOI 10.1016/0195-6671(87)90008-5; CHITALEY S. D. Mrs., 1951, PROC NATL INST SCI INDIA, V17, P373; Dogra NN, 2004, CURR SCI INDIA, V86, P1596; Geological Survey of India, 2001, DISTR RES MAP; Ghosh P, 2003, CRETACEOUS RES, V24, P743, DOI 10.1016/j.cretres.2003.08.002; Hansen HJ, 2001, P INDIAN AS-EARTH, V110, P133, DOI 10.1007/BF02702213; HISLOP S, 1859, Q J GEOL SOC LOND, V16, P154; Kar R.K., 1998, Geophytology, V27, P17; Kar RK., 2004, Geophytology, V33, P21; Kumaran KPN, 1997, CURR SCI INDIA, V72, P590; Mahabale T. S., 1981, PALEOBOTANIST, V<bold>27</bold>, P174; MATHUR NS, 1990, P IGCP 216 245 SEM C, P58; MEHROTRA NC, UNPUB MAHARASHTRA; Mohabey D.M., 2003, Gondwana Geological Magazine Special Volume, V6, P225; MOHABEY DM, 1993, PALAEOGEOGR PALAEOCL, V105, P83, DOI 10.1016/0031-0182(93)90108-U; Mohabey DM., 1996, Gondwana Geological Mag, V2, P349; Prakash T, 1990, P IGCP 216 245 SEM C, P68; Prakash U, 1963, PALEOBOTANIST, V12, P121; PRAKASH U, 1980, PALAEOBOT, V26, P279; Prakash U., 1962, PALAEOBOT, V11, P1; PRASAD GVR, 1989, J GEOL SOC INDIA, V34, P161; RANA RS, 1990, CURR SCI INDIA, V59, P49; RAO BRJ, 1981, MEM GEOL SOC INDIA, P287; SAHNI A, 1988, J GEOL SOC INDIA, V32, P382; SAMANT B, 2003, 19 IND C MICR STRAT, P63; Samant Bandana, 2003, Gondwana Geological Magazine, V18, P19; Singh RS, 2002, J GEOL SOC INDIA, V60, P213; SPICER RA, 1989, PHILOS T ROY SOC B, V325, P291, DOI 10.1098/rstb.1989.0090; TANDON SK, 1995, PALAEOGEOGR PALAEOCL, V117, P153, DOI 10.1016/0031-0182(94)00128-U; VONHUENE FB, 1933, MEM GEOL SURV INDIA, V2, P1; Whatley Robin, 2000, Revue de Micropaleontologie, V43, P173, DOI 10.1016/S0035-1598(00)90105-3	36	2	3	0	3	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622	0974-6889		J GEOL SOC INDIA	J. Geol. Soc. India	SEP	2005	66	3					267	272						6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	983CY					2025-03-11	WOS:000233209900002
J	Gottschling, M; Keupp, H; Plötner, J; Knop, R; Willems, H; Kirsch, M				Gottschling, M; Keupp, H; Plötner, J; Knop, R; Willems, H; Kirsch, M			Phylogeny of calcareous dinoflagellates as inferred from ITS and ribosomal sequence data	MOLECULAR PHYLOGENETICS AND EVOLUTION			English	Article						5.8S rRNA; Calciodinellaceac; internal transcribed spacer; paleontology; molecular systematics; secondary structure	SECONDARY STRUCTURE; SCRIPPSIELLA-TROCHOIDEA; DINOPHYCEAE; CALCIODINELLOIDEAE; PFIESTERIA; CYST; PERIDINIALES; DIVERSITY; GENERA; CLASSIFICATION	The phylogenetic relationships of calcareous dinoflagellates (i.e., Calciodinellaceae and Thoracosphaera) are investigated. Molecular data from the ribosomal 5.8S rRNA and highly conserved motifs of the ITS1 show Calciodinellaceae s.l. to be monophyletic when few non-calcareous taxa are included. They segregate into three monophyletic assemblages in a molecular analysis that considers the 5.8S rRNA and both the Internal Transcribed Spacer regions ITS1 and ITS2: a clade comprising species of Ensiculifera and Pentapharsodinium (E/P-clade), Scrippsiella s.l. (including fossil-based taxa such as Calciodinellum and Calcigonellum), and a heterogeneous group (T/P-clade) of calcareous (e.g., Thoracosphaera) and non-calcareous taxa (e.g., the highly toxic Pfiesteria). The potential to produce; calcareous structures is considered as apomorphic within alveolates, and non-calcareous taxa nesting with calcareous dinoflagellates may have reduced calcification secondarily. Molecular results do not contradict general evolutionary scenarios provided by previous morphological (mainly paleontological) investigations. (c) 2005 Elsevier Inc. All rights reserved.	Free Univ Berlin, Fachbereich Geol Wissensch Fachrichtung Palaontol, D-12249 Berlin, Germany; Humboldt Univ, Museum Nat, Inst Systemat Zool, Berlin, Germany; Univ Bremen, Fachbereich Geowissensch Hist Geol & Palaontol, Bremen, Germany	Free University of Berlin; Humboldt University of Berlin; University of Bremen	Free Univ Berlin, Fachbereich Geol Wissensch Fachrichtung Palaontol, Malteserstr 74-100, D-12249 Berlin, Germany.	caix@zedat.fu-berlin.de	Gottschling, Marc/K-2186-2014					Altschul SF, 1997, NUCLEIC ACIDS RES, V25, P3389, DOI 10.1093/nar/25.17.3389; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Coleman AW, 1998, PROTIST, V149, P135, DOI 10.1016/S1434-4610(98)70018-5; Cox E. 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Phylogenet. Evol.	SEP	2005	36	3					444	455		10.1016/j.ympev.2005.03.036	http://dx.doi.org/10.1016/j.ympev.2005.03.036			12	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	960LH	15964218				2025-03-11	WOS:000231591500002
J	Pucéat, E; Lécuyer, C; Reisberg, L				Pucéat, E; Lécuyer, C; Reisberg, L			Neodymium isotope evolution of NW Tethyan upper ocean waters throughout the Cretaceous	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						neodymium; cretaceous; tethys; oceanic circulation	FOSSIL FISH TEETH; NORTH-ATLANTIC; BIOGENIC APATITES; DEEP-WATER; DINOFLAGELLATE CYSTS; MEDITERRANEAN-SEA; PACIFIC-OCEAN; SEAWATER SR; ND ISOTOPES; CIRCULATION	Neodymium isotope compositions of twenty-four fish teeth, nineteen from the NW Tethys and five from different locations within the Tethys, are interpreted to reflect the evolution of Tethyan upper ocean water composition during the Cretaceous and used to track changes in erosional inputs to the NW Tethys and in oceanic circulation throughout the Cretaceous. The rather high epsilon(Nd) (up to -7.6) of the NW Tethyan upper ocean waters recorded from the Late Berriasian to the Early Aptian and the absence of negative excursions during this interval support the presence of a permanent westward flowing Tethys Circumglobal Current (TCC). This implies that temperature variations during this time period, inferred from the oxygen isotope analysis of fish tooth enamel, were not driven by changes in surface oceanic currents, but rather by global climatic changes. The results presented here represent a significant advance over previously published Cretaceous seawater Nd isotope records. Our newly acquired data now allow the identification of two stages of low epsilon(Nd) values in the NW Tethys, during the Early Albian-Middle Albian interval (down to -10) and the Santonian-Early Campanian (down to -11.4), which alternate with two stages of higher epsilon(Nd) values (up to -9) during the Late Albian-Turonian interval and the Maastrichtian. Used in conjunction with the oxygen isotope record, the fluctuations of epsilon(Nd) values can be related to major climatic, oceanographic, and tectonic events that appeared in the western Tethyan domain. (c) 2005 Elsevier B.V. All rights reserved.	Univ Lyon 1, CNRS, UMR 5125, Lab Paleoenvironm & Paleobiosphere, F-69622 Villeurbanne, France; Ctr Rech Petrog & Geochim, F-54501 Vandoeuvre Les Nancy, France; Inst Univ France, F-75005 Paris, France	Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); Universite de Lorraine; Institut Universitaire de France	CEA Saclay, Lab Sci Climat & Environm, CNRS, CEA,DSM,Ormes Merisiers, Bat 709, F-91191 Gif Sur Yvette, France.	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Sci. Lett.	AUG 15	2005	236	3-4					705	720		10.1016/j.epsl.2005.03.015	http://dx.doi.org/10.1016/j.epsl.2005.03.015			16	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	966UI					2025-03-11	WOS:000232047200011
J	Radley, JD				Radley, JD			Derived fossils in the southern English Wealden (non-marine early Cretaceous): a review	CRETACEOUS RESEARCH			English	Article						Wealden; Early Cretaceous; derived fossils; palaeoenvironments	ISLE-OF-WIGHT; STRATIGRAPHY; PALEONTOLOGY; ENGLAND; DORSET; BAY	Derived fossils occur in all the principal facies associations of the southern English Wealden succession (non-marine early Cretaceous). They confirm the presence of Palaeozoic and early-mid Mesozoic source massifs surrounding the Weald and Wessex depocentres, fringed by scarps and intrabasinal highs of Jurassic strata. The derived macrofossil material is largely siliceous and phosphatic. It gains abundance in lake strandline gravels but also occurs as scattered reptilian gastroliths and among lagoonal shell concentrations. Calcareous fossils are abundant at one site, reflecting proximity to source. Jurassic dinoflagellate cysts are widespread among finer-grained facies. (c) 2005 Elsevier Ltd. All rights reserved.	Warwickshire Museum, Warwick CV34 4SA, Warwick, England		Warwickshire Museum, Market Pl, Warwick CV34 4SA, Warwick, England.	jonradley@warwickshire.gov.uk						ALLEN P, 1964, NATURE, V202, P585, DOI 10.1038/202585b0; ALLEN P, 1981, J GEOL SOC LONDON, V138, P375, DOI 10.1144/gsjgs.138.4.0375; ALLEN P, 1991, CRETACEOUS RES, V12, P511, DOI 10.1016/0195-6671(91)90005-W; Allen P., 1961, Proceedings of the Geological Association, V72, P271; Allen P, 1998, P GEOLOGIST ASSOC, V109, P197, DOI 10.1016/S0016-7878(98)80066-7; ALLEN P, 1989, Proceedings of the Geologists' Association, V100, P529; ALLEN P, 1975, Proceedings of the Geologists' Association, V86, P389; ALLEN P, 1967, P GEOLOGISTS ASS, V78, P241; ALLEN P., 1960, P GEOL ASS, V71, P156; ALLEN P., 1955, GEOL MAG, V92, P265, DOI [10.1017/S0016756800064311, DOI 10.1017/50016756800064311]; ALLEN P, 1960, GEOLOGISTS ASS GUIDE; Allen P., 1991, Geological Society, London, Special Publications, V57, P13, DOI [10.1144/GSL.SP.1991.057.01.02, DOI 10.1144/GSL.SP.1991.057.01.02]; ALLEN P., 1962, P GEOL ASS, V73, P219; [Anonymous], 1987, BRIT MICROPALAEONTOL; Arkell WJ., 1960, P GEOLOGISTS ASS, V71, P165; Batten D., 1996, Palynology: principles and applications, P1011; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; Batten D.J., 1982, P278; BATTEN DJ, 1991, DEV SEDIMENTARY PROV, V57, P79; Casey R., 1961, Palaeontology, V3, P487; Ensom P.C., 1985, P DORSET NATURAL HIS, V106, P166; ENSOM PC, 1984, P DORS NAT HIST ARCH, V105, P89; Gale A.S., 2000, GEOLOGICAL HIST BRIT, P339; Garden I., 1991, Geological Society, London, Special Publications, V57, P273; Harding IC, 1995, CRETACEOUS RES, V16, P727, DOI 10.1006/cres.1995.1046; Horton A., 1974, 7416 I GEOL SCI; JARZEMBOWSKI E A, 1991, Proceedings of the Geologists' Association, V102, P83; KIRKALDY J.F., 1947, P GEOL ASS, V58, P223; KIRKALDY JF, 1948, P GEOLOGISTS ASS, V59, P80; Martill DM, 2000, NEUES JAHRB GEOL P M, P186; MARTILL DM, 2001, FIELD GUIDE FOSSILS; Oakley K. P., 1947, Proceedings of the Geologists' Association London, V58, P255; RADLEY JD, 1994, P GEOLOGIST ASSOC, V105, P199, DOI 10.1016/S0016-7878(08)80119-8; Radley JD, 1998, P GEOLOGIST ASSOC, V109, P187, DOI 10.1016/S0016-7878(98)80065-5; Radley JD, 1995, CRETACEOUS RES, V16, P717, DOI 10.1006/cres.1995.1045; Radley JD, 1998, P GEOLOGIST ASSOC, V109, P81, DOI 10.1016/S0016-7878(98)80008-4; RADLEY JD, 1993, P GEOLOGISTS ASS, V104, P71; Robinson SA, 2004, J GEOL SOC LONDON, V161, P133, DOI 10.1144/0016-764903-004; RUFFELL AH, 1994, P GEOLOGIST ASSOC, V105, P53, DOI 10.1016/S0016-7878(08)80138-1; SLADEN C P, 1984, Proceedings of the Geologists' Association, V95, P149; Stewart DJ, 1981, FIELD GUIDES MODERN; TOPLEY W, 1975, MEMOIR GEOLOGICAL SU; Underhill JR, 1998, GEOL SOC SPEC PUBL, V133, P1, DOI 10.1144/GSL.SP.1998.133.01.01; Watson J, 1996, CRETACEOUS RES, V17, P5, DOI 10.1006/cres.1996.0002; WEST IM, 1969, GEOL MAG, V106, P277, DOI 10.1017/S001675680005799X; White H.J., 1928, Memoir of the Geological Survey UK; Wimbledon WA, 1996, SEDIMENT GEOL, V102, P213, DOI 10.1016/0037-0738(95)00157-3	47	9	10	0	6	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	AUG	2005	26	4					657	664		10.1016/j.cretres.2005.03.002	http://dx.doi.org/10.1016/j.cretres.2005.03.002			8	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	978LC					2025-03-11	WOS:000232873700010
J	Sangiorgi, F; Fabbri, D; Comandini, M; Gabbianelli, G; Tagliavini, E				Sangiorgi, F; Fabbri, D; Comandini, M; Gabbianelli, G; Tagliavini, E			The distribution of sterols and organic-walled dinoflagellate cysts in surface sediments of the North-western Adriatic Sea (Italy)	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						sterols; dinocysts; North Adriatic Sea; surface sediments	INCREASED EUTROPHICATION; PHYTOPLANKTON BLOOM; 4-METHYL STEROLS; FATTY-ACID; GC-MS; MARINE; MATTER; BIOMARKERS; ESTUARY; CARBON	The distributions of sterols and organic-walled dinoflagellate cysts (dinocysts) in five NW Adriatic Sea surface sediment samples were investigated. Samples are representative of areas differently influenced by freshwater inputs, mainly coming from the Po River. All the investigated samples exhibit the same suite of principal sterols, with cholest-5-en-3 beta-ol (cholesterol), 4 alpha,23,24-trimethyl-5 alpha-cholest-22E-en-3 beta-ol (dinosterol), 24-ethylcholest-5-en-3 beta-ol (sitosterol) and 24-methyleholesta-5,22E-dien-3 beta-ol (brassicasterol or epibrassicasterol) displaying the highest concentrations and relative abundances. The distribution of sterols in the samples is not related to their distance from the coast and/or with the C/N ratios and suggests a prevalent input of marine, autochthonous organic matter in the surface sediments. In particular, the high abundance of dinosterol underlines the importance of dinoflagellate productivity in this area and its contribution to the organic matter in sediments. However, absolute and relative abundances of dinosterol do not follow the trend observed for dinocyst concentrations in the investigated samples, with the exception of Spiniferites spp. cysts and cysts produced by Gonyaulax species. (c) 2005 Elsevier Ltd. All rights reserved.	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Coast. Shelf Sci.	AUG	2005	64	2-3					395	406		10.1016/j.ecss.2005.03.005	http://dx.doi.org/10.1016/j.ecss.2005.03.005			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	950QV		Green Published			2025-03-11	WOS:000230873200025
J	Crouch, EM; Brinkhuis, H				Crouch, EM; Brinkhuis, H			Environmental change across the Paleocene-Eocene transition from eastern New Zealand: A marine palynological approach	MARINE MICROPALEONTOLOGY			English	Article						Late Paleocene; Early Eocene; initial Eocene thermal maximum; dinoflagellate cyst; spore; pollen; palynology; New Zealand; environmental change	DINOFLAGELLATE CYSTS; SEA-LEVEL; EL-KEF; CLIMATE; BOUNDARY; SECTION; BIOSTRATIGRAPHY; FORAMINIFERA; SEDIMENTS; PALEOGENE	Recent improvements in the resolution and calibration of dinoflagellate cyst (dinocyst) bioevents across the Paleocene-Eocene (P-E) transition in New Zealand allow better understanding of the relation between dinocyst variations and environmental change in southern mid-high latitudes during this 'greenhouse' climate. Combining information from land spore/pollen assemblages with coeval dinocyst records allows evaluation of plant changes in a marine-based timeframe. Palynological associations at Tawanui and Moeraki-Hampden, eastern New Zealand, fluctuate across the P-E transition and 'local palynological phases' are recognized. The onset of major fluctuations in dinocyst assemblages coincide with the intense warmth and excess carbon of the Initial Eocene thermal maximum (IETM). Changes in sea surface temperature (SST) appear to have been the main environmental factor that affected dinoflagellates. Short-lived intervals of higher SSTs, suggested by a high relative abundance of the Apectodinium complex, are seen during the IETM and lower Eocene. Abundant cysts of probable heterotrophic dinoflagellates suggest surface waters remained relatively eutrophic for up to 0.5 Myr after the onset of the IETM, perhaps in response to enhanced terrigenous input related to changes in the character and pattern of continental weathering. In contrast to dinocysts, spore/pollen assemblages suggest plant communities remained rather stable across the P E transition. Vegetation was dominated by a mesothermal conifer-dominated multistratal rainforest, and low-latitude Nypa mangroves were established by the uppermost Paleocene. Plants in this region show no clear response to the IETM and the predominant vegetation change may have occurred at least 1.5 Myr later, characterized by an increase in mesothermal-megathermal angiosperm plants. (c) 2005 Elsevier B.V. All rights reserved.	Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Univ Utrecht, Dept Geobiol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	GNS Science - New Zealand; Utrecht University	Inst Geol & Nucl Sci, POB 30-368, Lower Hutt, New Zealand.	e.crouch@gns.cri.nz	Crouch, Erica/C-2820-2013; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 2003, CAUSES CONSEQUENCES, DOI DOI 10.1130/0-8137-2369-8.351; [Anonymous], 2007, Paleopalynology; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Aubry MP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P158; Aubry MP, 2000, B SOC GEOL FR, V171, P461, DOI 10.2113/171.4.461; AUBRY MP, 2003, CAUSES CONSEQUENCES, V369, P551; Bains S, 2000, NATURE, V407, P171, DOI 10.1038/35025035; Ballance P.F., 1993, SEDIMENTARY BASINS W, V2, P93; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; BYBELL LM, 2001, EVENTS ASS LATE PALE, P18; Collinson M.E., 2000, Biotic Response to Global Change: the Last 145 Million Years, V145, P223; Collinson ME, 2000, GFF, V122, P36, DOI 10.1080/11035890001221036; Crouch EM, 2003, PALAEOGEOGR PALAEOCL, V194, P387, DOI 10.1016/S0031-0182(03)00334-1; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; CROUCH EM, 2001, LPP CONTRIBUTION SER, V14; Crouch Erica M., 2003, Geological Society of America Special Paper, V369, P113; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dupuis C, 2003, MICROPALEONTOLOGY, V49, P41, DOI 10.2113/49.Suppl_1.41; EDWARDS AR, 1970, P 2 PLANKT C ROM, V1, P381; EGGER H, 2003, SPECIAL PAPER GEOLOG, V369, P133; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Gingerich P. 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Micropaleontol.	AUG	2005	56	3-4					138	160		10.1016/j.marmicro.2005.05.002	http://dx.doi.org/10.1016/j.marmicro.2005.05.002			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	952XG					2025-03-11	WOS:000231038800004
J	Lenz, OK				Lenz, OK			Palynology and palaeoecology of a coastal swamp from the Middle Eocene of Central Europe - The Wulfersdorf seam group from the open cast mine Helmstedt, Lower Saxony	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			German	Review						palynology; taxonomy; palaeoecology; lignites; Germany; Middle Eocene	DINOFLAGELLATE CYSTS; ISOPOLLEN MAPS; TERTIARY; POLLEN; TAXONOMY; FACIES	A detailed palynological investigation of the Wulfersdorf seams and associated sediments within the Upper Seam Group of Helmstedt has been carried out with the aim of demonstrating the potential of palynological analysis for paleoecological information. 182 taxa of spores, pollen and plankton are described in a systematic chapter and figured on 14 plates. The results of quantitative analysis and the distribution of palynomorphs are presented in 12 high-resolution pollen diagrams from different sections of the lignite bearing succession. In order to provide a more objective ecological evaluation various methods of multivariate statistics such as cluster analysis and principal component analysis were applied. In addition, isopollen maps have been constructed from a carbonaceous band occurring within an estuarine interbed and representing a brief terrestrialisation event. Sampling was carried out along a narrow time plane during mining progress. Based on both, statistical analyses and isopollen maps, a detailed vegetation model of a Middle Eocene coastal swamp has been constructed. The Middle Eocene coastal plain vegetation in the Helmstedt area was characterized by a clear zonation in response to the proximity of the coast and exposure to salt-water. Thus, variations in composition of palynomorph assemblages are controlled by shifts of environment and facies rather than climatic effects. A mangrove belt comparable to modern mangroves is indicated by the restricted occurrence of pollen of Rhizophora, Avicennia and Nypa as well as the form taxon Psilodiporites iszkaszentgyoergyi of uncertain botanical affinity. Behind the mangrove zone, pollen of Restionaceae and Sparganiaceae/Typhaceae indicate the presence of a more open, marsh-like vegetation together with the closely associated Plicapollis pseudoexcelsus and Pompeckjoidaepollenites subhercynicus, probably pollen of woody plants of known resp. assumed juglandaceous affinity. Other elements, such as palms apparently grew in restricted stands, perhaps in tree islands dotting the more open marsh-like vegetation, since their pollen shows a patchy distribution. The main peat forming vegetation was a mire forest dominated by Fagaceae and associated with Myricaceae, Juglandaceae, Aquifoliaceae and Nyssaceae. This occured in alternation with a Corylaceae dominated forest including Cyrillaceae and Sapotaceae. Ericaceae probably formed an understorey on nutrient deficient soils.	Univ Gottingen, Geowissensch Zentrum, D-37077 Gottingen, Germany	University of Gottingen	Univ Gottingen, Geowissensch Zentrum, Goldschmidtstr 3, D-37077 Gottingen, Germany.	olenz@gwdg.de						[Anonymous], PALAEONTOGRAPHICA A; [Anonymous], 1963, Atlas der Mittel- und Jungtertiaren dispersen Sporen- und Pollen - sowie der Mikroplanktonformen des nordlichen Mitteleuropas 2; [Anonymous], BLUTENPFLANZEN WELT; [Anonymous], 1970, PALAONTOLOGISCHE A B, DOI DOI 10.1093/AOB/MCR249; [Anonymous], 1979, 4 INT PAL C LUCKN 19; [Anonymous], 1973, Katalog der fossilen Dinoflagellaten, Hystrichospharen und verwandten Mikrofossilien; [Anonymous], 1962, GEOLOGIE; [Anonymous], 1931, JB PREUISCHEN GEOLOG; Balme B.E., 1957, COMMONW SCI IND RES, V25, P1; Barthel M., 1976, ABH ZBL GEOL I BER, V26, P439; BATTEN DJ, 1996, PALYNOLOGY PRINCIPLE, V3, P205; Belz Gerhard, 1994, Palaeontographica Abteilung B Palaeophytologie, V233, P19; BENEDEK P N, 1981, Palaeontographica Abteilung B Palaeophytologie, V180, P39; Bennie J., 1886, Proc. 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J	Peña-Manjarrez, JL; Helenes, J; Gaxiola-Castro, G; Orellana-Cepeda, E				Peña-Manjarrez, JL; Helenes, J; Gaxiola-Castro, G; Orellana-Cepeda, E			Dinoflagellate cysts and bloom events at Todos Santos Bay, Baja California, Mexico, 1999-2000	CONTINENTAL SHELF RESEARCH			English	Article						dinoflagellate blooms; cysts; environmental factors; Baja California; Mexico	RED TIDE; NORTH; WATER	Forty-two species of dinoflagellate motile cells and 18 species of organic-walled dinoflagellate resting cysts were identified in samples collected at Todos Santos Bay, Baja California, Mexico, front September 1999 to June 2000. These temperate to cool-temperate species belong mainly to the families Gonyaulacaceae and Protoperidiniaceae. Lingulodinium polyedrum (Stein, 1883) Dodge 1989 was the dominant species both in the sediments and water column. During this period we observed planktonic motile cells, temporary cysts with cellulose walls, and resting cysts with resistant dinosporin walls. Two dinoflagellate blooms occurred in the spring to summer of 2000 allowing us to observe the timing of cyst production. The temporary cysts appeared between these blooms and also in the summer, whereas the resting cysts appeared during the preceding fall and winter. Resting cysts appeared in colder conditions, whereas the temporary cysts were produced within a particular thermal window and under nutrient depletion. Resting cysts were concentrated in discrete areas at depths of less than 25 in, and associated with sediments ranging from silt to fine sand. These cysts were abundant in the surface sediments during summer, fall and winter, whereas the motile cells dominated during the spring and summer, when the two L. polyedrum blooms were observed. The abundance of cells in the plankton, comprising motile cells and temporary cysts, appears to be inversely proportional to the concentration of resting cysts of the same species in the surface sediments. (c) 2005 Elsevier Ltd. All rights reserved.	CICESE, Dept Oceanog Biol, Div Oceanol, Ensenada, Baja California, Mexico; Ctr Estudios Tecnol Mar Ensenada, Direcc Gen Educ Ciencia & Tecnol Mar, Ensenada, Baja California, Mexico; CICESE, Dept Geol, Div Ciencias Tierra, Ensenada, Baja California, Mexico; Univ Autonoma Baja California, Fac Ciencias Marinas, Ensenada, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; Universidad Autonoma de Baja California		jopema@cicese.mx	Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879				Alvarez-Borrego J., 1982, Cal COFI Report, V23, P188; Alvarez-Sanchez L.G., 1988, CIENC MAR, V14, P135; Anderson D.M., 1985, P219; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; [Anonymous], NEOGENE QUATERNARY D; ARGOTE EML, 1991, ATMOSFERA, V4, P101; BLASCO D, 1977, LIMNOL OCEANOGR, V22, P255, DOI 10.4319/lo.1977.22.2.0255; CANNON JA, 1993, DEV MAR BIO, V3, P103; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Eppley R.W., 1975, P11; GREGORIO ED, 2000, B SO CALIFORNIA ACAD, V99, P147; HANSEN OH, 1965, J CONS PERM INT EXPL, V30, P3, DOI DOI 10.1093/ICESJMS/30.1.3; Hayward TL, 1995, CAL COOP OCEAN FISH, V36, P19; HOLMES RW, 1967, LIMNOL OCEANOGR, V12, P503, DOI 10.4319/lo.1967.12.3.0503; Kimor B., 1981, California Cooperative Oceanic Fisheries Investigations Reports, V22, P126; Kirk JT., 1994, LIGHT PHOTOSYNTHESIS, DOI DOI 10.1017/CBO9780511623370.005; Koroleff F., 1983, METHODS SEAWATER ANA, V2nd; Lewis Jane, 1995, P175; Mao Shaozhi, 1993, Palynology, V17, P47; Matsuoka K, 2003, J PLANKTON RES, V25, P1461, DOI 10.1093/plankt/fbg111; Matsuoka K., 1985, NATURAL SCI B, V25, P21; McQuoid MR, 2002, J PHYCOL, V38, P881, DOI 10.1046/j.1529-8817.2002.01169.x; Minobe S, 1999, GEOPHYS RES LETT, V26, P855, DOI 10.1029/1999GL900119; MONTIELNIEVES M, 1998, THESIS U AUT BAJA CA; MOREYGAINES G, 1981, USC SEA GRANT PUBLIC; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; Mudie PJ, 2001, J QUATERNARY SCI, V16, P595, DOI 10.1002/jqs.660; ORELLANACEPEDA E, 1993, 6 INT C TOX MAR PHYT; Peña-Manjarrez JL, 2001, CIENC MAR, V27, P543; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; SUTHERLAND TF, 1992, J PLANKTON RES, V14, P915, DOI 10.1093/plankt/14.7.915; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Venrick E., 1984, Calif. 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J	Jeong, HJ; Kim, JS; Park, JY; Kim, JH; Kim, S; Lee, I; Lee, SH; Ha, JH; Yih, WH				Jeong, HJ; Kim, JS; Park, JY; Kim, JH; Kim, S; Lee, I; Lee, SH; Ha, JH; Yih, WH			<i>Stoeckeria algicida</i> n. gen., n. sp (Dinophyceae) from the coastal waters off Southern Korea:: Morphology and small subunit ribosomal DNA gene sequence	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Dinoflagellate; DNA; HAB; heterotrophic; plankton; protist; protozoa; red tide	DINOFLAGELLATE; PROTOPERIDINIUM; PFIESTERIA; BEHAVIOR; GROWTH; RATES	This paper presents anew description of the morphology of the planktonic dinoflagellate Stoeckeria algicida n. gen., n. sp. and a report of the sequence of the small subunit rDNA (SS rDNA) from cultured cells. The vegetative biflagellated cell, gametes, triflagellated planozygotes, and cyst stages of this heterotrophic species were observed in cultures. The vegetative biflagellated cells are oval, with the cell length being considerably larger than the cell width. The ranges (and mean, n = 60) of cell length and width of live biflagellated cells satiated with the raphidophyte Heterosigma akashiwo were 14.4-20.8 mu m (16.8) and 10.0-17.4 mu m (12.9). respectively, while those of biflagellated cells starved for 3 d (n = 60) were 7.3-15.9 mu m (11.6) and 2.7-12.2 mu m (7.3), respectively. Thin plates of the vegetative biflagellated cells were arranged in a Kofoidian series of Po, cp, X, 4', 2a, 7", 6c, 6s, 5"', 0 (p), and 2"". When properly aligned, the sequence of the SS rDNA of the biflagellated cells of S. algicida (GenBank Accession no. AJ841809) was 3% different from that of a dinoflagellate from Shepherd's Crook and 4% different from that of Cryptoperidiniopsoid sp. brodyi, Pfiesteria spp., or Pfiesteria-like species. In a maximum-likelihood-distance phylogenetic tree generated using the SS rDNA sequences, Pfiesterio spp., Pfiesteria-like species, and a dinoflagellate from Shepherd's Crook were closest to S. algicida, but these dinoflagellates were clearly divergent with S. algicida. Based on morphological and genealogical analyses, we suggest that this is a new species in a new genus.	Seoul Natl Univ, Coll Nat Sci, Sch Earth & Environm Sci, Seoul 151747, South Korea; Seoul Natl Univ, Res Inst Oceanog, Seoul 151747, South Korea; Kunsan Natl Univ, Coll Ocean Sci & Technol, Dept Oceanog, Kunsan 573701, South Korea; Seoul Natl Univ, Coll Nat Sci, Sch Biol Sci, Seoul 151747, South Korea	Seoul National University (SNU); Seoul National University (SNU); Kunsan National University; Seoul National University (SNU)	Seoul Natl Univ, Coll Nat Sci, Sch Earth & Environm Sci, Seoul 151747, South Korea.	hjjeong@snu.ac.kr	Jeong, hae/B-8908-2009	Jeong, Hae Jin/0000-0003-3310-4335				ALTSCHUL SF, 1990, J MOL BIOL, V215, P403, DOI 10.1016/S0022-2836(05)80360-2; BURKHOLDER JM, 1995, ARCH PROTISTENKD, V145, P177, DOI 10.1016/S0003-9365(11)80314-3; Chun J., 2001, PHYDIT VERSION 3 1; Eppley RW., 1975, Proceedings of THE FIRST INTERNATIONAL CONFERENCE ON TOXIC DINOFLAGELLATE BLOOMS, P11; FELSENSTEIN J, 2004, PHYLIP PHYLOGENY INT; GIFFORD D J, 1991, Marine Microbial Food Webs, V5, P161; HANSEN PJ, 1991, MAR ECOL PROG SER, V69, P201, DOI 10.3354/meps069201; HOLMES RW, 1967, LIMNOL OCEANOGR, V12, P503, DOI 10.4319/lo.1967.12.3.0503; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Jeong H. 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Eukaryot. Microbiol.	JUL-AUG	2005	52	4					382	390		10.1111/j.1550-7408.2005.00051.x	http://dx.doi.org/10.1111/j.1550-7408.2005.00051.x			9	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	951PE	16014017				2025-03-11	WOS:000230942000012
J	Reddy, AN; Satyanarayana, K; Bhaktavatsala, KV; Narasimha, K; Nagaraj, M				Reddy, AN; Satyanarayana, K; Bhaktavatsala, KV; Narasimha, K; Nagaraj, M			Sequence stratigraphy and depositional process of Miocene sediments in KD-structure, deepwaters of Krishna-Godavari basin, India	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						KD-structure; sequence stratigraphy; systems tracts; depositional setting; Krishna-Godavari basin	GULF-OF-MEXICO	Detailed chronostratigraphic biodatums and lithofacies in combination with correlative seismic horizons recognized two 3(rd) order depositional sequences designated as Sequence 1 and Sequence 2 in stratigraphic order within Miocene in KD field. The biostratigraphic correlation has brought out that the Sequence 1 in shelf well GS-AD is sandrich and bounded by unconformable sequence boundaries, whereas coeval sequence in slope wells KDA and KDB, bounded by correlative conformities are dominated by clay rich system deposited during highstand sea-levels in early middle Miocene. The clays are planar bedded with glauconite and pyrite nuggets with abundant deepwater benthics in association with shelf derived foraminifera, inferring that these clays were derived into intraslope basins mainly as debris flow/ slump process. The Sequence 2 in wells KDA and KDB is represented by multiple sands with mudstone alternations, deposited during lowstand sea-levels. Biofacies are mixed with dominantly shelf derived benthics and the tests are commonly broken, abraded and occasionally ferruginised, suggesting reworking into intraslope basins as a result of relative sea-level fall during middle and late Miocene. The occurrence of abundant Paleocene to early Miocene dinoflagellate cyst assemblage are also suggesting reworking process into upper slope by network of active channel system and were redeposited by gravity-flow processes into intraslope basins. The present study indicates each intraslope basin acting as an independent petroleum system and matured organic rich Paleogene beds lying at the bottom are contributing hydrocarbons to middle Miocene reservoirs through active growth fault system.	ONGC Ltd, Reg Lab, Madras 600034, Tamil Nadu, India		Reddy, AN (通讯作者)，ONGC Ltd, Reg Lab, NH Rd, Madras 600034, Tamil Nadu, India.	anreddy_54@yahoo.com						[Anonymous], 15 IND C MICR STRAT; [Anonymous], 1977, MEMOIR AM ASS PETROL; Armentrout JM, 1995, SEPM CORE W, P165; ARMENTROUT JM, 1991, PALEONTOLOGIC CONSTR, P137; ARMENTROUT JM, 1996, 17 ANN RES C STRAT A, P7; Barker R.W., 1960, TAXONOMIC NOTES SPEC, P1; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bolli H.M., 1985, P155; Crews JR, 2000, AAPG BULL, V84, P1519; DOW WG, 1990, P GCSSEPM FDN 9 ANN, P139; EMERY D, 1995, BLACKWELL SCI, P1; GALLOWAY WE, 1995, FACIES SUBMARINE CAN, P1; JAIPRAKASH BC, 2001, UNPUB ONGC REP, P1; Kennett J.P., 1983, NEOGENE PLANKTONIC F, P1; Loeblich A.R.J., 1988, FORAMINIFERAL GENERA, P1; MALA J, 2001, UNPUB ONGC REP, P1; Miall A.D., 1997, GEOLOGY STRATIGRAPHI, P1; Migeon S, 2001, MAR PETROL GEOL, V18, P179, DOI 10.1016/S0264-8172(00)00060-X; Mitchum R.M., 1977, Seismic stratigraphy-applications to hydrocarbon exploration, P205; Murray J.W., 1971, ATLAS BRIT RECENT FO, P1; PRIOR DB, 1989, SEDIMENTOLOGY, V36, P1053, DOI 10.1111/j.1365-3091.1989.tb01542.x; RAJU DSN, 1984, UNPUB ONGC, P1; RAJU DSN, 1994, INDIAN J PETR GEOL, V3, P1; Reddy AN, 2000, J GEOL SOC INDIA, V56, P183; Shanmugam G, 1995, SEPM CORE W, P25; Stover L.E., 1978, ANALYSES PREPLEISTOC, P1; STURROCK SJ, 1996, SEQUENCE STRATIGRAPH, P89; Van Morkhoven F. P. C. M., 1986, Bulletin des Centres de Recherches ExplorationProduction ElfAquitaine, V11, P1; Van Wagoner J.C., 1988, SEPM, P39, DOI DOI 10.2110/PEC.88.01.0039; Venkatrangan R., 1993, LITHOSTRATIGRAPHY IN, P1; Williams G.L., 1985, P847; Williams G. L., 1993, GEOL SURV CANADA, P92; WILSON GJ, 1980, 92 NZ GEOL SURV, P1	33	1	1	0	3	SPRINGER INDIA	NEW DELHI	7TH FLOOR, VIJAYA BUILDING, 17, BARAKHAMBA ROAD, NEW DELHI, 110 001, INDIA	0016-7622			J GEOL SOC INDIA	J. Geol. Soc. India	JUL	2005	66	1					42	58						17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	962CT					2025-03-11	WOS:000231709300007
J	Lindberg, K; Moestrup, O; Daugbjerg, N				Lindberg, K; Moestrup, O; Daugbjerg, N			Studies on woloszynskioid dinoflagellates -: I:: <i>Woloszynskia coronata</i> re-examined using light and electron microscopy and partial LSU rDNA sequences, with description of <i>Tovellia</i> gen. nov and <i>Jadwigia</i> gen. nov (Tovelliaceae fam. nov.)	PHYCOLOGIA			English	Article							FLAGELLAR APPARATUS; RIBOSOMAL-RNA; AMPHIDINIUM DINOPHYCEAE; PHYLOGENETIC ANALYSES; MOLECULAR PHYLOGENY; POLARELLA-GLACIALIS; FRESH-WATER; ULTRASTRUCTURE; MORPHOLOGY; PROTISTS	Sediment samples were collected from a small pond in southern Sweden. Several cysts from the samples germinated into clonal cultures, identified as Woloszynskia coronata (Wolosz.) R.H. Thompson 1951. They were compared with other species of Woloszynskia established in culture, using scanning electron microscopy, transmission electron microscopy, partial large subunit ribosomal DNA (LSU rDNA) and morphology of the resting cysts. Significant differences were found, and we conclude that the genus Woloszynskia as presently circumscribed is artificial, and comprises at least four genera. In this first paper we transfer W. coronata to a new genus: Tovellia gen. nov., type species: Tovellia coronata (Wolosz.) comb. nov. Previous studies on ultrastructure and DNA sequencing referring to Wolosynskia coronota are based oil W. coronata var. glabra, which is raised to species level as Tovellia glabra sp. nov. Other species included in the new genus are Tovellia apiciulata (basionym Woloszynskia apiculata Stosch) and Tovellia stoschii (basionym Woloszvnskia stoschii R. Shyam & Sarma). Two identical Cultures presently identified as Woloszynskia limnetica Bursa (from University of Washington Culture Collection, Seattle) and W. pseudopalustris (J. Schiller) Kiselev [from Culture Collection of Algae at the University of Cologne, Cologne] differ from Tovellia in LSU rDNA sequences and in cyst type and are transferred to Jadwigia gen. nov., as J. applanata sp. nov. The most striking feature of Tovellia and Jadwigia is the anatomy of the eyespot, which is extraplastidial, and composed of nonmembrane bound lipid globules. This type of eyespot is also present in Katodinum campylops (T.M. Harris) A.R. Loebl., a species undoubtedly related to Tovellia, and in 'Glenodinium sp.' sensu Kreimer 1999, and together they form a distinct family, Tovelliaceae fam. nov.	Univ Copenhagen, Inst Biochem, Dept Phycol, DK-1353 Copenhagen, Denmark	University of Copenhagen	Univ Copenhagen, Inst Biochem, Dept Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen, Denmark.	moestrup@bi.ku.dk	Daugbjerg, Niels/D-3521-2014	Daugbjerg, Niels/0000-0002-0397-3073; Moestrup, Ojvind/0000-0003-0965-8645				Bibby B.T., 1972, British phycol J, V7, P85; Biecheler B., 1952, Bull. Biol. Fr. Belg., V36, P1; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BURSA A, 1958, J PROTOZOOL, V34, P299; Calado AJ, 2005, PHYCOLOGIA, V44, P112, DOI 10.2216/0031-8884(2005)44[112:OTFDPI]2.0.CO;2; Calado AJ, 2002, PHYCOLOGIA, V41, P567, DOI 10.2216/i0031-8884-41-6-567.1; Calado AJ, 1998, J PHYCOL, V34, P536, DOI 10.1046/j.1529-8817.1998.340536.x; Carty Susan, 2003, P685, DOI 10.1016/B978-012741550-5/50021-0; Chatton E, 1934, CR SOC BIOL, V115, P1036; CHRISTEN H. R., 1958, BER SCHWEIZ BOT GES, V68, P44; Crawford R.M., 1971, Nova Hedwigia, V22, P699; Crawford R. 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Math., Ser. B, V1915, P260	76	70	77	0	14	ALLEN PRESS INC	LAWRENCE	810 E 10TH ST, LAWRENCE, KS 66044 USA	0031-8884			PHYCOLOGIA	Phycologia	JUL	2005	44	4					416	440		10.2216/0031-8884(2005)44[416:SOWDIW]2.0.CO;2	http://dx.doi.org/10.2216/0031-8884(2005)44[416:SOWDIW]2.0.CO;2			25	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	948KM					2025-03-11	WOS:000230714700008
J	Mantle, DJ				Mantle, DJ			New dinoflagellate cyst species from the upper Callovian-lower Oxfordian <i>Rigaudella aemula</i> zone, Timor sea, northwestern Australia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; systematics; Callovian-Oxfordian; Timor Sea; northwestern Australia		Four new species of dinoflagellate cysts are described from Callovian to lower Oxfordian (Jurassic) sediments of the Timor Sea, northwestern Australia. These comprise Evansia? lacryma, Egmontodinium elongatum, Leptodinium? ancoralium, and Nannoceratopsis reticulata. They are rare to common constituents of the Rigaudella aemula dinoflagellate cyst Interval Zone, and may prove useful for regional biostratigraphic correlation. (c) 2005 Elsevier B.V. All rights reserved.	Univ Queensland, Dept Earth Sci, Brisbane, Qld 4072, Australia	University of Queensland	Mantle, DJ (通讯作者)，Univ Queensland, Dept Earth Sci, Brisbane, Qld 4072, Australia.	d.mantle@uq.edu.au						[Anonymous], ANAL PREPLEISTOCENE; ARDITTO PA, 1996, APPEA J, V36, P269; Backhouse J., 1988, GEOL SURV B, V135, P233; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BROOKS DM, 1996, APPEA J, V36, P142; Burger D., 1996, Palynology, V20, P49; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; Davey RJ., 1988, MEMOIR GEOLOGICAL SU, V13, P77; DAVEY RJ, 1982, DANMARKS GEOLOGISK B, P10; DEFLANDRE G, 1964, CR HEBD ACAD SCI, V258, P5027; Deflandre G., 1947, Bulletin de l'Inst Oceanogr Monaco No, V921, P1; DEFLANDRE G, 1939, STATION ZOOLOGIQUE W, V13, P147; EVITT WILLIAM R., 1961, MICROPALEONTOLOGY, V7, P305, DOI 10.2307/1484365; EVITT WR, 1985, AM ASS STRATIGRAPHIC, P333; Fensome R.A., 1993, Micropaleontology Press Special Paper; FENSOME RA, 1979, DINOFLAGELLATE CYSTS, V132, P1; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; GITMEZ GU, 1972, B BR MUS NAT HIS G, V21, P171; Gocht H., 1970, PALAEONTOGRAPHICA B, V129, P125; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P1; HELBY R, 1987, STUDIES AUSTR MESOZO, V4, P135; HELENES J, 1986, Palynology, V10, P73; Helenes Javier, 1997, Palynology, V21, P173; HOCKING RM, 1994, P PETR EXP SOC AUSTR, P22; JANSONIUS J, 1986, Palynology, V10, P201; Klement K. W., 1960, Palaeontographica, VA114, P1; KUMAR A, 1986, REV PALAEOBOT PALYNO, V48, P377, DOI 10.1016/0034-6667(86)90076-X; KUMAR A, 1987, Revista Espanola de Micropaleontologia, V19, P239; Mory A.J., 1988, N W SHELF AUSTR, P287; Patillo J., 1990, APEA J, V30, P27, DOI DOI 10.1071/AJ89002; POCOCK SAJ, 1972, PALAEONTOGR ABT B, V111, P1; POULSEN NE, 1992, REV PALAEOBOT PALYNO, V75, P33, DOI 10.1016/0034-6667(92)90148-A; POULSEN NE, 1996, CONTRIBUTION SERIES, V3; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Quattrocchio M., 1992, Revista Espanola de Micropaleontologia, V24, P67; RIDING JB, 2001, STUDIES AUSTR MESOZO, V24, P111; RIDING JB, 2001, STUDIES AUSTR MESOZO, V24, P65; SARJEANT WAS, 1982, CONTRIBUTIONS SERIES, V9; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; STEVENS J, 1987, STUDIES AUSTR MESOZO, V4, P165; STOVER LE, 1987, STUDIES AUSTR MESOZO, V4, P101; STOVER LEWIS E., 1966, J PALEONTOL, V40, P41; STOVER LS, 1987, MEMOIRS ASS AUSTR PA, P261; Whittam D.B., 1996, APPEA J, V36, P209; Wiggins V.D., 1975, Geoscience Man, V11, P95; WILLIAMS GL, 2000, CONTRIBUTIOS SERIES, V37; WILLIAMS GL, 1998, CONTRIBUTION SERIES, V34; WISEMAN JF, 1980, P 4 INT PAL C LUCKN, P330; WORMALD GB, 1988, N W SHELF AUSTR, P425	51	9	9	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUL	2005	135	3-4					245	264		10.1016/j.revpalbo.2005.05.004	http://dx.doi.org/10.1016/j.revpalbo.2005.05.004			20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	955BT					2025-03-11	WOS:000231200400007
J	Guerstein, GR; Junciel, GL; Guler, MV; Daners, G				Guerstein, GR; Junciel, GL; Guler, MV; Daners, G			<i>Diconodinium</i> <i>lurense</i> sp nov., a late Maastrichtian to Danian dinoflagellate cyst from southwest Atlantic basins	AMEGHINIANA			English	Article						biostratigraphy; dinoflagellate cysts; late Maastrichtian-Danian; southwest Atlantic	ARGENTINA; ISLAND	Upper Cretaceous and Cenozoic deposits from the Colorado and Austral basins, Argentina and the Punta del Este Basin, Uruguay contain diverse organic-walled dinoflagellate cysts, including Diconodinium lurense sp. nov. which occurs in the late Maastrichtian and Danian throughout the basins. The new species is characterized by an autophragm that is densely covered by short spines and by relatively long apical and antapical horns, and by a variable la to IPa archeopyle. On our evidence, the strati-graphical range of Diconodinium lurense sp. nov. is latest Maastrichtian to Danian, and is thus a useful biostratigraphical marker for the Cretaceous-Palaeogene transition in the southwest Atlantic basins.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Argentina; Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina; Fac Ciencias, Dept Palaeontol, Montevideo 11400, Uruguay	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad de la Republica, Uruguay	Univ Nacl Sur, Dept Geol, San Juan 670,B80001CN, RA-8000 Bahia Blanca, Argentina.	gmguerst@criba.edu.ar						[Anonymous], 1831, SYMBOLAE PHYSICAE PA; [Anonymous], 1993, SPEC PUBL NUMBER; [Anonymous], 1987, ASS AUSTRALASIAN PAL; Archangelsky S., 1997, PEJERREY X 1 OFFSHOR; Baschli O., 1885, WISSENSCHAFTLICH DAR, P865; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Brinkhuis H., 2003, P OC DRILL PROGR SCI, V189; Daners G., 2004, CUENCAS SEDIMENTARIA, P37; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Eisenack A., 1960, P R SOC VIC, V72, P1; FRYKLUND R, 1996, 13 C GEOL ARG 3 C EX, V8, P135; GAMERRO J C, 1981, Revista Espanola de Micropaleontologia, V13, P119; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Haeckel E., 1894, Systematische Phylogenie. Vol. 1. Systematische Phylogenie der Protisten und Pflanzen, V1; JUAN R, 1996, 13 C GEOL ARG 3 C EX, V7, P117; Kaasschieter J.P.H., 1963, TULSA GEOLOGICAL SOC, V31, P177; Macellari C.E., 1989, J S AM EARTH SCI, V2, P223; Malumian N, 1997, J S AM EARTH SCI, V10, P189, DOI 10.1016/S0895-9811(97)00015-1; Marenssi S, 2004, CRETACEOUS RES, V25, P907, DOI 10.1016/j.cretres.2004.08.004; Marenssi S. A., 2002, Rev. Asoc. Geol. Argent., V57, P341; Morgan R., 1977, Palynology, V1, P123; NULLO FE, 1981, CUENCAS SEDIMENTARIA, P181; Papu O.H., 1997, REV ESP PALEONTOL, V12, P197; Pascher A., 1914, Berlin Ber D bot Ges, V32; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Ucha N., 2003, CUENCAS SEDIMENTARIA, P171; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; WILLIAMS GL, 1998, SOC SEDIMENTARY GEOL, V60, P9; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; WOOD SE, 1992, ANTARCT SCI, V4, P327, DOI 10.1017/S0954102092000488	31	7	8	0	1	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	JUN 30	2005	42	2					329	338						10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	958WO					2025-03-11	WOS:000231479100005
J	Guler, MV; Guerstein, GR; Casadío, S				Guler, MV; Guerstein, GR; Casadío, S			New dinoflagellate cyst species from the Calafate Formation (Maastrichtian), Austral Basin, Argentina	AMEGHINIANA			English	Article						dinoflagellate cysts; Maastrichtian; Calafate Formation; Austral Basin; Argentina		The aim of this paper is to erect four new dinoflagellate cyst species from the Maastrichtian Calafate Formation, Austral Basin, Argentina. Andalusiella spinosa sp. nov. is strongly acrocavate and possesses a periphragm covered with spines. Palaeocystodinium pilatium sp. nov. has a periphragm densely covered with fine, flexuous, hair-like projections, shortening towards the end of the horns, and a finely granulate endophragm. The large peridinialean Caligodinium perforation sp. nov. shows the hypocystal archeopyle typical for the genus, with a simple triplacoid opercular piece and, a microfoveolate autophragm surrounded by a perforate flocculent calyptra. Hafniasphaera australis sp. nov. is differentiated from other species of the genus Hafniasphaera by the presence of a distinctive anterior ventral process which emerges at the junction of paraplates 1', 4' and as. These new species characterize the assemblages from deposits related to the South Atlantic transgression that occurred during Maastrichtian times at the southermost part of Argentina.	Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina; Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Univ Nacl La Pampa, Fac Ciencias Exactas & Nat, RA-6300 Santa Rosa, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina.	vguler@criba.edu.ar; gmguerst@criba.edu.ar; scasadio@cpenet.com.ar	Casadio, Silvio/A-5131-2010					Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; Baschli O., 1885, WISSENSCHAFTLICH DAR, P865; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; BOLTENHAGEN E, 1977, CAHIERS PALEONTOLOGY; BUJAK JP, 1983, AM ASOACIATION STRAT, V13; COOKSON IC, 1964, P ROYAL SOC VICTORIA, V77, P521; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; DRUGG W.S., 1967, PALAEONTOGRAPHICA B, V120, P1; Drugg W.S., 1970, P N AM PAL CONV CH G, P809; Ehrenberg CG, 1831, SYMBOLAE PHYS PARS Z; Fensome R.A., 1993, CLASSIFICATION FOSSI; FENSOME RA, 1998, DINOFLAJ GEOLOGICAL; Feruglio E., 1949, Descripcion geologica de la Patagonia; Furque G., 1973, Servicio Nacional de Mineria y Geologia, Boletin, V140, P1; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; IOANNIDES N.S., 1986, B GEOLOGICAL SURVEY, V371, P1; LENTIN JK, 1976, BIR7516 BEDF I OC RE, P1; Lindemann E, 1928, NATURLICHEN PFLANZEN, P3; Macellari C.E., 1989, J S AM EARTH SCI, V2, P223; Malumian N, 1997, J S AM EARTH SCI, V10, P189, DOI 10.1016/S0895-9811(97)00015-1; Malumian N., 1999, ANALES I GEOLOGIA RE, V29, P557; Manum S., 1964, Skrifter utgitt av det Norske Videnskapsakademi Mat Nat Kl NS, VNo. 17, P1; Manum Svein B., 1995, Palynology, V19, P183; Marenssi S, 2004, CRETACEOUS RES, V25, P907, DOI 10.1016/j.cretres.2004.08.004; Marenssi S. A., 2002, Rev. Asoc. Geol. Argent., V57, P341; Masure E, 1996, REV PALAEOBOT PALYNO, V91, P171, DOI 10.1016/0034-6667(95)00061-5; NULLO FE, 1981, CUENCAS SEDIMENTARIA, P181; Pascher A., 1914, Berlin Ber D bot Ges, V32; Riegel W., 1974, Revista Esp Micropaleont, V6, P347; Slimani H., 1994, MEMOIRES SERVIR EXPL, P37; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; WILSON GJ, 1977, NEW ZEAL J GEOL GEOP, V20, P563, DOI 10.1080/00288306.1977.10427601; WILSON GRAEME J., 1967, N Z J BOT, V5, P223; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321	38	8	9	0	0	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	JUN 30	2005	42	2					419	428						10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	958WO					2025-03-11	WOS:000231479100012
J	Beccaletto, L; Bartolini, AC; Martini, R; Hochuli, PA; Kozur, H				Beccaletto, L; Bartolini, AC; Martini, R; Hochuli, PA; Kozur, H			Biostratigraphic data from the Cetmi Melange, northwest Turkey: Palaeogeographic and tectonic implications	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						melange; NW Turkey; biostratigraphy; conodonta; foraminifera; radiolaria; palynomorphs	KARAKAYA COMPLEX; ARC ORIGIN; SUBDUCTION; EVOLUTION; ANATOLIA; GEOLOGY; BASIN; ASSOCIATIONS; METAMORPHISM; COLLISION	The Cetmi accretionary melange is cropping out in the Biga Peninsula of northwest Turkey. It is characterised by an isolated position, relatively far from the accretion complexes of the nearest suture zones, which raises the question of its lateral correlations. A detailed biostratigraphic investigation of the limestone and radiolarite blocks and the matrix of the Cetmi melange allowed to propose a solution for this palaeogeographic problem. Scarce red nodular limestones in the Han Bulog facies represent the oldest lithology in the melange. Their Late Scythian-Ladinian age is based on Chiosella gondolleloides, the co-occurrence of Gladigondolella sp. and Nicoraella cf. kockeli, and Paragondolella fuelopi. Light grey limestone blocks are a characteristic feature of the Cetmi melange. They occur in two distinct facies. Facies A consists of packstone to grainstone, and is characterised by unsorted and poorly washed pelbiosparites. Facies B consists of wackestone to packstone, and is characterised by poorly washed biopelmicrites to biopelsparites. The foraminiferal assemblage of Facies A, containing Triasina hantkeni, is of Late Norian to Rhaetian age. The foraminiferal assemblage of Facies B never contains T hantkeni, and is characteristic of a Late Triassic (Camian? to Norian-Rhaetian) age. Radiolarian cherts are widely distributed in the Cetmi melange. They record fully pelagic sedimentation from the Upper Bajocian to the Aptian. The matrix of the Cetmi melange consists of brown to black shales, sometimes silty or siliceous, intercalated with dark grey greywackes. Palynomorphs of one sample of brownish silty shale yielded an Early to Middle Albian age, based on the co-occurrence of several dinoflagellate cysts. The age of the matrix, representing the youngest lithology within the melange, and of the unconformable overlaying section (latest Albian-Cenomanian) indicate that the melange-forming process stopped between the Early Albian and the latest Albian-Cenomanian. At a regional scale, the Cetmi melange has little in common with the melanges from the Izmir-Ankara and Intra-Pontide sutures of northwestern Turkey precluding a direct correlation. On the other hand, the Cetmi melange shares several characteristics with the melange-like units of the eastern Rhodope Zone (Bulgaria and Greece), like a major Cenomanian transgression, the reworking of Triassic limestones and Middle Jurassic-Lower Cretaceous radiolarians, and the absence of Jurassic-Cretaceous passive margin lithologies. The occurrence of Rhodopian units on the Biga Peninsula suggests that the studied units represent an isolated fragment of the Rhodope Zone in NW Turkey. (c) 2005 Elsevier B.V. All rights reserved.	Univ Lausanne, Geosci & Environm Fac, Inst Geol & Paleontol, CH-1015 Lausanne, Switzerland; Univ Paris 06, Lab Micropaleontol, F-75252 Paris, France; Univ Geneva, Dept Geol & Paleontol, CH-1205 Geneva, Switzerland; Univ Zurich, Inst Paleontol, CH-8006 Zurich, Switzerland	University of Lausanne; Sorbonne Universite; University of Geneva; University of Zurich	Univ Lausanne, Geosci & Environm Fac, Inst Geol & Paleontol, BFSH-2, CH-1015 Lausanne, Switzerland.	laurent.beccaletto@igp.unil.ch; chiara@ccr.jussieu.fr; Rossana.Martini@terre.unige.ch; peter.hochuli@erdw.ethz.ch; kozurh@helka.iif.hu	Bartolini, Annachiara/AAO-7944-2020; Beccaletto, Laurent/AAN-8094-2020	Rossana, Martini/0000-0002-0674-863X; Beccaletto, Laurent/0000-0003-2132-1738				ALSHAIBANI S, 1982, ARC SCI GENEVE, P137; Altiner Demir, 1991, Geologica Romana, V27, P13; ALTNER D, 1980, RIV ITAL PALEONTOL S, V86, P705; [Anonymous], 1999, P INT S SHALLOW TETH, V5, P101; [Anonymous], THESIS U PARIS SUD O; [Anonymous], GREAT BRITAIN GEOLOG; [Anonymous], B GEOLOGICAL SOC FRA; Babic L, 2002, ECLOGAE GEOL HELV, V95, P263; BAILEY E, 1950, NATURE, V166, P938, DOI 10.1038/166938a0; Bailey E.B., 1953, Transactions of the Royal Society of Edinburgh, V62, P403, DOI DOI 10.1017/S0080456800009340; BAMGARTNER PO, 1985, MEMOIRES SOC HELVETI, P111; BAUMGARTNER P O, 1976, Eclogae Geologicae Helvetiae, V69, P601; Baumgartner P. 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Paleoclimatol. Paleoecol.	JUN 9	2005	221	3-4					215	244		10.1016/j.palaeo.2005.02.011	http://dx.doi.org/10.1016/j.palaeo.2005.02.011			30	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	934LK					2025-03-11	WOS:000229710100003
J	Filipsson, HL; Björk, G; Harland, R; McQuoid, MR; Nordberg, K				Filipsson, HL; Björk, G; Harland, R; McQuoid, MR; Nordberg, K			A major change in the phytoplankton of a Swedish sill fjord -: A consequence of engineering work?	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						diatoms; dinoflagellate cysts; environmental change; engineering work; fjord; Sweden	DINOFLAGELLATE CYST RECORD; WEST-COAST; KOLJO-FJORD; SURFACE SEDIMENTS; SWEDEN; VARIABILITY; SKAGERRAK; DIATOMS	A major phytoplankton change occurred during the late 1930s and early 1940s in Koljo Fjord, a sill fjord on the Swedish west coast. Dinoflagellate cyst concentrations increased tenfold over a short period of time, front hundreds of cysts per gram sediment to thousands; and the species composition of both dinoflagellate cysts and diatoms changed markedly. These changes took place during a period of extensive engineering work at the entrance to the fjord from the Skagerrak. At this time, the entire passage was straightened, a new channel was built in a previously shallow area, and the old connection was closed. This study investigates whether this engineering work could have sufficiently altered the surface-water circulation to bring about the change in the phytoplankton composition. Several mechanisms are explored by which the construction could have influenced the phytoplankton in the fjord. The primary mechanism is probably increased efficiency of tidal-generated surface-water exchange in the fjord, resulting in a larger transport of surface water from the Skagerrak and consequently a changed surface-water environment. This Study highlights how engineering work can have a Substantial impact on the local and regional marine environment, a factor that must not be overlooked in environmental planning. (c) 2005 Elsevier Ltd. All rights reserved.	Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden; DinoData Serv, Nottingham NG13 8AH, England; Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden	University of Gothenburg; University of Gothenburg	Filipsson, HL (通讯作者)，Univ Bremen, Dept Geosci, MARUM, POB 330 440, DE-28334 Bremen, Germany.	filipsson@uni-bremen.de	Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Nordberg, Kjell/0000-0003-0085-4607				[Anonymous], 2000, BIOL ATLAS ARCTIC SE; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Björk G, 2000, ESTUARIES, V23, P367, DOI 10.2307/1353329; Björk G, 2003, CONT SHELF RES, V23, P1143, DOI 10.1016/S0278-4343(03)00081-5; Dale B, 2000, T GEOBIOL, V15, P305; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Filipsson HL, 2004, J FORAMIN RES, V34, P277, DOI 10.2113/34.4.277; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Gustafsson B, 1999, CONT SHELF RES, V19, P1021, DOI 10.1016/S0278-4343(99)00008-4; Haamer J, 2000, J SHELLFISH RES, V19, P413; HANSSON W, 1979, ZINDERMANS; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HARLAND R, 1989, J GEOL SOC LONDON, V146, P945, DOI 10.1144/gsjgs.146.6.0945; Hasle G.R., 1973, 2 S RECENT FOSSIL MA, P1; HEILMANN JP, 1994, MAR ECOL PROG SER, V112, P213, DOI 10.3354/meps112213; Kennington K, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P166; Lindahl O., 2003, ICES MAR SCI S, V219, P387; McQuoid MR, 2004, LIMNOL OCEANOGR, V49, P1123, DOI 10.4319/lo.2004.49.4.1123; McQuoid MR, 2003, ESTUARIES, V26, P927, DOI 10.1007/BF02803351; McQuoid MR, 2002, J PHYCOL, V38, P881, DOI 10.1046/j.1529-8817.2002.01169.x; McQuoid MR, 1997, J PLANKTON RES, V19, P173, DOI 10.1093/plankt/19.2.173; MOHLENBERG F, 1995, OPHELIA, V42, P239, DOI 10.1080/00785326.1995.10431507; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Norén F, 1999, MAR ECOL PROG SER, V191, P187, DOI 10.3354/meps191187; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Svansson Artur., 1975, PHYS CHEM OCEANOGRAP; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	30	16	18	0	7	ACADEMIC PRESS LTD ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0272-7714			ESTUAR COAST SHELF S	Estuar. Coast. Shelf Sci.	JUN	2005	63	4					551	560		10.1016/j.ecss.2005.01.001	http://dx.doi.org/10.1016/j.ecss.2005.01.001			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	935UW					2025-03-11	WOS:000229809900008
J	Smith, BC; Persson, A				Smith, BC; Persson, A			Synchronization of encystment of <i>Scrippsiella</i> <i>lachrymosa</i> (Dinophyta)	JOURNAL OF APPLIED PHYCOLOGY			English	Article						cyst; dinoflagellate; encyst; gamete; mating; Scrippsiella lachrymosa	DINOFLAGELLATE GONYAULAX-TAMARENSIS; CYST FORMATION; GROWTH	The encystment of Scrippsiella lachrymosa cells (strain B-10), which can be induced reliably in encystment medium, was inhibited by stirring the culture. 100 mL cultures in glass beakers were stirred at 1 rotation s(-1). Stirring inhibited vegetative cells from congregating (swarming) at the walls of the culture container. When stirring was stopped, a rapid induction of sexual reproduction was seen. As soon as stirring stopped (within 2 min), cells were observed swarming near the edges of the glass beaker. Four days after cessation of stirring, large percentages of the cells were mating and, after 7 days, most were zygotes. Cultures were observed after 31, 38, and, 45 days of stirring. When cultures were stirred for 45 days, cysts developed in the stirred treatments, but these cysts were attached to flocculent material that had also formed in the medium. The use of this laboratory method is advantageous for the study of the mating through cyst stages of the dinoflagellate life history. This method may also demonstrate the need for a 'surface' as a place for the dinoflagellate to congregate in order to successfully encyst and may help explain environmental observations of encystment at pycnoclines.	Natl Marine Fisheries Serv, NOAA, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Natl Marine Fisheries Serv, NOAA, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514				ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Dale B., 1983, P69; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; Juhl AR, 2002, J PHYCOL, V38, P683, DOI 10.1046/j.1529-8817.2002.00165.x; Lewis J., 2001, lifehab life histories of microalgal species causing harmful blooms, P49; LEWIS J., 2001, LIFEHAB LIFE HIST MI, P121; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53; Sullivan JM, 2003, HARMFUL ALGAE, V2, P183, DOI 10.1016/S1568-9883(03)00039-8; Sullivan JM, 2003, J PHYCOL, V39, P83, DOI 10.1046/j.1529-8817.2003.02094.x; TAYLOR FJR, 1987, BOT MONOGR, V21, P224; Vogel S., 1994, LifeinMovingFluids: ThePhysicalBiologyofFlowRevisedandExpandedSecondEdition; Von Stosch HA., 1973, Br Phycol J, V8, P105	16	15	15	1	3	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-8971	1573-5176		J APPL PHYCOL	J. Appl. Phycol.	JUN	2005	17	4					317	321		10.1007/s10811-005-4944-6	http://dx.doi.org/10.1007/s10811-005-4944-6			5	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	954NB					2025-03-11	WOS:000231160700005
J	Gagnon, R; Levasseur, M; Weise, AM; Fauchot, J; Campbell, PGC; Weissenboeck, BJ; Merzouk, A; Gosselin, M; Vigneault, B				Gagnon, R; Levasseur, M; Weise, AM; Fauchot, J; Campbell, PGC; Weissenboeck, BJ; Merzouk, A; Gosselin, M; Vigneault, B			Growth stimulation of <i>Alexandrium tamarense</i> (Dinophyceae) by humic substances from the Manicouagan River (Eastern Canada)	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium tamarense; growth rate; humic substances; Manicouagan River; St. Lawrence Estuary	TOXIC DINOFLAGELLATE; PHYTOPLANKTON BLOOMS; MARINE-PHYTOPLANKTON; CYST FORMATION; COASTAL; IRON; TRANSPORT; DIATOMS; WATERS; JAPAN	In the St. Lawrence Estuary, annual recurrent blooms of the toxic dinoflagellate Alexandrium tamarense L. Balech are associated with brackish waters. Riverine inputs are suspected to favor bloom development by increasing water column stability and/or by providing growth stimulants such as humic substances (HS). A 17-day culture experiment was conducted to evaluate the importance of HS as growth factors for A. tamarense. Nonaxenic cultures were exposed to four HS extracts from three different sources: humic and fulvic acids isolated from the Manicouagan River, Quebec, Canada; humic acids from the Suwannee River, Georgia, United States; and a desalted alkaline soil extract. For each extract, four concentrations were tested as supplements to the artificial Keller medium, a nitrate-rich algal culture medium. Additions of HS from all sources significantly enhanced the overall growth rates relative to the controls. Concentrations of HS, estimated by UV spectrophotometry, remained constant throughout the exponential growth phase, suggesting that the HS were acting mainly as growth promoters during our experiment. Dose-response curves indicated that HS could increase the growth rate of A. tamarense even at low concentrations, such as those encountered in the St. Lawrence Estuary. Our results support the hypothesis that HS from the Manicouagan River plume can stimulate the development of toxic dinoflagellate blooms.	Fisheries & Oceans Canada, Maurice Lamontagne Inst, Mont Joli, PQ G5H 3Z4, Canada; Univ Quebec, INRS Eau Terre & Environm, Ste Foy, PQ G1V 4C7, Canada; Univ Quebec, Inst Sci Mer, Rimouski, PQ G5L 3A1, Canada; Nat Resources Canada, Canmet Mines & Mineral Sci Labs, Ottawa, ON K1A 0G1, Canada	Fisheries & Oceans Canada; University of Quebec; Institut national de la recherche scientifique (INRS); University of Quebec; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; CanmetMINING	Fisheries & Oceans Canada, Maurice Lamontagne Inst, 850 Route Mer, Mont Joli, PQ G5H 3Z4, Canada.	gagnonr@dfo-mpo.gc.ca	Campbell, Peter/H-4348-2011; Fauchot, Juliette/HHS-0759-2022; Gosselin, Michel/B-4477-2014	Gosselin, Michel/0000-0002-1044-0793				ACHIHA H, 1990, JPN J PHYCOL, V38, P31; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON MA, 1982, LIMNOL OCEANOGR, V27, P789, DOI 10.4319/lo.1982.27.5.0789; BARBER R T, 1969, Journal of Experimental Marine Biology and Ecology, V3, P191, DOI 10.1016/0022-0981(69)90017-3; BLASCO D, 1998, MONITORAGE PHYTOPLAN; BRASSARD P, 1984, CAN J FISH AQUAT SCI, V41, P166, DOI 10.1139/f84-017; Buffle J., 1988, COMPLEXATION REACTIO; Campbell P.G.C., 1995, Metal Speciation and Bioavailability in Aquatic Systems, P45; Campbell PGC, 1997, CAN J FISH AQUAT SCI, V54, P2543, DOI 10.1139/f97-161; CARLSSON P, 1995, MAR ECOL PROG SER, V127, P213, DOI 10.3354/meps127213; Carlsson P, 1999, AQUAT MICROB ECOL, V18, P23, DOI 10.3354/ame018023; Carlsson P, 1998, AQUAT MICROB ECOL, V16, P65, DOI 10.3354/ame016065; Carlsson P., 1998, NATO ASI Series Series G Ecological Sciences, V41, P509; CARLSSON P, 1993, ESTUAR COAST SHELF S, V36, P433, DOI 10.1006/ecss.1993.1026; DERAUSCH, 1990, SYMBIOSIS, V8, P117; Doblin MA, 1999, J EXP MAR BIOL ECOL, V236, P33, DOI 10.1016/S0022-0981(98)00193-2; Doblin MA, 2000, J PLANKTON RES, V22, P421, DOI 10.1093/plankt/22.3.421; Doucette G.J., 1998, HARMFUL ALGAE, P406; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Fauchot J, 2005, J PHYCOL, V41, P263, DOI 10.1111/j.1529-8817.2005.03092.x; Frangópulos M, 2004, HARMFUL ALGAE, V3, P131, DOI 10.1016/S1568-9883(03)00061-1; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; GRANELI E, 1990, J EXP MAR BIOL ECOL, V136, P89, DOI 10.1016/0022-0981(90)90189-J; Graneli E., 1985, P201; Graneli E., 1999, AQUAT ECOL, V33, P17, DOI DOI 10.1023/A:1009925515059; Hamasaki K, 2001, J PLANKTON RES, V23, P271, DOI 10.1093/plankt/23.3.271; McKnight DM., 1998, Aquatic humic substances: ecology and biochemistry, P9; HUDSON RJM, 1990, LIMNOL OCEANOGR, V35, P1002, DOI 10.4319/lo.1990.35.5.1002; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Juhl AR, 2001, LIMNOL OCEANOGR, V46, P758, DOI 10.4319/lo.2001.46.4.0758; KELLER MD, 1987, J PHYCOL, V23, P633; Koutitonsky V.G., 1991, CAN SPEC PUBL FISH A, V113, P57; Legrand C, 1998, AQUAT MICROB ECOL, V16, P81, DOI 10.3354/ame016081; LOEBLICH AR, 1975, J PHYCOL, V11, P80, DOI 10.1111/j.1529-8817.1975.tb02752.x; MCLACHLAN J, 1975, HDB PHYCOLOGICAL MET, P26; MOITA MT, 1993, DEV MAR BIO, V3, P299; MORLAIX M, 1992, COMP STUDY; Ohkubo N, 1998, ENVIRON TECHNOL, V19, P611, DOI 10.1080/09593331908616717; PAERL HW, 1988, LIMNOL OCEANOGR, V33, P823, DOI 10.4319/lo.1988.33.4_part_2.0823; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Petrovic M, 1996, WATER SCI TECHNOL, V34, P253, DOI 10.1016/S0273-1223(96)00752-4; PRAKASH A, 1973, LIMNOL OCEANOGR, V18, P516, DOI 10.4319/lo.1973.18.4.0516; SCHECHER WD, 1992, COMPUTERS ENV URBAN, V16; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; SMITH WO, 1982, J PLANKTON RES, V4, P651, DOI 10.1093/plankt/4.3.651; Sohet K., 1995, P669; SU HM, 1993, DEV MAR BIO, V3, P837; SULLIVAN JM, 1997, EFFECTS SMALL SCALE; Sunda WG., 1988, BIOL OCEANOGR, V6, P411, DOI DOI 10.1080/01965581.1988.10749543; SUNDA WG, 1998, SCI TOTAL ENVIRON, V219, P2; Therriault J.C., 1985, P141; THURMAN EM, 1981, ENVIRON SCI TECHNOL, V15, P463, DOI 10.1021/es00086a012; Toyota Takayoshi, 1994, Journal of Oceanography, V50, P499, DOI 10.1007/BF02235420; Vigneault B, 2000, ENVIRON SCI TECHNOL, V34, P3907, DOI 10.1021/es001087r; Weise AM, 2002, CAN J FISH AQUAT SCI, V59, P464, DOI 10.1139/F02-024; Yamamoto Tamiji, 1999, Phycological Research, V47, P27, DOI 10.1111/j.1440-1835.1999.tb00280.x	57	43	54	1	30	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	JUN	2005	41	3					489	497		10.1111/j.1529-8817.2005.00077.x	http://dx.doi.org/10.1111/j.1529-8817.2005.00077.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	930OV					2025-03-11	WOS:000229426700005
J	Kremp, A; Elbrächter, M; Schweikert, M; Wolny, JL; Gottschling, M				Kremp, A; Elbrächter, M; Schweikert, M; Wolny, JL; Gottschling, M			<i>Woloszynskia halophila</i> (Biecheler) comb. nov.:: A bloom-forming cold-water dinoflagellate co-occurring with <i>Scrippsiella hangoei</i> (Dinophyceae) in the Baltic Sea	JOURNAL OF PHYCOLOGY			English	Article						28S rRNA; dinoflagellate cysts; morphology; salinity tolerance; taxonomy; ultrastructure; Woloszynskia	RIBOSOMAL-RNA; SPRING-BLOOM; FLAGELLAR APPARATUS; RESTING CYSTS; ULTRASTRUCTURE; PHYTOPLANKTON; PHYLOGENY; MICROORGANISMS; IDENTIFICATION; GERMINATION	Molecular analyses and subsequent morphological reinvestigation of clonal isolates germinated from cysts previously assigned to Scrippsiella hangoei (Schiller) Larsen revealed considerable differences to vegetative cell isolates of this cold-water dinoflagellate from the northern Baltic Sea. The presence of hexagonal platelets on the cell surface and a characteristic acrobase on the episome agree with the description of Gymnodinium halophilum Biecheler. However, the arrangement of amphiesmal vesicles in more than nine latitudinal series indicates allocation of this dinoflagellate to Woloszynskia Thompson. We therefore reassign G. halophilum to Woloszynskia halophila. This species exhibits ultrastructural characteristics similar to Polarella glacialis Montresor et al. and symbiontic Gymnodinium Stein, such as stalked pyrenoids and a central eyespot consisting of multiple layers of crystal-filled vacuoles. A close relationship between these dinoflagellates is also supported by 28s rRNA sequence data. The preference for high salinities identifies W. halophila as a marine species. The spiny resting cysts of W. halophila are identical to the cysts formed during the massive encystment events previously attributed to S. hangoei in the Baltic Sea. This suggests that W. halophila is a significant contributor to the dinoflagellate spring blooms in the Baltic Sea. Scrippsiella hangoei clones, in turn, produce noncalcareous and smooth-walled cysts when crossed with a complementary mating type.	Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland; Deutsch Zentrum Marine Biodivers Forsch, Forschungsinst Senckenberg, Wattenmeerstn Sylt, D-25992 List Auf Sylt, Germany; Univ Stuttgart, Inst Biol, Abt Zool, D-70569 Stuttgart, Germany; Florida Marine Res Inst, Florida Inst Oceanog, St Petersburg, FL 33701 USA; Free Univ Berlin, Fachbereich Geol Wissensch, D-12249 Berlin, Germany	University of Helsinki; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Stuttgart; Free University of Berlin	Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland.	anke.kremp@helsinki.fi	Kremp, Anke/I-8139-2013; Gottschling, Marc/K-2186-2014	Schweikert, Michael/0000-0001-8869-709X; Wolny, Jennifer L./0000-0002-3556-5015				[Anonymous], 1996, ZOOL ANZ; [Anonymous], ACTA BOT FENN; [Anonymous], 1981, Fixation for electron microscopy; AUTIO R, 1990, ECOLOGICAL PLANKTON; Berard-Therriault L., 1999, Publ spec can sci halieut aquat, V128, P1; Bibby B.T., 1972, British phycol J, V7, P85; Biecheler B., 1952, Bull. 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Phycol.	JUN	2005	41	3					629	642		10.1111/j.1529-8817.2005.00070.x	http://dx.doi.org/10.1111/j.1529-8817.2005.00070.x			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	930OV					2025-03-11	WOS:000229426700018
J	Litaker, RW; Steidinger, KA; Mason, PL; Landsberg, JH; Shields, JD; Reece, KS; Haas, LW; Vogelbein, WK; Vandersea, MW; Kibler, SR; Tester, PA				Litaker, RW; Steidinger, KA; Mason, PL; Landsberg, JH; Shields, JD; Reece, KS; Haas, LW; Vogelbein, WK; Vandersea, MW; Kibler, SR; Tester, PA			The reclassification of <i>Pfiesteria shumwayae</i> (Dinophyceae):: <i>Pseudopfiesteria</i>, gen. nov.	JOURNAL OF PHYCOLOGY			English	Article						evolution; Pfiesteria-like dinoflagellates; Pfiesteria shumwayae; Pseudopfiesteria; ribosomal genes; taxonomy	LIFE-CYCLE; DINOFLAGELLATE PFIESTERIA; PISCICIDA DINOPHYCEAE; TOXIC DINOFLAGELLATE; SUBSTITUTION; DNA; IDENTIFICATION; PHYLOGENIES; OCELLATUM; DISCOVERY	Pfiesteria shumwayae Glasgow et Burkholder is assigned to a new genus Pseudopfiesteria gen. nov. Plate tabulation differences between Pfiesteria and Pseudopfiesteria gen. nov. as well as a maximum likelihood phylogenetic analysis based on rDNA sequence data warrant creation of this new genus. The Kofoidian thecal plate formula for the new genus is Po, cp, X, 4', 1a, 6 '', 6c, PC, 5+s, 5''', 0p, 2''''. In addition to having six precingular plates, P. shumwayae comb. nov. also has a distinctive diamond or rectangular-shaped anterior intercalary plate. Both Pfiesteria and Pseudopfiesteria gen. nov. are reassigned to the order Peridiniales based on an apical pore complex (APC) with a canal (X) plate that contacts a symmetrical 1', four to five sulcal plates, and the conservative hypothecal tabulation of 5''', 0p, and 2''''. These morphological characters and the life histories of Pfiesteria and Pseudopfiesteria are consistent with placement of both genera in the Peridiniales. Based on the plate tabulations for P. shumwayae, P. piscicida, and the closely related "cryptoperidiniopsoid" and "lucy" groups, the family Pfiesteriaceae is amended to include species with the following tabulation: 4-5', 0-2a, 5-6 '', 6c, PC, 5+s, 5''', 0p, and 2'''' as well as an APC containing a pore plate (Po), a closing plate (cp), and an X plate; the tabulation is expanded to increase the number of sulcal plates and to include a new plate, the peduncle cover (PC) plate. Members of the family have typical dinoflagellate life cycles characterized by a biflagellated free-living motile stage, a varying number of cyst stages, and the absence of multiple amoeboid stages.	Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, NOAA, Beaufort, NC 28516 USA; Florida Fish & Wildlife Conservat Commiss, Fish & Wildlife Res Inst, St Petersburg, FL 33701 USA; Coll William & Mary, Dept Environm & Aquat Anim Hlth, Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; Florida Fish & Wildlife Conservation Commission; William & Mary; Virginia Institute of Marine Science	Litaker, RW (通讯作者)，Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, NOAA, 101 Pivers Isl Rd, Beaufort, NC 28516 USA.	Wayne.Litaker@noaa.gov	Litaker, Richard/AAH-2036-2021	Reece, Kimberly/0000-0002-1751-1566; Shields, Jeffrey D./0000-0002-2658-4572				[Anonymous], 2002, PAUP 4 0 PHYLOGENETI; Boltovskoy A, 1999, GRANA, V38, P98, DOI 10.1080/713786927; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; BURKHOLDER JM, 1995, ARCH PROTISTENKD, V145, P177, DOI 10.1016/S0003-9365(11)80314-3; Coyne KJ, 2001, AQUAT MICROB ECOL, V24, P275, DOI 10.3354/ame024275; *CSIRO MAR RES, 2001, PFIEST SHUMW AUSTR; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome RA, 1999, GRANA, V38, P66; Glasgow HB, 2001, PHYCOLOGIA, V40, P234, DOI 10.2216/i0031-8884-40-3-234.1; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HASEGAWA M, 1985, J MOL EVOL, V22, P160, DOI 10.1007/BF02101694; Hershkovitz MA, 1998, METHOD BIOCHEM ANAL, V39, P189; Jakobsen KS, 2002, P ROY SOC B-BIOL SCI, V269, P211, DOI 10.1098/rspb.2001.1852; Kokocinski Mikolaj, 2003, Journal of Limnology, V62, P172; LANAVE C, 1984, J MOL EVOL, V20, P86, DOI 10.1007/BF02101990; LANDSBERG JH, 1994, DIS AQUAT ORGAN, V20, P23, DOI 10.3354/dao020023; Litaker R.W., 2002, Manual of environmental microbiology, V2nd, P342; Litaker RW, 2003, J PHYCOL, V39, P754, DOI 10.1046/j.1529-8817.2003.02112.x; Litaker RW, 2002, J PHYCOL, V38, P442, DOI 10.1046/j.1529-8817.2002.t01-1-01242.x; Litaker RW, 1999, J PHYCOL, V35, P1379, DOI 10.1046/j.1529-8817.1999.3561379.x; Mason PL, 2003, J PHYCOL, V39, P253, DOI 10.1046/j.1529-8817.2003.02089.x; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; Parrow MW, 2003, J PHYCOL, V39, P697, DOI 10.1046/j.1529-8817.2003.03057.x; Parrow MW, 2003, J PHYCOL, V39, P678, DOI 10.1046/j.1529-8817.2003.02146.x; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Rhodes LL, 2002, NEW ZEAL J MAR FRESH, V36, P621, DOI 10.1080/00288330.2002.9517117; Rublee PA, 2001, ENVIRON HEALTH PERSP, V109, P765, DOI 10.2307/3454924; Steidinger K, 2001, ENVIRON HEALTH PERSP, V109, P661, DOI 10.2307/3454911; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; THOMPSON JD, 1994, NUCLEIC ACIDS RES, V22, P4673, DOI 10.1093/nar/22.22.4673; Truby EW, 1997, MICROSC RES TECHNIQ, V36, P337; Vogelbein WK, 2001, ENVIRON HEALTH PERSP, V109, P687, DOI 10.2307/3454914; YANG ZB, 1994, J MOL EVOL, V39, P105; Yang ZH, 1996, TRENDS ECOL EVOL, V11, P367, DOI 10.1016/0169-5347(96)10041-0	36	51	56	1	12	BLACKWELL PUBLISHING INC	MALDEN	350 MAIN ST, MALDEN, MA 02148 USA	0022-3646			J PHYCOL	J. Phycol.	JUN	2005	41	3					643	651		10.1111/j.1529-8817.2005.00075.x	http://dx.doi.org/10.1111/j.1529-8817.2005.00075.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	930OV					2025-03-11	WOS:000229426700019
J	Patterson, RT; Prokoph, A; Kumar, A; Chang, AS; Roe, HM				Patterson, RT; Prokoph, A; Kumar, A; Chang, AS; Roe, HM			Late Holocene variability in pelagic fish scales and dinoflagellate cysts along the west coast of Vancouver Island, NE Pacific Ocean	MARINE MICROPALEONTOLOGY			English	Article						Holocene; northeast Pacific Ocean; fish scales; dinoflagellate cysts; paleoclimate; paleoproductivity	ODP LEG 169S; BRITISH-COLUMBIA; NORTHEAST PACIFIC; EFFINGHAM INLET; SAANICH INLET; CLIMATE-CHANGE; TIME-SERIES; SOLAR; SEDIMENTS; RECORD	Fish stocks and dinoflagellates are essential components of the marine food chain. Sediment cores from a predominantly anoxic basin in Effingham Inlet, Vancouver Island, British Columbia, archive a late Holocene (similar to 500-5300 years BP) record of paleoproductivity in the North American Coastal Upwelling Domain (CUD). We present evidence that late Holocene changes in the dinoflagellate cyst assemblages, sedimentary record, and fish stocks in the northeastern Pacific Ocean fluctuated, at least partially, in accordance with regional and global climate cycles. Principal components analysis (PCA), and trend, wavelet and spectral analyses were used to identify relationships, cycles and trends in sediment grey-scale values, and the abundances of fish scales and dinoflagellate cysts on centennial to millennial time scales. Most observed cycles fluctuated in intensity over time, particularly following transition of the regional climate to a higher rainfall phase that impacted coastal oceanic dynamics -3400 +/- 150 years ago. Correlation of the marine paleoproductivity records observed in Effingham Inlet with solar influenced climate proxy cycles observed in the North Atlantic region indicates that solar forcing at different scales might have influenced the climate in the northeast Pacific as well. In particular an 1100- to 1400-year cycle in regional climate is well represented in the fish productivity proxy and sedimentological record. It was also observed that colder water, high-productivity, Selenopeniphix nephroides and anchovy-dominated "Anchovy Regime" ecosystems alternate with wanner water, herring-dominated "Herring Regime" ecosystems at millennial time scales. The fish scale record preserved in Effingham Inlet indicates that the NE Pacific is now in transition from an 'anchovy-' to a 'herring'-dominated regime. (c) 2005 Elsevier B.V. All rights reserved.	Carleton Univ, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada; SPEEDSTAT, Ottawa, ON K1V 8T7, Canada; Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; Queens Univ Belfast, Sch Geog, Belfast BT9 6AZ, Antrim, North Ireland	Carleton University; University of Victoria; Queens University Belfast	Carleton Univ, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada.	tpatters@ccs.earleton.ca						[Anonymous], NOVA HEDWIGIA; [Anonymous], 1873, Archiv fur mikroskopische Anatomie; [Anonymous], SOC IND APPL MATH J; BAUMGARTNER TR, 1992, CAL COOP OCEAN FISH, V33, P24; BEAMISH RJ, 1993, CAN J FISH AQUAT SCI, V50, P2270, DOI 10.1139/f93-252; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Bond G, 2001, SCIENCE, V294, P2130, DOI 10.1126/science.1065680; Brodeur R.D., 1992, Fisheries Oceanography, V1, P32, DOI 10.1111/j.1365-2419.1992.tb00023.x; Bujak J., 1980, PALAEONTOLOGICAL ASS, V24, P1; Carslaw KS, 2002, SCIENCE, V298, P1732, DOI 10.1126/science.1076964; Chang AS, 2003, PALAIOS, V18, P477, DOI 10.1669/0883-1351(2003)018<0477:SSADRF>2.0.CO;2; CHAVEZ FP, 2003, PACIFIC OCEAN SCI, V299, P217; Christoforou P, 1997, GEOPHYS RES LETT, V24, P293, DOI 10.1029/97GL00017; Cuvier G.L.C.F.D., 1847, Histoire naturelle des poissons. 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Micropaleontol.	JUN	2005	55	3-4					183	204		10.1016/j.marmicro.2005.02.006	http://dx.doi.org/10.1016/j.marmicro.2005.02.006			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	935YO					2025-03-11	WOS:000229819500003
J	Wilson, GJ; Schioler, P; Hiller, N; Jones, CM				Wilson, GJ; Schioler, P; Hiller, N; Jones, CM			Age and provenance of Cretaceous marine reptiles from the South Island and Chatham Islands, New Zealand	NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS			English	Article						dinoflagellates; marine reptiles; New Zealand; South island; Marlborough; North Canterbury; northeast Otago; Chatham Islands; Upper Cretaceous; Maastrichtian Stage; Campanian Stage; Haumurian Stage	DINOFLAGELLATE BIOSTRATIGRAPHY; PIRIPAUAN	Analyses of dinoflagellate cysts from marine reptile sites in Marlborough, North Canterbury, North Otago, and on Chatham Island, indicate that the localities range from Early to latest Haumurian (Middle Campanian to Upper Maastrichtian) in age, spanning a period of c. 15 m.y. Sites in the Waipara River area are principally Upper Haumurian and range from the Alterbidinium acutulum Zone to the Manumiella druggii Zone. Sites in the Haumuri Bluff-Ngaroma Station-Cheviot/Jed River area are Lower Haumurian to lower Upper Haumurian and range from the Satyrodinium haumuriense Zone to the Isabelidinium pellucidum Zone. The Shag Point locality is Upper Haumurian (Alterbidinium acutulum Zone), indicating a general correlation with the Waipara localities. The Chatham Island locality is Lower Haumurian (S. haumuriense Zone), indicating a similar age to the oldest Haumuri Bluff sites. Material from two unknown sites appears to be from the Waipara River area, based on the associated dinoflagellate assemblages. Two marine reptile faunas are indicated: a Mid-Campanian to Early Maastrichtian fauna that is replaced by a Late Maastrichtian fauna.	Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark; Canterbury Museum, Christchurch, New Zealand; Univ Canterbury, Dept Geol Sci, Christchurch 1, New Zealand	GNS Science - New Zealand; Geological Survey Of Denmark & Greenland; University of Canterbury	Wilson, GJ (通讯作者)，Inst Geol & Nucl Sci, POB 30368, Lower Hutt, New Zealand.	graeme.wilson@gns.cri.nz	Jones, Craig/C-9693-2011					Andrews PB, 1987, NZ GEOLOGICAL SURVEY, V24; [Anonymous], 1993, I GEOLOGICAL NUCL SC; Browne G.H., 1985, New Zealand Geological Survey record, V6; CLARKE WB, 1861, RECENT GEOLOGICAL DI; Crampton J, 2000, NEW ZEAL J GEOL GEOP, V43, P309, DOI 10.1080/00288306.2000.9514890; Cruickshank ARI, 2002, PALAEONTOLOGY, V45, P557, DOI 10.1111/1475-4983.00249; CRUICKSHANK ARI, 1996, GEOLOGICAL SOC NZ A, V91, P62; HAAST J, 1918, J P PROVINCIAL COUNC, V24, P175; HAAST J, 1871, GEOLOGICAL SURVEY NZ, P25; HAAST J, 1871, GEOLOGICAL SOC NZ RE, P5; Hector J., 1874, T P NZ I, V6, P333; HECTOR J, 1887, COLONIAL MUSEUM GEOL, P9; Hood T.H.C., 1870, Q J GEOL SOC LOND, V26, P409; JONES CM, 1993, GEOLOGICAL SOC NZ MI, V79; Mason B. H., 1941, Transactions and Proceedings of the Royal Society of New Zealand, V71, P103; MCKAY A, 1877, GEOLOGICAL SURVEY NZ, P172; MCKAY A, 1877, GEOLOGICAL SURVEY NZ, P36; Owen R., 1861, Geologist, V4, P444; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Roncaglia L., 1997, IGNS SCI REPORT, V97, P1; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; Thomson J.A., 1920, T NZ I, V52, P322; Warren G., 1978, NZ GEOLOGICAL SURVEY, V92; WEBB PN, 1971, NEW ZEAL J GEOL GEOP, V14, P795, DOI 10.1080/00288306.1971.10426335; WEBB PN, 1966, NZ LATE CRETACEOUS F; Welles S.P., 1971, REC CANTERBURY MUS, V9, P1; WELLMAN H. W., 1959, TRANS ROY SOC NEW ZEALAND, V87, P99; Wilson D.D., 1963, New Zealand Geological Survey bulletin, V64; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; WILSON GJ, 1984, NEW ZEAL J BOT, V22, P549, DOI 10.1080/0028825X.1984.10425289; WILSON GJ, 1982, 52 PAL NZ GEOL SURV, P17; WILSON GJ, 1982, 63 PAL NZ GEOL SURV; YOUNG M, 1999, GEOLOGICAL SOC NZ A, V107, P178	33	25	27	0	5	RSNZ PUBLISHING	WELLINGTON	PO BOX  598, WELLINGTON, 00000, NEW ZEALAND	0028-8306			NEW ZEAL J GEOL GEOP	N. Z. J. Geol. Geophys.	JUN	2005	48	2					377	387		10.1080/00288306.2005.9515120	http://dx.doi.org/10.1080/00288306.2005.9515120			11	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	950DS					2025-03-11	WOS:000230838400011
J	Susek, E; Zonneveld, KAF; Fischer, G; Versteegh, GJM; Willems, H				Susek, E; Zonneveld, KAF; Fischer, G; Versteegh, GJM; Willems, H			Organic-walled dinoflagellate cyst production in relation to upwelling intensity and lithogenic influx in the Cape Blanc region (off north-west Africa)	PHYCOLOGICAL RESEARCH			English	Article						dust; north-west Africa; organic-walled dinoflagellate cysts; sediment trap; upwelling	NORTHWESTERN INDIAN-OCEAN; SHORT-TERM VARIABILITY; GONYAULAX-TAMARENSIS; PHYTOPLANKTON BLOOM; IRON CONCENTRATIONS; ANCHOR STATION; SEDIMENT TRAPS; SAHARAN DUST; SOMALI BASIN; SEA-SURFACE	Fossil dinoflagellate cyst assemblages are increasingly used in paleoclimatic research to establish paleoenvironmental reconstructions. To obtain reliable reconstructions, it is essential to know which physical factors influence the cyst production. Most information about the relationship between variations in physical parameters and cyst production is known from middle and higher latitudes. Information from the (sub)tropics is rare. To increase this information, the temporal variation in cyst assemblages from the upwelling area off north-west Africa (off Mauritania) has been compared to environmental conditions of the upper water column. Samples were collected by the sediment trap CB9, off north-west Africa (Cape Blanc, 21 degrees 15'2"N, 20 degrees 42'2"W) between 11 June 1998 and 7 November 1999 at 27.5-day intervals. Off Cape Blanc, upwelling occurs throughout the year with variable intensity. This region is also characterized by frequently occurring Saharan dust storms. Seasonal variations in dust input, upwelling intensity and sea surface temperature are reflected by the production of organic-walled dinoflagellate cyst assemblages. Several cyst taxa are produced throughout the sampling interval, with the highest fluxes at times of strongest upwelling relaxation and/or dust input (Echinidinium aculeatum Zonneveld, Echinidinium delicatum Zonneveld, Echinidinium granulatum Zonneveld, Echinidinium spp., Impagidinium aculeatum (Wall) Lentin et Williams, Impagidinium sphaericum (Wall) Lentin et Williams, Protoperidinium americanum (Gran et Braarud) Balech, Protoperidinium stellatum (Wall in Wall et Dale) Rochon et al., Protoperidinium spp., Selenopemphix nephroides (Benedek) Benedek et Sarjeant and Selenopemphix quanta (Bradford) Matsuoka). Species such as, for example, Bitectatodinium spongium (Zonneveld) Zonneveld et Jurkschat and Impagidinium patulum (Wall) Stover et Evitt do not show any production pattern related to a particular season of the year or to specific environmental conditions in the upper water column. The production of cysts of Protoperidinium monospinum (Paulsen) Zonneveld et Dale is restricted to intervals with increased nutrient concentrations in upper waters when sea surface temperatures at the sampling site is below approximately 24 degrees C.	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Res.	JUN	2005	53	2					97	112		10.1111/j.1440-183.2005.00377.x	http://dx.doi.org/10.1111/j.1440-183.2005.00377.x			16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	954UP					2025-03-11	WOS:000231180800003
J	Brenner, WW				Brenner, WW			Holocene environmental history of the Gotland Basin (Baltic Sea) - a micropalaeontological model	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						organic microfossils; Baltic sea; Gotland basin; salinity; palaeoecology; dinoflagellate morphology proxy	ICE LAKE; SEDIMENT CORES; STRATIGRAPHY; SALINITY; PROPER	Organic microfossils of a well-dated sediment core from Gotland Basin were analysed and used for the ecological interpretation of the Holocene history of this area. To avoid confusion with corrected and uncorrected C-14 ages, only calendar years BP are used. In the lowermost part organic microfossils are rare, but few marine dinoflagellate cysts between 11300 and 11000 years BP indicate the marine Yoldia Phase. At 9800 years BP a significant environmental change is indicated by the rapid increase of freshwater dinoflagellates and pine pollen. At the end of the freshwater stage an enormous abundance increase of cladoceran remains indicates an eutrophication event between 7600 and 7400 years BP. First permanent brackish water conditions of the surface water were established at 7400 years BP and the increasing salinity reached its maximum between 6700 and 6400 years BP. Further changes in the brackish surface water ecosystem of the Gotland Basin can be found at 5500, 4400, 3000, 1000, and 800 years BP, which are thought to be mainly climatically induced. (c) 2004 Elsevier B.V. All rights reserved.	GEOMAR, D-24148 Kiel, Germany	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	GEOMAR, Wischhofstr 1-3, D-24148 Kiel, Germany.	wolframbrenner@hotmail.com						ABELMANN A, 1985, GEOL PALAONTOL I U K, V9, P1; Andrén E, 2000, BOREAS, V29, P233; Andrén E, 2000, HOLOCENE, V10, P687, DOI 10.1191/09596830094944; ANDREN E, 1999, MEDDELANDEN STOCKHOL, V30, P114; [Anonymous], 2001, BALTICA; [Anonymous], 2001, Baltica; [Anonymous], MEERESKUNDE OSTSEE; BJORCK S, 1995, QUATERN INT, V27, P19, DOI 10.1016/1040-6182(94)00057-C; BRENNER W, 1994, REV PALAEOBOT PALYNO, V80, P209, DOI 10.1016/0034-6667(94)90002-7; Brenner W.W., 2001, BALTICA, V14, P40; Brenner Wolfram, 2002, Meyniana, V54, P17; CHRISTENSEN C, 1996, OXBOW MONOGRAPHS, V53, P15; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DIGERFELDT G, 1975, Boreas (Oslo), V4, P125; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; EMELYANOV EM, 1995, ONCEANOLOGY, V35, P99; ERONEN M, 1990, Geologiska Foreningens i Stockholm Forhandlingar, V112, P1; Gustafsson JA, 2002, MED SCI SYMP SER, V17, P1; Heinsalu A., 2000, BALTICA, V13, P51; HOFMANN W, 1987, INT REV GES HYDROBIO, V72, P97, DOI 10.1002/iroh.19870720112; HOFMANN W, 2001, BALTICA, V14, P52; HYVARINEN H, 1988, PROBLEMS BALTIC SEA, P25; Hyvarinen H, 1988, PROBLEMS BALTIC SEA, V148, P7; JANKE W, 1996, WARNSIGNALE OSTSEE, P30; JENSEN JB, 1995, QUATERN INT, V27, P59, DOI 10.1016/1040-6182(94)00061-9; Jensen JB, 1997, BOREAS, V26, P217, DOI 10.1111/j.1502-3885.1997.tb00853.x; Jensen JB, 1999, BOREAS, V28, P437, DOI 10.1080/030094899421966; KABAILIENE M, 1995, QUATERN INT, V27, P69, DOI 10.1016/1040-6182(94)00062-A; KESSEL H, 1979, QUATERNARY HIST BALT, V1, P127; KLIEWE H, 1978, PETERMANN GEOGR MITT, V122, P81; KOLP O, 1979, PETERMANN GEOGR MITT, V123, P177; KOLP O, 1976, PETERMANN GEOGR MITT, V120, P1; Kotilainen AT, 2000, MAR GEOL, V166, P51, DOI 10.1016/S0025-3227(00)00012-8; LEMKE W, 1997, 5 MARINE GEOLOGICAL; Lemke Wolfram, 1998, Meyniana, V50, P155; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATTHAUS W, 1990, BEITR MEERESKD, V61, P21; Matthaus W., 1994, Dtsch. Hydrogr, Zeitschrift, V46, P321, DOI [10.1007/BF02226309, DOI 10.1007/BF02226309]; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; McCartney Kevin, 1993, P143; MIDDELBURG JJ, 1991, GEOLOGY, V19, P679, DOI 10.1130/0091-7613(1991)019<0679:ORTFIS>2.3.CO;2; MUNTHE H, 1931, FORHANDLINGAR, V53, P159; Pankow H., 1990, OSTSEE ALGENFLORA, P648; PETERSEN KS, 1992, NATURE, V359, P679, DOI 10.1038/359679a0; PUNNING JM, 1988, BOREAS, V17, P27; Sohlenius G, 1998, BOREAS, V27, P101; Sohlenius G, 1996, MAR GEOL, V134, P183, DOI 10.1016/0025-3227(96)00047-3; STUIVER M, 1995, QUATERNARY RES, P44; Sundelin, 1922, GEOLOGISKA FORENINGE, V44, P543; Tappan H.N., 1980, PALEOBIOLOGY PLANT P, P1028; Voss M., 2001, BALTICA, V14, P131; Wall D., 1973, Geoscience Man, V7, P95; Westman P, 1999, J PALEOLIMNOL, V22, P53, DOI 10.1023/A:1008011511101; Winn K., 1986, Meyniana, V38, P61; Witkowski A., 1994, RECENT AND FOSSIL DI, V28, P312; Yu SY, 2003, BOREAS, V32, P578, DOI 10.1080/03009480310004161	59	52	53	1	8	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAY 13	2005	220	3-4					227	241		10.1016/j.palaeo.2004.12.010	http://dx.doi.org/10.1016/j.palaeo.2004.12.010			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	926ZR					2025-03-11	WOS:000229162700001
J	Gottschling, M; Knop, R; Plötner, J; Kirsch, M; Willems, H; Keupp, H				Gottschling, M; Knop, R; Plötner, J; Kirsch, M; Willems, H; Keupp, H			A molecular phylogeny of <i>Scrippsiella sensu lato</i> (Calciodinellaceae, Dinophyta) with interpretations on morphology and distribution	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Calcareous dinoflagellates; Calciodinellaceae; cryptic species; cyst; distribution; Internal Transcribed Spacer; molecular systematics; phylogeny; morphology; secondary structure; theca	DINOFLAGELLATE CYSTS; SECONDARY STRUCTURE; MARINE DINOFLAGELLATE; GENETIC DIVERSITY; NOV; PERIDINIALES; SEDIMENTS; TROCHOIDEA; SHIPS; RDNA	The phylogenetic relationships of Scrippsiella sensu lato ( including cyst taxa such as Calcigonellum, Calciodinellum, and Pernambugia) were investigated based on sequences from the ribosomal 5.8S rRNA and the Internal Transcribed Spacers ITS1 and ITS2, including interpretations on morphology and distribution. To attach importance to the cyst diversity present in calcareous dinoflagellates, a segregation of Scrippsiella sensu lato into four well-recognizable and monophyletic groups is proposed, corresponding to more- or less-established taxonomic units: (i) Calciodinellum ( including Calcigonellum and a few species assigned to Scrippsiella), (ii) Pernambugia ( presumptively including Lebessphaera), (iii) S. precaria and S. ramonii, and (iv) Scrippsiella sensu stricto comprising largely the S. trochoidea species complex. The phylogenetic relationships among these four groups are not sufficiently resolved. Molecular data suggest the existence of numerous cryptic taxa showing molecular, but not morphological, variation ( especially in Scrippsiella sensu stricto). Closely related strains have a wide range of distribution and occur ( at least partly) sympatrically in cold through to tropical seas of the world.	Free Univ Berlin, Fachbereich Geol Wissensch Fachrichtung Palaontol, D-12249 Berlin, Germany; Humboldt Univ, Museum Naturkunde, Inst Systemat Zool, D-10099 Berlin, Germany; Univ Bremen, Fachbereich Geowissensch Fachrichtung Hist Geol P, D-28359 Bremen, Germany	Free University of Berlin; Humboldt University of Berlin; Leibniz Institut fur Evolutions und Biodiversitatsforschung; University of Bremen	Free Univ Berlin, Fachbereich Geol Wissensch Fachrichtung Palaontol, Malteserstr 74-100, D-12249 Berlin, Germany.	caix@zedat.fu-berlin.de	Gottschling, Marc/K-2186-2014					[Anonymous], 2003, BOT JAHRB; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Coleman AW, 2003, TRENDS GENET, V19, P370, DOI 10.1016/S0168-9525(03)00118-5; Coleman AW, 1997, J MOL EVOL, V45, P168, DOI 10.1007/PL00006217; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DEFLANDRE G, 1947, CR HEBD ACAD SCI, V224, P1781; Edvardsen B, 2003, J PHYCOL, V39, P395, DOI 10.1046/j.1529-8817.2003.01252.x; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Fensome R.A., 1993, CLASSIFICATION FOSSI; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Goertzen LR, 2003, MOL PHYLOGENET EVOL, V29, P216, DOI 10.1016/S1055-7903(03)00094-0; Gottschling M, 2004, NUCLEIC ACIDS RES, V32, P307, DOI 10.1093/nar/gkh168; Gottschling M, 2001, PLANT BIOLOGY, V3, P629, DOI 10.1055/s-2001-19371; GOTTSCHLING M, 2005, IN PRESS MOL PHYLOGE; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; John U, 2003, MOL BIOL EVOL, V20, P1015, DOI 10.1093/molbev/msg105; KAMPTNER ERWIN, 1958, ARCH PROTISTENKUNDE, V103, P54; Karwath B, 2000, BERICHTE FACHBEREICH, V152, P1; Keupp H., 1987, Facies, V16, P37, DOI 10.1007/BF02536748; Keupp H., 1981, Facies, V5, P1, DOI 10.1007/BF02536655; Keupp H., 1989, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V106, P207; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P161; Keupp H., 1991, P267; Kohring Rolf, 2005, Palaeontologische Zeitschrift, V79, P79; Kohring Rolf, 1997, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V3, P151; KREMP A, 2005, IN PRESS J PHYCOL, V41; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Litaker RW, 2003, J PHYCOL, V39, P754, DOI 10.1046/j.1529-8817.2003.02112.x; McGovern TM, 2003, MOL ECOL, V12, P1207, DOI 10.1046/j.1365-294X.2003.01758.x; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 2003, PHYCOLOGIA, V42, P56, DOI 10.2216/i0031-8884-42-1-56.1; MONTRESOR M, 1988, PHYCOLOGIA, V27, P387, DOI 10.2216/i0031-8884-27-3-387.1; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Pin LC, 2001, MAR BIOTECHNOL, V3, P246, DOI 10.1007/s101260000073; Plötner J, 1998, J ZOOL SYST EVOL RES, V36, P191; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Rambaut A., 2001, SE AL SEQUENCE ALIGN; Ruiz GM, 2000, NATURE, V408, P49, DOI 10.1038/35040695; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Swofford D., 2002, PAUP PHYLOGENETIC AN; van der Strate HJ, 2002, J PHYCOL, V38, P572, DOI 10.1046/j.1529-8817.2002.t01-1-01170.x; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7; Wessel P., 1995, GENERIC MAPPING TOOL	47	47	52	1	7	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0967-0262	1469-4433		EUR J PHYCOL	Eur. J. Phycol.	MAY	2005	40	2					207	220		10.1080/09670260500109046	http://dx.doi.org/10.1080/09670260500109046			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	944LF					2025-03-11	WOS:000230429100007
J	Akkiraz, MS; Akgün, F				Akkiraz, MS; Akgün, F			Palynology and age of the Early Oligocene units in Cardak-Tokca Basin, Southwest Anatolia:: Paleoecological implications	GEOBIOS			English	Article						palynology; Early Oligocene; paleoecology; Southwest Anatolia	POLLEN	In this study, the lignite bearing sediments of Cardak-Tokca basin exposed in southwest Anatolia, were palynologically examined. A well preserved and diverse palynomorph assemblage indicating an Early Oligocene age was recovered from the Hayrettin and Tokca formations. The palynomorph assemblage is dominated by Pinus, Sparganiaceae, Juglandaceae and diverse tricolpate and tricolporate pollen. In addition a few species of marine dinoflagellate cysts were encountered as well. The Early Oligocene age is based primarily on the presence of stratigraphic markers such as: Boehlensipollis hohli, Slowakipollis hippophaeoides. Aglaoreidia cyclops, Dicolpopollis kockeli, Compositoipollenites rhizophorus ssp. burghasungensis, Mediocolpopollis compactus ssp. ellenhausensis, Pentapollenites pentangulus. Subtriporopollenites simplex and Intratriporopollenites instructus. Palynological data indicate a humid subtropical climatic conditions during the deposition of the Cardak-Tokca sediments. Ecological analysis of the palynomorph assemblage identifies several paleo-associations of montana, lowland and slope, swamp and water-edge and freshwater aquatic elements. In this study, Cardak-Tokca, Cankiri-Corum, Thrace and southwest Anatolian molasse basins (Kale-Tavas and Denizli) were correlated in accordance with their palynostratigraphic content and the results show that the deposition took place during the Early Oligocene in the Cardak-Tokca basin. This basin is older than Thrace basin and southwest Anatolian molasse basins (Kale-Tavas and Denizli molasse) which were deposited during the Late Oligocene-Early Miocene. (c) 2005 Elsevier SAS. All rights reserved.	Dokuz Eylul Univ, Muhendislik Fak Jeol Muhendisligi Bolumu, TR-35100 Izmir, Turkey	Dokuz Eylul University	Akkiraz, MS (通讯作者)，Dokuz Eylul Univ, Muhendislik Fak Jeol Muhendisligi Bolumu, TR-35100 Izmir, Turkey.	serkan.akkiraz@deu.edu.tr	Akgün, Funda/AAC-2859-2020; akkiraz, mehmet/ADP-2366-2022	Akgun, Funda/0000-0002-6028-6704				Akgün F, 2001, GEODIN ACTA, V14, P71, DOI 10.1016/S0985-3111(00)01054-8; AKGUN F, 2002, PALAEONTOL SINICA, V41, P576; AKYOL E, 1971, Pollen et Spores, V13, P117; AKYOL E, 1995, S GEOL THRAC BAS LUL, P28; ANDERSON JAR, 1975, REV PALAEOBOT PALYNO, V19, P291, DOI 10.1016/0034-6667(75)90049-4; [Anonymous], 1971, GEOL JB S; [Anonymous], 1970, Beihhefte zum Geologischen Jahrbuch; [Anonymous], 1988, Geologisches Jahrbuch Reihe A; BANDE MB, 1986, REV PALAEOBOT PALYNO, V49, P203, DOI 10.1016/0034-6667(86)90028-X; BATI Z, 1996, UNPUB PALYNOSTRATIGR, P1; BOULTER M C, 1982, Palynology, V6, P55; BOULTER MC, 1979, REV PALAEOBOT PALYNO, V28, P259, DOI 10.1016/0034-6667(79)90028-9; BUCHARDT B, 1978, NATURE, V275, P121, DOI 10.1038/275121a0; Cavagnetto C, 1996, REV PALAEOBOT PALYNO, V92, P281, DOI 10.1016/0034-6667(95)00096-8; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Chateauneuf J.J., 1972, B BRGM, V4, P59; Collinson M.E., 1992, Eocene-Oligocene Climatic and Biotic Evolution, P437; EDIGER VS, 1990, REV PALAEOBOT PALYNO, V62, P97, DOI 10.1016/0034-6667(90)90019-F; ELSIK W C, 1990, Palynology, V14, P91; Elsik W.C., 1974, Palaeontographica Abt B, V149, P90; Erdtman G., 1960, Botaniska Notiser, V113, P46; Fairchild W.W., 1969, PALAEONTOGRAPHICA B, V128, P81; FARLEY MB, 1990, PALAEOGEOGR PALAEOCL, V79, P11, DOI 10.1016/0031-0182(90)90103-E; FOWLER K, 1971, Pollen et Spores, V13, P135; FREDERIKSEN N O, 1980, Palynology, V4, P125; FREDERIKSEN N O, 1991, Palaios, V6, P564, DOI 10.2307/3514919; Frederiksen N.O., 1981, Communities of the Past, P493; FREDERIKSEN NO, 1985, AM ASS STRATIGRAPHIC, V15, P1; Gokcen N, 1982, YERBILIMLERI, V9, P111; GOKTAS F, 1989, CIVRIL CARDAK ARASTN; Gorin G., 1975, Bulletin Bureau de Recherches Geologiques et Minieres, V3, P147; Gruas-Cavagnetto C., 1968, Memoire de la Societe Geologique de France, V110, P1; GRUASCAVAGNETTO C, 1988, GEOLOGISCHES JB, V100, P288; Gurer OF, 1996, Turkish J Earth Sci, V5, P71, DOI DOI 10.55730/1300-0985.1729; Hakyemez H Y., 1989, Bulletin Mineral Research Exploration Institute, V109, P9; HAKYEMEZ HY, 1982, 7311 MIN RES EXPL I; Hochuli P.A., 1978, Beitrrage Palaontologie Osterreich, V4, P1; KEDVES M, 1970, Pollen et Spores, V12, P83; KEDVES M, 1969, POLLEN SPORES, V11, P385; Krutzsch W., 1967, GEOLOGISCHES JB, V3, P309; Krutzsch W., 1958, Z ANGEW GEOL, V3, P519; KRUTZSCH W, 1962, GEOLOGIE, V11, P265; Krutzsch W., 1970, Atlas der mittelund jungtertiaren dispersen Sporenund Pollensowie der Mikroplanktonformen des nordlichen Mitteleuropas VII; Krutzsch W., 1959, PALAEONTOGR ABT B, V105, P125; Krutzsch W., 1977, PALAEONTOGR ABT B, V163, P1; LAGENHEIM J.H., 1967, BOT MUSEUM LEAFLETS, V21, P289; LUTTIG G, 1976, PALEOGEOGRAPHIC ATLA; MAI DH, 1961, GEOLOGIE, V32, P413; Murriger F., 1951, NOTIZBLATT HESSICHES, V2, P87; NAKOMAN E, 1968, Pollen et Spores, V10, P521; Nakoman E., 1966, Annales de la Societe Geologique du Nord, V86, P65; NEBERT K, 1956, DENIZLI AETGOL MERKE; Nickel Birgit, 1996, Palaeontographica Abteilung B Palaeophytologie, V240, P1; OLLIVIERPIERRE MF, 1993, PALAEOGEOGR PALAEOCL, V103, P223, DOI 10.1016/0031-0182(93)90144-8; OLLIVIERPIERRE MF, 1980, MEM SOC GEOL MINERAL, V25, P1; Pflanzl G., 1956, NOTIZBLATT HESSISCHE, V84, P232; Potonie R., 1931, SITZUNGSBERICHTE GES, V1, P24; POTONIE R, 1960, GEOLOGISCHES JB S, V87, P1; Potonie R., 1934, ARBEITEN I PALAOBOTA, V5, P5; ROCHE E, 1988, GEOLOGISCHES JB, V100, P288; SAHBAZ A, 1992, 9 PETR C TURK, V2, P62; Salujha SK, 1974, PALAEOGENES KHASI JA, V21, P267; Samant Bandana, 1997, Palaeontographica Abteilung B Palaeophytologie, V245, P1; SCHALKE HJW, 1988, GEOLOGISCHES JB, V100, P288; SCHULER MC, 1988, GEOLOGISCHES JB, V100, P288; SENEL M, 1997, MADEN TETKIK ARAMA G, V16, P1; SHPUL VG, 2002, 6 EUR PAL PAL C, P160; TCHIHATCHEF L, 1869, GEOLOGIE; THOMSON P. W., 1953, PALAEONTOGRAPHICA, V94 B., P1; TSCHUDY RH, 1973, GEOLOGICAL SURVEY PR, V743, P400; VONDERBRELIE G, 1988, GEOLOGISCHES JB, V100, P288; Wilkinson G.C., 1980, PALAEONTOGR ABT B, V175, P27; WILKINSON GC, 1980, J GEOL SOC LONDON, V137, P65, DOI 10.1144/gsjgs.137.1.0065; WOLFE JA, 1967, 11 TOKY S PAC SCI C, V25, P67	74	28	30	0	7	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS	23 RUE LINOIS, 75724 PARIS, FRANCE	0016-6995			GEOBIOS-LYON	Geobios	MAY-JUN	2005	38	3					283	299		10.1016/j.geobios.2003.11.010	http://dx.doi.org/10.1016/j.geobios.2003.11.010			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	939VG					2025-03-11	WOS:000230100000001
J	Atanassova, J				Atanassova, J			Palaeoecological setting of the western Black Sea area during the last 15 000 years	HOLOCENE			English	Article						pollen analysis; dinoflagellate cysts; vegetation history; catastrophic flood; Black Sea; Lateglacial; Holocene	BULGARIA	Analysis of pollen, dinoflagellate cysts and lithology was carried out on ten cores from the western deep Black Sea and combined with radiocarbon dating to reconstruct the vegetation, climate and palaeoecological conditions. All the cores record a consistent sequence of Lateglacial and early Holocene steppe vegetation. which persisted until about 7100-7500 yr BP when Quercus, Corylus, Tilia and other temperate trees expanded, at about the same time as the influx of Mediterranean waters that resulted in sapropel deposition in the deep Black Sea. The sequence implies dry climatic conditions and a low level of the Black Sea during the early Holocene.	Sofia Univ St Kliment Ohridski, Fac Biol, Dept Bot, Sofia 1164, Bulgaria	University of Sofia	Atanassova, J (通讯作者)，Sofia Univ St Kliment Ohridski, Fac Biol, Dept Bot, 8 Dragan Tzankov Bd, Sofia 1164, Bulgaria.	atanassova_juliana@abv.bg		Atanassova, Juliana/0000-0002-1604-3836				Aksu A.E., 2002, GSA Today, V12, P4, DOI DOI 10.1130/1052-5173(2002)012<0004:PH0FTB>2.0.C0;2; [Anonymous], OKEANOLOGIYA; [Anonymous], NOAHS FLOOD NEW SCI; [Anonymous], 1974, AM ASS PETROLEUM GEO; ATANASSOVA ID, 1995, ENVIRON POLLUT, V87, P17, DOI 10.1016/S0269-7491(99)80003-7; Atanassova J., 1990, THESIS SOFIA U; Atanassova J, 1999, Acta Palaeobotanica, V2, P545; ATANASSOVA J, 1998, PROGR BOT RES P 1 BA, P25; Atanassova Juliana, 1995, P68; ATANOSSOVA J, 2002, P 6 NAT C BOT JUN 18, P141; Bozilova E, 1998, VEG HIST ARCHAEOBOT, V7, P141, DOI 10.1007/BF01374002; Bozilova E., 1994, VEG HIST ARCHAEOBOT, V3, P143, DOI [10.1007/BF00202022, DOI 10.1007/BF00202022]; Bozilova E., 1992, Vegetation History and Archaebotany, V1, P19; Bozilova E.D.B., 1986, STUDIA PRAEHISTORICA, V8, P160; Chepalyga A.L., 1984, Late Quaternary environments of the Soviet Union, P229; DEGENS E, 1973, C INT CNRS METH QUAN, P1; DEGENS ET, 1980, NEUES JB GEOLOGISCH, V5, P65; Faegri Knut., 1950, TXB MODERN POLLEN AN, DOI [10.1002/j.1477-8696.1954.tb01739.x, DOI 10.1002/J.1477-8696.1954.TB01739.X]; Filipova-Marinova M., 2003, Aspects of Palynology and Palaeoecology, P213; FILIPOVAMARINOV.M, 1990, GEOLOGICAL EVOLUTION, P34; Grimm EC., 1991, TILIA and TILIA GRAPH; Hay BJ, 1988, PALEOCEANOGRAPHY, V3, P491, DOI 10.1029/PA003i004p00491; HAY BJ, 1991, DEEP-SEA RES, V38, pS1211; JOHNSON RG, 2002, SECRETS ICE AGE ROLE; JONES GA, 1994, DEEP-SEA RES PT I, V41, P531, DOI 10.1016/0967-0637(94)90094-9; KHRISHEV K, 1988, GEOLOGICAL BALCANICA, V18, P5; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; MARINOVA E, 2005, VERGLEICHENDE PALAOE; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; ROZDESTVENSKY A, 1986, HYDROCHEMISTRY BULGA; Ryan WBF, 2003, ANNU REV EARTH PL SC, V31, P525, DOI 10.1146/annurev.earth.31.100901.141249; Ryan WBF, 1997, MAR GEOL, V138, P119, DOI 10.1016/S0025-3227(97)00007-8; SHOPOV V, 1989, BULGARIAN GEOLOGICAL, V50, P46; SHOPOV V L, 1992, Geologica Balcanica, V22, P59; STOCKMARR J, 1971, Pollen et Spores, V13, P615; TONKOV S, 1995, U SOFIA FACULTY BIOL, V87, P5; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WRIGHT H, 2003, ASPECTS PALYNOLOGY P, P68	38	51	52	1	15	ARNOLD, HODDER HEADLINE PLC	LONDON	338 EUSTON ROAD, LONDON NW1 3BH, ENGLAND	0959-6836			HOLOCENE	Holocene	MAY	2005	15	4					576	584		10.1191/0959683605hl832rp	http://dx.doi.org/10.1191/0959683605hl832rp			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	933EW					2025-03-11	WOS:000229612700009
J	Schioler, P				Schioler, P			Dinoflagellate cysts and acritarchs from the Oligocene-Lower Miocene interval of the Alma-1X well, Danish North Sea	JOURNAL OF MICROPALAEONTOLOGY			English	Article						Oligocene; Miocene; biostratigraphy; dinoflagellate cysts; North Sea	BIOSTRATIGRAPHY; STRATIGRAPHY; SYSTEMATICS; MARYLAND; VIRGINIA; ZONATION; EOCENE	This palynological study of cuttings samples from the Lark Formation in the Danish North Sea well Alma-1X documents for the first time in the public domain the succession of last occurrences of dinoflagellate cysts and acritarchs in the Oligocene-Lower Miocene interval of the Central North Sea. The distribution of dinoflagellates and acritarchs in the well demonstrates the potential for the development of a detailed subdivision of the Oligocene-Lower Miocene in the Central North Sea, based on the first downhole occurrences of key taxa. Five regional intra-Lark Formation seismic and petrophysical log markers can be dated with precision using dinoflagellate biostratigraphy. Four new species and one new subspecies of dinoflagellates are described from the study interval: Ampho-rosphaeridium? almae sp. nov., Filisphaera pachyderma sp. nov., Pentadinium corium sp. nov., Spiniferites pseudofurcatus verrucosus ssp. nov. and Thalassiphora rota sp. nov. Pseudospiniferites manumii Lund, 2002 is emended and transferred to the genus Spiniferites. J Micropalaeontol.	Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	pos@geus.dk						[Anonymous], 1988, Geol. 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Ser., V17, P129; Pross J., 1997, TUBINGER MIKROPALAON, V15, P1; SARJEANT W A S, 1970, Grana, V10, P74; Steininger FF, 1997, EPISODES, V20, P23; Strauss Christoph, 2001, Geologisches Jahrbuch Reihe A, V152, P395; Strauss Christoph, 1992, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V73, P159; Torricelli Stefano, 2001, Palynology, V25, P29, DOI 10.2113/0250029; Vandenberghe Noel, 2003, P419; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Williams Graham L., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P99; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zevenboom D., 1995, THESIS U UTRECHT NET; Zevenboom Daan, 1996, Giornale di Geologia (Bologna), V58, P81	61	45	47	0	1	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	MAY	2005	24		1				1	37		10.1144/jm.24.1.1	http://dx.doi.org/10.1144/jm.24.1.1			37	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	936FC		hybrid			2025-03-11	WOS:000229839900001
J	Morzadec-Kerfourn, MT				Morzadec-Kerfourn, MT			Interaction between sea-level changes and the development of littoral herbaceous vegetation and autotrophic dinoflagellates	QUATERNARY INTERNATIONAL			English	Article							CYSTS	In addition to sedimentological studies, palynological analyses provide specific criteria for the recognition of sea-level changes according to geographical situation. During periods of rapid rise in sea level, marine elastic sedimentation progrades towards the land and marine waters penetrate into estuaries bringing in assemblages of dinoflagellate cysts dominated by Spiniferites bentorii. In addition, in coastal lowlands, this progradation causes the formation of coastal barriers in front of the troughs closest to the shoreline. The impounding of fresh water leads to an increase in the development of aquatic plants. During phases of slower rise in sea level, on the other hand, the marshes extend out towards the sea over the clastic marine sediments. Chenopodiaceae are established at the base of the vegetation sequence, followed by Poaceae and then Cyperaceae. In coastal peat land, the development of Ericaceae and Sphagnum characterizes the maximum deceleration of sea-level rise. In estuaries, dinoflagellates are adapted to less renewed water, which are richer in nutrients supplied by continental runoff. Under these conditions, the assemblages tend to be almost monospecific containing Lingulodinium machaerophorum. (c) 2004 Elsevier Ltd and INQUA. All rights reserved.	Univ Rennes 1, Geol Lab, F-35042 Rennes, France	Universite de Rennes	Univ Rennes 1, Geol Lab, F-35042 Rennes, France.	marie-therese.morzadec@wanadoo.fr						Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Debenay JP, 2003, ESTUAR COAST SHELF S, V58, P843, DOI 10.1016/S0272-7714(03)00189-6; Delibrias G, 1971, QUATERNARIA, V14, P175; Fairbridge RhodesW., 1961, Physics and Chemistry of the Earth, V4, P99, DOI DOI 10.1016/0079-1946(61)90004-0; Godwin H., 1956, HIST BRIT FLORA FACT; Morzadec-Kerfourn M.-T., 1976, Revue Micropaleont, V18, P229; Morzadec-Kerfourn M.-T., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P121; MORZADECKERFOUR.M, 1995, J COASTAL RES, P197; MORZADECKERFOUR.MT, 1974, MEMOIRE SOC GEOLOGIQ, V17; REID PC, 1975, NEW PHYTOL, V75, P589, DOI 10.1111/j.1469-8137.1975.tb01425.x; Streif H., 1989, Coastal lowlands: geology and geotechnology, P213, DOI [10.1007/978-94-017-1064-0, DOI 10.1007/978-94-017-1064-0]; VISSET L, 1988, NEW PHYTOL, V110, P409, DOI 10.1111/j.1469-8137.1988.tb00279.x	13	17	19	0	1	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1040-6182	1873-4553		QUATERN INT	Quat. Int.	MAY	2005	133						137	140		10.1016/j.quaint.2004.10.006	http://dx.doi.org/10.1016/j.quaint.2004.10.006			4	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	905OA					2025-03-11	WOS:000227576900011
J	Udeze, CU; Oboh-Ikuenobe, FE				Udeze, CU; Oboh-Ikuenobe, FE			Neogene palaeoceanographic and palaeoclimatic events inferred from palynological data: Cape Basin off South Africa, ODP Leg 175	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						palynology; palynofacies; Neogene; palaeoceanography; palaeoclimate; Ocean Drilling Program Leg 175	WALLED DINOFLAGELLATE CYSTS; NORTH-ATLANTIC OCEAN; SURFACE SEDIMENTS; UPWELLING SYSTEM; EASTERN ENGLAND; ADJACENT SEAS; MIOCENE; PLIOCENE; PRESERVATION; PHYTOPLANKTON	Sites 1085, 1086 and 1087 were drilled off South Africa during Ocean Drilling Program (ODP) Leg 175 to investigate the Benguela Current System. While previous studies have focused on reconstructing the Neogene palaeoceanographic and palaeoclimatic history of these sites, palynology has been largely ignored, except for the Late Pliocene and Quaternary. This study presents palynological data from the upper Middle Miocene to lower Upper Pliocene sediments in Holes 1085A, 1086A and 1087C that provide complementary information about the history of the area. Abundant and diverse marine palynomorphs (mainly dinoflagellate cysts), rare spores and pollen, and dispersed organic matter have been recovered. Multivariate statistical analysis of dispersed organic matter identified three palynofacies assemblages (A, B, C) in the most continuous hole (1085A), and they were defined primarily by amorphous organic matter (AOM), and to a lesser extent black debris, structured phytoclasts, degraded phytoclasts, and marine palynomorphs. Ecostratigraphic interpretation based on dinoflagellate cyst, spore-pollen and palynofacies data allowed us to identify several palaeoceanographic and palaeoclimatic signals. First, the late Middle Miocene was subtropical, and sediments contained the highest percentages of land-derived organic matter, even though they are rich in AOM (palynofacies assemblage A). Second, the Late Miocene was cool-temperate and characterized by periods of intensified upwelling, increase in productivity, abundant and diverse oceanic dinoflagellate cysts, and the highest percentages of AOM (palynofacies assemblage C). Third, the Early to early Late Pliocene was warm-temperate with some dry intervals (increase in grass pollen) and intensified upwelling. Fourth, the Neogene "carbonate crash" identified in other southern oceans was recognized in two palynofacies A samples in Hole 1085A that are nearly barren of dinoflagellate cysts: one Middle Miocene sample (590 mbsf, 13.62 Ma) and one Upper Miocene sample (355 mbsf, 6.5 Ma). Finally, the extremely low percentages of pollen suggest sparse vegetation on the adjacent landmass, and Namib desert conditions were already in existence during the late Middle Miocene. (c) 2005 Elsevier B.V All rights reserved.	Univ Missouri, Dept Geol Sci & Engn, Rolla, MO 65409 USA	University of Missouri System; Missouri University of Science & Technology	Univ Missouri, Dept Geol Sci & Engn, Rolla, MO 65409 USA.	cudeze@geo.tamu.edu; ikuenobe@umr.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691				[Anonymous], NEOGENE QUATERNARY D; [Anonymous], S BRIT ECOLOGICAL SO; Batten D., 1996, Palynology: principles and applications, P1011; BECK JH, 2003, 36 ANN M AM ASS STRA; BOLLI HM, 1978, INITIAL REPORTS DEEP; BORK M, 2003, 7 INT C MOD FOSS DIN, P27; Boulter M. 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H., 1960, MEDED GEOL STICHTING, V1, P1; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	81	35	43	0	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	APR 18	2005	219	3-4					199	223		10.1016/j.palaeo.2004.12.026	http://dx.doi.org/10.1016/j.palaeo.2004.12.026			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	922KV					2025-03-11	WOS:000228837700001
J	Gedl, P; Leszczynski, S				Gedl, P; Leszczynski, S			Palynology of the Eocene-Oligocene transition in the marginal zone of the Magura Nappe at Folusz (Western Carpathians, Poland)	GEOLOGICA CARPATHICA			English	Article						Carpathians; Eocene-Oligocene transition; Magura Nappe; paleoenvironment; biostratigraphy; flysch deposits; dinocysts	DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY; DELTA; SEA	Palynological investigations of the deep-marine Upper Eocene-Lower Oligocene, mainly turbiditic and hemipelagic sediments exposed at Folusz (Siary Zone of Magura Nappe, Polish part of the Western Carpathians), revealed a prevalence of land plant remains in the palynofacies. Dinoflagellate cysts are the most frequent among marine palynomorphs. A Priabonian age is found in the lower part of the Szymbark Shale; a Rupelian age is determined for the investigated part of the Magura Beds. Dinoflagellate cyst distribution shows no major changes, contrary to an outstanding change recorded in the coeval sediments from other parts of the Polish Carpathians. This implies different paleoenvironmental conditions in the northern part of the Magura Basin during the latest Eocene and Early Oligocene. Occurrence of high-latitude dinoflagellate cysts in the lowermost part of the section may be related to a drop of temperature in the. surface waters of the sedimentary basin during the Late Eocene. Dinoflagellate cysts, whose motile stages are thought to have inhabited near-shore waters, are frequent in turbidites, whereas the hemipelagic/pelagic sediments usually contain more numerous oceanic specimens. Recycled dinoflagellate cysts occur more frequently in turbidite sediments.	Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland; Jagiellonian Univ, Inst Geol Sci, PL-30063 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Jagiellonian University	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl		Leszczynski, Stanislaw/0000-0003-4797-2918				BATTEN DJ, 1996, AM ASS STRATIGRAPHIC, V3, P10122; BENEDEK PN, 1986, NORDWESTDEUTSCHLAND, P157; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Birkenmajer K., 1989, Annales Societatis Geologorum Poloniae, V59, P145; Blaicher J., 1963, Kwartalnik Geologiczny, V7, P620; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 1995, SOC ECON PALEONT MIN, V54, P295; BROMOWICZ J, 1992, ZESZ NAUK AKAD GOR H, V54, P1; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Chateauneuf J.J., 1980, Memorie du Bureau de Recherches Geologiques et Minieres, V116, P1; Coccioni R, 2000, TERRA NOVA, V12, P258, DOI 10.1046/j.1365-3121.2000.00305.x; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; DALE B, 1996, AM ASS STRATIGRAPHIC, V3, P1249; ELBEIALY SY, 1988, NEWSL STRATIGR, V19, P131; Gedl P, 2004, GEOL SOC SPEC PUBL, V230, P309, DOI 10.1144/GSL.SP.2004.230.01.16; Gedl P., 2000, Studia Geologica Polonica, V117, P155; GEDL P, 1999, PRZEGL GEOL, V47, P394; Gedl Przemyslaw, 1995, Acta Palaeobotanica, V35, P195; Gruas-Cavagnetto C., 1988, Revue de Paleobiologie, V7, P163; Kopciowski R., 1996, B PANSTW I GEOL, V374, P21; Koszarski L, 1960, KWART GEOL, V4, P749; KOSZARSKI L, 1974, GEOL USTAV DIONYZA S, P180; KOSZARSKI L, 1968, M3491B I GEOL; KOSZARSKI L, 1976, SPRAW POSIEDZ KOM NA, V20, P174; Ksiazkiewicz M., 1956, Geologische Rundschau, V45, P369, DOI 10.1007/BF01802022; KSIAZKIEWICZ M, 1974, WYDAWNICTWA GEOLOGIC, P1; KsiaZkiewicz M., 1977, WYDAWNICTWA GEOLOGIC, P476; KSIAZKIEWICZ M, 1962, I GEOL WARSZAWA; LESZCZYNSKI S, 2001, IAS 2001 21 M DAV SW, P99; Leszczynski Stanislaw, 2002, Annales Societatis Geologorum Poloniae, V72, P201; MAIER D., 1959, NEUES JB F R GEOLOGI, V107, P278; MANUM SB, 1989, SCI RESULTS, V104, P611; Martini E., 1971, P 2 PLANKT C ROM 197, P739; Morgenroth P., 1966, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V127, P1; Nemcok M, 2000, GEOL CARPATH, V51, P281; Olszewka B., 1984, Prace Instytutu Geologicznego (Warsaw), V110, P1; OLSZEWSKI B, 1985, P REP 13 C KBGA POL, V1, P57; OSZCZYPKO N, 1991, P POL ACAD SCI EARTH, V39, P415; Oszczypko-Clowes Marta, 2001, Annales Societatis Geologorum Poloniae, V71, P139; POMEROL C, 1916, TERMINAL EOCENE EVEN, V9, P1; Powell AJ, 1992, BRIT MICROPALAEONTOL, P155; Rögl F, 1999, GEOL CARPATH, V50, P339; SIKORA W, 1970, I GEOL B, V235, P1; Stover L.E., 1993, B SOC BELG GEOL, V102, P5; STOVER LE, 1996, AM ASS STRATIGRAPHIC, V2, P641; SWIDZINSKI H, 1934, POSIEDZ NAUK PANSTW, V38, P29; SZAJNOCHA W, 1895, WYDZIAL KRAJOWY KROL, P1; van Mourik CA., 2000, P OCEAN DRILL PROGRA, V171, P1; VANCOUVERING JA, 1981, PALAEOGEOGR PALAEOCL, V36, P321, DOI 10.1016/0031-0182(81)90111-5; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; ZEVENBOOM D, 1995, THESIS U UTRECHT, P1	55	12	14	0	2	SLOVAK ACADEMIC PRESS LTD	BRATISLAVA	PO BOX 57 NAM SLOBODY 6, 810 05 BRATISLAVA, SLOVAKIA	1335-0552			GEOL CARPATH	Geol. Carpath.	APR	2005	56	2					155	167						13	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	931WR					2025-03-11	WOS:000229516700006
J	Figueroa, RI; Bravo, I				Figueroa, RI; Bravo, I			Sexual reproduction and two different encystment strategies of <i>Lingulodinium polyedrum</i> (Dinophyceae) in culture	JOURNAL OF PHYCOLOGY			English	Article						Dinophyceae; encystment; excystment; gametes; life cycle; Lingulodinium polyedrum; mating type; reproduction	DINOFLAGELLATE GYMNODINIUM-CATENATUM; GONYAULAX-POLYEDRA; CYST FORMATION; LIFE-HISTORY; POPULATION-DYNAMICS; BENTHIC CYSTS; MATING-TYPE; TAMARENSIS; TEMPERATURE; DARKNESS	Unreported aspects in the sexual cycle of the marine dinoflagellate Lingulodinium polyedrum (Stein) Dodge were described. Our observations included the description of two types of hypnozygote formation, because culture planozygotes were observed to encyst in two different ways: an ecdysal sexual stage or a spiny resting cyst. Phosphate deficiency was the main nutritional condition required for fusing gamete pairs to form resting cysts, whereas replete conditions prevented their appearance and favored the formation of ecdysal sexual forms. Mating experiments revealed the existence of two sexual types (+/-), which were enough to explain resting cyst appearance (simple heterothallism). Morphological aspects and timing of gamete mating, fusion, and the efficiency of encystment under different external levels of nitrate and phosphate were analyzed after isolating and monitoring individual pairs of fusing gametes. The staining of sexual stages showed that nuclear fusion was completed at the same time as the cytoplasmic fusion. After 1 to 2 h, the planozygotes presented one quadrolobulated nucleus. Germination of ecdysal sexual stages occurred after < 24-72 h, whereas excystment of resting cysts was dependent on the studied parental cross and took place after 2-4 months. Newly germinated cells from both types of cysts had a similar, big, U-shaped nucleus. Twenty-four to 48 h after excystment, the germlings divided by desmoschisis, a process before which enlargement of the nucleus was observed.	Inst Oceanog Vigo, Vigo, Spain	Spanish Institute of Oceanography	Inst Oceanog Vigo, Vigo, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015	Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X				ADAIR WS, 1983, CELL, V33, P183, DOI 10.1016/0092-8674(83)90347-1; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Beam C. A., 1980, BIOCH PHYSL PROTOZOA, V3, P171; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1990, Scientia Marina, V54, P287; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Dale B., 1983, P69; Delgado M., 1999, Harmful Algae News, V19, P1; DIWALD KARL, 1938, FLORA, V32, P174; Draisci R, 1999, TOXICON, V37, P1187, DOI 10.1016/S0041-0101(98)00254-2; DURR G, 1974, CELL TISSUE RES, V150, P21; DURR G, 1979, ARCH PROTISTENKD, V122, P55; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; FIGUEROA RI, 2005, IN PRESS PHYCOLOGIA; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garces E., 2002, LIFEHAB, P46; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Goodenough U.W., 1985, MBL (Marine Biology Laboratory) Lectures in Biology, V7, P123; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; HARDELAND R, 1994, EXPERIENTIA, V50, P60, DOI 10.1007/BF01992051; Hoekstra R F, 1987, Experientia Suppl, V55, P59; Imai I., 1998, PHYSL ECOLOGY HARMFU, P95; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; KITA T, 1985, B MAR SCI, V37, P643; KOFOID C.A., 1911, U CALIFORNIA PUBLICA, V8, P187; Kokinos John P., 1995, Palynology, V19, P143; LEWIS J, 1988, BRIT PHYCOL J, V23, P49, DOI 10.1080/00071618800650071; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; MARASOVIC I, 1993, DEV MAR BIO, V3, P139; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; Park Ho-Dong, 1992, Journal of the Faculty of Science Shinshu University, V27, P87; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; PFIESTER LA, 1989, INT REV CYTOL, V114, P249; SAKO Y, 1984, B JPN SOC SCI FISH, V50, P743; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wall D., 1971, Geoscience Man, V3, P1; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131	41	85	89	4	39	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	APR	2005	41	2					370	379		10.1111/j.1529-8817.2005.04150.x	http://dx.doi.org/10.1111/j.1529-8817.2005.04150.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	909KS		Bronze, Green Submitted			2025-03-11	WOS:000227859400016
J	Guasti, E; Kouwenhoven, TJ; Brinkhuis, H; Speijer, RP				Guasti, E; Kouwenhoven, TJ; Brinkhuis, H; Speijer, RP			Paleocene sea-level and productivity changes at the southern Tethyan margin (El Kef, Tunisia)	MARINE MICROPALEONTOLOGY			English	Article						organic-walled dinoflagellate cysts; benthic foraminifera; Paleocene; paleoenvironment; sea-level; tethys	CRETACEOUS-TERTIARY BOUNDARY; WALLED DINOFLAGELLATE CYSTS; BENTHIC FORAMINIFERAL ASSEMBLAGES; SURFACE TEMPERATURE; EVENTS; INDICATORS; SEDIMENTS; RECORD; PALEOPRODUCTIVITY; EXTINCTION	Integrated analysis of quantitative distribution patterns of organic-walled dinoflagellate cysts (dinocysts) and benthic foraminifera from the Paleocene El Kef section (NW Tunisia) allows the reconstruction of sea-level and productivity fluctuations. Our records indicate that the environment evolved from an initially oligotrophic, open marine, outer neritic to upper bathyal setting towards a more eutrophic inner neritic setting, influenced by coastal upwelling by the end of the Paleocene. An overall second order change in paleodepth is reflected by both microfossil groups. From the base of planktic foraminifera Zone P4 onwards, the main phase of shallowing is evidenced by an increase of inner neritic dinocysts of the Areoligera group, disappearance of deeper-water benthic foraminifera and increasing dominance of shallow-marine taxa (several bulimmids, Haplophragnioides spp., Trochammina spp.). The total magnitude of this shallowing is obscured by interaction with a signal of eutrophication, but estimated to be around 150 m (from similar to 200 to similar to 50 m). Superimposed on the overall trend, third order sea-level fluctuations have been identified and correlated to sequences in other regions. Paleoproductivity indicators (notably protoperidinioid dinocysts and buliminids) show a trend from an oligotrophic to a eutrophic setting. (c) 2005 Elsevier B.V. All rights reserved.	Univ Bremen, Dept Geosci, FB 5, D-28334 Bremen, Germany; Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Katholieke Univ Leuven, Dept Geog & Geol, B-3000 Louvain, Belgium	University of Bremen; Utrecht University; Utrecht University; KU Leuven	Univ Bremen, Dept Geosci, FB 5, POB 330440, D-28334 Bremen, Germany.	eguasti@uni-bremen.de; tkouwenh@geo.uu.nl; H.Brinkhuis@bio.uu.nl; robert.speijer@geo.kuleuven.ac.be	Brinkhuis, Henk/B-4223-2009; Speijer, Robert/H-5073-2016	Brinkhuis, Henk/0000-0003-0253-6610; Speijer, Robert/0000-0002-5873-7203				Adatte T, 2002, PALAEOGEOGR PALAEOCL, V178, P165, DOI 10.1016/S0031-0182(01)00395-9; Batten D., 1996, Palynology: principles and applications, P1011; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Billups K, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2004PA001011; BOBIER C, 1991, EUROPEAN GEOTRAVERSE, P371; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; 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Micropaleontol.	APR	2005	55	1-2					1	17		10.1016/j.marmicro.2005.01.001	http://dx.doi.org/10.1016/j.marmicro.2005.01.001			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	926DJ		Green Published			2025-03-11	WOS:000229102800001
J	de Vernal, A; Eynaud, F; Henry, M; Hillaire-Marcel, C; Londeix, L; Mangin, S; Matthiessen, J; Marret, F; Radi, T; Rochon, A; Solignac, S; Turon, JL				de Vernal, A; Eynaud, F; Henry, M; Hillaire-Marcel, C; Londeix, L; Mangin, S; Matthiessen, J; Marret, F; Radi, T; Rochon, A; Solignac, S; Turon, JL			Reconstruction of sea-surface conditions at middle to high latitudes of the Northern Hemisphere during the Last Glacial Maximum (LGM) based on dinoflagellate cyst assemblages	QUATERNARY SCIENCE REVIEWS			English	Article							ARTIFICIAL NEURAL NETWORKS; LABRADOR SEA; LATE QUATERNARY; ATLANTIC-OCEAN; ICE COVER; PLANKTONIC-FORAMINIFERA; HYDROGRAPHIC CONDITIONS; DINOCYST ASSEMBLAGES; MARINE ENVIRONMENTS; RECENT SEDIMENTS	A new calibration database of census counts of organic-walled dinoflagellate cyst (dinocyst) assemblages has been developed from the analyses of surface sediment samples collected at middle to high latitudes of the Northern Hemisphere after standardisation of taxonomy and laboratory procedures. The database comprises 940 reference data points from the North Atlantic, Arctic and North Pacific oceans and their adjacent seas, including the Mediterranean Sea, as well as epicontinental environments such as the Estuary and Gulf of St. Lawrence, the Bering Sea and the Hudson Bay. The relative abundance of taxa was analysed to describe the distribution of assemblages. The best analogue technique was used for the reconstruction of Last Glacial Maximum (LGM) sea-surface temperature and salinity during summer and winter, in addition to sea-ice cover extent, at sites from the North Atlantic (n = 63), Mediterranean Sea (it = 1) and eastern North Pacific (n = 1). Three of the North Atlantic cores, from the continental margin of eastern Canada, revealed a barren LGM interval, probably because of quasi-permanent sea ice. Six other cores from the Greenland and Norwegian seas were excluded from the compilation because of too sparse assemblages and poor analogue situation. At the remaining sites (n = 54), relatively close modern analogues were found for most LGM samples, which allowed reconstructions. The new LGM results are consistent with previous reconstructions based on dinocyst data, which show much cooler conditions than at present along the continental margins of Canada and Europe, but sharp gradients of increasing temperature offshore. The results also suggest low salinity and larger than present contrasts in seasonal temperatures with colder winters and more extensive sea-ice cover, whereas relatively warm conditions may have prevailed offshore in summer. From these data, we hypothesise low thermal inertia in a shallow and low-density surface water layer. (c) 2004 Elsevier Ltd. All rights reserved.	Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; Univ Bordeaux 1, CNRS, UMR 5805, Dept Geol & Oceanog, F-33405 Talence, France; Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany; Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales; Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Quebec	de Vernal, A (通讯作者)，Univ Quebec, Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	Hillaire-Marcel, Claude/H-1441-2012; Hillaire-Marcel, Claude/C-9153-2013; de Vernal, Anne/D-5602-2013	Solignac, Sandrine/0000-0003-3373-6922; Hillaire-Marcel, Claude/0000-0002-3733-4632; de Vernal, Anne/0000-0001-5656-724X; Marret-Davies, Fabienne/0000-0003-4244-0437; Matthiessen, Jens/0000-0002-6952-2494; Eynaud, Frederique/0000-0003-1283-7425				Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; Be A.W. 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Sci. Rev.	APR-MAY	2005	24	7-9					897	924		10.1016/j.quascirev.2004.06.014	http://dx.doi.org/10.1016/j.quascirev.2004.06.014			28	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	914VO					2025-03-11	WOS:000228256300006
J	Van Simaeys, S; Munsterman, D; Brinkhuis, H				Van Simaeys, S; Munsterman, D; Brinkhuis, H			Oligocene dinoflagellate cyst biostratigraphy of the southern North Sea Basin	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Oligocene; dinoflagellate cysts; biostratigraphy; North Sea Basin	MIOCENE; STRATIGRAPHY; TRANSITION; BELGIUM; AREA	The Rupelian (Lower Oligocene) and Chattian (Upper Oligocene) stratotype sections are both defined on the basis of the southern North Sea Basin sedimentary successions. The characterisation of biotic events occurring within the stratotypes (and equivalents) is vital for the recognition of these stages outside the North Sea Basin. Although the restricted marine setting of the North Sea Basin during most of the Paleogene clearly hampers 'traditional' calcareous microfossil calibration, organic-walled dinoflagellate cysts (dinocysts) are increasingly successful in the stratigraphic analysis and calibration of the marginal-marine North Sea Basin successions. Here we present a high-resolution Oligocene dinocyst biostratigraphic zonation scheme for the southern North Sea Basin based on previously published and new dinocyst studies from Belgium, northern Germany and The Netherlands. Eight (southern) North Sea Oligocene (NSO) dinocyst zones (biozones) and four subzones are here defined. Their application on a regional and inter-regional scale is discussed. The stratigraphic important Late Oligocene dinocyst taxon Triphragmadinium demaniae gen. and sp. nov. is formally described. (c) 2004 Elsevier B.V. All rights reserved.	Univ Louvain, B-3000 Louvain, Belgium; TNO, Natl Geol Survey, Netherlands Inst Appl Geosci, NL-3508 TA Utrecht, Netherlands; Univ Utrecht, Lab Paleobot & Palynol, NL-3584 CD Utrecht, Netherlands	Netherlands Organization Applied Science Research; Utrecht University	Univ Louvain, Redingenstr 16, B-3000 Louvain, Belgium.	stefaan.vansimaeys@geo.kuleuven.ac.be	Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BENEDEK PN, 1975, P 6 C REG COMM MED N, P43; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Brinkhuis H, 2000, REV PALAEOBOT PALYNO, V110, P93, DOI 10.1016/S0034-6667(99)00062-7; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 1995, SOC ECON PALEONT MIN, V54, P295; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak JP., 1980, PALAEONTOLOGICAL ASS, V24, P36; De Coninck J., 1999, B SOC BELG GEOL, V105, P171; De Coninck Jan, 1995, Mededelingen Rijks Geologische Dienst, V53, P65; Deconinck Jan, 2001, Service Geologique de Belgique Professional Paper, V294, P1; DeConto RM, 2003, NATURE, V421, P245, DOI 10.1038/nature01290; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Dybkjaer K, 2000, B GEOL SOC DENMARK, V47, P87; Eaton GL, 2001, NEUES JAHRB GEOL P-A, V219, P171, DOI 10.1127/njgpa/219/2001/171; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Gedl P., 2000, Studia Geologica Polonica, V117, P69; Heilmann-Clausen C., 1989, Geol. 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Palaeobot. Palynology	APR	2005	134	1-2					105	128		10.1016/j.revpalbo.2004.12.003	http://dx.doi.org/10.1016/j.revpalbo.2004.12.003			24	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	913MG					2025-03-11	WOS:000228155200006
J	Martínez, MA; Quattrocchio, ME; Prámparo, MB				Martínez, MA; Quattrocchio, ME; Prámparo, MB			Palynological analysis of the Los Molles Formation, Cuyo Group, Middle Jurassic of the Neuquen Basin, Argentina	AMEGHINIANA			Spanish	Article						palynology; systematics; Los Molles Formation; Middle Jurassic; Neuquen Basin; Argentina	BIOLOGICAL AFFINITIES; SEQUENCE STRATIGRAPHY; ACRITARCHS; MARINE	PALYNOLOGICAL ANALYSIS OF THE Los MOLLES FORMATION, CUYO GROUP, MIDDLE JURASSIC OF THE NEUQUEN BASIN, ARGENTINA. Sporomorphs and paleomicroplankton identified from the Middle Jurassic, Los Molles Formation, Cuyo Group, are described and illustrated in this contribution. The palynomorphs were recovered from three of the five sampled surface sections (Lohan Mahuida, Puente Picun Leufu, Puesto Policia, Los Molles and Cerro Lotena) located near Zapala city, Neuquen Basin, Argentina. The studied microfloras include 50 species of sporomorphs (20 spores and -30 pollen grains) and 31 species of paleomicroplankton (9 green algae, two dinoflagellate cysts and 20 acritarchs). Specimens belonging to the genera Divisisporites, Callialaspo rites, Monosillcitcs and one spore gen. et sp. indet. are described. Systematics include prasinophyte of the genera Cymatiosphaera, Pleurozonaria and Tasinnintes. Also included are acritarchs of the genera Baltisphaeridiuni, Filispliaeridium, Micrhystridium, Leiosphaeridia, Polygonium and Veryhachium. The new combination Cymatiosphaera volkheimerii (Quattrocchio) is proposed. The occurrence of the acritarchs Filisphaeridium balmei (Sarjeant) Sarjeant and Stancliffe, F. castaninuin (Valensi) Sarjeant and Stancliffe, F. densispinum (Valensi) Sarjeant and Stancliffe and Verylinchilon valensii (Valensi) Downie and Sarjeant is mentioned for the first time in the Neuquen Basin. The studied palynofloras are correlated with the Biozone of Callialasporites "complex" (Sub-biozone of Callialasporites trilobatus (Balme) Dev, Antulsporites snevus (Balme) Archangelsky and Gamerro and Klukisporites labiatus (Volkheimer) Baldoni and Archangelsky) previously proposed for this area of the Neuquen Basin. A Late Aalenian - Early Bajocian age is suggested for the studied sections.	Univ Nacl Sur, CONICET, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Ianigla, CONICET, CRICYT, Unidad Paleopalinol, RA-5500 Mendoza, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); University Nacional Cuyo Mendoza; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); CRICYT	Univ Nacl Sur, CONICET, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	martinez@criba.edu.ar; mquattro@criba.edu.ar; mpramparo@lab.cricyt.edu.ar						ABBINK OA, 1998, LAB PALEOBOTANY PALY; ALALMERY TK, 1986, J MICROPALAEONTOL, V5, P27; ALALMERY TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103; [Anonymous], [No title captured]; [Anonymous], 1980, PALEOBIOLOGY PLANT P; Balme B.E., 1957, COMMONW SCI IND RES, V25, P1; Brocke Rainer, 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P53; COLBATH G K, 1979, Palaeontographica Abteilung B Palaeophytologie, V171, P1; COLBATH GK, 1983, PHYCOLOGIA, V22, P249, DOI 10.2216/i0031-8884-22-3-249.1; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; COOKSON IC, 1947, ANTARCIC RES EXPEDIT, V8, P127; COOKSON ISABEL C., 1960, NYTT MAG BOT, V8, P5; COUPER R.A., 1958, PALAEONTOGRAPHICA, V103, P75; COUPER RA, 1953, NEW ZEALAND GEOLOGIC, V22, P3; Courtinat B, 1983, CAH MICROPALEONTOL E, V1, P1; DAVEY RJ, 1970, B BRIT MUS NAT HIST, V18, P335; DECONINCK J, 1965, ACAD ROYALE SCI LETT, V8, P36; Deflandre G., 1935, Bulletin Biologique de la France et de la Belgique, V69, P213; DEFLANDRE G., 1954, COMPTES RENDUS SOMMA, V12, P257; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE G, 1970, CAHIERS MICOPALEONTO, V2, P1; DEFLANDRE G, 1941, MEM ACAD SCI, V65, P1; DEUNFF J, 1951, CR HEBD ACAD SCI, V233, P321; Deunff J., 1954, Compte Rendu Sommaire de la Socit gologique de France, V13, P305; Downie C., 1959, Palaeontology, V2, P56; DOWNIE C, 1963, PALAEONTOLOGY, V6, P83; DOWNIE C, 1963, GEOLOGICAL SCI, V7, P1; Downte C., 1965, GEOLOGICAL SOC AM, V94, P1; EIKENACK A., 1972, NEUES JAHRBUCHFUR GE, P596; Eisenack A., 1958, Palaeontographica, V110A, P1; Eisenack A., 1958, Senckenbergiana lethaea, v, V39, P389; EISENACK ALFRED, 1931, PALAEONT ZEITSCHR, V13, P74; Eiserhardt K.-H., 1989, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V68, P79; Erdtman G., 1947, SVENSK BOT TIDSKR, V41, P104; Erkmen U., 1980, Geobios (Villeurbanne), V13, P45, DOI 10.1016/S0016-6995(80)80014-3; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Garcia V.M., 1994, REVISTA ASOCIACION G, V49, P184; GARCIA VM, 2000, 11 S ARG PAL PAL RES, P32; GARCIA VM, 1998, THESIS U NACIONAL SU; GROBER P, 1946, REVISTA ASOCIACION G, V1, P177; Gulisano C.A., 1984, Congreso Geologico Argentino, V9, P236; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; Guy-Ohlson Dorothy, 1994, Geobios Memoire Special (Villeurbanne), V17, P275; GUYOHLSON D, 1988, BOT MAR, V31, P447, DOI 10.1515/botm.1988.31.5.447; GUYOHLSON D, 1992, PHYCOLOGIA, V31, P523, DOI 10.2216/i0031-8884-31-6-523.1; JACOBSON S R, 1985, Palynology, V9, P165; Jansonius J., 1962, PALAEONTOGRAPHICA, V110, P35; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; Madler K., 1968, Beihefte zum Geologischen Jahrbuch, V58, P287; Martínez MA, 2002, AMEGHINIANA, V39, P221; MARTINEZ MA, 1999, THESIS U NACIONAL SU; MARTINEZ MA, 2001, REVISTA ESPANOLA MIN, V33, P31; Newton E.T., 1875, GEOL MAG, V2, v, P337, DOI DOI 10.1017/S001675680016008X; Nilsson T., 1958, LUNDS U ARSSKRIFT, V2, P1; Palliani Raffaela Bucefalo, 1996, Palynology, V20, P157; Pocock S.A.J., 1972, Palaeontographica Abteilung B Palaeophytologie, V137, P85; PRAMPARO MB, 1989, THESIS U NACIONAL RI; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Prauss M, 2001, PALAEOGEOGR PALAEOCL, V174, P221, DOI 10.1016/S0031-0182(01)00295-4; PRAUSS M, 1991, GEOL SOC SPEC PUBL, P335, DOI 10.1144/GSL.SP.1991.058.01.21; PRAUSS M, 1989, NEUES JB GEOLOGIE PA, V11, P671; PRAUSS M, 2000, NEUES JB GEOLOGIE PA, P107; Quattrocchio M, 1996, GEORES FORUM, V1&2, P467; Quattrocchio M.E., 1980, Opera Lilloana, V31, P1; Quattrocchio ME, 1996, GEORES FORUM, V1&2, P167; Riccardi A. 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W., 1953, PALAEONTOGRAPHICA, V94 B., P1; VALENSI L., 1948, BULL SOC GEOL FRANCE, V18, P537; VALENSI LIONEL, 1953, MEM SOC GEOL FRANCE, V68, P1; Vavrdova M., 1966, Casopis pro Mineralogii a Geologii, V11, P409; VOLKHEIMER W, 1974, Ameghiniana, V11, P135; VOLKHEIMER W, 1973, Ameghiniana, V10, P105; VOLKHEIMER W, 1975, Ameghiniana, V12, P193; Volkheimer W., 1968, AMEGHINIANA, V5, P333; Volkheimer W., 1972, Revista del Museo de la Plata, P101; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; Weaver C., 1931, Memoires of the University of Washington, V1, P1; Westermann G.E.G., 1979, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V164, P85; Wetzel O., 1933, Palaeontographica Stuttgart, V77, P141; WETZEL O, 1933, PALAEONTOGR ABT A, V77, P78; Zavala C, 1996, GEORES FORUM, V1&2, P295; Zavala C, 1996, GEORES FORUM, V1&2, P285; ZAVALA CA, 1993, THESIS U NACIONAL SU; [No title captured]	96	10	11	0	0	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	MAR 30	2005	42	1					67	92						26	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	922XA					2025-03-11	WOS:000228872000005
J	Lass, S; Vos, M; Wolinska, J; Spaak, P				Lass, S; Vos, M; Wolinska, J; Spaak, P			Hatching with the enemy:: <i>Daphnia</i> diapausing eggs hatch in the presence of fish kairomones	CHEMOECOLOGY			English	Article						inducible defences; resting egg; ephippia; infochemical; diapause	PREDATOR-INDUCED DIAPAUSE; CYCLICAL PARTHENOGEN; LIFE-HISTORY; RESTING EGGS; SEXUAL EGGS; MAGNA; SIZE; PATTERNS; DIFFERENTIATION; REPRODUCTION	Infochemicals are known to play a key role in mediating predator-prey interactions, both in aquatic and terrestrial communities. However, state-dependent variation may exist in how effectively individuals can use this information, depending on genotype, life stage and experience. For our study, we used the predator-prey model system fish-waterflea Daphnia magna Straus (Cladocera, Daphniidae). Adult Daphnia use fish-derived infochemicals, so-called kairomones, as indicators of predation risk, and exhibit a spectrum of morphological, behavioural and life-history responses to the presence of fish kairomones. Here, we investigate whether diapausing eggs, an embryonic resting stage in the life cycle of D. magna, also use fish kairomones and tune their hatching to the risk of fish predation, as reported for diapausing stages of dinoflagellates. In two laboratory experiments, we studied hatching proportion and time until hatching of D. magna diapausing eggs in the absence and presence of fish kairomones. D. magna families differed significantly in their response to the presence of fish kairomones; some families reduced hatching proportion, whereas others increased it. Our results imply genotype-dependent differences in the hatching reactions to fish kairomones as observed for other traits in adult Daphnia.	EAWAG, Dept Limnol, CH-8600 Dubendorf, Switzerland; NIOO KNAW, Ctr Limnol, Dept Food Web Studies, Netherlands Inst Ecol, NL-3631 AC Nieuwersluis, Netherlands; Univ Fribourg, Dept Biol, Unit Ecol & Evolut, CH-1700 Fribourg, Switzerland	Swiss Federal Institutes of Technology Domain; Swiss Federal Institute of Aquatic Science & Technology (EAWAG); Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); University of Fribourg	EAWAG, Dept Limnol, Uberlandstr 133,Postfach 611, CH-8600 Dubendorf, Switzerland.	sandra.lass@unifr.ch	Wolinska, Justyna/N-6455-2014; Vos, Matthijs/B-3802-2009	Wolinska, Justyna/0000-0003-2913-2923				[Anonymous], 2012, Biometry; Boersma M, 1996, CAN J FISH AQUAT SCI, V53, P18, DOI 10.1139/cjfas-53-1-18; Boersma M, 1998, AM NAT, V152, P237, DOI 10.1086/286164; Boersma M, 1999, LIMNOL OCEANOGR, V44, P393, DOI 10.4319/lo.1999.44.2.0393; Caceres CE, 1997, INVERTEBR BIOL, V116, P371, DOI 10.2307/3226870; Cáceres CE, 2001, FRESHWATER BIOL, V46, P1179, DOI 10.1046/j.1365-2427.2001.00737.x; CARVALHO GR, 1987, J ANIM ECOL, V56, P453, DOI 10.2307/5060; CARVALHO GR, 1983, FRESHWATER BIOL, V13, P37, DOI 10.1111/j.1365-2427.1983.tb00655.x; De Meester L, 1999, P ROY SOC B-BIOL SCI, V266, P2471; deMeester L, 1996, EVOLUTION, V50, P1293, DOI 10.1111/j.1558-5646.1996.tb02369.x; DEMEESTER L, 1993, FRESHWATER BIOL, V30, P219; DEMEESTER L, 1993, FRESHWATER BIOL, V30, P227; DEMEESTER L, 1993, OECOLOGIA, V96, P80, DOI 10.1007/BF00318033; Dicke M, 1988, FUNCT ECOL, V2, P131, DOI 10.2307/2389687; Dicke M., 1992, Insect Chemical Ecology: An Evolutionary Approach, P122; Haag CR, 2003, EVOLUTION, V57, P777, DOI 10.1111/j.0014-3820.2003.tb00289.x; Hairston NG, 2000, FRESHWATER BIOL, V45, P133; HALL DJ, 1976, ANNU REV ECOL SYST, V7, P177, DOI 10.1146/annurev.es.07.110176.001141; INNES D J, 1984, Genetics, V107, pS51; Karban R., 1997, Induced Responses to Herbivory, V1; Kats LB, 1998, ECOSCIENCE, V5, P569; KLEIVEN OT, 1992, OIKOS, V65, P197, DOI 10.2307/3545010; LAMPERT W, 1993, ECOLOGY, V74, P1455, DOI 10.2307/1940074; Lampert W., 1991, INT VER THEOR ANGEW, V24, P795; Lass S, 2001, HYDROBIOLOGIA, V442, P199, DOI 10.1023/A:1017538524539; LEIBOLD M, 1991, OECOLOGIA, V86, P342, DOI 10.1007/BF00317599; Li DQ, 2002, P ROY SOC B-BIOL SCI, V269, P2155, DOI 10.1098/rspb.2002.2140; MELLORS WK, 1975, ECOLOGY, V56, P974, DOI 10.2307/1936308; MULLER J, 1994, GENETICS AND EVOLUTION OF AQUATIC ORGANISMS, P342; Palo RT., 1991, PLANT DEFENSES MAMMA; PANCELLA JOHN R., 1963, CHESAPEAKE SCI, V4, P135, DOI 10.2307/1350746; PAREJKO K, 1990, HYDROBIOLOGIA, V198, P51, DOI 10.1007/BF00048622; Pijanowska J, 1996, J PLANKTON RES, V18, P1407, DOI 10.1093/plankt/18.8.1407; PROCTOR VW, 1964, ECOLOGY, V45, P656, DOI 10.2307/1936124; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Roitberg B.D., 1992, Insect Chemical Ecology: An evolutionary approach; *SAS I INC, 2002, JMP 5 0 1A; SCHWARTZ SS, 1987, FRESHWATER BIOL, V17, P373, DOI 10.1111/j.1365-2427.1987.tb01057.x; Sih A., 1987, P203; Slusarczyk M, 1999, OECOLOGIA, V119, P159, DOI 10.1007/s004420050772; SLUSARCZYK M, 1995, ECOLOGY, V76, P1008, DOI 10.2307/1939364; SOUTHWOOD TRE, 1978, EVOLUTION INSECT MIG, P277; Spaak P, 1997, LIMNOL OCEANOGR, V42, P753, DOI 10.4319/lo.1997.42.4.0753; Stoddart DM., 1980, ECOLOGY VERTEBRATE O; STROSS RG, 1966, ECOLOGY, V47, P368, DOI 10.2307/1932977; Tollrian R., 1999, ECOLOGY EVOLUTION IN; WEIDER LJ, 1987, ECOLOGY, V68, P188, DOI 10.2307/1938819; Weider LJ, 1997, P ROY SOC B-BIOL SCI, V264, P1613, DOI 10.1098/rspb.1997.0225; Weismann A., 1880, Z WISS ZOOL, V33, P55; WERNER EE, 1986, AM NAT, V128, P319, DOI 10.1086/284565; WOLF HG, 1989, FRESHWATER BIOL, V22, P471, DOI 10.1111/j.1365-2427.1989.tb01119.x; Zaffagnini F., 1987, Memorie dell'Istituto Italiano di Idrobiologia Dott Marco de Marchi, V45, P245	52	31	36	1	23	SPRINGER BASEL AG	BASEL	PICASSOPLATZ 4, BASEL, 4052, SWITZERLAND	0937-7409	1423-0445		CHEMOECOLOGY	Chemoecology	MAR	2005	15	1					7	12		10.1007/s00049-005-0286-8	http://dx.doi.org/10.1007/s00049-005-0286-8			6	Biochemistry & Molecular Biology; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Environmental Sciences & Ecology	904QW					2025-03-11	WOS:000227513800002
J	Medeanic, S; Dillenburg, SR				Medeanic, S; Dillenburg, SR			Palynology and <SUP>210</SUP>Pb datings:: First integrated approach to estimating anthropogenic impact on the environment of the Tramandai Lagoon and adjacent areas during the last century	JOURNAL OF COASTAL RESEARCH			English	Article						native vegetation; introduced plants; algae	VEGETATION; POLLEN	The shallow Tramandaf Lagoon in the southeastern Rio Grande do Sul State in Brazil is only 1.4 m deep, covers about 18.8km(2) and now is largely urbanized. The lagoon is influenced by man's impact on the area. This study uses Pb-210 dated, palynologically analyzed samples from a 1.32 m core. The major groups studied were pollen and spores of plants, zygospores and coenobias of freshwater algae Chlorophyta, dinoflagellate and silicoflagellate cysts. Three stages of environmental evolution are clearly evident - 1905-1933, 1933-1971, and 1971-1997. The last stage being particularly well expressed is characterized by reduced variety of native plants, significant distribution of introduced plants, increase in marine algae and decrease in freshwater algae connected to increase in antropogenic influence in this region.	UFRGS, CNPQ Grant, Inst Geosci, BR-91509900 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Medeanic, S (通讯作者)，UFRGS, CNPQ Grant, Inst Geosci, Bento Goncalves Ave 9500, BR-91509900 Porto Alegre, RS, Brazil.	svetlana.medeanic@ufrgs.br; sergio.dillenburg@ufrgs.br	Dillenburg, Sergio/C-4027-2013	Dillenburg, Sergio/0000-0003-0072-7018				[Anonymous], 2007, Paleopalynology; BOTTEMA S, 1990, MANS ROLE IN THE SHAPING OF THE EASTERN MEDITERRANEAN LANDSCAPE, P231; Bottema S., 1982, PALAEOHISTORIA, V24, P257; CLARK JS, 1984, J SEDIMENT PETROL, V54, P1249; Costa CSB, 1996, J COASTAL RES, V12, P133; Dillenburg SR, 1994, THESIS U FEDERAL RIO; DILLENBURG SR, 1995, P 5 C ASS BRAS EST Q, P224; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; HOOGHIEMSTRA H, 1993, REV PALAEOBOT PALYNO, V77, P235, DOI 10.1016/0034-6667(93)90006-G; Horrocks M, 2002, J ROY SOC NEW ZEAL, V32, P337, DOI 10.1080/03014223.2002.9517698; KERSHAW AP, 1994, REV PALAEOBOT PALYNO, V82, P83, DOI 10.1016/0034-6667(94)90021-3; LEGESSE D, 2002, PALAEOGEOGR PALAEOCL, V187, P207; RAMOS RF, 1977, THESIS U FEDERAL RIO; Reitz R., 1988, MADEIRA RIO GRANDE S; SILVA CS, 2002, COMORTAMENTO NUTR ME; SOARES LS, 1986, TRAMANDAI TERRA GENT; Tomazelli L.J., 1992, Pesquisas, V19, P3, DOI [DOI 10.22456/1807-9806, 10.22456/1807-9806.21318, DOI 10.22456/1807-9806.21318]; TOZZI HAM, 1999, THESIS U FEDERALRIO; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Villwock J.A., 1995, Notas Tecnicas, V8, P1; Woo HJ, 1998, REV PALAEOBOT PALYNO, V102, P289, DOI 10.1016/S0034-6667(98)80011-0	21	5	5	0	4	COASTAL EDUCATION & RESEARCH FOUNDATION	LAWRENCE	810 EAST 10TH STREET, LAWRENCE, KS 66044 USA	0749-0208			J COASTAL RES	J. Coast. Res.	SPR	2005					42		271	276						6	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	947FU					2025-03-11	WOS:000230629600030
J	Coyne, KJ; Cary, SC				Coyne, KJ; Cary, SC			Molecular approaches to the investigation of viable dinoflagellate cysts in natural sediments from estuarine environments	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article; Proceedings Paper	Symposium on Advances in the Molecular Ecology of Protists	JUN 02-06, 2004	Bryant Coll, Smithfield, RI	Int Soc Protistol	Bryant Coll	anoxia; cDNA; cytochrome; Delaware Inland Bays; excystment; germination; harmful algal blooms; mRNA; Pfiesteria; RT-PCR	ALEXANDRIUM-TAMARENSE DINOPHYCEAE; PFIESTERIA-PISCICIDA; GONYAULAX-TAMARENSIS; GENE-EXPRESSION; SERIAL ANALYSIS; MESSENGER-RNAS; RESTING CYSTS; GERMINATION; INITIATION; TOLERANCE	Molecular methods offer an efficient alternative to microscopic identification of dinotlagellate cysts in natural sediments. Unfortunately, amplification of DNA also detects the presence of dead cells and is not a reliable indication of cyst viability. Because mRNA transcripts are more labile than DNA, the presence of specific transcripts may be used as a proxy for cyst viability. Here, we evaluate mRNA detection capabilities for identification of viable cysts of the dinotlagellate, Pfiesteria piscicida, in natural sediment samples. We targeted transcripts for cytochrome c oxidase subunit 1, cytochrome b (COB), and Tags 343 and 277, recently identified by serial analysis of gene expression. Expression was confirmed in laboratory cultures and compared with natural sediment samples. Three of the transcripts were detected in sediments by RT-PCR. The fourth transcript, for COB, was not detected in sediments, perhaps because of down-regulation of the gene in anoxic conditions. Our results suggest that methods targeting specific mRNA transcripts may be useful for detection of viable cysts in natural sediment samples. In addition, dinotlagellate cysts, which sustain extended periods of anoxia, may provide an important source of data for studies of anoxia tolerance by microbial eukaryotes.	Univ Delaware, Coll Marine Studies, Lewes, DE 19958 USA; Univ Waikota, Hamilton, New Zealand	University of Delaware; University of Waikato	Univ Delaware, Coll Marine Studies, Lewes, DE 19958 USA.	kcoyne@udel.edu		Coyne, Kathryn/0000-0001-8846-531X; Cary, Stephen/0000-0002-2876-2387				ALTSCHUL SF, 1990, J MOL BIOL, V215, P403, DOI 10.1016/S0022-2836(05)80360-2; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; Caron DA, 2004, J EUKARYOT MICROBIOL, V51, P38, DOI 10.1111/j.1550-7408.2004.tb00159.x; Caron DA, 1999, HYDROBIOLOGIA, V401, P215, DOI 10.1023/A:1003721923719; CHOMCZYNSKI P, 1987, ANAL BIOCHEM, V162, P156, DOI 10.1006/abio.1987.9999; Coyne KJ, 2004, APPL ENVIRON MICROB, V70, P5298, DOI 10.1128/AEM.70.9.5298-5304.2004; Coyne KJ, 2001, AQUAT MICROB ECOL, V24, P275, DOI 10.3354/ame024275; Dagsgaard C, 2001, J BIOL CHEM, V276, P7593, DOI 10.1074/jbc.M009180200; Dempster EL., 1999, BIOTECHNIQUES, V27, P66; Díez B, 2001, APPL ENVIRON MICROB, V67, P2942, DOI 10.1128/AEM.67.7.2942-2951.2001; Doblin M.A., 2004, Harmful Algae 2002, P317; GELFAND R, 1981, MOL CELL BIOL, V1, P497, DOI 10.1128/MCB.1.6.497; Godhe Anna, 2002, Harmful Algae, V1, P361, DOI 10.1016/S1568-9883(02)00053-7; Guillard R. 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Eukaryot. Microbiol.	MAR-APR	2005	52	2					90	94		10.1111/j.1550-7408.2005.05202001.x	http://dx.doi.org/10.1111/j.1550-7408.2005.05202001.x			5	Microbiology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Microbiology	919EL	15817113				2025-03-11	WOS:000228601000003
J	Abreu, PC; Robaldo, RB; Sampaio, LA; Bianchini, A; Odebrecht, C				Abreu, PC; Robaldo, RB; Sampaio, LA; Bianchini, A; Odebrecht, C			Recurrent amyloodiniosis on broodstock of the Brazilian flounder <i>Paralichthys orbignyanus</i>:: Dinospore monitoring and prophylactic measures.	JOURNAL OF THE WORLD AQUACULTURE SOCIETY			English	Article							OCELLATUM BROWN 1931; DINOFLAGELLATE PARASITE; SPARUS-AURATA; MARINE FISH; SEA BREAM; INFECTIONS; BASS	Broodstock of the Brazilian flounder Paralichthys orbignyanus (Valenciennes, 1839) kept in the laboratory suffered recurrent heavy infestations by the ectoparasitic dinoflagellate Anzyloodinium cf. ocellatum. Between 10 January and 26 February 2003 we monitored A. cf. ocellatum dinospore (infectious motile stage) abundance in a maturation system in order to predict amyloodiniosis outbreaks. Though daily water exchange rate of the tank containing the specimens was 150% of total tank volume (2,500 L), by 15 January the dinospore abundance in the tank reached 1,800 cells/L and on 25 January 7,200 cells/L. There was a subsequent small decrease in dinospore abundance, but by the end of the study period counts were still around 3,000 cells/L. Infested fish were successfully treated with copper sulfate (1.5-mg Cu/L for 24 h during 7d). Observation of the biofilm from the bottom of the tank showed a high number of resting cysts (tomonts) of A. cf. ocellatum after treatment. Apparently, the copper sulfate forced the detachment of the trophonts (feeding parasitic growth stage), and generated the high number of tomonts at the bottom of the tank. The copper sulfate concentration used in the treatment was not effective to kill the tomonts. After a disease outbreak in March 2002 and fish recovery, the biofilm with tomonts at the bottom of the tank was removed by brushing and the use of hydrochloric acid (HCl 30% v/v). After this, no infestation occurred for at least a month. Meanwhile, fish in a nearby tank, where biofilm was not removed, had three amyloodiniosis outbreaks. Our results show that the water exchange rate applied was not sufficient to eliminate the dinospores from the water column, or to remove and eliminate the tomonts from the biofilm. We suggest that cleaning the biofilm of tanks after treatment of infested fish should be considered as a prophylactic measure in order to avoid recurrent amyloodiniosis.	Fundacao Univ Fed Rio Grande, FURG, Dept Oceanog, BR-96201900 Rio Grande, RS, Brazil; Fundacao Univ Fed Rio Grande, FURG, Dept Ciencias Fisiol, BR-96201900 Rio Grande, RS, Brazil	Universidade Federal do Rio Grande; Universidade Federal do Rio Grande	Fundacao Univ Fed Rio Grande, FURG, Dept Oceanog, Cx P 474, BR-96201900 Rio Grande, RS, Brazil.		Odebrecht, Clarisse/ISV-0176-2023; Bianchini, Adalto/C-5384-2013; Abreu, Paulo/A-5145-2013; Odebrecht, Clarisse/J-6855-2012	Bianchini, Adalto/0000-0002-7627-7650; Abreu, Paulo/0000-0002-7657-1112; Sampaio, Luis Andre/0000-0001-6533-1837; Odebrecht, Clarisse/0000-0001-7159-4713				Aiello P., 1986, Bulletin of the European Association of Fish Pathologists, V6, P110; ALVAREZPELLITERO P, 1995, J FISH DIS, V18, P105, DOI 10.1111/j.1365-2761.1995.tb00268.x; Benetti D. 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A., 2001, Journal of Applied Aquaculture, V11, P67, DOI 10.1300/J028v11n01_06; Sampaio LA, 2002, J EXP MAR BIOL ECOL, V269, P187, DOI 10.1016/S0022-0981(01)00395-1; SCHWARZ MH, 1998, PUBL VIRGINIA COOPER, V600; SCOTT P, 1993, AQUACULTURE VET; SMITH DM, 1994, NEUROGASTROENT MOTIL, V6, P79; Throndsen J., 1978, Preservation and storage, P69, DOI DOI 10.1111/J.0022-3646.1975.00142.X; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091	34	12	17	0	3	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0893-8849	1749-7345		J WORLD AQUACULT SOC	J. World Aquacult. Soc.	MAR	2005	36	1					42	50						9	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	917AX					2025-03-11	WOS:000228429300006
J	Vershinin, AO; Moruchkov, AA; Leighfield, T; Sukhanova, IN; Pan'kov, SL; Morton, SL; Ramsdell, JS				Vershinin, AO; Moruchkov, AA; Leighfield, T; Sukhanova, IN; Pan'kov, SL; Morton, SL; Ramsdell, JS			Potentially toxic algae in the coastal phytoplankton of the northeast Black Sea in 2001-2002	OCEANOLOGY			English	Article								During the period from June 2000 to April 2002, phytoplankton monitoring was carried out at three stations located on the Black Sea shore of the Caucasus. In the coastal phytoplankton of the Northeast Black Sea, 93 species belonging to 7 classes were found. Thirteen species from this list are known as toxic according to data obtained in other seas. Two species of diatoms, namely, Pseudo-nitzschia pseudodelicatissima and R pungens (their abundance in June 2001 was 693 x 10(3) cells/l) were identified. They are capable of causing amnesic shellfish poisoning; the manifestation of their toxic properties depends on the environmental conditions. A check of the corresponding mussel samples for the content of amnesic toxin such as domoic acid gave a negative result. In the summer of 2001, in the Black Sea, a dinoflagellate belonging to the Alexandrium genus was encountered for the first time. Many species of this genus can be a reason for the lethally dangerous paralytic shellfish poisoning. In February of 2002, hatching of cysts and a population outburst of Alexandrium spp. (4.5 x 10(3) cells/l) were observed. During the period from April to November, in the phytoplankton, species belonging to the Dinophysis genus, namely, D. rotundata, D. caudata, D. acuminata, D. hastata, D. fortii, D. norvegica, D. tripos, and D. sacculus (up to 3 x 10(3) cells/l), occurred during the period of the spring phytoplankton bloom. They are all known to be producers of toxins causing diarrhetic shellfish poisoning. The epiphytic dinophlagellate Prorocentrum lima was intermittently present in the samples collected during the period from May to November (the maximum abundance in September of 2001 was 400 cells/l). It was introduced into a laboratory culture and produced diarrhetic toxins, namely, okadaic acid and Dinophysis-toxin 1. P. lima is dangerous because it grows on macroalgae fouling mussels and oysters, including those in commercial mariculture. All the samples of mussel tissues taken in the summer of 2001 contained diarrhetic toxins that most likely originated from P lima. The toxin concentrations in the mussels did not exceed 0.2 μ g/g, of tissue and were lower than the maximum permissible concentration accepted in the European Community and Canada. The mixotrophic ichthyotoxic dinophlagellate Cochlodinium polykrikoides, which was first encountered off the Russian coast, featured a bloom in the area off Utrish in August of 2001 (the maximum abundance was up to 70 x 10(3) cells/l; the biomass was up to 620 μ g/l) and should be considered as a risk-factor for the caged fish aquaculture in the Black Sea.	Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia; Natl Ocean Serv, Ctr Coastal & Biomol Res, Charleston, SC USA; Bolshoi Utrish Expt Ctr Marine Biotechnol, Anapa, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA	Vershinin, AO (通讯作者)，Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow, Russia.			Leighfield, Tod/0000-0002-6780-8800				Bates S.S., 2001, HARMFUL ALGAL BLOOMS, P320; Davidovich NA, 1998, J PHYCOL, V34, P126, DOI 10.1046/j.1529-8817.1998.340126.x; HALLEGRAEFF GM, 1995, MANUAL HARMFUL ALGAL; IVANOV A. I., 1960, TRUDY VSESOIUZ GIDROBIOL OBSHCHESTVA, V10, P182; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Konovalova G. V., 1998, DINOFLAGELLATES DINO; LEIGHFIELD T, 2002, P 19 INT C HARMF ALG; Margalef R., 1958, Perspectives in Marine Biology, P323; Satake Masayuki, 1997, Natural Toxins, V5, P164; Sidari L, 1998, MAR BIOL, V131, P103, DOI 10.1007/s002270050301; Sukhanova IN, 1991, PHYTOPLANKTON STUDIE, P135; THOMAS GR, 1997, IDENTIFYING MARINE P; TRUQUET P, 2001, HARMFUL ALGAL BLOOMS, P286; Vershinin A., 2000, P 9 INT C HARMF ALG	14	16	21	0	4	INTERPERIODICA	BIRMINGHAM	PO BOX 1831, BIRMINGHAM, AL 35201-1831 USA	0001-4370			OCEANOLOGY+	Oceanology	MAR-APR	2005	45	2					224	232						9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	925YZ					2025-03-11	WOS:000229091000009
J	Garrido, R; Lagos, N; Lattes, K; Abedrapo, M; Bocic, G; Cuneo, A; Chiong, H; Jensen, C; Azolas, R; Henriquez, A; Garcia, C				Garrido, R; Lagos, N; Lattes, K; Abedrapo, M; Bocic, G; Cuneo, A; Chiong, H; Jensen, C; Azolas, R; Henriquez, A; Garcia, C			Gonyautoxin: New treatment for healing acute and chronic anal fissures	DISEASES OF THE COLON & RECTUM			English	Article						anal fissure; anal sphincters; gonyautoxin; new treatment	PARALYTIC SHELLFISH TOXINS; CYANOBACTERIUM CYLINDROSPERMOPSIS-RACIBORSKII; BOTULINUM TOXIN; NITROGLYCERIN OINTMENT; GLYCERYL TRINITRATE; DOUBLE-BLIND; SAXITOXIN; THERAPY; SPHINCTEROTOMY; TETRODOTOXIN	PURPOSE: The mayor symptoms of chronic anal fissure are permanent pain, intense pain during defecation that lasts for hours, blood in the stools, and sphincter cramps. It is subsequent to formation of fibrosis infiltrate that leads to an increased anal tone with poor healing tendency. This vicious circle leads to fissure recurrence and chronicity. This study was designed to show the efficacy of gonyautoxin infiltration in healing patients with anal fissures. METHODS: Gonyautoxin is a paralyzing phytotoxin produced by dinoflagellates. Fifty recruited patients received clinical examination, including proctoscopy and questionnaire to evaluate the symptoms. Anorectal manometries were performed before and after toxin injection. Doses of 100 units of gonyautoxin in a volume of 1 ml were infiltrated into both sides of the anal fissure in the internal anal sphincter. RESULTS: Total remission of acute and chronic anal fissures were achieved within 15 and 28 days respectively. Ninety-eight percent of the patients healed before 28 days with a mean time healing of 17.6 +/- 9 days. Only one relapsed during 14 months of follow-up. Neither fecal incontinence nor other side effects were observed. All patients showed immediate sphincter relaxation. The maximum anal resting pressures recorded after two minutes decreased to 56.2 +/- 12.5 percent of baseline. CONCLUSIONS: Gonyautoxin breaks the vicious circle of pain and spasm that leads to anal fissure. This study proposes gonyautoxin anal sphincter infiltration as safe and effective alternative therapeutic approach to conservative, surgical, and botulinum toxin therapies for anal fissures.	Univ Chile, Hosp Clin, Secc Coloproctol, Dept Cirugia, Santiago, Chile; Univ Chile, Fac Med, Dept Fisiol & Biofis, Lab Bioquim Membrana, Casilla 70005, Santiago, Chile	Universidad de Chile; Universidad de Chile	Univ Chile, Fac Med, Dept Fisiol & Biofis, Lab Bioquim Membrana, Casilla 70005, Santiago, Chile.	nlagos@med.uchile.cl		Garcia Mansilla, Carlos/0000-0001-7594-2156				Andrinolo D, 2002, TOXICON, V40, P699, DOI 10.1016/S0041-0101(01)00263-X; Andrinolo D, 1999, TOXICON, V37, P447, DOI 10.1016/S0041-0101(98)00173-1; Antropoli C, 1999, DIS COLON RECTUM, V42, P1011, DOI 10.1007/BF02236693; Bacher H, 1997, DIS COLON RECTUM, V40, P840, DOI 10.1007/BF02055444; Bailey HR, 2002, DIS COLON RECTUM, V45, P1192, DOI 10.1097/01.DRC.0000027060.14159.6E; BORODIC GE, 1994, DRUG SAFETY, V11, P145, DOI 10.2165/00002018-199411030-00001; Brisinda G, 1999, NEW ENGL J MED, V341, P65, DOI 10.1056/NEJM199907083410201; CATTERALL WA, 1979, J BIOL CHEM, V254, P1379; EISENHAMMER S, 1951, S Afr Med J, V25, P486; Ezri T, 2003, DIS COLON RECTUM, V46, P805, DOI 10.1007/s10350-004-6660-8; FAROUK R, 1994, DIS COLON RECTUM, V37, P424, DOI 10.1007/BF02076185; GORFINE SR, 1995, NEW ENGL J MED, V333, P1156, DOI 10.1056/NEJM199510263331718; GUI D, 1994, LANCET, V344, P1127, DOI 10.1016/S0140-6736(94)90633-5; HARADA T, 1982, AGR BIOL CHEM TOKYO, V46, P1861, DOI 10.1080/00021369.1982.10865327; HSU TC, 1984, DIS COLON RECTUM, V27, P475, DOI 10.1007/BF02555546; JOST WH, 1995, LANCET, V345, P188, DOI 10.1016/S0140-6736(95)90190-6; Jost WH, 1997, DIS COLON RECTUM, V40, P1029, DOI 10.1007/BF02050924; JOST WH, 1994, DIS COLON RECTUM, V37, P1321, DOI 10.1007/BF02257805; JOST WH, 1993, DIS COLON RECTUM, V36, P974, DOI 10.1007/BF02050639; KAO CY, 1966, PHARMACOL REV, V18, P997; KAO CY, 1965, J PHYSIOL-LONDON, V180, P50; KHUBCHANDANI IT, 1989, BRIT J SURG, V76, P431, DOI 10.1002/bjs.1800760504; Lagos N, 1999, TOXICON, V37, P1359, DOI 10.1016/S0041-0101(99)00080-X; Lagos N, 1998, BIOL RES, V31, P375; Lagos N., 2003, COMM TOXICOL, V9, P175, DOI DOI 10.1080/08865140302429; LAGOS N, 2000, PARALYTIC SHELLFISH, P203; LODER PB, 1994, BRIT J SURG, V81, P1386, DOI 10.1002/bjs.1800810949; Lund JN, 1996, BRIT J SURG, V83, P1335, DOI 10.1002/bjs.1800831006; Lund JN, 1997, LANCET, V349, P11, DOI 10.1016/S0140-6736(96)06090-4; Maria G, 1998, ANN SURG, V228, P664, DOI 10.1097/00000658-199811000-00005; Maria G, 1998, NEW ENGL J MED, V338, P217, DOI 10.1056/NEJM199801223380402; Mínguez M, 1999, DIS COLON RECTUM, V42, P1016, DOI 10.1007/BF02236694; MOCZYDLOWSKI E, 1984, J GEN PHYSIOL, V84, P687, DOI 10.1085/jgp.84.5.687; Molica R, 2002, PHYCOLOGIA, V41, P606, DOI 10.2216/i0031-8884-41-6-606.1; NARAHASHI T, 1972, FED PROC, V31, P1124; Onodera Hideyuki, 1997, Natural Toxins, V5, P146; OSHIMA Y, 1995, J AOAC INT, V78, P528; Perrotti P, 2002, DIS COLON RECTUM, V45, P1468, DOI 10.1007/s10350-004-6452-1; SCHANTZ EJ, 1975, J AM CHEM SOC, V97, P1238, DOI 10.1021/ja00838a045; STRICHARTZ GR, 1995, TOXICON, V33, P723, DOI 10.1016/0041-0101(95)00031-G	40	40	46	0	8	LIPPINCOTT WILLIAMS & WILKINS	PHILADELPHIA	TWO COMMERCE SQ, 2001 MARKET ST, PHILADELPHIA, PA 19103 USA	0012-3706	1530-0358		DIS COLON RECTUM	Dis. Colon Rectum	FEB	2005	48	2					335	340		10.1007/s10350-004-0893-4	http://dx.doi.org/10.1007/s10350-004-0893-4			6	Gastroenterology & Hepatology; Surgery	Science Citation Index Expanded (SCI-EXPANDED)	Gastroenterology & Hepatology; Surgery	903JY	15812585				2025-03-11	WOS:000227423300024
J	Joyce, LB; Pitcher, GC; du Randt, A; Monteiro, PMS				Joyce, LB; Pitcher, GC; du Randt, A; Monteiro, PMS			Dinoflagellate cysts from surface sediments of Saldanha Bay, South Africa: an indication of the potential risk of harmful algal blooms	HARMFUL ALGAE			English	Article						dinoflagellate cysts; harmful algal bloom; Saldanha Bay; upwelling	BENGUELA UPWELLING SYSTEM; SHELLFISH MARICULTURE; POPULATION-DYNAMICS; MARINE-SEDIMENTS; PHYTOPLANKTON; DINOPHYCEAE; DRIVEN	The distribution and abundance of dinoflagellate cysts from recent coastal sediments in Saldanha Bay, was investigated, and compared to the cyst assemblages of the adjacent coastal upwelling system as reflected in the sediments off Lambert's Bay on the southern Namaqua shelf. Twenty-two cyst types were identified from three sample sites off Lambert's Bay with recorded abundances between 1726 and 1863 cysts ml(-1) wet sediment. At least 21 distinctive cyst types were identified from 32 sample sites within Saldanha Bay. Cyst abundance in Saldanha Bay was relatively low, averaging 116 cysts ml(-1) wet sediment. The region off Lambert's Bay is especially susceptible to the formation of harmful algal blooms attributed to high biomass dinoflagellate blooms. Owing to these blooms and the retentive circulation characteristics of this area, cyst formation and deposition is high. Blooms can be advected into Saldanha Bay, but their development and duration in the Bay is restricted by the system of exchange that operates between the Bay and the coastal upwelling system, in that there is a net export of surface waters from the Bay. Consequently, fewer cysts are formed and deposited within the Bay thereby reducing the likelihood of in situ bloom development initiated from the excystment of cysts. (C) 2004 Elsevier B.V. All rights reserved.	Marine & Coastal Management, ZA-8012 Cape Town, Cape Town, South Africa; Univ Cape Town, Dept Zool, ZA-7701 Rondebosch, Cape Town, South Africa; CSIR, ZA-7759 Stellenbosch, South Africa	University of Cape Town; University of Cape Town; Council for Scientific & Industrial Research (CSIR) - South Africa	Joyce, LB (通讯作者)，Marine & Coastal Management, Private Bag X2,, ZA-8012 Cape Town, Cape Town, South Africa.	ljoyce@deat.gov.za	Monteiro, Pedro/D-3767-2009					ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; BALCH WM, 1983, CAN J FISH AQUAT SCI, V40, P244, DOI 10.1139/f83-287; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; BLANCO J, 1989, Scientia Marina, V53, P797; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; Dale B., 1983, P69; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; GRASSHOFF K, 1976, METHODS SEAWATER ANA, P103; GRINDLEY J R, 1970, Fisheries Bulletin South Africa, V6, P36; GRINDLEY J R, 1968, South African Journal of Science, V64, P420; Head M.J., 1996, Palynology: Principles and Applications, P1197; HESSE KJ, 1996, BIOL ECOLOGY SHALLOW, P11; Horstman DA., 1981, FISHERIES B S AFRICA, V15, P71; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Monteiro PMS, 1998, J SHELLFISH RES, V17, P3; Monteiro PMS, 1999, ESTUAR COAST SHELF S, V49, P877, DOI 10.1006/ecss.1999.0550; Nehring S., 1993, P INT COAST C INT DI, P454; NELSON G, 1983, PROG OCEANOGR, V12, P333, DOI 10.1016/0079-6611(83)90013-7; Pitcher GC, 2000, S AFR J MARINE SCI, V22, P255, DOI 10.2989/025776100784125681; Pitcher GC, 1998, MAR ECOL PROG SER, V172, P253, DOI 10.3354/meps172253; Pitcher GC, 1998, J SHELLFISH RES, V17, P15; PROBYN TA, 2000, S AFR J MARINE SCI, V22, P199; Satake Masayuki, 1997, Natural Toxins, V5, P164; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	29	57	67	0	14	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	FEB	2005	4	2					309	318		10.1016/j.hal.2004.08.001	http://dx.doi.org/10.1016/j.hal.2004.08.001			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	899UA					2025-03-11	WOS:000227169600011
J	Coppin, A; Varré, JS; Lienard, L; Dauvillée, D; Guérardel, Y; Soyer-Gobillard, MO; Buléon, A; Ball, S; Tomavo, S				Coppin, A; Varré, JS; Lienard, L; Dauvillée, D; Guérardel, Y; Soyer-Gobillard, MO; Buléon, A; Ball, S; Tomavo, S			Evolution of plant-like crystalline storage polysaccharide in the protozoan parasite <i>Toxoplasma gondii</i> argues for a red alga ancestry	JOURNAL OF MOLECULAR EVOLUTION			English	Article						T. gondii; plant-like metabolism; amylopectin; floridean starch; evolutionary origin; glucan water dikinase; isoamylase; rhodophyte	ADENOSINE-DIPHOSPHATE GLUCOSE; DIFFERENTIAL EXPRESSION; BACTERIAL GLYCOGEN; STAGE CONVERSION; STARCH; AMYLOPECTIN; DINOFLAGELLATE; SEQUENCE; APICOPLAST; ORIGIN	Single-celled apicomplexan parasites are known to cause major diseases in humans and animals including malaria, toxoplasmosis, and coccidiosis. The presence of apicoplasts with the remnant of a plastid-like DNA argues that these parasites evolved from photosynthetic ancestors possibly related to the dinoflagellates. Toxoplasma gondii displays amylopectin-like polymers within the cytoplasm of the dormant brain cysts. Here we report a detailed structural and comparative analysis of the Toxoplasma gondii, green alga Chlamydomonas reinhardtii, and dinoflagellate Crypthecodinium cohnii storage polysaccharides. We show Toxoplasma gondii amylopectin to be similar to the semicrystalline floridean starch accumulated by red algae. Unlike green plants or algae, the nuclear DNA sequences as well as biochemical and phylogenetic analysis argue that the Toxoplasma gondii amylopectin pathway has evolved from a totally different UDP-glucose-based metabolism similar to that of the floridean starch accumulating red alga Cyanidioschyzon merolae and, to a lesser extent, to those of glycogen storing animals or fungi. In both red algae and apicomplexan parasites, isoamylase and glucan-water dikinase sequences are proposed to explain the appearance of semicrystalline starch-like polymers. Our results have built a case for the separate evolution of semicrystalline storage polysaccharides upon acquisition of photosynthesis in eukaryotes.	Univ Sci & Tech Lille Flandres Artois, CNRS, UMR 8576, Chim Biol Lab, F-59655 Villeneuve Dascq, France; Univ Sci & Tech Lille Flandres Artois, CNRS, UMR 8022, Lab Informat Fondamentale Lille, F-59655 Villeneuve Dascq, France; Univ Paris 06, CNRS, UMR 7628, Lab Arago,Observ Oceanol, F-66651 Banyuls sur Mer, France; INRA, F-44316 Nantes 03, France	Universite de Lille; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Biology (INSB); Centre National de la Recherche Scientifique (CNRS); Universite de Lille; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); INRAE	Univ Sci & Tech Lille Flandres Artois, CNRS, UMR 8576, Chim Biol Lab, F-59655 Villeneuve Dascq, France.	Stan.Tomavo@univlille1.fr	; Dauvillee, David/A-2174-2009	Guerardel, Yann/0000-0003-4967-9512; Dauvillee, David/0000-0002-0751-9193; Ball, Steven/0000-0003-1629-1650; Varre, Jean-Stephane/0000-0001-6322-0519	NIAID NIH HHS [1R01AI045806-01A1, AI05093] Funding Source: Medline	NIAID NIH HHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Allergy & Infectious Diseases (NIAID))		Ball SG, 2003, ANNU REV PLANT BIOL, V54, P207, DOI 10.1146/annurev.arplant.54.031902.134927; Ballicora MA, 2003, MICROBIOL MOL BIOL R, V67, P213, DOI 10.1128/MMBR.67.2.213-225.2003; Buleon A, 1997, PLANT PHYSIOL, V115, P949, DOI 10.1104/pp.115.3.949; Cai XM, 2003, GENE, V321, P39, DOI 10.1016/j.gene.2003.08.008; Cavalier-Smith T, 1999, J EUKARYOT MICROBIOL, V46, P347, DOI 10.1111/j.1550-7408.1999.tb04614.x; Colleoni C, 1999, PLANT PHYSIOL, V120, P993, DOI 10.1104/pp.120.4.993; Douglas SE, 1999, J MOL EVOL, V48, P236, DOI 10.1007/PL00006462; Dzierszinski F, 1999, J BIOL CHEM, V274, P24888, DOI 10.1074/jbc.274.35.24888; Dzierszinski F, 2001, J MOL BIOL, V309, P1017, DOI 10.1006/jmbi.2001.4730; Fast NM, 2001, MOL BIOL EVOL, V18, P418, DOI 10.1093/oxfordjournals.molbev.a003818; Funes S, 2002, SCIENCE, V298, P2155, DOI 10.1126/science.1076003; GREENBERG E, 1964, J BIOL CHEM, V239, P4314; Harris JR, 2004, PARASITOLOGY, V128, P269, DOI 10.1017/S003118200300458X; Henrissat B, 2002, TRENDS GENET, V18, P437, DOI 10.1016/S0168-9525(02)02734-8; KARKHANIS YD, 1993, J EUKARYOT MICROBIOL, V40, P594, DOI 10.1111/j.1550-7408.1993.tb06113.x; Kohler S, 1997, SCIENCE, V275, P1485, DOI 10.1126/science.275.5305.1485; LIBESSART N, 1995, PLANT CELL, V7, P1117; LUFT BJ, 1988, J INFECT DIS, V157, P1, DOI 10.1093/infdis/157.1.1; LUFT BJ, 1992, CLIN INFECT DIS, V15, P211, DOI 10.1093/clinids/15.2.211; Maréchal E, 2001, TRENDS PLANT SCI, V6, P200, DOI 10.1016/S1360-1385(01)01921-5; Matsuzaki M, 2004, NATURE, V428, P653, DOI 10.1038/nature02398; McFadden GI, 1996, NATURE, V381, P482, DOI 10.1038/381482a0; Nyvall P, 1999, PLANTA, V209, P143, DOI 10.1007/s004250050616; PERRET E, 1993, J CELL SCI, V104, P639; Ral JP, 2004, PLANT PHYSIOL, V136, P3333, DOI 10.1104/pp.104.044131; RECONDO E, 1961, BIOCHEM BIOPH RES CO, V6, P85, DOI 10.1016/0006-291X(61)90389-8; Ritte G, 2002, P NATL ACAD SCI USA, V99, P7166, DOI 10.1073/pnas.062053099; RYLEY JF, 1969, J PARASITOL, V55, P839, DOI 10.2307/3277227; Seeber F, 1997, PARASITOL RES, V83, P309, DOI 10.1007/s004360050254; THOMPSON JD, 1994, NUCLEIC ACIDS RES, V22, P4673, DOI 10.1093/nar/22.22.4673; Tomavo S, 2001, INT J PARASITOL, V31, P1023, DOI 10.1016/S0020-7519(01)00193-X; Viola R, 2001, P ROY SOC B-BIOL SCI, V268, P1417, DOI 10.1098/rspb.2001.1644; Waller RF, 2003, SCIENCE, V301; Wilson RJM, 1996, J MOL BIOL, V261, P155, DOI 10.1006/jmbi.1996.0449; Zhang ZD, 1999, NATURE, V400, P155, DOI 10.1038/22099	35	87	103	0	24	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	0022-2844	1432-1432		J MOL EVOL	J. Mol. Evol.	FEB	2005	60	2					257	267		10.1007/s00239-004-0185-6	http://dx.doi.org/10.1007/s00239-004-0185-6			11	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Evolutionary Biology; Genetics & Heredity	898II	15785854				2025-03-11	WOS:000227070100012
J	Figueroa, RI; Bravo, I				Figueroa, RI; Bravo, I			A study of the sexual reproduction and determination of mating type of <i>Gymnodinium nolleri</i> (Dinophyceae) in culture	JOURNAL OF PHYCOLOGY			English	Article						Dinophyceae; encystment; gametes; Gymnodinium nolleri; life cycle; reproduction	LIFE-CYCLE; GYRODINIUM-UNCATENUM; GONYAULAX-TAMARENSIS; CATENATUM GRAHAM; DINOFLAGELLATE; CYST; TEMPERATURE; AUSTRALIA; SEDIMENTS; TASMANIA	Sexual reproduction of Gymnodinium nolleri (Ellegaard & Moestrup 1999) was studied by intercrossing experiments in all combinations of six clonal strains and backcrossing of five clonal F1 offspring. The results indicated that the conjugation of G. nolleri responded to the existence of more than two sexual types (complex heterothallism) and that compatibility between progeny of one cyst (inbreeding) was the rule. Sexual fusion, planozygote formation and development, cyst formation, and germination and planomeiocyte division were followed using time-lapse photography. This study revealed many similarities between the sexual stages and life cycle pattern of G. nolleri and the related G. catenatum and the existence under culture conditions of an alternative cycle between vegetative cells and zygotes without a hypnozygote stage. The fate of zygotes, division or encystment, was influenced by the nutritional status of the external medium. The division of G. nolleri planozygotes was promoted by high levels of external nutrients, whereas the maximum percentage of encystment was recorded when phosphates were reduced in the isolation medium. The division of zygotes might be different from both vegetative and planomeiocyte division because it resulted in two-cell chains with the cells not oriented in parallel.	Inst Oceanog Vigo, Vigo 36200, Spain	Spanish Institute of Oceanography	Inst Oceanog Vigo, Vigo 36200, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015	Figueroa, Rosa/0000-0001-9944-7993; Bravo, Isabel/0000-0003-3764-745X				ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; Coats DW, 2002, J PHYCOL, V38, P417, DOI 10.1046/j.1529-8817.2002.03832.x; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; DALE B, 2000, 9 INT C HARMF ALG BL; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; FRAGA S, 1988, ESTUAR COAST SHELF S, V27, P349, DOI 10.1016/0272-7714(88)90093-5; Goodenough U.W., 1985, MBL (Marine Biology Laboratory) Lectures in Biology, V7, P123; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; MATSUOKA K, 1994, BOT MAR, V37, P495, DOI 10.1515/botm.1994.37.6.495; MOITA MT, 1993, DEV MAR BIO, V3, P299; NEHRING S, 1995, J PLANKTON RES, V17, P85, DOI 10.1093/plankt/17.1.85; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1989, INT REV CYTOL, V114, P249; Pitcher G., 1995, P657; UCHIDA T, 1991, NIPPON SUISAN GAKK, V57, P1215, DOI 10.2331/suisan.57.1215; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Wall D., 1971, Geoscience Man, V3, P1	32	40	41	1	10	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2005	41	1					74	83		10.1111/j.1529-8817.2005.04045.x	http://dx.doi.org/10.1111/j.1529-8817.2005.04045.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	894KT		Green Submitted			2025-03-11	WOS:000226791300009
J	Jiménez-Moreno, G; Rodríguez-Tovar, FJ; Pardo-Igúzquiza, E; Fauquette, S; Suc, JP; Müller, P				Jiménez-Moreno, G; Rodríguez-Tovar, FJ; Pardo-Igúzquiza, E; Fauquette, S; Suc, JP; Müller, P			High-resolution palynological analysis in late early-middle Miocene core from the Pannonian Basin, Hungary:: climatic changes, astronomical forcing and eustatic fluctuations in the Central Paratethys	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						palynology; climatic quantification; cyclostratigraphy; eustatic changes; early middle Miocene; Pannonian Basin	ANTARCTIC ICE-SHEET; MARINE-SEDIMENTS; OLIGOCENE/MIOCENE BOUNDARY; MEDITERRANEAN PLIOCENE; DINOFLAGELLATE CYSTS; ADJACENT SEAS; POLLEN DATA; CALIBRATION; FREQUENCIES; NORTHERN	High-resolution palynological analysis in the Karpatian-Sarmatian (late early-middle Miocene) interval of the borehole Tengelic 2 (Hungary) reveals the existence of a forest organized in altitudinal belts developed in a subtropical-warm temperate humid climate, reflecting the so-called Miocene climatic optimum. Pollen changes from the late early Miocene to the middle Miocene are related to climatic variations. Values of mean annual temperature (Ta) between 18 and 20 degreesC and mean annual precipitation (Pa) between 1200 and 1400 mm have been estimated ("climatic amplitude method") for the Badenian. Decreasing during Late Badenian and Sarmatian, Ta and Pa about 16 degreesC and 1100 mm, have been interpreted as a climatic cooling correlated with the "Monterey cooling event" and related to the development of the East Antarctic Ice Sheet (EAIS). Alternation in pollen taxa (thermophilous vs. altitudinal elements) reflects the astronomical forcing on temperature and precipitation and then on vegetation, where obliquity and eccentricity cycles dominated. Eustatic changes determine Pinus and Pinaceae and dinocyst variations. (C) 2004 Elsevier B.V. All rights reserved.	Univ Granada, Dept Estratigrafia & Paleontol, Granada 18002, Spain; Univ Lyon 1, CNRS, UMR 5125, Lab Paleoenvironm & Paleobiosphere, F-69622 Villeurbanne, France; Univ Granada, Dept Geodinam, Granada 18002, Spain; Univ Montpellier 2, CNRS, UMR 5554, Inst Sci Evolut Montpellier,Equipe Paleoenvironm, F-34095 Montpellier, France; Geol Inst Hungary, Foldtani Intezet, H-1143 Budapest, Hungary	University of Granada; Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; University of Granada; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; HUN-REN; HUN-REN Research Centre for Astronomy & Earth Sciences; Institute for Geological & Geochemical Research - HAS		gonzaloj@ugr.es	Fauquette, Severine/M-3686-2019; Rodríguez-Tovar, Francisco/AAA-9041-2020; Jimenez-Moreno, Gonzalo/K-6753-2017; Pardo-Iguzquiza, Eulogio/A-6324-2013	Fauquette, Severine/0000-0003-0516-7734; Jimenez-Moreno, Gonzalo/0000-0001-7185-8686; Rodriguez-Tovar, Francisco/0000-0002-1400-2715; Pardo-Iguzquiza, Eulogio/0000-0002-3865-8639				Andreansky G., 1959, FLORA SARMATISCHEN S; [Anonymous], 1990, European Neogene Mammal Chronology, DOI DOI 10.1007/978-1-4899-2513-8_2; [Anonymous], MEDEDELINGEN GEOLOGI; [Anonymous], 1996, HIST MODERN FLORA CH; Aziz HA, 2000, EARTH PLANET SC LETT, V177, P9, DOI 10.1016/S0012-821X(00)00035-2; Báldi K, 2002, INT J EARTH SCI, V91, P490, DOI 10.1007/s005310100226; Barron Eduardo, 1999, Boletin de la Real Sociedad Espanola de Historia Natural Seccion Geologica, V95, P67; BEAUDOUIN C, 2003, THESIS U C BERNARD L, V1; BERGER A, 1992, SCIENCE, V255, P560, DOI 10.1126/science.255.5044.560; BERGER A, 1989, NATURE, V342, P133, DOI 10.1038/342133b0; BERGER AL, 1977, NATURE, V269, P44, DOI 10.1038/269044a0; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; Bertini A., 1994, HIST BIOL, V9, P3, DOI DOI 10.1080/10292389409380483; Bessedik M., 1985, THESIS U SCI TECHNIQ; BOHNHAVAS M, 1982, ANN GEOL PUBL HUNG, V65, P200; Cambon G, 1997, GRANA, V36, P105, DOI 10.1080/00173139709362596; COUR P, 1974, Pollen et Spores, V16, P103; Drivaliari A., 1993, THESIS U MONTPELLIER; Fauquette S, 1998, GEOBIOS-LYON, V31, P151, DOI 10.1016/S0016-6995(98)80035-1; Fauquette S, 1998, PALAEOGEOGR PALAEOCL, V144, P183, DOI 10.1016/S0031-0182(98)00083-2; Fauquette S, 2003, BOREAS, V32, P361, DOI 10.1080/03009480301825; Fauquette S, 1999, PALAEOGEOGR PALAEOCL, V152, P15, DOI 10.1016/S0031-0182(99)00031-0; FAUQUETTE S, 2004, IN PRESS PALAEOGEOGR; Flower B.P.J.C., 1997, P ODP SCI RESULTS, V154, P433, DOI [10.2973/odp, DOI 10.2973/ODP]; FLOWER BP, 1994, PALAEOGEOGR PALAEOCL, V108, P537, DOI 10.1016/0031-0182(94)90251-8; Hall IR, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2002PA000817; HALMAI J, 1982, ANN I GEOL PUBL HUNG, V65, P93; HAMOR G, 1995, MIOCENE PALAEOGEOGRA; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HEUSSER LE, 1988, MAR GEOL, V80, P131, DOI 10.1016/0025-3227(88)90076-X; HOLBOURN A, 2003, GEOPH RES ABSTR, V5, P6151; Hooghiemstra H., 1986, Meteor"Forschungsergeb. 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JAN 20	2005	216	1-2					73	97		10.1016/j.palaeo.2004.10.007	http://dx.doi.org/10.1016/j.palaeo.2004.10.007			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	887OH					2025-03-11	WOS:000226314900004
J	Mac Donagh, ME; Casco, MA; Claps, MC				Mac Donagh, ME; Casco, MA; Claps, MC			Colonization of a neotropical reservoir (Cordoba, Argentina) by <i>Ceratium hirundinella</i> (O. F. Muller) Bergh	ANNALES DE LIMNOLOGIE-INTERNATIONAL JOURNAL OF LIMNOLOGY			English	Article						Ceratium hirundinella; first record; phytoplankton dynamic; Rio Tercero Reservoir; rotifer predator	LAKE; MIGRATION; DYNAMICS	Blooms of Ceratium hirundinella (O. F. Muller) Bergh. have been detected in different water bodies in the Neotropical Region since 1990. The colonization began in Southern lakes, and during the last decade the dinoflagellate arrived and bloomed in subtropical reservoirs. fit this context the colonization of C. hirundinella and its population development have been analyzed from its first record in the Rio Tercero Reservoir (February 1999 to February 2001). Phytoplankton and physicochemical samples were obtained from three sampling stations at the Reservoir, one in the outlet of the water cooling channel of the nuclear power plant, and one in the nearest tributary (Quillinzo River). Two blooms of C. hirundinella were detected during the warm seasons with temperatures higher than 18 degrees C, and pH ranging between 8.5 and 8.9. Environmental conditions such as certain light intensity range and percentage of dissolved oxygen mentioned as favorable for Ceratium development were always recorded in Rio Tercero Reservoir. Cysts were observed in spring and summer months. Another dinoflagellate (Peridinium gatunense Nygaard) bloomed in previous Summer in this water body but its population density decreased during the invasive phase of colonization of C hirundinella. Asplanchna girodi, became the dominant zooplankter after the first bloom of C hirundinella. We believe that the presence of this dinoflagellate in the Neotropical Region Could be a regional phenomenon associated with some dispersal mechanisms and favorable local conditions for its proliferation like those recorded in the Rio Tercero Reservoir.	UNLP, Museo La Plata, RA-1900 La Plata, Argentina; UNLP, CONICET, ILPLA, RA-1988 Florencio Varela, Argentina; Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina	National University of La Plata; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of La Plata; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	UNLP, Museo La Plata, Paseo Bosque S-N, RA-1900 La Plata, Argentina.	mmacdonagh@fcnym.unlp.edu.au		Claps, Maria/0000-0002-7459-3238				Abakumov V. A., 1983, GUIDE METHODS HYDROB; [Anonymous], 1976, LIMNOLOGIA EMBALSES; ARNDT H, 1993, HYDROBIOLOGIA, V255, P231, DOI 10.1007/BF00025844; BUSTAMANTE MA, 2002, 4 INT C RES LIMN WAT, P58; Casco MA, 2002, INT VER THEOR ANGEW, V28, P1027; CONTI ALR, 1999, ACT C ARG GRAND PRES, P493; DOTTNE-LINDGREN A, 1975, Internationale Revue der Gesamten Hydrobiologie, V60, P115, DOI 10.1002/iroh.19750600105; GIRBAL A, 2000, SEM INT ID CONTR ALG; GUERRERO J., 1997, HARMFUL ALGAE NEWS, V16, P3; GUERRERO JM, 1998, SEM INT ID CONTR OL; HARRIS GP, 1979, FRESHWATER BIOL, V9, P413, DOI 10.1111/j.1365-2427.1979.tb01526.x; HEANEY SI, 1980, J ECOL, V68, P75, DOI 10.2307/2259245; Hillebrand H, 1999, J PHYCOL, V35, P403, DOI 10.1046/j.1529-8817.1999.3520403.x; JAMES WF, 1992, CAN J FISH AQUAT SCI, V49, P694, DOI 10.1139/f92-078; KAWABATA Z, 1988, HYDROBIOLOGIA, V169, P319, DOI 10.1007/BF00007555; LINDSTROM K, 1992, NORD J BOT, V12, P541, DOI 10.1111/j.1756-1051.1992.tb01833.x; Margalef R., 1983, Limnologia; MARINELARENA A, 1998, ESTUDIO LIMNOLOGICO; PADISAK J, 1985, FRESHWATER BIOL, V15, P43, DOI 10.1111/j.1365-2427.1985.tb00695.x; Pérez-Martínez C, 2002, J PLANKTON RES, V24, P89, DOI 10.1093/plankt/24.2.89; Pérez-Martínez C, 2001, HYDROBIOLOGIA, V452, P101, DOI 10.1023/A:1011928027819; Pollingher U., 1988, P134; POLLINGHER U, 1993, AQUAT SCI, V55, P10, DOI 10.1007/BF00877255; PROSPERI CH, 2000, SEM INT ID CONTR ALG; RAMON G, 1987, ACT 6 S NAC BOT CRIP, P109; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; RENGEFORS K, 1997, ACTA U UPSALIENSIS; Reynolds C.S., 1988, P388; Reynolds C.S., 1984, ECOLOGY FRESHWATER P; RODRIGUEZ MI, 2000, SEM INT ID CONTR ALG; SILVERIO MJ, 2001, 5 C LAT EC; SOTO D, 1999, 5 C LAT FIC, P23; Villalobos L, 2003, REV CHIL HIST NAT, V76, P563	34	24	31	3	19	EDP SCIENCES S A	LES ULIS CEDEX A	17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A, FRANCE	0003-4088	2100-000X		ANN LIMNOL-INT J LIM	Ann. Limnol.-Int. J. Limnol.		2005	41	4					291	299		10.1051/limn/2005020	http://dx.doi.org/10.1051/limn/2005020			9	Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	998LP		Green Published, Bronze			2025-03-11	WOS:000234320500007
J	Giraud, F; Courtinat, B; Garcia, JP; Baudin, F; Guillocheau, F; Dromart, G; Atrops, F; Collete, C				Giraud, F; Courtinat, B; Garcia, JP; Baudin, F; Guillocheau, F; Dromart, G; Atrops, F; Collete, C			Palynofacies and calcareous nannofossils in the Upper Kimmeridgian, southeastern Paris basin (France)	BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE			English	Article						palynofacies; calcareous nannofossils; Upper Kimmeridgian; Paris basin; marine shallow-water deposits; palaeoenvironments	DEPOSITIONAL SEQUENCES; DINOFLAGELLATE CYSTS; VOCONTIAN BASIN; ORGANIC FACIES; BIOSTRATIGRAPHY; NANNOPLANKTON	The Upper Kimmeridgian Members "Calcaires blancs superieurs" and the "Marnes a exogyres superieures" of the southeastern Paris basin were investigated for their palynofacies and calcareous nannofossils. These members display alternating limestone-marl lithotypes and represent shallow marine palaeoenvironments. The lower carbonate member is interpreted as a proximal palaeoenvironment (palaeobathymetry = 5 to 10 m), where storm and swell deposits were prevalent and the salinity was occasionally weak. The relative richness of brown phytoclasts in this part is favoured by good preservation related to restricted conditions, These conditions would explain the dominance of the nannofossil Cyclagelosphaera margerelii in the nannofossil assemblages. The palynological data as those of the nannofossil assemblages show variations in the shift from carbonate member to marly member. The dominance of brown phytoclasts over black phytoclasts, the presence of amorphous organic matter (AOM), and the highest abundance and diversity observed within the nannofossil assemblages suggest that the maximum of distality occurred during this transition, at the basal part of the Marries a Exogyres superieures. The upper part of the section (marly member) characterized by storm deposits and storm-coquina beds is deeper (palaeobathymetry probably between 10 and 40 m depth) than the lower part. Oxidizing depositional conditions prevailed and explained the abundance of black particles found in this upper part. while proximate cysts and elevated non-placolith coccolith abundances indicate that relationships with the open sea were probably more significant compared to the lower part. Towards the top of the section, recurrences of restricted conditions are reflected by relatively elevated amounts of AOM and the abundance peak of the nannofossil Biscutum ellipticum. This study shows that micropalaeontological signals can be well recorded in vast lagunal domains. We speculate that salinity, nutrient supply, and oxygenation of the waters control microfossil associations. In shallow environments, these parameters are particularly fluctuating, especially when freshwater dilutes marine waters in surface, on the occasion of rainy periods or of intense arrival of continental waters.	Univ Lyon 1, Unite Format & Rech Sci Terre, CNRS, UMR 5125, F-69622 Villeurbanne, France; Univ Bourgogne, Ctr Sci Terre, CNRS, UMR 5561, F-21000 Dijon, France; Univ Paris 06, UMR 5143, Dept Geol Sedimentaire, F-75252 Paris 05, France; Univ Rennes 1, Geosci Rennes, CNRS, UMR 6118, F-35042 Rennes, France; Assoc Geol Auboise, F-10300 St Savine, France	Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; Universite de Bourgogne; Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Rennes	Univ Lyon 1, Unite Format & Rech Sci Terre, CNRS, UMR 5125, F-69622 Villeurbanne, France.	bernard.courtinat@uni-lyon1.fr	Baudin, Francois/ITU-7485-2023; Giraud, Fabienne/B-4793-2012	Giraud, Fabienne/0000-0002-4732-4737; Baudin, Francois/0000-0003-3180-459X				[Anonymous], 1974, FOSSIL LIVING DINOFL; [Anonymous], 1985, LECT NOTES EARTH SCI; [Anonymous], 1994, SEDIMENTATION ORGANI; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bernier P., 1979, DOCUM LAB G OL FS LY, V75, P95; Bown Paul R., 1997, Journal of Nannoplankton Research, V19, P21; BOWN PR, 1988, NEWSL STRATIGR, V20, P91; BOWN PR, 1992, P OCEAN DRILL PROJ S, V123, P269; BOWN PR, 1998, BRIT MICROPAL SOC SE; BRALOWER TJ, 1989, MAR MICROPALEONTOL, V14, P153, DOI 10.1016/0377-8398(89)90035-2; Busson G., 1992, Revue de Paleobiologie, V11, P255; Claps M., 1995, Memorie di Scienze Geologiche Padova, V47, P179; Cobianchi M, 2001, PALAEOGEOGR PALAEOCL, V169, P219, DOI 10.1016/S0031-0182(01)00217-6; Colombié C, 2003, GEOBIOS-LYON, V36, P675, DOI 10.1016/j.geobios.2003.03.004; COOPER MKE, 1989, BR MICROPAL, P223; COURTINAT B, 1991, GEOBIOS-LYON, V24, P649, DOI 10.1016/S0016-6995(06)80293-7; COURTINAT B, 2002, REV MICROPALEONTOL, V45, P37; Courtinat Bernard, 2003, Revue de Micropaleontologie, V46, P11, DOI 10.1016/S0035-1598(03)00003-5; CROS L., 2001, Ph.D. thesis; Enay R, 2000, B SOC GEOL FR, V171, P673, DOI 10.2113/171.6.673; Fauconnier D, 1996, MAR PETROL GEOL, V13, P707, DOI 10.1016/0264-8172(95)00024-0; FRANK MC, 1995, J GEOL SOC LONDON, V152, P41, DOI 10.1144/gsjgs.152.1.0041; Guillocheau F, 2000, GEODIN ACTA, V13, P189, DOI 10.1016/S0985-3111(00)00118-2; GUILLOCHEAU F, 1991, B CENT RECH EXPL, V15, P383; HANTZPERGUE P, 1993, PALEOVOX, P31; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hill M.E. 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Soc. Geol. Fr.		2005	176	5					457	466		10.2113/176.5.457	http://dx.doi.org/10.2113/176.5.457			10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	015UW					2025-03-11	WOS:000235577700005
S	O'Keefe, JMK; Sancay, RH; Raymond, AL; Yancey, TE		Warwick, PD		O'Keefe, Jennifer M. K.; Sancay, Recep H.; Raymond, Anne L.; Yancey, Thomas E.			A comparison of late Paleocene and late Eocene lignite depositional systems using palynology, upper Wilcox and upper Jackson Groups, east-central Texas	COAL SYSTEMS ANALYSIS	Geological Society of America Special Papers		English	Article; Book Chapter						Wilcox Group; Jackson Group; Tertiary; lignite; coal; palynology; paleoecology; paleoclimatology; environmental change		Lignites of the Wilcox and Jackson Groups in east Texas were deposited in marginal marine depositional complexes during times of cyclic sediment deposition. Thick upper Wilcox lignites occur within cycles of estuarine strata. Thin upper Jackson lignites occur within strandplain/shoreface deposits. Palynology of the lignites and enclosing sediments reveal two distinct climatic regimes: warm and equable during Wilcox deposition versus variable warm-cool during Jackson deposition. Four palynologic assemblages have been recovered from lignite-bearing upper Wilcox strata, and six palynologic assemblages have been recovered from upper Jackson non-marine and marine strata. Wilcox lignites contain assemblages indicating change from closed-canopy freshwater swamps populated by a community dominated by chestnut and walnut family trees, to open-canopy swamps that add ferns to the community, to a community of palms and ferns that extends into the overlying marine-influenced mudstones, and capped by marine siliciclastics containing an assemblage of dinoflagellates and transported cypress pollen and fern spores. The Jackson assemblages indicate a transition from a palm-dominated community in the sands and silts to a fern marsh community in the silty mudstones and base of the lignites, to closed-canopy freshwater communities in the lignite populated by a tropical walnut and swamp tupelo, to an open-canopy community populated where ferns replace the tupelo, capped by a swamp community dominated by a chestnutlike tree and leather-wood, especially in lignites overlain by marine sediments; marine sediments contain an assemblage of dinoflagellates and transported pollen. The dominant tree in Wilcox swamp communities is chestnut, whereas Jackson swamps are dominated by a tropical walnut; ferns are common in both settings. The dominance of cypress in the estuarine-marine transition sediments of the Wilcox suggests an open-water transition between peat swamp and marginal marine environments. The dominance of the chestnutlike tree in the swamp-marine transition of the Jackson indicates a sharp boundary between peat swamp and marine environments.	[O'Keefe, Jennifer M. K.] Morehead State Univ, Dept Phys Sci, Morehead, KY 40351 USA; [Sancay, Recep H.] Turkish Petr Corp, Ankara, Turkey; [Raymond, Anne L.; Yancey, Thomas E.] Texas A&M Univ, Dept Geol & Geophys, College Stn, TX 77843 USA	Morehead State University; Turkish Petroleum Corporation (TPAO); Ministry of Energy & Natural Resources - Turkey; Texas A&M University System; Texas A&M University College Station	O'Keefe, JMK (通讯作者)，Morehead State Univ, Dept Phys Sci, Morehead, KY 40351 USA.							AYERS WB, 1987, GULF COAST LIGNITE G, P69; BENNINGHOFF W. S., 1962, POLLEN ET SPORES, V4, P332; Berggren WA, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P1; Berggren WilliamA., 1992, ECOENCE OLIGOCENE CL, P1; BREYER JA, 1986, J SEDIMENT PETROL, V56, P510; BREYER JA, 1987, GULF COAST LIGNITE G, P33; DEMCHUCK TD, 1992, THESIS U CALGARY CAL; ELSIK WC, 1968, U TEXAS AUSTIN BUREA, V90, P21; ENGLISH RE, 1988, THESIS SO ILLINOIS U; Galloway WE, 2000, AAPG BULL, V84, P1743; Gennett J.A., 1986, GULF COAST ASS GEOL, V36, P449; GENNETT JA, 1993, THESIS TEXAS A M U C; GRAHAM A, 1995, BIOTROPICA, V27, P20, DOI 10.2307/2388899; Graham A., 1999, Late Cretaceous and Cenozoic History of North American Vegetation; GUILLEMETTE RN, 1996, AAPG BULL, V80, P1503; Jones JG, 1991, GULF COAST ASS GEOLO, V41, P348; Klein G.D., 1998, SEDIMENT GEOL, P5; KLEIN JM, 2000, THESIS TEXAS A M U C; MAY AG, 1994, THESIS TEXAS A M U C; MUKHOPADHYAY PK, 1989, 188 U TEX AUST BUR E; MUKHOPADHYAY PK, 1987, GULF COAST LIGNITE G, P140; Nichols D.J., 1971, Geoscience Man, V3, P37; NICHOLS DJ, 1970, THESIS PENNSYLVANIA; Oboh FE, 1996, REV PALAEOBOT PALYNO, V91, P23, DOI 10.1016/0034-6667(95)00075-5; Raymond A, 1997, INT J COAL GEOL, V34, P195, DOI 10.1016/S0166-5162(97)00023-2; RICH F, 2002, REPORT PALYNOLOGICAL; SAMS RH, 1990, SEQUENCE STRATIGRAPH, V11, P307; SANCAY RH, 2000, THESIS TEXAS A M U C; WARWICK PD, 2000, 00143 US GEOL SURV; Yancey T.E., 1991, GULF COAST ASS GEOL; Yancey TE, 1997, INT J COAL GEOL, V34, P261, DOI 10.1016/S0166-5162(97)00025-6; Yancey TE, 2002, GREENHOUSE ICEHOUSE, P252	32	4	5	0	2	GEOLOGICAL SOC AMER INC	BOULDER	3300 PENROSE PL, PO BOX 9140, BOULDER, CO 80301 USA	0072-1077		978-0-8137-2387-7	GEOL SOC AM SPEC PAP			2005	387						59	71		10.1130/0-8137-2387-6.59	http://dx.doi.org/10.1130/0-8137-2387-6.59			13	Geochemistry & Geophysics; Geology	Book Citation Index– Science (BKCI-S)	Geochemistry & Geophysics; Geology	BLX62					2025-03-11	WOS:000271309200005
J	Dejax, J; Masure, E				Dejax, J; Masure, E			Palynological analysis of an amber-bearing, lignitic clay bed from the Uppermost Albian of Archingeay (Charente-Maritime, France).	COMPTES RENDUS PALEVOL			French	Article						palynology; dinoflagellates; palaeoenvironment; uppermost Albian; amber	CENOMANIENNE; VENDEE	Palynological analysis of an amber-bearing, lignitic clay bed from the Uppermost Albian of Archingeay (Charente-Maritime, France). An amber-bearing lignitic clay bed from Archingeay village (Charente-Maritime, France) yielded a well-preserved, rich and variegated palynoflora, whose origin is mixed between land plants and marine microflora. Its detailed analysis, through light and scanning electron microscopes, led to fulfil its inventory, then to propose a palaeoenvironmental reconstruction and to draw the palaeoclimate which prevailed over the region: an estuarine area under a rather humid, temperate to hot climate. A variety of ferns and resin-producing conifers grew near the shore-side and in the inward land; the angiosper-mous affinity is worthy of interest, although rather little diversified. Filamentous 'alge' grew in the rivers. The marine micro-flora, moderately diversified, comprises chitinous foraminifer linings. acritarchs and dinoflagellate cysts, arnong, which the Uppermost Albian guide taxa are present: the predoniniance of neritic species remains somewhat moderate. To cite this article: J. Dejax, E. Masure, C. R. Palevol 4 (2005). (C) 2005 Academie des sciences. POH par Elsevier SAS. Tons droits reserves.	Museum Natl Hist Nat, UMR Paleobiodivers & Paleoenvironm 5143, USM 02 03, Dept Hist Terre, F-75231 Paris 05, France; Univ Paris 06, UMR Paleobiodivers & Paleoenvironm 5143, CEPAGE, Lab Micropaleontol, F-75252 Paris, France	Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite	Dejax, J (通讯作者)，Museum Natl Hist Nat, UMR Paleobiodivers & Paleoenvironm 5143, USM 02 03, Dept Hist Terre, Case Postale 38,57,Rue Cuvier, F-75231 Paris 05, France.	dejax@mnhn.fr						ARNAUD H, 1977, MEM SOC GEOL FRANCE; Azema C., 1972, PALEOBIOLOGIE CONTIN, V3, P1; AZEMA C, 1979, 104 C NAT SOC SAV BO, V1, P197; AZENA C, 1971, REV PALAEOBOT PALYNO, V11, P267; Brenner G.J., 1976, ORIGIN EARLY EVOLUTI, P23; CHATEAUNEUF JJ, 1972, NOTICE CARTE ROCHEFO; COQUAND H, 1856, B SOC GEOL FRANCE, V14, P55; Costa L. I., 1992, BRIT MICROPALAEONTOL, P99; Crie L, 1890, ANN SOC SCI NATURELL, V26, P231; d'Archiac EJAD, 1837, Memoires de la Societe geologique de France, V2, P157; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; DEAK M.H., 1967, R MICROPALEONTOL, V10, P69; Dercourt J., 1993, ATLAS TETHYS PALAEOE; DETTMANN M.E., 1963, P ROY SOC VICTORIA, V77, P1; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; DURAND S, 1963, CR HEBD ACAD SCI, V257, P1492; DURAND S, 1958, CR HEBD ACAD SCI, V247, P684; FAUCONNIER D, 1976, CARTE GEOLOGIQUE FRA, V30; FOUCHER J.C., 1983, CAHIERS MICROPAL ONT, V4, P23; Foucher J.C., 1998, MESOZOIC CENOZOIC SE; Friis EM, 1999, ANN MO BOT GARD, V86, P259, DOI 10.2307/2666179; Gomez Bernard, 2004, Annales de Paleontologie, V90, P147, DOI 10.1016/j.annpal.2004.03.003; HASENBOEHLER B., 1981, THESIS U P M CURIE P, V6; Herngreen GF., 1996, Palynology: Principles and Applications, V3, P1157; HLUSTIK A, 1976, Vestnik Ustredniho Ustavu Geologickeho, V51, P37; HOCHULI PA, 1981, REV PALAEOBOT PALYNO, V35, P337, DOI 10.1016/0034-6667(81)90116-0; Lantz J., 1958, R MICROPALEONTOL, V1, P33; Manes W., 1853, DESCRIPTION PHYS GEO; MEUNIER A, 1999, AQUITAINE BASIN FRAN, V170, P873; Moreau P., 1993, THESIS U POITIERS; Moreau P., 1978, GEOLOGIE MEDITERRANE, V5, P125; MOREAU P, 1977, B SOC GEOLOGIQUE FRA, V19, P281; MoREAu P, 1996, GEOL FR, V1, P3; Néraudeau D, 2002, GEOBIOS-LYON, V35, P233, DOI 10.1016/S0016-6995(02)00024-4; Neraudeau D, 1997, B SOC GEOL FR, V168, P51; PERRICHOT V, 2003, THESIS U RENNES, V1; Pons D., 1979, SCIENCES, V1, P209; Pons D., 1996, Bulletin des Centres de Recherches ExplorationProduction ElfAquitaine, V16, P383; Potonie R., 1970, Beih. Geologisches Jahrbuch., V87, P1; POTONIE R., 1954, GEOL JAHRB, V69, P111; TERS M, 1959, SCIENCES, P675; VIDET B, 2005, OSTREIDES FACIES LIG, V4; VIDET B, 2004, THESIS U RENNES, V108; Williams G.L., 1985, P847; WILLIAMS GL, 1998, CONTRIB SER, V34, P817	45	40	42	0	3	EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS	23 RUE LINOIS, 75724 PARIS, FRANCE	1631-0683			CR PALEVOL	C. R. Palevol	JAN-FEB	2005	4	1-2					53	65		10.1016/j.crpv.2004.12.002	http://dx.doi.org/10.1016/j.crpv.2004.12.002			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	901OD					2025-03-11	WOS:000227290900007
J	Poulton, NJ; Keafer, BA; Anderson, DM				Poulton, NJ; Keafer, BA; Anderson, DM			Toxin variability in natural populations of <i>Alexandrium fundyense</i> in Casco Bay, Maine -: evidence of nitrogen limitation	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium; environmental factors; saxitoxin; Gulf of Maine; paralytic shellfish poisoning; nitrogen limitation	DINOFLAGELLATE GONYAULAX-TAMARENSIS; PROTOGONYAULAX-TAMARENSIS; SHELLFISH TOXINS; SPECIES COMPLEX; CYST FORMATION; PHOSPHORUS; GROWTH; DINOPHYCEAE; TEMPERATURE; CATENELLA	The dinoflagellate Alexandrium fundyense is a common, recurring harmful algal bloom (HAB) species in the Gulf of Maine. To date, most physiological measurements of phytoplankton in the field provide data on the entire community, yet efforts to obtain species-specific data are particularly important for understanding the ecological and physiological dynamics of HAB species, such as, Alexandrium. Alexandrium spp., do not usually dominate the planktonic community in the Gulf of Maine, but are of great interest due to the potent toxins produced. In order to determine the nutritional status of Alexandrium spp. in natural populations, indicators of nutrient deprivation need to be identified that are specific to that one species. To date, the saxitoxin content of A. fundyense is known to vary under different environmental conditions such as nitrogen and phosphorous limitation. However, in batch culture the composition of the toxin (the relative amounts of each saxitoxin derivative per cell) appears to be a stable quantity and thus is sometimes viewed as a biochemical marker of individual strains. In more recent studies, toxin composition has been shown to vary during progressive N- and P-limitation, once the cells are given time to achieve steady state in semi-continuous, nutrient-limited cultures. Using both the absolute toxin concentrations and relative proportion (mole % total toxin) of each toxin derivative, N- and P-limitation can be distinguished based on the observed trends in the different saxitoxin derivatives. In this study, we examine the toxin content and composition in natural A. fundyense populations during a spring bloom in Casco Bay, ME from April-June of 1998. This allows us to examine whether A. fundyense populations in the western Gulf of Maine are sufficiently homogenous to permit the detection of toxin composition and toxin content differences through time and space, and if so, to determine whether those changes are indicative of a particular nutritional state (e.g., N-limitation). Using both toxin composition and toxin ratios determined from field samples during an A. fundyense bloom, the ratios generally correlated with N-limitation in the Casco Bay region. (c) 2005 Elsevier Ltd. All rights reserved.	Bigelow Lab Ocean Sci, W Boothbay Harbor, ME 04575 USA; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02453 USA	Bigelow Laboratory for Ocean Sciences; Woods Hole Oceanographic Institution	Poulton, NJ (通讯作者)，Bigelow Lab Ocean Sci, 180 McKown Point Rd,POB 475, W Boothbay Harbor, ME 04575 USA.	npoulton@alum.mit.edu	anderson, david/E-6416-2011	Poulton, Nicole/0000-0003-3020-4509				ADACHI M, 1993, NIPPON SUISAN GAKK, V59, P1807, DOI 10.2331/suisan.59.1807; ANDERSON DM, 1990, TOXIC MARINE PHYTOPLANKTON, P41; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson DM, 1999, J PHYCOL, V35, P870, DOI 10.1046/j.1529-8817.1999.3540870.x; ANDERSON DM, 1998, PHYSL ECOLOGY HARMFU, V4, P29; BOCZAR BA, 1988, PLANT PHYSIOL, V88, P1285, DOI 10.1104/pp.88.4.1285; BOYER GL, 1987, MAR BIOL, V96, P123, DOI 10.1007/BF00394845; Cembella AD, 2000, PHYCOLOGIA, V39, P67, DOI 10.2216/i0031-8884-39-1-67.1; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; ESTRADA M, 1998, PHYSL ECOLOGY HARM G, V41; Flynn K, 1996, MAR BIOL, V126, P9, DOI 10.1007/BF00571372; FLYNN K, 1994, MAR ECOL PROG SER, V111, P99, DOI 10.3354/meps111099; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; Guillard R. R., 1975, Culture of Marine Invertebrate Animals, P2960; Hall S., 1982, PhD diss; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; MARTORANO CD, 1997, HARMFUL TOXIC ALGAL, P132; Matsuda A., 1996, Harmful and Toxic Algal Blooms, P305; OGATA T, 1987, MAR BIOL, V95, P217, DOI 10.1007/BF00409008; OSHIMA Y, 1993, MAR BIOL, V116, P471, DOI 10.1007/BF00350064; Oshima Y., 1995, MANUAL HARMFUL MARIN, P81; OSHIMA YS, 1989, P 7 IUPAC S; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; POULTON NJ, 2001, THESIS MIT CAMBRIDGE, P246; REDFIELD AC, 1958, AM SCI, V46, P205; RHEE GY, 1978, LIMNOL OCEANOGR, V23, P10, DOI 10.4319/lo.1978.23.1.0010; SAKO Y, 1993, DEV MAR BIO, V3, P87; Sako Yoshihiko, 1995, P345; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; Taroncher-Oldenburg G, 1999, NAT TOXINS, V7, P207, DOI 10.1002/1522-7189(200009/10)7:5<207::AID-NT61>3.0.CO;2-Q; TARONCHEROLDENB.G, 1998, THESIS MIT CAMBRIDGE, P205; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; Turner JT, 2000, MAR ECOL PROG SER, V203, P95, DOI 10.3354/meps203095; VALDERRAMA JC, 1981, MAR CHEM, V10, P109, DOI 10.1016/0304-4203(81)90027-X; WHITE AW, 1978, J PHYCOL, V14, P475	42	42	47	0	18	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0967-0645			DEEP-SEA RES PT II	Deep-Sea Res. Part II-Top. Stud. Oceanogr.		2005	52	19-21					2501	2521		10.1016/j.dsr2.2005.06.029	http://dx.doi.org/10.1016/j.dsr2.2005.06.029			21	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800009
J	Anderson, DM; Stock, CA; Keafer, BA; Nelson, AB; Thompson, B; McGillicuddy, DJ; Keller, M; Matrai, PA; Martin, J				Anderson, DM; Stock, CA; Keafer, BA; Nelson, AB; Thompson, B; McGillicuddy, DJ; Keller, M; Matrai, PA; Martin, J			<i>Alexandrium fundyense</i> cyst dynamics in the Gulf of Maine	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; cysts; excystment; encystment; Gulf of Maine	DINOFLAGELLATE GONYAULAX-TAMARENSIS; RED TIDE DINOFLAGELLATE; RESTING CYSTS; GEORGES BANK; GERMINATION; SEDIMENTS; DINOPHYCEAE; CIRCULATION; BLOOMS; MODEL	The flux of cells from germinated cysts is critical in the population dynamics of many dinoflagellates. Here, data from a large-scale cyst survey are combined with surveys in other years to yield an Alexandrium fundyense cyst distribution map for the Gulf of Maine that is massive in geographic extent and cyst abundance. The benthic cyst population extends nearly 500 km alongshore. Embedded within it are several distinct accumulation zones or '' seedbeds,'' each 3000-5000 km(2) in area. Maximal cyst abundances range from 2-20 x 10(6) cysts m(-2). Cysts are equally or more abundant in deeper sediment layers; nearshore, cysts are fewer by a factor of 10 or more. This cyst distribution reflects sedimentary dynamics and the location of blooms in overlying surface waters. The flux of germinated cells from sediments was estimated using a combination of laboratory measurements of cyst germination and autofluorescence and observations of cyst autofluorescence in the field. These measurements constrained a germination function that, when applied to the cyst distribution map, provided an estimate of the germination inoculum for a physical/biological numerical model. In the laboratory studies, virtually all cysts incubated at different temperatures and light regimes became autofluorescent, but the rate of development was slower at lower temperatures, with no difference between light and dark incubations. Germination rates were highest at elevated temperatures, and were 2-fold greater in the light than in the dark. Laboratory and field fluorescence measurements suggest that > 70% of the cysts in the top cm of sediment would germinate over a 60-90 day period in offshore waters. The combination of laboratory germination experiments and numerical modeling predicts nearly 100% germination of cysts in the top cm of sediment and resulting early season cell concentrations that are comparable in magnitude to observed cell distributions. It cannot account for late-season peaks in cell abundance that are heavily influenced by vegetative growth. Cyst germination flux from deep-water (> 50 m) cyst seedbeds is 14X the flux in shallow waters. A conceptual model is proposed that is consistent with observed and modeled A. fundyense cyst and motile cell distributions and dynamics in the Gulf of Maine. Cysts germinate within the Bay of Fundy seedbed, causing localized, recurrent blooms that are self-seeding and '' propagatory '' in nature, supplying cells that populate the eastern segment of the Maine Coastal Current (MCC) and eventually deposit cysts offshore of Penobscot and Casco Bays. These cysts serve as a seed population for western Maine blooms that are transported to the west by the western segment of the MCC, where cells are removed either by mortality or advection from the region. Without the localized, '' incubator '' characteristic of the Bay of Fundy bloom zone, A. fund.vense populations in the Gulf of Maine should diminish through time. Their persistence over many decades highlights the effectiveness of the mechanisms described here. (c) 2005 Elsevier Ltd. All rights reserved.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; Rutgers State Univ, Piscataway, NJ 08854 USA; Bigelow Lab Ocean Sci, Boothbay Harbor, ME 04575 USA; Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada	Woods Hole Oceanographic Institution; Rutgers University System; Rutgers University New Brunswick; Bigelow Laboratory for Ocean Sciences; Fisheries & Oceans Canada	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Stock, Charles/H-1281-2012	McGillicuddy, Dennis/0000-0002-1437-2425; Stock, Charles/0000-0001-9549-8013				Anderson D.M., 1985, P219; Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Bewley J D., 1982, Physiology and Biochemistry of Seeds; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CRAIB J. 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Part II-Top. Stud. Oceanogr.		2005	52	19-21					2522	2542		10.1016/j.dsr2.2005.06.014	http://dx.doi.org/10.1016/j.dsr2.2005.06.014			21	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800010
J	Kirn, SL; Townsend, DW; Pettigrew, NR				Kirn, SL; Townsend, DW; Pettigrew, NR			Suspended <i>Alexandrium</i> spp. hypnozygote cysts in the Gulf of Maine	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium; Alexandrium fundyense; cysts; excystment; Gulf of Maine; harmful algal blooms; HABs	DINOFLAGELLATE GONYAULAX-TAMARENSIS; RED-TIDE DINOFLAGELLATE; POPULATION-DYNAMICS; RESTING CYSTS; EXCAVATA; SEDIMENTS; GERMINATION; BLOOMS; DINOPHYCEAE; EVENTS	The life cycle of dinoflagellates of the genus Alexandrium includes sexual reproduction followed by the formation of a dormant hypnozygote cyst, which serves as a resting stage. Negatively buoyant cysts purportedly fall to the benthos where they undergo a mandatory period of quiescence. Previous reports of cysts in the surficial sediments of the Gulf of Maine, where Alexandrium blooms are well documented, show a broad distribution of cysts, with highest concentrations generally in sediments below 100 m depth. We report here an exploration of cysts suspended in the water column, where they would be better positioned to inoculate springtime Alexandrium populations. During cruises in February, April, and June of 2000, water samples were collected at depths just off the bottom (within 5 m), at the top of the bottom nepheloid layer, and near the surface (1 m) and examined for cyst concentrations. Suspended cysts were found throughout the Gulf of Maine and westernmost Bay of Fundy. Planktonic cyst densities were generally greater in near-bottom and top of the bottom nepheloid layer samples than in near-surface water samples; densities were of the order of 10(2) cysts m(-3) in surface waters, and 10(2)-10(3) cysts m(-3) at near-bottom depths. Temporally, they were most abundant in February and least abundant in April. Reports by earlier workers of cysts in the underlying sediments were on the order of 10(3) cysts cm(-3). We present calculations that demonstrate the likelihood of cyst resuspension from bottom sediments forced by swell and tidal currents, and propose that such resuspended cysts are important in inoculating the seasonal bloom. We estimate that suspended cysts may contribute significantly to the annual vegetative cell population in the Gulf of Maine. (c) 2005 Elsevier Ltd. All rights reserved.	Univ Maine, Sch Marine Sci, Orono, ME 04469 USA	University of Maine System; University of Maine Orono	Univ Maine, Sch Marine Sci, 5706 Aubert Hall, Orono, ME 04469 USA.	davidt@maine.maine.edu						Anderson D.M., 1985, P219; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Brown J, 2001, J PLANKTON RES, V23, P105, DOI 10.1093/plankt/23.1.105; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; EPPLEY RW, 1968, J PHYCOL, V4, P333, DOI 10.1111/j.1529-8817.1968.tb04704.x; GRANT WD, 1979, J GEOPHYS RES-OCEANS, V84, P1797, DOI 10.1029/JC084iC04p01797; Ippen A.T., 1966, ESTUARY COASTLINE HY; Joint I, 1997, J PLANKTON RES, V19, P937, DOI 10.1093/plankt/19.7.937; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; KELLER M, 1999, GULF MAINE NEWS, P4; KIRN SL, 2002, THESIS U MAINE; LEWIS CM, 1979, TOXIC DINOFLAGELLATE, V1, P235; LODER JW, 1986, CONT SHELF RES, V6, P397, DOI 10.1016/0278-4343(86)90080-4; Mackenzie L, 1996, PHYCOLOGIA, V35, P148, DOI 10.2216/i0031-8884-35-2-148.1; MARTIN JL, 1988, CAN J FISH AQUAT SCI, V45, P1968, DOI 10.1139/f88-229; MIDDLETON GV, 1984, 3 SOC EC PAL MIN; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; REID PC, 1978, NEW PHYTOL, V80, P219, DOI 10.1111/j.1469-8137.1978.tb02284.x; SCHOLIN CA, 1995, PHYCOLOGIA, V24, P474; Souza AJ, 2001, J MAR RES, V59, P1021, DOI 10.1357/00222400160497751; THOMPSON B, 2000, S HARMF MAR ALG US M; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; YENTSCH CM, 1980, BIOSCIENCE, V30, P251, DOI 10.2307/1307880; YENTSCH CM, 1979, TOXIC DINOFLAGELLATE, V1, P127	39	27	30	0	15	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0967-0645	1879-0100		DEEP-SEA RES PT II	Deep-Sea Res. Part II-Top. Stud. Oceanogr.		2005	52	19-21					2543	2559		10.1016/j.dsr2.2005.06.009	http://dx.doi.org/10.1016/j.dsr2.2005.06.009			17	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800011
J	Matrai, P; Thompson, B; Keller, M				Matrai, P; Thompson, B; Keller, M			Circannual excystment of resting cysts of <i>Alexandrium</i> spp. from eastern Gulf of Maine populations	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						dinoflagellate; cyst; circannual; Gulf of Maine; Alexandrium; toxic	DINOFLAGELLATE GONYAULAX-TAMARENSIS; RED TIDE DINOFLAGELLATE; PHYTOPLANKTON BLOOMS; COASTAL CURRENT; GROWTH RHYTHM; CLOCK; DINOPHYCEAE; SEDIMENTS; DYNAMICS; EXCAVATA	Species of the marine dinoflagellate Alexandrium, present in most of the Gulf of Maine (GOM), Bay of Fundy and Gulf of St. Lawrence as well as in many other areas of the world, are known to cause toxicity to marine organisms and humans alike. Excystment of Alexandrium fundyense from the eastern region of the GOM (Penobscot Bay to Bay of Fundy) was followed through four germination cycles (4 years). An annual, free-running oscillation in germination was observed under constant environmental conditions, indicating control by an endogenous clock for these eastern cysts, as shown earlier for cysts from the western region of the GOM. This circannual endogenous, clock had an average period of 11 months. The phase of germination remained constant for cysts from all three stations sampled. Cysts did not germinate, despite favorable growth conditions, in summer-to-fall and this timing was consistent among cysts from all stations. The timing of cyst germination is highly relevant to modeling of Alexandrium sp. bloom initiation and depletion, as there are cyst '' seed beds '' near shore and offshore in the eastern and western regions of the GOM. (c) 2005 Elsevier Ltd. All rights reserved.	Bigelow Lab Ocean Sci, W Boothbay Harbor, ME 04575 USA	Bigelow Laboratory for Ocean Sciences	Matrai, P (通讯作者)，Bigelow Lab Ocean Sci, 180 McKown Pt, W Boothbay Harbor, ME 04575 USA.	pmatrai@bigelow.org						Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Alvarez JD, 2002, NATURE, V419, P798, DOI 10.1038/419798a; Anderson D.M., 1985, P219; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1997, LIMNOLOGY OCEANOGRAP, P42; [Anonymous], 1997, ADV MAR BIOL; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BROOKS DA, 1989, J MAR RES, V47, P303, DOI 10.1357/002224089785076299; COSTAS E, 1989, CHRONOBIOLOGIA, V16, P265; COSTAS E, 1991, PHYCOLOGIA, V30, P597, DOI 10.2216/i0031-8884-30-6-597.1; Dale B., 1983, P69; DIECK IT, 1991, J PHYCOL, V27, P341, DOI 10.1111/j.0022-3646.1991.00341.x; Dunlap JC, 1999, CELL, V96, P271, DOI 10.1016/S0092-8674(00)80566-8; Eilertsen HC, 2000, S AFR J MARINE SCI, V22, P323, DOI 10.2989/025776100784125717; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; GWINNER E, 1986, ZOOPHYSIOLOGY, P18; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; LUNING K, 1991, BOT ACTA, V104, P157; Lynch DR, 1997, CONT SHELF RES, V17, P605, DOI 10.1016/S0278-4343(96)00055-6; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Okamoto OK, 2003, J PHYCOL, V39, P519, DOI 10.1046/j.1529-8817.2003.02170.x; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; REID PC, 1978, NEW PHYTOL, V80, P219, DOI 10.1111/j.1469-8137.1978.tb02284.x; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; SPECTOR DL, 1984, DINOFLAGELLATES; SWEENEY, 1969, RHYTHMIC PHENOMENA P; Tomas C.R., 1997, IDENTIFYING MARINE P IDENTIFYING MARINE P, P858, DOI DOI 10.1016/B978-012693018-4/50004-5; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; WALL D, 1975, 1ST P INT C TOX DIN, P249; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	37	56	67	0	15	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0967-0645			DEEP-SEA RES PT II	Deep-Sea Res. Part II-Top. Stud. Oceanogr.		2005	52	19-21					2560	2568		10.1016/j.dsr2.2005.06.013	http://dx.doi.org/10.1016/j.dsr2.2005.06.013			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800012
J	Martin, JL; Page, FH; Hanke, A; Strain, PM; LeGresley, MM				Martin, JL; Page, FH; Hanke, A; Strain, PM; LeGresley, MM			<i>Alexandrium fundyense</i> vertical distribution patterns during 1982, 2001 and 2002 in the offshore Bay of Fundy, eastern Canada	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article							DINOFLAGELLATE GONYAULAX-EXCAVATA; RED-TIDE DINOFLAGELLATE; CYST FORMATION; FISH KILLS; MIGRATION; TOXINS; PLANKTON; GULF; ZOOPLANKTON; TAMARENSIS	An understanding of population dynamics of individual species and strains of Alexandrium spp. is important to achieving the greater knowledge needed for forecasting Occurrences, predicting consequences and determining mechanisms for bloom initiation and growth. Alexandrium fundyense populations were observed during July in the offshore waters of the Bay of Fundy (eastern Canada) at: 3-h intervals during a 54-h period in 1982, 2-h intervals during 30 and 22-h periods in 2001; and 2 h intervals for a 26 h period in 2002. Results suggest that A. fundyense vegetative cells (including duplets) and planozygotes concentrate in the upper layers, with highest concentrations observed in most surface samples. Concentrations decreased with depth. Cell concentrations of A. fundyense greater than 10(5) cells L-1 were detected. and concentrations varied considerably over the sampling periods. CTD data indicated that the water column was weakly stratified throughout each sampling period. Nutrient analysis suggests that silicates and phosphates in surface waters were not limiting, but nitrate values were lower in the upper layers than at depth. Statistical analyses of the profile data indicated that the observed counts were over dispersed or patchy. The pairwise comparison of the profiles did not support a diurnal vertical migration of cells over the depth range sampled ill any of the surveys. Shifts in density were detected across the two sampling sessions of 2001, but these differences were unrelated to an effect of photoperiod. Analyses of grouped profiles also failed to detect changes in the daytime versus nighttime distribution of cells with depth. (c) 2005 Elsevier Ltd. All rights reserved.	Fisheries & Oceans Canada, Biol Stn, St Andrews, NB E5B 2L9, Canada; Fisheries & Oceans Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada	Fisheries & Oceans Canada; Bedford Institute of Oceanography; Fisheries & Oceans Canada	Martin, JL (通讯作者)，Fisheries & Oceans Canada, Biol Stn, 531 Brandy Cove Rd, St Andrews, NB E5B 2L9, Canada.		Martin, Jennifer/G-5217-2011					Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Beet A, 2003, MAR ECOL PROG SER, V262, P285, DOI 10.3354/meps262285; Bumpus D.F., 1965, Serial Atlas of the Marine Environment; Cembella A.D., 1989, P81; Cullen J.J., 1985, Contributions in Marine Science, V27, P135; Cullen J. 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Oceanogr.		2005	52	19-21					2569	2592		10.1016/j.dsr2.2005.06.010	http://dx.doi.org/10.1016/j.dsr2.2005.06.010			24	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800013
J	McGillicuddy, DJ; Anderson, DM; Lynch, DR; Townsend, DW				McGillicuddy, DJ; Anderson, DM; Lynch, DR; Townsend, DW			Mechanisms regulating large-scale seasonal fluctuations in <i>Alexandrium fundyense</i> populations in the Gulf of Maine:: Results from a physical-biological model	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						phytoplankton; population dynamics; red tides; paralytic shellfish poisoning; USA; Gulf of Maine	DINOFLAGELLATE GONYAULAX-TAMARENSIS; GROWTH IRRADIANCE RELATIONSHIP; RED TIDE DINOFLAGELLATE; COASTAL CURRENT; MARINE-PHYTOPLANKTON; CYST FORMATION; INTERSPECIFIC DIFFERENCES; GEORGES BANK; FOOD WEBS; CIRCULATION	Observations of Alexandrium fundyense in the Gulf of Maine indicate several salient characteristics of the vegetative cell distributions: patterns of abundance are gulf-wide in geographic scope; their main features occur in association with the Maine Coastal Current; and the center of mass of the distribution shifts upstream from west to east during the growing season from April to August. The mechanisms underlying these aspects are investigated using coupled physical-biological simulations that represent the population dynamics of A. fundyense within the seasonal mean flow. A model that includes germination, growth, mortality, and nutrient limitation is qualitatively consistent with the observations. Germination from resting cysts appears to be a key aspect of the population dynamics that confines the cell distribution near the coastal L margin, as simulations based on a uniform initial inoculum of vegetative cells across the Gulf of Maine produces blooms that are broader in geographic extent than is observed. In general, cells germinated from the major cyst beds (in the Bay of Fundy and near Penobscot and Casco Bays) are advected in the alongshore direction from east to west in the coastal current. Growth of the vegetative cells is limited primarily by temperature from April through June throughout the gulf, whereas nutrient limitation occurs in July and August in the western gulf. Thus the seasonal shift in the center of mass of L cells from west to east can be explained by changing growth conditions: growth is more rapid in the western gulf early in I the season due to warmer temperatures, whereas growth is more rapid in the eastern gulf later in the season due to severe nutrient limitation in the western gulf during that time period. A simple model of encystment based on nutrient limitation predicts deposition of new cysts in the vicinity of the observed cyst bed offshore of Casco and Penobscot Bays, suggesting a pathway of re-seeding the bed from cells advected downstream in the coastal current. A retentive gyre at the mouth of the Bay of Fundy tends to favor re-seeding that cyst bed from local populations. (c) 2005 Elsevier Ltd. All rights reserved.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; Dartmouth Coll, Thayer Sch Engn, Hanover, NH 03755 USA; Univ Maine, Sch Marine Sci, Orono, ME 04469 USA	Woods Hole Oceanographic Institution; Dartmouth College; University of Maine System; University of Maine Orono	McGillicuddy, DJ (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	dmcgillicuddy@whoi.edu	anderson, david/E-6416-2011	McGillicuddy, Dennis/0000-0002-1437-2425				Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; ANDERSON DM, 1985, P 3 INT C ELS NEW YO; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Bigelow H.B., 1927, FISH B-NOAA, V40, P511; Bisagni JJ, 1996, CONT SHELF RES, V16, P1, DOI 10.1016/0278-4343(95)00002-I; Blumberg A., 1993, J. Environ. Eng., V1, P31, DOI DOI 10.1093/icesjms/fsm103; BROOKS DA, 1989, J MAR RES, V47, P303, DOI 10.1357/002224089785076299; BROOKS DA, 1994, J PHYS OCEANOGR, V24, P2387, DOI 10.1175/1520-0485(1994)024<2387:AMSOTB>2.0.CO;2; BROOKS DA, 1985, J GEOPHYS RES-OCEANS, V90, P4687, DOI 10.1029/JC090iC03p04687; Eilertsen HC, 2000, S AFR J MARINE SCI, V22, P323, DOI 10.2989/025776100784125717; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; Garside C, 1996, ESTUAR COAST SHELF S, V42, P617, DOI 10.1006/ecss.1996.0040; GODIN G, 1968, 1965 CURRENT SURVEY; HE R, 2005, IN PRESS J GEOPHYS R; Hetland RD, 2002, J MAR RES, V60, P763, DOI 10.1357/002224002321505129; KEAFER BA, 1993, DEV MAR BIO, V3, P763; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; LANGDON C, 1988, J PLANKTON RES, V10, P1291, DOI 10.1093/plankt/10.6.1291; LANGDON C, 1987, J PLANKTON RES, V9, P459, DOI 10.1093/plankt/9.3.459; LIEBIG J, 1845, CHEM PROCESSES NUTR; Lynch DR, 1996, CONT SHELF RES, V16, P875, DOI 10.1016/0278-4343(95)00028-3; Lynch DR, 1997, CONT SHELF RES, V17, P605, DOI 10.1016/S0278-4343(96)00055-6; Lynch DR, 2001, J ATMOS OCEAN TECH, V18, P962, DOI 10.1175/1520-0426(2001)018<0962:IMFLAH>2.0.CO;2; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; MARTIN JL, 1988, CAN J FISH AQUAT SCI, V45, P1968, DOI 10.1139/f88-229; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; Naimie CE, 1996, J GEOPHYS RES-OCEANS, V101, P6469, DOI 10.1029/95JC03698; Naimie CE, 2001, DEEP-SEA RES PT II, V48, P501, DOI 10.1016/S0967-0645(00)00087-4; PAGE FH, 2002, 10 INT C HARMF ALG S; Petrie B, 2000, CAN J FISH AQUAT SCI, V57, P2536, DOI 10.1139/cjfas-57-12-2536; Pettigrew NR, 1998, J GEOPHYS RES-OCEANS, V103, P30623, DOI 10.1029/98JC01625; PLATT T, 1976, J PHYCOL, V12, P421, DOI 10.1111/j.1529-8817.1976.tb02866.x; POULTON N, 2001, THESIS MIT CAMBRIDGE; PRAKASH A, 1967, J FISHERIES RES BOAR, V24; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; SIGNELL RP, 1993, ESTUARINE COASTAL MO, V3, P578; Teegarden GJ, 1996, J EXP MAR BIOL ECOL, V196, P145, DOI 10.1016/0022-0981(95)00128-X; Townsend DW, 2001, CONT SHELF RES, V21, P347, DOI 10.1016/S0278-4343(00)00093-5; Turner JT, 1997, LIMNOL OCEANOGR, V42, P1203, DOI 10.4319/lo.1997.42.5_part_2.1203; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; Xue HJ, 2000, J PHYS OCEANOGR, V30, P1111, DOI 10.1175/1520-0485(2000)030<1111:AMSOTS>2.0.CO;2; Yamamoto T, 2002, J PLANKTON RES, V24, P33, DOI 10.1093/plankt/24.1.33	52	124	134	1	40	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0967-0645	1879-0100		DEEP-SEA RES PT II	Deep-Sea Res. Part II-Top. Stud. Oceanogr.		2005	52	19-21					2698	2714		10.1016/j.dsr2.2005.06.021	http://dx.doi.org/10.1016/j.dsr2.2005.06.021			17	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT		Green Submitted			2025-03-11	WOS:000234265800019
J	Stock, CA; McGillicuddy, DJ; Solow, AR; Anderson, DM				Stock, CA; McGillicuddy, DJ; Solow, AR; Anderson, DM			Evaluating hypotheses for the initiation and development of <i>Alexandrium fundyense</i> blooms in the western Gulf of Maine using a coupled physical-biological model	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						modeling; statistical analysis; algal blooms; red tides; Alexandrium fundyense; harmful algal blooms	DINOFLAGELLATE GONYAULAX-TAMARENSIS; GROWTH IRRADIANCE RELATIONSHIP; MARINE-PHYTOPLANKTON; COASTAL CURRENT; DATA ASSIMILATION; GEORGES BANK; INTERSPECIFIC DIFFERENCES; SKELETONEMA-COSTATUM; VERTICAL MIGRATION; CYST FORMATION	A coupled physical/biological model and observations are used to investigate the factors governing the initiation and development of an Alexandrium fundyense bloom in the western Gulf of Maine (WGOM) during the spring of 1993 (March 19-June 6). The physical circulation is simulated using a 3D primitive equation model forced by climatological sea-surface elevation and observed winds, irradiance, and river outflow. This is Coupled with a biological model constructed from laboratory and field data that estimates the germination and growth rates of A.fundyense as a function of environmental conditions. Four biological model structures of increasing complexity are considered, with each structure representing a hypothesis for factors controlling bloom initiation and development. The model/data fit is optimized over the uncertainty in the parameters to which the model is most sensitive. The significance of changes in the model/data fit between model structures is quantified using a maximum likelihood ratio test. The baseline biological model, which parameterizes growth as only a function of temperature, salinity, and light, severely over-estimates observed A. fundyense abundance in the late spring. It is thus rejected with greater than 99% confidence in favor of biological models that include a mortality term or a dependence of growth on dissolved inorganic nitrogen (DIN). The overall best-fit simulation uses both nitrogen dependence and mortality. However, simulations using one or the other of these factors could not be differentiated from the best-fit case with greater than 90% confidence. The best-fit model captures the general timing and magnitude of the observed bloom and some of its secondary features. However, considerable misfits may exist in the point-to-point comparison, and some regional misfits remain. Diagnosis of the cell budget suggests that germination from a large cyst bed offshore of Casco Bay provides the majority of cells comprising spring A. fundyense populations within the WGOM. The size of the modeled bloom is largely set by the size of this cyst-driven source. Transport of cells from the eastern Gulf of Maine becomes increasingly important later in the spring. Net growth of the modeled A. fundyense Populations is first limited by low water temperatures and then by the combined influence of nitrogen limitation and mortality. This results in low domain-averaged net growth rates (< 0.05day(-1)) throughout much of the simulation. However, rates are sometimes elevated locally and therefore add notable spatial structure to the bloom. Primary uncertainties within the biological model include spatial and temporal variability in mortality, and the influence of sediment dynamics and inter-annual variability in the cyst abundance on the size and spatial character of the cyst driven source. As the dynamics governing these processes become better understood, the approach herein can be extended to accommodate additional dynamical model complexity. However, the ability of the model/data comparison to constrain and support the inclusion of additional biological processes is dependent on both the availability of A. fundyense observations and the physical model skill. (c) 2005 Elsevier Ltd. All rights reserved.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Stock, CA (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	cstock@whoi.edu	Stock, Charles/H-1281-2012; anderson, david/E-6416-2011	Stock, Charles/0000-0001-9549-8013; McGillicuddy, Dennis/0000-0002-1437-2425				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; [Anonymous], 1985, Numerical Recipes: The Art of Scientific Computing; BAUERFEIND E, 1986, MAR BIOL, V93, P323, DOI 10.1007/BF00401099; Blumberg A., 1993, J. 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Oceanogr.		2005	52	19-21					2715	2744		10.1016/j.dsr2.2005.06.022	http://dx.doi.org/10.1016/j.dsr2.2005.06.022			30	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	997RT					2025-03-11	WOS:000234265800020
J	Anderson, DM; Keafer, BA; McGillicuddy, DJ; Mickelson, MJ; Keay, KE; Libby, PS; Manning, JP; Mayo, CA; Whittaker, DK; Hickey, JM; He, RY; Lynch, DR; Smith, KW				Anderson, DM; Keafer, BA; McGillicuddy, DJ; Mickelson, MJ; Keay, KE; Libby, PS; Manning, JP; Mayo, CA; Whittaker, DK; Hickey, JM; He, RY; Lynch, DR; Smith, KW			Initial observations of the 2005 <i>Alexandrium fundyense</i> bloom in southern New England:: General patterns and mechanisms	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium fundyense; cysts; Gulf of Maine; PSP; harmful algal blooms; red tides	MAINE COASTAL CURRENT; HUMIC SUBSTANCES; GULF; PHYTOPLANKTON; CIRCULATION; TAMARENSE; PLUME; MODEL; DINOFLAGELLATE; DINOPHYCEAE	From May to July, 2005, an extensive bloom of Alexandrium fundyense occurred along the coast of southern New England. The outbreak eventually closed shellfish beds from central Maine to Massachusetts, including Nantucket Island and portions of Martha's Vineyard, and resulted in the closure of 40,000 km 2 of offshore federal waters as well. The coastal Alexandrium bloom was exceptional in several ways: high toxin levels were measured farther south than ever before in New England; levels of toxicity in many locations were higher than previously observed at those stations; for the first time toxicity at some locations was above quarantine levels; cell concentrations far exceeded those observed in the coastal waters of southern New England in the past; and for the first time in the region the governors of Maine and Massachusetts officially declared the red tide to be a disaster, clearing the way for federal assistance. Initial observations suggest that several factors contributed to this bloom. Abundant rainfall and heavy snowmelt substantially increased the amount of fresh water entering the Gulf of Maine. Combined with other freshwater inputs, we hypothesize that this provided macro- and micro-nutrients, a stratified water column, and a transport mechanism that led to high cell abundances and broad, region-wide dispersal of the organism. Warm temperatures in western waters also would have favored A. fundyense growth. In addition, several storms with strong winds out of the northeast occurred at times when cells were abundant and in locations where the winds could advect them into Massachusetts and Cape Cod Bays and keep them there, leading to high cell concentrations and toxicity. Another contributing factor may have been the high abundance of newly deposited cysts in western Gulf of Maine sediments, as documented in a fall 2004 survey. Here, we evaluate this bloom and the patterns of toxicity in light of the conceptual models for A. fundyense dynamics developed during the Ecology and Oceanography of Harmful Algal Blooms (ECOHAB)-Gulf of Maine (GOM) program. Several features of the 2005 bloom conform to the mechanisms proposed in those models, including the alongshore transport of cells in major water masses and episodic intrusions of cells toward shore due to downwelling-favorable wind forcings. The models need to be refined and expanded, however, based on new data and observations. For example, it is now clear that cells and bloom patches can reach the outer side of Cape Cod and even Nantucket and Martha's Vineyard. Transport to the coastal waters of Rhode Island and even Connecticut/Long Island is also possible. A critical modification also may be necessary in terms of mechanisms through which A. fundyense cells occur in Massachusetts Bay. In the past, toxicity only developed when blooms were transported from the north and into the bay via the western segment of the Maine Coastal Current. Now, it is possible that the bay might serve as a source of cells through the germination of cysts deposited in those waters during the 2005 bloom. If proven in subsequent surveys, this potential for in situ bloom development Could have major implications on the timing and extent of toxicity within Massachusetts Bay and southern New England waters in future years. (c) 2005 Elsevier Ltd. All rights reserved.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; Massachusetts Water Resources Author, Boston, MA 02129 USA; Battelle Mem Inst, Brunswick, ME 04011 USA; NE Fisheries Sci Ctr, Woods Hole, MA 02543 USA; Provincetown Ctr Coastal Studies, Provincetown, MA 02657 USA; Massachusetts Div Marine Fisheries, Pocasset, MA 02559 USA; Dartmouth Coll, Hanover, NH 03755 USA	Woods Hole Oceanographic Institution; National Oceanic Atmospheric Admin (NOAA) - USA; Massachusetts Division of Marine Fisheries; Dartmouth College	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Smith, Karl/GZK-8749-2022; He, Ruoying/C-5598-2015	McGillicuddy, Dennis/0000-0002-1437-2425; He, Ruoying/0000-0001-6158-2292; Smith, Keston/0009-0004-7973-6543				Anderson D, 2005, DEEP-SEA RES PT II, V52, P2365, DOI 10.1016/j.dsr2.2005.08.001; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2467, DOI 10.1016/j.dsr2.2005.06.015; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Bisagni JJ, 1996, CONT SHELF RES, V16, P1, DOI 10.1016/0278-4343(95)00002-I; BUTMAN B, 1975, 7715 MIT; CULLEN JJ, 1998, PHYSL ECOLOGY HARMFU, P559; DAVIS RE, 1985, J GEOPHYS RES-OCEANS, V90, P4756, DOI 10.1029/JC090iC03p04756; Fong DA, 2001, J GEOPHYS RES-OCEANS, V106, P1067, DOI 10.1029/2000JC900134; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; Gagnon R, 2005, J PHYCOL, V41, P489, DOI 10.1111/j.1529-8817.2005.00077.x; Geyer W.R., 1992, Physical Oceanographic Invertigation of Massachusetts and Cape Cod Bays; Grasshoff K., 1999, METHODS SEAWATER ANA, DOI 10.1002/9783527613984; Hartwell A.D., 1975, P47; HE R, 2005, J GEOPHYS RES, V110, P100; Hetland RD, 2002, J MAR RES, V60, P763, DOI 10.1357/002224002321505129; HORWITZ W, 1980, OFFICIAL METHODS ANA, P298; HURST JW, 1975, TOXIC DINOFLAGELLATE, P525; Keafer BA, 2005, DEEP-SEA RES PT II, V52, P2674, DOI 10.1016/j.dsr2.2005.06.016; Keafer BA, 2005, DEEP-SEA RES PT II, V52, P2631, DOI 10.1016/j.dsr2.2005.06.017; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Luerssen RM, 2005, DEEP-SEA RES PT II, V52, P2656, DOI 10.1016/j.dsr2.2005.06.025; Lynch DR, 1996, CONT SHELF RES, V16, P875, DOI 10.1016/0278-4343(95)00028-3; Lynch DR, 1997, CONT SHELF RES, V17, P605, DOI 10.1016/S0278-4343(96)00055-6; Lynch DR, 2001, J ATMOS OCEAN TECH, V18, P962, DOI 10.1175/1520-0426(2001)018<0962:IMFLAH>2.0.CO;2; Lynch DR, 1998, CONT SHELF RES, V18, P607, DOI 10.1016/S0278-4343(98)00007-7; McGillicuddy DJ, 2005, DEEP-SEA RES PT II, V52, P2698, DOI 10.1016/j.dsr2.2005.06.021; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; MELLOR GL, 1982, REV GEOPHYS, V20, P851, DOI 10.1029/RG020i004p00851; Pettigrew NR, 2005, DEEP-SEA RES PT II, V52, P2369, DOI 10.1016/j.dsr2.2005.06.033; PRAKASH A, 1968, LIMNOL OCEANOGR, V13, P598, DOI 10.4319/lo.1968.13.4.0598; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Smagorinsky J., 1963, Mon. 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J	Golovnina, EA; Polyakova, EI				Golovnina, EA; Polyakova, EI			Dinoflagellate cysts in bottom sediments of the White Sea (Western Arctic)	DOKLADY EARTH SCIENCES			English	Article							SURFACE CONDITIONS; ASSEMBLAGES		Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117997, Russia; Moscow MV Lomonosov State Univ, Geog Fac, Moscow 119992, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology; Lomonosov Moscow State University	Russian Acad Sci, PP Shirshov Oceanol Inst, Nakhimovskii Pr 36, Moscow 117997, Russia.	aksqa@aha.ru; yi@polyakova.geogr.msu.su	Polyakova, Yelena/L-8889-2015; Novichkova, Ekaterina/B-5807-2017	Novichkova, Ekaterina/0000-0001-5687-1719				[Anonymous], 1971, POLLEN SPORES; Dale A.L., 1992, Ocean Biocoenosis Series, P45; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; LISITSYN AP, 2003, URGENT PROBLEMS OCEA, P554; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie PJ, 2001, J QUATERNARY SCI, V16, P595, DOI 10.1002/jqs.660; Okolodkov Yu B, 2000, THESIS ST PETERSBURG; RATKOVA TM, 2000, BERICHTE POLARFORSCH, V359, P23; ROCHON A, 1999, AM ASSOC STRATIGR CO, V35; SEMONA GI, 1983, TRUDY BELOMORSKOI BI, V6, P3; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650	13	4	4	0	0	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1028-334X	1531-8354		DOKL EARTH SCI	Dokl. Earth Sci.	JAN-FEB	2005	400	1					136	139						4	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	904RZ					2025-03-11	WOS:000227516700033
J	Sluijs, A; Pross, J; Brinkhuis, H				Sluijs, A; Pross, J; Brinkhuis, H			From greenhouse to icehouse; organic-walled dinoflagellate cysts as paleoenvironmental indicators in the Paleogene	EARTH-SCIENCE REVIEWS			English	Review						(marine) eukaryotic plankton; dinoflagellates; organic-walled hypnozygotic dinoflagellate cysts; paleoenviromnent; paleoclimate; Paleogene; Paleocene; Eocene; Oligocene	CRETACEOUS-TERTIARY BOUNDARY; NORTHERN NORTH-ATLANTIC; SEA-SURFACE TEMPERATURE; EOCENE-OLIGOCENE TRANSITION; CALCAREOUS NANNOFOSSIL; OCEAN PRODUCTIVITY; MIDDLE EOCENE; MARINE; CARBON; BIOSTRATIGRAPHY	Dinoflagellates are an important component of the extant eukaryotic plankton. Their organic-walled, hypnozygotic cysts (dinocysts) provide a rich, albeit incomplete, history of the group in ancient sediments. Building on pioneering studies of the late 1970s and 1980s, recent drilling in the Southern Ocean has provided a wealth of new dinocyst data spanning the entire Paleogene. Such multidisciplinary studies have been instrumental in refining existing and furnishing new concepts of Paleogene paleoenvironmental and paleoclimatic reconstructions by means of dinocysts. Because dinocysts notably exhibit high abundances in neritic settings, dinocyst-based environmental and paleoclimatic information is important and complementary to the data derived from typically more offshore groups as planktonic foraminifera, coccolithophorids, diatoms and radiolaria. By presenting case-studies from around the globe, this contribution provides a concise review of our present understanding of the paleoenvironmental significance of dinocysts in the Paleogene (65-25 Ma). Representing Earth's greenhouse-icehouse transition, this episode holds the key to the understanding of extreme transient climatic change. We discuss the potential of dinocysts for the reconstruction of Palcogene sea-surface productivity, temperature, salinity, stratification and paleo-oxygenation along with their application in sequence stratigraphy, oceanic circulation and general watermass reconstructions. (C) 2004 Elsevier B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Tubingen, Inst Geosci, D-72076 Tubingen, Germany; Goethe Univ Frankfurt, Inst Geol & Paleontol, D-60054 Frankfurt, Germany	Utrecht University; Eberhard Karls University of Tubingen; Goethe University Frankfurt	Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	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Rev.	JAN	2005	68	3-4					281	315		10.1016/j.earscirev.2004.06.001	http://dx.doi.org/10.1016/j.earscirev.2004.06.001			35	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	889VT		Green Published			2025-03-11	WOS:000226471600004
J	Lambert, O				Lambert, O			Systematics and phylogeny of the fossil beaked whales <i>Ziphirostrum</i> du Bus, 1868 and <i>Choneziphius</i> Duvernoy, 1851 (Mammalia, Cetacea, Odontoceti), from the Neogene of Antwerp (North of Belgium)	GEODIVERSITAS			English	Article						Mammalia; Cetacea; Odontoceti; Ziphiidae; Ziphirostrum; Choneziphius; Miocene; Pliocene; Belgium; fossil; phylogeny; new genius; new species	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; ZIPHIIDAE; MIOCENE; MORPHOLOGY	A systematic revision of the fossil beaked whales (Cetacea, Odontoceti, Ziphiidae) Ziphirostrum du Bus, 1868 and Choneziphius Duvernoy, 1851 from the Neogene of Antwerp (Belgium, southern margin of the North Sea Basin) is undertaken. It is based on several rostra and partial skulls from the collection of the Institut royal des Sciences naturelles de Belgique. From the previous conclusions about those taxa, dating from the beginning of the 20th century and suggesting only one species in each genus, Mioziphius (Ziphirostrum) belgicus and Choneziphius planirostris, the following modifications are proposed. The genus Ziphirostrum includes three species: Z. marginatum, Z turniense, and Z recurvus n. comb. Basicranial fragments and teeth of Z marginatum are described for the first time. Besides the most common species Choneziphius planirostris, the species C. macrops is identified from Antwerp and the east coast of North America. A new genus and species Beneziphius brevirostris n. gen., n. sp. is described on the basis of two specimens characterized by a short and pointed rostrum. Two partial skulls are placed in Ziphiidae aff. Eboroziphius, a genus known from the east coast of North America. The genus name Aporotus is restored, with a large species A. recurvirostris, and a smaller species A. dicyrtus. A parsimony analysis including fossil A and extant ziphiid taxa shows a sister-group relationship between Choneziphius + (Tusciziphius + Ziphius) and Ziphirostrum + Beneziphius gen. The poorly known Aporotus seems more closely related to Choneziphius + (Tusciziphius + Ziphius), but additional morphological information is needed.	Inst Royal Sci Nat Belgique, Dept Paleontol, B-1000 Brussels, Belgium		Inst Royal Sci Nat Belgique, Dept Paleontol, Rue Vautier 29, B-1000 Brussels, Belgium.	olivier.lambert@naturalsciences.be	Lambert, Olivier/AEN-2469-2022	Lambert, Olivier/0000-0003-0740-5791				Abel O., 1905, Memoires du Musee royal d'histoire naturelle de Belgique, V3, P1; Abel O., 1919, Die Stamme der Wirbeltiere; [Anonymous], 1998, CLASSIFICATION MAMMA; [Anonymous], 1910, B US NATL MUSEUM, DOI DOI 10.5479/SI.03629236.73.I; Bianucci Giovanni, 1997, Palaeontographia Italica, V84, P163; Bianucci Giovanni, 1992, Bollettino della Societa Paleontologica Italiana, V31, P261; Bianucci Giovanni, 1994, Bollettino della Societa Paleontologica Italiana, V33, P231; BOSSELAERS M, 2004, GEOLOGICA BELGIC, V7, P227; Cuvier G, 1823, RECHERCHES OSSEMENTS; Dalebout ML, 1998, MOL ECOL, V7, P687, DOI 10.1046/j.1365-294x.1998.00380.x; Dalebout ML, 2003, MAR MAMMAL SCI, V19, P421, DOI 10.1111/j.1748-7692.2003.tb01314.x; Dalebout ML, 2002, MAR MAMMAL SCI, V18, P577, DOI 10.1111/j.1748-7692.2002.tb01061.x; de Muizom C., 1991, B MUS NATL HIST NAT, V3-4, P279; de Muizon C., 1985, Travaux de l'Institut Francais d'Etudes Andines, V27, P1; DELHEID E, 1896, ANN SOC ROYAL MALACO, V31, P20; du Bus B.A.L., 1868, B ACAD ROYALE SCI BE, V25, P621; DUBUS BAL, 1897, B ACAD ROYALE SCI BE, V34, P491; DUVERNOY G, 1851, ZOOLOGIE, V15, P52; Fordyce R.E., 2001, Secondary Adaptation of Tetrapods to Life in Water, P169; FORDYCE RE, 1994, ANNU REV EARTH PL SC, V22, P419, DOI 10.1146/annurev.ea.22.050194.002223; Fordyce RE, 2002, ANTARCT SCI, V14, P37, DOI 10.1017/S0954102002000561; Geisler Jonathan H., 2003, Journal of Mammalian Evolution, V10, P23, DOI 10.1023/A:1025552007291; GERVAIS P, 1859, ZOOLLGIE PALEONTOLOG; Glaessmer M. 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J	Niebuhr, B				Niebuhr, B			Geochemistry and time-series analyses of orbitally forced Upper Cretaceous marl-limestone rhythmites (Lehrte West Syncline, northern Germany)	GEOLOGICAL MAGAZINE			English	Article						Cretaceous; Germany; geochemistry; diagenesis; rhythmite; cyclic processes; time series analysis	DIAGENESIS; SEDIMENTS; SUCCESSIONS; FREQUENCIES; CARBONATES; BARITE; BASIN; CYCLE; OPAL; SEA	A cyclic marl-limestone succession of Middle-Late Campanian age has been investigated with respect to a Milankovitch-controlled origin of geochemical data. In general, the major element geochemistry of the marl-limestone rhythmites can be explained by a simple two-component mixing model with the end-members calcium carbonate and `average shale'-like material. Carbonate content varies from 55 to 90%. Non-carbonate components are clay minerals (illite, smectite) and biogenic silica from sponge spicules, as well as authigenically formed zeolites (strontian heulandite) and quartz. The redox potential suggests oxidizing conditions throughout the section. Trace element and stable isotopic data as well as SEM investigations show that the carbonate mud is mostly composed of low-magnesium calcitic tests of planktic coccolithophorids and calcareous dinoflagellate cysts (calcispheres). Diagenetic overprint results in a decrease of 2 parts per thousand delta(18)O and an increase in Mn of up to 250 ppm. However, the sediment seems to preserve most of its high Sr content compared to the primary low-magnesium calcite of co-occurring belemnite rostra. The periodicity of geochemical cycles is dominated by 413 ka and weak signals between 51 and 22.5 ka, attributable to orbital forcing. Accumulation rates within these cycles vary between 40 and 50 m/Ma. The resulting cyclic sedimentary sequence is the product of (a) changes in primary production of low-magnesium calcitic biogenic material in surface waters within the long eccentricity and the precession, demonstrated by the CaCO3 content and the Mg/Al, Mn/Al and Sr/Al ratios, and (b) fluctuations in climate and continental weathering, which changed the quality of supplied clay minerals (the illite/smectite ratio), demonstrated by the K/Al ratio. High carbonate productivity correlates with smectite-favouring weathering (semi-arid conditions, conspicuously dry and moist seasonal changes in warmer climates). Ti as the proxy indicator for the detrital terrigenous influx, as well as Rb, Si, Zr and Na, shows only low frequency signals. indicating nearly constant rates of supply throughout the more or less pure pelagic carbonate deposition of the long-lasting third-order Middle-Upper Campanian sedimentary cycle.	Univ Wurzburg, Inst Palaontol, D-97070 Wurzburg, Germany	University of Wurzburg	Niebuhr, B (通讯作者)，Univ Wurzburg, Inst Palaontol, Pleicherwall 1, D-97070 Wurzburg, Germany.	niebuhr@mail.uni-wuerzburg.de						[Anonymous], NATO ASI SERIES C; Arthur M.A., 1985, Fine-grained deposits and biofacies of the Western Interior Seaway: evidence of cyclic sedimentary processes. 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B., 1930, B SERVICE GEOLOGIQUE, V6, P485; Taylor S.R., 1985, CONTINENTAL CRUST; Veizer J, 1999, CHEM GEOL, V161, P59, DOI 10.1016/S0009-2541(99)00081-9; VEIZER J, 1974, J SEDIMENT PETROL, V44, P93; VEIZER J, 1977, J SEDIMENT PETROL, V47, P565; VEIZER J, 1983, OTTAWA CARLETON CTR, V682; VOLKMANN R, 1998, BERICHTE NATURHISTOR, V140, P121; von Rad, 1979, GEOL RUNDSCH, V68, P1025, DOI 10.1007/BF02274685; VONSCHLOTHEIM EF, 1913, LEONHARDST TASCENBUC, V7; Weaver C.E., 1989, Clays, Muds, and Shales, V44, P819; Wedepohl K.H., 1991, Metals and Their Compounds in the Environment, P3; Wedepohl K.H., 1971, Physics and Chemistry of the Earth, V8, P305, DOI [10.1016/0079-1946(71)90020-6, DOI 10.1016/0079-1946(71)90020-6]; Weedon G.P., 2003, TIME SERIES ANAL CYC; Wilson M.J., 1987, HDB DETERMINATIVE ME	69	53	61	0	25	CAMBRIDGE UNIV PRESS	NEW YORK	40 WEST 20TH ST, NEW YORK, NY 10011-4211 USA	0016-7568			GEOL MAG	Geol. Mag.	JAN	2005	142	1					31	55		10.1017/S0016756804009999	http://dx.doi.org/10.1017/S0016756804009999			25	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	919LP					2025-03-11	WOS:000228619800004
J	Volkova, VS; Kuz'mina, OB; Kul'kova, IA				Volkova, VS; Kuz'mina, OB; Kul'kova, IA			Marine and continental Paleogene and Miocene of southern Baraba facies region of West Siberia: Stratigraphy and microphytofossils	GEOLOGIYA I GEOFIZIKA			Russian	Article						palynology; dinocysts; spores; pollen; Paleogene; Miocene; West Siberia	DEPOSITS; NEOGENE	This paper reports new data on geological structure, palynostratigraphy, and paleomagnetism obtained from reference BH-9 as well as from BH-2. BH-6, and BH-13 drilled in the south of the Novosibirsk Region. The rock lithology has been described to follow the stratigraphic sequence. The question of recognition of the Upper Cretaceous is discussed. Zonal complexes of dinocysts, spores, and pollen are characterized. The marine deposits date from the Paleocene and Miocene, and the continental ones, from the Oligocene and Miocene. The data on microphytofossils confirm the recurrent character of development of the Tavda sea basin in the late Middle-Late Eocene. Cysts of dinoflagellates of the genus Pseudokomewuia were established for the first time in the Upper Oligocene sediments (Turtas lake-sea), which suggested a connection of the Turtas basin with southern seas through the Turgai trough at the beginning of Zhuravka time. The range of occurrence of dinocysts is bordered south of 55degreesN. Until recently, dinocysts of the genus Pseudokomewuia have been established only in China and North America. and now they are found in West Siberia as well. These findings are of great interest for solving questions of paleogeography and paleoecology.	Russian Acad Sci, Inst Petr & Gas Geol, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Volkova, VS (通讯作者)，Russian Acad Sci, Inst Petr & Gas Geol, Prosp Koptyuga 3, Novosibirsk 630090, Russia.		Kuzmina, Olga/I-9547-2018					ANDREEVAGRIGORO.AS, 1991, THESIS KIEV; [Anonymous], B SOC GEOL FR, DOI DOI 10.1080/00241160410006483; ARKHIPOV SA, 1970, ZAPADNOSIBIRSKAYA RA; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BEAMOVSKII VN, 1989, GEOL GEOFIZ, P47; CHATENEUF J, 1980, B BRQM, V16, P59; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; COSTA LJ, 1988, 124 RAH RES INT GEOL, P508; DOLYA ZA, 2001, PRIRODA PRIRODOPOLZO, P99; GRICHUK VP, 1948, ANAL ISKOPAEMYKH PYL; HE CQ, 1984, MEMOIRS NANJING I GE, V19, P143; KRASHENINNIKOV VA, 1996, GEOLOGICHESKIE BIOTI; Kul'kova I.A, 1994, MIKROFITOFOSSILII DE, P98; Kulkova I.A., 1990, GEOL GEOFIZ+, P25; Kulkova IA, 1997, GEOL GEOFIZ, V38, P581; KULKOVA IA, 1987, GEOL GEOFIZ, P11; Kuz'mina OB, 2003, GEOL GEOFIZ, V44, P348; Kuzmina, 2001, NOVOSTI PALEONTOLOGI, P135; Martini E., 1971, P 2 PLANKT C ROM 197, P739; PANOVA LA, 1977, KAINOZOISKIE FLORY S, P40; Shatsky S.B., 1984, SREDA ZHIZN RUBEZHAK, P9; *SNIIG MS, 2001, UN REG STRAT SKHEM N; VASILEVA ON, 1990, DIATOMOVYE VODOROSLI; Volkova VS, 2002, GEOL GEOFIZ, V43, P1017; Vozzhennikova T.F., 1979, Dinocysts and Their Stratigraphic Significance	25	10	13	0	0	RUSSIAN ACAD SCIENCES SIBERIAN BRANCH	NOVOSIBIRSK	S P C  U I G G M  S B  R A S, 3 AKADEMIKA KOPTYGA PROSPEKT, 630090 NOVOSIBIRSK, RUSSIA	0016-7886			GEOL GEOFIZ	Geol. Geofiz.		2005	46	1					60	71						12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	894VI					2025-03-11	WOS:000226819300005
C	Warrington, G		Pirrie, D		Warrington, G.			THE CHARMOUTH 16A BOREHOLE, DORSET, UK: PALYNOLOGY OF THE PENARTH GROUP AND THE BASAL LIAS GROUP (UPPER TRIASSIC - LOWER JURASSIC)	GEOSCIENCE IN SOUTH-WEST ENGLAND, VOL 11, PT 2, 2005	Proceedings of the Ussher Society		English	Proceedings Paper	43rd Annual Meeting of the Ussher-Society	JAN 03-06, 2005	Newquay, ENGLAND	Ussher Soc			SOUTH-WEST ENGLAND; AMMONITE FAUNAS; BOUNDARY; SUCCESSION; SOMERSET; BRITAIN; DEVON; BAY	Palynomorphs from a succession proved in a cored borehole at Charmouth, in the Dorset and East Devon Coast World Heritage Site, amplify the incomplete palynological documentation of the Penarth Group and basal Lias Group previously available from coastal exposures and a borehole in east Devon. Units examined are the upper Westbury Formation, the Lilstock Formation, including beds (the Cotham Member) that are typically poorly exposed, and the Blue Lias, to a level in the Hettangian Stage. Miospore associations increase in diversity upwards through the upper Westbury Formation and the Gotham Member, into the basal Langport Member; associations from higher beds, particularly in the Blue Lias Formation, are less diverse. A change from dinoflagellate cyst-dominated to acritarch-dominated organic-walled microplankton associations occurs above the basal Langport Member.				gw47@le.ac.uk						Callomon JH, 1995, FIELD GEOLOGY OF THE BRITISH JURASSIC, P51; Cope J.C.W, 1980, Special Report, 14; CULSHAW MG, 1973, 39 I GEOL SCI GEOPH; FISHER M J, 1985, Pollen et Spores, V27, P95; GALLOIS RW, 2003, COAST COUNTRY GEOLOG, P55; Hallam A., 1960, Proceedings of the Geologists' Association, V71, P47, DOI 10.1016/S0016-7878(60)80031-4; HART MB, 1982, GEOLOGY DEVON, P179; Hesselbo SP, 2004, J GEOL SOC LONDON, V161, P365, DOI 10.1144/0016-764903-033; Hesselbo SP, 1995, FIELD GEOLOGY OF THE BRITISH JURASSIC, P105; Hesselbo SP, 2002, GEOLOGY, V30, P251, DOI 10.1130/0091-7613(2002)030<0251:TAMEAT>2.0.CO;2; Hounslow MW, 2004, PALAEOGEOGR PALAEOCL, V213, P331, DOI 10.1016/j.palaeo.2004.07.018; *I GEOL SCI, 1974, 747 I GEOL SCI; JUKESBROWNE AJ, 1902, Q J GEOL SOC LOND, V58, P279; Lang W. D., 1924, Proceedings of the Geologists' Association London, V35, P169; Lott G. K., 1988, P YORKS GEOL SOC, V47, P139, DOI [10.1144/pygs.47.2.139, DOI 10.1144/PYGS.47.2.139]; MAYALL MJ, 1983, GEOL MAG, V120, P613, DOI 10.1017/S001675680002776X; ORBELL G., 1973, Bulletin of the Geological Survey of Great Britain, V44, P1; Page KN, 2002, PROC USSHER, V10, P293; Page KN, 1998, PROC USSHER, V9, P231; Pálfy J, 2001, GEOLOGY, V29, P1047, DOI 10.1130/0091-7613(2001)029<1047:CIAAOG>2.0.CO;2; Powell A.J., 1992, P1; Richardson L., 1906, P GEOLOGISTSASSOCIAT, V19, P401, DOI 10.1016/S0016-7878(06)80067-2; Simms MJ, 2003, GEOLOGY, V31, P557, DOI 10.1130/0091-7613(2003)031<0557:UESFTL>2.0.CO;2; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; Warrington G., 1981, P61; Warrington G, 1995, PROC USSHER, V8, P426; Warrington G, 1997, PROC USSHER, V9, P153; Warrington G., 1986, P USSHER SOC, V6, P368; WARRINGTON G, 1977, B GEOLOGICAL SURVEY, V57, P40; Warrington G., 1978, V68, P22; Warrington G, 1901, P USSHER SOC, V5, P24; WARRIT B, 1980, PLANT CELL ENVIRON, V3, P13, DOI 10.1111/j.1365-3040.1980.tb00092.x; WHITTAKER A, 1974, REPORT CHARMOU UNPUB; Wignall PB, 2001, P GEOLOGIST ASSOC, V112, P349, DOI 10.1016/S0016-7878(01)80014-6	34	8	8	0	8	USSHER SOC	EXETER	UNIV EXETER DEPT GEOLOGY, NORTH PARK ROAD, EXETER EX4 4QE, DEVON, ENGLAND	0566-3954			PROC USSHER	Proc. USSHER		2005	11		2				109	116						8	Geology; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Geology	BOC67					2025-03-11	WOS:000276191500006
S	Horton, JW; Aleinikoff, JN; Kunk, MJ; Gohn, GS; Edwards, LE; Self-Trail, JM; Powars, DS; Izett, GA		Kenkmann, T; Horz, F; Deutsch, A		Horton, J. Wright, Jr.; Aleinikoff, John N.; Kunk, Michael J.; Gohn, Gregory S.; Edwards, Lucy E.; Self-Trail, Jean M.; Powars, David S.; Izett, Glen A.			Recent research on the Chesapeake Bay impact structure, USA-Impact debris and reworked ejecta	LARGE METEORITE IMPACTS III	Geological Society of America Special Papers		English	Article; Book Chapter						Chesapeake; impact; crater; ejecta; cataclastic; shock; resurge; SHRIMP; argon; geochronology; dinoflagellate; nannofossil	ATLANTIC COASTAL-PLAIN; GEOCHEMICAL CHARACTERISTICS; TEKTITE FRAGMENTS; AGE; BARBADOS; EOCENE; SITE; GEOCHRONOLOGY; POLYMORPH; HISTORY	Four new coreholes in the western annular trough of the buried, late Eocene Chesapeake Bay impact structure provide samples of shocked minerals, cataclastic rocks, possible impact melt, mixed sediments, and damaged microfossils. Parautochthonous Cretaceous sediments show an upward increase in collapse, sand fluidization, and mixed sediment injections. These impact-modified sediments are scoured and covered by the upper Eocene Exmore beds, which consist of highly mixed Cretaceous to Eocene sediment clasts and minor crystalline-rock clasts in a muddy quartz-glauconite sand matrix. The Exmore beds are interpreted as seawater-resurge debris flows. Shocked quartz is found as sparse grains and in rock fragments at all four sites in the Exmore, where these fallback remnants are mixed into the resurge deposit. Crystalline-rock clasts that exhibit shocked quartz or cataclastic fabrics include felsites, granitoids, and other plutonic rocks. Felsite from a monomict cataclasite boulder has a sensitive high-resolution ion microprobe U-Pb zircon age of 613 +/- 4 Ma. Leucogranite from a polymict cataclasite boulder has a similar Neoproterozoic age based on muscovite 40Ar/39Ar data. Potassium-feldspar 40Ar/39Ar ages from this leucogranite show cooling through closure (similar to 150 degrees C) at ca. 261 Ma without discernible impact heating. Spherulitic felsite is under investigation as a possible impact melt. Types of crystalline clasts, and exotic sediment clasts and grains, in the Exmore vary according to location, which suggests different provenances across the structure. Fractured calcareous nannofossils and fused, bubbled, and curled dinoflagellate cysts coexist with shocked quartz in the Exmore, and this damage may record conditions of heat, pressure, and abrasion due to impact in a shallow-marine environment.	[Horton, J. Wright, Jr.; Gohn, Gregory S.; Edwards, Lucy E.; Self-Trail, Jean M.; Powars, David S.] US Geol Survey, Reston, VA 20192 USA; [Aleinikoff, John N.; Kunk, Michael J.] US Geol Survey, Denver Fed Ctr, Denver, CO 80225 USA; [Izett, Glen A.] Coll William & Mary, Dept Geol, Williamsburg, VA 23285 USA	United States Department of the Interior; United States Geological Survey; United States Department of the Interior; United States Geological Survey; William & Mary	Horton, JW (通讯作者)，US Geol Survey, MS 926A,12201 Sunrise Valley Dr, Reston, VA 20192 USA.	whorton@usgs.gov		Kunk, Michael/0000-0003-4424-7825				ALEINIKOFF JN, 1995, AM J SCI, V295, P428, DOI 10.2475/ajs.295.4.428; Alexander Jr E.C., 1978, 4 INT C GEOCHR COSM, P78; ALLEN EP, 1968, N CAROLINA GEOLOGICA, V81; [Anonymous], 2001, BERKELEY GEOCHRONOLO; [Anonymous], UNIFIED NOMENCLATURE; [Anonymous], 88261 US GEOL SURV; BOHLKE JK, 1995, WATER RESOUR RES, V31, P2319, DOI 10.1029/95WR01584; Bohor B.F., 1988, Proceedings of the 26th Lunar and Planetary Science Conference, V19, P114; CATCHINGS RD, 2001, 01407 US GEOL SURV; CATCHINGS RD, 2005, STUDIES CHE IN PRESS; Chesner CA, 1998, J PETROL, V39, P397, DOI 10.1093/petrology/39.3.397; Compston W., 1984, Journal of Geophysical Research, V89, P525, DOI 10.1029/JB089iS02p0B525; CROFT SK, 1981, GEOCHIM COSM SUPPL, V15, P207; Dalrymple G.B., 1981, 1176 GEOL SOC; Deino A.L., 2001, BERKELEY GEOCHRONO A, V1; Edwards LE, 2003, PALAIOS, V18, P275, DOI 10.1669/0883-1351(2003)018<0275:IDTDFT>2.0.CO;2; EDWARDS LE, 2005, STUDIES CHE IN PRESS; FETTER AH, 1995, J GEOL, V103, P313, DOI 10.1086/629749; FLECK RJ, 1977, GEOCHIM COSMOCHIM AC, V41, P15, DOI 10.1016/0016-7037(77)90184-3; FREDERIKSEN NO, 2005, STUDIES CHE IN PRESS, pCHD; GLASS BP, 1995, GEOCHIM COSMOCHIM AC, V59, P4071, DOI 10.1016/0016-7037(95)00290-G; Glass BP, 2002, AM MINERAL, V87, P562; Glass BP, 2001, GEOLOGY, V29, P371, DOI 10.1130/0091-7613(2001)029<0371:DOHPZP>2.0.CO;2; GLASS BP, 1989, METEORITICS, V24, P209, DOI 10.1111/j.1945-5100.1989.tb00695.x; GLASS BP, 1986, CHEM GEOL, V59, P181, DOI 10.1016/0168-9622(86)90070-9; GLASS BP, 2002, GEOLOGICAL SOC AM AB, V34, P465; GOHN GS, 2002, GEOLOGICAL SOC AM AB, V34, P465; GOHN GS, 2005, STUDIES CHE IN PRESS; Goldberg, 1994, Geology and Field Trip Guide, Western Flank of the Raleigh Metamorphic Belt, North Carolina, P13; Grieve RAF, 1996, METEORIT PLANET SCI, V31, P6, DOI 10.1111/j.1945-5100.1996.tb02049.x; *HAMPT ROADS PLANN, 1999, HAMPTON ROADS PLANNI, V2, P2; Harris NBW, 1986, GEOL SOC SPEC PUBL, V19, P67, DOI 10.1144/GSL.SP.1986.019.01.04; Horton J.W., 1994, Geological Society of America Abstracts with Programs, V26, P21; Horton Jr. J.W., 2002, EOS T AM GEOPHYS U S, V83, pS351; HORTON JW, 2005, STUDIES CHE IN PRESS; HORTON JW, 2004, ICDP USGS WORKSH DEE; HORTON JW, 2001, GEOL SOC AM ABSTR, V33, pA448; HORTON JW, 2003, LPI CONTRIBUTION, V1167; HORTON JW, 1999, GEOLOGICAL SOC AM AB, V31, pA476; HORTON JW, 2002, GEOLOGICAL SOC AM AB, V34, P466; Izett G.A., 1990, 249 GEOL SOC AM; KAMO SL, 2002, LPI CONTRIBUTION, V1109; KOEBERL C, 1988, EARTH PLANET SC LETT, V87, P286, DOI 10.1016/0012-821X(88)90016-7; Koeberl C, 1996, SCIENCE, V271, P1263, DOI 10.1126/science.271.5253.1263; KOEBERL C, 2001, LPI CONTRIBUTION, V1080; LEBAS MJ, 1986, J PETROL, V27, P745, DOI 10.1093/petrology/27.3.745; LEFORT JP, 1991, TECTONICS, V10, P213, DOI 10.1029/90TC00911; Ludwig K.R., 2003, ISOPLOT 3.00: A Geochronological Toolkit for Microsoft Excel; McDougall I., 1999, GEOCHRONOLOGY THERMO; MCFARLAND ER, 2005, STUDIES CHE IN PRESS; Melosh H.J., 1989, IMPACT CRATERING GEO; Melosh HJ, 1999, ANNU REV EARTH PL SC, V27, P385, DOI 10.1146/annurev.earth.27.1.385; NGO HH, 1985, GEOCHIM COSMOCHIM AC, V49, P1479, DOI 10.1016/0016-7037(85)90297-2; Obermeier S.F., 2001, 01029 US GEOL SURV; OLSON SM, 2003, 03307 US GEOL SURV; Owens BE, 2003, GEOL SOC AM BULL, V115, P972, DOI 10.1130/B25258.1; PEARCE JA, 1984, J PETROL, V25, P956, DOI 10.1093/petrology/25.4.956; Poag C.W., 1999, Chesapeake Invader: Discovering America's Giant Meteorite Crater; POAG CW, 1994, GEOLOGY, V22, P691, DOI 10.1130/0091-7613(1994)022<0691:MMIOVS>2.3.CO;2; Poag CW, 2002, DEEP-SEA RES PT II, V49, P1081, DOI 10.1016/S0967-0645(01)00144-8; Poag CW, 2002, GEOLOGY, V30, P995; POAG CW, 1992, GEOLOGY, V20, P771, DOI 10.1130/0091-7613(1992)020<0771:DSDPSB>2.3.CO;2; Poag CW, 1996, METORIT PLANET SCI, V31, P218, DOI 10.1111/j.1945-5100.1996.tb02015.x; POAG CW, 1999, GEOLOGICAL SOC AM SP, V339, P149; POAG CW, 1999, BERICHTE POLARFORSCH, V343, P79; POAG CW, 2005, STUDIES CHE IN PRESS; POAG CW, 2004, CHESAPEAKE BAY IMPAC; POWARS D. 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J	Anderson, DM; Keafer, BA; Geyer, WR; Signell, RP; Loder, TC				Anderson, DM; Keafer, BA; Geyer, WR; Signell, RP; Loder, TC			Toxic <i>Alexandrium</i> blooms in the western Gulf of Maine:: The plume advection hypothesis revisited	LIMNOLOGY AND OCEANOGRAPHY			English	Article							COASTAL CURRENT; GONYAULAX-TAMARENSIS; PHYTOPLANKTON; CIRCULATION; GROWTH; TRANSPORT; MECHANISM; DYNAMICS; MODEL	The plume advection hypothesis links blooms of the toxic dinoflagellate Alexandrium fundyense in the western Gulf of Maine (GOM) to a buoyant plume derived from river outflows. This hypothesis was examined with cruise and moored-instrument observations in 1993 when levels of paralytic shellfish poisoning (PSP) toxins were high, and in 1994 when toxicity was low. A coupled physical-biological model simulated hydrography and A. fundyense distributions. Initial A. fundyense populations were restricted to low-salinity nearshore waters near Casco Bay, but also occurred in higher salinity waters along the Plume boundary. This suggests two sources of cells-those from shallow-water cyst populations and those transported to shore from offshore blooms in the eastern segment of the Maine coastal current (EMCC). Observations confirm the role of the Plume in A. fundyense transport and growth. Downwelling-favorable winds in 1993 transported the plume and its cells rapidly alongshore, enhancing toxicity and propagating PSP to the south. In 1994, sustained upwelling moved the plume offshore, resulting in low toxicity in intertidal shellfish. A. fundyense blooms were likely nutrient limited, leading to low growth rates and moderate cell abundances. These observations and mechanisms were reproduced by coupled physical-biological model simulations. The plume advection hypothesis provides a viable explanation for outbreaks of PSP in the western GOM, but should be refined to include two sources for cells that populate the Plume and two major pathways for transport: one within the low-salinity plume and another where A. fundyense cells originating in the EMCC are transported along the outer boundary of the plume front with the western segment of the Maine coastal current.	Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA 02543 USA; US Geol Survey, Woods Hole, MA 02543 USA; Univ New Hampshire, Inst Earth, Durham, NH 03824 USA	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; United States Department of the Interior; United States Geological Survey; University System Of New Hampshire; University of New Hampshire	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.		anderson, david/E-6416-2011	Signell, Richard/0000-0003-0682-9613				ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1992, P GULF MAIN WORKSH W, P217; *AOAC, 1980, OFF METH AN, P298; Bigelow H.B., 1927, FISH B-NOAA, V40, P511; Bisagni JJ, 1996, CONT SHELF RES, V16, P1, DOI 10.1016/0278-4343(95)00002-I; Blumberg A.F., 1991, A Primer for ECOM-si; Blumberg A.F., 1987, Three Dimensional Ocean Models, P1; BLUMBERG AF, 1985, J HYDRAUL ENG-ASCE, V111, P273; BROOKS DA, 1989, J MAR RES, V47, P303, DOI 10.1357/002224089785076299; BROOKS DA, 1994, J PHYS OCEANOGR, V24, P2387, DOI 10.1175/1520-0485(1994)024<2387:AMSOTB>2.0.CO;2; BROOKS DA, 1985, J GEOPHYS RES-OCEANS, V90, P4687, DOI 10.1029/JC090iC03p04687; BUTMAN B, 1975, 7715 WOODS HOL OC I; Fong DA, 2001, J GEOPHYS RES-OCEANS, V106, P1067, DOI 10.1029/2000JC900134; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; FRANKS PJS, 1997, 97498 US GEOL SURV; GERACI JR, 1989, CAN J FISH AQUAT SCI, V46, P1895, DOI 10.1139/f89-238; Geyer W.R., 1992, Physical Oceanographic Invertigation of Massachusetts and Cape Cod Bays; Geyer WR, 2004, CONT SHELF RES, V24, P1339, DOI 10.1016/j.csr.2004.04.001; GLIBERT PM, 1977, 7747 WOODS HOL OC I; Hetland RD, 2002, J MAR RES, V60, P763, DOI 10.1357/002224002321505129; HONG DA, 1997, J MARINE SYST, V12, P69; KEAFER BA, 1993, DEV MAR BIO, V3, P763; LARGE WG, 1981, J PHYS OCEANOGR, V11, P324, DOI 10.1175/1520-0485(1981)011<0324:OOMFMI>2.0.CO;2; Lynch DR, 1997, CONT SHELF RES, V17, P605, DOI 10.1016/S0278-4343(96)00055-6; LYNCH DR, 1993, J PHYS OCEANOGR, V23, P2222, DOI 10.1175/1520-0485(1993)023<2222:TMTAIR>2.0.CO;2; MARTORANO CD, 1997, THESIS U NEW HAMPSHI; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; MELLOR GL, 1982, REV GEOPHYS, V20, P851, DOI 10.1029/RG020i004p00851; Pettigrew NR, 1998, J GEOPHYS RES-OCEANS, V103, P30623, DOI 10.1029/98JC01625; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; PRAKASH A, 1968, LIMNOL OCEANOGR, V13, P598, DOI 10.4319/lo.1968.13.4.0598; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; TOWNSEND DW, 2001, CONTINENTAL SHELF RE, V48, P159; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; White A.W., 1989, P395; WHITE AW, 1993, DEV MAR BIO, V3, P435; WHITE DNJ, 1987, SPEC REP CHEM SOC, V6, P38	40	61	72	2	17	AMER SOC LIMNOLOGY OCEANOGRAPHY	WACO	5400 BOSQUE BLVD, STE 680, WACO, TX 76710-4446 USA	0024-3590			LIMNOL OCEANOGR	Limnol. Oceanogr.	JAN	2005	50	1					328	345		10.4319/lo.2005.50.1.0328	http://dx.doi.org/10.4319/lo.2005.50.1.0328			18	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	888XF		Bronze			2025-03-11	WOS:000226406800031
J	Pospelova, V; Chmura, GL; Boothman, WS; Latimer, JS				Pospelova, V; Chmura, GL; Boothman, WS; Latimer, JS			Spatial distribution of modern dinoflagellate cysts in polluted estuarine sediments from Buzzards Bay (Massachusetts, USA) embayments	MARINE ECOLOGY PROGRESS SERIES			English	Article						dinoflagellate cyst; Eutrophication; heavy metals; sewage; wastewater treatment plant; PCBs; Apponagansett Bay; New Bedford Harbor	NEW-BEDFORD HARBOR; NEW-ENGLAND USA; ENVIRONMENTAL-FACTORS; INDUSTRIAL-POLLUTION; APPONAGANSETT BAY; HUMAN DISTURBANCE; NORWEGIAN FJORD; YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION	Analysis of the spatial distribution of the dinoflagellate cyst assemblages in 19 surface sediment samples collected from 3 Buzzards Bay (Massachusetts, USA) embayments revealed the potential applicability of dinoflagellate cysts as biological indicators of environmental conditions in estuarine systems. Sites with the highest levels of toxic pollution and hypertrophic conditions are characterized by the lowest dinoflagellate cyst species-richness and concentrations. Among the abiotic factors influencing the distribution of dinoflagellate cysts, nutrients and toxic pollution are the major controls, as in these embayments salinity and temperature variability is low. Principal component analysis, based on the proportions of cyst taxa, indicated that cyst assemblages gradually change when moving away from the sources of nutrient pollution, sewage outfalls in particular.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K7, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K7, Canada; Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; US Environm Protect Agcy, NHEERL, Off Res & Dev, Atlantic Ecol Div, Narragansett, RI 02882 USA	University of Victoria; United States Environmental Protection Agency	McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 2K7, Canada.	vpospe@uvic.ca	Latimer, James/C-1632-2009; Chmura, Gail/LNI-4648-2024	Pospelova, Vera/0000-0003-4049-8133; Chmura, Gail/0000-0001-7163-3903				ABUHILAL AH, 1990, MAR POLLUT BULL, V21, P190, DOI 10.1016/0025-326X(90)90501-X; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Bergen BJ, 1998, ENVIRON SCI TECHNOL, V32, P3496, DOI 10.1021/es980413o; BORKMAN DG, 1993, MAR ECOL PROG SER, V100, P27, DOI 10.3354/meps100027; BOTHNER MH, 1994, MAR ENVIRON RES, V38, P43, DOI 10.1016/0141-1136(94)90045-0; Chmura GL, 2004, SCI TOTAL ENVIRON, V320, P225, DOI 10.1016/j.scitotenv.2003.08.003; COSTA JE, 1999, MANAGING ANTHROPOGEN; COSTA JE, 1996, REPORT BUZZARDS BAY; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; Dale B., 1996, PALYNOLOGY PRINCIPLE, P249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; Fensome R.A., 1993, CLASSIFICATION FOSSI; FENSOME RA, 1996, PALYNOLOGY PRINCIPLE, P107; Fisher RA, 1943, J ANIM ECOL, V12, P42, DOI 10.2307/1411; Gibson GR, 2000, 822B00024 EPA OFF WA; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Howes B.L., 1999, BAYWATCHERS 2 NUTR R; HOWES BL, 1996, 31 US GEOL SURV NAT; JACOBSON DM, 1994, PHYCOLOGIA, V33, P97, DOI 10.2216/i0031-8884-33-2-97.1; Latimer JS, 2003, SCI TOTAL ENVIRON, V313, P153, DOI 10.1016/S0048-9697(03)00269-9; LENTIN JK, 1993, CONTRIBUTION SERIES, V28; Mackay D.W., 1972, MAR POLLUT BULL, V3, P7; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; NIXON SW, 1995, OPHELIA, V41, P199, DOI 10.1080/00785236.1995.10422044; PIERCE RW, 1994, MAR ECOL PROG SER, V112, P225, DOI 10.3354/meps112225; Pospelova V, 2004, REV PALAEOBOT PALYNO, V128, P7, DOI 10.1016/S0034-6667(03)00110-6; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Pospelova V, 2002, J PHYCOL, V38, P593, DOI 10.1046/j.1529-8817.2002.t01-1-01206.x; Rego S., 1996, EPA600R96097 NAT HLT; Reid P. C., 1978, CONTRIBUTION SERIES, V5, P147; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; *SAIC, 1991, CHAR POLL INP BUZZ B; SOMMER U, 1995, LIMNOL OCEANOGR, V40, P1272; STOCKMARR J, 1971, Pollen et Spores, V13, P615; SUMMERHAYES CP, 1985, CONTRIBUTION SEDIMEN; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; TERKLA DG, 1990, EC GROWTH ENV CHANGE; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Tsirtsis G, 1998, ENVIRON MONIT ASSESS, V50, P255, DOI 10.1023/A:1005883015373; TURNER JT, 2000, 9903MWI MASS DEP ENV; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D, 1966, NATURE, V211, P1125	54	113	120	0	12	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2005	292						23	40		10.3354/meps292023	http://dx.doi.org/10.3354/meps292023			18	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	937MJ		Bronze			2025-03-11	WOS:000229927900003
J	McQuoid, MR				McQuoid, MR			Influence of salinity on seasonal germination of resting stages and composition of microplankton on the Swedish west coast	MARINE ECOLOGY PROGRESS SERIES			English	Article						resting stages; cysts; spores; germination; diatoms; dinoflagellates; salinity; pH	SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; OBLEA-ROTUNDA DIPLOPSALIDACEAE; CYST-THECA RELATIONSHIP; CONFERVACEA CLEVE GRAN; BALTIC SEA; GYMNODINIUM-CATENATUM; SPRING BLOOM; MARINE-PHYTOPLANKTON; PLANKTONIC DIATOMS; NORTH-ATLANTIC	Surface sediment from Gullmar Fjord, Sweden was cultured in the laboratory to assess the influence of different salinities on the germination of benthic resting stages and subsequent vegetative growth. Sediment cultures were grown in media with salinities of 15, 25, and 35 parts per thousand in both spring and summer conditions. Many microplankton species grew in the cultures. Dominant taxa were the diatoms Chaetoceros, Detonula, Skeletonema, and Thalassiosira, and the dinoflagellates Diplopsalis, Scrippsiella, and Oblea. Growth of T. minima and T. pseudonana after more than 2 yr of storage provides new evidence of a dormant stage in these species. Salinity significantly influenced germination only in D. confervacea and O. rotunda, but it showed significant effects on growth for all the dominant taxa. Salinity optima of the microplankton in the experiments were compared to salinity ranges of these species in fjords on the Swedish west coast. In the fjords, D. confervacea grows poorly at salinities > 27 parts per thousand and may be outcompeted by halotolerant species, such as C. socialis and T. minima. Because salinity is most variable in spring, a wide salinity tolerance is particularly advantageous during this season. The dominant dinoflagellates were well adapted to salinities between 22 and 35 parts per thousand, and O. rotunda is favored at the high end of this range. Results illustrate how climate-related changes in sea-surface salinity may alter the microplankton community on the Swedish west coast through direct effects on resting-stage germination and planktonic growth.	Gothenburg Univ, Dept Marine Ecol, S-40530 Gothenburg, Sweden	University of Gothenburg	McQuoid, MR (通讯作者)，Gothenburg Univ, Dept Marine Ecol, Box 461, S-40530 Gothenburg, Sweden.	melissa.mcquoid@marbot.gu.se						ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; Belgrano A, 1999, P ROY SOC B-BIOL SCI, V266, P425, DOI 10.1098/rspb.1999.0655; BINDER BJ, 1987, J PHYCOL, V23, P99; Blanco J., 1985, P79; BRAND LE, 1984, ESTUAR COAST SHELF S, V18, P543, DOI 10.1016/0272-7714(84)90089-1; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CANNON JA, 1993, DEV MAR BIO, V3, P103; CARLSSON P, 1995, MAR ECOL PROG SER, V127, P213, DOI 10.3354/meps127213; Chomérat N, 2004, EUR J PHYCOL, V39, P317, DOI 10.1080/09670260410001712590; Edwards M, 2002, MAR ECOL PROG SER, V239, P1, DOI 10.3354/meps239001; EILERTSEN HC, 1995, MAR ECOL PROG SER, V116, P303, DOI 10.3354/meps116303; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Goffart A, 2002, MAR ECOL PROG SER, V236, P45, DOI 10.3354/meps236045; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Gustafsson B, 1996, J SEA RES, V35, P39, DOI 10.1016/S1385-1101(96)90733-9; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; Hinga KR, 2002, MAR ECOL PROG SER, V238, P281, DOI 10.3354/meps238281; HOLLIBAUGH JT, 1981, J PHYCOL, V17, P1; Hurlbert S.H., 2001, RECONNAISSANCE BIOL; Irigoien X, 2000, J PLANKTON RES, V22, P2367, DOI 10.1093/plankt/22.12.2367; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kim DI, 2004, J PLANKTON RES, V26, P61, DOI 10.1093/plankt/fbh001; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; Kristiansen S., 1998, HYDROBIOLOGIA, V363, P169; LANGE CB, 1992, SARSIA, V77, P173, DOI 10.1080/00364827.1992.10413503; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; LEWIS J, 1990, BRIT PHYCOL J, V25, P339, DOI 10.1080/00071619000650381; Lindahl O, 1998, ICES J MAR SCI, V55, P723, DOI 10.1006/jmsc.1998.0379; LINDAHL O, 1983, MAR ECOL PROG SER, V10, P119, DOI 10.3354/meps010119; McQuoid MR, 2003, ESTUARIES, V26, P927, DOI 10.1007/BF02803351; McQuoid MR, 2002, J PHYCOL, V38, P881, DOI 10.1046/j.1529-8817.2002.01169.x; MCQUOID MR, 1995, J PHYCOL, V31, P44, DOI 10.1111/j.0022-3646.1995.00044.x; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; MONTRESOR M, 2001, LIFEHAB LIFE HIST MI, P18; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; Oku O, 1997, MAR BIOL, V127, P515, DOI 10.1007/s002270050040; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; RIJSTENBIL JW, 1989, MAR BIOL, V101, P121, DOI 10.1007/BF00393485; Robineau B, 1997, J MARINE SYST, V11, P81, DOI 10.1016/S0924-7963(96)00030-9; Schrum C, 2001, CLIM RES, V18, P31, DOI 10.3354/cr018031; SMAYDA TJ, 1969, J PHYCOL, V5, P150, DOI 10.1111/j.1529-8817.1969.tb02596.x; SNOEIJS P, 1999, INTERCALIBRATION DIS, V1; STROM SL, 1993, LIMNOL OCEANOGR, V38, P965, DOI 10.4319/lo.1993.38.5.0965; TAYLOR FJR, 1993, ECOLOGY FISH KILLING; Tiselius P, 1996, J PLANKTON RES, V18, P133, DOI 10.1093/plankt/18.2.133; Weise AM, 2002, CAN J FISH AQUAT SCI, V59, P464, DOI 10.1139/F02-024; Yamamoto T, 2003, J PLANKTON RES, V25, P63, DOI 10.1093/plankt/25.1.63	54	47	61	1	29	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2005	289						151	163		10.3354/meps289151	http://dx.doi.org/10.3354/meps289151			13	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	923RV		Bronze			2025-03-11	WOS:000228927900014
C	Gedl, P		Tyszka, J; OliwkiewiczMiklasinska, M; Gedl, P; Kaminski, MA		Gedl, P			<i>In situ</i> and recycled dinoflagellate cysts from Middle Miocene deposits at Beczyn, Carpathian Foredeep, Poland	Methods and Applications in Micropalaeontology	Studia Geologica Polonica - Series		English	Proceedings Paper	5th Micropalaeontological Workshop (Mikro 2005)	JUN 08-10, 2005	Szymbark, POLAND	Carl Zeiss Ltd, Cleka, Polskie Gornictwo Naftowe i Gzaownictwo SA, Precoptic Co Wojciechowscy Spolka Jawna, Stamptex		Miocene; biostratigraphy; dinocysts; Carpathians; Carpathian foredeep	ADJACENT SEAS; SEDIMENTS; NORTH	Middle Miocene clays exposed at Beczyn (Carpathian Foredeep) contain frequent organic-walled dinoflagellate cysts. The age-assessment of the dinocysts from the clays at Beczyn suggests their Early Badenian age (interregional dinocyst zone D17). However, dinocyst assemblage is in large part composed of recycled pre-Miocene specimens. Late Cretaceous and Palaeogene dinocysts are the most frequent among the forms treated as recycled. Occurrence of so frequent recycled dinocysts points at erosion of pre-Miocene substratum during the Early Badenian.	Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Gedl, P (通讯作者)，Polish Acad Sci, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.							Alexandrowicz S.W., 1982, Geol. Q, V26, P470; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1997, BULL POL ACAD SCI EA; Costa L. I., 1988, GEOL JB; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; EDWARDS JW, 1984, CULT MED PSYCHIAT, V8, P1, DOI 10.1007/BF00053099; Garecka M., 1999, PR PA STW I GEOL, V168, P29; Gedl P., 2000, Studia Geologica Polonica, V117, P155; Gedl P., 1997, B POLISH ACAD SCI EA, V45, P191; GEDL P, 1995, SZATA ROSLINNA POLSK, P114; Gedl P., 1999, GEOL Q, V43, P479; Gedl Przemyslaw, 2004, Tomy Jurajskie, V2, P49; Gedl Przemyslaw, 1996, Annales Societatis Geologorum Poloniae, V66, P191; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; KRACH W, 1948, ANN SOC GEOLOGIQUE P, V18, P273; Luczkowska E., 1957, Annales de la Societe Geologique de Pologne, V25, P305; MALECKI J, 1949, ANN SOC GEOLOGIQUE P, V19, P487; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; Manum S. B., 1976, Initial Rep Deep Sea Drilling Project, V38, P897; MOENKE MARIA, 1953, ACTA GEOL POLONICA, V3, P239; NOWAK W, 1959, INSTYTUT GEOLOGICZNY, V131, P149; Olszewska B., 1999, Pr. Pastw. Inst. Geol, V168, P9; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Powell A.J., 1992, P155; Powell A.J., 1986, AASP CONTRIB SERIES, V17, P105; Rochon Andre, 1999, AASP Contributions Series, V35, P1; SCHILLER B, 1976, SPRAWOZDANIE POSIEDZ, V20, P164; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALL D, 1969, J PHYCOL, V5, P140, DOI 10.1111/j.1529-8817.1969.tb02595.x; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V28, P1; Wojcik A., 1999, PRACE PIG, V168, P231; ZEVENBOOM D, 1995, THESIS U UTRECHT, P1; [No title captured]	37	14	14	0	0	INSTYTUT NAUK GEOLOGICZNYCH POLSKIEJ AKADEMII NAUK	WARSZAWA	UL TWARDA 51-55, WARSZAWA, 00-818, POLAND	0081-6426		83-918081-4-9	STUD GEOL POLON			2005	124						371	394						24	Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Paleontology	BEA73					2025-03-11	WOS:000236486000023
C	Gedl, P; Worobiec, E		Tyszka, J; OliwkiewiczMiklasinska, M; Gedl, P; Kaminski, MA		Gedl, P; Worobiec, E			Organic-walled dinoflagellate cysts from Miocene deposits of the Legnica-33/56 borehole (Fore-Sudetic Monocline) as indicators of marine ingression in south-western Poland	METHODS AND APPLICATIONS IN MICROPALAEONTOLOGY	Studia Geologica Polonica - Series		English	Proceedings Paper	5th Micropalaeontological Workshop (Mikro 2005)	JUN 08-10, 2005	Szymbark, POLAND	Carl Zeiss Ltd, Cleka, Polskie Gornictwo Naftowe i Gzaownictwo SA, Precoptic Co Wojciechowscy Spolka Jawna, Stamptex		Middle Miocene; Muzakow series; Polish Lowland; dinoflagellate cysts (dinocysts); palaeoenvironment		Marine dinoflagellate cysts are described from the basal part of the Muzakow series in the Legnica-33/56 borehole (Fore-Sudetic Monocline, south-western Poland). Their occurrence reflects marine ingression that covered this area during the Middle Miocene. Qualitative composition of dinocyst and sporomorph assemblages allows reconstructing the palaeoenvironment of present-day Legnica vicinity as a shallow marine bay with rich vegetation of the Everglades-type.	Polish Acad Sci, Cracow Res Ctr, Inst Geol Sci, PL-31002 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Polish Acad Sci, Cracow Res Ctr, Inst Geol Sci, Senacka 1, PL-31002 Krakow, Poland.	ndgedl@cyf-kr.edu.pl		Worobiec, Elzbieta/0000-0001-5997-9602				[Anonymous], 1978, Podrecznik analizy py3kowej; Ciuk E., 1970, Kwart. Geol., V14, P754; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; DYJOR S, 1969, PRACE GEOLOGIZNO MIN, V11, P67; DYJOR S, 1973, PRACE GEOLOGIZNO MIN, V111, P3; Dyjor S, 1978, PRZEW 50 ZJAZD PTG Z, P210; DYJOR S, 1986, PRZEGLAD GEOLOGICZNY, V7, P380; Dyjor S, 1986, GEOLOGIA, V12, P7; DYJOR S, 1982, STAN ROZPOZNANIA STR, P339; DYJOR S, 1986, GEOLOGIA, V12, P25; DYJOR S, 1969, ACTA UNIVERSITATIST, V86, P3; Dyjor S., 1978, PRZEW 50 ZJAZD POL T, P66; DYJOR S, 1994, PRAC NAUK I GORN POL, V74, P82; Dyjor S, 1970, GEOL QUARTER, V14, P819; Gedl P, 2005, STUD GEOL POLON, V124, P371; GEDL P, 1998, B POLISH ACAD SCI EA, V45, P191; GEDL P, 1995, SZATA ROSLINNA POLSK, P114; Gedl Przemyslaw, 1996, Annales Societatis Geologorum Poloniae, V66, P191; GEIDL P, 1999, GEOL Q, V43, P479; Giel M.D., 1979, Kwartalnik Geologiczny, V23, P663; JAHN A, 1984, Geologia Sudetica (Wroclaw), V18, P7; Jaron L., 1978, PRZ GEOL, V24, P579; LUCZKOWSKA E, 1971, ANN SOC GEOL POL, V41, P337; Moore P.D., 1994, Pollen Analysis; OBERC J, 1968, PRZEGLAD GEOLOGICZNY, V16, P498; Piwocki M, 1995, PRZ GEOL, V43, P916; PIWOCKI M, 1975, I GEOLOGICZNY B, V384, P73; Piwocki M., 1997, GEOL Q, V41, P21; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rusbult J., 1992, N JB GEOL PALAONT MH, V3, P150; SADOWSKA A, 1977, Acta Palaeobotanica, V18, P87; SADOWSKA A, 1970, THESIS WROCLAW U; SADOWSKA A, 1981, STRATIGRAPHY LEGNICA; STACHURSKA A, 1971, ANN SOC GEOLOGIQUE P, V41, P359; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; Worobiec E., 2000, THESIS POLISH ACAD S THESIS POLISH ACAD S; WOROBIEC E, 2001, P 22 S GEOL COAL BEA, P125	38	6	7	0	0	INSTYTUT NAUK GEOLOGICZNYCH POLSKIEJ AKADEMII NAUK	WARSZAWA	UL TWARDA 51-55, WARSZAWA, 00-818, POLAND	0081-6426		83-918081-4-9	STUD GEOL POLON			2005	124						395	410						16	Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Paleontology	BEA73					2025-03-11	WOS:000236486000024
J	Kaminski, MA; Silye, L; Kender, S				Kaminski, MA; Silye, L; Kender, S			Miocene deep-water agglutinated Foraminifera from ODP Hole 909c: Implications for the paleoceanography of the Fram Strait Area, Greenland Sea	MICROPALEONTOLOGY			English	Article							CENTRAL ARCTIC-OCEAN; BENTHIC FORAMINIFERA; NORTH SEAS; LABRADOR; BIOSTRATIGRAPHY; PLIOCENE	Deep-water agglutinated Foraminifera (DWAF) are investigated from Miocene sediments recovered from ODP Hole 909C in the Fram Strait, Norwegian-Green land Sea. We studied 125 samples from Cores 909C-50R to -103R. and recovered over 60 species of DWAF. The faunal succession in Hole 909C is subdivided into three assemblages based on the stratigraphic ranges of characteristic cosmopolitan taxa. These are: (1) a diverse Reticulophraginium amplectens - Reophanus berggreni Assemblage in Cores 909C-100R-2 to -91R-1 (1040.71-952.78mbsf); (2) a Reticulophragmium amplectens Assemblage in Cores 909C-87R-2, to -71R-3 (915.7-762.68mbsf); and (3) a low-diversity Reticulophraginium rotundidorsatum Assemblage in Cores 909C-71R-1 to -55R-1 (759.68-605.52mbsf). The DWAF assemblages are correlated to the standard chronostratigraphy using dinoflagellate cysts and magnetostratigraphy. The stratigraphic ranges of some well-known Palcogene DWAF species extend far into the Miocene at this locality, confirming tire hypothesis that the Arctic and northern Norwegian Sea basins served as a refuge for these species long after they disappeared from the North Atlantic stratigraphic record. The taxonomic affinities of the Miocene assemblages from Hole 909C supports the idea that an estuarine Circulation pattern has been in place between the Arctic Ocean and Greenland Sea basins since at least the early Miocene. Changes in the benthic foraminiferal morphogroups within the R. rotundidorsatum Assemblage correlate with an increase in total organic carbon, indicating an increase in oceanic productivity in the Fram Strait region during the late Miocene.	UCL, Dept Earth Sci, London WC1E 6BT, England; Univ Babes Bolyai, Dept Geol, Cluj Napoca 400084, Romania	University of London; University College London; Babes Bolyai University from Cluj	UCL, Dept Earth Sci, Gower St, London WC1E 6BT, England.	s.kender@ucl.ac.uk	Kaminski, Michael/K-3334-2012; Kender, Sev/B-9409-2016; Silye, Lorand/C-1568-2009	Kender, Sev/0000-0003-4216-3214; Kaminski, Michael A/0000-0002-7344-5874; Silye, Lorand/0000-0001-7306-6041				Altenbach AV, 1999, J FORAMIN RES, V29, P173; [Anonymous], [No title captured]; [Anonymous], 1996, P OCEAN DRILLING PRO; [Anonymous], P OCEAN DRILLING PRO; [Anonymous], 1884, Rept. Sci. Res. Voy. H.M.S. Challenger, Zool.; [Anonymous], PALEOECOLOGY BIOSTRA; BERGGREN WA, 1990, NATO ADV SCI I C-MAT, V327, P53; BERRY E. 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A., 1961, T VSESOYUZNOGO NAUCH, V170, P170; von Hantken M., 1875, MITTHEILUNGEN JAHRBU, V4, P1; von Hantken M., 1868, MAGYAR FOLDTANI TARS, V4, P75; Winkler A, 2002, INT J EARTH SCI, V91, P133, DOI 10.1007/s005310100199; Wolf-Welling Thomas C.W., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P515; Wollenburg JE, 1998, MAR MICROPALEONTOL, V34, P153, DOI 10.1016/S0377-8398(98)00007-3	73	39	46	0	13	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2005	51	5					373	403		10.2113/gsmicropal.51.5.373	http://dx.doi.org/10.2113/gsmicropal.51.5.373			31	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	026EM		Green Submitted			2025-03-11	WOS:000236320300002
J	Riding, JB				Riding, James B.			The Late Jurassic dinoflagellate cyst <i>Gonyaulacysta ceratophora</i> (Cookson & Eisenack 1960) comb. nov., emend. nov.	PALYNOLOGY			English	Article							GUSTAV GROUP; BAY	The Late Jurassic (early Oxfordian to earliest Tithonian) dinoflagellate cyst Scriniodinium ceratophorum Cookson & Eisenack 1960 from Australia was originally described as having smooth walls and lacking tabulation except for the archeopyle and the cingulum. The type is an atypical end member of this distinctive species; most forms have partially developed tabulation. The species is closely related to Gonyaulacysta jurassica (Deflandre 1939) Norris & Sarjeant 1965. It has a relatively large epicyst, an apparently similar tabulation pattern to Gonyaulacysta jurassica and exhibits neutral torsion. Scriniodinium ceratophorum is therefore transferred to Gonyaulacysta and emended to include partially tabulate forms.	British Geol Survey, Kingsley Dunham ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk						[Anonymous], 1978, ANALYSES PREPLEISTOC; Brenner W., 1988, TUBINGER MIKROPALAON, V6; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; DAVEY RJ, 1988, GEOLOGICAL SURVEY PA, V13; DEFLANDRE G, 1964, CR HEBD ACAD SCI, V258, P5027; DETTMANN ME, 1987, BRIT ANTARCT SURV B, P13; DUCHENE RJ, 1986, B CTR RECH EXPLORATI, V12; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Foster C, 2001, MEMOIR ASS AUSTRALAS, V24, pi; Helby R., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P125; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; HELENES J, 1986, Palynology, V10, P73; Helenes Javier, 1997, Palynology, V21, P173; KEATING JM, 1992, ANTARCT SCI, V4, P279, DOI 10.1017/S0954102092000440; Patillo J., 1990, APEA J, V30, P27, DOI DOI 10.1071/AJ89002; Riding J.B., 1992, P7; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P141; Riding James B., 2002, Palynology, V26, P5, DOI 10.2113/0260005; Riding JB, 1998, CRETACEOUS RES, V19, P87, DOI 10.1006/cres.1998.0098; RIDING JB, 1992, NEWSL STRATIGR, V26, P19; Riding JB, 1997, SCOT J GEOL, V33, P59, DOI 10.1144/sjg33010059; Riding JB, 2002, CRETACEOUS RES, V23, P739, DOI 10.1006/cres.2002.1024; Sarjeant W.A.S., 1982, AM ASS STRATIGRAPHIC, V9; SARJEANT WAS, 1969, B BR MUS NAT HIST S, V3, P7; Whittam D.B., 1996, APPEA J, V36, P209; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; WILSON GJ, 1982, NZ GEOLOGICAL SURVEY, V59; [No title captured]	29	6	6	0	1	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2005	29						13	22		10.2113/29.1.13	http://dx.doi.org/10.2113/29.1.13			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	057PR					2025-03-11	WOS:000238608200002
J	Schrank, E				Schrank, Eckart			Dinoflagellate cysts and associated aquatic palynomorphs from the Tendaguru Beds (Upper Jurassic-Lower Cretaceous) of southeast Tanzania	PALYNOLOGY			English	Review							PALYNOLOGY; ARGENTINA; FRANCE; MEMBER	Dinoflagellate cysts and associated aquatic palynomorphs have been recovered from the dinosaur-bearing Tendaguru Beds (Upper Jurassic-Lower Cretaceous) at Tendaguru, a hill in southeast Tanzania. Palynofloras from these beds are generally dominated by pollen grains of Mesozoic conifers (mainly Classopollis), but dinoflagellate cysts occur sporadically throughout the succession. They attain highest relative abundances and diversities in the marine intercalations between the Saurian Beds, namely in the Nerinea Bed (between the Lower and Middle Saurian Beds) and even more so in the Trigonia smeei Bed (between the Middle and Upper Saurian Beds). Peak levels of dinoflagellate cysts correspond to times when the shallow marine environments of the Nerinea and Trigonia smeei Beds had access to the open sea, while scarcity or absence of dinoflagellate cysts in the Saurian Beds is related to intervals of restricted access to the sea in tidal flat and coastal plain environments. Four informal dinoflagellate cyst assemblages can be distinguished in the Tendaguru Beds: (1) the Rigaudella aemula-Chlamydophorella wallala assemblage from the Nerinea Bed (Oxfordian to Kimmeridgian); (2) the Endoscrinium attadalense-Ctenidodinium sellwoodii group assemblage from the Middle Saurian Bed (late Kimmeridgian); (3) the Dingodinium jurassicum-Kilwacysta assemblage from the Trigonia smeei Bed (Tithonian); (4) the Muderongia-Oligosphaeridium assemblage probably from the Trigonia schwarzi Bed at Namunda Plateau, 8 km south of Tendaguru (late Valanginian to Hauterivian). The age determinations are based on correlation with known dinoflagellate cyst ranges and zonations in Australia, Europe and elsewhere. However, the stratigraphic position and previous biostratigraphic interpretations of the Tendaguru Beds based on ammonites, charophytes and ostracods were also taken into consideration. One new genus (Kilwacysta), three new species (Kilwacysta multiramosa, Kilwacysta semiseptata and Protobatioladinium lindiensis) and the new combination Barbatacysta capitata are proposed.	Tech Univ Berlin, Inst Angew Geowissensch, D-10587 Berlin, Germany	Technical University of Berlin	Schrank, E (通讯作者)，Tech Univ Berlin, Inst Angew Geowissensch, Sekr EB10 Enrst Reuter Pl 1, D-10587 Berlin, Germany.	e.schrank@tu-berlin.de						ABERHAN M, 2002, PALAEOECOLOGY DEPOSI, V5, P19; [Anonymous], 1998, GEOLOGICAL TIME TABL; Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; BALDUZZI A, 1992, J AFR EARTH SCI, V15, P405, DOI 10.1016/0899-5362(92)90025-8; Batten D., 1996, Palynology: principles and applications, P1011; BATTEN D J, 1988, Cretaceous Research, V9, P337, DOI 10.1016/0195-6671(88)90007-9; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BELOW R, 1982, JB GEOLOGIE PALAONTO, P137; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BOLTENHAGEN E, 1977, CAHIERS PALEONTOLOGI; Borel CM, 2003, AMEGHINIANA, V40, P531; BRENNER W, 1988, MORPHOLOGIE OKOLOGIE, V6; Burger D., 1994, AGSO Journal of Australian Geology and Geophysics, V15, P89; Burger D., 1996, Palynology, V20, P49; CHEN YY, 1982, MICROPALEONTOLOGY, V28, P31, DOI 10.2307/1485359; CHEN YY, 1978, THESIS U ARIZONA; CLARKE RFA, 1967, VERHANDELINGEN KONIN, V24; Conway B.H., 1990, ISR GEOL SURV B, V82, P1; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; Costa L. 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J	Riding, JB				Riding, James B.			Middle and Upper Jurassic (Callovian to Kimmeridgian) palynology of the onshore Moray Firth Basin, northeast Scotland	PALYNOLOGY			English	Review							STAFFIN BAY; FLORA; SUTHERLAND; BRORA; MICROPLANKTON; ASSEMBLAGES; BOUNDARY; SCOTTISH; POLLEN; FACIES	The Brora Coal, Brora Argillaceous, Brora Arenaceous, Balintore and Kimmeridge Clay formations of the onshore Moray Firth Basin represent an important Middle to Upper Jurassic (Callovian to Lower Kimmeridgian) reference section close to hydrocarbon-rich North Sea basins. This composite succession at Brora and Balintore is c. 233 m thick; it is mudstone/siltstone-dominated and largely rich in zonal and subzonal ammonites. For example, the Callovian succession at Brora is virtually complete, with coverage of all seven ammonite zones. All the five formations examined have yielded abundant palynofloras. The lithostratigraphic units sampled, except the Brora Coal Formation, have yielded rich associations of dinoflagellate cysts. The majority of the Inverbrora Member of the Brora Coal Formation at its type section at Brorais of early Callovian age based on dinoflagellate cysts; this member yielded Meiourogonyaulax caytonensis and Mendicodinium groenlandicum and these species preclude a Bathonian age. This member has been previously attributed to the late Bathonian. Dinoflagellate cysts are diverse and abundant in the overlying Brora Argillaceous to Kimmeridge Clay formations, therefore indicating open marine conditions. The stratigraphic distributions and relative proportions of these Callovian to Lower Kimmeridgian dinoflagellate cyst floras are largely consistent with those reported elsewhere in northern Europe, and the established dinoflagellate cyst biozonations can be readily applied to the Inner Moray Firth Basin. Some taxa, such as Gonyaulacysta dentata, are of distinct Boreal affinity. Furthermore, some minor stratigraphic anomalies were noted, including the range base of Scriniodinium crystallinum being in the early Oxfordian at Balintore. In England and Germany, this bioevent occurs in the late Callovian. Some notable dinoflagellate cyst abundance phenomena were observed. An example of this is the prominence of Korystocysta spp. in the Middle Callovian. This and other quantitative phenomena are of correlative significance. Marine palynomorph diversity increased markedly during the Callovian, stabilizing in the Lower Oxfordian. A suite of characteristic dinoflagellate cysts became extinct in the Middle Oxfordian, and some typically Late Jurassic elements became more prominent at this time. The early Kimmeridgian palynofloras from Ethic are entirely typical of this interval elsewhere in Europe.	British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk						ANDREWS IJ, 1990, UNITED KINGDOM OFFSH; [Anonymous], T EDINBURGH GEOLOGIC; [Anonymous], INT S JUR STRAT ERL; Arkell W.J., 1942, Q J GEOLOGICAL SOC L, V98, P187; Arkell W.J., 1933, The Jurassic System in Great Britain; Bailey E.B., 1932, Transaction of the Royal Society of Edinburgh, V57, P429, DOI DOI 10.1017/S0080456800016768; Barron H.F., 1989, Northwest European Micropalaeontology and Palynology, P193; Batten D.J., 1978, CONTINENTAL SHELF I, V100, P97; BATTEN DJ, 1986, SCOT J GEOL, V22, P85, DOI 10.1144/sjg22010085; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Berridge N. 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J	Heilmann-Clausen, C; Van Simaeys, S				Heilmann-Clausen, Claus; Van Simaeys, Stefaan			Dinoflagellate cysts from the Middle Eocene to ?lowermost Oligocene succession in the Kysing Research Borehole, Central Danish Basin	PALYNOLOGY			English	Review							NORTH-SEA; SOUTHERN ENGLAND; BIOSTRATIGRAPHY; STRATIGRAPHY; TRANSITION; ATLANTIC; ZONATION; NEOGENE; UPLIFT; AREA	Rich and well-preserved assemblages of organic walled dinoflagellate cysts in 50 samples from a 154 m thick and almost complete, Middle Eocene to ?lowermost Oligocene section from the Kysing Research Borehole in eastern Jylland, Denmark are systematically described. One genus Costacysta gen. nov., and twelve species Chiropteridium eocaenicum sp. nov., Costacysta bucina gen. et sp. nov., Distatodinium pilosum sp. nov., Echinidinium? lucidum sp. nov., Hapsocysta kysingensis sp. nov., Horologinella?pentagonalis sp. nov., Operculodinium eisenackii sp. nov., Phthanoperidinium cornutum sp. nov., Selenopemphix septum sp. nov., Svalbardella partimtabulata sp. nov., Thalassiphora gracilis sp. nov. and Thalassiphora microperforata sp. nov. are formally described. The genus Hapsocysta is emended, and is considered to be a senior synonym of Piccoladinium. The gradual change of the dinoflagellate cyst assemblages in this section demonstrates that sedimentation was almost continuous during the time span of ca. 12 Ma. The biostratigraphic resolution based on dinoflagellate cyst events is generally finer than the calcareous nannofossil NP biozonation. A comparison with published dinoflagellate cyst data from the Norwegian-Greenland Sea shows that several important events are mainly synchronous throughout the region, suggesting a general similarity of the water masses. An isolated occurrence of Svalbardella suggests a short cooling event during early Bartonian times. The palynofacies in most of the section is almost purely of pelagic type. A more proximal, mid shelf palynofacies and a distinctive episode of reworking coincide with the Upper Eocene Moesgaard Clay and indicate a brief, but rather large sea level fall during the deposition of this unit. The Eocene/Oligocene boundary is tentatively identified near the base of the Viborg Formation, and approximately coincides with increased reworking of dinoflagellate cysts and a strong increase in bisaccate pollen, indicating more proximal conditions and possibly also a climatic cooling.	Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; Univ Loughborough, B-3000 Louvain, Belgium	Aarhus University	Heilmann-Clausen, C (通讯作者)，Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark.	claus.heilmann@geo.au.dk; stefaan.vansimaeys@geo.kuleuven.ac.be	Heilmann-Clausen, Claus/A-4848-2012					Agelopoulos J, 1967, THESIS EBERHARD KARL; ANDERSEN HL, 1977, DANSK GEOLOGISK FORE, P69; [Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1988, Geol. 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J	Ratkova, TN; Wassmann, P				Ratkova, TN; Wassmann, P			Sea ice algae in the White and Barents seas: composition and origin	POLAR RESEARCH			English	Article							PHYTOPLANKTON; GREENLAND; PROTOZOOPLANKTON; ASSEMBLAGES; BIOMASS; DIATOMS; CARBON; VOLUME; BIOTA	To examine algae populations, three expeditions (in March 2001, April 2002 and February 2003) were conducted in the Guba Chupa (Chupa Estuary; north-western White Sea), and one cruise was carried out in the open part of the White Sea in April 2003 and in the northern part of the Barents Sea in July 2001. Sea ice algae and phytoplankton composition and abundance and the content of sediment traps under the land-fast ice in the White Sea and annual and multi-year pack ice in the Barents Sea were investigated. The community in land-fast sea ice was dominated by pennate diatoms and its composition was more closely related to that of the underlying sediments than was the community of the pack ice, which was dominated by flagellates, dinoflagellates and centric diatoms. Algae were far more abundant in land-fast ice: motile benthic and ice-benthic species found favourable conditions in the ice. The pack ice community was more closely related to that of the surrounding water. It originated from plankton incorporation during sea ice formation and during seawater flood events. An additional source for ice colonization may be multi-year ice. Algae may be released from the ice during brine drainage or sea ice melting. Many sea ice algae developed spores before the ice melt. These algae were observed in the above-bottom sediment traps all year around. Three possible fates of ice algae can be distinguished: 1) suspension in the water column, 2) sinking to the bottom and 3) ingestion by herbivores in the ice, at the ice-water interface or in the water column.	Russian Acad Sci, Shirshov Inst Oceanol, Moscow 117997, Russia; Univ Tromso, Norwegian Coll Fishery Sci, NO-9037 Tromso, Norway	Russian Academy of Sciences; Shirshov Institute of Oceanology; UiT The Arctic University of Tromso	Russian Acad Sci, Shirshov Inst Oceanol, Nakhimovsky Ave 36, Moscow 117997, Russia.	trat@orc.ru						Buck KR, 1998, POLAR BIOL, V20, P377, DOI 10.1007/s003000050317; DRUZHKOV NV, 2003, OPYT SYSTEMMYKH OKEA, P325; Gogorev R. M., 1998, NEWS SYSTEMATICS LOW, V32, P8; Gradinger R, 1999, MAR BIOL, V133, P745, DOI 10.1007/s002270050516; Gradinger R, 1999, DEEP-SEA RES PT II, V46, P1457, DOI 10.1016/S0967-0645(99)00030-2; Gradinger R, 1998, J PLANKTON RES, V20, P871, DOI 10.1093/plankt/20.5.871; Hendey N. 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En Analyse Af Forekomsten Af Alger Og Heterotrofe Protister (Ekskl. Ciliater) i Kattegat; THRONDSEN J, 2003, NORSK KYST PLANKTON; Tomas C.R., 1997, IDENTIFYING MARINE P IDENTIFYING MARINE P, P858, DOI DOI 10.1016/B978-012693018-4/50004-5; TUSCHLING K, 2000, OEKOLOGIE PHYTOPLANK, P347; ULANOVA AA, 2003, THESIS SAINT PETERSB; von Quillfeldt CH, 2000, BOT MAR, V43, P499, DOI 10.1515/BOT.2000.050; von Quillfeldt CH, 2003, POLAR BIOL, V26, P806, DOI 10.1007/s00300-003-0549-1; Von Quillfeldt CH, 1996, THESIS U TROMSO; vonQuillfeldt CH, 1997, J MARINE SYST, V10, P211, DOI 10.1016/S0924-7963(96)00056-5; Weissenberger J, 1998, POLAR BIOL, V20, P178, DOI 10.1007/s003000050294; Weissenberger J, 1998, POLAR BIOL, V19, P151, DOI 10.1007/s003000050228; Zhitina L. S., 1990, BIOL MONITORING PRIB, V41-49	51	60	69	1	28	OPEN ACADEMIA AB	SPANGA	STORMBYVAGEN 6, SPANGA, SE-163 55, SWEDEN	0800-0395	1751-8369		POLAR RES	Polar Res.		2005	24	1-2					95	110		10.1111/j.1751-8369.2005.tb00143.x	http://dx.doi.org/10.1111/j.1751-8369.2005.tb00143.x			16	Ecology; Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Oceanography	948TP					2025-03-11	WOS:000230738900009
J	Head, MJ; Seidenkrantz, MS; Janczyk-Kopikowa, Z; Marks, L; Gibbard, PL				Head, MJ; Seidenkrantz, MS; Janczyk-Kopikowa, Z; Marks, L; Gibbard, PL			Last Interglacial (Eemian) hydrographic conditions in the southeastern Baltic Sea, NE Europe, based on dinoflagellate cysts	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	22nd Conference of the Baltic Oceanographers (CBO)/Baltic Sea Science Congress (BSSC)	NOV 25-29, 2001	STOCKHOLM, SWEDEN	Stockholm Marine Res Ctr, Konung Carl XVI Gustafs Stiftelse Forskning Utbildning, Marianne & Marcus Wallenberg Fdn, Swedish Res Council, Swedish Environm Protect Agcy, WWF Sweden, Henrik Granholms Stiftelse, Natl Board Fisheries, Umea Marine Res Ctr, Swedish Meteorol & Hydrol Inst			RECENT SEDIMENTS; LIFE-CYCLE; MORPHOLOGY; CLIMATE; DENMARK; WESTERN; SALINITY; GERMANY; RECORD	A rich organic-walled dinoflagellate cyst and pollen record from the Licze borehole in northern Poland has been used to reconstruct the hydrographic history of the southeastern Baltic Sea during the Last Interglacial (Eemian Stage, Late Pleistocene). Warm, saline waters (ca. 10-15 psu) entered the site from the North Sea within the first few hundred years of the Eemian, corresponding to the Pinus Betula (E1) or Pinus-Betula-Ulmus (E2) regional pollen assemblage zones (RPAZ). By about 300 years (beginning of RPAZ E3), dinoflagellate cyst assemblages were already indicating summer sea-surface salinities in excess of about 15 psu and temperatures that perhaps exceeded 27degreesC. Warm and saline conditions of 15-20 psu or more, at least twice present levels, persisted throughout the early Eemian. A rise in sea level at Licze appears to correlate with a similar event in eastern Denmark, as both coincide with the increase in Corylus (ca. 750 years into the interglacial). This sea-level rise might therefore have a basinwide extent, and appears to correspond to an opening of the Danish Belts. There is little if any evidence of arctic waters throughout the sequence. Whereas dinoflagellate cysts reflect sustained high salinites within the upper water column, a concomitant increase in abundance of the chlorococcalean alga Pediastrum within the Carpinus-Corylus-Alnus (E5) RPAZ indicates an escalating freshwater input, presumably from the proto-Vistula whose mouth was nearby. This suggests the development of a thin, seasonal, low-salinity surface layer below which dinoflagellates lived in more saline waters. Increasing fluvial influence suggests shallowing through RPAZ E5. This study is the first to document dinoflagellate cysts from the Eemian of the southeastern Baltic Sea, and reveals a flora with distinctive Lusitanian/Mediterranean affinities. (C) 2004 Elsevier Ltd and INQUA. All rights reserved.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; Polish Geol Inst, PL-00975 Warsaw, Poland; Univ Warsaw, Inst Geol, PL-02089 Warsaw, Poland	University of Cambridge; Aarhus University; Polish Geological Institute - National Research Institute; Polish Geological Institute - National Research Institute; University of Warsaw	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk	Gibbard, Phil/AAU-8014-2021; Marks, Leszek/ABF-3641-2020; Seidenkrantz, Marit-Solveig/A-3451-2012; Marks, Leszek/F-2981-2013	Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Marks, Leszek/0000-0002-4507-1828				Andersen S. T., 1961, Danmarks Geologiske Undersogelse II.Raekke, V75, P1; Andersen S. 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Int.		2005	130						3	30		10.1016/j.quaint.2004.04.027	http://dx.doi.org/10.1016/j.quaint.2004.04.027			28	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	889DR					2025-03-11	WOS:000226424200002
C	Ilyina VI; Nikitenko, BL; Glinskikh, LA		Powell, AJ; Riding, JB		Ilyina, VI; Nikitenko, BL; Glinskikh, LA			Foraminifera and dinotlagellate cyst zonation and stratigraphy of the Callovian to Volgian reference section in the Tyumenskaya superdeep well (West Siberia, Russia)	RECENT DEVELOPMENTS IN APPLIED BIOSTRATIGRAPHY	MICROPALAEONTOLOGICAL SOCIETY SPECIAL PUBLICATIONS		English	Proceedings Paper	Joint Meeting of the TMS/35th Annual Meeting of the American-Association-of-Stratigraphic-Palynologists/North American Micropaleontology Section of the SEPM	SEP 11-13, 2002	Univ Coll London, London, ENGLAND	TMS, Amer Assoc Stratigraph Palynol, SEPM, Amer Micropaleontol Sect	Univ Coll London		DINOFLAGELLATE CYSTS	The Callovian to Volgian section in the Tyumenskaya superdeep well SDW-6 is very important for the development and improvement of Jurassic biostratigraphy in West Siberia. It was drilled with almost continuous recovery of core (about 200 m), which is characterized by rich assemblages of microfossils. In this paper the results of micropalaeontological and palynological studies of the most complete Jurassic succession in the north of West Siberia are discussed, taking into consideration the problems of bio- and lithostratigraphy of the region. The comprehensive analysis of the stratigraphical distribution of the different microfossil groups (foraminifers, microforaminifers, ostracods, dinoflagellate cysts, acritarchs, prasinophytes, spores and pollen) allows the creation of a detailed zonation. For the first time. an almost continuous sequence of dinoflagellate cyst zones for the Callovian-Middle Volgian has been established in the north of West Siberia, providing the basis for development of the Jurassic dinofiagellate cyst zonation in West Siberia. Distinctive features of microbenthos communities and microphytoplankton associations reflecting biofacies have been studied. The pattern of distribution of microbenthic communities and microphytoplankton associations, depending on changes of transgressive-regressive events and palaeoenvironments in the Callovian to Volgian, has been established.	RAS, Siberian Branch, Inst Petr Geol, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Ilyina VI (通讯作者)，RAS, Siberian Branch, Inst Petr Geol, Koptyug Av 3, Novosibirsk 630090, Russia.		Nikitenko, Boris/S-9028-2017; Glinskikh, Larisa/Y-8646-2018					Beisel A.L., 2002, RUSSIAN GEOLOGY GEOP, V43, P763; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BULYNNIKOVA SP, 1990, ATLAS MOLLYUSKOV FOR, V1, P3; DAVIES EH, 1983, GEOLOGICAL SURVEY CA, V359, P3; DIKOVSKII AA, 1996, SOSTOYANNII VYPOLNEN, P63; EKHLAKOV YA, 1996, TYUMENSKAYA SVERKHGL, P79; EKHLAKOV YA, 1991, SOV GEOL, V8, P80; FENSOME RA, 1993, SPECIAL PUBLICATION, V7, P3; Fisher M.J., 1980, P 4 INT PAL C LUCKN, V2, P313; GLINSKIKH LA, 1999, RUSSIAN GEOLOGY GEOP, V40, P1043; Ilyina V.I., 1988, Palynology in the USSR, P103; ILYINA VI, 1998, AKTUALNYE VOPROSY GE, V1, P215; ILYINA VI, 1985, JURASSIC PALYNOLOGY, P3; ILYINA VI, 1991, STRATIGRAFIYA PALEOG; JOHNSON CD, 1973, B CAN PETROL GEOL, V21, P179; KAPLAN ME, 1973, REPORTS RES ACAD USS, V209, P691; KIRICHKOVA AI, 1999, STRATIGRAFIYA GEOLOG, V7, P71; KONTOROVICH AE, 1975, GEOLOGY OIL GAS W SI, P3; KONTOROVICH AE, 2001, MAT M TECTONICS NEOG, V1, P307; LEBEDEV IV, 1972, STRATIGRAPHY PALAEON, P3; Lebedeva NK, 1999, GRANA, V38, P134, DOI 10.1080/00173139908559222; LENTIN JK, 1993, AM ASS STRATIGRAPHIC, V28, P3; LUTOVA ZV, 1981, STRATIGRAPHY FORAMIN, P3; MAZUR VB, 1996, PERM KAMSKIJ NAUCHNO, P3; Meledina S.V., 1998, Stratigrafiya Geologicheskaya Korrelyatsiya, V6, P29; MELEDINA SV, 1994, BOREAL MIDDLE JURASS, P1; Mickey MB, 1998, OIL GAS J, V96, P84; NESTEROV II, 1991, 5 INT REG STRAT M ME, P3; Pinous OV, 1999, MAR PETROL GEOL, V16, P245, DOI 10.1016/S0264-8172(98)00078-6; Poulsen Niels E., 1993, Acta Geologica Polonica, V43, P251; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; RIDING J B, 1984, Palynology, V8, P195; Riding J.B., 1999, American Association of Stratigraphic Palynologists Contributions Series, V36, P1; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; RILEY L A, 1982, Palynology, V6, P193; SAKS VN, 1969, OPORNYJ RAZREZ VERHN, P3; SAKS VN, 1976, STRATIGRAPHY JURASSI, P3; SHAROVSKAYA NV, 1968, NAUCHNO ISSLEDOVATEL, V23, P106; SHURYGIN BN, 2000, STRATIGRAPHY OIL GAS, P3; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; Smelror M., 1993, Norwegian Petroleum Society Special Publications, V2, P495; Smelror M., 1988, Gronlands Geologiske Undersogelse Rapport, V137, P135, DOI [DOI 10.34194/RAPGGU.V137.8019, 10.34194/rapggu.v137.8019]; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P3; Woollam R., 1983, I GEOLOGICAL SCI REP, V83; Zakharov V.A., 1997, RUSS GEOL GEOPHYS+, V38, P965	46	25	28	0	0	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			1-86239-187-4	MICROPAL SOC SPEC PU			2005							109	144						36	Geology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BDM08					2025-03-11	WOS:000234239500008
C	Dale, B; Dale, AL; Prince I		Powell, AJ; Riding, JB		Dale, B; Dale, AL; Prince, I			Statistical modelling of ecological signals: a new method for biostratigraphy	RECENT DEVELOPMENTS IN APPLIED BIOSTRATIGRAPHY	MICROPALAEONTOLOGICAL SOCIETY SPECIAL PUBLICATIONS		English	Proceedings Paper	Joint Meeting of the TMS/35th Annual Meeting of the American-Association-of-Stratigraphic-Palynologists/North American Micropaleontology Section of the SEPM	SEP 11-13, 2002	Univ Coll London, London, ENGLAND	TMS, Amer Assoc Stratigraph Palynol, SEPM, Amer Micropaleontol Sect	Univ Coll London		ORDINATION	Research over the past few decades has shown that recent marine dinoflagellate cyst assemblages are strongly influenced by environmental factors, and statistical modelling of ecological signals (SMES) therefore has potential application for interpretation of fossil dinocysts in biostratigraphy. Towards this end a global database of recent cyst distributions from known environments has been developed using statistical methods that most accurately reflect and quantify the ecological signals expressed by the cysts. The first test is reported here of the application of SMES to industrial biostratigraphy using a palynology dataset from four wells along an onshore-offshore transect from the Norwegian North Sea provided by Statoil. The wells were part of a larger study on palaeoenvironments previously completed by Statoil on approximately 48 wells, where some of the traditional multivariate statistical methods had been tried but without success. The palaeoenvironment was thus partly understood, allowing the SMES method to be tested against a control. Correspondence analysis on the dinocyst data from each well allowed the identification of the statistically most important species, and the relative positions of these species along the two most important axes suggested ecological trends (the coastal/occanic being most dominant). Tracking these down-hole showed two major shifts in each well that could be correlated between all wells; the shifts corresponded to major flooding surfaces previously identified, and suggested orientation of the well sites relative to a palaeo-shoreline. This first test strongly suggests that these methods offer a much quicker, and more robust application for palaeoenvironmental interpretations from the dinocysts in biostratigraphic datasets.	Univ Oslo, Dept Geosci, N-0316 Oslo, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Dept Geosci, PB 1047, N-0316 Oslo, Norway.	Barrie.dale@geo.uio.no						[Anonymous], 1996, Palynology: principles and applications; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Dale Amy L., 2002, P259; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; HILL MO, 1973, J ECOL, V61, P237, DOI 10.2307/2258931; HILL MO, 1980, VEGETATIO, V42, P47, DOI 10.1007/BF00048870; Jongman R.H.G., 1995, Data Analysis in Community and Landscape Ecology; LAURSEN GV, 2002, PALAEOENVIRONMENTS M, P47; ter Braak C.J.F., 1996, UNIMODAL MODELS RELA; Ter Braak C.J.F, 1998, CANOCO RELEASE 4 REF; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7	12	7	7	0	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND			1-86239-187-4	MICROPAL SOC SPEC PU			2005							179	203						25	Geology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BDM08					2025-03-11	WOS:000234239500011
J	Stickley, CE; Brinkhuis, H; Schellenberg, SA; Sluijs, A; Röhl, U; Fuller, M; Grauert, M; Huber, M; Warnaar, J; Williams, GL				Stickley, CE; Brinkhuis, H; Schellenberg, SA; Sluijs, A; Röhl, U; Fuller, M; Grauert, M; Huber, M; Warnaar, J; Williams, GL			Timing and nature of the deepening of the Tasmanian Gateway -: art. no. PA4027	PALEOCEANOGRAPHY			English	Article						Eocene; Oligocene transition; Tasmanian Gateway; diatoms and dinoflagellate cysts	EOCENE-OLIGOCENE; MIDDLE EOCENE; DINOFLAGELLATE CYSTS; SCOTIA SEA; STRATIGRAPHY; BIOSTRATIGRAPHY; EVOLUTION; DIATOMS	Tectonic changes that produced a deep Tasmanian Gateway between Australia and Antarctica are widely invoked as the major mechanism for Antarctic cryosphere growth and Antarctic Circumpolar Current (ACC) development during the Eocene/Oligocene (E/O) transition (similar to34-33 Ma). Ocean Drilling Program (ODP) Leg 189 recovered near-continuous marine sedimentary records across the E/O transition interval at four sites around Tasmania. These records are largely barren of calcareous microfossils but contain a rich record of siliceous- and organic-walled marine microfossils. In this study we integrate micropaleontological, sedimentological, geochemical, and paleomagnetic data from Site 1172 (East Tasman Plateau) to identify four distinct phases (A-D) in the E/O Tasmanian Gateway deepening that are correlative among ODP Leg 189 sites. Phase A, prior to similar to35.5 Ma: minor initial deepening characterized by a shallow marine prodeltaic setting with initial condensation episodes. Phase B, similar to35.5-33.5 Ma: increased deepening marked by the onset of major glauconitic deposition and inception of energetic bottom-water currents. Phase C, similar to33.5-30.2 Ma: further deepening to bathyal depths, with episodic erosion by increasingly energetic bottom-water currents. Phase D, <30.2 Ma: establishment of stable, open-ocean, warm-temperate, oligotrophic settings characterized by siliceous- carbonate ooze deposition. Our combined evidence indicates that this early Oligocene Tasmanian Gateway deepening initially produced an eastward flow of relatively warm surface waters from the Australo-Antarctic Gulf into the southwestern Pacific Ocean. This "proto-Leeuwin'' current fundamentally differs from previous regional reconstructions of eastward flowing cool water (e.g., a "proto-ACC'') during the early Oligocene and thereby represents an important new constraint for reconstructing regional- to global-scale dynamics for this major global change event.	Cardiff Univ, Sch Earth Ocean & Planetary Sci, Cardiff CF10 3YE, S Glam, Wales; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 Utrecht, Netherlands; San Diego State Univ, Dept Geol Sci, San Diego, CA 92182 USA; Univ Bremen, Dept Geosci, RCOM, D-330440 Bremen, Germany; Univ Hawaii Manoa, Sch Ocean & Earth Sci & Technol, Hawaii Inst Geophys & Planetol, Honolulu, HI 96822 USA; Univ Copenhagen, Dept Geog, DK-1350 Copenhagen, Denmark; Purdue Univ, W Lafayette, IN 47907 USA; Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada	Cardiff University; Utrecht University; California State University System; San Diego State University; University of Bremen; University of Hawaii System; University of Hawaii Manoa; University of Copenhagen; Purdue University System; Purdue University; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Cardiff Univ, Sch Earth Ocean & Planetary Sci, Cardiff CF10 3YE, S Glam, Wales.	cathy@earth.cf.ac.uk	Brinkhuis, Henk/B-4223-2009; Sluijs, Appy/B-3726-2009; Rohl, Ursula/G-5986-2011; Huber, Matthew/A-7677-2008	Brinkhuis, Henk/0000-0003-0253-6610; Sluijs, Appy/0000-0003-2382-0215; Rohl, Ursula/0000-0001-9469-7053; Huber, Matthew/0000-0002-2771-9977				Agrawal Y.C., 1991, PRINCIPLES METHODS A, P119, DOI [10.1017/CBO9780511626142.012, DOI 10.1017/CBO9780511626142.012]; [Anonymous], ANTARCTIC RES SERIES; [Anonymous], P ODP SCI RESULTS; [Anonymous], NZ DEP SCI IND RES B; [Anonymous], DSIR B; Bains S, 1999, SCIENCE, V285, P724, DOI 10.1126/science.285.5428.724; Baldauf J.G., 1992, EOCENE OLIGOCENE CLI, P310; Baldauf J.G., 1991, PROC OCEAN DRILL SCI, V119, P547, DOI [10.2973/odp.proc.sr.119.135.1991, DOI 10.2973/ODP.PROC.SR.119.135.1991]; Barker PF, 2001, EARTH-SCI REV, V55, P1, DOI 10.1016/S0012-8252(01)00055-1; BARRON JA, 2004, IN PRESS COMMEMORATI; BATTARBEE R.W., 2003, Handbook of Holocene Palaeoecology and Palaeohyrology, P527, DOI DOI 10.1127/NOVA_HEDWIGIA/2015/0263; BATTARBEE RW, 1982, LIMNOL OCEANOGR, V27, P184, DOI 10.4319/lo.1982.27.1.0184; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bohaty SM, 2003, GEOLOGY, V31, P1017, DOI 10.1130/G19800.1; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; BRINKHUIS H, 1992, VOLUME NEOGENE QUATE, P219; CLOWES C D, 1985, Palynology, V9, P27; Cookson I. 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ODP, V189, P1, DOI DOI 10.2973/ODP.PROC.SR.189.111.2004; Stover L.E., 1975, Geoscience Man, V11, P35; Stover L.E., 1996, Palynology: Principles and Applications, V2, P641; Truswell EM, 1997, AUST J EARTH SCI, V44, P633, DOI 10.1080/08120099708728342; WILLIAMS GL, 1998, CONTRIB SER AM ASS S, V34; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; WILSON GRAEME J., 1967, NZ J BOT, V5, P57; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321; Wrenn J H., 1998, Terra Antarctica, V5, P553; WRENN JH, 1982, SCIENCE, V216, P187, DOI 10.1126/science.216.4542.187; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zachos JC, 1996, PALEOCEANOGRAPHY, V11, P251, DOI 10.1029/96PA00571	78	206	225	1	57	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0883-8305	1944-9186		PALEOCEANOGRAPHY	Paleoceanography	DEC 18	2004	19	4							PA4027	10.1029/2004PA001022	http://dx.doi.org/10.1029/2004PA001022			18	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	881QY		Green Submitted, Bronze, Green Published			2025-03-11	WOS:000225884500002
J	Christensen, JT; Cedhagen, T; Hylleberg, J				Christensen, JT; Cedhagen, T; Hylleberg, J			Late-Holocene salinity changes in Limfjorden, Denmark	SARSIA			English	Article						macrofauna; salinity changes; dinoflagellate cysts; Limtjorden; Holocene	C-14 DATA	Sub-fossil remains of macrofauna extracted from a 5.3m sediment core in the central part of Limfjorden indicate marked changes in salinity. Sub-fossils in the lower part of the core indicate marine conditions similar to those of the present North Sea, while the upper 2 m of the core represents periods of brackish conditions alternating with periods of intermediate salinity similar to the present condition, indicative of alternating opening and closure of the fjord to the west. Precise C-14 dating of changes is hampered by variable marine reservoir effects and the addition of old carbonate from ground-water runoff. Salinity indications from dinoflagellate cyst assemblages from this core, but published elsewhere, are in accordance with those from macrofauna assemblages.	Aarhus Univ, Inst Biol Sci, Dept Marine Ecol, DK-8000 Aarhus C, Denmark	Aarhus University	Aarhus Univ, Inst Biol Sci, Dept Marine Ecol, DK-8000 Aarhus C, Denmark.	tang@biology.au.dk	Christensen, Jens/J-7280-2013; Cedhagen, Tomas/J-6426-2013	Christensen, Jens/0000-0003-2370-2702; Cedhagen, Tomas/0000-0003-4550-8177				[Anonymous], RANDERS FJORDS NATUR; CHRISTIANSEN C, 1990, CATENA S, V18, P61; Collin J. S., 1884, LIMFJORDENS TIDLIGER; CRISP DJ, 1964, J ANIM ECOL, V33, P165, DOI 10.2307/2355; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Head M.J., 1996, Palynology: Principles and Applications, P1197; HeierNielsen S, 1995, RADIOCARBON, V37, P875, DOI 10.1017/S0033822200014958; KRISTENSEN P, 1995, HOLOCENE, V5, P313, DOI 10.1177/095968369500500306; Lowe JJ, 2000, RADIOCARBON, V42, P53, DOI 10.1017/S0033822200053054; Nielsen S. H, 1992, DANSK GEOLOGISK FORE, P39; Nordberg K, 1991, PALEOCEANOGRAPHY, V6, P461, DOI 10.1029/91PA01132; NORDBERG K, 1988, MAR GEOL, V83, P135, DOI 10.1016/0025-3227(88)90056-4; Petersen, 1985, J DANISH ARCHAEOLOGY, V4, P7, DOI [10.1080/0108464X.1985.10589932, DOI 10.1080/0108464X.1985.10589932]; Petersen K. S., 1980, DANSK GEOLOGISK FORE, P15; Petersen K.S., 1976, Danm. Geol. Unders, V1975, P75; PETERSEN KS, 1992, NATURE, V359, P679, DOI 10.1038/359679a0; RASMUSSEN E, 1973, Ophelia, V11, P1; STUIVER M, 1977, RADIOCARBON, V19, P355, DOI 10.1017/S0033822200003672; STUIVER M, 1993, RADIOCARBON, V35, P215, DOI 10.1017/S0033822200013904; Tanner W.F., 1993, The Holocene, V3, P220, DOI DOI 10.1177/095968369300300304; Taylor F.J.R., 1987, BOT MONOGR, V21, P399	22	12	12	0	1	TAYLOR & FRANCIS AS	OSLO	KARL JOHANS GATE 5, NO-0154 OSLO, NORWAY	0036-4827			SARSIA	Sarsia	DEC 8	2004	89	6					379	387		10.1080/00364820410002640	http://dx.doi.org/10.1080/00364820410002640			9	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	888LI					2025-03-11	WOS:000226375200002
J	McCarthy, FMG; Findlay, DJ; Little, ML				McCarthy, FMG; Findlay, DJ; Little, ML			The micropaleontological character of anomalous calcareous sediments of late Pliocene through early Pleistocene age below the CCD in the northwestern North Pacific Ocean	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						late cenozoic palynology; planktonic foraminifera; productivity; terrigenous flux; carbonate preservation; matuyama chron	DINOFLAGELLATE CYST ASSEMBLAGES; DEEP-SEA; EQUATORIAL PACIFIC; ATMOSPHERIC TRANSPORT; CALCIUM-CARBONATE; EOLIAN DEPOSITION; POLLEN RECORD; EL-NINO; HISTORY; PRODUCTIVITY	Calcium carbonate was preserved more than I km below the modem calcite compensation depth (CCD) at ODP Site 1179 over several short intervals around 2.5-2.4, 1.65 and 0.9-0.7 Ma. This anomalous preservation resulted from a combination of increased production of planktonic foraminiferal tests at the sea-surface and increased rate of sedimentation to the sea floor. The abundance of dinoflagellate cysts in calcareous sediments records intense plankton blooms, and the preservation of oxidation-susceptible round brown Brigantedinium cysts in foraminifer-rich samples supports the theory of rapid burial. The rise in sea-surface productivity was driven by enhanced flux of continentally derived limiting nutrients, consistent with the pollen evidence of continental aridification, cooling, and an increase in wind strength, The abundant pollen, dominated by steppe herb and montane-boreal conifer taxa, contrasts with lower pollen concentrations dominated by temperate-subtropical deciduous tree and Taxodium-type pollen in non-calcareous sediments. (C) 2004 Elsevier B.V. All rights reserved.	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	francine@craton.geol.broclcu.ca						An ZS, 2000, QUATERNARY SCI REV, V19, P171, DOI 10.1016/S0277-3791(99)00060-8; Andersson C, 1998, MAR GEOL, V150, P51, DOI 10.1016/S0025-3227(98)00053-X; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Archer DE, 2000, GLOBAL BIOGEOCHEM CY, V14, P269, DOI 10.1029/1999GB900053; Archer DE, 1996, GLOBAL BIOGEOCHEM CY, V10, P159, DOI 10.1029/95GB03016; Berger W., 1992, CENTENARY JAPANESE M, P15; Berger W.H., 1979, FORAMINIFERAL ECOLOG, V6; Black DE, 2001, GEOLOGY, V29, P1075, DOI 10.1130/0091-7613(2001)029<1075:PFRTTE>2.0.CO;2; DUCE RA, 1991, LIMNOL OCEANOGR, V36, P1715, DOI 10.4319/lo.1991.36.8.1715; DUCE RA, 1980, SCIENCE, V209, P1522, DOI 10.1126/science.209.4464.1522; Farrell JW, 1989, PALEOCEANOGRAPHY, V4, P447, DOI 10.1029/PA004i004p00447; FINDLAY DJ, 2003, 2003 CANQUA M HAL NS; Hebbeln D, 2000, DEEP-SEA RES PT II, V47, P2101, DOI 10.1016/S0967-0645(00)00018-7; HERGUERA JC, 1994, GEOLOGY, V22, P629, DOI 10.1130/0091-7613(1994)022<0629:GTPDIP>2.3.CO;2; Heusser L. 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Paleoclimatol. Paleoecol.	DEC 2	2004	215	1-2					1	15		10.1016/j.palaeo.2004.07.032	http://dx.doi.org/10.1016/j.palaeo.2004.07.032			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	885WD					2025-03-11	WOS:000226187100001
J	Willumsen, PS				Willumsen, PS			Palynology of the Lower Eocene deposits of northwest Jutland, Denmark	BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK			English	Article						palynology; early Eocene; spores and pollen; Stolle Klint Clay; Fur Formation; tephrachronology; biostratigraphy; correlation		Early Eocene spores and pollen assemblages from the uppermost part of the Stolle Mint Clay and the overlying Fur Formation are diverse and well preserved. The terrestrial microflora comprises 42 species of spores and 108 species of pollen and four spores and pollen zones are established i.e. Interpollis velum-Labrapollis globosus, Basopollis atumenscens, Basopollis orthobasalis and Thomsonipollis magnificus zones. The zones are directly correlated to the existing tephrachronology and stratigraphy. The dinoflagellate cysts assemblages are referred to Zones 6 and 7 of Heilmann-Clausen or the upper part of the Apectodinium hyperacanthum and Glaphyrocysta ordinata Interval Biozone of Powell. A marked shift in the terrestrial and marine palynomorph assemblages takes place at the transition between the two oldest spore and pollen zones at c. 1.2 m below ash layer -19b.	Univ Oslo, Dept Geosci, NO-0316 Oslo, Norway	University of Oslo	Univ Oslo, Dept Geosci, POB 1047, NO-0316 Oslo, Norway.	pi.willumsen@geo.uio.no						Andersen N.M., 1996, NATURENS VERDEN, V11/12, P417; [Anonymous], DANMARKS GEOLOGISK A; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Beyer C, 2001, NEWSL STRATIGR, V39, P1; Boggild O.B., 1918, DANMARKS GEOLOGISKE, V33; Bonde N., 1974, Tertiary Times, V2, P29; BONDE N, 1979, MEDEDELINGEN WERKGRO, V16, P1; BONDE N, 1987, MOLER FOSSILER ISAER; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; CEPEK P, 1989, GEOLOGISCH JB A, V111, P403; Collinson M.E., 2003, Causes and Consequences of Globally Warm Climates in the Early Paleogene, V369, P333; Crouch EM, 2003, PALAEOGEOGR PALAEOCL, V194, P387, DOI 10.1016/S0031-0182(03)00334-1; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; Danielsen M., 1997, AARHUS GEOSCIENCES, P19; DECONINCK J, 1993, B SOC BELG GEOL, V102, P105; Egger H, 2000, B SOC GEOL FR, V171, P207, DOI 10.2113/171.2.207; Fenner J., 1994, AARHUS GEOSCIENSE, V1, P99; FREDERIKSEN N O, 1979, Palynology, V3, P129; Gry H, 1979, DANMARKS GEOLOGISKE, V26; GRY H, 1964, DANSK NATUR DANSK SK, P45; Gry H., 1940, MEDDELELSER DANSK GE, V9, P586; HANSEN M, 1979, B GEOLOGICAL SOC DEN, V27, P89; Heilmann-Clausen C., 1982, Newsletters on Stratigraphy, V11, P55; HEILMANN-CLAUSEN C, 1985, Bulletin of the Geological Society of Denmark, V33, P287; Heilmann-Clausen C, 1994, GFF, V116, P51, DOI 10.1080/11035899409546149; HEILMANNCLAUSEN C, 1995, AARHUS GEOKOMPENDIER, V1, P70; HEILMANNCLAUSEN C, 1988, PALAEOGENE DINOFLA A, V100, P339; Hochuli P.A., 1984, Paleobiologie continentale, V14, P301; KLINT KES, 1995, DANMARKS GEOLOGISK A, V35; Knox R.W.O., 1996, GEOLOGICAL SOC SPECI, V103, P209; KNOX R.W. O'B., 1979, J GEOL SOC LOND, V136, P463; KNOX RWO, 1992, GEOLOGICAL SOC LONDO, V70, P169; KNOX RWO, 1997, AARHUS GEOSCIENCE, V6, P7; KNOX RWO, 1992, LITHOSTRATIGRAPHIC N, pA1; Knox RWO'B, 1989, GEOL JB A, VA111, P217; Krutzsch W., 1971, ATLAS MITTEL JUNGTER; Krutzsch W., 1960, FREIBERGER FORSCH C, V86, P54; Krutzsch W., 1966, ABHANDLUNGEN ZENTRAL, V8, P112; LARSSON S G, 1975, Bulletin of the Geological Society of Denmark, V24, P193; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; Martinsen O.J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European Basins, P91; MEYER KJ, 1989, GEOLOGISCH JB A, V111, P523; MEYER KJ, 1988, GEOLOGISCH JB A, V100, P88; MITHLENER AG, 1996, GEOLOGICAL SOC SPECI, V101, P255; Mudge D.C., 1996, CORRELATION EARLY PA, V101, P91; NIELSEN OB, 1986, GEOSKRIFTER, V24, P235; PEDERSEN G K, 1983, Bulletin of the Geological Society of Denmark, V32, P43; PEDERSEN GK, 1981, SEDIMENTOLOGY, V28, P487, DOI 10.1111/j.1365-3091.1981.tb01697.x; Pedersen SAS, 1996, B GEOL SOC DENMARK, V42, P153; Powell A.J., 1992, P155; POWELL AJ, 1988, REV PALAEOBOT PALYNO, V56, P327, DOI 10.1016/0034-6667(88)90064-4; ROCHE E, 1983, PHYSIOGEO, V6, P13; SCHRODER T, 1992, J MICROPALAEONTOL, V2, P113; SWISHER CC, 1991, INT ANN M FIELD C 2, V16; THOMAS JE, 1996, SPECIAL PUBLICATIONS, V101, P115; Tschudy R.H, 1973, 743B US GEOL SURV, V743; TSCHUDY RH, 1981, REV PALAEOBOT PALYNO, V35, P283, DOI 10.1016/0034-6667(81)90113-5; WILLMANN R, 1990, INSEKTEN FUR FORMATI; Willumsen P. S., 1997, THESIS AARHUS U DENM, P147; WILLUMSEN PS, 1998, LAB GEOLOGIE SEDIMEN, V1, P130; WING SL, 1991, GEOLOGY, V19, P1189, DOI 10.1130/0091-7613(1991)019<1189:EEBACC>2.3.CO;2	61	24	28	0	4	GEOLOGICAL SOC DENMARK	COPENHAGEN	OSTER VOLDGADE 5-7, DK-1350 COPENHAGEN, DENMARK	2245-7070			B GEOL SOC DENMARK	Bull. Geol. Soc. Den.	DEC	2004	51		2				141	157						17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	885NO					2025-03-11	WOS:000226164400004
J	Marenssi, S; Guler, V; Casadío, S; Guerstein, R; Papú, O				Marenssi, S; Guler, V; Casadío, S; Guerstein, R; Papú, O			Sedimentology and palynology of the calafate formation (Maastrichtian), Austral Basin, Southern Patagonia, Argentina	CRETACEOUS RESEARCH			English	Article						sedimentology; calafate formation; palynology; Maastrichtian; Austral Basin; Southern Argentina	NEUQUEN BASIN; PALEOGENE; BOUNDARY; MODEL	The Calafate Formation crops out in south-western Santa Cruz Province. Argentina, and displays a stacking of asymmetrical coarsening-fining-upward cycles. These cycles are interpreted as the product of short-lived transgressive-resgressive events in which the coarsening upward part represents sedimentary aggradation with a stable or decreasing sea level. Sedimentological and palynological analyses indicate nearshore marine conditions. Even though the existence of an estuary or incised valley cannot be determined, this is the most probable palaeogeographic model. Based oil dinoflagellate cysts. The base of the section is considered to be not older than Maastrichtian. The presence of the oyster Ambigostrea clarae (Ihering) occurring together with the dinoflagellate cyst species Mamumiella druggii (Stover) Bujak and Davies and Eisenackia circumtabulata Drugg in the middle part of the section indicates an age no older than late Maastrichtian. According to sedimentological data, deposits representing the Cretaceous-Palaeogene transition would have been eroded, which is confirmed by the presence of Grapnelispora loncochensis Papu. This megaspore is a consistent component of the Maastrichtian assemblages from Patagonia. (C) 2004 Elsevier Ltd. All rights reserved.	Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; Inst Antartico Argentino, RA-1010 Buenos Aires, DF, Argentina; Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Argentina; Univ Nacl La Pampa, Fac Ciencias Exactas & Nat, La Pampa, Argentina; Ctr Reg Invest Cientificas & Tecnol, Inst Argentino Nivol Glaciol & Ciencias Ambiental, Unidad Paleopalinol, RA-5500 Mendoza, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Instituto Antartico Argentino; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina.	vguler@criba.edu.ar	Casadio, Silvio/A-5131-2010					ALLEN JRL, 1980, SEDIMENT GEOL, V26, P281, DOI 10.1016/0037-0738(80)90022-6; [Anonymous], 1987, ASS AUSTRALASIAN PAL; ARBE H, 1984, NOV C GEOL ARG SAN C, P124; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; BRENNER RL, 1985, SEDIMENTOLOGY, V32, P363, DOI 10.1111/j.1365-3091.1985.tb00517.x; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Cant D.J., 1986, SHELF SANDS SANDSTON, P303; Casadío S, 1998, AMEGHINIANA, V35, P449; DANERS G, 2004, IN PRESS 4 C UR GEOL; Daners G., 2004, CUENCAS SEDIMENTARIA, P37; DEMOWBRAY T, 1984, J SEDIMENT PETROL, V54, P811; DeRaaf J.F.M., 1971, GEOL MIJNBOUW-N J G, V50, P479; Feldmann R.M., 1997, The Antarctic Region: Geological Evolution and Processes, P1007; FELDMANN RM, 1995, J PALEONTOL, V69, P1; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; HARRIS PT, 1988, SEDIMENT GEOL, V57, P273, DOI 10.1016/0037-0738(88)90034-6; Macellari C.E., 1989, J S AM EARTH SCI, V2, P223; Malumian N, 1997, J S AM EARTH SCI, V10, P189, DOI 10.1016/S0895-9811(97)00015-1; MANASSERO MJ, 1992, REV ASOCIACION GEOLO, V47, P73; MANASSERO MJ, 1990, REV ASOCIACION GEOLO, V45, P37; MARENSSI SA, 2002, GEOLOGICA ARGENTINA, V57, P341; NULLO FE, 1981, CUENCAS SEDIMENTARIA, P181; PAPU O H, 1990, Ameghiniana, V27, P289; Papu O.H., 1997, REV ESP PALEONTOL, V12, P197; Papu O.H., 1995, SUS RELACIONES CONUN, P195; Papú OH, 2002, AMEGHINIANA, V39, P415; Papu Oscar Hugo, 1993, Ameghiniana, V30, P143; Ramos V.A., 1994, EARTH EVOLUTION SERI, P315; RICCARDI AC, 1988, GEOLOGICAL SOC AM ME, V168; Riggi, 1979, REV ASOC GEOL ARGENT, V34, P255; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Sepulveda E., 1989, B INSTITUTO GEOCIENC, V7, P163, DOI [10.11606/issn.2317-8078.v0i7p163-171, DOI 10.11606/ISSN.2317-8078.V0I7P163-171]; STOUGH JB, 1968, PALEONTOLOGICAL CONT, V32, P1; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104	35	41	47	0	2	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	DEC	2004	25	6					907	918		10.1016/j.cretres.2004.08.004	http://dx.doi.org/10.1016/j.cretres.2004.08.004			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	884ZB					2025-03-11	WOS:000226124100006
J	Tamelander, T; Heiskanen, AS				Tamelander, T; Heiskanen, AS			Effects of spring bloom phytoplankton dynamics and hydrography on the composition of settling material in the coastal northern Baltic Sea	JOURNAL OF MARINE SYSTEMS			English	Article						spring bloom; sedimentation; diatoms; Dinoflagellates; Baltic sea; study site coordinates: N59 degrees 51.3 ', E23 degrees 15.9 ' (XII), N59 degrees 47.4 '; E23 degrees 19.9 ' (P3) and N59 degrees 46.4 ', E23 degrees 15.8 ' (La)	SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; ORGANIC-MATTER; SEDIMENTATION; NUTRIENT; FINLAND; SINKING; GULF; MICROORGANISMS; SUCCESSION; VELOCITIES	The phytoplankton species succession and sedimentation characteristics were studied on a sheltered and an open coastal station during a spring bloom in the northern Baltic Sea. Biomass (phytoplankton carbon and chlorophyll a), inorganic nutrients and particulate organic carbon and nitrogen (POC and PON) were determined in the suspended material. Sediment traps moored at different depths were used to determine the vertical flux of total particulate material (TPM), POC and PON, chlorophyll a, phaeopigments and phytoplankton carbon. The spring phytoplankton biomass was dominated by dinoflagellates that formed a dense bloom of short duration, whereas diatoms were present in the water column throughout the spring period in more moderate biomasses. The vertical flux of phytoplankton carbon was however dominated by diatoms at all times. The formation of resting stages increased the sedimentation of dinoflagellates, but compared to. the suspended biomass of vegetative cells, their sinking rates were low. The ambient silicate concentration did probably not limit diatom growth; these were rather removed from the surface layer through sinking, a situation beneficial for dinoflagellates capable to exploit deep nutrient reserves through vertical migration. Due to rapid sinking soon after bloom formation and high specific loss rates, diatoms can be considered important contributors to the vertical flux of autochtonous material. Dinoflagellates mostly disintegrate in the water column and may settle as phytodetritus, except for the fraction of the populations that form rapidly sinking cysts. In addition to vertical export, advection of water from the stations seems to have been an important loss factor in the phytoplankton community. The two stations differed in that resuspension and input from littoral sources to the vertical flux were more important in the inner and shallower archipelago zone. This was also reflected in the C/N ratio of the settling material and in the bottom surface layer. In our study area, both the hydrographical regime and the species composition of the phytoplankton community were found to affect sedimentation characteristics and the composition of the settling material during the spring period. (C) 2004 Elsevier B.V. All rights reserved.	Finnish Inst Marine Res, FIN-00931 Helsinki, Finland; Finnish Environm Inst, FIN-00251 Helsinki, Finland	Finnish Environment Institute	Norwegian Polar Res Inst, Polar Environm Ctr, N-9296 Tromso, Norway.	tobias@npolar.no	Heiskanen, Anna-Stiina/B-2933-2013	Heiskanen, Anna-Stiina/0000-0003-2229-1171				ALLDREDGE AL, 1989, DEEP-SEA RES, V36, P159, DOI 10.1016/0198-0149(89)90131-3; [Anonymous], OPHELIA S; [Anonymous], [No title captured]; [Anonymous], ACTA BOT FENN; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; Edler L., 1979, Baltic Mar Biol Publ, V5, P1; EGGE JK, 1992, MAR ECOL PROG SER, V83, P281, DOI 10.3354/meps083281; ELMGREN R, 1984, Rapports et Proces-Verbaux des Reunions Conseil International pour l'Exploration de la Mer, V183, P152; FORSSKAHL M, 1982, NETH J SEA RES, V16, P290, DOI 10.1016/0077-7579(82)90037-0; GOLDMAN JC, 1987, LIMNOL OCEANOGR, V32, P1239, DOI 10.4319/lo.1987.32.6.1239; Grasshoff K., 1976, METHODS SEAWATER ANA, V2nd; GREBMEIER JM, 1988, MAR ECOL PROG SER, V48, P57, DOI 10.3354/meps048057; HAAPALA J, 1994, ESTUAR COAST SHELF S, V38, P507, DOI 10.1006/ecss.1994.1035; Heiskanen AS, 1995, HYDROBIOLOGIA, V316, P211, DOI 10.1007/BF00017438; Heiskanen AS, 1999, HYDROBIOLOGIA, V393, P127, DOI 10.1023/A:1003539230715; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; HEISKANEN AS, 1994, ARCH HYDROBIOL, V131, P175; HEISKANEN AS, 1995, MAR ECOL PROG SER, V122, P45, DOI 10.3354/meps122045; Heiskanen AS, 1998, ESTUAR COAST SHELF S, V46, P703, DOI 10.1006/ecss.1997.0320; HILTON J, 1985, LIMNOL OCEANOGR, V30, P1131, DOI 10.4319/lo.1985.30.6.1131; KAHRU M, 1990, CONT SHELF RES, V10, P329, DOI 10.1016/0278-4343(90)90055-Q; KANSANEN PH, 1991, HYDROBIOLOGIA, V222, P121, DOI 10.1007/BF00006100; KONONEN K, 1988, PHYTOPLANKTON SUMMER, V6, P281; Kremp A, 2000, PHYCOLOGIA, V39, P183, DOI 10.2216/i0031-8884-39-3-183.1; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; KUPARINEN J, 1993, ADV MAR BIOL, V29, P73, DOI 10.1016/S0065-2881(08)60130-3; Kuparinen J, 2001, AMBIO, V30, P190, DOI 10.1639/0044-7447(2001)030[0190:EASPCF]2.0.CO;2; LAAKKONEN A, 1981, MERI, V9, P3; LEVASSEUR M, 1984, MAR ECOL PROG SER, V19, P211, DOI 10.3354/meps019211; LIGNELL R, 1993, MAR ECOL PROG SER, V94, P239, DOI 10.3354/meps094239; LIRDWITAYAPRASIT T, 1990, J PHYCOL, V26, P299, DOI 10.1111/j.0022-3646.1990.00299.x; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; NIEMI A, 1987, ANN BOT FENN, V24, P333; Niemi A, 1973, Acta Botanica Fennica, V100, P1; Olli K, 1997, HYDROBIOLOGIA, V363, P179, DOI 10.1023/A:1003186024477; PASSOW U, 1991, MAR BIOL, V108, P449, DOI 10.1007/BF01313655; Rahm L, 1996, MAR ECOL PROG SER, V130, P221, DOI 10.3354/meps130221; Reigstad M, 1996, SARSIA, V80, P245, DOI 10.1080/00364827.1996.10413599; Reigstad M, 2000, THESIS U TROMSO; SCHULZ S, 1984, OPHELIA S, V3, P213; Smayda T. 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DEC	2004	52	1-4					217	234		10.1016/j.jmarsys.2004.02.001	http://dx.doi.org/10.1016/j.jmarsys.2004.02.001			18	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	878UL					2025-03-11	WOS:000225672500012
J	Wang, ZH; Matsuoka, K; Qi, YZ; Chen, JF				Wang, ZH; Matsuoka, K; Qi, YZ; Chen, JF			Dinoflagellate cysts in recent sediments from Chinese coastal waters	MARINE ECOLOGY-PUBBLICAZIONI DELLA STAZIONE ZOOLOGICA DI NAPOLI I			English	Article						Dinoflagellate; resting cyst; harmful algal bloom; the China Sea; Alexandrium	RECENT MARINE-SEDIMENTS; THECA RELATIONSHIPS; YOKOHAMA-PORT; TOKYO-BAY; DINOPHYCEAE; EUTROPHICATION; TEMPERATURE; INDICATOR; SALINITY; SEA	Surface sediments were collected from 10 locations to study the distribution of dinoflagellate resting cysts in Chinese coastal waters from July 2000 to May 2002. Sixty-one cyst morphotypes representing 14 genera of three orders were identified in this survey. Seventeen cyst types were recorded for the first time from Chinese coasts. Rich cyst assemblages were recorded in closed or semi-closed nearshore harbors. Scrippsiella trochoidea was the most dominant and common cyst type in this survey, especially in sediments from Daya Bay, Dapeng Bay and Shenzhen Bay. However, Protoperidinium cysts were the most diversified group, predominating in Changjiang River Estuary, Zhujiang River Estuary, Zhelin bay and the Nanao Island area. Cyst concentrations in the top 2 cm surface sediments varied from 258 to 25,037 cysts.g(-1) dry weight sediment, and abundance was lower in Changjiang River Estuary and Zhujiang River Estuary. Cysts of two dinoflagellates capable of producing paralytic shellfish poisoning (PSP) -Alexandrium spp. and Gymnodinium catenatum- were detected almost in all locations. Furthermore, the ellipsoidal Alexandrium catenella and A. tamarense cyst complex was frequently observed in the surface sediment from Daya Bay, where high contents of PSP toxin and PSP episodes have been reported. Detailed descriptions and illustrations are provided of those cysts of newly recorded species, unidentified species, toxic species and dominant species.	Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Peoples R China; Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan	Jinan University; Chinese Academy of Sciences; Nagasaki University	Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Peoples R China.	twzh@jnu.edu.cn						Anderson D.M., 1984, Seafood toxins, P125; ANDERSON DM, 1988, J PHYCOL, V24, P255; Anderson DM, 1996, TOXICON, V34, P579, DOI 10.1016/0041-0101(95)00158-1; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P243; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Chen Ju-fang, 2000, Marine Environmental Science, V19, P20; Cho H.-J., 1999, E CHINA SEA, V2, P73; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Cho Hyun-Jin, 2001, Journal of Fisheries Science and Technology, V4, P120; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; EPPLEY RW, 1979, OCEANOL ACTA, V2, P241; ERADLEDENN E, 1993, DEV MARINE BIOL, V3, P109; Fensome R.A., 1993, CLASSIFICATION FOSSI; FUKUYO Y, 1982, B148R1418, P205; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Head M.J., 1996, Palynology: Principles and Applications, P1197; HONG CJ, 2003, RED TIDES CHINESE CO, P159; Huang He., 1997, Macroeconomic Dynamics, V1, P7; Huang X., 2000, Marine Environ. 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J. Appl. Ecol., V14, P1031; Zhou Ming-Jiang, 2001, Chinese Bulletin of Life Sciences, V13, P54	72	52	63	2	38	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0173-9565			MAR ECOL-P S Z N I	Mar. Ecol.-Pubbl. Stn. Zool. Napoli	DEC	2004	25	4					289	311		10.1111/j.1439-0485.2004.00035.x	http://dx.doi.org/10.1111/j.1439-0485.2004.00035.x			23	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	878GT					2025-03-11	WOS:000225635500004
J	Tanimura, Y; Shimada, C				Tanimura, Y; Shimada, C			Calcareous dinoflagellates from a northwestern Pacific sediment trap and their paleoceanographic implications	MICROPALEONTOLOGY			English	Article							EQUATORIAL ATLANTIC-OCEAN; WESTERN TROPICAL ATLANTIC; SUBTROPICAL MODE WATER; THORACOSPHAERA-HEIMII; SURFACE SEDIMENTS; QUATERNARY EASTERN; MEDITERRANEAN SEA; NORTH PACIFIC; LIFE-CYCLE; CYSTS	Year-round changes in species composition and flux of calcareous dinoflagellates at station JT (34degrees09.8'N, 141degrees59.3'E; water depth, 8942m; trap depth, 916m) are reported. A time-series of thirteen sedinient-trap samples of 29 days each, between March 5, 1991 and March 2, 1992, provided materials for this study. Vegetative cysts of a calcareous dinoflagellate, Thoracosphaera heimii, were found to be overwhelmingly dominant forming >95% of the calcareous dinoflagellate associations in all trap samples. Its' flux ranges from 10,000 shells(.)m(-2.)day(-1) in May 1991,to 76,000 shells(.-2.)day(-1) in September, 1991. Cysts of other calcareous dinoflagellates (Leonella granifera, Calciodinellum albatrosianum and Calciodinellum levantinum) were also found, with a maximum flux of 11,000 shells(.)m(-2.)day(-1) for C. albatrosianum between December, 1991 and January, 1992. Based on physiological information, we suggest that species flux depends on water mass distribution linked to migration of the path of the subtropical Kuroshio Current. High to moderate flux of T. heimii occurred when the current took a meandering or a straight nearshore pathway. Waters southeast of the current prevailed over the trap station during this time. The most favorable environment, May, 199 1, for T heimii production seems to occur around a shallow thermocline formed above Subtropical Mode Water (STMW) in the waters southeast of the current. The species flux dropped when the current took an offshore pathway and flowed over the trap station. Surface and subsurface waters of the Kuroshio Current, especially during summer to autumn, is not productive of this species. The species flux also dropped while a "cold water mass" (i.e. lower salinity water cut off from the subarctic Oyashio Current) emerged over the trap station. Three cysts, L. granifera, C. albatrosianum and C. levantinum, show broadly similar abundance fluctuations to T.heimii. This close relationship between temporal changes in T. heimii productivity and path migrations of the Kuroshio Current, which is linked to the wind stress field over the North Pacific, should potentially provide information for potentially reconstructions.	Natl Sci Museum, Dept Geol, Tokyo 1690073, Japan; Univ Tsukuba, Doctoral Program Earth Evolut Sci, Grad Sch Life & Environm Sci, Tsukuba, Ibaraki 3058572, Japan	National Museum of Nature and Science; University of Tsukuba	Tanimura, Y (通讯作者)，Natl Sci Museum, Dept Geol, Tokyo 1690073, Japan.	tanimura@kahaku.go.jp						AKITOMO K, 1991, J GEOPHYS RES-OCEANS, V96, P2549, DOI 10.1029/90JC02030; Akitomo K., 1997, J. 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J	Munsterman, DK; Brinkhuis, H				Munsterman, DK; Brinkhuis, H			A southern North Sea Miocene dinoflagellate cyst zonation	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						southern North Sea; the Netherlands; Miocene; Breda Formation; biostratigraphy; sequence stratigraphy; palynology; organic-walled dinoflagellate cysts	ROER VALLEY GRABEN; INTEGRATED STRATIGRAPHY; DEPOSITIONAL HISTORY; DIEST FORMATION; RIFT SYSTEM; TERTIARY; BELGIUM; BASIN; BIOSTRATIGRAPHY; NETHERLANDS	An integrated stratigraphical analysis emphasizing organic-walled dinoflagellate cyst (dinocyst) distribution has been carried out on multiple boreholes penetrating the Miocene in the subsurface of the Netherlands (southern North Sea Basin). The bulk of the investigated successions is attributed to the Breda Formation, a regional lithostatigraphical unit most complete in the south-eastern part of the Netherlands. In concert with a first regional integrated bio (chrono) sequence-stratigraphical framework, fourteen informal dinocyst zones for the southern North Sea Miocene (SNSM), and three subzones are proposed for the Breda Formation. By also integrating (chrono)stratigraphic information from Mediterranean and North Atlantic dinocyst studies a first ever detailed age-model is here proposed for the Miocene in the subsurface of the Netherlands.	Netherlands Inst Appl Geosci TNO, Natl Geol Survey, NL-3508 TA Utrecht, Netherlands; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	Netherlands Organization Applied Science Research; Utrecht University	Munsterman, DK (通讯作者)，Netherlands Inst Appl Geosci TNO, Natl Geol Survey, POB 80015, NL-3508 TA Utrecht, Netherlands.		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J. Geosci.	DEC	2004	83	4					267	285		10.1017/S0016774600020369	http://dx.doi.org/10.1017/S0016774600020369			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	896SE		Green Submitted, Bronze			2025-03-11	WOS:000226953000003
J	Versteegh, GJM; Blokker, P				Versteegh, GJM; Blokker, P			Resistant macromolecules of extant and fossil microalgae	PHYCOLOGICAL RESEARCH			English	Article; Proceedings Paper	7th International Conference on Modern and Fossil Dinoflagellated (DINO 7)	SEP 21-25, 2003	Nagasaki, JAPAN	Minist Educ Cultures, Sports, Sci & Technol, Nagasaki Univ, Fac Fisheries, Asian Natl Environm Sci Ctr, Univ Tokyo, Japanese Soc Phycol, Plankton Soc Japan, Lab Aquat Sci Consultant Co Ltd, Yamasita Med Instrument Co Ltd, Japanese Soc Phycol		algaenan; biomacromolecule; dinosporin; geomacromolecule; palynomorph; selective preservation	WALL (TLS)-CONTAINING MICROALGAE; CELL-WALL; BOTRYOCOCCUS-BRAUNII; CHEMICAL-STRUCTURE; GREEN-ALGAE; GEOCHEMICAL IMPLICATIONS; KEROGEN FORMATION; ORGANIC-MATTER; OUTER WALLS; NEOPROTEROZOIC ACRITARCHS	The occurrence and composition of macromolecular resistant walls of microalgae and their fossil macromolecular counterparts are reviewed. To date, several algal groups have been identified to produce fossilizable biomacromolecules. Only two biosynthetic pathways seem to be responsible for this, of which the acetate/malate pathway used by Chlorophyta, Eustigmatophyta and Dinophyta is considered to lead to a series of closely related resistant biomacromolecules, called algaenans. Algaenans consist of a network of predominantly linear carbon chains. A different, as yet unidentified, pathway is used by the Dinophyta to produce the aromatic walls of their cysts. The polyketide or acetogenic pathway may have been responsible for resorcinol-based algae or bacteria-derived microfossils of the acritarch Gloeocapsamorpha prisca, either through synthesis of the biomacromolecule or through a third pathway, the post-mortem polymerization of its resorcinol lipids. The post-mortem polymerization of lipids also appears to be responsible for the formation of fatty acid-based macromolecules in Eocene dinoflagellate-shaped remains from Pakistan. Finally, there is a clear need for elucidating the chemical differences between the biomacromolecules produced by the algae and their fossil analogs in the sediments. This notably applies to the release and condensation of aliphatic and aromatic moieties both at normal and at elevated temperature and pressure conditions.	Hanse Wissensch Kolleg, D-27753 Delmenhorst, Germany; Vrije Univ Amsterdam, Inst Ecol Sci, Fac Earth & Life Sci, NL-1081 HV Amsterdam, Netherlands	Vrije Universiteit Amsterdam	Hanse Wissensch Kolleg, Lehmkuhlenbusch 4, D-27753 Delmenhorst, Germany.	gerardv@nioz.nl	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				AKEN ME, 1985, S AFR J BOT, V51, P408, DOI 10.1016/S0254-6299(16)31617-9; Allard B, 2000, PHYTOCHEMISTRY, V54, P369, DOI 10.1016/S0031-9422(00)00135-7; Allard B, 1998, ORG GEOCHEM, V28, P543, DOI 10.1016/S0146-6380(98)00012-6; Allard B, 2001, PHYTOCHEMISTRY, V57, P459, DOI 10.1016/S0031-9422(01)00071-1; [Anonymous], GEOLOGICAL SOC SPECI; [Anonymous], 1993, ORGANIC GEOCHEMISTRY; Arouri K, 1999, ORG GEOCHEM, V30, P1323, DOI 10.1016/S0146-6380(99)00105-9; Arouri KR, 2000, ORG GEOCHEM, V31, P75, DOI 10.1016/S0146-6380(99)00145-X; ASHRAF M, 1980, ANN BOT-LONDON, V46, P485, DOI 10.1093/oxfordjournals.aob.a085942; ATKINSON AW, 1972, PLANTA, V107, P1, DOI 10.1007/BF00398011; Batten DJ., 1996, Palynology: principles and applications, P191; BERKALOFF C, 1983, PHYTOCHEMISTRY, V22, P389, DOI 10.1016/0031-9422(83)83010-6; BERNER R A, 1989, Global and Planetary Change, V1, P97, DOI 10.1016/0921-8181(89)90018-0; Bertheas O, 1999, PHYTOCHEMISTRY, V50, P85, DOI 10.1016/S0031-9422(98)00481-6; BIEDLINGMAIER S, 1987, Z NATURFORSCH C, V42, P245; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; Blokker P, 1998, ORG GEOCHEM, V29, P1453, DOI 10.1016/S0146-6380(98)00111-9; Blokker P, 1998, PHYTOCHEMISTRY, V49, P691, DOI 10.1016/S0031-9422(98)00229-5; Blokker P, 1999, PLANTA, V207, P539, DOI 10.1007/s004250050515; Blokker P, 2001, GEOCHIM COSMOCHIM AC, V65, P885, DOI 10.1016/S0016-7037(00)00582-2; Blokker P, 2000, GEOCHIM COSMOCHIM AC, V64, P2055, DOI 10.1016/S0016-7037(00)00367-7; Blokker P., 2000, Geologica Ultratrajectina, V193, P1; BLOM AV, 1936, VERNIS, V13, P156; BRUNNER U, 1985, CAN J BOT, V63, P2221, DOI 10.1139/b85-315; Burczyk J, 1999, PHYTOCHEMISTRY, V51, P491, DOI 10.1016/S0031-9422(99)00063-1; BURCZYK J, 1987, PHYTOCHEMISTRY, V26, P113; BURCZYK J, 1987, PHYTOCHEMISTRY, V26, P121; Butterfield NJ, 1998, GEOLOGY, V26, P963, DOI 10.1130/0091-7613(1998)026<0963:DOWFIP>2.3.CO;2; COMBAZ A, 1971, SPOROPOLLENIN, P621; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DAMSTE JSS, 1990, ORG GEOCHEM, V16, P1077; DAMSTE JSS, 1993, GEOCHIM COSMOCHIM AC, V57, P389; de Leeuw J.W., 1993, ORG GEOCHEM, P23, DOI [10.1007/978-1-4615-2890-6_2, DOI 10.1007/978-1-4615-2890-6_2]; DERENNE S, 1992, ORG GEOCHEM, V19, P299, DOI 10.1016/0146-6380(92)90001-E; Derenne S, 1997, GEOCHIM COSMOCHIM AC, V61, P1879, DOI 10.1016/S0016-7037(97)00042-2; DERENNE S, 1992, PHYTOCHEMISTRY, V31, P1923, DOI 10.1016/0031-9422(92)80335-C; Derenne S, 1996, ORG GEOCHEM, V24, P617, DOI 10.1016/0146-6380(96)00053-8; DERENNE S, 1994, GEOCHIM COSMOCHIM AC, V58, P3703, DOI 10.1016/0016-7037(94)90160-0; DEVRIES PJR, 1983, ACTA BOT NEERL, V32, P25, DOI 10.1111/j.1438-8677.1983.tb01674.x; Fensome R.A., 1993, CLASSIFICATION MODER; Fensome RA, 1999, GRANA, V38, P66; Fjällström P, 2002, IND CROP PROD, V16, P173, DOI 10.1016/S0926-6690(02)00035-3; Foster C.B., 2002, Palynology, V26, P35, DOI [10.1080/01916122.2002.9989566, DOI 10.1080/01916122.2002.9989566]; Gelin F, 1999, ORG GEOCHEM, V30, P147, DOI 10.1016/S0146-6380(98)00206-X; Gelin F, 1997, ORG GEOCHEM, V26, P659, DOI 10.1016/S0146-6380(97)00035-1; GOOD BH, 1978, AM J BOT, V65, P27, DOI 10.2307/2442549; Greenwood PF, 2000, GEOCHIM COSMOCHIM AC, V64, P1249, DOI 10.1016/S0016-7037(99)00326-9; GUNNISON D, 1975, APPL MICROBIOL, V29, P729, DOI 10.1128/AEM.29.6.729-738.1975; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; HARVEY GR, 1983, MAR CHEM, V12, P119, DOI 10.1016/0304-4203(83)90075-0; HEGEWALD E, 1989, ARCH HYDROBIOL, V82, P119; HEGEWALD E, 1988, Archiv fuer Hydrobiologie Supplement, V78, P465; Hemsley A.R., 1993, GRANA S, V1, P2; Hemsley A.R., 1994, NERC Spec. 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Res.	DEC	2004	52	4					325	339		10.1111/j.1440-1835.2004.tb00342.x	http://dx.doi.org/10.1111/j.1440-1835.2004.tb00342.x			15	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	876DJ					2025-03-11	WOS:000225475800003
J	Kawamura, H				Kawamura, H			Dinoflagellate cyst distribution along a shelf to slope transect of an oligotrophic tropical sea (Sunda Shelf, South China Sea)	PHYCOLOGICAL RESEARCH			English	Article; Proceedings Paper	7th International Conference on Modern and Fossil Dinoflagellated (DINO 7)	SEP 21-25, 2003	Nagasaki, JAPAN	Minist Educ Cultures, Sports, Sci & Technol, Nagasaki Univ, Fac Fisheries, Asian Natl Environm Sci Ctr, Univ Tokyo, Japanese Soc Phycol, Plankton Soc Japan, Lab Aquat Sci Consultant Co Ltd, Yamasita Med Instrument Co Ltd, Japanese Soc Phycol		dinoflagellate cyst; modern; South China Sea; Sundra Shelf	SURFACE SEDIMENTS; COASTAL WATERS; AUSTRALIA	From 51 surface samples collected along a shelf to slope transect of the Sunda Shelf, South China Sea, 36 taxa of organic-walled dinoflagellate cysts are identified. Oligotrophic tropical shelf assemblages on the Sunda Shelf are dominated by gonyaulacoids such as Spiniferites species, Operculodinium centrocarpum and Operculodinium israelianum. Concentrations of dinoflagellate cysts in the shelf sediments are generally low and correlate well with the content of fine-grained (clay and silt fraction) sediments. Detailed comparisons of sediment grain-size distributions to concentrations of dominant dinoflagellate taxa (Spiniferites species, O. centrocarpum and O. israelianum) in the shelf sediments indicate that these taxa behave in water like sediment particles with size range phi 5.75-6.25 (13-18 mum). In contrast, slope assemblages in fine-grained sediments are dominated by protoperidinioids. This may reflect higher nutrient availability as a result of weak winter upwelling. The concentrations of dinoflagellate cysts in the shelf sediments are mainly controlled by transport and winnowing processes and are probably not representative of surface water conditions.	Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany	University of Kiel	Kawamura, H (通讯作者)，Hokkaido Univ, Div Biol Sci, Grad Sch Sci, Kita Ku, N 10 W 8, Sapporo, Hokkaido 0600810, Japan.	hkawamura@nature.sci.hokudai.ac.jp						[Anonymous], NOVA HEDWIGIA; [Anonymous], REPORT SERIES BEDFOR; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1961, PHYS OCEANOGRAPHY SE; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BIEBOW N, 1996, 57 GEOMAR FORSCH MAR; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bujak J.P., 1983, AASP CONTRIBUTION SE, V13; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; CHO HJ, 1999, E CHINA SEA, P73; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; DALE B, 1993, NATO ASI SER, V1, P521; HARLAND R, 1977, PALAEONTOGR ABT B, V14, P87; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 1999, J PALEONTOL, V73, P1; KOBAYASHI S, 1991, Bulletin of Plankton Society of Japan, V38, P9; KOBAYASHI S, 1986, Bulletin of Plankton Society of Japan, V33, P81; LEE JB, 1994, 2 INT S MAR SCI EXPL, P1; LIRDWITAYAPRASI.T, 1998, 1 TECHN SEM MAR FISH, P311; Lirdwitayaprasit T., 1998, 2 TECHN SEM MAR FISH, P310; Liu KK, 2002, DEEP-SEA RES PT I, V49, P1387, DOI 10.1016/S0967-0637(02)00035-3; Liu WT, 1999, GEOPHYS RES LETT, V26, P1473, DOI 10.1029/1999GL900289; MANTELL GA, 1854, MEDALS CREATION 1 LE; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATSUOKA K, 1994, BOT MAR, V37, P495, DOI 10.1515/botm.1994.37.6.495; MATSUOKA K, 1983, Palaeontographica Abteilung B Palaeophytologie, V187, P89; MATSUOKA K, 1985, NAT SCI B, V25, P1; Matsuoka K, 1981, B FACULTY LIBERAL AR, V21, P59; MATSUOKA K, 1999, E CHINA SEA, P195; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; McMinn Andrew, 1992, Palynology, V16, P13; MUDI PJ, 1996, PALYNOLOGY PRINCIPLE, P843; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; NINO H, 1966, J SEDIMENTA PETROL, V36, P152; PAULSEN J, 1998, THESIS C ALBRECHT U; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Rao C. 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Kiel, V86, P1; STOCKMARR J, 1971, Pollen et Spores, V13, P615; SZAREK R, 2001, THESIS C ALBRECHTS U; Targarona J, 1999, GRANA, V38, P170; TERBRAAK CJF, 1998, CANOCO, V4; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D, 1970, Micropaleontology (New York), V16, P47, DOI 10.2307/1484846; WALL D., 1967, PALAEONTOLOGY, V10, P95; Wu G, 1995, CHINESE SCI BULL, V40, P545; WU G, 2000, TROP OCEANOL, V19, P7	57	37	41	2	12	BLACKWELL PUBLISHING ASIA	CARLTON	54 UNIVERSITY ST, P O BOX 378, CARLTON, VICTORIA 3053, AUSTRALIA	1322-0829			PHYCOL RES	Phycol. Res.	DEC	2004	52	4					355	375		10.1111/j.1440-1835.2004.tb00345.x	http://dx.doi.org/10.1111/j.1440-1835.2004.tb00345.x			21	Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	876DJ					2025-03-11	WOS:000225475800006
J	Azanza, RV; Siringan, FP; San Diego-Mcglone, ML; Yñiguez, AT; Macalalad, NH; Zamora, PB; Agustin, MB; Matsuoka, K				Azanza, RV; Siringan, FP; San Diego-Mcglone, ML; Yñiguez, AT; Macalalad, NH; Zamora, PB; Agustin, MB; Matsuoka, K			Horizontal dinoflagellate cyst distribution, sediment characteristics and benthic flux in Manila Bay, Philippines	PHYCOLOGICAL RESEARCH			English	Article; Proceedings Paper	7th International Conference on Modern and Fossil Dinoflagellated (DINO 7)	SEP 21-25, 2003	Nagasaki, JAPAN	Minist Educ Cultures, Sports, Sci & Technol, Nagasaki Univ, Fac Fisheries, Asian Natl Environm Sci Ctr, Univ Tokyo, Japanese Soc Phycol, Plankton Soc Japan, Lab Aquat Sci Consultant Co Ltd, Yamasita Med Instrument Co Ltd, Japanese Soc Phycol		benthic flux; dinoflagellate cyst; harmful algal bloom; porewater nutrients; Prodinium bahamense var. compressum; sediment	RED TIDE BLOOMS; NORWEGIAN FJORD; WATERS; INDICATORS; DIFFUSION; POLLUTION	The lateral variation of sediment properties and associated cyst content of sediment in Manila Bay were determined and their possible role/s in the occurrences of Pyrodinium bahamense Plate var. compressum (Bohm) Steidinger, Tester et Taylor toxic blooms were assessed. Manila Bay's surface sediment was determined to be silt dominated. Clay generally increased towards the coast, probably as a result of flocculation and rapid deposition upon entry of sediments from the rivers. High sand content characterized the southeastern part of the bay attributed to the greater sand inputs and relatively strong currents in this area. Bulk densities were lower in the eastern side of the bay from dilution by high organic load from sewage and urban areas. Benthic flux calculations, particularly NH3, suggest more than 50% nutrient contribution comes from sediments. In general, dinoflagellate cyst density increased from the center of the bay towards the coast, except in Pampanga Bay where it decreased near the coasts. A maximum of 23 dinoflagellate species were identified: 5 were autotrophic (Lingulodinium polyedrum (Stein) Dodge, Gonyaulax spp., Pyrophacus steinii (Schiller) Wall et Dale, Protoceratium reticulatum (Claparede et Lachmann) Butschli, and Pyrodinium bahamense var. compressum), and the rest were predominantly composed of Protoperidinium spp. and Diplopsalis spp. Heterotrophs comprised about 70% of the total cyst counts. Pyrodinium counts increased towards the north-western part of the bay where it was the dominant autotroph species. Negative correlations were observed for live Pyrodinium cyst density and N flux, P flux, ratio of N to P and total organic carbon (TOC) content. However, areas with high N:P ratio contain abundant Pyrodinium live cysts.	Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines; Univ Philippines, Natl Inst Geol Sci, Quezon City 1101, Philippines; Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Natl Ctr Caribbean Coral Reef Res, Miami, FL 33149 USA; Nagasaki Univ, Fac Fisheries, Nagasaki 8528521, Japan	University of the Philippines System; University of the Philippines Diliman; University of the Philippines System; University of the Philippines Diliman; University of Miami; Nagasaki University	Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines.	rhod@upmsi.ph	Zamora, Peter/N-6568-2019; Azanza, Rhodora/HGU-5811-2022; Agustin, Melissa/AAI-8621-2020	Agustin, Melissa/0000-0001-9189-0851				ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; [Anonymous], 1996, HARMFUL TOXIC ALGAL; Bajarias FA., 1996, HARMFUL TOXIC ALGAL, P49; BAJARIAS FFA, 1995, INT SEM MAR FISH ENV, P139; Berner R.A., 1980, EARLY DIAGENESIS; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; CLINE JD, 1969, LIMNOL OCEANOGR, V14, P454, DOI 10.4319/lo.1969.14.3.0454; Corrales R.A., 1995, P573; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; delas Alas J. 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L, 1996, HARMFUL TOXIC ALGAL, P189	44	38	42	1	20	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1322-0829	1440-1835		PHYCOL RES	Phycol. Res.	DEC	2004	52	4					376	386						11	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	876DJ					2025-03-11	WOS:000225475800007
J	Wang, ZH; Qi, YZ; Lu, SH; Wang, Y; Matsuoka, K				Wang, ZH; Qi, YZ; Lu, SH; Wang, Y; Matsuoka, K			Seasonal distribution of dinoflagellate resting cysts in surface sediments from Changjiang River Estuary	PHYCOLOGICAL RESEARCH			English	Article; Proceedings Paper	7th International Conference on Modern and Fossil Dinoflagellated (DINO 7)	SEP 21-25, 2003	Nagasaki, JAPAN	Minist Educ Cultures, Sports, Sci & Technol, Nagasaki Univ, Fac Fisheries, Asian Natl Environm Sci Ctr, Univ Tokyo, Japanese Soc Phycol, Plankton Soc Japan, Lab Aquat Sci Consultant Co Ltd, Yamasita Med Instrument Co Ltd, Japanese Soc Phycol		Alexandrium; Changjiang River Estuary; cyst; dinoflagellate; East China Sea	YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION; ASSEMBLAGES; SEA	In order to understand the distribution of dinoflagellate cysts, surface sediments were collected from 15 stations in Changjiang River Estuary from 122degreesE to 123.5degreesE and from 29degreesN to 32degreesN in four cruises from May 2002 to February 2003. In the present study, 38 different cyst morphotypes representing 21 genera and 6 groups were identified, while 1 type was not identified into genus level. Species number and cell density of dinoflagellate cysts ranged from 10 to 25 species and from 12 to 587 per gram of dry weight, respectively. There were no obvious differences in cyst composition and density among seasons. However, the highest cyst species number and density were recorded in summer and winter, respectively. Cysts of heterotrophic dinoflagellates, which held 55.7% of the overall cyst density averagely, dominated cyst assemblages. Cyst density and species number increased from the west to the east, from the north to the south within the study area. Cysts of toxic dinoflagellates Alexandrium catenella and Alexandrium tamarense complex distributed widely and were observed in almost all stations, with the maximum cell density of 81 per gram of dry weight.	Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Peoples R China; Nagasaki Univ, Fac Fisheries, Lab Coast Environm Sci, Nagasaki 8528521, Japan	Chinese Academy of Sciences; Jinan University; Nagasaki University	Jinan Univ, Inst Hydrobiol, Guangzhou 510632, Peoples R China.	twzh@jnu.edu.cn						Cao Peikui, 1995, J E CHINA NORMAL U, V1, P81; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; HONG CJ, 2003, RED TIDES CHINESE CO, P159; HONG JC, 1994, OCEANOLOGIA LIMNOLOG, V25, P179; HUAN W, 2004, PEOPLES DAILY   0514, P2; Huang X., 2000, Marine Environ. Ental Sci., V19, P1; Jiang Tianjiu, 2003, Yingyong Shengtai Xuebao, V14, P1156; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; LU D, 2002, IOC NEWSLETTER TOXIC, V23, P1; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K., 2000, TECHNICAL GUIDE MODE; MATSUOKA K, 1999, W PART E CHINA SEA E, V2, P195; Matsuoka Kazumi, 1995, Fossils (Tokyo), V59, P32; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Shannon C.E., 1964, MATH THEORY COMMUNIC; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; Wang Zhao-Hui, 2003, Acta Ecologica Sinica, V23, P2073; Wang Zhao-Hui, 2003, Oceanologia et Limnologia Sinica, V34, P422; Wang ZX, 2004, RARE METALS, V23, P32; Zhou M, 2003, Chin. J. Appl. Ecol., V14, P1031; Zhou Ming-Jiang, 2001, Chinese Bulletin of Life Sciences, V13, P54; [No title captured]	27	28	37	2	14	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1322-0829	1440-1835		PHYCOL RES	Phycol. Res.	DEC	2004	52	4					387	395		10.1111/j.1440-183.2004.00356.x	http://dx.doi.org/10.1111/j.1440-183.2004.00356.x			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	876DJ					2025-03-11	WOS:000225475800008
J	Wang, ZH; Matsuoka, K; Qi, YZ; Chen, JF; Lu, SH				Wang, ZH; Matsuoka, K; Qi, YZ; Chen, JF; Lu, SH			Dinoflagellate cyst records in recent sediments from Daya Bay, South China Sea	PHYCOLOGICAL RESEARCH			English	Article; Proceedings Paper	7th International Conference on Modern and Fossil Dinoflagellated (DINO 7)	SEP 21-25, 2003	Nagasaki, JAPAN	Minist Educ Cultures, Sports, Sci & Technol, Nagasaki Univ, Fac Fisheries, Asian Natl Environm Sci Ctr, Univ Tokyo, Japanese Soc Phycol, Plankton Soc Japan, Lab Aquat Sci Consultant Co Ltd, Yamasita Med Instrument Co Ltd, Japanese Soc Phycol		Alexandrium; Daya Bay; dinoflagellate cyst; parralytic shellfish poisoning; the South China Sea	YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION; ASSEMBLAGES; INDICATOR	Nine sediment cores of 8-26 cm in length were collected from two basins of Daya Bay, the South China Sea, by Tokyo University Fisheries Oceanography Laboratory core sampler in August 2001 to investigate the distribution of dinoflagellate resting cysts. In the present study, 51 different cyst morphotypes representing 22 genera were identified from 65 sediment samples. Among them, there were 21 autotrophic species and 30 heterotrophic ones. Cyst species richness in each sample varied from 12 to 29, while the values of Shannon-Weaver diversity index (H') were between 0.15 and 4.13. There were an obvious increase in both species richness and values of H' in 2-6 cm sediments. Cyst concentrations varied from 154 to 113 483 cysts per gram dry weight sediment, and were much higher in upper sediments. Scrippsiella trochoidea was the most dominant cyst type, which took up over 90% of cyst assemblages in the upper sediments. The abrupt increase of S. trochoidea cysts in the surface sediments reflected the bloom of this species in Daya Bay in 2000. The results from cyst assemblages showed some trend of changes in water quality in this area, and indicated a typical type of pollution caused by cultural eutrophication, which started in the 1980s and greatly accelerated in the middle of 1990s. Cysts of Alexandrium, mainly those of Alexandrium catenella and Alexandrium tamarense complex, occurred frequently and abundantly in this area, with the highest concentration and relative frequency of 503 cysts per gram dry weight sediment and 22.3%, respectively. The high abundance of Alexandrium cysts provided rich 'seed bed' for Alexandrium blooms and was also an important source of paralytic shellfish poisoning toxins, especially in winter.	Jinan Univ, Inst Hydrobiol, Coll Life Sci & Technol, Guangzhou 510632, Peoples R China; Nagasaki Univ, Fac Fisheries, Lab Coast Environm Sci, Nagasaki 8528521, Japan	Jinan University; Chinese Academy of Sciences; Nagasaki University	Jinan Univ, Inst Hydrobiol, Coll Life Sci & Technol, Guangzhou 510632, Peoples R China.	twzh@jnu.edu.cn						Anderson DM, 1996, TOXICON, V34, P579, DOI 10.1016/0041-0101(95)00158-1; ANDERSON DM, 1984, ACS SYM SER, P123; Chen H, 2000, EUR J MASS SPECTROM, V6, P19, DOI 10.1255/ejms.301; Cho H.-J., 1999, E CHINA SEA, V2, P73; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; COOPER SR, 1993, ESTUARIES, V16, P617, DOI 10.2307/1352799; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; Dale B., 1983, P69; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; EPPLEY RW, 1979, OCEANOL ACTA, V2, P241; Fensome R.A., 1993, CLASSIFICATION FOSSI; Head M.J., 1996, Palynology: Principles and Applications, P1197; HUANG NM, 1999, RAD PROTECTION B, V19, P12; HUANG NM, 2003, RAD PROTECTION B, V23, P35; Jiang T., 2000, CHINA ENV SCI, V20, P341; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; Lin Yantang, 1999, Tropic Oceanology, V18, P90; Lin Yantang, 1994, OCEANOLOGY LIMNOLOGY, V25, P220; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MATSUOKA K, 1995, FOSSILS, V59, P31; Matsuoka Kazumi, 1999, Fossils (Tokyo), V66, P1; OSHIMA Y, 1992, TOXICON, V30, P1539, DOI 10.1016/0041-0101(92)90025-Z; Pati AC, 1999, MAR BIOL, V134, P419, DOI 10.1007/s002270050558; 彭云辉, 1999, [台湾海峡, Journal of Oceanography in Taiwan Strait], V18, P26; PENG YH, 2001, J FISH CHINA, V25, P161; PENG YH, 1998, MAR ENV SCI, V17, P12; [彭云辉 Peng Yunhui], 2002, [海洋通报, Marine Science Bulletin], V21, P44; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Qi Y.Z., 2001, ACTA ECOL SIN, V21, P1825; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Qi YZ, 2004, HYDROBIOLOGIA, V512, P209, DOI 10.1023/B:HYDR.0000020329.06666.8c; Qiu Y.W., 2001, ACTA OCEANOL SIN, V23, P85, DOI 10.3321/j.issn:0253-4193.2001.01; Riegman R, 1995, WATER SCI TECHNOL, V32, P63, DOI 10.1016/0273-1223(95)00682-6; SCHWINGHAMER P, 1994, AQUACULTURE, V122, P171, DOI 10.1016/0044-8486(94)90508-8; Shannon C.E., 1964, MATH THEORY COMMUNIC; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; Tsirtsis G, 1998, ENVIRON MONIT ASSESS, V50, P255, DOI 10.1023/A:1005883015373; Wang X.P., 1996, T OCEAN LIMNOL, V4, P20, DOI [10.13984/j.cnki.cn37-1141.1996.04.004, DOI 10.13984/J.CNKI.CN37-1141.1996.04.004]; Wang Zhao-Hui, 2003, Acta Ecologica Sinica, V23, P2073; [王朝晖 Wang Zhaohui], 2004, [海洋环境科学, Marine Environmental Science], V23, P25; Wu Guo-xuan, 2000, Tropic Oceanology, V19, P8; Xiao Yong-Zhi, 2003, Acta Hydrobiologica Sinica, V27, P372; Xiao Yong-zhi, 2001, Marine Sciences (Beijing), V25, P50; Xu N, 2001, ACTA SCI CIRCUMSTANT, V21, P400; ZHANG GD, 1999, ELECT POWER, V32, P34; Zheng AR., 2001, MAR SCI, V25, P48; Zheng L., 1997, J TROP SUBTROP BOT, V5, P10; Zhong Si-sheng, 2002, Marine Environmental Science, V21, P34	50	54	59	0	28	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1322-0829	1440-1835		PHYCOL RES	Phycol. Res.	DEC	2004	52	4					396	407		10.1111/j.1440-1835.2004.tb00348.x	http://dx.doi.org/10.1111/j.1440-1835.2004.tb00348.x			12	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	876DJ					2025-03-11	WOS:000225475800009
J	Ghasemi-Nejad, E; Agha-Nabati, A; Dabiri, O				Ghasemi-Nejad, E; Agha-Nabati, A; Dabiri, O			Late triassic dinoflagellate cysts from the base of the Shemshak Group in north of Alborz Mountains, Iran	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Triassic; dinoflagellates; palynozone; palaeoenvironment; Alborz; Iran		The basal part of the Shemshak Group in the Galandrud area, north of the Alborz Mountains, Iran, was investigated palynologicaly. The section studied is located about 16 km south of Ruyan city (Alam-Deh). It attains a thickness of 590 m, and consists of limestones, shales, sandstones and siltstones. A total of 29 samples were collected and treated for palynological analysis. An assemblage of dinoflagellate cysts was encountered. Two palynological zones are erected on the basis of dinoflagellate cysts and discussed briefly. These are the Rhaetogonyaulax wigginsii and Rhaetogonyaulax rhaetica biozones. They are placed in a superzone, the Rhaetogonyaulax superzone and are quite comparable to the well-known biozones established for the Triassic sediments of Australia. The ratios of terrestrial to marine palynomorphs of the recorded assemblage from the base of the group show that parts of the section represent deposition in a marine environment. In late Norian, however, a regression of the sea caused sediments of the lower Rhaetian to be deposited in deltaic conditions. (C) 2004 Elsevier B.V. All rights reserved.	Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran	University of Tehran	Univ Tehran, Fac Sci, Dept Geol, Enghelab Ave, Tehran, Iran.	eghasemi@khayam.ut.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068				AGHANABATI A, 1997, GEOL SURV MINER EXPL, V65; Ainsworth N.R., 1989, Northwest European Micropaleontology and Palynology, P1; ALAVINAINI M, 1982, J SCI GEOL SURV MINE, V5, P38; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 2007, Paleopalynology; ASSERETO A, 1966, RIV ITAL PALEONTOL S, V72, P1133; Batten D., 1994, Cahiers de Micropaleontologie, V9, P21; Batten D.J., 1996, Palynology: Principles and Applications, P1065; BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; CARTIER ET, 1971, GEOLOGIE UNTERN CHAL, V164, P1; DABIRI O, 2002, THESIS PERSIAN; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; MCINTYRE DJ, 1977, GEOSCI MAN, V4, P111; Morbey S.J., 1978, Palinologia numero extraordinario, V1, P355; Nicoll R.S., 1994, J AUSTR GEOLOGY GEOP, V15, P101; *NISCO, 1998, PALYNOLOGICAL STUDY, V2, P1; VAHDATIDANESHMA.F, 1982, GEOLOGICAL SURVEY MI, P1; WILLIAMS GL, 1998, AASP CONTRIB SER, V34; WOOLLAM R, 1983, I GEOL SCI REP, V83, P1	19	21	21	0	0	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	DEC	2004	132	3-4					207	217		10.1016/j.revpalbo.2004.07.001	http://dx.doi.org/10.1016/j.revpalbo.2004.07.001			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	882JC					2025-03-11	WOS:000225934200004
J	Beaudouin, C; Dennielou, B; Melki, T; Guichard, F; Kallel, N; Berné, S; Huchon, A				Beaudouin, C; Dennielou, B; Melki, T; Guichard, F; Kallel, N; Berné, S; Huchon, A			The late-quaternary climatic signal recorded in a deep-sea turbiditic levee (Rhone Neofan, Gulf of Lions, NW Mediterranean):: palynological constraints	SEDIMENTARY GEOLOGY			English	Article						turbidites; palynology; late pleistocene; holocene; Mediterranean Sea	POLLEN DISTRIBUTION; MARINE-SEDIMENTS; SURFACE SEDIMENTS; FAN; TRANSPORT; RESPONSES	Siliciclastic turbidites represent huge volumes of sediments, which are of particular significance for (1) petroleum researchers, interested in their potential as oil reservoirs and (2) sedimentologists, who aim at understanding sediment transport processes from continent to deep-basins. An important challenge when studying marine turbidites has been to establish a reliable chronology for the deposits. Indeed, conventional marine proxies applied to hemipelagic sediments are often unreliable in detrital clays. In siliciclastic turbidites, those proxies can be used only in hemipelagic intervals, providing a poor constraint on their chronology. In this study, we have used sediments from the Rhone Neofan (NW Mediterranean Sea) to demonstrate that pollen grains can provide a high-resolution chronostratigraphical framework for detrital clays in turbidites. Vegetation changes occurring from the end of Marine Isotopic Stage 3 to the end of Marine Isotopic Stage 2 (from similar to30 to similar to18 ka cal. BP) are clearly recorded where other proxies have failed previously, mainly because the scarcity of foraminifers in these sediments prevented any continuous Sea Surface Temperature (SST) record and radiocarbon dating to be obtained. We show also that the use of palynology in turbidite deposits is able to contribute to oceanographical and sedimentological purposes: (1) Pinus pollen grains can document the timing of sea-level rise, (2) the ratio between pollen grains transported from the continent via rivers and dinoflagellate cysts (elutriating) allows us to distinguish clearly detrital sediments from pelagic clays. Finally, taken together, all these tools show evidence that the Rhone River disconnected from the canyon during the sea-level rise and thus evidence the subsequent rapid starvation of the neofan at 18.5 ka cal. BP. Younger sediments are hemipelagic: the frequency of foraminifers allowed to date sediments with radiocarbon. First results of Sea Surface Temperature obtained on foraminifers are in good agreement with the dinoflagellate cysts climatic signal. Both provide information on the end of the deglaciation and the Holocene. (C) 2004 Elsevier B.V. All rights reserved.	Univ Lyon 1, Lab PaleoEnvironm & PaleobioSphere, CNRS, UMR 5125, F-69622 Villeurbanne, France; IFREMER, Ctr Brest, Lab Environm Sedimentaires Geosci Marines, F-29280 Plouzane, France; Fac Sci Sfax, Sfax 3018, Tunisia; LSCE Vallee, F-91198 Gif Sur Yvette, France	Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; Ifremer; Universite de Sfax; Faculty of Sciences Sfax; Universite Paris Saclay	Univ Lyon 1, Lab PaleoEnvironm & PaleobioSphere, CNRS, UMR 5125, Campus Doua,Batiment Geode,2 Rue Dubois, F-69622 Villeurbanne, France.	celia.beaudouin@univ-lyon.fr		Dennielou, Bernard/0000-0002-9528-2746				ALOISI JC, 1973, CR ACAD SCI D NAT, V277, P145; ALOISI JC, 1986, THESIS U PERPIGNAN F; [Anonymous], 2012, Biometry; BEAUDOUIN C, IN PRESS J COASTAL R; BEAUDOUIN C, 2003, THESIS U LYON FRANCE; BEAUDOUIN C, IN PRESS MARINE PETR; Blum MD, 2000, SEDIMENTOLOGY, V47, P2, DOI 10.1046/j.1365-3091.2000.00008.x; BONNEL C, IN PRESS MARINE PETR; BUONCRISTIANI JF, 2001, 8 C FRANC SED ASF PA, P63; Cambon G, 1997, GRANA, V36, P105, DOI 10.1080/00173139709362596; Combourieu-Nebout N, 1998, QUATERNARY SCI REV, V17, P303, DOI 10.1016/S0277-3791(97)00039-5; Curray JR, 2002, MAR PETROL GEOL, V19, P1191, DOI 10.1016/S0264-8172(03)00035-7; DROZ L, 1985, AAPG BULL, V69, P460; Droz L, 2001, MAR GEOL, V176, P23, DOI 10.1016/S0025-3227(01)00147-5; DROZ L, 1983, THESIS U PARIS 6 PAR; Dupont LM, 2003, QUATERNARY SCI REV, V22, P157, DOI 10.1016/S0277-3791(02)00032-X; Flood R.D., 1991, Seismic facies and late Quaternary growth of Amazon submarine fan, Seismic facies and sedimentary processes of submarine fans and turbidite systems, P415, DOI DOI 10.1007/978-1-4684-8276-8_23; FLOOD RD, 1997, P OC DRILL PROGR SCI, V155, P696; Goñi MFS, 2000, QUATERNARY RES, V54, P394, DOI 10.1006/qres.2000.2176; Gregory WA, 1992, PALAIOS, V7, P3, DOI DOI 10.2307/3514794; Haberle S., 1997, Proc. 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Geol.	NOV 15	2004	172	1-2					85	97		10.1016/j.sedgeo.2004.07.008	http://dx.doi.org/10.1016/j.sedgeo.2004.07.008			13	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	874JJ					2025-03-11	WOS:000225346400005
J	Willumsen, PS				Willumsen, PS			Two new species of the dinoflagellate cyst genus <i>Carpatella</i> Grigorovich, 1969 from the Cretaceous-Tertiary transition in New Zealand	JOURNAL OF MICROPALAEONTOLOGY			English	Article							BIOSTRATIGRAPHY; BOUNDARY	A palynological study of Upper Cretaceous and Lower Paleocene sections from South Island, New Zealand, revealed the presence of two new species of Carpatella: Carpatella septata sp. nov. and Carpatella truncata sp. nov. Both species are stratigraphically important and the first occurrence of C. septata is a significant uppermost Maastrichtian event. Carpatella truncata is restricted to a narrow stratigraphical interval in the lowest Paleocene. J Micropalaeontol. 23(2): 119-125 November 2004.	Victoria Univ Wellington, Wellington, New Zealand	Victoria University Wellington	Willumsen, PS (通讯作者)，Univ Oslo, Inst Geofag, POB 1047, N-0316 Oslo, Norway.	pi.willumsen@geo.uio.no						[Anonymous], 1989, NZ GEOL SURV REC; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 1978, GEOLOGICAL SCI; DAMASSA S P, 1988, Palynology, V12, P167; EVITT WR, 1985, SPOROPELLENIN DINOFL; Fensome R.A., 1993, Micropaleontology Press Special Paper; FIELD BD, 1981, NZ GEOLOGICAL SCI G, V45, P1; Grigorovich AS., 1969, PALEONTOL SB, V6, P74; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; Hansen J. M., 1979, CRETACEOUS TERTIARY, P136; HANSEN JM, 1979, DAN GEOL UNDERS ARBO, P131; He C.-q., 1984, Acta Palaeontologica Sinica, V23, P768; HE CQ, 1991, LATE CREATCEOUS EARL; HELENES J, 1984, Palynology, V8, P107; HELENES J, 1986, Palynology, V10, P73; Hollis C.J., 1997, I GEOLOGICAL NUCL SC, V17; Hollis CJ, 2003, NEW ZEAL J GEOL GEOP, V46, P209, DOI 10.1080/00288306.2003.9515005; HOLLIS CJ, 1993, MAR MICROPALEONTOL, V21, P295, DOI 10.1016/0377-8398(93)90024-R; HOLLIS CJ, 2000, INTERRAD 2000 9 M IN; King P.R., 1999, CRETACEOUS RECENT SE; KJELLSTROM G, 1981, GEOL FOREN STOCK FOR, V103, P271, DOI 10.1080/11035898109454523; Partridge A., 1976, Australian Petroleum Exploration Association Journal, V16, P73; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Williams G.L., 2000, GLOSSARY TERMINOLOGY, V37; WILLIAMS GL, 1998, LENTIN WILLIAMS INDE, V34; Willumsen PS, 2000, GFF, V122, P180, DOI 10.1080/11035890001221180; WILLUMSEN PS, 2002, JOINT M AASP TMS NAM; Wilson G.J., 1988, New Zealand Geological Survey Paleontological Bulletin, V57, P1; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; Wilson G.J., 1987, NZ Geol. Surv. Rec, V20, P8	30	23	25	0	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	NOV	2004	23		2				119	125		10.1144/jm.23.2.119	http://dx.doi.org/10.1144/jm.23.2.119			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	941KK		hybrid			2025-03-11	WOS:000230213500004
J	Bison, KM; Wendler, J; Versteegh, GJM; Willems, H				Bison, KM; Wendler, J; Versteegh, GJM; Willems, H			<i>Tetratropis terrina</i> sp nov., a new calcareous dinoflagellate cyst from the Upper Campanian <i>polyplocum</i> zone of Lagerdorf (NW Germany)	JOURNAL OF MICROPALAEONTOLOGY			English	Article							CHALK	A new calcareous dinoflagellate cyst species, Tetratropis terrina sp. nov., with an apparent stratigraphically narrow range is described from the Upper Campanian Bostrychoceras polyplocum zone of the Lagerdorf chalk sequence (NW Germany). The electron microscopic and light microscopic analyses show that T terrina has both a pithonelloid wall type with uniformly inclined wall crystallites and a reduced peridiniacean paratabulation pattern. The prominent morphological similarities of T terrina to the other two Tetratropis species (T patina and T corbula) justify the affiliation of the new species to the genus. As a result of the extension of the morphological spectrum by the new species, the genus Tetratropis Willems 1990 has been emended. J Micropalaeontol. 23(2): 127-132, November 2004.	Univ Bremen, Div Palaeontol, FB 5, D-28334 Bremen, Germany; Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; Univ Utrecht, Fac Earth Sci, NL-3594 Utrecht, Netherlands	University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Bison, KM (通讯作者)，Univ Bremen, Div Palaeontol, FB 5, Postfach 330440, D-28334 Bremen, Germany.	kbison@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				Ernst H, 1984, MITTEILUNGEN GEOLOGI, V57, P137; Fensome R.A., 1993, Micropaleontology Press Special Paper; Hildebrand-Habel Tania, 1997, Courier Forschungsinstitut Senckenberg, V201, P177; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; Keupp Helmut, 1994, Abhandlungen der Geologischen Bundesanstalt (Vienna), V50, P197; Schulz M. G., 1984, EXKURSIONSFUHRER ERD, P483; Wendler J, 2004, REV PALAEOBOT PALYNO, V129, P133, DOI 10.1016/j.revpalbo.2003.12.011; Willems H., 1990, Senckenbergiana Lethaea, V70, P239; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; WILLEMS H, 1985, Senckenbergiana Lethaea, V66, P177; Young JR, 1997, PALAEONTOLOGY, V40, P875	12	5	5	1	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	NOV	2004	23		2				127	132		10.1144/jm.23.2.127	http://dx.doi.org/10.1144/jm.23.2.127			6	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	941KK		Green Submitted, hybrid			2025-03-11	WOS:000230213500005
J	Spezzaferri, S; Rögl, F				Spezzaferri, S; Rögl, F			<i>Bolboforma</i> (Phytoplankton Incertae Sedis), <i>Bachmayerella</i> and other Calciodinelloidea (Phytoplankton) from the Middle Miocene of the Alpine-Carpathian Foredeep (Central Paratethys)	JOURNAL OF MICROPALAEONTOLOGY			English	Article							CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; FORMATION MOLASSE BASIN; GRUND FORMATION; STRATIGRAPHY	Bolboforma is a microfossil of uncertain origin with affinities to protophytic algae. It generally occurs at high latitudes and/or in cool and temperate waters and has a high stratigraphic potential especially for the Miocene. Calcareous cysts of dinoflagellates represent the 'benthic cyst stage' of unicellular organisms belonging to the marine phytoplankton. The occurrence of Bolboforma, Bachmayerella is documented here and, for the first time, some calcareous cysts of dinoflagellates tentatively attributed to Alasphaera and Pithonella from Badenian (Langhian-Middle Miocene) sediments in Austrian and Moravian localities. Alasphaera and Pithonella were previously described from Cretaceous and Danian sediments only, therefore, their range has been extended into the Paratethyan Middle Miocene. Correlation of Bolboforma bioevents with standard geological time-scales allows confirmation, and in some cases refinement, of age assignments based on other microfossil groups, such as foraminifera and calcareous nannofossils, in Paratethyan areas. In particular, this paper presents a case study of the biostratigraphy of the Grund Formation outcropping at its type locality in Lower Austria. Age attribution of the Grund Formation has been uncertain for some time. The recovery of Praeorbulina glomerosa circularis and Uvigerina macrocarinata, associated with Bolboforma reticulata, allows the correlation of the Grund Formation with the Early Badenian (Middle Miocene). As planktonic foraminifera are generally very rare or absent in shelf deposits of many other Austrian and Moravian Middle Miocene sedimentary sequences, Bolboforma, and in particular B. reticulata, remains an important biomarker to identify lower Badenian sediments. Additionally, the new species Bolboforma gneixendorfensis Spezzaferri & Rogl is described. It is generally double-chambered with a weakly reticulate wall texture and is associated with Bolboforma reticulata, B. bireticulata and/or B. moravica. J. Micropalaeontol. 23(2): 139-152, November 2004.	Dept Geosci Geol & Paleontol, CH-1700 Fribourg, Switzerland; Nat Hist Museum, A-1014 Vienna, Austria		Dept Geosci Geol & Paleontol, Ch Du Musee 6, CH-1700 Fribourg, Switzerland.	silvia.spezzaferri@unifr.ch; fred.roegl@nhm-wien.ac.at						[Anonymous], 1990, European Neogene Mammal Chronology, DOI DOI 10.1007/978-1-4899-2513-8_2; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BIZON G, 1977, REV MICROPALEONTOL, V20, P140; Bolli H.M., 1974, Initial Rep Deep Sea Drilling Project, V27, P843; Brzák M, 2001, SCRIPTA FACULTATIS SCIENTIARUM NATURALIUM UNIVERSITATIS MASARYKIANAE BRUNENSIS - GEOLOGY, VOL 30/2000, P65; BRZOBOHATY R, 1983, 18 EUR C MICR EXC GU, P153; CICHA I, 1999, ZPRAVY GEOLOGICKYCH, P12; CICHA I, 1996, JB GEOL BUNDESANST, V139, P295; Cicha I., 1998, ABH SENCKENB NATF GE, V549, P1; Cooke PJ, 2002, PALAEOGEOGR PALAEOCL, V188, P73, DOI 10.1016/S0031-0182(02)00531-X; Coric S, 2004, GEOL CARPATH, V55, P165; Coric S, 2004, GEOL CARPATH, V55, P207; Coric S, 2004, GEOL CARPATH, V55, P147; CTYROKY P, 1996, JB GEOL BUNDESANST, V139, P296; CTYROKY P, 1997, JB GEOL BUNDESANST, V140, P283; DANIELS C. 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II Planktonic Conf, Roma, V2, P738; ODRZYWOLSKABIEN.E, 1976, KWARTALNIK GEOLOGICZ, V20, P551; Pallant A., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P381; Papp A., 1978, CHRONOSTRATIGRAPHIE, P168; PERVESLER P, 2002, MOL M 2002 WIEN 5 7, P25; PETROVA, 2001, GEOLOGY, V30, P55; POAG C W, 1986, Palaios, V1, P162, DOI 10.2307/3514510; POAG CW, 1987, INITIAL REP DEEP SEA, V95, P429; POIGNANT A, 1992, CR ACAD SCI II, V315, P1155; Poignant Armelle, 1997, Revue de Micropaleontologie, V40, P71, DOI 10.1016/S0035-1598(97)90101-X; Qvale G., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P487; Redinger J., 1992, ANN NATURHISTORISCHE, VA94, P15; RIO D, 1997, DEVELOP PAL, V15, P57; Roetzel R., 1999, ARBEITSTAGUNG GEOLOG; ROETZEL R, 1999, ARBEITSTAGUNG GEOLOG, P328; Rögl F, 1999, GEOL CARPATH, V50, P339; ROGL F, 1976, INIT REPTS DSDP, V35, P713; ROGL F, 1976, INITIAL REPORTS DEEP, V35, P701; ROGL F, 2002, COURIER FORSCH I SEN, V237, P47; ROGL F, 1979, ANN NATURHISTORISCHE, V82, P83; Spezzaferri, 2003, ANN NATURHIST MUS A, V104, P23; Spezzaferri S, 2004, GEOL CARPATH, V55, P155; Spezzaferri S, 2001, MAR MICROPALEONTOL, V43, P223, DOI 10.1016/S0377-8398(01)00032-9; Spezzaferri Silvia, 1998, Proceedings of the Ocean Drilling Program Scientific Results, V160, P125; Spezzaferri Silvia, 1998, Proceedings of the Ocean Drilling Program Scientific Results, V152, P201; Spiegler D., 2001, Geologisches Jahrbuch Reihe A, V152, P461; SPIEGLER D, 1991, J FORAMIN RES, V21, P126, DOI 10.2113/gsjfr.21.2.126; SPIEGLER D, 2002, P 8 BIANN M NO EUR C, P133; SPIEGLER D, 2004, PALAONTOLOGISCHES Z; Spiegler D, 1992, ANN NATURHISTORISCHE, V94, P59; SPIEGLER D, 1987, WERKGROUP TERTIAIRE, V24, P157; Spiegler Dorothee, 2001, Geologisches Jahrbuch Reihe A, V152, P175; Spiegler Dorothee, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P35; Spiegler Dorothee, 1996, Meyniana, V48, P135; STRANIK Z, 2000, SLOVAK GEOL MAGAZINE, V6, P88; Svabenicka L., 1999, B PANSTWOWEGO I GEOL, V387, P187; SZCHECHURA J, 1986, ACTA PALAEONTOLOGICA, V31, P213; SZCHECHURA J, 1997, B POLISH ACAD SCI EA, V45, P133; WEINHANDL R, 1957, VERH GEOL BUNDSANST, P120; Zuschin Martin, 2001, Historical Biology, V15, P123	71	7	7	0	4	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	NOV	2004	23		2				139	152		10.1144/jm.23.2.139	http://dx.doi.org/10.1144/jm.23.2.139			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	941KK		hybrid			2025-03-11	WOS:000230213500008
J	Hildebrand-Habel, T; Willems, H				Hildebrand-Habel, T; Willems, H			New calcareous dinoflagellates (Calciodinelloideae) from the Middle Coniacian to Upper Santonian chalks of Lagerdorf (northern Germany)	JOURNAL OF MICROPALAEONTOLOGY			English	Article							SOUTH ATLANTIC-OCEAN; WESTERN TROPICAL ATLANTIC; SURFACE SEDIMENTS; CYSTS; SEA; RECONSTRUCTION; ASSOCIATIONS; RISE	Three new calcareous dinotlagellate species from the Middle Coniacian to Upper Santonian chalks of Lagerdorf (northern Germany) are formally described: Calcicarpinum macrogranulum n. sp., Pirumella fragilis n. sp. and Ruegenia quinqueangulata n. sp. The species show differing vertical distribution patterns which might result from local sea-level changes: P. fragilis and R. quinqueangulata are restricted to the possibly transgressive upper Mid-Coniacian to Lower Santonian interval and C macrogranulum occurs consistently only in the probably regressive lower Mid-Coniacian and Middle to Upper Santonian intervals. J. Micropalaeontol. 23(2): 181-190, November 2004.	Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	University of Oslo; University of Bremen	Hildebrand-Habel, T (通讯作者)，Univ Oslo, Dept Geosci, POB 1047 Blindern, N-0316 Oslo, Norway.		Hildebrand-Habel, Tania/F-3590-2011					[Anonymous], CONTACT HILLS 90; Bolli H.M., 1974, Initial Rep Deep Sea Drilling Project, V27, P843; Bolli H.M., 1980, Initial Reports of the Deep Sea Drilling Project, V50, P525; BUTSCHLI O, 1885, KLASSEN ORDNUNGEN TH, V1, P865; Deflandre G., 1949, BOTANISTE, V34, P191; DIASBRITO D, 1985, COLETANEA TRABALHOS, V27, P307; EHRENBERG C.G., 1831, SYMBOLAE PHYS ZOOLOG; Ehrmann W. U., 1986, Geologisches Jahrbuch  Reihe A, V97, P3; Ernst G., 1974, Mitteilungen geol-palaont Inst Univ Hamburg, V43, P5; Ernst G., 1966, Mitteilungen aus dem Geologischen Staatsinstitut in Hamburg, V35, P115; Ernst H., 1978, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V48, P53; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; FENSOME RA, 1993, CLASSIFICATION LIVIN, P1; Haeckel E., 1894, SYSTEMATISCHE PHYLOG, V1, P1; HAKANSSON R., 1974, Pelagic sediments on land and under the sea, V1, P211; Hancock J.M., 1979, J GEOL SOC LONDON, V136, P175, DOI [DOI 10.1144/GSJGS.136.2.0175, 10.1144/gsjgs.136.2.0175]; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hildebrand-Habel T, 1999, REV PALAEOBOT PALYNO, V106, P57, DOI 10.1016/S0034-6667(98)00079-7; Hildebrand-Habel T, 2000, INT J EARTH SCI, V88, P694, DOI 10.1007/s005310050298; Hildebrand-Habel T, 2003, PALAEOGEOGR PALAEOCL, V197, P293, DOI 10.1016/S0031-0182(03)00470-X; Hildebrand-Habel Tania, 1997, Courier Forschungsinstitut Senckenberg, V201, P177; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; Keupp H., 1992, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V3, P191; Keupp H., 1989, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V106, P165; KEUPP H, 1984, Palaeontologische Zeitschrift, V58, P9; Keupp H., 1981, Facies, V5, P1, DOI 10.1007/BF02536655; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P161; Keupp H., 1984, Facies, V10, P153, DOI 10.1007/BF02536691; Keupp H, 2001, PALAEOGEOGR PALAEOCL, V174, P251, DOI 10.1016/S0031-0182(01)00296-6; Keupp Helmut, 1992, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V3, P121; Keupp Helmut, 1995, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V16, P155; Keupp Helmut, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V196, P221; Kienel Ulrike, 1994, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V12, P1; LENTIN JK, 1993, AASP CONTRIBUTION SE, V28; LENTIN JK, 1985, CANADIAN TECHNICAL R, V60; Pascher A., 1914, Berlin Ber D bot Ges, V32; Reháková D, 2000, GEOL CARPATH, V51, P229; Schmid F., 1982, Geologisches Jahrbuch  Reihe A, V61, P7; Schonfeld J., 1996, MITTEILUNGEN GEOLOGI, V77, P545; Schulz M.-G., 1978, NEWSL STRATIGR, V7, P73; SCHULZ MG, 1990, BEITRAGE GEOLOGIE PA, V10, P173; STRENG M, 2004, J NANNOPLANKTON RES, V26; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7; Vink A, 2002, PALAEOGEOGR PALAEOCL, V178, P53, DOI 10.1016/S0031-0182(01)00368-6; Vink A, 2001, PALEOCEANOGRAPHY, V16, P479, DOI 10.1029/2000PA000582; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; WILLEMS H, 1985, Senckenbergiana Lethaea, V66, P177; Willems H., 1992, Zeitschrift fuer Geologische Wissenschaften, V20, P155; WILLIAMS GL, 1998, AASP CONTRIBUTION SE, V34; Young JR, 1997, PALAEONTOLOGY, V40, P875; Zugel Peter, 1994, Courier Forschungsinstitut Senckenberg, V176, P1; Zugel Peter, 1996, Mitteilungen aus dem Geologisch-Palaeontologischen Institut der Universitaet Hamburg, V77, P191	56	1	1	1	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	NOV	2004	23		2				181	190		10.1144/jm.23.2.181	http://dx.doi.org/10.1144/jm.23.2.181			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	941KK		hybrid			2025-03-11	WOS:000230213500013
J	Manca, M; Carnovale, A; Alemani, P				Manca, M; Carnovale, A; Alemani, P			Exotopic protrusions and ellobiopsid infection in zooplanktonic copepods of a large, deep subalpine lake, Lago Maggiore, in northern Italy	JOURNAL OF PLANKTON RESEARCH			English	Article							1ST OBSERVATIONS; MICHIGAN	Exotopic protrusions were first recorded on zooplanktonic copepods of Lago Maggiore in 1992. They were classified into two types: (i) type I, the most abundant, dark, spherical and granular; (ii) type II, small, transparent and nongranular. They most commonly appeared on the lateral surface of adult Eudiaptomus padanus at the articulation of the second and third prosomal segments. Regular monitoring from 1994 to 2002 revealed the presence of additional, more complex protrusions, which may be later developmental stages of those already reported. In some instances, protrusions could be identified as successive stages of infection by ellobiopsids. The ellobiopsids are protists of uncertain taxonomic position, most probably achlorophyllous dinoflagellates, which during a phase of their life cycle parasitize zooplanktonic Crustacea. Originally described from marine organisms, the ellobiopsids have been reported from freshwater organisms only recently. They appear to herniate by puncturing the body of the host; this might explain the presence of host cells inside the cysts. Exotopic protrusions seem to represent a stable component of calanoid copepods from Lago Maggiore; however, they have been recently found to be more diverse in morphology and found to affect additional hosts, such as copepodites and nauplii of Cyclops abyssorum, which are the second most important copepod species of the lake.	CNR, ISE, Sez Idrobiol & Ecol Acque Interne, I-28922 Verbania, Italy	Consiglio Nazionale delle Ricerche (CNR); Istituto per lo Studio degli Ecosistemi (ISE-CNR)	CNR, ISE, Sez Idrobiol & Ecol Acque Interne, Largo Tonolli 52, I-28922 Verbania, Italy.	m.manca@ise.cnr.it						Ambrosetti W., 1999, J Limnol, V58, P1, DOI DOI 10.4081/JLIMNOL.1999.1; [Anonymous], 1989, ADV MAR BIOL, DOI DOI 10.1016/S0065-2881(08)60189-3; Bridgeman TB, 2000, CAN J FISH AQUAT SCI, V57, P1539, DOI 10.1139/cjfas-57-8-1539; CRISAFI P, 1975, Bollettino di Pesca Piscicoltura e Idrobiologia, V30, P207; GALT JH, 1970, ELLOBIOPSIS MICROBIO, V71, P295; Guzzella L, 1998, FRESEN ENVIRON BULL, V7, P79; Manca M, 2000, INT REV HYDROBIOL, V85, P209; MANCA M, 2003, 46 C GREAT LAK INT A; MANCA M, 1993, P 5 INT C CONS MAN L, P140; MANCA M, 1999, ZOOPL TUM WORKSH 15; Manca Marina, 1996, Memorie dell'Istituto Italiano di Idrobiologia, V54, P161; Messick GA, 2004, ZOOL STUD, V43, P314; Omair M, 1999, CAN J FISH AQUAT SCI, V56, P1711, DOI 10.1139/cjfas-56-10-1711; RAYNER NA, 1986, J PLANKTON RES, V8, P837, DOI 10.1093/plankt/8.5.837; Silina N., 1994, Hydrobiol. J., V30, P52; WEISSMAN P, 1990, LIMNOL OCEANOGR, V35, P954; XU ZK, 1991, HYDROBIOLOGIA, V209, P183, DOI 10.1007/BF00015341	17	10	11	1	4	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	NOV	2004	26	11					1257	1263		10.1093/plankt/fbh117	http://dx.doi.org/10.1093/plankt/fbh117			7	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	873DO		Bronze			2025-03-11	WOS:000225259800001
J	Flaim, G; Hansen, G; Moestrup, O; Corradini, F; Borghi, B				Flaim, G; Hansen, G; Moestrup, O; Corradini, F; Borghi, B			Reinterpretation of the dinoffagellate '<i>Glenodinium sanguineum'</i> in the reddening of Lake Tovel, Italian Alps	PHYCOLOGIA			English	Article								Lake Tovel in the Italian Alps is famous for its blood-red water during summer, caused by a dinoflagellate named Glenodinium sanguineum. The red colour has been largely absent since 1964 and a project aimed at understanding the underlying cause of the colour change was begun in 2000. It appears that there are three dinoflagellates in the lake that morphologically somewhat resemble 'G. sanguineum'. One of these agrees with the 'red form' of G. sanguineum studied in the detailed work of Baldi (1941). and is now very scarce in the plankton. The other agrees with Baldi's 'green form' and now dominates the plankton. Transmission electron microscopy has demonstrated that the third taxon is identical to what Dodge et al. (1987) identified as G. sanguineum from Lake Tovel. It did not develop a red colour under any of the growth conditions used in our experiments. The red form is very similar to Woloszynskia coronata, but differs in cyst morphology. It is shown that the red and green forms of G. sanguineum sensu Baldi are clearly distinct species. Reduction in nutrient loads entering the lake subsequent to changes in animal husbandry practices in the lake's catchment occurred around 1964. This apparently tipped the balance between the three species of dinoflagellates, resulting in the near disappearance of the red form from the plankton and concomitant disappearance of the red colour from the lake.	Ist Agrario, I-38010 San Michele All Adige, TN, Italy; Univ Copenhagen, Inst Biol, Dept Phycol, DK-1353 Copenhagen, Denmark	Fondazione Edmund Mach; University of Copenhagen	Flaim, G (通讯作者)，Ist Agrario, I-38010 San Michele All Adige, TN, Italy.	giovanna.flaim@ismaa.it	Flaim, Giovanna/AAD-5013-2020; Hansen, Gert/P-3328-2014; Flaim, Giovanna/C-7622-2016	Hansen, Gert/0000-0002-5751-8316; Moestrup, Ojvind/0000-0003-0965-8645; Flaim, Giovanna/0000-0002-1753-5605				Andersen RA, 1997, J PHYCOL, V33, P1, DOI 10.1111/j.0022-3646.1997.00001.x; ARRIGHETTI A, 1979, QUADERNI ESPERIENZE, V5, P1; Baldi E., 1938, Studi Trentini Trento, V19, P247; Baldi E., 1941, Memorie del Museo di Storia Naturale della Venezia Tridentina, V6, P1; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CANTONATI M, 2002, STUDI TRENTINI SCI N, V78, P167; Cantonati Marco, 2003, Journal of Limnology, V62, P79; Cavalca L, 2001, ANN MICROBIOL, V51, P159; Corradini F., 2001, ATTI ASS ITALIANA OC, V14, P209; DIESING K.M., 1866, SITZUNGBERICHTE MATH, V52, P287; DODGE J D, 1970, Studi Trentini di Scienze Naturali Sezione B Biologica, V47, P91; DODGE J D, 1987, Archiv fuer Hydrobiologie Supplement, V78, P125; Flaim G, 2003, HYDROBIOLOGIA, V502, P357, DOI 10.1023/B:HYDR.0000004293.59239.6f; FRESHFIELD DW, 1975, ITALIAN ALPS SKETCHE; GRUNG M, 1993, BIOCHEM SYST ECOL, V21, P757, DOI 10.1016/0305-1978(93)90088-9; LARGAIOLLI V, 1907, NUOVA NOTARISIA, V18, P1; LINDBERG K, 2004, STUDY FRESHWATER DIN; LOEBLICH AR, 1980, TAXON, V29, P321, DOI 10.2307/1220299; MARCHESONI V, 1941, STUDI TRENTINI SCI N, V22, P11; Marchesoni V., 1959, NATURA ALPINA, V10, P37; MIOLA A, 1982, Studi Trentini di Scienze Naturali Acta Biologica, V59, P23; Paganelli Arturo, 1992, Memorie dell'Istituto Italiano di Idrobiologia Dott Marco de Marchi, V50, P225; Parducz B., 1967, International Review of Cytology, V21, P91, DOI 10.1016/S0074-7696(08)60812-8; Popovsky J., 1990, Dinophyceae (Dinoflagellida); Rodriguez S., 1999, Algological Studies, V95, P15; TAYLOR FJR, 1987, BIOL DINOFLAGELLATES, P723; TOLOTTI M, 1999, P 8 INT C CONS MAN L, V2; Tomasi G, 1989, NATURA ALPINA, V40, P1; WOLOSYNSKA J, 1917, B INT ACAD SCI C B B, V57, P114; [No title captured]	30	12	13	0	4	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	NOV	2004	43	6					737	743		10.2216/i0031-8884-43-6-737.1	http://dx.doi.org/10.2216/i0031-8884-43-6-737.1			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	886IQ					2025-03-11	WOS:000226220900012
J	Holeck, KT; Mills, EL; MacIsaac, HJ; Dochoda, MR; Colautti, RI; Ricciardi, A				Holeck, KT; Mills, EL; MacIsaac, HJ; Dochoda, MR; Colautti, RI; Ricciardi, A			Bridging troubled waters: Biological invasions, transoceanic shipping, and the Laurentian Great Lakes	BIOSCIENCE			English	Article						Great Lakes; ship vector; ballast; nonindigenous species; vector assignment protocol	AMPHIPOD ECHINOGAMMARUS-ISCHNUS; MUSSEL DREISSENA-POLYMORPHA; BALLAST WATER; DINOFLAGELLATE CYSTS; RISK-ASSESSMENT; DISPERSAL; SHIPS; CONSERVATION; ORGANISMS; TRANSPORT	Release of contaminated ballast water by transoceanic ships has been implicated in more than 70% of faunal nonindigenous species (NIS) introductions to the Great Lakes since the opening of the St. Lawrence Seaway in 1959. Contrary to expectation, the apparent invasion rate increased after the initiation of voluntary guidelines in 1989 and mandatory regulations in 1993 for open-ocean ballast water exchange by ships declaring ballast on board (BOB). However, more than 90% of vessels that entered during the 1990s declared no ballast on board (NOBOB) and were not required to exchange ballast, although their tanks contained residual sediments and water that would be discharged in the Great Lakes. Lake Superior receives a disproportionate number of discharges by both BOB and NOBOB ships, yet it has sustained surprisingly few initial invasions. Conversely, the waters connecting Lakes Huron and Erie are an invasion hotspot despite receiving disproportionately few ballast discharges. Other vectors, including canals and accidental release, have contributed NIS to the Great Lakes and may increase in relative importance in the future. Based on our knowledge of NIS previously established in the basin, we have developed a vector assignment protocol to systematically ascertain vectors by which invaders enter the Great Lakes.	Cornell Univ, Biol Field Stn, Bridgeport, CT USA; Cornell Univ, Dept Nat Resources, Ithaca, NY 14853 USA; Univ Windsor, Great Lakes Inst Environm Res, Windsor, ON N9B 3P4, Canada	Cornell University; Cornell University; University of Windsor	Cornell Univ, Biol Field Stn, Bridgeport, CT USA.	kth1@cornell.edu	Ricciardi, Anthony/A-8536-2010; macisaac, hugh/AAE-3742-2020; Colautti, Robert/E-6804-2011	Ricciardi, Anthony/0000-0003-1492-0054; Colautti, Robert/0000-0003-4213-0711				Apte Smita, 2000, Biological Invasions, V2, P75, DOI 10.1023/A:1010024818644; Arnott DL, 1996, CAN J FISH AQUAT SCI, V53, P646, DOI 10.1139/cjfas-53-3-646; *ASI, 1996, EX AQ NUIS SPEC INTR; Bailey SA, 2003, LIMNOL OCEANOGR, V48, P1701, DOI 10.4319/lo.2003.48.4.1701; bij de Vaate A, 2002, CAN J FISH AQUAT SCI, V59, P1159, DOI 10.1139/F02-098; Bruno JF, 2003, TRENDS ECOL EVOL, V18, P119, DOI 10.1016/S0169-5347(02)00045-9; Carlton JT, 1996, BIOL CONSERV, V78, P97, DOI 10.1016/0006-3207(96)00020-1; CARLTON JT, 1989, CONSERV BIOL, V3, P265, DOI 10.1111/j.1523-1739.1989.tb00086.x; 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J	Vecoli, M; Le Hérissé, A				Vecoli, M; Le Hérissé, A			Biostratigraphy, taxonomic diversity and patterns of morphological evolution of Ordovician acritarchs (organic-walled microphytoplankton) from the northern Gondwana margin in relation to palaeoclimatic and palaeogeographic changes	EARTH-SCIENCE REVIEWS			English	Review						acritarchs; Cambro-Ordovician; biodiversity; biostratigraphy; palaeobiogeography; palaeoceanography	SILURIAN OCEANIC EPISODES; ARENIG EARLY ORDOVICIAN; EUROPEAN SUTURE ZONE; YANGTZE GORGES AREA; CAMBRIAN-ORDOVICIAN; ALGERIAN SAHARA; ACID-RESISTANT; HUBEI PROVINCE; IAPETUS OCEAN; DIVERSIFICATION	Acritarchs, the fossilizable, resting cysts of phytoplanktonic algal protists, are the dominant component of marine organic-walled microfossils in the Palaeozoic. The majority of acritarchs show strong similarities with dinoflagellate cysts in morphological and biogeochemical features, as well as distributional patterns in the sediments. The production of these organic-walled microfossils and their distribution and survivorship in the sediments were controlled by differences in ecological tolerances and life cycle (autecology) of the planktonic parent organisms. Calculation of evolutionary rates and development of a detailed diversity curve at specific level, form the basis for discussing the influence of global palaeoenvironmental perturbations on the evolution of organic-walled microphytoplankton in northern Gondwana during latest Cambrian through Ordovician times. The potential of acritarchs for biostratigraphic correlation at the regional scale (northern Gondwana domain) is much improved by our detailed revision of distributional patterns of 245 acritarch taxa. The most important Cambro-Ordovician acritarch bio-events are short periods of diversification, which also correspond to introduction of morphological innovations, observed in latest Cambrian and earliest Tremadoc, late Tremadoc, early Arenig, basal Llanvirn, and latest Ashgill, and an important extinction phase in the early Caradoc. Overall, acritarch diversity increased from the basal Ordovician up to the middle Llanvirn, then declined in the early and middle Caradoc. During Ashgill times, the assemblages are poorly diversified at the generic level as a result of a combined effect of sea level drawdown and onset of glacial conditions, but no major extinction event is observed in connection with the end-Ordovician biotic crisis. The peak in acritarch diversity during Middle Ordovician times appears to be correlated to maximum spread of palaeogeographical assembly. Acritarch dynamics appear largely uncorrelated to second order sea-level oscillations; the primary abiotic controls on acritarch evolution were palaeogeographical and the associated palaeoceanographic changes (especially during Middle Ordovician), and the end-Ordovician palaeoclimatic shift. The acritarch fossil record provides important information on the evolution of oceanic primary producers, however, the relationships between acritarch diversity, oceanic productivity, and evolution of invertebrate animals are proving much more complex than previously thought. In particular, the hypothesis of a causal relationship between changes in acritarch diversity and metazoan evolution in the Palaeozoic is not supported by our data. (C) 2004 Elsevier B.V. All rights reserved.	Univ Bretagne Occidentale, Lab Paleontol, UMR 6538, CNRS, F-29285 Brest, France	Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Univ Sci & Tech Lille Flandres Artois, UMR 8014, Lab Paleontol & Paleogeog Paleozoique LP3, UMR 8014 & FR 1818 CNRS, Bat SN5, F-59655 Villeneuve Dascq, France.	marco.vecoli@univ-lille1.fr	Vecoli, Marco/AAK-5473-2020	Vecoli, Marco/0000-0001-9203-7625				ALAMERI TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103, DOI 10.1016/0031-0182(83)90007-X; ALBANI R, 1985, MEMORIE SERIE A, V91, P1; ALBANO E, 1989, FREE RADICAL BIO MED, V6, P3, DOI 10.1016/0891-5849(89)90152-4; [Anonymous], J SCI; [Anonymous], GSA SPEC PAP; [Anonymous], [No title captured]; [Anonymous], THESIS TU BERLIN; [Anonymous], 1974, PALAEONTOGRAP ABT B; [Anonymous], 1971, GRES PALEOZOIQUE INF; [Anonymous], 1967, Acta de la Socit, Linnenne de Bordeaux; [Anonymous], 1969, PALAEONTOL POLONCA; BABIN C, 1993, B SOC GEOL FR, V164, P141; Bambach RK, 1999, GEOBIOS-LYON, V32, P131, DOI 10.1016/S0016-6995(99)80025-4; Barnes C.R., 1996, Global Events and Event Stratigraphy, P139; BENTON MJ, 1995, SCIENCE, V268, P52, DOI 10.1126/science.7701342; Bergstrom S.M., 1990, Geological Society Memoir, P105, DOI 10.1144/GSL.MEM.1990.012.01.09; Berry WBN., 1995, STUDIES GEOPHYS EFFE, P34; Berthelsen A., 1992, CONTINENT REVEALED E, P153; Bickert T, 1997, GEOCHIM COSMOCHIM AC, V61, P2717, DOI 10.1016/S0016-7037(97)00136-1; BOURAHROUH A, 2002, THESIS U RENNES 1; Brenchley P.J., 1995, Modern Geology, V20, P69; Brenchley P J., 1988, Bulletin of the British Museum of Natural History (Geology), V43, P377; Brocke R, 2000, REV PALAEOBOT PALYNO, V113, P27, DOI 10.1016/S0034-6667(00)00050-6; Brocke Rainer, 1995, P473; BUCEFALOPALLIAN.R, 2002, ANN M CURIE FELLOWSH, V2, P39; Burmann G., 1970, Palaontologische Abh Berlin (Abt B), V3, P289; Carr ID, 2002, J PETROL GEOL, V25, P259, DOI 10.1111/j.1747-5457.2002.tb00009.x; Christiansen JL, 1999, TERRA NOVA, V11, P73, DOI 10.1046/j.1365-3121.1999.00229.x; COCCHIO A, 1981, THESIS U P SABATIER; Cocchio A.-M., 1982, Revue de Micropaleontologie, V25, P26; COCKS LRM, 1990, GEO SOC MEM, V12, P97, DOI 10.1144/GSL.MEM.1990.012.01.08; Cocks LRM, 1997, GEOL MAG, V134, P627, DOI 10.1017/S0016756897007425; COCKS LRM, 1982, J GEOL SOC LONDON, V139, P465, DOI 10.1144/gsjgs.139.4.0465; COCKS LRM, 1998, GEOLOGICA, V42, P399; COLBATH G K, 1979, Palaeontographica Abteilung B Palaeophytologie, V171, P1; COLBATH GK, 1990, GEO SOC MEM, V12, P207, DOI 10.1144/GSL.MEM.1990.012.01.19; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; COOPER AH, 1990, GEOLOGICAL MAGAZINE, V127, P137; COOPER RA, 1992, GLOBAL PERSPECTIVES ON ORDOVICIAN GEOLOGY, P3; COOPER RA, 1999, 8 INT S ORD SYST QUO, V43, P1; Cope JCW, 1999, GEOBIOS-LYON, V32, P175, DOI 10.1016/S0016-6995(99)80029-1; CRAMER F H, 1977, Micropaleontology (New York), V23, P339, DOI 10.2307/1485220; Cramer FH, 1968, NEUES JB GEOLOGIE PA, V10, P591; Cramer FH., 1971, REV ESP MICROPALEONT, P1; Cramer FH., 1974, Palaeontographica. 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Rev.	OCT	2004	67	3-4					267	311		10.1016/j.earscirev.2004.03.002	http://dx.doi.org/10.1016/j.earscirev.2004.03.002			45	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	897WP					2025-03-11	WOS:000227037000003
J	Svobodová, M; Hradecká, L; Skupien, P; Svábenická, L				Svobodová, M; Hradecká, L; Skupien, P; Svábenická, L			Microfossils of the Albian and Cenomanian shales from the Stramberk area (Silesian Unit, Outer Western Carpathians, Czech Republic)	GEOLOGICA CARPATHICA			English	Article						Cretaceous; Outer Western Carpathians; palynomorphs; foraminifers; calcareous nannofossils; biostratigraphy; paleoecology	BASIN	Microbiostratigraphic study of sporomorphs, dinoflagellate cysts, foraminifers and calcareous nannofossils documented the age and paleoenvironmental features of black and grey-green, organic-rich sediments in the classical area of Stramberk (Baska Formation, Silesian Unit, Outer Western Carpathians). Age-assessments suggest Late Albian and Cenomanian age (foraminiferal Zones Rotalipora appenninica, R. reicheli and X cushmani; nannoplankton Zones BC27/UCO-UC4). The character of dinoflagellate cyst assemblages (e.g. presence Pterodinium) reflects open-sea enviroment. The presence of calcareous foraminifers and nannofossils gives an evidence of depositional conditions above the carbonate compensation depth (CCD). The presence of some terrestrial and non-marine aquatic palynomorphs (e.g. Tetraporina, Lecaniella) documents the proximity of a continent and fluvio-lacustrine influences. The presence of microfossils tolerating low-oxygen bottom conditions such as foraminifers of genus Lingulogavelinella and jaws of polychateous annelids (scolecodonts) reflect a dysaerobic bottom environment. Co-occurrence of Boreal and Tethyan species encountered in foraminiferal and palynomorph assemblages documents the influences from the higher latitudes on the depositional area of northern Tethys. Moreover, Lower-?Middle Cenomanian sporomorphs (angiosperms) have similar character to others of the same age from the Blansko Graben, in the SE part of the Bohemian Cretaceous Basin, which is situated on the SE border of the West European plate.	Acad Sci Czech Republ, Inst Geol, Prague 16500 6, Czech Republic; Czech Geol Survey, Prague 11821 1, Czech Republic; Tech Univ Ostrava, Ostrava 70833, Czech Republic	Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Czech Geological Survey; Technical University of Ostrava	Acad Sci Czech Republ, Inst Geol, Rozvojova 135, Prague 16500 6, Czech Republic.	msvobodova@gli.cas.cz; hradecka@cgu.cz; skupien@vsb.cz; svab@cgu.cz	Svobodova, Marcela/I-8793-2014; Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X				Bown P.R., 1998, P86; Burnett J.A., 1998, P132; COURTINAT B, 1990, GEOBIOS-LYON, V23, P387, DOI 10.1016/S0016-6995(06)80268-8; ELIAS M, 1965, 7 C SOFIA 2, V1, P257; ELIAS M, 1983, VEST USTR UST GEOL, V58, P235; Elias M., 1963, VESTNIK CESKEHO GEOL, V38, P133; ELIAS M., 1970, Sbornik Geologickych Ved, Rada G, V18, P7; Eliasˇ M., 2003, TECHNICKE UNIVERZITY, V49, P7; HANZLIKOVA E, 1973, Sbornik Geologickych Ved Rada P Paleontologie, V15, P119; Hanzlikova E, 1962, MS ARCH USTR UST GEO; Hanzlkova E., 1963, Geologicky Sbornik Slovensk Akad, V14, P37; Hlustik A., 1979, ACTA MUSEI MORAVIAE, V64, P25; HOUSA V, 1996, ZPR GEOL VYZK V R, P95; HOUSA V, 1987, ATT 2 CONV INT F E A, V87, P365; HOUSA V., 1976, Casopis Slezskeho Musea A, V25, P119; HOUSA V, 1976, CAS SLEZ MUZ SER A, V25, P65; Hradecka L., 1993, SBORNIK GEOLOGICKYCH, V33, P79; JARVIS I, 1988, Cretaceous Research, V9, P3, DOI 10.1016/0195-6671(88)90003-1; JUHASZ M, 1983, ACTA GEOL HUNG, V26, P1; Juhasz M., 1983, Acta Geologica Hungarica, V26, P41; KOUTSOUKOS EAM, 1990, T ROY SOC EDIN-EARTH, V81, P221, DOI 10.1017/S0263593300005253; KREJCI O, 1999, GEOL VYZK MOR SLEZ R, P56; Leerveld H., 1995, LPP Contribution Series, V2, P1; Lister J.K., 1988, Palaeontographica Abteilung B, V210, P8; LOEBLICH AR, 1988, NOSTRAND REINHOLD, P1; MATEJKA A, 1955, ZPR GEOL VYZK ROCE 1, P110; MATEJKA A, 1949, SBOR STAT GEOL UST, P293; MENCIK E, 1983, ROZPR USTR UST GEOL, P1; PICHA F, IN PRESS AAPG MEMOIR; Robaszynski F, 1995, B SOC GEOL FR, V166, P681; ROTH PH, 1986, MAR MICROPALEONTOL, V10, P235, DOI 10.1016/0377-8398(86)90031-9; SISSINGH W, 1977, Geologie en Mijnbouw, V56, P37; SKUPIEN P, 2003, SBOR PRACI VYS SK BA, V8, P65; Skupien P, 1997, SBOR VED PRACI VYS S, P34; SKUPIEN P, 1999, THESIS VSB TU OSTRAV, P1; Skupien Petr, 1999, Vestnik Ceskeho Geologickeho Ustavu, V74, P1; Stranik Z., 1997, GEOL VYZK MOR SLEZ R, P43; Stranik Zdenek, 1996, Vestnik Ceskeho Geologickeho Ustavu, V71, P1; SVOBODOVA M, 1987, Vestnik Ustredniho Ustavu Geologickeho, V62, P165; Svobodova M., 1999, Acta Palaeobot. Suppl., V2, P199; SVOBODOVA M, 1998, ZPR GEOL VYZK ROCE, P71; Svobodova Marcela, 1998, Vestnik Ceskeho Geologickeho Ustavu, V73, P229; ULICNY D, 1993, CRETACEOUS RES, V14, P211, DOI 10.1006/cres.1993.1015; Vavrdova M., 1981, Casopis pro Mineralogii a Geologii, V26, P421; Vavrdova M, 1964, CAS NAR MUZ ODD PRIR, V133, P37; VAVRDOVA M, 1964, SBOR GEOL VED R P, V4, P91	46	15	17	0	6	SLOVAK ACAD SCIENCES GEOLOGICAL  INST	BRATISLAVA	DUBRAVSKA CESTA 9, BRATISLAVA, 840 05, SLOVAKIA	1335-0552	1336-8052		GEOL CARPATH	Geol. Carpath.	OCT	2004	55	5					371	388						18	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	874RK					2025-03-11	WOS:000225367300003
J	Smith, BC; Persson, A				Smith, BC; Persson, A			Dinoflagellate cyst production in one-liter containers	JOURNAL OF APPLIED PHYCOLOGY			English	Article						Alexandrium; cyst; dinoflagellate; gamete; mating; Scrippsiella	GONYAULAX-TAMARENSIS	Methods for the production of dinoflagellate cysts in two types of 1 L containers have been developed. Using these methods, dinoflagellate cysts can be produced in amounts large enough for shellfish grazing experiments or whenever large amounts of cysts are needed. The species used were Scrippsiella lachrymosa (B-10) and toxic Alexandrium fundyense (CB501 and GTM25). Cultures of S. lachrymosa yielded 628 +/- 74 cysts mL(-1) and A. fundyense cultures yielded 350 +/- 98 cysts mL(-1). Findings suggest that aspects of the boundary layer between the media and the wall of the container are important for gamete mating; especially, the slope of the container wall appears to be relevant, which offers some explanation of previous observations that the shape of the container is important in the formation of dinoflagellate resting cysts. These observations may support the theory that physical interfaces in nature facilitate dinoflagellate encystment.	NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Smith, BC (通讯作者)，NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514				Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; ELBRACHTER M, 2002, 10 INT C HARMF ALG 2; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Lazier J. R. N., 1991, DYNAMICS MARINE ECOS; LEWIS J., 2001, LIFEHAB LIFE HIST MI, P121; PARKER NS, 2001, P 9 INT C HARMF ALG; Smayda Theodore J., 2002, Harmful Algae, V1, P95, DOI 10.1016/S1568-9883(02)00010-0; Sullivan JM, 2003, HARMFUL ALGAE, V2, P183, DOI 10.1016/S1568-9883(03)00039-8; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; Vogel S., 1994, LifeinMovingFluids: ThePhysicalBiologyofFlowRevisedandExpandedSecondEdition; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	13	16	17	0	7	KLUWER ACADEMIC PUBL	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-8971			J APPL PHYCOL	J. Appl. Phycol.	OCT	2004	16	5					401	405		10.1023/B:JAPH.0000047951.72497.53	http://dx.doi.org/10.1023/B:JAPH.0000047951.72497.53			5	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Marine & Freshwater Biology	870FF					2025-03-11	WOS:000225042300007
J	Kim, SH; Kim, KY; Kim, CH; Lee, WS; Chang, M; Lee, JH				Kim, SH; Kim, KY; Kim, CH; Lee, WS; Chang, M; Lee, JH			Phylogenetic analysis of harmful algal bloom (HAB)-causing dinoflagellates along the Korean coasts, based on SSU rRNA gene	JOURNAL OF MICROBIOLOGY AND BIOTECHNOLOGY			English	Article						SSU rDNA; dinoflagellate; harmful algal bloom; phylogeny	18S RDNA SEQUENCES; PFIESTERIA-PISCICIDA; BAYESIAN-INFERENCE; DINOPHYCEAE; IDENTIFICATION; YESSOTOXIN; TAMARENSE; CYST	Twenty-three cultures of harmful algal bloom (HAB)causing dinoflagellates were isolated from the coastal waters of Korea. For each of the 14 morphospecies, the nuclear-encoded small subunit (SSU) rDNA was analyzed to determine the phylogenetic relatedness of the species. Despite temporal and spatial isolation, 3-4 clonal cultures of Alexandrium catenella, Cochlodinium polykrikoides, and Gymnodinium catenatum had 100% identical SSU rDNA sequences. In contrast, heterogeneities in the SSU rDNA sequences were observed in Akashiwo sanguinea and Lingulodinium polyedrum strains. Extreme sequence polymorphism was shown within the SSU rRNA genes of an Al tamarense clonal culture. A homology search in GenBank revealed that 11 dinoflagellate species were located in clusters corresponding to their morphological classification. The SSU rDNA sequences of C polykrikoides,Gyrodinium instriatum, and Pheopolykrikos hartmannii, which were determined for the first time in this study, showed the following phylogenetic relationships: C. polykrikoides formed an independent branch separated from other dinoflagellates; Gyr. instriatum was placed in a monophyletic group with Gyr. dorsum and Gyr. uncatenum; and Ph. hartmanii, which forms a distinct two-celled pseudocolony, belonged to Gymnodinium sensu Hansen and Moestrup.	Korea Ocean Res & Dev Inst, Microbiol Lab, Ansan 425600, South Korea; Sungkyunkwan Univ, Dept Biol Sci, Suwon 440746, South Korea; Sungkyunkwan Univ, Basic Sci Res Inst, Suwon 440746, South Korea; Pukyong Natl Univ, Dept Aquaculture, Pusan 608737, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Sungkyunkwan University (SKKU); Sungkyunkwan University (SKKU); Pukyong National University	Korea Ocean Res & Dev Inst, Microbiol Lab, POB 29, Ansan 425600, South Korea.	jlee@kordi.re.kr						Adachi M, 1997, FISHERIES SCI, V63, P701, DOI 10.2331/fishsci.63.701; Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.x; AKIBA T., 1949, JAPANESE JOUR EXPT MED, V20, P271; Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; Baek SH, 2003, J MICROBIOL BIOTECHN, V13, P651; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; CAVALIERSMITH T, 1993, MICROBIOL REV, V57, P953, DOI 10.1128/MMBR.57.4.953-994.1993; CHO CH, 1978, B KOREAN FISH SOC, V11, P111; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Draisci R, 1999, TOXICON, V37, P1187, DOI 10.1016/S0041-0101(98)00254-2; Edgcomb VP, 2002, P NATL ACAD SCI USA, V99, P7658, DOI 10.1073/pnas.062186399; Faus M.A., 2002, SMITHSONIAN I CONTRI, V42, P1; Fukuyo Y., 1990, RED TIDE ORGANISMS J, P84; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HAN MS, 1992, J PLANKTON RES, V14, P1581, DOI 10.1093/plankt/14.11.1581; Han Myung-Soo, 1993, Korean Journal of Phycology, V8, P7; HERZOG M, 1986, P NATL ACAD SCI USA, V83, P8644, DOI 10.1073/pnas.83.22.8644; Huelsenbeck JP, 2001, SCIENCE, V294, P2310, DOI 10.1126/science.1065889; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; IWASAKI H, 1961, BIOL BULL-US, V121, P173, DOI 10.2307/1539469; Jin E, 2003, J MICROBIOL BIOTECHN, V13, P165; Kim C.-H., 1997, Algae, V12, P269; Kim H.G., 1997, RECENT RES TIDES KOR, P280; Kim Hak Gyoon, 1996, Journal of the Korean Fisheries Society, V29, P837; Kim Hak Gyoon, 1997, Ocean Research (Seoul), V19, P185; Kim Keun-Yong, 2002, Algae, V17, P11; Kofoid C. 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Microbiol. Biotechnol.	OCT	2004	14	5					959	966						8	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	867BO					2025-03-11	WOS:000224817300011
J	Thomson, PG; Wright, SW; Bolch, CJS; Nichols, PD; Skerratt, JH; McMinn, A				Thomson, PG; Wright, SW; Bolch, CJS; Nichols, PD; Skerratt, JH; McMinn, A			Antarctic distribution, pigment and lipid composition, and molecular identification of the brine dinoflagellate <i>Polarella glacialis</i> (Dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						27-nor-24-methylcholest-5; 22E-dien-3 beta-ol; Antarctic fast ice; photosynthetic pigments; Polarella glacialis; polyunsaturated fatty acids; rDNA; sterols	FATTY-ACID; SEA-ICE; STEROL COMPOSITION; ALEXANDRIUM DINOPHYCEAE; GYMNODINIUM-CATENATUM; SOUTHERN-OCEAN; MCMURDO SOUND; MICROALGAE; CYST; PHYTOPLANKTON	Polarella glacialis (Montresor et al.) was identified in Davis Station sea ice by morphological and DNA sequence comparison of cultures with those of the authentic strain P. glacialis CCMP 1383 isolated from McMurdo Sound. Cells and cysts of the Davis isolate (FL1B) were morphologically indistinguishable from P. glacialis, and comparison of the large subunit rDNA of both cultures demonstrated only 0.2% sequence divergence over 1366 base pairs. The photosynthetic pigments of P. glacialis (strains FL1B and CCMP 1383) were typical of dinoflagellates, with peridinin (contributing up to 31%) as the major accessory pigment. Extremely high levels of polyunsaturated fatty acids (PUFA, up to 76.3%) were characteristic of P. glacialis isolate FL1B. The high PUFA concentration of this species is thought to be an adaptation to survive the cold temperatures of the upper fast ice. The sterol profile of FL1B was atypical of dinoflagellates, with 4-desmethylsterols (up to 79%) in greater abundance than 4alpha-methyl sterols (up to 24%). 27-Nor-24-methylcholest-5,22E-dien-3beta-ol was identified as the principle sterol in P. glacialis, contributing up to 64% of the total sterol composition.	Australian Antarctic Div, Dept Environm & Heritage, Kingston, Tas 7050, Australia; Antarctic Climate & Ecosyst CRC, Kingston, Tas 7050, Australia; Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia; CSIRO Marine Res, Hobart, Tas 7001, Australia; Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia; Univ Tasmania, Antarctic Climate & Ecosyst CRC, Hobart, Tas 7001, Australia	Australian Antarctic Division; University of Tasmania; University of Tasmania; Commonwealth Scientific & Industrial Research Organisation (CSIRO); University of Tasmania; University of Tasmania	Thomson, PG (通讯作者)，Australian Antarctic Div, Dept Environm & Heritage, Channel Highway, Kingston, Tas 7050, Australia.	Paul.Thomson@aad.gov.au	McMinn, Andrew/A-9910-2008; Bolch, Christopher/J-7619-2014; skerratt, jennifer/N-4313-2019; Nichols, Peter/C-5128-2011; skerratt, jennifer/F-2010-2015	skerratt, jennifer/0000-0001-9023-4692				Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; [Anonymous], 1984, LIPIDS PLANTS MICROB; Bell MV, 1997, PHYTOCHEMISTRY, V45, P303, DOI 10.1016/S0031-9422(96)00867-9; Bjornland T., 1997, PHYTOPLANKTON PIGMEN, P578; BLIGH EG, 1959, CAN J BIOCHEM PHYS, V37, P911; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; DUNSTAN GA, 1992, J EXP MAR BIOL ECOL, V161, P115, DOI 10.1016/0022-0981(92)90193-E; DUNSTAN GA, 1993, J APPL PHYCOL, V5, P71, DOI 10.1007/BF02182424; GARRISON DL, 1989, POLAR BIOL, V10, P211; GILLAN FT, 1983, ADV ORG GEOCHEM, P198; GOAD LJ, 1982, LIPIDS, V17, P853, DOI 10.1007/BF02534578; HALLEGRAEFF GM, 1991, J PHYCOL, V27, P591, DOI 10.1111/j.0022-3646.1991.00591.x; HARVEY HR, 1988, PHYTOCHEMISTRY, V27, P1723, DOI 10.1016/0031-9422(88)80432-1; Harvey HR, 1997, J EUKARYOT MICROBIOL, V44, P189, DOI 10.1111/j.1550-7408.1997.tb05698.x; HARVEY HR, 1991, GEOCHIM COSMOCHIM AC, V55, P3387, DOI 10.1016/0016-7037(91)90496-R; JEFFREY SW, 1975, J PHYCOL, V11, P374, DOI 10.1111/j.0022-3646.1975.00374.x; Jeffrey SW., 1997, Phytoplankton pigments in oceanography, P343; JOHANSEN JE, 1974, PHYTOCHEMISTRY, V13, P2261, DOI 10.1016/0031-9422(74)85038-7; Leblond JD, 2002, J PHYCOL, V38, P670, DOI 10.1046/j.1529-8817.2002.01181.x; Mansour MP, 1999, PHYTOCHEMISTRY, V50, P541, DOI 10.1016/S0031-9422(98)00564-0; Mansour MP, 1999, J PHYCOL, V35, P710, DOI 10.1046/j.1529-8817.1999.3540710.x; Mantoura R.F.C., 1997, PHYTOPLANKTON PIGMEN, P407; MCMINN A, 1993, J PLANKTON RES, V15, P935; MEDLIN LK, 1994, PHYCOLOGIA, V33, P199, DOI 10.2216/i0031-8884-33-3-199.1; Millie D.F., 1993, Curr. 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Res, V1, P1; Montresor M, 2003, POLAR BIOL, V26, P186, DOI 10.1007/s00300-002-0473-9; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; NAPOLITANO GE, 1988, PHYTOCHEMISTRY, V27, P1751, DOI 10.1016/0031-9422(88)80437-0; NICHOLS DS, 1993, ANTARCT SCI, V5, P271, DOI 10.1017/S0954102093000367; NICHOLS PD, 1984, PHYTOCHEMISTRY, V23, P1043, DOI 10.1016/S0031-9422(00)82605-9; NICHOLS PD, 1991, PHYTOCHEMISTRY, V30, P3209, DOI 10.1016/0031-9422(91)83177-M; Piretti MV, 1997, J PHYCOL, V33, P61, DOI 10.1111/j.0022-3646.1997.00061.x; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Stoecker DK, 1997, J PHYCOL, V33, P585, DOI 10.1111/j.0022-3646.1997.00585.x; STOECKER DK, 1992, MAR ECOL PROG SER, V84, P265, DOI 10.3354/meps084265; Stoecker DK, 1998, J PHYCOL, V34, P60, DOI 10.1046/j.1529-8817.1998.340060.x; VOLKMAN J K, 1991, Journal of Planar Chromatography - Modern TLC, V4, P19; Volkman JK, 1998, ORG GEOCHEM, V29, P1163, DOI 10.1016/S0146-6380(98)00062-X; VOLKMAN JK, 1989, J EXP MAR BIOL ECOL, V128, P219, DOI 10.1016/0022-0981(89)90029-4; Wakeham SG, 1995, DEEP-SEA RES PT I, V42, P1749, DOI 10.1016/0967-0637(95)00074-G; WAKEHAM SG, 1991, DEEP-SEA RES, V38, P5943; Walsh D, 1998, BIOCHEM SYST ECOL, V26, P495, DOI 10.1016/S0305-1978(98)00006-4; WITHERS N, 1987, BIOL DINOFLAGELLATES, P316; Wright SW, 1996, MAR ECOL PROG SER, V144, P285, DOI 10.3354/meps144285; Zapata M, 2000, MAR ECOL PROG SER, V195, P29, DOI 10.3354/meps195029	47	44	48	1	29	BLACKWELL PUBLISHING INC	MALDEN	350 MAIN ST, MALDEN, MA 02148 USA	0022-3646			J PHYCOL	J. Phycol.	OCT	2004	40	5					867	873		10.1111/j.1529-8817.2004.03169.x	http://dx.doi.org/10.1111/j.1529-8817.2004.03169.x			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	858GA					2025-03-11	WOS:000224179100009
J	Gu, HF; Lan, DZ; Fang, Q; Wang, ZL				Gu, HF; Lan, DZ; Fang, Q; Wang, ZL			Cyst formation, development of <i>Alexandrium tamarense</i> from Yangtse River Estuary and its relation to bloom dynamics	ACTA BOTANICA SINICA			English	Article						cyst; Alexandrium tamarense; Yangtse River estuary; bloom	GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; BENTHIC CYSTS; DINOFLAGELLATE; DINOPHYCEAE; SCRIPPSIELLA; GERMINATION; REPRODUCTION; ENCYSTMENT; SEDIMENTS	The toxic dinoflagellate - Alexandrium tamarense (Lebour) Balech, formed resting cysts in f/2 media with low nitrate concentrations. Among the concentrations tested, f/20 NO3- was the most effective to induction with an encystment percentage of 2.0 in batch culture. About 73.2% and 17.6% of cysts were produced on 8 and 9 d after transferring. Newly formed cysts developed accumulation body 3 d later and kept forming mucilaginous substance, which might help their dispersal and survival. The mandatory dormancy period of resting cysts was 15 and 10 d when stored at 15 and 20 degreesC respectively. The cysts could germinate without temperature change, with germination of 75.6% 20 d after formation at 20 degreesC. The Alexandrium cyst density in the surface sediment of DG-26 station reached above 25 cysts/g in May and November of 2002, and dropped to 4.5 and 0.9 cysts/g in August of 2002 and February of 2003, suggesting that Alexandrium cysts might have germinated in spring and autumn 2002. Cysts produced during the bloom returned to water column soon, whatever the season and water temperature were. The cyst density in the surface sediment at DG-26 station in May, 2003 was only 3.3 cysts/g and the cysts were newly formed. In the Yangtse River estuary, the inoculum size was not a major factor to determine the outbreak of A. tamarense bloom.	State Ocean Adm, Inst Oceanog 3, Xiamen 631005, Peoples R China; Ocean Univ Qingdao, Qingdao 266003, Peoples R China; State Ocean Adm, Inst Oceanog 1, Qingdao 266011, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Ocean University of China; First Institute of Oceanography, Ministry of Natural Resources	State Ocean Adm, Inst Oceanog 3, Xiamen 631005, Peoples R China.	haifenggu@yahoo.com	Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171				ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Blanco Juan, 1995, P563; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; GU HF, 2003, CHIN J APPL ECOL, V14, P1081; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Jin X.L., 1992, MARINE GEOLOGY E CHI; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; LI RX, 1995, P 2 M CHIN COMM SCOR, P36; MOREYGAINES G, 1980, PHYCOLOGIA, V19, P230, DOI 10.2216/i0031-8884-19-3-230.1; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; Wang J. H., 2003, Chin. J. Appl. Ecol, V14, P1065; WANG WF, 1994, MARINE SCI B, V13, P53; WANG ZH, 2003, CHINESE J APPL ECOLO, V14, P1039; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; ZINGMARK RG, 1970, J PHYCOL, V6, P122, DOI 10.1111/j.0022-3646.1970.00122.x	26	3	6	0	9	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	0577-7496	1672-9072		ACTA BOT SIN	Acta Bot. Sin.	SEP	2004	46	9					1025	1031						7	Biochemistry & Molecular Biology; Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Plant Sciences	856GX					2025-03-11	WOS:000224034800003
J	Marret, F; Scourse, J; Austin, W				Marret, F; Scourse, J; Austin, W			Holocene shelf-sea seasonal stratification dynamics: a dinoflagellate cyst record from the Celtic Sea, NW European shelf	HOLOCENE			English	Article						dinocysts; shelf sea; Holocene; seasonal stratification; Celtic Sea; NW European shelf	SURFACE SEDIMENTS; NORTH-ATLANTIC; BENTHIC FORAMINIFERA; CLIMATE; OCEAN; PHYTOPLANKTON; DISTRIBUTIONS; EVOLUTION; REGIMES; FRONTS	Published records of the Holocene evolution of seasonal strati. cation in the Celtic Sea (NW European shelf) have been based on benthic proxies, notably benthic foraminifera and associated stable isotopic data. We have investigated organic-walled dinoflagellate cyst assemblages from a well-dated Holocene sequence from the central Celtic Sea in order to assess the signal from this planktonic proxy and to reconstruct paired bottom- and surface-water conditions through time. This sequence has, on the basis of the benthic proxies, been interpreted previously as a record of the replacement of tidally mixed water by stratified water associated with tidal-front migration during the early Holocene. Interpretation of the dinocyst record has been facilitated by a parallel study of the distribution of cysts from Celtic Sea surface sediments and their relationship with seasonal water masses. The dinocyst stratigraphy indicates mixed-water conditions during the early Holocene consistent with reduced water depths (hence lowered sea level) over the core site. The first significant change in the dinocyst assemblages is recorded at around 6650 cal. years BP and indicates a transition from mixed-frontal conditions to seasonal strati. cation. This interpretation of frontal migration is consistent with changes in the benthic foraminiferal assemblages and associated stable isotopes at the same core depth. From 6650 to 3600 cal. years BP, the significant occurrence of Bitectatodinium tepikiense accompanied by Spiniferites elongatus is attributed to strong seasonality, with winter sea-surface temperatures possibly below 5degreesC. Another transition at 3600 cal. years BP is attributed to a reduction in seasonality generated by milder winter conditions linked to a stronger influence of the thermohaline circulation over the studied area. This transition is not recorded by the benthic proxies and is attributed to climate forcing rather than to any change in tidal dynamics. It is notable that many mires in western Britain record distinct wet shifts contemporary with this change.	Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales; Univ St Andrews, Sch Geog & Geosci, St Andrews KY16 9AL, Fife, Scotland	Bangor University; University of St Andrews	Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales.	f.marret@bangor.ac.uk		Marret-Davies, Fabienne/0000-0003-4244-0437				AUSTIN RM, 1991, TERRA NOVA, V3, P276, DOI 10.1111/j.1365-3121.1991.tb00145.x; Austin WEN, 1997, J GEOL SOC LONDON, V154, P249, DOI 10.1144/gsjgs.154.2.0249; Barber K. 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J. R., 1987, BOT MONOGR, V21; TETT P, 1986, ESTUAR COAST SHELF S, V23, P641, DOI 10.1016/0272-7714(86)90104-6; VanGeel B, 1996, J QUATERNARY SCI, V11, P451, DOI 10.1002/(SICI)1099-1417(199611/12)11:6<451::AID-JQS275>3.0.CO;2-9; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALSH JJ, 1981, NATURE, V291, P196, DOI 10.1038/291196a0; WOLLAST R, 1991, PHYS CH EAR, P365; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	48	20	21	0	10	SAGE PUBLICATIONS LTD	LONDON	1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND	0959-6836	1477-0911		HOLOCENE	Holocene	SEP	2004	14	5					689	696		10.1191/0959683604hl747rp	http://dx.doi.org/10.1191/0959683604hl747rp			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	850UI					2025-03-11	WOS:000223638700005
J	Vandenberghe, N; Van Simaeys, S; Steurbaut, E; Jagt, JWM; Felder, PJ				Vandenberghe, N; Van Simaeys, S; Steurbaut, E; Jagt, JWM; Felder, PJ			Stratigraphic architecture of the Upper Cretaceous and Cenozoic along the southern border of the North Sea Basin in Belgium	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article; Proceedings Paper	Symposium on the Paleogene Preparing for Modern Life and Climate	AUG 25-30, 2003	Leuven, BELGIUM	Int Subcommiss Paleogene Stratig		sequence stratigraphy; North Sea Basin; Late Cretaceous; Cenozoic	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; BOOM CLAY FORMATION; SEQUENCE STRATIGRAPHY; AREA; BOUNDARY; DENUDATION; MIOCENE	The Late Cretaceous and Cenozoic sedimentary record in the Campine Basin along the southern border of the North Sea Basin is analysed in terms of sequence stratigraphy. All available biostratigraphic, and in some cases, magnetostratigraphic data are used to constrain the sequence chronostratigraphy. The relative geographic extent of the strata is used as an indication of the relative sea level. Tectonic and eustatic components could be distinguished in several cases using regional geological information. Generally, sequences consist of transgressive and highstand systems tracts only and have flat, abrasion-type lower boundaries. Lowstand deposits are only identified as infill of erosional space, which generally implies marked tectonic uplift. Several eustatic and tectonic events can be correlated with similar events known elsewhere in the North Sea Basin. The time intervals spanned by the different sequences vary considerably, pointing out different control mechanisms.	Hist Geol, Redingenstr 16, B-3000 Louvain, Belgium; Inst Royal Sci Nat Belgique, B-1000 Brussels, Belgium; Nat Hist Museum Maastricht, NL-6211 KJ Maastricht, Netherlands		Hist Geol, Redingenstr 16, B-3000 Louvain, Belgium.	vandenberghe@geo.kuleuven.ac.be						Abreu V.S., 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, V60, P245; ALBERS HJ, 1979, ASPEKTE KREIDE EUROP, P47; ALI JR, 1993, GEOLOGICAL SOC LONDO, V70, P99; Andersen MS, 2002, GEOL SOC SPEC PUBL, V196, P291, DOI 10.1144/GSL.SP.2002.196.01.16; [Anonymous], 1996, GEOLOGICAL SOC LONDO, DOI DOI 10.1144/GSL.SP.1996.101.01.02; BAL SG, 1990, TOELICHTENDE VERHAND, V29, P63; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P101; Christensen WK, 1997, ACTA PALAEONTOL POL, V42, P457; Dahalane Zalihata, 2003, Guide Economique de Comores; De Batist M, 1998, GEOL MIJNBOUW, V77, P17, DOI 10.1023/A:1003446611678; De Coninck J., 1996, B SOC BELG GEOL, V104, P151; DEBATIST M, 1995, J GEOL SOC LONDON, V152, P27, DOI 10.1144/gsjgs.152.1.0027; DEBATIST M, 1989, THESIS RU GENT; DEBATIST M, 1989, QUATERNARY TERTIARY, P75; DECONINCK J, 1977, NATUURWETENSCHAPPELI, V57, P224; DEMYTTENAERE R, 1989, KLASSE WETENSCHAPPEN, V51, P51; DUPUIS C, 1984, CR ACAD SCI II, V298, P53; DUPUIS C, 1987, ANN SOC GEOL NORD, V105, P233; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; ERNST G, 1994, SEQUENCE STRATIGRAPH, P128; FELDER PJ, 1985, 214 GEOL DIENST BELG; FELDER WM, 2001, GEOLOGIE NEDERLAND; Grimm K.I., 2001, Aardkundige Mededelingen, V11, P9; Gullentops F., 1963, ETUDE DIVERS FACIES; Hager H, 1998, B GEOL SOC DENMARK, V45, P53; HARDENBOL J, 2003, S PAL LEUV AUG 25 30; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; HENRIET JP, 1989, QUATERNARY TERTIARY, P29; Herman J., 2000, Geologica Belgica, V3, P231, DOI 10.20341/gb.2014.031; Herngreen G.F.W., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V61, P1; Houthuys R., 1990, AARDKD MEDED, V5, P1; Huuse M, 2002, GEOL SOC SPEC PUBL, V196, P209, DOI 10.1144/GSL.SP.2002.196.01.13; Jagt John W. 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J. Geosci.	SEP	2004	83	3					155	171		10.1017/S0016774600020229	http://dx.doi.org/10.1017/S0016774600020229			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology	887TN		Green Published			2025-03-11	WOS:000226328500002
J	Van Simaeys, S				Van Simaeys, S			The Rupelian-Chattian boundary in the North Sea Basin and its calibration to the international time-scale	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article; Proceedings Paper	Symposium on the Paleogene Preparing for Modern Life and Climate	AUG 25-30, 2003	Leuven, BELGIUM	Int Subcommiss Paleogene Stratig		biochronostratigraphy; dinoflagellate cysts; North Sea Basin; Rupelian-Chattian boundary; Tethyan Ocean	DINOFLAGELLATE CYSTS; EOCENE; BIOSTRATIGRAPHY; STRATOTYPE; TRANSITION; REGION	The classical problem of the nature and age of the Rupelian-Chattian (Early-Late Oligocene) unconformity in its type region is here approached using organic walled dinoflagellate cyst (dinocyst) correlations between the North Sea Basin and well-calibrated central Italian (Tethyan Ocean) sections. Useful Oligocene dinocyst events are the last occurrence of Enneadocysta pectiniformis (similar to29.3 Ma), and the first occurrences of Saturnodinium pansum (similar to29.4 Ma), Distatodinium biffii (similar to27.9 Ma) and Artemisiocysta cladodichotoma (similar to26.7 Ma). The latter event marks the earliest Chattian. The improved correlations indicate that the Rupelian-Chattian (R-C) boundary is associated with the so-called 'Oligocene Glacial Maximum'. This phase of important global cooling and glacio-eustatic sea level fall is genetically related to the unconformity between the classic Oligocene stages. Subsequent global warming (so-called 'Late Oligocene Warming Event'), induced a major sea level rise, leading e.g. to the time-transgressive deposition of the typical basal Chattian glauconitic sands. The oldest of the Chattian units have a GPTS age of similar to26.7 Ma. It further appears that a hiatus of similar to500 kyrs spans the classic Rupelian-Chattian unconformity.	Univ Louvain, B-3000 Louvain, Belgium		Van Simaeys, S (通讯作者)，Univ Louvain, Redingenstr 16, B-3000 Louvain, Belgium.	stefaan.vansimaeys@geo.kuleuven.ac.be						Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; Brinkhuis H., 1995, SOC ECON PALEONT MIN, V54, P295; COCCIONI R, UNPUB B GEOLOGICAL S; De Man E, 2004, NETH J GEOSCI, V83, P227, DOI 10.1017/S0016774600020291; De Man Ellen, 2004, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V74, P177; DOPPERT JWC, 1983, MEDEDELINGEN RIJKS G, V37, P4; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Ellermann C., 1958, Fortschritte in der Geologie von Rheinland und Westfalen, V1-2, P205; Indans J., 1965, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V123, P20; Indans J., 1958, Fortschritte in der Geologie von Rheinland und Westfalen, V1-2, P223; King C., 1989, P418; KING C, 1983, REPORT I GEOLOGICAL, V82, P1; Miller KG, 1998, REV GEOPHYS, V36, P569, DOI 10.1029/98RG01624; MILLER KG, 1991, J GEOPHYS RES-SOLID, V96, P6829, DOI 10.1029/90JB02015; Odin G. S., 1988, EOCENE OLIGOCENE BOU, P253; ODIN GS, 1989, CR ACAD SCI II, V309, P1939; Ruffer T., 1998, Society for Sedimentary Geology Special Publication, V60, P751, DOI [10.2110/ pec.98.02.0119, DOI 10.2110/PEC.98.02.0119]; Salvador A., 1994, Geological Society of America, P1; Scotese C. R., 1992, 200692 PALEOMAP U TE; Sissingh W, 2003, PALAEOGEOGR PALAEOCL, V196, P229, DOI 10.1016/S0031-0182(03)00320-1; Steininger FF, 1997, EPISODES, V20, P23; ULLEBERG K, 1987, Bulletin of the Geological Society of Denmark, V36, P191; Van Simaeys S, 2004, PALAEOGEOGR PALAEOCL, V208, P31, DOI 10.1016/j.palaeo.2004.02.029; Vandenberghe N., 2001, AARDKUNDIGE MEDEDELI, V11, P69; VANSIMAEYS S, IN PRESS OLIGOCENE D; VANSIMAEYS S, UNPUB GEOLOGY; VANSIMAEYS S, IN PRESS REV PALEOBO; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zevenboom D., 1995, PhD Thesis Diss; Ziegler P.A., 1990, GEOLOGICAL ATLAS W C	36	26	28	0	3	VEENMAN DRUKKERS	EDE	P O BOX 18, 6710 BA EDE, NETHERLANDS	0016-7746			NETH J GEOSCI	Neth. J. Geosci.	SEP	2004	83	3					241	248		10.1017/S0016774600020308	http://dx.doi.org/10.1017/S0016774600020308			8	Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Geology	887TN		Bronze			2025-03-11	WOS:000226328500010
J	Dybkjær, K				Dybkjær, K			Dinocyst stratigraphy and palynofacies studies used for refining a sequence stratigraphic model -: uppermost Oligocene to lower Miocene, Jylland, Denmark	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Denmark; upper Oligocene-lower Miocene; biostratigraphy; palynology; palynofacies; dinoflagellate cysts; sequence stratigraphy	NORTH-SEA BASIN; DINOFLAGELLATE CYSTS; INTEGRATED STRATIGRAPHY; BIOSTRATIGRAPHY; SUCCESSIONS; MINERALOGY; DEPOSITS; SECTION; MARGIN; MIDDLE	The uppermost Oligocene-Miocene deposits in the central and southern parts of Jylland, Denmark, comprise a complex succession of siliciclastic, paralic deposits. The coarse-grained parts of the succession comprise important groundwater reservoirs. A sequence stratigraphic model has gradually been developed during the last 7 years and the succession is now subdivided into six sequences (sequence A-F). The model is based on a combination of seismic data, geophysical logs and lithological data from boreholes and sedimentological measurements of outcrops. The present study documents the composition of assemblages of organic-walled dinoflagellates (dinocysts) in the lower part of the succession (sequences A-C). The data come from seven water supply boreholes and one outcrop section. The dinocyst data are an important tool for pointing out the sequence stratigraphic surfaces in the individual boreholes, showing distinct changes at the sequence boundaries and increased relative abundance and diversity of dinocysts at marine flooding surfaces. The dinocysts are also used for correlating between the studied boreholes and outcrops, for interpreting changes in the depositional environment and for dating the sequences in more detail than earlier datings based on molluscs and foraminifers. The datings allow correlation to eustatic sea-level curves. The good match between the sequence development and climatic changes suggests that eustatic sea-level changes were the main factor in sequence formation and changes in the depositional environment. (C) 2004 Elsevier B.V. All rights reserved.	Geol Survey Denmark & Greenland, GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018					[Anonymous], 827 I GEOL SCI; [Anonymous], 1988, Geol. 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Palaeobot. Palynology	SEP	2004	131	3-4					201	249		10.1016/j.revpalbo.2004.03.006	http://dx.doi.org/10.1016/j.revpalbo.2004.03.006			49	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	849VL					2025-03-11	WOS:000223569200004
J	Gárate-Lizárraga, I; López-Cortes, DJ; Bustillos-Guzmán, J; Hernández-Sandoval, F				Gárate-Lizárraga, I; López-Cortes, DJ; Bustillos-Guzmán, J; Hernández-Sandoval, F			Blooms of <i>Cochlodinium polykrikoides</i> (Gymnodiniaceae) in the Gulf of California, Mexico	REVISTA DE BIOLOGIA TROPICAL			English	Article						Cochlodinium polykrikoides; blooms; caged fish mortality; Bahia de la Paz; Gulf of California	RED TIDE DINOFLAGELLATE; DINOPHYCEAE; PHYTOPLANKTON; SHELLFISH; MORTALITY; WATERS	Cochlodinium polykrikoides was the species responsible for the discoloration that occurred between September 15(th) and 27(th), 2000 in a shallow coastal lagoon located in the southern part of the Bahia de La Paz, on the west side of the Gulf of California. Blooms of C. polykrikoides were observed four days after two rainy days with a seawater temperature of 29 to 31degreesC. Nutrient concentration ranges during the bloom were 0.165-0.897 muM NO2+NO3, 0.16-3.25 muM PO4, and 1.0-35.36 muM SiO4. Abundance of C. polykrikoides ranged from 360 x 103 to 7.05 x 10(6)/cells l(-1). Biomass expressed in terms of chlorophyll a was high, ranging from 2.7 to 56.8 mg/m(3). A typical dinoflagellate pigment profile (chlorophyll a and c, peridinin, diadinoxantin, and beta-carotene) was recorded. In this study, the red tide occurred in front of several fish and shrimp-culture ponds. No PST toxins were found in the samples. However, 180 fish were found dead in the infected fish-pond; the gills were the most affected part. C. polykrikoides is a cyst-forming species that recurs in this area. New blooms were observed in November 2000 and September-November 2001 in the same area. Anthropogenic activities, such as cutrophication caused by water discharge in this shallow lagoon, and nutrient enrichment in the culture ponds, as well as effects from precipitation and wind stress, could have favored the outbreak of this dinoflagellate.	IPN, CICIMAR, Dept Plancton & Ecol Marina, La Paz 23000, Baja Calif Sur, Mexico; Ctr Invest Biol Noroeste, La Paz 23000, Baja Calif Sur, Mexico	Instituto Politecnico Nacional - Mexico; Telefonica SA; CIBNOR - Centro de Investigaciones Biologicas del Noroeste	IPN, CICIMAR, Dept Plancton & Ecol Marina, Apdo Postal 592, La Paz 23000, Baja Calif Sur, Mexico.	igarate@ipn.mx	Gárate-Lizárraga, Ismael/GRS-5815-2022	Garate-Lizarraga, Ismael/0000-0002-3835-183X				Alonso-Rodríguez R, 2000, MAR POLLUT BULL, V40, P331, DOI 10.1016/S0025-326X(99)00225-8; BUSTILLOSGUZMAN J, 1995, MAR ECOL PROG SER, V124, P247, DOI 10.3354/meps124247; CERVANTESDUARTE R, 2001, OCEANIDES, V16, P1; Cho ES, 2001, BOT MAR, V44, P57, DOI 10.1515/BOT.2001.008; Cortes-Altamirano R, 1997, CIENC MAR, V15, P31; Cortes-Altamirano R., 2002, ATLAS BIODIVERSIDAD, P29; Figueroa-Torres M. 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Biol. Trop.	SEP	2004	52			1			51	58						8	Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics	859VT	17465117				2025-03-11	WOS:000224296700006
J	Kremp, A; Anderson, DM				Kremp, A; Anderson, DM			Lectin binding patterns of <i>Scrippsiella lachrymosa</i> (Dinophyceae) in relation to cyst formation and nutrient conditions	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						dinoflagellates; gametes; glycoconjugates; lectins; nutrient status; Scrippsiella lachrymosa; sexual reproduction	DISSOLVED ORGANIC NITROGEN; GAMETE RECOGNITION; POPULATION-DYNAMICS; CONCANAVALIN-A; LIFE-CYCLE; DINOFLAGELLATE; ENCYSTMENT; PHYTOPLANKTON; GLYCOPROTEINS; TUNICAMYCIN	In many dinoflagellates, it has been a challenging task to study the qualitative and quantitative processes leading to encystment because gametes are often not morphologically distinguishable from other vegetative cells. We examined whether sexual differentiation is accompanied by changes in cell surface glycoprotein properties that are reflected in the binding patterns of complementary lectins. Labeling percentages of nine different fluorescein isothiocyanate (FITC)-conjugated lectins were analyzed together with cell and cyst abundance in N-deplete and f/2 control cultures of Scrippsiella lachrymosa Lewis throughout an encystment experiment. Although labeling varied between lectins and treatments and considerable changes occurred through time, no direct correlation was observed between glycoconjugate proper-ties and sexual life cycle processes. A conspicuous decrease in labeling of lectins that are complementary to amino sugars (in particular, with WGA, a lectin that is complementary to N-acetylglucosamine) was observed in the low nitrogen treatment, suggesting a link between the nutrient status of a cell and expression of surface carbohydrates. Presumably, the reduction of N-acetylglucosamine residues was an early indication of N stress in cell populations. Labeling experiments with phosphate-limited cells showed that the decrease in WGA-complementary amino-sugar residues was not specific for N stress, but appeared to be a general response to nutrient limitation. Our findings confirm that glycoconjugate composition of dinoflagellate cells can change depending on their physiological state, which has to be considered when applying lectins for taxonomic differentiation of dinoflagellate species. (C) 2004 Elsevier B.V. All rights reserved.	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Exp. Mar. Biol. Ecol.	AUG 30	2004	307	2					165	181		10.1016/j.jembe.2004.02.004	http://dx.doi.org/10.1016/j.jembe.2004.02.004			17	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	840PY					2025-03-11	WOS:000222872700002
J	Fistarol, GO; Legrand, C; Rengefors, K; Granéli, E				Fistarol, GO; Legrand, C; Rengefors, K; Granéli, E			Temporary cyst formation in phytoplankton:: a response to allelopathic competitors?	ENVIRONMENTAL MICROBIOLOGY			English	Article							PRYMNESIUM-PARVUM; IN-SITU; DINOFLAGELLATE; POPULATION; MECHANISMS; PLANKTON	Competition among phytoplankton for limiting resources may involve direct or indirect interactions. A direct interaction of competitors is the release of chemicals that inhibit other species, a process known as allelopathy. Here, we investigated the allelopathic effect of three toxic microalgae species (Alexandrium tamarense, Karenia mikimotoi and Chrysochromulina polylepis) on a natural population of the dinoflagellate Scrippsiella trochoidea. Our major findings were that in addition to causing death of S. trochoidea cells, the allelopathic species also induced the formation of temporary cysts in S. trochoidea. Because cysts were not lysed, encystment may act as a defence mechanism for S. trochoidea to resist allelochemicals, especially when the allelopathic effect is moderate. By forming temporary cysts, S. trochoidea may be able to overcome the effect of allelochemicals, and thereby have an adaptive advantage over other organisms unable to do so.	Univ Kalmar, Div Marine Sci, Dept Biol & Environm Sci, S-39231 Kalmar, Sweden; Lund Univ, Dept Ecol, S-22362 Lund, Sweden	University of Kalmar; Linnaeus University; Lund University	Univ Kalmar, Div Marine Sci, Dept Biol & Environm Sci, S-39231 Kalmar, Sweden.	giovana.salomon@hik.se	Rengefors, Karin/K-5873-2019; Graneli, Edna/F-5936-2015	Rengefors, Karin/0000-0001-6297-9734				ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1985, J PHYCOL, V21, P200; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Arzul G, 1999, J EXP MAR BIOL ECOL, V232, P285, DOI 10.1016/S0022-0981(98)00120-8; Balzer I, 1996, BRAZ J MED BIOL RES, V29, P95; CHUAYCHAN S, 1998, THESIS NORWEGIAN U S; Dale B., 1983, P69; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fistarol GO, 2003, MAR ECOL PROG SER, V255, P115, DOI 10.3354/meps255115; FISTAROL GO, 2004, IN PRESS AQUAT MICRO, V35; Fryxell G.A., 1983, Survival Strategies of the algae, P1; Gisselson LÅ, 2001, LIMNOL OCEANOGR, V46, P1237, DOI 10.4319/lo.2001.46.5.1237; Gisselson LÅ, 1999, MAR ECOL PROG SER, V184, P55, DOI 10.3354/meps184055; Granéli E, 2003, HARMFUL ALGAE, V2, P135, DOI 10.1016/S1568-9883(03)00006-4; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; Hairston NG, 2001, EVOLUTION, V55, P2203, DOI 10.1111/j.0014-3820.2001.tb00736.x; Hansson LA, 1996, P ROY SOC B-BIOL SCI, V263, P1241, DOI 10.1098/rspb.1996.0182; Harvell CD, 1998, ECOLOGY AND EVOLUTION OF INDUCIBLE DEFENSES, P3; KEATING KI, 1977, SCIENCE, V196, P885, DOI 10.1126/science.196.4292.885; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Lampert W., 1997, Limnoecology: The ecology of lakes and streams; Legrand C, 2003, PHYCOLOGIA, V42, P406, DOI 10.2216/i0031-8884-42-4-406.1; LEWIS WM, 1986, AM NAT, V127, P184, DOI 10.1086/284477; LIRDWITAYAPRASIT T, 1990, TOXIC MARINE PHYTOPLANKTON, P294; LUCAS CE, 1947, BIOL REV, V22, P270, DOI 10.1111/j.1469-185X.1947.tb00335.x; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; PRATT DM, 1966, LIMNOL OCEANOGR, V11, P447, DOI 10.4319/lo.1966.11.4.0447; Rengefors K, 2003, LIMNOL OCEANOGR, V48, P1167, DOI 10.4319/lo.2003.48.3.1167; Rengefors K, 2001, LIMNOL OCEANOGR, V46, P1990, DOI 10.4319/lo.2001.46.8.1990; RENGEFORS K, 1998, P ROY SOC LOND B BIO, V265, P1; Rice E.L, 1984, ALLELOPATHY, P292; Seigler DS, 1996, AGRON J, V88, P876, DOI 10.2134/agronj1996.00021962003600060006x; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P1; Uchida T, 1999, J EXP MAR BIOL ECOL, V241, P285, DOI 10.1016/S0022-0981(99)00088-X; Uchida T., 1996, HARMFUL TOXIC ALGAL, P369; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Van Donk E, 1998, ECOLOGY AND EVOLUTION OF INDUCIBLE DEFENSES, P89; Vardi A, 2002, CURR BIOL, V12, P1767, DOI 10.1016/S0960-9822(02)01217-4; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wolfe GV, 2000, BIOL BULL-US, V198, P225, DOI 10.2307/1542526	43	72	88	0	45	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1462-2912	1462-2920		ENVIRON MICROBIOL	Environ. Microbiol.	AUG	2004	6	8					791	798		10.1111/j.1462-2920.2004.00609.x	http://dx.doi.org/10.1111/j.1462-2920.2004.00609.x			8	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	836TL	15250881	Green Published			2025-03-11	WOS:000222578600004
J	Parrow, MW; Burkholder, JM				Parrow, MW; Burkholder, JM			The sexual life cycles of <i>Pfiesteria piscicida</i> and cryptoperidiniopsoids (Dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						chromosomes; dinoflagellate; gametes; meiosis; nuclear cyclosis; planozygote; sexual reproduction	TOXIC DINOFLAGELLATE; MEIOTIC PROPHASE; FISSION YEAST; COMPLEX; REPRODUCTION; MEIOSIS; CULTURE; MORPHOLOGY; MOVEMENT; NOV	Sexual life cycle events in Pfiesteria piscicida and cryptoperidiniopsoid heterotrophic dinoflagellates were determined by following the development of isolated gamete pairs in single-drop microcultures with cryptophyte prey. Under these conditions, the observed sequence of zygote formation, development, and postzygotic divisions was similar in these dinoflagellates. Fusion of motile gamete pairs each produced a rapidly swimming uninucleate planozygote with two longitudinal flagella. Planozygotes enlarged as they fed repeatedly on cryptophytes. In < 12 h in most cases, each planozygote formed a transparent-walled nonmotile cell (cyst) with a single nucleus. Zygotic cysts did not exhibit dormancy under these conditions. In each taxon, dramatic swirling chromosome movements (nuclear cyclosis) were found in zygote nuclei before division. In P piscicida, nuclear cyclosis occurred in the zygotic cyst or apparently earlier in the planozygote. In the cryptoperidiniopsoids, nuclear cyclosis occurred in the zygotic cyst. After nuclear cyclosis, a single cell division occurred in P piscicida and cryptoperidiniopsoid zygotic cysts, producing two offspring that emerged as biflagellated cells. These two flagellated cells typically swam for hours and fed on cryptophytes before encysting. A single cell division in these cysts produced two biflagellated offspring that also fed before encysting for further reproduction. This sequence of zygote development and postzygotic divisions typically was completed within 24 h and was confirmed in examples from different isolates of each taxon. Some aspects of the P piscicida sexual life cycle determined here differed from previous reports.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA	North Carolina State University	N Carolina State Univ, Ctr Appl Aquat Ecol, 620 Hutton St,Suite 104, Raleigh, NC 27606 USA.	mwparrow@unity.ncsu.edu	Parrow, Matthew/HMO-6676-2023	Parrow, Matthew/0000-0002-3197-2510				BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C. A., 1980, BIOCH PHYSL PROTOZOA, V3, P171; BHAUD Y, 1988, J CELL SCI, V89, P197; Biecheler B., 1952, Bull. Biol. Fr. 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Phycol.	AUG	2004	40	4					664	673		10.1111/j.1529-8817.2004.03202.x	http://dx.doi.org/10.1111/j.1529-8817.2004.03202.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	844PK					2025-03-11	WOS:000223171900006
J	Cyprien, AL; Visset, L; Carcaud, N				Cyprien, AL; Visset, L; Carcaud, N			Evolution of vegetation landscapes during the Holocene in the central and downstream Loire basin (Western France)	VEGETATION HISTORY AND ARCHAEOBOTANY			English	Article						palynology; palaeoenvironment; Loire Valley; Holocene; marine trangression; human impact	ARMORICAN; END	Nine sites along the downstream and middle section of the Loire river at Cordemais (Loire Atlantique, France) situated in the estuary to Saint-Nicolas-de-Bourgueil (Indre et Loire, France) were investigated. Interdisciplinary studies combined palynology, geography, archaeology, sedimentology and history, thus enabling us to reconstruct the evolution and the long-term response of the Loire valley ecosystem to natural variations and anthropogenic pressure from the Preboreal to the present in an integrated manner. The Atlantic marine transgression (between 7000 and 5000 B.P.) caused the level of brackish water to increase at Oudon between 6740(+205)/(-200) and 5010(+115)/(-100) B.P. This phenomenon, which was the first of its kind to be detected near the central Loire region (approximately 80 km from the current mouth of the Loire river), was accompanied by the development of subhalophile vegetation (Chenopodiaceae) and the appearance of dinoflagellate cysts. A regressive phase occurred during the Subboreal, about 4500 B.P., and led to the erosion of most of the estuarian sediments and to the disappearance of plant species linked to salinity at Oudon: peat deposits built up at most other sites. Human activities had an early effect; moderate deforestation took place at Champtoce about 6600 B.P. as farming was already orientated towards rearing animals. However, possibly cultivated plants were present towards the middle and the end of the Neolithic period (wheat, rye, buckwheat, flax) at about 5600 B.P. and chestnut and walnut were probably exploited in the Loire valley region at about 4600 B.P. The Bronze Age seemed to mark a phase when societies settled down (planting of vineyards) and deforestation peaked from the Gallo-Roman period onwards. The textile industry (flax, hemp), in the context of crop rotation set up during the Iron Age, developed rapidly during the Middle Ages, whereas nowadays the rearing of animals is the dominant activity in the Loire Valley, following the introduction of maize into the region in 1950.	Fac Sci & Tech, Lab Ecol & Paleoenvironm Atlantiques, UMR 6566, CNRS, F-44322 Nantes 03, France; Univ Angers, Lab Sci Environm Amenagement, UFR Sci, F-49000 Angers, France	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite d'Angers	Fac Sci & Tech, Lab Ecol & Paleoenvironm Atlantiques, UMR 6566, CNRS, 2 Rue Houssiniere,BP 92208, F-44322 Nantes 03, France.	geminaecol@svt.univ-nantes.fr						[Anonymous], QUATERNAIRE; [Anonymous], 2001, QUATERNAIRE; [Anonymous], 1998, La foret, l'homme et le troupeau dans les Pyrenees: 6000 ans d'histoire de l'environnement entre Garonne et Mediterranee. 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Archeol. Ouest, V13, P79, DOI [10.3406/rao.1996.1041, DOI 10.3406/RAO.1996.1041]; VISSET L, 1980, MEMOIRE SOC ETUDES S, V4, P87; VISSET L, 1980, B SOC SCI NATURELLES, V2, P129; Visset L., 1999, Quaternaire, V10, P247; VOELTZEL D, 1987, THESIS U AIX MARSEIL	60	26	27	0	11	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	0939-6314	1617-6278		VEG HIST ARCHAEOBOT	Veg. Hist. Archaeobot.	AUG	2004	13	3					181	196		10.1007/s00334-004-0042-y	http://dx.doi.org/10.1007/s00334-004-0042-y			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	848LI					2025-03-11	WOS:000223468700003
J	Bennike, O				Bennike, O			Holocene sea-ice variations in Greenland: onshore evidence	HOLOCENE			English	Article						palaeoclimate; sea ice; driftwood; Greenland; arctic; holocene; climate optimum	LATE QUATERNARY HISTORY; CANADIAN ARCTIC ARCHIPELAGO; DRIFTWOOD; MOLLUSKS; SVALBARD; REMAINS; LAND; AGE	The oldest dated driftwood log from northern Greenland is c. 9300 cal. years old, which is about 2000 years younger than the beginning of the last deglaciation and 2000 years younger than the oldest driftwood on Svalbard. Driftwood entry to northern Greenland was rare until 7400 cal. years BP, indicating more severe summer sea-ice conditions than at present. More open water than at present probably characterized the period between 6800 and 5500 cal. years BP, during which time driftwood stranded on the beaches of Nioghalvfjerdsfjorden that is now covered by a floating glacier. In central East Greenland, the occurrence of the extralimital species Mytilus edulis in the time interval from c. 8500 to 6000 cal. years BP indicates more open water than at present, and in northwest Greenland studies of dinoflagellate cysts in a marine core indicate warmer surface waters, and hence less sea ice than at present from 7300 to 3700 cal. years BP.	Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	obe@geus.dk	Bennike, Ole/G-7070-2018	Bennike, Ole/0000-0002-5486-9946				Alley R., 1995, ANN GLACIOL, V21, P64, DOI DOI 10.1017/S0260305500015615; ANDREWS JT, 1981, QUATERNARY PALEOCLIM, P13; [Anonymous], 1945, MEDDR GRONLAND; [Anonymous], 1977, Rapp. Gronlands Geol. 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J	De Schepper, S; Head, MJ; Louwye, S				De Schepper, S; Head, MJ; Louwye, S			New dinoflagellate cyst and incertae sedis taxa from the Pliocene of Northern Belgium, Southern North Sea Basin	JOURNAL OF PALEONTOLOGY			English	Article							DIEST FORMATION; ACRITARCHS; GENERA; MORPHOLOGY; SECTION	New dinoflagellate cyst taxa have been recovered from Pliocene deposits in the Antwerp area of Belgium, where a detailed analysis of the Kattendijk and Lillo formations has yielded a diverse dinoflagellate record for the southern margin of the North Sea Basin. Four new species and two new genera of dinoflagellate cysts are recognized: the gonyaulacaceans Spiniferites coniconcavus n. sp. and Pyxidinopsis braboi n. sp., the goniodomacean Desotodinium wrennii n. gen. and sp., and the protoperidiniacean Scaldecysta doelensis n. gen. and sp. The protoperidiniacean genus Barssidinium Lentin, Fensome, and Williams, 1994 has been emended from new observations on the tabulation of Barssidinium pliocenicum (Head, 1993) Head, 1994a emend. The excellent preservation of the Belgian material accounts for these new observations. Barssidinium wrennii Lentin, Fensome, and Williams, 1994 is considered a taxonomic junior synonym of Barssidinium pliocenicum (Head, 1993) Head, 1994a, which thus becomes the correct name for the type of the genus. The new marine incertae sedis palynomorph Waaslandia geminifera n. gen. and sp. is also proposed.	Univ Cambridge, Godwin Inst Quarternary Res, Dept Geog, Cambridge CB2 3EN, England; Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium	University of Cambridge; Ghent University	Univ Cambridge, Godwin Inst Quarternary Res, Dept Geog, Downing Pl, Cambridge CB2 3EN, England.	smad2@cam.ac.uk; mh300@cam.ac.uk; stephen.louwye@rug.ac.be	Louwye, Stephen/D-3856-2012; De Schepper, Stijn/A-2836-2011	Louwye, Stephen/0000-0003-4814-4313; De Schepper, Stijn/0000-0002-6934-0914				[Anonymous], 1894, SYSTEMATISCHE PHYLOG, DOI DOI 10.3931/E-RARA-72554-XVI,[1]-400; Balech E., 1988, Publ. Espec. Inst. Esp. 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R., 1883, ORGANISMUS INFUSIONS; WALL D, 1971, J PHYCOL, V7, P221, DOI 10.1111/j.1529-8817.1971.tb01507.x; WALL D., 1967, PALAEONTOLOGY, V10, P95; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; Wilson G.J., 1988, NZ GEOLOGICAL SURVEY, V57; WRENN JH, 1986, 1 S NEOG DIN CRYST B, V17, P169; Zevenboom D., 1995, THESIS U UTRECHT DEN	68	43	44	0	11	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0022-3360	1937-2337		J PALEONTOL	J. Paleontol.	JUL	2004	78	4					625	644		10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2	http://dx.doi.org/10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	836UF					2025-03-11	WOS:000222580600002
J	Mattioli, E; Pittet, B; Palliani, RB; Röhl, HJ; Schmid-Röhl, A; Morettini, E				Mattioli, E; Pittet, B; Palliani, RB; Röhl, HJ; Schmid-Röhl, A; Morettini, E			Phytoplankton evidence for the timing and correlation of palaeoceanographical changes during the early Toarcian oceanic anoxic event (Early Jurassic)	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article; Proceedings Paper	Conference on Organic-Carbon Burial, Climate Change and Ocean Chemistry (Mesozoic-Palaeogene)	DEC 09-11, 2002	London, ENGLAND			early Toarcian; anoxic event; nannoplankton; microplankton; calcification	GEOCHEMICAL EVIDENCE; MASS EXTINCTIONS; ATMOSPHERIC CO2; KIMMERIDGE CLAY; GAS-HYDRATE; SEA-LEVEL; ENGLAND; BASIN; PALEOCEANOGRAPHY; DISSOCIATION	The causes and duration of the early Toarcian anoxic event are controversial. Integration of data from calcareous and organic phytoplankton provides a biochronological framework that allows precise correlations across the western Tethys. In particular, the Carinolithus superbus nannofossil Zone can be used to correlate the levels enriched in organic matter and the related delta(13)C negative excursion. Although a variable duration is given in the literature for this negative excursion, it is likely that it lasted between 520 and 650 ka. Increased atmospheric pCO(2), related to excess volcanic emissions (magmatic activity in the Karoo and Ferrar Provinces), had an impact on climate and ocean chemistry, and marked the inception of a biotic crisis affecting many organisms. The beginning of the crisis within shallow carbonate platforms, documented at southern latitudes, predates the levels enriched in organic matter. Dinoflagellate cysts experienced a decrease in abundance in the C superbus Zone, until they temporarily disappeared. The nannoplankton crisis was twofold: a decrease in size and low calcified specimens are observed in addition to a drastic decrease in absolute abundance. The increased atmospheric pCO(2), as a result of the magmatic activity and temporarily amplified by transient methane release, could have been the trigger for the biocalcification crisis, which first affected the probably more reactive neritic system, and eventually the nannoplankton community.	Univ Lyon 1, UMR 5125, UFR Sci Terre, F-69622 Villeurbanne, France; Univ Perugia, Dept Earth Sci, I-06123 Perugia, Italy	Universite Claude Bernard Lyon 1; University of Perugia	Mattioli, E (通讯作者)，Univ Lyon 1, UMR 5125, UFR Sci Terre, 2 Rue Dubois, F-69622 Villeurbanne, France.	mattioli@univ-lyonl.fr	Mattioli, Emanuela/D-7951-2012; Pittet, Bernard/B-9664-2012	Schmid-Rohl, Annette Petra/0000-0002-1510-5986; Mattioli, Emanuela/0000-0003-0990-1641				BASSOULLET JP, 1993, ATLAS TETHYS PALEOEN; Beerling DJ, 2002, AM J SCI, V302, P28, DOI 10.2475/ajs.302.1.28; Bjerrum CJ, 2001, PALEOCEANOGRAPHY, V16, P390, DOI 10.1029/2000PA000512; Bombardiere Luca, 1993, Palaeopelagos, V3, P113; Bown P.R., 1987, Special Papers in Palaeontology, V38, P1; Claps M., 1995, Memorie di Scienze Geologiche Padova, V47, P179; Cohen AS, 2004, GEOLOGY, V32, P157, DOI 10.1130/G20158.1; Dromart G, 1996, B SOC GEOL FR, V167, P423; Elmi S., 1993, GEOBIOS, V17, P149; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; Guex Jean, 2001, Bulletin de la Societe Vaudoise des Sciences Naturelles, V87, P277; HALLAM A, 1987, MARINE PETROLEUM SOU, V26, P251; HARDING SM, 2002, GEOL SOC LOND ABSTR, P86; Harries PJ, 1999, PALAEOGEOGR PALAEOCL, V154, P39, DOI 10.1016/S0031-0182(99)00086-3; Hesselbo SP, 2000, NATURE, V406, P392, DOI 10.1038/35019044; HOWARTH MK, 1973, GEOLOGY, V24, P235; Jenkyns HC, 1997, SEDIMENTOLOGY, V44, P687, DOI 10.1046/j.1365-3091.1997.d01-43.x; JENKYNS HC, 1988, AM J SCI, V288, P101, DOI 10.2475/ajs.288.2.101; Jenkyns HC, 2002, J GEOL SOC LONDON, V159, P351, DOI 10.1144/0016-764901-130; Mattioli E, 2004, PALAEOGEOGR PALAEOCL, V205, P295, DOI 10.1016/j.palaeo.2003.12.013; Mattioli E, 2002, MAR MICROPALEONTOL, V45, P175, DOI 10.1016/S0377-8398(02)00039-7; Mattioli E, 1999, RIV ITAL PALEONTOL S, V105, P343, DOI 10.13130/2039-4942/5380; McArthur JM, 2000, EARTH PLANET SC LETT, V179, P269, DOI 10.1016/S0012-821X(00)00111-4; MONACO P, 1999, PALEOPELAGOS SPECIAL, V3, P127; Morettini E., 1998, Lower Jurassic Stable Isotope Stratigraphy (Carbon, Oxygen, Nitrogen) of the Mediterranean Tethys (Central Italy and Southern Spain); Pálfy J, 2002, GEOL SOC AM SPEC PAP, V356, P523; Palliani RB, 1998, PALAEOGEOGR PALAEOCL, V142, P33, DOI 10.1016/S0031-0182(97)00152-1; Palliani RB, 2002, MAR MICROPALEONTOL, V46, P223; Palliani RB, 1998, J MICROPALAEONTOL, V17, P153, DOI 10.1144/jm.17.2.153; Riebesell U, 2000, NATURE, V407, P364, DOI 10.1038/35030078; Riegraf W., 1985, TUBINGERMIKROPALAONT, V3, P1; Röhl HJ, 2001, PALAEOGEOGR PALAEOCL, V165, P27, DOI 10.1016/S0031-0182(00)00152-8; Röhl U, 2000, GEOLOGY, V28, P927, DOI 10.1130/0091-7613(2000)28<927:NCFTLP>2.0.CO;2; Saelen G, 1998, GEOLOGY, V26, P747, DOI 10.1130/0091-7613(1998)026<0747:EOROIL>2.3.CO;2; Schmid-Röhl A, 2002, GEOBIOS-LYON, V35, P13, DOI 10.1016/S0016-6995(02)00005-0; Venturi Federico, 1999, Palaeopelagos Special Publication, V3, P89; VETO I, 2002, 60 GEOL SOC; Wignall PB, 2001, EARTH-SCI REV, V53, P1, DOI 10.1016/S0012-8252(00)00037-4; WILLIAMS JR, 1995, PALEOCEANOGRAPHY, V10, P815, DOI 10.1029/95PA00977; Winter Amos, 1994, P161; YOUNG JR, 1991, PALAEONTOLOGY, V34, P843	41	109	112	1	15	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0016-7649	2041-479X		J GEOL SOC LONDON	J. Geol. Soc.	JUL	2004	161		4				685	693		10.1144/0016-764903-074	http://dx.doi.org/10.1144/0016-764903-074			9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology	836KP					2025-03-11	WOS:000222554900015
J	Olli, K				Olli, K			Temporary cyst formation of <i>Heterocapsa triquetra</i> (Dinophyceae) in natural populations	MARINE BIOLOGY			English	Article							ALEXANDRIUM-TAYLORI DINOPHYCEAE; COASTAL BALTIC-SEA; LIFE-HISTORY; RED TIDE; GYRODINIUM-UNCATENUM; GONYAULAX-TAMARENSIS; DINOFLAGELLATE; GROWTH; CIRCULARISQUAMA; TEMPERATURE	Heterocapsa triquetra (Ehrenberg) Stein is a phototrophic marine dinoflagellate with wide coastal distribution. It is known to be capable of mixotrophy and diel vertical migration. The species was particularly abundant in the Gulf of Finland (the Baltic Sea) during the summers of 1996 and 1998, leading to discolouration of water on the south-west coast of Finland. Large-scale (50 m(3)) coastal mesocosm experiments in the north-west Gulf of Finland (the Baltic Sea) in the summers of 1996 and 1998 with daily mineral nutrient additions provoked a biomass increase of phytoplankton dominated by H. triquetra. From the first days of the experiment temporary cysts of H. triquetra were found in the bottom sediment water of the mesocosms. Maximum temporary cyst production rates reached values up to 20x10(6) cysts m(-2) day(-1), accounting for <1% of the depth-integrated motile population size. The environmental features favouring temporary cyst production remain uncertain; zooplankton grazing and nutrient stress are potential factors. Temporary cysts of H. triquetra were observed in a unialgal culture (f/2 medium) isolated in summer 1999 from Eel Pond (Woods Hole, Mass., USA).	Univ Tartu, Inst Bot & Ecol, EE-51005 Tartu, Estonia; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	University of Tartu; Woods Hole Oceanographic Institution	Olli, K (通讯作者)，Univ Tartu, Inst Bot & Ecol, Lai 40, EE-51005 Tartu, Estonia.	olli@ut.ee	Olli, Kalle/G-5389-2010					AELION CM, 1985, J PLANKTON RES, V7, P821, DOI 10.1093/plankt/7.6.821; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; ANDERSON DM, 1985, J PHYCOL, V21, P200; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; [Anonymous], ACTA BOT FENN; BALZER I, 1992, CHRONOBIOL INT, V9, P260, DOI 10.3109/07420529209064535; BRAARUD T, 1951, AVH NORSK VIDENSK MN, V2, P2; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Garces E., 2002, LIFEHAB, P46; GIFFORD DJ, 1985, MAR ECOL PROG SER, V23, P257, DOI 10.3354/meps023257; GRZEBYK D, 1996, J PLANKTON RES, V35, P331; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HAAPALA J, 1994, ESTUAR COAST SHELF S, V38, P507, DOI 10.1006/ecss.1994.1035; HANSEN PJ, 1995, MAR ECOL PROG SER, V121, P65, DOI 10.3354/meps121065; HARDELAND R, 1994, EXPERIENTIA, V50, P60, DOI 10.1007/BF01992051; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kamiyama T, 1997, MAR BIOL, V128, P509, DOI 10.1007/s002270050117; Kim H.-G., 1990, Bulletin of the Korean Fisheries Society, V23, P468; KITA T, 1985, B MAR SCI, V37, P643; KIVI K, 1993, LIMNOL OCEANOGR, V38, P893, DOI 10.4319/lo.1993.38.5.0893; LARSSON U, 2001, OSTERSJO 98, P27; Legrand C, 1998, AQUAT MICROB ECOL, V15, P65, DOI 10.3354/ame015065; Lindholm T, 1999, HYDROBIOLOGIA, V393, P245, DOI 10.1023/A:1003563022422; Lindholm Tore, 1995, Memoranda Societatis pro Fauna et Flora Fennica, V71, P10; Montresor M., 2002, LIFEHAB LIFE HIST MI, P18; Nagasaki K, 2000, NIPPON SUISAN GAKK, V66, P666; NAKAMURA Y, 1995, AQUAT MICROB ECOL, V9, P157, DOI 10.3354/ame009157; Naustvoll LJ, 2000, PHYCOLOGIA, V39, P448, DOI 10.2216/i0031-8884-39-5-448.1; Olli K, 1996, J PHYCOL, V32, P535, DOI 10.1111/j.0022-3646.1996.00535.x; Olli K, 1996, J PLANKTON RES, V18, P1587, DOI 10.1093/plankt/18.9.1587; Olli K, 2001, MAR ECOL PROG SER, V217, P219, DOI 10.3354/meps217219; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1977, J PHYCOL, V13, P92, DOI 10.1111/j.0022-3646.1977.00092.x; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; SCHMITTER RE, 1979, TOXIC DINOFLAGELLATE; STOECKER DK, 1985, J PLANKTON RES, V7, P85, DOI 10.1093/plankt/7.1.85; Tarutani K, 2001, AQUAT MICROB ECOL, V23, P103, DOI 10.3354/ame023103; VALIKANGAS ILMARI, 1926, ACTA ZOOL FENNICA, V1, P1; Walker L.M., 1984, P19; Xiao Yong-zhi, 2001, Marine Sciences (Beijing), V25, P50	44	31	33	1	26	SPRINGER	NEW YORK	233 SPRING STREET, NEW YORK, NY 10013 USA	0025-3162			MAR BIOL	Mar. Biol.	JUL	2004	145	1					1	8		10.1007/s00227-004-1295-9	http://dx.doi.org/10.1007/s00227-004-1295-9			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	833VV					2025-03-11	WOS:000222369500001
J	Kennaway, GM; Lewis, JM				Kennaway, GM; Lewis, JM			An ultrastructural study of hypnozygotes of <i>Alexandrium</i> species (Dinophyceae)	PHYCOLOGIA			English	Article							MARINE PLANKTONIC DIATOMS; SEXUAL REPRODUCTION; GONYAULAX-TAMARENSIS; CYST FORMATION; DINOFLAGELLATE; EXCAVATA; WALL	Light, scanning and transmission electron microscopy were carried out on Alexandrium tamarense and A. fundyense hypnozygotes (cysts) from cultures and marine sediments. Transmission electron microscopy protocols were adapted to improve the quality Of Ultrathin sections. Cell contents of hypnozygotes were reduced compared to vegetative stages and were largely made up of storage vesicles in a dense, granular matrix. Chloroplasts and other organelles (Golgi bodies, endoplasmic reticulum and mitochondria) were observed as whorls of undifferentiated membranes and the nucleus was compressed with strongly condensed, granular chromosomes. Two types of accumulation bodies were found, some composed of dense amorphous material and others containing polygonal crystalline inclusions. Both types contained numerous membrane profiles. In cross section, the hypnozygote wall was made up of three layers divided by membranes: an outer layer with a thin electron-dense distal surface and membrane that formed the interface with the environment; a wide middle layer of striated material and membrane (possibly involved in deposition of cyst wall material); and a narrow unstructured inner layer and membrane lying close to the cytoplasmic membrane of the cell. Comparative analysis of cyst wall structure with other dinoflagellate species showed this three layered structure is common among refractive cysts. Energy dispersive X-ray analysis of the cyst wall surface demonstrated that the principal components of the cyst wall were sulphur and silica.	Univ Westminster, Sch Biosci, Phytosci Res Grp, London W1W 6UW, England	University of Westminster	Univ Westminster, Sch Biosci, Phytosci Res Grp, London W1W 6UW, England.	gabrielle@kennaway.net						ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], 1968, PALAEONTOGRAPHICA B; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bibby B.T., 1972, British phycol J, V7, P85; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; CORLISS JO, 1982, CILIATED PROTOZOA; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; DODGE JD, 1970, J PHYCOL, V6, P137, DOI 10.1111/j.1529-8817.1970.tb02372.x; DURR G, 1979, ARCH PROTISTENKD, V122, P121; Fensome R.A., 1993, Micropaleontology Press Special Paper; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; GAO XP, 1989, BRIT PHYCOL J, V24, P153; Glauert A.M., 1998, PRACT MET E, V17; GORDON DC, 1970, DEEP-SEA RES, V17, P175, DOI 10.1016/0011-7471(70)90096-3; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Heissenberger A, 1996, MAR ECOL PROG SER, V135, P299, DOI 10.3354/meps135299; Jacobson DM, 1996, J PHYCOL, V32, P279, DOI 10.1111/j.0022-3646.1996.00279.x; Jux U., 1971, Palaeontogr. 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B, V132, P165; JUX U, 1968, PALAEONTOGR ABT B, V123, P147; Kalicharan D, 1998, J ELECTRON MICROSC, V47, P645, DOI 10.1093/oxfordjournals.jmicro.a023638; Karnovsky M.J., 1971, Proc 11th Annu Mtg Am Soc Cell Biol, P146; KARNOVSKY MJ, 1965, J CELL BIOL, V27, pA137; Kokinos John P., 1995, Palynology, V19, P143; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; MAPLETOFT H, 1966, NEW PHYTOL, V65, P54, DOI 10.1111/j.1469-8137.1966.tb05414.x; MEKSUMPUN S, 1994, PHYCOLOGIA, V33, P275, DOI 10.2216/i0031-8884-33-4-275.1; MOLLENHAUER HH, 1964, STAIN TECHNOL, V39, P111; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; MORRILL LC, 1981, J PHYCOL, V17, P315, DOI 10.1111/j.0022-3646.1981.00315.x; Olli K, 1996, J PHYCOL, V32, P535, DOI 10.1111/j.0022-3646.1996.00535.x; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Pfiester L.A., 1984, P181; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1976, J PHYCOL, V12, P234; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; REYNOLDS ES, 1963, J CELL BIOL, V17, P208, DOI 10.1083/jcb.17.1.208; Spector D.L., 1984, P365; SPURR AR, 1969, J ULTRA MOL STRUCT R, V26, P31, DOI 10.1016/S0022-5320(69)90033-1; Von Stosch HA., 1973, Br Phycol J, V8, P105; YENTSCH CM, 1980, BIOSCIENCE, V30, P251, DOI 10.2307/1307880; ZHOU J, 1994, J PHYCOL, V30, P39, DOI 10.1111/j.0022-3646.1994.00039.x	44	14	17	0	7	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	JUL	2004	43	4					353	363						11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	844FK					2025-03-11	WOS:000223142800003
J	Hemsley, AR; Lewis, J; Griffiths, PC				Hemsley, AR; Lewis, J; Griffiths, PC			Soft and sticky development: some underlying reasons for microarchitectural pattern convergence	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	General Meeting and Workshop of the Commission-Internationale-de-Microfloredu-Paleozoique (CIMP)	SEP 05-07, 2002	Lille, FRANCE	Commiss Int Microflore Paleozo		microstructure; pattern formation; self-assembly; colloid; spores; pollen; dinoflagellate	SPOROPOLLENIN; SELAGINELLA; WALLS; ELECTRON	Surface sculpture of spores, pollen and other walled microscopic organisms commonly resembles patterns seen elsewhere in nature. These patterns are often species specific and of significant use in taxonomic study, particularly so in the fossil record where other data may be minimal. It can be argued that patterning, which must be governed to some extent by genotype, could simply reflect other natural patterns as a result of physical and chemical interaction during development. But does this diminish the view that patterning can often perform important biological functions? With examples drawn from fossil and living walled structures, we analyse the complex relationship between genetic constraints, construction mechanism and biological function, and we conclude that similar function may often result in similar pattern, perhaps further enhanced by similar aspects of development. The genetic complement, by way of selection, 'learns' to repeat the pattern, but each pattern creation mechanism retains a 'personal signature' reflecting its evolutionary history. With this new perspective in mind, we assess the potential implications in the study of Palaeozoic microfossils when many different groups are first developing surface patterning. (C) 2004 Elsevier B.V. All rights reserved.	Cardiff Univ, Dept Earth Sci, Cardiff CF10 3YE, S Glam, Wales; Univ Westminster, Sch Biosci, London W1M 8JS, England; Cardiff Univ, Dept Chem, Cardiff CF10 3TB, S Glam, Wales	Cardiff University; University of Westminster; Cardiff University	Hemsley, AR (通讯作者)，Cardiff Univ, Dept Earth Sci, Pk Pl, Cardiff CF10 3YE, S Glam, Wales.	hemsleyAR@cardiff.ac.uk	Griffiths, Peter/F-7347-2012	Griffiths, Peter/0000-0002-6686-1271				Adams M, 1998, NATURE, V393, P349, DOI 10.1038/30700; BALL P, 1994, DESIGNING MOL WORLD, P216; Barnes SH., 1986, POLLEN SPORES FORM F, P71; BOLICK MR, 1981, REV PALAEOBOT PALYNO, V35, P61, DOI 10.1016/0034-6667(81)90014-2; CHALONER W.G., 1976, EVOLUTIONARY SIGNIFI, P1; Chaloner W.G., 1986, Pollen and Spores: Form and Function, P103; CHAPMAN DJ, 1985, GEOLOGICAL FACTORS E, P23; COLLINSON ME, 1993, GRANA S, V1, P31; Cooper-Driver GA., 2001, Plants Invade the Land: Evolution and Environmental Perspectives, P159; Crane PR., 1986, Pollen and Spores: Form and Function, P179; Dickinson HG., 1986, POLLEN SPORES FORM F, P1; EVANS DF, 1994, COLLOIDAL DOMAIN PHY, P325; Everett D.H., 1988, Basic Principles of Colloid Science, DOI DOI 10.1039/9781847550200; GABARAYEVA NI, 2000, POLLEN SPORES MORPHO, P1; Gunning B.E.S., 1986, Plant Cell Biology. 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Palaeobot. Palynology	JUL	2004	130	1-4					105	119		10.1016/j.revpalbo.2003.12.004	http://dx.doi.org/10.1016/j.revpalbo.2003.12.004			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	834UB					2025-03-11	WOS:000222435300006
J	Mullins, GL; Aldridge, RJ; Siveter, DJ				Mullins, GL; Aldridge, RJ; Siveter, DJ			Microplankton associations, biofacies and palaeoenvironment of the type lower Ludlow Series, Silurian	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	General Meeting and Workshop of the Commission-Internationale-de-Microfloredu-Paleozoique (CIMP)	SEP 05-07, 2002	Lille, FRANCE	Commiss Int Microflore Paleozo		acritarchs; prasinophytes; Silurian; biofacies; palaeoenvironment; Ludlow	DINOFLAGELLATE CYSTS; DEVONIAN ACRITARCHS; OCEANIC EPISODES; ORGANIC-MATTER; ACID-RESISTANT; BIOGEOGRAPHY; CHITINOZOANS; ORDOVICIAN; WENLOCK; NORTH	The acritarchs and prasinophyte algae from the type lower Ludlow Series of the Goggin Road section, Ludlow, England, are resolved into seven recurrent associations comprising taxa with similar environmental preferences. Endemic and environmentally sensitive associations of acritarchs and prasinophytes are identified and high-resolution fluctuations in the early Ludlow palaeoenvironment are established. An early Ludlow crisis in the acritarchs is recognized in the lower part of the Middle Elton Formation, when an abrupt palaeoenvironmental change in the Ludlow area resulted in a large decline in the abundance of the acritarchs, but allowed Tasmanites and retiolitid graptolites to flourish briefly. Cymbosphaeridium sp. A, Pulvinosphaeridium ludlowense and Multiplicisphaeridium arbusculum forma A are taxa possibly specialized, or produced as a response, to a stressed palaeoenvironment, as they are most abundant when other acritarchs and prasinophytes are uncommon. The low abundance of acritarchs and prasinophytes in the Upper Elton Formation may be related to high sedimentation rates and to the slumping of sediments caused by instability on the shelf of the Welsh Basin, or to lower plankton productivity. (C) 2004 Elsevier B.V. All rights reserved.	Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England	University of Leicester	Univ Leicester, Dept Geol, Univ Rd, Leicester LE1 7RH, Leics, England.	glm2@leicester.ac.uk						ALAMERI TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103, DOI 10.1016/0031-0182(83)90007-X; ALDRIDGE RJ, 1993, J GEOL SOC LONDON, V150, P501, DOI 10.1144/gsjgs.150.3.0501; ALDRIDGE RJ, 1989, NATL MUSEUM WALES GE, V9, P274; [Anonymous], 1971, POLLEN SPORES; BASSETT MG, 1979, FIELD M GREAT BRIT M, P48; BERRY WBN, 1972, P 24 INT GEOL C MONT, V7, P59; Bickert T, 1997, GEOCHIM COSMOCHIM AC, V61, P2717, DOI 10.1016/S0016-7037(97)00136-1; BOALCH GT, 1969, J MAR BIOL ASSOC UK, V49, P129, DOI 10.1017/S0025315400046464; CATTELL RB, 1966, MULTIVAR BEHAV RES, V1, P245, DOI 10.1207/s15327906mbr0102_10; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; COLBATH GK, 1990, PALAEOZOIC PALAEOGEO, V12, P97; COLBATH GK, 1980, MICROPALEONTOLOGY, V1, P97; COMBAZ A, 1967, Review of Palaeobotany and Palynology, V1, P309, DOI 10.1016/0034-6667(67)90131-5; COMBAZ A, 1966, PALEOBOTANIST, V15, P29; Cramer F.H., 1979, Palinologia, V1, P17; CRAMER F H, 1969, Journal of Paleontology, V43, P485; CRAMER F. 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E., 1978, 7830 I GEOL SCI, P1; WHITE JM, 1989, POLLEN SPORES, V30, P131; Wicander R, 1997, REV PALAEOBOT PALYNO, V98, P125, DOI 10.1016/S0034-6667(97)00017-1; WOODCOCK NH, 2000, BRIT SILURIAN STRATI, V19, P3; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	86	17	17	0	4	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUL	2004	130	1-4					163	194		10.1016/j.revpalbo.2003.12.006	http://dx.doi.org/10.1016/j.revpalbo.2003.12.006			32	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	834UB					2025-03-11	WOS:000222435300009
J	Stricanne, L; Munnecke, A; Pross, J; Servais, T				Stricanne, L; Munnecke, A; Pross, J; Servais, T			Acritarch distribution along an inshore-offshore transect in the Gorstian (lower Ludlow) of Gotland, Sweden	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	General Meeting and Workshop of the Commission-Internationale-de-Microfloredu-Paleozoique (CIMP)	SEP 05-07, 2002	Lille, FRANCE	Commiss Int Microflore Paleozo		acritarchs; palynomorphs; palaeoecology; Gotland; silurian; ludlow	OLIGOCENE DINOFLAGELLATE CYSTS; BRACHIOPOD SHELLS; STABLE-ISOTOPES; MIDDLE; ORDOVICIAN; ATLANTIC; GERMANY; FACIES; NORTH; SEAS	To better understand palaeoecological signatures in Palaeozoic acritarch assemblages, the distribution of palynomorphs has been quantitatively studied in eight localities from the Gorstian, lower Ludlow (Late Silurian) of Gotland, Sweden. The localities are situated along an inshore-offshore transect comprising shallow marine lagoonal environments to distal shelf facies. Process-bearing acritarchs and sphaeromorphs constitute the main components within the palynomorph assemblages. The lateral distribution of palynomorphs exhibits characteristic features at three different levels as follows. (1) With regard to the overall composition of the palynomorph assemblages, the abundance of process-bearing acritarchs increases towards the distal shelf, while the abundance of sphaeromorphs decreases. (2) At the generic level, the acritarchs Micrhystridium and Dilatisphaera are more abundant in the proximal facies, while Evittia, Percultisphaera and Oppilatala are more common in distal environments. (3) At an infrageneric level, Micrhystridium morphotypes with shorter processes are mainly present in proximal environments, while those with longer and ramified processes occur in more distal shelf environments. The palynomorph distribution along the inshore-offshore transect highlights the potential of acritarchs and prasinophytes as palaeoenvironmental indicators. (C) 2004 Elsevier B.V. All rights reserved.	Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany; Univ Sci & Technol Lille, Lab Paleontol & Paleogeog Paleozo LP3, CNRS, UMR 8014, F-59655 Villeneuve Dascq, France; Univ Sci & Technol Lille, CNRS, FR 1818, F-59655 Villeneuve Dascq, France; Univ Erlangen Nurnberg, Inst Paleontol, D-91054 Erlangen, Germany	Eberhard Karls University of Tubingen; Universite de Lille; Centre National de la Recherche Scientifique (CNRS); Centre National de la Recherche Scientifique (CNRS); Universite de Lille; University of Erlangen Nuremberg	Univ Tubingen, Inst Geowissensch, Sigwartstr 10, D-72076 Tubingen, Germany.	ludovic.stricanne@uni-tuebingen.de	Munnecke, Axel/G-3698-2010; Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018	Munnecke, Axel/0000-0002-6898-1082; Servais, Thomas/0000-0002-4089-7874				ALAMERI TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103, DOI 10.1016/0031-0182(83)90007-X; [Anonymous], 1980, PALEOBIOLOGY PLANT P; BERG U, 1989, ADV PHYS ORG CHEM, V25, P1; BERGMAN CF, 1987, THESIS; Bickert T, 1997, GEOCHIM COSMOCHIM AC, V61, P2717, DOI 10.1016/S0016-7037(97)00136-1; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BRITO IGNACIO MACHADO, 1967, MICROPALEONTOLOGY [NY], V13, P473, DOI 10.2307/1484722; COLBATH G K, 1980, Micropaleontology (New York), V26, P97, DOI 10.2307/1485278; Cramer F.H., 1967, B INSTITUTO GEOLOGIC, V77, P225; CRAMER FH, 1970, DISTRIBUTION SELECTE; CRAMER FH, 1979, GOTLAND SVER GEOL C, V762, P39; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Deflandre G., 1945, Annales de Paleontologie, V31, P41; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEJEKHOWSKY B, 1963, CR SEANCES SOC BIOGE, V345, P567; Deunff J., 1954, Compte Rendu Sommaire de la Socit gologique de France, V13, P305; Dorning K.J., 1987, P266; Dorning K.J., 1981, P31; Dorning K.J., 1987, P256; DORNING KJ, 1981, REV PALAEOBOT PALYNO, V34, P175, DOI 10.1016/0034-6667(81)90037-3; DOWNIE CHARLES, 1960, MICROPALEONTOLOGY, V6, P197, DOI 10.2307/1484467; EIKENACK A., 1965, NEUES JAHRBUCHFUR GE, V122, P257; EIKENACK A., 1954, SENCKENBERG LETHAEA, V34, P205; Eisenack A., 1958, Palaeontographica, V110A, P1; Eisenack A., 1968, NEUES JB GEOL PAL, V131, P1; EISENACK A, 1931, PALAEONTOL Z, V13, P75; EISENACK ALFRED, 1955, SENCKENBERGIANA LETHAEA, V36, P157; EISENACK ALFRED, 1938, ZEITSCHR GESCHIEBE FORSCH, V14, P1; Eisenaek A., 1959, Palaeontographica, VA112, P193; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Hagstrom J, 1997, GFF, V119, P301, DOI 10.1080/11035899709546492; JACOBSON SR, 1979, J PALEONTOL, V53, P1197; Jeppsson L, 2000, J GEOL SOC LONDON, V157, P1137, DOI 10.1144/jgs.157.6.1137; JEPPSSON L, 1990, J GEOL SOC LONDON, V147, P663, DOI 10.1144/gsjgs.147.4.0663; KIRJANOV VW, 1978, AKRITARCHI SILURA VO, P1; Laufeld S., 1974, Fossils Strata, VNo. 5, P1; Laufeld S., 1974, SVERIGES GEOLOGISKA, V750, P1, DOI DOI 10.18261/8200093581-1974-01; le Herisse A., 1989, Palaeontographia Italica, V76, P57; Li J, 2004, REV PALAEOBOT PALYNO, V130, P141, DOI 10.1016/j.revpalbo.2003.12.005; LISTER TR, 1970, PALAEONTOGR SOC MONO, V1, P1; Loeblich A.R. Jr, 1976, Palaeontographica Abteilung B Palaeophytologie, V159, P1; LOEBLICH AR, 1975, P N AM PAL C G, P705; Munnecke A, 1996, FACIES, V34, P159, DOI 10.1007/BF02546162; Munnecke Axel, 1996, Palynology, V20, P163; PLAYFORD G, 1977, GEOL SURV CAN B, V179, P1; Pross J, 2002, MAR MICROPALEONTOL, V45, P1, DOI 10.1016/S0377-8398(01)00046-9; PROSS J, IN PRESS PALAONTOL Z; RAMSKOLD L, 1986, PALAEONTOLOGY, V29, P527; RICHARDSON JB, 1990, J GEOL SOC LONDON, V147, P675, DOI 10.1144/gsjgs.147.4.0675; Riding James B., 1999, Palynology, V23, P15; RIEGEL W, 1974, REV PALAEOBOT PALYNO, V18, P29, DOI 10.1016/0034-6667(74)90006-2; Samtleben C, 1996, GEOL RUNDSCH, V85, P278, DOI 10.1007/s005310050074; Samtleben C, 2000, FACIES, V43, P1, DOI 10.1007/BF02536983; SARJEANT WAS, 1994, MICROPALEONTOLOGY, V40, P1, DOI 10.2307/1485800; SERVAIS T, IN PRESS PALAEONTOLO; Stancliffe RPW, 1996, MICROPALEONTOLOGY, V42, P151, DOI 10.2307/1485867; Staplin F. L., 1961, Palaeontology, V4, P392; Staplin F. L., 1965, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V123, P167; Stockmans F., 1960, Senckenbergiana Lethaea, V41, P1; TAPPAN H, 1971, Micropaleontology (New York), V17, P385, DOI 10.2307/1484870; THUSU B, 1973, Palaeontology (Oxford), V16, P799; VANGUESTAINE M, 1997, ACRITARCHA PRAHA 199, V40, P681; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wall D., 1962, GEOL MAG, V99, P353, DOI [10.1017/S0016756800058465, DOI 10.1017/S0016756800058465]; WETZEL O, 1952, GEOL JB, V66, P391; WETZEL O., 1933, PALAEONTOGRAPHICA A, V78, P1; WICANDER E.R., 1974, Palaeontographica, Abt B, V148, P9; Wicander R, 1997, REV PALAEOBOT PALYNO, V98, P125, DOI 10.1016/S0034-6667(97)00017-1; Zebera K., 1935, Bull int Acad tcheque Sci Cl Math etc Prag, V36, P88	71	43	47	0	3	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUL	2004	130	1-4					195	216		10.1016/j.revpalbo.2003.12.007	http://dx.doi.org/10.1016/j.revpalbo.2003.12.007			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	834UB					2025-03-11	WOS:000222435300010
J	Wiese, F; Cech, S; Ekrt, B; Kost'ák, M; Mazuch, M; Voigt, S				Wiese, F; Cech, S; Ekrt, B; Kost'ák, M; Mazuch, M; Voigt, S			The Upper Turonian of the Bohemian Cretaceous Basin (Czech Republic) exemplified by the Upohlavy working quarry:: integrated stratigraphy and palaeoceanography of a gateway to the Tethys	CRETACEOUS RESEARCH			English	Review						Upper Cretaceous; Turonian; Czech Republic; Bohemia; integrated stratigraphy; biosedimentation; palaeoceanography; oligotrophic system	CALCAREOUS DINOFLAGELLATE CYSTS; EQUATORIAL ATLANTIC-OCEAN; SEA-LEVEL CHANGES; SEQUENCE STRATIGRAPHY; NORTHERN GERMANY; CENTRAL-EUROPE; ISOTOPE STRATIGRAPHY; PECINOV QUARRY; CARBON-ISOTOPE; MARINE	The north Bohemian Cretaceous (Bohemian Cretaceous Basin, Czech Republic) is located between the northern temperate areas and the Tethys. As a gateway to the Tethys, lithology, fauna and integrated stratigraphy (litho-, bio-, event, sequence, stable isotope stratigraphy) of the Upper Turonian succession in the Upohlavy working quarry are described. Due to a large hiatus, the delta(13)C curve cannot be used for stratigraphic purposes at the base of the section. Up-section, the curve exhibits the well-known middle Upper Turonian positive excursion. Biostratigraphic and sequence stratigraphic subdivisions permit good correlation with other European Cretaceous basins. The inoceramid bivalve assemblage enables correlation with the US Western Interior. Palaeoceanographically, a positive peak in the delta(18)O curve above the hiatus indicates the upper part of the Late Turonian cooling event observed in other areas. The cooling was accompanied by a southward shift of a cool/temperate oceanic biosedimentary system, expressed by the sudden turnover from siliciclastic towards pelagic carbonate deposition. It is associated with the establishment of presumed oligotrophic conditions in the immediate vicinity of the West Sudetic Island, as indicated by the sudden decrease of macrofaunal abundance and diversity. (C) 2004 Elsevier Ltd. All rights reserved.	FU Berlin, Fachrichtung Palaontol, D-12249 Berlin, Germany; Czech Geol Survey, Prague 11821 1, Czech Republic; Natl Museum, Prague 11579 1, Czech Republic; Charles Univ, Fac Sci, Inst Geol & Palaeontol, Prague 12843 2, Czech Republic; Univ Cologne, Inst Geol, D-50674 Cologne, Germany	Free University of Berlin; Czech Geological Survey; National Museum; Charles University Prague; University of Cologne	Wiese, F (通讯作者)，FU Berlin, Fachrichtung Palaontol, Malteserstr 74, D-12249 Berlin, Germany.	frwiese@snafu.de; cech@cgu.cz; ekrtb@nm.cz; kostak@natur.cuni.cz; mmazuch@centrum.cz; silke.voigt@uni-koeln.de	; Mazuch, Martin/I-5964-2017; Voigt, Silke/G-7270-2017; Kostak, Martin/I-6006-2017	Wiese, Frank/0000-0002-6910-2166; Mazuch, Martin/0000-0002-1697-3742; Voigt, Silke/0000-0002-2560-5933; Kostak, Martin/0000-0002-0818-3505				ADAMS T. 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Res.	JUN	2004	25	3					329	352		10.1016/j.cretres.2004.01.003	http://dx.doi.org/10.1016/j.cretres.2004.01.003			24	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	827MW					2025-03-11	WOS:000221905000003
J	Galeotti, S; Brinkhuis, H; Huber, M				Galeotti, S; Brinkhuis, H; Huber, M			Records of post-Cretaceous-Tertiary boundary millennial-scale cooling from the western Tethys: A smoking gun for the impact-winter hypothesis?	GEOLOGY			English	Article						K-T boundary; foraminifera; dinoflagellates; extraterrestrial impact; cooling	BENTHIC FORAMINIFERA; CLIMATE; EXTINCTION; TUNISIA; TERRESTRIAL; CIRCULATION; SIMULATION; ANHYDRITE; CHICXULUB; EVENT	The record of both dinoflagellate cysts and benthic foraminifera across the Cretaceous-Tertiary boundary at El Kef, Tunisia, reveals a brief expansion of the Boreal bioprovince into the western Tethys, suggesting that an similar to2 k.y. cooling occurred during the earliest Danian. We show that this prolonged cooling phase is consistent with the oceanographic response to an impact winter.	Univ Urbino, Ist Geol, I-61029 Urbino, Italy; Univ Urbino, Ctr Geobiol, I-61029 Urbino, Italy; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47906 USA	University of Urbino; University of Urbino; Utrecht University; Purdue University System; Purdue University	Galeotti, S (通讯作者)，Univ Urbino, Ist Geol, Localita Crocicchia, I-61029 Urbino, Italy.		Brinkhuis, Henk/B-4223-2009; Huber, Matthew/A-7677-2008	Huber, Matthew/0000-0002-2771-9977; Brinkhuis, Henk/0000-0003-0253-6610; Galeotti, Simone/0000-0001-9636-9344				ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], 356 GEOL SOC AM; Arenillas I, 2002, GEOL SOC AM SPEC PAP, V356, P253; Bendtsen J, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2002GL014829; BOLTOVSKOY E, 1991, J PALEONTOL, V65, P175, DOI 10.1017/S0022336000020394; BRETT R, 1992, GEOCHIM COSMOCHIM AC, V56, P3603, DOI 10.1016/0016-7037(92)90406-9; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Brummer G.-J. A., 1988, Planktonic Foraminifers as Tracers of Ocean-Climate History, P293; Coccioni R, 1998, B SOC GEOL FR, V169, P271; Dressler B.O., 2003, EOS Transactions American Geophysical Union, V84, P125, DOI DOI 10.1029/2003EO140001; Galeotti S, 2002, PALAEOGEOGR PALAEOCL, V178, P197, DOI 10.1016/S0031-0182(01)00396-0; GRADSTEIN FM, 1989, MICROPALEONTOLOGY, V35, P72, DOI 10.2307/1485538; Gupta SC, 2001, EARTH PLANET SC LETT, V188, P399, DOI 10.1016/S0012-821X(01)00327-2; Huber M, 2001, GEOPHYS RES LETT, V28, P3481, DOI 10.1029/2001GL012943; Huber M, 2000, PALEOCEANOGRAPHY, V15, P443, DOI 10.1029/1999PA000455; KELLER G, 1988, PALAEOGEOGR PALAEOCL, V66, P153, DOI 10.1016/0031-0182(88)90198-8; Lomax B, 2001, EARTH PLANET SC LETT, V192, P137, DOI 10.1016/S0012-821X(01)00447-2; Luder T, 2002, GEOL SOC AM SPEC PAP, V356, P717; Lyle M, 1997, PALEOCEANOGRAPHY, V12, P161, DOI 10.1029/96PA03330; MAGARITZ M, 1992, PALAEOGEOGR PALAEOCL, V91, P291, DOI 10.1016/0031-0182(92)90073-E; Mukhopadhyay S, 2001, SCIENCE, V291, P1952, DOI 10.1126/science.291.5510.1952; Pierazzo E, 2003, ASTROBIOLOGY, V3, P99, DOI 10.1089/153110703321632453; Pope KO, 1997, J GEOPHYS RES-PLANET, V102, P21645, DOI 10.1029/97JE01743; RYDER G., 1996, 307 GEOL SOC AM; SMIT J, 1980, NATURE, V285, P198, DOI 10.1038/285198a0; SMIT J, 1997, MAR MICROPALEONTOL, V29, P67; Speijer R.P., 1994, Geologica Ultraiectinia, V124, P19; Stüben D, 2003, PALAEOGEOGR PALAEOCL, V199, P107, DOI 10.1016/S0031-0182(03)00499-1; Vallis GK, 2000, J PHYS OCEANOGR, V30, P933, DOI 10.1175/1520-0485(2000)030<0933:LSCAPO>2.0.CO;2; Wilf P, 2003, P NATL ACAD SCI USA, V100, P599, DOI 10.1073/pnas.0234701100	31	51	55	1	11	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613	1943-2682		GEOLOGY	Geology	JUN	2004	32	6					529	532		10.1130/G20439.1	http://dx.doi.org/10.1130/G20439.1			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	826SS					2025-03-11	WOS:000221849500018
J	Garcés, E; Bravo, I; Vila, M; Figueroa, RI; Masó, M; Sampedro, N				Garcés, E; Bravo, I; Vila, M; Figueroa, RI; Masó, M; Sampedro, N			Relationship between vegetative cells and cyst production during <i>Alexandrium minutum</i> bloom in Arenys de Mar harbour (NW Mediterranean)	JOURNAL OF PLANKTON RESEARCH			English	Article							DINOFLAGELLATE GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; POPULATION-DYNAMICS; SEXUAL REPRODUCTION; SPRING-BLOOM; LIFE-CYCLE; DINOPHYCEAE; SCRIPPSIELLA; JAPAN; BAY	A recurrent Alexandrium minutum bloom in the Arenys de Mar harbour (Catalan coast, North Western Mediterranean) was monitored in order to establish the relationship between vegetative cells and cyst production. The bloom lasted from January 21 to February 24, 2002 and reached cell concentrations of up to 47 x 10(6) cell L-1. Two aspects related to the resting cysts deposition were studied: (i) production of resting cysts during the bloom period (by means of sediment traps) and (ii) distribution of resting cysts in the sediment after the bloom (May 2002). Cyst formation in Arenys clearly started in a period with high vegetative cell densities in the water column. Once production was initiated encystment fluxes remained constant for two weeks, and covering the periods of maintenance and decline of the bloom. High cyst fluxes (up to 6000 cysts cm(-2) day(-1)) were quantified as a result of the high vegetative cell concentration. Moreover, encystment occurring in less than 1% of the total population indicates that most of the cells are not involved in resting cysts formation. A comparison of the resting cyst flux values obtained from the sediment traps and the resting cyst concentrations in surface sediment (628-3270 cysts cm(-3)) three months later, revealed that the number of cysts in the sediment decreased during that time. The studies of excystment showed a high germination percentage (91%) and germling viability (100%). These data, together with the resting cyst distribution in the sediment, are important in assessing the role of resting cysts in the bloom dynamics of A. minutum in confined waters.	CSIC, Inst Ciencies Mar, Barcelona, Spain; Inst Oceanog Vigo, Vigo, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Spanish Institute of Oceanography		esther@icm.csic.es	Bravo, Isabel/D-3147-2012; Garces, Esther/C-5701-2011; Figueroa, Rosa/M-7598-2015; SAMPEDRO, NAGORE/I-1767-2015; Vila, Magda/B-2447-2014	Bravo, Isabel/0000-0003-3764-745X; Garces, Esther/0000-0002-2712-501X; Figueroa, Rosa/0000-0001-9944-7993; SAMPEDRO, NAGORE/0000-0002-0829-5152; Vila, Magda/0000-0002-6855-841X				Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BLANCO J, 1986, Boletin Instituto Espanol de Oceanografia, V3, P81; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; BRAVO I, 1997, INFORMES TECNICOS I, V168, P32; Calbet A, 2003, MAR ECOL PROG SER, V259, P303, DOI 10.3354/meps259303; DELGADO M, 1990, Scientia Marina, V54, P1; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; FORTEZA V, 1998, 8 INT C HARMF ALG VI, P58; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Garcés E, 1999, J PLANKTON RES, V21, P2373, DOI 10.1093/plankt/21.12.2373; Gardner WD., 2000, The changing ocean carbon cycle: a mid-term synthes is of the Joint Global Ocean Flux Study, P240; Giacobbe MG, 1996, ESTUAR COAST SHELF S, V42, P539, DOI 10.1006/ecss.1996.0035; Giangrande A, 2002, J SEA RES, V47, P97, DOI 10.1016/S1385-1101(01)00103-4; GRASSOHOFF K, 1983, METHODS SEA WATER AN; Halim Y., 1960, Vie et Milieu, V11, P102; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; LEWIS J, 2002, LIFEHAB LIFE HIST MI; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Nehring Stefan, 1994, Harmful Algae News, V9, P1; Probert I, 2002, CRYPTOGAMIE ALGOL, V23, P343; Probert I.P., 1999, Ph.D. Thesis; Tsujino M, 2001, NIPPON SUISAN GAKK, V67, P850; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Vila M, 2001, J PLANKTON RES, V23, P497, DOI 10.1093/plankt/23.5.497; WALKER LM, 1979, J PHYCOL, V15, P312; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; WELSCHMEYER NA, 1994, LIMNOL OCEANOGR, V39, P1985, DOI 10.4319/lo.1994.39.8.1985; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	39	92	96	0	24	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	JUN	2004	26	6					637	645		10.1093/plankt/fbh065	http://dx.doi.org/10.1093/plankt/fbh065			9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	825HI		Bronze			2025-03-11	WOS:000221746500005
J	Slimani, H				Slimani, H			A reappraisal of the dinoflagellate cyst genus <i>Montanarocysta</i>	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Montanarocysta; ornamentation; sexifonn gonyaulacacean tabulation	ENGLAND	The dinocyst genus Montanarocysta Corradini is emended, based on re-examination of the holotype, the paratype and wel preseved specimens of the type species, Montanarocysta aemiliana Corradini. This re-examination shows that M. aemiliana has a sexiform gonyaulacaccan tabulation incompletely delineated by processes and septa, a large untabulated ventral area, an apical archeopyle type (tA)a with well-developed precingular accessory sutures, and a simple adnate operculum attached to the sulcal as and precingular plates 1" and 6". Maghrebinia chleuh Below and Maghrebinia mirabilis (Below) Masure are here transferred to Montanarocysta, since they have closely similar morphology to M. aemiliana. Previously Atopodinium Drugg has been considered as taxonomic senior synonym of Maghrebinia Below and Bejuia Stover Williams, and the species in these two genera have been transferred to Atopodinium. From the present analyses, Atopodinium is separated from Montanarocysta on the ornamentation: Atopodinium has a more subdued ornamentation, consisting of ridges, folds, grana and gemmae; whereas Montanarocysta is characterised by processes and septa. Maghrebinia is herein retained as separate genus, which has a ceratocoryacean tabulation and contains the single species Maghrebinia perforata Below. (C) 2004 Elsevier B.V. All rights reserved.	Univ Mohammed V Agdal, Inst Sci, Dept Geol, Rabat, Morocco	Mohammed V University in Rabat	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Dept Geol, Ave Ibn Batouta,BP 703, Rabat, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913				ANTONESCU E, 2001, IUGS SPECIAL PUBLICA, V19, P253; Arai M., 1992, B S CRETACEO BRASIL, V2, P27; BEJU D, 1983, J PALEONTOL, V57, P106; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BUTSCHLI O, 1885, KLASSEN ORDNUNGEN TH, V1, P865; Cavagnetto Carla, 1998, Geodiversitas, V20, P239; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; FENSOME RA, 1993, MICROPALEONTOL; Masue Edwige, 1991, Palynology, V15, P63; MASURE E, 1981, B CTR RECHERCHE EXPL, V12, P361; Masure E., 1985, CAMPANIEN STRATOTYPI, V10, P41; MASURE E, 1988, SCI RESULTS, V101, P121; Pascher A., 1914, Berlin Ber D bot Ges, V32; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; SCHIOLER P, 1992, REV PALAEOBOT PALYNO, V72, P1, DOI 10.1016/0034-6667(92)90171-C; SCHIOLER P, 2001, IUGS SPECIAL PUBLICA, V19, P222; Slimani H, 1996, ANN SOC GEOL BELG, V117, P371; SLIMANI H., 2000, MEMOIRS GEOLOGICAL S, V46; SLIMANI H, 1995, THESIS PALEONTOLOGIE; Slimani Hamid, 2001, Geologica et Palaeontologica, V35, P161; Smelror M, 1996, NEWSL STRATIGR, V34, P109; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; von Stein F. R., 1883, ORGANISMUS INFUSIONS; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34	27	1	1	0	0	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUN	2004	129	4					175	185		10.1016/j.revpalbo.2004.01.006	http://dx.doi.org/10.1016/j.revpalbo.2004.01.006			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	828XK					2025-03-11	WOS:000222006800001
J	Van Simaeys, S; De Man, E; Vandenberghe, N; Brinkhuis, H; Steurbaut, E				Van Simaeys, S; De Man, E; Vandenberghe, N; Brinkhuis, H; Steurbaut, E			Stratigraphic and palaeoenvironmental analysis of the Rupelian-Chattian transition in the type region: evidence from dinoflagellate cysts, foraminifera and calcareous nannofossils	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						Rupelian-Chattian boundary; north Sea Basin; dinoflagellate cysts; benthic foraminifera; calcareous nannofossils	LATE EOCENE; BIOSTRATIGRAPHY; ATLANTIC; MAGNETOSTRATIGRAPHY; NANNOPLANKTON; SEQUENCE; TERTIARY; OCEAN; SEAS	Quantitative analysis of organic-walled dinoflagellate cysts (dinocysts), foraminifera and calcareous nannofossils from boreholes in Belgium and Germany enables the recognition of biotic events and reconstruction of environmental change in the late Rupelian and early Chattian in their type region the southern North Sea Basin. Compared to the early Rupelian depositional conditions (neritic) do not seem to have substantially changed during the late Rupelian. The microfossil groups died indicate relatively cold-water conditions in an outer-shelf environment. The boundary between the (lower) Rupelian stratotype section and the Upper Rupelian subsurface succession can be recognized by the first occurrence (FO) of Saturnodinium pansum and the last occurrence (LO) of Enneadocysta pectiniformis (dinocysts). The traditional Rupelian-Chattian (R-C) boundary definition, at the base of the benthic foraminiferal Asterigerinoides guerichi acme known as the Asterigerina Horizon, is upheld here. In terms of dinocyst biostratigraphy, it coincides with the FO of Artemisiocysta cladodichotoma and the recurrence of Pentadinium imaginatum, falling within the middle of the NP24* nannofossil zone (* points to the substitute zonation for the North Sea Basin). The traditional R-C boundary coincides with an abrupt return of shallow warm-water conditions and represents a third-order sequence boundary. The R-C boundary is overlain by transgressive Chattian deposits, which correspond to a distinct warming event. This pulse may correlate with the globally detected Late Oligocene Warming Event, which has an approximate age of 26 Ma. A mid-Chattian hiatus coincides with the NP24*/NP25* boundary and with the simultaneous disappearance of several dinocyst taxa. A detailed literature study proved that the LO of the planktonic foraminiferal genus Chiloguembelina is globally diachronous. Hence, the validity of this Chiloguembelina extinction as a global R-C boundary criterion can be questioned. This study offers new perspectives for the search for a R-C boundary Global Stratotype Section and Point (GSSP). (C) 2004 Elsevier B.V. All rights reserved.	Univ Louvain, B-3000 Louvain, Belgium; Inst Royal Sci Nat Belgique, B-1000 Brussels, Belgium; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	Utrecht University	Van Simaeys, S (通讯作者)，Univ Louvain, Redingenstr 16, B-3000 Louvain, Belgium.	stefaan.vansimaeys@geo.kuteuven.ac.be	Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				Anderson A.J., 1971, Stratotypes of Mediterranean Neogene Stages, P69; ANDERSON AJ, 1961, MEYNIANA, V10, P118; [Anonymous], P 1 INT C PLANKT MIC; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; [Anonymous], 1995, Publ. Society for Sedimentary Geology. III. Cenozoic Era; Berggren W.A., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P551, DOI 10.2973/odp.proc.sr.120.151.1992; Berggren W. 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Paleoclimatol. Paleoecol.	MAY 31	2004	208	1-2					31	58		10.1016/j.palaeo.2004.02.029	http://dx.doi.org/10.1016/j.palaeo.2004.02.029			28	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	829IE					2025-03-11	WOS:000222040400003
J	Tsujino, M; Uchida, T				Tsujino, M; Uchida, T			Fate of resting cysts of <i>Alexandrium</i> spp. ingested by <i>Perinereis nuntia</i> (Polychaeta) and <i>Theola fragilis</i> (Mollusca)	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Alexandrium spp.; resting cysts; faecal pellet; Perinereis nuntia; Theola fragilis; grazing	SETO-INLAND-SEA; TOXIC DINOFLAGELLATE; HIROSHIMA-BAY; DINOPHYCEAE; TAMARENSE; JAPAN; GERMINATION; SEDIMENTS; ABUNDANCE; ECOLOGY	The ingestion of resting cysts of Alexandrium spp. by Perinereis nuntia (Polychaeta) and Theola fragilis (Mollusca) was experimentally examined in the laboratory. P. nuntia and T. fragilis were cultured in bottom sediment containing a high density of Alexandrium cysts under dark conditions. Moreover, to evaluate the degree and consequence of being ingested, the density of cysts in the control sediment (no macrobenthic organisms) and the germination capability of the cysts in the faccal pellets of the two species of macrobenthos were examined. Cysts in the culture sediment were found to be ingested by both P. nuntia and T. fragilis. No difference in the density of cysts between the sediments cultured with and without P. nuntia was observed. However, the density of cysts in the sediments with T. fragilis decreased by 24% compared to the density in the control sediment. It is possible that most of the cysts ingested were digested by T. fragilis. The rate of Alexandrium cyst digestion by this species is estimated 594 cysts/individual/ day. It is estimated that 91% of the cysts ingested by T. fragilis were partially or totally digested and only 9% were excreted in a viable state during the experiment. Thus, T. fragilis has a stronger affect on the abundance of Alexandrium cysts compared with P. nuntia. No significant difference was observed between the germination success of the cysts from faecal pellets of P. nuntia and T. fragilis compared to the cysts in the control sediment. If, however, the necessary light for the cysts to germinate is cut off by being enclosed within the faecal pellet, the germination rate of cysts from the faecal pellets may be suppressed. (C) 2003 Elsevier B.V. All rights reserved.	Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Coastal Environm & Productivity Div, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Coastal Environm & Productivity Div, Hiroshima 7390452, Japan.	Itaoka@fra.affrc.go.jp						Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; IMABAYASHI H, 1984, B JPN SOC SCI FISH, V50, P1855; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; REID PC, 1987, J PLANKTON RES, V9, P249, DOI 10.1093/plankt/9.1.249; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; Tsujino M, 2001, NIPPON SUISAN GAKK, V67, P850; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Yamamoto Tamiji, 1999, Phycological Research, V47, P27, DOI 10.1111/j.1440-1835.1999.tb00280.x	15	14	17	0	4	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0022-0981	1879-1697		J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	MAY 26	2004	303	1					1	10		10.1016/j.jembe.2003.10.018	http://dx.doi.org/10.1016/j.jembe.2003.10.018			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	821SG					2025-03-11	WOS:000221482300001
J	Reichart, GJ; Brinkhuis, H; Huiskamp, F; Zachariasse, WJ				Reichart, GJ; Brinkhuis, H; Huiskamp, F; Zachariasse, WJ			Hyperstratification following glacial overturning events in the northern Arabian Sea	PALEOCEANOGRAPHY			English	Article						Arabian Sea; dinoflagelates cysts; oxygen minimum zone	OXYGEN MINIMUM ZONE; INDIAN-OCEAN; LATE QUATERNARY; GREENLAND ICE; SEDIMENTS; CLIMATE; DENITRIFICATION; ARAGONITE; RECORDS; CYSTS	Correlations between Arabian Sea organic carbon and GISP2 delta(18)O records indicate a pronounced oxygen minimum zone (OMZ) during interstadials, whereas well-oxygenated conditions prevailed during stadials. Local deep winter mixing ventilated intermediate water during the coldest stadials, corresponding to North Atlantic Heinrich events. Here we show that in the Arabian Sea periods of climatic warming following Heinrich events H6-H4 and the Younger Dryas (YD) are characterized by dominant Polysphaeridium zoharyi (dinoflagellate) cysts. The finding of assemblages dominated by P. zoharyi in the open ocean is unusual because today similar assemblages are restricted to lagoonal settings. It is postulated that the highly saline mixed layer and the strong density gradient which characterized Arabian Sea hydrography after H6-H4 and the YD simulated a shallow seafloor, thereby enabling germination of cysts prior to sinking. The strong density gradient following cold stadials should have facilitated the rapid reestablishment of a pronounced OMZ during interstadials.	Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Fac Earth Sci, NL-3584 CD Utrecht, Netherlands	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Utrecht University; Utrecht University	Reichart, GJ (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Handelshafen 12,Bldg Co-12, D-27570 Bremerhaven, Germany.	greichart@awi-bremerhaven.de	Brinkhuis, Henk/B-4223-2009; Reichart, Gert-Jan/N-6308-2018	Brinkhuis, Henk/0000-0003-0253-6610; Reichart, Gert-Jan/0000-0002-7256-2243				ALTABET MA, 1995, NATURE, V373, P506, DOI 10.1038/373506a0; Altabet MA, 2002, NATURE, V415, P159, DOI 10.1038/415159a; BERGER WH, 1978, DEEP-SEA RES, V25, P447, DOI 10.1016/0146-6291(78)90552-0; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Cutler KB, 2003, EARTH PLANET SC LETT, V206, P253, DOI 10.1016/S0012-821X(02)01107-X; DANSGAARD W, 1993, NATURE, V364, P218, DOI 10.1038/364218a0; DEVILLIERS S, 1995, SCIENCE, V269, P1247, DOI 10.1126/science.269.5228.1247; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; GROOTES PM, 1993, NATURE, V366, P552, DOI 10.1038/366552a0; Jannink NT, 1998, DEEP-SEA RES PT I, V45, P1483, DOI 10.1016/S0967-0637(98)00027-2; KINSMAN DJJ, 1969, GEOCHIM COSMOCHIM AC, V33, P1, DOI 10.1016/0016-7037(69)90089-1; Mix AC, 2001, QUATERNARY SCI REV, V20, P627, DOI 10.1016/S0277-3791(00)00145-1; MORZADEC-KERFOURN M.T., 1983, CAHIERS MICROPALEONT, V1983, P15; NAQVI SWA, 1987, J MAR RES, V45, P1049, DOI 10.1357/002224087788327118; OLSON DB, 1993, DEEP-SEA RES PT II, V40, P673, DOI 10.1016/0967-0645(93)90051-N; Prins MA, 2000, MAR GEOL, V169, P327, DOI 10.1016/S0025-3227(00)00086-4; Reichart GJ, 2003, MAR MICROPALEONTOL, V49, P303, DOI 10.1016/S0377-8398(03)00050-1; Reichart GJ, 2002, GEOL SOC SPEC PUBL, V195, P407, DOI 10.1144/GSL.SP.2002.195.01.22; Reichart GJ, 1998, PALEOCEANOGRAPHY, V13, P607, DOI 10.1029/98PA02203; Reichart GJ, 2002, MAR GEOL, V185, P403, DOI 10.1016/S0025-3227(02)00184-6; SCHMITZ B, 1987, MAR GEOL, V76, P195, DOI 10.1016/0025-3227(87)90029-6; Schulz H, 1998, NATURE, V393, P54, DOI 10.1038/31750; Schulz H, 2002, QUATERNARY RES, V57, P22, DOI 10.1006/qres.2001.2291; SWALLOW JC, 1984, DEEP-SEA RES, V31, P639, DOI 10.1016/0198-0149(84)90032-3; van der Weijden CH, 1999, DEEP-SEA RES PT I, V46, P807, DOI 10.1016/S0967-0637(98)00093-4; Von Stackelberg U., 1972, METEOR FORSCHUNGS C, V9, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Weaver PPE, 1999, PALEOCEANOGRAPHY, V14, P336, DOI 10.1029/1999PA900009; WILLIAMS GL, 1998, LENTIN WILLIAMS INDE; WINGARD GL, 1995, OFR95628 US GEOL SUR; Wyrtki K., 1971, BIOL INDIAN OCEAN; Wyrtki K., 1973, ECOL STUD, V3, P18, DOI [DOI 10.1007/978-3-642-65468-8_3, DOI 10.1007/978-3-642-65468-83]; YOU Y, 1993, DEEP-SEA RES PT I, V40, P13, DOI 10.1016/0967-0637(93)90052-5	34	49	52	0	8	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0883-8305	1944-9186		PALEOCEANOGRAPHY	Paleoceanography	MAY 7	2004	19	2							PA2013	10.1029/2003PA000900	http://dx.doi.org/10.1029/2003PA000900			8	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	819SK		Bronze, Green Published			2025-03-11	WOS:000221335100001
J	Sangiorgi, F; Donders, TH				Sangiorgi, F; Donders, TH			Reconstructing 150 years of eutrophication in the north-western Adriatic Sea (Italy) using dinoflagellate cysts, pollen and spores	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						eutrophication; dinoflagellate cysts; pollen; sediment core; Adriatic Sea	INDUSTRIAL-POLLUTION; NORWEGIAN FJORD; LATE-HOLOCENE; INDICATORS; ASSEMBLAGES; BAY; APPEARANCE; ECOSYSTEM; SEDIMENTS; PLANKTON	Recent trends in the trophic conditions of the north-western Adriatic Sea have been evaluated using organic-walled dinoflagellate cysts (dinocysts), pollen and spores. Palynological analyses performed on a sediment core covering the period AD 1830-1990 have revealed a progressive increase in eutrophication beginning in the 20th century. The first signal of a change seems to occur earlier in the terrestrial ecosystem and later in the marine realm. Pollen data indicate that the source of enhanced nutrient loading to the North Adriatic Sea, which partly resulted from increased wetland reclamation and forest clearance, began at about AD 1910. The clear shift in the relative abundance of the dinocyst Lingulodinium machaerophorum at AD 1930 suggests an increase in eutrophication. Dinocyst assemblages point to stressful conditions from AD 1960, reaching a maximum at about AD 1978. Subsequently eutrophication levels decrease, although dinocyst diversity suggests that the ecosystem has not completely recovered. (C) 2004 Elsevier Ltd. All rights reserved.	Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, I-48100 Ravenna, Italy; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	University of Bologna; Utrecht University	Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, Via S Alberto 163, I-48100 Ravenna, Italy.	franci@ambra.unibo.it	Donders, Timme/J-5044-2012	Donders, Timme/0000-0003-4698-3463; Sangiorgi, Francesca/0000-0003-4233-6154				Acri Francesco, 2000, Bollettino del Museo Civico di Storia Naturale di Venezia, V50, P131; AFAGNA L, 1989, DUALISMO SVILUPPO NE, P281; Alberighi L., 1997, Biologia Marina Mediterranea, V4, P17; Andersen S. T., 1970, Danmarks geologiske Undersogelse, Kobenhavn (Ser. II), V96, P1; [Anonymous], 1992, Sci. 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Coast. Shelf Sci.	MAY	2004	60	1					69	79		10.1016/j.ecss.2003.12.001	http://dx.doi.org/10.1016/j.ecss.2003.12.001			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	820LR		Green Published			2025-03-11	WOS:000221391100007
J	Louwye, S; Head, MJ; De Schepper, S				Louwye, S; Head, MJ; De Schepper, S			Dinoflagellate cyst stratigraphy and palaeoecology of the Pliocene in northern Belgium southern North Sea Basin	GEOLOGICAL MAGAZINE			English	Article						palynology; dinoflagellate cysts; Pliocene; Belgium; North Sea	EASTERN ENGLAND; DEPOSITIONAL HISTORY; SINGA SECTION; ATLANTIC; MIOCENE; NEOGENE; BIOSTRATIGRAPHY; ASSEMBLAGES; ACRITARCHS; GENERA	Dinoflagellate cysts and other palynomorphs from the Pliocene Kattendijk and Lillo formations, exposed in two temporary outcrops in northern Belgium, provide new information on the biostratigraphic position and sequence stratigraphic interpretation of these units. Dinoflagellate cysts from the Kattendijk Formation indicate an age between about 5.0 Ma and 4.7-4.4 Ma (early Early Pliocene) in our sections, confirming a correlation with standard sequence 3.4 and implying a slightly greater age than the Ramsholt Member of the Coralline Crag Formation of eastern England. The unconformity at the base of the Kattendijk Formation was not seen, but presumably correlates with sequence boundary Me2 at 5.73 Ma. The overlying Lillo Formation is late Early Pliocene or early Late Pliocene (c. 4.2-2.6 Ma) in age, and the unconformity at its base may be correlated with sequence boundary Za2 at 4.04 Ma or Pial at 3.21 Ma. The Oorderen Sands and superjacent Kruisschans Sands members (Lillo Formation) are both part of the same depositional cycle. They were probably deposited before 2.74 Ma, and certainly before the onset of Northern Hemisphere cooling at c. 2.6 Ma. Evidence from dinoflagellate cysts indicates that both a shelly unit at the base of the Lillo Formation and the lower part of the overlying Oorderen Sands were deposited during a conspicuously cool climatic phase, with warmer temperatures returning during later deposition of the Oorderen Sands and Kruisschans Sands members. Many dinoflagellate cyst and acritarch species are reported here for the first time from the southern North Sea Basin. Selenopemphix conspicua (de Verteuil & Norris, 1992) stat. nov. is proposed.	Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; State Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium	University of Cambridge; Ghent University	Univ Cambridge, Dept Geog, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk	De Schepper, Stijn/A-2836-2011; Louwye, Stephen/D-3856-2012	De Schepper, Stijn/0000-0002-6934-0914; Louwye, Stephen/0000-0003-4814-4313				[Anonymous], NOVA HEDWIGIA; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; BERBEEK J, 1988, NW EUROPEAN TERTIARY, P267; BERGGREN WA, 1977, MAR MICROPALEONTOL, V2, P265, DOI 10.1016/0377-8398(77)90015-9; BERGGREN WA, 1973, NATURE, V243, P391, DOI 10.1038/243391a0; BERGGREN WA, 1995, GEOCHRONOLOGY TIME S, V54, P29; Blow W.H., 1979, CAINOZOIC GLOBIGERIN; Bukry D., 1975, Initial Rep Deep Sea Drilling Project, V32, P677, DOI 10.2973/dsdp.proc.32.124.1975; Bukry D., 1973, Initial Reports DSDP, V15, P685, DOI DOI 10.2973/DSDP.PROC.15.116.1973; CAMBRIDGE PG, 1977, B GEOLOGICAL SOC NOR, V29, P23; COGELS P., 1874, Annales de la Societe Malacologique de Belgique, V9, P7; COSTA LI, 1979, INITIAL REPORTS DEEP, V48, P513; Dale B., 1983, P69; de Heinzelin de Braucourt J, 1952, B SOC BELGE GEOLOGIE, V61, P106; de Heinzelin J., 1950, B I ROYAL SCI NATURE, V26, P1; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A., 1989, Proceedings of the Ocean Drilling Program Scientific results, V105, P401, DOI DOI 10.2973/0DP.PR0C.SR.105.134.1989; De Verteuil L., 1996, P OCEAN DRILLING PRO, V150, P439; De Verteuil L., 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs, P391; DEHEINZELIN J, 1955, B SOC BELG GEOL, V64, P463; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Doppert J.W.C., 1979, MEDEDELINGEN RIJKS G, V31, P1; DOPPERT JW, 1985, B GEOLOGICAL SOC NOR, V35, P47; DUMONT A, 1839, B ACAD ROY BELGIQUE, V6, P479; GAEMERS PAM, 1988, NW EUROPEAN TERTIARY, P379; GRAMANNF, 1988, NW EUROPEAN TERTIARY, P240; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; Harland R., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P531; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; HEAD M. 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J	Sun, XX; Choi, JK				Sun, XX; Choi, JK			Recovery and fate of three species of marine dinoflagellates after yellow clay flocculation	HYDROBIOLOGIA			English	Article						cyst; marine dinoflagellates; recovery; yellow clay	HARMFUL ALGAL BLOOMS; CYST FORMATION; RED-TIDE; TOXIC DINOFLAGELLATE; RESTING CYSTS; SCRIPPSIELLA; DINOPHYCEAE; GERMINATION; MANAGEMENT; SEXUALITY	The recovery and fate of three species of dinoflagellates, Alexandrium tamarense, Cochlodinium polykrikoides and Scrippsiella trochoidea, after having been sedimented by yellow clay, were investigated in the laboratory. The effect of burying period in yellow clay pellet and mixing on the recovery of settled algal cells were studied. The morphological changes of algal cells in yellow clay pellet were also tracked. Results showed that there was almost no recovery for A. tamarense and C. polykrikoides, and the cells decomposed after 2-3 days after visible changes in morphology and chloroplasts. There was some recovery for S. trochoidea. Moreover, S. trochoidea cysts were formed in clay pellet during the period of about 14 days, with the highest abundance of 87 000 cysts g(-1) clay and the incidence of cyst formation of 6.5%, which was considered as a potential threat for the further occurrence of algal blooms. S. trochoidea cysts were isolated from yellow clay and incubated to test their viability, and a germination ratio of more than 30% was obtained after incubation for 1 month. These results showed the species specificity of the mitigation effect of yellow clay. It is suggested that cautions be taken for some harmful species and thorough risk assessments be conducted before using this mitigation strategy in the field.	Inha Univ, Reg Res Ctr Coastal Environm Yellow Sea, Inchon 402751, South Korea; Inha Univ, Dept Oceanog, Inchon 402751, South Korea; Chinese Acad Sci, Inst Oceanol, Qingdao 266071, Peoples R China	Inha University; Inha University; Chinese Academy of Sciences; Institute of Oceanology, CAS	Choi, JK (通讯作者)，Inha Univ, Reg Res Ctr Coastal Environm Yellow Sea, Inchon 402751, South Korea.	xiaoxiasun@hotmail.com; jkchoi@inha.ac.kr						Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1978, J PHYCOL, V14, P124; ARCHAMBAULT MC, 2002, 10 INT C HARMF ALG F, P15; BRAVO I, 1998, HARMFUL ALGAE, P356; Burkholder JM, 1998, ECOL APPL, V8, pS37; Cahoon AB, 1999, NATO ASI 3 HIGH TECH, V64, P195; CEMBELLA AD, 1990, TOXIC MARINE PHYTOPLANKTON, P333; Choi Hee Gu, 1998, Journal of the Korean Fisheries Society, V31, P109; CHOI HG, 1999, B NATL FISH RES DEV, V57, P105; EWERT L, 2002, 10 INT C HARMF ALG F, P87; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hallin M, 1997, INST MATH S, V31, P47; Hill Walter, 1996, P121, DOI 10.1016/B978-012668450-6/50034-5; Hurst J.W., 1985, P427; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; LEWIS MA, 2002, 10 INT C HARMF ALG F, P169; LIRDWITAYAPRASIT T, 1990, TOXIC MARINE PHYTOPLANKTON, P294; Matsuoka K., 2000, Technical Guide for Modern Dinoflagellate Cyst Study, P6; Montresor M, 2003, J EXP MAR BIOL ECOL, V287, P209, DOI 10.1016/S0022-0981(02)00549-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Na G.-H., 1996, J. Aquacult., V9, P239; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; Park Young-Tae, 1998, Journal of the Korean Fisheries Society, V31, P920; Peterson Christopher G., 1996, P375, DOI 10.1016/B978-012668450-6/50042-4; POWER ME, 1990, ECOLOGY, V71, P897, DOI 10.2307/1937361; Qin Xiaoming, 1997, Oceanologia et Limnologia Sinica, V28, P594; Sengco MR, 2001, MAR ECOL PROG SER, V210, P41, DOI 10.3354/meps210041; SENGCO MR, 2002, 10 INT C HARMF ALG F, P256; Shirota A., 1989, International Journal of Aquaculture and Fisheries Technology, V1, P25; Shirota A., 1989, International Journal of Aquaculture and Fisheries Technology, V1, P195; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Shumway SE, 2003, HARMFUL ALGAE, V2, P1, DOI 10.1016/S1568-9883(03)00002-7; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WHANG JY, 2000, P 3 INT S HARMF ALG, P28; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Yentsch C.M., 1979, P127; Yu Z., 1994, J NAT DISASTERS, P105; Yu Z.M., 1995, Chin. J. Oceanol. Limnol., V13, P62, DOI [10.1007/BF02845350, DOI 10.1007/BF02845350]; Yu Zhi-Ming, 1994, Chinese Journal of Oceanology and Limnology, V12, P193; Yu Zhi-Ming, 1994, Chinese Journal of Oceanology and Limnology, V12, P316; Zhiming Y, 1998, OCEANOLOGIA LIMNOLOG, V29, P47; Zingone A, 2000, OCEAN COAST MANAGE, V43, P725, DOI 10.1016/S0964-5691(00)00056-9	51	21	21	1	15	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0018-8158			HYDROBIOLOGIA	Hydrobiologia	MAY	2004	519	1-3					153	165		10.1023/B:HYDR.0000026502.05971.bf	http://dx.doi.org/10.1023/B:HYDR.0000026502.05971.bf			13	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	817UT					2025-03-11	WOS:000221203100015
J	Khowaja-Ateequzzaman; Garg, R				Khowaja-Ateequzzaman; Garg, R			Re-interpretation of the archaeopyle type in the dinoflagellate cyst <i>Leberidocysta ? scabrata</i> (Jain & Taugourdeau-Lantz, 1973) Stover & Evitt, 1978 and its taxonomic reallocation	JOURNAL OF MICROPALAEONTOLOGY			English	Article							CAUVERY BASIN; DALMIAPURAM FORMATION; INDIA; DISTRICT; TRICHINOPOLY	The holotype and some additional specimens from the type material of the dinoflagellate cyst species Leberidocysta? scabrata (Jain & Taugourdeau-Lantz, 1973) Stover & Evitt, 1978, described from the Grey Shale Member (Lower Albian), Dalmiapuram Formation, Cauvery Basin, southern India are re-investigated. The diagnosis is emended and the species is reallocated to the genus Ovoidinium Davey, 1970, emend. Lentin & Williams, 1976.	Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	khowaja_ateeq@yahoo.com						[Anonymous], PALAEONTOLOGY; [Anonymous], [No title captured]; [Anonymous], 1978, GEOLOGICAL SCI; Banerji R. K., 1973, J PALAEONTOLOGICAL S, V17, P7; BANERJI RK, 1982, J GEOL SOC INDIA, V23, P450; BANERJI RK, 1972, J PALAEONTOLOGICAL S, V15, P32; Bhatia SB., 1969, B INDIAN GEOLOG ASSO, V2, P105; Blanford H. F., 1862, Memoirs of the Geological Survey of India, V4, P1; BUJAK JP, 1983, AM ASS STRATIGRAPHIC, V13; CHIPLONKAR GW, 1975, CURR SCI INDIA, V44, P123; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; EVITT WR, 1967, STANFORD U PUBLICATI, V10; HELENES J, 1983, MICROPALEONTOLOGY, V29, P255, DOI 10.2307/1485733; JAFAR SA, 1989, CURR SCI INDIA, V58, P358; JAIN K P, 1973, Geophytology, V3, P52; JAIN KP, 1969, CURR SCI INDIA, V38, P549; Jain KP., 1977, PALEOBOTANIST, V24, P170; Kale A.S., 1992, Memorie di Scienze Geologiche, VXLIII, P89; Lentin J.K., 1985, CAN TECH REP HYDROG, V60, P1; Lentin J.K., 1989, American Association of Stratigraphic Palynologists, Contributions Series, V20; LENTIN JK, 1976, BIR7516 BEDF I OC RE, P1; Mehrotra N.C., 1984, Journal of Micropalaeontology, V3, P43; NORVICK M. S., 1976, AUSTR BUREAU MINERAL, V151, P21; Phansalkar V.G., 1983, Palaeontological Society of India Special Publication, P120; RAMANATHAN S, 1968, MEMOIRS GEOLOGICAL S, V2, P152; RAMASAMY S, 1991, J GEOL SOC INDIA, V37, P577; RAO VR, 1971, ANN GEOL DEP A M U A, V5, P353; SINGH C, 1971, RES COUNCIL ALBERTA, V28, P301; SUBBARAMAN JV, 1968, MEMOIRS GEOLOGICAL S, V2, P92; Sundaram R, 2001, CRETACEOUS RES, V22, P743, DOI 10.1006/cres.2001.0287; Sundaram R., 1986, RECORD GEOLOG SURV I, V115, P9; Sundaram R., 1979, Geological Survey of India, Miscellaneous Publications, V45, P111; Tewari Archana, 1996, P789; VENKATACHALAPATHY R, 1995, CRETACEOUS RES, V16, P415, DOI 10.1006/cres.1995.1029; Wilson GT, 1980, 92 NZ GEOL SURV	37	0	0	0	0	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	MAY	2004	23		1				11	14		10.1144/jm.23.1.11	http://dx.doi.org/10.1144/jm.23.1.11			4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	826JN		hybrid			2025-03-11	WOS:000221825500003
J	Dodsworth, P				Dodsworth, P			The distribution of dinoflagellate cysts across a Late Cenomanian carbon isotope (δ<SUP>13</SUP>C) anomaly in the Pulawy borehole, central Poland	JOURNAL OF MICROPALAEONTOLOGY			English	Article							TURONIAN BOUNDARY	Late Cenomanian dinoflagellate cyst assemblages in the Pulawy borehole, central Poland, exhibit similarities with those from west European and North American localities. A comparable change in assemblage composition around the base of a positive carbon isotope (delta(13)C) anomaly occurs in all three areas.	Univ Sheffield, Palynol Res Facil, Sheffield S3 7HF, S Yorkshire, England	University of Sheffield	Dodsworth, P (通讯作者)，Ichron Ltd, Unit 5, Gadbrook Business Ctr, Dalby Court, Northwich CW9 7TN, Cheshire, England.	dodsworth@ichron.com		Dodsworth, Paul/0000-0002-8895-9472				DAVEY RJ, 1976, REV PALAEOBOT PALYNO, V22, P307, DOI 10.1016/0034-6667(76)90028-2; Dodsworth P, 2000, J MICROPALAEONTOL, V19, P69, DOI 10.1144/jm.19.1.69; Hart MB, 1996, GEOL SOC SP, P265, DOI 10.1144/GSL.SP.1996.001.01.20; MARSHALL KL, 1988, REV PALAEOBOT PALYNO, V54, P85, DOI 10.1016/0034-6667(88)90006-1; PERYT D, 1993, PALAEOGEOGR PALAEOCL, V104, P185, DOI 10.1016/0031-0182(93)90130-B; PERYT D, 1994, TERRA NOVA, V6, P158, DOI 10.1111/j.1365-3121.1994.tb00649.x; SCHLANGER S O, 1976, Geologie en Mijnbouw, V55, P179; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34	8	7	8	0	2	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	MAY	2004	23		1				77	80		10.1144/jm.23.1.77	http://dx.doi.org/10.1144/jm.23.1.77			4	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	826JN		hybrid			2025-03-11	WOS:000221825500009
J	Streng, M; Hildebrand-Habel, T; Willems, H				Streng, M; Hildebrand-Habel, T; Willems, H			A proposed classification of archeopyle types in calcareous dinoflagellate cysts	JOURNAL OF PALEONTOLOGY			English	Review							SOUTH ATLANTIC-OCEAN; SEA DRILLING PROJECT; RIO-GRANDE RISE; DSDP SITE 357; SP-NOV; MEDITERRANEAN-SEA; MARINE DINOFLAGELLATE; THECA RELATIONSHIPS; SURFACE SEDIMENTS; LATE QUATERNARY	The phylogenetic significance of archeopyles in calcareous dinoflagellates cysts has been evaluated, and a classification model is developed that focuses on the archeopyle categories and types established for organic-walled dinoflagellates by Evitt (1967, 1985). Several of Evitt's archeopyle categories are presently recognized within the calcareous dinoflagellate cysts: apical, intercalary, and combination archeopyles, which are here subdivided into eight archeopyle types and several variations. Archeopyles that cannot be assigned to a distinct type, and those with outlines that do not allow an accurate interpretation, are together placed in a separate category: miscellaneous archeopyles. The stratigraphic distribution of the different archeopyle types reveals a phylogenetic trend characterized by an increase of the number of plates involved in archeopyle formation. The first calcareous dinotlagellate cysts to appear in the late Triassic have a monoplacoid apical archeopyle. The first taxa that show an archeopyle involving more than one plate are from the Early Cretaceous, with the first triplacoid apical archeopyle appearing at the Berriasian/Valanginian boundary. This is followed by the first combination archeopyle, which includes six plates, in the middle Aptian. Epitractal archeopyles originated no earlier than the early Oligocene. At the beginning of the Paleogene, species with a combination archeopyle increased in abundance, progressively replacing species possessing an apical archeopyle that dominated during the Mesozoic. Newly described species are: Calciodinellum clamosum, accommodating the two subspecies Calciodinellum clamosum subsp. clamosum Autonym, and Calciodinellum clamosum subsp. latum; Calciodinellum kerguelense; Fuettererella belliata; and Pernambugia? patata. New combinations are: Cervisiella oper-culata (Bramlette and Martini, 1964); Praecalcigonellum sulcatum (Keupp, 1979a); and Praecalcigonellum dolium (Keupp, 1979b). Because of the new interpretation of their archeopyles we emend the following genera: Cervisiella Hildebrand-Habel, Willems, and Versteegh, 1999; Echinodinella Keupp, 1980; Fuettererella Kohring, 1993a; and Pernambugia Janofske and Karwath in Karwath (2000). The species Orthopithonella? minuta and Pirumella johnstonei, which have been previously synonymized with Fuettererella deflandrei, are retained as independent taxa.	Uppsala Univ, Inst Geoventenskaper, S-75236 Uppsala, Sweden; Univ Oslo, Inst Geol, N-0316 Oslo, Norway; Univ Bremen, FB Geowissensch 5, D-28334 Bremen, Germany	Uppsala University; University of Oslo; University of Bremen	Streng, M (通讯作者)，Uppsala Univ, Inst Geoventenskaper, Norbyvagen 22, S-75236 Uppsala, Sweden.	michael.streng@geo.uu.se	Hildebrand-Habel, Tania/F-3590-2011					AKSELMAN R, 1990, MAR MICROPALEONTOL, V16, P169, DOI 10.1016/0377-8398(90)90002-4; [Anonymous], CONTRIBUTIONS SERIES; [Anonymous], REV MICROPALEONTOL; [Anonymous], 1978, DEEP SEA DRILL PROJ; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1996, Palynology: principles and applications; Bajraktarevic Z., 1983, Geoloski Vjesnik (Zagreb), V36, P9; Balech E., 1967, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nat (Hidrologia), V2, P77; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; BALECH E, 1990, HELGOLANDER MEERESUN, V44, P387, DOI 10.1007/BF02365475; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BERGGREN WA, 1985, GEOL SOC AM BULL, V96, P1407, DOI 10.1130/0016-7606(1985)96<1407:CG>2.0.CO;2; BERGGREN WA, 1985, MEMOIRS GEOLOGICAL S, V10, P147; Bolli H.M., 1974, Initial Rep Deep Sea Drilling Project, V27, P843; Bolli H.M., 1978, Initial Reports of the Deep Sea Drilling Project, V44, P911; Bolli H.M., 1980, Initial Reports of the Deep Sea Drilling Project, V50, P525; BORZA K, 1972, Geologicky Zbornik, V23, P139; BRALOWER TJ, 1991, MAR MICROPALEONTOL, V17, P119, DOI 10.1016/0377-8398(91)90025-2; BRAMLETTE M. 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J	Köthe, A				Köthe, A			Dinocyst investigation of Early Miocene glauconitic sands in the clay pit OLFRY/Vechta (Lower Saxony)	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-MONATSHEFTE			German	Article								A glauconitic layer which discontinuously overlies the Rupel Clay Formation was investigated on organic walled dinoflagellate cysts (dinocysts) in the clay pit OLFRY/Vechta. The uppermost part of the exposed Rupel Clay Formation is dated as Early Oligocene (Rupelian, D14 na). A phosphorite nodule from 4 cm above the base of the glauconitic layer and the glauconitic layer itself are dated as Early Miocene (zone D16 = DN2). The hiatus in between the Rupel Clay Formation and the glauconitic layer was at least 8.5 Ma. Reworking and bioturbation seriously complicated the zonation. The dinocyst assemblages indicate a shallow marine environment throughout the investigated sediments. Only the salinity seems to vary: reduced salinity is indicated in the Rupel Clay Formation, the phosphorite nodule represents normal salinity and the glauconitic sand increased salinity.	Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany		Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany.	angelika-koethe@web.de						Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; DANIELS CH, 1993, B SOC BELG GEOL, V102, P79; de Verteuil Laurent, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P129; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Gramann F., 1980, GEOLOGISCHES JB A, V54, P57; GRAMANN F, 1990, NLFB ARCHIV NR PB, P3215; GRIPP K, 1941, SCHR WIRTSCHAFTSWISS, V3, pS500; HARDENBOL J, 1998, SOC SED GEOL SPEC PU, V60, P8; HENJESKUNST F, 1993, UNPUB BGR BERICH ARC, P3215; Jaramillo CA, 1999, PALAEOGEOGR PALAEOCL, V145, P259, DOI 10.1016/S0031-0182(98)00126-6; KOTHE A, 1989, UNPUB BGR ARCHIV NR; KOTHE A, 1990, UNPUB BGR ARCHIV NR, P3215; KOTHE A, 1989, BGR ARCHIV NR PA, P3215; KREUZER H, 1980, GEOL JB, V54, P61; VONDANIELS CH, 1984, UNPUB NLFB BERICHT A, P3215; Williams Graham L., 1998, AASP Contributions Series, V34, P1; 1991, UNPUB BGR ARCHIV NR, P3215; 1990, UNPUB BGR BERICHT AR, P3215; 1990, GEOL JB A, V118, P3; UNPUB REV PALEOBIOL	20	0	0	0	0	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0028-3630			NEUES JAHRB GEOL P-M	Neues Jahrb. Geol. Palaontol.-Monatsh.	MAY	2004		5					257	277						21	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	827DD					2025-03-11	WOS:000221878000001
J	Dupont, LM; Kim, JH; Schneider, RR; Shi, N				Dupont, LM; Kim, JH; Schneider, RR; Shi, N			Southwest African climate independent of Atlantic sea surface temperatures during the Younger	QUATERNARY RESEARCH			English	Article						pollen; dinoflagellate cysts; alkenones; SST; deglaciation; southwestern Africa	LAST GLACIAL MAXIMUM; LATE QUATERNARY; SOUTHERN-AFRICA; LATE PLEISTOCENE; GREENLAND; POLLEN; VEGETATION; CAPE; SEDIMENTS; RECORDS	To investigate land-sea interactions during deglaciation, we compared proxies for continental (pollen percentages and accumulation rates) and marine conditions (dinoflagellate cyst percentages and alkenone-derived sea surface temperatures). The proxies were from published data from an AMS-radiocarbon-dated sedimentary record of core GeoB 1023-5 encompassing the past 21,000 years. The site is located at ca. 2000 m water depth just north of the Walvis Ridge and in the vicinity of the Cunene River mouth. We inter that the parallelism between increasing sea surface temperatures and a southward shift of the savanna Occurred only during the earliest part of the deglaciation. After the Antarctic Cold Reversal, southeast Atlantic sea surface temperatures no longer influenced the vegetation development in the Kalahari. Stronger trade winds during the Antarctic Cold Reversal and the Younger Dryas period probably caused increased upwelling off the coast of Angola. A southward shift of the Atlantic anti-cyclone could have resulted in both stronger trade winds and reduced impact of the Westerlies on the climate of southwestern Africa. (C) 2004 University of Washington. All rights reserved.	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Res.	MAY	2004	61	3					318	324		10.1016/j.yqres.2004.02.005	http://dx.doi.org/10.1016/j.yqres.2004.02.005			7	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	823BV					2025-03-11	WOS:000221585600008
