﻿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	Dybkjær, K				Dybkjær, K			Morphological and abundance variations in <i>Homotryblium</i>-cyst assemblages related to depositional environments;: uppermost Oligocene-Lower Miocene, Jylland, Denmark	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Denmark; Upper Oligocene-Lower Miocene; biostratigraphy; palynology; palaoeecology; dinoflagellate cysts; Homotryblium	DINOFLAGELLATE CYSTS; NORTH; SEDIMENTS; SALINITY; PLIOCENE; GERMANY; EOCENE; AREA	Abundant occurrences of Homotryblium dinoflagellate cysts have been interpreted as reflecting deposition in near-shore, marginal marine areas, either in hypersaline or low-salinity environments. It has also been suggested that the process length of Homotryblium cysts is related to proximity to the coast. The present study provides new insights in the ecology of Homotryblium and adds important information about the use of the morphological variations of Homotryblium cysts for environmental reconstructions. It presents an example where Homotryblium cysts show high relative abundances in a low-salinity, partly restricted marine depositional environment. Four different species of Homotryblium were recorded. Homotryblium? additense is proposed as a new species. The regional palaeogeographic distribution of the four species: H.? additense, Homotryblium vallum, Homotryblium plectilum and Homotryblium tenuispinosum, shows a distinct depositional proximal-distal distribution pattern. H.? additense occurs only in a narrow stratigraphic interval in the most proximal part of the study area. H. vallum only occurs sporadically, mainly in the proximal parts of the study area. H. plectilum dominates the proximal areas while H. tenuispinosum dominates the more distal areas. Variations in abundance and cyst-type also seem to respond to systems tracts, sequence boundaries and flooding surfaces. The observed distributional patterns of Homotryblium species strongly indicate a response to the salinity of the depositional environment. It is further suggested that at least some of the recorded species of Homotryblium originated from the same motile dinoflagellate species, producing cysts of different morphology in response to variations in salinity, a phenomenon known from extant dino flagellates. (C) 2004 Elsevier B.V. All rights reserved.	GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018					[Anonymous], 9210 GEOL SURV CAN; 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; Bujak J. 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E., 1977, AM ASS STRATIGRAPHIC, V5A, P66; Van Mourik CA, 2001, GEOL SOC SPEC PUBL, V183, P225, DOI 10.1144/GSL.SP.2001.183.01.11; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wall D., 1973, Geoscience Man, V7, P95; Williams D.B., 1971, MICROPALAEONTOLOGY O, P91; Williams G.L., 1977, Oceanic Micropalaeontology, V2, P1231; WILLIAMS GL, 1977, MAR MICROPALEONTOL, V2, P223, DOI 10.1016/0377-8398(77)90012-3; Zevenboom D., 1995, THESIS U UTRECHT NET; Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	61	46	51	0	1	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	APR 13	2004	206	1-2					41	58		10.1016/j.palaeo.2003.12.021	http://dx.doi.org/10.1016/j.palaeo.2003.12.021			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	811IB					2025-03-11	WOS:000220764500003
J	Toth, GB; Norén, F; Selander, E; Pavia, H				Toth, GB; Norén, F; Selander, E; Pavia, H			Marine dinoflagellates show induced life-history shifts to escape parasite infection in response to water-borne signals	PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES			English	Article						dinoflagellate; induced resistance; parasite; water-borne signal	DEFENSE; HERBIVORY; PLANTS; DINOPHYCEAE; GROWTH	Many dinoflagellate species form dormant resting cysts as a part of their life cycle, and in some freshwater species, hatching of these cysts can be delayed by the presence of water-borne signals from grazing zooplankton. Some marine dinoflagellates can form temporary cysts, which may function to resist unfavourable short-term environmental conditions. We investigated whether the marine dinoflagellate Alexandrium ostenfeldii is able to induce an increased resistance to the parasitic flagellate Parvilucifera infectans by forming temporary cysts. We performed several laboratory experiments where dinoflagellates were exposed either to direct contact with parasites or to filtered water from cultures of parasite-infected conspecifics (parasite-derived signals). Infection by P. infectans is lethal to motile A. ostenfeldii cells, but temporary cysts were more resistant to parasite infection. Furthermore, A. ostenfeldii induced a shift in life-history stage (from motile cells to temporary cysts) when exposed to parasite-derived water-borne signals. The response was relaxed within a couple of hours, indicating that A. ostenfeldii may use this behaviour as a short-term escape mechanism to avoid parasite infection. The results suggest that intraspecies chemical communication evoked by biotic interactions can be an important mechanism controlling life-history shifts in marine dinoflagellates, which may have implications for the development of toxic algal blooms.	Tjarno Marine Biol Lab, SE-45296 Stromstad, Sweden; Kristineberg Marine Res Stn, SE-45034 Fiskebackskil, Sweden		Toth, GB (通讯作者)，Tjarno Marine Biol Lab, SE-45296 Stromstad, Sweden.	gunilla.toth@tmbl.gu.se	Toth, Gunilla/E-8737-2013; Pavia, Henrik/G-2764-2013	Selander, Erik/0000-0002-2579-0841; Toth, Gunilla/0000-0002-1225-7773				ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; Arimura G, 2000, NATURE, V406, P512, DOI 10.1038/35020072; Arnold TM, 2001, J PHYCOL, V37, P1026, DOI 10.1046/j.1529-8817.2001.01130.x; Chivers DP, 1998, ECOSCIENCE, V5, P338, DOI 10.1080/11956860.1998.11682471; Crespi BJ, 2001, TRENDS ECOL EVOL, V16, P178, DOI 10.1016/S0169-5347(01)02115-2; Dolch R, 2000, OECOLOGIA, V125, P504, DOI 10.1007/s004420000482; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Erard-Le Denn E, 2000, ESTUAR COAST SHELF S, V50, P109, DOI 10.1006/ecss.1999.0537; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Hansson LA, 1996, P ROY SOC B-BIOL SCI, V263, P1241, DOI 10.1098/rspb.1996.0182; HERMS DA, 1992, Q REV BIOL, V67, P283, DOI 10.1086/417659; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Karban R, 2000, OECOLOGIA, V125, P66, DOI 10.1007/PL00008892; Karban R., 1997, Induced Responses to Herbivory, V1; Kats LB, 1998, ECOSCIENCE, V5, P361, DOI 10.1080/11956860.1998.11682468; Lürling M, 2001, PROTIST, V152, P7, DOI 10.1078/1434-4610-00038; Miller MB, 2001, ANNU REV MICROBIOL, V55, P165, DOI 10.1146/annurev.micro.55.1.165; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; Potin P, 1999, CURR OPIN MICROBIOL, V2, P276, DOI 10.1016/S1369-5274(99)80048-4; Potin P, 2002, CURR OPIN PLANT BIOL, V5, P308, DOI 10.1016/S1369-5266(02)00273-X; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Shapiro JA, 1998, ANNU REV MICROBIOL, V52, P81, DOI 10.1146/annurev.micro.52.1.81; Tillmann U, 2002, MAR ECOL PROG SER, V230, P47, DOI 10.3354/meps230047; Tollrian R., 1999, ECOLOGY EVOLUTION IN; Toth GB, 2000, P NATL ACAD SCI USA, V97, P14418, DOI 10.1073/pnas.250226997; Underwood AJ., 1996, Experiments in Ecology: Their Logical Design and Interpretation Using Analysis of Variance	26	55	57	0	27	ROYAL SOC	LONDON	6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND	0962-8452			P ROY SOC B-BIOL SCI	Proc. R. Soc. B-Biol. Sci.	APR 7	2004	271	1540					733	738		10.1098/rspb.2003.2654	http://dx.doi.org/10.1098/rspb.2003.2654			6	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	808JN	15209107	Green Published			2025-03-11	WOS:000220565500011
J	Fistarol, GO; Legrand, C; Selander, E; Hummert, C; Stolte, W; Granéli, E				Fistarol, GO; Legrand, C; Selander, E; Hummert, C; Stolte, W; Granéli, E			Allelopathy in <i>Alexandrium</i> spp.:: effect on a natural plankton community and on algal monocultures	AQUATIC MICROBIAL ECOLOGY			English	Article						Alexandrium; allelopathy; natural community; algal monocultures; cysts; paralytic shellfish poison; PSP method; PSP toxins	CHRYSOCHROMULINA-POLYLEPIS; BACTERIAL ABUNDANCE; SHORT-TERM; DINOFLAGELLATE; PHYTOPLANKTON; GROWTH; BLOOM; MECHANISMS; TOXICITY; SUBSTANCES	We studied allelopathy in the dinoflagellate genus Alexandrium by testing the effect of A. tamarense on a natural plankton community from Hopavagen Bay, Trondheimsfjord, Norway, and the effect of toxic and non-toxic strains of A. tamarense and a toxic strain of A. minutum on algal monocultures. Also, a possible relation between the allelopathic effect and the production of paralytic shellfish poison (PSP) toxin was investigated. A. tamarense affected the whole phytoplankton community by decreasing the growth rate and changing the community structure (relative abundance of each species, dominant species). A negative effect of A. tamarense was also observed on ciliates, but not on bacteria numbers, In the bioassay with algal monocultures, the diatom Thalassiosira weissflogii and the cryptophyte Rhodomonas sp. were exposed to the filtrate of Alexandrium spp. All tested Alexandrium strains negatively affected T weissflogii and Rhodomonas sp. cultures, independent of whether PSP toxins were produced. The compounds released by Alexandrium caused lysis of natural and cultured algal cells, suggesting that the allelopathic effect may be connected with previously described ichthyotoxic and haemolytic properties of Alexandrium. Furthermore, the observation that several components of the plankton community were affected by compounds released by A. tamarense emphasizes the importance of allelopathy for the ecology of this species.	Univ Kalmar, Dept Biol & Environm Sci, Marine Sci Div, S-39231 Kalmar, Sweden; Univ Gothenburg, Tjarno Marine Biol Lab, S-45296 Stromstad, Sweden; Labor WEJ, D-21107 Hamburg, Germany	University of Kalmar; Linnaeus University; University of Gothenburg	Univ Kalmar, Dept Biol & Environm Sci, Marine Sci Div, S-39231 Kalmar, Sweden.	giovana.salomon@hik.se	Graneli, Edna/F-5936-2015	Selander, Erik/0000-0002-2579-0841				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; ARZUL G, 1993, DEV MAR BIO, V3, P719; Bagoien E, 1996, MAR BIOL, V126, P361, DOI 10.1007/BF00354618; BLANCO J, 1988, AQUACULTURE, V68, P289, DOI 10.1016/0044-8486(88)90242-6; CANNON JA, 1990, TOXIC MARINE PHYTOPLANKTON, P110; Carlsson P, 2001, LIMNOL OCEANOGR, V46, P108, DOI 10.4319/lo.2001.46.1.0108; CHUAYCHAN S, 1998, THESIS NORWEGIAN U S; delGiorgio P, 1996, LIMNOL OCEANOGR, V41, P783, DOI 10.4319/lo.1996.41.4.0783; Edvardsen B., 1998, NATO ASI Series Series G Ecological Sciences, V41, P193; Einhellig FA, 2002, ALLELOPATHY: FROM MOLECULES TO ECOSYSTEMS, P1; Fistarol GO, 2003, MAR ECOL PROG SER, V255, P115, DOI 10.3354/meps255115; Frangóulos M, 2000, MAR ECOL PROG SER, V203, P161, DOI 10.3354/meps203161; Granéli E, 2003, HARMFUL ALGAE, V2, P135, DOI 10.1016/S1568-9883(03)00006-4; GROSS EM, 1991, J PHYCOL, V27, P686, DOI 10.1111/j.0022-3646.1991.00686.x; Guillard R. 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Microb. Ecol.	APR 1	2004	35	1					45	56		10.3354/ame035045	http://dx.doi.org/10.3354/ame035045			12	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	815DL		Bronze			2025-03-11	WOS:000221022900004
J	Trop, JM; Ridgway, KD; Sweet, AR				Trop, JM; Ridgway, KD; Sweet, AR			Stratigraphy, palynology, and provenance of the Colorado Creek basin, Alaska, USA: Oligocene transpressional tectonics along the central Denali fault system	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							THRUST-TOP BASIN; YUKON-TERRITORY; DEPOSITIONAL SYSTEMS; CANTWELL BASIN; SUTURE ZONE; SLIP; DISPLACEMENT; TRANSITION; EARTHQUAKE; KINEMATICS	New sedimentologic, biostratigraphic, and compositional data from a 415-m-thick section of siliciclastic and volcanic strata document Oligocene synthrusting sedimentation south of the McKinley segment of the Denali fault system. Strata of the Colorado Creek basin are presently exposed on the south side of the central Alaska Range in the footwalls of north-dipping thrust faults. New measured sections define a three-part stratigraphy. Lowermost strata consist of a similar to30-m-thick unit of marine sandstone and mudstone that contain Late Cretaceous dinoflagellate taxa. The middle unit consists of similar to330 m of conglomerate, sandstone, and mudstone interpreted as braided stream and floodplain deposits. This middle unit contains early Oligocene pollen and spore assemblages. The upper unit is 55 m thick and contains lava flows, tuff, and pumice interpreted as the product of subaerial volcanic eruptions. Direct age data are lacking from the upper unit. Compositional data from the middle unit indicate that detritus was derived from sedimentary and igneous source terranes exposed on both the north and south side of the McKinley fault. Matching source lithologies north of the McKinley fault with conglomerate clast types in the Colorado Creek basin implies 30-33 km of maximum post-early Oligocene dextral displacement along the fault. We interpret the Oligocene strata of the Colorado Creek basin as a product of transpressional deformation that produced north-dipping thrust faults associated with strike-slip displacement on the central Denali fault. Our data from the Colorado Creek basin, in combination with previous studies, document a major episode of middle Eocene - late Oligocene synorogenic sedimentation along the Denali fault from British Columbia to southwestern Alaska.	Bucknell Univ, Dept Geol, Lewisburg, PA 17837 USA; Purdue Univ, Dept Earth & Atmospher Sci, W Lafayette, IN 47907 USA; Geol Survey Canada, Calgary, AB T2L 2A7, Canada	Bucknell University; Purdue University System; Purdue University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Bucknell Univ, Dept Geol, Lewisburg, PA 17837 USA.	jtrop@bucknell.edu						[Anonymous], 1963, Atlas der Mittel- und Jungtertiaren dispersen Sporen- und Pollen - sowie der Mikroplanktonformen des nordlichen Mitteleuropas 2; [Anonymous], 2002, US GEOLOGICAL SURVEY; [Anonymous], 1988, VOLCANIC SUCCESSIONS, DOI DOI 10.1016/0377-0273(89)90099-1; [Anonymous], 1974, TECTONICS SEDIMENTAT; Boothroyd J.C., 1975, GLACIOFLUVIAL GLACIO, P193; Christie-Blick N., 1985, STRIKE SLIP DEFORMAT, V37, P1, DOI [10.2110/pec.85.37.0001, DOI 10.2110/PEC.85.37.0001]; COLE RB, 1993, J SEDIMENT PETROL, V63, P152; Cole RB, 1999, TECTONICS, V18, P1224, DOI 10.1029/1999TC900033; COLE RB, 1999, GEOL SOC AM ABSTR, V31, P46; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; CSEJTEY B, 1982, J GEOPHYS RES, V87, P3741, DOI 10.1029/JB087iB05p03741; CSEJTEY B, 1994, US GEOLOGICAL SURVEY, P157; CSEJTEY B, 1998, EOS T AGU S, V79, pF876; CSEJTEY B, 1984, US GEOLOGICAL SURVEY, P77; DICKEY DB, 1984, SEDIMENT GEOL, V38, P443, DOI 10.1016/0037-0738(84)90089-7; DODDS CJ, 1992, GEOL SURV CAN GEOLOG, V4, P656; Eberhart-Phillips D, 2003, SCIENCE, V300, P1113, DOI 10.1126/science.1082703; EISBACHER GH, 1976, CAN J EARTH SCI, V13, P1495, DOI 10.1139/e76-157; EISBACHER GH, 1977, GEOLOGICAL SURVEY B, V771, P319; Fischer R.V., 1984, Pyroclastic Rocks; Frederiksen N., 1983, Contributions Series, V12, P32; FREDERIKSEN NO, 1980, 1084 US GEOL SURV; GILBERT WG, 1981, 153 AL DIV GEOL GEOP; GRANTZ A, 1966, THESIS STANFORD U PA; HARDING TP, 1974, AAPG BULL, V58, P1290; Helby R., 1987, PALYNOLOGICAL ZONATI; HICKMAN RG, 1977, GEOL SOC AM BULL, V88, P1217, DOI 10.1130/0016-7606(1977)88<1217:SGOTNR>2.0.CO;2; INGERSOLL RV, 1984, J SEDIMENT PETROL, V54, P103; IOANNIDES NS, 1986, GEOLGICAL SURVEY CAN, V371; KRUTZSCH W, 1962, GEOLOGIE, V11, P265; LANPHERE MA, 1978, CAN J EARTH SCI, V15, P817, DOI 10.1139/e78-086; Loeblich A.R., 1966, STUDIES TROPICAL OCE, V3; Lowey GW, 1998, B CAN PETROL GEOL, V46, P379; MARTIN HA, 1966, CAN J BOTANY, V44, P171, DOI 10.1139/b66-025; McIntyre D.J., 1991, TERTIARY FOSSIL FORE, P83, DOI DOI 10.4095/131949; Nichols DJ., 1973, Geoscience and Man, V7, P103, DOI DOI 10.1080/00721395.1973.9989740; Nokleberg W.J., 1994, The Geology of Alaska, P311, DOI DOI 10.1130/DNAG-GNA-G1.311; NOKLEBERG WJ, 1985, GEOL SOC AM BULL, V96, P1251, DOI 10.1130/0016-7606(1985)96<1251:OATEOT>2.0.CO;2; Norris G., 1986, GEOLOGICAL SURVEY CA, V340; NORRIS G, 1997, GEOLOGICAL SURVEY CA, V523; ONEILL JM, IN PRESS US GEOLOGIC; PAGE R, 1971, J GEOPHYS RES, V76, P8534, DOI 10.1029/JB076i035p08534; PIEL KM, 1971, CAN J BOTANY, V49, P1885, DOI 10.1139/b71-266; Plafker G., 1977, The United States Geological Survey in Alaska; Accomplishments during 1976, pB67; Plafker George., 1994, The Geology of Alaska, VG-1, P989, DOI [10.1130/DNAG-GNA-G1.989, DOI 10.1130/DNAG-GNA-G1.989]; Ratchkovski NA, 2002, B SEISMOL SOC AM, V92, P998, DOI 10.1785/0120010182; REED BL, 1974, GEOL SOC AM BULL, V85, P1883, DOI 10.1130/0016-7606(1974)85<1883:OPAHOM>2.0.CO;2; RICHTER DH, 1971, GEOL SOC AM BULL, V82, P1529, DOI 10.1130/0016-7606(1971)82[1529:QFITEA]2.0.CO;2; Ridgway K., 1992, Yukon Geol, V3, P1; Ridgway K.D., 1993, Processes controlling the composition of clastic sediments, V284, P67, DOI DOI 10.1130/SPE284-P67; RIDGWAY KD, 1993, SEDIMENTOLOGY, V40, P645, DOI 10.1111/j.1365-3091.1993.tb01354.x; RIDGWAY KD, 1995, GEOL SOC AM BULL, V107, P676, DOI 10.1130/0016-7606(1995)107<0676:CIFCAT>2.3.CO;2; Ridgway KD, 1997, GEOL SOC AM BULL, V109, P505, DOI 10.1130/0016-7606(1997)109<0505:TTBFAA>2.3.CO;2; RIDGWAY KD, 1992, THESIS U ROCHESTER R; RIDGWAY KD, 1999, SHORT NTOES ALASKA G, V119, P77; STOUT JH, 1980, CAN J EARTH SCI, V17, P1527, DOI 10.1139/e80-160; STOUT JH, 1973, GEOL SOC AM BULL, V84, P939, DOI 10.1130/0016-7606(1973)84<939:EFQMOT>2.0.CO;2; THOMSON PW, PALAEONTOGRAPHICA B; Traverse A, 1955, 5151 US BUR MIN, V5151; Trop JM, 2002, GEOL SOC AM BULL, V114, P693, DOI 10.1130/0016-7606(2002)114<0693:MSBDOT>2.0.CO;2; Trop JM, 1997, J SEDIMENT RES, V67, P469; WILSON LR, 1946, AM J BOT, V33, P271, DOI 10.2307/2437433; Wolfe J. A., 1977, Paleogene floras from the Gulf of Alaskaregion; Woodcock NJ., 1994, Continental deformation, P251; WRUCKE CT, 1998, EOS T AGU S, V79, pF876	65	24	30	0	5	CANADIAN SCIENCE PUBLISHING	OTTAWA	65 AURIGA DR, SUITE 203, OTTAWA, ON K2E 7W6, CANADA	0008-4077	1480-3313		CAN J EARTH SCI	Can. J. Earth Sci.	APR	2004	41	4					457	480		10.1139/E04-003	http://dx.doi.org/10.1139/E04-003			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	814SF					2025-03-11	WOS:000220993700006
J	Nguyen-Ngoc, L				Nguyen-Ngoc, L			An autecological study of the potentially toxic dinoflagellate <i>Alexandrium affine</i> isolated from Vietnamese waters	HARMFUL ALGAE			English	Article						Alexandrium affine; Vietnamese waters; taxonomy; autecology	LIFE-HISTORY; GONYAULAX-TAMARENSIS; CYST FORMATION; DINOPHYCEAE; SEXUALITY; GROWTH	The potentially toxic dinoflagellate species Alexandrium affine isolated from Ha Long Bay (Tonkin Gulf), Vietnam was Cultured and maintained for morphological, physiological and toxicological Studies. Classical morphological examinations including plate pattern were in good agreement with the international nomenclature of the species. The fine structure of A. affine, including morphology of its developmental stages during vegetative and sexual reproduction was found to be typical of other species in the genus. Two general trends in growth of A. Affine from Vietnamese waters were apparent: (1) growth rates were low at low salinities (10 and 15 psu) in all experimental temperatures (21-27degrees); (2) growth rates were high at salinities 25, 30. and 35 psu in all temperatures. There were no significant differences in growth rates at different salinities at low temperature (21degreesC). and the most significant difference in growth rate was between high temperature-high salinity and high temperature-low salinity. The optimum temperature and salinity for growth were 24degreesC and 30 psu. Maximum division rates per day (0.5-0.7) were at salinities 30 and 35 psu and at temperatures 24 and 27degreesC. But the best conditions for division rate were 21 and 24degreesC at salinities 30 and 35 psu. Toxicity analyses indicated A. affine to be both toxic and non-toxic at certain times. In the former case, toxicity was very low, 2.28 fmol per cell; the toxicity component of A. affine was compared with that of A. leei and the mussel Perna viridis including neoSTX, STX, and GTX(1)-GTX(4). (C) 2004 Elsevier B.V. All rights reserved.	Inst Oceanog, Nha Trang, Vietnam	Vietnam Academy of Science & Technology (VAST)	Inst Oceanog, Cau Da 01, Nha Trang, Vietnam.	habviet@dng.unn.vn	Nguyen, Lam/R-1094-2019					Anderson D. M., 2001, DOCUMENT 201 MR 011; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Balech E., 1985, P33; CANNON JA, 1993, DEV MAR BIO, V3, P741; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Fukuyo Y., 1985, P27; Graneli E., 1985, P201; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; HALLEGRAEFF GM, 1995, IOC MANUAL GUIDE; HANSEN G, 1993, PHYCOLOGIA, V32, P73, DOI 10.2216/i0031-8884-32-1-73.1; Hansen G, 1998, EUR J PHYCOL, V33, P281; Heath Dwight B., 1995, International Handbook on Alcohol and Culture, P1; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; KITA T, 1985, B MAR SCI, V37, P643; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; MACKENZIE L, 1992, J PHYCOL, V28, P399, DOI 10.1111/j.0022-3646.1992.00399.x; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; NGUYENNGOC L, 2002, THESIS U COPENHAGEN; PARTENSKY F, 1988, J PHYCOL, V24, P408, DOI 10.1111/j.1529-8817.1988.tb04484.x; PHANICHYAKARN V, 1993, DEV MAR BIO, V3, P165; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; SILVA ES, 1995, PHYCOLOGIA, V34, P396, DOI 10.2216/i0031-8884-34-5-396.1; SILVA ES, 1962, BOT MAR, V2, P75; Spector D.L., 1984, P107; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; Von Stosch HA., 1973, Br Phycol J, V8, P105; Yoshida M, 2000, FISHERIES SCI, V66, P177, DOI 10.1046/j.1444-2906.2000.00029.x; Zar J.H, 1999, BIOSTAT ANAL, V4th	30	42	47	1	16	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	APR	2004	3	2					117	129		10.1016/S1568-9883(03)00062-3	http://dx.doi.org/10.1016/S1568-9883(03)00062-3			13	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	813RY					2025-03-11	WOS:000220925400002
J	Yoo, JS; Shin, HW				Yoo, JS; Shin, HW			Effects of basic oxygen furnace slag and inorganic nutrients on the germination of resting cysts of two toxic dinoflagellates	JOURNAL OF ENVIRONMENTAL BIOLOGY			English	Article						BOF slag; resting cyst; toxic dinoflagellate; red tide		Effects of basic oxygen furnace (BOF) slag, inorganic nutrients and H2S on the germination of resting cysts of two toxic dinoflagellates Alexandrium catenella/tamarense and Gymnodinium catenatum were studied in batch cultures. The germination rate of the test species has increased by 23-25%, when the concentration of NO3--N or H2S in culture medium has increased to 2.0 ppm. At the treatment of enriched NH4+-N and PO43--p, the germination of resting cyst was increased. Nevertheless, the increased range in germination rates was less than those of NO3--N and H2S. When BOF slag in culture medium increased to 50 mg/ml (or 500 g/m(2)), the cyst germination rate fell to less than 5%. At higher level of concentrations germination was completely inhibited. Adding BOF slag to the culture medium reduced the concentration of inorganic salts and H2S in seawater and sediments, resulting in the inhibition of cyst germination. These findings demonstrate the potential use of BOF slag on the sediments seed bank of red tide organism because it has an ability to inhibit resting cysts germination.	Korea Maritime Univ, Res Inst Marine Sci & Technol, Pusan 606791, South Korea; Soonchunhyang Univ, Dept Marine Biotechnol, Asan 336745, South Korea	Korea Maritime & Ocean University; Soonchunhyang University	Korea Maritime Univ, Res Inst Marine Sci & Technol, Pusan 606791, South Korea.	jsyoo@hhu.ac.kr						ANDERSON D, 1985, TOXIC DINOFLAGELLATE, P279; ANDERSON DM, 1980, J PHYCOL, V16, P166; BINDER BJ, 1987, J PHYCOL, V23, P99; Dale B., 1983, P69; HORI T, 1993, ILLUSTRATED ATLAS LI, V3, P313; HYUN JH, 1997, J KOREA SOLID WASTES, V14, P640; KIM CH, 1994, J AQUAC, V7, P251; KIM CH, 1987, KOREAN J PHYCOL, V2, P211; Kim H.G., 1993, ILLUSTRATION PLANKTO, P97; Kim H.G., 2000, HDB OCEANOGRAPHY MAR; Kim H.G., 1996, HARMFUL TOXIC ALGAL, P57; LEE CI, 1999, STUDY DEV SOIL CONDI; LEE CI, 1999, STUDY CONTROL CAUSAT; LEE GS, 1990, CHEM ENG J BIOCH ENG, V44, P1, DOI 10.1016/0300-9467(90)80049-I; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Montani Shigeru, 1995, P627; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; Sundstrom B, 1990, TOXIC MARINE PHYTOPL, P537; Yoo Jong Su, 2000, Journal of Fisheries Science and Technology, V3, P26	19	3	3	0	4	TRIVENI ENTERPRISES	LUCKNOW	C/O KIRAN DALELA, 1/206 VIKAS NAGAR, KURSI RD, LUCKNOW 226 022, INDIA	0254-8704			J ENVIRON BIOL	J.Environ.Biol.	APR	2004	25	2					147	150						4	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	812YC	15529870				2025-03-11	WOS:000220873800005
J	Montresor, M; John, U; Beran, A; Medlin, LK				Montresor, M; John, U; Beran, A; Medlin, LK			<i>Alexandrium tamutum</i> sp nov (Dinophyceae):: A new nontoxic species in the genus <i>Alexandrium</i>	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium; Alexandrium minutum; Alexandrium tamarense; Alexandrium tamutum sp nov.; LSU rDNA; Mediterranean Sea; phylogeny; SSU rDNA; taxonomy	INTERNAL TRANSCRIBED SPACER; SHELLFISH POISONING TOXINS; NORTH-AMERICAN; MINUTUM HALIM; SEQUENCE COMPARISONS; NATURAL-POPULATIONS; UNITED-STATES; RIBOSOMAL DNA; RESTING CYST; LIFE-HISTORY	A new species of the dinoflagellate genus Alexandrium, A. tamutum sp. nov., is described based on the results of morphological and phylogenetic studies carried out on strains isolated from two sites in the Mediterranean Sea: the Gulf of Trieste (northern Adriatic Sea) and the Gulf of Naples (central Tyrrhenian Sea). Vegetative cells were examined in LM and SEM, and resting cysts were obtained by crossing strains of opposite mating type. Alexandrium tamutum is a small-sized species, resembling A. minutum in its small size, the rounded-elliptical shape and the morphology of its cyst. The main diagnostic character of the new species is a relatively wide and large sixth precingular plate (6'), whereas that of A. minutum is much narrower and smaller. Contrary to A. minutum, A. tamutum strains did not produce paralytic shellfish poisoning toxins. Phylogenies inferred from the nuclear small subunit rDNA and the D1/D2 domains of the large subunit nuclear rDNA of five strains of A. tamutum and numerous strains of other Alexandrium species showed that A. tamutum strains clustered in a well-supported clade, distinct from A. minutum.	Stn Zool A Dohrn, I-80121 Naples, Italy; Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; Lab Biol Marina, I-34010 Trieste, Italy	Stazione Zoologica Anton Dohrn; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Stn Zool A Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@szn.it	medlin, linda/G-4820-2010; John, Uwe/S-3009-2016	Montresor, Marina/0000-0002-2475-1787; medlin, linda k/0000-0001-6014-8339; Beran, Alfred/0000-0003-3723-4161; John, Uwe/0000-0002-1297-4086				ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.x; 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, 1999, J PHYCOL, V35, P870, DOI 10.1046/j.1529-8817.1999.3540870.x; [Anonymous], IOC TAXONOMIC REFERE; BALECH E, 1989, PHYCOLOGIA, V28, P206, DOI 10.2216/i0031-8884-28-2-206.1; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Béchemin C, 1999, AQUAT MICROB ECOL, V20, P157, DOI 10.3354/ame020157; 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; Chang FH, 1997, TOXICON, V35, P393, DOI 10.1016/S0041-0101(96)00168-7; Ciminiello P, 2000, TOXICON, V38, P1871, DOI 10.1016/S0041-0101(00)00099-4; Codd GA, 1999, EUR J PHYCOL, V34, P405, DOI 10.1017/S0967026299002255; COSTAS E, 1995, J PHYCOL, V31, P801, DOI 10.1111/j.0022-3646.1995.00801.x; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; DELGADO M, 1990, Scientia Marina, V54, P1; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; Doyle J. 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Phycol.	APR	2004	40	2					398	411		10.1111/j.1529-8817.2004.03060.x	http://dx.doi.org/10.1111/j.1529-8817.2004.03060.x			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	805GI		Green Submitted			2025-03-11	WOS:000220354400018
J	Wendler, J; Willems, H				Wendler, J; Willems, H			Pithonelloid wall-type of the Late Cretaceous calcareous dinoflagellate cyst genus <i>Tetratropis</i>	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						calcareous dinoflagellate cysts; Pithonelloideae; upper Cretaceous; paratabulation; palaeoecology	RECONSTRUCTION; CHALK	The late Cretaceous calcareous dinoflagellate genus Tetratropis features both a pithonelloid wall-type (evenly inclined wall-components, proven here by a polarisation optical revision) and a peridinialean paratabulation strongly suggesting a dinoflagellate origin of at least part of the Pithonelloideae. This affinity with dinoflagellates sheds more light on the palaeoccology of the Pithonelloideae (commonly termed "calcispheres"), which are characteristic of the middle to Late Cretaceous. The very short-term stratigraphic occurrence of all Tetratropis species is comparable to the distribution pattern of other calcareous dinoflagellate cyst species with a distinctive paratabulation and is thought to reflect a narrow palaeoecological niche. Tetratropis species can be interpreted either as paratabulated morphotypes of otherwise atabulate Pithonelloideae formed under exceptional palaeoenvironmental conditions or as invaders from a highly specific palaeoecological niche during short-term palaeoceanographic events probably related to the initiation of the Late Cretaceous global cooling. (C) 2004 Elsevier B.V. All rights reserved.	Univ Bremen, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich 5,Postfach 330440, D-28334 Bremen, Germany.	wendler@uni-bremen.de						Barrera E, 1999, GEOL S AM S, P245; BISON KM, UNPUB J MICROPALAEON; Bonet F., 1956, B ASOC MEX GEOL PET, V8, P389; BUTSCHLI O, 1885, KLASSEN ORDNUNGEN TH, V1, P865; DUFOUR T, 1968, CR ACAD SCI D NAT, V266, P1947; EHRENBERG CG, 1731, SYMBOLAE PHYSICAE SE; Ernst H, 1984, MITTEILUNGEN GEOLOGI, V57, P137; Fensome R.A., 1993, Micropaleontology Press Special Paper; Frakes LA, 1999, GEOL S AM S, P49; Haeckel E., 1894, Systematische Phylogenie. Vol. 1. Systematische Phylogenie der Protisten und Pflanzen, V1; Hildebrand-Habel Tania, 1997, Courier Forschungsinstitut Senckenberg, V201, P177; Janofske D., 1992, INA Newsletter, V14, P14; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; Kaufmann FJ, 1865, URWELT SCHWEIZ, P194; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P127; Keupp H., 1987, Facies, V16, P37, DOI 10.1007/BF02536748; Keupp H, 2001, PALAEOGEOGR PALAEOCL, V174, P251, DOI 10.1016/S0031-0182(01)00296-6; Keupp Helmut, 1994, Abhandlungen der Geologischen Bundesanstalt (Vienna), V50, P197; KIENEL U, 1994, BERLINER GEOWISSEN E; NEUMANN C, 1999, BERLINER GEOWISSEN E, V31; Pascher A., 1914, Berlin Ber D bot Ges, V32; Villain J.-M., 1981, CRETACEOUS RES, V2, P435; Villain J.-M., 1975, Palaeontographica A, V149, P193; Wendler J, 2002, GEOL SOC AM SPEC PAP, V356, P265; Wendler J, 2002, CRETACEOUS RES, V23, P213, DOI 10.1006/cres.2002.0311; Wendler J, 2002, PALAEOGEOGR PALAEOCL, V179, P19, DOI 10.1016/S0031-0182(01)00366-2; Wendler J, 2001, REV PALAEOBOT PALYNO, V115, P69, DOI 10.1016/S0034-6667(01)00050-1; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Willems H, 1996, GEOL MIJNBOUW, V75, P215; Willems H., 1992, Zeitschrift fuer Geologische Wissenschaften, V20, P155; WILLEMS H, 1990, SENCKENBERG LETH, V70, P237; Young JR, 1997, PALAEONTOLOGY, V40, P875; ZUGEL P, 1994, COURIER FORSCHUNGSIN, V176	33	8	8	0	2	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	2004	129	3					133	140		10.1016/j.revpalbo.2003.12.011	http://dx.doi.org/10.1016/j.revpalbo.2003.12.011			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	809SI					2025-03-11	WOS:000220656000002
J	Tommasa, LD; Danovaro, R; Belmonte, G; Boero, F				Tommasa, LD; Danovaro, R; Belmonte, G; Boero, F			Resting stage abundance in the biogenic fraction of surface sediments from the deep Mediterranean Sea	SCIENTIA MARINA			English	Article; Proceedings Paper	36th Symposium of the European-Marine-Biological-Association	SEP 17-22, 2001	Menorca, SPAIN	European Marine Biolog Assoc		resting stages; deep sea; Mediterranean; biogenic sediments; cyst morphology	WALLED DINOFLAGELLATE CYSTS; RECENT MARINE-SEDIMENTS; CALANOID COPEPOD EGGS; SHIPS BALLAST WATER; SCRIPPSIELLA-TROCHOIDEA; THECA RELATIONSHIPS; ATLANTIC-OCEAN; DINOPHYCEAE; TRANSPORT; PLANKTON	The presence of resting stages in neritic areas is well known, while their occurrence in the deep sea realm has seldom been considered. Recent investigations showed strict interactions between neritic and deep sea domains, due to up-and down-wellimg phenomena driven by submarine canyons. To estimate the presence of resting stages in deep bottom sediments. seven sediment cores. collected along a trans-Mediterranean transect by means a multi-corer during the TRANSMED Survey ( 1999), were studied. Most biogenic sediment was composed of Foraminifera tests (tens of thousand tests cm(-3)), Calciodinellium albatrosianium and Leonella granifera (Dinophyta) cysts (up to thousands cysts cm(-3)). E even dinocyst morphotypes were recorded mainly as empty shells (seven calcareous-walled: C. albatrosianium, Calciperidinium asymmetricum, Leonella granifera, Scrippsiella trochoidea, S. precaria type 1, S. precaria type 2, S. regolis; four organic-walled: Impagidinium aculeatum, unid. dinocyst 1, unid. dinocyst 2 and unid. dinocyst 3), while no metazoan resting eggs were observed. The presence of viable resting stages in deep bottom surface sediments was much lower than ill neritic areas, suggesting that oceanic species do not produce cysts for a "benthic resting" strategy. Further taxonomic and biogeographic Studies are needed to better understand the ecological dynamics of oceanic plankton in the Mediterranean Sea.	Univ Lecce, DISTEBA, I-73100 Lecce, Italy; Univ Ancona, Fac Sci, Sez Biol Marina, I-60131 Ancona, Italy	University of Salento; Marche Polytechnic University	Univ Lecce, DISTEBA, Complesso ECOTEKNE, I-73100 Lecce, Italy.	genuario.belmonte@unile.it	BELMONTE, GENUARIO/AAG-4029-2020; Boero, Ferdinando/B-4494-2008	Boero, Ferdinando/0000-0002-6317-2710				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; Belmonte G, 1995, OLSEN INT S, P53; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; BOERO F, 1994, MAR ECOL-P S Z N I, V15, P3, DOI 10.1111/j.1439-0485.1994.tb00038.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; BROS WE, 1987, J EXP MAR BIOL ECOL, V114, P63; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; Dale B., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; 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Mar.	APR	2004	68			1			103	111		10.3989/scimar.2004.68s1103	http://dx.doi.org/10.3989/scimar.2004.68s1103			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	816RE					2025-03-11	WOS:000221126200011
J	Chmura, GL; Santos, A; Pospelova, V; Spasojevic, Z; Lam, R; Latimer, JS				Chmura, GL; Santos, A; Pospelova, V; Spasojevic, Z; Lam, R; Latimer, JS			Response of three paleo-primary production proxy measures to development of an urban estuary	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						Buzzards Bay; urbanization; forest clearance; industrialization; algal blooms; pollution; phytoplankton; benthic algae	DINOFLAGELLATE CYST; NUTRIENT LIMITATION; BIOGENIC SILICA; CHESAPEAKE BAY; TROPHIC STATUS; YOKOHAMA-PORT; TOKYO-BAY; LAND-USE; EUTROPHICATION; MARINE	In this study we present a novel comparison of three proxy indicators of paleoproductivity, pigments, biogenic silica (BSi), and cysts of autotrophic dinoflagellates measured in cored sediments from New Bedford Harbor, Massachusetts. In addition to detailed historical reports we use palynological signals of land clearance, changes in the ratio of centric and pennate diatoms, sedimentary organic carbon and stable carbon isotopes to constrain our interpretations. Our study spans the period from prior to European settlement to similar to1977, during which watersheds were cleared, port development occurred and much of the coastal property became industrialized. The combined effects of nutrient loading from watershed clearance and urban sewage on the estuarine ecosystem shifted not only levels of primary production, but also the nature of the production. Our proxies show that when European colonists first arrived the estuarine production was benthic-dominated, but eventually became pelagic-dominated. Importance of water column production (by diatoms and dinoflagellates) rapidly increased as soil nitrogen was released following forest clearance. Stabilization in rates of forest clearance is reflected as a decline in production. However, population increases in the urbanizing watershed brought new sources of nutrients through direct sewage discharge, apparently again stimulating primary production. We assume that early 20th century changes in sewage discharge and introduction of heavy metals into Harbor waters caused a temporary reduction in primary production. The introduction of a new sewer outfall near the core site and changes in estuarine hydrography due to construction of a hurricane barrier across the mouth of the harbor are reflected by renewed water column production, but decreases in the population of diatoms and dinoflagellates. Fossil pigments suggest renewed water column production in the latest years recorded by our sediment core. (C) 2003 Elsevier B.V. All rights reserved.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada; US EPA, Off Res & Dev, NHEERL, Atlantic Ecol Div, Narragansett, RI 02882 USA	United States Environmental Protection Agency	McGill Univ, Dept Geog, 805 Sherbrooke St,W, Montreal, PQ H3A 2K6, Canada.	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Total Environ.	MAR 29	2004	320	2-3					225	243		10.1016/j.scitotenv.2003.08.003	http://dx.doi.org/10.1016/j.scitotenv.2003.08.003			19	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	806MY	15016509				2025-03-11	WOS:000220439200010
J	Green, DH; Llewellyn, LE; Negri, AP; Blackburn, SI; Bolch, CJS				Green, DH; Llewellyn, LE; Negri, AP; Blackburn, SI; Bolch, CJS			Phylogenetic and functional diversity of the cultivable bacterial community associated with the paralytic shellfish poisoning dinoflagellate <i>Gymnodinium catenatum</i>	FEMS MICROBIOLOGY ECOLOGY			English	Article						dinoflagellate; paralytic shellfish poisoning; small subunit rDNA; cultivable bacterial diversity; Rhodobacteraceae; Alteromonadaceae; aerobic anoxygenic photosynthesis; hydrocarbon utilisation; Gymnodinium catenatum	ALEXANDRIUM DINOPHYCEAE; PROROCENTRUM-LIMA; MARINE BACTERIUM; SODIUM-CHANNEL; CYST FORMATION; HIROSHIMA BAY; ALGAL BLOOM; TOXINS; SAXITOXIN; GROWTH	Gymnodinium catenatum is one of several dinoflagellates that produce a suite of neurotoxins called the paralytic shellfish toxins (PST), responsible for outbreaks of paralytic shellfish poisoning in temperate and tropical waters. Previous research suggested that the bacteria associated with the surface of the sexual resting stages (cyst) were important to the production of PST by G. catenatum. This study sought to characterise the cultivable bacterial diversity of seven different strains of G. catenatum that produce both high and abnormally low amounts of PST, with the long-term aim of understanding the role the bacterial flora has in bloom development and toxicity of this alga. Sixty-one bacterial isolates were cultured and phylogenetically identified as belonging to the Protcobacteria (70%), Bacteroidetes (26%) or Actinobacteria (3%). The Alphaproteobacteria were the most numerous both in terms of the number of isolates cultured (49%) and were also the most abundant type of bacteria in each G. catenatum culture. Two phenotypic (functional) traits inferred from the phylogenetic data were shown to be a common feature of the bacteria present in each G. catenatum culture: firstly, Alphaproteobacteria capable of aerobic anoxygenic photosynthesis, and secondly, Gammaproteobacteria capable of hydrocarbon utilisation and oligotrophic growth. In relation to reports of autonomous production of PST by dinoflagellate-associated bacteria, PST production by bacterial isolates was investigated, but none were shown to produce any PST-like toxins. Overall, this study has identified a number of emergent trends in the bacterial community of G. catenatum which are mirrored in the bacterial flora of other dinoflagellates, and that are likely to be of especial relevance to the population dynamics of natural and harmful algal blooms. (C) 2003 Federation of European Microbiological Societies. Published by Elsevier B.V. All rights reserved.	Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA37 1QA, Argyll, Scotland; Australian Inst Marine Sci, Townsville, Qld 4810, Australia; CSIRO, Hobart, Tas, Australia	University of the Highlands & Islands; Australian Institute of Marine Science; Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Green, DH (通讯作者)，Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA37 1QA, Argyll, Scotland.	david.green@sams.ac.uk	Bolch, Christopher/J-7619-2014; Blackburn, Susan/M-9955-2013; Llewellyn, Lyndon/F-6030-2011; Negri, Andrew/G-9909-2017; Green, David/E-2533-2012	Llewellyn, Lyndon/0000-0003-1680-1796; Negri, Andrew/0000-0003-1388-7395; Green, David/0000-0001-7499-6021				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; [Anonymous], 1999, ANTO LEEUWEN; Azam F, 1998, SCIENCE, V280, P694, DOI 10.1126/science.280.5364.694; Baker TR, 2003, TOXICON, V41, P339, DOI 10.1016/S0041-0101(02)00314-8; Béjà O, 2002, NATURE, V415, P630, DOI 10.1038/415630a; Béjà O, 2001, NATURE, V411, P786, DOI 10.1038/35081051; Bell W. 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Ecol.	MAR 15	2004	47	3					345	357		10.1016/S0168-6496(03)00298-8	http://dx.doi.org/10.1016/S0168-6496(03)00298-8			13	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	803XO	19712323	Bronze, Green Published, Green Accepted			2025-03-11	WOS:000220264000009
J	Esper, O; Versteegh, GJM; Zonneveld, KAF; Willems, H				Esper, O; Versteegh, GJM; Zonneveld, KAF; Willems, H			A palynological reconstruction of the Agulhas Retroflection (South Atlantic Ocean) during the Late Quaternary	GLOBAL AND PLANETARY CHANGE			English	Article						dinoflagellate cysts; pollen and spores; Agulhas current; Cape Basin; orbital forcing; palaeoceanography	WALLED DINOFLAGELLATE CYSTS; LAST GLACIAL MAXIMUM; LONG-TERM VARIATIONS; SURFACE SEDIMENTS; INDIAN-OCEAN; EQUATORIAL ATLANTIC; MEDITERRANEAN SEA; ORGANIC-MATTER; SINGA SECTION; ARABIAN SEA	Here, we reconstruct the varying influence of the Agulhas Current (AgC), the South Atlantic Current and the Antarctic Circumpolar Current on the Agulhas Retroflection (AgR) in the eastern South Atlantic Ocean for the last 160,000 years on the basis of the dinoflagellate cysts, pollen and spores present in a sediment core (GeoB 3603-2) from the southeastern Cape Basin offshore South Africa, where the Agulhas Current enters the Atlantic Ocean. Our analyses reveal strong orbital forcing on the heat exchange between the Indian Ocean and the South Atlantic Ocean during the Late Quaternary. Maxima in local productivity appear to be primarily related to a strengthening of the ocean circulation as a result of the high seasonal contrast during precession maxima. During precession minima, seasonal contrast was low and stratified, oligo- to mesotrophic conditions prevailed, notably when these minima coincided with the glacial terminations. The clear presence of periodicities on a sub-Milankovitch scale as well as modulations of the primary frequencies demonstrate that the Agulhas Retroflection furthermore is modulated substantially by complex interactions between the subtropical, 'precession-driven', climate and ocean circulation systems, and the southern, 'obliquity-driven', high latitudes. (C) 2004 Elsevier B.V All rights reserved.	Univ Bremen, Fachbereich 5, D-28334 Bremen, Germany; Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands	University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Esper, O (通讯作者)，Univ Bremen, Fachbereich 5, Postfach 330 440, D-28334 Bremen, Germany.	esper@uni-bremen.de	; Versteegh, Gerard J.M./H-2119-2011	Esper, Oliver/0000-0002-4342-3471; Versteegh, Gerard J.M./0000-0002-9320-3776				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]; BERGER AL, 1978, QUATERNARY RES, V9, P139, DOI 10.1016/0033-5894(78)90064-9; Bickert T, 1996, SOUTH ATLANTIC, P599; Blackman R. 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Planet. Change	MAR	2004	41	1					31	62		10.1016/j.gloplacha.2003.10.002	http://dx.doi.org/10.1016/j.gloplacha.2003.10.002			32	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	779XH					2025-03-11	WOS:000189327000003
J	Roncaglia, L; Kuijpers, A				Roncaglia, L; Kuijpers, A			Palynofacies analysis and organic-walled dinoflagellate cysts in late-Holocene sediments from Igaliku Fjord, South Greenland	HOLOCENE			English	Article						palynofacies; palynology; dinoflagellate cysts; palaeoccanography; hydrography; climatic change; sea-surface temperatures; East Greenland Current; late Holocene	SEA-SURFACE CONDITIONS; NORTH-ATLANTIC; AGE CALIBRATION; DATA-BASE; ICE; CLIMATE; INDICATORS; ASSEMBLAGES; TRACERS; WEDDELL	This study characterizes late-Holocene (past 3300 years) variations in organic matter deposition in the outer part of lgaliku Fjord, South Greenland, and uses this information to assess palaeohydrographic conditions. Except for two, all residues were characterized by abundant organic matter, with amorphous material dominating. The late-Holocene sediments in the deeper parts of the outer lgaliku Fjord have generally been deposited under anoxic to suboxic conditions with relatively low terrestrial/freshwater influx. The organic-walled dinoflagellate cyst assemblages suggest the continuous presence of water masses derived from the East Greenland Current, while changes in sea-surface temperature during the last 3300 years have also been interpreted. Terrestrial influx was reflected by the continuous occurrence of leaf tissue, which increased in abundance in sediments younger than AD 960. Pseudo-amorphous phytoclasts occurred in sediments older than AD 770, and sporomorphs were rare throughout. Acritarchs and organic-walled dinoflagellate cysts dominated the assemblages in the sediments. Relatively high amounts of benthic foraminiferal linings in the interval AD 960-1285 suggests increased nutrient availability, which may be ascribed to strong, wind-induced mixing of the water-column or higher fluxes of organic material. Sparse organic matter was recorded in sediments of age C. AD 1125 pointing to significant oxidation due to highly oxic bottom-water conditions.	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.	lr@geus.dk						ACKLEY SF, 1994, DEEP-SEA RES PT I, V41, P1583, DOI 10.1016/0967-0637(94)90062-0; ANDERSEN OGN, 1977, OPHELIA, V16, P205; Batten D., 1996, Palynology: principles and applications, P1011; Batten DJ, 1998, CRETACEOUS RES, V19, P279, DOI 10.1006/cres.1998.0116; BILODEAU G, 1990, CAN J EARTH SCI, V27, P946, DOI 10.1139/e90-098; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; BROECKER WS, 1994, NATURE, V372, P421, DOI 10.1038/372421a0; Buch E., 2000, Scientific report, V12, P1; Buck KR, 1998, POLAR BIOL, V20, P377, DOI 10.1007/s003000050317; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Campbell ID, 1998, GEOLOGY, V26, P471, DOI 10.1130/0091-7613(1998)026<0471:LHYCPA>2.3.CO;2; DahlJensen D, 1998, SCIENCE, V282, P268, DOI 10.1126/science.282.5387.268; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Davies SM, 2001, J QUATERNARY SCI, V16, P99, DOI 10.1002/jqs.611; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1987, POLLEN SPORES, V29, P291; Fensome R. 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J	Head, MJ; Riding, JB; Eidvin, T; Chadwick, RA				Head, MJ; Riding, JB; Eidvin, T; Chadwick, RA			Palynological and foraminiferal biostratigraphy of (Upper Pliocene) Nordland Group mudstones at Sleipner, northern North Sea	MARINE AND PETROLEUM GEOLOGY			English	Article						dinoflagellate cysts; foraminifera; stable isotopes; Pliocene; North Sea	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CAINOZOIC STRATIGRAPHY; UTSIRA FORMATION; DIEST FORMATION; NEOGENE; MIOCENE; SEDIMENTS; ATLANTIC; UPLIFT; PRESERVATION	The Nordland Group is an important stratigraphical unit within the upper Cenozoic of the northern North Sea. At its base lies the Utsira Sand, a dominantly sandy regional saline aquifer that is currently being utilized for carbon dioxide sequestration from the Sleipner gas and condensate field. A 'mudstone drape' immediately overlies the Utsira Sand, forming the caprock for this aquifer. The upper part of the Utsira Sand was recently dated as Early Pliocene, but the precise age of the overlying Nordland Group mudstones has remained uncertain. Dinoflagellate cyst, pollen and spore, foraminiferal and stable isotopic analyses have been performed on these mudstones from a conventional core within the interval 913.10-906.00 m (drilled depth) in Norwegian sector well 15/9-A-11. The samples lie closely above the Utsira Sand. Results give a Gelasian (late Late Pliocene) age for this interval, with a planktonic foraminiferal assemblage at 913.10 m indicating warm climatic conditions and an age between 2.4 and 1.8 Ma. An abundance of the cool-tolerant dinoflagellate cysts Filisphaera filifera and Habibaosta tectata at 906.00 m, along with evidence from pollen and foraminifera, points to deposition during a cool phase of the Gelasian. Dating the mudstone drape provides useful insights into depositional processes. It seems likely that the Utsira Sand, a basinal lowstand deposit, became progressively starved of elastic input as sea level rose and shorelines retreated. The mudstone drape is interpreted as a highstand deposit, perhaps including a maximum flooding surface. Overlying prograding wedges of the Nordland Group form a regressive succession, characterized by increased sedimentary input and rates of deposition of at least 25 cm per 1000 years, which is more than five times that of the Utsira Sand. This is the first published study of a dinoflagellate cyst assemblage from the Upper Pliocene of the northern North Sea. The new dinoflagellate cyst species Echinidinium nordlandensis Head sp. nov. and Echinidinium sleipnerensis Head & Riding sp. nov. are formally described. (C) 2003 NERC. Published by Elsevier Ltd. All rights reserved.	Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England; Norwegian Petr Directorate, N-4003 Stavanger, Norway	University of Cambridge; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Univ Cambridge, Dept Geog, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk; jbri@bgs.ac.uk; tor.eidvin@npd.no; rach@bgs.ac.uk						[Anonymous], 2003, The Millenium Atlas: petroleum geology of the central and northern North Sea; [Anonymous], 1989, NORWEGIAN PETROLEUM; Baklid A., 1996, SPE Annual technical Conference and Exhibition, Denver, Colorado, USA, P1, DOI 10.2118/36600-MS.ocietyofPetroleumEngineers; BALDAUF JG, 1987, INITIAL REP DEEP SEA, V94, P1159; Bennike O, 2002, PALAEOGEOGR PALAEOCL, V186, P1, DOI 10.1016/S0031-0182(02)00439-X; 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; CHADWICK RA, 2004, IN PRESS ENERGY; Chadwicks RA, 2001, GREENHOUSE GAS CONTROL TECHNOLOGIES, P349; COPLEN TB, 1995, J RES NATL INST STAN, V100, P285, DOI 10.6028/jres.100.021; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; de Vernal A., 1989, Proceedings of the Ocean Drilling Program Scientific results, V105, P401, DOI DOI 10.2973/0DP.PR0C.SR.105.134.1989; Deegan C.E., 1977, NORWEGIAN PETROLEUM, V1; Eidvin T, 2001, NORSK GEOL TIDSSKR, V81, P119; Eidvin T, 1999, NORSK GEOL TIDSSKR, V79, P97, DOI 10.1080/002919699433843; Eidvin T, 2000, MAR PETROL GEOL, V17, P579, DOI 10.1016/S0264-8172(00)00008-8; EIDVIN T, 2002, ONSHORE OFFSHORE REL, V2, P51; Fensome R.A., 1993, Micropaleontology Press Special Paper; FEYLINGHANSSEN RW, 1983, NPD B, V2, P109; Flower Benjamin P., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P19; Fronval T., 1996, PROC OCEAN DRILL SCI, V151, P455, DOI DOI 10.2973/ODP.PROC.SR.151.134.1996; Fyfe J.A., 2003, MILLENNIUM ATLAS PET, P279; Galloway WE, 2002, J SEDIMENT RES, V72, P476, DOI 10.1306/110801720476; GALLOWAY WE, 1993, PETROLEUM GEOLOGY OF NORTHWEST EUROPE: PROCEEDINGS OF THE 4TH CONFERENCE, P33, DOI 10.1144/0040033; GHAZI SA, 1992, NORSK GEOL TIDSSKR, V72, P285; GILTNER JP, 1987, NORSK GEOL TIDSSKR, V67, P339; Gregersen U, 1997, MAR PETROL GEOL, V14, P893, DOI 10.1016/S0264-8172(97)00036-6; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Hansen S, 1996, NORSK GEOL TIDSSKR, V76, P245; Harland R., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P531; HARLAND R, 1980, Grana, V19, P211; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head M. 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J	Abbink, OA; Van Konijnenburg-Van Cittert, JHA; Visscher, H				Abbink, OA; Van Konijnenburg-Van Cittert, JHA; Visscher, H			A sporomorph ecogroup model for the Northwest European Jurassic - Lower Cretaceousi: concepts and framework	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Review						palynology; palaeobotany; Late Jurassic; palaeo-ecology; palaeoclimate; sea-level	SPORES INSITU; DINOFLAGELLATE CYSTS; MALE CONE; POLLEN; YORKSHIRE; ENGLAND; PALYNOLOGY; EVOLUTION; CLIMATES; ECOLOGY	Based on recent vegetation distribution and an integration of macropalaeobotanical and palynological information, a palaeo-community model is explored that may permit detailed interpretations of quantitative sporomorph distribution patterns in the Jurassic and Early Cretaceous of NW-Europe in terms of changes in palaeoenvironment (sea-level, climate). The conceptual model is based on the recognition of Sporomorph Ecogroups (SEGs) that reflect broad co-existing plant communities, viz. upland, lowland, river, pioneer, coastal, and tidally-influenced SEGs. In successive palynological assemblages, shifts in the relative abundance of SEGs are thought to be indicators of sea-level changes. Climatic changes may be recognised through significant shifts within the quantitative composition of individual SEGs.	TNO NITG, NL-3508 TA Utrecht, Netherlands; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Natl Museum Nat Hist, NL-2300 RA Leiden, Netherlands	Netherlands Organization Applied Science Research; Utrecht University	TNO NITG, POB 80015, NL-3508 TA Utrecht, Netherlands.	o.abbink@nitg.tno.nl; konijnenburg@naturalis.nl; h.visscher@bio.uu.nl		Visscher, Henk/0000-0002-9276-0220				Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; ABBINK OA, 1998, LPP CONTRIBUTION B, V8; ALVIN KL, 1982, REV PALAEOBOT PALYNO, V37, P71, DOI 10.1016/0034-6667(82)90038-0; [Anonymous], 1964, YORKSHIRE JURASSIC F; [Anonymous], B BUREAU RECHERCHES; [Anonymous], 1979, Sciences; [Anonymous], 1980, MEM MUS NAT HIST NAT; [Anonymous], 1961, YORKSHIRE JURASSIC F; [Anonymous], REV PALAEOBOTANY PAL; BAKKER K, 1985, INLEIDING TOT OECOLO, P2; BATTEN D J, 1973, Palaeontology (Oxford), V16, P399; Batten D.J., 1978, PUBLICATION I KONTIN, V100, P97; BATTEN D.J., 1975, P GEOL ASS, V85, P433; BATTEN DJ, 1976, P GEOL ASS, V87, P431; Beck CB, 1988, Origin and evolution of gymnosperms, P382; BIRKELUND T, 1978, Palaeontology (Oxford), V21, P31; BIRKS H.J.B., 1980, QUATERNARY PALAEOECO; Boulter M., 1993, Special Papers in Palaeontology, V49, P125; BRENNER GJ, 1963, DEP GEOLOGY MINES WA, V27, P1; 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; BROUTIN J, 1975, 100 C NAT SOC SAV PA, V2, P29; Brown S., 1990, Introduction to the petroleum geology of the North Sea, P219; Brugman W. 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J. Geosci.	MAR	2004	83	1					17	31		10.1017/S0016774600020436	http://dx.doi.org/10.1017/S0016774600020436			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	847SM		Green Submitted, Bronze			2025-03-11	WOS:000223415200002
J	Servais, T; Stricanne, L; Montenari, M; Pross, J				Servais, T; Stricanne, L; Montenari, M; Pross, J			Population dynamics of galeate acritarchs at the Cambrian-Ordovician transition in the Algerian Sahara	PALAEONTOLOGY			English	Article						acritarchs; dinoflagellates; ecophenotypism; Cambrian-Ordovician; Algeria	DINOFLAGELLATE-CYSTS; MORPHOLOGY; CHITINOZOANS; MICROFOSSILS; SEDIMENTS	Galeate acritarchs are a major component of Late Cambrian and Early Ordovician palynological assemblages. The populations of galeate acritarchs from the Cambrian-Ordovician transition section in borehole Nl-2 of the Algerian Sahara show a gradual increase in process length and in complexity of the process structures through the succession. While the number of striate elements at the process base, the number of distal ramifications, and the number of membranes between the processes increases progressively, the central body diameter shows only minor variation within the succession. The galeate acritarchs are here interpreted as probably being resting cysts of a microorganism similar to modern dinoflagellates. Published laboratory culture experiments on living dinoflagellates document a considerable morphological variation with respect to the process morphology of the resting cysts that can be produced by a single biologically defined species. Based on these experiments, it is possible to interpret the morphological changes in the galeate acritarchs as being possibly related to changing ecological conditions. By analogy to the cyst distribution of modern dinoflagellates, changing salinity may have played an important role. Depending on environmental parameters, and perhaps on the maturity attained before rupture of the outer membrane during cyst formation, the galeate acritarchs may show a wide variety of process morphologies that have to date been used to describe four genera (morphogenera) and 84 species (morphospecies).	USTL, CNRS, UMR 8014, F-59655 Villeneuve Dascq, France; Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany; Univ Tubingen, Museum Geowissensch, D-72076 Tubingen, Germany	Centre National de la Recherche Scientifique (CNRS); Universite de Lille; Eberhard Karls University of Tubingen; Eberhard Karls University of Tubingen	USTL, CNRS, UMR 8014, SN5, F-59655 Villeneuve Dascq, France.	Thomas.Servais@univ-lille1.fr; ludovic.stricanne@uni-tuebingen.de; michael.montenari@uni-tuebingen.de; joerg.pross@uni-tuebingen.de	Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018	Servais, Thomas/0000-0002-4089-7874				[Anonymous], THESIS TU BERLIN; [Anonymous], 1989, PALAEONTOGRAPHICA IT, V76, P1; Bagnoli G, 2001, REV PALAEOBOT PALYNO, V117, P195, DOI 10.1016/S0034-6667(01)00090-2; Brenner W.W., 2001, BALTICA, V14, P40; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; Cramer F.H., 1970, REV ESPANOLA MICROPA; DALE B, 1996, PALYNOLOGY PRINCIPLE, V3, P911; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DEUNFF J, 1974, Geobios (Villeurbanne), V7, P5, DOI 10.1016/S0016-6995(74)80016-1; Deunff J., 1961, Revue de Micropaleontologie, V4, P37; Deunff J., 1964, Revue de Micropaleontologie, V7, P119; Dorning K.J., 1981, P31; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P298, DOI 10.1073/pnas.49.3.298; Fatka O., 1999, Palynology, V23, P153; Feist-Burkhardt S, 1996, 9 INT PAL C 23 28 JU, P42; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fensome RA, 1999, GRANA, V38, P66; Hallett R., 2000, THESIS U WESTMINSTER; Kokinos John P., 1995, Palynology, V19, P143; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; le Herisse A., 1989, Palaeontographia Italica, V76, P57; Legrand P., 1974, Bulletin Soc Hist nat Afr N, V64, P159; Legrand P., 1985, LOWER PALEOZOIC NW W, P5; Leppig U, 2000, MAR MICROPALEONTOL, V40, P1, DOI 10.1016/S0377-8398(00)00027-X; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; MOLYNEUX S G, 1988, Transactions of the Royal Society of Edinburgh Earth Sciences, V79, P43; Molyneux S.G., 1996, Palynology, V1, P493; Molyneux SG, 1999, GEOL SOC SPEC PUBL, V160, P23, DOI 10.1144/GSL.SP.1999.160.01.03; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; Montenari M, 2000, CR ACAD SCI II A, V330, P493, DOI 10.1016/S1251-8050(00)00182-8; MULLINS GL, 2001, MONOGRAPH PALAEONTOG, V155; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; OWENS RM, 2001, EARLY PALAEOZOIC PAL, P49; Paris F, 2000, REV PALAEOBOT PALYNO, V113, P87, DOI 10.1016/S0034-6667(00)00054-3; RASUL S M, 1974, Palaeontology (Oxford), V17, P41; SARJEANT WAS, 1994, MICROPALEONTOLOGY, V40, P1, DOI 10.2307/1485800; Servais T., 1993, Special Papers in Palaeontology, V48, P79; Servais T, 1996, PALAEONTOLOGY, V39, P389; SERVAIS T., 1998, ANN SOC GEOL BELG, V120, P1; Servais T., 1997, ACTA U CAROLINAE GEO, V40, P631; Servais Thomas, 1995, Palynology, V19, P191; Stricanne L, 2002, REV PALAEOBOT PALYNO, V118, P239, DOI 10.1016/S0034-6667(01)00117-8; TAPPAN H, 1971, Micropaleontology (New York), V17, P385, DOI 10.2307/1484870; Taylor FJR, 1999, J PHYCOL, V35, P1; Turon J.L., 1984, MEM I GEOL BASSIN AQ, V17, P1; Vanguestaine M, 2002, REV PALAEOBOT PALYNO, V118, P269, DOI 10.1016/S0034-6667(01)00119-1; Vavrdova M., 1990, Casopis pro Mineralogii a Geologii, V35, P239; VECOLI M, 1995, CR ACAD SCI II, V320, P515; Vecoli Marco, 1999, Bollettino della Societa Paleontologica Italiana, V38, P343; Vecoli Marco, 1999, Palaeontographia Italica, V86, P1; Vecoli Marco, 1996, Bollettino della Societa Paleontologica Italiana, V35, P3; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wall D., 1974, BLACK SEA GEOLOGY CH, V20, P364	59	48	56	0	1	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0031-0239	1475-4983		PALAEONTOLOGY	Paleontology	MAR	2004	47		2				395	414		10.1111/j.0031-0239.2004.00367.x	http://dx.doi.org/10.1111/j.0031-0239.2004.00367.x			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	803UM		Bronze			2025-03-11	WOS:000220256000010
J	Marret, F; Leroy, S; Chalié, F; Gasse, F				Marret, F; Leroy, S; Chalié, F; Gasse, F			New organic-walled dinoflagellate cysts from recent sediments of Central Asian seas	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Caspian Sea; Aral Sea; late Holocene	CASPIAN SEA; BLACK; ASSEMBLAGES; ATLANTIC; MARMARA; HISTORY; BASIN; LAKE	Recent to sub-recent sediments from the Caspian Sea, the Kara-Bogaz-Gol Bay, the Enseli lake and the Aral Sea contain the new organic-walled dinoflagellate cysts Caspidinium, Caspidinium rugosum and Impagidinium caspienense. C. rugosum has S-type paratabulation, dextral torsion and low relief intratabular ornamentation. L caspienense has low intratabular suturo-cavate relief, parasutural septa irregular in height and a high septum at the junction of paraplate I and the sulcus. The accompanying species consist of Spiniferites cruciformis, Lingulodinium machaerophorum, Pyxidinopsis psilata, cysts of Pentapharsodinium dalei and Brigantedinium spp. S. cruciformis varies from specimens with a cruciform body with a well-developed postero-lateral membranous flange to specimens with a pear-shaped body, reduced processes and no flange. Sea-surface data from these Central Asian seas suggests that the two new taxa C rugosum and I caspienense are probably related to low salinity conditions (12-13). (C) 2004 Elsevier B.V All rights reserved.	Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales; Brunel Univ, Dept Geog & Earth Sci, Uxbridge UB8 3PH, Middx, England; CNRS, CEREGE, UMR 6635, F-13545 Aix En Provence 04, France	Bangor University; Brunel University; Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD)	Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales.	f.marret@bangor.ac.uk; suzanne.leroy@brunel.ac.uk; chalie@cerege.fr; gasse@cerege.fr	Leroy, Suzanne/D-3996-2009	Marret-Davies, Fabienne/0000-0003-4244-0437				AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; ATANASSOVA ID, 1995, ENVIRON POLLUT, V87, P17, DOI 10.1016/S0269-7491(99)80003-7; Boomer I, 2000, QUATERNARY SCI REV, V19, P1259, DOI 10.1016/S0277-3791(00)00002-0; BOZILOVA E, 1997, ANN U SOFIA FAC BIOL, V89, P69; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DERCOURT J, 1985, B SOC GEOL FR, V1, P637; Dumont HJ, 1998, LIMNOL OCEANOGR, V43, P44, DOI 10.4319/lo.1998.43.1.0044; Eaton GL, 1996, REV PALAEOBOT PALYNO, V91, P151, DOI 10.1016/0034-6667(95)00073-9; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; EVITT WR, 1985, REV PALAEOBOT PALYNO, V45, P35, DOI 10.1016/0034-6667(85)90064-8; Fensome R.A., 1993, MICROPALEONTOL SPEC, V7; Froehlich K, 1999, SCI TOTAL ENVIRON, V238, P419, DOI 10.1016/S0048-9697(99)00154-0; Giralt S, 2003, EARTH PLANET SC LETT, V212, P225, DOI 10.1016/S0012-821X(03)00259-0; GROSSWALD MG, 1980, QUATERNARY RES, V13, P1, DOI 10.1016/0033-5894(80)90080-0; GROSSWALD MG, 1993, NATO ASI SER, V1, P1; Kasymov Abdul, 1999, Polish Ecological Studies, V22, P83; KAZANCI N, UNPUB J PALEOLIMNOL; Kloosterboer-van Hoeve ML, 2001, PALAEOGEOGR PALAEOCL, V173, P61, DOI 10.1016/S0031-0182(01)00314-5; KLOOSTERBOERVAN.M, 2000, LPP CONTRIBUTIONS SE, V12; Kosarev A N., 1994, The Caspian Sea; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Lepeshevkov I.N., 1981, PERSPECTIVES USE SAL; LEROY S, 2000, ELDP ESF M PALL IT 7, V7, P45; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Mamedov AV, 1997, QUATERN INT, V41-2, P161, DOI 10.1016/S1040-6182(96)00048-1; Mangerud J, 2001, J QUATERNARY SCI, V16, P773, DOI 10.1002/jqs.661; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; 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; ROCHON A, 1999, CONTRIB SER AM ASS S, V35; Rochon Andre, 2002, Palynology, V26, P95, DOI 10.2113/0260095; Rodionov S.N., 1994, Global and regional climate interaction: the Caspian Sea experience; SHIKLOMANOV IA, 1995, UNESCO IHP IOC IAEA, V108, P1; Stover LE, 1978, ANAL PREPLEISTOCENE; Svitoch AA, 2000, OCEANOLOGY+, V40, P868; Targarona J, 1999, GRANA, V38, P170; Traverse A., 1978, Initial Reports of the Deep Sea Drilling Project, V42B, P993; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WILLIAMS GL, 1998, CONTRIB SER AM ASS S, V34; Zenkevitch L., 1963, BIOL SEAS USSR	43	97	98	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	2004	129	1-2					1	20		10.1016/j.revpalbo.2003.10.002	http://dx.doi.org/10.1016/j.revpalbo.2003.10.002			20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	802TW		Green Submitted			2025-03-11	WOS:000220186800001
J	Eldrett, JS; Harding, IC; Firth, JV; Roberts, AP				Eldrett, JS; Harding, IC; Firth, JV; Roberts, AP			Magnetostratigraphic calibration of Eocene-Oligocene dinoflagellate cyst biostratigraphy from the Norwegian-Greenland Seal	MARINE GEOLOGY			English	Article						Eocene; Oligocene; dinoflagellate cysts; magnetobiostratigraphy; biostratigraphy; Norwegian-Greenland Sea	NORTH-SEA; TRANSITION; EVOLUTION; SEDIMENTS; HIATUSES; ZONATION	The presence of abundant age-diagnostic dinoflagellate cysts in Ocean Drilling Program (ODP) Hole 913B (Leg 151), Deep Sea Drilling Project Hole 338 (Leg 38) and ODP Hole 643A (Leg 104) has enabled the development of a new biostratigraphy for the Eocene-Oligocene interval in the Norwegian-Greenland Sea. This development is important because the calcareous microfossils usually used for biostratigraphy in this age interval are generally absent in high latitude sediments as a result of dissolution. In parallel with this biostratigraphic analysis, we developed a magnetic reversal stratigraphy for these Norwegian-Greenland Sea sequences. This has allowed independent age determination and has enabled the dinocyst biostratigraphy to be firmly tied into the global geomagnetic polarity timescale (GPTS). The relatively high resolution of this study has enabled identification of dinoflagellate cyst assemblages that have affinities with those from the North Sea and the North Atlantic, which allows regional correlation. Correlation of each site with the GPTS has also allowed comparison of the stratigraphic record preserved in each drill-hole. Hole 913B is the most complete and is the best-preserved record of the Eocene and Oligocene in the Northern Hemisphere high latitudes, and can serve as a reference section for palaeoenvironmental reconstructions of this age interval. (C) 2003 Elsevier B.V. All rights reserved.	Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England; Ocean Drilling Program, College Stn, TX 77845 USA	University of Southampton; NERC National Oceanography Centre; Texas A&M University System; Texas A&M University College Station	Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England.	ich@soc.soton.ac.uk	Harding, Ian/K-3320-2012; Roberts, Andrew/E-6422-2010	Eldrett, James/0000-0001-5196-3112; Roberts, Andrew P./0000-0003-0566-8117; Harding, Ian/0000-0003-4281-0581				Abreu VS, 1998, AAPG BULL, V82, P1385; Acton GD, 2002, J GEOPHYS RES-SOL EA, V107, DOI 10.1029/2001JB000518; [Anonymous], 9210 GEOL SURV CAN; [Anonymous], 1994, NATO ASI SERIES; [Anonymous], 1994, J MICROPALAEONTOL, DOI [10.1144/jm.13.1.55, DOI 10.1144/JM.13.1.55]; Armstrong Howard A., 1999, P181; AUBRY M, 1983, 89 LAB GEOL; AUBRY MP, 1985, GEOLOGY, V13, P198, DOI 10.1130/0091-7613(1985)13<198:NEPMBA>2.0.CO;2; BERGGREN WA, 1995, SEPM SPEC PUBL, V54; BIGG PJ, 1982, REV ESP MICROPALEONT, V13, P367; 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; BROWN S, 1984, INITIAL REP DEEP SEA, V81, P565; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; BUJAK J P, 1979, Micropaleontology (New York), V25, P308, DOI 10.2307/1485305; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; BUJAK J.P., 1980, DINOFLAGELLATE CYSTS, V24, P36; CANDE SC, 1992, J GEOPHYS RES-SOL EA, V97, P13917, DOI 10.1029/92JB01202; CANDE SC, 1995, J GEOPHYS RES-SOL EA, V100, P6093, DOI 10.1029/94JB03098; Carney JL., 1995, SEPM SPECIAL PUBLICA, P23, DOI DOI 10.2110/PEC.95.53.0023; Cepek P., 1988, GEOLOGISCHES JB A, VA100, P275; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Costa L.I., 1988, GEOL JB A, V100, P330; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Damassa S. 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W., 1988, GEOL JB A, VA100, P273; Williams G.L., 1985, P847; Williams G.L., 1977, P1231; Williams G.L., 1975, GEOL SURV CAN PAP, V2, P107, DOI DOI 10.4095/102513; WILLIAMS GL, 1999, UNPUB MESOZOIC CENOZ; WILLIAMS GL, 2001, UNPUB UPPER CRETACEO; WILLIAMS GL, 1998, AASP CONTRIB SER, V34; Williams Graham L., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P99; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; ZACHOS JC, 1994, PALEOCEANOGRAPHY, V9, P353, DOI 10.1029/93PA03266	86	107	113	0	10	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0025-3227	1872-6151		MAR GEOL	Mar. Geol.	FEB 28	2004	204	1-2					91	127		10.1016/S0025-3227(03)00357-8	http://dx.doi.org/10.1016/S0025-3227(03)00357-8			37	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	779VF					2025-03-11	WOS:000189321600006
J	Meier, KJS; Zonneveld, KAF; Kasten, S; Willems, H				Meier, KJS; Zonneveld, KAF; Kasten, S; Willems, H			Different nutrient sources forcing increased productivity during eastern Mediterranean S1 sapropel formation as reflected by calcareous dinoflagellate cysts	PALEOCEANOGRAPHY			English	Article						calcareous dinoflagellate cysts; sapropel S1; Mediterranean Sea	LAST GLACIAL MAXIMUM; PLANKTONIC ASSEMBLAGES; AEGEAN SEA; HOLOCENE; CIRCULATION; PALEOCIRCULATION; RECONSTRUCTION; INTERRUPTION; DEPOSITION; SEDIMENTS	[1] Comparison of calcareous dinoflagellate cyst assemblages with Ba, Al, Mn, and Fe records from three sediment cores collected in the eastern Mediterranean Sea indicate that calcareous dinoflagellate cysts are generally resistant to postdepositional dissolution. Cyst association changes during and after sapropel S1 formation can therefore be closely related to variability in surface water productivity. Two groups of cysts are defined: those having highest abundances within the sapropelic and postsapropelic sediments. The temporal cyst distributions suggest increased freshwater input mainly from the Nile and a shallowing of the pycnocline as the most important processes increasing nutrient concentration in the photic zone, thus leading to increased productivity and organic carbon fluxes during sapropel formation. Furthermore, a general warming trend at the beginning of S1 formation and a slight salinity decrease are reconstructed.	Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Dept Geosci, POB 330440, D-28334 Bremen, Germany.	sebastian.meier@unibremen.de	; Meier, K. J. Sebastian/H-7914-2014	Kasten, Sabine/0000-0001-7453-5137; Meier, K. J. 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J	Zonneveld, K				Zonneveld, K			Potential use of stable oxygen isotope composition of <i>Thoracosphaera heimii</i> (Dinophyceae) for upper watercolumn (thermocline) temperature reconstruction	MARINE MICROPALEONTOLOGY			English	Article						calcareous-walled dinoflagellate cysts; stable oxygen isotopes; palaeotemperature; thermocline/deep chloropliyll maximum	SEAWATER CARBONATE CONCENTRATION; CALCAREOUS DINOFLAGELLATE CYSTS; DIEL VERTICAL MIGRATION; UPPER WATER COLUMN; ATLANTIC-OCEAN; SPATIAL-DISTRIBUTION; EQUATORIAL ATLANTIC; LIFE-CYCLE; FORAMINIFERA; DISEQUILIBRIUM	To investigate the potential use of the stable isotope composition of the vegetative cysts of the photosynthetic dinoflagellate Thoracosphaera heimii for quantitative palaeotemperature reconstructions a method has been developed to purify T heimii cysts from sediment samples. Stable oxygen and carbon isotopes have been measured on T heimii cysts from 21 surface sediment samples from the equatorial Atlantic and South Atlantic Oceans. Calculated temperatures based on the palaeotemperature equation for inorganic calcite precipitation generally reflect mean annual temperatures of the upper water column, notably of thermocline depths. Although the present results suggest that the isotopic composition of T heimii shells might be formed in equilibrium with the seawater in which the shells are being formed, future investigations are required to determine possible effects of metabolic and kinetic processes on the fractionation process. This pilot study therefore forms the basis for future investigations on the development of this tool and the determination of a species-specific palaeotemperature equation. The wide geographic and stratigraphic distribution of T heimii cysts in sediments, the stable position of T heimii within the water column and the high resistance of its cysts against calcite dissolution underline its potential for a wide usability in palaeotemperature reconstructions. (C) 2003 Elsevier B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, Bremen, Germany	University of Bremen	Zonneveld, K (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Bremen, Germany.	zonnev@uni-bremen.de						ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; ANDERSON TF, 1983, UTRECHT MICROPALEONT, V30, P189; BAUMANN KH, 2003, S ATLAND LATE QUATER; Bemis BE, 1998, PALEOCEANOGRAPHY, V13, P150, DOI 10.1029/98PA00070; Bickert T., 2000, Mar Geochem. 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Micropaleontol.	FEB	2004	50	3-4					307	317		10.1016/S0377-8398(03)00097-5	http://dx.doi.org/10.1016/S0377-8398(03)00097-5			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	800DG					2025-03-11	WOS:000220008500007
J	Solignac, S; de Vernal, A; Hillaire-Marcel, C				Solignac, S; de Vernal, A; Hillaire-Marcel, C			Holocene sea-surface conditions in the North Atlantic - contrasted trends and regimes in the western and eastern sectors (Labrador Sea vs. Iceland Basin)	QUATERNARY SCIENCE REVIEWS			English	Article							LAST GLACIAL MAXIMUM; DEEP CIRCULATION; LATE QUATERNARY; BARENTS SEA; ICE COVER; CLIMATE; SEDIMENTS; RECONSTRUCTION; GREENLAND; SALINITY	Two sediment cores from the Labrador Sea and one from the Iceland Basin were analysed in order to compare Holocene sea-surface conditions across the northern North Atlantic. delta(18)O measurements on meso- and epi-planktonic foraminifera (Neogloboquadrina pachyderma left-coiling and Globigerina bulloides), along with sea-surface condition reconstructions using transfer functions based on dinoflagellate cyst assemblages, were used to document thermohaline properties of the upper water column. At the Labrador Sea sites, a decreasing trend in sea-surface temperature following an early Holocene maximum, is observed. At the Iceland Basin site, a hiatus between 13 and 8 ka BP prevents us from documenting the entire Holocene, but a stable to slightly decreasing trend is observed from 8 ka BP onwards. Sea-surface salinity and potential density (sigma(0)) show little variation at the Orphan Knoll site in the Labrador Sea since 7 ka BP, whereas they depict a decreasing trend at the two other sites since ca 8 ka BP. This shift in sigma(0) values suggests a progressive enhancement of Labrador Sea Water formation and a relative decrease in the Nordic seas components Of the North Atlantic Deep Water (i.e., Denmark Strait Overflow Water and Norwegian Sea Overflow Water). Discrepancies are also observed with regard to millennial-frequency oscillations in sea-surface conditions. At the easternmost site, they likely match previously documented cold water pulses in the north-eastern Atlantic, whereas they do not show any clear pattern at the westernmost sites. Hence, the western and eastern areas show different behaviours with respect to both long-term and high-frequency fluctuations. (C) 2003 Elsevier Ltd. All rights reserved.	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J	Smith, GA; Harding, IC				Smith, GA; Harding, IC			New dinoflagellate cyst species from Upper Jurassic to Lower Cretaceous sediments of the Volgian lectostratotype sections at Gorodische and Kashpir, Volga Basin, Russia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; Russia; Jurassic; Cretaceous; Volgian; Valanginian		Six new dinoflagellate cyst species are described from a high-resolution palynological study of the Volgian (Upper Jurassic) to Valanginian (Lower Cretaceous) sequences at the Gorodische and Kashpir sections in the Volga Basin, Russia. The following taxa are described: Aprobolocysta pustulosa sp. nov., Cyclonephelium? bulbosum sp. nov., Meiourogonyaulax distincta sp. nov., Cribroperidinium magnificum sp. nov., Cribroperidinium undoryensis sp. nov., and Thalassiphora? robusta sp. nov. These new dinocyst species are stratigraphically restricted and may prove to be useful taxa for regional biostratigraphic correlation. (C) 2003 Elsevier B.V. All rights reserved.	Univ Southampton, Sch Ocean & Earth Sci, Southampton Oceanog Ctr, Southampton SO14 3BZ, Hants, England; Univ Bristol, Dept Earth Sci, Bristol BS8 1RJ, Avon, England	NERC National Oceanography Centre; University of Southampton; University of Bristol	Univ Southampton, Sch Ocean & Earth Sci, Southampton Oceanog Ctr, Empress Dock, Southampton SO14 3BZ, Hants, England.	ich@soc.soton.ac.uk	Harding, Ian/K-3320-2012	Harding, Ian/0000-0003-4281-0581				[Anonymous], 2007, Paleopalynology; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Bailey D, 1997, P YORKS GEOL SOC, V51, P235, DOI 10.1144/pygs.51.3.235; BLOM GI, 1984, 27 INT GEOL C USSR C, P71; Durr G., 1987, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V176, P67; Fensome R.A., 1993, Micropaleontology Press Special Paper; FUNKHOUSER JOHN W., 1959, MICROPALEONTOLOGY, V5, P369, DOI 10.2307/1484431; Hantzpergue P, 1998, MEMOIR MUS NATL HIST, V179, P9; HOGG NM, 1994, UNPUB RES STUDY BORE; Iosifova EK, 1996, REV PALAEOBOT PALYNO, V91, P187, DOI 10.1016/0034-6667(95)00064-X; Kofoid Charles Atwood, 1909, Archiv fuer Protistenkunde Jena, V16; LENTIN JK, 1990, AM ASS STRATIGRAPHIC, V23; Lord A.R., 1987, NEUES JB GEOL PAL, V10, P577; Mesezhnikov M.S., 1977, JURASSIC CRETACEOUS; Riding J.B., 1999, AM ASS STRATIGRAPHIC, V36; Riding James B., 2001, Memoir of the Association of Australasian Palaeontologists, V24, P65; SARJEANT W A S, 1984, Palaeontographica Abteilung B Palaeophytologie, V191, P154; Smith G.A., 1999, THESIS U BRISTOL THESIS U BRISTOL; Vozzhennikova T.F., 1967, FOSSIL PERIDINEAE JU; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	21	8	9	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	FEB	2004	128	3-4					355	379		10.1016/S0034-6667(03)00155-6	http://dx.doi.org/10.1016/S0034-6667(03)00155-6			25	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	768HW					2025-03-11	WOS:000188538400009
J	Westphal, H; Munnecke, A; Pross, J; Herrle, JO				Westphal, H; Munnecke, A; Pross, J; Herrle, JO			Multiproxy approach to understanding the origin of Cretaceous pelagic limestone-marl alternations (DSDP site 391, Blake-Bahama Basin)	SEDIMENTOLOGY			English	Article						calcareous nannofossils; Cretaceous; differential diagenesis; limestone-marl alternations; palynomorphs; DSDP	OLIGOCENE DINOFLAGELLATE CYSTS; DEEP-SEA SEDIMENTS; NORTH-ATLANTIC; CARBONATE; DIAGENESIS; CYCLES; NANNOFOSSILS; DISSOLUTION; SEQUENCES; SITE-534	Limestone-marl alternations are usually directly interpreted to reflect cyclic palaeoenvironmental signals. However, uncertainty in such interpretations stems from the differential diagenesis that most limestone-marl alternations have undergone. Differential diagenesis results in markedly different alterations between limestones and marls and in the loss of comparability of many measurable parameters. For an unequivocal interpretation of the origin of rhythmic alternations, diagenetically robust parameters or parameters that clearly indicate the degree of diagenetic bias are required. The present study uses a multiproxy approach (independent biotic, sedimentary and geochemical parameters) in order to unravel the palaeoenvironmental signal recorded in Valanginian (Early Cretaceous) limestone-marl alternations from the Blake-Bahama Basin (DSDP site 391). Using this approach, terrestrial and marine influences can be distinguished, changes in nutrient levels estimated and prediagenetic differences in the non-carbonate fraction constrained. Surprisingly, no systematic variations in any of these parameters were observed between limestone and marl layers, implying that none of these was directly responsible for the formation of the rhythmic alternation. Hence, none of the current models of sedimentary formation of limestone-marl rhythmites is applicable here. Calcareous nannofossils are equally well preserved in limestone and marl layers, ruling out their dissolution in marl layers as a source of the calcite cement in the limestone beds. Sr values of 700-900 p.p.m. indicate that aragonite may have been present in the original, pelagic sediment. The assumption of fine-grained sedimentary aragonite imported from nearby carbonate platforms as the source of the cement would explain a number of otherwise enigmatic features in these rhythmites, including the source of the calcite cement observed in the limestones, the equally good preservation of calcareous nannofossils in limestones and marls and the higher concentration of calcareous nannofossils in marl layers. The study demonstrates that examination of diagenetically inert parameters or parameters in which diagenetic effects can be filtered can yield unexpected results. Clearly, careful analysis of such parameters needs to be undertaken in order to make reliable palaeoenvironmental interpretations from rhythmite successions.	Leibniz Univ Hannover, Inst Geol, D-30167 Hannover, Germany; Univ Erlangen Nurnberg, Inst Palaontol, D-91054 Erlangen, Germany; Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany	Leibniz University Hannover; University of Erlangen Nuremberg; Eberhard Karls University of Tubingen	Univ Erlangen Nurnberg, Inst Palaontol, Loewenichstr 28, D-91054 Erlangen, Germany.	hildegard.westphal@pal.uni-erlangen.de	Herrle, Jens/B-9088-2008; Westphal, Hildegard/ACQ-0391-2022; Munnecke, Axel/G-3698-2010	Westphal, Hildegard/0000-0001-7324-6122; Munnecke, Axel/0000-0002-6898-1082				[Anonymous], 1982, CYCLIC EVENT STRATIF; [Anonymous], 1982, Cyclic and Event Stratification; Arthur M.A., 1984, MILANKOVITCH CLIMATE, P191; Arthur M. 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J	Kumaran, KPN; Shindikar, M; Limaye, RB				Kumaran, KPN; Shindikar, M; Limaye, RB			Mangrove associated lignite beds of Malvan, Konkan: Evidence for higher sea-level during the Late Tertiary (Neogene) along the west coast of India	CURRENT SCIENCE			English	Article							UPLIFT	Fossil pneumatophores (breathing roots) of Avicennia are recovered and reported from the lignite beds exposed in Kolamb well-section near Malvan, Konkan area of western Maharashtra. The accrued palynoflora is dominated by mangroves (Avicennia, Aegialitis, Excoecaria, Rhizophora and Sonneratia). The spores of mangrove fern (Acrostichum aureum) an estuarine fungus Cirrenalia indicate that these lignites are autochthonous and deposited in a near-shore environment. Presence of foraminiferal linings (= microforaminifera), dinoflagellate cysts, a few calcareous nannofossils and scolecodonts is an irrefutable proof of marine and brackish water influence during the deposition of lignites under intertidal/tidal swampy condition (mangrove influenced) with fair input from freshwater swamps and hinterland. Freshwater-related forms, viz. Ceratopteris thalictroides, Nymphaeaceae, Ctenolophonaceae and hinterland taxa (Cullenia/Durio) of Bombacaceae along with abundance of microthyriaceous fungi in the palynoflora imply a warm humid tropical climate with high precipitation during the depositional period. The presence of Ctenolophon engle-rianus (= Ctenolophonidites costatus) in Kolamb lignites suggests the Late Neogene (Late Miocene-Early Pliocene) age. The occurrence of pneumatophores and associated lignite deposits similar to37 m above the present mean sea-level, and much inland, clearly indicates the higher sea-level strand during Late Neogene along the west coast of India.	Agharkar Res Inst, Geol & Palaeontol Grp, Pune 411004, Maharashtra, India	Department of Science & Technology (India); Agharkar Research Institute (ARI)	Kumaran, KPN (通讯作者)，Agharkar Res Inst, Geol & Palaeontol Grp, Pune 411004, Maharashtra, India.	kpnkumaran@hotmail.com						Bruckner H., 1987, EXPLORATION TROPICS, P173; ELLISON JC, 1989, PALAEOGEOGR PALAEOCL, V74, P327, DOI 10.1016/0031-0182(89)90068-0; Guleria J.S., 1992, PALAEOB OTANIST, V40, P285, DOI DOI 10.54991/JOP.1991.1780; GUZDER S, 1980, QUATERNARY ENV STONE, P100; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Kohlmeyer J., 1979, Marine mycology. The higher fungi.; Kulkarni A.R, 1984, P 10 IND C IND MICR, P515; Kulkarni A.R., 1980, GEOPHYTOLOGY, V10, P125; Martinsen O.J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European Basins, P91; PHADTARE N R, 1980, Geophytology, V10, P158; POWAR KB, 1993, CURR SCI INDIA, V64, P793; RAJAGURU SN, 1984, P S QUAT EP DEP GEOL, P1; Rajshekhar C, 1998, CURR SCI INDIA, V74, P705; Ramanujam C. G. K., 1996, GEOPHYTOLOGY, V25, P1; Ramanujam CGK., 1980, Botanique, V9, P119; RAO MG, 1995, BIRBAL SAHNI CENTENA, P371; Saxena R.K., 1995, GEOPHYTOLOGY, V24, P229; Tomlinson P.B., 2016, The Botany of Mangroves, V2nd, DOI [10.1017/CBO9781139946575, DOI 10.1017/CBO9781139946575]; WILKINSON CJ, 1871, REC GEOL SURV INDIA, V4, P44	19	23	23	0	6	CURRENT SCIENCE ASSN	BANGALORE	C V RAMAN AVENUE, PO BOX 8005, BANGALORE 560 080, INDIA	0011-3891			CURR SCI INDIA	Curr. Sci.	JAN 25	2004	86	2					335	340						6	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	770TN					2025-03-11	WOS:000188747100030
J	Cao, WQ; Lin, YS; Fang, LP				Cao, WQ; Lin, YS; Fang, LP			Abundance and distribution of dinoflagellate cysts in Xiamen Western Harbor	ACTA OCEANOLOGICA SINICA			English	Article						dinoflagellate; cysts; abundance; distribution; Xiamen	AUSTRALIA	In a grid investigation, dinoflagellate cysts were collected from sediments in Xiamen Western Harbor in May of 2000, from which five species of cysts were identified: Alexandrium tamarensis, A. minutum, Lingulodinium polyedra, Gonyaulax scrippsae and Gymnodinium catenatum, account for about 21% in the species composition. The quantitative analysis of the sediments shows that the number of dinoflagellate cysts varies from 51 to 256 cysts/g of sediment, the highest value (>200 cysts/g) being recorded at the stations of the central part of the bay, while the lowest (<100 cysts/g) at the bay mouth. A good linear relationship is found between cyst amount and fine-grained sediments. Complex physiognomies on the seabed, topographty in the bay and weak water exchange are the main factors not only in cyst accumulation but also in their distribution pattern, and have resulted in the difference in cyst densities between the inner bay and the outer bay in the harbor.	Xiamen Univ, Dept Oceanog, Xiamen 361005, Peoples R China	Xiamen University	Cao, WQ (通讯作者)，Xiamen Univ, Dept Oceanog, Xiamen 361005, Peoples R China.	wqcao@xmu.edu.cn	郑, 连明/GZL-5449-2022; Lin, YS/G-3394-2010; Cao, WQ/G-2994-2010					Anderson D.M., 1984, Seafood toxins, P125; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; 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; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; CHEN CM, 1996, P 2 M CHIN COMM SCOR, P108; Dale B., 1983, P69; DODGE JD, 1985, ATLAS DINOFLAGELLATE, P201; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; KOBAYASHI S, 1981, Bulletin of Plankton Society of Japan, V28, P53; Li Chao, 2003, Journal of Oceanography in Taiwan Strait, V22, P38; LIAO SM, 1988, J OCEANOGRAPHY TAIWA, V7, P44; LIN YS, 2002, OCEANOLOGIA LIMNOLOG, V33, P405; Lin Yuanshao, 1996, Journal of Oceanography in Taiwan Strait, V15, P16; Matsuoka K., 1989, P461; MATSUOKA K, 1995, TRAIN WORKSH MON PSP; MATSUOKA K, 1985, RED TIDES BIOL ENV S, P461; MATSUYAMA Y, 1995, PARAPLEGIA, V33, P381, DOI 10.1038/sc.1995.87; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Qi Yuzao, 1994, Oceanologia et Limnologia Sinica, V25, P206; *SOA 3 I OC, 1993, COLL PAP RED TID SUR; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1967, REV PALAEOBOT PALYNO, V2, P249; WANG SJ, 1987, J OCEANOGRAPHY TAIWA, V6, P349; WANG WF, 1994, MARINE SCI B, V13, P53; WANG ZH, 2003, CHINESE J APPL ECOLO, V14, P1039; Zeng G., 1987, Journal of Oceanography in Taiwan Strait, V6, P1; Zheng L., 1997, J TROP SUBTROP BOT, V5, P10; Zheng Lei, 1995, Journal of Jinan University, V16, P121	32	0	0	0	4	CHINA OCEAN PRESS	BEIJING	INTERNATIONAL DEPT, 8 DA HUI SHI, BEIJING 100081, PEOPLES R CHINA	0253-505X			ACTA OCEANOL SIN	Acta Oceanol. Sin.		2004	23	2					347	357						11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	834MN					2025-03-11	WOS:000222415300015
J	Mandal, J; Vijaya, M				Mandal, J; Vijaya, M			Oligocene-Miocene palynomorphs from subsurface sediments, West Bengal, India	ALCHERINGA			English	Article						Palynology; late Oligocene; early Miocene; Damodar Basin; India	DINOFLAGELLATE CYSTS; ADJACENT SEAS; BASIN; NORTH	Palynological studies of Cenozoic sediments from borehole PGD-1A in the easternmost extension of the Damodar Basin, West Bengal, India, provide important new palynological data from this basin, where previous data are rare. The palynoassemblage includes Striatriletes, Crassoretitriletes, Bacutriporites, Cauveripollis, Cheilanthoidspora, Palaeoma/vaceaepollis, Tricollareporites, Pinuspollenites and Tsugaepollenites which suggest a late Oligocene - early Miocene age. Dinocyst genera such as Selenopemphix, Tuberculodinium, Hystrichokolpoma and Thalasiphora, recorded from the borehole, also support this age assignment. The assemblage indicates a tropical to subtropical humid climate with high rainfall. Deposition of the studied strata took place in a delta under shallow marine influence; this is the first evidence that a marine transgression extended into the Damodar Basin and that mangrove forest developed in the area.	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.	jagannathprasadm@yahoo.co.uk						[Anonymous], 9210 GEOL SURV CAN; Baksi S.K., 1980, GEOPHYTOLOGY, V10, P199; Baksi S.K., 1972, SEMINAL PALAEOPALYNO, P188; BAKSI SK, 1981, REV PALAEOBOT PALYNO, V31, P335; BANDE M B, 1980, Geophytology, V10, P146; Banerjee D., 1973, PALEOBOTANIST, V20, P1; Bera Subir, 1995, Indian Journal of Earth Sciences, V22, P149; BHATTACHARJI TK, 1990, UNPUB STATUS REPORT; Bose TK., 1998, TREES WORLD; DASSHARMA S, 1993, P 2 SEM PETR BAS IND, V1, P61; Deb U., 1970, Q J GEOLOGICAL MININ, V42, P127; GHOSH PK, 1982, ACTA BOT INDICA, V10, P50; Guleria J.S., 1992, PALAEOB OTANIST, V40, P285, DOI DOI 10.54991/JOP.1991.1780; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Kar, 1984, I FR PONDICHERRY TRA, V19, P1; Kar R.K., 1991, J PALYNOLOGY, V25, P171; Kar R.K., 1985, Palaeobotanist, V34, P1; Kar RK., 1994, PALAEOBOTANIST, V42, P183; Kumar M, 2001, GEOBIOS-LYON, V34, P241, DOI 10.1016/S0016-6995(01)80072-3; Mabberley D.J., 1997, PLANT BOOK, VSecond; Mathur Y K, 1987, GEOSCI J, V18, P109; MEHROTRA NC, 1992, NEOGENE Q DINOFLAGEL, P197; MEHROTRA NC, 1993, P 2 SEM PETR BAS IND, V1, P83; MORLEY RJ, 1982, REV PALAEOBOT PALYNO, V36, P65, DOI 10.1016/0034-6667(82)90014-8; MORZADEC MT, 1983, CAH MICROPALEONTOL, P15; MULLER J, 1981, BOT REV, V47, P1, DOI 10.1007/BF02860537; SAXENA R.K., 1987, PALEOBOTANIST, V35, P150; VENKATACHALA B.S., 1989, PALEOBOTANIST, V37, P1; Venkatachala BS, 1973, PALEOBOTANIST, V20, P238; Vijaya, 2000, ALCHERINGA, V24, P125, DOI 10.1080/03115510008619529; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	31	4	5	0	2	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0311-5518	1752-0754		ALCHERINGA	Alcheringa		2004	28	2					493	503		10.1080/03115510408619298	http://dx.doi.org/10.1080/03115510408619298			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	862KY					2025-03-11	WOS:000224490800013
J	McMinn, A; Heijnis, H; Murray, A; Hallegraeff, G				McMinn, A; Heijnis, H; Murray, A; Hallegraeff, G			Diatom and dinoflagellate assemblages of the Hawkesbury River, NSW, over the last two centuries: evidence for changes in hydrology	ALCHERINGA			English	Article						diatoms; dinoflagellates; hydrology; Hawkesbury River	NEW-SOUTH-WALES; NUTRIENT ENRICHMENT; NITZSCHIA-PUNGENS; PSEUDO-NITZSCHIA; AUSTRALIA; SEDIMENT; CYSTS; RESPONSES; HISTORY; WATERS	Diatom and dinoflagellate cyst analysis of a 77 cm long sediment core from Cowan Creek, Hawkesbury River estuary, N.S.W., revealed changes in the catchment hydrology over the last 266 years. High abundances of the freshwater/brackish diatom genus Cyclotella at the base of the core imply sustained periods of reduced salinity that now no longer occur. Reduction of freshwater flow after approximately circa 1800 (60 cm) has allowed the development of marine planktonic diatoms Thalassiosira spp., Ditylum brightwellii, Rhizosolenia setigera, Pseudo-nitzschia pungens and Chaetoceros spp. Benthic diatom diversity has remained relatively unchanged. The toxic dinoflagellate Gymnodinium catenatum, although identified in a cyst survey in April 1995, was not found in the sediment cores. Changes in dinoflagellate assemblage are consistent with the effects of increasing urbanisation and eutrophication.	Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia; Australian Nucl Sci & Technol Org, Environm Div, Menai, NSW 2234, Australia; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	University of Tasmania; Australian Nuclear Science & Technology Organisation; University of Tasmania	Univ Tasmania, Inst Antarctic & So Ocean Studies, Box 252-77, Hobart, Tas 7001, Australia.	andrew.mcminn@utas.edu.au; hhx@ansto.gov.au; gustaff.hallegraeff@utas.edu.au	Heijnis, Hendrik/A-6673-2010; McMinn, Andrew/A-9910-2008; Hallegraeff, Gustaaf/C-8351-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343; Heijnis, Hendrik/0000-0002-7601-3452				AJAMI P, 2001, P LINN SOC N S W, V123, P1; [Anonymous], 1999, Bibliotheca Diatomologica; [Anonymous], 1999, RAPID BIOASSESSMENT; BATES SS, 1989, CAN J FISH AQUAT SCI, V46, P1203, DOI 10.1139/f89-156; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CROSSEY MJ, 1988, HYDROBIOLOGIA, V162, P109, DOI 10.1007/BF00014533; Cunningham L, 2003, J PHYCOL, V39, P490, DOI 10.1046/j.1529-8817.2003.01251.x; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Dickman M, 1997, HYDROBIOLOGIA, V352, P149; Growns IO, 2001, REGUL RIVER, V17, P275, DOI 10.1002/rrr.622; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1994, BOT MAR, V37, P397, DOI 10.1515/botm.1994.37.5.397; HASLE GR, 1995, J PHYCOL, V31, P428, DOI 10.1111/j.0022-3646.1995.00428.x; Hillebrand H, 1997, MAR ECOL PROG SER, V160, P35, DOI 10.3354/meps160035; IRWIN A, 2003, HARMFUL ALGAE, V36, P1; JOHN J, 1983, BIBLIOTHECA PHYCOLOG, V64, P359; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; McMinn A, 2003, ALCHERINGA, V27, P135, DOI 10.1080/03115510308619554; MCMINN A, 1992, QUATERNARY RES, V38, P347, DOI 10.1016/0033-5894(92)90043-I; McMinn A, 2002, ALCHERINGA, V26, P519, DOI 10.1080/03115510208619541; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; MCMINN A, 2001, HARMFUL ALGAL BLOOMS, P477; Mitrovic SM, 2001, INT REV HYDROBIOL, V86, P285; Neale JL, 1996, QUATERNARY SCI REV, V15, P581, DOI 10.1016/0277-3791(96)00010-8; Roy PS, 2001, ESTUAR COAST SHELF S, V53, P351, DOI 10.1006/ecss.2001.0796	25	4	4	2	19	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0311-5518	1752-0754		ALCHERINGA	Alcheringa		2004	28	2					505	514		10.1080/03115510408619299	http://dx.doi.org/10.1080/03115510408619299			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	862KY					2025-03-11	WOS:000224490800014
J	Joyce, LB				Joyce, LB			Dinoflagellate cysts in recent marine sediments from Scapa Flow, Orkney, Scotland	BOTANICA MARINA			English	Article						Alexandrium tamarense; dinoflagellate cysts; Scapa Flow; seedbeds; surface sediments	SETO-INLAND-SEA; RESTING CYSTS; THECA RELATIONSHIPS; GONYAULAX-EXCAVATA; ALEXANDRIUM-TAMARENSE; POPULATION-DYNAMICS; COASTAL SEDIMENTS; ATLANTIC-OCEAN; BENTHIC CYSTS; ADJACENT SEAS	To determine the composition, abundance and horizontal distribution of resting cysts in modern coastal sediments from Scapa Flow, Orkney, Scotland, sediment samples were collected from 12 stations. Twentysix dinoflagellate cyst types representing eight motiledefined genera and one cystdefined genus were observed. Four species or species groups dominated the assemblage for the Flow as a whole, Scrippsiella trochoidea, unidentified round brown cysts, Polykrikos schwartzii and Alexandrium tamarense. Total cyst abundance ranged from 371524 cysts ml(-1) wet sediment. The majority of cysts occurred in the central area of the Flow, where higher densities were observed. Of particular importance is the distribution and abundance of cysts of A. tamarense. Since 1991 there have been annual toxic episodes of paralytic shellfish poisoning, caused by the vegetative stage of A. tamarense, in Scapa Flow, leading to widespread bans on all shellfish activities for months at a time. Cysts of A. tamarense were widely distributed within the Flow and ranged from 0212 cysts ml(-1) wet sediment. The overall widespread distribution and higher abundances of cysts of A. tamarense in the central areas of the Flow indicate potential seedbeds for initiation of future vegetative growth and subsequent outbreaks of paralytic shellfish poisoning.	Heriot Watt Univ, Stromness KW16 3AW, Orkney, Scotland	Heriot Watt University	Seaport Aquarium, Private Bag X2, ZA-8012 Cape Town, South Africa.	ljoyce@deat.gov.za						Anderson D.M., 1985, P219; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; 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, 1995, MANUAL HARMFUL MARIN, 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; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BRAY JR, 1957, ECOL MONOGR, V27, P326, DOI 10.2307/1942268; BULLER AT, 1974, POTENTIAL MOVEMENT O, P62; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; Dale B., 1983, P69; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dodge J.D., 1982, Marine Dinoflagellates of the British Isles, P303; DODGE JD, 1991, NEW PHYTOL, V118, P593, DOI 10.1111/j.1469-8137.1991.tb01000.x; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; FUKUYO Y, 1985, B MAR SCI, V37, P529; Gayoso AM, 2001, J PLANKTON RES, V23, P463, DOI 10.1093/plankt/23.5.463; GOWEN RJ, 1990, SCOTTISH SHELLFISH G, V7, P18; HARLAND R, 1981, Palynology, V5, P65; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HARLAND R, 1977, PALEOBOT PALYNOL, V16, P229; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEAD MJ, 2002, J QUATERNARY SCI, V16, P621; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Ishikawa Akira, 2000, Plankton Biology and Ecology, V47, P12; Joint I, 1997, J PLANKTON RES, V19, P937, DOI 10.1093/plankt/19.7.937; JOYCE LB, 2001, THESIS HERIOTWATT U, P232; KOBAYASHI S, 1991, Bulletin of Plankton Society of Japan, V38, P9; Kotani Yuichi, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P104; Lee J.B., 1994, P 2 INT S MAR SCI EX, P1; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Lewis J., 1985, P85; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Lewis Jane, 1995, P175; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; LEWIS JM, 1985, THESIS U LONDON, P294; Marret F, 2003, MAR MICROPALEONTOL, V47, P101, DOI 10.1016/S0377-8398(02)00095-6; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1987, Bull. 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Marina		2004	47	3					173	183		10.1515/BOT.2004.018	http://dx.doi.org/10.1515/BOT.2004.018			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	837CK					2025-03-11	WOS:000222604900001
J	Orlova, TY; Morozova, TV; Gribble, KE; Kulis, DM; Anderson, DM				Orlova, TY; Morozova, TV; Gribble, KE; Kulis, DM; Anderson, DM			Dinoflagellate cysts in recent marine sediments from the east coast of Russia	BOTANICA MARINA			English	Article						Alexandrium spp.; cysts; dinoflagellates; toxic species	SP-NOV DINOPHYCEAE; RESTING CYSTS; GYMNODINIUM-CATENATUM; THECA RELATIONSHIPS; MICRORETICULATE CYST; GONYAULAX-EXCAVATA; SCRIPPSIELLA; SEA; EUTROPHICATION; PERIDINIALES	Fortytwo different dinoflagellate cyst types were found in recent sediment samples collected between July 1999September 2002 from 44 stations along the eastern coast of Russia. This represents the first survey of recent dinoflagellate cysts in Russian marine waters. Forty cysts were identified to the species level, representing 17 genera. The most common cysts were those of ellipsoidal Alexandrium spp., Protoceratium reticulatum, Gonyaulax spp., Polykrikos kofoidii, P. schwartzii, Protoperidinium americanum, P. minutum, P. conicoides, P. subinerme, P. conicum and Scrippsiella trochoidea. Fifteen of the dinoflagellate species have not previously been recorded as motile cells in Russian marine waters: Alexandrium cf. minutum, Cochlodinium cf. polykrikoides, Diplopsalis cf. lebourae, Fragilidium mexicanum, Gonyaulax elongata, G. membranaceae, Gymnodinium cf. catenatum, Pentapharsodinium dalei, P. tyrrhenicum, Protoperidinium americanum, P. cf. avellanum, Scrippsiella cf. lachrymosa, S. cf. precaria, S. cf. rotunda and Warnowia cf. rosea. Cysts of the potentially toxic species Alexandrium cf. minutum, A. tamarense and Gymnodinium cf. catenatum were also found in this survey. Ellipsoidal Alexandrium tamarense type cysts were widely distributed and dominated many localities in the study area. These data suggest that additional cyst surveys should be conducted in areas of the eastern Russian coastline not yet investigated, and that the potential for paralytic shellfish poisoning toxicity as a result of blooms of toxic species may be more widespread than previously documented.	Russian Acad Sci, Inst Marine Biol, Far E Branch, Vladivostok 690041, Russia; 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; Woods Hole Oceanographic Institution	Russian Acad Sci, Inst Marine Biol, Far E Branch, Vladivostok 690041, Russia.	torlova@ibm.dvo.ru	Morozova, Tatiana/G-4468-2018; Orlova, Tatiana/AAU-8448-2020	Gribble, Kristin/0000-0002-8781-9523; Orlova, Tatiana/0000-0002-5246-6967				Anderson D.M., 1984, Seafood toxins, P125; ANDERSON DM, 1988, J PHYCOL, V24, P255; 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; [Anonymous], RUSS J MAR BIOL; [Anonymous], P 13 S SALD MAR BIOL; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; Balech E., 1988, Anales Del Instituto De Biologia Serie Zoologia, V58, P479; BLANCO J, 1989, Scientia Marina, V53, P785; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BUJAK J P, 1986, Palynology, V10, P235; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; Ellegaard M, 2003, PHYCOLOGIA, V42, P151, DOI 10.2216/i0031-8884-42-2-151.1; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; Ellegaard M, 2001, PHYCOLOGIA, V40, P542, DOI 10.2216/i0031-8884-40-6-542.1; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FUKUYO Y, 1977, Bulletin of Plankton Society of Japan, V24, P11; FUKUYO Y, 1982, FUNDAMENTAL STUDIES, P205; Gail G. 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Marina		2004	47	3					184	201		10.1515/BOT.2004.019	http://dx.doi.org/10.1515/BOT.2004.019			18	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	837CK					2025-03-11	WOS:000222604900002
J	Morquecho, L; Lechuga-Devéze, CH				Morquecho, L; Lechuga-Devéze, CH			Seasonal occurrence of planktonic dinoflagellates and cyst production in relationship to environmental variables in subtropical Bahia Concepcion, Gulf of California	BOTANICA MARINA			English	Article						Alexandrium pseudogonyaulax; cyst production rates; cyst traps; Gulf of California; Gymnodinium catenatum; red tide-forming dinoflagellates	LIFE-CYCLE; GYMNODINIUM-CATENATUM; POPULATION-DYNAMICS; SEDIMENT TRAPS; SCRIPPSIELLA; DINOPHYCEAE	We studied seasonal prevalence of dinoflagellates and of cyst production in relation to hydrological factors in Bahia Concepcion, Mexico. In situ production of dinoflagellate cysts was recorded for the first time in Mexico. The resting stage of toxic Gymnodinium catenatum, potentially toxic Alexandrium pseudogonyaulax, and other red tideforming dinoflagellates were collected in traps. Cyst associations were linked with the composition of vegetative stages in the water column, and production yields (128 to 1.465x10(6) cysts m(-2) d(-1)) were comparable with other reports in areas around the world. Seasonal abundance of major meroplankton dinoflagellates and relationships with yields of newlyformed cysts coincides with hydrographic transitional periods in the water column in spring and early fall. From factor analysis, the physicochemical variables that correlate with the presence of the major meroplanktonic species are, in descending order of importance: temperature, phosphates, dissolved oxygen, silicate, nitrite, and nitrate. In Bahia Concepcion, Gonyaulacales and Scrippsiella trochoidea cysts are present during declines in algal blooms as a mechanism to counteract adverse conditions, and to secure an inoculum for blooming when favorable conditions return. In contrast, G. catenatum cysts maintain the motile stage over prolonged periods with recurrent germination.	CIBNOR, La Paz 23000, Baja Calif Sur, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste	CIBNOR, Apartado Postal 128, La Paz 23000, Baja Calif Sur, Mexico.	lourdesm04@cibnor.mx	Morquecho, Lourdes/JPY-0626-2023	Morquecho, Lourdes/0000-0003-2963-8836				ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1998, NATO ASI SER, P475; Band-Schmidt CJ, 2003, BOT MAR, V46, P44, DOI 10.1515/BOT.2003.007; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLASCO D, 1977, LIMNOL OCEANOGR, V22, P255, DOI 10.4319/lo.1977.22.2.0255; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Dale B., 1983, P69; Eppley RW., 1975, Proceedings of THE FIRST INTERNATIONAL CONFERENCE ON TOXIC DINOFLAGELLATE BLOOMS, P11; GARATELIZARRAGA I, 2002, 10 INT C HARMF ALG B, P101; GILBERT P, 2001, GLOBAL ECOLOGY OCEAN, P86; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; GREGORIO ED, 2000, B SO CALIFORNIA ACAD, V99, P147; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; 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; MARASOVIC I, 1989, ESTUAR COAST SHELF S, V28, P35, DOI 10.1016/0272-7714(89)90039-5; Matsuoka K., 2000, GUIA TECNICA ESTUDIO, P30; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MONTRESOR M, 2001, LIFEHAB LIFE HIST MI, P18; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; MORQUECHO L, 2001, SUSTENTABILIDAD BIOD, P281; PFEISTER LA, 1987, BIOL DINOFLAGELLATES, P611; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Sherman BH, 2000, MAR POLLUT BULL, V41, P232, DOI 10.1016/S0025-326X(00)00113-2; STRICKLAND JDH, 1972, B FISH RES BD CANADA, V16, P311; TAKEUCHI T, 1995, 7 INT C TOX PHYT SEN, P49; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Wendler I, 2002, MAR MICROPALEONTOL, V46, P1, DOI 10.1016/S0377-8398(02)00049-X	32	37	41	0	18	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055	1437-4323		BOT MAR	Bot. Marina		2004	47	4					313	322		10.1515/BOT.2004.037	http://dx.doi.org/10.1515/BOT.2004.037			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	849QV					2025-03-11	WOS:000223556000007
J	Hernández-Becerril, DU; Bravo-Sierra, E				Hernández-Becerril, DU; Bravo-Sierra, E			New records of planktonic dinoflagellates (Dinophyceae) from the Mexican Pacific Ocean	BOTANICA MARINA			English	Article						dinoflagellates; Mexican pacific ocean; new records; phytoplankton	BAJA-CALIFORNIA; MARINE-PHYTOPLANKTON; CALCAREOUS CYSTS; LIFE-CYCLE; GULF; CERATIUM; COASTS	Phytoplankton samples were taken during several oceanographic cruises in the Mexican Pacific Ocean (1998-2000), following three different protocols of collection and analysis, and from the material we report six new records of planktonic dinoflagellates in the region. Two species, Asterodinium spinosum and Brachydinium capitatum, are unarmored, another species, Actiniscus pentasterias, has internal siliceous skeletons, whereas Thoracosphaera heimii usually develops a calcareous coccoid vegetative stage. Calciodinellum operosum produces calcareous cysts that were also found in this study, and Achradina pulchra has an internal skeleton of organic material. Three species, A. spinosum, B. capitatum and C. operosum, were represented by very few specimens, whereas all others were more frequent. Brief descriptions and illustrations of these species by light and scanning electron microscopy are provided. The methods and techniques to study this group have been diverse and useful in finding a greater diversity. The world distribution of the species recorded here is revised.	Univ Nacl Autonoma Mexico, Lab Divers & Ecol Fitoplancton Marino, Inst Ciencias Mar & Limnol, Mexico City 04510, DF, Mexico	Universidad Nacional Autonoma de Mexico	Univ Nacl Autonoma Mexico, Lab Divers & Ecol Fitoplancton Marino, Inst Ciencias Mar & Limnol, Apso Postal 70-305, Mexico City 04510, DF, Mexico.	dhernand@mar.icmyl.unam.mx						Abboud-Abi Saab M., 1989, Lebanese Science Bulletin, V5, P5; ALLEN WINFRED EMORY, 1941, AMER MIDLAND NAT, V26, P603, DOI 10.2307/2420738; [Anonymous], 2003, PLANCTOLOG A MEXICAN; [Anonymous], 1970, MEMOIRS HOURGLASS CR; BALECH E, 1988, PUBLICACIONES ESPECI, V1, P310; Berard-Therriault L., 1999, Publication speciale canadienne des sciences halieutiques et aquatiques, V128, P387, DOI DOI 10.1046/j.1469-1809.1999.6320101.x; Bollmann J, 2002, MAR MICROPALEONTOL, V44, P163, DOI 10.1016/S0377-8398(01)00040-8; BURSA AS, 1969, J PROTOZOOL, V16, P411, DOI 10.1111/j.1550-7408.1969.tb02290.x; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; Fensome R.A., 1993, Micropaleontology Press Special Paper; Gómez F, 2003, J MAR BIOL ASSOC UK, V83, P173, DOI 10.1017/S0025315403006945h; GOMEZ F, 2003, 7 INT C MOD FOSS DIN, P40; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HANSEN G, 1993, J PHYCOL, V29, P486, DOI 10.1111/j.1529-8817.1993.tb00150.x; HANSEN G, 1992, PLANKTON INDRE DANSK, P45; HERNANDEZ-BECERRIL D U, 1988, Investigacion Pesquera (Barcelona), V52, P517; HERNANDEZ-BECERRIL D U, 1988, Revista Latinoamericana de Microbiologia, V30, P187; Hernandez-Becerril David U., 1991, Anales del Instituto de Ciencias del Mar y Limnologia Universidad Nacional Autonoma de Mexico, V18, P77; HERNANDEZBECERRIL DU, 1988, BOT MAR, V31, P423, DOI 10.1515/botm.1988.31.5.423; HERNANDEZBECERRIL DU, 1992, REV BIOL TROP, V40, P101; HERNANDEZBECERRIL DU, 1989, NOVA HEDWIGIA, V48, P33; INOUYE I, 1983, S AFR J BOT, V2, P63, DOI 10.1016/S0022-4618(16)30147-4; KOFOID CA, 1907, ZOOL HARVARD COLL, V50, P163; KONOVALOVA GV, 1998, DINOFLAGELLATAE DINO, P299; LARSEN J, 1991, SYST ASSOC SPEC VOL, V45, P313; LEGER G, 1972, Bulletin de l'Institut Oceanographique (Monaco), V70, P1; Licea S., 1995, DINOFLAGELADAS GOLFO, P165; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; NIVAL P, 1969, Protistologica, V5, P125; ORR W N, 1976, Micropaleontology (New York), V22, P92, DOI 10.2307/1485323; OSIRIOTAFALL BF, 1942, AN ESC NAC CIENC BIO, V2, P435; OSTERGAARD M, 1998, J PHYCOL, V34, P558; Schiller J., 1937, DINOFLAGELLATAE P 10, VII, P589; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; SOURNIA A, 1991, J PLANKTON RES, V13, P1093, DOI 10.1093/plankt/13.5.1093; SOURNIA A, 1972, Phycologia, V11, P71, DOI 10.2216/i0031-8884-11-1-71.1; SOURNIA A, 1979, BOT MAR, V22, P183, DOI 10.1515/botm.1979.22.3.183; Sournia A., 1986, ATLAS PHYTOPLANCTON, VI, P216; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; TAYLOR F. J. R., 1963, JOUR S AFRICAN BOT, V29, P75; TAYLOR FJ.R., 1987, BIOL DINOFLAGELLATES, P1; Throndsen Jahn, 1997, P591, DOI 10.1016/B978-012693018-4/50007-0; WILLIAMS GL, 1998, AASP CONTRIBUTIONS S, V34, P351	45	24	26	0	8	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055	1437-4323		BOT MAR	Bot. Marina		2004	47	5					417	423		10.1515/BOT.2004.051	http://dx.doi.org/10.1515/BOT.2004.051			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	876AS					2025-03-11	WOS:000225468300009
C	Edinger, JE; Boatman, CD; Kolluru, VS		Spaulding, ML		Edinger, JE; Boatman, CD; Kolluru, VS			Influence of multi algal groups in the calibration of a water quality model	ESTUARINE AND COASTAL MODELING, PROCEEDINGS			English	Proceedings Paper	8th International Conference on Estuarine and Coastal Modeling	NOV 03-05, 2003	Monterey, CA				DINOFLAGELLATE; AREA	A management tool based on scientific inquiry rather than politics is needed for policy makers to make environmentally sound decisions regarding difficult issues, which will only occur more frequently as coastal populations continue to increase. Typically, a well-calibrated hydrodynamic and water quality model is used as the management tool. The development of a water quality and circulation model is based on field data that encompasses the factors affecting the water body, and the model is used to evaluate the potential effects of changing point source loadings under varying operational and environmental conditions. The level of predictability depends on the goodness of field data needed for model calibration and for setting up input data, assuming all the relevant water quality processes are simulated correctly. But there are times when good field data are available, yet the calibration is not good. In such a situation, it is conventional to revisit the algorithms used for the various water quality processes. This approach was attempted in a recent project where a three-dimensional hydrodynamic and water quality model called GEMSS was applied to predict the quality of water in the Budd Inlet, located in the Southern Puget Sound (Washington, USA). Within GEMSS, the use of the water quality model called WQDPM, which is a modified version of EPA's Eutro5 water quality model, did not predict the vertical structure of dissolved oxygen and phytoplankton at different locations in the Budd Inlet. The phytoplankton was modeled in Eutro5 as a single algal group. In order to improve the calibration, the alternate water quality model called WQCBM available in GEMSS was used. This model includes different forms of organic carbon that can be related to sediment exchange processes. WQCBM simulates five interacting subsystems: net phytoplankton production, the phosphorus cycle, the nitrogen cycle, the dissolved oxygen balance, and the particulate organic carbon balance. The carbon based model was updated to include dinoflagellates and diatoms for the simulation of phytoplankton dynamics. The ability of dinoflagellates to undergo diel vertical migration and to actively take up nutrients at night greatly improved the prediction of dissolved oxygen and chlorophyll vertical structures. The concept of using spores and cysts as primary sources for algal blooming is discussed using numerical tank simulations.	JE Edinger Assoc, Wayne, PA USA		JE Edinger Assoc, Wayne, PA USA.							Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; Cerco C.F., 2000, Water Qual. Ecosyst. Model, V1, P5, DOI [10.1023/A:1013964231397, DOI 10.1023/A:1013964231397]; CULLEN JJ, 1983, MAR BIOL, V62, P81; Edinger J. E., 2002, WATERBODY HYDRODYNAM; Edinger JE, 2003, WATER AIR SOIL POLL, V147, P163, DOI 10.1023/A:1024576916233; EPPLEY RW, 1968, J PHYCOL, V4, P333, DOI 10.1111/j.1529-8817.1968.tb04704.x; Godhe A, 2002, MAR ECOL PROG SER, V240, P71, DOI 10.3354/meps240071; GODHE A, 2003, IN PRESS AQUATIC MIC; Godhe Anna, 2002, Harmful Algae, V1, P361, DOI 10.1016/S1568-9883(02)00053-7; Greer SP, 2002, J PHYCOL, V38, P116, DOI 10.1046/j.1529-8817.2002.00178.x; HARRIS GP, 1979, FRESHWATER BIOL, V9, P413, DOI 10.1111/j.1365-2427.1979.tb01526.x; KAMYKOWSKI D, 1986, J PLANKTON RES, V8, P275, DOI 10.1093/plankt/8.2.275; KAMYLKOWSKI D, 1988, LIMNOL OCEANOGR, V33, P55; KOLLURU VS, 2003, ASCE EST COAST MOD C; KOLLURU VS, 2001, TECHNICAL DOCUMENTAT; KRALLIS GA, 2002, ASCE ENG MECH DIV C; Mcgillicuddy DJ, 2003, J PLANKTON RES, V25, P1131, DOI 10.1093/plankt/25.9.1131; TYLER MA, 1978, LIMNOL OCEANOGR, V23, P227, DOI 10.4319/lo.1978.23.2.0227; WU J, 1998, P MIDATL IND WAST C; YAMAZAKI H, 1991, DEEP-SEA RES, V38, P219, DOI 10.1016/0198-0149(91)90081-P	20	0	0	0	1	AMER SOC CIVIL ENGINEERS	NEW YORK	UNITED ENGINEERING CENTER, 345 E 47TH ST, NEW YORK, NY 10017-2398 USA			0-7844-0734-7				2004							388	406						19	Engineering, Civil; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S)	Engineering; Marine & Freshwater Biology	BBW43					2025-03-11	WOS:000228129600025
J	Joyce, LB; Pitcher, GC				Joyce, LB; Pitcher, GC			Encystment of <i>Zygabikodinium lenticulatum</i> (Dinophyceae) during a summer bloom of dinoflagellates in the southern Benguela upwelling system	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Zygabikodinium lenticulatum; encystment; upwelling; dinoflagellate bloom; southern Benguela	LIFE-CYCLE; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; CYST PRODUCTION; ONAGAWA BAY; RED TIDE; SCRIPPSIELLA; GERMINATION; SEXUALITY; SINKING	A sediment trap was placed off Lambert's Bay in the southern Benguela upwelling system for 20 days in March 2001 to investigate the flux of dinoflagellate cysts from the upper mixed layer. A dinoflagellate bloom dominated by the small autotroph Gyrodinium zeta, developed in late March in association with intense stratification of the water column. The bloom included several heterotrophic species, in particular Zygabikodinium lenticulatum. The mass sedimentation of cysts of Z. lenticulatum, indicated by their dominance in the sediment trap, coincided with the maximum abundance of the vegetative stage. Observations of few cysts in the upper mixed layer indicated that cysts were formed over a short period and sank rapidly in the water column. Current patterns revealed predominantly northward flow in surface waters and southward flow in bottom waters, with current shear noticeable between 20 and 30 m depth. The formation of cysts by Z. lenticulatum under these patterns of flow serves to retain the population, preventing washout from the coastal environment. Analysis of sediment samples revealed that Z. lenticulatum also dominated the cyst assemblage of the sediments. Experimental results indicated a dormancy period of approximately 48 days, however, only a small fraction of cysts (20-28%) germinated under experimental conditions. (C) 2003 Elsevier Ltd. All rights reserved.	Marine & Coastal Management, ZA-8012 Cape Town, South Africa; Univ Cape Town, Dept Zool, ZA-7701 Cape Town, South Africa	University of Cape Town	Marine & Coastal Management, Private Bag X2,Rogge Bay, ZA-8012 Cape Town, South Africa.	ljoyce@mcm.wcape.gov.za						ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; 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 DM, 1984, AM CHEM SOC, V11, P125; ANDERSON DM, 1998, US LIMNOLOGY OCEANOG, V42, P1009; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; BINDER BJ, 1987, J PHYCOL, V23, P99; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Dale B., 1983, P69; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; 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; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; 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; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; KINGSTON P, 1989, MARINE POLLUTION B, V20, P119; 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; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V44, P217; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Mosterd S.A., 1983, S AFR J MAR SCI, V1, P189, DOI [10.2989/025776183784447584, DOI 10.2989/025776183784447584]; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Nehring S., 1993, INTERDISCIPLINARY DI, P454; Parsons TR, 1984, MANUAL CHEM BIOL MET; PFEISTER LA, 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; Pitcher G.C., 1986, South African Journal of Marine Science, V4, P231, DOI [10.2989/025776186784461657, DOI 10.2989/025776186784461657]; 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; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175	41	21	21	0	4	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.	JAN	2004	59	1					1	11		10.1016/j.ecss.2003.07.001	http://dx.doi.org/10.1016/j.ecss.2003.07.001			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	763WN					2025-03-11	WOS:000188123600001
J	MacKenzie, L; de Salas, M; Adamson, J; Beuzenberg, V				MacKenzie, L; de Salas, M; Adamson, J; Beuzenberg, V			The dinoflagellate genus <i>Alexandrium</i> (Halim) in New Zealand coastal waters:: comparative morphology, toxicity and molecular genetics	HARMFUL ALGAE			English	Article						Alexandrium; dinoflagellates; morphology; toxicity; molecular genetics	PARALYTIC SHELLFISH TOXINS; SP-NOV DINOPHYCEAE; OSTENFELDII DINOPHYCEAE; SPECIES COMPLEX; NORTH-AMERICAN; IDENTIFICATION; TAMARENSE; DNA; PCR; HETEROGENEITY	Morphological descriptions, toxicity data and an analysis of LSU rRNA gene sequences are presented for seven species within the marine dinoflagellate genus Alexandrium (Halim), identified in New Zealand coastal waters. All species were established in culture and comparison of their morphology with descriptions from the literature showed these isolates to correspond to the previously described taxa: A. catenella,A. tamarense,A.fraterculus,A. concavum,A. ostenfeldii,A. margalefi and A. pseudogoniaulax. With the exception of A. ostenfeldii, none of these species has previously been recorded in New Zealand. Most of these species are widespread and common, though they are rarely abundant, A. fraterculus has been the most frequent bloom former. Three species, A. catenella, A. tamarense, A. ostenfeldii, produced paralytic shellfish poisoning (PSP) toxins but to date only A. catenella has been associated with a significant shellfish-toxin contamination event. A. catenella and A. tamarense isolates produced toxin profiles predominating in low specific toxicity N-sulfo-carbamoyl analogues, and had identical LSU rRNA gene sequences which place them within the Pacific/Asian clade. The formation of putative hypnozygotes in mating experiments between A. tamarense and some A. catenella isolates suggested these were sexually compatible. However, although >70% of these cysts germinated, the survival of the progeny was poor. A. pseudogoniaulax and A. concavum are the most distantly related to other species within the genus. (C) 2004 Elsevier B.V. All rights reserved.	Cawthron Inst, Nelson, New Zealand; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	Cawthron Institute; University of Tasmania	Cawthron Inst, Private Bag 2, Nelson, New Zealand.	lincoln.mackenzie@cawthron.org.nz						Adachi M, 1996, J PHYCOL, V32, P1049, DOI 10.1111/j.0022-3646.1996.01049.x; Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Anderson DM, 1999, J PHYCOL, V35, P870, DOI 10.1046/j.1529-8817.1999.3540870.x; [Anonymous], 1996, HARMFUL TOXIC ALGAL; Balech E., 1985, P33; BALECH E, 1989, PHYCOLOGIA, V28, P206, DOI 10.2216/i0031-8884-28-2-206.1; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Band-Schmidt CJ, 2003, PHYCOLOGIA, V42, P261, DOI 10.2216/i0031-8884-42-3-261.1; BATES M, 1993, MISC S RSNZ, V24, P35; Benavides H., 1995, P113; Biecheler B., 1952, Bull. Biol. Fr. 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J	Sombrito, EZ; Bulos, AD; Maria, EJS; Honrado, MCV; Azanza, RV; Furio, EF				Sombrito, EZ; Bulos, AD; Maria, EJS; Honrado, MCV; Azanza, RV; Furio, EF			Application of <SUP>210</SUP>Pb-derived sedimentation rates and dinoflagellate cyst analyses in understanding <i>Pyrodinium bahamense</i> harmful algal blooms in Manila Bay and Malampaya Sound, Philippines	JOURNAL OF ENVIRONMENTAL RADIOACTIVITY			English	Article; Proceedings Paper	Conference of the South-Pacific-Environmental-Radioactivity-Association	MAY 13-17, 2002	Sydney, AUSTRALIA	S Pacific Environm Radioact Assoc		Pyrodinium bahamense var. compressum; harmful algal bloom; Pb-210-derived sedimentation rates; algal cysts; Manila Bay; Malampaya Sound	PB-210	The number of areas affected by toxic harmful algal bloom (HAB) in the Philippines has been increasing since its first recorded occurrence in 1983. Thus far, HAB has been reported in about 20 areas in the Philippines including major fishery production areas. The HAB-causing organism (Pyrodinium bahamense var. compressurn) produces a cyst during its life cycle. Pyrodinium cysts which are deposited in the sediment column may play a role in initiating a toxic bloom. Pb-210-derived sedimentation rate studies in the two important fishing grounds of Manila Bay and Malampaya Sound, Palawan have shown that Pyrodinium cysts may have been present in the sediment even before the first recorded toxic algal bloom in these areas. High sedimentation rates (approximately I cm/year) have been observed in the Northern and Western parts of Manila Bay. The results indicate that the sedimentation processes occurring in these bays would require subsurface cyst concentration analysis in evaluating the potential of an area to act as seed bed. (C) 2004 Elsevier Ltd. All rights reserved.	Philippine Nucl Res Inst, Quezon City 1101, Philippines; Univ Philippines, Marine Sci Inst, Quezon City 1101, Philippines; Bur Fisheries & Aquat Resources, Quezon City, Philippines	Philippine Nuclear Research Institute; University of the Philippines System; University of the Philippines Diliman	Sombrito, EZ (通讯作者)，Philippine Nucl Res Inst, Commonwealth Ave, Quezon City 1101, Philippines.	ezsombrito@pnri.dost.gov.ph	Azanza, Rhodora/HGU-5811-2022					Anderson D.M., 1984, SEAFOOD TOXINS, V262, P125; ANDERSON DM, 1989, ICLARM CONT, V21, P81; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; [Anonymous], 1996, HARMFUL TOXIC ALGAL; BORJA VM, 2000, HAB 2000 C TASM AUST; BRUGAM RB, 1978, QUATERNARY RES, V9, P349, DOI 10.1016/0033-5894(78)90038-8; Corrales R.A., 1995, P573; Dale B., 1983, P69; *EMB DENR, 1991, REP MAN BAY MON PROG; Estudillo RA, 1987, Philippine Journal of Fisheries, V20, P1; FURIO EF, 2000, DISTRIBUTION PYRODIN; Goldberg E.D., 1963, RADIOACTIVE DATING I, P121; Matsuoka K., 1989, P461; McMinn A., 2001, ANSTO Environment Workshop: Archives of Human Impact of the Last 200 years, P54; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; ROBBINS JA, 1975, GEOCHIM COSMOCHIM AC, V39, P285, DOI 10.1016/0016-7037(75)90198-2; SMITH JN, 1980, GEOCHIM COSMOCHIM AC, V44, P225, DOI 10.1016/0016-7037(80)90134-9; SOMBRITO EZ, 2001, PHILIPP NUCL J, V13, P1; USUP G, 1998, NATO ASI SER, P81; Villanoy C. L, 1996, HARMFUL TOXIC ALGAL, P189; YNIGUEZ AT, 2000, HAB 2000 C TASM AUST	21	21	23	1	8	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0265-931X			J ENVIRON RADIOACTIV	J. Environ. Radioact.		2004	76	1-2			SI		177	194		10.1016/j.jenvrad.2004.03.025	http://dx.doi.org/10.1016/j.jenvrad.2004.03.025			18	Environmental Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	844LJ	15245847				2025-03-11	WOS:000223159400011
C	Harding, IC; Trippier, S; Steele, J		Walker, EA; WenbanSmith, F; Healy, F		Harding, IC; Trippier, S; Steele, J			The provenancing of flint artefacts using palynological techniques	LITHICS IN ACTION	LITHIC STUDIES SOCIETY OCCASIONAL PAPER		English	Proceedings Paper	Conference on Lithic Studies in the Year 2000	SEP, 2000	Natl Museum & Gallery, Cardiff, WALES	Litthic Studies Soc	Natl Museum & Gallery		DINOFLAGELLATE CYST BIOSTRATIGRAPHY; ARCHAEOLOGICAL SITES; MINE PRODUCTS; CHERT; IDENTIFICATION; RECOGNITION; ACTIVATION; ENGLAND; AXES	The provenancing of flint artefacts has proved problematic in the past. Acid maceration to extract age-diagnostic organic-walled microplankton from sedimentary materials is a technique routinely employed in both industrial hydrocarbon exploration and Quaternary studies. Here we assess the application of this technique to provenance determination of flint nodules from three locations (two in southern England and one in the Inner Hebrides, Scotland), each of which has abundant local evidence of flint utilization for artefact manufacture in prehistory. We show that, whilst not all flint nodules yield abundant or well preserved organic-walled microfossil assemblages, there is a significant potential for the use of this technique, which deserves further investigation.	Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England	NERC National Oceanography Centre; University of Southampton			Harding, Ian/K-3320-2012	Harding, Ian/0000-0003-4281-0581				ANDERTON R., 1979, DYNAMIC STRATIGRAPHY; [Anonymous], 1994, MEMOIRES SERVIR EXPL; [Anonymous], MUNCHNER GEOWISSEN A; ASPINALL A, 1972, ARCHAEOMETRY, V14, P41, DOI 10.1111/j.1475-4754.1972.tb00049.x; BRISTOW CR, 1990, BRIT GEOLOGICAL SURV, V189; BROOKS I.P., 1989, Breaking the stony silence: papers from the Sheffield Lithics Conference 1988, P53; BROOKS IP, 1989, THESIS U SHEFFIELD; Cackler PR, 1999, J ARCHAEOL SCI, V26, P389, DOI 10.1006/jasc.1998.0340; Carson G.A., 1987, GEOLOGICAL SOC LONDO, V36, P87; Costa L.I., 1992, P99; CRADDOCK PT, 1983, ARCHAEOMETRY, V25, P135, DOI 10.1111/j.1475-4754.1983.tb00672.x; DEBRUIN M, 1972, ARCHAEOMETRY, V14, P55, DOI 10.1111/j.1475-4754.1972.tb00050.x; DEFLANDRE G, 1966, GALLIA PREHISTOIRE, V9, P380; Deflandre G., 1936, Annales de paleontologie, V25, P151; EHRENBERG CG, 1838, KONIGLICHE AKAD WISS, P109; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fitzpatrick MEJ, 1995, CRETACEOUS RES, V16, P757, DOI 10.1006/cres.1995.1048; Foucher J.-C., 1976, Revue Micropaleont, V18, P213; Foucher J.-C., 1979, Palaeontographica Abteilung B Palaeophytologie, V169, P78; Foucher J.-C., 1981, Cretaceous Research, V2, P331, DOI 10.1016/0195-6671(81)90021-5; Glover J. E., 1993, Journal of the Royal Society of Western Australia, V76, P41; GOWLETT JAJ, 2000, J HUM EVOL, V38, P13; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; HOARD RJ, 1993, AM ANTIQUITY, V58, P698, DOI 10.2307/282203; JARVIS I, 1987, MICROPALAEONTOLOGY C, P138; Jarvis I., 1987, Proceedings of the Geologists' Association, V98, P51; JULIG PJ, 1991, ARCHAEOMETRY 90, P435; Larick RR., 1986, SCI STUDY FLINT CHER, P111; Lejeune-Carpentier M., 1938, Annales de la Societe gdologique de Belgique, V62, pB163; Louwye Stephen, 1995, Annales de la Societe Geologique de Belgique, V118, P147; Luedtke BarbaraE., 1992, An Archaeologist's Guide to Chert and Flint; LUEDTKE BE, 1979, AM ANTIQUITY, V44, P744, DOI 10.2307/279116; LUEDTKE BE, 1978, AM ANTIQUITY, V43, P413, DOI 10.2307/279398; Markham M, 1998, PROC USSHER, V9, P218; MARSHALL GD, 2001, MACDONALD I MONOGRAP, P75; MAUGER M, 1984, B SOC PREHISTORIQUE, V80, P228; MITHEN S, 2001, SO HEBRIDES MESOLITH; Pollock SG, 1999, J ARCHAEOL SCI, V26, P269, DOI 10.1006/jasc.1998.0335; Prince IM, 1999, REV PALAEOBOT PALYNO, V105, P143, DOI 10.1016/S0034-6667(98)00077-3; REID KC, 1984, 2 SO ILL U CTR ARCH, P253; Shackley MS, 1998, J ARCHAEOL SCI, V25, P259, DOI 10.1006/jasc.1997.0247; SIEVEKIN.GD, 1970, NATURE, V228, P251, DOI 10.1038/228251a0; SIEVEKING GD, 1972, ARCHAEOMETRY, V14, P151, DOI 10.1111/j.1475-4754.1972.tb00061.x; Surmely F, 1998, CR ACAD SCI II A, V326, P595, DOI 10.1016/S1251-8050(98)80212-7; TINGLE M., 1998, Archaeological Journal, V155, P292; Tocher B.A., 1987, P138; Valensi L, 1955, BULL SOC PREHIST FR, V52, P584, DOI 10.3406/bspf.1955.3263; Valensi L., 1960, Bulletin de la Societe Prehistorique Franqaise, V57, P80; Wetzel O., 1933, PALAEONTOGRAPHICA, V77, P141; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817; WILSON HE, 1981, GEOLOGY IRELAND, P201; Wrenn J.H., 1996, 9 INT PAL C HOUST TE, P176; YUN H-S, 1981, Palaeontographica Abteilung B Palaeophytologie, V177, P1	53	6	6	0	4	OXBOW BOOKS	OXFORD	PARK END PLACE, OXFORD OX1 1HN, ENGLAND			1-84217-130-5	LITHIC STUD SOC OCC			2004		8					78	88						11	Anthropology; Archaeology	Conference Proceedings Citation Index - Social Science &amp; Humanities (CPCI-SSH)	Anthropology; Archaeology	BBW81					2025-03-11	WOS:000228177600009
J	Olli, K; Neubert, MG; Anderson, DM				Olli, K; Neubert, MG; Anderson, DM			Encystment probability and encystment rate: new terms to quantitatively describe formation of resting cysts in planktonic microbial populations	MARINE ECOLOGY PROGRESS SERIES			English	Article						life cycle; encystment; cyst yield; population dynamics; dinoflagellates	DINOFLAGELLATE GONYAULAX-TAMARENSIS; LIFE-CYCLE; GYRODINIUM-UNCATENUM; ALEXANDRIUM-TAMARENSE; TOXIC DINOFLAGELLATE; DINOPHYCEAE; TEMPERATURE; GERMINATION; EXCYSTMENT; SEXUALITY	Many dinoflagellates and other groups of phytoplankton have benthic resting cysts as part of their life cycle. Details of transitions among life cycle stages are few in the literature and often do not meet the rigorous standards needed for across-species generalisations or model parameterisation. One regularly reported but poorly understood aspect is the cyst yield, a quantitative characterisation of cyst formation in relation to the size of the vegetative population. The literature provides various formulae for calculating cyst yield; however, not all of these give biologically meaningful results, Here we introduce 2 new terms, 'encystment probability' and 'encystment rate' to quantitatively describe and easily calculate the average cyst formation potential of a population during a given time interval. Encystment probability (phi) is defined as the average probability of vegetative cells in a population switching to sexual reproduction (i.e. transforming into gametes which subsequently fuse to form planozygotes) as opposed to continuing vegetative growth through binary fission. Encystment rate (epsilon) is an exponential loss rate from the vegetative population; it is the difference between the instantaneous growth rate of the population (mu) and the apparent increase of the vegetative cell population (mu - epsilon), provided no other losses take place. We propose a method of calculating encystment rate and encystment probability from readily available variables such as the number of vegetative cells at the beginning and end of a time interval and the number of resting cysts formed during the same period.	Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; Univ Tartu, Inst Bot & Ecol, EE-51005 Tartu, Estonia	Woods Hole Oceanographic Institution; University of Tartu	Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	kalle.olli@ut.ee	Olli, Kalle/G-5389-2010					AGBETI MD, 1995, J PHYCOL, V31, P70, DOI 10.1111/j.0022-3646.1995.00070.x; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; 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; BINDER BJ, 1987, J PHYCOL, V23, P99; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; CAIN JR, 1976, J PHYCOL, V12, P383, DOI 10.1111/j.0022-3646.1976.00383.x; CETTA CM, 1990, J EXP MAR BIOL ECOL, V135, P69, DOI 10.1016/0022-0981(90)90199-M; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Dale B., 1983, P69; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; GREEN JC, 1982, BRIT PHYCOL J, V17, P363, DOI 10.1080/00071618200650381; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Head M.J., 1996, Palynology: Principles and Applications, P1197; 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; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; LEWIS J, 2002, LIFEHAB LIFE HIST MI, V12, P49; Li RH, 1997, J PHYCOL, V33, P576, DOI 10.1111/j.0022-3646.1997.00576.x; LIRDWITAYAPRASIT T, 1990, J PHYCOL, V26, P299, DOI 10.1111/j.0022-3646.1990.00299.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; NAKAMURA Y, 1990, Journal of the Oceanographical Society of Japan, V46, P35, DOI 10.1007/BF02124813; OKELLEY JC, 1983, J PHYCOL, V19, P57, DOI 10.1111/j.0022-3646.1983.00057.x; Olli K, 1996, J PHYCOL, V32, P535, DOI 10.1111/j.0022-3646.1996.00535.x; 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, Botanical Monographs (Oxford), V21, P611; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; SMETACEK VS, 1985, MAR BIOL, V84, P239, DOI 10.1007/BF00392493; TRIEMER RE, 1980, J PHYCOL, V16, P46, DOI 10.1111/j.0022-3646.1980.00046.x; vanDok W, 1997, J PHYCOL, V33, P12; VANSTOSCH HA, 1973, BR PHYCOL J, V8, P105; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; YOSHIMATSU S, 1987, Bulletin of Plankton Society of Japan, V34, P25	37	14	15	0	8	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2004	273						43	48		10.3354/meps273043	http://dx.doi.org/10.3354/meps273043			6	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	838CQ		Bronze			2025-03-11	WOS:000222691100004
J	Barnard, R; Batten, S; Beaugrand, G; Buckland, C; Conway, DVP; Edwards, M; Finlayson, J; Gregory, LW; Halliday, NC; John, AWG; Johns, DG; Johnson, AD; Jonas, TD; Lindley, JA; Nyman, J; Pritchard, P; Reid, PC; Richardson, AJ; Saxby, RE; Sidey, J; Smith, MA; Stevens, DP; Taylor, CM; Tranter, PRG; Walne, AW; Wootton, M; Wotton, COM; Wright, JC				Barnard, R; Batten, S; Beaugrand, G; Buckland, C; Conway, DVP; Edwards, M; Finlayson, J; Gregory, LW; Halliday, NC; John, AWG; Johns, DG; Johnson, AD; Jonas, TD; Lindley, JA; Nyman, J; Pritchard, P; Reid, PC; Richardson, AJ; Saxby, RE; Sidey, J; Smith, MA; Stevens, DP; Taylor, CM; Tranter, PRG; Walne, AW; Wootton, M; Wotton, COM; Wright, JC		Continuous Plankton Recorder	Continuous plankton records: Plankton atlas of the North Atlantic Ocean (1958-1999). II. Biogeographical charts	MARINE ECOLOGY PROGRESS SERIES			English	Article							SEA; ABUNDANCE; CYSTS	The following CPR Atlas contains the biogeographical distribution of 240 common pelagic plankton taxa of the North Sea and North Atlantic Ocean. The biogeographical charts were produced using data collected by the Continuous Plankton Recorder (CPR) survey from 1958 to 1999, incorporating over 155 000 plankton samples. The methodology on spatial interpretation of CPR data and protocols of the CPR survey are fully described in Beaugrand (2004, this volume). The charts are printed in alphabetical order of the genera within each major taxon. Nomenclature for diatoms is based on Hasle & Syvertsen (1996), for dinoflagellates on Steidinger & Tangen (1996), and for copepods on Park (1995) and Mauchline (1998). Details on selected taxa (indicated by * on the charts) are given following the index of the charts.	Sir Alister Hardy Fdn Ocean Sci, The Laboratory, Plymouth PL1 2PB, Devon, England		Barnard, R (通讯作者)，Sir Alister Hardy Fdn Ocean Sci, The Laboratory, Citadel Hill, Plymouth PL1 2PB, Devon, England.		Stevens, Darren/A-9110-2015; BEAUGRAND, GREGORY/LWI-2327-2024; Richardson, Anthony/B-3649-2010	Wootton, Marianne/0000-0003-2553-6322; Richardson, Anthony/0000-0002-9289-7366; BEAUGRAND, GREGORY/0000-0002-0712-5223; Edwards, Martin/0000-0002-5716-4714				BAINBRIDGE V., 1963, BULL MARINE ECOL, V6, P40; Beaugrand G, 2004, MAR ECOL PROG SER, P3; COLEBROOK JM, 1982, J PLANKTON RES, V4, P435, DOI 10.1093/plankt/4.3.435; COOMBS S H, 1980, Bulletins of Marine Ecology, V8, P229; COOPER G. A., 1963, BULL MAR ECOL, V6, P31; Edwards M, 2001, J MAR BIOL ASSOC UK, V81, P207, DOI 10.1017/S0025315401003654; FROST BW, 1989, CAN J ZOOL, V67, P525, DOI 10.1139/z89-077; GIESKES W W C, 1971, Netherlands Journal of Sea Research, V5, P342, DOI 10.1016/0077-7579(71)90017-2; GIESKES W W C, 1971, Netherlands Journal of Sea Research, V5, P377, DOI 10.1016/0077-7579(71)90018-4; Hasle Grethe R., 1996, P5, DOI 10.1016/B978-012693015-3/50005-X; HENDEY N.I., 1964, INTRO ACCOUNT SMALLE; HUNT H G, 1968, Bulletins of Marine Ecology, V6, P225; John A.W.G., 1987, Journal of Micropalaeontology, V6, P61; JOHN AWG, 1983, BRIT PHYCOL J, V18, P61, DOI 10.1080/00071618300650071; LINDLEY J A, 1975, Bulletins of Marine Ecology, V8, P201; LINDLEY JA, 1989, OLSEN INT S, P407; LINDLEY JA, 1977, J BIOGEOGR, V4, P121, DOI 10.2307/3038157; Lindley JA, 2002, MAR BIOL, V141, P153, DOI 10.1007/s00227-002-0803-z; LINDLEY JA, 1987, J MAR BIOL ASSOC UK, V67, P145, DOI 10.1017/S0025315400026424; Mauchline J, 1998, ADV MAR BIOL, V33, P1; Mchardy R. A., 1970, THESIS U EDINBURGH; OWENS NJP, 1989, J MAR BIOL ASSOC UK, V69, P813, DOI 10.1017/S0025315400032185; Park T., 1995, Bulletin of the Scripps Institution of Oceanography of the University of California, V29, P1; REES C. B., 1954, BULL MARINE ECOL, V4, P47; REES C. B., 1954, BULL MARINE ECOL, V4, P21; REID PC, 1978, NEW PHYTOL, V80, P219, DOI 10.1111/j.1469-8137.1978.tb02284.x; ROBINSON G. A., 1965, BULL MAR ECOL, V6, P141; ROBINSON GA, 1980, J MAR BIOL ASSOC UK, V60, P675, DOI 10.1017/S0025315400040364; ROSKELL J, 1975, Bulletins of Marine Ecology, V8, P185; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; WILLIAMS R, 1975, Bulletins of Marine Ecology, V8, P167; WILLIAMS R, 1981, MAR ECOL PROG SER, V4, P289, DOI 10.3354/meps004289; WILLIAMS R, 1975, Bulletins of Marine Ecology, V8, P215	33	86	98	0	31	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2004				S			11	75						65	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	812FG					2025-03-11	WOS:000220824800004
J	Roncaglia, L				Roncaglia, L			Palynofacies analysis and organic-walled dinoflagellate cysts as indicators of palaeo-hydrographic changes: an example from Holocene sediments in Skalafjord, Faroe Islands	MARINE MICROPALEONTOLOGY			English	Article						Faroe; north Atlantic ocean; holocene; hydrography; dinoflagellates; palynofacies	LATE QUATERNARY; LAST DEGLACIATION; AGE CALIBRATION; NORTH-ATLANTIC; NORDIC SEAS; EASTERN; REGION; OCEAN; EUTROPHICATION; STRATIGRAPHY	This study documents Holocene variations in organic matter deposition from ca. 6350 cal yr BC to AD 1430 in Skalafjord, Faroe Islands, and uses this information to assess palaeo-hydrographic conditions. The chronology of the interval studied is based on five AMS C-14 ages. Based on the total sedimentary organic content, the sediments dating to ca. 6350 cal yr BC to AD 160 have been deposited under dysoxic bottom water conditions suggesting good ventilation in the water column. The sediments dating to ca. AD 160-1090 have been deposited under decreasing oxygen availability; from AD 1090 to 1430, suboxic bottom water conditions characterised the fjord. High terrestrial influx characterised most sediments in the study interval; however, moderate terrestrial influx was recorded in sediments dating to ca. 6350-5670 cal yr BC. Based on the dinoflagellate cyst assemblages, changes in the nutrient availability were inferred in the waters of the fjord over the study period. The nutrients were minimal at ca. 6350-5670 cal yr BC; they increased in the interval ca. 5670-685 cal yr BC and became very abundant at ca. 695 cal yr BC to AD 1260. A decreasing trend in nutrient availability was inferred in sediments of age ca. AD 1260-1430. A qualitative approach was used for the reconstruction of Holocene sea-surface temperature conditions based on dinoflagellate cyst and acritarch assemblages. The estimated sea-surface parameters highlighted the Mid-Holocene final stage of the Climatic Optimum (ca. 6350-5300 cal yr BC), the Neo-glaciation period (ca. 5300 cal yr BC to AD 260), a general climatic amelioration during the period ca. AD 260-1090 and a cooling at ca. AD 1090-1260. (C) 2003 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.	lr@geus.dk						Andersen MS, 2000, GLOBAL PLANET CHANGE, V24, P239, DOI 10.1016/S0921-8181(00)00011-4; [Anonymous], 1999, P OCEAN DRILLING PRO; [Anonymous], DGU DATADOKUMENTATIO; [Anonymous], FISKIRANNSOKNIR; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Batten D. 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Micropaleontol.	JAN	2004	50	1-2					21	42		10.1016/S0377-8398(03)00065-3	http://dx.doi.org/10.1016/S0377-8398(03)00065-3			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	770HQ					2025-03-11	WOS:000188717500002
J	Vink, A				Vink, A			Calcareous dinoflagellate cysts in South and equatorial Atlantic surface sediments: diversity, distribution, ecology and potential for palaeoenvironmental reconstruction	MARINE MICROPALEONTOLOGY			English	Article						calcareous dinoflagellate cysts; Thoracosphaera heimii; South Atlantic; surface sediments; ecology; statistical analysis	WESTERN TROPICAL ATLANTIC; UPPER WATER COLUMN; SCRIPPSIELLA-TROCHOIDEA; THORACOSPHAERA-HEIMII; SPATIAL-DISTRIBUTION; QUATERNARY EASTERN; OCEAN; DINOPHYCEAE; SEA; CALCIODINELLOIDEAE	Several marine, peridiniphycidean dinoflagellate species produce calcareous cysts during their life cycle, which are relatively resistant to chemical and physical degradation and are therefore often found in large quantities in oceanic bottom sediments. Although the use of these calcareous cysts as proxies for palaeoenvironmental and palaeoclimatic reconstructions has seen many advances over the last decade, until now only relatively patchy and regional information was available on their recent distribution patterns and ecology, especially at the species level. In this paper, comprehensive calcareous cyst diversity and distribution data have been compiled from published and unpublished work for 167 South and equatorial Atlantic Ocean surface sediments, ranging from 20degreesN to 50degreesS, and 30degreesE to 65degreesW. The main aim has been to focus on the complex, often non-linear, relationships between individual species' distributions and the physicochemical and trophic conditions of the overlying (sub)surface waters through the use of x-y graphs of cyst abundance vs. (sub)surface water environmental parameters, and detrended correspondence analyses. Ten cyst species and the calcareous vegetative coccoid species Thoracosphaera heimii were observed in the bottom sediments, each species showing its own characteristic distribution pattern in relation to the environmental conditions of the upper water masses above them (e.g. sea surface temperature, productivity, stratification). The sensitive reactions of various species to unique combinations of environmental parameters shows that each species has its own specific ecological traits, thus rejecting the bundled use of 'calcareous cyst accumulation' as a general proxy for oligotrophy or stratification in future palaeoenvironmental analyses. The acquired 'reference' data set of this study is large and diverse enough to allow its future application in quantitative palaeoenvironmental reconstruction models, and shows that there is still an enormous reconstruction potential concealed in many fossil calcareous dinoflagellate cyst assemblages. (C) 2003 Elsevier B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissenschaften 5, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich Geowissenschaften 5, Postfach 330 440, D-28334 Bremen, Germany.	vink@micropal.uni-bremen.de	Vink, Annemiek/GXG-6435-2022	Vink, Annemiek/0000-0002-5178-9721				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; [Anonymous], BERICHTE FACHBEREICH; Beaufort L, 1997, SCIENCE, V278, P1451, DOI 10.1126/science.278.5342.1451; BERGER WH, 1985, PALAEOGEOGR PALAEOCL, V50, P167; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; Bleil U., 2001, BERICHTE FACHBEREICH, V172, P1; BLEIL U, 1998, BERICHTE FACHBEREICH, V95, P1; BLEIL U, 1996, BERICHTE FACHBEREICH, V77, P1; Boltovskoy E, 1996, MAR MICROPALEONTOL, V28, P53, DOI 10.1016/0377-8398(95)00076-3; COSTAS E, 1989, CHRONOBIOLOGIA, V16, P265; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DALE B, 1992, OCEAN BIOCOENOSIS SE, V5, P33; DEVEY CW, 1999, BERICHTE FACHBEREICH, V137, P1; EKAU W, 1991, BRAZILIAN GERMAN V H; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; FISCHER G, 1999, BERICHTE FACHBEREICH, V130, P1; FISCHER G, 1998, BER FACHBEREICH GEOW, V94, P1; GILBERT MW, 1983, MAR MICROPALEONTOL, V7, P385, DOI 10.1016/0377-8398(83)90017-8; GINGELE F, 1994, PALEOCEANOGRAPHY, V9, P151, DOI 10.1029/93PA02559; GROOTES PM, 1993, NATURE, V366, P552, DOI 10.1038/366552a0; HEMLEBEN C, 1998, 982 METEOR I MEER U, P1; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; HONJO S, 1976, MAR MICROPALEONTOL, V1, P65, DOI 10.1016/0377-8398(76)90005-0; Imbrie J., 1971, LATE CENOZOIC GLACIA, P71; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; JANOFSKE D, 2000, BERICHTE FACHBEREICH, V152, P94; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; Kamptner E., 1963, Annalen des Naturhistorischen Museums in Wien, V66, P139; KAMPTNER E, 1967, Annalen des Naturhistorischen Museums in Wien, V71, P117; 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; KERNTOPF B, 1997, BERICHTE FACHBEREICH, V103; LAMPITT RS, 1993, NATURE, V362, P737, DOI 10.1038/362737a0; Meier KJS, 2003, MAR MICROPALEONTOL, V48, P321, DOI 10.1016/S0377-8398(03)00028-8; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; MOLFINO B, 1990, SCIENCE, V249, P766, DOI 10.1126/science.249.4970.766; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Mudie P. 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Micropaleontol.	JAN	2004	50	1-2					43	88		10.1016/S0377-8398(03)00067-7	http://dx.doi.org/10.1016/S0377-8398(03)00067-7			46	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	770HQ					2025-03-11	WOS:000188717500003
J	Kurita, H				Kurita, H			Paleogene dinoflageflate cyst biostratigraphy of northern Japan	MICROPALEONTOLOGY			English	Review							SEDIMENTS; WATER	This study establishes for the first time in Japan a Paleogene dinoflagellate cyst biostratigraphic zonation, which enables dating and correlation of Paleogene shallow marine sediments in the northwestern Pacific where other marine planktonic microfossils are extremely rare. This study uses previously-dated outcrop sections in northern Japan and proposes nineteen dinoflagellate cyst biozones for the interval of the Paleocene-Lower Miocene, except the middle Middle Eocene where appropriate marine sections were not available. Comparison between assemblages from various other localities in Japan and Sakhalin Island, Far East Russia, confirms that the biostratigraphic zonation proposed here is applicable to the northern Japan and Sakhalin region. The taxonomic part describes 36 taxa that include three new species, Spinidinium pentagonum Kurita, sp. nov. from the Eocene, and Spinidinium? tripylum Kurita, sp. nov. and Williamsidinium diaphanes Kurita, sp. nov. from the Oligocene.	Japan Petr Explorat Co Ltd, JAPEX, Res Ctr, Chiba 2610025, Japan		Kurita, H (通讯作者)，Niigata Univ, Fac Sci, Dept Geol, Niigata 950 2181, Japan.	kurita@sc.niigata-u.ac.jp	Kurita, Hiroshi/KIC-0968-2024					[Anonymous], J GEOLOGICAL SOC JAP; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, Palynology: principles and applications; Asano K., 1962, Contributions from the Institute of Geology and Paleontology Tohoku University, V57, P1; BARSS MS, 1979, 7824 GEOL SURV CAN, P1; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bujak J., 1980, PALAEONTOLOGICAL ASS, V24, P1; BUJAK J P, 1986, Palynology, V10, P235; Bujak J.P., 1986, Contribution Series, V17, P7; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; BUJAK JP, 1983, AM ASS STRATIGRAPHIC, V13; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; CANDE SC, 1992, J GEOPHYS RES-SOL EA, V97, P13917, DOI 10.1029/92JB01202; CANDE SC, 1995, J GEOPHYS RES-SOL EA, V100, P6093, DOI 10.1029/94JB03098; DAVEY RJ, 1966, GEOLOGY S, V3; EATON G L, 1976, Bulletin of the British Museum (Natural History) Geology, V26, P227; Elsik W.C., 1977, Palynology, V1, P95; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Gladenkov A.Y., 1995, P OCEAN DRILLING PRO, V145, P21, DOI [10.2973/odp.proc.sr.145.105.1995, DOI 10.2973/ODP.PROC.SR.145.105.1995]; Gocht H., 1969, Palaeontogra, V126, P1; HE C-Q, 1990, Acta Micropalaeontologica Sinica, V7, P403; HE CQ, 1980, SOME NEW GENERA OLIG, P1; HE CQ, 1984, MEMOIRS NANJING I GE, V19, P143; Head Martin J., 1993, Palynology, V17, P201; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; HONDA Y, 1987, B GEOLOGICAL SURVEY, V38, P81; HOYANAGI K, 1985, EARTH SCI, V39, P74; HUZIOKA K, 1941, JUBILEE PUBLICATION, V2, P952; JIABO, 1978, PALEOGENE DINOFLAGEL; JOLLEY DW, 1992, REV PALAEOBOT PALYNO, V74, P207, DOI 10.1016/0034-6667(92)90008-5; KAIHO K, 1992, MAR MICROPALEONTOL, V18, P229, DOI 10.1016/0377-8398(92)90014-B; KAIHO K, 1984, Science Reports of the Tohoku University Second Series (Geology), V55, P1; KAIHO K, 1984, Science Reports of the Tohoku University Second Series (Geology), V54, P95; KAIHO K, 1986, P JPN ACAD B-PHYS, V62, P145, DOI 10.2183/pjab.62.145; KAIHO K, 1990, GUIDEBOOK FIELD TRIP; KAIHO K, 1984, J GEOLOGICAL SOC JAP, V90, P815; Kaiho K., 1984, BIOSTRATIGRAPHY INT, P35; KAIHO K, 1983, KASEKI, V34, P41; KAIHO K, 1984, BIOSTRATIGRAPHY INT, P49; KAIHO K, 1986, TERMINAL EOCENE EVEN, P159; KURITA H, 1994, REV PALAEOBOT PALYNO, V84, P129, DOI 10.1016/0034-6667(94)90047-7; Kurita H., 2000, J GEOGR, V109, P187; Kurita H., 2000, J JAPANESE ASS PETRO, V65, P58; KURITA H, 1998, RES REPORT JAPEX RES, V13, P11; Kurita H., 1997, J GEOL SOC JPN, V103, P1179; KURITA H, 1998, 1998 ANN M PAL SOC J, V69; KURITA H, 1996, 1996 ANN M PAL SOC J, V135; Kurita Hiroshi, 1995, Palynology, V19, P119; Kurita Hiroshi, 1994, Journal of the Geological Society of Japan, V100, P292; Kurita Hiroshi, 1998, Journal of the Geological Society of Japan, V104, P56; Kurita Hiroshi, 1998, Journal of the Geological Society of Japan, V104, P808; LENTIN J K, 1983, Palynology, V7, P147; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; MAIYA S, 1981, REPORTS RES PROJECT, P23; MAIYA S, 1981, FUNDAMENTAL DATA JAP, P38; MATSUBARA E, 1988, T JPN I MET, V29, P1, DOI 10.2320/matertrans1960.29.1; MATSUI M, 1987, COMMEMORATIVE VOLUME, P137; Matsuoka K., 1974, Transactions Proc Palaeont Soc Japan, VNo. 94, P319; MATSUOKA K, 1987, MICROPALEONTOLOGY, V33, P214, DOI 10.2307/1485638; MATSUOKA K, 1983, Palaeontographica Abteilung B Palaeophytologie, V187, P89; MATSUOKA K, 1984, BIOSTRATIGRAPHY INT, P65; Matsuoka K., 1987, Bull. 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J	Meier, KJS; Höll, C; Willems, H				Meier, KJS; Höll, C; Willems, H			Effect of temperature on culture growth and cyst production in the calcareous dinoflagellates <i>Calciodinellum albatrosianum</i>, <i>Leonella granifera</i> and <i>Pernambugia tuberosa</i>	MICROPALEONTOLOGY			English	Article; Proceedings Paper	Workshop on Extant Coccolithophorid Research	OCT, 2003	Iraklion, GREECE	Int Nannoplankton Assoc			THORACOSPHAERA-HEIMII DINOPHYCEAE; WESTERN TROPICAL ATLANTIC; SMALL-SCALE TURBULENCE; UPPER WATER COLUMN; SURFACE SEDIMENTS; SPATIAL-DISTRIBUTION; QUATERNARY EASTERN; POTENTIAL USE; LIFE-CYCLE; OCEAN	Modem and Late Quaternary oceanic assemblages of calcareous dinoflagellate cysts are often dominated by the species Calciodinellum albatrosianum, Leonella granifera and Pernambligia tuberosa. Their distribution in surface sediments of the South and equatorial Atlantic Ocean has been found to be related to a set of environmental parameters such as temperature, nutrient concentration, stratification and salinity. However, the direct influence of single parameters on the species is as yet unknown. In order to determine the effect of temperature on culture growth and cyst production, strains of the species were investigated in a temperature gradient box under controlled laboratory conditions. Whereas culture growth was observed over a relatively broad range of 12.3-30.4degreesC in C. albatrosianum, 15.5- 30.7degreesC in L. granifera, and 13.3-32.8degreesC in P. tuberosa, fossilisable cysts were mainly produced in a smaller range of 16.1-21.7degreesC in C. albatrosianum, 18.0-24.0degreesC in L. granifera and 22.3-27.6degreesC in P. tuberosa. By comparing laboratory and field data it is shown that a good correlation exists in P. tuberosa, whereas in C. albatrosianum and L. granifera higher temperatures of fossilisable cyst production were expected from the field data. As possible explanations different depths of vegetative reproduction and cyst production and seasonality in cyst production are discussed.	Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany	Natural History Museum London; University of Bremen	Nat Hist Museum, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.	S.Meier@nhm.ac.uk	Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. 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J	Versteegh, GJM; Blokker, P; Wood, GD; Collinson, ME; Damsté, JSS; de Leeuw, JW				Versteegh, GJM; Blokker, P; Wood, GD; Collinson, ME; Damsté, JSS; de Leeuw, JW			An example of oxidative polymerization of unsaturated fatty acids as a preservation pathway for dinoflagellate organic matter	ORGANIC GEOCHEMISTRY			English	Article							RUTHENIUM TETROXIDE DEGRADATION; ALGA BOTRYOCOCCUS-BRAUNII; FRESH-WATER ALGAE; CHEMICAL-STRUCTURE; LINSEED OIL; SCENEDESMUS-COMMUNIS; TETRAEDRON-MINIMUM; FLASH PYROLYSIS; ORIGIN; LIPIDS	A palynologically monotypic assemblage from the Eocene Jatta Gypsum Formation has (Pakistan) been analyzed microscopically and chemically. Scanning electron microscopy shows that the palynomorphs are solid to spongeous dinoflagellate (Division Dinophyta) remains embedded in an amorphous ground mass. Unlike dinollagellate resting and temporary cysts, a resistant outer wall is absent and the fossils are presently interpreted to be the internal contents ("dinocasts") of a motile thecate dinoflagellate. Chemical analysis shows that the microfossils are highly aliphatic and consist of polymerized free lipids, likely to have been predominantly C-18 and C-16 fatty acids with a predominantly C-9 mid-chain functionality. We suggest that these "dinocasts" have been formed post-mortem by oxidative polymerization of these lipids, derived from cellular membranes and storage vesicles. Additionally, lipids from outside may have contributed, during or after polymerization of the cell contents. Our hypothesis is supported by chemical analysis of autoxidized vegetable oil and contrasts with the generally accepted opinion that algal remains are preserved via the so-called selective preservation pathway only. In the present case, the unique morphological preservation of the "dinocasts" enabled linking of the post-mortem polymerized free lipids to their microalgal source. However, upon regular, less ideal, morphological preservation conditions such linkage is impossible since "amorphous" particles would result. We propose, therefore, that oxidative polymerization of lipids may be responsible for much more of the amorphous marine organic matter in sediments than presently acknowledged. (C) 2004 Elsevier Ltd. All rights reserved.	Hanse Wissenschaftskolleg, D-27753 Delmenhorst, Germany; Univ Utrecht, Dept Geosci, NL-3508 TA Utrecht, Netherlands; IRF Grp Inc, Katy, TX 77494 USA; Univ London Royal Holloway & Bedford New Coll, Dept Geol, Egham TW20 0EX, Surrey, England; Univ Utrecht, Dept Biol, NL-3508 TB Utrecht, Netherlands	Utrecht University; University of London; Royal Holloway University London; Utrecht University	Hanse Wissenschaftskolleg, Lehmkuhlenbusch 4, D-27753 Delmenhorst, Germany.	gerardv@nioz.nl	de Leeuw, Jan/F-6471-2011; Sinninghe Damste, Jaap/F-6128-2011; Versteegh, Gerard J.M./H-2119-2011	Sinninghe Damste, Jaap/0000-0002-8683-1854; Versteegh, Gerard J.M./0000-0002-9320-3776				Allard B, 2001, PHYTOCHEMISTRY, V57, P459, DOI 10.1016/S0031-9422(01)00071-1; [Anonymous], ACTA PALAEOBOTANIC S; Blokker P, 1998, ORG GEOCHEM, V29, P1453, DOI 10.1016/S0146-6380(98)00111-9; 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; Blom A. 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Geochem.		2004	35	10					1129	1139		10.1016/j.orggeochem.2004.06.012	http://dx.doi.org/10.1016/j.orggeochem.2004.06.012			11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	859YY					2025-03-11	WOS:000224305500006
C	Hunt, CO		Beaudoin, AB; Head, MJ		Hunt, CO			Palynostratigraphy of the classic Portland and Purbeck sequences of Dorset, southern England, and the correlation of Jurassic-Cretaceous boundary beds in the Tethyan and Boreal realms	PALYNOLOGY AND MICROPALAEONTOLOGY OF BOUNDARIES	Geological Society Special Publication		English	Proceedings Paper	Annual Meeting of the Geological-Association-of-Canada/Mineralogical-Association-of-Canada	MAY 26-29, 2002	Saskatoon, CANADA	Geol Assoc Canada, Mineral Assoc Canada			STRATA	Placement of the Jurassic-Cretaceous boundary and its correlation between the Tethyan and Boreal realms are still contentious. The distribution of stratigraphically significant dinoflagellate cysts in the Portland Stone and Purbeck formations of the Isle of Purbeck, Dorset, UK provides a basis for direct correlation between these sections and the type Berriasian in southeast France. The base of the Berriasian - and thus of the currently accepted Jurassic-Cretaceous boundary-most probably lies at the base of the Cypris Freestones in the Purbeck Formation. Miospore correlation between the Dorset sections and ammonite-bearing rocks in the Spilsby Province suggests that the base of the Cretaceous lies close to the base of the Subcraspidites preplicomphalus zone in the Boreal Realm.	Univ Huddersfield, Huddersfield HD1 3DH, W Yorkshire, England	University of Huddersfield	Univ Huddersfield, Huddersfield HD1 3DH, W Yorkshire, England.	c.o.hunt@hud.ac.uk	Hunt, Chris/AAG-3327-2020	Hunt, Chris/0000-0003-0330-8871				Abbink OA, 2001, P YORKS GEOL SOC, V53, P275, DOI 10.1144/pygs.53.4.275; Ainsworth NR, 1998, GEOL SOC SPEC PUBL, V133, P103, DOI 10.1144/GSL.SP.1998.133.01.06; ALLEN P, IN PRESS GEOLOGICAL; [Anonymous], 1996, Palynology: principles and applications; BENTON MJ, 1995, CHAPMAN HALL GCR SER; BIRKELUND T, 1983, DAN GEOL UNDERS ARBO, P53; Blanc E, 1996, CRETACEOUS RES, V17, P403, DOI 10.1006/cres.1996.0025; BRISTOW HW, 1857, VERTICAL SECTIONS GE; Casey R., 1963, S E UNION SCI SOC, V117, P1; CASEY R, 1967, P GEOL SOC LOND, V1640, P246; Casey R., 1973, BOREAL LOWER CRETACE, P193; COE AL, 1996, SPECIAL PUBLICATION, V103, P109; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Hawkes PW, 1998, GEOL SOC SPEC PUBL, V133, P39, DOI 10.1144/GSL.SP.1998.133.01.03; HEILMANN-CLAUSEN C., 1987, DANMARKS GEOLOGISKE, V17, P1; Hoedemaeker PJ, 1999, GEOL CARPATH, V50, P101; Hunt C.O., 1987, P208; HUNT C O, 1985, Pollen et Spores, V27, P419; Monteil E., 1992, Revue de Paleobiologie, V11, P273; Monteil E., 1992, Revue de Paleobiologie, V11, P299; Norris G., 1965, New Zealand Journal of Geology and Geophysics, V8, P792; NORRIS G., 1969, PALAEONTOLOGY, V12, P574; Ogg J.G., 1994, GEOBIAS, V17, P519, DOI [10.1016/S0016-6995(94)80217-3, DOI 10.1016/S0016-6995(94)80217-3, https://doi.org/10.1016/S0016-6995(94)80217-3]; OGG JG, 1986, GEOLOGY, V14, P547, DOI 10.1130/0091-7613(1986)14<547:MOTJB>2.0.CO;2; Piasecki S., 1984, Bull Geol Soc Den, V32, P154; Riding J.B., 1992, P7; SEY II, 1997, INT SUBCOMMISSION JU, V24, P50; TESTOLIN R, 1992, ACTA HORTIC, V313, P99, DOI 10.17660/ActaHortic.1992.313.11; TOWNSON WG, 1975, GEOL SOC LONDON J, V131, P619; WEST I M, 1975, Proceedings of the Geologists' Association, V86, P205; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; Wimbledon W.A., 1978, Journal of the Geological Society (London), V135, P183, DOI 10.1144/gsjgs.135.2.0183; Wimbledon W.A., 1984, INT S JUR STRAT ERL, V2, P533; WIMBLEDON WA, 1983, GEOL MAG, V120, P267, DOI 10.1017/S0016756800025450; WIMBLEDON WA, 1980, SPECIAL REPORTS GEOL, V14, P85; WIMBLEDON WA, 1986, P DORSET NATURAL HIS, V108, P127; WIMBLEDON WA, 1995, FIELD GEOLOGY BRIT J, P51; 1975, C CRETACE INFERIEUR, V86, P1	40	20	22	0	21	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		1-86239-160-2	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2004	230						175	185		10.1144/GSL.SP.2004.230.01.09	http://dx.doi.org/10.1144/GSL.SP.2004.230.01.09			11	Geology; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BBX62					2025-03-11	WOS:000228280100009
C	Gedl, P		Beaudoin, AB; Head, MJ		Gedl, P			Dinoflagellate cyst record of the deep-sea Cretaceous-Tertiary boundary at Uzgrun, Carpathian Mountains, Czech Republic	PALYNOLOGY AND MICROPALAEONTOLOGY OF BOUNDARIES	Geological Society Special Publication		English	Proceedings Paper	Annual Meeting of the Geological-Association-of-Canada/Mineralogical-Association-of-Canada	MAY 26-29, 2002	Saskatoon, CANADA	Geol Assoc Canada, Mineral Assoc Canada			CALCAREOUS NANNOFOSSIL; NORTHWEST TUNISIA; EL-KEF; SECTION; BIOSTRATIGRAPHY; EXTINCTION; PALYNOLOGY; NETHERLANDS; OLIGOCENE; SEDIMENTS	The record of organic-walled dinoflagellate cysts in deep-sea facies across the Cretaceous-Tertiary boundary is poorly known. A detailed study of uppermost Maastrichtian-lowermost Danian Tethyan deep-sea flysch sediments deposited below the carbonate compensation depth at Uzgrun, in the Czech Republic, has yielded numerous and relatively well-preserved dinoflagellate cysts. Their distribution allows the Cretaceous-Tertiary boundary to be placed within a 73 em interval, within which an iridium anomaly occurs. Assemblages show no major shifts within the boundary interval, but gradual changes were recorded that possibly relate to sea-level fluctuations and/or nutrient availability. High concentrations of peridinioids appear to indicate upwelling in this part of the Tethys near the Cretaceous Tertiary boundary. The presence of thermophilic dinoflagellate cysts throughout the section points to a stable, warm-temperate to subtropical climate during the latest Maastrichtian and earliest Danian. Events, such as the Areoligera sp. acme, Manumiella seelandica acme and the Spinidinium sp. acme, known from other Cretaceous-Tertiary boundary sections around the world, were recognized within the studied material.	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						ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], 1996, Palynology: principles and applications; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R.A., 1988, Geological Society of America Memoir, V169, P155; Askin Rosemary A., 1996, P7; Benson D.G. 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McKenzie He., 1982, GEOLOGICAL SOCIETYOF, V190, P353; Powell AJ, 1992, BRIT MICROPALAEONTOL, P155; RAUP DM, 1986, SCIENCE, V231, P833, DOI 10.1126/science.11542060; RAUP DM, 1984, P NATL ACAD SCI-BIOL, V81, P801, DOI 10.1073/pnas.81.3.801; Rauscher R., 1982, Sci. Geol. Bull., V35, P97; ROMEIN AJT, 1981, P K NED AKAD B PHYS, V84, P295; Smit J, 1996, GEOL MIJNBOUW, V75, P283; SRIVASTAVA SK, 1994, REV PALAEOBOT PALYNO, V83, P137, DOI 10.1016/0034-6667(94)90065-5; STRONG CP, 1995, NEW ZEAL J GEOL GEOP, V38, P171, DOI 10.1080/00288306.1995.9514649; WILLIAMS GL, 1998, CONTRIBUTIONS AM ASS, V28, P1; Yepes Oscar, 2001, Palynology, V25, P217, DOI 10.2113/0250217	54	22	23	0	5	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		1-86239-160-2	GEOL SOC SPEC PUBL			2004	230						257	273		10.1144/GSL.SP.2004.230.01.13	http://dx.doi.org/10.1144/GSL.SP.2004.230.01.13			17	Geology; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BBX62					2025-03-11	WOS:000228280100013
C	Gedl, P		Beaudoin, AB; Head, MJ		Gedl, P			Dinoflagellate cyst record of the Eocene-Oligocene boundary succession in flysch deposits at Leluchow, Carpathian Mountains, Poland	PALYNOLOGY AND MICROPALAEONTOLOGY OF BOUNDARIES	Geological Society Special Publication		English	Proceedings Paper	Annual Meeting of the Geological-Association-of-Canada/Mineralogical-Association-of-Canada	MAY 26-29, 2002	Saskatoon, CANADA	Geol Assoc Canada, Mineral Assoc Canada			ADJACENT SEAS; SEDIMENTS; NORTH; STRATIGRAPHY; ZONATION	Organic-walled dinoflagellate cysts from Eocene-Oligocene transitional deposits have been studied in a section at Leluchow, Flysch Carpathians, Poland. The Eocene-Oligocene boundary, as based on dinoflagellate cyst distribution, is placed in the upper part of the Leluchow Marl Member. The main biostratigraphic events associated with this boundary interval are the highest occurrence of Areosphaeridium michoudii and Areosphaeridium diktyoplokum, and the lowest occurrence of Wetzeliella gochtii. Distinct changes in dinoflagellate cyst assemblages and palynofacies across the Eocene-Oligocene boundary at Leluchow imply a drop in relative sea-level within the Carpathian flysch basin that might correlate with a major eustatic fall during the earliest Oligocene. A drop in sea surface temperature is recognized prior to the Eocene-Oligocene boundary, and evidence is presented for an increase in nutrient level and decrease in salinity within the photic zone during the earliest Oligocene.	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; BARBIN V., 1986, DEV PALEONTOLOGY STR, V9, P49, DOI DOI 10.1016/S0920-5446(08)70093-1; 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; Birkenmajer K., 1989, Annales Societatis Geologorum Poloniae, V59, P145; BLAICHER J, 1963, ASS GEOL KARP BALK 5, P67; 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, 1992, THESIS U UTRECHT; 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, 1994, J MICROPALAEONTOL, V12, P119; Chateauneuf J.-J, 1978, B BUREAU RECHERCHES, V2-1978, P55; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; COSTA LI, 1979, INITIAL REPORTS DEEP, V48, P513; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; GEDL P, 1999, PRZEGL GEOL, V47, P394; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Kothe A., 1990, GEOLOGISCHES JB A, V118, P1; KSIAZKIEWICZ M, 1977, GEOLOGY POLAND, V4, P476; Ksikiewicz M, 1959, B ACAD POL SCI, V7, P773; Leszczyski S., 1997, ANN SOC GEOL POL, V67, P367; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; OKADA H, 1980, MAR MICROPALEONTOL, V5, P321, DOI 10.1016/0377-8398(80)90016-X; OLSZEWSKA B, 1985, 13 C KBGA POL CRAC S, V1, P57; OSZCZYPKO M, 1990, STUDIA GEOLOGICA POL, V97, P109; Oszczypko Marta, 1996, Annales Societatis Geologorum Poloniae, V66, P1; Oszczypko N., 1992, GEOL CARPATH, V43, P333; Oszczypko-Clowes M, 1999, GEOL CARPATH, V50, P59; Oszczypko-Clowes Marta, 2001, Annales Societatis Geologorum Poloniae, V71, P139; Oszczypko-Clowes Marta, 1998, Slovak Geological Magazine, V4, P107; Powell AJ, 1992, BRIT MICROPALAEONTOL, P155; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rogl F., 1983, Ann. 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Wien, V85A, P135; Swidzinski H., 1961, B ACAD POL SCI SGG, V9, P109; SWIDZINSKI H, 1961, B ACAD POL SCI SGG, V9, P99; SWIDZINSKI H, 1939, B PANSTWOWEGO I GEOL, V18, P88; SWIDZINSKI H, 1934, POSIEDZENIA NAUKOWE, V39, P18; VANCOUVERING JA, 1981, PALAEOGEOGR PALAEOCL, V36, P321, DOI 10.1016/0031-0182(81)90111-5; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1993, 9210 GEOL SURV CAN, P1; WILLIAMS GL, 1998, CONTRIBUTIONS AM ASS, V28, P1; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zevenboom D., 1995, PhD Thesis Diss	46	19	20	1	1	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		1-86239-160-2	GEOL SOC SPEC PUBL			2004	230						309	324		10.1144/GSL.SP.2004.230.01.16	http://dx.doi.org/10.1144/GSL.SP.2004.230.01.16			16	Geology; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BBX62					2025-03-11	WOS:000228280100016
C	Guerstein, GR; Guler, MV; Casadío, S		Beaudoin, AB; Head, MJ		Guerstein, GR; Guler, MV; Casadío, S			Palynostratigraphy and palaeoenvironments across the Oligocene-Miocene boundary within the Centinela Formation, southwestern Argentina	PALYNOLOGY AND MICROPALAEONTOLOGY OF BOUNDARIES	Geological Society Special Publication		English	Proceedings Paper	Annual Meeting of the Geological-Association-of-Canada/Mineralogical-Association-of-Canada	MAY 26-29, 2002	Saskatoon, CANADA	Geol Assoc Canada, Mineral Assoc Canada			SANTA-CRUZ PROVINCE; DINOFLAGELLATE CYSTS; COLORADO BASIN; BIOSTRATIGRAPHY; TERTIARY; STRATIGRAPHY; CORE; AREA; AGE	Palynological analysis of the Centinela Formation, exposed in the foothills of the Patagonian Andes, has revealed the presence of pollen, dinoflagellate cysts, and chlorococcalean and prasinophycean algae. These groups are here reported from the Centinela Formation for the first time. Sporomorph and dinoflagellate cyst assemblages suggest a Late Oligocene and Early Miocene age. These results coincide with a Sr-87/Sr-86 age close to the age of the Oligocene-Miocene boundary obtained from the lower part of the section. Palynological information from the Centinela Formation permits correlation with Upper Oligocene and Lower Miocene units cropping out along the Atlantic Patagonian coast. Assemblages from the lower part of the section suggest that the beds were deposited under marine, near-shore palaeoenvironmental conditions with a strong continental influence. In the middle part of the section, high dinoflagellate cyst ratios coincide with a maximum flooding surface recorded in the Centinela Formation. Towards the top of the Centinela Formation, the sporomorph assemblages reflect the development of vegetation adapted to coastal environments, which agrees with the sparse occurrence of marine palynomorphs. A new dinoflagellate species, Hystrichostrogylon sulcatum, is proposed. This species appears to range across the Oligocene-Miocene boundary and is particularly abundant in the lowest Miocene.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.		Casadio, Silvio/A-5131-2010					Barreda V, 2000, AMEGHINIANA, V37, P103; Barreda V, 2000, AMEGHINIANA, V37, P3; Barreda VD, 1998, AMEGHINIANA, V35, P321; BARREDA VD, 2000, NEOGENO ARGENTINA CG, V14, P103; BARREDA VD, 2002, GEOLOGIA RECURSOS NA, V11, P545; Barreda Viviana D., 1997, Ameghiniana, V34, P283; Barreda Viviana D., 1996, Ameghiniana, V33, P35; Barreda Viviana D., 1993, Palynology, V17, P169; Bellosi E.S., 1995, Boletin de Informaciones Petroleras. 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K., 1994, Papers and Proceedings of the Royal Society of Tasmania, V128, P1; Malumian N., 1998, 10 C LAT GEOL 6 C NA, V1, P125; MALUMIAN N, 2002, GEOLOGFIA RECURSOS N, V15, P237; Malumian N., 1999, GEOLOGIA ARGENTINA, V29, P557; NELSON CS, 1978, NEW ZEAL J GEOL GEOP, V21, P553, DOI 10.1080/00288306.1978.10424086; Ottone E.G., 1998, REV ESP MICROPALEONT, V30, P35; Palamarczuk S, 1998, AMEGHINIANA, V35, P415; PINERO L, 1983, THESIS U NACL BUENOS; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Riccardi A.C., 1980, Simposio de Geologia Regional Argentina. Academia Nacional de Ciencias, P1173; THOMSEN E, 1985, Bulletin of the Geological Society of Denmark, V33, P341; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; Williams Graham L., 1998, AASP Contributions Series, V34, P1; WRENN J H, 1988, Palynology, V12, P129	50	31	35	0	2	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		1-86239-160-2	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2004	230						325	343		10.1144/GSL.SP.2004.230.01.17	http://dx.doi.org/10.1144/GSL.SP.2004.230.01.17			19	Geology; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Paleontology	BBX62					2025-03-11	WOS:000228280100017
J	Rochon, A; Marret, F				Rochon, A; Marret, F			Middle latitude dinoflagellates and their cysts: increasing our understanding on their distribution	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Editorial Material							SEA-SURFACE CONDITIONS; THECA RELATIONSHIPS; LIFE-CYCLE; GYMNODINIUM-CATENATUM; GYRODINIUM-UNCATENUM; RECENT SEDIMENTS; LATE QUATERNARY; NORTH-ATLANTIC; DINOPHYCEAE; OCEAN		Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; UQAM, ISMER, Rimouski, PQ G5L 3A, Canada; Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5AB, Anglesey, Wales	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Quebec; University of Quebec Montreal	Rochon, A (通讯作者)，Geol Survey Canada Atlantic, Nat Resources Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada.			Marret-Davies, Fabienne/0000-0003-4244-0437				ANDERSON DM, 1985, J PHYCOL, V21, P200; [Anonymous], QUANTIFICATIONS CHAN; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Dale B., 1983, P69; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; 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, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Esper O, 2002, MAR MICROPALEONTOL, V46, P177, DOI 10.1016/S0377-8398(02)00041-5; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Hallett RI, 1999, THESIS U WESTMINSTER; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HARLAND R, 1982, Palynology, V6, P9; HARLAND R, 1980, Grana, V19, P211; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Marret F, 2001, J QUATERNARY SCI, V16, P739, DOI 10.1002/jqs.648; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen J, 2001, NORTHERN NORTH ATLANTIC: A CHANGING ENVIRONMENT, P105; Matthiessen J, 1991, 7 GEOMAR; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; McMinn Andrew, 1992, Palynology, V16, P13; McMinn Andrew, 1994, Palynology, V18, P41; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; MUDIE PJ, 1980, THESIS DALHOUSIE U H; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rochon A, 1999, AM ASS STRATIGR PALY, V35; Solomon S, 2000, INT J EARTH SCI, V89, P503, DOI 10.1007/s005310000126; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1	50	8	9	0	4	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2004	128	1-2					1	5		10.1016/S0034-6667(03)00109-X	http://dx.doi.org/10.1016/S0034-6667(03)00109-X			5	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500001
J	Pospelova, V; Chmura, GL; Walker, HA				Pospelova, V; Chmura, GL; Walker, HA			Environmental factors influencing the spatial distribution of dinoflagellate cyst assemblages in shallow lagoons of southern New England (USA)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			dinoflagellate cysts; estuaries; nutrients; Waquoit Bay; temperature; salinity	NORTHERN NORTH-ATLANTIC; SEA-SURFACE CONDITIONS; COASTAL LAGOONS; LATE QUATERNARY; ADJACENT SEAS; RHODE-ISLAND; SEDIMENTS; AUSTRALIA; MORPHOLOGY; ESTUARIES	Surface sediment samples from 24 sites within eleven back-barrier lagoons of Rhode Island and Massachusetts (USA) contain abundant (200-6000 cysts cm(-3)) and diverse (up to 40 taxa) dinoflagellate cyst assemblages. The lowest cyst concentrations and diversity are observed in lagoons with low salinity ( < 10). The pattern of spatial distribution of dinoflagellate cysts in these shallow estuarine environments is described. We assessed the relationship between the available multi-year water quality data and the composition of the dinoflagellate cyst assemblages using canonical correspondence analysis. Temperature and salinity are found to be the primary abiotic factors influencing cyst distribution in the coastal lagoons. (C) 2003 Elsevier B.V. All rights reserved.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada; US EPA, Off Res & Dev, NHEERL, Atlantic Ecol Div, Narragansett, RI 02882 USA	United States Environmental Protection Agency	Univ Victoria, Sch Earth & Ocean Sci, Petch 168,POB 3055 STN CSC, Victoria, BC V8W 3P6, Canada.	vpospe@uirc.ca	Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903; Pospelova, Vera/0000-0003-4049-8133				[Anonymous], OCEANOL ACTA; [Anonymous], 1988, ADV ECOLOGICAL RES A; [Anonymous], UNIMODAL METHODS REL; AVANZO CD, 1994, ESTUARIES, V17, P131; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; BOOTHROYD JC, 1985, MAR GEOL, V63, P35, DOI 10.1016/0025-3227(85)90079-9; Boynton W.R., 1982, ESTUARINE COMP, P69, DOI [DOI 10.1016/B978-0-12-404070-0.50011-9, 10.1016/B978-0-12-404070-0.50011-9]; Brawley JW, 2000, J ENVIRON QUAL, V29, P1448, DOI 10.2134/jeq2000.00472425002900050011x; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DARNELL RM, 1981, P INT S EFF NUTR ENR, P225; 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; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; EVITT W R, 1968, Stanford University Publications in the Geological Sciences, V12, P1; GIBLIN AE, 1990, WHOI9021; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HOARE R, 1996, WORLD CLIMATE US CLI; LEE V, 1985, ESTUARIES, V8, P191, DOI 10.2307/1352200; LEE V, 1980, 73 U RHOD ISL MAR CO; Lee V., 1997, Rhode Island Salt Pond Water Quality, Salt Pond Watchers Monitoring Data 1985-1994; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; MCMINN A, 1989, MICROPALEONTOLOGY, V35, P1, DOI 10.2307/1485534; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; MORZADECKERFOUR.M, 1989, 4 INT C MOD FOSS DIN, P81; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. 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Palynology	JAN	2004	128	1-2					7	34		10.1016/S0034-6667(03)00110-6	http://dx.doi.org/10.1016/S0034-6667(03)00110-6			28	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500002
J	Marret, F; Eiríksson, J; Knudsen, KL; Turon, JL; Scourse, JD				Marret, F; Eiríksson, J; Knudsen, KL; Turon, JL; Scourse, JD			Distribution of dinoflagellate cyst assemblages in surface sediments from the northern and western shelf of Iceland	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			dinoflagellate cysts; shelf seas; Iceland; recent distribution; Irminger Current	EAST GREENLAND CURRENT; ATLANTIC; OCEAN; PRODUCTIVITY; HOLOCENE; REGION	in order to provide calibration for palaeoceanographic investigations, 54 surface sediment samples from the northern and western margin of Iceland and Greenland have been analysed for their dinoflagellate cyst assemblages. Relatively high diversity was observed with a total of 28 taxa. Cysts of Pentapharsodinium dalei are dominant accompanied by Operculodinium centrocarpum and Nematosphaeropsis labyrinthus. Three groups of assemblages have been recognised based on multivariate statistical analyses and these are related to surface water masses and currents. The first association, Group I, located west of Iceland, is characterised by high abundance of O. centrocarpum and N. labyrinthus accompanied by significant occurrence of the beterotrophic taxa Brigantedinium spp., Selenopemphix quanta, cysts of Polykrikos schwartzii and cysts of Protoperidinium americanum. This region is under the influence of the Irminger Current (IC) and contains the most productive waters around Iceland. The second association, Group 11, comprising high relative abundance of cysts of P. dalei accompanied by significant occurrence of O. centrocarpum and a very high concentration (up to 256920 cysts/g), is situated in the northern Icelandic shelf, in the Polar Front realm, i.e. the marginal zone between the East Icelandic Current (EIC) and the northern branch of the IC. The third group (Group 111) is in the region influenced by the East Greenland Current and the EIC and characterised by the codominance of cysts of P. dalei and O. centrocarpum, relatively high representation of Impagidinium pallidum and low concentrations (from 370 to 56220 cysts/g). This investigation demonstrates that dinocyst distribution is clearly related to upper water mass physical factors. Advection of temperate species around Iceland suggests significant transport by surface currents, especially the IC; however, the apparent boundaries between the associations and decreasing percentages related to environmental gradients indicate that dispersal by surface transport is limited by the ecological requirements of the dinoflagellate cells. Bottom currents may play a role in the accumulation rate of cysts. (C) 2003 Elsevier B.V. All rights reserved.	Univ Wales, Sch Ocean Sci, Menai Bridge, Anglesey, Wales; Univ Iceland, Inst Sci, IS-101 Reykjavik, Iceland; Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; Univ Bordeaux 1, Dept Geol & Oceanog, F-33405 Talence, France	University of Iceland; Aarhus University; Universite de Bordeaux	Univ Wales, Sch Ocean Sci, Menai Bridge, Anglesey, Wales.	f.marret@bangor.ac.uk	Knudsen, Karen/A-4849-2012; Eiriksson, Jon/J-4262-2014	Marret-Davies, Fabienne/0000-0003-4244-0437; Eiriksson, Jon/0000-0001-5598-2417				AAGAARD K, 1968, ARCTIC, V21, P181; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; Andrews JT, 2001, QUATERNARY RES, V56, P199, DOI 10.1006/qres.2001.2253; [Anonymous], 1988, NATURE CONTINENTAL S, DOI DOI 10.1016/C2013-0-11665-0; Belkin IM, 1998, PROG OCEANOGR, V41, P1, DOI 10.1016/S0079-6611(98)00015-9; Bersch M, 1999, DEEP-SEA RES PT II, V46, P55, DOI 10.1016/S0967-0645(98)00114-3; Clarke K R., 1994, An approach to statistical analysis and interpretation; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Eiríksson J, 2000, J QUATERNARY SCI, V15, P23, DOI 10.1002/(SICI)1099-1417(200001)15:1<23::AID-JQS476>3.0.CO;2-8; Fensome R.A., 1993, MICROPALEONTOL SPEC, V7; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Gudmundsson K, 1998, ICES J MAR SCI, V55, P635, DOI 10.1006/jmsc.1998.0391; HANSEN B, 2000, 200003 ICES CM; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Jiang H, 2001, MAR MICROPALEONTOL, V41, P73, DOI 10.1016/S0377-8398(00)00053-0; Knudsen KL, 2002, MAR GEOL, V191, P165, DOI 10.1016/S0025-3227(02)00530-3; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; LEFEVRE J, 1986, ADV MAR BIOL, V23, P163; Malmberg SA, 1997, ICES J MAR SCI, V54, P300, DOI 10.1006/jmsc.1997.0221; MALMBERG SA, 1982, 1982GEN4 ICES CM; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 2003, MAR MICROPALEONTOL, V47, P101, DOI 10.1016/S0377-8398(02)00095-6; 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; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. 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Palynology	JAN	2004	128	1-2					35	53		10.1016/S0034-6667(03)00111-8	http://dx.doi.org/10.1016/S0034-6667(03)00111-8			19	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500003
J	Eynaud, F; Turon, JL; Duprat, J				Eynaud, F; Turon, JL; Duprat, J			Comparison of the Holocene and Eemian palaeoenvironments in the South Icelandic Basin: dinoflagellate cysts as proxies for the North Atlantic surface circulation	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			dinoflagellate cyst (dinocyst); palaeoclimatology; Marine Isotopic Stage 5; Holocene; Eemian	OXYGEN-ISOTOPE RECORDS; SEA-SURFACE; NORWEGIAN SEA; COLD EVENT; ENVIRONMENTAL-CHANGES; LAST DEGLACIATION; NORDIC SEAS; ICE CORE; BP EVENT; OCEAN	A precise assessment of the hydrological changes in the northern Atlantic Ocean throughout the last climatic cycle stands as one of the key priorities for understanding the mechanisms of global climate change. A high resolution micropalaeontological study of a sediment core (MD95-2015) retrieved from the South Icelandic Basin, allows us to infer patterns of North Atlantic surface hydrological changes during the present (Holocene) and the ultimate (Marine Isotopic Stage 5) Interglacial periods. The downcore distribution of organic-walled dinoflagellate cysts (dinocysts) is used, in conjunction with additional proxies (sediment magnetic susceptibility, CaCO3, stables isotopes and planktic foraminifer assemblages) to identify climatic instabilities of various amplitudes. These events are mostly characterised by prominent changes in relative abundance of the dinocysts Spiniferites mirabilis and Operculodinium centrocarpum, whose maximum values are thought to trace sea-surface temperature peaks at the core site. Two hypsithermal periods are identified on this basis, between 126 and 120 kyr BP and from 9.2 to 5.7 cal kyr BP (similar to8-5 C-14 kyr BP), respectively. Some discrepancies between the micropalaeontological tracers used are discussed here in the light of their qualitative and quantitative (transfer functions) ecological interpretation. (C) 2003 Elsevier B.V. All rights reserved.	Univ Bordeaux 1, UMR CNRS EPOC 5805, Dept Geol & Oceanog, F-33405 Talence, France	Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux	Univ Bordeaux 1, UMR CNRS EPOC 5805, Dept Geol & Oceanog, Ave Fac, F-33405 Talence, France.	eynaud@geocean.u-bordeaux.fr; turon@geocean.u-bordeaux.f; j.duprat@geocean.u-bordeaux.fr		Eynaud, Frederique/0000-0003-1283-7425				Aksu A.E., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P617, DOI 10.2973/odp.proc.sr.105.140.1989; Alley RB, 1997, GEOLOGY, V25, P483, DOI 10.1130/0091-7613(1997)025<0483:HCIAPW>2.3.CO;2; ANKLIN M, 1993, NATURE, V364, P203, DOI 10.1038/364203a0; Baldini JUL, 2002, SCIENCE, V296, P2203, DOI 10.1126/science.1071776; Barber DC, 1999, NATURE, V400, P344, DOI 10.1038/22504; Bard E, 1998, GEOCHIM COSMOCHIM AC, V62, P2025, DOI 10.1016/S0016-7037(98)00130-6; BASSINOT F, 1996, RAPPORTS CAMPAGNE ME; Boessenkool KP, 2001, GLOBAL PLANET CHANGE, V30, P33, DOI 10.1016/S0921-8181(01)00075-3; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; Broecker WS, 1990, PALEOCEANOGRAPHY, V5, P469, DOI 10.1029/PA005i004p00469; CORTIJO E, 1994, NATURE, V372, P446, DOI 10.1038/372446a0; Cortijo E, 1999, PALEOCEANOGRAPHY, V14, P23, DOI 10.1029/1998PA900004; Cortijo E, 2000, QUATERNARY SCI REV, V19, P227, DOI 10.1016/S0277-3791(99)00063-3; 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, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; De Vernal A., 1996, CAHIERS GEOTOP, V3; De Vernal A., 1993, Nato. 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Palaeobot. Palynology	JAN	2004	128	1-2					55	79		10.1016/S0034-6667(03)00112-X	http://dx.doi.org/10.1016/S0034-6667(03)00112-X			25	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500004
J	McCarthy, FMG; Gostlin, KE; Mudie, PJ; Pedersend, RO				McCarthy, FMG; Gostlin, KE; Mudie, PJ; Pedersend, RO			The palynological record of terrigenous flux to the deep sea:: late Pliocene -: Recent examples from 41°N in the abyssal Atlantic and Pacific oceans	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			late Cenozoic marine palynology; abyssal sedimentation; terrigenous flux; turbidites	DINOFLAGELLATE CYST ASSEMBLAGES; WESTERN NORTH-ATLANTIC; POLLEN DISTRIBUTION; CALCIUM-CARBONATE; SEDIMENTS; TRANSPORT; PRODUCTIVITY; PRESERVATION; FLUCTUATIONS; PLEISTOCENE	Sediments of late Pliocene to Recent age from two abyssal sites at 41degreesN latitude (ODP Site 898 in the eastern Atlantic Ocean and ODP Site 1179 in the western Pacific Ocean) generally contain sparse palynomorph assemblages dominated by oxidation-resistant gonyaulacacean dinoflagellate cysts. Some samples at both sites had unexpectedly high palynomorph concentrations, high P:D (pollen: dinoflagellate cyst) and low G:P (gonyaulacacean:protoperidiniacean) values. These samples record an increase in terrigenous flux and in the rate of sedimentation. Sedimentological data from ODP Hole 898A support the interpretation of pollen and protoperidiniacean dinoflagellate cyst-rich calcareous sandy muds as distal turbidites. We suggest that palynological analysis is more accurate than sediment grain size in distinguishing distal turbidites from pelagites. Similar palynological assemblages in biosiliceous oozes at Site 1179 have a different origin. The close correlation of peaks in total palynomorph concentration with anomalous preservation of protoperidiniacean dinoflagellate cysts as well as biogenic calcium carbonate I km below the modern CCD suggests a link between terrigenous flux and sea surface productivity. The increased flux of biogenic particles (including planktonic foraminiferal tests) driven by the increased availability of continentally derived limiting nutrients in oceanic waters appears mainly responsible for the increased sedimentation rate which allows oxidation-susceptible dinoflagellate cysts and dissolution- susceptible calcareous microfossils to be preserved. The ages of these palynomorph-rich calcareous intervals at this and several other nearby sites in the western North Pacific suggest that the resulting sequestration of both organic and inorganic carbon affected the greenhouse effect sufficiently to drive late Cenozoic global cooling. (C) 2003 Elsevier B.V. All rights reserved.	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; Univ Toronto, Dept Geol, Toronto, ON M5S 3B1, Canada; Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada; Schlumberger, N-5257 Kokstad, Norway	Brock University; University of Toronto; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Schlumberger	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.							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Palaeobot. Palynology	JAN	2004	128	1-2					81	95		10.1016/S0034-6667(03)00113-1	http://dx.doi.org/10.1016/S0034-6667(03)00113-1			15	Plant Sciences; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500005
J	Sprangers, M; Dammers, N; Brinkhuis, H; van Weering, TCE; Lotter, AF				Sprangers, M; Dammers, N; Brinkhuis, H; van Weering, TCE; Lotter, AF			Modern organic-walled dinoflagellate cyst distribution offshore NW Iberia; tracing the upwelling system	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			organic-walled dinoflagellate cysts; modern distribution; upwelling; Iberia; bioproductivity; transport	NORTHEAST ATLANTIC; WATER MASSES; SURFACE SEDIMENTS; PENINSULA; OCEAN; HYDROGRAPHY; MARGIN; MATTER	The northwest Iberian ocean margin experiences seasonal upwelling of nutrient-rich water resulting in enhanced primary productivity. The quantitative organic-walled dinoflagellate cyst distribution and that of other palynomorphs has been determined in 37 box core-tops along three transects to trace the upwelling signal. Oligotrophic Impagidinium spp. represent the dominant offshore elements. Cysts of heterotrophic Protoperidinium spp. mainly occur in sediments of the seasonal upwelling area on the shelf and slope and show a sharp decrease offshore. The eutrophic autotrophic taxon Lingulodinium machaerophorum is also abundant in sediments of the seasonal upwelling area on the shelf and slope, and also decreases more offshore. Both relative as well as absolute numbers of these taxa may be used to trace the upwelling system despite potential taphonomic problems. Considering the overall similar environmental conditions with respect to the other two transects, the elevated palynomorph concentrations in the shielded Nazare Canyon samples may be seen to represent the actual fluxes of palynomorphs along the Iberian coast. If accepted, this would indicate a preservational and transport loss of cysts of an order of magnitude in other transects. (C) 2003 Published by Elsevier B.V.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Netherlands Inst Sea Res, NIOZ, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	m.sprangers@bio.uu.nl	Brinkhuis, Henk/B-4223-2009; Lotter, Andre F./C-3477-2008	Lotter, Andre F./0000-0002-2954-8809; Brinkhuis, Henk/0000-0003-0253-6610				Bao R, 1997, MAR GEOL, V144, P117, DOI 10.1016/S0025-3227(97)00080-7; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Cotte-Krief MH, 2000, MAR CHEM, V71, P199, DOI 10.1016/S0304-4203(00)00049-9; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FIUZA AFD, 1982, OCEANOL ACTA, V5, P31; Fiuza AFG, 1998, DEEP-SEA RES PT I, V45, P1127, DOI 10.1016/S0967-0637(98)00008-9; NEVES R, 1999, MODELING CIRCULATION, P169; Olli K, 2001, PROG OCEANOGR, V51, P443, DOI 10.1016/S0079-6611(01)00079-9; Peliz AJ, 1999, INT J REMOTE SENS, V20, P1363, DOI 10.1080/014311699212786; Pérez FF, 1999, J MARINE SYST, V19, P27, DOI 10.1016/S0924-7963(98)00022-0; Rochon A., 1999, AASP CONTRIBUTION SE, V35; Schmidt S, 2001, MAR GEOL, V173, P55, DOI 10.1016/S0025-3227(00)00163-8; Smyth TJ, 2001, PROG OCEANOGR, V51, P269, DOI 10.1016/S0079-6611(01)00070-2; Stevens I, 2000, J MARINE SYST, V26, P53, DOI 10.1016/S0924-7963(00)00038-5; Targarona J, 1999, GRANA, V38, P170; Traverse A., 1988, PALEOPALYNOLOGY, P375; van Aken HM, 2000, DEEP-SEA RES PT I, V47, P757, DOI 10.1016/S0967-0637(99)00092-8; van Aken HM, 2000, DEEP-SEA RES PT I, V47, P789, DOI 10.1016/S0967-0637(99)00112-0; VANWEERING TCE, 1999, 2 OMEX, P83; Wall D., 1977, MAR MICROPALEONTOL, V30, P319; WILLIAMS GL, 1998, LENTIN WILLIAMS INDE; Zonneveld K.A.F., 1996, LPP CONTRIBUTIONS SE, V3; 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	25	51	55	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2004	128	1-2					97	106		10.1016/S0034-6667(03)00114-3	http://dx.doi.org/10.1016/S0034-6667(03)00114-3			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	758UV		Green Submitted			2025-03-11	WOS:000187669500006
J	Harland, R; Nordberg, K; Filipsson, HL				Harland, R; Nordberg, K; Filipsson, HL			The seasonal occurrence of dinoflagellate cysts in surface sediments from Koljo Fjord, west coast of Sweden - a note	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			flocculent layer; dinoflagellate cysts; seasonal succession; ecology; Koljo Fjord; Sweden	INDUSTRIAL-POLLUTION; NORWEGIAN FJORD; SWEDISH FJORD; YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION; INDICATORS; ASSEMBLAGES; CLIMATE; NORWAY	The opportunistic collection of the flocculent layer, over the spring to late summer seasons, has provided information on the seasonal dinoflagellate cyst sedimentation in Koljo Fjord, on the west coast of Sweden. The dinoflagellate cyst assemblages within the flocculent layer can be both diverse and contain many cysts. The cyst assemblages do not remain constant over time but demonstrate seasonality. Our very limited dataset of six samples suggests that the spring bloom is characterised by round, brown Protoperidinium cysts together with subsidiary Pentapharsodinium dalei and Protoperidinium conicum. The early summer assemblage differs in containing higher proportions of P. dalei with fewer round, brown Protoperidinium cysts together with relatively minor amounts of Lingulodinium polyedrum and Polykrikos schwartzii. The late summer cyst flora is co-dominated by Lingulodinium polyedrum and round, brown Protoperidinium cysts, together with minor amounts of P. dalei and Spiniferites spp. including Spiniferites bentorii. Cyst production within the different species occurs at times of the year when the surface water conditions within the fjord are suitable. This probably reflects, all or in part, the stability of the upper water column, the relative availability of nutrients and the overall phytoplankton productivity. (C) 2004 Elsevier B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Anim & Plant Sci, Palynol Res Facil, Sheffield S10 2TN, S Yorkshire, England; Gothenburg Univ, Ctr Earth Sci, Dept Oceanog, S-40530 Gothenburg, Sweden	University of Sheffield; University of Gothenburg	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.		Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Nordberg, Kjell/0000-0003-0085-4607				ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; AURE J, 1989, ESTUAR COAST SHELF S, V28, P59, DOI 10.1016/0272-7714(89)90041-3; BARNETT PRO, 1984, OCEANOL ACTA, V7, P399; Björk G, 2000, ESTUARIES, V23, P367, DOI 10.2307/1353329; 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, 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, 2000, APPL MICROFOSSILS EN, P305; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Gustafsson M, 1999, J SEA RES, V41, P163, DOI 10.1016/S1385-1101(99)00002-7; HARLAND R, 2004, REV PALAEOBOT PALYNO, V128; HEANEY S I, 1981, Journal of Plankton Research, V3, P331, DOI 10.1093/plankt/3.2.331; Lewis J., 1985, P85; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; MACISAAC JJ, 1978, LIMNOL OCEANOGR, 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; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Rosenberg R, 1996, J SEA RES, V35, P1, DOI 10.1016/S1385-1101(96)90730-3; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Smayda T.J., 1980, PHYSIOLOGICAL ECOLOG, P493; Taylor F.J.R., 1987, Botanical Monographs (Oxford), V21, P398; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	29	47	48	2	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2004	128	1-2					107	117		10.1016/S0034-6667(03)00115-5	http://dx.doi.org/10.1016/S0034-6667(03)00115-5			11	Plant Sciences; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500007
J	Harland, R; Nordberg, K; Filipsson, HL				Harland, R; Nordberg, K; Filipsson, HL			A high-resolution dinoflagellate cyst record from latest Holocene sediments in Koljo Fjord, Sweden	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			dinoflagellate cysts; latest Holocene; Koljo Fjord; palaeoenvironments; hydrography; nutrient availability; eutrophication; salinity; NAO	NORTHEAST ATLANTIC-OCEAN; SWEDISH WEST-COAST; SKAGERRAK-KATTEGAT; QUALITY ASSESSMENT; EASTERN ENGLAND; SURFACE; NORWAY; ASSEMBLAGES; INDICATORS; PLIOCENE	A high-resolution dinoflagellate cyst record is detailed for the very latest Holocene sediments preserved in a silled fjord from western Sweden. Koljo Fjord is characterised by brackish water conditions together with intermittent deep-water renewal and oxygen depletion. The data provide information derived from the phytoplankton populations living in the surface waters, including possible changes to the nutrient availability and salinity regimes using an actualistic ecological approach. The cyst record provides evidence that the dinoflagellate populations within the surface waters of the fjord over the last 155 years or so have fluctuated markedly. The dinoflagellate cyst record from Core KG1A demonstrates a 10-fold increase in both total cyst numbers and Lingulodinium polyedrum since c. 1938, and a shift from assemblages with high Pentapharsodinium dalei to those with high L. polyedrum and Protoceratium reticulatum from about 1980. These fluctuations are singly and/or collectively indicative of possible cultural changes within the fjord; the effects of the North Atlantic Oscillation on both deep-water renewal and seasonality; nutrient enhancement (eutrophication?); and increased water column stability. (C) 2003 Elsevier B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Anim & Plant Sci, Palynol Res Facil, Sheffield S10 2TN, S Yorkshire, England; Gothenburg Univ, Ctr Earth Sci, Dept Oceanog, S-40530 Gothenburg, Sweden	University of Sheffield; University of Gothenburg	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.		; Filipsson, Helena/F-7419-2011	Nordberg, Kjell/0000-0003-0085-4607; Filipsson, Helena/0000-0001-7200-8608				Andersson L, 1996, J SEA RES, V35, P63, DOI 10.1016/S1385-1101(96)90735-2; 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; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P207; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; 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; DALE B, 1998, 6 INT C MOD FOSS DIN, P27; de Vernal A, 2000, CAN J EARTH SCI, V37, P725, DOI [10.1139/cjes-37-5-725, 10.1139/e99-091]; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Eppley RW., 1975, Proceedings of THE FIRST INTERNATIONAL CONFERENCE ON TOXIC DINOFLAGELLATE BLOOMS, P11; Fjellsa A, 1996, PALAEOGEOGR PALAEOCL, V124, P87, DOI 10.1016/0031-0182(96)00009-0; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; Gundersen N, 1988, THESIS U OSLO, P1; Gustafsson M, 2002, HOLOCENE, V12, P325, DOI 10.1191/0959683602hl547rp; Gustafsson M, 1999, J SEA RES, V41, P163, DOI 10.1016/S1385-1101(99)00002-7; HARLAND R, 1989, J GEOL SOC LONDON, V146, P945, DOI 10.1144/gsjgs.146.6.0945; HARLAND R, 1994, PALAEONTOLOGY, V37, P263; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; HARLAND R, 1991, GEOL MAG, V128, P647, DOI 10.1017/S0016756800019749; HARLAND R, 1995, HOLOCENE, V5, P220, DOI 10.1177/095968369500500210; HARLAND R, 2004, REV PALAEOBOT PALYNO, V128; HARLAND R, 2000, RH000801 DIN SERV, P1; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 1999, J PALEONTOL, V73, P1; Head MJ, 1998, GEOL MAG, V135, P803, DOI 10.1017/S0016756898001745; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; MACISAAC JJ, 1978, LIMNOL OCEANOGR, V23, P1; MADSEN A, 1992, 8 INT PAL C AIX EN P, P95; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; Nilsson HC, 1997, J MARINE SYST, V11, P249, DOI 10.1016/S0924-7963(96)00111-X; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; REID PC, 1972, J MAR BIOL ASSOC UK, V52, P939, DOI 10.1017/S0025315400040674; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rosenberg R, 1996, J SEA RES, V35, P1, DOI 10.1016/S1385-1101(96)90730-3; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; THORSEN TA, 1996, 9 INT PAL C HOUST TX, P160; WILLIAMS D.B., 1971, MICROPALAEONTOLOGY O; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	46	45	46	0	8	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2004	128	1-2					119	141		10.1016/S0034-6667(03)00116-7	http://dx.doi.org/10.1016/S0034-6667(03)00116-7			23	Plant Sciences; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500008
J	Mudie, PJ; Rochon, A; Aksu, AE; Gillespie, H				Mudie, PJ; Rochon, A; Aksu, AE; Gillespie, H			Late glacial, Holocene and modern dinoflagellate cyst assemblages in the Aegean-Marmara-Black Sea corridor: statistical analysis and re-interpretation of the early Holocene Noah's Flood hypothesis	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			palynology; dinoflagellate cysts; eastern Mediterranean; Aegean Sea; Black Sea; Marmara Sea; Noah's Flood; palaeosalinity	LATE QUATERNARY CORES; ORGANIC-MATTER; MEDITERRANEAN SEA; WATER; OUTFLOW; EVOLUTION; SEDIMENTS; ATLANTIC; HISTORY; S1	Understanding of the history of water exchange between the Mediterranean and Black seas has been hampered by the lack of continuous microfossil records for Holocene cores from the Marmara Sea Gateway (Aegean-Marmara-Black Sea corridor), and by the lack of core-top data linking modern microfossil assemblages with sea surface conditions. Based on molluscs, an abrupt transition from freshwater to marine conditions at ca. 7.5 ka has been postulated, with interpretation of this event as the basis for the story of Noah's Flood. We have re-examined this hypothesis using organic-walled dinoflagellate cysts that show excellent preservation and moderate to high diversity in Pleistocene-Holocene sediments of the Marmara Sea Gateway. Principle component analysis of 16 core-top samples shows that an assemblage dominated by cysts of autotrophic gonyaulacoids distinguishes the hypersaline Aegean-Mediterranean water (salinity 31-38), whereas heterotrophic protoperidinioids characterise the low-salinity Marmara-Black Sea water (salinity similar to 14-25). About 150 samples from eight cores, with multiple radiocarbon ages spanning the past similar to 33 000 years, show correlatable major changes in cyst assemblages along the Marmara-Black Sea corridor. Variation in length and shape of gonyaulacoid species processes decreases upcore from basal units where there are no-analogue assemblages of cysts with highly variable spine development. It is shown that these variable and no-analogue assemblages correspond to brackish conditions (salinity similar to4-12) when calibrated against delta(18)O data and salinity estimates derived from planktonic foraminifera. Salinity reconstructions indicate that the Aegean and Marmara seas were connected by similar to 11 ka when the Marmara Sea was a brackish or low-salinity sea (similar to 12-17) and that the Black Sea was flowing into the Marmara Sea by at least 10.2 - 9.5 ka. There is no evidence to support either the idea that the Black Sea was a large freshwater lake suitable for farming in the early Holocene or that a sudden (< 500-yr) flooding of the Black Sea by a 100-m-high waterfall of Mediterranean water occurred at 7.5 ka. It is shown that there is a need for precise use of salinity terms when reconstructing the history of saline lakes in the context of Neolithic human occupation so that the likelihood of agricultural settlement can be evaluated realistically. (C) 2003 Elsevier B.V. All rights reserved.	Geol Survey Canada, Bedford Inst Oceanog, Atlantic Geosci Ctr, Dartmouth, NS B2Y 4A2, Canada; Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada	Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland	UQAR, ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	andre_rochon@uqar.gc.ca						Abrajano T, 2002, MAR GEOL, V190, P151, DOI 10.1016/S0025-3227(02)00346-8; Aksu A.E., 2002, GSA Today, V12, P4, DOI DOI 10.1130/1052-5173(2002)012<0004:PH0FTB>2.0.C0;2; Aksu AE, 1999, MAR GEOL, V153, P275, DOI 10.1016/S0025-3227(98)00078-4; 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; Arthur MA, 1998, PALEOCEANOGRAPHY, V13, P395, DOI 10.1029/98PA01161; Ballard RD, 2000, MAR GEOL, V170, P253, DOI 10.1016/S0025-3227(00)00108-0; *BLACK SEA PIL, 1990, MARM DEN BLACK SEA A; Bogucki P, 1996, AM SCI, V84, P242; Boudreau BP, 1989, PALEOCEANOGRAPHY, V4, P157, DOI 10.1029/PA004i002p00157; BOZILOVA E, 1996, PALAEOECOLOGICAL EVE, P701; BUKRY D, 1974, AM ASS PET GEOL MEM, V20, P364; CIVILI FS, 1992, SEMI-ENCLOSED SEAS, P6; DALE B, 1996, PALYNOLOGY PRINCIPLE, V3, P124; Daskalov GM, 2002, MAR ECOL PROG SER, V225, P53, DOI 10.3354/meps225053; DEUSER WG, 1972, J GEOPHYS RES, V77, P1071, DOI 10.1029/JC077i006p01071; DODGE JD, 1994, REV PALAEOBOT PALYNO, V84, P169, DOI 10.1016/0034-6667(94)90049-3; DUMAN M, 1994, GEO-MAR LETT, V14, P272, DOI 10.1007/BF01274063; EREMEEV VN, 1995, B I OCEANOGR MONACO, V15, P27; FAIRBRIDGE RW, 1966, ENCY OCEANOGRAPHY, P490; Fonselius S. 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Palaeobot. Palynology	JAN	2004	128	1-2					143	167		10.1016/S0034-6667(03)00117-9	http://dx.doi.org/10.1016/S0034-6667(03)00117-9			25	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500009
J	Radi, T; de Vernal, A				Radi, T; de Vernal, A			Dinocyst distribution in surface sediments from the northeastern Pacific margin (40-60°N) in relation to hydrographic conditions, productivity and upwelling	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	Workshop on Middle Latitude Dinoflagellates and Their Cysts	APR 29-MAY 02, 2002	NOVA SCOTIA, CANADA			Northeastern Pacific; productivity; upwelling; dinocyst assemblages	DINOFLAGELLATE CYST ASSEMBLAGES; LATITUDE MARINE ENVIRONMENTS; NORTHERN NORTH-ATLANTIC; LAST DEGLACIATION; BRITISH-COLUMBIA; INDIAN-OCEAN; SEA; INDICATORS; TRACERS; EUTROPHICATION	Seventy-six surface marine sediment samples from the northwest margin of North America, between 40degreesN and 60degreesN, were analysed for their palynological content in order to document the regional distribution of dinocyst assemblages and their relationships with environmental conditions (sea-surface temperature and salinity, productivity and upwelling). The results illustrate a high concentration of dinocysts, notably in the neritic area (up to 34 000 cysts cm(-3)) and a relatively high species diversity with 32 taxa identified. The assemblages include cysts of both autotrophic and heterotrophic species. Brigantedinium spp. accompanied by other heterotrophic taxa such as Votadinium spp., Quinquecuspis concreta, Trinovantedinium variabile and Lejeunecysta spp. dominate in the nearshore areas influenced by seasonal upwelling. The offshore sites are dominated by autotrophic taxa represented mainly by Operculodinium centrocarpum, Pyxidinopsis reticulata, Nematosphaeropsis labyrinthus and Impagidinium aculeatum in the south, and by O. centrocarpum, Pentapharsodinium dalei, Spiniferites ramosus and Spiniferites elongatus in the Gulf of Alaska. Principal component analysis demonstrates that the regional distribution of dinocyst assemblages is controlled by the primary productivity and upwelling, and by the winter temperature gradient. (C) 2003 Elsevier B.V. All rights reserved.	Uqam, Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Radi, T (通讯作者)，Uqam, Geotop, CP 8888,Succ Ctr Ville, Montreal, PQ H3C 3P8, Canada.		de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; 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, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1987, POLLEN SPORES, V29, P291; de Vernal A., 1999, CAHIERS GEOTOP, V3; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Guilbault JP, 2003, QUATERNARY SCI REV, V22, P839, DOI 10.1016/S0277-3791(02)00252-4; Guiot J., 1996, Dendrochronologia, V14, P295; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; HUYER A, 1983, PROG OCEANOGR, V12, P259, DOI 10.1016/0079-6611(83)90010-1; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Matsuoka K, 2000, MICROPALEONTOLOGY, V46, P360; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Matsuoka K., 1987, Bull. 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Palaeobot. Palynology	JAN	2004	128	1-2					169	193		10.1016/S0034-6667(03)00118-0	http://dx.doi.org/10.1016/S0034-6667(03)00118-0			25	Plant Sciences; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	758UV					2025-03-11	WOS:000187669500010
J	Borel, CM; Guerstein, GR; Prieto, AR				Borel, CM; Guerstein, GR; Prieto, AR			Holocene aquatic palynomorphs (algae and acritarchs) from Laguna Hinojales (Buenos Aires, Argentina): paleoecological interpretation	AMEGHINIANA			Spanish	Article						palynology; algae; acritarchos; holocene; Buenos Aires; Argentina	NOORD-HOLLAND; CHLOROPHYTA; ACARTIIDAE; MORPHOLOGY; EGGS; PROV	Holocene palynological samples from the Laguna Hinojales (37similar to 34' S; 57degrees 27' W), southeastern Buenos Aires province, contain algae (Chlorophyta, Cyanophyta and Dinoflagellata) and acritarchs. The chlorophycean algae consist of cenobia of Pediastrum musterii Tell and Mataloni, P. boryantim (Turpin) Meneghini, and Scenedesmus sp., colonies of Botryococois braunii Mitzing, zygospores of Debarya madrasensis lyengar, Motigeotia laetenvirens (Braun) Wittrock, Moitgeotia sp., Zygnenia sp. and Spirogyra spp., and spores of Desmidiaceae. Cyanophycean sheets and akinetes of Gloeotrichia sp. are well preserved. The assemblages also contain freshwater dinoflagellates, represented by a peridinioid genus. Among the acritarchs, Cobricosphaeridium spp. reach highest percentages in the lowermost part of the core, where possibly freshwater algal spores are also present. These palynomorphs, produced by organisms from plankton and benthic communities, are used as indicators of nutrient, depth and salinity changes. Variable size and salinity of the water body are inferred from fluctuating frequencies of algae and acritarchs between ca. 4,500 - 2,100 C-14 yr B.P. From 2,100 C-14 yr B.P, algal assemblages indicate a freshening of the water and a gradual transition to favourable trophic conditions in the shallow lake. Higher values of Pediastrum spp., Scenedesmus sp., and Zygnemataceae, along with low frequencies of Botryococcus braunii reflect elevated nutrient levels in a relatively shallow lake. The improvement of climatic conditions, especially an increase in average temperature, probably was responsible for the expansion of aquatic plants and natural eutrophication of the water environment. After 400 14C yr B.P. the spectrum suggests a shallow eutrophic lake. However, alternating intervals, less favourable for algae, reflect a reduction in the water body size, possibly related to periods of lower precipitation.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Argentina; Univ Nacl Mar Del Plata, Fac Ciencias Exactas & Nat, Consejo Nacl Invest Cient & Tecn, Lab Paleoecol & Palinol, RA-7600 Mar Del Plata, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of Mar del Plata	Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Argentina.	maborel@criba.edu.ar; gmguerst@criba.edu.ar; aprieto@mdp.edu.ar		Borel, C. 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J	Warny, SA; Bart, PJ; Suc, JP				Warny, SA; Bart, PJ; Suc, JP			Timing and progression of climatic, tectonic and glacioeustatic influences on the Messinian Salinity Crisis	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						palynology; neogene; Mediterranean; Antarctica; dinoflagellate; Messinian	DINOFLAGELLATE CYSTS; ATLANTIC COAST; LATE MIOCENE; MOROCCO; CHRONOLOGY; CORE	New palynological analysis of the continuous Upper Neogene sequence from the Rifian Corridor at Sale (Morocco) permits the deconvolution of climatic, tectonic and eustatic control on the Messinian Salinity Crisis via two indices: (1) a 'distance-from-shore' index based on dinoflagellate cyst versus pollen distribution, and (2) a land-climate index based on detailed pollen analysis. This new pollen analysis indicates that the Messinian Salinity Crisis (similar to6.8 Ma to similar to5.3 Ma) was not associated with major climate change. Detailed analyses of dinoflagellate cyst ecology at Sale correlated to the Sale delta(18)O record show that initial shoaling of the Rifian Corridor after similar to7.3 Ma primarily resulted from tectonic uplift. However, from similar to6.5 Ma to similar to5.4 Ma, the Rifian Corridor was sufficiently shallow to have experienced significant restriction of Atlantic inflow during at least four small-amplitude glacioeustatic lowstands. At similar to5.4 Ma, abrupt increase in the ratio of continental- versus marine-derived palynomorphs indicates that restriction intensified as tectonic uplift significantly outpaced gradual glacioeustatic rise. Despite eustatic rise at similar to5.32 Ma, the Sale palynological data show that the Rifian Corridor experienced a second major drop in relative sea level (tectonic uplift or increased sedimentation). Therefore, termination of the Messinian Salinity Crisis was probably associated with a breach elsewhere along the Gibraltar Arc. (C) 2003 Elsevier B.V. All rights reserved.	Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; Univ Lyon 1, CNRS, UMR 5125, F-69622 Villeurbanne, France	Louisiana State University System; Louisiana State University; Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS)	Warny, SA (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.		Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X				Benson R.H., 1991, Paleoceanography, V6, P164; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; EDWARDS LE, 1991, QUATERNARY SCI REV, V10, P259, DOI 10.1016/0277-3791(91)90024-O; FAUQUETTE S, PALAEOGEOGR PALAEOCL; Hambrey M.J., 1991, Proc. Ocean Drilling Program Scientific Results, V119, P77; HAMILTON W, 1972, 456C US GEOL SURV; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head MJ, 1998, J PALEONTOL, V72, P797, DOI 10.1017/S0022336000027153; HODELL DA, 1994, PALEOCEANOGRAPHY, V9, P835, DOI 10.1029/94PA01838; Hodell DA, 2001, PALEOCEANOGRAPHY, V16, P164, DOI 10.1029/1999PA000487; Hsu K J., 1978, Initial Reports of the Deep Sea Drilling Project, VXLII, P943, DOI DOI 10.2973/DSDP.PR0C.42-1.149.1978; HSU KJ, 1977, NATURE, V267, P399, DOI 10.1038/267399a0; Krijgsman W, 1999, NATURE, V400, P652, DOI 10.1038/23231; Lentin J.K., 1993, A.S.S.P., V28, P1; Morzadec-Kerfourn M.-T., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P121; REID PC, 1975, NEW PHYTOL, V75, P589, DOI 10.1111/j.1469-8137.1975.tb01425.x; Santarelli A, 1998, MAR MICROPALEONTOL, V33, P273, DOI 10.1016/S0377-8398(97)00042-X; Shackleton N.J., 1995, Proc. Ocean Drill. Program, V138, P73, DOI [DOI 10.2973/ODP.PROC.SR.138.106.1995, 10.2973/odp.proc.sr.138.106.1995.]; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; Warny SA, 2002, MICROPALEONTOLOGY, V48, P257, DOI 10.2113/48.3.257	21	62	69	0	10	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	DEC 15	2003	202	1-2					59	66		10.1016/S0031-0182(03)00615-1	http://dx.doi.org/10.1016/S0031-0182(03)00615-1			8	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	756AT					2025-03-11	WOS:000187444200003
J	Cai, XM; Fuller, AL; McDougald, LR; Zhu, G				Cai, XM; Fuller, AL; McDougald, LR; Zhu, G			Apicoplast genome of the coccidian <i>Eimeria tenella</i>	GENE			English	Article						Eimeria tenella; apicomplexa; coccidia; apicoplast; plastid; organellar genome; phylogeny; evolution	PARASITE PLASMODIUM-FALCIPARUM; APICOMPLEXAN PARASITES; CRYPTOSPORIDIUM-PARVUM; TOXOPLASMA-GONDII; GENE-TRANSFER; PLASTIDS; NUCLEAR; ORIGIN; TARGET; MITOCHONDRION	Unicellular apicomplexans possess an algal-originated plastid referred to as an apicoplast. Although apicomplexan parasites are comprised of highly diverse protists, the complete apicoplast genome sequences have only been determined from the hematozoan Plasmodium falciparum and cyst-forming coccidian Toxoplasma gondii. Here, we report the third complete sequence of apicoplast genome from the intestinal coccidian Eimeria tenella that may serve as a new drug target against coccidiosis in the livestock. The AT-rich E. tenella plastid genome is a 35-kb circular element. Its gene organization resembles more closely that of T. gondii than P. falciparum. Although the E. tenella plastid genome contains an almost identical set of genes to that found in P. falciparum and T. gondii, its encoded genes share low or moderate homologies with their counterparts in the other two apicomplexans. With the addition of this coccidian plastid genome sequence, we attempted to reexamine the apicoplast genome evolution and performed phylogenetic reconstructions using maximum likelihood and Bayesian inference (BI) methods based on a concatenated dataset of plastid-encoded rpoB, rpoC1 and rpoC2 proteins. All resulting rpo protein trees placed apicoplast as a sister to Euglena within the green lineage. On the other hand, many recent studies based on the organization of plastid genes and some nuclear-encoded plastid proteins have supported a common red algal ancestry of apicomplexan and dinoflagellate plastids. If the apicoplast indeed originated from a red ancestor, the green relationship of apicomplexan genes would probably imply that the ancestral host that gave rise to the (red) apicoplast might have already contained some primary green plastid genes. (C) 2003 Elsevier B.V. All rights reserved.	Coll Vet Med, Dept Vet Pathobiol, College Stn, TX 77843 USA; Univ Georgia, Dept Poultry Sci, Athens, GA 30602 USA; Texas A&M Univ, Fac Genet Program, College Stn, TX 77843 USA	Texas A&M University System; Texas A&M University College Station; University System of Georgia; University of Georgia; Texas A&M University System; Texas A&M University College Station	Zhu, G (通讯作者)，Coll Vet Med, Dept Vet Pathobiol, College Stn, TX 77843 USA.		ZHU, GUAN/D-8147-2011	Zhu, Guan/0000-0003-3888-0659	NIAID NIH HHS [R01-AI44594] 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))		Blanchard JL, 1999, J EUKARYOT MICROBIOL, V46, P367, DOI 10.1111/j.1550-7408.1999.tb04615.x; Douglas SE, 1999, BIOL BULL, V196, P397, DOI 10.2307/1542979; Dunn PPJ, 1998, PARASITOL RES, V84, P272, DOI 10.1007/s004360050394; Fast NM, 2001, MOL BIOL EVOL, V18, P418, DOI 10.1093/oxfordjournals.molbev.a003818; Fichera ME, 1997, NATURE, V390, P407, DOI 10.1038/37132; Funes S, 2002, SCIENCE, V298, P2155, DOI 10.1126/science.1076003; He CY, 2001, EMBO J, V20, P330, DOI 10.1093/emboj/20.3.330; Jomaa H, 1999, SCIENCE, V285, P1573, DOI 10.1126/science.285.5433.1573; Kohler S, 1997, SCIENCE, V275, P1485, DOI 10.1126/science.275.5305.1485; Lang-Unnasch N, 1998, INT J PARASITOL, V28, P1743, DOI 10.1016/S0020-7519(98)00136-2; Martin W, 1998, NATURE, V393, P162, DOI 10.1038/30234; Mcdougald LR, 1998, POULTRY SCI, V77, P1156, DOI 10.1093/ps/77.8.1156; McFadden GI, 1997, BIOESSAYS, V19, P1033, DOI 10.1002/bies.950191114; Moreira D, 2001, RES MICROBIOL, V152, P771, DOI 10.1016/S0923-2508(01)01260-8; OBA T, 1991, BIOCHIMIE, V73, P1109, DOI 10.1016/0300-9084(91)90153-R; Oborník M, 2002, GENE, V285, P109, DOI 10.1016/S0378-1119(02)00427-4; Ralph SA, 2001, DRUG RESIST UPDATE, V4, P145, DOI 10.1054/drup.2001.0205; Roos DS, 1999, CURR OPIN MICROBIOL, V2, P426, DOI 10.1016/S1369-5274(99)80075-7; Roos DS, 2002, PHILOS T R SOC B, V357, P35, DOI 10.1098/rstb.2001.1047; Roos DS, 1999, PARASITOL TODAY, V15, P41, DOI 10.1016/S0169-4758(98)01367-2; Rotte C, 2001, MOL BIOL EVOL, V18, P710, DOI 10.1093/oxfordjournals.molbev.a003853; Stoebe B, 1999, TRENDS GENET, V15, P344, DOI 10.1016/S0168-9525(99)01815-6; Surolia N, 2001, NAT MED, V7, P167, DOI 10.1038/84612; Waller RF, 1998, P NATL ACAD SCI USA, V95, P12352, DOI 10.1073/pnas.95.21.12352; Weissig V, 1997, DNA CELL BIOL, V16, P1483, DOI 10.1089/dna.1997.16.1483; Wilson RJM, 2002, J MOL BIOL, V319, P257, DOI 10.1016/S0022-2836(02)00303-0; Wilson RJM, 1996, J MOL BIOL, V261, P155, DOI 10.1006/jmbi.1996.0449; Zhao XM, 2001, INT J PARASITOL, V31, P715, DOI 10.1016/S0020-7519(01)00136-9; ZHU G, 1992, J PARASITOL, V78, P1067, DOI 10.2307/3283231; Zhu G, 2000, MICROBIOL-SGM, V146, P315, DOI 10.1099/00221287-146-2-315	30	99	125	0	19	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0378-1119			GENE	Gene	DEC 4	2003	321						39	46		10.1016/j.gene.2003.08.008	http://dx.doi.org/10.1016/j.gene.2003.08.008			8	Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Genetics & Heredity	753WA	14636990				2025-03-11	WOS:000187252900004
J	Okamoto, OK; Hastings, JW				Okamoto, OK; Hastings, JW			Genome-wide analysis of redox-regulated genes in a dinoflagellate	GENE			English	Article						gene expression; microarrays; oxidative stress; reactive nitrogen species; reactive oxygen species	SUPEROXIDE-DISMUTASE; GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; LUCIFERASE GENE; BINDING PROTEIN; CYST FORMATION; EXPRESSION; GROWTH; ALGA; CLONING	In this study, the effects of 1 mM sodium nitrite, a reactive nitrogen species (RNS) generator, and 0.5 mM paraquat, which produces reactive oxygen species (ROS), on gene expression in the marine dinoflagellate species Pyrocystis lunula were investigated using microarrays containing 3500 complementary DNAs (cDNAs). A total of 246 differentially expressed genes were identified under these treatments: 204 genes were specifically regulated in response to nitrite and 37 genes specifically to paraquat. Only six genes showed a dependence on both nitrite and paraquat, indicating that the two agents act predominantly via distinct pathways. Although many of these redox-regulated genes encode proteins from a diverse range of functional categories, the majority of them (68%) represent novel sequences. Temporary abnormal spherical cells occurred in nitrite-treated cultures, but not in those exposed to paraquat, suggesting that this response involves a specific pathway triggered by RNS. The genes involved include one that encodes a transcription factor unique to dinoflagellates (HPI), and genes encoding proteins similar to those regulating developmental processes in plants and animals such as NYD-SP5, shaggy and calcium-dependent kinases, the COP9 signalosome complex, ubiquitin-related proteases and a metacaspase. (C) 2003 Elsevier B.V. All rights reserved.	Harvard Univ, Dept Mol & Cellular Biol, Cambridge, MA 02138 USA	Harvard University	Harvard Univ, Dept Mol & Cellular Biol, 16 Divin Ave, Cambridge, MA 02138 USA.	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R., 1987, Botanical Monographs, V21, P1; Wargo MJ, 2001, SCIENCE, V294, P2477; WOLTERS J, 1991, BIOSYSTEMS, V25, P75, DOI 10.1016/0303-2647(91)90014-C; Zou S, 2000, P NATL ACAD SCI USA, V97, P13726, DOI 10.1073/pnas.260496697	40	66	77	1	15	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0378-1119	1879-0038		GENE	Gene	DEC 4	2003	321						73	81		10.1016/j.gene.2003.07.003	http://dx.doi.org/10.1016/j.gene.2003.07.003			9	Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Genetics & Heredity	753WA	14636994				2025-03-11	WOS:000187252900008
J	Hald, M; Husum, K; Vorren, TO; Grosfjeld, K; Jensen, HB; Sharapova, A				Hald, M; Husum, K; Vorren, TO; Grosfjeld, K; Jensen, HB; Sharapova, A			Holocene climate in the subarctic fjord Malangen, northern Norway: a multi-proxy study	BOREAS			English	Article							SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST ASSEMBLAGES; MODERN BENTHIC FORAMINIFERA; WESTERN NORWAY; NORWEGIAN SEA; BARENTS SEA; PHYSICAL OCEANOGRAPHY; OCEAN CIRCULATION; ISOTOPE RECORD; OXYGEN-ISOTOPE	A Holocene sedimentary record from the deep-silled Malangen fjord in northern Norway reveals regional changes in sedimentary environment and climate. Down-core analysis of two sediment cores includes multi-core sensor logging, grain size, x-radiography, foraminifera, oxygen isotopes, dinoflagellates, pollen, trace elements and radiocarbon datings. The cores are located just proximal to the submarine Younger Dryas moraine complex, and reveal the deglaciation after Younger Dryas and the postglacial evolution. Five sedimentary units have been identified. The oldest units, V and IV, bracket the Younger Dryas glacial readvance in the fjord between 12 700 cal. years BP and 11 800 cal. years BP. This is followed by deposition of glaciomarine sediments (units IV and III) starting around 12 100 cal. years BP. Glaciomarine sedimentation ceased in the fjord c . 10 300 cal. years BP and was replaced by open marine sedimentation (units II and I). A rapid stepwise warming occurred during the Preboreal. Onset of surface water warming lagged bottom water warming by several hundred years. The delta(18)O record indicates a significant, gradual bottom water cooling ( c . 4degreesC) between 8000 and 2000 cal. years BP, a trend also supported by the other proxy data. Other records in the region, as well as GCM simulations, also support this long-term climatic evolution. Superimposed on this cooling were brief warmings around 6000 cal. years BP and 2000 cal. years BP. The long-term change may be driven by orbitally forced reduction in insolation, whereas the short-term changes may be linked to for example solar forcing, meltwater and NAO changes all causing regional changes in the North Atlantic heat transport.	Univ Tromso, Dept Geol, NO-9037 Tromso, Norway; Geol Survey Norway, NO-7491 Trondheim, Norway; Geol Survey Norway, Polar Environm Ctr, NO-9296 Tromso, Norway; St Petersburg State Univ, Div Hist Geol, St Petersburg 199034, Russia	UiT The Arctic University of Tromso; Geological Survey of Norway; Geological Survey of Norway; Saint Petersburg State University	Univ Tromso, Dept Geol, NO-9037 Tromso, Norway.	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J	Yu, SY; Andrén, E; Barnekow, L; Berglund, BE; Sandgren, P				Yu, SY; Andrén, E; Barnekow, L; Berglund, BE; Sandgren, P			Holocene palaeoecology and shoreline displacement on the Biskopsmala Peninsula, southeastern Sweden	BOREAS			English	Article							SEA-LEVEL RISE; BALTIC SEA; DINOFLAGELLATE CYSTS; LAST DEGLACIATION; AGE CALIBRATION; WESTERN NORWAY; RESERVOIR AGES; CIRCULATION; SEDIMENT; HISTORY	High-resolution palaeoecological proxies of pollen, macrofossils and diatoms from an isolation lake provide a long-term record of the Holocene landscape history and shoreline displacement on the Biskopsmala Peninsula in central Blekinge, SE Sweden. During the Preboreal/Boreal transition, the peninsula was sparsely vegetated by woodlands, along with lateglacial dwarf shrub/steppe communities. The lake basin was isolated from the shallow Yoldia Sea during this time. The regional climate improved from 10 700 cal. BP, evident as progressive expansion of Pinus -dominated mixed forest with deciduous trees. The lake basin was probably connected with the Ancylus Lake during the period 10 700-10 100 cal. BP. Subsequently the basin became isolated again, corresponding to the Early Littorina Sea phase. Replacement of freshwater diatoms by those with brackish-water affinity at 8100 cal. BP indicates the initial transgression of the Littorina Sea in this basin. But not until 7500 cal. BP were brackish conditions fully established. Peaks of brackish-marine diatoms and dinoflagellates during 7500-7000 cal. BP indicate increased saltwater inflow to the Baltic Sea in response to global meltwater pulse 3. However, interactive changes in seagrass and stonewort macrofossil concentrations suggest that three minor transgressions during 5900-5300, 5000-4700 and 4400-4000 cal. BP occurred locally, associated with centennial-scale variations in regional wind pattern or coastal storminess. By 3000 cal. BP, the lake basin was finally isolated from the Baltic, and thereafter the landscape on the peninsula became gradually more influenced by human activities.	Lund Univ, Dept Geol, SE-22363 Lund, Sweden; Uppsala Univ, Dept Earth Sci, SE-75236 Uppsala, Sweden	Lund University; Uppsala University	Yu, SY (通讯作者)，Lund Univ, Dept Geol, Tornavagen 13, SE-22363 Lund, Sweden.							Andersson HC, 2002, TELLUS A, V54, P76, DOI 10.1034/j.1600-0870.2002.00288.x; Andrén E, 2000, BOREAS, V29, P233; ANDREN E, 1999, MEDDELANDEN STOCKHOL, V302; Andrén T, 2002, BOREAS, V31, P226, DOI 10.1080/030094802760260346; [Anonymous], GFF; [Anonymous], SOC SCIENT FENN COMM; BATTARBEE R.W., 2003, Handbook of Holocene Palaeoecology and Palaeohyrology, P527, DOI DOI 10.1127/NOVA_HEDWIGIA/2015/0263; Behre KE., 1988, Handbook of Vegetation Science, Volume 7: Vegetation History, V7, P633; BERGLUND B E, 1971, Geologiska Foreningens i Stockholm Forhandlingar, V93, P625; Berglund B. 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J	Li, G; Yang, Q				Li, G; Yang, Q			Confirmation of an Early Cretaceous age for the Qihulin Formation in eastern Heilongjiang Province, China: constraints from a new discovery of radiolarians	CRETACEOUS RESEARCH			English	Article						Early Cretaceous; radiolarians; biostratigraphy; Qihulin Formation; Northeastern China	NORTHEAST CHINA; JIXI GROUPS; LONGZHAOGOU; BIVALVES; ASIA; BIRD	The coal-bearing, alternating marine and non-marine Longzhaogou Group in eastern Heilongjiang, northeastern China, has long been considered as Jurassic, or mainly Jurassic, in age. However, recent studies have demonstrated that the ammonites and dinoflagellate cysts are of Early Cretaceous age. This has now been confirmed by new radiolarian evidence. The radiolarian fauna recovered from the upper Qihulin Formation of the Longzhaogou Group consists of nine poorly preserved species referable to nine genera. Novixitus is a Cretaceous genus, and the specimens of Archaeodictyomitra sp. and Xitus sp. recovered resemble A. vulgaris Pessagno and X. spicularius (Aliev), respectively. (C) 2003 Elsevier Ltd. All rights reserved.	Chinese Acad Sci, Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China	Chinese Academy of Sciences	Li, G (通讯作者)，Chinese Acad Sci, Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 E Beijing Rd, Nanjing 210008, Peoples R China.							ALIEV KS, 1965, LOWER CRETACEOUS DEP, P1; BATTEN DJ, 1998, GEOLOGY TODAY, V14, P169; Chen J. H., 1989, S CRET S CHIN, P311; Chen Jin-Hua, 1999, Acta Palaeontologica Sinica, V38, P454; Chen P.-j., 1988, Acta Palaeontologica Sinica, V27, P659; Chen PJ, 1998, NATURE, V391, P147, DOI 10.1038/34356; CHEN PJ, 1992, ASPECTS NONMARINE CR, P1; Futakami Masao, 1995, Journal of the Geological Society of Japan, V101, P79; Gu Z., 1962, The Jurassic and Cretaceous of China, P1; Gu Z. W., 1983, FOSSILS MIDDLE UPPER, P4; Gu Z. W., 1997, LOWER CRETACEOUS BIV; GU ZW, 1982, SCI SIN B-CHEM B A M, V25, P438; Gu ZW., 1984, FOSSILS MIDDLE UPPER, P49; GU ZW, 1984, DEV GEOSCIENCE, P119; HAO YC, 1982, ACTA GEOL SIN-ENGL, V56, P187; He Cheng-Quan, 1999, Acta Palaeontologica Sinica, V38, P183; Hou LH, 1999, CHINESE SCI BULL, V44, P834, DOI 10.1007/BF02885031; HUANG BH, 1963, CHINESE SCI BULL, V14, P69; Ji Q, 1998, NATURE, V393, P753, DOI 10.1038/31635; JU RH, 1982, CHINESE ACAD GEOLOGI, V5, P1; Kelly Simon R.A., 1994, Acta Palaeontologica Sinica, V33, P509; LI WR, 1986, GEOL MEM MINISTRY  2, V5, P59; Liang Z, 1982, CHINESE ACAD GEOL SC, V5, P63; O'Dogherty L., 1994, Memoires de Geologie, V21, P1; PESSAGNO E.A., 1977, CUSHMAN FDN SPECIAL, V15, P1; *RES TEAM MES COAL, 1986, STUD LONGZH GROUP E; RUSSELL DA, 1993, CAN J EARTH SCI, V30, P2002, DOI 10.1139/e93-176; Sha J.-g., 1990, Journal of Stratigraphy, V14, P226; 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, 1993, GEOL MAG, V130, P533, DOI 10.1017/S0016756800020586; Sun G, 2002, SCIENCE, V296, P899, DOI 10.1126/science.1069439; SUZUKI KOITI, 1949, JAPANESE JOUR GEOL AND GEOGR, V21, P91; Teraoka Y., 1986, Bulletin of the Geological Survey of Japan, V37, P417; Thurow J., 1988, Proceedings of the Ocean Drilling Program Scientific Results, V103, P379, DOI 10.2973/odp.proc.sr.103.148.1988; Tumanda F.P., 1989, Science Reports of the Institute of Geoscience University of Tsukuba Section B Geological Sciences, V10, P1; Wang Y. G, 1983, FOSSILS MIDDLE UPPER, P100; Zhang FC, 2000, SCIENCE, V290, P1955, DOI 10.1126/science.290.5498.1955	38	12	16	0	5	ACADEMIC PRESS LTD ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	DEC	2003	24	6					691	696		10.1016/j.cretres.2003.07.004	http://dx.doi.org/10.1016/j.cretres.2003.07.004			6	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	750VK					2025-03-11	WOS:000187019000005
J	Debenay, JP; Carbonel, P; Morzadec-Kerfourn, MT; Cazaubon, A; Denèfle, M; Lézine, AM				Debenay, JP; Carbonel, P; Morzadec-Kerfourn, MT; Cazaubon, A; Denèfle, M; Lézine, AM			Multi-bioindicator study of a small estuary in Vendee (France)	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						periphytic algae; sporopollinic material; ostracoda; foraminifera; estuary; Atlantic	SALT-MARSH FORAMINIFERA; SEA-LEVEL; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; RIVER ESTUARY; ASSEMBLAGES; NORTH; COAST; PHYTOPLANKTON; INDICATORS	Surficial sediment (about 5 mm) was scraped off in 15 stations selected in the Vie Estuary, a small estuary on the French Atlantic coast. The samples, prepared using the suitable methods, were used for comparing the behaviour of periphytic algae, sporopollinic and other palynologic material, ostracoda and foraminifera for proposing a synthetic evaluation of the information provided by each of them. Dinoflagellate cysts, which are found in an almost monospecific assemblage in low-salinity water, are dispersed by tidal currents, but the location of tintinnids in only the lower reaches shows a limited inward transport. Sporopollinic material is clearly related to the adjacent vegetation, indicating a local origin, and then little influence of transport on the microbenthos, even if fragments of freshwater crustaceans and of Pediastrum alga are found down to the mouth in the sporopollinic deposits. This limited transport of microbenthos allows the use of periphytic algae, benthic ostracoda and benthic foraminifera as indicators of local environmental conditions. It was then possible to determine the extent of marine influence in the estuary, to discriminate between the main channel and adjacent basins, and between different stages of evolution of the basins, from a recently dug basin to a eutrophicated one. (C) 2003 Elsevier Ltd. All rights reserved.	Fac Sci, Geol Lab, UPRES EA 2644, F-49045 Angers, France; LEBIM, Ile Yeu, France; CNRS, EPOC, UMR 5805, Dept Geol & Oceanog, F-33405 Talence, France; Univ Bordeaux 1, F-33405 Talence, France; Univ Rennes 1, Inst Geol, F-35042 Rennes, France; Univ Aix Marseille 3, Fac Sci & Tech St Jerome, Lab Ecol Eaux Continentales Mediterraneennes, F-13395 Marseille 20, France; CNRS, URA 141, Lab Geog Phys, F-92195 Meudon, France; Univ Paris 06, CNRS, URA 1761, F-75252 Paris 5, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Universite de Rennes; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Universite Paris-Est-Creteil-Val-de-Marne (UPEC); Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite	Fac Sci, Geol Lab, UPRES EA 2644, 2 Bd Lavoisier, F-49045 Angers, France.	debenay@univ-angers.fr	Lézine, Anne-Marie/A-5618-2013	LEZINE, Anne-Marie/0000-0002-3555-5124				ADMIRAAL W, 1982, ESTUAR COAST SHELF S, V14, P471, DOI 10.1016/S0302-3524(82)80071-6; Admirall W., 1984, Progress on Phycological Research, V3, P269; [Anonymous], 1976, MEMOIRES LINST GEOL; [Anonymous], 1999, Institute of Geological and Nuclear Sciences Monograph; [Anonymous], GREEN ALGAL GENERA S; [Anonymous], 1992, NEOGENE QUATERNARY D; Ballouche A., 1986, PROC S CLIMATIC FLUC, P517; BRUSH GS, 1981, LIMNOL OCEANOGR, V26, P295, DOI 10.4319/lo.1981.26.2.0295; Bryce S, 1998, MAR GEOL, V149, P55, DOI 10.1016/S0025-3227(98)00013-9; Carbonel P., 1988, P157; Carbonel P., 1980, MEMOIRES LINSTITUT G, V11, P1; CARBONEL P, 1973, B I GEOLOGIE BASSIN, V14, P75; Carter R.G. 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K., 1997, Archaeology Severn Estuary., V8, P29; Haslett SK, 2001, ESTUAR COAST SHELF S, V52, P143, DOI 10.1006/ecss.2000.0740; Hay MB, 2003, MAR MICROPALEONTOL, V48, P291, DOI 10.1016/S0377-8398(03)00025-2; HAYWARD BW, 1994, MICROPALEONTOLOGY, V40, P185, DOI 10.2307/1485816; Hippensteel SP, 2000, J FORAMIN RES, V30, P272, DOI 10.2113/0300272; HURLBERT SH, 1984, ECOL MONOGR, V54, P187, DOI 10.2307/1942661; JAGO CF, 1980, SEDIMENT GEOL, V26, P21, DOI 10.1016/0037-0738(80)90004-4; JENNINGS AE, 1992, J FORAMIN RES, V22, P13, DOI 10.2113/gsjfr.22.1.13; Lapointe M, 2000, MAR MICROPALEONTOL, V40, P43, DOI 10.1016/S0377-8398(00)00031-1; LAUT LLM, 1999, CUSHM FDN RES S QUAT; Le Campion J., 1970, Bull. Inst. geol. Bassin Aquitaine, VNo. 8, P3; Morzadec-Kerfourn M.-T., 1976, Revue Micropaleont, V18, P229; Morzadec-Kerfourn M.-T., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P267; Morzadec-Kerfourn M. 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C., 1994, Diatom Research, V9, P451; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALTON WILLIAM R., 1952, CONTR CUSHMAN FOUND FORAMINIFERAL RES, V3, P56; Yassini I., 1969, Bulletin de l'Institut de Geologie du Bassin d'Aquitaine, V7, P1; 2000, 90354 NF T MIN ENV A	65	37	39	0	17	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.	DEC	2003	58	4					843	860		10.1016/S0272-7714(03)00189-6	http://dx.doi.org/10.1016/S0272-7714(03)00189-6			18	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	753TY					2025-03-11	WOS:000187247700013
J	Matsuoka, K; Joyce, LB; Kotani, Y; Matsuyama, Y				Matsuoka, K; Joyce, LB; Kotani, Y; Matsuyama, Y			Modern dinoflagellate cysts in hypertrophic coastal waters of Tokyo Bay, Japan	JOURNAL OF PLANKTON RESEARCH			English	Article							MARINE-SEDIMENTS; YOKOHAMA-PORT; RESTING CYSTS; EUTROPHICATION; INDICATORS; PHYTOPLANKTON; DINOPHYCEAE; POLLUTION; NORTH	A survey of dinoflagellate resting cysts in surface sediment samples was carried out in Tokyo Bay, Japan, to document their horizontal distribution. At least 21 different cyst types were found. Dominant cyst types allowed the recognition of assemblages which form three different dinoflagellate cyst communities: the innermost part of the Bay, the central area and the mouth area. In all stations in Tokyo Bay, heterotrophic dinoflagellate cysts always occupied more than half of the cyst populations. Cysts of Polykrikos schwartzii/kofoidii are the most abundant heterotrophic species. These assemblages may reflect highly nutrient-enriched (hypertrophic) and turbulent water conditions. Among the cyst types found were probable ellipsoidal cysts of Alexandrium tamarense. This is the first record of toxic Alexandrium species cysts in Tokyo Bay sediments.	Nagasaki Univ, Fac Fisheries, Coastal Environm Sci, Nagasaki 8528521, Japan; Heriot Watt Univ, ICIT, Old Acad, Stromness, Orkney, England; Fisheries Res Agcy, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Hiroshima 7390452, Japan	Nagasaki University; Heriot Watt University; Japan Fisheries Research & Education Agency (FRA)	Matsuoka, K (通讯作者)，Nagasaki Univ, Fac Fisheries, Coastal Environm Sci, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.			Matsuyama, Yukihiko/0000-0002-2775-1723				Anderson Donald M., 1994, Scientific American, V271, P52; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; 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; Guo XY, 1998, CONT SHELF RES, V18, P677, DOI 10.1016/S0278-4343(98)80017-4; Hallegraeff GM, 1995, IOC MANUALS GUIDES; Han MS, 2000, J PLANKTON RES, V22, P1221, DOI 10.1093/plankt/22.7.1221; HAN MS, 1984, J PLANKTON RES, V15, P1425; JACOBSEN RT, 1986, J PHYS CHEM REF DATA, V15, P736; Kawabe M, 1998, OCEAN COAST MANAGE, V41, P19, DOI 10.1016/S0964-5691(98)00075-1; Lee J.B., 1994, P 2 INT S MAR SCI EX, P1; MATSUMOTO E, 1983, Chikyukagaku, V17, P27; Matsuoka K, 2000, PHYCOLOGIA, V39, P82, DOI 10.2216/i0031-8884-39-1-82.1; MATSUOKA K, 1976, Publications of the Seto Marine Biological Laboratory, V23, P351; 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., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; MATSUOKA K, 1982, FUNDAMENTAL STUDIES, P197; Matsuoka K., 1987, Bull. Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; NEHRING S, 1992, P INT COAST C ICC KI, P454; NIXON SW, 1995, OPHELIA, V41, P199, DOI 10.1080/00785236.1995.10422044; Nomura Hideaki, 1997, Mer (Tokyo), V35, P107; Ogura N., 1996, POLLUTION DISASTER T, P61; OSHIMA Y, 1992, TOXICON, V30, P1539, DOI 10.1016/0041-0101(92)90025-Z; SCHWINGHAMER P, 1994, AQUACULTURE, V122, P171, DOI 10.1016/0044-8486(94)90508-8; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Yoshida Y, 1998, NIPPON SUISAN GAKK, V64, P259	32	86	100	0	6	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	DEC	2003	25	12					1461	1470		10.1093/plankt/fbg111	http://dx.doi.org/10.1093/plankt/fbg111			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	753LH					2025-03-11	WOS:000187232500002
J	Sangiorgi, F; Capotondi, L; Nebout, NC; Vigliotti, L; Brinkhaus, H; Giunta, S; Lotter, AF; Morigi, C; Negri, A; Reichart, GJ				Sangiorgi, F; Capotondi, L; Nebout, NC; Vigliotti, L; Brinkhaus, H; Giunta, S; Lotter, AF; Morigi, C; Negri, A; Reichart, GJ			Holocene seasonal sea-surface temperature variations in the southern Adriatic Sea inferred from a multiproxy approach	JOURNAL OF QUATERNARY SCIENCE			English	Article						Adriatic sea; Holocene; multiproxy approach; SST; seasonality	LATE QUATERNARY LACUSTRINE; CENTRAL MEDITERRANEAN SEA; LAST 16,000 YEARS; DINOFLAGELLATE CYSTS; MAGNETIC-PROPERTIES; SAPROPEL FORMATION; MARINE-SEDIMENTS; DENSE WATER; ATLANTIC; RECORD	Holocene cooling events have been reconstructed for the southern Adriatic Sea (central Mediterranean) by means of analyses of organic walled dinoflagellate cysts, planktonic foraminifera, oxygen isotopes, calcareous nanoplankton, alkenones and pollen from a sediment core. Two cooling events have been detected, during which sea-surface temperatures (SSTs) were ca. 2degreesC lower. Unravelling the SST signal into dominant seasonal components suggests maximum winter cooling of 2degreesC at around 6.0 ka, whereas the cooling at ca. 3.0 ka might be the result of a spring temperature cooling of 2-3degreesC. The events, lasting several hundred years, are apparently synchronous with those in the Aegean Sea, where they have been related to known cooling events from the Greenland ice-core record. A distinct interruption in Adriatic Sea sapropel S1 is not clearly accompanied by a local drop in winter temperatures, but seems to be forced by ventilation, which probably occurred earlier in the Aegean Sea and was Subsequently transmitted to the Adriatic Sea. Copyright ( C) 2003 John Wiley Sons, Ltd.	Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, I-48100 Ravenna, Italy; CNR, Ist Geol Marina, I-40129 Bologna, Italy; Ctr Etud Saclay, Orme Merisiers, LSCE, F-91191 Gif Sur Yvette, France; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Ancona, Ist Sci Mare, I-60131 Ancona, Italy; Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	University of Bologna; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Universite Paris Saclay; Utrecht University; Marche Polytechnic University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, Via Ariani 1, I-48100 Ravenna, Italy.	franci@ambra.unibo.it	Brinkhuis, Henk/IUO-8165-2023; Negri, Alessandra/D-4085-2011; Vigliotti, Luigi/AAX-2638-2020; Lotter, Andre F./C-3477-2008; Capotondi, Lucilla/C-8874-2015; Morigi, Caterina/L-3883-2016; Reichart, Gert-Jan/N-6308-2018	Negri, Alessandra/0000-0002-8133-3936; 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Quat. Sci.	DEC	2003	18	8					723	732		10.1002/jqs.782	http://dx.doi.org/10.1002/jqs.782			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	758VA		Green Published			2025-03-11	WOS:000187670300004
J	Friedrich, O; Meier, KJS				Friedrich, O; Meier, KJS			Stable isotopic indication for the cyst formation depth of Campanian/Maastrichtian calcareous dinoflagellates	MICROPALEONTOLOGY			English	Article							SOUTH ATLANTIC-OCEAN; PLANKTONIC-FORAMINIFERA; SEA; RISE	delta(18)O and delta(13)C values for the calcareous dinoflagellate species Orthopithonella? globosa (Futterer 1984) Lentin and Williams 1985 and Pirumella krasheninnikovii (Bolli 1974) Lentin and Williams 1993 from latest Campanian and earliest Maastrichtian of ODP Hole 690C (Weddell Sea, Antarctic Ocean) have been studied in order to evaluate the species' depth habitat in the water column and their applicability in paleoceanographic studies. The calcareous dinoflagellates show isotopic values comparable to probably shallow-dwelling planktic foraminifera from the same samples in delta(18)O, but have an offset of about -5parts per thousand to -7parts per thousand, in delta(13)C. This suggests that calcareous dinoflagellate oxygen isotopes may provide information for paleoceanographic reconstructions of sea-surface water temperatures, whereas their extremely light carbon isotope values are probably due to photosynthetic processes.	Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany; Univ Bremen, Fachgebiet Hist Geol & Palaontol, D-28334 Bremen, Germany	Eberhard Karls University of Tubingen; University of Bremen	Friedrich, O (通讯作者)，Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30622 Hannover, Germany.	oliver.friedrich@bgr.de	Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. Sebastian/0000-0002-3918-4092				[Anonymous], 1978, DEEP SEA DRILL PROJ; Barreara E., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P813, DOI 10.2973/odp.proc.sr.113.137.1990; Barrera E, 1999, GEOL S AM S, P245; BAUMANN KH, 2003, IN PESS LATE QUATERN; BINDER BJ, 1987, J PHYCOL, V23, P99; Bolli H.M., 1974, Initial Rep Deep Sea Drilling Project, V27, P843; DEFLANDRE G, 1947, CR HEBD ACAD SCI, V224, P1781; Deflandre G., 1949, BOTANISTE, V34, P191; DHONDT S, 1995, PALEOCEANOGRAPHY, V10, P123, DOI 10.1029/94PA02671; Ennyu A, 2002, MAR MICROPALEONTOL, V46, P317, DOI 10.1016/S0377-8398(02)00079-8; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; FAIRBANKS RG, 1982, NATURE, V298, P841, DOI 10.1038/298841a0; FUTTERER DK, 1984, INITIAL REP DEEP SEA, V74, P533; GOODNEY DE, 1980, MAR MICROPALEONTOL, V5, P31, DOI 10.1016/0377-8398(80)90005-5; Hemleben C., 1989, MODERN PLANKTONIC FO, DOI [10.1007/978-1-4612-3544-6, DOI 10.1007/978-1-4612-3544-6]; 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; HUBER BT, 1995, GEOL SOC AM BULL, V107, P1164, DOI 10.1130/0016-7606(1995)107<1164:MLCCOT>2.3.CO;2; JANOFSKE D, 2000, THESIS U BREMEN, P94; Keupp H., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P497, DOI 10.2973/odp.proc.sr.122.189.1992; Keupp H., 1987, Facies, V16, P37, DOI 10.1007/BF02536748; KEUPP H, 1981, FACIES, V5; Keupp Helmut, 1993, Zitteliana, V20, P25; MEIER KJS, IN PRESS PALEOCEANOG; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Mulitza S., 1999, USE PROXIES PALEOCEA, P427, DOI DOI 10.1007/978-3-642-58646-0_17; Niebler H.-S., 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic, P165; Vink A, 2001, PALEOCEANOGRAPHY, V16, P479, DOI 10.1029/2000PA000582; VINK A, IN PRESS MARINE MICR; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Ziveri P, 2003, EARTH PLANET SC LETT, V210, P137, DOI 10.1016/S0012-821X(03)00101-8; ZONNEVELD K, IN PRESS MARINE MICR	32	20	20	0	1	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology	WIN	2003	49	4					375	380		10.1661/0026-2803(2003)049[0375:SIIFTC]2.0.CO;2	http://dx.doi.org/10.1661/0026-2803(2003)049[0375:SIIFTC]2.0.CO;2			6	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	762LK					2025-03-11	WOS:000187973200004
J	Gjani, E; Meço, S; Strauch, F				Gjani, E; Meço, S; Strauch, F			Litho-biostratigraphic data on the Tirana Depression (Albania) and their correlation with the Periadriatic Depression	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-MONATSHEFTE			English	Article						stratigraphy; biostratigraphy; palaeoecology; palaeoclimatology; dinoflagellate cysts; spores and pollen assemblages; Lower Oligocene; Middle-Upper; Miocene; Tirana Depression; Brad section; Ndroqi section		Lithology, dinoflagellate cysts and spores-pollen stratigraphy of the Brari section are described. Calibration is provided by planktonic foraminiferal biozones. Dinocysts and spores and pollen assemblages and their distribution have been used to identify the palaeoenvironnient and palaeoclimatology.	Polytech Univ Tirana, Fac Geol & Min, Tirana, Albania; Univ Munster, Inst Geol Palaontol, D-48149 Munster, Germany	Polytechnic University of Tirana (UPT); University of Munster	Gjani, E (通讯作者)，Polytech Univ Tirana, Fac Geol & Min, Tirana, Albania.							ALIAJ S, 1996, UNPUB NEOTECTONIC ST; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; GELATI R, 1997, RIV ITAL PALEONT STR, V103, P1; GJANI E, 1995, ROMANIAN J STRATIGR, V76, P35; GJANI E, 1989, THESIS POLYTECHNIC U; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Iaccarino S., 1985, P283; MUHAMETI P, 1993, UNPUB PALYNOSTRATIGR; Powell A.J., 1986, AASP CONTRIB SERIES, V17, P105; PRILLO S, 1994, UNPUB BIOSTRATIGRAPH; SHEHU R, 1981, INT S HELL AR TRENCH, P95; SIMONE L, 1998, SEDIMENT GEOL AMSTER, V60, P647; SOREL D, 1992, B SOC GEOL FR, V163, P447; WILLIAMS GL, 1975, B GEOL SURV CANADA, V236; Williams GL., 1977, American Association of Stratigraphic Palynologists Contribution Series A, V5, P14; WILLIAMS GL, 1985, CAMBRIDGE EARTH SCI, P847; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169	17	0	0	0	3	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0028-3630			NEUES JAHRB GEOL P-M	Neues Jahrb. Geol. Palaontol.-Monatsh.	DEC	2003		12					723	738						16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	758MT					2025-03-11	WOS:000187638400002
J	Molinet, C; Lafon, A; Lembeye, G; Moreno, CA				Molinet, C; Lafon, A; Lembeye, G; Moreno, CA			Spatial and temporal distribution patterns of blooms of <i>Alexandrium catenella</i> (Whedon & Kofoid) Balech 1985, on inland seas of northwest Patagonia, Chile	REVISTA CHILENA DE HISTORIA NATURAL			Spanish	Article						Alexandrium catenella; distribution; inland seas; southern Chile	CYSTS; DINOPHYCEAE; TAMARENSE	The presence of the toxic dinoflagellate Alexandrium catenella was first recorded during the early 1990s in the fjords and inland seas of the Chilean Northwest Patagonia. In 1995 regular phytoplankton monitoring programs were initiated with the financial support of different national institutions with the purpose of detecting these toxic dinoflagellates and assessing their effects on shellfish. During this period, an important but incomplete database was obtained, due mainly to the different work objectives of each monitoring program. In this paper we review the available data, searching for patterns that help us to gain insights into the temporal and spatial distribution of A catenella in this region. During the early years (1995 to 1998) the sampling was undertaken monthly and since later 2000 onwards, samples were taken every week but in fewer sampling stations. Phytoplankton and shellfish samples were collected in the same stations but these varied in number every year. From late 1995 to 2002 four toxic algae blooms of A. catenella were recorded with different intensity and distribution patterns. However, a pattern became apparent when the distribution was expanding northwards (from 45degrees47' S in 1996 to 42degrees S, Chiloe in 2002). All four algae blooms recorded were highly seasonal,(spanning from January to March) and were correlated with the highest paralytic shellfish poisoning (PSP) records. We suggest that benthic cyst beds are a very important factor in initiating toxic dinoflagellate blooms of A. catenella in the fjords and inland seas of southern Chile, whose life cycle shows a biannual occurrence, possibly due to variations in environmental conditions. This apparent cycle could be a response to oscillations in the neighbor ocean affecting general circulation patterns as well as water column features (e.g., temperature) of inland seas, favoring or inhibiting these toxic blooms. Expanding spatial distribution of A. catenella blooms seems to be strongly related to surface water drift driven by wind forcing as well as by circulation features of inland seas in northwest Patagonia in southern Chile.	Univ Austral Chile, Ctr Univ Trapananda, Coyhaique, Chile; Univ Austral Chile, Inst Ecol & Evoluc, Valdivia, Chile	Universidad Austral de Chile; Universidad Austral de Chile	Univ Austral Chile, Ctr Univ Trapananda, Portales 73, Coyhaique, Chile.	cmolinet@uach.cl						Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; 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, 1999, P 6 CAN WORKSH HARMF, P88; *ASS OFF AN CHEM, 1980, OFF METH AN, P298; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; Cortes-Altamirano R., 1996, Harmful and Toxic Algal Blooms, P101; Dahl E, 2001, PHYCOLOGIA, V40, P223, DOI 10.2216/i0031-8884-40-3-223.1; Eilertsen H.C., 1998, HARMFUL ALGAE, P196; FRAGA S, 1993, TOXIC PHYTOPLANKTON; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; Godhe A, 2002, MAR ECOL PROG SER, V240, P71, DOI 10.3354/meps240071; Guzm L., 1975, AN I PATAGONIA, V6, P229; Guzman L., 2002, FLORACIONES ALGALES, P235; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; HALTEAD W, 1984, WHO OFFSET PUBLICATI, V79; HEAPS A, QUASIBIENNIAL ZONAL; HELBLING EW, 2001, MARINE ECOLOGY PROGR, V211, P49; HOLTON JR, 2002, R REED S; Itakura S, 2001, PHYCOLOGIA, V40, P263, DOI 10.2216/i0031-8884-40-3-263.1; Jellett J.F., 1993, WORLD AQUACULT, V24, P32; LEMBEYE G, 1997, RESULTADOS CRUCERO C, V3, P73; LEMBEYE G, 1998, 9749 FIP U AUSTR CHI; Lembeye G., 1975, I PATAGONIA 6, V1-2, P197; LEMBEYE G, 1996, RESULTADOS CRUCERO C, V2, P64; LEMBEYE G, 1997, 9523B FIP U AUSTR CH; LEMBEYE-V G, 1981, Anales del Instituto de la Patagonia, V12, P273; LEMBEYE-V G, 1981, Anales del Instituto de la Patagonia, V12, P277; Matthews SG., 1996, Harmful and Toxic Algal Blooms, P89; MOLINET C, 1998, ANAL MONITOREO MAREA; MOLINET C, 2002, MONITOREO FITOPLANCT; Munoz Pablo, 1992, Revista de Biologia Marina, V27, P187; ORLOVA TY, 2002, HARMFUL ALGAL BLOOMS, V23, P47; Park J.S., 1967, B FISHERIES RES DEV, V1, P63; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; Piumsomboon A., 2001, Harmful Algal Blooms 2000, P12; Reid PC, 2001, MAR ECOL PROG SER, V215, P283, DOI 10.3354/meps215283; SALINAS S, 2002, RESULTADOS CRUCERO C, P33; SATINELLI N, 2002, FLORACIONES ALGALES, P199; SEGUEL M, 2002, RESULTADOS CRUCERO C, P91; Silva N., 1998, CIENC TECNOL MAR, V21, P17; Silva N., 1997, Cienc. Technol. Mar, V20, P23; Silva-S. Nelson, 1995, Revista de Biologia Marina, V30, P207; Sordo I, 2001, ESTUAR COAST SHELF S, V53, P787, DOI 10.1006/ecss.2000.0788; Strub P.T., 1998, SEA, V11., P273; Taylor FJR, 1996, CAN J FISH AQUAT SCI, V53, P2310, DOI 10.1139/f96-181; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; Uribe J.C., 1988, ANS I 5 SER CS NTS P, V18, P97; URIBE JC, 1995, 9316 FIP U MAG; Vila M, 2001, MAR ECOL PROG SER, V222, P73, DOI 10.3354/meps222073; Weise AM, 2002, CAN J FISH AQUAT SCI, V59, P464, DOI 10.1139/F02-024; White WB, 1996, NATURE, V380, P699, DOI 10.1038/380699a0	54	66	67	1	24	SOC BIOLGIA CHILE	SANTIAGO	CASILLA 16164, SANTIAGO 9, CHILE	0716-078X	0717-6317		REV CHIL HIST NAT	Rev. Chil. Hist. Nat.	DEC	2003	76	4					681	698						18	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	760EK					2025-03-11	WOS:000187798500011
J	Adachi, M; Kanno, T; Okamoto, R; Itakura, S; Yamaguchi, M; Nishijima, T				Adachi, M; Kanno, T; Okamoto, R; Itakura, S; Yamaguchi, M; Nishijima, T			Population structure of <i>Alexandrium</i> (Dinophyceae) cyst formation-promoting bacteria in Hiroshima Bay, Japan	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							DINOFLAGELLATE GONYAULAX-TAMARENSIS; FRAGMENT-LENGTH-POLYMORPHISM; INTERNAL TRANSCRIBED SPACER; RIBOSOMAL-RNA GENES; SP-NOV; MARINE-BACTERIA; SP. NOV.; CLASS PROTEOBACTERIA; PROROCENTRUM-LIMA; ALPHA-SUBCLASS	A total of 31 bacterial isolates that have potential Alexandrium cyst formation-promoting activity (Alex-CFPB) were isolated from Hiroshima Bay (Japan), which is characterized by seasonal blooms of the toxic dinoflagellate Alexandrium tamarense. The population structure of Alex-CFPB was analyzed by means of restriction fragment length polymorphism analysis of the 16S rRNA genes (16S rDNA). Fourteen ribotypes, A to N, were observed among the 31 isolates of Alex-CFPB by using four restriction enzymes, MboI, HhaI, RsaI and BstUI. Among them, seven isolates, which were obtained from the seawater samples taken during the peak and termination periods of the A. tamarense bloom in 1998, belonged to ribotype A. This result suggests that bacterial strains of ribotype A may be dominant in the Alex-CFPB assemblages during these periods. The partial 16S rDNA-based phylogenetic tree of 10 ribotypes studied showed that nine of them fell into the Rhodobacter group of the alpha subclass of the Proteobacteria. Eight of nine ribotypes of the Rhodobacter group fell into the lineage of the Roseobacter subgroup, and one fell into the Rhodobacter subgroup. The non-Rhodobacter group type fell into the Marinobacterium-Neptunomonas-Pseudomonas group of the gamma-Proteobacteria. Isolates of Alex-CFPB ribotypes A and C do not have clear growth-promoting activities but have strong cyst formation-promoting activities (CFPAs) under our laboratory conditions. These results show that the Alex-CFPB assemblage may consist of various bacteria that belong mainly to the Roseobacter group and have strong CFPAs. These results suggest that not only the Alexandrium cyst formation-inhibiting bacteria (Alex-CFIB) reported previously but also Alex-CFPB, especially bacteria of ribotype A, may play significant roles in the process of encystment and bloom dynamics of Alexandrium in the natural environment.	Kochi Univ, Lab Aquat Environm Sci, Fac Agr, Kochi 7838502, Japan; Fisheries Agcy Japan, Natl Res Inst Fisheries & Environm Seto Inland Se, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Kochi University; Japan Fisheries Research & Education Agency (FRA)	Adachi, M (通讯作者)，Kochi Univ, Lab Aquat Environm Sci, Fac Agr, Kochi 7838502, Japan.							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Environ. Microbiol.	NOV	2003	69	11					6560	6568		10.1128/AEM.69.11.6560-6568.2003	http://dx.doi.org/10.1128/AEM.69.11.6560-6568.2003			9	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	740XK	14602614	Green Published			2025-03-11	WOS:000186427800030
J	Head, MJ; Borel, CM; Guerstein, GR; Harland, R				Head, MJ; Borel, CM; Guerstein, GR; Harland, R			The problematic aquatic palynomorph genus <i>Cobricosphaeridium</i> Harland and Sarjeant, 1970 emend., with new records from the Holocene of Argentina	JOURNAL OF PALEONTOLOGY			English	Article							DINOFLAGELLATE CYSTS; MORPHOLOGY; CHLOROPHYTA; ACARTIIDAE; EGGS	The aquatic palynomorph genus Cobricosphaeridium Harland and Sarjeant, 1970 was described from Holocene deposits of Australia. Restudy of the type material shows that these palynomorphs may represent the eggs of crustaceans, and that earlier attributions to the division Dinoflagellata are unsustainable. The genus Aquadulcum Harland and Sarjeant, 1970, also first described as a dinoflagellate from the Holocene of Australia, is treated as a synonym of Cobricosphaeridium, and the following new combinations are proposed: C. awendae, C. myalupense, C. pikeae, C. serpens, C. yanchepense, C.? ovatum, and C.? vermiculatum. Previous records of the genus are restricted to the Holocene and indicate a freshwater affinity. Cobricosphaeridium has now been found in Holocene subsurface brackish deposits of Laguna Hinojales in eastern Argentina. This is the first record of this genus from South America and unequivocally extends its ecological range into a brackish environment. Several species are represented, including Cobricosphaeridium hinojalensis new species; and their potential as paleoenvironmental indicators is evaluated.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, RA-8000 Bahia Blanca, Buenos Aires, Argentina; DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Anim & Plant Sci, Palynol Res Facil, Sheffield S10 2TN, S Yorkshire, England	University of Cambridge; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Sheffield	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk; maborel@criba.edu.ar; gmguerst@criba.edu.ar; rex.harland@ntlworld.com		Borel, C. Marcela/0000-0001-5772-4534				BATTEN D.J., 1996, PALYNOLOGY PRINCIPLE, V1, P205; Belmonte G, 1997, CRUSTACEANA, V70, P114, DOI 10.1163/156854097X00401; Belmonte G, 1998, J MARINE SYST, V15, P35, DOI 10.1016/S0924-7963(97)00047-X; 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, IN PRESS SIGNIFICADO; BURDEN ET, 1986, CAN J EARTH SCI, V23, P43, DOI 10.1139/e86-005; Castro-Longoria E, 2001, CRUSTACEANA, V74, P225, DOI 10.1163/156854001505479; Churchill D. M., 1962, Grana Palynologica, V3, P29; DORBIGNY A., 1835, Revue Mag Zool, V5, P1; DORBIGNY AD, 1839, RAMON SAGRA HIST PHY, P1; Ehrenberg C.G., 1840, CHARACTERISTIK 274 N; Ehrenberg C. 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Paleontol.	NOV	2003	77	6					1159	1181		10.1666/0022-3360(2003)077<1159:TPAPGC>2.0.CO;2	http://dx.doi.org/10.1666/0022-3360(2003)077<1159:TPAPGC>2.0.CO;2			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	744PN		Green Published			2025-03-11	WOS:000186641000012
J	Nohr-Hansen, H				Nohr-Hansen, H			Dinoflagellate cyst stratigraphy of the palaeogene strata from the Hellefisk-1, Ikermiut-1, Kangamiut-1, Nukik-1, Nukik-2 and Qulleq-1 wells, offshore West Greenland	MARINE AND PETROLEUM GEOLOGY			English	Article						dinoflagellate cyst stratigraphy; palaeogene; offshore West Greenland	GLOBAL STRATOTYPE SECTION; LABRADOR SEA; NORTH-SEA; BIOSTRATIGRAPHY	A new Palaeogene dinoflagellate cyst stratigraphy from offshore West Greenland has been described based on the strata from the Hellefisk-1, Ikermiut-1, Kangamiut-1, Nukik-1, Nukik-2 and Qulleq-1 wells. Twenty-one palynological intervals are defined from the Late Eocene to the late Early Paleocene. This stratigraphy has been correlated with a new microfossil zonation and previous established North Sea zonations. The stratigraphy and well correlation are based on last appearance datum events and abundances of stratigraphically important species from 355 samples, 148 of which are sidewall core samples. A major middle Eocene hiatus spanning the early Lutetian and a major Early Paleocene hiatus spanning the Late Santonian, Late Cretaceous to the early Danian have been recognised from the offshore deposits. (C) 2002 Elsevier Ltd. 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.	HNH@geus.dk	Nohr-Hansen, Henrik/G-9058-2018	Nohr-Hansen, Henrik/0000-0002-9291-8104				[Anonymous], 1988, Geol. 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Pet. Geol.	NOV	2003	20	9					987	1016	PII S0264-8172(02)00116-2	10.1016/S0264-8172(02)00116-2	http://dx.doi.org/10.1016/S0264-8172(02)00116-2			32	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	769HA					2025-03-11	WOS:000188642500002
J	Rasmussen, JA; Nohr-Hansen, H; Sheldon, E				Rasmussen, JA; Nohr-Hansen, H; Sheldon, E			Palaeoecology and palaeoenvironments of the lower palaeogene succession, offshore West Greenland	MARINE AND PETROLEUM GEOLOGY			English	Article						North Atlantic; palaeogene; palaeoenvironment; microfossils; palynomorphs	DINOFLAGELLATE CYSTS; FORAMINIFERAL BIOSTRATIGRAPHY; LATE EOCENE; NORTH; LABRADOR; SEA; SEDIMENTS; DINOCYST; REGIONS	The microfossil and palynofloral assemblages of the Paleocene to middle Eocene succession, offshore West Greenland, have been investigated. Several taxa, which are believed to reflect specific palaeoenvironments were selected, and their relative abundances measured. Subsequently, an interpretation of the changing depositional settings in the Hellefisk-1, Ikermiut-1, Kangamiut-1, Nukik-1 and Nukik-2 boreholes through the lower Palaeogene has been made. (C) 2004 Elsevier Ltd. All rights reserved.	Geol Survey Denmark & Greenland, Dept Stratig, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Dept Stratig, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	jar@geus.dk	Rasmussen, Jan Audun/Q-7472-2018; Nohr-Hansen, Henrik/G-9058-2018; Sheldon, Emma/H-5281-2018	Rasmussen, Jan Audun/0000-0003-0520-9148; Nohr-Hansen, Henrik/0000-0002-9291-8104; Sheldon, Emma/0000-0003-4353-8241				[Anonymous], 1996, SPECIAL PUBLICATIONS, DOI DOI 10.1144/GSL.SP.1996.101.01.17; AUBRY MP, 2002, ANN REPORT 2001 PALE; Batten DJ., 1996, Palynology: principles and applications, P191; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BERGGREN WA, 1975, PALAEOGEOGR PALAEOCL, V18, P73, DOI 10.1016/0031-0182(75)90025-5; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; BROTZEN F, 1948, SVERIGES GEOLOGISK C, P493; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Chalmers J. 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Pet. Geol.	NOV	2003	20	9					1043	1073		10.1016/j.marpetgeo.2003.11.001	http://dx.doi.org/10.1016/j.marpetgeo.2003.11.001			31	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	769HA					2025-03-11	WOS:000188642500005
J	Piasecki, S				Piasecki, S			Neogene dinoflagellate cysts from Davis Strait, offshore West Greenland	MARINE AND PETROLEUM GEOLOGY			English	Article						neogene; dinoflagellate cysts; Qulleq-1; West Greenland	PLIOCENE; UPLIFT; GENERA	The Qulleq-1 exploration well was drilled offshore West Greenland in the year 2000. The well penetrated Neogene sediments and a limited number of samples were studied for their content of dinoflagellate cysts in order to determine the age of the succession. Other relevant data 14 from the region are restricted to ODP cores drilled in the late 1980s in Baffin Bay and Labrador Sea so all new information is important. The horizontally stratified Cenozoic succession drapes the crests of rotated fault-block of Cretaceous sediments. Four stratigraphical units were discriminated in the Neogene succession: Upper Pliocene, Lower Pliocene, Upper Miocene and Middle Miocene. A similar to40 Myr hiatus separates Neogene from Palaeogene sediments, and Miocene sediments are separated from Pliocene sediments by a similar to2 Myr hiatus. The dinoflagellate flora is comparable to other North Atlantic sites but is depleted in terms of recovery. The fairly rich Miocene flora diminishes in the Lower Pliocene and almost disappears in the Upper Pliocene, probably reflecting deterioration of the climate. The dinoflagellate assemblages indicate deposition in open marine environments. Both Middle and Upper Miocene assemblages are characterised by abundant Operculodinium giganteum, Operculodinium centrocarpum, Spiniferites pseudofurcatus, Habibacysta tectata, Pyxidiniopsis pastilliformis, Labyrinthodinium truncatum and Spiniferites spp. The Pliocene assemblages are characterised by the stepwise disappearance of Miocene dinoflagellates; Cymatiosphaera spp., Nematosphaeropsis spp. and Impagidinium spp. become dominant in poor assemblages. Reworked spores, pollen and dinoflagellate cysts from Upper Palaeozoic, Mesozoic and Palaeogene sources are abundant throughout the Neogene. (C) 2002 Elsevier Ltd. All rights reserved.	Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.	sp@geus.dk						Berggren W.A., 1972, Initial Reports of the Deep Sea Drilling Project, V12, P965; CHALMERS JA, 2001, GEOLOGICAL SOC SPECI, V187, P79; Chalmers JK, 2000, GLOBAL PLANET CHANGE, V24, P311, DOI 10.1016/S0921-8181(00)00015-1; Christiansen FG., 2001, GEOLOGY GREENLAND SU, V189, P24; Corradini D., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P221; Dam G, 1999, J GEOL SOC LONDON, V156, P653; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; 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, MICROPALEONTOLOGY S, V42, P172; 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.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P515, DOI 10.2973/odp.proc.sr.105.178.1989; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; Head MJ, 2000, J PALEONTOL, V74, P812, DOI 10.1666/0022-3360(2000)074<0812:GWANGD>2.0.CO;2; LENTIN JK, 1994, CAN J EARTH SCI, V31, P567, DOI 10.1139/e94-050; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; Matsuoka K., 1992, NEOGENE QUATERNARY D, P165; Mudie P.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P587, DOI 10.2973/odp.proc.sr.104.174.1989; NOHRHANSEN H, 2000, 2000101 GEOL SURV DE; NOHRHANSEN H, 2002, MARINE PETROLEUM GEO; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Piasecki S, 2002, MAR PETROL GEOL, V19, P55, DOI 10.1016/S0264-8172(01)00053-8; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Powell A.J., 1992, P155; ROLLE F, 1985, CAN J EARTH SCI, V22, P1001, DOI 10.1139/e85-105; Smelror Morton, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P83; VERSTEEGH GJM, 1995, REV PALAEOBOT PALYNO, V85, P213, DOI 10.1016/0034-6667(94)00127-6; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	29	37	38	0	3	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0264-8172	1873-4073		MAR PETROL GEOL	Mar. Pet. Geol.	NOV	2003	20	9					1075	1088	PII S0264-8172(02)00089-2	10.1016/S0264-8172(02)00089-2	http://dx.doi.org/10.1016/S0264-8172(02)00089-2			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	769HA					2025-03-11	WOS:000188642500006
J	Reichart, GJ; Brinkhuis, H				Reichart, GJ; Brinkhuis, H			Late quaternary <i>Protoperidinium</i> cysts as indicators of paleoproductivity in the northern Arabian Sea	MARINE MICROPALEONTOLOGY			English	Article						organic-walled dinoflagellate cysts; Protoperidinium; planktonic foraminifera; geochemistry; Arabian Sea; marine productivity	OXYGEN MINIMUM ZONE; ORGANIC-MATTER; INDIAN-OCEAN; ENHANCED PRESERVATION; VERTICAL-DISTRIBUTION; BENTHIC FORAMINIFERA; SEDIMENTS; RECORD; OCEANOGRAPHY; DEGRADATION	The reliability of organic-walled cysts of the heterotrophic dinoflagellate Protoperidinium as paleoproductivity indicators and the influence of bottom water oxygenation on cyst preservation is assessed by using Arabian Sea records of the past similar to 125 kyr as a natural laboratory. Multidisciplinary geochemical, micropaleontological and palynological datasets are integrated to analyze the relationship between Protoperidinium cyst concentrations and other paleoproductivity proxies. Differential preservation potential is quantified in order to establish threshold oxidative degradation values for a possible application of quantitative Protoperidinium cyst records in paleoenvironmental reconstructions. Results indicate that variations in Protoperidinium cyst concentration closely correspond to other marine productivity and/or upwelling proxies. Although oxygenation will lead to significant cyst degradation, and thus decreased concentrations, down-core patterns in Protoperidinium cyst concentration still primarily reflect changes in sea surface productivity. In view of differential preservation among dinoflagellate cysts, down-core variations in relative abundance of Protoperidinium should be treated with caution. (C) 2003 Elsevier B.V. All rights reserved.	Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; Univ Utrecht, Fac Earth Sci, Dept Geochem, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Palaeobot & Palynol Lab, 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, D-27570 Bremerhaven, Germany.	greichart@awi-bremerhaven.de	Brinkhuis, Henk/B-4223-2009; Reichart, Gert-Jan/N-6308-2018	Reichart, Gert-Jan/0000-0002-7256-2243; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 1984, MARINE GEOLOGY OCEAN; Brock JC, 1992, PALEOCEANOGRAPHY, V7, P799, DOI 10.1029/92PA01267; Codispoti L. 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Micropaleontol.	NOV	2003	49	4					303	315		10.1016/S0377-8398(03)00050-1	http://dx.doi.org/10.1016/S0377-8398(03)00050-1			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	751EN		Green Published			2025-03-11	WOS:000187040000001
J	Nagai, S; Itakura, S; Matsuyama, Y; Kotani, Y				Nagai, S; Itakura, S; Matsuyama, Y; Kotani, Y			Encystment under laboratory conditions of the toxic dinoflagellate <i>Alexandrium tamiyavanichii</i> (Dinophyceae) isolated from the Seto Inland Sea, Japan	PHYCOLOGIA			English	Article							SEXUAL REPRODUCTION; LIFE-HISTORY; GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; COHORTICULA; GERMINATION; CYSTS; CELLS; GULF	The encystment of the toxic dinoflagellate Alexandrium tamiyavanichii, isolated from the Seto Inland Sea, Japan, was clarified for the first time under laboratory conditions. Sexual reproduction was by conjugation of isogametes, and plasmogamy was completed 60-80 min after conjugation started, producing a planozygote with one transverse and two longitudinal flagella, and forming a cyst. Cysts were vertically compressed or spherical. Cysts were 45-75 mum long, 35-60 mum wide and 40-60 mum high. The surface of cysts was smooth, and there was no paratabulation. Encystment through sexual reproduction was observed in 54 pairs out of 136, which included 16 self-crossing by use of 16 nonaxenic clonal strains. No planozygote formation or encystment was found with any self-crossing, indicating the heterothallism of this species.	Fisheries Res Agcy Japan, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Saeki, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Fisheries Res Agcy Japan, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Saeki, Hiroshima 7390452, Japan.	snagai@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063; Matsuyama, Yukihiko/0000-0002-2775-1723				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; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BALECH E, 1994, T AM MICROSC SOC, V113, P216, DOI 10.2307/3226651; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Delgado M, 1997, J PLANKTON RES, V19, P749, DOI 10.1093/plankt/19.6.749; 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; FUKUYO Y, 1988, Bulletin of Plankton Society of Japan, V35, P9; Fukuyo Y., 1989, P403; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Guillard R. 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J	Riding, JB; Rose, J; Booth, SJ				Riding, JB; Rose, J; Booth, SJ			Allochthonous and indigenous palynomorphs from the Devensian of the Warham Borehole, Stiffkey, north Norfolk, England; evidence for sediment provenance	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							PLEISTOCENE; POLLEN; TILLS; CRAG; UK	Late Devensian glaciolacustrine sediments proved by the Warham Borehole, near Stiffkey, north Norfolk, have yielded abundant and diverse recycled palynomorphs of Carboniferous, Permian, Triassic, Jurassic, Early Cretaceous and Palaeogene age. Indigenous Quaternary palynomorphs are a relatively minor component of the palynofloras; Carboniferous and Jurassic palynomorphs are the most commonly occurring forms. Middle Jurassic spores and pollen and Toarcian (Lower Jurassic) and Kimmeridgian (Upper Jurassic) dinoflagellate cysts are prominent, and the latter may indicate derivation from particularly resistant Toarcian and Kimmeridgian lithologies. Surprisingly, few grains were derived from the Chalk Group, which crops out locally. The recycled palynomorphs are interpreted as having been derived from local glacial deposits and then incorporated into the glaciolacustrine sediments of proglacial Lake Stiffkey, at the margin of the Late Devensian ice sheet. The lowest sample studied was the most productive palynologically. It was probably derived from nearby Lowestoft Till, an interpretation that agrees with the sedimentological evidence. The allochthonous palynomorphs from samples collected higher in the glaciolacustrine succession were probably derived from glaciogenic sediments deposited at the margin of the Late Devensian ice sheet. Based on the palynofloras, the Late Devensian ice flowed south from Scotland across the northern Pennines and NE England, down the western flank of the North Sea Basin to north Norfolk. The terrestrial nature of the indigenous Quaternary palynomorphs recovered is consistent with an ice-marginal and glaciolacustrine depositional setting.	British Geol Survey, Keyworth NG12 5GG, Notts, England; Univ London Royal Holloway & Bedford New Coll, Dept Geog, Egham TW20 0EX, Surrey, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of London; Royal Holloway University London	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.		Rose, Jim/H-8944-2019					[Anonymous], 2000, QUATERNARY NEWSL; [Anonymous], B GEOL SOC NORFOLK; [Anonymous], 1996, Palynology: principles and applications; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; Batten DJ., 1996, Palynology: principles and applications, P191; Boulton G.S., 1977, BRIT QUATERNARY STUD, P231; Brand D, 2002, P YORKS GEOL SOC, V54, P35, DOI 10.1144/pygs.54.1.35; BUTTERWORTH MA, 1985, POLLEN SPORE BIOSTRA, P3; Catt J. A., 1966, Proc Yorks geol (polyt) Soc, V35, P375; Clayton G., 1977, MEDEDELINGEN RIJKS G, V29; Costa L. I., 1992, BRIT MICROPALAEONTOL, P99; Davey RJ, 2001, NEUES JAHRB GEOL P-A, V219, P83, DOI 10.1127/njgpa/219/2001/83; DREIMANIS A, 1989, CAN J EARTH SCI, V26, P1667, DOI 10.1139/e89-143; GALE SJ, 1986, NAR VALLEY N NORFOLK, P66; HANSEN JM, 1980, B GEOLOGICAL SOC DEN, V28, P131; HEILMANNCLAUSEN C, 1987, DANMARKS GEOLOGISK A, V17; Herngreen G.F.W., 2000, MEDEDELINGEN NEDERLA, V63; Hunt C. 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A., 1978, P YORKS GEOL SOC, V42, P55, DOI DOI 10.1144/PYGS.42.1.55; Morbey S.J., 1978, CONTINENTAL SHELF I, V100, P47; Morbey S.J., 1978, Palinologia numero extraordinario, V1, P355; ORBELL G., 1973, Bulletin of the Geological Survey of Great Britain, V44, P1; Palliani RB, 2000, P YORKS GEOL SOC, V53, P1, DOI 10.1144/pygs.53.1.1; PARTINGTON MA, 1993, PETROLEUM GEOLOGY NW, V1, P371; PERRIN RMS, 1979, PHILOS T ROY SOC B, V287, P535, DOI 10.1098/rstb.1979.0083; Powell AJ, 1992, BRIT MICROPALAEONTOL, P155; RAWSON PF, 1978, 9 GEOL SOC LOND; RIDING J B, 1988, Palynology, V12, P65; 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., 1999, AM ASS STRATIGRAPHIC, V36; Riding James B., 1991, Palynology, V15, P115; Riding JB, 1997, P GEOLOGIST ASSOC, V108, P25, DOI 10.1016/S0016-7878(97)80003-X; Riding JB, 2000, P GEOLOGIST ASSOC, V111, P161, DOI 10.1016/S0016-7878(00)80006-1; RIDING JB, 2001, IR01155 BRIT GEOL SU; RIDING JB, 2000, WH200011R BRIT GEOL; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; RIDING JB, 2002, IR02154 BRIT GEOL SU; RIDING JB, 1999, WH9998R BRIT GEOL SU; ROSE J, 1985, BOREAS, V14, P225; SRIVASTAVA SK, 1987, GEOBIOS-LYON, V20, P5, DOI 10.1016/S0016-6995(87)80057-8; SRIVASTAVA SK, 1978, BIOL MEM, V3, P1; STRAW A, 1960, P GEOLOGISTS ASS, V71, P374; TROTTER FM, 1932, Q J GEOL SOC LOND, V69, P374; WARRINGTON G, 1985, POLLEN SPORE BIOSTRA, P11; West RG, 1999, QUATERNARY SCI REV, V18, P1247, DOI 10.1016/S0277-3791(98)00067-5; WOOD GD, 1996, AM ASS STRATIGRAPHIC, V1, P29	50	14	14	0	5	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.	NOV	2003	54		4				223	235		10.1144/pygs.54.4.223	http://dx.doi.org/10.1144/pygs.54.4.223			13	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	747PK					2025-03-11	WOS:000186813200001
J	Torricelli, S; Amore, MR				Torricelli, S; Amore, MR			Dinoflagellate cysts and calcareous nannofossils from the Upper Cretaceous Saraceno formation (Calabria, Italy): Implications about the history of the Liguride Complex	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						biostratigraphy; organic-walled dinoflagellate cysts; calcareous nannofossils; Late Cretaceous; Liguride Complex; southern Apennines; Italy	NORTHERN APENNINES; BIOSTRATIGRAPHY; ZONATION	Organic-walled dinoflagellate cysts and calcareous nannofossils recovered from the turbidites of the Saraceno Formation out-cropping in the type area (north-eastern Calabria, Italy) are presented. They provide new information about the age of the Saraceno Formation, hence a constraint to reconstruct the timing of deformations that affected the Liguride Complex. The distribution of dinoflagellate cysts and calcareous nannofossils in the succession studied is compared with biostratigraphies available for the Upper Cretaceous. Accordingly, the age of the lower-most part of the Fiumara Saraceno section is latest Albian to Turonian, whereas the upper part of the section is dated as late Campanian-?earliest Maastrichtian. A hiatus spanning the Coniacian, the Santoman and most of the Campanian is inferred between these two successions, which are also distinguished by the presence and absence of flint respectively. Consistencies and discrepancies of the present data with biostratigraphical information previously published for the Saraceno Formation, are discussed.	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.	maria.rosa.amore@agip.it						[Anonymous], 1963, MEM SOC GEOL ITAL; [Anonymous], 1978, RIV IT PALEONT; [Anonymous], 1996, Palynology: principles and applications; ANTONESCU E, 2001, CAMPANIAN MAASTRICHT, P253; Aurisano R.W., 1989, Palynology, V13, P143; Baruffini L, 2000, RIV ITAL PALEONTOL S, V106, P73, DOI 10.13130/2039-4942/5391; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; Bown P., 1998, CALCAREOUS NANNOFOSS; Bralower TJ, 1988, PALEOCEANOGRAPHY, V3, P275, DOI 10.1029/PA003i003p00275; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Erba E., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V129, P179, DOI 10.2973/odp.proc.sr.129.118.1992; Erba E., 1995, Proc. ODP, V144, P873; Fensome R.A., 1993, Micropaleontology Press Special Paper; GRADSTEIN FM, 1994, J GEOPHYS RES-SOL EA, V99, P24051, DOI 10.1029/94JB01889; KIRSCH KH, 1991, MUNCHNER GEOWISSENSC, V22; KNOTT SD, 1987, TECTONOPHYSICS, V142, P217, DOI 10.1016/0040-1951(87)90124-7; MCMINN A, 1988, ALCHERINGA, V12, P137, DOI 10.1080/03115518808619002; Mohr B. A. R., 1997, Palynology, V21, P41; Ogniben L., 1969, MEMORIE SOC GEOLOGIC, V8, P453; Perch-Nielsen K., 1985, P427; Perch-Nielsen K., 1985, P329; Riegel W., 1974, Revista Esp Micropaleont, V6, P347; Robaszynski F., 1985, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V9, P1; Roncaglia L, 1997, REV PALAEOBOT PALYNO, V97, P177, DOI 10.1016/S0034-6667(96)00070-X; Roncaglia L, 1997, NEWSL STRATIGR, V35, P29; ROTH PH, 1978, CRETACEOUS NANNOPLAN, V17, P731; Schioler P., 2001, Developments in Palaeontology and Stratigraphy, V19, P221; Selli R., 1962, MEM SOC GEOL ITAL, V3, P737; SILVA IP, 1999, GEOLOGICAL SOC AM SP, V332, P301, DOI DOI 10.1130/0-8137-2332-9.301; SISSINGH W, 1977, Geologie en Mijnbouw, V56, P37; Tremolada F, 2002, RIV ITAL PALEONTOL S, V108, P441, DOI 10.13130/2039-4942/5487; Van Dijk JP, 2000, TECTONOPHYSICS, V324, P267, DOI 10.1016/S0040-1951(00)00139-6; Vezzani L., 1968, Geologica Romana, V7, P229; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P817; WILLIAMS GL, SCI RESULTS ODP LEG; Yepes Oscar, 2001, Palynology, V25, P217, DOI 10.2113/0250217	36	18	19	0	1	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.	NOV	2003	109	3					499	516		10.13130/2039-4942/5519	http://dx.doi.org/10.13130/2039-4942/5519			18	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	761MP					2025-03-11	WOS:000187912800007
J	Salomon, PS; Janson, S; Granéli, E				Salomon, PS; Janson, S; Granéli, E			Parasitism of <i>Dinophysis norvegica</i> by <i>Amoebophrya</i> sp in the Baltic sea	AQUATIC MICROBIAL ECOLOGY			English	Article						phytoplankton; interspecific interactions; parasitism; Dinoflagellates; Amoebophrya; Dinciphysis norvegica; Baltic sea	DINOFLAGELLATE AKASHIWO-SANGUINEA; CHESAPEAKE BAY; GYMNODINIUM-SANGUINEUM; HOST-SPECIFICITY; GENERATION TIME; CERATII; INFECTION; STRAINS	The temporal and vertical distribution of the infection of the dinoflagellate Dinophysis norvegica by the endoparasite Amoebophrya sp. was investigated at a fixed sampling location in the Baltic Sea during 2000 and 2001. Infected hosts were detected by epifluorescence microscopy after DAPI staining. The maximum depth-averaged parasite prevalence was 2.3 % in July 2000 and 1.8 % in August 2001. The percentage of infected hosts was usually higher close to the thermocline than at the surface. The highest parasite prevalence at a specific depth (4.8 %) was found at 20 m in August 2001. No correlation was observed between parasite prevalence and host abundance or dissolved nutrient (N and P) concentrations, neither for depth-averaged nor discrete depth measurements. However, temperature seemed to be an important factor influencing infection of D. norvegica by Amoebophrya sp., with infected host cells observed only above 12degreesC. Amoebophrya sp. was only sporadically observed inside other dinoflagellate species, indicating specificity towards D. norvegica. The seasonal pattern of infection suggests the existence of a dormancy stage of the parasite dinospores. The low prevalence observed during this study indicates that parasitism by Amoebophrya sp. is not a relevant loss factor for D. norvegica in the Baltic Sea.	Univ Kalmar, Dept Biol & Environm Sci, S-39182 Kalmar, Sweden	University of Kalmar; Linnaeus University	Salomon, PS (通讯作者)，Univ Kalmar, Dept Biol & Environm Sci, Landgangen 3, S-39182 Kalmar, Sweden.		Graneli, Edna/F-5936-2015; Salomon, Paulo/D-3310-2011					Cachon J., 1964, Annales des Sciences Naturelles (12), V6, P1; Cachon J., 1969, Protistologica, V5, P535; Cachon J., 1987, The Biology of Dinoflagellates, P571; CARPENTER EJ, 1995, EUR J PHYCOL, V30, P1, DOI 10.1080/09670269500650751; Coats DW, 1999, J EUKARYOT MICROBIOL, V46, P402, DOI 10.1111/j.1550-7408.1999.tb04620.x; Coats DW, 2002, J PHYCOL, V38, P520, DOI 10.1046/j.1529-8817.2002.t01-1-01200.x; COATS DW, 1994, J EUKARYOT MICROBIOL, V41, P586, DOI 10.1111/j.1550-7408.1994.tb01520.x; Coats DW, 1996, AQUAT MICROB ECOL, V11, P1, DOI 10.3354/ame011001; Combes C, 2001, Parasitism: the ecology and evolution of intimate interactions; DREBES G, 1984, HELGOLANDER MEERESUN, V37, P603; FRITZ L, 1992, J PHYCOL, V28, P312, DOI 10.1111/j.0022-3646.1992.00312.x; Gisselson Lars-Ake, 2002, Harmful Algae, V1, P401, DOI 10.1016/S1568-9883(02)00050-1; Gunderson JH, 2002, J EUKARYOT MICROBIOL, V49, P469, DOI 10.1111/j.1550-7408.2002.tb00230.x; Gunderson JH, 2001, J EUKARYOT MICROBIOL, V48, P670, DOI 10.1111/j.1550-7408.2001.tb00207.x; Janson S, 2000, PARASITOL RES, V86, P929, DOI 10.1007/s004360000272; Johansson M, 2002, AQUAT MICROB ECOL, V28, P69, DOI 10.3354/ame028069; Maranda L, 2001, J PHYCOL, V37, P245, DOI 10.1046/j.1529-8817.2001.037002245.x; Nishitani L., 1985, P225; TAYLOR FJR, 1968, J FISH RES BOARD CAN, V25, P2241, DOI 10.1139/f68-197; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Valderama J. C., 1995, IOC Manuals and Guides, V33, P251; van Donk E., 1989, P171; VANDONK E, 1983, FRESHWATER BIOL, V13, P241; WAKEMAN JS, 1982, J SHELLFISH RES, V2, P122; Yih W, 2000, J EUKARYOT MICROBIOL, V47, P504, DOI 10.1111/j.1550-7408.2000.tb00082.x	25	31	32	0	11	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055			AQUAT MICROB ECOL	Aquat. Microb. Ecol.	OCT 14	2003	33	2					163	172		10.3354/ame033163	http://dx.doi.org/10.3354/ame033163			10	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	738VK		Bronze			2025-03-11	WOS:000186308400006
J	Wilmsen, M				Wilmsen, M			Sequence stratigraphy and palaeoceanography of the Cenomanian Stage in northern Germany	CRETACEOUS RESEARCH			English	Review						Cretaceous; Cenomanian; sequence stratigraphy; nearshore-to-outer shelf; high-frequency cycles; bioevents; graphic correlation; palaeoceanograph	CALCAREOUS DINOFLAGELLATE CYSTS; SEA-LEVEL; PARIS BASIN; PALAEOCEANOGRAPHIC EVENTS; NORTHWEST EUROPE; WESTERN INDIA; LOWER SAXONY; CARBON FLUX; SHELL BEDS; TIME-SCALE	The sequence stratigraphic and sedimentologic analysis of a 180-km nearshore (SSE) to outer shelf (NNW) transect shows the pulsatory nature of the 'Cenomanian transgression' in northern Germany. Five complete and the lower part of a sixth third-order depositional sequence can be recognized: DS Ce I and DS Ce II (Mantelliceras mantelli Zone); DS Cc III (Mantelliceras dixoni Zone); DS Ce IV (Cunningtoniceras inerme to lower Acanthoceras jukesbrownei Zone); DS Ce V [Acanthoceras jukesbrownei Zone to Calycoceras (P.) guerangeri Zone]; DS Cc VI (Metoicoceras geslinianum Zone to lower Turonian). In inner and mid-shelf settings, sequence boundaries are mostly represented by stratigraphic gaps. A major sea-level fall occurred at the Early/Middle Cenomanian transition (sequence boundary SB Ce III). Maximum transgression during the Cenomanian is indicated by the deposition of homogeneous pelagic sediments of the 'Poor rhotomagense Limestones' (Late Cenomanian sequence DS Cc V). Graphic correlation of the sections investigated with a composite standard suggests that the inner and middle shelf sections were strongly controlled by available accommodation space during the Early and Middle Cenomanian. From the late Middle Cenomanian, non-accommodation controlled deposition of the 'Poor rhotomagense Limestones' occurred across the whole of the transect. Apart from the third-order depositional sequences. a hierarchy of stacked higher frequency (fourth- to sixth-order) cycles can be recognized. The basal elements are sixth-order cycles, represented by dm- to metre-scale marl-limestone 'precession couplets'. Fifth-order cycles are represented by bundles of four to six couplets separated by dark marker marls, inferred to record the ca. 100 ky short eccentricity cycle. Fourth-order cycles are sets of four (three to five) fifth-order cycles. Their boundaries are significant erosion surfaces associated with subordinate sea-level fall, occasionally coinciding with third-order sequence boundaries. Most of the 'classic' Cenomanian bioevents can be accommodated into the sequence stratigraphic framework. Three main types of bioevents are recognized: 'onlapping bioevents' at the transgressive surface or in the early transgressive systems tract, 'maximum flooding bioevents', and 'late highstand bioevents'. Onlapping and late highstand bioevents developed mainly either in response to sedimentologic and taphonomic processes such as winnowing and condensation, or owing to faunal migration during transgression. Maximum flooding bioevents are related to blooms of specialist taxa adapted to low food supplies and low-energy conditions. Two contrasting sedimentary systems can be recognized based on the nature of the dominant planktic carbonate component: an Early to early Middle Cenomanian 'calcisphere system' ('Planer'), characterized by high CaCO3 accumulation rates (up to 80 m/my), a relatively high input of terrigenous material, and dense macroinvertebrate faunal communities; and a late Middle and Late Cenomanian 'coccolith system' ('Poor rhotomagense Limestones'), characterized by low CaCO3 accumulation rates (13-18 m/my), low terrigenous input, and impoverished benthic communities. The 'calcisphere system' is interpreted to reflect eu-/mesotrophic middle shelf 'green' water masses with high primary productivity and high food supplies supporting a rich suspension- and deposit-feeding benthos. The 'Poor rhotomagense Limestones' document deposition from a low-productivity, oligotrophic outer shelf water mass (oceanic 'blue water'). The change between the two systems was caused by the Middle Cenomanian transgression, associated with the breakdown of shelf-front systems and the onlap of stratified, 'oceanic' water masses. The strongly reduced surface water productivity of the oligotrophic 'coccolith system' resulted in the disappearance of dense benthic communities during the late Middle and Late Cenomanian. (C) 2003 Elsevier Ltd. All rights reserved.	Univ Wurzburg, Inst Paleontol, D-97070 Wurzburg, Germany	University of Wurzburg	Wilmsen, M (通讯作者)，Univ Wurzburg, Inst Paleontol, Pleicherwall 1, D-97070 Wurzburg, Germany.	m.wilmsen@mail.uni-wuerzburg.de						AIGNER T., 1982, SENCKENB MARIT, V14, P183; Altenbach AV, 2001, J FORAMIN RES, V31, P79, DOI 10.2113/0310079; [Anonymous], 1995, TERRA NOSTRA; [Anonymous], 1984, SCHRIFTENREIHE ERDWI; [Anonymous], LECT NOTES EARTH SCI; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; [Anonymous], Q J GEOL SOC LOND; Badaye H, 1986, THESIS FREIE U BERLI; Baldschuhn R., 1991, EUROPEAN ASS PETROLE, V1, P149; BANERJEE I, 1991, SEDIMENTOLOGY, V38, P913, DOI 10.1111/j.1365-3091.1991.tb01879.x; BERGER A, 1989, NATURE, V342, P133, DOI 10.1038/342133b0; Biju-DuvAl B., 2000, ATLAS PERI TETHYS PA; BLAKE JA, 1994, DEEP-SEA RES PT II, V41, P875, DOI 10.1016/0967-0645(94)90052-3; Bower C. 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J	Tongiorgi, M; Yin, LM; Di Milia, A				Tongiorgi, M; Yin, LM; Di Milia, A			Lower Yushanian to lower Zhejiangian palynology of the Yangtze Gorges area (Daping and Huanghuachang sections), Hubei Province, South China	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			English	Review						acritarchs; systematics; biostratigraphy; biofacies; sea-level; arenig; South China	EARLY ORDOVICIAN SEDIMENTS; ACRITARCH ASSEMBLAGES; ARENIGIAN ACRITARCHS; MIDDLE; NORTH; STRATIGRAPHY; TECTONICS; SERIES; OLAND; PALYNOSTRATIGRAPHY	The Lower to Middle Ordovician Dawan Formation and the base of the overlying Guniutan Formation have been sampled for palynomorphs at Daping (Yichang area, South China) with the aim to discuss the environmental history of the lower Yushanian to lower Zhejiangian Stages (Arenig) from South China. Two samples from the Huanghuachang section (the same area) were also examined for comparison. Fifty-three samples from Daping proved to be palyniferous, while 17 of 70 were barren or nearly so. The resultant taxonomic database comprises 129 acritarch taxa, belonging to 41 genera and two species of prasinophycean algae. The morphology and the systematic status of most taxa are discussed in detail and their geographic and stratigraphic distribution are documented. Two new acritarch species (Dasydorus microcephalus, and Tenuirica? gradata) and four new varieties [Cymatiogalea granulata VAVRDOVA 1966 var. changjiangensis, Pacbyspbaeridium rhabdocladium (Lu 1987 emend. TONGIORGI et al. 1995) RIBECAI et TONGIORGI 1999 var. striatellum, Petemospbaeridium dissimile GORKA 1969 var. contractum, and Stelliferidium striatulum (VAVRDOVA 1966) emend. DEUNFF et al. 1974 var. radiatum] are instituted; Stelomorpha crassula (VARDOVA 1990b) is proposed as a new combination. A compositional analysis of samples from Daping, embracing the middle Oepikodus evae through the lower Lenodus variabilis conodont zonal interval, is based on relative percentages of acritarchs belonging to nine morphological classes (Veryhachid-, Diacromorph-, Sphaeromorph-, Micrhystrid-, Polygonid-, Peteinosphaerid-, Baltisphaerid-, Galeata, and Others). SIMPSON'S (unbiased) Dominance Index is then extrapolated from 45 of the more productive samples of the Dawan Formation. To understand the compositional fluctuations through the Daping section, an interpretative model is elaborated, by analogy with WALL et al.'s (1977) study of the distribution of dinoflagellate cysts in the sediments of modern seas, integrated with reported correlations between trophic levels and phytoplankton diversity. According to the integrated model, two principal concurrent ecological trends influence the distribution of phytoplankton diversity; the first lies in the inshore to offshore transect, while the second corresponds to a climatic (temperature) variation through time. The model predicts that phytoplankton diversity increases (and dominance decreases) from mesotrophic-eutrophic, cold (regressive), proximal habitats, towards warmer (transgressive), distal, oligotrophic environments. With this approach, a large dominance peak situated in the upper Paroistodus originalis conodont Zone is considered indicative of an important regression separating Middle and Upper Members of the Dawan Formation. The multivariate Correspondence Analysis proved very useful to investigate the acritarch biofacies, which characterize the various habitats on the platform during both regressive and transgressive events. This analysis enables identification of four main biofacies, each referable to a particular environment, as follows: Biofacies I (Galeata Biofacies), from cool waters of eutrophic, upwelling influenced, coastal habitats; Biofacies II (Baltisphaerid-Petemosphaerid Biofacies), from temperate waters of inshore, mesotrophic habitats; Biofacies III (Veryhachid-Diacromorph-Polygonid Blofacies) from temperate waters of offshore, moderately to highly oligotrophic environments; and, Biofacies IV (Barakella, Picostella, Striatotbeca Biofacies), from temperate, oceanic, highly oligotrophic habitats. Biofacies I corresponds to regression, while Blofacies II-IV correspond to a range of environments during transgressive episodes. Although acritarch biofacies are conceptually unrelated to inferred palaeogeographic settings, the more distal habitats (Biofacies III and IV), influenced by oceanic waters, would be expected to show more "Mediterranean" than "Baltic" acritarch characteristics. Conversely, "Baltic" attributes would be embodied by acritarch assemblages from proximal or internal situations (Biofacies II), having more restricted circulation of warmer inshore or estuarine waters. Consequently, the more substantial transgressions could be signalled by the occurrence of "Mediterranean"-type assemblages, while the essentially unaffected, more internal contemporaneous habitats could retain "Baltic" attributes. A more reliable indicator of sea-level fluctuation is the Diversity Index. The acritarch diversity curve measured at Daping can be correlated with the global sea-level curve reported for the Arenig, as follows: a) a large transgressive peak extends from the topmost Oepikodus evae to the entire Baltoniodus? triangularis-B. navis Zone, b) a negative trend comprises the lower two-thirds of the R originalis Zone, c) a transgressive tendency covers the upper third of the P originalis Zone and the lower Microzarkodina parva-Baltoniodus norrlandicus Zone, with a maximum in the upper part of the latter, followed by d) a short-term regressive trend, with a minimum in the middle Lenodus antivariabilis Zone, and by e) an apparent further positive trend in the upper L. antivariabilis Zone. The evolutionary consequences of these events are discussed, taking into account the importance of the different biofacies for the adaptative changes of the phytoplankton across repeated extinction (regressive) events. Abandonment of the current "palaeophytogeogeographic" terminology ("Mediterranean Province", "Baltic Province") is proposed, in favour of different terms ("Mediterranean palynoflora", "Baltic palynoflora") that are more closely related to both the environmental/ecological factors and the evolutionary adaptations of the phytoplankton in response to such factors.	Univ Pisa, Dipartimento Sci Terra, I-56126 Pisa, Italy; Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China	University of Pisa; Chinese Academy of Sciences	Univ Pisa, Dipartimento Sci Terra, Via S Maria 53, I-56126 Pisa, Italy.							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Abt. B-Palaophytol.	OCT	2003	266	1-6					1	U78						235	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	753HV					2025-03-11	WOS:000187226700001
J	Slimani, H				Slimani, H			A new genus and two new species of dinoflagellate cysts from the Upper Cretaceous of the Maastrichtian type area and Turnhout (northern Belgium)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Campanian-Maastrichtian; Maastricht area; northern Belgium	NETHERLANDS	Campanian and Maastrichtian chalks from Beutenaken and Hallembaye quarries in the Maastrichtian type area and from the Turnhout borehole in northern Belgium contain two new dinoflagellate cysts, Batiacasphaera solida, Slimani sp. nov. and Neosphaerodictyon filosum, Slimani gen. et sp. nov. Batiacasphaera solida is coarsely granulate to tuberculate. The type of the new genus Neosphaerodictyon is a chorate gonyaulacoid, bearing 1 filamentous process per plate and with an apical archeopyle (tA) and characteristic reticulate periphragm. Both have distinctive morphologies and restricted occurrences in the Campanian (B. solida) and in the Campanian and Early Maastrichtian (M filosum) stages.. and are therefore considered to be potential stratigraphical markers. (C) 2003 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, POB 703,Ave Ibn Batouta, Rabat, Morocco.		Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913				[Anonymous], P 2 PLANKT C ROM 197; [Anonymous], MEMOIRS; ANTONESCU E, 2001, IUGS SPECIAL PUBLICA, V19, P235; Brinkhuis H, 2000, REV PALAEOBOT PALYNO, V110, P93, DOI 10.1016/S0034-6667(99)00062-7; COOKSON I.C., 1974, PALAEONTOGRAPHICA, V148, P44; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; Davey R.J., 1979, Palynology, V3, P209; DAVEY R J, 1969, Palaeontologia Africana, V12, P1; Davey R. J., 1966, STUDIES MEZOZOIC C S, V3, P53; DAVEY RJ, 1969, B BRIT MUS NAT HIST, V17, P1; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DODEKOVA L, 1974, BULG ACAD NAUKITE IZ, V23, P25; DRUGG WS, 1970, P N AM PAL CONV, V2, P809; EISENACK A., 1963, NEUES JB F R GEOLOGI, V118, P260; Eisenack A, 1963, NEUES JB GEOLOGIE PA, V2, P98; Felder W.M., 1975, Publicaties van het Natuurhistorisch Genootschap in Limburg, V24, P1; Fensome R.A., 1993, Micropaleontology Press Special Paper; Foucher J.-C., 1983, 7 S ASS PAL LANG FRA; FOUCHER JC, 1985, CAMPANIAN MAASTRICHT, V9, P32; GULINCK M, 1954, B SOC BELG GEOL, V68, P147; HABIB D, 1989, PALAEOGEOGR PALAEOCL, V74, P23, DOI 10.1016/0031-0182(89)90018-7; HOFKER J, 1966, PALAEONTOGR S, V10; JANSONIUS J, 1989, REV PALAEOBOT PALYNO, V61, P63, DOI 10.1016/0034-6667(89)90062-6; Keutgen N., 1990, MEDEDELINGEN RIJKS G, V44, P1; KEUTGEN N, 1998, 287 GEOL SURV BELG; KEUTGEN N, 1996, THESIS RHEINISH WEST; KEUTGEN N, 1995, 2 INT S CRET STAG BO, P176; Klumpp B., 1953, Palaeontographica A, V103, P377; LOUWYE S, 1991, THESIS RIJKSUNIVERSI; Louwye Stephen, 1993, Bulletin de la Societe Belge de Geologie, V101, P255; Mohr B. A. R., 1997, Palynology, V21, P41; Robaszynski F., 1985, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V9, P1; Sarjeant WAS., 1962, PALAEONTOLOGY, V5, P478; Schioler P, 1997, MAR MICROPALEONTOL, V31, P65, DOI 10.1016/S0377-8398(96)00058-8; Schmid F., 1959, Annales de la Societe Geologique de Belgique Bull, V82, P235; Schulz M.-G, 1983, ZITTELIANA, V10, P653; Schumacker-Lambry J., 1977, MACRO MICROFOSSILES, P45; SLIMANI H, 2000, NOUVELLE ZONATION KY, V46; Slimani H, 1995, THESIS RIJKSUNIVERSI; Slimani Hamid, 2001, Geologica et Palaeontologica, V35, P161; VERBEEK JW, 1983, B GEOL SOC DEN, V33, P197; WILLIAMS GL, 1998, AASP CONTRIBUTION SE, V34; Wilson G.J., 1971, MERCIAN GEOL, V4, P29; Wilson GJ., 1974, THESIS U NOTTINGHAM; WILSON GRAEME J., 1967, N Z J BOT, V5, P223	46	8	8	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	OCT	2003	126	3-4					267	277		10.1016/S0034-6667(03)00091-5	http://dx.doi.org/10.1016/S0034-6667(03)00091-5			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	733VG					2025-03-11	WOS:000186020900008
J	Guler, MV				Guler, MV			Neogene Protoperidiniaceae dinoflagellate cysts from the Colorado Basin, Argentina	AMEGHINIANA			Spanish	Article						Protoperidiniaceae; systematics; neogene; Colorado Basin	SEDIMENTS; BIOSTRATIGRAPHY; NORTH; BOREHOLE; PROVINCE; NORFOLK; OCEAN	NEOGENE PROTOPERIDINIACEA DINOFLAGELLATE CYSTS FROM THE COLORADO BASIN, ARGENTINA. Protoperidiniacean dinoflagellate cysts assemblages caracterize two middle Miocene - lower Pliocene outcropping sections from Colorado Basin. Twelve protoperidinioid cyst species and one species of the diplopsalioid genera Dubridinium Reid are described. Selenopemphix brevispinosa subsp. brevispinosa Head is documented for the first time from Argentina and Dubridinium sp. is described and illustrated for the first time from pre-Pleistocene deposits.	Univ Nacl Sur, CONICET, Dept Geol, 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)	Univ Nacl Sur, CONICET, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	vguler@criba.edu.ar						[Anonymous], 1976, BEDFORD I OCEANOGRAP; [Anonymous], 1980, 2 S GEOL REG ARG; [Anonymous], NEOGENE QUATERNARY D; Aramayo S. 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L., 1998, AM ASS STRATIGRAPHIC, V34; WILLIAMS GL, 1998, SOC SEDIMENTARY GEOL, V60, P9; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Zavala C., 2000, Geotemas, V1, P217; ZAVALA C, 2000, 2 C LAT SED RES, P186; ZINSMEISTER WJ, 1981, SCIENCE, V212, P440, DOI 10.1126/science.212.4493.440; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1	60	6	6	0	2	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014	1851-8044		AMEGHINIANA	Ameghiniana	SEP 30	2003	40	3					457	467						11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	746MN					2025-03-11	WOS:000186750300016
J	Yagishita, K; Obuse, K; Kurita, H				Yagishita, K; Obuse, K; Kurita, H			Lithology and palynology of Neogene sediments on the narrow edge of the Kitakami Massif (basement rocks), northeast Japan: Significant change for depositional environments as a result of plate tectonics	ISLAND ARC			English	Article						allochthonous lignites; boulders; continental Paleogene Pacific Coast; dinoflagellate cysts; island arc; Neogene fluvial (flood) deposits; pollen assemblages	RIVER; SANDSTONE; EVOLUTION; FACIES	A controversial stratigraphic section, the Taneichi Formation, is exposed along the Pacific Coast of northeastern Honshu, the main island of the Japanese Archipelago. Although most sediments of the formation have long been dated as late Cretaceous, the northern section of it has been assigned to (i) the Upper Cretaceous; (ii) the Paleogene; or (iii) the Neogene. In the present report, we present the data of palynological and sedimentological studies, showing that the northern section should be assigned to the Neogene. A more important point in the present study is that we invoke some basic principles of fluvial sedimentology to resolve this stratigraphic subject. The lignite layers full of Paleogene-Miocene dinoflagellate cysts and pollen assemblages drape over the boulder-sized (>40 cm in diameter) clasts in the northern section. However, the layers totally consist of aggregates of small lignite chips, indicating that the lignites are allochthonous materials. The mega-clasts with derived microfossils in the lignites are thought to have been deposited as Neogene fluvial (flood) sediments in the newly formed Japanese Archipelago. Prior to the Miocene, the northern Honshu was part of the Eurasian Plate, thus the boulder-sized clasts cannot be envisaged as long river flood deposits along the continental Paleogene Pacific Coast. Instead, the mega-clasts with the draping lignites were probably derived from nearby Miocene highlands in the newly born island arc.	Iwate Univ, Fac Educ, Dept Geol, Morioka, Iwate 0208550, Japan; Japan Petr Explorat Co Ltd, JAPEX Res Ctr, Mihama Ku, Chiba 2610025, Japan; Niigata Univ, Fac Sci, Dept Geol Sci, Niigata 9502181, Japan	Iwate University; Niigata University	Yagishita, K (通讯作者)，Iwate Univ, Fac Educ, Dept Geol, Morioka, Iwate 0208550, Japan.		Kurita, Hiroshi/KIC-0968-2024					[Anonymous], MEM GEOL SOC JAPAN; [Anonymous], 2007, Paleopalynology; BARWIS JH, 1985, J SEDIMENT PETROL, V55, P907; CANT D.J., 1978, FLUVIAL SEDIMENTOLOG, P627; CANT DJ, 1978, SEDIMENTOLOGY, V25, P625, DOI 10.1111/j.1365-3091.1978.tb00323.x; Costa J.E., 1974, GEOLOGY, V2, P301, DOI DOI 10.1130/0091-7613(1974)2<301:SMAPEO>2.0.CO;2; COTTER E, 1975, J SEDIMENT PETROL, V45, P669; DEERY JR, 1977, T GULF COAST ASS GEO, V27, P259; DICKINSON WR, 1979, AAPG BULL, V63, P2164; Futakami M., 1987, B IWATE PREFECTURAL, V5, P103; GRAHAM SA, 1976, J SEDIMENT PETROL, V46, P620; HEIN FJ, 1977, CAN J EARTH SCI, V14, P562, DOI 10.1139/e77-058; Kanisawa S., 1988, Earth Science (Chikyu Kagaku), V42, P220; KODAMA Y, 1994, J SEDIMENT RES A, V64, P68; MATSUMOTO T, 1985, P JPN ACAD B-PHYS, V61, P106, DOI 10.2183/pjab.61.106; MATSUMOTO T, 1986, B IWATE PREFECTURAL, V4, P17; McCabe P.J., 1984, SEDIMENTOLOGY COAL C, P13; MIALL AD, 1977, EARTH-SCI REV, V13, P1, DOI 10.1016/0012-8252(77)90055-1; MIKI A, 1977, Journal of the Faculty of Science Hokkaido University Series IV Geology and Mineralogy, V17, P399; Mori K., 1992, 29 IGC FIELD TRIP GU, V1, P81; Nadon GC, 1998, GEOLOGY, V26, P727, DOI 10.1130/0091-7613(1998)026<0727:MATOPT>2.3.CO;2; OBUSE A, 1996, 103 ANN M GEOL SOC J, P105; OTOFUJI Y, 1985, EARTH PLANET SC LETT, V75, P265, DOI 10.1016/0012-821X(85)90108-6; Pettijohn F.J., 1975, SEDIMENTARY ROCKS, V3rd; Powell A.J., 1992, STRATIGRAPHIC INDEX; Rodriguez AB, 2000, J SEDIMENT RES, V70, P283, DOI 10.1306/2DC40911-0E47-11D7-8643000102C1865D; SAITO Y, 1982, J GEOPHYS RES, V87, P3691, DOI 10.1029/JB087iB05p03691; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; SUGIYAMA R, 1987, REG M GEOL SOC JAP T, V18, P5; Takahashi K., 1990, Bulletin of the Faculty of Liberal Arts, Nagasaki University, Natural Science, V30, P133; Terui K., 1975, Journal geol Soc Japan, V81, P783; VANWAGONER JC, 1990, AAPG METHODS EXPLORA, V7, P8; Williams G.L., 1993, Geol. Surv. Can. Pap.; Yagishita K, 1997, SEDIMENT GEOL, V109, P53, DOI 10.1016/S0037-0738(96)00058-9; YAGISHITA K, 1994, SEDIMENT GEOL, V93, P155, DOI 10.1016/0037-0738(94)90002-7; YAGISHITA K, 1997, MEMOIRS GEOLOGICAL S, V48, P76	36	3	3	0	2	BLACKWELL PUBLISHING ASIA	CARLTON	54 UNIVERSITY ST, P O BOX 378, CARLTON, VICTORIA 3053, AUSTRALIA	1038-4871			ISL ARC	Isl. Arc.	SEP	2003	12	3					268	280		10.1046/j.1440-1738.2003.00399.x	http://dx.doi.org/10.1046/j.1440-1738.2003.00399.x			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	717HK					2025-03-11	WOS:000185081700003
J	Mcgillicuddy, DJ; Signell, RP; Stock, CA; Keafer, BA; Keller, MD; Hetland, RD; Anderson, DM				Mcgillicuddy, DJ; Signell, RP; Stock, CA; Keafer, BA; Keller, MD; Hetland, RD; Anderson, DM			A mechanism for offshore initiation of harmful algal blooms in the coastal Gulf of Maine	JOURNAL OF PLANKTON RESEARCH			English	Article							RED-TIDE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; RESTING CYSTS; SHELLFISH TOXICITY; FLUX MEASUREMENTS; CHESAPEAKE BAY; ALEXANDRIUM; SEDIMENTS; ESTUARINE; EXCAVATA	A combination of observations and model results suggest a mechanism by which coastal blooms of the toxic dinoflagellate Alexandrium fundyense can be initiated from dormant cysts located in offshore sediments. The mechanism arises from the joint effects of organism behavior and the wind-driven response of a surface-trapped plume of fresh water originating from riverine sources. During upwelling-favorable winds, the plume thins vertically and extends offshore; downwelling winds thicken the plume and confine it to the nearshore region. In the western Gulf of Maine, the offshore extent of the river plume during upwelling conditions is sufficient to entrain upward-swimming A. fundyense cells germinated from offshore cyst beds. Subsequent downwelling conditions then transport those populations towards the coast.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; US Geol Survey, Woods Hole, MA 02543 USA; Bigelow Lab Ocean Sci, W Boothbay Harbor, ME 04575 USA; Texas A&M Univ, College Stn, TX 77843 USA	Woods Hole Oceanographic Institution; United States Department of the Interior; United States Geological Survey; Bigelow Laboratory for Ocean Sciences; Texas A&M University System; Texas A&M University College Station	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	dmcgillicuddy@whoi.edu	anderson, david/E-6416-2011; Stock, Charles/H-1281-2012; Hetland, Robert/E-2614-2012	Stock, Charles/0000-0001-9549-8013; McGillicuddy, Dennis/0000-0002-1437-2425; Signell, Richard/0000-0003-0682-9613; Hetland, Robert/0000-0001-9531-2119				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, 1984, ACS SYM SER, V262, P125; 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, 1993, J PLANKTON RES, V15, P563, DOI 10.1093/plankt/15.5.563; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; ANDERSON DM, 2000, ALEXANDRIUM BLOOMS W; ANDERSON DM, 1995, MANUAL HARMFUL MARIN, P229; [Anonymous], 1996, PATTERNS OCEAN OCEAN; Blumberg AF., 1987, A description of a three-dimensional coastal ocean circulation model, V4, P1, DOI [DOI 10.1029/CO004P0001, 10.1029/co004p0001]; BRIN KH, 1998, SEA, V10; CRAIB J. 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Plankton Res.	SEP	2003	25	9					1131	1138		10.1093/plankt/25.9.1131	http://dx.doi.org/10.1093/plankt/25.9.1131			8	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	718LX		Bronze			2025-03-11	WOS:000185148600010
J	Parrow, MW; Burkholder, JM				Parrow, MW; Burkholder, JM			Estuarine heterotrophic cryptoperidiniopsoids (Dinophyceae): Life cycle and culture studies	JOURNAL OF PHYCOLOGY			English	Review						cell cycle; dinoflagellates; flow cytometry; heterotrophy; meiosis; mixotrophy; nuclear cyclosis; phagotrophy; planozygote; reproduction	PFIESTERIA-PISCICIDA DINOPHYCEAE; RED TIDE DINOFLAGELLATE; RELATIVE PLOIDY LEVELS; COMPLEX CELL-CYCLE; CRYPTHECODINIUM-COHNII; MARINE DINOFLAGELLATE; FLOW-CYTOMETRY; AMYLOODINIUM-OCELLATUM; GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE	Cryptoperidiniopsoids are an unclassified group of delicately thecate heterotrophic dinoflagellates known to be common in eastern U.S. estuarine waters. Over the past 10 years cryptoperidiniopsoids were isolated from different geographical regions and cultured with cryptophyte algal prey. In the seven clonal isolates examined, reproduction was strongly linked to the availability of prey cells. The dinoflagellates phagocytized the contents of prey cells through a tube-like peduncle, similarly as close relatives of Pfiesteria spp. and several other heterotrophic species. Cell division occurred while encysted, most commonly yielding two biflagellated offspring. Abundant fusing gametes, phagotrophic planozygotes, and cysts with a pronounced nuclear cyclosis characterized persistent sexuality. Cysts with nuclear cyclosis produced two flagellated offspring cells. The resistance of reproductive cysts to antimicrobial treatments was examined, and a simple high-yield technique was developed for population synchronization while ridding the dinoflagellates of most contaminating vacuolar prey DNA and external contaminants. The DNA content and population DNA profiles of synchronously excysted cryptoperidiniopsoids from different isolates were measured using flow cytometry and were related to the life history of these and other dinoflagellates. Cryptophyte-fed cultures with versus without extracellular bacteria were compared, and bacteria apparently promoted cryptoperidiniopsoid feeding and growth. Externally bacteria-free dinoflagellates were cultured in media enriched with dissolved organic nutrients, and nutritional benefit may have occurred in some treatments. The potential for mixotrophic nutrition from maintenance of cryptophyte chloroplasts was examined using flow cytometrically sorted cells, but evidence of kleptoplastidy was not found in these isolates under the conditions imposed.	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				Alavi M, 2001, ENVIRON MICROBIOL, V3, P380, DOI 10.1046/j.1462-2920.2001.00207.x; ALLEN RD, 1983, J MICROSC-OXFORD, V129, P3, DOI 10.1111/j.1365-2818.1983.tb04157.x; ANDERSON DM, 1995, MANUAL HARMFUL MARIN, P229; Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; Azanza MPV, 2001, LETT APPL MICROBIOL, V33, P371, DOI 10.1046/j.1472-765X.2001.01013.x; BAGWELL CB, 1989, CYTOMETRY, V10, P689; BARKER H. ALBERT, 1935, ARCH MIKROBIOL, V6, P157, DOI 10.1007/BF00407285; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C.A., 1984, P263; Beam C. 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Phycol.	AUG	2003	39	4					678	696		10.1046/j.1529-8817.2003.02146.x	http://dx.doi.org/10.1046/j.1529-8817.2003.02146.x			19	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	706JT					2025-03-11	WOS:000184451100007
J	Parrow, MW; Burkholder, JM				Parrow, MW; Burkholder, JM			Reproduction and sexuality in <i>Pfiesteria shumwayae</i> (Dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						chromosomes; dinoflagellate; meiosis; meiotic prophase; mitosis; nuclear cyclosis; palintomy; phagotrophy; sexual reproduction	DINOFLAGELLATE GYMNODINIUM-CATENATUM; RED-TIDE DINOFLAGELLATE; ALEXANDRIUM-TAYLORI DINOPHYCEAE; LIFE-CYCLE; TOXIC DINOFLAGELLATE; PISCICIDA; HISTORY; COMPLEX; CHROMOSOME; BEHAVIOR	Pfiesteria shumwayae is a heterotrophic dinoflagellate with a widespread distribution in temperate-subtropical estuarine waters. In this study, five clonal isolates from the eastern coast of North America, one from New Zealand, and a mixed composite of clones were cultured in aquaria and fed live fish. Division, sexuality, and phagotrophic feeding on fish were studied by LM, SEM, and flow cytometry. The development of reproductive cysts isolated from aquaria was followed. Synchronously excysted flagellate populations were examined for sexuality and then for feeding behavior and reproduction when given larval fish. Reproductive cysts varied in size and underwent protoplast division(s), most commonly producing two to eight biflagellated offspring. Fusing gametes, resulting planozygotes, and nuclear cyclosis were documented as evidence of sexuality. Gametes emerged from cysts, and fusions were approximately isogamous. Resulting planozygotes had two longitudinal flagella and one transverse flagellum and apparently fed before encysting. Distinct and lengthy chromosome movements (nuclear cyclosis) occurred in presumed zygotic cysts before nuclear division(s). These cysts did not exhibit dormancy in growing cultures and produced two or four biflagellated offspring. Flagellated cells fed on surficial fish tissues and then encysted for reproduction. Stages indicating a completed sexual cycle (fusion, planozygotes, and nuclear cyclosis) were uncommon or absent in clonal cultures but were relatively abundant in the mixed clone culture. Self-sterility factors apparently influenced sexuality. Starved populations formed quiescent cysts that released swimming cells when food was provided. Pfiesteria shumwayae was similar in reproduction and sexuality to closely related species.	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				ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1995, MANUAL HARMFUL MARIN, P229; BAGWELL CB, 1989, CYTOMETRY, V10, P689; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C.A., 1984, P263; Beam C. 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Phycol.	AUG	2003	39	4					697	711		10.1046/j.1529-8817.2003.03057.x	http://dx.doi.org/10.1046/j.1529-8817.2003.03057.x			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	706JT					2025-03-11	WOS:000184451100008
J	Bailey, SA; Duggan, IC; van Overdijk, CDA; Jenkins, PT; MacIsaac, HJ				Bailey, SA; Duggan, IC; van Overdijk, CDA; Jenkins, PT; MacIsaac, HJ			Viability of invertebrate diapausing eggs collected from residual ballast sediment	LIMNOLOGY AND OCEANOGRAPHY			English	Article							RESTING EGGS; GREAT-LAKES; DINOFLAGELLATE CYSTS; WATER; ZOOPLANKTON; DISPERSAL; INVASION; TRANSPORT; COMMUNITIES; TEMPERATURE	Natural or anthropogenic movement of sediments may be an important vector for the dispersal of invertebrate resting stages between water bodies. Here we record the presence of invertebrate diapausing eggs in residual sediments from transoceanic: vessels and explore whether these may pose an invasion risk. Viability of diapausing eggs was explored under light and dark conditions using sediment collected from eleven tanks on nine vessels operating on the Great Lakes. Seventeen cladoceran, copepod, and rotifer taxa were identified. Four of the species hatched have not yet been reported as established in the Great Lakes. Egg viability for individual species varied from 0% to 92%. Exposure to saline water may impact egg viability of some freshwater species. Generally, the proportion of eggs hatched in light and dark treatments did not differ significantly, indicating that light was not required to terminate diapause. As a result, eggs could potentially hatch in dark ballast tanks when immersed in freshwater loaded as ballast during operation on the Great Lakes. Viability of diapausing eggs differed among ballast tanks on a single vessel, indicating that tanks with independent ballast histories have different invasion risks. While additional work is needed to quantify risk, results from this study indicate that vessels entering the Great Lakes with only residual ballast are a potential vector for the introduction of new nonindigenous species during multiport operations.	Univ Windsor, Great Lakes Inst Environm Res, Windsor, ON N9B 3P4, Canada; Philip T Jenkins & Associates Ltd, Fonthill, ON LOS 1E1, Canada	University of Windsor	Univ Windsor, Great Lakes Inst Environm Res, Windsor, ON N9B 3P4, Canada.	sarahbailey@canada.com	macisaac, hugh/AAE-3742-2020; Duggan, Ian/G-2275-2012; Bailey, Sarah/E-8356-2010	Duggan, Ian/0000-0002-6037-9759; Bailey, Sarah/0000-0003-3635-919X				[Anonymous], BALL WAT MAN VESS EN; Bilton DT, 2001, ANNU REV ECOL SYST, V32, P159, DOI 10.1146/annurev.ecolsys.32.081501.114016; Burgess B, 2001, MAR ECOL PROG SER, V214, P161, DOI 10.3354/meps214161; Cáceres CE, 2002, OECOLOGIA, V131, P402, DOI 10.1007/s00442-002-0897-5; COLAUTTI RI, INVASION PATHWAYS AN; DESTASIO BT, 1989, ECOLOGY, V70, P1377; DODSON DI, 1991, ECOLOGY CLASSIFICATI, P723; Drake Lisa A., 2001, Biological Invasions, V3, P193, DOI 10.1023/A:1014561102724; DUMONT HJ, 1983, HYDROBIOLOGIA, V104, P19, DOI 10.1007/BF00045948; Edmondson W.T., 1966, Freshwater Biology, VSecond; Figuerola J, 2002, FRESHWATER BIOL, V47, P483, DOI 10.1046/j.1365-2427.2002.00829.x; Grice G.D., 1981, Oceanography and Marine Biology an Annual Review, V19, P125; HAIRSTON NG, 1995, ECOLOGY, V76, P1706, DOI 10.2307/1940704; Hairston NG, 1996, LIMNOL OCEANOGR, V41, P1087, DOI 10.4319/lo.1996.41.5.1087; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Hariston NG, 1999, LIMNOL OCEANOGR, V44, P477; Hebert P.D.N., 1995, DAPHNIA N AM ILLUSTR; HEBERT PDN, 1980, SCIENCE, V207, P1363, DOI 10.1126/science.207.4437.1363; HEBERT PDN, 1978, BIOL REV, V53, P387, DOI 10.1111/j.1469-185X.1978.tb00860.x; Hebert PDN, 2002, CAN J FISH AQUAT SCI, V59, P1229, DOI 10.1139/F02-091; Jenkins DG, 1998, ECOL MONOGR, V68, P421, DOI 10.1890/0012-9615(1998)068[0421:DSCDIS]2.0.CO;2; Jenkins DG, 1998, HYDROBIOLOGIA, V387, P15, DOI 10.1023/A:1017080029317; KELLY JM, 1993, J SHELLFISH RES, V12, P405; KOSTE W, 1989, Transactions of the Royal Society of South Australia, V113, P85; LOCKE A, 1993, CAN J FISH AQUAT SCI, V50, P2086, DOI 10.1139/f93-232; LUTZ RV, 1992, MAR BIOL, V114, P241, DOI 10.1007/BF00349525; MacIsaac HJ, 2002, CAN J FISH AQUAT SCI, V59, P1245, DOI 10.1139/F02-090; Madhupratap M, 1996, MAR BIOL, V125, P77, DOI 10.1007/BF00350762; Marcus NH, 1996, HYDROBIOLOGIA, V320, P141, DOI 10.1007/BF00016815; MAY L, 1987, HYDROBIOLOGIA, V147, P335, DOI 10.1007/BF00025763; MILLS EL, 1993, J GREAT LAKES RES, V19, P1, DOI 10.1016/S0380-1330(93)71197-1; Parker BR, 1996, CAN J ZOOL, V74, P1292, DOI 10.1139/z96-144; Ricciardi A, 2000, TRENDS ECOL EVOL, V15, P62, DOI 10.1016/S0169-5347(99)01745-0; Ricciardi A, 2001, CAN J FISH AQUAT SCI, V58, P2513, DOI 10.1139/cjfas-58-12-2513; Ruiz GM, 2000, ANNU REV ECOL SYST, V31, P481, DOI 10.1146/annurev.ecolsys.31.1.481; SCHWARTZ SS, 1987, FRESHWATER BIOL, V17, P373, DOI 10.1111/j.1365-2427.1987.tb01057.x; Shurin JB, 2000, ECOLOGY, V81, P3074, DOI 10.1890/0012-9658(2000)081[3074:DLIRAT]2.0.CO;2; Stemberger R.S., 1979, EPA600479021 ENV MON; STROSS RG, 1966, ECOLOGY, V47, P368, DOI 10.2307/1932977; VIITASALO M, 1994, MAR BIOL, V120, P455, DOI 10.1007/BF00680221; Wallace R.L., 1991, P187; WILLIAMS RJ, 1988, ESTUAR COAST SHELF S, V26, P409, DOI 10.1016/0272-7714(88)90021-2	44	88	97	0	19	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0024-3590	1939-5590		LIMNOL OCEANOGR	Limnol. Oceanogr.	JUL	2003	48	4					1701	1710		10.4319/lo.2003.48.4.1701	http://dx.doi.org/10.4319/lo.2003.48.4.1701			10	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	702WN		Green Submitted			2025-03-11	WOS:000184247900032
J	Hay, MB; Pienitz, R; Thomson, RE				Hay, MB; Pienitz, R; Thomson, RE			Distribution of diatom surface sediment assemblages within Effingham Inlet, a temperate fjord on the west coast of Vancouver Island (Canada)	MARINE MICROPALEONTOLOGY			English	Article						diatoms; fjords; principal component analysis; Vancouver Island; British Columbia	BRITISH-COLUMBIAN FJORDS; SAANICH INLET; PHYTOPLANKTON ECOLOGY; DINOFLAGELLATE CYSTS; LAMINATED SEDIMENTS; SECHELT-INLET; NORWAY; CLIMATE; OXYGEN; RECORD	Twenty-nine surface sediment samples from Effingham Inlet, a small fjord on the west coast of Vancouver Island, British Columbia, were analyzed for diatoms. This fjord has been selected for paleoceanographic investigation due to the presence of laminated sediments resulting from the dysoxic to anoxic bottom water conditions in the inner and outer basins of the inlet. Distributional patterns of the diatom microflora reflected proximity to littoral regions, phytoplankton production, and marine influence from outside the fjord. Principal components and cluster analyses of the microflora established four diatom assemblages with a clear separation between the inner and outer basin diatom floras. Inner basin stations were characterized by elevated absolute abundance with assemblages dominated by spring-early summer bloom taxa including Skeletonema costatum, Thalassiosira nordenskioeldii, and Thalassiosira pacifica. Chaetoceros spp. resting spores were abundant throughout Effingham Inlet, with the exception of the stations closest to the fjord head. Stations located in the outer basin and towards the fjord mouth had relatively lower absolute abundance yet showed a higher relative and absolute abundance of Thalassionema nitzschioides, Rhizosolenia setigera, Coscinodiscus radiatus, Ditylum brightwellii, Odontella longicruris, and Paralia sulcata in relation to the inner basin. Many of these latter taxa are often associated with late summer and autumn conditions in fjords along coastal British Columbia. Oceanographic data for Effingham Inlet suggest that increased offshore penetration is more likely to occur from summer to early fall, with a more restricted offshore influence in the inner basin. Diatom surface sediment assemblages in Effingham Inlet appear to reflect incursions of offshore waters into the fjord. Absolute abundance estimates and the preservation of lightly silicified taxa suggest excellent preservation of fossil material in the sediments of the predominantly anoxic inner basin. Preservation in the outer basin is reduced, reflecting more frequent recharge by oxygenated waters spilling over the outer sill into the basin. Our findings suggest the inner basin should be an optimal site for reconstruction of diatom production, with records from the outer basin providing more consistent information about offshore influence and coastal up,welling conditions over the Holocene. Estimates of diatom abundance within the inner basin sediment may serve as a good proxy of production, although proxy tracers of bottom water conditions and sedimentological analyses must be coupled to the diatom record to ensure depositional conditions were not influencing valve preservation or abundance. Our results suggest that fjords can serve as good environments for paleoceanographic reconstructions of both inshore and offshore conditions although careful site selection and understanding of processes affecting the microfossil record are essential. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Laval, Dept Geog, Paleolimnol Paleoecol Lab, Quebec City, PQ G1K 7P4, Canada; Univ Laval, Ctr Etud Nord, Quebec City, PQ G1K 7P4, Canada; Fisheries Oceans Canada Inst Ocean Sci, Sidney, BC V8L 4B2, Canada	Laval University; Laval University; Fisheries & Oceans Canada	Univ Laval, Dept Geog, Paleolimnol Paleoecol Lab, Quebec City, PQ G1K 7P4, Canada.	mb_hay@yahoo.com; reinhard.pienitz@cen.ulaval.ca; thomsonR@pac.dfo-mpo.gc.ca		Pienitz, Reinhard/0000-0002-3613-1673; Hay, Murray/0000-0002-6850-8842				ALBRIGHT LJ, 1992, CAN J FISH AQUAT SCI, V49, P1924, DOI 10.1139/f92-213; Allen SE, 2001, CAN J FISH AQUAT SCI, V58, P671, DOI 10.1139/cjfas-58-4-671; [Anonymous], P ODP SCI RESULTS; [Anonymous], P COLL NAT SCI SEOUL; [Anonymous], 2000, ANNOTATED DIATOM MIC; BURRELL DC, 1988, OCEANOGR MAR BIOL, V26, P143; Clague JJ, 1999, J COASTAL RES, V15, P45; Crosta X, 1997, MAR MICROPALEONTOL, V29, P283, DOI 10.1016/S0377-8398(96)00033-3; DALLIMORE A, 2001, THESIS CARLETON U; FREELAND HJ, 1982, J MAR RES, V40, P1069; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; Gustafsson M, 2002, HOLOCENE, V12, P325, DOI 10.1191/0959683602hl547rp; HAIGH R, 1992, MAR ECOL PROG SER, V89, P117, DOI 10.3354/meps089117; HASLE GR, 1984, J PLANKTON RES, V6, P493, DOI 10.1093/plankt/6.3.493; Hasle Grethe R., 1996, P5, DOI 10.1016/B978-012693015-3/50005-X; HOBSON LA, 1983, SEDIMENT GEOL, V36, P117, DOI 10.1016/0037-0738(83)90005-2; Hobson LA, 2001, MAR GEOL, V174, P125, DOI 10.1016/S0025-3227(00)00146-8; Hobson LA, 1997, MAR ECOL PROG SER, V150, P263, DOI 10.3354/meps150263; HOBSON LA, 1980, FJORD OCEANOGRAPHY, P423; Jennings AE, 1996, HOLOCENE, V6, P179, DOI 10.1177/095968369600600205; Karpuz NK, 1990, PALEOCEANOGRAPHY, V5, P557, DOI 10.1029/PA005i004p00557; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; Lisitzin AP., 1971, The Micropalaeontology of Oceans, P173; MACKAS DL, 1987, J GEOPHYS RES-OCEANS, V92, P2907, DOI 10.1029/JC092iC03p02907; MAYNARD N G, 1976, Paleobiology, V2, P99; McMinn A, 2001, HOLOCENE, V11, P291, DOI 10.1191/095968301671577682; McMinn Andrew, 1995, Diatom Research, V10, P145; McQuoid Melissa R., 1998, Diatom Research, V13, P311; McQuoid MR, 2001, MAR GEOL, V174, P111, DOI 10.1016/S0025-3227(00)00145-6; McQuoid MR, 1997, J PLANKTON RES, V19, P173, DOI 10.1093/plankt/19.2.173; Mikalsen G, 2001, HOLOCENE, V11, P437, DOI 10.1191/095968301678302878; Patterson RT, 2000, MICROPALEONTOLOGY, V46, P229, DOI 10.2113/46.3.229; Patterson RT, 2000, J FORAMIN RES, V30, P321, DOI 10.2113/0300321; PICKARD GL, 1961, J FISH RES BOARD CAN, V18, P907, DOI 10.1139/f61-062; PICKARD GL, 1963, J FISH RES BOARD CAN, V20, P1109, DOI 10.1139/f63-080; RAO VNR, 1976, SYESIS, V9, P173; Reigstad M, 1996, SARSIA, V80, P245, DOI 10.1080/00364827.1996.10413599; Rines JEB, 2002, MAR ECOL PROG SER, V225, P123, DOI 10.3354/meps225123; Roelofs A.K., 1983, THESIS U BRIT COLUMB; SANCETTA C, 1988, DEEP-SEA RES, V35, P71, DOI 10.1016/0198-0149(88)90058-1; SANCETTA C, 1989, J PLANKTON RES, V11, P503, DOI 10.1093/plankt/11.3.503; Sancetta C, 1989, PALEOCEANOGRAPHY, V4, P235, DOI 10.1029/PA004i003p00235; SCHIMMELMANN A, 1992, MAR GEOL, V106, P279, DOI 10.1016/0025-3227(92)90134-4; Schrader H.-J., 1978, Utrecht Micropaleontological Bulletins, P129; SHEMESH A, 1989, QUATERNARY RES, V31, P288, DOI 10.1016/0033-5894(89)90010-0; SKJOLDAL HR, 1986, MAR ECOL PROG SER, V30, P49, DOI 10.3354/meps030049; STOCKNER JG, 1977, J FISH RES BOARD CAN, V34, P907, DOI 10.1139/f77-142; STOCKNER JG, 1979, J FISH RES BOARD CAN, V36, P657, DOI 10.1139/f79-095; Stockwell D.A., 1991, PROC OCEAN DRILL SCI, P667; Stronach J. A., 1993, Marine Geodesy, V16, P1, DOI 10.1080/15210609309379675; TAKAHASHI M, 1978, J EXP MAR BIOL ECOL, V31, P283, DOI 10.1016/0022-0981(78)90064-3; TAKAHASHI M, 1977, DEEP-SEA RES, V24, P775, DOI 10.1016/0146-6291(77)90499-4; Taylor F, 2001, MAR MICROPALEONTOL, V41, P25, DOI 10.1016/S0377-8398(00)00049-9; Taylor FJR, 1996, CAN J FISH AQUAT SCI, V53, P2310, DOI 10.1139/f96-181; TAYLOR FJR, 1994, MAR ECOL PROG SER, V103, P151, DOI 10.3354/meps103151; Ter Braak C.J.F, 1998, CANOCO RELEASE 4 REF; TERBRAAK CJF, 1988, LWA8802 GLW AGR MATH; Thomson R.E., 1989, Effects of ocean variability on recruitment and an evaluation of parameters used in stock assessment models, V108, P265; Thomson RE, 1998, J GEOPHYS RES-OCEANS, V103, P3033, DOI 10.1029/97JC03220; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; THULIN B, 1992, HYDROBIOLOGIA, V235, P471, DOI 10.1007/BF00026235; Timothy DA, 2001, MAR CHEM, V73, P37, DOI 10.1016/S0304-4203(00)00071-2; TIMOTHY DA, 2001, THESIS BRIT COLUMBIA; Ware D.M., 1989, Effects of ocean variability on recruitment and an evaluation of parameters used in stock assessment models, V108, P359; WASSMANN P, 1991, OCEANOGR MAR BIOL, V29, P87; WELSCHMEYER NA, 1985, MAR BIOL, V90, P75, DOI 10.1007/BF00428217; Zar J.H., 2010, BIOSTAT ANAL; [No title captured]	68	35	37	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	JUL	2003	48	3-4					291	320		10.1016/S0377-8398(03)00025-2	http://dx.doi.org/10.1016/S0377-8398(03)00025-2			30	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	690AR					2025-03-11	WOS:000183525600006
J	Meier, KJS; Willems, H				Meier, KJS; Willems, H			Calcareous dinoflagellate cysts in surface sediments from the Mediterranean Sea: distribution patterns and influence of main environmental gradients	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate; calcareous cysts; ecology; Mediterranean Sea	EQUATORIAL ATLANTIC-OCEAN; WESTERN TROPICAL ATLANTIC; UPPER WATER COLUMN; THORACOSPHAERA-HEIMII; SPATIAL-DISTRIBUTION; GENERAL-CIRCULATION; LIFE-CYCLE; EASTERN; SCRIPPSIELLA; DINOPHYCEAE	The distribution of calcareous dinoflagellate cysts in surface sediments from the Mediterranean Sea was quantitatively analysed. The samples contain 11 cyst species and the vegetative coccoid Thoracosphaera heimii. Cyst abundance increases towards the deeper parts of the basins and is generally higher in the eastern Mediterranean Sea. Three major distribution characteristics exist: (1) different assemblages in oceanic and neritic regions, (2) little agreement with the associations of areas studied so far like the Atlantic Ocean, and (3) a unique oceanic assemblage in the eastern Mediterranean Sea. A gradual change in cyst assemblages from the western to the eastern Mediterranean Sea was observed and statistically compared with the main environmental gradients in the upper water column. Temperature, nitrate concentration and possibly salinity appear to be the most important factors controlling cyst production. Three groups containing cysts with similar environmental preferences can be distinguished: (1) an eastern Mediterranean group related to relatively high temperature and salinity but low nitrate concentration, (2) a group of more or less consistently abundant cosmopolitan species tolerating or even preferring relatively low temperature and salinity but high nitrate concentration, and (3) a group containing species that are possibly adapted to neritic environments and have probably been transported from coastal areas into the studied regions. In contrast to other calcareous plankton, calcareous dinoflagellate cysts correlate strongly with the main environmental gradients in the Mediterranean Sea, bearing a high potential for palaeoenvironmental reconstructions. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachberiech Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Meier, KJS (通讯作者)，Univ Bremen, Fachberiech Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.		Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. Sebastian/0000-0002-3918-4092				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; [Anonymous], 1988, OCEANOL ACTA; ANTOINE D, 1995, J GEOPHYS RES-OCEANS, V100, P16193, DOI 10.1029/95JC00466; BAUMANN KH, 2002, LATE Q S ATLANTIC RE; Berland Brigitte R., 1988, Oceanologica Acta Special Issue, V9, P163; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DALE B, 1992, OCEAN BIOCOENOSIS SE, V5, P33; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; Hieke W., 1999, METEOR BER U HAMBURG, V99, P1; HILL MO, 1980, VEGETATIO, V42, P47, DOI 10.1007/BF00048870; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Höll C, 2000, QUATERNARY RES, V54, P58, DOI 10.1006/qres.2000.2139; INOUYE I, 1983, S AFR J BOT, V2, P63, DOI 10.1016/S0022-4618(16)30147-4; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; JANOFSKE D, 2000, ECOLOGICAL STUDIES L; 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; Keupp Helmut, 1999, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V30, P33; Keupp Helmut, 1993, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V9, P25; KNAPPERTSBUSCH M, 1993, MAR MICROPALEONTOL, V21, P219, DOI 10.1016/0377-8398(93)90016-Q; Kohring Rolf, 1997, Neues Jahrbuch fuer Geologie und Palaeontologie Monatshefte, V3, P151; Kohring Rolf, 1993, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V9, P15; LAVIOLETTE PE, 1990, J GEOPHYS RES-OCEANS, V95, P1511, DOI 10.1029/JC095iC02p01511; LEHUCHER PM, 1995, OCEANOL ACTA, V18, P255; Levitus S., 1994, WORLD OCEAN ATLAS, V4; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; LOCHET F, 1990, HYDROBIOLOGIA, V207, P95, DOI 10.1007/BF00041445; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; Mercone D, 2000, PALEOCEANOGRAPHY, V15, P336, DOI 10.1029/1999PA000397; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; 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; Patzold J., 2000, OSTLICHES MITTELMEER, P00; Pinardi N, 2000, PALAEOGEOGR PALAEOCL, V158, P153, DOI 10.1016/S0031-0182(00)00048-1; PUJOL C, 1995, MAR MICROPALEONTOL, V25, P187, DOI 10.1016/0377-8398(95)00002-I; RAIMBAULT P, 1993, DEEP-SEA RES PT I, V40, P791, DOI 10.1016/0967-0637(93)90072-B; ROBINSON AR, 1992, EARTH-SCI REV, V32, P285, DOI 10.1016/0012-8252(92)90002-B; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; SPURR AR, 1969, J ULTRA MOL STRUCT R, V26, P31, DOI 10.1016/S0022-5320(69)90033-1; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; ter Braak C.J.F., 1987, P91; TERBRAAK CJF, 1998, CANONICAL COMMUNITY; VAISALA V, 1925, COMMENT PHYS MAT SOC, V2, P1; 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, 2002, PALAEOGEOGR PALAEOCL, V178, P53, DOI 10.1016/S0031-0182(01)00368-6; Vink A, 2001, PALEOCEANOGRAPHY, V16, P479, DOI 10.1029/2000PA000582; VINK A, 2002, LATE QUATERNARY S AT; Wendler I, 2002, GLOBAL PLANET CHANGE, V34, P219, DOI 10.1016/S0921-8181(02)00117-0; Wendler I, 2002, MAR MICROPALEONTOL, V46, P1, DOI 10.1016/S0377-8398(02)00049-X; YACOBI YZ, 1995, J MARINE SYST, V6, P179, DOI 10.1016/0924-7963(94)00028-A; ZAVATARELLI M, 1995, J PHYS OCEANOGR, V25, P1384, DOI 10.1175/1520-0485(1995)025<1384:ANSOTM>2.0.CO;2; Ziveri P, 2000, PALAEOGEOGR PALAEOCL, V158, P175, DOI 10.1016/S0031-0182(00)00049-3; Zonneveld KAF, 2000, REV PALAEOBOT PALYNO, V111, P197, DOI 10.1016/S0034-6667(00)00024-5; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	58	24	24	0	13	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	JUL	2003	48	3-4					321	354		10.1016/S0377-8398(03)00028-8	http://dx.doi.org/10.1016/S0377-8398(03)00028-8			34	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	690AR					2025-03-11	WOS:000183525600007
J	Carvalho, MD				Carvalho, MD			Paleoecological and paleoclimatic studies based on palynology of Pliocene and Pleistocene sediments from the Foz do Amazonas Basin, Brazil	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							FOREST DEVELOPMENT; POLLEN RECORD; RAIN-FOREST; QUATERNARY; COLOMBIA; ANDES	Pliocene and Pleistocene palynomorphs from a well drilled in the Foz do Amazonas Basin were studied for paleoecological and paleoclimatic interpretation. The taxa recorded are related to the vegetation of the Andean Cordillera and Amazon Plain and allow interpretations of the paleoclimate of the region. The following six palynoecological groups were established: pteridophyte spores, fungal spores, tropical flora, savanna and mountain flora (associated with glacial periods), and dinoflagellates (associated with interglacial periods). A total of five paleoclimatic phases were recognized: phases 1, 3 and 5 related to interglacial periods and phases 2 and 4 to glacial periods.			Carvalho, MD (通讯作者)，Estrada Rio Pau,2303 Bl 17-201, BR-21650000 Rio De Janeiro, RJ, Brazil.							ABSABER AN, 1977, PALEOCLIMAS, V3, P19; ABSY ML, 1991, CR ACAD SCI II, V312, P673; [Anonymous], LEIDSE GEOL MEDED; BOER NP, 1965, GEOL MIJNBOUW, V44, P254; BRANDAO JAS, 1995, B GEOCI PETROBRAS, V8, P91; BUSH MB, 1990, QUATERNARY RES, V34, P330, DOI 10.1016/0033-5894(90)90045-M; CASTRO JC, 1978, OFFSHORE TECHNOLOGY, V3265, P1843; ELSIK W C, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P137; ELSIK WC, 1976, GEOSCI MAN, V15, P155; GERMERAAD JH, 1968, REV PALAEOBOT PALYNO, V6, P177; Haberle S., 1997, Proc. Ocean Drill. Progr. Sci. Results, V155, P381, DOI 10.2973/odp.proc.sr.155.225.1997; Hammen T.van der., 1972, GEOLOGIE MIJNBOUW, V51, P641; HANSEN BCS, 1994, PALAEOGEOGR PALAEOCL, V109, P263, DOI 10.1016/0031-0182(94)90179-1; Heusser CalvinJ., 1971, POLLEN SPORES CHILE; HOOGHIEMSTRA H, 1989, PALAEOGEOGR PALAEOCL, V72, P11, DOI 10.1016/0031-0182(89)90129-6; Hooghiemstra H, 1998, EARTH-SCI REV, V44, P147, DOI 10.1016/S0012-8252(98)00027-0; HOOGHIEMSTRA H, 1994, PALAEOGEOGR PALAEOCL, V109, P211, DOI 10.1016/0031-0182(94)90177-5; HOORN C, 1995, GEOLOGY, V23, P237, DOI 10.1130/0091-7613(1995)023<0237:ATAACF>2.3.CO;2; HORN SP, 1985, INITIAL REP DEEP SEA, V84, P533; LEDRU MP, 1993, QUATERNARY RES, V39, P90, DOI 10.1006/qres.1993.1011; Muller J., 1987, CONTRIBUTIONS SERIES, V19, P7; MULLER JAN, 1959, MICROPALEONTOLOGY, V5, P1, DOI 10.2307/1484153; REGALI MSP, 1982, 2 C BRAS PETR RIO JA; Roubik DW., 1991, MONOGRAPHS SYSTEMATI, V36, P1; van der Hammen T., 1974, J BIOGEOGR, V1, P3; Van der Hammen T., 1963, LEIDSE GEOLOGISCHE M, V29, P125; VANDERHAMMEN T, 1994, PALAEOGEOGR PALAEOCL, V109, P247, DOI 10.1016/0031-0182(94)90178-3; WALTER H., 1984, VEGETACAO ZONAS CLIM; WIJNINGA VM, 1990, REV PALAEOBOT PALYNO, V62, P249, DOI 10.1016/0034-6667(90)90091-V; WIJNINGA VM, 1990, REV PALAEOBOT PALYNO, V78, P69	30	4	5	0	5	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	JUL	2003	229	1					1	18						18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	712QU					2025-03-11	WOS:000184809000001
J	Quattrocchio, ME; Sarjeant, WAS				Quattrocchio, ME; Sarjeant, WAS			Dinoflagellates from the Chorrillo Chico Formation (Paleocene) of southern Chile	AMEGHINIANA			English	Article						dinoflagellates; Chorrillo Chico Formation; paleocene; southern Chile	CRETACEOUS-TERTIARY BOUNDARY; CYST; STRATIGRAPHY; SEQUENCE	Twenty-seven dinoflagellate taxa from the Chorrillo Chico Formation at Punta Prat, western side of the Brunswick Peninsula (Chile), are recognized. Stratigraphically important species include: Cassidium fragile (Harris) Drugg, Deflandrea cygniformis Pothe de Baldis, D. fuegensis Menendez, Eisenackia crassitabulata Deflandre and Cookson, Glaphyrocysta cf. retiintexta (Cookson) Stover and Evitt, Impagidinium cassiculuni Wilson, Isabelidinium bakeri (Deflandre and Cookson) Lentin and Williams, Palaeocystodinium golzowense Alberti, Palaeoperidinium pyrophorum (Ehrenberg) Evitt, Damaza and Albert, Pyxidiniopsis crassimurata Wilson, Spiniferella cornuta (Gerlach) Stover and Hardenboll, Spiniferites (Hafniasphaera) cryptovesiculata (Hansen) stat. nov. and Turbiosphaera filosa (Wilson) Archangelsky. The Tribe Spinidineae of Bujak and Davies is elevated to subfamily status and emended; its type genus, Spinidinhini, is likewise emended. Two new genera, Volkheimeridium and Magallanesium, are proposed, nine species being placed within these genera. The genus Alisocysta Stover and Evitt is treated as a taxonomic synonym of Eisenackia Deflandre and Cookson; its constituent species are transferred to the latter genus and a new species, E. chilensis, is described. The species bergmannii, previously placed in Operculodinium, is transferred to Lingulodinium and emended. A mid to late Paleocene age is proposed for the studied section. Assemblages are compared with those,reported from other basins, especially those of the Southern Hemisphere.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); University of Saskatchewan	Quattrocchio, ME (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.							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J	Godhe, A; McQuoid, MR				Godhe, A; McQuoid, MR			Influence of benthic and pelagic environmental factors on the distribution of dinoflagellate cysts in surface sediments along the Swedish west coast	AQUATIC MICROBIAL ECOLOGY			English	Article						cysts; dinoflagellate; dinophyceae; surface sediment; CCA; PLS; environmental factors	THECA RELATIONSHIP; MARINE-SEDIMENTS; NARRAGANSETT BAY; NORWEGIAN FJORD; RESTING CYSTS; GULLMAR-FJORD; BALTIC SEA; DINOPHYCEAE; INDICATORS; DIATOM	Abundance and frequency of dinoflagellate cysts in 19 surface sediment samples from the northern part of the Swedish west coast has been related to physical and chemical characters of the sediment, hydrography of the overlying water column, and plankton species data from the area. Density of cysts varied between 5000 and 10 1000 cysts g(-1) dw, and the most commonly encountered species were Lingulodinium polyedrum and Protoceratium reticulatum. In all, 46 environmental variables were tested for their relation to dinoflagellate cyst densities, proportion of autotrophic and heterotrophic taxa, and individual species distribution and frequency. The outcomes of multivariate analyses, projection to latent structures (PLS) and canonical correspondence analysis (CCA) were consistent with each other and the actual cyst count. The density of the total cyst assemblage (>90% autotrophic taxa) was primarily related to surface temperature, macronutrients, and inversely to phytoplankton competitors, such as diatoms. The abundance of heterotrophic taxa was governed by the preferences of their prey, i.e. diatom-favourable conditions, and, in most cases, higher proportions of heterotrophic taxa were found at well-mixed sites. Some possible effects of anthropogenic contaminants were also noted. Several taxa showed distinct distribution patterns with respect to the environmental variables. A discrepancy between the species constituting the planktonic and the benthic community was revealed when data from 6 yr of plankton monitoring was compared to the data on distribution of dinoflagellate cysts. In particular, cyst-forming species were only a minor part of the plankton, suggesting that these dinoflagelldtes spend much of their life in the sediments.	Gothenburg Univ, Dept Marine Ecol, S-40530 Gothenburg, Sweden	University of Gothenburg	Gothenburg Univ, Dept Marine Ecol, POB 461, S-40530 Gothenburg, Sweden.	anna.godhe@marbot.gu.se						[Anonymous], 1988, ADV ECOLOGICAL RES A; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Archer SD, 1996, MAR ECOL PROG SER, V139, P239, DOI 10.3354/meps139239; Björk G, 2000, ESTUARIES, V23, P367, DOI 10.2307/1353329; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; CATO I, 1997, SEDIMENTOLOGICAL INV; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B., 1979, P443; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; DODGE JD, 1982, MARIEN DINOFLAGELLAT; DRESBES G, 1974, MARINES PHYTOPLANKTO; 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, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Eriksson L., 1999, Umetrics; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; Goodman D. 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JUN 6	2003	32	2					185	201		10.3354/ame032185	http://dx.doi.org/10.3354/ame032185			17	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	695HR		Bronze			2025-03-11	WOS:000183825500008
J	Servais, T; Li, J; Molyneux, S; Raevskaya, E				Servais, T; Li, J; Molyneux, S; Raevskaya, E			Ordovician organic-walled microphytoplankton (acritarch) distribution: the global scenario	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	Meeting on Early Palaeozoic Palaeogeographies and Palaeobiogeographies of Western Europe and North Africa	SEP, 2001	UNIV SCI & TECHNOL LILLE, VILLENEUVE ASCQ, FRANCE		UNIV SCI & TECHNOL LILLE	acritarchs; Ordovician; palaeobiogeography	PALEOGEOGRAPHIC SIGNIFICANCE; ARENIGIAN ACRITARCHS; SOUTH-CHINA; PALEOBIOGEOGRAPHY; AFFINITIES; SEDIMENTS; MIDDLE; NORTH; BIOSTRATIGRAPHY; BIOGEOGRAPHY	A number of palacobiogeographical models for Ordovician organic-walled microphytoplankton (acritarchs, prasinophytes, and related groups) have been published during the past 30 years. A modern synthesis of Ordovician acritarch palacobiogeography, based on previously published acritarch 'provinces' and global distribution models, as well as new plots on recently compiled palacogeographical maps is presented. Review of the literature and new plots indicate that a number of preliminary conclusions can be drawn. Following minor biogeographical differentiation of acritarch assemblages during the Cambrian, 'provincialism' started at the Cambrian-Ordovician boundary. In the late Tremadocian a warm-water assemblage, containing the genera Aryballomorpha, Athabascaella and Lua, but no diacrodians, seems to be limited to low-latitude localities such as Laurentia and North China. From the late Tremadocian and throughout most of the Arenig a peri-Gondwana acritarch assemblage with the easily recognisable taxa Arbusculidium filamentosum, Coryphidium, and Striatotheca is present on the southern margin of Gondwana, and its distribution corresponds almost exactly with that of the Calymenacean-Dalmanitacean trilobite fauna. It seems reasonable to consider the acritarchs of Baltica as belonging to a temperate-water 'province', which was probably not restricted to the palaeocontinent of Baltica but had a wider distribution at about the same latitude, as some of the elements recorded from Baltica also occur in South China and Argentina. The maximum separation of the continents during the Arenigian, reflected by a pronounced biogeographical differentiation of most Ordovician fossil groups, led to the development of geographically distinct acritarch assemblages. Data from the late Middle Ordovician and the Late Ordovician remain too poor to elucidate global palaeobiogeographical patterns. The biogeographical distribution of Ordovician acritarchs appears similar to that of the resting cysts of modern dinoflagellates, primarily controlled by latitude but also following the continental margins. (C) 2003 Elsevier Science B.V. All rights reserved.	USTL, CNRS, UMR 8014, SN5,Lab Paleontol & Paleogeog Paleozoique LP, F-59655 Villeneuve Dascq, France; Acad Sinica, Nanjing Inst Geol & Palaeontol, Nanjing, Peoples R China; British Geol Survey, Keyworth NG12 5GG, Notts, England; St Petersburg State Univ, Geol Fac, St Petersburg 199034, Russia	Universite de Lille; Centre National de la Recherche Scientifique (CNRS); Chinese Academy of Sciences; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Saint Petersburg State University	USTL, CNRS, UMR 8014, SN5,Lab Paleontol & Paleogeog Paleozoique LP, F-59655 Villeneuve Dascq, France.	thomas.servais@univ-lille1.fr	Raevskaya, Elena/AAD-1285-2021; Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018	Raevskaya, Elena/0000-0002-0587-7499; Servais, Thomas/0000-0002-4089-7874				ACHAB A, 1992, J GEOL, V100, P621, DOI 10.1086/629612; Achab A., 1991, Geological Survey of Canada Paper, V90, P135; ACHAB A, 1988, CAN J EARTH SCI, V25, P635, DOI 10.1139/e88-061; ALBANI R, 1989, Bollettino della Societa Paleontologica Italiana, V28, P3; An T., 1987, EARLY PALEOZOIC CONO; [Anonymous], ACTA U CAROL GEOL; [Anonymous], GEOLOGICAL SURVEY CA; [Anonymous], 1996, P 9 INT PAL C HOUST; [Anonymous], 1988, Earth Environ. 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JUN 5	2003	195	1-2					149	172		10.1016/S0031-0182(03)00306-7	http://dx.doi.org/10.1016/S0031-0182(03)00306-7			24	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	686XE					2025-03-11	WOS:000183345600008
J	Hoedemaeker, PJ; Herngreen, GFW				Hoedemaeker, PJ; Herngreen, GFW			Correlation of Tethyan and Boreal Berriasian - Barremian strata with emphasis on strata in the subsurface of the Netherlands	CRETACEOUS RESEARCH			English	Review						correlation; Lower Cretaceous; sequence stratigraphy; biostratigraphy; the Netherlands; England; Germany; France; Spain	DINOFLAGELLATE CYST STRATIGRAPHY; MAGNETOSTRATIGRAPHY; BIOSTRATIGRAPHY; BOUNDARY; CARAVACA; PLATFORM; FLUCTUATIONS; STRATOTYPE; PATTERNS; PROVINCE	The standard Tethyan Berriasian-Barremian successions of France and Spain are correlated with the Boreal successions of England, Germany and the Netherlands. Special emphasis is placed on the correlation and sequence stratigraphy of the main hydrocarbon-producing strata of the Berriasian-Barremian stages in the four main basins in the subsurface of the Netherlands and the Dutch part of the North Sea continental shelf. All available biostratigraphic, magnetostratigraphic, and sequence-stratigraphic correlation data-sets were used to draw this correlation chart. Many lacunae in shallow marine successions could be correlated with sediments in deeper marine successions. Some sequence boundaries are tectonically enhanced and were accompanied by extra large falls in sea level; they initiated important changes in the biota and sedimentary regimes of western Europe, viz, the boundaries of the so-called 'transgressive regressive facies cycles' of Jacquin & de Graciansky. (C) 2003 Elsevier Ltd. All rights reserved.	Museum Natl Hist Nat, NL-2300 RA Leiden, Netherlands; TNO, Netherlands Inst Appl Geosci, Natl Geol Surv, Utrecht, Netherlands	Netherlands Organization Applied Science Research	Museum Natl Hist Nat, POB 9517, NL-2300 RA Leiden, Netherlands.	hoedemaeker@naturalis.nnm.nl; g.f.w.herngreen@bio.uu.nl						Aguado R, 2000, CRETACEOUS RES, V21, P1, DOI 10.1006/cres.2000.0198; Anderson F.W., 1973, Geological J Special Issue, VNo. 5, P101; Anderson F.W., 1985, Journal of Micropalaeontology, V4, P1; Anderson F. 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JUN	2003	24	3					253	275		10.1016/S0195-6671(03)00044-2	http://dx.doi.org/10.1016/S0195-6671(03)00044-2			25	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	723PC					2025-03-11	WOS:000185439900002
J	Hollis, CJ; Strong, CP				Hollis, CJ; Strong, CP			Biostratigraphic review of the Cretaceous/Tertiary boundary transition, mid-Waipara River section, North Canterbury, New Zealand	NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS			English	Article						Paleocene; Foraminifera; Radiolaria; palynomorphs; calcareous nannofossils; Antarcticella pauciloculata Zone; stratotype; paleoenvironment; biosiliceous	TERTIARY BOUNDARY; FLAXBOURNE RIVER; FORAMINIFERA; MIDLATITUDE; MARLBOROUGH; EXTINCTION	The mid-Waipara River section is the most complete known record of the Cretaceous/Tertiary (K/T) boundary transition in a South Pacific neritic setting. For local studies it provides a crucial link between bathyal marine and terrestrial records. The section contains abundant and diverse palynomorphs, including dinoflagellate cysts and terrestrial spores and pollen, as well as significant occurrences of biostratigraphically important foraminiferal, calcareous nannofossil, and radiolarian species. Examination of new and existing micropaleontology samples reveals a potentially complete early Paleocene foraminiferal succession correlated to Foraminiferal Zones PO to P1a-c. Although Cretaceous and basal Paleocene radiolarian assemblages lack age-diagnostic species, higher Paleocene radiolarian assemblages can be correlated to Radiolarian Zones RP2-RP4. Analysis of the distribution of RP3 and RP4 zonal markers in archival samples indicates that the sample sequence of Jenkins, previously published in 1971, is not in stratigraphic order. Bioturbation through the boundary interval and postdepositional leaching are thought to have contributed to relatively low levels of enrichment of K/T boundary fingerprint elements: Ir, Ni, Cr, and Zn. The K/T boundary coincides with a marked decrease in carbonate content, while correlated trends in Si/Al and Ba/Al indicate that biosiliceous productivity increased across the boundary. Extremely low carbonate content and common siliceous microfossils through 30 in of lower Paleocene strata suggest that cool oceanographic conditions prevailed in the northern Canterbury Basin for the first 1-2 m.y. of the Cenozoic.	Inst Geol & Nucl Sci, Lower Hutt, New Zealand	GNS Science - New Zealand	Hollis, CJ (通讯作者)，Inst Geol & Nucl Sci, POB 30368, Lower Hutt, New Zealand.		Hollis, Christopher/D-3560-2011	Hollis, Christopher John/0000-0001-8840-9852				ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], NZ GEOLOGICAL SURVEY; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BERGGREN WA, 1997, MICROPALEONTOLOGY S1, V43, P116; BROOKS RR, 1986, GEOLOGY, V14, P727, DOI 10.1130/0091-7613(1986)14<727:SOOIAA>2.0.CO;2; BROOKS RR, 1986, NEW ZEAL J GEOL GEOP, V29, P1; BROWNE GH, 1985, 6 NZ GEOL SURV; Couper R. A., 1960, NZ GEOLOGICAL SURVEY, V32; Edwards A. 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J	Marret, F; Zonneveld, KAF				Marret, F; Zonneveld, KAF			Atlas of modern organic-walled dinoflagellate cyst distribution	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						dinoflagellates; organic-walled cysts; geographic distribution; (palaeo-)ecology	GYMNODINIUM-CATENATUM GRAHAM; UPPER QUATERNARY SEDIMENTS; NORTHWESTERN INDIAN-OCEAN; NORTHERN NORTH-ATLANTIC; RECENT MARINE-SEDIMENTS; SEA-SURFACE CONDITIONS; NEW-SOUTH-WALES; ARABIAN SEA; RESTING CYSTS; MICRORETICULATE CYST	This Atlas summarises the global distribution of extant organic-walled dinoflagellate cysts in the form of 61 maps illustrated by the relative abundance of individual cyst taxa,in recent marine sediments from the Atlantic Ocean and adjacent basins, the Antarctic region (South Atlantic, southwestern, Pacific and southern Indian Ocean sections),. the Arabian Sea and the northwestern Pacific. This synthesis is based on the integration of literature sources together with data from 835 marine surface sediments prepared on a comparable methodology and taxonomy. The relationships between distribution patterns of cyst species and the surface-water parameters (temperature, salinity, phosphate and nitrate concentrations) are documented with graphs depicting the relative abundance of species in relation to seasonal and annual values of the above mentioned parameters at the sample sites. Two ordination techniques (detrended correspondence analysis and canonical correspondence analysis) have been carried out to statistically illustrate the relationships between species distribution and sea-surface conditions. Results have been compared with previously published records and an overview of the ecological significance of each individual species is presented. Characterisations of selected environments as well as a discussion about how additional processes such as preservation and transport could have affected the present dataset are included. This Atlas forms the basic printed version of an international database that will be freely available within the PANGAEA database: http:// www.pangaea.de and on the web site www.pangea.de/projects/dino-atlas. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Bremen, Div Palaeontol, D-28334 Bremen, Germany; Univ Coll N Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales	University of Bremen; Bangor University	Univ Bremen, Div Palaeontol, FB 5-Geowissensch,Postfach 330440, D-28334 Bremen, Germany.	f.marret@bangor.ac.uk; zonnev@uni-bremen.de		Marret-Davies, Fabienne/0000-0003-4244-0437				AKSELMAN R, 1987, Boletim do Instituto Oceanografico, V35, P17; Aksu AE, 1988, PALEOCEANOGRAPHY, V3, P519, DOI 10.1029/PA003i005p00519; Alldredge AL, 1998, J PLANKTON RES, V20, P393, DOI 10.1093/plankt/20.3.393; Allison Peter A., 1995, Geological Society Special Publication, V83, P97, DOI 10.1144/GSL.SP.1995.083.01.06; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], 1969, HOT BRINES RECENT HE; [Anonymous], 1983, OC ANOGRAPH TROP; BAKKEN K, 1986, BOREAS, V15, P185; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; BALECH E, 1970, ANTARCT ECOL, P143; BARTON ED, 1989, DEEP-SEA RES, V36, P1121, DOI 10.1016/0198-0149(89)90082-4; BAUER S, 1991, DEEP-SEA RES, V38, P531, DOI 10.1016/0198-0149(91)90062-K; BELOW R, 1992, NEOGENE QUATERNARY D, P1; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Berger WH, 1996, SOUTH ATLANTIC, P1; BERRIT GR, 1966, P S OCEANOGRAPHY FIS, P13; Biebow N., 1996, 57 GEOM; Bint A.N., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P329; BLANCO J, 1989, Boletin Instituto Espanol de Oceanografia, V5, P11; BLANCO J, 1989, Scientia Marina, V53, P785; BLANCO J, 1989, Scientia Marina, V53, P813; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; BLANCO J, 1989, Scientia Marina, V53, P797; BLANCO J, 1983, INVEST PESQ, V52, P335; BLEIL U, 1996, BERICHTE FACHBEREICH, V77, P1; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; 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; BRADFORD MR, 1975, CAN J BOT, V53, P3064, DOI 10.1139/b75-335; BRINK KH, 1991, J GEOPHYS RES, V45, P497; BROCK JC, 1991, J GEOPHYS RES-OCEANS, V96, P20623, DOI 10.1029/91JC01711; BRUCE JG, 1979, J GEOPHYS RES-OCEANS, V84, P7742, DOI 10.1029/JC084iC12p07742; BRUCE JG, 1974, J MAR RES, V32, P419; BRUCE JG, 1973, DEEP-SEA RES, V20, P837, DOI 10.1016/0011-7471(73)90005-3; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Cho H.J., 1999, P 2 INT WORKSH OC FI, P73; COLIN C, 1991, OCEANOL ACTA, V14, P223; CURRIE RI, 1971, BIOL INDIAN OCEAN, P37; 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, 1985, NORSK GEOL TIDSSKR, V65, P97; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; DALE B., 1994, CARBON CYCLING GLOBA, P521; 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; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; de Vernal A., 1989, Proceedings of the Ocean Drilling Program Scientific results, V105, P401, DOI DOI 10.2973/0DP.PR0C.SR.105.134.1989; Deacon G.E. 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Palaeobot. Palynology	JUN	2003	125	1-2					1	200		10.1016/S0034-6667(02)00229-4	http://dx.doi.org/10.1016/S0034-6667(02)00229-4			200	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	689EL					2025-03-11	WOS:000183478600001
J	Crouch, EM; Dickens, GR; Brinkhuis, H; Aubry, MP; Hollis, CJ; Rogers, KM; Visscher, H				Crouch, EM; Dickens, GR; Brinkhuis, H; Aubry, MP; Hollis, CJ; Rogers, KM; Visscher, H			The <i>Apectodinium</i> acme and terrestrial discharge during the Paleocene-Eocene thermal maximum:: new palynological, geochemical and calcareous nannoplankton observations at Tawanui, New Zealand	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Paleocene-Eocene thermal maximum; dinoflagellate cyst; Apectodinium; geochemistry; calcareous nannoplankton; terrigenous delivery	PALAEOCENE/EOCENE BOUNDARY; ISOTOPE EXCURSION; PACIFIC-OCEAN; BIGHORN BASIN; CARBON; DINOFLAGELLATE; CLIMATE; SEA; PERTURBATIONS; PRODUCTIVITY	Manifestations of profound perturbations in biogeochemical systems during the Paleocene-Eocene thermal maximum (PETM) include a prominent global negative delta(13)C and a pronounced increase in the relative abundance of dinoflagellate cysts (dinocysts) assigned to the genus Apectodinium. While motile representatives of Apectodinium were most likely thermophilic and heterotrophic, the underlying causes of this dinoflagellate response are not well understood. Here we provide new insight by examining the palynology, chemistry and calcareous nannoplankton across the PETM in a continental slope section at Tawanui, New Zealand. Across the PETM, marked changes in the relative abundance of Apectodinium vary antithetically with significant changes in the delta(13)C of carbonate and organic matter. In general, the high relative abundance of Apectodinium relates to enhanced concentrations of dinocysts, signifying a 'bloom' of Apectodinium in surface waters during the PETM. Changes in Apectodinium and delta(13)C records correspond to variations in many other parameters, including a smaller negative shift in bulk carbonate delta(13)C than expected, increased terrestrial palynomorphs, elevated TOC and C/N ratios, lower carbonate contents, higher SiO2 and Al2O3 contents, and lower Si/Al ratios. All of these variations can be explained by an increase in delivery of terrigenous material to the continental margin. A peak in the relative abundance of Glaphyrocysta dinocysts at the onset of the PETM may indicate greater down slope transport of neritic material. Changes in calcareous nannoplankton abundances suggest increased nutrient availability in surface waters during the PETM. The combined results show that Apectodinium-dominated assemblages, global perturbations in carbon isotopes and enhanced terrigenous delivery closely correspond in time at Tawanui. A sudden and massive carbon injection to the ocean-atmosphere system may have enhanced weathering and increased terrigenous inputs to continental margins during the PETM. We further suggest that these inputs caused the Apectodinium acme by elevating primary productivity in marginal seas. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Dept Geobiol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Rice Univ, Dept Earth Sci, Houston, TX 77005 USA; James Cook Univ N Queensland, Sch Earth Sci, Townsville, Qld 4811, Australia; Rutgers State Univ, Dept Geol Sci, Piscataway, NJ 08854 USA	Utrecht University; GNS Science - New Zealand; Rice University; James Cook University; Rutgers University System; Rutgers University New Brunswick	Crouch, EM (通讯作者)，Univ Utrecht, Dept Geobiol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		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Paleoclimatol. Paleoecol.	MAY 25	2003	194	4					387	403		10.1016/S0031-0182(03)00334-1	http://dx.doi.org/10.1016/S0031-0182(03)00334-1			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	682HH					2025-03-11	WOS:000183085300003
J	Gómez, F				Gómez, F			Checklist of Mediterranean free-living dinoflagellates	BOTANICA MARINA			English	Review							SP-NOV DINOPHYCEAE; DIPLOPSALIS-GROUP DINOPHYCEAE; CALCAREOUS RESTING CYST; NORTHERN ADRIATIC SEA; PHYTOPLANKTON ASSEMBLAGES; MARINE DINOFLAGELLATE; VENICE LAGOON; LIFE-HISTORY; AEGEAN SEA; GENUS	An annotated checklist of the free-living dinoflagellates (Dinophyceae) of the Mediterranean Sea, based on literature records, is given. The distribution of 673 species in 9 Mediterranean sub-basins is reported. The number of taxa among the sub-basins was as follows: Ligurian (496 species), Balear-Provencal (360), Adriatic (322), Tyrrhenian (284), Ionian (283), Levantine (268), Aegean (182), Albordn (179) and Algerian Seas (151).	Univ Tokyo, Dept Aquat Biosci, Bunkyo Ku, Tokyo 1138657, Japan	University of Tokyo	Gómez, F (通讯作者)，Univ Tokyo, Dept Aquat Biosci, Bunkyo Ku, 1-1-1 Yayoi, Tokyo 1138657, Japan.	fernando.gomez@fitoplancton.com	Gomez, Fernando/B-2495-2009	Gomez, Fernando/0000-0002-5886-3488				Abboud-Abi Saab M., 1985, LEB SCI B, V1, P197; ALFINITO S, 1988, NOVA HEDWIGIA, V46, P357; ANDREIS C, 1975, Giornale Botanico Italiano, V109, P387; ANDREIS C, 1982, BOT MAR, V25, P225, DOI 10.1515/botm.1982.25.5.225; [Anonymous], 2008, FOOD SCI TECHN-BOCA; Athanassopoulos G., 1931, Bulletin de l'Institut Oceanographique Monaco, V576, P1; Athanassopoulos G., 1930, Bulletin de l'Institut Oceanographique Monaco, Vno. 565, P1; ATHANASSOPOULOS G., 1931, BULL INST OCEANOGR [MONACO], V588, P1; BALECH E, 1976, VIE MILIEU B OCEANOG, V26, P27; BALECH E, 1990, HELGOLANDER MEERESUN, V44, P387, DOI 10.1007/BF02365475; BALECH E, 1988, PUB ESP I ESPANOL OC, V1; Balkis Neslihan, 2001, Oebalia, V26, P97; BALLE P, 1961, RAPP P REUN COMMN IN, V16, P231; Bernhard M., 1967, Pubblicazioni della Stazione Zoologica di Napoli, V35, P137; Biecheler B., 1939, Bulletin de la Societe Zoologique de France, V64, P12; Biecheler B., 1938, Bulletin de la Societe Zoologique de France, V63, P9; BIECHELER BERTHE, 1934, COMPT REND ACAD SCI [PARIS], V198, P404; BLASCO D, 1974, RAPP COMM INT MER ME, V22, P65; Bohm A., 1933, Archiv fuer Protistenkunde, V80, P303; BOHM A., 1931, BOT ARCH, V31, P349; BOHM ANTON, 1933, ARCH PROTISTENK, V80, P351; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; BOUQUAHEUX F, 1972, CAH BIOL MAR, V13, P1; BOUQUAHEUX F, 1971, Archiv fuer Protistenkunde, V113, P314; BRAVO I, 1990, TOXIC MARINE PHYTOPL, P26; CABRINI M, 1988, NOVA THALASSIA, V9, P11; Cachon J., 1969, Protistologica, V5, P11; Cachon J., 1967, Protistologica, V3, P313; CACHON J., 1964, B I OCEANOGR MONACO, V62, P1; Cachon J., 1967, Protistologica, V3, P427; CACHON JEAN, 1966, PROTISTOLOGICA, V2, P23; CARBONELLMOORE MC, 1994, REV PALAEOBOT PALYNO, V84, P23, DOI 10.1016/0034-6667(94)90039-6; Caroppo C., 1995, Oebalia, V21, P61; Caroppo C, 2001, CONT SHELF RES, V21, P1839, DOI 10.1016/S0278-4343(01)00028-0; Caroppo C, 1999, BOT MAR, V42, P389, DOI 10.1515/BOT.1999.045; Caroppo C, 2000, J PLANKTON RES, V22, P381, DOI 10.1093/plankt/22.2.381; CARRADA GC, 1991, J PLANKTON RES, V13, P229, DOI 10.1093/plankt/13.1.229; CHATTON EDOUARD, 1933, BULL SOC ZOOL FRANCE, V58, P251; Cho ES, 2001, BOT MAR, V44, P57, DOI 10.1515/BOT.2001.008; CHRETIENNOTDINET MJ, 1993, PHYCOLOGIA, V32, P159, DOI 10.2216/i0031-8884-32-3-159.1; Ciminiello P, 2000, TOXICON, V38, P1871, DOI 10.1016/S0041-0101(00)00099-4; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; DASILVA NML, 1991, THESIS U P M CURIE P; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; De Angelis G., 1994, Oebalia, V20, P21; DELGADO M, 1987, Investigacion Pesquera (Barcelona), V51, P517; DELGADO M, 1990, Scientia Marina, V54, P169; DELGADO M, 1991, Scientia Marina, V55, P1; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; DODGE JD, 1993, BOT MAR, V36, P137, DOI 10.1515/botm.1993.36.2.137; DODGE JD, 1975, BOT J LINN SOC, V71, P103, DOI 10.1111/j.1095-8339.1975.tb02449.x; Dogiel V., 1906, Mitteilungen aus der Zoologischen Station zu Neapel Berlin, V18, P1; Dowidar N.M., 1974, Bulletin Inst Oceanogr Fish Cairo, V4, P319; DREBES G, 1981, BRIT PHYCOL J, V16, P207, DOI 10.1080/00071618100650211; EL-MAGHRABY A. 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Marina	MAY	2003	46	3					215	242		10.1515/BOT.2003.021	http://dx.doi.org/10.1515/BOT.2003.021			28	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	680ZN					2025-03-11	WOS:000183010100001
J	Hardeland, R; Poeggeler, B				Hardeland, R; Poeggeler, B			Non-vertebrate melatonin	JOURNAL OF PINEAL RESEARCH			English	Review						algae; antioxidative protection; circadian rhythms; dinoflagellates; fungi; invertebrates; melatonin; plants	DINOFLAGELLATE GONYAULAX-POLYEDRA; ARYLALKYLAMINE N-ACETYLTRANSFERASE; DROSOPHILA-MELANOGASTER; CIRCADIAN RHYTHMICITY; LIFE-SPAN; ANTIOXIDATIVE PROTECTION; INDUCED ENCYSTMENT; OXIDATIVE STRESS; CYST FORMATION; EDIBLE PLANTS	Melatonin has been detected in bacteria, eukaryotic unicells, macroalgae, plants, fungi and various taxa of invertebrates. Although precise determinations are missing in many of these organisms and the roles of melatonin are still unknown, investigations in some species allow more detailed conclusions. Non-vertebrate melatonin is not necessarily circadian, and if so, not always peaking at night, although nocturnal maxima are frequently found. In the cases under study, the major biosynthetic pathway is identical with that of vertebrates. Mimicking of photoperiodic responses and concentration changes upon temperature decreases have been studied in more detail only in dinoflagellates. In plants, an involvement in photoperiodism seems conceivable but requires further support. No stimulation of flowering has been demonstrated to date. A participation in antioxidative protection might be possible in many aerobic non-vertebrates, although evidence for a contribution at physiological levels is mostly missing. Protection from stress by oxidotoxins or/and extensions of lifespan have been shown in very different organisms, such as the dinoflagellate Lingulodinium , the ciliate Paramecium , the rotifer Philodina and Drosophila . Melatonin can be taken up from the food, findings with possible implications in ecophysiology as well as for human nutrition and, with regard to high levels in medicinal plants, also in pharmacology.	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J	Harris, AJ; Tocher, BA				Harris, AJ; Tocher, BA			Palaeoenvironmental analysis of Late Cretaceous dinoflagellate cyst assemblages using high-resolution sample correlation from the Western Interior Basin, USA	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; palaeoenvironment; Late Cretaceous; North America	CENOMANIAN-TURONIAN BOUNDARY; UNITED-STATES; NORTH-AMERICA; GREENHORN SEA; STRATIGRAPHY; CIRCULATION; EXTINCTION; SEDIMENTS	The Cretaceous geological record of the Western Interior Seaway of North America is one of the most thoroughly studied in the world. Extensive work on the lithostratigraphy, biostratigraphy, and geochemistry has resulted in a high-resolution chronostratigraphic framework, allowing precise, bed-by-bed correlation between sections hundreds of kilometres apart. Late Cenomanian to Early Turonian marine strata from five sites along a transect from Arizona to Kansas have been analysed for their palynological assemblages. At the time of deposition, the sites are thought to have been palaeoenvironmentally very different in terms of shoreline proximity, bathymetry, and salinity. Precise correlation of samples between the sites using the high-resolution stratigraphy has provided a valuable testing ground for a comparison of the dinoflagellate cyst assemblages. A number of species are determined to have palaeoenvironmental preferences in terms of salinity and shoreline proximity and this is supported by integration with the lithostratigraphy, macropalaeontology, micropalaeontology, and geochemistry. Previous palaeoenvironmental interpretations suggest that one Kansas site had comparatively much higher levels of primary productivity and this is reflected in the high ratio at this site of peridinioid to gonyaulacoid cysts. The high-resolution correlation also shows that a number of the biostratigraphically useful dinoflagellate cyst taxa had synchronous or near-synchronous range tops and bases across the basin. This integrated, high-resolution study with tight chronostratigraphic control supports the use of dinoflagellate cysts, not only as biostratigraphic tools but also for palaeoenvironmental and palaeoecological interpretation. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Glamorgan, Sch Appl Sci, Pontypridd CF37 1DL, M Glam, Wales; STATOIL, N-4035 Stavanger, Norway	University of South Wales	Harris, AJ (通讯作者)，Univ Glamorgan, Sch Appl Sci, Pontypridd CF37 1DL, M Glam, Wales.							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Micropaleontol.	MAY	2003	48	1-2					127	148		10.1016/S0377-8398(03)00002-1	http://dx.doi.org/10.1016/S0377-8398(03)00002-1			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	680GC					2025-03-11	WOS:000182967100007
J	Yamaguchi, M				Yamaguchi, M			Studies on prediction and biological control of the harmful algal blooms	NIPPON SUISAN GAKKAISHI			Japanese	Review							DINOFLAGELLATE HETEROCAPSA-CIRCULARISQUAMA; HETEROSIGMA-AKASHIWO RAPHIDOPHYCEAE; ALEXANDRIUM-TAMARENSE DINOPHYCEAE; PHOSPHORUS-LIMITED CULTURES; SPP. DINOPHYCEAE; GROWTH-KINETICS; RESTING CYSTS; HIROSHIMA BAY; INLAND SEA; ABUNDANCE		Fisheries Res Agcy, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Yamaguchi, M (通讯作者)，Fisheries Res Agcy, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Ohno, Hiroshima 7390452, Japan.							ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], P 1 INT C TOX DIN BL; CEMBELLA AD, 1984, CRC CR REV MICROBIOL, V11, P13, DOI 10.3109/10408418409105902; Eppley R., 1980, PRIMARY PRODUCTIVITY, V19, P231, DOI [10.1007/978-1-4684-3890-1_13, DOI 10.1007/978-1-4684-3890-1_13]; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HONJO T, 1990, TOXIC MARINE PHYTOPLANKTON, P165; Imai I., 1998, PHYSL ECOLOGY HARMFU, P95; Itakura S, 2002, FISHERIES SCI, V68, P77, DOI 10.1046/j.1444-2906.2002.00392.x; Itakura S, 2001, PHYCOLOGIA, V40, P263, DOI 10.2216/i0031-8884-40-3-263.1; IWASAKI H, 1979, BIOCH PHYSL PROTOZOA, V1, P357; Iwataki M, 2002, FISHERIES SCI, V68, P1161, DOI 10.1046/j.1444-2906.2002.00549.x; MCDUFF RE, 1982, LIMNOL OCEANOGR, V27, P783, DOI 10.4319/lo.1982.27.4.0783; Nagasaki K, 1997, AQUAT MICROB ECOL, V13, P135, DOI 10.3354/ame013135; NAGASAKI K, 1994, MAR BIOL, V119, P307, DOI 10.1007/BF00349570; Nagasaki K, 1998, AQUAT MICROB ECOL, V14, P109, DOI 10.3354/ame014109; Tarutani K, 2000, APPL ENVIRON MICROB, V66, P4916, DOI 10.1128/AEM.66.11.4916-4920.2000; Tarutani K, 2001, AQUAT MICROB ECOL, V23, P103, DOI 10.3354/ame023103; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2; WEILER CS, 1979, J EXP MAR BIOL ECOL, V39, P1, DOI 10.1016/0022-0981(79)90002-9; Yamaguchi, 1996, HARMFUL TOXIC ALGAL, P177; Yamaguchi M, 1997, J PLANKTON RES, V19, P1167, DOI 10.1093/plankt/19.8.1167; Yamaguchi M, 2002, FISHERIES SCI, V68, P1012, DOI 10.1046/j.1444-2906.2002.00526.x; 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; YAMAGUCHI M, 1994, PHYCOLOGIA, V33, P163, DOI 10.2216/i0031-8884-33-3-163.1; YAMAGUCHI M, 1992, MAR BIOL, V112, P191, DOI 10.1007/BF00702461; Yamasaki T, 2001, NDT&E INT, V34, P207, DOI 10.1016/S0963-8695(00)00060-8	27	0	0	2	16	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	MAY	2003	69	3					322	325						4	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	703XW		Bronze			2025-03-11	WOS:000184308800002
J	Barreda, V; Limarino, C; Fauqué, L; Tripaldi, A; Net, L				Barreda, V; Limarino, C; Fauqué, L; Tripaldi, A; Net, L			First palynological record for the lower member of Cerro Morado Formation (Miocene), La Rioja Precordillera.	AMEGHINIANA			Spanish	Article						palynology; sedimentology; Miocene; Cerro Morado Formation; Precordillera; La Rioja province	PROVINCE	FIRST PALYNOLOGICAL RECORD FOR THE LOWER MEMBER OF CERRO MORADO FORMATION (MIOCENE), LA RIOJA PRECORDILLERA. The finding of palynological remains in the lower member of the Cerro Morado Formation is reported for the first time. The fossiliferous levels are located at the headwaters of the Guandacol river in southwestern La Rioja Province. In this area the Cerro Morado Formation has been divided into two members. The lower member, composed of sandstones, mudstones and scarse conglomerates and limestones, contains the palynological remains. described in this paper. The palynological assemblages are not diverse, they are poorly preserved and dominated by aquatic elements mainly related to colonial green algae (Pediastrum spp., Botryococcus sp.) and dinoflagellates. Spore-pollen assemblages consist of aquatic herbs of Restionaceae (Milfordia sp.) and Malvaceae (Baumannipollis chubutensis Barreda, Baumannipollis sp., Malvacipolloides comodoroensis Barreda). Typical lake shore vegetation consisted of members of Ephedraceae [Equisetosporites claricristatus (Shakmundes) Barreda, E. notensis (Cookson) Romero, E. lusaticus (Krutzsch) Barreda] and scarse Chenopodiaceae (Chenopodipollis chenopodiaceoides (Martin) Truswell). Pollen grains related to Podocarpaceae (Podocarpidites marwickii Couper, P. elegans Romero) and Fagaceae (Nothofagidites acromegacanthus Menendez and Caccavari, N. americanus Zamaloa, N. saraensis Menendez and Caccavari) are also present, although in low percentages. The known stratigraphic ranges of the recognized species, and the similarities of these assemblages to others previously described from Argentina, point to an Early to Middle Miocene age for this unit. Finally, sedimentological and palynological. evidences suggest the development of a large and perennial water body during the time of deposition of the lower member of Cerro Morado Formation.	Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, RA-1405 Buenos Aires, DF, Argentina; Univ Buenos Aires, Fac Ciencias Exactas & Nat, Consejo Nacl Invest Cient & Tecn, Dept Ciencias Geol, RA-1428 Buenos Aires, DF, Argentina; Serv Geol Minero Argentino, Buenos Aires, DF, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); University of Buenos Aires	Barreda, V (通讯作者)，Consejo Nacl Invest Cient & Tecn, Museo Argentino Ciencias Nat Bernardino Rivadavia, Av Angel Gallardo 470, RA-1405 Buenos Aires, DF, Argentina.			Limarino, Carlos/0000-0002-9891-143X; Barreda, Viviana Dora/0000-0002-1560-1277				[Anonymous], REV ASOCIACION GEOLO; Barreda VD, 1998, AMEGHINIANA, V35, P321; BARREDA VD, 2000, NEOGENO ARGENTINA CG, V14, P103; Barreda Viviana D., 1996, Ameghiniana, V33, P35; BORELLO A, 1968, COMISION INVESTIGACI, V7, P3; DODSON JR, 1974, AUST J BOT, V22, P709, DOI 10.1071/BT9740709; FURQUE G, 1979, SERVICIO GEOLOGICO N, V164; Furque G., 1963, B DIRECCION NACL GEO, V92, P1; Jordan T.E., 1993, XII Congreso Geologico Argentino y II Congreso de Exploracion de Hirdocarburos, Actas, VII, P132; LIMARINO CO, REV ASOCIACION GEOLO, V57, P289; NORRIS G., 1992, PALYNOLOGY, V16, P234; Ottone E.G., 1998, REV ESP MICROPALEONT, V30, P35; PRAMPARO M, 1995, 6 C ARG PAL BIOESTR, V1, P207; Pramparo Mercedes B., 1996, Ameghiniana, V33, P397; REYNOLDS C S, 1968, British Phycological Bulletin, V3, P451; REYNOLDS JH, 1990, GEOL SOC AM BULL, V102, P1607, DOI 10.1130/0016-7606(1990)102<1607:NDOTFS>2.3.CO;2; SIMON W, 1987, ASOCIACION GEOLOGI A, V2, P370; SINGH G, 1981, J GEOL SOC AUST, V28, P435, DOI 10.1080/00167618108729180; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Witkowski A, 1990, ACTA GEOL POL, V40, P1	20	8	9	0	0	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana	MAR 30	2003	40	1					81	87						7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	665BB					2025-03-11	WOS:000182098800005
J	Lee, JJ; Shpigel, M; Freeman, S; Zmora, O; Mcleod, S; Bowen, S; Pearson, M; Szostek, A				Lee, JJ; Shpigel, M; Freeman, S; Zmora, O; Mcleod, S; Bowen, S; Pearson, M; Szostek, A			Physiological ecology and possible control strategy of a toxic marine dinoflagellate, <i>Amphidinium</i> sp., from the benthos of a mariculture pond	AQUACULTURE			English	Article						mariculture contaminant; Amphidinium sp.; toxic dinoflagellate; eurytrophic dinoflagellate; sedimentation pond flora	PHYTOPLANKTON	Some species of Amphidinium are known to have produced toxins. When a species of Amphidinium bloomed in a mariculture sediment pond fed by effluent water from semi-intensive fishponds, it was isolated and its physiological ecology was investigated to find its tolerances and optima for population growth (temperature, salinity, pH, nitrate/ammonia, phosphorus, and vitamin B-12). In a preliminary test, an ether-soluble extract was toxic to mice. The Amphidinium sp. was eurytrophic, with a great facility for luxury consumption and the ability to store nitrate and phosphate for several generations. It needs vitamin B-12 and formed cysts when exposed to high levels of ammonium. Its maximum growth rate was 1 division/day, and it grew well between 20 and 33 degreesC. It was tolerant of a wide range of pH (6.5-9.5; optima 6.5-8.6) and salinities (20-50 parts per thousand; optima 22-32 parts per thousand). The Amphidinium was outcompeted by diatoms if the Si/N ratio was kept at 1:1 or greater, suggesting that this factor could control its growth in sedimentation ponds used in integrated systems to grow mollusks. Eurytrophic organisms are difficult to control by environmental methods, thus, vigilance is required to ensure that bivalves fed from sediment ponds are not contaminated with toxins from this or any other dinoflagellate. (C) 2003 Elsevier Science B.V. All rights reserved.	CUNY City Coll, Dept Biol, New York, NY 10031 USA; Natl Ctr Mariculture, Elat, Israel	City University of New York (CUNY) System; City College of New York (CUNY)	Lee, JJ (通讯作者)，CUNY City Coll, Dept Biol, Convent Ave & 138 St, New York, NY 10031 USA.							CAOVIEN M, 1968, CR HEBD ACAD SCI, V267, P701; DORTCH Q, 1984, MAR BIOL, V81, P237, DOI 10.1007/BF00393218; EPPLEY RW, 1969, LIMNOL OCEANOGR, V14, P194, DOI 10.4319/lo.1969.14.2.0194; FERNANDEZ ML, 1995, MANUAL HARMFUL MARIN, V33; FUKUDA K, 1998, REC RES DEV FERMEN 1, V1, P47; Halim Y., 1969, Oceanogr. mar. Biol., V7, P231; KIMOR B, 1977, MAR BIOL, V42, P55, DOI 10.1007/BF00392014; LEE JJ, UNPUB AQUACULTURE; LEE JJ, UNPUB J EUKARYOT MIC; LEE RE, 1989, PHYCOLOGY, P338; LEWIS RJ, 1995, MANUAL HARMFUL MARIN, V33; LOEBLICH AR, 1966, PHYKOS, V5, P216; Neori A, 1998, AQUACULT ENG, V17, P215, DOI 10.1016/S0144-8609(98)00017-X; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1984, AM J BOT, V71, P1121, DOI 10.2307/2443388; PROVASOLI L, 1957, ARCH MIKROBIOL, V25, P392, DOI 10.1007/BF00446694; Provasoli L, 1963, S MARINE MICROBIOLOG, P105; Shpigel M., 1993, Aquaculture and Fisheries Management, V24, P529, DOI 10.1111/j.1365-2109.1993.tb00628.x; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Steidinger K.A., 1984, P201; TAYLOR FJ.R., 1987, BIOL DINOFLAGELLATES, P398; TAYLOR FJR, 1983, ENDOCYTOBIOLOGY, V2, P1009; THOMAS WH, 1980, J EXP MAR BIOL ECOL, V45, P25, DOI 10.1016/0022-0981(80)90067-2; THOMAS WH, 1963, LIMNOL OCEANOGR, V8, P357, DOI 10.4319/lo.1963.8.3.0357; TINDAL DR, 1984, J AM CHEM SOC, V262, P21; WEDEMAYER GJ, 1982, J PHYCOL, V18, P13, DOI 10.1111/j.1529-8817.1982.tb03152.x; WILSON MK, 1984, 2 DIV RES SEM CSIRO	27	14	20	1	14	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0044-8486			AQUACULTURE	Aquaculture	MAR 17	2003	217	1-4					351	371	PII S0044-8486(02)00373-3	10.1016/S0044-8486(02)00373-3	http://dx.doi.org/10.1016/S0044-8486(02)00373-3			21	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	648BE					2025-03-11	WOS:000181129300028
J	Montresor, M; Nuzzo, L; Mazzocchi, MG				Montresor, M; Nuzzo, L; Mazzocchi, MG			Viability of dinoflagellate cysts after the passage through the copepod gut	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						copepods; cysts; Dinoflagellates; grazing; Scrippsiella; viability	DINOPHYCEAE RESTING CYSTS; NORTHERN BALTIC SEA; PLANKTONIC DIATOMS; FEEDING-BEHAVIOR; DIAPAUSE EGGS; SCRIPPSIELLA; ZOOPLANKTON; SEDIMENTS; ECOLOGY; GERMINATION	Several dinoflagellate species form nonmotile, thick-walled resting cysts in their life cycle. Cysts can be ingested by planktonic and benthic organisms, but there is scarce information concerning their survival after the passage through the digestive apparatus of the grazers. We tested the germination capability of cysts produced by two neritic dinoflagellates, Scrippsiella trochoidea (F. Stein) A.R. Loeblich and Scrippsiella ramonii Montresor, after their ingestion by four copepod species. Experiments have been carried out with four species: Acartia clausi Giesbrecht, 1889; Centropages typicus Kroyer, 1849; Temora stylifera Dana, 1849; and Clausocalanus lividus Frost and Fleminger, 1968. Copepods were fed either with motile cells or cysts, and feeding and clearance rates were estimated for A. clausi, C. lividus and T stylifera. Grazing rates on both dinollagellates was much higher for vegetative cells than for cysts. Resting cysts were isolated from the faccal pellets and incubated to test their germination capability. S. trochoidea cysts eaten by C. typicus and T stylifera showed a high germination rate, while cysts of the same species were not viable after the passage through the gut of A. clausi and C lividus. In contrast, S. ramonii cysts were never able to germinate after being ingested by copepods. The observed variation in viability among the two cyst types and the different survival rates observed for S. trochoidea cysts might be related to differences in cyst morphology and to differences in the digestive process among the tested copepod species. (C) 2002 Elsevier Science B.V. All rights reserved.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@szn.it		Montresor, Marina/0000-0002-2475-1787				Albertsson J, 2001, MAR BIOL, V138, P793, DOI 10.1007/s002270000498; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; ANRAKU M, 1963, LIMNOL OCEANOGR, V8, P116, DOI 10.4319/lo.1963.8.1.0116; Belmonte G, 1997, HYDROBIOLOGIA, V355, P159, DOI 10.1023/A:1003071205424; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; Clegg JS, 1997, J EXP BIOL, V200, P467; CONWAY DVP, 1994, MAR ECOL PROG SER, V106, P303, DOI 10.3354/meps106303; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DAHMS HU, 1995, HYDROBIOLOGIA, V306, P199, DOI 10.1007/BF00017691; Dale B., 1983, P69; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Frost B., 1968, Bulletin Scripps Institution of Oceanography Technical Series, V12, P1; FROST BW, 1972, LIMNOL OCEANOGR, V17, P805, DOI 10.4319/lo.1972.17.6.0805; Giangrande A, 2002, J SEA RES, V47, P97, DOI 10.1016/S1385-1101(01)00103-4; Grice G.D., 1981, Oceanography and Marine Biology an Annual Review, V19, P125; Guerrero F, 1998, J PLANKTON RES, V20, P305, DOI 10.1093/plankt/20.2.305; Hairston N.G. 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Exp. Mar. Biol. Ecol.	MAR 11	2003	287	2					209	221	PII S0022-0981(02)00549-X	10.1016/S0022-0981(02)00549-X	http://dx.doi.org/10.1016/S0022-0981(02)00549-X			13	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	653BB					2025-03-11	WOS:000181414400005
J	Morquecho, L; Lechuga-Devéze, CH				Morquecho, L; Lechuga-Devéze, CH			Dinoflagellate cysts in recent sediments from Bahia Concepcion Gulf of California	BOTANICA MARINA			English	Article							RECENT MARINE-SEDIMENTS; GYMNODINIUM-CATENATUM; RED-TIDE; AUSTRALIA; PHYTOPLANKTON; TASMANIA; PACIFIC; NORWAY; WATERS; GENUS	The composition, abundance, and distribution of dinoflagellate resting cysts in recent sediments were analyzed at 12 sites in Bahfa Concepcion in the subtropical Gulf of California. Calcareous and organic Peridiniales, Gonyaulacales, and Gymnodiniales were identified at species level (25 cyst types). Empty cysts constituted 75-90% of cysts in the samples. Cyst assemblages were dominated by calcareous Peridiniales (30-70%) and Gonyaulacales (13-44%), represented mainly by Scrippsiella trochoidea and Lingulodinium polyedrum. In the first centimeter of sediment, cyst counts varied from 173 to 9, 933 cysts g(-1) wet weight, and increased in abundance in the inner area of the bay. Cysts of the toxic species Gymnodinium catenatum were also detected, and successful cyst germination of Alexandrium margalefii is described. Cyst abundance and distribution patterns suggest that the bay acts as a cyst trap, and that the cyst assemblages reflect the local community of meroplanktonic dinoflagellates.	CIBNOR, La Paz 23000, BCS, Mexico	CIBNOR - Centro de Investigaciones Biologicas del Noroeste	Morquecho, L (通讯作者)，CIBNOR, Apartado Postal 128, La Paz 23000, BCS, Mexico.		Morquecho, Lourdes/JPY-0626-2023	Morquecho, Lourdes/0000-0003-2963-8836				Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; [Anonymous], 1996, Diatomeas del Golfo de California; [Anonymous], P 1 INT C TOX DIN BL; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1989, Scientia Marina, V53, P785; BLANCO J, 1989, Scientia Marina, V53, P813; BLANCO J, 1989, Scientia Marina, V53, P797; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BRAY J. ROGER, 1957, ECOL MONOGR, V27, P325, DOI 10.2307/1942268; Bustillos-Guzmán J, 2000, J EXP MAR BIOL ECOL, V249, P77, DOI 10.1016/S0022-0981(00)00188-X; CHRETIENNOTDINET MJ, 1993, PHYCOLOGIA, V32, P159, DOI 10.2216/i0031-8884-32-3-159.1; Cortes-Altamirano Roberto, 1995, Revista Latinoamericana de Microbiologia, V37, P337; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Eppley RW., 1975, Proceedings of THE FIRST INTERNATIONAL CONFERENCE ON TOXIC DINOFLAGELLATE BLOOMS, P11; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garate-Lizarraga I., 2000, Harmful Algae News, V21, P7; GILMARTIN M, 1978, ESTUAR COAST MAR SCI, V7, P29, DOI 10.1016/0302-3524(78)90055-5; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Graham H.W., 1942, SCI RESULTS CRUISE 7, V3, P1; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hernandez Becerril D.U., 1987, Revista Latinoamericana de Microbiologia, V29, P171; HERNANDEZBECERRIL DU, 1987, NOVA HEDWIGIA, V45, P237; HORIGUCHI T, 1983, BOT MAG TOKYO, V96, P351, DOI 10.1007/BF02488179; Imamura K, 1987, GUIDE STUDIES RED TI, P54; Ishikawa Akira, 1993, Bulletin of Plankton Society of Japan, V40, P1; Lechuga-Devéze CH, 1998, B MAR SCI, V63, P503; Lechuga-Devéze CH, 2001, REV BIOL TROP, V49, P525; Licea S., 1995, Dinoflageladas del Golfo de California; MARGALEF RAMON, 1956, INVEST PESQ, V5, P113; MARTINEZHERNAND.E, 1991, DISTRIBUTION QUISTES, V57; Matsuoka K., 1989, P461; Matsuoka K., 2000, GUIA TECNICA ESTUDIO, P30; MATSUOKA K, 1992, NEOGENE QUANTERNARY, P32; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; MEE LD, 1986, MAR ENVIRON RES, V19, P77, DOI 10.1016/0141-1136(86)90040-1; MENDHAL KH, 1997, PLIOCENE CARBONATES, P36; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; MORQUECHOESCAMI.ML, 2001, SUSTENTABILIDAD BIOD, P281; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Obeso-Nieblas M., 1996, CICIMAR OCEANIDES, V11, P1; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; PFIESTER LA, 1987, BIOL DINOFLAGELLATES, P1123; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P589; Riegman R., 1998, NATO ASI SERIES G41, P475; Sierra-Beltran A. P., 1996, HARMFUL TOXIC ALGAL, P105; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; SWEENEY BM, 1975, P 1 INT C TOX DIN BL, P225; TAYLOR FJ.R., 1987, BIOL DINOFLAGELLATES, P1; TOMAS CR, 1996, LIVING MARINE DIATOM; 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; Wall D., 1986, THESIS U SASKATCHEWA	56	38	43	0	3	WALTER DE GRUYTER & CO	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055			BOT MAR	Bot. Marina	MAR	2003	46	2					132	141		10.1515/BOT.2003.014	http://dx.doi.org/10.1515/BOT.2003.014			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	662DD					2025-03-11	WOS:000181930200003
J	Persson, A; Rosenberg, R				Persson, A; Rosenberg, R			Impact of grazing and bioturbation of marine benthic deposit feeders on dinoflagellate cysts	HARMFUL ALGAE			English	Article						deposit feeder; dinoflagellate; cyst; sediment; grazing	SEDIMENTS; ECOLOGY	The impact of benthic deposit feeders on marine dinoflagellate cysts was studied by adding a concentrated natural Swedish cyst assemblage to sediment with different deposit feeders in replicate 4-1 aquaria. The deposit feeders used were the bivalve Abra nitida, the echinoderm Amphiura filiformis, and the polychaetes Melinna cristata and Nereis diversicolor. These species occur naturally near the Swedish west coast and were selected to represent different ways of feeding. The results showed a significant relative decrease of unfossilizable cyst species; whereas, the common fossilizable species Lingulodinium polyedrum significantly increased in the cyst assemblage after grazing. This work suggests that differences in dinoflagellate cyst compositions can in part be caused by different animal grazing behaviors. (C) 2003 Elsevier Science B.V. All rights reserved.	Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden; Univ Gothenburg, Kristineberg Marine Res Stn, Dept Marine Ecol, SE-45034 Fiskebackskil, Sweden	University of Gothenburg; University of Gothenburg	Persson, A (通讯作者)，NOAA, NMFS Milford Lab, 212 Rogers Ave, Milford, MA USA.	apersson@clam.mi.nmfs.gov; r.rosenberg@kmf.gu.se		Persson, Agneta/0000-0003-0202-6514				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; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BRAVO I, 1998, HARMFUL ALGAE, P356; Chester R., 1990, MAR GEOCHEMISTRY; Dale B., 1983, P69; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; LAROCQUE R, 1990, TOXIC MARINE PHYTOPLANKTON, P368; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; LOPEZ GR, 1987, Q REV BIOL, V62, P235, DOI 10.1086/415511; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; REID PC, 1987, J PLANKTON RES, V9, P249, DOI 10.1093/plankt/9.1.249; SONNEMANN JA, 1997, AUSTR BOT MAR, V40, P147; TAGHON GL, 1984, LIMNOL OCEANOGR, V29, P64, DOI 10.4319/lo.1984.29.1.0064; TURGEON J, 1990, TOXIC MARINE PHYTOPLANKTON, P238; Underwood AJ., 1996, Experiments in Ecology: Their Logical Design and Interpretation Using Analysis of Variance; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	26	37	40	1	11	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	MAR	2003	2	1					43	50		10.1016/S1568-9883(03)00003-9	http://dx.doi.org/10.1016/S1568-9883(03)00003-9			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	812UM					2025-03-11	WOS:000220864400004
J	Irwin, A; Hallegraeff, GM; McMinn, A; Harrison, J; Heijnis, H				Irwin, A; Hallegraeff, GM; McMinn, A; Harrison, J; Heijnis, H			Cyst and radionuclide evidence demonstrate historic <i>Gymnodinium catenatum</i> dinoflagellate populations in Manukau and Hokianga Harbours, New Zealand	HARMFUL ALGAE			English	Article						dinoflagellate cysts; sediment depth cores; Gymnodinium catenatum; PSP; New Zealand	MICRORETICULATE CYST; INDICATORS; EUTROPHICATION; BLOOMS; DINOPHYCEAE; SEDIMENTS; POLLUTION; CLIMATE; UNIQUE	Between May 2000 and February 2001, a major bloom of the toxic dinoflagellate Gymnodinium catenatum (a causative organism of Paralytic Shellfish Poisoning, PSP) affected over 1500 km of coastline of New Zealand's North Island. As this was the first record of this species in New Zealand, we aimed to resolve whether this represented a recent introduction/spreading event or perhaps an indigenous cryptic species stimulated by environmental/climatic change. To answer this question, we analysed for G. catenatum resting cysts in Pb-210 dated sediment cores (18-34 cm long; sedimentation rates 0.34-0.69 cm per year) collected by SCUBA divers from Manukau Harbour, where the species was first detected, and from Hokianga Harbour, where the highest shellfish toxicity was recorded, while using Wellington Harbour as a well-monitored control site. The results of this study conclusively demonstrate that abundant G. catenatum has been in northern New Zealand at least since the early 1980s, increasing up to 1200 cysts/g around the year 2000, but with low cyst concentrations possibly present since at least 1937. In contrast, Wellington Harbour cores contained only very sparse G. catenatum cysts (8 cysts/g), present only to a depth of 7 cm (surface mixed layer depth), reflecting an apparent recent range expansion of this dinoflagellate in New Zealand, possibly stimulated by unusual climatic conditions associated with the 2000 La Nina event. The significant increases since the early 1980s also of Protoperidinium cysts at Hokianga Harbour and of Gonyaulax, Protoperidinium and Protoceratium cysts at Manukau Harbour suggest a broad scale environmental change has occurred in Northland, New Zealand. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia; Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia; Australian Nucl Sci & Technol Org, Menai, NSW 2234, Australia	University of Tasmania; University of Tasmania; Australian Nuclear Science & Technology Organisation	Univ Tasmania, Sch Plant Sci, GPO Box 252-55, Hobart, Tas 7001, Australia.	hallegraeff@utas.edu.au	Heijnis, Hendrik/A-6673-2010; McMinn, Andrew/A-9910-2008; Hallegraeff, Gustaaf/C-8351-2013; Harrison, Jennifer/G-4238-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343; Heijnis, Hendrik/0000-0002-7601-3452; Harrison, Jennifer/0000-0003-0716-2398				ANDERSON DM, 1988, J PHYCOL, V24, P255; BALDWIN RL, 1990, SYSTEMS THEORY APPL, P1; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; 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, 2002, 10 INT C HARM AL, P32; BRUGAM RB, 1978, QUATERNARY RES, V9, P349, DOI 10.1016/0033-5894(78)90038-8; CHANG FH, 2001, P MAR BIOTK WORKSH W, P165; 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; Goff JR, 1998, NEW ZEAL J MAR FRESH, V32, P181, DOI 10.1080/00288330.1998.9516818; 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; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; Holmes MJ, 2002, J PHYCOL, V38, P96, DOI 10.1046/j.1529-8817.2002.01153.x; Ikeda T., 1989, P411; Mackenzie L, 2001, GYMNODINIUM CATENATU, P1; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; McMinn A., 2001, P HARMF ALG BLOOMS 2, P477; MCMINN A, 1997, MAR ECOL PROGR SER, V161, P163; RHODES LL, 1993, NEW ZEAL J MAR FRESH, V27, P419, DOI 10.1080/00288330.1993.9516583; TAYLOR MD, 2001, DELIMITATION STUDY T, P1; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; TODD K, 1999, P REP 1 C HARMF ALG; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1	27	28	31	0	11	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAR	2003	2	1					61	74	PII S1568-9883(02)00084-7	10.1016/S1568-9883(02)00084-7	http://dx.doi.org/10.1016/S1568-9883(02)00084-7			14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	812UM					2025-03-11	WOS:000220864400006
J	Haya, K; Martin, JL; Robinson, SMC; Martin, JD; Khots, A				Haya, K; Martin, JL; Robinson, SMC; Martin, JD; Khots, A			Does uptake of <i>Alexandrium fundyense</i> cysts contribute to the levels of PSP toxin found in the sea scallop, <i>Placopecten magellanicus</i>?	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Placopecten magellanicus; PSP toxin	DINOFLAGELLATE GONYAULAX-EXCAVATA; PARALYTIC SHELLFISH POISON; BAY	Atlantic sea scallops, Placopecten magellanicus, in most areas of the Bay of Fundy, New Brunswick, Canada, have year-round concentrations of paralytic shellfish posioning (PSP) toxins greater than the regulatory concentration of 80 mug STXeq. 100g(-1) wetweight. Scallops (mean shell height of 10.7cm, age 3-5 years) were collected by SCUBA and individually tagged near Parker Island, Bay of Fundy. Half were hung 2 in below the low tide water level and the remainder were placed on the bottom (11 m depth at low tide) under the scallops held at 2 in. Scallop, water and sediment samples were collected monthly for determination of concentrations of PSP toxins and Alexandrium fundyense. In October, 1993, mean concentrations of PSP toxins in digestive gland, and mantle were 3205 and 1018 mug STX eq. 100 g(-1) wet weight, respectively. Eight months later (June 1994), PSP concentrations in digestive glands from the surface and bottom had declined to 504 and 682 mug STX eq. 100 g(-1) wet weight, respectively, whereas those in the mantle had declined to 802 and 681 mug STX eq. 100 g(-1) wet weight. During July 1994, A. fundyense concentrations observed at Parker Island and offshore were 320 cells l(-1) and 14,200 cells l(-1), respectively. Subsequently, toxin concentrations in surface and bottom scallop digestive glands increased to 12,720 and 11,408 mug STX eq. 100 g(-1) wet weight, whereas concentrations in mantles increased to 2126 and 1748 mug STX eq. 100 g(-1) wet weight, respectively. Concentrations of PSP toxins in these tissues in October 1994 were similar to those measured in October 1993. Concentrations of PSP toxin were less than the regulatory concentration in the gonads and non-detectable in adductor muscles of all scallops sampled. There were no statistically significant differences in profiles for uptake and depuration of PSP toxins in scallops held at the surface compared to those from bottom, suggesting that A. fundyense cysts at the concentrations found in the sediment (45 cysts cm(-3)) did not contribute significantly to the year-round presence of PSP toxins within scallop tissues. The year-round occurrence of PSP toxin is probably due to accumulation during summer blooms followed by a very slow rate of depuration. Crown Copyright (C) 2002 Published by Elsevier Science B.V All rights reserved.	Fisheries & Oceans Canada, Canada Biol Stn, St Andrews, NB E5B 2L9, Canada	Fisheries & Oceans Canada	Haya, K (通讯作者)，Fisheries & Oceans Canada, Canada Biol Stn, 531 Brand Cove Rd, St Andrews, NB E5B 2L9, Canada.	hayak@mar.dfo-mpo.gc.ca	Martin, Jennifer/G-5217-2011	Robinson, Shawn/0000-0002-1705-7930				ANDERSON DM, 1984, ACS SYM SER, V262, P125; *AOAC, 1990, OFF METH AN, P881; BOURNE N, 1965, J FISH RES BOARD CAN, V22, P1137, DOI 10.1139/f65-102; Bricelj V. Monica, 1998, Reviews in Fisheries Science, V6, P315, DOI 10.1080/10641269891314294; CEMBELLA AD, 1993, J SHELLFISH RES, V12, P389; JAMIESON GS, 1983, CAN J FISH AQUAT SCI, V40, P313, DOI 10.1139/f83-046; Martin J.L., 1994, P 4 CAN WORKSH HARMF, V2016, P22; MARTIN JL, 1988, CAN J FISH AQUAT SCI, V45, P1968, DOI 10.1139/f88-229; MARTIN JL, 2001, P 7 CAN WORKSH HARM, P100; MARTIN JL, 1999, PHYTOPLANKTON MONITO, P132; MEDCOF JC, 1947, B FISH RES BD CAN, V75, P32; ROBINSON SMC, 1999, P 6 CAN WORKSH HARM, P87; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Sommer H, 1937, ARCH PATHOL, V24, P560; Trites R.W., 1983, Marine and Coastal Systems of the Quoddy Region, New Brunswick, P9; Waiwood B.A., 1995, P525; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156	17	12	15	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAR	2003	2	1					75	81	PII S1568-9883(02)00068-9	10.1016/S1568-9883(02)00068-9	http://dx.doi.org/10.1016/S1568-9883(02)00068-9			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	812UM					2025-03-11	WOS:000220864400007
J	Pearce, MA; Jarvis, I; Swan, ARH; Murphy, AM; Tocher, BA; Edmunds, WM				Pearce, MA; Jarvis, I; Swan, ARH; Murphy, AM; Tocher, BA; Edmunds, WM			Integrating palynological and geochemical data in a new approach to palaeoecological studies: Upper Cretaceous of the Banterwick Barn Chalk borehole, Berkshire, UK	MARINE MICROPALEONTOLOGY			English	Review						Late Cretaceous; Turonian; Coniacian; Chalk; dinoflagellate cysts; geochemistry; chemostratigraphy; stable isotopes; palaeoenvironments	CENOMANIAN-TURONIAN BOUNDARY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CARBON-ISOTOPE; SOUTHERN ENGLAND; MARINE-SEDIMENTS; NORTH PACIFIC; PARIS BASIN; SEA-LEVEL; STRATIGRAPHY; PALEOPRODUCTIVITY	The dinoflagellate cyst record from an Upper Cretaceous (uppermost Cenomanian-upper Coniacian) Chalk core, drilled at Banterwick Barn, Berkshire, is described and statistically correlated with elemental and stable isotope bulk sediment geochemical data from the same core. Seventy-two dinocyst species and subspecies are recorded, and stable carbon and oxygen isotopic (delta(13)C, delta(18)O) trends are documented. Lithostratigraphy and chemostratigraphic correlation of the delta(13)C curve with an expanded section at Dover, Kent, are used to identify stratigraphically significant marls, and determine the positions of macrofossil zones and stage boundaries in the Banterwick Barn core. These data indicate that > 30 m of chalk at Dover are represented by < 2 m of Chalk Rock at Banterwick Barn, with much of the succession being absent due to erosion and non-deposition. First and last appearance datums (FAD, LAD), first and last common occurrences, and acmes of key Turonian-Coniacian dinocyst species are documented and compared with other records from the Anglo-Paris Basin. A new subspecies, Senoniasphaera rotundata alveolata is proposed, which has a FAD in the lower Turonian and last appears (LAD) in the lower Coniacian. Senoniasphaera rotundata rotundata [autonym, herein] has its FAD in the middle Turonian, first common occurrence in the uppermost Turonian, and LAD in the upper Coniacian. An extremely impoverished assemblage of dinocysts in the highest Cenomanian to lowest Turonian is considered to be largely a preservational artefact of intraclastic nodular and calcarenitic chalks, and is not related directly to the well-documented global oceanic anoxic event (OAE2) occurring at that time (similar to 93.5 Ma). A sharp increase in dinocyst abundance in the lower Turonian corresponds with a change in lithology to more marly chalks. A gradual decrease in the number of species is observed through the middle Turonian to upper Coniacian; delta(18)O records show that this was associated with global climatic cooling. Cluster analysis of the dinocyst abundance record with geochemical data indicates four distinct species groups with characteristic geochemical associations, i.e. Groups 1-4. Groups 1 and 2 are associated with phases of increased siliciclastic supply; a positive correlation with higher VC values differentiates the latter. Group 3 is independent of carbonate and detrital input, and Group 4 is associated with high carbonate flux and low detrital supply. These groupings suggest that cyst-forming dinoflagellates exhibited a range of ecological niches in the Late Cretaceous. Although the relationship between the encystment process and the geochemical associations is unclear, key environmental factors are likely to be sea-level and climate related, including water depth, turbidity, nutrient supply, sea-surface temperature, and environmental stability/predictability. Integrated geochemical and palynological studies have great potential for inter-regional correlation and palaeoenvironmental interpretation. (C) 2002 Elsevier Science B.V. All rights reserved.	Millennia Ltd, Unit 3, Alton GU34 2PJ, Hants, England; Kingston Univ, Ctr Earth & Environm Sci Res, Sch Earth Sci & Geog, Kingston upon Thames KT1 2EE, Surrey, England; STATOIL, N-4035 Stavanger, Norway; British Geol Survey, Hydrogeol Grp, Wallingford OX10 8BB, Oxon, England	Kingston University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Pearce, MA (通讯作者)，Millennia Ltd, Unit 3, Weyside Pk,Newman Lane, Alton GU34 2PJ, Hants, England.	martin.pearce@millennialimited.com	Jarvis, Ian/A-1637-2008	Jarvis, Ian/0000-0003-3184-3097; Pearce, Martin/0000-0001-7856-1076				Abreu V.S., 1998, SOC EC PALEONTOLOGIS, V60, P75, DOI [DOI 10.2110/PEC.98.02.0075, DOI 10.2110/PEC.98.02.0075.ALBERTA]; ANDERSON TF, 1983, SHORT COURSE; Aurisano R.W., 1989, Palynology, V13, P143; AZEMA C, 1981, REV PALAEOBOT PALYNO, V35, P237, DOI 10.1016/0034-6667(81)90111-1; BATTEN DJ, 1991, GEOL JB, V12, P105; Batten DJ., 1988, The Chalk District of the Euregio Meuse-Rhine, P95; BELOW R, 1996, ANN MUSEI CIVICI R S, V11, P231; BRIDEAUX WW, 1971, PALAEOGEOGR PALAEOCL, V9, P101, DOI 10.1016/0031-0182(71)90035-6; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Bromley R.G., 1982, Cretaceous Research, V3, P273, DOI DOI 10.1016/0195-6671(82)90030-1; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Chatwin CP, 1908, P GEOL ASS, V20, P390, DOI [10.1016/S0016-7878(08)80289-1, DOI 10.1016/S0016-7878(08)80289-1]; Clarke LJ, 1999, GEOLOGY, V27, P699, DOI 10.1130/0091-7613(1999)027<0699:NOIEFL>2.3.CO;2; Clarke R. 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R. H., 1995, INTRO GEOLOGICAL DAT; SWEENEY BM, 1987, BOT MONOGRAPHS; Taylor F.J.R., 1987, BOT MONOGRAPHS; Tocher B.A., 1987, P138; Tocher BA, 1996, J MICROPALAEONTOL, V15, P55, DOI 10.1144/jm.15.1.55; Tocher BA, 1995, J MICROPALAEONTOL, V14, P97, DOI 10.1144/jm.14.2.97; TOCHER BA, 1984, THESIS CITY LONDON P; TOCHER BA, 1994, B INF GEOL BASSIN PA, V13, P13; Voigt S, 1997, PALAEOGEOGR PALAEOCL, V134, P39, DOI 10.1016/S0031-0182(96)00156-3; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	106	76	80	1	11	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	MAR	2003	47	3-4					271	306	PII S0377-8398(02)00132-9	10.1016/S0377-8398(02)00132-9	http://dx.doi.org/10.1016/S0377-8398(02)00132-9			36	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	656UQ					2025-03-11	WOS:000181627600004
J	Ellegaard, M; Daugbjerg, N; Rochon, A; Lewis, J; Harding, I				Ellegaard, M; Daugbjerg, N; Rochon, A; Lewis, J; Harding, I			Morphological and LSU rDNA sequence variation within the <i>Gonyaulax spinifera-Spiniferites</i> group (Dinophyceae) and proposal of <i>G-elongata</i> comb. nov and <i>G-membranacea</i> comb. nov.	PHYCOLOGIA			English	Article							CYST-THECA RELATIONSHIPS; SUBUNIT RIBOSOMAL-RNA; DINOFLAGELLATE CYSTS; ADJACENT SEAS; SEDIMENTS; PHYLOGENY; GENERA; NORTH	Cultures were established from cysts of the cyst-based taxa Spiniferites elongatus and S. membranaceus. Motile cells and cysts from both cultures and sediment samples were examined using light and scanning electron microscopy. The cyst-theca relationship was established for S. elongatus. The motile cells have the tabulation pattern 2 pr, 4', 6", 6c, greater than or equal to 4s, 6"', 1p, 1'''', but they remain unattributable to previously described Gonyaulax species. There was large variation in process length and process morphology in cysts from both cultures and wild samples and there was variation in ornamentation and in the development of spines and flanges in motile cells. A new combination, G. elongata (Reid) Ellegaard et al. comb. nov. is proposed, following new rules of the International Code of Botanical Nomenclature that give genera based on extant forms priority over genera based on fossil forms. Extreme morphological variation in the cyst and motile stages of S. membranaceus is described and this species is also transferred to the genus Gonyaulax, as G. membranacea (Rossignol) Ellegaard et al. comb. nov. Approximately 1500 bp of large subunit (LSU) rDNA were determined for these two species and for G. baltica, G. cf. spinifera (= S. ramosus) and G. digitalis (= Bitectatodinium tepikiense). LSU rDNA showed sequence divergences similar to those estimated between species in other genera within the Gonyaulacales; a phylogeny for the Gonyaulacales was established, including novel LSU rDNA sequences for Alexandrium margalefii, A. pseudogonyaulax and Pyrodinium bahamense var. compressum. Our results show that motile stages obtained from the germination of several cysts of the 'fossil-based' Spiniferites and B. tepikiense, which were previously attributed to 'Gonyaulax spinifera group undifferentiated', belong to distinct species of the genus Gonyaulax. These species show small morphological differences in the motile stage but relatively high sequence divergence. Moreover, this group of species is monophyletic, supported by bootstrap values of 100% in parsimony and maximum likelihood analyses.	Univ Copenhagen, Inst Bot, Dept Phycol, DK-1353 Copenhagen K, Denmark; Univ Westminster, Sch Biosci, Phytosci Res Grp, London W1W 6UW, England; Univ Copenhagen, Inst Bot, Dept Phycol, DK-1353 Copenhagen K, Denmark; Univ Southampton, Sch Earth & Ocean Sci, Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England	University of Copenhagen; University of Westminster; University of Copenhagen; NERC National Oceanography Centre; University of Southampton	Ellegaard, M (通讯作者)，Univ Copenhagen, Inst Bot, Dept Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.		Harding, Ian/K-3320-2012; Ellegaard, Marianne/H-6748-2014; Daugbjerg, Niels/D-3521-2014	Harding, Ian/0000-0003-4281-0581; Daugbjerg, Niels/0000-0002-0397-3073				[Anonymous], P YORKSHIRE GEOL SOC; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; DALE B, 1978, Palynology, V2, P187; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; DAUGBJERG N, 1994, J PHYCOL, V30, P991, DOI 10.1111/j.0022-3646.1994.00991.x; Doyle JJ., 1987, PHYTOCHEM B BOT SOC, V19, P11, DOI DOI 10.1016/0031-9422(80)85004-7; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Faure-Fremiet E., 1908, ANN SCI NAT ZOOL, V9, p[209, 15]; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; Fensome R.A., 1993, CLASSIFICATION FOSSI; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Greuter W., 2000, INT CODE BOT NOMENCL; Guillard RRL., 1973, HDB PHYCOLOGICAL MET, P69; Hallett RI, 1999, THESIS U WESTMINSTER; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; HANSEN G, 1993, PHYCOLOGIA, V32, P73, DOI 10.2216/i0031-8884-32-1-73.1; HARLAND R, 1986, Palynology, V10, P25; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HARLAND R, 1982, Palynology, V6, P9; HARLAND R, 1980, Grana, V19, P211; Head M.J., 1996, Palynology: Principles and Applications, P1197; KOFOID C.A., 1911, U CALIFORNIA PUBLICA, V8, P187; LENAERS G, 1989, J MOL EVOL, V29, P40, DOI 10.1007/BF02106180; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; Lewis J, 1999, GRANA, V38, P113, DOI 10.1080/00173139908559220; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Matsuoka K., 1987, Bull. 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Sci., V28, P35; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Reid P.C., 1974, Nova Hedwigia, V25, P579; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SWOFFORD DL, 1998, PAUPASTERISK PHYLOGE; 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; WILLIAMS GL, 1998, CONTRIBUTION SERIES, V34; WILLIAMS GL, 2000, CONTRIBUTION SERIES, V37; Wuyts J, 2001, NUCLEIC ACIDS RES, V29, P175, DOI 10.1093/nar/29.1.175	44	69	75	0	21	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAR	2003	42	2					151	164		10.2216/i0031-8884-42-2-151.1	http://dx.doi.org/10.2216/i0031-8884-42-2-151.1			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	675DC					2025-03-11	WOS:000182676900005
J	Montresor, M; Lovejoy, C; Orsini, L; Procaccini, G; Roy, S				Montresor, M; Lovejoy, C; Orsini, L; Procaccini, G; Roy, S			Bipolar distribution of the cyst-forming dinoflagellate <i>Polarella glacialis</i>	POLAR BIOLOGY			English	Article							SEA-ICE; PFIESTERIA-PISCICIDA; MOLECULAR EVOLUTION; GENETIC-VARIATION; ELLIS FJORD; PHYLOGENY; SYMBIODINIUM; PHYTOPLANKTON; FORAMINIFERA; ANTARCTICA	Morphological investigations of motile cells and cysts of a small dinoflagellate (strain CCMP 2088) isolated from Canadian Arctic waters were carried out under both light and scanning electron microscopy. This species strongly resembled Polarella glacialis (strain CCMP 1383), which up to now was known only from Antarctic sea ice. The photosynthetic pigment composition of strain CCMP 2088 is typical of dinoflagellates, with peridinin as a major accessory pigment. Phylogenetic relationships between the two strains and other dinoflagellate species were inferred from SSU nrDNA using Neighbour Joining and weighted parsimony analyses. Our results showed that strain CCMP 2088 and P. glacialis (strain CCMP 1383) grouped in the same clade (Suessiales clade), showing high similarity values (0.99%). Morphological and molecular data support the assignment of the Arctic strain to P. glacialis. The free-living Gymnodinium simplex and the two P. glacialis strains have a basal position in the Suessiales clade, as compared to Symbiodinium spp.	Staz Zool Anton Dohrn, I-80121 Naples, Italy; Univ Laval, GIROQ, Quebec City, PQ G1K 7P4, Canada; Univ Quebec, Inst Sci Mer Rimouski & Quebec Ocean, Rimouski, PQ G5L 3A1, Canada	Stazione Zoologica Anton Dohrn; Laval University; University of Quebec	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@szn.it	Orsini, Luisa/B-6773-2009; Procaccini, Gabriele/AAA-7040-2019; Procaccini, Gabriele/A-6618-2010; Lovejoy, Connie/A-3756-2008	Procaccini, Gabriele/0000-0002-6179-468X; Orsini, Luisa/0000-0002-1716-5624; Montresor, Marina/0000-0002-2475-1787; Lovejoy, Connie/0000-0001-8027-2281				Aagaard K., 1994, POLAR OCEANS THEIR R, P5; Bjornland T., 1997, PHYTOPLANKTON PIGMEN, P578; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; Carlos AA, 1999, J PHYCOL, V35, P1054, DOI 10.1046/j.1529-8817.1999.3551054.x; CRAME JA, 1993, J BIOGEOGR, V20, P145, DOI 10.2307/2845668; Darius HT, 2000, J PHYCOL, V36, P951, DOI 10.1046/j.1529-8817.2000.99088.x; Darling KF, 2000, NATURE, V405, P43, DOI 10.1038/35011002; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; DODGE JD, 1974, J MAR BIOL ASSOC UK, V54, P171, DOI 10.1017/S0025315400022141; FENSOME R. 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MAR	2003	26	3					186	194		10.1007/s00300-002-0473-9	http://dx.doi.org/10.1007/s00300-002-0473-9			9	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	657PT					2025-03-11	WOS:000181676100007
J	Miller, TR; Belas, R				Miller, TR; Belas, R			<i>Pfiesteria piscicida</i>, <i>P-shumwayae</i>, and other <i>Pfiesteria</i>-like dinoflagellates	RESEARCH IN MICROBIOLOGY			English	Review						Pfiesteria piscicida; Pfiesteria shumwayae; harmful algae; toxin; life stages; detection; microbial community structure	TOXIC ESTUARINE DINOFLAGELLATE; NITROGEN UPTAKE; FISH KILLS; LIFE-CYCLE; DINOPHYCEAE; COMPLEX; IDENTIFICATION; BEHAVIOR; RECEPTOR; CULTURE	Pfiesteria piscicida and Pfiesteria shumwayae are estuarine dinoflagellates thought to be responsible for massive fish deaths and associated human illnesses in the southeastern United States. These dinoflagellates are described as having a complex life cycle involving flagellated zoospores, cysts, and amoeboid stages. Although no Pfiesteria toxin has been identified, certain strains of these dinoflagellates are thought to produce a water-soluble toxin that can kill fish and cause human illness. Recent reports show no evidence for amoeboid stages and indicate that a much more-simplified life cycle exists. In addition, researchers have shown that P. shumwayae only kills fish through direct contact that does not necessarily involve the production of one or more toxins. This review summarizes these and other recent findings with an emphasis on establishing basic facts regarding the toxicity and life history of Pfiesteria dinoflagellates. (C) 2002 Editions scientifiques et medicales Elsevier SAS. All rights reserved.	Univ Maryland, Inst Biotechnol, Ctr Marine Biotechnol, Baltimore, MD 21202 USA	University System of Maryland; University of Maryland Baltimore	Univ Maryland, Inst Biotechnol, Ctr Marine Biotechnol, 701 E Pratt St, Baltimore, MD 21202 USA.	belas@umbi.umd.edu	Miller, Todd/Y-3612-2019	Miller, Todd/0000-0002-2113-1662	NIEHS NIH HHS [P01-ES9563] Funding Source: Medline	NIEHS NIH HHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS))		Berg GM, 1997, MAR BIOL, V129, P377, DOI 10.1007/s002270050178; Berry JP, 2002, P NATL ACAD SCI USA, V99, P10970, DOI 10.1073/pnas.172221699; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; 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, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; 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; Coats DW, 1999, J EUKARYOT MICROBIOL, V46, P402, DOI 10.1111/j.1550-7408.1999.tb04620.x; Fairey ER, 1999, NAT TOXINS, V7, P415, DOI 10.1002/1522-7189(199911/12)7:6<415::AID-NT81>3.0.CO;2-E; Glasgow HB, 2000, ECOL APPL, V10, P1024, DOI 10.1890/1051-0761(2000)010[1024:WQTAMI]2.0.CO;2; Glasgow HB, 2001, PHYCOLOGIA, V40, P234, DOI 10.2216/i0031-8884-40-3-234.1; Glasgow HB, 2001, ENVIRON HEALTH PERSP, V109, P715, DOI 10.2307/3454919; GLASGOW HB, 1995, J TOXICOL ENV HEALTH, V46, P501, DOI 10.1080/15287399509532051; Kaiser J, 2002, SCIENCE, V298, P346, DOI 10.1126/science.298.5592.346; Kimm-Brinson KL, 2001, ENVIRON HEALTH PERSP, V109, P457, DOI 10.2307/3454703; Lewitus AJ, 1999, J PHYCOL, V35, P303, DOI 10.1046/j.1529-8817.1999.3520303.x; Lewitus AJ, 1999, J PHYCOL, V35, P1430, DOI 10.1046/j.1529-8817.1999.3561430.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; Marshall HG, 2000, J EXP MAR BIOL ECOL, V255, P51, DOI 10.1016/S0022-0981(00)00288-4; Moe CL, 2001, ENVIRON HEALTH PERSP, V109, P781, DOI 10.2307/3454927; Moeller PDR, 2001, ENVIRON HEALTH PERSP, V109, P739, DOI 10.2307/3454921; NOGA EJ, 1993, VET REC, V133, P96, DOI 10.1136/vr.133.4.96; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; Rublee P. A., 1999, Virginia Journal of Science, V50, P325; Rublee PA, 2001, ENVIRON HEALTH PERSP, V109, P765, DOI 10.2307/3454924; Shoemaker RC, 2001, ENVIRON HEALTH PERSP, V109, P539, DOI 10.2307/3454715; SONNENBERG JL, 1989, J NEUROSCI RES, V24, P72, DOI 10.1002/jnr.490240111; 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; VERMA IM, 1987, ADV CANCER RES, V49, P29, DOI 10.1016/S0065-230X(08)60793-9; Vogelbein WK, 2002, NATURE, V418, P967, DOI 10.1038/nature01008	33	15	17	4	16	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0923-2508	1769-7123		RES MICROBIOL	Res. Microbiol.	MAR	2003	154	2					85	90		10.1016/S0923-2508(03)00027-5	http://dx.doi.org/10.1016/S0923-2508(03)00027-5			6	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	667YA	12648722	Bronze			2025-03-11	WOS:000182261400003
J	Iakovleva, AI; Kulkova, IA				Iakovleva, AI; Kulkova, IA			Paleocene-Eocene dinoflagellate zonation of Western Siberia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						biostratigraphy; dinoflagellate cysts; late Paleocene-Eocene; Western Siberia	STRATIGRAPHY	This paper presents a new Paleocene-Eocene dinoflagellate zonation of Western Siberia. Twelve dinoflagellate zones are recognised in the Western Siberian lithological formations and are compared with the corresponding zones in NW Europe and the former Soviet Union. The interpretation of the age of these zones permits stratigraphical age determinations to be made for the Western Siberian regional lithological formations. The absence in the northern West Siberian sections of equivalents of the NW European Lutetian dinoflagellate zones suggests an interruption in marine sedimentation during this part of the middle Eocene. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Montpellier 2, UMR CNRS 5554, ISEM, Lab Paleoenvironm & Palynol, F-34095 Montpellier, France; Russian Acad Sci, Inst Geol, Paleoflorist Lab, Moscow 109017, Russia; Russian Acad Sci, Palynol Lab, Associated Inst Geol Geophys & Mineral, Novosibirsk 630090, Russia	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Sobolev Institute of Geology & Mineralogy of the Russian Academy of Sciences	Univ Nacl Autonoma Mexico, Inst Geol, Delegac Coyoacan, Mexico City 04510, DF, Mexico.	iakovl@yahoo.com	IAKOVLEVA, ALINA/ABH-9243-2020					Akhmet'ev MA, 2001, STRATIGR GEO CORREL+, V9, P373; ALESKEROVA ZT, 1956, ABSTRACTS INTERDEPAR; Andreeva-Grigorovich AS., 1991, THESIS GEOLOGICAL I; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; [Anonymous], 1984, ENV LIFE TURN EPOCHS; BERGGREN WA, 1995, SOC EC PALEONTOL MIN, V54; Berggren WA, 1994, GFF, V116, P44, DOI 10.1080/11035899409546145; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Caro Y., 1973, Revista Esp Micropaleont, V5, P329; Cavelier C., 1983, GEOL FRANCE, V3, P261; Chateauneuf J.-J., 1978, Bulletin du Bureau de Recherches Geologiques et Minieres Paris Section 4 Geologie Generale, V1978, P59; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; EREMEEVA AE, 1956, INT C CONC SYNTH STR; GLEZER ZI, 1974, FOSSIL MODERN DIATOM, P109; Harrison JC, 1999, B CAN PETROL GEOL, V47, P223; HEILMANNCLAUSEN C, 1985, GEOL SURV DEN PAP SE, V7; Iakovleva A.I., 2001, Revista Espanola de Micropaleontologia, V33, P1; Iakovleva AI, 2000, NEWSL STRATIGR, V38, P13, DOI 10.1127/nos/38/2000/13; IAKOVLEVA AI, 2000, THESIS U MONTPELLIER; Iakovleva Alina I., 2000, Palynology, V24, P187, DOI 10.2113/0240187; ILYINA VI, 1994, OIGGIM T, V818; KULKOVA I. A., 1990, GEOL GEOFIZ, V1, P25; KULKOVA IA, 1988, PLANT MICROFOSSILS S, P25; 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; MUDGE DC, 1994, MAR PETROL GEOL, V11, P166, DOI 10.1016/0264-8172(94)90093-0; Mudge DC, 1996, MAR PETROL GEOL, V13, P295, DOI 10.1016/0264-8172(95)00066-6; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Powell A.J., 1992, P155; ROSTOVTSEV NN, 1955, SBORNIK VSEGEI, V2, P3; Schmitz B, 1994, GFF, V116, P39, DOI 10.1080/11035899409546141; Shatskii S.B, 1984, ENV LIFE BOUNDARIES, P9; Shatsky S.B., 1969, PROBLEMS STRATIGRAPH, P156; Shatsky S.B., 1978, PALEOGEN NEOGEN SIBI, P3; SHATSKY SB, 1975, THESIS SNIGIMS NOVOS; SIGOV AP, 1956, INT C CONC SYNTH STR, P25; VASILIEVA ON, 1990, PALYNOLOGY STRAIGRAP; Vozzhennikova T.F., 1967, FOSSIL PERIDINEAE JU; VOZZHENNIKOVA TF, 1960, P I GEOL GEOPHYS SIB, V1, P7; VOZZHENNIKOVA TF, 1963, FUNDAMENTALS PALEONT, P171; ZAPOROZHETS NI, 1991, IZV AKAD NAUK KAZAKH, V6, P37	43	22	24	0	3	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	2003	123	3-4					185	197	PII S0034-6667(02)00117-3	10.1016/S0034-6667(02)00117-3	http://dx.doi.org/10.1016/S0034-6667(02)00117-3			13	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	664GJ					2025-03-11	WOS:000182053100001
J	Schrank, E				Schrank, E			Small acritarchs from the Upper Cretaceous: taxonomy, biological affinities and palaeoecology	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						acritarchs; dinoflagellates; palaeoecology; Cretaceous; Egypt	DINOFLAGELLATE; CLASSIFICATION; NETHERLANDS; SEDIMENTS; ESTONIA; USA	A systematic study of small acritarchs (most commonly around 10 gm) from the Late Campanian (Duwi (Phosphate) Formation) and Maastrichtian (Dakhla Shale) of Egypt, based on scanning electron miscroscopy, resulted in the identification of nine genera and 27 species, among them the new genus Recticystis and 14 new species, namely Operculites bigranulatus, Bacillidinium partitum, Mecsekia acuta, M. curvispina, M. triangula, Recticystis hemispinosus, Clavaticystis septatus, C. furcatus, Odontothrix multiornatus, Filisphaeridium paucigranulosum, Cymatiosphaera parvirugosa, C muralis, C. polyornata and C. triradiata. In addition, the following new combinations are proposed: Cymatiosphaera coronis (Habib and Knapp), Mecsekia minor (Takahashi) and Mecsekia ariakense (Takahashi). Small acritarchs are thought to include cysts of dinoflagellates because of significant morphological similarities (cyst shape, chasmic and tremic archeopyles, spinose arid septate ornaments) to certain organic-walled and calcareous dinoflagellate cysts. Small size in acritarchs is regarded as an adaptation to a planktonic and possibly to an interstitial mode of life. Small acritarchs attain the highest diversity and abundance in the well agitated environment of the phosphoritic sandstones. In the pores between the sand grains they, were: protected from the wave action and currents which moved away most of the larger dinoflagellates.. Dinoflagellates are common in the associated shales representing a more quiet marine environment. The interpretation of some small spinulose acritarchs as interstitial dinoflagellates may also be supported by the presence of spinose cysts with a chasmic archeopyle in the modern dinoflagellate Polykrikos which includes interstitial forms. (C) 2003 Elsevier Science B.V. All rights reserved.	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, Sekt EB 10,Ernst Reuter Pl 1, D-10587 Berlin, Germany.							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Palaeobot. Palynology	MAR	2003	123	3-4					199	235	PII S0034-6667(02)00228-2	10.1016/S0034-6667(02)00228-2	http://dx.doi.org/10.1016/S0034-6667(02)00228-2			37	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	664GJ					2025-03-11	WOS:000182053100002
J	Masó, M; Garcés, E; Pagès, F; Camp, J				Masó, M; Garcés, E; Pagès, F; Camp, J			Drifting plastic debris as a potential vector for dispersing Harmful Algal Bloom (HAB) species	SCIENTIA MARINA			English	Article						dinoflagellates; Alexandrium; temporary cyst; HAB; plastic debris; Mediterranean	ALEXANDRIUM-TAYLORI DINOPHYCEAE; TRANSPORT; LIFE; SEA	Macroscopic observations of floating plastic debris collected at several places along the Catalan coast (northwestern Mediterranean) showed conspicuous green-yellow patches adhered to them. The microscopic examination of these patches showed that they were constituted mainly of benthic diatoms and small flagellates (<20 mum). Potential harmful dinoflagellates such as Ostreopsis sp. and Coolia sp., resting cysts of unidentified dinoflagellates and both temporary cysts and vegetative cells of Alexandrium taylori were also found. Plastic debris is considered to be one of the most serious problems affecting the marine environment. We suggest drifting plastic debris as a potential vector for microalgae dispersal.	CSIC, Inst Ciencies Mar, CMIMA, 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)	Masó, M (通讯作者)，CSIC, Inst Ciencies Mar, CMIMA, Passeig Maritim Barceloneta 37-49, E-08003 Barcelona, Spain.		Garces, Esther/C-5701-2011	Garces, Esther/0000-0002-2712-501X; Camp, Jordi/0000-0002-5202-9783				BALECH E, 1994, T AM MICROSC SOC, V113, P216, DOI 10.2307/3226651; Barnes DKA, 2002, NATURE, V416, P808, DOI 10.1038/416808a; BESADA EG, 1982, B MAR SCI, V32, P723; BOMBER JW, 1988, B MAR SCI, V43, P204; DOUGLAS AW, 1987, MAR POLL B, V18, P303; Faust MA, 1996, J EXP MAR BIOL ECOL, V197, P159; FLO E, 2001, UNPUB RESIDUS SOLIDS; GABRIELIDES GP, 1991, MAR POLL B, V13, P437; GALGANI F, 1995, MAR POLLUT BULL, V30, P713, DOI 10.1016/0025-326X(95)00055-R; 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; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Laabir M, 1999, J SHELLFISH RES, V18, P217; Minchin D, 1996, MAR POLLUT BULL, V32, P855, DOI 10.1016/S0025-326X(96)00045-8; MORRIS RJ, 1980, MAR POLLUT BULL, V11, P125, DOI 10.1016/0025-326X(80)90073-9; Nehring S, 1998, ARCH FISH MAR RES, V46, P181; PRUTER AT, 1987, MAR POLLUT BULL, V18, P305, DOI 10.1016/S0025-326X(87)80016-4; SCHOLIN CA, 1996, PHYSL ECOLOGY HARMFU, V41, P13; WINSTON JE, 1982, MAR POLLUT BULL, V13, P348, DOI 10.1016/0025-326X(82)90038-8	19	230	265	5	136	INST CIENCIAS MAR BARCELONA	BARCELONA	PG MARITIM DE LA BARCELONETA, 37-49, 08003 BARCELONA, SPAIN	0214-8358			SCI MAR	Sci. Mar.	MAR	2003	67	1					107	111		10.3989/scimar.2003.67n1107	http://dx.doi.org/10.3989/scimar.2003.67n1107			5	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	654UR		Green Submitted, gold			2025-03-11	WOS:000181514900012
J	Lim, DI; Park, YA				Lim, DI; Park, YA			Late quaternary stratigraphy and evolution of a Korean tidal flat, haenam bay, southeastern yellow sea, Korea	MARINE GEOLOGY			English	Article						late Quaternary stratigraphy; Korean tidal flat; last interglacial; oxidized layer; regional unconformity; southeastern Yellow Sea	DINOFLAGELLATE CYSTS; WEST-COAST; CLAY; PLEISTOCENE; SEDIMENTS; DEPOSITS; LEVEL	Sediment cores from a tidal flat in the southeastern Yellow Sea, Korea, contain two major depositional units, a Holocene unit (Unit I) and an underlying late Pleistocene unit (Unit II). Unit I (up to 15 m thick) is a middle to late Holocene, coarsening-upward transgressive deposit. Unit II (about 10 m thick) is interpreted as tidal-flat deposits from the last interglacial period (probably oxygen-isotope stage 5e), based on its many tide-influenced signatures such as laminated silt/clay, tidal rhythmites, fossil crab burrows, authigenic minerals (pyrite and halite), clay mineral composition and a dinoflagellate cyst assemblage comparable to that of Unit I. Units I and II are separated by a regional unconformity which is highlighted by a yellow 'oxidized layer' in uppermost Unit II. The layer contains abundant evidence of subaerial exposure, including a yellowish sediment color, semi-consolidation, desiccation cracks, cryoturbation structures, and high degree of magnetic susceptibility. Two major interglacial highstands (Units I and II) and one glacial lowstand (uppermost oxidized layer of Unit II) thus characterize coastal to nearshore tidal deposits along the eastern margin of the Yellow Sea (western Korea). (C) 2002 Elsevier Science B.V. All rights reserved.	Korea Ocean Res & Dev Inst, Marine Environm & Climate Change Lab, Seoul 425600, South Korea; Seoul Natl Univ, Res Inst Oceanog, Seoul 151742, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Seoul National University (SNU)	Lim, DI (通讯作者)，Korea Ocean Res & Dev Inst, Marine Environm & Climate Change Lab, Ansan,POB 29, Seoul 425600, South Korea.		Lim, Dhongil/ACH-3964-2022	Lim, Dhongil/0000-0002-0832-2907				AN ZS, 1990, QUATERN INT, V8, P91; BISCAYE PE, 1965, GEOL SOC AM BULL, V76, P803, DOI 10.1130/0016-7606(1965)76[803:MASORD]2.0.CO;2; BOUCHARD M, 1995, GEOMORPHOLOGY, V12, P75, DOI 10.1016/0169-555X(94)00078-6; Butrym J., 1964, Folia Quat, V17, P1; Byun H., 1995, Unpublished Ph.D. Thesis; CANN JH, 1988, QUATERNARY RES, V29, P153, DOI 10.1016/0033-5894(88)90058-0; CHAPPELL J, 1986, NATURE, V324, P137, DOI 10.1038/324137a0; Chappell J, 1996, EARTH PLANET SC LETT, V141, P227, DOI 10.1016/0012-821X(96)00062-3; Choi KS, 2001, J SEDIMENT RES, V71, P680, DOI 10.1306/2DC4095F-0E47-11D7-8643000102C1865D; CHOI KS, 2001, THESIS SEOUL NATL U; CHOUGH SK, 1983, MARINE GEOLOGY KOREA; Chun J.H., 2000, J GEOLOGICAL SOC KOR, V36, P517; CHUN JH, 1995, J GEOLOGICAL SOC KOR, V31, P546; Folk R. 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Geol.	FEB 15	2003	193	3-4					177	194		10.1016/S0025-3227(02)00663-1	http://dx.doi.org/10.1016/S0025-3227(02)00663-1			18	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	651AF					2025-03-11	WOS:000181296600002
J	Barrón, E; Azerêdo, AC				Barrón, E; Azerêdo, AC			Palynology of the Jurassic (Callovian-Oxfordian) succession from Pedrogao (Lusitanian Basin, Portugal).: Palaeoecological and palaeobiogeographical aspects	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							DINOFLAGELLATE CYSTS	A palynological study of the Jurassic deposits front the Pedrogao section allowed the identification of 53 taxa belonging to different protoctist groups, vascular cryptogams, gymnosperms and anthophytes. The analysis of the palynological associations after grouping the taxa according to the denominated Sporo-morph Ecogroup Model allowed the reconstruction of the type of vegetation which grew in the zone. It was composed of Cheirolepidiaceae and Araucariaceae typical of coastal environments, and communities of vascular cryptogams and gyrymosperms characteristic of dry and marshy areas. The climate was dry subtropical. The diversity and evenness values reflect marine influence in the basal and topmost deposits of the succession. The palynoflora is in accordance with the palaeoclimatic characteristics inferred for the Middle and Late Jurassic of Portugal by VAKHRAMEEV (1991), but the obtained data only partially corroborate the palaeoecological interpretations made by this author.	Univ Complutense Madrid, Fac Ciencias Geol, Dept Paleontol, E-28040 Madrid, Spain; Univ Lisbon, Fac Ciencias, Dept & Ctr Geol, P-1749016 Lisbon, Portugal	Complutense University of Madrid; Universidade de Lisboa	Barrón, E (通讯作者)，Univ Complutense Madrid, Fac Ciencias Geol, Dept Paleontol, Ciudad Univ S-N, E-28040 Madrid, Spain.		Barrón, Eduardo/L-4726-2014; Azeredo, Ana/B-6325-2013	Azeredo, Ana/0000-0002-1244-4843; Barron, Eduardo/0000-0003-4979-1117				Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; Almeras Y., 1991, Memorias e Noticias Publicacoes do Museu e Laboratorio Mineralogico e Geologico da Universidade de Coimbra, V112, P239; [Anonymous], 2007, Paleopalynology; Azeredo A.C., 1998, CUADERNOS GEOLOG A I, V24, P99; AZEREDO AC, 2000, PASSAGEM JURASSICO M; AZEREDO AC, IN PRESS SEDIMENTOLO; AZEREDO AC, 1993, THESIS U LISBOA; Barron E., 1999, Temas Geologico-Mineros, Instituto Tecnologico Geominero de Espana, V26, P186; BEERBOWER J R, 1969, Journal of Paleontology, V43, P1184; BOLAND DC, 1986, THESIS MEMORIAL U NE; Boulter M., 1993, Special Papers in Palaeontology, V49, P125; Cabral Maria Cristina, 2002, Geodiversitas, V24, P61; CABRAL MC, 1999, PAL ASS WORKSH LISB, P21; CABRAL MC, 1998, COMMUNICACOES I GEOL, V84, P74; CASTRO L, 1996, THESIS U LISBOA; Colin JP, 2000, MICROPALEONTOLOGY, V46, P123, DOI 10.2113/46.2.123; Duarte L.V., 1995, THESIS U COIMBRA; El Beialy Salah Y., 1997, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V204, P379; El-Shamma A., 1997, N JB GEOL PALAONT AB, V206, P133; FAUCONNIER D, 1997, BULL CENT RECH ELF E, V17, P225; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; GrambastFessard N., 1985, Revue de Micropaleontologie, V28, P58; Guy D.J.E., 1971, PUBLICATIONS I MINER, V168, P1; Guy-Ohlson D., 1986, JURASSIC PALYNOLOGY; LUND J J, 1985, Bulletin of the Geological Society of Denmark, V33, P371; MAGURRAN E, 1991, ECOLOGICAL DIVERSITY; Mohr B.A.R., 1989, Berliner Geowissenschaftliche Abhandlungen. 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Geologie und Palaontologie, V106, P291; Mohr B.A.R., 1988, Neus Jahrbuch fur Geologie und Palaontologie Abhandlungen, V176, P245; Mouterde R., 1979, Ciencias da Terra, V5, P29; PAIS J, 1974, Boletim da Sociedade Geologica de Portugal, V19, P19; Pais J., 1976, INTRO PALEOBOTANICA; PEREIRA R, 1999, EUR PAL ASS WORKSH L, P84; Pereira R., 1998, COMUN I GEOL MINEIRO, V84, pA79; Pocock S., 1962, PALAEONTOGRAPHICA, V111, P1; Pocock S.A.J., 1970, PALAEONTOGRAPHICA, V130, P12; Ramalho M.M., 1971, COMUNICACOES SERVICO, V55, P133; Ramalho MM., 1971, Mem Serv Geol Portugal, V19, P1; Ramalho MM., 1981, Comunicacoes dos Servicos Geologicos de Portugal, V67, P41; RAMALHO MM, 1970, ETOL SOC GEOL PORTUG, V17, P123; RIBEIRO A., 1979, Introduction a la Geologie Generale du Portugal; Riley L.A., 1974, BIRBAL SAHNI I PALEO, V3, P33; Ruget-Perrot C., 1961, Memorias dos Servicos Geologicos de Portugal, nova serie, V7, P1; SCHULZ E, 1967, PALAEONTOGR ABH B, V112, P427; Smelror M., 1991, Revista Espanola de Micropaleontologia, V23, P47; STANCLIFFE RPW, 1990, MICROPALEONTOLOGY, V36, P197, DOI 10.2307/1485506; Thusu B., 1985, Journal of Micropalaeontology, V4, P113; Vakhrameev V.A., 1991, JURASSIC CRETACEOUS; van Erve A., 1988, N JB GEOL PAL ONT MH, V4, P246, DOI [10.1127/njgpm/1988/1988/246, DOI 10.1127/NJGPM/1988/1988/246]; van Erve A.W., 1988, Journal of Micropalaeontology, V7, P217; VINK A, 1995, THESIS UTRECHT U; 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; WIJLAARS AMF, 1995, THESIS UTRECHT U; Williams G.L., 1985, P847; Wilson R.C., 1979, Ciencias da Terra (Universidade Nova de Lisboa), V5, P53; Wright V.P., 1985, Palaeoalgology: Contemporary Research and Applications, P330, DOI [10.1007/978-3-642-70355-3_27, DOI 10.1007/978-3-642-70355-3_27]	56	17	18	0	4	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	FEB	2003	227	2					259	286						28	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	664VZ					2025-03-11	WOS:000182085000005
J	Derby, ML; Galliano, M; Krzanowski, JJ; Martin, DF				Derby, ML; Galliano, M; Krzanowski, JJ; Martin, DF			Studies of the effect of Ψ-APONIN from <i>Nannochloris</i> sp on the Florida red tide organism <i>Karenia brevis</i>	TOXICON			English	Article						red tide; brevetoxin; microtox analyzer; Karenia brevis; Nannochloris sp.		Studies were conducted on the conditions under which the red tide organism, Karenia brevis (a.k.a., Gymnodinium? breve), was treated with Nannochloris sp. The latter organism is known to produce cytolytic agents called Apparent Oceanic Naturally Occurring Cytolin (APONINs). Conventional wisdom might suggest that brevetoxins would be released upon destruction of the single-celled dinoflagellate K. brevis and that efforts to treat red tide outbreaks would lead to release of brevetoxins and enhanced toxicity toward marine species. Earlier studies described conditions by which K. brevis cells were converted to a nonmotile form when cultures of K. brevis were treated with an isolate (Psi-APONIN) produced by Nannochloris sp. but when centrifuged only a small amount of the toxin was released. The present study confirms that the toxin is not released when the K. brevis is undisturbed, however, when the culture is stressed (stirred with a magnetic stirring bar for 24, 48, and 72 h) toxin was released, and the toxicity could be measured using a Microtox analyzer. In the study, it was found that at as few as eighty cells of K. brevis produced a toxic effect of 20% as measured by the effect on Vibrio fischeri. Nannochloris sp. had no effect on the bacteria used in the Microtox analyzer, nor did interaction of Nannochloris sp. with K. brevis in the short term. This effect is presumed to be due to the production of Psi-APONIN and conversion of K. brevis to a non-motile or resting form. (C) 2002 Elsevier Science Ltd. All rights reserved.	Univ S Florida, Dept Chem, Inst Environm Studies, Tampa, FL 33620 USA; Univ S Florida, Coll Med, Dept Pharmacol & Therapeut, Tampa, FL 33620 USA	State University System of Florida; University of South Florida; State University System of Florida; University of South Florida	Martin, DF (通讯作者)，Univ S Florida, Dept Chem, Inst Environm Studies, SCA 400,4202 E Fowler Ave, Tampa, FL 33620 USA.							Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; BADEN DG, 1989, FASEB J, V3, P1807, DOI 10.1096/fasebj.3.7.2565840; Brydon G A, 1971, Environ Lett, V1, P235; DEMAJID LP, 1983, MICROBIOS LETT, V22, P59; DERBY ML, 2002, THESIS U S FLORIDA T; DOIG MT, 1974, THESIS U S FLORIDA T; ENG-WILMOT D L, 1981, Microbios Letters, V17, P109; ENGWILMOT DL, 1979, J PHARM SCI-US, V68, P963, DOI 10.1002/jps.2600680812; Harvell CD, 1999, SCIENCE, V285, P1505, DOI 10.1126/science.285.5433.1505; Hemmert W.H., 1975, Proceedings of the First International Conference on Toxic Dinoflagellate Blooms, P489; Martin Dean F., 1998, Florida Scientist, V61, P10; MARTIN DF, 1976, J ENVIRON SCI HEAL A, V11, P385, DOI 10.1080/10934527609385780; MARTIN DF, 1973, TRACE METALS METAL O, pCH12; MARTIN DF, 1975, P 1 INT C TOX DIN BL, P287; MCCOY LF, 1977, CHEM-BIOL INTERACT, V17, P17, DOI 10.1016/0009-2797(77)90068-0; MOON R E, 1981, Microbios Letters, V18, P103; MOON RE, 1984, ACS SYM SER, V268, P381; Pérez E, 1997, BIOMED LETT, V56, P7; PEREZ E, 1999, THESIS U S FLORIDA T; ROUNSEFELL GA, 1966, 35 US FISH WILD SERV; SHIMODA T, 1988, J ALLERGY CLIN IMMUN, V81, P1187, DOI 10.1016/0091-6749(88)90889-5; Steidinger K A, 1973, CRC Crit Rev Microbiol, V3, P49, DOI 10.3109/10408417309108745; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; STEIDINGER KA, 1999, HARMFUL MICROALGAE A; TAFT WH, 1986, J ENVIRON SCI HEAL A, V21, P107, DOI 10.1080/10934528609375279; 1999, USER MANUAL MICROOMN	26	7	9	1	8	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0041-0101			TOXICON	Toxicon	FEB	2003	41	2					245	249	PII S0041-0101(02)00285-4	10.1016/S0041-0101(02)00285-4	http://dx.doi.org/10.1016/S0041-0101(02)00285-4			5	Pharmacology & Pharmacy; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Toxicology	643VG	12565744				2025-03-11	WOS:000180881400015
J	Zhang, Q; Gradinger, R; Zhou, QS				Zhang, Q; Gradinger, R; Zhou, QS			Competition within the marine microalgae over the polar dark period in the Greenland Sea of high Arctic	ACTA OCEANOLOGICA SINICA			English	Article						competition; marine microalgae; dark; the Greenland Sea; Arctic	DIATOM MORTALITY; ICE MICROALGAE; LIPID-CONTENT; COMMUNITIES; SURVIVAL; PHYSIOLOGY; GROWTH; ALGAE; LIGHT; BLOOM	With the onset of winter, polar marine microalgae would have faced total darkness for a period of up to 6 months. A natural autumn community of Arctic sea ice microalgae was collected for dark survival experiments from the Greenland Sea during the ARKTIS-X1/2 Expedition of RV Polarstern in October 1995. After a dark period of 161 days, species dominance in the algal assemblage have changed from initially pennate diatoms to small phytoflagellates ( < 20 mu m). Over the entire dark period, the mean algal growth rate was - 0. 01 d(-1). Nearly all diatom species had negative growth rates, while phytoflagellate abundance increased. Resting spore formation during the dark period was observed in less than 4.5% of all cells and only for dinoflagellates and the diatom Chaetoceros spp. We assume that facultative heterotrophy and energy storage are the main processes enabling survival during the dark Arctic winter. After an increase in light intensity, microalgal cells reacted with fast growth within days. Phytoflagellates had the highest growth rate, followed by Nitzschia frigida - Further investigations and experiments should focus on the mechanisms of dark survival (mixotrophy and energy storage) of polar marine microalgae.	State Ocean Adm, Lab Ocean Dynam Proc & Satellite Oceanog, Hangzhou 310012, Peoples R China; State Ocean Adm, Inst Oceanog 2, Hangzhou 310012, Peoples R China; Univ Alaska, Inst Marine Sci, Fairbanks, AK 99775 USA	Ministry of Natural Resources of the People's Republic of China; Second Institute of Oceanography, Ministry of Natural Resources; University of Alaska System; University of Alaska Fairbanks	Zhang, Q (通讯作者)，State Ocean Adm, Lab Ocean Dynam Proc & Satellite Oceanog, Hangzhou 310012, Peoples R China.	zhangqing@sio.zj.edu.cn	Gradinger, Rolf/E-4965-2015	Gradinger, Rolf/0000-0001-6035-3957				ALLEN MB, 1970, R701 U AL I MAR SCI; ALLEN MB, 1971, ANNU REV ECOL SYST, P261; ANDERSSON A, 1989, MICROB ECOL, V17, P251, DOI 10.1007/BF02012838; Arrigo KR, 1997, SCIENCE, V276, P394, DOI 10.1126/science.276.5311.394; BARRETT SM, 1995, J PHYCOL, V31, P360, DOI 10.1111/j.0022-3646.1995.00360.x; BUNT JS, 1972, LIMNOL OCEANOGR, V17, P458, DOI 10.4319/lo.1972.17.3.0458; Cota G.F., 1991, Journal of Marine Systems, V2, P279, DOI DOI 10.1016/0924-7963(91)90037-U; FAHL K, 1993, POLAR BIOL, V13, P405, DOI 10.1007/BF01681982; FRYXELL GA, 1994, MEMOIRS CALIFORNIA A, V17, P437; GOSSELIN M, 1990, J PHYCOL, V26, P220, DOI 10.1111/j.0022-3646.1990.00220.x; GRADINGER R, 1991, POLAR RES, V10, P295, DOI 10.1111/j.1751-8369.1991.tb00655.x; *HELCOM, 1988, BALTIC MARINE PROT C; Horner R., 1985, P83; HORNER R, 1972, LIMNOL OCEANOGR, V17, P454, DOI 10.4319/lo.1972.17.3.0454; Ikavalko J, 1997, POLAR BIOL, V17, P473, DOI 10.1007/s003000050145; KUOSA H, 1992, POLAR BIOL, V12, P333; LEGENDRE L, 1992, POLAR BIOL, V12, P429; MATHEKE GEM, 1974, J FISH RES BOARD CAN, V31, P1779, DOI 10.1139/f74-226; MCKENZIE CH, 1995, J PHYCOL, V31, P19, DOI 10.1111/j.0022-3646.1995.00019.x; MEDLIN LK, 1990, BRIT ANTARCTIC SURVE; NICHOLS PD, 1988, J PHYCOL, V24, P90; Palmisano A.C., 1985, P131; PALMISANO AC, 1982, J PHYCOL, V18, P489; PALMISANO AC, 1983, CAN J MICROBIOL, V29, P157, DOI 10.1139/m83-026; PALMISANO AC, 1987, MAR ECOL PROG SER, V35, P165, DOI 10.3354/meps035165; Peters E, 1996, J EXP MAR BIOL ECOL, V207, P25, DOI 10.1016/S0022-0981(96)02520-8; Peters E, 1996, J PLANKTON RES, V18, P953, DOI 10.1093/plankt/18.6.953; SMITH REH, 1993, MAR ECOL PROG SER, V97, P19, DOI 10.3354/meps097019; Smith W.O., 1990, POLAR OCEANOGRAPHY, P477, DOI 10.1016/C2009-0-21623-0; SPINDLER M, 1990, NATO ADV SCI I C-MAT, V308, P173; SYVERTSEN EE, 1991, POLAR RES, V10, P277, DOI 10.1111/j.1751-8369.1991.tb00653.x; WHITE AW, 1974, J PHYCOL, V10, P292	32	16	20	1	35	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	0253-505X			ACTA OCEANOL SIN	Acta Oceanol. Sin.		2003	22	2					233	242						10	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	710RU					2025-03-11	WOS:000184694300008
J	Lan, DZ; Li, C; Fang, Q; Gu, HF				Lan, DZ; Li, C; Fang, Q; Gu, HF			Preliminary study on taxonomy of dinoflagellate cysts from major estuary and bays of Fujian Province, China	ACTA OCEANOLOGICA SINICA			English	Article						Fujian Province; sediment; dinoflagellate resting cysts; taxonomy	TOXIC DINOFLAGELLATE; ALEXANDRIUM; SEDIMENTS	According to the morphology, wall structure, color, ornamentation, etc., 25 species belonging to 9 genera are identified and described from 144 sediment samples of the Xiamen Harbor, the mouth of the Minjiang River and the Sansha Bay. Among them there are 2 toxic species: Alexandrium minutun,A. tamarenes, 4 harmful species: Alexandrium affine,Lingulodinium polX drum, Scrippsiella trochoide,Gonyaulax spinifera. It shows that 11 species of dinoflagellate cysts (Alexandrium affine, A. minutum, Diplopelta cf. parva, Polykrikos cf. schwartzii, protoceratium reticulatum, Protoperidinium minutum, P. cf. minutum, P. cf americanum and Alexandrium sp., Protoperidinium sp. 1, P. sp. 2) are first recorded along the coast of Fujian Province, China. These newly discovered species might be transported to the coastal sea of Fujian Province by ballast water of international trade vessels.	State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China; Xiamen Univ, Inst Subtrop Oceanog, Dept Oceanog, Xiamen 361005, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Xiamen University	State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China.		Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171				Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Anderson D.M., 1984, Seafood toxins, P125; Anderson DM, 1996, TOXICON, V34, P579, DOI 10.1016/0041-0101(95)00158-1; [Anonymous], 2000, Ecol. Sci.; 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 CY, 2001, J EXP MAR BIOL ECOL, V262, P211, DOI 10.1016/S0022-0981(01)00291-X; CHEN JR, 2002, XIAMEN EVENING  0528; Chen Ju-fang, 2000, Marine Environmental Science, V19, P20; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; DAVID W, 2001, CONTINENTAL SHELF RE, V21, P347; Doblin MA, 2000, J PLANKTON RES, V22, P421, DOI 10.1093/plankt/22.3.421; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; Ishikawa Akira, 1993, Bulletin of Plankton Society of Japan, V40, P1; JEROEN CJM, 2002, MAR POLICY, V26, P59; KARIN AF, 2001, PROGR OCEANOGRAPHY, V48, P25; Lin J.M., 1988, MARINE ENV SCI, V7, P22; LIN JM, 1995, BIODIVERSITY, V3, P187; Marshall HG, 2000, J EXP MAR BIOL ECOL, V255, P51, DOI 10.1016/S0022-0981(00)00288-4; MATINA A, 2000, J PLANKTON RES, V22, P421; Matsuoka K., 2000, Technical guide for modern dinoflagellate cyst study, P1; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Qi Yuzao, 1991, Journal of Jinan University, V12, P92; SHI YB, 1992, P MAR ENV WORKSH; Sierra-Beltrán AP, 1998, TOXICON, V36, P1493, DOI 10.1016/S0041-0101(98)00139-1; WANG WF, 1994, MARINE SCI B, V13, P53; Zheng Lei, 1995, Journal of Jinan University, V16, P121	29	0	1	1	14	SPRINGER	NEW YORK	ONE NEW YORK PLAZA, SUITE 4600, NEW YORK, NY, UNITED STATES	0253-505X	1869-1099		ACTA OCEANOL SIN	Acta Oceanol. Sin.		2003	22	3					395	406						12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	731JN					2025-03-11	WOS:000185880700006
J	Gu, HF; Fang, Q; Sun, J; Lan, DZ; Cai, F; Gao, ZY				Gu, HF; Fang, Q; Sun, J; Lan, DZ; Cai, F; Gao, ZY			Dinoflagellate cysts in recent marine sediment from Guangxi, China	ACTA OCEANOLOGICA SINICA			English	Article						dinoflagellate cysts; surface sediment; Guangxi	GONYAULAX-EXCAVATA	Total of 33 species of dinoflagellate cysts were discovered from surface sediment in the sea region of Guangxi, among them 12 cyst types (Diplopsalopsis sp. 1, D. sp. 2, D. sp. 3, Cochlodinium sp., Protoperidinium sp. 1, P. sp. 2, P. compressum, Scrippsiella sp. 1, S. sp. 2, Alexandrium sp. 1, A. sp. 2, A. sp. 3) were first reported from the South China Sea. And one cyst type (Cochlodinium sp.) was first reported in the world. Scrippsiella trochoidea is the dominant species in this area, accounting for 45% of all the cysts. There are 2 cysts of toxic dinoflagellate (Alexandrium tamarensis and Gymnodinium catenatum) But there is no relationship between cyst number and grain size distribution.	State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China; Ocean Univ China, Coll Marine Life Sci, Qingdao 266003, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Ocean University of China	Gu, HF (通讯作者)，State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China.		Sun, Jun/A-5254-2009; Gu, Haifeng/ADN-4528-2022	Sun, Jun/0000-0001-7369-7871; Gu, Haifeng/0000-0002-2350-9171				ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; FUKUYO Y, 1982, REPORTS ENV SCI B, P205; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Imai K, 2001, BMC PSYCHIATRY, V1, DOI 10.1186/1471-244X-1-1; Ishikawa Akira, 1993, Bulletin of Plankton Society of Japan, V40, P1; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Matsuoka K., 1989, P461; MATSUOKA K, 1982, REPORTS ENV SCI B, V148, P197; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1987, GUIDE STUDIES RED TI, P399; MONTRESOR M, 1988, PHYCOLOGIA, V27, P387, DOI 10.2216/i0031-8884-27-3-387.1; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Reid P.C., 1974, Nova Hedwigia, V25, P579; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Zheng L., 1997, J TROP SUBTROP BOT, V5, P10	22	4	8	0	8	CHINA OCEAN PRESS	BEIJING	INTERNATIONAL DEPT, 8 DA HUI SHI, BEIJING 100081, PEOPLES R CHINA	0253-505X			ACTA OCEANOL SIN	Acta Oceanol. Sin.		2003	22	3					407	419						13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	731JN					2025-03-11	WOS:000185880700007
J	Band-Schmidt, CJ; Lechuga-Devéze, CH; Kulis, DM; Anderson, DM				Band-Schmidt, CJ; Lechuga-Devéze, CH; Kulis, DM; Anderson, DM			Culture studies of <i>Alexandrium affine</i> (Dinophyceae), a non-toxic cyst forming dinoflagellate from Bahia Concepcion, Gulf of California	BOTANICA MARINA			English	Article							GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; LIFE-HISTORY; GERMINATION; GROWTH; POPULATION; SEXUALITY	Alexandrium affine (Inoue et Fukuyo) Balech, isolated from Bahia Concepcion (Gulf of California), was studied to determine the effect of environmental factors on cyst germination and vegetative growth. Alexandrium affine was homothallic and isogamous, and formed cysts in nutrient-deficient (N- or P-limiting) medium. The maturation period of newly formed cysts varied between two weeks and three months, depending on the storage temperature, with colder temperatures prolonging the process. The rate of germination increased with increasing temperature, and was not significantly influenced by light. Germination experiments suggest a broad temperature window for A. affine cysts, ranging from 5 to 25degreesC. The optimal vegetative growth rates were 0.25 to 0.34 day(-1) at 20-30degreesC. No vegetative growth was observed below 15degreesC or above 35degreesC. With HPLC toxin analyses, we confirm that this species does not produce saxitoxins. These data on the dormancy, excystment, and growth characteristics seem to be regulated by the environmental constraints of this subtropical bay.	CIBNOR, La Paz 23000, BCS, Mexico; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Woods Hole Oceanographic Institution	CIBNOR, Apdo Postal 128, La Paz 23000, BCS, Mexico.	cband@cibnor.mx	anderson, david/E-6416-2011	Band-Schmidt, Christine Johanna/0000-0002-8251-9820				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, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; 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; [Anonymous], 1997, ADV MAR BIOL; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; BRAVO I, 1986, Investigacion Pesquera (Barcelona), V50, P313; Bustillos-Guzmán J, 2000, J EXP MAR BIOL ECOL, V249, P77, DOI 10.1016/S0022-0981(00)00188-X; CANNON JA, 1993, DEV MAR BIO, V3, P103; Dale B., 1983, P69; DRESSLER R, 1981, PRELIMINARY KNOWLEDG, P1; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; Flynn K, 1996, MAR BIOL, V126, P9, DOI 10.1007/BF00571372; FRAGA S, 1993, DEV MAR BIO, V3, P59; FRGA S, 1989, RED TIDES BIOL ENV S, P281; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Fukuyo Y., 1985, P27; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; GONGORAGONZALEZ D, 2001, THESIS U AUTONOMA BA; GRATELIZARRAGA I, 2001, PHYSICOCHEMICAL CHAR, P56; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kim H.-G., 1990, Bulletin of the Korean Fisheries Society, V23, P468; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; Lechuga-Devéze CH, 2000, ECOVIS WORLD MG SER, P245; Lechuga-Devéze CH, 2001, REV BIOL TROP, V49, P525; LEE GS, 1990, CHEM ENG J BIOCH ENG, V44, P1, DOI 10.1016/0300-9467(90)80049-I; LEINONENDUFRESN.E, 2000, 9 INT C HARMF ALG BL, P163; Mateo-Cid L.E., 1993, Ciencias Marinas, V19, P41; MORQUECHOESCAMI.ML, 2002, 12 REUN NAC SOC MEX, P93; Oshima Y., 1995, MANUAL HARMFUL MARIN, P81; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, 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; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SHUMILIN E, 1996, ACTAS INAGEQ, V2, P79; SIDABUTAR T, 2000, 9 INT C HARMF ALG BL, P220; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; VERA G, 1999, 105 IMARPE, P12; WAGEY GA, 2000, 9 INT C HARMF ALG BL, P243; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; Yoshida M., 2000, 9 INT C HARMF ALG BL, P248	47	27	31	0	13	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055	1437-4323		BOT MAR	Bot. Marina	JAN	2003	46	1					44	54		10.1515/BOT.2003.007	http://dx.doi.org/10.1515/BOT.2003.007			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	653UE					2025-03-11	WOS:000181454800006
J	Cho, HJ; Kim, CH; Moon, CH; Matsuoka, K				Cho, HJ; Kim, CH; Moon, CH; Matsuoka, K			Dinoflagellate cysts in recent sediments from the southern coastal waters of Korea	BOTANICA MARINA			English	Article						dinoflagellate cysts; morphology; southern coastal waters of Korea	RECENT MARINE-SEDIMENTS; AUSTRALIA	Thirtyseven different types of dinoflagellate cysts were recorded in surface sediments, sampled at offshore and inshore stations from the southern coastal waters of Korea. Because of their atypical morphologies, Votadinium calvum, Quinquecuspis concretum, Protoperidinium sp. and two types of Brigantedinium are described and discussed in more detail. The concentrations of dinoflagellate cysts were approximately four times higher at offshore stations than those at inshore stations. This study provides a database on dinoflagellate cyst distribution and composition in the southern coastal waters of Korea, where dinoflagellate cysts have been little studied.	Cheju Natl Univ, Marine & Environm Res Inst, Jocheon Eup 695814, Jeju, South Korea; Pukyong Natl Univ, Dept Aquaculture, Pusan 608737, South Korea; Pukyong Natl Univ, Dept Oceanog, Pusan 608737, South Korea; Nagasaki Univ, Fac Fisheries, Nagasaki 8528521, Japan	Jeju National University; Pukyong National University; Pukyong National University; Nagasaki University	Cho, HJ (通讯作者)，Cheju Natl Univ, Marine & Environm Res Inst, 3288 Hamdeok Ri, Jocheon Eup 695814, Jeju, South 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; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; 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; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Ishikawa Akira, 2000, Plankton Biology and Ecology, V47, P12; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; Lee J.B., 1994, P 2 INT S MAR SCI EX, P1; Lee Joon-Baek, 1998, Journal of Fisheries Science and Technology, V1, P283; Matsuoka K, 1999, E CHINA SEA, P195; Matsuoka K., 1987, Bull. Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; Matsuoka Kazumi, 1999, Fossils (Tokyo), V66, P1; McMinn Andrew, 1992, Palynology, V16, P13; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Park J.S., 1990, Bull. Korean Fish. Soc, V23, P208; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	21	13	15	2	11	WALTER DE GRUYTER & CO	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055			BOT MAR	Bot. Marina		2003	46	4					332	337		10.1515/BOT.2003.030	http://dx.doi.org/10.1515/BOT.2003.030			6	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	698FE					2025-03-11	WOS:000183986700002
J	Bucur, II; Senowbari-Daryan, B; Majidifard, MR				Bucur, II; Senowbari-Daryan, B; Majidifard, MR			Neocomian microfossil association from the taft area near Yazd (central Iran)	FACIES			English	Article						algae; systematic paleontology; central Iran; Cretaceous	ALGAE	An assemblage of microfossils, including calcareous green algae (dasycladaleans: Deloffrella quercifoliipora, Bakalovaella elitzae, Salpingoporella cf. muehlbergii, Terquemella sp., Neomeris sp., and Cylindroporella? sp.; Halimedaceans/Gymnocodiaceans: Boueina sp. Perinocalculus aff. minutus), red algae (Solenoporaceans?: Marinella lugeoni), cysts of dinoflagellates? (Cadosina fusca fusca, Colomisphaera aff. conferta) and foraminifers (Torinosuella peneropliformis, Charentia cuvillieri, Commaliama sp.) is described from the carbonate beds within the terrigenous-carbonate Sangestan Formation (Upper Jurassic - Neocomian) exposed near the small village of Zereshk, approximately 63 km SW of Yazd, central Iran. The micropaleontological assemblage indicates a late Neocomian (Hauterivian) age of the carbonate beds.	Univ Babes Bolyai, Dept Geol, R-3400 Cluj Napoca, Romania; Univ Erlangen Nurnberg, Inst Paleontol, D-91054 Erlangen, Germany; Geol Survey Iran, Tehran, Iran	Babes Bolyai University from Cluj; University of Erlangen Nuremberg	Bucur, II (通讯作者)，Univ Babes Bolyai, Dept Geol, M Kogalniceanu Str 1, R-3400 Cluj Napoca, Romania.		Bucur, Ioan/B-7064-2011					BAKALOVA D., 1971, Bulletin of the Geological Institute, Bulgarian Academy of Sciences-Committee of Geology (Series Paleontology), V20, P123; Barattolo F, 1985, B SOC NATUR NAPOLI, V93, P1; BORZA K, 1986, Acta Geologica Hungarica, V29, P133; BUCUR I.I., 1994, Beitrage zur Palaontologie, Wien, V19, P13; BUCUR I.I., 1999, Spec. Pub., V2, P53; BUCUR I.I., 2001, ALGAE CARBONATE PLAT, P137; BUCUR II, 1993, REV ESP MICROPALEONT, V15, P93; Bucur II, 2002, ACTA PALAEONTOLOGICA, V3, P41; Bucur Ioan I., 2000, Revue de Paleobiologie, V19, P435; FARRES F, 1977, ANN MINES GEOLOGIE, V28, P239; GRANIER B, 1992, J AFR EARTH SCI, V14, P239, DOI 10.1016/0899-5362(92)90101-H; GRANIER B, 1987, B SOC GEOL FRANCE, V8, P1089; Granier B., 1993, Revue de Paleobiologie, Geneve, V12, P19; Granier B., 1986, MEDITERR NEA SER GEO, V5, P5; JEROTIJEVICPOLA.S, 1998, B GEOINSTITUT, V35, P229; Leinfelder R.R., 1986, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V7, P1; MAJIDIFARD MR, 1996, GEOSCIENCES GEOL SUR, V5, P2; Masse J.-P., 1995, Proceedings of the Ocean Drilling Program, Scientific Results, V144, P221; Masse P, 1995, B CENT RECH EXPL, V19, P301; Maync W., 1959, Eclogae Geologicae Helvetiae, V52, P5; Misik M., 1990, KNIHOVNICKA ZEMNIHO, V9, P25; PARTOWAZAR H, 1981, UNPUB MESOZOIC PALEO; PFENDER J, 1939, B LAB GEOL GEOGRAPH, V66, P1; Radoicic R, 1980, B ACAD SERBE SCI SNM, V20, P109; REHANEK J, 1985, Vestnik Ustredniho Ustavu Geologickeho, V60, P171; TEHRANI KK, 1981, GEOSCIENCES GEOL SUR, V7; YABE H, 1926, JAPAN SEC SERV GEOL, V9	27	18	19	0	2	INSTITUT PALAONTOLOGIE UNIVERSITAT ERLANGEN-NURNBERG	ERLANGEN	LOEWENICHSTRABE 20, D-91054 ERLANGEN, GERMANY	0172-9179			FACIES	Facies		2003	48						217	222		10.1007/BF02667540	http://dx.doi.org/10.1007/BF02667540			6	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	680QU		Bronze			2025-03-11	WOS:000182989500015
J	Kuz'mina, OB; Volkova, VS; Gnibidenko, ZN; Lebedeva, NK				Kuz'mina, OB; Volkova, VS; Gnibidenko, ZN; Lebedeva, NK			Microphytofossils and magnetostratigraphy of Upper Cretaceous and Cenozoic deposits of the southeastern West Siberian Plain	GEOLOGIYA I GEOFIZIKA			Russian	Article						palynology; dinoflagellates; spores; pollen; magnetostratigraphy; magnetozone; Upper Cretaceous; Cenozoic; Upper Ob' region; West Siberia		A combined palynological and paleomagnetic study of core samples of Upper Cretaceous and Cenozoic deposits from four boreholes drilled in the Upper Ob' region has been carried out with regard to the edition of the State Geological Map2000. Palynological and paleomagnetic descriptions have been performed according to four and one boreholes, respectively. Fourteen spore-and-pollen assemblages have been recognized in the deposits under study. They characterize the marine Eocene (Lyulinvor and Tavda Horizons), continental Paleogene (Allyin, Novomikhailovka, and Zhuravka Horizons), and Neogene (Abrosimovka, Beshcheul, Tavolzhan, and Pavlodar Horizons). Features of flora changes. at Cenozoic borderlines (Eocene- Oligocene, Oligocene-Miocene, and Middle-Late Miocene) and their stratigraphic significance are outlined. A paleomagnetic section has been compiled for borehole 10. It includes 19 major magnetozones of different polarities: nine in the Paleogene, eight in the Neogene, and two in the Quaternary. They correspond to the rank of orthozones, paleobotanically characterized and referred to the regional stratigraphic scheme. Some. of these orthozones are referred to the Berggren time scale. These data allowed subdivision of the Upper Cretaceous and Cenozoic deposits under consideration, estimation of the completeness of the section, rock dating, and refinement of the stratigraphic volume of the Upper Cretaceous, and Cenozoic formations and regional horizons exposed in the boreholes.	Russian Acad Sci, Geol Geophys & Mineral Joint Inst, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Kuz'mina, OB (通讯作者)，Russian Acad Sci, Geol Geophys & Mineral Joint Inst, Prosp Koptyuga 3, Novosibirsk 630090, Russia.		Kuzmina, Olga/I-9547-2018; Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303				[Anonymous], 2001, UNIFITSIROVANNYE REG; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Gnibidenko ZN, 1999, GEOL GEOFIZ, V40, P1808; GNIBIDENKO ZN, 2000, K GEOL SIB DALN VOST, P375; GNIBIDENKO ZN, 1991, 13 INT C INQUA, P114; GNIBIDENKO ZN, 1996, GEOL GEOFIZ, V37, P75; GNIBIDENKO ZN, 2001, PROBLEMS REGIONAL GE, P29; ILINA VI, 1994, MIKROFITOFOSSILII DE; KANYGIN AV, 1999, GEOLGOICHESKOE STROE, V1; Kulkova IA, 1997, GEOL GEOFIZ, V38, P581; Kuzmina, 2001, NOVOSTI PALEONTOLOGI, P135; KUZMINA OB, 2001, 2 MEZHD S EV ZHIZN Z, P364; Panova L. A., 1971, KAINOZOISKIE FLORY S, P40; POSEPLOVA GA, 1982, GEOFIZICHESKIE METOD, P76; Pospelova G. A., 1976, IZV AN SSSR GEOL, P19; Shatsky S.B., 1978, PALEOGEN NEOGEN SIBI, P3; VOLKOVA VS, 2002, GEOL GEOFIZ, P1017; Zaporozhets N.I., 1993, STRATIGR GEOL CORREL, V1, P128; 1996, GEOLOGICHESKIE BIO 1	19	18	27	0	1	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.		2003	44	4					348	363						16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	676TE					2025-03-11	WOS:000182767700008
J	Lebedeva, NK; Zverev, KV				Lebedeva, NK; Zverev, KV			Sedimentological and palynological analysis of the Cenomanian-Turonian event in northern Siberia	GEOLOGIYA I GEOFIZIKA			Russian	Article						sedimentology; palynology; paleogeography; Late Cretaceous; northern Siberia	STRATIGRAPHY; SECTIONS	,,Oceanic Anoxic Event" on the boundary of Cenomanian-Turonian (OAE2) is a bright episode in Cretaceous history. Results of the sedimentological and palynological researches of Cenomanian-Turonian of terrigenous deposits on the Lower Agapa River (Ust'-Yenisei region) are introduced. Sedimentological features of deposits and their facies relationships have been studied in detail. The rhythmicity of anoxic and normal-marine situations is revealed characteristic for ,,Black shale" facies. It is well expressed in shift of shallow marine sandy formations with benthonic faunas by black and dark gray fissile clays with pyrite, without macrofaunas, reflecting situations of stagnation. Qualitative and quantitative variations in structure of organic-wall microphytoplankton, dynamics of taxonomical diversity of dinoflagellate cysts are fixed depending on facies. The distribution of palynomorphs in Cenomanian-Turonian sediments in different locales is held.	Russian Acad Sci, Inst Petr & Gas Geo, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Lebedeva, NK (通讯作者)，Russian Acad Sci, Inst Petr & Gas Geo, Prosp Koptyuga 3, Novosibirsk 630090, Russia.		Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303				Batten D.J., 1991, GEOL JAHRB REIHE A, V120, P105; Elsik W.C., 1977, Palynology, V1, P95; EVITT WR, 1985, THEIR MORPHOLOGY INT; Fensome R.A., 1990, CONTRIBUTION SERIES, V25; Heckel P.H., 1972, RECOGNITION ANCIENT, P226, DOI DOI 10.2110/PEC.72.02.0226; ILINA VI, 1994, MIKROFITOFOSSILII DE; JARVIS I, 1988, Cretaceous Research, V9, P3, DOI 10.1016/0195-6671(88)90003-1; JENKYNS HC, 1980, J GEOL SOC LONDON, V137, P171, DOI 10.1144/gsjgs.137.2.0171; KHOMENTOVSKII OV, 1998, THESIS SO RAN NOVOSI; KRASILOV VA, 1985, MELOVOI PERIOD EVOLY; Li H, 1996, PALAIOS, V11, P15, DOI 10.2307/3515113; MARSHALL KL, 1988, REV PALAEOBOT PALYNO, V54, P85, DOI 10.1016/0034-6667(88)90006-1; MURDMAA IO, 1979, GEOLOGICHESKIE FORMA, P943; NAIDIN DP, 1986, PALEOGEOGRAFIYA PELE; POSAMENTIER HW, 1992, AAPG BULL, V76, P1687; Sachs V.N., 1957, T NIIGA, V90, P118; Sahagian D, 1996, AAPG BULL, V80, P1433; SCHLANGER SC, 1976, GEOL MIJNBOUW, P179; SCHLANGER SC, 1982, NTURE ORIGIN CRETACE; Tocher BA, 1995, J MICROPALAEONTOL, V14, P97, DOI 10.1144/jm.14.2.97; Zakharov V.A., 1989, GEOL GEOFIZ+, P10; ZAKHAROV VA, 1994, EKOSISTEMNYE PERESTR, P139; ZAKHAROV VA, 1993, PROBLEMY DOANTROPOGE, P25; ZAKHAROV VA, 1998, K AKT VOPROS GEOL GE, P210; ZAKHAROV VA, 1991, GEOL GEOFIZ, P9; 1991, 5 MEZHV REG STRAT SO	26	9	12	0	5	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.		2003	44	8					769	780						12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	729BX					2025-03-11	WOS:000185752100003
J	Zavada, MS				Zavada, MS			The ultrastructure of angiosperm pollen from the Lower Cenomanian of the Morondova Basin, Madagascar	GRANA			English	Article							PALEOMAGNETIC EVIDENCE; DIVERSITY	Samples collected from Cretaceous sediments of the Morondova Basin, southwest Madagascar yielded a palynoflora composed of spores of ferns and fern allies, pollen of gymnosperms and angiosperms, and dinoflagellates. In addition, a diverse fauna of ammonites was recovered along with the microflora. The species of dinoflagellates and ammonites suggest an Early Cenomanian age. Ninety-two percent of the microflora is comprised of fern spores and gymnosperm pollen. Approximately twenty species of angiosperm pollen comprise 3.6% of the flora, a majority of which are monosulcate and disulcate, including Clavatipollenites, Retimonocolpites, and Liliacidltes. Single occurrences of tricolpates and tricolporates are also recorded. The low abundance of angiosperms, and the taxonomic position of the angiosperm pollen are more reminiscent of Lower Cretaceous palynofloras from the Barremian-Albian. The low abundance of angiosperms and high diversity relative to the ferns and gymnosperms suggest that angiosperms arrived on Madagascar by long distance dispersal.	Providence Coll, Dept Biol, Providence, RI 02918 USA	Providence College	Providence Coll, Dept Biol, Providence, RI 02918 USA.							[Anonymous], 2007, Paleopalynology; Appert O., 1973, SCHWEIZ PALAONTOL AB, V94, P1; Barron E.J., 1981, ECLOGAE GEOL HELV, V74, P443; BARSS MS, 1973, 7326 GEOL SURV CAN D; Brenner Gilbert J., 1996, P91, DOI 10.1007/978-0-585-23095-5_5; Burden ET., 1989, AASP Contributions Series, V21; CHEN YY, 1978, THESIS U ARIZONA TUC; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; DARRACOTT BW, 1974, EARTH PLANET SC LETT, V24, P282, DOI 10.1016/0012-821X(74)90106-X; Dettmann M.E., 1992, Palaeobotanist, V41, P224; DETTMANN ME, 1990, REV PALAEOBOT PALYNO, V65, P131, DOI 10.1016/0034-6667(90)90064-P; EMBLETON BJJ, 1975, EARTH PLANET SC LETT, V27, P329, DOI 10.1016/0012-821X(75)90045-X; Friis EM, 1999, ANN MO BOT GARD, V86, P259, DOI 10.2307/2666179; Friis EM, 2000, GRANA, V39, P226, DOI 10.1080/00173130052017262; HEDLUND RW, 1966, OKLA GEOL SURV B, V112; HEIRTZLER JR, 1971, SCIENCE, V174, P488, DOI 10.1126/science.174.4008.488; HERNGREEN GFW, 1982, MICROPALEONTOLOGY, V28, P97, DOI 10.2307/1485364; HUGHES N.F., 1991, Journal of Micropalaeontology, V10, P75, DOI [10.1144/jm.10.1.75, DOI 10.1144/JM.10.1.75]; HUGHES NF, 1994, PALEOBIOL SER, V1; Huynh K-L, 1976, Linnean Society Symposium Series, P101; LENTIN JK, 1973, 7342 GEOL SURV CAN D; Lupia R, 1999, PALEOBIOLOGY, V25, P305, DOI 10.1017/S009483730002131X; May F.E., 1971, Geoscience and Man, v, V7, P57; MCELHINNY MW, 1976, GEOLOGY, V4, P455, DOI 10.1130/0091-7613(1976)4<455:PEFTLO>2.0.CO;2; McLachlan I.R., 1978, DEEP SEA DRILLING PR, V40, P857; Myers N, 2000, NATURE, V403, P853, DOI 10.1038/35002501; Penny J. H., 1988, J MICROPALAEONTOL, V7, P201, DOI DOI 10.1144/JM.7.2.201; Pervinquiere L., 1910, M MOIRES SOCI T G OL, V17, P1; PIERCE RL, 1961, MINN GEOL SURV B, V42; RABINOWITZ PD, 1982, SCIENCE, V215, P663, DOI 10.1126/science.215.4533.663; ROMANS R C, 1975, Pollen et Spores, V17, P273; Schatz GE, 1996, COLLOQ SEMI, P73; SCOTT L, 1976, Pollen et Spores, V18, P563; SHIELDS O, 1977, J GEOL, V85, P236, DOI 10.1086/628288; SINGH C, 1971, B RES COUNC ALBERTA, V28, P1; SMITH AG, 1970, NATURE, V225, P139, DOI 10.1038/225139a0; SPICER RA, 1999, UNDERSTANDING CLIMAT; Srivastava SK., 1975, Paleobiologie Continentale, V6, P1; STOREY M, 1995, SCIENCE, V267, P852, DOI 10.1126/science.267.5199.852; TRIPATHI A, 1991, PALEOBOTANIST, V39, P50; VENKATACHALA B S, 1974, Geophytology, V4, P153; WACHTEL AW, 1980, SCANNING, V3, P302, DOI 10.1002/sca.4950030410; WRIGHT JB, 1970, EARTH PLANET SC LETT, V8, P267, DOI 10.1016/0012-821X(70)90188-3	43	5	5	0	4	TAYLOR & FRANCIS AS	OSLO	KARL JOHANS GATE 5, NO-0154 OSLO, NORWAY	0017-3134	1651-2049		GRANA	Grana		2003	42	1					20	32						13	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	660VR					2025-03-11	WOS:000181855200003
J	Palliani, RB; Riding, JB				Palliani, RB; Riding, JB			<i>Umbriadinium</i> and <i>Polarella</i>:: an example of selectivity in the dinoflagellate fossil record	GRANA			English	Article							SEA-ICE; SUESSIACEAE	The extant Antarctic dinoflagellate genus Polarella and the southern European Early Jurassic dinoflagellate cyst Umbriadinium are extremely similar in morphology, particularly in their size, ornamentation and tabulation. Polarella is therefore placed in the subfamily Umbriadinioideae on this morphological evidence. The two genera, however, are maintained as separate entities for several reasons including minor differences in tabulation. This means that the stratigraphical distribution of the subfamily Umbriadinioideae is extended from the Early Jurassic (late Pliensbachian - early Toarcian) to Recent. The two species (Polarella glacialis and Umbriadinium mediterraneense) are separated by around 187 Ma. This large stratigraphical gap is an example of the selectivity of the dinoflagellate fossil record, produced by the loss of the capacity of Polarellal Umbriadinium to produce fossilisable cysts during the early Toarcian. The widely differing records of these genera attests to their longevity and wide geographical and ecological ranges.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy; British Geol Survey, Keyworth NG12 5GG, Notts, England	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Univ Perugia, Dept Earth Sci, Piazza Univ, I-06100 Perugia, Italy.	Rbucefa@tin.it; jbri@bgs.ac.uk						[Anonymous], 1985, SPOROPOLLENIN DINOFL; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BINT A N, 1986, Palynology, V10, P135; DEGRACIANSKY PC, 1998, SP PUBL SOC SED GEOL, V60; Fensome R.A., 1993, 7 AM MUS NAT HIST; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fensome RA, 1999, GRANA, V38, P66; Greuter W., 2000, REGN VEG, V138; Head M.J., 1996, Palynology: Principles and Applications, P1197; LOEBLICH AR, 1979, J MAR BIOL ASSOC UK, V59, P195, DOI 10.1017/S0025315400046270; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; MOLDOWAN JM, 1996, GEOLOGY, V24, P158; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; Palliani Raffaella Bucefalo, 1997, Palynology, V21, P197; Palliani RB, 2000, J MICROPALAEONTOL, V19, P133, DOI 10.1144/jm.19.2.133; Rees P.M., 2000, WARM CLIMATES EARTHS, P297, DOI [10.1017/CBO9780511564512.011, DOI 10.1017/CBO9780511564512.011]; Stoecker DK, 1997, J PHYCOL, V33, P585, DOI 10.1111/j.0022-3646.1997.00585.x; Stoecker DK, 1998, J PHYCOL, V34, P60, DOI 10.1046/j.1529-8817.1998.340060.x; Taylor FJR, 1999, J PHYCOL, V35, P1; TAYLOR MJ, 1987, CRYOBIOLOGY, V24, P91, DOI 10.1016/0011-2240(87)90011-3; Wall D., 1975, Micropalaeontology, V21, P14, DOI 10.2307/1485153; WILLIAMS GL, 1998, AASP CONTRIB SER, V34	22	6	8	1	4	TAYLOR & FRANCIS AS	OSLO	KARL JOHANS GATE 5, NO-0154 OSLO, NORWAY	0017-3134	1651-2049		GRANA	Grana		2003	42	2					108	111		10.1080/00173130310012495	http://dx.doi.org/10.1080/00173130310012495			4	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	701BC					2025-03-11	WOS:000184144800007
J	Willard, DA; Cronin, TM; Verardo, S				Willard, DA; Cronin, TM; Verardo, S			Late-Holocene climate and ecosystem history from Chesapeake Bay sediment cores, USA	HOLOCENE			English	Review						palaeoclimate; climatic change; estuarine sediments; drought; pollen; dinoflagellate cysts; anthropogenic impacts; Chesapeake Bay; late Holocene	NORWEGIAN SKAGERRAK COAST; NORTHERN GREAT-PLAINS; CENTRAL UNITED-STATES; CARBON ISOTOPIC RECORD; DINOFLAGELLATE-CYSTS; ANTHROPOGENIC INFLUENCE; OXYGEN CONCENTRATIONS; ATLANTIC OCEAN; ADJACENT SEAS; STABLE OXYGEN	Palaeoclimate records from late-Holocene sediments in Chesapeake Bay, the largest estuary in the USA, provide evidence that both decadal to centennial climate variability and European colonization had severe impacts on the watershed and estuary. Using pollen and dinoflagellate cysts as proxies for mid-Atlantic regional precipitation, estuarine salinity and dissolved oxygen (DO) during the last 2300 years, we identified four dry intervals, centred on AD 50 (P1/D1), AD 1000 (P2/D2), AD 1400 (P3) and AD 1600 (P4). Two centennial-scale events, P1/D1 and P2/D2, altered forest composition and led to increased salinity and DO levels in the estuary. Intervals P3 and P4 lasted several decades, leading to decreased production of pine pollen. Periods of dry mid-Atlantic climate correspond to 'megadroughts' identified from tree-ring records in the southeastern and central USA. The observed mid-Atlantic climate variability may be explained by changes in atmospheric circulation resulting in longer-term, perhaps amplified, intervals of meridional flow. After European colonization in the early seventeenth century, forest clearance for agriculture, timber and urbanization altered estuarine water quality, with dinoflagellate assemblages indicating reduced DO and increased turbidity.	US Geol Survey, Natl Ctr 926A, Reston, VA 20192 USA; Atlantic Geoserv Inc, Oakton, VA USA	United States Department of the Interior; United States Geological Survey	Willard, DA (通讯作者)，US Geol Survey, Natl Ctr 926A, Reston, VA 20192 USA.			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J	Head, MJ; Norris, G				Head, MJ; Norris, G			New species of dinoflagellate cysts and other palynomorphs from the latest Miocene and Pliocene of DSDP hole 603C, western North Atlantic	JOURNAL OF PALEONTOLOGY			English	Article							DRILLING-PROJECT LEG-93; LOWER CONTINENTAL RISE; NEOGENE; BIOSTRATIGRAPHY	Detailed investigation of the essentially complete uppermost Miocene through Lower Pleistocene sequence in Deep Sea Drilling Project (DSDP) Hole 603C, western North Atlantic, has revealed the presence of the new dinoflagellate cyst species Lejeunecysta hatterasensis, Lejeunecysta interrupta, Corrudinium devernaliae, and Pyxidinopsis vesiculata, as well as the acritarchs Leiosphaeridia rockhallensis Head new species and Leffingwellia costata new genus and species. Independent magnetobiostratigraphic control of DSDP Hole 603C constrains the ranges of these new species. Lejeunecysta interrupta n. sp. appears to range no higher than lowermost Pliocene at 5.2 Ma, Pyxidinopsis vesiculata n. sp. has a range top at about 4.5 Ma in the Lower Pliocene, Corrudinium devernaliae n. sp. has a well-defined range of 4.7-4.1 Ma within the Lower Pliocene, and Leiosphaeridia rockhallensis n. sp. has a similarly well-defined range of 4.4-3.9 Ma within the Lower Pliocene. The presence of Leiosphaeridia rockhallensis n. sp. in the Ramsholt Member of the Coralline Crag Formation, eastern England, supports an Early Pliocene age for this member.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada	University of Cambridge; University of Toronto	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk; norris@quartz.geology.utoronto.ca						[Anonymous], 1885, HG BRONNS KLASSEN OR; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; Balech E., 1988, Publ. Espec. Inst. Esp. 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J	Yamamoto, T; Seike, T				Yamamoto, T; Seike, T			Modelling the population dynamics of the toxic dinoflagellate <i>Alexandrium tamarense</i> in Hiroshima Bay, Japan.: II.: Sensitivity to physical and biological parameters	JOURNAL OF PLANKTON RESEARCH			English	Article							DIEL VERTICAL MIGRATION; GONYAULAX-TAMARENSIS; RED-TIDE; PHYTOPLANKTON; BLOOMS; CYSTS; SEA; TEMPERATURE; MECHANISMS; CAPACITY	Using the numerical model developed in a previous paper [Yamamoto et al. (2002c) J. Plankton Res., 24, 33-47], the sensitivity of population dynamics of Alexandrium tamarense to physical and biological parameters was analysed. Horizontal and vertical diffusions led to the dispersion of dense A. tamarense populations in the surface layer of the innermost portion of the bay. Temperature and salinity influenced the timing of the A. tamarense bloom due to its stenothermal and stenohaline characteristics. Although increasing the light intensity caused the bloom of A. tamarense to begin earlier, it lowered the cell density at the bloom peak as a result of phosphate depletion in the ambient water. Both increasing the cyst density and the excystment rate had little influence on the population dynamics of A. tamarense vegetative cells. Increasing the phosphate concentration led to increases in cell density of A. tamarense, indicating that growth is phosphate-limited. Oysters, which are cultured intensively in this bay, appear to stimulate the bloom of A. tamarense through the regeneration of phosphorus from their faeces/pseudofaeces. The phosphorus reduction measure that has been taken since 1980 and the recent construction of a large dam are discussed as important factors that may influence the population dynamics of A. tamarense.	Hiroshima Univ, Grad Sch Biosphere Sci, Higashihiroshima 7398528, Japan	Hiroshima University	Yamamoto, T (通讯作者)，Hiroshima Univ, Grad Sch Biosphere Sci, Higashihiroshima 7398528, Japan.							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Plankton Res.	JAN	2003	25	1					63	81		10.1093/plankt/25.1.63	http://dx.doi.org/10.1093/plankt/25.1.63			19	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	636PH		Bronze			2025-03-11	WOS:000180464700004
J	Kremp, A; Shull, DH; Anderson, DM				Kremp, A; Shull, DH; Anderson, DM			Effects of deposit-feeder gut passage and fecal pellet encapsulation on germination of dinoflagellate resting cysts	MARINE ECOLOGY PROGRESS SERIES			English	Article						dinoflagellate cysts; deposit feeder; germination; fecal pellets; Scrippsiella lachrymosa	NORTHERN BALTIC SEA; SETO INLAND SEA; SCRIPPSIELLA-TROCHOIDEA; GONYAULAX-TAMARENSIS; PLANKTONIC DIATOMS; PARTICLE-TRANSPORT; COPEPOD NAUPLII; BENTHIC CYSTS; SPRING BLOOM; SEDIMENT	Many species of dinoflagellates spend much of their lives buried in sediments as resting cysts. While on the bottom, cysts may pass through the guts of deposit feeders before conditions become favorable for germination. Little is known, however, about how dinoflagellate cysts are affected by deposit-feeder digestion, fecal pellet formation, and translocation within the sediment column. To answer the question of whether gut passage or pelletization reduces cyst germination, we fed cysts of the dinoflagellate Scrippsiella lachrymosa to 3 polychaete deposit feeders, Capitella sp., Streblospio benedicti, and Polydora cornuta. Fecal pellets of these species have different morphologies and represent a wide range of pellet robustness. To examine the effects of longer gut-passage times, cysts were incubated in the digestive fluids of the polychaete Arenicola marina for up to 24 h, and monitored to determine germination success. Cysts were remarkably resistant to digestion by deposit-feeding polychaetes, and were capable of germinating even within the robust fecal pellets of Capitella. In fact, cysts were more likely to germinate within fecal pellets of Capitella than outside those pellets. Thus, pellets may be favorable environments for germination of resting cysts. Our data suggest that deposit-feeder gut passage and pelletization do not substantially reduce germination of dinoflagellate cysts in the field, and may even enhance it.	Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; Western Washington Univ, Dept Environm Sci, Bellingham, WA 98225 USA	Woods Hole Oceanographic Institution; Western Washington University	Kremp, A (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	anke.kremp@helsinki.fi	Kremp, Anke/I-8139-2013; Shull, David/IUP-8150-2023					Ahrens MJ, 2001, MAR ECOL PROG SER, V212, P145, DOI 10.3354/meps212145; Albertsson J, 2001, MAR BIOL, V138, P793, DOI 10.1007/s002270000498; 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; BINDER BJ, 1987, J PHYCOL, V23, P99; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; Cáceres CE, 1998, ERGEB LIMNOL, V52, P163; CAMMEN LM, 1980, OECOLOGIA, V44, P303, DOI 10.1007/BF00545232; Dale B., 1983, P69; FORBES TL, 1987, BIOL BULL-US, V172, P187, DOI 10.2307/1541792; FORBES TL, 1990, J EXP MAR BIOL ECOL, V143, P209, DOI 10.1016/0022-0981(90)90071-J; Giangrande A, 2002, J SEA RES, V47, P97, DOI 10.1016/S1385-1101(01)00103-4; Grant BR, 1996, ECOLOGY, V77, P489, DOI 10.2307/2265624; Hansson LA, 1996, LIMNOL OCEANOGR, V41, P1312, DOI 10.4319/lo.1996.41.6.1312; Head RM, 1999, FRESHWATER BIOL, V41, P759, DOI 10.1046/j.1365-2427.1999.00421.x; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Henriksen K., 1983, ECOL B, V35, P193; Huber G., 1923, FLORA JENA, V116, P114; Ichimi K, 2001, FISHERIES SCI, V67, P1178, DOI 10.1046/j.1444-2906.2001.00378.x; IMAI I, 1991, MAR POLLUT BULL, V23, P165, DOI 10.1016/0025-326X(91)90668-I; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; JUMARS PA, 1981, MAR GEOL, V42, P155, DOI 10.1016/0025-3227(81)90162-6; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kearns CM, 1996, HYDROBIOLOGIA, V332, P63, DOI 10.1007/BF00020780; Kokinos John P., 1995, Palynology, V19, P143; Kremp A, 2000, J PLANKTON RES, V22, P2155, DOI 10.1093/plankt/22.11.2155; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; Levin L, 1997, J MAR RES, V55, P595, DOI 10.1357/0022240973224337; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; Luckenbach MW, 1999, AQUAT BOT, V62, P235, DOI 10.1016/S0304-3770(98)00098-9; MARCUS NH, 1984, MAR ECOL PROG SER, V15, P47, DOI 10.3354/meps015047; MAYER LM, 1997, J MAR RES, V55, P1; McQuoid MR, 2002, J PHYCOL, V38, P881, DOI 10.1046/j.1529-8817.2002.01169.x; Montani Shigeru, 1995, P627; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; 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; 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; PLANTE C, 1992, MICROB ECOL, V23, P257, DOI 10.1007/BF00164100; Ramsay F., 2002, The Statistical Sleuth, V2nd; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; RHOADS D C, 1970, Journal of Marine Research, V28, P150; SANDERS HL, 1962, LIMNOL OCEANOGR, V7, P63, DOI 10.4319/lo.1962.7.1.0063; SELF RFL, 1988, J MAR RES, V46, P119, DOI 10.1357/002224088785113685; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; Shull DH, 2002, LIMNOL OCEANOGR, V47, P1530, DOI 10.4319/lo.2002.47.5.1530; Shull DH, 2001, J MAR RES, V59, P453, DOI 10.1357/002224001762842271; SMETACEK VS, 1985, MAR BIOL, V84, P239, DOI 10.1007/BF00392493; Ståhl-Delbanco A, 2002, LIMNOL OCEANOGR, V47, P1836, DOI 10.4319/lo.2002.47.6.1836; TAGHON GL, 1984, LIMNOL OCEANOGR, V29, P64, DOI 10.4319/lo.1984.29.1.0064; Tsujino M, 2002, J EXP MAR BIOL ECOL, V271, P1, DOI 10.1016/S0022-0981(02)00024-2	55	22	25	2	13	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2003	263						65	73		10.3354/meps263065	http://dx.doi.org/10.3354/meps263065			9	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	761UV		Green Submitted, Bronze			2025-03-11	WOS:000187934600005
J	Zhang, XS; Anderson, JT; Hood, RR				Zhang, XS; Anderson, JT; Hood, RR			Modeling <i>Pfiesteria piscicida</i> population dynamics:: a new approach for tracking size and mass in mixotrophic species	MARINE ECOLOGY PROGRESS SERIES			English	Article						modeling; Pfiesteria size; Pfiesteria abundance; encystment	FREE-LIVING PROTOZOA; ESTUARINE DINOFLAGELLATE; COASTAL WATERS; BLOOM DYNAMICS; FISH KILLS; SEA; MICROZOOPLANKTON; DINOPHYCEAE; IMPACTS; GROWTH	We have developed a generalized dynamic, numerical model to study Pfiesteria population dynamics based on available observations and literature. We have incorporated formulations into this model which allow us to track changes in cell size in relation to food availability and other environmental conditions, which can be used for modeling a variety of cell-size dependent physiological functions. With this model, we are able to follow the time dependency of both individual size and abundance of Pfiesteria zoospores in cultures. We also have developed a general, starvation-based trigger mechanism for cyst formation for mixotrophic species like Pfiesteria, which is based on the size of zoospores determined by previous food conditions and the decrease or increase in size determined by the current food conditions. The model results suggest that zoospore concentration can be regulated effectively by both bottom-up control by food availability and the top-down control by zooplankton grazing. Model sensitivity analysis shows that the results are fairly robust with respect to changes in the model parameter values. This paper represents a significant step forward in our efforts to model complicated life-cycle phenomena in dinoflagellates like Pfiesteria and, in so doing, also provides some important new approaches for tracking cell size and cyst formation.	Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA	University System of Maryland; University of Maryland Center for Environmental Science	Zhang, XS (通讯作者)，Univ Maryland, Ctr Environm Sci, Horn Point Lab, POB 775, Cambridge, MD 21613 USA.	zhang@hpl.umces.edu	hood, raleigh/F-9364-2013	Hood, Raleigh/0000-0002-7248-3481				ANDERSEN V, 1986, J PLANKTON RES, V8, P1091, DOI 10.1093/plankt/8.6.1091; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; Anderson JT, 2003, MAR ECOL PROG SER, V246, P105, DOI 10.3354/meps246105; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; ARKINSON A, 1995, ICES J MAR SCI, V52, P385; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; 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; CARLOTTI F, 1989, MAR ECOL PROG SER, V56, P225, DOI 10.3354/meps056225; Carlotti F., 2000, P571, DOI 10.1016/B978-012327645-2/50013-X; Caron D.A., 1990, P307; CORLISS JO, 1974, T AM MICROSC SOC, V93, P578, DOI 10.2307/3225158; Donaghay PL, 1997, LIMNOL OCEANOGR, V42, P1283, DOI 10.4319/lo.1997.42.5_part_2.1283; FASHAM MJR, 1990, J MAR RES, V48, P591, DOI 10.1357/002224090784984678; FENCHEL T, 1982, MAR ECOL PROG SER, V9, P25, DOI 10.3354/meps009025; FENCHEL T, 1983, MICROB ECOL, V9, P99, DOI 10.1007/BF02015125; Franks PJS, 1997, LIMNOL OCEANOGR, V42, P1273, DOI 10.4319/lo.1997.42.5_part_2.1273; GIFFORD DJ, 1988, B MAR SCI, V43, P458; GLASGOW HB, 1998, HARMFUL MICROALGAE, P394; Hood RR, 2001, DEEP-SEA RES PT II, V48, P1609, DOI 10.1016/S0967-0645(00)00160-0; KISHI M, 1986, ECOL MODEL, V31, P145, DOI 10.1016/0304-3800(86)90061-X; Lewitus AJ, 1999, J PHYCOL, V35, P303, DOI 10.1046/j.1529-8817.1999.3520303.x; LI A, 1998, THESIS U MARYLAND; MALLIN MA, 1995, J PLANKTON RES, V17, P351, DOI 10.1093/plankt/17.2.351; McCreary JP, 1996, PROG OCEANOGR, V37, P193, DOI 10.1016/S0079-6611(96)00005-5; Steele J. H., 1974, STRUCTURE MARINE ECO, DOI DOI 10.4159/HARVARD.9780674592513; Stickney HL, 2000, ECOL MODEL, V125, P203, DOI 10.1016/S0304-3800(99)00181-7; Stoecker DK, 2000, AQUAT MICROB ECOL, V22, P261, DOI 10.3354/ame022261; Stoecker DK, 1999, J EUKARYOT MICROBIOL, V46, P397, DOI 10.1111/j.1550-7408.1999.tb04619.x; Stoecker DK, 2002, AQUAT MICROB ECOL, V28, P79, DOI 10.3354/ame028079; Stoecker DK, 2002, MAR ECOL PROG SER, V233, P31, DOI 10.3354/meps233031; Stoecker DK, 1998, EUR J PROTISTOL, V34, P281, DOI 10.1016/S0932-4739(98)80055-2; WYATT T, 1973, NATURE, V244, P238, DOI 10.1038/244238a0	35	4	4	1	4	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2003	256						29	44		10.3354/meps256029	http://dx.doi.org/10.3354/meps256029			16	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	712QT		Bronze			2025-03-11	WOS:000184808900003
J	Anderson, JT; Stoecker, DK; Hood, RR				Anderson, JT; Stoecker, DK; Hood, RR			Formation of two types of cysts by a mixotrophic dinoflagellate, <i>Pfiesteria piscicida</i>	MARINE ECOLOGY PROGRESS SERIES			English	Article						Pfiesteria piscicida; harmful algal blooms; kleptochloroplastidy; mixotrophy; life history transformations; resting stages	AMBUSH-PREDATOR DINOFLAGELLATE; TOXIC DINOFLAGELLATE; LIFE-CYCLE; ESTUARINE DINOFLAGELLATE; GYRODINIUM-UNCATENUM; SPRING-BLOOM; DINOPHYCEAE; ENCYSTMENT; TEMPERATURE; STAIN	Despite the widespread occurrence of mixotrophic dinoflagellates, most research on cyst formation in dinoflagellates has focused on phototrophic organisms or on factors affecting phototrophic growth (i.e. light intensity and nutrient supply). Presumably, factors that stimulate cyst formation in mixotrophic organisms would be combinations of those factors that affect phototrophic and phagotrophic growth (such as limiting light intensity and limiting prey concentrations). The toxic dinoflagellate Pfiesteria piscicida is an interesting test case because it has a complex life history and is considered mixotrophic. Recently, a form of P. piscicida has been described that does not have the ability to produce toxins (termed 'non-inducible'). The objectives of this study were to identify which life stages are likely to be present in a mixotrophic culture of 'non-inducible' F piscicida and to determine the morphological differences based on fluorescent stain uptake. Also, we examined which combinations of adverse environmental factors (low light intensity and low prey concentrations) affect life stage transformations. In this culture, we observed 3 distinct life stages (a zoospore stage, and 2 cysts). One of the cysts (termed Cyst A) has a thick cell wall and appears to form from actively feeding zoospores regardless of light intensity. The second type of cyst (Cyst B) has a much thinner cell wall and only forms from recently fed zoospores maintained in complete darkness. During the experiment, encystment rates to either cyst were low, suggesting that encystment will not dramatically affect bloom dynamics on small timescales.	Univ Maryland, Ctr Environm Sci, Horn Point Environm Lab, Cambridge, MD 21613 USA	University System of Maryland; University of Maryland Center for Environmental Science	Anderson, JT (通讯作者)，Skidaway Inst Oceanog, 10 Ocean Sci Circle, Savannah, GA 31411 USA.	anderson@skio.peachnet.edu	hood, raleigh/F-9364-2013; stoecker, diane/F-9341-2013	Hood, Raleigh/0000-0002-7248-3481				AGBETI MD, 1931, J PHYCOL, V31, P70; ANDERSON DM, 1985, J PHYCOL, V21, P200; Anderson JT, 2003, MAR ECOL PROG SER, V246, P105, DOI 10.3354/meps246105; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P667, DOI 10.2307/3454912; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; 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; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; delGiorgio P, 1996, LIMNOL OCEANOGR, V41, P783, DOI 10.4319/lo.1996.41.4.0783; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; GREENSPAN P, 1985, J CELL BIOL, V100, P965, DOI 10.1083/jcb.100.3.965; HAAS LW, 1982, ANN I OCEANOGR PARIS, V58, P261; HARDELAND R, 1994, EXPERIENTIA, V50, P60, DOI 10.1007/BF01992051; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Jakobsen HH, 2000, MAR ECOL PROG SER, V201, P121, DOI 10.3354/meps201121; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Jochem FJ, 1999, MAR BIOL, V135, P721, DOI 10.1007/s002270050673; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Lebaron P, 1998, APPL ENVIRON MICROB, V64, P2697; Lewitus AJ, 1999, J PHYCOL, V35, P303, DOI 10.1046/j.1529-8817.1999.3520303.x; MALLIN MA, 1995, J PLANKTON RES, V17, P351, DOI 10.1093/plankt/17.2.351; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; PFIESTER LA, 1998, BIOL DINOFLAGELLATES, P611; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Sanderson BL, 1996, CAN J FISH AQUAT SCI, V53, P1409, DOI 10.1139/cjfas-53-6-1409; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; Skovgaard A, 1998, AQUAT MICROB ECOL, V15, P293, DOI 10.3354/ame015293; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; STOECKER DK, 1988, MAR BIOL, V99, P415, DOI 10.1007/BF02112135; Stoecker DK, 2000, AQUAT MICROB ECOL, V22, P261, DOI 10.3354/ame022261; Stoecker DK, 1999, J EUKARYOT MICROBIOL, V46, P397, DOI 10.1111/j.1550-7408.1999.tb04619.x; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163	38	12	15	2	7	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2003	246						95	104		10.3354/meps246095	http://dx.doi.org/10.3354/meps246095			10	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	647GM		Bronze			2025-03-11	WOS:000181085100007
J	Anderson, JT; Hood, RR; Zhang, X				Anderson, JT; Hood, RR; Zhang, X			Quantification of <i>Pfiesteria piscicida</i> growth and encystment parameters using a numerical model	MARINE ECOLOGY PROGRESS SERIES			English	Article						Pfiesteria piscicida; harmful algal blooms; numerical models; kleptochloroplastidy; mixotrophy; life history transformations; resting stages	AMBUSH-PREDATOR DINOFLAGELLATE; TOXIC DINOFLAGELLATE; LIFE-CYCLE; ESTUARINE DINOFLAGELLATE; GYRODINIUM-UNCATENUM; FISH KILLS; DINOPHYCEAE; MIXOTROPHY; BEHAVIOR; CHLOROPLASTS	In the past decade, there has been growing interest in understanding the physiological ecology and life cycle of toxic forms of Pfiesteria piscicida. However, transformations among non-inducible (NON-IND; formerly described as nontoxic) stages have received less attention despite the fact that NON-IND stages are found in nature and may be ecologically important as prey and predators. NON-IND stages are also mixotrophic and have the ability to retain and utilize prey chloroplasts in a process termed 'kleptoplastidic mixotrophy'. Quantifying growth, grazing and encystment rates from P. piscicida laboratory experiments is confounded by the interrelationship between mixotrophy and life stage transformations. By fitting a numerical model to a laboratory experiment on NON-IND P. piscicida, we were able to isolate the potential mechanisms that cause encystment and speculate on the interrelationship between adverse conditions (i.e. low light and limiting prey) and life stage transformations. The structure of the laboratory experiment allowed for the estimation of several growth and encystment parameters including grazing rates, gross growth and assimilation efficiencies, as well as the retention time of chloroplasts. Model results suggest a link between encystment and mixotrophic ability. Furthermore, the model results suggest that encystment rates and gross growth and assimilation efficiencies calculated from the model are lower than expected.	Univ Maryland, Ctr Environm Sci, Horn Point Environm Lab, Cambridge, MD 21613 USA	University System of Maryland; University of Maryland Center for Environmental Science	Anderson, JT (通讯作者)，Skidaway Inst Oceanog, 10 Ocean Sci Circle, Savannah, GA 31411 USA.	anderson@skio.peachnet.edu	hood, raleigh/F-9364-2013	Hood, Raleigh/0000-0002-7248-3481				AGBETI MD, 1995, J PHYCOL, V31, P70, DOI 10.1111/j.0022-3646.1995.00070.x; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1985, J PHYCOL, V21, P200; Anderson JT, 2003, MAR ECOL PROG SER, V246, P95, DOI 10.3354/meps246095; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; BOCKSTAHLER KR, 1993, J EUKARYOT MICROBIOL, V40, P49, DOI 10.1111/j.1550-7408.1993.tb04881.x; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P667, DOI 10.2307/3454912; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; 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; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; CONOVER RJ, 1978, MARINE ECOLOGY, V44; Dent J.B., 1979, Systems Simulations in Agriculture; FASHAM MJR, 1990, J MAR RES, V48, P591, DOI 10.1357/002224090784984678; FIELDS SD, 1991, J PHYCOL, V27, P525, DOI 10.1111/j.0022-3646.1991.00525.x; FROST BW, 1972, LIMNOL OCEANOGR, V17, P805, DOI 10.4319/lo.1972.17.6.0805; Giacobbe MG, 1997, J PHYCOL, V33, P73, DOI 10.1111/j.0022-3646.1997.00073.x; Harris R., 2000, ICES Zooplankton Methodology Manual, DOI [10.1016/b978-0-12-327645-2.x5000-2, DOI 10.1016/B978-0-12-327645-2.X5000-2]; JACOBSON DM, 1994, PHYCOLOGIA, V33, P97, DOI 10.2216/i0031-8884-33-2-97.1; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Lewitus AJ, 1999, J PHYCOL, V35, P303, DOI 10.1046/j.1529-8817.1999.3520303.x; LI A, 1998, THESIS U MARYLAND CT, pCH6; LI A, 1998, THESIS U MARYLAND CT; Lowe J.A., 1991, FISH KILLS COASTAL W; MALLIN MA, 1995, J PLANKTON RES, V17, P351, DOI 10.1093/plankt/17.2.351; Paerl HW, 1998, MAR ECOL PROG SER, V166, P17, DOI 10.3354/meps166017; Pfiester L.A., 1987, BIOL DINOFLAGELLATES; PFIESTER LA, 1987, BIPOL DINOFLAGELLATE; POPOVSKY J, 1982, ARCH PROTISTENKD, V125, P115, DOI 10.1016/S0003-9365(82)80011-0; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; *SAS, 1998, SAS STAT SOFTW VERS; Skovgaard A, 1998, AQUAT MICROB ECOL, V15, P293, DOI 10.3354/ame015293; STEELE JH, 1977, SEA IDEAS OBSERVATIO; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Stickney HL, 2000, ECOL MODEL, V125, P203, DOI 10.1016/S0304-3800(99)00181-7; STOECKER DK, 1990, MAR BIOL, V107, P491, DOI 10.1007/BF01313434; STOECKER DK, 1988, MAR BIOL, V99, P415, DOI 10.1007/BF02112135; Stoecker DK, 1999, J EUKARYOT MICROBIOL, V46, P397, DOI 10.1111/j.1550-7408.1999.tb04619.x; Stoecker DK, 1998, EUR J PROTISTOL, V34, P281, DOI 10.1016/S0932-4739(98)80055-2; Straile D, 1997, LIMNOL OCEANOGR, V42, P1375, DOI 10.4319/lo.1997.42.6.1375; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163	44	7	7	0	5	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2003	246						105	113		10.3354/meps246105	http://dx.doi.org/10.3354/meps246105			9	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	647GM		Bronze			2025-03-11	WOS:000181085100008
J	Marret, F; Scourse, J				Marret, F; Scourse, J			Control of modern dinoflagellate cyst distribution in the Irish and Celtic seas by seasonal stratification dynamics	MARINE MICROPALEONTOLOGY			English	Article						shelf sea; dinoflagellate cyst; stratification; tidal front; mixed waters	SP-NOV DINOPHYCEAE; SURFACE CONDITIONS; NORTH-ATLANTIC; MICRORETICULATE CYST; GYMNODINIUM-NOLLERI; COMMUNITY STRUCTURE; MARINE-SEDIMENTS; ENGLISH-CHANNEL; LATE QUATERNARY; ADJACENT SEAS	Surface sediments from seven stations located in the seasonally stratified, frontal and mixed water regions in the Celtic and Irish seas have been analysed for their dinoflagellate cyst assemblages and dinosterol content. A total of 45 dinoflagellate cyst taxa have been identified and the assemblages related to surface and sediment conditions. Sediments from the mixed water region, at 30 in water depth, are characterised by a relatively low cyst concentration (similar to2300 cysts/g dry weight) and high relative abundances of Lingulodinium machaerophorum accompanied by Spiniferites membranaceus, Brigantedinium spp. and Dubridinium caperatum. Assemblages from stratified and frontal water stations are dominated by Spiniferites ramosus associated with Operculodinium centrocarpum, Brigantedinium spp., cysts of Polykrikos schwartzii and Selenopemphix quanta. Ordination techniques performed on a restricted number of 35 taxa from the assemblages differentiated the stratified and frontal assemblages based on the abundance of the less abundant species Bitectatodinium tepikiense and Spiniferites elongatus. Among the environmental parameters (sea-surface temperature and salinity, stratification index, chlorophyll concentration and sediment grain-size classes), the seasonal stratification and sedimentological context, itself a function of tidal dynamics, explain most of the variance in the environmental conditions. These results indicate that dinoflagellate cyst analyses of shelf sediment records can be used to document the planktonic signal of seasonal stratification dynamics. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Coll N Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales	Bangor University	Marret, F (通讯作者)，Univ Coll N Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales.	f.marret@bangor.ac.uk; j.scourse@bangor.ac.uk		Marret-Davies, Fabienne/0000-0003-4244-0437				Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; [Anonymous], SEA; [Anonymous], NOVA HEDWIGIA; [Anonymous], 1988, NATURE CONTINENTAL S, DOI DOI 10.1016/C2013-0-11665-0; Austin WEN, 1997, J GEOL SOC LONDON, V154, P249, DOI 10.1144/gsjgs.154.2.0249; BALCH WM, 1983, CAN J FISH AQUAT SCI, V40, P244, DOI 10.1139/f83-287; BERGER WH, 1989, LIFE SCI R, V44, P1; 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 CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BOON JJ, 1979, NATURE, V277, P125, DOI 10.1038/277125a0; Clarke K R., 1994, An approach to statistical analysis and interpretation; 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Micropaleontol.	JAN	2003	47	1-2					101	116	PII S0377-8398(02)00095-6	10.1016/S0377-8398(02)00095-6	http://dx.doi.org/10.1016/S0377-8398(02)00095-6			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	623TJ					2025-03-11	WOS:000179718700004
J	Ismael, AA; Khadr, AM				Ismael, AA; Khadr, AM			<i>Alexandrium minutum</i> cysts in sediment cores from the Eastern Harbour of Alexandria, Egypt	OCEANOLOGIA			English	Article						Alexandrium minutum; cysts; sediment cores; Eastern Harbour		Alexandrium minutum cysts were studied in sediment cores from its type locality, the Eastern Harbour of Alexandria, following the disappearance of the species from the plankton since 1994. Three cores were sampled in the summer of 1999 along the north-south axis of the harbour. The sediments were subjected to grain size analysis and their organic carbon content was determined. The sediments consisted of medium, coarse and very coarse sand. Grain size and organic carbon content were negatively and significantly correlated in core I but followed a parallel trend in cores 2 and 3. Seven dinoflagellate cysts, representing 6 genera were identified from the cores. Their relative abundance showed a remarkable difference. A. minutum cysts contributed a maximum of 17.4% to the total cysts. The distribution profile of A. minutum cysts in the cores reflects the bloom duration but not its productivity. The cyst distribution in the cores is the resultant of two opposite processes, the sedimentation rate and the continuous erosion of the bottom sediments, which is not related to sediment texture.	Univ Alexandria, Fac Sci, Dept Oceanog, EG-21511 Alexandria, Egypt	Egyptian Knowledge Bank (EKB); Alexandria University	Univ Alexandria, Fac Sci, Dept Oceanog, EG-21511 Alexandria, Egypt.	amany_3@yahoo.com	Ismael, Amany/N-8517-2017	Ismael, Amany/0000-0002-3693-3422				ALBIB W, 1995, MAR LIFE, V5, P11; [Anonymous], P 1 INT C TOX DIN BL; DENN EE, 1993, TOXIC PHYTOPLANKTON, P109; DUGHIEM M, 2002, THESIS ALEXANDRIA U; El Wakeel S.K., 1957, J CONS INT EXPLOR ME, V22, P180, DOI 10.1093/icesjms/22.2.180; ELDIN AB, 1998, THESIS ALEXANDRIA U; ELFISHAWI NM, 1993, VOLUMETRIC HYDROGRAP, V15, P59; ELSAYED M, 1999, WORKSH STATUS PILOT; ELWAKEEL SK, 1978, MAR GEOL, V27, P137, DOI 10.1016/0025-3227(78)90077-4; Fernex FE, 2001, HYDROBIOLOGIA, V450, P31, DOI 10.1023/A:1017558413882; Folk R. L., 1957, Jour. Sed. Petrol., V27, P3, DOI [10.1306/74d70646-2b21-11d7-8648000102c1865, 10.1306/74D70646-2B21-11D7-8648000102C1865D]; Halim Y., 1960, Vie et Milieu, V11, P102; Ismael A., 2001, HARMFUL ALGAL BLOOMS, P141; Ismael A. A., 1993, THESIS ALEXANDRIA U; ISMAEL AA, 2001, DINOFLAGELLATE CYSTS, V36; JAMMO KM, 2001, THESIS ALEXANDRIA U; Labib Wagdy, 1994, Chemistry and Ecology, V9, P75, DOI 10.1080/02757549408038566; Matsuoka K., 1989, P461; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; NESSIM RB, 1994, P 4 INT C ENV PROT M, P1; Sultan HA, 1975, THESIS ALEXANDRIA U; Zaghloul F.A., 1990, B HIGH I PUB HLTH AL, V20, P875; ZAGHLOUL FA, 1992, SCIENCE OF THE TOTAL ENVIRONMENT, SUPPLEMENT 1992, P727; ZAGHLOUL FA, 1988, B NATL I OCEANOGR FI, V117, P39	24	13	13	0	1	POLISH ACAD SCIENCES INST OCEANOLOGY	SOPOT	POWSTANCOW WASZAWY 55, PL-81-712 SOPOT, POLAND	0078-3234	2300-7370		OCEANOLOGIA	Oceanologia		2003	45	4					721	731						11	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	761CX					2025-03-11	WOS:000187883400013
J	Polyakova, EI; Dzhinoridze, RN; Novichkova, TS; Golovnina, EA				Polyakova, EI; Dzhinoridze, RN; Novichkova, TS; Golovnina, EA			Diatoms and palynomorphs in the White Sea sediments as indicators of ice and hydrological conditions	OCEANOLOGY			English	Article							DISTRIBUTION PATTERNS; LAPTEV SEA; ASSEMBLAGES; ALGAE	Comprehensive studies of diatoms and palynomorphs from the White Sea sediments revealed the following features of the composition of their assemblages. The species composition of the plankton diatoms and dinoflagellate cysts in the sediments reflects the features of the high-latitude position of the sea and the impact of the Arctic and North Atlantic water masses on its hydrological regime. But on the other hand, the spatial distribution of plankton species in the surface sediments-that is, both diatoms and dinoflagellate cysts-matches the distribution of the main types of water masses in the White Sea. The characteristic property of the diatom and dinoflagellate cyst assemblages is the presence, in high concentrations, of relatively thermophillic species of an Atlantic genesis in their composition.	Moscow MV Lomonosov State Univ, Fac Biol, Moscow, Russia; St Petersburg State Univ, Fac Geog, St Petersburg, Russia	Lomonosov Moscow State University; Saint Petersburg State University	Moscow MV Lomonosov State Univ, Fac Biol, Moscow, Russia.		Polyakova, Yelena/L-8889-2015; Novichkova, Ekaterina/B-5807-2017	Novichkova, Ekaterina/0000-0001-5687-1719				[Anonymous], 1982, MORYA SSSR; [Anonymous], 1971, POLLEN SPORES; ARZHANOVA NV, 1994, KOMPLEKSNYE ISSLEDOV, P25; Barss M. S, 1973, 7326 GEOL SURV CAN P, V73, P1; BATTARBE.RW, 1973, LIMNOL OCEANOGR, V18, P647, DOI 10.4319/lo.1973.18.4.0647; Bauch HA, 2000, INT J EARTH SCI, V89, P569, DOI 10.1007/s005310000122; BAUCH HA, 2002, PALAEOCEANOGRAPHY; BEKLEMISHEV KB, 1986, T VSESOYUZNOGO GIDRO, P7; Bondarchuk L.L., 1985, ECOL FAUNA FLORA COA, P74; Cremer H, 1999, MAR MICROPALEONTOL, V38, P39, DOI 10.1016/S0377-8398(99)00037-7; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Dzhinoridze R.N, 1978, MARINE MICROPALEONTO, P41; DZHINORIDZE RN, 1972, DOKL AKAD NAUK SSSR+, V204, P207; DZHINORIDZE RN, 1971, THESIS LENINGRAD; HORNER RA, 1990, POLAR MARINE DIATOMS, P19; Kiselev I.A., 1950, PANTSIRNYE ZHGUTIKON; KISELEV IA, 1939, T GOS GIDR INT LEN; KISELEV IA, 1925, ISSLEDOVANIYA RUSSKI, V105, P43; KISELEV IA, 1957, MAT KOMPLEKSNOMU IZU; KOKIN K A, 1970, Botanicheskii Zhurnal (St. Petersburg), V55, P499; KOLTSOVA TI, 1971, THESIS MOSCOW; KUNPIRRUNG M, 1999, LAND OCEAN SYSTEM SI, P561; LEVANDER KM, 1916, MIDDEL SOC PRO FAUNA, P42; Makarova I.V., 1988, DIATOMOVYE VODOROSLI; *MATISHOV GG, 1997, PLANKTON MOREI ZAPAD; 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; Melnikov I. A., 1989, Ekosistema arkticheskogo morskogo l'da. Ecosystem of the Arctic sea ice; MEREZHSKOVSKII KS, 1978, T SPB OBSHCHESTVA ES; MIKHAILOVSKY GE, 1989, OKEANOLOGIYA+, V29, P796; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; NEVESSKII EN, 1977, SEDIMENTOGENEZ ISTOR; Okolodkov Y. B., 1992, P NIPR S POLAR BIOL, P28; Okolodkov Yu B, 2000, THESIS ST PETERSBURG; Pankow H., 1990, OSTSEE ALGENFLORA; PETROV AK, 1967, OPT SPEKTROSK, P15; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Polyakova E.I, 1997, ARKTICHESKIE MORYA E; Polyakova EI, 2000, DOKL AKAD NAUK+, V370, P686; POLYAKOVA YI, 2003, IN PRESS SIBERIAN RI; Rat'kova T. N., 2000, BER POLARFORSCHUNG, V359, P97; RATKOVA TM, 2000, BERICHTE POLARFORSCH, V359, P23; REINGARD L, 1982, B SOC IMPER NET MOSC, V57; Rochon A., 1999, AM ASS STRATIGR PALY, V35, P146; Romankevich E.A., 2001, TSIKL UGLERODA ARKTI; SEMINA GI, 1980, BIOL MORYA; SEMINA GI, 1983, PLANKTONNAYA FLORA B, P3; Semina HJ, 1997, ADV MAR BIOL, V32, P527; SERGEEVA OM, 1991, ISSLEDOVANIE FITOPLA, P82; Simonsen R., 1962, Int. Rev. Ges. Hydrobiol. Beihefte, V1, P9; SYVERTSEN EE, 1991, POLAR RES, V10, P277, DOI 10.1111/j.1751-8369.1991.tb00653.x; TSENKOVSKII LS, 1981, T SANKT PETERBURGSKO; vonQuillfeldt CH, 1997, J MARINE SYST, V10, P211, DOI 10.1016/S0924-7963(96)00056-5; Zhitina L. S., 1990, BIOL MONITORING PRIB, V41-49	54	9	12	0	1	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0001-4370	1531-8508		OCEANOLOGY+	Oceanology		2003	43			S			S144	S158						15	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	760AV					2025-03-11	WOS:000187789000012
J	Montresor, M; Sgrosso, S; Procaccini, G; Kooistra, WHCF				Montresor, M; Sgrosso, S; Procaccini, G; Kooistra, WHCF			Intraspecific diversity in <i>Scrippsiella trochoidea</i> (Dinophyceae):: evidence for cryptic species	PHYCOLOGIA			English	Article							INTERNAL TRANSCRIBED SPACER; RECENT MARINE-SEDIMENTS; RIBOSOMAL DNA; DINOFLAGELLATE CYSTS; QUATERNARY EASTERN; SEQUENCES; ECOLOGY; REGION; RAPHIDOPHYCEAE; POPULATION	Scrippsiella trochoidea is a widely distributed neritic dinoflagellate that produces calcareous resting cysts. We assessed the level of intraspecific diversity at the molecular, morphological and physiological levels among 15 strains identified as S. trochoidea and isolated from the Gulf of Naples (Italy, Mediterranean Sea), and an additional isolate from the Faeroe Islands. We investigated the morphology of motile cells and cysts, mating modality, encystment success, and growth rates at different light irradiances. The ribosomal DNA internal transcribed spacer (ITS) region was sequenced to infer phylogenetic relationships among the S. trochoidea strains and closely related species. The molecular analysis revealed a well-supported lineage comprising strains with a Scrippsiella plate pattern. Within this clade, a number of distinct ITS haplotypes were recorded but the relationships among them were only partially resolved. The 16 S. trochoidea isolates grouped into five single-strain clades and three multi-strain clades. The grouping of haplotypes in a series of distinct clades suggests the existence of cryptic species within what has previously been considered a single species, based on the morphological features of the motile cells and cysts. Some of the ITS haplotypes were distinguishable visually, based on minor morphological features of the motile cells and cysts, but in two cases morphologically almost identical strains fell into different clades. Our results showed that the majority of the strains are homothallic; only S. trochoidea v. aciculifera from the Faeroe Islands is heterothallic. Cyst production rates were notable for their diversity, even among strains grouping with the same ITS haplotype, as were growth rates at different light irradiances. Based on phylogenetic results, two new combinations are proposed: S. operosa (Deflandre) Montresor comb. nov. and S. infula (Deflandre) Montresor comb. nov.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@alpha.szn.it	Procaccini, Gabriele/AAA-7040-2019; Procaccini, Gabriele/A-6618-2010	Montresor, Marina/0000-0002-2475-1787; Procaccini, Gabriele/0000-0002-6179-468X; Kooistra, Wiebe/0000-0002-8641-9739				ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; 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; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Arnheim N., 1983, P38; Balech E., 1966, NEOTROPICA, V12, P103; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. Mexico, V7, P57; Berard-Therriault L., 1999, Publication speciale canadienne des sciences halieutiques et aquatiques, V128; 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; Brand L. E., 1989, BIOL OCEANOGR, V6, P397; Coleman AW, 1997, J MOL EVOL, V45, P168, DOI 10.1007/PL00006217; Connell LB, 2000, MAR BIOL, V136, P953, DOI 10.1007/s002270000314; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1992, WOODS HOLE OCEANOGRA, P1; DEFLANDRE G, 1947, CR HEBD ACAD SCI, V224, P1781; Deflandre G., 1949, BOTANISTE, V34, P191; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; Doyle J. J., 1987, FOCUS, V19, P11; Durand C, 2002, J EVOLUTION BIOL, V15, P122, DOI 10.1046/j.1420-9101.2002.00370.x; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Fensome R.A., 1993, Micropaleontology Press Special Paper; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; GAO XP, 1989, PHYCOLOGIA, V28, P342; GAO XP, 1989, BRIT PHYCOL J, V24, P153; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; GREUTER W., 1994, International code of botanical nomenclature (Tokyo Code); Greuter W., 2000, INT CODE BOT NOMENCL; HALLEGRAEFF GM, 1992, MAR POLLUT BULL, V25, P186, DOI 10.1016/0025-326X(92)90223-S; HAVSKUM H, 1991, CALCIODINELLUM FAERO; HERNANDEZBECERRIL DU, 1987, NOVA HEDWIGIA, V45, P237; Hey J, 2001, TRENDS ECOL EVOL, V16, P326, DOI 10.1016/S0169-5347(01)02145-0; HILLIS DM, 1992, J HERED, V83, P189, DOI 10.1093/oxfordjournals.jhered.a111190; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; KELLER MD, 1987, J PHYCOL, V23, P633; Keupp H., 1989, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V106, P207; KISHINO H, 1989, J MOL EVOL, V29, P170, DOI 10.1007/BF02100115; KLIMYUK VI, 1993, PLANT J, V3, P493, DOI 10.1046/j.1365-313X.1993.t01-26-00999.x; Kohring Rolf, 1993, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V6, P1; Kooistra WHCF, 2001, J SEA RES, V46, P213, DOI 10.1016/S1385-1101(01)00086-7; LaJeunesse TC, 2001, J PHYCOL, V37, P866, DOI 10.1046/j.1529-8817.2001.01031.x; Larsen A, 1997, J PHYCOL, V33, P1007, DOI 10.1111/j.0022-3646.1997.01007.x; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; MADDISON WP, 1997, MACCLADE ANAL PHYLOG; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MUNOZ-S P, 1983, Revista de Biologia Marina, V19, P63; NEHRING S, 1995, HELGOLANDER MEERESUN, V49, P375, DOI 10.1007/BF02368363; Nichols R, 2001, TRENDS ECOL EVOL, V16, P358, DOI 10.1016/S0169-5347(01)02203-0; Okolodkov YB, 1998, SARSIA, V83, P267, DOI 10.1080/00364827.1998.10413687; PFIESTER LA, 1989, INT REV CYTOL, V114, P249; Posada D, 1998, BIOINFORMATICS, V14, P817, DOI 10.1093/bioinformatics/14.9.817; Procaccini G, 1996, MAR ECOL PROG SER, V140, P153, DOI 10.3354/meps140153; Rambaut A., 1995, SE AL SEQUENCE ALIGN; RISEBERG LH, 1993, HYBRID ZONES EVOLUTI, P70; Rynearson TA, 2000, LIMNOL OCEANOGR, V45, P1329, DOI 10.4319/lo.2000.45.6.1329; SANG T, 1995, P NATL ACAD SCI USA, V92, P6813, DOI 10.1073/pnas.92.15.6813; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; Sokal R.R., 1995, BIOMETRY; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; Steidinger K.A., 1997, IDENTIFYING MARINE P, P387; SWOFFORD DL, 2001, PAUPASTERISK PHYLOGE; TAMURA K, 1993, MOL BIOL EVOL, V10, P512, DOI 10.1093/oxfordjournals.molbev.a040023; Veron J.E.N., 1995, Corals in Space and Time: The Biogeography and Evolution of the Scleractinia; WENDEL JF, 1995, P NATL ACAD SCI USA, V92, P280, DOI 10.1073/pnas.92.1.280; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	68	141	152	3	29	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	JAN	2003	42	1					56	70		10.2216/i0031-8884-42-1-56.1	http://dx.doi.org/10.2216/i0031-8884-42-1-56.1			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	655EM					2025-03-11	WOS:000181538400007
C	Sheldon, E		Versteegh, G; Willems, H		Sheldon, E			New nannofossil dating of the initial early paleocene volcanism in Nuussuaq, central West Greenland	PROCEEDINGS OF THE 8TH INTERNATIONAL NANNOPLANKTON ASSOCIATION CONFERENCE	COURIER FORSCHUNGSINSTITUT SENCKENBERG SERIES		English	Proceedings Paper	8th Conference of the International-Nannoplankton-Association	SEP 11-15, 2000	Univ Bremen, Dept Hist Geol/Palaeontol, Bremen, GERMANY	Int Nannoplankton Assoc	Univ Bremen, Dept Hist Geol/Palaeontol	West Greenland; calcareous nannofossils; Paleocene; dinoflagellate cyst; biostratigraphy		Mudstones from the Nuussuaq Basin, onshore West Greenland (figs. 1, 2) yield calcareous nannofossils. The dating of these mudstones using nannofossils and dinoflagellate cysts has enabled a detailed Lower Paleocene biostratigraphic zonation to be established. Samples from four onshore wells and three outcrop sections yield low abundance and low diversity assemblages and date the youngest mudstones as Late Danian, upper nannofossil zones NP4 - ?lower NP5 (MARTINI 1971), correlating with NNTp5B (VAROL 1998). The nannofossil data and complimentary palynological dating not only allow a relatively accurate dating of the sediments deposited in the Early Paleocene, but along with published 40Ar/39Ar and magnetostratigraphic data provide more rigorous constraints on the timing of the initiation of volcanism onshore West Greenland and the North Atlantic Igneous province. Mudstones from the Nuussuaq Basin, onshore West Greenland (figs. 1, 2) yield calcareous nannofossils. The dating of these mudstones using nannofossils and dinoflagellate cysts has enabled a detailed Lower Paleocene biostratigraphic zonation to be established. Samples from four onshore wells and three outcrop sections yield low abundance and low diversity assemblages and date the youngest mudstones as Late Danian, upper nannofossil zones NP4 - ?lower NP5 (MARTINI 1971), correlating with NNTp5B (VAROL 1998). The nannofossil data and complimentary palynological dating not only allow a relatively accurate dating of the sediments deposited in the Early Paleocene, but along with published 40Ar/39Ar and magnetostratigraphic data provide more rigorous constraints on the timing of the initiation of volcanism onshore West Greenland and the North Atlantic Igneous province. Mudstones from the Nuussuaq Basin, onshore West Greenland (figs. 1, 2) yield calcareous nannofossils. The dating of these mudstones using nannofossils and dinoflagellate cysts has enabled a detailed Lower Paleocene biostratigraphic zonation to be established. Samples from four onshore wells and three outcrop sections yield low abundance and low diversity assemblages and date the youngest mudstones as Late Danian, upper nannofossil zones NP4 - ?lower NP5 (MARTINI 1971), correlating with NNTp5B (VAROL 1998). The nannofossil data and complimentary palynological dating not only allow a relatively accurate dating of the sediments deposited in the Early Paleocene, but along with published 40Ar/39Ar and magnetostratigraphic data provide more rigorous constraints on the timing of the initiation of volcanism onshore West Greenland and the North Atlantic Igneous province.	Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Ostervoldgade 10, DK-1350 Copenhagen K, Denmark.		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M., 1980, THESIS U COPENHAGEN, P1; HERNGREEN GFW, 1998, MEDEDELINGEN NEDERLA, V61, P3; JURGENSEN T, 1974, Bulletin of the Geological Society of Denmark, V23, P225; Mai H, 1999, MAR MICROPALEONTOL, V36, P1, DOI 10.1016/S0377-8398(98)00023-1; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; Nohr-Hansen H, 2000, GFF, V122, P115, DOI 10.1080/11035890001221115; Nohr-Hansen H, 2002, GEOL SOC SPEC PUBL, V197, P111, DOI 10.1144/GSL.SP.2002.197.01.06; NohrHansen H, 1997, GEOLOGY, V25, P851, DOI 10.1130/0091-7613(1997)025<0851:PASAAN>2.3.CO;2; NOHRHANSEN H, 2000, JAHRBUCH GEOLOGIE PA, V219, P153; PERCH-NIELSEN K, 1973, Bulletin of the Geological Society of Denmark, V22, P79; Perch-Nielsen K., 1985, P427; Piasecki S., 1992, RAPP GRONL GEOL UNDE, V154, P13, DOI DOI 10.34194/RAPGGU.V154.8166; Riisager P, 1999, GEOPHYS J INT, V137, P774, DOI 10.1046/j.1365-246x.1999.00830.x; SARGEANT WAS, 1974, FOSSIL LIVING DINOFL, P1; Sheldon Emma, 2000, Journal of Nannoplankton Research, V22, P199; Sikora PJ, 1999, GEOL SOC SPEC PUBL, V152, P113, DOI 10.1144/GSL.SP.1999.152.01.07; Storey M, 1998, EARTH PLANET SC LETT, V160, P569, DOI 10.1016/S0012-821X(98)00112-5; van Heck S.E., 1987, Abhandlungen der Geologischen Bundesanstalt (Vienna), V39, P285; VAROL O, 1989, BR MICROPAL, P267; Varol O., 1998, P200	28	1	1	0	1	E SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG	STUTTGART	JOHANNESTRASSE 3, W-7000 STUTTGART, GERMANY	0341-4116		3-510-61361-9	COUR FOR SEKENBG	Cour. Forschung Seckenbg.		2003	244						37	45						9	Marine & Freshwater Biology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology; Paleontology	BAG68					2025-03-11	WOS:000222119600003
C	Durán, I; Ruiz, M; Fasola, A; Lorente, MA		Versteegh, G; Willems, H		Durán, I; Ruiz, M; Fasola, A; Lorente, MA			Biofacies development related to upwelling systems based on high-resolution biostratigraphic studies in southwest Venezuela	PROCEEDINGS OF THE 8TH INTERNATIONAL NANNOPLANKTON ASSOCIATION CONFERENCE	COURIER FORSCHUNGSINSTITUT SENCKENBERG SERIES		English	Proceedings Paper	8th Conference of the International-Nannoplankton-Association	SEP 11-15, 2000	Univ Bremen, Dept Hist Geol/Palaeontol, Bremen, GERMANY	Int Nannoplankton Assoc	Univ Bremen, Dept Hist Geol/Palaeontol	Tethys; Upper Cretaceous; Venezuela; nannofossils; dinoflagellate cysts; foraminifera		New studies show evidence of repetitive upwelling events taking place in the southwestern Tethys margin from the Turonian through the Maastrichtian. On the basis of comparative analyses of sedimentological and biotic characteristics, seven subcropping sections from along the northern border of the Barinas Basin, southwestern Venezuela are interpreted environmentally. Zones II and III of the upwelling model (JONEs et al. 1983) were found to be represented by the sections. The presence of laminated dark shales, phosphate pellets, abundant fish debris, glauconite, diatoms, radiolaria, dinoflagellates, and biogenic chert, support the upwelling model within a continental shelf, with the upwelling centre located over the mid-inner shelf. The following biofacies are established: Planktic Foraminifers Biofacies (Key Association LCL) associated to light yellow glauconitic wackestones-mudstones, suggesting high productivity and well oxygenated marine conditions; Buliminids and Planktic Foraminifers, Diatoms, Radiolaria and Calcareous Nannoplankton Biofacies in dark grey calcareous shales with wackestones-mudstones (Key Association DCS) that we associated with Zone III; Diatoms, Radiolaria and Dinoflagellate Biofacies in dark grey shales and dolomites interstratified with yellow-brown sandstones and black phosphorites, indicative of Zone II, see fig. 5 (Key Association LSS); and Fish debris Biofacies in phosphorites and dark grey shales, associated with Zone III (Key Association P). Low diversity and high abundance assemblages, typical of opportunistic species characterise the microfaunal associations. These assemblages are considered survivors of anoxic to dysoxic conditions due to the upwelling. The subsequent high productivity conditions, associated to high salinity and low oxygen level of the water mass, result in high mortality which is reflected by the presence of fish debris and phosphate nodules. The biofacies succession shows a tendency of the upwelling to have changed from more distal during the Turonian-Coniacian to more proximal environments during the Santonian-Maastrichtian.	PDVSA, Explorat, Caracas 1010A, Venezuela	PDVSA	Durán, I (通讯作者)，PDVSA, Explorat, Apdo 829,Piso 13, Caracas 1010A, Venezuela.		FERNANDEZ, MIGUEL/Y-4230-2019					Barss M. S., 1973, 7326 GEOL SURV CAN; CODECIDO GF, 1972, 4 C GEOL VEN DIR GEO, V5, P773; DOUGLAS R, 1998, PALEOECOLOGIA PALEOA; DURAN I, 1966, NEW TOOL ENV INTERPR; Jones BH., 1983, Coastal Upwelling Its Sediment Record, P37; KISSER GD, 1989, RELACIONES ESTRATIGR; Parnaud F., 1995, AAPG Memoir, V62, P681; Renz O., 1959, Boletin de Geologia, V5, P3, DOI DOI 10.1016/j.chemgeo.2006.02.012; SILVA IP, 1999, GEOLOGICAL SOC AM SP, V332, P301, DOI DOI 10.1130/0-8137-2332-9.301	9	0	0	0	1	E SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG	STUTTGART	JOHANNESTRASSE 3, W-7000 STUTTGART, GERMANY	0341-4116		3-510-61361-9	COUR FOR SEKENBG			2003	244						47	59						13	Marine & Freshwater Biology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology; Paleontology	BAG68					2025-03-11	WOS:000222119600004
J	Turon, JL; Lézine, AM; Denèfle, M				Turon, JL; Lézine, AM; Denèfle, M			Land-sea correlations for the last glaciation inferred from a pollen and dinocyst record from the Portuguese margin	QUATERNARY RESEARCH			English	Article						pollen; dinocysts; Eastern Atlantic; last glacial; heinrich events; paleoenvironments; paleoclimate	NORTH-ATLANTIC OCEAN; ACCELERATOR MASS-SPECTROMETRY; ICE-RAFTED DETRITUS; HEINRICH EVENTS; ICEBERG DISCHARGES; INTERGLACIAL TRANSITION; SURFACE TEMPERATURE; VEGETATION HISTORY; IBERIAN PENINSULA; CLIMATIC CHANGES	Pollen and dinoflagellate cyst assemblages from Core SU 81-18 recovered off Portugal (37degrees46'N, 10degrees11'W; 3135-m water depth) have been used to document the short-term environmental changes that occurred in southwest Europe since 25,000 yr B.P. The relationship between the oceanic and continental environments has been further examined by the use of other marine proxies (coarse sedimentary fraction, foraminifera.) and by comparison with proximal land pollen records. Heinrich 2 (H2) and Heinrich 1 (111) events were the most extreme parts of the highly variable last glacial period, with the maximum extension of dry steppe on land and the occurrence of cool and dilute waters at the core site. Our study shows that H I and H2 are divided in two distinct phases: one with Neogloboquadrina pachyderma left coiling associated with the maximum input of ice rafted debris, reflecting the in situ release of icebergs and the occurrence of cool and dilute seawater at the core site; the other with dinoflagellate cysts of subpolar affinity, Bitectatodinium tepikiense, reflecting a seasonal control marked by warm summer SST and cold winter SST. (C) 2003 Elsevier Science (USA). All rights reserved.	Univ Bordeaux 1, EPOC UMR CNRS 5805, Dept Geol & Oceanog, F-33405 Talence, France; CNRS, URA141, F-92195 Meudon, France; Univ Paris 06, CNRS, ESA Paleontol & Stratig 7073, F-75252 Paris, France	Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS)	Turon, JL (通讯作者)，Univ Bordeaux 1, EPOC UMR CNRS 5805, Dept Geol & Oceanog, F-33405 Talence, France.		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Res.	JAN	2003	59	1					88	96		10.1016/S0033-5894(02)00018-2	http://dx.doi.org/10.1016/S0033-5894(02)00018-2			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	652YF					2025-03-11	WOS:000181407900010
J	Schioler, P; Crampton, JS; Laird, MG				Schioler, P; Crampton, JS; Laird, MG			Palynofacies and sea-level changes in the Middle Coniacian-Late Campanian (Late Cretaceous) of the East Coast Basin, New Zealand	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						New Zealand; Late Cretaceous; biostratigraphy; palynology; palynofacies; sequence stratigraphy	NORTHEAST SOUTH-ISLAND; DINOFLAGELLATE CYSTS; TERTIARY BOUNDARY; ORGANIC FACIES; ADJACENT SEAS; BIOSTRATIGRAPHY; STRATIGRAPHY; SEDIMENTS; PIRIPAUAN; SECTIONS	A palynofacies analysis of four sections through the Paton and Herring Formations of the East Coast Basin in southern Marlborough indicates that the two formations were deposited on the inner to mid-shelf in a marine environment with conspicuous input of plant material from adjacent land area. The Paton Formation was deposited on the inner to mid-shelf under oxic conditions and in proximity to a river delta, possibly in a deltafront setting. Its lower part is clearly less marine than its upper part, pointing to an overall deepening trend with time. The deposition of the Herring Formation took place farther offshore, on the mid-shelf, in a mud-dominated environment under poorly oxygenated conditions at the sediment/water interface, following a landward shift of shoreline. A stratigraphic analysis of changes in palynofacies and lithology through the four sections allows a breakdown of the succession into seven depositional sequences, separated by unconformities or their correlative conformities. A regional sea-level curve for the Middle Coniacian-Upper Campanian in the East Coast Basin is proposed on the basis of the inferred sequences and chronostratigraphic control from dinoflagellate biostratigraphy. The sea-level cycles thus inferred for the East Coast Basin show a poor correlation with the re-scaled Haq cycle chart, suggesting that regional tectonics rather than eustasi controlled the East Coast Basin sequences. (C) 2002 Elsevier Science B.V. All rights reserved.	Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark; Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Univ Canterbury, Dept Geol Sci, Christchurch 1, New Zealand	Geological Survey Of Denmark & Greenland; GNS Science - New Zealand; University of Canterbury	Schioler, P (通讯作者)，Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen, Denmark.		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Paleoclimatol. Paleoecol.	DEC 5	2002	188	3-4					101	125	PII S0031-0182(02)00548-5	10.1016/S0031-0182(02)00548-5	http://dx.doi.org/10.1016/S0031-0182(02)00548-5			25	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	621QU					2025-03-11	WOS:000179601600001
J	Riding, JB; Crame, JA				Riding, JB; Crame, JA			Aptian to Coniacian (Early-Late Cretaceous) palynostratigraphy of the Gustav Group, James Ross Basin, Antarctica	CRETACEOUS RESEARCH			English	Article						James Ross Basin; Antarctica; Cretaceous palynostratigraphy; dinoflagellate cysts	BACK-ARC BASIN; PENINSULA REGION; ISLAND AREA; STRATIGRAPHY; PALYNOLOGY; POINT; STAGE; AGE	The Gustav Group, of the James Ross Basin, Antarctic Peninsula, forms part of a major Southern Hemisphere Cretaceous reference section. Palynological data, chiefly from dinoflagellate cysts, integrated with macrofaunal evidence and strontium isotope stratigraphy, indicate that the Gustav Group, which is approximately 2.6 km thick, is Aptian-Coniacian in age. Aptian-Coniacian palynofloras in the James Ross Basin closely resemble coeval associations from Australia and New Zealand, and Australian palynological zonation schemes are applicable to the Gustav Group. The lowermost units, the coeval Pedersen and Lagrelius Point formations, have both yielded early Aptian dinoflagellate cysts. Because the overlying Kotick Poirit Formation is of early to mid Albian age, the Aptian/Albian boundary is placed, questionably, at the Lagrelius Point Formation-Kotick Point Formation boundary on James Ross Island, and this transition may be unconformable. Although the Kotick Point Formation is largely early Albian on dinoflagellate cyst evidence, the uppermost part of the formation appears to be of mid Albian age. This differentiation of the early and mid Albian has refined the age of the formation, previously considered to,be Aptian-Alblan, based on macrofaunal evidence. The Whisky Bay Formation is of late Albian to latest Turonian age on dinoflagellate cyst evidence and this supports the macrofaunal ages. Late Albian palynofloras have been recorded from the Gin Cove, lower Tumbledown Cliffs, Bibby Point and the lower-middle Lewis Hill members. However, the Cenomanian age of the upper Tumbledown Cliffs and Rum Cove members, based on molluscan evidence, is not supported by the dinoflagellate cyst floras and further work is required on this succession. The uppermost part of the Whisky Bay Formation in north-west James Ross Island is of mid to late Turonian age and this is confirmed by strontium isotope stratigraphy. The uppermost unit, the Hidden Lake Formation, is Coniacian in age on both palaeontological and strontium isotope evidence. The uppermost part of the formation appears to be early Santonian based on dinoflagellate cysts, but strontium isotope stratigraphy constrains this as being no younger than late Coniacian. This refined palynostratigraphy greatly improves the potential of the James Ross Basin as a major Cretaceous Southern Hemisphere reference section. (C) 2003 Published by Elsevier Science Ltd.	British Geol Survey, Keyworth NG12 5GG, Notts, England; British Antarctic Survey, Cambridge CB3 0ET, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.							[Anonymous], 1983, BR ATARCTIC SURV B; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 1989, Journal of South American Earth Sciences; Backhouse J., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P205; BACKHOUSE J, 1988, B GEOLOGICAL SURVEY, V135; Baldoni A.M., 1989, Ser Cient. 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L., 1998, AM ASS STRATIGRAPHIC, V34; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; Zinsmeister William J., 1996, P303; [No title captured]	86	54	63	0	2	ACADEMIC PRESS LTD ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	DEC	2002	23	6					739	760		10.1006/cres.2002.1024	http://dx.doi.org/10.1006/cres.2002.1024			22	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	692RD					2025-03-11	WOS:000183673300005
J	Ibrahim, MIA				Ibrahim, MIA			Late Albian-Middle Cenomanian palynofacies and palynostratigraphy, Abu Gharadig-5 well, Western Desert, Egypt	CRETACEOUS RESEARCH			English	Article						Kharita; Bahariya; Egypt; Albian; Cenomanian; TOC; palynomorphs; palaeoenvironment; hydrocarbons; source potential	CRETACEOUS PHYTOGEOPROVINCES; DINOFLAGELLATE CYSTS; OIL-FIELD; POLLEN; PALYNOMORPHS; FORAMINIFERA; PALYNOLOGY; SEDIMENTS; BIOSTRATIGRAPHY; MICROPLANKTON	Quantitative analyses of palynomorph assemblages, particulate organic matter (kerogen), and total organic carbon (TOC) have been made on samples of the Albian-Cenomanian Kharita and Bahariya formations encountered in the Abu Gharadig-5 well, Western Desert, Egypt. Two assemblage palynozones are defined: Assemblage Zone A (Kharita Formation) of late Albian-early Cenomanian age and Assemblage Zone B (Bahariya Formation) of early-middle Cenomanian age. Palynofacies of the Kharita Formation suggest that sedimentation of these strata took place in a warm, shallow, nearshore-marine environment. The deposition of the lower Bahariya Formation took place initially in similar conditions but subsequently further offshore in somewhat deeper water of the inner shelf. The relatively high percentage of Ephedripites, Afropollis and elaterate pollen in both formations indicates an and climate. The Kharita Formation yields kerogen types III and IV whereas the assemblages recovered from the Bahariya Formation contain types II and III. The TOC is generally between 0.42 and 0.65% in the Kharita Formation, while it ranges between 0.42 and 0.80% in samples of the Bahariya Formation. The spores and pollen grains are pale in colour, hence little source potential for hydrocarbons is indicated. (C) 2003 Published by Elsevier Science Ltd.	Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria 21511, Egypt	Egyptian Knowledge Bank (EKB); Alexandria University	Ibrahim, MIA (通讯作者)，Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria 21511, Egypt.		Ibrahim, Mohammed/IUQ-7100-2023	Ibrahim, Mohamed Ismail Abdou/0000-0002-5782-0435				Abdel-Kireem M R., 1993, Geoscientific Research in Northeast Africa, P375; Abdel-Kireem M. 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Res.	DEC	2002	23	6					775	788		10.1006/cres.2002.1027	http://dx.doi.org/10.1006/cres.2002.1027			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	692RD					2025-03-11	WOS:000183673300007
J	Rat'kova, TN; Wassmann, P				Rat'kova, TN; Wassmann, P			Seasonal variation and spatial distribution of phyto- and protozooplankton in the central Barents Sea	JOURNAL OF MARINE SYSTEMS			English	Article						Arctic; Barents Sea; picoplankton; nanoplankton; microplankton; seasonal succession; microbial loop; top-down regulation	NORTH NORWEGIAN SHELF; MARGINAL ICE-ZONE; CALANUS-GLACIALIS; BIOMASS; CARBON; ABUNDANCE; PHYTOPLANKTON; DYNAMICS; BLOOM; EDGE	Seasonal and geographical variations of suspended single-celled organisms on a transect across the western part of the Barents Sea in March and May 1998 and in June-July 1999 revealed that pico- and nanoplankton flagellates and monads (< 2 and 2-20 mum, respectively) entirely dominated total algae and protozoa numbers and biomass in March and in June-July, but in May, microplankton (>20 mum) prevailed in total biomass, In general, spring bloom progresses independently of the southern part of the Atlantic Water (AW) and follows the receding ice edge in the Arctic Water (ArW) to the north. The blooms started almost simultaneously and had similar composition (small diatom Chaetoceros socialis dominated total phytoplankton biomass) in both localities, so the share of resting spores, indicating the age of the bloom, differed markedly. As for underwater rise-the Sentralbanken (SBW) altered this pattern, and the spring bloom spreads from north to the south from the rise to the trench. The next stage of the bloom was dominated by the large diatoms Thalassiosira antarctica var. borealis above the Sentralbanken, in the Polar Front (PF) and in the ice-edge areas. In the southern part of transect, this stage of the spring bloom had a delay or was absent due to low stability of water column and/or due to grazing impact. The presence of ribbon-shaped forming species indicated the earlier stage of bloom in Marginal Ice Zone (MIZ). In May 1998 as well as in June/July 1999, at the ice-covered stations, early spring conditions-rather similar to the conditions in March 1998-were observed. Summer conditions at most of the stations in June-July 1999 were characterized by high species diversity of diatoms and dinoflagellates. High abundance of heterotrophic dinoflagellates and protozoans indicated the active functioning of the microbial loop in the nutritive chains. (C) 2002 Elsevier Science B.V. All rights reserved.	Russian Acad Sci, PP Shirshov Oceanol Inst, Moscow 117851, Russia; Univ Tromso, Norwegian Coll Fishery Sci, N-9037 Tromso, Norway	Russian Academy of Sciences; Shirshov Institute of Oceanology; UiT The Arctic University of Tromso	Russian Acad Sci, PP Shirshov Oceanol Inst, Nakhimovsky Ave 36, Moscow 117851, Russia.	trat@orc.ru						ADLANDSVIK B, 1991, POLAR RES, V10, P45, DOI 10.1111/j.1751-8369.1991.tb00633.x; ALLEN AE, 2002, J MAR SYST; ARASHKEVICH E, 2002, J MAR SYST; ARASHKEVICH EG, 1984, OKEANOLOGIYA+, V24, P677; AZAM F, 1991, POLAR RES, V10, P239, DOI 10.1111/j.1751-8369.1991.tb00649.x; Backhaus JO, 1999, MAR ECOL PROG SER, V189, P77, DOI 10.3354/meps189077; BATHMANN UV, 1990, MAR ECOL PROG SER, V60, P225, DOI 10.3354/meps060225; BRAARUD T, 1953, CONSEIL PERMANENT IN, V133, P1; BURSA AS, 1963, S MARINE MICROBIOLOG, P625; Druzhkov N.V., 1997, PLANKTON SEA W ARCTI, P145; DRUZHKOV NV, 1992, STRUCTURAL CHARACTER, P83; DRUZHKOV NV, 1992, ROLE AUTOTROPHIC NAN, P97; EILERTSEN HC, 1989, POLAR BIOL, V9, P253, DOI 10.1007/BF00263773; EVENSEN A, 1994, THESIS U TROMSO, P137; Falk-Petersen S, 2000, J MARINE SYST, V27, P131, DOI 10.1016/S0924-7963(00)00064-6; GARRISON DL, 1989, POLAR BIOL, V9, P341, DOI 10.1007/BF00442524; Gradinger R, 1999, DEEP-SEA RES PT II, V46, P1457, DOI 10.1016/S0967-0645(99)00030-2; Guillard R.R.L., 1978, Phytoplankton Manua", P182; Hansen B, 1996, POLAR BIOL, V16, P115; HANSEN B, 1990, MAR BIOL, V104, P5, DOI 10.1007/BF01313151; Hansen GA, 1995, ECOLOGY OF FJORDS AND COASTAL WATERS, P73; HASLE GR, 1997, IDENTIFYING MARINE P, P334; Hegseth EN, 1995, ECOLOGY OF FJORDS AND COASTAL WATERS, P45; Hegseth EN, 1998, POLAR RES, V17, P113, DOI 10.1111/j.1751-8369.1998.tb00266.x; KASHKIN NI, 1964, T OKEANOL I AKAD NAU, V65, P49; KONOVALOVA GV, 1998, DINOFLAGELLATAE FAR; KRISTIANSEN S, 1994, LIMNOL OCEANOGR, V39, P1630, DOI 10.4319/lo.1994.39.7.1630; KRISTIANSEN S, 1991, POLAR RES, V10, P187, DOI 10.1111/j.1751-8369.1991.tb00644.x; LAPPALAINEN TN, 1960, T MURMANSK MORSK BIO, V2, P41; Larionov V.V., 1997, PLANKTON MOREI ZAPAD, P65; LOENG H, 1991, POLAR RES, V10, P5, DOI 10.1111/j.1751-8369.1991.tb00630.x; Luchetta A, 2000, J MARINE SYST, V27, P177, DOI 10.1016/S0924-7963(00)00066-X; MAKAREVICH PR, 1992, PHYTOPLANKTON BARENT, P17; MAKAREVICH PR, 1994, ALGOLOGIA, V1, P113; Menden-Deuer S, 2000, LIMNOL OCEANOGR, V45, P569, DOI 10.4319/lo.2000.45.3.0569; MIKHAILOVSKY GE, 1989, OKEANOLOGIYA+, V29, P796; Okolodkov YB, 1998, SARSIA, V83, P267, DOI 10.1080/00364827.1998.10413687; OLLI K, 2002, J MAR SYST; Owrid G, 2000, POLAR RES, V19, P155, DOI 10.1111/j.1751-8369.2000.tb00340.x; Pautova L. 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Mar. Syst.	DEC	2002	38	1-2					47	75	PII S0924-7963(02)00169-0	10.1016/S0924-7963(02)00169-0	http://dx.doi.org/10.1016/S0924-7963(02)00169-0			29	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	619WF					2025-03-11	WOS:000179499900004
J	Wakefield, MI; Monteil, E				Wakefield, MI; Monteil, E			Biosequence stratigraphical and palaeoenvironmental findings from the Cretaceous through Tertiary succession, Central Indus Basin, Pakistan	JOURNAL OF MICROPALAEONTOLOGY			English	Article							LOWER MAESTRICHTIAN FORAMINIFERA; DINOFLAGELLATE CYSTS; PALEOSLOPE MODEL; SEDIMENTS; PATTERNS; SYSTEMS; OCEAN; SEA	Integrated analysis of foraminiferal and palynological data from the Duljan-1 well, Central Indus Basin, Pakistan, is used to identify critical surfaces (candidate sequence boundaries (SB) and maximum flooding surfaces (MFS)) and construct a biosequence stratigraphical framework. Within the Barremian through Bartonian-Priabonian? succession 15 depositional sequences have been recognized, each with a candidate MFS. These biosequences are shown to equate with the local lithostratigraphy and tentatively with the 'global' large-scale depositional cycles of Haq et al. (1987). Detailed dating has enabled seven candidate MFS to be tentatively equated with MFS identified on the nearby Arabian plate (Sharland et al., 2001). A combination of detailed age dating and palaeobathymetric determinations indicates significant basin uplift and erosion at end Cretaceous and end Eocene times, the latter coinciding with closure of Neo-Tethys. Smaller-scale unconformities are also noted. Multi-disciplinary palaeoenvironmental interpretations enable recognition of detailed changes in water mass conditions. Palynological data suggest these changes result from variations in terrestrial/freshwater input, though evidence of periodically low oxygen bottom water conditions/shallowing of the oxygen minimum zone, possibly 'Oceanic Anoxic Event-2' (OAE-2; late Cenomanian-Turonian) is suggested as a further control.	BG Grp, Reading RG6 1PT, Berks, England; Geosci Australia, Canberra, ACT 2601, Australia	Royal Dutch Shell; BG Group; Geoscience Australia	BG Grp, 100 Thames Valley Pk Dr, Reading RG6 1PT, Berks, England.							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DEC	2002	21		2				115	130		10.1144/jm.21.2.115	http://dx.doi.org/10.1144/jm.21.2.115			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	664NR		hybrid			2025-03-11	WOS:000182067600003
J	Head, MJ				Head, MJ			<i>Echinidinium zonneveldiae</i> sp nov., a dinoflagellate cyst from the Late Pleistocene of the Baltic Sea, northern Europe	JOURNAL OF MICROPALAEONTOLOGY			English	Article								The dinoflagellate cyst species Echinidinium zonneveldiae sp. nov. is described from last interglacial (Eemian Stage; Upper Pleistocene) deposits of the southern Baltic Sea, where it contributes to the characterization of a diverse interglacial dinoflagellate flora represented by more than 50 species. Echinidinium zonneveldiae is a probable heterotrophic species and does not occur in the region today. The nomenclatural status of the genus Echinidinium Zonneveld, 1997 ex Head et al., 2001 a is clarified, and it is noted that two of the seven species assigned to Echinidinium are not validly described.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England	University of Cambridge	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk						ABE TH, 1981, KYOTO U PUBL SETO MA, V6, P1; Balech E., 1988, Publ. Espec. Inst. Esp. Oceanogr., V1, P1; Brenner WW, 2001, NEUES JAHRB GEOL P-A, V219, P229, DOI 10.1127/njgpa/219/2001/229; BUTSCHLI O., 1885, KLASSEN ORDNUNGEN TH, P865; Fensome R.A., 1993, CLASSIFICATION FOSSI; Funder S, 2002, PALAEOGEOGR PALAEOCL, V184, P275, DOI 10.1016/S0031-0182(02)00256-0; Greuter W., 2000, Regnum Vegetabile, V138, P1; Haeckel E., 1894, SYSTEMATISCHE PHYLOG, P1; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HEAD MJ, 2001, BALT SEA SCI C NOV 2, V79; Kristensen P, 2000, BOREAS, V29, P103, DOI 10.1080/030094800750044295; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 2000, DEEP-SEA RES PT II, V47, P2229, DOI 10.1016/S0967-0645(00)00023-0; ZONNEVELD KAF, 1996, LPP CONTRIBUTIONS SE, V3, P1	15	24	24	0	3	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	DEC	2002	21		2				169	173		10.1144/jm.21.2.169	http://dx.doi.org/10.1144/jm.21.2.169			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	664NR		hybrid			2025-03-11	WOS:000182067600009
J	Burkholder, JM; Glasgow, HB				Burkholder, JM; Glasgow, HB			The life cycle and toxicity of <i>Pfiesteria piscicida</i> revisited	JOURNAL OF PHYCOLOGY			English	Editorial Material						amoebae; dinoflagellates; division cysts; life cycles; nuclear cyclosis; Pfiesteria; sexual reproduction; toxic zoospores; vegetative reproduction	RAT PITUITARY-CELLS; PARASITIC DINOFLAGELLATE; ENDEMIC STICKLEBACK; COMPLEX; DINOPHYCEAE; IDENTIFICATION; ASSOCIATION; MORPHOLOGY; HISTORIES; RECEPTOR	Despite use of excellent molecular techniques, Litaker et al. (2002) cannot provide insights about the life history of toxic Pfiesteria piscicida because they showed no data in support of having used toxic strains; rather they presented evidence that they used non-inducible strains. Litaker et al. did not find amoeboid stages or a chrysophyte-like cyst stage in several cultures and unequivocally concluded that the stages do not exist in all P. piscicida strains. Thus, they did not consider the tenet that absence of evidence does not constitute proof of absence. Apparent discrepancies between the research by Litaker et al. and previous research on Pfiesteria can be resolved as follows: First, Litaker et al. did not use toxic strains. We have reported findings (similar to Litaker et al.) showing few amoeboid transformations in non-inducible strains, which manifest some but not all of the forms that have been documented in some toxic strains. We, and others, have documented active toxicity to fish, transformations to amoebae, and chrysophyte-like cysts in some clonal toxic strains. Second, the data from several recent publications, which were available but not mentioned by Litaker et al. or by Coats (2002) in accompanying commentary, have verified P. piscicida amoebae, chrysophyte-like cysts, and other stages in some toxic strains through a combination of approaches including PCR data from clonal cultures.	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.	joann_burkholder@ncsu.edu						Appleton PL, 1998, PARASITOLOGY, V116, P115, DOI 10.1017/S0031182097002096; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C.A., 1984, P263; Beam C. 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A., 1999, Virginia Journal of Science, V50, P325; Samet J, 2001, ENVIRON HEALTH PERSP, V109, P639, DOI 10.2307/3454910; Seaborn David W., 1999, Virginia Journal of Science, V50, P337; SPERO HJ, 1981, J PHYCOL, V17, P43, DOI 10.1111/j.1529-8817.1981.tb00817.x; SPRINGER J, 2002, IN PRESS MAR ECOL PR; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Stoecker DK, 2002, AQUAT MICROB ECOL, V28, P79, DOI 10.3354/ame028079; TURGEON DD, 2001, PROTOCOLS MONITORING; Von Stosch HA., 1973, Br Phycol J, V8, P105	55	17	19	1	11	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	DEC	2002	38	6					1261	1267		10.1046/j.1529-8817.2002.02096.x	http://dx.doi.org/10.1046/j.1529-8817.2002.02096.x			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	627CG					2025-03-11	WOS:000179910900021
J	Litaker, RW; Vandersea, MW; Kibler, SR; Noga, EJ; Tester, PA				Litaker, RW; Vandersea, MW; Kibler, SR; Noga, EJ; Tester, PA			Reply to comment on the life cycle and toxicity of <i>Pfiesteria piscicida</i> revisited	JOURNAL OF PHYCOLOGY			English	Editorial Material						Pfiesteria; amoeba; dinoflagellate; division cyst; life cycle; meiosis; sexual reproduction	ALEXANDRIUM-TAYLORI DINOPHYCEAE; SEXUAL REPRODUCTION; DINOFLAGELLATE; HISTORY; COMPLEX; PYRROPHYTA	Free-living, marine dinoflagellates are typified by a well-defined, haplontic life cycle with relatively few stages. The most unusual departure from this life cycle is one reported for the heterotrophic dinoflagellate Pfiesteria piscicida Steidinger et Burkholder. This species is alleged to have at least 24 life cycle stages including amoebae and a chrysophyte-like cyst form (Burkholder et al. 1992, Burkholder and Glasgow 1997a) not previously known in free-living marine dinoflagellates. Litaker et al. (2002) redescribed the life cycle of P. piscicida from single-cell isolates and found only life cycle stages typical of free-living marine dinoflagellates. The discrepancy between these observations and the life cycle reported in the literature prompted a rigorous study to resolve the life cycle of P. piscicida. Burkholder and Glasgow (2002) took exception to this study, arguing that Litaker et al. (2002) misunderstood the life cycle of P. piscicida and ignored recent publications. We present a rebuttal of their criticisms and suggest a simple way to resolve the discrepancies in the P. piscicida life cycle.	Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, NOAA, Beaufort, NC 28516 USA; N Carolina State Univ, Coll Vet Med, Raleigh, NC 27606 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; North Carolina State University	Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, NOAA, 101 Pivers Isl Rd, Beaufort, NC 28516 USA.	wayne_litaker@med.unc.edu	Litaker, Richard/AAH-2036-2021					BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C.A., 1984, P263; Beam C. A., 1980, BIOCH PHYSL PROTOZOA, V3, P171; BHAUD Y, 1988, J CELL SCI, V89, P197; Burkholder JM, 2002, J PHYCOL, V38, P1261, DOI 10.1046/j.1529-8817.2002.02096.x; 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, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; BURSA A, 1970, ARCTIC ALPINE RES, V1, P152; 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; DREBES G, 1988, HELGOLANDER MEERESUN, V42, P563, DOI 10.1007/BF02365627; FAUST MA, 1993, DEV MAR BIO, V3, P121; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Gordon A. S., 2002, Harmful Algae, V1, P85, DOI 10.1016/S1568-9883(02)00008-2; KELLEY I, 1990, J PHYCOL, V26, P167, DOI 10.1111/j.0022-3646.1990.00167.x; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; 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; Melo AC, 2001, ENVIRON HEALTH PERSP, V109, P731, DOI 10.2307/3454920; Moeller PDR, 2001, ENVIRON HEALTH PERSP, V109, P739, DOI 10.2307/3454921; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; Parrow Matthew, 2002, Harmful Algae, V1, P5, DOI 10.1016/S1568-9883(02)00009-4; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; PFIESTER LA, 1984, AM J BOT, V71, P1121, DOI 10.2307/2443388; PFIESTER LA, 1979, NATURE, V279, P421, DOI 10.1038/279421a0; POPOVSKY J, 1982, ARCH PROTISTENKD, V125, P115, DOI 10.1016/S0003-9365(82)80011-0; TOFFER KL, 1998, HARMFUL ALGAE, P278; Von Stosch HA., 1973, Br Phycol J, V8, P105; WALKER LM, 1979, J PHYCOL, V15, P312; Walter P., 2002, MOL BIOL CELL	35	6	6	1	5	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	DEC	2002	38	6					1268	1272		10.1046/j.1529-8817.2002.02133.x	http://dx.doi.org/10.1046/j.1529-8817.2002.02133.x			5	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	627CG					2025-03-11	WOS:000179910900022
J	Harper, FM; Hatfield, EA; Thompson, RJ				Harper, FM; Hatfield, EA; Thompson, RJ			Recirculation of dinoflagellate cysts by the mussel, <i>Mytilus edulis</i> L., at an aquaculture site contaminated by <i>Alexandrium fundyense</i> (Lebour) Balech	JOURNAL OF SHELLFISH RESEARCH			English	Article						dinoflagellate; Alexandrium; cysts; mussel; aquaculture; PSP	GONYAULAX-EXCAVATA; RESTING CYSTS; OSTENFELDII DINOPHYCEAE; SEDIMENTS; TOXICITY; BLOOMS; BIODEPOSITION; GERMINATION; TAMARENSIS; BAY	Holding suspension-feeding bivalves at an aquaculture site may facilitate the maintenance of toxic dinoflagellate populations by concentrating transient vegetative cells or resuspended cysts. To examine the role of the mussel, Mytilus edulis, in recirculating cysts within an aquaculture site contaminated with the dinoflagellate Alexandrium fundyense, sediment cores and fecal samples were collected in September and October 1996. In the interim period, a bloom of A. fundyense vegetative cells began. Mussels egested similar concentrations of dinoflagellate cysts (Scrippsiella sp., A. fundyense, and an unknown Grey species) regardless of the location of the mussel sock in the site, or the position of the mussel in the water column. In September, more putative A. ostenfeldii cysts were egested in feces collected from the bottom of two socks than in those from the top. One sock was located at greater depths near a barrier island and the other in a shallow northeastern cove. Within each dinoflagellate species, there were no significant differences between cyst concentrations in sediment throughout the site, the exception being the high concentrations in September of putative A. ostenfeldii beneath the sock located near a barrier island (182 cysts(.)cm(-3)). Post-bloom, there were significantly fewer A. fundyense cysts in the sediment underlying the sock near a barrier island. In contrast, there were significantly more putative A. ostenfeldii cysts in the sediment in the shallow northeastern cove (580 cysts-cm(-3)). The daily replenishment rate of A. ostenfeldii cysts in bottom sediments by mussel fecal deposition was estimated as 2 x 10(5) Cysts m(-2) d(-1), or about 8%. This may be a considerable contribution to the maintenance of this dinoflagellate species in a mussel aquaculture site, but further studies are required to compare other inputs and outputs of cysts to establish the relative importance of bivalve aquaculture.	Mem Univ Newfoundland, Ctr Ocean Sci, St John, NF A1C 5S7, Canada	Memorial University Newfoundland	Dalhousie Univ, Dept Biol, Halifax, NS B3H 4J1, Canada.							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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.	DEC	2002	21	2					471	477						7	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	638ND					2025-03-11	WOS:000180576400010
J	Jago, CF; Jones, SE				Jago, CF; Jones, SE			Diagnostic criteria for reconstruction of tidal continental shelf regimes: changing the paradigm	MARINE GEOLOGY			English	Article; Proceedings Paper	Geoscience 2000 Conference	APR, 2000	UNIV MANCHESTER, MANCHESTER, ENGLAND		UNIV MANCHESTER	biogeochemical flux; tidal shelf deposits; fine sediments	SOUTHERN NORTH-SEA; DINOFLAGELLATE BLOOMS; PARTICLE AGGREGATION; PHYTOPLANKTON BLOOMS; CHLOROPHYLL MAXIMUM; VERTICAL STRUCTURE; SUSPENDED MATTER; SAND TRANSPORT; THERMAL FRONT; DIATOM BLOOM	A biogeochemical flux paradigm is presented which provides a conceptual and numerical framework for reconstructing the dynamical and biogeochemical regimes of ancient tide-driven continental shelves. The paradigm links turbulence. primary production. and suspended particulate matter flux in the water column to microbiological and isotopic proxies in the sediment record and identifies the diagnostic signatures of sediments deposited in stratified. frontal, and mixed dynamic regimes of tidal shelves. The critical governing processes in the water column and at the sediment/water interface are temperature, particulate organic carbon supply. and benthic oxygen consumption, which exhibit strong gradients across tidal mixing fronts, The diagnostic proxies in the sediment record are microplanktonic (e.g. dinoflagellate cysts) and microbenthic (e.g, foraminifera) and their associated stable isotopic properties. Advanced numerical models are available which incorporate biophysical coupling in the water column and benthic boundary layer and which simulate biogeochemical and ecological processes and organic fluxes to the seabed. These models offer potential advances for interpreting microbiological and isotopic proxies of biogeochemical regime preserved in the fine sediment record. Quaternary shelf deposits provide the best potential validation of the biogeochemical flux paradigm since most Quaternary species are living today. but the paradigm is applicable to ancient tidal shelf deposits. The paradigm is particularly applicable to the fine sediment record which potentially preserves the most complete history of shelf evolution. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Wales, Sch Ocean Sci, Marine Sci Labs, Bangor LL59 5AB, Gwynedd, Wales	Bangor University	Univ Wales, Sch Ocean Sci, Marine Sci Labs, Bangor LL59 5AB, Gwynedd, Wales.	c.f.jago@bangor.ac.uk						ALLDREDGE AL, 1993, DEEP-SEA RES PT I, V40, P1131, DOI 10.1016/0967-0637(93)90129-Q; ALLDREDGE AL, 1988, LIMNOL OCEANOGR, V33, P339, DOI 10.4319/lo.1988.33.3.0339; ANDERSON GC, 1969, LIMNOL OCEANOGR, V14, P386, DOI 10.4319/lo.1969.14.3.0386; ANDERTON R, 1976, SEDIMENTOLOGY, V23, P429, DOI 10.1111/j.1365-3091.1976.tb00062.x; [Anonymous], 1985, Proceedings of the 19th European Marine Biology Symposium, 1985 1985; [Anonymous], COASTAL ESTUARINE SC, DOI DOI 10.1029/C0003P0063; 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; Bale AJ, 1998, CONT SHELF RES, V18, P1333, DOI 10.1016/S0278-4343(98)00046-6; BANKS NL, 1973, SEDIMENTOLOGY, V20, P213, DOI 10.1111/j.1365-3091.1973.tb02046.x; Beardall J., 1978, Biologia Contemporanea, V5, P163; 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Geol.	NOV 30	2002	191	3-4					95	117	PII S0025-3227(02)00527-3	10.1016/S0025-3227(02)00527-3	http://dx.doi.org/10.1016/S0025-3227(02)00527-3			23	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Oceanography	616GN					2025-03-11	WOS:000179296200002
J	Howe, JA; Harland, R; Pudsey, CJ				Howe, JA; Harland, R; Pudsey, CJ			Dinoflagellate cyst evidence for Quaternary palaeoceanographic change in the northern Scotia Sea, South Atlantic Ocean	MARINE GEOLOGY			English	Article						Antarctic Circumpolar Current; dinollagellate cysts; palaeoceanography; glacial cycles; radiocarbon dating	ANTARCTIC CIRCUMPOLAR CURRENT; FALKLAND TROUGH; WEDDELL SEAS; DEEP-WATER; SEDIMENTS; PRESERVATION; CIRCULATION; CLIMATE; HISTORY; EVENTS	A dinoflagellate cyst record has been examined from two cores recovered from the crest and margins of a sediment drift in water depths of 3500-4500 m in the northern Scotia Sea, South Atlantic Ocean. 46 dinoflagellate cyst analyses have been conducted, covering a time-span ranging from the Holocene down to MIS 6, representing about 160 ka. This provides a resolution of approximately 3500 years. The sediments are predominantly fine-grained contourites and diatom-rich hemipelagites, capped by sandy-silty contourites rich in the planktonic foraminifer Neogloboquadrina pachyderma. The cores can be subdivided into four dinoflagellate cyst units, supported by diatom and radiolarian biostratigraphy, biogenic barium geochemistry, oxygen isotopes and magnetic susceptibility curves. The youngest dinoflagellate cyst unit was found only in the core from the drift crest, and has been dated at between 4380 and 12275 yr BP by radiocarbon dating. The unit is characterised by autotrophic dinoflagellate cysts with similarities to modem cysts from the region, although the assemblages display some marked internal variability that may suggest rather unstable Holocene oceanographic conditions. The next downhole unit was found in both cores and provided radiocarbon ages of 14 580 yr BP and 16 840 yr BP. Recovered cyst assemblages suggest deposition within or near to maximum sea ice limits, corresponding to a northward shift of the Antarctic Convergence during the Last Glacial Maximum within oxygen Marine Isotope Stage (MIS) 2. The final two units lack radiocarbon age control. The next downhole unit is characterised by heterotrophic dinoflagellate cysts such as round, brown Protoperidinium spp. and Selenopemphix antarctica, indicating deposition within maximum sea ice limits. This unit has a wide age range within MIS 5a-d including MIS 6. Toward the base of this unit the assemblage contains autotrophic dinoflagellate cysts such as Impagidium spp., Protoceratium reticulatum and Spiniferites spp., indicative of warmer, interglacial conditions, suggesting a retreat of the Antarctic Convergence and interpreted as MIS 5e, the last interglacial. MIS 3-4 are not resolved by the dinoflagellate cysts. The oldest unit recovered is marked by a return to heterotrophic dinoflagellate cysts with deposition in the presence of seasonal sea ice and open water, suggesting the Antarctic Convergence was now northward of the core site. The dinoflagellate cyst assemblages recovered from the cores illustrate the glacial-interglacial dynamism between two important biogeographical boundaries; the Antarctic Convergence. to the north and the maximum sea ice limit toward the south. (C) 2002 Elsevier Science B.V. All rights reserved.	Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA34 4AD, Argyll, Scotland; DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Palynol Res Facil, Dept Anim & Plant Sci, Sheffield S3 7HF, S Yorkshire, England; British Antarctic Survey, Cambridge CB3 0ET, England	University of the Highlands & Islands; University of Sheffield; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	Howe, JA (通讯作者)，Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA34 4AD, Argyll, Scotland.							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Geol.	NOV 20	2002	191	1-2					55	69	PII S0025-3227(02)00498-X	10.1016/S0025-3227(02)00498-X	http://dx.doi.org/10.1016/S0025-3227(02)00498-X			15	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	611GN					2025-03-11	WOS:000179008200004
J	Saito, K; Drgon, T; Robledo, JAF; Krupatkina, DN; Vasta, GR				Saito, K; Drgon, T; Robledo, JAF; Krupatkina, DN; Vasta, GR			Characterization of the rRNA locus of <i>Pfiesteria piscicida</i> and development of standard and quantitative PCR-based detection assays targeted to the nontranscribed spacer	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							RIBOSOMAL-RNA GENES; PERKINSUS-MARINUS; ENVIRONMENTAL EXPOSURE; CRASSOSTREA-VIRGINICA; PHYLOGENETIC ANALYSIS; DIAGNOSTIC ASSAY; EASTERN OYSTER; FISH KILLS; DINOFLAGELLATE; DNA	Pfiesteria piscicida is a heterotrophic dinoflagellate widely distributed along the middle Atlantic shore of the United States and associated with fish kills in the Neuse River (North Carolina) and the Chesapeake Bay (Maryland and Virginia). We constructed a genomic DNA library from clonally cultured P. piscicida and characterized the nontranscribed spacer (NTS), small subunit, internal transcribed spacer 1 (ITS1), 5.8S region, ITS2, and large subunit of the rRNA gene cluster. Based on the P. piscicida ribosomal DNA sequence, we developed a PCR-based detection assay that targets the NTS. The assay specificity was assessed by testing clonal P. piscicida and Pfiesteria shumwayae, 35 additional dinoflagellate species, and algal prey (Rhodomonas sp.). Only P. piscicida and nine presumptive P. piscicida isolates tested positive. All PCR-positive products yielded identical sequences for P. piscicida, suggesting that the PCR-based assay is species specific. The assay can detect a single P. piscicida zoospore in 1 ml of water, 10 resting cysts in 1 g of sediment, or 10 fg of P. piscicida DNA in 1 mug of heterologous DNA. An internal standard for the PCR assay was constructed to identify potential false-negative results in testing of environmental sediment and water samples and as a competitor for the development of a quantitative competitive PCR assay format. The specificities of both qualitative and quantitative PCR assay formats were validated with >200 environmental samples, and the assays provide simple, rapid, and accurate methods for the assessment of P. piscicida in water and sediments.	Univ Maryland, Ctr Marine Biotechnol, Inst Biotechnol, Baltimore, MD 21202 USA	University System of Maryland; University of Maryland Baltimore	Univ Maryland, Ctr Marine Biotechnol, Inst Biotechnol, 701 E Pratt St, Baltimore, MD 21202 USA.	vasta@umbi.umd.edu	Vasta, Gerardo/LXU-3978-2024		NIEHS NIH HHS [5-P01-ES09563] Funding Source: Medline	NIEHS NIH HHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS))		ALLEN JR, 1975, CELL, V6, P161, DOI 10.1016/0092-8674(75)90006-9; Anderson D.M., 1985, P219; AUSUBEL MF, 1999, SHORT PROTOCOLS MOL, P1; Bena G, 1998, J MOL EVOL, V46, P299, DOI 10.1007/PL00006306; Bever C T Jr, 1998, Md Med J, V47, P120; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 2001, ENVIRON HEALTH PERSP, V109, P745, DOI 10.2307/3454922; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; Chou CH, 1999, GENOME, V42, P1088, DOI 10.1139/gen-42-6-1088; CILIBERTO G, 1983, CELL, V32, P725, DOI 10.1016/0092-8674(83)90058-2; COATAS E, 1995, J PHYCOL, V31, P801; CORTADAS J, 1982, EMBO J, V1, P1075, DOI 10.1002/j.1460-2075.1982.tb01299.x; Coss CA, 2001, J EUKARYOT MICROBIOL, V48, P52, DOI 10.1111/j.1550-7408.2001.tb00415.x; DALRYMPLE BP, 1990, MOL BIOCHEM PARASIT, V43, P117, DOI 10.1016/0166-6851(90)90136-A; Davis L.G., 1994, BASIC METHODS MOL BI; de la Herrán R, 2000, PARASITOLOGY, V120, P345, DOI 10.1017/S003118209900565X; Desjardin LE, 1998, J CLIN MICROBIOL, V36, P1964, DOI 10.1128/JCM.36.7.1964-1968.1998; GLASGOW HB, 1995, J TOXICOL ENV HEALTH, V46, P501, DOI 10.1080/15287399509532051; Grattan LM, 1998, LANCET, V352, P532, DOI 10.1016/S0140-6736(98)02132-1; GUAY JM, 1992, GENE, V114, P165, DOI 10.1016/0378-1119(92)90570-F; Guillard R. 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Environ. Microbiol.	NOV	2002	68	11					5394	5407		10.1128/AEM.68.11.5394-5407.2002	http://dx.doi.org/10.1128/AEM.68.11.5394-5407.2002			14	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	611PU	12406730	Green Published, Bronze			2025-03-11	WOS:000179027600025
J	Wu, GX; Qin, JG; Deng, B; Li, CX				Wu, GX; Qin, JG; Deng, B; Li, CX			Palynomorphs in the first paleosol layer in the Yangtze Delta and their paleoenvironmental implication	CHINESE SCIENCE BULLETIN			English	Article						Yangtze Delta; paleosol layer; sporopollen; phytoplankton; paleoenvironment		The relatively abundant palynomorphs were recovered from the samples of the first paleosol layer of core CY in Shanghai for the first time. A total of 55 genera and families of spore, pollen and phytoplankton were identified. According to the characteristics of the palynological assemblages, the depositional conditions in the development period of the paleosols were discussed and the microfossil evidence to study the origin of the paleosols in the Yangtze Delta area was provided as well. The research results show that paleosols should be freshwater deposits. The palynological assemblage sequence in the first paleosol layer reveals fluctuations of freshwater palynomorphs, mainly Concentricystis, and terricolous herbs pollen, reflecting the alternations of deposition and exposure in the development period of the paleosols. Concentricystis developed prosperously in the period of flood, while terricolous herbs grew on the emerged land in the period of exposure. The variations in the palynological assemblages suggest that the depositional conditions were various during the formation of the paleosols, and resulted in obvious stage characteristics of the paleosol's development. The dinoflagellate cysts occur in low abundance in the palynological assemblages of the first paleosol layer of core CY, indicating that the area where core CY lies was influenced by seawater in the depositional period of the parent materials of the paleosols.	Tongji Univ, Minist Educ, Key Lab Marine Geol, Shanghai 200092, Peoples R China	Tongji University	Wu, GX (通讯作者)，Tongji Univ, Minist Educ, Key Lab Marine Geol, Shanghai 200092, Peoples R China.		Deng, Bing/F-7623-2014					Chen Q.X., 1998, CHINESE SCI BULL, V43, P2557; GRENFELL HR, 1995, REV PALAEOBOT PALYNO, V84, P201, DOI 10.1016/0034-6667(94)00134-6; HU HJ, 1980, FRESHWATER ALGA CHIN, P314; Li C.X., 1986, Chin. Sci. Bull., V31, P1650; LI CX, 1998, STRATIGRAPHY LATE Q; Liu C. T., 1995, INTERMETALLIC COMPOU, V2, P17; ROCHON A, 1999, DISTRIBUTION RECENT, P12; Sun S., 1987, SCI CHINA SER B, P1329; WANG KF, 1987, SCI CHINA SER B, P874; WANG KF, 1984, ACTA OCEANOLOGICA SI, V6, P485; Zheng X, 1995, QUATERNARY RES, P258, DOI 10.13249/j.cnki.sgs.2006.05.012; ZHENG XM, 1999, AEOLIAN LOESS DEPOSI	12	4	6	0	1	SCIENCE CHINA PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	1001-6538			CHINESE SCI BULL	Chin. Sci. Bull.	NOV	2002	47	21					1837	1841		10.1360/02tb9401	http://dx.doi.org/10.1360/02tb9401			5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	606VC					2025-03-11	WOS:000178754200017
J	Wendler, I; Zonneveld, KAF; Willems, H				Wendler, I; Zonneveld, KAF; Willems, H			Oxygen availability effects on early diagenetic calcite dissolution in the Arabian Sea as inferred from calcareous dinoflagellate cysts	GLOBAL AND PLANETARY CHANGE			English	Article; Proceedings Paper	Symposium on From Process Studies to Reconstruction of the Palaeoenvironment	APR 25-29, 2000	NICE, FRANCE			dinoflagellates; calcite dissolution; early diagenesis; organic matter; Arabian Sea	ORGANIC-MATTER PRESERVATION; CONTINENTAL-MARGIN SEDIMENTS; WESTERN EQUATORIAL ATLANTIC; NORTHWESTERN INDIAN-OCEAN; MINIMUM ZONE; SURFACE SEDIMENTS; ENHANCED PRESERVATION; SULFATE REDUCTION; CACO3 DISSOLUTION; SPATIAL-DISTRIBUTION	In oceanic regions with high primary production, such as the Arabian Sea, the primary signals of proxies are often altered by diagenetic processes. The present study aims at assessing the effects of early diagenesis on calcareous dinoflagellate cysts, which represent a relatively new tool for reconstructing the paleoenvironmental conditions within the photic zone. For this purpose, surface sediment samples from within and below the oxygen minimum zone (OMZ) of the northeastern and southwestem Arabian Sea have been analysed quantitatively for their calcareous dinoflagellate cyst content. The calculated cyst accumulation rates (ARs), the relative abundances and cyst fragmentation values were compared to bottom water oxygen (BWO) content and ARs of organic carbon at the sample positions. Different patterns were found in the northeastern and southwestern part of the Arabian Sea. In the SW, no relationship between cyst ARs and BWO is distinguishable, and the distribution of cyst ARs is thought to largely reflect primary cyst production. In the NE, much higher ARs of all species are found in samples from within the OMZ in comparison to samples from below it. This is interpreted to result from better calcite preservation within the OMZ, presumably due to reduced oxic degradation of organic matter. The differential drop of cyst ARs of the individual species at the lower boundary of the OMZ in the NE Arabian Sea, as well as the species-specific change in relative abundance and fragmentation, indicate different sensitivity to calcite dissolution of the different species. These results show that early diagenetic calcite dissolution can change both relative and absolute abundances of calcareous dinoflagellate cysts, which has to be considered if using them for paleoenvironmental reconstructions. Furthermore, it is shown that considerable calcite dissolution can occur above the carbonate saturation horizon in high productive areas. However, calcite preservation can be substantially increased, as soon as oxygen concentrations are too low for oxic degradation of OM. Under low oxic conditions (within and near the OMZ), the main factor controlling organic matter (OM) preservation appears to be BWO concentrations. Under higher oxygen levels (below similar to 1500 m depth in the NE Arabian Sea) there seems to be an increasing influence of bioturbation and sedimentation rate on the preservation of OM by controlling its oxygen exposure time. This study presents an example of a highly productive basin in which differences in early diagenetic processes can lead to the preservation of a signal that is either dominated by primary production (off Somalia) or by secondary alteration (off Pakistan), although in both areas, an oxygen depleted zone is present. For estimating the effects of early diagenetic calcite dissolution in a sediment by metabolic CO2 (and probably by H2S oxidation), not only the content of organic carbon but also other geochemical proxies for paleoredox-conditions have to be included for paleoenvironmental reconstructions. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich 5, D-28334 Bremen, Germany	University of Bremen	Wendler, I (通讯作者)，Univ Bremen, Fachbereich 5, Postfach 330 440, D-28334 Bremen, Germany.							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Planet. Change	NOV	2002	34	3-4					219	239	PII S0921-8181(02)00117-0	10.1016/S0921-8181(02)00117-0	http://dx.doi.org/10.1016/S0921-8181(02)00117-0			21	Geography, Physical; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	623PF					2025-03-11	WOS:000179711500008
J	Palliani, RB; Mattioli, E; Riding, JB				Palliani, RB; Mattioli, E; Riding, JB			The response of marine phytoplankton and sedimentary organic matter to the early Toarcian (Lower Jurassic) oceanic anoxic event in northern England	MARINE MICROPALEONTOLOGY			English	Article						calcareous nannofossils; dinoflagellate cysts; biostratigraphy; geochemistry; palaeoceanography; Lower Jurassic	SEA-LEVEL; TETHYAN LOWER; CARBONATES; SECTION; ARDECHE; EXAMPLE; SHALES; BASIN	Early Toarcian organic-rich sediments, reflecting the Lower Jurassic oceanic anoxic event, were investigated in the Brown Moor Borehole, North Yorkshire (northern England). Integrated micropalaeontological (calcareous nannofossils and dinoflagellate cysts) and geochemical (rock-eval pyrolysis) analyses reveal a sequence of changes mainly driven by palaeoecological shifts. These changes mainly involve the composition, source and preservation rate of sedimentary organic matter as well as algal population dynamics. A sequence of successive disappearances of individual species during the early Toarcian (Dactylioceras semicelatum and Harpoceras exaratum Ammonite Subzones) affect the composition of the phytoplankton assemblages which become gradually dominated by opportunistic taxa. This range top sequence is followed by the temporary disappearance of both calcareous nannofossils and dinoflagellate cysts (the disappearance event), which are replaced by Tasmanites. An increase in type II kerogen marks this interval. These modifications were related to a gradual water stratification and to the development of a stable pycnocline. These factors controlled the development of an oxygen-minimum zone within the water column and the distribution of nutrients in the surface waters. The disappearance event is coincident with the maximum extent of the oxygen minimum zone. A repopulation event and an increase in type III kerogen mark the end of the phytoplankton crisis in the upper part of the H. exaratum Ammonite Subzone. Preadapted survivors (e.g. Biscutum dubium, Biscutum finchii and Crepidolithus crassus) mainly characterise the repopulated calcareous nannofossil assemblages, whereas a significant turnover affected the dinoflagellate cyst community. The re-established phytoplankton populations are a response to the gradual restoration of mixed marine waters, characterised by meso-eutrophic conditions at the surface and by sustained nutrient regeneration. The integrated calcareous nannofossil and dinoflagellate cyst biostratigraphy provided a reliable biochronological framework for the Brown Moor Borehole succession, allowing correlation with lower Toarcian anoxic strata in central Italy. The integrated micropalaeontological approach indicates some diachroneity of Lower Jurassic Ammonite zones in the Boreal and Tethyan realms. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Perugia, Dipartimento Sci Terra, I-06100 Perugia, Italy; British Geol Survey, Nottingham NG12 5GG, England; Univ Lyon 1, Ctr Sci Terre, F-69622 Villeurbanne, France	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universite Claude Bernard Lyon 1	Univ Perugia, Dipartimento Sci Terra, Piazza Univ, I-06100 Perugia, Italy.	rbucefa@tin.it	Mattioli, Emanuela/D-7951-2012					[Anonymous], 1987, ASS AUSTRALASIAN PAL; BARTOLINI A, 1996, SEPM IAS RES C ARB G, P19; Batten D., 1994, Cahiers de Micropaleontologie, V9, P21; BAUDIN F, 1989, THESIS U P M CURIE P; Bown P. 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Abh., V136, P345; MUTTERLOSE J, 1989, BR MICROPAL, P122; Palliani RB, 1998, PALAEOGEOGR PALAEOCL, V142, P33, DOI 10.1016/S0031-0182(97)00152-1; 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, 1998, J MICROPALAEONTOL, V17, P153, DOI 10.1144/jm.17.2.153; PALLIANI RB, 1993, PALEOPELAGOS, V3, P129; PALLIANI RB, 1995, EUROPAL, V8, P60; Parisi G, 1996, GEOBIOS-LYON, V29, P469, DOI 10.1016/S0016-6995(96)80006-4; Pittet B, 1997, SEDIMENTOLOGY, V44, P915, DOI 10.1046/j.1365-3091.1997.d01-58.x; Powell J.H., 1984, P YORKS GEOL SOC, V45, P51, DOI DOI 10.1144/PYGS.45.1-2.51; PRAUSS H, 1996, NEUES JB GEOL PAL, V200, P107; 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; Pross J, 2001, PALAEOGEOGR PALAEOCL, V166, P369, DOI 10.1016/S0031-0182(00)00219-4; Riding J.B., 1992, P7; 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 JB, 1996, B SOC GEOL FR, V167, P3; Röhl HJ, 2001, PALAEOGEOGR PALAEOCL, V165, P27, DOI 10.1016/S0031-0182(00)00152-8; Roth P.H., 1986, Geological Society Special Publication, P299, DOI 10.1144/GSL.SP.1986.021.01.22; Saelen G, 1996, PALAIOS, V11, P97, DOI 10.2307/3515065; Schopler E, 2000, J AUTISM DEV DISORD, V30, P1; STRATE J, 1999, J UNDERGRADUATE RES; Tissot B.P., 1978, PETROLEUM FORMATION, DOI DOI 10.1007/978-3-642-96446-6; TYSON RV, 1987, MARINE PETROLEUM SOU, P47; VANHELDEN BGT, 1977, GEOLOGICAL SURVEY CA, V77, P163; WEISSERT H, 1991, B SOC GEOL FR, V162, P1133; Wilde P., 1990, Lecture Notes in Earth Sciences, V30, P85; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Woollam R., 1983, 832 I GEOL	74	131	138	0	10	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	NOV	2002	46	3-4					223	245	PII S0377-8398(02)00064-6					23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	618RJ					2025-03-11	WOS:000179430800001
J	Wierzbowski, A; Smelror, M; Mork, A				Wierzbowski, A; Smelror, M; Mork, A			Ammonites and dinoflagellate cysts in the Upper Oxfordian and Kimmeridgian of the northeastern Norwegian Sea (Nordland VII offshore area): biostratigraphical and biogeographical significance	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							NORWAY	Ammonites and dinoflagellate cysts recovered from Upper Oxfordian and Kimmeridgian deposits in a core 6814/04-U-01 from offshore northern Nordland, Norway, allow a detailed biostratigraphic subdivision of the studied sequence. The numerous ammonites of the families Cardioceratidae and Aulacostephanidae found in the Kimmeridgian strata show both Boreal and Subboreal affinities and allow a correlation with the standard Boreal and Subboreal biostratigraphic zonations. The Kimmeridgian ammonite fauna from offshore northern Nordland shows an intermediate character between the Subboreal fauna of Northwest Europe and the Boreal fauna of the southern Barents Shelf and Svalbard. The dinoflagellate cyst assemblages are typically of low diversity and are related to the Upper Jurassic Boreal/Arctic Paragonyaulacysta borealis assemblage. They apparently seem to show the same type of provincialism within the "Kimmeridge Clay Sea" as the ammonites.	Univ Warsaw, Inst Geol, PL-02089 Warsaw, Poland; Geol Survey Norway, N-7491 Trondheim, Norway; SINTEF, Petr Res, N-7465 Trondheim, Norway	University of Warsaw; Polish Geological Institute - National Research Institute; Geological Survey of Norway; SINTEF	Wierzbowski, A (通讯作者)，Univ Warsaw, Inst Geol, Al Kwirki I Wigury 93, PL-02089 Warsaw, Poland.							ARHUS N, 1989, NORSK GEOL TIDSSKR, V69, P39; BIRDEAUX WW, 1976, GEOL SURV CANADA B, V259; BIRKELUND T, 1978, Palaeontology (Oxford), V21, P31; Birkelund T., 1983, Proceedings of the Geologists' Association, V94, P289; BIRKELUND T, 1985, GRONLANDS GEOLOGISKE, V153, P1; Bj?rke T., 1980, NORSK POLARINSTITUTT, V172, P145; CALLOMON JH, 1985, SPEC PAP PALAEONTOL, V33, P49; HAKANSSON E, 1981, Bulletin of the Geological Society of Denmark, V30, P11; HANTZPERGUE P, 1989, CAH PALEONT CTR NAT; Ilyina V.I., 1988, Palynology in the USSR, P103; MESEZHNIKOV MS, 1973, PALEONTOL ZH, V3, P35; MESEZHNIKOV MS, 1989, MIDDLE UPPER OXFORDI, P30; Miller R.G., 1990, Deposition of Organic Facies: American Association of Petroleum Geologists, V30, P13, DOI DOI 10.1306/ST30517C2; NOhr-Hansen H., 1986, GEOL SOC DENMARK B, V35, P31; Piasecki S., 1980, Middle to Late Jurassic dinoflagellate cyst stratigraphy from Milne Land and Jameson Land (East Greenland) correlated with ammonite stratigraphy; Poulsen N.E., 1996, AM ASS STRATIGR PALY, V31; RIDING J B, 1988, Palynology, V12, P65; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; Shulgina N.I., 1992, GEOLOGICHESKAYA ISTO, P106; Smelror M, 1998, POLAR RES, V17, P181, DOI 10.1111/j.1751-8369.1998.tb00271.x; Smelror M., 2001, NORWEGIAN PETROLEUM, V10, P211; SYKES R M, 1979, Palaeontology (Oxford), V22, P839; 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; WIERZBOWSKI A, 1989, Acta Palaeontologica Polonica, V34, P355; WIERZBOWSKI A, 1990, NEWSL STRATIGR, V22, P7; Wierzbowski Andrzej, 1993, Acta Geologica Polonica, V43, P229; Wignall P.B., 1991, GEOLOGICAL SOC LONDO, P291; Ziegler B., 1962, Palaeontographica, VA119, P1	29	16	21	1	6	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	NOV	2002	226	2					145	164		10.1127/njgpa/226/2002/145	http://dx.doi.org/10.1127/njgpa/226/2002/145			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	623KZ					2025-03-11	WOS:000179703400001
J	Kim, CH; Cho, HJ; Shin, JB; Moon, CH; Matsuoka, K				Kim, CH; Cho, HJ; Shin, JB; Moon, CH; Matsuoka, K			Regeneration from hyaline cysts of <i>Cochlodinium polykrikoides</i> (Gymnodiniales, Dinophyceae), a red tide organism along the Korean coast	PHYCOLOGIA			English	Article							GONYAULAX-TAMARENSIS; DINOFLAGELLATE; REPRODUCTION; SEDIMENTS; AUSTRALIA; WATERS	Recently, the Korean coast has suffered from recurrent red tides caused by the dinoflagellate, Cochlodinium polykrikoides, which has caused tremendous damage to aquaculture. In this study, the hyaline cysts produced by C. polykrikoides are described. These cysts can survive up to 6 months when preserved at 4degreesC in the dark. Cochlodinium polykrikoides motile cells regenerated successfully when transferred to 20degreesC, a photon flux density of 40 mumol photons m(-2) s(-1), and 14:10 h light-dark photoperiod. The formation of hyaline cysts in the life cycle of C. polykrikoides may act as an overwintering survival strategy, the cysts being able to initiate harmful blooms when favourable conditions return.	Pukyong Natl Univ, Dept Oceanog, Nam Gu, Pusan 608737, South Korea; Pukyong Natl Univ, Dept Aquaculture, Nam Gu, Pusan 608737, South Korea; Nagasaki Univ, Fac Fisheries, Nagasaki 8528521, Japan	Pukyong National University; Pukyong National University; Nagasaki University	Cho, HJ (通讯作者)，Pukyong Natl Univ, Dept Oceanog, Nam Gu, 599-1 Daeyeon Dong, Pusan 608737, South Korea.		Shin, Jun-Bong/AAI-9964-2021					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; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Cho ES, 2001, BOT MAR, V44, P57, DOI 10.1515/BOT.2001.008; Dale B., 1983, P69; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; IWASAKI H, 1961, BIOL BULL-US, V121, P173, DOI 10.2307/1539469; Kim CS, 1999, J PLANKTON RES, V21, P2105, DOI 10.1093/plankt/21.11.2105; Kim HG, 1997, RECENT RED TIDES KOR; Kofoid C. A., 1921, Memoirs of the University of California, V5, P1; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; MATSUOKA K, 1986, J PLANKTON RES, V8, P811, DOI 10.1093/plankt/8.4.811; Park JG, 2001, PHYCOLOGIA, V40, P292, DOI 10.2216/i0031-8884-40-3-292.1; Rosales-Loessener F, 1996, HARMFUL TOXIC ALGAL, P193; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	17	44	50	1	9	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	NOV	2002	41	6					667	669		10.2216/i0031-8884-41-6-667.1	http://dx.doi.org/10.2216/i0031-8884-41-6-667.1			3	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	632RM					2025-03-11	WOS:000180236700011
J	Baruffini, L; Lottaroli, F; Torricelli, S				Baruffini, L; Lottaroli, F; Torricelli, S			Integrated high-resolution stratigraphy of the lower oligocene Tusa Tuffite Formation in the Calabro-Lucano area and Sicily (southern Italy)	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						biostratigraphy; dinoflagellate cysts; calcareous nannofossils; turbidites; volcaniclastic layers; lower Oligocene; southern Apennines; Italy	CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; DINOFLAGELLATE CYSTS; EOCENE; CURRENTS; BASIN	Shale samples from the volcaniclastic turbidites ascribed to the Tusa Tuffite Formation (Tufiti di Tusa Auct.) cropping out at the Canale Candela section (Calabro-Lucano boundary, southern Italy) have yielded rich, diverse and well-preserved palynomorph and calcareous nannofossil assemblages. They allow the consistent recognition of both dinoflagellate cyst and calcareous nannofossil zones previously defined in bio- and magnetostratigraphically well calibrated pelagic sequences of the central and northern Apennines. Thus they give the Canale Candela section a first order correlation to the standard chronostratigraphic scale with high precision. On this basis, an earliest Oligocene age is assigned to this succession. Poorly preserved sparse palynological and calcareous nannofossil assemblages have been recovered from the Tusa Tuffite at the type-locality (Nebrodi Mountains, NE Sicily). Hence, no biozonation is proposed for the Tusa section. The overall composition of the Tusa assemblages, however, unequivocally supports the correlation with the Canale Candela volcaniclastic turbidites. The detailed age assessment of the Tusa Tuffite outcrops investigated, as well as facies similarities, give a broad regional correlation with other Rupelian volcaniclastic successions of the Alps/Apennines system, namely the Aveto Formation belonging to the Subligurian Domain of the northern Apennines, the Ranzano Formation belonging to the Epiligurian succession of the northern Apennines and the Taveyanne Sandstones of the western Alps. In this framework, we suggest that a single regional event of rise and erosion of a volcanic arc occurred in the Alps/Apennines orogenic system during the Early Oligocene.	ENI SPA, Agip Div, I-20100 Milan, Italy	Eni SpA	ENI SPA, Agip Div, POB 12069, I-20100 Milan, Italy.	stefano.torricelli@agip.it						[Anonymous], 1960, Riv Minerar Siciliana; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; Backmann J., 1987, Abhandlungen der Geologischen Bundesanstalt (Vienna), V39, P21; BERGGREN WA, 1995, SEPM SPEC PUB, V54; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; Blow W. 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Elf-Aquitaine, V2, P265; Lentini F., 1979, Geologica Romana, V18, P215; MAIORANO P, 1998, RIV ITAL PALEONTOL S, V104, P291; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; MATTIOLI M, 1997, ACTA NATUR ATENEO PA, V33, P89; MONECHI S, 1986, PALAEOGEOGR PALAEOCL, V57, P61, DOI 10.1016/0031-0182(86)90006-4; MORGENROTH P., 1966, PALAEONTOGRAPHICA, V119, P1; Mutti E., 1992, SPECIAL PUBLICATION; Mutti E., 1987, MARINE CLASTIC SEDIM, P1, DOI 10.1007/978-94-009-3241-8_1; NOCCHI M, 1986, TERMINAL EOCENE EVEN; Ogniben L., 1969, MEMORIE SOC GEOLOGIC, V8, P453; OKADA H, 1980, MAR MICROPALEONTOL, V5, P321, DOI 10.1016/0377-8398(80)90016-X; Perch-Nielsen K., 1985, P427; PICKERING KT, 1985, SEDIMENTOLOGY, V32, P373, DOI 10.1111/j.1365-3091.1985.tb00518.x; Romein A.J.T., 1979, Utrecht Micropaleontological Bulletins, V22; ROTH P H, 1970, Eclogae Geologicae Helvetiae, V63, P799; ROTH PH, 1971, P 2 C PLANKT MICR RO, P739; RUFFINI R, 1995, ACC NAZ LINCEI SCRIT, V15, P359; SILVA IP, 1988, SPEC PUBL, P137; TORRICELLI S, 2000, P 7 TUN PETR EXPL PR; Torricelli Stefano, 2001, Palynology, V25, P29, DOI 10.2113/0250029; Wezel F.C., 1973, B SOC GEOL ITAL, V92, P193; WILLIAMS GL, 1998, AM ASS STRATIGR PALY, V34; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zuppetta A., 1984, B SOC GEOL ITAL, V103, P623	49	7	8	0	0	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.	NOV	2002	108	3					457	477		10.13130/2039-4942/5488	http://dx.doi.org/10.13130/2039-4942/5488			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	622YX					2025-03-11	WOS:000179676700008
J	Kim, YO; Park, MH; Han, MS				Kim, YO; Park, MH; Han, MS			Role of cyst germination in the bloom initiation of <i>Alexandrium tamarense</i> (Dinophyceae) in Masan Bay, Korea	AQUATIC MICROBIAL ECOLOGY			English	Article						Alexandrium tamarense; cyst germination; vegetative population	DINOFLAGELLATE GONYAULAX-TAMARENSIS; NORTHEAST JAPAN; BENTHIC CYSTS; ONAGAWA BAY; TEMPERATURE	The role of cyst germination in the bloom initiation of the toxic dinoflagellate Alexandrium tamarense was examined in Masan Bay, Korea. Germination success was measured by the incubation of cysts isolated monthly from natural sediments and compared with vegetative cells and environmental factors (temperature, salinity and dissolved oxygen) in the water column. Germination maxima (80 to 90 %) were observed during the period of decreasing water temperature in December 1996 and November 1997, while little or no germination occurred in summer. The seasonal germination exhibited an opposing pattern with temperature and similar seasonalities with salinity and dissolved oxygen, respectively. The bimodal nature of A. tamarense blooms, a large bloom in spring and a much smaller bloom in fall, was observed. Excysted cells in early spring can initiate the spring bloom and then proliferate to the bloom peak in increasing temperatures. Massive germination in fall contributes directly to the small bloom in fall. A temporal discrepancy between the peak of germination success and of vegetative population was found in A. tamarense dynamics from Korean coastal waters.	Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea; Hanyang Univ, Dept Environm Sci, Seoul 133791, South Korea	Hanyang University; Hanyang University	Han, MS (通讯作者)，Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	hanms@hanyang.ac.kr	KIM, YOUNG JIN/E-9374-2011					ANDERSON DM, 1980, J PHYCOL, V16, P166; 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, 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 Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; BLOMQVIST P, 1995, CAN J FISH AQUAT SCI, V52, P551, DOI 10.1139/f95-056; CANNON JA, 1993, DEV MAR BIO, V3, P103; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; 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; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Itakura S, 2001, PHYCOLOGIA, V40, P263, DOI 10.2216/i0031-8884-40-3-263.1; Kim H.G., 1996, HARMFUL TOXIC ALGAL, P57; Kim HM, 2000, INT J ORIENT MED, V1, P1; Mendez S.M., 1996, HARMFUL TOXIC ALGAL, P113; OGATA T, 1987, MAR BIOL, V95, P217, DOI 10.1007/BF00409008; PARK MH, 1999, THESIS HANYANG U SEO; Parsons T.R., 1984, A Manual of Chemical and Biological Methods for Seawater Analysis, P135, DOI [10.1016/B978-0-08-030287-4.50041-4, DOI 10.1016/B978-0-08-030287-4.50041-4]; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Sekiguchi K., 1996, HARMFUL TOXIC ALGAL, P223; Therriault J.C., 1985, P141; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x	25	55	64	1	10	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055			AQUAT MICROB ECOL	Aquat. Microb. Ecol.	OCT 23	2002	29	3					279	286		10.3354/ame029279	http://dx.doi.org/10.3354/ame029279			8	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	615QF		Bronze			2025-03-11	WOS:000179257300006
J	Pospelova, V; Chmura, GL; Boothman, WS; Latimer, JS				Pospelova, V; Chmura, GL; Boothman, WS; Latimer, JS			Dinoflagellate cyst records and human disturbance in two neighboring estuaries, New Bedford Harbor and Apponagansett Bay, Massachusetts (USA)	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						buzzards bay; eutrophication; heavy metals; marine pollution; nutrient loading; organic carbon; PCBs; species richness	INDUSTRIAL-POLLUTION; NORWEGIAN FJORD; CHESAPEAKE BAY; YOKOHAMA-PORT; TOKYO-BAY; LAND-USE; INDICATORS; EUTROPHICATION; ASSEMBLAGES; COMMUNITIES	The dinoflagellate cyst records in sediments from New Bedford Harbor and Apponagansett Bay demonstrate sensitivity to environmental change caused by human activity in the watersheds over the last 500 years. Changes in the species richness, as well as absolute and relative abundance of dinoflagellate cyst taxa reflect recent periods of development around the estuaries. Cyst taxa sensitive to these changes include Dubridinium spp., Polykrikos schwartzii, Lingulodinium machaerophorum, Operculodinium israelianum and Selenopemphix quanta. The greatest changes in the dinoflagellate cyst record occur during the 20th century, when New Bedford Harbor was exposed to both toxic pollution and heavy nutrient loading from point and non-point sources. Apponagansett Bay was not subject to industrial pollution and nutrient enrichment has been lower (from non-point sources). In Apponagansett Bay there is an increase in the dinoflagellate cyst species richness while species richness first increased, then declined in New Bedford Harbor. During the same period, the total dinoflagellate cyst concentration in New Bedford Harbor fluctuated over a wide range. The decline of species richness and the large fluctuations in the total cyst abundances signal the intensified anthropogenic disturbance in the watershed, notably a high degree of eutrophication and toxic pollution. (C) 2002 Elsevier Science B.V. All rights reserved.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada; US EPA, Off Res & Dev, NHEERL, Atlantic Ecol Div, Narragansett, RI 02882 USA	United States Environmental Protection Agency	Pospelova, V (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 2K6, Canada.		Latimer, James/C-1632-2009; Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903; Pospelova, Vera/0000-0003-4049-8133				ABDELRHMAN MA, UNPUB MODELING HURRI; [Anonymous], 1999, DIATOMS APPL ENV EAR; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; BARON WR, 1985, CLIMATIC CHANGE CANA, V5, P229; Boynton W.R., 1982, ESTUARINE COMP, P69, DOI [DOI 10.1016/B978-0-12-404070-0.50011-9, 10.1016/B978-0-12-404070-0.50011-9]; BRUGAM RB, 1978, QUATERNARY RES, V9, P349, DOI 10.1016/0033-5894(78)90038-8; BRUSH GS, 1984, QUATERNARY RES, V22, P91, DOI 10.1016/0033-5894(84)90009-7; CHMURA GL, 1995, J COASTAL RES, V11, P124; COOPER SR, 1993, ESTUARIES, V16, P617, DOI 10.2307/1352799; COOPER SR, 1995, ECOL APPL, V5, P703, DOI 10.2307/1941979; COSTA JE, 1996, REPORT BUZZARDS BAY; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; 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; *ENV DAT INF SERV, 1983, CLIM NORM US BAS 195; EPPLEY RW, 1979, OCEANOL ACTA, V2, P241; Evgenidou A, 1999, BIOL BULL, V197, P292, DOI 10.2307/1542659; Fensome R.A., 1993, CLASSIFICATION FOSSI; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Höll C, 2000, PALAEOGEOGR PALAEOCL, V160, P69, DOI 10.1016/S0031-0182(00)00047-X; Howes B., 1999, BAYWATCHERS; Jacobson DM, 1996, J PHYCOL, V32, P279, DOI 10.1111/j.0022-3646.1996.00279.x; LATIMER JS, UNPUB ENV STRESS REC; Lentin J.K., 1993, A.S.S.P., V28, 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; MCCLELAND JW, 1996, MARINE ECOL PROGR SE, V68, P259; NEILSON BJ, 1981, CHESAPEAKE RES CONSO, V90; NELSON WG, 1996, EP600R96097 NAT HLTH; NIXON SW, 1995, OPHELIA, V41, P199, DOI 10.1080/00785236.1995.10422044; PAERL HW, 1988, LIMNOL OCEANOGR, V33, P823, DOI 10.4319/lo.1988.33.4_part_2.0823; Pesch CE, 2001, MAR POLLUT BULL, V42, P339, DOI 10.1016/S0025-326X(00)00153-3; Pospelova V, 2002, J PHYCOL, V38, P593, DOI 10.1046/j.1529-8817.2002.t01-1-01206.x; POSPELOVA V, 1998, RAPPORT BOTANISK SER, V1, P122; PRUELL RJ, 1990, MAR ENVIRON RES, V29, P77, DOI 10.1016/0141-1136(90)90030-R; ROFFINOLI RJ, 1981, SOIL SURVEY BRISTOL; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; SOMMER U, 1995, LIMNOL OCEANOGR, V40, P1272; STOCKMARR J, 1971, Pollen et Spores, V13, P615; SUMMERHAYES CP, 1977, WHOI76115; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Tsirtsis G, 1998, ENVIRON MONIT ASSESS, V50, P255, DOI 10.1023/A:1005883015373; Voyer RA, 2000, ENVIRON HIST-US, V5, P352, DOI 10.2307/3985481	47	108	115	1	22	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0048-9697			SCI TOTAL ENVIRON	Sci. Total Environ.	OCT 21	2002	298	1-3					81	102	PII S0048-9697(02)00195-X	10.1016/S0048-9697(02)00195-X	http://dx.doi.org/10.1016/S0048-9697(02)00195-X			22	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	635DW	12449331				2025-03-11	WOS:000180383700007
J	Hiscott, RN; Aksu, AE; Yasar, D; Kaminski, MA; Mudie, PJ; Kostylev, VE; MacDonald, JC; Isler, FI; Lord, AR				Hiscott, RN; Aksu, AE; Yasar, D; Kaminski, MA; Mudie, PJ; Kostylev, VE; MacDonald, JC; Isler, FI; Lord, AR			Deltas south of the Bosphorus Strait record persistent Black Sea outflow to the Marmara Sea since ∼ 10 ka	MARINE GEOLOGY			English	Article						Marmara Sea; Black Sea; transgression; deltas; sequence stratigraphy	RADIOCARBON AGE CALIBRATION; AEGEAN SEA; LEVEL; CONNECTION; RATES	At the southern exit of the Bosphorus Strait in the northeastern Marmara Sea, high-resolution seismic profiles reveal two lobate, progradational delta lobes in modem water depths of similar to40-65 m. The younger delta was active from similar to10 to 9 ka based on radiocarbon dates of equivalent prodelta deposits and the elevation of its topset-to-foreset transition. The topset-to-foreset transition climbs in the seaward direction because the delta prograded into a rising sea. Low abundances of marine fauna and flora in the 10-9-ka interval support a deltaic interpretation. There are no rivers in the area that could have fed the delta; instead, all evidence points to the strait itself as the source of sediment and water. When this outflow was strongest (similar to 10.6-6.0 ka), sapropels accumulated in basinal areas of both the Aegean and Marmara seas. Benthic foraminiferal and dinoflagellate cyst data from contemporary deposits elsewhere in the Marmara Sea point to the continual presence through the Holocene of a surface layer of brackish water that we ascribe to this same outflow from the Black Sea through the Bosphorus Strait. By similar to 9.1-8.5 ka, two-layer flow developed in the Bosphorus Strait as global sea level continued to rise, and the sediment supply to the younger delta was cut off because the outflowing Black Sea water ceased to be in contact with the, floor of the strait. The older delta lobe lies below a prominent lowstand unconformity and is tentatively interpreted to have formed from similar to 29.5 to 23.5 ka (oxygen-isotopic stage 3) when the Marmara Sea stood at similar to -55 m and a second sapropel accumulated in deep basinal areas. Crown Copyright (C) 2002 Elsevier Science B.V. All rights reserved.	Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada; Dokuz Eyul Univ, Inst Marine Sci & Technol, TR-35340 Izmir, Turkey; UCL, Dept Geol Sci, London WC1E 6BT, England; Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada	Memorial University Newfoundland; Dokuz Eylul University; University of London; University College London; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada.	rhiscott@sparky2.esd.mun.ca	Yasar, Dogan/AAC-1866-2020; Kaminski, Michael/K-3334-2012					Abbott R.T., 1998, COMPENDIUM SEASHELLS; Abrajano T, 2002, MAR GEOL, V190, P151, DOI 10.1016/S0025-3227(02)00346-8; Aksu A.E., 2000, GEOLOGICAL SOC AM, V10, P3; Aksu AE, 1999, MAR GEOL, V153, P275, DOI 10.1016/S0025-3227(98)00078-4; AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; AKSU AE, 2002, MAR GEOLP, V190; AKSU AE, 2002, MAR GEOL, V190; [Anonymous], 1981, SYSTEMATIC INDEX REC; [Anonymous], NOAHS FLOOD; Athersuch J., 1989, SYNOPSES BRIT FAUNA, V43, DOI [10.1017/s0025315400059178, DOI 10.1017/S0025315400059178]; BESIKTEPE ST, 1994, PROG OCEANOGR, V34, P285, DOI 10.1016/0079-6611(94)90018-3; Bogdanova C, 1969, BASIC FEATURES GEOLO, P131; Brown DN, 1999, MATER RES SOC SYMP P, V577, P47, DOI 10.1557/PROC-577-47; Çagatay MN, 2000, MAR GEOL, V167, P191, DOI 10.1016/S0025-3227(00)00031-1; Emeis K.-C., 1996, Proceedings of the Ocean Drilling Program, V160, P21; FAIRBANKS RG, 1989, NATURE, V342, P637, DOI 10.1038/342637a0; Görür N, 2001, MAR GEOL, V176, P65, DOI 10.1016/S0025-3227(01)00148-7; HEGARTY KA, 1988, AAPG BULL, V72, P615; Hiscott RN, 2001, MAR GEOL, V175, P67, DOI 10.1016/S0025-3227(01)00118-9; HISCOTT RN, 2002, MAR GEOL, V190; KAMINSKI MA, 2002, MAR GEOL, V190; Kennett J.P., 1983, NEOGENE PLANKTONIC F; Kleijne A., 1993, Morphology, Taxonomy and Distribution of extant coccolithophorids (calcareous nannoplankton); KULAL Z, 1971, GEOLOGY RECENT SEDIM; LaneSerff GF, 1997, PALEOCEANOGRAPHY, V12, P169, DOI 10.1029/96PA03934; Latif M.L., 1992, 922 MIDDL E TU I MAR; MACDONALD JC, 2000, THESIS MEMORIAL U NE; MCINNIS D, 1998, EARTH            AUG, P46; Mestel R, 1997, NEW SCI, V156, P24; MORDUKHAIBOLTOV.FD, 1972, KEYS IDENTIFICATION, V3; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; MUDIE PJ, 2002, MAR GEOL, V190; Oezsoy E., 1995, B FTH I OCEANOGRAPHY, V15, P1; Oktay FY, 2002, MAR GEOL, V190, P367, DOI 10.1016/S0025-3227(01)00246-8; Pfannenstiel M, 1944, GEOL RUNDSCH, V34, P334, DOI 10.1007/BF01803097; Polat C. S., 1996, CIESME SCI SERIES, V2, P167; POPPE GT, 1993, EUROPEAN SHEASHELLS, V2; POPPE GT, 1991, EUROPEAN SHEASHELLS, V1; Ryan WBF, 1997, MAR GEOL, V138, P119, DOI 10.1016/S0025-3227(97)00007-8; Skene KI, 1998, J SEDIMENT RES, V68, P1077, DOI 10.2110/jsr.68.1077; SMITH AD, 1995, GEOL SOC AM BULL, V107, P923, DOI 10.1130/0016-7606(1995)107<0923:HRSPIT>2.3.CO;2; Stuiver M, 1998, RADIOCARBON, V40, P1127, DOI 10.1017/S0033822200019172; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Winter A., 1994, COCCOLITHOPHORES; Yaltirak C, 2002, MAR GEOL, V190, P493, DOI 10.1016/S0025-3227(02)00360-2; Yim WWS, 1999, QUATERN INT, V55, P77, DOI 10.1016/S1040-6182(98)00029-9	47	78	79	0	19	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0025-3227	1872-6151		MAR GEOL	Mar. Geol.	OCT 15	2002	190	1-2					95	118	PII S0025-3227(02)00344-4	10.1016/S0025-3227(02)00344-4	http://dx.doi.org/10.1016/S0025-3227(02)00344-4			24	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	612KN					2025-03-11	WOS:000179074200008
J	Mudie, PJ; Rochon, A; Aksu, AE; Gillespie, H				Mudie, PJ; Rochon, A; Aksu, AE; Gillespie, H			Dinoflagellate cysts, freshwater algae and fungal spores as salinity indicators in Late Quaternary cores from Marmara and Black seas	MARINE GEOLOGY			English	Article						dinoflagellate cysts; acritarchs; fungi; freshwater algae; Marmara Sea; Black Sea; paleosalinity; Quaternary palynology; aerobic decay	ORGANIC-MATTER; AEGEAN SEA; POLLEN; PRESERVATION; ASSEMBLAGES; CIRCULATION; MORPHOLOGY; SEDIMENTS; BEAUFORT; MARINE	Seismic profiles and mollusks have been used to suggest that from similar to 12 500 to 7000 yr BP, the Black Sea was an isolated freshwater lake containing potable water and implying a surface salinity of < 1. According to Ryan and Pitman (1999), these circumstances encouraged Neolithic settlement and farming on the shore of the Black Sea. This model conflicts with previous studies of dinoflagellate cysts and seismic profiles from the Marmara Sea. Here we investigate Ryan and Pittman's model using palynological studies of organic-walled dinoflagellate cysts, acritarchs, freshwater algae, microforaminifera, and fungal remains as tracers of changes in surface salinity for seven cores of pleniglacial to Holocene sediments from the Marmara and Black seas. Core-top data from 16 sites along a salinity gradient from 39.5 in the Aegean Sea to similar to 17 in the Black Sea show that the dinocyst species Impagidinium aculeatum, Impagidinium patulum, Operculodinium israelianum, Polysphaeridium zoharyi and Nematosphaeropsis labyrinthus are markers of Mediterranean Sea water and summer surface salinity > 24, and that Spiniferites cruciformis, Spiniferites inaequalis, Peridinium ponticum, Polykrikos spp. and Quinquecuspis concreta characterize the lower salinity of the Marmara and/or Black seas. The core-top data and correlatable down-core assemblage changes in time-equivalent sapropelic and brown muds show that there is no evidence for differential aerobic decay of dinocysts in the study area. The main acritarchs are Sigmopollis psilatum, Concentricystes cf. C rubinus and cf. Acritarch-8 of Traverse (1978), all of which are absent from the Aegean Sea and decrease in abundance with increasing salinity; the first two taxa have been reported previously as freshwater species. Fungal remains show a similar distribution pattern to the freshwater acritarchs, indicating their origin from terrestrial environments. Freshwater Chlorococcales are almost confined to the Black Sea but they have rare occurrences in the Aegean, indicating long-distance transport. Microforaminiferal linings are abundant in the Marmara Sea but are absent in deep water of the Black Sea. In the Marmara Sea, mid-late Holocene assemblages (<7 ka) are dominated by Lingulodinium machaerophorum, Operculodinium centrocarpum and halophilic Mediterranean Spiniferites spp. (S. mirabilis, S. hyperacanthus, S. bentorii), and a diversity of heterotrophic protoperidinioid and Polykrikos species are present in both sapropels and brown lutites. In contrast, the early Holocene interval (including sapropels) has fewer halophilic Spiniferites spp. and other Mediterranean taxa (O. israelianum, Polysphaeridium zoharyi) and more low salinity indicators (P. ponticum, Pyxidinopsis psilata and S. cruciformis), suggesting that the overflow of Black Sea water was greater than now. The time-equivalent early Holocene unit in the Black Sea has a higher percentage of taxa found in freshwater environments (including S. cruciformis forms 1-3; Gonyaulax apiculata, fungal remains and freshwater acritarchs) but the continued presence of Spiniferites morphotypes and other taxa associated with brackish (similar to 7-18) to saline surface water indicates that there was some Mediterranean water present at this time. The late glacial and Pleniglacial sediments in the Marmara Sea contain a lower diversity of dinoflagellates, dominated by S. cruciformis and P. psilata, as in early Holocene sediments of the Black Sea but including the short-spine morphotypes of S. cruciformis which are not found in freshwater lakes. We conclude that although the glacial stages were marked by much lower sea-surface temperatures, there was either some periodic marine influence or the marine dinocysts were living in a brackish water environment (similar to7-18) with the freshwater species being transported from glacial lakes. Overall, there is no palynological evidence that the surface salinity of the Black or Marmara seas was ever as low as a freshwater lake. This finding is consistent with models that estimate the time required to desalinate the Black Sea after closing of the Marmara-Bosphorus gateway. Crown Copyright (C) 2002 Elsevier Science B.V. All rights reserved.	Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; Mem Univ Newfoundland, Dept Earth Sci, Ctr Earth Resources Res, St John, NF A1B 3X5, Canada	Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland	Geol Survey Canada Atlantic, Bedford Inst Oceanog, 1 Challenger Dr,Box 1006, Dartmouth, NS B2Y 4A2, Canada.	mudie@agc.bio.ns.ca						Abrajano T, 2002, MAR GEOL, V190, P151, DOI 10.1016/S0025-3227(02)00346-8; Aksu AE, 1999, MAR GEOL, V153, P275, DOI 10.1016/S0025-3227(98)00078-4; AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; 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; AKSU AE, 2002, MAR GEOL, V190; [Anonymous], NOAHS FLOOD NEW SCI; [Anonymous], 2007, Paleopalynology; AUBERT M, 1990, REV INT OCEANOGRAPHI, V100; Batten D., 1996, Palynology: principles and applications, P1011; BATTEN DJ, 1996, PALYNOLOGY PRINCIPLE, V3, P191; BENLI HA, 1987, THESIS DOKUZ EYLUL U; BESIKTEPE ST, 1994, PROG OCEANOGR, V34, P285, DOI 10.1016/0079-6611(94)90018-3; BODEANU N, 1993, DEV MAR BIO, V3, P203; Bologa A.S., 1995, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V15, P85; Boudreau BP, 1989, PALEOCEANOGRAPHY, V4, P157, DOI 10.1029/PA004i002p00157; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BURDEN ET, 1986, CAN J EARTH SCI, V23, P43, DOI 10.1139/e86-005; CHEDDADI R, 1991, MAR GEOL, V100, P53, DOI 10.1016/0025-3227(91)90224-R; CHEDDADI R, 1995, PALEOCEANOGRAPHY, V10, P301, DOI 10.1029/94PA02673; Cross A.T., 1966, MAR GEOL, V4, P467, DOI [10.1016/0025-3227(66)90012-0, DOI 10.1016/0025-3227(66)90012-0]; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Degens E, 1974, The Black Sea - Geology, Chemistry and Biology, P396; DEGENS ET, 1974, AAPG MEMOIR, V20, P183; Duman M, 1992, THESIS DOKUZ EYLUL U; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Gheorghian M., 1978, Initial Reports of the Deep Sea Drilling Project, V42, P783, DOI 10.2973/dsdp.proc.42-2.140.1978; GUYOHLSON D, 1996, PALYNOLOGY PRINCIPLE, V3, P181; Harrison SP, 1996, QUATERNARY RES, V45, P138, DOI 10.1006/qres.1996.0016; HARRISON SP, 1993, CLIM DYNAM, V8, P189, DOI 10.1007/BF00207965; HEAD MJ, 1993, J PALEONTOL, V67, P1; HISCOTT RN, 2002, LATE QUATERNARY HIST; JARZEN D M, 1986, Palynology, V10, P35; Kohlmeyer J., 1979, Marine Mycology; 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; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; Mudie P.J., 1974, Ecology of halophytes, P565, DOI 10.1007/978-94-011-0818-8_2; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; MUDIE PJ, 2002, MAR GEOL, V190; MUDIE PJ, 2002, J QUATERNARY SCI, V16, P603; NORRIS G, 1970, REV PALAEOBOT PALYNO, V10, P131, DOI 10.1016/0034-6667(70)90016-3; Oezsoy E., 1995, B FTH I OCEANOGRAPHY, V15, P1; OGUZ T, 1993, DEEP-SEA RES PT I, V40, P1597, DOI 10.1016/0967-0637(93)90018-X; Oktay FY, 2002, MAR GEOL, V190, P367, DOI 10.1016/S0025-3227(01)00246-8; OZSOY E, 1991, NATO ADV SCI I C-MAT, V351, P17; Ozsoy E., 1996, CIESM Science Series 2, Straits and Channels chpt 10, P187; Percival S.F. 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L., 1998, AM ASS STRATIGRAPHIC, V34; 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	72	112	114	0	17	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0025-3227	1872-6151		MAR GEOL	Mar. Geol.	OCT 15	2002	190	1-2					203	231	PII S0025-3227(02)00348-1	10.1016/S0025-3227(02)00348-1	http://dx.doi.org/10.1016/S0025-3227(02)00348-1			29	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	612KN					2025-03-11	WOS:000179074200012
J	Sangiorgi, F; Capotondi, L; Brinkhuis, H				Sangiorgi, F; Capotondi, L; Brinkhuis, H			A centennial scale organic-walled dinoflagellate cyst record of the last deglaciation in the South Adriatic Sea (Central Mediterranean)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Adriatic Sea; deglaciation; dinoflagellate cysts; paleotemperature; paleoproductivity	NORTH-ATLANTIC OCEAN; GENERAL-CIRCULATION; LEVEL RECORD; DENSE WATER; ICE-CORE; SEDIMENTS; RADIOCARBON; CLIMATE; EVENT; STRATIGRAPHY	A high-resolution study of sea surface temperature (SST) and primary productivity changes during the last deglaciation in the South Adriatic Sea is presented on the basis of organic-walled dinoflagellate cysts (dinocysts), compared with stable oxygen and carbon isotope records derived from Globigerina bulloides. Two more defined warming phases between 14.75 and 14.10 cal kyr BP (GI-1e) and between 13.85 and 13.25 cal. kyr BP (GI-1c), and perhaps a mild one between 12.95 and 12.60 cal kyr BP (GI-1a), interrupted by two cold events between 14.10 and 13.85 cal kyr BP (GI-1d) and between 13.25 and 12.95 cal kyr BP (GI-1b) are highlighted. Weaker SST oscillations occurred within the relatively stable periods GS-2a (17.00-14.75 cal kyr BP), GS-1 (or Younger Dryas, 12.60-11.60 cal kyr BP) and Early Holocene. Several dinocyst proxies used to evaluate surface primary productivity suggest that the cold events GI-1d and GI-1b are associated with episodes of both enhanced primary productivity and, perhaps, improved organic matter preservation due to reduced deep water formation. Phases of more pronounced increased surface primary productivity without stagnation in bottom waters are recorded during GI-1c and early GS-1. Freshwater (Po River) discharge seems to be the cause of enhanced productivity during event GI-1c (at 13.4 cal kyr BP) and, probably, during GI-1d. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bologna, Ctr Interdiparitmentale Ric Sci Ambientali, I-48100 Ravenna, Italy; CNR, Ist Geol Marina, I-40129 Bologna, Italy; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	University of Bologna; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR); Utrecht University	Univ Bologna, Ctr Interdiparitmentale Ric Sci Ambientali, Via Ariani 1, I-48100 Ravenna, Italy.	franci@ambra.unibo.it	Brinkhuis, Henk/B-4223-2009; Capotondi, Lucilla/C-8874-2015	Sangiorgi, Francesca/0000-0003-4233-6154; Capotondi, Lucilla/0000-0003-3282-7910; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 1999, P OCEAN DRILLING PRO; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Artegiani A, 1997, J PHYS OCEANOGR, V27, P1492, DOI 10.1175/1520-0485(1997)027<1492:TASGCP>2.0.CO;2; ARTEGIANI A, 1989, OCEANOL ACTA, V12, P151; Asioli A, 2001, QUATERNARY SCI REV, V20, P1201, DOI 10.1016/S0277-3791(00)00147-5; Asioli A, 1999, J QUATERNARY SCI, V14, P373, DOI 10.1002/(SICI)1099-1417(199907)14:4<373::AID-JQS472>3.0.CO;2-T; Bard E, 1996, NATURE, V382, P241, DOI 10.1038/382241a0; BETHOUX JP, 1989, DEEP-SEA RES, V36, P769, DOI 10.1016/0198-0149(89)90150-7; BIGNAMI F, 1990, J GEOPHYS RES-OCEANS, V95, P7249, DOI 10.1029/JC095iC05p07249; Bjorck S, 1998, J QUATERNARY SCI, V13, P283, DOI 10.1002/(SICI)1099-1417(199807/08)13:4<283::AID-JQS386>3.0.CO;2-A; BOND G, 1992, NATURE, V360, P245, DOI 10.1038/360245a0; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; Cacho I, 2001, PALEOCEANOGRAPHY, V16, P40, DOI 10.1029/2000PA000502; Capotondi L, 1999, MAR GEOL, V153, P253, DOI 10.1016/S0025-3227(98)00079-6; Capotondi L, 1996, QUAT, V9, P679; CENTIS M, 1989, THESIS U URBINO; Clark PU, 1996, PALEOCEANOGRAPHY, V11, P563, DOI 10.1029/96PA01419; Combourieu-Nebout N, 1998, QUATERNARY SCI REV, V17, P303, DOI 10.1016/S0277-3791(97)00039-5; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; DALE B., 1994, CARBON CYCLING GLOBA, P521; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FAIRBANKS RG, 1992, RADIOCARBON AFTER FOUR DECADES, P473; FAIRBANKS RG, 1989, NATURE, V342, P637, DOI 10.1038/342637a0; Gaines G., 1987, The Biology of Dinoflagellates, P224; GROOTES PM, 1993, NATURE, V366, P552, DOI 10.1038/366552a0; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JORISSEN FJ, 1993, MAR MICROPALEONTOL, V21, P169, DOI 10.1016/0377-8398(93)90014-O; KROM MD, 1991, OCEANOL ACTA, V14, P189; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; LOWE JJ, 1992, BOREAS, V21, P193; Maisch M., 1982, Geographica Helvetica, V37, P93, DOI [10.5169/seals-58303, DOI 10.5169/SEALS-58303]; MANGERUD J, 1974, Boreas (Oslo), V3, P109; Mercone D, 2000, PALEOCEANOGRAPHY, V15, P336, DOI 10.1029/1999PA000397; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; ORLIC M, 1992, OCEANOL ACTA, V15, P109; Paterne M, 1999, PALEOCEANOGRAPHY, V14, P626, DOI 10.1029/1998PA900022; Pinardi N, 2000, PALAEOGEOGR PALAEOCL, V158, P153, DOI 10.1016/S0031-0182(00)00048-1; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rohling EJ, 1998, PALEOCEANOGRAPHY, V13, P316, DOI 10.1029/98PA00671; SANGIORGI F, 2001, THESIS U BOLOGNA; Sbaffi L, 2001, MAR GEOL, V178, P39, DOI 10.1016/S0025-3227(01)00185-2; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Taragona i Pujola J., 1997, LPP CONTR SERIES, V7, P1; Turon J.-L., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P313; Turon J.-L., 1984, thesis; VERGNAUD-GRAZZINI C., 1992, RAPPORTS COMMISSION, V33, P327; Walker MJC, 1999, QUATERNARY SCI REV, V18, P1143, DOI 10.1016/S0277-3791(99)00023-2; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Watts WA, 1996, QUATERNARY SCI REV, V15, P113, DOI 10.1016/0277-3791(95)00038-0; Williams Graham L., 1998, AASP Contributions Series, V34, P1; WILLIS KJ, 1994, QUATERNARY SCI REV, V13, P769, DOI 10.1016/0277-3791(94)90104-X; Zonneveld KAF, 1996, PALAEOGEOGR PALAEOCL, V122, P89, DOI 10.1016/0031-0182(95)00091-7; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1; ZORE A, 1963, ACTA ADRIAT, V10, P1	57	32	32	0	5	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	OCT 15	2002	186	3-4					199	216	PII S0031-0182(02)00450-9	10.1016/S0031-0182(02)00450-9	http://dx.doi.org/10.1016/S0031-0182(02)00450-9			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	609UF					2025-03-11	WOS:000178922400002
J	Probert, I; Lewis, J; Denn, EEL				Probert, I; Lewis, J; Denn, EEL			Morphological details of the life history of <i>Alexandrium minutum</i> (Dinophyceae)	CRYPTOGAMIE ALGOLOGIE			English	Article						dinoflagellate; Alexandrium minutum; life-cycle; marine microalgae; reproduction; morphology	RED-TIDE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; TOXIN PROFILES; HALIM; REPRODUCTION; AUSTRALIA; CYCLE; CYST	Different life stages and the processes of asexual division and sexual fusion of the toxic dinoflagellate Alexandrium minutum are reported. Asexual division is oblique, with the two identically sized daughter cells sharing the parent theca and synthesizing the remaining plates. As in many dinoflagellate species, gametes are indistinguishable from vegetative cells prior to mating. During gamete fusion, which is initiated by flagellar attachment, a wide range of relative gamete orientations were observed. The longitudinal flagella of resultant motile planozygotes are not necessarily situated adjacent to each other, and planozygotes have thus perhaps not been recognised in previous studies which used this characteristic for identification. There are similarities between the life histories of A. minutum and the closely related species A. tamarense. Dinoflagellates exhibit various modes of reproduction and the details of life histories which may cause confusion are highlighted.	Univ Westminster, Sch Biosci, London W1M 8JS, England; IFREMER, Ctr Brest, F-29280 Plouzane, France	University of Westminster; Ifremer	Probert, I (通讯作者)，Univ Caen, LBBM, F-14032 Caen, France.		Probert, Ian/M-9807-2019					ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; BALECH E, 1989, PHYCOLOGIA, V28, P206, DOI 10.2216/i0031-8884-28-2-206.1; Balech E., 1995, Sherkin Island Marine Station; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; Chang F.H., 1995, P145; CHANG FH, 1996, P MARINE BIOTOXIN WO, V5, P2; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; DENN EE, 1991, P 1990 KOR FRENCH SE, P85; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; FLYNN K, 1994, MAR ECOL PROG SER, V111, P99, DOI 10.3354/meps111099; FRANCO JM, 1994, J APPL PHYCOL, V6, P275, DOI 10.1007/BF02181938; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; GAO XP, 1989, PHYCOLOGIA, V28, P342; Halim Y., 1960, Vie et Milieu, V11, P102; KELLER MD, 1987, J PHYCOL, V23, P633; MacKenzie L, 1997, NEW ZEAL J MAR FRESH, V31, P403, DOI 10.1080/00288330.1997.9516773; MONTAGNES D J S, 1987, Marine Microbial Food Webs, V2, P83; Nehring Stefan, 1994, Harmful Algae News, V9, P1; OSHIMA Y, 1989, NIPPON SUISAN GAKK, V55, P925, DOI 10.2331/suisan.55.925; PARTENSKY F, 1989, J PHYCOL, V25, P741, DOI 10.1111/j.0022-3646.1989.00741.x; TAKAHASHI K, 1985, J RADIO RES LAB, V32, P129; Walker L., 1984, MARINE PLANKTON LIFE	23	10	10	2	12	ADAC-CRYPTOGAMIE	PARIS	12 RUE DE BUFFON, 75005 PARIS, FRANCE	0181-1568			CRYPTOGAMIE ALGOL	Cryptogam. Algol.	OCT-DEC	2002	23	4					343	355						13	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	648BM					2025-03-11	WOS:000181130000006
J	Yamaguchi, M; Itakura, SG; Nagasaki, K; Kotani, Y				Yamaguchi, M; Itakura, SG; Nagasaki, K; Kotani, Y			Distribution and abundance of resting cysts of the toxic <i>Alexandrium</i> spp. (Dinophyceae) in sediments of the western Seto Inland Sea, Japan	FISHERIES SCIENCE			English	Article						Alexandrium catenella; Alexandrium tamarense; cyst; paralytic shellfish poisoning; Seto Inland Sea	DINOFLAGELLATE CYSTS; GONYAULAX-EXCAVATA; HIROSHIMA-BAY; TAMARENSIS; CATENELLA	Sediment samples were collected from 135 stations in the western part of the Seto Inland Sea (Iyo Nada, Suo Nada, Beppu Bay, Tokuyama Bay, Hiroshima Bay, Aki Nada, Hiuchi Nada and Bingo Nada) to determine the horizontal distribution and abundance of resting cysts of Alexandrium spp. (A. tamarense+ A. catenella). Enumeration of the cysts was performed using the primuline-staining direct count method. Cysts of Alexandrium spp. were rarely found in Iyo Nada, Suo Nada and Beppu Bay, but were widely distributed in Tokuyama Bay, Hiroshima Bay, Aki Nada, Hiuchi Nada and Bingo Nada. Cyst concentrations ranged from not detected (ND) to 14, ND to 17, ND to 4, 93 to 8137, 8 to 4454, ND to 6, ND to 18 and 4-29cysts/cm(3) wet sediment in Iyo Nada, Suo Nada, Beppu Bay, Tokuyama Bay, Hiroshima Bay, Aki Nada, Hiuchi Nada and Bingo Nada, respectively. The majority of cysts occurred in Tokuyama Bay and Hiroshima Bay, where higher densities were observed in the inner bay and along the coastal margin. Relatively higher cyst concentrations were observed at stations with a higher mud content. The abundance of Alexandrium spp. cysts in western Seto Inland Sea is lower than in the eastern Seto Inland Sea, except for Tokuyama Bay and Hiroshima Bay. However, because sporadic blooms of Alexandrium have been observed, continuing monitoring is necessary to prevent paralytic shellfish poisoning outbreaks in this area.	Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Hiroshima 7390452, Japan.	mineo@affrc.go.jp						Anderson D.M., 1985, P219; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1974, SEAFOOD TOXINS, P125; ANRAKU M, 1984, TOXIC RED TIDES SHEL, P105; BABA T, 2000, B YAMAGUCHI NAIKAI F, V28, P1; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; ETOH T, 1997, B FUKUOKA FISH MAR T, V7, P59; FUKUYO Y, 1985, B MAR SCI, V37, P529; Kamiyama T, 1996, J PLANKTON RES, V18, P1253, DOI 10.1093/plankt/18.7.1253; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kotani Yuichi, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P104; NAKASUGI Y, 1998, B JPN SOC FISH OCEAN, V62, P187; OKAICHI T, 1977, Nippon Suisan Gakkaishi, V43, P1251; Sakamoto Setsuko, 1999, Bulletin of Fisheries and Environment of Inland Sea, V1, P55; TURGEON J, 1990, TOXIC MARINE PHYTOPLANKTON, P238; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; Wall D., 1971, Geoscience Man, V3, P1; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Yamaguchi, 1996, HARMFUL TOXIC ALGAL, P177; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; Yamasaki T, 2001, NDT&E INT, V34, P207, DOI 10.1016/S0963-8695(00)00060-8; YAMASHITA A, 2001, B EHIME PREF FISH EX, V9, P35; Yoshimatsu S., 1992, B AKASHIWO RES I KAG, V4, P1; YOSHIMATSU S, 1983, B KAGAWA PREF FISH E, V20, P23	24	26	33	1	15	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	2002	68	5					1012	1019		10.1046/j.1444-2906.2002.00526.x	http://dx.doi.org/10.1046/j.1444-2906.2002.00526.x			8	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	609UP		Bronze			2025-03-11	WOS:000178923200008
J	Bennike, O; Abrahamsen, N; Bak, M; Israelson, C; Konradi, P; Matthiessen, J; Witkowski, A				Bennike, O; Abrahamsen, N; Bak, M; Israelson, C; Konradi, P; Matthiessen, J; Witkowski, A			A multi-proxy study of Pliocene sediments from Ile de France, North-East Greenland	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Greenland; Pliocene; mollusc; foraminifer; diatom; dinoflagellate; geochronology; Gauss chron	STRONTIUM ISOTOPIC COMPOSITION; DINOFLAGELLATE CYSTS; ARCTIC-OCEAN; MOLLUSCAN FAUNAS; MARINE DEPOSITS; LATE NEOGENE; PALEOCLIMATE; ENGLAND; BIOSTRATIGRAPHY; RECONSTRUCTION	A multi-technique approach has been used to study a Pliocene shallow water marine deposit, designated the (I) over cap le de France Formation, in North-East Greenland. The sequence is correlated on the basis of Sr-87-Sr-86 ratios in shells and palaeomagnetic studies with the Gauss normal polarity chron, which is dated to between 2.60 and 3.58 Ma years BP. This dating is in accordance with amino acid epimerisation and evidence from dinoflagellates, foraminifers and molluscs. Sediments, marine molluscs and foraminifers show that the sequence was deposited on the inner shelf, below storm wave base. Seawater temperatures were much higher than today, as demonstrated by the occurrence of a number of southern extra-limital species. The same applies to air temperature, and the few remains of land plants may indicate a forested upland with Picea and Thuja. A number of extinct taxa are present, including Nucula jensenii that is erected as a new species. (C) 2002 Elsevier Science B.V. All rights reserved.	Geol Survey Denmark & Greenland, DK-2400 Copenhagen NV, Denmark; Aarhus Univ, Dept Earth Sci, DK-8200 Aarhus N, Denmark; Univ Szczecin, Inst Marine Sci, PL-71412 Szczecin, Poland; Statens Inst Stralehyg, DK-2730 Herlev, Denmark; Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Geological Survey Of Denmark & Greenland; Aarhus University; University of Szczecin; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark.	obe@geus.dk	Abrahamsen, Niels/A-3553-2012; Bennike, Ole/G-7070-2018	Bennike, Ole/0000-0002-5486-9946; Matthiessen, Jens/0000-0002-6952-2494; Witkowski, Andrzej/0000-0003-1714-218X				ABRAHAMSEN N, 1986, PHYS EARTH PLANET IN, V44, P53, DOI 10.1016/0031-9201(86)90114-7; ALLISON RC, 1978, VELIGER, V21, P171; [Anonymous], 1991, BACILLARIOPHYCEAE; Bennike O., 1998, GEOLOGY GREENLAND SU, V180, P155, DOI 10.34194/ggub.v180.5100; BENNIKE O, 1990, MEDD GRONL GEOSCI, V23; Bennike O., 2000, GEOLOGY GREENLAND SU, V186, P29, DOI DOI 10.34194/GGUB.V186.5212; BENNIKE O, 1989, WERKGROUP TERT KWART, V26, P137; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; BOCHER J, 1995, MEDD GRONL GEOSCI, V33; BRIGHAMGRETTE J, 1992, ARCTIC, V45, P74; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Channell J. 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Paleoclimatol. Paleoecol.	OCT 1	2002	186	1-2					1	23	PII S0031-0182(02)00439	10.1016/S0031-0182(02)00439-X	http://dx.doi.org/10.1016/S0031-0182(02)00439-X			23	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	601HA					2025-03-11	WOS:000178439400001
J	Mao, SZ; Huang, CY; Lei, ZQ				Mao, SZ; Huang, CY; Lei, ZQ			Late Oligocene to early Miocene dinoflagellate cysts from the Kuohsing area, central Taiwan	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Taiwan; Oligocene; Miocene; dinoflagellate stratigraphy; environmental interpretation	NORTH-ATLANTIC OCEAN; ADJACENT SEAS; EOCENE; STRATIGRAPHY; DINOCYSTS; EVOLUTION; SEDIMENTS	Two dinoflagellate assemblages, first defined from the Pearl River Mouth Basin of the South China Sea, occur in the Oligocene-lower Miocene sediments of the Kuohsing area, Taiwan. The older Holnotryblium plectilum-Cordosphaeridium gracile Assemblage (1), characterized by the last occurrence of Chiropteridium lobospinosum, Cordosphaeridium gracile, Homotryblium abbreviatum, Homotryblium tenuispinosum, and Membranophoridium aspinatum, is late Oligocene; the younger Polysphaeridium zoharyi-Lingulodinium machaerophorum Assemblage (11), characterized by the first occurrence of Hystrichosphaeropsis obscura, Melitasphaeridium choanophorum and Tuberculodinium vancampoae, is early Miocene. The dominance/abundance of Polysphaeridium zoharyi in some of the Kuohsing samples suggests that the sediments of this area were deposited on a tropical-subtropical, inner neritic shelf. Slight sea-level fluctuations during the period of deposition reflect two shifts from an outer inner neritic to an inner inner neritic shelf, and ultimately to an inner outer neritic shelf environment at the time of highest sea-level. The present study strengthens previous findings that P. zoharyi is a warm-water indicator restricted to low latitudes, whereas Bitectatodinium tepikiense and Deflandrea are temperate- to cold-water indicators restricted to middle and high latitudes; and, that Nematosphaeropsis labyrinthus and Impagidinium prefer outer neritic/oceanic environments, whereas P. zoharyi prefers a shallow, inner neritic environment. (C) 2002 Elsevier Science B.V. All rights reserved.	China Univ Geosci, Dept Geol & Mineral Resources, Beijing 100083, Peoples R China; Taiwan Natl Univ, Dept Geol, Taipei, Taiwan; China Offshore Oil Nanhai E Corp, Ctr Sci & Technol, Guangzhou, Peoples R China	China University of Geosciences; National Taiwan University; China National Offshore Oil Corporation (CNOOC)	Mao, SZ (通讯作者)，China Univ Geosci, Dept Geol & Mineral Resources, 29 Xueyuan Rd, Beijing 100083, Peoples R China.							[Anonymous], 9210 GEOL SURV CAN; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1988, Geol. 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Palynology	OCT	2002	122	1-2					77	98	PII S0034-6667(01)00144-0	10.1016/S0034-6667(01)00144-0	http://dx.doi.org/10.1016/S0034-6667(01)00144-0			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	617FG					2025-03-11	WOS:000179350500006
J	Dale, B; Dale, AL; Jansen, JHF				Dale, B; Dale, AL; Jansen, JHF			Dinoflagellate cysts as environmental indicators in surface sediments from the Congo deep-sea fan and adjacent regions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; bottom sediments; Congo River; deep-sea fan; correspondence analysis; transfer function; paleoceanography	CANONICAL CORRESPONDENCE-ANALYSIS; SOUTH-ATLANTIC; MARINE-SEDIMENTS; NORTH-ATLANTIC; FORAMINIFERA; TEMPERATURE; CIRCULATION; VEGETATION; MELTWATER; NICHE	Forty-nine surface sediment samples from the Congo deep-sea fan and adjacent hydrographic environments were prepared palynologically and analyzed for fossilizable dinoflagellate cysts. The main objective was to investigate the extent to which cysts reflect present-day hydrography, and therefore may be used downcore as paleoceanographic indicators. The region sampled covers a range of marine environments including the Congo River plume, the area of pronounced upwelling off West-Central Africa, and a nearshore-offshore gradient from coastal to oceanic waters. This is the first study of the effect of a major tropical river plume on associated cyst assemblages. Cyst counts were low, particularly near the river mouth and furthest offshore. A combination of statistical treatments was used to analyze the surface cyst assemblages, including cluster analysis, correspondence analysis and canonical correspondence analysis. This helped to identify five distinctive sample groupings representing the main ecological signals in the cyst assemblage data. Group A, dominated by spherical brown protoperidinioid cysts, is an upwelling signal. Group B, dominated by the cosmopolitan species O. centrocarpum, is the main signal for the river plume effect, interpreted as reflecting the environmental instability this creates. Group C, dominated by S. delicatus with accessory O. centrocarpum, characterizes the outer plume, somehow reflecting the mixing of progressively diluted river plume water and the surrounding oceanic waters. Group D, with high proportions of Impagidinium and Nematosphaeropsis together with O. centrocarpurn and S. delicatus, characterizes the location of the Angola-Benguela Front. Group E, with mainly Impagidinium species, is an oceanic signal. The identification of nutrients and water stability as main determining factors influencing cyst signals has implications for cyst-based paleoenviromnental interpretations using transfer functions, which are developed almost exclusively from comparisons with more easily available data for sea-surface temperature, salinity, and sea ice. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Oslo, Dept Geol, N-0316 Oslo, Norway; GeoRes Consulting, N-2100 Skarnes, Norway; Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands	University of Oslo; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Univ Oslo, Dept Geol, PB 1047, N-0316 Oslo, Norway.	barrie.dale@uio.geologi.no; georc@online.no; jansen@nioz.nl						ABRANTES F, UNPUB DIATOMS SURFAC; Anderson NJ, 2000, EUR J PHYCOL, V35, P307, DOI 10.1080/09670260010001735911; [Anonymous], 1996, Palynology: principles and applications; AUSTIN MP, 1980, VEGETATIO, V42, P11, DOI 10.1007/BF00048865; BROECKER WS, 1989, NATURE, V341, P318, DOI 10.1038/341318a0; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; CADEE GC, 1978, NETH J SEA RES, V12, P368, DOI 10.1016/0077-7579(78)90040-6; DALE AL, QUATERNARY ENV MICRO; DALE B, 1985, NORSK GEOL TIDSSKR, V65, P97; Dale B., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; DALE B, IN PRESS QUATERNARY; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B, UNPUB PALEOGEOGR PAL; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 1996, NATURE, V381, P774, DOI 10.1038/381774a0; DEVERNAL A, 1998, DINO, P30; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Dupont L, 1999, PALAEOECO A, V26, P61; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; GAUCH HG, 1972, ECOLOGY, V53, P446, DOI 10.2307/1934231; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; GUIOT J, 1990, INSU MONOGR, V1; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HILL MO, 1973, J ECOL, V61, P237, DOI 10.2307/2258931; HILL MO, 1980, VEGETATIO, V42, P47, DOI 10.1007/BF00048870; HILL MO, 1979, DECORONA FORTRAN PRO; Imbrie J., 1971, LATE CENOZOIC GLACIA, P71; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Jansen JHF, 1996, S ATLANTIC PRESENT C, P363; Joliffe I.T., 1986, Principal Component Analysis; Jongman R.H.G., 1995, Data Analysis in Community and Landscape Ecology; KENKEL NC, 1986, ECOLOGY, V67, P919, DOI 10.2307/1939814; LESPERANCE PJ, 1990, PALAEONTOLOGY, V33, P209; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 1999, CR ACAD SCI II A, V329, P721, DOI 10.1016/S1251-8050(00)88491-8; MEEUWIS JM, 1990, S AFR J MARINE SCI, V9, P261; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; MUDIE PJ, 1990, NATO ADV SCI I C-MAT, V308, P609; MUDIE PJ, 1996, AASP FDN, V21, P843; Murray JW, 2001, MAR MICROPALEONTOL, V41, P1, DOI 10.1016/S0377-8398(00)00057-8; PETERSON RG, 1991, PROG OCEANOGR, V26, P1, DOI 10.1016/0079-6611(91)90006-8; Powell A.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V112, P297, DOI 10.2973/odp.proc.sr.112.196.1990; REID PC, 1972, J MAR BIOL ASSOC UK, V52, P939, DOI 10.1017/S0025315400040674; Reyment R.A., 1991, Multidimensional Palaeobiology; Rochon A, 1998, QUATERNARY RES, V49, P197, DOI 10.1006/qres.1997.1956; ROCHON A, 1999, AASP CONTRIB SER, V35; SCHNEIDER RR, 1995, PALEOCEANOGRAPHY, V10, P197, DOI 10.1029/94PA03308; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; ter Braak C.J.F., 1996, UNIMODAL MODELS RELA; ter Braak C.J. 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Paleoclimatol. Paleoecol.	SEP 15	2002	185	3-4					309	338	PII s0031-0182(02)00380-2	10.1016/S0031-0182(02)00380-2	http://dx.doi.org/10.1016/S0031-0182(02)00380-2			30	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	598GY					2025-03-11	WOS:000178268800004
J	Kosobokova, KN; Hirche, HJ; Scherzinger, T				Kosobokova, KN; Hirche, HJ; Scherzinger, T			Feeding ecology of <i>Spinocalanus antarcticus</i>, a mesopelagic copepod with a looped gut	MARINE BIOLOGY			English	Article							FATTY-ACID COMPOSITION; MARINE SNOW; CALANOID COPEPODS; ATLANTIC-OCEAN; ARCTIC-OCEAN; FOOD; CYANOBACTERIA; DETRITUS; SEA; ZOOPLANKTON	Spinocalanus antarcticus, an abundant mes-opelagic copepod in polar seas, has a greatly elongated and looped midgut, contrary to most other copepod species. The total gut length is 1.77, 1.86 and 1.90 times the total body length in adult females, CV and CIV, respectively. Gross morphology of the midgut is similar in all copepodite stages and adults ' It is described here from specimens collected in the Arctic Ocean. In stratified samples from the deep Amundsen and Makarov Basins S. antarcticus showed a clear preference for the depth layer between 100 and 500 m. Generally, the guts were packed with material, but most of it was impossible to identify. In most specimens the digestive tract was filled with undefined detritus particles ("detritus balls"). They were almost spherical, heterogeneous organic aggregates of 40-100 mum diameter, with small clay-sized mineral flakes imbedded. Mineral particles in the size range of 1-10 mum were found in large quantities in the guts of many specimens. Cysts of Chrysophycea and dinoflagellates and fragments of dinoflagellates, diatoms, tintinnids and radiolarians, as well as skeletons of silicoflagellates, were rather rare; some animal remnants were also found. A high carbon/nitrogen ratio (8.9) and very high lipid content (54% of dry weight) indicated a very good nutritional state. The adaptive significance and possible feeding strategy of this deep-water copepod is discussed.	Russian Acad Sci, PP Shirshov Inst Oceanol, Moscow 117853, Russia	Russian Academy of Sciences; Shirshov Institute of Oceanology	Hirche, HJ (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr 1, D-27568 Bremerhaven, Germany.		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Biol.	SEP	2002	141	3					503	511		10.1007/s00227-002-0848-z	http://dx.doi.org/10.1007/s00227-002-0848-z			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	606EZ					2025-03-11	WOS:000178722300010
J	Wendler, I; Zonneveld, KAF; Willems, H				Wendler, I; Zonneveld, KAF; Willems, H			Production of calcareous dinoflagellate cysts in response to monsoon forcing off Somalia: a sediment trap study	MARINE MICROPALEONTOLOGY			English	Article						calcareous dinoflagellate cysts; ecology; dissolution; Arabian Sea; monsoon	EASTERN EQUATORIAL ATLANTIC; WESTERN TROPICAL ATLANTIC; SPATIAL-DISTRIBUTION; QUATERNARY EASTERN; SURFACE SEDIMENTS; INDIAN-OCEAN; PHYTOPLANKTON; CALIFORNIA; HEIMII	To study the ecology of calcareous dinoflagellates we examined the impact of the SW and NE monsoons on cyst formation using sediment trap material, collected at 1032 in water depth, off Somalia from June 1992 to February 1993. The results do not confirm the relationship between cyst production and lower nutrient concentrations, as highest cyst fluxes were recorded during late SW monsoon under the relatively nutrient-rich and less agitated conditions of mature upwelled water. Lowest cyst fluxes were found under strongly stratified, nutrient-depleted surface waters, during the inter-monsoon. Although all of the studied species seem to prefer a stratified water column, an elevated concentration of nutrients appears to be necessary to maintain high cyst production. Comparison of the mean cyst flux to the sediment trap with that into the underlying surface sediments reveals a loss of 81-96%, which can be attributed to calcite dissolution. The relatively small spheres of Thoracosphaera heimii are affected more than the cysts of the other species. (C) 2002 Elsevier Science B.V. All rights reserved.	Fachbereich 5 Geowissensch, D-28334 Bremen, Germany	University of Bremen	Fachbereich 5 Geowissensch, Postfach 330 440, D-28334 Bremen, Germany.	flatter@uni-bremen.de						[Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; BANSE K, 1986, MAR ECOL PROG SER, V34, P201, DOI 10.3354/meps034201; BLASCO D, 1977, LIMNOL OCEANOGR, V22, P255, DOI 10.4319/lo.1977.22.2.0255; Boyer T.P., 1994, NOAA TECHNICAL REPOR, V81, P1; Broerse ATC, 2000, DEEP-SEA RES PT II, V47, P2179, DOI 10.1016/S0967-0645(00)00021-7; BRUMMER GJA, UNPUB MONSOONAL EXPO; BRUMMER GJA, 1995, TRACING SEASONAL UPW, V4, P55; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; GOODMAN D, 1984, J MAR RES, V42, P1019, DOI 10.1357/002224084788520800; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; Höll C, 2000, QUATERNARY RES, V54, P58, DOI 10.1006/qres.2000.2139; 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; 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; KERNTOPF B, 1997, THESIS; Margalef R., 1978, OECOL AQUATICA, V3, P97; MEIER KJS, IN PRESS J PHYCOL; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; SCHOTT F, 1983, PROG OCEANOGR, V12, P357, DOI 10.1016/0079-6611(83)90014-9; SHANNON LV, 1986, OCEANOGR MAR BIOL, V24, P65; SMITH SL, 1980, SCIENCE, V209, P597, DOI 10.1126/science.209.4456.597; Swallow J.C., 1976, Deep Sea Research and Oceanographic Abstracts, V13, P861, DOI DOI 10.1016/0011-7471(76)90908-6; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; THOMAS W H, 1990, Journal of Applied Phycology, V2, P71, DOI 10.1007/BF02179771; THOMAS WH, 1992, DEEP-SEA RES, V39, P1429, DOI 10.1016/0198-0149(92)90078-8; Van Weering TCE, 1997, DEEP-SEA RES PT II, V44, P1177, DOI 10.1016/S0967-0645(97)00029-5; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; 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; WENDLER I, IN PRESS GLOB PLANET; WENDLER I, IN PRESS SPEC PUBL G; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Zonneveld KAF, 2000, REV PALAEOBOT PALYNO, V111, P197, DOI 10.1016/S0034-6667(00)00024-5	35	38	40	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	SEP	2002	46	1-2					1	11	PII S0377-8398(02)00049-X	10.1016/S0377-8398(02)00049-X	http://dx.doi.org/10.1016/S0377-8398(02)00049-X			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	603TL					2025-03-11	WOS:000178576100001
J	Esper, O; Zonneveld, KAF				Esper, O; Zonneveld, KAF			Distribution of organic-walled dinoflagellate cysts in surface sediments of the Southern Ocean (eastern Atlantic sector) between the Subtropical Front and the Weddell Gyre	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; modern; ecology; South Atlantic; Southern Ocean	ANTARCTIC CIRCUMPOLAR CURRENT; LATITUDE MARINE ENVIRONMENTS; LATE QUATERNARY; COMMUNITY STRUCTURE; FALKLAND TROUGH; NORTH-ATLANTIC; INDIAN-OCEAN; BOTTOM WATER; SEA; AFRICA	Thirty-two surface sediment samples from the Southern Ocean (eastern Atlantic sector), between the Subtropical Front and the Weddell Gyre, were investigated to provide information on the distribution of modem organic-walled dinoflagellate cysts in relation to the oceanic fronts of the Antarctic Circumpolar Current (ACC). A clearly distinguishable distribution pattern was observed in relation to the water masses and fronts of the ACC. The dinoflagellate cysts of species characteristic of open oceanic environments, such as Impagidinium species, are highly abundant around the Subtropical Front, whereas south of this front, cosmopolitan species such as Nematosphaeropsis labyrinthus and the cysts of Protoceratium reticulatum characterise the transition from subtropical to subantarctic surface waters. The subantarctic surface waters are dominated by the cysts of heterotrophic dinoflagellates, such as Protoperidinium spp. and Selenopemphix antarctica. The cysts of Protoperidinium spp. form the dominant part of the assemblages around the Antarctic Polar Front, whereas S. antarctica concentrations increase further to the south. The presence of S. antarctica in sediments of the Maud Rise, a region of seasonal sea-ice cover, reflects its tolerance for low temperatures and sea-ice cover. A previously undescribed species, Cryodinium meridianum gen. nov. sp. nov., has a restricted distribution pattern between the Antarctic Polar Front and the ACC-Weddell Gyre Boundary. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Esper, O (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330 440, D-28334 Bremen, Germany.			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Micropaleontol.	SEP	2002	46	1-2					177	208	PII S0377-8398(02)00041-5	10.1016/S0377-8398(02)00041-5	http://dx.doi.org/10.1016/S0377-8398(02)00041-5			32	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	603TL					2025-03-11	WOS:000178576100010
J	Warny, SA; Wrenn, JH				Warny, SA; Wrenn, JH			Upper Neogene dinoflagellate cyst ecostratigraphy of the Atlantic coast of Morocco	MICROPALEONTOLOGY			English	Article							NORTH-ATLANTIC; MIOCENE; STRATIGRAPHY; OCEAN; CORE; SEA	New palynological data from the Sale brickyard (Atlantic coast of northern Morocco) are analyzed for their late Neogene biostratigraphical implications and the relationship with paleoenviron mental changes. Palynological zones (I to VI) described in this paper are based on palynomorph concentrations, fluctuations in species distribution, ratios between marine and continental palynomorphs, and the Last Appearance Datums (LADS) of twelve species. The brevity of some of the ranges in comparison with published dinoflagellates ranges from other locations is analyzed in view of important ecological events that took place in the Gibraltar Arc area at the end of the Miocene. Zone boundaries reflect global glacio-eustatic and/or local tectonic events that induced major modifications to the Atlantic/Mediterranean connections. The palynological data allow to differenciate time of eustatic versus tectonic control and permit to define how the paleoceanographic evolution of the Rifian Strait eventually led to the Messinian Salinity Crisis. We postulate that the nine LADs taking place at the Mio/Pliocene boundary results from the reconfiguration of oceanic circulation pattern and environmental conditions in the Gibraltar Strait area, as marine communication between the Atlantic Ocean and the Mediterranean Sea resumed, marking the end of the Messinian Salinity Crisis.	Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University	Warny, SA (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.		Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X				[Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, Palynology: principles and applications; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Benson R.H., 1991, Paleoceanography, V6, P164; BENSON RH, 1995, PALEOCEANOGRAPHY, V10, P1, DOI 10.1029/94PA02581; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; CANDE SC, 1995, J GEOPHYS RES-SOL EA, V100, P6093, DOI 10.1029/94JB03098; Clauzon G, 1996, GEOLOGY, V24, P363, DOI 10.1130/0091-7613(1996)024<0363:AIOTMS>2.3.CO;2; De Verteuil L., 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs, P391; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Duffield S.L., 1986, Papers from the First Symposium on Neogene Dinoflagellate Cyst Biostratigraphy. vol, V17, P27; EDWARDS LE, 1984, INITIAL REP DEEP SEA, V81, P581; ELBEIALY SY, 1990, J AFR EARTH SCI, V11, P291, DOI 10.1016/0899-5362(90)90007-2; Habib D., 1972, Initial Rep Deep Sea Drilling Project, V11, P367; Harland R., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P531; HARLAND R, 1978, I KONTINENTALSOKKELU, V100, P7; 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.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; HEAD MJ, 1989, 1 AASP PALYNOLOGIC S; HILGEN FJ, 2000, 11 C REG COMM MED NE, P5; HODELL DA, 1994, PALEOCEANOGRAPHY, V9, P835, DOI 10.1029/94PA01838; Hodell DA, 2001, PALEOCEANOGRAPHY, V16, P164, DOI 10.1029/1999PA000487; Hsu K.J., 1973, INITIAL REPORTS DEEP, V13, P1203; JARVIS I, 1985, INITIAL REP DEEP SEA, V85, P407; LENTIN JK, 1994, CAN J EARTH SCI, V31, P567, DOI 10.1139/e94-050; LONDEIX L, 1998, PLIOCENE TIME CHANGE, P65; MUDIE PJ, 1986, INITIAL REPORTS DEEP, V94, P785; PIASECKI S, 1980, GEOLOGICAL SURVEY B, V24, P53; Powell A.J., 1986, Contribution Series, V17, P83; Powell A.J., 1986, AASP CONTRIB SERIES, V17, P105; Powell A.J., 1986, AASP Contrib. Ser., V17, P129; SHACKLETON NJ, 1995, P OC DRILL PROGR SCI; Versteegh G.J.M., 1995, PALAEOENVIRONMENTAL; WARNY S, 1999, THESIS CATHOLIC U LO; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; Williams G.L, 1985, plankton stratigraphy; WILLIAMS GL, 1974, 7430 GEOL SURV CAN, V2, P107; WRENN J H, 1988, Palynology, V12, P129; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169	39	25	29	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	FAL	2002	48	3					257	272		10.2113/48.3.257	http://dx.doi.org/10.2113/48.3.257			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	628AT					2025-03-11	WOS:000179970100004
J	Anil, AC; Venkat, K; Sawant, SS; Dileepkumar, M; Dhargalkar, VK; Ramaiah, N; Harkantra, SN; Ansari, ZA				Anil, AC; Venkat, K; Sawant, SS; Dileepkumar, M; Dhargalkar, VK; Ramaiah, N; Harkantra, SN; Ansari, ZA			Marine bioinvasion: Concern for ecology and shipping	CURRENT SCIENCE			English	Article							INFECTIOUS-DISEASE; CLIMATE	Marine bioinvasion - introduction of marine organisms alien to local ecosystem through ship hulls and ballast water - has serious consequences to native biota, fishery and general coastal ecosystem. Over 80% of the world cargo is mobilized transoceanically and over 12 billion tones of ballast water is filled at one part of the ocean and discharged at the other. These ballast waters offer conducive situation for bacteria, viruses, algae, dinoflagellates and a variety of macro-faunal larval/cyst stages to translocate to alien regions, usually along the coasts of the continents. As an example, there are over 18 species of animals and plants documented along the Indian coasts as those that might have got invaded and established. They can cause deleterious effects to local flora and fauna through their toxigenic, proliferative and over-competitive characteristics. This article points out the threats arising out of marine bioinvasion and various technological developments needed to deal with this unavoidable scourge in global shipping transport.	Natl Inst Oceanog, Panaji 403004, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Anil, AC (通讯作者)，Natl Inst Oceanog, Panaji 403004, Goa, India.							Ahlstedt Steven A., 1994, Journal of Shellfish Research, V13, P330; BHATT YM, 1960, CURR SCI, V11, P439; Chandra Mohan P., 1994, P59; Colwell RR, 1996, SCIENCE, V274, P2025, DOI 10.1126/science.274.5295.2025; *IOC UNESCO, 1998, HARMF ALG NEWS, P17; Karande A.A., 1975, Bulletin of the Department of Marine Sciences University of Cochin, V7, P455; Lobitz B, 2000, P NATL ACAD SCI USA, V97, P1438, DOI 10.1073/pnas.97.4.1438; Meenakshi VK, 1998, INDIAN J MAR SCI, V27, P477; PEARCE F, 1995, NEW SCI, V2003, P38; Raju G.J.V.J., 1988, P513; RAJU PR, 1974, CURR SCI INDIA, V43, P52; Rao K. S., 1988, Marine biodeterioration., P57; RENGANATHAN TK, 1981, CURR SCI INDIA, V50, P1008; Ruiz GM, 2000, NATURE, V408, P49, DOI 10.1038/35040695; Santhakumaran L.N., 1986, Mahasagar, V19, P271; Santhakumaran L.N., 1985, Mahasagar, V18, P57; Untawale A.G., 1980, MAHASAGAR B NATL I O, V23, P179; VENUGOPALAN V P, 1987, Biological Oceanography, V5, P133; Venugopalan V.P., 1986, Mahasagar, V19, P213; WAGH AB, 1974, J BOMBAY NAT HIST SO, V70, P399	20	58	65	1	22	CURRENT SCIENCE ASSN	BANGALORE	C V RAMAN AVENUE, PO BOX 8005, BANGALORE 560 080, INDIA	0011-3891			CURR SCI INDIA	Curr. Sci.	AUG 10	2002	83	3					214	218						5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	600PP					2025-03-11	WOS:000178400000010
J	El Beialy, SY; Ali, AS				El Beialy, SY; Ali, AS			Dinoflagellates from the Miocene Rudeis and Kareem formations borehole GS-78-1, Gulf of Suez, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						dinoflagellates; Miocene; Rudeis; Kareem; Gulf; Egypt	STRATIGRAPHY	The Miocene Rudeis and the Kareem formations encountered in the Neogene part of the GS-78-1 borehole, Gulf of Suez produced diverse assemblages of dinoflagellate cysts, spores and pollen. The Early Miocene (Burdigalian) age assigned to the Rudeis Formation and the Early-?Middle Miocene (Langhian-Serravallian) age postulated for the Kareem formation is based on the presence of dinoflagellate cysts. These offer a good basis for biostratigraphic correlation of the Miocene deposits in the Gulf of Suez with those in the Nile Delta and Sinai in Egypt, and also with those present in key sections from the Mediterranean, the Canadian offshore sequences, Northwest Europe and from the North Atlantic. The terrestrial palynoflora (spores and pollen) affords no really precise, independent testimony as to the age of the samples, apart from being generally indicative of a Neogene age, in accord with the established gross age of the sediments, derived mainly from planktonic forams, calcareous nannoplankton and dinoflagellate cysts. The Rudeis Formation was deposited in a relatively deep water environment, based on the abundance fluctuations in miospores and dinoflagellates. However, the miospores recovered from the Rudeis Formation give an equivocal signal with respect to depositional environment. Such observed incursions of terrestrial elements in the Rudeis Formation could indicate that they might have been carried about within the basin of deposition by the waters of the Mediterranean Sea, or that they were displaced into a deep water setting. The overlying Kareem Formation was identified as an outer continental shelf deposit to upper bathyal (distal) environment because it contains a higher percentage of marine dinoflagellate cysts in most investigated samples, except in its uppermost part which shows the lowest percentage of marine forms. These include Spiniferites ramosus, S. pseudofurcatus, Operculodinium centrocarpum, Polysphaeridium zoharyi, Systematophora placacantha and Lingulodinium machaerophorum. The consistent presence of P. zoharyi in the Kareem Formation indicates that the Gulf of Suez was at times in the tropical to subtropical belt during the Early-?Middle Miocene age. (C) 2002 Elsevier Science Ltd. All rights reserved.	El Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt	Egyptian Knowledge Bank (EKB); Mansoura University; Egyptian Knowledge Bank (EKB); Tanta University	El Beialy, SY (通讯作者)，El Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt.		Soliman, Ali/R-1583-2018; Beialy, Salah/AAD-7329-2020	Soliman, Ali/0000-0001-7366-4607				ABDINE AS, 1984, EGYPTIAN J GEOLOGY, V28, P1; Ahmed A.B.A., 1994, P 12 EG GEN PETR COR, P468; [Anonymous], 1984, PETROLEUM EXPLORATIO; [Anonymous], EG GEN PETR CORP 8 E; [Anonymous], N JB GEOL PALAONT MH; [Anonymous], N JB GEOL PALAONTOL; [Anonymous], 1989, MICROFACIES EL UNPUB; ARAFA A. 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E., 1977, AM ASS STRATIGRAPHIC, V5A, P66; STOVER LE, 1978, GEOSCIENCE SERIES, V15; Stratigraphic Sub-Committee of the National Committee of Geological Sciences, 1974, EGYPTIAN J GEOLOGY, V18, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILIAMS GL, 1977, OCEANIC MICROPALAEON, P1231; Williams G.L., 1985, P847; Williams G.L., 1975, GEOL SURV CAN PAP, V2, P107, DOI DOI 10.4095/102513; WILLIAMS G.L., 1978, INITIAL REPORTT FHE, P783; WILLIAMS GL, 1988, AM ASS STRATIGRAPHIC, V34; YOUSSEF AA, 1988, NEUES JB GEOLOGIE PA, V177, P225; ZEVENBOOM D, 1995, THESIS U UTRECHT NET, P5	62	30	33	0	2	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0899-5362			J AFR EARTH SCI	J. Afr. Earth Sci.	AUG	2002	35	2					235	245	PII S0899-5362(02)00099-4	10.1016/S0899-5362(02)00099-4	http://dx.doi.org/10.1016/S0899-5362(02)00099-4			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	616KB					2025-03-11	WOS:000179302000006
J	Ellegaard, M; Lewis, J; Harding, I				Ellegaard, M; Lewis, J; Harding, I			Cyst-theca relationship, life cycle, and effects of temperature and salinity on the cyst morphology of <i>Gonyaulax baltica</i> sp nov (Dinophyceae from the Baltic Sea area]	JOURNAL OF PHYCOLOGY			English	Article						Gonyaulax; Gonyaulax baltica sp nov.; morphological variation; paleoecology; salinity; Spiniferites bulloideus; temperature	DINOFLAGELLATE; DINOPHYCEAE; SEDIMENTS; GROWTH	A new species of Gonyaulax, here named Gonyaulax baltica sp. nov., has been isolated from sediment samples from the southeastern Baltic. Culture strains were established from individually isolated cysts, and cyst formation was induced in a nitrogen-depleted medium. Although G. baltica cysts are similar to some forms attributed to Spiniferites bulloideus and the motile stage of G. baltica has affinities with G. spinifera, the combination of features of cyst and motile stage of G. baltica is unique. The culture strains were able to grow at salinity levels from 5 to 55 psu and formed cysts from 10 to 50 psu. Cultures at each salinity level were grown at 12, 16, and 20degrees C. Temperature- and salinity-controlled morphological variability was found in the resting cysts. Central body size varied with temperature and salinity, and process length varied with salinity. Cysts that formed at extreme salinity levels displayed lower average process length than cysts formed at intermediate salinity levels, and central body length and width were lowest at higher temperature and lower salinity. Models for the relationship between central body size and temperature/salinity and process length and salinity have been developed and may be used to determine relative paleosalinity and paleotemperature levels. Our results on salinity-dependent process length confirm earlier reports on short-spined cysts of this species found in low salinity environments, and the model makes it possible to attempt to quantify past salinity levels.	Univ Westminster, Sch Biosci, Phytosci Res Grp, London W1W 6UW, England; Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England	University of Westminster; NERC National Oceanography Centre; University of Southampton	Lewis, J (通讯作者)，Univ Westminster, Sch Biosci, Phytosci Res Grp, 115 New Cavendish St, London W1W 6UW, England.		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Phycol.	AUG	2002	38	4					775	789		10.1046/j.1529-8817.2002.01062.x	http://dx.doi.org/10.1046/j.1529-8817.2002.01062.x			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	590RU					2025-03-11	WOS:000177836500018
J	Chen, CY; Chou, HN				Chen, CY; Chou, HN			Fate of paralytic shellfish poisoning toxins in purple clam <i>Hiatula rostrata</i>, in outdoor culture and laboratory culture	MARINE POLLUTION BULLETIN			English	Article						purple clams; paralytic shellfish poisoning toxins; dinoflagellates; outdoor culture	RESTING CYSTS; DINOFLAGELLATE; ALEXANDRIUM; TOXICITY; TAIWAN	Purple clams (Hiatula rostrata Lighttoot) accumulate paralytic shellfish poisoning (PSP) toxins produced by a toxic strain of the dinoflagellate Alexandrium minutum Halim. The results confirm the data of our previous study concerning the muscle and siphon that were not showing a gradual rise in toxicity when shellfish accumulated more A. minutum. However, muscle and siphon are intermittently toxic both in exposure and depuration period in laboratory cultured purple clams. PSP toxins were detected in outdoor cultured purple clams, whereas no A. minutum were found in the culture pond during most of the survey time. The outdoor cultured purple clams need longer time to decrease toxicity to allowable levels than laboratory cultured purple clams. It was shown that laboratory data may not predict times over which pond-cultured purple clams may prove toxic to consumers. (C) 2002 Elsevier Science Ltd. All rights reserved.	Natl Sci Council, Sci & Technol Informat Ctr, Taipei 10636, Taiwan; Natl Taiwan Univ, Inst Fisheries Sci, Taipei 10617, Taiwan	National Taiwan University	Natl Sci Council, Sci & Technol Informat Ctr, 16F,106,Hoping E Rd,Sec 2, Taipei 10636, Taiwan.	cychen@mail.stic.gov.tw						Bricelj V. Monica, 1995, P413; BRICELJ VM, 1990, MAR ECOL PROG SER, V63, P177, DOI 10.3354/meps063177; BRICELJ VM, 1991, MAR ECOL PROG SER, V74, P33, DOI 10.3354/meps074033; Chen CY, 1998, TOXICON, V36, P515, DOI 10.1016/S0041-0101(97)00093-7; Chen CY, 2001, TOXICON, V39, P1029, DOI 10.1016/S0041-0101(00)00242-7; Chou HN, 1999, MANUAL MICROALGAL TO, P23; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; Gallacher S, 1997, APPL ENVIRON MICROB, V63, P239, DOI 10.1128/AEM.63.1.239-245.1997; GENENAH AA, 1981, J AGR FOOD CHEM, V29, P1289, DOI 10.1021/jf00108a047; Hallegraeff G.M., 1989, P77; Hallegraeff GM., 1995, MANUAL HARMFUL MARIN, P1, DOI DOI 10.1016/J.SCITOTENV.2020.139515; Horwitz W., 1995, OFFICIAL METHODS ASS, V35, P21; HWANG DF, 1987, B JPN SOC SCI FISH, V53, P623; Hwang DF, 1999, FISHERIES SCI, V65, P171, DOI 10.2331/fishsci.65.171; HWANG DF, 1995, J NAT TOXINS, V4, P173; Keller M.D., 1985, P113; Lassus P, 1996, J NAT TOXINS, V5, P107; Levasseur M., 1996, HARMFUL TOXIC ALGAL, P363; LIRDWITAYAPRASIT T, 1990, TOXIC MARINE PHYTOPLANKTON, P294; MARTIN JL, 1990, TOXIC MARINE PHYTOPLANKTON, P379; NAGASHIMA Y, 1987, NIPPON SUISAN GAKK, V53, P819; OSHIMA Y, 1992, TOXICON, V30, P1539, DOI 10.1016/0041-0101(92)90025-Z; Oshima Yasukatsu, 1995, P475; Shumway S.E., 1995, Manual on Harmful Marine Microalgae, P433; SULLIVAN JJ, 1985, J FOOD SCI, V50, P26, DOI 10.1111/j.1365-2621.1985.tb13269.x; WHITE AW, 1993, DEV MAR BIO, V3, P441	26	12	15	1	11	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	AUG	2002	44	8					733	738	PII S0025-326X(01)00307-1	10.1016/S0025-326X(01)00307-1	http://dx.doi.org/10.1016/S0025-326X(01)00307-1			6	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	592HE	12269475	Green Published			2025-03-11	WOS:000177930500013
J	Demske, D; Mohr, B; Oberhänsli, H				Demske, D; Mohr, B; Oberhänsli, H			Late Pliocene vegetation and climate of the Lake Baikal region, southern East Siberia, reconstructed from palynological data	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Central Asia; Late Pliocene; lacustrine sediments; pollens; palaeovegetation; palaeoclimate	LAST 2.5; RECORD; LOESS; RIFT; HISTORY; SEDIMENTATION; POLLEN; CHINA; FIELD; PART	Palynomorphs from a palacomagnetically dated Late Pliocene sediment core (3.6-2.35 Ma) reflect highly variable climatic conditions and repeated expansion of steppe and boreo-alpine vegetation. Mixed coniferous forests (Picea. Tsuga, Pinus) with associated broadleaved taxa (Quercus, Corylus, Ulmus, Tilia) were affected by dry and cold intervals already between 3.48 and 3.39 Ma. Peak records of non-arboreal pollen types and spores. including subarctic-boreo-alpine Selaginella selaginoides, evidence advances of open vegetation, which can be correlated to glacial marine oxygen isotope stages. A cooling trend occurred from 3.15 Ma to 2.5 Ma, documented by cold-dry intervals and increased fluctuations of Picea and Pinus. Around 3-2.9 Ma the palaeoclimate variation pattern shifted towards cold-dry and warm-moist oscillations. Cooling strengthened after 2.89 Ma and severely restricted Tsuga development. Cool and oligotrophic limnic conditions are documented by abundant Gonyaulax dinoflagellate cysts in the interval 2.65-2.57 Ma. Due to decreasing precipitation extensive areas with open steppe and rock-steppe vegetation became permanently established after 2.62 Ma. Dry conditions became a dominant environmental factor in the Baikal region. coeval in time with the Red Clay-Loess shift in northern China. This climatic transition can be explained as a consequence of major intensification of Northern Hemisphere Glaciation around 2.75 Ma evidenced by marine records of ice-rafted debris. (C) 2002 Elsevier Science B.V. All rights reserved.	Humboldt Univ, Museum Nat Kunde, D-10115 Berlin, Germany; Alfred Wegener Inst Polar & Marine Res, Forsch Stelle Potsdam, D-14473 Potsdam, Germany; Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany	Humboldt University of Berlin; Leibniz Institut fur Evolutions und Biodiversitatsforschung; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences	Free Univ Berlin, Inst Geol Wissensch, FR Palaontol, FB Geowissensch, Malteserstr 74-100 Haus D, D-12249 Berlin, Germany.	demske@zedat.fu-berlin.de						Alexeeva NV, 2000, QUATERN INT, V68, P5, DOI 10.1016/S1040-6182(00)00028-8; [Anonymous], 1997, EOS Transactions of the American Geophysical Union, V78, P597; [Anonymous], 1999, PLIOCENE TIME CHANGE; Back S, 1998, J GEOL SOC LONDON, V155, P61, DOI 10.1144/gsjgs.155.1.0061; BELOV AV, 1972, VEGETATION S E SIBER; Belova V.A., 1985, VEGETATION CLIMATE L; Bezrukova EV, 1999, GEOL GEOFIZ, V40, P739; BEZRUKOVA EV, 1999, PALEOGEOGRAPHY PRIBA; Bradbury J. 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J	Prasad, B; Pundeer, BS				Prasad, B; Pundeer, BS			Palynological events and zones in Cretaceous-Tertiary Boundary sediments of Krishna-Godavari and Cauvery basins, India	PALAEONTOGRAPHICA ABTEILUNG B-PALAOPHYTOLOGIE			English	Review						K-TB palynology; events and zones; Krishna-Godavari and Cauvery basins; India	DECCAN FLOOD BASALTS; K/T BOUNDARY; WESTERN INTERIOR; SEYMOUR-ISLAND; NEW-MEXICO; EL-KEF; VOLCANISM; CANADA; EXTINCTIONS; MEGHALAYA	Marine sediments across the K-T Boundary in Krishna-Godavari and Cauvery basins recorded rich and diversified palynological assemblages of spore-pollen and dinoflagellate cysts. Stratigraphically potential and age marker Maastrichtian and Danian palynofossils are identified and documented from three well sections for the recognition of palynological events and zones in the K-T transition sediments. In the studied K-TB sections, the characteristic Maastrichtian spore-pollen species, such as Aquilapollenites bengalensis, Gabonisporis bacaricumulus, Ghoshispora bella, Ariadnaesporites spiralis and Azolla cretacea, referable to the Aquilapollenites bengalensis Zone, disappear at the level at which the age marker dinoflagellate cysts, viz., Palynodinium grallator, Dinogymnium acuminatum and Triblastula utinensis show their last occurrences marking the Maastrichtian-Danian boundary. The last occurrence level of these palynofossils is also very close to the disappearance events of Abathomphalus mayaroensis, Globotruncana stuarti, Rugoglobigerina rugosa (forams) and Micula murus (nannoplankton) which define the K-T Boundary globally. Spore-pollen species, such as Gabonisporis vigourouxii, Scollardia trapaformis and Triporoletes asper disappear a little prior to the K-T extinction level and associated with the last occurrence level of dinoflagellate cysts - Circulodinium distinctum, Phelodinium magnificum and Andalusiella gabonensis. Other marker spore-pollen species, viz., Callistopollenites tumidoporus, Clavatricolporites lecticiae and Racemonocolpites maximus disappear much before the K-T extinction level near the boundary of Early and Late Maastrichtian, and their last occurrence level corresponds to the disappearance event of Xenascus ceratioides and Isabelidinium belfastense. The other important spore-pollen, such as Mulleripollis, Psittacopollis, Spinizonocolpites, Cranwellia, Equisetosporites and Racemonocolpites, which are very rarely represented in the Maastrichtian sediments, range across the K-T Boundary. These forms become quite abundant in the Danian sediments belonging to the Racemonocolpites romanus Zone and the Mulleripollis bolpurensis Zone of spore-pollen. The last occurrences of Racemonocolpites romanus and Cranwellia cauveriensis correspond to the LAD of Damassadinium californicum. However, Rutihesperipites trochuensis and Spinizonocolpites baculatus disappear at the last occurrence level of Cerodinium diebelii in the Lower Selandian and both the above events occur very close to the combined P3 / P2 foraminiferal zone. The recovered palynological. assemblages and recognised bio-events suggest that the palynofloral changes during K-T transition period were rather selective and gradual in Krishna-Godavari and Cauvery basins. The abrupt disappearance of palynomorphs and fern spore abundance-anomaly (FSAA) are not observed at or near the K-T Boundary. The observed selective and gradual disappearance of palynomorphs at only species level in the successive intertrappean beds, representing K-T transition sediments, is probably due to adverse environmental and climatic conditions caused by extensive Deccan volcanic activities in central India.	Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Dehra Dun 248195, Uttar Pradesh, India	Oil & Natural Gas Corporation	Prasad, B (通讯作者)，Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Dehra Dun 248195, Uttar Pradesh, India.							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Abt. B-Palaophytol.	AUG	2002	262	1-4					39	+						40	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	635LD					2025-03-11	WOS:000180399600003
J	Lindström, S				Lindström, S			<i>Lunnomidinium scaniense</i> Lindstrom, gen. et sp nov., a new suessiacean dinoflagellate cyst from the Rhaetian of Scania, southern Sweden	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Sweden; dinoflagellate cyst; Suessiaceae; Lunnomidinium; Late Triassic; Rhaetian		The dinoflagellate cyst Lunnomidinium scaniense gen. et sp. nov. is present in the lower part of a thin sequence of Rhaetian sedimentary rocks exposed in the Lunnom Coal and Clay Pit in NW Scania, southern Sweden! It occurs in diverse, Rhaetian palynomorph assemblages, dominated by spores and pollen, but with rare specimens of the dinoflagellate cysts Rhaetogonyaulax rhaetica (Sarjeant) Loeblich and Loeblich 1968, Shublikodinium sp. and Beaumontella? caminuspina (Wall) Below 1987. Lunnomidinium scaniense is characterized by an epicystal {tAtItP} archeopyle, a large number of paraplates arranged in seven or eight latitudinal series, and intratabular ornamentation in some but not all of the paraplate series. Thus, L. scaniense is assignable to the family Suessiaceae. Lunnomidinium scaniense can be subdivided into two different morphological varieties, based on the autophragm ornamentation and cyst size. (C) 2002 Elsevier Science B.V. All rights reserved.	Lund Univ, Dept Geol, SE-22362 Lund, Sweden	Lund University	Lindström, S (通讯作者)，Lund Univ, Dept Geol, Solvegatan 13, SE-22362 Lund, Sweden.		Lindström, Sofie/G-5481-2018	Lindstrom, Malin Sofie/0000-0001-8278-1055				[Anonymous], 1996, Palynology: principles and applications; Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; BATTEN D.J., 1996, PALYNOLOGY PRINCIPLE, V1, P205; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Fensome R.A., 1993, CLASSIFICATION FOSSI; GRADSTEIN FM, 1996, EPISODES, V19, P1; GUYOHLSON D, 1992, REV PALAEOBOT PALYNO, V71, P1, DOI 10.1016/0034-6667(92)90155-A; Lund J.J., 1977, DANMARKS GEOLOGISKE, V109, P103, DOI DOI 10.34194/RAEKKE2.V109.6900; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; Norling Erik, 1993, Sveriges Geologiska Undersokning Serie Ca Avhandlingar och Uppsatser, V82, P1; Palliani Raffaella Bucefalo, 1997, Palynology, V21, P197; Palliani RB, 2000, J MICROPALAEONTOL, V19, P133, DOI 10.1144/jm.19.2.133; Sivhed U, 1984, SVERIGES GEOLOGISK C, V78, P1	13	9	10	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUL 30	2002	120	3-4					247	261	PII S0034-6667(02)00079-9	10.1016/S0034-6667(02)00079-9	http://dx.doi.org/10.1016/S0034-6667(02)00079-9			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	593ZE					2025-03-11	WOS:000178023700005
J	Harland, R; Pudsey, CJ				Harland, R; Pudsey, CJ			Protoperidiniacean dinoflagellate cyst taxa from the Upper Miocene of ODP Leg 178, Antarctic Peninsula	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Ocean Drilling Program; Miocene; Antarctica; Southern Ocean; dinotlagellate cysts; Protoperidiniaceae; palaeoceanography	SURFACE SEDIMENTS; FALKLAND TROUGH; LATE QUATERNARY; PACIFIC MARGIN; WEDDELL; SEA; SCOTIA; OCEAN; DRIFT	Protoperidiniacean dinoflagellate cysts have been recovered from Upper Miocene sediments of Hole 1095, ODP Leg 178, drilled to the west of the Antarctic Peninsula. These cysts make up virtually the entire dinoflagellate cyst assemblages, and three new species are formally described herein as Selenopemphix bothrion sp. nov., Selenopemphix kepion sp. nov. and Selenopemphix minys sp. nov., together with one informal taxon and two species attributed to published taxa. The occurrence of Late Miocene protoperidiniacean-dominated assemblages in the vicinity of the Antarctic continent is of special interest. Their presence may indicate the initiation of the Antarctic Circumpolar Current and increased nutrient supply within the Southern Ocean as the Antarctic Divergence became established. A comparison with several other protoperidiniacean dinoflagellate assemblages of similar age in other parts of the world rovides some preliminary evidence for possible concomitant oceanographic change at this time. (C) 2002 Elsevier Science B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Anim & Plant Sci, Palynol Res Facil, Sheffield S10 2TN, S Yorkshire, England; British Antarctic Survey, Cambridge CB3 0ET, England	University of Sheffield; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.	rex.harland@ntlworld.com						[Anonymous], 1985, SPOROPOLLENIN DINOFL; BALECH E, 1965, BIOL ANTARCTIC SE 2, V5, P107; Balech E., 1988, Publ. Espec. Inst. Esp. Oceanogr., V1, P1; BALECH E, 1975, PUBL I ANTARCT ARGEN, V11, P1; BALECH E., 1973, Contrib Inst Antartico Argentino, V107, P1; Barker P.F., 1999, P ODP INIT REP, V178; Barker P.F., 1999, PROC OCEAN DRILL INI, P178; BARKER PF, 1995, P ODP INIT REP, V178; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Blow W. H., 1969, P199; Bujak J.P., 1983, AM ASS STRATIGRAPHIE, V13, P1; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Camerlenghi A, 1997, ANTARCT SCI, V9, P426, DOI 10.1017/S0954102097000552; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; De Verteuil L., 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs, P391; DODGE JD, 1987, J PLANKTON RES, V9, P685, DOI 10.1093/plankt/9.4.685; Duffield S.L., 1986, Papers from the First Symposium on Neogene Dinoflagellate Cyst Biostratigraphy. vol, V17, P27; Fensome RA, 1998, TAXON, V47, P695, DOI 10.2307/1223586; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Harland R, 1999, REV PALAEOBOT PALYNO, V107, P265, DOI 10.1016/S0034-6667(99)00023-8; Harland R, 1998, PALAEONTOLOGY, V41, P1093; HASSLER L, 2001, P ODP SCI RESULTS, P178; 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.J., 1996, Palynology: Principles and Applications, P1197; HEAD MJ, 1993, J PALEONTOL, V67, P1; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hillenbrand C.D., 2001, Proc. ODP, Sci. Results, V178; Kennett J.P., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P937; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 2001, J QUATERNARY SCI, V16, P739, DOI 10.1002/jqs.648; MATSUOKA K, 1982, REV PALAEOBOT PALYNO, V38, P109, DOI 10.1016/0034-6667(82)90052-5; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; Pudsey CJ, 1998, ANTARCT SCI, V10, P286, DOI 10.1017/S0954102098000376; PUDSEY CJ, 2001, P ODP SCI RESULTS, V178; REBESCO M, 1997, ANTARCT RES SER, V71, P29; Rebesco M., 1998, TERRA ANTARCTICA, V5, P715; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WOLFWELLING TCW, 2001, P ODP SCI RESULTS, V178; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; WRENN JH, 1999, PALYNOLOGY, V23, P268	43	6	6	0	4	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUL 30	2002	120	3-4					263	284	PII S0034-6667(02)00080-5	10.1016/S0034-6667(02)00080-5	http://dx.doi.org/10.1016/S0034-6667(02)00080-5			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	593ZE					2025-03-11	WOS:000178023700006
J	Ichimi, K; Suzuki, T; Ito, A				Ichimi, K; Suzuki, T; Ito, A			Variety of PSP toxin profiles in various culture strains of <i>Alexandrium tamarense</i> and change of toxin profile in natural <i>A-tamarense</i> population	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Alexandrium tamarense; PSP; toxic dinoflagellate	PARALYTIC SHELLFISH TOXINS; DINOFLAGELLATE PROTOGONYAULAX-TAMARENSIS; SCALLOP PATINOPECTEN-YESSOENSIS; CATENELLA; TOXICITY; GROWTH; TEMPERATURE; JAPAN	Paralytic shellfish poisoning (PSP) toxin profiles were compared between clonal and axenic culture strains of Alexandrium tamarense prepared from cysts. The cysts were collected from two stations in northern Japan. The major toxin components of A. tamarense were C2 and GTX4, however, the proportions of C2 and GTX4 varied largely 0.7-78.8 mol% and 79.4-8.5 mol%, respectively. Some culture strains contained significantly higher proportion of neoSTX than other strains. These results indicate that strains with various toxin profiles exist in the same region, and suggest that the comparison of the toxin profiles between strains at different localities is considerably difficult. A drastic change of the toxin profile was observed in natural plant-tonic populations containing A. tamarense. This may be explained by the presence of a lot of plank-tonic populations with various toxin profiles growing around the sea area. (C) 2002 Elsevier Science B.V. All rights reserved.	Tohoku Natl Fisheries Res Inst, Shiogama, Miyagi 9850001, Japan; Miyagi Prefecture Fisheries Res & Dev Ctr, Ishinomaki, Miyagi 9862135, Japan	Japan Fisheries Research & Education Agency (FRA)	Ichimi, K (通讯作者)，Kagawa Univ, Fac Agr, 2393 Ikenobe, Kagawa 7610795, Japan.	ichimi@stmail.ag.kagawa-u.ac.jp						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, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; Hwang DF, 2000, TOXICON, V38, P1491, DOI 10.1016/S0041-0101(00)00080-5; Ichimi K, 2001, J EXP MAR BIOL ECOL, V261, P17, DOI 10.1016/S0022-0981(01)00256-8; Ichimi Kazuhiko, 2000, Bulletin of Tohoku National Fisheries Research Institute, V63, P119; IMAMURA K, 1987, GUIDE STUDIES RED TI, P72; ISHIDA Y, 1993, DEV MAR BIO, V3, P881; Kawabata T., 1962, Bulletin of the Japanese Society of Scientific Fisheries, V28, P344; KIM CH, 1993, NIPPON SUISAN GAKK, V59, P641, DOI 10.2331/suisan.59.641; KIM CH, 1993, NIPPON SUISAN GAKK, V59, P633, DOI 10.2331/suisan.59.633; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; MARANDA L, 1985, ESTUAR COAST SHELF S, V21, P401, DOI 10.1016/0272-7714(85)90020-4; OGATA T, 1982, B JPN SOC SCI FISH, V48, P563; OGATA T, 1987, TOXICON, V25, P923, DOI 10.1016/0041-0101(87)90154-1; OGATA T, 1987, MAR BIOL, V95, P217, DOI 10.1007/BF00409008; Okaichi T, 1983, IUPAC PESTICIDE CHEM, P141; OSHIMA Y, 1990, TOXIC MARINE PHYTOPLANKTON, P391; OSHIMA Y, 1982, B JPN SOC SCI FISH, V48, P525; OSHIMA Y, 1995, J AOAC INT, V78, P528; OSHIMA Y, 1982, B JPN SOC SCI FISH, V48, P851; PROVASOLI L, 1957, ARCH MIKROBIOL, V25, P392, DOI 10.1007/BF00446694; Ravn H, 1995, J APPL PHYCOL, V7, P589, DOI 10.1007/BF00003947; Sakamoto Setsuko, 1998, Bulletin of Nansei National Fisheries Research Institute, V31, P45; SAKO Y, 1992, BIOSCI BIOTECH BIOCH, V56, P692, DOI 10.1271/bbb.56.692; Suzuki T, 1998, FISHERIES SCI, V64, P850, DOI 10.2331/fishsci.64.850; 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	28	59	64	1	11	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0022-0981			J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	JUL 3	2002	273	1					51	60	PII S0022-098(02)00137-5	10.1016/S0022-0981(02)00137-5	http://dx.doi.org/10.1016/S0022-0981(02)00137-5			10	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	566GN					2025-03-11	WOS:000176418700004
J	Courtinat, B; Piriou, S				Courtinat, B; Piriou, S			Palaeoenvironmental distribution of the Rhaetian dinoflagellate cysts <i>Dapcodinium priscum</i> EVITT, 196 1, emend. Below, 1987 and <i>Rhaetogonyaulax rhaetica</i> (SARJEANT) LOEBLICH and LOEBLICH, 1976, emend. Harland et al., 1975, emend.: Below, 1987	GEOBIOS			English	Article							BRENT-GROUP; FRANCE; PALYNOLOGY; NORWAY; TOOL	In almost all Rhaetian marine assemblages of the Tethyan Realm, two dinoflagellate cyst species, Dapcodinium priscum EVITT, 1961, emend. Below, 1987, and Rhaetogonyaulax rhaetica (SARJEANT) LOEBLICH and LOEBLICH, 1976, emend. Harland et al., 1975, emend. Below 1987 are dominant. Thus, when one is relatively frequent the other scarce and vice versa. This paper considers the inverse relationship of the two species in 235 rock samples taken from Rhaetian strata well exposed along the western margin of the Mesozoic intracratonic basin of south-eastern France. The palynological variables recorded from the samples (seven types of phytoclasts and three marine taxa: D. priscum, R. rhaetica and micrhystridids) were submitted to principal components analysis, which shows that D. priscum occurs in deposits that reflect nearshore and restricted marine environments. R. rhaetica is indicative of more marine environments at greater water depth, as indicated by the relatively high proportions of buoyant needle-like phytoclasts. These observations suggest that D. priscum is the cyst of an opportunistic, euryhaline dinoflagellate taxon that occupied various ecological niches while R. rhaetica inhabited more normal open marine environments. The palaeoenvironmental distribution seems to have been influenced by the energy level of the water column. D. priscum is found in deposits that denote high to low energy while R. rhaetica is found in low energy sediments. Micrhystridid occurrences are similar to those of D. priscum; they are uncommon when the abundance of R. rhaetica increases. (C) 2002 Editions scientifiques et medicales Elsevier SAS. All rights reserved.	Univ Lyon 1, Ctr Sci Terre, F-69622 Villeurbanne, France	Universite Claude Bernard Lyon 1	Courtinat, B (通讯作者)，Univ Lyon 1, Ctr Sci Terre, Batiment Geode,43,Blvd 11 Novembre, F-69622 Villeurbanne, France.							Adloff M. C., 1982, B INFORM GEOLOGUES B, V19, P9; [Anonymous], SCI GEOLOGIQUES B; [Anonymous], 1994, SEDIMENTATION ORGANI; Batten D., 1994, Cahiers de Micropaleontologie, V9, P21; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BRYANT ID, 1988, MAR PETROL GEOL, V5, P108; BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; COURTINAT B, 1998, GEOLOGIE FRANCE, P3; Deflandre G., 1945, Annales de Paleontologie, V31, P41; Doubinger J., 1977, SCI GEOL B, V30, P59; Dromart G, 1996, MAR PETROL GEOL, V13, P653, DOI 10.1016/0264-8172(96)00009-8; DROMART G, 1993, MEMOIRE HABILITATION; Fauconnier D, 1996, MAR PETROL GEOL, V13, P707, DOI 10.1016/0264-8172(95)00024-0; GORIN GE, 1991, PALAEOGEOGR PALAEOCL, V85, P303, DOI 10.1016/0031-0182(91)90164-M; HART G F, 1986, Palynology, V10, P1; Hubbard RNLB, 2000, PALAIOS, V15, P120, DOI 10.2307/3515498; Morbey J., 1975, Palaeontographica B, V152, P1; MORBEY SJ, 1974, REV PALAEOBOT PALYNO, V17, P161, DOI 10.1016/0034-6667(74)90097-9; Morgenroth P., 1970, Neues Jb. Geol. Palaont. Abh., V136, P345; Mussard JM, 1997, B CENT RECH EXPL, V21, P265; MUSSARD JM, 1994, B CENT RECH EXPL, V18, P463; POULSEN N.E., 1996, American Association of Stratigraphic Palynologists, Contribution Series, V31, P1; SCHUURMAN WML, 1977, REV PALAEOBOT PALYNO, V23, P159, DOI 10.1016/0034-6667(77)90007-0; Staplin FL., 1969, B CANADIAN PETROL GE, V17, P47; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; VANDERZWAN CJ, 1990, REV PALAEOBOT PALYNO, V62, P157, DOI 10.1016/0034-6667(90)90021-A; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; Whitaker M.F., 1992, Geology of the Brent Group, V61, P169; Whitaker M.F., 1984, Usage of Palynostratigraphy and Palynofacies in Definition of Troll Field Geology	29	12	12	0	0	EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS CEDEX 15	23 RUE LINOIS, 75724 PARIS CEDEX 15, FRANCE	0016-6995			GEOBIOS-LYON	Geobios	JUL-AUG	2002	35	4					429	439	PII S0016-6995(02)00038-4	10.1016/S0016-6995(02)00038-4	http://dx.doi.org/10.1016/S0016-6995(02)00038-4			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	623PM					2025-03-11	WOS:000179712100003
J	Versteegh, GJM; Zonneveld, KAF				Versteegh, GJM; Zonneveld, KAF			Use of selective degradation to separate preservation from productivity	GEOLOGY			English	Article						dinoflagellates; lipids; organic carbon; pollen; preservation; productivity	WALLED DINOFLAGELLATE CYSTS; ORGANIC-MATTER; SOUTH ATLANTIC; UPWELLING SYSTEM; PALEOPRODUCTIVITY; TEMPERATURE; VARIABILITY; SEDIMENTS; OCEAN	The assessment of diagenetic influences on the sedimentary record is problematic despite its crucial importance for accurate environmental reconstruction and understanding of biochemical cycles. We propose a general applicable method that uses differences in degradation rates of organic components to separate degradation and productivity. We demonstrate this method on a southeastern Atlantic sediment core covering the past 145 k.y. The new method solves discrepancies between existing organic matter, silica- and carbonate-based productivity reconstructions, and emphasizes the importance of bottom- and pore-water characteristics for transformation of the sedimentary record.	Nederlands Inst Onderzoek Zee, NL-1797 SZ Texel, Netherlands; Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Nederlands Inst Onderzoek Zee, Landsdiep 4, NL-1797 SZ Texel, Netherlands.		Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				Abrantes F, 2000, EARTH PLANET SC LETT, V176, P7, DOI 10.1016/S0012-821X(99)00312-X; Bickert T, 1999, DEEP-SEA RES PT II, V46, P437, DOI 10.1016/S0967-0645(98)00098-8; BICKERT T, 1998, S ATLANTIC, P599; DAMSTE JSS, 1998, 18 INT M ORG GEOCH S, P33; EGLINTON TI, 2001, P WORKSH ALK BAS PAL, V2; ESPER O, 2001, BERICHTE FACHBEREICH, V189, P1; GINGELE FX, 1995, USE PROXIES OCEANOGR, P365; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Hartnett HE, 1998, NATURE, V391, P572, DOI 10.1038/35351; Hedges J.I., 1993, Organic Geochemistry; HEDGES JI, 1995, MAR CHEM, V49, P81, DOI 10.1016/0304-4203(95)00008-F; Hinrichs KU, 1999, ORG GEOCHEM, V30, P341, DOI 10.1016/S0146-6380(99)00007-8; KIRST G, 1998, BERICHTE FACHBEREICH, V118, P1; Kirst GJ, 1999, QUATERNARY RES, V52, P92, DOI 10.1006/qres.1999.2040; Little MG, 1997, PALAEOGEOGR PALAEOCL, V130, P135, DOI 10.1016/S0031-0182(96)00136-8; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Prahl FG, 1997, ORG GEOCHEM, V27, P141, DOI 10.1016/S0146-6380(97)00078-8; Romero O.E., 1999, Use of Proxies in Paleoceanography, P365, DOI DOI 10.1007/978-3-642-58646-0_14; Rullkotter J., 2000, Marine Geochemistry, P129; Schmiedl G, 1997, PALAEOGEOGR PALAEOCL, V130, P43, DOI 10.1016/S0031-0182(96)00137-X; Schulz H.D., 2000, Marine Geochemistry, DOI [10.1007/978-3-662-04242-7_5, DOI 10.1007/978-3-662-04242-7_5]; Shi N, 2001, EARTH PLANET SC LETT, V187, P311, DOI 10.1016/S0012-821X(01)00267-9; Summerhayes CP, 1995, PROG OCEANOGR, V35, P207, DOI 10.1016/0079-6611(95)00008-5; Summons RE, 1993, Organic Geochemistry Principles and Applications, P3; Ufkes E, 2000, MAR MICROPALEONTOL, V40, P23, DOI 10.1016/S0377-8398(00)00030-X; Versteegh GJM, 2000, GEOCHIM COSMOCHIM AC, V64, P1879, DOI 10.1016/S0016-7037(99)00398-1; Wefer G., 1999, Use of proxies in paleoceanography, P1; 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; 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	31	91	101	0	19	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613	1943-2682		GEOLOGY	Geology	JUL	2002	30	7					615	618		10.1130/0091-7613(2002)030<0615:UOSDTS>2.0.CO;2	http://dx.doi.org/10.1130/0091-7613(2002)030<0615:UOSDTS>2.0.CO;2			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	569NB					2025-03-11	WOS:000176607500009
J	Garcés, E; Masó, M; Camp, J				Garcés, E; Masó, M; Camp, J			Role of temporary cysts in the population dynamics of <i>Alexandrium taylori</i> (Dinophyceae)	JOURNAL OF PLANKTON RESEARCH			English	Article							LIFE-HISTORY; HETEROCAPSA-CIRCULARISQUAMA; GONYAULAX-TAMARENSIS; DINOFLAGELLATE; GROWTH; BLOOM	Although temporary cyst stages are common in dinoflagellates, their role remains unclear. Every year Alexandrium taylori (Dinophyceae) forms dense patches (10(6) cells l(-1)) along La Fosca beach (Spain, northwest Mediterranean), which last for 2 months (July, August). One of the characteristics of the life history of A. taylori is the shift from a vegetative motile stage to non-motile temporary cysts. Here we present the temporal changes in the abundance of temporary cysts in sediments and their in situ encystment and excystment rates. The in situ encystment rate of temporary cysts from the water column to the sediment ranged from 1.8 x 10(6) to 4.4 x 10(6) cysts m(-2) day(-1,) whereas the excystment rate was between 0.9 x 10(6) to 2.7 x 10(6) cysts m(-2) day(-1) during the bloom period. Some of the temporary cysts in the sediment took more than 1 day to produce vegetative cells and remained viable for at least 4 days. We propose that temporary cyst formation in this species is a tool for reducing population losses. The production of temporary cysts can be an advantage since part of the population is stored in the sediments.	Inst Ciencias Mar, E-08039 Barcelona, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Garcés, E (通讯作者)，Inst Ciencias Mar, P Joan de Borbo,S-N, E-08039 Barcelona, Spain.		; Garces, Esther/C-5701-2011	Camp, Jordi/0000-0002-5202-9783; Garces, Esther/0000-0002-2712-501X				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; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Ellegaard M, 1998, J PLANKTON RES, V20, P1743, DOI 10.1093/plankt/20.9.1743; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; 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, IN PRESS LIFEHLAB LI; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Hallegraeff Gustaaf., 1995, Manual on Harmful Marine Microalgae; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; KITA T, 1985, B MAR SCI, V37, P643; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; Margalef R, 1997, SCI MAR, V61, P109; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; Nagasaki K, 2000, NIPPON SUISAN GAKK, V66, P666; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Schmitter R.E., 1979, P123; Uchida T, 1999, J EXP MAR BIOL ECOL, V241, P285, DOI 10.1016/S0022-0981(99)00088-X; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	21	44	48	1	13	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	JUL	2002	24	7					681	686		10.1093/plankt/24.7.681	http://dx.doi.org/10.1093/plankt/24.7.681			6	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	574VD		Bronze			2025-03-11	WOS:000176909500005
J	Troedson, AL; Riding, JB				Troedson, AL; Riding, JB			Upper oligocene to lowermost Miocene strata of King George Island, South Shetland Islands, Antarctica: Stratigraphy, facies analysis, and implications for the glacial history of the Antarctic Peninsula	JOURNAL OF SEDIMENTARY RESEARCH			English	Article							DEBRIS FLOW DEPOSITS; DINOFLAGELLATE CYSTS; PACIFIC MARGIN; WEDDELL SEA; ROSS; ENVIRONMENT; RETREAT; FJORDS	The Cape Melville Formation (CMF), exposed on southeastern King George Island, South Shetland Islands, provides rare evidence of extensive earliest Miocene glaciation in the Antarctic Peninsula region. The formation records the presence of regional marine-based grounded ice on the continental shelf. It overlies disconformably the upper Oligocene Destruction Bay Formation, which consists of sandstones recording nonglacial shallow marine conditions. Four units have been identified within the approximately 150 m thickness of the CMF. The basal unit (A) consists of coarse glacigenic debris-flow facies interbedded with glaciomarine mudstone and sandstone. The overlying unit (B) is mainly fine-grained. This succession may represent relatively ice-proximal deposition followed by glacial retreat and/or relative sea-level rise. The upper CMF (units C and D) was deposited in an ice-distal marine environment, with intermittent input of coarse glacigenic debris, mainly from ice rafting. Thin beds of pelagic carbonate ooze within unit C indicate periods of low terrigenous sediment input and high productivity. Lithologically diverse glacigenic gravel clasts (mainly ice-rafted debris) in the CMF had a wide regional source area, suggesting that ice cover was widespread regionally and included calving ice margins. For a small proportion of clasts; the nearest known source is the mountains fringing the southern Weddell Sea. Such clasts were presumably transported north in debris-laden icebergs by a strong, cold Weddell Sea surface current. A temperate glacial setting is tentatively inferred from the CMF. Palynological results confirm and enhance the paleoenvironmental interpretation from the sedimentology, and include the first early Miocene dinoflagellate cyst assemblages recorded on the Antarctic Peninsula. This reappraisal of the glacial record from the CMF provides valuable constraints on the Antarctic cryosphere and regional paleoenvironments in the mid-Cenozoic.	British Antarctic Survey, NERC, Cambridge CB3 0ET, England; British Geol Survey, Nat Environm Res Council, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Geol Survey New S Wales, POB 536, St Leonards, NSW 2065, Australia.							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Sediment. Res.	JUL	2002	72	4					510	523		10.1306/110601720510	http://dx.doi.org/10.1306/110601720510			14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	602LB					2025-03-11	WOS:000178505800007
J	Nagai, S; Matsuyama, Y; Takayama, H; Kotani, Y				Nagai, S; Matsuyama, Y; Takayama, H; Kotani, Y			Morphology of <i>Polykrikos kofoidii</i> and <i>P-schwartzii</i> (Dinophyceae, Polykrikaceae) cysts obtained in culture	PHYCOLOGIA			English	Article							DINOFLAGELLATE POLYKRIKOS; GYMNODINIUM-CATENATUM; PLANKTON; CELLS	We induced oncystment in Polykrikos kofoidii and P. schwartzii under laboratory conditions by repeated starvation and feeding of strains previously maintained on a prey culture of Cochlodinium sp. We demonstrate the morphological differences of the pseudocolonies and cysts and also describe the time course of the encystment process in both species. Polykrikos kofoidii cysts were ovoid, with the posterior part wider than the anterior part, thus showing a longitudinal asymmetry, and the cyst wall was commonly covered with coarse reticulate ornaments. They possessed a network of ridges formed by the periphragm and bifurcate, trifurcate, or spinous processes were usually well developed. In contrast, P. schwartzii cysts were typically elongate-elliptical or spindle-shaped and showed a rather evident longitudinal symmetry. They were covered with cylindrical, hatchet-shaped or spinous processes, arranged to form shelf-like ornamentation as seen in the light microscope. The morphological differences between the cysts of the two dinoflagellates allow unambiguous identification of the cysts, judging by data from several strains of both P. kofoidii and P. schwartzii. Cyst formation in both species progressed according to a similar time course: 1.5-2.5 hours elapsed from the time when pseudocolonies stopped swimming and sank to the bottom to when the cysts completed their ornamentation.	Fisheries Res Agcy Japan, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Saeki, Hiroshima 7390452, Japan; Hiroshima Fisheries Expt Stn, Ondo, Hiroshima 7371207, Japan	Japan Fisheries Research & Education Agency (FRA)	Nagai, S (通讯作者)，Fisheries Res Agcy Japan, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Tox Phytoplankton Sect, Ohno, Saeki, Hiroshima 7390452, Japan.		Nagai, Satoshi/HOA-8686-2023	Matsuyama, Yukihiko/0000-0002-2775-1723; Nagai, Satoshi/0000-0001-7510-0063				[Anonymous], 1873, Archiv fur mikroskopische Anatomie; [Anonymous], 1998, HARMFUL ALGAE XUNTA; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Bolch CJS, 2001, PHYCOLOGIA, V40, P162, DOI 10.2216/i0031-8884-40-2-162.1; CARRETO JI, 1986, J PLANKTON RES, V8, P15, DOI 10.1093/plankt/8.1.15; Cho Hyun-Jin, 2000, Plankton Biology and Ecology, V47, P134; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; FUKUYO Y, 1982, FUNDAMENTAL STUDIES, P205; HARLAND R, 1981, Palynology, V5, P65; Kofoid C. A., 1921, Memoirs of the University of California, V5, P1; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; Matsuoka K, 2000, MICROPALEONTOLOGY, V46, P360; Matsuoka K, 2000, PHYCOLOGIA, V39, P82, DOI 10.2216/i0031-8884-39-1-82.1; MATSUOKA K, 1990, ILLUSTRATED GUIDE MA, P70; Matsuyama Y, 1999, AQUAT MICROB ECOL, V17, P91, DOI 10.3354/ame017091; MOREYGAINES G, 1980, PHYCOLOGIA, V19, P230, DOI 10.2216/i0031-8884-19-3-230.1; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; REID PC, 1978, NEW PHYTOL, V80, P219, DOI 10.1111/j.1469-8137.1978.tb02284.x; SILVA ES, 1995, PHYCOLOGIA, V34, P396, DOI 10.2216/i0031-8884-34-5-396.1; TAKAHASHI K, 1985, J RADIO RES LAB, V32, P129; TAKEUCHI T, 1984, OUTBREAK GYMNODINIUM, P85; Uchida Takuji, 1996, Phycological Research, V44, P119, DOI 10.1111/j.1440-1835.1996.tb00040.x; Von Stosch HA., 1973, Br Phycol J, V8, P105; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Williams G.L., 2000, American Association of Stratigraphic Palynologists Contributions Series, V37, P1; Yamasaki T, 2001, NDT&E INT, V34, P207, DOI 10.1016/S0963-8695(00)00060-8	28	18	19	1	8	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	JUL	2002	41	4					319	327		10.2216/i0031-8884-41-4-319.1	http://dx.doi.org/10.2216/i0031-8884-41-4-319.1			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	596WX					2025-03-11	WOS:000178190400002
J	Skupien, P; Vasícek, Z				Skupien, P; Vasícek, Z			Lower cretaceous ammonite and dinocyst biostratigraphy and paleoenvironment of the silesian basin (Outer Western Carpathians)	GEOLOGICA CARPATHICA			English	Article						Silesian Unit; Lower Cretaceous; Barremian-Aptian; dinoflagellate cysts; ammonites; paleoecology	DINOFLAGELLATE CYSTS	The basinal, or Godula Sequence of the Silesian Unit of the Outer Western Carpathians incorporated in the present nappe structure is characterized by a considerable thickness of Lower Cretaceous dark-grey, prevailingly pelitic deposits. Barremian and Lower Aptian ammonites occur in several isolated fossiliferous beds. Non-calcareous dinoflagellate associations were analysed in the same beds to provide a correlation of both ammonite and dinoflagellate ranges. Where index ammonites are missing, associations of dinocysts become a key stratigraphic element in thick lithologically monotonous deposits. The composition of dinocysts also supports environmental and paleoclimatic reconstructions in the area studied.	Tech Univ Ostrava, Inst Geol Engn, CZ-70833 Ostrava, Czech Republic	Technical University of Ostrava	Skupien, P (通讯作者)，Tech Univ Ostrava, Inst Geol Engn, 17 Iistopadu, CZ-70833 Ostrava, Czech Republic.	petr.skupien@vsb.cz; zdenek.vasicek@vsb.cz	Vasicek, Zdenek/I-2303-2014; Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X				BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; Costa L.I., 1992, P99; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Delanoy G., 1998, Annales du Museum d'Histoire Naturelle de Nice, V12, P1; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; Hoedemaeker P.J., 1993, Revista Espanola de Paleontologia, V8, P117; Hohenegger L, 1861, GEOGNOSTISCHEN VERHA, P1; KLAJMON P, 1997, GEOL VYZK MOR SLEZ V, V4, P32; Leereveld H, 1997, CRETACEOUS RES, V18, P421, DOI 10.1006/cres.1997.0071; Leerveld H., 1995, LPP Contribution Series, V2, P1; Mencik E., 1983, USTR UST GEOL NCSAV, P1; SKUPIEN P, 2000, 6 INT CRET S VIENN, P128; Skupien P, 1997, SBOR VED PRACI VYS S, P34; SKUPIEN P, 1999, THESIS VSB TU OSTRAV, P1; Skupien P., 1998, GEOL VYZK MOR SLEZ R, P39; Uhlig V., 1883, Denkschriften der Kaiserlichen Akademie der Wissenschaften Wien, Mathematisch-Naturwissenschaftliche Klasse, V46, P127; VASICEK Z, 1977, Casopis Slezskeho Muzea Serie A Vedy Prirodni, V26, P129; Vasicek Z., 1972, ROZPRAVY USTREDNIHO, V38, P1; VASICEK Z, UNPUB J CZECH GEOL S; VASICEK Z, 1973, SBOR VED PRACI VYS S, V18, P101; VASICEK Z, 1981, SBOR VED PRACI VYS S, V25, P193; VASICEK Z, 1981, SBORNIK VEDECKYCH PR, V25, P119; VASICEK Z, 1969, SBOR VED PRACI VYS S, V15, P121; Vasicek Zdenek, 1998, Vestnik Ceskeho Geologickeho Ustavu, V73, P331; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9	25	22	23	0	5	SLOVAK ACADEMIC PRESS LTD	BRATISLAVA	PO BOX 57 NAM SLOBODY 6, 810 05 BRATISLAVA, SLOVAKIA	1335-0552			GEOL CARPATH	Geol. Carpath.	JUN	2002	53	3					179	189						11	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	590RQ					2025-03-11	WOS:000177836200005
J	Litaker, RW; Vandersea, MW; Kibler, SR; Madden, VJ; Noga, EJ; Tester, PA				Litaker, RW; Vandersea, MW; Kibler, SR; Madden, VJ; Noga, EJ; Tester, PA			Life cycle of the heterotrophic dinoflagellate <i>Pfiesteria piscicida</i> (Dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						dinospore; division cyst; homothallic; hypnocyst; hypnozygote; in situ hybridization; planomeiocyte; planozygote; PNA probe; resting cyst; temporary cyst	ALEXANDRIUM-TAYLORI DINOPHYCEAE; AMBUSH-PREDATOR DINOFLAGELLATE; WHOLE-CELL HYBRIDIZATION; SEXUAL REPRODUCTION; TOXIC DINOFLAGELLATE; GYMNODINIUM-FUNGIFORME; PHANTOM DINOFLAGELLATE; GONYAULAX-TAMARENSIS; FISH KILLS; RED TIDE	The putatively toxic dinoflagellate Pfiesteria piscicida (Steidinger et Burkholder) has been reported to have an unusual life cycle for a free-living marine dinoflagellate. As many as 24 life cycle stages were originally described for this species. During a recent phylogenetic study in which we used clonal cultures of P. piscicida , we were unable to confirm many reported life cycle stages. To resolve this discrepancy, we undertook a rigorous examination of the life cycle of P. piscicida using nuclear staining techniques combined with traditional light microscopy, high-resolution video microscopy, EM, and in situ hybridization with a suite of fluorescently labeled peptide nucleic acid (PNA) probes. The results showed that P. piscicida had a typical haplontic dinoflagellate life cycle. Asexual division occurred within a division cyst and not by binary fission of motile cells. Sexual reproduction of this homothallic species occurred via the fusion of isogamous gametes. Examination of tanks where P. piscicida was actively feeding on fish showed that amoebae were present; however, they were contaminants introduced with the fish. Whole cell probing using in situ hybridization techniques confirmed that these amoebae were hybridization negative for a P. piscicida -specific PNA probe. Direct observations of clonal P. piscicida cultures revealed no unusual life cycle stages. Furthermore, the results of this study provided no evidence for transformations to amoebae. We therefore conclude that P. piscicida has a life cycle typical of free-living marine dinoflagellates and lacks any amoeboid or other specious stages.	NOAA, Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, Beaufort, NC 28516 USA; Univ N Carolina, Program Mol Biol & Biotechnol, Chapel Hill, NC 27599 USA; Univ N Carolina, Microscopy Serv Lab, Chapel Hill, NC 27599 USA; N Carolina State Univ, Coll Vet Med, Raleigh, NC 27606 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; University of North Carolina; University of North Carolina Chapel Hill; University of North Carolina; University of North Carolina Chapel Hill; North Carolina State University	NOAA, Natl Ocean Serv, Ctr Coastal Fisheries & Habitat Res, 101 Pivers Isl Rd, Beaufort, NC 28516 USA.	Wayne.Litaker@noaa.gov	Litaker, Richard/AAH-2036-2021					ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BHAUD Y, 1988, J CELL SCI, V89, P197; BURKHOLDER J, 2000, S HARMF ALG US MAR B; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; BURKHOLDER JM, 1993, 9308 EPA; Campbell N.A., 1996, Biology, V4th; Carlsson C, 1996, NATURE, V380, P207, DOI 10.1038/380207a0; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; DEMERS DB, 1995, 6 INT S HUM ID; DREBES G, 1988, HELGOLANDER MEERESUN, V42, P563, DOI 10.1007/BF02365627; FAUST MA, 1993, DEV MAR BIO, V3, P121; FRANKER CK, 1971, J PHYCOL, V7, P165, DOI 10.1111/j.0022-3646.1971.00165.x; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; Gaines G., 1987, The Biology of Dinoflagellates, P224; 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; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Glasgow HB, 2000, ECOL APPL, V10, P1024, DOI 10.1890/1051-0761(2000)010[1024:WQTAMI]2.0.CO;2; Grattan LM, 2001, BIOSCIENCE, V51, P853, DOI 10.1641/0006-3568(2001)051[0853:HHROET]2.0.CO;2; GREEN FJ, 1990, SIGMAALDRICH HDB STA; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HIMES M, 1975, P NATL ACAD SCI USA, V72, P4546, DOI 10.1073/pnas.72.11.4546; Hoffman G.L., 1967, PARASITES N AM FRESH, DOI DOI 10.1525/9780520320253; KIBLER SR, 1999, THESIS OLD DOMINION; KITA T, 1985, B MAR SCI, V37, P643; LEWITUS AJ, 1995, ESTUARIES, V18, P373, DOI 10.2307/1352319; Litaker R.W., 2002, Manual of environmental microbiology, V2nd, P342; Litaker RW, 1999, J PHYCOL, V35, P1379, DOI 10.1046/j.1529-8817.1999.3561379.x; MARASOVIC I, 1989, ESTUAR COAST SHELF S, V28, P35, DOI 10.1016/0272-7714(89)90039-5; Miller PE, 1998, J PHYCOL, V34, P371, DOI 10.1046/j.1529-8817.1998.340371.x; Miller PE, 2000, J PHYCOL, V36, P238, DOI 10.1046/j.1529-8817.2000.99041.x; Nadakavukaren M., 1985, Botany: an introduction to plant biology; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; 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, 1989, INT REV CYTOL, V114, P249; Sampayo M.A. de M., 1985, P125; SCHNEPF E, 1992, EUR J PROTISTOL, V28, P3, DOI 10.1016/S0932-4739(11)80315-9; Sindermann C.J., 1970, Principal diseases of marine fish and shellfish; SPECTOR DL, 1981, AM J BOT, V68, P34, DOI 10.2307/2442989; SPERO HJ, 1981, J PHYCOL, V17, P43, DOI 10.1111/j.1529-8817.1981.tb00817.x; SPERO HJ, 1982, J PHYCOL, V18, P356, DOI 10.1111/j.1529-8817.1982.tb03196.x; SPERO HJ, 1979, THESIS TEXAS A M U C; Steidinger K.A., 1980, P407; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Von Stosch HA., 1973, Br Phycol J, V8, P105; Walker L.M., 1984, P19; WALKER LM, 1979, J PHYCOL, V15, P312; WALL D, 1975, 1ST P INT C TOX DIN, P249; ZINGMARK RG, 1970, J PHYCOL, V6, P122, DOI 10.1111/j.0022-3646.1970.00122.x	54	66	79	1	24	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	JUN	2002	38	3					442	463		10.1046/j.1529-8817.2002.t01-1-01242.x	http://dx.doi.org/10.1046/j.1529-8817.2002.t01-1-01242.x			22	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	563AY					2025-03-11	WOS:000176232300004
J	Coats, DW; Park, MG				Coats, DW; Park, MG			Parasitism of photosynthetic dinoflagellates by three strains of <i>Amoebophrya</i> (Dinophyta):: Parasite survival, infectivity, generation time, and host specificity	JOURNAL OF PHYCOLOGY			English	Article						Akashiwo sanguinea; Gymnodinium instriatum; Karlodinium micrum; plankton; protist; red tide	CHESAPEAKE-BAY; GYMNODINIUM-SANGUINEUM; POPULATION-DYNAMICS; CERATIUM; REPRODUCTION; LAKES	Amoebophrya ceratii (Koeppen) Cachon is an obligate parasite of dinoflagellates and may represent a species complex. However, little is known about the biology and host range of different strains of Amoebophrya Cachon. Here, we determined parasite generation time and dinospore infectivity, survival, and ability to infect nonprimary hosts for strains of Amoebophrya from Akashiwo sanguinea (Hirasaka) G. Hansen et Moestrup, Gymnodinium instriatum (Freudenthal et Lee) Coats comb. nov., and Karlodinium micrum (Leadbeater et Dodge) J. Larsen. Akashiwo sanguinea was readily infected, with parasite prevalence reaching 100% in dinospore:host inoculations above a 10:1 ratio. Parasitism also approached 100% in G. instriatum , but only when inoculations exceeded a 40:1 ratio. Karlodinium micrum appeared partially resistant to infection, as parasite prevalence saturated at 92%. Parasite generation time differed markedly among Amoebophrya strains. Survival and infectivity of dinospores decreased over time, with strains from G. instriatum and A. sanguinea unable to initiate infections after 2 and 5 days, respectively. By contrast, dinospores from Amoebophrya parasitizing K. micrum remained infective for up to 11 days. Akashiwo sanguinea and G. instriatum were not infected when exposed to dinospores from nonprimary Amoebophrya strains. Karlodinium micrum , however, was attacked by dinospores of Amoebophrya from the other two host species, but infections failed to reach maturity. Observed differences in host-parasite biology support the hypothesis that Amoebophrya ceratii represents a complex of host-specific species. Results also suggest that Amoebophrya strains have evolved somewhat divergent survival strategies that may encompass sexuality, heterotrophy during the "free-living" dinospore stage, and dormancy.	Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA	Smithsonian Institution; Smithsonian Environmental Research Center	Coats, DW (通讯作者)，Smithsonian Environm Res Ctr, POB 28, Edgewater, MD 21037 USA.			Coats, D Wayne/0000-0002-0636-189X				Anderson DM, 1997, NATURE, V388, P513, DOI 10.1038/41415; Cachon J., 1964, Annales des Sciences Naturelles (12), V6, P1; Cachon J., 1987, The Biology of Dinoflagellates, P571; CANTER HM, 1984, NEW PHYTOL, V97, P601, DOI 10.1111/j.1469-8137.1984.tb03624.x; Coats DW, 1999, J EUKARYOT MICROBIOL, V46, P402, DOI 10.1111/j.1550-7408.1999.tb04620.x; COATS DW, 1994, J EUKARYOT MICROBIOL, V41, P586, DOI 10.1111/j.1550-7408.1994.tb01520.x; Coats DW, 1996, AQUAT MICROB ECOL, V11, P1, DOI 10.3354/ame011001; COATS DW, 1982, MAR BIOL, V67, P71, DOI 10.1007/BF00397096; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Doucette G.J., 1998, NATO ASI Series Series G Ecological Sciences, V41, P619; Elbrachter M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P351; Erard-Le Denn E, 2000, ESTUAR COAST SHELF S, V50, P109, DOI 10.1006/ecss.1999.0537; FREUDENTHAL HD, 1963, J PROTOZOOL, V10, P182, DOI 10.1111/j.1550-7408.1963.tb01659.x; Galigher A.E., 1971, Essentials of practical microtechnique, V1st; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Gunderson J., 2000, Journal of Eukaryotic Microbiology, V47, p4A; HEANEY SI, 1988, HYDROBIOLOGIA, V161, P133, DOI 10.1007/BF00044106; Kirchner Marianna, 1999, Advances in Limnology, V54, P297; Li AS, 2000, J PLANKTON RES, V22, P2105, DOI 10.1093/plankt/22.11.2105; Maranda L, 2001, J PHYCOL, V37, P245, DOI 10.1046/j.1529-8817.2001.037002245.x; Montagnes D.J.J., 1993, Handbook of Methods in Aquatic Microbial Ecology, P229; Nishitani L., 1985, P225; NISHITANI L, 1984, AQUACULTURE, V39, P317, DOI 10.1016/0044-8486(84)90274-6; Norén F, 1999, EUR J PROTISTOL, V35, P233, DOI 10.1016/S0932-4739(99)80001-7; Park MG, 2002, MAR ECOL PROG SER, V227, P281, DOI 10.3354/meps227281; SILVA E S, 1985, Protistologica, V21, P429; SOMMER U, 1984, HYDROBIOLOGIA, V109, P159, DOI 10.1007/BF00011574; Starr RC, 1993, J PHYCOL S, V29, P94; Tarutani K, 2001, AQUAT MICROB ECOL, V23, P103, DOI 10.3354/ame023103; TAYLOR FJR, 1968, J FISH RES BOARD CAN, V25, P2241, DOI 10.1139/f68-197; Yih W, 2000, J EUKARYOT MICROBIOL, V47, P504, DOI 10.1111/j.1550-7408.2000.tb00082.x	31	130	149	2	34	BLACKWELL PUBLISHING INC	MALDEN	350 MAIN ST, MALDEN, MA 02148 USA	0022-3646			J PHYCOL	J. Phycol.	JUN	2002	38	3					520	528		10.1046/j.1529-8817.2002.t01-1-01200.x	http://dx.doi.org/10.1046/j.1529-8817.2002.t01-1-01200.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	563AY					2025-03-11	WOS:000176232300011
J	Pospelova, V; Head, MJ				Pospelova, V; Head, MJ			<i>Islandinium brevispinosum</i> sp nov (Dinoflagellata), a new organic-walled dinoflagellate cyst from modern estuarine sediments of New England (USA)	JOURNAL OF PHYCOLOGY			English	Article						Atlantic Ocean; estuaries; Islandinium brevispinosum; modern sediments; Massachusetts; nutrients; organic-walled dinoflagellate cysts; Rhode Island; salinity; USA	NORTHERN NORTH-ATLANTIC; SEA-ICE COVER; BAY; RECONSTRUCTION; ASSEMBLAGES; TEMPERATURE; SALINITY	Modern estuarine environments remain underexplored for dinoflagellate cysts, despite a rapidly increasing knowledge of cyst distributions in open marine sediments. A study of modern estuarine sediments in New England has revealed the presence of Islandinium brevispinosum sp. nov., a new organic-walled dinoflagellate cyst that is locally common and probably of heterotrophic affinity. Resistance of this cyst to standard palynological processing indicates its geological preservability, although fossils are not yet known. Previously assigned species of the genus Islandinium are characteristic of polar and subpolar environments today and cold paleoenvironments in the Quaternary. The present record of I. brevispinosum extends the ecological and geographical range of this genus into the warm temperate zone, where I. brevispinosum occupies specific environments with reduced salinities and elevated nutrient levels.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada; Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England	University of Cambridge	Pospelova, V (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 2K6, Canada.			Pospelova, Vera/0000-0003-4049-8133				ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson JT, 1998, ECOL MODEL, V112, P85; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Balech E., 1988, Publ. Espec. Inst. Esp. Oceanogr., V1, P1; BERGH R. S, 1881, DANSK NATURHISTORI 4, V3, P60; BOOTHROYD JC, 1985, MAR GEOL, V63, P35, DOI 10.1016/0025-3227(85)90079-9; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; de Vernal A, 2000, CAN J EARTH SCI, V37, P725, DOI [10.1139/cjes-37-5-725, 10.1139/e99-091]; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; de Vernal A, 1996, NATURE, V381, P774, DOI 10.1038/381774a0; Fensome R.A, 1993, AM MUSEUM NATURAL HI; GRAN H. H., 1935, JOUR BIOL BD CANADA, V1, P279; Haeckel E., 1894, Systematische Phylogenie. Vol. 1. Systematische Phylogenie der Protisten und Pflanzen, V1; HARLAND R, 1980, Grana, V19, P211; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hillaire-Marcel C, 2001, NATURE, V410, P1073, DOI 10.1038/35074059; Howes B., 1999, BAYWATCHERS; Jorgensen E., 1899, BERGENS MUSEUMS AARB, V2, P1; Keller AA, 1999, LIMNOL OCEANOGR, V44, P344, DOI 10.4319/lo.1999.44.2.0344; Lamontagne MG, 1995, BIOGEOCHEMISTRY, V31, P63; LEE V, 1997, RHODE ISLAND SEA GRA, V1470; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Mudie P. J., 1985, Quaternary Environments: Eastern Canadian Arctic, Baffin Bay And West Greenland, P263; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; Paulsen O., 1904, MEDD KOMM HAVUNDERS, V1, P1; PAULSEN O., 1907, SERIE PLANKTON, V1, P1; PIERCE RW, 1994, MAR ECOL PROG SER, V112, P225, DOI 10.3354/meps112225; POSPELOVA V, 2002, IN PRESS SCI TOTAL E; Rochon Andre, 1999, AASP Contributions Series, V35, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	35	56	56	0	3	BLACKWELL PUBLISHING INC	MALDEN	350 MAIN ST, MALDEN, MA 02148 USA	0022-3646			J PHYCOL	J. Phycol.	JUN	2002	38	3					593	601		10.1046/j.1529-8817.2002.t01-1-01206.x	http://dx.doi.org/10.1046/j.1529-8817.2002.t01-1-01206.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	563AY		Bronze			2025-03-11	WOS:000176232300019
J	Meier, KJS; Janofske, D; Willems, H				Meier, KJS; Janofske, D; Willems, H			New calcareous dinoflagellates (Calciodinelloideae) from the Mediterranean Sea	JOURNAL OF PHYCOLOGY			English	Article						calcareous cyst; Calciodinelloideae; Dinoflagellata; Mediterranean Sea; morphology; taxonomy	EQUATORIAL ATLANTIC-OCEAN; MARINE DINOFLAGELLATE; SURFACE SEDIMENTS; CYSTS; DINOPHYCEAE; SCRIPPSIELLA; PERIDINIALES; EASTERN	Investigations on calcareous dinoflagellates from surface sediments from the Mediterranean Sea revealed 14 species, including one new genus and four previously undescribed species: Calciodinellum levantinum sp. nov., Calciodinellum elongatum nov. comb., Lebessphaera urania gen. nov. et sp. nov., and Scripp- siella triquetracapitata sp. nov. Furthermore, Fuettererella cf. tesserula , so far only known from the fossil record, was found. The cyst-theca relationships of C. levantinum and C. elongatum are given, based on strains established from water samples of the Mediterranean Sea and the Atlantic Ocean. This study gives an insight into the importance of the modern Mediterranean Sea as an unique region concerning calcareous cyst producing dinoflagellates.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Meier, KJS (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.		Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. 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Phycol.	JUN	2002	38	3					602	615		10.1046/j.1529-8817.2002.t01-1-01191.x	http://dx.doi.org/10.1046/j.1529-8817.2002.t01-1-01191.x			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	563AY					2025-03-11	WOS:000176232300020
J	Bolch, CJS; Reynolds, MJ				Bolch, CJS; Reynolds, MJ			Species resolution and global distribution of microreticulate dinoflagellate cysts	JOURNAL OF PLANKTON RESEARCH			English	Article							GYMNODINIUM-CATENATUM DINOPHYCEAE; RECENT MARINE-SEDIMENTS; SP-NOV DINOPHYCEAE; RESTING CYSTS; GRAHAM DINOPHYCEAE; PLANKTON; BLOOMS; COAST; TEMPERATURE; KATTEGAT	The distribution, abundance and morphology of microreticulate dinoflagellate cysts were examined from samples collected from the coastal waters of Australia, the Baltic Sea, Hong Kong and Uruguay. On the basis of a combination of size range, variation in microreticulate pattern, and cyst wall colour, the three microreticulate species Gymnodinium catenatum (36-62 mum diameter), Gymnodinium nolleri (25-40 mum) and Gymnodinium microreticulatum (17-29 mum) could be distinguished. Only G. catenatum and G. microreticulatum were found at Australian sites. Gymnodinium microreticulatum was rare but widespread in sediments from Tasmania and temperate and tropical sites on mainland Australia, whereas G. catenatum was restricted to the eastern coast of Tasmania, southern Victoria, Port Lincoln [South Australia (SA)] and the Hawkesbury Estuary [New South Wales (NSW)]. Significant variation in G. catenatum mean cyst size was observed between sites, with mean diameters varying from 40.1 mum (Hawkesbury River, NSW) to 52.3 mum (Port Lincoln SA). Laboratory experiments suggest that cyst size may be predominantly a genetically determined, population-specific character, rather than being influenced by environmental parameters. Using the species criteria refined from the dataset, existing reports of microreticulate cysts are re-examined, and the global distribution of microreticulate cyst species and the biogeography of the toxic dinoflagellate G. catenatum are re-evaluated.	Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Oban PA34 4AD, Argyll, Scotland; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	University of the Highlands & Islands; University of Tasmania	Univ Tasmania, Sch Aquaculture, Locked Bag 3, Launceston, Tas 7250, Australia.	chris.bolch@utas.edu.au	Bolch, Christopher/J-7619-2014					Akselman R., 1998, HARMFUL ALGAE, P122; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; Amorim A., 1998, Harmful Algae. 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Plankton Res.	JUN	2002	24	6					565	578		10.1093/plankt/24.6.565	http://dx.doi.org/10.1093/plankt/24.6.565			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	572VU		Green Submitted, Bronze, Green Accepted			2025-03-11	WOS:000176796300003
J	Mudie, PJ; Rochon, A; Levac, E				Mudie, PJ; Rochon, A; Levac, E			Palynological records of red tide-producing species in Canada: past trends and implications for the future	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	Symposium on Palynology and Micropaleontology in Canadian Geoscience - New Frontiers and Application	MAY 29-JUN 02, 2000	UNIV CALGARY, CALGARY, CANADA	GeoCanada, Canadian Assoc Palynol	UNIV CALGARY	red tides; harmful algae; dinoflagellate cysts; Holocene; marine varves	SAANICH INLET; DINOFLAGELLATE CYSTS; BRITISH-COLUMBIA; INTERANNUAL VARIABILITY; POSTGLACIAL SEDIMENTS; LAMINATED SEDIMENTS; SCOTIAN SHELF; ASSEMBLAGES; BASIN; EUTROPHICATION	Increases in 'red tides' and other harmful algal blooms (HABs) during the past 50 yr on both the Atlantic and Pacific coasts of Canada suggest that global-scale factors, such as climate change and increased international shipping trade, are the driving forces. Because the historical record is too short to understand the long-term dynamics of HABs, the Holocene history of harmful phytoplankton species was examined using ultra-high resolution studies (annual to decadal scale) of dinoflagellate cysts as a proxy for 'red tide' production. Paleoecological transfer functions were then applied to the cyst assemblage data to determine correlations with changes in sea surface temperature and salinity. Pacific records were obtained from varved marine sediments in Saanich Inlet, British Columbia, and in the Santa Barbara Basin off California. Comparison of annual cyst production and historical plankton data provides cyst:theca ratios from which the magnitude of past bloom size can be evaluated. The 10 500-yr Pacific record clearly shows that the largest blooms correspond to cysts of Protoceratium reticulation and Gonyaulax spinifera during the early Holocene. Sporadic blooms of potentially toxic Alexandrium spp., Lingulodinium polyedrum and Gymnodinium spp. also occurred from ca. 7000 to 5000 yr BP and more frequently from ca. 2000 to 3000 yr BP. Individual Holocene blooms were up to 10 times larger than in the historical record but they almost always occurred sequentially, without overlap of 'red tide' species. In pre-historical times, the bloom cycles started and stopped abruptly in 10 yr or less, and they persisted for about 100-1000 yr. In contrast, the variability and near-concurrence of species blooms in the modern (past 60 yr) record is unmatched in the past, and suggests disequilibrium of the natural ecosystem structure, Atlantic records from La Have and Emerald basins on the Scotian Shelf are less precise because bioturbation limits time resolution to ca. 25 yr. However, cyst abundances of cf. Alexandrium, Protoceratium reticulatum, Gonyaulax spinifera and Lingulodinium polyedrum were also an order of magnitude larger in the early Holocene, where they correspond to a summer sea surface warming of 2-5degreesC. Lesser peaks also appear during the past 2000 yr where they apparently correspond to a slight increase in winter temperature. There is no evidence of much lower salinity that would support stronger stratification. The similarity of pre-industrial age cyst records of 'red tide' histories in the oceanographically different Pacific and Atlantic regions of Canada indicates that climate change (including surface temperature and storminess) is the main driving force stimulating blooms. This implies that HABs will reoccur regardless of efforts to limit spreading. However, reduced pollution may decrease the HAB diversity, thereby stabilizing the population dynamics and increasing the predictability of bloom occurrences. (C) 2002 Elsevier Science B.V. All rights reserved.	Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada; Dalhousie Univ, Ctr Marine Geol, Halifax, NS B3H 3J5, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Dalhousie University	Geol Survey Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	mudie@agc.bio.ns.ca						Abuso Z.V., 1999, ASEAN MARIEN ENV MAN, P488; Anderson D.M., 1985, P219; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; ANDERSON DM, 1994, SCI AM, V271, P62, DOI 10.1038/scientificamerican0894-62; [Anonymous], 1985, TOXIC DINOFLAGELLATE; BALCH WM, 1979, P 2 INT C TOX DIN BL, P275; Barss M. S, 1973, 7326 GEOL SURV CAN P, V73, P1; BlaisStevens A, 1997, CAN J EARTH SCI, V34, P1345, DOI 10.1139/e17-107; Burkholder JM, 1998, ECOL APPL, V8, pS37; CARRETO JI, 1986, J PLANKTON RES, V8, P15, DOI 10.1093/plankt/8.1.15; Cembella Allan D., 1998, NATO ASI Series Series G Ecological Sciences, V41, P381; Cullen J. 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Paleoclimatol. Paleoecol.	JUN 1	2002	180	1-3					159	186	PII S0031-0182(01)00427-8	10.1016/S0031-0182(01)00427-8	http://dx.doi.org/10.1016/S0031-0182(01)00427-8			28	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	566LQ					2025-03-11	WOS:000176429900008
J	Kumar, A; Patterson, RT				Kumar, A; Patterson, RT			Dinoflagellate cyst assemblages from Effingham Inlet, Vancouver Island, British Columbia, Canada	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	Symposium on Palynology and Micropaleontology in Canadian Geoscience - New Frontiers and Application	MAY 29-JUN 02, 2000	UNIV CALGARY, CALGARY, CANADA	GeoCanada, Canadian Assoc Palynol	UNIV CALGARY	fjord; palynomorphs; dinoflagellate cysts; salinity; oceanography	SEDIMENTS	A palynological study of surface samples from Effingham Inlet, southwestern Vancouver Island., British Columbia, was carried out to assess environmental and oceanographic controls on the distribution of dinoflagellate cyst species. Generally dinoflagellate cyst assemblages from all samples are dominated by Operculodinium centrocarpum sensu Wall and Dale, 1966, Spiniferites spp. and round brown (protoperidinioid) cysts. The differences among the assemblages are mainly in relative and absolute abundance of various taxa, presence and absence of various protoperidinioid taxa. species diversity (Shannon Diversity Index), dinoflagellate cyst concentration in the samples, and ratio of terrestrial to marine palynomorphs. Dinoflagellate cyst assemblages in the two sub-basins of this inlet are quite distinct, with the inner basin characterized by lower diversity and the outer basin being characterized by higher diversity due to the occurrence of several protoperidiniacean species. Primary productivity in this inlet is enhanced by periodic incursion of nutrient-rich surface water from the Pacific Ocean which is related to coastal upwelling. Primary productivity is higher in the outer basin than the inner basin. (C) 2002 Elsevier Science B.V. All rights reserved.	Carleton Univ, Coll Nat Sci, Ottawa Carleton Geosci Ctr, Ottawa, ON K1S 5B6, Canada; Carleton Univ, Coll Nat Sci, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada	University of Ottawa; Carleton University; Carleton University	Kumar, A (通讯作者)，Carleton Univ, Coll Nat Sci, Ottawa Carleton Geosci Ctr, 1125 Colonel By Dr, Ottawa, ON K1S 5B6, Canada.							Aksu A.E., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P617, DOI 10.2973/odp.proc.sr.105.140.1989; [Anonymous], 1980, PALEOBIOLOGY PLANT P; 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., 1996, PALYNOLOGY PRINCIPLE, P1249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1999, CAHIERS GEOTOP, V3; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Favorite F., 1976, INT N PACIFIC FISHER, V33; Fensome R.A., 1993, CLASSIFICATION FOSSI; GRIFFIN DA, 1989, COASTAL SHELF SCI, V30, P275; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head M. J., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P1; HEAD MJ, 2002, IN PRESS J QUAT SCI, V16; HEUSSER LE, 1983, CAN J EARTH SCI, V20, P873, DOI 10.1139/e83-077; Kendrew W.G., 1955, The climate of central Canada, P1; KUMAR A, 2000, 2 INT C APPL MICR ME; Mudie P.J., 1996, American Association of Stratigraphic Palynology Foundation, P843; MUDIE PJ, 1998, GEOL ASS CAN MIN ASS, pA30; MUDIE PJ, 1998, RAPPORT BOTANISK SER, P117; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Okaichi T., 1989, RED TIDES BIOL ENV S; PATTERSON RT, 1995, GEOGR PHYS QUATERN, V49, P409, DOI 10.7202/033063ar; Patterson RT, 2000, J FORAMIN RES, V30, P321, DOI 10.2113/0300321; Powell A.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V112, P297, DOI 10.2973/odp.proc.sr.112.196.1990; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Sageman BB, 1997, PALAIOS, V12, P449, DOI 10.2307/3515383; Smith E, 1998, J MATER SCI, V33, P29, DOI 10.1023/A:1004373024644; Taylor F. J. R., 1987, BOT MONOGR, V21; Thomson R.E., 1981, CAN SPEC PUBL FISH A, V56; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962	31	30	36	0	8	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	JUN 1	2002	180	1-3					187	206	PII S0031-0182(01)00428-X	10.1016/S0031-0182(01)00428-X	http://dx.doi.org/10.1016/S0031-0182(01)00428-X			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	566LQ					2025-03-11	WOS:000176429900009
J	Tsujino, M; Kamiyama, T; Uchida, T; Yamaguchi, M; Itakura, S				Tsujino, M; Kamiyama, T; Uchida, T; Yamaguchi, M; Itakura, S			Abundance and germination capability of resting cysts of <i>Alexandrium</i> spp. (Dinophyceae) from faecal pellets of macrobenthic organisms	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Alexandrium spp. resting cysts; macrobenthos; faecal pellets; predation	GONYAULAX-TAMARENSIS; HIROSHIMA-BAY; DINOFLAGELLATE; TEMPERATURE; SEDIMENTS	The Alexandrium spp. resting cysts were found abundantly in faecal pellets collected from the bottom sediments at two stations in Hiroshima Bay. It is considered that these faecal pellets were excreted by the macrobenthos, such as polychaeta and mollusca, based on their size and morphology. Polychaeta was the most dominant macrobenthos, and mollusca was the second most dominant group in Hiroshima Bay. The resting cysts of Alexandrium spp. in the bottom sediments at the two stations were counted in both the faecal pellets of macrobenthos and in the surrounding sediment. As a result, the number of cysts in the faecal pellets accounted for 28.9-35.2% of total cysts. In addition, cysts isolated from faecal pellets had almost the same germination ability as those in the sediment. Thus, Alexandrium cysts are tolerant to the predation and digestive processes of macrobenthic organisms. (C) 2002 Elsevier Science B.V. All rights reserved.	Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Coastal Environm & Prod Div, Hiroshima 7390452, Japan; Tohoku Natl Fisheries Res Inst, Fisheries Res Agcy, Coastal Fisheries & Aquaculture Div, Shiogama, Miyagi 9850001, Japan; Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA)	Tsujino, M (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Coastal Environm & Prod Div, Hiroshima 7390452, Japan.							ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; IMABAYASHI H, 1984, B JPN SOC SCI FISH, V502, P1855; KUDENOV JD, 1982, MAR BIOL, V70, P181, DOI 10.1007/BF00397683; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Takasugi Yoshio, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P187; Tsujino M, 2001, NIPPON SUISAN GAKK, V67, P850; Yamaguchi, 1996, HARMFUL TOXIC ALGAL, P177; 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; YOKOYAMA H, 1988, J EXP MAR BIOL ECOL, V123, P41, DOI 10.1016/0022-0981(88)90108-6	13	21	27	1	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0022-0981			J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	MAY 10	2002	271	1					1	7	PII S0022-0981(02)00024-2	10.1016/S0022-0981(02)00024-2	http://dx.doi.org/10.1016/S0022-0981(02)00024-2			7	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	550NE					2025-03-11	WOS:000175508500001
J	McQuoid, MR; Godhe, A; Nordberg, K				McQuoid, MR; Godhe, A; Nordberg, K			Viability of phytoplankton resting stages in the sediments of a coastal Swedish fjord	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						anoxia; cyst; diatom; dinoflagellate; laminated sediment; MPN; resting stages; spore; survival	MARINE PLANKTONIC DIATOMS; DINOFLAGELLATE CYSTS; CHAETOCEROS-PSEUDOCURVISETUS; SPORES; BACILLARIOPHYCEAE; GERMINATION; BAY; HYDROGRAPHY; RECRUITMENT; SURVIVAL	Viable diatom and dinoflagellate resting stages were recovered from sediments in Koljo Fjord on the west coast of Sweden. To determine the maximum survival time of buried resting stages, samples from sediment depths down to 50 cm were incubated at temperatures of 3, 10 and 18 degreesC. Sediment cores were dated by Pb-210 and the age of samples containing viable resting stages was determined using the constant rate of supply model. Dilution cultures of surface sediments allowed semiquantitative estimates of the potential seed bank. Dinoflagellate cysts from species such as Diplopsalis sp.. Gymnodinium nolleri, Oblea rotunda and Protoceratium reticulatum were viable clown to 15 cm depth, or 37 years old. Spores and resting cells of the diatoms Chaetoceros spp., Detonzda confervacea and Skeletonema costatum were viable to over 40 cm depth. and may have been buried for Man. decades. The seed bank of living resting stages in surficial sediments was found to be rich (c. 57000 diatom resting stages g(-1) wet weight and c. 200 dinoflagellate cysts g(-1) wet weight), and the percentage of viable resting stages was higher for spore- and cyst-forming species. The oxygen-deficient sediments in Koljo Fjord appear to be a natural conservator of cell viability, a condition not easily simulated in laboratory studies. These results are ecologically important since spores and cysts are a repository of genetic material able to repopulate waters if resuspended and exposed to suitable light, temperature and nutrients.	Univ Gothenburg, Dept Marine Bot, SE-40530 Gothenburg, Sweden; Univ Gothenburg, Dept Oceanog, SE-40530 Gothenburg, Sweden	University of Gothenburg; University of Gothenburg	Univ Gothenburg, Dept Marine Bot, POB 461, SE-40530 Gothenburg, Sweden.	melissa.mcquoid@marbot.gu.se		Nordberg, Kjell/0000-0003-0085-4607				AN KH, 1992, BOT MAR, V35, P61, DOI 10.1515/botm.1992.35.1.61; Anderson D.M., 1985, P219; 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; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; 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; BLANCO J, 1990, Scientia Marina, V54, P287; CARRICK HJ, 1993, LIMNOL OCEANOGR, V38, P1179, DOI 10.4319/lo.1993.38.6.1179; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; Clegg JS, 1997, J EXP BIOL, V200, P467; Dale B., 1983, P69; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; FIGUEIRAS FG, 1991, J PLANKTON RES, V13, P589, DOI 10.1093/plankt/13.3.589; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Guppy M, 1999, BIOL REV, V74, P1, DOI 10.1017/S0006323198005258; Gustafsson M, 1999, J SEA RES, V41, P163, DOI 10.1016/S1385-1101(99)00002-7; HANSEN G, 1992, PLANKTON INDRE DANSK, P45; Hargraves P.E., 1975, Nova Hedwigia, V53, P229; HARLAND R, 1999, RH990501, P1; Harris ASD, 1998, J EXP MAR BIOL ECOL, V231, P21, DOI 10.1016/S0022-0981(98)00061-6; HARRIS ASD, 1995, THESIS U WESTMINSTER; Hasle Grethe R., 1997, P5, DOI 10.1016/B978-012693018-4/50004-5; HOLLIBAUGH JT, 1981, J PHYCOL, V17, P1; HUBER G., 1923, FLORA, V16, P114; Imai I., 1984, Bulletin of Plankton Society of Japan, V31, P123; IMAI I., 1990, B COAST OCEANOGR, V28, P75; 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; JOSEFSON A, 2000, AM SOC LIMN OC ANN M; Julius M. L., 2000, Journal of Phycology, V36, P34; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; KUWATA A, 1993, MAR ECOL PROG SER, V102, P245, DOI 10.3354/meps102245; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; LIVINGSTONE D, 1980, BRIT PHYCOL J, V15, P357, DOI 10.1080/00071618000650361; MARCUS NH, 1994, LIMNOL OCEANOGR, V39, P154, DOI 10.4319/lo.1994.39.1.0154; Marcus NH, 1998, LIMNOL OCEANOGR, V43, P763, DOI 10.4319/lo.1998.43.5.0763; MARCUS NH, 1986, LIMNOL OCEANOGR, V31, P206, DOI 10.4319/lo.1986.31.1.0206; 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; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Oku O, 1999, MAR BIOL, V135, P425, DOI 10.1007/s002270050643; Perata P, 1997, ANN BOT-LONDON, V79, P49, DOI 10.1093/oxfordjournals.aob.a010306; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; PITCHER GC, 1991, PROG OCEANOGR, V28, P39, DOI 10.1016/0079-6611(91)90020-M; Riaux-Gobin C, 1996, PHYCOLOGIA, V35, P368, DOI 10.2216/i0031-8884-35-4-368.1; RiauxGobin C, 1997, DEEP-SEA RES PT II, V44, P1033, DOI 10.1016/S0967-0645(96)00106-3; RIAUXGOBIN C, 1992, CR ACAD SCI III-VIE, V314, P545; Rines J.E.B., 1988, The Chaetoceros Ehrenberg (Bacillariphyceae) Flora of Narragansett Bay, Rhode Island, U.S.A; SAKSHAUG E, 1986, J PLANKTON RES, V8, P619, DOI 10.1093/plankt/8.4.619; Sancetta C, 1989, PALEOCEANOGRAPHY, V4, P235, DOI 10.1029/PA004i003p00235; Shimada H., 1996, HARMFUL TOXIC ALGAL, P219; SICKOGOAD L, 1986, J PHYCOL, V22, P22, DOI 10.1111/j.1529-8817.1986.tb02510.x; Smetacek V, 1999, NATURE, V397, P475, DOI 10.1038/17219; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; Throndsen J., 1978, Monographs on oceanographic methodology, P218; ZGUROVSKAYA LN, 1977, OCEANOLOGY, V17, P75	64	150	174	2	57	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	2002	37	2					191	201		10.1017/S0967026202003670	http://dx.doi.org/10.1017/S0967026202003670			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	553VJ					2025-03-11	WOS:000175696400005
J	Barski, M				Barski, M			<i>Eodinia poulseni</i> sp nov., a dinoflagellate cyst from Middle Jurassic of Central Poland	JOURNAL OF MICROPALAEONTOLOGY			English	Article								A new species of dinoflagellate, Eodinia poulseni, is described from the Middle Jurassic of Central Poland. Light and scaning electron microscopy shows that this species has a complex cyst wall consisting of autophragm and ectophragm. Eodinia poulseni sp. nov. has similarities to some common Middle Jurassic species. especially when separate hypocysts are observed. Important differences between Eodinia pachytheca, Mosaicodinium mosaicum, Wanaea acollaris, W. cornucavata and Hurlandsia rugarum are discussed. Some phylogenetic and environmental relationships to the Early Cretaceous freshwater species Hurlandsia rugarum are suggested. H. rugarum shows similarity in archaeopyle, overall shape and tabulation formula but is acavate and also distinct from E. poulseni in time.	Univ Warsaw, Dept Geol, PL-02089 Warsaw, Poland	University of Warsaw	Barski, M (通讯作者)，Univ Warsaw, Dept Geol, 93 Zwirki I Wigury Str, PL-02089 Warsaw, Poland.			Barski, Marcin/0000-0002-4102-3538				Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; DODEKOVA L, 1975, BULG ACAD SCI PALAEO, V2, P17; Gocht H., 1975, Neues Jb Geol Paleont Abh, V148, P12; Lister J.K., 1988, NEUES JB GEOL PALAON, V8, P505; POULSEN NE, 1990, GEOLOGICAL SURVEY DE, V10; Poulsen Niels E., 1998, Acta Geologica Polonica, V48, P237; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1	7	0	0	1	4	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	MAY	2002	21		1				43	49		10.1144/jm.21.1.43	http://dx.doi.org/10.1144/jm.21.1.43			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	570YX		hybrid			2025-03-11	WOS:000176689000007
J	Duxbury, S				Duxbury, S			Two new Early Cretaceous dinocyst species from the Central North Sea Basin	JOURNAL OF MICROPALAEONTOLOGY			English	Article							DINOFLAGELLATE CYSTS	Two new species of dinocyst, Cerbia monilis and Hapsocysta susanac are described from the Lower Cretaceous of the Central North Sea Basin. The first ranges across the Aptian/Albian boundary and the latter is restricted to the Early to Middle Albian interval; both are valuable index taxa in this area. Hapsocysta susanae is remarkably similar to cysts 'without walls' described from the Late Oligocene and Early Miocene, and detailed comparisons are made. The ranges of the two species described here are illustrated against regional lithostratigraphic and biostratigraphic schemes.	Duxbury Stratigraph Consultants, Aberdeen AB15 8TT, Scotland		Duxbury, S (通讯作者)，Duxbury Stratigraph Consultants, 4 Coldstone Ave, Aberdeen AB15 8TT, Scotland.							Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1885, HG BRONNS KLASSEN OR; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; Damassa SP, 1997, REV PALAEOBOT PALYNO, V98, P159, DOI 10.1016/S0034-6667(97)00020-1; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Duxbury S, 2001, NEUES JAHRB GEOL P-A, V219, P95, DOI 10.1127/njgpa/219/2001/95; Eisenack A., 1958, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V106, P383; Eisenack A., 1960, P R SOC VIC, V72, P1; Fensome RA., 1993, CLASSIFICATION FOSSI; Jeremiah JM, 2000, PETROL GEOSCI, V6, P309, DOI 10.1144/petgeo.6.4.309; Johnson H., 1993, Lithostratigraphic Nomenclature of the UK North Sea; MANUM SB, 1979, REV PALAEOBOT PALYNO, V28, P237, DOI 10.1016/0034-6667(79)90026-5; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; MORGAN RP, 1980, MEM GEOL SURV NSW PA, V18, P1; Norris G., 1965, Palaeontological Bulletin Wellington, V40, P1; Pascher A., 1914, Berlin Ber D bot Ges, V32; SARJEANT WAS, 1985, REV PALAEOBOT PALYNO, V45, P47, DOI 10.1016/0034-6667(85)90065-X; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; WETZEL O., 1933, PALAEONTOGRAPHICA A, V78, P1	21	8	8	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.	MAY	2002	21		1				75	80		10.1144/jm.21.1.75	http://dx.doi.org/10.1144/jm.21.1.75			6	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	570YX		hybrid			2025-03-11	WOS:000176689000010
J	Streng, M; Hildebrand-Habel, T; Willems, H				Streng, M; Hildebrand-Habel, T; Willems, H			Revision of the genera <i>Sphaerodinella</i> Keupp and Versteegh, 1989 and <i>Orthopithonella</i> Keupp <i>in</i> Keupp and Mutterlose, 1984 (Calciodinelloideae, Calcareous Dinoflagellate cysts)	JOURNAL OF PALEONTOLOGY			English	Article							SOUTH ATLANTIC-OCEAN; GERMANY	The genus Sphaerodinella Keupp and Versteegh. 1989, became obsolete by the assignment of its type S. albatrosiana (Kamptner, 1963) to the genus Calciodinellum Deflandre, 1947. For the single remaining species of Sphaerodinella, which does not fit into the genus Calciodinellum, the new genus Caracomia is proposed, whose type is C. arctica (Gilbert and Clark, 1983) new genus, new combination. Additionally, a new species of Caracomia is described: Caracomia stella new genus and species. The regional distribution of the two species of Caracomia shows distinct regional preferences: Caracomia arctica is restricted to cold waters of both hemispheres, whereas Caracomia stella as yet has only been described from warmer environments. Thus, C. arctica can be used as a cold water indicator. Comparison of Caracomia with other genera has shown a close relationship to the type of Orthopithonella and exposed a common misinterpretation of this genus. Therefore, the genus Orthopithonella Keupp in Keupp and Mutterlose. 1984, is emended to unquestionably accommodate only the type O. gustafsonii.	Univ Bremen, D-28334 Bremen, Germany	University of Bremen	Streng, M (通讯作者)，Univ Bremen, POB 330 FB-5, D-28334 Bremen, Germany.		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Paleontol.	MAY	2002	76	3					397	407		10.1666/0022-3360(2002)076<0397:ROTGSK>2.0.CO;2	http://dx.doi.org/10.1666/0022-3360(2002)076<0397:ROTGSK>2.0.CO;2			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	548PV					2025-03-11	WOS:000175398500001
J	Lilly, EL; Kulis, DM; Gentien, P; Anderson, DM				Lilly, EL; Kulis, DM; Gentien, P; Anderson, DM			Paralytic shellfish poisoning toxins in France linked to a human-introduced strain of <i>Alexandrium catenella</i> from the western Pacific:: evidence from DNA and toxin analysis	JOURNAL OF PLANKTON RESEARCH			English	Article							SPECIES COMPLEX; GENETIC-MARKERS; DINOPHYCEAE; IDENTIFICATION; TAMARENSIS; BLOOMS; WATERS; CYSTS	In 1998, the toxins responsible for paralytic shellfish poisoning (PSP) were detected in Thau Lagoon, France. The causative organism was identified as Alexandrium tamarense, a member of the 'tamarensis' species complex. This dinoflagellate was first observed in the lagoon in 1995 by a monitoring programme following more than a decade with no observations of this species. The species is thus new to these waters, but its origins were unknown. In this paper, morphological and molecular data are anaysed for two clonal cultures established from the 1998 bloom. These data are compared to results from Alexandrium isolates originating elsewhere in the world to infer an origin. Thecal plate morphology, restriction fragment length polymorphism, DNA sequencing and toxin analyses demonstrate that the Thau Lagoon strains are A. catenella, and are closely related to populations of A. catenella found in temperate Asia, specfically the Japanese Temperate Asian riboype of the tamarense/catenella/fundyense species complex. They show no homology with strains from western European waters, including the Mediterranean. Until now, the Japanese Temperate Asian ribotype has not been reported outside the western Pacific. The most likely scenario is that A. catenella was introduced to Thau Lagoon via the ballast water of a ship docked at Sete, France, a shipping port in direct communication with the lagoon. This case provides a clear example of the dispersal of a toxic Alexandrium species, probably via human activities.	Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; IFREMER, Ctr Rech Ecol Marine & Aquaculture, F-17137 Lhoumeau, France	Woods Hole Oceanographic Institution; Ifremer	Lilly, EL (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.		anderson, david/E-6416-2011					ABADIE E, 1999, CONTAMINATION ETANG; Anderson D.M., 1989, P11; 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; Balech E., 1985, P33; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; GIBSON T, 1994, CLUSTAL, V10; 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; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; Oshima Y., 1989, 7 INT IUPAC S MYC PH, P319; SAIKI RK, 1988, SCIENCE, V239, P487, DOI 10.1126/science.2448875; 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, 1996, J PHYCOL, V32, P1022, DOI 10.1111/j.0022-3646.1996.01022.x; SMAYDA TJ, 1989, COASTAL ESTUARINE ST, P213; SWOFFORD DL, 2001, PAUP PHYLOGENETIC AN; Vila M, 2001, J PLANKTON RES, V23, P497, DOI 10.1093/plankt/23.5.497	21	132	142	1	32	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	MAY	2002	24	5					443	452		10.1093/plankt/24.5.443	http://dx.doi.org/10.1093/plankt/24.5.443			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	558FQ		Bronze			2025-03-11	WOS:000175956000003
J	Eynaud, F; Turon, JL; Matthiessen, J; Kissel, C; Peypouquet, JP; De Vernal, A; Henry, M				Eynaud, F; Turon, JL; Matthiessen, J; Kissel, C; Peypouquet, JP; De Vernal, A; Henry, M			Norwegian sea-surface palaeoenvironments of marine oxygen-isotope stage 3: the paradoxical response of dinoflagellate cysts	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; Norwegian Sea; marine oxygen-isotope stage 3; sea-ice cover; North Atlantic Oscillation	NORTHERN NORTH-ATLANTIC; EAST GREENLAND CURRENT; LAST GLACIAL PERIOD; CLIMATE RECORDS; RAPID CHANGES; NORDIC SEAS; ICE; SEDIMENTS; OCEAN; KA	High-resolution marine palynological data have been obtained from two very long sediment cores (MD952009 and MD952010) retrieved from the southern Norwegian Sea. The dinoflagellate cyst assemblages show pronounced fluctuations in composition, which correlate strongly with magnetic susceptibility records and also mimic the delta(18)O signal of the GISP2 Greenland ice-core. If focusing on the period from 48 to 30 cal. kyr BP, this correlation suggests a paradoxical response of the sea-surface environments to the atmospheric conditions over Greenland: when the Greenland delta(18)O signal reflects warm interstadial conditions, the Norwegian Sea depicts cold sea-surface temperatures with quasi-perennial sea-ice cover (based on dinoflagellate cysts). In contrast, when the Greenland delta(18)O records cold stadial periods, the Norwegian Sea-surface temperatures are warm (based on dinoflagellate cysts), probably linked to inflow of the North Atlantic Drift. These results, similar in both cores, are contrary to those of previous studies and shed light on a possible decoupling of Norwegian sea surface-water conditions and atmospheric conditions over Greenland. This decoupling could be linked to an atmosphere-ocean system behaving similar to that which the Northern Hemisphere is experiencing at present, i.e. strongly variable owing to the North Atlantic Oscillation. Copyright (C) 2002 John Wiley Sons, Ltd.	Univ Bordeaux 1, Dept Geol & Oceanog, CNRS, UMR EPOC 5805, F-33405 Talence, France; Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; CEA, CNRS, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France; Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Universite Paris Saclay; CEA; Centre National de la Recherche Scientifique (CNRS); University of Quebec; University of Quebec Montreal	Eynaud, F (通讯作者)，Univ Bordeaux 1, Dept Geol & Oceanog, CNRS, UMR EPOC 5805, Ave Fac, F-33405 Talence, France.		Catherine, Kissel/AAH-1647-2019; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Matthiessen, Jens/0000-0002-6952-2494; Eynaud, Frederique/0000-0003-1283-7425				[Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BALBON E, 2000, THESIS PARIS 11 ORSA; BASSINOT F, 1996, IFRTP PUBLICATIONS; BISCHOF JF, 1994, MAR GEOL, V117, P35, DOI 10.1016/0025-3227(94)90005-1; Blindheim J, 2000, DEEP-SEA RES PT I, V47, P655, DOI 10.1016/S0967-0637(99)00070-9; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; BOND G, 1992, NATURE, V360, P246; BOND GC, 1995, SCIENCE, V267, P1005, DOI 10.1126/science.267.5200.1005; Broecker WS, 1990, PALEOCEANOGRAPHY, V5, P469, DOI 10.1029/PA005i004p00469; Cortijo E, 1997, EARTH PLANET SC LETT, V146, P29, DOI 10.1016/S0012-821X(96)00217-8; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DANSGAARD W, 1993, NATURE, V364, P218, DOI 10.1038/364218a0; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1996, CAHIERS GEOTOP, V3, P1; De Vernal A., 1993, Nato. 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J	Pross, J; Schmiedl, G				Pross, J; Schmiedl, G			Early Oligocene dinoflagellate cysts from the Upper Rhine Graben (SW Germany): paleoenvironmental and paleoclimatic implications	MARINE MICROPALEONTOLOGY			English	Article						paleogene; Rupelian; dinoflagellates; paleoenvironment; humidity variations; Central Europe	NORTH-ATLANTIC OCEAN; SPECIES-DIVERSITY; LATE EOCENE; CLIMATE; SEA; EVOLUTION; SEDIMENTS; PLIOCENE	Using principal component analysis and cyst diversity and equity trends, we can recognize four distinct dinoflagellate cyst (dinocyst) assemblages from four Rupelian (Early Oligocene) cores in the Mainz Embayment of the northern Rhine Graben (SW Germany), These assemblages are the Spiniferites ramosus (PC1), Thalassiphora pelagica (PC2), Homotryblium tenuispinosum (PC3), and Vozzhennikovia spinula (PC4) assemblages. The four cores provide an onshore-offshore transect in the Mainz Embayment. The H. tenuispinosum assemblage shows high factor loadings in proximal to intermediate cores, which is interpreted to reflect temporary high-salinity conditions. Mean dinocyst diversity and equity increase with distance from the Mid-Rupelian shoreline, indicating increasingly stable paleoenvironmental conditions towards the center of the Mainz Embayment. Within individual cores, changes in dinocyst assemblages through time are related to paleoenvironmental and paleoclimatological changes. The three proximal to intermediate cores show dominance of the H. tenuispinosum assemblage repeatedly alternating with high factor loadings of the T pelagica assemblage. In both cases, dinocyst diversity and equity tend to be reduced. Highest factor loadings of the S. ramosus assemblage occur in intervals where neither of the above assemblages is dominant and tend to coincide with dinocyst diversity and equity maxima. We interpret this distribution pattern to denote different paleoceanographic conditions, reflecting drier and more humid phases in the Early Oligocene of Central Europe. During relatively dry periods, increased salinity conditions prevailed in proximal to intermediate settings of the Mainz Embayment, as reflected by the dominance of the H. tenuispinosum assemblage. During more humid periods, increased runoff led to higher nutrient availability and the formation of a pycnocline separating slightly less saline surface waters from higher saline deeper waters, thus impeding vertical circulation. These environmental conditions are documented in high loadings of the T. pelagica assemblage which is indicative of increased eutrophication and/or oxygen-depleted bottom waters. Transitions between drier and more humid periods, i.e. episodes of normal marine conditions, are characterized by high loadings predominantly of the S. ramosus assemblage as well as increased dinocyst diversity and equity values. We propose that the alternations between drier and more humid phases may be related to variations in the ocean-atmosphere moisture flux from the North Atlantic into Central Europe bearing a high-latitude climate signal. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Tubingen, Inst & Museum Geol & Paleontol, D-72076 Tubingen, Germany	Eberhard Karls University of Tubingen	Univ Tubingen, Inst & Museum Geol & Paleontol, Sigwartstr 10, D-72076 Tubingen, Germany.	joerg.pross@uni-tuebingen.de	Schmiedl, Gerhard/E-6644-2017	Schmiedl, Gerhard/0000-0002-2177-6858				Abreu VS, 1998, AAPG BULL, V82, P1385; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; [Anonymous], PALAEONTOGRAPHICA A; [Anonymous], NEOGENE QUATERNARY D; BALDI T, 1984, ECLOGAE GEOL HELV, V77, P1; BARRON EJ, 1989, GLOBAL PLANET CHANGE, V75, P157; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Beyrich E., 1854, Verhandlungen der Preuf3ischen Akademie der Wissenschaften, V1854, P640; Bice KL, 2000, PALAEOGEOGR PALAEOCL, V161, P295, DOI 10.1016/S0031-0182(00)00072-9; 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; 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Micropaleontol.	MAY	2002	45	1					1	24	PII S0377-8398(01)00046-9	10.1016/S0377-8398(01)00046-9	http://dx.doi.org/10.1016/S0377-8398(01)00046-9			24	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	566HJ					2025-03-11	WOS:000176420800001
J	Ibrahim, MIA; Ela, NMA; Kholeif, SE				Ibrahim, MIA; Ela, NMA; Kholeif, SE			Dinoflagellate cyst biostratigraphy of Jurassic-Lower Cretaceous formations of the North Eastern Desert, Egypt	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Review							MICROPLANKTON; PALYNOLOGY; STRATIGRAPHY; BOREHOLES; SYSTEM; BASIN; AREA	Cyst assemblages (184 species) belonging to 68 genera) recovered from the Jurassic to Lower Cretaceous strata of three deep wells (Abu Hammad-1, Kabrit-1 and Q-71-IX) located in the northern part of the Eastern Desert, Egypt, allow to recognize twelve informal biozones ranging from the Albian to the Toarcian or Aalenian. These biozones are correlated with well-documented zonations established for the same interval from other localities in and outside Egypt.	Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria, Egypt; Cairo Univ, Fac Sci, Dept Geol, Giza, Egypt; Natl Inst Oceanog & Fisheries, Alexandria, Egypt	Egyptian Knowledge Bank (EKB); Alexandria University; Egyptian Knowledge Bank (EKB); Cairo University; Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF)	Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria, Egypt.	mohamedibrahim59@hotmail.com	Ibrahim, Mohammed/IUQ-7100-2023	Ibrahim, Mohamed Ismail Abdou/0000-0002-5782-0435				Abou Ela N.M., 1990, EARTH SCI, V4, P95; ALFAR DM, 1966, GEOLOGY COAL DEPOSIT, V37; [Anonymous], [No title captured]; [Anonymous], ERSTE ROCKS D; Bailey D.A., 1991, Journal of Micropalaeontology, V9, P245; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Berthou P.Y., 1986, Comunicacoes dos Servicos Geologicos de Portugal, V72, P119; BERTHOU PY, 1990, REV PALAEOBOT PALYNO, V66, P313, DOI 10.1016/0034-6667(90)90045-K; Brenner G.J., 1974, Bulletin of the Geological Survey of Israel, V59, P1; BRENNER W., 1988, Tubinger Mikropalaontologische Mitteilungen, V6, P1; Bujak J.P., 1977, Developments in Palaeontology and Stratigraphy, V6, P321; BUJAK JP, 1978, GEOLOGICAL SURVEY CA, V297, P1; CONWAY BH, 1978, REV PALAEOBOT PALYNO, V26, P337, DOI 10.1016/0034-6667(78)90041-6; COURTINAT B, 1989, ORGANOCLASTS FORMATI, V150; DAVEY R J, 1974, Palaeontology (Oxford), V17, P623; Davey R.J., 1974, S STRATIGRAPHIC PALY, V3, P41; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; DAVEY RJ, 1982, GEOL SURV DENMARK B, V6; DAVIES E. 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Jahrb. Geol. Palaontol.-Abh.	MAY	2002	224	2					255	319						65	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	559RL					2025-03-11	WOS:000176039100004
J	Boucsein, B; Knies, J; Stein, R				Boucsein, B; Knies, J; Stein, R			Organic matter deposition along the Kara and Laptev Seas continental margin (eastern Arctic Ocean) during last deglaciation and Holocene: evidence from organic-geochemical and petrographical data	MARINE GEOLOGY			English	Article						organic petrology; Kara sea; Laptev sea; deglaciation; Holocene	NORTHERN BARENTS SEA; LATE WEICHSELIAN GLACIATION; FRANZ-VICTORIA-TROUGH; ATLANTIC-WATER; FRESH-WATER; EQUATORIAL ATLANTIC; CARBON DEPOSITION; ICE-SHEET; SEDIMENTS; CIRCULATION	Organic petrologic (maceral analysis) and bulk organic-geochemical studies were performed on five sediment cores from the Eurasian continental margin to reconstruct the environmental changes during the last similar to 13 000 yr. The core stratigraphy is based on AMS-C-14 dating, and correlation by magnetic susceptibility and lithostratigraphic characteristics. Variations in terrigenous, freshwater, and marine organic matter deposition document paleoceano-graphic and paleoclimatic, changes during the transition from the last deglaciation to the Holocene. Glacigenic diamictons deposited in the St. Anna Trough (northern Kara Sea) during the Last Glacial Maximum (LGM) are characterized by reworked terrigenous organic matter. In contrast, the Laptev Sea shelf was not covered by an ice-sheet, but was exposed by the lowered sea level. Increased deposition of marine organic matter (MOM) during deglaciation indicates enhanced surface-water productivity, possibly related to influence of Atlantic waters. The occurrence of freshwater alginite gives evidence for river discharge to the Kara and Laptev Seas after the LGM. At the eastern Laptev Sea slope, the first influence of Atlantic water masses is indicated by an increase in the contents of MOM and dinoflagellate cysts, with Operculodinium centrocarpum prior to similar to 10 000 yr BP. High sedimentation rates in the Kara and the Laptev Seas with the adjacent slope at the beginning of the Holocene are presumably related to increased freshwater and sediment discharge from the Siberian rivers. Evidence for elevated Holocene freshwater discharge to the Laptev Sea has been found between similar to 9.8 and 9 kyr BP, at similar to 5 kyr BP and at similar to 2.5 kyr BP. In the Kara Sea, an increased freshwater signal is obvious at similar to 8.5 kyr BP and at similar to 5 kyr BP. Higher portions of MOM were accumulated in the St. Anna Trough and at the Eurasian continental margin at several intervals during the Holocene. Increased primary productivity during these intervals is explained by seasonally ice-free conditions possibly associated with increased inflow of Atlantic waters. (C) 2002 Elsevier Science B.V. All rights reserved.	Alfred Wegener Inst Polar & Marine Res, D-27517 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Boucsein, B (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr,POB 120 161, D-27517 Bremerhaven, Germany.			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Geol.	APR 30	2002	183	1-4					67	87	PII S0025-3227(01)00249-3	10.1016/S0025-3227(01)00249-3	http://dx.doi.org/10.1016/S0025-3227(01)00249-3			21	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	561DA					2025-03-11	WOS:000176121100005
J	Wendler, J; Gräfe, KU; Willems, H				Wendler, J; Gräfe, KU; Willems, H			Reconstruction of mid-Cenomanian orbitally forced palaeoenvironmental changes based on calcareous dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Cretaceous; Cenomanian; Milankovitch cycles; palaeoceanography; calcareous dinoflagellate cysts; gamma ray	PARIS BASIN; TIME-SCALE; SEDIMENTS; PALEOCLIMATE; PRODUCTIVITY; SUCCESSIONS; ATLANTIC; NORTH; SEA; PALEOCEANOGRAPHY	Mid-Cenomanian, precession-controlled (21 ka) chalk-marl couplets of the Cap Blanc Nez section (Anglo-Paris Basin) have been studied with focus on the effects which Milankovitch cycles have had on the palaeoenvironment. In this paper, we present micropalaeontological and lithological proxies that enable the reconstruction of both the cycle architecture and the transformation of the orbitally forced signal into the sediment. A palaeoecological reconstruction based on changes in calcareous dinoflagellate cysts (c-dinocysts) assemblages was carried out, in which two characteristic ecological assemblages of c-dinocysts were identified. Gradual changes in absolute and relative abundance of the cyst species in these assemblages over several couplets depict a bundling pattern which is interpreted to reflect the modulation of the intensity of the precession cycle by the eccentricity cycle (100 ka). The stacking pattern in the natural gamma ray signal and the carbonate and TOC content has the same period and provides lithological support of the bundling. A shelf basin circulation model is proposed to explain the relation between orbitally forced climate change, its palaeoenvironmental consequences and the resulting sedimentary cyclicity. Variations in surface water circulation are reflected in the sediment by the chalk-marl couplets, the most distinctive couplets ocurring at the base and top of the bundles. While the chalks reflect well-mixed surface water conditions, the marls, particularly those at the bundle boundaries, can be interpreted as the sedimentary expression of stratified water masses. During deposition of these marls, reduced oceanic mixing due to low seasonality during strong precession maxima at the eccentricity maxima caused periods of water column stratification that in turn led to nutrient depletion and decreased productivity in the surface water masses. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich 5, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich 5, POB 330440, D-28334 Bremen, Germany.	wendler@uni-bremen.de						[Anonymous], 1986, GEOLOGY, V14, P153; [Anonymous], MILANKOVITCH CLIMA 1; AROSTEGUI J, 1991, CLAY MINER, V26, P535, DOI 10.1180/claymin.1991.026.4.08; BARRON EJ, 1989, GLOBAL PLANET CHANGE, V75, P157; BARRON EJ, 1983, EARTH-SCI REV, V19, P305, DOI 10.1016/0012-8252(83)90001-6; BEIN A, 1976, Micropaleontology (New York), V22, P83, DOI 10.2307/1485322; 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]; Bignot G., 1964, Revue de Micropaleontologie, V7, P138; Bottjer DJ, 1986, PALEOCEANOGRAPHY, V1, P467, DOI 10.1029/PA001i004p00467; BOUYX E, 1986, Cretaceous Research, V7, P327, DOI 10.1016/0195-6671(86)90008-X; Boyd R., 1994, Special Publication of the International Association of Sedimentologists, V19, P145; BRALOWER TJ, 1984, GEOLOGY, V12, P614, DOI 10.1130/0091-7613(1984)12<614:LPASDC>2.0.CO;2; 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Paleoclimatol. Paleoecol.	APR 15	2002	179	1-2					19	41	PII S0031-0182(01)00366-2	10.1016/S0031-0182(01)00366-2	http://dx.doi.org/10.1016/S0031-0182(01)00366-2			23	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	560QX					2025-03-11	WOS:000176093700002
J	Wendler, J; Gräfe, KU; Willems, H				Wendler, J; Gräfe, KU; Willems, H			Palaeoecology of calcareous dinoflagellate cysts in the mid-Cenomanian Boreal Realm:: implications for the reconstruction of palaeoceanography of the NW European shelf sea	CRETACEOUS RESEARCH			English	Article						Cenomanian; palaeoecology; calcispheres; calcareous dinoflagellate cysts; Pithonelloideae; Boreal Realm; epicontinental seas	ATLANTIC-OCEAN; PARIS BASIN; LIFE-CYCLE; PALEOCEANOGRAPHY; PRODUCTIVITY; CHALK; STRATIGRAPHY; BIOGEOGRAPHY; CIRCULATION; CARBONATES	A transect from the bathyal to proximal shelf facies of the Boreal Realm was investigated to compare spatial and temporal distribution changes of calcareous dinoflagellate cysts (c-dinocysts) throughout the mid-Cenomanian in order to gain information on the ecology of these organisms. Pithonelloideae dominated the cyst assemblages to more than 95% on the shelf, a prevalence that can be observed throughout most of the Upper Cretaceous. The affinity of this group with the dinoflagellates, which is still controversially discussed, can be confirmed, based on evidence from morphological features and distribution patterns. The consistent prevalence of Pithonella sphaerica and P. ovalis in c-dinocyst assemblages throughout the Upper Cretaceous indicates that they were produced more frequently than cysts of the other species and might, therefore, represent a vegetative dinoflagellate life stage. P. sphaerica and P. ovalis are interpreted as eutrophic species. P. sphaerica is the main species in a marginal-shelf upwelling area, offshore Fennoscandia. Here, sedimentary cyclicity appears to have been reduced to the strongest light/dark changes, while in the outer shelf sediments, light/dark cycles are well-developed and show pronounced temporal assemblage changes. Cyclic fluctuations in the P. sphaerica/P. ovalis ratio reflect shifts of the preferred facies zones and indicate changes in surface mixing patterns. During periods of enhanced surface mixing most parts of the shelf were well-ventilated, and nutrient-enriched surface waters led to high productivity and dominance of the Pithonelloideae. These conditions on the shelf contrasted with those in the open ocean, where more oligotrophic and probably stratified waters prevailed, and an assemblage with very few Pithonelloideae and dominance of Cubodinellum renei and Orthopithonella? gustafsonii was characteristic. While orbitally-forced light/dark sedimentary cyclicity of the shelf sections was mainly related to surface-water carbonate productivity changes, no cyclic modulation of productivity was observed in the oceanic profile. Therefore, dark layer formation in the open ocean was predominantly controlled by the cyclic establishment of anoxic bottom water conditions. Orbitally-forced interruptions in mixing on the shelf resulted in cyclic periods of stratification and oligotrophy in the surface waters, an expansion of oceanic species to the outer shelf, and a shelfward shift of pithonelloid-facies zones, which were probably related to shelfward directed oceanic ingressions. (C) 2002 Elsevier Science Ltd. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Wendler, J (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.							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Res.	APR	2002	23	2					213	229		10.1006/cres.2002.0311	http://dx.doi.org/10.1006/cres.2002.0311			17	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	599LF					2025-03-11	WOS:000178335500004
J	Le Hérissé, A				Le Hérissé, A			Paleoecology, biostratigraphy and biogeography of late Silurian to early Devonian acritarchs and prasinophycean phycomata in well A161, Western Libya, North Africa	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						Siluro/Devonian; acritarchs; prasinophytes; biostratigraphy; paleoceanography; biogeography	DINOFLAGELLATE CYSTS; OCEANIC EPISODES; ORDOVICIAN; CHITINOZOA; MIDDLE; BASIN; BOUNDARY; WENLOCK; LUDLOW; MICROPHYTOPLANKTON	Diverse and well preserved acritarch and prasinophycean phycomata assemblages were recovered from the late Silurian to Lower Devonian strata of well A 161 in western Libya, and four distinct acritarch biozones are recognized, based on the stratigraphic distribution of 156 species. The palynoflora is independently dated by means of chitinozoans, and allows discussion of the evolution of acritarchs and prasinophyte phycomata across the Ludlow-Pridoli boundary in relation to probable major climatic change, as well as in the early and middle Pridoli, and the lower Lochkovian. Correlations are proposed with the British Isles, Baltica, and Algerian Sahara. Sedimentation occurred in shallow high-energy conditions throughout, but with periodic rise of sea level. The changes in marine to terrestrial palynomorph ratios through the section document the relationship between marine palynomorph assemblages and sea surface conditions in these marginal marine environments. The major drift of Gondwana towards low latitudes during the Ludlow-Pridoli transition seems to have been the driving force behind homogenization of assemblages on the two sides of the Rheic ocean, and explains the similarities between phytoplanktonic assemblages of the north Gondwanan margin and the South of Baltica. The data suggest that the Rheic ocean was almost closed by the late Silurian, and had become restricted to a moderately deep sea. In the Lochkovian the microflora are strongly facies-dependent and delineate more restricted provinces such as the Ibarmaghian domain in the sense of Plusquellec (1987) including the Maghreb and Ibero-Armorican areas. Nine new species are described: Arkonia nova, Arkonia paulumstriata, ?Cymatiosphaera florida, Cymatiosphaera nimia, Dactylofusa hispidusa, Disparifusa quasibernesgae, Evittia areolata, Multiplicisphaeridium verticisum, and ?Villosacapsula steemansii. In addition, three new combinations are suggested: Visbysphaera bonita (Cramer) comb. nov., Visbysphaera jardinei (Cramer) comb. nov. and Visbysphaera albanega (Cramer et al.) comb. nov. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bretagne Occidentale, CNRS, UMR 6538, F-29285 Brest, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale		alain.le.herisse@univ-brest.fr						ALAMERI TK, 1983, PALAEOGEOGR PALAEOCL, V44, P103, DOI 10.1016/0031-0182(83)90007-X; ALAMERI TK, 1980, THESIS U LONDON LOND; [Anonymous], SERIE CORRELACION GE; [Anonymous], 1998, PALAEONTOLOGY; Bellini E., 1980, GEOLOGY LIBYA, P3; BERRY WBN, 1973, 147 GEOL SOC AM; Boumendjel K., 1987, PhD Thesis; Brocke Rainer, 1996, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V200, P53; BUREET MB, 1990, THESIS U P M CURIE P; BURET MB, 1986, CR ACAD SCI II, V302, P1009; Caron M, 1999, B SOC GEOL FR, V170, P145; Chauvel J.J., 1981, NOTES MEM COMP FR PE, V16, P25; COLBATH G K, 1980, Micropaleontology (New York), V26, P97, DOI 10.2307/1485278; COLBATH GK, 1983, PHYCOLOGIA, V22, P249, DOI 10.2216/i0031-8884-22-3-249.1; COMBAZ A., 1964, REV MICROPALDONTOL, V7, P205; Cramer F.H., 1976, Palaeontographica Abteilung B Palaeophytologie, V158, P72; CRAMER F H, 1976, Revista Espanola de Micropaleontologia, V8, P439; Cramer FH., 1974, Palaeontographica. 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Palaeobot. Palynology	APR	2002	118	1-4			SI		359	395	PII S0034-6667(01)00123-3	10.1016/S0034-6667(01)00123-3	http://dx.doi.org/10.1016/S0034-6667(01)00123-3			37	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	577KE					2025-03-11	WOS:000177059400020
J	Peshin, SS; Lall, SB; Gupta, SK				Peshin, SS; Lall, SB; Gupta, SK			Potential food contaminants and associated health risks	ACTA PHARMACOLOGICA SINICA			English	Review						food contamination; organophosphorus compounds; oils; aromatic hydrocarbons; heavy ions; microbiology; fungi	DRINKING-WATER; POLYCHLORINATED-BIPHENYLS; EDIBLE MUSHROOMS; ALUMINUM CONTENT; FRUITING BODIES; EPIDEMIC DROPSY; HEAVY-METALS; OCHRATOXIN-A; EXPOSURE; MERCURY	The potential toxicants in food are derived from natural or industrial sources. Compounds like lectins and glycoalkaloids that are toxic to man are naturally present in some vegetables like potatoes or legumes. A wide variety of marine toxins mostly produced by dinoflagellates occuring secondarily in molluscs and mussels are usually ingested by human beings causing poisoning. On the other hand, toxic compounds find their way into food during manufacture, storage, or transportation. These include largely the industrial contaminants, persistent organic pollutants (POP), pesticides, heavy metals, and toxins of fungal and bacterial origin. Further, toxic compounds like higher alcohols may be produced as byproducts during processing. Migration of compounds from packaging materials into packaged food like contamination with lead from solder in certain metal cans is well known. Additives (emulsifiers, preservatives, and antioxidants) could also influence the quality of foods. Solvent residues may find their way into food as a result of their use in extraction processes like the use of trichloroethylene and methylene chloride in decaffeination of coffee. In addition, poor hygiene, storage, and preparation may also lead to food contamination by various microbes and ova or cysts of nematodes. The problem of food contamination can be overcome to a great extent by regular surveillance and monitoring programmes and strict implementation of food and adulteration act. In the present review some of these aspects of food contamination have been discussed in detail.	All India Inst Med Sci, Dept Pharmacol, Natl Poisons Informat Ctr, New Delhi 110029, India	All India Institute of Medical Sciences (AIIMS) New Delhi	All India Inst Med Sci, Dept Pharmacol, Natl Poisons Informat Ctr, New Delhi 110029, India.	skgup@hotmail.com						ABE T, 1995, ARCH ENVIRON HEALTH, V50, P367, DOI 10.1080/00039896.1995.9935969; Ahmed MT, 2000, J HAZARD MATER, V80, P1, DOI 10.1016/S0304-3894(00)00300-9; Alaluusua S, 1996, EUR J ORAL SCI, V104, P493, DOI 10.1111/j.1600-0722.1996.tb00131.x; ARIM RH, 1995, FOOD ADDIT CONTAM, V12, P291, DOI 10.1080/02652039509374306; ARMON SS, 1989, ANAEROBIC INFECT HUM, P601; ASKEW GL, 1994, PEDIATRICS, V94, P381; Assimon SA, 1997, FOOD ADDIT CONTAM A, V14, P483; BAKIR F, 1980, POSTGRAD MED J, V56, P1, DOI 10.1136/pgmj.56.651.1; BAKIR F, 1973, SCIENCE, V181, P230, DOI 10.1126/science.181.4096.230; Bennett GA, 1996, ADV EXP MED BIOL, V392, P317; Boros LG, 1998, LEUKEMIA RES, V22, P849, DOI 10.1016/S0145-2126(98)00052-6; BORRIELLO SP, 1984, LANCET, V1, P305; BRADBERRY SM, 1994, J TOXICOL-CLIN TOXIC, V32, P173, DOI 10.3109/15563659409000447; Braune B, 1999, SCI TOTAL ENVIRON, V230, P145, DOI 10.1016/S0048-9697(99)00038-8; BROKONS JA, 1995, ENV HLTH PERSPECT, V103, P608; Buchet JP, 1996, ARCH TOXICOL, V70, P773, DOI 10.1007/s002040050339; BUCHET JP, 1994, ENVIRON RES, V66, P44, DOI 10.1006/enrs.1994.1043; CASTLE L, 1994, FOOD ADDIT CONTAM, V11, P79, DOI 10.1080/02652039409374204; CHAN CF, 1990, LINEAR MULTILINEAR A, V27, P189; Chao WY, 1997, ARCH ENVIRON HEALTH, V52, P257, DOI 10.1080/00039899709602195; Chaudhry R, 1998, BMJ-BRIT MED J, V317, P268, DOI 10.1136/bmj.317.7153.268; COLBORN T, 1993, ENVIRON HEALTH PERSP, V101, P378, DOI 10.2307/3431890; Craig PH, 1999, J TOXICOL ENV HEAL B, V2, P281, DOI 10.1080/109374099281142; CZEIZEL AE, 1993, LANCET, V341, P539, DOI 10.1016/0140-6736(93)90293-P; Dan G., 1998, Indian Journal of Pharmacology, V30, P129; Das M, 1997, CRIT REV TOXICOL, V27, P273, DOI 10.3109/10408449709089896; DAVIS LE, 1994, ANN NEUROL, V35, P680, DOI 10.1002/ana.410350608; delaPaz MP, 1996, FOOD CHEM TOXICOL, V34, P251, DOI 10.1016/0278-6915(95)00111-5; Delcourt A, 1994, Boll Chim Farm, V133, P235; deMejia EG, 1996, ARCH ENVIRON CON TOX, V31, P581, DOI [10.1007/BF00212443, 10.1007/s002449900147]; deOliveira CAF, 1997, REV SAUDE PUBL, V31, P417, DOI 10.1590/S0034-89101997000400011; DHAVAN AS, 1995, J AOAC INT, V78, P693; DONG HQ, 1993, CHANG HUA NEI KO TSA, V32, P813; Dudka S, 1999, J ENVIRON SCI HEAL B, V34, P681, DOI 10.1080/03601239909373221; Dunnick J., 1988, HDB TOXICITY INORGAN, P55; EASTWOOD JB, 1990, LANCET, V336, P462, DOI 10.1016/0140-6736(90)92012-7; FEINGLASS EJ, 1973, NEW ENGL J MED, V288, P828, DOI 10.1056/NEJM197304192881608; Fillastre JP, 1997, B ACAD NAT MED PARIS, V181, P1447; FRANCHI E, 1994, MUTAT RES, V320, P23, DOI 10.1016/0165-1218(94)90056-6; FRIES GF, 1995, J ANIM SCI, V73, P1639; GAST RK, 1990, AVIAN DIS, V34, P991, DOI 10.2307/1591394; GOLDFRANK LR, 1994, GOLDFRANKS TOXICOLOG, P921; Greenaway Christina, 1996, Journal of Emergency Medicine, V14, P339, DOI 10.1016/0736-4679(96)00045-5; Guillen M. 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Sin.	MAR	2002	23	3					193	202						10	Chemistry, Multidisciplinary; Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Chemistry; Pharmacology & Pharmacy	528BH	11918841				2025-03-11	WOS:000174223200001
J	Moorlock, BSP; Riding, JB; Hamblin, RJO; Allen, P; Rose, J				Moorlock, BSP; Riding, JB; Hamblin, RJO; Allen, P; Rose, J			The Pleistocene College Farm Silty Clay at Great Blakenham, Suffolk, England - additional information on the course of the early River Thames	GEOLOGIE EN MIJNBOUW-NETHERLANDS JOURNAL OF GEOSCIENCES			English	Article						England; Suffolk; Pleistocene; Crag; Thames	NORWICH CRAG FORMATIONS; RED CRAG; PALYNOMORPHS; NORFOLK; LITHOSTRATIGRAPHY; PALEOGEOGRAPHY; SEDIMENTS; DEPOSITS; BOREHOLE; GRAVELS	The Pleistocene College Farm Silty Clay Member of the Creeting Formation at Great Blakenham, Suffolk, south-east England is shown to contain indigenous and recycled dinoflagellate cysts and other derived palynomorphs. The indigenous dinoflagellate cysts indicate a marine influence during deposition of the clay, whilst the other palynomorphs demonstrate derivation of sediment from a wide catchment of Carboniferous, Jurassic and Cretaceous bedrocks. It is argued, by comparison with palynological data from the Chillesford Clay Member of the Norwich Crag Formation some 25km to the east, that these sediments were eroded from western, south-central and south-eastern Britain, and transported by the early River Thames to its estuary, where they were redeposited at the western margin of the Crag Basin, during the Early Pleistocene Tiglian TC3 Substage. This interpretation refines earlier research which concluded the College Farm Silty Clay was deposited in a predominantly freshwater environment, such as a lagoon, without any direct access to the sea or major river.	British Geol Survey, Keyworth NG12 5GG, Notts, England; Univ London, Dept Geog, Egham TW20 0EX, Surrey, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of London; Royal Holloway University London	British Geol Survey, Keyworth NG12 5GG, Notts, England.	bspm@bgs.ac.uk	Rose, Jim/H-8944-2019					ALLEN P, 1983, THESIS U LONDON; ALLEN P, 1984, FIELD GUIDE GIPPING; [Anonymous], B GEOLOGICAL SOC NOR; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; Costa L. I., 1992, BRIT MICROPALAEONTOL, P99; DEJONG J, 1988, PHILOS T ROY SOC B, V318, P603, DOI 10.1098/rstb.1988.0025; Farr K.M., 1989, Northwest European micropalaeontology and palynology, P265; FIELD MH, 1992, GEOL MAG, V129, P363, DOI 10.1017/S0016756800019300; Funnell BM, 1996, QUATERNARY SCI REV, V15, P391, DOI 10.1016/0277-3791(96)00022-4; Gibbard PL, 1996, QUATERNARY SCI REV, V15, P413, DOI 10.1016/0277-3791(96)00013-3; GIBBARD PL, 1991, QUATERNARY SCI REV, V10, P23, DOI 10.1016/0277-3791(91)90029-T; Gibbard PL, 1998, MEDEDELINGEN NEDERLA, V60, P239; Gradstein FM, 1996, EPISODES, V19, P3, DOI 10.18814/epiiugs/1996/v19i1.2/002; Hamblin RJO, 1997, P GEOLOGIST ASSOC, V108, P11, DOI 10.1016/S0016-7878(97)80002-8; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Harland R., 1992, P253; 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, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; HEY RW, 1977, GEOL MAG, V114, P219, DOI 10.1017/S0016756800044800; Komar P.D., 1976, BEACH PROCESSES SEDI; MARKHAM RAD, 1972, T SUFFOLK NATURALIST, V15, P520; Riding J.B., 1992, P7; RIDING J B, 1988, Palynology, V12, P65; Riding JB, 1997, SCOT J GEOL, V33, P59, DOI 10.1144/sjg33010059; Riding JB, 1997, P GEOLOGIST ASSOC, V108, P25, DOI 10.1016/S0016-7878(97)80003-X; Riding JB, 2000, P GEOLOGIST ASSOC, V111, P161, DOI 10.1016/S0016-7878(00)80006-1; ROSE J, 1976, NATURE, V263, P492, DOI 10.1038/263492a0; Rose J, 2002, P GEOLOGIST ASSOC, V113, P47, DOI 10.1016/S0016-7878(02)80006-2; Rose J, 2001, QUATERN INT, V79, P5, DOI 10.1016/S1040-6182(00)00119-1; Rose J, 1999, P GEOLOGIST ASSOC, V110, P93, DOI 10.1016/S0016-7878(99)80063-7; Rose J., 1977, J GEOLOGICAL SOC, V133, P83, DOI DOI 10.1144/GSJGS.133.1.0083; ROSE J, 2000, QUATERNARY NORFOLK S, P35; Suc JP, 1997, QUATERN INT, V40, P37, DOI 10.1016/S1040-6182(96)00059-6; WEST R.G., 1980, PREGLACIAL PLEISTOCE; WHITEMAN CA, 1992, QUATERNARY SCI REV, V11, P363, DOI 10.1016/0277-3791(92)90007-U; ZALASIEWICZ JA, 1991, PHILOS T R SOC B, V333, P81, DOI 10.1098/rstb.1991.0061; ZALASIEWICZ JA, 1985, GEOL MAG, V122, P287, DOI 10.1017/S0016756800031502	39	7	7	0	0	VEENMAN DRUKKERS	EDE	P O BOX 18, 6710 BA EDE, NETHERLANDS	0016-7746			GEOL MIJNBOUW-N J G	Geol. Mijnb.-Neth. J. Geosci.	MAR	2002	81	1					9	17						9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	572GU					2025-03-11	WOS:000176766400002
J	Giangrande, A; Montresor, M; Cavallo, A; Licciano, M				Giangrande, A; Montresor, M; Cavallo, A; Licciano, M			Influence of <i>Naineris laevigata</i> (Polychaeta: Orbiniidae) on vertical grain size distribution, and dinoflagellate resting stages in the sediment	JOURNAL OF SEA RESEARCH			English	Article						bioturbation; vertical sediment distribution; resting stages; Polychaeta; Mediterranean Sea	NORTHERN BALTIC-SEA; DUTCH WADDEN SEA; COMMUNITY STRUCTURE; MONOPOREIA-AFFINIS; MARINE-SEDIMENTS; COPEPOD NAUPLII; BIOTURBATION; SCRIPPSIELLA; REWORKING; CYSTS	Short-term experiments were performed with the polychaete Naineris laevigata Grube. a conveyor-belt deposit feeder, to evaluate: the daily sediment reworking rate, the influence of the activity of this burrowing worm on the vertical redistribution of the sediment and dinoflagellate cysts. We also tested the germination success of cysts after their passage through the g-ut of the polychaete. Vertical particle distribution was studied in small aquaria with and without worms and with an initially layered sediment. After 30 days, sediment cores were collected in controls and treatments at 3 different depths (upper, intermediate and deep) and the diameter of 100 particles from each depth was measured to obtain the size-frequency distribution. The burrowing activity of 3 worms may completely mix a pre-existent layering within 30 days. The translocation of a mud layer from 4 cm. depth towards the surface was observed. The mud layer deposited on the surface by the end of the experiment was at least 1 cm thick. Daily average production of faecal pellets was 0.443+/-0.032 g per worm. From the first day of the experiment, the particle size distribution of the faecal pellets released at the surface revealed the presence of sediment and cysts originating from underlying layers. Tests showed that the germination percentage of the cysts significantly diminished after passage through the guts of the worms. Our results indicate that N. laevigata is an effective vertical mixer of sediment and plays a role in the vertical transport and germination success of resting stages. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Lecce, Dipartimento Biol, Stn Biol Marina, I-73100 Lecce, Italy; Staz Zool Anton Dohrn, I-80121 Naples, Italy	University of Salento; Stazione Zoologica Anton Dohrn	Univ Lecce, Dipartimento Biol, Stn Biol Marina, I-73100 Lecce, Italy.	gianadri@ilenic.unile.it	Licciano, Margherita/L-2242-2019	Giangrande, Adriana/0000-0003-4531-2377; Montresor, Marina/0000-0002-2475-1787				Albertsson J, 2000, MAR BIOL, V136, P611, DOI 10.1007/s002270050721; Albertsson J, 2001, MAR BIOL, V138, P793, DOI 10.1007/s002270000498; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; BELMONTE G, 1996, BIOL ECOLOGY SHALLOW, P53; BINDER BJ, 1987, J PHYCOL, V23, P99; Blanchard GF, 1997, MAR ECOL PROG SER, V151, P17, DOI 10.3354/meps151017; BRAY J. ROGER, 1957, ECOL MONOGR, V27, P325, DOI 10.2307/1942268; BRENCHLEY GA, 1981, J MAR RES, V39, P767; Cáceres CE, 1998, ERGEB LIMNOL, V52, P163; Cadee G. 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Sea Res.	MAR	2002	47	2					97	108	PII S1385-1101(01)00103-4	10.1016/S1385-1101(01)00103-4	http://dx.doi.org/10.1016/S1385-1101(01)00103-4			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	554FU					2025-03-11	WOS:000175725100002
J	Galeotti, S; Coccioni, R				Galeotti, S; Coccioni, R			Changes in coiling direction of <i>Cibicidoides pseudoacutus</i> (Nakkady) across the Cretaceous-Tertiary boundary of Tunisia:: palaeoecological and biostratigraphic implications	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	International Workshop on Cretaceous-Paleogene Transition in Tunisia	MAY, 1998	TUNIS, TUNISIA			benthic foraminifera; coiling ratio; biostratigraphy; palaeoecology; Cretaceous-Tertiary boundary; Tunisia	EL-KEF; PLANKTIC FORAMINIFERA; BENTHIC FORAMINIFERA; STABLE ISOTOPE; EXTINCTION; EVENTS; MODEL	The analysis of coiling direction preference in the benthic foraminifera Cibicidoides pseudoacutus (Nakkady) has been carried out across the Cretaceous-Tertiary boundary (K-T boundary) from four Tunisian sections representing a palacobathymetric transect from a middle-outer neritic to lower upper bathyal depositional setting. Our study reveals that C. pseudoceutus developed a preference for sinistral coiling in a short time period during the lowermost Danian. The comparison of the coiling ratio (number of sinistral vs. dextral individuals) record with isotope data and dinoflagellate cyst assemblage distribution suggests that the development of sinistrally coiled populations of Cibicidoides pseudoacutus might be related to a short-term cooling of both surface and bottom waters which occurred at the K T boundary and lasted for some 7 kyr. The continuous occurrence and the high abundance of Cibicidoides pseudoacutus through the K T boundary in neritic to upper bathyal depositional environments around southern Tethys make identification of the shift in its coiling ratio relatively easy. The development of a sinistrally coiled population in this benthic foraminiferal species is regarded as a potential marker for the base of planktonic foraminiferal Zone PO in Tethyan shallow water settings. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Urbino, Ist Geol, I-61029 Urbino, Italy; Univ Urbino, Ctr Palinol, I-61029 Urbino, Italy	University of Urbino; University of Urbino	Galeotti, S (通讯作者)，Univ Urbino, Ist Geol, Campus Sci,Localita Crocicchia, I-61029 Urbino, Italy.	s.galeotti@uniurb.it		Galeotti, Simone/0000-0001-9636-9344; COCCIONI, Rodolfo/0000-0003-2333-4030				Adatte T., 1998, International Workshop on Cretaceous-Tertiary Transition, Office National des Mines, Direction du Service Geologique, P7; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BOLTOVSKOY E, 1991, J PALEONTOL, V65, P175, DOI 10.1017/S0022336000020394; 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; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; Brummer G.-J. 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J	Luciani, V				Luciani, V			High-resolution planktonic foraminiferal analysis from the Cretaceous-Tertiary boundary at Ain Settara (Tunisia): evidence of an extended mass extinction	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	International Workshop on Cretaceous-Paleogene Transition in Tunisia	MAY, 1998	TUNIS, TUNISIA			Cretaceous-Tertiary boundary; hiatus; mass extinction; biostratigraphy; planktonic foraminifera; central-northern Tunisia	EL-KEF; CALCAREOUS NANNOFOSSIL; ENVIRONMENTAL-CHANGES; STABLE-ISOTOPE; SPECIES SURVIVORSHIP; DINOFLAGELLATE CYSTS; NORTHEASTERN MEXICO; CHANNEL DEPOSITS; CHICXULUB CRATER; IMPACT	The Ain Settara section, located in the Kalaat-Senan area of north-central Tunisia. spans the Cretaceous-Tertiary (K T) boundary which is characterized by a red layer and a thin non-bioturbated boundary clay. Sediment accumulation across the K T boundary at Ain Settara was probably interrupted by three short hiatuses and/or condensed sedimentation. The first hiatus occurs at the top of the CF1 Zone the second hiatus/condensation occurred just below the boundary clay and the third hiatus at the P0/P1a boundary, in the earliest Danian. These hiatuses are marked by weak unconformities, bioturbation and sudden disappearances/appearances of species which are known to disappear/evolve sequentially in continuous sections. Quantitative high-resolution plank-tonic foraminiferal analysis across zones CF1(upper), P0 and P1a(1) reveals an extended and selective mass extinction. All 41% of the species which disappeared at or below the K-T boundary are rare to very rare and primarily ecologically specialized keeled deeper-dwelling tropical-subtropical forms (Globotruncana, Globotruncanita, Gublerina, Planoglobulina, Rosita (Contusotruncana), Racemiguembelina). Their combined relative abundance varies between 10% and 15% of the total population at the end of the Maastrichtian. The K-T crisis thus appears more catastrophic when viewed in tropical Subtropical assemblages and based on analysis of larger species (>200 mum) which preferentially includes the more specialized forms, though, in fact, the K T mass extinction actually involved a relatively small part of the foraminiferal population in terms of relative abundance. The pattern of extinction and changes in dominant population at Ain Settara appear to be very similar to the planktonic foraminiferal turnover of the other north-central Tunisian sections (El Kef, Elles). The selective mass extinction pattern suggests that the catastrophic effects of the bolide impact superimposed those related to long-term environmental changes, such as variations in temperature, sea-level and associated water-mass changes. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Ferrara, Dipartimento Sci Terra, I-4410 Ferrara, Italy	University of Ferrara	Univ Ferrara, Dipartimento Sci Terra, Corso Ercole I Este 32, I-4410 Ferrara, Italy.	lev@unife.it	Luciani, Valeria/K-8572-2015					Abramovich S, 1998, GEOLOGY, V26, P63, DOI 10.1130/0091-7613(1998)026<0063:DOTMPE>2.3.CO;2; ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; ALVAREZ W, 1992, GEOLOGY, V20, P697, DOI 10.1130/0091-7613(1992)020<0697:PIDATC>2.3.CO;2; [Anonymous], SPECIAL PUBLICATION; Arenillas I, 2000, J FORAMIN RES, V30, P202, DOI 10.2113/0300202; Arz J.A., 1999, Revista Espanola de Micropaleontologia, V31, P297; BARRERA E, 1994, GEOLOGY, V22, P877, DOI 10.1130/0091-7613(1994)022<0877:GECPTC>2.3.CO;2; Barrera E, 1990, PALEOCEANOGRAPHY, V5, P867, DOI 10.1029/PA005i006p00867; BENABDELKADER OB, 1992, INT WORKSH CRETACE 1, P9; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BOURGEOIS J, 1988, SCIENCE, V241, P567, DOI 10.1126/science.241.4865.567; 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Paleoclimatol. Paleoecol.	FEB 28	2002	178	3-4					299	319	PII S0031-0182(01)00400-X	10.1016/S0031-0182(01)00400-X	http://dx.doi.org/10.1016/S0031-0182(01)00400-X			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology; Paleontology	558CX					2025-03-11	WOS:000175949500009
J	Itakura, S; Yamaguchi, M; Yoshida, M; Fukuyo, Y				Itakura, S; Yamaguchi, M; Yoshida, M; Fukuyo, Y			The seasonal occurrence of <i>Alexandrium tamarense</i> (Dinophyceae) vegetative cells in Hiroshima Bay, Japan	FISHERIES SCIENCE			English	Article						Alexandrium tamarense; bloom; environmental condition; Hiroshima Bay; population dynamics; seasonal occurrence; vegetative cells	GONYAULAX-TAMARENSIS; INLAND-SEA; CYSTS; PROTOGONYAULAX; TOXIFICATION; ASSOCIATION; GERMINATION; PREFECTURE; CATENELLA; EXCAVATA	The seasonal bloom of the toxic dinoflagellate Alexandrium tamarense, with reference to the ambient oceanographic conditions in Hiroshima Bay, Seto Inland Sea, Japan is described. Long-term observations on the vegetative cells of A. tamarense were conducted biweekly to monthly at one fixed station in northern Hiroshima Bay, where recurrent paralytic shellfish poisoning (PSP) incidents have been occurring since 1992. Over the 5-year study period, from April 1994 to December 1998, vegetative cells of A. tamarense were detected each year within the period from January to June. Observed annual maximum cell densities of A. tamarense reached 10(3)-10(4) cells/L, and mostly peaked at a depth layer of 5 m at the sampling station in April or May. Oceanographic conditions during the bloom period were as follows: water temperatures ranged from 10.2degreesC to 20.2degreesC, and thermal stratification gradually developed around April. Inorganic nutrient concentrations were markedly low throughout the bloom period. Particularly, the annual lowermost concentration Of SiO(2)- Si was observed each year during this period. These environmental features indicate that the occurrence of vegetative cells of A. tamarense seems to be explained by temperature and nutrient conditions and that the A. tamarense bloom developed subsequently to or concomitantly with the diatom spring bloom.	Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Harmful Phytoplankton Sect, Hiroshima 7390452, Japan; Nagasaki Univ, Fac Fisheries, Nagasaki 8528521, Japan; Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, Tokyo 1138657, Japan	Japan Fisheries Research & Education Agency (FRA); Nagasaki University; University of Tokyo	Itakura, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Harmful Phytoplankton Sect, Ohno, Hiroshima 7390452, Japan.	itakura@affrc.go.jp						ACHIHA H, 1990, Japanese Journal of Phycology, V38, P51; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; 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; ASAKAWA M, 1995, TOXICON, V33, P691, DOI 10.1016/0041-0101(94)00177-A; ASAKAWA M, 1993, J FOOD HYG SOC JPN, V34, P50, DOI 10.3358/shokueishi.34.50; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P611; 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, 1982, THESIS U TOKYO TOKYO; Itakura S, 2001, PHYCOLOGIA, V40, P263, DOI 10.2216/i0031-8884-40-3-263.1; Itakura S., 1990, B NANSEI NATL FISH R, V23, P27; Kotani Yuichi, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P104; LABARBERASANCHE.A, 1993, TOXIC PHYTOPLANKTON, P763; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; Nagai S., 1996, HARMFUL TOXIC ALGAL, P239; OGATA T, 1982, B JPN SOC SCI FISH, V48, P563; SEKIGUCHI K, 1985, B TOHOKU REG FISH R, V48, P115; Strickland J.D.H., 1972, FISHERIES RES BOARD, V2nd; SU HM, 1993, DEV MAR BIO, V3, P837; UCHIDA T, 1980, Japanese Journal of Phycology, V28, P133; WHITE AW, 1976, J FISH RES BOARD CAN, V33, P2598, DOI 10.1139/f76-306; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; YAMAMOTO M, 1996, HARMFUL TOXIC ALGAL, P19; Yamamoto T., 1995, Japanese Journal of Phycology, V43, P91; Yamamoto Tamiji, 1997, Japanese Journal of Phycology, V45, P95; YUASA I, 1990, FISH OCEANOGR, V54, P129	28	20	30	1	11	SPRINGER TOKYO	TOKYO	1-11-11 KUDAN-KITA, CHIYODA-KU, TOKYO, 102-0073, JAPAN	0919-9268			FISHERIES SCI	Fish. Sci.	FEB	2002	68	1					77	86		10.1046/j.1444-2906.2002.00392.x	http://dx.doi.org/10.1046/j.1444-2906.2002.00392.x			10	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	528KZ		Bronze			2025-03-11	WOS:000174244100011
J	Holmes, MJ; Bolch, CJS; Green, DH; Cembella, AD; Teo, SLM				Holmes, MJ; Bolch, CJS; Green, DH; Cembella, AD; Teo, SLM			Singapore isolates of the dinoflagellate <i>Gymnodinium catenatum</i> (dinophyceae) produce a unique profile of paralytic shellfish poisoning toxins	JOURNAL OF PHYCOLOGY			English	Article						ballast water; dinoflagellate; Gymnodinium catenatum; mass spectrometry; paralytic shellfish poisoning; rDNA; ribosomal RNA gene; toxin	SHIPS BALLAST WATER; ALEXANDRIUM DINOPHYCEAE; MICRORETICULATE CYST; SPECIES COMPLEX; ULTRASTRUCTURE; TAMARENSE; SEQUENCES; TRANSPORT; STRAINS; GROWTH	We investigated the cell morphology, toxicity and toxin composition, and rDNA sequences of clonal cultures of the chain-forming dinoflagellate Gymndinium catenatum H.W.Graham isolated from the port of Singapore. The cell morphology was consistent with most descriptions of this species except for sparsely distributed putative trichocyst pores visible on some cells under SEM. Nucleotide sequences (697 base pair) of the D1-D2 conserved regions and intervening variable domain of the large subunit rDNA were identical among isolates from Singapore and those of all other global populations examined so far (from Australia, China, Japan, Korea, New Zealand, Spain, and Uruguay), and this is consistent with the morphological conservatism of the species. Among isolates of G. catenatum that produce toxins associated with paralytic shellfish poisoning, the cellular toxicity of Singapore clones, as determined by intraperitoneal mouse bioassay (30-50 pg saxitoxin equivalents-cell(-1)) and immunoassay (24 +/- 8 saxitoxin equivalents-cell(-1)) was relatively high. The mouse bioassay toxicity was comparable with that of Spanish and Philippine isolates that have undergone acid hydrolysis. However, analysis of toxin composition of Singapore clones by HPLC with fluorescence detection or HPLC-mass spectrometry/mass spectrometry revealed a unique toxin profile that was dominated by the highly potent carbamate toxins, primarily gonyautoxin (GTX) I and 4 with lesser amounts of GTX2, GTX3, neosaxitoxin, and saxitoxin. No N-sulfocarbamoyl, decarbamoyl, or deoxy-decarbamoyl toxins were detected. In contrast, less potent N-sulfocarbamoyl toxins dominate the toxin profiles of all other global populations examined to date (from Australia, China, Japan, New Zealand, the Philippines, Portugal, Spain, and Uruguay). The lack of genetic diversity found among broadly distributed populations of G. catenatum is consistent with the hypothesis of a relatively recent global spread of this species. Yet the unique toxin profile of Singapore strains indicates that it is unlikely that this strain has been recently translocated from any of the populations with characterized toxin profiles. In any case, the unique carbamate-dominated toxin profile may be a useful signature to identify the potential spread of this strain from the port of Singapore, one of the world's busiest.	Dunstaffnage Marine Res Lab, Scottish Assoc Marine Sci, Oban PA34 4AD, Argyll, Scotland; Natl Res Council Canada, Inst Marine Biosci, Halifax, NS B3H 3Z1, Canada; Natl Univ Singapore, Trop Marine Sci Inst, Singapore 119260, Singapore	University of the Highlands & Islands; International Business Machines (IBM); IBM Canada; National Research Council Canada; National University of Singapore	Natl Univ Singapore, Dept Biol Sci, Singapore 119260, Singapore.	dbshmj@nus.edu.sg	Bolch, Christopher/J-7619-2014; Green, David/E-2533-2012	TEO, SERENA LAY MING/0000-0002-3309-4715; Green, David/0000-0001-7499-6021				Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1989, TOXICON, V27, P665, DOI 10.1016/0041-0101(89)90017-2; *AOAC, 1980, OFF METH AN, P298; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; 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; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; BRAVO I, 1986, Investigacion Pesquera (Barcelona), V50, P313; 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; CHUAH AL, 1998, THESIS NATL U SINGAP; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; FLYNN K, 1994, MAR ECOL PROG SER, V111, P99, DOI 10.3354/meps111099; FUKUYO Y, 1993, DEV MAR BIO, V3, P875; Gin KYH, 2000, J PLANKTON RES, V22, P1465, DOI 10.1093/plankt/22.8.1465; HALL S, 1984, ACS SYM SER, V262, P113; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; 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; HOLMES MJ, 1991, TOXICON, V29, P761, DOI 10.1016/0041-0101(91)90068-3; MACKENZIE L, 2001, GYMNODINIUM CATENATU; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; Mendez S.M., 2001, HARMFUL ALGAL BLOOMS, P352; MOREYGAINES G, 1982, PHYCOLOGIA, V21, P154, DOI 10.2216/i0031-8884-21-2-154.1; Negri A P., 2001, Harmful Algal Blooms 2000, P210; OSHIMA Y, 1993, MAR BIOL, V116, P471, DOI 10.1007/BF00350064; Oshima Y., 1995, MANUAL HARMFUL MARIN, P81; Parkhill JP, 1999, J PLANKTON RES, V21, P939, DOI 10.1093/plankt/21.5.939; Quilliam MA., 2001, Mycotoxins and Phycotoxins in Perspective at the Turn of the Century, P383; REES AJJ, 1991, PHYCOLOGIA, V30, P90, DOI 10.2216/i0031-8884-30-1-90.1; REGUERA B, 1990, TOXIC MARINE PHYTOPLANKTON, P316; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SIDABUTAR T, 1999, ASEAN MARINE ENV MAN, P438; TAN CTT, 1987, PROGR VENOM TOXIN RE, P429; TAYLOR FJR, 1995, UNESCO IOC MANUAL GU, V33, P283; USUP G, 1998, PHYSL ECOLOGY HARMFU, P81; Walsh D, 1998, BIOCHEM SYST ECOL, V26, P495, DOI 10.1016/S0305-1978(98)00006-4; YUKI K, 1987, Bulletin of Plankton Society of Japan, V34, P109	41	53	55	0	30	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2002	38	1					96	106		10.1046/j.1529-8817.2002.01153.x	http://dx.doi.org/10.1046/j.1529-8817.2002.01153.x			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	525EJ					2025-03-11	WOS:000174055500008
J	Olli, K; Anderson, DM				Olli, K; Anderson, DM			High encystment success of the dinoflagellate <i>Scrippsiella</i> cf. <i>lachrymosa</i> in culture experiments	JOURNAL OF PHYCOLOGY			English	Article						dinophyceae; encystment; germination; life cycle; resting cysts; Scrippsiella cf. lachrymosa	ALEXANDRIUM-TAMARENSE DINOPHYCEAE; CYST FORMATION; SEXUAL REPRODUCTION; GONYAULAX-TAMARENSIS; LIFE-CYCLE; GYMNODINIUM-CATENATUM; GYRODINIUM-UNCATENUM; TEMPERATURE; GERMINATION; PHOSPHORUS	Close to 100% encystment efficiency and a yield above 105 cysts(.)mL(-1) were routinely achieved in full strength f/2 medium-based batch cultures (883 muM NO3- and 36 muM PO4-3) of the marine dinoflagellate Scrippsiella cf. lachrymosa Lewis. Increases in cell density led to nutrient depletion in this enriched medium, which was the most likely cause for initiation of cyst formation. Lowering the concentration of either nutrient to 1/10 the initial levels decreased the encystment efficiency, whereas use of ammonium as the N source resulted in both low cell yield and low encystment efficiency. The mandatory dormancy period was ca. 60 days and was not affected by cold dark storage of the cysts. Cysts produced in the initial phase of sexual reproduction were relatively large (length 47 mum, width 31 mum) with a heavy calcareous cover. Cysts produced thereafter lacked apparent calcareous cover and were smaller (length 29 mum, width 19 mum). The decrease of cyst volume (by a factor of 0.24-0.4) suggested strong resource limitation during the course of encystment. However, after the mandatory dormancy period, germination success of the smaller cysts was higher (80%), compared with the larger cysts that had been produced initially (50%). Germling survival (74%) was independent of cyst type but was enhanced by higher nutrient concentration during incubation. The ratio, of initial nutrient concentration in the medium to the cyst yield was used as a proxy to estimate the cellular nutrient quota. The conservative estimates of 9 pmol N(.)cyst(-1) and 0.4 pmol P(.)cyst(-1) obtained in this manner are at the low end of the range of previous published estimates for other dinoflagellate cysts. Given the high encystment observed in laboratory experiments, we have no reason to assume an inherently lower encystment success in dinoflagellate field populations. Our results do not challenge the low nutrient paradigm for dinoflagellate sexuality. We believe that the high encystment success and cyst yield of this particular species is at least partly due to its ability to achieve very high cell densities in cultures, which evidently leads to nutrient depletion even in f/2 medium.	Woods Hole Oceanog Inst, Biol Dept, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Woods Hole Oceanog Inst, Biol Dept, MS 32, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Olli, Kalle/G-5389-2010					Agresti A., 1984, ANAL ORDINAL CATEGOR, V1st; Anderson D.M., 1998, PHYSL ECOLOGY HARMFU, P19; 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, 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, 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 CA, 1974, NATURE, V250, P435, DOI 10.1038/250435a0; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BINDER BJ, 1986, THESIS MIT CAMBRIDGE; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; Dale B., 1983, P69; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; EPPLEY R W, 1978, P217; Fryxell G.A., 1983, Survival Strategies of the algae, P1; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; LIRDWITAYAPRASIT T, 1990, J PHYCOL, V26, P299, DOI 10.1111/j.0022-3646.1990.00299.x; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; MOREYGAINES G, 1980, PHYCOLOGIA, V19, P230, DOI 10.2216/i0031-8884-19-3-230.1; MURPHY J, 1962, ANAL CHIM ACTA, V26, P31; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; 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, 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; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; Rengefors K, 1999, EUR J PHYCOL, V34, P171, DOI 10.1017/S0967026299002012; Stosch H.A., 1964, Helgolander Wissenschaftliche Meeresuntersuchungen, V10, P140; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Von Stosch HA., 1973, Br Phycol J, V8, P105; VONSTOSCH HA, 1965, NATURWISSENSCHAFTEN, V52, P311; WALKER LM, 1979, J PHYCOL, V15, P312; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; ZINGMARK RG, 1970, J PHYCOL, V6, P122, DOI 10.1111/j.0022-3646.1970.00122.x	51	60	67	1	13	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	2002	38	1					145	156		10.1046/j.1529-8817.2002.01113.x	http://dx.doi.org/10.1046/j.1529-8817.2002.01113.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	525EJ					2025-03-11	WOS:000174055500013
J	Persson, A				Persson, A			Proliferation of cryptic protists and germination of resting stages from untreated sediment samples with emphasis on dinoflagellates	OPHELIA			English	Article						ciliates; cysts; diatoms; dinoflagellates; Eastern Skagerrak; protists; germination	GLOBAL DIVERSITY; CYST FORMATION; BALTIC SEA; PROTOZOA; DIATOMS	Incubation of untreated sediment samples from the northern part of the Swedish west coast resulted in a conspicuous proliferation of various protists. Samples from ten coastal sites were incubated in filtered seawater and the resulting vegetative stages were recorded for a period of two weeks. At least 47 different dinoflagellate taxa were encountered as vegetative stages, more than 46 different ciliate taxa and at least 64 living diatom taxa were present. There were also cyanobacteria, haptophytes, cryptophytes, euglenophytes, prasinophytes, chlorophytes and amoebae. As total 263 taxa were identified from less than 100 cm(3) sediment, suggesting that most microorganisms are ubiquitous, present almost everywhere within their geographic region, but often rare or cryptic. All dinoflagellates present in the area that are known to be cyst-producing were found, corresponding to 25% of the known dinoflagellates at the Swedish west coast. Approximately 26% of the planktonic and 22% of the pennate diatoms recorded at the Swedish west coast were present in the samples.	Univ Gothenburg, Dept Marine Bot, SE-40530 Gothenburg, Sweden	University of Gothenburg	Persson, A (通讯作者)，Univ Gothenburg, Dept Marine Bot, Box 461, SE-40530 Gothenburg, Sweden.							ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; BINDER BJ, 1987, J PHYCOL, V23, P99; 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; COSTAS E, 1990, TOXIC MARINE PHYTOPLANKTON, P280; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B., 1979, P443; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; EDLER L, 1995, FYTOPLANKTON ARSRAPP; ELBRACHTER M, 1994, REV PALAEOBOT PALYNO, V84, P101, DOI 10.1016/0034-6667(94)90043-4; Erard-Le Denn Evelyne, 1995, P725; FAUST MA, 1990, TOXIC MARINE PHYTOPLANKTON, P138; Fenchel T, 1997, OIKOS, V80, P220, DOI 10.2307/3546589; Finlay BJ, 1998, INT J PARASITOL, V28, P29, DOI 10.1016/S0020-7519(97)00167-7; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; GEDZIOROWSKA D, 1990, TOXIC MARINE PHYTOPLANKTON, P155; GOLLASCH S, IN PRESS CANADIAN J; GRANELI E, 1989, RED TIDES BIOL ENV S; GUJER W, 1983, WATER SCI TECHNOL, V15, P127, DOI 10.2166/wst.1983.0164; Harris ASD, 1998, J EXP MAR BIOL ECOL, V231, P21, DOI 10.1016/S0022-0981(98)00061-6; Huber G., 1922, Z BOTANIK, V14, P337; Jones A.R., 1974, CILIATES; KUYLENSTIERNA M, 2001, CHECKLIST PHYTOPLANT; KUYLENSTIERNA M, 1990, THESIS GOTEBORG U GO; KUYLENSTIERNA M, 1990, THESIS GOTEBORG U GO, V1; LEWIS CM, 1907, BIOL DINOFLAGELLATES, P235; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; Matsuoka K, 2001, SCI TOTAL ENVIRON, V264, P221, DOI 10.1016/S0048-9697(00)00718-X; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; 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; *NIVA, 1996, 349996 NIVA; Olli K, 1996, J PHYCOL, V32, P535, DOI 10.1111/j.0022-3646.1996.00535.x; Pazos Y., 1995, P651; Persson A, 2000, J PLANKTON RES, V22, P803, DOI 10.1093/plankt/22.4.803; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Persson A., 2001, Ph.D. Thesis; PERSSON A, 2000, P 9 INT C HARMF ALG; REID PC, 1978, J MAR BIOL ASSOC UK, V58, P551, DOI 10.1017/S0025315400041205; Rosenberg R, 1996, J SEA RES, V35, P1, DOI 10.1016/S1385-1101(96)90730-3; ROUND FE, 1990, TOXIC DINOFLAGELLATE, P125; Simpson R.L., 1989, ECOLOGY SOIL SEED BA; SONNEMANN JA, 1997, BOT MAR, V40, P147; van den Hoek C., 1995, Algae. An introduction to phycology; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Werner D., 1977, The Biology of Diatoms; 1995, GOTEBORGS BOHUS LANS	52	20	21	0	8	OPHELIA PUBLICATIONS	STENSTRUP	KIRKEBY SAND 19, DK-5771 STENSTRUP, DENMARK	0078-5326			OPHELIA	Ophelia	FEB	2002	55	3					151	166						16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	530DU					2025-03-11	WOS:000174341000002
J	Vink, A; Brune, A; Höll, C; Zonneveld, KAF; Willems, H				Vink, A; Brune, A; Höll, C; Zonneveld, KAF; Willems, H			On the response of calcareous dinoflagellates to oligotrophy and stratification of the upper water column in the equatorial Atlantic Ocean	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cyst; calcareous; equatorial Atlantic; late quaternary; stratification; oligotrophy	LATE QUATERNARY PALEOCEANOGRAPHY; SEA-SURFACE TEMPERATURES; TROPICAL ATLANTIC; THORACOSPHAERA-HEIMII; SPATIAL-DISTRIBUTION; SEASONAL CYCLE; CARBONATE; NORTH; CIRCULATION; SEDIMENTS	Large numbers of calcareous dinoflagellate cysts and the vegetative calcareous coccoid species Thoracosphaera heimii are generally found in sediments underlying oligotrophic and/or stratified (sub)surface water environments. It is difficult to distinguish between the relative importance of these two environmental parameters on calcareous cyst and T. heimii distribution as they usually covary, but this information is essential if we want to apply cysts properly in the reconstruction of palaeoenvironments and past surface water hydrography. In the multi-proxy core GeoB 1523-1 from the Ceara Rise region in the western equatorial Atlantic Ocean (covering the past 155 ka), periods of greatest oligotrophy are not synchronous with periods of greatest stratification (Ruhlemann et al., Mar. Geol. 135 (1996) 127152; Mulitza et al., Geology 25 (1997) 335-338; Mulitza et al., Earth Planet. Sci. Lett. 155 (1998) 237-249), giving us the unique opportunity to differentiate between the effects of both parameters on cyst accumulation. The calcareous cyst record of the core reflects prominent increases in accumulation rate of nearly all observed species only during the nutrient-enriched but more stratified isotopic (sub)stages 5.5, 5.3, 5.1 and 1. In this respect, the distribution trends in the core are more similar to those of the eastern equatorial upwelling region (GeoB 1105-4) than they are to those of the oligotrophic north-eastern Brazilian continental slope (GeoB 2204-2), even though temporal changes in bioproductivity are principally in antiphase between the eastern and western equatorial regions. We conclude that stratification of the upper water column and the presence of a well-developed thermocline are probably the more important factors controlling cyst distribution in the equatorial Atlantic, whereas the state of oligotrophy secondarily influences cyst production within a well-stratified environment. (C) 2002 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich 5, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich 5, Postfach 330 440, D-28334 Bremen, Germany.	vink@micropal.uni-bremen.de	Vink, Annemiek/GXG-6435-2022	Vink, Annemiek/0000-0002-5178-9721				[Anonymous], USE PROXIES PALEOCEA, DOI DOI 10.1007/978-3-642-58646-0_12; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; BACON MP, 1984, ISOT GEOSCI, V2, P97; Bickert T, 1996, SOUTH ATLANTIC, P599; BINDER BJ, 1987, J PHYCOL, V23, P99; Durkoop A, 1997, PALEOCEANOGRAPHY, V12, P764, DOI 10.1029/97PA02270; EPPLEY RW, 1980, ANAL MARINE ECOSYSTE, P343; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; Fensome R.A., 1993, Micropaleontology Press Special Paper; Francois R, 1990, PALEOCEANOGRAPHY, V5, P761, DOI 10.1029/PA005i005p00761; Frank M., 1999, Use of Proxies in Paleoceanography, P409, DOI [10.1007/978-3-642-58646-016, DOI 10.1007/978-3-642-58646-016]; Ganopolski A, 1998, NATURE, V391, P351, DOI 10.1038/34839; Haddad GA, 1996, PALEOCEANOGRAPHY, V11, P701, DOI 10.1029/96PA02406; HASTENRATH S, 1987, J PHYS OCEANOGR, V17, P1518, DOI 10.1175/1520-0485(1987)017<1518:ACOSTS>2.0.CO;2; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; Imbrie J., 1984, Milankovitch and Climate: Understanding the Response to Astronomical Forcing, -, V1, P269; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; JANOFSKE D, 2000, 152 U BREM FACHB GEO, P94; 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; Kinkel H, 2000, MAR MICROPALEONTOL, V39, P87, DOI 10.1016/S0377-8398(00)00016-5; LEDRU MP, 1992, CR ACAD SCI II, V314, P117; LEROUX M, 1993, GLOBAL PLANET CHANGE, V7, P69, DOI 10.1016/0921-8181(93)90041-L; MARTINSON DG, 1987, QUATERNARY RES, V27, P1, DOI 10.1016/0033-5894(87)90046-9; McIntyre A, 1989, PALEOCEANOGRAPHY, V4, P19, DOI 10.1029/PA004i001p00019; Mix AC, 1986, PALEOCEANOGRAPHY, V1, P339, DOI 10.1029/PA001i003p00339; Mix AC, 1986, PALEOCEANOGRAPHY, V1, P43, DOI 10.1029/PA001i001p00043; MOLFINO B, 1990, SCIENCE, V249, P766, DOI 10.1126/science.249.4970.766; Mulitza S, 1997, GEOLOGY, V25, P335, DOI 10.1130/0091-7613(1997)025<0335:PFAROP>2.3.CO;2; Mulitza S, 1998, EARTH PLANET SC LETT, V155, P237, DOI 10.1016/S0012-821X(98)00012-0; MULITZA S, 1994, 57 U BREM FACHB GEOW, P1; MullerKarger FE, 1995, DEEP-SEA RES PT I, V42, P2127, DOI 10.1016/0967-0637(95)00085-2; MULLERKARGER FE, 1988, NATURE, V333, P56, DOI 10.1038/333056a0; PETERSON RG, 1991, PROG OCEANOGR, V26, P1, DOI 10.1016/0079-6611(91)90006-8; Prell WL, 1986, PALEOCEANOGRAPHY, V1, P137, DOI 10.1029/PA001i002p00137; RICHARDSON PL, 1987, J GEOPHYS RES-OCEANS, V92, P3691, DOI 10.1029/JC092iC04p03691; Ruhlemann C, 1996, MAR GEOL, V135, P127, DOI 10.1016/S0025-3227(96)00048-5; Rühlemann C, 2001, PALEOCEANOGRAPHY, V16, P293, DOI 10.1029/1999PA000474; RUHLEMANN C, 1996, 84 U BREM FACH GEOW, P1; Schneider RR, 1996, SOUTH ATLANTIC, P527; SCHULZ HD, 1991, M162 REC BEL, P1; SLOWEY NC, 1995, PALEOCEANOGRAPHY, V10, P715, DOI 10.1029/95PA01166; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; THUNELL RC, 1982, MAR GEOL, V47, P165, DOI 10.1016/0025-3227(82)90067-6; VANDERHAMMEN T, 1994, PALAEOGEOGR PALAEOCL, V109, P247, DOI 10.1016/0031-0182(94)90178-3; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; Vink A, 2001, PALEOCEANOGRAPHY, V16, P479, DOI 10.1029/2000PA000582; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wefer G, 1996, SOUTH ATLANTIC, P461; WEFER G, 1996, S ATLANTIC PRESENT P; WENDLER I, 2002, IN PRESS GLOB PLANET; Zonneveld KAF, 2000, REV PALAEOBOT PALYNO, V111, P197, DOI 10.1016/S0034-6667(00)00024-5	53	37	37	0	13	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	FEB 1	2002	178	1-2					53	66	PII S0031-0182(01)00368-6	10.1016/S0031-0182(01)00368-6	http://dx.doi.org/10.1016/S0031-0182(01)00368-6			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	552LV					2025-03-11	WOS:000175622600004
J	Ten-Hage, L; Robillot, C; Turquet, J; Le Gall, F; Le Caer, JP; Bultel, V; Guyot, M; Molgó, J				Ten-Hage, L; Robillot, C; Turquet, J; Le Gall, F; Le Caer, JP; Bultel, V; Guyot, M; Molgó, J			Effects of toxic extracts and purified borbotoxins from <i>Prorocentrum borbonicum</i> (Dinophyceae) on vertebrate neuromuscular junctions	TOXICON			English	Article						benthic dinoflagellates; borbotoxin; mass spectrometry; neuromuscular junction; Prorocentrum borbonicum; toxicity	OKADAIC ACID PRODUCTION; CORAL-REEF ECOSYSTEM; MARINE DINOFLAGELLATE; BENTHIC DINOFLAGELLATE; INDIAN-OCEAN; PALYTOXIN; LIMA	Benthic dinoflagellates of the genus Prorocentrum are common in tropical and subtropical water and several species produce phycotoxins potentially involved in human toxic outbreaks. The toxic dinoflagellate Prorocentrum borbonicum collected at La Reunion Island (France) was cultured in laboratory. A crude extract of the organism displayed significant toxicity in mice characterized by progressive limb paralysis, severe dyspnea, and death, and the toxicity was retained, after partition, in the extract's butanol-soluble fraction (BSF). Electrophysiological experiments characterizing the fraction's effect on isolated vertebrate neuromuscular preparations revealed that it depolarizes the muscle membrane and reduces the driving force for endplate potentials (EPPs) evoked by nerve stimulation, blocking directly- and indirectly-elicited muscle twitches. The depolarization induced by P. borbonicum BSF was not due to Na+ influx through voltage-dependent Na+ channels, since tetrodotoxin neither prevented nor suppressed the depolarization. However, ouabain, a specific ligand of the Na/K ATPase, reduced the depolarization. These results suggest the presence of palytoxin-like compounds in the fraction. HPLC-MS and MSIMS analysis showed the presence of several toxins having identical UV absorbance, among which two new isomeric toxins, borbotoxin-A and -B, of molecular mass of 1037.6 Da were isolated. The purified borbotoxin-A, had no effect on the resting membrane potential of muscle fibers and did not affect directly-elicited muscle twitches. However, the toxin reduced nerve-evoked muscle twitches, in a dose-dependent manner, reduced EPPs' amplitudes and completely blocked miniature endplate potentials. These observations suggest that the main action of borbotoxin-A is to block post-synaptic nicotinic ACh receptors. (C) 2001 Elsevier Science Ltd. All rights reserved.	Inst Fed Neurobiol Alfred Fessard, CNRS UPR 9040, Neurobiol Cellulaire & Mol Lab, F-91198 Gif Sur Yvette, France; Agence Rech & Valorisat Marine, F-97490 Ste Clotilde, France; Ecole Super Phys & Chim Ind Ville Paris, CNRS ERS 657, Lab Environm & Chim Analyt, F-75005 Paris, France; Natl Museum Nat Hist, CNRS ESA 8041, Lab Chim Substances Nat, F-75005 Paris, France; Natl Museum Nat Hist, Lab Cryptogam, F-75005 Paris, France	Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); Universite PSL; Ecole Superieure de Physique et de Chimie Industrielles de la Ville de Paris (ESPCI); Centre National de la Recherche Scientifique (CNRS); Museum National d'Histoire Naturelle (MNHN); Museum National d'Histoire Naturelle (MNHN)	Molgó, J (通讯作者)，Inst Fed Neurobiol Alfred Fessard, CNRS UPR 9040, Neurobiol Cellulaire & Mol Lab, 1 Ave Terrasse, F-91198 Gif Sur Yvette, France.		Ten-Hage, Loïc/T-2789-2019					BIALOJAN C, 1988, BIOCHEM J, V256, P283, DOI 10.1042/bj2560283; BOMBER JW, 1991, BIOL OCEANOGR, V6, P291; DELCASTILLO J, 1978, J CELL BIOL, V78, P782, DOI 10.1083/jcb.78.3.782; DEMOTTA GE, 1992, B SOC PATHOL EXOT, V85, P489; FRELIN C, 1995, GEN PHARMACOL, V26, P33, DOI 10.1016/0306-3623(94)00133-8; HABERMANN E, 1989, TOXICON, V27, P1171, DOI 10.1016/0041-0101(89)90026-3; Hu TM, 1996, J NAT PROD, V59, P1010, DOI 10.1021/np960439y; Hu TM, 1995, TETRAHEDRON LETT, V36, P9273, DOI 10.1016/0040-4039(95)02010-M; HU TM, 1995, J CHEM SOC CHEM COMM, P597, DOI 10.1039/c39950000597; Lewis Richard J., 1994, Natural Toxins, V2, P56, DOI 10.1002/nt.2620020203; Lewis RJ, 1999, PROCEEDINGS OF THE 5TH INDO-PACIFIC FISH CONFERENCE, P739; Morton SL, 1998, TOXICON, V36, P201, DOI 10.1016/S0041-0101(97)00054-8; MURAKAMI Y, 1982, B JPN SOC SCI FISH, V48, P69; MURATA M, 1990, J AM CHEM SOC, V112, P4380, DOI 10.1021/ja00167a040; MURATA M, 1987, TETRAHEDRON LETT, V28, P5869, DOI 10.1016/S0040-4039(01)81076-5; NAKAMURA H, 1993, TOXICON, V31, P371, DOI 10.1016/0041-0101(93)90172-F; PROVASOLI L, 1958, ANNU REV MICROBIOL, V12, P279, DOI 10.1146/annurev.mi.12.100158.001431; SATAKE M, 1997, BIOSCI BIOTECH BIOCH, V60, P2103; TASUMOTO T, 1979, TOXIC DINOFLAGELLATE, P495; Ten-Hage L, 2000, TOXICON, V38, P1043, DOI 10.1016/S0041-0101(99)00216-0; Ten-Hage L, 2000, PHYCOLOGIA, V39, P296, DOI 10.2216/i0031-8884-39-4-296.1; TINDALL D R, 1989, Toxicon, V27, P83; TINDALL DR, 1984, SEAFOOD TOXINS, P225; TORIGOE K, 1988, J AM CHEM SOC, V110, P7876, DOI 10.1021/ja00231a048; USAMI M, 1995, J AM CHEM SOC, V117, P5389, DOI 10.1021/ja00124a034	25	23	24	1	15	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0041-0101			TOXICON	Toxicon	FEB	2002	40	2					137	148		10.1016/S0041-0101(01)00200-8	http://dx.doi.org/10.1016/S0041-0101(01)00200-8			12	Pharmacology & Pharmacy; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Toxicology	499CQ	11689235				2025-03-11	WOS:000172553800004
J	Adachi, M; Matsubara, T; Okamoto, R; Nishijima, T; Itakura, S; Yamaguchi, M				Adachi, M; Matsubara, T; Okamoto, R; Nishijima, T; Itakura, S; Yamaguchi, M			Inhibition of cyst formation in the toxic dinoflagellate <i>Alexandrium</i> (Dinophyceae) by bacteria from Hiroshima Bay, Japan	AQUATIC MICROBIAL ECOLOGY			English	Article						Alexandrium; dinoflagellate; bacteria; cyst	GONYAULAX-TAMARENSIS; SPERM FORMATION; GERMINATION; PROMOTION; SEXUALITY; EXCAVATA; BLOOMS	The relationship between the abundance of the toxic marine dinoflagellate Alexandrium tamarense (Lebour) Balech and cyst formation-inhibiting bacteria (Alex-CFIB) was investigated in samples taken from the water column in Hiroshima Bay (Japan) in 1999. The cell density of A. tamarense peaked in the middle of April and blooms declined in May. Alex-CFIB were detected during the bloom period as well as the non-bloom period in 1999 by means of the most probable number (MPN) bioassay as well as the colony counting method. A total of 32 strains that had potential Alexandrium cyst formation-inhibiting activities (CFIB) were isolated from the seawater samples from Hiroshima Bay throughout the year. The population structure and genetic diversity of Alex-CFIB, were analyzed by means of restriction fragment length polymorphism (RFLP) of the 16S ribosomal RNA genes (16S rDNA). Five ribotypes, Ia to Id and II types, were determined among the 32 strains of Alex-CFIB. Most of the strains belonged to ribotype I, suggesting that bacteria of ribotype I may be dominant in the Alex-CFIB assemblages in the field seawater. Almost the entire 16S rDNA-based phylogenetic tree showed that ribotypes I and II fell into the class Proteobacteria gamma-subdivision Alteromonas group and the Vibrio group, respectively. The 6-well microplate approach clarified that Alex-CFIB, obtained in this study do not have growth-inhibiting activities, and Alex-CFIB of ribotype I (Alteromonas group) have strong activities of encystment inhibition among these ribotypes. The existence not only of Alexandrium cyst formation-promoting bacteria (Alex-CFPB) reported previously but also of Alex-CFIB, in Hiroshima Bay throughout the year suggests that Alex-CFPB, as well as Alex-CFIB, especially bacteria of ribotype I, may play significant roles in the process of encystment and bloom dynamics of Alexandrium in the natural environment.	Kochi Univ, Fac Agr, Lab Aquat Environm Sci, Nankoku, Kochi 7838502, Japan; Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Harmful Algal Bloom Div, Harmful Phytoplankton Sect, Hiroshima 7390452, Japan	Kochi University; Japan Fisheries Research & Education Agency (FRA)	Kochi Univ, Fac Agr, Lab Aquat Environm Sci, Nankoku, Kochi 7838502, Japan.	madachi@cc.kochi-u.ac.jp						Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; 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; [Anonymous], 2012, Biometry; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; 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; Jukes TH., 1969, MAMMALIAN PROTEIN ME, P21, DOI [10.1016/b978-1-4832-3211-9.50009-7, DOI 10.1016/B978-1-4832-3211-9.50009-7]; NAGAI S, 1994, FISHERIES SCI, V60, P625, DOI 10.2331/fishsci.60.625; Nagai S, 1998, PHYCOLOGIA, V37, P363, DOI 10.2216/i0031-8884-37-5-363.1; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; SAITOU N, 1987, MOL BIOL EVOL, V4, P406, DOI 10.1093/oxfordjournals.molbev.a040454; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; Sambrook J., 1989, MOL CLONING LAB MANU; SAWAYAMA S, 1993, NIPPON SUISAN GAKK, V59, P291; SAWAYAMA S, 1991, THESIS KYOTO U; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; Steidinger K.A., 1975, P153; 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; Yoshinaga I, 1998, MAR ECOL PROG SER, V170, P33, DOI 10.3354/meps170033; YOSHINAGA I, 1995, FISHERIES SCI, V61, P780, DOI 10.2331/fishsci.61.780	28	19	21	1	10	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055	1616-1564		AQUAT MICROB ECOL	Aquat. Microb. Ecol.	JAN 18	2002	26	3					223	233		10.3354/ame026223	http://dx.doi.org/10.3354/ame026223			11	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	520MV		Bronze			2025-03-11	WOS:000173786400002
J	Parrow, MW; Burkholder, JA				Parrow, MW; Burkholder, JA			Flow cytometric determination of zoospore DNA content and population DNA distribution in cultured <i>Pfiesteria</i> spp. (Pyrrhophyta)	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						cell cycle; dinoflagellates; flow cytometry; P. piscicida; P. shumwayae; SYTOX green	LIFE-CYCLE; CELL-CYCLE; TOXIC DINOFLAGELLATE; CRYPTHECODINIUM-COHNII; REFERENCE-STANDARDS; RAPID METHOD; GENOME SIZE; PISCICIDA; BEHAVIOR; PHYTOPLANKTON	The relative cellular DNA content from 23 different clonal cultures of Pfiesteria spp. zoospores was determined using a DNA fluorochrome and flow cytometry, Significant differences between Pfiesteria pisicida and P. shumwayae were detected, both in mean zoospore DNA content and population cell cycle DNA distribution. Intraspecific differences in DNA content were found between clonal zoospore cultures established from different geographical regions. Long-term cultures (years) of P. piscicida were available for testing, and a negative correlation was observed between zoospore DNA content and time in culture. Zoospore cell cycle-related DNA distributions were also markedly different between the two species in these clonal cultures. In most cultures tested, P piscicida zoospores exhibited bit-nodal DNA flow histograms with G1-S-G2 + M distributions, typical of eukaryotic asynchronously cycling cells. In contrast, cultures of P shumwayae zoospores exhibited one DNA peak distribution, indicative of synchronized cells, The data are consistent with the hypothesis that P. shumwayae zoospores are interphasic cells, and mitosis in zoospore cultures of this species predominantly occurs as benthic or adherent non-motile division cysts. Light microscopy observations of the nuclear condition of electrostatically sorted zoospores of each Pfiesteria species also support (his hypothesis. If highly conserved, this disparity in modes of vegetative reproduction would ramify the population dynamics of the two Pfiesteria species. (C) 2002 Elsevier Science B.V. All rights reserved.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA	North Carolina State University	Burkholder, JA (通讯作者)，N Carolina State Univ, Ctr Appl Aquat Ecol, 620 Hutton St,Suite 104, Raleigh, NC 27606 USA.	joann_burkholder@ncsu.edu	Parrow, Matthew/HMO-6676-2023	Parrow, Matthew/0000-0002-3197-2510				ALLEN IC, 2000, THESIS U N CAROLINA; BAGWELL CB, 1989, CYTOMETRY, V10, P689; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; Beam C.A., 1984, P263; BHAUD Y, 1991, J CELL SCI, V100, P675; Bhaud Y, 2000, J CELL SCI, V113, P1231; Bibby B.T., 1972, British phycol J, V7, P85; BOUCHER N, 1991, MAR ECOL PROG SER, V71, P75, DOI 10.3354/meps071075; 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; BURKHOLDER JM, 1995, ARCH PROTISTENKD, V145, P177, DOI 10.1016/S0003-9365(11)80314-3; BURKHOLDER JM, 2001, IN PRESS ENV HLTH S, V5; Cheng YQ, 1999, MICROBIOL-UK, V145, P3539, DOI 10.1099/00221287-145-12-3539; Chisholm S.W., 1986, Can Bull Fish Aquat Sci, V214, P343; Collier JL, 2000, J PHYCOL, V36, P628, DOI 10.1046/j.1529-8817.2000.99215.x; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Edvardsen B, 1996, J PHYCOL, V32, P94, DOI 10.1111/j.0022-3646.1996.00094.x; Eschbach E, 2001, CYTOMETRY, V44, P126, DOI 10.1002/1097-0320(20010601)44:2<126::AID-CYTO1091>3.0.CO;2-N; FAUST MA, 1993, DEV MAR BIO, V3, P115; FENSOME RA, 1998, 3653 DINOFLAJ GEOL S; FRANKER CK, 1971, J PHYCOL, V7, P165, DOI 10.1111/j.0022-3646.1971.00165.x; Glasgow HB, 2001, PHYCOLOGIA, V40, P234, DOI 10.2216/i0031-8884-40-3-234.1; Graham L.E., 2000, Algae; GRAY JW, 1987, TECHNIQUES CELL CYCL, P93; Green JC, 1996, J MARINE SYST, V9, P33, DOI 10.1016/0924-7963(96)00014-0; HOLMHANSEN O, 1969, SCIENCE, V163, P87, DOI 10.1126/science.163.3862.87; HOLT JR, 1982, AM J BOT, V69, P1165, DOI 10.2307/2443090; HORIGUCHI T, 1988, BOT MAG TOKYO, V101, P255, DOI 10.1007/BF02488603; Johnston JS, 1999, AM J BOT, V86, P609, DOI 10.2307/2656569; KARENTZ D, 1983, J PROTOZOOL, V30, P581, DOI 10.1111/j.1550-7408.1983.tb05481.x; KELLEY I, 1989, J PHYCOL, V25, P241, DOI 10.1111/j.1529-8817.1989.tb00118.x; KEMPTON JW, 1999, PCR FISH ASSAYS DETE; Lewitus AJ, 1999, J PHYCOL, V35, P303, DOI 10.1046/j.1529-8817.1999.3520303.x; Loeblich A.R., 1981, Journal of Plankton Research, V3, P67, DOI 10.1093/plankt/3.1.67; Loeblich A.R. 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Exp. Mar. Biol. Ecol.	JAN 3	2002	267	1					35	51		10.1016/S0022-0981(01)00343-4	http://dx.doi.org/10.1016/S0022-0981(01)00343-4			17	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	508MN					2025-03-11	WOS:000173093000003
J	McMinn, A				McMinn, A			Marine Quaternary dinoflagellate cysts of Australia, Papua-New Guinea, New Zealand and the Southern Ocean: a review	ALCHERINGA			English	Article						Quaternary; Pleistocene; recent; dinoflagellate cyst; biostratigraphy; palaeotemperature; salinity; Australia; New Zealand; Southern Ocean	GYMNODINIUM-CATENATUM; CHATHAM RISE; SEDIMENTS; WATERS; WALES	Dinoflagellate cysts are widespread in Australian, Papua-New Guinea, New Zealand and Southern Ocean Pleistocene and Recent marine sediments. They occur in estuaries and deltas as well as on the continental shelf and in ocean basins. They have proven invaluable in palaeoecology for the interpretation of changing temperature, salinity and distance from shore in particular. These changes have also been used to examine climate change in Quaternary sequences. A small number of First Appearance Datums (FADs) and Last Appearance Datums (LADs) within this time period allows only limited biostratigraphic definition. LADs within the Pleistocene of southern Australia include Achomosphaera ramulifera and Spiniferites rubinus. Introduction within the past 50 years of several taxa, such as Gymnodinium catenatum and Gymnodinium microreticulatum, has been attributed to ballast water import.	Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia	University of Tasmania	McMinn, A (通讯作者)，Univ Tasmania, Inst Antarctic & So Ocean Studies, Box 252-77, Hobart, Tas 7001, Australia.		McMinn, Andrew/A-9910-2008					[Anonymous], NEOGENE QUATERNARY D; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Bint A.N., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P329; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; CLOWES C D, 1985, New Zealand Journal of Geology and Geophysics, V28, P152; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Evitt W. R., 1961, Micropaleontology, V7, P385, DOI 10.2307/1484378; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Harland R, 1999, REV PALAEOBOT PALYNO, V107, P265, DOI 10.1016/S0034-6667(99)00023-8; HARLAND R, 1982, PALAEONTOLOGY, V29, P321; Head M.J., 1996, Palynology: Principles and Applications, P1197; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Matsuoka Kazumi, 1997, Palynology, V21, P19; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; MCMINN A, 1992, QUATERNARY RES, V38, P347, DOI 10.1016/0033-5894(92)90043-I; MCMINN A, 1989, MICROPALEONTOLOGY, V35, P1, DOI 10.2307/1485534; MCMINN A, 1992, MICROPALEONTOLOGY, V38, P315, DOI 10.2307/1485797; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; McMinn A., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P429, DOI 10.2973/odp.proc.sr.123.120.1992; McMinn A, 2001, MAR MICROPALEONTOL, V43, P207, DOI 10.1016/S0377-8398(01)00026-3; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; McMinn A, 1997, MAR MICROPALEONTOL, V29, P407, DOI 10.1016/S0377-8398(96)00012-6; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; MCMINN A, 1994, P ODP SCI RESULTS, V133, P93; MCMINN A, 1994, P ODP SCI RESULTS, V133, P97; MCMINN A, IN PRESS HARMFUL ALG; MCMINN A, 1991, Q NOTES NEW S WALES, V85, P1; McMinn A., 1992, NEOGENE QUATERNARY D, P147; MCMINN A, 1988, P LINN SOC N S W, V109, P175; McMinn Andrew, 1992, Palynology, V16, P13; McMinn Andrew, 1994, Palynology, V18, P41; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; SUN XK, 1994, MAR MICROPALEONTOL, V23, P345, DOI 10.1016/0377-8398(94)90023-X; Thom B.G., 1984, COASTAL GEOMORPHOLOG; Thorsen TA, 1998, PALAEOGEOGR PALAEOCL, V143, P159, DOI 10.1016/S0031-0182(98)00079-0; Wall D., 1965, Grana Palynologica, V6, P297; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363	38	3	3	0	4	GEOLOGICAL SOCIETY AUSTRALIA INC	SYDNEY	701 WYNYARD HOUSE, 301 GEORGE STREET, SYDNEY, NSW 2000, AUSTRALIA	0311-5518			ALCHERINGA	Alcheringa		2002	26	3-4					519	530		10.1080/03115510208619541	http://dx.doi.org/10.1080/03115510208619541			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	614AY					2025-03-11	WOS:000179165700011
J	Guler, MV; Guerstein, GR; Malumián, N				Guler, MV; Guerstein, GR; Malumián, N			Biostratigraphy of the Neogene Barranca Final Formation of the Colorado Basin, Argentina	AMEGHINIANA			Spanish	Article						biostratigraphy; dinoflagellate cysts; neogene; Colorado Basin; Argentina	DINOFLAGELLATE CYSTS; EASTERN ENGLAND; BOREHOLE; PLIOCENE	Dinoflagellate cysts from the Barranca Final Formation type section are diverse and well preserved. The assemblages are dominated by the Order Gonyaulacales, with subordinate Peridiniales represented only by protoperidiniaceans. Based on selected dinoflagellate cyst events, and in accordance with the foraminiferal data, we suggest a Middle to Late Miocene age for the section. Labyrinthodinium truncatum subsp. truncatum Piasecki ranges from latest Early Miocene or early Middle Miocene through Late Miocene and Selenopemphix dionaeacysta Head et al, has its range base within the Middle Miocene. The occurrences of these species together with the presence of Brigantedinium cariacoense (Wall) Reid confirms an age not older than Middle Miocene for the bottom of the section. The low representation of oceanic species, such as Impagidinium spp., the presence of Nematosphaeropsis rigida Wrenn (inner to outer? neritic), the diverse representation of protoperidinacean species (inner neritic), and the abundance of euryhaline forms, particularly specimens of the Operculodinium centrocarpum/israelianum complex, Tuberculodinium vancampoae Wall and Lingulodinium hemicystum McMinn, reflect estuarine to inner neritic conditions for the lower part of the section. Tuberculodinium vancampoae and Lingulodinium machaerophorum (Deflandre y Cookson) Wall suggest warm temperate to tropical conditions. Upwards, the assemblages are characterized by an increased terrigenous influx together with the apparent disappearance of most dinocyst taxa. Within the generally estuarine palaeoenvironment, the occurrence of oceanic to neritic markers coinciding with a glauconitic section, suggests a marine flooding Surface.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Argentina; Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; Serv Geol Minero Argentina, RA-1107 Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Guler, MV (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Argentina.							[Anonymous], 1979, AMEGHINIANA; BECKER D, 1980, ACTAS, V2, P315; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bertels A., 1979, Ameghiniana, V16, P273; del Rio C.J., 1992, Anales de la Academia Nacional de Ciencias Exactas Fisicas y Naturales de Buenos Aires, V42, P205; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Fensome R.A., 1993, Micropaleontology Press Special Paper; FENSOME RA, 1998, DINOFLAJ GEOLOGICAL; Gamerro J.C., 1981, REV ESP MICROPALEONT, V13, P110; Guerstein GR, 2000, AMEGHINIANA, V37, P81; GUERSTEIN GR, IN PRESS AMEGHINIANA; Guler M.V., 2001, Revista Espanola de Micropaleontologia, V33, P183; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head Martin J., 1993, Palynology, V17, P201; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 1999, J PALEONTOL, V73, P1; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; Kaasschieter J.P., 1965, Actas II Jornada Geologia Argentina, V3, P251; Kaasschieter J.P.H., 1963, TULSA GEOLOGICAL SOC, V31, P177; Londeix L., 1999, PLIOCENE TIME CHANGE, P65; MALUMIAN N, 1972, Ameghiniana, V9, P97; MALUMIAN N, 1970, Ameghiniana, V7, P173; Malumian N., 1998, ACTAS X C LATINOAM G, V1, P125; MALUMIAN N, 1996, REL 13 C GEOL ARG 3, P74; Malumian N., 1999, ANALES I GEOLOGIA RE, V29, P557; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; ODIN GS, 1981, SEDIMENTOLOGY, V28, P611, DOI 10.1111/j.1365-3091.1981.tb01925.x; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Powell A.J., 1992, P155; QUATTROCCHIO M, 1988, REV ASOCIACION GEOLO, V43, P375; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; SCASSO RA, 1999, ACTAS, V1, P73; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1998, MESOZOIC CENOZOIC SE	35	15	16	0	1	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana		2002	39	1					103	110						8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	553FH					2025-03-11	WOS:000175664800008
C	Wendler, J; Willems, H		Koeberl, C; MacLeod, KG		Wendler, J; Willems, H			Distribution pattern of calcareous dinoflagellate cysts across the Cretaceous-Tertiary boundary (Fish Clay, Stevns Klint, Denmark): Implications for our understanding of species-selective extinction	CATASTROPHIC EVENTS AND MASS EXTINCTIONS: IMPACTS AND BEYOND	Geological Society of America Special Papers		English	Proceedings Paper	International Interdisciplinary Conference on Catastrophic Events and Mass Extinctions - Impacts and Beyond	JUL 09-12, 2000	UNIV VIENNA, VIENNA, AUSTRIA	Lunar & Planetary Inst, Barringer Crater Co, European Sci Fdn Impact, Fed Minist Educ, Sci, and Culture, Geolog Survey Austria, Vienna Convent Bureau, Int Assoc Geochem & Cosmochem, Finnegan, Micromass, & Cameca Instruments	UNIV VIENNA		K/T BOUNDARY; MASS EXTINCTION; ATLANTIC-OCEAN; EL-KEF; FORAMINIFERA; TUNISIA; EVENTS; CHALK	The distribution patterns of calcareous dinoflagellate cysts were studied in the classic Cretaceous-Tertiary (K-T) boundary section of Stevns Klint, Denmark, focusing mainly on the response of the cyst association to an abrupt environmental catastrophe. A major part of the Fish Clay, which covers the K-T boundary at its base and is exposed in the investigated section, contains fallout produced by an asteroid impact. Calcareous dinoflagellate cysts are the best-preserved remains of carbonate-producing phytoplankton in this layer. The potential of this group of microfossils for the analysis of survival strategies and extinction patterns has been underestimated. The cyst species of the investigated section can be grouped into four assemblages that represent victims, survivors, opportunists, and specially adapted forms. The victims (Pithonel-loideae) were an extremely successful group throughout the Upper Cretaceous, but were restricted to the narrow outer shelf. This restriction minimized their spatial distribution, which generally should be large to facilitate escape from unfavorable conditions. Spatial restriction optimized the population decrease by mass mortality, disabling a successful recovery. In contrast, the survivors that became the dominating group in the Danian had a wide spatial range from the shelf environment to the oceanic realm. A unique calcareous dinocyst assemblage in the Fish Clay shows that even under the stressed conditions immediately following the impact event, some species flourished due to special adaptation or high ecological tolerance. The ability of these dinoflagellate species to form calcareous resting cysts in combination with their generally wide spatial distribution in a variety of environments appears to be the main reason for a low extinction rate at the K-T boundary as opposed to the high extinction rate of other phytoplankton groups, such as the coccolithophorids.	Univ Bremen, Dept Geol, D-28334 Bremen, Germany	University of Bremen	Wendler, J (通讯作者)，Univ Bremen, Dept Geol, POB 330440, D-28334 Bremen, Germany.	wendler@uni-bremen.de						ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; Birkelund T., 1982, Geological Society of America Special Papers, V190, P373; 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; Christensen L., 1973, B GEOL SOC DENMARK, V22, P193; Dale B., 1983, P69; Dali-Ressot M.-D., 1987, THESIS U TUNIS TUNIS; Fensome R.A., 1993, Micropaleontology Press Special Paper; FUTTERER DK, 1984, INITIAL REP DEEP SEA, V74, P533; FUTTERER DK, 1990, SCI RESULTS OCEAN DR, P533; Gale AS, 1999, PHILOS T R SOC A, V357, P1815, DOI 10.1098/rsta.1999.0402; GRIFFIS K, 1990, LETHAIA, V23, P379, DOI 10.1111/j.1502-3931.1990.tb01370.x; GRIFFIS K, 1989, PALAEOGEOGR PALAEOCL, V67, P305; Håkansson E, 1999, PALAEOGEOGR PALAEOCL, V154, P67, DOI 10.1016/S0031-0182(99)00087-5; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hardenbol J., 1998, SEPM SPECIAL PUBLICA; HILDEBRAND AR, 1991, GEOLOGY, V19, P867, DOI 10.1130/0091-7613(1991)019<0867:CCAPCT>2.3.CO;2; Hildebrand-Habel T, 1999, REV PALAEOBOT PALYNO, V106, P57, DOI 10.1016/S0034-6667(98)00079-7; Janofske D, 2000, J PHYCOL, V36, P178, DOI 10.1046/j.1529-8817.2000.98224.x; KASTNER M, 1984, SCIENCE, V226, P137, DOI 10.1126/science.226.4671.137; KELLER G, 1988, PALAEOGEOGR PALAEOCL, V66, P153, DOI 10.1016/0031-0182(88)90198-8; Keller G., 1995, PALEOGEOGR PALEOCLIM, V119, P221; KELLER G, 2000, SPR M AMICO 2000 AST, V11, P28; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P127; KIENEL U, 1994, THESIS BERLINER GEOW, V12; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; MACLEOD N, 1991, GEOLOGY, V19, P497, DOI 10.1130/0091-7613(1991)019<0497:HDAMEA>2.3.CO;2; Marshall CR, 1996, SCIENCE, V274, P1360, DOI 10.1126/science.274.5291.1360; Mitchell SF, 1998, PALAEOGEOGR PALAEOCL, V137, P103, DOI 10.1016/S0031-0182(97)00087-4; Molina E, 1998, B SOC GEOL FR, V169, P351; NEUMANN C, 1999, THESIS BERLINER GE E, V31; OLSSON RK, 1993, PALAIOS, V8, P127, DOI 10.2307/3515167; POPE KO, 1994, EARTH PLANET SC LETT, V128, P719, DOI 10.1016/0012-821X(94)90186-4; Pospichal J.J., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P735, DOI 10.2973/odp.proc.sr.122.187.1992; POSPICHAL JJ, 1994, GEOLOGY, V22, P99, DOI 10.1130/0091-7613(1994)022<0099:CNATKT>2.3.CO;2; SCHMITZ B, 1992, PALAEOGEOGR PALAEOCL, V96, P233, DOI 10.1016/0031-0182(92)90104-D; SCHMITZ B, 1990, GEOLOGY, V18, P93; Smit J, 1999, ANNU REV EARTH PL SC, V27, P75, DOI 10.1146/annurev.earth.27.1.75; SMIT J., 1982, Geological implications of impacts of large asteroids and comets on the Earth, P329; SMIT J, 2000, SCHRIFTENREIHE DTSCH, V11, P46; Villain J.-M., 1981, CRETACEOUS RES, V2, P435; Ward PD, 1995, PALAIOS, V10, P530, DOI 10.2307/3515092; Wendler J, 2001, REV PALAEOBOT PALYNO, V115, P69, DOI 10.1016/S0034-6667(01)00050-1; WENDLER J, 2001, THESIS U BREMEN; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Willems H, 1996, GEOL MIJNBOUW, V75, P215; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; Willems Helmut, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V198, P141; Young JR, 1997, PALAEONTOLOGY, V40, P875; ZUGEL P, 1994, VERBREITUNG KALKIGER, V176	50	35	35	0	2	GEOLOGICAL SOC AMER INC	BOULDER	3300 PENROSE PL, PO BOX 9140, BOULDER, CO 80301 USA	0072-1077		0-8137-2356-6	GEOL SOC AM SPEC PAP			2002	356						265	275						11	Geochemistry & Geophysics; Geology	Conference Proceedings Citation Index - Science (CPCI-S)	Geochemistry & Geophysics; Geology	BV31N					2025-03-11	WOS:000178575200019
J	Meggers, H; Freudenthal, T; Nave, S; Targarona, J; Abrantes, F; Helmke, P				Meggers, H; Freudenthal, T; Nave, S; Targarona, J; Abrantes, F; Helmke, P			Assessment of geochemical and micropaleontological sedimentary parameters as proxies of surface water properties in the Canary Islands region	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Review							PLANKTONIC-FORAMINIFERA; NORTHWEST AFRICA; CARBON FLUX; PRODUCTIVITY GRADIENT; CONTINENTAL-MARGIN; CALCIUM-CARBONATE; SEASONAL-CHANGES; CLIMATIC-CHANGE; DEEP-OCEAN; TEMPERATURE	The Canary Islands region occupies a key position with respect to biogeochemical cycles, with the zonal transition from oligotrophic to nutrient-rich waters and the contribution of Saharan dust to the particle flux. We present the distribution of geochemical proxies (TOC, carbonate, delta(15)N, delta(13)C(org), C/N-ratio) and micropaleontological parameters (diatoms, dinoflagellates, foraminifera, pteropods), in 80 surface-sediment samples in order to characterise the influence of coastally upwelled water on the domain of the subtropical gyre. Results of the surface-sediment analyses confirmed the high biomass gradient from the coast to the open ocean inferred from satellite data of surface chlorophyll or SST. The distribution of total dinoflagellate cysts, the planktic foraminifera species Globigerina bulloides, the diatom resting spore Chaetoceros spp., and TOC concentration coincided well with the areas of strong filament production off Cape Ghir and Cape Yubi. The warm-water planktic foraminifera Globigerinoides ruber (white), the diatom Nitzschia spp., and the delta(15)N-values showed the opposite trend with high values in the open ocean. Factor analyses on the planktic foraminifera species distribution indicated three major assemblages in the Canary Islands region that represent the present surface-water conditions from the upwelling influenced region via a mixing area towards the subtropical gyre. (C) 2002 Elsevier Science Ltd. All rights reserved.	Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; Inst Geol & Mineiro, Dept Geol Marinha, P-2720 Alfragide, Portugal; Univ Barcelona, Dept Estratig & Paleontol, E-08071 Barcelona, Spain	University of Bremen; University of Barcelona	Univ Bremen, Dept Geosci, Post Box 330440, D-28334 Bremen, Germany.	meggers@allgeo.uni-bremen.de	Abrantes, Fatima/N-7253-2019; Nave, Sílvia/AAU-4670-2020; Abrantes, Fatima/B-5985-2013	Abrantes, Fatima/0000-0002-9110-0212				Abrantes F, 2002, DEEP-SEA RES PT II, V49, P3599, DOI 10.1016/S0967-0645(02)00100-5; Abrantes F, 1999, OCEANOL ACTA, V22, P67, DOI 10.1016/S0399-1784(99)80034-6; ABRANTES F, 1988, MAR GEOL, V85, P15, DOI 10.1016/0025-3227(88)90082-5; ABRANTES F, 1994, CARBON CYCLING GLACI, V17, P425; ALTABET MA, 1994, GLOBAL BIOGEOCHEM CY, V8, P103, DOI 10.1029/93GB03396; [Anonymous], 1990, PALAEOGEOG PALAEOCLI; [Anonymous], METEOR FORSCHUNGSERG; [Anonymous], OCEAN DATA VIEW; Aristegui J, 1997, DEEP-SEA RES PT I, V44, P71, DOI 10.1016/S0967-0637(96)00093-3; ARISTEGUI J, 1994, DEEP-SEA RES PT I, V41, P1509, DOI 10.1016/0967-0637(94)90058-2; Barcena MA, 1998, MAR MICROPALEONTOL, V35, P91, DOI 10.1016/S0377-8398(98)00012-7; Barton E., 1998, The Sea: The Global Coastal Ocean. 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Part II-Top. Stud. Oceanogr.		2002	49	17					3631	3654	PII S0967-0645(02)00103-0	10.1016/S0967-0645(02)00103-0	http://dx.doi.org/10.1016/S0967-0645(02)00103-0			24	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	596TX					2025-03-11	WOS:000178183000015
J	Hamel, D; de Vernal, A; Gosselin, M; Hillaire-Marcel, C				Hamel, D; de Vernal, A; Gosselin, M; Hillaire-Marcel, C			Organic-walled microfossils and geochemical tracers: sedimentary indicators of productivity changes in the North Water and northern Baffin Bay during the last centuries	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article							CONTINENTAL-SHELF SEDIMENTS; SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYSTS; BIOGENIC SILICA; CARBON ACCUMULATION; MARINE-SEDIMENTS; DAVIS STRAIT; DEEP-SEA; POLYNYA; ENVIRONMENT	Analyses performed on 26 surface sediment samples collected with a box corer at 17 stations throughout the North Water and northern Baffin Bay (75-79degreesN; 68-80degreesW) revealed abundant organic-walled microfossils, mostly dinoflagellate cysts (10(3)-10(4) cysts g(-1)) and organic linings of benthic foraminifers (10(2)-10(3) OLg(-1)), as well as high organic carbon concentrations (0.87-2.81% dry weight). These data indicate high productivity in both the pelagic and benthic environments of the North Water and slightly lower productivity in northern Baffin Bay. The data also showed calcium carbonate and biogenic silica dissolution throughout the study area. The dinocyst assemblages were relatively uniform in the North Water and dominated by heterotrophic taxa (Algidasphaeridium? minutum and Brigantedinium spp.), whereas northern Baffin Bay assemblages were dominated by autotrophic taxa, notably Operculodinium centrocarpum and Spiniferites elongatus. The difference between these two assemblages may be related to higher diatomaceous primary production in the North Water than in northern Baffin Bay, since diatoms constitute the principal food source of heterotrophic dinoflagellates. The biogeographical boundary between the North Water and northern Baffin Bay has been maintained for at least the last few centuries as shown by analyses of microfossils and geochemical tracers in two sediment cores, one taken in the southeastern part of the North Water (76degrees17'N, 72degrees02'W) and the other in northeastern Baffin Bay (75degrees35'N, 70degrees48'W). The analyses of the North Water core revealed relatively uniform microfossil assemblages and organic carbon fluxes ranging from 1.1 to 1.5 mg C-org cm(-2) yr(-1) for the last few centuries, which corresponded to 4-6% of the present annual primary production in the euphotic zone. These data suggest high productivity and relatively stable conditions in the polynya on a decadal time scale. In the northeastern Baffin Bay core, the analyses indicated generally lower organic carbon fluxes, ranging from 0.3 to 0.6 mg C-org cm(-2) yr(-1), and (from the microfossil data) significant variations in sea-surface conditions at this lower latitude over the last centuries. (C) 2002 Elsevier Science Ltd. All rights reserved.	Univ Quebec, Inst Sci Mer Rimouski, ISMER, Rimouski, PQ G5L 3A1, Canada; Univ Quebec, Ctr Rech Geochim Isotop & Geochronol, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec; University of Quebec Montreal	Hamel, D (通讯作者)，Univ Quebec, Inst Sci Mer Rimouski, ISMER, 310 Allee des Ursulines, Rimouski, PQ G5L 3A1, Canada.		Hillaire-Marcel, Claude/H-1441-2012; Gosselin, Michel/B-4477-2014; Hillaire-Marcel, Claude/C-9153-2013; de Vernal, Anne/D-5602-2013	Gosselin, Michel/0000-0002-1044-0793; Hillaire-Marcel, Claude/0000-0002-3733-4632; de Vernal, Anne/0000-0001-5656-724X				AKSU AE, 1983, MAR GEOL, V53, P331, DOI 10.1016/0025-3227(83)90049-X; AKSU AE, 1987, CAN J EARTH SCI, V24, P1833, DOI 10.1139/e87-174; AMBROSE WG, 1995, J GEOPHYS RES-OCEANS, V100, P4411, DOI 10.1029/94JC01982; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; [Anonymous], 1999, BIOSTAT ANAL; [Anonymous], 1996, PALYNOLOGY PRINCIPLE; BACLE J, 2000, THESIS MCGILL U MONT; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Blake W, 1998, B GEOL SOC DENMARK, V44, P129; Clough LM, 1997, DEEP-SEA RES PT II, V44, P1683, DOI 10.1016/S0967-0645(97)00052-0; DahlJensen D, 1998, SCIENCE, V282, P268, DOI 10.1126/science.282.5387.268; 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, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEMASTER DJ, 1981, GEOCHIM COSMOCHIM AC, V45, P1715, DOI 10.1016/0016-7037(81)90006-5; DeMaster DJ, 1996, J GEOPHYS RES-OCEANS, V101, P18501, DOI 10.1029/96JC01634; DEMASTER DJ, 1991, MAR CHEM, V35, P489, DOI 10.1016/S0304-4203(09)90039-1; DEVERNAL A, 1999, UNPUB CAHIERS GEOTOP, V3; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; DUNBAR IM, 1969, ARCTIC, V44, P438; Dunbar M.J., 1981, Polynyas in the Canadian Arctic, P29; FLYNN WW, 1968, ANAL CHIM ACTA, V43, P221, DOI 10.1016/S0003-2670(00)89210-7; GREBMEIER JM, 1995, J GEOPHYS RES-OCEANS, V100, P4439, DOI 10.1029/94JC02198; HAMEL D, 2001, THESIS U QUEBEC RIMO; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hutchins DA, 1998, NATURE, V393, P561, DOI 10.1038/31203; KAWAKITA M, 1990, Journal of the Oceanographical Society of Japan, V46, P1, DOI 10.1007/BF02334219; KU TL, 1967, PROG OCEANOGR, V4, P95; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; LEDUC J, 2001, THSIS U QUEBEC MONTR; Levac E, 2001, J QUATERNARY SCI, V16, P353, DOI 10.1002/jqs.614; LEVENTHAL J, 1990, GEOCHIM COSMOCHIM AC, V54, P2621, DOI 10.1016/0016-7037(90)90249-K; LOUCHEUR V, 1999, THESIS U QUEBEC MONT; Matishov GG, 1999, WORLD RESOURCE REV, V11, P190; MAYER LM, 1994, GEOCHIM COSMOCHIM AC, V58, P1271, DOI 10.1016/0016-7037(94)90381-6; Melling H, 2001, ATMOS OCEAN, V39, P301, DOI 10.1080/07055900.2001.9649683; MICHEL C, 2002, J GEOPHYSICAL RES; MORTLOCK RA, 1989, DEEP-SEA RES, V36, P1415, DOI 10.1016/0198-0149(89)90092-7; Mostajir B, 2001, AQUAT MICROB ECOL, V23, P205, DOI 10.3354/ame023205; Mucci A, 2000, DEEP-SEA RES PT II, V47, P733, DOI 10.1016/S0967-0645(99)00124-1; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. 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Part II-Top. Stud. Oceanogr.		2002	49	22-23					5277	5295	PII S0967-0645(02)00190-X	10.1016/S0967-0645(02)00190-X	http://dx.doi.org/10.1016/S0967-0645(02)00190-X			19	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	612CD					2025-03-11	WOS:000179055800023
C	Sarjeant, WAS		Oldroyd, DR		Sarjeant, WAS			'As chimney-sweepers, come to dust': a history of palynology to 1970	EARTH INSIDE AND OUT: SOME MAJOR CONTRIBUTIONS TO GEOLOGY IN THE TWENTIETH CENTURY	Geological Society Special Publication		English	Proceedings Paper	31st International Geological Congress	AUG 16-18, 2000	RIO DE JANEIRO, BRAZIL	Int Commiss Hist Geol Sci, IGCP 404, INQUA			HYDROCARBONS; HYSTRICHOSPHERES; MICROORGANISMS; LIMESTONE; FOSSILS	A brief overview is given of the various fields of palynology, their practical applications being stressed. Particular attention is thereafter paid to the history of palaeopalynology, here considered as the study of pre-Quaternary palynomorphs. This is presented as three stages: the period of pioneer discoveries (to 1918); years of slow progress (1919-1945); and a post-World War II period of accelerating discoveries (1946-1970). Developments concerning the different groups of palynomorphs during these periods are successively presented, under six headings: spores and pollen; dinoflagellates (and acritarchs); prasinophytes; scolecodonts; chitinozoans; and other palynomorphs. The changes brought about in palynology by improving preparation techniques and microscopical equipment are stressed. A brief overview is attempted concerning the developments since 1970, consequent upon ever-expanding research, new preparation techniques and new technology. As conclusion, an overview is presented of the history of palynology and likely future developments are discussed.	Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada	University of Saskatchewan	Univ Saskatchewan, Dept Geol Sci, 114 Sci Pl, Saskatoon, SK S7N 5E2, Canada.							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J	Matsuoka, K				Matsuoka, Kazumi			Implication of cyst morphology to dinoflagellate taxonomy	FISHERIES SCIENCE			English	Article						dinoflagellate cyst; taxonomy; archeopyle; Alexandrium; Gymnodinium catenatum	MOTILE STAGE RELATIONSHIPS; THECA RELATIONSHIP; DINOPHYCEAE; NOV	A part of modem dinoflagellates produce resting cysts. Morphology of such cysts is rather simple and different from that of motile vegetative cells. For this reason, two independent classification systems, one for motile forms and the other for resting cysts are developed independently For understanding the evolution of dinofiagellates, we should unite these two systems. Important characters for dinoflagellate cyst identification are the shape of the cyst body and its ornamentation, wall structure and colour, and the type of aperture or archeopyle. The archeopyle is subdivided into three major groups; saphopylic, theropylic and cryptopylic types. In general, the first two types are developed in thecate peridiniales and gonyaulacales, and the last type is mainly formed in athecate gymnodiniales cysts. Observations of archeopyle types and wall composition in modern cysts have shown these features to be in dinoflagellate taxonomy. In the genus Protoperidinium, another new subgenus should be established for species having a combination apical archeopyle corresponding to three apical plates. Alexandrium tamarense has a chasmic archeopyle, but it is not clear in many cases. It may be the result of diminishing the opening on the cyst surface after gemination because of its thin and flexible cyst wall.	Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan	Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan.	kazu-mtk@net.nagasaki-u.ac.jp						Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; Dale B., 1983, P69; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P298, DOI 10.1073/pnas.49.3.298; Evitt WR, 1963, NATL ACAD SCI P, V49, P158; FENSOME RA, 1993, MICROPAL SPEC PUBL, V7; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Kokinos John P., 1995, Palynology, V19, P143; LEWIS J, 1990, BRIT PHYCOL J, V25, P339, DOI 10.1080/00071619000650381; Lewis J, 2001, EUR J PHYCOL, V36, P137, DOI 10.1017/S0967026201003171; Lewis J, 1987, HOUR MICROPALAEONTOL, V3, P113; Lewis J, 1999, GRANA SUPPL, V3, P1; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Matsuoka K., 2000, TECHNICAL GUIDE MODE; Matsuoka K, 1985, REV PALAEOBOT PALYNO, V45, P255; Matsuoka K., 1987, Bull. Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; Sarjeant WAS, 1984, CAN J BOT, V60, P922; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Yuki Katsuhisa, 1996, Bulletin of Plankton Society of Japan, V43, P46; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1	21	1	1	1	8	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.		2002	68			1			507	510		10.2331/fishsci.68.sup1_507	http://dx.doi.org/10.2331/fishsci.68.sup1_507			4	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	V15CR		Bronze			2025-03-11	WOS:000207780600135
J	Louwye, S				Louwye, S			Dinoflagellate cyst biostratigraphy of the Upper Miocene Deurne Sands (Diest Formation) of northern Belgium, southern North Sea Basin	GEOLOGICAL JOURNAL			English	Article						dinoflagellate cysts; acritarchs; biostratigraphy; Upper Miocene; Deurne Sands; southern North Sea Basin	EASTERN ENGLAND; DEPOSITIONAL HISTORY; PLIOCENE; STRATIGRAPHY	Diverse and well-preserved palynomorph assemblages recovered from the Deurne Sands, a local member of the Upper Miocene Diest Formation near Antwerp, allow the recognition of dinoflagellate cyst biozones defined in the North Atlantic realm (East Coast, USA) and the North Sea region (Nieder Ochtenhausen well, northern Germany). Based on the dinoflagellate cyst assemblages and the calcareous microfossils, the deposition of the Deurne Sands took place at some time during middle to late Tortonian (Late Miocene). These sands can be correlated biostratigraphically with the Dessel Sands in the Campine area of northern Belgium. This correlation demonstrates the existence of two separate and. contemporary depositional areas in northern Belgium during early Late Miocene times. Copyright (C) 2002 John Wiley Sons, Ltd.	State Univ Ghent, Lab Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，State Univ Ghent, Lab Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				Blow W. H., 1969, P199; de Meuter F., 1980, Aardkundige Mededelingen, V1, P79; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Meuter F. J. C, 1970, Bull. Soc. belge Geol. Paleont. Hydrol., V79, P175; De Verteuil L., 1996, P OCEAN DRILLING PRO, V150, P439; de Verteuil Laurent, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P129; DEMEUTER F, 1976, GEOLOGICAL SURVEY BE, P1; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Doppert J.W.C., 1979, MEDEDELINGEN RIJKS G, V31, P1; GLIBERT M, 1955, B I ROYAL SCI NATURE, V31, P1; GLIBERT M, 1962, S STRAT NEOG NORD HE, P40; GULLENTOPS F, 1983, GUIDES GEOLOGIQUES R, P164; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head Martin J., 1993, Paleontological Society Memoir, V31, P1; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 1998, GEOL MAG, V135, P803, DOI 10.1017/S0016756898001745; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; HERNGREEN GFW, 1987, MEDEDELINGEN WERKGRO, V24, P31; HINSCH W, 1988, NW EUROPEAN TERTIARY, P344; Hooyberghs H., 1988, NW EUROPEAN TERTIARY, V100, P190; HOOYBERGHS H, 1972, KLASSE WETENSCHAPPEN, V34, P1; Hooyberghs H.J.F., 1983, Aardkundige Mededelingen, V2, P1; Hooyberghs Herman J.F., 1996, Tertiary Research, V17, P15; *IGCP 124 WORK GRO, 1988, NW EUR TERT BAS A, P145; LAGA P G H, 1972, Bulletin de la Societe Belge de Geologie de Paleontologie et d'Hydrologie, V81, P211; Lagaaij R., 1952, MEDEDELINGEN GEOLOGI, V5, P1; Louwye S, 2000, GEOL MAG, V137, P381, DOI 10.1017/S0016756800004258; Louwye S, 1999, GEOL MIJNBOUW, V78, P31, DOI 10.1023/A:1003793300214; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; MARTINI E, 1973, NEUES JB GEOLOGIE PA, V9, P555; Mudie P.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P587, DOI 10.2973/odp.proc.sr.104.174.1989; NUST H, 1861, B ACAD ROYALE BELGIQ, V12, P198; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Powell A.J., 1992, P155; 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]; SPIEGLER D, 1988, NW EUROPEAN TERTIA A, P152; STRAUSS C, IN PRESS GEOLOGISC A, V111; TAVERNIER R, 1963, MEM SOC BELG GEOL PA, V8, P7; VERBEEK J, 1988, NW EUROPEAN TERTIA A, P267; WILLEMS W, 1988, NW EUROPEAN TERTIA A, P179; Williams Graham L., 1998, AASP Contributions Series, V34, P1; Zevenboom D., 1995, PhD Thesis Diss	43	37	38	1	7	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0072-1050			GEOL J	Geol. J.	JAN-MAR	2002	37	1					55	67		10.1002/gj.900	http://dx.doi.org/10.1002/gj.900			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	528BP					2025-03-11	WOS:000174224000005
J	Nikitenko, BL; Il'ina, VI; Glinskikh, LA				Nikitenko, BL; Il'ina, VI; Glinskikh, LA			Stratigraphy, microfossils, and biofacies in the reference section of Callovian and Upper Jurassic from the Tyumen' superdeep well (<i>West Siberia</i>)	GEOLOGIYA I GEOFIZIKA			Russian	Article						Callovian; Upper Jurassic; stratigraphy; biofacies; community; foraminifers; microforaminifers; dinocysts; zonal scales; eaeustatic Tyumen' superdeep well (SD-6); West Siberia		The Callovian and Upper Jurassic section in the Tyumen' superdeep well SD-6 (West Siberia) drilled with almost continuous recovery of core (about 200 m) and characterized by rich assemblages of microfossils is a unique object for development and improvement of Jurassic regional biostratigraphic schemes of West Siberia based on microfossils. This paper presents results of micropaleontological and palynological research (foraminifers, microforaminifers, ostracods, dinoflagellate cysts, acritarchs, prasinophytes as well as spores and pollen grains of terrestrial plants) and bio- and lithostratigraphic features of the uppermost Middle and Upper Jurassic part of the reference section from the Tyumen' superdeep well. The Vasyugan, Georgievka, and Bazhenov Formations are described in detail, taking into consideration their micropaleontological and palynological characteristics. The structural features of sand productive beds of J(2)(0) and J(1) groups in the Vasyugan Formation and J(1)(0) group at the base of the Georgievka Formation are discussed. Comprehensive lithostratigraphic analysis of Callovian-Upper Jurassic part of the section SD-6 and biostratigraphic data allow us to localize the boundaries of some formations, subformations, and beds in this well, The main regularities of stratigraphic and lateral distribution of Callovian and Upper Jurassic formations as well as their thickness in the Urengoi district and adjacent territories are revealed. Analysis of stratigraphic distribution of microfossil species allow a detailed zonal subdivision of reference section SD-6, with this section being the most complete Jurassic succession In northern West Siberia. The Jurassic regional-scale biostratons were revealed in Siberia according to foraminifers (f-zones), some of them being proposed for West Siberia for the first time. Also for the first time, an almost continuous sequence of dinocyst-based biostratons (dinozones) for Callovian-Middle Volgian has been established in a single section. It may be the basis for the development of Jurassic zonal scale according to dinocysts for West Siberia. Distinctive features of microbenthos communities and microphytoplankton associations reflecting blofacies have been studied. The main regularities of distribution of microbenthic communities and microphytoplankton associations depending on changes of transgressive-regressive events and paleoenvironments in the Callovian-Late Jurassic have been established.	Russian Acad Sci, Inst Petr & Gas Geol, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Nikitenko, BL (通讯作者)，Russian Acad Sci, Inst Petr & Gas Geol, Prosp Koptyuga 3, Novosibirsk 630090, Russia.		Glinskikh, Larisa/Y-8646-2018; Nikitenko, Boris/S-9028-2017	Glinskikh, Larisa/0000-0001-8241-188X				[Anonymous], 1976, STRATIGRAFIYA YURSKO; [Anonymous], 1969, Reference Section of the Upper Jurassic Beds of the Kheta River Basin: Khatanga Depression; DAVIES EH, 1983, GEOL SURV CANADA B, V359; DIKOVSKII AA, 1996, TYUMENSKAYA SVERKHGL, P63; EKHLAKOV YA, 1996, TYUMENSKAYA SVERKHGL, P79; EKHLAKOV YA, 1991, SOV GEOL, P80; Fisher M.J., 1980, P 4 INT PAL C LUCHN, V2, P313; Glinskikh LA, 1999, GEOL GEOFIZ+, V40, P1059; Ilina V.I, 1991, STRATIGRAFIYA PALEOG, P42; ILINA VI, 1998, AKTUALNYE VOPROSY GE, V1, P215; ILINA VI, 1997, BIOSTRATIGRAFIYA NEF, P86; ILYINA VI, 1996, 9 IPC HOUST TEX US; JOHNSON CD, 1973, B CAN PETROL GEOL, V21, P179; KIRICHKOVA AI, 1999, STRATIGRAFIYA GEOLOG, V7, P71; Kontorovich A.E., 1975, Petroleum Geology in West Siberia; KONTOROVICH AE, 2001, SOV TEKT NEOG OBSHCH, V1, P307; Lutova Z.V., 1981, Stratigraphy and Foraminifera of the Callovian of the North of Central Siberia; Meledina S.V., 1998, Stratigrafiya Geologicheskaya Korrelyatsiya, V6, P29; Meledina S.V., 1994, Boreal Middle Jurassic of Russia (Ammonites and Zonal Stratigraphy of the Bajocian, Bathonian, and Callovian; MICKEY M, OIL GAS J, V96, P84; Nikitenko B.L., 2000, STRATIGRAFIYA NEFTEG; PINOUS OV, 1999, MAR PETROL GEOL, P245; Poulsen Niels E., 1993, Acta Geologica Polonica, V43, P251; Riding J.B., 1992, P7; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; RIDING J B, 1984, Palynology, V8, P195; Riding J.B., 1999, AASP Contributions Series, V36; RILEY L A, 1982, Palynology, V6, P193; SHAROVSKAYA NV, 1968, UCHENYE ZAPISKI PALE, P106; Shurygin BN, 1999, GEOL GEOFIZ, V40, P843; SHURYGIN BN, 1995, GEOL GEOFIZ, V36, P324; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; SMELROR M, 1988, RAPP GRONL GEOL UNDE, V137, P135; SMELROR M., 1992, NPF SPECIAL PUBLICAT, P495; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; Woollam R., 1983, 832 I GEOL SCI; ZAKHAROV VA, 1997, GEOL GEOFIZ, V38, P99; 1996, TYUMENSKAYA SVERKHGL; 1972, STRATOGRAFOPALEONTOL; 1991, 5 MEZHV REG STRAT SO; 1990, ATLAS MOLLYUSKOV FOR, V1; 1990, ATLAS MOLLYUSKOV FOR, V2	42	7	11	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.		2002	43	8					762	790						29	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	590WL					2025-03-11	WOS:000177847300005
J	Volkova, VS; Kul'kova, IA; Kuz'mina, OB				Volkova, VS; Kul'kova, IA; Kuz'mina, OB			Palynostratigraphy of Paleogene and Neogene deposits of the Baraba-Kulunda facies zone of West Siberia	GEOLOGIYA I GEOFIZIKA			Russian	Article						dinoflagellates; spores; pollen; formations : Lyulinvor, Tavda, Zhuravka, Abrosimov, Beshcheul' and Tavolga; vegetation; West Siberia		New data are reported to give stratigraphic support for the age of Paleogene marine and Paleogene-Neogene continental deposits exposed in three wells drilled on the Irtysh River near the town of Omsk, West Siberia. According to dinoflagellates and SPA, two formations, Lyulinvor and Tavda, have been recognized as part of the marine Paleogene. On the basis of dinocysts, two zones are established in the Lyulinvor Formation, named after the index species: Dracodinium varielongitudum-D. simile Zone and Charlesdowniea coleopthrypta rotundata-Ch. coelothrypta Zone, corresponding to nannoplankton zones 11-14. The sediments date from the, Lower Eocene-early Middle Eocene (Yprian-lower Lutetian Stages). The marine Tavda Formation also comprises two zones of dinocysts: Rhombodinium draco-Areosphaeridium dictyoplocus, comparable with nannoplankton zones 16-19. The age of the formation is constrained by the late Middle and Late Eocene (upper Lutetian-Barlonlan-Priabonian Stages). The Paleogene and Neogene continental deposits are characterized by eight palynocomplexes, providing support for recognition in wells of the Zhuravka, Abrosimov, Beshcheul', and Tavolga Formations. The development of vegetation is subdivided into three steps: tropical, Turgai, and post-Turgai.	Russian Acad Sci, Siberian Div, Inst Oil & Gas, Novosibirsk 630090, Russia; Novosibirsk Archaeol & Ethnog Inst, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences	Volkova, VS (通讯作者)，Russian Acad Sci, Siberian Div, Inst Oil & Gas, Prosp Koptyuga 3, Novosibirsk 630090, Russia.		Kuzmina, Olga/I-9547-2018					ANDREEVAGRIGORO.AS, 1991, THESIS KIEV; BENYAMOVSKII VN, 1989, GEOL GEOFIZ, P47; Boitsova E.P., 1973, MARINE CONTINENTAL P, P78; BOITSOVA EP, 1964, T VSEGEI, V102, P115; BOITSOVA EP, 1972, THESIS VSEGEI LENING; BOITSOVA EP, 1973, PALINOLOGIYA KAINOFI, P42; BUGROVA EM, 1991, ZONALNAYA STRATIGRAF, P130; CAVELIER C, 1986, B SOC GEOL FR, V2, P255; CHATENEUF J, 1980, B BRQM, V16, P59; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; COSTA LJ, 1988, GEOL JAHR, V10, P508; FREIMAN EV, 1969, T SNIIGGMS, V84, P142; GNIBIDENKO ZN, 1991, GEOL GEOFIZ, P71; GURARI FG, 1959, STRATIGRAFIYA TRETIC, P206; JOANNIDES NS, 1986, GEOL SURV CON, V371, P3; KOROBKOV AI, 1965, THESIS VSEGEI LENING; Kothe A., 1990, GEOL JB A, V118, P3; 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; KULKOVA IA, 1998, MIKROFOSSILII STRATI, P25; LYUBOMIROVA KA, 1976, PALINOLOGICHESKIE IS, V374, P33; LYUBOMIROVA KA, 1971, PALINOLOGIYA NEFTYAN, P66; Martini E., 1971, P 2 PLANKT C ROM 197, P739; MARTYNOV V.A., 2000, STRATIGR GEOL CORREL, V8, P78; NIKITIN VP, 1999, THESIS RAN NOVOSIBIR; NIKOLAEV VA, 1963, KAINOZOI ZAPADNOI, P3; Panova L. A., 1968, PALINOLOGICHESKII ME, P206; Panova L. A., 1971, KAINOZOISKIE FLORY S, P40; PANOVA LA, 1967, THESIS VSEGEI LENING; Podobina V.M., 1998, Foraminifera and Biostratigraphy of the Paleogene of Western Siberia; Shatsky S.B., 1984, SREDA ZHIZN RUBEZHAK, P9; Shatsky S.B., 1978, PALEOGEN NEOGEN SIBI, P3; Vasil'eva O.N., 1990, PALINOLOGIYA STRATIG; VOLKOVA IS, 1988, PALINOLOGIYA SSSR, P31; Volkova VS, 2000, GEOL GEOFIZ, V41, P62; VOLKOVA VS, 1990, 4 IGG SO AN SSSR; VOLKOVA VS, 1996, STRATIGRAFIYA GEOLOG, V4, P83; Vozzhennikova T.F., 1979, Dinocysts and Their Stratigraphic Significance; ZYKIN VS, 1991, EVOLYUTSIYA KLIMATA, P5; Zykin VS., 1982, PROBLEMS STRATIGRAPH, P66; 1999, ZAPADNOI SIBIRI, V1; 1996, GEOLOGICHESKIE BIO 1; 1989, RESHENIE 16 PLENUMA, P51	45	13	22	0	1	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.		2002	43	11					1017	1037						21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	620EA					2025-03-11	WOS:000179519900005
J	Piasecki, S; Gregersen, U; Johannessen, PN				Piasecki, S; Gregersen, U; Johannessen, PN			Lower Pliocene dinoflagellate cysts from cored Utsira Formation in the Viking Graben, northern North Sea	MARINE AND PETROLEUM GEOLOGY			English	Article						dinoflagellate cysts; Lower Pliocene; Utsira Formation; Sleipner field; North Sea	STRATIGRAPHY; UPLIFT; QUANTIFICATION; BASIN	The Utsira Formation covers an area of at least 75 x 450 km(2) with its main, sandy depocentre in the, Here in the Sleipner area, the formation is c. 300 in thick and pinches out to the west, south and east. It consists of unconsolidated, very fine-to medium-grained sand mainly composed of quartz with small amounts of glaucony, shell fragments and lignite, probably deposited by turbidite flows. Earlier biostratigraphical studies of the Utsira Formation have been based on cuttings and the age has been considered to be mainly Late Miocene potentially including latest Middle Miocene and earliest Pliocene. In the present study. core samples from the well 15/9-A23 situated in the Sleipner area have been studied. Dinoflagellate cysts were prepared from seven samples of very fine- to fine-grained sand taken from a core in the interval of 1080.0-1084.99 in. A mixture of Middle and Upper Miocene stratigraphic marker-species indicate significant reworking of older species into younger strata. The main stratigraphical problem is therefore to distinguish reworked species from the in situ flora. The presumed in situ dinoflagellate flora comprises overall Upper Miocene to Pliocene species with relatively few species of precise and clear stratigraphical significance. A single record of Selenopemphix armageddonensis in the lowest sample suggests top Miocene or younger strata. Several dinoflagellate cysts in the assemblage are well known from the Pliocene or even the Pleistocene of the North Atlantic region. Some acritarchs are particularly characteristic of the Pliocene of the northern North Atlantic region. This age is supported by the presence of species such as Hystrichokolpoma rigaudiae and Reticulatosphaera actinocoronata which are reported to range into the Lower Pliocene in the northern North Atlantic region. But the youngest possible age of these samples based on the content of dinoflagellate cysts is strongly dependent on the interpretation of which species that are considered reworked. However Amiculosphaera umbracula, Invertocysta lacrymosa and Ataxiodinium zevenboomii are generally reported to reach stratigraphically not much higher than mid-Pliocene. The age of the cored interval of the Utsira Formation is therefore considered to be Early Pliocene, and this makes a significant part of the formation younger than indicated by previously published biostratigraphic data. (C) 2002 Elsevier Science Ltd. All rights reserved.	Geol Survey Denmark & Greenland, DK-2400 Copenhagen NV, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark.	sp@geus.dk; ugr@gh.gl; pjo@geus.dk	Johannessen, Peter/G-9912-2018; Gregersen, Ulrik/G-9185-2018	Johannessen, Peter/0000-0003-0819-4850; Gregersen, Ulrik/0000-0001-5946-2582				[Anonymous], 1988, Geol. Jahrbuch, Reihe A; Chadwicks RA, 2001, GREENHOUSE GAS CONTROL TECHNOLOGIES, P349; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A., 1989, P OCEAN DRILLING PRO, V105, P387, DOI DOI 10.2973/0DP.PR0C.SR.105.133.1989; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; EDWARDS JW, 1984, CULT MED PSYCHIAT, V8, P1, DOI 10.1007/BF00053099; Eidvin T, 1999, NORSK GEOL TIDSSKR, V79, P97, DOI 10.1080/002919699433843; Eidvin T, 2000, MAR PETROL GEOL, V17, P579, DOI 10.1016/S0264-8172(00)00008-8; FYFE A, 2002, MILLENIUM ATLAS PETR, pCH16; GALLOWAY WE, 1993, PETROLEUM GEOLOGY OF NORTHWEST EUROPE: PROCEEDINGS OF THE 4TH CONFERENCE, P33, DOI 10.1144/0040033; GHAZI SA, 1992, NORSK GEOL TIDSSKR, V72, P285; Gregersen U, 1997, MAR PETROL GEOL, V14, P893, DOI 10.1016/S0264-8172(97)00036-6; GREGERSEN U, 2000, 62 EAGE C TECHN EXH; Hansen S, 1996, NORSK GEOL TIDSSKR, V76, P245; Hardenbol J., 1998, MESOZOIC CENOZOIC SE; 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.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; HEAD MJ, 1999, PALYNOLOGY; Isaksen D., 1989, NPD B, V5, P1; Japsen P, 2000, GLOBAL PLANET CHANGE, V24, P165, DOI 10.1016/S0921-8181(00)00006-0; JORDT H, 1995, MAR PETROL GEOL, V12, P845, DOI 10.1016/0264-8172(95)98852-V; LENTIN JK, 1994, CAN J EARTH SCI, V31, P567, DOI 10.1139/e94-050; Louwye S, 1999, REV PALAEOBOT PALYNO, V107, P109, DOI 10.1016/S0034-6667(99)00012-3; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; MANGERUD G, 1999, SEDIMENTARY ENV OFFS; 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; Martinsen N., 1999, PETROLEUM GEOLOGY NW, P293, DOI DOI 10.1144/0050293; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Powell A.J., 1992, P155; Riis F, 1996, GLOBAL PLANET CHANGE, V12, P331, DOI 10.1016/0921-8181(95)00027-5; Riis F., 1992, Structural and Tectonic Modelling and its Application to Petroleum Geology, V1, P163, DOI [10.1016/B978-0-444-88607-1.50016-4, DOI 10.1016/B978-0-444-88607-1.50016-4]; Rundberg Y., 1989, Unpubl. Ph. D. Thesis; Smelror Morton, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P83; WILKINSON IP, 1999, WH99124R BRIT GEOL S; Zevenboom D, 1995, THESIS U UTRECHT UTR	38	28	28	0	6	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0264-8172	1873-4073		MAR PETROL GEOL	Mar. Pet. Geol.	JAN	2002	19	1					55	67	PII S0264-8172(01)00053-8	10.1016/S0264-8172(01)00053-8	http://dx.doi.org/10.1016/S0264-8172(01)00053-8			13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	539LH					2025-03-11	WOS:000174871200004
J	Springer, JJ; Shumway, SE; Burkholder, JM; Glasgow, HB				Springer, JJ; Shumway, SE; Burkholder, JM; Glasgow, HB			Interactions between the toxic estuarine dinoflagellate <i>Pfiesteria piscicida</i> and two species of bivalve molluscs	MARINE ECOLOGY PROGRESS SERIES			English	Article						Argopecten irradians; Crassostrea virginica; oyster; Pfiesteria; scallop; shellfish; temporary cyst; toxic dinoflagellate	RAT PITUITARY-CELLS; PROTOGONYAULAX-TAMARENSIS; CRASSOSTREA-VIRGINICA; BEHAVIOR; MANAGEMENT; SHUMWAYAE; RECEPTOR; IMPACTS; SCIENCE; COMPLEX	Toxic strains of Phesteria spp. produce toxin(s) that can cause finfish death, but much less is known about impacts of Phesteria on shellfish. Here we conducted 4 experiments to examine interactions between shellfish and toxic (actively toxic or TOX-A from finfish-killing cultures and potentially toxic or TOX-B from cultures without finfish) and non-inducible (NON-IND, apparently incapable of killing fish via a toxic effect) strains of P. piscicida. First (Expt 1), we documented direct physical attack by P. piscicida TOX-A, TOX-B, and NON-IND zoospores on larvae of the bay scallop Argopecten irradians (Lamarck, 1819) and the eastern oyster Crassostrea virginica (Gmelin, 1791). Within 5 min zoospores swarmed around larvae that had discarded their vela, and attached with their peduncles. Within 15 min they had penetrated into the shellfish visceral cavity and had begun to feed aggressively; after 30 min all shellfish tissues except the adductor muscle had been consumed. Second, we tested the response of scallop larvae to P. piscicida (TOX-A or TOX-B) or. cryptomonads (as controls) that were held in dialysis tubing (0.22 mum porosity) to prevent direct contact. After 60 min larval survival was 0% in the TOX-A treatment, 100% in the cryptomonad control, and intermediate in TOX-B and TOX-B+ cryptomonad treatments. The data indicate a toxic effect of P. piscicida zoospores on the larvae, separate from the physical effect shown in Expt 1. Third, we compared grazing by juvenile and adult oysters on TOX-A, TOX-B, and NON-IND P. piscicida zoospores from the medium. After 60 min, grazing by juvenile oysters significantly differed as NON-IND TOX-B TOX-A. In contrast, adult oysters grazed significantly fewer TOX-A zoospores and maintained comparable grazing on TOX-B and NON-IND zoospores. Thus juvenile oysters, but not adults, were sensitive to residual toxicity of TOX-B zoospores, and both life-history stages were sensitive to TOX-A zoospores. The adverse effects of toxic strains on larval survival and juvenile grazing indicate that P. piscicida could potentially affect shellfish recruitment. Fourth, we assessed zoospore survival after passage through the digestive tract of adult oysters. The feces contained many temporary cysts from zoospores, and within 24 h > 75 % of the cysts produced motile cells. The data indicate that adult oysters would be poor biocontrol agents of P. piscicida, given the high survival of ingested zoospores following gut passage and fecal elimination; and that oysters could act as vectors of toxic P. piscicida strains if transported from affected estuaries to other waters.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA; Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA	North Carolina State University; University of Connecticut	N Carolina State Univ, Ctr Appl Aquat Ecol, 620 Hutton St,Suite 104, Raleigh, NC 27606 USA.							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Ecol.-Prog. Ser.		2002	245						1	10		10.3354/meps245001	http://dx.doi.org/10.3354/meps245001			10	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	637UC		Bronze			2025-03-11	WOS:000180531300001
J	Seo, KS; Fritz, L				Seo, KS; Fritz, L			Ultrastructure of vegetative cysts of <i>Pyrocystis</i> (Dinophyta), with special reference to PAS bodies and trichocysts	PHYCOLOGIA			English	Article							LOCALIZATION; GONYAULAX; NOCTILUCA	The ultrastructure of two dinoflagellates. the lunate Pyrocystis lunula and the spherical Pyrocystis noctiluca, is described scanning electron microscopy and transmission electron microscopy, with an emphasis using fluorescence microscopy. cryo-scanning electron microscopy and transmission electron microscopy, with an emphasis on periodic acid-Schiff reagent (PAS) bodies and trichocysts. Seen in section. the cytoplasm of Pyrocystis cells is separated into two distinct areas: a core area and a peripheral area. The core area contains most of the cellular organelles, including the PAS bodies. Trichocysts exist in both species, even though the cyst wall contains no pores for ejection. A possible role of trichocysts in dinoflagellate cysts is discussed.	No Arizona Univ, Dept Biol Sci, Flagstaff, AZ 86011 USA	Northern Arizona University	Natl Sci Fdn, 4201 Wilson Blvd, Arlington, VA 22230 USA.	lfritz@nsf.gov						BEHRMANN G, 1995, PROTOPLASMA, V185, P22, DOI 10.1007/BF01272750; BOUCK GB, 1966, PROTOPLASMA, V61, P205, DOI 10.1007/BF01247920; Bozzola J.J., 1992, ELECTRON MICROS; BULLOCK GR, 1984, J MICROSC-OXFORD, V133, P1, DOI 10.1111/j.1365-2818.1984.tb00458.x; Dodge J. D., 1973, FINE STRUCTURE ALGAL; Dodge JD., 1987, The Biology of Dinoflagellates, P92; ELBRACHTER M, 1978, HELGOLAND WISS MEER, V31, P347, DOI 10.1007/BF02189487; ELBRACHTER M, 1987, BOT MAR, V30, P233, DOI 10.1515/botm.1987.30.3.233; Fensome R.A., 1993, Micropaleontology Press Special Paper; Hausmann K., 1996, PROTOZOOLOGY, P338; Horiguchi Takeo, 1995, Phycological Research, V43, P129, DOI 10.1111/j.1440-1835.1995.tb00016.x; Hunter E., 1993, PRACTICAL ELECT MICR; LIVOLANT F, 1982, BIOL CELL, V43, P217; Maranda L, 1996, J PHYCOL, V32, P873, DOI 10.1111/j.0022-3646.1996.00873.x; MESSER G, 1971, J ULTRA MOL STRUCT R, V37, P94, DOI 10.1016/S0022-5320(71)80043-6; NICOLAS MT, 1987, J CELL SCI, V87, P189; PINCEMIN JM, 1982, ARCH PROTISTENKD, V125, P95, DOI 10.1016/S0003-9365(82)80009-2; SCHMITTER RE, 1981, J CELL SCI, V51, P15; Seo K.S., 2000, Ultrastructure and life cycle of two vegetative forming dinoflagellates: Pyrocystis lunula and pyrocystis noctiluca; 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; SWEENEY BM, 1979, J PHYCOL, V15, P23; SWEENEY BM, 1979, BIOL DINOFLAGELLATES, P269; SWIFT E, 1973, Phycologia, V12, P90, DOI 10.2216/i0031-8884-12-1-90.1; SWIFT E, 1973, J PHYCOL, V9, P420, DOI 10.1111/j.0022-3646.1973.00420.x; TAYLOR DL, 1968, J MAR BIOL ASSOC UK, V48, P349, DOI 10.1017/S0025315400034548; TROMMER G, 1985, ELECTRON LETT, V21, P458, DOI 10.1049/el:19850325; ZHOU J, 1994, J PHYCOL, V30, P39, DOI 10.1111/j.0022-3646.1994.00039.x	29	6	6	1	10	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	JAN	2002	41	1					10	14		10.2216/i0031-8884-41-1-10.1	http://dx.doi.org/10.2216/i0031-8884-41-1-10.1			5	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	534NG					2025-03-11	WOS:000174592000002
C	Wendler, I; Zonneveld, KAF; Willems, H		Clift, PD; Kroon, D; Gaedicke, C; Craig, J		Wendler, I; Zonneveld, KAF; Willems, H			Calcareous cyst-producing dinoflagellates: ecology and aspects of cyst preservation in a highly productive oceanic region	TECTONIC AND CLIMATIC EVOLUTION OF THE ARABIAN SEA REGION	Geological Society Special Publication		English	Proceedings Paper	Meeting of the Geological-Society-of-London	APR 04-05, 2001	PICCADILLY, ENGLAND	Geol Soc London, Tecton Studies, Geol Soc London, Marine Studies, Geol Soc London, Petr Grp			EQUATORIAL ATLANTIC-OCEAN; UPPER WATER COLUMN; NORTHWESTERN INDIAN-OCEAN; NORTHEASTERN ARABIAN SEA; OXYGEN MINIMUM ZONE; MIXED-LAYER DEPTH; SURFACE SEDIMENTS; THORACOSPHAERA-HEIMII; SOUTHWEST MONSOON; LATE QUATERNARY	Absolute and relative abundances of calcareous dinoflagellate cyst species in surface sediment samples from the Arabian Sea are compared with environmental parameters of the upper 100 m of the water column to gain information on their largely unknown autecology Ten species or morphotypes were encountered of which four occurred only as accessories. On the basis of the distribution patterns of the six more abundant species or morphotypes, the studied area is subdivided into three provinces, demonstrating a clear relationship to monsoon-controlled upper-ocean conditions. The two dominant species, Thoracosphaera heimii and Orthopithonella granifera, show opposite trends in distribution of both their absolute and relative abundances. In the NE Arabian Sea, low absolute and relative abundances of T heimii are mainly attributed to enhanced dissolution of the small tests in this region, whereas elevated concentrations of O. granifera seem to be related to higher water temperatures and the influence of the Indus River. Sphaerodinella albatrosiana and Calciodinellum operosum are most abundant in the open ocean, associated with lower nutrient levels, relatively high temperatures and low seasonality. Spiny cysts (mainly represented by Scrippsiella trochoidea), in contrast, exhibit a more shelf-ward distribution and are most abundant in regions that are influenced by coastal upwelling, characterized by eutrophic and rather unstable conditions with seasonally lower temperatures and a shallow thermocline. A generally negative correlation of calcareous dinoflagellate cysts with primary productivity or high nutrient concentrations, as proposed by other workers, cannot be confirmed. Cyst accumulation rates off Somalia show that strong turbulence and high current speeds are unfavourable for calcareous dinoflagellates, suggesting that these organisms are more successful under rather stratified conditions.	Univ Bremen, FB 5, D-28334 Bremen, Germany	University of Bremen		flatter@uni-bremen.de						Allen W. 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Soc. Spec. Publ.		2002	195						317	340		10.1144/GSL.SP.2002.195.01.17	http://dx.doi.org/10.1144/GSL.SP.2002.195.01.17			24	Geology; Geosciences, Multidisciplinary; Oceanography	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Oceanography	BW43W					2025-03-11	WOS:000181985300017
J	Peña-Manjarrez, JL; Gaxiola-Castro, G; Helenes-Escamilla, J; Orellana-Cepeda, E				Peña-Manjarrez, JL; Gaxiola-Castro, G; Helenes-Escamilla, J; Orellana-Cepeda, E			Cysts of <i>Lingulodinium polyedrum</i>, red tide producing organism in the Todos Santos Bay (winter-spring, 2000)	CIENCIAS MARINAS			English	Article						dinoflagellates; cysts; red tide; blooms; Todos Santos Bay	GONYAULAX-TAMARENSIS; SCRIPPSIELLA	Dinoflagellate cysts with dinosporin walls were identified for the first time in samples collected at Todos Santos Bay, Baja California, Mexico, during winter-spring 2000. Eighteen neritic species characteristic of temperate to temperate-cool neritic regions were identified, mainly from the Gonyaulacaceae and Congruentidiaceae families. The cysts were concentrated in the coastal zone, at depths shallower than 25 m, associated with surface fine sediments. Lingulodinium polyedrum (Stein) Dodge was the dominant species in both the sediments and in the water column, producing spring and summer red tides in the area.	Ctr Invest Cient & Educ Super Ensenada, Dept Ecol, Ensenada, Baja California, Mexico; Ctr Invest Cient & Educ Super Ensenada, Dept Geol, Ensenada, Baja California, Mexico; Univ Autonoma Baja California, Fac Ciencias Marinas, Ensenada, Baja California, Mexico; Direcc Gen Educ Ciencia & Tecnol Mar, Secretaria Educ Publ, Mexico City 06090, DF, 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	Peña-Manjarrez, JL (通讯作者)，Ctr Invest Cient & Educ Super Ensenada, Dept Ecol, Km 107,Carretera Tijuana Ensenada, Ensenada, Baja California, Mexico.		Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879				Anderson D.M., 1985, P219; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1995, MANUAL HARMFUL MARIN, P229; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; CEMBELLA AD, 1998, ALGAL BLOOMS, P649; GREGORIO ED, 2000, B SO CALIFORNIA ACAD, V99, P147; Head M.J., 1996, Palynology: Principles and Applications, P1197; HOLMES RW, 1967, LIMNOL OCEANOGR, V12, P503, DOI 10.4319/lo.1967.12.3.0503; Kahru M, 1998, J GEOPHYS RES-OCEANS, V103, P21601, DOI 10.1029/98JC01945; Kimor B., 1981, California Cooperative Oceanic Fisheries Investigations Reports, V22, P126; Kokinos John P., 1995, Palynology, V19, P143; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; MARTINEZHERNAND.E, 1991, PALEONTOLOGIA MEXICA, V57; Matsuoka K., 1985, NATURAL SCI B, V25, P21; MONTIEL NM, 1998, THESIS UABC FCM ENSE; MOREYGAINES G, 1981, USC SEA GRANT PUBLIC; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; ORELLANACEPEDA E, 1999, 4 C LAT MAL COQ CHIL; ORELLANACEPEDA E, 1993, 6 INT C TOX MAR PHYT, P152; ROCHON A, 1999, PALYNOLOGYSTS FDN CO, V35; Sgrosso S, 2001, MAR ECOL PROG SER, V211, P77, DOI 10.3354/meps211077; SUTHERLAND TF, 1992, J PLANKTON RES, V14, P915, DOI 10.1093/plankt/14.7.915; SWEENEY BM, 1975, P 1 INT C TOX DIN BL, P225; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; WOOD GD, 1996, AM ASS STRATIGRAPHIC, V1, P29	28	13	14	0	10	INSTITUTO INVESTIGACIONES OCEANOLOGICAS, U A B C	BAJA CALIFORNIA	APARTADO POSTAL 423, ENSENADA, BAJA CALIFORNIA 22800, MEXICO	0185-3880			CIENC MAR	Ceinc. Mar.	DEC	2001	27	4					543	558						16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	498XR					2025-03-11	WOS:000172539300004
J	Ichimi, K; Montani, S				Ichimi, K; Montani, S			Effects of deposit feeder ingestion on the survival and germination of marine flagellate cysts	FISHERIES SCIENCE			English	Article						benthos; cyst; deposit feeder; flagellate; germination	PARTICLE-SIZE SELECTION; GONYAULAX-TAMARENSIS; DINOFLAGELLATE CYSTS; SEDIMENT REWORKING; BLOOMS		Kagawa Univ, Fac Agr, Kagawa 7610795, Japan	Kagawa University	Ichimi, K (通讯作者)，Kagawa Univ, Fac Agr, Kagawa 7610795, Japan.							Anderson D.M., 1985, P219; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; 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; CADEE GC, 1979, NETH J SEA RES, V13, P441, DOI 10.1016/0077-7579(79)90017-6; FENCHEL T, 1975, MAR BIOL, V30, P119, DOI 10.1007/BF00391586; HYLLEBERG J, 1975, MAR BIOL, V32, P167, DOI 10.1007/BF00388509; Imai I, 1990, B NANSEI NATL FISH R, V23, P63; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; POWELL EN, 1977, INT REV GES HYDROBIO, V62, P385, DOI 10.1002/iroh.1977.3510620305; Rhoads D.C., 1974, Oceanography mar Biol, V12, P263; RISK MJ, 1977, J SEDIMENT PETROL, V47, P1425; TAKEUCHI T, 1990, Bulletin of Plankton Society of Japan, V37, P157; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	16	9	10	2	6	JAPANESE SOC FISHERIES SCIENCE	TOKYO	C/O TOKYO UNIV FISHERIES, KONAN 4, MINATO, TOKYO, 108-8477, JAPAN	0919-9268			FISHERIES SCI	Fish. Sci.	DEC	2001	67	6					1178	1180		10.1046/j.1444-2906.2001.00378.x	http://dx.doi.org/10.1046/j.1444-2906.2001.00378.x			3	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	505ZF		Bronze			2025-03-11	WOS:000172944900025
J	Marret, F; Scourse, JD; Versteegh, G; Jansen, JHF; Schneider, R				Marret, F; Scourse, JD; Versteegh, G; Jansen, JHF; Schneider, R			Integrated marine and terrestrial evidence for abrupt Congo River palaeodischarge fluctuations during the last deglaciation	JOURNAL OF QUATERNARY SCIENCE			English	Article						Congo; ITCZ; palynology; precipitation; tropical climate change	EAST EQUATORIAL ATLANTIC; ICE-CORE RECORD; LATE PLEISTOCENE; LATE QUATERNARY; OCEAN CIRCULATION; CLIMATIC CHANGES; ORGANIC-MATTER; WEST-AFRICA; SEDIMENTS; EVENT	We present a high-resolution reconstruction of tropical palaeoenvironmental changes for the last deglacial transition (18 to 9 cal. kyr BP) based on integrated oceanic and terrestrial proxies from a Congo fan core. Pollen, grass cuticle, Pediastrum and dinoflagellate cyst fluxes, sedimentation rates and planktonic foraminiferal delta O-18 ratios, u(87)(K); sea-surface temperature and alkane/alkenone ratio data highlight a series of abrupt changes in Congo River palaeodischarge. A major discharge pulse is registered at around 13.0 cal, kyr BP which we attribute to latitudinal migration of the Intertropical Convergence Zone (ITCZ) during deglaciation. The data indicate abrupt and short-lived changes in the equatorial precipitation regime within a system of monsoonal dynamics forced by precessional cycles. The phases of enhanced Congo discharge stimulated river-induced upwelling and enhanced productivity in the adjacent ocean. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales; Netherlands Inst Sea Res, NIOZ, NL-1790 AB Den Burg, Texel, Netherlands; Univ Bremen, D-28334 Bremen, Germany	Bangor University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bremen	Marret, F (通讯作者)，Univ Wales Bangor, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales.		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Quat. Sci.	DEC	2001	16	8					761	766		10.1002/jqs.646	http://dx.doi.org/10.1002/jqs.646			6	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	506VE		Bronze			2025-03-11	WOS:000172991800002
J	Matthiessen, J; Knies, J; Nowaczyk, NR; Stein, R				Matthiessen, J; Knies, J; Nowaczyk, NR; Stein, R			Late Quaternary dinoflagellate cyst stratigraphy at the Eurasian continental margin, Arctic Ocean: indications for Atlantic water inflow in the past 150,000 years	GLOBAL AND PLANETARY CHANGE			English	Article; Proceedings Paper	Annual QUEEN Workshop	APR, 2000	LUND, SWEDEN			Eastern Arctic Ocean; Late Quaternary; stratigraphy; stable oxygen isotopes; magnetostratigraphy; paleomagnetic excursions; dinoflagellate cysts	POLAR NORTH-ATLANTIC; LAST-GLACIAL-MAXIMUM; SEA-ICE SHEET; DEPOSITIONAL ENVIRONMENT; FRAM STRAIT; LAPTEV SEA; FORAMINIFERAL STRATIGRAPHY; GEOMAGNETIC EXCURSIONS; LATE PLEISTOCENE; SEDIMENT CORES	Four sediment cores located at the Eurasian continental margin underlying the Atlantic layer have been studied for their dinoflagellate cyst content. Concentrations of distinct dinoflagellate cyst taxa display fluctuations in the late Quaternary, which are linked to changes in the inflow of relatively warm Atlantic surface and near-surface waters, resulting in increased local production of cysts in certain time intervals. Based on the assumption that marked changes in strength of inflow occurred synchronously at the Eurasian continental margin, concentration maxima can be used to correlate sediment cores. A dinoflagellate cyst record from the northern Barents Sea continental margin has been related to the stable oxygen isotope and paleomagnetic records to provide direct chronological information. The combination of these methods permits definition of stratigraphic sections equivalent to oxygen isotope stages in carbonate-poor sequences from the Eurasian continental margin. Previous age models of sediment cores are revised, based on dinoflagellate cyst abundance peaks and species distribution, but a firm chronostratigraphy of sedimentary sequences at the eastern Laptev Sea continental margin cannot be established because of the weak signal at the sites furthest from Fram Strait. In the past 150,000 years, the influence of Atlantic (sub-) surface waters generally decreased from west to east along the Eurasian continental margin, in particular during the glacials. Pronounced concentration maxima of cosmopolitan and temperate-subpolar dinoflagellate cysts indicate the inflow of Atlantic waters and seasonally increased production of cysts in the Holocene and Eemian. The Holocene is well-marked at the entire Eurasian continental margin but it is more difficult to assess the extent of (sub-) surface water inflow during the Eemian, which may have only reached the western Laptev Sea continental margin. (C) 2001 Elsevier Science B.V. All rights reserved.	Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; Geoforschungszentrum Potsdam, Projektbereich Sedimente & Beckenbildung 3 3, D-14473 Potsdam, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences	Matthiessen, J (通讯作者)，Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany.			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Planet. Change	NOV	2001	31	1-4			SI		65	86		10.1016/S0921-8181(01)00113-8	http://dx.doi.org/10.1016/S0921-8181(01)00113-8			22	Geography, Physical; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	511LR					2025-03-11	WOS:000173265800005
J	Levac, E				Levac, E			High resolution Holocene palynological record from the Scotian Shelf	MARINE MICROPALEONTOLOGY			English	Article						palynology; Holocene; dinoflagellate cysts; pollen; transfer functions; paleoceanography	WESTERN NORTH-ATLANTIC; CONTINENTAL-MARGIN; MARINE-SEDIMENTS; EMERALD BASIN; ST-LAWRENCE; POLLEN; DINOFLAGELLATE; SEA; TERRESTRIAL; CIRCULATION	Because of their location at the confluence of polar and subtropical airmasses and near a transition zone between the cold Labrador Current and the Gulf Stream, the Atlantic Provinces experience some of the most dynamic climate conditions in Canada. Major climate changes occurred during the Holocene, as shown by pollen records from takes, but previous paleoceanographic studies. based on low-resolution proxy-data records do not show major changes during the past 8000 years. Therefore, the Holocene history of Canada's Atlantic region was examined using a high-resolution palynological record from the Scotian Shelf (La Have Basin). Sea surface conditions were reconstructed using proxy-data from dinoflagellate cysts and paleobioclimatic transfer functions. Ocean-atmosphere interactions are determined by onshore-offshore correlation of marine and pollen records from Nova Scotia. Results show a succession of major paleoceanographic events. Sea surface temperatures (SST) (February and August) up to 5 degreesC higher than today's average and slightly higher salinity are reconstructed between 10.5 and 8.5 ka. The last pulse of meltwater from the residual ice sheet affected the shelf waters between 8.5 and 6.5 ka by lowering the SST (in February) and the salinity. Most previous studies failed to record this event. Since 6.5 ka, August temperature generally remained around today's value. while February temperature was generally 2 degreesC above it. except for recurring colder and lower salinity intervals. These cold intervals have a recurrence of about 1000 years. A slight cooling of summer SST is recorded in the last 500 years. Comparison with climatic reconstructions from Nova Scotia pollen records shows a difference in timing between ocean and atmosphere. The onset of the climatic optimum (hypsithermal) in Nova Scotia lags by about 2000 years (until 8 ka) relative to the ocean but it lasted longer. The Neoglacial cooling in Atlantic Canada however, started earlier (2 ka) than the late Holocene ocean cooling. La Have Basin's Holocene paleoceanography presents some differences from most other studies from the region: (1) the hypsithermal started earlier; (2) the last pulse of meltwater is recorded; (3) the last 6500 years are punctuated by colder intervals. Increased productivity and blooms of toxic algae in the early Holocene are probably due to a combination of factors: increased nutrients and a greater stability of the water column because of meltwaters, higher SST and increased upwelling or storm activity. (C) 2001 Elsevier Science B.V. All rights reserved.	Dalhousie Univ, Ctr Marine Geol, Halifax, NS B3H 3J5, Canada	Dalhousie University	Dalhousie Univ, Ctr Marine Geol, Halifax, NS B3H 3J5, Canada.	elevac@is2.dal.ca						AMOS CL, 1991, CONT SHELF RES, V11, P1037, DOI 10.1016/0278-4343(91)90090-S; Anderson C., 1987, Science Review 1987, Research, P25; ANDERSON PM, 1988, SCIENCE, V241, P1043, DOI 10.1126/science.241.4869.1043; Anderson T.W., 1985, Pollen records of Late-Quaternary North American sediments, P281; BALSAM W, 1981, PALAEOGEOGR PALAEOCL, V35, P215, DOI 10.1016/0031-0182(81)90098-5; BALSAM WL, 1976, MAR GEOL, V21, P121, DOI 10.1016/0025-3227(76)90053-0; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; BUCKLEY DE, 1991, CONT SHELF RES, V11, P1099, DOI 10.1016/0278-4343(91)90093-L; CAMPBELL C, 1999, THESIS ST MARYS U HA; CARRETO JI, 1986, J PLANKTON RES, V8, P15, DOI 10.1093/plankt/8.1.15; DAVIS RB, 1975, QUATERNARY RES, V5, P395, DOI 10.1016/0033-5894(75)90040-X; DE VERNAL A, 1992, GEOLOGY, V20, P527, DOI 10.1130/0091-7613(1992)020<0527:QAOCDI>2.3.CO;2; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; DEVERNAL A, 1992, NEOGENE QUATERNARY D, P298; DRINKWATER KF, 1999, 199 HYDR OC SCI; Edgecombe RB, 1999, CAN J EARTH SCI, V36, P805, DOI 10.1139/e99-083; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; *ENV CAN, 1984, CLIM ATL CAN SER MAP; *ENV CAN, 1989, EC LAND CLASS SER, V23, P118; Fensome RA, 1998, TAXON, V47, P695, DOI 10.2307/1223586; FILLON RH, 1976, MAR GEOL, V20, P7, DOI 10.1016/0025-3227(76)90072-4; Gajewski K, 2000, CAN J EARTH SCI, V37, P661, DOI [10.1139/cjes-37-5-661, 10.1139/e99-065]; GREEN DG, 1985, CAN J BOT, V65, P1163; GUIOT J, 1990, INSU MONOGRAPHIE, V1, P253; Hare FK, 1997, CAG CAN G, P3; KEIGWIN LD, 1995, PALEOCEANOGRAPHY, V10, P973, DOI 10.1029/95PA02643; King L.H., 1986, Bulletin, V363, DOI [10.4095/120601, DOI 10.4095/120601]; Kutzbach J. 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Micropaleontol.	NOV	2001	43	3-4					179	197		10.1016/S0377-8398(01)00033-0	http://dx.doi.org/10.1016/S0377-8398(01)00033-0			19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	493JL					2025-03-11	WOS:000172218900001
J	McMinn, A; Howard, WR; Roberts, D				McMinn, A; Howard, WR; Roberts, D			Late Pliocene dinoflagellate cyst and diatom analysis from a high resolution sequence in DSDP Site 594, Chatham Rise, south west Pacific	MARINE MICROPALEONTOLOGY			English	Article						pliocene; dinoflagellate; diatom; Chatham Rise; DSDP Site 594	CANONICAL CORRESPONDENCE-ANALYSIS; NORTHERN-HEMISPHERE GLACIATION; SEA-SURFACE TEMPERATURE; ATLANTIC OCEAN; SINGA SECTION; SEDIMENTS; AUSTRALIA; CARBONATE; EVOLUTION; CLIMATE	A high resolution mixed carbonate and siliciclastic sequence from DSDP Site 594 contains a detailed record of climate change in the late Pliocene. The sequence can be accurately dated by the LAD of Nitzschia weaveri, the LAD of Thalassiosira insigna. the LAD of T. vulnifica and the LAD of T. kolbei diatom datums. Carbonate content and delta (18) signatures provide added resolution and place the sequence between isotope stages 100 and 9. The sequence contains well-preserved and diverse dinoflagellate cyst floras. Use of principal component (PCA) and canonical correspondence analyses (CCA) identifies changes in the assemblages that principally reflect warming and cooling trends. Species associated with warmer climates included Impagidinium patulum, I. paradoxum and I sp. cf. paradoxum while those from cooler climates include Invertecysta tabulata and I. velorum. CCA is shown to be a valuable method of determining the past environmental preferences of extinct species such as I. tabulata. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia; Univ Tasmania, Antartic CRC, Hobart, Tas 7001, Australia	University of Tasmania; University of Tasmania	McMinn, A (通讯作者)，Univ Tasmania, Inst Antarctic & So Ocean Studies, Box 252C, Hobart, Tas 7001, Australia.		McMinn, Andrew/A-9910-2008	Roberts, Donna/0000-0001-6701-6662				BARTON CE, 1986, INITIAL REP DEEP SEA, V90, P1273, DOI 10.2973/dsdp.proc.90.136.1986; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; CIESIELSKI PF, 1986, INITIAL REP DEEP SEA, V90, P863; Cronin TM, 1996, GEOLOGY, V24, P695, DOI 10.1130/0091-7613(1996)024<0695:PMOFCA>2.3.CO;2; DEMENOCAL PB, 1995, SCIENCE, V270, P53, DOI 10.1126/science.270.5233.53; DOWSETT HJ, 1990, MAR MICROPALEONTOL, V16, P1, DOI 10.1016/0377-8398(90)90026-I; EDWARDS L E, 1982, Palynology, V6, P105; EDWARDS LE, 1991, QUATERNARY SCI REV, V10, P259, DOI 10.1016/0277-3791(91)90024-O; EDWARDS LE, 1984, INITIAL REP DEEP SEA, V81, P581; EDWARDS LE, 1992, AM ASS STRATIGR PALY; Fenner J.M., 1991, Proceedings of the Ocean Drilling Program, Scientific Results, V114, P97, DOI DOI 10.2973/ODP.PROC.SR.114.133.1991; Gersonde R, 1998, MICROPALEONTOLOGY, V44, P84, DOI 10.2307/1486086; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Harwood D.M., 1992, PROC OCEAN DRILL SCI, V120, P683, DOI [10.2973/odp.proc.sr.120.160.1992, DOI 10.2973/ODP.PROC.SR.120.160.1992]; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P423, DOI 10.2973/odp.proc.sr.105.135.1989; Head MJ, 1999, J PALEONTOL, V73, P1; Head MJ, 1998, GEOL MAG, V135, P803, DOI 10.1017/S0016756898001745; HEAD MJ, 1998, AAPG BULL, V82, P10; HEAD MJ, 1999, DAWN QUATERNARY, P199; HODELL DA, 1991, QUATERNARY SCI REV, V10, P205, DOI 10.1016/0277-3791(91)90019-Q; JONES GA, 1983, J SEDIMENT PETROL, V53, P655, DOI 10.1306/212F825B-2B24-11D7-8648000102C1865D; JUGGINS S, 1994, CALIBRATE PROGRAM SP; King AL, 2000, GEOLOGY, V28, P659, DOI 10.1130/0091-7613(2000)028<0659:MPSSTC>2.3.CO;2; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Maslin MA, 1998, QUATERNARY SCI REV, V17, P411, DOI 10.1016/S0277-3791(97)00047-4; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; McMinn A., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V123, P429, DOI 10.2973/odp.proc.sr.123.120.1992; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; McMinn A, 1997, MAR MICROPALEONTOL, V29, P407, DOI 10.1016/S0377-8398(96)00012-6; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; MCMINN A, 1994, P ODP SCI RESULTS, V133, P93; MCMINN A, 1994, P ODP SCI RESULTS, V133, P97; McMinn A., 1992, NEOGENE QUATERNARY D, P147; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; NELSON CS, 1985, INITIAL REPORTS DEEP, V90, P1425; Powell A.J., 1986, AASP Contrib. 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Micropaleontol.	NOV	2001	43	3-4					207	221		10.1016/S0377-8398(01)00026-3	http://dx.doi.org/10.1016/S0377-8398(01)00026-3			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	493JL					2025-03-11	WOS:000172218900003
J	Ellegaard, M; Dale, B; Amorim, A				Ellegaard, M; Dale, B; Amorim, A			The acritarchous resting cyst of the athecate dinoflagellate <i>Warnowia</i> cf. <i>rosea</i> (Dinophyceae)	PHYCOLOGIA			English	Article							MARINE-SEDIMENTS; ALEXANDRIUM	Cysts of the athecate dinoflagellate Warnowia cf. rosea were found in surface sediment samples from the Norwegian coast near Bergen and from the coast of Portugal. The cyst has not been described before and is acritarch-like, in that the germination opening. a simple median split, is identical to chasmic openings found in fossil acritarchs, The cyst is 30-45 by 28-43 mum and light brown with irregular tufts of darker brown material and fused darker brown processes. The cyst often disintegrates rapidly after germination, and it is destroyed by palynological processing, Such a cyst would not be expected to persist in the fossil record. Nevertheless. its morphology supports the idea that athecate dinoflagellates Lire represented by acritarchs in the older geological record, predating the first morphologically identifiable dinoflagellate cysts.	Univ Copenhagen, Inst Bot, Dept Phycol, DK-1353 Copenhagen K, Denmark; Univ Oslo, Inst Geol, N-0316 Oslo 3, Norway; Univ Lisbon, Fac Ciencias, Inst Oceanog, P-1749016 Lisbon, Portugal	University of Copenhagen; University of Oslo; Universidade de Lisboa	Univ Copenhagen, Inst Geog, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	me@geogr.ku.dk	Ellegaard, Marianne/H-6748-2014; Amorim, Ana/AAA-2615-2020	Amorim, Ana/0000-0002-9612-4280				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; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Doblin MA, 1999, J PLANKTON RES, V21, P1153, DOI 10.1093/plankt/21.6.1153; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; FUKUYO Y, 1982, 148R14 B, P205; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; HANSEN G, 1992, HAVFORSKNING MILJOST, V11, P45; Head M.J., 1996, Palynology: Principles and Applications, P1197; Kofoid C. A., 1921, Memoirs of the University of California, V5, P1; LARSEN J, 1991, SYST ASSOC SPEC VOL, V45, P313; Larsen N.H., 1994, SCANDINAVIAN CULTURE; Lindemann E., 1928, Die Naturlichen Pflanzenfamilien nebst ihren Gattungen und wichtigeren Arten insbesondere den Nutzpflanzen. Zweite stark vermehrte und verbesserte; MATSUOKA K, 1986, J PLANKTON RES, V8, P811, DOI 10.1093/plankt/8.4.811; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Sournia A., 1986, Introduction, Cyanophycees, Dictyophycees, Raphidophycees, P219; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Williams G.L., 2000, Association of Stratigraphic Palynologists Contributions Series, V37, P1	20	7	7	0	9	ALLEN PRESS INC	LAWRENCE	810 E 10TH ST, LAWRENCE, KS 66044 USA	0031-8884			PHYCOLOGIA	Phycologia	NOV	2001	40	6					542	546		10.2216/i0031-8884-40-6-542.1	http://dx.doi.org/10.2216/i0031-8884-40-6-542.1			5	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	520AV					2025-03-11	WOS:000173758500003
J	Amorim, A; Dale, B; Godinho, R; Brotas, V				Amorim, A; Dale, B; Godinho, R; Brotas, V			<i>Gymnodinium catenatum</i>-like cysts (Dinophyceae) in recent sediments from the coast of Portugal	PHYCOLOGIA			English	Article							SP. INED. DINOPHYCEAE; SP-NOV DINOPHYCEAE; DINOFLAGELLATE CYSTS; MICRORETICULATE CYST; SODIUM POLYTUNGSTATE; NOLLERI ELLEGAARD; PHYTOPLANKTON; VIGO; RIA; EXCYSTMENT	Gymnodinium catenatum has been responsible for the main paralytic shellfish poisoning (PSP) events reported along the Iberian coast, where much research effort has been put into understanding its bloom dynamics. Identification of a benthic resting stage in its life cycle raised questions regarding the implications of this life stage Cur bloom dynamics. When first described, the microreticulate cyst of G. catenatum was considered unique, but recently, two additional naked dinoflagellate species with different-sized microreticulate cyst, have been described. viz. G. nolleri and G. microreticulatum. Here, we report on the size distribution of microreticulate cysts from recent sediments along the Portuguese coast and describe the Occurrence of G. microreticulatum in European coastal waters. We also present field data on the distribution of G. catenatum cysts, which support the growing evidence for a planktonic origin for G. catenatum blooms in Iberian waters rather than in benthic cyst beds.	Univ Lisbon, Inst Oceanog, P-1749016 Lisbon, Portugal; Univ Oslo, Dept Geol, N-0316 Oslo, Norway	Universidade de Lisboa; University of Oslo	Univ Lisbon, Inst Oceanog, P-1749016 Lisbon, Portugal.	ajamorim@fc.ul.pt	Amorim, Ana/AAA-2615-2020; Godinho, Rita Mendes/K-2233-2013; Brotas, Vanda/A-2410-2012	Amorim, Ana/0000-0002-9612-4280; Godinho, Rita Mendes/0000-0003-2467-3915; Brotas, Vanda/0000-0001-8612-4167				AMBAR I, 1994, SECOND INTERNATIONAL CONFERENCE ON AIR-SEA INTERACTION AND ON METEOROLOGY AND OCEANOGRAPHY OF THE COASTAL ZONE, P286; Amorim A., 1998, Harmful Algae. 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J	Abbink, OA; Callomon, JH; Riding, JB; Williams, PDB; Wolfard, A				Abbink, OA; Callomon, JH; Riding, JB; Williams, PDB; Wolfard, A			Biostratigraphy of Jurassic-Cretaceous boundary strata in the Terschelling Basin, The Netherlands	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article								The Jurassic-Cretaceous boundary beds in the Scruff Greensand Formation from Dutch sector North Sea wells L06-2 (between 2245.36 m and 2262.76 m) and L06-3 (between 2028.90 m and 2037.80 m) have yielded both ammonite faunas and abundant marine and terrestrial palynomorphs. Ammonite endemism in Europe was intense at the Jurassic-Cretaceous boundary. This means that pan-European correlations of Jurassic-Cretaceous boundary beds based on macrofossils are problematical. The ammonite faunas of wells L06-2 and L06-3 provide the most extensive and complete marine macrofossil record so far across the Volgian-Ryazanian (Jurassic-Cretaceous) boundary in the Spilsby Province and the North Sea Basin. The Primitivus, Preplicomphalus, Lamplughi, Runctoni and Kochi Zones have been identified. In both wells, the occurrences of the dinoflagellate cyst Gochteodinia virgula mean that the successions are no older than latest mid-Volgian. The dinoflagellate cyst associations of L06-2 are indicative of the late Volgian/early Ryazanian. The range tops of Gochteodinia virgula and Amphorula expirata are revised as a result of correlations with the ammonite zonation. Dinoflagellate cyst floras in L06-3 are indicative of the latest Volgian-?earliest Ryazanian. In particular. the co-occurrence of Batioladinium? gochtii and Gochteodinia virgula at 2030.60 m in well L06-3 together with ammonite data, indicates that this horizon is of latest Volgian (Lamplughi Zone) age. Both wells contain reworked palynomorphs, including recycled older Late Jurassic dinoflagellate cysts. In addition, the palynological assemblages yield relatively diverse sporomorph associations. The sporomorph succession of both wells is used to establish an ammonite-calibrated sporomorph chronostratigraphy. Comparison with other studies suggests that the Jurassic/Cretaceous boundary occurs within the Cherty 'Freshwater' Beds of the Purbeck Limestone Group in Dorset, southern England., and within the Serpulite Member of Germany.	Univ Utrecht, Fac Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; UCL, Dept Chem, Christopher Ingold Lab, London WC1H 0AJ, England; British Geol Survey, Nottingham NG12 5GG, England; Nederlandse Aardolie Maatschappij BV, NL-9400 HH Assen, Netherlands	Utrecht University; University of London; University College London; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	TNO, NITG, PMO, Paleoenvironm Res Sect, Postbus 80015, NL-3508 TA Utrecht, Netherlands.	jbri@bgs.ac.uk						Abbink O.A., 1998, LAB PALAEOBOTANY PAL, V8, P192; ALLEN P, 1991, CRETACEOUS RES, V12, P511, DOI 10.1016/0195-6671(91)90005-W; ARKELL WJ, 1957, TREATISE INVERTEBR L, pL341; Batten D.J., 1982, P278; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; BIRKELUND T, 1983, GEOLOGICAL SURVEY DE, P53; BURGER D., 1966, LEID GEOL MEDED, V35, P209; Callomon J.H., 1995, MILESTONES GEOLOGY, V16, P127, DOI DOI 10.1144/GSL.MEM.1995.016.01.14; CALLOMON JH, 1985, SPEC PAP PALAEONTOL, V33, P49; CALLOMON JH, 1996, TREATISE INVERTEBR L, V4, P17; CALLOMON JH, 1983, MEM CAN SOC PETR GEO, V8, P349; CASEY R., 1973, BOREAL LOWER CRETACE, P193; Costa L.I., 1992, P99; COUPER R.A., 1958, PALAEONTOGRAPHICA, V103, P75; D0RH0FER G., 1977, GEOL JB SER, P1; Davey R.J., 1982, DANMARKS GEOLOGISK B, V6; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; DORHOFER G, 1979, AM ASS STRATIGRAPHIC, V0005, P00101; DORING H, 1966, ABHANDLUNGEN ZENTRAL, V8, P46; DORING H, 1966, ABHANDLUNGEN ZENTRAL, V8, P61; DORING H, 1965, GEOLOGIE, V47, P1; Drhfer G., 1977, PALYNOLOGY, V1, P79, DOI [10.1080/01916122.1977.9989151, DOI 10.1080/01916122.1977.9989151]; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Elstner F., 1993, ZITTELIANA, V20, P389; Fisher M.J., 1980, P 4 INT PAL C LUCHN, V2, P313; HALLAM A, 1984, PALAEOGEOGR PALAEOCL, V47, P195, DOI 10.1016/0031-0182(84)90094-4; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; HEILMANNCLAUSEN C, 1987, DANMARKS GEOLOGISKE, V17; Herngreen G. 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Quat. Sci.	OCT	2001	16	7					595	602		10.1002/jqs.660	http://dx.doi.org/10.1002/jqs.660			8	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200001
J	Mudie, PJ; Rochon, A				Mudie, PJ; Rochon, A			Distribution of dinoflagellate cysts in the Canadian Arctic marine region	JOURNAL OF QUATERNARY SCIENCE			English	Article						Canadian Arctic channels; Beaufort Sea; North Water polynya; dinoflagellate cysts; primary productivity	SEA-SURFACE CONDITIONS; BAFFIN-BAY; SEDIMENTS; ASSEMBLAGES; BEAUFORT; PRESERVATION; WEDDELL; LAPTEV; OCEAN	The Canadian Arctic is a major gateway for transport of freshwater from the Arctic Ocean to the North Atlantic. This region comprises the Beaufort Sea, the Canadian Arctic Archipelago (CAA) and northern sections of Baffin and Hudson bays. Subregional differences include major freshwater runoff to the Beaufort Sea and Hudson Bay, presence of Pacific and Atlantic Intermediate water in the west, and Atlantic Water in Baffin and Hudson bays. Principal component analysis of 50 core-top samples shows four subregional dinoflagellate cyst assemblages. Outer Beaufort Shelf Assemblage I is co-dominated by Operculodinium centrocarpum s.l. and Brigantedinium spp., with minor cysts of Pentapharsodinium dalei, Algidasphaeridium? minutum s.l. and cysts of Polykrikos spp. Assemblage II in the Canadian Arctic Archipelago is co-dominated by Brigantedinium sop., A.? minutum s.l. and cysts of Polykrikos spp., including two Arctic morphotypes. Assemblage III in the North Water polynya exclusively comprises A.? minutum s.l. and Brigantedinium spp. Assemblage IV in Baffin Bay is dominated by O. centrocarpum s.l. and Spiniferites spp., with Brigantedinium spp. on the shelves. The ratio of gonyaulacoid to protoperidinioid cysts (G : P) generally decreases with increased sea-ice cover, but it may also decrease in river plumes and in polynyas. Copyright (C) 2001 John Wiley & Sons, Ltd.	Geol Survey Canada Atlantic, Dept Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Geol Survey Canada Atlantic, Dept Nat Resources Canada, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	mudie@agc.bio.ns.ca		Boessenkool, Karin/0000-0003-0887-4864				ANDREWS JT, 1991, CONT SHELF RES, V11, P791, DOI 10.1016/0278-4343(91)90080-P; [Anonymous], 617 FISH MAR SERV; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; BURSA A, 1961, J FISH RES BOARD CAN, V18, P51, DOI 10.1139/f61-004; BURSA AS, 1961, J FISH RES BOARD CAN, V18, P563, DOI 10.1139/f61-046; Carmack EC, 2000, NATO SCI S PRT 2 ENV, V70, P91; Chu PC, 1999, J ATMOS OCEAN TECH, V16, P613, DOI 10.1175/1520-0426(1999)016<0613:AGMFTB>2.0.CO;2; 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, 1987, PALAEOGEOGR PALAEOCL, V61, P97, DOI 10.1016/0031-0182(87)90042-3; DICKINS DF, 1978, STUDY ICE CONDITIONS; GRONTVED J, 1938, MEDDELELSER OM GRONL, V82, P161; GUIOT J, 1995, QUANTIFICATION CHANG; HARGRAVE BT, 2001, IN PRESS DEEP SEA RE, V2; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Hill PR, 1999, CAN J EARTH SCI, V36, P549, DOI 10.1139/e99-003; HSAIO SIC, 1979, 146 FISH MAR SERV; HSAIO SIC, 1979, 155 FISH MAR SERV; HSAIO SIC, 1980, MARINE BIOL STUDY BR; HSIAO SIC, 1983, NOVA HEDWIGIA, V37, P225; KIPP NG, 1976, GEOL SOC AM MEM, V145, P3, DOI DOI 10.1130/MEM145-P3; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; Levac E, 2001, J QUATERNARY SCI, V16, P353, DOI 10.1002/jqs.614; Macdonald RW, 1999, GEOPHYS RES LETT, V26, P2223, DOI 10.1029/1999GL900508; MacLean B., 1989, 8911 GEOL SURV CAN; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; McCarthy Francine M. 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J., 1985, Quaternary Environments: Eastern Canadian Arctic, Baffin Bay And West Greenland, P263; MUDIE PJ, 1992, NEOGENE Q DINOFLAGEL; *NODC, 1994, WORLD OC ATL; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; Okolodkov YB, 1998, SARSIA, V83, P267, DOI 10.1080/00364827.1998.10413687; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Solomon S, 2000, INT J EARTH SCI, V89, P503, DOI 10.1007/s005310000126; Taylor R.B., 1983, SHORELINES ISOSTASY, P53; TIBBS JF, 1967, ARCTIC, V20, P247; TOPHAM DR, 1983, J GEOPHYS RES-OCEANS, V88, P2888, DOI 10.1029/JC088iC05p02888; VILKS G, 1979, GEOLOGICAL SURVEY CA, V303; VILKS G, 1986, ARCTIC SEAS CLIMATOL, P497; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	46	74	84	1	15	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0267-8179	1099-1417		J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					603	620		10.1002/jqs.658	http://dx.doi.org/10.1002/jqs.658			18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ		Bronze			2025-03-11	WOS:000172174200002
J	Head, MJ; Harland, R; Matthiessen, J				Head, MJ; Harland, R; Matthiessen, J			Cold marine indicators of the late Quaternary:: the new dinoflagellate cyst genus <i>Islandinium</i> and related morphotypes	JOURNAL OF QUATERNARY SCIENCE			English	Article						Islandinium minutum; Multispinula; Algidasphaeridium; Echinidinium; Quaternary dinoflagellate cysts; modern Arctic distributions	NORTHERN NORTH-ATLANTIC; SURFACE SEDIMENTS; FALKLAND TROUGH; SEA; ASSEMBLAGES; WEDDELL; CLIMATOSTRATIGRAPHY; SCOTIA	Round, brown, spiny dinoflagellate cysts characterise many modern high-latitude assemblages. Abundance is often highest where summer sea-surface temperatures seldom exceed 7 degreesC and where winter sea-surface temperatures are around 0 degreesC, making this morphological group important for reconstructing cold intervals within marine Quaternary sequences. Our analysis of modern sediments from the Beaufort Sea of Arctic Canada, the Kara and Laptev seas of Arctic Russia, and across the Arctic Ocean, allows us to recognise the new cyst genus Islandinium along with the extant species Islandinium minutum (Harland and Reid in Harland et al., 1980) new combination (basionym: Multispinula? minuta), Islandinium? cezare (de Vernal et al., 1989 ex de Vernal in Rochon et al., 1999) new status and combination (basionym: Multispinula? minuta var. cezare) sensu lato, and Echinidinium karaense new species. Of these, the generotype Islandinium minutum is a well-known but morphologically problematic species. We have re-examined the type material from the Beaufort Sea and studied specimens from across the Arctic, and our observations clarify ambiguities in the original description of this species. The archeopyle of Islandinium minutum results from the loss of three apical plates, an unusual style among peridiniphycidean dinoflagellates. The asymmetrical location of these plates around the apex is distinctive, and probably contributed to earlier misunderstandings of the archeopyle. Previous attributions to Multispinula? and Algidasphaeridium? are unsustainable. Maps showing the distribution of Islandinium minutum are given for the Northern Hemisphere and show this species to be polar to north-temperate, whereas Islandinium? cezare s.l. and Echinidinium karaense appear to be more restricted to polar environments. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England; DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England; Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany	University of Cambridge; University of Sheffield; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				Abe T. H., 1941, REC OCEAN OGR WORKS JAPAN, V12, P121; Abe T. 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Quat. Sci.	OCT	2001	16	7					621	636		10.1002/jqs.657	http://dx.doi.org/10.1002/jqs.657			20	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200003
J	Kunz-Pirrung, M				Kunz-Pirrung, M			Dinoflagellate cyst assemblages in surface sediments of the Laptev Sea region (Arctic Ocean) and their relationship to hydrographic conditions	JOURNAL OF QUATERNARY SCIENCE			English	Article						Arctic Ocean; Laptev Sea; surface sediments; dinoflagellate cyst distribution; polar estuarine environment	MARINE-SEDIMENTS; ATLANTIC; ICE; EXPORT; WATER; NORTH	The occurrence and distribution of dinoflagellate cysts in surface sediments from the Laptev Sea shelf and the adjacent continental margin have been studied in relation to surface water conditions. Assemblages were interpreted by visual inspection and Q-mode factor analysis. The inner Laptev shelf is a type-area for polar environments because of the near absence of relatively warm waters from the Pacific or Atlantic oceans and an extensive seasonal sea-ice cover. Assemblages are of low diversity and are dominated by the cold water taxon Islandinium minutum and related morphotypes. The common occurrence of distinctive polykrikoid cyst morphotypes is an indicator of polar environments. Furthermore, a strong supply of fresh water in summer influences the surface water conditions, and is a major factor controlling the occurrence and distribution of dinoflagellate cysts. The dinoflagellate cysts Nematosphaeropsis labyrinthus and Operculodinium centrocarpum are restricted to the continental margin, suggesting a relation to the inflow of relatively warm Atlantic waters along the Eurasian continental margin. An abundance maximum of Brigantedinium spp. at the shelf break is related to the mean position of the marginal ice zone. Copyright (C) 2001 John Wiley & Sons, Ltd.	Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Kunz-Pirrung, M (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr, D-27568 Bremerhaven, Germany.		; de Vernal, Anne/D-5602-2013	Guiot, Joel/0000-0001-7345-4466; de Vernal, Anne/0000-0001-5656-724X				AAGAARD K, 1989, J GEOPHYS RES-OCEANS, V94, P14485, DOI 10.1029/JC094iC10p14485; Aagaard K., 1994, POLAR OCEANS THEIR R, P5; [Anonymous], NOVA HEDWIGIA; [Anonymous], 1971, POLLEN SPORES; BIEBOW N, 1996, 57 GEOMAR, P1; Burenkov V. 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Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rossak B.T., 1999, LAND OCEAN SYSTEMS S, P587, DOI [10.1007/978-3-642-60134-7_45, DOI 10.1007/978-3-642-60134-7_45]; Schauer U, 1997, J GEOPHYS RES-OCEANS, V102, P3371, DOI 10.1029/96JC03366; Sieger R., 1999, EOS Trans. Am. Geophys. Union, V80, P223, DOI [10.1029/99EO00171, DOI 10.1029/99EO00171]; SUSLOV SP, 1961, PHYSICAL GEOGRAPHY A; Timokhov L.A., 1994, REPORTS POLAR RES, P15; Treshnikov A.F, 1985, ATLAS ARCTIC; TUSCHLING K, 1996, THESIS U KIEL GOTTIN; *UNESCO, 1985, IAPSO PUBL SER, V45, P32; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1998, AM ASS STRATIGRAPHIC, V34, P856	46	54	60	1	7	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					637	649		10.1002/jqs.647	http://dx.doi.org/10.1002/jqs.647			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200004
J	Grosfjeld, K; Harland, R				Grosfjeld, K; Harland, R			Distribution of modern dinoflagellate cysts from inshore areas along the coast of southern Norway	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; modern; distribution; southern Norway; oceanography	SEDIMENTS; HOLOCENE; FJORD; NORTH	Surface sediment samples from inshore areas along the coast of Norway, from Kragero in the south to Kristiansund in mid-Norway, were analysed for their dinoflagellate cyst content in order to establish a modern reference data base. Ultimately these data should furnish a firm foundation for dinoflagellate cyst research in the area in terms of both their spatial and their temporal records. Our aim is to build a data base containing reference samples from the various fjords and inshore areas along the entire Norwegian coast. Dinoflagellate cysts have been recovered from all the samples studied and three main areas have been distinguished based upon their cyst assemblages; the western part of Skagerrak, the southwestern coast of Norway bordering the North Sea, and the west coast of Norway bordering the Norwegian Sea. The dinoflagellate cyst assemblages from these areas are, most probably, closely related to oceanographic parameters and reflect latitudinal or climatic trends along this stretch of the coast. Copyright (C) 2001 John Wiley & Sons, Ltd.	Geol Survey Norway, N-7491 Trondheim, Norway; DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Anim & Plant Sci, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England	Geological Survey of Norway; University of Sheffield	Grosfjeld, K (通讯作者)，Geol Survey Norway, N-7491 Trondheim, Norway.							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., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DALE B, 2000, APPL MICROFOSSILS EN, P305; Fjellsa A, 1996, PALAEOGEOGR PALAEOCL, V124, P87, DOI 10.1016/0031-0182(96)00009-0; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; Gundersen N., 1988, THESIS U OSLO; Harland R., 1996, Proceedings of the Yorkshire Geological Society, V51, P65; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; HARLAND R, 1995, HOLOCENE, V5, P220, DOI 10.1177/095968369500500210; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; *NODC, 1994, WORLD OC ATL; NORDBERG K, IN PRESS J SEA RES; REID PC, 1975, NEW PHYTOL, V75, P589, DOI 10.1111/j.1469-8137.1975.tb01425.x; REID PC, 1977, CONTRIBUTION SERIE A, V1, P147; RINDE E, 1998, KYSTOKOLOGI DENRUSSU; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Sejrup HP, 2001, J QUATERNARY SCI, V16, P181, DOI 10.1002/jqs.593; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	23	33	33	0	4	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					651	659		10.1002/jqs.653	http://dx.doi.org/10.1002/jqs.653			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200005
J	Boessenkool, KP; Van Gelder, MJ; Brinkhuis, H; Troelstra, SR				Boessenkool, KP; Van Gelder, MJ; Brinkhuis, H; Troelstra, SR			Distribution of organic-walled dinoflagellate cysts in surface sediments from transects across the Polar Front offshore southeast Greenland	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; east Greenland; Polar Front; surface sediment; water mass properties	NORTHERN NORTH-ATLANTIC; LAST DEGLACIATION; OCEAN; WATER	The Polar Front along the southeast Greenland Margin denotes the contrasting hydrographic properties of the polar and Atlantic water masses on either side. The remains of planktonic organisms in underlying sediments are expected to reflect these contrasts. To test this, we quantitatively analysed the organic-walled dinoflagellate cyst (dinocyst) assemblages in surface sediments from transects across the present-day Polar Front on the southeast Greenland Margin. Proportional differences are found between the composition of the dinocyst assemblages on either side of the Polar Front. The influence of polar water can be traced in the dinocyst record as high abundances of Algidasphaeridium? minutum and the presence of Pentapharsodinium dalei. The influence of Atlantic water is reflected in the presence of Operculodinium centrocarpum and Selenopemphix quanta. All samples include taxa from both environments, but the quantitative composition of the cyst assemblages clearly reflects the hydrographic features of the overlying surface water masses. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Free Univ Amsterdam, Inst Earth Sci, NL-1081 HV Amsterdam, Netherlands	Utrecht University; Vrije Universiteit Amsterdam	Boessenkool, KP (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Troelstra, Simon/O-2355-2019; Brinkhuis, Henk/B-4223-2009; de Vernal, Anne/D-5602-2013	Boessenkool, Karin/0000-0003-0887-4864; de Vernal, Anne/0000-0001-5656-724X; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 1986, NORDIC SEAS, DOI DOI 10.1007/978-1-4615-8035-5; [Anonymous], NEOGENE QUATERNARY D; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DICKSON RR, 1988, PROG OCEANOGR, V20, P103, DOI 10.1016/0079-6611(88)90049-3; DICKSON RR, 1990, NATURE, V344, P848, DOI 10.1038/344848a0; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; LUCOTTE M, 1994, CAN J EARTH SCI, V31, P5, DOI 10.1139/e94-002; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Rochon A., 1999, CONTRIBUTIONS SERIES, V35; RUDDIMAN WF, 1981, PALAEOGEOGR PALAEOCL, V35, P145; SOMMERHOFF G, 1974, DTSCH HYYDROGRAPHISC, V27, P114; Swift J., 1986, NORDIC SEAS, P129, DOI DOI 10.1007/978-1-4615-8035-5_5; TARGARONA J, 1997, THESIS UTRECHT U; Traverse A., 1988, PALEOPALYNOLOGY, P375; TROELSTRA SR, 1997, LATE QUATERNARY PALA; WILLIAMS GL, 1998, LENTIN WILLIAMS INDE; Zonneveld KAF, 1997, QUATERNARY SCI REV, V16, P187, DOI 10.1016/S0277-3791(96)00049-2; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	19	28	28	1	4	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					661	666		10.1002/jqs.654	http://dx.doi.org/10.1002/jqs.654			6	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200006
J	Radi, T; De Vernal, A; Peyron, O				Radi, T; De Vernal, A; Peyron, O			Relationships between dinoflagellate cyst assemblages in surface sediment and hydrographic conditions in the Bering and Chukchi seas	JOURNAL OF QUATERNARY SCIENCE			English	Article						Bering Sea; Chukchi Sea; dinocysts; sea-ice cover; sea-surface temperature	LATITUDE MARINE ENVIRONMENTS; ICE EDGE; NORTH PACIFIC; ARCTIC-OCEAN; INDIAN-OCEAN; SPRING BLOOM; SHELF; SALINITY; STRAIT; FLOW	Palynological analyses were performed on 52 surface sediment samples from the eastern part of the Bering Sea and Chukchi Sea in order to document the regional distribution of dinoflagellate cyst assemblages and their relationship with sea-surface conditions. The assemblages present a relatively high species diversity (20 taxa are recovered routinely), especially in the Bering Sea, where they are dominated by Operculodinium centrocarpum and the cyst of Pentapharsodinium dalei accompanied mainly by Spiniferites elongatus s.l., Spiniferites ramosus, Impagidinium pallidum, Brigantedinium spp., Islandinium minutum, Selenopemphix quanta, Selenopemphix nephroides, Quinquecuspis concreta and the cyst of Polykrikos kofoidii. The percentages of the main taxa vary with latitude, and principal component analysis shows that the distribution of assemblages is closely related to hydrographic conditions, notably the seasonal duration of sea-ice cover and the sea-surface temperature in February. The dinoflagellate cyst assemblages from the Bering Sea differ significantly from those of subarctic seas of the North Atlantic, with respect to their species composition and relationships with sea-surface conditions. In particular, the occurrence of the cyst of Polykrikos kofoidii and Quinquecuspis concreta and the positive correlation between the percentages of Operculodinium centrocarpum and the extent of sea-ice, constitute peculiar features in the Bering Sea assemblages. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Quebec, Geotop, Ctr Rech Geochim Isotop & Geochronol, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Radi, T (通讯作者)，Univ Quebec, Geotop, Ctr Rech Geochim Isotop & Geochronol, POB 8888, Montreal, PQ H3C 3P8, Canada.		de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Matthiessen, Jens/0000-0002-6952-2494				AAGAARD K, 1985, J GEOPHYS RES-OCEANS, V90, P7213, DOI 10.1029/JC090iC04p07213; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; BUJAK J P, 1986, Palynology, V10, P235; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; CAVALIERI DJ, 1987, J GEOPHYS RES-OCEANS, V92, P7141, DOI 10.1029/JC092iC07p07141; CAVALIERI DJ, 1994, J GEOPHYS RES-OCEANS, V99, P18343, DOI 10.1029/94JC01169; Chen CS, 1997, J MAR RES, V55, P293, DOI 10.1357/0022240973224391; CHEN CTA, 1993, CONT SHELF RES, V13, P67, DOI 10.1016/0278-4343(93)90036-W; COACHMAN LK, 1988, J GEOPHYS RES-OCEANS, V93, P15535, DOI 10.1029/JC093iC12p15535; COACHMAN LK, 1993, CONT SHELF RES, V13, P481, DOI 10.1016/0278-4343(93)90092-C; CODISPOTI LA, 1982, NATURE, V296, P242, DOI 10.1038/296242a0; COONEY RT, 1982, MAR BIOL, V70, P187, DOI 10.1007/BF00397684; Cooper LW, 1997, J GEOPHYS RES-OCEANS, V102, P12563, DOI 10.1029/97JC00015; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 2000, CAN J EARTH SCI, V37, P725, DOI [10.1139/cjes-37-5-725, 10.1139/e99-091]; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 1997, PALEOCEANOGRAPHY, V12, P821, DOI 10.1029/97PA02167; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1999, 3 GEOTOP U QUEB MONT; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; FUKUCHI M, 1993, CONT SHELF RES, V13, P693, DOI 10.1016/0278-4343(93)90100-C; Gadd N.R., 1988, The late Quaternary development of the Champlain Sea basin; GREBMEIER JM, 1993, CONT SHELF RES, V13, P653, DOI 10.1016/0278-4343(93)90098-I; GREBMEIER JM, 1995, J GEOPHYS RES-OCEANS, V100, P4439, DOI 10.1029/94JC02198; Guiot J., 1996, Dendrochronologia, V14, P295; HANSELL DA, 1993, CONT SHELF RES, V13, P601, DOI 10.1016/0278-4343(93)90096-G; HARLAND R, 1980, Grana, V19, P211; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; LOUCHEUR V, 1999, THESIS U QUEBEC MONT; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Marret F, 2001, CAN J EARTH SCI, V38, P373, DOI 10.1139/e00-092; MATSUBARA E, 1988, T JPN I MET, V29, P1, DOI 10.2320/matertrans1960.29.1; Matsuoka K, 2000, MICROPALEONTOLOGY, V46, P360; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Matsuoka K., 1987, Bull. Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; Matsuoka Kazumi, 1997, Palynology, V21, P19; MATTHEWS J, 1969, NEW PHYTOL, V68, P161, DOI 10.1111/j.1469-8137.1969.tb06429.x; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; MAYNARD NG, 1987, J GEOPHYS RES-OCEANS, V92, P7127, DOI 10.1029/JC092iC07p07127; MOREYGAINES G, 1980, PHYCOLOGIA, V19, P230, DOI 10.2216/i0031-8884-19-3-230.1; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. J., 1985, Quaternary Environments: Eastern Canadian Arctic, Baffin Bay And West Greenland, P263; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; NIEBAUER HJ, 1990, J GEOPHYS RES-OCEANS, V95, P22229, DOI 10.1029/JC095iC12p22229; NIEBAUER HJ, 1988, J GEOPHYS RES-OCEANS, V93, P5051, DOI 10.1029/JC093iC05p05051; NIEBAUER HJ, 1995, CONT SHELF RES, V15, P1859, DOI 10.1016/0278-4343(94)00097-7; *NODC, 1994, WORLD OC ATL; OVERLAND JE, 1987, J GEOPHYS RES-OCEANS, V92, P7097, DOI 10.1029/JC092iC07p07097; Reed RK, 1997, J MAR RES, V55, P565, DOI 10.1357/0022240973224328; ROACH AT, 1995, J GEOPHYS RES-OCEANS, V100, P18443, DOI 10.1029/95JC01673; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A., 1999, SPECIAL CONTRIBUTION, V35; SPRINGER AM, 1993, CONT SHELF RES, V13, P575, DOI 10.1016/0278-4343(93)90095-F; Stabeno PJ, 1998, J MAR RES, V56, P239, DOI 10.1357/002224098321836172; THOMSON SE, 1981, SPECIAL PUBLICATION, V56; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; WALSH JJ, 1986, CONT SHELF RES, V5, P259, DOI 10.1016/0278-4343(86)90018-X; WALSH JJ, 1989, PROG OCEANOGR, V22, P277, DOI 10.1016/0079-6611(89)90006-2; Zonneveld KAF, 1997, QUATERNARY SCI REV, V16, P187, DOI 10.1016/S0277-3791(96)00049-2; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	65	77	83	0	11	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					667	680		10.1002/jqs.652	http://dx.doi.org/10.1002/jqs.652			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200007
J	de Vernal, A; Henry, M; Matthiessen, J; Mudie, PJ; Rochon, A; Boessenkool, KP; Eynaud, F; Grosfjeld, K; Guiot, J; Hamel, D; Harland, R; Head, MJ; Kunz-Pirrung, M; Levac, E; Loucheur, V; Peyron, O; Pospelova, V; Radi, T; Turon, JL; Voronina, E				de Vernal, A; Henry, M; Matthiessen, J; Mudie, PJ; Rochon, A; Boessenkool, KP; Eynaud, F; Grosfjeld, K; Guiot, J; Hamel, D; Harland, R; Head, MJ; Kunz-Pirrung, M; Levac, E; Loucheur, V; Peyron, O; Pospelova, V; Radi, T; Turon, JL; Voronina, E			Dinoflagellate cyst assemblages as tracers of sea-surface conditions in the northern North Atlantic, Arctic and sub-Arctic seas:: the new '<i>n</i>=677' data base and its application for quantitative palaeoceanographic reconstruction	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; northern North Atlantic and Arctic; temperature; salinity; sea-ice	LATITUDE MARINE ENVIRONMENTS; PALYNOLOGICAL EVIDENCE; POLLEN DATA; LABRADOR SEA; ICE COVER; SEDIMENTS; SALINITY; TEMPERATURE; TERRESTRIAL	The distribution of dinoflagellate cyst (dinocyst) assemblages in surface sediment samples from 677 sites of the northern North Atlantic, Arctic and sub-Arctic seas is discussed with emphasis on the relationships with sea-surface parameters, including sea-ice cover, salinity and temperature of the coldest and warmest months. Difficulties in developing a circum-Arctic data base include the morphological variation within taxa (e.g. Operculodinium centrocarpum, Islandinium? cezare and Polykrikos sp.), which probably relate to phenotypic adaptations to cold and/or low salinity environments. Sparse hydrographical data, together with large interannual variations of temperature and salinity in surface waters of Arctic seas constitute additional limitations. Nevertheless, the use of the best-analogue technique with this new dinocyst data base including 677 samples permits quantitative reconstruction of sea-surface conditions at the scale of the northern North Atlantic and the Arctic domain. The error of prediction calculated from modern assemblages is +/-1.3 degreesC and +/-1.8 degreesC for the temperature of February and August, respectively, +/-1.8 for the salinity, and +/-1.5 months yr(-1) for the sea-ice cover. Application to late Quaternary sequences from the western and eastern subpolar North Atlantic (Labrador Sea and Barents Sea) provide reconstructions compatible with those obtained using the previous dinocyst data base (n = 371), which mainly included modern data from the northern North Atlantic. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany; Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada; Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Bordeaux 1, Dept Geol & Oceanog, CNRS, UMR 5805, F-33405 Talence, France; Geol Survey Norway, N-7002 Trondheim, Norway; CNRS, CEREGE, F-13545 Aix En Provence 4, France; DinoData Serv, Bingham NG13 8AH, England; Univ Sheffield, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England; Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; Dalhousie Univ, Dept Earth Sci, Halifax, NS B3H 3J5, Canada; McGill Univ, Ctr Climate & Global Change Res, Montreal, PQ H3A 2K6, Canada; McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada	University of Quebec; University of Quebec Montreal; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Utrecht University; Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Geological Survey of Norway; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); University of Sheffield; University of Cambridge; Dalhousie University	de Vernal, A (通讯作者)，Univ Quebec, Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada.		Guiot, Joel/G-7818-2011; de Vernal, Anne/D-5602-2013	Boessenkool, Karin/0000-0003-0887-4864; Pospelova, Vera/0000-0003-4049-8133; Eynaud, Frederique/0000-0003-1283-7425; de Vernal, Anne/0000-0001-5656-724X				Birks H.J.B., 1995, STAT MODELLING QUATE; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; de Vernal A, 2000, CAN J EARTH SCI, V37, P725, DOI [10.1139/cjes-37-5-725, 10.1139/e99-091]; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; de Vernal A, 1996, NATURE, V381, P774, DOI 10.1038/381774a0; De Vernal A., 1993, Nato. Asi. Ser, VI12, P611, DOI DOI 10.1007/978-3-642-85016-5_34; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DEVERNAL A, 1999, 3 U QUEB MONTR; DEVERNAL A, 1987, GEROGR PHYS QUATERN, V41, P265; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Eynaud F., 1999, KYSTES DINOFLAGELLES; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; GROSFJELD K, J QUATERNARY SCI, V16, P651; Guiot J., 1996, Dendrochronologia, V14, P295; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; HAMEL D, 2001, PALYNOMORPHES TRACEU; HARLAND R, 1981, Palynology, V5, P65; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hillaire-Marcel C, 2001, GEOPH MONOG SERIES, V126, P83; Hillaire-Marcel C, 2001, NATURE, V410, P1073, DOI 10.1038/35074059; HILLAIREMARCEL C, 1994, CAN J EARTH SCI, V31, P63, DOI 10.1139/e94-007; HUTSON WH, 1980, SCIENCE, V207, P64, DOI 10.1126/science.207.4426.64; Imbrie J., 1971, LATE CENOZOIC GLACIA, P71; Kucera M, 1998, MAR MICROPALEONTOL, V34, P117, DOI 10.1016/S0377-8398(97)00047-9; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; KUNZPIRRUNG M, 1998, BERICHTE POLARFORSCH, V281, P117; Levac E, 2001, J QUATERNARY SCI, V16, P353, DOI 10.1002/jqs.614; Levac E, 1997, CAN J EARTH SCI, V34, P1358, DOI 10.1139/e17-108; LOENG H, 1991, POLAR RES, V10, P5, DOI 10.1111/j.1751-8369.1991.tb00630.x; MALMGREN B, 2001, IN PRESS PALEOCEANOG, V16; Malmgren BA, 1997, PALAEOGEOGR PALAEOCL, V136, P359, DOI 10.1016/S0031-0182(97)00031-X; MARKHAM WE, 1980, ATLAS GALCES LITTORA; Marret F., 1993, PALYNOSCIENCES, V2, P267; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; McCarthy Francine M. G., 2000, Palynology, V24, P63, DOI 10.2113/0240063; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. J., 1985, Quaternary Environments: Eastern Canadian Arctic, Baffin Bay And West Greenland, P263; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; *NODC, 1994, WORLD OC ATL; Peyron O, 1998, QUATERNARY RES, V49, P183, DOI 10.1006/qres.1997.1961; Peyron O, 2000, QUATERNARY RES, V54, P90, DOI 10.1006/qres.2000.2136; PEYRON O, 2001, J QUATERNARY SCI; Pflaumann U, 1996, PALEOCEANOGRAPHY, V11, P15, DOI 10.1029/95PA01743; Prell W.L., 1985, The Stability of Low-Latitude Sea-Surface Temperatures: An Evaluation of the CLIMAP Reconstruction with Emphasis on the Positive SST Anomalies; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rochon A, 1998, QUATERNARY RES, V49, P197, DOI 10.1006/qres.1997.1956; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A., 1999, SPECIAL CONTRIBUTION, V35; TAYLOR FJR, 1987, BOT MONOGRAPHAS, V21; TERBRAAK CJF, 1989, HYDROBIOLOGIA, V178, P209, DOI 10.1007/BF00006028; TURON JL, 1984, THESIS U BORDEAUX 1, V17; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; Waelbroeck C, 1998, PALEOCEANOGRAPHY, V13, P272, DOI 10.1029/98PA00071; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	65	290	304	0	23	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					681	698		10.1002/jqs.659	http://dx.doi.org/10.1002/jqs.659			26	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200008
J	Peyron, O; De Vernal, A				Peyron, O; De Vernal, A			Application of artificial neural networks (ANN) to high-latitude dinocyst assemblages for the reconstruction of past sea-surface conditions in Arctic and sub-Arctic seas	JOURNAL OF QUATERNARY SCIENCE			English	Article						transfer function; neural network; dinoflagellate cyst; palaeoceanography; sub-Arctic seas and North Atlantic	DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; MODERN ANALOG TECHNIQUE; LABRADOR-SEA; PALYNOLOGICAL EVIDENCE; MARINE ENVIRONMENTS; ICE COVER; TEMPERATURE; OCEAN; SALINITY	The artificial neural network (ANN) method was applied to dinoflagellate cyst (dinocyst) assemblages to estimate palaeoceanographical conditions. The ANN method was adapted to three distinct data bases covering the northern North Atlantic (N = 371), plus the Arctic seas (N = 540) and the Bering Sea (N = 646). The relative abundance of 23 dinocyst taxa was calibrated against hydrographic variables (sea-surface temperature, salinity and density in February and August, and seasonal extent of sea-ice cover) using ANNs. The estimation of hydrographical parameters based on an ANN yields high coefficients of correlation between observations and reconstructions for each variable selected. The validation tests performed on the different data bases suggest more accurate calibration at the scale of the North Atlantic and Arctic (N = 540) than on a multibasin scale, i.e. when including the subpolar North Pacific (N = 646). The ANN calibrations and the modern analogue technique (MAT) have been applied to two sequences from the northwest North Atlantic spanning the past 25 000 yr for the purpose of comparison. Both approaches yielded similar results, generally within the range of their respective uncertainties, demonstrating their suitability. The main discrepancies generally correspond to assemblages with poor modern analogues for which we have to admit a higher degree of uncertainties in the reconstruction, whatever the approach used. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Univ Quebec, Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada.	r21024@er.uqam.ca	de Vernal, Anne/D-5602-2013					Anderson J.A., 1987, Neurocomputing; [Anonymous], 1996, Palaeoclimates; Birks HJB, 1998, J PALEOLIMNOL, V20, P307, DOI 10.1023/A:1008038808690; Braconnot P, 2000, J CLIMATE, V13, P1537, DOI 10.1175/1520-0442(2000)013<1537:OFIRTK>2.0.CO;2; Caudill Maureen., 1992, UNDERSTANDING NEURAL, V1; Crosta X, 1998, PALEOCEANOGRAPHY, V13, P284, DOI 10.1029/98PA00339; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; de Vernal A, 2000, CAN J EARTH SCI, V37, P725, DOI [10.1139/cjes-37-5-725, 10.1139/e99-091]; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 1996, NATURE, V381, P774, DOI 10.1038/381774a0; de Vernal A., 1993, NATO ASI SERIES, V12, P611; Devillers R, 2000, MAR GEOL, V166, P103, DOI 10.1016/S0025-3227(00)00007-4; Dollfus D, 1999, NEURAL NETWORKS, V12, P553, DOI 10.1016/S0893-6080(99)00011-8; EFRON B, 1979, ANN STAT, V7, P1, DOI 10.1214/aos/1176344552; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Guiot J., 1996, Dendrochronologia, V14, P295; GUIOT J, 1987, QUATERNARY RES, V28, P100, DOI 10.1016/0033-5894(87)90036-6; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; HAMEL D, IN PRESS DEEP SEA RE; Hewitt CD, 1998, GEOPHYS RES LETT, V25, P361, DOI 10.1029/97GL03721; Hillaire-Marcel C, 2001, NATURE, V410, P1073, DOI 10.1038/35074059; Hillaire-Marcel C, 2000, CAN J EARTH SCI, V37, P795, DOI [10.1139/cjes-37-5-795, 10.1139/e99-108]; HILLAIREMARCEL C, 1994, CAN J EARTH SCI, V31, P63, DOI 10.1139/e94-007; HILLAIREMARCEL C, AM GEOPHYSICAL UNION; HUTSON WH, 1980, SCIENCE, V207, P64, DOI 10.1126/science.207.4426.64; Imbrie J., 1971, LATE CENOZOIC GLACIA; Karpuz NK, 1990, PALEOCEANOGRAPHY, V5, P557, DOI 10.1029/PA005i004p00557; Keller T, 2000, CR ACAD SCI III-VIE, V323, P913, DOI 10.1016/S0764-4469(00)01238-5; KOC N, 1993, QUATERNARY SCI REV, V12, P115, DOI 10.1016/0277-3791(93)90012-B; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Lek S, 1996, ECOL MODEL, V90, P39, DOI 10.1016/0304-3800(95)00142-5; Levac E, 2001, J QUATERNARY SCI, V16, P353, DOI 10.1002/jqs.614; Levac E, 1997, CAN J EARTH SCI, V34, P1358, DOI 10.1139/e17-108; Malmgren BA, 1996, PALEOCEANOGRAPHY, V11, P505, DOI 10.1029/96PA01237; Malmgren BA, 1997, PALAEOGEOGR PALAEOCL, V136, P359, DOI 10.1016/S0031-0182(97)00031-X; MARKHAM WE, 1980, ATLAS GLACES LITTORA; Masters T., 1993, Practical neural network recipes in C++; Moatar F, 1999, ECOL MODEL, V120, P141, DOI 10.1016/S0304-3800(99)00098-8; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; *NODC, 1994, WORLD OC ATL; Peyron O, 1998, QUATERNARY RES, V49, P183, DOI 10.1006/qres.1997.1961; Peyron O, 2000, QUATERNARY RES, V54, P90, DOI 10.1006/qres.2000.2136; Pflaumann U, 1996, PALEOCEANOGRAPHY, V11, P15, DOI 10.1029/95PA01743; Pisias NG, 1997, PALEOCEANOGRAPHY, V12, P365, DOI 10.1029/97PA00582; Prell W.L., 1985, The Stability of Low-Latitude Sea-Surface Temperatures: An Evaluation of the CLIMAP Reconstruction with Emphasis on the Positive SST Anomalies; RACCA J, IN PRESS J PALEOLIMN, V26; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Rochon A, 1998, QUATERNARY RES, V49, P197, DOI 10.1006/qres.1997.1956; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Stoner JS, 1998, EARTH PLANET SC LETT, V159, P165, DOI 10.1016/S0012-821X(98)00069-7; Stoner JS, 2000, EARTH PLANET SC LETT, V183, P161, DOI 10.1016/S0012-821X(00)00272-7; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; Waelbroeck C, 1998, PALEOCEANOGRAPHY, V13, P272, DOI 10.1029/98PA00071; Wasserman P. D., 1989, Neural computing: Theory and practice; WASSERMAN PD, 1993, ADV METHOD NEURAL CO; Zielinski U, 1998, PALEOCEANOGRAPHY, V13, P365, DOI 10.1029/98PA01320	59	26	26	0	4	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0267-8179	1099-1417		J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					699	709		10.1002/jqs.651	http://dx.doi.org/10.1002/jqs.651			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200009
J	Kunz-Pirrung, M; Matthiessen, J; De Vernal, A				Kunz-Pirrung, M; Matthiessen, J; De Vernal, A			Late Holocene dinoflagellate cysts as indicators for short-term climate variability in the eastern Laptev Sea (Arctic Ocean)	JOURNAL OF QUATERNARY SCIENCE			English	Article						Siberian Arctic; Laptev Sea; dinoflagellate cysts; Holocene; palaeoenvironmental reconstructions	ADJACENT SEAS; RUSSIA; SEDIMENTS; REGION; NORTH; AGE	A sediment sequence from the eastern Laptev Sea shelf (Siberian Arctic, Russia) has been studied for dinoflagellate cysts in order to reconstruct sea-surface conditions during the late Holocene. Variability of assemblage composition and derived sea-surface temperature estimates indicate that the neoglacial cooling was not a gradual climate change from 2510 to 900 cal. yr BP. Relatively stable conditions, with temperatures that were warmer than today, were punctuated by a few cooling events in summer on centennial time-scales. During these events temperatures reached modern values. This suggests that modern conditions may have been established abruptly within a short period in the past 1000 yr, which is not documented in our record. Copyright (C) 2001 John Wiley & Sons, Ltd.	Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Quebec; University of Quebec Montreal	Kunz-Pirrung, M (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr, D-27568 Bremerhaven, Germany.		de Vernal, Anne/D-5602-2013					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], 1999, LAND OCEAN SYSTEMS S, DOI DOI 10.1007/978-3; 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, GLOBAL PLANETARY CHA; Briffa KR, 2000, QUATERNARY SCI REV, V19, P87, DOI 10.1016/S0277-3791(99)00056-6; Cremer H, 1998, BERICHTE POLARFORSCH, V260, P1; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DMITRENKO IA, 1995, REPORTS POLAR RES, V182, P22; Duplessy JC, 2001, BOREAS, V30, P2; Dyke AS, 1997, ARCTIC, V50, P1; EARLE CJ, 1994, ARCTIC ALPINE RES, V26, P60, DOI 10.2307/1551878; Eicken H, 1997, CONT SHELF RES, V17, P205, DOI 10.1016/S0278-4343(96)00024-6; Forman SL, 1997, GEOPHYS RES LETT, V24, P885, DOI 10.1029/97GL00761; Hahne J., 1999, Land-Ocean Systems in the Siberian Arctic: Dynamics and History, P407, DOI DOI 10.1007/978-3-642-60134-7_33; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Holmes M.L., 1974, MARINE GEOLOGY OCEAN, P211, DOI DOI 10.1007/978-3-642-87411-6_9; KASSENS H, 1994, BERICHTE POLARFORSCH, V151; Khotinsky N.A., 1984, Late Quaternary Environments of the Soviet Union, P305; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Kunz-Pirrung M., 1998, BERICHTE POLARFORSCH, V281; LETOLLE R, 1993, MAR CHEM, V43, P47, DOI 10.1016/0304-4203(93)90215-A; Lozhkin AV, 2001, QUATERNARY SCI REV, V20, P217, DOI 10.1016/S0277-3791(00)00121-9; MacDonald GM, 2000, QUATERNARY RES, V53, P302, DOI 10.1006/qres.1999.2123; MacDonald GM, 1998, ARCTIC ALPINE RES, V30, P334, DOI 10.2307/1552005; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; PEREGOVICH B, 1999, BERICHTE POLARFORSCH, V316; Pisaric MFJ, 2001, ARCT ANTARCT ALP RES, V33, P19, DOI 10.2307/1552273; POLYAKOVA YI, 1999, LAND OCEAN SYSTEMS S, P615; ROCHON A, 1999, AM ASS STRAT PAL CON, V35; Stuiver M, 1998, RADIOCARBON, V40, P1041, DOI 10.1017/S0033822200019123; Timokhov L.A., 1994, REPORTS POLAR RES, P15; *UNESCO, 1985, IAPSO PUBL SER, V45, P32; Velichko AA, 1997, QUATERN INT, V41-2, P71, DOI 10.1016/S1040-6182(96)00039-0; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34	44	10	13	0	3	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					711	716		10.1002/jqs.649	http://dx.doi.org/10.1002/jqs.649			6	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200010
J	Voronina, E; Polyak, L; De Vernal, A; Peyron, O				Voronina, E; Polyak, L; De Vernal, A; Peyron, O			Holocene variations of sea-surface conditions in the southeastern Barents Sea, reconstructed from dinoflagellate cyst assemblages	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cysts; Holocene; Barents Sea; palaeoceanography; sea-surface reconstructions	LATITUDE MARINE ENVIRONMENTS; NORTH-ATLANTIC; SKAGERRAK-KATTEGAT; RECENT SEDIMENTS; ARCTIC RUSSIA; OCEAN; CLIMATE; PALEOCEANOGRAPHY; ICELAND; TRACERS	Palynomorphs were analysed in two sediment cores from the southeastern Barents Sea representing the past 8.3 and 4.4 kyr. High dinocyst contents and species diversity enabled the application of the best analogue method to quantitatively reconstruct sea-surface salinities temperatures and ice cover using 677 modern reference sites from the North Atlantic and Arctic seas, including new data from the Barents Sea reported here. At the southern core site, where waters are affected by the Atlantic inflow, sea-surface conditions were relatively warm and stable between ca. 8000 and 5000 calendar yr BP. In contrast, the past 5 kyr had periods with cooler temperatures and extended ice cover, fluctuating mostly at 1-1.5 kyr frequencies at both sites. Most pronounced coolings occurred around 8.1, 5, 3.5-3.2 and 2.5 ka. The northern site additionally shows younger cooling events, tentatively dated to 1.4, 0.3 and 0.1 ka. Identified variations in sea-surface conditions indicate changes in Atlantic water inputs to the Barents Sea. Our results generally correlate to palaeoclimatic reconstructions from northwestern Eurasia, exemplified by palynological records from Karelia. This correlation suggests that sea-surface variations in the Barents Sea reflect large-scale changes in atmospheric and oceanic interactions between the North Atlantic and the Arctic. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA	University of Quebec; University of Quebec Montreal; University System of Ohio; Ohio State University	Voronina, E (通讯作者)，Univ Quebec, Geotop, POB 8888, Montreal, PQ H3C 3P8, Canada.		de Vernal, Anne/D-5602-2013					Alley RB, 1997, GEOLOGY, V25, P483, DOI 10.1130/0091-7613(1997)025<0483:HCIAPW>2.3.CO;2; ALLEY RB, 1999, POLAR GEOGRAPHY, V23, P119; Andreev AA, 2000, J PALEOLIMNOL, V24, P81, DOI 10.1023/A:1008121917521; [Anonymous], CALIB RADIOCARBON CA; Barber DC, 1999, NATURE, V400, P344, DOI 10.1038/22504; Bianchi GG, 1999, NATURE, V397, P515, DOI 10.1038/17362; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; CONRADSEN K, 1995, PALEOCEANOGRAPHY, V10, P801, DOI 10.1029/95PA01142; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1999, UNPUB TECHNIQUE PREP; Duplessy JC, 2001, BOREAS, V30, P2; Guiot J., 1996, Dendrochronologia, V14, P295; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; Hald M, 1999, PALAEOGEOGR PALAEOCL, V146, P229, DOI 10.1016/S0031-0182(98)00133-3; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; JACOBSEN DM, 1986, J PHYCOL, V34, P153; JENNINGS A, 2000, SEA ICE CLIMATE SYST, P32; Jiang H, 1997, HOLOCENE, V7, P301; KLIMANOV VA, 1984, DOKL AKAD NAUK SSSR, V274, P1163; KOC N, 1993, QUATERNARY SCI REV, V12, P115, DOI 10.1016/0277-3791(93)90012-B; Kutzbach J. 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Quat. Sci.	OCT	2001	16	7					717	726		10.1002/jqs.650	http://dx.doi.org/10.1002/jqs.650			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200011
J	Matthiessen, J; Knies, J				Matthiessen, J; Knies, J			Dinoflagellate cyst evidence for warm interglacial conditions at the northern Barents Sea margin during marine oxygen isotope stage 5	JOURNAL OF QUATERNARY SCIENCE			English	Article						Arctic Ocean; Quaternary; marine oxygen isotope stage 5; palaeoenvironment; dinoflagellate cysts	NORWEGIAN-GREENLAND SEA; LAST 150000 YEARS; ARCTIC-OCEAN; ICE-SHEET; YERMAK PLATEAU; FORAMINIFERAL STRATIGRAPHY; CARBONATE DISSOLUTION; NORDIC SEAS; FRAM STRAIT; C-14 AGES	Dinoflagellate cyst analysis has been conducted on a sediment core from the northern Barents Sea margin (eastern Arctic Ocean) to reconstruct sea-surface conditions during marine oxygen isotope stage 5. Cyst concentrations and composition of assemblages display a distinct variability reflecting deglacial warming and the onset of relatively warm interglacial conditions in early stage 5. Dinoflagellate cyst assemblages of the last interglacial, which corresponds broadly to substage 5e, are comparable with those from recent sediments of the area, but have lower abundances of cold water taxa. Such assemblages suggest that sea-surface temperatures of the last interglacial were therefore at least as warm as today or even warmer. After a distinct cooling, relatively stable cold conditions with minor periods of surface water warming prevailed from mid-substages 5d to 5b. Temperatures might have been similar in substages 5a and 5e, but the different compositions of assemblages indicate a stronger stratification of surface waters, probably owing to a larger meltwater supply, in substage 5a. These results are compared with previous studies on marine carbonate and calcareous microfossil records from the Fram Strait and Yermak Plateau area, which show that the general view of a cold last interglacial in the eastern Arctic Ocean is untenable. Copyright (C) 2001 John Wiley & Sons, Ltd.	Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; Geol Survey Norway, N-7491 Trondheim, Norway	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Geological Survey of Norway	Matthiessen, J (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr, D-27568 Bremerhaven, Germany.			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L., 1998, AM ASS STRATIGRAPHIC, V34; Wollenburg JE, 2001, PALEOCEANOGRAPHY, V16, P65, DOI 10.1029/1999PA000454; Wollenburg JE, 1998, J FORAMIN RES, V28, P268, DOI 10.2113/gsjfr.28.4.268; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	74	35	35	0	10	JOHN WILEY & SONS LTD	W SUSSEX	BAFFINS LANE CHICHESTER, W SUSSEX PO19 1UD, ENGLAND	0267-8179			J QUATERNARY SCI	J. Quat. Sci.	OCT	2001	16	7					727	737		10.1002/jqs.656	http://dx.doi.org/10.1002/jqs.656			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200012
J	Marret, F; De Vernal, A; Benderra, F; Harland, R				Marret, F; De Vernal, A; Benderra, F; Harland, R			Late Quaternary sea-surface conditions at DSDP Hole 594 in the southwest Pacific Ocean based on dinoflagellate cyst assemblages	JOURNAL OF QUATERNARY SCIENCE			English	Article						dinoflagellate cyst; Southern Ocean; transfer function; Recent; late Quaternary	LAST GLACIAL MAXIMUM; LATITUDE MARINE ENVIRONMENTS; SOUTHEASTERN NEW-ZEALAND; SOUTHERN-OCEAN; INDIAN-OCEAN; ATLANTIC SECTOR; RECENT SEDIMENTS; FALKLAND TROUGH; BIOGENIC SILICA; CHATHAM RISE		Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales; Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England	University of Quebec; University of Quebec Montreal; University of Sheffield	Marret, F (通讯作者)，Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales.		de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Marret-Davies, Fabienne/0000-0003-4244-0437				Abelmann A, 1999, PALEOCEANOGRAPHY, V14, P410, DOI 10.1029/1998PA900024; ALLOWAY BV, 1992, QUATERNARY RES, V38, P170, DOI 10.1016/0033-5894(92)90054-M; ANDERSON JB, 1975, MAR GEOL, V19, P315, DOI 10.1016/0025-3227(75)90083-3; [Anonymous], NEOGENE QUATERNARY D; Barrows TT, 2000, PALEOCEANOGRAPHY, V15, P95, DOI 10.1029/1999PA900047; Be A.W. 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Quat. Sci.	OCT	2001	16	7					739	751		10.1002/jqs.648	http://dx.doi.org/10.1002/jqs.648			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	492NJ					2025-03-11	WOS:000172174200013
J	Vink, A; Rühlemann, C; Zonneveld, KAF; Mulitza, S; Hüls, M; Willems, H				Vink, A; Rühlemann, C; Zonneveld, KAF; Mulitza, S; Hüls, M; Willems, H			Shifts in the position of the North Equatorial Current and rapid productivity changes in the western Tropical Atlantic during the last glacial	PALEOCEANOGRAPHY			English	Article							CALCAREOUS DINOFLAGELLATE CYSTS; GREENLAND ICE CORE; HEINRICH EVENTS; CARIBBEAN SEA; THERMOHALINE CIRCULATION; THORACOSPHAERA-HEIMII; SPATIAL-DISTRIBUTION; NORTHEASTERN BRAZIL; ICEBERG DISCHARGES; SURFACE SEDIMENTS	High-resolution, well-dated calcareous dinoflagellate cyst and organic carbon records from a 58 kyr sediment core (M35003-4) located southeast of the island of Grenada show that rapid and pronounced changes in cyst association and accumulation and organic carbon deposition occurred, controlled by (1) a significant southward shift in the position of the North Equatorial Current during the last glacial period and the Younger Dryas cold interval and (2) rapid changes in local productivity in marine isotopic stage 3 that are associated with variations in Orinoco River nutrient discharge and coastal upwelling strength. Prominent cyst accumulation peaks representing extremely oligotrophic and stratified thermocline: conditions mimic the Greenland ice core and northern Atlantic Dansgaard/Oeschger stadials and Heinrich events. We provide new evidence for a coupled tropical/high-latitude Atlantic climate system during the last glacial period and suggest that changes in the zonality of the low-latitude winds may play an important role in modulating rapid interhemispheric climate variability.	Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; GEOMAR, Res Ctr Marine Geosci, D-24148 Kiel, Germany; Univ Bremen, Dept Geosci, Bremen, Germany	University of Bremen; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Bremen	Univ Bremen, Dept Geosci, POB 330440,Klagenfurter Str, D-28334 Bremen, Germany.	vink@micropal.uni-bremen.de; ruehl@uni-bremen.de; zonnev@uni-bremen.de; smul@geo.palmod.uni-bremen.de; mhuels@geomar.de; willems@uni-bremen.de	Vink, Annemiek/GXG-6435-2022; Mulitza, Stefan/G-5357-2011; Huels, Matthias/F-9228-2013	Vink, Annemiek/0000-0002-5178-9721; Mulitza, Stefan/0000-0002-3842-1447; Huels, Matthias/0000-0003-4259-2967				[Anonymous], USE PROXIES PALEOCEA, DOI DOI 10.1007/978-3-642-58646-0_12; [Anonymous], 1988, PROBLEM KLIMA NDERUN; [Anonymous], 1955, J GEOL; Arz HW, 1998, QUATERNARY RES, V50, P157, DOI 10.1006/qres.1998.1992; Arz HW, 1999, EARTH PLANET SC LETT, V167, P105, DOI 10.1016/S0012-821X(99)00025-4; BALSAM WL, 1995, PALEOCEANOGRAPHY, V10, P493, DOI 10.1029/95PA00421; BASSINOT FC, 1997, P OCEAN DRILL PROGRA, V154, P269; Behl RJ, 1996, NATURE, V379, P243, DOI 10.1038/379243a0; BINDER BJ, 1987, J PHYCOL, V23, P99; Blunier T, 1998, NATURE, V394, P739, DOI 10.1038/29447; Blunier T, 2001, SCIENCE, V291, P109, DOI 10.1126/science.291.5501.109; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; BOND G, 1992, NATURE, V360, P245, DOI 10.1038/360245a0; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; BOND GC, 1995, SCIENCE, V267, P1005, DOI 10.1126/science.267.5200.1005; Charles CD, 1996, EARTH PLANET SC LETT, V142, P19, DOI 10.1016/0012-821X(96)00083-0; CLARK PU, 1999, MECH GLOBAL CLIMATE, V112; Curry WB, 1997, PALEOCEANOGRAPHY, V12, P1, DOI 10.1029/96PA02413; DAMUTH JE, 1977, GEOL SOC AM BULL, V88, P695, DOI 10.1130/0016-7606(1977)88<695:LQSITW>2.0.CO;2; DANSGAARD W, 1993, NATURE, V364, P218, DOI 10.1038/364218a0; DANSGAARD W, 1985, PALAEOGEOGR PALAEOCL, V50, P185; Durkoop A, 1997, PALEOCEANOGRAPHY, V12, P764, DOI 10.1029/97PA02270; Elliot M, 1998, PALEOCEANOGRAPHY, V13, P433, DOI 10.1029/98PA01792; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; FONTUGNE MR, 1981, OCEANOL ACTA, V4, P85; Giraudeau J., 1992, Mem. 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J	Prauss, M				Prauss, M			Sea-level changes and organic-walled phytoplankton response in a Late Albian epicontinental setting, Lower Saxony basin, NW Germany	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Albian; palynology; sequence stratigraphy	KIRCHRODE-I BOREHOLE; CRETACEOUS-TERTIARY BOUNDARY; DINOFLAGELLATE CYSTS; SHAFTESBURY FORMATION; SEDIMENTS; BIOSTRATIGRAPHY; GEOCHEMISTRY; PALYNOLOGY; SEQUENCES; HANNOVER	Samples from a 245 in long core from the Upper Albian of NW Germany have been analysed palynologically. In accordance with the concept of 'sequence palynology' of Prauss (1993), two completed cycles of 3rd order sea level change are inferred, superimposed by a 2nd order cycle. During the 3rd order cycles the response of both the ratio of terrigenous sporomorphs to marine palynomorphs (t/m index) and dinoflagellate diversity shows a gradual decrease within the 'transgressive systems tracts'. The quantitative response of certain dinoflagellate taxa, however, is different within each 3rd order cycle. The abundance of skolochorate cysts increases strongly only during the earlier cycle. This difference is suggested to be a function of the 2nd order cycle, which is transgressive during most of the earlier 3rd order cycle but regressive throughout the later one. The layer at about 135 in is interpreted to represent the 'maximum flooding surface' of the 2nd order cycle. The succession in peak abundance of the dinoflagellate genera Oligosphaeridium --> Surculosphaeridium --> Pterodinitun may characterise a 'transgressive systems tract' to 'early highstand systems tract' interval during a 3rd order cycle. However, the proportions of Surculosphaeridium respond much more distinctly to the 2nd order sea level changes, being highest during the corresponding 'maximum flooding surface'. Higher proportions of Palaeoperidinium cretaceum may indicate enhanced primary productivity and/or estuarine circulation during transgressive and advanced 'late highstand' conditions. With respect to water mass characteristics within the photic zone, no clear dominance of Tethyan or Arctic waters is distinguishable, based on dinoflagellate taxa. A rather mixed water mass dominated by cosmopolitan and 'Boreal' taxa seems to be present throughout most of the section. The influence of warmer water masses, largely indicated by the proportion of skolochorate cysts, is enhanced during each transgressive interval of the 3rd order cycles, but it is less well developed within the 'transgressive systems tract' at the top of the section. It is suggested that a strong Tethyan influence, in terms of water mass introduction into the NW German basin, was predominant only during the transgressive pulse of the 2nd order cycle. Above 135 in the Tethyan or warm water influence is considered largely as a function of oceanic circulation rather than sea level rise, but is episodically enhanced during the relatively weak pulses of 3rd order transgressions. Certain dinoflagellate taxa, known from the Upper Albian Arctic region (Vesperopsis mayii, Luxadinium primulum, L. propatulum, Luxadinium cf. L. primulum) are absent. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Gottingen, Inst Geol & Palaeontol, D-37077 Gottingen, Germany	University of Gottingen	Univ Gottingen, Inst Geol & Palaeontol, Goldschmidtstr 3, D-37077 Gottingen, Germany.	mpraus@gwdg.de						ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; [Anonymous], 1979, ECOLOGICAL PROCESSES; [Anonymous], 2000, Gottinger Arbeiten Zur Geologie Und Palaontologie; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; *BCCP GROUP, 1994, ZENTRALBLATT GEOLO 1, P809; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRIDEAUX W. 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Paleoclimatol. Paleoecol.	SEP 20	2001	174	1-3			SI		221	249		10.1016/S0031-0182(01)00295-4	http://dx.doi.org/10.1016/S0031-0182(01)00295-4			29	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	485ED					2025-03-11	WOS:000171739800012
J	Keupp, H				Keupp, H			Palaeoenvironmental interpretation of Late Albian calcareous dinoflagellate cysts from the Kirchrode I borehole (Lower Saxony basin, NW Germany)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						cretaceous; pycnocline; calcareous dinoflagellates		Late Albian calcareous dinoflagellate cyst assemblages from samples of the Kirchrode I borehole contains 38 morphospecies, which represent a flora of moderate warm water conditions in an oceanic-controlled epicontinental regime. The vertical changes of cyst associations reflect sea level fluctuations. The regressive phases of the highstand are characterised by the exclusive occurrence of benthic resting cysts, while planktonic counterparts joined during transgressive phases. Floral exchanges via the water masses, which were influenced by the Tethys, were in progress only during phases of relatively strong currents, in particular during transgressions. In contrast, the highstand, during which water circulation decreased, can be characterised by autochthonous morphotypes, reflecting an epicontinental habitat. The corresponding cyclic, intraspecies change of cyst diameter is interpreted to reflect changes in productivity, which were probably controlled by eccentricity cycles. (C) 2001 Elsevier Science B.V. All rights reserved.	Free Univ Berlin, Inst Palaeontol, D-12249 Berlin, Germany	Free University of Berlin	Keupp, H (通讯作者)，Free Univ Berlin, Inst Palaeontol, Malteserstr 74-100,House D, D-12249 Berlin, Germany.							BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Bolli H.M., 1974, Initial Rep Deep Sea Drilling Project, V27, P843; Bujak J.P, 1983, AM ASS STRATIGRAPHIC, V13, P203; Cepek P, 2001, PALAEOGEOGR PALAEOCL, V174, P181; Esper O, 2000, INT J EARTH SCI, V88, P680, DOI 10.1007/s005310050297; FENNER F, 1996, VIR INF VER, V6, P5; Fenner J, 2001, PALAEOGEOGR PALAEOCL, V174, P33, DOI 10.1016/S0031-0182(01)00286-3; Fenner J, 2001, PALAEOGEOGR PALAEOCL, V174, P5, DOI 10.1016/S0031-0182(01)00285-1; Fensome R.A., 1993, CLASSIFICATION FOSSI; HESSELBO SP, 1990, J GEOL SOC LONDON, V147, P549, DOI 10.1144/gsjgs.147.3.0549; JANOFSKE D, 1995, J NANNOPLANKTON RES, V17, P64; JANOFSKE D, 1992, BERLINER GEOWISS A E, V4; Jendrzejewski L, 2001, PALAEOGEOGR PALAEOCL, V174, P107, DOI 10.1016/S0031-0182(01)00289-9; Kaufmann FJ, 1865, URWELT SCHWEIZ, P194; Keupp H., 1992, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V3, P211; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P127; Keupp H., 1987, Facies, V16, P37, DOI 10.1007/BF02536748; Keupp H., 1981, Facies, V5, P1, DOI 10.1007/BF02536655; Keupp H., 1980, Facies, V2, P123, DOI 10.1007/BF02536464; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P161; Keupp H., 1979, Bericht der Naturhistorischen Gesellschaft zu Hannover, V122, P7; Keupp H., 1984, Facies, V10, P153, DOI 10.1007/BF02536691; KEUPP H, 1994, CRETACEOUS RES, V15, P739, DOI 10.1006/cres.1994.1040; KEUPP H, 1990, CALCAREOUS ALGAE STR, P267; Keupp H., 1982, GEOLOGISCHES JB A, V65, P307; Keupp Helmut, 1992, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V3, P121; Keupp Helmut, 1993, Zitteliana, V20, P25; Keupp Helmut, 1995, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V16, P155; Keupp Helmut, 1994, Abhandlungen der Geologischen Bundesanstalt (Vienna), V50, P197; KIENL U, 1994, BERLINER GEOWISS A E, V12; KOHRING R, 1993, BERLINER GEOWISS E, V6; MONNET B, 1993, BERLINER GEOWISS A E, V75; NEUMANN C, 1999, BERLINER GEOWISS A E, V31; PFLAUMANN U, 1978, INITIAL REPORTS DEEP, V41, P817; Prauss M, 2001, PALAEOGEOGR PALAEOCL, V174, P221, DOI 10.1016/S0031-0182(01)00295-4; Prauss M.L., 1993, Neues Jahrbuch fur Geologie und Palaontologie Abhandlungen, V190, P143; Prokoph A, 2001, PALAEOGEOGR PALAEOCL, V174, P67, DOI 10.1016/S0031-0182(01)00287-5; PROKOPH A, 1994, TUBINGER GEOWISS A A, V19; Rachold V, 2001, PALAEOGEOGR PALAEOCL, V174, P121, DOI 10.1016/S0031-0182(01)00290-5; RACHOLD VE, 1994, THESIS U GOTTINGEN; THUROW J, 1994, ZENTRALBL GEOL PALAO, V7, P809; Villain J.-M., 1981, CRETACEOUS RES, V2, P435; Wiedmann J, 2001, PALAEOGEOGR PALAEOCL, V174, P161, DOI 10.1016/S0031-0182(01)00292-9; ZUGEL P, 1994, COUR FORSCH I SENCKE, V176	44	11	12	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	SEP 20	2001	174	1-3			SI		251	267		10.1016/S0031-0182(01)00296-6	http://dx.doi.org/10.1016/S0031-0182(01)00296-6			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	485ED		Bronze			2025-03-11	WOS:000171739800013
J	Boessenkool, KP; Brinkhuis, H; Schönfeld, J; Targarona, J				Boessenkool, KP; Brinkhuis, H; Schönfeld, J; Targarona, J			North Atlantic sea-surface temperature changes and the climate of western Iberia during the last deglaciation;: a marine palynological approach	GLOBAL AND PLANETARY CHANGE			English	Article; Proceedings Paper	Workshop on Rapid Climatic Warming at the End of the Last Glacial - Palaeodata Analysis and Climate Modeling	FEB 22-24, 2000	HAARLEM, NETHERLANDS	NRP		sea-surface temperature; northeast Atlantic; palynology; paleoclimate; upper Quaternary; Iberian Peninsula	NORTHEASTERN ATLANTIC; DINOFLAGELLATE CYSTS; PORTUGUESE MARGIN; ADJACENT SEAS; OCEAN; SEDIMENTS; RECORDS; ICE; VEGETATION; SALINITY	Sea-surface temperature (SST) variations based on delta O-18 and dinoflagellate cyst records in core SO75-6KL indicate that shifts in the position of the North Atlantic polar front during the last deglaciation led to sudden changes of the SST in the offshore area of Portugal. Our data show that the onset of the two major cooling events, attributed to Heinrich event 1 (H1) and the Younger Dryas (YD), occurred within 600 and 400 years, respectively. The first-order land-sea correlation, provided by the pollen record of SO75-6KL, enables a detailed evaluation of the response of the vegetation on land to altered heat and moisture transport from the North Atlantic Ocean toward SW Europe. The expansion of aridity-tolerant vegetation, as reflected in the pollen record of steppe taxa, occurred within 350 and 180 years from the onset of the cooling events connected to H1 and the YD, respectively. The inception of the warmer interval assigned to the Bolling-Allerod Interstadial shows a less sudden response, probably due to competition or to the lower migration rates for deciduous trees such as Quercus compared to most steppe taxa. (C) 2001 Elsevier Science BN. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; GEOMAR Res Ctr Marine Geosci, D-24148 Kiel, Germany; Univ Barcelona, Grup Recerca Consolidat Geol Marina, E-08028 Barcelona, Spain	Utrecht University; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Barcelona	Boessenkool, KP (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610; Boessenkool, Karin/0000-0003-0887-4864				Allen JRM, 1996, J QUATERNARY SCI, V11, P125, DOI 10.1002/(SICI)1099-1417(199603/04)11:2<125::AID-JQS232>3.0.CO;2-U; [Anonymous], 1984, POLLEN SPORES; [Anonymous], 2007, Paleopalynology; AUSTIN WEN, 1995, RADIOCARBON, V37, P53, DOI 10.1017/S0033822200014788; BARD E, 1987, NATURE, V328, P791, DOI 10.1038/328791a0; BOND G, 1992, NATURE, V360, P245, DOI 10.1038/360245a0; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DUPLESSY JC, 1981, PALAEOGEOGR PALAEOCL, V35, P121, DOI 10.1016/0031-0182(81)90096-1; FOLLAND CK, 1986, NATURE, V320, P602, DOI 10.1038/320602a0; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head M.J., 1996, Palynology: Principles and Applications, P1197; Huntley B., 1983, ATLAS PRESENT POLLEN, P688; Kroon D, 1997, PALEOCEANOGRAPHY, V12, P755, DOI 10.1029/97PA02289; LAMB HF, 1995, NATURE, V373, P134, DOI 10.1038/373134a0; LOWE JJ, 1994, J QUATERNARY SCI, V9, P185, DOI 10.1002/jqs.3390090215; MASLIN MA, 1995, PALEOCEANOGRAPHY, V10, P527, DOI 10.1029/94PA03040; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Pons A., 1986, QUATEMARY CLIMATE W, P405; Rognon P., 1987, ABRUPT CLIMATE CHANG, P209; RUDDIMAN WF, 1981, PALAEOGEOGR PALAEOCL, V35, P145; RUDDIMAN WF, 1977, GEOL SOC AM BULL, V88, P1813, DOI 10.1130/0016-7606(1977)88<1813:LQDOIS>2.0.CO;2; Schönfeld J, 2000, PALAEOGEOGR PALAEOCL, V159, P85, DOI 10.1016/S0031-0182(00)00035-3; TARGARONA J, 1997, LPP CONTRIBUTIONS SE, V7; TURNER C, 1988, PHILOS T ROY SOC B, V318, P451, DOI 10.1098/rstb.1988.0019; vanderKnaap WO, 1997, REV PALAEOBOT PALYNO, V97, P239, DOI 10.1016/S0034-6667(97)00008-0; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS GL, 1998, LENTIN WILLIAMS INDE; Zahn R, 1997, PALEOCEANOGRAPHY, V12, P696, DOI 10.1029/97PA00581; ZAHN R, 1997, THESIS GEOMAR KIEL	30	47	55	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0921-8181			GLOBAL PLANET CHANGE	Glob. Planet. Change	SEP	2001	30	1-2			SI		33	39		10.1016/S0921-8181(01)00075-3	http://dx.doi.org/10.1016/S0921-8181(01)00075-3			7	Geography, Physical; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	478DX					2025-03-11	WOS:000171328600004
J	Godhe, A; Norén, F; Kuylenstierna, M; Ekberg, C; Karlson, B				Godhe, A; Norén, F; Kuylenstierna, M; Ekberg, C; Karlson, B			Relationship between planktonic dinoflagellate abundance, cysts recovered in sediment traps and environmental factors in the Gullmar Fjord, Sweden	JOURNAL OF PLANKTON RESEARCH			English	Article							ULTRAVIOLET-RADIATION; NATURAL PHYTOPLANKTON; SPRING-BLOOM; DINOPHYCEAE; ENCYSTMENT; SCRIPPSIELLA; GROWTH; LAKE; TEMPERATURE; ASSEMBLAGES	In order to study the relationship between planktonic dinoflagellates, cyst production and environmental factors,a sediment trap study was conducted in the Gullmar Fjord, Swedish West coast, during 21 days in May-June 1998. Five locations for sediment traps were randomly selected every third day. The traps were moored at the five locations and moved to new locations after 3 days. At every location, a CTD depth profile was obtained and Water samples were collected for plankton, chlorophyll a and nutrient analysis. Meteorological and hydrographic data for the period were obtained from continuous monitoring. Three dinoflagellate species, which have not previously been recorded from the Kattegat or the Skagerrak (Scrippsiella crystallina, Scrippsiella lachrymosa and Scrippsiella trifida), were encountered during the analysis of cysts from. the sediment traps. The abundance of the different species in the motile form encountered in the water column and cyst form encountered in the sediment traps varied greatly. The discrepancy between the number and species encountered in traps and water samples is discussed. No density-dependent relationship between the abundance of planktonic gst-forming dinoflagellates and the number of cysts recovered could be observed. A multiple regression showed that the variation in cyst yield from the traps for the most abundant species was correlated with water sur a,face temperature, ambient light radiation and the depth of the halocline. The nutrient concentrations (NH4+, NO2-, NO3- and PO43-), which are known to play a crucial role in induction of sexuality and cyst formation. under laboratory conditions, correlated poorly with the number of dinoflagellate cysts encountered in the traps.	Univ Gothenburg, Inst Bot, Dept Marine Bot, SE-40530 Gothenburg, Sweden; Chalmers Univ Technol, Dept Nucl Chem, SE-41296 Gothenburg, Sweden	University of Gothenburg; Chalmers University of Technology	Godhe, A (通讯作者)，Univ Gothenburg, Inst Bot, Dept Marine Bot, Box 461, SE-40530 Gothenburg, Sweden.		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Plankton Res.	SEP	2001	23	9					923	938		10.1093/plankt/23.9.923	http://dx.doi.org/10.1093/plankt/23.9.923			16	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	477MF					2025-03-11	WOS:000171286800002
J	Mudie, PJ; Aksu, AE; Yasar, D				Mudie, PJ; Aksu, AE; Yasar, D			Late Quaternary dinoflagellate cysts from the Black, Marmara and Aegean seas: variations in assemblages, morphology and paleosalinity	MARINE MICROPALEONTOLOGY			English	Article						sea surface salinity; Quaternary; dinocyst morphology; Black Sea; Marmara Sea; Aegean Sea	MARINE-SEDIMENTS; CHRONOLOGY; SALINITY; HISTORY; POLLEN	The link between sea surface salinity (SSS) and dinoflagellate cyst morphology was studied quantitatively in cores of Late Quaternary mud from the Black, Marmara and Aegean seas, where oxygen isotopic and planktonic foraminiferal data show salinities of about 5-19, 15-22 and 36-39 ppt, respectively. In the Black Sea, late glacial muds contain low-diversity assemblages of the cruciform species Spiniferites cruciformis and Pyxidinopsis psilata, with most S. cruciformis cysts having expanded septal membranes (form 1: circular outline, form 2: irregular). The assemblage is associated with surface salinities of <7 ppt. Overlying sapropelic muds have salinity estimates of similar to 14-18 ppt and contain Lingulodinium machaerophorum-Spiniferites-Cymatiosphaera assemblages, with many L. machaerophorum cysts having short processes and S. cruciformis with reduced septa (forms 3, 4 and 5). The late Holocene coccolith-rich sediments, with salinity of similar to 18-20 ppt, have diverse assemblages of Brigantedinium, Peridinium ponticum and other protoperidinioids, together with normal cysts of L machaerophorum and Operculodinium centrocarpum (sensu Wall and Dale (1966), Nature 211, 1025-1026) that bear long processes. In the northeast Aegean core, stenohaline species and morphotypes are rare, occurring only as low percentages of S. cruciformis forms 3 and 4, and O. centrocarpum var. 'truncatum' in a mid-Holocene sapropel that was deposited during a period of high runoff and Black Sea water outflow. Marmara Sea cores record surface salinities of 14-18 ppt during late glacial sapropel deposition and 20-22 ppt for the overlying marine sediments. The sapropel is dominated by S. cruciformis forms I and 2 and by P. psilata, with common L. machaerophorum (clavate and normal forms). In surface sediments, L. machaerophorum is co-dominant with O. centrocarpum (normal and truncate forms), Brigantedinium and Spiniferites spp. Percentages of S. cruciformis (five forms) and L. machaerophorum (two forms) plotted against proxy-salinity data, however, show no clear correlation, indicating that morphological variation is not a simple function of salinity. (C) 2001 Elsevier Science B.V. All rights reserved.	Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada; Dokuz Eylul Univ, Inst Marine Sci & Technol, TR-35340 Izmir, Turkey	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland; Dokuz Eylul University	Geol Survey Canada Atlantic, Box 1006, Dartmouth, NS B2Y 4A2, Canada.	mudie@agc.bio.ns.ca; aaksu@sparky2.esd.mun.ca	Yasar, Dogan/AAC-1866-2020					AKSU AE, 1995, MAR GEOL, V123, P33, DOI 10.1016/0025-3227(95)80003-T; Aksu AE, 1999, MAR GEOL, V153, P275, DOI 10.1016/S0025-3227(98)00078-4; AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; AKSU AW, 1999, P EM COMM WORKSH LAN; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; Crusius J, 1992, PALEOCEANOGRAPHY, V7, P215, DOI 10.1029/92PA00279; Dale B., 1988, 7 INT PAL C BRISB, P33; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DEMETRESCU E, 1989, REV PALAEOBOT PALYNO, V59, P51, DOI 10.1016/0034-6667(89)90005-5; DEUSER WG, 1972, J GEOPHYS RES, V77, P1071, DOI 10.1029/JC077i006p01071; DUMAN M, 1994, GEO-MAR LETT, V14, P272, DOI 10.1007/BF01274063; DUMAN M, 1992, THESIS DOKUZ EYLUL U, P1; Eaton GL, 1996, REV PALAEOBOT PALYNO, V91, P151, DOI 10.1016/0034-6667(95)00073-9; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Head M. 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Micropaleontol.	SEP	2001	43	1-2					155	178		10.1016/S0377-8398(01)00006-8	http://dx.doi.org/10.1016/S0377-8398(01)00006-8			24	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	479PQ					2025-03-11	WOS:000171413100007
J	Kloosterboer-van Hoeve, ML; Steenbrink, J; Brinkhuis, H				Kloosterboer-van Hoeve, ML; Steenbrink, J; Brinkhuis, H			A short-term cooling event, 4.205 million years ago, in the Ptolemais Basin, northern Greece	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						climate; palynology; sedimentology; lacustrine sediments; Pliocene; Greece	AEGEAN SEA	A distinct clay-rich layer in the otherwise regular succession of alternating lignites and marls of the early Pliocene Ptolemais Formation reveals an equally distinct palynomorph assemblage; only in this layer (fresh water) dinoflagellate cysts, Spiniferites cruciformis and Gonyaulax apiculata, are encountered. These co-occurring dinoflagellate species may be taken to indicate that surface water temperatures must have been remarkably low for early Pliocene mid-latitudes, contrasting other indications that overall warm humid climates prevailed at this time. A multi-component study of this so-called 'dinolayer' with an astrochronologically derived age of 4.205 +/- 0.01 Ma was undertaken to further investigate the apparently contrasting climatic signals. Integrated sedimentological, micropaleontological, palynological and geochemical data indicate that the dinolayer was deposited in a shallow fresh water lake. The pollen record points to slightly cooler conditions during deposition of the dinolayer in comparison with conditions just below and above. An anomalously low winter temperature is proposed as a possible cause for the recorded phenomena. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, Fac Biol, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Dept Geol, Fac Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; Utrecht University	Univ Utrecht, Palaeobot & Palynol Lab, Fac Biol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	m.l.vanhoeve@bio.uu.nl	Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				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; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; Anastopoulos J.C, 1972, GEOL GEOPHYS RES, VXVI, P1; [Anonymous], 1963, POST PALAEOZOIC OSTR; [Anonymous], 2000, 385 US GEOL SURV; BOHNCKE S, 1988, BOREAS, V17, P403; BOURRELLY P, 1980, Cryptogamie Algologie, V1, P161; DANIELOPOL DL, 1993, 2 EUR OSTR M, P84; DOBLER F, 1991, THESIS G AUGUST U, P80; EHLERS E, 1960, BERICHT BISHER RAHME, P1; EVITT WR, 1985, REV PALAEOBOT PALYNO, V45, P35, DOI 10.1016/0034-6667(85)90064-8; GRAMANN A, 1960, FOSSILIEN BRAUNKOHLE, P37; GRIFFITHS HI, 1995, OSTRACODA AND BIOSTRATIGRAPHY, P291; HOEVE MLK, 2000, THESIS U UTRECHT; HUBERPESTRALOZZ.G, 1968, PHYTOPLANKTON SUSSWA; KAOURAS G, 1989, THESIS G AUGUST U GO; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; Larcher W., 1981, Components of productivity of Mediterranean-climate regions. Basic and applied aspects, P259; LASKAR J, 1990, ICARUS, V88, P266, DOI 10.1016/0019-1035(90)90084-M; Lourens LJ, 1996, PALEOCEANOGRAPHY, V11, P391, DOI 10.1029/96PA01125; Mai D.H., 1995, Tertiare Vegetationsgeschichte Europas; MEYERS PA, 1995, PHYSICS CHEM LAKES, P276; MUDIE PJ, 2001, IN PRESS MAR MICROPA; MUDIE PJ, 1998, MUS RAPP BOT SER, V1; PAPAKONSTANTINO.A, 1979, BERLINER GEOWISS ABH, V13, P1; RIEGEL W, 1994, PALYNOLOGY, V18, P258; Salvi G, 1995, ATTI MUS GEOL PALEON, V3, P81; Shackleton N.J., 1995, Proc. Ocean Drill. Program, V138, P73, DOI [DOI 10.2973/ODP.PROC.SR.138.106.1995, 10.2973/odp.proc.sr.138.106.1995.]; SHACKLETON NJ, 1989, P OC DRILL PROGR SCI, V111, P285; Steenbrink J, 1999, PALAEOGEOGR PALAEOCL, V152, P283, DOI 10.1016/S0031-0182(99)00044-9; TIEDEMANN R, 1994, PALEOCEANOGRAPHY, V9, P619, DOI 10.1029/94PA00208; TYSON RV, 1995, DISTRIBUTION PALYNOM, P309; Van de Weerd A., 1983, Geologischen Jahrbuch B, V48, P3; van Vugt N, 1998, EARTH PLANET SC LETT, V164, P535, DOI 10.1016/S0012-821X(98)00236-2; VANDEWEERD A, 1979, P K NED AKAD B PHYS, V82, P127; VELITZELOS E, 1990, REV PALAEOBOT PALYNO, V62, P291, DOI 10.1016/0034-6667(90)90092-W; VETOULIS DG, 1957, ANN GEOL PAYS HELL, V8, P48; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Wall D., 1973, Geoscience Man, V7, P95; Wall D., 1974, BLACK SEA GEOLOGY CH, V20, P364	41	13	13	0	1	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	SEP 1	2001	173	1-2					61	73		10.1016/S0031-0182(01)00314-5	http://dx.doi.org/10.1016/S0031-0182(01)00314-5			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	472MH					2025-03-11	WOS:000170987600005
J	Dale, B				Dale, B			The sedimentary record of dinoflagellate cysts: looking back into the future of phytoplankton blooms	SCIENTIA MARINA			English	Article						dinoflagellate cysts; algal blooms; eutrophication; molecular genetics; paleoceanography; transfer functions	NORWEGIAN FJORD; INDICATORS; EUTROPHICATION; POLLUTION; NORWAY	Marine systems are not as well understood as terrestrial systems, and there is still a great need for more primary observations, in the tradition of the old-time naturalists, before newer methods such as molecular genetics and modeling can be fully utilized. The scientific process whereby the smaller, detailed "building blocks" of observation are ultimately linked towards better understanding natural systems is illustrated from my own career experience, especially with regard to the dinoflagellates and plankton blooms. Some dinoflagellates produce a fossilizable resting stage (cyst) in their life cycle, and dinoflagellate cysts have become one of the most important groups of microfossils used in geological exploration (e.g. oil and gas). This has stimulated both paleontological and biological research producing detailed "building blocks" of information, currently scattered throughout the respective literature. Here, I attempt to bring together the present day perspective, from biology, with the past, from paleontology, as the most comprehensive basis for future work on the group. This shows the cysts to be the critical link needed for focusing future molecular genetics studies towards a more verifiable view of evolutionary pathways, and it also suggests new integrated methods for studying past, present, and future blooms. The large, rapidly growing field of harmful algal bloom studies is producing many different "building blocks", but plankton blooms as episodic phenomena are still poorly understood. This is largely due to the general lack of long-term datasets allowing identification of the changing environmental factors that permit certain species to bloom at unpredictable intervals of time. Cysts in sediments are useful environmental indicators today, e.g. reflecting aspects of climate and pollution, and provide information directly relevant to some dinoflagellate blooms. They therefore may be used for obtaining retrospective information from the sedimentary record on the history of blooms, in turn suggesting information relevant for future blooms and the way we study them.	Univ Oslo, Dept Geol, N-0316 Oslo, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Dept Geol, POB 1047 Blindern, N-0316 Oslo, Norway.							[Anonymous], 1987, BOT MONOGR; [Anonymous], 1980, MICROFOSSILS; [Anonymous], 1996, Palynology: principles and applications; DALE AL, IN PRESS QUATERNARY; Dale B., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; DALE B, 1978, Palynology, V2, P187; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B, IN PRESS QUATERNARY; DALE B, 2000, ENV MICROPALEONTOLOG, P305; DALE B, 2000, 9 INT C HARMF ALG BL; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P158, DOI 10.1073/pnas.49.2.158; Fensome R.A., 1993, CLASSIFICATION FOSSI; Imbrie J., 1971, LATE CENOZOIC GLACIA, P71; JANNASCH HW, 1997, ANNU REV MICROBIOL, P5; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; REGUERA B, 1998, HARMFUL ALGAE; SAETRE MLL, 2001, DINOFLAGELLATE CYSTS; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Thorsen TA, 1998, PALAEOGEOGR PALAEOCL, V143, P159, DOI 10.1016/S0031-0182(98)00079-0; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Van Der Hamen T., 1971, The Late Cenozoic Glacial Ages, P391; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; 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	97	104	0	25	INST CIENCIAS MAR BARCELONA	BARCELONA	PASSEIG JOAN DE BORBO, 08039 BARCELONA, SPAIN	0214-8358			SCI MAR	Sci. Mar.	SEP	2001	65			2			257	272		10.3989/scimar.2001.65s2257	http://dx.doi.org/10.3989/scimar.2001.65s2257			16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	480LJ		Green Submitted, gold			2025-03-11	WOS:000171462600020
J	Marangoni, C; Pienaar, RN; Sym, SD				Marangoni, C; Pienaar, RN; Sym, SD			Possible introduction of alien phytoplankton via shipping ballast water: A South African perspective	SOUTH AFRICAN JOURNAL OF BOTANY			English	Article; Proceedings Paper	Meeting on Marine Botany in the Western Indian Ocean	DEC 12-16, 2000	MAPUTO, MOZAMBIQUE				DINOFLAGELLATE CYSTS; NEW-ZEALAND; SEDIMENTS; TRANSPORT	Saldanha Bay is one of a few sites along the South African coast that is suitable for both shipping and mariculture. Ships visiting Saldanha Bay carry ballast water which, although essential, has been implicated in the transport of alien organisms. This study investigates the possible introduction of alien phytoplankton into Saldanha Bay by ballast water. The phytoplankton composition of Saldanha Bay was determined by collecting seasonal samples. Most of the 173 taxa encountered belonged to the Bacillariophyta (diatoms) and Dinophyta (dinoflagellates). The greatest species diversity in the water column was encountered during summer and autumn, but the greatest diversity of encysted organisms in the bottom sediment was encountered during winter. A catalogue of all organisms encountered was prepared to serve as a baseline for future investigations in the area. Ballast water samples, collected from 36 ships, were dominated by diatoms (64 species). Only 9 cosmopolitan species were found to be common to both the ballast waters and Saldanha Bay samples implying that the ballast water discharged into the area is not introducing any foreign organisms capable of establishing new populations. To obtain a more accurate assessment of this threat to South Africa, the methods of sampling ballast waters needs to be re-examined. Other ports also need to be investigated, especially Richards Bay, South Africa's busiest port. Ballast water introductions of phytoplankton, seaweeds or animals into this species rich area could have damaging ecological and economic consequences.	Univ Witwatersrand, Sch Anim Plant & Environm Sci, ZA-2050 Wits, South Africa	University of Witwatersrand	Marangoni, C (通讯作者)，Univ Witwatersrand, Sch Anim Plant & Environm Sci, Private Bag 3, ZA-2050 Wits, South Africa.							[Anonymous], IOC MANUALS GUIDES; BALDWIN RP, 1992, J ROY SOC NEW ZEAL, V22, P229, DOI 10.1080/03036758.1992.10420818; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; 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; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hasle G.R, 1978, Phytoplankton manual, P136; HAY CH, 1990, BRIT PHYCOL J, V25, P301, DOI 10.1080/00071619000650331; HERBERT PDN, 1990, CAN J ZOOL, V69, P405; JACKSON LF, 1993, 3 NAT MAR C DURB S A; JONES MM, 1991, 11 BUR RUR RES; KELLY JM, 1993, J SHELLFISH RES, V12, P405; MARANGONI C, 1998, THESIS U WITWATERSRA; MARIN B, 1994, J PHYCOL, V30, P659, DOI 10.1111/j.0022-3646.1994.00659.x; McLachlan J., 1973, Handbook of Phycological Methods, Culture Methods and Growth Measurements, P25; MONTEIRO PMS, 1990, S AFR J SCI, V86, P454; MONTEIRO PMS, 1996, P AQUACULT ASS S AFR, V5, P16; Pitcher G. C., 1998, HARMFUL ALGAL BLOOMS; PITCHER GC, 1996, P AQUACULT ASS S AFR, V5, P87; Taylor F.J.R., 1978, PHYTOPLANKTON MANUAL, P143; WILLIAMS RJ, 1988, ESTUAR COAST SHELF S, V26, P409, DOI 10.1016/0272-7714(88)90021-2; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	23	14	14	1	7	BUREAU SCIENTIFIC PUBL	PRETORIA	P O BOX 1758, PRETORIA 0001, SOUTH AFRICA	0254-6299			S AFR J BOT	S. Afr. J. Bot.	SEP	2001	67	3					465	474		10.1016/S0254-6299(15)31165-0	http://dx.doi.org/10.1016/S0254-6299(15)31165-0			10	Plant Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	502CU		hybrid			2025-03-11	WOS:000172726800015
J	Iakovleva, AI; Brinkhuis, H; Cavagnetto, C				Iakovleva, AI; Brinkhuis, H; Cavagnetto, C			Late Palaeocene-Early Eocene dinoflagellate cysts from the Turgay Strait, Kazakhstan; correlations across ancient seaways	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palaeocene-Eocene; Sokolovskaya and Polosataya formations; Turgay Trough; Northern Kazakhstan; dinoflagellate cysts; biostratigraphy; sequence stratigraphy; late Palaeocene thermal maximum	NORTH-SEA; BIOSTRATIGRAPHY; STRATIGRAPHY	The results of a quantitative palynological analysis, emphasizing organic-walled dinoflagellate cysts (dinocysts), of Palaeocene-Eocene deposits exposed in the Sokolovsky Quarry (Turgay Trough, Northern Kazakhstan) are presented here. Located in the ancient Turgay Strait, a former seaway presumed to have connected the Tethyan and Boreal oceans and seas in the early Palaeogene, the Sokolovsky Quarry outcrop occupies a key position for the analysis of connections between these realms. In general, the dinocyst succession of Sokolovsky closely resembles coeval Arctic Ocean-North Sea Basin counterparts; only in one interval endemic and/or possibly Tethyan species co-occur. The successive dinocyst assemblages allow recognition of the Late Palaeocene-Early Eocene P5a, P5b, P6a, P6b and E2 zones established in the North Sea Basin. The succession is interpreted to represent parts of several third-order sea level cycles correlative with those recognised in the North Sea Basin. Detailed comparison with similar studies from southeastern England allows the recognition of (parts of) third order cycles Thanetian-1 (Tht-1), 2, 4, 5, and Ypresian (Ypr)-3. In addition, two important stratigraphic gaps within the Palaeocene-Eocene succession are recognised, possibly reflecting times of sea level lowering. These gaps are inferred from (1) the absence of a complete P5b/P6a transition, (2) the absence of zone El, and (3) (bio)sequence stratigraphy. Combined results indicate that the Turgay Strait flooded from the north between similar to 57.8 and 57.1 Ma (cycles Tht-1 and 2, in part, with a minor missing section). During the 'second' phase of Turgay-flooding (similar to 56.4-55.3 Ma), evidence may be taken to indicate increased influence from the Tethyan Ocean and/or warmer conditions. Deposits reflecting the Late Palaeocene Thermal Maximum, associated with this interval, are present at Sokolovsky Quarry. This interval is marked by abundant Apectodinium spp., including A. augustum, and organic-rich layers. A third flooding is correlative to the London Clay transgression (from similar to 54.5 Ma). From our study, no decisive evidence has become available that confirms that a connection between the Arctic and Tethyan oceans via the Turgay Strait in the early Palaeogene existed. Nevertheless, during intervals of major sea level fall, the Turgay Strait depression may be regarded to have been an important feature for migrating terrestrial biota. Four new wetzeliellioid taxa Apectodinium sp. A, Apectodinium sp. B, Wilsonidium? sp. A and Wilsonidium? sp. B are described from the Palaeocene part of the section. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, Sect Bot Paleoecol, NL-3584 CD Utrecht, Netherlands; Russian Acad Sci, Inst Geol, Palaeoflorist Lab, Moscow 109017, Russia; Univ Montpellier 2, ISEM, UMR CNRS 5554, Lab Paleoenvironm & Palynol, F-34095 Montpellier, France	Utrecht University; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier	Brinkhuis, H (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Sect Bot Paleoecol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		IAKOVLEVA, ALINA/ABH-9243-2020; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				ANDREEVAGRIGORO.AS, 1991, THESIS GEOLOGICAL I; [Anonymous], 2003, STUD GEOPHYS GEOD; BENYAMOVSKY VN, 1989, IZV VYSSH UCHEBN ZAV, V10, P3; BENYAMOVSKY VN, 1991, IZV VYSSH UCHEBN ZAV, V7, P3; BERGGREN WA, 1995, SEPM SPEC PUBL, V54; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Crouch EM, 2000, GFF, V122, P40, DOI 10.1080/11035890001221040; ERDTMANN G, 1943, INTRO POLLEN ANAL; GROSSHEIM VA, 1975, STRATIGRAPHY USSR; Heilmann-Clausen C, 2000, GFF, V122, P69, DOI 10.1080/11035890001221069; Heilmann-Clausen C, 1994, GFF, V116, P51, DOI 10.1080/11035899409546149; HEILMANNCLAUSEN C, 1985, GEOL SURV DENMARK A, V7; IAKOVLEVA AI, 2000, THESIS U MONTPELLIER; LAVROV VV, 1957, MARINE PALAEOGENE UR; MUDGE DC, 1994, MAR PETROL GEOL, V11, P166, DOI 10.1016/0264-8172(94)90093-0; Mudge DC, 1996, MAR PETROL GEOL, V13, P295, DOI 10.1016/0264-8172(95)00066-6; OVECHKIN NK, 1954, PALAEOGENE SEDIMENTS; OVECHKIN NK, 1962, T VSEGEI, P3; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Powell A.J., 1992, P155; RADIONOVA EP, 2001, B SGF, V1720; Schmitz B., 2000, GFF, V122; VASILEVA ON, 1994, PALINOLOGICHESKIE KR, P109; WILLIAMS GL, 1998, AASP CONTRIBUTIONS S, V34; Yanshin AL, 1953, GEOLOGY N ARAL REGIO; ZACHOS JC, 1993, J GEOL, V101, P191, DOI 10.1086/648216	28	86	93	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	AUG 15	2001	172	3-4					243	268		10.1016/S0031-0182(01)00300-5	http://dx.doi.org/10.1016/S0031-0182(01)00300-5			26	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	467AY					2025-03-11	WOS:000170679400005
J	Coyne, KJ; Hutchins, DA; Hare, CE; Cary, SC				Coyne, KJ; Hutchins, DA; Hare, CE; Cary, SC			Assessing temporal and spatial variability in <i>Pfiesteria piscicida</i> distributions using molecular probing techniques	AQUATIC MICROBIAL ECOLOGY			English	Article						Pfiesteria; harmful algal blooms; PCR-FFD; DGGE; Delaware Inland Bays; Broadkill River; Pocomoke River; sediments; cysts	AMBUSH-PREDATOR DINOFLAGELLATE; 16S RIBOSOMAL-RNA; PHANTOM DINOFLAGELLATE; ENVIRONMENTAL CONTROLS; FISH KILLS; PCR; DNA; BACILLARIOPHYCEAE; ELECTROPHORESIS; FLUORESCENCE	The toxic dinoflagellate Pfiesteria piscicida has been identified in coastal waters and estuaries along the Atlantic coast of the United States. Estuaries in the mid-Atlantic region, in particular, have been targeted as high-risk areas for toxic blooms since reports of Pfiesteria-related fish kills in the Pocomoke River, Maryland, in 1997. The development of monitoring strategies for these areas requires that the presence of Pfiesteria be rapidly and accurately assessed. Routine monitoring by light microscopy lacks both the sensitivity and accuracy required for species-specific detection and enumeration of Pfiesteria, especially at the low levels normally found in non-bloom conditions. In this study, we developed 2 molecular techniques to identify and enumerate P. piscicida in the Delaware Inland Bays and the Pocomoke River. The first technique, denaturing gradient gel electrophoresis (DGGE), was used to identify several similar but distinct strains of Pfiesteria in water and their benthic stages (cysts or amoebae) in sediment samples. A comparison of DGGE analyses of Pfiesteria community structure in the Pocomoke River and the Delaware Inland Bays revealed subtle differences in strain composition. A second technique, PCR-fluorescent fragment detection (PCR-FFD), was designed for quantitative enumeration of Pfiesteria in water samples. This technique offers a 1000-fold increase in sensitivity over microscopic techniques. To demonstrate the utility of PCR-FFD, we conducted a study of Pfiesteria at the Roosevelt Inlet, Lewes, Delaware. Pfiesteria concentrations over 2 tidal cycles were correlated to other physical, biological and chemical variables, Overall, our data establish the presence of Pfiesteria as a minor but prevalent member of the phytoplankton community in mid-Atlantic estuaries.	Univ Delaware, Grad Coll Marine Studies, Lewes, DE 19958 USA	University of Delaware	Cary, SC (通讯作者)，Univ Delaware, Coll Marine Studies, 700 Pilottown Rd, Lewes, DE 19958 USA.		; Hutchins, David/D-3301-2013	Coyne, Kathryn/0000-0001-8846-531X; Cary, Stephen/0000-0002-2876-2387; Hutchins, David/0000-0002-6637-756X				Anderson D.M., 1989, P11; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Burkholder JM, 1997, J EUKARYOT MICROBIOL, V44, P200, DOI 10.1111/j.1550-7408.1997.tb05700.x; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; CARTER HH, 1967, 13 J HOPK U CHES BAY, P46; Dempster EL., 1999, BIOTECHNIQUES, V27, P66; DEWITT P, 1973, HYDROGRAPHY BROADKIL, V14, P28; GALLAGHER JC, 1982, J PHYCOL, V18, P148, DOI 10.1111/j.1529-8817.1982.tb03169.x; GALLAGHER JC, 1998, PHYSL ECOLOGY HARMFU, P225; GLASGOW HB, 1995, J TOXICOL ENV HEALTH, V46, P501, DOI 10.1080/15287399509532051; Grattan L M, 1998, Md Med J, V47, P127; 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]; HOBBIE JE, 1977, APPL ENVIRON MICROB, V33, P1225, DOI 10.1128/AEM.33.5.1225-1228.1977; *HORS WITT INC, 1998, ASS NITR LOAD DEL IN; LEWITUS AJ, 1995, ESTUARIES, V18, P373, DOI 10.2307/1352319; Liu WT, 1997, APPL ENVIRON MICROB, V63, P4516, DOI 10.1128/AEM.63.11.4516-4522.1997; LU W, 1994, NATURE, V368, P269, DOI 10.1038/368269a0; Mackenzie L, 1996, PHYCOLOGIA, V35, P148, DOI 10.2216/i0031-8884-35-2-148.1; Maidak BL, 1999, NUCLEIC ACIDS RES, V27, P171, DOI 10.1093/nar/27.1.171; *MAR DEP NAT RES, 1997, REP GOV BLUE RIBB CI; MEDLIN L, 1988, GENE, V71, P491, DOI 10.1016/0378-1119(88)90066-2; MILLER RW, 1989, DEL CONSERVATIONIST, V32, P38; MUYZER G, 1993, APPL ENVIRON MICROB, V59, P695, DOI 10.1128/AEM.59.3.695-700.1993; Oldach DW, 2000, P NATL ACAD SCI USA, V97, P4303, DOI 10.1073/pnas.97.8.4303; Parsons ML, 1999, J PHYCOL, V35, P1368, DOI 10.1046/j.1529-8817.1999.3561368.x; Pinckney JL, 1997, CAN J FISH AQUAT SCI, V54, P2491, DOI 10.1139/cjfas-54-11-2491; PORCHER C, 1992, BIOTECHNIQUES, V13, P106; Price KS, 1998, ENVIRON MONIT ASSESS, V51, P285, DOI 10.1023/A:1005951706152; Rublee P. A., 1999, Virginia Journal of Science, V50, P325; Scholin C.A., 1998, PHYSL ECOLOGY HARMFU, P337; Skov J, 1997, PHYCOLOGIA, V36, P374, DOI 10.2216/i0031-8884-36-5-374.1; SMITH SW, 1994, COMPUT APPL BIOSCI, V10, P671; Strickland J.D.H., 1972, FISHERIES RES BOARD, V2nd; *WEST RF INC, 1993, CHAR INL BAYS EST RE; WOOD AM, 1992, J PHYCOL, V28, P723, DOI 10.1111/j.0022-3646.1992.00723.x	37	99	118	1	30	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055			AQUAT MICROB ECOL	Aquat. Microb. Ecol.	JUL 18	2001	24	3					275	285		10.3354/ame024275	http://dx.doi.org/10.3354/ame024275			11	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	458QR		Bronze			2025-03-11	WOS:000170206500006
J	Slimani, H				Slimani, H			New species of dinoflagellate cysts from the Campanian-Danian chalks at Hallembaye and Turnhout (Belgium) and at Beutenaken (the Netherlands)	JOURNAL OF MICROPALAEONTOLOGY			English	Article								A palynological study of Campanian-Danian chalks from the quarries at Beutenaken and Hallembaye (Maastricht region) and from a borehole at Turnhout (northern Belgium) has revealed the presence of seven new species and subspecies of dinoflagellate cysts: Exochosphaeridium? Masureae sp. nov., Leberidocysta chlamydata subsp. schiolerii subsp. nov., Odontochitina streelii sp. nov., Pervosphaeridium septatum sp. nov., Spiniferites ramosus subsp. pterocoelus subsp. nov., Stephodinium? spinosum sp. nov. and Xenascus wetzelii sp. nov. Nexosispinum? complicatum described by Slimani (1996) as a new species is now a junior synonym of Pulchrasphaera minuscula Schioler et al. (1997).	Univ Mohammed 5, Inst Sci, Dept Geol, Rabat, Morocco	Mohammed V University in Rabat	Slimani, H (通讯作者)，Univ Mohammed 5, Inst Sci, Dept Geol, Ave Ibn Batouta,BP 703, Rabat, Morocco.		Slimani, Hamid/AAL-4055-2020	Slimani, Hamid/0000-0001-6392-1913				Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], P 2 PLANKT C ROM 197; BINT A N, 1986, Palynology, V10, P135; CLARKE R F A, 1968, Taxon, V17, P181, DOI 10.2307/1216512; Clarke R. F. A., 1967, Verb K ned Akad Wet Amst, V24, P1; Cookson I. C., 1962, Micropaleontology, V8, P485, DOI 10.2307/1484681; COOKSON I C, 1969, Journal of the Royal Society of Western Australia, V52, P3; Corradini D., 1973, B SOC PALEONTOL ITAL, V11, P119; Davey R.J., 1966, STUDIES MESOZOIC CAI, P28; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; Davey R.J., 1966, STUDIES MESOZOIC CAI, P53; DAVEY RJ, 1979, INITIAL REPORTS DEEP, V48, P546; de Coninck J., 1986, Mededelingen Rijks Geologische Dienst, V40, P1; Deflandre G., 1935, Bulletin Biologique de la France et de la Belgique, V69, P213; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; DEFLANDRE G., 1936, ACTUALITIS SCI INDUS, V335, P1; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DeFLANDRE GEORGES, 1943, BULL SOC GEOL FRANCE, V13, P499; Ehrenberg C.G., 1838, KONIGLICHE AKAD WISS, V1838, P109; Evitt W.R., 1985, Sporopollen in Dinoflagellate Cysts: Their Morphology and Interpretation; Foucher J.-C., 1985, The Campanian-Maastrichtian Boundary in the chalky facies close to the typeMaastrichtian; FOUCHER JC, 1983, 8 S ASS PAL LANG FRA; IOANNIDES NS, 1986, B GEOLOGICAL SURVEY, V371; KIRSCH KH, 1991, MUNCHNER GEOWISSEN A, V22; Lentin J.K., 1993, Fossil Dinoflagellates: Index to Genera and Species, V28; LENTIN JK, 1989, FOSSIL DINOFLAGELLAT, V20; LOEBLICH AR, 1966, STUDIES TROPICAL OCE; LOUWYE S, 1991, THESIS FACULTEIT WET; Mantell G.A, 1850, A Pictorial Atlas of Fossil Remains Consisting of Coloured Illustrations Selected from Parkinson's "Organic Remains of a Former World", and Artis's "Antediluvian Phytology; Marheinecke U., 1986, GEOLOGISCHES JB A, V93, P3; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; MASURE E, 1985, CRETACEOUS RES, V6, P199, DOI 10.1016/0195-6671(85)90045-X; Masure E., 1985, CAMPANIEN STRATOTYPI, V10, P41; SARJEANT W A S, 1970, Grana, V10, P74; 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; SCHUMACKERLAMBR.J, 1977, S APP TECHN REC PAL; SLIMANI H, 1995, THESIS LAB PALEONTOL; Slimani H, 1996, ANN SOC GEOL BELG, V117, P371; Slimani H., 1994, MEMOIRES SERVIR EXPL, P37; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; Stover L.E., 1987, AM ASS STRATIGRAPHIE, V18, P1; STOVER LE, 1987, ASS AUSTR PALEONT ME, V4, P101; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Wetzel O., 1933, PALAEONTOGRAPHICA, V77, P141; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; Wilson GJ., 1974, THESIS U NOTTINGHAM; YUN H-S, 1981, Palaeontographica Abteilung B Palaeophytologie, V177, P1	49	19	20	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.	JUL	2001	20		1				1	11		10.1144/jm.20.1.1	http://dx.doi.org/10.1144/jm.20.1.1			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	459VT		hybrid			2025-03-11	WOS:000170272700001
J	Zaragosi, S; Eynaud, F; Pujol, C; Auffret, GA; Turon, JL; Garlan, T				Zaragosi, S; Eynaud, F; Pujol, C; Auffret, GA; Turon, JL; Garlan, T			Initiation of the European deglaciation as recorded in the northwestern Bay of Biscay slope environments (Meriadzek Terrace and Trevelyan Escarpment): a multi-proxy approach	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Bay of Biscay; Europe; Heinrich events; dinoflagellata; slope environment	NORTH-ATLANTIC OCEAN; HEINRICH EVENT 1; ICE-SHEET; DINOFLAGELLATE CYSTS; ICEBERG DISCHARGES; SEA; SAND; SEDIMENTS; TIDE; RAY	Three cores retrieved on the northwestern slope of the Bay of Biscay are described and discussed in the light of the European last deglaciation history. This integrated sedimentological and micropalaeontological study provides a detailed evolution scheme for the deep and sea-surface conditions of the Bay during the final deglacial step, with a direct link with the continental palaeoenvironments. As early as 15 ka C-14-BP, a European precursor melting event is recorded as a purge of the Channel and Irish Sea palaeoriver systems. 'Pleni-Heinrich event conditions' occurred in the Bay of Biscay between 14.4 and 13 ka C-14-BP with a typical Canadian signature only recorded at 13 ka C-14-BP, namely 1 ka later than the first evidence of melting of the British Ice-sheet. Our data demonstrate that, following Heinrich event 2, the Last Glacial Maximum was characterised by a gradual warming accompanied by, at least, two pulses of the North Atlantic Drift. These North Atlantic Drift/heat northward penetrations are supposed to have primarily forced the Heinrich event 1 collapse. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Bordeaux 1, Dept Geol & Oceanog, F-33405 Talence, France; SHOM, Ctr Hydrog, F-29275 Brest, France	Universite de Bordeaux	Univ Bordeaux 1, Dept Geol & Oceanog, Ave Fac, F-33405 Talence, France.	s.zaragosi@geocean.u-bordeaux.fr	ZARAGOSI, Sébastien/JXL-2488-2024	Eynaud, Frederique/0000-0003-1283-7425; Zaragosi, Sebastien/0000-0002-1456-8129				[Anonymous], 1981, Geol Soc Amer Map Chart Ser; [Anonymous], 1997, Proceedings of the Ocean Drilling Program Scientific Results, V155, P611; Auffret GA, 1996, GEO-MAR LETT, V16, P76, DOI 10.1007/BF02202601; Bard E, 1998, GEOCHIM COSMOCHIM AC, V62, P2025, DOI 10.1016/S0016-7037(98)00130-6; Berne S, 1998, J SEDIMENT RES, V68, P540, DOI 10.2110/jsr.68.540; BOND GC, 1995, SCIENCE, V267, P1005, DOI 10.1126/science.267.5200.1005; Broecker W, 1992, CLIM DYNAM, V6, P265, DOI 10.1007/BF00193540; Broecker WS, 1990, PALEOCEANOGRAPHY, V5, P469, DOI 10.1029/PA005i004p00469; Caralp M, 1981, B I GEOL BASSIN AQUI, V31, P411; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; de Vernal A, 2000, QUATERNARY SCI REV, V19, P65, DOI 10.1016/S0277-3791(99)00055-4; de Vernal A., 1996, CAHIERS GEOTOP, V3, P1; Elliot M, 1998, PALEOCEANOGRAPHY, V13, P433, DOI 10.1029/98PA01792; EYNAUD F, 1999, THESIS BORDEAUX 1 U, P1; FAIRBANKS RG, 1989, NATURE, V342, P637, DOI 10.1038/342637a0; GIBBARD PL, 1988, PHILOS T ROY SOC B, V318, P559, DOI 10.1098/rstb.1988.0024; Gibbard PL., 1995, Island Britain-A Quaternary Perspective, P15; Grousset FE, 2000, GEOLOGY, V28, P123; Hansel A.K., 1992, Sverige Geologiska Undersokning, Series Ca, V81, P133; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Hesse R, 1998, GEOLOGY, V26, P103, DOI 10.1130/0091-7613(1998)026<0103:DFOLPH>2.3.CO;2; Lagerklint IM, 1999, GEOLOGY, V27, P1099; LAMBECK K, 1995, J GEOL SOC LONDON, V152, P437, DOI 10.1144/gsjgs.152.3.0437; LEHMAN SJ, 1991, NATURE, V349, P513, DOI 10.1038/349513a0; Loncaric N, 1998, MAR GEOL, V152, P57, DOI 10.1016/S0025-3227(98)00064-4; MACAYEAL DR, 1993, PALEOCEANOGRAPHY, V8, P775, DOI 10.1029/93PA02200; Manabe S, 2000, QUATERNARY SCI REV, V19, P285, DOI 10.1016/S0277-3791(99)00066-9; McCabe AM, 1998, NATURE, V392, P373, DOI 10.1038/32866; McCabe M, 1998, J QUATERNARY SCI, V13, P549, DOI 10.1002/(SICI)1099-1417(1998110)13:6<549::AID-JQS394>3.0.CO;2-A; Migeon S, 1999, GEO-MAR LETT, V18, P251, DOI 10.1007/s003670050076; Morzadec-Kerfourn M. T., 1977, Revue Micropaleont, V20, P157; PUJOL C, 1980, MEM I GEOL BASSIN AQ, V10, P1; Revel M, 1996, MAR GEOL, V131, P233, DOI 10.1016/0025-3227(96)00005-9; Reynaud JY, 1999, MAR GEOL, V161, P339, DOI 10.1016/S0025-3227(99)00033-X; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Rosell-Melé A, 1998, PALEOCEANOGRAPHY, V13, P694, DOI 10.1029/98PA02355; SchaferNeth C, 1997, GEOL RUNDSCH, V86, P492, DOI 10.1007/s005310050156; SCHNEIDER R, 2000, PAGES NEWSLETTER, V8, P19; Scourse JD, 2000, EARTH PLANET SC LETT, V182, P187, DOI 10.1016/S0012-821X(00)00241-7; Snoeckx H, 1999, MAR GEOL, V158, P197, DOI 10.1016/S0025-3227(98)00168-6; STEIN R, 1996, PALEOCEANOGRAPHY N A, P135; Turon J.-L., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P313; Turon J.L., 1984, MEM I GEOL BASSIN AQ, V17, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Weilnet M., 1996, PALEOCLIMATES, V1, P283; WILLIAMS GL, 1998, AASP CONTRIB SER, V34; Zaragosi S, 2000, MAR GEOL, V169, P207, DOI 10.1016/S0025-3227(00)00054-2	47	96	99	0	10	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0012-821X	1385-013X		EARTH PLANET SC LETT	Earth Planet. Sci. Lett.	JUN 15	2001	188	3-4					493	507		10.1016/S0012-821X(01)00332-6	http://dx.doi.org/10.1016/S0012-821X(01)00332-6			15	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	445GH					2025-03-11	WOS:000169449400014
J	Ichimi, K; Yamasaki, M; Okumura, Y; Suzuki, T				Ichimi, K; Yamasaki, M; Okumura, Y; Suzuki, T			The growth and cyst formation of a toxic dinoflagellate, <i>Alexandrium tamarense</i>, at low water temperatures in northeastern Japan	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Alexandrium tamarense; cyst; toxic dinoflagellate; PSP	GONYAULAX-TAMARENSIS; BATCH CULTURES; RESTING CYSTS; RAPHIDOPHYCEAE; GERMINATION; ENCYSTMENT; SEXUALITY; YIELD	A field survey was carried out in early spring to investigate the growth physiology and efficiency of cyst formation of Alexandrium tamarense in low water temperatures. A bloom of A. tamarense occurred in a stratified water column, formed by river inflow. The in situ growth rate estimated from daily cell abundance was high, 0.33 divisions day(-1), at 7.5-9 degreesC. New cysts began to be observed during the late growth phase. Maximum cyst flux (600 cysts cm(-2) day(-1)) was observed just after maximum cell abundance occurred. PO4-P Chi a(-1) gradually decreased and reached extremely low levels beyond the mid-growth phase of A. tamarense. As sinking cysts were also recognized at that time, it suggests cyst formation may have been induced by depletion of phosphorus source. The incidence of cyst formation (C.I) was 30%. The number of C.I was the same as reported previously for batch cultures under conditions suitable for vegetative growth. These results indicate that A. tamarense grows with considerably higher growth rate and transforms to cysts in high numbers, in low water temperatures in the field. (C) 2001 Elsevier Science B.V. All rights reserved.	Tohoku Natl Fisheries Res Inst, Shiogama, Miyagi 9850001, Japan	Japan Fisheries Research & Education Agency (FRA)	Ichimi, K (通讯作者)，Kagawa Univ, Fac Agr, 2393 Ikenobe, Miki, Kagawa 7610795, Japan.							ACHIHA H, 1990, Japanese Journal of Phycology, V38, P51; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; 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, 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, 1978, J PHYCOL, V14, P124; BINDER BJ, 1987, J PHYCOL, V23, P99; Eppley R.W., 1977, The Biology of Diatoms, P24; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; FUKUYO Y, 1982, THESIS TOKYO U; ICHIMI K, 2000, JPN B TOHOKU NATL FI, V63, P119; IMAI I, 1989, MAR BIOL, V103, P235, DOI 10.1007/BF00543353; IMAMURA K, 1987, GUIDE STUDIES RED TI, P72; Ishibashi T., 1985, TAIKABUTSU, V6, P40; Kotani Yuichi, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P104; Margalef R., 1979, P89; NAKAMURA Y, 1990, Journal of the Oceanographical Society of Japan, V46, P35, DOI 10.1007/BF02124813; NAKAMURA Y, 1991, MAR ECOL PROG SER, V78, P273, DOI 10.3354/meps078273; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; Provasoli L., 1979, P1; Strickland JDH., 1972, J FISH RES BOARD CAN, V167, P21; SUZUKI R, 1990, Journal of the Oceanographical Society of Japan, V46, P190, DOI 10.1007/BF02125580; Therriault J.C., 1985, P141; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WATANABE MM, 1982, RES REP NATL I ENV S, V30, P27; WHITE AW, 1978, J PHYCOL, V14, P475; WHITE AW, 1976, J FISH RES BOARD CAN, V33, P2598, DOI 10.1139/f76-306; Yamaguchi, 1996, HARMFUL TOXIC ALGAL, P177; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; Yamamoto T., 1995, Japanese Journal of Phycology, V43, P91; Yamamoto Tamiji, 1997, Japanese Journal of Phycology, V45, P95	32	42	49	1	15	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0022-0981			J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	JUN 15	2001	261	1					17	29		10.1016/S0022-0981(01)00256-8	http://dx.doi.org/10.1016/S0022-0981(01)00256-8			13	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	441UT	11438103				2025-03-11	WOS:000169248500002
J	Fiet, N; Beaudoin, B; Parize, O				Fiet, N; Beaudoin, B; Parize, O			Lithostratigraphic analysis of Milankovitch cyclicity in pelagic Albian deposits of central Italy: implications for the duration of the stage and substages	CRETACEOUS RESEARCH			English	Article						Albian; ammonites; cyclostratigraphy; Milankovitch; Umbria-Marche; black shales	TIME SCALE; BASIN; CALIBRATION; AMMONITES; FRANCE; ZONES	Estimations of Albian Stage and substage durations are proposed on the basis of a cyclostratigraphic study of a continuous pelagic section of the 'Marne a Fucoidi' formation of the Umbria-Marche Basin, central Italy. An analysis of the vertical distribution of black shales, marls and limestones is documented. The black shales are organized in bundles of 3-5 levels (similar to 100 kyr) and composite groups (similar to 400 kyr), which are the sedimentary expressions of the two eccentricity modes of the Earth's orbit. The specific distribution of this lithology coupled with the vertical stacking of the marl-limestone couplets, interpreted as an expression of the precession of the equinoxes, enables the breakdown of the Albian Stage and its substages into astroclimatic cycles and calibration of their duration. The stratigraphic boundaries are fixed by a combination of planktonic foraminifera, calcareous nannofossils and dinoflagellate cyst 'events', which have been correlated with European ammonite biozonations. The Albian Stage is estimated to have lasted for 11.6 +/- 0.2 myr, and the Aptian/Albian boundary is proposed at 110.1 +/- 0.7 Ma. Substages are respectively estimated at 1 myr (Lower Albian), 3.7 myr (Middle Albian) and 3.4 myr (both Upper and uppermost Albian, also called Vraconian). These durations have enabled the determination of a new calibration of the average durations of the Albian ammonite zones, which are obtained by translation of the Italian micropaleontological data on the international chart. The duration of the biozones is very variable and the stratigraphic resolution of each zone fluctuates between 100 kyr for the Lower Albian and 1.7 myr for the uppermost Albian. The application of the new Albian durations in sequence stratigraphy has implications for the genetic causes of the unconformities, particularly for the Lower Albian where the unconformities were produced by astronomical parameters of the Earth's orbit. (C) 2001 Academic Press.	Ecole Natl Super Mines, CGES Sedimentol, F-77305 Fontainebleau, France; Univ Paris 11, Dept Geol, F-91405 Orsay, France	Universite PSL; MINES ParisTech; Universite Paris Saclay	Fiet, N (通讯作者)，Ecole Natl Super Mines, CGES Sedimentol, 35 Rue St Honore, F-77305 Fontainebleau, France.							AMEDRO F, 1992, B CENT RECH EXPL, V16, P187; Amedro Francis, 1995, Geologie de la France, V2, P25; [Anonymous], UTRECHT MICROPALEONT; [Anonymous], MILANKOVITCH CLIMA 1; [Anonymous], 1982, Cyclic and Event Stratification; ARTHUR MA, 1982, NATURE ORIGIN CRETAC, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BERGER A, 1992, SCIENCE, V255, P560, DOI 10.1126/science.255.5044.560; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; 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]; BERGER AL, 1976, ASTRON ASTROPHYS, V51, P127; Bralower T.J., 1995, Geochronology Time Scales and Global Stratigraphic Correlation, P65; BREHERET JG, 1997, THESIS U TOURS; CASTILLO PR, 1994, EARTH PLANET SC LETT, V123, P139, DOI 10.1016/0012-821X(94)90263-1; COCCIONI R, 1989, FOSSILI EVOLUZIONE A, P163; ERBA E, 1988, Rivista Italiana di Paleontologia e Stratigrafia, V94, P249; Fiet N, 1998, B SOC GEOL FR, V169, P221; Fiet N, 2001, CRETACEOUS RES, V22, P63, DOI 10.1006/cres.2000.0237; FIET N, 1998, THESIS ECOLE MINES P; Gale AS, 1996, CRETACEOUS RES, V17, P515, DOI 10.1006/cres.1996.0032; Gradstein F.M., 1995, GEOCHRONOLOGY TIME S, V54, P95; HALLAM A, 1985, GEOLOGICAL SOC LONDO, V10, P118; Hancock J.M., 1993, Evolution of the Western Interior Basin, V39, P453; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; HARDENBOL J, 1998, SEPM SPECIAL PUBLICA, V52, P1; Harland W.B., 1990, GEOLOGIC TIME SCALE; Hart Malcolm, 1996, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V66, P45; Herbert T.D., 1995, Geochronology, Time Scales, and Global Stratigraphic Correlation: SEPM Special Publication, v, V54, P81; HERBERT TD, 1986, NATURE, V321, P739, DOI 10.1038/321739a0; HERBERT TD, 1989, 28 INT GEOL C WASH D, P51; HILGEN FJ, 1991, EARTH PLANET SC LETT, V104, P226, DOI 10.1016/0012-821X(91)90206-W; KENNEDY WJ, 1982, NUMERICAL DATING STR, P104; KENT DV, 1985, GEOL SOC AM BULL, V96, P1419, DOI 10.1130/0016-7606(1985)96<1419:ACAJG>2.0.CO;2; LASKAR J, 1990, ICARUS, V88, P266, DOI 10.1016/0019-1035(90)90084-M; Latil J.L., 1994, Geologie Alpine, Memoire hors-serie, V20, P67; LONGORIA JF, 1984, MICROPALEONTOLOGY, V30, P225, DOI 10.2307/1485687; MOULLADE M, 1966, DOCUMENTS LAB GEOLOG, V15; Obradovich J.D., 1993, EVOLUTION W INTERIOR, V39, P379; Parize O, 1998, CR ACAD SCI II A, V326, P433, DOI 10.1016/S1251-8050(98)80067-0; PARK J, 1987, J GEOPHYS RES-SOLID, V92, P14027, DOI 10.1029/JB092iB13p14027; Pratt LM, 1986, PALEOCEANOGRAPHY, V1, P507, DOI 10.1029/PA001i004p00507; Premoli Silva I, 1995, PALAEONTOGRAPHIA ITA, V82, P1; ROBASZYNSKI F, 1993, B CENT RECH EXPL, V17, P395; Robaszynski F, 1995, B SOC GEOL FR, V166, P681; ROOTH CGH, 1978, EARTH PLANET SC LETT, V41, P387, DOI 10.1016/0012-821X(78)90169-3; SCHWARZACHER W, 1986, PALEOCEANOGRAPHY, V2, P79; Schwarzacher W., 1982, Cyclic and event stratification, P72; SIGAL J, 1977, GEOLOGIE MEDITERRANE, V4; TORNAGHI M E, 1989, Rivista Italiana di Paleontologia e Stratigrafia, V95, P223; Vail P., 1977, Seismic stratigraphy - applications to hydrocarbon exploration, V26, P63	51	41	49	0	4	ACADEMIC PRESS LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	JUN	2001	22	3					265	275		10.1006/cres.2001.0258	http://dx.doi.org/10.1006/cres.2001.0258			11	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	462CX					2025-03-11	WOS:000170404100001
J	Cho, HJ; Matsuoka, K				Cho, HJ; Matsuoka, K			Distribution of dinoflagellate cysts in surface sediments from the Yellow Sea and East China Sea	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cyst distribution; Alexandrium cysts; PIG value; Yellow Sea; East China Sea	ADJACENT SEAS; RESTING CYSTS; PHYTOPLANKTON; ALEXANDRIUM; DINOPHYCEAE; NORTH; BAY	The distribution of dinoflagellate cysts in surface sediment samples of the Yellow Sea and East China Sea has been examined from 48 samples. Emphasis has been placed on ellipsoidal cysts of the genus Alexandrium. Results show two concurrent cyst distribution trends in latitudinal and longitudinal directions. In the latitudinal trend, cysts are most abundant north of 34 degreesN in the Yellow Sea, where Spiniferites bulloideus (Deflandre et Cookson) Sarjeant, and ellipsoidal Alexandrium cysts generally dominate. Cyst concentration decreases towards both sides of the northern East China Sea in a longitudinal direction. Various factors such as cyst production, particle size of sediment and sedimentation rates may contribute to the dinoflagellate cyst distribution in the Yellow Sea and northern East China Sea. The protoperidinioid/gonyaulacoid (P/G) ratio, which is considered to increase in proportion with increasing primary production, is of limited use in comparing with other areas because its value remains high in both high and lower primary production areas in our study. (C) 2001 Elsevier Science B.V. All rights reserved.	Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan; Nagasaki Univ, Grad Sch Marine Sci & Engn, Nagasaki 8528521, Japan	Nagasaki University; Nagasaki University	Cho, HJ (通讯作者)，Pukyong Natl Univ, Dept Oceanog, Nam Gu, Pusan 608737, South Korea.							An K.H., 1998, THESIS PUKYONG NATL, P20; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; Cho H.J., 1999, P 2 INT WORKSH OC FI, P73; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Goodman D. K., 1987, BIOL DINOFLAGELLATES, P649; GUO YJ, 1991, OCEANOGR MAR BIOL, V29, P155; GUO YJ, 1996, YELLOW SEA, V2, P90; Hama T., 1997, J OCEANOGR, V53, P41, DOI [10.1007/BF02700748, DOI 10.1007/BF02700748]; HAMADA S, 1998, B SEIKAI NATL FISH R, V76, P27; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Ishikawa Akira, 2000, Plankton Biology and Ecology, V47, P12; KIM CH, 1999, JOINT S MAR SCI E CH, P8; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; KOBAYASHI S, 1991, Bulletin of Plankton Society of Japan, V38, P9; KOBAYASHI S, 1986, Bulletin of Plankton Society of Japan, V33, P81; KOTANI Y, 1998, SUISAN KAIYO KENKYU, V62, P104; Lee J.B., 1994, P 2 INT S MAR SCI EX, P1; Lee J. B, 1996, HARMFUL TOXIC ALGAL, P173; Lewis Jane, 1995, P175; MAEDA A, 1989, UMI SORA, V64, P257; Mao Shaozhi, 1993, Palynology, V17, P47; MATSON PL, 1994, FRONT ENDOCRINOL, V8, P155; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MATSUOKA K, 1994, B FACULTY LIBERAL AR, P121; Matsuoka K., 1999, P 2 INT WORKSH OC FI, P195; Matsuoka Kazumi, 1999, Fossils (Tokyo), V66, P1; McMinn Andrew, 1992, Palynology, V16, P13; NING XR, 1988, MAR ECOL PROG SER, V49, P141, DOI 10.3354/meps049141; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; TAKASUGI Y, 1998, SUISANN KAIYOU KENKY, V62, P187; TAKEUCHI T, 1994, B WAKAYAMA PREFECTUR, P53; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; 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; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; Xu XD, 1999, MAR GEOL, V156, P285, DOI 10.1016/S0025-3227(98)00183-2; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; *YOK ENV RES I, 1992, 102 YOK ENV RES I, P133	39	75	102	2	35	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	JUN	2001	42	3-4					103	123		10.1016/S0377-8398(01)00016-0	http://dx.doi.org/10.1016/S0377-8398(01)00016-0			21	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	450MV					2025-03-11	WOS:000169748500001
J	Kumaran, KPN; Limaye, RB; Rajshekhar, C; Rajagopalan, G				Kumaran, KPN; Limaye, RB; Rajshekhar, C; Rajagopalan, G			Palynoflora and radiocarbon dates of Holocene deposits of Dhamapur, Sindhudurg district, Maharashtra	CURRENT SCIENCE			English	Article							BC	Radiocarbon dates of carbonized wood (2110 +/- 80 yr BP) and oyster shells (7620 +/- 110 yr BP) obtained from the sub-surface sediments of Dhamapur well fall within the Holocene period and the environments in which the above got deposited, might have been subjected to the sea-level oscillations of the past. The big oyster shells with barnacle growth, reminiscent of rocky intertidal environment, have shown to be related to Saccostrea! sp, of Indo-West Pacific affinity. Presence of salt glands, presumably of mangrove plants, dinoflagellate cysts and organic-walled foraminiferal linings in the palynoflora assemblage infers that these elements must have been recruited from a shallow marine intertidal environment through creek channels, However, the carbonized wood materials and the palynoflora are essentially that of a lowland vegetation deposited in a freshwater facies. Further, larger proportion of pterido-phytic spores, reflects a swampy and marshy habitat. The abundance of particulate organic matter (palynodebris), including various fungal elements suggests that the area had been under dense forest cover, receiving heavy precipitation with greater atmospheric moisture at the time of deposition.	Agharkar Res Inst, Geol & Palaeontol Grp, Pune 411004, Maharashtra, India; Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Agharkar Research Institute (ARI); Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Kumaran, KPN (通讯作者)，Agharkar Res Inst, Geol & Palaeontol Grp, GG Agarkar Rd, Pune 411004, Maharashtra, India.							AGARWAL DP, 1972, PALEOBOTANIST, V21, P216; Caratini C., 1980, Proc. IV Intematl. Palynol. Conf, V3, P49; GUZDER S, 1980, QUARTERNARY ENV STON, P42; HASHIMI NH, 1995, J GEOL SOC INDIA, V46, P157; Kale V.S., 1985, B DECCAN COLL RES IN, V44, P153; Kumaran K.P.N., 1991, P S SIGN MANGR, P31; Ratan R., 1984, PALEOBOTANIST, V31, P218; STUIVER M, 1993, RADIOCARBON, V35, P137; STUIVER M, 1993, RADIOCARBON, V35, P1, DOI 10.1017/S0033822200013874; VISHNUMITTRE, 1975, PALAEOBOTANIST, V22, P111	10	11	11	0	2	CURRENT SCIENCE ASSN	BANGALORE	C V RAMAN AVENUE, PO BOX 8005, BANGALORE 560 080, INDIA	0011-3891			CURR SCI INDIA	Curr. Sci.	MAY 25	2001	80	10					1331	1336						6	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	438HV					2025-03-11	WOS:000169048300031
J	Lewis, J; Rochon, A; Ellegaard, M; Mudie, PJ; Harding, I				Lewis, J; Rochon, A; Ellegaard, M; Mudie, PJ; Harding, I			The cyst-theca relationship of <i>Bitectatodinium tepikiense</i> (Dinophyceae)	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Bitectatodinium; cyst-theca relationships; Gonyaulax; Spiniferites	DINOFLAGELLATE CYSTS; RECENT SEDIMENTS	Bitectatodinium tepikiense Wilson cysts, first described from Pleistocene sediments and generally associated with sediments in temperate to cold-temperate waters, were germinated to establish cultures. The motile thecate cells derived were referable to Gonyaulax digitale (Pouchet) Kofoid. For the first time detailed morphological information is given for the motile stage of this cyst-theca relationship. Cultures were re-encysted; the cultured cysts showed a range of morphology from spherical cysts to those with an apical boss. The taxonomy of Gonyaulax digitale and cyst-theca relationships within the Spiniferites plexus are discussed but, given the debate surrounding the status of the genera Gonyaulax and Spiniferites, no formal taxonomic reassignments are proposed. These observations confirm that establishing cultures of cyst taxa in problematic dinoflagellate groupings and meticulous high-resolution scanning electron microscopic observation of the specimens have great potential for elucidating cyst-theca relationships and clarifying dinoflagellate taxonomy.	Univ Westminster, Sch Biosci, London W1M 8JS, England; Univ Southampton, Sch Earth & Ocean Sci, Southampton Oceanog Ctr, Southampton SO14 3ZH, Hants, England; Geol Survey Canada Atlantic, Dartmouth, NS B27 4A2, Canada	University of Westminster; University of Southampton; NERC National Oceanography Centre; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Lewis, J (通讯作者)，Univ Westminster, Sch Biosci, 115 New Cavendish St, London W1M 8JS, England.		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H., 1928, Museum Notes Vancouver, V3, P20; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; 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; WALL D, 1970, Micropaleontology (New York), V16, P47, DOI 10.2307/1484846; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363; WOOD E. J. F., 1954, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V5, P171	45	35	37	0	2	CAMBRIDGE UNIV PRESS	PORT CHESTER	110 MIDLAND AVE, PORT CHESTER, NY 10573-9863 USA	0967-0262			EUR J PHYCOL	Eur. J. Phycol.	MAY	2001	36	2					137	146		10.1017/S0967026201003171	http://dx.doi.org/10.1017/S0967026201003171			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	454HX					2025-03-11	WOS:000169968100004
J	Gayoso, AM				Gayoso, AM			Observations on <i>Alexandrium tamarense</i> (Lebour) Balech and other dinoflagellate populations in Golfo Nuevo, Patagonia (Argentina)	JOURNAL OF PLANKTON RESEARCH			English	Article							BAHIA BLANCA ESTUARY; PHYTOPLANKTON; WATERS; BLOOM	The toxic dinoflagellate Alexandrium tamarense and other dinoflagellate species were studied, along with mater temperature and Nutrient concentrations,from September 1995 to December 1998 in the Golfo Nuevo, Chubut, Argentina. Nutrient concentrations were low, showing a peak of high concentration in winter and a phase of depletion in late spring and summer Dinoflagellates tended to be abundant during spring and summer, when Prorocentrum micans was the most important species. Other dinoflagellates were Pyrophacus horologium and Dinophysis acuminata. Ceratium tripes, C. fusus and C. horridum were present during the autumn, and a C. tripos peak up to 5.9 x 10(3) cell l(-1) was observed in May 1997. Alexandrium tamarense showed strong interannual variation, the highest concentration being found in spring (September-October) 1995, with densities up to 15 x 10(3) cells l(-1). The second A.tamarense peak was observed during October-November 1998 with maximal densities up to 5 x 10(3) cells l(-1). Moderately high A. tamarense cyst densities, up to 300 cysts cm(3) of sediment, were found in the deep zone of the Golfo Nuevo basin. Among meteorological variables, increased late winter rain and higher solar radiation during spring may have influenced A. tamarense blooms.	Consejo Nacl Invest Cient & Tecn, Ctr Nacl Patagon, RA-9120 Puerto Madryn, Chubut, Argentina	Centro Nacional Patagonico (CENPAT); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Gayoso, AM (通讯作者)，Consejo Nacl Invest Cient & Tecn, Ctr Nacl Patagon, Blvd Brown S-N,Casilla Correo 128, RA-9120 Puerto Madryn, Chubut, Argentina.							Anderson D. M., 1995, MANUAL HARMFUL MARIN, V33, P229; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; Carreto J.I., 1995, TOXIC PHYTOPLANKTON, P377; Carreto J.I., 1998, HARMFUL ALGAE, P131; CARRETO JI, 1986, J PLANKTON RES, V8, P15, DOI 10.1093/plankt/8.1.15; CARRETO JI, 1981, 399 CONTR I NAC INV; CHARPYROUBAUD CJ, 1982, OCEANOL ACTA, V5, P179; CIOCCO N, 1995, MARISQUERIA MED BUCE; ESTEVES JL, 1992, HYDROBIOLOGIA, V242, P115, DOI 10.1007/BF00018067; Gayoso AM, 1999, BOT MAR, V42, P367, DOI 10.1515/BOT.1999.042; Gayoso AM, 1998, ICES J MAR SCI, V55, P655, DOI 10.1006/jmsc.1998.0375; GLORIOSO PD, 1995, J GEOPHYS RES-OCEANS, V100, P13427, DOI 10.1029/95JC00942; HALLEGRAEFF GM, 1995, J PLANKTON RES, V17, P1163, DOI 10.1093/plankt/17.6.1163; Mendez S.M., 1996, HARMFUL TOXIC ALGAL, P113; Montoya Nora G., 1997, Revista de Investigacion y Desarrollo Pesquero, V11, P145; Mouzo F.H., 1978, Acta Oceanografica Argentina, V2, P69; 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; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; Strickland J.D.H., 1972, FISHERIES RES BOARD, V2nd	21	46	48	1	8	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	MAY	2001	23	5					463	468		10.1093/plankt/23.5.463	http://dx.doi.org/10.1093/plankt/23.5.463			6	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	441VX		Bronze			2025-03-11	WOS:000169251200002
J	Vila, M; Camp, J; Garcés, E; Masó, M; Delgado, M				Vila, M; Camp, J; Garcés, E; Masó, M; Delgado, M			High resolution spatio-temporal detection of potentially harmful dinoflagellates in confined waters of the NW Mediterranean	JOURNAL OF PLANKTON RESEARCH			English	Article							RED-TIDE DINOFLAGELLATE; ALEXANDRIUM-TAYLORI DINOPHYCEAE; LIFE-HISTORY; CYST; SEA; PHYTOPLANKTON; MINUTUM; LAGOON; DYNAMICS; ISOLATE	A systematic sampling programme war carried out in a large number of confined waters (principally harbours) along the Catalan coast (NW Mediterranean) in the context of a new Monitoring Programme. This Monitoring Programme was associated not only with areas subject to aquaculture activities, and therefore under legislation, but also with confined areas with a high risk of harmful algal blooms (HABs) occurrence, in order to provide an early warning of potentially widespread HABs. The systematic Programme war Performed weekly in summer and bi-monthly in winter for five-years. The main results were: (i) the detection of many harmful species and the presence of high numbers of harmful dinoflagellates, mainly of the genera Alexandrium and Dinophysis; (ii) the detection of Alexandrium catenella, new in the study area, which had hardly ever been detected in the Mediterranean Sea; (iii) the presence of some potentially harmful species, including Dinophysis sac culus, present at all periods of the year; (iv) bloom recurrence in several stations; (v) occasional coincidence of small-scale blooms, such as those confined inside the harbours, with widespread blooms (mesoscale blooms) of the same organism. The implications of this high frequency of HAB detection is discussed in relation to the suitability of this sampling programme (focused on confined waters) for the early detection of algal blooms.	Inst Ciencias Mar, Barcelona 08039, Catalonia, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Vila, M (通讯作者)，Inst Ciencias Mar, Passeig Joan De Borbo S-N, Barcelona 08039, Catalonia, Spain.		; Vila, Magda/B-2447-2014; Garces, Esther/C-5701-2011	Camp, Jordi/0000-0002-5202-9783; Vila, Magda/0000-0002-6855-841X; Garces, Esther/0000-0002-2712-501X				ABADIE E, 1999, CONTAMINATION ETANG; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], 1996, Harmful and Toxic Algal Blooms; [Anonymous], 4 REUN IB FIT TOX BI; [Anonymous], RAPP COMM INT MER ME; Aubry FB, 2000, BOT MAR, V43, P423, DOI 10.1515/BOT.2000.044; Bagoien E, 1996, MAR BIOL, V126, P361, DOI 10.1007/BF00354618; BALECH E, 1995, ISLAND MARINE STATIO; BALLANTINE DL, 1988, J EXP MAR BIOL ECOL, V119, P201, DOI 10.1016/0022-0981(88)90193-1; BELIN C, 1993, DEV MAR BIO, V3, P469; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; BONI L, 1993, DEV MAR BIO, V3, P475; BONI L, 1983, Giornale Botanico Italiano, V117, P115; BONI L, 1986, NOVA THALASSIA, V8, P237; BRAVO L, 1990, TOXIC MARINE PHYTOPL, P449; Caroppo C, 1999, AQUAT MICROB ECOL, V17, P301, DOI 10.3354/ame017301; CARRADA GC, 1991, J PLANKTON RES, V13, P229, DOI 10.1093/plankt/13.1.229; Ciminiello P., 1999, Harmful Algae News, V18, P3; DELGADO M, 1990, Scientia Marina, V54, P169; DELGADO M, 1990, Scientia Marina, V54, P1; DELGADO M, 1995, 5 C NAC AC ST CARL R, P700; DELGADO M, 1998, 5 REUN IB FIT TOX VI, P25; Delgado M, 1999, 6 REUN IB FIT TOX BI, P51; DELLALOGGIA R, 1993, DEV MAR BIO, V3, P483; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; FIEDLER PC, 1982, LIMNOL OCEANOGR, V27, P961, DOI 10.4319/lo.1982.27.5.0961; FORTEZA V, 1998, 8 INT C HARMF ALG VI, P58; Fraga S, 1995, PHYCOLOGIA, V34, P514, DOI 10.2216/i0031-8884-34-6-514.1; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; 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; Garcés E, 1999, J PLANKTON RES, V21, P1977, DOI 10.1093/plankt/21.10.1977; GARCES E, 1998, THESIS U BARCELONA; GARCES E, 2000, HAN, V20, P10; 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; GIACOBBE MG, 1995, AQUAT MICROB ECOL, V9, P63, DOI 10.3354/ame009063; Halim Y., 1960, Vie et Milieu, V11, P102; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; HONSELL G, 1993, DEV MAR BIO, V3, P127; HONSELL G, 1995, G BOT ITAL, V129, P391; HORWITZ W, 1980, OFFICIAL METHODS ANA, P298; ISMAEL AA, 2000, 9 INT C HARMF ALG BL, P24; LAKKIS S., 1995, RAPP COMM INT MER ME, V34, P212; MAESTRINI SY, 1996, PHYSL ECOLOGY HARMFU, P243; Maman L., 2000, 6 REUN IB FIT TOX BI, P41; Marasovic Ivona, 1995, P187; Margalef R., 1979, P89; MARGALEF R, 1978, OCEANOL ACTA, V1, P493; MARGALEF R, 1969, INVEST PESQ, V33, P345; MARGALEF R, 1987, Investigacion Pesquera (Barcelona), V51, P121; MONTRESOR M, 1990, TOXIC MARINE PHYTOPLANKTON, P82; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MONTRESOR M, 2000, 9 INT C HARMF ALG BL, P182; MOZETIC P, 1995, RAPP COMM INT MER ME, V34, P214; PAGOU K, 1990, TOXIC MARINE PHYTOPLANKTON, P206; PAULMIER G, 1995, CRYPTOGAMIE ALGOL, V16, P77; SAMSONKECHACHA FL, 1992, RAPP COMM INT MER ME, V33, P103; Sidari L., 1995, P231; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Sorokin YI, 1999, ESTUAR COAST SHELF S, V48, P325, DOI 10.1006/ecss.1998.0423; Sournia Alain, 1995, P103; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; TAGMOUTITALHA F, 1996, HARMFUL TOXIC ALGAL, P85; Teegarden GJ, 1999, MAR ECOL PROG SER, V181, P163, DOI 10.3354/meps181163; THRONDSEN J, 1995, IOC MANUALS GUIDES, V33, P63; TOGNETTO L, 1995, BOT MAR, V38, P291, DOI 10.1515/botm.1995.38.1-6.291; Van Dolah FM, 2000, ENVIRON HEALTH PERSP, V108, P133, DOI 10.1289/ehp.00108s1133; VILA M, 2001, IN PRESS HARMFUL ALG; VILA M, 2001, IN PRESS MAR ECOL PR; WRIGHT JLC, 1996, PHYSL ECOLOGY HARMFU, P427	74	131	138	1	30	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	MAY	2001	23	5					497	514		10.1093/plankt/23.5.497	http://dx.doi.org/10.1093/plankt/23.5.497			18	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	441VX		Bronze			2025-03-11	WOS:000169251200005
J	Levac, E; De Vernal, A; Blake, W				Levac, E; De Vernal, A; Blake, W			Sea-surface conditions in northernmost Baffin Bay during the Holocene: palynological evidence	JOURNAL OF QUATERNARY SCIENCE			English	Article						sea-surface; Baffin Bay; Holocene; polynya; palynology; transfer function	CANADIAN ARCTIC ARCHIPELAGO; ELLESMERE-ISLAND; DINOFLAGELLATE-CYSTS; AGE CALIBRATION; C-14 AGES; MARINE; ICE; QUATERNARY; POLLEN; GREENLAND	The analysis of cores collected in northernmost Baffin Bay, from within the area of the North Water Polynya, permits definition of a composite sedimentary sequence ca. 12 m thick spanning the last 10000 C-14 yr, with only a few discontinuities. Palynological analyses were performed in order to reconstruct changes in surface water conditions and biogenic production. Transfer functions, using dinocyst assemblages, were applied to estimate sea-surface temperature (SST) and salinity, as well as the seasonal duration of sea ice cover. At the base of the record, prior to 9300 C-14 yr BP, dinocysts and organic linings of benthic foraminifers are sparse, indicating harsh conditions and low productivity. After ca. 9300 C-14 yr BP, the increased concentration of benthic foraminifers (up to 10(3) linings cm(-3)) and dinocyst fluxes (10(2)-10(3) cysts cm(-2) yr(-1)) reveals high biological productivity related to open-water conditions. The early to middle Holocene, from ca. 9000 to ca. 3600 C-14 yr BP, is marked by relatively high species diversity in dinocyst assemblages and the significant occurrence of autotrophic taxa such as Spiniferites elongatus, Pentapharsodinium dalei and Impagidinium pallidum. This assemblage suggests conditions at least as warm as at present. From ca. 6400 to ca. 3600 C-14 yr BP, transfer functions indicate warmer conditions than at present, with SST in August fluctuating up to 5.5 degreesC. After 3600 C-14 yr BP, the dinocyst record suggests a trend of decreasing temperature toward modern values, marked by recurrent cooling events. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; Dalhousie Univ, Dept Earth Sci, Halifax, NS B3H 3J5, Canada; Geol Survey Canada, Ottawa, ON K1A 0E8, Canada	University of Quebec; University of Quebec Montreal; Dalhousie University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Univ Quebec, GEOTOP, POB 8888, Montreal, PQ H3C 3P8, Canada.	r21024@er.uqam.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				AKSU AE, 1983, MAR GEOL, V53, P331, DOI 10.1016/0025-3227(83)90049-X; ANDREWS JT, 1980, ARCTIC ALPINE RES, V12, P41, DOI 10.2307/1550589; [Anonymous], 1985, Quaternary Environments: Eastern Canadian Arctic; [Anonymous], CALIB RADIOCARBON CA; [Anonymous], ACTA U OULUENSIS SCI; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; AUSTIN WEN, 1995, RADIOCARBON, V37, P53, DOI 10.1017/S0033822200014788; Barber DC, 1999, NATURE, V400, P344, DOI 10.1038/22504; BARD E, 1994, EARTH PLANET SC LETT, V126, P275, DOI 10.1016/0012-821X(94)90112-0; Bard E, 1988, PALEOCEANOGRAPHY, V3, P635, DOI 10.1029/PA003i006p00635; Blake Jr W., 1979, 791C GEOL SURV CAN, P105; BLAKE W, 1989, RADIOCARBON, V31, P570; BLAKE W, 1992, CAN J EARTH SCI, V29, P1958, DOI 10.1139/e92-153; BLAKE W, 1995, CANQUA CGRG JOINT M; Blake W.J., 1992, MEDD GR NL GEOSCI, V27, P1; Blake W, 1998, B GEOL SOC DENMARK, V44, P129; Bourgeois JC, 2000, QUATERNARY RES, V54, P275, DOI 10.1006/qres.2000.2156; Bourgeois JC, 1985, ANN GLACIOL, V7, P109, DOI DOI 10.1017/S0260305500006005; BRADLEY RS, 1990, QUATERNARY SCI REV, V9, P365, DOI 10.1016/0277-3791(90)90028-9; BRASSARD GR, 1978, CAN J BOT, V56, P1852, DOI 10.1139/b78-224; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1996, 3 U QUEB; DUNBAR M, 1972, PROC R SOC EDIN B-BI, V72, P231, DOI 10.1017/S0080455X00001788; Dyke AS, 1997, ARCTIC, V50, P1; Dyke AS, 1996, ARCTIC, V49, P235; England J, 1999, QUATERNARY SCI REV, V18, P421, DOI 10.1016/S0277-3791(98)00070-5; FISHER DA, 1995, HOLOCENE, V5, P19, DOI 10.1177/095968369500500103; Fredskild B., 1985, Geoscience, V14, P1; FUNDER S, 1991, PALAEOGEOGR PALAEOCL, V85, P123, DOI 10.1016/0031-0182(91)90029-Q; FUNDER S, 1978, DANISH METEOROLOGICA, V4, P175; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; Haflidason H, 2000, J QUATERNARY SCI, V15, P3, DOI 10.1002/(SICI)1099-1417(200001)15:1<3::AID-JQS530>3.0.CO;2-W; HEGG O, 1963, AXEL HEIBERG ISLAND, P217; Ito H., 1982, ZURCHER GEOGRAPHISCH, V7, P1; Kelly M, 1999, QUATERNARY SCI REV, V18, P373, DOI 10.1016/S0277-3791(98)00004-3; KOERNER RM, 1990, NATURE, V343, P630, DOI 10.1038/343630a0; KOERNER RM, 1989, QUATERNARY GEOLOGY C, P464; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; Kutzbach J. 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J	Howe, JA; Stoker, MS; Woolfe, KJ				Howe, JA; Stoker, MS; Woolfe, KJ			Deep-marine seabed erosion and gravel lags in the northwestern Rockall Trough, North Atlantic Ocean	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article						Rockall Trough; erosion; gravel; sediment transport; contourite	FENI DRIFT; DINOFLAGELLATE CYSTS; FALKLAND TROUGH; SEDIMENT DRIFTS; SLOPE-CURRENT; CONTOURITES; DEPOSITS; VELOCITY; FACIES	A zone of active seabed erosion has been identified in the northwestern Rockall Trough using seismic reflection profiles and cores. The region from George Bligh Bank to Rockall Bank has been subject to vigorous bottom-current activity, for at least the last 35 Ma. Bottom currents originate from southward flowing North Atlantic Deep Water, in water depths of 500-2000 m. Acoustic character mapping reveals a zone of erosion extending over 8500 km(2) along the northwestern margins of the trough. The erosion surface is characterized by an acoustically reflective seabed, with occasional parallel to transparent reflectors. These are the result of strong bottom-currents exposing the underlying volcanic basement, drift sequences and fall sediments. The erosion surface is covered by a < 10 m veneer of Quaternary sediment. The majority of the basin consists of well-stratified. parallel Quaternary drift and hemipelagite sequences. Along the western margin of the trough, these sediments form broad-sheeted drifts. Eocene sediments adjacent to George Bligh Bank have been exposed by strong bottom-currents for the last 35 Ma, compared with the flanks of Rockall Bank, where sedimentation was intermittent. Core sampling from George Bligh Bank and Rockall Bank recovered Quaternary gravelly-sandy muds interpreted as gravel lags, and muddy sandy contourites; overlying early-mid-Eocene aged sediments. The gravels represent the influence of a strongest North Atlantic Deep Water flow, winnowing coarse sediment into 'lags', commonly preserved within sandy contourite sequences.	Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, POB 3, Oban PA34 4AD, Argyll, Scotland; Univ Highlands & Isl Project, Dunstaffnage Marine Lab, Oban PA34 4AD, Argyll, Scotland; British Geol Survey, Edinburgh EH9 3LA, Midlothian, Scotland; James Cook Univ N Queensland, Sch Earth Sci, Townsville, Qld 4811, Australia	University of the Highlands & Islands; University of the Highlands & Islands; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; James Cook University	Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, POB 3, Oban PA34 4AD, Argyll, Scotland.			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Geol. Soc.	MAY	2001	158		3				427	438		10.1144/jgs.158.3.427	http://dx.doi.org/10.1144/jgs.158.3.427			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	428JM					2025-03-11	WOS:000168458600005
J	Burkholder, JM; Glasgow, HB; Deamer-Melia, N				Burkholder, JM; Glasgow, HB; Deamer-Melia, N			Overview and present status of the toxic <i>Pfiesteria</i> complex (Dinophyceae)	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA				ESTUARINE DINOFLAGELLATE; PHANTOM DINOFLAGELLATE; P-2Z RECEPTOR; WATER-QUALITY; LIFE-CYCLE; PISCICIDA; ATP; CHROMOSOMES; MANAGEMENT; EXPOSURE	This paper reviews the Pfiesteria issue and Pfiesteria science and presents new information on variation in toxicity among Pfiesteria strains, culture effects on their toxicity, the trophic interactions of pfiesteria spp., and impacts on fish and mammals. We also assess Pfiesteria spp. impacts on fish in comparison to certain other estuarine dinoflagellates of similar appearance. Species of the toxic Pfiesteria complex (TPC) thus far include P. piscicida and P. shumwayae. These species share morphological and genetic similarities, and both have toxic strains that (1) show strong attraction to live fish; (2) exhibit toxicity that is triggered by live fish or their fresh tissues and excreta; and (3) produce toxin(s) that cause fish stress, disease and death under ecologically relevant conditions (the standardized fish bioassay process involves testing live Pfiesteria cells at similar densities to those encountered during Pfiesteria-related fish kill/disease events). Both Pfiesteria species also have a complex life cycle with multiple amoeboid, flagellated and Cyst stages, several of which are ichthyotoxic. TPC species are eurythermal and euryhaline, with prey spanning the estuarine food web, from bacteria to mammalian tissues. They can be stimulated directly or indirectly by nitrogen and phosphorus enrichment. Toxic strains can be either actively or potentially toxic (the TOX-A and TOX-B functional types, respectively); in addition, c. 40% of randomly isolated clones have been found to be benign [the noninducible or NON-IND functional type, which apparently lacks the ability to produce bioactive substances (toxins) that cause fish disease or death]. These functional types differ significantly in response to algal prey, predators, nutrients and fish. Moreover, as an apparent artifact of culture conditions, toxic strains generally lose their ability to cause fish death and disease and become NON-IND within weeks to months. At low cell densities, toxic strains can be causative agents of acute and/or chronic diffuse and focal lesions and of other fish diseases, as demonstrated in fish bioassays. A partially purified, water-soluble Pfiesteria toxin disrupts calcium metabolism in rat pituitary cells and mimics an adenosine triphosphate neurotransmitter that targets P2X(7) purinoreceptors found predominantly on immune cells. Respiratory, visual, and neurological impacts have been sustained by people exposed to aerosols from fish-killing Pfiesteria cultures or to water and aerosols during estuarine fish kills associated with toxic Pfiesteria. Neurocognitive impacts from exposure to toxic Pfiesteria have been replicated experimentally in small mammals. Toxic strains of Pfiesteria species have been confirmed from mid-Atlantic and Gulf Coast estuaries in the United States and from northern Europe and New Zealand, indicating that these toxic dinoflagellates are cosmopolitan in distribution.	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.	joann_burkholder@ncsu.edu						ALLEN IC, 2000, THESIS U NC GREENSBO; ANDERSON RH, 1991, J CARDIAC SURG, V6, P41, DOI 10.1111/j.1540-8191.1991.tb00562.x; [Anonymous], ALGAL TOXINS SEAFOOD; BADEN DG, 1997, NAT I ENV HLTH SCI N; Bates S.S., 1998, Physiological Ecology of Harmful Algal Blooms, P267; BOESCH D, 1997, CAMBRIDGE CONSENSUS; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; BUCKLANDNICKS JA, 1990, J PHYCOL, V26, P539, DOI 10.1111/j.0022-3646.1990.00539.x; Burkholder J.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P175; Burkholder JM, 1999, HUM ORGAN, V58, P443, DOI 10.17730/humo.58.4.976098q356672751; Burkholder JM, 1997, J ENVIRON QUAL, V26, P1451, DOI 10.2134/jeq1997.00472425002600060003x; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; 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, 1999, SCI AM, V281, P42, DOI 10.1038/scientificamerican0899-42; Burkholder JM, 1998, ECOL APPL, V8, pS37; BURKHOLDER JM, 1992, LIMNOL OCEANOGR, V37, P974, DOI 10.4319/lo.1992.37.5.0974; BURKHOLDER JM, 2000, OPPORTUNITIES ENV AP, P126; BURSA A, 1970, ARCTIC ALPINE RES, V1, P152; Bursa A. 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J	Glasgow, HB; Burkholder, JM; Morton, SL; Springer, J				Glasgow, HB; Burkholder, JM; Morton, SL; Springer, J			A second species of ichthyotoxic <i>Pfiesteria</i> (Dinamoebales, Dinophyceae)	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA				TOXIC DINOFLAGELLATE; FISH KILLS; PISCICIDA; COMPLEX; MANAGEMENT; IMPACTS; RIVER; ASSAY	A second toxic species within the family Pfiesteriaceae, Pfiesteria shumwayae Glas.-ow & Burkholder sp. nov., is described from the New River Estuary and the Neuse Estuary of the Albemarle-Pamlico Estuarine Ecosystem, USA. The species is polymorphic and multiphasic, with flagellated, amoeboid and cyst stages. The flagellated zoospores (diameter 8-24 mum) have permanently condensed chromosomes (mesokaryotic nucleus); a chrysophyte-like cyst (diameter 6-25 mum) With organic scales and bracts; and thin thecal plates arranged in a Kofoidian series of Po, cp, X, 4', 1a, 6", 6c, 4s, 5"', 2''''. The benthic filopodial (filose), lobopodial (lobose) and rhizopodial amoeboid stages (5-250 mum) have an outer covering that ranges from rough to smooth in texture, depending on the stage of origin and the prey source, Pfiesteria shumwayae amoebae have a normal eukaryote nucleus and cysts of multiple sizes (diameter 4-25 mum) With a reticulate outer covering, Toxic strains of the two Pfiesteria species have overlapping distributions in the mid-Atlantic and southeastern United States and Scandinavia, with toxic P. shumwayae also having been verified from New Zealand. Pfiesteria shumwayae is similar to P. piscicida in its complex life cycle, general nutrition, attraction to live fish prey, and ichthyotoxic activity that is stimulated by the presence of live fish or their fresh tissues and excreta. However, it can be distinguished from P. piscicida morphologically by having six precingular plates and a four-sided I a plate, as well as genetically, on the basis of its 18S ribosomal DNA sequence.	N Carolina State Univ, Ctr Appl Aquat Ecol, Raleigh, NC 27606 USA; NOAA, Natl Ocean Serv, Ctr Coastal Environm Hlth & Biomol Res, Marine Biotoxin Program, Charleston, SC 29412 USA	North Carolina State University; National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA	N Carolina State Univ, Ctr Appl Aquat Ecol, 620 Hutton St,Suite 104, Raleigh, NC 27606 USA.	howard_glasgow@ncsu.edu						ALLEN IC, 2000, THESIS U N CAROLINA; BOVEE EC, 1979, MARINE FLORA FAUNA N; BUCKLANDNICKS J, 1995, ARCH PROTISTENKD, V145, P165, DOI 10.1016/S0003-9365(11)80313-1; BURKHOLDE RJM, 1999, MICROBIAL SIGNALING, P220; Burkholder J.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P175; Burkholder JM, 2001, PHYCOLOGIA, V40, P186, DOI 10.2216/i0031-8884-40-3-186.1; Burkholder JM, 1999, MAR ECOL PROG SER, V179, P301, DOI 10.3354/meps179301; Burkholder JM, 1997, J ENVIRON QUAL, V26, P1451, DOI 10.2134/jeq1997.00472425002600060003x; BURKHOLDER JM, 1995, MAR ECOL PROG SER, V124, P43, DOI 10.3354/meps124043; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; 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, 1998, ECOL APPL, V8, pS37; BURKHOLDER JM, 1992, LIMNOL OCEANOGR, V37, P974, DOI 10.4319/lo.1992.37.5.0974; Burrells W., 1977, MICROSCOPE TECHNIQUE; BURSA A, 1970, ARCTIC ALPINE RES, V1, P152; Bursa A. 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A., 1999, Virginia Journal of Science, V50, P325; SCHNEPF E, 1992, EUR J PROTISTOL, V28, P3, DOI 10.1016/S0932-4739(11)80315-9; Seaborn David W., 1999, Virginia Journal of Science, V50, P337; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; Shumway Sandra E., 1995, Reviews in Fisheries Science, V3, P1; Smith S.A., 1988, P 3 INT C PATH MAR A, P167; SPRINGER JJ, 2000, THESIS N CAROLINA ST; Steidinger K.A., 1984, P201; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; STEIDINGER KA, 1989, HARMFUL MARINE ALGAL, P83; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; Tanner R. S., 2007, Manual of environmental microbiology, P69; *WALZ GMBH H, 1999, PHYT AN PHYTO PAMS S; West G.S., 1927, TREATISE BRIT FRESHW	55	56	61	1	12	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	MAY	2001	40	3					234	245		10.2216/i0031-8884-40-3-234.1	http://dx.doi.org/10.2216/i0031-8884-40-3-234.1			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Marine & Freshwater Biology	465MG					2025-03-11	WOS:000170592300006
J	Hamer, JP; Lucas, IAN; McCollin, TA				Hamer, JP; Lucas, IAN; McCollin, TA			Harmful dinoflagellate resting cysts in ships' ballast tank sediments: potential for introduction into English and Welsh waters	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA				ALEXANDRIUM; DINOPHYCEAE; TRANSPORT	Sediment samples taken from ballast tanks of ships in English and Welsh ports were examined for the presence of dinoflagellate resting cysts. Cysts with apparently viable cell contents, identifiable to at least genus level, were found in 69% of samples; 48 species were identified, representing 20 genera. A maximum of 22 cyst types were found in a single sample, but most samples contained less than five. Maximum recorded cyst concentration was 8950 cysts ml(-1) wet sediment. The majority of samples contained < 400 cysts ml(-1). Potentially harmful cyst types included toxic, bloom-forming, and nonindigenous species. Alexandrium species were recorded in 25% of samples, A. tamarense/catenella cysts being the most common, occurring in 17% of samples. In addition to the germination of observed cysts, slurry enrichments also produced motile stages of smaller species unrecorded in microscopical surveys. Most cyst types found in this study have been recorded from UK waters, although a number of species previously unrecorded were identified. Our findings agree with other studies and demonstrate the frequent occurrence of the resting cysts of potentially harmful dinoflagellate species in ballast tank sediments. The lack of any clear correlation between the dinoflagellate cyst assemblage and the origin of the ballast water was ascribed to the complex nature of ballast water management on modern vessels with dedicated ballast tanks. Based on these findings, we question the scope for predicting the presence of particular harmful dinoflagellate cysts in specified ballast tank sediments for the majority of UK shipping traffic.	Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales		Hamer, JP (通讯作者)，Univ Wales, Sch Ocean Sci, Menai Bridge, Menai Bridge LL59 5EY, Gwynedd, Wales.							Anderson D.M., 1989, P11; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Guillard RRL., 1973, HDB PHYCOLOGICAL MET, P69; HALLEGRAEFF GM, 1988, J PLANKTON RES, V10, P533, DOI 10.1093/plankt/10.3.533; 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, IOC MANUALS GUIDES, V1, P33; Hamer J. P., 1998, RAPPORT BOT SERIE, V1, P53; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Harvey M, 1999, 2268 FISH AQ SCI; Hay C., 1997, 417 CAWTHR I; IMAI I, 1988, Bulletin of Plankton Society of Japan, V35, P35; KELLY JM, 1993, J SHELLFISH RES, V12, P405; LARSEN J, 1995, PHYCOLOGIA, V34, P135, DOI 10.2216/i0031-8884-34-2-135.1; MACDONALD EM, 1998, 397 FISH RES SERV MA; Matsuura K, 1995, STUD APPL ELECTROMAG, V7, P381; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	20	53	59	6	25	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAY	2001	40	3					246	255		10.2216/i0031-8884-40-3-246.1	http://dx.doi.org/10.2216/i0031-8884-40-3-246.1			10	Plant Sciences; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	465MG					2025-03-11	WOS:000170592300007
J	Itakura, S; Yamaguchi, M				Itakura, S; Yamaguchi, M			Germination characteristics of naturally occurring cysts of <i>Alexandrium tamarense</i> (Dinophyceae) in Hiroshima Bay, Inland Sea of Japan	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA				DINOFLAGELLATE GONYAULAX-EXCAVATA	In order to examine temporal changes in the germination ability, time to germination and autofluorescence properties of the resting cysts of the toxic dinoflagellate Alexandrium tamarense, a long-term investigation was conducted in Hiroshima Bay. In Hiroshima Bay, a spring bloom (March to May) of A. tamarense has been observed almost every year since 1992. Approximately 50 resting cysts were isolated monthly from the bottom sediment between June 1994 and June 1997. The cysts were incubated from the day of sampling onwards under in situ bottom water temperature conditions, and germination success and the emission of autofluorescence were checked every day. High germination success rates (> 50%) were observed between December and April each year (bottom water temperature = 10.0-16.5 degreesC), with an average germination time of 10.2 days (n = 455). Resting cysts were found to start to emit red autofluorescence a few days before germination (average duration = 3.1 days, n = 449), and germination time was nearly constant within the temperature range 10-20 degreesC. From June to November, germination success rates were considerably lower (0-40%, bottom water temperature = 14.6-23.9 degreesC). No germination at all was observed in September (bottom temperature = 23.6-23.9 degreesC). The relationship between the incubation temperature and the rate of germination success indicates that the resting cysts have a temperature 'window' (c. 10-15 degreesC) for germination, which controls the seasonal change in germination ability. The present results indicate that the germination characteristics of A. tamarense resting cysts are well adapted to the ambient water temperature rhythm in temperate shallow coastal environments, allowing A. tamarense to seed vegetative cell populations for the spring bloom.	Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Harmful Phytoplankton Sect, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Itakura, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Harmful Phytoplankton Sect, Hiroshima 7390452, Japan.							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, 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., 1995, IOC MAN GUIDES, V33, P229; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; [Anonymous], 1986, B TOHOKU REGIONAL FI; ASAKAWA M, 1995, TOXICON, V33, P691, DOI 10.1016/0041-0101(94)00177-A; Asakawa M., 1995, J FOOD HYG SOC JPN, V34, P50; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; FUKUYO Y, 1985, B MAR SCI, V37, P529; FUKUYO Y, 1982, THESIS U TOKYO; Kotani Yuichi, 1998, Bulletin of the Japanese Society of Fisheries Oceanography, V62, P104; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; UCHIDA T, 1980, Japanese Journal of Phycology, V28, P133; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; YAMAMOTO M, 1996, HARMFUL TOXIC ALGAL, P19; Yamamoto Tamiji, 1997, Japanese Journal of Phycology, V45, P95; YENTSCH CM, 1980, BIOSCIENCE, V30, P251, DOI 10.2307/1307880	20	38	44	1	10	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAY	2001	40	3					263	267		10.2216/i0031-8884-40-3-263.1	http://dx.doi.org/10.2216/i0031-8884-40-3-263.1			5	Plant Sciences; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	465MG					2025-03-11	WOS:000170592300009
J	Kitaguchi, H; Hiragushi, N; Mitsutani, A; Yamaguchi, M; Ishida, Y				Kitaguchi, H; Hiragushi, N; Mitsutani, A; Yamaguchi, M; Ishida, Y			Isolation of an algicidal marine bacterium with activity against the harmful dinoflagellate <i>Heterocapsa</i> <i>circularisquama</i> (Dinophyceae)	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA				RED TIDE; GYMNODINIUM-NAGASAKIENSE; GLIDING BACTERIUM; HIROSHIMA BAY; PEARL OYSTERS; CYTOPHAGA SP; JAPAN; GROWTH; SEA; RAPHIDOPHYCEAE	Red tides of a harmful dinoflagellate, Heterocapsa circularisquama, have caused mass mortality of bivalves such as oysters in western Japan since 1988. For the purpose of microbial control of the occurrence of these red tides, H. circularisquama-killing bacteria were screened. Although the frequency of H. circularisquama-killing microorganisms was low during the sampling period, a marine bacterium strain EHK-1, which had a strong algicidal activity against H. circularisquama, was isolated from the seawater of Etajima Bay, in the Seto Inland Sea of Japan. Strain EHK-1 killed H. circularisquama within 24 hours when the H. circularisquama culture in exponential phase was inoculated with this bacterium at a density of 1 x 10(5) cells ml(-1). Strain EHK-1 lysed both the vegetative cells and temporary cysts of H. circularisquama. Strain EHK-1 is a novel algicidal bacterium according to 16S rRNA-based phylogenetic analysis.	Fukuyama Univ, Hiroshima 7290292, Japan; Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan	Fukuyama University; Japan Fisheries Research & Education Agency (FRA)	Kitaguchi, H (通讯作者)，Fukuyama Univ, Sanzo 1,Gakuen Cho, Hiroshima 7290292, Japan.							CHEN LCM, 1969, J PHYCOL, V5, P211, DOI 10.1111/j.1529-8817.1969.tb02605.x; DAFT MJ, 1975, FRESHWATER BIOL, V5, P577, DOI 10.1111/j.1365-2427.1975.tb00157.x; Doucette GJ, 1999, J PHYCOL, V35, P1447, DOI 10.1046/j.1529-8817.1999.3561447.x; FELSENSTEIN J, 1985, EVOLUTION, V39, P783, DOI 10.1111/j.1558-5646.1985.tb00420.x; FUKAMI K, 1991, NIPPON SUISAN GAKK, V57, P2321; FUKAMI K, 1992, NIPPON SUISAN GAKK, V58, P1073; Horiguchi Takeo, 1995, Phycological Research, V43, P129, DOI 10.1111/j.1440-1835.1995.tb00016.x; IMAI I, 1991, NIPPON SUISAN GAKK, V57, P1409, DOI 10.2331/suisan.57.1409; 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, 1999, Bulletin of Plankton Society of Japan, V46, P172; Imai Ichiro, 1998, Phycological Research, V46, P139, DOI 10.1111/j.1440-1835.1998.tb00106.x; ISHIDA Y, 1986, MAR ECOL PROG SER, V30, P197, DOI 10.3354/meps030197; Itoh K., 1987, GUIDE STUDIES RED TI, P122; Kim MC, 1998, MAR ECOL PROG SER, V170, P25, DOI 10.3354/meps170025; KIMURA M, 1980, J MOL EVOL, V16, P111, DOI 10.1007/BF01731581; Kondo R, 1999, FISHERIES SCI, V65, P432, DOI 10.2331/fishsci.65.432; Lovejoy C, 1998, APPL ENVIRON MICROB, V64, P2806; Maeda T, 1998, FISHERIES SCI, V64, P861, DOI 10.2331/fishsci.64.861; MATSUYAMA Y, 1995, NIPPON SUISAN GAKK, V61, P35; Matsuyama Y, 1997, MAR ECOL PROG SER, V146, P73, DOI 10.3354/meps146073; MITSUTANI A, 1992, NIPPON SUISAN GAKK, V58, P2159; Mitsutani Atsushi, 1997, Journal of National Fisheries University, V45, P165; Nagai K, 1996, AQUACULTURE, V144, P149, DOI 10.1016/S0044-8486(96)01307-5; Nagasaki K, 2000, NIPPON SUISAN GAKK, V66, P666; NISHIHARA T, 1986, EISEI KAGAKU, V32, P226, DOI 10.1248/jhs1956.32.226; SAITOU N, 1987, MOL BIOL EVOL, V4, P406, DOI 10.1093/oxfordjournals.molbev.a040454; STEWART JR, 1969, SCIENCE, V164, P1523, DOI 10.1126/science.164.3887.1523; THOMPSON JD, 1994, NUCLEIC ACIDS RES, V22, P4673, DOI 10.1093/nar/22.22.4673; Yamaguchi, 1998, B NANSEI NATL FISH R, V31, P53; YAMAMOTO Y, 1981, Japanese Journal of Limnology, V42, P20; YAMAMOTO Y, 1990, J PHYCOL, V26, P457, DOI 10.1111/j.0022-3646.1990.00457.x; YOSHINAGA I, 1995, FISHERIES SCI, V61, P780, DOI 10.2331/fishsci.61.780; YOSHINAGA I, 1998, MARINE ECOLOGY PROGR, V170, P32	34	12	15	1	6	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAY	2001	40	3					275	279		10.2216/i0031-8884-40-3-275.1	http://dx.doi.org/10.2216/i0031-8884-40-3-275.1			5	Plant Sciences; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	465MG					2025-03-11	WOS:000170592300011
J	Lewis, J; Kennaway, G; Franca, S; Alverca, E				Lewis, J; Kennaway, G; Franca, S; Alverca, E			Bacterium-dinoflagellate interactions:: investigative microscopy of <i>Alexandrium</i> spp. (Gonyaulacales, Dinophyceae)	PHYCOLOGIA			English	Article; Proceedings Paper	9th International Conference on Harmful Algal Blooms	FEB 07-11, 2000	HOBART, AUSTRALIA					The association of bacteria With dinoflagellates has been a neglected field of study, which has gained prominence in recent years because of the possible role of bacteria in toxin synthesis. A number of dinoflagellates undergo sexual reproduction, passing through various life-cycle stages in addition to the vegetative form. The presence of bacteria within dinoflagellates has been well established, but their presence throughout the dinoflagellate life-cycle has not been investigated. Using cultures of Alexandrium (A. tamarense, A. fundyense), We investigated the association of bacteria With various vegetative growth phases (lag, log, stationary) and sexual life-cycle stages (planozygote, planomeiocyte, hypnozygote), using scanning electron microscopy, transmission electron microscopy (TEM) and epifluorescence microscopy. Bacteria were found to be associated with the surfaces of vegetative cells, planozygotes, hypnozygotes and planomeiocytes. TEM showed bacteria to be present within all vegetative growth phases, as well as in the sexual planozygote, cyst and planomeiocyte. The presence of intracellular bacteria in vegetative cells was also confirmed using DAPI staining combined with epifluorescence microscopy, and lipopolysaccharide staining combined with TEM.	Univ Westminster, Sch Biosci, Appl Ecol Res Grp, London W1M 8JS, England; Natl Inst Hlth Dr Ricardo Jorge, LME, P-1649016 Lisbon, Portugal	University of Westminster; Instituto Nacional de Saude Dr. Ricardo Jorge	Univ Westminster, Sch Biosci, Appl Ecol Res Grp, 115 New Cavendish St, London W1M 8JS, England.	lewisjm@westminster.ac.uk						Bibby B.T., 1972, British phycol J, V7, P85; CHANG J, 1994, J PLANKTON RES, V16, P197, DOI 10.1093/plankt/16.2.197; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; CHAPMAN DV, 1981, BRIT PHYCOL J, V16, P183, DOI 10.1080/00071618100650191; Dale B., 1983, P69; DEMPSEY MJ, 1981, MAR BIOL, V61, P305, DOI 10.1007/BF00401570; DETRAUBENBERG CR, 1995, EUR J PROTISTOL, V31, P318, DOI 10.1016/S0932-4739(11)80096-9; Doucette G.J., 1998, PHYSL ECOLOGY HARMFU, P619; Franca Susana, 1995, P45; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; GAO XP, 1989, BRIT PHYCOL J, V24, P153; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; KARNOVSKY MJ, 1965, J CELL BIOL, V27, pA137; PREER JR, 1974, BACTERIOL REV, V38, P113, DOI 10.1128/MMBR.38.2.113-163.1974; SILVA E S, 1985, Protistologica, V21, P429; SILVA ES, 1978, PROTISTOLOGICA, V14, P113; Silva ES., 1982, MAR PHARM SCI, V2, P269, DOI [10.1515/9783110837506-015, DOI 10.1515/9783110837506-015]; SOYER MO, 1977, BIOL CELLULAIRE, V30, P297; Steidinger K.A., 1996, Nova Hedwigia Beiheft, V112, P415; THIERY JP, 1974, J MICROSC-PARIS, V21, P225	20	27	34	2	24	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	MAY	2001	40	3					280	285		10.2216/i0031-8884-40-3-280.1	http://dx.doi.org/10.2216/i0031-8884-40-3-280.1			6	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Marine & Freshwater Biology	465MG					2025-03-11	WOS:000170592300012
J	Swadling, KM; Dartnall, HJG; Gibson, JAE; Saulnier-Talbot, E; Vincent, WF				Swadling, KM; Dartnall, HJG; Gibson, JAE; Saulnier-Talbot, E; Vincent, WF			Fossil rotifers and the early colonization of an Antarctic lake	QUATERNARY RESEARCH			English	Article						fossil; rotifers; Notholca; Holocene; Antarctic biogeography; lakes; paleoecology; colonization	VESTFOLD HILLS; COPEPODA; HISTORY; LIFE	Early Holocene sediments from a continental Antarctic lake (Ace Lake, Vestfold Hills, East Antarctica) contained abundant fossil rotifers of the genus Notholca, The fossil is similar to specimens of Notholca sp, present in modern-day Ace Lake and other fresh and brackish lakes of the Vestfold Hills. Cyanobacteria and protists (chrysophyte cysts, dinoflagellate cysts, and rhizopod tests) were also recovered from the core samples. These sediments were deposited early in the freshwater phase of Ace Lake, soon after deglaciation of the area, The occurrence of this trophically diverse assemblage of organisms at an early stage in the evolution of the lake suggests either that they were part of an endemic Antarctic flora and fauna which pre-dated the last glacial maximum and survived in glacial refugia or that efficient intercontinental dispersal had occurred. (C) 2001 University of Washington.	Univ Laval, Ctr Etud Nord, Ste Foy, PQ G1K 7P4, Canada; Macquarie Univ, Dept Biol Sci, N Ryde, NSW 2109, Australia; Australian Antarctic Div, Kingston, Tas 7050, Australia	Laval University; Macquarie University; Australian Antarctic Division	Univ Tasmania, Sch Zool, GPO Box 252-5, Hobart, Tas 7001, Australia.		Saulnier-Talbot, Émilie/HPC-6771-2023; Vincent, Warwick/AAH-6152-2019	Swadling, Kerrie/0000-0002-7620-841X; Saulnier-Talbot, Emilie/0000-0002-7193-0577; Vincent, Warwick/0000-0001-9055-1938				Adamson D., 1986, Antarctic oasis: terrestrial environments and history of the Vestfold Hills, P63, DOI DOI 10.1093/MOLBEV/MSH157; BAYLY IAE, 1993, PROC INT ASSOC THEOR, V25, P975; BAYLY IAE, 1978, AUST J MAR FRESH RES, V29, P817; BAYLY IAE, 1994, POLAR BIOL, V14, P253; CWYNAR LC, 1995, QUATERNARY RES, V43, P405, DOI 10.1006/qres.1995.1046; DARTNALL HJG, 2000, 141 ANARE; ELLISEVANS JC, 1990, P NIPR S POL BIOL, V3, P151; EVERITT DA, 1981, HYDROBIOLOGIA, V83, P225, DOI 10.1007/BF00008270; Gibson JAE, 1998, POLAR BIOL, V19, P148, DOI 10.1007/s003000050227; Hariston NG, 1999, LIMNOL OCEANOGR, V44, P477; HAWES I, 1992, POLAR BIOL, V12, P587; Kerfoot WC, 1999, LIMNOL OCEANOGR, V44, P1232, DOI 10.4319/lo.1999.44.5.1232; KUTIKOVA LA, 1964, INFORMATION B, V1, P88; Rankin L.M., 1999, POLARFORSCHUNG, V66, P33; Roberts D, 1999, HOLOCENE, V9, P515, DOI 10.1191/095968399672424476; Roberts D, 1999, HOLOCENE, V9, P401, DOI 10.1191/095968399671725699; Vincent W.F., 2006, The Ecology of Cyanobacteria, P321, DOI [10.1007/0-306-46855-7_12, DOI 10.1007/0-306-46855-7_12]; Vincent WF, 2000, NATURWISSENSCHAFTEN, V87, P137, DOI 10.1007/s001140050692; Vincent WF, 2000, ANTARCT SCI, V12, P374, DOI 10.1017/S0954102000000420; Vincent WF, 2000, SCIENCE, V287, P2421; Walker IR, 1997, J PALEOLIMNOL, V18, P165, DOI 10.1023/A:1007997602935; Zwartz D, 1998, EARTH PLANET SC LETT, V155, P131, DOI 10.1016/S0012-821X(97)00204-5	22	18	19	1	11	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0033-5894	1096-0287		QUATERNARY RES	Quat. Res.	MAY	2001	55	3					380	384		10.1006/qres.2001.2222	http://dx.doi.org/10.1006/qres.2001.2222			5	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	436VR					2025-03-11	WOS:000168957000013
J	Wendler, J; Wendler, I; Willems, H				Wendler, J; Wendler, I; Willems, H			<i>Orthopithonella collaris</i> sp nov., a new calcareous dinoflagellate cyst from the K/T boundary (Fish Clay, Stevns Klint/Denmark)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						calcareous dinoflagellate cysts; K/T boundary; Boreal; Fish Clay; Stevns Klint	CRETACEOUS-TERTIARY BOUNDARY; DENMARK; KLINT	A new calcareous dinoflagellate cyst species, Orthopithonella collaris sp. nov., is described from the Cretaceous/Tertiary (K/T) boundary clay (Fish Clay) of Stevns Klint, Denmark, on the basis of SEM studies and light-microscopic analyses of thin sections of single specimens. The species has: been found exclusively in the Fish Clay and as such may be a potential marker for the WT boundary. Its pulse-like occurrence is thought to be due to the abrupt, relatively short-term ecological catastrophe associated with the WT boundary event. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Wendler, J (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.							ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; [Anonymous], [No title captured]; Birkelund T., 1982, Geological Society of America Special Papers, V190, P373; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BUTSCHLI O, 1885, KLASSEN ORDNUNGEN TH, V1, P865; Christensen L., 1973, B GEOL SOC DENMARK, V22, P193; Ehrenberg C.G., 1831, SYMBOLAE PHYSICAE PA; Fensome R. A., 1993, MICROPALAEONTOLOGY, V7; Futterer D.K., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P533; FUTTERER DK, 1984, DEEP SEA DRILLING PR, P533; Haeckel E., 1894, SYSTEMATISCHE PHYLOG, P400; Hildebrand-Habel T, 1999, REV PALAEOBOT PALYNO, V106, P57, DOI 10.1016/S0034-6667(98)00079-7; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; KASTNER M, 1984, SCIENCE, V226, P137, DOI 10.1126/science.226.4671.137; Keupp H., 1991, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V134, P127; Keupp H., 1989, Berliner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V106, P207; Keupp H., 1984, Facies, V10, P153, DOI 10.1007/BF02536691; Kienel U., 1994, BERLINER GEOWISSENSC, V12, P87; NEUMANN C, 1999, BERLINER GEOWISS ABH, V31, P79; Pascher A., 1914, Berlin Ber D bot Ges, V32; SCHMITZ B, 1992, PALAEOGEOGR PALAEOCL, V96, P233, DOI 10.1016/0031-0182(92)90104-D; Smit J, 1999, ANNU REV EARTH PL SC, V27, P75, DOI 10.1146/annurev.earth.27.1.75; WENDLER J, 2001, UNPUB SPEC VOL C CAT; WENDLER J, 2001, UNPUB ANAL MID CENOM; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Willems H, 1996, GEOL MIJNBOUW, V75, P215; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; Willems Helmut, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V198, P141; Young JR, 1997, PALAEONTOLOGY, V40, P875; ZUGEL P, 1994, COURIER FORSCH I SEN, V176	30	10	10	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAY	2001	115	1-2					69	77		10.1016/S0034-6667(01)00050-1	http://dx.doi.org/10.1016/S0034-6667(01)00050-1			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	453GF	11425348				2025-03-11	WOS:000169907600004
J	Crouch, EM; Heilmann-Clausen, C; Brinkhuis, H; Morgans, HEG; Rogers, KM; Egger, H; Schmitz, B				Crouch, EM; Heilmann-Clausen, C; Brinkhuis, H; Morgans, HEG; Rogers, KM; Egger, H; Schmitz, B			Global dinoflagellate event associated with the late Paleocene thermal maximum	GEOLOGY			English	Article						late Paleocene thermal maximum; dinoflagellates	PRODUCTIVITY; EXTINCTION; CHRONOLOGY; PALEOGENE; MARINE; END	The late Paleocene thermal maximum, or LPTM (ca. 55 Ma), represents a geologically brief time interval (similar to 220 k.y.) characterized by profound global warming and associated environmental change. The LPTM is marked by a prominent negative carbon isotope excursion (CIE) interpreted to reflect a massive and abrupt input of C-12-enriched carbon to the ocean-atmosphere reservoir, possibly as a result of catastrophic gas-hydrate release, on time scales equivalent to present-day rates of anthropogenic carbon input. The LPTM corresponds to important changes in the global distribution of biota, including mass extinction of marine benthic organisms, The dinoflagellate cyst record indicates that surfaced-dwelling marine plankton in marginal seas also underwent significant perturbations during the LPTM. We report on the dramatic response of representatives of the genus Apectodinium from two upper Paleocene-lower Eocene sections in the Southern (New Zealand) and Northern (Austria) Hemispheres, where the dinoflagellate records are directly correlated with the CIE, benthic foraminifera extinction event, and calcareous nannofossil zonation. The results indicate that the inception of Apectodinium-dominated assemblages appears to be synchronous on a global scale, and that the event is precisely coincident with the beginning of the LPTM. Apectodinium markedly declined in abundance near the end of the LPTM. This Apectodinium event may be associated with (1) exceptionally high global sea-surface temperatures and/or (2) a significant increase in marginal-marine surface-water productivity, Such a globally synchronous acme of dinoflagellate cysts is unprecedented within the dinoflagellate cyst fossil record.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Aarhus Univ, Inst Geol, DK-8000 Aarhus C, Denmark; Inst Geol & Nucl Sci, Lower Hutt, New Zealand; Geol Bundesanstalt, A-1031 Vienna, Austria; Ctr Earth Sci, SE-40530 Gothenburg, Sweden	Utrecht University; Aarhus University; GNS Science - New Zealand	Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Heilmann-Clausen, Claus/A-4848-2012; Rogers, Karyne/ABF-9317-2021; Brinkhuis, Henk/B-4223-2009; Crouch, Erica/C-2820-2013	Rogers, Karyne/0000-0001-8464-4337; Brinkhuis, Henk/0000-0003-0253-6610				Aubry MP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P158; Bains S, 2000, NATURE, V407, P171, DOI 10.1038/35025035; 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; Clyde WC, 1998, GEOLOGY, V26, P1011, DOI 10.1130/0091-7613(1998)026<1011:MCRTTL>2.3.CO;2; COSTA L I, 1976, Palaeontology (Oxford), V19, P591; DICKENS GR, 1995, PALEOCEANOGRAPHY, V10, P965, DOI 10.1029/95PA02087; Dickens GR, 1999, NATURE, V401, P752, DOI 10.1038/44486; Dickens GR, 2000, B SOC GEOL FR, V171, P37; Egger H, 2000, GFF, V122, P44, DOI 10.1080/11035890001221044; Egger H, 2000, B SOC GEOL FR, V171, P207, DOI 10.2113/171.2.207; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; Jan du Chene R.E., 1984, Cah. Micropaleontol., V3, P5; Jolley DW, 1998, REV PALAEOBOT PALYNO, V99, P265, DOI 10.1016/S0034-6667(97)00039-0; Kaiho K, 1996, PALEOCEANOGRAPHY, V11, P447, DOI 10.1029/96PA01021; Kelly DC, 1996, GEOLOGY, V24, P423; KENNETT JP, 1991, NATURE, V353, P225, DOI 10.1038/353225a0; KOCH PL, 1992, NATURE, V358, P319, DOI 10.1038/358319a0; Norris RD, 1999, NATURE, V401, P775, DOI 10.1038/44545; Partridge A., 1976, Australian Petroleum Exploration Association Journal, V16, P73; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; ROGERS KM, 2001, IN PRESS NZ J GEOLOG; Röhl U, 2000, GEOLOGY, V28, P927, DOI 10.1130/0091-7613(2000)28<927:NCFTLP>2.0.CO;2; Schmitz B, 1997, TERRA NOVA, V9, P95, DOI 10.1111/j.1365-3121.1997.tb00011.x; SCOTESE CP, 1992, 200692 U TEXAS ARLIN; Thomas DJ, 1999, PALEOCEANOGRAPHY, V14, P561, DOI 10.1029/1999PA900031; Thomas E., 1996, Geological Society Special Publication, V101, P401, DOI 10.1144/GSL.SP.1996.101.01.20; Thomas E, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P214; Wilson G.J., 1988, NZ GEOLOGICAL SURVEY, V57; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; ZACHOS JC, 1993, J GEOL, V101, P191, DOI 10.1086/648216	32	260	291	0	57	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613	1943-2682		GEOLOGY	Geology	APR	2001	29	4					315	318		10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2	http://dx.doi.org/10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	414YP					2025-03-11	WOS:000167694000007
J	Reguera, B; González-Gil, S				Reguera, B; González-Gil, S			Small cell and intermediate cell formation in species of <i>Dinophysis</i> (Dinophyceae, Dinophysiales)	JOURNAL OF PHYCOLOGY			English	Article						Dinophysis; DSP dinoflagellates; life cycle; morphological variability; polymorphism	DINOFLAGELLATE GENUS; LIFE-HISTORY; D-NORVEGICA; ACUMINATA; COMPLEX; FRESH; ACUTA	Observations of two distinct size classes with similar shape in natural populations of Dinophysis Ehrenberg were first reported by Jorgensen in 1923 and intermediate forms exhibiting a continuum between the typical vegetative cell and a putative small cell by Wood in 1954. Focused attention on Dinophysis spp, associated with diarrhetic shellfish intoxications in the last decade has provided new examples of small cells ill the genus, sometimes with contours dissimilar from the corresponding vegetative cells; dimorphic individuals; and large/small cell couplets, This work was based on in situ observations during intensive sampling for cell cycle studies of Dinophysis acuminata Claparede ct Lachmann, Dinophysis acuta Ehrenberg, Dinophysis caudata Saville-Kent, and Dinophysis tripos Gourret; on laboratory incubations of D. acuminata; and on a thorough search of documented information on morphological variability of Dinophysis spp, During ill situ division, most dividing cells exhibit a normal longitudinal fission, but some (1%-10%) undergo a "depauperating" fission, leading to pairs of dimorphic cells with dissimilar moieties, After separation and sulcal list regeneration, these dimorphic cells become D. skagii Paulsen, D, dens Pavillard, D. diegensis Kofoid, and D, diegensis Kofoid var. curvata-like individuals, which can also be observed forming couplets D, acuminata/D. skagii, D. acuta/D. dens, and D. caudata/D. diegensis attached by their ventral margins. Small cells can grow again to large size, as shown in laboratory incubations of D, acuminata, thus partly explaining observations of thecal intercalary bands, and intermediate forms, The sexual nature of the small cells will not be unequivocally demonstrated until controlled germination of the alleged cyst forms is achieved, and some intermediate forms may correspond to undescribed stages after cyst germination. These observations suggest common patterns in the life cycle of Dinophysis spp, Intraspecific morphological variability of Dinophysis spp, in a given geographic area can largely be attributed to small cell formation, as a response to changing environmental conditions, and may be a part of the sexual cycle of these species. Small cells seem to be able to enlarge, leading to intermediate cell and further vegetative cell formation as part of a three-looped life history pattern in Dinophysis.	Ctr Oceanog Vigo, Inst Espanol Oceanog, Vigo 36280, Spain	Spanish Institute of Oceanography	Ctr Oceanog Vigo, Inst Espanol Oceanog, Aptdo 1552, Vigo 36280, Spain.	beatriz.reguera@vi.ico.es	Reguera, Beatriz/AAG-8273-2020; Gonzalez-Gil, Sonsoles/K-8410-2019	Reguera, Beatriz/0000-0003-4582-9798; Gonzalez-Gil, Sonsoles/0000-0002-9186-9865				BALECH E, 1976, SARSIA, P75; BARDOUIL M, 1991, CR ACAD SCI III-VIE, V312, P663; BHAUD Y, 1988, J CELL SCI, V89, P197; Bravo I., 1995, P21; BURKHOLDER JM, 1992, NATURE, V360, P768, DOI 10.1038/360768e0; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; BURKHOLDER JM, 1998, NATO ASI SERIES G, V4, P175; CARPENTER EJ, 1988, MAR ECOL-PROG SER, V89, P83; Delgado M., 1996, HARMFUL TOXIC ALGAL, P261; Dodson A.N., 1978, Phytoplankton Manual, P104; FUKUYO Y, 1981, OTSUCHI MAR RES CENT, V7, P3; Giacobbe MG, 1997, J PHYCOL, V33, P73, DOI 10.1111/j.0022-3646.1997.00073.x; HANSEN G, 1993, PHYCOLOGIA, V32, P73, DOI 10.2216/i0031-8884-32-1-73.1; HANSEN PJ, 1991, MAR ECOL PROG SER, V69, P201, DOI 10.3354/meps069201; HERNANDEZBECERRIL DU, 1992, REV BIOL TROP, V40, P101; JACOBSON DM, 1994, PHYCOLOGIA, V33, P97, DOI 10.2216/i0031-8884-33-2-97.1; Jorgensen E., 1923, REP DAN OCEANOGR EXP, V2, P1; KELLER MD, 1987, J PHYCOL, V11, P80; KIMMEL BL, 1988, ARCH HYDROBIOL, V113, P577; Kofoid C.A., 1907, University of California Publications Zoology, V3, P299; KOFOID CHARLES ATWOOD, 1928, MEM MUS COMP ZOOL HARVARD COLLEGE, V51, P1; Koike Kazuhiko, 2000, Phycological Research, V48, P121, DOI 10.1111/j.1440-1835.2000.tb00206.x; LASSUS P, 1991, CRYPTOGAMIE ALGOL, V12, P1; Lindahl O., 1986, International council for the exploration of the sea; 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; MACKENZIE L, 1989, 4 INT C TOX MAR PHYT, P99; MAESTRINI SY, 1995, AQUAT MICROB ECOL, V9, P177, DOI 10.3354/ame009177; Marín I, 2001, BIOTECHNIQUES, V30, P88, DOI 10.2144/01301st05; MCDUFF RE, 1982, LIMNOL OCEANOGR, V27, P783, DOI 10.4319/lo.1982.27.4.0783; MCLACHLAN JL, 1993, DEV MAR BIO, V3, P143; MOITA MT, 1993, DEV MAR BIO, V3, P153; Palma A.S., 1998, Harmful Algae, P124; PARTENSKY F, 1989, J PHYCOL, V25, P741, DOI 10.1111/j.0022-3646.1989.00741.x; PAULSEN O, 1949, D KONGEL DANSKE VI B, V6, P1; Peperzak L. 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J. F., 1954, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V5, P171; Zingone A, 1998, EUR J PHYCOL, V33, P259	55	61	66	1	15	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	APR	2001	37	2					318	333		10.1046/j.1529-8817.2001.037002318.x	http://dx.doi.org/10.1046/j.1529-8817.2001.037002318.x			16	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	427DH					2025-03-11	WOS:000168389200015
J	Torricelli, S				Torricelli, S			Dinoflagellate cyst stratigraphy of the Lower Cretaceous Monte Soro Flysch in Sicily (S Italy)	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						biostratigraphy; dinoflagellate cysts; pollen; acritarchs; turbidites; maghrebian chain; Lower Cretaceous; Sicily; Italy	APTICORE SOUTHERN ALPS	Rich and well preserved palynological assemblages recovered from two outcrop sections in the Monte Sore Flysch (Nebrodi Mountains, NE Sicily, Italy) are documented and discussed. They provide new and valuable information for age determination and correlation within this turbidite unit in the type-area. The dinoflagellate cyst zonation scheme established for the Lower Cretaceous in the western Mediterranean region, is successfully applied to the lower portion of the Monte Sore Flysch sampled at Vallone Rosmarino, ranging in age from the latest Valanginian to the Late Hauterivian. The Pizzo Gilormo section exhibits a fining and thinning-upward sequence and is dated as Early Aptian through latest Aptian. Turbidites of the Monte dell'Abate succession are proved to be a lateral equivalent of the Monte Sore Flysch at the Pizzo Gilormo section. Overlying these turbidites, the shales cropping out at Portella Buffali mark in the Early Albian the beginning of the deposition of the Argille Scagliose Superiori. Although the Barremian was nor detected in the material of the present study it is documented both in the literature and in the succession drilled by Agip close to Randazzo. Finally, an age extending from the latest Valanginian to the latest Aptian is established by means of paly nomorphs for the Monte Sore Flysch. Owing to their abundance, diversity, excellent preservation and consistent record throughout the composite succession of the Monte Sore Flysch, dinoflagellate cysts represent an optimal tool for age and palaeoenvironmental assessment within this unit. The reappraisal of the dinoflagellate species Hystrichosphaeridium? atlasiense Below is proposed: a single-plate precingular archeopyle is documented for the cyst, which precludes its assignment to the genus Hystrichosphaeridium Deflandre and suggests the attribution to the genus Kleithriasphaeridium Davey, herein emended. The first appearance of Kleithriasphaeridium atlasiense (Below, 1982) Torricelli comb. nov. is proposed as an important biostratigraphic event close to the Aptian/Albian boundary in the Tethyan Realm.	ENI SPA, Agip Div, LABO, STIG, I-20100 Milan, Italy	Eni SpA	ENI SPA, Agip Div, LABO, STIG, POB 12069, I-20100 Milan, Italy.	stefano.torricelli@agip.it						[Anonymous], 1960, Riv Minerar Siciliana; [Anonymous], 1996, Palynology: principles and applications; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BOUILLIN JP, 1995, CR ACAD SCI II, V320, P601; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; CARMISCIANO R, 1983, B ACCADEMIA GIOENIA, V16, P113; CATALANO R, 1982, GUIDA GEOLOGIA SICIL, P9; COCCIONI R, 1994, CRETACEOUS RES, V15, P599, DOI 10.1006/cres.1994.1035; DAVEY R J, 1974, Palaeontology (Oxford), V17, P623; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; DAVEY RJ, 1974, BIRBAL SAHNI I PALAE, V3, P41; Doyle J.A., 1982, B CENT RECH EXPL, V6, P39; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Erba E, 1999, J FORAMIN RES, V29, P371; Erba Elisabetta, 1996, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V66, P31; FENSOME RA, 1993, MICROPALAEONTOLOGY P, V7; Habib D., 1987, INITIAL REPORTS DEEP, P751; Heilmann-Clausen Claus, 1995, Geologisches Jahrbuch Reihe A, V141, P257; HOCHULI PA, 1981, REV PALAEOBOT PALYNO, V35, P337, DOI 10.1016/0034-6667(81)90116-0; Leereveld H, 1997, CRETACEOUS RES, V18, P421, DOI 10.1006/cres.1997.0071; Leereveld H, 1997, CRETACEOUS RES, V18, P385, DOI 10.1006/cres.1997.0070; LEEREVELD H, 1995, LPP FOUND CONTRIB SE, V2; Lentini F., 1995, Studi Geol. 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L., 1998, AM ASS STRATIGRAPHIC, V34	41	18	21	0	1	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	2001	107	1					79	105		10.13130/2039-4942/5425	http://dx.doi.org/10.13130/2039-4942/5425			27	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	437XW					2025-03-11	WOS:000169025500004
J	Marret, F; de Vernal, A; Pedersen, TF; McDonald, D				Marret, F; de Vernal, A; Pedersen, TF; McDonald, D			Middle Pleistocene to Holocene palynostratigraphy of Ocean Drilling Program Site 887 in the Gulf of Alaska, northeastern North Pacific	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article							DINOFLAGELLATE CYST DISTRIBUTION; LATITUDE MARINE ENVIRONMENTS; SUB-ARCTIC PACIFIC; OF-ALASKA; SEDIMENTS; SEA; PHYTOPLANKTON; GLACIATION; AMERICA; IRON	A palynological investigation was undertaken on the upper 29 m of sediment at Ocean Drilling Program (ODP) Site 887, spanning the last 430 000 years (i.e., isotopic stages 12 to 1). Pollen and dinocyst assemblages reveal a major ecostratigraphical boundary at the Middle-Late Pleistocene transition. The Middle Pleistocene pollen data document the occurrence of a spruce forest vegetation in the source area, likely located on the adjacent Alaskan coast, whereas the Late Pleistocene is marked by higher inputs of pine, shrub, and herb taxa, suggesting predominant inputs from a more open landscape. The Middle Pleistocene is characterized by a low diversity in dinocyst assemblages, which are dominated by Operculodinium centrocarpum, whereas the Late Pleistocene is marked by the significant occurrence of Pentapharsodinium dalei, Pyxidinopsis reticulata, and by high percentages of Brigantedinium spp. Such assemblages suggest open oceanic and cool temperate conditions during the Middle Pleistocene, changing toward generally colder and less saline conditions during the Late Pleistocene. In addition, large fluctuations in the dinocyst assemblages during the Late Pleistocene are recorded in phase with the main shifts in the isotopic stratigraphy. A new dinocyst taxon, Spiniferites alaskensis sp. nov., exclusively recorded in sediments of the isotopic substage 5e, is described herein.	Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; Univ British Columbia, Vancouver, BC V6T 1Z4, Canada; Lorax Environm Serv Ltd, Vancouver, BC, Canada	University of Quebec; University of Quebec Montreal; University of British Columbia	Marret, F (通讯作者)，Univ Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Anglesey, Wales.	f.marret@bangor.ac.uk	; de Vernal, Anne/D-5602-2013	Marret-Davies, Fabienne/0000-0003-4244-0437; de Vernal, Anne/0000-0001-5656-724X				Ager T.A., 1985, POLLEN RECORDS LATE, P353; Ager ThomasA., 1983, HOLOCENE, V2, P128; ANDERSON PM, 1988, SCIENCE, V241, P1043, DOI 10.1126/science.241.4869.1043; ANDERSON PM, 1989, J BIOGEOGR, V16, P573, DOI 10.2307/2845212; [Anonymous], NATO ASI SERIES; [Anonymous], 1975, 835 US GEOL SURV; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Boyd P, 1999, DEEP-SEA RES PT II, V46, P2405, DOI 10.1016/S0967-0645(99)00069-7; Cullen JJ, 1995, LIMNOL OCEANOGR, V40, P1336, DOI 10.4319/lo.1995.40.7.1336; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DE VERNAL A, 1992, GEOLOGY, V20, P527, DOI 10.1130/0091-7613(1992)020<0527:QAOCDI>2.3.CO;2; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 1997, PALEOCEANOGRAPHY, V12, P821, DOI 10.1029/97PA02167; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1996, 3 GEOTOP; GUOIT J, 1990, I NATL SCI U MONOGRA, V1; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEINRICH A. 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Ocean Drill. Prog. Sci. Results, V145, P577, DOI [10.2973/odp.proc.ir.145.1993, DOI 10.2973/ODP.PROC.IR.145.1993]; Rea D.K., 1993, P OCEAN DRILLING PRO, V145; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; Sabin AL, 1996, QUATERNARY RES, V46, P48, DOI 10.1006/qres.1996.0043; SHACKLETON NJ, 1969, PROC R SOC SER B-BIO, V174, P135, DOI 10.1098/rspb.1969.0085; SUNDA WG, 1995, MAR CHEM, V50, P189, DOI 10.1016/0304-4203(95)00035-P; Svensson A, 2000, J GEOPHYS RES-ATMOS, V105, P4637, DOI 10.1029/1999JD901093; Taylor F. J. R., 1987, BOT MONOGR, V21; Varela DE, 1999, DEEP-SEA RES PT II, V46, P2505, DOI 10.1016/S0967-0645(99)00074-0; WARREN BA, 1983, J MAR RES, V41, P327, DOI 10.1357/002224083788520207; Winograd IJ, 1997, QUATERNARY RES, V48, P141, DOI 10.1006/qres.1997.1918; Wong CS, 1999, DEEP-SEA RES PT II, V46, P2735, DOI 10.1016/S0967-0645(99)00082-X; Zahn R, 1991, PALEOCEANOGRAPHY, V6, P543, DOI 10.1029/91PA01327	51	38	39	0	19	CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS	OTTAWA	1200 MONTREAL ROAD, BUILDING M-55, OTTAWA, ON K1A 0R6, CANADA	0008-4077	1480-3313		CAN J EARTH SCI	Can. J. Earth Sci.	MAR	2001	38	3					373	386		10.1139/e00-092	http://dx.doi.org/10.1139/e00-092			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	412YB					2025-03-11	WOS:000167581100004
J	Bian, LZ; Zhang, SC; Zhang, BM; Mao, SZ; Yin, LM				Bian, LZ; Zhang, SC; Zhang, BM; Mao, SZ; Yin, LM			A kind of coccoid dinoflagellates-like fossils gives a new explanation of source of dinosterane in the Early-Middle Cambrian	CHINESE SCIENCE BULLETIN			English	Article						coccoid dinoflagellates-like fossils; dinoflagellate-specific biomarkers; Cambrian; Tarim Basin	ANCESTORS	The coccoid fossils covered with thick gelatinous envelop containing several gametes are discovered in gyps and salt deposits of Cambrian, H-4 well and chert bed of the base of Yuertus Formation (is an element of (1)(1)) of Xiaoerbulake Section. The fossils are described and compared with coccoid dinoflagellates. These fossils may be a coccoid life-cycle stage (vegetative cyst) of coccoid dinoflagellates. If this identification is correct, the coccoid dinoflagellates-like fossils could give a reasonable explanation of the dinoflagellate-specific biomarkers from Cambrian, H-4 well, Tarim Basin.	China Natl Petr Corp, Res Inst Petr Explorat & Dev, Beijing 100083, Peoples R China; China Univ Geosci, Beijing 100083, Peoples R China; Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, Nanjing 210008, Peoples R China	China National Petroleum Corporation; China University of Geosciences; Chinese Academy of Sciences	Bian, LZ (通讯作者)，Nanjing Univ, Dept Earth Sci, Nanjing 210093, Peoples R China.							Fensome R.A., 1993, CLASSIFICATION FOSSI; Moldowan JM, 1998, SCIENCE, V281, P1168, DOI 10.1126/science.281.5380.1168; Moldowan JM, 1996, GEOLOGY, V24, P159; TAPPAN H, 1980, PALEOBIOLOGY PLANT P, P225	4	8	12	0	8	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING 100717, PEOPLES R CHINA	1001-6538			CHINESE SCI BULL	Chin. Sci. Bull.	MAR	2001	46	5					420	+		10.1007/BF03183280	http://dx.doi.org/10.1007/BF03183280			5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	424RE					2025-03-11	WOS:000168244600019
J	Townsend, DW; Pettigrew, NR; Thomas, AC				Townsend, DW; Pettigrew, NR; Thomas, AC			Offshore blooms of the red tide dinoflagellate, <i>Alexandrium</i> sp., in the Gulf of Maine	CONTINENTAL SHELF RESEARCH			English	Article						Gulf of Maine; red tides; Alexandrium; nutrients; phytoplankton; hydrography	HALF-SATURATION CONSTANTS; GONYAULAX-TAMARENSIS; MARINE-PHYTOPLANKTON; COASTAL CURRENT; RESTING CYSTS; EXCAVATA; GROWTH; IRRADIANCE; DYNAMICS; NITROGEN	Paralytic shellfish poisoning (PSP) occurs nearly every year in the Gulf of Maine. In a study of dynamics of the causative organism, the toxic dinoflagellate Alexandrium sp., we conducted three surveys of the coastal and offshore waters of Gulf of Maine during the summer of 1998, sampling more than 200 stations during each cruise in June, July and August. Hydrographic data were collected and concentrations of phytoplankton chlorophyll, inorganic nutrients and densities of Alexandrium cells were measured in discrete water samples. The distributions of Alexandrium at the surface and in subsurface waters displayed maximum cell densities in the offshore waters of the Gulf on all three cruises. Highest cell densities in surface waters (ca. 5.5 x 10(3) cells l(-1)) were observed in two broad patches: one in the Bay of Fundy and another in shelf and offshore waters of the central and eastern Gulf of Maine in association with the Eastern Maine Coastal Current. Highest subsurface densities of cells appeared to be associated with the frontal edges beyond the cold surface waters associated with the Eastern Maine Coastal Current. As the summer progressed, the highest surface densities of Alexandrium receded toward the eastern portions of the Gulf and the Bay of Fundy. We suggest that the offshore distributions of relatively high densities of Alexandrium are naturally occurring and can be related to inorganic nutrient fluxes, and to the ambient light field as it varies seasonally and vertically. Locations of high cell densities were described and interpreted using a nondimensional light-nutrient parameter, computed as the ratio of the depth of the 10% surface irradiance to the depth of 4 muM NO3 concentration. Possible mechanisms responsible for periodic development of PSP outbreaks in nearshore shellfish beds are discussed. (C) 2001 Elsevier Science Ltd. All rights reserved.	Univ Maine, Sch Marine Sci, Orono, ME 04469 USA	University of Maine System; University of Maine Orono	Townsend, DW (通讯作者)，Univ Maine, Sch Marine Sci, 5741 Libby Hall, Orono, ME 04469 USA.							ADACHI M, 1993, NIPPON SUISAN GAKK, V59, P1171; 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; [Anonymous], J MARINE RES; BISAGNI JJ, 1995, CONT SHELF RES, V16, P1; Bond R M., 1975, Proceedings of the First International Conference on Toxic Dinoflagellate Blooms, P473; Bricelj V. Monica, 1998, Reviews in Fisheries Science, V6, P315, DOI 10.1080/10641269891314294; BROOKS DA, 1989, J MAR RES, V47, P303, DOI 10.1357/002224089785076299; Chang FH, 1997, NEW ZEAL J MAR FRESH, V31, P1, DOI 10.1080/00288330.1997.9516740; DENMAN KL, 1978, J MAR RES, V36, P693; EPPLEY RW, 1969, J PHYCOL, V5, P375, DOI 10.1111/j.1529-8817.1969.tb02628.x; EPPLEY RW, 1969, LIMNOL OCEANOGR, V14, P912, DOI 10.4319/lo.1969.14.6.0912; EPPLEY RW, 1968, J PHYCOL, V4, P333, DOI 10.1111/j.1529-8817.1968.tb04704.x; Ganong W.F., 1889, B NATURAL HIST SOC N, V8, P1; GREENBERG DA, 1983, J PHYS OCEANOGR, V13, P886, DOI 10.1175/1520-0485(1983)013<0886:MTMBCI>2.0.CO;2; Hurst J W., 1975, Proceedings of the First International Conference on Toxic Dinoflagellate Blooms, P525; HURST JW, 1981, CANADIAN J FISHERIES, V38, P151; LANGDON C, 1987, J PLANKTON RES, V9, P459, DOI 10.1093/plankt/9.3.459; LoCicero V.R., 1975, P 1 INT C TOX DINO P 1 INT C TOX DINO, P447; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; MacIsaac J., 1979, P107; MARTIN JL, 1988, CAN J FISH AQUAT SCI, V45, P1968, DOI 10.1139/f88-229; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Pettigrew NR, 1998, J GEOPHYS RES-OCEANS, V103, P30623, DOI 10.1029/98JC01625; RASMUSSEN J, 1989, J PLANKTON RES, V11, P747, DOI 10.1093/plankt/11.4.747; SASNER JJ, 1975, P 1 INT C TOX DIN BL, P571; Seliger H.H., 1979, P239; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; SVERDRUP HU, 1946, OCEANS THEIR PHYSICS; THAYER PE, 1983, CAN J FISH AQUAT SCI, V40, P1308, DOI 10.1139/f83-149; Townsend DW, 1998, J MARINE SYST, V16, P283, DOI 10.1016/S0924-7963(97)00024-9; 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; YENTSCH CM, 1986, TIDAL MIXING PLANKTO, P224	35	104	110	1	24	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0278-4343			CONT SHELF RES	Cont. Shelf Res.	MAR	2001	21	4					347	369		10.1016/S0278-4343(00)00093-5	http://dx.doi.org/10.1016/S0278-4343(00)00093-5			23	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	410AB					2025-03-11	WOS:000167416900002
J	Dupont, LM; Bonner, B; Schneider, R; Wefer, G				Dupont, LM; Bonner, B; Schneider, R; Wefer, G			Mid-Pleistocene environmental change in tropical Africa began as early as 1.05 Ma	GEOLOGY			English	Article						pollen; dinoflagellates; mid-Pleistocene climatic shift; tropical Africa; vegetation	EAST EQUATORIAL ATLANTIC; DINOFLAGELLATE CYSTS; ATMOSPHERIC CO2; CLIMATE CHANGES; VEGETATION; SEDIMENTS; HISTORY; ONSET	Palynological records from the Congo fan reveal environmental change in equatorial Africa occurring 1.05 Ma ago, 100 k.y. before the mid-Pleistocene climatic shift at 0.9 Ma. Prior to 1.05 Ma, a glacial-interglacial rhythm is not obvious in the African vegetation variation. Afterwards, Podocarpus spread in the mountains of central Africa mainly during glacials and Congo River discharge decreased. The sequence of vegetation variation associated with the mid-Pleistocene glacials and interglacials differed from that observed during the late Pleistocene. Between 0.9 and 0.6 Ma, interglacials were characterized by warm dry conditions and glacials were characterized by cool humid conditions, while during the past 0.2 Ma glacials were cold and dry and interglacials warm and humid. Our data indicate that before the Northern Hemisphere ice caps dramatically increased in size (0.9-0.6 Ma), low-latitude climate forcing and response in the tropics played an important role in the initiation of 100 k.y. ice-age cycles. During the mid to late Pleistocene, however, the climate conditions in the tropics were increasingly influenced by the glacial-interglacial variations of continental ice sheets.	Geosci Bremen, D-28334 Bremen, Germany		Dupont, LM (通讯作者)，Geosci Bremen, POB 330440, D-28334 Bremen, Germany.		Wefer, Gerold/S-2291-2016	Wefer, Gerold/0000-0002-6803-2020; Schneider, Ralph/0000-0003-1453-9181; Dupont, Lydie/0000-0001-9531-6793				Berger W, 1998, PROC OCEAN DRILL PRO, V175, P561; Berger W.H., 1994, POLAR OCEANS THEIR R, V85, P295, DOI DOI 10.1029/GM085P0295; BERGER WH, 1992, NATURWISSENSCHAFTEN, V79, P541, DOI 10.1007/BF01131410; Cowling SA, 1999, QUATERNARY RES, V52, P237, DOI 10.1006/qres.1999.2065; CROWLEY TJ, 1995, GLOBAL BIOGEOCHEM CY, V9, P377, DOI 10.1029/95GB01107; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DEMENOCAL PB, 1995, SCIENCE, V270, P53, DOI 10.1126/science.270.5233.53; Dupont L, 1999, PALAEOECO A, V26, P61; Dupont LM, 2000, PALAEOGEOGR PALAEOCL, V155, P95, DOI 10.1016/S0031-0182(99)00095-4; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; Hooghiemstra H, 1995, BIODIVERSITY AND CONSERVATION OF NEOTROPICAL MONTANE FORESTS, P35; HOOGHIEMSTRA H, 1993, QUATERNARY SCI REV, V12, P141, DOI 10.1016/0277-3791(93)90013-C; Jahns S, 1996, VEG HIST ARCHAEOBOT, V5, P207, DOI 10.1007/BF00217498; Jolly D, 1997, SCIENCE, V276, P786, DOI 10.1126/science.276.5313.786; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Mudelsee M, 1997, GEOL RUNDSCH, V86, P499, DOI 10.1007/s005310050157; POLLARD D, 1983, J GEOPHYS RES-OCEANS, V88, P7705, DOI 10.1029/JC088iC12p07705; Raymo ME, 1997, PALEOCEANOGRAPHY, V12, P546, DOI 10.1029/97PA01019; Raymo ME, 1997, PALEOCEANOGRAPHY, V12, P577, DOI 10.1029/97PA01169; Rutherford S, 2000, NATURE, V408, P72, DOI 10.1038/35040533; Schneider RR, 1997, PALEOCEANOGRAPHY, V12, P463, DOI 10.1029/96PA03640; SHACKLETON NJ, 1990, T ROY SOC EDIN-EARTH, V81, P251, DOI 10.1017/S0263593300020782; TEXTIER D, 1997, CLIM DYNAM, V13, P865; Versteegh GJM, 1997, MAR MICROPALEONTOL, V30, P319, DOI 10.1016/S0377-8398(96)00052-7; Wefer G., 1998, Proceedings of the Ocean Drilling Program, Initial Reports, V175; Wefer G., 1998, Proceedings of the Ocean Drilling Program, Initial Reports, V175, P487; WHITE F, 1983, NATURAL RECOURSES RE, V20; ZONNEVELD K, 1996, PALAEOCLIMATIC PALAE	28	103	114	0	16	GEOLOGICAL SOC AMERICA, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613			GEOLOGY	Geology	MAR	2001	29	3					195	198		10.1130/0091-7613(2001)029<0195:MPECIT>2.0.CO;2	http://dx.doi.org/10.1130/0091-7613(2001)029<0195:MPECIT>2.0.CO;2			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	405WU					2025-03-11	WOS:000167184200001
J	Mehrotra, NC; Swamy, SN; Rawat, RS				Mehrotra, NC; Swamy, SN; Rawat, RS			Reworked Carboniferous palynofossils from Panna Formation, Bombay offshore basin: Clue to a hidden target for hydrocarbon exploration	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						Carboniferous; palynofossils; Panna Formation; Bombay offshore basin; hydrocarbon		A reworked Carboniferous palynofossil assemblage from the subsurface sections of the Early Eocene basal clastics of Panna Formation, Bombay offshore basin has been discovered. This assemblage is recorded at various stratigraphic levels of the studied well sections along with the indigenous Early Eocene dinoflagellate cysts and spore-pollen taxa. Initial studies have suggested more than one possibility of explaining the provenance of reworked sediments containing the Carboniferous palynofossils. One possibility is that these might have been derived from the erosion of Early Palaeozoic sediments present in the Deccan volcanic province. Alternatively, these sediments could result from long distance transport of reworked material from Saudi Arabia-Africa region in the west which were deposited in the Bombay offshore region during Early Eocene. Available evidences, for and against these two possibilities are discussed. Our studies show that the Carboniferous reworked assemblage is confined to the Heera-Bassein block. The reworking in the Panna Formation might have taken place by palaeorivulets cutting through the thin Deccan Trap flows, exposed in the faulted blocks. A model explaining the mechanism of reworking has been presented. Organic matter studies indicate the presence of mature sediments below the Deccan Trap, which suggest a possible hidden basin to be a new exploration target for hydrocarbon.	Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Dehra Dun 248195, Uttar Pradesh, India	Oil & Natural Gas Corporation	Mehrotra, NC (通讯作者)，Oil & Nat Gas Corp Ltd, KDM Inst Petr Explorat, Dehra Dun 248195, Uttar Pradesh, India.		Swamy, Narasimha/AAF-6687-2019	S, Narasimha Swamy/0000-0002-5798-961X				Khanna A. K., 1983, J PALAEONTOL SOC IND, V28, P95; KHANNA AK, 1980, P 11 HIM GEOL SEM BI, P15; MATHUR RB, 1993, INDIAN PETROLEUM PUB, V2, P365; MEHROTRA NC, 1998, P 16 ICMS NIO GOA JA; Rawat R.S., 1997, ONGC Bulletin, V33, P123; RAWAT RS, 1996, 15 ICMS DEHR DUN, P657; SRINIVASAN S, 1995, P PETR 1995 NEW DELH, V1, P1; Staplin FL., 1969, B CANADIAN PETROL GE, V17, P47; TEWARI RS, 1987, PALEOBOTANIST, V36, P339; TEWARI RS, 1984, PALEOBOTANIST, V32, P341; VENKATACHALA BS, 1972, GEOPHYTOLOGY, V3, P26; VENKATACHALA BS, 1972, GEOPHYTOLOGY, V2, P107; VISWANATHIAH MN, 1977, INDIAN MINERALOGIST, V18, P122; ZUTSHI PL, 1993, KDMIPE ONGC PUBLICAT	14	4	4	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	MAR	2001	57	3					239	248						10	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	408BJ					2025-03-11	WOS:000167306400004
J	Bolch, CJS				Bolch, CJS			PCR protocols for genetic identification of dinoflagellates directly from single cysts and plankton cells	PHYCOLOGIA			English	Article							GYMNODINIUM-CATENATUM; RIBOSOMAL DNA; ALEXANDRIUM DINOPHYCEAE; MARINE-SEDIMENTS; POLYMORPHIC DNA; RESTING CYSTS; AMPLIFICATION; SEQUENCES; REGIONS; NOV	A simple preparation method and PCR protocol are described which allow successful PCR amplification of partial ribosomal RNA gene sequences from as little as one dinoflagellate cyst or vegetative cell. Amplification from single or small numbers of cysts can be applied to a range of morphologically identifiable cyst species and produces rDNA sequence data identical to those obtained from DNA extractions from cultured vegetative cells. Applications of the approach have the potential to aid phylogenetic studies of dinoflagellates and other microalgae by (1) improving taxonomic sampling of unculturable and heterotrophic species, (2) providing data to Link cysts of unknown affinity with their potential planktonic cell counterparts; and (3) confirming the identification of cysts that cannot be germinated or are nonviable. Examples are presented where this method was used to confirm the identity and distribution of nonviable microreticulate cysts in coastal marine sediment samples, such as those of the recently described species Gymnodinium microreticulatum.	Dunstaffnage Marine Res Lab, Oban PA34 4AD, Argyll, Scotland; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia	University of Tasmania	Bolch, CJS (通讯作者)，Dunstaffnage Marine Res Lab, POB 3, Oban PA34 4AD, Argyll, Scotland.	cjsb@dml.ac.uk	Bolch, Christopher/J-7619-2014					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; AGUILERA A, 2000, 9 INT C HARMF ALG BL, P74; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; BOLCH CJ, 1998, HARMFUL MICROALGAE, P283; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BOLCH CJS, 1998, 6 INT C MOD FOSS DIN, P18; DALE B, 1993, DEV MAR BIO, V3, P47; Grzebyk D, 1998, J PHYCOL, V34, P1055, DOI 10.1046/j.1529-8817.1998.341055.x; Hansen G, 2000, J PHYCOL, V36, P394, DOI 10.1046/j.1529-8817.2000.99172.x; Hansen PJ, 1999, J EUKARYOT MICROBIOL, V46, P382, DOI 10.1111/j.1550-7408.1999.tb04617.x; Head M.J., 1996, Palynology: Principles and Applications, P1197; Howitt CA, 1996, BIOTECHNIQUES, V21, P32; JORGENSEN RA, 1988, ANN MO BOT GARD, V75, P1238, DOI 10.2307/2399282; MAZURIER SI, 1992, RES MICROBIOL, V143, P499, DOI 10.1016/0923-2508(92)90096-7; Miller PE, 1998, J PHYCOL, V34, P371, DOI 10.1046/j.1529-8817.1998.340371.x; 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; SAUNDERS GW, 1997, PLANT SYST EVOL S, V11, P237; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Scholin CA, 1995, PHYCOLOGIA, V34, P472, DOI 10.2216/i0031-8884-34-6-472.1; SCHWINGHAMER P, 1991, LIMNOL OCEANOGR, V36, P588, DOI 10.4319/lo.1991.36.3.0588; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; Tyrrell JV, 1997, NEW ZEAL J MAR FRESH, V31, P551, DOI 10.1080/00288330.1997.9516788; ZHANG L, 1992, P NATL ACAD SCI USA, V89, P5847, DOI 10.1073/pnas.89.13.5847	25	53	64	3	25	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAR	2001	40	2					162	167		10.2216/i0031-8884-40-2-162.1	http://dx.doi.org/10.2216/i0031-8884-40-2-162.1			6	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	453GU					2025-03-11	WOS:000169908800007
J	Akhmet'ev, MA; Aleksandrova, GN; Amon, EO; Beniamovskii, VN; Bugrova, EM; Vasil'eva, ON; Glezer, ZI; Zhelezko, VI; Zaporozhets, NI; Kozlova, SE; Nikolaeva, IA; Oreshkina, TV; Panova, LA; Radionova, EP; Strel'nikova, NI; Yakovleva, AI				Akhmet'ev, MA; Aleksandrova, GN; Amon, EO; Beniamovskii, VN; Bugrova, EM; Vasil'eva, ON; Glezer, ZI; Zhelezko, VI; Zaporozhets, NI; Kozlova, SE; Nikolaeva, IA; Oreshkina, TV; Panova, LA; Radionova, EP; Strel'nikova, NI; Yakovleva, AI			Biostratigraphy of the marine Paleogene in the West Siberian Plate	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Paleocene; Eocene; Oligocene; West Siberian plate; foraminifers; dinocysts; radiolarians; diatoms; Elasmobranchii; mollusks; silicoflagellates; ostracodes; spore-pollen assemblages; Talitsa; Lyulin-Vor and Tavda horizons; Serov and Irbit formations	NORTH-SEA; STRATIGRAPHY; BOUNDARY	The regional stratigraphic scheme suggested for the marine Paleogene deposits in the West Siberian plate is based on investigation results of macro- and microfossils (foraminifers, dinoflagellates, radiolarians, diatomaceous algae, silicoflagellates, Elasmobranchii, ostracodes, pollen, and spores). In the West Siberian plate, like in many structural-facies zones of the East European platform, there was a hiatus in sedimentation at the Cretaceous-Paleogene boundary. The Talitsa Horizon corresponds here to the Danian and Selandian presumably coupled with the initial Thanetian. The lower Lyulin-Vor Subhorizon is dated bask to the late Paleocene; the middle Lyulin-Vor Subhorizon is correlated with the Ypresian, and the upper one is attributed to the interval spanning the second half of the Ypresian and Lutetian, The Tavda Horizon of the Bartonian-Priabonian age presumably comprises as well the terminal Lutetian, The Kurgan Beds is. str,) representing marine facies of the Atlym Horizon correspond in the type area (near the town of Kurkan) to the lower Oligocene. Boundaries of these lithostratigraphic units are diachronous, since the Paleoarctis in the north and the Tethys in the south were connected with the epicontinental West Siberian sea basin producing an irregular impact on sedimentation in the latter.	Russian Acad Sci, Inst Geol, Moscow 109017, Russia; Russian Acad Sci, Inst Geol & Geochem, Ural Div, Yekaterinburg 629151, Russia; All Russia Res Inst Geol, St Petersburg 199026, Russia; All Russia Res Inst Petr Prospecting, St Petersburg 191104, Russia; St Petersburg State Univ, St Petersburg 199034, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences; A.P. Karpinsky Russian Geological Research Institute (VSEGEI); Saint Petersburg State University	Akhmet'ev, MA (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevskii Per 7, Moscow 109017, Russia.		Galina, Aleksandrova/AAW-8215-2020; Oreshkina, Tatyana/ABC-6121-2021; Amon, Edward/AAP-2133-2021; Васильева, Ольга/B-6221-2018	Oreshkina, Tatiana V./0000-0002-7477-7272				AKHMETEV MA, IN PRESS STRATIGRAFI; AKHMETIEV M. A., 1992, B MOSKOVSKOGO OBSHCH, V67, P96; Amon E.O., 1990, PROBLEMY STRATIGRAFI, P25; ANDREEVAGRIGORO.AS, 1991, THESIS KIEV STATE U; [Anonymous], RADIOLYARII PALEOGEN; Aubry M.-P., 1996, ISR J EARTH SCI, V44, P239; Aubry MP, 1999, EARTH-SCI REV, V46, P99, DOI 10.1016/S0012-8252(99)00008-2; BAKIEVA LB, 1994, EOCENE MICROPHYTOFOS, P106; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Cavelier C., 1983, GEOL FRANCE, V3, P261; Chirva SA, 1973, MORSKOI KONTINENTALN, P69; Costa L. I., 1988, GEOL JB; DARGEVICH VA, 1984, SREDA ZHIZN RUBEZHAK, P78; FARLEY B, 1998, CHRONOSTRATIGRAPHY S; Gleser Z.I., 1979, Sov. 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Geol. Correl.	MAR-APR	2001	9	2					132	158						27	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	423GL					2025-03-11	WOS:000168167000003
J	Zonneveld, KAF; Versteegh, GJM; de Lange, GJ				Zonneveld, KAF; Versteegh, GJM; de Lange, GJ			Palaeoproductivity and post-depositional aerobic organic matter decay reflected by dinoflagellate cyst assemblages of the Eastern Mediterranean S1 sapropel	MARINE GEOLOGY			English	Article						dinoflagellate cyst; preservation; organic matter; calcite; oxygen	ATLANTIC-OCEAN; EQUATORIAL ATLANTIC; SURFACE SEDIMENTS; DEEP-SEA; POSTDEPOSITIONAL OXIDATION; QUATERNARY EASTERN; PLIOCENE SAPROPEL; MARINE-SEDIMENTS; NORTH-ATLANTIC; INDIAN-OCEAN	In the reconstruction of bioproductivity in surface waters the extent to which a proxy has been diagenetically altered is often a matter of debate. Here we investigate how organic- and calcareous-walled dinoflagellate cysts can be used for separately estimating bioproductivity and oxygen related diagenesis. This is achieved by studying the cyst content of the most recent Eastern Mediterranean sapropel S1, that is thought to have been deposited Lender conditions of increased primary production in surface waters and possible anoxia in the bottom waters. Based on chemical evidence, it has been shown that the visible sapropelic layer represents only the residual lower part of what was initially a much thicker sapropel. as a result of post depositional decay of organic matter related to oxygen penetration into the sediments. The effect of aerobic organic matter decay on the cyst associations is studied through the comparison of the unaffected, lower part of the initial sapropel and the 'oxidised' upper part. Comparing the unaffected sapropelic sediments with pre- and post-sapropelic material gives insight into the relationship between fossil cysts assemblages and palaeoproductivity. Impagidinium aculeatum, Impagidinium patulum, Operculodinium israelianum, Polysphaeridium zoharyi and probably Impagidinium spp., Impagidinium paradoxum and Nematosphaeropsis labyrinthus are very resistant against aerobic decay and their accumulation rates appear to be primarily related to productivity in surface waters. Protoperidinium and Echinidinium species, on the other hand, are shown to be very sensitive and can be used to recognise oxygen-related decay. The calcaerous-walled dinoflagellate cysts seem to be unaffected by oxic organic matter decay in Mediterranean sediments. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands; Univ Utrecht, Inst Earth Sci, Dept Geochem, NL-3508 TA Utrecht, Netherlands	University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University	Zonneveld, KAF (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.		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Geol.	FEB 15	2001	172	3-4					181	195		10.1016/S0025-3227(00)00134-1	http://dx.doi.org/10.1016/S0025-3227(00)00134-1			15	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	409EL					2025-03-11	WOS:000167371500002
J	Pross, J				Pross, J			Paleo-oxygenation in Tertiary epeiric seas: evidence from dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; paleoenvironment; oxygen depletion; Oligocene; Mainz embayment; Germany	SINKING	The dinoflagellate cyst record from an epeiric setting in the Oligocene of Southwest Germany exhibits major changes associated with variations in paleo-oxygenation inferred from benthic foraminifera. Dinoflagellate cyst diversity and equitability strongly decline in the case of extreme oxygen depletion. The relative abundance of the dinoflagellate cyst Thalassiphora pelagica inversely correlates with the availability of benthic oxygen. The T. pelagica spectrum consists of different morphotypes which are considered to represent different stages within the cystal part of the T. pelagica life cycle following the concept of Benedek and Gocht. The distribution of these morphotypes is also linked to oxygen availability. Horizons with highest T. pelagica abundances are characterized by the occurrence of T. pelagica specimens representing an early stage in cyst formation. A model is proposed that uses T. pelagica as a proxy to assess oxygenation both at the sediment surface and in the water column. The occurrence of T. pelagica specimens representing an early stage in cyst formation is interpreted to reflect the extension of oxygen-depletion upwards into the water column. Because T, pelagica is an easily recognized, globally distributed element of Paleogene and Early Neogene dinoflagellate cyst assemblages, the application of this model may be of importance in the reconstruction of paleo-oxygenation in epeiric settings from these times. Its sensitivity to changes in benthic oxygenation can be as high as (if not higher than) that of the approach based on foraminifera. Moreover, it is applicable to decalcified sediments. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Tubingen, Inst & Museum Geol & Palaontol, D-72076 Tubingen, Germany	Eberhard Karls University of Tubingen	Pross, J (通讯作者)，Univ Tubingen, Inst & Museum Geol & Palaontol, Sigwartstr 10, D-72076 Tubingen, Germany.							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B., 1990, SPECIAL PAPERS PALAE, V43; Williams GL., 1977, American Association of Stratigraphic Palynologists Contribution Series A, V5, P14; Zhao Yun-Yun, 1992, Acta Micropalaeontologica Sinica, V9, P291; Ziegler P.A., 1990, GEOLOGICAL ATLAS W C; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	46	74	79	0	3	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	FEB 15	2001	166	3-4					369	381		10.1016/S0031-0182(00)00219-4	http://dx.doi.org/10.1016/S0031-0182(00)00219-4			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	402YB					2025-03-11	WOS:000167014800007
J	Sejrup, HP; Haflidason, H; Flatebo, T; Kristensen, DK; Grosfjeld, K; Larsen, E				Sejrup, HP; Haflidason, H; Flatebo, T; Kristensen, DK; Grosfjeld, K; Larsen, E			Late-glacial to Holocene environmental changes and climate variability: evidence from Voldafjorden, western Norway	JOURNAL OF QUATERNARY SCIENCE			English	Article						late-glacial; holocene; fjord; Norway; climate variability	MODERN BENTHIC FORAMINIFERA; NORDIC SEAS; STOREGGA TSUNAMI; NORTH-SEA; SEDIMENTS; FJORD; STRATIGRAPHY; SVALBARD; REGION; OCEAN	Sedimentological, micropalaeontological (benthic foraminifers and dinoflagellate cysts), stable isotope data and AMS C-14 datings on cores and surface samples, in addition to acoustic data, have been obtained from Voldafjorden, western Norway. Based on these data the late glacial and Holocene sedimentological processes and variability in circulation and fiord environments are outlined. Glacial marine sedimentation prevailed in the Voldafjorden between 11.0 kyr and 9.2 kyr BP (radiocarbon years). In the later part of the Allerod period, and for the rest of the Holocene, there was deposition of fine-grained normal marine sediments in the fjord basin. Turbidite layers, recorded in core material and on acoustic profiles, dated to ca. 2.1, 6.9-7.6, ca. 9.6 and ca. 11.0 kyr BP, interrupted the marine sedimentation. The event dated to between 6.9 and 7.6 kyr BP probably corresponds to a tsunami resulting from large-scale sliding on the continental margin off Norway (the Storegga Tsunami). During the later part of the Allerod period, Voldafjorden had a strongly stratified water column with cold bottom water and warm surface water, reaching interglacial temperatures during the summer seasons. During the Younger Dryas cold event there was a return to arctic sea-surface summer temperatures, possibly with year-round sea-ice cover, the entire benthic fauna being composed of arctic species. The first strong Holocene warming, observed simultaneously in bottom and sea-surface temperature proxies, occurred at ca. 10.1 kyr BP. Bottom water proxies indicate two cold periods, possibly with 2 degreesC lowering of temperatures, at ca. 10.0 (PBO 1) and at 9.8 kyr BP (PBO 2). These events may both result from catastrophic outbursts of Baltic glacial lake water. The remainder of the Holocene experienced variability in basin water temperature, indicated by oxygen isotope measurements with an amplitude of ca. 2 degreesC, with cooler periods at ca. 8.4-9.0, 5.6, 5.2, 4.6, 4.2, 3.5, 2.2, 1.2 and 0.4-0.8 kyr BP. Changes in the fjord hydrology through the past 11.3 kyr show a close correspondence, both in amplitude and timing of events, recorded in cores from the Norwegian Sea region and the North Atlantic. These data suggest a close relationship between fjord environments and variability in large-scale oceanic circulation. Copyright (C) 2001 John Wiley & Sons, Ltd.	Univ Bergen, Dept Geol, N-5007 Bergen, Norway; Geol Survey Norway, N-7002 Trondheim, Norway	University of Bergen; Geological Survey of Norway	Univ Bergen, Dept Geol, Allegt 41, N-5007 Bergen, Norway.	sejrup@geol.uib.no						AARSETH I, 1974, Boreas (Oslo), V3, P3; AARSETH I, 1989, MAR GEOL, V88, P1, DOI 10.1016/0025-3227(89)90002-9; Aarseth I, 1997, MAR GEOL, V143, P39, DOI 10.1016/S0025-3227(97)00089-3; AARSETH I, 1975, SARSIA, P43; Andrews J.T., 1985, Quaternary Environments, Eastern Canadian Arctic, Baffin Bay and Western Greenland, P69; Austin W.E.N., 1994, Cushman Foundation for Foraminiferal Research Special Publication, V32, P103; AUSTIN WEN, 1996, SPECIAL PUBLICATION, V3, P187; BARD E, 1994, EARTH PLANET SC LETT, V126, P275, DOI 10.1016/0012-821X(94)90112-0; Birks HH, 1996, QUATERNARY RES, V45, P119, DOI 10.1006/qres.1996.0014; Bjorck S, 1997, J QUATERNARY SCI, V12, P455; Boden P, 1997, PALEOCEANOGRAPHY, V12, P39, DOI 10.1029/96PA02879; Bond G, 1997, SCIENCE, V278, P1257, DOI 10.1126/science.278.5341.1257; Bondevik S, 1997, BOREAS, V26, P29, DOI 10.1111/j.1502-3885.1997.tb00649.x; Bondevik S, 1997, SEDIMENTOLOGY, V44, P1115, DOI 10.1046/j.1365-3091.1997.d01-63.x; Conradsen Keld, 1994, Cushman Foundation for Foraminiferal Research Special Publication, V32, P53; Craig H, 1965, CITY, P9; Dahl SO, 1996, HOLOCENE, V6, P381, DOI 10.1177/095968369600600401; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DOMACK EW, 1994, MAR GEOL, V121, P161, DOI 10.1016/0025-3227(94)90028-0; Elverhoi A., 1983, POLAR RES-SWEDEN, V1, P1, DOI [DOI 10.1111/J.1751-8369.1983.TB00697.X, DOI 10.3402/POLAR.V1I2.6978]; FEYLING-HANSSEN R W, 1971, Bulletin of the Geological Society of Denmark, V21, P72; FEYLINGHANSSEN RW, 1964, NORGES GEOLOGISKE UN, V225; FLATEBO T, 1998, THESIS U BERGEN; Gade H., 1980, Fjord Oceanography, P453; Grosfjeld K, 1999, BOREAS, V28, P403, DOI 10.1080/030094899422127; GROSSMAN EL, 1987, J FORAMIN RES, V17, P48, DOI 10.2113/gsjfr.17.1.48; HAFLIDASON H, 1995, GEOLOGY, V23, P1059, DOI 10.1130/0091-7613(1995)023<1059:CROTLG>2.3.CO;2; HAFLIDASON H, 1997, GEONYTT, V1, P44; Hafsten Ulf, 1983, Norsk Geografisk Tidsskrift Norwegian Journal of Geography, V37, P63, DOI [10.1080/00291958308552089, DOI 10.1080/00291958308552089, DOI 10.5194/bg-10-3145-2013]; Hald M, 1997, J FORAMIN RES, V27, P101, DOI 10.2113/gsjfr.27.2.101; Hald M, 1998, GEOLOGY, V26, P615, DOI 10.1130/0091-7613(1998)026<0615:EPCITN>2.3.CO;2; HALD M, 1992, J FORAMIN RES, V22, P347, DOI 10.2113/gsjfr.22.4.347; Hansen A, 1995, POLAR RES, V14, P215, DOI 10.1111/j.1751-8369.1995.tb00690.x; Helle H.B., 1978, Hydrodynamics of Estuaries and Fjords, V23, P441; Holtedahl H., 1975, Norges geologiske undersokelse, V323, P1; Hooke RL, 1996, GLOBAL PLANET CHANGE, V12, P237, DOI 10.1016/0921-8181(95)00022-4; Jansen E., 1989, Quaternary International, V1, P151, DOI 10.1016/1040-6182(89)90013-X; Johannessen T., 1994, NATO ASI SERIES 1, V17, P61, DOI DOI 10.1007/978-3-642-78737-9_4; KLITGAARDKRISTE.D, IN PRESS PALEOCEANOG; KNUDSEN K L, 1987, Bulletin of the Geological Society of Denmark, V36, P289; Knudsen KL, 1994, B GEOL SOC DENMARK, V41, P203; KNUDSEN KL, 1990, MAR GEOL, V101, P113; KOC N, 1994, GEOLOGY, V22, P523, DOI 10.1130/0091-7613(1994)022<0523:ROTHLN>2.3.CO;2; Kristensen DK, 1996, SARSIA, V81, P97, DOI 10.1080/00364827.1996.10413615; LABEYRIE LD, 1992, QUATERNARY SCI REV, V11, P401, DOI 10.1016/0277-3791(92)90022-Z; LARSEN E, 1984, ARCTIC ALPINE RES, V16, P137, DOI 10.2307/1551067; Larsen E, 1998, J QUATERNARY SCI, V13, P17, DOI 10.1002/(SICI)1099-1417(199801/02)13:1<17::AID-JQS337>3.3.CO;2-2; MATTHEWS JA, 1992, GEOLOGY, V20, P991, DOI 10.1130/0091-7613(1992)020<0991:ANAHCC>2.3.CO;2; MIKALSEN G, IN PRESS HOLOCENE; MURRAY J.W., 1971, ATLAS BRIT RECENT FO; Murray J W., Ecology and Palaeoecology of Benthic Foraminifera; NAGY I, 1965, NORSK POLARINSTITUTT, P109; NESJE A, 1993, QUATERNARY SCI REV, V12, P255, DOI 10.1016/0277-3791(93)90081-V; PAETZEL M, 1991, NORSK GEOL TIDSSKR, V71, P65; PAETZEL M, 1992, MAR GEOL, V105, P23, DOI 10.1016/0025-3227(92)90179-L; Rochon A, 1998, QUATERNARY RES, V49, P197, DOI 10.1006/qres.1997.1956; Saelen O. 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FEB	2001	16	2					181	198		10.1002/jqs.593	http://dx.doi.org/10.1002/jqs.593			18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	416CE					2025-03-11	WOS:000167761700008
J	Matsuoka, K				Matsuoka, K			Further evidence for a marine dinoflagellate cyst as an indicator of eutrophication in Yokohama Port, Tokyo Bay, Japan. Comments on a discussion by B. Dale	SCIENCE OF THE TOTAL ENVIRONMENT			English	Editorial Material									Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan	Nagasaki University	Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.	kazu-mtk@net.nagasaki-u.ac.jp						Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B, 2000, SCI TOTAL ENV; *ENV CONS BUR METR, 1993, REP SURV AQ ORG 1991; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; Furota T., 1994, THINKING MARINE ENV, P69; Ishimaru T., 1995, KAIYO KAGAKU, V27, P434; Matsuoka K., 1989, P461; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Sato H., 1995, 116 YOK ENV RES I, P63; YAMAGUCHI M, 1995, NIPPON SUISAN GAKK, V61, P700; YAMOCHI S, 1984, Journal of the Oceanographical Society of Japan, V40, P343, DOI 10.1007/BF02303338; *YOK ENV RES I, 1992, 102 YOK ENV RES I	14	43	46	1	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0048-9697	1879-1026		SCI TOTAL ENVIRON	Sci. Total Environ.	JAN 17	2001	264	3					221	233		10.1016/S0048-9697(00)00718-X	http://dx.doi.org/10.1016/S0048-9697(00)00718-X			13	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	394ZW	11213193				2025-03-11	WOS:000166555100003
J	Dale, B				Dale, B			Marine dinoflagellate cysts as indicators of eutrophication and industrial pollution: a discussion	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						dinoflagellate cyst; eutrophication; marine pollution; coastal environment; Tokyo Bay; Norwegian fjords	NORWEGIAN FJORD	The results from an investigation of dinoflagellate cysts as indicators of eutrophication in Tokyo Bay, Japan, by Matsuoka [Sci Total Environ 231 (1999) 17] are discussed with reference to other pertinent literature not discussed in the original article. Both the Japanese study and previous work from Norwegian fjords show that pollution (including cultural eutrophication) may produce changes in the phytoplankton reflected by a shift from more autotrophic - to more heterotrophic - dominance of cyst assemblages. However, this is a proportional change that seems likely to result from reduced autotrophic production rather than the increased heterotrophic production suggested by Matsuoka. This is not unequivocal evidence of eutrophication, since Tokyo Bay is impacted also by heavy industrial pollution, the possible effects of which cannot be distinguished. and the quantitative method used for estimating changes in cyst productivity is flawed. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Oslo, Dept Geol, N-0316 Oslo, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Dept Geol, PB 1047 Blindern, N-0316 Oslo, Norway.							CONLEY DJ, 1993, MAR ECOL PROG SER, V101, P179, DOI 10.3354/meps101179; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; 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; DALE B, IN PRESS ENV MICROPA; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; MATSUOKA K, 1989, RED TIDES BIOL ENV S, P467; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406	10	81	90	2	18	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0048-9697			SCI TOTAL ENVIRON	Sci. Total Environ.	JAN 17	2001	264	3					235	240		10.1016/S0048-9697(00)00719-1	http://dx.doi.org/10.1016/S0048-9697(00)00719-1			6	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	394ZW	11213194				2025-03-11	WOS:000166555100004
J	Guerstein, GR; Junciel, GL				Guerstein, GR; Junciel, GL			Cenozoic dinoflagellate cysts from the Colorado Basin, Argentina.	AMEGHINIANA			Spanish	Article						dinoflagellate cysts; biostratigraphy; paleoenvironments; cenozoic; Colorado Basin; Argentina	BIOSTRATIGRAPHY; MIOCENE; PALYNOMORPHS; PROVINCE; EOCENE; AREA	Cenozoic sediments from the well Cx-1 of offshore Colorado Basin were studied. The dinoflagellate cysts assemblages are diverse and well preserved providing stratigraphic control for the section. Selected dinoflagellate cyst last occurrences or abundance events suggest seven age intervals: Maastrichtian, Paleocene, Late Eocene to Early Oligocene, Late Oligocene to Early Miocene, Mid Miocene, Late Miocene and Late Miocene to Early Pliocene. These results are compared with previous studies, carried out by other authors exhibiting a consistent succession of events throughout the basin. Qualitative and quantitative dinoflagellate cyst data allow the recognition of apparent sea level changes. Sediments ranging from Maastrichtian to Selandian in age show a gradual rise in sea level. These assemblages bear both gonyaulacacean and peridiniacean dinoflagellate cysts suggesting open marine conditions with a marked fall in sea level at the top of this interval. Sediments interpreted as Late Eocene to Early Oligocene in age were deposited in a more open marine environment. At the Early Oligocene/Late Oligocene boundary a second low see level episode occurred. Throughout the Late Oligocene to Early Miocene and Mid to Late Miocene intervals high dinocyst abundances and the presence of oceanic species suggest a sea level highstand. Upwards the dominance of terrestrially derived palynomorphs as well as the scarcity of dinoflagellate cysts indicate nearshore depositional environments at the end of the Miocene-Early Pliocene.	Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Univ Nacl Sur, Dept Geol, Comis Invest Cient Provincia Buenos Aires, 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); Comision de Investigaciones Cientificas; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.							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L., 1998, AM ASS STRATIGRAPHIC, V34; WILLIAMS GL, 1993, 9210 GEOL SURV CAN, P1; WILLIAMS GL, 1998, SOC SEDIMENTARY GEOL, V60, P9; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Yrigoyen M.R., 1975, C GEOL ARG REL, V6, P139; ZAMBRANO JJ, 1980, 2 S GEOL REG ARG AC, V2, P1033	42	19	20	0	4	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana		2001	38	3					299	316						18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	491NC					2025-03-11	WOS:000172113900007
J	Taoufiq, NB; Barhoun, N				Taoufiq, NB; Barhoun, N			Upper Tortonian vegetation, climate and marine environment in the Taza-Guercif basin (Rifian corridor, Eastern Morocco)	GEOBIOS			Spanish	Article						tortonian; rifian corridor; Morocco; continental environment; marine environment	MEDITERRANEAN PLIOCENE; DINOFLAGELLATE CYSTS; ADJACENT SEAS; SEDIMENTS; MIOCENE; EVOLUTION; NORTH; OCEAN; TIME	The oued Msoun section (Middle Tortonian) is located in the eastern part of the Rifian corridor. Its age is ca. 7.5 Ma. According to pollen record, it has been possible to reconstruct vegetation and climate at such a low Mediterranean latitude. The Avicennia mangrove developed along the coastline which was edged by a subdesertic vegetation. Altitudinal organising of the vegetation favoured development of forest environments. Climate was subtropical to tropical, very dry along the shoreline and more humid in altitude. Marine epicontinental environment characterised by a high temperature (subtropical to tropical) sea-surface water is deduced from foraminifers and dinocysts. Editions scientifiques et medicales Elsevier SAS.	Univ Hassan II Mohammedia, Fac Sci Ben MSik, Casablanca, Morocco	Hassan II University of Casablanca	Taoufiq, NB (通讯作者)，Univ Hassan II Mohammedia, Fac Sci Ben MSik, BP 7955, Casablanca, Morocco.							Bachiri Taoufiq N., 2000, PALEONTOL EVOL, V32-33, P127; Barbero M., 1981, Anales Jard Bot Madrid, V37, P467; Benzaquen M., 1965, Etude stratigraphique preliminaire des formations dubasin de Guercif; BERNINI M, 1992, B SOC GEOL FR, V163, P73; BERNINI M, 1992, NOTES MEMOIRES SERVI, V366, P59; Bernini M., 1996, Notes et Memoires Serv. Geol. Maroc., V387, P85; Bertini A, 1998, MICROPALEONTOLOGY, V44, P413, DOI 10.2307/1486042; Bessedik M., 1984, Paleobiologie Continentale, V14, P153; Bessedik M., 1985, Reconstitution des environnements miocenes des regions nord-ouest mediterraneennes a partir de la palynologie; Bessedik M., 1984, Rev. Paleobiol., P25; BRAHIM LA, 1990, J AFR EARTH SCI, V11, P273, DOI 10.1016/0899-5362(90)90005-Y; Chikhi H., 1992, Geol Mediter, Marseille, V19, P19; CHOUBERT, 1962, LIVRE MEMOIRE P FALL, V1, P447; COLLETTA B, 1977, THESIS U GRENOBLE; COUR P., 1978, ANN MINES BELG, P155; DEVERNAL A, 1994, PLIOCENE TERRESTRIAL, P4; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; ELMOKHTARI J, 1990, THESIS U PARMA; Fauquette S, 1998, GEOBIOS-LYON, V31, P151, DOI 10.1016/S0016-6995(98)80035-1; Fauquette S, 1999, PALAEOGEOGR PALAEOCL, V152, P15, DOI 10.1016/S0031-0182(99)00031-0; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Hilgen FJ, 1995, EARTH PLANET SC LETT, V136, P495, DOI 10.1016/0012-821X(95)00207-S; Hodell DA, 1989, PALEOCEANOGRAPHY, V4, P467, DOI 10.1029/PA004i004p00467; KASSAS M, 1957, J ECOL, V44, P187; Krijgsman W, 1995, EARTH PLANET SC LETT, V136, P475, DOI 10.1016/0012-821X(95)00206-R; Krijgsman W, 1997, PALAEOGEOGR PALAEOCL, V133, P27, DOI 10.1016/S0031-0182(97)00039-4; Krijgsman W, 1999, MAR GEOL, V153, P147, DOI 10.1016/S0025-3227(98)00084-X; KRIJGSMAN W, 1997, EARTH PLANET SC LETT, V133, P27; Londeix L., 1999, PLIOCENE TIME CHANGE, P65; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; MEON H, 1986, GEOBIOS-LYON, V19, P601, DOI 10.1016/S0016-6995(86)80057-2; Michard A., 1976, Notes et Memoires du Service geologique, V252, P1; MOREL JL, 1989, GEODIN ACTA, V3, P283, DOI 10.1080/09853111.1989.11105193; MOREL JL, 1993, B SOC GEOL FR, V164, P79; Nix H., 1982, EVOLUTION FLORA FAUN, P47; SIERRO FJ, 1993, MAR MICROPALEONTOL, V21, P21; SUC JP, 1995, REV PALAEOBOT PALYNO, V87, P51, DOI 10.1016/0034-6667(94)00144-9; SUC JP, 1990, CR HEBD ACAD SCI, V3, P1701; SUC JP, 1989, B SOC GEOLOGIQUE FRA, V8, P541; Suc JP, 1986, B CENT RECH EXPL, V10, P477; TAOUFIQ NB, 2000, THESIS U CASABLANCA; TAYECH B, 1984, THESIS U LYON; Turon J.-L., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P313; Turon J.L., 1984, MEM I GEOL BASSIN AQ, V17, P1; 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; WARNY S., 1999, THESIS U CATHOLIQUE; WERNLI R, 1988, NOTES MEMOIRES SERVI, V331, P1; Zizi M., 1996, MEMOIR MUS NATL HIST, V170, P87	49	5	5	0	6	UNIV CLAUDE BERNARD-LYONI	VILLEURBANNE CEDEX	CENTRE DES SCI DE LA TERRE 43 BLVD DU 11 NOVEMBRE, 69622 VILLEURBANNE CEDEX, FRANCE	0016-6995			GEOBIOS-LYON	Geobios		2001	34	1					13	24						12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	489ER					2025-03-11	WOS:000171979500002
J	Louwye, S				Louwye, S			New Species of Dinoflagellate Cysts from the Berchem Formation, Miocene, Northern Belgium (Southern North Sea Basin)	GEOBIOS			English	Article						Dynoflagellate Cysts; New Species; Miocene; North Sea Basin; Belgium	EASTERN ENGLAND; PLIOCENE; GENERA	Four previously undescribed dinoflagellate species were encountered during a detailed biostratigraphic analysis of the Miocene Berchem Formation in northern Belgium: Ataxiodinium scaldemense nov. sp., Operculodinium? borgerholtense nov. sp., Bitectalodinium heistense nov. sp. and Pyxidinopsis brabantiana nov. sp. A formal description and assessment of the stratigraphic ranges of the new species are given. (C) Editions scientifiques et medicales Elsevier SAS.	State Univ Ghent, Lab Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，State Univ Ghent, Lab Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				[Anonymous], 1988, GEOLOGISCHES JB A; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1976, PROFESSIONAL PAPER G; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Blow W.H., 1979, CAINOZOIC GLOBIGERIN; Bukry D., 1973, Initial Reports DSDP, V15, P685, DOI DOI 10.2973/DSDP.PROC.15.116.1973; BUTSCHLI O, 1885, HG BRONNS KLASSEN OR, V1, P865; de Meuter F., 1980, Aardkundige Mededelingen, V1, P79; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; de Verteuil L., 1996, MICROPALEONTOLOGY, V42; DEHEINZELIN J, 1955, B SOC BELG GEOL, V64, P463; Doppert J.W.C., 1979, MEDEDELINGEN RIJKS G, V31, P1; Drugg W.S., 1967, Palaeontographica Abteilung B, V120; Fensome R.A., 1993, Micropaleontology Press Special Paper; Gaemers P.A.M, 1988, GEOLOGISCHES JB, V100, P379; HABIB D, 1976, MICROPALEONTOLOGY, V4, P373; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; 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; Hooyberghs H.J.F., 1983, Aardkundige Mededelingen, V2, P1; HOOYBERGHS H. J. F., 1988, GEOLOGISCHES JB A, VA100, P190; Hooyberghs HJF, 1996, GEOL MIJNBOUW, V75, P33; HUYGHEBAERT B, 1979, MEDEDELINGEN WERKGRO, V16, P59; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Louwye S, 2000, GEOL MAG, V137, P381, DOI 10.1017/S0016756800004258; LOUWYE S, IN PRESS GEOLOGICA B, V3, P1; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; MARTINI E, 1973, NEUES JB GEOLOGIE PA, V9, P555; Matsuoka K., 1992, NEOGENE QUATERNARY D, P165; Matsuoka Kazumi, 1997, Palynology, V21, P19; NYST H, 1845, MEMOIRES ACAD ROYALE, V17, P1; NYST HG, 1861, B ACAD ROYALE BELGIQ, V2, P29; Odin G. S., 1974, B SOC BELG GEOL, V83, P35; Pascher A., 1914, Berlin Ber D bot Ges, V32; Reid P.C., 1974, Nova Hedwigia, V25, P579; 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]; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Verbeek J., 1988, GEOLOGISCHES JB A, V100, P267; VERSTEEGH GJM, 1995, REV PALAEOBOT PALYNO, V85, P213, DOI 10.1016/0034-6667(94)00127-6; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WALL D., 1967, PALAEONTOLOGY, V10, P95; Willems W., 1988, GEOLOGISCHES JB A, V100, P179; Williams Graham L., 1998, AASP Contributions Series, V34, P1; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363	48	9	9	0	11	UNIV CLAUDE BERNARD-LYONI	VILLEURBANNE CEDEX	CENTRE DES SCI DE LA TERRE 43 BLVD DU 11 NOVEMBRE, 69622 VILLEURBANNE CEDEX, FRANCE	0016-6995			GEOBIOS-LYON	Geobios		2001	34	2					121	130						10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	489EV					2025-03-11	WOS:000171979800001
J	Mikalsen, G; Sejrup, HP; Aarseth, I				Mikalsen, G; Sejrup, HP; Aarseth, I			Late-Holocene changes in ocean circulation and climate: foraminiferal and isotopic evidence from Sulafjord, western Norway	HOLOCENE			English	Article						Late Holocene; benthonic foraminifera; stable isotopes; palaeoceanography; climatic variations; fjords; western Norway	RECENT BENTHIC FORAMINIFERA; NORTH-ATLANTIC; DINOFLAGELLATE CYSTS; SURFACE SEDIMENTS; NORWEGIAN FJORDS; PAST CLIMATE; ICE-AGE; OXYGEN; SEA; RECORD	A 278 cm long sediment core spanning the last 5500 years was collected from 440 m water depth in Sulafjorden, western Norway. Detailed analyses of benthonic foraminfera, stable isotopes and lithology have been performed on the core, and a chronology based on five AMS dates on benthonic foraminifera has been established. The foraminiferal assemblages consist of species that are common in the North Sea region today. The benthonic fauna seems to respond to changes in oxygenation of the bottom water in the fjord indicating relatively low dissolved oxygen contents prior to c. 2000 cal. sc followed by a gradual increase until c. 700 cal. BC. The oxygen levels in the water masses are assumed to reflect the ingress of oceanic water from the shelf. Downcore variations in the oxygen isotope ratios in the benthonic species Uvigerina mediterranea in Sulafjorden are interpreted to reflect temperature variations with a minimum amplitude of 2 degreesC. The isotopic data indicate five cold periods at c. 2150-1800 cal. BC, c. 850-600 cal, BC, 150 cal. BC to cal. AD 150, c, cal. AD 500-650, and one in the top of the core corresponding to the 'Little Ice Age' (c. cal. AD 1625). These periods are characterized by 1.5-2 degreesC reduction in the bottom-water temperatures in Sulafjorden. Some of the cold periods in the fjord record are contemporaneous with the Holocene ice-rafting events in the North Atlantic and glacier fluctuations in western Norway and Northern Scandinavia. This implies that late-Holocene climate fluctuations in Scandinavia are caused by circulation changes in the North Atlantic region.	Univ Bergen, Dept Geol, N-5007 Bergen, Norway	University of Bergen	Univ Tromso, Dept Geol, N-9037 Tromso, Norway.							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C	Wicander, R		Hoover, RB; Levin, GV; Paepe, RR; Rozanov, AY		Wicander, R			Acritarchs: Proterozoic and Paleozoic enigmatic organic-walled microfossils	INSTRUMENTS, METHODS, AND MISSIONS FOR ASTROBIOLOGY IV	PROCEEDINGS OF THE SOCIETY OF PHOTO-OPTICAL INSTRUMENTATION ENGINEERS (SPIE)		English	Proceedings Paper	Conference on Instruments, Methods, and Missions for Astrobiology IV	JUL 29-30, 2001	SAN DIEGO, CA	SPIE		acritarch; organic-walled microfossil; cyst; fossil eukaryotic phytoplankton; Proterozoic; Paleozoic	MIDDLE; OHIO; MICROPHYTOPLANKTON; AFFINITIES; IOWA; USA	Acritarchs are organic-walled cysts of unicellular protists that cannot be assigned to any known group of organisms. Most acritarchs are probably the resting cysts of marine eukaryotic phytoplankton. Some acritarchs are thought to be dinoflagellate cysts but lack the requisite morphology to make a positive attribution. Others, however, can be confidently assigned to the chlorophytes (green algae). but for convenience, are still commonly included in the acritarchs. Thus, acritarchs are a heterogeneous. polyphyletic collection of organic-walled microfossils of unknown or uncertain origin. Acritarchs vary in size from <10 mum to more than 1 mm, but the majority of species range from 15 to 80 mum. Because of their small size, abundance and diversity,. as well as widespread distribution. acritarchs are very useful in biostratigraphic correlation, as well as palcobiogeographic and paleoenvironmental studies. Acritarchs are found throughout the geologic column but were most common during the Late Proterozoic and Paleozoic. Because they represent the fossil record of the base of the marine food chain during the Proterozoic and Paleozoic, acritarchs played an important role in the evolution of the global marine ecosystem.	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L., 1961, Palaeontology, V4, P392; Strother P.K., 1996, Palynology: Principles and Applications, Volume, V1, P81, DOI DOI 10.1016/0034-6667(95)00117-4; Strother P. K., 1994, Sedimentation of organic particles, P489; Talyzina NM, 2000, REV PALAEOBOT PALYNO, V108, P37, DOI 10.1016/S0034-6667(99)00032-9; TAPPAN H, 1980, PALEOBIOLOGY PLANT P, pCH3; THUSU B, 1972, J SEDIMENT PETROL, V42, P930; Tongiorgi Marco, 1999, Bollettino della Societa Paleontologica Italiana, V38, P297; UPSHAW CF, 1964, SOC EC PALAEONTOL MI, V11, P153; van Waveren I.M., 1994, Scripta Geologica, V105, P53; Van Waveren Isabel M., 1993, Special Papers in Palaeontology, V48, P111; Vavrdova M, 1997, REV PALAEOBOT PALYNO, V98, P33, DOI 10.1016/S0034-6667(97)00023-7; VAVRDOVA M, 1974, REV PALAEOBOT PALYNO, V18, P171, DOI 10.1016/0034-6667(74)90016-5; Vavrdova Milada, 1992, Acta Universitatis Carolinae Geologica, V0, P361; Vidal G, 1997, PALEOBIOLOGY, V23, P230, DOI 10.1017/S0094837300016808; White M.C., 1862, Am. Jour. Sci, V33, P385; Wicander R, 1997, REV PALAEOBOT PALYNO, V98, P125, DOI 10.1016/S0034-6667(97)00017-1; WICANDER R, 1983, OHIO J SCI, V83, P2; WICANDER R, 1985, MICROPALEONTOLOGY, V31, P97, DOI 10.2307/1485481; Wicander R, 1999, J PALEONTOL, V73, P1; WOOD GD, 1997, ACTA U CAROLINAE GEO, V40, P703	54	0	0	1	5	SPIE-INT SOC OPTICAL ENGINEERING	BELLINGHAM	1000 20TH ST, PO BOX 10, BELLINGHAM, WA 98227-0010 USA	0277-786X		0-8194-4209-7	P SOC PHOTO-OPT INS			2001	4495						331	340						10	Astronomy & Astrophysics; Instruments & Instrumentation	Conference Proceedings Citation Index - Science (CPCI-S)	Astronomy & Astrophysics; Instruments & Instrumentation	BU13L					2025-03-11	WOS:000175125700033
J	Brown, J; Fernand, L; Horsburgh, KJ; Hill, AE; Read, JW				Brown, J; Fernand, L; Horsburgh, KJ; Hill, AE; Read, JW			Paralytic shellfish poisoning on the east coast of the UK in relation to seasonal density-driven circulation	JOURNAL OF PLANKTON RESEARCH			English	Article							NORTH-SEA; GYRE; VARIABILITY	Paralytic shellfish poisoning (PSP) toxin associated with the dinoflagellate Alexandrium tamarense is found on the north-east coast of the UK in late spring/early summer. Severe outbreak an sporadic, and knowledge of the cause and origin of the phytoplankton blooms and whether they develop from a diffuse source or from a seed population is uncertain. Recent observations of the circulation of the region demonstrate a persistent southward near-coastal flow associated with strong bottom fronts bounding a pool of cold dense bottom water isolated below the seasonal (spring/summer) thermocline. Flows extend continuously for similar to 500 km from the Firth of Forth to Flamborough Head before passing offshore to the Dogger Bank. These observations suggest that dinoflagellates originating from the high concentrations of A. tamarense cysts in the sediment of the Firth of Forth act to maintain a dinoflagellate population in the coastal region south to Flamborough Head, thereby maintaining the risk of PSP outbreaks.	Ctr Environm Fisheries & Aquaculture Sci, Lowestoft Lab, Lowestoft NR33 0HT, Suffolk, England; Univ Wales Bangor, Marine Sci Labs, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales; Bidston Observ, Proudman Oceanog Lab, Birkenhead L43 7RA, Merseyside, England	Centre for Environment Fisheries & Aquaculture Science; Bangor University; NERC National Oceanography Centre	Ctr Environm Fisheries & Aquaculture Sci, Lowestoft Lab, Pakefield Rd, Lowestoft NR33 0HT, Suffolk, England.							ADAMS JA, 1968, NATURE, V220, P24, DOI 10.1038/220024a0; 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; [Anonymous], 86 MAFF DIR FISH RES; Ayres P. A., 1975, Environmental Health, V83, P261; AYRES PA, 1978, 40 MAFF DFR, P1; Backhaus J., 1983, North Sea Dynamics, P63; Brown J, 1996, SEA TECHNOL, V37, P23; Brown J, 1999, ESTUAR COAST SHELF S, V48, P343, DOI 10.1006/ecss.1999.0426; BROWN J, 1997, CADMIUM CHROMIUM SED; COULSON JC, 1968, NATURE, V220, P23, DOI 10.1038/220023a0; Davies A.M, 1983, North Sea Dynamics, P44; DURANCE JA, 1989, DTSCH HYDROGR Z, V42, P271; ELLIOTT AJ, 1991, CONT SHELF RES, V11, P453, DOI 10.1016/0278-4343(91)90053-9; Fernand L., 1999, THESIS U WALES BANGO; GARRETT CJR, 1981, PHILOS T R SOC A, V302, P653; GMITROWICZ EM, 1993, CONT SHELF RES, V13, P863, DOI 10.1016/0278-4343(93)90014-O; HIGMAN W, 1995, STUDY ALEXANDRIUM CY; Hill AE, 1997, ESTUAR COAST SHELF S, V44, P83, DOI 10.1016/S0272-7714(97)80010-8; Hill AE, 1997, ESTUAR COAST SHELF S, V45, P473, DOI 10.1006/ecss.1996.0198; HILL AE, 1994, CONT SHELF RES, V14, P479, DOI 10.1016/0278-4343(94)90099-X; Horsburgh K.J., 1999, THESIS U WALES BANGO; Horsburgh KJ, 1998, ESTUAR COAST SHELF S, V47, P285, DOI 10.1006/ecss.1998.0354; Horsburgh KJ, 2000, PROG OCEANOGR, V46, P1, DOI 10.1016/S0079-6611(99)00054-3; HOWARTH MJ, 1993, PHIL T R SOC LONDO A, V343, P5; Joint I, 1997, J PLANKTON RES, V19, P937, DOI 10.1093/plankt/19.7.937; JOINT L, 1994, COASTAL ZONE COLOR S; Lee AJ., 1981, Atlas of the seas around the British Isles; LEWIS J, 1993, INVESTIGATION DISTRI; Lewis Jane, 1995, P175; LOEWE P, 1996, DTSCH HYDROGR Z, V48, P175; LWIZA KMM, 1991, CONT SHELF RES, V11, P1379, DOI 10.1016/0278-4343(91)90041-4; PRANDLE D, 1984, PHILOS T R SOC A, V310, P407, DOI 10.1098/rsta.1984.0002; Proctor R, 1996, J MARINE SYST, V8, P285, DOI 10.1016/0924-7963(96)00011-5; ROBINSON GA, 1968, NATURE, V220, P22, DOI 10.1038/220022a0; SIMPSON JH, 1974, NATURE, V250, P404, DOI 10.1038/250404a0; UNESCO, 1981, UNESCO TECHN PAP MAR, V36; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; WYATT T, 1993, DEV MAR BIO, V3, P73	40	31	31	0	7	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	JAN	2001	23	1					105	116		10.1093/plankt/23.1.105	http://dx.doi.org/10.1093/plankt/23.1.105			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	405JB		Bronze			2025-03-11	WOS:000167155300012
J	Kremp, A				Kremp, A			Effects of cyst resuspension on germination and seeding of two bloom-forming dinoflagellates in the Baltic Sea	MARINE ECOLOGY PROGRESS SERIES			English	Article						cysts; dinoflagellates; germination; Peridiniella; resuspension; Scrippsiella turbulence	SCRIPPSIELLA-HANGOEI; GONYAULAX-TAMARENSIS; RESTING CYSTS; CELL-DIVISION; PHYTOPLANKTON; TURBULENCE; SEDIMENTATION; DINOPHYCEAE; DARKNESS; FINLAND	The implications of cyst resuspension on germination and subsequent seeding of the 2 spring-bloom dinoflagellates Scrippsiella hangoei (Schiller) Larsen and Peridiniella catenata (Levender) Balech from the Baltic Sea were investigated in a field study and laboratory experiments. Sedimentation of resuspended cysts was monitored by an automated sediment trap in 2 consecutive winters prior to and throughout the germination period off the SW coast of Finland. The effects of increased irradiances and water motion on germination and germling survival were tested by incubating cysts at different light levels and in turbulent water, Cyst fluxes of both species were low during the calm and cold winter of 1998/1999. In 1999/2000, heavy storms caused strong resuspension of S. hangoei cysts, Light significantly increased the germination frequency of S. hangoei cysts and supported germling survival and cell division. In P. catenata, the percentage of excystment was not significantly influenced by light and germination was successfully completed in both darkness and light. Subsequent growth of the species, however, required light, although maximum cell numbers were encountered at an irradiance as low as 10 mu mol m(-2) s(-1). Small-scale turbulence reduced the germination frequency of S. hangoei but did not affect excystment in P. catenata. No negative effects on subsequent growth were detected. The favourable effects of light on germination and germling survival of S. hangoei emphasize that resuspension would be advantageous for the bloom initiation of this species. Cyst resuspension seems to be less important in P. catenata population dynamics, since germination can be successfully completed in darkness and the amount of cysts transported to the water surface is insignificant even with strong turbulent mixing. It is concluded that cyst resuspension may be advantageous for dinoflagellate bloom initiation, depending on its extent and timing and the specific germination requirements of the respective organism.	Univ Helsinki, Div Hydrobiol, Dept Systemat & Ecol, FIN-00014 Helsinki, Finland; Tvarminne Zool Stn, SF-10900 Hango, Finland	University of Helsinki	Kremp, A (通讯作者)，Univ Helsinki, Div Hydrobiol, Dept Systemat & Ecol, POB 17, FIN-00014 Helsinki, Finland.	anke.kremp@helsinki.fi	Kremp, Anke/I-8139-2013					Andersen NM, 1998, ENTOMOL SCAND, V29, P1; 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, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], OPHELIA S; [Anonymous], ACTA BOT FENN; BALCH WM, 1983, CAN J FISH AQUAT SCI, V40, P244, DOI 10.1139/f83-287; BERDALET E, 1992, J PHYCOL, V28, P267, DOI 10.1111/j.0022-3646.1992.00267.x; BINDER BJ, 1986, NATURE, V322, P659, DOI 10.1038/322659a0; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Cullen J. 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L, 1996, HARMFUL TOXIC ALGAL, P189; WHITE AW, 1976, J FISH RES BOARD CAN, V33, P2598, DOI 10.1139/f76-306	44	55	62	0	21	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2001	216						57	66		10.3354/meps216057	http://dx.doi.org/10.3354/meps216057			10	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	462AF		Bronze			2025-03-11	WOS:000170395500005
J	Sgrosso, S; Esposito, F; Montresor, M				Sgrosso, S; Esposito, F; Montresor, M			Temperature and daylength regulate encystment in calcareous cyst-forming dinoflagellates	MARINE ECOLOGY PROGRESS SERIES			English	Article						calcareous cysts; cysts; daylength; dinoflagellates; encystment; Calciodinellum; Scrippsiella; Pentapharsodinium	QUATERNARY EASTERN; PHYTOPLANKTON; SCRIPPSIELLA; DINOPHYCEAE; GROWTH; BAY; SEXUALITY; DYNAMICS; PATTERNS; ECOLOGY	We tested the effect of temperature (15, 20, and 25 degreesC), daylength (8:16, 12:12 and 16:8 h light:dark cycles), and culture medium (K/5 and K/50) conditions on cyst production in batch cultures of 4 dinoflagellate species that form calcareous resting stages (Scrippsiella trochoidea var. aciculifera, Pentapharsodinium tyrrhenicum, Calciodinellum operosum and S. rotunda). The 4 species showed different encystment patterns at the temperature conditions tested; cyst production was inversely related to daylength conditions, and higher cyst yields were obtained with the less concentrated growth medium. Experiments with semi-continuous cultures of S, rotunda, in which nutrient concentration was kept within values comparable to in situ concentrations, were carried out with the aim of decoupling the effect of nutrient depletion on cyst production from that of daylength. Cyst production in this species, kept at a constant growth rate in non-depleted nutrient conditions, was only obtained at the shortest daylengths, thus supporting the role of short daylength in inducing the production of calcareous cysts. Our data suggest that encystment in the 4 species is regulated by a complex interplay of at least 3 factors: daylength, temperature and nutrient concentration. These results contribute to explain the timing of resting-stage production at sea, and point to the possible role of daylength as an environmental signal for the regulation of life cycles in dinoflagellates.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@alpha.szn.it		Montresor, Marina/0000-0002-2475-1787				ANDERSON DM, 1985, J PHYCOL, V21, P200; 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; Anderson Donald M., 1997, Limnology and Oceanography, V42, P1009; [Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; BINDER BJ, 1986, NATURE, V322, P659, DOI 10.1038/322659a0; BINDER BJ, 1987, J PHYCOL, V23, P99; Burkhardt S, 1999, MAR ECOL PROG SER, V184, P31, DOI 10.3354/meps184031; COSTAS E, 1989, CHRONOBIOLOGIA, V16, P265; D'Onofrio G, 1999, J PHYCOL, V35, P1063, DOI 10.1046/j.1529-8817.1999.3551063.x; DALE B, 1992, DINOFLAGELLATE CONTR, P1; DRING MJ, 1988, ANNU REV PLANT PHYS, V39, P157, DOI 10.1146/annurev.pp.39.060188.001105; Dring MJ, 1984, Progress in phycological research, V8, P159; EILERTSEN HC, 1995, MAR ECOL PROG SER, V116, P303, DOI 10.3354/meps116303; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Grasshoff K., 1983, Methods of seawater analysis; HADER DP, 1991, PHOTOCHEM PHOTOBIOL, V54, P143, DOI 10.1111/j.1751-1097.1991.tb01998.x; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Hiltz M, 2000, PHYCOLOGIA, V39, P59, DOI 10.2216/i0031-8884-39-1-59.1; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Kamykowski D, 1998, J PLANKTON RES, V20, P1781, DOI 10.1093/plankt/20.9.1781; Karentz D, 1998, J PLANKTON RES, V20, P145, DOI 10.1093/plankt/20.1.145; KELLER MD, 1987, J PHYCOL, V23, P633; Keupp H., 1991, P267; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; MCQUOID MR, 1995, J PHYCOL, V31, P44, DOI 10.1111/j.0022-3646.1995.00044.x; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; NEHRING S, 1995, HELGOLANDER MEERESUN, V49, P375, DOI 10.1007/BF02368363; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PIERCE RW, 1994, MAR ECOL PROG SER, V112, P225, DOI 10.3354/meps112225; Roenneberg T, 1996, PHYSIOL PLANTARUM, V96, P733, DOI 10.1111/j.1399-3054.1996.tb00250.x; Roenneberg T, 1996, FASEB J, V10, P1443, DOI 10.1096/fasebj.10.12.8903515; SICKOGOAD L, 1989, J PLANKTON RES, V11, P375, DOI 10.1093/plankt/11.2.375; Sokal R.R., 1995, BIOMETRY; SWEENEY BM, 1984, PLANT PHYSIOL, V75, P242, DOI 10.1104/pp.75.1.242; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; WALL D, 1968, Journal of Paleontology, V42, P1395; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; ZINGONE A, 1990, MAR ECOL-P S Z N I, V11, P157, DOI 10.1111/j.1439-0485.1990.tb00236.x	45	59	69	1	25	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2001	211						77	87		10.3354/meps211077	http://dx.doi.org/10.3354/meps211077			11	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	412NM		Green Submitted, Bronze			2025-03-11	WOS:000167561300007
J	Guerstein, GR; Williams, GL; Fensome, RA				Guerstein, GR; Williams, GL; Fensome, RA			<i>Cannosphaeropsis quattrocchiae</i>, a new species of dinoflagellate cyst from the mid Cenozoic of the Colorado Basin, Argentina	MICROPALEONTOLOGY			English	Article							MIOCENE	Cannosphaeropis quattrocchiae n. sp., from the Cenozoic of the Colorado Basin, resembles two other species, Cannosphaeropsis utinensis and Cannosphaeropsis passio, and has been confused with the former. However, separation of the three species, based in part on the location of the processes, allows for their use in refining Cenozoic stratigraphy and paleoecology. On present evidence, the last appearance datum of Cannosphaeropsis quattrocchiae appears to be early Miocene, whereas Cannosphaeropsis passio is known only from the mid Miocene. Cannosphaeropsis utinensis, primarily a late Cretaceous species, occurs occasionally in lower Paleocene sediments. Geographically, Cannosphaeropsis utinensis and Cannosphaeropsis passio are known only from the Northern Hemisphere, whereas Cannosphaeropsis quattrocchiae is known only from the Southern Hemisphere.	Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, RA-8000 Bahia Blanca, Argentina; Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, San Juan 670, RA-8000 Bahia Blanca, Argentina.							[Anonymous], 1976, BEDFORD I OCEANOGRAP; [Anonymous], 1996, Palynology: principles and applications; ARCHANGELSKY S, 1996, 13 C GEOL ARG 3 C EX, V4, P67; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; Barrett AJ, 1996, PERSPECT DRUG DISCOV, V6, P1, DOI 10.1007/BF02174042; BECKER D, 1980, 2 C ARG PAL BIOESTR, V2, P315; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; Brosius M., 1963, Z DTSCH GEOLOGISCHEN, V114, P32; BROWN S, 1984, INITIAL REPORTS DEEP, V80, P643; Bujak J. P., 1980, SPECIAL PAPERS PALEO, V24; Bujak J.P., 1986, Contribution Series, V17, P7; BUJAK JP, 1978, GEOLOGICAL SURVEY CA, V297; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; Cookson I. C., 1961, Proceedings of the Royal Society of Victoria N S, V74, P69; Cookson I. 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J	Piasecki, S				Piasecki, S			Three new Middle Jurassic dinoflagellate cysts from East Greenland	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article								Three new species of dinoflagellate cysts are described from the Middle Jurassic successions in East Greenland. Dinoflagellate assemblages are recovered from thin mud shales within a Middle Jurassic succession otherwise dominated by coarse-grained marine sandstone. The new species are morphological characteristic and stratigraphic useful within the Upper Bathonian to Callovian. Evansia janeae n.sp. is described from the Charcot Bugt Formation in Milne Land, central East Greenland. The large 31 archaeopyle of E. janeae n. sp. is consistently and characteristically developed whereas the shape and sculpture vary significantly. Valvaeodinium leneae n.sp. and Valvaeodinium hanneae n.sp. are described from northern Hold with Hope and Store Koldewey, North East Greenland. Both species expose an archacopyle in the apical legion with a composite operculum of two opercular pieces, interpreted as a type Al. However, V. leneae has two wall layers closely apressed whereas V. hanneae is cavate with membranous filling of the cavation.	Geol Survey Denmark & Greenland, DK-2400 Copenhagen NV, Denmark	Geological Survey Of Denmark & Greenland	Piasecki, S (通讯作者)，Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark.							BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; CALLOMON JH, 1980, GEOL MAG, V117, P211, DOI 10.1017/S0016756800030442; Callomon JH, 1993, B GEOL SOC DENMARK, V40, P83; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; Davies E.H., 1983, GEOLOGICAL SURVEY CA, V359; EISENACK A, 1969, NEUES JB GEOLOGIE PA, P337; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; GOCHT H, 1957, PALAEONTOL Z, V33, P50; HAKANSSON E, 1981, Bulletin of the Geological Society of Denmark, V30, P11; HANSEN J M, 1979, Micropaleontology (New York), V25, P113, DOI 10.2307/1485261; Milner P. S, 1996, FORMATION SOURCE RES, VII; MILNER PS, 1996, FORMATION SOURCE RES, V1; Morgenroth P., 1970, Neues Jb. Geol. Palaont. Abh., V136, P345; Pascher A., 1914, Berlin Ber D bot Ges, V32; PIASECKI S, 2001, JURASSIC DINOFLAGELL; Piasecki S., 1996, FORMATION SOURCE RES, V1; PIASECKI S, 1996, FORMATION SOURCE RES, P1; PIASECKI S, 2001, GEOLOGY GREENLAND SU; PIASECKI S, 1994, WANDEL SEA BASIN, P1; Pocock S.A.J., 1972, Palaeontographica Abteilung B Palaeophytologie, V137, P85; Ravn JPJ., 1911, MEDDELELSER GRONLAND, V45, P437, DOI [10.5962/bhl.title.29066, DOI 10.5962/BHL.TITLE.29066]; Smelror M., 1991, Journal of Micropalaeontology, V10, P175; Stemmerik L., 1997, Geology of Greenland Survey Bulletin, V176, P29, DOI [10.34194/ggub.v176.5058, DOI 10.34194/GGUB.V176.5058]; Stemmerik L., 1990, RAPPORT GRONLANDS GE, V148, P123, DOI DOI 10.34194/RAPGGU.V148.8131; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; VOSGERAU H, 2001, GEOLOGY GREENLAND SU; VOZZHENNIKOVA TF, 1979, AKAD NAUK SSSR SIBIR, V422, P1	29	2	2	1	3	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					15	31		10.1127/njgpa/219/2001/15	http://dx.doi.org/10.1127/njgpa/219/2001/15			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000003
J	Feist-Burkhardt, S; Monteil, E				Feist-Burkhardt, S; Monteil, E			Gonyaulacacean dinoflagellate cysts with multi-plate precingular archaeopyle	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							SEA DRILLING PROJECT; STRATIGRAPHY; MIDDLE	The morphology of fossil gonyaulacacean dinoflagellate cysts with multi-plate precingular archaeopyle has been analysed in detail using different microscopical methods, namely transmitted light microscopy, scanning electron microscopy and the new technique of confocal laser scanning microscopy. The analyses made evident, that important morphological characteristics used so far for the differentiation of the two genera Dissiliodiniun DRUGG 1978 emend. BAILEY & PARTINGTON 1991 and Durotrigia BAILEY 1987 are not appropriate. The genus Dissiliodinium is therefore emended. For the unambiguous differentiation between the genera Dissiliodinium acid Durotrigia the manner of how paratabulation is expressed on the cyst's surface is used as discriminating feature. In the genus Dissiliodinium paratabulation may be expressed by negative structures, such as grooves, reduction of ornamentation or penitabular ornamentation, in the genus Durotrigia paratabulation is expressed by elevated, positive structures, such as septa, crests or ridges. Five new species from the early Middle Jurassic of England, France and Germany are described, three belong to the genus Dissiliodinium (D. baileyi n. sp., D. lichenoides n.sp., D. minimum n.sp.), one to Durotrigia (D. omentifera n.sp.) and one to the new genus Cavatodissiliodinium with the type species C. hansgochtii n.g. et n.sp. Some complementary remarks on the morphology of the early Cretaceous species Dissiliodinium curiosum BURGER Br SARJEANT 1995 are provided. A summary of the major morphological features for specific separation as well as the known geographical and stratigraphical distribution is documented for all species belonging to the genus Dissiliodinium. All newly described taxa are considered to be useful stratigraphical markers.	Tech Univ Darmstadt, Inst Geol & Palaeontol, D-64287 Darmstadt, Germany; BG Technol, Gas Res & Technol Ctr, Loughborough LE11 3GR, Leics, England	Technical University of Darmstadt	Tech Univ Darmstadt, Inst Geol & Palaeontol, Schnittspahnstr 9, D-64287 Darmstadt, Germany.	feist@bio.tu-darmstadt.de; eric.monteil@bgtech.co.uk	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242				[Anonymous], 1985, SPOROPOLLENIN DINOFL; Bailey D., 1987, Journal of Micropalaeontology, V6, P89; Bailey D.A., 1991, Journal of Micropalaeontology, V9, P245; BAILEY D A, 1990, Palynology, V14, P135; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Burger D., 1996, Palynology, V20, P49; Burger Dennis, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V197, P119; Burkhalter RM, 1997, ECLOGAE GEOL HELV, V90, P269; CASSENS CB, UNPUB REV PALAEOBOT; CASSENS CB, 1999, THESIS DARMSTADT U T; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Feist-Burkhardt S, 1999, BULL CENT RECH ELF E, V22, P103; FEISTBURKHARDT S, 1990, B CENT RECH EXPL, V14, P611; FEISTBURKHARDT S, 1992, PALYNOLOGY, V16, P219; FEISTBURKHARDT S, 1999, LEICA CONFOCAL APPL, P6; FEISTBURKHARDT S, 1998, BULL CENT RECH ELF E, V21, P31; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fenton J.P.G., 1980, Palaeontology (Oxford), V23, P151; GASSMANN G, 1990, JAHRESHEFTE GEOLOGIS, V32, P159; GOCHT H, 1974, Archiv fuer Protistenkunde, V116, P381; GOCHT H, 1981, N JB GEOL PALAONT MH, P149; GOCHT H, 1987, N JB GEOL PALAONT MH, P705; HABIB D, 1987, INITIAL REP DEEP SEA, V93, P751; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; Leereveld H, 1997, CRETACEOUS RES, V18, P385, DOI 10.1006/cres.1997.0070; LONDEIX L, 1990, THESIS U BORDEAUX 1; Pourtoy D., 1989, THESIS U BORDEAUX 1; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; RIOULT M, 1991, B CENT RECH EXPL, V15, P101	36	32	33	0	0	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					33	81		10.1127/njgpa/219/2001/33	http://dx.doi.org/10.1127/njgpa/219/2001/33			49	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000004
J	Duxbury, S				Duxbury, S			A palynological zonation scheme for the lower cretaceous - United Kingdom Sector, Central North Sea	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							DINOFLAGELLATE	Detailed stratigraphic studies of Lower Cretaceous sections in the Moray Firth area of the U.K.C.S. have included palynological analyses of approximately 30 wells in quadrants 13 and 14. Thirty-two zones have been defined in the Valanginian to Albian interval, based on the consistent recognition of over 170 palynofloral events. The positions of 14 Maximum Flooding Surfaces have been recorded within this zonation scheme. Twelve species and one sub-species of stratigraphically significant dinoflagellate cysts are described as new.	Duxbury Stratig Consultants, Aberdeen AB15 8TT, Scotland		Duxbury Stratig Consultants, 4 Coldstone Ave, Aberdeen AB15 8TT, Scotland.							[Anonymous], PALAEONTOLOGY; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1988, GEOLOGICAL SURVEY PA; [Anonymous], 1996, Palynology: principles and applications; BAILEY DA, 1997, J MICROPALAEONTOL, V9, P245; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BRIDEAUX W. W., 1975, GEOLOGICAL SURVEY CA, V252, P1; BUTSCHLI, 1885, KLASSEN ORDNUNGEN TH, P865; Davey R.J., 1974, S STRATIGRAPHIC PALY, V3, P41; Davey R.J., 1966, STUDIES MESOZOIC CAI, P28; Davey R.J., 1979, American Association of Stratigraphic Palynologists Contributions Series, V5B, P48; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; DAVEY RJ, 1969, BRIT MUSEUM NATURAL, V3, P4; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; 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; Eisenack A., 1958, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V106, P383; EISENACK A, 1963, N JB PALAONT ABH, V110, P98; Fensome R.A., 1993, CLASSIFICATION FOSSI; Gocht H., 1957, Palaeontologische Zeitschrift, V31, P163; GOCHT H., 1959, PAL ONTOLOGISCHE Z, V33, P50; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; Heilmann-Clausen Claus, 1995, Geologisches Jahrbuch Reihe A, V141, P257; HELENES J, 1984, Palynology, V8, P107; Johnson H., 1993, Lithostratigraphic Nomenclature of the UK North Sea; Klement K. W., 1960, Palaeontographica, VA114, P1; Lentin J. K., 1977, Bedford Institute of Oceanography, Report Series; LENTIN J. K., 1973, 7342 GEOL SURV CAN; MORGAN RP, 1980, MEM GEOL SURV NSW PA, V18, P1; NeaLE J.W., 1962, GEOL MAG, V99, P439; Pascher A., 1914, Berlin Ber D bot Ges, V32; SARJEANT WAS, 1985, REV PALAEOBOT PALYNO, V45, P47, DOI 10.1016/0034-6667(85)90065-X; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; [No title captured]	34	43	43	0	4	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					95	137		10.1127/njgpa/219/2001/95	http://dx.doi.org/10.1127/njgpa/219/2001/95			43	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000006
J	Schioler, P; Roncaglia, L; Wilson, GJ				Schioler, P; Roncaglia, L; Wilson, GJ			<i>Alterbidinium</i>?: <i>novozealandicum</i>, a new dinoflagellate from the Herring Formation (Upper Cretaceous), southern Marlborough, New Zealand	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							BIOSTRATIGRAPHY; ISLAND	The new dinoflagellate Alterbidinium? novozealandicum n.sp. from the uppermost lower Haumurian (middle to upper Campanian) Isabelidinium korojo-nense Interval Zone in New Zealand, is a large, fusiform, dorso-ventrally compressed, peridinioid cyst without endocyst. The apical part of the cyst has two folds on the dorsal side. The cyst bears a long apical horn and a long left antapical horn. The right antapical horn is very reduced. The paratabulation is expressed by the intercalary 2a periarcheopyle only. Alterbidinium? novozealandicum was encountered in a narrow stratigraphic interval in the Herring Formation, and may be a potential stratigraphic marker.	Geol Survey Denmark & Greenland, DK-2400 Copenhagen, Denmark	Geological Survey Of Denmark & Greenland	Schioler, P (通讯作者)，Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen, Denmark.							[Anonymous], I GEOL NUCL SCI MONO; [Anonymous], 1987, ASS AUSTRALASIAN PAL; Askin RA, 1999, J PALEONTOL, V73, P373, DOI 10.1017/S0022336000027888; Crampton J, 2000, NEW ZEAL J GEOL GEOP, V43, P309, DOI 10.1080/00288306.2000.9514890; EVANS PR, 1971, GEOLOGY GEOPHYSICS A, V134, P30; Fensome R.A., 1993, MICROPALEONTOL SPEC, V7; GRADSTEIN FM, 1994, J GEOPHYS RES-SOL EA, V99, P24051, DOI 10.1029/94JB01889; KHOWAJAATEEQUZZ, 1991, PALAEOBOT, V39, P37; LENTIN J K, 1986, Palynology, V10, P111; LENTIN JK, 1976, BIR7516 BEDF I OC RE, P1; Marshall N.G., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P195; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Roncaglia L, 1999, REV PALAEOBOT PALYNO, V106, P121, DOI 10.1016/S0034-6667(99)00005-6; Roncaglia L, 2000, ALCHERINGA, V24, P135, DOI 10.1080/03115510008619530; Roncaglia L., 1997, IGNS SCI REPORT, V97, P1; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; WILLIAMS GL, 1998, AM ASS STRATIGR PALY, V34	17	2	2	0	1	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0077-7749			NEUES JAHRB GEOL P-A	Neues. Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					139	152		10.1127/njgpa/219/2001/139	http://dx.doi.org/10.1127/njgpa/219/2001/139			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000007
J	Eaton, GL; Fensome, RA; Riding, JB; Williams, GL				Eaton, GL; Fensome, RA; Riding, JB; Williams, GL			Re-evaluation of the status of the dinoflagellate cyst genus <i>Cleistosphaeridium</i>	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Review							MIDDLE EOCENE; LOWER OLIGOCENE; ATLANTIC-OCEAN; NORTH-SEA; BIOSTRATIGRAPHY; MIOCENE; DINOCYST; STRATIGRAPHY; ZONATION; GULF	Although the typically Cenozoic dinoflagellate cyst genus Cleistosphaeridium resembles the Jurassic genus Systematophora in its epical archeopyle, skolochorate form and the presence of penitabular process complexes, other morphological features indicate that the two genera are not closely related. For example, pick-like processes endings (termed "dolabrate" herein) are characteristic of species of Cleistosphaeridium, but not of Systematophora. The unrelated nature of the two genera is supported by their very different stratigraphic ranges. Thus, Cleistosphaeridium is considered not to be a taxonomic synonym of Systematophora. Its type material is re-examined, the diagnoses of Cleistosphaeridium and Cleistosphaeridium diversispinosum are emended, and three new combinations are proposed: Cleistosphaeridium placacanthum. Cleistosphaeridium ancyreum and Cleistosphaeridium polypetellum A critical review of the biostratigraphic occurrence of the four species of Cleistosphaeridium yields the following confirmed ranges: Cleistosphaeridium diversispinosum,a - Early Eocene to Early Oligocene; Cleistosphaeridium placacanthum - Mid Eocene to Late Miocene with most records in the Oligocene to Early Miocene; Cleistosphaeridium ancyreum - Early Eocene to Mid Miocene; Cleistosphaeridium polypetellum - Early to Mid Eocene. There appear to he general morphological tendencies from more to less membranous processes in the Eocene and, throughout the range of the genus, increasing development of basal ridges connecting the processes within a complex.	Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; Geol Survey Canada, Dartmouth, NS B2Y 4A2, Canada; British Geol Survey, Keyworth NG12 5GG, Notts, England	Natural History Museum London; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Eaton, GL (通讯作者)，Nat Hist Museum, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.							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H., 1990, VEROFFENTLICHUNGEN A, VA10, P11; Weyns W., 1970, B SOC BELG GEOL, V79, P247; Williams G. L., 1975, GEOLOGICAL SURVEY CA, V236; WILLIAMS GL, 1966, BRIT MUSEUM B, V3, P20; Wilson G.J., 1988, NZ GEOLOGICAL SURVEY, V57; Zaporozhets NI., 1989, PALEOFLORISTICS STRA, P85	118	39	42	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.	JAN	2001	219	1-2					171	205		10.1127/njgpa/219/2001/171	http://dx.doi.org/10.1127/njgpa/219/2001/171			35	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000009
J	Pross, J				Pross, J			Dinoflagellate cyst biogeography and biostratigraphy as a tool for palaeoceanographic reconstructions: An example from the Oligocene of western and northwestern Europe	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							NORTH-SEA; EOCENE	The Last Occurrence (LO) pattern of the wetzelloid dinoflagellate cysts Wetzeliella symmetrica WEILER 1956, Wetzeliella gochtii COSTA & DOWNIE 1976, and Rhombodinium draco GOCHT 1955 in Early Oligocene sediments from western and northwestern Europe shows a strong diachronism. Oldest LOs are observed in the southern Dart of this region (i.e., in the Upper Rhine Graben and Mainz Embayment), wheras LOs in the Northwest European Tertiary Basin are younger. This diachronism is interpreted to reflect palaeoenvironmental and palaeoceanographic changes within the seaway connecting the Tethys with the Northwest European Tertiary Basin. The dependence of W. symmetrica, W. gochtii, and R. draco LOs on regional palaeoenvironmental conditions demonstrates the need to analyze the palaeoecology of fossil dinoflagellate cysts prior to using them for long-distance correlations.	Inst & Museum Geol & Palaontol, D-72076 Tubingen, Germany	Eberhard Karls University of Tubingen	Pross, J (通讯作者)，Inst & Museum Geol & Palaontol, Sigwartstr 10, D-72076 Tubingen, Germany.							[Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1988, Geol. 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Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					207	219		10.1127/njgpa/219/2001/207	http://dx.doi.org/10.1127/njgpa/219/2001/207			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000010
J	Brenner, WW; Biebow, N				Brenner, WW; Biebow, N			Missing autofluorescence of recent and fossil dinoflagellate cysts - an indicator of heterotrophy?	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Article							RECENT SEDIMENTS; MICROSCOPY; GROWTH	Epifluorescence investigations of recent and fossil dinoflagellate cysts assemblages show that several groups of cysts have no autofluorescence in neither the recent and the fossil record. Additional micro-absorption photometric investigations nor the different chemical behaviour confirm the assumption that the non-autofluorescing cysts differ in biomacromolecular composition from the sporopollenin/dinosporin of the autofluorescing cysts. No chemical similarity to the material of other non-autofluorescing or partly non-autofluorescing fossil organic-walled microfossils such as microforaminiferal linings, scolecodonts or fungal spores could be found. Based on the investigated Recent material and the known correlation of cysts and vegetative stage of dinoflagellates, the non-autofluorescing cysts seem to be associated with heterotrophic dinoflagellates. The possibly general heterotrophic nature of fossil non-fluorescing dinoflagellate cysts is discussed.	GEOMAR, D-24148 Kiel, Germany	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Brenner, WW (通讯作者)，GEOMAR, Wischhofstr 1-3, D-24148 Kiel, Germany.							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Jahrb. Geol. Palaontol.-Abh.	JAN	2001	219	1-2					229	240		10.1127/njgpa/219/2001/229	http://dx.doi.org/10.1127/njgpa/219/2001/229			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	399VL					2025-03-11	WOS:000166834000012
J	Blackburn, SI; Bolch, CJS; Haskard, KA; Hallegraeff, GM				Blackburn, SI; Bolch, CJS; Haskard, KA; Hallegraeff, GM			Reproductive compatibility among four global populations of the toxic dinoflagellate <i>Gymnodinium catenatum</i> (Dinophyceae)	PHYCOLOGIA			English	Article							DINOPHYCEAE; STRAINS; CYST; SEX	Reproductive compatibility was examined among 21 strains of Gymnodinium catenatum derived from four different populations from across the globe: Tasmania, Australia (15 strains), Japan (2 strains), Spain (2 strains) and Portugal (2 strains). Pairwise crossing of strains demonstrated extensive intrapopulation compatibility (to resting cyst formation) among all four populations. The observations were most consistent with a heterothallic. multiple-group mating system, requiring more than two groups to explain the pairwise crossing data. Despite the ability of strains from different populations to produce resting cysts, the viability of progeny was highly variable among interpopulation crosses. Cysts from all crosses showed a high germination percentage (93-100%) and released a swimming planomeiocyte. Crosses between different Tasmanian strains, and those between Spanish and Japanese strains, showed high post-meiotic viability (65% and 80%, respectively). However, progeny from Tasmanian-Spanish and Tasmanian-Japanese crosses showed very low post-meiotic viability (5-10%), indicating a higher level of somatic incompatibility between these populations. Significant differences in sexual life-history (e.g. rate of gamete formation and cyst dormancy) were also noted between interpopulation crosses, suggesting genetically determined strain- and population-level differences. The crossing data indicate a high level of mating diversity within the Australian population and show that the Japanese and Spanish populations are more closely related to each other than to Australian populations; this is supported by molecular studies. Implications for the proposed global dispersal of G. catenatum and the use of interbreeding to examine population relationships are discussed. New measures are proposed for examining strain (RC,) and population (RC,) levels of reproductive compatibility, respectively, which are calculated as the product of proportion of successful matings (termed the compatibility index) and the number of cysts produced (average vigour) in successful crosses.	CSIRO, Hobart, Tas 7001, Australia; Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia; BiometricsSA, S Australian Res & Dev Inst, Adelaide, SA 5001, Australia	Commonwealth Scientific & Industrial Research Organisation (CSIRO); University of Tasmania	CSIRO, GPO Box 1538, Hobart, Tas 7001, Australia.	susan.blackburn@marine.csiro.au; cjsb@dml.ac.uk	Blackburn, Susan/M-9955-2013; Bolch, Christopher/J-7619-2014; Hallegraeff, Gustaaf/C-8351-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343				AMMERMANN D, 1982, ARCH PROTISTENKD, V126, P373, DOI 10.1016/S0003-9365(82)80054-7; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; [Anonymous], 1976, EVOLUTION DIVERSITY; BALECH E., 1964, BOL INST BIOL MAR MAR DEL PLATA, V4, P1; Bell G., 1982, The Masterpiece of Nature: The Evolution and Genetics of Sexuality, DOI 10.4324/9780429322884; BINDER BJ, 1987, J PHYCOL, V23, P99; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLACKBURN SI, 1987, BRIT PHYCOL J, V22, P277, DOI 10.1080/00071618700650341; BOLCH CJ, 1998, HARMFUL MICROALGAE, P283; Bolch CJS, 1999, J PHYCOL, V35, P356, DOI 10.1046/j.1529-8817.1999.3520356.x; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; CAVALIERSMITH T, 1993, MICROBIOL REV, V57, P953, DOI 10.1128/MMBR.57.4.953-994.1993; COLEMAN AW, 1977, AM J BOT, V64, P361, DOI 10.2307/2441980; COLEMAN AW, 1975, J PHYCOL, V11, P282, DOI 10.1111/j.0022-3646.1975.00282.x; DESTOMBE C, 1990, PHYCOLOGIA, V29, P316, DOI 10.2216/i0031-8884-29-3-316.1; Dini Fernando, 1993, Advances in Microbial Ecology, V13, P85; 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; 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; ESSER K, 1965, INCOMPATIBILITY FUNG; ESTRADA M, 1984, INVEST PESQ, V48, P31; FUKUYO Y, 1993, DEV MAR BIO, V3, P875; Godhe Anna, 1996, Harmful Algae News, V15, P1; Goodenough U, 1985, ORIGIN EVOLUTION SEX, P123; GOODENOUGH U W., 1991, Microbial Cell-Cell Interactions, P71; 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; 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; Hoekstra R F, 1987, Experientia Suppl, V55, P59; ICHIMURA T, 1990, BIOL APPROACHES EVOL, P309; KASAI F, 1991, Journal of Phycology, V27, P37; LABARBERASANCHEZ A, 1993, DEV MAR BIO, V3, P281; LOEBLICH AR, 1975, J PHYCOL, V11, P80, DOI 10.1111/j.1529-8817.1975.tb02752.x; MACLEAN JL, 1989, MAR POLLUT BULL, V20, P304, DOI 10.1016/0025-326X(89)90152-5; McMinn A, 1997, MAR ECOL PROG SER, V161, P165, DOI 10.3354/meps161165; MENDEZ S, 1993, 6 INT C TOX MAR PHYT, P139; Nanney D.L., 1980, Experimental ciliatology: an introduction to genetic and developmental analysis in ciliates; OSHIMA Y, 1993, MAR BIOL, V116, P471, DOI 10.1007/BF00350064; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PROCTOR V W, 1975, Phycologia, V14, P97, DOI 10.2216/i0031-8884-14-2-97.1; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; Sonneborn T.M., 1957, SPECIES PROBLEM, P155; SONNEBORN TM, 1975, T AM MICROSC SOC, V94, P155, DOI 10.2307/3224977; Tagmouti F., 1995, 7 INT C TOX PHYT SEN, P40; Von Stosch HA., 1973, Br Phycol J, V8, P105; WATANABE MM, 1982, RES REP NATL I ENV S, V30, P27; WIESE L, 1983, AM NAT, V122, P806, DOI 10.1086/284173; WIESE L, 1977, AM NAT, V111, P733, DOI 10.1086/283202; YOSHIMATSU S, 1984, Bulletin of Plankton Society of Japan, V31, P107; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131	54	108	111	5	15	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	JAN	2001	40	1					78	87		10.2216/i0031-8884-40-1-78.1	http://dx.doi.org/10.2216/i0031-8884-40-1-78.1			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	443MT					2025-03-11	WOS:000169345500008
J	Zonneveld, KAF; Hoek, RP; Brinkhuis, H; Willems, H				Zonneveld, KAF; Hoek, RP; Brinkhuis, H; Willems, H			Geographical distributions of organic-walled dinoflagellate cysts in surficial sediments of the Benguela upwelling region and their relationship to upper ocean conditions	PROGRESS IN OCEANOGRAPHY			English	Review							SHORT-TERM VARIABILITY; CANONICAL CORRESPONDENCE-ANALYSIS; NORTHWESTERN INDIAN-OCEAN; RECENT MARINE-SEDIMENTS; ANCHOR STATION; ATLANTIC-OCEAN; SURFACE SEDIMENTS; LAST DEGLACIATION; NORTH-ATLANTIC; ADJACENT SEAS	The organic walled cyst content of 41 surface sediment samples from the south-eastern South Atlantic Ocean have been studied to create a dataset that can be used for palaeoceanographic reconstructions. In order to obtain insight into which environmental factors influence the distribution of individual cyst species, the cyst associations have been compared with oceanographic characteristics of the overlying water masses, i.e. temperature, salinity, density and stratification gradients. The associations and relationships have been established by Visual examination of the dataset and the multivariate ordination techniques, Detrended Correspondence Analysis and Canonical Correspondence Analysis. Special attention has been given to the factors of transport and preservation of the cysts. Five associations have been recognised as being characteristic of (1) areas influenced by coastal upwelling and/or river outflow, (2) open ocean, (3) Agulhas Current and southern Benguela Current, (4) Benguela Current and (5) Walvis Bay, shelf break area. The factors dominant in influencing either directly or indirectly the cyst distributions appear to be the stratification in the upper 50 m of the water column, nutrient concentration and seasonality. Variations in sea surface temperatures and salinities have only minor effect on cyst distribution. (C) 2001 Elsevier Science Ltd. All rights reserved.	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Oceanogr.		2001	48	1					25	72		10.1016/S0079-6611(00)00047-1	http://dx.doi.org/10.1016/S0079-6611(00)00047-1			48	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	396WF					2025-03-11	WOS:000166659900002
J	Tripathi, A				Tripathi, A			Permian, Jurassic and Early Cretaceous palynofloral assemblages from subsurface sedimentary rocks in Chuperbhita Coalfield, Rajmahal Basin, India	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynodating; Permian; Jurassic; Early Cretaceous; Rajmahal Basin; India		The results of a palynological analysis of the sedimentary sequence of Borehole RCH-151, Chuperbhita Coalfield, Rajmahal Basiri, Bihar are presented here. The borehole penetrated the Rajmahal Formation (comprising two traps sandwiching an intertrappean bed), the thinly represented Dubrajpur Formation and in its lower part, the Coal Measures. The coal-bearing interval is associated with Scheuringipollenites barakarensis, Faunipollenites varius, Densipollenites indicus, Gondisporites raniganjensis and Densipollenites magnicorpus Assemblage Zones. The presence of these biostratigraphic units indicates correlation with the Barakar Formation (Early Permian) and the Barren Measures and Raniganj Formations (both Late Permian). This is the first record, in the Chuperbhita Coalfield, of Late Permian strata, which appear to represent a condensed sequence. Prior to the present study, the Permian succession was thought to have been associated entirely with the Barakar Formation. The overlying Dubrajpur Formation yielded a distinct spore-pollen assemblage (in association with the first report of dinoflagellate, Phallocysta), which is assigned to the newly identified Callialasporites turbatus palynozone of latest Early to early Middle Jurassic age. The diverse spore-pollen flora of the intertrappean bed (Rajmahal Formation) incorporates several age marker taxa, viz. Undulatisporites, Leptolepidites, Klukisporites, Ruffordiaspora, and Coptospora. The assemblages from intertrappean beds are correlated with the Ruffordiaspora australiensis palynozone of Australia. Thus the palynodating indicates Permian, latest Early to early Mid-Jurassic and Early Cretaceous age for the strata studied. This is the first record of definite jurassic microfossils from the non-marine sequence of Rajmahal Basin, India. (C) 2001 Elsevier Science B.V. All rights reserved.	Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Tripathi, A (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.							[Anonymous], 1992, PALAEOBOTANIST; [Anonymous], 1987, ASS AUSTRALASIAN PAL; Baksi A.K., 1992, S MES MAGM E MARG IN, P16; BANERJEE M, 1990, REV PALAEOBOT PALYNO, V65, P239, DOI 10.1016/0034-6667(90)90074-S; Banerjee M., 1988, J PALAEONTOL SOC IND, V33, P73; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; BURGER D, 1990, 198938 BUR MIN RES; BURGER D, 1990, 198939 BUR MIN RES; BURGER D, 1996, AUSTR PHANEROZOIC TI, P160; BURGER D, 1995, 2 SERIES BUR MINERAL; Dettmann M.E, 1986, ASS AUSTR PALAEONTOL, V3, P79; Jain KP., 1984, Journal of the Palaeontological Society of India, V29, P67; KOSHAL V.N., 1975, Quart. Jour. Geol. Min. Metal. Soc, V47, P79; Kumar P., 1990, PALEOBOTANIST, V37, P367; Lentin J.K., 1989, American Association of Stratigraphic Palynologists Contributions Series, V20, P1; MAHESHWARI HK, 1983, P S CRET IND PAL PAL, P158; NORRIS G., 1969, PALAEONTOLOGY, V12, P574; NORRIS G, 1973, P 3 INT PAL C PAL ME; PRABHAKAR M, 1989, P 12 IND C MICR STRA, P50; Quattrocchio ME, 1996, GEORES FORUM, V1&2, P167; Raja Rao CS., 1987, B GEOL SURV INDIA A, V45, P300; RAMANUJAM CGK, 1993, GONDWANA GEOL MAG SP, P462; Sah SCD., 1965, Palaeobotanist, V13, P264, DOI [10.54991/jop.1964.702, DOI 10.54991/JOP.1964.702]; Schrank E, 1998, J AFR EARTH SCI, V26, P167, DOI 10.1016/S0899-5362(98)00004-9; Singh H.P., 1988, J. Palaeosci., V36, P168; SRIVASTAVA S. K., 1966, MICROPALENTOLOGY, V12, P87, DOI 10.2307/1484541; SRIVASTAVA SK, 1987, GEOBIOS-LYON, V20, P5, DOI 10.1016/S0016-6995(87)80057-8; Stover L.E., 1987, AM ASS STRATIGRAPHIE, V18, P1; TIWARI R S, 1974, Geophytology, V4, P111; Tiwari R. S., 1984, P 5 IND GEOPH C LUCK, P207; Tiwari RS, 1996, REV PALAEOBOT PALYNO, V94, P169, DOI 10.1016/0034-6667(95)00112-3; TIWARI RS, 1995, CRETACEOUS RES, V16, P53, DOI 10.1006/cres.1995.1004; Tiwari RS., 1988, PALEOBOTANIST, V36, P87; Traverse A., 1988, Palaeopalynology; TRIPATHI A, 2000, IN PRESS P NAT SEM R; Vijaya, 1997, CRETACEOUS RES, V18, P833, DOI 10.1006/cres.1997.0090; Vijaya, 1997, CRETACEOUS RES, V18, P37, DOI 10.1006/cres.1996.0048	37	22	27	0	6	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2001	113	4					237	259		10.1016/S0034-6667(00)00062-2	http://dx.doi.org/10.1016/S0034-6667(00)00062-2			23	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	423FR	11179715				2025-03-11	WOS:000168165200002
J	Kouli, K; Brinkhuis, H; Dale, B				Kouli, K; Brinkhuis, H; Dale, B			<i>Spiniferites</i> <i>cruciformis</i>:: a fresh water dinoflagellate cyst?	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellates; late Quaternary; lacustrine sediments; Greece	AEGEAN SEA	Palynological studies of cored lacustrine sediments from the late Quaternary of Lake Kastoria, northern Greece, revealed a Late Glacial interval with abundant dinoflagellate cysts. Cyst assemblages include two identifiable species, Spiniferites cruciformis and Gonyaulax apiculata. The presence of the fresh water species G. apiculata is consistent with the lacustrine setting of these deposits, but that of S. cruciformis is anomalous. Previously, this species has only been recorded in abundance from presumed brackish marine sediments from the Black Sea and Marmara Sea sediments where geochemical data clearly record brackish salinities. Therefore, it has been regarded as a low salinity cyst type with a wide range of morphological variation that some workers have suggested to reflect salinity fluctuations. Specimens from Greece display only part of the range of morphological variability previously described from these (brackish) marine settings. Encountered morphological variation includes ellipsoidal/pentameral and cruciform endocyst shapes with rare intermediate shapes, and highly variable septa development. Specimens characterized by extremely reduced ornamentation known from (brackish) marine environments have not been recorded. Our records of S. cruciformis indicate that: (1) it could thrive in fresh water conditions; and (2) that apparently most of the strong morphological variations of the cysts are an intrinsic phenomenon for this taxon, and may only partly be linked to salinity variations as suggested earlier. We suggest that S. cruciformis essentially is a fresh water taxon, and that its records in (brackish) marine environments, with the exception of specimens with strongly reduced ornamentation, may be due to transportation, to short-lived fresh water surface conditions in such environments, or to tolerance of the species to brackish conditions. (C) 2001 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Athens, Dept Hist Geol & Paleontol, GR-15784 Athens, Greece; Univ Oslo, Dept Geol, N-0316 Oslo, Norway	Utrecht University; National & Kapodistrian University of Athens; University of Oslo	Brinkhuis, H (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Brinkhuis, Henk/B-4223-2009; Kouli, Katerina/M-8243-2013	Brinkhuis, Henk/0000-0003-0253-6610; Kouli, Katerina/0000-0003-1656-1091				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; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; ANAGNOSTIDIS K, 1980, ARCH HYDROBIOL, V89, P313; Bottema S., 1974, THESIS GRONINGEN; BOURRELLY P, 1980, Cryptogamie Algologie, V1, P161; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; EVITT WR, 1985, REV PALAEOBOT PALYNO, V45, P35, DOI 10.1016/0034-6667(85)90064-8; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; HICKEL B, 1986, ARCH HYDROBIOLOGIE S, V72, P227; HUBERPESTALOZZI G, 1968, BINNENGEWASSER, V16, P1; KOULI K, 1999, P 5 C HELL GEOGR SOC, P439; Koussouris Th., 1987, GeoJournal, V14, P377, DOI 10.1007/BF00208214; MUDIE PJ, 1998, NTNU VITENSK MUS RAP, P116; MUDIE PJ, 2000, MAR MICROPALEONTOL; OVERBECK J, 1982, ARCH HYDROBIOL, V95, P365; Panagos A., 1989, ANN GEOLOGIQUES PAYS, V34, P105; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Vafeiadis P., 1983, THESIS ARISTOTELIAN; VANHOEVE ML, 1998, NTNU VITENSK MUS RAP, P68; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; Wall D., 1973, Geoscience Man, V7, P95; Wall D., 1974, BLACK SEA GEOLOGY CH, V20, P364, DOI [10.1306/m20377c3, DOI 10.1306/M20377C3]	23	64	67	0	3	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN	2001	113	4					273	286		10.1016/S0034-6667(00)00064-6	http://dx.doi.org/10.1016/S0034-6667(00)00064-6			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	423FR	11179717				2025-03-11	WOS:000168165200004
J	Boucsein, B; Fahl, K; Stein, R				Boucsein, B; Fahl, K; Stein, R			Variability of river discharge and Atlantic-water inflow at the Laptev Sea continental margin during the past 15,000 years: implications from maceral and biomarker records	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						organic-carbon source; organic petrology; biomarker Arctic Ocean; Laptev Sea; Last Glacial Holocene; Termination 1	ORGANIC-MATTER; ARCTIC-OCEAN; LENA RIVER; SEDIMENTATION-RATE; MARINE-SEDIMENTS; SIBERIA; PRODUCTIVITY; HOLOCENE; ELEMENTS; PHYTOPLANKTON	In order to reconstruct the depositional environment from the Laptev Sea continental slope and shelf during the past similar to 15,000 years BP maceral analysis was carried out on two sediment cores (PS2458-4, PS2725-5) and compared with organic-geochemical parameters. During the transition from the Last Glacial to the Holocene the environment of the Laptev Sea shelf was controlled by the post-glacial sea level rise, variations in river discharge, surface-water productivity, and Atlantic-water inflow along the EUrasian continental margin. Based on our results, we identify the following significant changes of the environment: (a) at approximately 13,500 years BP the first step of deglaciation (Termination 1a) is documented by the deposition of marine and fresh-water organic matter; (b) at approximately 10,400 years BP the first post-glacial influence of Atlantic-water inflow along the Eastern Laptev Sea continental margin is indicated by an increase in marine organic matter; (c) at the beginning of the Holocene an increased fluvial supply is documented by an increase in fresh-water alginite; and (d) since similar to 9500-8000 years BP modern marine conditions are established at the Laptev Sea continental margin as documented in increased amounts of marine macerals, biomarkers (dinosterol, brassicasterol, short-chain fatty acids), and dinoflagellate cysts.	Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Boucsein, B (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr,POB 120161, D-27515 Bremerhaven, Germany.			Stein, Ruediger/0000-0002-4453-9564; Fahl, Dr., Kirsten/0000-0001-9317-4656				[Anonymous], ADV PETROLEUM GEOCHE; [Anonymous], 1999, LAND OCEAN SYSTEMS S; [Anonymous], J GEOPHYS RES; Bauch HA, 1999, BOREAS, V28, P194, DOI 10.1111/j.1502-3885.1999.tb00214.x; Behrends M, 1999, REP POLAR RES, V310, P1; Behrends M., 1999, LAND OCEAN SYSTEMS S, P265, DOI [10.1007/978-3-642-60134-7_24, DOI 10.1007/978-3-642-60134-7_24]; BERGER AL, 1978, QUATERNARY RES, V9, P139, DOI 10.1016/0033-5894(78)90064-9; BERGER WH, 1989, LIFE SCI RES REPORT, V44, P471; Boetius A, 1998, DEEP-SEA RES PT I, V45, P239, DOI 10.1016/S0967-0637(97)00052-6; Boetius A., 1996, SURFACE SEDIMENT COM, V212, P213; Boucsein B, 2000, MAR GEOL, V162, P573, DOI 10.1016/S0025-3227(99)00066-3; Cremer H., 1999, Land-Ocean Systems in the Siberian Arctic, P533; DUNAYEV NN, 1988, ARCTIC RES ADV PROSP, V2, P70; EMERSON S, 1985, DEEP-SEA RES, V32, P1, DOI 10.1016/0198-0149(85)90014-7; Fahl K, 1999, MAR CHEM, V63, P293, DOI 10.1016/S0304-4203(98)00068-1; Fahl K, 1997, ORG GEOCHEM, V26, P379, DOI 10.1016/S0146-6380(97)00007-7; FAIRBANKS RG, 1989, NATURE, V342, P637, DOI 10.1038/342637a0; FUTTERER DK, 1994, REP POLAR RES, V149, P1; Gordeev VV, 1996, AM J SCI, V296, P664, DOI 10.2475/ajs.296.6.664; Hahne J, 1997, VEG HIST ARCHAEOBOT, V6, P1, DOI 10.1007/BF01145880; Hald M, 1999, PALAEOGEOGR PALAEOCL, V146, P229, DOI 10.1016/S0031-0182(98)00133-3; Heiskanen AS, 1996, MAR CHEM, V53, P229, DOI 10.1016/0304-4203(95)00091-7; HOLEMANN JA, 1994, MAR GEOL, V121, P87, DOI 10.1016/0025-3227(94)90159-7; Holmes M.L., 1974, MARINE GEOLOGY OCEAN, P211, DOI DOI 10.1007/978-3-642-87411-6_9; Khotinsky NA, 1997, QUATERN INT, V41-2, P67, DOI 10.1016/S1040-6182(96)00038-9; Kleiber H.P., 1999, LAND OCEAN SYSTEMS S, P657; KUNZPIRRUNG M, 1998, REP POLAR RES, V281, P1; Kuptsov VM, 1996, MAR CHEM, V53, P301, DOI 10.1016/0304-4203(95)00096-8; KUZIMA S, 1999, REP POLAR RES, V315, P179; Lara RJ, 1998, MAR CHEM, V59, P301, DOI 10.1016/S0304-4203(97)00076-5; LEGENDRE L, 1992, POLAR BIOL, V12, P429; Leveille JC, 1997, J PLANKTON RES, V19, P469, DOI 10.1093/plankt/19.4.469; Lindemann F., 1998, REP POLAR RES, V283, P1; MARTIN JM, 1993, MAR CHEM, V43, P185, DOI 10.1016/0304-4203(93)90224-C; MATTHIESSEN J, 2000, INT J EARTH SCI; Monserud RA, 1998, PALAEOGEOGR PALAEOCL, V139, P15, DOI 10.1016/S0031-0182(97)00127-2; MULLER C, 1999, REP POLAR RES, V329, P1; MULLER C, 2000, INT J EARTH SCI; MULLER PJ, 1979, DEEP-SEA RES, V26, P1347, DOI 10.1016/0198-0149(79)90003-7; PEDERSEN TF, 1990, AAPG BULL, V74, P454; Peregovich B, 1999, BOREAS, V28, P205, DOI 10.1111/j.1502-3885.1999.tb00215.x; Rachold V., 1999, Land-Ocean Systems in the Siberian Arctic, P223, DOI DOI 10.1007/978-3-642-60134-7_21; Rachor E., 1997, Reports on Polar and Marine Research, V226, P1; SPIELHAGEN RF, 1996, QUAT ENV EUR N QUEEN; Stach E., 1982, STACHS TXB COAL PETR, P535; STEIN R, 1990, GEO-MAR LETT, V10, P37, DOI 10.1007/BF02431020; Stein R, 2000, GEO-MAR LETT, V20, P27, DOI 10.1007/s003670000028; Stein R, 1991, LECT NOTES EARTH SCI, V34, P217; Stein R., 1999, LAND OCEAN SYSTEMS S, P635; Stromberg J.-O., 1989, P402; Taylor G., 1998, GEOL MAG, DOI DOI 10.1017/S0016756899463320; VANANDEL TH, 1975, GEOL SOC AM MEM, V143, P134; Velichko AA, 1997, QUATERN INT, V41-2, P71, DOI 10.1016/S1040-6182(96)00039-0; WAGNEXR T, 1994, MAR GEOL, V120, P335, DOI 10.1016/0025-3227(94)90066-3; Welte D.H., 1984, PETROLEUM FORMATION; WIESNER MG, 1990, ORG GEOCHEM, V15, P419, DOI 10.1016/0146-6380(90)90169-Z	56	14	16	1	7	SPRINGER-VERLAG	NEW YORK	175 FIFTH AVE, NEW YORK, NY 10010 USA	1437-3254			INT J EARTH SCI	Int. J. Earth Sci.	DEC	2000	89	3					578	591		10.1007/s005310000111	http://dx.doi.org/10.1007/s005310000111			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	385TW					2025-03-11	WOS:000166020600014
J	Marshall, HG; Gordon, AS; Seaborn, DW; Dyer, B; Dunstan, WM; Seaborn, AM				Marshall, HG; Gordon, AS; Seaborn, DW; Dyer, B; Dunstan, WM; Seaborn, AM			Comparative culture and toxicity studies between the toxic dinoflagellate <i>Pfiesteria piscicida</i> and a morphologically similar cryptoperidiniopsoid dinoflagellate	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						Pfiesteria piscicida; Cryptoperidiniopsis gen. nov.; toxicity; dinoflagellates	ESTUARINE DINOFLAGELLATE; PHANTOM DINOFLAGELLATE; FISH KILLS; PHAGOTROPHY; IMPACTS; COMPLEX; RIVER	A series of fish bioassays using cultures of the toxic dinoflagellate, Pfiesteria piscicida and a cryptoperidiniopsoid dinoflagellate indicated various degrees of toxicity for Pfiesteria piscicida and no toxicity by the cryptoperidiniopsoid. P. piscicida maintained toxicity in the presence of live fish, and this toxicity was perpetuated following a series of inoculations to other culture vessels. Differences in the onset and magnitude of the fish deaths occurred, requiring 16 days for the initial fish death when using P. piscicida from a culture that had previously been maintained on algal cells, to kills within hours when using a culture that had recently (previous day) killed fish. Autopsies of moribund fish from the test and control fish bioassays indicated a general lack of bacterial infection, which ensued following death of other autopsied fish. Moreover, bacterial comparisons of waters in the fish bioassay and control fish cultures indicated that similar bacterial concentrations were present. Neither oxygen or ammonia levels were determined to be factors in the fish death. Life stages of a cryptoperidiniopsoid dinoflagellate from Virginia estuaries were also identified, including motile zoospore, gametes, planozygote, amoebae, and cyst stages. The cryptoperidiniopsioid did not initiate fish deaths in bioassays conducted over a 14-week period at zoospore concentrations of ca. 700-800 cells ml(-1). Elemental X-ray analysis of the scales from cysts of this dinoflagellate and P. piscicida indicate that they both contain silicon. Overall, the data from this study demonstrate that the cryptoperidiniopsoid possesses several similar life stages and feeding patterns as P. piscicida, but was not toxic to fish. (C) 2000 Elsevier Science B.V. All rights reserved.	Old Dominion Univ, Dept Biol Sci, Norfolk, VA 23529 USA; Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, Norfolk, VA 23529 USA	Old Dominion University; Old Dominion University	Old Dominion Univ, Dept Biol Sci, Norfolk, VA 23529 USA.							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A., 1999, Virginia Journal of Science, V50, P325; SCHNEPF E, 1992, EUR J PROTISTOL, V28, P3, DOI 10.1016/S0932-4739(11)80315-9; Seaborn David W., 1999, Virginia Journal of Science, V50, P337; SPERO HJ, 1982, J PHYCOL, V18, P356, DOI 10.1111/j.1529-8817.1982.tb03196.x; Steidinger KA, 1996, J PHYCOL, V32, P157, DOI 10.1111/j.0022-3646.1996.00157.x; Steidinger Karen A., 1995, P83; Steidinger Karen A., 1993, P1; Tomas C.R., 1996, IDENTIFYING MARINE D, P598; Truby EW, 1997, MICROSC RES TECHNIQ, V36, P337; *WOODS HOL OC INST, 2000, GLOSSARY PFIESTERIA	47	50	54	0	6	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0022-0981	1879-1697		J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	DEC 1	2000	255	1					51	74		10.1016/S0022-0981(00)00288-4	http://dx.doi.org/10.1016/S0022-0981(00)00288-4			24	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	379KA	11090852				2025-03-11	WOS:000165640200004
J	Palliani, RB; Riding, JB				Palliani, RB; Riding, JB			Subdivision of the dinoflagellate cyst Family Suessiaceae and discussion of its evolution	JOURNAL OF MICROPALAEONTOLOGY			English	Article							ZOOXANTHELLAE	The recent description of Umbriadinium mediterraneense Bucefalo Palliani & Riding 1997 from the Early Jurassic of central Italy and Greece has provided new information on the phylogeny of the dinoflagellate cyst Family Suessiaceae. On the basis of the morphology of the five suessiacean genera, a subdivision of the family into two new subfamilies is proposed. These are the Late Triassic Suessioideae and the Early Jurassic Umbriadinoideae. The evolution of the Family Suessiaceae is related to the evolution of scleractinian corals, largely on the basis of the similarity of their evolutionary patterns and geographical palaeodistributions.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy; British Geol Survey, Keyworth NG12 5GG, Notts, England	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Palliani, RB (通讯作者)，Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy.							[Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1987, ASS AUSTRALASIAN PAL; BEAUVAIS L, 1986, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V194, P1; BEAUVAIS L, 1984, PALAEONTOGRAPHICA AM, V54, P219; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Bown Paul R., 1992, Journal of Micropalaeontology, V11, P177; BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; Davies E.H., 1983, GEOLOGICAL SURVEY CA, V359; DORHOFER G, 1980, ROYAL ONTARIO MUSEUM; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FISHER M J, 1979, Palynology, V3, P265; FLUGEL E, 1996, CARBONATES GLOBAL CH, P54; FLUGEL E, 1994, 288 GEOL SOC AM, P247; Hallam A, 1996, GEOL SOC SPEC PUBL, V102, P231, DOI 10.1144/GSL.SP.1996.001.01.16; HALLAM A, 1990, GEOL SOC AM SPEC PAP, V247, P577; HARLAND R, 1975, Palaeontology (Oxford), V18, P847; KRASIMOV EV, 1984, PALAEONTOGRAPHICA AM, V54, P225; LOEBLICH AR, 1979, J MAR BIOL ASSOC UK, V59, P195, DOI 10.1017/S0025315400046270; Morbey J., 1975, Palaeontographica B, V152, P1; Morbey S.J., 1978, Palinologia numero extraordinario, V1, P355; Newell N. D., 1971, American Mus Novit, VNo. 2465, P1; Palliani Raffaella Bucefalo, 1997, Palynology, V21, P197; PALLIANI RB, 1996, THESIS U PERUGIA ITA; Poulsen N. E., 1996, AM ASS STRATIGRAPHIC, V31; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; ROWAN R, 1991, SCIENCE, V251, P1348, DOI 10.1126/science.251.4999.1348; SCHUURMAN WML, 1979, REV PALAEOBOT PALYNO, V27, P53, DOI 10.1016/0034-6667(79)90044-7; STANLEY G D JR, 1988, Palaios, V3, P170; STANLEY GD, 1981, GEOLOGY, V9, P507, DOI 10.1130/0091-7613(1981)9<507:EHOSCA>2.0.CO;2; STANLEY GD, 1995, PALEOBIOLOGY, V21, P179, DOI 10.1017/S0094837300013191; STANLEY GD, 1992, ENCY EARTH SYSTEM SC, V4, P375; Talent J.A., 1988, Senckenbergiana Lethaea, V69, P315	32	10	11	0	3	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	DEC	2000	19		2				133	137		10.1144/jm.19.2.133	http://dx.doi.org/10.1144/jm.19.2.133			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	385UJ		hybrid			2025-03-11	WOS:000166021900004
J	Courtinat, B				Courtinat, B			Review of the dinoflagellate cyst <i>Subtilisphaera</i>? <i>inaffecta</i> (Drugg, 1978) Bujak & Davies, 1983 and <i>S</i>.? <i>paeminosa</i> (Drugg, 1978) Bujak & Davies, 1983	JOURNAL OF MICROPALAEONTOLOGY			English	Article								Research carried out on the Upper Jurassic dinoflagellate cyst assemblages of the SubTethyan marine realm, show that populations of the dinoflagellate cysts Subtilisphaera? inaffecta and S.? paeminosa are predominant in shallow water marginal marine or brackish environments. The distribution of groups of dinoflagellate cysts, micrhystridid acritarchs and variations of terrestrial inputs represented by phytoclasts are presumed parameters of the salinity balance during such Late Jurassic depositional environments. In this context, the shagreenate to faintly granulate S.? inaffecta appears to be an opportunistic taxon with an ability to prosper in brackish environments. In contrast, the coarsely granulate to pustulate paeminosa form is seemingly less eurytopic and flourishes with success in shallow, marginal marine, environments. SEM studies reveals that the two morphotypes possess transapical archaeopyle sutures on what is usually considered the antapex. Following these observations the cysts are interpreted in a reverse sense. Consequently, the attribution to the genus Subtilisphaera becomes inappropriate. The two morphotypes, interpreted as variants of a single species, are attributed to the genus Corculodinium Batten & Lister, 1988 for which a new emendation is proposed. The specific epithet inaffecta is considered legal over paeminosa.	Univ Lyon 1, UFR Sci Terre, F-69622 Villeurbanne, France	Universite Claude Bernard Lyon 1	Courtinat, B (通讯作者)，Univ Lyon 1, UFR Sci Terre, 43 Bd 11 Novembre 1918, F-69622 Villeurbanne, France.							BARON H, 1989, NW EUROPEAN MICROPAL, P193; 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; Bernier P., 1979, DOCUM LAB G OL FS LY, V75, P95; BIRD D F, 1992, Journal of Phycology, V28, P16; BRENNER W., 1988, Tubinger Mikropalaontologische Mitteilungen, V6, P1; Bujak J.P., 1983, AM ASS STRATIGRAPHIE, V13, P1; Courtinat B., 1989, Documents des Laboratoires de Geologie de la Faculte des Sciences de Lyon, V105, P1; COX BM, 1987, GEOLOGICAL SOC LONDO, V55, P169; DODEKOVA L, 1992, Geologica Balcanica, V22, P33; Dodekova Lilia, 1994, Geologica Balcanica, V24, P11; DOWNIE CHARLES, 1957, QUART JOUR GEOL SOC LONDON, V112, P413; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; DURR G, 1988, TUBINGER MIKROPALAON, V5, 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; Feist-Burkhardt S, 1996, 9 INT PAL C 23 28 JU, P42; Fisher M.J., 1980, P 4 INT PAL C LUCHN, V2, P313; GITMEZ G U, 1972, Bulletin of the British Museum (Natural History) Geology, V21, P173; Gitmez G.U., 1970, B BRIT MUS NAT HIST, V18, P233; Ioannides N.S., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P471; IOANNIDES N S, 1976, Micropaleontology (New York), V22, P443, DOI 10.2307/1485174; Jain K.P., 1973, PALAEOBOTANIST, V20, P22; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; Lentin J.K., 1985, CAN TECH REP HYDROG, V60, P1; LENTIN JK, 1976, BIR7516 BEDF I OC RE, P1; LORD AR, 1987, NEUES JB GEOLOGIE PA, P577; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; NORHHANSEN H, 1986, GEOLOGICAL SOC DENMA, V35, P31; POULSEN N.E., 1996, American Association of Stratigraphic Palynologists, Contribution Series, V31, P1; Poulsen N.E., 1994, GEOBIOS, V7, P409; POULSEN NE, 1992, REV PALAEOBOT PALYNO, V75, P33, DOI 10.1016/0034-6667(92)90148-A; POULSEN NE, 1991, GEOLOGICAL SURVEY B, V16, P7; POULSEN NE, 1994, GEOBIOS, V17, P401; Poulsen Niels E., 1993, Acta Geologica Polonica, V43, P251; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Raynaud J.F., 1978, Palinologia, numero extraordinario, V1, P387; Riding J.B., 1992, P7; RIDING J B, 1988, Palynology, V12, P65; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Schrank E, 1984, BERL GEO ABH, V50, P189; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; WOOLLAM R, 1983, 832 I GEOL SCI REP, P1	45	9	10	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.	DEC	2000	19		2				165	175		10.1144/jm.19.2.165	http://dx.doi.org/10.1144/jm.19.2.165			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	385UJ		hybrid			2025-03-11	WOS:000166021900009
J	Rubino, F; Belmonte, G; Miglietta, AM; Geraci, S; Boero, F				Rubino, F; Belmonte, G; Miglietta, AM; Geraci, S; Boero, F			Resting stages of plankton in recent North Adriatic sediments	MARINE ECOLOGY-PUBBLICAZIONI DELLA STAZIONE ZOOLOGICA DI NAPOLI I			English	Article						North Adriatic Sea; dinoflagellates; resting stages; cyst bank	DINOFLAGELLATE CYSTS; GYMNODINIUM-CATENATUM; MARINE-SEDIMENTS; COASTAL WATERS; SP-NOV; VERTICAL-DISTRIBUTION; MICRORETICULATE CYST; CALANOID COPEPOD; EGGS; DINOPHYCEAE	Plankton-derived resting stages were found in 26 sediment cores collected in the North Adriatic Sea; 46 morphotypes were identified, 38 were attributed to taxa according to their morphology and, in some hatching cases, also according to the morphology of the derived active forms. Six species of Dinophyta were recorded for the first time from the North Adriatic Sea. Each morphotype was described in detail. Twenty-nine resting stages were Dinophyta; one was a Chrysophyta; two were Tintinnina; and six were metazoans. At every site Dinophyta cysts were more abundant than Metazoa cysts. Cyst bank densities were variable, with empty forms generally more abundant than full ones; cyst concentrations were highest at the mouth of the Po River delta.	Univ Lecce, Dipartimento Biol, Stn Biol Marina, I-73100 Lecce, Italy; CNR, Ist Sperimentale Talassograf A Cerruti, I-74100 Taranto, Italy; CNR, Ist Corros Marina Met, I-16149 Genoa, Italy	University of Salento; Consiglio Nazionale delle Ricerche (CNR); Consiglio Nazionale delle Ricerche (CNR)	Boero, F (通讯作者)，Univ Lecce, Dipartimento Biol, Stn Biol Marina, Via Prov Monteroni, I-73100 Lecce, Italy.	boero@unile.it	Boero, Ferdinando/B-4494-2008; Rubino, Fernando/GOP-0332-2022; BELMONTE, GENUARIO/AAG-4029-2020	Rubino, Fernando/0000-0003-2552-2510; Boero, Ferdinando/0000-0002-6317-2710				ANDERSON DM, 1988, J PHYCOL, V24, P255; ANGELANTONI A, 1978, PUBBL I GEOL MAR CNR, V9, P79; [Anonymous], NOVA HEDWIGIA; [Anonymous], GIORNALE BOT ITALIAN; ANTIA AN, 1993, J PLANKTON RES, V15, P99, DOI 10.1093/plankt/15.1.99; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Belmonte G, 1997, CRUSTACEANA, V70, P114, DOI 10.1163/156854097X00401; Belmonte G, 1995, OLSEN INT S, P53; BELMONTE G, 1992, B ZOOL, V59, P363, DOI 10.1080/11250009209386694; BELMONTE G, 1998, BIOL MAR MEDIT, V6, P172; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; BOERO F, 1994, MAR ECOL-P S Z N I, V15, P3, DOI 10.1111/j.1439-0485.1994.tb00038.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bolch CJS, 1999, PHYCOLOGIA, V38, P301, DOI 10.2216/i0031-8884-38-4-301.1; BROS WE, 1987, J EXP MAR BIOL ECOL, V114, P63; CRUZADO A, 1990, P WORKSH EUTR REL PH, P193; Dale B., 1983, P69; DUFF KE, 1995, ATLAS CHRYSOPHYCEAN; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; Fonda Umani S., 1985, Oebalia, V11, P141; FONDAUMANI S, 1991, MARINE EUTROPHICATIO, P347; GAO XP, 1991, BRIT PHYCOL J, V26, P21, DOI 10.1080/00071619100650031; GARRISON DL, 1984, MARINE PLANKTON LIFE, P19; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Head M.J., 1996, Palynology: Principles and Applications, P1197; Kobayashi S., 1984, Japanese Journal of Phycology (Sorui), V32, P251; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Lewis J., 1984, Journal of Micropalaeontology, V3, P25; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; LINDLEY JA, 1990, MAR BIOL, V104, P209, DOI 10.1007/BF01313260; Madhupratap M, 1996, MAR BIOL, V125, P77, DOI 10.1007/BF00350762; MARCHETTI R, 1990, P WORKSH EUTR REL PH, P21; MARCUS NH, 1990, MAR BIOL, V105, P413, DOI 10.1007/BF01316312; MARCUS NH, 1995, MAR BIOL, V123, P459, DOI 10.1007/BF00349225; MARCUS NH, 1994, LIMNOL OCEANOGR, V39, P154, DOI 10.4319/lo.1994.39.1.0154; Marcus NH, 1998, LIMNOL OCEANOGR, V43, P763, DOI 10.4319/lo.1998.43.5.0763; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; MATSUOKA K, 1982, REV PALAEOBOT PALYNO, V38, P109, DOI 10.1016/0034-6667(82)90052-5; Matsuoka K., 1985, NATURAL SCI B, V25, P21; MCQUOID MR, 1995, J PHYCOL, V31, P44, DOI 10.1111/j.0022-3646.1995.00044.x; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; 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; OTT JA, 1992, OLSEN INT S, P367; Ott Jorg A., 1995, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V15, P133; PAGNOTTA R, 1990, WATER POLLUTION RES, P115; Pati AC, 1999, MAR BIOL, V134, P419, DOI 10.1007/s002270050558; Reid P.C., 1974, Nova Hedwigia, V25, P579; REID PC, 1978, J MAR BIOL ASSOC UK, V58, P551, DOI 10.1017/S0025315400041205; Rubino F., 1998, BIOL MAR MEDIT, V5, P253; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; VIITASALO M, 1994, MAR BIOL, V120, P455, DOI 10.1007/BF00680221; Vollenweider R.A., 1992, MARINE COASTAL EUTRO, P63; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	58	35	40	0	15	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0173-9565			MAR ECOL-P S Z N I	Mar. Ecol.-Pubbl. Stn. Zool. Napoli	DEC	2000	21	3-4					263	284		10.1046/j.1439-0485.2000.00725.x	http://dx.doi.org/10.1046/j.1439-0485.2000.00725.x			22	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	385KM					2025-03-11	WOS:000166003300007
J	Matsuoka, K; Cho, HJ				Matsuoka, K; Cho, HJ			Morphological variation in cysts of the gymnodinialean dinoflagellate <i>Polykrikos</i>	MICROPALEONTOLOGY			English	Article							RECENT SEDIMENTS	On the basis of both a literature survey and incubation experiments, the cyst-motile form relationship in the two Polykrikos species (Dinophyceae), P. schwartzii and P. kofoidii, must be reassessed. Surface ornamentation of the cysts of P. schwartzii and P. kofoidii has been considered the most important morphological feature differentiating these species. The cyst of P. schwartzii has been considered to be characterized by reticulate ornament, and that of P. kofoidii by separate, rod-like processes. In our incubation experiments, P. kofoidii produced a cyst covered with complete reticulate ornament; this species also germinated from a cyst with incomplete reticulate ornament. We found four morphological types of Polykrikos cysts in the surface sediments of Omura Bay. The ornament varied from rod-like elements (Type 1), to separate rows of lumina (Spe 2), shelf-like ornament with incomplete reticulum (Type 3), to a complete reticulum (Type 4). Our observations show that cysts of P. kofoidii have not only variants with rod-like processes, but also forms with a reticulate network, and that intermediate forms sometimes occur. In particular, the presence of intermediate forms strongly suggests that a separator based on the surface ornament of cysts is not effective for differentiating these two species. Therefore, the taxonomic criterion that cysts with reticulate ornament are identical to P. schwartzii and those with rod-like form to P. kofoidii, is considered untenable.	Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan; Nagasaki Univ, Grad Sch Marine Sci & Engn, Nagasaki 8528521, Japan	Nagasaki University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.							DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DODGE J, 1982, MARINE DINOFLAGELLAT, P120; FUKUYO Y, 1981, FUNDAMENTAL STUDIES, P205; HARLAND R, 1981, Palynology, V5, P65; KOFOID CA, 1921, FREE LIVING UNARMORE, P395; Kokinos John P., 1995, Palynology, V19, P143; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; Matsuoka K., 1989, P461; MOREYGAINES G, 1980, PHYCOLOGIA, V19, P230, DOI 10.2216/i0031-8884-19-3-230.1; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; REID PC, 1978, NEW PHYTOL, V80, P219, DOI 10.1111/j.1469-8137.1978.tb02284.x; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	13	15	17	0	2	MICROPALEONTOLOGY PRESS	NEW YORK	AMER MUSEUM NAT HISTORY 79TH ST AT CENTRAL PARK WEST, NEW YORK, NY 10024 USA	0026-2803			MICROPALEONTOLOGY	Micropaleontology	WIN	2000	46	4					360	364						5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	381RD					2025-03-11	WOS:000165776100005
J	Coccioni, R; Basso, D; Brinkhuis, H; Galeotti, S; Gardin, S; Monechi, S; Spezzaferri, S				Coccioni, R; Basso, D; Brinkhuis, H; Galeotti, S; Gardin, S; Monechi, S; Spezzaferri, S			Marine biotic signals across a late Eocene impact layer at Massignano, Italy: evidence for long-term environmental perturbations?	TERRA NOVA			English	Article							MIDDLE EOCENE; PALEOCLIMATIC IMPLICATIONS; SHOCKED QUARTZ; SOUTH-ATLANTIC; OLIGOCENE; TRANSITION; OCEAN; STRATIGRAPHY; BOUNDARY; STRATEGY	The Eocene-Oligocene transition marks the passage from 'greenhouse' conditions to an 'icehouse' state, with progressive global cooling starting in the early middle Eocene. The late Eocene presents substantial evidence for extraterrestrial impacts whose effects on living organisms and climatic changes are still not completely clear. A high-resolution, microfloral and faunal investigation has been carried out in a 4-m-thick segment of the Massignano Global Stratotype Section and Point for the Eocene-Oligocene boundary. The studied interval includes a late Eocene (35.7 +/- 0.4 Myr old) impactoclastic layer containing several cosmic signatures. The impact event recorded at Massignano had no abrupt, dramatic effects on marine biota in terms of extinction. However, significant quantitative changes in the calcareous plankton and dinoflagellate cyst assemblages occurred 60 kyr after the impact event. The observed pattern is intepreted as reflecting a long-term re-organization of water structure.	Univ Urbino, Ist Geol, I-61209 Urbino, Italy; Univ Urbino, Ctr Palinol, I-61209 Urbino, Italy; Dipartimento Sci Terra, I-20133 Milan, Italy; Univ Utrecht, Inst Palaeoclimate & Palaeoenvironm Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Univ Paris 06, Dept Geol Sedimentaire, ESA, CNRS 7073 1761, F-75252 Paris, France; Dipartimento Sci Terra, I-50121 Florence, Italy; Univ Vienna, Inst Geol & Palaeontol, GeoZentrum, Vienna, Austria	University of Urbino; University of Urbino; Utrecht University; Sorbonne Universite; University of Florence; University of Vienna	Coccioni, R (通讯作者)，Univ Urbino, Ist Geol, Campus Sci,Local Crocicchia, I-61209 Urbino, Italy.		Gardin, Silvia/F-6920-2010; Brinkhuis, Henk/B-4223-2009; monechi, simonetta/AAN-6148-2020; Basso, Daniela/B-7693-2013	Brinkhuis, Henk/0000-0003-0253-6610; Basso, Daniela/0000-0002-9352-3569; Galeotti, Simone/0000-0001-9636-9344; COCCIONI, Rodolfo/0000-0003-2333-4030				[Anonymous], 2003, STUD GEOPHYS GEOD; AUBRY MP, 1993, EOCENEOLIGOCENE CLIM, P273; BENSON RH, 1975, LETHAIA, V8, P69, DOI 10.1111/j.1502-3931.1975.tb00919.x; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BICE D, 1988, INT UNION GEOLOGICAL, P111; Blow W.H., 1979, The Cenozoic Globigerinidae, VI-III, P1; BLOW WH, 1969, 1ST P INT C PLANKT M, V1, P199; BOERSMA A, 1988, Rivista Italiana di Paleontologia e Stratigrafia, V93, P479; Bottomley R, 1997, NATURE, V388, P365, DOI 10.1038/41073; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Clymer AK, 1996, GEOLOGY, V24, P483, DOI 10.1130/0091-7613(1996)024<0483:SQFTLE>2.3.CO;2; COCCIONI R, 1988, INT SUBCOMMISSION PA, P59; COCCIONI R, IN PRESS SPEC PAP GE; Coxall HK, 2000, GEOLOGY, V28, P87, DOI 10.1130/0091-7613(2000)28<87:HDAAEL>2.0.CO;2; Farley KA, 1998, SCIENCE, V280, P1250, DOI 10.1126/science.280.5367.1250; FIELD JG, 1982, MAR ECOL PROG SER, V8, P37, DOI 10.3354/meps008037; KAIHO K, 1994, GEOLOGY, V22, P719, DOI 10.1130/0091-7613(1994)022<0719:BFDOIA>2.3.CO;2; KELLER G, 1983, MAR MICROPALEONTOL, V7, P463, DOI 10.1016/0377-8398(83)90011-7; Keller Gerta, 1992, P218; Koeberl C, 1996, SCIENCE, V271, P1263, DOI 10.1126/science.271.5253.1263; KOTHE A, 1990, GEOL JB, V118; Kring DA., 2000, GSA TODAY, V10, P1; Kruskal J.B., 1977, Statistical Methods for Digital Computers, P296; Langenhorst F, 1996, GEOLOGY, V24, P487, DOI 10.1130/0091-7613(1996)024<0487:COSQIL>2.3.CO;2; MOLINA E, 1993, GEOL MAG, V130, P483, DOI 10.1017/S0016756800020550; MONECHI S, 1986, PALAEOGEOGR PALAEOCL, V57, P61, DOI 10.1016/0031-0182(86)90006-4; MONTANARI A, 1993, PALAIOS, V8, P420, DOI 10.2307/3515017; Montanari A, 1998, PLANET SPACE SCI, V46, P271, DOI 10.1016/S0032-0633(97)00130-X; Montanari A., 1988, INT SUBCOMMISSION PA, P195; NOCCHI M, 1988, DEV PALAEONT STRAT, V9, P25; PEARSON PN, 1993, J FORAMIN RES, V23, P123, DOI 10.2113/gsjfr.23.2.123; Pierrard O, 1998, GEOLOGY, V26, P307, DOI 10.1130/0091-7613(1998)026<0307:ENRSIU>2.3.CO;2; Prothero D.R., 1994, The Eocene-Oligocene Transition: Paradise Lost; SILVA IP, 1989, MAR MICROPALEONTOL, V14, P357; SILVA IP, 1993, EPISODES, V16, P379, DOI 10.18814/epiiugs/1993/v16i3/002; SPEZZAFERRI S, 1991, PALAEOGEOGR PALAEOCL, V83, P217, DOI 10.1016/0031-0182(91)90080-B; SPEZZAFERRI S, 1995, PALAEOGEOGR PALAEOCL, V114, P43, DOI 10.1016/0031-0182(95)00076-X; SPEZZAFERRI S, IN PRESS J FORAM RES; SPEZZAFERRI S, 1992, THESIS U MILAN; Toon O.B., 1994, Hazards Due to Comets and Asteroids, P791; Vonhof HB, 2000, GEOLOGY, V28, P687; VONHOF HB, 1998, STRONTIUM STRATIGRAP, P77; Wei W., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P979, DOI 10.2973/odp.proc.sr.120.199.1992; WEI WC, 1990, PALAEOGEOGR PALAEOCL, V79, P29, DOI 10.1016/0031-0182(90)90104-F; ZACHOS JC, 1994, PALEOCEANOGRAPHY, V9, P353, DOI 10.1029/93PA03266	45	38	40	0	5	BLACKWELL SCIENCE LTD	OXFORD	P O BOX 88, OSNEY MEAD, OXFORD OX2 0NE, OXON, ENGLAND	0954-4879			TERRA NOVA	Terr. Nova	DEC	2000	12	6					258	263		10.1046/j.1365-3121.2000.00305.x	http://dx.doi.org/10.1046/j.1365-3121.2000.00305.x			6	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	480RF					2025-03-11	WOS:000171475300003
J	Ciminiello, P; Fattorusso, E; Forino, M; Montresor, M				Ciminiello, P; Fattorusso, E; Forino, M; Montresor, M			Saxitoxin and neosaxitoxin as toxic principles of Alexandrium andersoni (Dinophyceae) from the Gulf of Naples, Italy	TOXICON			English	Article						Alexandrium andersoni; PSP; saxitoxin; neosaxitoxin	PROTOGONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; DINOFLAGELLATE; WATERS	A clonal culture of Alexandrium andersoni, obtained from germination of a resting cyst, collected From the Gulf of Naples, was found positive for PSP toxicity by mouse bioassay. The toxicity profile of this dinoflagellate consists mainly of toxins belonging to the saxitoxin class, in particular of Saxitoxin (STX) and Neosaxitoxin (NEO), as determined by a wide MS and (1)H NMR analysis. This represents the first report of the presence of A, andersoni in the Mediterranean Sea, as well as of its toxicity. (C) 2000 Elsevier Science Ltd. All rights reserved.	Univ Naples Federico 2, Dipartimento Chim Sostanze Nat, I-80131 Naples, Italy; Staz Zool Anton Dohrn, I-80121 Naples, Italy	University of Naples Federico II; Stazione Zoologica Anton Dohrn	Fattorusso, E (通讯作者)，Univ Naples Federico 2, Dipartimento Chim Sostanze Nat, Via D Montesano 49, I-80131 Naples, Italy.	fattoru@unina.it		Montresor, Marina/0000-0002-2475-1787; Forino, Martino/0000-0001-8036-3546				ALAM MI, 1979, J PHYCOL, V15, P106, DOI 10.1111/j.0022-3646.1979.00106.x; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Balech E., 1995, The genus Alexandrium Halim (dinoflagellata), P151, DOI [10.2307/3226651., DOI 10.2307/3226651]; CEMBELLA AD, 1987, BIOCHEM SYST ECOL, V15, P171, DOI 10.1016/0305-1978(87)90018-4; DELGADO M, 1999, SCI MAR, V54, P1; FRANCO JR, 1994, J APPL PHYCOL, V6, P272; FROTEZA V, 1998, HARMFUL ALGAE, P58; GARCES E, 1998, HARMFUL ALGAE XUNTA, P167; Hall S., 1982, THESIS U ALASKA; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; HONSELL G, 1995, GIORNALE BOTANICO IT, V129, P390; KELLER MD, 1987, J PHYCOL, V23, P633; Labib Wagdy, 1996, Marine Life, V5, P11; LEDOUX M, 1993, DEV MAR BIO, V3, P413; MACKENZIE L, 1997, NEW ZEAL J MAR FRESH, V31, P401; MARANDA L, 1985, ESTUAR COAST SHELF S, V21, P401, DOI 10.1016/0272-7714(85)90020-4; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; NOGUCHI T, 1990, TOXIC MARINE PHYTOPLANKTON, P493; OSHIMA Y, 1989, NIPPON SUISAN GAKK, V55, P925, DOI 10.2331/suisan.55.925; OSHIMA Y, 1982, B JPN SOC SCI FISH, V48, P851; Oshima Y., 1995, MANUAL HARMFUL MARIN, P81; Shimizu Y., 1979, P321; Sorokin YI, 1996, J SEA RES, V35, P251, DOI 10.1016/S1385-1101(96)90752-2; SOURNIA A, 1991, PHYTOPLANCTON NUISIB, P83	26	53	56	1	19	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0041-0101			TOXICON	Toxicon	DEC	2000	38	12					1871	1877		10.1016/S0041-0101(00)00099-4	http://dx.doi.org/10.1016/S0041-0101(00)00099-4			7	Pharmacology & Pharmacy; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Toxicology	343XZ	10858525				2025-03-11	WOS:000088729300020
J	Kremp, A				Kremp, A			Distribution, dynamics and <i>in situ</i> seeding potential of <i>Scrippsiella hangoei</i> (Dinophyceae) cyst populations from the Baltic Sea	JOURNAL OF PLANKTON RESEARCH			English	Article							DINOFLAGELLATE GONYAULAX-EXCAVATA; RED TIDE DINOFLAGELLATE; RESTING CYSTS; INLAND SEA; SEDIMENTS; RECRUITMENT; JAPAN; BAY; PLANKTON; COPEPODS	The distribution and seasonal dynamics of cyst populations of the spring bloom dinoflagellate Scrippsiella hangoei were studied in surface sediments on the southwest coast of Finland, Baltic Sea. In situ germination was assessed by monitoring the fraction of empty cysts and chlorophyll a fluorescence in cyst populations at different coastal sites throughout the annual cycle. Scrippsiella hangoei resting cysts were widely distributed in the study area and occurred in exceptionally large numbers (magnitudes of 10(4)-10(6) cysts cm(-3)) at all sampling locations between the innermost parts of the coastal archipelago and the open Gulf of Finland. The decreases in cyst number in winter and the increases occurring in late spring reflected the dynamics of germination and encystment of the species. Chlorophyll fluorescence appeared in mid-winter in similar to 40% of cysts from well-aerated basins and 6-15% of cysts from temporarily anoxic sediments. A generally low increase in the proportion of empty cysts indicated that only a part of the potentially germinable cysts actually germinates. Given the high cyst concentrations in the sediments, the potential for germination is considerable, despite the environmentally and physiologically determined losses. In contrast, the size of the vegetative inoculum is very low, indicating that the survival of germlings is problematic under harsh winter conditions. This is an unusual life cycle strategy; however, the early release of cells into the water column provides a high probability for successful bloom initiation under the unpredictable meteorological conditions in winter and early spring, which often lead to the sudden onset of favourable growth conditions.	Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, FIN-00014 Helsinki, Finland	University of Helsinki	Kremp, A (通讯作者)，Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, POB 17, FIN-00014 Helsinki, Finland.		Kremp, Anke/I-8139-2013					*ALG, 1999, BALT SEA ALG; Anderson D.M., 1985, P219; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; BERDALET E, 1992, J PHYCOL, V28, P267, DOI 10.1111/j.0022-3646.1992.00267.x; Blanco Juan, 1995, P563; DESTASIO BT, 1989, ECOLOGY, V70, P1377; Eilertsen H.C., 1998, HARMFUL ALGAE, P196; FRENCH FW, 1980, MAR BIOL LETT, V1, P185; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; Halme Erkki, 1944, ANN ZOOL SOC ZOOL BOT FENNICAE VANAMO, V10, P1; Hansson LA, 1996, LIMNOL OCEANOGR, V41, P1312, DOI 10.4319/lo.1996.41.6.1312; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; KASAHARA S, 1975, MAR BIOL, V31, P25, DOI 10.1007/BF00390644; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; KIVI K, 1986, OPHELIA S, V4, P101; 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; LARSEN J, 1995, PHYCOLOGIA, V34, P135, DOI 10.2216/i0031-8884-34-2-135.1; Malkki P, 1985, FINNISH MARINE RES, V252, P1; MARCUS NH, 1986, LIMNOL OCEANOGR, V31, P206, DOI 10.4319/lo.1986.31.1.0206; Marcus NH, 1996, HYDROBIOLOGIA, V320, P141, DOI 10.1007/BF00016815; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Niemi A, 1973, Acta Botanica Fennica, V100, P1; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; POLLINGHER U, 1993, AQUAT SCI, V55, P11; RENGEFORS K, 1998, ARCH HYDROBIOL SPEC, V51, P23; Steidinger K.A., 1975, P153; STIPA T, 1996, REP SER GEOPHYS, V34, P1; TRIMBEE AM, 1984, J PLANKTON RES, V6, P897, DOI 10.1093/plankt/6.5.897; VIITASALO M, 1994, HYDROBIOLOGIA, V102, P417; Voipio A., 1981, The Baltic Sea; 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, 1996, HARMFUL TOXIC ALGAL, P177; YENTSCH CM, 1980, BIOSCIENCE, V30, P251, DOI 10.2307/1307880	37	29	35	2	5	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	NOV	2000	22	11					2155	2169		10.1093/plankt/22.11.2155	http://dx.doi.org/10.1093/plankt/22.11.2155			15	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	377WN		Bronze			2025-03-11	WOS:000165549400009
J	Seo, KS; Fritz, L				Seo, KS; Fritz, L			Cell-wall morphology correlated with vertical migration in the non-motile marine dinoflagellate <i>Pyrocystis noctiluca</i>	MARINE BIOLOGY			English	Article							NITRATE; PHYTOPLANKTON; POPULATIONS; FUSIFORMIS; CARBON; GROWTH; BLOOM; SEA	We report an ultrastructural study of the morphological changes in cells of the marine dinoflagellate Pyrocystis noctiluca Murray, which correlate with its vertical migration pattern. Cells alternate between a large, highly vacuolated, positively buoyant, vegetative cyst surrounded by a dinosporin-containing wall and a smaller, more compact, negatively buoyant, cellulose-bounded cell. The cyst wall is composed of two layers: a thin smooth outer layer, thought to be composed of dinosporin, and a thick inner layer that likely to be cellulosic. One or two thecate cells are formed from within the cysts. Thecate cells are smaller, more compact and contain many small translucent bodies. They are surrounded by a typical dinoflagellate amphiesmal layer composed of membranes and cellulose plates. The amphiesmal layer appears only in recently divided cells and exists for only one night. By the following day, the cellulose wall has been replaced by a new dinosporin wall synthesized from beneath the cellulose thecal layer. The cyst stage is suggested as being optimized for photosynthesis, whereas the compact, negatively buoyant, thecate form is thought to allow nutrient uptake in deeper waters. Vertical migration in this species is thus correlated with the presence of dinosporin wall during most of its stay in the upper waters, alternating with a brief thecate wall in deeper nutrient-rich waters. This is the first report correlating dinoflagellate vertical migration with changes in cell-wall composition.	No Arizona Univ, Dept Biol Sci, Flagstaff, AZ 86011 USA	Northern Arizona University	No Arizona Univ, Dept Biol Sci, Box 5640, Flagstaff, AZ 86011 USA.	Lawrence.Fritz@nau.edu						BALLEK RW, 1986, J EXP MAR BIOL ECOL, V101, P175, DOI 10.1016/0022-0981(86)90048-1; BHOVICHITRA M, 1977, LIMNOL OCEANOGR, V22, P73, DOI 10.4319/lo.1977.22.1.0073; Boyd CN, 1999, J EXP BOT, V50, P461, DOI 10.1093/jexbot/50.333.461; CULLEN JJ, 1981, MAR BIOL, V62, P81, DOI 10.1007/BF00388169; EGGERSDORFER B, 1991, FEMS MICROBIOL ECOL, V85, P319, DOI 10.1016/0378-1097(91)90191-C; ELBRACHTER M, 1978, HELGOLAND WISS MEER, V31, P347, DOI 10.1007/BF02189487; EPPLEY RW, 1968, J PHYCOL, V4, P333, DOI 10.1111/j.1529-8817.1968.tb04704.x; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FRITZ L, 1986, THESIS RUTGERS U NEW; Hays GC, 1995, LIMNOL OCEANOGR, V40, P1461, DOI 10.4319/lo.1995.40.8.1461; HEISKANEN AS, 1995, MAR ECOL PROG SER, V122, P45, DOI 10.3354/meps122045; LIEBERMAN OS, 1994, J PHYCOL, V30, P964, DOI 10.1111/j.0022-3646.1994.00964.x; MacIntyre JG, 1997, MAR ECOL PROG SER, V148, P201, DOI 10.3354/meps148201; MORRILL LC, 1981, J PHYCOL, V17, P315, DOI 10.1111/j.0022-3646.1981.00315.x; PINCEMIN JM, 1981, ARCH PROTISTENKD, V124, P271, DOI 10.1016/S0003-9365(81)80020-6; PINCEMIN JM, 1982, ARCH PROTISTENKD, V125, P95, DOI 10.1016/S0003-9365(82)80009-2; PINCEMIN JM, 1978, ARCH PROTISTENKD, V120, P401, DOI 10.1016/S0003-9365(78)80031-1; Qi Yuzao, 1997, Oceanologia et Limnologia Sinica, V28, P458; RIVKIN RB, 1984, DEEP-SEA RES, V31, P353, DOI 10.1016/0198-0149(84)90089-X; RIVKIN RB, 1979, LIMNOL OCEANOGR, V24, P107, DOI 10.4319/lo.1979.24.1.0107; Sukhanova I.N., 1973, LIFE ACTIVITIES PELA, P218; Sukhanova IN, 1973, LIFE ACTIVITY PELAGI, P210; SWIFT E, 1970, J PHYCOL, V6, P79, DOI 10.1111/j.0022-3646.1970.00079.x; SWIFT E, 1976, LIMNOL OCEANOGR, V21, P418, DOI 10.4319/lo.1976.21.3.0418; SWIFT E, 1971, J PHYCOL, V7, P89, DOI 10.1111/j.1529-8817.1971.tb01486.x; Villareal TA, 1999, NATURE, V397, P423, DOI 10.1038/17103; VILLAREAL TA, 1994, J PHYCOL, V30, P1, DOI 10.1111/j.0022-3646.1994.00001.x; VILLAREAL TA, 1995, J PHYCOL, V31, P689, DOI 10.1111/j.0022-3646.1995.00689.x; WALKER DR, 1991, S AFR J MARINE SCI, V10, P61; Watanabe M, 1995, LIMNOL OCEANOGR, V40, P1447, DOI 10.4319/lo.1995.40.8.1447	30	12	14	1	14	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	0025-3162	1432-1793		MAR BIOL	Mar. Biol.	NOV	2000	137	4					589	594		10.1007/s002270000374	http://dx.doi.org/10.1007/s002270000374			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	376CJ					2025-03-11	WOS:000165440400004
J	Vink, A; Zonneveld, KAF; Willems, H				Vink, A; Zonneveld, KAF; Willems, H			Organic-walled dinoflagellate cysts in western equatorial Atlantic surface sediments: distributions and their relation to environment	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; ecology; Holocene; statistical analysis; western equatorial Atlantic	RECENT MARINE-SEDIMENTS; INDIAN-OCEAN; PALYNOMORPH DISTRIBUTION; NORTH-ATLANTIC; ADJACENT SEAS; AUSTRALIA; EASTERN; TEMPERATURE; CIRCULATION; DISPERSAL	In contrast to the wide range of studies carried out in temperate and high-latitude oceanic regions, only a few studies have focused on recent and Holocene organic-walled dinoflagellate cyst assemblages from the tropics. This information is, however, essential for fully understanding the ability of species to adapt to different oceanographic regimes, and ultimately their potential application to local and regional palaeoenvironmental and palaeoceanographic reconstructions. Surface sediment samples of the western equatorial Atlantic Ocean north of Brazil, an area greatly influenced by Amazon River discharge waters, were therefore analysed in detail for their organic-walled dinoflagellate cyst content. A diverse association of 43 taxa was identified, and large differences in cyst distribution were observed. The cyst thanatocoenosis in bottom sediments reflects the seasonal advection of Amazon River discharge water through the Guyana Current and the North Equatorial Countercurrent well into the North Atlantic. To establish potential links between cyst distribution and the environmental conditions of the upper water column, distribution patterns were compared with mean temperature, salinity, density and stratification gradients within the upper water column (0-100 m) over different times of the year, using correspondence analysis and canonical correspondence analysis. The analyses show that differences in these parameters only play a subordinate role in determining species distribution. Instead, nutrient availability, or related factors, dominates the distribution pattern. The only possible indicators of slightly reduced salinities are Trinovantedinium applanatum and Lingulodinium machaerophorum. Four assemblage groups of cyst taxa with similar environmental affinities related to specific water masses/currents can be distinguished and have potential for palaeoenvironmental reconstruction. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Vink, A (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330 440, D-28334 Bremen, Germany.		Vink, Annemiek/GXG-6435-2022	Vink, Annemiek/0000-0002-5178-9721				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; [Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1996, Am. Assoc. Strat. 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Palaeobot. Palynology	NOV	2000	112	4					247	286		10.1016/S0034-6667(00)00046-4	http://dx.doi.org/10.1016/S0034-6667(00)00046-4			40	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	393DJ	11134709				2025-03-11	WOS:000166453700004
J	Kennedy, WJ; Gale, AS; Bown, PR; Caron, M; Davey, RJ; Gröcke, J; Wray, DS				Kennedy, WJ; Gale, AS; Bown, PR; Caron, M; Davey, RJ; Gröcke, J; Wray, DS			Integrated stratigraphy across the Aptian-Albian boundary in the Marnes Bleues, at the Col de Pre-Guittard, Arnayon Drome), and at Tartonne (Alpes-de-Haute-Provence), France:: a candidate Global Boundary Stratotype Section and boundary point for the base of the Albian Stage	CRETACEOUS RESEARCH			English	Review						boundary stratotype; palynomorphs; calcareous nannofossils; planktonic foraminifera; ammonites; trace elements; rare earth elements; major elements; oxygen; carbon; stronrium isotopes; Cretaceous; Aptian; Albian; France	PLANKTONIC-FORAMINIFERA; ISOTOPE STRATIGRAPHY; DINOFLAGELLATE CYSTS; ANOXIC EVENT; AMMONITES; EUROPE; RECORD; BIOSTRATIGRAPHY; NANNOFOSSILS; EVOLUTION	The history of definition of the Aptian-Albian boundary is reviewed with particular reference to the ammonite schemes of Brinkmann (1937), Breistroffer (1947), Casey (1961a, 1996, 1999), Kemper (1982), Owen (1996, 1999), and Ruffell & Owen (1995). The classic sequence in the Hannover area of Germany described by Brinkmann (1937) is reviewed in the light of subsequent work. The definition of the base of the Albian Stage at the first occurrence of the ammonite Proleymeriella schrammeni (Jacob, 1907) is rejected as it can only be recognised over a limited area near Hannover; no more widely recognised secondary markers have been documented, and there is no permanent section at the present rime. An alternative Aptian-Albian boundary, defined by the first occurrence of the ammonite Leymeriella (L.) tardefurcata (d'Orbigny, 1841) in the expanded Marnes Bleues section at Tartonne, Alpes-de-Haute-Provence, France, is suggested. The palynomorph, coccolith, planktonic foraminiferan, ammonite, and inoceramid bivalve sequence, organic and inorganic carbon, trace, rare earth, and major element record, oxygen and carbon isotope sequence, and strontium isotope data are presented for sections at the Col de Pre-Guittard, Arnayon (Drome), and Tartonne (Alpes-de-Haute-Provence) and described in detail. The Pre-Guittard section, considered as a candidate Global Boundary Stratotype Section (GSS) for the base of the Albian Stage at the Second International Symposium on Cretaceous Stage Boundaries held in Brussels in September 1995, provides a standard section for the boundary interval in SE France. It is, however, unsuitable as a GSS, as there is a hiatus at the critical level in the section. In contrast, the Tartonne section is a potential GSS. The Boundary Point for the base of the Albian Stage suggested here is the first criterion proposed at Brussels: the first appearance of the ammonite Leymeriella (L.) tardefurcata at the base of the Niveau Paquier within the expanded Marnes Bleues sequence. The first appearance is only 60 cm above the last record of its presumed ancestor, L. (L.) germanica Casey, 1957. So defined, the boundary lies within the Prediscosphaera columnata Nannofossil (NF) Zone NC/CC8, and the planktonic foraminiferal Hedbergella planispira Partial Range Zone. There is no major or trace element event associated with the proposed boundary, nor is there any distinctive oxygen or carbon isotopic signal. Strontium isotope data from the Tartonne section are compatible with those elsewhere in the basin, and show that the base of the Albian, defined by the first appearance of L. (L.) taudefurcata corresponds to an Sr-87/Sr-86 ratio of 0.707339 +/- 2. Systematic sections deal with a new palynomorph, calcareous nannofossils and ammonites; full range data and taxonomic indices are given for the first two groups. (C) 2000 Academic Press.	Univ Oxford, Museum Nat Hist, Oxford OX1 3PW, England; Univ Greenwich, Sch Earth & Environm Sci, Chatham ME4 4TB, Kent, England; UCL, Dept Geol Sci, London WC1E 6BT, England; Univ Fribourg, Inst Geol, CH-1700 Fribourg, Switzerland; Robertson Res Int Ltd, Llanrhos LL30 1SA, Llandudno, Wales; Dept Earth Sci, Oxford OX1 3PR, England	University of Oxford; University of Greenwich; University of London; University College London; University of Fribourg	Univ Oxford, Museum Nat Hist, Parks Rd, Oxford OX1 3PW, England.		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L., 1998, AM ASS STRATIGRAPHIC, V34; Wilson E. O., 1967, The Theory of Island Biogeography; Wilson PA, 1998, NATURE, V392, P889, DOI 10.1038/31865; Wind F.H., 1979, Initial Reports of the Deep Sea Drilling Project, V47, P221; Wise S. W, 1977, Initial Rep Deep Sea Drilling Project, V36, P269; WOLLEMANN A, 1907, Z DTSCH GEOLOGISCHEN, V59, P55; Wray DS, 1998, P YORKS GEOL SOC, V52, P95, DOI 10.1144/pygs.52.1.95; Wright C.W., 1996, TREATISE INVERTEBR 1; WRIGHT CW, 1957, TREATISE INVERTEBR 1; WRIGHT CW, 1984, PALAEONTOLOGICAL SOC; Young Jeremy R., 1996, P261; Zittel K. A. von, 1895, GRUNDZUGE PALAEONTOL	318	140	162	1	11	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	OCT	2000	21	5					591	720		10.1006/cres.2000.0223	http://dx.doi.org/10.1006/cres.2000.0223			130	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	377FW					2025-03-11	WOS:000165503500002
J	Peralta, PI; Volkheimer, W				Peralta, PI; Volkheimer, W			Early Cretaceous sea level variations and changes in dinocyst assemblages and organic matter components in the Neuquen Basin, western Argentina	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-MONATSHEFTE			English	Article							DINOFLAGELLATE CYSTS; SEDIMENTS; NORTH	At the Cerro Negro de Covunco locality, Neuquen Province, central western Argentina, the Agrio Formation is represented by grey pelites and sandstones corresponding to marine ingressions during Early Cretaceous times. These sediments bear well preserved assemblages of dinocysts, pollen grains, spores and organic matter (remains of plant tissues: tracheid fragments, cuticles, leaf fragments; fungal spores, marine algae). The analysis of these elements allowed determination of palynofacies. The following qualitative and quantitative criteria, indicating distal-proximal changes in the coastal - open sea line, were used to convert palynofacies observations into a tentative paleoenvironmental curve: ratio of continental to marine organic constituents, proportion of blade-shaped inertinite to total inertinite, and finally size, sorting and roundness of equidimensional inertinite particles; ratio of inertinite to vitrinite, proportion of biostructured tissue, diversity and dominance of dinocyst species and dominant cyst morphotype. The paleoenvironmental curve derived from organic matter shows oscillations between a more proximal (more shallow water, high energy) and a more distal (deeper water, low energy) environment. The maximum registered depth at the Cerro Negro tie Covunco locality indicates a depth not greater than the depth of an external neritic sea and the minimum depth registered of a coastal environment. These variations yielded by the organic matter components, combined with sedimentologic information and the invertebrate faunal data, confirm changes occurred in the sea level with regressions and ingressions of the sea in this part of the Neuquen Basin during the Early Cretaceous.	IANIGLA, RA-5500 Mendoza, Argentina; CONICET, RA-5500 Mendoza, Argentina	University Nacional Cuyo Mendoza	Peralta, PI (通讯作者)，IANIGLA, Ruiz Leal S-N Parque,Gral San Martin CC 330, RA-5500 Mendoza, Argentina.							BATTEN D J, 1973, Palaeontology (Oxford), V16, P1; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; DENISON C, 1995, SEDIMENTARY ORGANIC; Goodman DK., 1979, Palynology, V3, P169; GORIN GE, 1991, PALAEOGEOGR PALAEOCL, V85, P303, DOI 10.1016/0031-0182(91)90164-M; HABIB D, 1983, INITIAL REP DEEP SEA, V76, P781; HABIB D, 1989, PALAEOGEOGR PALAEOCL, V74, P23, DOI 10.1016/0031-0182(89)90018-7; Habib D., 1982, Nature and Origin of Cretaceous Carbon-Rich Facies; HABIB D, 1979, MAURICE EWING SERIES, V3, P420; HAIRD JD, 1980, WILDLIFE MANAGEMENT, V16, P269; LAENZA HA, 1981, CUENCAS SEDIMENTARIA, V2, P559; LEANZA H A, 1981, Ameghiniana, V18, P1; Leanza H.A., 1981, Neues Jahrbuch fur Geologie und Palaointologie, Abhandlungen, V161, P62; PARRY CC, 1981, PETR GEOLOGY CONTINE; PERALTA P, 1997, N JB GEOL PALAONT, V204, P3; PERALTA P, 1996, REV ESP MICROPALEONT, V2, P45; Quattrocchio M, 1996, GEORES FORUM, V1&2, P467; Quattrocchio M., 1985, Ameghiniana, V21, P187; QUATTROCCHIO M, 1980, OPERA LILLOANA, V31, P59; QUATTROCCHIO M, 1982, 3 C ARG PAL BIOESTR, P107; QUATTROCCHIO ME, 1990, REV PALAEOBOT PALYNO, V65, P319, DOI 10.1016/0034-6667(90)90082-T; QUATTROCCHIO ME, 1983, ASOC GEOL ARGENTINA, V38, P34; SCOTT RW, 1978, TEX U BUR EC GEOL, V89, P169; SPALLETTI LA, 1992, CUARTA REUNION ARGEN, V1, P33; Steffen D., 1993, SOURCE ROCKS SEQUENC, V37, P49; 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; TYSON RV, 1989, NW EUROPEAN MICROPAL; VOLKHEIMER W, 1977, Ameghiniana, V14, P162; VOLKHEIMER W, 1981, 8TH ACT C GEOL ARG S, V4, P761; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9	32	3	5	0	0	E SCHWEIZERBARTSCHE VERLAGS	STUTTGART	NAEGELE U OBERMILLER JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	0028-3630			NEUES JAHRB GEOL P-M	Neues Jahrb. Geol. Palaontol.-Monatsh.	OCT	2000		10					613	631						19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	368PK					2025-03-11	WOS:000090126500003
J	Köhler, J; Clausing, A				Köhler, J; Clausing, A			Taxonomy and palaeoecology of dinoffagellate cysts from Upper Oligocene freshwater sediments of Lake Enspel, Westerwald area, Germany	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; Enspel; freshwater; Germany; palaeoecology; Upper Oligocene	MESSEL	Freshwater dinoflagellates play an important role as primary producers in the lacustrine environment. A new species of dinoflagellates, Cleistosphaeridium lacustre, is described from Upper Oligocene sediments of palaeo-lake Enspel. They are associated with other phytoplankton, such as diatoms, chrysophytes, green algae and benthic cyanobacteria. Mass occurrences of this species are interpreted as algal blooms and may partly reflect seasonal successions. This phenomenon was controlled by volcanic activities in the depositional area, which led to an increase in nutrient supply. (C) 2000 Elsevier Science B.V. All rights reserved.	Inst Geol Wissensch & Geiseltalmuseum, D-06108 Halle, Germany; Hess Landesmuseum, D-64283 Darmstadt, Germany		Clausing, A (通讯作者)，Inst Geol Wissensch & Geiseltalmuseum, Domstr 5, D-06108 Halle, Germany.							BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BOURRELLY P, 1970, ALGEURS EAU DOUCE, V3; Clausing Andreas, 1998, Hallesches Jahrbuch fuer Geowissenschaften Reihe B Geologie Palaeontologie Mineralogie, V20, P119; DAVEY RJ, 1966, BRIT MUSEUM GEOLOG S, V3; Felder M., 1998, MAINZER GEOWISSENSCH, V27, P101; Gaupp R., 1998, HALLESCHES JB GEOW B, V20, P97; GOTH K, 1988, NATURE, V336, P759, DOI 10.1038/336759a0; GOTH K, 1990, MESSELER OLSCHIEFER, V113; HABERMEHL G, 1983, NATURWISSENSCHAFTEN, V70, P566, DOI 10.1007/BF00376676; Harris W.K., 1973, Spec. Publ. Geol. Soc. Aust, V4, P159; HE C., 1991, Late Cretaceous -Early Tertiary Microphytoplankton from the Western Tarim Basin in Southern Xinjiang, China; HE CQ, 1989, SERIES STRATIGRAPHY; HE CQ, 1981, TERTIARY PALAEONTOLO, P60; HOTTENROTT M, 1988, Geologisches Jahrbuch Hessen, V116, P113; JIABO, 1978, PALEOGENE DINOFLAGEL; KOHLER J, 1997, THESIS U TUBINGEN; Krutzsch W, 1962, HALLESCHES JB MITTEL, V4, P40; LAMBERT A, 1979, SEDIMENTOLOGY, V26, P453, DOI 10.1111/j.1365-3091.1979.tb00920.x; Lentin JK., 1993, AM ASS STRATIGRAPHIC, V28, P856; MARTINI E, 1993, MONUMENT GRUBE MES 1, V2, P39; MARTINI E, 1988, BEITRAGE NATURKUNDE, V24, P55; MORS T, 1995, SEDIMENTATIONSGESICH, V187; Mosbrugger V, 1997, PALAEOGEOGR PALAEOCL, V134, P61, DOI 10.1016/S0031-0182(96)00154-X; NICKEL B, 1996, MAINZER NATURWISSENS, V18, P148; NORRIS G, 1972, GEOSCI MAN, V4, P49; PIRRUNG BM, 1998, MAINZER NATURWISSENS, V20, P118; Pollingher U., 1987, Botanical Monographs (Oxford), V21, P502; POPOVSKY J., 1990, Susswasserflora von Mitteleuropa, P272; Rullkotter J., 1988, COURIER FORSCHUNGSIN, V107, P37; SCHILLING AJ, 1891, ALLGEMEINE BOTANISCH, V74, P220; Schulz U., 1997, WURZBURGER GEOGRAPHI, V41, P195; Storch G, 1996, NATURE, V379, P439, DOI 10.1038/379439a0; STOVER LE, 1978, GEOLOGICAL SCI, P15; TRAVERSE A, 1955, 5151 US DEP INT BUR; Wan Chuan-biao, 1994, Acta Palaeontologica Sinica, V33, P499; Wuttke M., 1993, MAINZER NATURWISSENS, V31, P115; WUTTKE M, 1993, SEDIMENT, V93, P8; Zippi Pierre A., 1998, Micropaleontology (New York), V44, P1, DOI 10.2307/1485998	39	18	22	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	OCT	2000	112	1-3					39	49		10.1016/S0034-6667(00)00034-8	http://dx.doi.org/10.1016/S0034-6667(00)00034-8			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	371VL	11042325				2025-03-11	WOS:000165199900003
J	Schrank, E; Mahmoud, MS				Schrank, E; Mahmoud, MS			New taxa of angiosperm pollen, miospores and associated palynomorphs from the early Late Cretaceous of Egypt (Maghrabi Formation, Kharga Oasis)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						angiosperms; Cenomanian; Cretaceous; Egypt; palynology; pollen	PALYNOLOGY; STRATIGRAPHY; SEDIMENTS; SPORES; SUDAN	A palynological investigation of samples from various boreholes in the Maghrabi Formation (Kharga Oasis, southern Egypt) resulted in the recovery of pollen and spore assemblages associated with rare marine palynofossils (dinoflagellates, foraminiferal linings) and freshwater algae (e.g. Botryococcus, Ovoidites parvus, Pediastrum, Scenedesmus). The general composition of the assemblages is largely consistent with the estuarine and tidal flat conditions characteristic of the Maghrabi Formation. The formal descriptions of the following new taxa are given: Cicatricosisporites kedvesii Schrank, sp. nov., Equisetosporites lawalii Schrank, sp. nov., Dettmannaepollenites clavatus Schrank, sp. nov., and Integritetradites porosus Schrank and Mahmoud, gen. nov. and sp. nov. Combined scanning electron microscopic and light microscopic techniques have been applied to hand-picked grains to illustrate the new taxa. The palynological ages assigned to the Maghrabi samples are mainly based on angiosperm pollen and range from undifferentiated Cenomanian for an Integritetradites porosus assemblage without triporates to Late Cenomanian-Early Turonian for another assemblage which has I. porosus associated with rare triporate pollen grains (Proteacidites/'Triorites' spp.). (C) 2000 Elsevier Science B.V. All rights reserved.	Tech Univ Berlin, Inst Angew Geowissensch 2, D-10587 Berlin, Germany; Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt	Technical University of Berlin; Egyptian Knowledge Bank (EKB); Assiut University	Schrank, E (通讯作者)，Tech Univ Berlin, Inst Angew Geowissensch 2, Sekr EB 10,Ernst Reuter Pl 1, D-10587 Berlin, Germany.		Mahmoud, Magdy/ABD-1262-2020					ABDELMOHSEN S, 1992, EGYPT J AFR EARTH SC, V14, P567; Azema C, 1974, PALEOBIOL CONTINET M, V5, P1; BALTES N, 1966, P 2 W AFR MICR COLL, P3; BARTHOUX MJ, 1925, MEM I EGYPT, V7, P65; BATTEN D J, 1988, Cretaceous Research, V9, P337, DOI 10.1016/0195-6671(88)90007-9; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; Boltenhagen E, 1977, CAH PALEONTOL, P1; Brasil do, B TEC PETROBRAS, V17, P263; Brenner Gilbert J., 1996, P91, DOI 10.1007/978-0-585-23095-5_5; Crane P.R, 1990, MAJOR EVOLUTIONARY R, P377; Daugherty L.H., 1941, CARNEGIE I WASH YR B, V526, P1; Dettmann M. 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Pal, V29, P61; LEJALNICOL A, 1987, BERLINER GEOWISS ABH, V120, P957; LENTIN JK, 1981, SERIES BI R 8112, P1; MAMI L, 1993, THESIS U REIMS CHAMP; MEON H, 1991, Palaeontographica Abteilung B Palaeophytologie, V223, P107; MULLER J, 1981, BOT REV, V47, P1, DOI 10.1007/BF02860537; Penny J., 1986, SP PAP PALAEONTOL, V35, P121; PENNY J H J, 1991, Palaeontographica Abteilung B Palaeophytologie, V222, P31; POCOCK SAJ, 1988, REV PALAEOBOT PALYNO, V55, P337, DOI 10.1016/0034-6667(88)90092-9; Potoni ~e R., 1933, BERLINISCHE GESELLSC, V33, P517; RETALLACK G J, 1986, Cretaceous Research, V7, P227, DOI 10.1016/0195-6671(86)90027-3; SAAD S I, 1976, Pollen et Spores, V18, P407; Schrank E, 1998, J AFR EARTH SCI, V26, P167, DOI 10.1016/S0899-5362(98)00004-9; SCHRANK E, 1987, Cretaceous Research, V8, P29, DOI 10.1016/0195-6671(87)90010-3; SCHRANK E, 1992, CRETACEOUS RES, V13, P351, DOI 10.1016/0195-6671(92)90040-W; SCHRANK E, 1994, GEOL RUNDSCH, V83, P773; SCHRANK E., 1990, Berliner geowissenschaftliche Abhandlungen. Abteilung A, V120, P149; Schrank E., 1995, BERLINER GEOWISSENSC, V177, P1; Schrank E., 1987, BERLINER GEOWISS ABH, V75, P249, DOI DOI 10.1016/0195-6671(92)90040-W; SINGH C, 1971, B RES COUNC ALBERTA, V28, P1; Singh C., 1971, RES COUNCIL ALBERTA, V28, pi; Singh C., 1983, ALBERTA RES COUNCIL, V44, P1; SINGH C, 1971, RES COUNCIL ALBERTA, V28, P301; Soliman H.A., 1977, Revue Micropaleont, V20, P114; Srivastava S.K., 1968, CAN J EARTH SCI, V5, P211, DOI DOI 10.1139/E68-022; SRIVASTAVA SK, 1972, REV PALAEOBOT PALYNO, V14, P217, DOI 10.1016/0034-6667(72)90021-8; STOVER LEWIS E., 1964, MICRO PALEONTOLOGY, V10, P145, DOI 10.2307/1484637; Thiergart F., 1937, GEOLOGISCHEN LANDESA, V58, P282; Uwins F.J.R., 1988, SUBSURFACEPALYNOSTRA, P215; ZAVADA M S, 1990, Palynology, V14, P41; Zhang Y-Y, 1999, ACTA PALAEONTOLOGICA, V38, P435	62	24	28	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	OCT	2000	112	1-3					167	188		10.1016/S0034-6667(00)00040-3	http://dx.doi.org/10.1016/S0034-6667(00)00040-3			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	371VL	11042331				2025-03-11	WOS:000165199900009
J	Dybkjaer, K; Rasmussen, ES				Dybkjaer, Karen; Rasmussen, Erik Skovbjerg			Palynological dating of the Oligocene - Miocene successions in the Lille Baelt area, Denmark	BULLETIN OF THE GEOLOGICAL SOCIETY OF DENMARK			English	Article						palynology; sequence stratigraphy; Late Oligocene; Early Miocene; Hagenor; Hindsgavl; Ronshoved; Lille Baelt; Denmark	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; INTEGRATED STRATIGRAPHY; SEQUENCE	A new geological model for the succession outcropping in the Lille Baelt area, Denmark, is proposed. The model is based on dinoflagellate cyst stratigraphy on the three sections at Hindsgavl, Hagenor and Ronshoved combined with earlier biostratigraphic studies and sequence stratigraphic correlation of outcrops and borings. Our results indicate that there have been two periods with lagoonal and nearshore marine deposition in the Lille Baelt area separated by a hiatus of at least 3.5 million years. The first period occurred in Late Oligocene or earliest Early Miocene (early Aquitanian) time and is represented by the deposits at Hindsgavl. The second period occurred in Early Miocene (early to mid-Burdigalian) time and is represented by the deposits at Hagenor and Ronshoved. The deposits at Hindsgavl are time equivalent with the lagoonal upper part of the Vejle Fjord Formation and the overlying nearshore marine sand at Hvidbjerg. The deposits at Hagenor and Ronshoved correlate with the lower part of the offshore marine Arnum Formation and thus represent part of the coastline during the early to mid-Burdigalian.	[Dybkjaer, Karen; Rasmussen, Erik Skovbjerg] Geol Survey Denmark & Greenland GEUS, DK-2400 Copenhagen NV, Denmark	Geological Survey Of Denmark & Greenland	Dybkjaer, K (通讯作者)，Geol Survey Denmark & Greenland GEUS, Thoravej 8, DK-2400 Copenhagen NV, Denmark.	kd@geus.dk; esr@geus.dk	Dybkjær, Karen/G-5223-2018					[Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1988, Geol. 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L., 1998, AM ASS STRATIGRAPHIC, V34; Williams G.L., 1999, MESOZOIC CENOZOIC DI; WILLIAMS GL, 1998, SOC SEDIMENTARY GEOL, V60; Williams Graham L., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P99; Zevenboom D, 1995, THESIS U UTRECHT UTR; Zevenboom Daan, 1996, Giornale di Geologia (Bologna), V58, P81; Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	62	33	34	0	3	GEOLOGICAL SOC DENMARK	COPENHAGEN	OSTER VOLDGADE 5-7, DK-1350 COPENHAGEN, DENMARK	2245-7070			B GEOL SOC DENMARK	Bull. Geol. Soc. Den.	SEP	2000	47		1				87	103						17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	V62RG					2025-03-11	WOS:000204236000007
J	Head, MJ				Head, MJ			<i>Geonettia waltonensis</i>, a new Goniodomacean dinoflagellate from the Pliocene of the North Atlantic region, and its evolutionary implications	JOURNAL OF PALEONTOLOGY			English	Article							LOWER CONTINENTAL RISE; STRATIGRAPHY; NEOGENE; SYSTEMATICS; MARYLAND; VIRGINIA; SITE-603; CORE	A new species of the unusual dinoflagellate cyst genus Geonettia de Verteuil and Norris, 1996a is here described from the Pliocene of the western North Atlantic and eastern England. Geonettia it waltonensis new species is only the second species to be formally described for this genus, whose type, G. clineae de Verteuil and Norris. 1996a, has a range of Miocene through Pliocene. Geonettia is a gonyaulacalean, goniodomacean genus of the subfamily Pyrodinioideae and is closely related to Eocladopyxis Morgenroth, 1966 and Capisocysta Warny and Wrenn, 1997, also found in the Cenozoic. However, Geonettia is the only known dinoflagellate cyst genus to have plates that dissociate extensively on both epi- and hypocyst during excystment. Geonettia waltonensis has this style of excystment, but its hypocystal tabulation is more akin to Capisocysta lata Head. 1998a than to G. clineae. Comparison of tabulation and other morphological features suggests that during the late Miocene, Capisocysta lata evolved from Geonettia waltonensis or a closely related species through failure of its epicystal plates to dissociate. Geonettia waltonensis probably did not evolve directly from G. clineae but may represent a separate lineage within Geonettia that arose during the Miocene.	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Cambridge CB2 3EN, England	University of Cambridge	Univ Cambridge, Dept Geog, Godwin Inst Quaternary Res, Downing Pl, Cambridge CB2 3EN, England.	mh300@cam.ac.uk						[Anonymous], 1996, Palynology: principles and applications; ANSTEY CE, 1992, UNPUB THESIS U TORON; BALECH E, 1985, REV PALAEOBOT PALYNO, V45, P17, DOI 10.1016/0034-6667(85)90063-6; BERGGREN WA, 1995, GEOL SOC AM BULL, V107, P1272, DOI 10.1130/0016-7606(1995)107<1272:LNCNPI>2.3.CO;2; BUJAK JP, 1980, PALAEONTOLOGY, V24, P26; BUTSCHLI O., 1885, KLASSEN ORDNUNGEN TH, P865; CANNINGA G, 1987, INITIAL REPORTS DEEP, V93, P839; Davey R.J., 1966, STUDIES MESOZOIC CAI, P53; De Verteuil L., 1996, P OCEAN DRILLING PRO, V150, P439; de Verteuil Laurent, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P129; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P263, DOI 10.2307/1485875; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P83; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FUNNELL BM, 1977, BRIT QUATERNARY STUD, P247; HAGGERTY J, 1987, INITIAL REPORTS DE 2, V93, P1285; 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.J., 1996, Palynology: Principles and Applications, P1197; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head MJ, 1999, J PALEONTOL, V73, P1; Head MJ, 1998, J PALEONTOL, V72, P797, DOI 10.1017/S0022336000027153; Head MJ, 1998, GEOL MAG, V135, P803, DOI 10.1017/S0016756898001745; HEAD MJ, 1996, PALYNOLOGY, V20, P241; Headley JM, 1997, J WORLD HIST, V8, P1, DOI 10.1353/jwh.2005.0080; Hodgson G.E., 1987, P44; KOLEV SM, 1993, UNPUB THESIS U TORON; LIENGJARERN M, 1980, Palaeontology (Oxford), V23, P475; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; MAALOULEH K, 1987, INITIAL REP DEEP SEA, V93, P481; McLean D.M., 1976, Micropaleontology, V22, P347, DOI 10.2307/1485256; MORGENROTH P., 1966, PALAEONTOGRAPHICA, V119, P1; MOULLADE M, 1987, INITIAL REPORTS DEEP, V93, P1271; MUZA JP, 1987, INITIAL REP DEEP SEA, V93, P593, DOI DOI 10.2973/DSDP.PR0C.93.115.198; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; Plate Ludwig, 1906, Archiv fuer Protistenkunde Jena, V7, P411; ROSSIGNOL MARTINE, 1962, POLLEN SPORES, V4, P121; SRIVASTAVA SP, 1987, P OC DRILL PROGR SCI, V105; TAYLOR FJR, 1989, ICLARM CONT, V21, P207; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; van Hinte J.E., 1987, INITIAL REPORTS DEEP, V93; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5	44	8	8	0	0	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0022-3360	1937-2337		J PALEONTOL	J. Paleontol.	SEP	2000	74	5					812	827		10.1666/0022-3360(2000)074<0812:GWANGD>2.0.CO;2	http://dx.doi.org/10.1666/0022-3360(2000)074<0812:GWANGD>2.0.CO;2			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	356CN					2025-03-11	WOS:000089426900004
J	Hamer, JP; McCollin, TA; Lucas, IAN				Hamer, JP; McCollin, TA; Lucas, IAN			Dinoflagellate cysts in ballast tank sediments: Between tank variability	MARINE POLLUTION BULLETIN			English	Article							MARINE ORGANISMS; RISK ASSESSMENT; WATER; TRANSPORT; INTRODUCTIONS		Univ Coll N Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales	Bangor University	Univ Coll N Wales, Sch Ocean Sci, Menai Bridge LL59 5EY, Gwynedd, Wales.							Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; 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; Hallegraeff GM, 1995, IOC MANUALS GUIDES; HAMER JP, 1998, NIGES TEKNISK NATURV, V1, P53; HARVEY M, 1999, CANADIAN TECHNICAL R, V2268; HAY C, 1997, 417 CAWTH I; Hayes KR, 1998, ICES J MAR SCI, V55, P201, DOI 10.1006/jmsc.1997.0342; KELLY JM, 1993, J SHELLFISH RES, V12, P405; LAING I, 1995, BALLAST WATER EXCHAN; Macdonald E.M., 1998, 397 FRS MAR LAB; MATSUOKA K, 1995, IOC MANUALS GUIDES	15	51	57	3	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.	SEP	2000	40	9					731	733		10.1016/S0025-326X(99)00198-8	http://dx.doi.org/10.1016/S0025-326X(99)00198-8			3	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	351QG					2025-03-11	WOS:000089169200014
J	Zonneveld, KAF; Brune, A; Willems, H				Zonneveld, KAF; Brune, A; Willems, H			Spatial distribution of calcareous dinoflagellate cysts in surface sediments of the Atlantic Ocean between 13°N and 36°S.	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						calcareous algae; dinoflagellates; palaeo-ecology; palaeo-oceanography	EQUATORIAL ATLANTIC; QUATERNARY EASTERN; CALCIUM-CARBONATE; DEEP-SEA; ASSEMBLAGES; DISSOLUTION; CIRCULATION; RATES	To enhance the limited information available about the palaeo-ecological significance of calcareous dinoflagellates, we have studied their lateral distribution in surface sediments of the equatorial and south Atlantic between 13 degrees N and 36 degrees S. Calcareous dinoflagellate cysts appear to be widely distributed throughout the studied area. In the surface sediments, concentrations (cyst per gram dry sediment) of the vegetative stage Thoracosphaera heimii are generally higher than that of the (presumably) calcareous resting cysts. Distribution patterns in surface sediments of Orthopithonella granifera (Futterer) Keupp and Versteegh, Rhabdothorax spp. Kamptner., Sphaerodinella albatrosiana (Kamptner) Keupp and Versteegh S. albatrosiana praratabulated, Sphaerodinella tuberosa var. 1 (Kamptner) Keupp and Versteegh and S. tuberosa var. 2 and the ratios between these species have been compared with temperature, salinity, density and stratification gradients in the upper water column. Rhabdothorax spp. is characteristically present in sediments of more temperate regions characterized by high seasonality. Dinoflagellates producing these cysts are able to tolerate high nutrient concentrations, and mixing of the water column. S. albatrosiana is abundant in regions characterized by high sea surface temperatures and oligotrophic surface water conditions. In contrast, the distribution of S. tuberosa var. 2 is negatively related to temperature. The other cyst species did not show a characteristic pattern in relation to the studied environmental gradients. The ratio of Sphaerodinella tuberosa var. 2 to Orthopithonella granifera can be used for reconstructing the presence of stratification in the upper 50 m of the water column, whereas the ratios of S. tuberosa var. 2 to Sphaerodinella albatuosiana and of O. granifera to Rhabdothorax spp. might be used for palaeotemperature reconstructions. Calcareous dinoflagellate cysts are abundant in oligotrophic areas and may be useful for the reconstruction of palaeoenvironmental conditions. (C) 2000 Elsevier Science B.V. All rights reserved.	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.							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J. R., 1987, BOT MONOGR, V21; THUNELL RC, 1982, MAR GEOL, V47, P165, DOI 10.1016/0025-3227(82)90067-6; VERARDO DJ, 1994, PALEOCEANOGRAPHY, V9, P63, DOI 10.1029/93PA02901; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; Wefer G, 1996, SOUTH ATLANTIC, P461; WEFER G, 1996, BERICHTE FACHBEREICH, V79, P1; WILEMS H, 1992, Z GEOL WISSENSCHAFT, V20, P155; Willems H, 1996, GEOL MIJNBOUW, V75, P215; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; YOUNG JR, IN PRESS DEEP SEA RE, V2; Zugel Peter, 1994, Courier Forschungsinstitut Senckenberg, V176, P1	67	31	32	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	SEP	2000	111	3-4					197	223		10.1016/S0034-6667(00)00024-5	http://dx.doi.org/10.1016/S0034-6667(00)00024-5			27	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	362ZK	11035166				2025-03-11	WOS:000089808000002
J	Glasgow, HB; Burkholder, JM				Glasgow, HB; Burkholder, JM			Water quality trends and management implications from a five-year study of a eutrophic estuary	ECOLOGICAL APPLICATIONS			English	Review						Albemarle-Pamlico ecosystem; North Carolina; algal bloom; chlorophyll; estuary; fish kills; hypoxia; Neuse River and Estuary; nitrogen; phosphorus; river; suspended solids; toxic Pfiesteria complex	NEUSE RIVER ESTUARY; NORTH-CAROLINA; FISH KILLS; NUTRIENT LIMITATION; CHESAPEAKE BAY; ENVIRONMENTAL CONTROLS; DISTRIBUTION PATTERNS; SHALLOW ESTUARIES; COASTAL-PLAIN; PHYTOPLANKTON	The Neuse River and Estuary, a major tributary of the second largest estuary on the United States mainland, historically has sustained excessive blooms of algae and toxic dinoflagellates, hypoxia, and fish kills. Previous attempts have been made to use shortterm databases of 2-3 years, or data sets from infrequent (monthly) sampling, to assess whether nutrient inputs to the Neuse are increasing and supporting higher algal production. These previous efforts also have relied on single-point-determined flow velocity data, at upstream sites remote from the estuary, to estimate the volume of how in quantifying nutrient loading to the estuary. We completed a five-year study of the Neuse, including a comparative inventory of nutrients to the watershed from point sources and from concentrated animal operations (CAOs) as recent nonpoint sources, as well as an intensive assessment of water quality over time in the mesohaline estuary. Estimates of nutrient loads were based on volume of flow data from shore-to-shore transect cross sections, taken with a boat-mounted acoustic Doppler current profiler at the westernmost edge of the estuary. A total of 441 point dischargers contributed at least 3.34 x 10(8) L effluent/d to the Neuse system, much of which came from municipal wastewater treatment giants (2.03 x 10(8) L effluent/d, excluding periods of plant malfunctions; total annual loadings of at least 9 x 10(5) kg P and 2.1 x 10(6) kg N, with a 17% increase in human population over the past decade). The Neuse basin also included 554 CAOs, with 76% in swine production (1.7 x 10(6) animals, from a 285% increase in the past decade) and 23% in poultry (5.5 x 10(5) animals). An estimated 5.9 x 10(9) kg manure produced by swine and poultry during 1998 contributed similar to 4.1 x 10(7) kg N and 1.4 x 10(7) kg P to the Neuse watershed. About 20% of the area in the watershed now has enough manure from CAOs to exceed the P requirements of all nonlegume crops and forages. About two-thirds of the N- and P-rich feeds for these animals are imported (with 4.0 x 10(7) kg N and 1.6 x 10(7) kg P in 1998); thus, the watershed increasingly has become a nutrient sink. Over the five-year study in the Neuse Estuary study area, P loading significantly declined (by an estimated 14%), whereas TN (total nitrogen) loading significantly increased (by an average of 16%) and TNi (total inorganic nitrogen) increased by similar to 38%. The increased inorganic N (N-i), partly related to severe storms with high precipitation in years 4-5, coincided with a decrease in phytoplankton biomass (as chlorophyll a) that likely reflected displacement/washout of algal populations and cysts. Thus, while both N and P supplies have increased in the watershed, there is evidence for a significant increase in N-i loading but, as yet, no apparent signal for increased P in the lower estuary. Weather patterns ultimately control when/whether the elevated Ni supply will support increased algal production, so that estuarine algal blooms, hypoxia, and fish kills will remain difficult, at best, to predict in modeling efforts. We recommend that decadal data sets, with sufficient sampling frequency to capture nutrient loadings from major storm events, be used to assess fluctuations in algal production of lower rivers and estuaries, and relationships with changing nutrient inputs. Given increased N and P supplies in the Neuse watershed from ongoing growth of both human and swine populations, a current management goal of 30% N reduction should be altered to include increased focus on Ni and strengthened comanagement of P As for estuaries in other regions, nutrient reduction goals should be interpreted as "moving targets" that likely will have to be substantially adjusted upward, over time, to accomplish noticeable reductions in algal blooms, hypoxia, and fish kills in the lower Neuse River and Estuary.	N Carolina State Univ, Dept Bot, Raleigh, NC 27695 USA	North Carolina State University	Burkholder, JM (通讯作者)，N Carolina State Univ, Dept Bot, Box 7510, Raleigh, NC 27695 USA.							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Appl.	AUG	2000	10	4					1024	1046						23	Ecology; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	339UJ					2025-03-11	WOS:000088496000008
J	Reháková, D				Reháková, D			Calcareous dinoflagellate and calpionellid bioevents versus sea-level fluctuations recorded in the West-Carpathian (Late Jurassic/Early Cretaceous) pelagic environments	GEOLOGICA CARPATHICA			English	Article						Upper Jurassic; Lower Cretaceous; Western Carpathians; calcareous dinoflagellates; calpionellids; integrated biochronology; paleoecology; sea-level changes	EVOLUTION; GERMANY; SEDIMENTARY; CHALK	Recently established separate dinoflagellate cyst zonation combined with the successive calpionellid events contribute to the HIRES of the Upper Jurassic and Lower Cretaceous Tethyan pelagic carbonate sequences. Compositional changes in dinoflagellate and calpionellid assemblages are correlated with eustatic sea-level fluctuations. Thus, parallel calpionellid and cyst zonations give us more precise tools for the subdivision of deposits investigated as well as for better understanding and reconstruction of the paleoceanographical and paleoecological conditions of the ancient marine environments. The calcareous resting cyst distribution is shown to be influenced by the whole complex of environmental factors such as sea-level transgressive/regressive pulses, hydrological regime, nutrient content etc.	Slovak Acad Sci, Inst Geol, Bratislava 84226, Slovakia	Slovak Academy of Sciences	Reháková, D (通讯作者)，Slovak Acad Sci, Inst Geol, Dubravska Cesta 9, Bratislava 84226, Slovakia.		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Carpath.	AUG	2000	51	4					229	243						15	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	351FA					2025-03-11	WOS:000089146100002
J	Vonhof, HB; Smit, J; Brinkhuis, H; Montanari, A; Nederbragt, AJ				Vonhof, HB; Smit, J; Brinkhuis, H; Montanari, A; Nederbragt, AJ			Global cooling accelerated by early late Eocene impacts?	GEOLOGY			English	Article						eocene; meteorites; climate effects; ODP Site 689	PROJECT HOLE 689B; MAUD-RISE; OLIGOCENE TRANSITION; SHOCKED QUARTZ; SOUTHERN-OCEAN; STREWN FIELD; MASSIGNANO; BOUNDARY; AGE; MICROTEKTITES	At Ocean Drilling Program Site 689 (Maud Rise, Southern Ocean), delta(18)O records of fine-fraction bulk carbonate and benthic foraminifers indicate that accelerated climate cooling took place following at least two closely spaced early late Eocene extraterrestrial impact events. A simultaneous surface-water productivity increase, as interpreted front delta(13)C data, is explained by enhanced water-column mixing due to increased latitudinal temperature gradients. These isotope data appear to be in concert with organic-walled dinoflagellate-cyst records across the same microkrystite-bearing impact-ejecta layer in the mid-latitude Massignano section (central Italy). In particular, the strong abundance increase of Thalassiphora pelagica is interpreted to indicate cooling or increased productivity at Massignano. Because impact-induced cooling processes are active on time scales of a few years at most, the estimated 100 k.y: duration of the cooling event appears to be too long to be explained by impact scenarios alone. This implies that a feedback mechanism, such as a global albedo increase due to extended snow and ice cover, may have sustained impact-induced cooling for a longer time after the impacts.	Free Univ Amsterdam, Fac Earth Sci, NL-1081 HV Amsterdam, Netherlands; Univ Utrecht, Lab Palaeobot & Palynol, NL-3585 CD Utrecht, Netherlands; Osservatorio Geol & Coldigioco, I-62020 Frontale Di Apiro, MC, Italy; UCL, Dept Geol Sci, London WC1E 6BT, England	Vrije Universiteit Amsterdam; Utrecht University; University of London; University College London	Vonhof, HB (通讯作者)，Free Univ Amsterdam, Fac Earth Sci, Boelelaan 1085, NL-1081 HV Amsterdam, Netherlands.		Brinkhuis, Henk/B-4223-2009	Vonhof, Hubert/0000-0002-0897-8244; Smit, Jan/0000-0002-6070-4865; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], INITIAL REPORTS OCEA; [Anonymous], GEOLOGICAL SOC AM AB; Bottomley R, 1997, NATURE, V388, P365, DOI 10.1038/41073; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; BRINKHUIS H, 1995, EFFECTS IMPACTS ATMO, P40; Clymer AK, 1996, GEOLOGY, V24, P483, DOI 10.1130/0091-7613(1996)024<0483:SQFTLE>2.3.CO;2; DiesterHaass L, 1996, GEOLOGY, V24, P163, DOI 10.1130/0091-7613(1996)024<0163:EOTITS>2.3.CO;2; DIESTERHAASS L, 1995, PALAEOGEOGR PALAEOCL, V113, P311, DOI 10.1016/0031-0182(95)00067-V; Farley KA, 1998, SCIENCE, V280, P1250, DOI 10.1126/science.280.5367.1250; GLASS BP, 1985, J GEOPHYS RES-SOLID, V90, pD175, DOI 10.1029/JB090iS01p00175; Glass BP, 1999, METEORIT PLANET SCI, V34, P197, DOI 10.1111/j.1945-5100.1999.tb01746.x; GLASS BP, 1986, CHEM GEOL, V59, P181, DOI 10.1016/0168-9622(86)90070-9; GLASS BP, 1982, J GEOPHYS RES, V87, P425; KELLER G, 1986, MAR MICROPALEONTOL, V10, P267, DOI 10.1016/0377-8398(86)90032-0; Koeberl C, 1996, SCIENCE, V271, P1263, DOI 10.1126/science.271.5253.1263; KOEBERL C, 1988, P 19 LUN PLAN SCI C, P745; Kothe A., 1990, GEOLOGISCHES JB, V118; Langenhorst F, 1996, GEOLOGY, V24, P487, DOI 10.1130/0091-7613(1996)024<0487:COSQIL>2.3.CO;2; MAURRASSE F, 1974, CAR GEOL C T GUAD JU, P205; MEAD GA, 1995, PALEOCEANOGRAPHY, V10, P327, DOI 10.1029/94PA03069; MONTANARI A, 1993, PALAIOS, V8, P420, DOI 10.2307/3515017; Pierrard O, 1998, GEOLOGY, V26, P307, DOI 10.1130/0091-7613(1998)026<0307:ENRSIU>2.3.CO;2; POAG CW, 1994, GEOLOGY, V22, P691, DOI 10.1130/0091-7613(1994)022<0691:MMIOVS>2.3.CO;2; SANFILIPPO A, 1985, NATURE, V314, P613, DOI 10.1038/314613a0; Stott L.D., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P849, DOI 10.2973/odp.proc.sr.113.187.1990; Toon O.B., 1994, Hazards Due to Comets and Asteroids, P791; Vonhof HB, 1999, METEORIT PLANET SCI, V34, P747, DOI 10.1111/j.1945-5100.1999.tb01387.x; VONHOF HB, 1998, THESIS FREE U AMSTER; WEI W, 1994, PALAEOGEOGR PALAEOCL, V114, P101; WHITEHEAD J, 2000, P LUN PLAN SCI C 31; Zachos JC, 1996, PALEOCEANOGRAPHY, V11, P251, DOI 10.1029/96PA00571; [No title captured]	33	94	111	0	11	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0016-8505			GEOLOGY	Geology	AUG	2000	28	8					687	690						4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	339FC					2025-03-11	WOS:000088466100004
J	Eynaud, F; Turon, JL; Sánchez-Goñi, MF; Gendreau, S				Eynaud, F; Turon, JL; Sánchez-Goñi, MF; Gendreau, S			Dinoflagellate cyst evidence of 'Heinrich-like events' off Portugal during the Marine Isotopic Stage 5	MARINE MICROPALEONTOLOGY			English	Article						dinocyst; Bitectatodinium tepikiense; IRD; Portugal; last interglacial	NORTHEASTERN ATLANTIC-OCEAN; GLACIAL NORTH-ATLANTIC; LAST DEGLACIATION; PALYNOLOGICAL EVIDENCE; RECENT SEDIMENTS; IBERIAN MARGIN; ADJACENT SEAS; TORE SEAMOUNT; RECONSTRUCTION; TEMPERATURE	Dinoflagellate cysts were analysed from IMAGES core MD952042 (37 degrees 48'N; 10 degrees 01 'W) retrieved from the Tagus Abyssal Plain. Previous results of stable isotope and magnetic susceptibility measurements as well as of planktonic foraminiferal temperature reconstruction from this core, suggest the occurrence of "Heinrich-like events" (i.e. large ice-sheet decay) during Marine Isotopic Stage 5 (MIS 5). Dinoflagellate assemblages of this time period have revealed six dinocyst events that are characterised by peaks in Bitectatodinium tepikiense percentages. These events occur synchronously with "Heinrich-like events" previously identified. They are coeval with major retreats of the forest on land, indicating, therefore, drastic changes in the regional climate. However, results from the Ice-Rafted Detritus (IRD) analysis of the >150 mu m lithic fraction shows that MIS 5 of MD952042 has only recorded one significant input of iceberg discharge, located at the MIS 6/MIS 5 transition. It seems therefore that it is the only event that could be called a "true Heinrich event". (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Bordeaux 1, CNRS, UMR EPOC 5805, DGO, F-33405 Talence, Bourdeaux, France	Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Univ Bordeaux 1, CNRS, UMR EPOC 5805, DGO, 1 Ave Fac, F-33405 Talence, Bourdeaux, France.	eynaud@geocean.u-bordeaux.fr; turon@geocean.u-bordeaux.fr; mfsg@geocean.u-bordeaux.fr; s.gendreau@geocean.u-bordeaux.fr	Sanchez Goñi, Maria Fernanda/R-3699-2019	Sanchez Goni, Maria Fernanda/0000-0001-8238-7488; Eynaud, Frederique/0000-0003-1283-7425				ABRANTES F, 1991, MAR MICROPALEONTOL, V17, P285, DOI 10.1016/0377-8398(91)90017-Z; [Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Baas JH, 1997, PALAEOGEOGR PALAEOCL, V130, P1, DOI 10.1016/S0031-0182(96)00135-6; BARD E, 1987, NATURE, V328, P791, DOI 10.1038/328791a0; BIEBOW N, 1996, DINOFLAGELLATENZYSTE, V57; BOULDOIRE X, 1996, AGU FALL M, pF21; CANDON L, 1996, AGU FALL M, pF21; Cayre O, 1999, PALEOCEANOGRAPHY, V14, P384, DOI 10.1029/1998PA900027; CAYRE O, 1996, AGU FALL M, pF21; CAYRE O, 1997, THESIS U AIX MARSEIL; CAYRE O, 1997, EUG STRASB, P618; Combourieu-Nebout N, 1998, QUATERNARY SCI REV, V17, P303, DOI 10.1016/S0277-3791(97)00039-5; COSTE B, 1986, OCEANOL ACTA, V9, P149; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; 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, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; DEVERNAL A, 1996, CAHIERS GEOTOP, P1; DEVILLERS R, 1998, MUS RAPP BOT 1, P32; DODGE JD, 1991, NEW PHYTOL, V118, P593, DOI 10.1111/j.1469-8137.1991.tb01000.x; FENSOME RA, 1998, 3653 DINOFLAJ GEOL S; FIUZA AFD, 1982, OCEANOL ACTA, V5, P31; Goñi MFS, 1999, EARTH PLANET SC LETT, V171, P123; GROUSSET FE, 1993, PALEOCEANOGRAPHY, V8, P175, DOI 10.1029/92PA02923; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HARLAND R, 1995, HOLOCENE, V5, P220, DOI 10.1177/095968369500500210; HEINRICH H, 1988, QUATERNARY RES, V29, P142, DOI 10.1016/0033-5894(88)90057-9; LANCELOT Y, 1998, PAGES OP SCI M; Lebreiro SM, 1996, MAR GEOL, V131, P47, DOI 10.1016/0025-3227(95)00142-5; Lebreiro SM, 1997, PALEOCEANOGRAPHY, V12, P718, DOI 10.1029/97PA01748; LENTIN JK, 1989, AASP FDN, V20; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; MARRET F, 1994, MAR GEOL, V118, P107, DOI 10.1016/0025-3227(94)90115-5; Marret F., 1993, PALYNOSCIENCES, V2, P267; MARTINSON DG, 1987, QUATERNARY RES, V27, P1, DOI 10.1016/0033-5894(87)90046-9; Maslin M, 1998, GEOL SOC SPEC PUBL, V131, P91, DOI 10.1144/GSL.SP.1998.131.01.07; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; MATTHIESSEN J, 1997, GRZYBOWSKI FDN SPECI, P149; MCMANUS JF, 1994, NATURE, V371, P326, DOI 10.1038/371326a0; Morzadec-Kerfourn M. 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L., 1984, MEMOIRES I GEOLOGIE, V17; TURON JL, 1978, CR ACAD SCI D NAT, V286, P1861; TURON JL, 1995, 14 S APLF PAL CHANG; vanWeering TCE, 1996, MAR GEOL, V131, P1, DOI 10.1016/0025-3227(95)00140-9; VERBITSKY M, 1995, PALEOCEANOGRAPHY, V10, P59, DOI 10.1029/94PA02815; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	64	43	43	0	7	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	AUG	2000	40	1-2					9	21		10.1016/S0377-8398(99)00045-6	http://dx.doi.org/10.1016/S0377-8398(99)00045-6			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	346GA					2025-03-11	WOS:000088861400002
J	Louwye, S; De Coninck, J; Verniers, J				Louwye, S; De Coninck, J; Verniers, J			Shallow marine Lower and Middle Miocene deposits at the southern margin of the North Sea Basin (northern Belgium): dinoflagellate cyst biostratigraphy and depositional history	GEOLOGICAL MAGAZINE			English	Article							EASTERN ENGLAND; PLIOCENE; STRATIGRAPHY	Detailed dinoflagellate cyst analysis of the Lower-Middle Miocene Berchem Formation at the southernmost margin of the North Sea Basin (northern Belgium) allowed a precise biostratigraphical positioning and a reconstruction of the depositional history. The two lower members of the formation (Edegem Sands and decalcified Kiel Sands) are biostratigraphically regarded as one unit since no significant break within the dinocyst assemblages is observed. The base of this late (or latest) Aquitanian-Burdigalian unit coincides with sequence boundary Aq3/Burl as defined by Hardenbol and others, in work published in 1998. A hiatus at the Lower-Middle Miocene transition separates the upper member (the Antwerpen Sands) from the underlying member. The greater part of the Antwerpen Sands were deposited in a Langhian (latest Burdigalian?)-middle Serravallian interval. The base of this unit coincides with sequence boundary Bur5/Lan1. Biostratigraphical correlation points to a diachronous post-depositional decalcification within the formation since parts of the decalcified Kiel Sands can be correlated with parts of the calcareous fossil-bearing section, up to now interpreted as Antwerpen Sands. The dinoflagellate cyst assemblages are dominated by species with a inner neritic preference, although higher numbers of oceanic taxa in the upper part of the formation indicate incursions of oceanic watermasses into the confined depositional environment of the southern North Sea Basin.	State Univ Ghent, Lab Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，State Univ Ghent, Lab Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Verniers, Jacques/B-8024-2009; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				[Anonymous], 2003, STUD GEOPHYS GEOD; 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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JUL	2000	137	4					381	394		10.1017/S0016756800004258	http://dx.doi.org/10.1017/S0016756800004258			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	353JB					2025-03-11	WOS:000089270100004
J	Kremp, A; Anderson, DM				Kremp, A; Anderson, DM			Factors regulating germination of resting cysts of the spring bloom dinoflagellate <i>Scrippsiella hangoei</i> from the northern Baltic Sea	JOURNAL OF PLANKTON RESEARCH			English	Article							GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; DINOPHYCEAE; SEDIMENTATION; EXCYSTMENT; TEMPERATURE; DARKNESS; EGGS	The role of cyst germination as a factor in bloom initiation was investigated for the dinoflagellate Scrippsiella hangoei (Schiller) Larsen from the northern Baltic Sea. This species blooms in very cold, often ice-covered waters, and is responsible for a significant fraction of the production in that region. Dormancy, temperature, oxygen and light were studied as factors potentially controlling the germination of S. hangoei resting cysts. Laboratory-stored and field-collected cysts began to germinate in December following a mandatory dormancy period lasting 6 months. Germination after this maturation interval was maximal when temperatures were within a 0-9 degrees C 'window'. Mandatory dormancy is therefore the primary factor regulating the timing of germination in this species, as temperatures in the natural environment normally fall within this range at the time when S. hangoei cysts deposited the preceding year have matured. Non-optimal temperatures, darkness and low oxygen conditions all maintain a state of quiescence in the cysts. Cysts could germinate in darkness, but the rate of excystment was significantly higher in the light. Likewise, excystment was completely inhibited in anoxic conditions and was reduced under severe hypoxia, with normal germination under moderate hypoxic concentrations. Temporary exposure to high sulfide concentrations permanently reduced germination potential, indicating that S. hangoei cysts have low resistance to oxygen deficiency. Prolonged periods of anoxia at the sediment surface, as frequently occurs in the study area, might reduce the size of the viable cyst pool and thus, alter the magnitude of the inoculum for S. hangoei bloom initiation. Together, these internal and external regulatory factors play important roles in the bloom dynamics of this important dinoflagellate.	Univ Helsinki, Div Hydrobiol, Dept Systemat & Ecol, FIN-00014 Helsinki, Finland; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	University of Helsinki; Woods Hole Oceanographic Institution	Kremp, A (通讯作者)，Univ Helsinki, Div Hydrobiol, Dept Systemat & Ecol, POB 17, FIN-00014 Helsinki, Finland.		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Plankton Res.	JUL	2000	22	7					1311	1327		10.1093/plankt/22.7.1311	http://dx.doi.org/10.1093/plankt/22.7.1311			17	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	337XT		Green Submitted, Bronze			2025-03-11	WOS:000088389100006
J	Nagasaki, K; Yamaguchi, M; Imai, I				Nagasaki, K; Yamaguchi, M; Imai, I			Algicidal activity of a killer bacterium against the harmful red tide dinoflagellate <i>Heterocapsa circularisquama</i> isolated from Ago Bay, Japan	NIPPON SUISAN GAKKAISHI			Japanese	Article							HETEROSIGMA-AKASHIWO VIRUS; RAPHIDOPHYCEAE; GROWTH; SEA	Algicidal activity of a bacterium strain Cytophaga sp. AA8-2 against the harmful red tide causing alga Heterocapsa circularisquama was investigated. Physiological conditions of host cells, incubation temperature and existence of ambient organic substrates or co-existing bacteria affected the lethal effect of Cytophaga sp. AA8-2. Bacterial lysis of H. circularisquama was caused more rapidly at higher incubation temperature (20-30 degrees C). Growth of 6 among 7 H. circularisquama strains tested was inhibited by Cytophaga sp. AA8-2, the levels of which were varied. Apart of H. circularisquama cells in a culture formed temporary cysts to survive the bacterial attack. The envelope of the temporary cyst of H. circularisquama was composed of a markedly thicker layered structure (209+/-72 nm) than that of the vegetative cell (40+/-15 nm).	Natl Res Inst Fisheries & Environm Inland Sea, Harmful Phytoplankton Sect, Harmful Algal Bloom Div, Hiroshima 7390452, Japan; Kyoto Univ, Grad Sch Agr, Lab Marine Environm Microbiol, Kyoto 6068502, Japan	Japan Fisheries Research & Education Agency (FRA); Kyoto University	Nagasaki, K (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Harmful Phytoplankton Sect, Harmful Algal Bloom Div, Hiroshima 7390452, Japan.							CHEN LCM, 1969, J PHYCOL, V5, P211, DOI 10.1111/j.1529-8817.1969.tb02605.x; FUKAMI K, 1992, NIPPON SUISAN GAKK, V58, P1073; FUKAMI K, 1998, HARMFUL TOXIC ALGAL, P335; HARA Y, 1982, Japanese Journal of Phycology, V30, P47; Honjo T, 1998, HARMFUL ALGAE, P224; Horiguchi Takeo, 1995, Phycological Research, V43, P129, DOI 10.1111/j.1440-1835.1995.tb00016.x; IMAI I, 1993, MAR BIOL, V116, P527, DOI 10.1007/BF00355470; ISHIDA Y, 1986, MAR ECOL PROG SER, V30, P197, DOI 10.3354/meps030197; Kim MC, 1998, MAR ECOL PROG SER, V170, P25, DOI 10.3354/meps170025; Kondo R, 1999, FISHERIES SCI, V65, P432, DOI 10.2331/fishsci.65.432; Nagasaki K, 1998, AQUAT MICROB ECOL, V15, P211, DOI 10.3354/ame015211; Nagasaki K, 1999, APPL ENVIRON MICROB, V65, P898; Nagasaki K, 1997, AQUAT MICROB ECOL, V13, P135, DOI 10.3354/ame013135; Nagasaki K, 1998, AQUAT MICROB ECOL, V14, P109, DOI 10.3354/ame014109; Uchida T, 1999, J EXP MAR BIOL ECOL, V241, P285, DOI 10.1016/S0022-0981(99)00088-X	15	42	47	0	3	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	JUL	2000	66	4					666	673						8	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	350ZM					2025-03-11	WOS:000089131600013
J	Höll, C; Zonneveld, KAF; Willems, H				Höll, C; Zonneveld, KAF; Willems, H			Organic-walled dinoflagellate cyst assemblages in the tropical Atlantic Ocean and oceanographical changes over the last 140 ka	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Atlantic; cyst; dinoflagellate; palaeoenvironment; Quaternary; tropical	SEA-SURFACE TEMPERATURE; SOUTH-ATLANTIC; INDIAN-OCEAN; EQUATORIAL ATLANTIC; SEASONAL CYCLE; ADJACENT SEAS; LABRADOR SEA; ICE AGES; SEDIMENTS; DEGLACIATION	A palaeoceanographic reconstruction of the Late Quaternary tropical Atlantic Ocean has been made on the basis of dinoflagellate cyst associations of two sediment cores: the first core was recovered from below the highly productive waters of the equatorial divergence and the second from the oligotrophic western tropical Atlantic Ocean. Palaeoenvironmental indicators for productivity, sea surface temperature (SST) and salinity (SSS) based on selected organic-walled dinoflagellate cyst species have been established. On the basis of these palaeoenvironmental indicators, a strengthened intensity of the equatorial divergence in the eastern region during glacials and cold periods of interglacials has been reconstructed. The highest SST probably occurred around substage 5.5 and might refer to weakest upwelling intensity. In comparison, SST and SSS appear to have been generally higher in the western tropical Atlantic Ocean, with probably enhanced values during glacial intervals. Pronounced differences in accumulation rates and relative abundances of cysts formed by congruentidiacean dinoflagellates and relative abundances of oligotrophic cyst species between the eastern and the western region can be related to differences in palaeoproductivity, suggesting much higher values in the eastern area. The coherence between variation in frequency of the indicators for productivity and the boreal summer insolation and monsoon intensity in the eastern tropical Atlantic Ocean suggests an oceanographic reflection of regional intertropical, rather than boreal, dynamics. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-23334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-23334 Bremen, Germany.	willems@micropal.uni-bremen.de						AKSU AE, 1992, PALAEOGEOGR PALAEOCL, V92, P121, DOI 10.1016/0031-0182(92)90138-U; AKSU AE, 1985, MAR MICROPALEONTOL, V9, P537, DOI 10.1016/0377-8398(85)90017-9; [Anonymous], 1969, HOT BRINES RECENT HE; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; Berger WH., 1989, PRODUCTIVITY OCEAN P, P429; Bickert T, 1996, SOUTH ATLANTIC, P599; BICKERT T, 1992, THESIS BER FACHBER G, V27; BIEBOW N, 1995, THESIS C ALBRECHTS U; Billups K, 1996, PALEOCEANOGRAPHY, V11, P217, DOI 10.1029/95PA03773; BLEIL U, 1994, METEOR BERICHTE, V941; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BREWSTERWINGARD GL, 1996, 96732 US GEOL SURV; *CLIMAP PROJ MEMB, 1981, GSA MAP CHART SERIES, V36; CRANFIELD DE, 1989, DEEP-SEA RES, V36, P121; Curry WB, 1996, SOUTH ATLANTIC, P577; DALE B, 1985, NORSK GEOL TIDSSKR, V65, P97; DALE B., 1994, CARBON CYCLING GLOBA, P521; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; Durkoop A, 1997, PALEOCEANOGRAPHY, V12, P764, DOI 10.1029/97PA02270; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; EDWARDS LE, 1996, 9 INT PAL C HOUST TE, P37; Emerson S, 1988, PALEOCEANOGRAPHY, V3, P621, DOI 10.1029/PA003i005p00621; Emerson S., 1985, CARBON CYCLE ATMOSPH, V32, P78, DOI DOI 10.1029/GM032P0078; EPPLEY RW, 1974, 1ST P INT C TOX DIN, P11; Fensome R.A., 1993, SPECIAL PUBLICATION; Giraudeau J., 1992, Mem. 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L., 1998, AM ASS STRATIGRAPHIC, V34; Zonneveld KAF, 1996, PALAEOGEOGR PALAEOCL, V122, P89, DOI 10.1016/0031-0182(95)00091-7; Zonneveld KAF, 1997, QUATERNARY SCI REV, V16, P187, DOI 10.1016/S0277-3791(96)00049-2; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; ZONNEVELD KAF, 1995, REV PALAEOBOT PALYNO, V84, P221, DOI 10.1016/0034-6667(94)00117-3; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	73	6	7	1	3	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	JUL 1	2000	160	1-2					69	90		10.1016/S0031-0182(00)00047-X	http://dx.doi.org/10.1016/S0031-0182(00)00047-X			22	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	327ZN					2025-03-11	WOS:000087824500005
J	Höll, C; Kemle-von Mücke, S				Höll, C; Kemle-von Mücke, S			Late Quaternary upwelling variations in the eastern equatorial Atlantic Ocean as inferred from dinoflagellate cysts, planktonic foraminifera, and organic carbon content	QUATERNARY RESEARCH			English	Article						dinoflagellates; planktonic foraminifera; stable oxygen isotopes; eastern equatorial Atlantic upwelling; late Quaternary	FRACTIONATION; CIRCULATION; ATMOSPHERE; SEDIMENTS; NORTH; SEA	Analysis of multiple proxies shows that eastern equatorial Atlantic upwelling was subdued during isotope stage 5.5, more intense during stages 4, 5.2, 5.4, and 6, and most intense early in stage 2. These findings are based on proxy measures from a core site about 600 km southwest of Liberia. The proxies include total organic carbon content, the ratio of peridinoid and oceanic organic-walled dinoflagellate cyst species, accumulation rates of calcareous dinoflagellates, estimates of sea surface paleotemperatures, the difference in stable oxygen isotope composition between two species of planktonic foraminifera that lire at different water depths, and the abundance of the planktonic foraminifera Neogloboquadrina dutertrei. Most of these parameters consistently vary directly or inversely with one another. Slight discrepancies between the individual parameters show the usefulness of a multiple proxy approach to reconstruct paleoenvironments. Our data confirm that northern summer insolation strongly influences upwelling in the eastern equatorial Atlantic Ocean. (C) 2000 University of Washington.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Univ Bremen, Fachbereich Geowissensch 5, Postfach 330 440, D-28334 Bremen, Germany.	hoell@micropal.uni-bremen.de						AKSU AE, 1992, PALAEOGEOGR PALAEOCL, V92, P121, DOI 10.1016/0031-0182(92)90138-U; [Anonymous], 1989, Utrecht Micropaleontological Bulletins; Baumann K.-H., 1999, USE PROXIES PALEOCEA, P117, DOI [10.1007/978-3-642-58646, DOI 10.1007/978-3-642-58646-0_4]; BERGER WH, 1967, SCIENCE, V156, P383, DOI 10.1126/science.156.3773.383; BONNEAU MC, 1980, OCEANOL ACTA, V3, P377; BOYLE EA, 1982, SCIENCE, V218, P784, DOI 10.1126/science.218.4574.784; DITTERT N, 1998, 126 U BREM FACHB GEO; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; EPSTEIN S, 1953, GEOL SOC AM BULL, V64, P1315, DOI 10.1130/0016-7606(1953)64[1315:RCITS]2.0.CO;2; FAIRBANKS RG, 1982, NATURE, V298, P841, DOI 10.1038/298841a0; HASTENRATH S, 1987, J PHYS OCEANOGR, V17, P1518, DOI 10.1175/1520-0485(1987)017<1518:ACOSTS>2.0.CO;2; Hemleben C., 1989, MODERN PLANKTONIC FO, DOI [10.1007/978-1-4612-3544-6, DOI 10.1007/978-1-4612-3544-6]; HERBLAND A, 1979, J MAR RES, V37, P87; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; Imbrie J., 1971, LATE CENOZOIC GLACIA, P71; Imbrie J., 1984, Milankovitch and Climate: Understanding the Response to Astronomical Forcing, -, V1, P269; JONES JAMES I., 1967, MICRO PALEONTOLOGY [NY], V13, P489, DOI 10.2307/1484724; Kemle-von Mucke S., 1999, USE PROXIES PALEOCEA, P91, DOI DOI 10.1007/978-3-642-58646-03; Kemle-von Mucke Sylvia, 1999, P43; KEMLEVONMUCKE S, 1994, 55 U BREM FACHB GEOW; Levitus S., 1982, 13 NOAA, DOI [10.1029/EO064i049p00962-02, DOI 10.1029/EO064I049P00962-02]; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; LYLE M, 1988, NATURE, V335, P529, DOI 10.1038/335529a0; MARTINSON DG, 1987, QUATERNARY RES, V27, P1, DOI 10.1016/0033-5894(87)90046-9; McIntyre A, 1989, PALEOCEANOGRAPHY, V4, P19, DOI 10.1029/PA004i001p00019; MEINECKE G, 1992, 29 U BREM FACHB GEOW; Mix AC, 1996, SOUTH ATLANTIC, P503; PETERSON RG, 1991, PROG OCEANOGR, V26, P1, DOI 10.1016/0079-6611(91)90006-8; Pflaumann U, 1996, PALEOCEANOGRAPHY, V11, P15, DOI 10.1029/95PA01743; PHILANDER SGH, 1986, J GEOPHYS RES-OCEANS, V91, P14192, DOI 10.1029/JC091iC12p14192; PRELL WL, 1987, J GEOPHYS RES-ATMOS, V92, P8411, DOI 10.1029/JD092iD07p08411; Ravelo AC, 1990, PALEOCEANOGRAPHY, V5, P409, DOI 10.1029/PA005i003p00409; Ravelo AC, 1992, PALEOCEANOGRAPHY, V7, P815, DOI 10.1029/92PA02092; SHACKLETON NJ, 1983, NATURE, V306, P319, DOI 10.1038/306319a0; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wefer G, 1996, SOUTH ATLANTIC, P461; WEFER G, 1989, 7 U BREM FACHB GEOW; Wolff T, 1999, PALEOCEANOGRAPHY, V14, P374, DOI 10.1029/1999PA900011; ZONNEVELD KAF, IN PRESS REV PALAEOB	41	7	7	0	1	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0033-5894	1096-0287		QUATERNARY RES	Quat. Res.	JUL	2000	54	1					58	67		10.1006/qres.2000.2139	http://dx.doi.org/10.1006/qres.2000.2139			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	337TD					2025-03-11	WOS:000088377000006
J	Shi, N; Dupont, LM; Beug, HJ; Schneider, R				Shi, N; Dupont, LM; Beug, HJ; Schneider, R			Correlation between vegetation in southwestern Africa and oceanic upwelling in the past 21,000 years	QUATERNARY RESEARCH			English	Article						aridification; upwelling; pollen; dinoflagellate cyst; interhemispheric asynchrony; southwestern Africa	DINOFLAGELLATE CYSTS; CLIMATE CHANGES; ICE-CORE; LEVEL FLUCTUATIONS; EQUATORIAL AFRICA; ISOTOPE PROFILES; MARINE-SEDIMENTS; SOUTHERN-AFRICA; NORTH-ATLANTIC; ADJACENT SEAS	Dinoflagellate cyst and pollen records from marine sediments off the southwestern African coast reveal three major aridification periods since the last glaciation and an environmental correlation between land and sea. Abundant pollen of desert, semi-desert, and temperate plants 21,000-17,500 cal yr B.P. show arid and cold conditions in southwestern Africa that correspond to low sea surface temperatures and enhanced upwelling shown by dinoflagellate cysts. Occurrence of Restionaceae in the pollen record suggests northward movement of the winter-rain regime that influenced the study area during the last glacial maximum. Decline of Asteroideae, Restionaceae, and Ericaceae in the pollen record shows that temperate vegetation migrated out of the study area about 17,500 cal yr B.P., probably because of warming during the last deglaciation. The warming in southwestern Africa was associated with weakened upwelling and increased sea surface temperatures, 2000-2800 years earlier than in the Northern Hemisphere. Aridification 14,300-12,600 cal Jr B.P. is characterized by a prominent increase of desert and semi-desert pollen without the return of temperate vegetation. This aridification corresponds to enhanced upwelling off Namibia and cooler temperatures in Antarctica, and it might have been influenced by oceanic thermohaline circulation. Aridification 11,000-8900 cal yr B.P, is out of phase with the northern African climate. Reduction of the water vapor supply in southwestern Africa at that time may be related to northward excursions of the Intertropical Convergence Zone. (C) 2000 University of Washington.	Univ Gottingen, D-37073 Gottingen, Germany; Univ Bremen, D-28334 Bremen, Germany	University of Gottingen; University of Bremen	Shi, N (通讯作者)，Univ Gottingen, Wilhelm Weber St 2, D-37073 Gottingen, Germany.			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Res.	JUL	2000	54	1					72	80		10.1006/qres.2000.2145	http://dx.doi.org/10.1006/qres.2000.2145			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	337TD					2025-03-11	WOS:000088377000008
J	McCarthy, FMG; Gostlin, KE				McCarthy, FMG; Gostlin, KE			Correlating Pleistocene sequences across the New Jersey margin	SEDIMENTARY GEOLOGY			English	Article; Proceedings Paper	Annual Meeting of the Geological-Society-of-America	OCT 26-29, 1998	TORONTO, CANADA	Geol Soc Amer		palynomorphs; dinocysts; quaternary; sequence stratigraphy	WESTERN NORTH-ATLANTIC; DINOFLAGELLATE CYSTS; SEA-LEVEL; QUATERNARY SEDIMENTS; POLLEN DISTRIBUTION; FORTRAN-77 PROGRAM; BOTTOM SEDIMENTS; MARINE-SEDIMENTS; COASTAL-PLAIN; ADJACENT SEAS	The biostratigraphic ranges of palynomorphs, as well as climatostratigraphic changes recorded by both marine and terrestrial palynomorphs, provide one of the few means of dating and correlating neritic environments where calcareous microfossils are rare. The transport of terrestrial palynomorphs to marine environments also allows for direct land-sea correlation. In addition, palynological assemblages provide insights into sediment transport and sea levels. Over 500 m of upper Pleistocene sediments were recovered in ODP Hole 1073A on the upper New Jersey slope. Palynomorphs in this Hole record rapid progradation during the late Pleistocene. A prominent unconformity, pp3(s), forms the upper boundary of this thick progradational sequence. Palynological analysis from ODP Sites 1072 and 1073 allows this surface to be correlated from the outer shelf to the upper slope, and also suggests that it was generated during a sea level lowstand, probably during Oxygen Isotope Stage 12 (similar to 450-425 ka). Both the Atlantic Coastal Plain and ODP Site 1072 on the outer New Jersey shelf appear to have become erosional during this progradational phase which began around the time that the magnitude of Northern Hemisphere ice accumulation increased. This suggests that sediments prograded across the New Jersey margin as accommodation in inner neritic and coastal environments decreased in response to amplified glacioeustatic fluctuation and substantially increased sediment availability (supplied by glacial erosion). Erosion associated with the generation of unconformity pp3(s) appears to have increased accommodation on the New Jersey margin, allowing sediments to aggrade on the continental shelf and even to accumulate on the Atlantic Coastal Plain during interglacial highstands. The upper Pleistocene architecture of the New Jersey margin appears to have been controlled by glacioeustatic fluctuations and the accompanying increase in sediment supply. In contrast, unconformable surface pp4(s) is more complex and separates upper Miocene sediments deposited between 7.4 and 5.9 Ma from lower Pleistocene sediments deposited prior to approximately 1.4 Ma in Hole 1072A, whereas in Hole 1073A, pp4(s) is in sediments of early Pleistocene age, between 1.6 and 1.3 Ma. These data suggest that unconformity pp4(s) was generated during the early Pleistocene, but there is no clear palynological evidence that glacioeustasy was responsible for the generation of this unconformity. (C) 2000 Elsevier Science B.V. All rights reserved.	Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Brock University	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.							AUSTIN JA, 1998, INITIAL REPORTS OD A, V174; AUSTIN JA, 1998, ODP INIT REPTS A, V174, P99; BENNINGHOFF W. 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Geol.	JUL	2000	134	1-2					181	196		10.1016/S0037-0738(00)00019-1	http://dx.doi.org/10.1016/S0037-0738(00)00019-1			16	Geology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Geology	341YG					2025-03-11	WOS:000088618100012
J	Stoecker, DK; Gustafson, DE; Baier, CT; Black, MMD				Stoecker, DK; Gustafson, DE; Baier, CT; Black, MMD			Primary production in the upper sea ice	AQUATIC MICROBIAL ECOLOGY			English	Article						sea ice; Antarctica; McMurdo Sound; ice algae; cysts; hypnozygotes; dinoflagellates; Polarella; diatoms; chrysophytes; primary productivity	ANTARCTIC PACK-ICE; PHOTOSYNTHESIS-IRRADIANCE RELATIONSHIPS; MICROBIAL COMMUNITIES SIMCO; CHLOROPHYLL-A-CARBON; MCMURDO-SOUND; WEDDELL SEA; ALGAE; MICROALGAE; ASSEMBLAGES; NUTRIENT	Observations and experiments were conducted on fast ice in McMurdo Sound, Antarctica, to investigate seasonal changes in primary production in the upper sea ice interior. In November and early December 1995, a dense phytoflagellate assemblage developed in the brine channels and pockets at a snow-free site. Primary production was calculated from C-14 measurements of primary productivity in brine samples combined with estimates of the proportion of the ice volume occupied by brine. On 4 December 1995, when the dinoflagellate Polarella glacialis dominated, estimated daily production peaked at 12.4 mg C m(-2) in the upper 50 cm of ice. On this date, brine temperature was similar to-3 degrees C and brine salinity was similar to 60. By mid-December, daily production declined by 77%, but chlorophyll-specific rates of photosynthesis remained high. The decline in production coincided with encystment of P. glacialis and nutrient depletion, the former triggered by the latter. Primary production continued to decrease during December and January. On 9 January 1996, when ice temperatures were similar to-1 degrees C and brine salinity was similar to 20, there was a brief bloom of small pennate diatoms in the upper ice interior, but chlorophyll-specific rates of photosynthesis were low and estimated daily production was <1 mg C m(-2). Based on C-14 uptake and brine volume, algal production in the upper 50 cm of sea ice was 181 mg C m(-2) for the season (mid-November through mid-January). Increases in phytoflagellate biomass in the upper 90 cm of ice for this same period indicated that production was greater than or equal to 256 mg C m(-2). Brief early season blooms of cryo- and halo-tolerant phytoflagellates accounted for most of the primary production in the upper sea ice interior.	Univ Maryland, Horn Point Environm Lab, Ctr Environm Sci, Cambridge, MD 21613 USA	University System of Maryland; University of Maryland Center for Environmental Science	Univ Maryland, Horn Point Environm Lab, Ctr Environm Sci, POB 775, Cambridge, MD 21613 USA.	stoecker@hpl.umces.edu	stoecker, diane/F-9341-2013; Black, Megan/G-6410-2016	Black, Megan/0000-0001-5511-1419				ACKLEY SF, 1979, DEEP-SEA RES, V26, P269, DOI 10.1016/0198-0149(79)90024-4; ACKLEY SF, 1994, DEEP-SEA RES PT I, V41, P1583, DOI 10.1016/0967-0637(94)90062-0; [Anonymous], 2012, Biometry; Archer SD, 1996, MAR ECOL PROG SER, V135, P179, DOI 10.3354/meps135179; Arrigo K, 1998, ANTARCT RES SER, V73, P23; ARRIGO KR, 1991, J GEOPHYS RES-OCEANS, V96, P10581, DOI 10.1029/91JC00455; Arrigo KR, 1997, SCIENCE, V276, P394, DOI 10.1126/science.276.5311.394; ARRIGO KR, 1995, MAR ECOL PROG SER, V127, P255, DOI 10.3354/meps127255; Buck KR, 1998, POLAR BIOL, V20, P377, DOI 10.1007/s003000050317; DIECKMANN GS, 1991, POLAR BIOL, V11, P449; FRITSEN CH, 1994, SCIENCE, V266, P782, DOI 10.1126/science.266.5186.782; GARRISON DL, 1991, MAR ECOL PROG SER, V75, P161, DOI 10.3354/meps075161; GARRISON DL, 1986, BIOSCIENCE, V36, P243, DOI 10.2307/1310214; GARRISON DL, 1989, POLAR BIOL, V10, P211; Geider RJ, 1997, MAR ECOL PROG SER, V148, P187, DOI 10.3354/meps148187; GLEITZ M, 1995, MAR CHEM, V51, P81, DOI 10.1016/0304-4203(95)00053-T; GLEITZ M, 1991, POLAR BIOL, V11, P385; GRADINGER R, 1991, POLAR RES, V10, P295, DOI 10.1111/j.1751-8369.1991.tb00655.x; GRADINGER R, 1992, POLAR BIOL, V12, P727; HENLEY WJ, 1993, J PHYCOL, V29, P729, DOI 10.1111/j.0022-3646.1993.00729.x; HOLEN DA, 1995, CHRYSOPHYTE ALGAE, P119; HORNER R, 1992, POLAR BIOL, V12, P417; HSIAO SIC, 1980, ARCTIC, V33, P768; Ikavalko J, 1997, POLAR BIOL, V17, P473, DOI 10.1007/s003000050145; JASSBY AD, 1976, LIMNOL OCEANOGR, V21, P540, DOI 10.4319/lo.1976.21.4.0540; KIRST GO, 1995, J PHYCOL, V31, P181, DOI 10.1111/j.0022-3646.1995.00181.x; KOTTMEIER ST, 1988, POLAR BIOL, V8, P293, DOI 10.1007/BF00263178; LEGENDRE L, 1992, POLAR BIOL, V12, P429; LIZOTTE MP, 1992, POLAR BIOL, V12, P497; LIZOTTE MP, 1991, MAR ECOL PROG SER, V71, P175, DOI 10.3354/meps071175; Maykut G.A., 1985, Sea Ice Biota, P21; MCCONVILLE MJ, 1983, J PHYCOL, V19, P431, DOI 10.1111/j.0022-3646.1983.00431.x; Mock T, 1999, MAR ECOL PROG SER, V177, P15, DOI 10.3354/meps177015; Montresor M, 1999, J PHYCOL, V35, P186, DOI 10.1046/j.1529-8817.1999.3510186.x; PALMISANO AC, 1983, POLAR BIOL, V2, P171, DOI 10.1007/BF00448967; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; RAND JH, 1985, CORPS ENG PUBL, V8521; Robinson DH, 1997, MAR ECOL PROG SER, V147, P243, DOI 10.3354/meps147243; Sandgren C.D., 1988, P9; Stoecker DK, 1999, J EUKARYOT MICROBIOL, V46, P397, DOI 10.1111/j.1550-7408.1999.tb04619.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; SYVERTSEN EE, 1993, POLAR BIOL, V13, P61; Watanabe K., 1990, P136; WEEKS WF, 1982, CORPS ENG MONOGR, V821; WEISSENBERGER J, 1992, LIMNOL OCEANOGR, V37, P179, DOI 10.4319/lo.1992.37.1.0179; WELSCHMEYER NA, 1984, LIMNOL OCEANOGR, V29, P135, DOI 10.4319/lo.1984.29.1.0135; Wheeler PA, 1996, NATURE, V380, P697, DOI 10.1038/380697a0	50	39	44	0	23	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055	1616-1564		AQUAT MICROB ECOL	Aquat. Microb. Ecol.	JUN 15	2000	21	3					275	287		10.3354/ame021275	http://dx.doi.org/10.3354/ame021275			13	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	327UV		Bronze			2025-03-11	WOS:000087813000007
J	Karwath, B; Janofske, D; Tietjen, F; Willems, H				Karwath, B; Janofske, D; Tietjen, F; Willems, H			Temperature effects on growth and cell size in the marine calcareaous dinoflagellate <i>Thoracospaera heimii</i>	MARINE MICROPALEONTOLOGY			English	Article; Proceedings Paper	7th Conference of the International-Nannoplankton-Association (INA7)	FEB, 1998	PUERTO RICO	Int Nannoplankton Assoc		marine; calcareous dinoflagellates; growth; culture experiments; actuopalaeontology	QUATERNARY EASTERN; LIFE-CYCLE; DINOPHYCEAE; ATLANTIC; CYSTS	Growth experiments were carried out on the marine calcareous dinoflagellate Thoracosphaera heimii. Two strains (A603, GeoB 86) of the phototrophic, predominantly vegetative coccoid T. heimii were cultured at different temperature and nutrient levels. For the temperature experiment a gradient box was developed to allow the simultaneous testing of a wide range of temperatures on phytoplankton. During the investigations T. heimii was growing from 14 to 27 degrees C. Exponential growth rates do not show an unimodal response curve vs. temperature: values rise with increasing temperatures toward maximal growth rates around 27 degrees C. At low temperatures exponential growth is extremely long (over 50 days). In f/2 culture medium T. heimii (A603) is less efficient at high temperatures than at low temperatures, final yield was about five times higher at 16 degrees C than at 27 degrees C. Growth rate and final yield at 27 degrees C are approximately the same for all experiments, despite different nutrient levels. Mean shell diameters show no clear relation to growth temperature. Calcification of T. heimii shells is inversely related to temperature. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; Fachbereich Prod Tech, D-28359 Bremen, Germany	University of Bremen; University of Bremen	Karwath, B (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330 440, D-28334 Bremen, Germany.							BJORNLAND T, 1990, BIOCHEM SYST ECOL, V18, P307, DOI 10.1016/0305-1978(90)90002-W; BRAND L E, 1981, Journal of Plankton Research, V3, P193, DOI 10.1093/plankt/3.2.193; DALE B, 1992, OCEAN BIOCOENSIS SER, V5; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DALE B, 1992, OCEAN BIOCOENOSIS SE, V5, P33; Fensome R.A., 1993, Micropaleontology Press Special Paper; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hildebrand-Habel T, 2000, INT J EARTH SCI, V88, P694, DOI 10.1007/s005310050298; Hildebrand-Habel Tania, 1997, Courier Forschungsinstitut Senckenberg, V201, P177; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; HOLL C, 1998, BER FACHBER GEOWISS, V127, P121; INOUYE I, 1983, S AFR J BOT, V2, P63, DOI 10.1016/S0022-4618(16)30147-4; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; JONES GJ, 1983, J PHYCOL, V19, P416, DOI 10.1111/j.0022-3646.1983.00416.x; Karwath B, 2000, INT J EARTH SCI, V88, P668, DOI 10.1007/s005310050296; KELLER MD, 1987, J PHYCOL, V23, P633; KERNTOPF B, 1997, BER FACHBER GEOWISS, V103, P137; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; ROWAN R, 1992, P NATL ACAD SCI USA, V89, P3639, DOI 10.1073/pnas.89.8.3639; SOROKIN C, 1973, HDB PHYCOLOGICAL MET, p3P21; Tang EPY, 1996, J PHYCOL, V32, P80, DOI 10.1111/j.0022-3646.1996.00080.x; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; TURON JL, 1980, MEM MUS NAT HIST NAT, V27, P269; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; WILEMS H, 1996, GEOL MIJNBOUW, V75, P215; ZONNEVELD KAF, 1999, PROXIES PALEOCEANOGR, P145	30	23	23	0	8	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	JUN	2000	39	1-4					43	51		10.1016/S0377-8398(00)00013-X	http://dx.doi.org/10.1016/S0377-8398(00)00013-X			9	Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	332DJ					2025-03-11	WOS:000088058100005
J	Helenes, J				Helenes, J			<i>Exochosphaeridium alisitosense</i> n. sp., a new gonyaulacoid dinoflagellate from the Albian of Baja California, Mexico	MICROPALEONTOLOGY			English	Article								A new species of skolochorate dinoflagellate cyst, Exochosphaeridium alisitosense, from upper Albian strata in Baja California, Mexico is described. The genus Exochosphaeridium is emended to include fossil dinoflagellate cysts with nontabular to intratabular processes, occasionally modified in the antapical area and with a short apical horn, and assigned to the subfamily Cribroperidinioideae. E. alisitosense, has intratabular processes and a reticulate antapical area that together with the adjacent paraplates, delineates a symmetrical sexiform arrangement with dextral torsion. This species also has an S-type ventral organization with an A/ai paratabulation pattern.	CICESE, Dept Geol, Ensenada 22830, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Helenes, J (通讯作者)，CICESE, Dept Geol, Km 107 Carretera Tijuana Ensenada, Ensenada 22830, Baja California, Mexico.		Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879				ALLISON EC, 1955, J PALEONTOL, V29, P400; ALLISON EC, 1974, GUIDEBOOK GEOLOGY PE, P20; ALLISON EC, 1964, AAPG MEMOIR, V3, P3; Almazan-Vazquez E, 1988, REVISTA, V7, P41; [Anonymous], 1985, SPOROPOLLENIN DINOFL; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1984, INITIAL REP DEEP SEA, V79, P621; Busby C, 1998, GEOLOGY, V26, P227, DOI 10.1130/0091-7613(1998)026<0227:EMFCMF>2.3.CO;2; COOKSON I C, 1982, Palaeontographica Abteilung B Palaeophytologie, V184, P23; DAMASSA S P, 1984, Palynology, V8, P51; de Coninck J., 1983, Tertiary Research, V5, P83; DEVERTEUIL L, 1996, MICROPALEONTOLOGY S, V42, pR1; Fensome R.A., 1993, SPECIAL PUBLICATION; FIRTH J V, 1987, Palynology, V11, P199; GSTIL GR, 1975, GEOLOGICAL SOC AM ME, V140, P1; HELENES J, 1984, Palynology, V8, P107; HELENES J, 1986, Palynology, V10, P73; HELENES J, 1984, GEOLOGY BAJA CALIFOR, V39, P80; LENTIN JK, 1985, CANADIAN TECHNICAL R, V60; MACBEGGS J, 1984, GEOLOGY BAJA CALIFOR, V39, P43; MATSUOKA K, 1984, T P PALAEONTOLOGY SO, V134, P374; SINGH C, 1971, B RES COUNC ALBERTA, V28, P1; Slimani Hamid, 1994, Memoires pour Servir a l'Explication des Cartes Geologiques et Minieres de la Belgique, V37, P1; STOVER LE, 1987, ASS AUSTR PALAEONTOL, V4, P227; VALENSI LIONEL, 1955, BULL SOC GEOL FRANCE, V5, P35; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; Williams J.D., 1975, Bulletin Ala Mus nat Hist, VNo. 1,1975, P1; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	28	7	7	1	1	MICROPALEONTOLOGY PRESS	NEW YORK	AMER MUSEUM NAT HISTORY 79TH ST AT CENTRAL PARK WEST, NEW YORK, NY 10024 USA	0026-2803			MICROPALEONTOLOGY	Micropaleontology	SUM	2000	46	2					135	142		10.2113/46.2.135	http://dx.doi.org/10.2113/46.2.135			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	330PA					2025-03-11	WOS:000087969400003
J	Brinkhuis, H; Klinkenberg, E; Williams, GL; Fensome, RA				Brinkhuis, H; Klinkenberg, E; Williams, GL; Fensome, RA			Two unusual new dinoflagellate cyst genera from the Bunde Borehole, Maastrichtian type area, southern Netherlands	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						biostratigraphy; Danian; dinoflagellates; Maastrichtian		Maastrichtian and Danian deposits from the Bunde Borehole in the Maastrichtian type area contain the morphologically unusual dinoflagellate species Spumadinium felderorum gen. et sp. nov, and Lasagniella herngreenii gen. et sp, nov., both of which have archeopyles formed by the loss of several paraplates. In S. felderorum the paraplates forming the operculum or opercular pieces appear to be the third and fourth precingulars (3 "-4 ") plus the first and second anterior intercalaries (1a-2a). This suggests that Spumadinium, although having a wall resembling some cribroperidinioids, is a cladopyxiinean. L. herngreenii is unique in having up to eight wall layers, separated and supported by buttresses. The archeopyle is also a combination type but formed by loss of one apical (3'), three anterior intercalary (1a-3a) and three precingular (3 "-5 ") paraplates. Thus, Lasagniella is assignable to the Peridiniales. The distinctive morphology and restricted ranges of the two genera make them useful stratigraphic markers for the Upper Maastrichtian-Danian. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 Utrecht, Netherlands; Geol Survey Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada	Utrecht University; Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Brinkhuis, H (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 Utrecht, Netherlands.		Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				ALBERT NR, 1986, MICROPALEONTOLOGY, V32, P303, DOI 10.2307/1485724; Batten DJ., 1988, The Chalk District of the Euregio Meuse-Rhine, P95; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; COOKSON IC, 1970, NEUES JB GEOLOGIE PA; Deflandre G., 1936, Annales de paleontologie, V25, P151; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Eisenack A., 1954, Palaeontographica A, V105, P49; ELSIK WC, 1977, PALYNOLOGY, V1, P952; Fensome R.A., 1993, CLASSIFICATION FOSSI; HANSEN J M, 1977, Bulletin of the Geological Society of Denmark, V26, P1; Head MJ, 1999, J PALEONTOL, V73, P577, DOI 10.1017/S0022336000032406; HERNGREEN GFW, 1986, REV PALAEOBOT PALYNO, V48, P1, DOI 10.1016/0034-6667(86)90055-2; HERNGREEN GFW, 1998, 61 TNO NED I TOEG GE; Hofker J., 1966, Palaeontographica Suppl, V10, P1; KEDVES M, 1980, Pollen et Spores, V22, P483; Robaszynski F., 1985, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V9, P1; 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; SCHUMACKERLAMBR.J, 1978, PALYNOLOGIE LANDENIE; SCHUMACKERLAMBR.J, 1977, HANDO ASS PAL LANG F, P45; Slimani H, 1996, ANN SOC GEOL BELG, V117, P371; Slimani Hamid, 1994, Memoires pour Servir a l'Explication des Cartes Geologiques et Minieres de la Belgique, V37, P1; Wilson G.J., 1971, P 2 PLANKT C ROM 197, P1259; Wilson GJ., 1974, THESIS U NOTTINGHAM	25	9	9	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUN	2000	110	1-2					93	110		10.1016/S0034-6667(99)00062-7	http://dx.doi.org/10.1016/S0034-6667(99)00062-7			18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	342LQ	10908787				2025-03-11	WOS:000088646400003
J	Devillers, R; de Vernal, A				Devillers, R; de Vernal, A			Distribution of dinoflagellate cysts in surface sediments of the northern North Atlantic in relation to nutrient content and productivity in surface waters	MARINE GEOLOGY			English	Article						dinocyst; nitrate; North Atlantic; nutrient; palynology; productivity	LATITUDE MARINE ENVIRONMENTS; OCEANIC PRIMARY PRODUCTION; ORGANIC-CARBON; NITROGEN-FIXATION; PACIFIC-OCEAN; LABRADOR SEA; PRESERVATION; CHLOROPHYLL	Analyses of dinoflagellate cyst assemblages from the surface sediments of 371 sites from the North Atlantic Ocean were performed in order to define relationships with nitrate, phosphate, silica and productivity in the upper water layer. Statistical analyses reveal close links between dinocyst assemblages and nitrate content in February that provide a measurement of nitrate availability. Amongst the taxa in the assemblages, Nematosphaeropsis labyrinthus, which positively correlates with nutrients, shows an eutrophic relationship, whereas Impagidinium aculeatum, Impagidinium patulum; Spiniferites ramosus, Spiniferites mirabilis and Lingulodinium machaerophorum have a rather oligotrophic relationship. On these grounds, transfer functions were tested using multiple regressions and the best analogue technique to reconstruct nitrate content. Both methods yielded reasonable estimates and allow the reconstruction of the nitrate concentrations in February with an accuracy better than 1.45 mu mol m(-3). At the scale of the study area, there are also tenuous links between the dinocyst assemblages and productivity. Transfer functions were tentatively tested for the reconstruction of annual productivity and yield estimates with an accuracy of about 26.5 gC m(-2) year(-1). These results demonstrate that dinocyst assemblages can be used for the reconstruction of productivity and nitrates. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Univ Quebec, GEOTOP, CP 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	rodolphe.devillers@scg.ulaval.ca; r21024@er.uqam.ca	Devillers, Rodolphe/R-3700-2019; de Vernal, Anne/D-5602-2013	Devillers, Rodolphe/0000-0003-0784-847X; de Vernal, Anne/0000-0001-5656-724X				[Anonymous], 1989, PLANKTON ECOLOGY SUC; [Anonymous], NATO ASI SERIES; [Anonymous], 1990, SAS/STAT User's Guide: Version 6; [Anonymous], 1987, BIOL DINOFLAGELLATES; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P43, DOI 10.1029/95GB02831; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; BARNES R.S, 1982, INTRO MARINE ECOLOGY; BROWN J, 1989, OCEAN CIRCULATION, V1; CANFIELD DE, 1994, CHEM GEOL, V114, P315, DOI 10.1016/0009-2541(94)90061-2; 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; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; 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; FARRELL JW, 1995, NATURE, V377, P514, DOI 10.1038/377514a0; Feldman G., 1989, Eos Trans. 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C., 1963, SEA, VPP, P26; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A., 1999, SPECIAL CONTRIBUTION, V35; Sarnthein M, 1988, PALEOCEANOGRAPHY, V3, P361, DOI 10.1029/PA003i003p00361; SCHNEPF E, 1992, EUR J PROTISTOL, V28, P3, DOI 10.1016/S0932-4739(11)80315-9; SEVRINREYSSAC J, 1983, CAHIERS MICROPALEONT, P7; SHACKLETON NJ, 1983, NATURE, V306, P319, DOI 10.1038/306319a0; SPECTOR DL, 1984, DINOFLAGELLATES; Summerhayes C.P., 1996, Oceanography: An Illustrated Text; SUNDA WG, 1991, NATURE, V351, P55, DOI 10.1038/351055a0; TURON J, 2016, TU VOIS GENRE; Turon J.-L., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P313; Tyrrell T, 1997, NATURE, V387, P793, DOI 10.1038/42915; ZONNEVELD K, 1996, LPP CONTRIBUTION SER, V3	66	84	87	3	8	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0025-3227	1872-6151		MAR GEOL	Mar. Geol.	MAY 15	2000	166	1-4					103	124		10.1016/S0025-3227(00)00007-4	http://dx.doi.org/10.1016/S0025-3227(00)00007-4			22	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	317WY					2025-03-11	WOS:000087251000007
J	Dodsworth, P				Dodsworth, P			Trans-Atlantic dinoflagellate cyst stratigraphy across the Cenomanian-Turonian (Cretaceous) Stage boundary	JOURNAL OF MICROPALAEONTOLOGY			English	Article							WESTERN INTERIOR; MASS EXTINCTIONS; GREENHORN FORMATION; UNITED-STATES; EVENT; ENGLAND; BASIN; BIOSTRATIGRAPHY; FLUCTUATIONS; COLORADO	The principal palynological proxy for the Cenomanian-Turonian Stage boundary, the top of consistent/common Litosphaeridium siphoniphorum (a dinoflagellate cyst), occurs in Greenhorn Bed 73 at the international stratotype section, west of Pueblo, Colorado, USA. This datum occurs in the same position, as indicated by planktonic foraminifera (a few beds higher than the range top of R. cushmani), ammonites (upper part of the S. gracile/M. geslinianum Zone) and geochemistry (immediately below maximum delta(13)C values), at Pueblo (Western Interior Basin) and localities in southern England (Wessex-Paris Basin) and northern Germany (Lower Saxony Basin). Of over 100 dinoflagellate cyst taxa recorded from Pueblo and a correlative section at Lulworth, southern England, possibly as few as six do not range into the Turonian. In the uppermost Cenomanian - lowermost Turonian succession at Pueblo, there are no consistent absences of any common taxa (with four exceptions) and there is no evidence for a collapse in cyst-forming dinoflagellate populations during the Cenomanian-Turonian boundary mass extinction interval/'oceanic anoxic event'. However, the composition of palynological assemblages from the Upper Cenomanian appears to reflect palaeoenvironmental stress and/or an increase in the supply of land-derived and relatively nearshore palynomorphs.	Univ Sheffield, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England	University of Sheffield	Millennia Ltd, Unit 3, Weyside Pk,Newman Lane, Alton GU34 2PJ, Hants, England.	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Micropalaentol.	MAY	2000	19		1				69	84		10.1144/jm.19.1.69	http://dx.doi.org/10.1144/jm.19.1.69			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	322YD		hybrid			2025-03-11	WOS:000087536300010
J	Kremp, A				Kremp, A			Morphology and germination pattern of the resting cyst of <i>Peridiniella catenata</i> (Dinophyceae) from the Baltic Sea	PHYCOLOGIA			English	Article							GONYAULAX-TAMARENSIS; VERTICAL MIGRATION; SPRING-BLOOM; SEDIMENTATION; EXCAVATA	The resting cyst of the cold-water dinoflagellate Peridiniella catenata is described from sediments collected off the southwest coast of Finland, Baltic Sea. The timing of germination was determined for this cyst type, and the dynamics of benthic cysts and planktonic cells were investigated during the seasonal cycle. The discoid, colourless, and thin-walled cysts germinated after a dormancy period of six months, and the emerging vegetative cells were identified as P. catenata. Synchronized excystment occurred in midwinter at 2 degrees C. The decrease of cyst abundance in the surface sediments coincided with the appearance of vegetative cells in the water column. The decay of the vegetative population was followed by a massive input of cysts into the sediments. It is concluded that cyst formation, dormancy interval, and the timing of germination play a role in regulating the seasonal appearance of P. catenata in the water column.	Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, FIN-00014 Helsinki, Finland	University of Helsinki	Kremp, A (通讯作者)，Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, POB 17, FIN-00014 Helsinki, Finland.	anke.kremp@helsinki.fi	Kremp, Anke/I-8139-2013					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], ACTA BOT FENN; BRALEWSKA JM, 1992, P 1992 INT COUNC EXP; Dale B., 1983, P69; DODGE JD, 1987, ARCH PROTISTENKD, V134, P139, DOI 10.1016/S0003-9365(87)80067-2; Hansen G, 1998, EUR J PHYCOL, V33, P293, DOI 10.1080/09670269810001736793; Heiskanen AS, 1995, HYDROBIOLOGIA, V316, P211, DOI 10.1007/BF00017438; HSIAO SIC, 1977, CAN J BOT, V55, P685, DOI 10.1139/b77-083; 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; LARSSON U, 1986, CONTR ASKO LAB U STO, V30, P1; Levander K.M., 1894, ACTA SOC FAUNA FLORA, V9, P1; LIGNELL R, 1993, MAR ECOL PROG SER, V94, P239, DOI 10.3354/meps094239; MULLERHAECKEL A, 1981, SARSIA, V66, P267; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; Olli K, 1997, HYDROBIOLOGIA, V363, P179, DOI 10.1023/A:1003186024477; PASSOW U, 1991, MAR BIOL, V110, P455, DOI 10.1007/BF01344364; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Rengefors K, 1998, J PHYCOL, V34, P568, DOI 10.1046/j.1529-8817.1998.340568.x; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; Steidinger K.A., 1975, P153; Wasmund N, 1998, J PLANKTON RES, V20, P1099, DOI 10.1093/plankt/20.6.1099; YENTSCH CM, 1980, BIOSCIENCE, V30, P251, DOI 10.2307/1307880	24	17	17	0	11	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	MAY	2000	39	3					183	186		10.2216/i0031-8884-39-3-183.1	http://dx.doi.org/10.2216/i0031-8884-39-3-183.1			4	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	363YJ					2025-03-11	WOS:000089865000002
J	Palliani, RB; Riding, JB				Palliani, RB; Riding, JB			A palynological investigation of the Lower and lowermost Middle Jurassic strata (Sinemurian to Aalenian) from North Yorkshire, UK	PROCEEDINGS OF THE YORKSHIRE GEOLOGICAL SOCIETY			English	Article							TOARCIAN; PHYTOPLANKTON	A palynological investigation of the Lower and lowermost Middle Jurassic (Sinemurian to Aalenian) strata of North Yorkshire has been undertaken which incorporates material from the BGS Brown Moor Borehole, near Acklam and the coastal outcrops between Staithes and Robin Hood's Bay. The resulting dataset is an additional contribution to the Jurassic dinoflagellate cyst biostratigraphy of northern England. Two distinctive variants of Liasidium variabile appear to have biostratigraphical significance in the Upper Sinemurian of North Yorkshire. Specimens of L. variabile from the Caenisites turneri Ammonite Zone, the Eparietites denotatus Ammonite Subzone and the Oxynoticeras simpsoni Ammonite Subzone have short apical and antapical horns. Forms from the overlying uppermost Oxynoticeras oxynotum Ammonite Zone, however, are characterized by elongate apical horns and rounded hypocysts. The regional dinoflagellate cyst diversity increase in the late Pliensbachian and the disappearance of many dinoflagellate cysts in the Lower Toarcian are both interpreted as being related to eustatic fluctuations. The paucity of dinoflagellate cysts close to the Dactylioceras tenuicostatum-Harpoceras falciferum Ammonite zonal transition in the Lower Toarcian was caused by the spread of widespread marine anoxia during the Lower Toarcian maximum flooding event. A new species of dinoflagellate cyst, Nannoceratopsis symmetrica, is described.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy; British Geol Survey, Keyworth NG12 5GG, Notts, England	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Univ Perugia, Dept Earth Sci, Piazza Univ, I-06100 Perugia, Italy.	j.riding@bgs.ac.uk						[Anonymous], 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins; BAIRSTOW LF, 1969, INT FIELD S BRIT JUR, pC24; Baldanza Angela, 1996, Palaeopelagos, V5, P161; Batten D., 1994, Cahiers de Micropaleontologie, V9, P21; BRENNER W., 1986, Neues Jahrbuch fur Geologie und Paleontologie Abhandlungen, V173, P131; Cope J. C. 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Yorks. Geol. Soc.	MAY	2000	53		1				1	16		10.1144/pygs.53.1.1	http://dx.doi.org/10.1144/pygs.53.1.1			16	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	317UJ					2025-03-11	WOS:000087245100001
J	Iakovleva, AI; Oreshkina, TV; Alekseev, AS; Rousseau, DD				Iakovleva, AI; Oreshkina, TV; Alekseev, AS; Rousseau, DD			A new Paleogene micropaleontological and palaeogeographical data in the Petchora Depression, northeastern European Russia	COMPTES RENDUS DE L ACADEMIE DES SCIENCES SERIE II FASCICULE A-SCIENCES DE LA TERRE ET DES PLANETES			English	Article						Paleogene; northeastern Europe; stratigraphy; dinoflagellates; diatoms; benthic foraminiferas; palaeogeography		A new bore-hole from the Petchora Depression (northeastern Europe) yielded a rich Paleocene-Eocene record which allowed, for the first time, the study of dinoflagellate cysts in the whole Polar and Pre-Polar Ural region. The simultaneous occurrence of dinoflagellates in the whole section, benthic foraminifera in the Palaeocene part and diatoms in the Eocene section permits a high-resolution biostratigraphy. The lithological and micropalaeontological analyses suggest the existence of a marine basin in the Polar and Pre-Polar Ural area and its constant communications with the west Siberian epicontinental sea during the Thanetian-Ypresian. (C) 2000 Academie des sciences / Editions scientifiques ct medicales Elsevier SAS.	Univ Montpellier 2, Palaeobot & Palynol Lab, UMR CNRS 5554, Isem, F-34095 Montpellier, France; Russian Acad Sci, Inst Geol, Paleoflorist Lab, Moscow 109017, Russia; Russian Acad Sci, Inst Geol, Lab Micropaleontol, Moscow 109017, Russia; Moscow State Univ, Dept Geol, Moscow 119899, Russia; Columbia Univ, Lamont Doherty Geol Observ, Palisades, NY 10964 USA	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences; Lomonosov Moscow State University; Columbia University	Iakovleva, AI (通讯作者)，Univ Montpellier 2, Palaeobot & Palynol Lab, UMR CNRS 5554, Isem, Case 61, F-34095 Montpellier, France.		IAKOVLEVA, ALINA/ABH-9243-2020; Oreshkina, Tatyana/ABC-6121-2021; Rousseau, Denis-Didier/I-6892-2012	Rousseau, Denis-Didier/0000-0003-2475-3405; Oreshkina, Tatiana V./0000-0002-7477-7272				AFANASIEVA TA, 1988, RUSS GEOL C SIKT, P127; AFANSIEVA TA, 1996, PALEOGENE NEOGENE W; ANDREEVAGRIGORO.AS, 1991, DETAILED PALEOGENE S; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; ARANASIEVA TA, 1994, P 12 GEOL C SIKT, P83; BELKIN VI, 1965, NEW STRATIGRAPHICAL, V5, P76; BERGGREN WA, 1995, SOC EC PALEONTOLOGIS, V54, P195; Cavelier C., 1983, GEOL FRANCE, V3, P261; CHATEAUNEUF JJ, 1978, B BRGM, V4, P59; DERTEV AK, 1963, ANN VNIGRI, V20, P65; GLEZER ZI, 1994, REGIONAL GEOLOGY MET, V2, P148; GRAMBERG IS, 1984, GEOLOGICAL STRUCTURE; Grantz A., 1990, The Arctic Ocean region; HEILMANNCLAUSEN C, 1985, DANMARKS GEOLOGISK A, V7; IIYINA VI, 1994, OIGGIM PUBLICATION; Kazmin V.G., 1998, The paleogeographic atlas of northern Eurasia; Marincovich Jr L., 1990, ARCTIC OCEAN REGION, P403; MARINCOVICH L, 1992, ICAM P, P45; Nazarov M.A., 1993, BYUL MOSK OBSHCH ISP, V68, P13; ORESHKINA TV, 1998, GIN RAN PUBLICATION, V500, P183; Podobina V. M., 1990, Byulleten' Moskovskogo obshchestva ispytateley prirody Bulletin of the Moscow Society of Nature Testers, Geology branch, V65, P61; Powell A.J., 1992, P155; Shatsky S.B., 1978, PALEOGEN NEOGEN SIBI, P3; STEPANOV IS, 1991, IZV VISSH UCHEB ZAV, V3, P142; Strelnikova NI., 1992, PALEOGENE DIATOMS; THIEDE J, 1990, ARCTIC OCEAN REGION, P427; USTINOV YY, 1958, B SCI INFORMATION, V1, P5; VASILIEVA O.N, 1990, PALYNOLOGY STRATIGRA; ZIEGLER AM, TIDAL FRICTION EARTH, V3	30	14	15	0	1	EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	PARIS CEDEX 15	23 RUE LINOIS, 75724 PARIS CEDEX 15, FRANCE	1251-8050			CR ACAD SCI II A	Comptes Rendus Acad. Sci. Ser II-A	APR 15	2000	330	7					485	491		10.1016/S1251-8050(00)00180-4	http://dx.doi.org/10.1016/S1251-8050(00)00180-4			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	310CY					2025-03-11	WOS:000086810000005
J	Persson, A				Persson, A			Possible predation of cysts - a gap in the knowledge of dinoflagellate ecology?	JOURNAL OF PLANKTON RESEARCH			English	Article							ALEXANDRIUM; SEDIMENTS; DYNAMICS; COPEPODS; BAY	A theoretical model of dinoflagellate ecology is presented. The model incorporates currently neglected aspects of potential importance in the field of plankton research, such as losses to the cyst seed bank due to predation or microbial degradation.	Univ Gothenburg, Dept Marine Bot, SE-40530 Gothenburg, Sweden	University of Gothenburg	Persson, A (通讯作者)，Univ Gothenburg, Dept Marine Bot, Box 461, SE-40530 Gothenburg, Sweden.			Persson, Agneta/0000-0003-0202-6514				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; [Anonymous], 1998, HARMFUL ALGAE XUNTA; Boyer G.L., 1985, P407; BRAVO I, 1998, HARMFUL ALGAE, P356; Bricelj V.M., 1998, HARMFUL ALGAE, P453; Bricelj V. Monica, 1995, P413; BRICELJ VM, 1990, TOXIC MARINE PHYTOPLANKTON, P269; CEMBELLA AD, 1990, TOXIC MARINE PHYTOPLANKTON, P333; Dale B., 1979, P443; DALE B, 1983, SURVIVAL STRATEGIES, P86; DESTASIO BT, 1989, ECOLOGY, V70, P1377; DODGE JD, 1982, MARINE DINOFLAGELLAT, P80; DUTZ J, 1997, 8 INT C HARMF ALG JU, P66; FENCHEL T, 1969, Ophelia, V6, P1; FUTUYMA DJ, 1986, EVOLUTIONARY BIOL, P28; Gaines G., 1987, The Biology of Dinoflagellates, P224; GUJER W, 1983, WATER SCI TECHNOL, V15, P127, DOI 10.2166/wst.1983.0164; HUNTLEY M, 1986, MAR ECOL PROG SER, V28, P105, DOI 10.3354/meps028105; Hurst J.W., 1985, P427; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; IVES DJ, 1985, TOXIC DINOFLAGELLATE, P413; Jeong H., 1998, HARMFUL ALGAE, P179; Latz MI, 1996, MAR ECOL PROG SER, V132, P275, DOI 10.3354/meps132275; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; LIRDWITAYAPRASIT T, 1990, TOXIC MARINE PHYTOPLANKTON, P294; Louda SM., 1989, ECOLOGY SOIL SEEDBAN, P25; Lovejoy C, 1998, APPL ENVIRON MICROB, V64, P2806; MACKENZIE L, 1998, HARMFUL ALGAE, P237; Matsuyama Y., 1998, HARMFUL ALGAE, P422; REID PC, 1987, J PLANKTON RES, V9, P249, DOI 10.1093/plankt/9.1.249; Rosenberg R, 1996, J SEA RES, V35, P1, DOI 10.1016/S1385-1101(96)90730-3; Sellner K.G., 1985, P245; Shumway S.E., 1985, P389; SHUMWAY S E, 1988, Journal of Shellfish Research, V7, P643; Teegarden GJ, 1996, J EXP MAR BIOL ECOL, V196, P145, DOI 10.1016/0022-0981(95)00128-X; Turner J.T, 1998, HARMFUL ALGAE, P379; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WHITE AW, 1982, CAN J FISH AQUAT SCI, V39, P1185, DOI 10.1139/f82-156; YAN T, 1997, 8 INT C HARMF ALG JU, P216; Yentsch C.M., 1979, P127; Yoshinaga Ikuo, 1995, P687; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; [No title captured], DOI DOI 10.1016/J.JASMS.2007.11.001	45	37	40	1	6	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	APR	2000	22	4					803	809		10.1093/plankt/22.4.803	http://dx.doi.org/10.1093/plankt/22.4.803			7	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	302YL		Bronze			2025-03-11	WOS:000086394000012
J	Baruffini, L; Lottaroli, F; Torricelli, S; Lazzari, D				Baruffini, L; Lottaroli, F; Torricelli, S; Lazzari, D			Stratigraphic revision of the Eocene Albidona Formation in the Type Locality (Calabria, Southern Italy)	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						biostratgraphy; calcareous nannofossils; dinoflagellate cysts; turbidites; turbidite system; Eocene; tertiary; Southern Apennines; Italy	TURBIDITY CURRENTS; MEGATURBIDITES; DEPOSITS; FLOWS; BASIN; SPAIN	Original biostratigraphic and sedimentologic data of the type section of the Albidona Formation (Liguride Complex, Southern Apennines, Italy) are presented and discussed. Since its definition in 1962, this lithostratigraphic unit has been the object of controversial interpretations in terms of age attribution and paleotectonic significance. Based on cross-observations performed on calcareous nannofossils and palynomorphs, we conclude that the Albidona Formation should be assigned to the Eocene. Based on this evidence, a review of the previous biostratigraphic literature is provided. Furthermore, we recognise four different turbidite systems (named A to D), bounded by minor stratigraphic hiatuses, that are characterised by different sedimentary facies associations and petrofacies. The overall vertical arrangement demonstrates that the Albidona Formation was deposited in a tectonically mobile basin during a phase of deformation older than the apenninic deformation and may likely be referred to the alpine tectonics of the Calabrian are. Moreover, the relationship with the underlying folded unit suggests that the Albidona Formation may be interpreted as an episutural deposit relevant co a Paleogene deformation that affected the older units of the Liguride Complex. Based on stratigraphic and sedimentological features, we suggest a correlation of the Albidona Formation with analogue turbidite suites cropping out in the Apennines, and we discuss their significance in the context of the Eocene tectonic paroxysm in the Mediterranean area.	Eniricerche SpA, I-20097 San Donato Milanese, Italy	Eni SpA	Eniricerche SpA, I-20097 San Donato Milanese, Italy.	fabio.lottaroli@asp.it						Amore F.O., 1988, Bollettino della Societa Geologica Italiana, V107, P219; AMORE FO, 1988, SOC GEOLOGICA ITALIA, V41, P285; [Anonymous], 1963, MEM SOC GEOL ITAL; [Anonymous], 1978, RIV IT PALEONT; [Anonymous], GEOL ROM; [Anonymous], 1996, Palynology: principles and applications; Aubry M.-P., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P471, DOI 10.2973/odp.proc.sr.120.149.1992; AUBRY MP, 1986, PALAEOGEOGR PALAEOCL, V55, P267, DOI 10.1016/0031-0182(86)90154-9; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; BOCCALETTI M, 1987, CARTA STRUTTURALE AP; Bonardi G., 1985, Bollettino della Societa Geologica Italiana, V104, P539; Bonardi G., 1988, Memorie della Societa Geologica Italiana, V41, P17; BRALOWER JT, 1995, P ODP SCI RES, V143, P31; Bukry D., 1975, Initial Rep Deep Sea Drilling Project, V32, P677, DOI 10.2973/dsdp.proc.32.124.1975; BUKRY D, 1973, INITIAL REPTS DSDP, V15, P487; BYBELL LM, 1995, P ODP SCI RES X, V150, P91; CATANZARITI R., 1997, MEM SCI GEOL, V49, P207; CIAMPO G, 1984, B SOC GEOL ITAL, V103, P333; Cita MB, 1996, SEDIMENT GEOL, V104, P155, DOI 10.1016/0037-0738(95)00126-3; Colella A., 1988, MEM SOC GEOL ITAL, V41, P791; Crescenti U., 1966, Bollettino della Societa Geologica Italiana, V85, P541; Critelli S., 1990, B SOC GEOL ITAL, V109, P511; Decima F.Proto., 1975, Schweiz. Paleontol. Abh, V97, P35; DICKINSO.WR, 1970, J SEDIMENT PETROL, V40, P695, DOI 10.1306/74D72018-2B21-11D7-8648000102C1865D; Dickinson WR., 1985, NATO ADV STUDY I SER, V148, P331; Gazzi P., 1966, Mineralogica e Petrografia Acta, V12, P69; GHEZZI G, 1963, B SERV GEOL IT ROMA, V84, P3; GNACCOLINI M, 1968, RIV ITAL PALEONTOL S, V74, P1233; KASTENS KA, 1984, MAR GEOL, V55, P13, DOI 10.1016/0025-3227(84)90130-0; KNOTT SD, 1987, TECTONOPHYSICS, V142, P217, DOI 10.1016/0040-1951(87)90124-7; LABAUME P, 1987, GEO-MAR LETT, V7, P91, DOI 10.1007/BF02237988; Lentini F., 1987, Memor. Soc. Geol. Ital, V38, P259; MARJANAC T, 1990, SEDIMENTOLOGY, V37, P921, DOI 10.1111/j.1365-3091.1990.tb01834.x; MONECHI S, 1985, MAR MICROPALEONTOL, V9, P419, DOI 10.1016/0377-8398(85)90009-X; MORELLI LA, 1976, B SOC GEOL ITAL, V17, P1; MOSTARDINI F, 1966, B SERV GEOL IT ROMA, V86, P57; Mutti E., 1995, Memorie di Scienze Geologiche, V47, P217; Mutti E., 1992, SPECIAL PUBLICATION; Mutti E., 1987, MARINE CLASTIC SEDIM, P1, DOI 10.1007/978-94-009-3241-8_1; Nocchi M., 1986, Developments in Palaeontology and Stratigraphy, V9, P25; Ogniben L., 1969, MEMORIE SOC GEOLOGIC, V8, P453; OKADA H, 1980, MAR MICROPALEONTOL, V5, P321, DOI 10.1016/0377-8398(80)90016-X; PANTIN HM, 1987, SEDIMENTOLOGY, V34, P1143, DOI 10.1111/j.1365-3091.1987.tb00597.x; Perch-Nielsen K., 1985, P427; Pescatore T., 1966, GEOL ROMANA, V5, P99; PICKERING KT, 1985, SEDIMENTOLOGY, V32, P373, DOI 10.1111/j.1365-3091.1985.tb00518.x; Pospichal J.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P613, DOI 10.2973/odp.proc.sr.113.205.1990; ROMEIN A. J. T., 1979, UTRECHT MICROPALAEON, V22, P1; SEGURET M, 1984, MAR GEOL, V55, P117, DOI 10.1016/0025-3227(84)90136-1; Selli R., 1962, MEM SOC GEOL ITAL, V3, P737; SILVA IP, 1988, SPEC PUBL, P137; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; VANDIJK JP, 1998, 79 C SOC GEOL IT 21, V756; Vezzani L., 1966, Bollettino della Societa Geologica Italiana, V85, P767; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; Zuffa G.G., 1987, MARINE CLASTIC SEDIM, P39, DOI DOI 10.1007/978-94-009-3241-8_2; ZUFFA GG, 1980, J SEDIMENT PETROL, V50, P21; Zuppetta A., 1984, B SOC GEOL ITAL, V103, P159	58	14	14	0	0	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	2000	106	1					73	98		10.13130/2039-4942/5391	http://dx.doi.org/10.13130/2039-4942/5391			26	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	321KH					2025-03-11	WOS:000087454300004
J	Dunstan, SL; Sala-Newby, GB; Fajardo, AB; Taylor, KM; Campbell, AK				Dunstan, SL; Sala-Newby, GB; Fajardo, AB; Taylor, KM; Campbell, AK			Cloning and expression of the bioluminescent photoprotein pholasin from the bivalve mollusc <i>Pholas dactylus</i>	JOURNAL OF BIOLOGICAL CHEMISTRY			English	Article							DINOFLAGELLATE GONYAULAX-POLYEDRA; LUCIFERIN-BINDING-PROTEIN; INFLUENZA-VIRUS; GLYCOSYLATION; AEQUORIN; CELLS; GENE; HEMAGGLUTININ; CALSEQUESTRIN; REQUIREMENTS	Pholasin is the photoprotein responsible for luminescence in the bivalve Pholas dactylus and consists of a luciferin tightly bound to a glycosylated protein, It is a sensitive indicator of reactive oxygen species. A full-length clone encoding apopholasin was isolated from a P. dactylus light organ cDNA library. The unprocessed apoprotein contained 225 amino acids, starting with a signal peptide of 20 amino acids, 3 predicted N-linged glycosylation sites, 1 O-linked site, no histidines, and 7 cysteines, The recombinant apoprotein was expressed in cell extracts and insect cells. The size of the apoprotein expressed in cell extracts and the cytosol of insect cells was 26 kDa but that of the fully processed protein was 34 kDa, as was native pholasin. Both the processed and unprocessed recombinant apoproteins were recognized by a polyclonal antibody raised against native pholasin, Acid methanol extracts from Pholas added to recombinant apoprotein resulted in chemiluminescence triggered by sodium hypochlorite but not photoprotein formation. These results have important implications in understanding the molecular evolution of bioluminescence and will allow the development of recombinant pholasin as an intracellular indicator of reactive oxygen species.	Univ Wales, Coll Med, Dept Biochem Med, Cardiff CF14 4XN, S Glam, Wales	Cardiff University	Campbell, AK (通讯作者)，Univ Wales, Coll Med, Dept Biochem Med, Heath Pk, Cardiff CF14 4XN, S Glam, Wales.		Taylor, Kathryn/O-3401-2014	Taylor, Kathryn/0000-0002-9576-9490				Badminton MN, 1995, BIOCHEM BIOPH RES CO, V217, P950, DOI 10.1006/bbrc.1995.2862; BADMINTON MN, 1995, EXP CELL RES, V216, P236, DOI 10.1006/excr.1995.1030; Bairoch A, 1997, NUCLEIC ACIDS RES, V25, P217, DOI 10.1093/nar/25.1.217; BASSOT JM, 1966, BIOLUMINESCENCE PROG, P559; BAUSE E, 1983, BIOCHEM J, V209, P331, DOI 10.1042/bj2090331; Bellamacina CR, 1996, FASEB J, V10, P1257, DOI 10.1096/fasebj.10.11.8836039; Boettcher KJ, 1996, J COMP PHYSIOL A, V179, P65; BOWTELL D, 1987, ANAL BIOCHEM, V163, P391; Campbell A. K., 1994, BIOLUMINESCENCE CHEM; Campbell A.K., 1988, CHEMILUMINESCENCE PR; CAMPBELL AK, 1990, MAR BIOL, V104, P219, DOI 10.1007/BF01313261; CERUTTI PA, 1985, SCIENCE, V227, P375, DOI 10.1126/science.2981433; CHIRGWIN JM, 1979, BIOCHEMISTRY-US, V18, P5294, DOI 10.1021/bi00591a005; COTTON B, 1989, BIOCHEM SOC T, V17, P705, DOI 10.1042/bst0170705; DEWET JR, 1987, MOL CELL BIOL, V7, P725, DOI 10.1128/MCB.7.2.725; Dubois R, 1887, COMPT REND SOC BIOL, V39, P564; FINDLAY JBC, 1989, PROTEINS EQUENCING P; Finkel T, 1998, CURR OPIN CELL BIOL, V10, P248, DOI 10.1016/S0955-0674(98)80147-6; GALLAGHER PJ, 1992, J VIROL, V66, P7136, DOI 10.1128/JVI.66.12.7136-7145.1992; GROPPE JC, 1993, ANAL BIOCHEM, V210, P337, DOI 10.1006/abio.1993.1205; HANSEN JE, 1995, BIOCHEM J, V308, P801, DOI 10.1042/bj3080801; Harvey E.N., 1952, BIOLUMINESCENCE; HASTINGS JW, 1989, J BIOLUM CHEMILUM, V4, P12, DOI 10.1002/bio.1170040105; Hastings JW, 1996, GENE, V173, P5, DOI 10.1016/0378-1119(95)00676-1; HEARING J, 1989, J CELL BIOL, V108, P355, DOI 10.1083/jcb.108.2.355; Hecker KH, 1996, BIOTECHNIQUES, V20, P478; HENRY JP, 1977, BIOCHEMISTRY-US, V16, P2517, DOI 10.1021/bi00630a031; HENRY JP, 1975, BIOCHEMISTRY-US, V14, P3458, DOI 10.1021/bi00686a026; Hsu TA, 1996, PROTEIN EXPRES PURIF, V7, P281, DOI 10.1006/prep.1996.0040; Johnson F.H., 1978, Methods in Enzymology, V57, P271; Johnson TM, 1996, P NATL ACAD SCI USA, V93, P11848, DOI 10.1073/pnas.93.21.11848; KENDALL JM, 1992, BIOCHEM BIOPH RES CO, V189, P1008, DOI 10.1016/0006-291X(92)92304-G; KORSMEYER SJ, 1995, BBA-MOL BASIS DIS, V1271, P63, DOI 10.1016/0925-4439(95)00011-R; KOZAK M, 1991, J BIOL CHEM, V266, P19867; KUMAR S, 1990, FEBS LETT, V268, P287, DOI 10.1016/0014-5793(90)81029-N; KUROSE K, 1989, P NATL ACAD SCI USA, V86, P80, DOI 10.1073/pnas.86.1.80; LEE DH, 1993, J BIOL CHEM, V268, P8842; Li LM, 1998, PLANT MOL BIOL, V36, P275, DOI 10.1023/A:1005941421474; Markesbery WR, 1997, FREE RADICAL BIO MED, V23, P134, DOI 10.1016/S0891-5849(96)00629-6; Michelson A.M., 1978, Methods in Enzymology, V57, P385; MULLER T, 1990, J BIOLUM CHEMILUM, V5, P25, DOI 10.1002/bio.1170050106; NICOL JAC, 1960, J MAR BIOL ASSOC UK, V39, P109, DOI 10.1017/S002531540001314X; Nielsen H, 1997, PROTEIN ENG, V10, P1, DOI 10.1093/protein/10.1.1; Ohmiya Y, 1997, FEBS LETT, V404, P115, DOI 10.1016/S0014-5793(97)00105-1; OHNISHI M, 1987, BIOCHEMISTRY-US, V26, P7458, DOI 10.1021/bi00397a039; ORR WC, 1994, SCIENCE, V263, P1128, DOI 10.1126/science.8108730; OSTWALD TJ, 1974, J BIOL CHEM, V249, P5867; Rees JF, 1998, J EXP BIOL, V201, P1211; RICHTER C, 1995, INT J BIOCHEM CELL B, V27, P647, DOI 10.1016/1357-2725(95)00025-K; ROBERTS PA, 1987, ANAL BIOCHEM, V160, P139, DOI 10.1016/0003-2697(87)90624-5; ROSENFELD J, 1992, ANAL BIOCHEM, V203, P173, DOI 10.1016/0003-2697(92)90061-B; SALANEWBY GB, 1994, BBA-PROTEIN STRUCT M, V1206, P155, DOI 10.1016/0167-4838(94)90084-1; SAMBROOK J, 1989, MOL CLONING LAB MANA; TAYLOR KM, 1994, IMMUNOLOGY, V83, P501; THOMPSON EM, 1989, P NATL ACAD SCI USA, V86, P6567, DOI 10.1073/pnas.86.17.6567; Thomson CM, 1997, J BIOLUM CHEMILUM, V12, P87, DOI 10.1002/(SICI)1099-1271(199703/04)12:2<87::AID-BIO438>3.0.CO;2-8; Tooze SA, 1998, BBA-MOL CELL RES, V1404, P231, DOI 10.1016/S0167-4889(98)00059-7; Wallace DC, 1998, NAT GENET, V19, P105, DOI 10.1038/448; WATKINS NJ, 1993, BIOCHEM J, V293, P181, DOI 10.1042/bj2930181; WINNEPENNINCKX B, 1993, TRENDS GENET, V9, P407	60	29	34	1	11	AMER SOC BIOCHEMISTRY MOLECULAR BIOLOGY INC	BETHESDA	9650 ROCKVILLE PIKE, BETHESDA, MD 20814 USA	0021-9258			J BIOL CHEM	J. Biol. Chem.	MAR 31	2000	275	13					9403	9409		10.1074/jbc.275.13.9403	http://dx.doi.org/10.1074/jbc.275.13.9403			7	Biochemistry & Molecular Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology	299PF	10734085				2025-03-11	WOS:000086206500049
J	Crouch, EM; Bujak, JP; Brinkhuis, H				Crouch, EM; Bujak, JP; Brinkhuis, H			Southern and Northern Hemisphere dinoflagellate cyst assemblage changes in association with the late Paleocene thermal maximum	GFF			English	Article									Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Lexis Grp, Blackpool FY3 8NA, Lancs, England	Utrecht University	Crouch, EM (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Crouch, Erica/C-2820-2013; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610				Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Kaiho K, 1996, PALEOCEANOGRAPHY, V11, P447, DOI 10.1029/96PA01021; Kemp AES, 1999, NATURE, V398, P57, DOI 10.1038/18001; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; TARGARONA J, 1997, LPP CONTRIBUTION SER, V7	7	9	9	0	6	SWEDISH SCIENCE PRESS	UPPSALA	BOX 118, S751 04 UPPSALA, SWEDEN	1103-5897			GFF	GFF	MAR	2000	122		1				40	41		10.1080/11035890001221040	http://dx.doi.org/10.1080/11035890001221040			2	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	293LN					2025-03-11	WOS:000085853400018
J	Steurbaut, E; De Coninck, J; Dupuis, C; King, C				Steurbaut, E; De Coninck, J; Dupuis, C; King, C			Dinoflagellate cyst events and depositional history of the Paleocene/Eocene boundary interval in the southern North Sea Basin	GFF			English	Article							STRATA		Royal Belgian Inst Nat Sci, BE-1000 Brussels, Belgium; Katholieke Univ Leuven, Louvain, Belgium; State Univ Ghent, Lab Paleontol, BE-9000 Ghent, Belgium; Fac Polytech Mons, BE-7000 Mons, Belgium; Univ Greenwich, Dept Earth & Environm Sci, Chatham Maritime, Kent, England	Royal Belgian Institute of Natural Sciences; KU Leuven; Ghent University; University of Mons; University of Greenwich	Steurbaut, E (通讯作者)，Royal Belgian Inst Nat Sci, 29 Vautierstr, BE-1000 Brussels, Belgium.							[Anonymous], 1996, SPECIAL PUBLICATIONS, DOI DOI 10.1144/GSL.SP.1996.101.01.17; [Anonymous], 1999, B SOC BELG GEOL; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Boggild O. B, 1918, Bull. Geol. Soc. Den., V33, P1; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; De Coninck J, 1999, B SOC GEOL FR, V170, P77; De Coninck J., 1991, B SOC BELG GEOL, V97, P287; De Coninck Jan, 1994, Bulletin de la Societe Belge de Geologie, V102, P105; DUPUIS C, 1990, TOELICHTENDE VERHAND, V29, P33; DUPUIS C, 1998, MEMOIRE SCI TERRE, V34, P60; EGGER H, IN PRESS B SOC GEOLO; ELLISON RA, 1994, P GEOLOGIST ASSOC, V105, P187, DOI 10.1016/S0016-7878(08)80118-6; Heilmann-Clausen C., 1989, Geol. Jahrb., V111, P1; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; Heilmann-Clausen C, 1994, GFF, V116, P51, DOI 10.1080/11035899409546149; HEILMANNCLAUSEN C, 1998, STRATA, V1, P60; Knox R.W.O., 1996, GEOLOGICAL SOC SPECI, V103, P209; Knox RWO, 1998, NEWSL STRATIGR, V36, P49; Kothe A., 1990, GEOL JB A, V118, P3; MERCIERCASTIAUX M, 1988, ANN SOC GEOL NORD, V107, P139; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Powell A.J., 1992, P155; Steurbaut E, 1999, B SOC GEOL FR, V170, P217; STEURBAUT E, 1998, STRATA, V1, P122; Steurbaut Etienne, 1998, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V247, P91; THIRY M, 1998, MEMOIRES SCI TERRE, V34, P39; THIRY M, 1998, MEMOIRES SCI TERRE E, V34, P28; VANHUIS A, 1992, P 5 INT WORK C STOR, V1, P99; [No title captured]	29	9	10	0	8	SWEDISH SCIENCE PRESS	UPPSALA	BOX 118, S751 04 UPPSALA, SWEDEN	1103-5897			GFF	GFF	MAR	2000	122		1				154	157		10.1080/11035890001221154	http://dx.doi.org/10.1080/11035890001221154			4	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	293LN					2025-03-11	WOS:000085853400076
J	Esper, O; Zonneveld, KAF; Höll, C; Karwath, B; Kuhlmann, H; Schneider, RR; Vink, A; Weise-Ihlo, I; Willems, H				Esper, O; Zonneveld, KAF; Höll, C; Karwath, B; Kuhlmann, H; Schneider, RR; Vink, A; Weise-Ihlo, I; Willems, H			Reconstruction of palaeoceanographic conditions in the South Atlantic Ocean at the last two Terminations based on calcareous dinoflagellate cysts	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						calcareous dinoflagellate cysts; palaeoceanography; Late Quaternary; glacial terminations; South Atlantic Ocean	WESTERN TROPICAL ATLANTIC; QUATERNARY EASTERN; DEEP-SEA; PRESERVATION; TEMPERATURE; CIRCULATION; SCALES; WATER	Despite the increasing interest in the South Atlantic Ocean as a key area of the heat exchange between the southern and the northern hemisphere, information about its palaeoceanographic conditions during transitions from glacial to interglacial stages, the so-called Terminations, are not well understood. Herein we attempt to increase this information by studying the calcareous dinoflagellate cysts and the shells of Thoracosphaera heimii (calcareous cysts) of five Late Quaternary South Atlantic Ocean cores. Extremely high accumulation rates of calcareous cysts at the Terminations might be due to a combined effect of increased cyst production and better preservation as result of calm, oligotrophic conditions in the upper water layers. Low relative abundance of Sphaerodinella albatrosiana compared with Sphaerodinella tuberosa in the Cape Basin may be the result of the relatively colder environmental conditions in this region compared with the equatorial Atlantic Ocean with high relative abundance of S. albatrosiana. Furthermore, the predominance of S. tuberosa during glacials and interglacials at the observed site of the western Atlantic Ocean reflects decreased salinity in the upper water layer.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Willems, H (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330 440, D-28334 Bremen, Germany.		Vink, Annemiek/GXG-6435-2022	Vink, Annemiek/0000-0002-5178-9721; Esper, Oliver/0000-0002-4342-3471; Schneider, Ralph/0000-0003-1453-9181; Kuhlmann, Holger/0000-0001-8932-7031				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; Baumann K.-H., 1999, USE PROXIES PALEOCEA, P117, DOI [10.1007/978-3-642-58646, DOI 10.1007/978-3-642-58646-0_4]; Bickert T, 1996, SOUTH ATLANTIC, P599; Bickert T., 1992, BER FACHBEREICH GEOW, V27, P1; BLEIL U, 1996, BERICHTE FACHBEREICH, V77, P1; BROECKER WS, 1982, PROG OCEANOGR, V11, P151, DOI 10.1016/0079-6611(82)90007-6; CEPEK M, 1996, BERICHTE FACHB GEOWI, V86, P1; Curry WB, 1996, SOUTH ATLANTIC, P577; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DALE B, 1992, OCEAN BIOCOENOSIS SE, V5, P33; DIESTERHAASS L, 1985, MAR GEOL, V65, P145, DOI 10.1016/0025-3227(85)90051-9; Durkoop A, 1997, PALEOCEANOGRAPHY, V12, P764, DOI 10.1029/97PA02270; EMERSON S, 1981, J MAR RES, V39, P139; Feldman G., 1989, Eos Trans. 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J., 1960, Discovery Reports, V31, P123; Höll C, 1999, PALAEOGEOGR PALAEOCL, V146, P147, DOI 10.1016/S0031-0182(98)00141-2; Holl C, 1998, MAR MICROPALEONTOL, V33, P1, DOI 10.1016/S0377-8398(97)00033-9; HOUGHTON RW, 1991, J GEOPHYS RES-OCEANS, V96, P15173, DOI 10.1029/91JC01442; HOWARD WR, 1994, PALEOCEANOGRAPHY, V9, P453, DOI 10.1029/93PA03524; Imbrie J, 1992, PALEOCEANOGRAPHY, V7, P701, DOI 10.1029/92PA02253; JAHNKE RA, 1994, GEOCHIM COSMOCHIM AC, V58, P2799, DOI 10.1016/0016-7037(94)90115-5; Janofske Dorothea, 1996, Bulletin de l'Institut Oceanographique Numero Special (Monaco), V14, P295; KAMPTNER E, 1967, Annalen des Naturhistorischen Museums in Wien, V71, P117; Le JN, 1992, PALEOCEANOGRAPHY, V7, P21, DOI 10.1029/91PA02854; Little MG, 1997, PALEOCEANOGRAPHY, V12, P568, DOI 10.1029/97PA00823; LONGHURST A, 1993, DEEP-SEA RES PT I, V40, P2145, DOI 10.1016/0967-0637(93)90095-K; MARTINSON DG, 1987, QUATERNARY RES, V27, P1, DOI 10.1016/0033-5894(87)90046-9; Mix AC, 1996, SOUTH ATLANTIC, P503; MUCKE SK, 1994, BERICHTE FACHB GEOWI, V55, P1; MULLER C, 1976, GEOL JB D, V17, P33; PETERSON RG, 1991, PROG OCEANOGR, V26, P1, DOI 10.1016/0079-6611(91)90006-8; REID JL, 1989, PROG OCEANOGR, V23, P149, DOI 10.1016/0079-6611(89)90001-3; RUHLEMANN C, 1996, BERICHT FACHB GEOWIS, V84, P1; SHANNON LV, 1985, OCEANOGR MAT BIOL AN, V23, P183; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2; Vink A, 2000, MAR MICROPALEONTOL, V38, P149; WAFER G, 1989, BERICHTE FACHB GEOWI, V7, P1; WALL D, 1968, Journal of Paleontology, V42, P1395; WEEKS SJ, 1994, J GEOPHYS RES-OCEANS, V99, P7385, DOI 10.1029/93JC02143; Wefer G, 1996, SOUTH ATLANTIC, P461; WEFER G, 1990, BERICHTE FACHB GEOWI, V11, P1; WEFER G, 1996, BERICHTE FACHBEREICH, V79, P1; WEFER G, 1994, BERICHT FACHB GEOWIS, V44, P1; WINTER A, 1990, PALEOCEANOGRAPHY, V6, P20; ZONNEVELD KAF, IN PRESS REV PALAEOB	49	31	32	0	7	SPRINGER VERLAG	NEW YORK	175 FIFTH AVE, NEW YORK, NY 10010 USA	1437-3254			INT J EARTH SCI	Int. J. Earth Sci.	MAR	2000	88	4					680	693		10.1007/s005310050297	http://dx.doi.org/10.1007/s005310050297			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	331DZ					2025-03-11	WOS:000088003200009
J	Ellegaard, M				Ellegaard, M			Variations in dinoflagellate cyst morphology under conditions of changing salinity during the last 2000 years in the Limfjord, Denmark	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						cyst; dinoflagellate; Holocene; Lingulodinium; Operculodinium; Protoceratium; recent; salinity; Spiniferites	MARINE-SEDIMENTS; RESTING CYSTS; LATE-HOLOCENE; FLUCTUATIONS; AUSTRALIA; SEA	Morphological variations are examined in the dinoflagellate cysts Spiniferites spp., Lingulodinium polyedrum and Protoceratium reticulatum (= Operculodinium centrocarpum) from a core taken in the Bjornsholm Bay, the Limfjord, Denmark. The fjord has a history of changing salinity, and unusual cyst morphotypes are found in the greatest numbers during periods of inferred low salinity. Variation occurs primarily in cyst process morphology, and the aberrant morphotypes have processes that are shorter, thicker and/or more membranous. The different morphotypes are described and compared with other varieties and forms of the three taxa and to other closely related taxa. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Copenhagen, Inst Bot, Dept Phycol, DK-1353 Copenhagen K, Denmark	University of Copenhagen	Ellegaard, M (通讯作者)，Univ Copenhagen, Inst Bot, Dept Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.		Ellegaard, Marianne/H-6748-2014					[Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; CHRISTENSEN JT, UNPUB LATE HOLOCENE; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; HALL SAV, 1996, 9 INT PAL C HOUST TX, P58; Hallett R.I, 1996, 9 INT PAL C HOUST TX, P59; HARLAND R, 1973, REV PALAEOBOT PALYNO, V16, P229, DOI 10.1016/0034-6667(73)90021-3; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Head Martin J., 1993, Palynology, V17, P201; HYLLEBJERG J, 1992, 4 DAN GEOL SURV, P37; Kokinos John P., 1995, Palynology, V19, P143; KRISTENSEN P, 1995, HOLOCENE, V5, P313, DOI 10.1177/095968369500500306; LENTIN JK, 1993, AM ASS STRATIGRAPHIC, V1854; LEWIS J, 1998, 6 INT C MOD FOSS DIN, P92; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka Kazumi, 1997, Palynology, V21, P19; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; Morzadec-Kerfourn M. T., 1977, Revue Micropaleont, V20, P157; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; MUDIE PJ, 1980, THESIS DALHOUSIE U H; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Nordli E., 1951, Nyt Magazin for Naturvidenskaberne, V88, P207; PETERSEN KS, 1992, LIMFJORDSPROJEKTET, P17; PETERSEN KS, 1990, LIMFJORDSPROJEKTET, P13; Phipps D., 1984, PAPERS GEOLOGY D PAR, V11, P1; Reid P.C., 1974, Nova Hedwigia, V25, P579; ROSSIGNOL MARTINE, 1962, POLLEN SPORES, V4, P121; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; Wall D., 1973, Geoscience Man, V7, P95; WALL D., 1967, PALAEONTOLOGY, V10, P95; Williams D.B., 1967, MAR GEOL, V5, P389; 1995, VANDMILJO LIMFJORDEN	41	113	120	0	14	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	2000	109	1					65	81		10.1016/S0034-6667(99)00045-7	http://dx.doi.org/10.1016/S0034-6667(99)00045-7			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	307YW	10708791				2025-03-11	WOS:000086682600004
J	Mahmoud, MS; Moawad, ARMM				Mahmoud, MS; Moawad, ARMM			Jurassic-Cretaceous (Bathonian to Cenomanian) palynology and stratigraphy of the West Tiba-1 borehole, northern Western Desert, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article							DINOFLAGELLATE CYSTS; TERTIARY BOUNDARY; ISRAEL	Land-derived pollen and spores and marine dinoflagellate cysts were extracted from the Jurassic and Cretaceous sediments of the West Tiba-1 borehole, northern Western Desert, Egypt. On the basis of the recovered palynomorphs, of known stratigraphical significance, the following stages were assessed: Bathonian-Oxfordian (Middle-Late Jurassic) and Hauterivian, Aptian-Early Albian, Late Albian-Early Cenomanian, Early Cenomanian and Late Cenomanian (Early-Middle Cretaceous). No palynomorphs diagnostic for the Berriasian, Valanginian and Barremian stages (Early Cretaceous) were depicted. Based on the nature and composition of the identified palynomorph content, five informal palynomorph assemblage zones were recognised. These are: the Gonyaulacysta jurassica-Korystocysta kettonensis Assemblage Zone (PI, Bathonian-Oxfordian), Ephedripites-Aeguitriradites verrucosus Assemblage Zone (PII, Hauterivian), Afropollis jardinus-Duplexisporites generalis-Tricalpites Assemblage Zone (PIII, Aptian-Early Albian), Nyssapollenites-Elaterosporites Assemblage Zone (PIV, Late Albian-Early Cenomanian) and Assemblage Zone PV (Early-Late Cenomanian). The latter zone was differentiated into two subzones, namely the Classopollis brasiliensis-Elaterosporites klaszii Assemblage Subzone (PVa, Early Cenomanian) and Afropollis kahramanensis-Triporates Assemblage Subzone (PVb, Late Cenomanian). The time stratigraphy of the studied interval was revised. The occurrences and types of the dinoflagellate cysts, extracted from the studied succession, reflect a general shallow (shelf) marine palaeoenvironment. (C) 2000 Elsevier Science Limited. All rights reserved.	Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt	Egyptian Knowledge Bank (EKB); Assiut University	Mahmoud, MS (通讯作者)，Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt.		Mahmoud, Magdy/ABD-1262-2020					ABOULA ELA N. 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Afr. Earth Sci.	FEB	2000	30	2					401	416		10.1016/S0899-5362(00)00026-9	http://dx.doi.org/10.1016/S0899-5362(00)00026-9			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	313CQ					2025-03-11	WOS:000086983100011
J	Janofske, D				Janofske, D			<i>Scrippsiella trochoidea</i> and <i>Scrippsiella regalis</i>, nov comb. (Peridiniales, Dinophyceae):: A comparison	JOURNAL OF PHYCOLOGY			English	Article						Atlantic Ocean; biomineralization; calcareous cyst; Calciodinelloideae; crystallography; Scrippsiella regalis; Scrippsiella trochoidea; theca; ultrastructure	DINOFLAGELLATE RESTING CYSTS; MARINE-SEDIMENTS; NORTH-SEA; ULTRASTRUCTURE; PHYTOPLANKTON; AUSTRALIA; GERMANY; BIGHT	Culture experiments on dinoflagellates from the Atlantic Ocean revealed Scrippsiella regalis (Gaarder) Janofske, nov. comb., a calciodinelloid species with a spherical spiny calcareous cyst, This calcareous cyst was collected previously from plankton and sediment samples, where it was described as the coccolithophorid Discosphaera regalis Gaarder or was often mistaken for the cyst of Scrippsiella trochoidea (von Stein) Loeblich III. The morphological features of both the cellulosic theca and the calcareous cyst of S, trochoidea and S, regalis were compared with respect to their systematic position and the emendation of taxa, Both species were found to have different distribution patterns. Scrippsiella trochoidea is known only from the neritic environment, whereas S, regalis has been found mostly in oceanic samples, The preservation of these spiny calcareous dinocysts in the (fossil) sediment was dependent on the ultrastructure of the calcareous layer of the cyst wall.	Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany	University of Bremen	Janofske, D (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330440, D-28334 Bremen, Germany.							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Phycol.	FEB	2000	36	1					178	189		10.1046/j.1529-8817.2000.98224.x	http://dx.doi.org/10.1046/j.1529-8817.2000.98224.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	294NN					2025-03-11	WOS:000085917500022
J	Torricelli, S				Torricelli, S			Lower Cretaceous dinoflagellate cyst and acritarch stratigraphy of the Cismon APTICORE (Southern Alps, Italy)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						acritarchs; new taxa; biostratigraphy; dinoflagellate cysts; Italy; Lower Cretaceous; Southern Alps	EISENACK 1958; SECTION; SEA	A pelagic sedimentary succession, virtually complete from the Upper Hauterivian to the Upper Aptian and unconformably overlain by the Middle-Upper Albian p.p., was continuously cored in the Belluno Basin (southern Alps, NE Italy) as part of the APTICORE Program. APTICORE at Cismon Valley penetrated 131.8 m of limestones, marls and black shales, with 100% recovery of good quality cored material. One hundred and forty-six samples recovered from the marl and shale beds of the Cismon core were processed and analyzed for palynomorphs. Most of them yielded relatively rich and fairly well preserved assemblages of marine and terrestrially-derived palynomorphs. The results of a qualitative study of dinoflagellate cysts and acritarchs are presented and discussed. The distributions of 150 taxa are tabulated against the chronostratigraphy independently established on the basis of original litho-, bio-, chemo-, magnetostratigraphic investigations and of correlations with extensively studied sections outcropping in the vicinity of the Cismon drill site. The acritarch Pinocchiodinium erbae gen. et sp. nov. is described. Due to its distinctive morphology and extremely constant occurrence also in the black shales of the Selli Level, it is proposed as a marker species for the Aptian sediments of the Tethys. The dinoflagellate cysts Kallosphaeridium dolomiticum sp. nov. and Nexosispinum hesperus brevispinosum subsp. nov, are described from the Upper Hauterivian. Additional taxonomic remarks are made about other dinoflagellate cyst species, including the emendations of Tanyosphaeridium magneticum Davies 1983 and Bourkidinium granulatum Morgan 1975. The biostratigraphic value of selected taxa is discussed and compared with data known both from the Tethyan and Boreal realms. In particular, the extinction of Bourkidinium granulatum emend. is proposed as the best dinoflagellate cyst event for the delimitation of the Hauterivian-Barremian boundary in the Northern Hemisphere. The first appearance datums of Prolixosphaeridium parvispinum and Odontochitina operculata, and the slightly younger last appearance datum of Nexosispinum vetusculum are confirmed as useful biohorizons for recognition of the lower part of the Upper Barremian and hence for the approximation of the Lower-Upper Barremian boundary. The last occurrences of Rhynchodiniopsis aptiana and Phoberocysta neocomica are calibrated in the basal Aptian. (C) 2000 Elsevier Science B.V. All rights reserved.	ENI SpA, Agip Div, STIG, I-20100 Milan, Italy	Eni SpA	Torricelli, S (通讯作者)，ENI SpA, Agip Div, STIG, POB 12069, I-20100 Milan, Italy.	stefano.torricelli@agip.it						ARHUS N, 1991, CRETACEOUS RES, V12, P209; ARTHUR MA, 1990, NATO ADV SCI I C-MAT, V304, P75; 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; BINT A N, 1986, Palynology, V10, P135; BRIDEAUX W., 1971, PALAEONTOGRAPHICA B, V135, P53; BRIDEAUX WW, 1975, B GEOL SURV CAN, V252, P85; BRIDEAUX WW, 1977, B GEOL SURV CAN, V281, P89; BUJAK JP, 1978, GEOLOGICAL SURVEY CA, V297, P1; Cecca Fabrizio, 1996, Rivista Italiana di Paleontologia e Stratigrafia, V102, P417; CHANNELL JET, 1979, EARTH PLANET SC LETT, V42, P153, DOI 10.1016/0012-821X(79)90021-9; COOKSON IC, 1958, ROYAL SOC VICTORIA P, V70, P19; DAVEY R J, 1969, Bulletin of the British Museum (Natural History) Geology, V17, P105; DAVEY R J, 1974, Palaeontology (Oxford), V17, P623; Davey R.J., 1979, Initial Reports of the Deep Sea Drilling Project, V48, P547; Davey R.J., 1978, INIT REPS DSDP, V40, P883, DOI [10.2973/dsdp.proc.40.125.1978, DOI 10.2973/DSDP.PROC.40.125.1978]; Davey R.J., 1973, REV ESP MICROPALEONT, V5, P173; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; DAVEY RJ, 1974, BIRBAL SAHNI I PALAE, V3, P41; DAVIES E. H., 1983, GEOL SURV CAN B, V359, P1; DOLDING PJD, 1992, ANTARCT SCI, V4, P311, DOI 10.1017/S0954102092000476; DUCHENE RJ, 1986, B CTR RECH EXPLOR PR, V12, P1; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Eisenack A., 1960, P R SOC VIC, V72, P1; ERBA E, 1994, PALEOCEANOGRAPHY, V9, P483, DOI 10.1029/94PA00258; Erba E, 1998, RIV ITAL PALEONTOL S, V104, P181, DOI 10.13130/2039-4942/5330; ERBA E, 1999, IN PRESS J FORAM RES; Erba Elisabetta, 1996, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V66, P31; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P158, DOI 10.1073/pnas.49.2.158; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Fensome R.A., 1993, CLASSIFICATION FOSSI; HABIB D, 1987, INITIAL REPORTS DEEP, V92, P751; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; HEILMANNCLAUSEN C, 1987, TGEOL SURV DENMARK A, V17, P1; HELENES J, 1984, Palynology, V8, P107; Iosifova EK, 1996, REV PALAEOBOT PALYNO, V91, P187, DOI 10.1016/0034-6667(95)00064-X; Larson R.L., 1993, APTICORE ALBICORE WO; Leereveld H, 1997, CRETACEOUS RES, V18, P421, DOI 10.1006/cres.1997.0071; LEEREVELD H, 1988, 7 INT PAL C BRISB AU, P92; Leerveld H., 1995, LPP Contribution Series, V2, P1; Lentin J.K., 1993, A.S.S.P., V28, P1; Lister Janice K., 1995, Geologisches Jahrbuch Reihe A, V141, P367; LONDEIX L, THESIS U BORDEAUX; LUCAS-CLARK J, 1984, Palynology, V8, P165; LUTAT P, 1995, THESIS U HANNOVER; Millioud M.E., 1969, 1ST P INT C PLANKT M, V2, P420; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; MORGAN R, 1975, J PROC R SOC N S W, V108, P157; Nohr-Hansen Henrik, 1993, Gronlands Geologiske Undersogelse Bulletin, V166, P1; POURTOY D, 1989, THESIS U BORDEAUX; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; Reneville P. D., 1981, B CEN RECH EXPLOR PR, V5, P1; SARJEANT WAS, 1985, REV PALAEOBOT PALYNO, V45, P47, DOI 10.1016/0034-6667(85)90065-X; SINGH C, 1971, B RES COUNC ALBERTA, V28, P1; Singh C., 1983, ALBERTA RES COUNCIL, V44, P1; SRIVASTAVA SK, 1984, CAHIERS MICROPALEONT, P1; Stover L.E., 1987, ASS AUST PALAEONTOL, V4, P261; STOVER LE, 1987, ASS AUSTR PALAEONTOL, V4, P227; Williams G.L., 1985, P847; Williams Graham L., 1998, AASP Contributions Series, V34, P1; WILPSHAAR M, 1995, CRETACEOUS RES, V16, P273, DOI 10.1006/cres.1995.1020	64	33	37	0	3	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	FEB	2000	108	3-4					213	266		10.1016/S0034-6667(99)00041-X	http://dx.doi.org/10.1016/S0034-6667(99)00041-X			54	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	318RG	10704645				2025-03-11	WOS:000087297200005
C	Cooper, RA; Crampton, JS; Uruski, CI			CM; CM	Cooper, RA; Crampton, JS; Uruski, CI			The time-calibrated composite - A powerful tool in basin exploration	2000 NEW ZEALAND PETROLEUM CONFERENCE PROCEEDINGS			English	Proceedings Paper	8th New Zealand Petroleum Conference	MAR 19-22, 2000	CHRISTCHURCH, NEW ZEALAND	Crown Minerals, Contact, Fletcher Challenge Energy, NZ Oil & Gas, PEANZ, Shell Co Ltd, Westech Orion, Methanex, Natl Gas Coprp, Venture Taranaki				The Taranaki Basin has a complex geological history and biostratigraphic data are key to resolving many stratigraphic and structural problems facing the explorationist. Biostratigraphic data, however, are themselves complex and contradictory; inconsistencies in fossil ranges can be caused by incomplete sampling, misidentification, sedimentary reworking, and real variations in the distribution of species. Because of these factors, the problem of correlation Is enormous when dealing with large numbers of fossil species in many wells. Quantitative stratigraphic methods address these problems by using a variety of objective or semi-objective mathematical approaches. A quantitative biostratigraphic analysis of eight Taranaki exploration wells demonstrates that a substantial amount of new high resolution biostratigraphic information can be extracted from existing data. The range tops of 87 taxa, representing foraminifers, nannofossils, pollen, spores, and dinoflagellates, in cuttings samples have been used to derive a precise correlation of the eight wells that compares favourably with seismic correlations. The PC program, Constrained Optimisation (CONOP), which employs the principles of both graphic correlation and unitary association, has been used, and the method extended to derive a composite section that is calibrated against the time scale. Using this "time-calibrated composite", the depositional history of the well sequences can be determined, and the stratigraphic position, age and duration of unconformities can be determined. From the eight wells studied, it appears that during the Paleocene through Oligocene interval, there were short pulses of relatively rapid deposition separated by periods of nondeposition. A regional unconformity at the base of the Eocene is revealed. The time-calibrated composite promises to be a powerful tool in basin analysis, particularly for detecting sequence boundaries.	Inst Geol & Nucl Sci, Lower Hutt, New Zealand	GNS Science - New Zealand	Cooper, RA (通讯作者)，Inst Geol & Nucl Sci, POB 30-368, Lower Hutt, New Zealand.		Crampton, James/G-1381-2012					ALROY J, 1994, PALEOBIOLOGY, V20, P191, DOI 10.1017/S0094837300012677; Chambers J. M., 1983, GRAPHICAL METHODS DA; COOPER RA, AAPG B; Geux J., 1991, Biochronological Correlations; Kemple W.G., 1995, Graphic correlation, V53, P65, DOI DOI 10.2110/PEC.95.53.0065; King P.R., 1999, Institute of Geological and Nuclear Sciences folio series, V1; King SM, 1996, VISUAL NEUROSCI, V13, P1, DOI 10.1017/S0952523800007082; MANN KO, 1995, SEPM SPECIAL PUBLICA, V53; MORGANS HEG, 1996, 9638 I GEOL NUCL SCI, P1	9	1	3	0	0	CROWN MINERALS MINISTRY ECONOMIC DEVELOPMENT	WELLINGTON	PO BOX 1473, WELLINGTON, NEW ZEALAND			0-478-23482-1				2000							346	354						9	Energy & Fuels; Engineering, Petroleum; Geosciences, Multidisciplinary	Conference Proceedings Citation Index - Science (CPCI-S)	Energy & Fuels; Engineering; Geology	BU96T					2025-03-11	WOS:000177511800036
J	Roncaglia, L				Roncaglia, L			A new dinoflagellate species from the Upper Cretaceous of New Zealand - a morphological intermediate between three genera	ALCHERINGA			English	Article						New Zealand; Conway siltstone; dinoflagellates; taxonomy; Campanian; Upper Cretaceous		The new dinoflagellate Isabelidinium marshallii sp. nov. was encountered in the lower to middle Campanian Satyrodinium haumuriense Interval Zone and in the middle to upper Campanian Isabelidinium korojonense Interval Zone, in southern Marlborough, South Island, New Zealand. The new taxon is attributed to Isabelidinium but it also closely resembles species of Alterbidinium and Satyrodinium. Despite its close morphological affiliation to three dinoflagellate genera, I. marshallii represents a discrete population of peridinioid cysts that has a stratigraphically useful range in New Zealand.	Univ Modena & Reggio Emilia, Dipartimento Sci Terra, I-41100 Modena, Italy	Universita di Modena e Reggio Emilia	Roncaglia, L (通讯作者)，Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark.							[Anonymous], 1987, ASS AUSTRALASIAN PAL; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin RA, 1999, J PALEONTOL, V73, P373, DOI 10.1017/S0022336000027888; EVANS PR, 1971, GEOLOGY GEOPHYSICS A, V134, P30; Fensome RA., 1993, MICROPALEONTOLOGY, V7; Field BD., 1997, INST GEOL NUCL SCI M, V19; KHOWAJAATEEQUZZ.GR, 1991, PALEOBOTANIST, V39, P37; LENTIN J K, 1986, Palynology, V10, P111; LENTIN JK, 1975, CAN J BOT, V53, P2147, DOI 10.1139/b75-241; MARSHALL NG, 1990, ALCHERINGA, V14, P1, DOI 10.1080/03115519008619004; MARSHALL NG, 1988, ASS AUSTR PALEONTOLO, V5, P195; Pascher A., 1914, Berlin Ber D bot Ges, V32; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Roncaglia L, 1999, REV PALAEOBOT PALYNO, V106, P121, DOI 10.1016/S0034-6667(99)00005-6; Roncaglia L., 1997, IGNS SCI REPORT, V97, P1; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; Warren G., 1978, New Zealand Geological Survey Bulletin, V92, P1; Williams GL., 1985, FOSSIL DINOFLAGELLAT; WILLIAMS GL, 1998, AM ASS STRAT PALYNOL, V34; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; WILSON GJ, 1984, NEW ZEAL J BOT, V22, P549, DOI 10.1080/0028825X.1984.10425289	21	2	2	1	1	GEOLOGICAL SOCIETY AUSTRALIA INC	SYDNEY	701 WYNYARD HOUSE, 301 GEORGE STREET, SYDNEY, NSW 2000, AUSTRALIA	0311-5518			ALCHERINGA	Alcheringa		2000	24	1-2					135	146		10.1080/03115510008619530	http://dx.doi.org/10.1080/03115510008619530			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	305GZ					2025-03-11	WOS:000086532200012
J	Guerstein, GR; Guler, MV				Guerstein, GR; Guler, MV			Biostratigraphy based on Eocene-Miocene dinoflagellate cysts from (YPF) Ombucta x-1 borehole, Colorado Basin, Argentina	AMEGHINIANA			Spanish	Article						biostratigraphy; dinoflagellate cyst events; Eocene-Miocene; Colorado Basin; Argentina		Sediments between 250 and 850 metres deep from the exploration Ombucta x-1 borehole, located onshore Colorado Basin, were studied palynologically. Dinoflagellate cysts are present in varying amounts allowing age interpretation for the section. Selected dinoflagellate cyst events, mainly last occurrences, suggest five age intervals: late Miocene to early Pliocene, late Miocene, mid Miocene, Oligocene to early Miocene and Eocene to Oligocene. The comparison of the selected dinoflagellate events with previous studies carried out by other authors indicates that these events are consistent throughout the basin. The composition of the dinoflagellate assemblages, with dominance of gonyaulocoids over peridinioids, reflects poor nutrient oceanic conditions. Law dinocyst/pollen ratios at the end of the Miocene and during the Oligocene suggest relatively nearshore environments confirmed by high dominance of the complex Operculodinium israelianum/centrocarpum. Sediments ranging from mid to early Miocene in age show high dinocyst/pollen ratios associated with oceanic species acmes.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; Comis Invest Cient Prov Buenos Aires, Buenos Aires, DF, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Comision de Investigaciones Cientificas	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.							[Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1981, COMITE SUDAMERICANO; ARCHANGELSKY S, 1996, 13 C GEOL ARG 3 C EX, V4, P67; BECKER D, 1980, 2 C ARG PAL BIOESTR, V2, P315; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BUJAK JP, 1980, PALAEONTOLOGY, V24, P26; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; EDWARDS LE, 1996, AM ASS STRATIGRAPHIC, V3, P985; FENSOME RA, 1998, D3653 DINOFLAJ GEOL; FENSOME RA, 1993, 7 MICR PRESS; FRYKLUND R, 1996, 13 C GEOL ARG 3 C EX, V8, P135; GAMERRO J C, 1981, Revista Espanola de Micropaleontologia, V13, P119; Guerstein G.R., 1990, Revista Espanola de Micropaleontologia, V22, P459; Guerstein G.R., 1990, Revista Espanola de Micropaleontologia, V22, P167; Guerstein G.R., 1995, ASOCIACION PALEONTOL, V3, P63; Guerstein G. R., 1990, REV ESP MICROPALEONT, V22, P33; GUERSTEIN GR, IN PRESS MICROPALEON; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P423, DOI 10.2973/odp.proc.sr.105.135.1989; Head Martin J., 1998, Mededelingen Nederlands Instituut voor Toegepaste Geowetenschappen TNO, V60, P199; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; HEUSSER L E, 1984, Palynology, V8, P225; Kaasschieter J.P.H., 1963, TULSA GEOLOGICAL SOC, V31, P177; Lesta P., 1978, 7 C GEOL ARG NEUQ AC, V1, P701; MALUMIAN N, 1972, Ameghiniana, V9, P97; MALUMIAN N, 1970, Ameghiniana, V7, P173; MALUMIAN N, 1998, 10 C LAT GEOL 6 C NA, V1, P114; Malumian N., 1998, 10 C LAT GEOL 6 C NA, V1, P125; Malumian N., 1996, GEOLOGIA RECURSOS NA, P73; MATSUOKA K, 1992, NEOGENE QUATERNARY D, P162; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; Palamarczuk S, 1998, AMEGHINIANA, V35, P415; Quattrocchio, 1997, REV ESP MICROPALEONT, V29, P115; Quattrocchio, 1988, 2 JORN GEOL BON BAH, P27; QUATTROCCHIO M, 1988, REV ASOCIACION GEOLO, V43, P375; Quattrocchio Mirta E., 1996, Revista Espanola de Micropaleontologia, V28, P111; Ruiz L.C., 1997, REV ESP MICROPALEONT, V29, P13; RUIZ LC, 1994, THESIS U NACIONAL SU; RUIZ LC, 1996, GEOLOGIE AFRIQUE ATL, P361; UCHUPI E, 1991, MAR GEOL, V102, P1, DOI 10.1016/0025-3227(91)90003-M; VERA ToRRES J. A., 1994, ESTRATIGRAFIA PRINCI; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D., 1967, PALAEONTOLOGY, V10, P95; WILLIAMS G. L., 1998, AM ASS STRATIGRAPHIC, V34; WILLIAMS GL, 1998, SOC SEDIMENTARY GEOL, V60; ZAMBRANO JJ, 1980, 2 S GEOL REG ARG AC, V2, P1033	45	14	15	1	2	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana		2000	37	1					81	90						10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	313XL					2025-03-11	WOS:000087024900008
J	Barreda, V; Palamarczuk, S				Barreda, V; Palamarczuk, S			Palynostratigraphy of Late Oligocene-Miocene deposits in the southern San Jorge gulf area, Santa Cruz Province, Argentina	AMEGHINIANA			Spanish	Article						pollen; spores; dinocysts; Oligocene; Miocene; Santa Cruz Province; Argentina	DINOFLAGELLATE CYSTS	A preliminar palynostratigraphic framework is proposed for Cenozoic deposits cropping out in the southern San Jorge Gulf area, Santa Cruz Province, Argentina. Pollen and spores assemblages and associated dinoflagellate cysts recovered from three sections, Mazarredo, Punta Nava and Ei Fare, were analysed. On the basis of the palynological content two units were recognised and informally named: Unit 1 and Unit 2. Unit 1, represented in Mazarredo and Punta Nava sections, was assigned to the Late Oligocene. The paleoenvironment was identified as a lagoon for the former and inner shelf for the latter. The underlying Unit 2, comprising the top of Punta Nava and El Fare sections, is considered to be Early Miocene in age and deposited in a sublitoral to coastal environment. It can be correlated with the Chenque Formation (Chubut Province). Both dinoflagellate cyst and adjacent land derived pollen and spores suggest humid and warm-temperate climatic conditions for the Late Oligocene and a slight deterioration for the Early Miocene.	CIRGEO, RA-1414 Buenos Aires, DF, Argentina		Barreda, V (通讯作者)，CIRGEO, JR de Velazco 847, RA-1414 Buenos Aires, DF, Argentina.			Barreda, Viviana Dora/0000-0002-1560-1277				[Anonymous], 1996, Palynology: principles and applications; Anzotegui L.M., 1986, Facena, V6, P101; Barreda V.D., 1999, Revista Espanola de Micropaleontologia, V31, P53; Barreda VD, 1998, AMEGHINIANA, V35, P321; Barreda Viviana D., 1997, Ameghiniana, V34, P283; Barreda Viviana D., 1996, Ameghiniana, V33, P35; Barreda Viviana D., 1993, Palynology, V17, P169; Barrett EJ, 1997, SOC SCI J, V34, P131, DOI 10.1016/S0362-3319(97)90046-X; BELLOSI E, 1995, B INFORMACIONES PETR, V4, P50; BERTELS A, 1978, 2 C ARG PAL BIOESTR, V2, P213; BERTELS A, 1975, REV ESP MICROPALEONT, V7, P426; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Dettmann M.E., 1987, BRIT ANTARCTIC SURVE, V77, P13; DUENAS H, 1980, REV PALAEOBOT PALYNO, V30, P313, DOI 10.1016/0034-6667(80)90016-0; FASOLA A, 1969, Ameghiniana, V6, P3; FEAGLE JG, 1995, 6 C ARG PAL BIOESTR, V1, P129; GRAHAM A, 1996, INT COMP C P, V1, P123; Guerstein G. R., 1990, REV ESP MICROPALEONT, V22, P33; GUYOHLSON D, 1996, PALYNOLOGY PRINCIPLE, P181; LEGARRETA L, 1990, 2 S TERC CHIL CONC A, V1, P135; Legarreta Leonardo, 1994, Ameghiniana, V31, P257; LIMA M R D, 1985, Anais da Academia Brasileira de Ciencias, V57, P183; M?ller KJ., 1987, FOSSILS STRATA, V19, P1; Macphail M. K., 1994, Papers and Proceedings of the Royal Society of Tasmania, V128, P1; Malumian N., 1998, 10 C LAT GEOL 6 C NA, V1, P285; Malumian N., 1989, REV ASOC GEOL ARGENT, V43, P257; MARTIN HA, 1982, ANN MO BOT GARD, V69, P625, DOI 10.2307/2399086; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; Mildenhall D.C., 1989, New Zealand Geological Survey Paleontological Bulletin, V59, P1; MULLER J, 1981, BOT REV, V47, P1, DOI 10.1007/BF02860537; Nanez C., 1988, REV ASOC GEOL ARGENT, V43, P493; Ottone E.G., 1998, REV ESP MICROPALEONT, V30, P35; Palamarczuk S, 1998, AMEGHINIANA, V35, P415; Parma S.G., 1989, Ameghiniana, V25, P213; PARMA SG, 1985, REV ASOCIACION GEOLO, V37, P23; Pocknall D.T., 1984, New Zealand Geological Survey Paleontological Bulletin, V51, P1; Romero EJ., 1978, AMEGHINIANA, V15, P209; STOVER L E, 1973, Proceedings of the Royal Society of Victoria, V85, P237; Windhausen A., 1924, Boletin Academia Nacional de Ciencias, V27, P167	39	49	53	0	3	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana		2000	37	1					103	118						16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	313XL					2025-03-11	WOS:000087024900010
J	Palamarczuk, S; Barreda, V				Palamarczuk, S; Barreda, V			Late Paleogene-Early Neogene palynology, Aries x-1 well, Argentine continental shelf, Tierra del Fuego, Argentina.	AMEGHINIANA			Spanish	Article						dinoflagellates; pollen and spores; palynostratigraphy; Argentine continental shelf; Oligocene; Miocene	OLIGOCENE; PROVINCE	Nineteen cutting samples from the Aries x-l well, drilled in the Argentine continental shelf, offshore Tierra del Fuego, were analized for palynology. Marine and terrestrial palynomorph assemblages, fairly well preserved, though neither diverse nor abundant, were recovered throughout the studied interval, comprising depths between 240-640 m. Four sections, D, C, B and A from bottom to top are informally proposed on the basis of the palynological content. Sections D through B are considered Oligocene in age, most probably Upper Oligocene, whereas section A yielded Early Miocene assemblages, according to previously recorded species distribution in nearby areas. Two marine events were recognized in sections C and A respectively. The first is characterized by the presence of high amounts of protoperidinioid dinoflagellate cysts (up to 98%) mostly Brigantedinium sp., and the second, by equivalent amounts of both major dinocyst groups-gonyaulacoids, protoperidiniods- with absolute dominance of Nematosphaeropsis rigida Wrenn (32% of the assemblage). An environmental trend from estuarine-transitional restricted (section C) to neritic nearshore marine (section A) is suggested. Terrestrial palynomorphs are abundant in sections C and A. Levels 500-550 m have large amounts of Nothofagidites spp., pterydophyte spores and fungal remains, probably reflecting forest vegetation in the surrounding area. The interval 260-300 m,section A, yielded a diverse pollen grain assemblage mostly composed of the herbaceous and shrubby families Cyperaceae, Asteraceae, Chenopodiaceae and Anacardiaceae.	Ctr Invest Recursos Geol, RA-1414 Buenos Aires, DF, Argentina		Palamarczuk, S (通讯作者)，Ctr Invest Recursos Geol, JR de Velazco 847, RA-1414 Buenos Aires, DF, Argentina.			Barreda, Viviana Dora/0000-0002-1560-1277				Barreda V, 2000, AMEGHINIANA, V37, P103; Barreda V, 2000, AMEGHINIANA, V37, P3; Barreda VD, 1998, AMEGHINIANA, V35, P321; Barreda Viviana D., 1997, Ameghiniana, V34, P283; Barreda Viviana D., 1996, Ameghiniana, V33, P35; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; BRADFORD MR, 1975, CAN J BOT, V53, P3064, DOI 10.1139/b75-335; Cross A.T., 1966, MAR GEOL, V4, P467, DOI [10.1016/0025-3227(66)90012-0, DOI 10.1016/0025-3227(66)90012-0]; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; DEVERNAL A, 1992, AM ASS STRATIGRAPHIC, P329; HEAD MJ, 1992, AM ASS STRATIGRAPHIC, P1; MALUMIAN N, 1999, ACTAS, V1, P369; Matsuoka Kazumi, 1997, Palynology, V21, P19; Mildenhall D.C., 1989, New Zealand Geological Survey Paleontological Bulletin, V59, P1; Palamarczuk S, 1998, AMEGHINIANA, V35, P415; Pocknall D.T., 1984, New Zealand Geological Survey Paleontological Bulletin, V51, P1; POCKNALL DT, 1985, NEW ZEAL J GEOL GEOP, V28, P329; STOVER L E, 1973, Proceedings of the Royal Society of Victoria, V85, P237	18	32	34	0	0	ASOCIACION PALEONTOLOGICA ARGENTINA	BUENOS AIRES	MAIPU 645, 1ER PISO, 1006 BUENOS AIRES, ARGENTINA	0002-7014			AMEGHINIANA	Ameghiniana		2000	37	2					221	234						14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	341LF					2025-03-11	WOS:000088591300011
J	Godhe, A; Karunasagar, I; Karunasagar, I; Karlson, B				Godhe, A; Karunasagar, I; Karunasagar, I; Karlson, B			Dinoflagellate cysts in recent marine sediments from SW India	BOTANICA MARINA			English	Article							GYMNODINIUM-CATENATUM; ADJACENT SEAS; RESTING CYSTS; DINOPHYCEAE; AUSTRALIA; TASMANIA; NORWAY; WATERS; NORTH	During the period February-June 1996, dinoflagellate cysts were sampled and examined from surface sediments from two different estuaries and three different offshore sites around Mangalore, SW India. Forty-three different types of cysts were recorded in the sediment, of which 38 cysts belonged to the orders Gonyaulacales, Gymnodinales and Peridiniales. Five cyst types could not be identified. Five types of cysts recorded belonged to the potentially toxic genera of Alexandrium Halim emend. Balech and Gymnodinium Stein. The toxic species Gymnodinium catenatum Graham was studied, for the first time, in Indian waters. The cyst flora from SW India is compared to earlier studies on cyst biodiversity and biogeography from the tropics. To our knowledge this is the first study of dinoflagellate cysts in recent coastal sediments from Indian waters.	Univ Gothenburg, Dept Marine Biol, Inst Bot, SE-40530 Gothenburg, Sweden; Univ Agr Sci Mangalore, Coll Fisheries, Dept Fishery Microbiol, Mangalore 575002, India	University of Gothenburg; College of Fisheries, Mangalore; University of Agricultural Sciences Bangalore	Godhe, A (通讯作者)，Univ Gothenburg, Dept Marine Biol, Inst Bot, Box 461, SE-40530 Gothenburg, Sweden.		Karlson, Bengt/HII-5550-2022	Karlson, Bengt/0000-0002-7524-3504				ANDERSON DM, 1988, J PHYCOL, V24, P255; [Anonymous], 1989, 1 IND FISH FOR P AS; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; 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; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Dale B., 1979, P443; DALE B, 1994, NATO ASI SER, V17, P521; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; 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; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; ERADLEDENN E, 1993, TOXIC PHYTOPLANKTON, P109; Fukuyo Y., 1990, RED TIDE ORGANISMS J, P430; Godhe Anna, 1996, Harmful Algae News, V15, P1; 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]; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Karunasagar I., 1989, P65; KARUNASAGAR I, 1984, CURR SCI INDIA, V53, P247; KARUNASAGAR I, 1990, TOXICON, V28, P868, DOI 10.1016/S0041-0101(09)80010-X; Karunasagar Iddya, 1992, Journal of Shellfish Research, V11, P477; 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; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; PERSSON A, 1997, 8 INT C HARMF ALG VI, P161; SOETRE MML, 1994, DINOFLAELLATCYSTOR S; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; SUBRAHMANYAN R., 1954, INDIAN JOUR FISH, V1, P182; Taylor F.J.R., 1973, P155; Thomsen HA., 1992, Plankton i Indre Danske Farvande. En Analyse Af Forekomsten Af Alger Og Heterotrofe Protister (Ekskl. Ciliater) i Kattegat; TOMAS CR, 1996, INDENTIFYING MARINE; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1968, NEW PHYTOL, V67, P315, DOI 10.1111/j.1469-8137.1968.tb06387.x; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D., 1967, PHYCOLOGIA, V6, P83; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1	45	52	61	0	12	WALTER DE GRUYTER & CO	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055			BOT MAR	Bot. Marina	JAN	2000	43	1					39	48		10.1515/BOT.2000.004	http://dx.doi.org/10.1515/BOT.2000.004			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	284HT					2025-03-11	WOS:000085326700004
J	Persson, A; Godhe, A; Karlson, B				Persson, A; Godhe, A; Karlson, B			Dinoflagellate cysts in recent sediments from the west coast of Sweden	BOTANICA MARINA			English	Article							MOTILE STAGE RELATIONSHIPS; GYMNODINIUM-CATENATUM; MARINE-SEDIMENTS; RESTING CYSTS; DINOPHYCEAE; NORWAY; FJORD; AUSTRALIA; TASMANIA	This is the first study of dinoflagellate cysts in recent coastal sediments from the Swedish west coast. Sediments from 19 sites were investigated. Fifty-four types of cysts were encountered, of these 40 were identified to species level, representing 13 genera. The most common species were those of Lingulodinium polyedrum, Protoceratium reticulatum, Scrippsiella trochoidea, Pentapharsodinium dalei and Gonyaulax cf. spinifera. Cysts of the potentially toxic species Alexandrium minutum and Alexandrium tamarense were widely distributed as well as Gymnodinium nolleri, the non-toxic G. catenatum-like microreticulate cyst found in Northern Europe. Nine of the species found in this survey have not previously been reported from Sweden: Diplopelta parva, D. symmetrica, Diplopsalopsis latipeltata, Diplopsalis lebourae, Protoperidinium americanum, P. avellana, P. divaricatum, P. nudum and P. stellatum.	Univ Gothenburg, Dept Marine Bot, SE-40530 Gothenburg, Sweden	University of Gothenburg	Persson, A (通讯作者)，Univ Gothenburg, Dept Marine Bot, Box 461, SE-40530 Gothenburg, Sweden.		Karlson, Bengt/HII-5550-2022	Persson, Agneta/0000-0003-0202-6514; Karlson, Bengt/0000-0002-7524-3504				ANDERSON DM, 1980, J PHYCOL, V16, P166; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; 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 CJS, 1998, RAPP BOT SER, P18; BRAVO I, 1997, HARMFUL ALGAE NEWS, V16, P4; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Dale B., 1979, P443; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; DALE B, 1993, DEV MAR BIO, V3, P47; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DALE B, 1994, NATO ASI SER, V1, P521; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; Drebes G., 1974, MARINES PHYTOPLANKTO; 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, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; Ellegaard M., 1998, THESIS U COPENHAGEN; ERARDLEDENN E, 1993, DEV MAR BIO, V3, P109; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Fukuyo Yasuo., 1990, RED TIDE ORGANISMS J; Godhe Anna, 1996, Harmful Algae News, V15, P1; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; MATSUOKA K, 1988, REV PALAEOBOT PALYNO, V56, P95, DOI 10.1016/0034-6667(88)90077-2; Morzadec-Kerfourn M. T., 1977, Revue Micropaleont, V20, P157; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; *NIVA, 1996, SED GOT BOH KYSTV 19; PEPERZAK L, 1996, HARMFUL TOXIC ALGAL, P169; Rosenberg R, 1996, J SEA RES, V35, P1, DOI 10.1016/S1385-1101(96)90730-3; SOETRE MML, 1994, DINOFLAGELLATCYSTER; SONNEMANN JA, 1997, BOT MAR, V40, P147; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; Tomas C.R, 1997, Identifying Marine Phytoplankton, P387; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1968, NEW PHYTOL, V67, P315, DOI 10.1111/j.1469-8137.1968.tb06387.x; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D., 1967, PHYCOLOGIA, V6, P83; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1	47	90	97	0	18	WALTER DE GRUYTER & CO	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055			BOT MAR	Bot. Marina	JAN	2000	43	1					69	79		10.1515/BOT.2000.006	http://dx.doi.org/10.1515/BOT.2000.006			11	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	284HT					2025-03-11	WOS:000085326700006
J	Benoit, É; Laurent, D; Mattei, C; Legrand, AM; Molgó, J				Benoit, É; Laurent, D; Mattei, C; Legrand, AM; Molgó, J			Reversal of Pacific ciguatoxin-1B effects on myelinated axons by agents used in ciguatera treatment	CYBIUM			English	Article; Proceedings Paper	1st Ichtyological Conference in France, RIF 2000	MAR 29-31, 2000	PARIS, FRANCE			ciguatera fish poisoning; ciguatoxins; Na+ channels; myelinated axons; therapeutic agents; cellular electrophysiology; axonal volume	SODIUM-CHANNELS; MANNITOL; BREVETOXINS; TERMINALS	Ciguatera fish poisoning is a distinctive form of ichthyosarcotoxism characterised mainly by gastrointestinal and neurological disturbances. The ciguatoxins, responsible for this poisoning, are complex polyethers produced by toxic strains of the dinoflagellate Gambierdiscus toxicus. These toxins are increased to dangerous levels for man during their transmission through herbivorous and carnivorous fish, various species being contaminated. The known molecular target of ciguatoxins is the voltage-gated Na+ channel. During the action of these toxins, the permanent opening of channels, at the resting membrane potential, produces a continuous entry of Naf ions in excitable cells causing a marked increase in membrane excitability and in cellular volume. To precise the neurocellular basis of the efficacy of some agents used in clinical and traditional treatments of ciguatera, their effects were studied on frog myelinated axons exposed to Pacific ciguatoxin-1B (CTX-1B). During the action of this toxin, the increase in axonal volume and membrane excitability was reversed by lidocaine (a local anaesthetic), by CaCl2 and by hyperosmotic external solutions (containing D-mannitol, sucrose or tetramethylammonium chloride). The CTX-1B-induced hyperexcitability of the membrane was also reversed by extracts of Argusia argentea leaves or Davallia solida rhizomes, used traditionally in New-Caledonia. It is concluded that the various agents studied are able to counteract the neurocellular effects of CTX-1B in myelinated axons. These results are of particular interest since they provide a scientific basis to understand the beneficial action of therapeutic agents used in the treatment of ciguatera fish poisoning.	CNRS, Neurobiol Cellulaire & Mol Lab, UPR 9040, Bat 32, F-91198 Gif Sur Yvette, France; Inst Rech Dev, Lab Subst Nat, Noumea 98848, New Caledonia; Inst Rech Med Louis Malarde, Unite Oceanog Med, Papeete, Tahiti, France	Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD)		benoit@nbcm.cnrs-gif.fr		BENOIT, Evelyne/0000-0001-5501-0888				ALLSOP JL, 1986, REV NEUROL-FRANCE, V142, P590; AMADE P, 1992, REC ADV TOXINOL RES, V2, P503; Benoit E, 1996, NEUROSCIENCE, V71, P1121, DOI 10.1016/0306-4522(95)00506-4; Benoit Evelyne, 1994, Memoirs of the Queensland Museum, V34, P461; BIDARD JN, 1984, J BIOL CHEM, V259, P8353; Blythe Donna G., 1994, Memoirs of the Queensland Museum, V34, P465; CAMERON J, 1991, J NEUROL SCI, V101, P93, DOI 10.1016/0022-510X(91)90022-Y; Dechraoui MY, 1999, TOXICON, V37, P125, DOI 10.1016/S0041-0101(98)00169-X; GLAZIOU P, 1994, TOXICON, V32, P863, DOI 10.1016/0041-0101(94)90365-4; HAMBLIN PA, 1995, N-S ARCH PHARMACOL, V352, P236; Hogg RC, 1998, NEUROSCI LETT, V252, P103, DOI 10.1016/S0304-3940(98)00575-8; Laurent D, 1993, GRATTE CIGUATERA REM; Lewis RJ, 1998, J AM CHEM SOC, V120, P5914, DOI 10.1021/ja980389e; LOMBET A, 1987, FEBS LETT, V219, P355, DOI 10.1016/0014-5793(87)80252-1; Mattei C, 1999, BRAIN RES, V847, P50, DOI 10.1016/S0006-8993(99)02032-6; Mattei C, 1997, NEUROSCI LETT, V234, P75, DOI 10.1016/S0304-3940(97)00665-4; MOLGO J, 1990, BRIT J PHARMACOL, V99, P695, DOI 10.1111/j.1476-5381.1990.tb12991.x; Molgo Jordi, 1994, Memoirs of the Queensland Museum, V34, P577; MURATA M, 1990, J AM CHEM SOC, V112, P4380, DOI 10.1021/ja00167a040; PALAFOX NA, 1988, JAMA-J AM MED ASSOC, V259, P2740, DOI 10.1001/jama.259.18.2740; PEARN JH, 1989, MED J AUSTRALIA, V151, P77, DOI 10.5694/j.1326-5377.1989.tb101165.x; Poli MA, 1997, TOXICON, V35, P733, DOI 10.1016/S0041-0101(96)00166-3; Purcell CE, 1999, TOXICON, V37, P67, DOI 10.1016/S0041-0101(98)00134-2; RUSSELL FE, 1991, J TOXICOL-TOXIN REV, V10, P37, DOI 10.3109/15569549109058575; SWIFT AEB, 1993, J TOXICOL-CLIN TOXIC, V31, P1, DOI 10.3109/15563659309000371	25	14	17	0	2	SOC FRANCAISE D ICHTYOLOGIE	PARIS	MUSEUM NATL D HISTOIRE NATURELLE, 43 RUE CUVIER, 75231 PARIS, FRANCE	0399-0974			CYBIUM	Cybium		2000	24	3		S			33	40						8	Zoology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Zoology	401YY					2025-03-11	WOS:000166958100005
J	Zonneveld, KAF; Brummer, GJA				Zonneveld, KAF; Brummer, GJA			(Palaeo-)ecological significance, transport and preservation of organic-walled dinoflagellate cysts in the Somali Basin, NW Arabian Sea	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article; Proceedings Paper	9th Meeting of the European-Union-of-Geoscientists (EUG 9)	MAY 23-27, 1997	STRASBOURG, FRANCE	European Union Geosci			GONYAULAX-TAMARENSIS; INDIAN-OCEAN; SOUTHWEST MONSOON; LAST DEGLACIATION; MARINE-SEDIMENTS; NORTH-ATLANTIC; ADJACENT SEAS; PRODUCTIVITY; SURFACE; TEMPERATURE	To date, relatively little information is available about factors influencing organic-walled cyst production of tropical dinoflagellates and processes influencing the final burial of cysts in bottom sediments, such as transport and preservation. To extend this information, cyst fluxes were documented for three sediment traps from June 1992 to February 1993 at two sites in the Somali Basin (northwestern Arabian Sea) as well as the cyst association of underlying sediments. By comparing cyst associations of contemporaneously collected trap samples at different depths at one site, information about transport and processes of decay in the water column was obtained. Neither transport nor decay appears to have any detectable influence on cyst association during cyst settlement through the water column. Comparing the trap associations with the underlying sediments indicates that downslope transport appears to have influenced the cyst association on a local scale only. Species-selective decay, probably related to the presence of oxygen bottom sediments, has influenced the cyst association most pronouncedly at the most offshore site. Relating variations in the trap associations with environmental conditions of the overlying surface waters indicates that highest production of both filled and empty cysts occurs during the SW Monsoon upwelling. Based on this correlation three groups of species can be distinguished: Species with highest fluxes during (1) the first-half of the SW Monsoon (June-August); Bitectatodinium spongium, Echinidinium granulatum, Echindinium transparantum, Echinidnium spp., cysts of Protoperidinium compressum and cysts of Protoperidinium subinerme, (2) the transition between the SW-Monsoon and inter-Monsoon; Spiniferites mirabilis and Spiniferites spp., (3) no particular season; all other species. Cyst associations of all trap samples are dominated by cyst of Protoperidinium species. Cysts with highest fluxes during the SW-Monsoon form about a third of the associations. (C) 2000 Elsevier Science Ltd. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; Netherlands Inst Sea Res, Dept Marine Chem & Geol, NL-1790 AB Den Burg, Netherlands	University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Zonneveld, KAF (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.		Brummer, Gerard/I-1187-2014					ABRAHAMS MV, 1993, ECOLOGY, V74, P258, DOI 10.2307/1939521; AKSU AE, 1992, PALAEOGEOGR PALAEOCL, V92, P121, DOI 10.1016/0031-0182(92)90138-U; 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 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; [Anonymous], NOVA HEDWIGIA; [Anonymous], 1996, Am. Assoc. Strat. 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R., 1987, BOT MONOGR, V21; Turon J.L., 1984, MEM I GEOL BASSIN AQ, V17, P1; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; VANHINTE JE, 1995, TRACING SEASONAL UPW, V4; Veldhuis MJW, 1997, DEEP-SEA RES PT I, V44, P425, DOI 10.1016/S0967-0637(96)00116-1; VERSTEEGH GJM, 1994, MAR MICROPALEONTOL, V23, P147, DOI 10.1016/0377-8398(94)90005-1; Versteegh GJM, 1996, GLOBAL PLANET CHANGE, V11, P155, DOI 10.1016/0921-8181(95)00054-2; Walker L.M., 1984, P19; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WILLIAMS D.B., 1971, MICROPALAEONTOLOGY O; 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; Zonneveld KAF, 1997, QUATERNARY SCI REV, V16, P187, DOI 10.1016/S0277-3791(96)00049-2; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1; ZONNEVELD KAF, 1995, REV PALAEOBOT PALYNO, V84, P221, DOI 10.1016/0034-6667(94)00117-3; ZONNEVELD KAF, 1997, DEEP SEA RES; ZONNEVELD KAF, 1996, LPP CONTRIBUTIONS SE, V3, P1; ZONNEVELD KAF, 1997, IN PRESS REV PALAEOB	88	102	108	0	5	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.		2000	47	9-11					2229	2256		10.1016/S0967-0645(00)00023-0	http://dx.doi.org/10.1016/S0967-0645(00)00023-0			28	Oceanography	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	322DQ					2025-03-11	WOS:000087495300024
J	Hochuli, PA; Frank, SM				Hochuli, PA; Frank, SM			Palynology (dinoflagellate cysts, spore-pollen) and stratigraphy of the Lower Carnian Raibl Group in the Eastern Swiss Alps	ECLOGAE GEOLOGICAE HELVETIAE			English	Article						Austroalpine Silvretta Nappe; Early Carnian; stratigraphy; palynoloyg; dinoflagellate cysts; spore-pollen; organic matter; maturity	VITRINITE REFLECTANCE; ILLITE-CRYSTALLINITY; OBERHALBSTEIN; METAMORPHISM; MITTELBUNDEN; DIAGENESIS; PATTERN	Within the almost purely dolomitic units of the Triassic of the Austroalpine realm (Ladinian to Norian), the Cluozza Member is characterized as a conspicuously siliciclastic interval in the upper part of the Raibl Group. It represents a well-defined correlateable event in the Austroalpine Upper Triassic of Graubunden. Based on the present palynological evidence it can be assigned to the Early Carnian (Julian). The composition of the palynological assemblages is closely comparable to those of the upper Lunzer beds in the Alpine realm and to the Schilfsandstein in the Germanic basin. The palynological and lithological evidence indicates that these sediments have been deposited under humid conditions. The data also suggest that that Cluozza Member corresponds to the transgressive phase of an Early Carnian sequence (Car1 or Car2). The dinoflagellate cysts observed in the studied assemblages are not only the oldest found in the Northern Hemisphere but represent worldwide the oldest dinoflagellate records from low latitude sites.	ETH Zentrum, Fed Inst Technol, Dept Earth Sci, CH-8092 Zurich, Switzerland; Dr von Moos AG, Geotechn Buro, CH-8037 Zurich, Switzerland	Swiss Federal Institutes of Technology Domain; ETH Zurich	ETH Zentrum, Fed Inst Technol, Dept Earth Sci, CH-8092 Zurich, Switzerland.							[Anonymous], 1983, Prace Instytutu Geologicznego; [Anonymous], S E P M SPEC VOL J S; [Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 1996, Palynology: principles and applications; ARAKEL AV, 1982, J SEDIMENT PETROL, V52, P109; Batten D., 1996, Palynology: principles and applications, P1011; BATTEN DJ, 1973, PALAEONTOLOGY, V11, P1; Brenner W., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P487; Brenner W., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V122, P413, DOI 10.2973/odp.proc.sr.122.157.1992; BUJAK J P, 1976, Micropaleontology (New York), V22, P44, DOI 10.2307/1485320; EICHENBERGER U, 1986, MITT GEOL I U ETH ZU, V252, P1; Fensome R.A., 1993, CLASSIFICATION FOSSI; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; FRANK SM, 1986, MITT GEOL I ETH U ZU, V269, P1; FROITZHEIM N, 1994, ECLOGAE GEOL HELV, V87, P559; FURRER H, 1992, ECLOGAE GEOL HELV, V85, P245; FURRER H, 1985, MITT GEOL I ETH U ZU, V248, P1; Gianolla P., 1998, Mesozoic and Cenozoic sequence stratigraphy of European basins, P719, DOI 10.2110/pec.98.02.0719; Hardenbol J., 1998, Mesozoic and Cenozoic sequence chronostratigraphic framework of European basins; HEUNISCH C, 1986, Palaeontographica Abteilung B Palaeophytologie, V200, P33; Heunisch C., 1999, TRIAS GANZ ANDERE WE, P207; Hochuli P.A., 1989, CORRELATION HYDROCAR, P131; Hochuli P.A., 1998, SEPM SPEC PUBL, V60; Janofske Dorothea, 1992, Berliner Geowissenschaftliche Abhandlungen Reihe E Palaeobiologie, V4, P1; KLAUS W., 1960, JB GEOL BUNDE S ANT, V5, P107; Köppen A, 2000, PALAEOGEOGR PALAEOCL, V161, P193, DOI 10.1016/S0031-0182(00)00123-1; Leschik G., 1955, Schweiz. Palaontol. Abh., V72, P1; Lieberman H.M., 1979, Verhandlungen der Geologischen Bundesanstalt Wien, V2, P85; MAHLMANN RF, 1995, SCHWEIZ MINER PETROG, V75, P85; Mahlmann RF, 1996, SCHWEIZ MINER PETROG, V76, P23; MEISTER P, 1999, THESIS ETH ZURICH, P1; Reeves C., 1976, CALICHE ORIGIN CLASS; Ruffer T., 1995, SEQUENCE STRATIGRAPH, P161, DOI [10.1007/978-94-015-8583-5_7, DOI 10.1007/978-94-015-8583-5_7]; SCHEURING B W, 1970, Schweizerische Palaeontologische Abhandlungen, V88, P1; Schlager W., 1974, Mitteilungen geol Ges Wien, V66-67, P165; SIMMS MJ, 1989, GEOLOGY, V17, P265, DOI 10.1130/0091-7613(1989)017<0265:SOCCAE>2.3.CO;2; Spitz A., 1914, Beitraege zur Geologischen Karte der Schweiz, V44; Stover L.E., 1987, Memoir of the Association of Australasian Palaeontologists, V4, P101; Trumpy R., 1980, GEOLOGY SWITZERLAN A; VANDEREEM JGLA, 1983, REV PALAEOBOT PALYNO, V39, P189, DOI 10.1016/0034-6667(83)90016-7; VISSCHER H, 1994, REV PALAEOBOT PALYNO, V83, P217, DOI 10.1016/0034-6667(94)90070-1; Visscher H., 1981, Geol. Rundsch., V702, P625, DOI 10.1007/BF01822140; WIGGINS V D, 1973, Micropaleontology (New York), V19, P1, DOI 10.2307/1484961	43	45	49	0	2	BIRKHAUSER VERLAG AG	BASEL	VIADUKSTRASSE 40-44, PO BOX 133, CH-4010 BASEL, SWITZERLAND	0012-9402			ECLOGAE GEOL HELV	Eclogae Geol. Helv.		2000	93	3					429	443						15	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	395PJ					2025-03-11	WOS:000166588500011
J	Kim, YO; Han, MS				Kim, YO; Han, MS			Seasonal relationships between cyst germination and vegetative population of <i>Scrippsiella trochoidea</i> (Dinophyceae)	MARINE ECOLOGY PROGRESS SERIES			English	Article						Scrippsiella trochoidea; cyst germination; vegetative population; dormant period	GONYAULAX-TAMARENSIS; DINOFLAGELLATE CYSTS; NORTHEAST JAPAN; ONAGAWA BAY; BENTHIC CYSTS; RESTING CYSTS; ADJACENT SEAS; SEDIMENTS; DYNAMICS; BLOOMS	The seasonal occurrence of vegetative cells and cysts of the dinoflagellate Scrippsiella trochoidea in the water column was investigated in Yongil Bay (southeastern coast of Korea). To measure germination ratios of cysts, cysts were isolated monthly from natural sediment samples and incubated in the laboratory. Vegetative cell numbers peaked in June to July, when the surface water temperature increased to over 18 degreesC. Mass encystments were detected in the water column in August 1996 and July 1997, when the vegetative population flourished. Active germination was observed during the period of decreasing water temperature in September and October, when the vegetative population declined. Thus, there was an opposing pattern of seasonality in the potential germination of cysts and the proliferation of vegetative cells, whereby decreases in one paralleled increases in the other. The dormant period of cysts was ca 60 d, far longer than reported previously. Germination ratios increased in October 1996 and September 1997 after a 2 mo dormancy period following the mass encystments. Germination appears to be flexible with respect with length of dormancy and the age composition of cysts, both of which are based on the time and the scale of encystments as well as on conditions in the benthic environment.	Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea	Hanyang University	Hanyang Univ, Dept Life Sci, Seoul 133791, South Korea.	hanms@email.hanyang.ac.kr						Adachi R., 1972, Journal Fac Fish prefect Univ Mie, V9, P9; Anderson D.M., 1985, P219; 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; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; BINDER BJ, 1987, J PHYCOL, V23, P99; BRAARUD T, 1951, PHYSIOL PLANTARUM, V4, P28, DOI 10.1111/j.1399-3054.1951.tb07512.x; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; ISHIKAWA A, 1994, MAR BIOL, V119, P39, DOI 10.1007/BF00350104; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; ISHIKAWA A, 1995, THESIS TOHOKU U SEND; KIM CH, 1987, KOREAN J PHYCOL, V2, P211; Matsuoka K., 1989, P461; MONTAGNES D J S, 1987, Marine Microbial Food Webs, V2, P83; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Park J.S., 1989, P37; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Qin Xiao-ming, 1997, Chinese Journal of Oceanology and Limnology, V15, P173; REID PC, 1972, J MAR BIOL ASSOC UK, V52, P939, DOI 10.1017/S0025315400040674; SILVA E, 1962, NOTAS ESTUD INST BIOL MARITIMA, V26, P1; WALKER LM, 1979, J PHYCOL, V15, P312; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; 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; WATANABE MM, 1982, RES REP NATL I ENV S, V30, P27	28	41	52	1	14	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2000	204						111	118		10.3354/meps204111	http://dx.doi.org/10.3354/meps204111			8	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	365GW		Bronze			2025-03-11	WOS:000089943900010
J	Boddy, L; Morris, CW; Wilkins, MF; Al-Haddad, L; Tarran, GA; Jonker, RR; Burkill, PH				Boddy, L; Morris, CW; Wilkins, MF; Al-Haddad, L; Tarran, GA; Jonker, RR; Burkill, PH			Identification of 72 phytoplankton species by radial basis function neural network analysis of flow cytometric data	MARINE ECOLOGY PROGRESS SERIES			English	Article						radial basis functions; neural networks; principal component analysis; dinoflagellates; pyrmnesiomonads; flagellates; cryptomonads; diatoms	MARINE-PHYTOPLANKTON; CLASSIFICATION; SPORES; ALGAE	Radial basis function artificial neural networks (ANNs) were trained to discriminate between phytoplankton species based on 7 flow cytometric parameters measured on axenic cultures. Comparison was made between the performance of networks restricted to using radially-symmetric basis functions and networks using more general arbitrarily oriented ellipsoidal basis functions, with the latter proving significantly superior in performance. ANNs trained on 62, 54 and 72 taxa identified them with respectively 77, 73 and 70% overall success. As well as high success in identification, high confidence of correct identification was also achieved. Misidentifications resulted from overlap of character distributions. Improved overall identification success can be achieved by grouping together species with similar character distributions. This can be done within genera or based on groupings indicated in dendrograms constructed for the data on all species. When an ANN trained on 1 data set was tested with data on cells grown under different light conditions, overall successful identification was low (<20%), but when an ANN was trained on a combined data set identification success was high (>70%). Clearly it is essential to include data on cells covering the whole spectrum of biological variation. Ways of obtaining data for training ANNs to identify phytoplankton from field samples are discussed.	Univ Cardiff, Cardiff Sch Biosci, Cardiff CF10 3TL, S Glam, Wales; Univ Glamorgan, Sch Comp, Pontypridd CF37 1DL, M Glam, Wales; Plymouth Marine Lab, Ctr Coastal & Marine Sci, Plymouth PL1 3DH, Devon, England; Aquasense Lab, NL-1090 HC Amsterdam, Netherlands	Cardiff University; University of South Wales; Plymouth Marine Laboratory	Univ Cardiff, Cardiff Sch Biosci, Cardiff CF10 3TL, S Glam, Wales.	boddyl@cardiff.ac.uk	Boddy, Lynne/A-7250-2010; Alhaddad, Lina/AAV-6854-2021	Boddy, Lynne/0000-0003-1845-6738				BALFOORT HW, 1992, J PLANKTON RES, V14, P575, DOI 10.1093/plankt/14.4.575; BODDIE J, 1994, DATAMATION, V40, P15; BODDY L, 1999, MACHINE LEARNING MET, P37; BODDY L, 1998, INTELLIGENT ENG SYST, V8, P655; BURKILL PH, 1990, PHILOS T ROY SOC A, V333, P99, DOI 10.1098/rsta.1990.0141; Carr MR, 1996, J PLANKTON RES, V18, P1225, DOI 10.1093/plankt/18.7.1225; Caudill M., 1990, Naturally intelligent systems; CHEN S, 1991, IEEE T NEURAL NETWOR, V2, P302, DOI 10.1109/72.80341; Culverhouse PF, 1996, MAR ECOL PROG SER, V139, P281, DOI 10.3354/meps139281; DEMERS S, 1992, CYTOMETRY, V13, P291, DOI 10.1002/cyto.990130311; Dunn G., 1982, INTRO MATH TAXONOMY; Frankel DS, 1996, CYTOMETRY, V23, P290, DOI 10.1002/(SICI)1097-0320(19960401)23:4<290::AID-CYTO5>3.0.CO;2-L; FRANKEL DS, 1989, CYTOMETRY, V10, P540, DOI 10.1002/cyto.990100509; Fu L., 1994, NEURAL NETWORKS COMP; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Haykin S., 1994, NEURAL NETWORKS COMP; Hofstraat J.W., 1991, Journal of Fluorescence, V1, P249, DOI 10.1007/BF00865249; Hush DR, 1993, IEEE SIGNAL PROC MAG, V10, P8, DOI 10.1109/79.180705; Jeffrey SW., 1997, PHYTOPLANKTON PIGMEN; Jonker RR, 1995, WATER SCI TECHNOL, V32, P177, DOI 10.1016/0273-1223(95)00696-6; Kohonen T., 1998, Neurocomputing, V21, P1, DOI 10.1016/S0925-2312(98)00030-7; Morgan A, 1998, MYCOL RES, V102, P975, DOI 10.1017/S0953756297005947; MORRIS CW, 1992, MYCOL RES, V96, P697, DOI 10.1016/S0953-7562(09)80501-7; MORRIS CW, 1996, INTELLIGENT ENG SYST, V6, P629; Richard MD, 1991, NEURAL COMPUT, V3, P461, DOI 10.1162/neco.1991.3.4.461; SCHALKOFF R., 1992, PATTERN RECOGN; SMITS JRM, 1992, ANAL CHIM ACTA, V258, P11, DOI 10.1016/0003-2670(92)85193-A; Sneath P. H., 1973, Numerical Taxonomy: The Principles and Practice of Numerical Classification; WETTSCHERECK D, 1992, ADV NEUR IN, V4, P1133; WILKINS MF, 1994, COMPUT APPL BIOSCI, V10, P285; Wilkins MF, 1999, APPL ENVIRON MICROB, V65, P4404; WILKINS MF, 1994, BINARY-COMPUT MICROB, V6, P64; Wilkins MF, 1996, COMPUT APPL BIOSCI, V12, P9	33	62	75	1	13	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		2000	195						47	59		10.3354/meps195047	http://dx.doi.org/10.3354/meps195047			13	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	308MD		Bronze			2025-03-11	WOS:000086715100004
J	Vink, A; Zonneveld, KAF; Willems, H				Vink, A; Zonneveld, KAF; Willems, H			Distributions of calcareous dinoflagellate cysts in surface sediments of the western equatorial Atlantic Ocean, and their potential use in palaeoceanography	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; calcareous; ecology; western equatorial Atlantic; statistical analysis	NORTH-ATLANTIC; DEEP-SEA; CALCIUM-CARBONATE; CACO3 DISSOLUTION; MARINE-SEDIMENTS; ADJACENT SEAS; CEARA RISE; DEGLACIATION; CIRCULATION; DISPERSAL	Only very few studies focus on recent calcareous dinoflagellate cyst diversity, geographic distribution and ecology, so that information on the distribution patterns and environmental affinities of individual cyst species is extremely limited. This information is, however, essential if we want to use calcareous dinoflagellate cysts for palaeoenvironmental reconstruction Surface sediment samples from the generally oligotrophic western equatorial Atlantic Ocean, offshore northeast Brazil, were therefore quantitatively analysed for their calcareous dinoflagellate cyst content, including the calcareous vegetative coccoid Thoracosphaera heimii. Seven calcareous dinoflagellate cyst species/morphotypes and T. heimii were encountered in high concentrations throughout the area. Substantial differences in the distribution patterns were observed. The highest concentrations of cysts are found in sediments of the more oligotrophic, oceanic regions, beyond the influence of Amazon River discharge waters. Dinoflagellates producing calcareous cysts thus appear to be capable of surviving low nutrient concentrations and produce large numbers of cysts in relatively stable and predictable environments affected by minimal seasonality. To test for the environmental affinities of individual species, distribution patterns in surface sediments were compared with temperature, salinity, density and stratification gradients within the upper water column (0-100 m) over different times of the year, using principal components analysis and redundancy analysis. T. heimii and four of the seven encountered cyst species (Sphaerodinella? albatrosiana, two morphotypes of Sphaerodinella? tuberosa and Scrippsiella regalis) relate to these parameters significantly and the variations in the cyst associations appear to be associated with the different surface water currents characterising the area. The results imply that calcareous dinoflagellate cyst distributions can potentially be used to distinguish between different open oceanic environments and they could, therefore, be useful in tracing water mass movements throughout the late Quaternary. (C) 2000 Elsevier Science B.V. All rights reserved.	Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Willems, H (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.		Vink, Annemiek/GXG-6435-2022	Vink, Annemiek/0000-0002-5178-9721				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; [Anonymous], NEOGENE QUATERNARY D; [Anonymous], 1996, Am. Assoc. Strat. 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A., 1990, International Journal of Geographical Information Systems, V4, P313, DOI 10.1080/02693799008941549; PETERSON RG, 1991, PROG OCEANOGR, V26, P1, DOI 10.1016/0079-6611(91)90006-8; PHILANDER SGH, 1986, J GEOPHYS RES-OCEANS, V91, P14192, DOI 10.1029/JC091iC12p14192; PHILANDER SGH, 1986, J GEOPHYS RES-OCEANS, V91, P14212, DOI 10.1029/JC091iC12p14212; Pilskaln CH, 1987, GLOBAL BIOGEOCHEM CY, V1, P31, DOI 10.1029/GB001i001p00031; Pond S., 1983, INTRO DYNAMICAL OCEA, V2nd; RICHARDSON PL, 1994, J GEOPHYS RES-OCEANS, V99, P5081, DOI 10.1029/93JC03486; RICHARDSON PL, 1984, J PHYS OCEANOGR, V14, P633; Ruddiman WF, 1997, MAR GEOL, V136, P189, DOI 10.1016/S0025-3227(96)00069-2; Ruhlemann C, 1996, MAR GEOL, V135, P127, DOI 10.1016/S0025-3227(96)00048-5; SCHLUNZ B, 1998, BERICHTE FACHBEREICH, V116, P1; SCHULZ HD, 1991, FACHBEREICH GEOWISSE, V19, P1; STRAMMA L, 1990, DEEP-SEA RES, V37, P1875, DOI 10.1016/0198-0149(90)90083-8; TANGEN K, 1982, MAR MICROPALEONTOL, V7, P193, DOI 10.1016/0377-8398(82)90002-0; THUNELL RC, 1982, MAR GEOL, V47, P165, DOI 10.1016/0025-3227(82)90067-6; VAISALA V, 1925, COMMENT PHYS MAT SOC, V2, P1; VERARDO DJ, 1994, PALEOCEANOGRAPHY, V9, P63, DOI 10.1029/93PA02901; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Zonneveld KAF, 1996, PALAEOGEOGR PALAEOCL, V122, P89, DOI 10.1016/0031-0182(95)00091-7; ZONNEVELD KAF, 1999, IN PRESS USE PROXIES	74	38	40	0	12	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	JAN	2000	38	2					149	180						32	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	273CD					2025-03-11	WOS:000084688900003
J	Iakovleva, AI; Kulkova, IA; Cavagnetto, C				Iakovleva, AI; Kulkova, IA; Cavagnetto, C			Eocene microphytofossils (dinoflagellate cysts and continental palynomorphs) of Northwestern Siberia (Severnaya Sosva Basin)	NEWSLETTERS ON STRATIGRAPHY			English	Article								A palynological study (dinoflagellates and pollen grains) was carried out in two boreholes through the Eocene of the Severnaya Sosva River Basin in the north of Western Siberia. Five zones were identified: two (Dracodinium varielongitudum and Charlesdowniea coleothrypta zones) in the Ypresian, and three (Rhombodinium draco, Rhombodinium pouosum and Kisselevia ornata zones) in the Bartonian. The absence of the dinoflagellate zones characterizing the Lutetian in other regions suggests an interruption in marine sedimentation in Northwestern Siberia during the beginning of the Middle Eocene. A palaeoecological interpretation of some dinoflagellate: groups was proposed. It shows a shallow marine environment with a reduced salinity, followed by a marine basin regression during the Bartonian. For the first time the ecology of the acritarch genera Paucilobimorpha and Tritonites was interpreted.	Univ Montpellier 2, Lab Paleoenvironm & Palynol, UMR CNRS 5554, ISEM, F-34095 Montpellier 5, France; Russian Acad Sci, Inst Geol, Lab Paleofloras, Moscow 109107, Russia; Russian Acad Sci, Associated Inst Geol Geophys & Mineral, Palynol Lab, Novosibirsk 630090, Russia	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences; Russian Academy of Sciences; Sobolev Institute of Geology & Mineralogy of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Iakovleva, AI (通讯作者)，Univ Montpellier 2, Lab Paleoenvironm & Palynol, UMR CNRS 5554, ISEM, Case 61, F-34095 Montpellier 5, France.		IAKOVLEVA, ALINA/ABH-9243-2020					ANDREEVAGRIGORO.AS, 1991, DETAILED PALEOGENE S; ANDREEVAGRIGORO.AS, 1985, GEOLOGICHESKIY J, V6, P112; [Anonymous], 2003, STUD GEOPHYS GEOD; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; BERGGREN WA, 1995, SOC EC PALEONTOLOGIS, V54, P195; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BROWN S, 1984, INITIAL REP DEEP SEA, V81, P565; Bujak J., 1980, PALAEONTOLOGICAL ASS, V24, P1; BUJAK J P, 1979, Micropaleontology (New York), V25, P308, DOI 10.2307/1485305; Caro Y., 1973, Revista Esp Micropaleont, V5, P329; Cavelier C., 1983, GEOL FRANCE, V3, P261; de Coninck J., 1988, Bulletin de la Societe Belge de Geologie, V97, P287; Heilmann-Clausen C., 1988, GEOLOGISCHES JB A, V100, P339; ILYINA VI, 1994, MICROPHYTOFOSSILS DE; KOTHE A, 1990, GEOLOGISCHES JB A, V118; KULKOVA IA, 1988, PLANT MICROFOSSILS S, P25; KULKOVA IA, 1990, GEOL GEOPHYSICS, V10, P25; NEILSEN OB, 1986, GEOSKRIFTER, V24, P235; Petrova I.A., 1986, RECOMMENDATIONS METH; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Powell AJ, 1992, BRIT MICROPALAEONTOL, P155; ROSTOVTSEV NN, 1955, SBORNIK VSEGEI, V2, P3; SCHUMACKERLAMBR.J, 1978, LAB PAL PAL, V8; Shatskii S.B, 1984, ENV LIFE BOUNDARIES, P9; Shatsky S.B., 1969, PROBLEMS STRATIGRAPH, P156; SHATSKY SB, 1989, CENOZOIC SIBERIA NE, P4; SIGOV AP, 1956, INT C CONC SYNTH STR, P25; Strelnikova NI., 1992, PALEOGENE DIATOMS; VASSILIEVA ON, 1990, PALYNOLOGY STRATIGRA; Vereshagin V.N., 1982, STRATIGRAPHICAL DICT; VOZZHENNIKOVA TF, 1963, OSNOVI PALEONTOLOGII, P179; VOZZHENNIKOVA TF, 1967, AKAD NAUK SSSR SIB O; VOZZHENNIKOVA TF, 1965, AKAD NAUK SSSR SIB O; VOZZHENNIKOVA TF, 1960, AKAD NAUK SSSR SIBIR, V1, P7; Williams G.L., 1977, Oceanic Micropalaeontology, V2, P1231	35	5	7	0	0	GEBRUDER BORNTRAEGER	STUTTGART	JOHANNESSTR 3A, D-70176 STUTTGART, GERMANY	0078-0421			NEWSL STRATIGR	Newsl. Stratigr.		2000	38	1					13	38		10.1127/nos/38/2000/13	http://dx.doi.org/10.1127/nos/38/2000/13			26	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	346VG					2025-03-11	WOS:000088891300002
J	Higgs, KT; Jones, GL				Higgs, KT; Jones, GL			Palynological evidence for Mesozoic karst at Piltown, Co. Kilkenny	PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION			English	Article; Proceedings Paper	Conference on Ireland Since the Carboniferous	SEP 09-10, 1998	ULSTER MUSEUM, BELFAST, NORTH IRELAND		ULSTER MUSEUM		IRISH	Exploration drilling by Pasminco Australia Ltd. in 1993 at Piltown near Carrick-on-Suir. encountered brown. yellow and fawn clays of the Piltown Clay Formation (new name) lying on and in Carboniferous limestone. Palynological analysis of these clays indicates that they are late Jurassic to early Cretaceous in age. The palynomorphs are well preserved but not abundant. They consist mostly of terrestrially derived spores and pollen grains, though the rare occurrence of dinoflagellate cysts indicates a weak marine influence in some of the sediments. The presence of these Mesozoic sediments within karstified limestone implies an active karat system before and/or during late Jurassic-early Cretaceous times in south County Kilkenny.	Natl Univ Ireland Univ Coll Cork, Dept Geol, Cork, Ireland	University College Cork	Higgs, KT (通讯作者)，Natl Univ Ireland Univ Coll Cork, Dept Geol, Cork, Ireland.							[Anonymous], 1996, Palynology: principles and applications; Batten D.J., 1996, Palynology: Principles and Applications, V2, P807; Batten D.J., 1996, Palynology: principles and applications, V2, P795; Boulant J.A., 1980, Handbook of the Hypothalamus, V3, P1; COXON P, 1987, P ROYAL IR AC B, V87, P2; Drew DP, 2000, P GEOLOGIST ASSOC, V111, P345, DOI 10.1016/S0016-7878(00)80090-5; DUNOYER GV, 1865, MEMOIRS GEOLOGICAL S; Evans A, 1998, MAR PETROL GEOL, V15, P299, DOI 10.1016/S0264-8172(98)00024-5; HERNGREEN GFW, 1989, GEOL MIJNBOUW-N J G, V68, P73; Higgs K., 1986, IRISH J EARTH SCI, P99; HUNT C O, 1985, Pollen et Spores, V27, P419; Jennings JosephN., 1985, Karst Geomorphology; JONES GL, 1992, TERRA NOVA, V4, P238, DOI 10.1111/j.1365-3121.1992.tb00478.x; Keeley ML, 1996, TERRA NOVA, V8, P259, DOI 10.1111/j.1365-3121.1996.tb00755.x; KEELEY ML, 1983, J EARTH SCI-DUBLIN, V5, P107; KEELEY ML, 1980, THESIS U DUBLIN; MITCHELL GF, 1980, J EARTH SCI R DUBL S, V3, P13; NAYLOR D, 1992, BASINS ATLANTIC SEAB, V62, P255; NAYLOR D, 1998, IRISH SHORE LINES GE; Self C.A., 1981, Caves of County Clare; Shannon PM, 1998, J PETROL GEOL, V21, P125, DOI 10.1111/j.1747-5457.1998.tb00651.x; Staplin FL., 1977, PALYNOLOGY, V1, P9, DOI [DOI 10.1016/j.coal.2012.06.002, 10.1080/01916122.1977.9989146, DOI 10.1080/01916122.1977.9989146]; Staplin FL., 1969, B CANADIAN PETROL GE, V17, P47; Walsh P. T., 1966, Quarterly Journal of the Geological Society of London, V122, P63; WATTS W. A., 1957, SCI PROC ROY DUBLIN SOC, V27, P309	25	10	11	0	4	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0016-7878			P GEOLOGIST ASSOC	Proc. Geol. Assoc.		2000	111		4				355	362		10.1016/S0016-7878(00)80091-7	http://dx.doi.org/10.1016/S0016-7878(00)80091-7			8	Geology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	423MZ					2025-03-11	WOS:000168181200007
J	de Vernal, A; Hillaire-Marcel, C				de Vernal, A; Hillaire-Marcel, C			Sea-ice cover, sea-surface salinity and halo-/thermocline structure of the northwest North Atlantic: modern versus full glacial conditions	QUATERNARY SCIENCE REVIEWS			English	Article; Proceedings Paper	1st PAGES Open Science Meeting	APR 19-23, 1998	UNIV LONDON, LONDON, ENGLAND		UNIV LONDON		LATITUDE MARINE ENVIRONMENTS; NORWEGIAN-GREENLAND SEA; MODERN ANALOG TECHNIQUE; LABRADOR SEA; DINOFLAGELLATE CYSTS; PLANKTONIC-FORAMINIFERA; PALYNOLOGICAL EVIDENCE; OCEANOGRAPHIC CHANGES; SEDIMENTATION-RATES; YOUNGER DRYAS	Seasonal sea-ice develops along the eastern continental margins in the northern North Atlantic, where freshwater and/or meltwater outflow are responsible for relatively low salinity in surface waters and very pronounced water mass stratification. Sea-ice constitutes a major parameter in the marine ecosystem since the duration and extent of its seasonal spreading constrain the plankton distribution and the related microfossil assemblages on the sea floor. Organic-walled dinoflagellate cysts that are highly resistant to dissolution were recovered from surface sediments of the northern North Atlantic, and used to develop transfer functions (best analogue method) for the reconstruction of the seasonal spreading and duration of sea-ice cover, in addition to salinity and temperature of the warmest month of the year. Application of the best analogue approach to cores from the Labrador Sea reveals large variations in sea-ice cover and sea-surface conditions throughout the last glacial stage and during the early Holocene. Isotopic analyses in epipelagic and mesopelagic planktonic foraminifers also suggest important changes in salinity and temperature gradients between the surface and sub-surface water masses. Specific study of the last glacial maximum LGM time slice (16-20 ka on a C-14 time scale) in the northwestern North Atlantic shows much more extensive sea-ice than at present, with perennial sea-ice lying along the continental margins of eastern Canada. Seasonal spreading of the cover of sea-ice offshore was accompanied by large seasonal contrasts in temperature, with very cold winters but relatively warm summers, a pattern linked to strong stratification between a buoyant low saline surface layer having a low thermal inertia, and the underlying intermediate oceanic waters. (C) 1999 Elsevier Science Ltd. All rights reserved.	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J	Eilertsen, HC; Wyatt, T				Eilertsen, HC; Wyatt, T			Phytoplankton models and life history strategies	SOUTH AFRICAN JOURNAL OF MARINE SCIENCE-SUID-AFRIKAANSE TYDSKRIF VIR SEEWETENSKAP			English	Article; Proceedings Paper	International Symposium and Workshop on Harmful Algal Blooms in the Benguela Current and Other Upwelling Ecosystems	NOV 05-06, 1998	MINIST FISHERIES & MARINE RESOURCES, SWAKOPMUND, NAMIBIA	World Bank, Intergovt Oceanog Commiss	MINIST FISHERIES & MARINE RESOURCES		POPULATION-DYNAMICS; BARENTS SEA; INTERANNUAL VARIABILITY; ENVIRONMENTAL-FACTORS; NORTHEAST JAPAN; WESTERN NORWAY; SPRING BLOOM; NOVA-SCOTIA; ONAGAWA BAY; OCEAN	Phytoplankton models generally do not consider the initial phases of seed stocks and deal only with the vegetative growth phase, ignoring life history strategies. Some quantitatively important diatoms, such as species of Chaetoceros and Skeletonema, have special strategies with respect to the timing of the planktonic phase that cannot be explained purely on the basis of environmental clues. In Norwegian waters and elsewhere, the first Chaetoceros bloom of the growth season usually starts in mid March, initiated by C. socialis. Other Chaetoceros species appear in the water column later. Species of dinoflagellates like Alexandrium also bloom at certain times of the year. In many cases, phytoplankton inocula originate from resuspension of bottom-dwelling spores or cysts rather than from residual planktonic vegetative cells, and it is probable that, in some species. inoculation events are controlled by endogenous biological clocks. The sequential appearance of different Chaetoceros species may be related to day-length-regulated germination of sports. Most Chaetoceros species have few generations, but they appear at opportunistic rimes in the plankton. In contrast. Skelelonema costatum and Scrippsiella trochoidea appear at any time of the year. Some modelling results can be improved by including the dynamics of phytoplankton seed stocks in the sediments.	Univ Tromso, NFH, Inst Marine & Freshwater Biol, N-9037 Tromso, Norway	UiT The Arctic University of Tromso	Univ Tromso, NFH, Inst Marine & Freshwater Biol, N-9037 Tromso, Norway.	eilertsen.hc@nfh.uit.no						ACKERFORS H, 1975, LYSEKIL, V179, P140; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; [Anonymous], ACTA BOT FENNICA; [Anonymous], 1983, INTRO SOLAR RAD; [Anonymous], 1983, ESTUARIES ENCLOSED S; Bagge P., 1971, MERENTUTKIMUSLAIT JU, V233, P19; Bakker C., 1978, Hydrobiological Bulletin, V12, P226, DOI 10.1007/BF02259185; BECK PA, 1980, THESIS U TROMSO; Blumberg AF., 1987, A description of a three-dimensional coastal ocean circulation model, V4, P1, DOI [DOI 10.1029/CO004P0001, 10.1029/co004p0001]; BRAARUD T, 1974, SARSIA, P63; BROWN RL, 1990, PACIFIC RIM CONGRESS 90, VOL 2, P1; CADEE GC, 1986, MAR BIOL, V93, P281, DOI 10.1007/BF00508265; COLEBROOK JM, 1979, MAR BIOL, V51, P23, DOI 10.1007/BF00389027; CONOVER RJ, 1984, CAN J FISH AQUAT SCI, V41, P232, DOI 10.1139/f84-027; 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Oceanogr, V2, P231; ZGUROVSKAYA LN, 1979, BIOL MORYA KIEV, V51, P46; ZIEMANN DA, 1991, MAR BIOL, V109, P321, DOI 10.1007/BF01319400	90	34	35	2	25	SEA FISHERIES RESEARCH INST DEPT ENVIRONMENT AFFAIRS	CAPE TOWN	PRIVATE BAG X2 ROGGE BAY 8012, CAPE TOWN, SOUTH AFRICA	0257-7615			S AFR J MARINE SCI	South Afr. J. Mar. Sci.-Suid-Afr. Tydsk. Seewetens.		2000	22						323	338		10.2989/025776100784125717	http://dx.doi.org/10.2989/025776100784125717			16	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	428LR		Bronze			2025-03-11	WOS:000168463600024
J	Courtinat, B				Courtinat, B			Review of the dinoflagellate cyst <i>Stephanelytron</i> Sarjeant 1961 emend	JOURNAL OF MICROPALAEONTOLOGY			English	Article							BIOSTRATIGRAPHY	The stratigraphic distribution of the Late Callovian to Early Oxfordian dinoflagellate cyst Stephanelytron on Sarjeant 1961 emend provides new evidence pertaining to its evolution. Middle and Upper Callovian times favoured the development of speciations to a short-ranging Stephanelytron community with corona(s) in ventral-posterior position (Stephanelytron brontes, S, callovianum, S. ceto and S, tabulophorum) from eurytopic species with antapical coronas (S. caytonense, S. membranoidium, S. redcliffense and S. scarburghense). The former group of species (except S. tabulophorum) may represent an example of peripatric speciation from an unfavourable mutation. The reduced stratigraphic range gives the appearance of an endemic population. The genus Lagenadinium Piel, 1985 is a junior synonym of Stephanelytron Sarjeant, 1961. A new emendation of Stephanelytron, two new combinations (S. callovianum and S. membranoidium) and two new species (?S. brontes and S. ceto) are proposed.	Univ Lyon 1, UFR Sci Terre, F-69622 Villeurbanne, France	Universite Claude Bernard Lyon 1	Courtinat, B (通讯作者)，Univ Lyon 1, UFR Sci Terre, 43 Blvd 11 Novembre 1918, F-69622 Villeurbanne, France.							ARHUS N, 1986, NORSK GEOLOGISK TIDD, V69, P39; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Cariou E., 1997, B CTR RECHERCHES ELF; COURTINAT B, 1980, DOCUMENT LAB GEOLOGI, V78, P3; COURTINAT B, 1989, DOCUMENT LAB GEOLOGI, V105; Davey R.J., 1987, Memoir of Geological Survey of Papua New Guinea, V13, P1; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; Davey RJ., 1979, AM ASS STRATIGRAPHIC, V5B, P49; DIMTER A, 1990, PALAEOGEOGR PALAEOCL, V80, P173, DOI 10.1016/0031-0182(90)90131-P; DODEKOVA L, 1992, Geologica Balcanica, V22, P33; DODEKOVA L, 1990, Geologica Balcanica, V20, P3; DODEKOVA L, 1975, BULG ACAD SCI PALAEO, V2, P17; DURR G, 1988, TUBINGER MIKROPALAON, V5, P1; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Erkmen U., 1980, Geobios (Villeurbanne), V13, P45, DOI 10.1016/S0016-6995(80)80014-3; Fauconnier D, 1996, MAR PETROL GEOL, V13, P707, DOI 10.1016/0264-8172(95)00024-0; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; FENSOME RA, 1979, GRONLANDS GEOLOGISKE, V132, P1; GITMEZ G U, 1972, Bulletin of the British Museum (Natural History) Geology, V21, P173; Gitmez G.U., 1970, B BRIT MUS NAT HIST, V18, P233; HABIB D, 1983, INITIAL REPORTS DSDP, V26, P623; HERNGREEN DFW, 1984, MEDEDELINGEN RIJKS G, V37, P96; LENTIN JK, 1990, CONTRIBUTIONS SERIES, V23, P1; LISTER J K, 1988, Palaeontographica Abteilung B Palaeophytologie, V210, P9; Mayr E., 1954, EVOLUTION PROCESS, P157; ODIN GS, 1990, GEOCHRONIQUE, V35, P12; PIEL KM, 1985, REV PALAEOBOT PALYNO, V45, P107, DOI 10.1016/0034-6667(85)90066-1; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; RIDING J B, 1988, Palynology, V12, P65; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; RIDING JB, 1992, BRIT MICROPALAEONTOL, P7; SARJEANT W. A. S., 1961, PALAEONTOLOGY, V4, P90; SARJEANT W. A. S, 1968, R MICROPALEONTOL, V10, P221; SARJEANT WA, 1979, CONTRIBUTIONS SER 5B, V2, P133; Sarjeant WAS., 1962, PALAEONTOLOGY, V5, P478; Smelror M., 1989, Palynology, V13, P121; SMELROR M, 1989, REV PALAEOBOT PALYNO, V61, P139, DOI 10.1016/0034-6667(89)90066-3; SMELROR M, 1988, RAPP GRONLANDS GEOLO, V137, P137; Stancliffe R.P.W., 1991, Journal of Micropalaeontology, V10, P185; STOVER L E, 1977, Micropaleontology (New York), V23, P330, DOI 10.2307/1485219; TAUGOURDEAULANT.J, 1985, DOCUMENTS BUREAU REC, V9511, P149; TAUGOURDEAULANT.J, 1984, DOCUMENTS BUREAU REC, V811, P59; THOMAS JE, 1988, REV PALAEOBOT PALYNO, V56, P313, DOI 10.1016/0034-6667(88)90063-2; Wheeler J.W., 1990, Modern Geology, V14, P267; Whitaker M.F., 1992, Geology of the Brent Group, V61, P169; WIERZBOWSKI A, 1990, NEWSL STRATIGR, V22, P7; WOLFARD A, 1981, REV PALAEOBOT PALYNO, V34, P321, DOI 10.1016/0034-6667(81)90048-8; ZOTTO M, 1987, MICROPALEONTOLOGY, V33, P193, DOI 10.2307/1485637	48	3	4	0	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH, AVON, ENGLAND BA1 3JN	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	DEC	1999	18		2				169	182		10.1144/jm.18.2.169	http://dx.doi.org/10.1144/jm.18.2.169			14	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	274QG		hybrid			2025-03-11	WOS:000084776100008
J	Garcés, E; Masó, M; Camp, J				Garcés, E; Masó, M; Camp, J			A recurrent and localized dinoflagellate bloom in Mediterranean beach	JOURNAL OF PLANKTON RESEARCH			English	Article							HARMFUL ALGAL BLOOMS; GONYAULAX-TAMARENSIS; PHYTOPLANKTON BLOOMS; POPULATION-DYNAMICS; ALEXANDRIUM-TAYLORI; LIFE; DINOPHYCEAE; MAINE; GULF	A recurrent, prolonged and singular bloom of Alexandrium taylori Balech in an open beach (La Fosca, Spain, NW Mediterranean) is described. Alexandrium taylori appears at several places along a wide area of the NW Mediterranean (Costa Brave) during the summer, reaching concentrations up to 10(5) cells 1(-1), but it only proliferates persistently, massively (densities >10(6) cells 1(-1)) and recurrently during August in La Fosca beach. The A.taylori bloom can be considered a manifestation of large-scale proliferation in a restricted area, where coupling between resting cysts in the sediment and bloom outbreak is not a major factor compared to the interaction of local environmental conditions with the planktonic organism's life history. From observations of environmental conditions (the environmental window) and the multiscale spatio-temporal distributions and life history of A.taylori, we describe the bloom dynamics and answer some critical questions about the different phases of the bloom. Some of these answers are: (i) the source of the A.taylori population is widespread offshore and is not located directly at the beach; (ii) high cell densities are reached and maintained with a moderate in situ growth and low loss rates; (iii) temporary cysts act as a reserve of the population.	Inst Ciencias Mar, Barcelona 08039, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Garcés, E (通讯作者)，Inst Ciencias Mar, P Joan de Borbo S-N, Barcelona 08039, Spain.		; Garces, Esther/C-5701-2011	Camp, Jordi/0000-0002-5202-9783; Garces, Esther/0000-0002-2712-501X				Anderson D.M., 1989, P11; 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; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Delgado M, 1997, J PLANKTON RES, V19, P749, DOI 10.1093/plankt/19.6.749; DELGADO M, 1990, Scientia Marina, V54, P1; FIGUEIRAS FG, 1994, J PLANKTON RES, V16, P857, DOI 10.1093/plankt/16.7.857; FRANKS PJS, 1992, MAR BIOL, V112, P165, DOI 10.1007/BF00349740; FRANKS PJS, 1992, MAR BIOL, V112, P153, DOI 10.1007/BF00349739; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garces E, 1998, J PHYCOL, V34, P880, DOI 10.1046/j.1529-8817.1998.340880.x; GARCES EP, 1998, THESIS U BARCELONA B; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Halim Y., 1960, Vie et Milieu, V11, P102; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HORSTMANN U, 1980, J PHYCOL, V16, P481, DOI 10.1111/j.1529-8817.1980.tb03064.x; LOMBARD EH, 1971, J PHYCOL, V7, P188, DOI 10.1111/j.1529-8817.1971.tb01500.x; MARGALEF R, 1969, INVEST PESQ, V33, P345; MARGALEF R., 1957, INVEST PESQ, V8, P89; Margalef R, 1997, SCI MAR, V61, P109; MARGALEF R, 1987, Investigacion Pesquera (Barcelona), V51, P121; MONTRESOR M, 1990, TOXIC MARINE PHYTOPLANKTON, P82; SELIGER HH, 1970, LIMNOL OCEANOGR, V15, P234, DOI 10.4319/lo.1970.15.2.0234; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; Steidinger K A, 1973, CRC Crit Rev Microbiol, V3, P49, DOI 10.3109/10408417309108745; Strickland J.D. H., 1968, A Practical Handbook of Seawater Analysis, V2nd; THRONDSEN J, 1995, ESTIMATING CELL NUMB; TYLER MA, 1981, LIMNOL OCEANOGR, V26, P310, DOI 10.4319/lo.1981.26.2.0310; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; YENTSCH CS, 1963, DEEP-SEA RES, V10, P221, DOI 10.1016/0011-7471(63)90358-9	34	68	72	1	9	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	DEC	1999	21	12					2373	2391		10.1093/plankt/21.12.2373	http://dx.doi.org/10.1093/plankt/21.12.2373			19	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	266EK					2025-03-11	WOS:000084287500009
J	Purkerson, SL; Baden, DG; Fieber, LA				Purkerson, SL; Baden, DG; Fieber, LA			Brevetoxin modulates neuronal sodium channels in two cell lines derived from rat brain	NEUROTOXICOLOGY			English	Article						Na+ channel; brevetoxin; single channel; patch clamp; neurotoxic shellfish poisoning; cell lines	CAT SENSORIMOTOR CORTEX; PTYCHODISCUS-BREVIS; NA+ CHANNEL; HIPPOCAMPAL-NEURONS; SENSORY NEURONS; MESSENGER-RNAS; DINOFLAGELLATE; SLICES; TOXINS; NERVE	Single Na+ channel currents were recorded from cell-attached membrane patches from two neuronal cell lines derived from rat brain, B50 and B104, and compared before and after exposure of the cells to purified brevetoxin, PbTx-3. B50 and B104 Na+ channels usually exhibited fast activation and inactivation as is typical of TTX-sensitive Na+ channels. PbTx-3 modified channel gating in both cell lines. PbTx-3 caused (1) significant increases in the frequency of channel reopening, indicating a slowing of channel inactivation, (2) a change in the voltage dependence of the channels, promoting channel opening during steady-state voltage clamp of the membrane at voltages throughout the activation range of Na+ currents, but notably near the resting potential of these cells (-60 - -50 mV), and (3) a significant, 6.7 mV hyperpolarized shift in the threshold potential for channel opening. Na+ channel slope conductance did not change in PbTx-3-exposed 850 and B104 neurons. These effects of Pbx-3 may cause hyperexcitability as well as inhibitory effects in intact brain. (C) 1999 Intox Press, Inc.	Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine Biol & Fisheries, NIEHS Marine & Freshwater Biomed Sci Ctr, Miami, FL 33149 USA	University of Miami; National Institutes of Health (NIH) - USA; NIH National Institute of Environmental Health Sciences (NIEHS)	Fieber, LA (通讯作者)，Univ Miami, Rosenstiel Sch Marine & Atmospher Sci, Div Marine Biol & Fisheries, NIEHS Marine & Freshwater Biomed Sci Ctr, 4600 Rickenbacker Cswy, Miami, FL 33149 USA.			Fieber, Lynne/0000-0002-7717-2260	NIEHS NIH HHS [ES05785, ES05705, ES05853] Funding Source: Medline	NIEHS NIH HHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS))		ALZHEIMER C, 1993, J NEUROSCI, V13, P660; APLAND JP, 1993, BRAIN RES BULL, V31, P201, DOI 10.1016/0361-9230(93)90026-8; ATCHISON WD, 1986, BRIT J PHARMACOL, V89, P731, DOI 10.1111/j.1476-5381.1986.tb11177.x; AULD VJ, 1988, NEURON, V1, P449, DOI 10.1016/0896-6273(88)90176-6; BADEN DG, 1982, TOXICON, V20, P457, DOI 10.1016/0041-0101(82)90009-5; BADEN DG, 1989, FASEB J, V3, P1807, DOI 10.1096/fasebj.3.7.2565840; BAINES D, 1992, MOL BRAIN RES, V16, P330, DOI 10.1016/0169-328X(92)90243-5; BIROSN HL, 1980, BRIT J PHARMACOL, V70, P249; BLACK JA, 1994, MOL BRAIN RES, V23, P235, DOI 10.1016/0169-328X(94)90230-5; BOHLE T, 1995, BIOPHYS J, V68, P121, DOI 10.1016/S0006-3495(95)80166-9; BORISON HL, 1985, TOXICON, V23, P517, DOI 10.1016/0041-0101(85)90036-4; CAMPBELL DT, 1993, PFLUG ARCH EUR J PHY, V423, P492, DOI 10.1007/BF00374946; Chang SY, 1996, BIOPHYS J, V70, P2581, DOI 10.1016/S0006-3495(96)79829-6; Crill WE, 1996, ANNU REV PHYSIOL, V58, P349, DOI 10.1146/annurev.physiol.58.1.349; DESHPANDE SS, 1993, TOXICON, V31, P459, DOI 10.1016/0041-0101(93)90181-H; DibHajj SD, 1996, FEBS LETT, V384, P78, DOI 10.1016/0014-5793(96)00273-6; FRENCH CR, 1985, NEUROSCI LETT, V56, P289, DOI 10.1016/0304-3940(85)90257-5; FRENCH CR, 1990, J GEN PHYSIOL, V95, P1139, DOI 10.1085/jgp.95.6.1139; GAWLEY RE, 1995, CHEM BIOL, V2, P533, DOI 10.1016/1074-5521(95)90187-6; HAMILL OP, 1981, PFLUG ARCH EUR J PHY, V391, P85, DOI 10.1007/BF00656997; Hille B., 1992, Ionic Channels of Excitable Membranes, V42, P1439; HUANG JMC, 1984, J PHARMACOL EXP THER, V229, P615; IKEDA SR, 1986, J NEUROPHYSIOL, V55, P527, DOI 10.1152/jn.1986.55.3.527; Jeglitsch G, 1998, J PHARMACOL EXP THER, V284, P516; KAYANO T, 1988, FEBS LETT, V228, P187, DOI 10.1016/0014-5793(88)80614-8; KIRSCH GE, 1989, J GEN PHYSIOL, V93, P85, DOI 10.1085/jgp.93.1.85; LLINAS R, 1980, J PHYSIOL-LONDON, V305, P171, DOI 10.1113/jphysiol.1980.sp013357; MOORMAN JR, 1990, NEURON, V4, P243, DOI 10.1016/0896-6273(90)90099-2; NODA M, 1986, NATURE, V320, P188, DOI 10.1038/320188a0; Penner R, 1995, SINGLE CHANNEL RECOR, V2nd; SAH P, 1988, J GEN PHYSIOL, V91, P373, DOI 10.1085/jgp.91.3.373; SCHREIBMAYER W, 1992, BIOCHIM BIOPHYS ACTA, V1104, P223; SCHUBERT D, 1974, NATURE, V249, P224, DOI 10.1038/249224a0; SEGAL MM, 1994, J NEUROPHYSIOL, V72, P1874, DOI 10.1152/jn.1994.72.4.1874; SHERIDAN RE, 1989, FEBS LETT, V247, P448, DOI 10.1016/0014-5793(89)81389-4; STAFSTROM CE, 1985, J NEUROPHYSIOL, V53, P153, DOI 10.1152/jn.1985.53.1.153; TAYLOR CP, 1988, TRENDS NEUROSCI, V11, P375, DOI 10.1016/0166-2236(88)90070-7; TAYLOR CP, 1993, TRENDS NEUROSCI, V16, P455, DOI 10.1016/0166-2236(93)90077-Y; WU CH, 1988, ANNU REV PHARMACOL, V28, P141; WU CH, 1985, TOXICON, V23, P481, DOI 10.1016/0041-0101(85)90032-7	40	35	42	0	6	INTOX PRESS INC	LITTLE ROCK	PO BOX 24865, LITTLE ROCK, AR 72221 USA	0161-813X			NEUROTOXICOLOGY	Neurotoxicology	DEC	1999	20	6					909	920						12	Neurosciences; Pharmacology & Pharmacy; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Neurosciences & Neurology; Pharmacology & Pharmacy; Toxicology	281FZ	10693972				2025-03-11	WOS:000085148400005
J	Morgans, HEG; Edwards, AR; Scott, GH; Graham, IJ; Kamp, PJJ; Mumme, TC; Wilson, GJ; Wilson, GS				Morgans, HEG; Edwards, AR; Scott, GH; Graham, IJ; Kamp, PJJ; Mumme, TC; Wilson, GJ; Wilson, GS			Integrated stratigraphy of the Waitakian-Otaian stage boundary stratotype, Early Miocene, New Zealand	NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS			English	Article						Oligocene; Miocene; Waitakian; Otaian; stage boundary stratotype; lithostratigraphy; biostratigraphy; geochronology; integrated stratigraphy; Bluecliffs Silt; Otekaike Limestone; planktonic foraminifera; benthic foraminifera; calcareous nannofossils; Mollusca; palynoflora; dinoflagellates; Radiolaria; oxygen isotopes; carbon isotopes; strontium isotopes	SOUTHWEST PACIFIC; SOUTHERN AUSTRALIA; EVENTS; BIOSTRATIGRAPHY; FORAMINIFERA; QUATERNARY; OLIGOCENE; TERTIARY; NEOGENE; MARGIN	The base of the type section of the Otaian Stage at Bluecliffs, South Canterbury, is recognised as the stratotype for the boundary between the Waitakian and Otaian Stages. Principal problems with the boundary are the restriction of existing bioevent proxies to shelf and upper slope environments and its uncertain age. These topics are addressed by a multidisplinary study of a 125 m section about the boundary, which examines its lithostratigraphy, depositional setting, biostratigraphy, correlation, and geochronology. The lower siltstone lithofacies (0-38.5 m) was deposited at upper bathyal depths (200-600 m) in a marginal basin which was partially sheltered from fully oceanic circulation by a submarine high and islands. The site was covered by cool-temperate water and was probably adjacent to the Subtropical Convergence. This unit is succeeded by the banded lithofacies (38.5-106 m) and the upper siltstone lithofacies (basal 19 m studied). Paleodepth probably declined up-sequence, but deposition at shelf depths is not definitely indicated. A cyclic pattern of abundance spikes in benthic and planktonic foraminifera commences 9 m above base and extends to 73 m in the banded lithofacies. Oxygen isotope excursions (up to 2.08 parts per thousand) in Euuvigerina miozea and Cibicides novozelandicus are greatest within the interval containing the abundance spikes. The stage boundary occurs in the banded lithofacies at the highest abundance spike (73 m). Although condensed intervals might affect the completeness of the section, they are not associated with sedimentary discontinuities, and we consider that the section is suitable as a biostratigraphic reference. Spores, pollens, dinoflagellates, calcareous nannofossils, foraminifera, bryozoans, and ostracods are preserved near the boundary, but molluscs principally occur higher, in the shallower upper siltstone lithofacies. Siliceous microfossils are rare. There is considerable scope for further biostratigraphic research. The primary event marking the boundary at 73 m is the appearance of the benthic foraminifer Ehrebergina marwicki. This is a distinctive and widely distributed event but is restricted to shelf and upper bathyal environments. Supplementary events in planktonic foraminifera and calcareous nannofossils were researched. Highest occurrences of Globigerina brazieri and G. euapertura are recorded at 47 and 58 m. There is a marked decline in relative abundance of Paragloborotalia spp. at 62 m. Helicosphaera carteri becomes more abundant than H. euphratis between 56 and 87 m. These events are not exact proxies for the boundary but they may usefully indicate proximity to it. They occur in the interval of prominent spikes in foraminiferal abundance. The Waitakian-Otaian boundary is dated at 21.7 h/Ia by strontium isotopes. Stable primary remanence could not be determined in a pilot paleomagnetic study of Bluecliffs specimens. However, specimens trended towards reversed polarity, and remagnetisation great circle analysis will allow directions to be calculated in future collections.	Inst Geol & Nucl Sci Ltd, Lower Hutt, New Zealand; Stratig Solut Ltd, Waikanae, New Zealand; Univ Waikato, Dept Earth Sci, Hamilton, New Zealand	GNS Science - New Zealand; University of Waikato	Morgans, HEG (通讯作者)，Inst Geol & Nucl Sci Ltd, POB 30 368, Lower Hutt, New Zealand.		Wilson, Gary/B-3803-2010	/0000-0002-2111-6817; Wilson, Gary/0000-0003-0025-3641; Kamp, Peter/0000-0002-2563-884X				ALLAN R. 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Z. J. Geol. Geophys.	DEC	1999	42	4					581	614		10.1080/00288306.1999.9514864	http://dx.doi.org/10.1080/00288306.1999.9514864			34	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	275NX		Bronze, Green Submitted			2025-03-11	WOS:000084827200008
J	Menichini, M				Menichini, M			Planktonic foraminiferal biostratigraphy and palaeoclimatic modeling of the pelagic Oligocene-Basal Miocene from the Piobbico Area (Marche basin, Central Italy)	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						Central Apennine; Inner Marchean Basin; Oligocene-Miocene; biostratigraphy; planktonic foraminifers; dinoflagellate cysts	INTEGRATED STRATIGRAPHY; SECTION; GUBBIO	In the Piobbico area (Pesaro, Central Italy, Inner Marchean Basin), outcrops of Paleogene to Early Miocene pelagic sediments are widespread and mainly consist of marls and marry limestones. In this paper two sections have been considered in the near Pieve d'Accinelli (PDA and PDA bis). A detailed biostratigraphic study was performed on planktonic foraminiferal assemblages using the standard zonations. PDA bis section spans from Early Oligocene to basal Aquitanian (Zone P20 to Subzone N4a), while PDA section is included in Zone N4 (Early Aquitanian). "Standard" bioevents such as the LO (Last Occurrence) of "Globigerina" ampliapertura, Chiloguembelina spp., Paragloborotalia opima opima and the FO (First Occurrence) of Paragloborotalia kugleri and of Globoquadrina dehiscens, together with other "added" bioevents, have been identified. Moreover, several peaks in abundance occur such as a fair peak of Dentoglobigerina in the middle-upper portion of Subzone P21b, a strong increase in abundance of Tenuitella and Catapsydrax groups in Subzone P21b, an increase in abundance of Dentoglobigerina at the top of Zone P22, of Globoquadrina in Subzone N4a, of Globigerinoides spp, at the top of Subzone N4a and of Globoquadrina dehiscens in Subzone N4b. A preliminary study of dinoflagellate cyst assemblages was carried out around Early Oligocene/Late Oligocene boundary Two bioevents such as a peak in abundance of Svalbardella cooksonae at the base of Subzone P21b and the FO of Impaginodinium minor at the base of Zone P22 have been identified. On the ground of a semiquantitative analysis of the planktonic foraminiferal assemblages, a paleoclimatic pattern has been tentatively inferred. This analysis suggests cool-temperate conditions at the top of Zone P20. In the lower part of the Late Oligocene the assemblages indicate the outset of very cool conditions, while the interval that spans Zone P22 to Subzone N4b is characterized by a generalized paleoclimatic instability.	Univ Perugia, Dipartimento Sci Terra, I-06100 Perugia, Italy	University of Perugia	Univ Perugia, Dipartimento Sci Terra, I-06100 Perugia, Italy.							Baumann P., 1970, Eclog. geol. Helv., V63, P1133; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BERGGREN WA, 1988, MICROPALEONTOLOGY, V34, P362, DOI 10.2307/1485604; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; Biolzi M., 1985, Memorie di Scienze Geologiche, V37, P303; Boersma A, 1987, PALEOCEANOGRAPHY, V2, P287, DOI 10.1029/PA002i003p00287; Coccioni R., 1997, Developments in Palaeontology and Stratigraphy, V15, P279; COCCIONI R, 1989, 28 INT GEOL C WASH D, V1, P308; Coccioni Rodolfo, 1994, Giornale di Geologia (Bologna), V56, P55; Guerrera F., 1977, G GEOL, V42, P109; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; LI Q, 1992, P ODP SCI RES, V20, P569; Luciani Valeria, 1996, Memorie di Scienze Geologiche, V48, P155; MOLINA E, 1979, THESIS U GRANDADA ZA; MONACO P, 1988, THESIS U PERUGIA PER; Montanari A., 1997, Developments in Palaeontology and Stratigraphy, V15, P249; MONTANARI A, 1991, NEWSL STRATIGR, V23, P151; Novaretti Anna, 1997, Palaeopelagos, V6, P299; SHAFIK S, 1978, BMR (Bureau of Mineral Resources) Journal of Australian Geology and Geophysics, V3, P135; SPEZZAFERRI S, 1991, PALAEOGEOGR PALAEOCL, V83, P217, DOI 10.1016/0031-0182(91)90080-B; SPEZZAFERRI S, 1995, PALAEOGEOGR PALAEOCL, V114, P43, DOI 10.1016/0031-0182(95)00076-X; Spezzaferri S., 1994, Paleontographia Italica, V81; Spezzaferri Silvia, 1996, Giornale di Geologia (Bologna), V58, P119; Spezzaferri Silvia, 1992, Palaeopelagos, V2, P79; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; Zevenboom D., 1995, PhD Thesis Diss	26	5	5	0	5	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.	DEC	1999	105	3					417	438		10.13130/2039-4942/5383	http://dx.doi.org/10.13130/2039-4942/5383			22	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	275CT					2025-03-11	WOS:000084802400005
J	Huault, V				Huault, V			Dinoflagellate cyst zonation of the Aalenian-Oxfordian interval on the southern margin of the Paris Basin	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			French	Review						stratigraphy; palynology; dinoflagellate; Dogger; Paris Basin	CYCLES; DOGGER	A palynostratigraphical analysis has been performed on the Dogger and the lower Maim strata in Burgundy. It is based on 400 samples recovered from 27 outcrops and 7 boreholes located in the southeast of the Paris Basin. Most of the outcrops and drillings have good macropalaeontological control (ammonites and brachiopods). The spectrum of dinoflagellate cysts comprises 102 species (within 54 genera). 46 species (30 genera) can be used as marker fossils and form the basis of a biozonation of the Aalenian-Oxfordian interval that comprises 9 zones and 7 subzones which have been correlated with the standard ammonite zonation. Similarities and differences between this work and zonations proposed in surrounding areas have been demonstrated. This highlights the pivotal role of the Jurassic of the Paris basin in understanding the influence of provincialism on the palynostratigraphy of Western Europe. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Nancy 1, UMR G2R 7566, F-54506 Vandoeuvre Nancy, France	Universite de Lorraine	Huault, V (通讯作者)，Univ Nancy 1, UMR G2R 7566, BP 239, F-54506 Vandoeuvre Nancy, France.							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Palaeobot. Palynology	NOV	1999	107	3-4					145	190		10.1016/S0034-6667(99)00021-4	http://dx.doi.org/10.1016/S0034-6667(99)00021-4			46	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	262PN					2025-03-11	WOS:000084075800002
J	Harland, R; FitzPatrick, MEJ; Pudsey, CJ				Harland, R; FitzPatrick, MEJ; Pudsey, CJ			Latest Quaternary dinoflagellate cyst climatostratigraphy for three cores from the Falkland Trough, Scotia and Weddell seas, Southern Ocean	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; late quaternary; climatostratigraphy; Antarctica; Southern Ocean; palaeoceanography	ANTARCTIC CIRCUMPOLAR CURRENT; NORTHEASTERN ATLANTIC-OCEAN; LAST-GLACIAL-MAXIMUM; PALYNOMORPH DISTRIBUTION; DIATOM DISTRIBUTION; SURFACE SEDIMENTS; MARINE-SEDIMENTS; AUSTRALIA; RECONSTRUCTION; STRATIGRAPHY	Dinoflagellate cyst analysis has been undertaken on three Kasten cares taken from the Falkland Trough, Scotia Sea and Weddell Sea in the area of the Antarctic Peninsula. Two of these cores ape situated to the north of the maximum sea-ice limit and one, from the Weddell Sea, is sited within the maximum sea-ice limit. The recovered dinoflagellate cyst assemblages underscore the importance of the maximum sea-ice limit as a basic biogeographic boundary for dinoflagellate cyst distributions. Our results also demonstrate that in general the palaeoceanography of the Holocene and Late Pleistocene has remained reasonably constant and reflects present conditions to a large extent. The relatively constant environments, as evidenced within these latest Quaternary sequences, is in marked contrast to the situation within the North Atlantic Ocean where, during the same time span, marked climatic and oceanographic change has been documented from marine, terrestrial and ice-core records. The stability of the Southern Ocean circulation undoubtedly has important consequences on the maintenance of the global thermohaline circulation system over the period since the last deglaciation until the present time. (C) 1999 Elsevier Science B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Ctr Palynol, Dept Earth Sci, Sheffield S3 7HF, S Yorkshire, England; Univ Plymouth, Dept Geol Sci, Plymouth PL4 8AA, Devon, England; British Antarctic Survey, Cambridge CB3 0ET, England	University of Sheffield; University of Plymouth; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.	rexharland@msn.com						[Anonymous], NASA SP; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Bint A.N., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P329; Blackford J.J., 1991, HOLOCENE, V1, P63, DOI DOI 10.1177/095968369100100108; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BURCKLE LH, 1984, MAR MICROPALEONTOL, V9, P241, DOI 10.1016/0377-8398(84)90015-X; CHARLES CD, 1990, NATO ADV SCI I C-MAT, V308, P519; Crosta X, 1998, PALEOCEANOGRAPHY, V13, P284, DOI 10.1029/98PA00339; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DANSGAARD W, 1989, NATURE, V339, P532, DOI 10.1038/339532a0; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DUPLESSY JC, 1993, PALEOCEANOGRAPHY, V8, P341, DOI 10.1029/93PA00455; Dymond J, 1992, PALEOCEANOGRAPHY, V7, P163, DOI 10.1029/92PA00181; EDWARDS LE, 1991, QUATERNARY SCI REV, V10, P259, DOI 10.1016/0277-3791(91)90024-O; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FOSTER TD, 1980, DEEP-SEA RES, V27, P367, DOI 10.1016/0198-0149(80)90032-1; Gilbert IM, 1998, SEDIMENT GEOL, V115, P185, DOI 10.1016/S0037-0738(97)00093-6; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; HARLAND R, 1989, J GEOL SOC LONDON, V146, P945, DOI 10.1144/gsjgs.146.6.0945; HARLAND R, 1994, PALAEONTOLOGY, V37, P263; HARLAND R, 1988, NEW PHYTOL, V108, P111, DOI 10.1111/j.1469-8137.1988.tb00210.x; Harland R, 1998, PALAEONTOLOGY, V41, P1093; HARLAND R, 1995, HOLOCENE, V5, P220, DOI 10.1177/095968369500500210; HARLAND R, 1988, PALAEONTOLOGY, V31, P877; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JORDAN RW, 1992, MAR MICROPALEONTOL, V19, P201, DOI 10.1016/0377-8398(92)90029-J; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; LOCARNINI RA, 1993, J MAR RES, V51, P135, DOI 10.1357/0022240933223846; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; MCMINN A, 1991, MICROPALEONTOLOGY, V37, P269, DOI 10.2307/1485890; McMinn A, 1995, MICROPALEONTOLOGY, V41, P383, DOI 10.2307/1485813; McMinn A, 1997, MAR MICROPALEONTOL, V29, P407, DOI 10.1016/S0377-8398(96)00012-6; MCMINN A, 1990, REV PALAEOBOT PALYNO, V65, P305, DOI 10.1016/0034-6667(90)90080-3; McMinn Andrew, 1992, Palynology, V16, P13; McMinn Andrew, 1994, Palynology, V18, P41; Moreton SG, 1998, ANN GLACIOL, V27, P285; MORLEY JJ, 1979, EARTH PLANET SC LETT, V44, P383, DOI 10.1016/0012-821X(79)90077-3; Nurnberg CC, 1997, PALEOCEANOGRAPHY, V12, P594, DOI 10.1029/97PA01130; OESCHGER H, 1984, AM GEOPHYS UNION MON, V29, P299; Olbers D.J., 1992, The hydrographic atlas of the Southern Ocean; ORSI AH, 1995, DEEP-SEA RES PT I, V42, P641, DOI 10.1016/0967-0637(95)00021-W; ORSI AH, 1993, DEEP-SEA RES PT I, V40, P169, DOI 10.1016/0967-0637(93)90060-G; Pudsey CJ, 1998, MAR GEOL, V148, P83, DOI 10.1016/S0025-3227(98)00014-0; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; ROCHON A, 1997, THESIS U QUEBEC MONT; SUN XK, 1994, MAR MICROPALEONTOL, V23, P345, DOI 10.1016/0377-8398(94)90023-X; TAYLOR KC, 1993, NATURE, V361, P432, DOI 10.1038/361432a0; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WESTALL F, 1991, P ODP SCI RESULTS, V114, P609; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zielinski U, 1997, PALAEOGEOGR PALAEOCL, V129, P213, DOI 10.1016/S0031-0182(96)00130-7	57	15	15	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	NOV	1999	107	3-4					265	281		10.1016/S0034-6667(99)00023-8	http://dx.doi.org/10.1016/S0034-6667(99)00023-8			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	262PN					2025-03-11	WOS:000084075800008
J	Perovic, S; Wetzler, C; Brümmer, F; Elbrächter, M; Tretter, L; Wichels, A; Müller, WEG; Schröder, HC				Perovic, S; Wetzler, C; Brümmer, F; Elbrächter, M; Tretter, L; Wichels, A; Müller, WEG; Schröder, HC			Changes of ICE protease activities caused by toxic supernatants of dinoflagellates (<i>Prorocentrum</i> species) from marine algal blooms	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						marine toxins; algal blooms; caspases; ICE; CPP32; Mch2; cell viability; dinoflagellate; Prorocentrum	OKADAIC ACID; CELL-DEATH; POLY(ADP-RIBOSE) POLYMERASE; GYMNODINIUM-CATENATUM; CYSTEINE PROTEASE; FAMILY PROTEASE; SHELLFISH; APOPTOSIS; ACTIVATION; CLEAVAGE	Marine phytotoxins may become a major health problem for humans because of their ability to contaminate seafood and to cause shellfish poisoning. In this report, the cytotoxic effects and the effects on intracellular caspase activities of culture supernatants from different dinoflagellate Prorocentrum clones were determined. Among the clones tested, I? tepsium BAH ME-140 and P. lima BAH ME-130 K1 and K2 clones but not P. minimum and I! micans were found to be toxic on rat pheochromocytoma PC12 cells, mouse lymphoma L5178Y cells and rat primary neurons. A significant increase in the specific activities of caspase 1 (ICE), caspase 3 (CPP32) and caspase 6 (Mch2) to 149-167% was observed after treatment of neurons with P. lima BAH ME-130 K2 supernatant for 72 h; in PC12 cells, the increase in these enzyme activities was much smaller. An even stronger and faster effect on caspase activities, compared to the K2 clone, was observed following treatment of PC12 cells and neuronal cells with P. lima BAH ME-130 K1 supernatant. The maximal increase in caspase activities in PC12 cells (CPP32, 364%; and Mch2, 166%) and in neurons (CPP32, 162%; and Mch2, 111%)was observed after 24 h; no significant change of ICE activity was found during that incubation period. After 48 h the specific activities of all caspases strongly decreased. Incubation of PC12 cells with I! tepsium BAH ME-140 for 24 h had almost no effect on caspase activities, while a small increase in CPP32- (148%) and Mch2- (115%) but not in ICE-activity was detected after 48 h. In neurons, only an increase in CPP32 activity (to 130%) was observed with this dinoflagellate supernatant after 24 h. The P. lima protein phosphatase inhibitor okadaic acid (0.5 ng/ml) caused a time-dependent increase in caspase activities in PC12 cells. A much higher effect was observed in neuronal cells; after 72 h, the specific activities of ICE, CPP32 and Mch2 increased to 295%, 146% and 235%, respectively. These results indicate that disturbances of caspase activities may contribute to the neurotoxic effects of certain dinoflagellate supernatants.	Johannes Gutenberg Univ Mainz, Angew Mikrobiol Abt, Inst Physiol Chem, D-55099 Mainz, Germany; Univ Stuttgart, Abt Zool, Inst Biol, D-70569 Stuttgart, Germany; Wattenmeerstn Sylt AWI, Forschungsinst Senckenberg, D-25992 List Auf Sylt, Germany; Semmelweis Univ, H-1444 Budapest, Hungary; Biol Anstalt Helgoland, Abt Meeresmikrobiol, D-27483 Helgoland, Germany	Johannes Gutenberg University of Mainz; University of Stuttgart; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Semmelweis University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Johannes Gutenberg Univ Mainz, Angew Mikrobiol Abt, Inst Physiol Chem, Duesbergweg 6, D-55099 Mainz, Germany.	hschroed@mail.uni-mainz.de	Müller, W./AAR-8651-2020; Tretter, Laszlo/ACI-2689-2022; Wichels, Antje/R-6992-2016	Wichels, Antje/0000-0002-2060-1845; Tretter, Laszlo/0000-0001-5638-2886				Anderson DM, 1996, TOXICON, V34, P579, DOI 10.1016/0041-0101(95)00158-1; ANDERSON DM, 1989, TOXICON, V27, P665, DOI 10.1016/0041-0101(89)90017-2; [Anonymous], [No title captured]; Armstrong RC, 1996, J BIOL CHEM, V271, P16850, DOI 10.1074/jbc.271.28.16850; ARTECHE E, 1995, PLANTA MED, V61, P13, DOI 10.1055/s-2006-957989; Arzul G, 1996, AQUAT LIVING RESOUR, V9, P95, DOI 10.1051/alr:1996012; Aune T, 1997, Arch Toxicol Suppl, V19, P389; BOLAND MP, 1993, FEBS LETT, V334, P13, DOI 10.1016/0014-5793(93)81670-U; Bouaicha N, 1997, TOXICON, V35, P273, DOI 10.1016/S0041-0101(96)00069-4; Burkholder JM, 1998, ECOL APPL, V8, pS37; CANDENAS ML, 1994, N-S ARCH PHARMACOL, V350, P315; Carmody EP, 1996, TOXICON, V34, P351, DOI 10.1016/0041-0101(95)00141-7; Dawson JF, 1996, BIOCHEM CELL BIOL, V74, P559, DOI 10.1139/o96-460; DING RC, 1994, CANCER RES, V54, P4627; Enari M, 1996, NATURE, V380, P723, DOI 10.1038/380723a0; Fessard V., 1994, Natural Toxins, V2, P322, DOI 10.1002/nt.2620020512; Gago-Martinez Ana, 1996, Natural Toxins, V4, P72, DOI 10.1002/19960402NT3; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Hodgkiss IJ, 1997, HYDROBIOLOGIA, V352, P141, DOI 10.1023/A:1003046516964; HU TM, 1995, J CHEM SOC CHEM COMM, P597, DOI 10.1039/c39950000597; HUMMERT C, 1995, HARMFUL MARINE ALGAL; Janicke RU, 1996, EMBO J, V15, P6969, DOI 10.1002/j.1460-2075.1996.tb01089.x; JURANOVIC LR, 1991, REV ENVIRON CONTAM T, V117, P51; KARUNASAGAR I, 1990, TOXICON, V28, P868, DOI 10.1016/S0041-0101(09)80010-X; LAZEBNIK YA, 1994, NATURE, V371, P346, DOI 10.1038/371346a0; Liu XS, 1996, J BIOL CHEM, V271, P13371, DOI 10.1074/jbc.271.23.13371; LOWRY OH, 1951, J BIOL CHEM, V193, P265; LUCKAS B, 1994, ANAL CONTAMINANTS ED, P509; Martin SJ, 1996, J BIOL CHEM, V271, P28753, DOI 10.1074/jbc.271.46.28753; McLachlan J. 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J. Protistol.	OCT 15	1999	35	3					267	274		10.1016/S0932-4739(99)80004-2	http://dx.doi.org/10.1016/S0932-4739(99)80004-2			8	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	259DX					2025-03-11	WOS:000083880200004
J	D'Onofrio, G; Marino, D; Bianco, L; Busico, E; Montresor, M				D'Onofrio, G; Marino, D; Bianco, L; Busico, E; Montresor, M			Toward an assessment on the taxonomy of dinoflagellates that produce calcareous cysts (Calciodinelloideae, Dinophyceae): A morphological and molecular approach	JOURNAL OF PHYCOLOGY			English	Article						calcareous cysts; Calciodinelloideae; Dinophyceae; Ensiculifera; ITS; Pentapharsodinium; phylogeny; rDNA; Scrippsiella; taxonomy	RIBOSOMAL DNA; EVOLUTIONARY IMPLICATIONS; MARINE DINOFLAGELLATE; NOV DINOPHYCEAE; NUCLEAR RDNA; RESTING CYST; COMB-NOV; SEQUENCES; SCRIPPSIELLA; SEDIMENTS	In recent years an unified classification system for both fossil cysts and extant dinoflagellate species has been proposed. This classification has prompted investigations aimed at testing the phylogenetic validity of the distinctive morphological characters of both vegetative cells and cysts. We have focused on a group of dinoflagellates that produce calcareous resting cysts, which are abundant in marine neritic and oceanic waters and form wide fossil deposits. Extant species are included in the genera Scrippsiella, Ensiculifera, and "Pentapharsodinium'' (subfamily Calciodinelloideae), which are distinguished by the number and/or shape of the cingular plates of their planktonic vegetative stages. On the other hand, the classification of fossil cysts is based on the morphology of the calcareous covering and on the orientation of crystals. In this study we combine the information derived from morphological traits of both motile stages and cysts with that obtained from nucleotide sequence analysis of the ribosomal DNA internal transcribed spacers (ITS), We also describe the vegetative cell produced by the calcareous cyst Calcigonellum infula and a new variety, Scrippsiella trochoidea var. aciculifera var. nov. Molecular analyses confirm the monophyletic origin of the genus Scrippsiella, whereas the "Pentapharsodinium'' and Ensiculifera species are grouped together in another monophyletic cluster. The coupled morphological and molecular approach supports the taxonomic value of some of the characters of the planktonic stage, such as the cingular plate number. On the other hand, it questions the validity of other morphological characters of both vegetative and encysted stages. Our data provide a phylogenetic classification of these dinoflagellates; however, they also open a debate that would imply a redefinition of the characters to be used for the circumscription of the subfamily Calciodinelloideae.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@alpha.szn.it		Montresor, Marina/0000-0002-2475-1787				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; AKSELMAN R, 1990, MAR MICROPALEONTOL, V16, P169, DOI 10.1016/0377-8398(90)90002-4; [Anonymous], MEDD KOMM HAVUNDER P; [Anonymous], 1883, ORGANISMUS INFUSIONS; BALDWIN BG, 1995, ANN MO BOT GARD, V82, P247, DOI 10.2307/2399880; 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., 1966, NEOTROPICA, V12, P103; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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III, 1965, TAXON, V14, P15, DOI 10.2307/1216704; MAROTEAUX L, 1985, BIOSYSTEMS, V18, P307, DOI 10.1016/0303-2647(85)90031-0; MATSUOKA K, 1990, Bulletin of Plankton Society of Japan, V37, P127; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; 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, 1993, J PHYCOL, V29, P223, DOI 10.1111/j.0022-3646.1993.00223.x; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; MORRILL L C, 1981, Journal of Plankton Research, V3, P53, DOI 10.1093/plankt/3.1.53; NEHRING S, 1995, HELGOLANDER MEERESUN, V49, P375, DOI 10.1007/BF02368363; PIERCE RW, 1994, MAR ECOL PROG SER, V112, P225, DOI 10.3354/meps112225; Pillmann A, 1997, EUR J PHYCOL, V32, P379, DOI 10.1017/S0967026297001352; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; SAUNDER SGW, 1997, ORIGINS ALGAE THEIR, P237; SCHLOTTERER C, 1994, MOL BIOL EVOL, V11, P513; SCHOLIN CA, 1993, J PHYCOL, V29, P209, DOI 10.1111/j.0022-3646.1993.00209.x; Spalter RA, 1997, BIOCHEM SYST ECOL, V25, P231, DOI 10.1016/S0305-1978(96)00111-1; Steidinger Karen A., 1997, P387, DOI 10.1016/B978-012693018-4/50005-7; SUH YB, 1993, AM J BOT, V80, P1042, DOI 10.2307/2445752; SUSANNA A, 1995, AM J BOT, V82, P1056, DOI 10.2307/2446236; Swofford D. L., 1998, MAC VERSION 311 COMP; Throndsen J., 1978, Preservation and storage, P69, DOI DOI 10.1111/J.0022-3646.1975.00142.X; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2; WALL D, 1968, Journal of Paleontology, V42, P1395; White TJ., 1990, PCR PROTOCOLS GUIDE, P315; ZECHMAN FW, 1994, J PHYCOL, V30, P507, DOI 10.1111/j.0022-3646.1994.00507.x; [No title captured]	75	64	68	1	6	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	OCT	1999	35	5					1063	1078		10.1046/j.1529-8817.1999.3551063.x	http://dx.doi.org/10.1046/j.1529-8817.1999.3551063.x			16	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	254QG					2025-03-11	WOS:000083623200020
J	Nuzzo, L; Montresor, M				Nuzzo, L; Montresor, M			Different excystment patterns in two calcareous cyst-producing species of the dinoflagellate genus <i>Scrippsiella</i>	JOURNAL OF PLANKTON RESEARCH			English	Article							DINOPHYCEAE RESTING CYSTS; POPULATION-DYNAMICS; BENTHIC CYSTS; GERMINATION; DARKNESS	Scrippsiella rotunda and Scrippsiella trochoidea var. aciculifera (order Peridiniales, subfamily Calciodinelloideae) are autotrophic orthoperidinioid dinoflagellates producing calcareous resting cysts, which are at times abundant in coastal marine sediments. We have carried out laboratory experiments to investigate features of cyst germination in the two species, including dormancy length, germination pattern and germination success, over an annual cycle and under different light and temperature conditions. The maturation period for S.rotunda cysts was between 17 and 24 weeks, while that of S.trochoidea var, aciculifera was much shorter, ranging between 2 and 5 weeks. Both species required exposure to light for germination, while temperature shifts (from 14 to 20 degrees C) in the dark did not induce excystment of mature cysts. In both species, germination was not synchronous, but distributed over a variable time interval, suggesting a high physiological diversity within the cyst pool. Moreover, exposure to light of S.rotunda cysts that had not completed maturation impaired the germination of a great percentage of the cysts. Differences in dormancy length may partially explain the distinct cyst production patterns observed for the two species in the Gulf of Naples.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Nuzzo, L (通讯作者)，Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.			Montresor, Marina/0000-0002-2475-1787				ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BINDER BJ, 1986, NATURE, V322, P659, DOI 10.1038/322659a0; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; DONOFRIO G, 1999, IN PRESS J PHYCOL, V35; Head M.J., 1996, Palynology: Principles and Applications, P1197; Huber G., 1923, FLORA JENA, V116, P114; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; KELLER MD, 1987, J PHYCOL, V23, P633; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; Marcus NH, 1996, HYDROBIOLOGIA, V320, P141, DOI 10.1007/BF00016815; MCQUOID MR, 1995, J PHYCOL, V31, P44, DOI 10.1111/j.0022-3646.1995.00044.x; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; PFEISTER LA, 1987, BIOL DINOFLAGELLATES, P611; 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; Sandgren C.D., 1983, P23; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	24	36	38	3	6	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	OCT	1999	21	10					2009	2018		10.1093/plankt/21.10.2009	http://dx.doi.org/10.1093/plankt/21.10.2009			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	247RX		Bronze			2025-03-11	WOS:000083234700013
J	Feist-Burkhardt, S; Pross, J				Feist-Burkhardt, S; Pross, J			Morphological analysis and description of Middle Jurassic dinoflagellate cyst marker species using confocal laser scanning microscopy, digital optical microscopy, and conventional light microscopy	BULLETIN DU CENTRE DE RECHERCHES ELF EXPLORATION PRODUCTION			English	Article						confocal laser scanning microscopy; digital optical microscopy; dinoflagellata; Middle Jurassic; new taxa; Calvados; France; Hildesheim; Niedersachsen		Two relatively new microscopy techniques, confocal laser scanning microscopy (CLSM) and digital optical microscopy (DOM), which allow three-dimensional reconstructions and stereoscopic visualisations of embedded specimens, are for the first time applied to the morphological analysis of fossil dinoflagellate cysts. Four Middle Jurassic dinoflagellate cyst species, each representing a different basic type of morphology, were selected for a comparative morphological study in CLSM, DOM and conventional light microscopy. Results are compared and advantages of each method in the application to dinoflagellate cyst palynology are discussed. Two stratigraphically important species, Protobatioladinium mercieri sp. nov. and Wanaea cornucavata sp. nov, from the Middle Jurassic of Normandy, France, are described using information obtained by the application of the three different microscopy techniques.	Tech Univ Darmstadt, Inst Geol & Palaeontol, D-64287 Darmstadt, Germany; Univ Tubingen, Inst & Museum Geol & Palaeontol, D-72076 Tubingen, Germany	Technical University of Darmstadt; Eberhard Karls University of Tubingen	Feist-Burkhardt, S (通讯作者)，Tech Univ Darmstadt, Inst Geol & Palaeontol, Schnittspahnstr 9, D-64287 Darmstadt, Germany.		Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242				BELOW R, 1990, Palaeontographica Abteilung B Palaeophytologie, V220, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Birkmann H, 1996, J PALEONTOL, V70, P1084, DOI 10.1017/S0022336000038774; DODEKOVA L, 1990, Geologica Balcanica, V20, P3; DODEKOVA L, 1975, BULG ACAD SCI PALAEO, V2, P17; Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Feist-Burkhardt Susanne, 1995, Palynology, V19, P167; FEISTBURKHARDT S, 1998, BULL CENT RECH ELF E, V21, P31; Fensome R.A., 1981, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V161, P47; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; FOSTER B, 1990, Palynology, V14, P212; Gocht H., 1970, PALAEONTOGRAPHICA B, V129, P125; MERCIER J, 1938, C R SOMM SOC GEOL FR, V7, P114; Monteil E., 1992, Revue de Paleobiologie, V11, P273; NOHR-HANSEN H, 1986, Bulletin of the Geological Society of Denmark, V35, P31; OConnor B, 1996, MICROPALEONTOLOGY, V42, P395, DOI 10.2307/1485963; PROSS J, 1997, TUB MIKROPALAONTOL M, V15; RIDING JB, 1985, REV PALAEOBOT PALYNO, V45, P149, DOI 10.1016/0034-6667(85)90068-5; SCOTT AC, 1991, REV PALAEOBOT PALYNO, V67, P133, DOI 10.1016/0034-6667(91)90019-Y; STANCLIFFE RPW, 1990, MICROPALEONTOLOGY, V36, P197, DOI 10.2307/1485506; Webb Robert H., 1995, P571; Woolham R., 1982, Journal of Micropalaeontology, V1, P45	23	25	28	0	0	ELF EXPLORATION PRODUCTS	PAU CEDEX	ELF EXPLORATION EDITIONS, CSTJF-AVENUE LARRIBAU, 64018 PAU CEDEX, FRANCE	1279-8215			BULL CENT RECH ELF E	Bull. Cent. Rech. Elf Explor. Prod.	SEP 30	1999	22	1					103	145						43	Energy & Fuels; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Energy & Fuels; Geology	261PG					2025-03-11	WOS:000084017100006
J	Vardi, A; Berman-Frank, I; Rozenberg, T; Hadas, O; Kaplan, A; Levine, A				Vardi, A; Berman-Frank, I; Rozenberg, T; Hadas, O; Kaplan, A; Levine, A			Programmed cell death of the dinoflagellate <i>Peridinium gatunense</i> is mediated by CO<sub>2</sub> limitation and oxidative stress	CURRENT BIOLOGY			English	Article							MARINE-PHYTOPLANKTON; LAKE KINNERET; APOPTOSIS	The phytoplankton assemblage in Lake Kinneret is dominated in spring by a bloom of the dinoflagellate Peridinium gatunense, which terminates sharply in summer [1]. The pH in Peridinium patches rises during the bloom to values higher than pH9 [2] and results in CO2 limitation. Here we show that depletion of dissolved CO2 (CO2(dis)) stimulated formation of reactive oxygen species (ROS) and induced cell death in both natural and cultured Peridinium populations. In contrast, addition of CO2 prevented ROS formation. Catalase inhibited cell death in culture, implicating hydrogen peroxide (H2O2) as the active ROS. Cell death was also blocked by a cysteine protease inhibitor, E-64, a treatment which stimulated cyst formation. Intracellular ROS accumulation induced protoplast shrinkage and DNA fragmentation prior to cell death. We propose that CO2 limitation resulted in the generation of ROS to a level that induced programmed cell death, which resembles apoptosis in animal and plant cells. Our results also indicate that cysteine protease(s) are involved in processes that determine whether a cell is destined to die or to form a cyst.	Hebrew Univ Jerusalem, Dept Plant Sci, IL-91904 Jerusalem, Israel; Israel Oceanog & Limnol Res, Yigal Allon Kinneret Limnol Lab, IL-14102 Tiberias, Israel; Hebrew Univ Jerusalem, Avron Evenari Minerva Ctr, IL-91904 Jerusalem, Israel	Hebrew University of Jerusalem; Israel Oceanographic & Limnological Research Institute; Hebrew University of Jerusalem	Levine, A (通讯作者)，Hebrew Univ Jerusalem, Dept Plant Sci, IL-91904 Jerusalem, Israel.		Kaplan, Aaron/GLN-5655-2022; Levine, Alex/A-6867-2008	Kaplan, Aaron/0000-0002-0815-5731; Berman-Frank, Ilana/0000-0003-3497-1844; Vardi, Assaf/0000-0002-7079-0234				AMEISEN JC, 1995, CELL DEATH DIFFER, V2, P285; Berges JA, 1998, LIMNOL OCEANOGR, V43, P129, DOI 10.4319/lo.1998.43.1.0129; BermanFrank I, 1995, J PHYCOL, V31, P906, DOI 10.1111/j.0022-3646.1995.00906.x; Butow BJ, 1997, J PHYCOL, V33, P780, DOI 10.1111/j.0022-3646.1997.00780.x; Collen J, 1997, J PHYCOL, V33, P643, DOI 10.1111/j.0022-3646.1997.00643.x; EMILIANI C, 1996, NATURE, V366, P217; KORSMEYER SJ, 1995, BBA-MOL BASIS DIS, V1271, P63, DOI 10.1016/0925-4439(95)00011-R; Levine A, 1996, CURR BIOL, V6, P427, DOI 10.1016/S0960-9822(02)00510-9; Madeo F, 1999, J CELL BIOL, V145, P757, DOI 10.1083/jcb.145.4.757; Mills JC, 1998, J CELL BIOL, V140, P627, DOI 10.1083/jcb.140.3.627; POLLINGHER U, 1986, HYDROBIOLOGIA, V138, P127, DOI 10.1007/BF00027236; REDFIELD AC, 1958, AM SCI, V46, P205; ROYALL JA, 1993, ARCH BIOCHEM BIOPHYS, V302, P348, DOI 10.1006/abbi.1993.1222; SERRUYA C, 1978, MONOGRAPHICA BIOL, P185; Solomon M, 1999, PLANT CELL, V11, P431, DOI 10.1105/tpc.11.3.431; Sterner R.W., 1989, P107; Thornberry NA, 1998, SCIENCE, V281, P1312, DOI 10.1126/science.281.5381.1312; Veldhuis MJW, 1997, J PHYCOL, V33, P527, DOI 10.1111/j.0022-3646.1997.00527.x; VERNET G, 1990, BIOCHIM BIOPHYS ACTA, V1048, P281, DOI 10.1016/0167-4781(90)90068-D	19	250	296	1	62	CURRENT BIOLOGY LTD	LONDON	84 THEOBALDS RD, LONDON WC1X 8RR, ENGLAND	0960-9822			CURR BIOL	Curr. Biol.	SEP 23	1999	9	18					1061	1064		10.1016/S0960-9822(99)80459-X	http://dx.doi.org/10.1016/S0960-9822(99)80459-X			4	Biochemistry & Molecular Biology; Biology; Cell Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Life Sciences & Biomedicine - Other Topics; Cell Biology	239AD	10508616	Bronze			2025-03-11	WOS:000082745900028
J	Batten, DJ; Gray, J; Harland, R				Batten, DJ; Gray, J; Harland, R			Palaeoenvironmental significance of a monospecific assemblage of dinoflagellate cysts from the Miocene Clarkia Beds, Idaho, USA	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						fauna; flora; dinoflagellate cysts; nonmarine; palaeoenvironment; Clarkia Beds; Miocene; Idaho; USA		A single dinoflagellate cyst species occurs abundantly in nonglacial varved lacustrine deposits of the Miocene Clarkia Lake succession in northern Idaho. Previously of uncertain affinity, it is now identified as Pseudokomewuia (Pseudokomewuia) aff. granulata He 1980. The variety of other biological groups that are represented by fossils in the succession provides a basis for making observations on ecological associations and climatic conditions during the period of deposition of the sediments. The cysts do not occur in the alluvial (floodplain) and poorly laminated, early lacustrine facies that underlie the varved unit, nor in the overlying late lacustrine, oxidised, silty clay facies. They are associated only with sediment-couplets considered to reflect accumulation in temperature-stratified water approximately 8-12 m deep that overturned periodically. It is likely that the dinoflagellates inhabited the warm, epilimnic, oxygenated layer above the cool deep water in which oxygen levels were low rendering this environment inhospitable to both animals and plants, but favouring the preservation of organic matter. Their absence from the unlaminated deposits of the early and late lacustrine facies may not mean that the motile dinoflagellates were not present in the shallower waters they represent but simply that the cysts were not preserved. These beds accumulated in oxidising environments and are palynologically barren. The land plant mega- and microfossil records suggest that the vegetation of the surrounding hills consisted of mixed deciduous-coniferous forest of a character that is typical of a moist (summer-wet) warm-temperate climate. This is also implied by some of the fauna (e.g., the salmonid fish and the gastropod Bellamya). These observations add significantly to palaeoecological conclusions drawn from the few records of nonmarine dinoflagellate cysts from Cretaceous and younger successions elsewhere, most of which have been associated with quiet lacustrine or lagoonal habitats. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Wales, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales; Univ Oregon, Dept Biol, Eugene, OR 97403 USA; Univ Sheffield, Dept Earth Sci, Ctr Palynol, Sheffield S3 3HF, S Yorkshire, England; DinoData Serv, Nottingham NG13 8AH, England	Aberystwyth University; University of Oregon; University of Sheffield	Batten, DJ (通讯作者)，Univ Wales, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales.							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Paleoclimatol. Paleoecol.	SEP 15	1999	153	1-4					161	177		10.1016/S0031-0182(99)00103-0	http://dx.doi.org/10.1016/S0031-0182(99)00103-0			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	236KE					2025-03-11	WOS:000082598100010
J	Grosfjeld, K; Larsen, E; Sejrup, HP; De Vernal, A; Flatebo, T; Vestbo, M; Haflidason, H; Aarseth, I				Grosfjeld, K; Larsen, E; Sejrup, HP; De Vernal, A; Flatebo, T; Vestbo, M; Haflidason, H; Aarseth, I			Dinoflagellate cysts reflecting surface-water conditions in Voldafjorden, western Norway during the last 11 300 years	BOREAS			English	Article							LATITUDE MARINE ENVIRONMENTS; SKAGERRAK-KATTEGAT; NORTH-ATLANTIC; PALYNOLOGICAL EVIDENCE; NORWEGIAN SEA; DEGLACIATION; PALEOENVIRONMENTS; SEDIMENTS; AGE; CORES	Abundant dinocysts in a high-resolution core from Voldafjorden, western Norway, reflect changes in sea surface-water conditions during the last c. 11300 BP. The period from c. 11300 to 10800 BP (Late Allerod) was characterized by cool temperate surface-waters, high annual temperature variation and relatively strong stratification of the water column, which is characteristic of fjord environments. Due to the stratification of the surface waters, the uppermost layer may have warmed considerably. This generated a principal difference in temperature conditions between land and sea, with slightly higher temperatures in the marine environments. The period from c. 10800 to 10000 BP is characterized by very harsh conditions, with sea surface-water temperatures close to freezing and long lasting seasonal sea-ice cover. Similar temperature changes at the beginning and end of the Younger Dryas are characteristic for NW Europe, but those in Voldafjorden differ from those in the open sea and in the Norwegian Channel by being significantly larger. The stratification of the water column during the Late Allerod was probably broken down because of incipient inflow of temperate normal saline waters, which caused a marked sea surface-water warming, at c. 10000 BP. Surface-water conditions close to those of today were gradually established between c. 10000 and 9500 BP. However, these interglacial conditions were abruptly interrupted by a significant drop in winter sea surface-water temperature and salinity occurring around 9700 BP. From c. 9500 to 7000 BP the influence of temperate normal saline water masses increased stepwise until full interglacial conditions were established around c. 7000 BP. The change in the dinocyst assemblage around 7000 BP in Voldafjorden was probably related to the onset of the modern Norwegian Coastal Current, previously documented in cores from the Skagerrak and the Mid-Norwegian Continental Shelf. The last c. 7000 BP is characterized by relatively stable surface-water conditions, pos possibly interrupted by periods of cooling or decreased inflow of temperate normal saline water. Like several other dinoflagellate cyst records from the Norwegian-Greenland Sea, O. centrocarpum peak values are between 4000 and 5000 BP, suggesting a regional scale oceanographic change.	Geol Survey Norway, N-7002 Trondheim, Norway; Univ Bergen, N-5007 Bergen, Norway; Univ Quebec, Geotop, UQUAM, Montreal, PQ H3C 3P8, Canada	Geological Survey of Norway; University of Bergen; University of Quebec; University of Quebec Montreal	Grosfjeld, K (通讯作者)，Geol Survey Norway, POB 3006, N-7002 Trondheim, Norway.		de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				Aarseth I, 1997, MAR GEOL, V143, P39, DOI 10.1016/S0025-3227(97)00089-3; ABIDI N, 1998, 6 INT C MOD FOSS DIN, P12; [Anonymous], NOR GEOGR TIDSSKR; BAUMANN KH, 1992, MAR MICROPALEONTOL, V20, P129, DOI 10.1016/0377-8398(92)90003-3; Birks HH, 1996, QUATERNARY RES, V45, P119, DOI 10.1006/qres.1996.0014; BIRKS HH, 1999, IN PRESS J PALEOLIMN; Bjorck S, 1996, SCIENCE, V274, P1155, DOI 10.1126/science.274.5290.1155; Bondevik S, 1997, BOREAS, V26, P29, DOI 10.1111/j.1502-3885.1997.tb00649.x; BROOKS SJ, 1999, IN PRESS J PALEOLIMN; Brooks Stephen J., 1997, Quaternary Proceedings, V5, P49; CONRADSEN K, 1995, PALEOCEANOGRAPHY, V10, P801, DOI 10.1029/95PA01142; Dahl S.O., 1994, The Holocene, V4, P269; Dahl SO, 1996, HOLOCENE, V6, P381, DOI 10.1177/095968369600600401; DALE B, 1977, BRIT PHYCOL J, V12, P241, DOI 10.1080/00071617700650261; Dale B., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; DALE B, 1996, AM ASS STRATIGRAPHIC, V3, P1149; DALE B, 1994, NATO ASI SER, V1, P521; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; DUIGAN CA, 1999, IN PRESS J PALEOLIMN; FARETH OW, 1987, NORGES GEOLOGISKE UN, V408; FLATEBO T, 1998, THESIS U BERGEN; GUIOT J, 1990, I NATL SCI U MONOGRA, V1; Gulliksen S, 1998, HOLOCENE, V8, P249, DOI 10.1191/095968398672301347; HAFLIDASON H, 1995, GEOLOGY, V23, P1059, DOI 10.1130/0091-7613(1995)023<1059:CROTLG>2.3.CO;2; Hald M, 1998, GEOLOGY, V26, P615, DOI 10.1130/0091-7613(1998)026<0615:EPCITN>2.3.CO;2; Jiang H, 1997, HOLOCENE, V7, P301; Jonsgard Birgitte, 1995, Lindbergia, V20, P64; KARPUZ N, 1993, QUATERNARY SCI REV, V12, P115; Karpuz NK, 1992, PALEOCEANOGRAPHY, V7, P499, DOI 10.1029/92PA01651; KLITGAARD D, 1994, MARINE GEOLOGICAL CR, P102; Knudsen KL, 1996, BOREAS, V25, P65; LARSEN E, 1991, J QUATERNARY SCI, V6, P263, DOI 10.1002/jqs.3390060402; LARSEN E, 1984, ARCTIC ALPINE RES, V16, P137, DOI 10.2307/1551067; Larsen E, 1998, J QUATERNARY SCI, V13, P17, DOI 10.1002/(SICI)1099-1417(199801/02)13:1<17::AID-JQS337>3.3.CO;2-2; LEHMAN SJ, 1992, NATURE, V356, P757, DOI 10.1038/356757a0; LEMDAHL G, 1999, IN PRESS J PALEOCLIM, V18; LENTIN JK, 1993, AM ASS STRATIGRAPHIC, V20; MANGERUD J, 1979, BOREAS, V8, P179, DOI 10.1111/j.1502-3885.1979.tb00798.x; MANGERUD J, 1974, Boreas (Oslo), V3, P109; MANGERUD J, 1984, QUATERNARY RES, V21, P85, DOI 10.1016/0033-5894(84)90092-9; MANGERUD J, 1975, QUATERNARY RES, V5, P263, DOI 10.1016/0033-5894(75)90028-9; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; Matthiessen Jens, 1997, Grzybowski Foundation Special Publication, V5, P149; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Mudie P. 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J	Kremp, A; Heiskanen, AS				Kremp, A; Heiskanen, AS			Sexuality and cyst formation of the spring-bloom dinoflagellate <i>Scrippsiella hangoei</i> in the coastal northern Baltic Sea	MARINE BIOLOGY			English	Article							RED TIDE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; PERIDINIUM-CINCTUM; LIFE-CYCLE; DINOPHYCEAE; ENCYSTMENT; SEDIMENTATION; PHYTOPLANKTON; REPRODUCTION	The temporal sequence and the magnitude of the sexual reproduction and subsequent cyst deposition of the common spring-bloom dinoflagellate Scrippsiella hangoei (Schiller) Larsen was studied during spring 1996 on the SW coast of Finland, Baltic Sea. The abundances of the different size of fractions of S. hangoei (14 to 18 mu m, 18 to 22 mu m and >22 mu m) were monitored in the water column, and the deposition of resting cysts was measured using moored sediment traps. Cyst sedimentation rates were measured throughout the seasonal cycle in order to estimate cyst resuspension rates for the quantitative assessment of the fraction of population undergoing encystment. The onset of sexual reproduction, indicated by a significant increase of the small cells (14 to 18 mu m) representing gametes, occurred in a nutrient replete environment well before the exponential growth phase and peak abundances of vegetative cells. Gamete formation was followed by high abundances of large cells (>22 mu m) representing planozygotes, and subsequent sedimentation of resting cysts. Approximately 60% of the asexually growing bloom population was estimated to form planozygotes, suggesting that encystment was an important factor in bloom termination and possibly plays a role in the regulation of the magnitude of the bloom. Finally encystment accounted for 40% of the entire S. hangoei population, resulting in a considerable loss of the bloom population and an input of the vernal phytoplankton biomass to the benthos.	Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, FIN-00014 Helsinki, Finland; Tvarminne Zool Stn, FIN-10900 Henko, Finland; Finnish Environm Inst, FIN-00251 Helsinki, Finland	University of Helsinki; Finnish Environment Institute	Kremp, A (通讯作者)，Univ Helsinki, Dept Systemat & Ecol, Div Hydrobiol, POB 17, FIN-00014 Helsinki, Finland.		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Biol.	SEP	1999	134	4					771	777		10.1007/s002270050594	http://dx.doi.org/10.1007/s002270050594			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	237BG					2025-03-11	WOS:000082633300020
J	Louwye, S				Louwye, S			New species of organic-walled dinoflagellates and acritarchs from the Upper Miocene Diest Formation, northern Belgium (southern North Sea Basin)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; Upper Miocene; North Sea Basin; Belgium; stratigraphy	GENERA	A palynological investigation of the shallow marine Diest Formation (Upper Miocene) in northern Belgium has revealed the presence of five previously undescribed dinoflagellate cyst species and one acritarch. A formal description and a preliminary assessment of the stratigraphical ranges of following species is given: Bitectatodinium?? arborichiarum Louwye, sp. nov., Operculodinium antwerpensis Louwye, sp. nov., Batiacasphaera deheinzelinii Louwye, sp. nov., Cerebrocysta lagae Louwye, sp. nov., Barssidinium taxandrianum Louwye, sp. nov. and Palaeostomocystis globosa Louwye, sp. nov. (C) 1999 Elsevier Science B.V. All rights reserved.	State Univ Ghent, Lab Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，State Univ Ghent, Lab Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				[Anonymous], 1979, CAINOZOIC GLOBIGERIN; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Bujak JP., 1980, PALAEONTOLOGICAL ASS, V24, P36; BUTSCHLI O, 1885, HG BRONNS KLASSEN OR, V1, P865; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Meuter F. J. C, 1970, Bull. Soc. belge Geol. Paleont. Hydrol., V79, P175; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; DRUGG WS, 1970, P N AM PAL CONV, V2, P809; Fensome R.A., 1993, CLASSIFICATION FOSSI; GLIBERT M, 1962, SOC BELGE GEOL MEM, V6, P40; GLIBERT M, 1955, B I ROYAL SCI NATURE, V31, P1; HAECKEL E, 1894, ENTWURF EINES NATURL; 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.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P453, DOI 10.2973/odp.proc.sr.105.136.1989; Head M. J., 1994, Palynology, V17, P201, DOI [10.1080/01916122.1993.9989428, DOI 10.1080/01916122.1993.9989428]; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; HINSCH W., 1988, GEOLOGISCHES JB A, VA100, P344; HOOYBERGHS H J F, 1972, Mededelingen van de Koninklijke Academie voor Wetenschappen Letteren en Schone Kunsten van Belgie Klasse der Wetenschappen, V34, P1; HOOYBERGHS H. J. F., 1988, GEOLOGISCHES JB A, VA100, P190; *IGCP 124 WORK GRO, 1988, GEOL JB A, V100, P145; LAGA P G H, 1972, Bulletin de la Societe Belge de Geologie de Paleontologie et d'Hydrologie, V81, P211; Lagaaij R., 1952, MEDEDELINGEN GEOLOGI, V5, P1; LENTIN JK, 1994, CAN J EARTH SCI, V31, P567, DOI 10.1139/e94-050; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; LOUWYE S, IN PRESS GEOL MIJNBO; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; MARTINI E, 1973, NEUES JB GEOLOGIE PA, V9, P555; Pascher A., 1914, Berlin Ber D bot Ges, V32; 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]; Rusbult J., 1992, N JB GEOL PALAONT MH, V3, P150; SCHILLER J, 1935, ZEHNTER BAND FLAGELL, P161; SPIEGLER D., 1988, GEOLOGISCHES JB A, VA100, P152; Stover L. E., 1977, AM ASS STRATIGRAPHIC, V5A, P66; TAVERNIER R, 1963, MEM SOC BELG GEOL PA, V8, P7; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Verbeek J., 1988, GEOLOGISCHES JB A, V100, P267; WALL D., 1967, PALAEONTOLOGY, V10, P95; Willems W., 1988, GEOLOGISCHES JB A, V100, P179; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363; Zevenboom D., 1995, PhD Thesis Diss	44	20	20	0	4	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	SEP	1999	107	1-2					109	123		10.1016/S0034-6667(99)00012-3	http://dx.doi.org/10.1016/S0034-6667(99)00012-3			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	241LA					2025-03-11	WOS:000082883600007
J	Uchida, T; Toda, S; Matsuyama, Y; Yamaguchi, M; Kotani, Y; Honjo, T				Uchida, T; Toda, S; Matsuyama, Y; Yamaguchi, M; Kotani, Y; Honjo, T			Interactions between the red tide dinoflagellates <i>Heterocapsa circularisquama</i> and <i>Gymnodinium mikimotoi</i> in laboratory culture	JOURNAL OF EXPERIMENTAL MARINE BIOLOGY AND ECOLOGY			English	Article						cell contact; Gymnodinium mikimotoi; Heterocapsa circularisquama; red tide; species interaction; temporary cyst	PEARL OYSTERS	Interactions between Heterocapsa circularisquama and Gymnodinium mikimotoi, causative red tide dinoflagellates, were investigated using bialgal cultures. G. mikimotoi was killed by H. circularisquama when the initial cell density of each species was set at 200 cells ml(-1). However, cells of H. circularisquama transformed to temporary cysts when the initial cell density of G. mikimotoi was increased to 2000 cells ml(-1), Thus the interaction between H, circularisquama and G. mikimotoi was found to be dependent upon the initial cell densities of the two species. Culture filtrate of H. circularisquama induced no inhibitory effect on the growth of G. mikimotoi. Similarly when separated by a membrane filter, G. mikimotoi grew well when cultured with H. circularisquama. G, mikimotoi appear to be killed by cell contact with H. circularisquama. In growth experiments using a culture filtrate of G. mikimotoi and cultures separated by a membrane filter, G. mikimotoi was shown to secrete a substance that inhibited the growth of H. circularisquama. However, the inhibitory effect of the medium was found at higher cell densities of G. mikimotoi than in the bialgal cultures at which the growth of H. circularisquama was suppressed and formed temporary cysts. It is likely that the inhibitory effect of G. mikimotoi on H. circularisquama in the bialgal cultures occurred mainly by direct cell contact. The growth of H. circularisquama and G. mikimotoi in the bialgal cultures was simulated using a mathematical model to quantify the interaction. The degree that G. mikimotoi was inhibited by H. circularisquama was found to be three times larger than the inhibitory effect of G. mikimotoi on H. circularisquama. (C) 1999 Elsevier Science B.V. All rights reserved.	Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; Natl Res Inst Aquaculture, Nansei, Mie 5160193, Japan; Kyushu Univ, Fac Agr, Higashi Ku, Fukuoka 8120053, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA); Kyushu University	Uchida, T (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan.			Matsuyama, Yukihiko/0000-0002-2775-1723				BRAND L E, 1981, Journal of Plankton Research, V3, P193, DOI 10.1093/plankt/3.2.193; HONJO T, 1978, Bulletin of Plankton Society of Japan, V25, P13; Honjo Tsuneo, 1994, Reviews in Fisheries Science, V2, P225; ISHIDA Y, 1986, MAR ECOL PROG SER, V30, P197, DOI 10.3354/meps030197; Itoh K., 1987, GUIDE STUDIES RED TI, P122; IWASA Y, 1998, SURI SEIBUTUGAKU NYU, P352; Maestrini S. Y., 1981, CAN B FISH AQUAT SCI, V210, P323; MATSUYAMA Y, 1995, NIPPON SUISAN GAKK, V61, P35; Matsuyama Y., 1996, Harmful and Toxic Algal Blooms, P247; Nagai K, 1996, AQUACULTURE, V144, P149, DOI 10.1016/S0044-8486(96)01307-5; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PRATT DM, 1966, LIMNOL OCEANOGR, V11, P447, DOI 10.4319/lo.1966.11.4.0447; Rice E. L., 1984, Allelopathy.; UCHIDA T, 1995, MAR ECOL PROG SER, V118, P301, DOI 10.3354/meps118301; UCHIDA T, 1977, Japanese Journal of Ecology, V27, P1; Uchida T., 1996, HARMFUL TOXIC ALGAL, P369; Yamaguchi M, 1997, J PLANKTON RES, V19, P1167, DOI 10.1093/plankt/19.8.1167	17	110	156	3	34	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0022-0981			J EXP MAR BIOL ECOL	J. Exp. Mar. Biol. Ecol.	AUG 17	1999	241	2					285	299		10.1016/S0022-0981(99)00088-X	http://dx.doi.org/10.1016/S0022-0981(99)00088-X			15	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	233XT					2025-03-11	WOS:000082453000008
J	Harland, R; Pudsey, CJ				Harland, R; Pudsey, CJ			Dinoflagellate cysts from sediment traps deployed in the Bellingshausen, Weddell and Scotia seas, Antarctica	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; modern; sediment traps; Antarctica; biogeography	ATLANTIC-OCEAN; INDIAN-OCEAN; TEMPORAL VARIABILITY; MICROBIAL COMMUNITY; CIRCUMPOLAR CURRENT; SURFACE SEDIMENTS; MARINE-SEDIMENTS; BOTTOM SEDIMENT; PACIFIC MARGIN; PARTICLE-FLUX	Dinoflagellate cysts have been recovered from six long-term (1-2 yr) sediment trap moorings deployed in the Bellingshausen, Weddell and Scotia seas, Antarctica. These traps, mostly moored near the sea bed to sample the nepheloid layer, were located both within and to the north of the maximum sea-ice limit. The numbers of cysts, together with the composition of the assemblages, reinforce the importance of the maximum sea-ice limit as a modern biogeographic boundary for the distribution of dinoflagellate cysts. Cysts derived from heterotrophic dinoflagellates make up the highest proportions within the assemblages recovered from the traps. One trap sampled the export production, revealing little difference in cyst flux over those sampling the nepheloid layer. Cyst Bur appears to be highest in areas closest to the Antarctic Convergence, north of the maximum sea-ice limit, and to high nutrient availability. There are, however, differences between the sediment trap assemblages and those recovered from core-top samples at the same or nearby sites. These differences, in the greater number of cysts, and in the higher numbers of round, brown Protoperidinium cysts in the traps, may reflect annual differences in the primary productivity and/or cyst production in the area. In some areas the sediment record may preserve little information about local surface water productivity because of the activity of bottom water currents, for example those arising from the Antarctic Circumpolar Current. (C) 1999 Elsevier Science B.V. All rights reserved.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Earth Sci, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England; British Antarctic Survey, Cambridge CB3 0ET, England	University of Sheffield; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.	rexharland@msn.com						ALLDREDGE AL, 1988, PROG OCEANOGR, V20, P41, DOI 10.1016/0079-6611(88)90053-5; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; 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; BALCH WM, 1983, CAN J FISH AQUAT SCI, V40, P244, DOI 10.1139/f83-287; BARBER M, 1995, ANTARCT SCI, V7, P39, DOI 10.1017/S0954102095000083; BARD E, 1990, NATURE, V345, P405, DOI 10.1038/345405a0; BARD E, 1993, RADIOCARBON, V35, P191, DOI 10.1017/S0033822200013886; BECQUEVORT S, 1992, POLAR BIOL, V12, P211; BODUNGEN BV, 1986, DEEP-SEA RES, V33, P177, DOI 10.1016/0198-0149(86)90117-2; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; Camerlenghi A, 1997, ANTARCT SCI, V9, P426, DOI 10.1017/S0954102097000552; CAMERLENGHI A, 1997, P 7 IN S ANT EARTH S, P705; Clarke A, 1996, LIMNOL OCEANOGR, V41, P1281, DOI 10.4319/lo.1996.41.6.1281; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DE VERNAL A, 1987, PALAEOGEOGR PALAEOCL, V61, P97, DOI 10.1016/0031-0182(87)90042-3; DODGE JD, 1987, J PLANKTON RES, V9, P685, DOI 10.1093/plankt/9.4.685; DUNBAR RB, 1981, GEOL SOC AM BULL, V92, P212, DOI 10.1130/0016-7606(1981)92<212:FPFTMB>2.0.CO;2; EVITT WR, 1985, AM ASS STRATIGR PALY; FISCHER G, 1988, NATURE, V335, P426, DOI 10.1038/335426a0; FOSTER TD, 1980, DEEP-SEA RES, V27, P367, DOI 10.1016/0198-0149(80)90032-1; GLOERSEN P, 1991, NATURE, V352, P33, DOI 10.1038/352033a0; GLOERSEN P, 1978, SP511 NASA; Grimm KA, 1997, SEDIMENT GEOL, V110, P151, DOI 10.1016/S0037-0738(97)00048-1; HARLAND R, 1989, J GEOL SOC LONDON, V146, P945, DOI 10.1144/gsjgs.146.6.0945; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Harland R, 1998, PALAEONTOLOGY, V41, P1093; HARLAND R, 1995, HOLOCENE, V5, P220, DOI 10.1177/095968369500500210; HILLAIREMARCEL C, 1994, CAN J EARTH SCI, V31, P139, DOI 10.1139/e94-012; HONJO S, 1976, MAR MICROPALEONTOL, V1, P65, DOI 10.1016/0377-8398(76)90005-0; Howe JA, 1999, J SEDIMENT RES, V69, P847, DOI 10.2110/jsr.69.847; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; Lampitt RS, 1997, DEEP-SEA RES PT I, V44, P1377, DOI 10.1016/S0967-0637(97)00020-4; LAMPITT RS, 1985, DEEP-SEA RES, V32, P885, DOI 10.1016/0198-0149(85)90034-2; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Matsuoka K., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1987, Bull. 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Micropaleontol.	AUG	1999	37	2					77	99		10.1016/S0377-8398(99)00016-X	http://dx.doi.org/10.1016/S0377-8398(99)00016-X			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	226VW					2025-03-11	WOS:000082044200001
J	Palliani, RB; Riding, JB				Palliani, RB; Riding, JB			Relationships between the early Toarcian anoxic event and organic-walled phytoplankton in central Italy	MARINE MICROPALEONTOLOGY			English	Article						lower Toarcian; central Italy; dinoflagellate cysts; prasinophytes; palaeoecology; organic facies; sequence stratigraphy	FRANCE	The integration of palynological and geochemical data from three lower Toarcian successions in central Italy reveals that the composition of organic walled phytoplankton assemblages were strongly affected by palaeoecological conditions related to bituminous sedimentation which accompanied the global anoxic event. The marked compositional variations of dinoflagellate cysts and prasinophytes, together with geochemical variations, have been linked to changes in surface water habitats during the lower Toarcian transgression. On the basis of the relationships between total organic carbon (TOC) and marine palynomorph assemblage composition, the lower Toarcian evolution of the Umbria-Marche Basin, central Italy, has been divided into four phases. Total organic carbon values rose significantly during the early Toarcian (Lower-middle Dactylioceras tenuicostatum ammonite Zone), and this can be linked to certain dinoflagellate cyst datums, for example the temporary disappearance of Mancodinium semitabulatum and the extinction of Luehndea spinosa. The presence of Umbriadinium mediterraneense and Valvaeodinium spp. accompany these moderately high TOC values. Subsequently, TOC levels increased to over 2% and prasinophytes became abundant in the Middle-upper D. tenuicostatum ammonite Zone. Mancodinium semitabulatum reappeared when TOC values eventually decreased in the Upper D, tenuicostatum ammonite Zone. This analysis has allowed the different sunlight requirements and life strategies of the early Toarcian Tethyan dinoflagellates to be modelled. Due to the cosmopolitan nature of the early Toarcian anoxic event, the principal marine palynological signals observed have been interpreted as sequence stratigraphical and palaeoecological indices. The Transgressive Systems Tract (TST) is accompanied by an increase in dinoflagellate cyst species diversity and a decrease in abundance. The: succeeding maximum flooding surface (mfs) corresponds with a prasinophyte acme. During the Highstand Systems Tract (HST), the phytoplankton shows an increase in abundance and a decrease in diversity. The range top of Luehndea spinosa appears to characterise the early Toarcian TST. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy; British Geol Survey, Keyworth NG12 5GG, Notts, England	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Palliani, RB (通讯作者)，Univ Perugia, Dept Earth Sci, Piazza Univ, I-06100 Perugia, Italy.							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AUG	1999	37	2					101	116		10.1016/S0377-8398(99)00017-1	http://dx.doi.org/10.1016/S0377-8398(99)00017-1			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	226VW					2025-03-11	WOS:000082044200002
J	Head, MJ; Nohr-Hansen, H				Head, MJ; Nohr-Hansen, H			The extant thermophilic dinoflagellate <i>Tectatodinium</i> <i>pellitum</i> (al. <i>Tectatodinium rugulatum</i>) from the Danian of Denmark	JOURNAL OF PALEONTOLOGY			English	Article							ADJACENT SEAS; NORTH; NETHERLANDS; SEDIMENTS; CYSTS	Tectatodinium rugulatum (Hansen, 1977) McMinn, 1988, from the lower Danian of Denmark, is considered conspecific with, and a junior synonym of, the extant thermophilic species Tectatodinium pellitum Wall, 1967. However, the Danian material, based on holotype and topotype specimens, appears to show a degree of morphologic variability not seen in younger material. The accepted stratigraphic range base of Tectatodinium pellitum is now extended to the lower Danian, where this species appears to be a useful biostratigraphic marker in the Danish North Sea basin.	Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada; Geol Survey Denmark & Greenland, DK-2400 Copenhagen NV, Denmark	University of Toronto; Geological Survey Of Denmark & Greenland	Head, MJ (通讯作者)，Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada.		Nohr-Hansen, Henrik/G-9058-2018	Nohr-Hansen, Henrik/0000-0002-9291-8104				BUTSCHLI O., 1885, KLASSEN ORDNUNGEN TH, P865; DALE B, 1997, 30 ANN M WOODS HOL M; du Chene R.E. Jan., 1988, Cahiers de Micropaleontologie, Centre Nationale de la Recherche Scientifique, V2, P147; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; 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; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HEAD MJ, 1994, MICROPALEONTOLOGY, V40, P289, DOI 10.2307/1485937; HERNGREEN GFW, 1986, REV PALAEOBOT PALYNO, V48, P1, DOI 10.1016/0034-6667(86)90055-2; Hultberg S.U., 1986, Journal of Micropalaeontology, V5, P37; KJELLSTROM G, 1981, GEOL FOREN STOCK FOR, V103, P271, DOI 10.1080/11035898109454523; LINDEMANN E, 1928, ZWEITE STARK VERMEHR, P3; MCMINN A, 1988, ALCHERINGA, V12, P137, DOI 10.1080/03115518808619002; 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; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; 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; WALL D., 1967, PALAEONTOLOGY, V10, P95	22	9	9	1	1	PALEONTOLOGICAL SOC INC	LAWRENCE	810 EAST 10TH ST, LAWRENCE, KS 66044 USA	0022-3360			J PALEONTOL	J. Paleontol.	JUL	1999	73	4					577	579		10.1017/S0022336000032406	http://dx.doi.org/10.1017/S0022336000032406			3	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	219HD					2025-03-11	WOS:000081601100003
J	Ellegaard, M; Moestrup, O				Ellegaard, M; Moestrup, O			Fine structure of the flagellar apparatus and morphological details of <i>Gymnodinium nolleri</i> sp nov (Dinophyceae), an unarmored dinoflagellate producing a microreticulate cyst	PHYCOLOGIA			English	Article							ELECTRON-MICROSCOPIC OBSERVATIONS; CATENATUM DINOPHYCEAE; INED. DINOPHYCEAE; ULTRASTRUCTURE; SEDIMENTS; AUSTRALIA; ELLEGAARD; TOXICITY; TASMANIA; LIGHT	A naked dinoflagellate producing microreticulate cysts is described as Gymnodinium nolleri sp. nov. It was previously misidentified as Gymnodinium catenatum based on strong morphological similarity with this species in both the cyst and motile stages. Gymnodinium nolleri differs from G. catenatum primarily in the size of the cyst and the Vegetative stage, G. nolleri being smaller although there is overlap, particularly in the size of the vegetative cell. The cyst of G. nolleri is 28-38 mu m in diameter, whereas G. catenatum measures 38-59 mu m. The vegetative cell of G. nolleri on average is 26 x 33 mu m and G. catenatum is 36 x 45 mu m. The motile stage of G. nolleri never forms long chains, whereas such chains are common in G. catenatum. The cyst of G. nolleri has fewer rows of polygons in the paracingulum than G. catenatum, and the polygons on the cyst are generally slightly smaller, although they appear larger due to the smaller size of the cyst. These differences and earlier described differences at the molecular level (large subunit ribosomal RNA sequence, isozyme profile, lack of paralytic shellfish poisoning (PSP) toxins in G. nolleri) justify describing G. nolleri as a new species. The fine structure of the flagellar apparatus of G. nolleri is included in the description. It shows features common to most dinoflagellates studied so far and has many similarities with the flagellar apparatus of 'Gymnodinium sp.' of Roberts (1986) and G. catenatum, e.g. a nuclear fibrous connective, longitudinal microtubular root-longitudinal basal body connectives, and a longitudinal microtubular root-ventral ridge connective.	Univ Copenhagen, Inst Bot, Dept Mycol & Phycol, DK-1353 Copenhagen K, Denmark	University of Copenhagen	Univ Copenhagen, Inst Bot, Dept Mycol & Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	mariane@bot.ku.dk	Ellegaard, Marianne/H-6748-2014	Moestrup, Ojvind/0000-0003-0965-8645				ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1989, TOXICON, V27, P665, DOI 10.1016/0041-0101(89)90017-2; 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, NORGES TEKNISK NATUR, V1, P1; BOLCH CJ, 1999, PHYCOLOGIA, V38; BRAVO I, 1997, HARMFUL ALGAE NEWS, V16, P4; Calado AJ, 1999, EUR J PHYCOL, V34, P179, DOI 10.1080/09670269910001736232; DODGE JD, 1969, NEW PHYTOL, V68, P613, DOI 10.1111/j.1469-8137.1969.tb06465.x; 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; FARMER MA, 1990, J PHYCOL, V26, P122, DOI 10.1111/j.0022-3646.1990.00122.x; FARMER MA, 1989, J PHYCOL, V25, P280, DOI 10.1111/j.1529-8817.1989.tb00124.x; Fraga S, 1995, PHYCOLOGIA, V34, P514, DOI 10.2216/i0031-8884-34-6-514.1; HAMER JP, 1998, NIGES TEKNISK NATURV, V1, P53; Hansen G, 1997, ARCH PROTISTENKD, V147, P381, DOI 10.1016/S0003-9365(97)80062-0; HANSEN G, 1993, J PHYCOL, V29, P486, DOI 10.1111/j.1529-8817.1993.tb00150.x; Hansen G, 1998, EUR J PHYCOL, V33, P281; Larsen N.H., 1994, SCANDINAVIAN CULTURE; LOEBLICH AR, 1975, J PHYCOL, V11, P80, DOI 10.1111/j.1529-8817.1975.tb02752.x; MOESTRUP O, 2000, FLAGELLATES; MOESTRUP O, 1998, NORGES TEKNISK NATUR, V1, P111; OSHIMA Y, 1993, DEV MAR BIO, V3, P907; REES AJJ, 1991, PHYCOLOGIA, V30, P90, DOI 10.2216/i0031-8884-30-1-90.1; ROBERTS K R, 1984, Journal of Phycology, V20, P28; ROBERTS KR, 1986, J PHYCOL, V22, P456, DOI 10.1111/j.1529-8817.1986.tb02489.x; ROBERTS KR, 1991, PROTOPLASMA, V164, P105, DOI 10.1007/BF01320818; Roberts KR, 1995, J PHYCOL, V31, P948, DOI 10.1111/j.0022-3646.1995.00948.x; ROBERTS KR, 1991, BIOL FREE LIVING HET, V4, P284; ROBERTSON S, 1995, PHYS PLASMAS, V2, P3, DOI 10.1063/1.871114; Thorsen TA, 1998, PALAEOGEOGR PALAEOCL, V143, P159, DOI 10.1016/S0031-0182(98)00079-0; WARNAAR J, 1998, NORGES TEKNISK NATUR, V1, P143; WILCOX LW, 1982, J PHYCOL, V18, P18	35	59	63	2	14	ALLEN PRESS INC	LAWRENCE	810 E 10TH ST, LAWRENCE, KS 66044 USA	0031-8884			PHYCOLOGIA	Phycologia	JUL	1999	38	4					289	300		10.2216/i0031-8884-38-4-289.1	http://dx.doi.org/10.2216/i0031-8884-38-4-289.1			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	241YB					2025-03-11	WOS:000082910500006
J	Bolch, CJS; Negri, AP; Hallegraeff, GM				Bolch, CJS; Negri, AP; Hallegraeff, GM			<i>Gymnodinium microreticulatum</i> sp nov (Dinophyceae):: a naked, microreticulate cyst-producing dinoflagellate, distinct from <i>Gymnodinium catenatum</i> and <i>Gymnodinium nolleri</i>	PHYCOLOGIA			English	Article							RECENT SEDIMENTS; COASTAL WATERS; RESTING CYSTS; AUSTRALIA; TASMANIA; STRAIN; GRAHAM	A new microreticulate cyst-producing dinoflagellate, Gymnodinium microreticulatum Belch et Hallegraeff (Gymnodiniaceae), is described from laboratory cultures established from germinated cysts collected from Newcastle Harbour, New South Wales, Australia. The species is a small, ovoid to biconical dinoflagellate with an anticlockwise apical groove encircling the apex. The vegetative cell and cyst features and the chloroplast structure and pigment composition are similar to those of the only two other known species forming microreticulate cysts, the PSP-toxin producer Gymnodinium catenatum Graham and the nontoxic Gymnodinium nolleri Ellegaard et Moestrup. Gymnodinium microreticulatum is also nontoxic, but the cysts (17-28 mu m in diameter) are much smaller and the vegetative cells (20-34 mu m long, 15-22 mu m wide) do not form chains and have a prominent, large nucleus positioned in the epicone of the cell. The cingulum is a descending left spiral that is displaced one fourth to one third the length of the cell with no torsion. DNA sequencing of the D1-D2 region of the large subunit ribosomal RNA gene indicates that the new species is genetically distinct (> 15% divergence) from but closely related to G. nolleri, G. catenatum, and several other gymnodinioid dinoflagellates with a horseshoe-shaped apical groove, a group that includes the type species Gymnodinium fuscum Stein.	Univ Tasmania, Sch Plant Sci, Hobart, Tas 7001, Australia; Australian Inst Marine Sci, Dampier, WA 6713, Australia	University of Tasmania; Australian Institute of Marine Science	Univ Tasmania, Sch Plant Sci, GPO Box 252-55, Hobart, Tas 7001, Australia.	cjsb@wpo.nerc.ac.uk	Bolch, Christopher/J-7619-2014; Negri, Andrew/G-9909-2017; Hallegraeff, Gustaaf/C-8351-2013	Negri, Andrew/0000-0003-1388-7395; Hallegraeff, Gustaaf/0000-0001-8464-7343				ANDERSON DM, 1988, J PHYCOL, V24, P255; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLACKBURN SI, 2000, IN PRESS PHYCOLOGIA; 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, 1998, NORGES TEKNISK NATUR, V1, P18; DALE B, 1993, DEV MAR BIO, V3, P47; 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; Fraga S, 1995, PHYCOLOGIA, V34, P514, DOI 10.2216/i0031-8884-34-6-514.1; HAGAR A, 1980, PIGMENTS PLANTS, P57; Hallegraeff G.M., 1989, P77; Hallegraeff G.M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P59; HULBURT EM, 1957, BIOL BULL, V122, P196; KIMBALL JF, 1965, J PROTOZOOL, V12, P577, DOI 10.1111/j.1550-7408.1965.tb03257.x; Kofoid C. 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J	Zonneveld, KAF; Jurkschat, T				Zonneveld, KAF; Jurkschat, T			<i>Bitectatodinium spongium</i> (Zonneveld, 1997) Zonneveld et Jurkschat, <i>comb.</i> <i>nov</i>. from modem sediments and sediment trap samples of the Arabian Sea (northwestern Indian Ocean):: taxonomy and ecological affinity	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Arabian Sea; dinoflagellate cyst; Bitectatodinium spongium; recent; ecological affinity; taxonomy	DINOFLAGELLATE CYST DISTRIBUTION; UPPER QUATERNARY SEDIMENTS; SOUTHWEST MONSOON; SURFACE SEDIMENTS; LAST DEGLACIATION; MARINE-SEDIMENTS; ATLANTIC-OCEAN; NORTH-ATLANTIC; SOMALI-CURRENT; ADJACENT SEAS	We present an emended diagnosis of Bitectatodinium spongium (Zonneveld, 1997) Zonneveld et Jurkschat, comb. nov. previously described as ?Algidasphaeridium spongium. New data from surface samples of the Pakistan shelf are combined with information from sediment traps off Somalia and Arabian Sea surface sediments to elucidate the taxonomy, ecological affinity and preservation of B. spongium. A pronounced relationship is detected between high concentrations of B. spongium and well-mixed, nutrient-rich surface waters, as observed in upwelling regions and in the vicinity of the Indus River outlet. High concentrations of this species are also found in coastal regions and regions with tropical sea surface temperature conditions. No relationship is observed between its distribution and differences in sea-surface salinity nor evidence for decay of B. spongium in relation to oxygen availability in bottom sediments. (C) 1999 Elsevier Science B.V. All rights reserved.	Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany; Fachbereich 5 Geowissensch, D-28334 Bremen, Germany	University of Bremen	Jurkschat, T (通讯作者)，Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany.							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Palaeobot. Palynology	JUL	1999	106	3-4					153	169		10.1016/S0034-6667(99)00007-X	http://dx.doi.org/10.1016/S0034-6667(99)00007-X			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	229YJ					2025-03-11	WOS:000082223300002
J	Lamolda, MA; Mao, SZ				Lamolda, MA; Mao, SZ			The Cenomanian-Turonian boundary event and dinocyst record at Ganuza (northern Spain)	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	Joint International Symposium of IGCP 350 on Cretaceous Environmental Change in East and South Asia/IGCP 362 on Tethyan and Boreal Cretaceous, at the 30th IGC	AUG 03-08, 1996	BEIJING, PEOPLES R CHINA	Academia_Sinica, Nanjing Inst Geol & Palaeontol, Peking Univ, Dept Geol, Natl Sci Fdn China, China Natl Comm IGCP, UNESCO, IUGS		dinocysts; bioevents; Cenomanian-Turonian; northern Spain	SEA-LEVEL CHANGE; DINOFLAGELLATE CYSTS; WESTERN INTERIOR; SEDIMENTS; SECTIONS; ENGLAND; BASIN	An excellent record of the Cenomanian-Turonian transition zone occurs in an expanded section near the Village of Ganuza, northern Spain. The sequence at Ganuza shows no evidence of stratigraphic discontinuities, and consists of an alternation of marl, marry limestone and limestone, which were deposited in a middle to outer shelf environment. Our results from palynological residues of 34 samples from the section indicate that number of cysts per gram of dry bulk sediment varies between a total of 7 and 236, and includes more than 130 taxa. Species diversity varies between 25 and 49 species and subspecies per sample. The Spiniferites ramosus group, together with two other important taxa, Trichodinium castanea and Exochosphaeridium phragmites dominate cyst assemblages. Other common taxa include Palaeohystrichophora infusorioides, Canningia reticulata, Pterodinium cingulatum, Coronifera oceanica, Florentinia mantellii, Cleistosphaeridium ?aciculare, Dapsilidinium laminaspinosum, and Xenascus ceratioides. Successive last occurrences of Florentia cooksoniae, Litosphaeridium siphoniphorum and Epelidosphaeridia spinosa (uppermost Cenomanian), and the first occurrence of Senoniasphaera rotundata (lower Turonian) are used to characterize the transition from Cenomanian to the Turonian. Our results show that dinocysts occur continuously throughout the Ganuza section across the C/T boundary event marked by only a slight decrease in species diversity. The most significant variation in the Ganuzan section in relation to the C/T boundary event is a decrease in cyst abundance from Late Cenomanian to earliest Turonian. The decline occurred just above a level marked by a benthic foraminiferal turnover as well as the extinction of Rotalipora cushmani. Dinocyst minimum abundances occurred slightly later than minimum abundances of nannofossils. Our dinocyst results are thus consistent with a decrease in productivity during the latest Cenomanian. A new cycle is marked by a strong recovery of dinocysts immediately above the boundary event, although a subsequent decrease recurred higher in the section. Dinoflagellates have a more general opportunistic behaviour than foraminifera and calcareous nannoflora, and such behaviour may offer a viable explanation to account for the different patterns of response observed between the dinocysts and the other microfossil groups. (C) 1999 Elsevier Science B.V. All rights reserved.	UPV, Fac Ciencias, Lejona 48940, Spain; China Univ Geosci, Dept Geol & Mineral Resources, Beijing 100083, Peoples R China	University of Basque Country; China University of Geosciences	Lamolda, MA (通讯作者)，UPV, Fac Ciencias, Campus Lejona, Lejona 48940, Spain.							[Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, Palynology: principles and applications; Clarke R. F. A., 1967, Verb K ned Akad Wet Amst, V24, P1; COLIN J P, 1982, Revista Espanola de Micropaleontologia, V14, P187; COURTINAT B, 1991, GEOBIOS-LYON, V24, P649, DOI 10.1016/S0016-6995(06)80293-7; COURTINAT B, 1993, MAR MICROPALEONTOL, V21, P249, DOI 10.1016/0377-8398(93)90017-R; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; DAVEY R.J., 1969, B BRIT MUS NAT HIST, V17, P103, DOI DOI 10.5962/P.313834; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DEBOER PL, 1986, GEOL SOC SPEC PUBL, V21, P321; DENNISON JOHN M., 1967, J PALEONTOL, V41, P706; Dodsworth Paul, 1996, Proceedings of the Yorkshire Geological Society, V51, P45; Downie C., 1971, Geoscience Man, V3, P29; Fitzpatrick MEJ, 1995, CRETACEOUS RES, V16, P757, DOI 10.1006/cres.1995.1048; Fitzpatrick MEJ, 1996, GEOL SOC SPEC PUBL, V102, P279, DOI 10.1144/GSL.SP.1996.001.01.21; FOUCHER JC, 1982, B CTR RECH EXPLOR PR, V6, P119; FOUCHER JC, 1980, REV MICROPALEONTOL, V22, P286; GOODMAN DK, 1987, BIOL DINOFLAGELLATES, V21; Goodman DK., 1979, Palynology, V3, P169; Gorostidi A., 1991, GEOGACETA, V10, P54; HABIB D, 1992, GEOLOGY, V20, P165, DOI 10.1130/0091-7613(1992)020<0165:DACNRT>2.3.CO;2; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; Head M.J., 1996, Palynology: Principles and Applications, P1197; HERNGREEN G F W, 1980, Revista Espanola de Micropaleontologia, V12, P23; JARVIS I, 1988, Cretaceous Research, V9, P3, DOI 10.1016/0195-6671(88)90003-1; Lamoida M.A., 1996, Geogaceta, V20, P1657; Lamolda M.A., 1989, P145; Lamolda M.A., 1982, MEMOIRES MUSEUM NA C, V49, P101; Lamolda MA, 1997, CRETACEOUS RES, V18, P331, DOI 10.1006/cres.1997.0061; LAMOLDA MA, 1994, CRETACEOUS RES, V15, P143, DOI 10.1006/cres.1994.1007; Lamolda Marcos A., 1996, Geological Society of India Memoirs, V37, P251; Lamolda Marcos A., 1995, Revista Espanola de Paleontologia, P101; LENTIN JK, 1993, ASSP FDN CONTRIB SER, V28; Li H, 1996, PALAIOS, V11, P15, DOI 10.2307/3515113; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; Mao S., 1988, ROYAL ONTARIO MUSEUM, V150, P1, DOI DOI 10.5962/BHL.TITLE.52243; Mao Shaozhi, 1998, Revista Espanola de Paleontologia, V13, P261; MARSHALL KL, 1988, REV PALAEOBOT PALYNO, V54, P85, DOI 10.1016/0034-6667(88)90006-1; PAUL CRC, 1994, GEOL MAG, V131, P801, DOI 10.1017/S0016756800012875; PAUL CRC, 1994, GEOLOGY, V22, P679, DOI 10.1130/0091-7613(1994)022<0679:IFACFI>2.3.CO;2; Peryt D, 1996, GEOL SOC SPEC PUBL, V102, P245, DOI 10.1144/GSL.SP.1996.001.01.18; SCULL BJ, 1966, GULF COAST ASS GEOLO, V16, P81; Tocher B.A., 1987, P138; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wiedman J., 1979, CUADERNOS GEOLOGIA I, V5, P127; Williams G.L., 1985, P847; Williams G.L., 1977, P1231; WILLIAMS GL, 1993, GEOL SURV CAN PAP, V9210, P1	50	32	36	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	JUN 15	1999	150	1-2					65	82		10.1016/S0031-0182(99)00008-5	http://dx.doi.org/10.1016/S0031-0182(99)00008-5			18	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	209RG					2025-03-11	WOS:000081062000007
J	Matsuoka, K				Matsuoka, K			Eutrophication process recorded in dinoflagellate cyst assemblages - a case of Yokohama Port, Tokyo Bay, Japan	SCIENCE OF THE TOTAL ENVIRONMENT			English	Article						dinoflagellate cyst; eutrophication; coastal environment; harmful phytoplankton; Tokyo Bay		To investigate temporal changes of water quality, a role of dinoflagellate cysts preserved in surface sediments was examined in Yokohama Port in Tokyo Bay, Japan. Two cores were collected, and sedimentation rates and ages of both were dated as approximately 1900 years or slightly older on the basis of Pb-210 and Cs-137 concentrations. The temporal change in dinoflagellate cyst assemblages in the two cores reflects eutrophication in Yokohama Port in the 1960s. Abrupt increases in the cysts of Gyrodinium instriatum cysts strongly suggests that a red tide was caused by this species around 1985. Dinoflagellate cyst assemblages in surface sediments appear to be good biomarkers of changes in the water quality of enclosed seas. (C) 1999 Elsevier Science B.V. All rights reserved.	Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, Nagasaki 8528521, Japan	Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Fac Fisheries, Lab Coastal Environm Sci, 1-14 Bunkyo Machi, Nagasaki 8528521, Japan.							[Anonymous], IOC MANUALS GUIDES; *BUR HARB YOK CIT, 1989, HIST YOK PORT GEN RE, P242; DALE B., 1994, CARBON CYCLING GLOBA, P521; Furota T., 1994, THINKING MARINE ENV, P69; GAINES G, 1984, J PLANKTON RES, V6, P1057, DOI 10.1093/plankt/6.6.1057; Ishimaru T, 1991, LA MER, V29, P180; Ishimaru T., 1995, KAIYO KAGAKU, V27, P434; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; Kitazato H., 1995, 11 YOK ENV RES I; KOJIMA N, 1992, REV PALAEOBOT PALYNO, V74, P339; MATSUMOTO E, 1983, Chikyukagaku, V17, P27; Matsumoto E, 1977, CHIKYU KAGAKU, V11, P51, DOI [10.14934/chikyukagaku.11.51, DOI 10.14934/CHIKYUKAGAKU.11.51]; MATSUOKA K, 1985, REV PALAEOBOT PALYNO, V44, P217, DOI 10.1016/0034-6667(85)90017-X; Matsuoka K., 1989, P461; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Matsuoka Kazumi, 1995, Fossils (Tokyo), V59, P32; SAKAMOTO IN, 1986, REGULATION NITROGEN, P96; Sato H., 1995, 116 YOK ENV RES I, P63; SHIRAYANAGI Y, 1995, 116 YOK ENV RES I, P5; TORIUMI S, 1986, 126 YOK ENV RES I, P273; TORIUMI S, 1989, 140 YOK ENV RES I, P341; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WATANABE M, 1997, SCI RED TIDES, P98; *YOK ENV RES I, 1992, 102 YOK ENV RES I, P133	24	141	171	1	35	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0048-9697			SCI TOTAL ENVIRON	Sci. Total Environ.	JUN 15	1999	231	1					17	35		10.1016/S0048-9697(99)00087-X	http://dx.doi.org/10.1016/S0048-9697(99)00087-X			19	Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	221TV	10466231				2025-03-11	WOS:000081743400002
J	Eriksson, B; Grönlund, T; Uutela, A				Eriksson, B; Grönlund, T; Uutela, A			Biostratigraphy of Eemian sediments at Mertuanoja, Pohjanmaa (Ostrobothnia), western Finland	BOREAS			English	Article							PLEISTOCENE STRATIGRAPHY; CENTRAL-EUROPE; CLIMATE; NORTH	The till-covered clay and silt deposits at Mertuanoja, Pohjanmaa (Ostrobothnia), western Finland, have been investigated in great detail. The Eemian interglacial environment is reconstructed here on the basis of pollen, diatom and dinoflagellate analyses. The pollen stratigraphy shows an interglacial vegetational succession reflecting stable climatic conditions typical of the Eemian Stage in the Pohjanmaa area. The initial Betula forests were followed by Pinus-Betula forests with Quercus. The next successional phase was dominated by Betula, Pinus and Alnus; temperate deciduous trees and Corylus. also grew in the area. Later, Picea advanced and temperate deciduous trees declined. Some Corylus was, however, still present and thermophilous Osmunda thrived in wet places. The diatom record indicates that the sediments were deposited first in a freshwater basin, then in the Eemian Baltic Sea, and finally in a freshwater basin once more. The presence of dinoflagellates demonstrates that the Eemian Baltic Sea, when at its maximum extent, was connected to the Atlantic Ocean, which brought northern cool-temperate surface waters to Finland as far north as Mertuanoja. Mertuanoja is the first interglacial site at which numerous dinoflagellate cysts were encountered in Finnish Quaternary sediments.	Geol Survey Finland, FIN-02151 Espoo, Finland; Univ Helsinki, Finnish Museum Nat Hist, Geol Museum, FIN-00014 Helsinki, Finland	Geological Survey of Finland (GTK); University of Helsinki	Eriksson, B (通讯作者)，Geol Survey Finland, POB 96, FIN-02151 Espoo, Finland.							Aalto Marjatta, 1992, Bulletin of the Geological Society of Finland, V64, P169; Alalammi P, 1987, ATLAS FINLAND; Alalammi P, 1988, ATLAS FINLAND; ANDERSON RW, 1991, PREVENTION HUMAN SER, V10, P9; [Anonymous], 1990, P 10 INT DIAT S 1988; Behre K.-E., 1986, EISZEITALT GGW, V36, P11, DOI [10.3285/eg.36.1.02, DOI 10.3285/EG.36.1.02]; Devyatova E.I., 1982, Prirodnaya sreda pozdnego pleistotcena i yeyo vliyanie na razvitie cheloveka v Severodvinskom basseine i v Karelii; Donner J., 1995, The Quaternary History of Scandinavia, V7; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; ERIKSSON B, 1993, GEOLOGICAL SURVEY FI, V372; ERONEN M, 1974, COMMENT PHYS-MATH, V44, P79; FENSOME RA, 1990, AASP CONTRIBUTION SE, V25; FORSSTROM L, 1988, PALAEOGEOGR PALAEOCL, V68, P317, DOI 10.1016/0031-0182(88)90049-1; Frenzel B., 1992, ATLAS PALEOCLIMATES; GENKAL S I, 1991, Diatom Research, V6, P255; GIBBARD P, 1979, ANN ACAD SCI FENN A3, V129; Gibbard P., 1989, ANN ACAD SCI FENN A3, V150; GRONLUND T, 1996, B GEOLOGICAL SOC FIN, V67, P61; Gronlund T., 1991, 102 GEOL SURV FINL; Gronlund T., 1991, GEOLOGICAL SURVEY FI, V352; HARLAND R, 1982, SVERIGES GEOLOGISK C, V794, P211; Hendey N.I., 1964, FISHERY INVESTIGAT 5, VIV; IISALO E, 1973, P1331009 GEOL SURV F; Iisalo E., 1996, GEOLOGI, V48, P58; Iisalo E., 1992, 112 GEOL SURV FINL; Khursevich G. K., 1990, P 10 INT DIAT S JOEN, P73; Kleman J, 1997, J GLACIOL, V43, P283, DOI 10.3189/S0022143000003233; KUJANSUU R, 1997, GEOLOGICAL SURVEY FI, P93; Lavrova M. A., 1960, CHETVERTICHNAYA GEOL; LIIVRAND E, 1991, 19 U STOCKH DEP QUAT; Litt T, 1996, VEG HIST ARCHAEOBOT, V5, P247, DOI 10.1007/BF00217502; Lundqvist J., 1992, GEOL SURV FINL SPEC, P43; MAMAKOWA K, 1989, Acta Palaeobotanica, V29, P11; MENKE B, 1984, GEOLOGISCHES JB A, V76; Nenonen K., 1995, PLEISTOCENE STRATIGR; Nenonen K., 1991, STRIAE, V34, P65; NIEMELA J, 1979, GEOLOGICAL SURVEY FI, V302; PELTONIEMI H, 1989, B GEOLOGICAL SOC FIN, V43, P209; Robertsson A. -M., 1992, SVERIGES GEOLOGISKA, V81, P299; Robertsson AM, 1997, BOREAS, V26, P237; Round F. E., 1992, Diatom Research, V7, P109; Round F E., 1990, Journal of the Marine Biological Association of the United Kingdom, V70, P924, DOI [10.1017/s0025315400059245, DOI 10.1017/S0025315400059245]; SAARNISTO M, 1995, GLAC DEP NE EUR, P3; SALONEN VP, 1992, BOREAS, V21, P253; SIMONSEN R, 1962, INT REV GESAMTE HYDR, V1; STOERMER EF, 1985, LIMNOL OCEANOGR, V30, P414, DOI 10.4319/lo.1985.30.2.0414; UUTELA A, IN PRESS B GEOLOGICA, V70; Uutela A., 1991, GEOLOGICAL SURVEY FI, V353; VIDAL G, 1988, Palynology, V12, P215; Volkova N.A., 1974, P194; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WETZEL W., 1952, GEOLOGISCHES JB HAMM, V66, P391; Zagwijn WH, 1996, QUATERNARY SCI REV, V15, P451, DOI 10.1016/0277-3791(96)00011-X; ZANS V, 1936, B COMMISSION GEOLOGI, V115, P231	54	17	17	0	2	SCANDINAVIAN UNIVERSITY PRESS	OSLO	PO BOX 2959 TOYEN, JOURNAL DIVISION CUSTOMER SERVICE, N-0608 OSLO, NORWAY	0300-9483			BOREAS	Boreas	JUN	1999	28	2					274	291						18	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	208NZ					2025-03-11	WOS:000080999100003
J	Mehrotra, NC; Kapoor, PN				Mehrotra, NC; Kapoor, PN			Palynology in hydrocarbon exploration - Advancements in Indian perspective	JOURNAL OF THE GEOLOGICAL SOCIETY OF INDIA			English	Article						palynology; hydrocarbons; exploration; dinoflagellate; India		Palynology plays an important role in cost effective exploration and exploitation of hydrocarbons. It consists of study of spores, pollen, dinoflagellate cysts, diatoms, nannoplankton, silicoflagellates, radiolaria, chitinozoa, algae and other organic remains. Study of spore, pollen, dinoflagellate cysts and nannoplankton help in precise dating of sediments, marking of hiatuses and correlating surface and subsurface samples by giving absolute ages in million years. Source rock study helps in visual typing of kerogen, quantitative assessment of organic matter, paleoenvironment and palynofacies interpretation. Spectral analysis gives precise thermal maturation levels. The integration of source rock parameters helps in deciphering source rock potential facies. Correlation of burial history curves with the source rock potential facies helps in the determination of time and duration of hydrocarbon generation. Examples from different sedimentary basins emphasizing the role of palynology in hydrocarbon exploration are cited. The biozonal comparisons and absolute pollen frequency (APF) values are being used for interpreting transgressive - regressive cycles. Paleogeographic maps can be reconstructed with palynological data. The chronostratigraphical correlation with seismic stratigraphy is being attempted in geologically synchronous stratal surfaces. Palynological studies support basin analysis leading to stratigraphic evolution and hydrocarbon prospect analysis. They also help to build sequence biostratigraphy and delineation of reservoir sands for effective reservoir management.	ONGC, KDM Inst Petr Explorat, Dehradun, India		Mehrotra, NC (通讯作者)，ONGC, KDM Inst Petr Explorat, Dehradun, India.							Brooks J., 1981, ORGANIC MATURATION S; KAPOOR PN, 1995, P PETR 95 NEW DELH, P97; KAPOOR PN, 1994, GEOSCI J, V15, P1; KAPOOR PN, 1997, P 2 INT PET C EXBN P, P141; KAPOOR PN, 1997, INDIAN J GEOL, V69, P83; MEHROTRA KL, 1990, SOURCE ROCK EVALUATI; MEHROTRA NC, 1997, UNPUB PALYNOSTRATIGR; Pocock S.A.J., 1988, Journal of Palynology, V23-24, P167; Swamy S.N., 1994, GEOSCI J, V15, P197; SWAMY SN, 1996, UNPUB SOURCE ROCK MO; VENKATACHALA BS, 1974, P 4 C IND MICR STRAT, P259; VENKATACHALA BS, 1984, B ONGC, V21, P28; Venkatachata B.S., 1981, PETROL ASIA J, V4, P80; WILSON LEONARD R., 1956, MICROPALEONTOLOGY, V2, P1; ZUTSHI PL, 1993, LITHOSTRATIGRAPHY IN	15	1	1	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	1999	53	6					637	648						12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	202UQ					2025-03-11	WOS:000080670900002
J	Palliani, RB; Riding, JB				Palliani, RB; Riding, JB			Early Jurassic (Pliensbachian-Toarcian) dinoflagellate migrations and cyst paleoecology in the Boreal and Tethyan realms	MICROPALEONTOLOGY			English	Article							MORGENROTH; EUROPE; EMEND	The discrepancies in the stratigraphical ranges of selected dinoflagellate cysts recorded in the Boreal and Tethyan realms have revealed two migrational events during the Early Jurassic. The first event occurred at the early-late Pliensbachian boundary and consists of mutual biotic exchanges between the two realms. This is linked to a major Early Jurassic transgression which improved marine communications between the Boreal and Tethyan areas. The second dinoflagellate migrational event occurred during the mid Toarcian and was driven by paleoenvironmental factors. The numerous available Lower Jurassic dinoflagellate cyst data from the Boreal and Tethyan realms indicates that phytoplankton distribution was profoundly affected by paleoecological factors. Information pertaining to the life strategies and the paleoecological requirements of the genera Luehndea, Nannoceratopsis and Valvaeodinium has also been determined.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy; British Geol Survey, Nottingham NG12 5GG, England	University of Perugia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Palliani, RB (通讯作者)，Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy.							ARKELLL WJ, 1956, JURASSIC GEOLOGY WOR; BALDANZA A, 1992, KNIHOVNICKA ZEMNIHO, V1, P111; Baldanza Angela, 1996, Palaeopelagos, V5, P161; BARTOLINI A, 1992, BENTHOS SENDAI, V90, P223; BAUDIN F, 1990, B SOC GEOL FR, V6, P123; Bown P.R, 1987, SPECIAL PAPERS PALEO, V38; Bucefalo Palliani R., 1994, PALEOPELAGOS, V4, P129; Cariou E., 1985, B SOC GEOL FR, V8, P679; Dale B., 1983, P69; DAVIES E H, 1985, Palynology, V9, P105; de Vains G., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P451; DODEKOVA L, 1989, Geologica Balcanica, V19, P88; FARAONI P, IN PRESS PALAEOPELAG, P6; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; GALACZ A, 1989, INT ASS SEDIMENTOLOG; Gardin Silvia, 1994, Geobios Memoire Special (Villeurbanne), V17, P229; Geczy B., 1984, Acta Geologica Academiae Scientiarum Hungaricae, V27, P379; Goodman D. K., 1987, BIOL DINOFLAGELLATES, P649; GORDON WA, 1970, GEOL SOC AM BULL, V81, P1689, DOI 10.1130/0016-7606(1970)81[1689:BOJF]2.0.CO;2; HALLAM A, 1983, PALAEOGEOGR PALAEOCL, V43, P181, DOI 10.1016/0031-0182(83)90010-X; HALLAM A, 1969, Palaeontology (Oxford), V12, P1; HALLAM A, 1987, MARINE PETROLEUM SOU, V26, P251; Hancock N. 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J	Hildebrand-Habel, T; Willems, H; Versteegh, GJM				Hildebrand-Habel, T; Willems, H; Versteegh, GJM			Variations in calcareous dinoflagellate associations from the Maastrichtian to Middle Eocene of the western South Atlantic Ocean (Sao Paulo Plateau, DSDP Leg 39, Site 356)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						calcareous dinoflagellates; Cretaceous; Tertiary; K T boundary; South Atlantic; DSDP	CRETACEOUS-TERTIARY BOUNDARY; NANNOFOSSIL; CYSTS; GEULHEMMERBERG; NANNOPLANKTON; NETHERLANDS; SUCCESSION; DINOCYSTS; DIVERSITY; TURNOVER	Calcareous dinoflagellates often dominate the dinoflagellate cyst assemblage in Cretaceous to Recent oceanic sediments. However, their distribution in Paleogene sediments has scarcely been studied. The investigation of samples from DSDP Site 356 for their calcareous dinoflagellate content revealed 35 mainly long-ranging taxa. The associations and characteristic wall types (pithonelloid, oblique, radial, tangential) fluctuate quantitatively and qualitatively in distinct stratigraphic patterns. Significant shifts, primarily at the K/T boundary and the Paleocene/Eocene boundary, reflect changes in environmental conditions. Certain dinoflagellates forming calcareous cysts, such as Operculodinella operculata, were well adapted to the relatively rapid change of environmental conditions at the K/T boundary, thus blooming to dominate the carbonate flux to the ocean floor. In contrast to the stable Paleocene associations, Eocene calcareous dinoflagellates show fluctuations in relative abundances. These fluctuations can possibly be attributed to redeposition related to increased seaward transport of specimens, due to strengthened western boundary currents. The flora includes two new genera, one new species, and two new forms: Retesphaera diadema Hildebrand-Habel, Willems et Versteegh, gen. et, sp. nov., Cervisiella saxea (Stradner, 1961) Hildebrand-Habel, Willems et Versteegh, gen. et comb. nov., Sphaerodinella? tuberosa forma elongata Hildebrand-Habel, Willems et Versteegh, comb. et forma nov., Sphaerodinella? tuberosa forma var variospinosa Hildebrand-Habel, Willems et Versteegh, comb. et forma nov.? Three new combinations are proposed: Cervisiella saxea (Stradner, 1961) Hildebrand-Habel, Willems et Versteegh, gen. et comb. nov., Operculodinella operculata (Bramlette et Martini, 1964) Hildebrand-Habel, Willems et Versteegh, comb. nov., and Sphaerodinella? tuberosa (Kamptner, 1963) Hildebrand-Habel, Willems et Versteegh, comb. nov. The genus Operculodinella Kienel, 1993 is emended. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Bremen, Dept Geol, D-28334 Bremen, Germany; Netherlands Inst Sea Res, NL-1797 AB Den Burg, Texel, Netherlands	University of Bremen; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Univ Bremen, Dept Geol, POB 330440, D-28334 Bremen, Germany.	hiha@micropal.uni-bremen.de	Hildebrand-Habel, Tania/F-3590-2011; Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776				[Anonymous], 1978, DEEP SEA DRILL PROJ; [Anonymous], 1959, ALGENKUNDE; [Anonymous], SEPM SPECIAL PUBLICA; Aubry M.-P., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P471, DOI 10.2973/odp.proc.sr.120.149.1992; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; BEIN A, 1976, Micropaleontology (New York), V22, P83, DOI 10.2307/1485322; 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; Bolli H.M., 1978, Initial Reports of the Deep Sea Drilling Project, V40, P819; Boudreaux J. 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Palaeobot. Palynology	JUN	1999	106	1-2					57	87		10.1016/S0034-6667(98)00079-7	http://dx.doi.org/10.1016/S0034-6667(98)00079-7			31	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	213BK					2025-03-11	WOS:000081252000002
J	Roncaglia, L; Schioler, P				Roncaglia, L; Schioler, P			<i>Alterbidinium austrinum</i> Roncaglia et Schioler, <i>sp nov</i>., a new dinoflagellate from the Conway Siltstone (Upper Cretaceous), southern Marlborough, New Zealand	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						New Zealand; dinoflagellates; taxonomy; Alterbidinium; Upper Cretaceous; Campanian		The new dinoflagellate Alterbidinium austrinum Roncaglia et Schioler, sp. nov. from the uppermost lower Haumurian (mid-upper Campanian) Isabelidinium korojonense Interval Zone in New Zealand, is a large, circumcavate, dorso-ventrally compressed, peridinioid cyst with subpentagonal outline. The pericyst bears two lateral and two or three antapical hems. One or two projections/horns usually occur at the apex. The endocyst is thin-walled, subcircular, and located centrally. The paratabulation is expressed by the paracingulum and the intercalary hexa 2a peri-archeopyle. Alterbidinium austrinum was encountered in a narrow stratigraphic interval in the Conway Siltstone, and may be a potential stratigraphic marker. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Modena & Reggio E, Dipartimento Sci Terra, I-41100 Modena, Italy; Geol Survey Denmark & Greenland GEUS, DK-2400 Copenhagen NV, Denmark	Universita di Modena e Reggio Emilia; Geological Survey Of Denmark & Greenland	Roncaglia, L (通讯作者)，Univ Modena & Reggio E, Dipartimento Sci Terra, Via Univ 4, I-41100 Modena, Italy.							Askin R.A., 1988, Geological Society of America Memoir, V169, P131; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; HARKER S D, 1990, Palaeontographica Abteilung B Palaeophytologie, V219, P1; KHOWAJAATEEQUZZ, 1991, PALAEOBOT, V39, P37; LENTIN J K, 1986, Palynology, V10, P111; Lentin J.K., 1985, CAN TECH REP HYDROG, V60, P1; Pascher A., 1914, Berlin Ber D bot Ges, V32; RONCAGLIA L, 1997, 97 NZ I GEOL NUCL SC; RONCAGLIA L, 1999, IN PRESS CRETACEOUS, V20; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; Warren G., 1978, New Zealand Geological Survey Bulletin, V92, P1; WILLIAMS GL, 1998, AM ASS STRATIGR PALY, V34	12	3	3	1	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUN	1999	106	1-2					121	129		10.1016/S0034-6667(99)00005-6	http://dx.doi.org/10.1016/S0034-6667(99)00005-6			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	213BK					2025-03-11	WOS:000081252000006
J	Okamoto, OK; Shao, LM; Hastings, JW; Colepicolo, P				Okamoto, OK; Shao, LM; Hastings, JW; Colepicolo, P			Acute and chronic effects of toxic metals on viability, encystment and bioluminescence in the dinoflagellate <i>Gonyaulax polyedra</i>	COMPARATIVE BIOCHEMISTRY AND PHYSIOLOGY C-TOXICOLOGY & PHARMACOLOGY			English	Article						luminescence; circadian rhythm; dinoflagellate; biological clock; Gonyaulax polyedra; pollutant metals; resting cysts; toxicity bioassays	FAST-FREEZE FIXATION; SUPEROXIDE-DISMUTASE; HEAVY-METALS; GROWTH; ORGANELLES; CADMIUM; ALGA; SCINTILLONS; IRRADIANCE; TRANSPORT	Toxicity bioassays based on survival were carried out with cells of the marine dinoflagellate Gonyaulax polyedra exposed to mercury (Hg2+), cadmium (Cd2+), lead (Pb2+) and copper (Cu2+). The toxicity scale of these metals found was Hg2+ > Cu2+ > Cd2+ > Pb2+. Cells exposed to metals promptly underwent encystment, which is an important strategy for surviving metal exposure. Following 48 h exposure to Cu2+, complete excystment occurred within 96 h after reinoculation of cells in fresh metal-free media, and with Pb2+ partial recovery occurred in that time. Bioluminescence was affected by the metals in a dose-dependent manner primarily by increasing he frequency of flashing, but the glow emission was also altered with acute Cu2+ and Pb2+ treatments, Several physiological processes in G. polyedra are under circadian control. Chronic exposures to metals caused no substantial alterations in the circadian rhythm of bioluminescence glow, indicating that the biological clock of this dinoflagellate is not sensitive to these metals at the concentrations tested. (C) 1999 Elsevier Science Inc. All rights reserved.	Univ Sao Paulo, Inst Quim, Dept Bioquim, Sao Paulo, Brazil; Harvard Univ, Dept Mol & Cellular Biol, Cambridge, MA 02138 USA	Universidade de Sao Paulo; Harvard University	Univ Sao Paulo, Inst Quim, Dept Bioquim, CP 26077, Sao Paulo, Brazil.	hastings@fas.harvard.edu	Colepicolo, Pio/C-1349-2013; Okamoto, Oswaldo Keith/C-5593-2013	Okamoto, Oswaldo Keith/0000-0002-8528-6225				ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], STRESS RESPONSES PLA; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; BEHRMANN G, 1995, PROTOPLASMA, V185, P22, DOI 10.1007/BF01272750; Broda H., 1986, Journal of Biological Rhythms, V1, P251, DOI 10.1177/074873048600100307; CHAN AT, 1980, J PHYCOL, V16, P428, DOI 10.1111/j.1529-8817.1980.tb03056.x; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Chapman PM, 1996, ENVIRON SCI TECHNOL, V30, pA448, DOI 10.1021/es962436d; CUMMING JR, 1990, STRESS RESPONSES PLA; Davies A.G., 1978, Advances in Marine Biology, V15, P381; DESJARDINS M, 1993, BIOCHEM CELL BIOL, V71, P176, DOI 10.1139/o93-028; ECKERT R, 1968, J GEN PHYSIOL, V52, P258, DOI 10.1085/jgp.52.2.258; FARMANFARMAIAN A, 1989, MAR ENVIRON RES, V28, P247, DOI 10.1016/0141-1136(89)90238-9; FRITZ L, 1990, J CELL SCI, V95, P321; GREEN DE, 1980, P NATL ACAD SCI-BIOL, V77, P257, DOI 10.1073/pnas.77.1.257; HALLIWELL B, 1991, FREE RADICAL BIO MED, P543; HAMILTON MA, 1977, ENVIRON SCI TECHNOL, V11, P714, DOI 10.1021/es60130a004; Hassan H.M., 1990, Stress Responses in Plants: Adaptation and Aclimation Mechanisms, P175; HASTINGS JW, 1961, J GEN PHYSIOL, V45, P69, DOI 10.1085/jgp.45.1.69; HASTINGS JW, 1958, BIOL BULL-US, V115, P440, DOI 10.2307/1539108; Hastings JW., 1991, COMP ANIMAL PHYSL NE, P435; HOLLIBAUGH JT, 1980, ESTUAR COAST MAR SCI, V10, P93, DOI 10.1016/S0302-3524(80)80052-1; Hollnagel HC, 1996, BRAZ J MED BIOL RES, V29, P105; Holovska K, 1996, COMP BIOCHEM PHYS B, V115, P451, DOI 10.1016/S0305-0491(96)00132-0; JOHNSON CH, 1986, AM SCI, V74, P29; Johnson CH, 1996, MOL MICROBIOL, V21, P5, DOI 10.1046/j.1365-2958.1996.00613.x; JOHNSON CH, 1984, SCIENCE, V223, P1428, DOI 10.1126/science.223.4643.1428; Kennish M. J., 1996, PRACTICAL HDB ESTUAR, P535; LAGE OM, 1994, EUR J PHYCOL, V29, P253, DOI 10.1080/09670269400650711; LAUBE VM, 1980, CAN J MICROBIOL, V26, P1300, DOI 10.1139/m80-217; MITCHELL GW, 1971, ANAL BIOCHEM, V39, P243, DOI 10.1016/0003-2697(71)90481-7; MORSE D, 1989, P NATL ACAD SCI USA, V86, P172, DOI 10.1073/pnas.86.1.172; NICOLAS MT, 1991, PROTOPLASMA, V160, P159, DOI 10.1007/BF01539967; NICOLAS MT, 1987, J CELL BIOL, V105, P723, DOI 10.1083/jcb.105.2.723; Okamoto OK, 1998, COMP BIOCHEM PHYS C, V119, P67, DOI 10.1016/S0742-8413(97)00192-8; Okamoto OK, 1996, J PHYCOL, V32, P74, DOI 10.1111/j.0022-3646.1996.00074.x; RAMALHO CB, 1995, PLANT PHYSIOL, V107, P225, DOI 10.1104/pp.107.1.225; REBHUN S, 1984, WATER RES, V18, P173, DOI 10.1016/0043-1354(84)90066-6; Reed R.H., 1990, HEAVY METAL TOLERANC, P105, DOI DOI 10.1016/j.biortech.2009.03.030; RIZZO PJ, 1991, J PROTOZOOL, V38, P246, DOI 10.1111/j.1550-7408.1991.tb04437.x; Robinson NJ, 1994, STRESS INDUCED GENE, P209; RODRIGUEZARIZA A, 1994, ENVIRON MOL MUTAGEN, V24, P116, DOI 10.1002/em.2850240207; ROENNEBERG T, 2000, IN PRESS METHODS ENZ, V305; Rosen BP, 1996, J BIOL INORG CHEM, V1, P273, DOI 10.1007/s007750050053; STEFFENS JC, 1990, STRESS RESPONSES PLA, P377; Sweeney B.M., 1987, RHYTHMIC PHENOMENA P, P172; SWEENEY BM, 1958, J PROTOZOOL, V5, P217, DOI 10.1111/j.1550-7408.1958.tb02555.x; Tang EPY, 1996, J PHYCOL, V32, P80, DOI 10.1111/j.0022-3646.1996.00080.x; Taylor F.J. R., 1987, Botanical Monographs, V21, P1; WIKFORS GH, 1982, MAR ECOL PROG SER, V7, P191, DOI 10.3354/meps007191	50	47	52	2	30	ELSEVIER SCIENCE INC	NEW YORK	STE 800, 230 PARK AVE, NEW YORK, NY 10169 USA	1532-0456	1878-1659		COMP BIOCHEM PHYS C	Comp. Biochem. Physiol. C-Toxicol. Pharmacol.	MAY	1999	123	1					75	83		10.1016/S0742-8413(99)00013-4	http://dx.doi.org/10.1016/S0742-8413(99)00013-4			9	Biochemistry & Molecular Biology; Endocrinology & Metabolism; Toxicology; Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Endocrinology & Metabolism; Toxicology; Zoology	199AR	10390059				2025-03-11	WOS:000080457500010
J	Rengefors, K; McCall, RD; Heaney, SI				Rengefors, K; McCall, RD; Heaney, SI			Quantitative X-ray microanalysis as a method for measuring phosphorus in dinoflagellate resting cysts	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Ceratium furcoides; Ceratium hirundinella; cyst; dinoflagellate; phosphorus; SEM; silicon; X-ray microanalysis; XRMA	SMALL PRODUCTIVE LAKE; CERATIUM-HIRUNDINELLA; VERTICAL MIGRATION; SCRIPPSIELLA-TROCHOIDEA; ELEMENTAL COMPOSITION; GONYAULAX-TAMARENSIS; PHYTOPLANKTON; AVAILABILITY; TEMPERATURE; DINOPHYCEAE	Energy dispersive X-ray microanalysis (XRMA) in a scanning electron microscope (SEM) was used as a method to measure elemental silicon (Si) and phosphorus (P) in dinoflagellate cysts. Cysts were prepared by quick jeep freezing and then freeze-drying, thereby avoiding the addition of preservatives. Cysts of Ceratium hirundinella collected from Lake Erken, Sweden and Esthwaite Water, UK, and Ceratium furcoides collected from Esthwaite Water, were analysed and compared. The hypothesis that cysts are able to assimilate P during dormancy was tested in the laboratory by incubating newly collected cysts of C. hirundinella in medium with and without phosphate. The analyses showed that there was no difference in P content between C. hirundinella and C. furcoides, suggesting that P content reflects differences in physiological status rather than species. C. hirundinella had a significantly higher Si content than C. furcoides, which agrees with earlier studies. Comparison of cysts of C. hirundinella from different years - 1995 (stored for 1 year), 1996 and 1997 - showed that the P content in cysts from 1995 was higher than that in cysts from the following 2 years, which indicates either that P was higher during encystment in 1995 or that cysts accumulated P during dormancy. The P uptake experiment showed a very slightly, but significantly, higher, P content in cysts incubated in P-rich medium.	Uppsala Univ, Dept Limnol, SE-75236 Uppsala, Sweden; Dept Agr No Ireland, Aquat Syst Grp, Belfast BT9 5PX, Antrim, North Ireland	Uppsala University	Rengefors, K (通讯作者)，Uppsala Univ, Dept Limnol, Norbyvagen 20, SE-75236 Uppsala, Sweden.	karin.rengefors@limno.uu.se	Rengefors, Karin/K-5873-2019	Rengefors, Karin/0000-0001-6297-9734				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; BEAKES GW, 1988, CAN J BOT, V66, P1054, DOI 10.1139/b88-151; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; CLAY S, 1991, SCANNING MICROSCOPY, V5, P207; DOTTNE-LINDGREN A, 1975, Internationale Revue der Gesamten Hydrobiologie, V60, P115, DOI 10.1002/iroh.19750600105; ElBestawy E, 1996, EUR J PHYCOL, V31, P157, DOI 10.1080/09670269600651331; Fryxell G.A., 1983, Survival Strategies of the algae, P1; Hairston N.G. Jr, 1987, P281; HAKANSSON L, 1978, SCRIPTA LIMNOLOGICA, V468; HALL DJ, 1991, J PHYCOL, V27, P537, DOI 10.1111/j.0022-3646.1991.00537.x; HEALEY FP, 1975, FISH MAR SERV RES DI, V585, P30; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HEANEY SI, 1980, J ECOL, V68, P75, DOI 10.2307/2259245; HEANEY SI, 1986, INT REV GES HYDROBIO, V71, P441, DOI 10.1002/iroh.19860710402; HEANEY SI, 1976, FRESHWATER BIOL, V6, P531, DOI 10.1111/j.1365-2427.1976.tb01644.x; HEANEY SI, 1980, FRESHWATER BIOL, V10, P163, DOI 10.1111/j.1365-2427.1980.tb01190.x; HEANEY SI, 1988, HYDROBIOLOGIA, V161, P133, DOI 10.1007/BF00044106; JAMES WF, 1992, CAN J FISH AQUAT SCI, V49, P694, DOI 10.1139/f92-078; LIRDWITAYAPRASIT T, 1990, J PHYCOL, V26, P299, DOI 10.1111/j.0022-3646.1990.00299.x; LOFGREN S, 1987, THESIS UPPSALA U; LUND J. W. G., 1964, INT VER THEOR ANGEW, V15, P37; LUND JWG, 1954, J ECOL, V42, P141; MACKERETH FJ, 1953, J EXP BOT, V4, P296, DOI 10.1093/jxb/4.3.296; Murphy J., 1966, ANAL CHIM ACTA, V27, P31, DOI DOI 10.1016/S0003-2670(00)88444-5; NAUWERCK ARNOLD, 1963, SYMBOLAE BOT UPSALIENSIS, V17, P1; Pettersson K, 1998, HYDROBIOLOGIA, V374, P21, DOI 10.1023/A:1017011420035; PETTERSSON K, 1985, INT REV GES HYDROBIO, V70, P527, DOI 10.1002/iroh.19850700407; PFEISTER LA, 1975, J PHYCOL, V11, P259; PFEISTER LA, 1976, J PHYCOL, V12, P234; POLLINGHER U, 1993, AQUAT SCI, V1, P10; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; Rengefors K, 1998, P ROY SOC B-BIOL SCI, V265, P1353, DOI 10.1098/rspb.1998.0441; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; Reynolds C.S., 1984, ECOLOGY FRESHWATER P; Tailing J.F., 1988, Algae and the Aquatic Environment, P1; TALLING J.F., 1971, MITTEL INT VERIENIGU, V19, P214; TAYLOR WD, 1988, CAN J FISH AQUAT SCI, V45, P1093, DOI 10.1139/f88-133; Ulen B., 1971, SCRIPTA LIMNOLOGICA, V270; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wall D., 1971, Geoscience Man, V3, P1; Wroblewski Joanna, 1993, P317, DOI 10.1017/CBO9780511600371.023	43	5	5	1	7	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0967-0262	1469-4433		EUR J PHYCOL	Eur. J. Phycol.	MAY	1999	34	2					171	177		10.1017/S0967026299002012	http://dx.doi.org/10.1017/S0967026299002012			7	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	210BT					2025-03-11	WOS:000081085800008
J	Sawada, M; Gajewski, K; de Vernal, A; Richard, P				Sawada, M; Gajewski, K; de Vernal, A; Richard, P			Comparison of marine and terrestrial Holocene climatic reconstructions from northeastern North America	HOLOCENE			English	Article						palaeoclimate; analog method; Labrador; Quebec; pollen; dinocyst; principal components analysis; marine records; terrestrial records; Holocene	DINOFLAGELLATE CYST ASSEMBLAGES; PALYNOLOGICAL EVIDENCE; SOUTHEASTERN LABRADOR; VEGETATIONAL HISTORY; POLLEN ASSEMBLAGES; MODERN ANALOGS; QUEBEC; SEA; ATLANTIC; SEDIMENTS	Quantitative climate reconstructions based on marine dinocysts and terrestrial pollen sequences are consistent through the Holocene in northeastern North America. Principal components analysis (PCA) indicates a large-scale climate signal in the dinocysts and pollen. The combined and separate analyses of marine and nearby terrestrial pollen sequences from Hudson Bay, Labrador and the St Lawrence estuary differentiate tundra, boreal forest and deciduous forest assemblages in time and space. These analyses indicate that the marine pollen record reflects vegetation changes of the regional terrestrial environment and allows direct correlations between the marine and terrestrial stratigraphies. Sea-surface temperatures estimated from dinocysts and terrestrial air temperatures from pollen using the method of modem analogs show that the three regions had differing climate histories associated with their location with respect to deglaciation and air mass boundaries. High frequency climatic changes reconstructed for the St Lawrence estuary and Gulf, and a cooling reconstructed for the period prior to 8000 yr BP, are less reliable due to the larger values of the dissimilarity coefficients. Prior to 6000 yr BP, cool temperatures reconstructed along the Labrador margins, both in the marine and terrestrial environments, are in agreement with climate simulations indicating the persistence of an anticyclone over the Quebec-Labrador ice sheet. In both Labrador and northwestern Quebec, a late-Holocene cooling affects sites in the forest-tundra, but is not evident in Boreal forest sites, suggesting movements in the mean position of the polar front.	Univ Ottawa, Dept Geog, Ottawa, ON K1N 6N5, Canada; Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; Univ Montreal, Dept Geog, Montreal, PQ H3C 3J7, Canada	University of Ottawa; University of Quebec; University of Quebec Montreal; Universite de Montreal	Sawada, M (通讯作者)，Univ Ottawa, Dept Geog, Ottawa, ON K1N 6N5, Canada.		Gajewski, Konrad/L-5128-2017; Sawada, Michael/O-8457-2019; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Sawada, Michael/0000-0001-5180-5325				ANDERSON PM, 1988, SCIENCE, V241, P1043, DOI 10.1126/science.241.4869.1043; ANDERSON PM, 1989, J BIOGEOGR, V16, P573, DOI 10.2307/2845212; Arigo R., 1986, Handbook of Holocene Palaeoecology and Palaeohydrology, P817; BILODEAU G, 1990, CAN J EARTH SCI, V27, P946, DOI 10.1139/e90-098; CALLEJA M, 1993, REV PALAEOBOT PALYNO, V79, P335, DOI 10.1016/0034-6667(93)90029-T; DAVIS RB, 1975, QUATERNARY RES, V5, P395, DOI 10.1016/0033-5894(75)90040-X; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; DEVERNAL A, 1986, CAHIERS GEOTOP, V3; DEVERNAL A, 1996, NATURE, V381, P744; DODGE JD, 1994, REV PALAEOBOT PALYNO, V84, P169, DOI 10.1016/0034-6667(94)90049-3; DUANE A, 1990, REV PALAEOBOT PALYNO, V63, P1, DOI 10.1016/0034-6667(90)90002-Z; Dyke AS, 1996, GEOGR PHYS QUATERN, V50, P125, DOI 10.7202/033087ar; ENGSTROM DR, 1985, CAN J BOT, V63, P543, DOI 10.1139/b85-070; GAJEWSKI K, 1995, QUATERNARY RES, V44, P228, DOI 10.1006/qres.1995.1067; GAJEWSKI K, 1992, ARCTIC ALPINE RES, V24, P329, DOI 10.2307/1551288; GAJEWSKI K, 1991, CAN J EARTH SCI, V28, P643, DOI 10.1139/e91-055; GAJEWSKI K, 1993, J ECOL, V81, P433, DOI 10.2307/2261522; GUIOT J, 1990, PALAEOGEOGR PALAEOCL, V80, P49, DOI 10.1016/0031-0182(90)90033-4; HEUSSER LE, 1990, QUATERNARY RES, V34, P101, DOI 10.1016/0033-5894(90)90075-V; HOOGHIEMSTRA H, 1992, REV PALAEOBOT PALYNO, V74, P1, DOI 10.1016/0034-6667(92)90137-6; JETTE H, 1992, GEOGR PHYS QUATERN, V46, P273, DOI 10.7202/032914ar; JOHNSTON RJ, 1980, MULTIVARIATE STAT AN, P127; KORVENA EV, 1971, MICROPALAEONTOLOGY O, P361; LABELLE C., 1981, Geographie physique et Quaternaire, V35, P345, DOI DOI 10.7202/1000544AR; LAMB HF, 1985, ECOL MONOGR, V55, P241, DOI 10.2307/1942559; LAMB HF, 1980, ARCTIC ALPINE RES, V12, P117, DOI 10.2307/1550510; Levac E, 1997, CAN J EARTH SCI, V34, P1358, DOI 10.1139/e17-108; LEZINE AM, 1991, QUATERNARY RES, V35, P456, DOI 10.1016/0033-5894(91)90058-D; Lezine AM, 1997, GEOLOGY, V25, P119, DOI 10.1130/0091-7613(1997)025<0119:EACITE>2.3.CO;2; Lynch EA, 1996, REV PALAEOBOT PALYNO, V94, P197, DOI 10.1016/S0034-6667(96)00040-1; MacRae RA, 1996, CAN J BOT, V74, P1687, DOI 10.1139/b96-205; MARCOUX N, 1995, CAN J EARTH SCI, V32, P79, DOI 10.1139/e95-008; MARRET F, 1994, REV PALAEOBOT PALYNO, V84, P1, DOI 10.1016/0034-6667(94)90038-8; MATSUOKA K, 1994, REV PALAEOBOT PALYNO, V84, P155, DOI 10.1016/0034-6667(94)90048-5; Ning S, 1997, VEG HIST ARCHAEOBOT, V6, P117, DOI 10.1007/BF01261959; OVERPECK JT, 1985, QUATERNARY RES, V23, P87, DOI 10.1016/0033-5894(85)90074-2; PRENTICE IC, 1980, REV PALAEOBOT PALYNO, V31, P71, DOI 10.1016/0034-6667(80)90023-8; PRENTICE IC, 1991, ECOLOGY, V72, P2038, DOI 10.2307/1941558; PRENTICE IC, 1985, QUATERNARY RES, V23, P76, DOI 10.1016/0033-5894(85)90073-0; Prentice IC, 1986, HDB HOLOCENE PALAEOE, P799; RICHARD P, 1976, CAN J EARTH SCI, V13, P145, DOI 10.1139/e76-014; RICHARD PJH, 1995, GEOGR PHYS QUATERN, V49, P117, DOI 10.7202/033033ar; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; Webb Thompson Iii, 1993, P415; WILLIAMS KM, 1995, ARCTIC ALPINE RES, V27, P352, DOI 10.2307/1552028; Wright HerbE., 1993, GLOBAL CLIMATES LAST	48	33	34	0	10	ARNOLD, HODDER HEADLINE PLC	LONDON	338 EUSTON ROAD, LONDON NW1 3BH, ENGLAND	0959-6836			HOLOCENE	Holocene	MAY	1999	9	3					267	277		10.1191/095968399671029755	http://dx.doi.org/10.1191/095968399671029755			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	194WV					2025-03-11	WOS:000080218500002
J	Askin, RA				Askin, RA			<i>Manumiella seymourensis</i> new species, a stratigraphically significant dinoflagellate cyst from the Maastrichtian of Seymour Island, Antarctica	JOURNAL OF PALEONTOLOGY			English	Article							LATE CRETACEOUS STRATIGRAPHY; LOPEZ-DE-BERTODANO; COCKBURN ISLAND; PENINSULA; EOCENE; POLLEN	The peridiniacean dinoflagellate cyst Manumiella seymourensis new species described herein characterizes Maastrichtian shallow marine sediments cropping out on Seymour Island, northeastern Antarctic Peninsula. It dominates palynological assemblages throughout the lower Maastrichtian (and possibly uppermost Campanian) to lower upper Maastrichtian part of the Lopez de Bertodano Formation. Despite its superficial similarity to some other southern mid to high paleolatitude Campanian-Maastrichtian species, M. seymourensis represents a discrete, biostratigraphically useful population of peridiniacean cysts. Its morphology and size parameters remain consistent throughout almost all of its stratigraphic range, equated with relatively stable environmental conditions throughout much of the Maastrichtian in the James Ross Basin. Morphological variations, equated with environmental change, are apparent in specimens in the lowermost and uppermost parts of its range.	Ohio State Univ, Byrd Polar Res Ctr, Columbus, OH 43210 USA	University System of Ohio; Ohio State University	Askin, RA (通讯作者)，Ohio State Univ, Byrd Polar Res Ctr, 1090 Carmack Rd, Columbus, OH 43210 USA.							[Anonymous], 1991, GEOLOGICAL EVOLUTION; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R.A., 1988, Geological Society of America Memoir, V169, P155; ASKIN RA, 1991, J S AM EARTH SCI, V4, P99, DOI 10.1016/0895-9811(91)90021-C; 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; ASKIN RA, 1994, REV PALAEOBOT PALYNO, V81, P151, DOI 10.1016/0034-6667(94)90105-8; Askin Rosemary A., 1996, P7; Baldoni A.M., 1986, Boletin del IG-USP, Serie Cientifica, V17, P89; Barreara E., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P813, DOI 10.2973/odp.proc.sr.113.137.1990; Barrera E, 1987, PALEOCEANOGRAPHY, V2, P21, DOI 10.1029/PA002i001p00021; DELVALLE RA, 1992, ANTARCT SCI, V4, P477, DOI 10.1017/S0954102092000695; Dettmann M.E., 1987, BRIT ANTARCTIC SURVE, V77, P13; Downie C., 1971, Geoscience Man, V3, P29; Elliot D.H., 1988, Geology and Paleontology of Seymour Island, Antarctic Peninsula, V169, P541, DOI [10.1130/MEM169-p541, DOI 10.1130/MEM169-P541]; ELLIOT DH, 1994, GEOLOGY, V22, P675, DOI 10.1130/0091-7613(1994)022<0675:IADATC>2.3.CO;2; Elliot DH, 1992, RECENT PROGR ANTARCT, P347; FRANCIS JE, 1986, PALAEONTOLOGY, V29, P665; Goodman DK., 1979, Palynology, V3, P169; GRANDE L, 1987, PALAEONTOLOGY, V30, P829; HARLAND R, 1973, Palaeontology (Oxford), V16, P665; Harwood D.M., 1988, Geology and Paleontology of Seymour Island, Antarctica Peninsula, V169, P55, DOI [10.1130/mem169-p55, DOI 10.1130/MEM169-P55]; Huber B.T., 1983, Antarctic Journal of the United States, V18, P72; HUBER B.T., 1988, Geology and Paleontology of Seymour Island, Antarctic Peninsula, V169, P163, DOI DOI 10.1130/MEM169-P163; Huber Brian T., 1992, Antarctic Research Series, V56, P31; KEATING JM, 1992, ANTARCT SCI, V4, P293, DOI 10.1017/S0954102092000452; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; LAWVER L.A., 1992, American Geophysical Union Antarctic Research Series, V56, P7; Macellari C.E., 1988, Geological Society of America Memoir, V169, P25; Mao S., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P307, DOI 10.2973/odp.proc.sr.120.190.1992; MARSHALL NG, 1990, ALCHERINGA, V14, P1, DOI 10.1080/03115519008619004; Palamarczuk S., 1984, 9 C GEOL ARG ACT, V1, P399; PIRRIE D, 1991, CRETACEOUS RES, V12, P227, DOI 10.1016/0195-6671(91)90036-C; Pirrie D, 1997, CRETACEOUS RES, V18, P109, DOI 10.1006/cres.1996.0052; Rinaldi C.A., 1982, Antarctic Geoscience, P281; SMITH D, 1992, AIDS, V6, P337, DOI 10.1097/00002030-199203000-00018; Stott L.D., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P829, DOI 10.2973/odp.proc.sr.113.158.1990; Tshudy D.M., 1988, Geological Society of America Memoir, V169, P291; WALL DAVID, 1965, MICRO PALEONTOLOGY, V11, P151, DOI 10.2307/1484516; WILSON GJ, 1984, NEW ZEAL J BOT, V22, P549, DOI 10.1080/0028825X.1984.10425289; Zinsmeister W.J., 1988, Geological Society of America Memoir, V169, P253; [No title captured]	42	14	15	0	0	PALEONTOLOGICAL SOC INC	LAWRENCE	810 EAST 10TH ST, LAWRENCE, KS 66044 USA	0022-3360			J PALEONTOL	J. Paleontol.	MAY	1999	73	3					373	379		10.1017/S0022336000027888	http://dx.doi.org/10.1017/S0022336000027888			7	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	198VW					2025-03-11	WOS:000080445800001
J	Hardeland, R				Hardeland, R			Melatonin and 5-methoxytryptamine in non-metazoans	REPRODUCTION NUTRITION DEVELOPMENT			English	Article; Proceedings Paper	8th Meeting of the European-Pineal-Society	JUL 03-07, 1999	TOURS, FRANCE	European Pineal Soc		algae; angiosperms; melatonin; 5-methoxytryptamine; protozoa	GONYAULAX-POLYEDRA; ANTIOXIDATIVE PROTECTION; INDUCED ENCYSTMENT; DINOFLAGELLATE; INDOLEAMINES; PLANTS; BIOLUMINESCENCE; RUBRUM; ALGA	Melatonin seems to be an almost ubiquitous substance, which has been detected not only in metazoans, but also in all major non-metazoan taxa investigated, including bacteria, dinoflagellates, euglenoids, trypanosomids, fungi, rhodophyceans, pheophyceans, chlorophyceans and angiosperms. Despite its vast abundance, little is known to date about its functions. Its presence is not necessarily associated with circadian rhythmicity, which is evident in yeast. Circadian rhythms of melatonin have been reported in non metazoans only for several unicellular organisms and in one angiosperm. In dinoflagellates, which have been studied in the most detail, the effects on enzyme activities and on phase shifting are known, but the most spectacular actions concerning the stimulation of bioluminescence, changes in cytoplasmic pH and induction of resting stages, can be related to a metabolite of melatonin, the 5-methoxytryptamine; therefore, melatonin should also be considered as a source of other agonists. (C) Inra/Elsevier, Paris.	Univ Gottingen, Inst Zool & Anthropol, D-37073 Gottingen, Germany	University of Gottingen	Univ Gottingen, Inst Zool & Anthropol, Berliner Str 28, D-37073 Gottingen, Germany.	rhardel@gwdg.de						[Anonymous], PLANT PHYSL; Antolín I, 1997, J PINEAL RES, V23, P182, DOI 10.1111/j.1600-079X.1997.tb00353.x; Balzer I, 1996, BOT ACTA, V109, P180, DOI 10.1111/j.1438-8677.1996.tb00560.x; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; BALZER I, 1991, COMP BIOCHEM PHYS C, V98, P395, DOI 10.1016/0742-8413(91)90223-G; BALZER I, 1993, INT CONGR SER, V1017, P183; BANERJEE S, 1973, EXP CELL RES, V78, P314, DOI 10.1016/0014-4827(73)90074-8; BANERJEE S, 1972, J PROTOZOOL, V19, P108, DOI 10.1111/j.1550-7408.1972.tb03423.x; BARTSCH I, 1999, IN PRESS BIOL RHYTHM; BENITEZKING G, 1993, EXPERIENTIA, V49, P635; DUBBELS R, 1995, J PINEAL RES, V18, P28, DOI 10.1111/j.1600-079X.1995.tb00136.x; Fuhrberg B, 1997, BIOL RHYTHM RES, V28, P144, DOI 10.1076/brhm.28.1.144.12978; Fuhrberg B, 1996, PLANTA, V200, P125; HARDELAND R, 1993, NEUROSCI BIOBEHAV R, V17, P347, DOI 10.1016/S0149-7634(05)80016-8; HARDELAND R, 1995, J PINEAL RES, V18, P104, DOI 10.1111/j.1600-079X.1995.tb00147.x; HARDELAND R, 1993, EXPERIENTIA, V49, P614, DOI 10.1007/BF01923941; HARDELAND R, 1993, TRENDS COMP BIOCH PH, V1, P71; HARDELAND R, 1999, IN PRESS ADV EXP MED; HARDELAND R, 1997, BIOMETEOROLOGY 2, V2, P278; Hardeland Ruediger, 1996, P25; HATTORI A, 1995, BIOCHEM MOL BIOL INT, V35, P627; JACKSON WT, 1969, J CELL SCI, V5, P745; Kolar J, 1997, PHYTOCHEMISTRY, V44, P1407, DOI 10.1016/S0031-9422(96)00568-7; Kolar J, 1995, BIOL RHYTHM RES, V26, P406; KOLAR J, 1999, IN PRESS BIOL RHYTHM; KUBIS HP, 1992, COMP BIOCHEM PHYS C, V102, P97, DOI 10.1016/0742-8413(92)90050-H; LORENZ M, 1999, IN PRESS BIOL RHYTHM; LUNING K, 1999, IN PRESS BIOL RHYTHM; Manchester LC, 1995, CELL MOL BIOL RES, V41, P391; Menendez-Pelaez A., 1992, Harderian glands: Porphyrin metabolism, behavioral, and endocrine effects, P219, DOI [10.1007/978-3-642-76685-5_13, DOI 10.1007/978-3-642-76685-5, DOI 10.1007/978-3-642-76685-513]; MENENDEZPELAEZ A, 1990, ADV PINEAL, V4, P75; POEGGELER B, 1991, Naturwissenschaften, V78, P268; POEGGELER B, 1989, Acta Endocrinologica Supplementum, V120, P97; POEGGELER B, 1994, J PINEAL RES, V17, P1, DOI 10.1111/j.1600-079X.1994.tb00106.x; REECE S, 1995, CAPS NEWS COMMUN, V14, P26; REITER RJ, 1995, J PINEAL RES, V18, P1, DOI 10.1111/j.1600-079X.1995.tb00133.x; SPRENGER J, 1999, IN PRESS CYTOLOGIA; Tilden AR, 1997, J PINEAL RES, V22, P102, DOI 10.1111/j.1600-079X.1997.tb00310.x; Tsim ST, 1998, J PINEAL RES, V24, P152, DOI 10.1111/j.1600-079X.1998.tb00528.x; Tsim ST, 1997, J CELL SCI, V110, P1387; VIVIENROELS B, 1993, EXPERIENTIA, V49, P642, DOI 10.1007/BF01923945; WERNER A, 1999, IN PRESS BIOL RHYTHM; WONG JTY, 1994, J MAR BIOL ASSOC UK, V74, P467, DOI 10.1017/S0025315400039515	43	77	86	1	11	EDP SCIENCES S A	LES ULIS CEDEX A	17, AVE DU HOGGAR, PA COURTABOEUF, BP 112, F-91944 LES ULIS CEDEX A, FRANCE	0926-5287			REPROD NUTR DEV	Reprod. Nutr. Dev.	MAY-JUN	1999	39	3					399	408		10.1051/rnd:19990311	http://dx.doi.org/10.1051/rnd:19990311			10	Developmental Biology; Nutrition & Dietetics; Reproductive Biology; Zoology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Developmental Biology; Nutrition & Dietetics; Reproductive Biology; Zoology	211WK	10420441	Bronze, Green Submitted			2025-03-11	WOS:000081184700012
J	Prince, IM; Jarvis, I; Tocher, BA				Prince, IM; Jarvis, I; Tocher, BA			High-resolution dinoflagellate cyst biostratigraphy of the Santonian-basal Campanian (Upper Cretaceous): new data from Whitecliff, Isle of Wight, England	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; Upper Cretaceous; biostratigraphy; chalk; Santonian; Campanian	ANGLO-PARIS BASIN; SOUTHERN ENGLAND; BOUNDARY; DISTRIBUTIONS; STRATIGRAPHY; INVERSION; CHALK	Results are presented of a high-resolution study of dinoflagellate cysts from part of the Upper Chalk succession on the Isle of Wight, southern England. The section was logged in detail, and stage and zonal boundaries were located using macrofossil data. Lower and middle Santonian samples are dominated by species of Senoniasphaera, Canningia, Circulodinium and Heterosphaeridium. Major changes in the dinocyst assemblages coincide with the base of the upper Santonian Uintacrinus socialis crinoid Zone, with an increase in abundance and diversity, and a shift to assemblages dominated by Spiniferites spp. and Palaeohystrichophora infusorioides Deflandre. Our palynological records (114 dinocyst, 4 acritarch species) provide the basis for a new event stratigraphy. Cyclonephelium filoreticulatum (Slimani) Prince, Jarvis et Tocher, comb. nov. temporarily disappears and an acme of Heterosphaeridium? heteracanthum (Deflandre et Cookson) Eisenack et Kjellstrom occur in the lower Santonian. The total range of Renidinium rigidum Prince, Jarvis et Tocher, sp. nov. and the FAD of Senoniasphaera protrusa Clarke et Verdier emend. lie within the middle Santonian. Raetiaedinium truncigerum (Deflandre) Kirsch and Pervosphaeridium monasteriense Yun first appear, and Hystrichostrogylon membraniphorum Agelopoulos reappears around the base of the upper Santonian. The FADs of Pervosphaeridium intervelum Kirsch and Thalassiphora? spinosa (Clarke et Verdier) Foucher, and the reappearance datums (RADs) of Chlamydophorella nyei Cookson et Eisenack, Subtilisphaera pontis-mariae (Deflandre) Lentin et Williams and Membranilarnacia polycladiata Cookson et Eisenack occur in the upper Santonian. No major changes in dinocyst assemblages occur at the Santonian/Campanian boundary, but a sequence of LADs occur in the basal lower Campanian, in the order: Xenascus perforatus (Vozzhennikova) Yun; Spinidinium echinoideum (Cookson et Eisenack) Lentin et Williams; Surculosphaeridium? longifurcatum (Firtion), Davey et al.; Raetiaedinium truncigerum (Deflandre) Kirsch and S. protrusa; Florentinia ferox (Deflandre) Duxbury; Acanthaulax wilsonii Yun and T.? spinosa, The range of Endoscrinium campanula (Gocht) Vozzhennikova extends into the upper Santonian. Additional taxonomic proposals are: Senoniasphaera Clarke emend.; S rotundata Clarke et Verdier emend,; Circulodinium latoaculeus (Yun) Prince, Jarvis et Tocher, comb, nov. (C) 1999 Elsevier Science B.V. All rights reserved.	STATOIL, Forus, N-4035 Stavanger, Norway; Kingston Univ, Sch Geol Sci, Ctr Earth & Environm Sci Res, Kingston upon Thames KT1 2EE, Surrey, England	Equinor; Kingston University	STATOIL, Forus, N-4035 Stavanger, Norway.	i.jarvis@kingston.ac.uk	Jarvis, Ian/A-1637-2008	Jarvis, Ian/0000-0003-3184-3097				Akimets V.S., 1978, Byulleten' Moskovskogo Obshchestva Ispytatelei Prirody Otdel Geologicheskii, V53, P42; Akimets V.S., 1979, Byulleten' Moskovskogo Obshchestva Ispytatelei Prirody Otdel Geologicheskii, V54, P112; [Anonymous], GEOL MAGAZ; [Anonymous], GEOL MAGAZ; [Anonymous], GEOL MAGAZ; BAILEY H W, 1984, Bulletin of the Geological Society of Denmark, V33, P31; Bailey H.W., 1983, NEWSL STRATIGR, V12, P29; Barr F. 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Palynology	MAY	1999	105	3-4					143	+		10.1016/S0034-6667(98)00077-3	http://dx.doi.org/10.1016/S0034-6667(98)00077-3			25	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	198GQ					2025-03-11	WOS:000080415500002
J	Hoedemaeker, PJ				Hoedemaeker, PJ			A Tethyan-Boreal correlation of pre-Aptian Cretaceous strata: Correlating the uncorrelatables	GEOLOGICA CARPATHICA			English	Article						Tethyan-Boreal correlation; pre-Aptian Cretaceous; biostratigraphy; magnetostratigraphy; sequence stratigraphy; Spain; France; Germany; England	DINOFLAGELLATE CYST STRATIGRAPHY; SOUTH-EAST FRANCE; SEQUENCE STRATIGRAPHY; NW GERMANY; MAGNETOSTRATIGRAPHY; BIOSTRATIGRAPHY; BOUNDARY; ENGLAND; SPAIN; PURBECK	Because of the high provinciality of the marine biota during the pre-Aptian Cretaceous times, there is no hope of a precise correlation of Tethyan with Boreal successions by means of biostratigraphy alone. Correlations with a detail as shown in the correlation schemes presented here, can be achieved only with the combination of all available correlation tools such as biostratigraphy, magnetostratigraphy and sequence stratigraphy.	Natl Museum Nat Hist, NL-2300 RA Leiden, Netherlands		Hoedemaeker, PJ (通讯作者)，Natl Museum Nat Hist, POB 9517, NL-2300 RA Leiden, Netherlands.							Aguirre Urreta Maria B., 1997, Geological Magazine, V134, P449, DOI 10.1017/S0016756897007206; ALLEN P, 1991, CRETACEOUS RES, V12, P511, DOI 10.1016/0195-6671(91)90005-W; Anderson F.W., 1985, Journal of Micropalaeontology, V4, P1; Anderson F.W., 1971, B GEOL SURV GT BRIT, V34, P1; Anderson F.W., 1973, BOREAL LOWER CRETACE, P101; ANDERSON FW, 1964, NATURE, V201, P907, DOI 10.1038/201907a0; ANDERSON FW, 1962, GEOL J, V3, P21; [Anonymous], DANMARKS GEOLOGISK B; [Anonymous], NEWSL STRATIGR; Arkell W. 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Carpath.	APR	1999	50	2					101	124						24	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	208MD					2025-03-11	WOS:000080994400002
J	Giacobbe, MG; Yang, XM				Giacobbe, MG; Yang, XM			The life history of <i>Alexandrium taylori</i> (Dinophyceae)	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium taylori; clonal cultures; cysts; morphology; Pyrrophyta; reproduction; sexuality	GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; DINOFLAGELLATE; TEMPERATURE; EXCYSTMENT	The gonyaulacoid dinoflagellate Alexandrium taylori Balech is reported for the first time from Italian waters. In July 1997, nonmotile stages of this species, both temporary and sexual resting cysts, were found in surface Ionian coastal waters (Mediterranean Sea) producing localized brownish-yellow patches. Clonal cultures were established, and the life history of A. taylori was studied in the laboratory. Asexual reproduction took place during a motile phase and produced two daughter cells remaining temporarily attached in pairs. This species exhibited isogamy, Small gametes were produced from vegetative cells through the release of a division cyst and multiple fission of the protoplast, Isogametes from the same clonal strain fused and underwent sexual reproduction, forming planozygotes that subsequently developed storage bodies and dark pigmentation. The maturation of the planozygote into hypnozygote also involved an increase in size and final shedding of flagella and theca. Hypnozygotes germinated within 15 days of their formation, and a naked planomeiocyte emerged from the archeopyle to undergo successive divisions and reestablish a haploid motile population.	CNR, Ist Sperimentale Talassograf, I-98122 Messina, Italy; Ocean Univ Qingdao, Qingdao 266003, Peoples R China	Consiglio Nazionale delle Ricerche (CNR); Ocean University of China	Giacobbe, MG (通讯作者)，CNR, Ist Sperimentale Talassograf, Via San Raineri 86, I-98122 Messina, Italy.	giacobbe@talas.ist.me.cnr.it						ANDERSEN RA, 1991, CATALOGUE STRAINS; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BALECH E, 1994, T AM MICROSC SOC, V113, P216, DOI 10.2307/3226651; BALECH E, 1990, TOXIC MARINE PHYTOPLANKTON, P77; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BLANCO J, 1989, Scientia Marina, V53, P785; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Delgado M, 1997, J PLANKTON RES, V19, P749, DOI 10.1093/plankt/19.6.749; ERKER EF, 1985, TOXICON, V23, P761, DOI 10.1016/0041-0101(85)90006-6; HALLEGRAEFF GM, 1991, BOT MAR, V34, P575, DOI 10.1515/botm.1991.34.6.575; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HONSELL G, 1993, DEV MAR BIO, V3, P127; HONSELL G, 1992, MARINE COASTAL EUTRO, P107; KITA T, 1985, B MAR SCI, V37, P643; KITA T, 1988, Bulletin of Plankton Society of Japan, V35, P1; Montresor M, 1996, MAR BIOL, V127, P55, DOI 10.1007/BF00993643; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; MONTRESOR M, 1990, TOXIC MARINE PHYTOPLANKTON, P82; MONTRESOR M, 1993, DEV MAR BIO, V3, P159; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; Sheehan DC., 1980, THEORY PRACTICE HIST; Steidinger Karen A., 1996, P387, DOI 10.1016/B978-012693015-3/50006-1; TERAO K, 1989, TOXIC MARINE PHYTOPL, P418; WALKER LM, 1979, J PHYCOL, V15, P312	26	50	51	2	9	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0022-3646			J PHYCOL	J. Phycol.	APR	1999	35	2					331	338		10.1046/j.1529-8817.1999.3520331.x	http://dx.doi.org/10.1046/j.1529-8817.1999.3520331.x			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	194YT		Bronze			2025-03-11	WOS:000080222900015
J	Pholpunthin, P; Fukuyo, Y; Matsuoka, K; Nimura, Y				Pholpunthin, P; Fukuyo, Y; Matsuoka, K; Nimura, Y			Life history of a marine dinoflagellate <i>Pyrophacus steinii</i> (Schiller) Wall <i>et</i> Dale	BOTANICA MARINA			English	Article							SEXUAL REPRODUCTION; DINOPHYCEAE; CYCLE; MORPHOLOGY; TAMARENSIS	The life history of a marine dinoflagellate Pyrophacus steinii (Schiller) Wall et Dale was investigated using clonal cultures isolated from Tokyo Bay. The asexual reproduction is binary fission of the eleutheroschisis type. All processes of asexual and sexual cell division occur inside the theca of the mother cells. Sexual reproduction is anisogamous and heterothallic. Male gametes differ from female gametes and vegetative cells in size, shape and plate tabulation. The female gametes can not be differentiated from the vegetative cells. Cell fusion between the male and female gametes occurs within a few hours to several days after inoculation of the male gametes into a culture of a non-male clone. Zygotes are similar to the vegetative cells in shape except possessing two longitudinal flagella. One to two days after plasmogamy, the zygotes become non-motile, and their protoplasts contract. Within 1 to 3 days, following the condensation of protoplast, they transform to hypnozygotes (resting cysts). The specific features of the life cycle can be summerized as: i) the asexual reproduction is eleutheroschisis, ii) sexual fusion occurs after inoculation of the small round thecate cells, which are equivalent to male gametes, into a culture of a non-male clone, iii) male gametes are distinctive from vegetative cells in their smaller size, round shape, fewer plate number and pale chloroplasts, iv) female gametes can not be differentiated from the vegetative cells, v) the sexual life cycle is anisogamous and heterothallic.	Prince Songkla Univ, Fac Sci, Dept Biol, Hat Yai 90112, Songkhla, Thailand; Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, Tokyo 113, Japan; Nagasaki Univ, Fac Fisheries, Dept Marine Biol, Nagasaki 8528521, Japan; Univ Tokyo, Fac Agr, Dept Fisheries Oceanog, Bunkyo Ku, Tokyo 113, Japan	Prince of Songkla University; University of Tokyo; Nagasaki University; University of Tokyo	Pholpunthin, P (通讯作者)，Prince Songkla Univ, Fac Sci, Dept Biol, Hat Yai 90112, Songkhla, Thailand.							BALECH E, 1978, Physis Seccion A los Oceanos y sus Organismos, V38, P27; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. Mexico, V7, P57; BEAM CA, 1974, NATURE, V250, P435, DOI 10.1038/250435a0; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; Faust MA, 1998, J PHYCOL, V34, P173, DOI 10.1046/j.1529-8817.1998.340173.x; FAUST MA, 1992, J PHYCOL, V28, P94; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; FUKUYO Y, 1987, GUIDE STUDIES RED TI, P54; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; KELLEY I, 1990, J PHYCOL, V26, P167, DOI 10.1111/j.0022-3646.1990.00167.x; KITA T, 1985, B MAR SCI, V37, P643; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; MATSUOKA K, 1985, T P PALAEONTOL SOC J, V140, P240; Matsuoka Kazumi, 1998, Paleontological Research, V2, P183; MONTRESOR M, 1994, B SOC ADRIATICA SCI, V125, P261; OGATA T, 1987, MAR BIOL, V95, P217, DOI 10.1007/BF00409008; 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, 1979, PHYCOLOGIA, V18, P13, DOI 10.2216/i0031-8884-18-1-13.1; PFIESTER LA, 1976, J PHYCOL, V12, P234; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; SAKO Y, 1984, B JPN SOC SCI FISH, V50, P743; SAKO Y, 1986, NIHON BISEIBUTSU SEI, V1, P19; SPERO HJ, 1981, J PHYCOL, V17, P43, DOI 10.1111/j.1529-8817.1981.tb00817.x; STEIDINGER K.A., 1967, FLA BD CONSERV MAR L, V1, P1; STOSCH HAV, 1965, NATURWISSENSCHAFTEN, V52, P112; Taylor F.J.R., 1976, BIBLIOTHECA BOT, V132, P1; WALL D, 1971, J PHYCOL, V7, P221, DOI 10.1111/j.1529-8817.1971.tb01507.x; XIAOPING G, 1989, Phycologia, V28, P342, DOI 10.2216/i0031-8884-28-3-342.1; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131; ZINGMARK RG, 1970, J PHYCOL, V6, P122, DOI 10.1111/j.0022-3646.1970.00122.x	32	6	8	1	10	WALTER DE GRUYTER & CO	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0006-8055			BOT MAR	Bot. Marina	MAR	1999	42	2					189	197		10.1515/BOT.1999.022	http://dx.doi.org/10.1515/BOT.1999.022			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	181ZM					2025-03-11	WOS:000079474100010
J	Dale, B; Thorsen, TA; Fjellså, A				Dale, B; Thorsen, TA; Fjellså, A			Dinoflagellate cysts as indicators of cultural eutrophication in the Oslofjord, Norway	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						eutrophication; marine pollution; sewage disposal; dinoflagellates; cysts; sedimentological tracers; fjords; Norway Coast	MARINE EUTROPHICATION; NORWEGIAN FJORD; SKAGERRAK; COMMUNITIES; POLLUTION; KATTEGAT; SEDIMENT; COAST; FISH; CORE	Dinoflagellate cyst records were analysed from four sediment cores from the inner Oslofjord. The cores covered the pre-industrial period, and the most important period of human population growth associated with industrial development of the region, from the mid-1800s to the present, including the reported development of cultural eutrophication. Comparisons between the cyst records and the known history of eutrophication suggest cyst signals that should prove useful for tracing the development of eutrophication. The eutrophication signal consisted of a doubling of total cyst concentration, and a married increase in one species in particular, Lingulodinium machaerophorum (from <5 to around 50% of the assemblages) with increased eutrophication. In the core considered most representative of general Rater quality in the inner fiord, these trends reversed back to pre-industrial levels during the 1980s and 1990s when improved sewage treatment took effect. (C) 1999 Academic Press.	Univ Oslo, Dept Geol, N-0316 Oslo, Norway; Statoil, N-4035 Stavanger, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Dept Geol, POB 1047, N-0316 Oslo, Norway.							ABDULLAH MI, 1992, HYDROBIOLOGIA, V235, P711, DOI 10.1007/BF00026259; ALHONEN P, 1979, ARCH HYDROBIOL, V86, P13; Alve E., 1991, Holocene, V1, P243, DOI 10.1177/095968369100100306; [Anonymous], 1996, Palynology: principles and applications; BADEN SP, 1990, AMBIO, V19, P113; BAKKEN K, 1983, THESIS U OSLO; Barss M. 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T., 1977, Revue Micropaleont, V20, P157; MUNTHEKAAS H, 1968, HELGOLAND WISS MEER, V17, P476, DOI 10.1007/BF01611248; NIXON SW, 1990, AMBIO, V19, P101; NIXON SW, 1995, OPHELIA, V41, P199, DOI 10.1080/00785236.1995.10422044; PAASCHE E, 1988, SARSIA, V73, P229, DOI 10.1080/00364827.1988.10413409; RICHARDSON K, 1995, OPHELIA, V41, P317, DOI 10.1080/00785236.1995.10422050; RISBERG J, 1990, AMBIO, V19, P167; ROSENBERG R, 1987, J EXP MAR BIOL ECOL, V105, P219, DOI 10.1016/0022-0981(87)90174-2; Rosenberg R, 1990, AMBIO, V19, P102; RUUD JT, 1968, HELGOLAND WISS MEER, V17, P510, DOI 10.1007/BF01611251; RUUD JT, 1968, HELGOLAND WISS MEER, V17, P455, DOI 10.1007/BF01611246; RYDBERG L, 1990, AMBIO, V19, P134; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; SIMOLA H, 1977, ANN BOT FENN, V14, P143; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Stockner J., 1972, Internationale Vereinigung fuer Theoretische und angewandte Limnologie Verhandlungen, P1018; Sy A, 1997, NATURE, V386, P675, DOI 10.1038/386675a0; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; Walsh J.J., 1981, Ecohydrodynamics, P13	52	153	175	3	42	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.	MAR	1999	48	3					371	382		10.1006/ecss.1999.0427	http://dx.doi.org/10.1006/ecss.1999.0427			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	183CE					2025-03-11	WOS:000079535800006
J	Gitmez, GU; Ertug, K				Gitmez, GU; Ertug, K			Dinoflagellate cysts and acritarchs from the Jurassic-Cretaceous boundary, northwest Anatolia, Turkey	MICROPALEONTOLOGY			English	Review								This paper presents the results of the first detailed study of organic microplankton assemblages from the Bilecik Formation (Middle-Upper Jurassic-Lower Cretaceous). The Bilecik Formation is exposed in northwest Anatolia, Turkey. Seventy-seven samples were analysed for organic microplankton. Although the resultant assemblages are varied, the species are represented in low numbers and their preservation is generally poor. A total of 97 species and subspecies of dinoflagellate cysts and acritarchs are recorded, Seventy-three species have been previously reported from the Middle and Upper Jurassic, fourteen other species were recorded for the first time in the Jurassic. Pollen and spores are abundant and varied.	Hacettepe Univ, Dept Geol Engn, TR-06532 Ankara, Turkey; Turkish Petr Corp, Res Ctr, TR-06520 Ankara, Turkey	Hacettepe University; Ministry of Energy & Natural Resources - Turkey; Turkish Petroleum Corporation (TPAO)	Gitmez, GU (通讯作者)，Hacettepe Univ, Dept Geol Engn, TR-06532 Ankara, Turkey.							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J	Bravo, I; Ramilo, I				Bravo, I; Ramilo, I			Distribution of microreticulate dinoflagellate cysts from the Galician and Portuguese coast	SCIENTIA MARINA			English	Article						cyst morphology; microreticulate cysts; Galicia; Gymnodium catenatum cyst	GYMNODINIUM-CATENATUM GRAHAM; TEMPERATURE; DINOPHYCEAE; AUSTRALIA; SEDIMENTS; TASMANIA; GROWTH	In May 1993, surface sediment samples from the west coast of thr Iberian Peninsula were collected with the aim of studying the geographic distribution of G. catenatum resting cysts. The sampling area ranged from 40 degrees 39' N (Portugal) to 42 degrees 38' N (Galicia, Spain). Cysts with exactly the same morphology as G. catenatum were found in a maximum concentration of 504 cysts.cm(-3) of sediment. Similar cysts but smaller (24-36 mu m) were found in a maximum concentration of 4488 cysts.cm(-3) of sediment. A bimodal size distribution of microreticulate cysts from the sediment indicates the probable existence of two cyst species. Differences in the microreticulation of the paracingulum were also observed. We compared the cysts from the sediment with G.catenatum cysts produced in cultures. The study on the distribution of cysts in the sediment also showed significant differences in the vertical profile concentrations of both cyst types. Differences in both the size and microreticulation morphology of the cysts found in the sediment of the continental shelf of Galicia and Portugal are also observed in the literature concerning other countries. The cysts of this species cited for the coasts of Northern Europe present characteristics similar to the cysts referred to in this communication as G. catenatum-like or small microreticulate cysts. The need to clarify the identity of cysts with microreticulation in the wall is discussed in order to identify the geographical distribution of the G. catenatum cyst.	Ctr Oceanog Vigo, IEO, Vigo 36280, Spain	Spanish Institute of Oceanography	Ctr Oceanog Vigo, IEO, Aptdo 1552, Vigo 36280, Spain.		Bravo, Isabel/D-3147-2012	Bravo, Isabel/0000-0003-3764-745X				ANDERSON DM, 1988, J PHYCOL, V24, P255; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1986, Boletin Instituto Espanol de Oceanografia, V3, P81; BLANCO J, 1989, Scientia Marina, V53, P813; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BOLCH CJ, 1998, TRONDHEIM RAPPORT BO, V1, P18; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; BRAVO I, 1998, HARMFUL ALGAE, P356; DALE B, 1993, DEV MAR BIO, V3, P47; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; ELLEGAARD M, IN PRESS PHYCOLOGIA; 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; NEHRING S, 1995, J PLANKTON RES, V17, P85, DOI 10.1093/plankt/17.1.85; Utermu┬hl H., 1958, MITT INT VER LIMNOL, V9, P1, DOI DOI 10.1080/05384680.1958.11904091	15	14	15	1	3	CONSEJO SUPERIOR INVESTIGACIONES CIENTIFICAS-CSIC	MADRID	VITRUVIO 8, 28006 MADRID, SPAIN	0214-8358	1886-8134		SCI MAR	Sci. Mar.	MAR	1999	63	1					45	50		10.3989/scimar.1999.63n145	http://dx.doi.org/10.3989/scimar.1999.63n145			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	178KK		Green Submitted, gold			2025-03-11	WOS:000079264700007
J	Kinzie, RA				Kinzie, RA			Sex, symbiosis and coral reef communities	AMERICAN ZOOLOGIST			English	Article; Proceedings Paper	Symposium on Coral Reefs and Environmental Changes - Adaptation, Acclimation, or Extinction at the Annual Meeting of the Society-for-Comparative-and-Integrative-Biology	JAN 03-07, 1998	BOSTON, MA	Soc Comparative & Integrative Biol			GREAT-BARRIER-REEF; POCILLOPORA-DAMICORNIS; DINOFLAGELLATE SYMBIONTS; MONTASTRAEA-ANNULARIS; SPORELING COALESCENCE; ECOSYSTEM PROCESSES; ACROPORA-PALIFERA; LUNAR PERIODICITY; GENUS ACROPORA; HIGH-LATITUDE	Questions about how today's corals and coral reefs will fare in a future that holds not only increasing direct anthropogenic impacts, but also global change, cannot be satisfactorily answered if we do not understand the relations of corals and reef systems to today's environmental conditions, This paper discusses four aspects of modern reef biology: coral reproduction coral population biology, the coral-zooxanthella symbiosis, and reef community ecology. Conclusions of this survey of current knowledge are that complexities of cnidarian reproductive biology, and our rudimentary knowledge of reproductive patterns in reef cnidarians, make forecasting based on current knowledge uncertain at best; new discoveries about the coral algal symbiotic system suggest a possible mode of adjustment to environmental change that warrants a strong research effort; coral communities of the future may well be unlike what we are familiar with today; and these new assemblages will be shaped by the interaction of novel environmental conditions and the characteristics of individual reef species.	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J	Gedl, E				Gedl, E			Lower Cretaceous palynomorphs from the Skole Nappe (Outer Carpathians, Poland)	GEOLOGICA CARPATHICA			English	Article						Early Cretaceous; Polish Flysch Carpathians; Skole Nappe; Spas Shale; paleoenvironment; biostratigraphy; palynofacies; Dinoflagellate cysts		Lower Cretaceous deposits of the Spas Shale from the Skole Nappe in Poland have been palynologically studied in several localities. Special emphasis has been put on the dinocyst assemblages. The Spas Shale consists of black shales which are intercalated with green shales in the uppermost parr. All the samples yielded rich and well preserved dinocyst and other palynomorph assemblages. The age of the studied deposits, based on dinocysts, spans from middle-late Barremian to latest Albian (Vraconian). Palynofacies of the middle-upper Barremian samples are characteristic for the neritic paleoenvironment. That contradicts previous data based on foraminiferal and lithological researches and may suggest transport of shallow marine organic matter into the deeper part of the basin. The Albian palynofacies is characteristic for an open marine paleoenvironment influenced by land-derived material. The studied dinocysts are almost entirely warm-water taxa. The presence of a few cold-water species in the Barremian samples suggests a connection between the Tethyan and Boreal provinces.	Jagiellonian Univ, Inst Geol Sci, PL-30063 Krakow, Poland	Jagiellonian University	Gedl, E (通讯作者)，Jagiellonian Univ, Inst Geol Sci, Oleandry 2A, PL-30063 Krakow, Poland.							Antonescu E., 1980, Anuarul Institutului de Geologie si Geofizica, V56, P97; BATTEN DJ, 1996, AM ASS STRAT PALYNOL, V3, P1011; 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; DUCHENE RJ, 1986, B CTR RECH EXPLOR PR, V12, P1; DUXBURY S, 1983, Palaeontographica Abteilung B Palaeophytologie, V186, P18; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Gucik S., 1963, Kwartalnik Geologiczny, V7, P257; HEILMANN-CLAUSEN C., 1987, DANMARKS GEOLOGISKE, V17, P1; Kotlarczyk J., 1979, BADANIA PALEONTOLOGI, P14; Kotlarczyk J., 1988, Przegl1d Geologiczny, V36, P325; Ksiazkiewicz M., 1956, Geologische Rundschau, V45, P369, DOI 10.1007/BF01802022; KSIAZKIEWICZ M, 1972, CARPATHIANS, V4, P1; LEEREVELD H, 1995, LAB PALEOBOT PALYN 2, P1; Lent John A., 1993, AM ASS STRAT PALY 28, P1; OLSZEWSKA B, 1984, PANSTW I GEOL B, V346, P7; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; Reneville P. D., 1981, B CEN RECH EXPLOR PR, V5, P1; SZYMAKOWSKA F, 1981, PANSTW I GEOL B, V331, P57; Vialov O.S., 1989, PALEONTOLOHYCHESKYI, V26, P71; VIALOV OS, 1988, AN USSR I GEOLOGII G, P1	23	16	16	1	2	SLOVAK ACADEMIC PRESS LTD	BRATISLAVA	PO BOX 57 NAM SLOBODY 6, 810 05 BRATISLAVA, SLOVAKIA	0016-7738			GEOL CARPATH	Geol. Carpath.	FEB	1999	50	1					75	90						16	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	188UY					2025-03-11	WOS:000079868200009
J	Montresor, M; Procaccini, G; Stoecker, DK				Montresor, M; Procaccini, G; Stoecker, DK			<i>Polarella glacialis</i>, gen. nov., sp. nov. (Dinophyceae):: Suessiaceae are still alive!	JOURNAL OF PHYCOLOGY			English	Article						Antarctica; cysts; Dinophyceae; phylogeny; Polarella glacialis sp. nov; sea ice; small-subunit (SSU) ribosomal RNA genes; Suessiaceae; Suessiales; Symbiodinium	ANTARCTIC SEA-ICE; MCMURDO-SOUND; FREUDENTHAL; BIOTA	The culture CCMP 1383, obtained from sea-ice brine collected in McMurdo Sound (Ross Sea, Antarctica), is a small gymnodinioid dinoflagellate, This species is very abundant in the upper land-fast sea ice, where it can both grow and overwinter as a spiny encysted stage. The motile vegetative stage and the cyst produced in the culture were studied by scanning electron microscopy (SEM) and transmission electron micrscopy (TEM), The amphiesma of the vegetative cells is constituted by thin vesicles that are organized into nine latitudinal series of plates: three in the epitheca, two in the cingulum, and four in the hypotheca, The same tabulation is reflected in the cyst wall by acicular processes arising from the center of paraplates, with the exception of the paracingulum, in which acicular processess are absent, On the basis of the peculiar plate pattern of this dinoflagellate, we establish the new genus Polarella and the new species Polarella glacialis (family Suessiaceae, order Suessiales), This species has a remarkable similarity with fossil Suessiaceae cysts dating back to the Triassic and Jurassic and represents, up to now, the only extant member of the subfamily Suessiaceae, Phylogenetic analysis based on the small-subunit ribosomal RNA gene confirmed the placement of this species in the order Suessiales and its close relationship with the genus Symbiodinium Freudenthal.	Staz Zool Anton Dohrn, I-80121 Naples, Italy; Univ Maryland, Horn Point Environm Lab, Ctr Environm Sci, Cambridge, MD 21613 USA	Stazione Zoologica Anton Dohrn; University System of Maryland; University of Maryland Center for Environmental Science	Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	mmontr@alpha.szn.it	Procaccini, Gabriele/AAA-7040-2019; stoecker, diane/F-9341-2013; Procaccini, Gabriele/A-6618-2010	Procaccini, Gabriele/0000-0002-6179-468X; Montresor, Marina/0000-0002-2475-1787				BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BUCK KR, 1992, J PHYCOL, V28, P15, DOI 10.1111/j.0022-3646.1992.00015.x; Fensome R.A., 1993, SPECIAL PUBLICATION; GARRISON DL, 1991, AM ZOOL, V31, P17; GARRISON DL, 1989, POLAR BIOL, V10, P211; HIGGINS DG, 1992, COMPUT APPL BIOSCI, V8, P189; HORIGUCHI T, 1994, PROTOPLASMA, V179, P142, DOI 10.1007/BF01403952; Ikavalko J, 1997, POLAR BIOL, V17, P473, DOI 10.1007/s003000050145; KELLER MD, 1987, J PHYCOL, V23, P633; KLIMYUK VI, 1993, PLANT J, V3, P493, DOI 10.1046/j.1365-313X.1993.t01-26-00999.x; LOEBLICH AR, 1979, J MAR BIOL ASSOC UK, V59, P195, DOI 10.1017/S0025315400046270; MARINO D, 1994, P 13 INT DIAT S, P229; Matsuoka K., 1989, P461; MCMINN A, 1993, J PLANKTON RES, V15, P925, DOI 10.1093/plankt/15.8.925; MCNALLY KL, 1994, J PHYCOL, V30, P316, DOI 10.1111/j.0022-3646.1994.00316.x; Meunier A., 1910, MICROPLANCTON MERS B; Okolodkov Yuri B., 1993, Polish Polar Research, V14, P25; PALMISANO AC, 1983, POLAR BIOL, V2, P171, DOI 10.1007/BF00448967; PHYLIP Felsenstein J, 1993, PHYLIP (phylogeny inference package); ROWAN R, 1992, P NATL ACAD SCI USA, V89, P3639, DOI 10.1073/pnas.89.8.3639; Saunders G.W., 1997, Origin of Algae and Their Plastids, P237, DOI [10.1007/978-3-7091-6542-3_13, DOI 10.1007/978-3-7091-6542-3_13]; SINECKER DK, 1993, MAR ECOL-PROG SER, V95, P103; 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; [Taylor F.J.R. Trench Trench], 1987, BIOL DINOFLAGELLATES, P530; TRENCH RK, 1987, J PHYCOL, V23, P469, DOI 10.1111/j.1529-8817.1987.tb02534.x; TRENCH RK, 1995, EUR J PHYCOL, V30, P149, DOI 10.1080/09670269500650911	28	108	115	3	17	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	FEB	1999	35	1					186	197		10.1046/j.1529-8817.1999.3510186.x	http://dx.doi.org/10.1046/j.1529-8817.1999.3510186.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	172LU					2025-03-11	WOS:000078926400024
J	Lewis, J; Harris, ASD; Jones, KJ; Edmonds, RL				Lewis, J; Harris, ASD; Jones, KJ; Edmonds, RL			Long-term survival of marine planktonic diatoms and dinoflagellates in stored sediment samples	JOURNAL OF PLANKTON RESEARCH			English	Article							GONYAULAX-TAMARENSIS; RESTING SPORES; FECAL PELLETS; GERMINATION; BACILLARIOPHYCEAE; CYSTS; DINOPHYCEAE; BLOOMS; WATER; LOCH	Sediment samples from Scottish coastal sites, taken over the last 9 years, were stored in closed containers at 5 degrees C. Slurry cultures were used to determine the survival of phytoplankton in these sediments. A range of diatom and dinoflagellate species survived for at least 27 months in these stored samples. A number of species grew for which no resting stage has yet been described: Thalassiosira angulata, T.pacifica, T.punctigera, T.eccentrica, T.minima and T.anguste-lineata. Notable results were survival times of 73 months for Skeletonema costatum, 96 months for Chaetoceros socialis, C.didymus and C.diadema, 109 months for Scrippsiella sp. and 112 months for Lingulo-dinium polyedrum. A single sample was stored and repeatedly cultured for diatoms over a period of 16 months. The number of species cultured from the sediment declined over this time. Lingulo-dinium polyedrum cysts isolated from sediments collected at least 18 months previously gave a hatching success of 97% and cysts isolated from a 9-year-old sample gave a hatching success of 3%. The study indicates the potential importance of coastal sediments as a source of phytoplankton to their overlying waters. The validity of using marine planktonic diatoms and dinoflagellates for modelling geological events is discussed.	Univ Westminster, Appl Ecol Res Grp, London W1M 8JS, England; Dunstaffnage Marine Res Lab, Oban PA34 4AD, Argyll, Scotland	University of Westminster	Lewis, J (通讯作者)，Univ Westminster, Appl Ecol Res Grp, 115 New Cavendish St, London W1M 8JS, England.							ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; ALVAREZ W, 1982, GEOL SOC AM SPEC PAP, V190, P305; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; 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; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO J, 1990, Scientia Marina, V54, P287; BUNT JS, 1972, LIMNOL OCEANOGR, V17, P458, DOI 10.4319/lo.1972.17.3.0458; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; Dale B., 1983, P69; DODSON AN, 1977, J EXP MAR BIOL ECOL, V26, P153, DOI 10.1016/0022-0981(77)90104-6; DOUCETTE GJ, 1983, MAR BIOL, V78, P1, DOI 10.1007/BF00392964; DOUCETTE GJ, 1982, EOS, V63, P47; DURBIN EG, 1978, MAR BIOL, V45, P31, DOI 10.1007/BF00388975; FOWLER SW, 1983, DEEP-SEA RES, V30, P963, DOI 10.1016/0198-0149(83)90051-1; FRENCH FW, 1980, MAR BIOL LETT, V1, P185; Fryxell G.A., 1983, SURVIVAL STRATEGIES; GRIFFIS K, 1988, PALAEOGEOGR PALAEOCL, V67, P305, DOI 10.1016/0031-0182(88)90158-7; GRIFFIS K, 1990, LETHAIA, V23, P379, DOI 10.1111/j.1502-3931.1990.tb01370.x; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hargraves P., 1983, SURVIVAL STRATEGIES, P49; Hargraves P.E., 1975, Nova Hedwigia, V53, P229; HARGREAVES PE, 1976, J PHYCOL, V12, P119; HARRIS ASD, 1995, EUR J PHYCOL, V30, P117, DOI 10.1080/09670269500650881; HARRIS ASD, 1995, THESIS U WESTMINSTER; HARRIS ASD, 1995, 111 DML MAR PHYS GRO; HEIMDAL B R, 1971, Norwegian Journal of Botany, V18, P153; HOLLIBAUGH JT, 1981, J PHYCOL, V17, P1; HUBER G., 1923, FLORA, V16, P114; Imai I., 1984, Bulletin of Plankton Society of Japan, V31, P123; IMAI I., 1990, B COAST OCEANOGR, V28, P75; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; KUWATA A, 1990, MAR BIOL, V107, P503, DOI 10.1007/BF01313435; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; LEWIS J, 1984, 114 SMBA; SICKOGOAD L, 1986, J PHYCOL, V22, P22, DOI 10.1111/j.1529-8817.1986.tb02510.x; SMAYDA TJ, 1974, MAR BIOL, V25, P195, DOI 10.1007/BF00394965; Syvertsen E.E., 1979, Nova Hedwigia Beih, V64, P41; Throndsen J., 1978, Monographs on oceanographic methodology, P218; UMEBEYASHI O, 1972, B TOKAI REGIONAL FIS, V69, P55; URBAN JL, 1993, BOT MAR, V36, P267, DOI 10.1515/botm.1993.36.4.267; Wall D., 1971, Geoscience Man, V3, P1; ZGUROVSKAYA LN, 1979, OCEANOLOGY, V19, P720	44	130	145	3	38	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	FEB	1999	21	2					343	354		10.1093/plankt/21.2.343	http://dx.doi.org/10.1093/plankt/21.2.343			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	168LV		Bronze			2025-03-11	WOS:000078695000009
J	Jaramillo, CA; Oboh-Ikuenobe, FE				Jaramillo, CA; Oboh-Ikuenobe, FE			Sequence stratigraphic interpretations from palynofacies, dinocyst and lithological data of Upper Eocene Lower Oligocene strata in southern Mississippi and Alabama, US Gulf Coast	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellates; palynofacies; graphic correlation; paleoecology; sequence stratigraphy; US Gulf Coast	DINOFLAGELLATE CYSTS; ADJACENT SEAS; SEDIMENTS; PLAIN; BOUNDARY; EXAMPLES; MEXICO; BASIN; NORTH	This paper presents new information on the sequence stratigraphy of the Upper Eocene-Lower Oligocene strata in southern Mississippi and Alabama, based on palynological and lithological data from five sections. By integrating Lithological characteristics with palynofacies assemblages, several dinocyst paleoecological groups, the Deflandrea group, and the abundance of reworked dinocysts in samples, paleobathymetric curves were reconstructed and used to revise the sequence stratigraphy of the area. We identified a maximum flooding surface in the middle of the Shubuta Clay Formation in southern Mississippi, and dated it as latest Eocene. In southern Alabama, the Eocene-Oligocene boundary was placed within a condensed section representing about 0.19 Ma, and it coincided with the Shubuta Clay-Vicksburg Group contact. This condensed section is equivalent to the accumulation of the upper Shubuta and Red Bluff Formations in southern Mississippi. The Forest W-Mint Spring contact, which has been interpreted as a sequence boundary that merged with a transgressive surface, does not correlate with the Tejas A (TA) 4.3/4.4 sequence boundary of Haq et al. (1988). The Pachuta Marl and lower Shubuta Clay Formations are constituents of a Late Eocene transgressive systems tract in southern Mississippi, but this systems tract extended to the Shubuta Clay-Vicksburg Group contact in southern Alabama. The overlying Early Oligocene highstand systems tract consisted of the upper Shubuta (in Mississippi), and the Red Bluff-Bumpnose-Forest Hill Formations. A thin sandstone in the Mint Spring was interpreted as a deposit of a possible lowstand systems tract above the sequence boundary in one southern Mississippi section. In general, the Mint Spring Marl and Marianna Limestone constituted a transgressive systems tract. (C) 1999 Elsevier Science B.V. All rights reserved.	Univ Florida, Florida Museum Nat Hist, Paleobot Lab, Gainesville, FL 32611 USA; Univ Missouri, Dept Geol & Geophys, Rolla, MO 65409 USA	State University System of Florida; University of Florida; University of Missouri System; Missouri University of Science & Technology	Univ Florida, Florida Museum Nat Hist, Paleobot Lab, Gainesville, FL 32611 USA.	carlos@flmhn.ufl.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691; jaramillo, carlos/0000-0002-2616-5079				[Anonymous], GEOLOGY N AM GULF ME; [Anonymous], 1990, GULF COAST ASS GEOL; [Anonymous], 2007, Paleopalynology; [Anonymous], 1988, SEA LEVEL CHANGES IN; [Anonymous], GULF COAST ASS GEOLO; [Anonymous], SPECIAL PUBLICATION; Batten D., 1996, Palynology: principles and applications, P1011; 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, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; Brinkhuis H., 1992, Eocene-Oligocene Climatic and Biotic Evolution, P327; Brinkhuis H., 1995, SOC ECON PALEONT MIN, V54, P295; BROWN S, 1984, P DSDP INIT REP, V81, P565; Bybell L.M., 1982, Transactions Gulf Coast Association of Geological Societies, V32, P295; BYBELL LM, 1983, T GULF COAST ASS GEO, V33, P253; CHATEAUNEUF JJ, 1983, SCI GEOL B, V36, P223; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Davey R.J, 1971, P 2 PLANKT C ROM, P331; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; Dockery David T. 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G., 1983, MISSISSIPPI BUREAU G, V125, P1; SIESSER WG, 1985, GEOL SOC AM BULL, V96, P827, DOI 10.1130/0016-7606(1985)96<827:COGCPP>2.0.CO;2; SOKAL ROBERT R., 1958, UNIV KANSAS SCI BULL, V38, P1409; STOVER LE, 1995, MICROPALEONTOLOGY, V41, P97, DOI 10.2307/1485947; *SYST, 1992, SYSTAT 5 MAC VERS 5; TEW BH, 1995, PALAIOS, V10, P133, DOI 10.2307/3515179; Traverse A., 1966, MAR GEOL, V4, P417, DOI DOI 10.1016/0025-3227(66)90010-7; VANVERGEN P, 1990, MEDED RIJKS GEOL DIE, V45, P1; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D, 1970, Micropaleontology (New York), V16, P47, DOI 10.2307/1484846; WILLIAMS D.B., 1971, MICROPALAEONTOLOGY O; WILLIAMS GL, 1977, MAR MICROPALEONTOL, V2, P223, DOI 10.1016/0377-8398(77)90012-3; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	73	48	62	0	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	FEB 1	1999	145	4					259	302		10.1016/S0031-0182(98)00126-6	http://dx.doi.org/10.1016/S0031-0182(98)00126-6			44	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	157FH					2025-03-11	WOS:000078049600001
J	De Coninck, J				De Coninck, J			Appearances of dinoflagellate species recorded in the Tienen Formation (Landen Group) and in the Kortrijk Formation (Ieper Group) in the Belgian Basin. Their relation to transgression phases in the southern part of the North Sea Basin	BULLETIN DE LA SOCIETE GEOLOGIQUE DE FRANCE			English	Article						Paleocene-Eocene; dinocysts; biostratigraphy; transgressions; North Sea Basin	EOCENE; CYSTS	In the Paleocene-Eocene transition deposits of Belgium, South England, North Germany and Denmark five biostratigraphic events in the succession of dinoflagellate cysts are selected. These successive events correspond to phases of increasing transgression in the southern North Sea Basin.	State Univ Ghent, Lab Paleontol, Vakgrp Geol & Bodemkunde, B-9000 Ghent, Belgium	Ghent University	De Coninck, J (通讯作者)，State Univ Ghent, Lab Paleontol, Vakgrp Geol & Bodemkunde, Krijgslaan 281-S8, B-9000 Ghent, Belgium.							[Anonymous], 1991, B SOC BELGE GEOLOGIE; [Anonymous], GEOLOGISCHES JB A; BOGGILD OB, 1918, DANMARKS GEOL UNDE 2, V33; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; DECONINCK J, 1998, IN PRESS B SOC BELGE; Dupuis C., 1985, B INF GEOL BASS PARI, V22, P19; 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., 1989, Geol. Jahrb., V111, P1; Heilmann-Clausen C., 1985, DGU, VA7, P1, DOI DOI 10.34194/SERIEA.V7.7026; Heilmann-Clausen Claus, 1993, Palynology, V17, P91; JOLLEY DW, 1989, REV PALAEOBOT PALYNO, V60, P361, DOI 10.1016/0034-6667(89)90050-X; KING C., 1990, MEMOIRES SERVIR EXPL, V29, P67; KING C, 1981, TERTIARY RES SPEC PA, V6; KNOX R W O, 1990, Proceedings of the Geologists' Association, V101, P145; Knox R.W.O., 1996, GEOLOGICAL SOC SPECI, V103, P209; KNOX R. W. O'B., 1990, TERTIARY RES, V11, P57; KNOX R. W. O'B., 1994, B SOC BELG GEOL, V102, P159; Knox RWO'B, 1989, GEOL JB A, VA111, P217; Kothe A., 1990, GEOL JB A, V118, P3; NIELSEN OB, 1986, GEOSKRIFTER, V24, P235; Powell A.J., 1996, Geological Society Special Publication, V101, P145, DOI 10.1144/GSL.SP.1996.101.01.10; Steurbaut E., 1994, Bulletin de la Societe Belge de Geologie, V102, P175; STEURBAUT E, 1998, STRATA 1, V9, P123; WILLEMS W, 1983, CONTINANTAL SHELF I, V108, P227; WILLEMS W, 1980, UNPUB FORMALINIFEREN; WILLIAMS GL, 1996, B BRIT MUS NATURAL S, V3, P20; WILLUMSEN P. S., 1998, STRATA 1, V9, P130; Wright C.A., 1972, Proceedings Geol Ass, V83, P413	29	5	7	0	6	SOC GEOL FRANCE	PARIS	77 RUE CLAUDE BERNARD, 75005 PARIS, FRANCE	0037-9409			B SOC GEOL FR	Bull. Soc. Geol. Fr.		1999	170	1					77	84						8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	166WR					2025-03-11	WOS:000078601300008
J	Steinhagen, D; Biffar, M; Korting, W				Steinhagen, D; Biffar, M; Korting, W			A dinoflagellate parasite from tropical fish	BULLETIN OF THE EUROPEAN ASSOCIATION OF FISH PATHOLOGISTS			English	Article							ENDEMIC STICKLEBACK; ASSOCIATION; CYCLE; HOST	In stocks of siluriform and cichlid ornamental fishes imparted from different locations in tropical Africa and South America. infections with vegetative cysts of a dinoflagellate occurred on skin, fins and gills. In affected fish the skin was covered with a greyish mucus layer and white spots developed like in infections with Ichthyophthirius multifiliis. The fish stopped feeding and in some stocks up the 100% of infected Fish died within 7 to 14 days. Treatments with standard procedures against ectoparasites were not successful. The dinoflagellates were identified based on the presence of a dinokaryotic nucleus with condensed chromosomes. On fish vegetative cysts but no trophonts were found. The cysts induced an epithelial cell hyperplasia. The epithelium cells formed a thickend layer which enclosed individual cysts or aggregates of cysts.	Tierarztlichen Hsch Hannover, Fachgebiet Fischkrankheiten & Fischhaltung, D-30559 Hannover, Germany; Aquarium Glaser, Rodgau, Germany	University of Veterinary Medicine Hannover	Steinhagen, D (通讯作者)，Tierarztlichen Hsch Hannover, Fachgebiet Fischkrankheiten & Fischhaltung, Buntenweg 17, D-30559 Hannover, Germany.			Steinhagen, Dieter/0000-0002-2303-8533				BUCKLANDNICKS JA, 1990, J PHYCOL, V26, P539, DOI 10.1111/j.0022-3646.1990.00539.x; Cachon J., 1987, The Biology of Dinoflagellates, P571; Hayat M.A., 1989, Principles and Techniques of Electron Microscopy: Biological Applications; LOM J, 1983, J FISH DIS, V6, P411, DOI 10.1111/j.1365-2761.1983.tb00096.x; Lom J., 1992, DEV AQUACULTURE FISH, V26; POLLINGHER U, 1987, BIOL DINOFLAGELLATES, P398; REIMCHEN TE, 1990, CAN J ZOOL, V68, P667, DOI 10.1139/z90-097; Romeis B., 1968, Mikroskopische Technik, V16th; [No title captured]	9	2	2	0	2	EUR ASSOC FISH PATHOLOGISTS	ABERDEEN	C/O DR DAVID BRUNO, MARINE LABORATORY, PO BOX 101, VICTORIA RD, ABERDEEN AB11 9DB, SCOTLAND	0108-0288			BULL EUR ASSN FISH P	Bull. Eur. Assoc. Fish Pathol.		1999	19	1					24	27						4	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology	229CX					2025-03-11	WOS:000082176900004
J	St-Onge, G; Leduc, J; Bilodeau, G; de Vernal, A; Devillers, R; Hillaire-Marcel, C; Loucheur, V; Marmen, S; Mucci, A; Zhang, D				St-Onge, G; Leduc, J; Bilodeau, G; de Vernal, A; Devillers, R; Hillaire-Marcel, C; Loucheur, V; Marmen, S; Mucci, A; Zhang, D			Characterization of recent Saguenay Fjord (Quebec) sediments based on physical, geochemical, isotopic and micropaleontological tracers	GEOGRAPHIE PHYSIQUE ET QUATERNAIRE			French	Article							ST-LAWRENCE ESTUARY; MARINE-SEDIMENTS; ORGANIC-CARBON; NORTH-ATLANTIC; BURIAL; CANADA; MATTER; PRESERVATION; RECORD; RATIOS	Characterization of recent Saguenay Fjord (Quebec) sediments based on physical, geochemical, isotopic and micropaleontological tracers. Physical (magnetic susceptibility, density, porosity and color), geochemical (C-org., C-inorg. and N), isotopic (C-13 and N-15 Of organic matter) and micropaleontological (foraminifera, diatoms, dinoflagellate cysts, pollen, spores) analyses were performed along a similar to 2 m core recovered from the inner basin of the Saguenay Fjord. The studied sequence spans approximatively 330 years. Two distinct lithostratigraphic units are defined. They indicate major changes in sedimentary dynamics. The bottom unit (below similar to 70 cm) reveals high terrigenous inputs characterized by low delta(13)C and delta(15)N values, high C/N ratios and the presence of detrital carbonates. This unit also depicts low marine microfossil concentrations and is tentatively assigned to the 1663 earthquake. The upper unit (similar to 70-0 cm) is characterized by high organic matter content, high marine biogenic content and reflects a hemipelagic sedimentation. The high diversity of the dinocyst assemblages and the high concentration of diatoms reveal both autotrophic and heterotrophic planktic production. The abundance of foraminifera linings suggests significant benthic production, whereas the rarity of benthic foraminifera shells provides evidence for calcium carbonate dissolution. Finally, pollen data, from the upper 30 cm of sediments, reflect an increase in non-arboreal inputs as a consequence of anthropogenic deforestation.	Univ Quebec, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	St-Onge, G (通讯作者)，Univ Quebec, CP 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.		Devillers, Rodolphe/R-3700-2019; Hillaire-Marcel, Claude/H-1441-2012; St-Onge, Guillaume/E-4828-2014; de Vernal, Anne/D-5602-2013; Hillaire-Marcel, Claude/C-9153-2013	Bilodeau, Guy/0000-0002-5419-9110; de Vernal, Anne/0000-0001-5656-724X; St-Onge, Guillaume/0000-0001-6958-4217; Devillers, Rodolphe/0000-0003-0784-847X; Hillaire-Marcel, Claude/0000-0002-3733-4632; Mucci, Alfonso/0000-0001-9155-6319				ANDERSON WT, 1985, POLLEN RECORDS LATE, P281; [Anonymous], GEOGRAPHIC PHYS QUAT; BASHAM PW, 1985, 8233 EARTH PHYS BRAN; BLANCHARD R, 1935, EST CANADA FRANCAIS, V2, P7; CANFIELD DE, 1994, CHEM GEOL, V114, P315, DOI 10.1016/0009-2541(94)90061-2; CORTIJO E, 1995, PALEOCEANOGRAPHY, V10, P911, DOI 10.1029/95PA02021; COTE R, 1979, NAT CAN, V106, P189; CRAIG H, 1957, GEOCHIM COSMOCHIM AC, V12, P133, DOI 10.1016/0016-7037(57)90024-8; DE VERNAL A, 1992, GEOLOGY, V20, P527, DOI 10.1130/0091-7613(1992)020<0527:QAOCDI>2.3.CO;2; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1996, CAHIER GEOTOP, V3; DEVERNAL A, 1991, PALYNOSCIENCES, V1, P145; DOIG R, 1986, CAN J EARTH SCI, V23, P930, DOI 10.1139/e86-094; DRAINVILLE G, 1968, Naturaliste Canadien (Quebec), V95, P809; Fortin G.R., 1995, Technical Report; GEARLING JN, 1988, LECT NOTES COASTAL O, V23, P69; INGALL ED, 1990, GEOCHIM COSMOCHIM AC, V54, P373, DOI 10.1016/0016-7037(90)90326-G; KUNZPIRRUNG M, 1997, THESIS U KIEL; LAPOINTE M, 1998, THESIS U QUEBEC MONT; LaSalle P., 1978, Depots meubles: Saguenay Lac Saint-Jean; Letolle R., 1980, Handbook of environmental isotope geochemistry. 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Phys. Quat.		1999	53	3					339	350		10.7202/004873ar	http://dx.doi.org/10.7202/004873ar			12	Geography, Physical; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Paleontology	331MC		Bronze			2025-03-11	WOS:000088022000005
J	Louwye, S; De Coninck, J; Verniers, J				Louwye, S; De Coninck, J; Verniers, J			Dinoflagellate cyst stratigraphy and depositional history of Miocene and Lower Pliocene formations in northern Belgium (southern North Sea Basin)	GEOLOGIE EN MIJNBOUW			English	Article						biostratigraphy; Diest Formation; Neogene		The occurrence of organic-walled dinoflagellate cysts (dinocysts) in the Diest Formation, a largely decalcified succession with a poor fossil content, and in the adjacent strata of Lower Miocene and Lower Pliocene formations, allowed a biostratigraphic evaluation of these deposits and an assessment of the hiatus between the lithostratigraphic units. The Diest Formation was deposited during Tortonian - Messinian times. Dinocyst biozones defined in the North Sea region and the U.S.A. East Coast are recognised within the Diest Formation, although environmental factors seem to have influenced the presence of some key zonal species in the shallow-marine deposits of northern Belgium. The two members of the Diest Formation studied, i.e., the Dessel Sands and the Diest Sands, appear to be strongly diachronous. The depocentre was located in the Campine area during the early Tortonian and shifted to the area north of Antwerp during late Tortonian to Messinian times. The age assessment provides a correlation of the sequence boundaries of Haq et al. (1987) at the top of the Diest Formation with SB 5.5.	State Univ Ghent, Inst Geol, Lab Palaeontol, B-9000 Ghent, Belgium	Ghent University	Louwye, S (通讯作者)，State Univ Ghent, Inst Geol, Lab Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Verniers, Jacques/B-8024-2009; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; BROWN S, 1985, INITIAL REP DEEP SEA, V80, P643; COSTA L, 1988, GEOL JB A, P321; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Meuter F. J. C, 1970, Bull. Soc. belge Geol. Paleont. Hydrol., V79, P175; DEHEINZELIN J, 1955, B SOC BELG GEOL, V64, P463; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; DUMONT A, 1839, B ACAD ROY BELGIQUE, V6, P479; EDWARDS LE, 1984, INITIAL REP DEEP SEA, V81, P581; GLIBERT M, 1955, B I ROYAL SCI NATURE, V31, P1; GULLENTOPS F, 1988, EXCURSION GUIDEBOOK, P225; GULLENTOPS F, 1983, GUIDES GEOLOGIQUES R, P164; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Head M.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V105, P467, DOI 10.2973/odp.proc.sr.105.137.1989; Head MJ, 1996, J PALEONTOL, V70, P543, DOI 10.1017/S0022336000023532; HERNGREEN GFW, 1987, MEDEDELINGEN WERKGRO, V24, P31; HINSCH W, 1988, GEOL JB A, P344; HOOYBERGHS H J F, 1972, Mededelingen van de Koninklijke Academie voor Wetenschappen Letteren en Schone Kunsten van Belgie Klasse der Wetenschappen, V34, P1; HOOYBERGHS HJF, 1988, GEOL JB A, P190; *IGCP 124 WORK GRO, 1988, GEOL JB A, P145; LAGA P G H, 1972, Bulletin de la Societe Belge de Geologie de Paleontologie et d'Hydrologie, V81, P211; Louwye S, 1998, B GEOL SOC DENMARK, V45, P73; LUND JJ, 1993, MUS NATURKUNDE BERLI, P27; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; MARTINI E, 1973, NEUES JB GEOLOGIE PA, V9, P555; NAKAGAWA H, 1994, RIV ITAL PALEONT STR, V80, P615; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Powell A.J., 1992, P155; SPIEGLER D, 1988, GEOL JB A, P152; TAVERNIER R, 1963, MEM SOC BELG GEOL PA, V8, P7; Van Adrichem Boogaert H.A., 1993, MEDED RIJKS GEOL DIE, V50; VANDENBERGHE N, 1998, SEPM SOC SEDIM GEOL, V60, P121; VERBEEK J, 1988, GEOL JB A, P267; WILLEMS W, 1988, GEOL JB A, P179; Williams Graham L., 1998, AASP Contributions Series, V34, P1; WOUTERS L, 1994, GEOLOGIE KEMPEN NIRA; Zevenboom D., 1995, Dinoflagellate Cysts from the Mediterranean Late Oligocene and Miocene	38	33	35	0	6	VEENMAN DRUKKERS	EDE	P O BOX 18, 6710 BA EDE, NETHERLANDS	0016-7746			GEOL MIJNBOUW	Geol. Mijnb.		1999	78	1					31	46		10.1023/A:1003793300214	http://dx.doi.org/10.1023/A:1003793300214			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	255YT					2025-03-11	WOS:000083698300003
J	Lewis, J; Rochon, A; Harding, I				Lewis, J; Rochon, A; Harding, I			Preliminary observations of cyst-theca relationships in <i>Spiniferites ramosus</i> and <i>Spiniferites membranaceus</i> (Dinophyceae)	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as			DINOFLAGELLATE RESTING CYSTS; RECENT SEDIMENTS	Motile thecal cells derived from the hatching of single cysts identified as Spiniferites membranaceus and S. ramosus have been used to establish cultures. These cultures were examined in order to assess the cyst-theca relationships of these two taxa. The cultures produced two different motile Gonyaulax species belonging to Kofoid's Spinifera group. These cultures were then induced to form a new cyst generation under uniform conditions, and examination of large numbers of the resulting cysts has shown that process development is an extremely variable phenomenon although process morphologies display a continuum within a species. Process length (and to a certain degree, process morphology) requires careful interpretation when used to discriminate Spiniferites taxa, in both modern and ancient environments.	Univ Westminster, Sch Biosci, London W1M 8JS, England	University of Westminster	Lewis, J (通讯作者)，Univ Westminster, Sch Biosci, 115 New Cavendish St, London W1M 8JS, England.		Harding, Ian/K-3320-2012					BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. Mexico, V7, P57; Claparede E, 1857, MEMOIRES I GENEVOIS, V6, P392; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DIESING KM, 1866, AKAD WISSENSCHAFT MN, V52, P287; DOBELL P E R, 1981, Palynology, V5, P99; DODGE JD, 1989, BOT MAR, V32, P275, DOI 10.1515/botm.1989.32.4.275; ELLEGAARD M, 1996, 9 INT PAL C HOUST 19; EVITT W. R., 1964, GEOL SCI, V10, P1; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Guillard RRL., 1973, HDB PHYCOLOGICAL MET, P69; Hall F, 1996, CD-ROM PROF, V9, P8; Harland R., 1977, Palaeontographica Abteilung B Palaeophytologie, V164, P87; Head M.J., 1996, Palynology: Principles and Applications, P1197; KOFOID C.A., 1911, U CALIFORNIA PUBLICA, V8, P187; Kokinos John P., 1995, Palynology, V19, P143; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Mantell G.A, 1850, A Pictorial Atlas of Fossil Remains Consisting of Coloured Illustrations Selected from Parkinson's "Organic Remains of a Former World", and Artis's "Antediluvian Phytology; Matsuoka K., 1987, Bull. Facult. Liberal Arts Nagasaki Univ. Nat. Sci., V28, P35; NEHRING S, 1994, OPHELIA, V39, P137, DOI 10.1080/00785326.1994.10429540; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Pouchet G, 1883, J ANATOM PHYSL NORM, V19, P399; Reid P.C., 1972, THESIS U SHEFFIELD; Taylor F.J.R., 1989, P295; WALL D, 1967, Review of Palaeobotany and Palynology, V2, P349, DOI 10.1016/0034-6667(67)90165-0; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1965, Grana Palynologica, V6, P297; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WALL D, 1970, Micropaleontology (New York), V16, P47, DOI 10.2307/1484846; WALL D., 1967, PALAEONTOLOGY, V10, P95	33	63	73	1	3	TAYLOR & FRANCIS AS	OSLO	CORT ADELERSGT 17, PO BOX 2562, SOLLI, 0202 OSLO, NORWAY	0017-3134			GRANA	Grana		1999	38	2-3					113	124		10.1080/00173139908559220	http://dx.doi.org/10.1080/00173139908559220			12	Plant Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	317LW					2025-03-11	WOS:000087227700006
J	Nohr-Hansen, H; Dam, G				Nohr-Hansen, H; Dam, G			<i>Trithyrodinium evittii</i> Drugg 1967 and <i>T-fragile</i> Davey 1969 an artificially split of one dinoflagellate cyst species -: Stratigraphic and palaeoenvironmental importance	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as			CRETACEOUS-TERTIARY BOUNDARY; ASSEMBLAGES; PALYNOLOGY; GEORGIA; SECTION	Based on morphological observations carried out on the same material, but submitted to different processing, Trithyrodinium fragile Davey 1969 is herein demonstrated to be a junior synonym of Trithyrodinium evittii Drugg 1967. From both original descriptions, the only way that the two species can be separated is by the presence or the absence of a thick brown organic layer on the surface of the endocyst. The present study proves that this is an artificial separation caused by different processing techniques. As a result, T. evittii is emended in order to encompass specimens, wholly or partially exhibiting this brown organic layer and previously attributed to T. fragile. These new observations also have stratigraphic and palaeoenvironmental implications. Combination of both synonym lists reveals that T. evittii, which is regarded as a warm mater species (58 degrees N to 52 degrees S) in the latest Cretaceous, migrated to higher latitudes (80 degrees N to 75 degrees S) in the earliest Paleocene. Consequently, an increase in oceanic circulation and/or temperature increase of the surface water is suggested during this epoch. In support of this contention, several peak occurrences of T. evittii are recorded just above the K/T boundary in high latitudes.	Geol Survey Denmark & Greenland, DK-2400 Copenhagen NV, Denmark	Geological Survey Of Denmark & Greenland	Geol Survey Denmark & Greenland, Thoravej 8, DK-2400 Copenhagen NV, Denmark.	hnh@geus.dk; gd@geus.dk	Dam, Gregers/G-4548-2018; Nohr-Hansen, Henrik/G-9058-2018	Nohr-Hansen, Henrik/0000-0002-9291-8104				[Anonymous], 1987, ASS AUSTRALASIAN PAL; [Anonymous], 1976, BEDFORD I OCEANOGRAP; ANTONESCU E, 1982, PALEONTOLOGIE, V3, P61; 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, 1998, GEOLOGICAL SOC AM ME, V169, P131; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; BUJAK JP, 1978, GEOLOGICAL SURVEY CA, V297, P1; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; Christensen L., 1973, B GEOL SOC DENMARK, V22, P193; DAVEY R J, 1969, Palaeontologia Africana, V12, P1; DRUGG W.S., 1967, PALAEONTOGRAPHICA B, V120, P1; EHRENBERG CG, 1831, SYMBOLAE PHYSICAE ZO, V10, P119; Fensome R.A., 1993, CLASSIFICATION FOSSI; FIRTH J V, 1987, Palynology, V11, P199; FIRTH JV, 1993, REV PALAEOBOT PALYNO, V79, P179, DOI 10.1016/0034-6667(93)90022-M; GAMERRO J C, 1981, Revista Espanola de Micropaleontologia, V13, P119; Haeckel E., 1894, Systematische Phylogenie. 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Systematische Phylogenie der Protisten und Pflanzen, V1; Hansen J.M., 1978, MICROPALEONTOLOGY, V25, P113; Hargrove DC, 1997, SEDIMENT GEOL, V108, P121, DOI 10.1016/S0037-0738(96)00050-4; IOANNIDES N.S., 1986, B GEOLOGICAL SURVEY, V371, P1; KURITA H, 1994, B GEOLOGICAL SURVEY, V479, P67; Kurita Hiroshi, 1995, Palynology, V19, P119; LINDGREN S, 1984, STOCKH CONTRIB GEOL, V39, P145; LYCK JM, 1997, OIL GEOLOGY THERMAL; Mao S., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V120, P307, DOI 10.2973/odp.proc.sr.120.190.1992; MAO S, 1988, LIFE SCI CONTRIBUTIO, V150, P1; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; MAY F E, 1980, Palaeontographica Abteilung B Palaeophytologie, V172, P10; McIntyre DJ, 1999, CAN J EARTH SCI, V36, P769, DOI 10.1139/e98-011; MOSHKOVITZ S, 1993, MICROPALEONTOLOGY, V39, P167, DOI 10.2307/1485838; NohrHansen H, 1997, GEOLOGY, V25, P851, DOI 10.1130/0091-7613(1997)025<0851:PASAAN>2.3.CO;2; NOHRHANSEN H, 1998, NTNU VITENSKAPSMUS B, P119; Owen H.G., 1983, Atlas of continental displacement, 200 million years to the present; Pascher A., 1914, Berlin Ber D bot Ges, V32; SCHRANK E, 1988, REV PALAEOBOT PALYNO, V56, P123, DOI 10.1016/0034-6667(88)90078-4; Smit J, 1996, GEOL MIJNBOUW, V75, P283; Soncini M.-J., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P427; Srivastava SK., 1995, PALEOBOTANIST, V42, P249, DOI DOI 10.54991/JOP.1993.1161; STRONG CP, 1995, NEW ZEAL J GEOL GEOP, V38, P171, DOI 10.1080/00288306.1995.9514649; Wilson G.J., 1987, NZ Geol. Surv. Rec, V20, P8	40	26	26	0	0	TAYLOR & FRANCIS AS	OSLO	KARL JOHANS GATE 5, NO-0154 OSLO, NORWAY	0017-3134	1651-2049		GRANA	Grana		1999	38	2-3					125	133		10.1080/00173139908559221	http://dx.doi.org/10.1080/00173139908559221			9	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences	317LW					2025-03-11	WOS:000087227700007
J	Lebedeva, NK; Nikitenko, BL				Lebedeva, NK; Nikitenko, BL			Dinoflagellate cysts and microforaminifera of the Lower Cretaceous Yatria River section, Subarctic Ural, NW Siberia (Russia). Biostratigraphy, palaeoenvironmental and palaeogeographic discussion	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as			ADJACENT SEAS; SEDIMENTS; NORTH	Rich assemblages of phytoplankton and microforaminifera (foraminifera linings) are found in the marine Lower Cretaceous section from the Yatria River (Subaretic Ural). The Lower Cretaceous (Upper Volgian to Lower Hauterivian) dinocyst and microforaminifera biostratigraphy is calibrated against the ammonite zones. The dinocyst stratigraphy differs from Arctic Canada zonation, except for the Berriasian Paragonyaulacysta? borealis zone, and shows significant similarity with the zonal subdivision of Boreal regions of Europe. The distribution of phytoplankton and microforaminifera is related to relative sea level variations. Consecutive changes of phytoplankton associations (2 in the Berriasian. 2 in the Valanginian-Early Hauterivian, 4 in the Early Hauterivian), lateral zonations of microforaminifera (2 in the Berriasian, 2 in the Valanginian) and their relation to environmental changes in the Lower Cretaceous seas of the Subarctic Ural Basin are established.	Russian Acad Sci, Inst Petr Geol, Siberian Branch, Novosibirsk 630090, 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, Inst Petr Geol, Siberian Branch, Koptug Av 3, Novosibirsk 630090, Russia.		Nikitenko, Boris/S-9028-2017; Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303				[Anonymous], GEOLOGICAL SURVEY CA; ARHUS N, 1990, POLAR RES, V8, P165, DOI 10.1111/j.1751-8369.1990.tb00383.x; ARHUS N, 1986, NORSK GEOLOGISK TIDS, V66, P17; BARSS MS, 1979, GEOL SURV CAN B, V7824; Beisel AL, 1997, GEOL GEOFIZ, V38, P1055; Davey R.J., 1982, GEOL SURV DENMARK, V6, P1; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DAVIES E. H., 1983, GEOL SURV CAN B, V359, P1; Duxbury S., 1977, Palaeontographica Abteilung B Palaeophytologie, V160, P17; Fedorova V. A., 1993, PHANEROZOIC STRATIGR, P172; Fisher M.J., 1980, P 4 INT PAL C LUCHN, V2, P313; Galeotti Simone, 1996, Palaeopelagos, V5, P3; GOLBERT AV, 1972, OPORNY RAZREZ NEOKOM; HAKANSSON E, 1981, Bulletin of the Geological Society of Denmark, V30, P11; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Ilyina V.I., 1988, Palynology in the USSR, P103; Lebedeva NK, 1998, GEOL GEOFIZ+, V39, P799; Leereveld H., 1995, Dinoflagellate cysts from the Lower Cretaceous Rio Argos sucession (SE Spain); MCINTYRE DJ, 1980, GEOL SURV CAN B, V320, P57; Poulsen N.E., 1994, GEOBIOS, V7, P409; Powell A.J., 1992, STRATIGRAPHIC INDEX; Prossl K.F., 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P93; RAWSON PF, 1982, AAPG BULL, V66, P2628; SCHULGINA NJ, 1994, CRETACEOUS RES, V15, P1; SHAHMUNDES VA, 1973, MICROPHYTOFOSSILS OL, P50; STANCLIFFE RPW, 1989, MICROPALEONTOLOGY, V35, P337, DOI 10.2307/1485676; van Helden B.G.T., 1986, Palynology, V10, P181; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WIGGINS VD, 1972, REV PALAEOBOT PALYNO, V14, P297, DOI 10.1016/0034-6667(72)90023-1; Woollam R., 1983, REP I GEOL SCI, V83, P1; ZAKHAROV VA, 1983, JURASSIC PALAEOGEOGR	31	22	22	0	1	TAYLOR & FRANCIS AS	OSLO	CORT ADELERSGT 17, PO BOX 2562, SOLLI, 0202 OSLO, NORWAY	0017-3134			GRANA	Grana		1999	38	2-3					134	143		10.1080/00173139908559222	http://dx.doi.org/10.1080/00173139908559222			10	Plant Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	317LW					2025-03-11	WOS:000087227700008
J	Mao, SZ; Wan, CB; Qiao, XY				Mao, SZ; Wan, CB; Qiao, XY			Cretaceous nonmarine dinoflagellates from northeast China	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as				Nonmarine Cretaceous dinoflagellates were recovered in the last decade from a number of basins in northeastern China, which are mostly oil-bearing. These dinoflagellates show close relationship to the water salinity of palaeoenvironments. Two types of dinoflagellate assemblages may be recognized, one from freshwater to slightly brackish and another from slightly brackish to brackish. The former is characterized by the high dominance of ceratioid cysts, particularly species of Nyktericysta and Vesperopsis whereas the composition of the latter is more varied with gonyaulacoid, peridinioid and ceratioid cysts, and varies with the water salinity. New emendations are proposed to the genera Nyktericysta and Vesperopsis based on new information gained from these nonmarine species and specimens. One new genera Quantouendinium is proposed to accommodate its species formerly placed improperly in Nyktericysta. Detailed descriptions and combinations or special remarks are given to the following species: they are Vesperopsis glabra, V. sanjiangensis, V. jixianensis, Nyktericysta reticulata. N. puyangensis, N. beierensis, N. (Hastodinium). ramuliformis. N. (Hailaera). hailaerensis, N. (Hailaera). nebulosa, Contrangularia reticulata, C. granulata, Quantouendinium dictyophorum, Q. microreticulata, Q. spinosum, Tetrachacysta granulata, T. spinulosa, T. tuberculata and an acritarch Spicadinium akidoton. One new genus Quantouendinium and one new species Vesperopsis yanjiensis are described. The palaeoecology of nonmarine dinoflagellates is discussed based on information gathered from China.	China Univ Geosci, Beijing 100083, Peoples R China	China University of Geosciences	Mao, SZ (通讯作者)，China Univ Geosci, Xueyuan Rd 29, Beijing 100083, Peoples R China.							[Anonymous], 1985, SPOROPOLLENIN DINOFL; Backhouse J., 1988, Geological Survey of Western Australia Bulletin, V135, P1; BACKHOUSE J, 1988, 7TH INT PAL C BRISB, P8; BATTEN D J, 1988, Cretaceous Research, V9, P171, DOI 10.1016/0195-6671(88)90016-X; BATTEN D.J., 1980, 5 INT PALYNOL C ABST, P32; BATTEN DJ, 1985, NEUES JB GEOLOGIE PA, V7, P42437; BINT A N, 1986, Palynology, V10, P135; Davey R.J., 1978, INIT REPS DSDP, V40, P883, DOI [10.2973/dsdp.proc.40.125.1978, DOI 10.2973/DSDP.PROC.40.125.1978]; *E EXPL DEV, 1976, LAT CRET PAL ASS SON; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; GAO R, 1992, ACTA PALAEONTOL SIN, V31, P18; GAO R.Q., 1992, CRETACEOUS NONMARINE; GU ZW, 1984, FOSSILS MIDDLE UPPER, V2; HAO YC, 1986, STRATIGRAPHY; Harding IC, 1995, CRETACEOUS RES, V16, P727, DOI 10.1006/cres.1995.1046; He Cheng-Quan, 1992, Acta Micropalaeontologica Sinica, V9, P183; HE CQ, 1989, EARLY TERTIARY DINOF; JIA B, 1978, EARLY TERTIARY DINOF; LENTIN J, 1998, LENTIN WILLIAMS INDE; LENTIN J, 1988, 6 INT PAL C CALG 198, P94; MAO S, 1995, EARLY TERTIARY TERRI; MAO SZ, 1989, EARTH SCI J CHINA U, V15, P283; MAO SZ, 1997, SEDIMENTARY ENV HYDR, P82; Marshall N.G., 1989, Palynology, V13, P21; PENG LC, 1997, SEDIMENTARY ENV HYDR, P120; Qiao X.-y., 1992, Acta Palaeontologica Sinica, V31, P30; QIAO XY, 1995, PETROLEUM GEOLOGY OI, V14, P19; Qiu Songyu, 1994, Marine Geology & Quaternary Geology (Beijing), V14, P97; SMITH AG, 1977, CAMBRIDGE EARTH SCI; Wan C.B., 1990, Petroleum Geology & Oilfield Development in Daqing, V9, P1, DOI [10.19597/j.issn.1000-3754.1990.03.002, DOI 10.19597/J.ISSN.1000-3754.1990.03.002]; WAN CB, 1994, ACTA PALAEONTOL, V33, P500; WAN CF, 1987, PETROLEUM EXPLORATIO, V6, P32; WAN CF, 1987, PETROLEUM EXPLORATIO, V14, P53; Wan Chuan-Biao, 1995, Acta Micropalaeontologica Sinica, V12, P51; WANG DP, 1994, EVOLUTION HIST SONGL; WANG HZ, 1980, TXB HIST GEOLOGY; WU C, 1997, SEDIMENTOLOGY PETROL; Yu, 1981, OIL GAS GEOLOGY, V2, P254; Zhang M M, 1978, VERTEBRAT PALASIATIC, V16, P229; ZIPPI P, 1988, 7TH INT PAL C BRISB, P189	40	17	19	0	3	TAYLOR & FRANCIS AS	OSLO	CORT ADELERSGT 17, PO BOX 2562, SOLLI, 0202 OSLO, NORWAY	0017-3134			GRANA	Grana		1999	38	2-3					144	161		10.1080/713786923	http://dx.doi.org/10.1080/713786923			18	Plant Sciences	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	317LW					2025-03-11	WOS:000087227700009
J	Targarona, J; Warnaar, J; Boessenkool, KP; Brinkhuis, H; Canals, M				Targarona, J; Warnaar, J; Boessenkool, KP; Brinkhuis, H; Canals, M			Recent dinoflagellate cyst distribution in the North Canary Basin, NW Africa	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as			GYMNODINIUM-CATENATUM GRAHAM; RECENT MARINE-SEDIMENTS; ATLANTIC-OCEAN; ADJACENT SEAS; RED TIDE; PHYTOPLANKTON; EASTERN; COAST; DINOPHYCEAE; AUSTRALIA	The North Canary Basin (NW Africa) falls within a major eastern boundary upwelling system. This part of the coastal upwelling system is seasonal and is characterised by the development of large filaments migrating seawards. Hence. 16 samples from this location were selected to identify an "upwelling signal'' in the composition of the dinoflagellate cyst assemblages. Samples closest to the most intense upwelling cells are dominated by L. machaerophorum and G. catenatum and Protoperidinium spp. These make up the "upwelling signal" characteristic for the system. Moreover, the "upwelling signal" can be advected offshore. with filaments that may extend as far as 300 km. Finally. the finding of cysts from G. catenatum, a toxic dinoflagellate, raises the need for a better understanding of the relationship between its presence and distribution in the region, and the coastal upwelling system.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	Utrecht University	Targarona, J (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		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J	Sarjeant, WAS; Taylor, FJRM				Sarjeant, WAS; Taylor, FJRM			Dinoflagellates, fossil and modern: certain unresolved problems	GRANA			English	Article; Proceedings Paper	6th International Conference on Modern and Fossil Dinoflagellates (DINO 6)	JUN, 1998	TRONDHEIM, NORWAY	Res Council Norway, Amerada Hess Norge AS, Amoco Norway Oil Co, AS Norske Shell, Nordk Hydro Produksjon as, Phillips Petr Co Norway, Saga Petr ASA, Statoil as			RIBOSOMAL-RNA GENE; ALEXANDRIUM-TAMARENSE; GONYAULAX-TAMARENSIS; MARINE-SEDIMENTS; NORTH-SEA; CYSTS; BLOOMS; ATLANTIC; MORPHOGENESIS; DINOPHYCEAE	We identify a variety of areas and topics that have received relatively little attention hitherto or where there are significant residual problems, following earlier researches. Questions of interest both to palaeontologists and neontologists are emphasized. They are presented in the hope of stimulating new researches on themes presently neglected.	Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada	University of Saskatchewan	Sarjeant, WAS (通讯作者)，Univ Saskatchewan, Dept Geol Sci, Saskatoon, SK S7N 5E2, Canada.							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J	Head, MJ; Westphal, H				Head, MJ; Westphal, H			Palynology and paleoenvironments of a Pliocene carbonate platform: The Clino core, Bahamas	JOURNAL OF PALEONTOLOGY			English	Review							DINOFLAGELLATE CYSTS; MARINE-SEDIMENTS; EASTERN ENGLAND; SINGA SECTION; NEOGENE; ATLANTIC; ALLOSTRATIGRAPHY; BIOSTRATIGRAPHY; STRATIGRAPHY; ASSEMBLAGES	Neritic dinoflagellates from periplatform (slope) carbonates of the Clino borehole, located on the western, leeward margin of the Great Bahama Bank, record environmental fluctuations on the platform top. A lower Pliocene interval (3.6-4.2 Ma) contains platform-top sediments shed onto the lower slope when the platform was open and ramplike. Despite this open topography, abundant Polysphaeridium zoharyi indicate the presence of restricted marine environments on the platform top. Terrestrial palynomorphs are rare throughout this interval and imply a mostly or fully submergent platform top. By late Pliocene times (about 2.1-2.3 Ma) the platform had become flat-topped and steep-sided, with the Clino site located on its upper slope. Samples characteristic of sea-level highstands and lowstands were selected for analysis. Polysphaeridium zoharyi is abundant only in lowstand samples and may have thrived in proximity to terrestrial vegetation. In highstand samples Lingulodinium machaerophorum replaces P. zoharyi, perhaps in response to less restricted marine environments on the platform top. This change in assemblages, along with apparent variations in cyst influx, reflects a fluctuating history of currents and salinities over the platform top in the late Pliocene. Upper Pliocene lowstand samples contain anomalously high proportions of terrestrial palynomorphs, allowing the identification of two phases of emergence and vegetation of the platform top. Palynology therefore appears to be a sensitive indicator of short-term (4th-order) sea-level change on carbonate platforms. Dinoflagellate concentrations correlate positively with carbonate compaction, and infer that compacted layers have undergone dissolution of their metastable constituents. Dinoflagellate concentrations therefore can be useful in the often difficult task of assessing compaction and dissolution in fine-grained limestones where other indicators are absent. The following dinoflagellate species are formally proposed: Operculodinium bahamense Head new species, Operculodinium? mega-granum Head new species, and Spiniferites rhizophorus Head new species.	Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada; Forschungszentrum Marine Geowissensch, GEOMAR, D-24148 Kiel, Germany	University of Toronto; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Head, MJ (通讯作者)，Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada.		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Paleontol.	JAN	1999	73	1					1	25						25	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	164YN					2025-03-11	WOS:000078491300001
J	Adachi, M; Kanno, T; Matsubara, T; Nishijima, T; Itakura, S; Yamaguchi, M				Adachi, M; Kanno, T; Matsubara, T; Nishijima, T; Itakura, S; Yamaguchi, M			Promotion of cyst formation in the toxic dinoflagellate <i>Alexandrium</i> (Dinophyceae) by natural bacterial assemblages from Hiroshima Bay, Japan	MARINE ECOLOGY PROGRESS SERIES			English	Article						Alexandrium; dinoflagellate; bacteria; cyst	GONYAULAX-TAMARENSIS; RED-TIDE; BLOOMS; GERMINATION; SEXUALITY; CATENELLA; EXCAVATA; GROWTH	The relationship between the abundance of the toxic marine dinoflagellate Alexandrium tamarense (Lebour) Balech and Alexandrium-cyst-formation-promoting bacteria (Alex-CFPB) was investigated in the water column of Hiroshima Bay (Japan) from 1997 to 1998. Cell density of A. tamar ense increased gradually from February to the middle of April, then peaked at the end of April and blooms declined rapidly in the beginning of May in both years. All seawater fractions collected from 5 m depth, where the density of A. tamarense cells was highest and which also contained the bulk of planktonic bacteria, promoted cyst formation of A. catenella (Whedon and Kofoid) Balech. This promotion was not caused by effects from nutrient Limitation. The number of Alex-CFPB in seawater samples, analyzed by means of the most probable number (MPN) method, increased from the beginning of the Alexandrium bloom and reached 3.60 x 10(3) and 1.00 x 10(3) cells ml(-1) at the peak bloom period at the end of April in 1997 and 1998, respectively. As the blooms declined, the number of Alex-CFPB decreased rapidly to less than 10 cells ml(-1). Alexandrium-cyst-formation-inhibiting bacteria (Alex-CFIB) were not detected. These results show a clear positive correlation between the abundance of A. tamarense and Alex-CFPB during blooms, which suggests that Alex-CFPB play a significant role in the process of encystment and bloom dynamics of Alexandrium in the field.	Kochi Univ, Fac Agr, Lab Aquat Environm Sci, Kochi 7838502, Japan; Fisheries Agcy Japan, Natl Res Inst Fisheries & Environm Seto Inland Se, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Kochi University; Japan Fisheries Research & Education Agency (FRA)	Adachi, M (通讯作者)，Kochi Univ, Fac Agr, Lab Aquat Environm Sci, Kochi 7838502, Japan.	madachi@cc.kochi-u.ac.jp						Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.x; Anderson D. M., 1995, MANUAL HARMFUL MARIN, V33, P229; 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; [Anonymous], 2012, Biometry; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; FUKAMI K, 1991, NIPPON SUISAN GAKK, V57, P2321; 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; Imai Ichiro, 1998, Plankton Biology and Ecology, V45, P19; Imai Ichiro, 1994, Bulletin of Japanese Society of Microbial Ecology, V9, P15; NAGAI S, 1994, FISHERIES SCI, V60, P625, DOI 10.2331/fishsci.60.625; Perez CC, 1998, J PHYCOL, V34, P242, DOI 10.1046/j.1529-8817.1998.340242.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PORTER KG, 1980, LIMNOL OCEANOGR, V25, P943, DOI 10.4319/lo.1980.25.5.0943; Riquelme C.E., 1987, Bulletin of Japanese Society of Microbial Ecology, V2, P29; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; SAKO Y, 1992, BIOSCI BIOTECH BIOCH, V56, P692, DOI 10.1271/bbb.56.692; SAWAYAMA S, 1993, NIPPON SUISAN GAKK, V59, P291; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; Steidinger K.A., 1975, P153; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; WATANABE MM, 1982, RES REP NATL I ENV S, V30, P27; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131; YOSHINAGA I, 1995, FISHERIES SCI, V61, P780, DOI 10.2331/fishsci.61.780	29	32	34	2	11	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630			MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		1999	191						175	185		10.3354/meps191175	http://dx.doi.org/10.3354/meps191175			11	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	280GY		Bronze			2025-03-11	WOS:000085094900016
J	Dickman, M; Zhang, FZ				Dickman, M; Zhang, FZ			Mid-ocean exchange of container vessel ballast water. 2: Effects of vessel type in the transport of diatoms and dinoflagellates from Manzanillo, Mexico, to Hong Kong, China	MARINE ECOLOGY PROGRESS SERIES			English	Article						ballast water; efficiency of open ocean exchange; non-indigenous species; harmful species; diatoms; dinoflagellates; Manzanillo, Mexico; Hong Kong, China	MARINE ORGANISMS; SHIPS; DISPERSAL	Plankton samples were collected from 4 container ships which took on ballast water in Manzanillo, Mexico, and discharged it 21 d later in Hong Kong, China. As expected, the lack of light during transport in ballast tanks was inimical to the survival of many autotrophic (phytoplankton) species. After 21 d at sea, few of the dinoflagellate and diatom species taken on in Manzanillo Harbour were alive in the ballast water delivered to Hong Kong. In addition, 5 ships from Manzanillo which reballasted with open ocean water were sampled. To assess the effectiveness of mid-ocean exchange, the mean number of diatoms and dinoflagellates in the coastal ballast water (838 cells l(-1)) was compared with the number in the open ocean ballast water (436 cells l(-1)) delivered to Hong Kong. Open ocean exchange of ballast water (reballasting) was 48 % effective in reducing diatom and dinoflagellate abundance. When we compared the Manzanillo study with our previous study of ships from Oakland, California, we concluded that the older container ships such as those coming from Manzanillo were not as effective in getting rid of diatom and dinoflagellate species as the newer container ships. This is probably because the reballasting design of the older ships is not as efficient in removing the water and sediments located near the bottom of the ballast tanks. This bottom water is associated with a large number of resting cysts and cells.	Univ Hong Kong, Dept Ecol & Biodivers, Hong Kong, Peoples R China	University of Hong Kong	Univ Hong Kong, Dept Ecol & Biodivers, Hong Kong, Peoples R China.	dickman@hkusua.hku.hk						[Anonymous], 1991, AQUACULTURISTS GUIDE; BELL GR, 1961, NATURE, V192, P279, DOI 10.1038/192279b0; CARLTON JT, 1993, SCIENCE, V261, P78, DOI 10.1126/science.261.5117.78; Carlton JT, 1996, BIOL CONSERV, V78, P97, DOI 10.1016/0006-3207(96)00020-1; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; Chu KH, 1997, HYDROBIOLOGIA, V352, P201, DOI 10.1023/A:1003067105577; Cohen A. 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R., 1996, Identification Marine Diatoms and Dinoflagellates; VILLAC MC, 1993, HYDROBIOLOGIA, V269, P213, DOI 10.1007/BF00028020; WILLIAMS RJ, 1988, ESTUAR COAST SHELF S, V26, P409, DOI 10.1016/0272-7714(88)90021-2; Yamaji, 1984, ILLUSTRATIONS MARINE; Yoshida M., 1996, HARMFUL TOXIC ALGAL, P205; Zhang FZ, 1999, MAR ECOL PROG SER, V176, P243, DOI 10.3354/meps176243	46	63	75	4	18	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0171-8630	1616-1599		MAR ECOL PROG SER	Mar. Ecol.-Prog. Ser.		1999	176						253	262		10.3354/meps176253	http://dx.doi.org/10.3354/meps176253			10	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	172HV		Bronze, Green Submitted			2025-03-11	WOS:000078918200022
J	Aksu, AE; Abrajano, T; Mudie, PJ; Yasar, D				Aksu, AE; Abrajano, T; Mudie, PJ; Yasar, D			Organic geochemical and palynological evidence for terrigenous origin of the organic matter in Aegean Sea sapropel S1	MARINE GEOLOGY			English	Article						sapropel S1; Aegean Sea; fatty acids; n-alkanes; palynology	EASTERN MEDITERRANEAN SAPROPELS; BANNOCK BASIN; SEDIMENTS; PRODUCTIVITY; MINERALOGY; INSOLATION; EVOLUTION; CLIMATE; MONSOON; RECORD	Organic geochemistry and micropaleontology are used to determine the origin of sapropel S1 in the Aegean Sea. Low-molecular-weight (C-15, C-17 and C-19) n-alkane data show that net primary productivity (NPP) increased from similar to 14,000 to 10,000 yr BP at the glacial interglacial transition, but the onset of S1 at 9600 yr BP marks a sharp decline in NPP, which remained low until similar to 8200 yr BP. The start of sapropel deposition is marked by increased total organic carbon (TOC) and pollen-spore concentrations, together with increased high-molecular-weight (C-27, C-29, C-31 and C-33) n-alkanes. Pollen assemblages show large influx of tree pollen from central-northern European forests. Increases in high-molecular-weight n-alkanes suggest greater influx of fresh vascular plant material at the start of S1, although the amount is small compared to other insoluble organic matter. Palynological studies showed that most of this insoluble organic matter are flocks of dark-brown amorphous kerogen, typical of terrigenous humic compounds. From similar to 8200 yr BP to the top of S1 at similar to 6400 yr BP, there is a decline in high-molecular-weight n-alkanes and terrigenous kerogen, and an increase in low-molecular-weight n-alkanes, suggesting that NPP recovered during the later deposition of S1 in the Aegean Sea. The increase in low-molecular-weight n-alkanes coincides with the recovery of coccolithophores and dinoflagellates, suggesting that these phytoplankton are primarily responsible for the low-molecular-weight n-alkane variations. These data from the Aegean Sea support the model for sapropel deposition resulting from increased influx of TOC during times of stagnant bottom water, but disagree with Mediterranean models prescribing a large increase in marine productivity. (C) 1999 Elsevier Science B.V. All rights reserved.	Mem Univ Newfoundland, Ctr Earth Resources Res, Dept Earth Sci, St Johns, NF A1B 3X5, Canada; Geol Survey Canada, Bedford Inst Oceanog, Atlantic Geosci Ctr, Dartmouth, NS B2Y 4A2, Canada; Dokuz Eylul Univ, Inst Marine Sci & Technol, TR-35340 Izmir, Turkey	Memorial University Newfoundland; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; Dokuz Eylul University	Aksu, AE (通讯作者)，Mem Univ Newfoundland, Ctr Earth Resources Res, Dept Earth Sci, St Johns, NF A1B 3X5, Canada.	aaksu@sparky2.esa.mun.ca	Yasar, Dogan/AAC-1866-2020					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; AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; [Anonymous], NATO ASI SERIES C; BROOKS J, 1978, ENV BIOCH GEOMICROBI, V1, P287; CALDER JOHN A., 1968, ENVIRON SCI TECHNOL, V2, P535, DOI 10.1021/es60019a001; Calvert S.E., 1992, PRODUCTIVITY ACCUMUL, P231; CALVERT SE, 1993, MAR GEOL, V113, P67, DOI 10.1016/0025-3227(93)90150-T; CALVERT SE, 1983, MEDITERRANEAN OCEANO, V6, P225; CALVERT SE, 1990, FACETS MODERN BIOGEO, P329; CASTRADORI D, 1993, PALEOCEANOGRAPHY, V8, P459, DOI 10.1029/93PA00756; CHEDDADI R, 1991, MAR GEOL, V100, P53, DOI 10.1016/0025-3227(91)90224-R; CITA MB, 1977, QUATERNARY RES, V8, P205, DOI 10.1016/0033-5894(77)90046-1; COMBAZ A., 1980, KEROGEN INSOLUBLE OR, P55; CRAMP A, 1988, PALAEOGEOGR PALAEOCL, V68, P61, DOI 10.1016/0031-0182(88)90017-X; Deines P., 1980, Handbook of environmental isotope geochemistry, P329, DOI [DOI 10.1016/B978-0-444-41780-0.50015-8, 10.1016/B978-0-444-41780-0.50015-8]; Eglinton G., 1963, CHEM PLANT TAXONOMY, P187; FONTUGNE M, 1978, EARTH PLANET SC LETT, V41, P365, DOI 10.1016/0012-821X(78)90191-7; Fontugne MR, 1992, PALEOCEANOGRAPHY, V7, P1, DOI 10.1029/91PA02674; FONTUGNE MR, 1983, THESIS U PARIS; HADDAD RI, 1992, ORG GEOCHEM, V19, P205, DOI 10.1016/0146-6380(92)90037-X; HOWELL MW, 1992, MAR GEOL, V103, P461, DOI 10.1016/0025-3227(92)90032-D; Intergovernmental Oceanographic Commission (IOC), 1981, INT BATH CHART MED; KELLER J, 1978, GEOL SOC AM BULL, V89, P591, DOI 10.1130/0016-7606(1978)89<591:EVAITM>2.0.CO;2; MEYERS PA, 1993, ORG GEOCHEM, V20, P867, DOI 10.1016/0146-6380(93)90100-P; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; NINKOVICH D, 1965, COLSTON RES SOC SUBM, P413; OLAUSSON E, 1961, STUDIES DEEP SEA COR, V8, P323; PICHLER H, 1976, NATURE, V262, P373, DOI 10.1038/262373a0; RAU GH, 1989, NATURE, V341, P516, DOI 10.1038/341516a0; RICHARDSON D, 1976, GEOL SOC AM BULL, V87, P110, DOI 10.1130/0016-7606(1976)87<110:UOKRZA>2.0.CO;2; ROHLING EJ, 1991, GEOL MIJNBOUW, V70, P253; ROSSIGNOLSTRICK M, 1983, NATURE, V304, P46, DOI 10.1038/304046a0; ROSSIGNOLSTRICK M, 1985, PALAEOGEOGR PALAEOCL, V49, P237, DOI 10.1016/0031-0182(85)90056-2; RYAN WBF, 1972, MEDITERRANEAN SEA NA, P149; SANCETTA C, 1994, PALEOCEANOGRAPHY, V9, P195, DOI 10.1029/94PA00090; SMITH DJ, 1986, PHILOS T R SOC LON A, V31, P375; SUTHERLAND HE, 1984, MAR GEOL, V56, P79, DOI 10.1016/0025-3227(84)90007-0; TENHAVEN HL, 1987, GEOCHIM COSMOCHIM AC, V51, P803; THUNELL RC, 1984, MAR GEOL, V59, P105, DOI 10.1016/0025-3227(84)90090-2; Tissot B.P., 1978, PETROLEUM FORMATION, DOI DOI 10.1007/978-3-642-96446-6; VERGNAUDGRAZZIN.C, 1986, MAR MICROPALEONTOL, V10, P35; WILLIAMS DF, 1978, SCIENCE, V201, P252, DOI 10.1126/science.201.4352.252; Zonneveld KAF, 1997, QUATERNARY SCI REV, V16, P187, DOI 10.1016/S0277-3791(96)00049-2	44	45	45	0	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0025-3227			MAR GEOL	Mar. Geol.	JAN	1999	153	1-4					303	318		10.1016/S0025-3227(98)00077-2	http://dx.doi.org/10.1016/S0025-3227(98)00077-2			16	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	152GY					2025-03-11	WOS:000077769400021
C	Srivastava, V; Msaky, E		Heine, K; Scott, L; Cadman, A; Verhoeven, R		Srivastava, V; Msaky, E			Albian-Cenomanian microfloral assemblages from Coastal Tanzania	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS, VOL. 26	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS		English	Proceedings Paper	3rd Conference on African Palynology	SEP 14-19, 1997	WITWATERSAND UNIV, JOHANNESBURG, SOUTH AFRICA	Int Assoc African Palynol	WITWATERSAND UNIV			Well preserved and diverse assemblages of dinoflagellate cysts and sporomorphs, recovered from Albian-Cenomanian sediments of coastal Tanzania, include stratigraphically important dinocyst species: Dinopterygium tuberculatum Litosphaeridium arundum, Litosphaeridium conispinusum,Litosphaeridium siphoniphorum, Odontochitina operculata, Oligosphaeridium pulcherrimum, Palaeohystrichophora infusorioides, Polysphaeridium pumilum, Systematophora cretacea and several Florentinia species. The Pteridophytic spore taxa Crybelosporites pannuceus and Zlivisporites blanensis are important components of most samples. Elaterosporites klaszii which its youngest occurrence in the early Cenomanian and Elaterosporites protensus in the Albian are recorded for the first time from Cretaceous sediments in Tanzania. Gymnosperm pollen include Classopollis brasiliensis, Classopollis spinosus, Callialasporites trilobatus, Ephedripites barghoornii and Ephedripites jansonii. Angiosperm pollen are represented by Tricolpites sp. and Tricolpopollenites sp. Microthyriaceae and other fungi are also present.	Univ Dar Es Salaam, Dar Es Salaam, Tanzania	University of Dar es Salaam	Srivastava, V (通讯作者)，Univ Dar Es Salaam, POB 35060, Dar Es Salaam, Tanzania.							Aurisano R.W., 1989, Palynology, V13, P143; BARSS MS, 1973, 73 GEOL SURV CAN; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Brasil do, B TEC PETROBRAS, V17, P263; CLARKE JL, 1984, PALYNOLOGY, V8, P165; DAVEY RJ, 1976, REV PALAEOBOT PALYNO, V22, P307, DOI 10.1016/0034-6667(76)90028-2; DAVEY RJ, 1982, 6 GEOL SURV DENM B; HERNGREEN G F W, 1981, Pollen et Spores, V23, P441; HERNGREEN GFW, 1982, MICROPALEONTOLOGY, V28, P97, DOI 10.2307/1485364; Jain K.P., 1975, Geophytology, V5, P126; 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]; KENT PE, 1961, I GEOL SCI LONDON GE, V6, P1; Lentin J.K., 1993, A.S.S.P., V28, P1; MSAKY E, 1997, IN PRESS P 2 TANZ GE; MSAKY E, 1995, IN PRESS TANZANIA J; QUENNEL AM, 1956, MEMOIR, V1, P1; Regali M., 1974, B TEC PETROBRAS, V17, P177; SRIVASTAVA S K, 1981, Palynology, V5, P1; Srivastava SK., 1975, Paleobiologie Continentale, V6, P1; SRIVASTAVA V, 1994, PALYNOLOGY, V30, P35; STOVER LE, 1961, MICROPALEONTOLOGY, V9, P85; Thusu B., 1985, Journal of Micropalaeontology, V4, P131; Verdier J.-P., 1975, Revue Micropaleont, V17, P191	24	3	3	0	1	A A BALKEMA PUBLISHERS	LEIDEN	SCHIPHOLWEG 107C, PO BOX 447, 2316 XC LEIDEN, NETHERLANDS	0168-6208		90-5410-476-7	PALAEOECO A			1999	26						31	+						13	Plant Sciences; Ecology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Environmental Sciences & Ecology; Paleontology	BP04K					2025-03-11	WOS:000084109100003
C	Dunay, RE; Brenac, PAR; Edwards, PG		Heine, K; Scott, L; Cadman, A; Verhoeven, R		Dunay, RE; Brenac, PAR; Edwards, PG			Palynology and micropalaeontology of the Messinian-Zanclean sequences offshore Equatorial Guinea	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS, VOL. 26	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS		English	Proceedings Paper	3rd Conference on African Palynology	SEP 14-19, 1997	WITWATERSAND UNIV, JOHANNESBURG, SOUTH AFRICA	Int Assoc African Palynol	WITWATERSAND UNIV		VEGETATION; PALEOENVIRONMENTS; CAMEROON; PLIOCENE; POLLEN	The Early Pliocene (Zanclean) to latest Miocene (late Messinian) sequence in Mobil/UMC Block B offshore Equatorial Guinea is defined by the appearance (last downhole occurrence, or LDO) of Podocarpus milanjianus, and the first downhole occurrence (FDO) of typical lower Pliocene/upper Miocene foraminifera. The reservoir horizons, which occur in the lower portion of this sequence, contain palynofloral assemblages characterised by abundant Pediastrum, common Botryococcus braunii and Gramineae as well as charred Gramineae cuticle. Rhizophora mangrove is poorly represented and marine dinocysts virtually absent. Deep marine foraminifera occur in discrete horizons. Gramineae maxima and common charred Gramineae cuticle suggest extension of savannahs and reflect a strongly seasonal, relatively dry and warm climate. This climatic shift is most likely associated with the latest Miocene (Messinian) worldwide sea level drop and associated aridity event, the so-called 'Messinian crisis'. The abundance of Pediastrum taxa is interpreted as a freshwater transport signal in the sequence. This signal indicates the occurrence of intermittent lacustrine environments which are contemporaneous with incisement and erosion of the continental shelf during this lowstand period at the Mio-Pliocene boundary. Subsequent transport and redeposition into a deeper marine setting occurred at the continental shelf palaeoslope surface, the sediments probably bypassing the upper reaches of the continental slope. The strong freshwater transport seaward probably occurred during the short, rainy season or during short, very erosive, humid cycles of this seasonal climate. Calcareous and agglutinated benthic foraminifera are rare and restricted to encapsulating bathyal marine shale horizons and confirm that the entire sedimentary package was deposited in slope or upper bathyal water depths. The biostratigraphic interpretation of the reservoir packages indicates destabilisation and mobilisation of nearshore sediments in response to high accomodation space which occurred immediately after Messinian canyon cutting on the continental slope. These sediments were deposited in continental slope settings as debris flows or turbidites. The overlying mudstone sequence, which constitutes the reservoir topseal, is characterised by significant increase of Rhizophora and the presence of common dinoflagellate cysts. This is interpreted as the landward development of mangrove under consistently humid conditions and increased sea levels.	Mobil N Sea Ltd, London WC2A 2EB, England	Exxon Mobil Corporation	Dunay, RE (通讯作者)，Mobil N Sea Ltd, 3 Clements Inn, London WC2A 2EB, England.							BESEMS R.E., 1993, GEOL SOC MALAYSIA B, V33, P65, DOI DOI 10.7186/BGSM33199306; Blow W.H., 1979, CAINOZOIC GLOBIGERIN; BLOW WH, 1969, 1ST P INT C PLANKT M, V1, P199; Brenac P., 1988, TRAVAUX SECTION SCI, V25, P91; GIRESSE P, 1994, PALAEOGEOGR PALAEOCL, V107, P65, DOI 10.1016/0031-0182(94)90165-1; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; LEROY S, 1994, PALAEOGEOGR PALAEOCL, V109, P295, DOI 10.1016/0031-0182(94)90181-3; Maley J, 1998, REV PALAEOBOT PALYNO, V99, P157, DOI 10.1016/S0034-6667(97)00047-X; MORLEY RJ, 1993, REV PALAEOBOT PALYNO, V77, P119, DOI 10.1016/0034-6667(93)90060-8; Poumot C., 1989, Centres for Research Exploration Production Elf Aquitaine, V13, P437; Thompson RS, 1996, MAR MICROPALEONTOL, V27, P27, DOI 10.1016/0377-8398(95)00051-8	11	0	0	0	1	A A BALKEMA PUBLISHERS	LEIDEN	SCHIPHOLWEG 107C, PO BOX 447, 2316 XC LEIDEN, NETHERLANDS	0168-6208		90-5410-476-7	PALAEOECO A			1999	26						45	57						13	Plant Sciences; Ecology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Environmental Sciences & Ecology; Paleontology	BP04K					2025-03-11	WOS:000084109100004
C	Dupont, L; Schneider, R; Schmüser, A; Jahns, S		Heine, K; Scott, L; Cadman, A; Verhoeven, R		Dupont, L; Schneider, R; Schmüser, A; Jahns, S			Marine-terrestrial interaction of climate changes in West Equatorial Africa of the last 190,000 years	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS, VOL. 26	PALAEOECOLOGY OF AFRICA AND THE SURROUNDING ISLANDS		English	Proceedings Paper	3rd Conference on African Palynology	SEP 14-19, 1997	WITWATERSAND UNIV, JOHANNESBURG, SOUTH AFRICA	Int Assoc African Palynol	WITWATERSAND UNIV		DINOFLAGELLATE CYSTS; ATLANTIC-OCEAN; SOUTH-ATLANTIC; ANGOLA BASIN; VEGETATION HISTORY; LATE PLEISTOCENE; ADJACENT SEAS; CONGO FAN; SEDIMENTS; PRODUCTIVITY	Palynological investigation of a marine piston core GeoB 1008-3 (6 degrees 35'S/10 degrees 19'E) from the highly productive area off the Congo fan provides a dinoflagellate cyst record reflecting marine surface water conditions during the last 190 ka and a pollen record of the vegetation changes in Central Africa induced by climatic fluctuations for the same period. The freshwater discharge of the Congo river is related to the intensity of the West African monsoon. During warmer and more humid phases, dinoflagellate cyst flux decreased in relation to lower productivity and increased freshwater input in the eastern South Atlantic. At the same time on the continent, the rain forest expanded. During the cooler interstadials of Stage 5, the Afromontane forest represented by Podocarpus pollen expanded to lower altitudes and occupied former areas of rain forest during periods showing intermediate levels for sea surface temperatures and river discharge. During the colder and more arid phases of glacial Stages 6 and 2, when freshwater run-off into the Gulf of Guinea decreased, dinoflagellate cysts were much more abundant. However, Stage 4 shows high levels of river discharge and a moderate dinoflagellate cyst flux coupled to low sea-surface temperatures of the eastern South Atlantic, while Stage 3 shows moderately high pollen percentages of the rain forest during phases with fluctuating fresh-water discharge and very low sea-surface temperatures. High sea levels at the beginning of the Last Interglacial and the Holocene favoured the expansion of mangroves.	Univ Bremen, D-28334 Bremen, Germany	University of Bremen	Dupont, L (通讯作者)，Univ Bremen, POB 330440, D-28334 Bremen, Germany.	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Afr. Surround. Isl.		1999	26						61	84						24	Plant Sciences; Ecology; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Plant Sciences; Environmental Sciences & Ecology; Paleontology	BP04K					2025-03-11	WOS:000084109100005
C	Benoit, E; Mattei, C; Legrand, AM; Molgó, J		Seret, B; Sire, JY		Benoit, E; Mattei, C; Legrand, AM; Molgó, J			Ionic basis of the neurocellular actions of pacific ciguatoxins implicated in ciguatera fish poisoning	PROCEEDINGS OF THE 5TH INDO-PACIFIC FISH CONFERENCE			English	Proceedings Paper	5th Indo-Pacific Fish Conference	NOV 03-08, 1997	NOUMEA, NEW CALEDONIA	French Soc Ichthyol Soc		ciguatera fish poisoning; ciguatoxins; D-mannitol; myelinated axone; motor nerve terminals; neuroblastoma cells; synaptosomes; electrophysiology; confocal laser scanning microscopy; action potential; voltage-dependent Na+ channels; Na+-Ca2+ exchange; intra-cellular Ca2+; cellular volume	DINOFLAGELLATE GAMBIERDISCUS-TOXICUS; TORPEDO CHOLINERGIC SYNAPTOSOMES; SENSITIVE SODIUM-CHANNELS; MOTOR-NERVE TERMINALS; BRAIN SYNAPTONEUROSOMES; ACETYLCHOLINE-RELEASE; GYMNOTHORAX-JAVANICUS; CALCIUM MOBILIZATION; MOLECULAR-STRUCTURE; RECEPTOR-SITE	Ciguatoxins are responsible for a human seafood poisoning named ciguatera, a disease linked to the benthic dinoflagellate Gambierdiscus toxicus and acquired by eating certain contaminated fish species. These toxins are complex, lipid-soluble, cyclic polyethers which bind with high affinity to a specific receptor site of the neuronal, voltage-sensitive Na+ channel-protein. Pharmacological studies reveal that ciguatoxins increase Na+ permeability of various excitable cell membranes, notably at the resting membrane potential. This action is attributed to modification of Na+ channels, which then remain permanently open. As a consequence, ciguatoxins evoke membrane depolarization, cause spontaneous and/or repetitive action potentials, and influence Na+-Ca2+ exchange in nerve membranes. Moreover, they induce mobilization of intracellular Ca2+ in nerve cells. Finally, ciguatoxins produce swelling of nerve cells due to continuous Na+ entry through toxin-opened Na+ channels, which induces an increase in intracellular Na+ concentration and an influx of water. These latter effects are prevented by blocking voltage-dependent Na+ channels and are reversed by hyperosmolar external solutions containing, in particular, D-mannitol. In conclusion, these neurocellular actions may explain some of the human neurological alterations induced by ciguatoxins and the efficacy of D-mannitol used as a clinical treatment of ciguatera.	CNRS, Neurobiol Cellulaire & Mol Lab, UPR 9040, F-91198 Gif Sur Yvette, France	Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS)	CNRS, Neurobiol Cellulaire & Mol Lab, UPR 9040, Bat 32-33,1 Ave Terrasse, F-91198 Gif Sur Yvette, France.	benoit@wat.nbcm.cnrs-gif.fr						ADACHI R, 1979, B JPN SOC SCI FISH, V45, P67; ALLSOP JL, 1986, REV NEUROL-FRANCE, V142, P590; ANDERSON DM, 1987, BIOL BULL, V172, P89, DOI 10.2307/1541609; BADEN DG, 1989, FASEB J, V3, P1807, DOI 10.1096/fasebj.3.7.2565840; BAGNIS R, 1977, CR ACAD SCI D NAT, V285, P105; Benoit E, 1996, NEUROSCIENCE, V71, P1121, DOI 10.1016/0306-4522(95)00506-4; Benoit E, 1992, Bull Soc Pathol Exot, V85, P497; BENOIT E, 1986, TOXICON, V24, P357, DOI 10.1016/0041-0101(86)90195-9; Benoit Evelyne, 1994, Memoirs of the Queensland Museum, V34, P461; BIDARD JN, 1984, J BIOL CHEM, V259, P8353; Blythe D G, 1992, Bull Soc Pathol Exot, V85, P425; CAMERON J, 1991, J NEUROL SCI, V101, P93, DOI 10.1016/0022-510X(91)90022-Y; CAMERON J, 1991, J NEUROL SCI, V101, P87, DOI 10.1016/0022-510X(91)90021-X; Carrasco MA, 1996, NEUROCHEM INT, V29, P637, DOI 10.1016/S0197-0186(96)00046-0; CATTERALL WA, 1992, PHYSIOL REV, V72, pS15, DOI 10.1152/physrev.1992.72.suppl_4.S15; DAVIS CC, 1948, BOT GAZ, V109, P358, DOI 10.1086/335488; FLOWERS AE, 1988, PROGR VENOM TOXIN RE, P411; GAWLEY RE, 1992, TOXICON, V30, P780, DOI 10.1016/0041-0101(92)90014-V; GILLESPIE NC, 1986, MED J AUSTRALIA, V145, P584, DOI 10.5694/j.1326-5377.1986.tb139504.x; GLAZIOU P, 1994, TOXICON, V32, P863, DOI 10.1016/0041-0101(94)90365-4; Gordon D, 1990, CURR OPIN CELL BIOL, V2, P695, DOI 10.1016/0955-0674(90)90113-S; GUSOVSKY F, 1987, MOL PHARMACOL, V32, P479; GUSOVSKY F, 1986, P NATL ACAD SCI USA, V83, P3003, DOI 10.1073/pnas.83.9.3003; HENZI V, 1992, NEUROSCIENCE, V46, P251, DOI 10.1016/0306-4522(92)90049-8; HERMONI M, 1987, ISRAEL J MED SCI, V23, P44; HOLMES MJ, 1991, TOXICON, V29, P761, DOI 10.1016/0041-0101(91)90068-3; KOSTYUK P, 1994, NEUROSCIENCE, V63, P381, DOI 10.1016/0306-4522(94)90537-1; Laurent D, 1993, GRATTE CIGUATERA REM; Legrand AM, 1989, J APPL PHYCOL, V1, P183, DOI 10.1007/BF00003882; LEGRAND AM, 1992, PROCEEDINGS OF THE THIRD INTERNATIONAL CONFERENCE ON CIGUATERA FISH POISONING, P25; LEWIS RJ, 1993, COMP BIOCHEM PHYS C, V106, P615, DOI 10.1016/0742-8413(93)90217-9; LEWIS RJ, 1992, TOXICON, V30, P915, DOI 10.1016/0041-0101(92)90390-Q; LEWIS RJ, 1991, TOXICON, V29, P1115, DOI 10.1016/0041-0101(91)90209-A; LOMBET A, 1987, FEBS LETT, V219, P355, DOI 10.1016/0014-5793(87)80252-1; Mattei C, 1997, NEUROSCI LETT, V234, P75, DOI 10.1016/S0304-3940(97)00665-4; MCDONOUGH PM, 1988, MOL PHARMACOL, V33, P310; MOLGO J, 1991, ANN NY ACAD SCI, V635, P485, DOI 10.1111/j.1749-6632.1991.tb36535.x; MOLGO J, 1990, BRIT J PHARMACOL, V99, P695, DOI 10.1111/j.1476-5381.1990.tb12991.x; MOLGO J, 1993, NEUROSCI LETT, V160, P65, DOI 10.1016/0304-3940(93)9000-4; Molgo J, 1992, Bull Soc Pathol Exot, V85, P486; MOLGO J, 1993, NEUROSCI LETT, V158, P147, DOI 10.1016/0304-3940(93)90250-O; MOLGO J, 1998, P 8 INT C HARMF ALG, P594; Molgo J., 1992, METHODS NEUROSCIENCE, V8, P149; Molgo Jordi, 1994, Memoirs of the Queensland Museum, V34, P577; MOROTGAUDRYTALA.Y, 1996, ANN NY ACAD SCI, V779, P404; MURATA M, 1989, J AM CHEM SOC, V111, P8929, DOI 10.1021/ja00206a032; MURATA M, 1990, J AM CHEM SOC, V112, P4380, DOI 10.1021/ja00167a040; PALAFOX NA, 1988, JAMA-J AM MED ASSOC, V259, P2740, DOI 10.1001/jama.259.18.2740; PAUILLAC S, 1995, HARMFUL MARINE ALGAL, P801; PEARN JH, 1989, MED J AUSTRALIA, V151, P77, DOI 10.5694/j.1326-5377.1989.tb101165.x; POLI MA, 1986, MOL PHARMACOL, V30, P129; RUSSELL FE, 1991, J TOXICOL-TOXIN REV, V10, P37, DOI 10.3109/15569549109058575; SCHEUER PJ, 1967, SCIENCE, V155, P1267, DOI 10.1126/science.155.3767.1267; SCHEUER PJ, 1994, TETRAHEDRON, V50, P3, DOI 10.1016/S0040-4020(01)80733-X; SHARKEY RG, 1987, MOL PHARMACOL, V31, P273; SWIFT AEB, 1993, J TOXICOL-CLIN TOXIC, V31, P1, DOI 10.3109/15563659309000371; TACHIBANA K, 1987, BIOL BULL-US, V172, P122, DOI 10.2307/1541611; TRAINER VL, 1994, J BIOL CHEM, V269, P19904; Vernoux JP, 1997, TOXICON, V35, P889, DOI 10.1016/S0041-0101(96)00191-2; YANO K, 1984, J BIOL CHEM, V259, P201; YASUMOTO T, 1977, B JPN SOC SCI FISH, V43, P1021, DOI 10.2331/suisan.43.1021; YASUMOTO T, 1993, CHEM REV, V93, P1897, DOI 10.1021/cr00021a011	62	0	0	0	2	SOCIETE FRANCAISE ICHTYOLOGIE	PARIS	43 RUE CUVIER, 75231 PARIS, CEDEX 05, FRANCE			2-9507330-5-0				1999							745	758						14	Ecology; Fisheries; Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S)	Environmental Sciences & Ecology; Fisheries; Marine & Freshwater Biology	BP33Q					2025-03-11	WOS:000084731300067
C	Lange, CB; Schimmelmann, A; Yasuda, MK; Berger, WH		Rose, MR; Wigand, PE		Lange, CB; Schimmelmann, A; Yasuda, MK; Berger, WH			Paleo climatic significance of marine varves off Southern California	PROCEEDINGS OF THE SOUTHERN CALIFORNIA CLIMATE SYMPOSIUM TRENDS AND EXTREMES OF THE PAST 2000 YEARS	TECHNICAL REPORTS-NATURAL HISTORY MUSEUM OF LOS ANGELES COUNTY-SERIES		English	Proceedings Paper	Southern California Climate Symposium on Trends and Extremes of the Past 2000 Years	OCT   25, 1991	LOS ANGELES, CA	Univ Nevada, Desert Res Inst, Nat Hist Museum Los Angeles Cty, So Calif Edison Co, Environm Affairs Div			SANTA-BARBARA-BASIN; OXYGEN-MINIMUM ZONE; EL-NINO EVENTS; LAST 8000 YEARS; CONTINENTAL BORDERLAND; SEDIMENT-TRAP; PEDRO BASINS; ORGANIC-CARBON; MONICA BASIN; MOLECULAR STRATIGRAPHY	Marine varves are discrete seasonal to annual laminations of accumulating sediment preserved in oxygen-depleted depositional environments. Each increment of deposition is a witness to the conditions of the environment. For example, the thickness of varves reflects precipitation, with wet years increasing river runoff and supplying more detritus to the accumulating sediment offshore. Dendrochronologic records of precipitation-sensitive trees can be correlated with depth-series of varve thickness. Unlike tree-rings, varves express a much larger variety of paleoclimatically significant parameters, i.e. physical (thickness, color, X-ray permeability), biological (coccoliths, diatoms, silicoflagellates, dinoflagellate cysts, radiolaria, foraminifera, ptero-pods, fish debris), and geochemical parameters (bulle organic and inorganic compositions, stable isotope ratios, molecular biomarkers). This study reviews the many multidisciplinary efforts that describe the marine varve records off Southern California. The main focus is on the Santa Barbara Basin with its excellent varve record that extends several thousand years into the past, but work that has been done in adjacent areas with varved records is also summarized. For the first time, a comprehensive, detailed varve chronology encompassing the period A.D. 1400-1987 from the Santa Barbara Basin, which includes an X-radiographic overview of all varved and non-varved intervals, together with correlated high-resolution porosity profiles is presented. Long-term and short-term variability in the basin in relationship to changes in the northeastern Pacific oceanographic circulation is reported. Microfossil and geochemical evidence of El Nino events is also included.	Univ Calif San Diego, Scripps Inst Oceanog, Geosci Res Div, La Jolla, CA 92093 USA	University of California System; University of California San Diego; Scripps Institution of Oceanography			Lange, Carina/AHC-2015-2022					ANDERSON RY, 1987, QUATERNARY RES, V28, P307, DOI 10.1016/0033-5894(87)90069-X; ANDERSON RY, 1990, INTERAGENCY ECOLOGIC, V23, P77; ANDERSON RY, 1989, GEOPHYS MONOGR SER, V55, P75; ANGEL MV, 1992, PROGR OCEANOGRAPHY, V30; [Anonymous], 1956, DENDROCLIMATIC CHANG; [Anonymous], [No title captured]; [Anonymous], 2021, ICE Age-Outs, DOI 10.4324/9780203505205; [Anonymous], P OC DRILL PROGR S 2; [Anonymous], 1984, Milankovitch and climate: understanding the response to astronomical forcing; [Anonymous], CALIFORNIA COOPERATI; ARENDS RG, 1980, PACIFIC COAST PALEOG, V4, P313; ARENDS RG, 1986, SILICEOUS MICROFOSSI, P39; AUBRY MP, 1982, INITIAL REP DEEP SEA, V64, P955; Bandy O. 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J	Palliani, RB; Mattioli, E				Palliani, RB; Mattioli, E			High resolution integrated microbiostratigraphy of the Lower Jurassic (late Pliensbachian early Toarcian) of central Italy	JOURNAL OF MICROPALAEONTOLOGY			English	Article								The integrated use of calcareous nannofossil and dinoflagellate cyst events in a study of the late Pliensbachian-early Toarcian interval in central Italy has yielded a high resolution biostratigraphy. The use of both the first and last occurrences of selected taxa belonging to the two phytoplankton groups allows the dating of the sediments with a very refined detail, even when lithologies are unfavourable to the preservation of one fossil group. The evolutionary history of calcareous nannofossils and dinoflagellate cysts during the early Jurassic and its links with global events are responsible for the high potential of this integrated biostratigraphy.	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy	University of Perugia	Univ Perugia, Dept Earth Sci, I-06100 Perugia, Italy.		Mattioli, Emanuela/D-7951-2012					Arkell W.J., 1956, Monograph of the Palaeontographical Society; Baldanza Angela, 1996, Palaeopelagos, V5, P161; BARTOLINI A, 1996, SEPM IAS RES C ARB G, P19; BOWN PR, 1988, NEWSL STRATIGR, V20, P91; Bown PR, 1996, GEORES FORUM, V1&2, P55; BOWN PR, 1987, PALEONTOLOGICAL ASS, V38; Bucefalo Palliani R., 1994, PALEOPELAGOS, V4, P129; COLACICCHI R, 1989, 2 INT S JUR STRAT, V2, P717; CRESTA S, 1989, 2 INT S JUR STRAT, V2, P729; Crux J.A., 1984, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V169, P160; GRADSTEIN FM, 1994, J GEOPHYS RES-SOL EA, V99, P24051, DOI 10.1029/94JB01889; HALLAM A, 1987, MARINE PETROLEUM SOU, V26, P251; Hallock P, 1987, PALEOCEANOGRAPHY, V2, P457, DOI 10.1029/PA002i005p00457; JENKYNS HC, 1985, GEOL RUNDSCH, V74, P505, DOI 10.1007/BF01821208; Jenkyns HC, 1997, SEDIMENTOLOGY, V44, P687, DOI 10.1046/j.1365-3091.1997.d01-43.x; MATTIOLI E, 1995, ACT C NAN, P83; MATTIOLI E, IN PRESS RIV ITALIAN; MATTIOLI E, 1995, EUROPAL, V8, P69; Mattioli Emanuela, 1996, Rivista Italiana di Paleontologia e Stratigrafia, V102, P397; MORBEY SJ, 1975, PALAEONTOGR ABT B, V153, P1; MORGENROTH P, 1970, NEUES JB GEOLOGIE PA, V163, P9; NINI C, 1995, 3 EPA WORKSH BLACK S, P53; Palliani Raffaela Bucefalo, 1996, Palynology, V20, P157; Palliani Raffaella Bucefalo, 1997, Palynology, V21, P91; Palliani Raffaella Bucefalo, 1997, Palynology, V21, P197; 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, 1997, REV PALAEOBOT PALYNO, V96, P99, DOI 10.1016/S0034-6667(96)00019-X; PALLIANI RB, 1993, PALEOPELAGOS, V3, P129; PALLIANI RB, IN PRESS MICROPALEON; PALLIANI RB, 1995, EUROPAL, V8, P60; PALLIANI RB, 1996, THESIS U PERUGIA ITA; PIALLI G, 1969, B SOC NATURALISTI, V78, P345; Reale V., 1992, Mem. Sc. Geol. Padova, V43, P41; Riding J.B., 1992, P7; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding J.B., 1984, Proceedings of the Yorkshire Geological Society, V45, P109; Roth PH, 1987, PALEOCEANOGRAPHY, V2, P601, DOI 10.1029/PA002i006p00601; Tyson R.V., 1987, Marine petroleum source rocks, V26, P47, DOI 10.1144/GSL.SP.1987.026.01.03; Wille W., 1979, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V158, P221; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; WOOLLAM R, 1983, 832 I GEOL SCI, P2	42	30	31	0	1	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	DEC	1998	17		2				153	172		10.1144/jm.17.2.153	http://dx.doi.org/10.1144/jm.17.2.153			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	152ZU		hybrid			2025-03-11	WOS:000077808900007
J	El-Mehdawi, AD				El-Mehdawi, AD			<i>Odontochitina tabulata</i> sp. nov.: A Late Santonian Early Campanian dinoflagellate cyst from SE Sirte Basin, Libya	JOURNAL OF MICROPALAEONTOLOGY			English	Article								Odontochitina tabulata, a new tabulated ceratioid species, has been recorded and described from core samples in Well C3-65 in the SE Sirte Basin. This species is characterized by parasutural and pandasutural features reflecting clear gonyaulacacean paratabulation. It has a short stratigraphic range and is considered as a valuable stratigraphic marker for the Late Santonian-Early Campanian. The diagnosis of the genus Odontochitina Deflandre, 1935 is emended to include forms having a well defined gonyaulacacean paratabulation and narrow pandasutural and parasutural ridges.	Arabian Gulf Oil Co, Explorat Div, Geol Lab, Benghazi, Libya		El-Mehdawi, AD (通讯作者)，Arabian Gulf Oil Co, Explorat Div, Geol Lab, POB 263, Benghazi, Libya.							[Anonymous], 1885, HG BRONNS KLASSEN OR; BINT A N, 1986, Palynology, V10, P135; CLARKE R F A, 1968, Taxon, V17, P181, DOI 10.2307/1216512; CLARKE RFA, 1967, EERSTE REEKS, V24, P1; COOKSON I C, 1970, Proceedings of the Royal Society of Victoria, V83, P137; COOKSON I C, 1969, Journal of the Royal Society of Western Australia, V52, P3; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; COOKSON ISABEL C., 1956, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V7, P183; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; DAVEY RJ, 1975, P 5 W AFR C MICR, V7, P50; Deflandre G., 1935, Bulletin Biologique de la France et de la Belgique, V69, P213; DEFLANDRE GEORGES, 1955, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V6, P242; Fensome R.A., 1993, CLASSIFICATION FOSSI; Gocht H., 1957, Palaeontologische Zeitschrift, V31, P163; PASCHER A, 1914, BOTANISCHE GESELLSCH, V29, P193; STOVER L E, 1978, Stanford University Publications in the Geological Sciences, V15, P1; STOVER LE, 1987, ASS AUSTR PALAEONTOL, V4, P297; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Wetzel O., 1933, PALAEONTOGRAPHICA, V77, P141; Willey Arthur, 1909	20	6	6	1	2	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH, AVON, ENGLAND BA1 3JN	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	DEC	1998	17		2				173	178		10.1144/jm.17.2.173	http://dx.doi.org/10.1144/jm.17.2.173			6	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	152ZU		hybrid			2025-03-11	WOS:000077808900008
J	Montresor, M; Zingone, A; Sarno, D				Montresor, M; Zingone, A; Sarno, D			Dinoflagellate cyst production at a coastal Mediterranean site	JOURNAL OF PLANKTON RESEARCH			English	Article							CALCAREOUS RESTING CYST; MARINE-SEDIMENTS; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; ATLANTIC-OCEAN; NORTH-ATLANTIC; ADJACENT SEAS; DINOPHYCEAE; SCRIPPSIELLA; ALEXANDRIUM	To assess the diversity and seasonality of dinoflagellate cyst production, surface sediment and trap samples were studied in the Gulf of Naples (Mediterranean Sea). A total of 59 different cyst morphotypes were recorded. At the stations within the 70 m isobath, sediment assemblages were dominated by calcareous Peridiniales (66-79%), while at the deepest stations non-calcareous Peridiniales attained the highest percentages (40-49%). The sediment trap sampling, carried out fortnightly over two annual cycles, revealed high production rates (up to 1.7 x 10(6) cysts m(-2) day(-1)) from spring to late autumn of both years, with a distinct seasonal production pattern. Although rather similar in species composition, the total cyst flux differed markedly between the 2 years (1.26 and 0.55 x 10(8) cysts m(-2) year(-1), respectively). Species-specific production patterns were observed: some species formed cysts over several months, others in restricted periods of the year. Cyst-forming species constituted a small part of the planktonic dinoflagellate populations recorded in the area. A coupling between the trap material and surface water plankton was observed for calcareous Peridiniales. This sampling approach allowed the detection of some species never recorded before in the gulf, including two potentially toxic species: Alexandrium andersoni and Gymnodinium catenatum-like species.	Staz Zool Anton Dohrn, I-80121 Naples, Italy	Stazione Zoologica Anton Dohrn	Montresor, M (通讯作者)，Staz Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.		Zingone, Adriana/E-4518-2010	Zingone, Adriana/0000-0001-5946-6532; Montresor, Marina/0000-0002-2475-1787; SARNO, DIANA/0000-0001-9697-5301				ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; 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, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; [Anonymous], NEOGENE QUATERNARY D; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); BINDER BJ, 1987, J PHYCOL, V23, P99; BLANCO J, 1995, J PLANKTON RES, V17, P283, DOI 10.1093/plankt/17.2.283; BOERO F, 1994, MAR ECOL-P S Z N I, V15, P3, DOI 10.1111/j.1439-0485.1994.tb00038.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BRAVO I, 1997, HARMFUL ALGAE NEWS, V16, P4; CABRINI ML, 1990, OEBALIA, V16, P599; CARRADA G C, 1980, Marine Ecology, V1, P105, DOI 10.1111/j.1439-0485.1980.tb00213.x; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; DAHMS HU, 1995, HYDROBIOLOGIA, V306, P199, DOI 10.1007/BF00017691; 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., 1983, P69; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P45; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; Delgado Olga, 1994, Scientia Marina, V58, P237; DODGE JD, 1991, NEW PHYTOL, V118, P593, DOI 10.1111/j.1469-8137.1991.tb01000.x; ELLEGAARD M, 1994, EUR J PHYCOL, V29, P183, DOI 10.1080/09670269400650631; FENSOME RA, 1993, MICROPALEONTOLOGY SP, V1; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Hesse KJ, 1995, OLSEN INT S, P11; Ishikawa A, 1997, J PLANKTON RES, V19, P1783, DOI 10.1093/plankt/19.11.1783; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; KNAUER GA, 1979, DEEP-SEA RES, V26, P97, DOI 10.1016/0198-0149(79)90089-X; Marino D., 1984, Lecture Notes on Coastal and Estuarine Studies, V8, P89; MENDEZ SM, 1993, DEV MAR BIO, V3, P287; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; MONTRESOR M, 1995, PHYCOLOGIA, V34, P87, DOI 10.2216/i0031-8884-34-1-87.1; MONTRESOR M, 1993, J PHYCOL, V29, P223, DOI 10.1111/j.0022-3646.1993.00223.x; MONTRESOR M, 1994, REV PALAEOBOT PALYNO, V84, P45, DOI 10.1016/0034-6667(94)90040-X; MUNOZ-S P, 1983, Revista de Biologia Marina, V19, P63; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; NEHRING S, 1995, HELGOLANDER MEERESUN, V49, P375, DOI 10.1007/BF02368363; Nordli E., 1951, Nyt Magazin for Naturvidenskaberne, V88, P207; Peters E, 1996, J EXP MAR BIOL ECOL, V207, P43, DOI 10.1016/0022-0981(95)02519-7; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; REID PC, 1975, NEW PHYTOL, V75, P589, DOI 10.1111/j.1469-8137.1975.tb01425.x; Scotto diCarlo., 1985, Nova Thalassia, V7, P99; Shannon C.E., 1949, MATH THEORY COMMUNIC, P1, DOI DOI 10.1063/1.3067010; Smayda TJ, 1997, LIMNOL OCEANOGR, V42, P1137, DOI 10.4319/lo.1997.42.5_part_2.1137; SMETACEK V, 1985, ESTUARIES, V8, P145, DOI 10.2307/1351864; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; STRATHMANN RR, 1967, LIMNOL OCEANOGR, V12, P411, DOI 10.4319/lo.1967.12.3.0411; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2; Versteegh GJM, 1997, MAR MICROPALEONTOL, V30, P319, DOI 10.1016/S0377-8398(96)00052-7; WALL D, 1968, Journal of Paleontology, V42, P1395; 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; WHITTAKER RH, 1952, ECOL MONOGR, V22, P1, DOI 10.2307/1948527; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; ZINGONE A, 1990, MAR ECOL-P S Z N I, V11, P157, DOI 10.1111/j.1439-0485.1990.tb00236.x; ZINGONE A, 1995, J PLANKTON RES, V17, P575, DOI 10.1093/plankt/17.3.575	62	156	164	2	10	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	DEC	1998	20	12					2291	2312		10.1093/plankt/20.12.2291	http://dx.doi.org/10.1093/plankt/20.12.2291			22	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	149VV					2025-03-11	WOS:000077627700004
J	Babaran, RP; Espinosa, RA; Abalos, TU				Babaran, RP; Espinosa, RA; Abalos, TU			Initiating and triggering mechanisms causing harmful algal blooms	JOURNAL OF SHELLFISH RESEARCH			English	Article; Proceedings Paper	2nd International Conference on Molluscan Shellfish Safety	NOV 17-21, 1997	ILOILO, PHILIPPINES			"seed bed" formation; harmful algal blooms; Pyrodinium bahamense var. compressum; prediction; shellfish safety		Algal blooms have been variously associated with such environmental factors as excessive eutrophication, but the actual mechanisms that eventually lead to excystment have never been completely understood. Using weather data and observations of bloom events involving Pyrodinium bahamense var. compressum in Manila Bay as a case study, the role of waves in the formation of the "seed bed," the suspension of cysts, and the transformation of cysts into vegetative cells is presented and discussed. Results suggest that waves generated by onshore wind may be important in the onset of P. bahamense blooms. These findings are significant, because they not only advance current knowledge about the life cycle of P, bahamense but also provide the possible missing links that have long been hindering the prediction of algal events involving other cyst-forming dinoflagellates. The results of the study may also be useful when formulating alternative strategies toward: (1) managing harmful algal blooms in existing mussel and shellfish culture areas; and (2) selecting new culture sites to ensure mussel and shellfish safety throughout the world.	Univ Philippines Visayas, Inst Marine Fisheries & Oceanol, Coll Fisheries, Iloilo 5023, Philippines; Univ Philippines Visayas, Coll Arts & Sci, Dept Phys Sci & Math, Iloilo 5023, Philippines; Univ Philippines Visayas, Coll Fisheries, Inst Fisheries Policy & Dev Studies, Iloilo 5023, Philippines	University of the Philippines System; University of the Philippines Visayas; University of the Philippines System; University of the Philippines Visayas; University of the Philippines System; University of the Philippines Visayas	Babaran, RP (通讯作者)，Univ Philippines Visayas, Inst Marine Fisheries & Oceanol, Coll Fisheries, Iloilo 5023, Philippines.			BABARAN, RICARDO/0000-0003-4652-3619				[Anonymous], 1984, SHOR PROT MAN, VI; [Anonymous], P 1 INT C TOX DIN BL; [Anonymous], 1996, HARMFUL TOXIC ALGAL; BABARAN RP, 1997, PHILIPPINE COASTAL M, P161; Bajarias FA., 1996, HARMFUL TOXIC ALGAL, P49; *BAS, 1990, FISH STAT; BRETCHNEIDER CL, 1965, GEN WAVES WIND STATE; GONZALES CL, 1989, ICLARM CONT, V21, P141; Horikawa K., 1978, Coastal engineering; Ingles J., 1997, PHILIPPINE COASTAL M, P15; Jeffreys H, 1925, P R SOC LOND A-CONTA, V107, P189, DOI 10.1098/rspa.1925.0015; Kinsman B., 1965, Wind Waves; PAERL HW, 1988, LIMNOL OCEANOGR, V33, P823, DOI 10.4319/lo.1988.33.4_part_2.0823; Villanoy C. L, 1996, HARMFUL TOXIC ALGAL, P189	14	7	8	1	20	NATL SHELLFISHERIES ASSOC	GROTON	C/O DR. SANDRA E. SHUMWAY, UNIV CONNECTICUT, 1080 SHENNECOSSETT RD, GROTON, CT 06340 USA	0730-8000			J SHELLFISH RES	J. Shellfish Res.	DEC	1998	17	5					1623	1626						4	Fisheries; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Fisheries; Marine & Freshwater Biology	187WN					2025-03-11	WOS:000079811400043
J	Bertini, A; Londeix, L; Maniscalco, R; Di Stefano, A; Suc, JP; Clauzon, G; Gautier, F; Grasso, M				Bertini, A; Londeix, L; Maniscalco, R; Di Stefano, A; Suc, JP; Clauzon, G; Gautier, F; Grasso, M			Paleobiological evidence of depositional conditions in the Salt Member, Gessoso-Solfifera Formation (Messinian, Upper Miocene) of Sicily	MICROPALEONTOLOGY			English	Article							MEDITERRANEAN SALINITY CRISIS; NORTH-ATLANTIC OCEAN; DINOFLAGELLATE CYSTS; MARINE-SEDIMENTS; ADJACENT SEAS; BASIN; STRATIGRAPHY; ENVIRONMENTS; EVAPORITES; TRIPOLI	The micropaleontology of clayey layers within halite and kainite bodies in the Salt Member of the Lower Evaporitic Complex, in the Messinian (uppermost Miocene) Gessoso-Solfifera Formation, has been studied in samples taken from Racalmuto and Realmonte salt mines on the southern coast of Sicily. Rich paleobiological associations have been observed of (on the whole) well preserved foraminifers, nannoplankton, dinoflagellate cysts and pollen grains. The integrated analyses point to several normal-marine influxes that interrupted the formation of the evaporite deposits. The greatest influx of marine water (in probable correspondence with high relative sea level) occurred during the deposition of the earliest Unit C. Based on these data, a time-scale of the Salt Member deposition may be proposed for the first time, placing the salt deposition between isotope stages TG20 and TG22, in the interval 5.72 to 5.75 Ma. The micropaleontology indicates that salt deposition took place under warm and dry conditions characteristic of tropical to subtropical climates, and that there was no significant climatic change associated with the Salinity Crisis.	Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy; Univ Bordeaux 1, URA 197 CNRS, Dept Geol & Oceanog, F-33405 Talence, France; Univ Catania, Ist Geol & Geofis, I-95129 Catania, Italy; Univ Lyon 1, Ctr Paleontol Stratig & Paleoecol, UMR 5565 CNRS, F-69622 Villeurbanne, France; CEREGE, UMR 6635, F-13545 Aix En Provence 04, France	University of Florence; Universite de Bordeaux; University of Catania; Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD)	Bertini, A (通讯作者)，Univ Florence, Dipartimento Sci Terra, Via G Pira 4, I-50121 Florence, Italy.		Maniscalco, Rosanna/GRY-5603-2022; Bertini, Adele/KFQ-7894-2024	BERTINI, Adele/0000-0002-9332-6725; Di Stefano, Agata/0000-0002-2953-4191; Maniscalco, Rosanna/0000-0003-1026-044X				[Anonymous], 1991, MEMORIE SOC GEOLOGIC; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; AUBRY MP, 1984, HDB CENOZOIC CALCERE, V1; BARBER PM, 1981, MAR GEOL, V44, P253, DOI 10.1016/0025-3227(81)90053-0; Barbieri F., 1974, ATENEO PARMENSE ACTA, V10, P15; BESSAIS E, 1988, GEOBIOS-LYON, V21, P49, DOI 10.1016/S0016-6995(88)80031-7; BOISSEAU T, 1990, B CENT RECH EXPL, V14, P541; BOMMARITO S, 1984, Naturalista Siciliano, V8, P49; BRADFORD M R, 1984, Palaeontographica Abteilung B Palaeophytologie, V192, P16; BRINKHUIS H, 1992, THESIS U UTRECHT; BUSSON G, 1983, B I GEOLOGIE BASSIN, V34, P59; Busson G, 1990, GEOLOGIE FRANCE, V3-4, P3; Butler R.W.H., 1993, BASIN RES, V5, P137; BUTLER RWH, 1995, GEOL SOC AM BULL, V107, P425, DOI 10.1130/0016-7606(1995)107<0425:TASSIM>2.3.CO;2; Cambon G, 1997, GRANA, V36, P105, DOI 10.1080/00173139709362596; Chumakov IS., 1973, INITIAL REPORTS DEEP, P1242; CITA M B, 1973, Rivista Italiana di Paleontologia e Stratigrafia, V79, P393; CITA MB, 1982, ALPINE MEDITERRANEAN, V7, P113; CITA MB, 1980, INITIAL REPORTS DEEP, V50, P497; Clauzon G, 1996, GEOLOGY, V24, P363, DOI 10.1130/0091-7613(1996)024<0363:AIOTMS>2.3.CO;2; CLAUZON G, 1982, B SOC GEOL FR, V24, P597; Clauzon G., 1973, INITIAL REPORT DEEP, P1251, DOI DOI 10.2973/DSDP.PR0C.13.144-5.1973; DECIMA A, 1971, RIV MINERARIA SICILI, V130, P172; Decima A., 1973, INITIAL REPORTS DEEP, P1234; Decima A., 1976, MEM SOC GEOL ITAL, P39; DEVERNAL A, 1986, THESIS U MONTREAL; di Stefano E., 1976, Memorie della Societa Geologica Italiana, V16, P95; Edwards. 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J	Harland, R; Pudsey, CJ; Howe, JA; Fitzpatrick, MEJ				Harland, R; Pudsey, CJ; Howe, JA; Fitzpatrick, MEJ			Recent dinoflagellate cysts in a transect from the Falkland trough to the Weddell Sea, Antarctica	PALAEONTOLOGY			English	Review							CIRCUMPOLAR CURRENT; MARINE-SEDIMENTS; ATLANTIC-OCEAN; DRAKE PASSAGE; INDIAN-OCEAN; SCOTIA SEA; WATER; AUSTRALIA; NORTH; FLOW	Dinoflagellate cyst analysis has been completed on core-top samples that form a transect from the area of the Falkland Islands to the Weddell Sea, Antarctica. This study is the first to document the distribution of the Recent dinoflagellate cyst thanatocoenosis in the area. All the dinoflagellate cysts recovered are described and at least two species, Dalella chathamense and Selenopemphix antarctica, are recognized as endemic to the southern hemisphere from the results of this study and from previous research. Data presented here reveal a clear latitudinal trend in the cyst distribution such that subdivision into two domains is possible. The first, to the south of 60 degrees S, is characterized by low numbers of cysts, low diversity and the presence of Impagidinium pallidum, Algidasphaeridium? minutum, Pentapharsodinium dalei?, round brown Protoperidinium cysts and Selenopemphix antarctica. The second, to the north of 60 degrees S, is characterized by richer assemblages, higher species diversity and the presence of Dalella chathamense, Impagidinium sphaericum, Nematosphaeropsis labyrinthus and high numbers of Selenopemphix antarctica. This division of the cyst assemblages coincides approximately with the northern winter limit of sea-ice and demonstrates the potential of dinoflagellate cyst analysis in the elucidation of the palaeoceanography of the area using this criterion.	DinoData Serv, Nottingham NG13 8AH, England; Univ Sheffield, Dept Earth Sci, Ctr Palynol, Sheffield S3 7HF, S Yorkshire, England; British Antarctic Survey, Cambridge CB3 0ET, England; Univ Plymouth, Dept Geol Sci, Plymouth PL4 8AA, Devon, England	University of Sheffield; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of Plymouth	Harland, R (通讯作者)，DinoData Serv, 50 Long Acre, Nottingham NG13 8AH, England.							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J	Head, MJ				Head, MJ			Pollen and dinoflagellates from the Red Crag at Walton-on-the-Naze, Essex: evidence for a mild climatic phase during the early Late Pliocene of eastern England	GEOLOGICAL MAGAZINE			English	Article							NORTH-ATLANTIC OCEAN; ADJACENT SEAS; MID-PLIOCENE; CYSTS; SEDIMENTS; RECONSTRUCTION; STRATIGRAPHY; PALYNOLOGY; BOREHOLE; NORFOLK	Spot sampling of the Red Crag Formation at Walton-on-the-Naze, Essex (= Walton Gray) has revealed a diverse record of dinoflagellates, pollen, and other palynomorphs. Pollen from a basal horizon is dominated by Pinus, but also contains high values of Sciadopitys and a small but diverse component of deciduous mesothermal trees. Taxodium is more common at 2 m above the base of the Red Crag and may represent a different part of a climate cycle. A mild- to warm-temperate climate is inferred for the Walton assemblages and a correlation with the Reuverian B pollen substage (Late Pliocene, 3.0 to > 2.6 Ma) is demonstrated, thereby constraining the timing of an important marine transgression in eastern England. Dinoflagellates from the basal horizon and from 2 m above the base of the Red Crag generally indicate a restricted marine environment, but outer neritic to oceanic dinoflagellates are occasionally present, and imply the penetration of more saline North Atlantic water masses into the southern North Sea basin. Mild- to warm-temperate conditions are indicated by the presence of several thermophilic species. The Walton assemblages have strong similarities with those of the mid-Pliocene Coralline Crag Formation of eastern England, but differ in the presence of Bitectatodinium tepikiense, which, along with an apparently reduced species richness, gives evidence of cooler conditions. A number of thermophilic species at Walton are not reported from younger Pliocene deposits in eastern England, perhaps reflecting a less equable climate after Northern Hemisphere cooling at 2.55 Ma.	Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada	University of Toronto	Head, MJ (通讯作者)，Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada.							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W., 1953, PALAEONTOGRAPHICA, V94 B., P1; Van Der Hamen T., 1971, The Late Cenozoic Glacial Ages, P391; VANVOORTHUYSEN JH, 1972, GEOL MIJNBOUW, V51, P627; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WEST RG, 1974, PHILOS T ROY SOC B, V269, P1, DOI 10.1098/rstb.1974.0039; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363; WOOD AM, 1993, QUATERNARY SCI REV, V12, P747, DOI 10.1016/0277-3791(93)90015-E; WOOD AM, 1996, B GEOLOGICAL SOC NOR, V44, P538; WOOD SV, 1866, Q J GEOL SOC LOND, V22, P538; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; ZAGWIJN W H, 1974, Boreas (Oslo), V3, P75; Zagwijn W. H., 1960, MEDED GEOL STICHTING, V1, P1; ZALASIEWICZ JA, 1988, PHILOS T R SOC B, V322, P221, DOI 10.1098/rstb.1988.0125	72	45	45	0	11	CAMBRIDGE UNIV PRESS	NEW YORK	40 WEST 20TH STREET, NEW YORK, NY 10011-4211 USA	0016-7568			GEOL MAG	Geol. Mag.	NOV	1998	135	6					803	817		10.1017/S0016756898001745	http://dx.doi.org/10.1017/S0016756898001745			15	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	151CA					2025-03-11	WOS:000077702200005
J	Butterfield, NJ; Rainbird, RH				Butterfield, NJ; Rainbird, RH			Diverse organic-walled fossils, including "possible dinoflagellates," from the early Neoproterozoic of arctic Canada	GEOLOGY			English	Article							EVOLUTION; CONSTRAINTS	A shallow-water shale unit from the early Neoproterozoic Wynniatt Formation, arctic Canada, preserves an unusually high diversity of organic-walled fossils, including abundant cyanobacteria, several multicellular protists and/or problematica, and more than 30 distinct acritarch species. Recognition of 13 new acritarchs, based on novel ornamentation, excystment structures, and/or wall structure, substantially increases their known diversity for this interval and points to a severe undersampling of the Proterozoic fossil record. Three of these new acritarchs exhibit features characteristic of dinoflagellate cysts and are reasonable candidates for early representatives of the clade, particularly in light of recent molecular phylogenetic analyses and biomarker data. The high diversity of acritarchs in the Wynniatt Formation also bolsters the potential for biostratigraphic resolution in the Neoproterozoic.	Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England; Geol Survey Canada, Ottawa, ON K1A 0E8, Canada	University of Cambridge; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada	Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England.		Butterfield, Nicholas/AAV-8215-2021	Butterfield, Nicholas/0000-0002-3046-7520; Rainbird, Robert/0000-0003-4538-4637				[Anonymous], 1985, SPOROPOLLENIN DINOFL; ASMEROM Y, 1991, GEOCHIM COSMOCHIM AC, V55, P2883, DOI 10.1016/0016-7037(91)90453-C; Butterfield N.J., 1994, PALEOBIOLOGY NEOPROT, V34; BUTTERFIELD NJ, 1992, PALAEONTOLOGY, V35, P943; BUTTERFIELD NJ, 1990, SCIENCE, V250, P104, DOI 10.1126/science.11538072; BUTTERFIELD NJ, 1995, LETHAIA, V28, P1, DOI 10.1111/j.1502-3931.1995.tb01587.x; GROTZINGER JP, 1995, SCIENCE, V270, P598, DOI 10.1126/science.270.5236.598; Hermann T.N., 1990, ORGANIC WORLD BILLIO; HOFMANN HJ, 1994, PALAEONTOLOGY, V37, P721; Knoll A.H., 1996, Palynology - principles and applications, V1, P51; KNOLL AH, 1994, P NATL ACAD SCI USA, V91, P6743, DOI 10.1073/pnas.91.15.6743; KNOLL AH, 1992, SCIENCE, V256, P622, DOI 10.1126/science.1585174; Kumar S, 1996, J MOL EVOL, V42, P183, DOI 10.1007/BF02198844; Moldowan JM, 1996, GEOLOGY, V24, P159; Philippe H, 1998, SYST ASSOC SPEC VOL, V56, P25; Rainbird RH, 1996, GEOL SOC AM BULL, V108, P454, DOI 10.1130/0016-7606(1996)108<0454:TENSSB>2.3.CO;2; SARJEANT W A S, 1978, Palynology, V2, P167; STANCLIFFE RPW, 1990, MICROPALEONTOLOGY, V36, P197, DOI 10.2307/1485506; Stiller JW, 1997, P NATL ACAD SCI USA, V94, P4520, DOI 10.1073/pnas.94.9.4520; SUMMONS RE, 1992, GEOCHIM COSMOCHIM AC, V56, P2437, DOI 10.1016/0016-7037(92)90200-3; SUMMONS RE, 1990, AM J SCI, V290A, P212; Vidal G, 1997, PALEOBIOLOGY, V23, P230, DOI 10.1017/S0094837300016808; VIDAL G, 1985, PRECAMBRIAN RES, V28, P349, DOI 10.1016/0301-9268(85)90038-5	23	82	99	0	7	GEOLOGICAL SOC AMER, INC	BOULDER	PO BOX 9140, BOULDER, CO 80301-9140 USA	0091-7613	1943-2682		GEOLOGY	Geology	NOV	1998	26	11					963	966		10.1130/0091-7613(1998)026<0963:DOWFIP>2.3.CO;2	http://dx.doi.org/10.1130/0091-7613(1998)026<0963:DOWFIP>2.3.CO;2			4	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	135MX					2025-03-11	WOS:000076807000001
J	Kelly, SRA; Whitham, AG; Koraini, AM; Price, SP				Kelly, SRA; Whitham, AG; Koraini, AM; Price, SP			Lithostratigraphy of the Cretaceous (Barremian-Santonian) Hold with Hope Group, NE Greenland	JOURNAL OF THE GEOLOGICAL SOCIETY			English	Article						Greenland; Cretaceous; lithostratigraphy; biostratigraphy	EAST GREENLAND	The finest exposures of Barremian to Santonian sedimentary rocks in the northern North Atlantic region are exposed in Hold with Hope, NE Greenland. These rocks comprise the Hold with Hope Group which, together with its constituent formations and members are defined here as new lithostratigraphic units. The strata are dated as Cretaceous by use of molluscan macrofaunas and dinoflagellate cysts. The marine mudstone-dominated Hold with Hope Group is over 1300 m thick and is divided into the Steensby Bjerg and Home Forland formations. The sandstone-dominated Steensby Bjerg Formation (Barremian-Albian) is 300 m thick. It rests with angular unconformity on sandstones attributed to the Vardekloft Formation (Middle Jurassic) and is subdivided into the Diener Bjerg, Gulelv, Stribedal, Blaelv, Stensio Plateau and Rodelv members. The mudstone-dominated Home Forland Formation (Albian-Santonian) is over 1000 m thick. It rests unconformably on the Steensby Bjerg, Vardekloft and Wordie Creek (Triassic) formations. It is subdivided into the Fosdalen, Nanok, Ostersletten, and Knudshoved members. The Hold with Hope Group is overlain unconformably by Tertiary basalts and sedimentary rocks. The original proximity of Hold with Hope to the Voring Basin is significant for possible Cretaceous hydrocarbon plays on the formerly adjacent NW European margin.	CASP, Cambridge CB3 0DJ, England; Southampton Oceanog Ctr, Dept Geol, Southampton SO14 3ZH, Hants, England	University of Cambridge; NERC National Oceanography Centre; University of Southampton	Kelly, SRA (通讯作者)，CASP, W Bldg Gravel Hill,Huntingdon Rd, Cambridge CB3 0DJ, England.							[Anonymous], 1935, MEDDELELSER GRONLAND, DOI DOI 10.1017/S1477201907002040; Birkelund T., 1965, Meddelelser om Gronland, V179, P1; Birkelund T., 1983, ZITTELIANA, V10, P7; Birkelund T., 1976, GEOLOGY GREENLAND, P304; Callomon JH, 1993, B GEOL SOC DENMARK, V40, P83; Casey R., 1961, Palaeontology, V3, P487; DELORIOL P, 1883, MEDDELELSER GRONLAND, V5, P203; Donovan D. 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Geol. Soc.	NOV	1998	155		6				993	1008		10.1144/gsjgs.155.6.0993	http://dx.doi.org/10.1144/gsjgs.155.6.0993			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	132PH					2025-03-11	WOS:000076638400008
J	Thorsen, TA; Dale, B				Thorsen, TA; Dale, B			Climatically influenced distribution of Gymnodinium catenatum during the past 2000 years in coastal sediments of southern Norway	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; Gymnodinium catenatum; climatic change; marine palaeoecology; Medieval Warm Period; Little Ice Age	UPPER QUATERNARY SEDIMENTS; DINOFLAGELLATE CYSTS; MARINE-SEDIMENTS; LATE HOLOCENE; DINOPHYCEAE; AUSTRALIA; SKAGERRAK; TASMANIA; KATTEGAT; RECORD	Dinoflagellate cyst analysis of cored late Holocene sediments from the Norwegian coast of the Skagerrak and northern North Sea confirms the conclusions of previous studies from the Kattegat that climate influenced the quantitative distribution of Gymnodinium catenatum Graham 1943. These studies provide some of the first data on the effect of small-scale climatic changes on one component of the phytoplankton during the past 2000 years. In core 9310 from the Skagerrak, as in previous cores from the Kattegat, G. catenatum cysts increase proportionally from about AD 0 to peak amounts at about AD 900, 1200 and 1450 corresponding to periods of relatively warmer climate. Proportional decreases in G. catenatum correspond to periods of cooler climate in the 900s and 1300s, and to the colder climate of the Little Ice Age climax in the 1600s. In the site of core 9307 from the North Sea coast higher proportions of G. catenatum (15%) were probably reached between 300 and 1000 years later than in the other cores, due to the location of this site being closer to the biogeographic limit for high proportions of the species. New results also suggest that high proportions of the species (2-58%) were confined to open coastal waters south of Bergen, Norway. Living and fossil cysts of G. catenatum in this region are small compared with reported sizes elsewhere (24-40 vs. 37-60 mu m), and may not be conspecific with G. catenatum. Irrespective of their taxonomy, the quantitative distribution of these cysts is influenced by climatic changes, and they are a reliable indicator of warmer water in more open coastal waters of Scandinavia during the late Holocene. (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Oslo, Dept Geol, N-0316 Oslo, Norway	University of Oslo	Thorsen, TA (通讯作者)，Univ Oslo, Dept Geol, POB 1047, N-0316 Oslo, Norway.	t.a.thorsen@geologi.uio.no						AMORIM A, 1998, IN PRESS P 8 INT C H; Andersen B.G., 1991, Striae, V34, P109; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON PM, 1988, SCIENCE, V241, P1043, DOI 10.1126/science.241.4869.1043; [Anonymous], 1983, PACT PUBLICATIONS; [Anonymous], 1977, CONTRIBUTIONS STRATI; [Anonymous], SCI AM; BAKKEN K, 1986, BOREAS, V15, P185; Barss M. 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Paleoclimatol. Paleoecol.	OCT 30	1998	143	1-3					159	177		10.1016/S0031-0182(98)00079-0	http://dx.doi.org/10.1016/S0031-0182(98)00079-0			19	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	133CF					2025-03-11	WOS:000076668300008
J	Anderson, JT				Anderson, JT			The effect of seasonal variability on the germination and vertical transport of a cyst forming dinoflagellate, Gyrodinium sp., in the Chesapeake Bay	ECOLOGICAL MODELLING			English	Article						seasonal variability; cyst forming dinoflagellate; germination and vertical transport	RED TIDE; PHYTOPLANKTON; ESTUARINE; BLOOMS; DISTRIBUTIONS; DINOPHYCEAE; SEDIMENTS; COASTAL; SYSTEM; MODEL	Seasonal dinoflagellate blooms frequently occur in estuaries such as the Chesapeake Bay. Studies have shown that environmental factors such as temperature, salinity, light intensity, nutrient availability and physical mixing can affect the seasonal and vertical distribution of motile dinoflagellates. Furthermore, these environmental factors can affect the life history of cyst forming dinoflagellates by inducing the formation of dormant cysts in unfavorable conditions and by inducing cyst germination in favorable conditions. A generalized, dynamic model, developed in Stella II, is proposed to examine combined effects of environmental processes on the life history and transport of a cyst forming dinoflagellate, Gyrodinium sp., in the Chesapeake Bay. The proposed model is arranged as a one-dimensional vertical column with no lateral migration or emigration to examine the role of local cysts in the formation of blooms. Two sampling stations provided by the EPA Chesapeake Bay Program, one at the mouth of the Potomac River (LE2.3) and the other in the main stem of the Chesapeake Bay (CB5.2), were used for comparison. Calibration was attempted using the Maryland Phytoplankton Taxon Survey, also provided by the EPA Chesapeake Bay Program, at MLE2.2 (a location upstream from station LE2.3). Observed cell concentrations for the winter and fall did not coincide with the cell concentrations calculated from the model for station LE2.3. This discontinuity suggests that cell migration from other portions of the Chesapeake Bay and the Potomac river could have contributed to the majority of observed winter and fall concentrations. Furthermore, observed cell concentrations at CB5.2 were the result of cell migration alone, due to the presence of a permanent pycnocline that inhibited cyst transport to the surface. The results of the proposed vertical transport model suggest that a three-dimensional model incorporating migration and emigration may be necessary in examining bloom formation. (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA	University System of Maryland; University of Maryland Center for Environmental Science	Anderson, JT (通讯作者)，Univ Maryland, Ctr Environm Sci, Horn Point Lab, Cambridge, MD 21613 USA.							ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; BLUMBERG AF, 1990, ESTUARIES, V13, P236, DOI 10.2307/1351914; BOCKSTAHLER KR, 1993, J EUKARYOT MICROBIOL, V40, P49, DOI 10.1111/j.1550-7408.1993.tb04881.x; Burkholder JM, 1997, LIMNOL OCEANOGR, V42, P1052, DOI 10.4319/lo.1997.42.5_part_2.1052; CERCO CF, 1993, J ENVIRON ENG-ASCE, V119, P1006, DOI 10.1061/(ASCE)0733-9372(1993)119:6(1006); COATS DW, 1984, J PHYCOL, V20, P351, DOI 10.1111/j.0022-3646.1984.00351.x; ESTEVES JL, 1992, HYDROBIOLOGIA, V242, P122; FIGUEIRAS FG, 1991, J PLANKTON RES, V13, P589, DOI 10.1093/plankt/13.3.589; FISHER TR, 1992, MAR ECOL PROG SER, V82, P51, DOI 10.3354/meps082051; FRAGA F, 1992, MAR ECOL PROG SER, V87, P123, DOI 10.3354/meps087123; Frank LM, 1997, ANN NEUROL, V42, P2; GALLEGOS CL, 1992, LIMNOL OCEANOGR, V37, P813, DOI 10.4319/lo.1992.37.4.0813; GERRITSEN J, 1994, ESTUARIES, V17, P403, DOI 10.2307/1352673; HALLEGRAEFF GM, 1992, MAR POLLUT BULL, V25, P186, DOI 10.1016/0025-326X(92)90223-S; HARDING LW, 1988, J PHYCOL, V24, P77; HEINIG C S, 1992, Journal of Shellfish Research, V11, P111; KEAFER BA, 1992, MAR MICROPALEONTOL, V20, P147, DOI 10.1016/0377-8398(92)90004-4; LITAKER W, 1993, MAR ECOL PROG SER, V94, P141, DOI 10.3354/meps094141; MARTIN DF, 1983, J ENVIRON SCI HEAL A, V18, P685, DOI 10.1080/10934528309375133; MCPHERSON BF, 1990, WATER RESOUR BULL, V26, P787; MORTON SL, 1992, J EXP MAR BIOL ECOL, V157, P79, DOI 10.1016/0022-0981(92)90076-M; OFFICER CB, 1984, SCIENCE, V223, P22, DOI 10.1126/science.223.4631.22; PAERL HW, 1988, LIMNOL OCEANOGR, V33, P823, DOI 10.4319/lo.1988.33.4_part_2.0823; TILSTONE GH, 1994, MAR ECOL PROG SER, V112, P241, DOI 10.3354/meps112241; TYLER MA, 1982, MAR ECOL PROG SER, V7, P163, DOI 10.3354/meps007163; TYLER MA, 1978, LIMNOL OCEANOGR, V23, P227, DOI 10.4319/lo.1978.23.2.0227; YAMAZAKI H, 1991, DEEP-SEA RES, V38, P219, DOI 10.1016/0198-0149(91)90081-P	27	5	7	1	13	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0304-3800			ECOL MODEL	Ecol. Model.	OCT 15	1998	112	2-3					85	109						25	Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	142BY					2025-03-11	WOS:000077181100002
J	Garces, E; Delgado, M; Maso, M; Camp, J				Garces, E; Delgado, M; Maso, M; Camp, J			Life history and in situ growth rates of Alexandrium taylori (Dinophyceae, Pyrrophyta)	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium; in situ growth rate; life history; planozygotes; resting cyst; temporary cyst	DINOFLAGELLATE GONYAULAX-TAMARENSIS; DNA-SYNTHESIS CYCLES; CYST FORMATION; SEXUAL REPRODUCTION; CELL-CYCLE; DIVISION; POPULATIONS; PYRRHOPHYTA; ESTUARY; CILIATE	Alexandrium taylori Balech is a phototrophic marine dinoflagellate. It produced recurrent blooms during the summer months (July and August) of 1994 to 1997 in La Fosca beach (NW Mediterranean). In addition to a motile vegetative form, A. taylori had two benthic forms: temporary cysts and resting cysts. Temporary cysts were a temporally quiescent stage produced from the ecdysis of the vegetative cell in both natural populations and laboratory cultures. Temporary cysts may divide to form motile cells. Resting cysts had a thicker wall than the temporary cysts and had a red accumulation body. Gametes and planozygotes were also observed in laboratory cultures. Alexandrium taylori showed in situ diurnal vertical migration with an increase of vegetative cells in the water column in the morning through midday, with concentrations peaking in the afternoon followed by lower levels at night. Most vegetative cells lost their thecae and flagella, and with them their motility, turning into temporary cysts that settled in the early evening: The number of temporary cysts in the water column rose in the evening and at night. The temporary cysts gave rise to motile cells the following morning. Synthesis of DNA occurred in vegetative cells at night, and a preferential period of cell division occurred at sunrise. The estimated division rate in the;field was 0.4-0.5 vegetative cells.day(-1). Temporary cysts had twice the DNA of a G(1) vegetative cell. The minimum in situ division rate of the temporary cysts was 0.14 day(-1). The role of the resting and temporary cyst population in the annual recurrence and maintenance of the A. taylori bloom is discussed.	Inst Ciencias Mar, Barcelona 08039, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Inst Ciencias Mar, P Joan de Borbo S-N, Barcelona 08039, Spain.	esther@icm.csic.es	Garces, Esther/C-5701-2011	Garces, Esther/0000-0002-2712-501X; Camp, Jordi/0000-0002-5202-9783				ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BALECH E, 1994, T AM MICROSC SOC, V113, P216, DOI 10.2307/3226651; BARLOW SB, 1988, PHYCOLOGIA, V27, P413, DOI 10.2216/i0031-8884-27-3-413.1; BIECHELER B, 1952, B BIOL FR BELG S, V20, P1; 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, 1985, MAR BIOL, V89, P83, DOI 10.1007/BF00392880; CHANG J, 1990, MAR ECOL PROG SER, V65, P293, DOI 10.3354/meps065293; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; CRAWFORD DW, 1992, MAR ECOL PROG SER, V79, P259; Delgado M, 1997, J PLANKTON RES, V19, P749, DOI 10.1093/plankt/19.6.749; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; ELBRACHTER M, 1978, HELGOLAND WISS MEER, V31, P347, DOI 10.1007/BF02189487; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; FRITZ L, 1989, J PHYCOL, V25, P95, DOI 10.1111/j.0022-3646.1989.00095.x; GARCES EP, 1998, THESIS U BARCELONA B; Grzebyk D, 1996, J PLANKTON RES, V18, P1837, DOI 10.1093/plankt/18.10.1837; HOHFELD I, 1992, J PHYCOL, V28, P82, DOI 10.1111/j.0022-3646.1992.00082.x; HORSTMANN U, 1980, J PHYCOL, V16, P481, DOI 10.1111/j.1529-8817.1980.tb03064.x; JONSSON PR, 1994, J EXP MAR BIOL ECOL, V175, P77, DOI 10.1016/0022-0981(94)90177-5; KITA T, 1985, B MAR SCI, V37, P643; KITA T, 1988, Bulletin of Plankton Society of Japan, V35, P1; Kita Takumi, 1993, Bulletin of Plankton Society of Japan, V39, P79; LOMBARD EH, 1971, J PHYCOL, V7, P188, DOI 10.1111/j.1529-8817.1971.tb01500.x; Montresor M, 1995, PHYCOLOGIA, V34, P444, DOI 10.2216/i0031-8884-34-6-444.1; MORRILL LC, 1981, J PHYCOL, V17, P315, DOI 10.1111/j.0022-3646.1981.00315.x; MORRILL LC, 1984, J MAR BIOL ASSOC UK, V64, P939, DOI 10.1017/S0025315400047354; OSTERGAARD M, 1997, EUR J PHYCOL, V32, P9; Sampayo M.A. de M., 1985, P125; Schmitter R.E., 1979, P123; SILVA ES, 1995, PHYCOLOGIA, V34, P396, DOI 10.2216/i0031-8884-34-5-396.1; Taylor F.J.R., 1987, General group characteristics; special features of interest; short history of dinoflagellate study; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; VAULOT D, 1992, LIMNOL OCEANOGR, V37, P644; Veldhuis MJW, 1997, J PHYCOL, V33, P527, DOI 10.1111/j.0022-3646.1997.00527.x; Von Stosch HA., 1973, Br Phycol J, V8, P105; VONSTOSCH HA, 1972, SOC BOT FR, V20, P201; YAMAGUCHI M, 1992, MAR BIOL, V112, P191, DOI 10.1007/BF00702461	38	66	68	1	13	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	OCT	1998	34	5					880	887		10.1046/j.1529-8817.1998.340880.x	http://dx.doi.org/10.1046/j.1529-8817.1998.340880.x			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	133AQ					2025-03-11	WOS:000076664600021
J	Dupont, LM; Marret, F; Winn, K				Dupont, LM; Marret, F; Winn, K			Land-sea correlation by means of terrestrial and marine palynomorphs from the equatorial East Atlantic: phasing of SE trade winds and the oceanic productivity	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						marine palynology; Brunhes chron; equator; West Africa; land-sea correlation; vegetation history; monsoon variation	DINOFLAGELLATE CYSTS; ORGANIC-MATTER; SOUTH-ATLANTIC; ARABIAN SEA; SURFACE TEMPERATURES; POLLEN DISTRIBUTION; TROPICAL ATLANTIC; WEST CAMEROON; ADJACENT SEAS; NW-AFRICA	Sporomorphs and dinoflagellate cysts from site GIK16867 in the northern Angola Basin record the vegetation history of the West African forest during the last 700 ka in relation to changes in salinity and productivity of the eastern Gulf of Guinea. During most cool and cold periods, the Afromontane forest, rather than the open grass-rich dry forest, expanded to lower altitudes partly replacing the lowland rain forest of the borderlands east of the Gulf of Guinea. Except in Stage 3, when oceanic productivity was high during a period of decreased atmospheric circulation, high oceanic productivity is correlated to strong winds. The response of marine productivity in the course of a climatic cycle, however, is earlier than that of wind vigour and makes wind-stress-induced oceanic upwelling in the area less likely. Monsoon variation is well illustrated by the pollen record of increased lowland rain forest that is paired to the dinoflagellate cyst record of decreased salinity forced by increased precipitation and run-off. (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Gottingen, Inst Palynol & Quaternary Sci, D-3400 Gottingen, Germany	University of Gottingen	Dupont, LM (通讯作者)，Univ Bremen, Dept Geosci, POB 330440, D-28334 Bremen, Germany.	dupont@allgeo.uni-bremen.de		Marret-Davies, Fabienne/0000-0003-4244-0437; Dupont, Lydie/0000-0001-9531-6793				[Anonymous], PALAEOECOL AFR; [Anonymous], 2004, J BIOGEOGR; [Anonymous], THESIS U MONTPELLIER; [Anonymous], VEGETATION HIST ARCH; [Anonymous], 1983, OC ANOGRAPH TROP; [Anonymous], 1992, Neogene and Quaternary dinoflagellate cysts and acritarchs; BARD E, 1990, NATURE, V345, P405, DOI 10.1038/345405a0; Bearman G., 1989, OCEAN CIRCULATION; BENGO MD, 1991, CR ACAD SCI II, V313, P843; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; BLOEMENDAL J, 1989, NATURE, V342, P897, DOI 10.1038/342897a0; BONIFAY D, 1992, MAR GEOL, V106, P107, DOI 10.1016/0025-3227(92)90057-O; Brenac P., 1988, TRAVAUX SECTION SCI, V25, P91; Chang P, 1997, NATURE, V385, P516, DOI 10.1038/385516a0; CLEMENS S, 1991, NATURE, V353, P720, DOI 10.1038/353720a0; COETZEE JA, 1967, PALAEOECOL AFR, V3; DALE B, 1996, P 9 INT PAL C HOUST, P28; DAVEY RJ, 1975, MAR GEOL, V18, P213, DOI 10.1016/0025-3227(75)90097-3; DEMENOCAL PB, 1993, J GEOPHYS RES-ATMOS, V98, P7265, DOI 10.1029/92JD02924; DEPLOEY J, 1969, PALAEOECOL AFR, V4, P65; DIESTERHAASS L, 1988, PALAEOGEOGR PALAEOCL, V65, P81, DOI 10.1016/0031-0182(88)90114-9; Dupont L.M., 1992, Vegetation History and Archaeobotany, V1, P163, DOI DOI 10.1007/BF00191556; DUPONT LM, 1993, QUATERNARY SCI REV, V12, P189, DOI 10.1016/0277-3791(93)90053-O; DUPONT LM, 1991, GEOL RUNDSCH, V80, P567, DOI 10.1007/BF01803687; Dupont LM, 1995, PALEOCLIMATE AND EVOLUTION, WITH EMPHASIS ON HUMAN ORIGINS, P289; Dupont LM, 1996, VEG HIST ARCHAEOBOT, V5, P273; DUPONT LM, 1998, IN PRESS PALAEOGEOGR; Dupont LM., 1989, Proceedings of the Ocean Drilling Program, Scientific Result, V108, P93; DUPONT LM, 1996, PALAEOECO A, V24, P85; Edwards LE., 1992, Neogene-Holocene dinoflagellate cysts and acritarchs, P259; ELENGA H, 1994, PALAEOGEOGR PALAEOCL, V109, P345, DOI 10.1016/0031-0182(94)90184-8; Elenga H., 1991, S AFR PAL, P239; EMEIS KC, 1995, QUATERNARY RES, V43, P355, DOI 10.1006/qres.1995.1041; FENSOME RA, 1993, CLASISFICATION LIVIN, V7; FREDOUX A, 1994, PALAEOGEOGR PALAEOCL, V109, P317, DOI 10.1016/0031-0182(94)90182-1; GIRESSE P, 1994, PALAEOGEOGR PALAEOCL, V107, P65, DOI 10.1016/0031-0182(94)90165-1; Giresse P., 1981, TRAV DOC ORSTOM, V138, P13; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEUSSER L, 1977, QUATERNARY RES, V7, P45, DOI 10.1016/0033-5894(77)90013-8; HEUSSER LE, 1988, MAR GEOL, V80, P131, DOI 10.1016/0025-3227(88)90076-X; HEUSSER LE, 1985, QUATERNARY RES, V24, P60, DOI 10.1016/0033-5894(85)90083-3; HOOGHIEMSTRA H, 1989, NATO ADV SCI I C-MAT, V282, P733; Hooghiemstra H., 1986, Meteor"Forschungsergeb. 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Paleoclimatol. Paleoecol.	OCT 1	1998	142	1-2					51	84		10.1016/S0031-0182(97)00146-6	http://dx.doi.org/10.1016/S0031-0182(97)00146-6			34	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	105CG					2025-03-11	WOS:000075054400004
J	Peeters, FJC; Hoek, RP; Brinkhuis, H; Wilpshaar, M; de Boer, PL; Krijgsman, W; Meulenkamp, JE				Peeters, FJC; Hoek, RP; Brinkhuis, H; Wilpshaar, M; de Boer, PL; Krijgsman, W; Meulenkamp, JE			Differentiating glacio-eustacy and tectonics; a case study involving dinoflagellate cysts from the Eocene-Oligocene transition of the Pindos Foreland Basin (NW Greece)	TERRA NOVA			English	Article							WESTERN GREECE; RECONSTRUCTION; STRATIGRAPHY; PLIOCENE; NORTH; SEA	In an attempt to discriminate between tectonically induced sealevel changes and glacio-eustacy, the Ekklissia and Arakthos sections (Epirus, NW Greece) are examined, applying (dinocyst) palynology, sedimentology and magnetostratigraphy. The sections, located in the Pindos Foreland Basin, both comprise the transition from pelagic limestones to hemipelagic silty clays and turbidite sandstones, reflecting the onset of flysch sedimentation as a result of the Pindos thrust activity. Despite an overall tectonic overprint, relative changes of sea level can be reconstructed, using (i) continental/marine palynomorph ratios, (ii) relative abundance of inshore and offshore dinoflagellate cysts, and (iii) taxa indicative of relatively cold and warm sea-surface temperature, that can be calibrated against the Global Polarity Time Scale (GPTS). Increased fluxes of marginal marine and continental palynomorphs coincide with colder periods on a 'third-order' scale, which thus appear to be related to glacioeustatic trends in sea-level. The larger scale is attributed to the increasing effect of tectonics and acts on a 'second-order scale'.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Vrije Univ Amsterdam, Fac Aardwetenschappen, NL-1081 HV Amsterdam, Netherlands; Univ Utrecht, Inst Aardwetenschappen, NL-3584 CD Utrecht, Netherlands; Univ Utrecht, Palaeomagnet Lab, NL-3584 CD Utrecht, Netherlands	Utrecht University; Vrije Universiteit Amsterdam; Utrecht University; Utrecht University	Peeters, FJC (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610; Krijgsman, Wout/0000-0002-1472-1074				[Anonymous], NEOGENE QUATERNARY D; Aubouin J., 1965, GEOSYNCLINES; AUBOUIN J, 1959, ANN GEOL PAYS HELL, V10; BERGGREN WA, 1995, SPEC PUBL SOC EC PAL, V54; 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 JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; EDWARDS LE, 1991, QUATERNARY SCI REV, V10, P259, DOI 10.1016/0277-3791(91)90024-O; FLEURY JJ, 1980, SOC GEOL NORD, V4; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; HEAD MJ, 1992, NEOGENE QARTERNARY D; HORNER F, 1983, TECTONOPHYSICS, V98, P11, DOI 10.1016/0040-1951(83)90208-1; *IGSR IFP, 1966, ET GEOL EP GREC NORD; Kennett J.P., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P937; KISSEL C, 1988, TECTONOPHYSICS, V146, P183, DOI 10.1016/0040-1951(88)90090-X; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; Miller KG, 1987, PALEOCEANOGRAPHY, V2, P1, DOI 10.1029/PA002i001p00001; PIPER DJW, 1978, J SEDIMENT PETROL, V48, P117; SAUNDERS JB, 1984, MICROPALEONTOLOGY, V30, P390, DOI 10.2307/1485710; Stover L.E., 1993, B SOC BELG GEOL, V102, P5; Traverse A., 1966, MAR GEOL, V4, P417, DOI DOI 10.1016/0025-3227(66)90010-7; UNDERHILL JR, 1989, GEOL SOC AM BULL, V101, P613, DOI 10.1130/0016-7606(1989)101<0613:LCDOTH>2.3.CO;2; Vail P.R., 1977, SEISMIC STRATIGRAPHY, P49, DOI DOI 10.1306/M26490C6; 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; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553; ZEVENBOOM D, 1995, THESIS UTRECHT U NET	28	11	12	0	5	BLACKWELL SCIENCE LTD	OXFORD	P O BOX 88, OSNEY MEAD, OXFORD OX2 0NE, OXON, ENGLAND	0954-4879			TERRA NOVA	Terr. Nova	OCT	1998	10	5					245	249						5	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	192KY					2025-03-11	WOS:000080078900003
J	Vidal, EAG; Haimovici, M				Vidal, EAG; Haimovici, M			Feeding and the possible role of the proboscis and mucus cover in the ingestion of microorganisms by rhynchoteuthion paralarvae (Cephalopoda: Ommastrephidae)	BULLETIN OF MARINE SCIENCE			English	Article							PHYTOPLANKTON-DERIVED DETRITUS; MICROBIAL AGGREGATION; MARINE SNOW; DEGRADATION; SUCCESSION; PARTICLES; SEAWATER	The diets of 72 rhynchoteuthion paralarvae of Illex argentinus (Catellanos, 1960) (1.0-8.0 mm ML) and two other ommastrephid squids from southern Brazil (28 degrees 09' S-34 degrees 20' S) were investigated by examination of their digestive tracts and mucus covering. A great diversity of microorganisms was identified on the mucus cover, on the proboscis suckers and in the digestive tracts of the rhynchoteuthions, including dinoflagellates, flagellates, ciliates, cysts and bacteria. Among the digestive tracts of Illex argentinus rhynchoteuthions examined, 55.6% were empty, 9.7% contained unrecognizable food and 34.7% contained recognizable food, which included microorganisms on mucus as well as copepod appendages. Microorganisms on mucus were found mainly inside the digestive tracts of small paralarvae, which also displayed high bacterial densities on their mucus cover. The presence of bacteria on the mucus cover and of mucus in the digestive tracts decreased with increasing paralarval size. The smallest rhynchoteuthion with copepod appendages in its digestive tract was 3.7 mm ML. These findings suggest that mucus enriched with microorganisms may be important in the diet of small rhynchoteuthions, and it is hypothesized that mucus could act as a substrate for microbial growth. The proboscis may play an important role in the ingestion of mucus.	Univ Texas, Med Branch, Inst Marine Biomed, Marine Resource Ctr Cephalopods, Galveston, TX 77555 USA; Univ Fed Rio Grande Sul, Dept Oceanog, BR-96201900 Rio Grande, Brazil	University of Texas System; University of Texas Medical Branch Galveston; Universidade Federal do Rio Grande do Sul	Vidal, EAG (通讯作者)，Univ Texas, Med Branch, Inst Marine Biomed, Marine Resource Ctr Cephalopods, 301 Univ Blvd, Galveston, TX 77555 USA.		Haimovici, Manuel/AAU-9161-2020; Vidal, Erica Alves Gonzalez/C-9032-2013	Haimovici, Manuel/0000-0003-1741-8182; Vidal, Erica Alves Gonzalez/0000-0003-4781-8670				ALLDREDGE AL, 1993, DEEP-SEA RES PT I, V40, P1131, DOI 10.1016/0967-0637(93)90129-Q; ALLDREDGE AL, 1988, PROG OCEANOGR, V20, P41, DOI 10.1016/0079-6611(88)90053-5; [Anonymous], 1984, MARINE FISH LARVAE; BALCH N, 1985, Vie et Milieu, V35, P243; BALCH N, 1988, MALACOLOGIA, V29, P103; BALDWIN BS, 1995, MAR ECOL PROG SER, V120, P135, DOI 10.3354/meps120135; BIDDANDA BA, 1988, MAR ECOL PROG SER, V42, P89, DOI 10.3354/meps042089; BIDDANDA BA, 1985, MAR ECOL PROG SER, V20, P241, DOI 10.3354/meps020241; BIDDANDA BA, 1988, MAR ECOL PROG SER, V42, P79, DOI 10.3354/meps042079; BOLETZKY S V, 1983, Memoirs of the National Museum of Victoria, V44, P147; BOUCAUDCAMOU E, 1995, B MAR SCI, V57, P313; Brock T.D., 1991, BIOL MICROORGANISMS, VSixth; DAVOLL PJ, 1986, MAR ECOL PROG SER, V33, P111, DOI 10.3354/meps033111; Durward R.D., 1980, International Commission for the Northwest Atlantic Fisheries Selected Papers, V6, P7; Haimovici M., 1995, ICES Marine Science Symposia, V199, P414; HOBBIE JE, 1977, APPL ENVIRON MICROB, V33, P1225, DOI 10.1128/AEM.33.5.1225-1228.1977; Lalli C.M., 1989, PELAGIC SNAILS; Lee PG, 1994, MAR FRESHW BEHAV PHY, V25, P35, DOI 10.1080/10236249409378906; LINLEY EAS, 1984, B MAR SCI, V35, P409; LINLEY EAS, 1986, AM MALACOL B, V4, P55; O'DOR R K, 1985, Vie et Milieu, V35, P267; Okiyama M., 1965, Bulletin of the Japan Sea Regional Fisheries Research Laboratory, VNo. 15, P39; Okutani T., 1983, Biological Oceanography, V2, P401; SOROKIN YI, 1977, MAR BIOL, V41, P107, DOI 10.1007/BF00394018; VECCHIONE M, 1991, B MAR SCI, V49, P300; VECCHIONE M, 1991, FISH B-NOAA, V89, P515; Vecchione M., 1987, P61; VIDAL EAG, 1994, ANTARCT SCI, V6, P275, DOI 10.1017/S0954102094000416; VIDAL EAG, 1994, THESIS U RIO GRANDE	29	46	46	0	5	ROSENSTIEL SCH MAR ATMOS SCI	MIAMI	4600 RICKENBACKER CAUSEWAY, MIAMI, FL 33149 USA	0007-4977			B MAR SCI	Bull. Mar. Sci.	SEP	1998	63	2					305	316						12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	161BV					2025-03-11	WOS:000078268900005
J	Head, MJ				Head, MJ			New goniodomacean dinoflagellates with a compound hypotractal archeopyle from the Late Cenozoic: Capisocysta Warny and Wrenn, emend.	JOURNAL OF PALEONTOLOGY			English	Article							PLIOCENE; CYSTS	Two new species of dinoflagellate are described from the upper Cenozoic of the North Atlantic region. They are assigned to the goniodomacean genus Capisocysta Warny and Wrenn, 1997 emend., whose archeopyle uniquely forms by the extensive and exclusive dissociation of hypocystal plates. Capisocysta lata new species is recorded from the upper lower Pliocene Coralline Crag Formation of eastern England, the lower and upper Pliocene of the subsurface Great Bahama Bank, and as a living cyst from Phosphorescence Bay, Puerto Rico. Capisocysta lyellii new species is reported from the Coralline Crag Formation of eastern England. Capisocysta provides the only unambiguous example of a hypocystal archeopyle in the order Gonyaulacales and the only example of a hypotractal archeopyle in the division Dinoflagellata. The spherical, proximate cysts have pre-formed lines of weakness that occur exclusively on the hypocyst, where they follow plate boundaries. Upon excystment, these sutures facilitate the separate release of plates 2-6''', ps, 1p, and 1''''. Sulcal plates Is and rs and postcingular plate 1"' typically remain attached to the epicyst, forming a distinctive hyposulcal tab. The single antapical plate in C. lata is represented in C. lyellii by two plates (left and right first antapical homologues) that are released separately. Capisocysta has a tropical to warm temperate distribution today. It thrived and perhaps formed blooms in tropical carbonate platform environments of the Bahamas during the Pliocene, and might prove to be a useful indicator of very warm intervals within the Pliocene of higher latitude regions including the southern North Sea basin. To facilitate discussion of Capisocysta, several morphological terms have been modified or newly introduced. These terms more precisely describe archeopyle position and extent in dinoflagellates.	Univ Toronto, Dept Geol, Ctr Earth Sci, Toronto, ON M5S 3B1, Canada	University of Toronto	Head, MJ (通讯作者)，Univ Toronto, Dept Geol, Ctr Earth Sci, Toronto, ON M5S 3B1, Canada.							[Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1885, HG BRONNS KLASSEN OR; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Dale B., 1983, P69; DAVEY RJ, 1966, GEOLOGY S, V3, P53; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P263, DOI 10.2307/1485875; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P83; Dorhofer G, 1980, LIFE SCI MISCELLANEO; Drugg W.S., 1970, N AM PAL CONV CHIC G, P809; EBERLL GP, 1997, 166 OC DRILL PROGR, P23; EVITT WR, 1977, 7624 GEOL SURV CAN, P1; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Harding Ian C., 1995, Palaeontology (Oxford), V37, P825; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 1997, J PALEONTOL, V71, P165, DOI 10.1017/S0022336000039123; HEAD MJ, IN PRESS DAWN QUATER; Hodgson G.E., 1987, P44; LEFEVRE M., 1933, BULL MUS NATION HIST NAT [PARIS], V5, P415; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; Levandowsky M., 1987, Botanical Monographs (Oxford), V21, P360; LIENGJARERN M, 1980, Palaeontology (Oxford), V23, P475; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; LYELL C, 1839, P GEOLOGICAL SOC LON, V3, P126; Manum Svein B., 1995, Palynology, V19, P183; MCLEAN DM, 1966, MICROPALEONTOLOGY, V22, P347; MORGENROTH P., 1966, PALAEONTOGRAPHICA, V119, P1; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; ROSSIGNOL MARTINE, 1962, POLLEN SPORES, V4, P121; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; WALL D, 1971, J PHYCOL, V7, P221, DOI 10.1111/j.1529-8817.1971.tb01507.x; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; WALL D., 1967, PALAEONTOLOGY, V10, P95; Warny SA, 1997, REV PALAEOBOT PALYNO, V96, P281, DOI 10.1016/S0034-6667(96)00056-5; WESTPHAL H, ADV CARBONATE SEQUEN; WESTPHAL H, 1997, THESIS C ALBRECHTS U; WILLIAMS GL, CONTRIBUTIONS SERI A, P78; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Wrenn JH, 1989, PALYNOLOGY, V13, P289	39	17	17	0	0	PALEONTOLOGICAL SOC INC	LAWRENCE	810 EAST 10TH ST, LAWRENCE, KS 66044 USA	0022-3360			J PALEONTOL	J. Paleontol.	SEP	1998	72	5					797	809		10.1017/S0022336000027153	http://dx.doi.org/10.1017/S0022336000027153			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	121AD					2025-03-11	WOS:000075989200001
J	Wood, SE; Gorin, GE				Wood, SE; Gorin, GE			Sedimentary organic matter in distal clinoforms of Miocene slope sediments: Site 903 of ODP Leg 150, offshore New Jersey (USA)	JOURNAL OF SEDIMENTARY RESEARCH			English	Article							STRATIGRAPHIC FRAMEWORK; SE FRANCE; CARBONATES; ATLANTIC; FACIES; MARGIN; MODEL	A study of sedimentary organic matter (palynofacies) was carried out for paleoenvironmental purposes in the siliciclastic, Miocene upper-slope sediments of Ocean Drilling Project (ODP) Site 903, Leg 150, Two groups of organic constituents were distinguished: a fraction derived from the continent, made of phytoclasts, pollen, and spores, and a marine fraction consisting of amorphous organic matter (AOM), dinoflagellate cysts, and foraminiferal linings, Palynofacies data reflect the overall trend of the Haq et al, (1987) eustatic curve. The rise in eustatic sea level during the early Miocene is associated with high levels of AOM and total organic carbon, indicative of low-energy, starved, deeper-water conditions. In contrast, during a fall in sea level from the early middle Miocene to the late Miocene. AOM became diluted by continental organic matter associated with prograding clinoforms. Site 903 penetrated the distal part of progradational, well-developed clinoforms of Miocene age. Most of the seismic reflections bounding these clinoforms are the pelagic correlatives to sequence boundaries observed beneath the adjacent shelf, and they correlate well with the sea-level records of Haq et al, (1987), Within packages of clinoforms, palynofacies show important percentage variations. In most cases, seismic reflectors (i.e., sequence boundary correlatives) seem to be associated with an increase in AOM indicative of a condensed section. Seismic stratigraphic interpretation landward of Site 903 indicates that these condensed sections may correspond to the downlap surface of prograding lowstand or highstand wedges. Above the condensed section, AOM becomes progressively diluted by the renewed progradation of terrigenous sediments. The concentration of marine AOM near sequence boundaries, the ages of which correlate with the Haq et al, (1987) eustatic curve, tends to demonstrate that the distribution of AOM in the middle and upper Miocene slope sediments at Site 903 may be to a large extent related to relative sea-level variations.	Univ Geneva, Dept Geol & Paleontol, CH-1211 Geneva 4, Switzerland	University of Geneva	Wood, SE (通讯作者)，Tile Cottage,6 Railway Terrace,Witton Le Wear, Bishop Auckland DL14 01L, Durham, England.		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Sediment. Res.	SEP	1998	68	5	A				856	868		10.2110/jsr.68.856	http://dx.doi.org/10.2110/jsr.68.856			13	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	125JC					2025-03-11	WOS:000076233600016
J	Ellegaard, M; Oshima, Y				Ellegaard, M; Oshima, Y			Gymnodinium nolleri Ellegaard et Moestrup sp. ined. (Dinophyceae) from Danish waters, a new species producing Gymnodinium catenatum-like cysts: molecular and toxicological comparisons with Australian and Spanish strains of Gymnodinium catenatum	PHYCOLOGIA			English	Article							GYRODINIUM-IMPUDICUM; RECENT SEDIMENTS; DINOFLAGELLATE; TEMPERATURE; TASMANIA; GROWTH; GENE	Gymnodinium nolleri Ellegaard et Moestrup sp. ined. (Dinophyceae) strains established from cysts collected at three marine locations in Denmark were compared to Australian and Spanish strains of Gymnodinium catenatum with respect to morphology, molecular characteristics, and content of paralytic shellfish poisoning (PSP) toxins. The Spanish and Australian strains were identical, but the Danish strains were smaller, formed only two-cell chains, and differed in rRNA sequence [large subunit (LSU) rRNA, D3 domain], and isozymes (malate dehydrogenase, esterase, phosphoglucoisomerase, and superoxide dismutase). None of the Danish strains tested contained detectable amounts of PSP toxins. In crossing experiments, Danish/Danish, Spanish/Spanish, and Spanish/Australian crosses produced cysts, but no resting cysts were found in Danish/Spanish or Danish/Australian crosses. The name Gymnodinium nolleri Ellegaard et Moestrup will be validly published separately.	Univ Copenhagen, Inst Bot, Dept Mycol & Phycol, DK-1353 Copenhagen K, Denmark; Tohoku Univ, Fac Agr, Dept Appl Biol Chem, Aoba Ku, Sendai, Miyagi 981, Japan	University of Copenhagen; Tohoku University	Univ Copenhagen, Inst Bot, Dept Mycol & Phycol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	mariane@bot.ku.dk	Ellegaard, Marianne/H-6748-2014					ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON RA, 1991, PROVASOLI GUILLARD C; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; BRAVO I, 1986, Investigacion Pesquera (Barcelona), V50, P313; BRAVO I, 1997, HARMFUL ALGAE NEWS, P16; CABOT EL, 1990, ESEE EYECALL SEQUENC; CEMBELLA AD, 1986, BIOCHEM SYST ECOL, V14, P311, DOI 10.1016/0305-1978(86)90107-9; COSTAS E, 1995, J PHYCOL, V31, P801, DOI 10.1111/j.0022-3646.1995.00801.x; DALE B, 1993, DEV MAR BIO, V3, P47; DALE B, 1993, DEV MAR BIO, V3, P53; DAUGBJERG N, 1994, J PHYCOL, V30, P991, DOI 10.1111/j.0022-3646.1994.00991.x; Doyle JJ., 1987, PHYTOCHEM B BOT SOC, V19, P11, DOI DOI 10.1016/0031-9422(80)85004-7; ELLEGAARD M, 1993, J PHYCOL, V29, P418, DOI 10.1111/j.1529-8817.1993.tb00142.x; ELLSTRAND NC, 1984, AM NAT, V123, P819, DOI 10.1086/284241; ENGELEN AH, 1995, THESIS U GRONINGEN; Fraga S, 1995, PHYCOLOGIA, V34, P514, DOI 10.2216/i0031-8884-34-6-514.1; Graham Herbert W, 1943, TRANS AMER MICROSC SOC, V62, P259, DOI 10.2307/3223028; HALLEGRAEFF GM, 1993, PHYCOLOGIA, V32, P79, DOI 10.2216/i0031-8884-32-2-79.1; HAYHOME BA, 1987, J PHYCOL, V23, P573; HAYHOME BA, 1989, MAR BIOL, V101, P427, DOI 10.1007/BF00541643; HAYHOME BA, 1983, AM J BOT, V70, P1165, DOI 10.2307/2443286; Larsen N.H., 1994, SCANDINAVIAN CULTURE; LOEBLICH AR, 1975, J PHYCOL, V11, P80, DOI 10.1111/j.1529-8817.1975.tb02752.x; MICHOT B, 1990, EUR J BIOCHEM, V188, P219, DOI 10.1111/j.1432-1033.1990.tb15393.x; NEHRING S, 1995, J PLANKTON RES, V17, P85, DOI 10.1093/plankt/17.1.85; NORDBERG K, 1988, MAR GEOL, V83, P135, DOI 10.1016/0025-3227(88)90056-4; OSHIMA Y, 1993, DEV MAR BIO, V3, P907; OSHIMA Y, 1987, TOXICON, V25, P1105, DOI 10.1016/0041-0101(87)90267-4; Oshima Y., 1995, IOC MANUALS GUIDES, V33, P81; Paulmier G, 1992, RIDRV92007 IFREMER R, V1-108; PEPERZAK L, 1996, HARMFUL TOXIC ALGAL, P169; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; REES AJJ, 1991, PHYCOLOGIA, V30, P90, DOI 10.2216/i0031-8884-30-1-90.1; ROSENDAHL S, 1992, METHOD MICROBIOL, V24, P169, DOI 10.1016/S0580-9517(08)70092-8; Sako Y., 1989, P325; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; SANGER F, 1977, P NATL ACAD SCI USA, V74, P5463, DOI 10.1073/pnas.74.12.5463; SCHOLIN C, 1995, PHYCOLOGIA, V34, P471; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; TAKAYAMA H, 1991, Bulletin of Plankton Society of Japan, V38, P53; Weeden N. F., 1989, ISOZYMES PLANT BIOL, P46; Weidema IR, 1996, HEREDITAS, V124, P121, DOI 10.1111/j.1601-5223.1996.00121.x	44	26	27	2	11	ALLEN PRESS INC	LAWRENCE	810 E 10TH ST, LAWRENCE, KS 66044 USA	0031-8884			PHYCOLOGIA	Phycologia	SEP	1998	37	5					369	378		10.2216/i0031-8884-37-5-369.1	http://dx.doi.org/10.2216/i0031-8884-37-5-369.1			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	140BQ					2025-03-11	WOS:000077067200007
J	Williams, RW				Williams, RW			Dinium-Alpha: a chronostratigraphical range, morphology and photomicrography database builder for dinoflagellate cyst taxa	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article; Proceedings Paper	IXth International Palynological Congress	JUN 23-25, 1996	HOUSTON, TEXAS			data storage; data retrieval; computer programs; dinoflagellates; morphology; biostratigraphy		Dinium-Alpha is a database front end application which runs under Microsoft Windows(TM) 95/NT. Dinium-Alpha provides the user with (1) a palynologically intuitive graphical interface which stores and retrieves morphological criteria, stratigraphical ranges and digital images of cyst taxa, and (2) an identification key which searches for cyst taxa on the basis of one or more user-selectable morphological criteria in combination with chronostratigraphical range parameters. Morphological criteria are depicted on the graphical interface by self-explanatory icons subdivided into four main categories: basic morphology, archeopyle type, cyst wall and chronostratigraphical ranges. Chronostratigraphical ranges are stored and queried using scrollable time scales accommodating several search strategies. Dinium-Alpha allows the user to search for cyst taxa using any combination of morphological criteria and chronostratigraphical range parameters. Chronostratigraphical ranges for individual taxa may also be differentiated according to paleogeographical or modern geographical realms (i.e. Tethyan, Boreal, North Sea etc.) and selectively queried. Dinium-Alpha is interfaced with portions of DinoSys, a comprehensive taxonomy and image database application developed by LPP, Laboratory of Palaeobotany and Palynology, University of Utrecht, enabling the user to retrieve information from the DinoSys database. (C) 1998 Elsevier Science B.V. All rights reserved.	Norwegian Petr Directorate, N-4001 Stavanger, Norway		Williams, RW (通讯作者)，Norwegian Petr Directorate, PB 600, N-4001 Stavanger, Norway.							CANDE SC, 1992, J GEOPHYS RES-SOL EA, V97, P13917, DOI 10.1029/92JB01202; DUCHENE RJ, 1986, B CTR RECH EXPLOR PR, V12, P1; EVITT WR, 1985, SPOROPOLLENIN DINOFA; GRADSTEIN FM, 1994, J GEOPHYS RES-SOL EA, V99, P24051, DOI 10.1029/94JB01889; MONTEIL E, 1990, B CENT RECH EXPL, V14, P597; STOVER LE, 1978, STANFORD U PUBL GEOL, V15; von Benedek P.N., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V162, P265; WILLIAMS GL, 1978, AM ASS STRATIGR P 2A, V2	8	0	0	0	1	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	SEP	1998	103	1-2					45	57		10.1016/S0034-6667(98)00025-6	http://dx.doi.org/10.1016/S0034-6667(98)00025-6			13	Plant Sciences; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	139QM					2025-03-11	WOS:000077040900005
J	Mahmoud, MS				Mahmoud, MS			Palynological dating of the Quseir formation, Kharga oasis (Egypt)	ARAB GULF JOURNAL OF SCIENTIFIC RESEARCH			English	Article								Previously reported fossil assemblages in the Quseir Formation do not contribute to definite age assessment. The formation was assigned a middle to late Campanian age according to its stratigraphic position below the well-dated (Campanian-Maastrichtian) Duwi (Phosphate) Formation No palynological work has previously been carried out on the Quseir Formation. Some arenaceous foraminifers (Campanian and Maastrichtian) were recorded from the Quseir Formation at Gebel Abu Had and Gebel Duwi (Eastern Desert). In the present study well-preserved palynomorphs have been recovered from shales equivalent to the Quseir Formation, in the Kharga subsurface section, Kharga Oasis. The presence of relatively large angiosperm pollen (e.g. Tricolpites spp., > 25 mu m) co-occurring with rare Dinogymnium dinocyst species indicate a Campanion age for the Quseir Formation. Moreover, pre-Turonian pollen (e.g. Classopollis and Eucommiidites) are lacking. The nature and frequency of the recovered palynomorphs imply shallow water deposition. This is essentially inferred from the high percentages of land-derived miospores associated with the dominance of palynofacies debris, accompanied by low percentages of marine dinoflagellate cysts. From the data, the deposition of the Quseir Formation began shallower tin the topmost parts of the formation) and were deepening upwards as documented in the overlying Duwi Formation.	Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt	Egyptian Knowledge Bank (EKB); Assiut University	Mahmoud, MS (通讯作者)，Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt.		Mahmoud, Magdi/I-8094-2019					Abdel Mohsen S., 1986, NEUES JB GEOL PAL, V6, P321; [Anonymous], 1957, Bulletin de I'Institut du desert d'Egypte, V1, P35; Awad G.A., 1965, EGYPT GEOL SURV PAP, V77, P1; BOLTENHAGEN E, 1977, CAHIERS MICROPALEONT; Hendriks F., 1984, Stratigr Sedimentol Framew, V50, P117; Hermina M., 1990, GEOLOGY EGYPT, P259; KEDVES M, 1986, Z GEOL WISSENSCHAFT, V14, P331; KENAWY AI, 1976, ACTA MINERALOGICA PE, V22, P311; LEEREVELD H, 1990, STUIFMAIL PALAEOBOTA, V8, P13; MAHMOUD MS, 1993, B FS ASSIUT U, V22, P113; MOHSEN SA, 1992, J AFR EARTH SCI, V14, P567, DOI 10.1016/0899-5362(92)90089-U; OMRAN AM, 1993, N JB GEOL PALAONT MO, V6, P345; Rauscher R., 1982, Sci. Geol. Bull., V35, P97; SAAD SL, 1976, POLLEN SPORES, V15, P407; SCHRANK E, 1992, CRETACEOUS RES, V13, P351, DOI 10.1016/0195-6671(92)90040-W; Schrank E., 1987, BERLINER GEOWISS ABH, V75, P249, DOI DOI 10.1016/0195-6671(92)90040-W; SRIVASTAVA SK, 1978, BIOL MEM, V3, P1; Taylor TN, 1981, PALAEOBOTANY INTRO F	18	4	4	0	0	ARAB BUREAU EDUCATION GULF STATES	RIYADH	PO BOX 94693, RIYADH 11614, SAUDI ARABIA	1015-4442			ARAB GULF J SCI RES	Arab Gulf J. Sci. Res.	AUG	1998	16	2					267	281						15	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	159CR					2025-03-11	WOS:000078154700002
J	Núñez-Betelu, K; Hills, LV				Núñez-Betelu, K; Hills, LV			A late Coniacian ceratioid dinoflagellate cyst, <i>Odontochitina octopus</i> sp.nov., from the Kanguk Formation, Canadian Arctic	CANADIAN JOURNAL OF EARTH SCIENCES			English	Article								A new species of dinoflagellate cyst, Odontochitina octopus sp.nov., is described from the Upper Cretaceous Kanguk Formation of the Sverdrup Basin, Canadian Arctic Islands. The features that support the proposal of this new species also necessitate the emendation of the genus. Odontochitina octopus is a large, cornucavate, and ceratioid cyst with four finger-like terminations on the apical horns and two terminations on both the postcingular and antapical horns. These finger-like terminations are unique to this new species and are formed by the detachment of the paraplates at mid-length of each horn. All other features of O. octopus conform with the previous description of the genus. In the Family Ceratiaceae four plates form the apical horn, whereas two plates are involved in both the postcingular and antapical horns. In O. octopus the mid-length detachment of the horn-forming paraplates seems to have developed the finger-like terminations. Since the nature and amount of pores and perforations in other species of Odontochitina are variable and possibly linked to changes in the environment, the presence of the multiple-fingered O. octopus in a single widespread horizon might also be indicative of short-lived unusual environmental conditions. At this horizon, which has been dated as late Coniacian by the ammonite Scaphites depressus Reeside, the palynomorph assemblage is highly dominated by marine species.	Univ Basque Country, Dept Stratig & Paleontol, Bilbao 48080, Basque Country, Spain; Univ Calgary, Dept Geol & Geophys, Calgary, AB T2N 1N4, Canada	University of Basque Country; University of Calgary	Univ Basque Country, Dept Stratig & Paleontol, POB 644, Bilbao 48080, Basque Country, Spain.	gpbnubek@lg.ehu.es						Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1985, SPOROPOLLENIN DINOFL; BINT A N, 1986, Palynology, V10, P135; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; COOKSON ISABEL C., 1956, AUSTRALIAN JOUR MARINE AND FRESHWATER RES, V7, P183; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; Deflandre G., 1935, Bulletin Biologique de la France et de la Belgique, V69, P213; DEFLANDRE G, 1955, AUSTR J MARINE FRESH, V6, P243; Evitt W.R., 1967, Stanford University Publications, Geological Sciences, V10, P1; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P158, DOI 10.1073/pnas.49.2.158; EVITT WR, 1963, P NATL ACAD SCI USA, V49, P298, DOI 10.1073/pnas.49.3.298; EVITT WR, 1977, 7624 GEOL SURV CAN; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; HAPPACHKASAN C, 1982, ARCH PROTISTENKD, V125, P181, DOI 10.1016/S0003-9365(82)80016-X; HILLS LV, 1994, CAN J EARTH SCI, V31, P733, DOI 10.1139/e94-066; Ioannides N. S., 1986, GEOLOGICAL SURVEY CA, V371; Lentin J.K., 1993, AM ASS STRATIGRAPHIC, V28; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; NORVICK MS, 1975, BUREAU MINERAL RESOU, V151, P89; Nunez-Betelu L., 1992, Revista Espanola de Paleontologia, V7, P185; Nunez-Betelu L., 1992, REV ESPANOLA PALEONT, V7, P197; Nunez-Betelu L.K, 1992, P 1992 INT C ARCT MA, P135; Nunez-Betelu L. K. M., 1994, THESIS U CALGARY CAL; Nunez-Betelu L.M., 1991, M.Sc. thesis; Nunez-Betelu LK, 1994, 2489 GEOL SURV CAN; NUNEZBETELU LK, 1995, P 1994 INT C ARCT MA, P43; NUNEZBETELU LK, 1995, P 1994 INT C ARCT MA, P54; PASCHER A, 1914, DTSCH BOT GESELLSCHA, V29, P193; Pollingher U., 1987, Botanical Monographs (Oxford), V21, P502; REESIDE JOHN B., 1927, U S GEOL SURV PROF PAPER, V150-A, P1; SARJEANT WAS, 1966, GEOLOGY S, V3, P199; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; VONSCHRANK F, 1793, NATURFORSCHER HALLE, V27, P26; Wall D., 1975, Micropalaeontology, V21, P14, DOI 10.2307/1485153; WALL J H, 1983, Bulletin of Canadian Petroleum Geology, V31, P246; Wetzel O., 1933, PALAEONTOGRAPHICA, V77, P141; Willey Arthur, 1909; WILLIAM SGL, 1978, AM ASS STRATIGRAPH A, V2	39	7	9	0	0	CANADIAN SCIENCE PUBLISHING, NRC RESEARCH PRESS	OTTAWA	65 AURIGA DR, SUITE 203, OTTAWA, ON K2E 7W6, CANADA	0008-4077	1480-3313		CAN J EARTH SCI	Can. J. Earth Sci.	AUG	1998	35	8					923	930		10.1139/e98-044	http://dx.doi.org/10.1139/e98-044			8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	157JG					2025-03-11	WOS:000078057300004
J	Rengefors, K; Anderson, DM				Rengefors, K; Anderson, DM			Environmental and endogenous regulation of cyst germination in two freshwater dinoflagellates	JOURNAL OF PHYCOLOGY			English	Article						anoxia; Ceratium hirundinella; cyst; dinoflagellate; dormancy germination; Peridinium aciculiferum; seasonal succession	DINOPHYCEAE RESTING CYSTS; GONYAULAX-TAMARENSIS; SCRIPPSIELLA-TROCHOIDEA; CERATIUM-HIRUNDINELLA; SEASONAL SUCCESSION; LAKE; TEMPERATURE; GROWTH; WATER; RECRUITMENT	The role of excystment in relation to seasonal succession was investigated in two freshwater dinoflagellates, Ceratium hirundinella (O.F. Muller) Dujardin and Peridinium aciculiferum (Lemmermann). Field studies and laboratory experiments were performed to determine which factors regulate the timing of cyst germination. Environmental factors (temperature, light, nutrients, and anoxia) and endogenous factors (maturation period and biological clock) were investigated. Our main results indicate that temperature and internal maturation period determine when germination can, occur. C. hirundinella had a maturation period of 4.5 months and germinated in the laboratory and in the field at temperatures above 6 degrees C. P. aciculiferum had a maturation period of 2.5 months and germinated in the laboratory and in the field at temperatures below 7 degrees C. In addition, our results indicated that both species were regulated by a biological clock. Furthermore, anoxia prevented the germination of C. hirundinella, contrary to results in earlier studies. To conclude, we could explain the appearance in plankton of the two dinoflagellate species through two main factors regulating excystment, that is, temperature and maturation period.	Uppsala Univ, Limnol Inst, SE-75236 Uppsala, Sweden; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	Uppsala University; Woods Hole Oceanographic Institution	Rengefors, K (通讯作者)，Uppsala Univ, Limnol Inst, Norbyvagen 20, SE-75236 Uppsala, Sweden.	Karin.Rengefors@limno.uu.se	Rengefors, Karin/K-5873-2019	Rengefors, Karin/0000-0001-6297-9734				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 DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; BEAKES GW, 1988, CAN J BOT, V66, P1054, DOI 10.1139/b88-151; BINDER BJ, 1987, J PHYCOL, V23, P99; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BLANKLEY FW, 1976, LIMNOL OCEANOGR, V21, P457; BLOMQVIST P, 1995, CAN J FISH AQUAT SCI, V52, P551, DOI 10.1139/f95-056; BLOMQVIST P, 1994, ARCH HYDROBIOL, V132, P141; Boero F, 1996, TRENDS ECOL EVOL, V11, P177, DOI 10.1016/0169-5347(96)20007-2; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Dale B., 1983, P69; ENDO T, 1984, Bulletin of Plankton Society of Japan, V31, P23; Fryxell G.A., 1983, Survival Strategies of the algae, P1; HAKANSSON L, 1978, SCRIPTA LIMNOLOGICA, V468; HANSSON LA, 1994, CAN J FISH AQUAT SCI, V51, P2825, DOI 10.1139/f94-281; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; Huber G., 1922, Z BOTANIK, V14, P337; Huber G., 1923, FLORA JENA, V116, P114; KRUPA D, 1981, EKOL POL-POL J ECOL, V29, P545; KRUPA D, 1981, EKOL POL-POL J ECOL, V29, P571; LUTZ RV, 1992, MAR BIOL, V114, P241, DOI 10.1007/BF00349525; 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; NAUWERCK ARNOLD, 1963, SYMBOLAE BOT UPSALIENSIS, V17, P1; Nehring S, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; PETTERSSON K, 1985, INT REV GES HYDROBIO, V70, P527, DOI 10.1002/iroh.19850700407; Pfiester L.A., 1987, Botanical Monographs (Oxford), V21, P611; POLLINGHER U, 1993, AQUAT SCI, V1, P10; RAHMBERG L, 1976, THESIS UPPSALA U UPP; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; Reynolds C.S., 1984, ECOLOGY FRESHWATER P; SOMMER U, 1986, ARCH HYDROBIOL, V106, P433; Von Stosch HA., 1973, Br Phycol J, V8, P105; Wall D., 1971, Geoscience Man, V3, P1; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	41	86	99	5	26	WILEY-BLACKWELL	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	AUG	1998	34	4					568	577		10.1046/j.1529-8817.1998.340568.x	http://dx.doi.org/10.1046/j.1529-8817.1998.340568.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	116FB					2025-03-11	WOS:000075712400002
J	Brinkhuis, H; Bujak, JP; Smit, J; Versteegh, GJM; Visscher, H				Brinkhuis, H; Bujak, JP; Smit, J; Versteegh, GJM; Visscher, H			Dinoflagellate-based sea surface temperature reconstructions across the Cretaceous-Tertiary boundary	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						dinoflagellate cysts; Cretaceous-Tertiary boundary; palaeoclimate	EL-KEF; CALCAREOUS NANNOFOSSILS; STABLE ISOTOPE; TUNISIA; EOCENE; CYSTS; BIOSTRATIGRAPHY; STRATIGRAPHY; FORAMINIFERA; EXTINCTIONS	Quantitative analysis of organic-walled dinoflagellate cyst (dinocyst) assemblages from closely spaced samples across the Cretaceous-Tertiary boundary (KTB) at El Kef (NW Tunisia), Caravaca (SE Spain) and Stevns Klint (E Denmark) allows for reconstructions of sea surface temperature (SST) trends. The combined dinocyst-based SST curves indicate relatively stable warm conditions during the latest Maastrichtian in contrast to strongly fluctuating and on average cooler conditions during the earliest Danian. In detail, the results indicate cooling across the KTB, immediately followed by an interval of pronounced warming, the latter recorded in all studied sections. Two more cooling pulses may be recognized in the overlying interval followed by a gradual return to stable, relatively warm conditions. Our data furthermore show that these KTB-related climatic changes invoked distinct migration among organic-walled cyst-producing dinoflagellates, a group not pushed to extinction at the KTB, recordable in both hemispheres. Recent models predict periods varying between several months to 8-13 yr of global cooling ('impact winter') and reduced solar transmission as a direct result of the Chicxulub KTB impact, followed by relatively long-term, excess CO2-related global warming. Our results are in line with such models, but suggest that the impact-related cooling phase may have lasted longer, and that marked climatic instability continued to some 100,000 yrs following the KTB event(s). (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Lexis Grp, Blackpool FY3 8NA, Lancs, England; Vrije Univ Amsterdam, Inst Earth Sci, Dept Sedimentary Geol, NL-1081 HV Amsterdam, Netherlands; Netherlands Inst Sea Res, NIOZ, Div Marine Biogeochem, NL-1790 AB Den Burg, Texel, Netherlands	Utrecht University; Vrije Universiteit Amsterdam; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Brinkhuis, H (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	h.brinkhuis@biol.ruu.nl	Brinkhuis, Henk/B-4223-2009; Versteegh, Gerard J.M./H-2119-2011	Smit, Jan/0000-0002-6070-4865; Brinkhuis, Henk/0000-0003-0253-6610; Versteegh, Gerard J.M./0000-0002-9320-3776				[Anonymous], NEOGENE QUATERNARY D; Askin R.A., 1988, Geological Society of America Memoir, V169, P155; Barrera E, 1990, PALEOCEANOGRAPHY, V5, P867, DOI 10.1029/PA005i006p00867; 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, 1988, REV PALAEOBOT PALYNO, V56, P5, DOI 10.1016/0034-6667(88)90071-1; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Brinkhuis H, 1994, GFF, V116, P46, DOI 10.1080/11035899409546146; BURKHOLDER JM, 1992, NATURE, V358, P407, DOI 10.1038/358407a0; COWIE JW, 1989, EPISODES, V12, P79, DOI 10.18814/epiiugs/1989/v12i2/003; DALE B, 1985, NORSK GEOL TIDSSKR, V65, P97; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DAMASSA S P, 1988, Palynology, V12, P167; DECONINCK J, 1982, GEOL MIJNBOUW, V61, P173; ELLIOT DH, 1994, GEOLOGY, V22, P675, DOI 10.1130/0091-7613(1994)022<0675:IADATC>2.3.CO;2; ESHET Y, 1994, MAR MICROPALEONTOL, V23, P231, DOI 10.1016/0377-8398(94)90014-0; GAINES G, 1984, J PLANKTON RES, V6, P1057, DOI 10.1093/plankt/6.6.1057; GINSBURG RN, 1997, MAR MICROPALEONTOL, V29, P65; HABIB D, 1992, GEOLOGY, V20, P157; Habib D, 1994, New Developments Regarding the K/T Event and other Catastrophes in Earth History. 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F., 1987, CANOCO A FORTRAN PRO; Ter Braak C.J.F., 1987, THESIS U WAGENINGEN; ter Braak C.J.F., 1990, UPDATED NOTES CANOCO; VERSLUIS AJ, 1994, J PHOTOCH PHOTOBIO B, V23, P141, DOI 10.1016/1011-1344(94)06998-0; VERSTEEGH GJM, 1994, REV PALAEOBOT PALYNO, V84, P181, DOI 10.1016/0034-6667(94)90050-7; Vonhof HB, 1996, GEOL MIJNBOUW, V75, P275; Walliser O.H., 1986, LECTURE NOTES EARTH, V8, P381; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; WILSON GJ, 1978, NEW ZEAL J GEOL GEOP, V21, P75, DOI 10.1080/00288306.1978.10420723; Wilson GJ., 1974, THESIS U NOTTINGHAM	69	155	164	0	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	AUG	1998	141	1-2					67	83		10.1016/S0031-0182(98)00004-2	http://dx.doi.org/10.1016/S0031-0182(98)00004-2			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	ZY418					2025-03-11	WOS:000074619300005
J	Rengefors, K; Karlsson, I; Hansson, LA				Rengefors, K; Karlsson, I; Hansson, LA			Algal cyst dormancy: a temporal escape from herbivory	PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES			English	Article						dinoflagellates; cysts; dormancy; germination; predator-avoidance strategy; herbivory	DINOFLAGELLATE; DAPHNIA; ZOOPLANKTON; PHOSPHORUS; DIAPAUSE; GROWTH; LAKE	Many phytoplankton species form resting cysts and remain dormant for part of the year. The subsequent excystment is regulated by the external environment and internal maturation processes. Here we assessed the excystment of the dinoflagellates Ceratium hirundinella and Peridinium aciculiferum in relation to herbivores and temperature in laboratory and field studies. C. hirundinella, which has a grazer-resistant morphology, forms summer blooms, whereas P. aciculiferum, which is vulnerable to grazers, grows underneath the ice during winter. In our study, herbivore abundance, and thereby grazing pressure, was low during periods when water temperatures were low, and the abundance of P. aciculiferum was high. In the laboratory experiment, excystment of C. hirundinella occurred at high temperatures irrespective of whether zooplankton exudate was added or not, whereas at intermediate temperatures, excystment was lower if zooplankton exudate was added. Germination of P. aciculiferum cysts was lower in the presence of exudate from a zooplankton culture than in controls at all temperatures. Our studies suggest that dinoflagellates use the presence of zooplankton in addition to temperature as a cue to determine when to excyst. Consequently, not only abiotic factors, but also the composition of the food web, may determine succession and composition of phytoplankton communities.	Uppsala Univ, Dept Limnol, S-75236 Uppsala, Sweden; Inst Ecol Limnol, S-22362 Lund, Sweden	Uppsala University	Rengefors, K (通讯作者)，Uppsala Univ, Dept Limnol, Norbyvagen 20, S-75236 Uppsala, Sweden.	karin.rengefors@1imno.uu.se	Hansson, Lars-Anders/HCI-2735-2022; Rengefors, Karin/K-5873-2019	Hansson, Lars-Anders/0000-0002-3035-1317; Rengefors, Karin/0000-0001-6297-9734				ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; BEAKES GW, 1988, CAN J BOT, V66, P1054, DOI 10.1139/b88-151; BERN L, 1994, FRESHWATER BIOL, V32, P105, DOI 10.1111/j.1365-2427.1994.tb00870.x; BERN L, 1990, J PLANKTON RES, V12, P1059, DOI 10.1093/plankt/12.5.1059; 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; Coleman A.W., 1983, P1; Dale B., 1983, P69; ENTZ GEZA, 1927, ARCH BALATONICUM, V1, P275; Hairston N.G. Jr, 1987, P281; Hairston Nelson G. Jr., 1996, P109; Hairston NG, 1996, ECOLOGY, V77, P2382, DOI 10.2307/2265740; HAKANSON L, 1978, SCRIPTA LIMNOLOGICA, V468, P1; Hansson LA, 1996, LIMNOL OCEANOGR, V41, P1312, DOI 10.4319/lo.1996.41.6.1312; Hansson LA, 1996, P ROY SOC B-BIOL SCI, V263, P1241, DOI 10.1098/rspb.1996.0182; Heaney S. I., 1985, MIGRATION MECH ADAPT, P114; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HENNING M, 1991, INT REV GES HYDROBIO, V76, P37, DOI 10.1002/iroh.19910760105; HESSEN DO, 1993, ARCH HYDROBIOL, V127, P129; Huber G., 1922, Z BOTANIK, V14, P337; Huber G., 1923, FLORA JENA, V116, P114; LAMPERT W, 1995, NATURE, V377, P479, DOI 10.1038/377479a0; LAMPERT W, 1994, LIMNOL OCEANOGR, V39, P1543, DOI 10.4319/lo.1994.39.7.1543; LINDSTROM K, 1991, J PHYCOL, V27, P207, DOI 10.1111/j.0022-3646.1991.00207.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; NAUWERCK ARNOLD, 1963, SYMBOLAE BOT UPSALIENSIS, V17, P1; PETTERSSON K, 1985, INT REV GES HYDROBIO, V70, P527, DOI 10.1002/iroh.19850700407; Pijanowska J, 1996, J PLANKTON RES, V18, P1407, DOI 10.1093/plankt/18.8.1407; Pollingher U., 1988, P134; POLLINGHER U, 1993, AQUAT SCI, V1, P10; Rengefors K, 1996, J PLANKTON RES, V18, P1753, DOI 10.1093/plankt/18.9.1753; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; RENGEFORS K, 1998, IN PRESS J PHYCOL, V34; RENGEFORS K, 1997, THESIS FACULTY SCI T; Reynolds C.S., 1984, ECOLOGY FRESHWATER P; SLUSARCZYK M, 1995, ECOLOGY, V76, P1008, DOI 10.2307/1939364; Sterner R.W., 1989, P107; WEYHENMEYER GA, 1996, THESIS FACULTY SCI T	39	108	123	3	34	ROYAL SOC	LONDON	6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND	0962-8452	1471-2954		P ROY SOC B-BIOL SCI	Proc. R. Soc. B-Biol. Sci.	JUL 22	1998	265	1403					1353	1358		10.1098/rspb.1998.0441	http://dx.doi.org/10.1098/rspb.1998.0441			6	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	103PV		Green Published			2025-03-11	WOS:000074967800013
J	Hathway, B; Macdonald, DIM; Riding, JB; Cantrill, DJ				Hathway, B; Macdonald, DIM; Riding, JB; Cantrill, DJ			Table Nunatak: a key outcrop of Upper Cretaceous shallow-marine strata in the southern Larsen Basin, Antarctic Peninsula	GEOLOGICAL MAGAZINE			English	Article							JAMES-ROSS-ISLAND; HUMMOCKY CROSS-STRATIFICATION; UNIDIRECTIONAL FLOWS; FOSSIL WOOD; NORTH; STRATIGRAPHY; SHELF; SEDIMENTATION; SEQUENCES; IRELAND	The northern, James Boss Island region of the Larsen Basin, on the eastern, back-are margin of the Antarctic Peninsula magmatic are, includes one of the thickest and most complete Upper Cretaceous sedimentary successions exposed in the Southern Hemisphere. However, the southern part of the basin remains poorly known, mainly owing to inaccessibility and lack of exposure. Table Nunatak, an isolated, l-km-long, 400-m-wide outcrop at the tip of Kenyon Peninsula, is the only known exposure of Upper Cretaceous or younger strata in this region. The 62-m-thick succession exposed there is assigned to the newly defined Table Nunatak Formation. It consists mainly of sharp-based, amalgamated beds of fine-grained sandstone up to 2.8 m thick, with subordinate intervals of intensely bioturbated mudstone. Wave ripples are present at some levels, and locally developed swaley cross-stratification provides evidence for storm-generated combined-flow deposition. However, most sandstone beds appear to be internally structureless apart from normal grading, and are interpreted as the direct suspension deposits of highly sediment-charged storm- and/or flood-related flows. The succession represents relatively nearshore deposition, probably at the mouth of a river or deltaic distributary channel. Charcoalified plant debris, abundant at the tops of some sandstone beds, suggests a periodically wildfire-swept hinterland forested largely by coniferous trees. Dinoflagellate cyst assemblages indicate a late Santonian age, and suggest correlation with the basal part of the Lachman Crags Member of the Santa Marta Formation (Marambio Group) on James Ross Island. Palaeocurrents, sandstone petrography and the high sediment supply rate proposed for the Table Nunatak Formation, suggest a relatively high-relief source area to the west, with large-scale erosion of granitoid plutons and metamorphic rocks, possibly related to are uplift during a mid-Cretaceous compressional episode. The formation is evidence of a major southward extension of the Upper Cretaceous strata exposed in the northern Larsen Basin, and suggests lateral continuity of shallow-marine deposition for at least 500-600 km along the Weddell Sea margin of the Antarctic Peninsula in Santonian times.	British Antarctic Survey, NERC, Cambridge CB3 0ET, England; British Geol Survey, Nottingham NG12 5GG, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Hathway, B (通讯作者)，British Antarctic Survey, NERC, High Cross,Madingley Rd, Cambridge CB3 0ET, England.		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G., 1985, PROVEN ARENITES, P165	69	9	9	0	8	CAMBRIDGE UNIV PRESS	NEW YORK	40 WEST 20TH STREET, NEW YORK, NY 10011-4211 USA	0016-7568			GEOL MAG	Geol. Mag.	JUL	1998	135	4					519	535		10.1017/S0016756898001241	http://dx.doi.org/10.1017/S0016756898001241			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	106TR					2025-03-11	WOS:000075167000006
J	Pedersen, GK; Larsen, LM; Pedersen, AK; Hjortkjaer, BF				Pedersen, GK; Larsen, LM; Pedersen, AK; Hjortkjaer, BF			The syn-volcanic Naajaat lake, Paleocene of West Greenland	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article; Proceedings Paper	1st Limno-Geological Congress on Research and Methods in Methods in Ancient and Modern Lacustrine Basins	AUG 21-25, 1995	COPENHAGEN, DENMARK			syn-volcanic lake; sediments; Paleocene; West Greenland; palaeolimnology	CARBON	The Naajaat lake in the Nuussuaq Basin on Disko and Nuussuaq formed in a geological setting between cratonic crystalline Precambrian rocks overlain by Cretaceous sediments and an actively forming Paleocene volcanic province. The lacustrine deposits, shales as well as hyaloclastite breccias, accumulated in low-lying areas inundated by fresh water and sealed off from marine transgressions by a broad subaerial volcanic terrain. Foreset-bedded hyaloclastite breccias demonstrate water depths of up to 450 m, and the area of the lake was 2500 km(2) at its maximum extent. The lake probably existed for less than 0.5 million years. The lake received clay and silt from two provenance areas. Quartz contents of more than 25% in the majority of the sediment samples indicate that large amounts of material were continuously supplied to the lake from the crystalline terrain, whereas the volcanic terrain supplied smectite and mixed-layer minerals to the lake, High kaolinite contents stem from the crystalline or both provenance areas, The shales are characterized by high TOC (up to 11%), lack of pyrite, presence of terrestrial spores and pollen and lack of marine dinoflagellates. The lacustrine sediments rest on an erosional unconformity and its correlative conformity. The unconformity developed during the latest Cretaceous and Early Paleocene. Five stages are recognized in the geological development of the lake. Stages 1-4 are characterized by accumulation of hyaloclastite breccias, rise in lake level, and eventual transgression of subaerial terrains. The rises in lake level were caused by stemming of fluvial run-off behind the aggrading volcanic pile. Stage 5 corresponds to cessation of volcanic activity, a stable lake level, and progradation of elastic sediments, resulting in infilling of the lake. During the lacustrine transgression only sediment in suspension was transported into the central parts of the lake. (C) 1998 Elsevier Science B.V, All rights reserved.	Univ Copenhagen, Inst Geol, DK-1350 Copenhagen K, Denmark; Geol Survey Denmark & Greenland, DK-2400 Copenhagen, Denmark; Geol Museum, DK-1350 Copenhagen K, Denmark; Danish Lithosphere Ctr, DK-1350 Copenhagen K, Denmark	University of Copenhagen; Geological Survey Of Denmark & Greenland	Pedersen, GK (通讯作者)，Univ Copenhagen, Inst Geol, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.		Larsen, Lotte/G-9326-2018; Pedersen, Gunver Krarup/G-9411-2018	Pedersen, Gunver Krarup/0000-0002-0792-2257				[Anonymous], 1975, Rapport Gronlands Geologiske Undersogelse, DOI DOI 10.34194/RAPGGU.V69.7407; BERNER RA, 1983, GEOCHIM COSMOCHIM AC, V47, P855, DOI 10.1016/0016-7037(83)90151-5; CHALMERS JA, 1995, MAR PETROL GEOL, V12, P205, DOI 10.1016/0264-8172(95)92840-S; Clarke D.B., 1976, GEOLOGY GREENLAND, P365; DAM G, 1998, IN PRESS SEPM SPEC P; DUEHOLM KS, 1993, J STRUCT GEOL, V15, P933, DOI 10.1016/0191-8141(93)90186-E; DUEHOLM KS, 1992, RAPPORT GRONLANDS GE, V156, P7; Flicoteaux R., 1984, Phosphate Minerals, P292; HENDERSON G, 1981, CANADIAN SOC PETROLE, V7, P399; HJORTKJAER BF, 1991, THESIS U COPENHAGEN; HJORTKJAER BF, 1995, 1 INT LIMN C 1995 CO, P50; JONES JG, 1970, GEOL MAG, V107, P13, DOI 10.1017/S0016756800054649; KOCH BE, 1959, MEDD GRONL, V162; KOCH BE, 1963, MEDD GRONL, V172; LARSEN LM, 1992, GEOL SOC LOND SPEC P, V68, P321; Pedersen A. K, 1973, RAPP GRONLANDS GEOL, V53, P21; Pedersen A.K., 1996, Bulletin Gronlands Geologiske Undersogelse, V171, P5, DOI DOI 10.34194/BULLGGU.V171.6731; PEDERSEN AK, 1985, RAPP GRONL GEOL UNDE, V124; PEDERSEN AK, 1992, RAPPORT GRONLANDS GE, V156, P19; PEDERSEN GK, 1995, 1 INT LIMN C 1995 CO, P105; Piasecki S., 1992, RAPP GRONL GEOL UNDE, V154, P13, DOI DOI 10.34194/RAPGGU.V154.8166; POREBSKI SJ, 1990, SPEC PUBL INT ASS SE, V10, P335; PULVERTAFT TCR, 1989, RAPP GRONL GEOL UNDE, V145, P28; RAISWELL R, 1988, J SEDIMENT PETROL, V58, P812; ROSENKRANTZ A, 1969, AAPG BULL, V12, P883; STOREY M, 1996, M TECT MAGM DEP PROC; TALBOT MR, 1989, PALAEOGEOGR PALAEOCL, V70, P121, DOI 10.1016/0031-0182(89)90084-9; Welte D.H., 1984, PETROLEUM FORMATION; WHITE JDL, 1992, SEDIMENTOLOGY, V39, P931, DOI 10.1111/j.1365-3091.1992.tb02160.x	29	26	26	0	9	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182			PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	JUL	1998	140	1-4					271	287		10.1016/S0031-0182(98)00034-0	http://dx.doi.org/10.1016/S0031-0182(98)00034-0			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S); Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	ZZ524					2025-03-11	WOS:000074738000016
J	Rengefors, K; Meyer, B				Rengefors, K; Meyer, B			Peridinium euryceps sp. nov. (Peridiniales, Dinophyceae), a cryophilic dinoflagellate from Lake Erken, Sweden	PHYCOLOGIA			English	Article							FRESH-WATER DINOFLAGELLATE; CYST FORMATION; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; TEMPERATURE; ULTRASTRUCTURE; ENCYSTMENT; PHOSPHORUS; CINCTUM; WILLEI	A new phototrophic species of freshwater dinoflagellates, Peridinium euryceps sp. nov., is described from Lake Erken, Sweden. It is a large and extremely flattened dinoflagellate with a characteristic shape and a tabulation that differs from known species of the same genus. Peridinium euryceps appears during winter underneath the ice, encysts at ice melt, and then remains dormant as cysts during summer. This new species has morphological and ecological similarities with Peridinium baicalense, a species endemic to Lake Baikal, Russia. The autoecology of P. euryceps is discussed, as well as the ecology of cryophilic and cold-stenothermic dinoflagellates in general. It is argued that these species have special adaptations for survival underneath the ice, such as a flattened shape and mixotrophic feeding.	Uppsala Univ, Dept Liminol, SE-75236 Uppsala, Sweden; Max Planck Inst Limnol, D-24306 Plon, Germany	Uppsala University; Max Planck Society	Rengefors, K (通讯作者)，Uppsala Univ, Dept Liminol, Norbyvagen 20, SE-75236 Uppsala, Sweden.	Karin.Rengefors@limno.uu.se	Rengefors, Karin/K-5873-2019	Rengefors, Karin/0000-0001-6297-9734				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; [Anonymous], TUSEN SJOAR VAXTPLAN; [Anonymous], SUSSWASSERFLORA MITT; BOLTOVSKOY A, 1976, Physis Seccion B las Aguas Continentales y sus Organismos, V35, P147; CHAPMAN AD, 1995, J PHYCOL, V31, P355, DOI 10.1111/j.0022-3646.1995.00355.x; Crawford R. M, 1970, Nova Hedwigia, V19, P825; FRIES M, 1969, Geologiska Foreningens i Stockholm Forhandlingar, V91, P353; GERRATH JF, 1974, CAN J BOT, V52, P683, DOI 10.1139/b74-086; HAKANSSON L, 1978, SCRIPTA LIMNOLOGICA; HAPPACHKASAN C, 1982, THESIS U MARBURG GER; HARDELAND R, 1994, EXPERIENTIA, V50, P60, DOI 10.1007/BF01992051; Holl K., 1928, Pflanzenforschung, V11, P1, DOI DOI 10.1007/s00248-006-9088-y; Huber-Pestalozzi G., 1968, PHYTOPLANKTON SUSSWA; KISSELEW J. A., 1935, BEIH BOT CENTRALBL ABT B, V53, P518; Lindemann E., 1920, Arch Naturg, section A, V84, P121; Loeblich A.R., 1970, P N AM PAL CONV CHIC, P867; Meyer B, 1997, NOVA HEDWIGIA, V65, P365; MORRILL LC, 1981, J PHYCOL, V17, P315, DOI 10.1111/j.0022-3646.1981.00315.x; MORRILL LC, 1983, INT REV CYTOL, V82, P151, DOI 10.1016/S0074-7696(08)60825-6; NAUWERCK ARNOLD, 1963, SYMBOLAE BOT UPSALIENSIS, V17, P1; Nebaeus M., 1984, VERH INT VER LIMNOL, V22, P719; Okolodkov YB, 1996, J EXP MAR BIOL ECOL, V202, P19, DOI 10.1016/0022-0981(96)00028-7; OSTENFELD CH, 1904, ROYAL SOC EDINBURGH, V25, P1126; PETTERSSON K, 1985, INT REV GES HYDROBIO, V70, P527, DOI 10.1002/iroh.19850700407; PFIESTER LA, 1976, J PHYCOL, V12, P234; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; Rengefors K, 1998, ERGEB LIMNOL, V51, P123; RENGEFORS K, 1998, P ROY SOC LOND B BIO, V265, P1; Rodhe W., 1955, Verhandlungen Internationalen Vereinigung Limnologie, V12, P117; STEINBERG C, 1981, Archiv fuer Hydrobiologie Supplement, V60, P289; *SWED MET HYDR I, 1983, SVENSKT SJOR; Taylor F.J. R., 1987, The biology of dinoflagellates, P399; Taylor FJR, 1987, BIOL DINOFLAGELLATES, P24; VONSTOSCH HA, 1969, HELGOLAND WISS MEER, V19, P558; WEDEMAYER GJ, 1982, J PHYCOL, V18, P13, DOI 10.1111/j.1529-8817.1982.tb03152.x; WILCOX LW, 1982, J PHYCOL, V18, P18; Woloszynska J., 1928, ARCH HYDROBIOLOGIE I, V3, P153	39	11	12	0	5	INT PHYCOLOGICAL SOC	LAWRENCE	NEW BUSINESS OFFICE, PO BOX 1897, LAWRENCE, KS 66044-8897 USA	0031-8884			PHYCOLOGIA	Phycologia	JUL	1998	37	4					284	291		10.2216/i0031-8884-37-4-284.1	http://dx.doi.org/10.2216/i0031-8884-37-4-284.1			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	119CQ					2025-03-11	WOS:000075878100007
J	Batten, DJ				Batten, DJ			Palaeoenvironmental implications of plant, insect and other organic-walled microfossils in the Weald Clay Formation (Lower Cretaceous) of southeast England	CRETACEOUS RESEARCH			English	Review						palynomorphs; microfossils; mesofossils; arthropods; insects; palynofacies; palaeoenvironments; Weald Clay Formation; Lower Cretaceous	ENGLISH WEALDEN; PURBECK-WEALDEN; BIOSTRATIGRAPHY; STRATIGRAPHY; PALEONTOLOGY; SUCCESSIONS; DRAGONFLIES; AFFINITIES; ODONATA; ORIGIN	A remarkable variety of plant and other organic-walled microfossils that are between 0.1 and 5.0 mm in maximum diameter has been recovered from two Weald Clay sections in Surrey, southeast England. The associations of these 'mesofossils' with each other, and with lithofacies, invertebrate macro- and microfossil occurrences and palynofacies require further investigation, but among a number of preliminary conclusions that have been drawn based on the data accumulated so far are the following. The amount of particulate organic matter of mesofossil size in a bed can usually be estimated from the general aspect of the lithology, but its composition is much harder to predict. As for older Wealden (Hastings Beds) occurrences, deposits in which megaspores are abundant often contain scattered small wood and cuticle fragments that are visible to the naked eye. Those displaying remains of insects of similar or larger size tend, not surprisingly, to yield the richest assemblages of mesofossil-sized fragments of this group. However, such zooclasts occur more widely than is apparent from the horizons that are obviously insect-bearing. This suggests that, more often than has generally been appreciated, minute black particles in standard palynological preparations of nonmarine sedimentary successions may include arthropod fragments. The common occurrence of charred remains of Weichselia reticulata and other plants in association with disarticulated bits of insects may partly reflect both a type of vegetation that was prone to desiccation and some of the insects that lived within it, lightning-induced fire during droughts having been responsible for their death. A tendency rewards an inverse relationship between this plant-insect association and large numbers of megaspores and/or seeds indicates that other habitats are also represented. Several of the megaspore genera are probably the products of aquatic or waterside plants. Delicate leafy shoots of uncertain affinity occur in several beds, but the general scarcity of larger pieces of wood and foliage suggests that the conifers and other gymnosperms may have been confined mainly to better drained parts of the Wealden lowland, and to the higher ground bordering it. Indicators of fresh to low salinity water were recovered from more than half of the samples examined. This is consistent with the general environment of sediment deposition inferred from the associated invertebrate faunas and dinoflagellate cyst assemblages. (C) 1998 Academic Press.	Univ Wales, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales	Aberystwyth University	Batten, DJ (通讯作者)，Univ Wales, Inst Geog & Earth Sci, Aberystwyth SY23 3DB, Dyfed, Wales.							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C., 1972, P GEOLOGISTS ASS, V83, P37, DOI 10.1016/S0016-7878(72)80023-3; WORSSAM BC, 1978, REPORT I GEOLOGICAL, V78; WORSSAM BC, 1977, P GEOLOGISTS ASS, V87, P429; Young B., 1988, GEOLOGY COUNTRY BRIG, P318	111	40	44	0	11	ACADEMIC PRESS LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671			CRETACEOUS RES	Cretac. Res.	JUN-AUG	1998	19	3-4					279	315		10.1006/cres.1998.0116	http://dx.doi.org/10.1006/cres.1998.0116			37	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	119HA					2025-03-11	WOS:000075888800003
J	Firth, JV; Clark, DL				Firth, JV; Clark, DL			An early Maastrichtian organic-walled phytoplankton cyst assemblage from an organic-rich black mud in Core Fl-533, Alpha Ridge: evidence for upwelling conditions in the Cretaceous Arctic Ocean	MARINE MICROPALEONTOLOGY			English	Article							DINOFLAGELLATE CYSTS; SEA; ENVIRONMENTS; CONSTRAINTS; ISRAEL; ORIGIN	A diverse assemblage of acritarchs, prasinophytes and dinoflagellate cysts occurs in an organic rich black mud in Con F1-533, taken from the Alpha Ridge, Arctic Ocean. Similarities between this assemblage and others described from the Canadian Arctic allow this black mud to be dated as early Maastrichtian, based primarily on the presence of Cerodinium leptodermum, and the absence of exclusively Campanian and upper Maastrichtian taxa. The high abundance of Comasphaeridium and marine derived amorphous organic matter may indicate a shelf to upper slope environment, possibly deposited during a marine transgression. An abundance of prasinophyte algal cysts, a moderately high peridinioid/gonyaulacoid dinoflagellate cyst ratio, and high species diversity indicate high paleoproductivity, most likely associated with upwelling conditions. When interpreted within the context of two nearby biosiliceous-rich Maastrichtian cores also taken from Alpha Ridge, and from paleogeographic reconstructions, these results indicate that an upwelling region probably existed along the eastern Arctic Ocean during at least part of the Maastrichtian, and formed different sedimentary facies in shelf to slope environments, similar to facies patterns recognized in lower latitude paleo-upwelling regions. (C) 1998 Elsevier Science B.V. All rights reserved.	Texas A&M Univ, Ocean Drilling Program, College Stn, TX 77845 USA; Univ Wisconsin, Dept Geol & Geophys, Madison, WI 53706 USA	Texas A&M University System; Texas A&M University College Station; University of Wisconsin System; University of Wisconsin Madison	Firth, JV (通讯作者)，Texas A&M Univ, Ocean Drilling Program, 1000 Discovery Dr,Res Pk, College Stn, TX 77845 USA.	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Micropaleontol.	JUN	1998	34	1-2					1	27		10.1016/S0377-8398(97)00046-7	http://dx.doi.org/10.1016/S0377-8398(97)00046-7			27	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	ZZ320					2025-03-11	WOS:000074717600001
J	Hasle, GR; Heimdal, BR				Hasle, GR; Heimdal, BR			The net phytoplankton in Kongsfjorden, Svalbard, July 1988, with general remarks on species composition of arctic phytoplankton	POLAR RESEARCH			English	Article							DINOPHYCEAE; PHAEOCYSTIS; SPITSBERGEN; MORPHOLOGY; NORTHWEST; OCEAN; SIZE; SEA	Examination of 17 samples collected by a 20 mu m meshed net in Kongsfjorden, Svalbard, 8-18 July 1988, Showed a dominance of dinoflagellates and the chrysophyte Dinobryon balticum in the surface layers, whereas the diatom and the haptophyte Phaeocystis pouchetii abundance increased with depth. The diatom Pseudo-nitzschia granii appeared together with P. pouchetii through the whole water column, and Actinocyclus curvatulus was one of the few diatoms present also in the surface samples. Two samples, from 15 and 50 m, respectively, were cleaned of organic material and mounted in Naphrax for a more critical identification of the diatoms. We were able to group the species according to habitats, especially types of ice. The planktonic Thalassiosira antarctica var. borealis, T. hyalina, T. nordenskioeldii, Bacterosira bathyomphala, Chaetoceros furcellatus, C. socialis and Fragilariopsis oceanica were present mainly as resting stages representing a post-bloom situation. These species and T. gravida appear early in the season and may have started to grow already under the ice. Fragilariopsis cylindrus and F. oceanica seem to have a closer affinity to ice than Thalassiosira and Chaetoceros spp. although they are common in the plankton. Some Nitzschia species which are usually regarded as typical sea-ice diatoms and have thicker and older ice as the main habitat were present only in small cell numbers in the plankton samples. The last component, evidently introduced from Atlantic water in the Norwegian Sea, consisted of diatoms with a more oceanic distribution, e.g. Fragilariopsis pseudonana and a small form of Thalassiosira bioculata.	Univ Oslo, Dept Biol, Sect Marine Bot, N-0316 Oslo 3, Norway; Univ Bergen, Dept Fisheries & Marine Biol, N-5020 Bergen, Norway	University of Oslo; University of Bergen	Univ Oslo, Dept Biol, Sect Marine Bot, POB 1069, N-0316 Oslo 3, Norway.							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An introduction to phycology; Vanhoffen E, 1897, Gronland-Expedition der Gesellschaft fur Erdkunde zu Berlin 1891-1893, unter Leitung von Erich von Drygalski, V2, P1; VAULOT D, 1994, J PHYCOL, V30, P1022, DOI 10.1111/j.0022-3646.1994.01022.x; Von Quillfeldt C. H., 1996, THESIS U TROMSO NORW	68	57	60	1	24	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0800-0395	1751-8369		POLAR RES	Polar Res.	JUN	1998	17	1					31	52		10.1111/j.1751-8369.1998.tb00257.x	http://dx.doi.org/10.1111/j.1751-8369.1998.tb00257.x			22	Ecology; Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Oceanography	112RD					2025-03-11	WOS:000075507200003
J	Meledina, SV; Ilyina, VI; Nal'nyaeva, TI				Meledina, SV; Ilyina, VI; Nal'nyaeva, TI			Parallel biostratigraphic scales of the Boreal Bathonian and Callovian in the North Pechora region as a tool for interregional correlations	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						cephalopods; dinocysts; Bathonian; Callovian; zonation; North Pechora region; Russia		Investigation results on ammonites, belemnites, and dinoflagellate cysts from Bathonian and Callovian deposits in the North Pechora region are used to elaborate the detailed stratigraphy and to correlate these deposits in the northern West Europe and Siberia. The Pechora basin, which was located in Jurassic time at the boundary between the Arctic and Boreal Atlantic paleobiogeographic provinces, incorporates faunas typical of neighboring regions and thus is an intermediate province linking Siberia with West Europe. The bed-by-bed study of sections exposed along tributaries of the Pechora River provided grounds to elaborate the Bathonian-Callovian biozonation of ammonites, belemnites, and dinoflagellate cysts. The ammonite zonation consisting of eleven units is correlated with the West European standard and East Siberian local zonations, The identified common species suggest that Pechora sections include the standard zigzag, herveyi, calloviense, athleta, and lamberti zones. Other units bearing only the arctic species are correlated with Bathonian and Callovian ammonite zones established in eastern and western Siberia. The revealed belemnite zonation includes five biostratigraphic units spanning the middle Bathonian and entire Callovian intervals. It is correlated with the regional ammonite scale and also with the East Siberian belemnite zonation. The Bathonian-Callovian succession of dinocysts assemblages is shown to include seven units ranked as zones or dinocyst beds. The dinocyst assemblages from Bathonian and Callovian deposits of the North Pechora and other regions of the Russian platform, along with similar assemblages from northern Siberia, are calibrated by comparison with dinoflagellate zonations in northwestern Europe and Arctic Canada. The mutually coordinated Bathonian-Callovian zonation of ammonite, belemnite, and dinocyst fossils is suggested to be a reliable biostratigraphic scale for interregional correlations in a vast area of northern Eurasia, Arctic regions, and America. The paper also includes description of Cadoceras pishmae Meledina, C. variabile Spath (ammonites), and Belemnopsis sp. ind.	Russian Acad Sci, Joint Inst Geol Geophys & Minerol, Siberian Div, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Meledina, SV (通讯作者)，Russian Acad Sci, Joint Inst Geol Geophys & Minerol, Siberian Div, Univ Pr 3, Novosibirsk 630090, Russia.							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I., 1991, STRATIGRAPHY PALAEOG, P42; ILYINA VI, 1991, P 3 INT S JUR STRAT, V1, P71; KAMYSHEVAELPATE.VG, 1959, STRATIGRAFIYA YURSKI; Kozlova G.E., 1994, BIOSTRATIGRAFIYA NEF, P49; Kravets V.S., 1976, BIOSTRATIGRAFIYA OTL, P27; KRYMGOLTS GA, 1929, T GEOLKOMA, V48, P1021; Meledina S.V., 1994, Boreal Middle Jurassic of Russia (Ammonites and Zonal Stratigraphy of the Bajocian, Bathonian, and Callovian; Meledina S.V, 1987, TR IGIG SO AN SSSR V; Meledina S.V, 1977, Ammonites and Zonal Stratigraphy of the Callovian of Siberia; MELEDINA SV, 1996, GEOL GEOFIZ, P25; MELEDINA SV, 1991, PALEONTOLOGIYA KORRE, P73; Nalnjaeva T.I., 1986, YURSKIE OTLOZHENIYA, P137; NALNYAEVA TI, 1983, PALEOBIOGEOGRAFIYA B, P113; POULTON TP, 1987, B GEOL SURV CAN, V358, P1; PUGACZEWSKA H, 1961, ACTA PALEONTOL POLON, V6; RIDING J B, 1984, Palynology, V8, P195; RIDING JB, 1992, STRATIGRAPHIC INDEX, P1; RILEY L A, 1982, Palynology, V6, P193; Saks V.N., 1964, VERKHNEYURSKIE NIZHN; Saks V.N., 1971, Problemy obshhey i regional'noy geologii-Problems of general and regional geology., P179; SAKS VN, 1966, VERKHNEYURSKIE NIZHN; SAKS VN, 1975, RANNE SREDNEYURSKIE; SARJEANT WAS, 1982, CONTRIB AM ASS STRAT, P1; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; SMELROR M, 1992, ARCTIC GEOLOGY PETRO, P495; Spath L. F., 1932, MEDDELELSER GRONLAND, V87, P1; STOYANOVA-VERGILOVA M.P., 1990, MEM DESCR CARTA GEOL, V40, P269; STOYANOVAVERGIL.M, 1982, PARAMEGATEUTHIS GUST, V73, P251; TEODOROVICH VI, 1971, B MOSK OVA ISPYT PRI, P62; Voronets N.S., 1962, STRATIGRAFIYA GOLOVO; YOKOVLEVA SP, 1993, BIOSTRATIGRAFIYA NEF, P125	46	8	8	0	0	INTERPERIODICA	BIRMINGHAM	PO BOX 1831, BIRMINGHAM, AL 35201-1831 USA	0869-5938			STRATIGR GEOL CORREL	Stratigr. Geol. Correl.	MAY-JUN	1998	6	3					234	248						15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	ZT161					2025-03-11	WOS:000074055300003
J	Costas, E; Nieto, B; Lopez-Rodas, V; Salgado, C; Toro, M				Costas, E; Nieto, B; Lopez-Rodas, V; Salgado, C; Toro, M			Adaptation to competition by new mutation in clones of <i>Alexandrium minutum</i>	EVOLUTION			English	Article						Alexandrium minutum; competition; spontaneous mutation	GENOTYPES; RATES	We describe two competition experiments between clones of the dinoflagellate Alexandrium minutum. In the first experiment, two clones originating from a single haploid cell competed until one of the clones was almost driven to extinction. In the second experiment, these two clones were allowed to compete with the original populations, which were previously kept as cysts. The results indicate that an improvement of the competitive ability in both clones has occurred during the history of competition. This adaptation to competition must be attributed to selection acting on the new genetic variation that has arisen by mutation.	Univ Complutense Madrid, Fac Vet, Dept Anim Prod, E-28040 Madrid, Spain; INIA, CIT, Area Mejora Genet, E-28040 Madrid, Spain	Complutense University of Madrid	Costas, E (通讯作者)，Univ Complutense Madrid, Fac Vet, Dept Anim Prod, E-28040 Madrid, Spain.		Toro, Miguel Angel/H-9370-2015	Toro, Miguel Angel/0000-0001-7460-2483				AYALA FJ, 1971, SCIENCE, V171, P820, DOI 10.1126/science.171.3973.820; BELL G, 1991, EVOLUTION, V45, P1036, DOI 10.1111/j.1558-5646.1991.tb04368.x; BRAND LE, 1981, EVOLUTION, V35, P1117, DOI 10.1111/j.1558-5646.1981.tb04981.x; COSTAS E, 1994, J PHYCOL, V30, P987, DOI 10.1111/j.0022-3646.1994.00987.x; COSTAS E, 1993, PHYCOLOGIA, V32, P351, DOI 10.2216/i0031-8884-32-5-351.1; DAWSON JM, 1983, AM NAT, V122, P292; Goodnight CJ, 1996, EVOLUTION, V50, P1241, DOI [10.2307/2410664, 10.1111/j.1558-5646.1996.tb02364.x]; HOULE D, 1996, GENETICS, V143, P1463; HUTCHINSON G, 1961, AM NAT, V95, P137, DOI 10.1086/282171; LYNCH M, 1988, GENET RES, V51, P137, DOI 10.1017/S0016672300024150; ORR HA, 1994, GENETICS, V136, P1475; PEREZTOME JM, 1982, NATURE, V299, P153, DOI 10.1038/299153a0; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; VANVALEN MJ, 1973, EVOL THEOR, V1, P292	14	9	10	1	7	SOC STUDY EVOLUTION	LAWRENCE	810 E 10TH STREET, LAWRENCE, KS 66044 USA	0014-3820			EVOLUTION	Evolution	APR	1998	52	2					610	613		10.2307/2411095	http://dx.doi.org/10.2307/2411095			4	Ecology; Evolutionary Biology; Genetics & Heredity	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Evolutionary Biology; Genetics & Heredity	ZM270	28568351				2025-03-11	WOS:000073521700028
J	Riding, JB; Ilyina, VI				Riding, JB; Ilyina, VI			A new dinoflagellate cyst from the Upper Bathonian (Middle Jurassic) strata of the Russian Platform	JOURNAL OF MICROPALAEONTOLOGY			English	Article								Protobatioladinium? elongatum sp. nov, is a distinctive, large, longitudinally elongate Upper Bathonian (Middle Jurassic) dinoflagellate cyst recorded from western Russia. This species is questionably attributed to Protobatioladinium because the archaeopyle type does not precisely conform to that of the genotype. This form is present, often abundantly, throughout the Upper Bathonian sediments of the central and northern Russian Platform and appears to be a reliable marker species.	British Geol Survey, Keyworth NG12 5GG, Notts, England; Russian Acad Sci, United Inst Geol Geophys & Mineral, Novosibirsk 630090, Russia	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Russian Academy of Sciences; Sobolev Institute of Geology & Mineralogy of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Riding, JB (通讯作者)，British Geol Survey, Keyworth NG12 5GG, Notts, England.							[Anonymous], 1978, ANALYSES PREPLEISTOC; HYINA VI, 1991, STRATIGRAPHY PALAEOG, P42; LENTIN JK, 1993, AMM ASS STRATIGRAPHI, V28; NOHR-HANSEN H, 1986, Bulletin of the Geological Society of Denmark, V35, P31; Riding JB, 1996, J MICROPALAEONTOL, V15, P150, DOI 10.1144/jm.15.2.150	5	1	1	0	1	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH, AVON, ENGLAND BA1 3JN	0262-821X			J MICROPALAEONTOL	J. Micropalaentol.	APR	1998	17		1				86	86		10.1144/jm.17.1.86	http://dx.doi.org/10.1144/jm.17.1.86			1	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	ZP299		hybrid			2025-03-11	WOS:000073738400007
J	Perez, CC; Roy, S; Levasseur, M; Anderson, DM				Perez, CC; Roy, S; Levasseur, M; Anderson, DM			Control of germination of Alexandrium tamarense (Dinophyceae) cysts from the lower St. Lawrence estuary (Canada)	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium tamarense; circannual rhythm; cyst germination; cyst maturation; light temperature; toxic dinoflagellate	DINOFLAGELLATE GONYAULAX-TAMARENSIS; EXCAVATA; BLOOMS; BAY	Cysts of the toxic dinoflagellate Alexandrium tamarense (Lebour) Balech 1992 from the lower St. Lawrence estuary were used in a test of the following hypotheses: (1) cyst germination is triggered by a change in temperature, and (2) germination rate varies throughout the year and is controlled by a circannual internal biological clock. Results show that cyst germination was not affected significantly by temperature of incubation over the range 1 degrees-16 degrees C, and light showed no significant stimulation of germination. This is supported by the lack of effect of cyst incubation conditions during evaluation of the seasonal changes in germination rate (two temperatures: 4 degrees and 15 degrees C, and two light conditions: darkness and 150 mu mol photons.m(-2).s(-1)). Thus, direct environmental control through short-term increases in temperature and exposure to light has no effect on the germination of the cysts tested. The rate of germination, observed monthly over a 16-month period showed low germination (<20%) over most of the period tested except for a maximum reaching more than 50% germination in August to October of the second year of the experiment. This pattern was observed for cysts both from monthly field collections and from laboratory-stored cysts kept under constant environmental conditions (4 degrees C, in the dark). The peak in germination observed under constant environmental conditions tin the laboratory), the almost coincidental increase in cyst germination observed for the field-collected cysts, and the absence of effects of temperature and light during incubation could be explained either by a temperature-controlled cyst maturation period (the time-temperature hypothesis of Huber and Nipkow 1923 or by the presence of an internal biological clock. However, the large decline in the rate of germination 2 months after the maximum provides strong support for the biological clock hypothesis. The ca. 12-month maturation (dormancy) period observed for the laboratory-stored cysts is the longest reported for this species to our knowledge; this might be related to the low storage temperature (4 degrees C), which is close to bottom temperatures generally encountered in this environment (0 degrees to 6 degrees C). Similar field and laboratory storage temperatures could explain the coincidental increase in germination rate in the fall of the second year if cyst maturation is controlled by temperature. A fraction of the laboratory-stored cysts did not follow a rhythmic pattern: A rather constant germination rate of about 20% was observed throughout the year. This continuous germination of likely mature cysts may supplement the local blooms of this toxic dinoflagellate, as these often occur earlier than peak germination observed in late summer. It seems that two cyst germination strategies are present in the St Lawrence: continuous germination after cyst maturation, with temperature controlling the length of the maturation period and germination controlled by a circannual internal rhythm.	Inst Natl Rech Sci Oceanol, Rimouski, PQ G5L 3A1, Canada; Univ Quebec, Dept Oceanog, Rimouski, PQ G5L 3A1, Canada; Fisheries & Oceans Canada, Maurice Lamontagne Inst, Mont Joli, PQ G5H 3Z4, Canada; Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA	University of Quebec; University of Quebec; Fisheries & Oceans Canada; Woods Hole Oceanographic Institution	Roy, S (通讯作者)，Inst Natl Rech Sci Oceanol, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	suzanne_roy@uqar.uquebec.ca						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, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; 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; BINDER BJ, 1986, NATURE, V322, P659, DOI 10.1038/322659a0; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; Cembella A.D., 1989, P81; *COMM EN AT, 1978, STAT APPL EXPL MES, V1; DALE B, 1977, SARSIA, V63, P29, DOI 10.1080/00364827.1977.10411318; Dale B., 1983, P69; Fukuyo Y., 1982, RES REP NATL I ENV S, V30, P43; GOSSELIN S, 1989, MAR ECOL PROG SER, V57, P1, DOI 10.3354/meps057001; HUBER G., 1923, FLORA, V16, P114; ISHIKAWA A, 1994, MAR BIOL, V119, P39, DOI 10.1007/BF00350104; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PFIESTER LA, 1975, J PHYCOL, V11, P259, DOI 10.1111/j.1529-8817.1975.tb02776.x; PRAKASH A, 1967, J FISH RES BOARD CAN, V24, P1589, DOI 10.1139/f67-131; PRAKASH A, 1971, FISHERIES RES BOARD, V177; ROBINEAU B, 1993, DEV MAR BIO, V3, P323; Silverberg N., 1990, Oceanography of a Large-Scale Estuarine System: The St. Lawrence. Coastal and Estuarine Studies, P202; Steidinger K.A., 1975, P153; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; Therriault J.C., 1985, P141; TURGEON J, 1990, TOXIC MARINE PHYTOPLANKTON, P238; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; VONSTOSCH HA, 1973, BR PHYCOL J, V8, P104; WALKER LM, 1979, J PHYCOL, V15, P312; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690; WATRAS CJ, 1982, J EXP MAR BIOL ECOL, V62, P25, DOI 10.1016/0022-0981(82)90214-3	33	53	64	1	18	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0022-3646			J PHYCOL	J. Phycol.	APR	1998	34	2					242	249		10.1046/j.1529-8817.1998.340242.x	http://dx.doi.org/10.1046/j.1529-8817.1998.340242.x			8	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	ZJ664					2025-03-11	WOS:000073239700006
J	Tsim, ST; Wong, JTY; Wong, YH				Tsim, ST; Wong, JTY; Wong, YH			Regulation of calcium influx and phospholipase C activity by indoleamines in dinoflagellate <i>Crypthecodinium cohnii</i>	JOURNAL OF PINEAL RESEARCH			English	Article						dinoflagellates; encystment; melatonin; 5-methoxytryptamine; calcium influx; phospholipase C; structure-activity relationship; mastoparan	MELATONIN RECEPTOR; PHARMACOLOGICAL CHARACTERIZATION; SEROTONIN RECEPTOR; INDUCED ENCYSTMENT; BINDING-SITES; GONYAULAX-POLYEDRA; TRYPANOSOMA-CRUZI; RAT HYPOTHALAMUS; ION-CHANNEL; CHICK BRAIN	Exogenous indoleamines such as melatonin and 5-methoxytryptamine have been shown to induce cyst formation (encystment) in many species of dinoflagellate. Induction of inositol phosphates formation by indoleamine has previously been demonstrated in Crypthecodinium cohnii. In addition, depletion of extracellular Ca2+ blocks the indoleamine-induced encystment. In the present study, 12 indoleamines (including melatonin and related compounds) were examined for their abilities to induce Ca2+ influx, inositol phosphates formation, and encystment in C. cohnii. The results showed that melatonin, 5-methoxytryptamine, and the peptide toxin mastoparan stimulated Ca-45(2+) influxes in dose-and time-dependent manners. The EC50 values of 5-methoxytrypramine and mastoparan to stimulate Ca-45(2+) uptake were 2 mM and 35 mu M, respectively. The 5-methoxytryptamine- and mastoparan-induced Ca-45(2+) influx were partially attenuated by the calcium channel blockers, verapamil and ruthenium red. A series of indoleamines were examined for their structure-activity relationship on the induction of encystment and formation of inositol phosphates. Melatonin-induced inositol phosphates formation was completely blocked by U73122, indicating the possible involvement of phospholipase C. Taken together, we conclude that indoleamines may induce encystment of the dinoflagellate C. cohnii via parallel activation of phospholipase C and Ca2+ influx signaling pathways. However, activation of phospholipase C and Ca2+ influx are not always necessary or sufficient for inducing encystment. Also, these data provided the first direct evidence of a Ca2+ influx regulating mechanism in dinoflagellate C. cohnii.	Hong Kong Univ Sci & Technol, Dept Biol, Kowloon, Peoples R China; Hong Kong Univ Sci & Technol, Biotechnol Res Inst, Kowloon, Peoples R China	Hong Kong University of Science & Technology; Hong Kong University of Science & Technology	Hong Kong Univ Sci & Technol, Dept Biol, Kowloon, Peoples R China.	boyung@usthk.ust.hk		Wong, Yung Hou/0000-0002-0123-7697				ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; BALZER I, 1991, SCIENCE, V253, P795, DOI 10.1126/science.1876838; BANERJEE S, 1972, J PROTOZOOL, V19, P108, DOI 10.1111/j.1550-7408.1972.tb03423.x; BERNAL J, 1991, J EXP BIOL, V155, P505; CHIESA R, 1993, J EUKARYOT MICROBIOL, V40, P800, DOI 10.1111/j.1550-7408.1993.tb04478.x; CONKLIN BR, 1992, J BIOL CHEM, V267, P31; DUBOCOVICH ML, 1988, FASEB J, V2, P2765, DOI 10.1096/fasebj.2.12.2842214; DUBOCOVICH ML, 1988, J PHARMACOL EXP THER, V246, P902; DUBOCOVICH ML, 1987, P NATL ACAD SCI USA, V84, P3916, DOI 10.1073/pnas.84.11.3916; DUBOCOVICH ML, 1995, TRENDS PHARMACOL SCI, V16, P50, DOI 10.1016/S0165-6147(00)88978-6; DUNCAN MJ, 1988, ENDOCRINOLOGY, V122, P1825, DOI 10.1210/endo-122-5-1825; EBISAWA T, 1994, P NATL ACAD SCI USA, V91, P6133, DOI 10.1073/pnas.91.13.6133; Eison Arlene S., 1993, Life Sciences, V53, P393; Faillace MP, 1996, J NEUROCHEM, V67, P623; FASOLATO C, 1994, TRENDS PHARMACOL SCI, V15, P77, DOI 10.1016/0165-6147(94)90282-8; Garrido MN, 1996, CELL MOL BIOL, V42, P221; Godson C, 1997, ENDOCRINOLOGY, V138, P397, DOI 10.1210/en.138.1.397; GOLDBERG JI, 1994, J NEUROBIOL, V25, P1545, DOI 10.1002/neu.480251207; HARDELAND R, 1995, J PINEAL RES, V18, P104, DOI 10.1111/j.1600-079X.1995.tb00147.x; Hardeland R, 1996, BRAZ J MED BIOL RES, V29, P119; Hardeland R, 1996, FRONT HORM RES, V21, P1; KOBILKA B, 1992, ANNU REV NEUROSCI, V15, P87, DOI 10.1146/annurev.neuro.15.1.87; Kruppel T, 1996, CELL CALCIUM, V19, P229, DOI 10.1016/S0143-4160(96)90024-X; LEWIS DFV, 1990, J PHARMACOL EXP THER, V252, P370; LIU F, 1995, FEBS LETT, V374, P273, DOI 10.1016/0014-5793(95)01129-3; MARICQ AV, 1991, SCIENCE, V254, P432, DOI 10.1126/science.1718042; McArthur AJ, 1997, ENDOCRINOLOGY, V138, P627, DOI 10.1210/en.138.2.627; Molinari EJ, 1996, EUR J PHARMACOL, V301, P159, DOI 10.1016/0014-2999(95)00870-5; MORIYOSHI K, 1991, NATURE, V354, P31, DOI 10.1038/354031a0; MULLINS UL, 1994, J PINEAL RES, V17, P33, DOI 10.1111/j.1600-079X.1994.tb00111.x; MULLINS UL, 1997, CELL SIGNAL, V9, P167; Navajas C, 1996, EUR J PHARMACOL, V304, P173, DOI 10.1016/0014-2999(96)00114-8; OZ HS, 1992, EXP PARASITOL, V74, P390, DOI 10.1016/0014-4894(92)90201-K; POEGGELER B, 1991, Naturwissenschaften, V78, P268; POPOVA JS, 1995, J NEUROCHEM, V64, P130; REPPERT SM, 1995, NEURON, V15, P1003, DOI 10.1016/0896-6273(95)90090-X; REPPERT SM, 1995, P NATL ACAD SCI USA, V92, P8734, DOI 10.1073/pnas.92.19.8734; REPPERT SM, 1994, NEURON, V13, P1177, DOI 10.1016/0896-6273(94)90055-8; ROSENSTEIN RE, 1991, J NEURAL TRANSM-GEN, V85, P243, DOI 10.1007/BF01244949; SALAMAN A, 1990, NEUROPEPTIDES, V16, P115, DOI 10.1016/0143-4179(90)90122-F; SATAKE N, 1986, GEN PHARMACOL, V17, P555; SHIBATA S, 1989, GEN PHARMACOL-VASC S, V20, P677, DOI 10.1016/0306-3623(89)90106-7; Sogin ML, 1991, CURR OPIN GENET DEV, V1, P457, DOI 10.1016/S0959-437X(05)80192-3; SUGAMORI KS, 1993, P NATL ACAD SCI USA, V90, P11, DOI 10.1073/pnas.90.1.11; SUGDEN D, 1991, BRIT J PHARMACOL, V104, P922, DOI 10.1111/j.1476-5381.1991.tb12527.x; SUGDEN D, 1995, BRIT J PHARMACOL, V114, P618, DOI 10.1111/j.1476-5381.1995.tb17184.x; Tsim ST, 1996, MOL MAR BIOL BIOTECH, V5, P162; Tsim ST, 1996, BIOL SIGNAL, V5, P22; Tsim ST, 1997, J CELL SCI, V110, P1387; VANECEK J, 1995, ENDOCRINOLOGY, V269, pE85; WICKMAN K, 1995, PHYSIOL REV, V75, P865, DOI 10.1152/physrev.1995.75.4.865; WITZ P, 1990, P NATL ACAD SCI USA, V87, P8940, DOI 10.1073/pnas.87.22.8940; WONG JTY, 1994, J MAR BIOL ASSOC UK, V74, P467, DOI 10.1017/S0025315400039515; Wong JTY, 1996, FRONT HORM RES, V21, P7; Wong YH, 1996, FRONT HORM RES, V21, P147; YUEH YG, 1993, J CELL BIOL, V123, P869, DOI 10.1083/jcb.123.4.869; YUNG LY, 1995, FEBS LETT, V372, P99, DOI 10.1016/0014-5793(95)00963-A; ZISAPEL N, 1983, BRAIN RES, V272, P378, DOI 10.1016/0006-8993(83)90588-7	58	16	16	1	8	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0742-3098	1600-079X		J PINEAL RES	J. Pineal Res.	APR	1998	24	3					152	161		10.1111/j.1600-079X.1998.tb00528.x	http://dx.doi.org/10.1111/j.1600-079X.1998.tb00528.x			10	Endocrinology & Metabolism; Neurosciences; Physiology	Science Citation Index Expanded (SCI-EXPANDED)	Endocrinology & Metabolism; Neurosciences & Neurology; Physiology	ZB677	9551852				2025-03-11	WOS:000072496500005
J	Santarelli, A; Brinkhuis, H; Hilgen, FJ; Lourens, LJ; Versteegh, GJM; Visscher, H				Santarelli, A; Brinkhuis, H; Hilgen, FJ; Lourens, LJ; Versteegh, GJM; Visscher, H			Orbital signatures in a Late Miocene dinoflagellate record from Crete (Greece)	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; Late Miocene; Mediterranean; Milankovitch theory; sapropels	POLARITY TIME-SCALE; ADJACENT SEAS; CYSTS; SEDIMENTS; PLIOCENE; BIOSTRATIGRAPHY; BOUNDARY; NORTH; CORE	A high-resolution palynological study of the cyclically bedded Faneromeni section (upper Tortonian-lower Messinian) on Crete (Greece) is presented. This study aims to recognize orbitally-driven variations in the palynological record and to validate the age model based on the astronomical calibration of the sedimentary cycles. Four palynology-based environmental proxies were utilised using interpretations of fossil dinoflagellate associations based on modem ecological characteristics. Cross-spectral analysis between the proxy records and astronomical target curve, the 65 degrees N summer, insolation, yielded in most cases significant spectral power and coherence in the precession and/or obliquity frequency bands. Precession-controlled variations in the proxy records are related to lithology and indicate that maxima in continental input and minima in sea surface salinity coincide with sapropel formation, The influence of obliquity is most dearly reflected in the index of continental versus marine palynomorphs (S-D). The absence of a distinct time lag relative to obliquity indicates that the 41-kyr component in continental input is controlled by oscillations in regional Mediterranean climate rather than by glacial cyclicity. Phase relations in the different astronomical frequency bands of the spectrum, as compared with the Mediterranean Pliocene, essentially confirm the validity of the Miocene astronomical time scale. Finally, a major non-cyclic change in the palynological assemblage at 6.68 Ma indicates enhanced salinity and decreased river discharge. This shift coincides with a significant drop in sedimentation rate informally termed the "Early Messinian Sediment starvation Event". (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; Inst Earth Sci, Dept Geol, NL-3584 CD Utrecht, Netherlands; Univ Urbino, Ist Geol, Ctr Palinol, I-61029 Urbino, Italy; Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands	Utrecht University; University of Urbino; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Santarelli, A (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		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J	McCarthy, FMG; Mudie, PJ				McCarthy, FMG; Mudie, PJ			Oceanic pollen transport and pollen:dinocyst ratios as markers of late Cenozoic sea level change and sediment transport	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						pollen transport; late Cenozoic; sea level; North Atlantic; dinocysts	NORTH-ATLANTIC OCEAN; DRILLING PROJECT LEG-94; LABRADOR-SEA; CONTINENTAL-MARGIN; MARINE-SEDIMENTS; HEINRICH EVENTS; EASTERN CANADA; DINOFLAGELLATE; GLACIATION; REGION	Palynological studies of late Cenozoic cores from nine sites show large peaks in the ratio of pollen and spores to dinocysts (P:D) which reflect major increases in terrigenous sediment influx to the North Atlantic Ocean. Under normal pelagic conditions in the North Atlantic, i.e., in the absence of ice rafting or mass wasting, P:D in oceanic sediments is low, usually <0.5. Geographic and temporal variation in P:D suggests that mass wasting during glacioeustatic sea level lowstands (cold isotopic stages) was the main source of these large pollen inputs to the deep sea during the latest Pliocene to Pleistocene. Pollen and sports, mostly deposited on continental shelves es during interglacial sea level highstands, are resuspended during lowstands and transported across the margins by turbidity currents and over the abyss by ocean currents. Peaks in P:D in deep sea sediments thus correlate with erosional unconformities that bound sequences on continental margins. These peaks of late Cenozoic pollen-spore influx are usually distinct from intervals of ice-rafted sediment deposition which are marked by large influxes of Mesozoic-Paleogene dinocysts of probable Norwegian Trough origin and Paleozoic acritarchs from bedrock eroded by Canadian Arctic glaciers. (C) 1998 Elsevier Science B.V.	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Paleoclimatol. Paleoecol.	APR	1998	138	1-4					187	206		10.1016/S0031-0182(97)00135-1	http://dx.doi.org/10.1016/S0031-0182(97)00135-1			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	ZH834					2025-03-11	WOS:000073152200011
J	Harding, IC				Harding, IC			A minute new cladopyxiinean dinocyst from Barremian (Cretaceous) sediments and its bearing on the acritarch vs. dinoflagellate cyst question	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; acritarchs; Early Cretaceous; new species; Germany; England		A minute new palynomorph, Fallaciodinium minutum Harding, gen. et sp. nov., measuring less than 20 mu m in diameter is described from western European Boreal sediments of a late Barremian (Early Cretaceous) age. This diminutive taxon strongly resembles an acanthomorph acritarch in light microscopic investigation, but electron microscopy has revealed dinoflagellate affinities in the form of an atypical cladopyxiinean paratabulation and an epitractal archaeopyle. This taxon serves to highlight several problems which still bias our perception of the dinoflagellate fossil record. (C) 1998 Elsevier Science B.V. All rights reserved.	Univ Southampton, Southampton Oceanog Ctr, Dept Geol, Southampton SO14 3ZH, Hants, England	University of Southampton; NERC National Oceanography Centre	Harding, IC (通讯作者)，Univ Southampton, Southampton Oceanog Ctr, Dept Geol, European Way, Southampton SO14 3ZH, Hants, England.	ich@mail.soc.soton.ac.uk	Harding, Ian/K-3320-2012					[Anonymous], 1985, SPOROPOLLENIN DINOFL; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; COLBATH GK, 1995, REV PALAEOBOT PALYNO, V86, P287, DOI 10.1016/0034-6667(94)00148-D; 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, 1978, Palynology, V2, P187; Davey R.J., 1974, S STRATIGRAPHIC PALY, V3, P41; DODSWORTH P, 1995, J MICROPALAEONTOL, V14, P6, DOI 10.1144/jm.14.1.6; DOWNIE C, 1964, PUB GEOL SCI, V7, 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; GALLOIS RW, 1971, ANN REP I GEOL SCI, P116; GENSOME RA, 1993, MICROPALAEONTOLOGY S, V7, P351; HABIB D, 1972, 9 DSDP, P367; HARDING I C, 1990, Palaeontographica Abteilung B Palaeophytologie, V218, P1; HARDING IC, 1986, THESIS U CAMBRIDGE; HUGHES NF, 1994, ENIGMA ANGIOSPERM OR, V1; KAYE PETER, 1964, GEOL MAG, V101, P340; Moldowan JM, 1996, GEOLOGY, V24, P159; Mutterlose J., 1984, Mitteilungen aus dem Geologischen Institut der Universitaet Hannover, V24, P1; Nicoll R.S., 1994, J AUSTR GEOLOGY GEOP, V15, P101; OGG G, 1994, MAR MICROPALEONTOL, V23, P241, DOI 10.1016/0377-8398(94)90015-9; Palliani RB, 1997, REV PALAEOBOT PALYNO, V96, P99, DOI 10.1016/S0034-6667(96)00019-X; SARJEANT W A S, 1978, Palynology, V2, P167; SCHRANK E, 1988, REV PALAEOBOT PALYNO, V56, P123, DOI 10.1016/0034-6667(88)90078-4; SCHRODER CJ, 1987, J FORAMIN RES, V17, P101, DOI 10.2113/gsjfr.17.2.101; SMART CW, 1994, MAR MICROPALEONTOL, V23, P89, DOI 10.1016/0377-8398(94)90002-7; Strother P.K., 1996, Palynology: Principles and Applications, Volume, V1, P81, DOI DOI 10.1016/0034-6667(95)00117-4; Swinnerton H. H., 1935, Quarterly Journal of the Geological Society of London, V91, P1; TAPPAN H, 1980, PALEOBIOLGOY PLANT P; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; TAYLOR FJR, 1994, EARLY LIFE EARTH, P312; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	34	0	0	0	0	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	1998	100	1-2					89	98		10.1016/S0034-6667(97)00058-4	http://dx.doi.org/10.1016/S0034-6667(97)00058-4			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ZT776					2025-03-11	WOS:000074124500005
J	Alldredge, AL; Passow, U; Haddock, SHD				Alldredge, AL; Passow, U; Haddock, SHD			The characteristics and transparent exopolymer particle (TEP) content of marine snow formed from thecate dinoflagellates	JOURNAL OF PLANKTON RESEARCH			English	Article							GONYAULAX-EXCAVATA; DIATOM BLOOMS; FLOCCULATION; ENCYSTMENT; PATCHES; SINKING; CYSTS; WATER; SEA	Abundant marine snow containing diatoms and detritus, but dominated by large, bioluminescent thecate dinoflagellates and their temporary vegetative cysts, especially several species of the genus Gonyaulax, was observed at six stations in the Santa Barbara Channel, California, in 1989 and 1994. These aggregates were unusually cohesive and mucus rich, and contained 2-4 times more mass, particulate organic carbon (POC), particulate organic nitrogen (PON) and chlorophyll a per unit aggregate volume than more common types of marine snow formed from diatoms, fecal matter, larvacean houses or miscellaneous detritus. However, the relationship between aggregate size and the concentration of TEP (transparent exopolymer particles which form the mucus matrix of most marine snow) was similar to that of other types of aggregates, suggesting that much of the copious gel-like material within dinoflagellate aggregates was not TEP. While this is the first report of abundant thecate dinoflagellates occurring within large, rapidly sinking marine aggregates, the data do not support the conclusion that mass aggregation and subsequent sedimentation of blooms is part of the life history adaptations of thecate dinoflagellates, as it is for some diatoms. The high abundance of free-living dinoflagellate cells and temporary cysts, and the similar proportion of dinoflagellates relative to other algal and chemical components in both aggregates and the surrounding seawater, indicate that the dinoflagellates were not differentially aggregating. Even so, passive accumulation of dinoflagellates in marine snow through aggregation processes may result in more rapid transport of dinoflagellate-generated material to the deep ocean, alter the nature of sinking particulate matter following dinoflagellate blooms, and increase the nutritional value of marine snow as a food source for zooplankton and fish.	Univ Calif Santa Barbara, Dept Ecol, Santa Barbara, CA 93106 USA; Univ Calif Santa Barbara, Dept Evolut & Marine Biol, Santa Barbara, CA 93106 USA; Univ Calif Santa Barbara, Inst Marine Sci, Santa Barbara, CA 93106 USA	University of California System; University of California Santa Barbara; University of California System; University of California Santa Barbara; University of California System; University of California Santa Barbara	Alldredge, AL (通讯作者)，Univ Calif Santa Barbara, Dept Ecol, Santa Barbara, CA 93106 USA.							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R., 1987, The biology of dinoflagellates, P399; Utermohl H., 1958, MITT INT VER THEOR A, V9, P1, DOI DOI 10.1080/05384680.1958.11904091; Walker L.M., 1984, P19	34	85	100	2	36	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873			J PLANKTON RES	J. Plankton Res.	MAR	1998	20	3					393	406		10.1093/plankt/20.3.393	http://dx.doi.org/10.1093/plankt/20.3.393			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	ZF441					2025-03-11	WOS:000072897800001
J	Zohary, T; Pollingher, U; Hadas, O; Hambright, KD				Zohary, T; Pollingher, U; Hadas, O; Hambright, KD			Bloom dynamics and sedimentation of Peridinium gatunense in Lake Kinneret	LIMNOLOGY AND OCEANOGRAPHY			English	Article							SPRING BLOOM; PHAEOCYSTIS-POUCHETII; CARBON FLOW; FOOD-WEB; PHYTOPLANKTON; SINKING; ISRAEL; CINCTUM; FATE; DECOMPOSITION	Temporal changes in the abundance of Peridinium gatunense Nygaard in the water column of warm monomictic Lake Kinneret were followed during 1990-1994. Sedimentation rates of this dinoflagellate were followed concurrently by means of sediment traps with and without a preservative (Formalin), positioned at the base of the epilimnion and within the hypolimnion, for exposure periods of 2-3 weeks. Upper trap catches of total P. gatunense (live cells + dead cells + thecae + protoplasts + cysts) were nearly always higher than lower trap catches, partly due to decomposition of the cells as they sank through the water column. Over the 5-year period, total P. gatunense sedimentation rates ranged over 4 orders of magnitude, from values <0.001 to 8.5 g (WW) m(-2) d(-1). A typical seasonal pattern was observed in which sedimentation rates were relatively low during the bloom increase phase, with thecae (from cell, division) being the main component, and increased substantially after the peak of the bloom, when the relative contribution of senescent cells, dead cells and protoplasts increased substantially. Cysts were trapped in low numbers, usually 1-2 orders of magnitude fewer than live cells. Interannual variations in total P. gatunense sedimentation were large and independent of the size of bloom-the proportion of annual P. gatunense production reaching the hypolimnetic traps ranged from 6% in 1994, the year with the largest bloom, to 68% in 1991, a year with an average-size bloom. The high value was exceptional and we speculated that it resulted from higher resuspension and more severe nutrient limitation of microbial decomposition during that low water level, drought year. On average, thecae accounted for 75% of total P. gatunense sedimentation despite being only 55% of the P. gatunense-produced biomass, suggesting that thecae were more refractory or less grazed than protoplasts. Thecal C:N:P ratio of >3,000:19:1 (vs. 276:51:1 for protoplasts) indicated that microbial decomposition of thecae is likely to require N and P inputs from other sources. Ultimately, our study highlights for the first time that annual dinoflagellate sedimentation rates may vary dramatically as a result of other processes such as decomposition, resuspension, and grazing, leading to dramatic variations in the amount of organic matter reaching the bottom sediments.	Israel Oceanog & Limnol Res, Yigal Allon Kinneret Limnol Lab, IL-14102 Tiberias, Israel	Israel Oceanographic & Limnological Research Institute	Zohary, T (通讯作者)，Israel Oceanog & Limnol Res, Yigal Allon Kinneret Limnol Lab, POB 345, IL-14102 Tiberias, Israel.		Hambright, Karl/D-4086-2012	Hambright, K. David/0000-0002-5592-963X				ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; [Anonymous], 1992, STAND METH EX WAT WA; Berman T., 1978, Monographiae Biologicae, V32, P269; BERMAN T, 1995, LIMNOL OCEANOGR, V40, P1064, DOI 10.4319/lo.1995.40.6.1064; Berman T., 1985, VERH INT VER LIMNOL, V22, P2850; BERMAN T., 1971, Mitt. Int. Ver. Theor. Angew. 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Oceanogr.	MAR	1998	43	2					175	186		10.4319/lo.1998.43.2.0175	http://dx.doi.org/10.4319/lo.1998.43.2.0175			12	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	ZR216		Bronze			2025-03-11	WOS:000073951900001
J	Rochon, A; de Vernal, A; Sejrup, HP; Haflidason, H				Rochon, A; de Vernal, A; Sejrup, HP; Haflidason, H			Palynological evidence of climatic and oceanographic changes in the North Sea during the last deglaciation	QUATERNARY RESEARCH			English	Article						quantitative reconstruction; dinoflagellate cyst; Younger Dryas; climatic change; marine palynology; North Sea; deglaciation	LATE WEICHSELIAN VEGETATION; SOUTHWESTERN NORWAY; FLORAL MIGRATION; POLLEN DISTRIBUTION; ATLANTIC OCEAN; GREENLAND; MARINE; SEDIMENTS; ROGALAND; EUROPE	Palynological analyses performed on cores from the Norwegian Channel (Troll 8903) led to reconstruction of the late-glacial variations in sea-surface conditions using dinoflagellate cyst data and permitted direct correlation with the vegetation history of northwestern Europe derived from pollen assemblages. By similar to 15,000 yr B.P., ice rapidly receded from the Norwegian shelf and relatively warm summer conditions prevailed in surface waters. A first late-glacial cooling marked by extensive seasonal sea-ice cover is dated at ca. 13,600-13,000 C-14 yr B.P., which coincides with the Oldest Dryas interval. During the Bolling-Allerod interval, a rise in sea-surface temperature both in February (up to 3 degrees C) and August (up to 15 degrees C) led to the establishment of ice-free conditions in the northern North Sea, while pollen data reveal a densification of the vegetation cover. The beginning of the Younger Dryas interval is marked by an increase in nonarboreal pollen input indicative of the opening of the forest vegetation cover, concomitant with a cooling of surface waters during winter and development of sea-ice cover. However, sea-surface conditions remained relatively warm in summer until about 10,300 yr B.P., when extremely cold conditions and extensive sea-ice cover developed (up to 7 months/yr). Improving conditions are recorded in surface waters by similar to 10,100 yr B.P., a few hundred years before the development of forest cover onshore, as shown by the pollen record. Such a discrepancy between marine and terrestrial indicators at the end of Younger Dryas time suggests a delayed response of the vegetation to regional climate warming. (C) 1998 University of Washington.	Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; Univ Bergen, Inst Geol, N-5007 Bergen, Norway	University of Quebec; University of Quebec Montreal; University of Bergen	Rochon, A (通讯作者)，Univ Westminster, Sch Biosci, 115 New Cavendish St, London W1M 8JS, England.		de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				ALLEY RB, 1993, NATURE, V362, P527, DOI 10.1038/362527a0; ALM T, 1993, HYDROBIOLOGIA, V264, P21, DOI 10.1007/BF00014661; AMMANN B, 1989, BOREAS, V18, P109, DOI 10.1111/j.1502-3885.1989.tb00381.x; ANDERSEN ES, 1995, BOREAS, V24, P47; ATKINSON TC, 1987, NATURE, V325, P587, DOI 10.1038/325587a0; BARD E, 1994, EARTH PLANET SC LETT, V126, P275, DOI 10.1016/0012-821X(94)90112-0; BIRKS HH, 1994, J QUATERNARY SCI, V9, P133, DOI 10.1002/jqs.3390090207; Birks HH, 1996, QUATERNARY RES, V45, P119, DOI 10.1006/qres.1996.0014; BOND G, 1992, NATURE, V360, P245, DOI 10.1038/360245a0; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; DE VERNAL A, 1994, CAN J EARTH SCI, V31, P48, DOI 10.1139/e94-006; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; DE VERNAL A, 1993, GEOGR PHYS QUATERN, V47, P167, DOI 10.7202/032946ar; de Vernal A., 1987, POLLEN SPORES, V29, P291; DEVERNAL A, 1986, THESIS U MONTREAL; Faegri K., 1989, Textbook of pollen analysis, V4; GUIOT J, 1987, QUATERNARY RES, V28, P100, DOI 10.1016/0033-5894(87)90036-6; GUIOT J, 1990, I NATL SCI UNIVERS I, V1; HAFLIDASON H, 1995, GEOLOGY, V23, P1059, DOI 10.1130/0091-7613(1995)023<1059:CROTLG>2.3.CO;2; HEUSSER LE, 1983, MAR MICROPALEONTOL, V8, P77, DOI 10.1016/0377-8398(83)90006-3; JONES GA, 1988, NATURE, V336, P56, DOI 10.1038/336056a0; KOC N, 1993, QUATERNARY SCI REV, V12, P115, DOI 10.1016/0277-3791(93)90012-B; LEHMAN SJ, 1992, NATURE, V356, P757, DOI 10.1038/356757a0; MANGERUD J, 1974, Boreas (Oslo), V3, P109; MANGERUD J, 1975, QUATERNARY RES, V5, P263, DOI 10.1016/0033-5894(75)90028-9; Mangerud J., 1970, Norsk Geografisk Tidsskrift, V24, P121, DOI [10.1080/00291957008551900, DOI 10.1080/00291957008551900]; MARKHAM W.E, 1988, Ice atlas: Hudson Bay and approaches; MARKHAM WE, 1980, ATLAS GLACES LITTORA; MATTHEWS J, 1969, NEW PHYTOL, V68, P161, DOI 10.1111/j.1469-8137.1969.tb06429.x; MATTHIESSEN J, 1995, MAR MICROPALEONTOL, V24, P307, DOI 10.1016/0377-8398(94)00016-G; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; MUDIE PJ, 1982, CAN J EARTH SCI, V19, P729, DOI 10.1139/e82-062; *NAT OC DAT CTR, 1994, WORLD OC ATL; Nordberg K, 1991, PALEOCEANOGRAPHY, V6, P461, DOI 10.1029/91PA01132; NORDDAHL H, 1992, BOREAS, V21, P23; PAUS A, 1989, REV PALAEOBOT PALYNO, V61, P177, DOI 10.1016/0034-6667(89)90032-8; PAUS A, 1990, NORSK GEOL TIDSSKR, V70, P135; PAUS A, 1988, BOREAS, V17, P113; PAUS A, 1995, REV PALAEOBOT PALYNO, V85, P243, DOI 10.1016/0034-6667(94)00130-C; PAUS A, 1989, J QUATERNARY SCI, V4, P224; PONS A, 1988, PALAEOGEOGR PALAEOCL, V66, P243, DOI 10.1016/0031-0182(88)90202-7; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; ROCHON A, 1997, THESIS U QUEBEC MONT; SEJRUP HP, 1994, BOREAS, V23, P1, DOI 10.1111/j.1502-3885.1994.tb00581.x; TURON JL, 1984, THESIS U BORDEAUX; WALKER MJC, 1994, J QUATERNARY SCI, V9, P109, DOI 10.1002/jqs.3390090204; Wohlfarth B, 1996, QUATERNARY SCI REV, V15, P267, DOI 10.1016/0277-3791(96)00001-7; Zielinski GA, 1996, QUATERNARY RES, V45, P109, DOI 10.1006/qres.1996.0013	48	53	56	0	7	ACADEMIC PRESS INC	SAN DIEGO	525 B ST, STE 1900, SAN DIEGO, CA 92101-4495 USA	0033-5894			QUATERNARY RES	Quat. Res.	MAR	1998	49	2					197	207		10.1006/qres.1997.1956	http://dx.doi.org/10.1006/qres.1997.1956			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	ZM315					2025-03-11	WOS:000073526200006
J	Jolley, DW				Jolley, DW			Palynostratigraphy and depositional history of the Palaeocene Ormesby/Thanet depositional sequence set in southeastern England and its correlation with continental West Europe and the Lista Formation, North Sea	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palaeocene; dinocysts; pollen; stratigraphy; Ormesby/Thanet	DINOFLAGELLATE CYSTS; STRATIGRAPHY; SEDIMENTS; EOCENE; UK	Analysis of palynofloras from eleven sections of the Late Palaeocene Thanet Sand and Ormesby Clay Formations of southeastern England has enabled construction of a stratigraphy for a period of approximately 2 Myr, based upon eighteen palynofloral association sequences. This high-resolution stratigraphy has allowed the accurate recognition of the extent of depositional sequences in the region. Deposition of claystones was initiated in Norfolk after 58.5 Ma as a prograding series of five parasequences. with the onset of sedimentation in the majority of the southeastern England area resulting from a subsequent rise in relative sea level at around 58 Ma. Relative sea levels reached a maximum at 57.91 Ma, after which a period of condensed sedimentation ensued. This first maximum flooding surface initiated deposition in the Far south of the area (Kent), and was succeeded by a distinct fall in relative sea level and subsequent retrogradation of sedimentary units. A major change in lithology and palynofloras is marked by the initiation of a further sequence at approximately 57.5 Ma, with a second maximum flooding surface occurring shortly afterwards, followed by prograding sedimentary units. The uppermost part of the Thanet Sand and Ormesby Clay formations is composed of two separate maximum flooding events, the uppermost of which is poorly preserved. The lack of any other depositional units between these events suggests the presence of a significant disconformity at this point. Comparison of the palynofloral association sequences and flooding events of southeastern England, with sections in Belgium, Denmark and with the Lista Formation in the North Sea. demonstrates a close affinity between these areas. The transgressive surface identified at the base of the Thanet Sand Formation in southeastern England is preserved as the shales immediately overlying the Balmoral tuffite of the Lista Formation, and as the bass of the Orp Sands in Belgium and Holmehus Formation in Denmark. The subsequent record of relative sea level change in the south is mirrored in the Lista Formation. with the maximum flooding events bring represented by shales and the intervening prograding sequences by siltstones and thick sands. This comparability of the record implies a similar regime of relative sea level change in the North Sea and southeastern England area throughout the deposition of the Lista/Omresby/Thaner sediments, prior to the contrasting environments of Sele Formation-Lambeth Group sedimentation. (C) 1998 Elsevier Science B.V.	Univ Sheffield, Ctr Palynol Studies, Sheffield S1 3JD, S Yorkshire, England	University of Sheffield	Jolley, DW (通讯作者)，Univ Sheffield, Ctr Palynol Studies, Mappin St, Sheffield S1 3JD, S Yorkshire, England.							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P., 1933, BULL TORREY BOT CLUB, V60, P479, DOI 10.2307/2480586	82	20	20	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	1998	99	3-4					265	315		10.1016/S0034-6667(97)00039-0	http://dx.doi.org/10.1016/S0034-6667(97)00039-0			51	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	ZJ339					2025-03-11	WOS:000073204100005
J	Riding, JB; Crame, JA; Dettmann, ME; Cantrill, DJ				Riding, JB; Crame, JA; Dettmann, ME; Cantrill, DJ			The age of the base of the Gustav Group in the James Ross Basin, Antarctica	CRETACEOUS RESEARCH			English	Article						Aptian; biostratigraphy; James Ross Basin; Antarctica; palynology	SEYMOUR-ISLAND; PENINSULA; PALYNOLOGY; STRATIGRAPHY; LIVINGSTON; POINT	The Lagrelius Point Formation from its type area in north-west James Ross Island, Antarctica has yielded dinoflagellate cysts indicative of an earliest Aptian age. Reworked palynomorphs presumed to be from the Nordenskjold Formation (Kimmeridgian-Berriasian) were also encountered. The Lagrelius Point Formation also contains Early Cretaceous spore-pollen floras of Austral aspect. The indigenous stratigraphically significant dinoflagellate cysts include Herenaeenia postprojecta, Muderongia spp., Odontochitina spp. and Ovoidinium cinctum. This assemblage indicates that the Lagrelius Point Formation, the oldest formation of the Gustav Group, is Aptian rather than Barremian in age. This in turn means that the base of the extensive Cretaceous marine succession in the James Ross Basin can be dated accurately for the first time. The Lagrelius Point Formation is correlated with the Australian Odontochitina operculata dinoflagellate cyst Oppel Zone and the Cyclosporites hughesii spore-pollen Interval Zone. The extensive record of Aptian marine sedimentation within the James Ross Basin can be correlated directly with that of other key localities in the Antarctic Peninsula and Scotia are regions. There is still the possibility of a major stratigraphical hiatus in the preceding Hauterivian-Barremian stages. (C) 1998 Academic Press Limited.	British Geol Survey, Nottingham NG12 5GG, England; British Antarctic Survey, NERC, Cambridge CB3 0ET, England; Univ Queensland, Dept Bot, St Lucia, Qld 4067, Australia	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of Queensland	British Geol Survey, Nottingham NG12 5GG, England.		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Res.	FEB	1998	19	1					87	105		10.1006/cres.1998.0098	http://dx.doi.org/10.1006/cres.1998.0098			19	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	ZJ997					2025-03-11	WOS:000073274700005
