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J	Kim, SY; Lim, DI; Cho, HJ				Kim, So-Young; Lim, Dhong-Il; Cho, Hyun-Jin			Dinoflagellate cyst assemblages from the northern shelf sediments of the East China Sea: An indicator of marine productivity	MARINE MICROPALEONTOLOGY			English	Article						Shelf sediments; Dinoflagellate cyst; Paleoenvironments; East China Sea	YANGTZE-RIVER ESTUARY; SURFACE SEDIMENTS; CHANGJIANG ESTUARY; PACIFIC MARGIN; ALGAL GROWTH; CROSS-SHELF; GORGES DAM; PHYTOPLANKTON; WATER; KUROSHIO	The dinoflagellate cyst assemblages from the northern shelf of the East China Sea were examined to assess their potential use as indicators of marine productivity in shelf environments. A characteristic disparity in the species compositions of dinoflagellate cysts between coastal sediments and outer-shelf sediments was observed. Coastal areas affected by fluvial freshwater input adjacent to the Changjiang River mouth were dominated by protoperidinioid species, whereas open sea shelf areas were dominated by gonyaulacoid species. The rarity of protoperidinioid cysts in the shelf sediment is primarily attributable to the deficit of silicate in the waters overlying the northern East China Sea shelf, associated with low supplies of suspended particulate matter from the adjacent continent. This would limit the growth of the protoperidinioid species, which feed on diatoms. In contrast, a constant supply of nitrogen generated by microbial nitrogen fixation appeared to have played an important role in supporting the production of gonyaulacoid species in this shelf region. Thus it was determined that dinoflagellate cyst assemblages in marine sediments are closely linked to significant changes in nutrient composition, leading to a selective advantage for the growth of favored taxa. This result suggests that gonyaulacoid dinoflagellate cysts are a potentially useful proxy indicator for low nutrient concentration levels, especially of silicate, in the shelf environment. (C) 2012 Elsevier By. All rights reserved.	[Lim, Dhong-Il] Korea Ocean Res & Dev Inst, S Sea Res Ctr, Lib Marine Samples LIMS, Jangmok Myun 656830, Geoje, South Korea; [Kim, So-Young] Korea Polar Res Inst, Div Polar Climate Res, Inchon 406840, South Korea; [Cho, Hyun-Jin] Korea Coast Guard, Marine Pollut Response Dept, Inchon 406741, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Korea Polar Research Institute (KOPRI); Korea Institute of Ocean Science & Technology (KIOST)	Lim, DI (通讯作者)，Korea Ocean Res & Dev Inst, S Sea Res Ctr, Lib Marine Samples LIMS, 391 Jangmok Ri, Jangmok Myun 656830, Geoje, South Korea.	oceanlim@kordi.re.kr	Lim, Dhongil/ACH-3964-2022; Kim, So-Young/JFS-7698-2023	Lim, Dhongil/0000-0002-0832-2907	Korea Ocean Research and Development Institute (KORDI) [PM56482]; Korea Polar Research Institute research program [PP12030]	Korea Ocean Research and Development Institute (KORDI); Korea Polar Research Institute research program(Korea Polar Research Institute of Marine Research Placement (KOPRI))	This study was supported by the Korea Ocean Research and Development Institute (KORDI) research program under grant no. PM56482. This study is also partly funded by the Korea Polar Research Institute research program (grant no. PP12030). We thank the Library of Marine Samples (LIMS) in KORDI for supplying the sediment samples.	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Micropaleontol.	DEC	2012	96-97						75	83		10.1016/j.marmicro.2012.09.003	http://dx.doi.org/10.1016/j.marmicro.2012.09.003			9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	039RL					2025-03-11	WOS:000311264100008
J	Tang, YZ; Gobler, CJ				Tang, Ying Zhong; Gobler, Christopher J.			The toxic dinoflagellate <i>Cochlodinium polykrikoides</i> (Dinophyceae) produces resting cysts	HARMFUL ALGAE			English	Article						Bloom initiation; Bloom expansion; Cochlodinium polykrikoides; Encystment; Excystment; Germination; Harmful algal bloom (HAB); Resting cyst	HARMFUL ALGAL BLOOMS; DIURNAL VERTICAL MIGRATION; RED TIDE BLOOMS; LONG-ISLAND; UNARMORED DINOFLAGELLATE; GONYAULAX-TAMARENSIS; SURFACE SEDIMENTS; COASTAL WATERS; NEW-YORK; GYMNODINIALES	While harmful algal blooms (HABs) caused by the toxic dinoflagellate Cochlodinium polykrikoides have been known to science for more than a century, the past two decades have witnessed an extraordinary expansion of these events across Asia, North America, and even Europe. Although the production of resting cysts and subsequent transport via ships' ballast water or/and the transfer of shellfish stocks could facilitate this expansion, confirmative evidence for cyst production by C. polykrikoides is not available. Here, we provide visual confirmation of the production of resting cysts by C. polykrikoides in laboratory cultures isolated from North America. Evidence includes sexually mating cell pairs, planozygotes with two longitudinal flagella, formation of both pellicular (temporary) cysts and resting cysts, and a time series of the cyst germination process. Resting cyst germination occurred up to 1 month after cyst formation and 2-40% of resting cysts were successfully germinated in cultures maintained at 18-21 degrees C. Pellicular cysts with hyaline membranes were generally larger than resting cysts, displayed discernable cingulum and/or sulcus, and reverted to vegetative cells within 24 h to similar to 1 week of formation. A putative armored stage of C. polykrikoides was not observed during any life cycle stage in this study. This definitive evidence of resting cyst production by C polykrikoides provides a mechanism to account for the recurrence of annual blooms in given locales as well as the global expansion of C. polykrikoides blooms during the past two decades. (C) 2012 Elsevier B.V. All rights reserved.	[Tang, Ying Zhong; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA	State University of New York (SUNY) System; Stony Brook University	Gobler, CJ (通讯作者)，SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA.	christopher.gobler@stonybrook.edu	Gobler, Christopher/JOZ-2924-2023		Suffolk County Department of Health Services, Office of Ecology; New Tamarind Foundation	Suffolk County Department of Health Services, Office of Ecology; New Tamarind Foundation	We acknowledge support from the Suffolk County Department of Health Services, Office of Ecology, and the New Tamarind Foundation. We are thankful for the assistance and cooperation of the Stony Brook - Southampton Marine Science Center staff. We thank Greg Doucette for providing a culture of CPCB-10 and Don Anderson for agreeing to share the culture. 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J	Soehner, S; Zinssmeister, C; Kirsch, M; Gottschling, M				Soehner, Sylvia; Zinssmeister, Carmen; Kirsch, Monika; Gottschling, Marc			Who am I - and if so, how many? Species diversity of calcareous dinophytes (Thoracosphaeraceae, Peridiniales) in the Mediterranean Sea	ORGANISMS DIVERSITY & EVOLUTION			English	Article						Calcareous dinophytes; ITS; Ribotype; Cryptic species	SP-NOV DINOPHYCEAE; DINOFLAGELLATE CYSTS; SCRIPPSIELLA-TROCHOIDEA; SURFACE SEDIMENTS; MARINE DINOFLAGELLATE; DNA BARCODES; PHYLOGENY; EVOLUTION; COMPLEX; SOUTH	The diversity of extant calcareous dinophytes (Thoracosphaeraceae, Dinophyceae) is not fully recorded at present. The establishment of algal strains collected at multiple localities is necessary for a rigorous study of taxonomy, morphology and evolution in these unicellular organisms. We collected sediment and water tow samples from more than 60 localities in coastal areas of the eastern Mediterranean Sea and documented 15 morphospecies of calcareous dinophytes. Internal transcribed spacer (ITS) barcoding identified numerous species of the Scrippsiella trochoidea species complex that were genetically distinct, but indistinguishable in gross morphology (i.e. with the same tabulation patterns of the motile theca and similar spiny coccoid stages). We assessed a possible minimal number of cryptic species using ITS ribotype networks that indicated the existence of at least 21 species within the Scrippsiella trochoidea species complex. Species diversity of calcareous dinophytes appears higher in the Mediterranean Sea than in other parts of the world's oceans such as the North Sea. Our data underline the importance of field work to record the diversity of calcareous dinophytes and other unicellular life forms.	[Soehner, Sylvia; Zinssmeister, Carmen; Gottschling, Marc] Univ Munich, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Soehner, Sylvia; Zinssmeister, Carmen] Free Univ Berlin, Fachbereich Geol Wissensch, Fachrichtung Palaontol, D-12249 Berlin, Germany; [Kirsch, Monika] Univ Bremen, Fachrichtung Hist Geol Palaontol, Fachbereich Geowissensch, D-28359 Bremen, Germany	University of Munich; Free University of Berlin; University of Bremen	Soehner, S (通讯作者)，Univ Munich, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	sylvia.soehner@biologie.uni-muenchen.de	Gottschling, Marc/K-2186-2014		Deutsche Forschungsgemeinschaft [KE 322/36, RI 1738/5, WI 725/25]; Munchener Universitatsgesellschaft	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Munchener Universitatsgesellschaft	We thank Julia Daum, Patricia Silva Flores and Martina Rom-Roeske for their assistance during cultivation of the strains. Mona Hoppenrath (Bremerhaven) and Michael Schweikert (Stuttgart) gave valuable advices in methodologies. We thank two anonymous reviewers for constructive and motivating reviews of our manuscript. Financial support was provided by the Deutsche Forschungsgemeinschaft (grants KE 322/36, RI 1738/5, and WI 725/25), and the Munchener Universitatsgesellschaft, which is grateful acknowledged here.	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J	Dybkjær, K; King, C; Sheldon, E				Dybkjaer, Karen; King, Chris; Sheldon, Emma			Identification and characterisation of the Oligocene-Miocene boundary (base Neogene) in the eastern North Sea Basin - based on dinocyst stratigraphy, micropalaeontology and δ<SUP>13</SUP>C-isotope data	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						North Sea Basin; Chattian; Aquitanian; Mi-1 glaciation event; Frida-1; Palynology; Micropalaeontology; delta C-13-isotopes	ORBITALLY-INDUCED OSCILLATIONS; GLOBAL STRATOTYPE SECTION; ANTARCTIC ICE-SHEET; ASTRONOMICAL CALIBRATION; DINOFLAGELLATE CYSTS; UPPERMOST OLIGOCENE; POINT GSSP; BIOSTRATIGRAPHY; TERTIARY; ISOTOPE	For the first time a combined palynological and delta C-13-isotope study has identified the Oligocene-Miocene boundary - and thus the base of the Neogene - within the North Sea Basin. The type section, the Lemme-Carrosio section in northern Italy, is correlated with the Frida-1 well in the eastern (Danish) part of the North Sea Basin using a combination of data from a previous dinocyst stratigraphic study and new delta C-13-isotope data. The results show that the Oligocene-Miocene boundary is located at a depth of 1440 m in the Frida-1 well. The Frida-1 delta C-13-isotope curve further reflects the Mi-1 glaciation event also recorded in the Lemme-Carrosio section. The dinocyst events bracketing the boundary in Frida-1 are; the last occurrence (LO) of Distatodinium biffii at 1630 m, below the boundary, the LO of Chiropteridium spp. at 1370 m and first occurrence (FO) of Ectosphaeropsis burdigalensis at 1330 m, both above the boundary. An influx of Deflandrea phosphoritica is found in an interval immediately below the boundary (1532-1490 m), while the genus Homotryblium occurs abundantly in a broader interval (1650-1330 m) encompassing the boundary. Hitherto unpublished data combined with new data provide a series of stratigraphically important nanno- and micropalaeontological events that frame/characterise the Oligocene-Miocene boundary within the North Sea Basin; an almost monospecific assemblage of Reticulofenestra bisecta at 1630 m, the LO of Elphidium subnodosum at 1625 m, the LO of Aulacodiscus insignis quadrata (Diatom sp. 3 of King, 1983) at 1610 m, the LO of Karreriella seigliei at 1580 m and the LO of Pararotalia canui at 1570 m, all below the boundary, and the FO of Aulacodiscus aemulans (Diatom sp. 5 of King, 1983) at 1410 m and the LO of Aulacodiscus aemulans at 1250 m, both above the boundary. The dinocyst, nanno- and micropalaeontological studies thus provide a series of bioevents and abundance variations which can be used to locate and to correlate the Oligocene-Miocene boundary within the eastern North Sea Basin more precisely than was previously possible. (C) 2012 Elsevier B.V. All rights reserved.	[Dybkjaer, Karen; Sheldon, Emma] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Dybkjær, K (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018; Sheldon, Emma/H-5281-2018	Sheldon, Emma/0000-0003-4353-8241				Andersen C., 1982, GEOLOGY DANISH CENTR, V8, P9, DOI 10.34194/serieb.v8.7063; Andreoni C., 1981, RIV ITAL PALEONTOL S, V87, P245; [Anonymous], 1988, Geol. Jahrbuch, Reihe A; [Anonymous], MICROPALEONTOLOGY S; [Anonymous], 2009, GLACIAL SEDIMENTARY; ANTHONISSEN E. 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NOV 20	2012	363						11	22		10.1016/j.palaeo.2012.08.007	http://dx.doi.org/10.1016/j.palaeo.2012.08.007			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	036IW					2025-03-11	WOS:000311020600002
J	Lei, Y; Servais, T; Feng, QL; He, WH				Lei, Yong; Servais, Thomas; Feng, Qinglai; He, Weihong			The spatial (nearshore-offshore) distribution of latest Permian phytoplankton from the Yangtze Block, South China	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Acritarchs diversity; Phytoplankton distribution; Late Permian; Paleoenvironment	GLOBAL STRATOTYPE SECTION; TRIASSIC BOUNDARY; ACRITARCH DISTRIBUTION; CONODONT ZONATION; FUNGAL EVENT; DINOFLAGELLATE CYSTS; CAMBRIAN-ORDOVICIAN; SURFACE SEDIMENTS; DONGPAN SECTION; MASS EXTINCTION	In order to analyze the spatial (paleoecological) distribution of the organic-walled microphytoplankton in the Late Permian, five sections from the Yangtze Block, South China, displaying different sediment fades types (from neritic to offshore paleoenvironments, including basinal facies) have been investigated palynologically. Based on the diversity and relative abundance of acritarch species and genera, the new data from the Permian provide similar patterns as those described from other geological periods: (1) low diversities with 2 to 4 acritarch species occur in nearshore environments, whereas the higher diversities (more than ten acritarch species) appear in the offshore environments; (2) at the generic level, the genera Leiosphaeridia. Reduviasporonites and Micrhystridium are distributed widely, from nearshore facies corresponding to shallow water environments to offshore fades corresponding to deeper water settings, whereas some genera, such as Dictyotidium and Veryhachium, have a narrower distribution. occurring on the continental shelf and towards the basin, indicating open marine environments; (3) the genus Schizosporis only occurs around the Permian-Triassic-Boundary (PTB), when the sea level declined, probably indicating nearshore environments with shallow water settings; (4) at the specific level, the species Micrhystridium breve, displaying short spines, and Leiosphaeridia minutissima are indicative of neritic facies, whereas the other species of Micrhystridium and Veryhachium with longer spines (e.g., Micrhystridium stellatum and Veryhachium hyalodermum) and Leiosphaeridia microgranifera indicate more open marine environments. Big spherical acritarch species (over 80 urn in diameter), such as Dictyotidium reticulatum, indicate shallow water environments; and (5) in the PTB strata, the relative abundance of the enigmatic Reduviasporonites, interpreted by some authors as a fungal spore, is not higher than 14% in every sample, indicating that a 'spike' of Reduviasporonites does not occur in the Yangtze area. Reduviasporonites chalastus (40 mu m in length) obviously dominates in shelf environments of shallow water, whereas the smaller Reduviasporonites catenulatus (15 mu m in length) are more common in deeper water. (C) 2012 Elsevier B.V. All rights reserved.	[Lei, Yong; Feng, Qinglai] China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China; [Lei, Yong; Servais, Thomas] Univ Lille 1, CNRS, UMR Geosyst 8217, F-59655 Villeneuve Dascq, France; [He, Weihong] China Univ Geosci, State Key Lab Biogeol & Environm Geol, Wuhan 430074, Peoples R China	China University of Geosciences; Universite de Lille; Centre National de la Recherche Scientifique (CNRS); China University of Geosciences	Feng, QL (通讯作者)，China Univ Geosci, State Key Lab Geol Proc & Mineral Resources, Wuhan 430074, Peoples R China.	leiyongdida@163.com; thomas.servais@univ-lille1.fr; qinglaifeng@cug.edu.cn; whzhang@cug.edu.cn	Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018	Servais, Thomas/0000-0002-4089-7874	National Science Foundation of China (NSFC) [40839903, 40921062]; Chinese 973 program [2011CB808800]; Chinese 111 program [B08030]; Ministry of Education of China [NCET-10-0712]; Fundamental Funds for the Central Universities; University of Lille 1; Conseil Regional du Nord (France)	National Science Foundation of China (NSFC)(National Natural Science Foundation of China (NSFC)); Chinese 973 program(National Basic Research Program of China); Chinese 111 program(Ministry of Education, China - 111 Project); Ministry of Education of China(Ministry of Education, China); Fundamental Funds for the Central Universities(Fundamental Research Funds for the Central Universities); University of Lille 1; Conseil Regional du Nord (France)	We wish to express sincere thanks to Mr. Qing Hu, Lei Zhang, Guichun Liu, Jun Shen, Yu Xiang and Miss Guozhen Xu and Xiaomei Nie for their help in field work. We acknowledge the remarks and suggestions of two anonymous referees who greatly approved the final version of the paper. This work was supported by the National Science Foundation of China (NSFC) projects no. 40839903, 40921062, the Chinese 973 (2011CB808800) and 111 (B08030) programs, the Ministry of Education of China (NCET-10-0712), and the Fundamental Funds for the Central Universities, as well as by grants of the University of Lille 1 ("Allocation Presidentielle" and "Bonus Qualite Recherche") and the Conseil Regional du Nord (France).	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J	Schreck, M; Matthiessen, J; Head, MJ				Schreck, Michael; Matthiessen, Jens; Head, Martin J.			A magnetostratigraphic calibration of Middle Miocene through Pliocene dinoflagellate cyst and acritarch events in the Iceland Sea (Ocean Drilling Program Hole 907A)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Miocene; Pliocene; dinoflagellate cyst; biostratigraphy; Iceland Sea; magnetostratigraphic calibration	BASIN NORTHERN BELGIUM; GOBAN SPUR REGION; PALEOENVIRONMENTAL INTERPRETATION; CALCAREOUS NANNOPLANKTON; DEPOSITIONAL HISTORY; RESEARCH BOREHOLE; BIOSTRATIGRAPHY; STRATIGRAPHY; MORPHOLOGY; PLEISTOCENE	A detailed dinoflagellate cyst investigation of the almost continuous Middle Miocene through Pliocene of Ocean Drilling Program Hole 907A in the Iceland Sea has been conducted at 100-kyr resolution. The investigated section is well constrained by magnetostratigraphy, providing for the first time an independent temporal control on a succession of northern high-latitude dinoflagellate cyst bioevents. Based on the highest/lowest occurrences (HO/LO) and highest common occurrence (HCO) of 20 dinoflagellate cyst taxa and one acritarch species, 26 bioevents have been defined and compared with those recorded at selected DSDP, ODP, and IODP sites from the North Atlantic and contiguous seas, and in outcrops and bore-holes from the onshore and offshore eastern U.S.A., and the North Sea and Mediterranean basins. Comparisons reveal near-synchronous HOs of the dinoflagellate cysts Batiacasphaera micropapillata (3.8-3.4 Ma, mid-Pliocene) and Reticulatosphaera actinocoronata (4.8-4.2 Ma, Lower Pliocene) across the Nordic Seas and North Atlantic, highlighting their value on a supraregional scale. This probably applies also to Hystrichosphaeropsis obscura (upper Tortonian), when excluding ODP Hole 907A where its sporadic upper stratigraphic range presumably relates to cooling in the early Tortonian. Over a broader time span within the upper Tortonian, the HO of Operculodinium piaseckii likely also permits correlation across the Nordic Seas and North Atlantic, and the HO of Labyrinthodinium truncatum appears useful in the Labrador and Nordic Seas. Biostratigraphic markers useful for regional rather than supraregional correlation are the HOs of Batiacasphaera hirsuta (c. 8.4 Ma, upper Tortonian) and Unipontidinium aquaeductus (c. 13.6-13.9 Ma, upper Langhian), the HCO of the acritarch Decahedrella martinheadii (c. 6.7-6.3 Ma, Messinian), and possibly the LO of Cerebrocysta irregulare sp. nov. (c. 13.8 Ma, uppermost Langhian) across the Nordic Seas. Since Habibacysta tectata, B. micropapillata, R. actinocoronata and D. martinheadii have been observed in the Arctic Ocean, they are potentially useful for high latitude correlations in the polar domain. The LOs of Habibacysta tectata and Unipontidinium aquaeductus suggest a mid- to late Langhian age (15.1-13.7 Ma) for deposits at the base of Hole 907A, thus providing new constraints on the age of basalts at the base of ODP Hole 907A. The stratigraphically important dinoflagellate cysts Cerebrocysta irregulare sp. nov., and Impagidinium elongatum sp. nov. are formally described. (C) 2012 Elsevier B.V. All rights reserved.	[Schreck, Michael; Matthiessen, Jens] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Brock University	Schreck, M (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Alten Hafen 26, D-27568 Bremerhaven, Germany.	Michael.Schreck@awi.de		Matthiessen, Jens/0000-0002-6952-2494	German Research Foundation [DFG MA 3913/2]; Natural Sciences and Engineering Research Council of Canada	German Research Foundation(German Research Foundation (DFG)); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This research uses samples and data provided by DSDP and ODP and we thank Walter Hale and Alex Wulbers for technical support while sampling at the IODP Core Repository, Bremen. We are grateful to Morten Smelror who shared unpublished data, and Stijn De Schepper for comments on an earlier draft of this manuscript. Support was provided by the German Research Foundation (DFG MA 3913/2) to J.M. and M.S., and a Natural Sciences and Engineering Research Council of Canada Discovery Grant to M.J.H. Dirk Munsterman and an anonymous reviewer improved the manuscript with their constructive comments.	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J	Mertens, KN; Rengefors, K; Moestrup, O; Ellegaard, M				Mertens, Kenneth Neil; Rengefors, Karin; Moestrup, Ojvind; Ellegaard, Marianne			A review of recent freshwater dinoflagellate cysts: taxonomy, phylogeny, ecology and palaeocology	PHYCOLOGIA			English	Review						Biecheleria; Ceratium; Gymnodinium; Parvodinium; Peridinium; Tovellia; Woloszynskia	POPULATION GENETIC-STRUCTURE; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; LIFE-CYCLE; PERIDINIUM-GATUNENSE; SCRIPPSIELLA-HANGOEI; SEASONAL SUCCESSION; DINOPHYCEAE; NOV; PHYTOPLANKTON	Resting stages (e.g. cysts) play an important role in the life history and ecology of phytoplankton, e.g. the survival, reproduction, genetic recombination, and dispersal of many species. Marine dinoflagellates cysts have been intensively studied by both geologists and biologists, but freshwater cysts have received less attention. There are approximately 350 freshwater dinoflagellate species, and resting cysts have been described for 84 species. We evaluated the descriptions, and we reproduced images for each cyst type. The review highlighted the importance of cyst characters for taxonomy and phylogeny. We suggested that shape, wall ornamentation and possibly the archeopyle and color were important morphological characteristics at the generic level and above. The ecology of freshwater dinoflagellate cysts was reviewed, and the ecological role of cysts was discussed. The potential of freshwater cysts for Quaternary palaeoecological reconstructions was highlighted, revealing that these could serve as useful indicators of temperature, pH and productivity.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Rengefors, Karin] Dept Ecol, S-22362 Lund, Sweden; [Moestrup, Ojvind; Ellegaard, Marianne] Univ Copenhagen, Fac Sci, Dept Biol, DK-1353 Copenhagen, Denmark	Ghent University; University of Copenhagen	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Rengefors, Karin/K-5873-2019; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Ellegaard, Marianne/H-6748-2014	Mertens, Kenneth/0000-0003-2005-9483; Rengefors, Karin/0000-0001-6297-9734; Ellegaard, Marianne/0000-0002-6032-3376; Moestrup, Ojvind/0000-0003-0965-8645	Research Foundation Flandres (FWO), Belgium	Research Foundation Flandres (FWO), Belgium(FWO)	Graham Williams, Rob Fensome and Peta Mudie (Geological Survey of Canada Atlantic, Canada), Malte Elbrachter (Alfred Wegener Institute for Polar and Marine Research, Germany), Anne de Vernal (Universite du Quebec a Montreal), Rien De Raedt (Ghent University Library), Vera Pospelova and Andrea Price (University of Victoria, Canada), Antonio Calado (Universidade de Aveiro, Portugal), Andre Rochon (ISMER, Canada) and Kazumi Matsuoka (Institute for East China Sea Research, Japan) helped find obscure literature. We also thank Alla Alster, Andres Boltovskoy, Antonio Calado, Guoqiang Chu, Sandra Craveiro, Niels Daugbjerg, Maura D'andrea, Giovanna Flaim, Graziano Di Giuseppe, John Dodge, Gert Hansen, Guo-Xiang Liu, Nina Lundholm, Barbara Meyer, Ho-Dong Park, Yoshiko Sako, Francesca Sangiorgi, Howard Spero, Massimiliano Tardio, Maria Temponeras, David Wall and Gary Wedemayer for permission to reproduce their images and drawings. Leen Degezelle is thanked for help with graphical design. Martin J. Head (Brock University) and two anonymous reviewers are thanked for suggestions and comments that significantly improved the manuscript. Kenneth Neil Mertens was supported by a post-doctoral fellowship from the Research Foundation Flandres (FWO), Belgium.	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J	Bradley, LR; Marret, F; Mudie, PJ; Aksu, AE; Hiscott, RN				Bradley, L. R.; Marret, F.; Mudie, P. J.; Aksu, A. E.; Hiscott, R. N.			Constraining Holocene sea-surface conditions in the south-western Black Sea using dinoflagellate cysts	JOURNAL OF QUATERNARY SCIENCE			English	Article						Black Sea; dinoflagellate cyst; Lingulodinium machaerophorum; Quaternary; sea-surface salinity	MEDITERRANEAN SEA; LATE PLEISTOCENE; MARMARA SEA; WATER; SHELF; AGE; RECONNECTION; STRATIGRAPHY; ASSEMBLAGES; MORPHOLOGY	This paper presents two dinoflagellate cyst records from the south-western shelf of the Black Sea. A new site, MAR05-13, from the Sakarya shelf is described and placed into context with site MAR02-45, similar to 250?km distant on the Thracian shelf. The records provide a centennial resolution of surface water conditions in the Holocene. Analysis of the data suggests that the surface salinity of the south-western shelf increased in a gradual and progressive manner. In the period similar to 11?0009000 cal a BP the assemblages suggest surface-water salinities between 713 psu. The initial arrival of euryhaline species, similar to 8100 cal a BP, is linked to the reconnection of the Black Sea and Marmara Sea. The suggested surface water changes related to the reconnection took approximately 1000 years. Following this initial change in assemblages, a further increase in the number of euryhaline species is noted between 5000 and 4000 cal a BP. This is linked to the establishment of more saline surface-water conditions, close to present-day values. The record for MAR05-13 highlights the complexity of the changes in cyst assemblages during the mid-Holocene. Copyright (c) 2012 John Wiley & Sons, Ltd.	[Bradley, L. R.; Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England; [Mudie, P. J.] Geol Survey Canada Atlantic, Dartmouth, NS, Canada; [Mudie, P. J.; Aksu, A. E.; Hiscott, R. N.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF, Canada	University of Liverpool; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland	Bradley, LR (通讯作者)，Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England.	l.r.bradley@liverpool.ac.uk	Bradley, Lee/AAA-6818-2019	Bradley, Lee/0000-0003-0833-9351; Marret-Davies, Fabienne/0000-0003-4244-0437	Leverhulme Trust; Natural Sciences and Engineering Research Council of Canada	Leverhulme Trust(Leverhulme Trust); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	We thank the officers and crew of the RV Koca Piri Reis for invaluable assistance during a succession of successful cruises. L. B. and F. M. thank the Leverhulme Trust for funding. P.J.M., A. E. A. and R.N.H. were partly funded by the Natural Sciences and Engineering Research Council of Canada. Helen Gillespie is thanked for preparation of the palynomorph samples. Jennifer Cranshaw contributed to early analysis of seismic and geochemical data from the Sakarya shelf. We thank Suzanne Leroy and a anonymous reviewer for their constructive criticisms that improved the paper.	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J	Kender, S; Stephenson, MH; Riding, JB; Leng, MJ; Knox, RWO; Peck, VL; Kendrick, CP; Ellis, MA; Vane, CH; Jamieson, R				Kender, Sev; Stephenson, Michael H.; Riding, James B.; Leng, Melanie J.; Knox, Robert W. O'B; Peck, Victoria L.; Kendrick, Christopher P.; Ellis, Michael A.; Vane, Christopher H.; Jamieson, Rachel			Marine and terrestrial environmental changes in NW Europe preceding carbon release at the Paleocene-Eocene transition	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Paleocene-Eocene boundary; PETM; carbon isotope excursion; paleoecology; paleoceanography; North Sea	THERMAL MAXIMUM; ISOTOPE EXCURSION; DINOFLAGELLATE CYSTS; VEGETATION DYNAMICS; ORGANIC-MATTER; BASIN; CLIMATE; STRATIGRAPHY; PALEOGENE; BOUNDARY	Environmental changes associated with the Paleocene-Eocene thermal maximum (PETM, similar to 56 Ma) have not yet been documented in detail from the North Sea Basin. Located within proximity to the North Atlantic igneous province (NAIP), the Kilda Basin, and the northern rain belt (paleolatitude 54 degrees N) during the PETM, this is a critical region for testing proposed triggers of atmospheric carbon release that may have caused the global negative carbon isotope excursion (CIE) in marine and terrestrial environments. The CIE onset is identified from organic matter delta C-13 in exceptional detail within a highly expanded sedimentary sequence. Pollen and spore assemblages analysed in the same samples for the first time allow a reconstruction of possible changes to vegetation on the surrounding landmass. Multiproxy palynological, geochemical, and sedimentologic records demonstrate enhanced halocline stratification and terrigenous deposition well before (10(3) yrs) the CIE, interpreted as due to either tectonic uplift possibly from a nearby magmatic intrusion, or increased precipitation and fluvial runoff possibly from an enhanced hydrologic cycle. Stratification and terrigenous deposition increased further at the onset and within the earliest CIE which, coupled with evidence for sea level rise, may be interpreted as resulting from an increase in precipitation over NW Europe consistent with an enhanced hydrologic cycle in response to global warming during the PETM. Palynological evidence indicates a flora dominated by pollen from coastal swamp conifers before the CIE was abruptly replaced with a more diverse assemblage of generalist species including pollen similar to modern alder, fern, and fungal spores. This may have resulted from flooding of coastal areas due to relative sea level rise, and/or ecologic changes forced by climate. A shift towards more diverse angiosperm and pteridophyte vegetation within the early CIE, including pollen similar to modern hickory, documents a long term change to regional vegetation. Crown Copyright (C) 2012 Published by Elsevier B.V. All rights reserved.	[Kender, Sev; Leng, Melanie J.; Kendrick, Christopher P.] British Geol Survey, NERC Isotope Geosci Lab, Nottingham NG12 5GG, England; [Leng, Melanie J.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England; [Peck, Victoria L.] British Antarctic Survey, Cambridge CB3 0ET, England; [Jamieson, Rachel] Univ Edinburgh, Sch Geosci, Edinburgh EH9 3JW, Midlothian, Scotland	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Leicester; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Antarctic Survey; University of Edinburgh	Kender, S (通讯作者)，British Geol Survey, NERC Isotope Geosci Lab, Nottingham NG12 5GG, England.	sev.kender@bgs.ac.uk	Vane, Christopher/A-8814-2008; Ellis, Michael/AAP-2039-2020; Ellis, Michael Alexander/M-4505-2018; Kender, Sev/B-9409-2016	Vane, Christopher/0000-0002-8150-3640; Ellis, Michael Alexander/0000-0002-6613-3565; Kender, Sev/0000-0003-4216-3214; Leng, Melanie/0000-0003-1115-5166; Kendrick, Christopher/0000-0003-0382-4868	NERC [bgs05002, nigl010001, bas0100024] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], 2002, BATLAS - Mid Norway Plate Reconstructions Atlas with Global and Atlantic Perspectives, P48; ARTHUR MA, 1994, GLOBAL BIOGEOCHEM CY, V8, P195, DOI 10.1029/94GB00297; Bice KL, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2001PA000678; Boulter M.C., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P663, DOI 10.2973/odp.proc.sr.104.192.1989; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; Brinkhuis H, 2006, NATURE, V441, P606, DOI 10.1038/nature04692; Bujak JP, 1998, LATE PALEOCENE-EARLY EOCENE CLIMATIC AND BIOTIC EVENTS IN THE MARINE AND TERRESTRIAL RECORDS, P277; Charles AJ, 2011, GEOCHEM GEOPHY GEOSY, V12, DOI 10.1029/2010GC003426; Collinson ME, 2009, GRANA, V48, P38, DOI 10.1080/00173130802707980; Crouch EM, 2003, PALAEOGEOGR PALAEOCL, V194, P387, DOI 10.1016/S0031-0182(03)00334-1; 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Sci. Lett.	NOV 1	2012	353						108	120		10.1016/j.epsl.2012.08.011	http://dx.doi.org/10.1016/j.epsl.2012.08.011			13	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	036GL		Green Published, Green Accepted, hybrid			2025-03-11	WOS:000311014300012
J	Dai, XF; Lu, DD; Xia, P; Wang, HX; He, PX				Dai, Xin-feng; Lu, Dou-ding; Xia, Ping; Wang, Hong-xia; He, Piao-xia			A 50-year temporal record of dinoflagellate cysts in sediments from the Changjiang estuary, East China Sea, in relation to climate and catchment changes	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						harmful algal bloom; eutrophication; climatic changes; man-induced effects; short time scale; Three Gorges Project	TOKYO-BAY; NORWEGIAN FJORD; COASTAL WATERS; YOKOHAMA-PORT; ADRIATIC SEA; WEST-COAST; EUTROPHICATION; PHYTOPLANKTON; INDICATORS; PRESERVATION	Dinoflagellate cysts (dinocyst) are often used to trace environmental history within the marine realm. However, the recognition of a eutrophication signal in dinocyst records is ambiguous. In addition, as few studies have focussed on the climate signal as recorded by dinocyst proxies over a moderately short time scale, a moderately short temporal record of dinocysts in sediments from two cores recovered in the Changjiang estuary, East China Sea was investigated. Total cyst concentrations and Paralytic Shellfish Poison (PSP) cyst concentrations increased with eutrophication, and total cyst concentrations, run-off from the Changjiang River and Oceanic Nino Index peaks co-occurred. Total cyst concentrations and PSP cyst concentrations may be a potential eutrophication signal in subtropical estuaries and the climate signal could be recorded in the cyst assemblages in estuaries within a moderately short time scale as the run-off from rivers and their nutrient load changed over time. (C) 2012 Elsevier Ltd. All rights reserved.	[Dai, Xin-feng; Lu, Dou-ding; Xia, Ping; Wang, Hong-xia; He, Piao-xia] SOA, Inst Oceanog 2, Key Lab Marine Ecosyst & Biogeochem, State Ocean Adm, Hangzhou 310012, Zhejiang, Peoples R China	Ministry of Natural Resources of the People's Republic of China; Second Institute of Oceanography, Ministry of Natural Resources	Lu, DD (通讯作者)，SOA, Inst Oceanog 2, Key Lab Marine Ecosyst & Biogeochem, State Ocean Adm, 36 Baochu Rd, Hangzhou 310012, Zhejiang, Peoples R China.	ludd21@126.com	Wang, Hongxia/AAU-5674-2021		973 Program [2010CB428702]; 863 Program [2007AA09Z110]; National public benefit research sector [201005031]; Second Institute of Oceanography, SOA [SZ1040]	973 Program(National Basic Research Program of China); 863 Program(National High Technology Research and Development Program of China); National public benefit research sector; Second Institute of Oceanography, SOA	We thank Haiyan Huang, Zhenyi Cao and Haili Yang for their help in cyst identification, data collection and sediment process. This study was supported by the 973 Program (2010CB428702), 863 Program (2007AA09Z110), National public benefit research sector (201005031) and Grant from the scientific research fund of the Second Institute of Oceanography, SOA (SZ1040).	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Natural Sciences], V35, P622	32	8	13	1	54	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.	OCT 20	2012	112				SI		192	197		10.1016/j.ecss.2012.07.016	http://dx.doi.org/10.1016/j.ecss.2012.07.016			6	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	031OQ					2025-03-11	WOS:000310652000020
J	Zinssmeister, C; Soehner, S; Kirsch, M; Facher, E; Meier, KJS; Keupp, H; Gottschling, M				Zinssmeister, Carmen; Soehner, Sylvia; Kirsch, Monika; Facher, Eva; Meier, K. J. Sebastian; Keupp, Helmut; Gottschling, Marc			SAME BUT DIFFERENT: TWO NOVEL BICARINATE SPECIES OF EXTANT CALCAREOUS DINOPHYTES (THORACOSPHAERACEAE, PERIDINIALES) FROM THE MEDITERRANEAN SEA	JOURNAL OF PHYCOLOGY			English	Article						coccoid cell; cytochrome b; distribution; molecular systematics; morphology; phylogeny; ribosomal RNA; thecate cell	MULTIPLE SEQUENCE ALIGNMENT; DINOFLAGELLATE CYSTS; SCRIPPSIELLA-TROCHOIDEA; RIBOSOMAL-RNA; MIXED MODELS; PHYLOGENY; CALCIODINELLOIDEAE; CLASSIFICATION; TERMINOLOGY; SEDIMENTS	The diversity of extant calcareous dinophytes (Thoracosphaeraceae, Dinophyceae) is currently not sufficiently recorded. The majority of their coccoid stages are cryptotabulate or entirely atabulate, whereas relatively few forms exhibit at least some degree of tabulation more than the archeopyle. A survey of coastal surface sediment samples from the Mediterranean Sea resulted in the isolation and cultivation of several strains of calcareous dinophytes showing a prominent tabulation. We investigated the morphologies of the thecate and the coccoid cells and conducted phylogenetic analyses using Maximum Likelihood and Bayesian approaches. The coccoid cells showed a distinct reflection of the cingulum (and were thus cingulotabulate), whereas thecal morphology corresponded to the widely distributed and species-rich Scrippsiella. As inferred from molecular sequence data (including 81 new GenBank entries), the strains belonged to the Scrippsiella sensu lato clade of the Thoracosphaeraceae and represented two distinct species. Morphological details likewise indicated two distinct species with previously unknown coccoid cells that we describe here as new, namely S. bicarinata spec. nov. and S. kirschiae spec. nov. Cingulotabulation results from the fusion of processes representing the pre- and postcingular plate series in S. bicarinata, whereas the ridges represent sutures between the cingulum and the pre- and postcingular series in S. kirschiae, respectively. Bicarinate cingulotabulation appears homoplasious among calcareous dinophytes, which is further supported by a comparison to similar, but only distantly related fossil forms.	[Facher, Eva; Gottschling, Marc] Univ Munich, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Zinssmeister, Carmen; Soehner, Sylvia; Keupp, Helmut] Free Univ Berlin, Fachbereich Geol Wissensch, Fachrichtung Palaontol, D-12249 Berlin, Germany; [Kirsch, Monika] Univ Bremen, Fachbereich Geowissensch, Fachrichtung Hist Geol Palaontol, D-28359 Bremen, Germany; [Meier, K. J. Sebastian] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany	University of Munich; Free University of Berlin; University of Bremen; University of Kiel	Gottschling, M (通讯作者)，Univ Munich, GeoBio Ctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@biologie.uni-muenchen.de	Gottschling, Marc/K-2186-2014; Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. Sebastian/0000-0002-3918-4092	Deutsche Forschungsgemeinschaft [KE 322/36, RI 1738/5, WI 725/25]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	We are grateful to T. Uhle (Berlin) for improvement of the Latin descriptions and to three anonymous reviewers for their critical reading of the manuscript. We thank the Deutsche Forschungsgemeinschaft (grants KE 322/36, RI 1738/5, and WI 725/25) for financial support.	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Sebastian, 2009, Berliner Palaeobiologische Abhandlungen, V10, P245; Meier KJS, 2002, J PHYCOL, V38, P602, DOI 10.1046/j.1529-8817.2002.t01-1-01191.x; Montresor M, 1997, J PHYCOL, V33, P122, DOI 10.1111/j.0022-3646.1997.00122.x; Montresor M, 2003, PHYCOLOGIA, V42, P56, DOI 10.2216/i0031-8884-42-1-56.1; MONTRESOR M, 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; Ronquist F, 2003, BIOINFORMATICS, V19, P1572, DOI 10.1093/bioinformatics/btg180; SARJEANT WAS, 1982, CAN J BOT, V60, P922, DOI 10.1139/b82-119; Satta CT, 2010, DEEP-SEA RES PT II, V57, P256, DOI 10.1016/j.dsr2.2009.09.013; Soehner S., ORG DIVERS IN PRESS; SPURR AR, 1969, J ULTRA MOL STRUCT R, V26, P31, DOI 10.1016/S0022-5320(69)90033-1; Stamatakis A, 2006, BIOINFORMATICS, V22, P2688, DOI 10.1093/bioinformatics/btl446; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Streng M, 2009, REV PALAEOBOT PALYNO, V153, P225, DOI 10.1016/j.revpalbo.2008.08.004; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Tillmann U., PROTIST, V163, DOI [10.1016/j. protis2011.10.005, DOI 10.1016/J.PROTIS2011.10.005]; VERSTEEGH GJM, 1993, REV PALAEOBOT PALYNO, V78, P353, DOI 10.1016/0034-6667(93)90071-2; WALL D, 1968, Journal of Paleontology, V42, P1395; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Willems H., 1988, Senckenbergiana Lethaea, V68, P433; Young JR, 1997, PALAEONTOLOGY, V40, P875; Zhang H, 2005, J PHYCOL, V41, P411, DOI 10.1111/j.1529-8817.2005.04168.x; Zhang H, 2007, J MOL EVOL, V65, P463, DOI 10.1007/s00239-007-9038-4; Zinssmeister C, 2011, SYST BIODIVERS, V9, P145, DOI 10.1080/14772000.2011.586071	63	17	19	1	24	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0022-3646	1529-8817		J PHYCOL	J. Phycol.	OCT	2012	48	5					1107	1118		10.1111/j.1529-8817.2012.01182.x	http://dx.doi.org/10.1111/j.1529-8817.2012.01182.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	015RA	27011272				2025-03-11	WOS:000309462500006
J	Mertens, KN; Bringué, M; Van Nieuwenhove, N; Takano, Y; Pospelova, V; Rochon, A; De Vernal, A; Radi, T; Dale, B; Patterson, RT; Weckström, K; Andrén, E; Louwye, S; Matsuoka, K				Mertens, Kenneth Neil; Bringue, Manuel; Van Nieuwenhove, Nicolas; Takano, Yoshihito; Pospelova, Vera; Rochon, Andre; De Vernal, Anne; Radi, Taoufik; Dale, Barrie; Patterson, R. Timothy; Weckstrom, Kaarina; Andren, Elinor; Louwye, Stephen; Matsuoka, Kazumi			Process length variation of the cyst of the dinoflagellate Protoceratium reticulatum in the North Pacific and Baltic-Skagerrak region: calibration as an annual density proxy and first evidence of pseudo-cryptic speciation	JOURNAL OF QUATERNARY SCIENCE			English	Article						Baltic-Skagerrak; Effingham Inlet; sediment trap; SSS; SST	SURFACE SEDIMENTS; BRITISH-COLUMBIA; VANCOUVER-ISLAND; EFFINGHAM INLET; SEA; ASSEMBLAGES; PRODUCTIVITY; DINOPHYCEAE; DIVERSITY; ATLANTIC	Process length variation of cysts of the dinoflagellate Protoceratium reticulatum (Claparede et Lachmann) Butschli in surface sediments from the North Pacific was investigated. The average process length showed a significant inverse relation to annual seawater density: st annual?=?-0.8674 x average process length?+?1029.3 (R2?=?0.84), with a standard error of 0.78?kg?m-3. A sediment trap study from Effingham Inlet in British Columbia revealed the same relationship between average process length and local seawater density variations. In the BalticSkagerrak region, the average process length variation was related significantly to annual seawater density: st annual?=?3.5457 x average process length?-?993.28 (R2?=?0.86), with a standard error of 3.09?kg?m-3. These calibrations cannot be reconciled, which accentuates the regional character of the calibrations. This can be related to variations in molecular data (small subunit, long subunit and internal transcribed spacer sequences), which show the presence of several genotypes and the occurrence of pseudo-cryptic speciation within this species. Copyright (C) 2012 John Wiley & Sons, Ltd.	[Mertens, Kenneth Neil; Louwye, Stephen; Matsuoka, Kazumi] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Bringue, Manuel; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada; [Van Nieuwenhove, Nicolas; De Vernal, Anne; Radi, Taoufik] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Van Nieuwenhove, Nicolas] Helmholtz Ctr Ocean Res Kiel, GEOMAR, Kiel, Germany; [Takano, Yoshihito; Matsuoka, Kazumi] Inst E China Sea Res ECSER, Nagasaki, Japan; [Rochon, Andre] Univ Quebec, Inst Sci Rimouski ISMER, Rimouski, PQ G5L 3A1, Canada; [Dale, Barrie] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [Patterson, R. Timothy] Carleton Univ, Ottawa Carleton Geosci Ctr, Ottawa, ON K1S 5B6, Canada; [Patterson, R. Timothy] Carleton Univ, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada; [Andren, Elinor] Sodertorn Univ, Sch Life Sci, Huddinge, Sweden	Ghent University; University of Victoria; University of Quebec; University of Quebec Montreal; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; University of Quebec; University of Oslo; Carleton University; University of Ottawa; Carleton University; Sodertorn University	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be	Van Nieuwenhove, Nicolas/IAQ-1532-2023; Mertens, Kenneth/AAO-9566-2020; Bringue, Manuel/KIH-8224-2024; Louwye, Stephen/D-3856-2012; de Vernal, Anne/D-5602-2013; Mertens, Kenneth/C-3386-2015	Louwye, Stephen/0000-0003-4814-4313; de Vernal, Anne/0000-0001-5656-724X; Weckstrom, Kaarina/0000-0002-3889-0788; Mertens, Kenneth/0000-0003-2005-9483; Pospelova, Vera/0000-0003-4049-8133; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Bringue, Manuel/0000-0003-4460-8344	Kakenhi [22-00805]; Natural Sciences and Engineering Research Council of Canada (NSERC)	Kakenhi(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	Sirje Vilbaste (Estonian University of Life Sciences) is thanked for providing samples from Estonia, which unfortunately did not contain enough cysts. K.N.M. is a postdoctoral fellow of FWO Belgium, who conducted this research at the University of Victoria (British Columbia, Canada) and partly at Nagasaki University and was supported by a Kakenhi grant 22-00805. The sediment trap data from Effingham Inlet was obtained through a Natural Sciences and Engineering Research Council of Canada Strategic Project grant to R.T.P. This research was partly supported by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a grant to V.P. Mr Hiromi Saitoh and Kimihiko Maekawa are thanked for assistance during sampling of Saroma Lake. Anna Godhe is thanked for providing a sample from Kattegat for molecular analysis. Two anonymous reviewers and the Editor are acknowledged, whose comments significantly improved the manuscript.	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Quat. Sci.	OCT	2012	27	7					734	744		10.1002/jqs.2564	http://dx.doi.org/10.1002/jqs.2564			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	019ML					2025-03-11	WOS:000309743800009
J	D'Silva, MS; Anil, AC; Borole, DV; Nath, BN; Singhal, RK				D'Silva, Maria Shamina; Anil, Arga Chandrashekar; Borole, Dnyandev Vaman; Nath, Bejugam Nagender; Singhal, Rakesh Kumar			Tracking the history of dinoflagellate cyst assemblages in sediments from the west coast of India	JOURNAL OF SEA RESEARCH			English	Article						Dinoflagellate Cysts; Harmful Algal Blooms; Organic Matter; Heterotrophic; Monsoon; India	RECENT MARINE-SEDIMENTS; PROTOPERIDINIUM CF DIVERGENS; ARABIAN SEA; ENVIRONMENTAL CHARACTERISTICS; THECA RELATIONSHIPS; SOUTHWEST MONSOON; BALLAST WATER; YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION	In order to trace the history of dinoflagellate cyst assemblages and provide new insights in to Harmful Algal Bloom (HAB) dynamics in monsoon-influenced tropical environments, sediment cores were collected from four different coastal locations along the west coast of India. The naturally occurring radionuclide Pb-210 activity in the sediment samples were measured; and subsequently the sedimentation rates (SRs) and ages were modeled. The SRs ranged from 0.15 +/- 0.01 to 2.80 +/- 0.38 cm/yr and provided coverage of time period spanning between 21 and 145 yr. Cysts of potential harmful dinoflagellates (Gonyaulax spinifera, Lingulodinium polyedrum, Protoceratium reticulatum and Scrippsiella trochoidea) were observed to be present earlier than the 20th century. Among the four sediment cores, significant temporal variations in cyst abundance were observed in the sediment core, off Mangalore. Two of the cores from off Mangalore and Cannanore were dominated by autotrophic cyst assemblages (Gonyaulax membranacea and Gonyaulax spinifera) in the deeper sediment sections. However, the upper sediment sections were dominated by heterotrophic forms. Temporal shifts in cyst assemblages from autotrophic to heterotrophic dinoflagellates in the Mangalore core coincided with high deposition of shells; carbon analyses (delta C-13(org) and C-org:N ratio) revealed shifts in organic matter type from terrestrial to marine source. The terrigenous input in this region, influenced by the monsoonal variations, can thus affect dinoflagellate assemblage structure and lead to changes in ecosystem functioning. (c) 2012 Elsevier B.V. All rights reserved.	[D'Silva, Maria Shamina; Anil, Arga Chandrashekar; Borole, Dnyandev Vaman; Nath, Bejugam Nagender] CSIR Natl Inst Oceanog, Panaji 403004, Goa, India; [Singhal, Rakesh Kumar] Bhabha Atom Res Ctr, Div Analyt Chem, Mod Labs, Bombay 400085, Maharashtra, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO); Bhabha Atomic Research Center (BARC)	Anil, AC (通讯作者)，CSIR Natl Inst Oceanog, Panaji 403004, Goa, India.	acanil@nio.org	Singhal, Rakesh Kumar/ITT-5521-2023	Singhal, Rakesh Kumar/0000-0002-6421-5110	Directorate General of Shipping. Government of India; Council of Scientific and Industrial Research (CSIR)	Directorate General of Shipping. Government of India(Ministry of Shipping, Government of IndiaDirectorate General of Shipping (DGS), Government of India); Council of Scientific and Industrial Research (CSIR)(Council of Scientific & Industrial Research (CSIR) - India)	We are grateful to Dr. S.R. Shetye, Director of National Institute of Oceanography for his support and encouragement. This work was carried out as part of Ballast Water Management Programme, India, funded by the Directorate General of Shipping. Government of India. We are also grateful to Dr. V.K. Banakar, Dr. P. Divakar Naidu, Dr. R. Saraswat, Dr. A. Mudholkar and Dr. R. Rengarajan (PRL) for their advice and help at various stages of research work. We thank Mr. Prakash Babu, Mr. S. Vijayan, Mrs. A. Garg and Mr. C. Morares for their technical support in sample analysis. We also thank Mr. V. Khedekar and Mr. A. Sardar for their help in SEM photomicrographs. We acknowledge the help of Mr. K. Venkat, Dr. R.K. Naik, Mr. Dhiraj to Mr. D.D. Narale during cruises, and our colleagues for their help and suggestions. The authors thank the anonymous reviewers for their suggestions which helped to improve the manuscript. M.S.D. acknowledges the Council of Scientific and Industrial Research (CSIR) for the award of Senior Research Fellowship (SRF). This is a NIO contribution (5207).	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Sea Res.	OCT	2012	73						86	100		10.1016/j.seares.2012.06.013	http://dx.doi.org/10.1016/j.seares.2012.06.013			15	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	009NN					2025-03-11	WOS:000309032600010
J	Shin, HH; Park, JS; Kim, YO; Baek, SH; Lim, D; Yoon, YH				Shin, Hyeon Ho; Park, Jong Sick; Kim, Young-Ok; Baek, Seung Ho; Lim, Dhongil; Yoon, Yang Ho			Dinoflagellate cyst production and flux in Gamak Bay, Korea: A sediment trap study	MARINE MICROPALEONTOLOGY			English	Article						Sediment trap; Surface sediment; Dinoflagellate cyst; Polykrikos species; Gamak Bay	POLYKRIKOS-KOFOIDII; SURFACE SEDIMENTS; ALEXANDRIUM-TAMARENSE; ECOLOGICAL ROLES; TOKYO-BAY; RED-TIDE; EUTROPHICATION; DINOPHYCEAE; SCRIPPSIELLA; TEMPERATURE	To develop a better understanding of the species composition and production of dinoflagellate cysts, including the ecological characteristics of Polykrikos species, a sediment trap study was conducted from June 2005 to June 2006 in Gamak Bay, Korea. Thirty-two dinoflagellate cyst taxa were identified in the sediment trap samples, and the dinoflagellate cyst assemblages were found to be dominated by cysts of Polykrikos kofoidii, Scrippsiella trochoidea, Protoperidinium spp., Polykrikos schwartzii, Gymnodinium catenatum and Ensiculifera carinata. The flux of dinoflagellate cysts ranged from 0.10 x 10(5) to 35.97 x 10(5) cysts m(-2) day(-1), and the highest flux occurred during summer, and was driven completely by the flux in the production of P. kofoidii and P. schwartzii cysts. The timing of the production of cysts of Polykrikos species seemed to be related to the appearance of G. catenatum as prey. The assemblages of dinoflagellate cysts in surface sediments from Gamak Bay, and their seasonal changes, were very similar to those in the sediment trap samples, which suggested that the monitoring of dinoflagellate cysts in sediment samples can provide information on the environmental conditions in Gamak Bay. (c) 2012 Elsevier B.V. All rights reserved.	[Park, Jong Sick; Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Yeosu 550749, South Korea; [Shin, Hyeon Ho] Korea Ocean Res & Dev Inst, Lib Marine Samples, Geoje 656830, South Korea; [Kim, Young-Ok; Baek, Seung Ho; Lim, Dhongil] Korea Ocean Res & Dev Inst, S Sea Inst, Geoje 656830, South Korea	Chonnam National University; Korea Institute of Ocean Science & Technology (KIOST); Korea Institute of Ocean Science & Technology (KIOST)	Yoon, YH (通讯作者)，Chonnam Natl Univ, Fac Marine Technol, Mipyeongro 386, Yeosu 550749, South Korea.	yoonyh@chonnam.ac.kr	KIM, YOUNG JIN/E-9374-2011; Lim, Dhongil/ACH-3964-2022	BAEK, SEUNG HO/0000-0002-5402-2518; Yoon, Yang Ho/0000-0001-8529-9512; Shin, Hyeon Ho/0000-0002-9711-6717; Baek, Seung Ho/0000-0003-2722-5907; Lim, Dhongil/0000-0002-0832-2907	Korea Ocean Research and Development Institute [PE98582]; program (Development of marine-bioenergy and assessment of the impact of climate change on marine ecosystem in the South Sea of Korea); Ministry of Land, Transport and Maritime Affairs of Korean Government	Korea Ocean Research and Development Institute; program (Development of marine-bioenergy and assessment of the impact of climate change on marine ecosystem in the South Sea of Korea); Ministry of Land, Transport and Maritime Affairs of Korean Government(Ministry of Land, Transport and Maritime Affairs (MLTM), Republic of Korea)	We thank all members of the Laboratory of Marine Bio-Environmental Science, Chonnam National University, for their kind help with the cyst analysis. This work was supported by a grant from the Korea Ocean Research and Development Institute (PE98582) and program (Development of marine-bioenergy and assessment of the impact of climate change on marine ecosystem in the South Sea of Korea) funded by Ministry of Land, Transport and Maritime Affairs of Korean Government.	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Micropaleontol.	OCT	2012	94-95						72	79		10.1016/j.marmicro.2012.06.005	http://dx.doi.org/10.1016/j.marmicro.2012.06.005			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	007RC					2025-03-11	WOS:000308904800006
J	Prauss, ML				Prauss, Michael L.			The Cenomanian/Turonian Boundary Event (CBE) at Tarfaya, Morocco, northwest Africa: Eccentricity controlled water column stratification as major factor for total organic carbon (TOC) accumulation: Evidence from marine palynology	CRETACEOUS RESEARCH			English	Article						Northwest Africa; Cenomanian; Turonian; Anoxic; Event; Palynology; Prasinophytes	SEA-LEVEL CHANGE; DINOFLAGELLATE CYSTS; PALEOENVIRONMENTAL ANALYSIS; WESTERN INTERIOR; ANOXIC EVENT; DINOCYST; BASIN; RECORD; STRATIGRAPHY; ASSEMBLAGES	From the exploration core S75 that covers the Cenomanian/Turonian Boundary Event (CTBE) and lower Turonian at Tarfaya, Morocco, northwest Africa, 96 samples from a section 24.5 m thick was analysed palynologically. The palynological data are discussed with various data on isotope- and bio-geochemistry as well as on time series analyses published by Kolonic et al. (2005, Paleoceanography 20, PA 1006) and Kuhnt et al. (2005, Int. J. Earth Sci. 94, 147-159). The dinocyst assemblage is of low to moderate diversity and strongly dominated by peridinioids throughout most of the section. It is suggested, that potentially eccentricity controlled cycles of increased total organic carbon (TOC) accumulation are closely related to increases of the ratio in proportions of peridinioid to gonaulacoid dinocysts (p/g ratio) and proportions of Botryocccus as well as of Bosedinia spp., a peridinioid cyst of probable strongly reduced-salinity water. At higher resolution, however, episodic increases in the p/g ratio are more punctuated in distribution and largely inversely correlated to abundances of Bosedinia spp. It is suggested that warm-humid climatic boundary conditions prevailed in the Tafaya region, episodically superimposed by upwelling events, reflected by increased proportions of Palaeohystrichophora spp. and Subtilisphaera spp. Accordingly, enhanced preservation, supported by strong episodic production pulses, is proposed for the TOC accumulation in the Tarfaya Basin. The p/g ratio peaks decrease both in prominence and frequency when pre-excursion values of delta C-13 isotopes are re-established after the positive anomaly. This may reflect a moderate shift in control from production to preservation of TOC following the CTBE proper. With respect to delta O-13 isotopes, episodes of pre-excursion values, possibly reflecting moderate cooling intervals and eustatic sea-level fall, are characterised by the appearance of dinocyst taxa diagnostic of neritic waters. This may reflect the gradual change from pelagic sedimentation characteristic of the plateau- and early recovery-period of delta C-13 isotopes towards neritic conditions within the late recovery and post-excursion period. Biomarkers suggestive of photic zone oxygen deficiency show only a limited relationship to the distribution of the different algal groups. However, according to the quantitative distribution of prasinophytes, considered to be critically controlled by ammonium availability, denitrification was more prominent during the late Cenomanian interval of the section and decreased significantly with the onset of the Turonian. (C) 2012 Elsevier Ltd. All rights reserved.	Free Univ Berlin, Inst Geol Sci, Sect Palaeontol, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Free Univ Berlin, Inst Geol Sci, Sect Palaeontol, Malteser Str 74-100,Bldg D, D-12249 Berlin, Germany.	mprauss@zedat.fu-berlin.de			Deutsche Forschungsgemeinschaft (DFG) [KE 322/39-1]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	Thomas Wagner, Civil Engineering and Geosciences, University of Newcastle, UK has provided sample material and great support during sampling. Data on TOC, isotopes and biomarkers were provided by Sadat Kolonic, Exploration Team Leader at Shell EP, Jordan. The constructive comments of two anonymous reviewers and the competent editing by David Batten are gratefully acknowledged. The study has been funded by a grant of the Deutsche Forschungsgemeinschaft (DFG), grant no. KE 322/39-1.	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Res.	OCT	2012	37						246	260		10.1016/j.cretres.2012.04.007	http://dx.doi.org/10.1016/j.cretres.2012.04.007			15	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	970VG					2025-03-11	WOS:000306159800022
J	Prauss, ML				Prauss, Michael L.			Potential freshwater dinocysts from marine upper Cenomanian to upper Coniacian strata of Tarfaya, northwest Africa: Three new species of <i>Bosedinia</i>	CRETACEOUS RESEARCH			English	Article						Dinoflagellate cysts; Bosedinia; Freshwater; Cenomanian; Turonian; Coniacian; Oceanic anoxic event	BOUNDARY EVENT CTBE; MOROCCO	Three new species of Bosedinia He emend. Chen et al. are described: B. alyeolata, B. spinosa and B. tarfayensis. The diagnosis of the genus Bosedinia is emended to include forms with an alveolate wall and/or hair-like spiny processes. The appearance in massive blooms across considerable section intervals closely related to and within oceanic anoxic event 2 (Cenomanian-Turonian) and anoxic event 3 (Coniacian-Santonian) suggests episodic salinity stratification as important aspect for enhanced organic carbon accumulation. (C) 2012 Elsevier Ltd. All rights reserved.	Free Univ Berlin, Inst Geol Sci, Palaeontol Sect, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Free Univ Berlin, Inst Geol Sci, Palaeontol Sect, Malteserstr 74-100,Bldg D, D-12249 Berlin, Germany.	mprauss@zedat.fu-berlin.de			Deutsche Forschungsgemeinschaft, DFG [KE 322/39-1]	Deutsche Forschungsgemeinschaft, DFG(German Research Foundation (DFG))	Sample material was provided by Wolfgang Kuhnt, University Kiel, Germany. Two anonymous reviewers provided constructive comments and suggestions and David Batten competently edited the manuscript. The project has been supported by a research grant from the Deutsche Forschungsgemeinschaft, DFG, grant number KE 322/39-1.	[Anonymous], 1985, SPOROPOLLENIN DINOFL; Chen Y.Y., 1988, CANADIAN TECHNICAL R, V103, P40; Cole J.M., 1991, NEOGENE QUATERNARY D, P181; Gebhardt H, 2010, MAR MICROPALEONTOL, V77, P25, DOI 10.1016/j.marmicro.2010.07.002; He C., 1984, Memoirs of Nanjing Institute of Geology and Palaeontology, P143; Jain KP., 1977, PALEOBOTANIST, V24, P170; Jamieson R., 2010, 3 INT PAL C IPC3; Kolonic S, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2003PA000950; Prauss ML, 2012, CRETACEOUS RES, V37, P246, DOI 10.1016/j.cretres.2012.04.007; Prauss ML, 2012, CRETACEOUS RES, V34, P233, DOI 10.1016/j.cretres.2011.11.004; Prauss ML, 2006, CRETACEOUS RES, V27, P872, DOI 10.1016/j.cretres.2006.04.004; SCHLANGER S O, 1976, Geologie en Mijnbouw, V55, P179; Schlanger S.O., 1987, Geological Society, London, Special Publications, V26, P371, DOI [10.1144/GSL.SP.1987.026.01.24, DOI 10.1144/GSL.SP.1987.026.01.24]; Zavattieri AM, 2006, PALAEONTOLOGY, V49, P1185, DOI 10.1111/j.1475-4983.2006.00596.x	14	14	14	1	7	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	OCT	2012	37						285	290		10.1016/j.cretres.2012.04.011	http://dx.doi.org/10.1016/j.cretres.2012.04.011			6	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	970VG					2025-03-11	WOS:000306159800025
J	Mertens, KN; Price, AM; Pospelova, V				Mertens, Kenneth Neil; Price, Andrea Michelle; Pospelova, Vera			Determining the absolute abundance of dinoflagellate cysts in recent marine sediments II: Further tests of the <i>Lycopodium</i> marker-grain method	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cyst; concentration; Lycopodium clavatum tablets; spike; absolute abundance	ASSEMBLAGES; BASIN; BAY	Lycopodium clavatum tablets are commonly added as a spike to determine dinoflagellate cyst concentrations in sediments. In this study we investigate the effects of different processing techniques on dinoflagellate cyst concentrations using well-mixed sediment samples from Saanich Inlet, British Columbia, Canada. At the onset of any dinoflagellate cyst investigation, we suggest following the recommendations of Maher (1981) to experimentally adjust the sample size to obtain a ratio close to similar to 2 of dinoflagellate cysts counted to Lycopodium spores counted, in order to obtain reproducible concentrations. Results further show that both oven-drying at similar to 45 degrees C and freeze-drying are viable, non-destructive techniques yielding reproducible results. Use of warm HCl (40-60 degrees C) for a short time (30 min) is harmless, whereas treatment with warm HF (40-60 degrees C) affects the reproducibility of the concentrations. Pre-sieving can result in loss of cysts and/or spike but this can be easily monitored by checking the residue. Perforated metal sieves show more consistent results than the Nitex nylon meshes. The use of 30 second sonication does not affect the reproducibility, and is advised to remove amorphous organic matter. Adding the Lycopodium spike at the end of preparation yields consistently lower concentrations, which were usually not reproducible, suggesting noticeable losses of Lycopodium spores during processing if the Lycopodium spores are added at the beginning. This method can be considered a viable alternative, but the discrepancy should be taken into account. (C) 2012 Elsevier B.V. All rights reserved.	[Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Price, Andrea Michelle; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada	Ghent University; University of Victoria	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be; pricea@uvic.ca; vpospe@uvic.ca	Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015	Pospelova, Vera/0000-0003-4049-8133; Mertens, Kenneth/0000-0003-2005-9483; Price, Andrea/0000-0002-5359-053X	Natural Sciences and Engineering Research Council of Canada (NSERC)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We are grateful to Captain Brown, crew of the MSV Strickland, Ms. Sarah Thornton and EOS313-2009 students for the help with sediment sample collection. Ms. Alanna Krepakevitch is thanked for her help during subsampling and freeze-drying. Dr. Kenneth Mertens is a postdoctoral fellow of FWO Belgium. This research was partly conducted by Dr. Kenneth Mertens while working as a postdoctoral researcher at University of Victoria, Canada. This research was partly supported by the Natural Sciences and Engineering Research Council of Canada (NSERC) through a grant to Dr. V. Pospelova. The editor and two anonymous reviewers are thanked for comments that improved the manuscript.	BENNINGHOFF W. 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Palaeobot. Palynology	SEP 15	2012	184						74	81		10.1016/j.revpalbo.2012.06.012	http://dx.doi.org/10.1016/j.revpalbo.2012.06.012			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	015GD					2025-03-11	WOS:000309433500006
J	Thomsen, E; Abrahamsen, N; Heilmann-Clausen, C; King, C; Nielsen, OB				Thomsen, Erik; Abrahamsen, Niels; Heilmann-Clausen, Claus; King, Chris; Nielsen, Ole Bjorslev			Middle Eocene to earliest Oligocene development in the eastern North Sea Basin: Biostratigraphy, magnetostratigraphy and palaeoenvironment of the Kysing-4 borehole, Denmark	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						North Sea; Eocene; Oligocene; Calcareous nannofossils; Foraminifera; Dinoflagellates; Magnetostratigraphy; Orbital Milankovitch cycles	CALCAREOUS NANNOFOSSIL MAGNETOBIOCHRONOLOGY; CONTESSA HIGHWAY SECTION; ASTRONOMICAL CALIBRATION; DINOFLAGELLATE CYSTS; MAUD-RISE; CLIMATE; STRATIGRAPHY; MORPHOMETRY; GREENHOUSE; EVOLUTION	The cored 154.5 m deep Kysing-4 borehole in central Jutland is unique for high northern latitudes because it comprises an almost complete Middle Eocene to lowermost Oligocene succession mostly in a highly calcareous facies with abundant well preserved microfossils and from an upper bathyal environment. It has therefore been possible to carry out biostratigraphical analyses of calcareous nannofossils, benthic and planktonic foraminifera as well as dinoflagellate cysts. In order to correlate the section to the geomagnetic polarity time scale a detailed palaeomagnetic analysis has been performed. The magnetobiostratigraphic calibration allowed a well constrained identification of nearly all magnetochrons between Chron C21 n and Chron C13n. The Eocene deposits consist mostly of calcareous ooze (Sovind Marl Formation with three new members formally defined), whereas the Oligocene Viborg Formation consists of moderately calcareous mud. Overall, the lithology of the deposits is in agreement with previous interpretations of a British provenance for the Eocene deposits and a Scandinavian provenance for the Oligocene deposits. Cyclic shifts in the clay/carbonate content during the Middle Eocene (chrons C19-C17) are attributed to orbitally controlled climate shifts. Obliquity seems to have been the dominating factor, but intervals dominated by precession end eccentricity signals also occur. A 10 m thick hitherto unknown black mud (Moesgaard Member) of Scandinavian provenance and deposited very rapidly during the late Eocene Chron C16n.1n is interpreted as a precursor event to the Oligocene mode of sedimentation. Both the Moesgaard Member and the Lower Oligocene Viborg Formation are associated with sea-level falls. (C) 2012 Elsevier B.V. All rights reserved.	[Thomsen, Erik; Abrahamsen, Niels; Heilmann-Clausen, Claus; Nielsen, Ole Bjorslev] Univ Aarhus, Dept Geosci, DK-8000 Aarhus C, Denmark	Aarhus University	Thomsen, E (通讯作者)，Univ Aarhus, Dept Geosci, Bldg 1672, DK-8000 Aarhus C, Denmark.	erik.thomsen@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; Nielsen, Ole/O-1060-2013; Thomsen, Erik/A-4842-2012; Abrahamsen, Niels/A-3553-2012		Danish Natural Research Council [21-00-0256, 272-08-0256]	Danish Natural Research Council(Danish Natural Science Research Council)	The Kysing-4 research borehole was financed by the Cenmove Project, Grant number 21-00-0256 from the Danish Natural Research Council to Soren Bom Nielsen and received additional support from Danish Natural Research Council project 272-08-0256. We are grateful to Jesper Olsen, who carried out the spectral analysis of the magnetic susceptibility data and contributed considerably to the age model. Uffe Korsbaek gave us access to the gamma ray emission data. Kirsten Rosendal made the majority of the nannofossil and dinoflagellate cysts preparations. Parts of the palaeomagnetic measurements were made by Mette K. Christensen, Tom Hagensen, Christoffer Mouritzen and Claus Beyer. Soren Bo Andersen carefully corrected several drafts of the manuscript We are extremely indebted to careful reviews by Etienne Steurbaut, Noel Vandenberghe and one anonymous reviewer.	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SEP 15	2012	350						212	235		10.1016/j.palaeo.2012.06.034	http://dx.doi.org/10.1016/j.palaeo.2012.06.034			24	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	004MM					2025-03-11	WOS:000308685800017
J	Schnyder, J; Deconinck, JF; Baudin, F; Colombié, C; Du Chêne, RJ; Gardin, S; Galbrun, B; de Rafélis, M				Schnyder, Johann; Deconinck, Jean-Francois; Baudin, Francois; Colombie, Claude; Du Chene, Roger Jan; Gardin, Sylvia; Galbrun, Bruno; de Rafelis, Marc			Purbeck beds (Late Jurassic) in the Phare de Chassiron section (Ile d'Oleron, NW Aquitaine Basin, France): Refined age-assignment and long-term depositional sequences	GEOBIOS			English	Article						Purbeck beds; Dinoflagellate; Nannofossils; Magnetostratigraphy; Aquitaine Basin; Late Jurassic	CRETACEOUS PLATFORM CARBONATES; SHALLOW-MARINE CARBONATES; DEEP-SEA CARBONATES; CLAY MINERALOGY; SOUTHERN ENGLAND; TRACE-ELEMENTS; SW FRANCE; DORSET; BOUNDARY; SEDIMENTOLOGY	In western european basins, lowering of relative sea-level during the Late Jurassic-Early Cretaceous led to the widespread deposition in numerous basins of so-called Purbeck facies. Age-assignment and long-distance correlations are difficult to establish in such shallow marine to continental deposits, where ammonites are generally lacking. This paper aims to present new biostratigraphical and sedimentological data from the Phare de Chassiron section. located at the western part of the Aquitaine Basin (SW France), where Purbeck beds crop out. Marine bands, interfingered within the Purbeck beds, allow refining the age-assignment of these beds using dinoflagellate cysts, calcareous nannofossils and magnetostratigraphy. Most of the Purbeck beds appear to have a Tithonian age. Uppermost beds of the section, although not precisely dated, are not younger than the Early Berriasian. Field sedimentology, palynofacies and trace-element data (strontium) on carbonates, allow depositional environments to be characterized and a sequence-stratigraphy scheme to be established. This section provides an unique, continuous record, within the Aquitaine Basin, of the final exposure, during the Tithonian, of the former Late Kimmeridgian open-marine platform. The Phare de Chassiron may be considered as one of the most important exposures of Purbeck facies of Tithonian age in Europe. (c) 2012 Published by Elsevier Masson SAS.	[Schnyder, Johann; Baudin, Francois; Galbrun, Bruno; de Rafelis, Marc] Univ Paris 06, CNRS, iSTeP, UMR 7193, F-75252 Paris 05, France; [Deconinck, Jean-Francois] Univ Bourgogne, CNRS, UMR Biogeosci 5561, F-21000 Dijon, France; [Colombie, Claude] Univ Lyon 1, CNRS, Lab Geol Lyon, UMR 5276, F-69622 Villeurbanne, France; [Gardin, Sylvia] Univ Paris 06, CNRS, UMR 7207, Ctr Rech Paleobiodiversite & Paleoenvironm, F-75252 Paris 05, France	Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); Universite de Bourgogne; Ecole Normale Superieure de Lyon (ENS de LYON); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite	Schnyder, J (通讯作者)，Univ Paris 06, CNRS, iSTeP, UMR 7193, Case 117,4 Pl Jussieu, F-75252 Paris 05, France.	johann.schnyder@upmc.fr	Colombié, Claude/C-8371-2012; 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J	Persson, A; Smith, BC; Alix, JH; Senft-Batoh, C; Wikfors, GH				Persson, Agneta; Smith, Barry C.; Alix, Jennifer H.; Senft-Batoh, Christina; Wikfors, Gary H.			Toxin content differs between life stages of <i>Alexandrium fundyense</i> (Dinophyceae)	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Bloom; Dinoflagellate; Gamete; Mating; Pellicle cyst; PST; Toxin; Zygote	SAXITOXIN PRODUCTION; MOLECULAR-CLONING; C2 TOXIN; DINOFLAGELLATE; NA+; TAMARENSE; ATPASE; ACCUMULATION; DYNAMICS; KINETICS	Different life stages of two mating-compatible clones of the paralytic shellfish toxin (PST)-producing dinoflagellate Alexandrium fundyense Balech were separated using a combination of techniques; culturing and sampling methods were used to separate vegetative cells and gametes, and sorting flow cytometry was used to separate zygotes. PST profiles were significantly different between life stages; the two gonyautoxins GTX1 and 2 were present in vegetative and senescent cells, but disappeared from gametes and zygotes. Toxin-profile changes were shown to occur very quickly in both strains when pellicle cyst formation was induced by shaking (four minutes) followed by rinsing on a screen. These pellicle cysts produced from exponentially-growing, vegetative cells lost GTX1 and 2 completely. Rapid toxin epimerization of GTX1 to GTX4 and GTX2 to GTX3 is one possible explanation, although the biological advantage of this remains unclear. Another possible explanation is that during the mating phase of a bloom or when cells are disturbed, GTX1 and GTX2 are released into the surrounding water. It may be advantageous for a dinoflagellate bloom to be surrounded by free toxins in the water. (c) 2012 Elsevier B.V. All rights reserved.	[Persson, Agneta] Univ Gothenburg, Dept Biol & Environm Sci, SE-40530 Gothenburg, Sweden; [Smith, Barry C.; Alix, Jennifer H.; Wikfors, Gary H.] Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA; [Senft-Batoh, Christina] Univ Connecticut, Dept Marine Sci, Groton, CT 06340 USA	University of Gothenburg; National Oceanic Atmospheric Admin (NOAA) - USA; University of Connecticut	Persson, A (通讯作者)，Smedjebacksvagen 13, SE-77190 Ludvika, Sweden.	agnetapersson77@gmail.com		Persson, Agneta/0000-0003-0202-6514; Batoh, Christina/0009-0007-5526-1485	Magnus Bergvall's Foundation; Oscar and Lili Lamm's Foundation; Adlerbert Foundation; NOAA Aquaculture Program and the Northeast Fisheries Science Center	Magnus Bergvall's Foundation; Oscar and Lili Lamm's Foundation; Adlerbert Foundation; NOAA Aquaculture Program and the Northeast Fisheries Science Center(National Oceanic Atmospheric Admin (NOAA) - USA)	Funding for this project was provided by Magnus Bergvall's Foundation, Oscar and Lili Lamm's Foundation, the Adlerbert Foundation, and by the NOAA Aquaculture Program and the Northeast Fisheries Science Center.[SS]	ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; 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WALKER LM, 1979, J PHYCOL, V15, P312; Wang DZ, 2008, MAR DRUGS, V6, P349, DOI 10.3390/md20080016; Wang DZ, 2002, J APPL PHYCOL, V14, P461, DOI 10.1023/A:1022326103191; Wang DZ, 2001, TOXICON, V39, P1533, DOI 10.1016/S0041-0101(01)00125-8; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	50	11	12	2	33	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	SEP	2012	19						101	107		10.1016/j.hal.2012.06.006	http://dx.doi.org/10.1016/j.hal.2012.06.006			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	009NY					2025-03-11	WOS:000309033700013
J	Nagai, S; Itakura, S				Nagai, Satoshi; Itakura, Shigeru			Specific detection of the toxic dinoflagellates <i>Alexandrium tamarense</i> and <i>Alexandrium catenella</i> from single vegetative cells by a loop-mediated isothermal amplification method	MARINE GENOMICS			English	Article						Alexandrium tamarense; Alexandrium catenella; Loop-mediated isothermal amplification; Molecular detection; Plankton monitoring; Paralytic shellfish poisoning	SP-NOV DINOPHYCEAE; SETO INLAND SEA; MICROSATELLITE MARKERS; LABORATORY CONDITIONS; PCR ASSAY; IDENTIFICATION; JAPANESE; ENCYSTMENT; WATERS; CYSTS	In this study, we succeeded in developing a loop-mediated isothermal amplification (LAMP) method that enables sensitive and specific detection of the toxic marine dinoflagellates Alexandrium tamarense and Alexandrium catenella from single cells of both laboratory cultures and naturally blooming cells within 25 min, by monitoring the turbidimeter from the start of the LAMP reaction. The fluorescence intensity was strong enough to allow discrimination between positive and negative results by naked eye under a UV lamp, even in amplified samples from a single cell, by using the LAMP method. Unambiguous detection by naked eye was possible even in half the volume of LAMP cocktail recommended by the manufacturer, suggesting the potential to significantly reduce the cost of Alexandrium monitoring. Therefore, we can conclude that this method is one of the most convenient, sensitive, and cost-effective molecular tools for Alexandrium monitoring. (C) 2012 Elsevier B.V. All rights reserved.	[Nagai, Satoshi; Itakura, Shigeru] Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan	Japan Fisheries Research & Education Agency (FRA)	Nagai, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Maruishi 2-17-5, Hiroshima 7390452, Japan.	snagai@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063	Fisheries Research Agency of Japan	Fisheries Research Agency of Japan	I would like to thank Dr. S. Yoshimatsu, Kagawa Prefecture Fisheries Research Institute, for providing clonal strains of A. affine and A. pseudogoniaulax. I also would like to express my gratitude to Dr. T. Kamiyama, National Research Institute of Fisheries and Environment of Inland Sea, Fisheries Research Agency of Japan, for his useful suggestions and encouragement during this study. This work was supported by a grant from the Fisheries Research Agency of Japan.	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Genom.	SEP	2012	7				SI		43	49		10.1016/j.margen.2012.03.001	http://dx.doi.org/10.1016/j.margen.2012.03.001			7	Genetics & Heredity; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Genetics & Heredity; Marine & Freshwater Biology	003NB	22897962				2025-03-11	WOS:000308617400009
J	Bogus, K; Harding, IC; King, A; Charles, AJ; Zonneveld, KAF; Versteegh, GJM				Bogus, Kara; Harding, Ian C.; King, Adrian; Charles, Adam J.; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.			The composition and diversity of dinosporin in species of the <i>Apectodinium</i> complex (Dinoflagellata)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinosporin; dinoflagellate; Apectodinium; cyst wall; biomacromolecule; FTIR	EOCENE THERMAL MAXIMUM; CYST-THECA RELATIONSHIP; CHEMICAL-STRUCTURE; FTIR SPECTROSCOPY; ORGANIC-MATTER; CELL-WALL; TEMPERATURE; MACROMOLECULES; SALINITY; ORIGIN	Organic-walled dinoflagellate cysts, produced as a result of sexual reproduction, are important tools for studies on recent and past environments. Additionally, the organic-walled cysts can be used as proxies for understanding the composition and chemical transformations of marine kerogen, the largest global organic carbon pool. However, any usage of dinoflagellate cysts in this manner is predicated on an understanding of the composition and transformations of this potential proxy. Dinoflagellate cyst walls are composed of "dinosporin", a refractory biomacromolecule that probably represents a suite of chemically distinct biopolymers. In order to investigate both the nature of dinosporin and the extent to which the composition of this biomacromolecule may differ between dinoflagellate cyst taxa, we analyzed cyst species from the genus Apectodinium. The species defined within this genus are visually similar with several seeming to represent end-members along a continuum of morphological variation. Micro-Fourier transform infrared (FTIR) analysis was performed on three of these morphospecies (identified visually as A. paniculatum, A. parvum and A. augustum) from two regionally distinct samples. The analyses showed consistent patterns with clear differences between the species. The dinosporin of A. paniculatum closely resembles cellulose and is rich in ether bonds (C - O), while the dinosporin of A. augustum contains more carboxyl (COOH) groups. A. parvum appears intermediate in many respects, despite representing an end-member in terms of morphology. These differences are consistent regardless of the regional setting or post-depositional conditions, and strongly suggest that the original cyst wall composition of the species differed when the cysts were formed. These data are the first to clearly show differences in cyst wall composition between species of the same genus and indicate that the chemical diversity of dinosporins is greater than previously thought. (C) 2012 Elsevier B.V. All rights reserved.	[Bogus, Kara; Zonneveld, Karin A. F.] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Bogus, Kara; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.] Marum Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Harding, Ian C.; King, Adrian; Charles, Adam J.] Univ Southampton, Sch Ocean & Earth Sci, Natl Oceanog Ctr Southampton, Southampton SO14 3ZH, Hants, England	University of Bremen; University of Bremen; University of Southampton; NERC National Oceanography Centre	Bogus, K (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28334 Bremen, Germany.	ka_bo@uni-bremen.de	Harding, Ian/K-3320-2012; Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776; Bogus, Kara/0000-0003-4690-0576; Harding, Ian/0000-0003-4281-0581	DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth History" (EUROPROX); DFG [VE-486/2, VE-486/3]; NERC; NERC CASE [NE/F006721/1]; Shell UK	DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth History" (EUROPROX)(German Research Foundation (DFG)); DFG(German Research Foundation (DFG)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC CASE(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Shell UK	S. Akbari is thanked for laboratory assistance and we also appreciate the technical assistance of R. Williams regarding the FTIR analysis. This manuscript benefited from the constructive comments of two anonymous reviewers and the editor (M. H. Stephenson). Financial support for KB and KAFZ was provided by the DFG (Deutsche Forschungsgemeinschaft) as part of the European Graduate College "Proxies in Earth History" (EUROPROX), and by the DFG to GJMV in the framework of a Heisenberg grant (VE-486/2 and /3). Financial support for AK was kindly provided by a NERC PhD studentship and for AJC by a NERC CASE PhD studentship (NE/F006721/1), in conjunction with Shell UK.	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Palaeobot. Palynology	SEP 1	2012	183						21	31		10.1016/j.revpalbo.2012.07.001	http://dx.doi.org/10.1016/j.revpalbo.2012.07.001			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	013IC					2025-03-11	WOS:000309298100003
J	Su-Myat; Maung-Saw-Htoo-Thaw; Matsuoka, K; Khin-Ko-Lay; Koike, K				Su-Myat; Maung-Saw-Htoo-Thaw; Matsuoka, Kazumi; Khin-Ko-Lay; Koike, Kazuhiko			Phytoplankton surveys off the southern Myanmar coast of the Andaman Sea: an emphasis on dinoflagellates including potentially harmful species	FISHERIES SCIENCE			English	Article						Alexandrium; Andaman Sea; Cyst; Dinoflagellate; Dinophysis; Harmful algal bloom; Mergui Archipelago; Myanmar	DIARRHETIC SHELLFISH TOXINS; DINOPHYSIS-CAUDATA; PERNA-VIRIDIS; ALGAL BLOOMS; CYSTS; BAY; SEDIMENTS	A detailed list of dinoflagellate species for the Mergui Archipelago, off southern Myanmar, was compiled for the first time. This was based on surveys conducted in two seasons in pre- and post-monsoons, and on observations for both plankton and cyst assemblages. In the plankton samples, 57 and 26 dinoflagellate species were recorded, respectively, in the pre- and post-monsoons. Among the list from plankton and cyst samples, harmful species were found: red-tide species including Prorocentrum spp. and Alexandrium affine, and causative species of paralytic shellfish poisoning, e.g., Alexandrium tamiyavanichii and Gymnodinium catenatum, and of diarrhetic shellfish poisoning, e.g., Dinophysis spp. Therefore, although no incidences have been reported yet, attention must be paid to these harmful algal bloom (HAB) events in Myanmar where exploitation of fishery resources is drastically increasing. Other dinoflagellate compositions were also unique and may relate to the oceanographic system in this region. In the pre-monsoon, rather rare oceanic species of Ornithocercus spp. were found concurrently with neritic species, probably due to the extensive southwesterly current from the Indian Ocean. Throughout the seasons, diverse species of Protoperidinium were predominately recorded in both planktonic and sediment samples, indicating richness of prey organisms probably sustained by upwelling systems.	[Koike, Kazuhiko] Hiroshima Univ, Grad Sch Biosphere Sci, Lab Marine Ecosyst Dynam, Higashihiroshima 7398528, Japan; [Su-Myat; Maung-Saw-Htoo-Thaw; Koike, Kazuhiko] Hiroshima Univ, Grad Sch Biosphere Sci, Hiroshima, Japan; [Matsuoka, Kazumi] Nagasaki Univ, Grad Sch Fisheries Sci & Environm Studies, Inst E China Sea Res, Nagasaki 852, Japan; [Khin-Ko-Lay] Minist Livestock & Fisheries, Dept Fisheries, Yangon, Myanmar	Hiroshima University; Hiroshima University; Nagasaki University	Koike, K (通讯作者)，Hiroshima Univ, Grad Sch Biosphere Sci, Lab Marine Ecosyst Dynam, Kagamiyama 1-4-4, Higashihiroshima 7398528, Japan.	kazkoike@hiroshima-u.ac.jp	Koike, Kazuhiko/A-3392-2019	Kazuhiko, Koike/0000-0001-5380-5839	Ministry of Education, Culture, Sports, Science, and Technology, Japan; Graduate School of Biosphere Science, Hiroshima University	Ministry of Education, Culture, Sports, Science, and Technology, Japan(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); Graduate School of Biosphere Science, Hiroshima University	S.M. was supported by the Ministry of Education, Culture, Sports, Science, and Technology, Japan. This work was partly supported by the 2010 Grant-in-Aid from the Dean of the Graduate School of Biosphere Science, Hiroshima University. We would like to thank U Myint Phay (DOF, Yangon) and Professor Dr. Swe Thwin (governmental adviser, Myanmar) for their guidance on sampling locations. We are also grateful to all members of DOF (Myeik) for their assistance with sampling. We wish to thank Dr. Vera Pospelova and Manuel Bringue (University of Victoria, Canada), for teaching us map construction, and also to Dr. Gerald Darnis (Universite Laval, Quebec, Canada) and Dr. Ryosuke Makabe (Hiroshima University), for teaching dendrogram construction. We are indebted to Dr. Kenneth Neil Mertens (Ghent University, Belgium) for providing taxonomic literature.	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Sci.	SEP	2012	78	5					1091	1106		10.1007/s12562-012-0534-0	http://dx.doi.org/10.1007/s12562-012-0534-0			16	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	002SD					2025-03-11	WOS:000308553900015
J	Al-Ameri, TK; Zumberge, J				Al-Ameri, Thamer K.; Zumberge, John			Middle and Upper Jurassic hydrocarbon potential of the Zagross Fold Belt, North Iraq	MARINE AND PETROLEUM GEOLOGY			English	Article						North Iraq; Palynomorphs; Hydrocarbon generation; Oil biomarkers; Jurassic-Lower Cretaceous source rocks; Cretaceous-Tertiary reservoir rocks	KEROGENS	Structured organic matters of the Palynomorphs of mainly dinoflagellate cysts are used in this study for dating the limestone, black shale, and marl of the Middle Jurassic (Bajocian-Bathonian) Sargelu Formation, Upper Jurassic (Upper Callovian - Lower Oxfordian) Naokelekan Formation, Upper Jurassic (Kimeridgian and Oxfordian) Gotnia and Barsarine Formations, and Upper Jurassic - Lower Cretaceous (Tithonian-Beriassian) Chia Gara source rock Formations while spore species of Cyathidites australis and Glechenidites senonicus are used for maturation assessments of this succession. Materials' used for this palynological study are 320 core and cutting samples of twelve oil wells and three outcrops in North Iraq. Terpane and sterane biomarker distributions, as well as stable isotope values, were determined for oils potential source rock extracts of Jurassic-Lower Cretaceous strata to determine valid oil-to-source rock correlations in North Iraq. Two subfamily carbonate oil types-one of Middle Jurassic age (Sargelu) carbonate rock and the other of mixed Upper Jurassic/Cretaceous age (Chia Gara) with Sargelu sources as well as a different oil family related to Triassic marls, were identified based on multivariate statistical analysis (HCA & PCA). Middle Jurassic subfamily A oils from Demir Dagh oil field correlate well with rich, marginally mature, Sargelu source rocks in well Mk-2 near the city of Baiji. In contrast, subfamily B oils have a greater proportion of C-28/C-29 steranes, indicating they were generated from Upper Jurassic/Lower Cretaceous carbonates such as those at Gillabat oil field north of Mansuriyah Lake. Oils from Gillabat field thus indicate a lower degree of correlation with the Sargelu source rocks than do oils from Demir Dagh field. Palynofacies assessments are performed for this studied succession by ternary kerogen plots of the phytoclast, amorphous organic matters, and palynomorphs. From the diagram of these plots and maturation analysis, it could be assessed that the formations of Chia Gara and Sargelu are both deposited in distal suboxic to anoxic basin and can be correlated with kerogens classified microscopically as Type A and Type B and chemically as Type II. The organic matter, comprised principally of brazinophyte algae, dinoflagellate cysts, spores, pollen, foraminifera test linings, and phytoclasts in all these formations and hence affected with upwelling current. These deposit contain up to 18 wt% total organic matters that are capable to generate hydrocarbons within mature stage of thermal alteration index (TAI) range in Stalplin's scale (Staplin, 1969) of 2.7-3.0 for the Chia Gara Formation and 2.9-3.1 for the Sargelu Formation. Case study examples of these oil prone strata are: one 7-m (23-ft) thick section of the Sargelu Formation averages 44.2 mg HC/g S2 and 439 degrees C Tmax (Rock-Eval pyrolysis analyses) and 16 wt% TOC especially in well Mk-2 whereas, one 8-m (26-ft) thick section of the Chia Gara and 1-m (3-ft) section of Naokelekan Formations average 44.5 mg HC/g S2 and 440 degrees C Tmax and 14 wt% TOC especially in well Aj-8. One-dimension, petroleum system models of key wells using IES PetroMod Software can confirm their oil generation capability. These hydrocarbon type accumulation sites are illustrated in structural cross sections and maps in North Iraq. (c) 2012 Elsevier Ltd. All rights reserved.	[Al-Ameri, Thamer K.] Univ Baghdad, Coll Sci, Dept Geol, Jadiriyah, Iraq; [Zumberge, John] GeoMark Res Ltd, Houston, TX 77095 USA	University of Baghdad	Al-Ameri, TK (通讯作者)，Univ Baghdad, Coll Sci, Dept Geol, Jadiriyah, Iraq.	thamer_alameri@yahoo.com						Al-Ameri TK, 2011, J PETROL GEOL, V34, P199, DOI 10.1111/j.1747-5457.2011.00501.x; Al-Ameri TK, 2011, MAR PETROL GEOL, V28, P880, DOI 10.1016/j.marpetgeo.2010.06.003; Al-Ameri TK, 2009, GEOARABIA, V14, P91; Al-Ameri TK, 1992, IRAQ J SCI, V36, P672; Al-Juboury AI, 2008, GEOARABIA, V13, P141; Al-Qayim B, 2010, GEOARABIA, V15, P49; Al-Sharhan AS, 1997, SEDIMENTRAY BASINS P; AlGailani M, 1996, OIL GAS J, V94, P108; Aqrawi A., 2010, The Petroleum Geology of Iraq; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: Principles and Applications, P1065; BUDAY T., 1980, The regional geology of Iraq: stratigraphy and paleogeography; Cross A.T., 1966, MAR GEOL, V4, P467, DOI [10.1016/0025-3227(66)90012-0, DOI 10.1016/0025-3227(66)90012-0]; Dunnington H.V., 1958, HABITAT OIL AAPG S, P1194, DOI DOI 10.1306/SV18350C49; Durand B., 1980, KEROGEN INSOLUBLE OR, P35; Espetalie J, 1977, REV I 3, V41, P75; GRANTHAM PJ, 1988, ORG GEOCHEM, V12, P61, DOI 10.1016/0146-6380(88)90115-5; Hall S.H., 2001, GEOARABIA SPECIAL PU, V2; Hunt J.M., 1996, PETROLEUM GEOLOGY GE; Integrated Exploration System (IES), 2007, PETROMOD PETR SYST M; Kent WN, 2010, GEOARABIA, V15, P147; Lewan MD, 2002, ORG GEOCHEM, V33, P1457, DOI 10.1016/S0146-6380(02)00182-1; MELIA MB, 1984, MAR GEOL, V58, P345, DOI 10.1016/0025-3227(84)90208-1; Peters K.E., 2005, The Biomarker Guide: Biomarkers and isotopes in petroleum exploration and earth history, V2; Pitman J.K., 2004, GeoArabia, V9, P41, DOI [10.2113/geoarabia090441, DOI 10.2113/GEOARABIA090441]; Pollastro R.M., 1999, 97470B US GEOL SURV, DOI 10.3133/ofr97470B; Powell A.J., 1992, PALYNOLOGICAL EXPRES, V64, P215, DOI [10.1144/GSL.SP.1992.064.01.14, DOI 10.1144/GSL.SP.1992.064.01.14]; RAHMAN M, 1995, J PETROL GEOL, V18, P91, DOI 10.1111/j.1747-5457.1995.tb00743.x; SOFER Z, 1984, AAPG BULL, V68, P31; 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; SWEENEY JJ, 1990, AAPG BULL, V74, P1559; THOMPSON CL, 1986, INT J COAL GEOL, V6, P229, DOI 10.1016/0166-5162(86)90003-0; Tyson R.V, 1995, Sedimentary Organic Matter: Organic Facies and Palynofacies, P1, DOI DOI 10.1007/978-94-011-0739-625; Tyson R.V., 1993, Applied Micropalaeontology, P153, DOI [10.1007/978-94-017-0763-35, DOI 10.1007/978-94-017-0763-35]; van Bellen, 1959, LEXIQUE STRATIGRAPHQ, VIII; Welte D.H., 1984, PETROLEUM FORMATION; Zumberge JE, 2005, AAPG BULL, V89, P1347, DOI 10.1306/05100504003	38	49	53	1	27	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0264-8172	1873-4073		MAR PETROL GEOL	Mar. Pet. Geol.	SEP	2012	36	1					13	34		10.1016/j.marpetgeo.2012.04.004	http://dx.doi.org/10.1016/j.marpetgeo.2012.04.004			22	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	991HK					2025-03-11	WOS:000307691900002
J	Agrawal, SC				Agrawal, S. C.			Factors controlling induction of reproduction in algae-review: the text	FOLIA MICROBIOLOGICA			English	Article							BLUE-GREEN-ALGAE; DINOFLAGELLATE HETEROCAPSA-CIRCULARISQUAMA; CHLOROCOCCUM-ECHINOZYGOTUM CHLOROPHYCEAE; SUCCESSFUL EXTERNAL FERTILIZATION; PSEUDO-NITZSCHIA-MULTISERIES; APHANIZOMENON-FLOS-AQUAE; OYSTER CRASSOSTREA-GIGAS; TEMPORARY CYST FORMATION; DRIED VEGETATIVE CELLS; LIFE-CYCLE STRATEGIES	This review surveys on the influence of different environmental factors like light (intensity, quality, photoperiod), temperature, season, nutrients (inorganic, organic), biotic factors (algal extracellular products, bacterial association, animals grazing), osmotic stress, pH of the medium, wave motion and mechanical shock, pollution, and radiations (UV, X-rays, gamma radiation) on the induction (or inhibition) of algal reproduction like cell division in unicellular algae, and formation of zoospores, aplanospores, akinetes, cysts, antheridia, oogonia, zygospores, etc.	Univ Allahabad, Dept Bot, Allahabad 211002, Uttar Pradesh, India	University of Allahabad	Agrawal, SC (通讯作者)，Univ Allahabad, Dept Bot, Allahabad 211002, Uttar Pradesh, India.	20.satish@gmail.com						ABDELRAHMAN MH, 1982, PHYSIOL VEG, V20, P155; Adachi M, 1999, MAR ECOL PROG SER, V191, P175, DOI 10.3354/meps191175; Adams DG, 1999, NEW PHYTOL, V144, P3, DOI 10.1046/j.1469-8137.1999.00505.x; AGRAWAL S C, 1983, Microbios Letters, V24, P27; Agrawal S. 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SEP	2012	57	5					387	407		10.1007/s12223-012-0147-0	http://dx.doi.org/10.1007/s12223-012-0147-0			21	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	988RW	22544815				2025-03-11	WOS:000307509300002
J	Nagai, S; Yamamoto, K; Hata, N; Itakura, S				Nagai, Satoshi; Yamamoto, Keigo; Hata, Naotugu; Itakura, Shigeru			Study of DNA extraction methods for use in loop-mediated isothermal amplification detection of single resting cysts in the toxic dinoflagellates <i>Alexandrium tamarense</i> and <i>A. catenella</i>	MARINE GENOMICS			English	Article						Alexandrium tamarense; Alexandrium catenella; Chelex buffer; DNA extraction; Resting cyst; Loop-mediated isothermal amplification	SP-NOV DINOPHYCEAE; GONYAULAX-TAMARENSIS; ABUNDANCE; SEDIMENTS; EXCAVATA	In a previous study, we experienced instable amplification and a low amplification success in loop-mediated isothermal amplification (LAMP) reactions from naturally occurring vegetative cells or resting cysts of the toxic dinoflagellates Alexandrium tamarense and Alexandrium catenella. In this study, we examined 4 methods for extracting DNA from single resting cysts of A. tamarense and A. catenella to obtain more stable and better amplification success and to facilitate unambiguous detection using the LAMP method. Apart from comparing the 4 different DNA extraction methods, namely, (1) boiling in Tris-EDTA (TE) buffer, (2) heating at 65 degrees C in hexadecyltrimethylammonium bromide buffer, (3) boiling in 0.5% Chelex buffer, and (4) boiling in 5% Chelex buffer, we also examined the need for homogenization to crush the resting cysts before DNA extraction in each method. Homogenization of resting cysts was found to be essential for DNA extraction in all 4 methods. The detection time was significantly shorter in 5% Chelex buffer than in the other buffers and the amplification success was 100% (65/65), indicating the importance of DNA extraction and the effectiveness of 5% Chelex buffer in the Alexandrium LAMP. (C) 2012 Elsevier B.V. All rights reserved.	[Nagai, Satoshi; Itakura, Shigeru] Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; [Yamamoto, Keigo] Osaka Prefectural Govt, Res Inst Environm Agr & Fisheries, Marine Fisheries Res Ctr, Osaka 5990311, Japan; [Hata, Naotugu] Mie Prefectural Sci & Technol Promot Ctr, Shima, Mie 5170404, Japan	Japan Fisheries Research & Education Agency (FRA)	Nagai, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Maruishi 2-17-5, Hiroshima 7390452, Japan.	snagai@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063	Fisheries Research Agency of Japan	Fisheries Research Agency of Japan	The authors would like to express their gratitude to Dr. T. Kamiyama, National Research Institute of Fisheries and Environment of Inland Sea, Fisheries Research Agency of Japan, for his useful suggestions and encouragement during this study. This work was supported by a grant from the Fisheries Research Agency of Japan.	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Genom.	SEP	2012	7				SI		51	56		10.1016/j.margen.2012.03.002	http://dx.doi.org/10.1016/j.margen.2012.03.002			6	Genetics & Heredity; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Genetics & Heredity; Marine & Freshwater Biology	003NB	22897963				2025-03-11	WOS:000308617400010
J	Yi, S; Bahk, JJ; Jia, HJ; Yoo, DG				Yi, Sangheon; Bahk, Jang-Jun; Jia, Hongjuan; Yoo, Dong-Geun			Pliocene-Pleistocene boundary determination in hemipelagic sediment from the Ulleung Basin (East Sea, offshore Korea) inferred from terrigenous and marine palynofloras	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						pollen; dinocysts; Pliocene-Pleistocene boundary; Ulleung Basin; East Sea; offshore Korea	SEISMIC STRATIGRAPHY; DINOFLAGELLATE CYST; CONTINENTAL-MARGIN; NORTH PACIFIC; BIOSTRATIGRAPHY; QUATERNARY; JAPAN	Palynofloral analysis was performed for the first time on sediment from the Ulleung Basin (East Sea, offshore Korea) to locate the Pliocene-Pleistocene boundary, which is very important in determining the depositional age of a stratigraphic unit that contains methane hydrate. Cores from the drill sites Ulleung Basin Gas Hydrate 1-9 (UBGH1-9) and Ulleung Basin Gas Hydrate 1-10 (UBGH1-10) in the Ulleung Basin produced abundant to common pollen grains and organic-walled dinoflagellate cysts. Age-diagnostic palynomorphs were present in certain intervals: 120-175 mbsf at site UBGH1-9 and 170-205 mbsf at site UBGH1-10. The biostratigraphically meaningful taxa were the pollen genera Carya. Liquidambar, and Fagus and the dinoflagellate cysts Capillicysta fusca, Filisphaera filifera subsp. pilosa, and Selenopemphix quanta. The latest stratigraphic occurrence of these pollen taxa in northeast Asia is the late Pliocene, and that of the dinoflagellate cysts is regarded as the late Pliocene in all aquatic areas, especially in the Pacific. The last appearance datum (LAD) of the age indicators in the two cores studied suggests that the Pliocene-Pleistocene boundary is at 120 mbsf at site UBGH1-9 and 170 mbsf at site UBGH1-10. (C) 2012 Elsevier B.V. All rights reserved.	[Yi, Sangheon] Korea Inst Geosci & Mineral Resources, Div Geol Res, Taejon 305350, South Korea; [Bahk, Jang-Jun; Yoo, Dong-Geun] Korea Inst Geosci & Mineral Resources, Petr & Marine Res Div, Taejon 305350, South Korea; [Jia, Hongjuan] Shijiazhuang Univ Econ, Shijiazhuang, Peoples R China	Korea Institute of Geoscience & Mineral Resources (KIGAM); Korea Institute of Geoscience & Mineral Resources (KIGAM); Hebei GEO University	Yi, S (通讯作者)，Korea Inst Geosci & Mineral Resources, Div Geol Res, Gwahang No 124, Taejon 305350, South Korea.	shyi@kigam.re.kr	Yoo, Dong-Geun/AAV-2826-2021; Yi, Sangheon/D-4780-2011; Bahk, Jangjun/KRQ-7992-2024	Bahk, Jangjun/0000-0003-1480-7414	Ulleung Basin Gas Hydrate R&D Organization of the KIGAM; Ministry of Knowledge Economy of Korea	Ulleung Basin Gas Hydrate R&D Organization of the KIGAM; Ministry of Knowledge Economy of Korea(Ministry of Trade, Industry & Energy (MOTIE), Republic of Korea)	This research was supported by the Ulleung Basin Gas Hydrate R&D Organization of the KIGAM, funded by the Ministry of Knowledge Economy of Korea. We sincerely thank anonymous reviewers for their constructive comments and improvements on manuscript.	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Palaeobot. Palynology	AUG 1	2012	181						54	63		10.1016/j.revpalbo.2012.05.002	http://dx.doi.org/10.1016/j.revpalbo.2012.05.002			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	983PE					2025-03-11	WOS:000307130400006
J	Peyrot, D; Barroso-Barcenilla, F; Feist-Burkhardt, S				Peyrot, Daniel; Barroso-Barcenilla, Fernando; Feist-Burkhardt, Susanne			Palaeoenvironmental controls on late Cenomanian-early Turonian dinoflagellate cyst assemblages from Condemios (Central Spain)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Cenomanian-Turonian; Dinoflagellate cysts; OAE 2; delta C-13; delta O-18; TOC	SEA-LEVEL CHANGE; CRETACEOUS-TERTIARY BOUNDARY; SEDIMENTARY ORGANIC-MATTER; OCEANIC ANOXIC EVENTS; ORBITAL TIME-SCALE; MARINE-SEDIMENTS; SURFACE SEDIMENTS; WESTERN INTERIOR; NORTH; ATLANTIC	A detailed account of the organic-walled dinoflagellate cyst succession and geochemical data (delta C-13(org), delta C-13(carb), delta O-18, CaCO3 and Total Organic Carbon) from an outcrop section in Condemios (Province of Guadalajara, Central Spain) are presented and statistically correlated in order to identify the palaeoenvironmental conditions prevailing in this palaeogeographical area. The geochemical data revealed low TOC contents, and stable isotope values moderately (delta C-13(org).delta C-13(carb)) to strongly (delta O-18) affected by diagenesis. The low organic content 1 of the studied material, the diverse macropalaeontological fauna recovered and the absence of Cyclonephelium distinctum and prasinophytes in the palynological assemblages do not support the presence of anoxic conditions in this depositional setting. Two transgressive pulses centred in the upper part of the Spathites (Jeanrogericeras) subconciliatus Zone and in the Choffaticeras (Leoniceras) luciae Subzone are inferred by the presence of a high number of blade-shaped opaque phytoclasts and high diversity values in the corresponding palynofacies and dinoflagellate cyst assemblages, respectively. (C) 2012 Elsevier B.V. All rights reserved.	[Peyrot, Daniel; Barroso-Barcenilla, Fernando] Fac CC Geol, Inst Geol Econ, Dept Paleontol, Madrid 28040, Spain; [Barroso-Barcenilla, Fernando] Univ Alcala de Henares, Fac Ciencias, Grp Invest IBERCRETA, Dept Geol, Alcala De Henares 28871, Spain; [Feist-Burkhardt, Susanne] SFB Geol Consulting & Serv, D-64372 Ober Ramstadt, Germany	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE); Universidad de Alcala	Peyrot, D (通讯作者)，Fac CC Geol, Inst Geol Econ, Dept Paleontol, Jose Antonio Novais 2, Madrid 28040, Spain.	danip@geo.ucm.es	Feist-Burkhardt, Susanne/B-1522-2009; peyrot, Daniel/AAI-6091-2020; Barroso-Barcenilla, Fernando/M-5578-2014	Barroso-Barcenilla, Fernando/0000-0002-7938-7230; Feist-Burkhardt, Susanne/0000-0001-6019-6242; peyrot, Daniel/0000-0002-3897-6733	Junta de Castilla-La Mancha (Spain) [PEI111-02377926]; Ministerio de Educacion y Ciencia (Spain) [GR58/08-B (BSCH-UCM), CGL2005-01 765/BTE, CG12008-03112/BTE, CGL2009-12008, CGL2011-25894]; Basler Stiftung fur Biologische Forschung (Switzerland)	Junta de Castilla-La Mancha (Spain); Ministerio de Educacion y Ciencia (Spain)(Spanish Government); Basler Stiftung fur Biologische Forschung (Switzerland)	This article is part of a PhD project of the Universidad Complutense de Madrid (Spain), supported by the projects PEI111-02377926 of the Junta de Castilla-La Mancha (Spain) and GR58/08-B (BSCH-UCM), CGL2005-01 765/BTE, CG12008-03112/BTE, CGL2009-12008 and CGL2011-25894 of the Ministerio de Educacion y Ciencia (Spain) with contributions of the Basler Stiftung fur Biologische Forschung (Switzerland). Maria Jose Comas Rengifo, Eduardo Barron and Laura Domingo are thanked for their comments. Maria Lema (Universidade da Coruna) and Lora Wingate (University of Michigan) are thanked for their technical support. The authors are also grateful to Paul Dodsworth, Martin Pearce and Robert Fensome who gave insightful comments to an earlier version of this manuscript.	AGUILAR M.J., 1971, ESTUDIOS GEOL GICOS, V27, P497; [Anonymous], 1987, GEOLOGICAL SOC LONDO; [Anonymous], 1996, Palynology: principles and applications; Barroso-Barcenilla F, 2011, J IBER GEOL, V37, P9, DOI 10.5209/rev_JIGE.2011.v37.n1.1; Barroso-Barcenilla F, 2011, P GEOLOGIST ASSOC, V122, P67, DOI 10.1016/j.pgeola.2010.11.002; Barroso-Barcenilla F., 2006, THESIS U COMPLUTENSE; Barroso-Barcenilla F, 2009, NEWSL STRATIGR, V43, P139, DOI 10.1127/0078-0421/2009/0043-0139; Batten D.J., 1982, J. 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Palaeobot. Palynology	JUL 15	2012	180						25	40		10.1016/j.revpalbo.2012.04.008	http://dx.doi.org/10.1016/j.revpalbo.2012.04.008			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	983ZM					2025-03-11	WOS:000307157200003
J	Mantle, DJ; Riding, JB				Mantle, Daniel J.; Riding, James B.			Palynology of the Middle Jurassic (Bajocian-Bathonian) <i>Wanaea verrucosa</i> dinoflagellate cyst zone of the North West Shelf of Australia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						biostratigraphy; dinoflagellate cysts; Wanaea verrucosa Zone; Middle Jurassic (Bajocian-Bathonian); North West Shelf; Australia	BAYU-UNDAN FIELD; SEQUENCE STRATIGRAPHY; STRATA; BASIN; ASSEMBLAGES; PALEOENVIRONMENTS; NORMANDY; AREA	Marine and terrestrial palynomorphs from the Middle Jurassic Wanaea verrucosa dinoflagellate cyst zone are documented from subsurface sections of the North West Shelf of Australia. Selected intervals in the Perseus-3A, Sunrise-2 and Sunset West-1 wells were studied in detail and record evidence of brackish to shallow marine successions in the Northern Carnarvon and Bonaparte basins. The palynological data derived from these three wells constitute the basis for the formal definition of this important dinoflagellate cyst biozone and its three constituent subzones. The base of the Lower W verrucosa Subzone is defined by the first appearance of the index species and is a relatively sparse, low diversity microphytoplankton assemblage; species richness increases up-section. The base of the succeeding Middle W verrucosa Subzone is defined by the range base of Valvaeodinium spinosum, and the Upper W. verrnucosa Subzone is defined by the incoming of the large and distinctive species Endoscrinium kempiae. Two new species, Meiourogonyaulax straussii sp. nov. and Valvaeodinium cookii sp. nov. are described and Jansonia scarffei is reattributed as Fostericysta scarffei (Tykoezinski et al. 2001) comb. nov. Taxa with epicystal and multiplate precingular archaeopyles are prominent, particularly in the Lower W. verrucosa Subzone; this represents the coeval evolutionary explosion of the gonyaulacacean dinoflagellate cysts observed in the latest Early to Late Bajocian of Europe. Further cosmopolitan dinoflagellate cyst occurrences are compared with European ranges to assign a Late Bajocian to Early Bathonian age to the W verrucosa Zone. The associated spore-pollen assemblages are transitional from the upper Dictyotosporites complex to the lower Contignisporites cooksoniae zones. The latter zone is defined by the first appearance of the index species, but considerable care is required to separate this species from the many intermediate forms of Striatella-Contignisporites that occur through this interval. The palynofloras are dominated by araucariacean monosaccates (particularly Callialas-porites spp.), corystosperm bisaccates (mostly Alisporites spp.) and moderately diverse bryophyte-lycophyte-pteridophyte spore assemblages. Crown Copyright (C) 2012 Published by Elsevier B.V. All rights reserved.	[Mantle, Daniel J.] Geosci Australia, Canberra, ACT 2601, Australia; [Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	Geoscience Australia; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Mantle, DJ (通讯作者)，Geosci Australia, GPO Box 378, Canberra, ACT 2601, Australia.	daniel.mantle@ga.gov.au			NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Aboul Ela N.M., 1988, ACTA PALAEONTOLOGICA, V33, P345; Aboul Ela N.M., 1990, EARTH SCI SER, V4, P95; Aboul Ela N.M., 1997, ACTA U CAROLINAE GEO, V41, P47; Aboul Ela NM., 1988, NUEUES JB GEOLOGIE P, V1988, P263; Ager D.V., 1975, P NO N SEA S NOR PET, V5, P1; Ainsworth B.R., 1998, GIANT GAS FIELD N W, P23; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], 1980, MEM MUS NAT HIST NAT; [Anonymous], LAB PALAEOBOTANY PAL; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V206, P1; Boulter M., 1993, Special Papers in Palaeontology, V49, P125; Bujak J.P., 1977, Developments in Palaeontology and Stratigraphy, V6, P321; Callomon John H., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P61; Cookson I.E., 1960, PALAEONTOLOGY, V2, P243; Cranwell, 1964, ANCIENT PACIFIC FLOR, P49; Davey R.J., 1980, INFERIOR OOLITE BAJO, V79, P6; Deflandre G., 1938, TRAVAUX STATION ZOOL, V13, P147; DODEKOVA L, 1990, Geologica Balcanica, V20, P3; El Beialy SY., 2002, EGYPTIAN J PALEONTOL, V2, P371; El Shamma A.A., 2001, J GEOL, V45, P567; Enay R, 1980, EXTRAIT LIVRE JUBILA, V10, P261; Erkmen U., 1980, GEOBIOS-LYON, V13, P45; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Feist-Burkhardt S, 2001, NEUES JAHRB GEOL P-A, V219, P33, DOI 10.1127/njgpa/219/2001/33; Feist-Burkhardt S, 1997, B CENT RECH EXPL, V21, P31; Feist-Burkhardt Susanne, 1994, Revue de Paleobiologie, V13, P313; Feist-Burkhardt S, 2010, LETHAIA, V43, P10, DOI 10.1111/j.1502-3931.2009.00170.x; FEISTBURKHARDT S, 1990, B CENT RECH EXPL, V14, P611; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42, P909; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fenton J.P.G., 1980, Palaeontology (Oxford), V23, P151; Fenton J.P.G., 1978, Palinologia, P233; FENTON JPG, 1981, REV PALAEOBOT PALYNO, V31, P249; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; Foster C, 2001, MEMOIR ASS AUSTRALAS, V24, pi; Gedl Przemyslaw, 2008, Studia Geologica Polonica, V131, P7; Geleta S., 1998, TUBINGTER MIKROPALAO, V16; Gocht H., 1970, PALAEONTOGRAPHICA B, V129, P125; GOWLAND S., 1991, P YORKS GEOL SOC, V49, P375; Guy-Ohlson D., 1986, JURASSIC PALYNOLOGY; Guy-Ohlson D., 1989, Northwest European micropalaeontology and palynology, P70; HALLAM A, 1983, PALAEOGEOGR PALAEOCL, V43, P181, DOI 10.1016/0031-0182(83)90010-X; Harris AJ, 2003, MAR MICROPALEONTOL, V48, P127, DOI 10.1016/S0377-8398(03)00002-1; Helal AH, 1965, NEUES JB GEOLOGIE PA, V123, P160; Helby R., 2004, UPDATE JURASSIC EARL; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Helby Robin, 2001, Memoir of the Association of Australasian Palaeontologists, V24, P221; Ilyina V.I., 1991, DINOCYST ZONATION BA, P42; ILYINA VI, 1986, REV PALAEOBOT PALYNO, V48, P357, DOI 10.1016/0034-6667(86)90073-4; Iturralde-Vinent MA, 2006, INT GEOL REV, V48, P791, DOI 10.2747/0020-6814.48.9.791; JOHNSON C D, 1973, Bulletin of Canadian Petroleum Geology, V21, P178; Klement K. 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Palaeobot. Palynology	JUL 15	2012	180						41	78		10.1016/j.revpalbo.2012.03.005	http://dx.doi.org/10.1016/j.revpalbo.2012.03.005			38	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	983ZM		Green Accepted			2025-03-11	WOS:000307157200004
J	Aleksandrova, GN; Oreshkina, TV; Iakovleva, AI; Radionova, EP				Aleksandrova, G. N.; Oreshkina, T. V.; Iakovleva, A. I.; Radionova, E. P.			Late Paleocene-Early Eocene diatoms and dinocysts from biosiliceous facies of the middle Trans-Urals region	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Trans-Urals region; late Paleocene; early Eocene; biostratigraphic subdivision; diatoms; dinocysts	NORTH-SEA; DINOFLAGELLATE CYSTS; MARINE PALEOGENE; BIOSTRATIGRAPHY; STRATIGRAPHY; DEPOSITS; SECTION	The Paleocene-Eocene transition is one of the most remarkable Cenozoic periods coinciding with the global thermal maximum (PETM). Based on the complex biostratigraphic analysis of diatoms, silicoflagellates, and dinocysts, this global event is revealed in three sections of the Middle Trans-Urals region (Kamyshlov, Korkino, Chumlyak) represented by marine biosiliceous sediments of the Serov and Irbit formations. The interval of the Trinacra ventriculosa-Hemiaulus proteus-Coscinodiscus uralensis diatom zones is marked by the appearance of new genera Moisseevia, Solium, Fenestrella, Craspedodiscus, Podosira, Pseudotriceratium, intense radiations of Grunoweiella and Coscinodiscus, and development of extreme morphotypes among silicoflagellates. The defined diatom assemblages differ slightly from their coeval counterparts from the Middle Volga region, which casts doubt upon the assumed stable water exchange between these basins. On the contrary, the dinocyst assemblages are lacking zonal index species (Appectodinium homomorphum, A. augustum) and Apectodinium acme characteristic of the transitional Paleocene-Eocene strata in many worldwide localities. The facies settings of his period with intense vertical mixing and relatively low temperatures and salinity are characterized by the dominant role of dinocysts belonging to the genera Areoligera, Deflandrea, Spiniferites, and Operculodinium.	[Aleksandrova, G. N.; Oreshkina, T. V.; Iakovleva, A. I.; Radionova, E. P.] Russian Acad Sci, Inst Geol, Moscow 119017, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Aleksandrova, GN (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevskii Per 7, Moscow 119017, Russia.	dinoflag@mail.ru	Galina, Aleksandrova/AAW-8215-2020; IAKOVLEVA, ALINA/ABH-9243-2020; Oreshkina, Tatyana/ABC-6121-2021	Oreshkina, Tatiana V./0000-0002-7477-7272	Russian Foundation for Basic Research [09-05-00210-a, 11-05-11431-a]; Presidium of the Russian Academy of Sciences [25];  [16.740.11.0050]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Presidium of the Russian Academy of Sciences(Russian Academy of Sciences); 	This work was supported by the Russian Foundation for Basic Research (project nos. 09-05-00210-a; G. N. Aleksandrova, A. I. Iakovleva; and 11-05-11431-a; G. N. Aleksandrova, T. V. Oreshkina), State contract no. 16.740.11.0050 (T. V. Oreshkina), and Program no. 25 of the Presidium of the Russian Academy of Sciences.	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Geol. Correl.	JUL	2012	20	4					380	404		10.1134/S0869593812030021	http://dx.doi.org/10.1134/S0869593812030021			25	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	985ZE					2025-03-11	WOS:000307308200003
J	Kupinska, M; Sachs, O; Sauter, EJ; Zonneveld, KAF				Kupinska, Monika; Sachs, Oliver; Sauter, Eberhard J.; Zonneveld, Karin A. F.			Aerobic degradation of organic carbon inferred from dinoflagellate cyst decomposition in Southern Ocean sediments	QUATERNARY RESEARCH			English	Article						Organic-walled dinoflagellate cysts; Oxygen; Organic carbon; Degradation	EASTERN ATLANTIC SECTOR; OXYGEN EXPOSURE TIME; SURFACE SEDIMENTS; FALKLAND TROUGH; PRESERVATION; MATTER; SEA; WEDDELL; SCOTIA; MODEL	Organic carbon (OC) burial is an important process influencing atmospheric CO2 concentration and global climate change; therefore it is essential to obtain information on the factors determining its preservation. The Southern Ocean (SO) is believed to play an important role in sequestering CO2 from the atmosphere via burial of OC. Here we investigate the degradation of organic-walled dinoflagellate cysts (dinocysts) in two short cores from the SO to obtain information on the factors influencing OC preservation. On the basis of the calculated degradation index kt, we conclude that both cores are affected by species-selective aerobic degradation of dinocysts. Further, we calculate a degradation constant k using oxygen exposure time derived from the ages of our cores. The constant k displays a strong relationship with pore-water O-2, suggesting that decomposition of OC is dependent on both the bottom- and pore-water O-2 concentrations. (C) 2012 University of Washington. Published by Elsevier Inc. All rights reserved.	[Kupinska, Monika; Zonneveld, Karin A. F.] Fachbereich 5 Geowissensch, D-28334 Bremen, Germany; [Sauter, Eberhard J.] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Sachs, Oliver] Eberhard & Partner AG, CH-5000 Aarau, Switzerland	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Kupinska, M (通讯作者)，Univ Szczecin, Geosci Fac, Mickiewicza 18, PL-70383 Szczecin, Poland.	monika.kodrans-nsiah@univ.szczecin.pl		Sauter, Eberhard/0000-0001-7954-952X	DFG grant EUROPROX	DFG grant EUROPROX	We thank Timothy G. Ferdelman (MPI, Bremen) and Ian C. Harding (NOC, Southampton) for helpful consultations. This study was supported by DFG grant EUROPROX.	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Res.	JUL	2012	78	1					130	138		10.1016/j.yqres.2012.04.001	http://dx.doi.org/10.1016/j.yqres.2012.04.001			9	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	969YV					2025-03-11	WOS:000306096200013
J	Hakimi, MH; Abdullah, WH; Shalaby, MR				Hakimi, Mohammed Hail; Abdullah, Wan Hasiah; Shalaby, Mohamed Ragab			Molecular composition and organic petrographic characterization of Madbi source rocks from the Kharir Oilfield of the Masila Basin (Yemen): palaeoenvironmental and maturity interpretation	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Biomarkers; Organic petrology; Thermal maturity; Depositional environment; Madbi source rock; Masila basin; Yemen	QISHN FORMATION; HYDROCARBONS; GEOCHEMISTRY; PETROLEUM; PRISTANE; PHYTANE; RATIO; GULF; ADEN	The upper part of Madbi Formation organic-rich shale is considered an important regional source rock in the Masila Basin, Yemen. Ten cutting samples from this Upper Jurassic organic-rich shale were collected from wells drilled in the Kharir Oilfield, Masila Basin in order to geochemically assess the type of organic matter, thermal maturity and depositional environment conditions. Results reveal that Upper Jurassic organic-rich shale samples contain high organic matter more than 2.0 wt.% TOC and have very good to excellent hydrocarbon potential. Marine algae organic matter is the main source input for the Upper Jurassic shale sequence studied. This has been identified from organic petrographic characteristics and from the n-alkane distributions, which dominated by n-C-14-n-C-20 alkanes. This is supported by the high value of the biomarker sterane/hopane ratio that approaches unity, as well as the relatively high C-27 sterane concentrations. A mainly suboxic depositional environment is inferred from pr/ph ratios (1.75-2.38). This is further supported by relatively high homohopane value, which is dominated by low carbon numbers and decrease towards the C-35 homohopane. The concentrations of C-35 homohopane are very low. The depositional environment conditions are confirmed by some petrographic characteristics (e.g. palynofacies). Detailed palynofacies analysis of Madbi shales shows that the Madbi shale formation is characterised by a mix of amorphous organic matter, dinoflagellates cysts and phytoclasts, representing a suboxic, open marine setting. The Upper Jurassic marine shale sequence in the Masila Basin is thermally mature for hydrocarbon generation as indicated by biomarker thermal maturity parameters. The 22 S/22 S + 22R C-32 homohopane has reached equilibrium, with values range from 0.58 to 0.62 which suggest that the Upper Jurassic shales are thermally mature and that the oil window has been reached. 20 S/(20 S + 20R) and beta beta/(beta beta + I +/- I +/-) C-29 sterane ratios suggest a similar interpretation, as do the moretane/hopane ratio. This is supported by vitrinite reflectance data ranging from 0.74% to 0.90%Ro and thermal alteration of pollen and spore. The thermal alteration index value is around 2.6-3.0, corresponding to a palaeotemperature range of 60-120A degrees C. These are the optimum oil-generating strata. On the basis of this study, the Madbi source rock was deposited under suboxic conditions in an open marine environment and this source rock is still within the oil window maturity range.	[Hakimi, Mohammed Hail] Taiz Univ, Dept Geol, Fac Sci Appl, Taizi 6803, Yemen; [Hakimi, Mohammed Hail; Abdullah, Wan Hasiah; Shalaby, Mohamed Ragab] Univ Malaya, Dept Geol, Kuala Lumpur 50603, Malaysia	Taiz University; Universiti Malaya	Hakimi, MH (通讯作者)，Taiz Univ, Dept Geol, Fac Sci Appl, Taizi 6803, Yemen.	ibnalhakimi@yahoo.com	Hakimi, Mohammed/ABG-3908-2021; Shalaby, Mohamed/B-5662-2017; Abdullah, Wan Hasiah/C-1007-2010	Shalaby, Mohamed/0000-0003-0556-2726; Abdullah, Wan Hasiah/0000-0002-6748-1019; Hakimi, Mohammed/0000-0002-3320-9690	Taiz University, Republic of Yemen	Taiz University, Republic of Yemen	This paper results from the work carried out for the PhD research project at the University of Malaya, Kuala Lumpur, Malaysia under the financial support of Government Scholarship from the Taiz University, Republic of Yemen. The authors would like to thank the authority of Total Oil Company and Petroleum Exploration and Production Authority, Yemen (PEPA) for providing the samples for this study. The authors are more grateful to the Department of Geology, University of Malaya for providing facilities to complete this research. The authors also thank the anonymous referees, editors and design staff of Arabian Journal Geosciences.	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J	Tauxe, L; Stickley, CE; Sugisaki, S; Bijl, PK; Bohaty, SM; Brinkhuis, H; Escutia, C; Flores, JA; Houben, AJP; Iwai, M; Jimenez-Espejo, FJ; McKay, R; Passchier, S; Pross, J; Riesselman, CR; Röhl, U; Sangiorgi, F; Welsh, K; Klaus, A; Fehr, A; Bendle, JAP; Dunbar, R; Gonzàlez, J; Hayden, T; Katsuki, K; Olney, MP; Pekar, SF; Shrivastava, PK; van de Flierdt, T; Williams, T; Yamane, M				Tauxe, L.; Stickley, C. E.; Sugisaki, S.; Bijl, P. K.; Bohaty, S. M.; Brinkhuis, H.; Escutia, C.; Flores, J. A.; Houben, A. J. P.; Iwai, M.; Jimenez-Espejo, Francisco J.; McKay, R.; Passchier, S.; Pross, J.; Riesselman, C. R.; Roehl, U.; Sangiorgi, F.; Welsh, K.; Klaus, A.; Fehr, A.; Bendle, J. A. P.; Dunbar, R.; Gonzalez, J.; Hayden, T.; Katsuki, K.; Olney, M. P.; Pekar, S. F.; Shrivastava, P. K.; van de Flierdt, T.; Williams, T.; Yamane, M.			Chronostratigraphic framework for the IODP Expedition 318 cores from the Wilkes Land Margin: Constraints for paleoceanographic reconstruction	PALEOCEANOGRAPHY			English	Article							PASS-THROUGH MAGNETOMETER; EOCENE-OLIGOCENE; CALIBRATION; SEA; AGE; MAGNETOSTRATIGRAPHY; PLATEAU; SECTION; RISE	The Integrated Ocean Drilling Program Expedition 318 to the Wilkes Land margin of Antarctica recovered a sedimentary succession ranging in age from lower Eocene to the Holocene. Excellent stratigraphic control is key to understanding the timing of paleoceanographic events through critical climate intervals. Drill sites recovered the lower and middle Eocene, nearly the entire Oligocene, the Miocene from about 17 Ma, the entire Pliocene and much of the Pleistocene. The paleomagnetic properties are generally suitable for magnetostratigraphic interpretation, with well-behaved demagnetization diagrams, uniform distribution of declinations, and a clear separation into two inclination modes. Although the sequences were discontinuously recovered with many gaps due to coring, and there are hiatuses from sedimentary and tectonic processes, the magnetostratigraphic patterns are in general readily interpretable. Our interpretations are integrated with the diatom, radiolarian, calcareous nannofossils and dinoflagellate cyst (dinocyst) biostratigraphy. The magnetostratigraphy significantly improves the resolution of the chronostratigraphy, particularly in intervals with poor biostratigraphic control. However, Southern Ocean records with reliable magnetostratigraphies are notably scarce, and the data reported here provide an opportunity for improved calibration of the biostratigraphic records. In particular, we provide a rare magnetostratigraphic calibration for dinocyst biostratigraphy in the Paleogene and a substantially improved diatom calibration for the Pliocene. This paper presents the stratigraphic framework for future paleoceanographic proxy records which are being developed for the Wilkes Land margin cores. It further provides tight constraints on the duration of regional hiatuses inferred from seismic surveys of the region.	[Tauxe, L.; Sugisaki, S.] Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA; [Stickley, C. E.] Univ Tromso, Dept Geol, Tromso, Norway; [Bijl, P. K.; Brinkhuis, H.; Houben, A. J. P.; Sangiorgi, F.] Univ Utrecht, Dept Earth Sci, Utrecht, Netherlands; [Bohaty, S. M.] Univ Southampton, Sch Ocean & Earth Sci, Southampton, Hants, England; [Escutia, C.; Jimenez-Espejo, Francisco J.; Gonzalez, J.] Univ Granada, Inst Andaluz Ciencias Tierra, CSIC, Armilla, Spain; [Flores, J. A.] Univ Salamanca, Fac Ciencias, Dept Geol, E-37008 Salamanca, Spain; [Iwai, M.] Kochi Univ, Dept Nat Environm Sci, Kochi 780, Japan; [McKay, R.] Victoria Univ Wellington, Antarctic Res Ctr, Wellington, New Zealand; [Passchier, S.] Montclair State Univ, Montclair, NJ USA; [Pross, J.] Goethe Univ Frankfurt, Inst Geosci, Frankfurt, Germany; [Riesselman, C. R.] US Geol Survey, Eastern Geol & Paleoclimate Sci Ctr, Reston, VA 22092 USA; [Roehl, U.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Welsh, K.] Univ Queensland, Sch Earth Sci, Brisbane, Qld, Australia; [Klaus, A.] Texas A&M Univ, US Implementing Org, Integrated Ocean Drilling Program, College Stn, TX USA; [Fehr, A.] Rhein Westfal TH Aachen, Inst Appl Geophys & Geothermal Energy, Aachen, Germany; [Bendle, J. A. P.] Univ Glasgow, Glasgow, Lanark, Scotland; [Dunbar, R.] Stanford Univ, Dept Geol & Environm Sci, Stanford, CA 94305 USA; [Hayden, T.] Western Michigan Univ, Dept Geol, Kalamazoo, MI 49008 USA; [Katsuki, K.] Korea Inst Geosci & Mineral Resources, Div Geol Res, Quaternary Geol Res Dept, Taejon, South Korea; [Olney, M. P.] Univ S Florida, Dept Geol, Tampa, FL 33620 USA; [Pekar, S. F.] Queens Coll, Sch Earth & Environm Sci, Flushing, NY USA; [Shrivastava, P. K.] Geol Survey India, Antarctica Div, Faridabad, India; [van de Flierdt, T.] Univ London Imperial Coll Sci Technol & Med, Dept Earth Sci & Engn, London, England; [Williams, T.] Columbia Univ, Lamont Doherty Earth Observ, Borehole Res Grp, Palisades, NY USA; [Yamane, M.] Univ Tokyo, Tokyo, Japan	University of California System; University of California San Diego; Scripps Institution of Oceanography; UiT The Arctic University of Tromso; Utrecht University; NERC National Oceanography Centre; University of Southampton; University of Granada; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto Andaluz de Ciencias de la Tierra (IACT); University of Salamanca; Kochi University; Victoria University Wellington; Montclair State University; Goethe University Frankfurt; United States Department of the Interior; United States Geological Survey; University of Bremen; University of Queensland; Texas A&M University System; Texas A&M University College Station; RWTH Aachen University; University of Glasgow; Stanford University; Western Michigan University; Korea Institute of Geoscience & Mineral Resources (KIGAM); State University System of Florida; University of South Florida; City University of New York (CUNY) System; Queens College NY (CUNY); Geological Survey India; Imperial College London; Columbia University; University of Tokyo	Tauxe, L (通讯作者)，Univ Calif San Diego, Scripps Inst Oceanog, 9500 Gilman Dr, La Jolla, CA 92093 USA.	ltauxe@ucsd.edu	Williams, Trevor/L-7670-2014; Röhl, Ursula/G-5986-2011; Passchier, Sandra/AAQ-2243-2021; McKay, Robert/N-2449-2015; Riesselman, Christina/H-5037-2012; Brinkhuis, Henk/IUO-8165-2023; Flores, José-Abel/D-4218-2009; Escutia, Carlota/B-8614-2015; Welsh, Kevin/A-9808-2012; JIMENEZ-ESPEJO, Francisco J./F-4486-2016; Passchier, Sandra/B-1993-2008	Dunbar, Robert/0000-0002-9728-5609; Escutia, Carlota/0000-0002-4932-8619; Welsh, Kevin/0000-0002-4834-4190; Bendle, James/0000-0002-6826-8658; Houben, Alexander/0000-0002-9497-1048; van de Flierdt, Tina/0000-0001-7176-9755; Bijl, Peter/0000-0002-1710-4012; McKay, Robert/0000-0002-5602-6985; Yamane, Masako/0000-0002-5063-0719; Iwai, Masao/0000-0001-7489-1262; JIMENEZ-ESPEJO, Francisco J./0000-0002-0335-8580; Passchier, Sandra/0000-0001-7204-7025; Riesselman, Christina/0000-0002-2436-4306; Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610	NSF [OCE1058858, OCE1054497]; Division Of Ocean Sciences; Directorate For Geosciences [1058858, 1060080, 1129101] Funding Source: National Science Foundation; NERC [NE/H014144/1, NE/I006257/1, NE/I00646X/1, NE/H014616/1, NE/H025162/1, NE/I00646X/2] Funding Source: UKRI	NSF(National Science Foundation (NSF)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We are deeply grateful for the hard work of the entire shipboard party of IODP Expedition 318, including scientific, technical, and support staff. In particular, we wish to thank Maggie Hastedt, whose tireless and cheerful help in the paleomagnetic laboratory was essential to the success of our investigations. We thank Joe Smoot, Jan Backman, two anonymous reviewers, and the Editor, Rainer Zahn, for careful review which greatly improved the manuscript. This research used samples and data provided by the Integrated Ocean Drilling Program (IODP). Funding for this research was provided by NSF grants OCE1058858 and OCE1054497 to L.T.	Acton GD, 2002, J GEOPHYS RES-SOL EA, V107, DOI 10.1029/2001JB000518; Agnini C, 2006, EARTH PLANET SC LETT, V241, P815, DOI 10.1016/j.epsl.2005.11.005; [Anonymous], 2010, ESSENTIALS CRYSTALLO; Bijl P. 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J	Sanchez-Cabeza, JA; Ruiz-Fernández, AC; de Vernal, A; Machain-Castillo, ML				Sanchez-Cabeza, Joan-Albert; Carolina Ruiz-Fernandez, Ana; de Vernal, Anne; Luisa Machain-Castillo, Maria			Reconstruction of Pyrodinium Blooms in the Tropical East Pacific (Mexico): Are They Related to ENSO?	ENVIRONMENTAL SCIENCE & TECHNOLOGY			English	Article							HARMFUL ALGAL BLOOMS; BAHAMENSE VAR. COMPRESSUM; MANILA BAY	Some microplanktonic species, mostly dinoflagellates, causing Harmful Algal Blooms (HABs), produce toxins which may affect the environment and human health, thus causing important economic losses. The dinoflagellate Pyrodinium bahamense var. compressum is one of the main species causing harmful algal blooms along the tropical Pacific. Although it was first reported along the Mexican coast in the 1970s, here we report that a sedimentary record of Pyrodinium cysts from the Gulf of Tehuantepec in the tropical East Pacific (Mexico), which spans from the 1860s, showed the continuous occurrence of Pyrodinium cysts and that their presence has been declining in the last few decades. Although Pyrodinium HABs have been attributed to El Nino events in the tropical Indo-West Pacific, the record shows that most blooms in the tropical East Pacific appear in periods of low sea surface temperature and higher rainfall, as can be observed during rapid shifts from cold (La Nina) to warm (El Nino) conditions in that region. This mechanism offers new ways to better predict and facilitate early detection of Pyrodinium HABs worldwide.	[Sanchez-Cabeza, Joan-Albert; Carolina Ruiz-Fernandez, Ana; Luisa Machain-Castillo, Maria] Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Mexico City 04510, DF, Mexico; [Sanchez-Cabeza, Joan-Albert] Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Bellaterra 08193, Spain; [Sanchez-Cabeza, Joan-Albert] Univ Autonoma Barcelona, Dept Fis, Bellaterra 08193, Spain; [de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada	Universidad Nacional Autonoma de Mexico; Autonomous University of Barcelona; Autonomous University of Barcelona; University of Quebec; University of Quebec Montreal	Sanchez-Cabeza, JA (通讯作者)，Univ Nacl Autonoma Mexico, Inst Ciencias Mar & Limnol, Mexico City 04510, DF, Mexico.	joanalbert.sanchez@uab.cat	Ruiz-Fernández, Ana Carolina/ABG-6985-2020; Sanchez-Cabeza, Joan-Albert/Q-2394-2016; de Vernal, Anne/D-5602-2013	RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249; MACHAIN-CASTILLO, MARIA LUISA/0000-0002-4973-4967; Sanchez-Cabeza, Joan-Albert/0000-0002-3540-1168; de Vernal, Anne/0000-0001-5656-724X	UNESCO Environment Chair at GEOTOP-UQAM-McGill; SRE; CONACYT;  [CONACyT SEP-2004-C01-45841-F]	UNESCO Environment Chair at GEOTOP-UQAM-McGill; SRE; CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); 	This work was partially funded by the UNESCO Environment Chair at GEOTOP-UQAM-McGill and the grant CONACyT SEP-2004-C01-45841-F. SRE and CONACYT provided support for academic exchange through the International Cooperation Program Mexico-Quebec 2007-2009. Thanks are due to Dr. R. Alonso-Rodriguez for help in taxonomic identification of cysts; the crew of the O/V El Puma for their support during sampling activities; and to M. Henry, M.C. Ramirez-Jauregui, G. Ramirez-Resendiz, H. Bojorquez-Leyva, L. H. Perez-Bernal, and V. Montes-Montes for their technical assistance. The Abstract Figure was kindly provided by M. en C. Roberto Cortes Altamirano.	Azanza RV, 2001, AMBIO, V30, P356, DOI 10.1639/0044-7447(2001)030[0356:APBITS]2.0.CO;2; Butschli O., 1885, BRONNS KLASSEN ORDNU, P906, DOI DOI 10.5962/BHL.TITLE.11642; Claparkle E., 1859, MEM INST NAT GENEV, V5-6, P480; Cortes-Altamirano R., 1996, Harmful and Toxic Algal Blooms, P101; Cuesta-Castillo L. 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Sci. Technol.	JUN 19	2012	46	12					6830	6834		10.1021/es204376e	http://dx.doi.org/10.1021/es204376e			5	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	959OA	22577973				2025-03-11	WOS:000305320900050
J	Shumilovskikh, LS; Tarasov, P; Arz, HW; Fleitmann, D; Marret, F; Nowaczyk, N; Plessen, B; Schlütz, F; Behling, H				Shumilovskikh, Lyudmila S.; Tarasov, Pavel; Arz, Helge W.; Fleitmann, Dominik; Marret, Fabienne; Nowaczyk, Norbert; Plessen, Birgit; Schluetz, Frank; Behling, Hermann			Vegetation and environmental dynamics in the southern Black Sea region since 18 kyr BP derived from the marine core 22-GC3	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pollen; Biomes; Multi-proxy reconstruction; Late-glacial; Holocene; Northern Anatolia	HOLOCENE CLIMATIC-CHANGE; LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYST ASSEMBLAGES; EASTERN MEDITERRANEAN REGION; NORTH-ATLANTIC OSCILLATION; PLANT MACROFOSSIL DATA; HIGH-RESOLUTION POLLEN; LATE QUATERNARY CORES; FORMER SOVIET-UNION; PALYNOLOGICAL EVIDENCE	Sediments from the Black Sea, a region historically dominated by forests and steppe landscapes, are a valuable source of detailed information on the changes in regional terrestrial and aquatic environments at decadal to millennial scales. Here we present multi-proxy environmental records (pollen, dinoflagellate cysts, Ca, Ti and oxygen isotope data) from the uppermost 305 cm of the core 22-GC3 (42 degrees 13.53'N, 36 degrees 29.55'E) collected from a water depth of 838 m in the southern part of the Black Sea in 2007. The records span the last similar to 18 kyr (all ages are given in cal kyr BP). The pollen data reveal the dominance of the Artemisia-steppe in the region, suggesting rather dry/cold environments similar to 18-14.5 kyr BP. Warming/humidity increase during melt-water pulses (similar to 16.1-14.5 kyr BP), indicated by delta O-18 records from the 22-GC3 core sediment and from the Sofular Cave stalagmite, is expressed in more negative delta C-13 values from the Sofular Cave, usually interpreted as the spreading of C3 plants. The records representing the interstadial complex (similar to 14.5-12.9 kyr BP) show an increase in temperature and moisture, indicated by forest development, increased primary productivity and reduced surface run-off, whereas the switch from primary terrigenous to primary authigenic Ca origin occurs similar to 500 yr later. The Younger Dryas cooling is clearly demonstrated by more negative delta C-13 values from the Sofular Cave and a reduction of pines. The early Holocene (11.7-8.5 kyr BP) interval reveals relatively dry conditions compared to the mostly moist and warm middle Holocene (8.5-5 kyr BP), which is characterized by the establishment of the species-rich warm mixed and temperate deciduous forests in the low elevation belt, temperate deciduous beech-hornbeam forests in the middle and cool conifer forest in upper mountain belt. The border between the early and middle Holocene in the vegetation records coincides with the opening of the Mediterranean corridor at similar to 8.3 kyr BP, as indicated by a marked change in the dinocyst assemblages and in the sediment lithology. Changes in the pollen assemblages indicate a reduction in forest cover after similar to 5 kyr BP, which was likely caused by increased anthropogenic pressure on the regional vegetation. (C) 2012 Elsevier B.V. All rights reserved.	[Shumilovskikh, Lyudmila S.] Univ Gottingen, Dept Palynol & Climate Dynam, Albrecht von Haller Inst Plant Sci, D-37073 Gottingen, Germany; [Tarasov, Pavel; Schluetz, Frank] Free Univ Berlin, Inst Geol Sci, Dept Palaeontol, D-12249 Berlin, Germany; [Arz, Helge W.] Leibniz Inst Balt Sea Res Warnemuende, D-18119 Rostock, Germany; [Fleitmann, Dominik] Univ Bern, Oeschger Ctr Climate Change Res, CH-3012 Bern, Switzerland; [Fleitmann, Dominik] Inst Geol Sci, CH-3012 Bern, Switzerland; [Marret, Fabienne] Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Nowaczyk, Norbert; Plessen, Birgit] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany; [Schluetz, Frank] Lower Saxony Inst Hist Coastal Res, D-26382 Wilhelmshaven, Germany	University of Gottingen; Free University of Berlin; University of Bern; University of Liverpool; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences	Shumilovskikh, LS (通讯作者)，Univ Gottingen, Dept Palynol & Climate Dynam, Albrecht von Haller Inst Plant Sci, Wilhelm Weber Str 2A, D-37073 Gottingen, Germany.	shumilovskikh@yahoo.com	Arz, Helge/A-6659-2013; Shumilovskikh, Lyudmila/P-2493-2015; Fleitmann, Domnik/HSF-0516-2023; Tarasov, Pavel/ABG-3993-2020	/0000-0002-7219-5009; Fleitmann, Dominik/0000-0001-5977-8835; Arz, Helge Wolfgang/0000-0002-1997-1718; Marret-Davies, Fabienne/0000-0003-4244-0437; Schroder, Birgit/0000-0003-4807-6357	German Research Foundation (DFG) [BE 2116/20-1, TA-540/1-2, AR 367/9-1, FL 710/1-1]	German Research Foundation (DFG)(German Research Foundation (DFG))	This paper is a contribution to the German Research Foundation (DFG) sponsored projects (BE 2116/20-1, TA-540/1-2; AR 367/9-1, FL 710/1-1) within the Priority Program 1266 "Integrated analysis of interglacial climate dynamics" (INTERDYNAMIC). We would like to thank Hans-Jurgen Beug, Galina Pashkevich and Eliso Kvavadze for providing us with necessary information, Erwin Bergmeier for consultation on vegetation in northern Turkey, Gilles Shephard and Laura Sutcliffe for polishing the English. Special thanks go to the editor of "Palaeogeography, Palaeoclimatology, Palaeoecology" Prof. A. Peter Kershaw and anonymous reviewers for critical reading and improving the manuscript. Finally, we thank the captain and crew of RV Meteor for their support and contribution to the overall success of the M72/5 Black Sea research cruise in 2007.	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Paleoclimatol. Paleoecol.	JUN 15	2012	337						177	193		10.1016/j.palaeo.2012.04.015	http://dx.doi.org/10.1016/j.palaeo.2012.04.015			17	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	969CA					2025-03-11	WOS:000306032100015
J	Nohr-Hansen, H				Nohr-Hansen, Henrik			Palynostratigraphy of the Cretaceous-lower Palaeogene sedimentary succession in the Kangerlussuaq Basin, southern East Greenland	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Cretaceous; Palaeogene; palynostratigraphy; dinocysts; Kangerlussuaq Basin; southern East Greenland	SEQUENCE STRATIGRAPHY; TERTIARY BOUNDARY; WEST GREENLAND; DINOFLAGELLATE; BIOSTRATIGRAPHY; EVENT	A new palynological event biostratigraphy for the Cretaceous-lower Palaeogene succession in the Kangerlussuaq Basin, onshore southern East Greenland is presented. Sixty-three biostratigraphical marker events are recognised, based on the first and last occurrences of dinoflagellate cysts and pollen from eleven key outcrop sections through the Sorgenfri, Christian IV, Sediment Bjerge and Vandfaldsdalen Formations of the Kangerdlugssuaq and Blosseville Groups. The palynological events are correlated with published event stratigraphies and with palynological zonations from North-East Greenland, West Greenland, North America, the North Sea and the Faroe-Shetland Basin. The palynological records date the Sorgenfri Formation as middle Albian to Coniacian or ?early Santonian, the Christian IV Formation as ?late Campanian to late Maastrichtian and the Sediment Bjerge Formation as late Danian to late Selandian. The biostratigraphic ranges of dinoflagellate cysts, pollen and macrofossils around the lower to upper Maasttichtian boundary are discussed and correlated. The palynological records and recent isotopic dating results (40Ar/39Ar) of volcanic rocks indicate that the youngest sediments of the Vandfaldsdalen Formation are of Thanetian or early Ypresian age. The study documents two major hiatuses in the area: the boundary between the Sorgenfri and Christian IV Formations spans the ?upper Coniacian-Santonian and Campanian, whilst the unconformity between the Christian IV and Sediment Bjerge Formations possibly spans the uppermost Maastrichtian and the lower Danian, indicating that the Cretaceous-Palaeogene boundary is represented by a major unconformity, as recognised widely around the northern North Atlantic. (C) 2012 Elsevier B.V. All rights reserved. A new palynological event biostratigraphy for the Cretaceous-lower Palaeogene succession in the Kangerlussuaq Basin, onshore southern East Greenland is presented. Sixty-three biostratigraphical marker events are recognised, based on the first and last occurrences of dinoflagellate cysts and pollen from eleven key outcrop sections through the Sorgenfri, Christian IV, Sediment Bjerge and Vandfaldsdalen Formations of the Kangerdlugssuaq and Blosseville Groups. The palynological events are correlated with published event stratigraphies and with palynological zonations from North-East Greenland, West Greenland, North America, the North Sea and the Faroe-Shetland Basin. The palynological records date the Sorgenfri Formation as middle Albian to Coniacian or ?early Santonian, the Christian IV Formation as ?late Campanian to late Maastrichtian and the Sediment Bjerge Formation as late Danian to late Selandian. The biostratigraphic ranges of dinoflagellate cysts, pollen and macrofossils around the lower to upper Maasttichtian boundary are discussed and correlated. The palynological records and recent isotopic dating results (40Ar/39Ar) of volcanic rocks indicate that the youngest sediments of the Vandfaldsdalen Formation are of Thanetian or early Ypresian age. The study documents two major hiatuses in the area: the boundary between the Sorgenfri and Christian IV Formations spans the ?upper Coniacian-Santonian and Campanian, whilst the unconformity between the Christian IV and Sediment Bjerge Formations possibly spans the uppermost Maastrichtian and the lower Danian, indicating that the Cretaceous-Palaeogene boundary is represented by a major unconformity, as recognised widely around the northern North Atlantic. (C) 2012 Elsevier B.V. All rights reserved.	[Nohr-Hansen, Henrik] GEUS, Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Nohr-Hansen, H (通讯作者)，GEUS, Geol Survey Denmark & Greenland, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	hnh@geus.dk	Nohr-Hansen, Henrik/G-9058-2018	Nohr-Hansen, Henrik/0000-0002-9291-8104				Antonescu E., 2001, Developments in Palaeontology and Stratigraphy, V19, P253; BINT A N, 1986, Palynology, V10, P135; Birkelund T., 1965, B GRONLANDS GEOLOGIS, V56; BRINKHUIS H, 1988, MAR MICROPALEONTOL, V13, P153, DOI 10.1016/0377-8398(88)90002-3; Catuneanu O, 1999, CAN J EARTH SCI, V36, P685, DOI 10.1139/e98-018; Costa L.I., 1992, P99; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; Dodsworth P, 2000, J MICROPALAEONTOL, V19, P69, DOI 10.1144/jm.19.1.69; Ebdon C.C., 1995, GEOLOGICAL SOC SPECI, V90, P50, DOI DOI 10.1144/GSL.SP.1995.090.01.03; Fensome R.A., 2004, AM STRATIGRAPHIC PAL, V42; Fensome R.A., 2008, Atlantic Geology, V44, P93, DOI DOI 10.4138/6506; FIRTH J V, 1987, Palynology, V11, P199; FIRTH JV, 1993, REV PALAEOBOT PALYNO, V79, P179, DOI 10.1016/0034-6667(93)90022-M; Gradstein F.M., 2004, A Geologic Time Scale; Hamberg L., 1990, KANGERDLUGSSUAQ STUD, P46; Hansen H, 2002, GEOL SOC SPEC PUBL, V197, P183, DOI 10.1144/GSL.SP.2002.197.01.08; Hansen J.M., 1978, MICROPALEONTOLOGY, V25, P113; Harding IC, 2011, EARTH PLANET SC LETT, V303, P97, DOI 10.1016/j.epsl.2010.12.043; Heilmann-Clausen C, 2008, NEWSL STRATIGR, V43, P55, DOI 10.1127/0078-0421/2008/0043-0055; HIGGINS AC, 1981, GEOL MAG, V118, P337, DOI 10.1017/S0016756800032210; Hjortkj├r B.F., 1999, IMPLICATIONS BREAK U; Jolley DW, 2004, PETROL GEOSCI, V10, P53, DOI 10.1144/1354-079302-511; Kennedy W. 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Soc. Denm. Bull, V33, P341; Waagstein R., 1995, TECTONICS SEDIMENTAT, P179, DOI DOI 10.1144/GSL.SP.1995.090.01.11; Wager L.R., 1934, MEDD GRONLAND, V105; WAGER L.R., 1947, Meddelelser om Gronland, V134; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1	72	51	52	0	14	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JUN 15	2012	178						59	90		10.1016/j.revpalbo.2012.03.009	http://dx.doi.org/10.1016/j.revpalbo.2012.03.009			32	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	961AB					2025-03-11	WOS:000305434700005
J	Liu, L; Guo, FJ; Crain, S; Quilliam, MA; Wang, XT; Rein, KS				Liu, Li; Guo, Fujiang; Crain, Sheila; Quilliam, Michael A.; Wang, Xiaotang; Rein, Kathleen S.			The structures of three metabolites of the algal hepatotoxin okadaic acid produced by oxidation with human cytochrome P450	BIOORGANIC & MEDICINAL CHEMISTRY			English	Article						Okadaic acid; Dinoflagellate; Algal toxin; Xenobiotic metabolism; Cytochrome P450	ASSAY	Four metabolites of okadaic acid were generated by incubation with human recombinant cytochrome P450 3A4. The structures of two of the four metabolites have been determined by MS/MS experiments and 1D and 2D NMR methods using 94 and 133 mu g of each metabolite. The structure of a third metabolite was determined by oxidation to a metabolite of known structure. Like okadaic acid, the metabolites are inhibitors of protein phosphatase PP2A. Although one of the metabolites does have an alpha,beta unsaturated carbonyl with the potential to form adducts with an active site cysteine, all of the metabolites are reversible inhibitors of PP2A. (C) 2012 Elsevier Ltd. All rights reserved.	[Liu, Li; Guo, Fujiang; Wang, Xiaotang; Rein, Kathleen S.] Florida Int Univ, Dept Chem & Biochem, Miami, FL 33199 USA; [Crain, Sheila; Quilliam, Michael A.] Natl Res Council Canada, Inst Marine Biosci, Halifax, NS B3H 3Z1, Canada	State University System of Florida; Florida International University; International Business Machines (IBM); IBM Canada; National Research Council Canada	Rein, KS (通讯作者)，Florida Int Univ, Dept Chem & Biochem, 11200 SW 8th St, Miami, FL 33199 USA.	reink@fiu.edu	Rein, Kathleen/AAP-3668-2021	Quilliam, Michael/0000-0002-2670-4220	National Institute of Environmental Health Sciences (NIEHS) [S11 ES11181]; NSF-NIEHS Oceans and Human Health Center (National Science Foundation) [0432368]; NSF-NIEHS Oceans and Human Health Center (NIEHS) [P50 ES12736-01]; Division Of Ocean Sciences; Directorate For Geosciences [0432368] Funding Source: National Science Foundation	National Institute of Environmental Health Sciences (NIEHS)(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); NSF-NIEHS Oceans and Human Health Center (National Science Foundation); NSF-NIEHS Oceans and Human Health Center (NIEHS); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was supported by the National Institute of Environmental Health Sciences (NIEHS) Grant S11 ES11181, the NSF-NIEHS Oceans and Human Health Center Program (National Science Foundation grant 0432368 and NIEHS grant P50 ES12736-01). Assistance with the NMR experiments from J.A. Walter (NRC) is greatly appreciated.	An TY, 2010, TOXICON, V55, P653, DOI 10.1016/j.toxicon.2009.08.018; Deeds JR, 2010, TOXICON, V55, P1138, DOI 10.1016/j.toxicon.2010.01.003; Fessard V, 1996, MUTAT RES-ENVIR MUTA, V361, P133, DOI 10.1016/S0165-1161(96)90248-4; Guo FJ, 2010, TOXICON, V55, P325, DOI 10.1016/j.toxicon.2009.08.007; HU TM, 1992, J NAT PROD, V55, P1631, DOI 10.1021/np50089a011; Le Hégarat L, 2004, ENVIRON TOXICOL, V19, P123, DOI 10.1002/tox.20004; Le Hegarat L, 2003, MUTAGENESIS, V18, P293, DOI 10.1093/mutage/18.3.293; MACKINTOSH RW, 1995, FEBS LETT, V371, P236, DOI 10.1016/0014-5793(95)00888-G; Miles CO, 2006, TOXICON, V48, P195, DOI 10.1016/j.toxicon.2006.04.018; Pinto-Silva CR, 2005, ARCH TOXICOL, V79, P422, DOI 10.1007/s00204-004-0645-1; Reguera Beatriz, 2008, P257; Simon Jean Francois, 1994, Natural Toxins, V2, P293, DOI 10.1002/nt.2620020508; Swanson KM, 2010, HARMFUL ALGAE, V9, P190, DOI 10.1016/j.hal.2009.10.001; TOHDA H, 1993, MUTAT RES, V289, P275, DOI 10.1016/0027-5107(93)90078-T; Tubaro A, 1996, TOXICON, V34, P743, DOI 10.1016/0041-0101(96)00027-X	15	12	12	1	7	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0968-0896	1464-3391		BIOORGAN MED CHEM	Bioorg. Med. Chem.	JUN 15	2012	20	12					3742	3745		10.1016/j.bmc.2012.04.046	http://dx.doi.org/10.1016/j.bmc.2012.04.046			4	Biochemistry & Molecular Biology; Chemistry, Medicinal; Chemistry, Organic	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Pharmacology & Pharmacy; Chemistry	948EN	22608922	Green Accepted			2025-03-11	WOS:000304486500007
J	Nanayakkara, KGN; Alam, AKMK; Zheng, YM; Chen, JP				Nanayakkara, K. G. Nadeeshani; Alam, A. K. M. Khorshed; Zheng, Yu-Ming; Chen, J. Paul			A low-energy intensive electrochemical system for the eradication of <i>Escherichia coli</i> from ballast water: Process development, disinfection chemistry, and kinetics modeling	MARINE POLLUTION BULLETIN			English	Article						Ballast water; E. coli; Electrochemical disinfection; Kinetics modeling	DINOFLAGELLATE CYSTS; INACTIVATION; OZONE; TRANSPORT; RISK	The invasion of biological organisms via ballast water has created threats to the environment and human health. In this study, a cost-effective electrochemical disinfection reactor was developed to inactivate Escherichia coli, one of the IMO-regulated indicator microbes, in simulated ballast water. The complete inactivation of E. coli could be achieved within a very short time (150, 120, or 60 s) with an energy consumption as low as 0.0090, 0.0074 or 0.0035 kWh/m(3) for ballast water containing E. coli at concentrations of 10(8), 10(7) and 10(6) CFU/100 mL, respectively. Electrochemical chlorination was the major disinfection mechanism in chloride-abundant electrolytes, whereas oxidants such as ozone and free radicals contributed to 20% of the disinfection efficiency in chloride-free electrolytes. Moreover, a disinfection kinetics model was successfully developed to describe the inactivation of E. coli. (C) 2012 Elsevier Ltd. All rights reserved.	[Nanayakkara, K. G. Nadeeshani; Alam, A. K. M. Khorshed; Zheng, Yu-Ming; Chen, J. Paul] Natl Univ Singapore, Dept Civil & Environm Engn, Singapore 119260, Singapore; [Alam, A. K. M. Khorshed] Germanischer Lloyd Singapore Pte Ltd, Singapore 239920, Singapore; [Nanayakkara, K. G. Nadeeshani] Inst Fundamental Studies, Kandy, Sri Lanka	National University of Singapore; National Institute of Fundamental Studies (NIFS)	Zheng, YM (通讯作者)，Natl Univ Singapore, Dept Civil & Environm Engn, 10 Kent Ridge Crescent, Singapore 119260, Singapore.	ym-zheng@hotmail.com; paulchen@nus.edu.sg	Chen, J. Paul/ABE-4267-2021; Zheng, Yu-Ming/B-5030-2012	Nanayakkara, Nadeeshani/0000-0002-2204-2063; Zheng, Yu-Ming/0000-0002-3858-1037; Chen, J. Paul/0000-0002-9964-293X	Maritime and Port Authority of Singapore [R-288-000-050-490, R-288-000-050-640, R-288-000-074-490]	Maritime and Port Authority of Singapore	The authors would like to express their appreciation to Maritime and Port Authority of Singapore (R-288-000-050-490, R-288-000-050-640 and R-288-000-074-490) for financial support of this study.	APHA, 1995, Standard methods for the examination of water and wastewater, V19th ed.; Cho M, 2003, APPL ENVIRON MICROB, V69, P2284, DOI 10.1128/AEM.69.4.2284-2291.2003; Deborde M, 2008, WATER RES, V42, P13, DOI 10.1016/j.watres.2007.07.025; Diao M, 2004, PROCESS BIOCHEM, V39, P1421, DOI 10.1016/S0032-9592(03)00274-7; Gregg MD, 2007, HARMFUL ALGAE, V6, P567, DOI 10.1016/j.hal.2006.08.009; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hendricks D.W., 2006, WATER TREATMENT UNIT, P1007; Herwig RP, 2006, MAR ECOL PROG SER, V324, P37, DOI 10.3354/meps324037; Hunt NK, 1999, WATER RES, V33, P2633, DOI 10.1016/S0043-1354(99)00115-3; Jeong J, 2006, ENVIRON SCI TECHNOL, V40, P6117, DOI 10.1021/es0604313; Li XY, 2004, J ENVIRON ENG, V130, P1217, DOI 10.1061/(ASCE)0733-9372(2004)130:10(1217); Li XY, 2002, J ENVIRON ENG-ASCE, V128, P697, DOI 10.1061/(ASCE)0733-9372(2002)128:8(697); Liang WY, 2005, ENVIRON SCI TECHNOL, V39, P4633, DOI 10.1021/es048382m; Matsunaga T, 2000, WATER RES, V34, P3117, DOI 10.1016/S0043-1354(00)00066-X; Nanayakkara KGN, 2011, MAR POLLUT BULL, V63, P119, DOI 10.1016/j.marpolbul.2011.03.003; Nilsen B., 2001, INT MAR ORG 1 INT BA, P126; PATERMARAKIS G, 1990, WATER RES, V24, P1491, DOI 10.1016/0043-1354(90)90083-I; Rigby GR, 1999, MAR ECOL PROG SER, V191, P289, DOI 10.3354/meps191289; Sarkka H, 2008, J HAZARD MATER, V156, P208, DOI 10.1016/j.jhazmat.2007.12.011; STONER GE, 1982, BIOELECTROCH BIOENER, V9, P229, DOI 10.1016/0302-4598(82)80013-5; Taylor MD, 2007, MAR ECOL PROG SER, V350, P41, DOI 10.3354/meps07016	21	24	26	1	58	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0025-326X	1879-3363		MAR POLLUT BULL	Mar. Pollut. Bull.	JUN	2012	64	6					1238	1245		10.1016/j.marpolbul.2012.01.018	http://dx.doi.org/10.1016/j.marpolbul.2012.01.018			8	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	969CG	22483951				2025-03-11	WOS:000306032700032
J	Bravo, I; Vila, M; Casablanca, S; Rodriguez, F; Rial, P; Riobó, P; Penna, A				Bravo, Isabel; Vila, Magda; Casablanca, Silvia; Rodriguez, Francisco; Rial, Pilar; Riobo, Pilar; Penna, Antonella			Life cycle stages of the benthic palytoxin-producing dinoflagellate <i>Ostreopsis</i> cf. <i>ovata</i> (Dinophyceae)	HARMFUL ALGAE			English	Article						Benthic dinoflagellates; Cyst; Harmful algae; Life cycle; Mediterranean Sea; Ostreopsis; Reproduction	GYMNODINIUM-CATENATUM DINOPHYCEAE; PHYTOPLANKTON GROWTH-RATES; DNA-SYNTHESIS CYCLES; SEXUAL REPRODUCTION; GONYAULAX-TAMARENSIS; ALEXANDRIUM-MINUTUM; COOLIA DINOPHYCEAE; MEDITERRANEAN SEA; CULTURE; GAMBIERDISCUS	The asexual and sexual reproduction of Ostreopsis cf. ovata was studied in the field and in cultures isolated from two locations in the Mediterranean Sea. Asexual division took place in the motile stage by the sharing of theca (desmoschisis). High cell-size variability and differences in division capability were detected in the cultures. Thecal analyses and nuclear division patterns allowed characterization of the different phases of dividing cells obtained during an in situ cell-cycle sampling performed off Llavaneres beach (Northeast Spain). During the 45-h cycle, binucleated cells accounted for 2.6% of the population. Division was initiated with the onset of dusk and reached a maximum 3-4 h before dawn. No dividing cells were detected after 09:00 AM. Sexuality occurred both in cultures and in natural populations of O. cf. ovata. Mating gamete pairs were the only sexual stages that could be distinguished from vegetative stages. The differences between these pairs and dividing cells are described herein. None of the individually isolated gamete pairs underwent fusion nor encystment, instead, in most of them one member of the gamete pair divided. Rather than plasmogamy, there was evidence of nuclear migration from one gamete to the other. Pellicle cysts, thin-walled cysts, and thecate cysts were also identified and studied. These cysts, embedded in abundant mucilage in a bloom-derived incubated sample, were able to germinate for as long as 6 months after their formation. Our results suggest that they constitute the overwintering population that causes recurrent blooms of O. cf. ovata in some areas of the Mediterranean Sea. (C) 2012 Elsevier By. All rights reserved.	[Bravo, Isabel; Rodriguez, Francisco; Rial, Pilar; Riobo, Pilar] IEO, CSIC, Unidad Asociada Fitoplancton Tox, Subida Radio Faro 50, Vigo 36390, Spain; [Vila, Magda] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Casablanca, Silvia; Penna, Antonella] Univ Urbino, Dept Biomol Sci, I-61100 Pesaro, Italy	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); University of Urbino	Bravo, I (通讯作者)，IEO, CSIC, Unidad Asociada Fitoplancton Tox, Subida Radio Faro 50, Vigo 36390, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Riobo, Pilar/K-1945-2017; Rodriguez, Francisco/A-5934-2019; Vila, Magda/B-2447-2014	Riobo, Pilar/0000-0002-1921-6229; Rodriguez, Francisco/0000-0002-6918-4771; Bravo, Isabel/0000-0003-3764-745X; Vila, Magda/0000-0002-6855-841X; CASABIANCA, Silvia/0000-0003-2670-5423	Spanish national project EBITOX [CTQ2008-06754-C04-04]	Spanish national project EBITOX	We thank Helena Hojas for her help in the culture and subsequent measurements of Ostreopsis, Amelia Villamarin for providing technical support, and Santiago Fraga for his assistance in elucidate the pattern of dividing cells. Mercedes Masso aboard the sailboat "Rael V" is gratefully acknowledged for the supply of samples from Croatia, and Cecilia Battochi for her assistance in overnight sampling at Llavaneres beach. We are also indebted to the Acena family, from the Restaurant Pins Mar (Sant Andreu de Llavaneres), for kindly offering us the use of their facilities. This work was supported by the Spanish national project EBITOX (CTQ2008-06754-C04-04). We also thank the CCVIEO-Microalgae Culture Collection of Institut Espanol de Oceanografia for providing culture strains.[SS]	Aligizaki K, 2006, HARMFUL ALGAE, V5, P717, DOI 10.1016/j.hal.2006.02.005; 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], P 14 INT C HARMF ALG; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Barone R., 2007, Harmful Algae News, V33, P1; BESADA EG, 1982, B MAR SCI, V32, P723; BHAUD Y, 1988, J CELL SCI, V89, P197; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Cao Vien M., 1967, CR HEBD ACAD SCI, V246, P1006; CARPENTER EJ, 1988, MAR ECOL PROG SER, V43, P105, DOI 10.3354/meps043105; CHANG J, 1991, MAR ECOL PROG SER, V78, P115, DOI 10.3354/meps078115; Ciminiello Patrizia, 2008, P287; Ciminiello P, 2011, TOXICON, V57, P376, DOI 10.1016/j.toxicon.2010.11.002; DODDS WK, 1995, J PHYCOL, V31, P2, DOI 10.1111/j.0022-3646.1995.00002.x; Elbrächter M, 2003, J PHYCOL, V39, P629, DOI 10.1046/j.1529-8817.2003.39041.x; FAUST MA, 1992, J PHYCOL, V28, P94; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2005, J PHYCOL, V41, P74, DOI 10.1111/j.1529-8817.2005.04045.x; Figueroa RI, 2008, AQUAT MICROB ECOL, V52, P13, DOI 10.3354/ame01206; Figueroa RI, 2008, HARMFUL ALGAE, V7, P653, DOI 10.1016/j.hal.2008.02.005; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Galluzzi L, 2004, APPL ENVIRON MICROB, V70, P1199, DOI 10.1128/AEM.70.2.1199-1206.2004; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Garces E, 1997, J PLANKTON RES, V19, P2067, DOI 10.1093/plankt/19.12.2067; Guillard R.R.L., 1973, HDB PHYCOLOGICAL MET, P289; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Guillou L, 2002, PROTIST, V153, P223, DOI 10.1078/1434-4610-00100; Hall T. 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J	Feifel, KM; Moore, SK; Horner, RA				Feifel, Kirsten M.; Moore, Stephanie K.; Horner, Rita A.			An Alexandrium Spp. Cyst Record from Sequim Bay, Washington State, USA, and its Relation to Past Climate Variability	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium; climate change; dinoflagellate cysts; Puget Sound; sea surface temperature; Sequim Bay	HARMFUL ALGAL BLOOMS; PARALYTIC SHELLFISH; PUGET-SOUND; GEODUCK CLAMS; RESTING CYSTS; TOXINS; ACCUMULATION; DINOPHYCEAE; OSCILLATION; CATENELLA	Since the 1970s, Puget Sound, Washington State, USA, has experienced an increase in detections of paralytic shellfish toxins (PSTs) in shellfish due to blooms of the harmful dinoflagellate Alexandrium. Natural patterns of climate variability, such as the Pacific Decadal Oscillation (PDO), and changes in local environmental factors, such as sea surface temperature (SST) and air temperature, have been linked to the observed increase in PSTs. However, the lack of observations of PSTs in shellfish prior to the 1950s has inhibited statistical assessments of longer-term trends in climate and environmental conditions on Alexandrium blooms. After a bloom, Alexandrium cells can enter a dormant cyst stage, which settles on the seafloor and then becomes entrained into the sedimentary record. In this study, we created a record of Alexandrium spp. cysts from a sediment core obtained from Sequim Bay, Puget Sound. Cyst abundances ranged from 0 to 400 cysts . cm-3 and were detected down-core to a depth of 100 cm, indicating that Alexandrium has been present in Sequim Bay since at least the late 1800s. The cyst record allowed us to statistically examine relationships with available environmental parameters over the past century. Local air temperature and sea surface temperature were positively and significantly correlated with cyst abundances from the late 1800s to 2005; no significant relationship was found between PDO and cyst abundances. This finding suggests that local environmental variations more strongly influence Alexandrium population dynamics in Puget Sound when compared to large-scale changes.	[Feifel, Kirsten M.; Horner, Rita A.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Moore, Stephanie K.] NOAA, NW Fisheries Sci Ctr, W Coast Ctr Oceans & Human Hlth, Seattle, WA 98112 USA	University of Washington; University of Washington Seattle; National Oceanic Atmospheric Admin (NOAA) - USA	Feifel, KM (通讯作者)，Univ Washington, Sch Oceanog, Seattle, WA 98195 USA.	kfei04@uw.edu			National Oceanic and Atmospheric Administration [NA04NOS4780273]; West Coast Center for Oceans and Human Health as part of the NOAA Oceans and Human Health Initiative, WCCOHH [39]	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); West Coast Center for Oceans and Human Health as part of the NOAA Oceans and Human Health Initiative, WCCOHH	This research project was funded by the National Oceanic and Atmospheric Administration Coastal Ocean Program under award number #NA04NOS4780273 to the University of Washington. We thank the crew of the R/V Thomas G. Thompson for helping to collect the piston core, J. Postel for helping to section the core, J. Masura for helping with cyst identification, C. Nittrouer for the use of his lab for <SUP>210</SUP>Pb analysis, N. Adams for his cartography skills, and N. Mantua for advice on climate data and the geoduck clam data set. Shellfish toxicity data are used courtesy of the Washington State Department of Health. This publication was also supported in part by the West Coast Center for Oceans and Human Health as part of the NOAA Oceans and Human Health Initiative, WCCOHH publication no. 39. The WCCOHH is part of the National Marine Fisheries Service's Northwest Fisheries Science Center, Seattle, Washington. This is ECOHAB publication 320.	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JUN	2012	48	3					550	558		10.1111/j.1529-8817.2012.01175.x	http://dx.doi.org/10.1111/j.1529-8817.2012.01175.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	952RP	27011070				2025-03-11	WOS:000304810200006
J	Houben, AJP; van Mourik, CA; Montanari, A; Coccioni, R; Brinkhuis, H				Houben, Alexander J. P.; van Mourik, Caroline A.; Montanari, Alessandro; Coccioni, Rodolfo; Brinkhuis, Henk			The Eocene-Oligocene transition: Changes in sea level, temperature or both?	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Sea level; Eocene-Oligocene transition; Organic walled dinoflagellate cysts; Temperature	DINOFLAGELLATE CYSTS; COASTAL-PLAIN; CLIMATE; BIOSTRATIGRAPHY; GREENHOUSE; BOUNDARY; ATLANTIC; MAGNETOSTRATIGRAPHY; ASSEMBLAGES; CALIBRATION	The Eocene-Oligocene Transition (EOT similar to 34 Ma) reflects the onset of major Antarctic glaciation. The primary geochemical signature of the EOT is two similar to 300 kyr spaced shifts in increasing deep-sea oxygen isotope values, possibly reflecting both global cooling a nd/or increasing ice volume. A way to assess the respective contribution of continental ice is to quantify concomitant glacio-eustatic sea level change. This is usually expressed in relatively shallow marine depositional settings. One potentially suitable region is in the Vicentinian Alps, NE Italy, where marginal marine deposits document sea level changes during the;EOT. By correlating stable isotope-, bio- and magnetostratigraphic information between three distant regions, we are able to relate the shallow marine sections to the Pacific oxygen isotope record from Ocean Drilling Program (ODP) Site 1218 of Coxall et al. (2005). Microfacies, sedimentological, and biotic analysis suggests that associated with the first isotope shift (EOT-1) sea level fell similar to 20 m, and with the ultimate shift, the Oligocene Isotope Event 1 (Oi-1) sea level fell some 50-60 m. Distribution patterns of temperature sensitive dinoflagellates from a coeval central Italian section reveal that the early stages of the EOT were accompanied by sea surface cooling, whereas no sustained cooling is noted in association with the Oi-1. This suggests that the initial EOT shift(s) reflect a mixed signal of ice volume and temperature whereas the Oi-1 primarily reflects expansion of the Antarctic cryosphere. (c) 2011 Elsevier B.V. All rights reserved.	[Houben, Alexander J. P.; Brinkhuis, Henk] Univ Utrecht, Lab Palaeobot & Palynol, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; [van Mourik, Caroline A.] Univ Stockholm, Dept Geol & Geochem, S-10691 Stockholm, Sweden; [Montanari, Alessandro] Osservatorio Geol Coldigioco, I-62020 Frontale Di Apiro, Italy; [Coccioni, Rodolfo] Univ Urbino, Inst Geol, I-61209 Urbino, Italy; [Coccioni, Rodolfo] Univ Urbino, Ctr Geobiol, I-61209 Urbino, Italy	Utrecht University; Stockholm University; University of Urbino; University of Urbino	Houben, AJP (通讯作者)，Univ Utrecht, Lab Palaeobot & Palynol, Inst Environm Biol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	A.J.P.Houben@uu.nl	Brinkhuis, Henk/IUO-8165-2023	Brinkhuis, Henk/0000-0003-0253-6610; COCCIONI, Rodolfo/0000-0003-2333-4030; Houben, Alexander/0000-0002-9497-1048	Statoil	Statoil	Statoil is greatly acknowledged for financial support. Discussions with Lucas Lourens, Frits Hilgen, Ben Slotnick, Stephen Schellenberg and Heiko Palike are much appreciated. We are grateful to Helen Coxall and Bridget Wade for their very constructive reviews.	Adams C.G., 1986, TERMINAL EOCENE EVEN, P237; [Anonymous], 1989, S.E.P.M. Spec. 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Paleoclimatol. Paleoecol.	JUN 1	2012	335				SI		75	83		10.1016/j.palaeo.2011.04.008	http://dx.doi.org/10.1016/j.palaeo.2011.04.008			9	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	960HM					2025-03-11	WOS:000305378600010
J	Riding, JB				Riding, James B.			The Jurassic dinoflagellate cyst <i>Gonyaulacysta dentata</i> (Raynaud 1978) Lentin & Vozzhennikova 1990 emend. nov.: An index species for the Late Callovian to earliest Oxfordian of the northern hemisphere	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Dinoflagellate cysts; Biostratigraphy; Palaeobiology; Provincialism; Mid-Late Jurassic; Northern hemisphere	MIDDLE; BASIN; BIOSTRATIGRAPHY; RUSSIA; SEA	Gonyaulacysta dentata is a very large and morphologically distinctive dinoflagellate cyst species which was first described from the Callovian (Middle Jurassic) strata of the Isle of Skye, northwest Scotland. The diagnosis and description of this species are emended herein in order to document the characteristic elongate pentagonal outline, the apicular structure, the bicavate cyst organisation, the prominent dorsal and lateral sutural crests which are typically denticulate, the discontinuous, low-relief midventral sutural ridges and the lack of a periarchaeopyle. Gonyaulacysta dentata is a reliable index taxon for the Late Callovian to earliest Oxfordian (Peltoceras athleta to Quenstedtoceras mariae zones) of the Boreal Realm and the Subboreal Province in the northern hemisphere. It is especially prominent in the Boreal Realm and the northern part of the Subboreal Province, and has been recorded from the Barents Sea region, arctic Canada, offshore Norway, the central and northern North Sea and northern Scotland. Typically this species represents a relatively low proportion of the overall dinoflagellate cyst assemblages. There are also reports of very rare specimens of Gonyaulacysta dentata from further south in the Northwest European Subprovince, i.e. France, Germany and Poland. It therefore appears to be a characteristic Boreal taxon, but low numbers migrated southwards into the Northwest European Subprovince due to a fall in palaeotemperatures during the Callovian-Oxfordian transition. The southwards expansion of this short-lived species parallels the southward migration of the Boreal ammonite family Cardioceratidae. There is a virtually mutually exclusive relationship between the Arctic species Gonyaulacysta dentata and the apparently warm-loving taxon Scriniodinium crystallinum during the Late Callovian to Early Oxfordian interval. This is consistent with the interpretation of Gonyaulacysta dentata as a cold water taxon. (C) 2012 Natural Environment Research Council. Published by Elsevier B.V. All rights reserved.	British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk			NERC [bgs05004] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Abbink O, 2001, GLOBAL PLANET CHANGE, V30, P231, DOI 10.1016/S0921-8181(01)00101-1; Andersen S.Th., 1960, DANMARKS GEOLOGISKE, VIV; [Anonymous], 1978, GEOLOGICAL SCI; ARHUS N, 1989, NORSK GEOL TIDSSKR, V69, P39; Arkell WJ, 1957, TREATISE INVERTEBR L; Beju D., 1971, ANN I GEOLOGICI PUBL, V54, P276; Beju D., 1982, PALYNOLOGY, V6, P273; Birkenmajer Krzysztof, 2007, Studia Geologica Polonica, V127, P51; Brideaux W.W., 1976, GEOLOGICAL SURVEY CA, V259; Bruch A., 1999, FOSSIL PLANTS SPORES, P26; CARIOU E, 1973, ATLAS PALAEOBIOGEOGR, P287; Cecca F, 2005, PALAEOGEOGR PALAEOCL, V222, P10, DOI 10.1016/j.palaeo.2005.03.009; Cushing EJ., 1961, Pollen et Spores, V3, P265; Davies E.H., 1983, GEOLOGICAL SURVEY CA, V359; Deflandre G., 1938, TRAVAUX STATION ZOOL, V13, P147; DIMTER A, 1990, PALAEOGEOGR PALAEOCL, V80, P173, DOI 10.1016/0031-0182(90)90131-P; Dromart G, 2003, EARTH PLANET SC LETT, V213, P205, DOI 10.1016/S0012-821X(03)00287-5; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fensome R.A., 1979, GRONLANDS GEOLOGISKE, V132; Gedl P, 2008, NEUES JAHRB GEOL P-A, V247, P209, DOI 10.1127/0077-7749/2008/0247-0209; Gedl Przemyslaw, 2008, Studia Geologica Polonica, V131, P7; Harding IC, 2011, REV PALAEOBOT PALYNO, V167, P82, DOI 10.1016/j.revpalbo.2011.07.002; Helenes Javier, 1997, Palynology, V21, P173; Herngreen G.F.W., 2000, MEDEDELINGEN NEDERLA, V63; Hesketh RAP, 2002, MAR PETROL GEOL, V19, P541, DOI 10.1016/S0264-8172(02)00026-0; Huault V, 1999, REV PALAEOBOT PALYNO, V107, P145, DOI 10.1016/S0034-6667(99)00021-4; Iosifova EK, 1996, REV PALAEOBOT PALYNO, V91, P187, DOI 10.1016/0034-6667(95)00064-X; Jenkyns HC, 2002, J GEOL SOC LONDON, V159, P351, DOI 10.1144/0016-764901-130; JOHNSON C D, 1973, Bulletin of Canadian Petroleum Geology, V21, P178; KUNZ R, 1990, Palaeontographica Abteilung B Palaeophytologie, V216, P1; LENTIN JK, 1990, AM ASS STRATIGRAPHIC, V23; LUND J J, 1985, Bulletin of the Geological Society of Denmark, V33, P371; MASURE E., 1986, B CTR RECHERCHES EXP, V12; Piasecki S., 1980, Middle to Late Jurassic dinoflagellate cyst stratigraphy from Milne Land and Jameson Land (East Greenland) correlated with ammonite stratigraphy; Piasecki Stefan, 2004, Geological Survey of Denmark and Greenland Bulletin, V5, P99; Piasecki Stefan, 2004, Geological Survey of Denmark and Greenland Bulletin, V5, P89; Piasecki Stefan, 2004, Geological Survey of Denmark and Greenland Bulletin, V5, P73; Poulsen N.E., 1985, Arsskrift for Dansk Geologisk Forening, V1984, P133; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; 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, 1990, Palynology, V14, P216; Riding J.B., 1982, Journal of Micropalaeontology, V1, P13; Riding J.B., 1987, Proceedings of the Yorkshire Geological Society, V46, P231; Riding J.B., 1993, LITHOSTRATIGRAPHIC N, pA1; Riding J.B., 1999, AM ASS STRATIGRAPHIC, V36; Riding JB, 2005, PALYNOLOGY, V29, P87, DOI 10.2113/29.1.87; Riding James B., 2002, Palynology, V26, P5, DOI 10.2113/0260005; Riding JB, 2011, REV PALAEOBOT PALYNO, V167, P212, DOI 10.1016/j.revpalbo.2011.07.008; Riding James B., 1999, Palynology, V23, P15; Riding JB, 2011, REV PALAEOBOT PALYNO, V163, P227, DOI 10.1016/j.revpalbo.2010.10.009; Riding JB, 2010, REV PALAEOBOT PALYNO, V162, P543, DOI 10.1016/j.revpalbo.2010.07.008; Riding JB, 1997, SCOT J GEOL, V33, P59, DOI 10.1144/sjg33010059; Sellwood BW, 2008, P GEOLOGIST ASSOC, V119, P5, DOI 10.1016/S0016-7878(59)80068-7; SMELROR M, 1988, REV PALAEOBOT PALYNO, V56, P275, DOI 10.1016/0034-6667(88)90061-9; SMELROR M, 1993, PALAEOGEOGR PALAEOCL, V102, P121, DOI 10.1016/0031-0182(93)90009-8; Smelror M., 1988, Gronlands Geologiske Undersogelse Rapport, V137, P135, DOI [DOI 10.34194/RAPGGU.V137.8019, 10.34194/rapggu.v137.8019]; Smelror M., 1991, Revista Espanola de Micropaleontologia, V23, P47; SMELROR M., 1992, NPF SPECIAL PUBLICAT, P495; Smith AG., 1994, ATLAS CENOZOIC MESOZ; Smith G.A., 1999, THESIS U BRISTOL UK; Stancliffe R. 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J	Mohamed, O; Piller, WE; Egger, H				Mohamed, Omar; Piller, Werner E.; Egger, Hans			The dinocyst record across the Cretaceous/Palaeogene boundary of a bathyal mid-latitude Tethyan setting: Gosau Group, Gams Basin, Austria	CRETACEOUS RESEARCH			English	Article						Eastern Alps; Dinocysts; Palynofacies; Biostratigraphy; Maastrichtian; Danian	CRETACEOUS-TERTIARY BOUNDARY; STABLE-ISOTOPE STRATIGRAPHY; NORTHERN CALCAREOUS ALPS; MASS EXTINCTION; DINOFLAGELLATE CYST; EL-KEF; PALEOGENE BOUNDARY; EASTERN ALPS; NEW-ZEALAND; SECTION	A high-resolution palynological study carried out across the Cretaceous/Palaeogene (K/Pg) boundary in two sections (Knappengraben and Gamsbach) of the Gosau Group near Gams (Gams Basin, Northern Calcareous Alps, Austria) has identified over 178 dinoflagellate species and subspecies from 89 rock samples. In most samples, the dinocysts are moderately well to well preserved, but associated with reworked material. Some well-known marker species around the K/Pg boundary, such as Carpatella cornuta, Spongodinium delitiense, Trithyrodinium evittii, Palynodinium grallator, Manumiella druggii, Cordosphaeridium fibrospinosum, Membranilarnacia? tenella, Senoniasphaera inornata, Damassadinium californicum, and Dinogymnium acuminatum have been recorded from the samples studied. In addition to these, Trabeculidinium quinquetrum, Lejeunecysta izerzenensis, Batiacasphaera rifensis, Impagidinium maghribensis and Cyclonophelium compactum represent local markers. A Spongodinium delinense acme is recorded in both sections above the K/Pg boundary and is interpreted to indicate a transient cooling event of oceanic surface waters. The stratigraphic distribution of the dinocyst species indicates that they were not seriously affected by the mass extinction event at the K/Pg boundary, but their diversity slightly increases above it. The composition of the assemblages, however, changes drastically. Six dinocyst assemblages and four palynofacies assemblages were identified by means of cluster analysis. Their distribution does not show any regular pattern. The increase of phytoclasts in the Danian clearly indicates enhanced terrestrially derived input into the basin. The palynological and sedimentological differences between the two sections can be explained by small scale local lateral variations. (C) 2011 Elsevier Ltd. All rights reserved.	[Mohamed, Omar; Piller, Werner E.] Graz Univ, Inst Earth Sci Geol & Palaeontol, A-8010 Graz, Austria; [Mohamed, Omar] Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt; [Egger, Hans] Geol Survey Austria, A-1030 Vienna, Austria	University of Graz; Egyptian Knowledge Bank (EKB); Minia University	Mohamed, O (通讯作者)，Graz Univ, Inst Earth Sci Geol & Palaeontol, Heinrichstr 26, A-8010 Graz, Austria.	omaraosman@yahoo.com		Piller, Werner E./0000-0003-2808-4720	Ministry of Higher Education of Egypt	Ministry of Higher Education of Egypt(Ministry of Higher Education & Scientific Research (MHESR))	We are indebted to Paul Schioler (Lower Hutt) and Vivi Vajda (Lund) for their helpful and constructive reviews. Thanks go to the staff of the geochemical laboratory of the Institute of Earth Sciences at Graz University. Hugh Rice corrected the English of the original manuscript. Omar Mohamed thanks the Ministry of Higher Education of Egypt for funding this study which is part of his PhD thesis.	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Surv. Rec, V20, P8	77	17	18	0	11	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	JUN	2012	35						143	168		10.1016/j.cretres.2011.12.007	http://dx.doi.org/10.1016/j.cretres.2011.12.007			26	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	911YQ					2025-03-11	WOS:000301761000012
J	Ivanova, EV; Murdmaa, IO; Karpuk, MS; Schornikov, EI; Marret, F; Cronin, TM; Buynevich, IV; Platonova, EA				Ivanova, Elena V.; Murdmaa, Ivar O.; Karpuk, Maria S.; Schornikov, Eugene I.; Marret, Fabienne; Cronin, Thomas M.; Buynevich, Ilya V.; Platonova, Elena A.			Paleoenvironmental changes on the northeastern and southwestern Black Sea shelves during the Holocene	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	6th IGCP 521 Plenary Meeting on Caspian-Black Sea-Mediterranean Corridors During the Last 30 ka - Sea Level Change and Human Adaptive Strategies	SEP 27-OCT 05, 2010	GREECE	Hydrobiol Stn Rhodes, Hellen Ctr Marine Res, Avalon Inst Appl Sci			DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; LATE PLEISTOCENE; MARMARA; LEVEL; ASSEMBLAGES; SALINITY; AGE; RECONNECTION; CALIBRATION	Four paleoceanographic events are distinguished during the Holocene based on changes in macro- and microfossil assemblages studied from three sediment cores (Ak 521, 522, 2571) from the outer northeast shelf and from core MAR02-45 situated on the southwest shelf of the Black Sea, west to the Bosphorus. The lithology and fossils were previously studied from cores Ak 521 and Ak 522 and MAR02-45. However, high resolution ostracod analyses from the AMS-C-14 dated core, Ak 2571, allowed for a revision of the taxonomy and paleoecological interpretation of this microfaunal group on the NE shelf. Downcore changes in the relative abundance of the polyhaline ostracods are found to be contemporaneous in all three cores from the NE shelf. As a result, centennial-millennial scale fluctuations of the bottom-water salinity are resolved in the area. A broader scale examination of paleoenvironmental changes between the NE and SW shelves is also made and the surface to bottom salinity gradient is discussed. An uncalibrated radiocarbon based chronology is used throughout this paper to facilitate comparison with the regional chronostratigraphy of marine transgression and regressions in the Black Sea. The calibrated ages corrected for the changes in reservoir age through the Holocene are also provided. The first paleoceanographic event is associated with the pulse of Mediterranean water previously established at about 9.8-9.3 ka BP. This event is clearly observed in the SW region but not on the NE shelf due to a hiatus in the longest core, Ak 521. The second event is represented on both the NE and SW shelves as a replacement of brackish benthic fauna and surface phytoplankton with marine ones between 8.4 and 6.9 ka BP, indicating a gradual increase in salinity. The third event is marked by opposing trends in surface and bottom-water salinity changes. On the NE shelf, bottom-water salinity rose to modern values by similar to 6.5 ka BP and then decreased within the interval similar to 6.4-5.3 ka BP as recorded by the ostracod assemblages. On the SW shelf, surface-water salinity reached modern values by 5.6 ka BP and remained constant until present day as inferred from the dinoflagellate cyst assemblages. The fourth event is marked by a recurring increase in bottom-water salinity to modern values indicated by the polyhaline ostracod assemblages at similar to 5.3 ka BP in the NE region, after which only minor salinity fluctuations are observed. (C) 2011 Elsevier Ltd and INQUA. All rights reserved.	[Ivanova, Elena V.; Murdmaa, Ivar O.] RAS, Shrshov Inst Oceanol, Moscow 117997, Russia; [Karpuk, Maria S.; Platonova, Elena A.] Moscow MV Lomonosov State Univ, Geol Fac, Moscow 119992, Russia; [Schornikov, Eugene I.] AV Zhirmunsky Inst Marine Biol, Far E Div RAS, Vladivostok 690041, Russia; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Cronin, Thomas M.] US Geol Survey, Natl Ctr 926A, Reston, VA 20191 USA; [Buynevich, Ilya V.] Temple Univ, Dept Earth & Environm Sci, Philadelphia, PA 19122 USA	Russian Academy of Sciences; Shirshov Institute of Oceanology; Lomonosov Moscow State University; Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences; University of Liverpool; United States Department of the Interior; United States Geological Survey; Pennsylvania Commonwealth System of Higher Education (PCSHE); Temple University	Ivanova, EV (通讯作者)，RAS, Shrshov Inst Oceanol, 36 Nakhimovsky Prosp, Moscow 117997, Russia.	e_v_ivanova@ocean.ru; murdmaa@mail.ru; mashita@mail.ru; eschornikov@yandex.ru; f.marret@liv.ac.uk; tcronin@usgs.gov; coast@temple.edu; ep081@uow.edu.au	Murdmaa, Ivar/T-3538-2017; Ivanova, Elena/B-3775-2016; Karpuk, Maria/S-2255-2017	BUYNEVICH, ILYA/0000-0002-3840-0208; Karpuk, Maria/0000-0003-4739-7554; Marret-Davies, Fabienne/0000-0003-4244-0437				Agalarova D.A., 1961, OSTRAKODY PLIOTSENOV; Aksu AE, 2002, MAR GEOL, V190, P61, DOI 10.1016/S0025-3227(02)00343-2; Algan O., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P603; Athersuch J., 1989, SYNOPSES BRIT FAUNA, V43, DOI [10.1017/s0025315400059178, DOI 10.1017/S0025315400059178]; Bahr A, 2008, GEOCHEM GEOPHY GEOSY, V9, DOI 10.1029/2007GC001683; Balabanov I., 2009, PALEOGEOGRAFICHESKIE; Balabanov I.P., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P711; Ballard RD, 2000, MAR GEOL, V170, P253, DOI 10.1016/S0025-3227(00)00108-0; Bogatko ON, 1979, KOMPLEKSNYE ISSLEDOV, P25; Boomer I, 2010, J MICROPALAEONTOL, V29, P119, DOI 10.1144/0262-821X10-003; Brückner H, 2010, QUATERN INT, V225, P160, DOI 10.1016/j.quaint.2008.11.016; Chepalyga A.L., 2002, RAZVITIE LANDSHAFTOV, P205; Chepalyga A. 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Int.	MAY 30	2012	261						91	104		10.1016/j.quaint.2011.11.015	http://dx.doi.org/10.1016/j.quaint.2011.11.015			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	950ZN					2025-03-11	WOS:000304690500009
J	Le Herisse, A; Masure, E; Javaux, EJ; Marshall, CP				Le Herisse, Alain; Masure, Edwige; Javaux, Emmanuelle J.; Marshall, Craig P.			THE END OF A MYTH: <i>ARPYLORUS ANTIQUUS</i> PALEOZOIC DINOFLAGELLATE CYST	PALAIOS			English	Article							BIOSTRATIGRAPHY; ACRITARCHS	Arpylorus antiquus, erected by Calandra in 1964, was isolated from upper Silurian sedimentary rocks from the Mechiguig 1 borehole in southern Tunisia, with other palynomorphs. The folded vesicle and the quadrangular form of the aperture break down into platelike fragments, resembling the tabulation of dinoflagellates. The presence of these elements has been used to interpret A. antiquus as a dinoflagellate cyst. The morphology and affinity of A. antiquus is reinterpreted herein based on investigation of larger sets of samples, including material from the type locality, together with material of Algeria, Saudi Arabia, and Brazil. More complete specimens than those previously described have been observed using gentle laboratory techniques, showing a large development of a fine membrane at the periphery of vesicles. This element was destroyed using classical palynological treatments, implying that the holotype is an incomplete specimen. The membrane at the periphery of vesicles and dorsoventral differentiation of these vesicles suggest that A. antiquus is a part of a more complex biological structure. We suggest a possible relationship with eurypterids, arthropods related to phyllocarids, represented by abundant fragments in the assemblages. Arpylorus antiquus is possibly a structure of storage. The chemical composition of A. antiquus using a Fourier transform infrared FTIR microspectroscopy analysis, reveals a wall composed of biopolymer that is not consistent with dinosporin. We conclude that Arpylorus antiquus is definitively not a dinoflagellate cyst. Although dinoflagellates may have older Paleozoic or even Proterozoic ancestors as the biomarker record may suggest, the dinoflagellate tabulation evolved only in the early Mesozoic.	[Le Herisse, Alain] Univ Brest, UMR CNRS 6538, IUEM, F-29238 Brest, France; [Masure, Edwige] Univ Paris 06, CR2P, UMR CNRS 7207, F-75005 Paris, France; [Javaux, Emmanuelle J.] Univ Liege, Dept Geol, B-4000 Liege 1, Belgium; [Marshall, Craig P.] Univ Kansas, Dept Geol, Lawrence, KS 66045 USA	Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Sorbonne Universite; University of Liege; University of Kansas	Le Herisse, A (通讯作者)，Univ Brest, UMR CNRS 6538, IUEM, CS 93837,6 Ave Gorgeu, F-29238 Brest, France.	alain.le.herisse@univ-brest.fr; edwige.masure@upmc.FR; EJ.Javaux@ulg.ac.be; cpmarshall@ku.edu						[Anonymous], 1985, SPOROPOLLENIN DINOFL; Braddy SJ, 1997, ZOOL J LINN SOC-LOND, V120, P435; Breuer Pierre, 2005, Carnets de Geologie, P3; BUJAK JP, 1981, CAN J BOT, V59, P2077, DOI 10.1139/b81-270; BUJAK JP, 1983, AM ASS STRATIGRAPHIC, V13; BURET M.B, 1990, THESIS U P M CURIE P; CALANDRA F, 1964, CR HEBD ACAD SCI, V258, P4112; Cocks LRM, 2002, J GEOL SOC LONDON, V159, P631, DOI 10.1144/0016-764901-118; Engel MS, 2004, NATURE, V427, P627, DOI 10.1038/nature02291; Evitt W.R., 1967, STANFORD U PUBIS GEO, V10, P1; Fensome R. A., 1993, CLASSIFICATION LIVIN; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Jansson IM, 2008, ALCHERINGA, V32, P285, DOI 10.1080/03115510802096226; JARDINE S, 1974, REV PALAEOBOT PALYNO, V18, P99, DOI 10.1016/0034-6667(74)90012-8; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Labandeira C, 2007, INSECT SCI, V14, P259, DOI 10.1111/j.1744-7917.2007.00152.x; Le Hérissé A, 2002, REV PALAEOBOT PALYNO, V118, P359, DOI 10.1016/S0034-6667(01)00123-3; Le Herisse A, 2001, SECAO EXPLORACAO PET, V20, P117; LE HERISSE A., 2000, 10 INT PAL C NANJ NA, P88; LOBOZIAK S, 1992, REV PALAEOBOT PALYNO, V74, P193, DOI 10.1016/0034-6667(92)90007-4; MANNING PL, 1995, PALAEONTOLOGY, V38, P287; Marshall CP, 2005, PRECAMBRIAN RES, V138, P208, DOI 10.1016/j.precamres.2005.05.006; Massa D., 1988, Paleozoique de Libye occidentale, stratigraphie paleogeographie; MCGREGOR DC, 1978, CAN J EARTH SCI, V15, P1292, DOI 10.1139/e78-136; PARIS F, 1978, ANN MINES BELG, P193; PLOTNICK R.E, 1996, AM PALEONTOLOGIST, V4, P1; REGALI MDP, 1986, MICROPALEONTOLOGY, V32, P163; SARJEANT W A S, 1978, Palynology, V2, P167; Spina A, 2009, PALAEOGEOGR PALAEOCL, V282, P1, DOI 10.1016/j.palaeo.2009.08.001; Steemans P, 2010, REV PALAEOBOT PALYNO, V162, P577, DOI 10.1016/j.revpalbo.2010.07.006; STOVER L.E., 1978, STANDFORD U PUBLICAT, V15; STUMP TE, 1995, REV PALAEOBOT PALYNO, V89, P5, DOI 10.1016/0034-6667(95)00038-Y; VERNIERS J, 1995, GEOL MAG, V132, P651, DOI 10.1017/S0016756800018896; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	34	12	14	0	20	SEPM-SOC SEDIMENTARY GEOLOGY	TULSA	6128 EAST 38TH ST, STE 308, TULSA, OK 74135-5814 USA	0883-1351	1938-5323		PALAIOS	Palaios	MAY-JUN	2012	27	5-6					414	423		10.2110/palo.2011.p11-110r	http://dx.doi.org/10.2110/palo.2011.p11-110r			10	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	972UB		Green Submitted			2025-03-11	WOS:000306304900014
J	Scalco, E; Brunet, C; Marino, F; Rossi, R; Soprano, V; Zingone, A; Montresor, M				Scalco, Eleonora; Brunet, Christophe; Marino, Francesca; Rossi, Rachele; Soprano, Vittorio; Zingone, Adriana; Montresor, Marina			Growth and toxicity responses of Mediterranean <i>Ostreopsis</i> cf. <i>ovata</i> to seasonal irradiance and temperature conditions	HARMFUL ALGAE			English	Article						Growth rates; HABs; Mediterranean Sea; Ostreopsis cf. ovata; Palytoxins; Photophysiology	COOLIA DINOPHYCEAE; PUTATIVE PALYTOXIN; AEGEAN SEA; DINOFLAGELLATE; PROLIFERATION; PHOTOPERIOD; MACROALGAE; ANALOGS; CARBON; CYSTS	The genus Ostreopsis includes several species capable of producing various palytoxin-like compounds which have harmful effects on humans and marine fauna. Species in this genus are regular members of the epiphytic community in tropical seas but their geographic range have shown an apparent expansion towards temperate regions in recent years. This is the case of the Mediterranean Sea, where Ostreopsis cf. ovata is responsible for intense blooms in summer and autumn. With the aim of describing the growth performances of O. cf. ovata, we carried out a multifactorial experiment in which strains isolated from 3 locations along the Italian coast were grown at different combinations of temperature, daylength and irradiance encompassing different seasonal conditions. Temperature constiained growth of O. cf. ovata within a window of 18-30 degrees C, while best performances were recorded at 22 and 26 degrees C. Growth was maximum at 12 h daylength, whereas it was limited by photon flux density at short daylength (9 h) and often showed photosaturation at the longest daylength (15 h). Cells with anomalous shape were found during the exponential phase at the lowest and highest temperatures, while cells with a reduced size were produced at all conditions except 18 degrees C. Total toxin concentration varied between the different environmental conditions and between exponential and post-exponential growth phases without a clear pattern, whereas toxin composition was less variable. Our results suggest that O. cf. ovata is adapted to intermediate temperatures and daylength conditions such as those recorded in the natural environment at the beginning of summer and/or at the beginning of autumn, when this dinoflagellate builds up its biomass along the coast of the Mediterranean Sea. Photosaturation instead occurs at the highest temperature and irradiance conditions, thus supporting the observations of generally lower cell abundances in late July-August. (C) 2012 Elsevier B.V. All rights reserved.	[Scalco, Eleonora; Brunet, Christophe; Marino, Francesca; Zingone, Adriana; Montresor, Marina] Stn Zool Anton Dohrn, I-80121 Naples, Italy; [Rossi, Rachele; Soprano, Vittorio] Ist Zooprofilatt Sperimentale Mezzogiorno, I-80055 Portici, Italy	Stazione Zoologica Anton Dohrn; IZS del Mezzogiorno	Montresor, M (通讯作者)，Stn Zool Anton Dohrn, Villa Comunale, I-80121 Naples, Italy.	marina.montresor@szn.it	brunet, christophe/AAD-7817-2021; Rossi, Rachele/AAS-9093-2021; Rossi, Rachele/N-5225-2015; Zingone, Adriana/E-4518-2010	Montresor, Marina/0000-0002-2475-1787; Rossi, Rachele/0000-0002-7570-2934; Zingone, Adriana/0000-0001-5946-6532	project 'Ostreopsis ovata e Ostreopsis spp.: nuovi rischi di tossicita microalgale nei mani italiani'; Ministero dell'Ambiente e della Tutela del Territorio e del Mare; project 'Monitoraggio di Ostreopsis ovata lungo le caste della regione Campania'; Regione Campania; Ministero della Salute; project 'Una nuova tossina nelle acque della Campania e del Mediterraneo, l'ovatossina: strategie analitiche e di protezione della salute e della sicurezza alimentare' [IZS-ME 03/07]	project 'Ostreopsis ovata e Ostreopsis spp.: nuovi rischi di tossicita microalgale nei mani italiani'; Ministero dell'Ambiente e della Tutela del Territorio e del Mare; project 'Monitoraggio di Ostreopsis ovata lungo le caste della regione Campania'; Regione Campania(Regione Campania); Ministero della Salute(Ministry of Health, Italy); project 'Una nuova tossina nelle acque della Campania e del Mediterraneo, l'ovatossina: strategie analitiche e di protezione della salute e della sicurezza alimentare'	The authors thank Antonella Penna (University of Urbino, Italy) for the genetic characterization of the strains and for providing strain CBA-T; Marina Monti (National Institute of Oceanography and Applied Geophysics, Trieste, Italy) for providing strain OS2T; Carmen Minucci and Gandi Forlani (SZN) for help in culture maintenance. E.S. was supported by the project 'Ostreopsis ovata e Ostreopsis spp.: nuovi rischi di tossicita microalgale nei mani italiani' funded by Ministero dell'Ambiente e della Tutela del Territorio e del Mare; F.M. and R.R. were supported by the project 'Monitoraggio di Ostreopsis ovata lungo le caste della regione Campania' funded by Regione Campania; V.S. by the project IZS-ME 03/07 'Una nuova tossina nelle acque della Campania e del Mediterraneo, l'ovatossina: strategie analitiche e di protezione della salute e della sicurezza alimentare' funded by Ministero della Salute.[SS]	Aligizaki K., 2010, 14 INT C HARMF ALG C, P25; Aligizaki K, 2008, TOXICON, V51, P418, DOI 10.1016/j.toxicon.2007.10.016; Aligizaki K, 2006, HARMFUL ALGAE, V5, P717, DOI 10.1016/j.hal.2006.02.005; [Anonymous], 2002, Identifying Harmful Marine Dinoflagellates; [Anonymous], 2003, Biol Ambient, DOI DOI 10.1021/AC060250J; Barone R., 2006, NATURALISTA SICILIAN, VIV, P401; BESADA EG, 1982, B MAR SCI, V32, P723; Brand L. 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J	Richerol, T; Pienitz, R; Rochon, A				Richerol, Thomas; Pienitz, Reinhard; Rochon, Andre			Modern dinoflagellate cyst assemblages in surface sediments of Nunatsiavut fjords (Labrador, Canada)	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Dinocysts; Nunatsiavut; Labrador; Fjord; Subarctic; Climate; Pollution; Surface sediments; Palynology	NORTHERN NORTH-ATLANTIC; LAST GLACIAL MAXIMUM; BEAUFORT SEA CANADA; HYDROGRAPHIC CONDITIONS; SOUTHEASTERN LABRADOR; VEGETATIONAL HISTORY; MEDITERRANEAN SEA; PCB CONTAMINATION; VANCOUVER-ISLAND; ECOLOGICAL ROLES	In order to document long-term climate cycles and predict future climate trends for the Arctic, geological records archived in ocean sediments can help establish the link between historical and pre-historical sea-surface parameters. Dinoflagellate cysts (dinocysts) are used as proxy indicators of sea-surface parameters (temperature, salinity, sea-ice cover, primary productivity) jointly with transfer functions and a modern dinocyst reference database, to reconstruct the evolution of sea-surface conditions at decadal and millennial timescales. Here we present the surface distribution of recent dinocyst assemblages in 13 surface samples collected in four Nunatsiavut fjords (northern Labrador, Canada) along a latitudinal gradient, and their relationship with various environmental and biological parameters. Dinocyst concentrations in surface sediments increased from the inner to the outer part of each fjord and also from the northernmost to the southernmost fjords. There was also a southward increase in the species diversity with an occurrence and a dominance of cysts from autotrophic dinoflagellates. The presence of cysts of the calcareous dinoflagellate species Scrippsiella cf. S. crystallina in Anaktalak Fjord, where mining activities are underway, appears to be an indicator of human-related pollution within the fjord. (C) 2012 Elsevier B.V. All rights reserved.	[Richerol, Thomas; Pienitz, Reinhard] Univ Laval, Lab Paleoecol Aquat, Ctr Etud Nord, Quebec City, PQ G1V 0A6, Canada; [Rochon, Andre] Univ Quebec, Lab Palynol Marine & Etud Phytoplancton Marin, Inst Sci Mer ISMER, Rimouski, PQ G5L 3A1, Canada	Laval University; University of Quebec	Richerol, T (通讯作者)，Univ Laval, Lab Paleoecol Aquat, Ctr Etud Nord, 2405 Rue Terrasse,Pavillon Abitibi Price, Quebec City, PQ G1V 0A6, Canada.	thomas.richerol.1@ulaval.ca	RICHEROL, Thomas/G-4598-2017	RICHEROL, Thomas/0000-0001-5295-0022; Pienitz, Reinhard/0000-0002-3613-1673	Natural Sciences and Engineering Research Council of Canada (NSERC); Center of Excellence ArcticNet; Nunatsiavut Government	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Center of Excellence ArcticNet; Nunatsiavut Government	This work was funded through grants from the Natural Sciences and Engineering Research Council of Canada (NSERC) and Center of Excellence ArcticNet awarded to Reinhard Pienitz and Andre Rochon, as well as through funding from the Nunatsiavut Government. We wish to thank the officers and crew of the CCGS Amundsen for their help and support during sediment sampling. We also wish to express our gratitude to the people who helped with the collection and analysis of the surface samples: Peter Hulse and Lina Stolze, Memorial University of Newfoundland: Tanya Brown, Royal Military College; Etienne Faubert, Lise Durantou-Munoz and Anne Fontaine, ISMER-UQAR: Nicolas Rolland, LPA-CEN Universite Laval; Marie-Josee Martineau, Universite Laval. Finally we are grateful to the editor of Marine Micropaleontology Richard Jordan, Kari Grosfjeld and one anonymous reviewer for helpful comments, as well as to the Ocean Mapping Group from the University of New Brunswick and to Josee Michaud from ArcticNet, Anne Beaudoin, Emmanuel L'Herault and Andree-Sylvie Carbonneau from CEN-Universite Laval for the help provided to process the new data obtained in order to enhance our manuscript.	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J	Quaijtaal, W; Brinkhuis, H				Quaijtaal, Willemijn; Brinkhuis, Henk			<i>Pentadinium alabamensis</i>: A new, unusual dinoflagellate from the early Oligocene of the Gulf Coast, Alabama, USA	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						organic walled dinoflagellate cysts; Eocene/Oligocene transition; St. Stephens Quarry; Alabama; USA	LATE EOCENE; GLOBAL CLIMATE; NORTH-SEA; TRANSITION; CYSTS; BIOSTRATIGRAPHY; STRATIGRAPHY; SEDIMENTS; DINOCYST; LEVEL	The Eocene-Oligocene Transition (EOT, similar to 34 Ma) marks the onset of major Antarctic ice sheets. The environmental consequences of the transition included major changes in e.g., sea level, temperature, and ocean circulation, complicating biostratigraphic correlations in this interval. Organic walled dinoflagellate cysts (dinocysts) however do show potential for EOT biostratigraphy, especially for ancient shallow marine settings. At St. Stephens Quarry, Alabama, USA, we found a new, extremely suturocavate dinocyst, Pentadinium alabamensis sp. nov., described herein. The range of the new species spans the critical EOT magnetosubchron C13n, making this taxon a useful biostratigraphic marker for this interval in the Gulf Coast region. The species appears to be associated with shallow marine, euryhaline conditions. (C) 2012 Elsevier B.V. All tights reserved.	[Quaijtaal, Willemijn] Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Quaijtaal, Willemijn; Brinkhuis, Henk] Univ Utrecht, Fac Geosci, Dept Earth Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands	Ghent University; Utrecht University	Quaijtaal, W (通讯作者)，Univ Ghent, Dept Geol & Soil Sci, Res Unit Palaeontol, Krijgslaan 281,S8-WE13, B-9000 Ghent, Belgium.	willemijn.quaijtaal@ugent.be	Quaijtaal, Willemijn/HNB-5108-2023; Brinkhuis, Henk/IUO-8165-2023	Quaijtaal, Willemijn/0000-0001-6016-0194; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 1995, Publ. Society for Sedimentary Geology. III. Cenozoic Era; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Benedek P.N.v., 1982, NEUES JAHRBUCH GEOLO, V162, P265; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Butschli O., 1885, Erster Band. Protozoa. Dr. H. G., Bronn's Klassen und Ordnungen des Thier-Reichs, wissenschaftlich dargestellt in Wort und Bild, P865; Coxall HK, 2005, NATURE, V433, P53, DOI 10.1038/nature03135; COXALL HK, 2007, MICROPALAEONTOLOGICA, P351; EDWARDS L E, 1982, Palynology, V6, P105; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; EVITT WR, 1977, GEOLOGICAL SURVEY CA, V76, P1; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R. A., 2008, AM ASS STRATIGRAPHIC, V1; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; Gerlach E., 1961, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V112, P143; Gocht H., 1969, Palaeontogra, V126, P1; Sancay RH, 2006, MICROPALEONTOLOGY, V52, P537, DOI 10.2113/gsmicropal.52.6.537; Hopmans EC, 2004, EARTH PLANET SC LETT, V224, P107, DOI 10.1016/j.epsl.2004.05.012; Jaramillo CA, 1999, PALAEOGEOGR PALAEOCL, V145, P259, DOI 10.1016/S0031-0182(98)00126-6; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Miller KG, 2008, GEOL SOC AM BULL, V120, P34, DOI 10.1130/B26105.1; MILLER KG, 1993, PALEOCEANOGRAPHY, V8, P313, DOI 10.1029/93PA00203; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; Pross J, 2002, MAR MICROPALEONTOL, V45, P1, DOI 10.1016/S0377-8398(01)00046-9; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Röhl U, 2004, GEOPH MONOG SERIES, V151, P127; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Sluijs A., 2003, PROC OCEAN DRILL SCI, V189, DOI [10.2973/odp.proc.sr.189.104.2003, DOI 10.2973/ODP.PROC.SR.189.104.2003]; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; TEW BH, 1995, PALAIOS, V10, P133, DOI 10.2307/3515179; Wade BS, 2012, GEOLOGY, V40, P159, DOI 10.1130/G32577.1; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588; Zachos JC, 1996, PALEOCEANOGRAPHY, V11, P251, DOI 10.1029/96PA00571	35	5	5	0	5	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAY 1	2012	175						47	54		10.1016/j.revpalbo.2012.03.002	http://dx.doi.org/10.1016/j.revpalbo.2012.03.002			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	950ZH					2025-03-11	WOS:000304689900005
J	Ribeiro, S; Amorim, A; Andersen, TJ; Abrantes, F; Ellegaard, M				Ribeiro, Sofia; Amorim, Ana; Andersen, Thorbjorn J.; Abrantes, Fatima; Ellegaard, Marianne			Reconstructing the history of an invasion: the toxic phytoplankton species Gymnodinium catenatum in the Northeast Atlantic	BIOLOGICAL INVASIONS			English	Article						Ballast; Dinoflagellates; Gymnodinium catenatum; Harmful algal blooms; Microreticulate cysts; Phytoplankton	SP-NOV DINOPHYCEAE; BALLAST WATER; MICRORETICULATE CYST; DINOFLAGELLATE CYSTS; COASTAL SEDIMENTS; NW; TRANSPORT; GALICIAN; TEMPERATURE; VARIABILITY	The phytoplankton species Gymnodinium catenatum is responsible for major worldwide losses in aquaculture due to shellfish toxicity. On the West coast of the Iberian Peninsula, toxic blooms have been reported since the mid-1970s. While the recent geographical spread of this species into Australasia has been attributed to human-mediated introduction, its origin in the Northeast Atlantic is still under debate. Gymnodinium catenatum forms a highly resistant resting stage (cyst) that can be preserved in coastal sediments, building-up an historical record of the species. Similar cyst types (termed microreticulate) are produced by other non-toxic Gymnodinium species that often co-occur with G. catenatum. We analysed the cyst record of microreticulate species in dated sediment cores from the West Iberian shelf covering the past ca. 150 years. Three distinct morphotypes were identified on the basis of cyst diameter and paracingulum reticulation. These were attributed to G. catenatum (35.6-53.3 mu m), G. nolleri (23.1-36.4 mu m), and G. microreticulatum (20.5-34.3 mu m). Our results indicate that G. catenatum is new to the NE Atlantic, where it appeared by 1,889 +/- A 10, expanding northwards along the West Iberian coast. The earliest record is from the southernmost sample, while in the central Portuguese shelf the species appears in sediments dated to 1,933 +/- A 3, and in the North, off Oporto, in 1,951 +/- A 4. On the basis of the cyst record and toxic bloom reports, we reconstruct the invasive pathway of G. catenatum in the NE Atlantic. Although human-mediated introduction cannot be discarded, the available evidence points towards natural range expansion, possibly from NW Africa.	[Ribeiro, Sofia] Geol Survey Denmark & Greenland GEUS, Dept Marine Geol & Glaciol, Copenhagen, Denmark; [Ribeiro, Sofia; Ellegaard, Marianne] Univ Copenhagen, Dept Biol, Marine Biol Sect, Copenhagen, Denmark; [Amorim, Ana] Univ Lisbon, Fac Ciencias, Ctr Oceanog, Lisbon, Portugal; [Andersen, Thorbjorn J.] Univ Copenhagen, Dept Geog & Geol, Copenhagen, Denmark; [Abrantes, Fatima] Unidade Geol Marinha, Lab Nacl Energia & Geol, Lisbon, Portugal	Geological Survey Of Denmark & Greenland; University of Copenhagen; Universidade de Lisboa; University of Copenhagen; Laboratorio Nacional de Energia e Geologia IP (LNEG)	Ribeiro, S (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Marine Geol & Glaciol, Copenhagen, Denmark.	sri@geus.dk	Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/AAZ-2782-2021; Abrantes, Fatima/N-7253-2019; Abrantes, Fatima/B-5985-2013; Ribeiro, Sofia/G-9213-2018; Amorim, Ana/AAA-2615-2020; Andersen, Thorbjorn Joest/N-7560-2014	Abrantes, Fatima/0000-0002-9110-0212; Ribeiro, Sofia/0000-0003-0672-9161; Amorim, Ana/0000-0002-9612-4280; Andersen, Thorbjorn Joest/0000-0001-5032-9945	European Union; Portuguese Foundation for Science and Technology [SFRH/BD/30847/2006]; Fundação para a Ciência e a Tecnologia [SFRH/BD/30847/2006] Funding Source: FCT	European Union(European Union (EU)); Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	This work was supported by the European Union through projects HOLSMEER and SEDPORT and by the Portuguese Foundation for Science and Technology through project INSPECT and a PhD grant to S. Ribeiro (SFRH/BD/30847/2006). The first author would like to thank Dr. M. MilHomens for information regarding the chronologies and geochemical analyses of the sediment cores, Prof. J. Carlton for useful comments on ballast-vectored introductions, and Dr. U. Holzwarth and Dr. K. Zonneveld for kindly lending their microscope slides from NW Africa.	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Invasions	MAY	2012	14	5					969	985		10.1007/s10530-011-0132-6	http://dx.doi.org/10.1007/s10530-011-0132-6			17	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	928VV					2025-03-11	WOS:000303017000006
J	Mertens, KN; Bradley, LR; Takano, Y; Mudie, PJ; Marret, F; Aksu, AE; Hiscott, RN; Verleye, TJ; Mousing, EA; Smyrnova, LL; Bagheri, S; Mansor, M; Pospelova, V; Matsuoka, K				Mertens, Kenneth Neil; Bradley, Lee R.; Takano, Yoshihito; Mudie, Petra J.; Marret, Fabienne; Aksu, Ali E.; Hiscott, Richard N.; Verleye, Thomas J.; Mousing, Erik A.; Smyrnova, Ludmila L.; Bagheri, Siamak; Mansor, Mashhor; Pospelova, Vera; Matsuoka, Kazumi			Quantitative estimation of Holocene surface salinity variation in the Black Sea using dinoflagellate cyst process length	QUATERNARY SCIENCE REVIEWS			English	Article						Paleosalinity; Lingulodinium machaerophorum; rDNA analysis; Caspian Sea; Sea of Azov; Black Sea; Marmara Sea	LAST 2000 YEARS; MARMARA SEA; MEDITERRANEAN SEA; RESERVOIR AGES; BALTIC SEA; WATER; CONNECTIONS; SHELF; RECONNECTION; ASSEMBLAGES	Reconstruction of salinity in the Holocene Black Sea has been an ongoing debate over the past four decades. Here we calibrate summer surface water salinity in the Black Sea, Sea of Azov and Caspian Sea with the process length of the dinoflagellate cyst Lingulodinium machaerophorum. We then apply this calibration to make a regional reconstruction of paleosalinity in the Black Sea, calculated by averaging out process length variation observed at four core sites from the Black Sea with high sedimentation rates and dated by multiple mollusk shell ages. Results show a very gradual change of salinity from similar to 14 +/- 0.91 psu around 9.9 cal ka BP to a minimum similar to 12.3 +/- 0.91 psu around 8.5 cal ka BP, reaching current salinities of similar to 17.1 +/- 0.91 psu around 4.1 cal ka BP. The resolution of our sampling is about 250 years, and it fails to reveal a catastrophic salinization event at similar to 9.14 cal ka BP advocated by other researchers. The dinoflagellate cyst salinity-proxy does not record large Holocene salinity fluctuations, and after early Holocene freshening, it shows correspondence to the regional sea-level curve of Bruckner et al. (2010) derived from Balabanov (2007). (c) 2012 Elsevier Ltd. All rights reserved.	[Mertens, Kenneth Neil; Verleye, Thomas J.] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Bradley, Lee R.; Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Takano, Yoshihito; Matsuoka, Kazumi] Inst E China Sea Res ECSER, Nagasaki 8528521, Japan; [Mudie, Petra J.] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Mudie, Petra J.; Aksu, Ali E.; Hiscott, Richard N.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada; [Mousing, Erik A.] Univ Copenhagen, Ctr Macroecol Evolut & Climate, Dept Biol, DK-2100 Copenhagen O, Denmark; [Smyrnova, Ludmila L.] Res Ctr State Oceanarium, UA-99024 Sevastopol, Ukraine; [Bagheri, Siamak] Iranian Fisheries Res Org IFRO, Inland Waters Aquaculture Inst, Anzali 66, Iran; [Bagheri, Siamak; Mansor, Mashhor] Univ Sains Malaysia, Sch Biol Sci, George Town 11800, Malaysia; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada	Ghent University; University of Liverpool; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland; University of Copenhagen; Universiti Sains Malaysia; University of Victoria	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	kenneth.mertens@ugent.be; l.r.bradley@liverpool.ac.uk; takadino@gmail.com; pmudie@nrcan.gc.ca; f.marret@liv.ac.uk; aaksu@mun.ca; rhiscott@mun.ca; thomas.verleye@ugent.be; eamousing@bio.ku.dk; inik48@inbox.ru; siamakbp@gmail.com; mashhor@usm.my; vpospe@uvic.ca; kazu-mtk@nagasaki-u.ac.jp	Смирнова, Людмила/AAG-2619-2021; Mertens, Kenneth/AAO-9566-2020; Bradley, Lee/AAA-6818-2019; Bagheri, Siamak/S-2035-2016; Mousing, Erik Askov/C-4371-2015; Mertens, Kenneth/C-3386-2015	Mousing, Erik Askov/0000-0003-1663-2507; Bradley, Lee/0000-0003-0833-9351; Bagheri, Siamak/0000-0002-4645-7634; Pospelova, Vera/0000-0003-4049-8133; Marret-Davies, Fabienne/0000-0003-4244-0437; Mertens, Kenneth/0000-0003-2005-9483	JSPS; Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT); Natural Sciences and Engineering Research Council of Canada (NSERC); Leverhulme Trust	JSPS(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)(Institute for the Promotion of Innovation by Science and Technology in Flanders (IWT)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Leverhulme Trust(Leverhulme Trust)	Kenneth N. Mertens is a Postdoctoral scholar of FWO Belgium. This research was conducted by the lead author at Nagasaki University, Japan thanks to a JSPS fellowship. Financial support to Thomas J. Verleye was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT). Petra Mudie, Ali Aksu, Richard Hiscott and Vera Pospelova are grateful for financial support from the Natural Sciences and Engineering Research Council of Canada (NSERC). Lee Bradley and Fabienne Marret thank the Leverhulme Trust for financial support. The officers and crew of RV Koca Piri Reis are thanked for facilitating the collection of the MAR cores in 2002 and 2005. Petra Mudie, Lee Bradley and Fabienne Marret acknowledge the help of Helen Gillespie, Memorial University of Newfoundland, in processing of samples from the MAR cores. Anna Linegar helped calibrate raw <SUP>14</SUP>C dates. Dr. Marcel van der Meer (NIOZ) is thanked for providing samples of boxcore BC53. Jennifer Cranshaw is acknowledged for clarifying the amount of core-top loss for MAR05-13P, and its correlation with MAR05-4G. We are grateful to Dr Igor Bondarev, National Academy of Science of Ukraine, Sevastopol, for diving to sample for living dinoflagellate cysts on the NW Black Sea shelf during INQUA 501 field trip 2. We thank Dennis Dunn, Adam Willingham, and Carrie Wolfe (the Southern California Marine Institute) for their assistance in sediment sampling in San Pedro Harbor, California. Neslihan Balkis is thanked for help with obtaining salinity data and Helmut Bruckner for communications on sea-level variations in the Black Sea. The comments of wo anonymous reviewers were appreciated.	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J	Pendea, IF; Chmura, GL				Pendea, I. Florin; Chmura, Gail L.			Calibration of pollen assemblages and carbon-nitrogen ratios to discriminate boreal wetland types	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						James Bay; tidal marsh; fen; bog; discriminant analysis	DINOFLAGELLATE CYST ASSEMBLAGES; VEGETATION RELATIONSHIPS; METHANE EMISSIONS; NORTHERN ONTARIO; ATMOSPHERIC CH4; LATE QUATERNARY; BAY; PEATLANDS; SURFACE; MODEL	Differentiation of boreal wetlands in the palaeo record is required for studies of isostacy and sea level change, landscape change, and climate dynamics. To develop palynomorph signatures and calibrate soil C-N ratios for boreal wetlands we sampled low and high elevation tidal marshes, fens and bogs along eastern James Bay, Canada. A discriminant analysis model showed that a small subset of palynomorph taxa can effectively discriminate between the four wetland types. Cyperaceae, Poaceae, and Potamogeton-Triglochin-type are important to the classification of high marshes. Bryidae spores and pollen of Myrica gale, Cyperaceae, and Poaceae are indicative of fen. Moss spores alone, primarily from Sphagnum, but also Bryidae type spores, derived from brown mosses are the indicators of bog. The use of palynomorph assemblages to discriminate among wetland types is not dependent upon the localized presence of a plant source as it would be using macrofossil analysis. C/N of bog soils can be clearly distinguished from fen and tidal marshes and can be used as a pollen-independent proxy to indicate fen to bog wetland succession. (C) 2011 Elsevier B.V. All rights reserved.	McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; Global Environm & Climate Change Ctr, Montreal, PQ H3A 2K6, Canada		Pendea, IF (通讯作者)，Lakehead Univ, Dept Interdisciplinary Studies, Orillia Campus,500 Univ Ave, Orillia, ON L3V0B9, Canada.	ifpendea@lakeheadu.ca	Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903	Social Sciences and Humanities Research Council; Natural Sciences and Engineering Research Council of Canada	Social Sciences and Humanities Research Council(Social Sciences & Humanities Research Council of Canada (SSHRC)); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This work is part of the European Science Foundation EUROCORES Programme BOREAS and is supported by funds from the Social Sciences and Humanities Research Council and the Natural Sciences and Engineering Research Council of Canada. We thank the people of the Wemindji Cree First Nation, in particular Fred Asquabaneskum and the Stewart family for their help and guidance during the field work. Many thanks to Jesse Sayles, Eby Heller and Tom Heller for their most valuable help during the sampling campaign. Also, we are indebted to our lab assistants - A. De Young, L Murchison, Z. Hudda, F. Syed, Y. Li, K. Yu, and N. Okere. We are most grateful to two anonymous reviewers for their comments and suggestions that helped improve the original manuscript.	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Palaeobot. Palynology	APR 15	2012	174						48	56		10.1016/j.revpalbo.2011.12.003	http://dx.doi.org/10.1016/j.revpalbo.2011.12.003			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	931AF					2025-03-11	WOS:000303185600004
J	Attaran-Fariman, G; Bolch, CJS				Attaran-Fariman, G.; Bolch, C. J. S.			Morphology and Phylogeny of <i>Scrippsiella trochoidea</i> (Dinophyceae) a potentially harmful bloom forming species isolated from the sediments of Iran's south coast	IRANIAN JOURNAL OF FISHERIES SCIENCES			English	Article						Cyst; Iran south coast; Molecular analysis; Morphology; Phylogeny; Scrippsiella trochoidea; Sediment; Vegetative cell	SP-NOV DINOPHYCEAE; CYST PRODUCTION; DINOFLAGELLATE; CALCIODINELLOIDEAE; IDENTIFICATION; PERIDINIALES; GULF	Phytoplankton cells and resting cysts of the species Scrippsiella trochoidea are regular and dominant components of the dinoflagellate flora of coastal marine waters and sediments around the world. This species is a common harmful bloom forming species in coastal waters. In this study, for the first time cyst of S. trochoidea were isolated from the sediments of southeast coast of Iran. Five strains from the germination of a single cyst belonged to S. trochoidea. In order to confirm identification of the species an excystment and encystment experiment, cyst and germinated cell morphology and plate pattern by light and electron microscopy (SEM) have been described. The nucleotide sequences of two highly diverse regions, the rDNA-ITS 1,2 and 5.8S-rDNA have been sequenced for all strains. Homologous sequences from GenBank with five Iranian strains were compared to find their phylogenetic relationship. Both NJ and MP phylogenetic and morphological analysis showed five strains of S. trochoidea from Iran were clustered with previously described S. trochoidea and Calciodinellum levantinum species, and its closest relationship was with Scrippsiella sp. strain with a 1.2-1.4% sequence divergence. Results indicate that molecular studies of rDNA if combined with morphological cyst and vegetative cells could be a valuable approach to identification and taxonomy of calciodinelloideae dinoflagellate.	[Attaran-Fariman, G.] Chabahar Maritime Univ, Marine Sci Fac, Chabahar, Iran; [Bolch, C. J. S.] Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia	University of Tasmania	Attaran-Fariman, G (通讯作者)，Chabahar Maritime Univ, Marine Sci Fac, Chabahar, Iran.	G.Attaran@cmu.ac.ir	Attaran Fariman, Gilan/ABC-4059-2021; Bolch, Christopher/J-7619-2014					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, 1997, J PHYCOL, V33, P440; Attaran-Fariman G, 2011, IRAN J FISH SCI, V10, P1; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J. Fish. Sci.	APR	2012	11	2					252	270						19	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	978OG					2025-03-11	WOS:000306752300002
J	Anglès, S; Garcés, E; Reñé, A; Sampedro, N				Angles, Silvia; Garces, Esther; Rene, Albert; Sampedro, Nagore			Life-cycle alternations in <i>Alexandrium minutum</i> natural populations from the NW Mediterranean Sea	HARMFUL ALGAE			English	Article						Bloom dynamics; Coastal zone; Encystment; Excystment; Harmful algal bloom; Resting cyst	DINOFLAGELLATE GONYAULAX-TAMARENSIS; RESTING CYSTS; RECENT SEDIMENTS; GYMNODINIUM-CATENATUM; SEXUAL REPRODUCTION; TOXIN COMPOSITION; NORTHEAST JAPAN; ONAGAWA BAY; DINOPHYCEAE; DYNAMICS	Life-cycle transitions play a key role in the bloom dynamics of many dinoflagellates. In this study, in situ excystment and encystment were monitored during recurrent Alexandrium minutum blooms in Arenys de Mar harbor (NW Mediterranean Sea) from October 2005 to May 2008. In addition, the dynamics of vegetative cells in the water column and resting cysts in the sediments were assessed. Excystment occurred continuously during the period studied. The excystment fluxes and the estimated excystment percentages indicated a pattern of alternating reduced and active excystment periods. From July to November, excystment percentages were <0.1%, whereas from December to June the A. minutum population underwent active excystment, with excystment percentages of 0.3-45.7%. Periods of active excystment coincided with increases in irradiance and water temperature, conditions also favorable for bloom development. During vegetative cell blooms, resting cyst formation coincided with periods marked by vegetative cell abundances in the water column of >2 x 10(3) cells l(-1). Resting cyst fluxes were higher when the abundance of vegetative cells in the overlying water column was greater. The excystment and encystment processes overlapped for 2 months during the extended blooms, indicating that newly formed resting cysts had overcome the mandatory dormancy period and were capable of germinating within the same bloom in which they were produced. Resting cysts in the surface sediment were rapidly depleted during periods of active excystment, but their production, although involving only a small fraction of the vegetative population, more than compensated for their loss. These results are discussed with respect to the role of frequent life-stage switches in determining the population dynamics and the maintenance of A. minutum blooms. (C) 2012 Elsevier B.V. All rights reserved.	[Angles, Silvia; Garces, Esther; Rene, Albert; Sampedro, Nagore] CSIC, Inst Ciencies Mar, 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)	Anglès, S (通讯作者)，CSIC, Inst Ciencies Mar, Pg Maritim de la Barceloneta 37-49, E-08003 Barcelona, Spain.	sangles@icm.csic.es	Garces, Esther/C-5701-2011; Rene, Albert/D-4560-2012; Angles, Silvia/B-9469-2011; SAMPEDRO, NAGORE/I-1767-2015	Garces, Esther/0000-0002-2712-501X; Rene, Albert/0000-0002-0488-3539; Angles, Silvia/0000-0003-0529-7504; SAMPEDRO, NAGORE/0000-0002-0829-5152	Creu Roja, Club Nlautic; Cofradia de Pescadors Sant Telm of Arenys de Mar harbor; EC [GOCE-CT-2005-003875]; Ramon y Cajal award from the MICINN	Creu Roja, Club Nlautic; Cofradia de Pescadors Sant Telm of Arenys de Mar harbor; EC(European Union (EU)European Commission Joint Research Centre); Ramon y Cajal award from the MICINN	The authors thank K. Van Lenning, X. Novell, and J. Riba for assistance with field work. K. Rengefors provided an excystment trap to be re-designed for this study. A. Jordi provided valuable help with the graphs. The authors thank the two anonymous reviewers who helped to improve the manuscript. Thanks are extended to Creu Roja, Club Nlautic, and Cofradia de Pescadors Sant Telm of Arenys de Mar harbor for their support. Data from the meteorological station were supplied by the Catalan Meteorological Service (Meteocat). This study was financed by the EC-funded research project SEED (GOCE-CT-2005-003875). The work of E. 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J	Anglès, S; Garcés, E; Hattenrath-Lehmann, TK; Gobler, CJ				Angles, Silvia; Garces, Esther; Hattenrath-Lehmann, Theresa K.; Gobler, Christopher J.			In situ life-cycle stages of <i>Alexandrium fundyense</i> during bloom development in Northport Harbor (New York, USA)	HARMFUL ALGAE			English	Article						Encystment; Excystment; Germination; Harmful algal bloom; Resting cyst	DINOFLAGELLATE GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; RESTING CYSTS; POPULATION-DYNAMICS; VEGETATIVE CELLS; RECENT SEDIMENTS; DINOPHYCEAE; PHYTOPLANKTON; MINUTUM; EVENTS	Knowledge of the specific life-cycle dynamics during harmful algal bloom (HAB) development is essential for understanding and forecasting the onset, evolution and future occurrence of these events. Life-cycle stages of the toxic dinoflagellate Alexandrium fundyense were monitored both in the water column and in the sediments from the onset to the decline of a bloom in Northport Harbor (New York, USA). Moreover, excystment and encystment were investigated in situ through the deployment of emergence and sediment traps, respectively. The bloom, the largest ever recorded on the east coast of the US south of Massachusetts, persisted for 6 weeks between April and June 2008, and reached maximum vegetative cell abundances of 1.3 x 10(6) cells l(-1). Resting cysts in the surface sediments were quantified at the onset of the bloom, all of which germinated during the development of the bloom. Excystment of these resting cysts provided inoculum of vegetative cells for bloom development. In the water column, first detection of planozygotes occurred during the exponential phase of the bloom at vegetative cell abundances of similar to 10(4) cells l(-1). Nonmotile planozygotes and resting cysts were observed in the sediment traps before the first peak of vegetative cells, coinciding with the detection of planktonic planozygotes. The estimated encystment and planozygote percentages were relatively low, indicating that a small proportion of the vegetative cell population was involved in sexual reproduction. However, encystment was a crucial process for replenishing the cyst stock of the A. fundyense population in the sediments as cyst densities were low before the bloom but high after it. For the first time, formation of pellicle cysts in the field by A. fundyense was observed, which coincided with high vegetative cell abundances in the water column during the bloom. (C) 2012 Elsevier B.V. All rights reserved.	[Angles, Silvia; Garces, Esther] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Hattenrath-Lehmann, Theresa K.; Gobler, Christopher J.] SUNY Stony Brook, Southampton, NY 11968 USA	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); State University of New York (SUNY) System; Stony Brook University	Anglès, S (通讯作者)，CSIC, Inst Ciencies Mar, Pg Maritim de la Barceloneta 37-49, E-08003 Barcelona, Spain.	sangles@icm.csic.es	Gobler, Christopher/JOZ-2924-2023; Angles, Silvia/B-9469-2011; Garces, Esther/C-5701-2011	Angles, Silvia/0000-0003-0529-7504; Garces, Esther/0000-0002-2712-501X	AGAUR (Generalitat de Catalunya); New York State Department of Environmental Conservation; USEPA's Long Island Sound Study; Ramon y Cajal contract from the MICINN	AGAUR (Generalitat de Catalunya)(Agencia de Gestio D'Ajuts Universitaris de Recerca Agaur (AGAUR)Generalitat de Catalunya); New York State Department of Environmental Conservation; USEPA's Long Island Sound Study; Ramon y Cajal contract from the MICINN	We thank the people at the laboratory, and especially those who helped with the fieldwork: A. Marcoval, C. Wall, J. Carroll, and B. Peterson. This research was funded by a BE-DGR-2007 fellowship from the AGAUR (Generalitat de Catalunya) and by the New York State Department of Environmental Conservation, NY Sea Grant, and the USEPA's Long Island Sound Study. The work of E. Garces was supported by a Ramon y Cajal contract from the MICINN.[SS]	Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1987, NATURE, V325, P616, DOI 10.1038/325616a0; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1979, ESTUAR COAST MAR SCI, V8, P279, DOI 10.1016/0302-3524(79)90098-7; ANDERSON DM, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Anglès S, 2012, HARMFUL ALGAE, V16, P1, DOI 10.1016/j.hal.2011.12.006; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; Dale B., 1983, P69; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; Fraga S., 2006, 12 INT C HARMF ALG C, P64; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Hattenrath TK, 2010, HARMFUL ALGAE, V9, P402, DOI 10.1016/j.hal.2010.02.003; Hattenrath-Lehmann TK, 2011, HARMFUL ALGAE, V11, P106, DOI 10.1016/j.hal.2011.08.005; Hégaret H, 2008, MAR ECOL PROG SER, V361, P169, DOI 10.3354/meps07375; Figueroa RI, 2006, J PHYCOL, V42, P1028, DOI 10.1111/j.1529-8817.2006.00262.x; JONES MN, 1984, WATER RES, V18, P643, DOI 10.1016/0043-1354(84)90215-X; Lilly EL, 2007, J PHYCOL, V43, P1329, DOI 10.1111/j.1529-8817.2007.00420.x; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; Parsons T.R., 1984, A manual for chemical and biological methods in seawater analysis; Persson A, 2008, HARMFUL ALGAE, V7, P798, DOI 10.1016/j.hal.2008.04.002; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Pitcher GC, 2007, HARMFUL ALGAE, V6, P823, DOI 10.1016/j.hal.2007.04.008; Probert I., 1999, THESIS U WESTMINSTER, P117; Rengefors K, 2004, AQUAT MICROB ECOL, V36, P213, DOI 10.3354/ame036213; Ribeiro S, 2011, NAT COMMUN, V2, DOI 10.1038/ncomms1314; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SCHREY SE, 1984, ESTUARIES, V7, P472, DOI 10.2307/1352050; SHUMWAY S E, 1990, Journal of the World Aquaculture Society, V21, P65, DOI 10.1111/j.1749-7345.1990.tb00529.x; Shumway SE, 2003, HARMFUL ALGAE, V2, P1, DOI 10.1016/S1568-9883(03)00002-7; STEIDINGER KA, 1975, ENVIRON LETT, V9, P129, DOI 10.1080/00139307509435842; Turner JT, 1997, LIMNOL OCEANOGR, V42, P1203, DOI 10.4319/lo.1997.42.5_part_2.1203; Uchida T, 2001, J PLANKTON RES, V23, P889, DOI 10.1093/plankt/23.8.889; Von Stosch HA., 1973, Br Phycol J, V8, P105; Walker L.M., 1984, P19; WALL D, 1970, Phycologia, V9, P151, DOI 10.2216/i0031-8884-9-2-151.1; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551	47	25	28	2	27	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	APR	2012	16						20	26		10.1016/j.hal.2011.12.008	http://dx.doi.org/10.1016/j.hal.2011.12.008			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	932NU					2025-03-11	WOS:000303298600003
J	Kocsis, L; Dulai, A; Bitner, MA; Vennemann, T; Cooper, M				Kocsis, Laszlo; Dulai, Alfred; Bitner, Maria Aleksandra; Vennemann, Torsten; Cooper, Matthew			Geochemical compositions of Neogene phosphatic brachiopods: Implications for ancient environmental and marine conditions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						North Sea; Paratethys; Brachiopods; Phosphate; Isotopes; Palaeo-environment	OXYGEN-ISOTOPE FRACTIONATION; DINOFLAGELLATE CYST STRATIGRAPHY; FE-MN CRUSTS; MIDDLE MIOCENE; CENTRAL PARATETHYS; BIOGENIC PHOSPHATE; REE CONTENTS; SHARK TEETH; ND ISOTOPES; SEA	Isotopic and trace element compositions of Miocene and Pliocene phosphatic brachiopods (Lingulidae and Discinidae) from southern North Sea, the Central Paratethys and the Atlantic coast of Europe were investigated in order to trace past environmental conditions and marine connections between the northern boreal and the southern subtropical-tropical marine basins. The North Sea genus Glottidia yielded low epsilon(Nd) and high delta O-18(PO4) values through the Mio-Pliocene indicating cold habitat temperature where the local seawater was dominated by the Atlantic Ocean. In contrast, the Middle Miocene Lingulidae and Discinidae of the Paratethys inhabited warm subtropical seawater with the possible influence of the Indian Ocean via the Mediterranean, as supported by their average epsilon(Nd) value of -8.3. The combined geochemical data support a thermal and marine separation of the Paratethys from the North Sea with no direct connection or major exchange of water from the Miocene onwards. The temperature in the Paratethys was very similar to that inferred from brachiopods from the Middle Miocene of western France, but the seawater epsilon(Nd) value here is identical to that of contemporaneous Atlantic Ocean. A Late Miocene lingulid brachiopod from southern Portugal has a high delta O-18(PO4), similar to the specimens investigated from the North Sea, reflecting either a deep water habitat or formation after the onset of major global cooling that resulted in an increased delta O-18 value of seawater. The epsilon(Nd) value of -8.4 for this site is compatible with an influence of Mediterranean outflow. (C) 2012 Elsevier B.V. All rights reserved.	[Kocsis, Laszlo; Vennemann, Torsten] Univ Lausanne, Inst Mineral & Geochim, CH-1015 Lausanne, Switzerland; [Dulai, Alfred] Hungarian Nat Hist Museum, Dept Geol & Paleontol, H-1431 Budapest, Hungary; [Bitner, Maria Aleksandra] Polish Acad Sci, Inst Paleobiol, PL-00818 Warsaw, Poland; [Cooper, Matthew] Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England	University of Lausanne; Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; NERC National Oceanography Centre; University of Southampton	Kocsis, L (通讯作者)，Univ Lausanne, Inst Mineral & Geochim, CH-1015 Lausanne, Switzerland.	laszlo.kocsis@unil.ch	Bitner, Maria Aleksandra/G-8932-2011	Bitner, Maria Aleksandra/0000-0002-2864-2967; Kocsis, Laszlo/0000-0003-4613-1850	Swiss National Science Foundation [SNF PBLA2-119669, SNF PZ00P2_126407/1]; Hungarian Scientific Research Fund (OTKA) [K77451]; European Commission [NL-TAF-3270]	Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); Hungarian Scientific Research Fund (OTKA)(Orszagos Tudomanyos Kutatasi Alapprogramok (OTKA)); European Commission(European Union (EU)European Commission Joint Research Centre)	The authors thank the Netherlands Centre for Biodiversity (NCB), Naturalis, in Leiden for providing fossils for this research and Dr. Frank Wesselingh and Ronald Pouwer at NCB for their assistance with the sampling. L.K. received support from the Swiss National Science Foundation (SNF PBLA2-119669 and SNF PZ00P2_126407/1) and from a grant to Clive Trueman, NERC (NE/C00390X/1), when this research was conducted. A.D. was supported by the Hungarian Scientific Research Fund (OTKA K77451) and European Commission's Synthesys project to Leiden (NL-TAF-3270). The authors appreciate the detailed constructive reviews of D.L. Rodland and three other anonymous reviewers on an earlier version of the manuscript.	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Paleoclimatol. Paleoecol.	APR 1	2012	326						66	77		10.1016/j.palaeo.2012.02.004	http://dx.doi.org/10.1016/j.palaeo.2012.02.004			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	926SK					2025-03-11	WOS:000302851200006
J	Pienkowski, AJ; England, JH; Furze, MFA; Marret, F; Eynaud, F; Vilks, G; MacLean, B; Blasco, S; Scourse, JD				Pienkowski, Anna J.; England, John H.; Furze, Mark F. A.; Marret, Fabienne; Eynaud, Frederique; Vilks, Gustav; MacLean, Brian; Blasco, Steve; Scourse, James D.			The deglacial to postglacial marine environments of SE Barrow Strait, Canadian Arctic Archipelago	BOREAS			English	Review							LAST GLACIAL MAXIMUM; LAURENTIDE ICE-SHEET; HOLOCENE PALAEOCEANOGRAPHIC CHANGES; STAINED BENTHIC FORAMINIFERA; WALLED DINOFLAGELLATE CYSTS; CENTRAL ELLESMERE-ISLAND; NORTHEAST WATER POLYNYA; QUEEN-ELIZABETH-ISLANDS; NORTHERNMOST BAFFIN-BAY; WESTERN ROSS-SEA	Core 86027-144 (74 degrees 15.56'N, 91 degrees 14.21'W) represents a rare, continuous record of Late Pleistocene to Holocene sediments from High Arctic Canada extending from the end of the Last Glaciation. Based on microfossils (dinocysts, non-pollen palynomorphs, benthic and planktonic foraminifera), foraminiferal delta O-18 and delta C-13, and sedimentology, seven palaeoenvironmental zones were identified. Zone I (>10.8 cal. ka BP) records deglaciation, ice-sheet destabilization, float-off and subsequent break-up. Zone II (c. 10.8-10.4 cal. ka BP) shows ice-proximal to ice-distal glaciomarine conditions, interrupted by pervasive land-fast sea-ice marked by a hiatus in coarse sediment deposition. Significant biological activity starts in Zone III (10.4-9.9 cal. ka BP), where planktonic foraminifera (Neogloboquadrina pachyderma) suggest early oceanic throughflow. Surface waters flowed NW-SE; however, the deep-water origin remains unclear (potentially NW Arctic Ocean or Baffin Bay). Postglacial amelioration (open-water season greater than present) in Zone IV (9.9-7.8 cal. ka BP) perhaps corresponds to the regional 'Holocene Thermal Maximum' previously proposed. A transitional period (Zone V; 7.8-6.7 cal. ka BP) of rapid environmental change fluctuating on a scale not observed today is marked by increasing sea-ice and reduced oceanic influence. This probably signals the exclusion of deeper Atlantic water owing to the glacioisostatic shallowing of inter-island sills, coupled with generally cooling climate. Conditions analogous to those at present, with increased sea-ice and modern microfossil assemblages, commence at c. 6.7 cal. ka BP (zones VI-VII). Although climate ultimately forces long-term environmental trends, core 86027-144 data imply that regional dynamics, especially changes in sea-level, exert a significant control on marine conditions throughout the Canadian Arctic Archipelago.	[England, John H.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB T6G 2E3, Canada; [Furze, Mark F. A.] Grant MacEwan Univ, Dept Phys Sci, Edmonton, AB T5J 2P2, Canada; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Eynaud, Frederique] Univ Bordeaux 1, Lab EPOC Environm & Paleoenvironm OCean, UMR CNRS 5805, F-33405 Talence, France; [Vilks, Gustav; MacLean, Brian; Blasco, Steve] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Scourse, James D.] Bangor Univ, Coll Nat Sci, Menai Bridge LL59 5AB, Anglesey, Wales	University of Alberta; University of Liverpool; Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bangor University	Pienkowski, AJ (通讯作者)，Bangor Univ, Coll Nat Sci, Menai Bridge LL59 5AB, Anglesey, Wales.	a.pienkowski@bangor.ac.uk	Pieńkowski, Anna/AAL-1312-2020; Pienkowski, Anna/J-9339-2013	Furze, Mark/0000-0003-4636-6182; Eynaud, Frederique/0000-0003-1283-7425; Pienkowski, Anna/0000-0002-3606-7130; Marret-Davies, Fabienne/0000-0003-4244-0437	Canadian Circumpolar Institute (CCI)	Canadian Circumpolar Institute (CCI)	This research constitutes part of a broader study of glaciation, sea-level adjustment and environmental change under J. England's NSERC Northern Chair Program, directly complementing other ongoing research in the western CAA by J. England, M. F. A. Furze, R. D. Coulthard, F. C. Nixon, T. R. Lakeman and J. Vaughan. Circumpolar/Boreal Research grants from the Canadian Circumpolar Institute (CCI) awarded to A. Pienkowski and J. England are gratefully acknowledged. Two FGSR (University of Alberta) awards (Research Abroad Travel Grant and J. Gordin Kaplan Graduate Student Award) enabled research visits at Universite Bordeaux-1, University of Liverpool, and Bangor University for A. Pienkowski. We thank Roy Coulthard (University of Alberta) for clarifying bowhead whale Delta R values. We acknowledge Brian Long (Bangor University), Irene Cooper and Bertha Hull (University of Liverpool), as well as Charlie Schweger and Harvey Friebe (University of Alberta) for generously enabling access to lab facilities and help with sample processing. We are grateful to Kate Jarrett, Owen Brown, Bill LeBlanc and Peta Mudie (GSC Atlantic) for help with core sampling, and for grain size and TOC measurements on this core record. We thank Tom Cronin (US Geological Survey) for help with ostracod identifications, and Trecia Schell (formerly Dalhousie University) for aiding in foraminifera identifications. Katrine Husum and Morten Hald (University of Tromso) are thanked for clarifying disequilibrium effects of the benthic foraminifera species used in this study. We thank Jon Eiriksson and Anne Jennings, whose comments greatly improved this paper. Jan A. Piotrowski is thanked for editorial handling of this manuscript.	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J	Verleye, TJ; Mertens, KN; Young, MD; Dale, B; McMinn, A; Scott, L; Zonneveld, KAF; Louwye, S				Verleye, Thomas J.; Mertens, Kenneth N.; Young, Marty D.; Dale, Barrie; McMinn, Andrew; Scott, Louis; Zonneveld, Karin A. F.; Louwye, Stephen			Average process length variation of the marine dinoflagellate cyst <i>Operculodinium centrocarpum</i> in the tropical and Southern Hemisphere Oceans: Assessing its potential as a palaeosalinity proxy	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Operculodinium centrocarpum; Process length; Salinity; Temperature; Density; Southern Hemisphere; Tropics	SEA-SURFACE TEMPERATURE; PROTOCERATIUM-RETICULATUM; HIGH-LATITUDE; ENVIRONMENTAL-FACTORS; RESTING CYSTS; BALTIC SEA; SALINITY; VARIABILITY; HOLOCENE; CHILE	The study investigates the morphological variability of the dinoflagellate cyst Operculodinium centrocarpum (resting cyst of Protoceratium reticulatum) in core-top samples distributed over the Southern Hemisphere and the tropics in relation to sea-surface temperature (SST) and sea-surface salinity (SSS) at the corresponding sites. The process lengths show a moderate inverse relationship to summer SST (sSST) (R-2 = 0.44) and sSSS/sSST (R-2 = 0.4), however, lateral transport of cysts probably produced noise in the plots. After excluding tropical and Southern Hemisphere sites considered to have been affected by long distance lateral transport, the relationship between process length and density follows the equation sD = 0.8422x + 1016.9 (R-2 = 0.55) with a Root Mean Square Error = 0.63 kg m(-3), while the negative correlation with sSST increases up to R-2 = 0.79. Next to salinity, this study thus highlights the importance of a second factor, temperature, affecting process length in the topics and the Southern Hemisphere oceans. (C) 2012 Elsevier B.V. All rights reserved.	[Verleye, Thomas J.; Mertens, Kenneth N.; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, B-9000 Ghent, Belgium; [Young, Marty D.] Australian Natl Univ, Dept Earth & Marine Sci, Canberra, ACT 0200, Australia; [Young, Marty D.] CSIRO Earth Sci & Resource Engn, N Ryde, NSW 2113, Australia; [Dale, Barrie] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [McMinn, Andrew] Univ Tasmania, Inst Antarctic & So Ocean Studies, Hobart, Tas 7001, Australia; [McMinn, Andrew] Univ Tasmania, Antarctic CRC, Hobart, Tas 7001, Australia; [Scott, Louis] Univ Free State, Dept Plant Sci, Bloemfontein, South Africa; [Zonneveld, Karin A. F.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany	Ghent University; Australian National University; Commonwealth Scientific & Industrial Research Organisation (CSIRO); University of Oslo; University of Tasmania; University of Tasmania; University of the Free State; University of Bremen	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, Knjgslaan 281 S8-WE13, B-9000 Ghent, Belgium.	stephen.louwye@ugent.be	Mertens, Kenneth/AAO-9566-2020; McMinn, Andrew/A-9910-2008; Scott, Louis/T-5279-2017; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Mertens, Kenneth/0000-0003-2005-9483; Louwye, Stephen/0000-0003-4814-4313	ANU-RSPAS PhD; Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)	ANU-RSPAS PhD; Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)(Institute for the Promotion of Innovation by Science and Technology in Flanders (IWT))	Anne-Marie Lezine (Lab. Des Sciences du Climat et de l'Environment, Gif-sur-Yvette) and Naima Abidi are greatly acknowledged for providing sample material from the West Indian Ocean. John Rogers and Amanda Rau (Dept. of Oceanography, University of Cape Town) are thanked for initially providing samples to Louis Scott. M.D. Young acknowledges the ANU-RSPAS PhD scholarship and Patrick De Deckker for making the eastern Indian/NW Australian coretops available. Also thanks to Annemiek Vink, Oliver Esper and Ulrike Holzwarth. Financial support to T.J. Verleye was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT). K.N. Mertens is a Postdoctoral fellow of FWO Belgium. The reviewers are kindly thanked for their constructive and careful review.	Aasen J, 2005, TOXICON, V45, P265, DOI 10.1016/j.toxicon.2004.10.012; Abidi N., 1997, THESIS U P M CURIE P, P183; [Anonymous], 1996, Am. Assoc. Strat. 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J	Prauss, ML				Prauss, Michael L.			The Cenomanian/Turonian Boundary event (CTBE) at Tarfaya, Morocco: Palaeoecological aspects as reflected by marine palynology	CRETACEOUS RESEARCH			English	Article						Cenomanian; Turonian; Event; Marine palynology; Prasinophytes; Anoxic; Tarfaya; NW Africa	SEA-LEVEL CHANGE; DINOFLAGELLATE CYSTS; WESTERN INTERIOR; ANOXIC EVENT; BASIN; STRATIGRAPHY; SEDIMENTS; DINOCYST; GERMANY; RECORD	Two sections from the Cenomanian-Turonian boundary event (CTBE) at Tarfaya, northwest Africa, were analysed fully quantitatively by marine palynology. The results are compared and integrated with published data from micropalaeontology, total organic carbon content (TOC), isotope geochemistry and, for selected intervals, the distribution of chlorobactanes. A rise in eustatic sea level, composed of several third-order transgression pulses, is reflected by various palynologic proxies. A combination of productivity and preservation is proposed as the main control on TOC accumulation preceding and across the CTBE. Strong episodic upwelling events, reflected by significant increases of the peridinioid/gonyaulacoid (p/g) ratio of dinocysts, are documented at the onset of eustatic transgression and closely preceding the onset as well as within the plateau stage of the positive delta C-13 anomaly. These events are considered as initial and sustaining causes respectively for TOC accumulation. The peak abundance of both green algal groups, Botryococcus and prasinophytes, is coincident with pelagic sedimentation and is strongly related to the increase of both oxygen deficiency in the water column and total organic carbon content. An episodic halocline stratification of the water column is suggested, possibly related to both a globally intensified hydrologic cycle and a current induced input of high- to middle-latitude surface waters into the Tarfaya Basin. This is corroborated by the prominent episodic appearance of Bosedinia, a peridinioid dinocyst with probable freshwater/reduced salinity affinity, as well as several euryhaline taxa common within late Mesozoic high to mid-latitude waters. A slight correlation with contents of chlorobactanes is documented at least for the prasinophyte distribution, which may reflect a moderate availability of reduced nitrogen within photic zone waters. However, maxima of chlorobactanes are related to palynologically barren or depleted intervals, possibly reflecting the sulfidic stage of redox conditions within photic zone waters. The almost coeval appearance of the suggested high-latitude taxon ?Ginginodinium sp. close to the onset of the delta C-13 anomaly both at Tarfaya and at Wunstorf, northwest Germany, corroborates a connection of surface water circulation between high and low latitude sites during the eustatic sea-level high. (C) 2011 Elsevier Ltd. All rights reserved.	Free Univ Berlin, Inst Geol Sci, Palaeontol Sect, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Free Univ Berlin, Inst Geol Sci, Palaeontol Sect, Malteserstr 74-100,Bldg D, D-12249 Berlin, Germany.	mprauss@zedat.fu-berlin.de			Deutsche Forschungsgemeinschaft, DFG [Ke 322/33-1]	Deutsche Forschungsgemeinschaft, DFG(German Research Foundation (DFG))	Sample material and data on foraminifera distribution have been provided by Wolfgang Kuhnt, University Kiel, Germany. Data on TOC, isotopes and chlorobactanes have been provided by Sadat Kolonic, Exploration Team Leader at Shell EP, Jordan. The project has been supported by a research grant from the Deutsche Forschungsgemeinschaft, DFG, grant number Ke 322/33-1. The constructive critics of two anonymous reviewers were appreciated.	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Res.	APR	2012	34						233	256		10.1016/j.cretres.2011.11.004	http://dx.doi.org/10.1016/j.cretres.2011.11.004			24	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	902GS					2025-03-11	WOS:000301027200022
J	Hakanen, P; Suikkanen, S; Franzén, J; Franzén, H; Kankaanpää, H; Kremp, A				Hakanen, Paeivi; Suikkanen, Sanna; Franzen, Johan; Franzen, Helene; Kankaanpaeae, Harri; Kremp, Anke			Bloom and toxin dynamics of <i>Alexandrium ostenfeldii</i> in a shallow embayment at the SW coast of Finland, northern Baltic Sea	HARMFUL ALGAE			English	Article						Alexandrium ostenfeldii; Baltic Sea; Bloom dynamics; Dinoflagellate; PSP toxin	HARMFUL ALGAL BLOOMS; POPULATION-DYNAMICS; DINOFLAGELLATE BLOOM; DINOPHYCEAE; WATERS; TOXICITY; GROWTH; LIMITATION; MORPHOLOGY; PROTISTS	In the past years, some coastal areas in the central and northern Baltic Sea have experienced recurrent blooms of the potentially toxic dinoflagellate Alexandrium ostenfeldii. The population. dynamics and spatial distribution of the species were studied in the Foglo archipelago, a bloom area in Aland, northern Baltic Sea. During a two-year survey, cell and toxin concentrations of A. ostenfeldii were recorded in summer phytoplankton communities and related to environmental parameters. The studies revealed that A. ostenfeldii blooms were restricted to a small area in a narrow sound, where cells of this species were detected from May to September in 2009 and 2010. A. ostenfeldii proliferated to bloom concentrations (1.7-2.1 x 10(5) cells L-1) only at water temperatures around 20 degrees C during warm periods in July and August. Abundance of A. ostenfeldii did not significantly correlate with dissolved inorganic nutrient concentrations (p = 0.4-0.6) but was related to high concentrations of resting cysts in the sediment (p < 0.001). The blooms were not monospecific but A. ostenfeldii was a part of a diverse productive phytoplankton community forming 30-60% of the total biomass during the abundance peaks. This study provides the first evidence of paralytic shellfish poisoning (PSP) toxins produced by dinoflagellate blooms in the Baltic Sea: PSP toxin dynamics correlated with the progression of the A. ostenfeldii bloom with toxin peaks mirroring the species abundance peaks. No other potentially toxic species were identified from the phytoplankton community. PSP toxin concentrations of up to 2.3 mu g L-1 measured in the A. ostenfeldii cell fraction suggest that blooms may have toxic effects on co-occurring biota. (C) 2011 Elsevier B.V. All rights reserved.	[Hakanen, Paeivi; Suikkanen, Sanna; Kremp, Anke] Ctr Marine Res, Finnish Environm Inst, FI-00251 Helsinki, Finland	Finnish Environment Institute	Hakanen, P (通讯作者)，Ctr Marine Res, Finnish Environm Inst, POB 140, FI-00251 Helsinki, Finland.	paivi.hakanen@ymparisto.fi	Kremp, Anke/I-8139-2013	Suikkanen, Sanna/0000-0002-0768-8149	Maj and Tor Nessling Foundation; Academy of Finland [128833]; Academy of Finland (AKA) [128833] Funding Source: Academy of Finland (AKA)	Maj and Tor Nessling Foundation; Academy of Finland(Research Council of Finland); Academy of Finland (AKA)(Research Council of Finland)	The authors wish to thank two anonymous reviewers for their constructive criticism, J. Oja for assistance in sampling and K. Erler for part of toxin analyses. 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J	Liu, DY; Shi, YJ; Di, BP; Sun, QL; Wang, YJ; Dong, ZJ; Shao, HB				Liu, Dongyan; Shi, Yajun; Di, Baoping; Sun, Qianli; Wang, Yujue; Dong, Zhijun; Shao, Hongbing			The impact of different pollution sources on modern dinoflagellate cysts in Sishili Bay, Yellow Sea, China	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cyst; Industrial pollution; Nutrient enrichment; Sishili Bay; Yellow Sea	INDUCED OXIDATIVE STRESS; SURFACE TEMPERATURE; YOKOHAMA-PORT; TOKYO-BAY; EUTROPHICATION; SEDIMENTS; PHYTOPLANKTON; DISTRIBUTIONS; INDICATORS	The spatial distribution of dinoflagellate cysts in the surface sediment of Sishili Bay, Yellow Sea, China, was studied, with the purpose of understanding the impact from nutrient enrichment and industrial pollution. Thirty-five dinoflagellate cyst taxa belonging to 15 genera and 3 unknown cysts were identified and quantified at 22 sampling sites. Autotrophic cysts (e.g., Spiniferites bentori var. truncata) and heterotrophic cysts (Brigantedinium sp.1 and Quinquecuspis concreta) dominated the sediment samples. The spatial distribution of cyst abundance showed a significant positive correlation with increased nutrients, but was negative to heavy metal pollution. The highest cyst abundance (with an average of 539 cysts g(-1) DW) occurred in Zone A, corresponding to nutrient enrichment caused by domestic sewage discharge. In contrast, the lowest cyst abundance (with an average of 131 cysts g-1 DW) occurred in Zone E. impacted heavily by the industrial pollution. The abundance of autotrophic cysts decreased dramatically in Zone E compared with heterotrophic cysts and showed a sensitivity to industrial pollution. How heavy metals affect physiological mechanisms in autotrophic and heterotrophic cysts differentially is in need of in-depth study. (C) 2011 Elsevier B.V. All rights reserved.	[Liu, Dongyan; Shi, Yajun; Di, Baoping; Wang, Yujue; Dong, Zhijun; Shao, Hongbing] Chinese Acad Sci, Yantai Inst Coastal Zone Res YIC, Key Lab Coastal Zone Environm Proc, Yantai 264003, Shandong, Peoples R China; [Liu, Dongyan; Shi, Yajun; Di, Baoping; Wang, Yujue; Dong, Zhijun; Shao, Hongbing] Chinese Acad Sci, YIC, Shandong Prov Key Lab Coastal Zone Environm Proc, Yantai 264003, Shandong, Peoples R China; [Shi, Yajun] Chinese Acad Sci, Grad Univ, Beijing 100049, Peoples R China; [Sun, Qianli] E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China	Chinese Academy of Sciences; Yantai Institute of Coastal Zone Research, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS; East China Normal University	Liu, DY (通讯作者)，Chinese Acad Sci, Yantai Inst Coastal Zone Res YIC, Key Lab Coastal Zone Environm Proc, Yantai 264003, Shandong, Peoples R China.	dyliu@yic.ac.cn	wang, yq/F-3244-2012; Qianli, Sun/GYU-4636-2022; Shi, Yajun/GPS-8969-2022; Dong, Zhijun/B-9172-2009	Dong, Zhijun/0000-0001-7692-5892	CAS [KZCX2-YW-Q07-04]; National Natural Science Foundation of China [40976097]; Science and Technology Planning Project of Shandong Province [2011GHY11525]; Yantai Science and Technology Bureau [0931041051]; Marine Special Scientific Fund for Non-Profit Public Industry [200805031]	CAS(Chinese Academy of Sciences); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); Science and Technology Planning Project of Shandong Province; Yantai Science and Technology Bureau; Marine Special Scientific Fund for Non-Profit Public Industry	We appreciate Dr. Kazumi Matsuoka for helping with taxonomic identification. The study was funded by CAS Innovative Programmer (No. KZCX2-YW-Q07-04), National Natural Science Foundation of China (No. 40976097), Science and Technology Planning Project of Shandong Province (No. 2011GHY11525), Yantai Science and Technology Bureau (No. 0931041051) and Marine Special Scientific Fund for Non-Profit Public Industry (No. 200805031).	Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; Bai Y. 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A., 1990, COAST ENG, V9, P35; Zhao Wei-hong, 2001, Chinese Journal of Oceanology and Limnology, V19, P178, DOI 10.1007/BF02863044	48	51	59	2	60	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	MAR	2012	84-85						1	13		10.1016/j.marmicro.2011.11.001	http://dx.doi.org/10.1016/j.marmicro.2011.11.001			13	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	915SJ		Green Published			2025-03-11	WOS:000302047400001
J	Grunert, P; Soliman, A; Coric, S; Roetzel, R; Harzhauser, M; Piller, WE				Grunert, Patrick; Soliman, Ali; Coric, Stjepan; Roetzel, Reinhard; Harzhauser, Mathias; Piller, Werner E.			Fades development along the tide-influenced shelf of the Burdigalian Seaway: An example from the Ottnangian stratotype (Early Miocene, middle Burdigalian)	MARINE MICROPALEONTOLOGY			English	Article						Ottnangian; stratotype; Burdigalian Seaway; facies; micropaleontology; sedimentology	CENTRAL PARATETHYS; BENTHIC FORAMINIFERA; MARINE MOLASSE; DINOFLAGELLATE CYSTS; CALCAREOUS NANNOFOSSILS; SURFACE SEDIMENTS; SALINITY CRISIS; PARALIA-SULCATA; ORGANIC-MATTER; BASIN	Herein, we report quantitative micropaleontological (benthic foraminifers, dinoflagellate cysts, calcareous nannoplankton), sedimentological (grain-size analysis) and geophysical (background gamma radiation) analyses from Ottnang-Schanze, the stratotype for the regional Ottnangian stage (Central Paratethys; Lower Miocene, middle Burdigalian). The revealed trends in bathymetry, primary productivity, bottom-water oxygenation and water energy allow exemplary insights into the paleoenvironment of the terminal Burdigalian Seaway. Several facies of a eutrophic environment are distinguished that reflect a transition from a suboxic outer neritic to upper bathyal towards a better oxygenated middle neritic setting under the influence of storm events and currents. A comparison with available data from Upper Austria and Bavaria consistently shows the regressive trend during the late early Ottnangian. In Upper Austria, the deep-water facies from the lower part of the stratotype represents the most distal sediments. The upper part together with localities closer to the northern coast records inner to middle neritic environments that are heavily affected by tidal currents. The facies distribution results from the progradation of a tide-influenced environment along the northern shelf of the North Alpine Foreland Basin, heralding the closure of the Burdigalian Seaway. The available age estimate for the stratotype constrains the onset of the regressive phase to 18 Ma. (C) 2011 Elsevier B.V. All rights reserved.	[Grunert, Patrick; Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Coric, Stjepan; Roetzel, Reinhard] Geol Survey Austria, A-1030 Vienna, Austria; [Harzhauser, Mathias] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1014 Vienna, Austria	University of Graz	Grunert, P (通讯作者)，Graz Univ, Inst Earth Sci, Heinrichstr 26, A-8010 Graz, Austria.	patrick.grunert@uni-graz.at	Soliman, Ali/R-1583-2018	Grunert, Patrick/0000-0002-3633-8674; Soliman, Ali/0000-0001-7366-4607; Harzhauser, Mathias/0000-0002-4471-6655; Piller, Werner E./0000-0003-2808-4720	Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	The authors would like to thank Ines Galovic (Croatian Geological Survey, Zagreb), Ralph Hinsch (Rohol-Aufsuchungs AG, Vienna), Fred Rogl (Natural History Museum Vienna), Christian Rupp (Geological Survey of Austria, Vienna) and Robert Scholger (University of Leoben) for many helpful comments and discussions. The manuscript benefited from the comments of two anonymous reviewers and Frans Jorissen. Anton Englert and Franz Topka (Natural History Museum Vienna) are acknowledged for assistance with the field-work. Peter Pohn (Wolfsegg) kindly provided access to the outcrop. This study was financially supported by the Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences).	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Micropaleontol.	MAR	2012	84-85						14	36		10.1016/j.marmicro.2011.11.004	http://dx.doi.org/10.1016/j.marmicro.2011.11.004			23	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	915SJ					2025-03-11	WOS:000302047400002
J	Bonnet, S; de Vernal, A; Gersonde, R; Lembke-Jene, L				Bonnet, Sophie; de Vernal, Anne; Gersonde, Rainer; Lembke-Jene, Lester			Modern distribution of dinocysts from the North Pacific Ocean (37-64°N, 144°E-148°W) in relation to hydrographic conditions, sea-ice and productivity	MARINE MICROPALEONTOLOGY			English	Article						North Pacific Ocean; Bering Sea; Okhotsk Sea; Transfer functions; Sea-surface	WALLED DINOFLAGELLATE CYSTS; SOUTHEASTERN BERING-SEA; RECENT MARINE-SEDIMENTS; SUB-ARCTIC PACIFIC; SURFACE SEDIMENTS; ALEUTIAN LOW; SELECTIVE PRESERVATION; BRITISH-COLUMBIA; HIGH-LATITUDES; ASSEMBLAGES	Palynological analyses were performed on 53 surface sediment samples from the North Pacific Ocean, including the Bering and Okhotsk Seas (37-64 degrees N, 144 degrees E-148 degrees W), in order to document the relationships between the dinocyst distribution and sea-surface conditions (temperatures, salinities, primary productivity and sea-ice cover). Samples are characterized by concentrations ranging from 18 to 143816 cysts/cm(3) and the occurrence of 32 species. A canonical correspondence analysis (CCA) was carried out to determine the relationship between environmental variables and the distribution of dinocyst taxa. The first and second axes represent, respectively, 47% and 17.8% of the canonical variance. Axis 1 is positively correlated with all parameters except to the sea-ice and primary productivity in August, which are on the negative side. Results indicate that the composition of dinocyst assemblages is mostly controlled by temperature and that all environmental variables are correlated together. The CCA distinguishes 3 groups of dinocysts: the heterotrophic taxa, the genera Impagidinium and Spiniferites as well as the cyst of Pentapharsodinium dalei and Operculodinium centrocarpum. Five assemblage zones can be distinguished: 1) the Okhotsk Sea zone, which is associated to temperate and eutrophic conditions, seasonal up-wellings and Amur River discharges. It is characterized by the dominance of O. centrocarpum, Brigantedinium spp. and Islandinium minutum; 2) the Western Subarctic Gyre zone with subpolar and mesotrophic conditions due to the Kamchatka Current and Alaska Stream inflows. Assemblages are dominated by Nematosphaeropsis labyrinthus, Pyxidinopsis reticulata and Brigantedinium spp.; 3) the Bering Sea zone, depicting a subpolar environment, influenced by seasonal upwellings and inputs from the Anadyr and Yukon Rivers. It is characterized by the dominance of I. minutum and Brigantedinium spp.; 4) the Alaska Gyre zone with temperate conditions and nutrient-enriched surface waters, which is dominated by N. labyrinthus and Brigantedinium spp. and 5) the Kuroshio Extension-North Pacific-Subarctic Current zone characterized by a subtropical and oligotrophic environment, which is dominated by O. centrocarpum, N. labyrinthus and warm taxa of the genus Impagidinium. Transfer functions were tested using the modem analog technique (MAT) on the North Pacific Ocean (=359 sites) and the entire Northern Hemisphere databases (=1419 sites). Results confirm that the updated Northern Hemisphere database is suitable for further paleoenvironmental reconstructions, and the best results are obtained for temperatures with an accuracy of +/-1.7 degrees C. (C) 2011 Elsevier B.V. All rights reserved.	[Bonnet, Sophie; de Vernal, Anne] Univ Quebec Montreal, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Montreal, PQ H3C 3P8, Canada; [Gersonde, Rainer; Lembke-Jene, Lester] Alfred Wegener Inst Polar & Marine Res AWI, Bremerhaven, Germany	University of Quebec; University of Quebec Montreal; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Bonnet, S (通讯作者)，Univ Quebec Montreal, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	sbrasta1@gmail.com; devernal.anne@uqam.ca; Rainer.Gersonde@awi.de; Lester.Lembke-Jene@awi.de	Lembke-Jene, Lester/ABC-6275-2020; de Vernal, Anne/D-5602-2013; Lembke-Jene, Lester/F-5084-2013	de Vernal, Anne/0000-0001-5656-724X; Lembke-Jene, Lester/0000-0002-6873-8533	German Ministry of Education and Science (Bundesministerium fir Bildung und Forschung); European Union [243908]; Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT); Natural Sciences and Engineering Research Council of Canada (NSERC)	German Ministry of Education and Science (Bundesministerium fir Bildung und Forschung); European Union(European Union (EU)); Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This study is a contribution to the international INOPEX (Innovative NOrth Pacific EXperiment) project funded by the German Ministry of Education and Science (Bundesministerium fir Bildung und Forschung) and led by the Alfred Wegener Institute for Polar and Marine Research (Bremerhaven, Germany). This is also a Past4Future contribution n<SUP>o</SUP>15. The research leading to these results has received funding from the European Union's Seventh Framework programme (FP7/2007-2013) under grant agreement no 243908, "Past4Future. Climate change - Learning from the past climate. Additional financial support was provided by the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) and the Natural Sciences and Engineering Research Council of Canada (NSERC). We wish to thank the Captain of the German ship RN Sonne, Lutz Mallon, as well as the crew members for their remarkable work, their support for the sampling and their good humor. We are also grateful to Maryse Henry (Geotop-UQAM) for her help in the laboratory and the management of the Northern Hemisphere dinocyst reference database, Taoufik Radi (Geotop-UQAM) for the dinocyst taxonomy in the North Pacific Ocean and Charles Gobeil for providing samples from the Bering Sea (SLIP#1, #2, #4). We appreciate comments and suggestions from the regional editor, Richard Jordan, and the three reviewers: Arun Kumar, Vera Pospelova and Fabienne Marret.	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Micropaleontol.	MAR	2012	84-85						87	113		10.1016/j.marmicro.2011.11.006	http://dx.doi.org/10.1016/j.marmicro.2011.11.006			27	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	915SJ					2025-03-11	WOS:000302047400006
J	Sliwinska, KK; Abrahamsen, N; Beyer, C; Brünings-Hansen, T; Thomsen, E; Ulleberg, K; Heilmann-Clausen, C				Sliwinska, Katarzyna K.; Abrahamsen, Niels; Beyer, Claus; Brunings-Hansen, Thomas; Thomsen, Erik; Ulleberg, Kaare; Heilmann-Clausen, Claus			Bio- and magnetostratigraphy of Rupelian-mid Chattian deposits from the Danish land area	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; magnetostratigraphy; benthic foraminifera; calcareous nannofossils; Rupelian; Chattian	NORTH-SEA BASIN; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; UMBRIA-MARCHE BASIN; CALCAREOUS NANNOPLANKTON; RESEARCH BOREHOLE; LOWER MIOCENE; OLIGOCENE; STRATIGRAPHY; SEQUENCE; FORAMINIFERA	The age of the lithostratigraphic units in the Oligocene succession of Denmark is not well known. In order to remedy this situation, an integrated bio-magnetostratigraphical study of the Rupelian-mid Chattian deposits was carried out on six key sections situated in central Jutland. The studied sections include all previously known lithostratigraphical units (i.e., the Grundfor and Viborg Clay Members of the Viborg Formation, Linde Clay, Hvorslev Clay, Branden Clay) and a new, informal Unit X. The biostratigraphical part of the paper critically discusses the differences in ranges of some dinoflagellate cysts in relation to the two most commonly applied dinocyst zonations, the D- and NSO-zonation. The local calcareous nannofossil zonation of the upper NP23-lower NP25 interval in the studied sections is correlated to the standard NP zonation via the Contessa Barbetti Road section in central Italy. The correlation shows that an interval of the range of the dinoflagellate cyst Svalbardella recognized within the lower Chattian Asterigerina guerichi guerichi Zone in Denmark and Belgium is coeval with the global Oi2b cooling event. The identified magnetic polarity intervals have been correlated with the global polarity time scale on the basis of the biostratigraphy. The Viborg Formation is thus referred to Chron C13n and the lowermost part of C12r; the Linde Clay is referred to lower Chron C12r; and the Hvorslev Clay is referred to Chron Cl1n, C10 and C9r, or only the Cl1n.ln-Cl0r interval. The Branden Clay is referred to Chron C9r, C9n and C8r. Unit X is referred to Chron C8n. (C) 2012 Elsevier BM. All rights reserved.	[Sliwinska, Katarzyna K.; Abrahamsen, Niels; Thomsen, Erik; Heilmann-Clausen, Claus] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Beyer, Claus] CB Magneto, DK-8670 Lasby, Denmark; [Brunings-Hansen, Thomas] Nat Styrelsen, Miljominist, DK-6760 Ribe, Denmark	Aarhus University	Sliwinska, KK (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	kasia.sliwinska@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; Thomsen, Erik/A-4842-2012; Abrahamsen, Niels/A-3553-2012; Sliwinska, Kasia K./G-9097-2018	Sliwinska, Kasia K./0000-0001-5488-8832	Det Frie Forskningsrad - Natur og Univers (FNU) [272-08-0256]; Aarhus University; Fur Museum (Denmark)	Det Frie Forskningsrad - Natur og Univers (FNU); Aarhus University; Fur Museum (Denmark)	Kirsten Rosendal (Dept. of Geoscience, AU) prepared palynological and calcareous nannofossil slides. Daniel C. Heubeck (DG, AU) washed foraminifera samples. 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Palaeobot. Palynology	FEB 15	2012	172						48	69		10.1016/j.revpalbo.2012.01.008	http://dx.doi.org/10.1016/j.revpalbo.2012.01.008			22	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	921CU					2025-03-11	WOS:000302456400005
J	Naidu, PD; Patil, JS; Narale, DD; Anil, AC				Naidu, P. Divakar; Patil, Jagadish S.; Narale, Dhiraj D.; Anil, A. C.			A first look at the dinoflagellate cysts abundance in the Bay of Bengal: implications on Late Quaternary Productivity and climate change	CURRENT SCIENCE			English	Article						Climate change; Cyst abundance and composition; dinoflagellates; geological past	ARABIAN SEA; INTERGLACIAL CONTRASTS; SEDIMENTS; RECORD; PALEOPRODUCTIVITY; FLUCTUATIONS; INDICATORS; FLUXES; CARBON; ALASKA	Abundance and composition of dinoflagellate cysts in a sediment core (SK218/1) from the Bay of Bengal were examined for the last 23 kyr. Cyst abundance at this site varied from 20 to 153 cysts/g dry wt, which is far less than that reported from other oceans. The Holocene harboured higher number of cysts (74-153 cysts/g dry wt) than the last glacial period (up to 67 cysts/g dry wt). Although cyst abundance is low at this site, the cyst composition and its abundance between Holocene and last glacial period reflect the affinity to climate change between these two periods, like other regions. Greater abundance of heterotroph and autotroph cysts and higher species diversity were noticed during Holocene than in the last glacial period, which supports earlier observations depicting higher productivity during the Holocene than in the last glacial period in the southwest monsoon-influenced regions of the India Ocean	[Naidu, P. Divakar; Patil, Jagadish S.; Narale, Dhiraj D.; Anil, A. C.] Natl Inst Oceanog CSIR, Panaji 403004, Goa, India	Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO)	Naidu, PD (通讯作者)，Natl Inst Oceanog CSIR, Panaji 403004, Goa, India.	divakar@nio.org	Naidu, Pothuri/AAH-1613-2019		ISRO-GBP; Ministry of Earth Sciences, Government of India	ISRO-GBP; Ministry of Earth Sciences, Government of India	We thank Dr Shetye, Director, National Institute of Oceanography, Goa for providing the necessary facilities and encouragement, and the anonymous reviewer for constructive comments. This work is financially supported by ISRO-GBP and Ministry of Earth Sciences, Government of India. This is National Institute of Oceanography Contribution No. 5107.	Bhushan R, 2001, MAR GEOL, V178, P95, DOI 10.1016/S0025-3227(01)00179-7; Curry W.B., 1992, Geological Society Special Publication, P93; D'Costa PM, 2008, ESTUAR COAST SHELF S, V77, P77, DOI 10.1016/j.ecss.2007.09.002; de Vernal A, 1997, PALEOCEANOGRAPHY, V12, P821, DOI 10.1029/97PA02167; DUPLESSY JC, 1982, NATURE, V295, P494, DOI 10.1038/295494a0; Gauns M, 2005, DEEP-SEA RES PT II, V52, P2003, DOI 10.1016/j.dsr2.2005.05.009; Godhe A, 2000, BOT MAR, V43, P39, DOI 10.1515/BOT.2000.004; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Hegde S, 2008, MAR ECOL PROG SER, V356, P93, DOI 10.3354/meps07259; HERGUERA JC, 1991, GEOLOGY, V19, P1173, DOI 10.1130/0091-7613(1991)019<1173:PFBFAG>2.3.CO;2; Mao Shaozhi, 1993, Palynology, V17, P47; Marret F, 2001, CAN J EARTH SCI, V38, P373, DOI 10.1139/e00-092; Marret F, 2009, QUATERN INT, V197, P72, DOI 10.1016/j.quaint.2007.01.010; Matsuoka K., 1989, P461; Matsuoka K., 2000, WESTPACHABWESTPACIOC, P1; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; Murray D.W., 1992, GEOL SOC SPEC PUBL L, V64, P301; Naidu PD, 2010, J QUATERNARY SCI, V25, P1138, DOI 10.1002/jqs.1392; Naidu PD, 1996, PALEOCEANOGRAPHY, V11, P129, DOI 10.1029/95PA03198; NAIDU PD, 1991, PALAEOGEOGR PALAEOCL, V86, P255, DOI 10.1016/0031-0182(91)90084-5; NAIDU PD, 1993, PALAEOGEOGR PALAEOCL, V103, P21; Pattan JN, 2003, PALAEOGEOGR PALAEOCL, V193, P575, DOI 10.1016/S0031-0182(03)00267-0; Pospelova V, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001251; Prell W.L., 1992, Synthesis of results from scientific drilling in the Indian Ocean, V70, P447, DOI [10.1029/gm070p0447, DOI 10.1029/GM070P0447]; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Reichart GJ, 2003, MAR MICROPALEONTOL, V49, P303, DOI 10.1016/S0377-8398(03)00050-1; Rochon A., 1999, AASP Contributions series, V35, P150; Rostek F, 1997, DEEP-SEA RES PT II, V44, P1461, DOI 10.1016/S0967-0645(97)00008-8; 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; 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]; Zonneveld KAF, 2000, DEEP-SEA RES PT II, V47, P2229, DOI 10.1016/S0967-0645(00)00023-0; ZONNEVELD KAF, 1995, REV PALAEOBOT PALYNO, V84, P221, DOI 10.1016/0034-6667(94)00117-3	33	7	8	0	5	INDIAN ACAD SCIENCES	BANGALORE	C V RAMAN AVENUE, SADASHIVANAGAR, P B #8005, BANGALORE 560 080, INDIA	0011-3891			CURR SCI INDIA	Curr. Sci.	FEB 10	2012	102	3					495	499						5	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	896CZ					2025-03-11	WOS:000300544300026
J	Rouis-Zargouni, I; Turon, JL; Londeix, L; Kallel, N; Essallami, L				Rouis-Zargouni, Imene; Turon, Jean-Louis; Londeix, Laurent; Kallel, Nejib; Essallami, Latifa			The last glacial-interglacial transition and dinoflagellate cysts in the western Mediterranean Sea	COMPTES RENDUS GEOSCIENCE			English	Article						Dinoflagellate cysts; Younger Dryas; Bolling/Allerod; Western Mediterranean; Nematosphaeropsis labyrinthus	RADIOCARBON AGE CALIBRATION; NORTHERN NORTH-ATLANTIC; HIGH-RESOLUTION RECORD; MILLENNIAL-SCALE; SURFACE CONDITIONS; LAKE AGASSIZ; DEGLACIATION; MARINE; HOLOCENE; SEDIMENTS	Using the analysis of dinoflagellate cysts in three deep-sea sediments cores situated in the Sicilian-Tunisian Strait, in the Gulf of Lions and in the Alboran Sea, we reconstruct the paleoenvironmental changes that took place during the last glacial-interglacial transition in the western Mediterranean Sea. The development of the warm microflora Impagidinium aculeatum and especially Spiniferites mirabilis appears to be an important proxy lot recognizing warm periods as the Bolling/Allerod and the Early Holocene. Bitectatodinium tepikiense, Spiruferites elongatus and Nematosphaeropsis labyrinth us mark the end of the Heinrich event 1 and the Younger Dryas. This cold microfloral association confirms the drastic climate changes in the western Mediterranean Sea synchronous to the dry and cold climate which occurred in the South European margin. The dinocyst N. labyrinthus shows high percentages in all studied regions during the Younger Dryas. Its distribution reveals a significant increase from the South to the North of this basin during this cold brief event. Thus, we note that this species can be considered as a new ecostratigraphical tracer of the Younger Dryas in the western Mediterranean Sea. (C) 2012 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.	[Rouis-Zargouni, Imene; Kallel, Nejib; Essallami, Latifa] Fac Sci Sfax, Lab GEOGLOB, Sfax 3028, Tunisia; [Rouis-Zargouni, Imene; Turon, Jean-Louis; Londeix, Laurent] Univ Bordeaux 1, UMR EPOC 5805, F-33405 Talence, France	Universite de Sfax; Faculty of Sciences Sfax; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux	Rouis-Zargouni, I (通讯作者)，Fac Sci Sfax, Lab GEOGLOB, Route Soukra,BP 802, Sfax 3028, Tunisia.	imenerouis@ymail.com; Jl.turon@epoc.u-bordeaux.fr; Llondeix@epoc.u-bordeaux.fr; nejib.kallel@fss.rnu.tn; ess_latifa@yahoo.fr			Institut National des Sciences de l'Univers (INSU) of the Centre National de la Recherche Scientifique (CNRS); RV Marion-Dufresne; IMAGES; Institut Paul-Emile-Victor (IPEV)	Institut National des Sciences de l'Univers (INSU) of the Centre National de la Recherche Scientifique (CNRS); RV Marion-Dufresne; IMAGES; Institut Paul-Emile-Victor (IPEV)	The authors thank the Institut National des Sciences de l'Univers (INSU) of the Centre National de la Recherche Scientifique (CNRS), the RV Marion-Dufresne officers and crew, the IMAGES program and the Institut Paul-Emile-Victor (IPEV) for support and organisation of the coring cruises (GINNA, GEOSCIENCES, PRIVILEGE). 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R. Geosci.	FEB	2012	344	2					99	109		10.1016/j.crte.2012.01.002	http://dx.doi.org/10.1016/j.crte.2012.01.002			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	921UV		hybrid			2025-03-11	WOS:000302504400005
J	Razumkova, ES				Razumkova, E. S.			Palynological Characterization of the Sarmatian Deposits of the Eastern Paratethys (Section Zelenskii Mountain-Cape Panagiya, Taman Peninsula)	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Neogene; Sarmatian Regional Stage; Eastern Parathetys; Taman Peninsula; spores and pollen; dinocysts	UPPER MIOCENE; DINOFLAGELLATE; MIDDLE	Palynological analysis of Sarmatian deposits found in the reference section Zelenskii Mountain-Cape Panagiya has produced new data on dinocysts and contributed to the palynological characteristics of the Sarmatian deposits of the Taman Peninsula. Six palynological assemblages have been found, reflecting the gradual replacement of forest associations with forest-steppe ones, and thus confirming the trend, revealed earlier, of climate aridization in the areas of the Eastern and Central Paratethys in the Late Sarmatian time. The distinctive cysts of the dinoflagellates Geonettia cf. clinea de Verteuil et Norris and Polykrikos schwarzii Butschli are identified in Sarmatian deposits of the Taman Peninsula for the first time.	Geologorazvedka Fed State Unitary Sci & Ind Enter, St Petersburg 192019, Russia		Razumkova, ES (通讯作者)，Geologorazvedka Fed State Unitary Sci & Ind Enter, Ul Knipovicha 11-2, St Petersburg 192019, Russia.	elena.razumkova@gmail.com		Razumkova, Elena/0000-0003-1856-9492	Netherlands Organization for Scientific Research [047.017.005/05-05-89000]; Russian Foundation for Basic Research [047.017.005/05-05-89000]	Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO)); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	This study was supported by the Netherlands Organization for Scientific Research and Russian Foundation for Basic Research, joint project no. 047.017.005/05-05-89000.	Akgun Funda, 2000, Turkish Journal of Earth Sciences, V9, P57; de Verteuil Laurent, 1997, Proceedings of the Ocean Drilling Program Scientific Results, V150X, P129; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P263, DOI 10.2307/1485875; Filippova N., 2002, STRATIGR GEOL CORREL, V10, P80; Filippova N.Yu., PALINOLOGIA STRATIGR, V2, P29; Filippova N.Yu., 2009, AKTUALNYE PROBLEMY N, P136; Goncharova I., 2009, AKT PROBL NEOG CHETV, P47; Ivanov D, 2002, PALAEOGEOGR PALAEOCL, V178, P19, DOI 10.1016/S0031-0182(01)00365-0; Jiménez-Moreno G, 2006, J MICROPALAEONTOL, V25, P113, DOI 10.1144/jm.25.2.113; Louwye S, 2007, GEOL MAG, V144, P33, DOI 10.1017/S0016756806002627; Nevesskaya LA, 2004, OBYASNITELNAYA ZAPIS; Panova L.A., PRAKTICHESKAYA PALIN, P183; Popov S.V., 1998, OPORNYE RAZREZY NEOG; Razumkova E.S., 2008, 19 VSER NAUCHN K STU, P38; Rochon Andre, 1999, AASP Contributions Series, V35, P1; Vernigorova Yu, 2006, PROBLEMY PALEONTOLOG, P231; Zaporozhets N.I., 1998, ORGANIKOSTENNYI FITO; Zaporozhets NI, 1999, STRATIGR GEOL CORREL, V7, P161	18	5	5	0	1	PLEIADES PUBLISHING INC	MOSCOW	PLEIADES PUBLISHING INC, MOSCOW, 00000, RUSSIA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	FEB	2012	20	1					97	108		10.1134/S0869593811060049	http://dx.doi.org/10.1134/S0869593811060049			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	920BW					2025-03-11	WOS:000302377400006
J	Soliman, A				Soliman, Ali			Oligocene dinoflagellate cysts from the North Alpine Foreland Basin: new data from the Eggerding Formation (Austria)	GEOLOGICA CARPATHICA			English	Article						Oligocene; Austria; North Alpine Foreland Basin; Eggerding Formation; paleoenvironment; dinocysts	LATE EOCENE; FLYSCH DEPOSITS; MOLASSE BASIN; LOWER MIOCENE; SOURCE ROCKS; STRATIGRAPHY; BIOSTRATIGRAPHY; SUCCESSION; BOUNDARY; WELL	In spite of detailed geological and geophysical investigations, information available on palynostratigraphy for the successions deposited in the Austrian part of the North Alpine Foreland Basin (NAFB) is scanty. For the first time, relatively diverse and well preserved Oligocene dinocyst assemblages, comprising 53 genera and 138 species, are presented from the organic-rich sediments of the Eggerding Formation. These assemblages contribute to the biostratigraphy of the Oligocene deposits within the NAFB. Dinocysts such as Chiropteridium lobospinosum, Membranophoridium aspinatum, Cordosphaeridium spp., Enneadocysta spp., Deflandrea spp., Spiniferites/Achomosphaera group, Hystrichokolpoma spp., Apteodinium spp., Glaphyrocysta/Areoligera complex and Wetzeliella spp. represent the main palynological elements. The occurrence of Chiropteridium spp., Tuberculodinium vancampoae, Distatodinium biffii and Wetzeliella gochtii is of particular importance for regional correlations within the Lower Oligocene sediments. A comparison with age-controlled assemblages from the North Sea Basin, Carpathian and circum-Mediterranean regions substantiate the attribution to the Rupelian. Lack or sporadic occurrence of the oceanic taxa (e.g. Nematosphaeropsis and Impagidinium) and dominance of Glaphyrocysta/Areoligera indicate an inner-neritic marine setting during the deposition of the studied intervals. Although, it is difficult to reconstruct precisely the climatic conditions based on the recorded dinocysts, warm? sea surface water is suggested. A variation in salinities is interpreted based on the abundances of Homotryblium spp. The abundance of Peridiniaceae taxa (e.g. Lejeunecysta, Wetzeliella, and Deflandrea) indicates nutrient-rich surface water.	[Soliman, Ali] Karl Franzens Univ Graz, Inst Erdewissensch Geol & Palaontol, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Dept Geol, Fac Sci, Tanta 31527, Egypt	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University	Soliman, A (通讯作者)，Karl Franzens Univ Graz, Inst Erdewissensch Geol & Palaontol, Heinrichstr 26, A-8010 Graz, Austria.	ali.soliman@uni-graz.at	Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607	OWA; FWF [21414-B16]	OWA; FWF(Austrian Science Fund (FWF))	Reinhard Sachsenhofer (Leoben) and Rohol-Aufsuchung AG (RAG) are thanked for the well data and samples. I am deeply indebted to Drs. W. Piller (Graz) and S. Torricelli (Milan) for their helpful comments on the early version. I gratefully acknowledge the constructive reviews of P. Gedl (Krakow) and the two anonymous reviewers. This work is supported by the OWA and FWF (Project No. 21414-B16).	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Carpath.	FEB	2012	63	1					49	70		10.2478/v10096-012-0004-8	http://dx.doi.org/10.2478/v10096-012-0004-8			22	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	911VS		gold			2025-03-11	WOS:000301748900004
J	Kern, AK; Harzhauser, M; Soliman, A; Piller, WE; Gross, M				Kern, Andrea K.; Harzhauser, Mathias; Soliman, Ali; Piller, Werner E.; Gross, Martin			Precipitation driven decadal scale decline and recovery of wetlands of Lake Pannon during the Tortonian	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						High resolution analysis; Pollen; Tortonian; Paleoclimate; Paleoenvironment; Plant-climate-interaction	WALLED DINOFLAGELLATE CYSTS; LATE MIOCENE CLIMATE; SURFACE SEDIMENTS; QUANTITATIVE-ANALYSIS; CENTRAL-EUROPE; SALT-MARSH; SEA; POLLEN; WATER; VEGETATION	High resolution pollen and dinoflagellate analyses were performed on a continuous 98-cm-long core from Tortonian deposits of Lake Pannon in the Styrian Basin in Austria. The sample distance of 1-cm corresponds to a resolution of roughly one decade, allowing insights into environmental and climatic changes over a millennium of Late Miocene time. Shifts in lake level, surface water productivity on a decadal- to centennialscale can be explained by variations of rainfall during the Tortonian climatic optimum. Related to negative fine scale shifts of mean annual precipitation, shoreline vegetation belts reacted in an immediate replacement of Poaceae by Cyperaceae as dominant grasses in the marshes fringing the lake. In contrast to such near-synchronous ecosystem-responses to precipitation, a delayed lake level rise of 4-6 decades is evident in the hydrological budget of Lake Pannon. This transgression, caused by a precipitation increase up to > 1200 mm/yr, resulted in a complete dieback of marshes. Simultaneously, "open-water" dinofiagellates, such as Impagidinium, took over in the brackish lagoon and fresh water dinollagellates disappeared. As soon as the rainfall switched back to moderate levels of - 1100-1200 mm/yr, the rise of the lake level slowed down, the marsh plants could keep up again and the former vegetation belts became re-established. Thus, mean annual precipitation, more than temperature, was the main driving force for high-frequency fluctuations in the Tortonian wetlands and surface water conditions of Lake Pannon. Such high resolution studies focusing on Tortonian decadal to centennial climate change will be crucial to test climate models which try to compare the Tortonian models with predictions for future climate change. (C) 2011 Elsevier B.V. All rights reserved.	[Kern, Andrea K.; Harzhauser, Mathias] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1010 Vienna, Austria; [Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Gross, Martin] Universalmuseum Joanneum, Abt Geol & Palaontol, A-8045 Graz, Austria	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University	Kern, AK (通讯作者)，Nat Hist Museum Vienna, Geol Paleontol Dept, Burgring 7, A-1010 Vienna, Austria.	andrea.kern@nhm-wien.ac.at	Soliman, Ali/R-1583-2018; Kern, Andrea K./V-5078-2017	Soliman, Ali/0000-0001-7366-4607; Piller, Werner E./0000-0003-2808-4720; Gross, Martin/0000-0002-5113-6069; Harzhauser, Mathias/0000-0002-4471-6655; Kern, Andrea K./0000-0002-9343-0696	FWF [P21414-B16, P21748-N21]; Austrian Science Fund (FWF) [P21414, P21748] Funding Source: Austrian Science Fund (FWF)	FWF(Austrian Science Fund (FWF)); Austrian Science Fund (FWF)(Austrian Science Fund (FWF))	The study was supported by the FWF-grants P21414-B16 (Millennialto centennial-scale vegetation dynamics and surface water productivity during the Late Miocene in and around Lake Pannon) and P21748-N21 (Evolution and Phylogeny in Cyprideis, Ostracoda). 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Paleoclimatol. Paleoecol.	FEB 1	2012	317						1	12		10.1016/j.palaeo.2011.11.021	http://dx.doi.org/10.1016/j.palaeo.2011.11.021			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	904QF	23576820	hybrid, Green Published			2025-03-11	WOS:000301212300001
J	Versteegh, GJM; Blokker, P; Bogus, KA; Harding, IC; Lewis, J; Oltmanns, S; Rochon, A; Zonneveld, KAF				Versteegh, Gerard J. M.; Blokker, Peter; Bogus, Kara A.; Harding, Ian C.; Lewis, Jane; Oltmanns, Sven; Rochon, Andre; Zonneveld, Karin A. F.			Infra red spectroscopy, flash pyrolysis, thermally assisted hydrolysis and methylation (THM) in the presence of tetramethylammonium hydroxide (TMAH) of cultured and sediment-derived <i>Lingulodinium polyedrum</i> (Dinoflagellata) cyst walls	ORGANIC GEOCHEMISTRY			English	Article							CELL-WALL; CHEMICAL-STRUCTURE; SPOROPOLLENIN BIOSYNTHESIS; POLLEN; ALGAENANS; PRODUCTS; SPECTROMETRY; DEGRADATION; MICROALGAE; CELLULOSE	The macromolecular composition of dinoflagellate cyst walls is poorly understood and is usually referred to as 'sporopollenin-like'. We have carried out micro-Fourier transform infra red (micro-FTIR) analysis of chemically untreated sediment-derived and enzymatically and chemically purified culture-derived Lingulodinium polyedrum cyst walls, which suggests an aliphatic polymer rich in C-O bonds and relatively poor in CH2 and CH3 groups, and which is much closer to cellulose than to sporopollenin or algaenan. This is in agreement with flash pyrolysis-gas chromatography-mass spectrometry (py-GC-MS), with and without tetramethylammonium hydroxide (TMAH) of purified culture derived cyst walls, which indicated an oxygen-rich polymer without normal or isoprenoid carbon chains. The results support a strongly cross-linked carbohydrate-based polymer and as such confirm earlier hypotheses that the cysts were unlike algaenan or sporopollenin, contrasting with the suggestion that the cyst walls were highly aromatic and contained tocopherol as a major monomeric building block. (C) 2011 Elsevier Ltd. All rights reserved.	[Versteegh, Gerard J. M.; Zonneveld, Karin A. F.] Univ Bremen, Kerogen Grp, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Versteegh, Gerard J. M.; Bogus, Kara A.; Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; [Blokker, Peter] Nalco Europe BV, Water R&D Europe, NL-2342 BV Oegstgeest, Netherlands; [Harding, Ian C.] Univ Southampton, Natl Oceanog Ctr Southampton, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England; [Lewis, Jane] Univ Westminster, Sch Biosci, London W1W 6UW, England; [Oltmanns, Sven] Bruker Opt GmbH, D-28359 Bremen, Germany	University of Bremen; University of Bremen; University of Southampton; NERC National Oceanography Centre; University of Westminster	Versteegh, GJM (通讯作者)，Univ Bremen, Kerogen Grp, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany.	versteegh@uni-bremen.de	Harding, Ian/K-3320-2012; Versteegh, Gerard J.M./H-2119-2011	Harding, Ian/0000-0003-4281-0581; Bogus, Kara/0000-0003-4690-0576; Versteegh, Gerard J.M./0000-0002-9320-3776	German Science Foundation (DFG) [VE-486/2 and /3]; Dutch Science Foundation (NWO); Natural Environmental Research Council (NERC)	German Science Foundation (DFG)(German Research Foundation (DFG)); Dutch Science Foundation (NWO)(Netherlands Organization for Scientific Research (NWO)); Natural Environmental Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We thank J. de Leeuw (Royal NIOZ) for constructive comments on an earlier version of the manuscript, and J.S. Watson and two anonymous reviewers for constructive comments. Financial support from the German Science Foundation (DFG) to G.J.M.V. (VE-486/2 and /3) and K.B. (EUROPROX), the Dutch Science Foundation (NWO) to P.B. and the Natural Environmental Research Council (NERC) to A.R. is gratefully acknowledged.	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Geochem.	FEB	2012	43						92	102		10.1016/j.orggeochem.2011.10.007	http://dx.doi.org/10.1016/j.orggeochem.2011.10.007			11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	885XP					2025-03-11	WOS:000299815000010
J	Anderson, DM; Alpermann, TJ; Cembella, AD; Collos, Y; Masseret, E; Montresor, M				Anderson, Donald M.; Alpermann, Tilman J.; Cembella, Allan D.; Collos, Yves; Masseret, Estelle; Montresor, Marina			The globally distributed genus <i>Alexandrium</i>: Multifaceted roles in marine ecosystems and impacts on human health	HARMFUL ALGAE			English	Review						Alexandrium; Harmful algal blooms; HAB; Biotoxins; Public health; Global dispersion	HARMFUL ALGAL BLOOMS; SP-NOV DINOPHYCEAE; REAL-TIME PCR; DINOFLAGELLATE GONYAULAX-TAMARENSIS; POPULATION GENETIC-STRUCTURE; SPECIES COMPLEX DINOPHYCEAE; DISSOLVED ORGANIC-CARBON; SMALL-SCALE TURBULENCE; TOXIC DINOFLAGELLATE; LIFE-HISTORY	The dinoflagellate genus Alexandrium is one of the major harmful algal bloom (HAB) genera with respect to the diversity, magnitude and consequences of blooms. The ability of Alexandrium to colonize multiple habitats and to persist over large regions through time is testimony to the adaptability and resilience of this group of species. Three different families of toxins, as well as an as yet incompletely characterized suite of allelochemicals are produced among Alexandrium species. Nutritional strategies are equally diverse, including the ability to utilize a range of inorganic and organic nutrient sources, and feeding by ingestion of other organisms. Many Alexandrium species have complex life histories that include sexuality and often, but not always, cyst formation, which is characteristic of a meroplanktonic life strategy and offers considerable ecological advantages. Due to the public health and ecosystem impacts of Alexandrium blooms, the genus has been extensively studied, and there exists a broad knowledge base that ranges from taxonomy and phylogeny through genomics and toxin biosynthesis to bloom dynamics and modeling. Here we present a review of the genus Alexandrium, focusing on the major toxic and otherwise harmful species. (C) 2011 Elsevier B.V. All rights reserved.	[Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Alpermann, Tilman J.] Senckenberg Res Inst, LOEWE Biodivers & Climate Res Ctr BiK F, D-60325 Frankfurt, Germany; [Cembella, Allan D.] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Collos, Yves; Masseret, Estelle] Univ Montpellier 2, CNRS, IRD, UMR 5119,UM2,UM1, F-34095 Montpellier, France; [Montresor, Marina] Stn Zool Anton Dohrn, I-80121 Naples, Italy	Woods Hole Oceanographic Institution; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Universite de Montpellier; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Stazione Zoologica Anton Dohrn	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, MS 32,266 Woods Hole Rd, Woods Hole, MA 02543 USA.	danderson@whoi.edu; Tilman.Alpermann@senckenberg.de; Allan.Cembella@awi.de; yves.collos@univ-montp2.fr; estelle.masseret@univ-montp2.fr; marina.montresor@szn.it	Alpermann, Tilman/JGE-0512-2023	Masseret, Estelle/0000-0001-6856-8637; Montresor, Marina/0000-0002-2475-1787; Cembella, Allan/0000-0002-1297-2240	National Institute of Environmental Health Sciences [1-P50-ES012742]; National Science Foundation through the Woods Hole Center for Oceans and Human Health [OCE-0430724]; NOAA [NA09NOS4780193, NA06OAR4170021, NA06NOS4780245]; Helmholtz Society initiative Earth and Environment; Hesse's Ministry of Higher Education, Research, and the Arts; French National Programme "Ecosphere Continentale et Cotiere-EC2CO"; Fondation pour la Recherche sur la Biodiversite-INVALEX [AAP-IN-2009-036]; ECOHAB [673]; Directorate For Geosciences; Division Of Ocean Sciences [0911031] Funding Source: National Science Foundation	National Institute of Environmental Health Sciences(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); National Science Foundation through the Woods Hole Center for Oceans and Human Health; NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Helmholtz Society initiative Earth and Environment; Hesse's Ministry of Higher Education, Research, and the Arts; French National Programme "Ecosphere Continentale et Cotiere-EC2CO"; Fondation pour la Recherche sur la Biodiversite-INVALEX; ECOHAB; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Support to DMA was provided by the National Institute of Environmental Health Sciences (1-P50-ES012742) and the National Science Foundation through the Woods Hole Center for Oceans and Human Health (OCE-0430724), and by NOAA Grants NA09NOS4780193, NA06OAR4170021 and NA06NOS4780245. Research funding to ADC and previously to TJA was furnished under the PACES Programme (Coast WP2) from the Helmholtz Society initiative Earth and Environment. Support to TJA was obtained by the research funding program LOEWE (Landes-Offensive zur Entwicklung Wissenschaftlich-okonomischer Exzellenz) of Hesse's Ministry of Higher Education, Research, and the Arts. Support to EM and YC was provided by grants from the French National Programme "Ecosphere Continentale et Cotiere-EC2CO and from the "Fondation pour la Recherche sur la Biodiversite-INVALEX project (AAP-IN-2009-036). This is ECOHAB contribution number 673. 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J	Imai, I; Yamaguchi, M				Imai, Ichiro; Yamaguchi, Mineo			Life cycle, physiology, ecology and red tide occurrences of the fish-killing raphidophyte <i>Chattonella</i>	HARMFUL ALGAE			English	Review						Chattonella; Cyst; Life cycle; Bloom ecology; Diatom; Red tide	SETO INLAND SEA; BACTERIUM CYTOPHAGA SP; ANTIQUA HADA ONO; MARINA RAPHIDOPHYCEAE; OVATA RAPHIDOPHYCEAE; HETEROSIGMA-AKASHIWO; ALGICIDAL BACTERIA; SUPEROXIDE ANION; NOV DICTYOCHOPHYCEAE; VERTICAL MIGRATION	The marine fish-killing raphidophytes of the genus Chattonella currently consist of five species, i.e. C. antiqua, C. marina, C. minima, C. ovata and C subsalasa. The distribution of Chattonella species was confirmed in tropical, subtropical and temperate regions in the world accompanying mass mortalities of fishes in nature and in aquaculture. The fish-killing mechanisms are still unclear, but suffocation is the ultimate cause of fish death. Increasing evidence is pointing towards the generation of reactive oxygen species (ROS, e.g. superoxide), which are responsible for the gill tissue injury and mucus production that leads to death of fishes. A taxonomic revision was proposed based on morphology and genetic diversity that Chattonella antiqua and Chattonella ovata should be varieties of Chattonella marina possessing nomenclatural priority. Optimum temperatures for growth are 25 degrees C for C. antiqua and C. marina, 25-30 degrees C for C. ovata and 20-30 degrees C for Chattonelia subsalsa. Adequate ranges of salinity for growth were about 20-30 for Chattonella species. Chattonella cells generally divide once a day. Laboratory culture experiments with artificial synthetic medium demonstrated that C antiqua, C. marina and C ovata used only Fe chelated with EDTA for growth, although tested diatoms and dinoflagellates used rather many kinds of chelated Fe. A suitable concentration of humic acid supplied with iron also had enhancing effects on the growth of C. antiqua. Diel vertical migration was observed in Chattonella, and the cells reached 7.5 m deep at night in the case of C. antiqua demonstrated by a mesocosm experiment in the Seto Inland Sea. Chattonella species have diplontic life history and have haploid cyst stage in their life cycle. Encystment was observed through formation of pre-encystment small cells after the depletion of nitrogen, and the small cells sink to the sea bottom to complete cyst formation by attachment to the solid surface such as diatom frustules and sand grains. Newly formed cysts are in the state of spontaneous dormancy and they need cold temperature period of four months or longer for maturation (acquisition of germination ability). Cysts germinate in early summer and resultant vegetative cells play an important role as seed populations in blooming in the summer season. However, relatively small part of cyst populations actually germinate from bottom sediments, and success of red tide formation is dependent on the growth in water columns. Since red tides of Chattonella were observed when diatoms were scarce in seawater, diatoms appear to have a key for the predominance of Chattonella in water columns. Diatom resting stages in sediments need light for germination/rejuvenation, whereas Chattonella cysts can germinate even in the dark, implying the selective germination of Chattonella cysts at the sea bottom under calm oceanographic conditions which contribute to bloom formation of Chattonella. As a mechanism of red tide occurrences of Chattonella in coastal sea, "diatom resting hypothesis" was presented. Biological control using diatoms is proposed through the germination/rejuvenation of resting stages suspending from bottom sediments to euphotic layer by sediment perturbation with submarine tractors or fishing trawling gears. Since diatoms have much higher growth rates, and newly joined diatom vegetative cells grow faster and prevent occurrence of Chattonella red tides as a result. As another prevention strategy for Chattonella red tides, algicidal bacteria inhabiting in seaweed beds and seagrass beds are presented. Co-culture of fish and seaweeds in aquaculture areas, and the developments of seaweed- and seagrass-beds would be practical and ultimately environment-friendly strategies for the prevention of harmful red tides of Chattonella by virtue of natural algicidal bacteria supplied from seaweeds and leaves of seagrass. (C) 2011 Elsevier B.V. All rights reserved.	[Imai, Ichiro] Hokkaido Univ, Grad Sch Fisheries Sci, Plankton Lab, Hakodate, Hokkaido 0418611, Japan; [Yamaguchi, Mineo] Natl Res Inst Fisheries & Environm Inland Sea, Res Ctr Environm Conservat, Hiroshima 7390452, Japan	Hokkaido University; Japan Fisheries Research & Education Agency (FRA)	Imai, I (通讯作者)，Hokkaido Univ, Grad Sch Fisheries Sci, Plankton Lab, Minato Cho, Hakodate, Hokkaido 0418611, Japan.	imai1ro@fish.hokudai.ac.jp			Fisheries Agency; Ministry of Environments; Ministry of Science and Culture, Japan [08660228, 16380131]; Grants-in-Aid for Scientific Research [08660228, 16380131] Funding Source: KAKEN	Fisheries Agency; Ministry of Environments; Ministry of Science and Culture, Japan; Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	Main part of the field studies in the Seto Inland Sea were carried out during a period I. Imai belonged to the Nansei National Fisheries Research Institute (present affiliation of M. Yamaguchi) and Kyoto University, and we are grateful to the people involved, especially Drs. A. Murakami, M. Anraku, F. Koga, K. Itoh, T. Honjo, Y. Matsuo, S. Itakura, K. Nagasaki, I. Yoshinaga and captains and crews of the research vessel Shirafuji-Maru, and Professor emeritus Y. Ishida, H. Nakahara and A. Uchida, and students at that time. We thank Dr. S. Yoshimatsu for his supplying a strain of C. subsalsa for taking photomicrographs. The studies were supported by grants from the Fisheries Agency, Ministry of Environments, and Ministry of Science and Culture, Japan (research no. 08660228 and 16380131). 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J	Hallegraeff, GM; Blackburn, SI; Doblin, MA; Bolch, CJS				Hallegraeff, G. M.; Blackburn, S. I.; Doblin, M. A.; Bolch, C. J. S.			Global toxicology, ecophysiology and population relationships of the chainforming PST dinoflagellate <i>Gymnodinium catenatum</i>	HARMFUL ALGAE			English	Review						Gymnodinium catenatum; Paralytic Shellfish Toxin profiles; Molecular Biogeography; Bloom Ecophysiology	SP-NOV DINOPHYCEAE; GULF-OF-CALIFORNIA; PARALYTIC SHELLFISH TOXINS; RECENT MARINE-SEDIMENTS; RED TIDE; MICRORETICULATE CYST; GRAHAM DINOPHYCEAE; BAHIA-CONCEPCION; BALLAST WATER; HIROSHIMA BAY	Increasing scientific awareness since the 1980s of the chain-forming dinoflagellate Gymnodinium catenatum has led to this species being reported with increased frequency in a globally increasing number of countries (23 at present). G. catenatum exhibits little molecular genetic variation in rDNA over its global range, in contrast to RAPD fingerprinting which points to high genetic variation within regional populations even between estuaries 50 km apart. All Australian and New Zealand strains possess a thymine nucleotide (T-gene) near the start of the 5.8S rRNA whereas all other global populations examined to date possess cytosine-nucleotide (C-gene), except for southern Japan which harbours both C-gene and T-gene strains. Together with cyst and plankton evidence this strongly suggests that both Australian and New Zealand populations have derived from southern Japan. Global dinoflagellate populations and cultures exhibit an extraordinary variation in PST profiles (STX and 21 analogues), but consistent regional patterns are evident with regard to the production of C1,2; C3,4; B1,2; and neoSTX analogues. PST profiles of cyst-derived cultures are deemed unrepresentative. Distinct ecophysiological differences exist between tropical (21-32 degrees C) and warm-temperate ecotypes (12-18 degrees C), but these appear unrelated to ITS genotypes and PST toxin phenotypes. On current evidence, cyst germination appears to play a minimal role in the bloom dynamics of this species, while seasonal and inter-annual bloom variations result from the physical constraints (temperature and light) on the growth of the dinoflagellates in the water column. G. catenatum exhibits a capacity to utilize many forms of nitrogen. Its chain formation and strong motility allow it to undergo retrieval migrations to exploit light and nutrient resource gradients in both stratified and mixed environments. Subtle strain-level variations in rnicronutrient (Se, humics) requirements and interaction with associated bacterial flora may provide a partial explanation for the contrasting inshore (Tasmanian), and offshore (Spain, Mexico) bloom patterns by the same species in different geographic regions. (C) 2011 Elsevier B.V. All rights reserved.	[Hallegraeff, G. M.] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas 7001, Australia; [Blackburn, S. I.] CSIRO Marine & Atmospher Res, Hobart, Tas 7001, Australia; [Doblin, M. A.] Univ Technol Sydney, Sydney, NSW 2007, Australia; [Bolch, C. J. 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J	Usup, G; Ahmad, A; Matsuoka, K; Lim, PT; Leaw, CP				Usup, Gires; Ahmad, Asmat; Matsuoka, Kazumi; Lim, Po Teen; Leaw, Chui Pin			Biology, ecology and bloom dynamics of the toxic marine dinoflagellate <i>Pyrodinium bahamense</i>	HARMFUL ALGAE			English	Review						Harmful algal blooms; Pyrodinium bahamense; HAB biology and ecology	HARMFUL ALGAL BLOOMS; SHELLFISH POISONING TOXINS; INDIAN RIVER LAGOON; VAR. COMPRESSUM; COASTAL WATERS; MANILA BAY; DINOPHYCEAE; PLATE; GULF; ALEXANDRIUM	It has been 40 years since the first recorded toxic bloom of Pyrodinium bahamense occurred in Papua New Guinea in 1972. Subsequently this species has increased in importance as a paralytic shellfish poisoning toxin (PSTs) producer in several regions of the world, especially in the Indo-west Pacific. P. bahamense is a thecate tropical/subtropical euryhaline dinoflagellate. Available data indicate that it forms blooms only in waters of 20 psu or higher salinity and at temperatures above 20 degrees C. It is monospecies with two varieties, namely var. compressum and var. bahamense. For many years it was widely accepted that only var. cornpressum is toxic and is limited to the tropical Pacific while var. bahamense is nontoxic and is limited to the tropical Atlantic. It is now known, however, that there are at least two locations where the varieties co-occur and it has also been proven that var. bahamense in Florida waters also produce PST. P. bahamense has a life cycle typical of many dinoflagellates. It has a heterothallic sexual cycle that produces a large spiny spherical resting cyst. The toxicity profile of P. bahamense is also very simple with most isolates producing only dc-STX, STX, neoSTX, B1 and B2 toxins. Further studies are needed in order to resolve the varietal status of the species and also to understand the environmental factors that determine its toxicity and bloom dynamics. (C) 2011 Elsevier ay. All rights reserved.	[Usup, Gires; Ahmad, Asmat] Univ Kebangsaan Malaysia, Fac Sci & Technol, Bangi 43600, Selangor, Malaysia; [Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 852, Japan; [Lim, Po Teen] Univ Malaysia Sarawak, Fac Resource Sci & Technol, Kota Samarahan 94300, Sarawak, Malaysia; [Leaw, Chui Pin] Univ Malaysia Sarawak, Inst Biodivers & Environm Conservat, Kota Samarahan 94300, Sarawak, Malaysia	Universiti Kebangsaan Malaysia; Nagasaki University; University of Malaysia Sarawak; University of Malaysia Sarawak	Usup, G (通讯作者)，Univ Kebangsaan Malaysia, Fac Sci & Technol, Bangi 43600, Selangor, Malaysia.	giresusup@gmail.com; asmat@ukm.my; kazu-mtk@nagasaki-u.ac.jp; ptlim@frst.unimas.my; cpleaw@ibec.unimas.my	Leaw, Chui Pin/F-5220-2012; Lim, Po Teen/C-9758-2013	Leaw, Chui Pin/0000-0003-3336-1438; Lim, Po Teen/0000-0003-2823-0564	government of Malaysia; government of Japan	government of Malaysia; government of Japan	The authors would like to thank the governments of Malaysia and Japan for financial support of projects that contributed to some of the data reported here. The authors also acknowledge their respective universities for additional financial and time support. K. Matsuoka acknowledges Dr. A.R. Almuftah for kindly providing plankton samples of the Persian Gulf and Dr. K. Mizushima for his kind preparation of cyst samples. 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J	Bowman, VC; Francis, JE; Riding, JB; Hunter, SJ; Haywood, AM				Bowman, Vanessa C.; Francis, Jane E.; Riding, James B.; Hunter, Stephen J.; Haywood, Alan M.			A latest Cretaceous to earliest Paleogene dinoflagellate cyst zonation from Antarctica, and implications for phytoprovincialism in the high southern latitudes	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Cretaceous; Paleogene; Seymour Island, Antarctica; dinoflagellate cysts; biostratigraphy; provincialism	JAMES-ROSS-ISLAND; NEW-ZEALAND; SEYMOUR-ISLAND; TERTIARY TRANSITION; AUSTRAL BASIN; VEGA-ISLAND; CAPE LAMB; STRATIGRAPHY; ARGENTINA; BOUNDARY	The thickest uppermost Cretaceous to lowermost Paleogene (Maastrichtian to Danian) sedimentary succession in the world is exposed on southern Seymour Island (65 degrees South) in the James Ross Basin, Antarctic Peninsula. This fossiliferous shallow marine sequence, which spans the Cretaceous-Paleogene boundary, has allowed a high-resolution analysis of well-preserved marine palynomorphs. Previous correlation of Cretaceous-Paleogene marine palynomorph assemblages in the south polar region relied on dinoflagellate cyst biozonations from New Zealand and southern Australia. The age model of the southern Seymour Island succession is refined and placed within the stratigraphical context of the mid to high southern palaeolatitudes. Quantitative palynological analysis of a new 1102 m continuous stratigraphical section comprising the uppermost Snow Hill Island Formation and the Lopez de Bertodano Formation (Marambio Group) across southern Seymour Island was undertaken. We propose the first formal late Maastrichtian to early Danian dinoflagellate cyst zonation scheme for the Antarctic based on this exceptional succession. Two new late Maastrichtian zones, including three sub-zones, and one new early Danian zone are defined. The oldest beds correlate well with the late Maastrichtian of New Zealand. In a wider context, a new South Polar Province based on Maastrichtian to Danian dinoflagellate cysts is proposed, which excludes most southern South American marine palynofloras. This interpretation is supported by models of ocean currents around Antarctica and implies an unrestricted oceanic connection across Antarctica between southern South America and the Tasman Sea. (C) 2011 Elsevier B.V. All rights reserved.	[Bowman, Vanessa C.; Francis, Jane E.; Hunter, Stephen J.; Haywood, Alan M.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England	University of Leeds; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Bowman, VC (通讯作者)，Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.	V.C.Bowman@leeds.ac.uk		Bowman, Vanessa/0000-0002-4887-3949	Natural Environment Research Council (NERC) Antarctic Funding Initiative [NE/C506399/1]; Transantarctic Association; Antarctic Science Bursary; NERC [bgs05004, NE/I00582X/1, NE/I005803/1] Funding Source: UKRI	Natural Environment Research Council (NERC) Antarctic Funding Initiative(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Transantarctic Association; Antarctic Science Bursary; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The authors acknowledge funding from the Natural Environment Research Council (NERC) Antarctic Funding Initiative Grant NE/C506399/1 entitled 'Terminal Cretaceous climate change and biotic response in Antarctica'. Fieldwork was supported by the British Antarctic Survey and H.M.S. Endurance. Vanessa C. Bowman thanks the Transantarctic Association and the Antarctic Science Bursary for additional research support, Rosemary Askin (formerly of The Ohio State University, Columbus, USA) and J. Alistair Crame (British Antarctic Survey) for useful discussions and Paul Markwick (GETECH) for the palaeogeographic base map. The Climate Change research programme of the British Geological Survey provided support for palynological processing. James B. Riding publishes with the permission of the Executive Director, British Geological Survey (NERC).	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J	Borges, MEN; Riding, JB; Fernandes, P; Matos, V; Pereira, Z				Borges, Marisa E. N.; Riding, James B.; Fernandes, Paulo; Matos, Vasco; Pereira, Zelia			Callovian (Middle Jurassic) dinoflagellate cysts from the Algarve Basin, southern Portugal	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynology; biostratigraphy; provincialism; Middle Jurassic (Callovian); Algarve Basin; Portugal	BAYU-UNDAN FIELD; TIMOR SEA; KIMMERIDGIAN PALYNOLOGY; SEQUENCE STRATIGRAPHY; REGION; NORTH; PALEOENVIRONMENTS; AUSTRALIA; STRATA	The palynology of three Callovian (Middle Jurassic) limestone-marl successions from the Algarve Basin in southern Portugal was studied. These localities are Baleeira Harbour, Mareta Beach and Telheiro Quarry; they provide a composite. succession, tied to ammonite zones, through the Lower, Middle and Upper Callovian from the western and eastern subbasins of the Algarve Basin. The three sections generally yielded relatively abundant marine and continental palynofloras. Diversity is low to moderate and the dinoflagellate cyst associations are dominated by Ctenidodinium spp., the Ellipsoidictyum/Valensiella group, Gonyaulacysta jurassica subsp. adecta, Korystocysta spp., Meiourogonyaulax spp., Pareodinia ceratophora, Sentusidinium spp., Surculosphaeridium? vestitum and Systematophora spp. Some intra-Callovian marker bioevents were recorded: these include the range bases of Ctenidodinium ornatum, Gonyaulacysta eisenackii, Korystocysta pachyderma, Mendicodinium groenlandicum, Rigaudella spp. and Surculosphaeridium? vestitum. The occurrences of Endoscrinium acroferum and Impletosphaeridium varispinosum in the Early to Middle Callovian of Mareta Beach and Telheiro Quarry are also characteristic of this interval. At Baleeira Harbour, the presence of Ctenidodinium continuum and Gonyaulacysta centriconnata in the Peltoceras athleta Zone confirms the Late Callovian age of this section. The successions studied were deposited in restricted infralittoral neritic marine environments which lack deep water circulation, and possibly represent restricted embayments. The relatively low diversity nature of the dinoflagellate cyst assemblages appears to be largely due to the highly enclosed nature of this depocentre. Many Callovian index dinoflagellate cyst taxa which are found in northwest Europe are absent in the Algarve Basin. These forms may have been intolerant of enclosed palaeoenvironments which have restricted or no deep circulation. The Callovian marine palynofloras from the Algarve Basin compare well to the few other published records from the Iberian Peninsula of this age. However they are significantly less diverse than coeval floras from elsewhere in the extensive Mid Latitude Callovian phytoprovince. Many typically Callovian dinoflagellate cysts are cosmopolitan, however some provincialism is clearly manifested. The Arctic and Austral Callovian phytoprovinces are characterised by key endemic taxa such as Paragonyaulacysta retiphragmata and Ternia balmei, which are not present in the Algarve Basin and are assumed to have been polar forms. (C) 2011 Natural Environment Research Council. Published by Elsevier BV. All Rights Reserved.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England; [Borges, Marisa E. N.; Fernandes, Paulo; Matos, Vasco] Univ Algarve, CIMA Ctr Invest Marinha & Ambiental, P-8005139 Faro, Portugal; [Borges, Marisa E. N.; Pereira, Zelia] LNEG LGM, P-4465965 Sao Mamede de Infesta, Portugal	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Universidade do Algarve; Laboratorio Nacional de Energia e Geologia IP (LNEG)	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	marisa.borges@lneg.pt; jbri@bgs.ac.uk; pfernandes@ualg.pt; vgmatos@ualg.pt; zelia.pereira@lneg.pt	Fernandes, Paulo/J-6577-2014; Pereira, Zelia/B-2740-2017	Fernandes, Paulo/0000-0003-4888-0230; Pereira, Zelia/0000-0003-3056-6219	Portuguese Foundation for Science and Technology [SFRH/BD/40428/2007];  [PTDC/CTE-GEX/72694/2006]; NERC [bgs05002] Funding Source: UKRI; Fundação para a Ciência e a Tecnologia [PTDC/CTE-GEX/72694/2006, SFRH/BD/40428/2007] Funding Source: FCT	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); ; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	The contribution of Marisa E.N. Borges represents part of PhD scholarship number SFRH/BD/40428/2007 awarded by the Portuguese Foundation for Science and Technology. This study is also a contribution to the project entitled 'Hydrocarbon source-rock potential of the Algarve Basin' (PTDC/CTE-GEX/72694/2006), also funded by the Portuguese Foundation for Science and Technology. The input of James B. Riding was completed under the BGS Individual Merit project Global Jurassic dinoflagellate cyst palaeobiology and its applications. Drs Javier Helenes (CICESE, Mexico) and Daniel J. Mantle (Morgan Goodall Palaeo Associates, Australia) are thanked for their very constructive reviews of an early draft of the manuscript. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	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Palaeobot. Palynology	JAN 15	2012	170						40	56		10.1016/j.revpalbo.2011.10.008	http://dx.doi.org/10.1016/j.revpalbo.2011.10.008			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	915RI		Green Published, Green Accepted			2025-03-11	WOS:000302044700004
J	Casabianca, S; Penna, A; Pecchioli, E; Jordi, A; Basterretxea, G; Vernesi, C				Casabianca, Silvia; Penna, Antonella; Pecchioli, Elena; Jordi, Antoni; Basterretxea, Gotzon; Vernesi, Cristiano			Population genetic structure and connectivity of the harmful dinoflagellate <i>Alexandrium minutum</i> in the Mediterranean Sea	PROCEEDINGS OF THE ROYAL SOCIETY B-BIOLOGICAL SCIENCES			English	Article						connectivity; population structure; HAB (harmful algal blooms); microsatellite; genetic distance; dinoflagellate	MICROSATELLITE MARKERS; MOLECULAR EVIDENCE; LARVAL DISPERSAL; BALLAST WATER; RESTING CYSTS; MARINE; COASTAL; CIRCULATION; BLOOM; OCEAN	The toxin-producing microbial species Alexandrium minutum has a wide distribution in the Mediterranean Sea and causes high biomass blooms with consequences on the environment, human health and coastal-related economic activities. Comprehension of algal genetic differences and associated connectivity is fundamental to understand the geographical scale of adaptation and dispersal pathways of harmful microalgal species. In the present study, we combine A. minutum population genetic analyses based on microsatellites with indirect connectivity (C-i) estimations derived from a general circulation model of the Mediterranean sea. Our results show that four major clusters of genetically homogeneous groups can be identified, loosely corresponding to four regional seas: Adriatic, Ionian, Tyrrhenian and Catalan. Each of the four clusters included a small fraction of mixed and allochthonous genotypes from other Mediterranean areas, but the assignment to one of the four clusters was sufficiently robust as proved by the high ancestry coefficient values displayed by most of the individuals (>84%). The population structure of A. minutum on this scale can be explained by microalgal dispersion following the main regional circulation patterns over successive generations. We hypothesize that limited connectivity among the A. minutum populations results in low gene flow but not in the erosion of variability within the population, as indicated by the high gene diversity values. This study represents a first and new integrated approach, combining both genetic and numerical methods, to characterize and interpret the population structure of a toxic microalgal species. This approach of characterizing genetic population structure and connectivity at a regional scale holds promise for the control and management of the harmful algal bloom events in the Mediterranean Sea.	[Casabianca, Silvia; Penna, Antonella] Univ Urbino, Dept Biomol Sci, I-61121 Pesaro, Italy; [Jordi, Antoni; Basterretxea, Gotzon] IMEDEA UIB CSIC, Esporles 07190, Spain	University of Urbino; Consejo Superior de Investigaciones Cientificas (CSIC); ATTITUS Educacao	Penna, A (通讯作者)，Univ Urbino, Dept Biomol Sci, I-61121 Pesaro, Italy.	antonella.penna@uniurb.it	Basterretxea, Gotzon/D-2314-2011; Jordi, Antoni/C-3935-2008	Jordi, Antoni/0000-0003-2637-8389; CASABIANCA, Silvia/0000-0003-2670-5423; Basterretxea, Gotzon/0000-0001-7466-1360	EC; Italian Ministry of University and Research [prot. 2007 FXSCL2, prot. 2007 R8AWYY_003];  [GOCE-CT-2005-003875]	EC(European Union (EU)European Commission Joint Research Centre); Italian Ministry of University and Research(Ministry of Education, Universities and Research (MIUR)); 	We thank Santiago Fraga and Isabel Bravo for providing us with strains; Luglie Antonella and Carmela Caroppo for field samples. Financial support was provided by the EC-funded Research Project SEED (Life cycle transformations among HAB species, and the environmental and physiological factors that regulate them), GOCE-CT-2005-003875; PRIN 2007 Italian Ministry of University and Research, prot. 2007 FXSCL2 Grant and prot. 2007 R8AWYY_003 Grant.	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R. Soc. B-Biol. Sci.	JAN 7	2012	279	1726					129	138		10.1098/rspb.2011.0708	http://dx.doi.org/10.1098/rspb.2011.0708			10	Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics; Environmental Sciences & Ecology; Evolutionary Biology	856WD	21593032	Green Published			2025-03-11	WOS:000297674300018
J	Gedl, P				Gedl, Przemyslaw			Reworked Eocene-Oligocene dinoflagellate cysts in the Miocene of the Carpathian Foredeep Basin: implications for Paleogene palaeogeography in SE Poland	GEOLOGICAL QUARTERLY			English	Article						dinoflagellate cysts; reworking; epicontinental Paleogene; palaeogeography; SE Poland	DEPOSITS; NORTHERN; ZONATION	Miocene strata of the Carpathian Foredeep Basin in Poland contain reworked Eocene and Oligocene dinoflagellate cysts, which come from two sources: the Flysch Carpathians and the epicontinental basin. The occurrence of the latter is almost the only trace of the epicontinental Eocene-Oligocene sedimentary cover, which extended across southwestern Poland, and is today nearly completely eroded. The distribution of epicontinental Eocene and Oligocene taxa in the Miocene strata of the northeastern part of the Carpathian Foredeep is uneven, clearly pointing to a limited extent of the host deposits and their variable erosion intensity. Erosion of the Eocene and Oligocene platform cover took place prior the Miocene transgression and took place also during the Badenian; its intensity increased during Late Badenian-Sarmatian tectonic movements, resulting in an increased frequency of reworked specimens in strata postdating the mid-Badenian deposits. Przemyslaw Gedl, Institute of Geological Sciences, Polish Academy of Sciences, Senacka 1, 31-002 Krakow, Poland, e-mail: ndgedl@cyf-kr.edu.pl (received: June 20, 2012; accepted: August 10, 2012; first published online: November 27, 2012).	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						Alexandrowicz S., 1961, Kwartalnik Geologiczny, V5, P646; Alexandrowicz S., 1956, Acta Geologica Polonica, V6, P301; Alexandrowicz S., 1958, Kwartalnik Geologiczny, V2, P54; Alexandrowicz S. W., 1963, Prace Instytutu Geologicznego Warszawa, V39, P1; Alexandrowicz S.W., 1982, Geol. Q, V26, P470; Alexandrowicz S. W., 1969, ANN SOC GEOL POL, V39, P681; [Anonymous], 1978, Geol. 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J	Egger, H; Mohamed, O; Freimoser, M				Egger, Hans; Mohamed, Omar; Freimoser, Matthias			OBITUARY FOR THE WALSERBERG SERIES IN THE CRETACEOUS OF THE EASTERN ALPS (AUSTRIA, GERMANY)	AUSTRIAN JOURNAL OF EARTH SCIENCES			English	Article						Rhenodanubian Zone; nannoplankton; dinoflagellates; Eastern Alps; Cretaceous; Walserberg	FLYSCH	New biostratigraphic investigations based on calcareous nannoplankton and dinoflagellates cysts indicate that the, Walserberg Series" near Salzburg comprises deposits from the Upper Aptian to the Mid-Campanian. Generally, deposition took place below the CCD. The major part of the sedimentary succession displays no similarities with coeval deposits of the Northern Calcareous Alps, but can be readily correlated with the Rhenodanubian Group of the Penninic Basin (Rehbreingraben Formation, Lower Varicoloured Marlstone, Reiselsberg Formation, Seisenburg Formation, Kalkgraben Formation, Hallritz Formation). Only one outcrop containing glaucophane bearing sandstone cannot be integrated into the Rhenodanubian Group and might be an equivalent of the Branderfleck Formation of the Northern Calcareous Alps. In any case, the term "Walserberg Series" can be abandoned.	[Egger, Hans] Geol Survey Austria, A-1030 Vienna, Austria; [Mohamed, Omar] Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt	Egyptian Knowledge Bank (EKB); Minia University	Egger, H (通讯作者)，Geol Survey Austria, Neulinggasse 38, A-1030 Vienna, Austria.	hans.egger@geologie.ac.at						Alberti G., 1961, Palaeontographica, V116, P1; Below R., 1982, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V164, P339; BELOW R, 1982, Revista Espanola de Micropaleontologia, V14, P23; BRINKHUIS H, 1988, REV PALAEOBOT PALYNO, V56, P5, DOI 10.1016/0034-6667(88)90071-1; Burnett J.A., 1998, P132; Egger H, 1992, Z DTSCH GEOL GES, V143, P51; Egger H., 1997, JAHRB GEOL BUNDESANS, V140, P47; Egger H, 2008, CRETACEOUS RES, V29, P405, DOI 10.1016/j.cretres.2007.03.002; Egger Hans, 1993, Zitteliana, V20, P59; FAUPL P, 1992, CRETACEOUS RES, V13, P387, DOI 10.1016/0195-6671(92)90006-C; Faupl P., 1984, MITT OSTERR GEOL GES, V77, P33; FREIMOSER M, 1972, GEOLOGICA BAVARICA, V66, P7; Gaupp RH., 1982, Zitteliana, V8, P33; Herngreen W.F.G., 1978, PALYNOLOGIA, V1, P273; Kirsch Karl-Heinz, 2003, Zitteliana Reihe A, V43, P143; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; Milloud M. E., 1975, FORUM ON DINOFLAGELL, V4, P65; Oberhauser R., 1968, Jahrbuch der Geologischen Bundesanstalt Wien, V111, P115; PERCH-NIELSEN K., 1985, CAMBRIDGE EARTH SCI, V11, P427; Prauss M., 1990, GEOLOGISCHES JAHRBUC, V121, P275; Prey S., 1968, VERHANDLUNGEN DER GE, V1968, pA41; Rauscher R., 1982, Sci. Geol. Bull., V35, P97; SISSINGH W, 1977, Geologie en Mijnbouw, V56, P37; Skupien Petr, 2003, Bulletin of Geosciences, V78, P67; von Eynatten H, 1996, GEOLOGY, V24, P691, DOI 10.1130/0091-7613(1996)024<0691:AALPDO>2.3.CO;2; von Eynatten H, 1999, SEDIMENT GEOL, V124, P81, DOI 10.1016/S0037-0738(98)00122-5; Wagreich M, 2006, CRETACEOUS RES, V27, P743, DOI 10.1016/j.cretres.2006.01.002; WEIDICH KF, 1984, GEOL RUNDSCH, V73, P517, DOI 10.1007/BF01824971; Williams G.L., 1985, P847; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Winkler W., 1988, Jahrbuch der Geologischen Bundesanstalt Wien, V131, P341; Woletz G., 1967, Geologische Rundschau, V56, P308	32	0	0	0	1	OESTERREICHISCHE  GEOLOGISCHE GESELLSCHAFT	VIENNA	C/O GEOLOGICAL SURVEY OF AUSTRIA, RASUMOFSKYGASSE 23,  POSTFACH 127, VIENNA, 1031, AUSTRIA	2072-7151			AUSTRIAN J EARTH SCI	Austrian J. Earth Sci.		2012	105	3					161	174						14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	096FV					2025-03-11	WOS:000315390500011
C	Yñiguez, AT; Cayetano, A; Villanoy, CL; Alabia, I; Fernandez, I; Palermo, JD; Benico, GA; Siringan, FP; Azanza, RV		Yang, Z; Chen, B		Yniguez, A. T.; Cayetano, A.; Villanoy, C. L.; Alabia, I.; Fernandez, I.; Palermo, J. D.; Benico, G. A.; Siringan, F. P.; Azanza, R. V.			Investigating the roles of intrinsic and extrinsic factors in the blooms of <i>Pyrodinium bahamense</i> var. <i>compressum</i> using an individual-based model	18TH BIENNIAL ISEM CONFERENCE ON ECOLOGICAL MODELLING FOR GLOBAL CHANGE AND COUPLED HUMAN AND NATURAL SYSTEM	Procedia Environmental Sciences		English	Proceedings Paper	18th Biennial ISEM Conference on Ecological Modelling for Global Change and Coupled Human and Natural Systems	SEP 20-23, 2011	Beijing Normal Univ, Beijing, PEOPLES R CHINA	Int Soc Ecol Modelling	Beijing Normal Univ	harmful algal blooms; Pyrodinium; Philippines; biophysical model; individual based model	NITRATE UPTAKE; MANILA BAY; GROWTH; TEMPERATURE; DYNAMICS; MAINE; GULF; DINOFLAGELLATE; PHYTOPLANKTON; PHILIPPINES	Harmful algal blooms are a recurrent, expensive and at times fatal problem plaguing the Philippines. In particular, Sorsogon Bay in the Bicol region has experienced prolonged shellfish bans due to blooms by the Paralytic Shellfish Poisoning causative species Pyrodinium bahamense var. compressum (Pbc). In order to help explore and understand the population dynamics of Pbc in Sorsogon Bay in relation to environmental factors, an individual-based model has been developed. This model accounts for key life history processes (reproduction, mortality, encystment, excystment) in a spatially-explicit setting. Vegetative cells and resting cysts are separately represented. Movement is due to advection rates from a 3D hydrodynamic model, as well as sinking rates. Asexual reproduction (population growth) occurs in response to light, temperature, salinity and nutrient conditions where the cells are spatially situated. Encystment and excystment processes are also spatially-explicit based on intrinsic factors, and environmental factors. Grazing effects on blooms are also being explored in the model. Results from field studies in the past years indicate that Pbc blooms develop a few months after the onset of rains, relatively lower temperature, and stratification of the water column. Pronounced blooms are observed at a particular time of the year and in certain areas of the Bay. Bloom formation patterns in the model are compared with these field results. This model will be used to further investigate the conditions leading to blooms and their decline, specifically the roles of transport, stratification, nutrients, cyst dynamics, and grazing on Pbc blooms in Sorsogon Bay. (C) 2011 Published by Elsevier B.V. Selection and/or peer-review under responsibility of School of Environment, Beijing Normal University.	[Yniguez, A. T.; Cayetano, A.; Villanoy, C. L.; Alabia, I.; Fernandez, I.; Palermo, J. D.; Benico, G. A.; Siringan, F. P.; Azanza, R. V.] Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines	University of the Philippines System; University of the Philippines Diliman	Yñiguez, AT (通讯作者)，Univ Philippines, Inst Marine Sci, Velasquez St, Quezon City 1101, Philippines.	atyniguez@gmail.com	Palermo, Joseph/AAM-5953-2020; Azanza, Rhodora/HGU-5811-2022; Benico, Garry/S-6313-2019; Alabia, Irene/V-2858-2019	Benico, Garry/0000-0002-2617-0222				Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Azanza R., 1997, SCI DILIMAN, V9, P1; Azanza R. 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L, 1996, HARMFUL TOXIC ALGAL, P189; Villanoy CL, 2006, HARMFUL ALGAE, V5, P156, DOI 10.1016/j.hal.2005.07.001; Yniguez AT, 2011, STRATIFICATION ALGAL, P36	28	7	8	0	20	ELSEVIER SCIENCE BV	AMSTERDAM	SARA BURGERHARTSTRAAT 25, PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1878-0296			PROCEDIA ENVIRON SCI			2012	13						1462	1476		10.1016/j.proenv.2012.01.138	http://dx.doi.org/10.1016/j.proenv.2012.01.138			15	Ecology; Environmental Sciences	Conference Proceedings Citation Index - Science (CPCI-S)	Environmental Sciences & Ecology	BDA87		gold			2025-03-11	WOS:000312386000136
J	Köthe, A				Koethe, Angelika			A revised Cenozoic dinoflagellate cyst and calcareous nannoplankton zonation for the German sector of the southeastern North Sea Basin	NEWSLETTERS ON STRATIGRAPHY			English	Article						calcareous nannoplankton; dinocysts; Cenozoic	RESEARCH BOREHOLE; OLIGOCENE/MIOCENE BOUNDARY; MIDDLE EOCENE; LATE PLIOCENE; BIOSTRATIGRAPHY; MIOCENE; STRATIGRAPHY; PLEISTOCENE; BELGIUM; CALIBRATION	The zonations of Martini (1971; Proc. II. Plankt. Conf. Roma 1970,739-785), Muller and Kothe (1988; Geologisches Jahrbuch A100,253-261) and Kothe (2003; Revue de Paleobiologie 22,895-923) are updated based on new dinoflagellate cyst (dinocyst) and calcareous nannoplankton data from the German sector of the North Sea Basin generated over the last ten years. The early Paleocene to Quaternary dinocyst and calcareous nannoplankton zones for this region are described. Dinocyst and calcareous nannoplankton index markers and additional markers are designated, and previously used marker taxa that have been recognized not to be suitable are discussed. The dinocyst zones DI* and D2* are defined for the German sector of the North Sea Basin for the first time. The zones D4*, D9*, D14*, and DN2* are refined, and zones D3* and D5* are modified. Five dinocyst zones (Germany DN-zones GDN11 to GDN15) for the Pliocene and Pleistocene are established. The calcareous nannoplankton zone NN3* is modified. Additional markers are presented for zones NN6 to NN18, for which almost none of Martini's (1971) index markers are present in the North Sea Basin. The combined zones NN6/7, NN8/10, NN12/15, and NN16/18, which allow a rough dating of this time interval, are described.	Bundesanstalt Geowissensch & Rohstoffe, D-30655 Hannover, Germany		Köthe, A (通讯作者)，Bundesanstalt Geowissensch & Rohstoffe, Stilleweg 2, D-30655 Hannover, Germany.	angelika.koethe@bgr.de						[Anonymous], 1988, Geol. Jahrbuch, Reihe A; [Anonymous], 1988, Geologisches Jahrbuch Reihe A; Anthonissen ED, 2008, NEWSL STRATIGR, V43, P33, DOI 10.1127/0078-0421/2008/0043-0033; Anthonissen ED, 2009, NEWSL STRATIGR, V43, P91, DOI 10.1127/0078-0421/2009/0043-0091; BUJAK J, 1994, J GEOL SOC LONDON, V151, P449, DOI 10.1144/gsjgs.151.3.0449; Cepek P., 1989, Geologisches Jahrbuch Reihe A, P403; Cepek P., 1988, GEOLOGISCHES JB A, VA100, P275; Costa L. 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Stratigr.		2012	45	3					189	220		10.1127/0078-0421/2012/0021	http://dx.doi.org/10.1127/0078-0421/2012/0021			32	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	054QX					2025-03-11	WOS:000312359400001
J	Anthonissen, ED				Anthonissen, Erik D.			A new Miocene biostratigraphy for the northeastern North Atlantic: an integrated foraminiferal, bolboformid, dinoflagellate and diatom zonation	NEWSLETTERS ON STRATIGRAPHY			English	Article						North Sea; Norwegian Sea; Foraminifera; Bolboforma; Dinocyst; Miocene; Neogene	DEEP-WATER CIRCULATION; NORWEGIAN CONTINENTAL-SHELF; BOUNDARY STRATOTYPE SECTION; OLIGOCENE-LOWER MIOCENE; POINT GSSP; UTSIRA FORMATION; SEA-LEVEL; PLIOCENE; NEOGENE; STRATIGRAPHY	This study presents a new Miocene biostratigraphic synthesis for the high-latitude northeastern North Atlantic region. Via correlations to the bio-magnetostratigraphy and oxygen isotope records of Ocean Drilling Program and Deep Sea Drilling Project Sites, the ages of shallower North Sea deposits have been better constrained. The result has been an improved precision and documentation of the age designations of the existing North Sea foraminiferal zonal boundaries of King (1989) and Gradstein and Backstrom (1996). All calibrations have been updated to the Astronomically Tuned Neogene Time Scale (ATNTS) of Lourens et al. (2004). This improved Miocene biozonation has been achieved through: the updating of age calibrations for key microfossil bioevents, identification of new events, and integration of new biostratigraphic data from a foraminiferal analysis of commercial wells in the North Sea and Norwegian Sea. The new zonation has been successfully applied to two commercial wells and an onshore research borehole. At these high latitudes, where standard zonal markers are often absent, integration of microfossil groups significantly improves temporal resolution. The new zonation comprises 11 Nordic Miocene (NM) Zones with an average duration of 1 to 2 million years. This multi-group combination of a total of 92 bioevents (70 foraminifers and bolboformids; 16 dinoflagellate cysts and acritarchs; 6 marine diatoms) facilitates zonal identification throughout the Nordic Atlantic region. With the highest proportion of events being of calcareous walled microfossils, this zonation is primarily suited to micropaleontologists. A correlation of this Miocene biostratigraphy with a re-calibrated oxygen isotope record for DSDP Site 608 suggests a strong correlation between Miocene planktonic microfossil turnover rates and the inferred paleoclimatic trends. Benthic foraminifera zonal boundaries appear to often coincide with Miocene global sequence boundaries. The biostratigraphic record is punctuated by four main stratigraphic hiati which show variation in their geographic and temporal extent. These are related to the following regional unconformities: basal Neogene, Lower/Middle Miocene ("mid-Miocene unconformity"), basal Upper Miocene and basal Messinian unconformities. Further coring of Neogene sections in the North Sea and Norwegian Sea may better constrain their extent and their effect on the biostratigraphic record.	[Anthonissen, Erik D.] Univ Oslo, Nat Hist Museum, N-0318 Oslo, Norway	University of Oslo	Anthonissen, ED (通讯作者)，Chevron, 1500 Louisiana St,Rm 27-108, Houston, TX 77004 USA.	orbulina@gmail.com			Natural History Museum, University of Oslo; Norwegian Interactive Lithostratigraphic Lexicon (NORLEX Project)	Natural History Museum, University of Oslo; Norwegian Interactive Lithostratigraphic Lexicon (NORLEX Project)	Many thanks go to Felix M. Gradstein for providing sample material and supervising this study. Karen Dybkjaer and the Geological Survey of Denmark and Greenland kindly gave access to valuable study material from the Sonder Vium research borehole. Support comes from the Natural History Museum, University of Oslo and the Norwegian Interactive Lithostratigraphic Lexicon (NORLEX Project).	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Stratigr.		2012	45	3					281	307		10.1127/0078-0421/2012/0025	http://dx.doi.org/10.1127/0078-0421/2012/0025			27	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	054QX					2025-03-11	WOS:000312359400005
J	Mays, CM; Stilwell, JD				Mays, Chris M.; Stilwell, Jeffrey D.			Judging an acritarch by its cover: the taxonomic implications of <i>Introvertocystis rangiaotea</i> gen. et sp nov from the Late Cretaceous (Cenomanian-Turonian) of the Chatham Islands, New Zealand	PALYNOLOGY			English	Article						acritarchs; Introvertocystis rangiaotea gen. et sp nov.; internal ornamentation; Cretaceous; Zealandia; Chatham Islands, Palaeostomocystis		Described here is a small acritarch with a fine reticulation on the internal surface of the cyst wall which provides a new criterion for future acritarch taxonomy. Sixty-six specimens of Introvertocystis rangiaotea gen. et sp. nov. have been identified from sediments of Ngaterian to Arowhanan age (Cenomanian to early Turonian; c. 99-92 Ma) within the Tupuangi Formation, Chatham Islands, New Zealand. The diagnostic feature of this fossil cyst is internal reticulation. This requires the emendment of the genus Palaeostomocystis. Some specimens may show waist constriction; this constriction is more common in larger specimens where it is suggestive of a paracingulum. However, the absence of a definite paracingulum, parasulcus or definable archeopyle precludes its assignment within the dinoflagellates. The wall structure is unusual in that the sculptural ornamentation is present on the internal surface, a feature that distinguishes it from all known acritarch genera.	[Mays, Chris M.; Stilwell, Jeffrey D.] Monash Univ, Sch Geosci, Clayton, Vic 3800, Australia	Monash University	Mays, CM (通讯作者)，Monash Univ, Sch Geosci, Wellington Rd, Clayton, Vic 3800, Australia.	chris.mays@monash.edu		Stilwell, Jeffrey Darl/0000-0002-9853-1322; Mays, Chris/0000-0002-5416-2289	Monash University Bridging and Research Initiatives Grant; Australian Postgraduate Award Scholarship	Monash University Bridging and Research Initiatives Grant; Australian Postgraduate Award Scholarship	The authors would like to thank the following people: D. Mantle, Geoscience Australia (Canberra, Australia) for his mentoring and assistance with the practical side of palynology; I. Raine, Geological and Nuclear Sciences (Lower Hutt, New Zealand) for kindly processing the sediment samples from which these specimens were found; A. Partridge for inspiration and advice; the residents of Pitt Island, especially J. Preece, B. Gregory-Hunt and D. Gregory-Hunt for allowing access to the outcrops on their land, as well as K. Lanauze and J. Lanauze for their assistance and support on Pitt Island; S. Poropat for assistance in the field and for editing; L. Sorrentino-Mariconda, D. Thompson and C. Rodriguez for their advice and encouragement. This investigation was funded by the Monash University Bridging and Research Initiatives Grant awarded to JDS and an Australian Postgraduate Award Scholarship awarded to CMM.	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J	Gedl, P; Ziaja, J				Gedl, Przemyslaw; Ziaja, Jadwiga			Palynofacies from Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Krakow-Silesia Homocline, Poland, with special emphasis on sporomorph eco-groups	ACTA GEOLOGICA POLONICA			English	Article						Palynofacies; Sporomorphs; Ore-bearing clays; Bathonian; Middle Jurassic; Palaeogeography; Epicontinental basin; Poland	POLISH JURA; RECONSTRUCTION; CONCRETIONS; WOOD	The palynological organic matter of dark clays from Bathonian ore-bearing clays exposed at Gnaszyn (Czestochowa, Krakow-Silesia Homocline, Poland) consists of high proportions of land-derived particles; aquatic elements (mainly dinoflagellate cysts) are comparatively rare. Terrestrial particles include black opaque phytoclasts, dark brown phytoclasts, cuticle remains and subordinate sporomorphs. The latter are represented by eighty-four taxa of spores and pollen grains. They represent various groups of plants, including Bryophyta, Sphenophyta, Lycophyta, Pteridophyta, Pteridospermophyta, Cycadophyta or Ginkgophyta and Coniferophyta. The most frequent sporomorphs in almost all samples from Gnaszyn are Callialasporites (Araucariaceae), Cerebropollenites and Perinopollenites elatoides (Taxodiaceae) pollen grains, fern spores with triradiate tetrad mark, bisaccate pollen grains belonging to conifers (Pinaceae or Podocarpaceae) and also to Pteridospermophyta. Quantitative analysis of the palynofacies shows fluctuations of particular element ratios, which correlate with lithology. Clay intervals that contain siderite concretion levels yielded lower amounts of cuticles in relation to sporomorphs (mainly pollen grains) and dinoflagellate cysts. Intervals of monotonous clays and silts are characterized by a higher ratio of cuticles in relation to other elements, especially dinoflagellate cysts. Also, quantitative analysis of the sporomorphs shows changes in frequency of the representatives of various plant communities, which coexisted during the Jurassic: Upland, Lowland, River, Pioneer, Coastal and Tidally-influenced. These changes might have reflected sea-level fluctuations, which affected vegetation growing on adjacent land. However, the dominance of Callialasporites pollen grains, which belong to the Coastal community, indicates that the Gnaszyn assemblage was mainly influenced by the seashore vegetation. The high frequency of Araucariaceae pollen grains and the presence of ferns representing the Osmundaceae, Cyatheaceae, Dicksoniaceae, Schizeaceae, Gleicheniaceae and Matoniaceae indicate a warm climate without large seasonal amplitudes during the deposition of the Gnaszyn succession.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland; [Ziaja, Jadwiga] Polish Acad Sci, W Szafer Inst Bot, PL-31512 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; W. Szafer Institute of Botany 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; J.Ziaja@botany.pl		Ziaja, Jadwiga/0000-0002-3562-4812				Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; Abbink OA, 2004, NETH J GEOSCI, V83, P17, DOI 10.1017/S0016774600020436; [Anonymous], 1976, PRACE I GEOLOGICZNEG; BALME BE, 1995, REV PALAEOBOT PALYNO, V87, P85; Batten D.J., 1996, Palynology: principles and applications, V2, P795; BOULTER MC, 1986, SEDIMENTOLOGY, V33, P871, DOI 10.1111/j.1365-3091.1986.tb00988.x; Chaloner W.G., 1968, Coal and Coal-bearing Strata; Dayczak-Calikowska K., 1976, GEOLOGY POLAND 2, V1, P241; Dayczak-Calikowska K., 1997, PRACE PANSTWOWEGO I, V153, P269; Dybkjaer K., 1991, DANMARKS GEOLOGISK A, V30, P1; FISHER M.J., 1980, Proceedings of the 4th International Palynological Conference, Lucknow 1976-1977, V2, P574; Gedl P, 2003, TOMY JURAJSKIE, V1, P19; Gedl P., 2006, JURASSIC POLAND ADJA, P151; Gedl P, 2012, ACTA GEOL POL, V62, P267, DOI 10.2478/v10263-012-0014-y; Götz AE, 2008, CRETACEOUS RES, V29, P1047, DOI 10.1016/j.cretres.2008.05.029; Kaim A, 2011, LETHAIA, V44, P109, DOI 10.1111/j.1502-3931.2010.00236.x; Konijnenburg-Van Cittert JHAV, 2002, REV PALAEOBOT PALYNO, V119, P113; Kontkiewicz S., 1890, PAMIETNIK FIZJOGRAFI, V10, P29; Kopik Janusz, 1998, Biuletyn Panstwowego Instytutu Geologicznego, V378, P67; Koppelhus E.B., 1996, American Association of Stratigraphic Palynologists Foundation, V2, P779; Koppelhus Eva Bundgaard, 1994, Palynology, V18, P139; Majewski W., 2000, ACTA GEOL POL, V50, P431; Malchus N, 2002, GEOBIOS-LYON, V35, P29, DOI 10.1016/S0016-6995(02)00007-4; Marynowski L, 2007, NATURWISSENSCHAFTEN, V94, P228, DOI 10.1007/s00114-006-0179-x; Matyja B.A., 2003, TOMY JURAJSKIE, V1, P3; Matyja Bronislaw Andrzej, 2000, Acta Geologica Polonica, V50, P191; Mohr B.A.R., 1989, Berliner Geowissenschaftliche Abhandlungen. 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Z., 1953, Prace Instytutu Geologicznego, V17, P1; SLADEN C P, 1984, Proceedings of the Geologists' Association, V95, P149; Steffen D., 1993, B CTR RECHERCHES EXP, V17, P235; Traverse A., 1988, Paleopalynology, P1; VANDERZWAN CJ, 1990, REV PALAEOBOT PALYNO, V62, P157, DOI 10.1016/0034-6667(90)90021-A; Whitaker M.F., 1984, NORSK PETROLEUMSFORE; Wierzbowski H, 2007, PALAEOGEOGR PALAEOCL, V254, P523, DOI 10.1016/j.palaeo.2007.07.010; Zaton M, 2004, GEOL Q, V48, P339; Zaton M., 2006, PRZ GEOL, V54, P131; Zatón M, 2006, GEOBIOS-LYON, V39, P426, DOI 10.1016/j.geobios.2005.02.001; Zaton M, 2006, NEUES JAHRB GEOL P-M, P385; Ziegler P.A., 1988, American Association Petrolium Geologists Memoir, V43, P1, DOI DOI 10.1306/M43478	41	18	18	1	8	POLSKA AKAD NAUK, POLISH ACAD SCIENCES, UNIV WARSAW, GEOLOGY DEPT	WARSZAWA	PL DEFILAD 1, WARSZAWA, 00-901, POLAND	0001-5709	2300-1887		ACTA GEOL POL	Acta Geol. Pol.		2012	62	3					325	349						25	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	021BR					2025-03-11	WOS:000309860800005
J	Gedl, P				Gedl, Przemyslaw			Organic-walled dinoflagellate cysts from the Bathonian ore-bearing clays at Gnaszyn, Krakow-Silesia Homocline, Poland - a palaeoenvironmental approach	ACTA GEOLOGICA POLONICA			English	Article						Dinoflagellate cysts; Bathonian; Middle Jurassic; Palaeoenvironment; Ore-bearing clays; Krakow-Silesia Homocline; Poland		Gedl, P. 2012. Organic-walled dinoflagellate cysts from the Bathonian ore-bearing clays at Gnaszyn, Krakow-Silesia Homocline, Poland - a palaeoenvironmental approach. Acta Geologica Polonica, 62 (3), 439-461. Warszawa. A succession of Middle-Upper Bathonian (Subcontractus-Retrocostatum zones) ore-bearing clays exposed at Gnaszyn has been investigated for the presence of dinoflagellate cysts. The assemblages are dominated by Ctenidodinium. However, analysis of diversity shows some subtle differences throughout the succession, possibly related to the palaeoenvironmental conditions in the photic zone. Impoverished assemblages, dominated by Ctenidodinium, occur mainly in monotonous muddy intervals. More diverse assemblages, albeit also dominated by Ctenidodinium, occur in intervals which contain siderite concretion levels. The taxonomic composition of the former assemblage seems to reflect slightly restricted conditions in the photic zone, possibly related to a minor reduction in salinity and/or increase in nutrient availability. More diverse dinoflagellate cyst assemblages reflect periods of less intense terrigenous influx and relatively higher, possibly normal, salinity. These changes were possibly caused by variable intensity of freshwater influx into the basin, controlled by sea-level fluctuations. Sea-level changes may be related to migrations of Tethyan water masses, which were probably partly responsible for the composition of the dinoflagellate cyst assemblages.	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						Birkenmajer Krzysztof, 2004, Studia Geologica Polonica, V123, P245; Birkenmajer Krzysztof, 2007, Studia Geologica Polonica, V127, P51; DAVIES EH, 1980, GEOL ASSOC CAN SPEC, V20, P361; Dayczak-Calikowska K., 1997, PRACE PANSTWOWEGO I, V153, P269; Dayczak-Calikowska K., 1988, KWART GEOL, V32, P117; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Fenton J.P.G., 1978, Palinologia, P233; Gedl P., 2012, ACTA GEOL POL, V62, P267; Gedl P., 2008, STUDIA GEOLOGICA POL, V131, P7; Gedl P., 2006, JURASSIC POLAND ADJA, P151; Gedl P., 2012, ACTA GEOL POL, V62, P325; Huault V., 1999, REV PALAEOBOT PALYNO, V107, P145; Kopik J., 1997, PRACE PANSTWOWEGO I, V153; Kopik Janusz, 1998, Biuletyn Panstwowego Instytutu Geologicznego, V378, P67; Majewski W., 2000, ACTA GEOL POL, V50, P431; Matyja B.A., 2003, TOMY JURAJSKIE, V1, P3; Pocock S.A.J., 1972, Palaeontographica Abteilung B Palaeophytologie, V137, P85; Poulsen Niels E., 1998, Acta Geologica Polonica, V48, P237; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Riding J.B., 1992, P7; Riding J.B., 1983, GLOUCESTERSHIRE ENGL, V9, P111; Riding James B., 1999, Palynology, V23, P15; Riding James B., 1991, Palynology, V15, P115; RIDING JB, 1985, REV PALAEOBOT PALYNO, V45, P149, DOI 10.1016/0034-6667(85)90068-5; Smelror M., 1989, Palynology, V13, P121; SMELROR M, 1993, PALAEOGEOGR PALAEOCL, V102, P121, DOI 10.1016/0031-0182(93)90009-8; Stancliffe R.P.W., 1988, INT S JUR STRAT, V2, P763; Wierzbowski H, 2007, PALAEOGEOGR PALAEOCL, V254, P523, DOI 10.1016/j.palaeo.2007.07.010; WOOLLAM R, 1983, Palynology, V7, P183; Woollam R., 1983, Report Institute of Geological Sciences, P1; Ziegler P.A., 1988, American Association Petrolium Geologists Memoir, V43, P1, DOI DOI 10.1306/M43478	31	7	7	0	2	POLSKA AKAD NAUK, POLISH ACAD SCIENCES, UNIV WARSAW, GEOLOGY DEPT	WARSZAWA	PL DEFILAD 1, WARSZAWA, 00-901, POLAND	0001-5709	2300-1887		ACTA GEOL POL	Acta Geol. Pol.		2012	62	3					439	461		10.2478/v10263-012-0025-8	http://dx.doi.org/10.2478/v10263-012-0025-8			23	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	021BR		Bronze			2025-03-11	WOS:000309860800012
J	Gedl, P; Kaim, A; Leonowicz, P; Boczarowski, A; Dudek, T; Kedzierski, M; Rees, J; Smolen, J; Szczepanik, P; Sztajner, P; Witkowska, M; Ziaja, J				Gedl, Przemyslaw; Kaim, Andrzej; Leonowicz, Paulina; Boczarowski, Aadrzej; Dudek, Teresa; Kedzierski, Mariusz; Rees, Jan; Smolen, Jolanta; Szczepanik, Patrycja; Sztajner, Przemyslaw; Witkowska, Magda; Ziaja, Jadwiga			Palaeoenvironmental reconstruction of Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Krakow-Silesia Homocline, Poland	ACTA GEOLOGICA POLONICA			English	Article						Bathonian; Jurassic; Palaeoenvironment; Ore-bearing clays; Poland	WOOD GENUS XENOXYLON; FAUNAL DYNAMICS; POLISH JURA; CARBONATE CONCRETIONS; CZESTOCHOWA AREA; ASSEMBLAGES	Gedl, P., Kaim, A., Leonowicz, P., Boczarowski, A., Dudek, T., Kedzierski, M., Rees, J., Smolen, J., Szczepanik, P., Sztajner, P., Witkowska, M. and Ziaja, J. 2012. Palaeoenvironmental reconstruction of Bathonian (Middle Jurassic) ore-bearing clays at Gnaszyn, Krakow-Silesia Homocline, Poland. Acta Geologica Polonica, 62 (3), 463-484. Warszawa. Multidisciplinary studies of the Middle-Upper Bathonian ore-bearing clays at Gnaszyn revealed variable palaeoenvironmental conditions during the deposition of this seemingly monotonous sequence. We interpret the conditions in the bottom environment and the photic zone, and also evaluate the influence of the adjacent land areas, based on sedimentology, geochemistry, sporomorphs and palynofacies composition, benthic (foraminifera, gastropods, bivalves, scaphopods, echinoderms), planktonic (calcareous nannoplankton, dinoflagellate cysts), and nektonic (sharks) fossils. The Gnaszyn succession originated relatively close to the shore, within reach of an intense supply of terrestrial fine clastic and organic particles. The latter are mainly of terrestrial origin and range from 1.5 to 2.5 wt.%. The precise water depth is difficult to estimate but most likely ranges from several tens of metres to a few hundred metres. All fossil groups show minor changes throughout the succession. As the climate seems to have been quite stable during this period we consider sea-level fluctuations to have been the main factor responsible for the changes. The terrestrial input, including freshwater and land-derived clastic and organic particles (sporomorphs and cuticles), increased during periods of sea-level lowstand. As a consequence, stress conditions (lower salinity, higher nutrient availability, lower water transparency) in the photic zone caused blooms of opportunistic planktonic taxa. Furthermore, a faster sedimentation rate led to oxygen depletion and deterioration of the living conditions in the bottom environment due to an increased accumulation of organic matter. As a result, the benthic biota became taxonomically impoverished and commonly dominated by juvenile forms. During periods of high sea level, the source areas were shifted away from the basin, resulting in a decrease in the terrestrial influx, increase in the salinity of surface waters, the appearance of more diverse phytoplankton assemblages, a lower sedimentation rate, and an improvement of living conditions at the bottom.	[Gedl, Przemyslaw; Dudek, Teresa] Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland; [Kaim, Andrzej] Polish Acad Sci, Inst Paleobiol, PL-00818 Warsaw, Poland; [Leonowicz, Paulina] Univ Warsaw, Inst Geol, PL-02089 Warsaw, Poland; [Boczarowski, Aadrzej] Univ Silesia, Fac Earth Sci, PL-41200 Sosnowiec, Poland; [Kedzierski, Mariusz; Szczepanik, Patrycja; Witkowska, Magda] Jagiellonian Univ, Inst Geol Sci, PL-30063 Krakow, Poland; [Smolen, Jolanta] Polish Geol Inst, PL-00975 Warsaw, Poland; [Sztajner, Przemyslaw] Univ Szczecin, Inst Marine Sci, Geol & Paleogeog Dept, PL-70383 Szczecin, Poland; [Ziaja, Jadwiga] Polish Acad Sci, W Szafer Inst Bot, PL-31512 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Paleobiology of the Polish Academy of Sciences; Polish Geological Institute - National Research Institute; University of Warsaw; University of Silesia in Katowice; Jagiellonian University; Polish Geological Institute - National Research Institute; University of Szczecin; Polish Academy of Sciences; W. Szafer Institute of Botany 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; kaim@twarda.pan.pl; Paulina.Leonowicz@uw.edu.pl; a.boczarowski@chello.pl; tereska_wing@yahoo.co.uk; mariusz.kedzierski@uj.edu.pl; janrees71@gmail.com; jolanta.smolen@pgi.gov.pl; szczep@ing.uj.edu.pl; sztajner@univ.szczecin.pl; magda.witkowsky@interia.pl; J.Ziaja@botany.pl	Kaim, Andrzej/G-6244-2010; Kedzierski, Mariusz/B-6138-2013	Kedzierski, Mariusz/0000-0002-1793-3160; Kaim, Andrzej/0000-0001-6186-5356; Ziaja, Jadwiga/0000-0002-3562-4812	Institute of Paleobiology of the Polish Academy of Sciences; Japan Society for the Promotion of Science (JSPS) [17.05324, 050500000614]; Polish Ministry of Science and Higher Education [N N307 116635]; Humboldt Fellowship	Institute of Paleobiology of the Polish Academy of Sciences; Japan Society for the Promotion of Science (JSPS)(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Polish Ministry of Science and Higher Education(Ministry of Science and Higher Education, Poland); Humboldt Fellowship(Alexander von Humboldt Foundation)	The research of A. Kaim was supported by the Institute of Paleobiology of the Polish Academy of Sciences, a Japan Society for the Promotion of Science (JSPS) Postdoctoral Fellowship for Foreign Researchers, JSPS research grant number 17.05324 (project number 050500000614), and a Polish Ministry of Science and Higher Education research grant N N307 116635, and completed during an Humboldt Fellowship.	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Pol.		2012	62	3					463	484						22	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	021BR					2025-03-11	WOS:000309860800013
J	Bogus, KA; Zonneveld, KAF; Fischer, D; Kasten, S; Bohrmann, G; Versteegh, GJM				Bogus, K. A.; Zonneveld, K. A. F.; Fischer, D.; Kasten, S.; Bohrmann, G.; Versteegh, G. J. M.			The effect of meter-scale lateral oxygen gradients at the sediment-water interface on selected organic matter based alteration, productivity and temperature proxies	BIOGEOSCIENCES			English	Article							WALLED DINOFLAGELLATE CYSTS; TETRAETHER MEMBRANE-LIPIDS; CORE-TOP CALIBRATION; NORTHERN ARABIAN SEA; MINIMUM ZONE; CONTINENTAL-MARGIN; SURFACE SEDIMENTS; ENHANCED PRESERVATION; BIOMARKER RECORD; MIDCHAIN DIOLS	A valid assessment of selective aerobic degradation on organic matter (OM) and its impact on OM-based proxies is vital to produce accurate environmental reconstructions. However, most studies investigating these effects suffer from inherent environmental heterogeneities. In this study, we used surface samples collected along two meter-scale transects and one longer transect in the northeastern Arabian Sea to constrain initial OM heterogeneity, in order to evaluate selective aerobic degradation on temperature, productivity and alteration indices at the sediment-water interface. All of the studied alteration indices, the higher plant alkane index, alcohol preservation index, and diol oxidation index, demonstrated that they are sensitive indicators for changes in the oxygen regime. Several export production indices, a cholesterol-based stanol/stenol index and dinoflagellate lipid- and cyst-based ratios, showed significant (more than 20%) change only over the lateral oxygen gradients. Therefore, these compounds do not exclusively reflect surface water productivity, but are significantly altered after deposition. Two of the proxies, glycerol dibiphytanyl glycerol tetraether-based TEX86 sea surface temperature indices and indices based on phytol, phytane and pristane, did not show any trends related to oxygen. Nevertheless, unrealistic sea surface temperatures were obtained after application of the TEX86, TEX86L, and TEX86H proxies. The phytol-based ratios were likely affected by the sedimentary production of pristane. Our results demonstrate the selective impact of aerobic organic matter degradation on the lipid and palynomorph composition of surface sediments along a short lateral oxygen gradient and suggest that some of the investigated proxies may be useful tracers of changing redox conditions at the sediment-water interface.	[Bogus, K. A.; Zonneveld, K. A. F.; Bohrmann, G.] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Bogus, K. A.; Zonneveld, K. A. F.; Fischer, D.; Bohrmann, G.; Versteegh, G. J. M.] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; [Kasten, S.] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	University of Bremen; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Bogus, KA (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28359 Bremen, Germany.	ka_bo@uni-bremen.de	; Versteegh, Gerard J.M./H-2119-2011; Bohrmann, Gerhard/D-4474-2017	Fischer, David/0000-0002-1698-5604; Versteegh, Gerard J.M./0000-0002-9320-3776; Bogus, Kara/0000-0003-4690-0576; Kasten, Sabine/0000-0001-7453-5137; Bohrmann, Gerhard/0000-0001-9976-4948	DFG-Research Center/Excellence Cluster MARUM "The Ocean in the Earth System"; DFG (Deutsche Forschungsgemeinschaft) as part of the International Graduate College "Proxies in Earth History" (EUROPROX); Helmholtz group; Heisenberg Fellowship [VE-486/2, VE-486/3]	DFG-Research Center/Excellence Cluster MARUM "The Ocean in the Earth System"(German Research Foundation (DFG)); DFG (Deutsche Forschungsgemeinschaft) as part of the International Graduate College "Proxies in Earth History" (EUROPROX)(German Research Foundation (DFG)); Helmholtz group; Heisenberg Fellowship(German Research Foundation (DFG))	We appreciate the efforts of the captain and crew of the R/V Meteor cruise M74/3, as well as the ROV "MARUM-QUEST 4000" team (MARUM, Bremen) for their excellent support during the cruise. We also thank S. Forke, G. Greif, and R. Himmelsbach for laboratory assistance. X. Liu was kind enough to perform the GDGT analysis. We thank the constructive criticism of two anonymous reviewers and the editor (J. Middelburg), whose comments improved this manuscript. Financial support was provided by the DFG-Research Center/Excellence Cluster MARUM "The Ocean in the Earth System", and the DFG (Deutsche Forschungsgemeinschaft) as part of the International Graduate College "Proxies in Earth History" (EUROPROX), as well as the Helmholtz group and a Heisenberg Fellowship (VE-486/2 and /3) to GJMV.	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J	Slimani, H; Louwye, S; Toufiq, A				Slimani, Hamid; Louwye, Stephen; Toufiq, Abdelkabir			New species of organic-walled dinoflagellate cysts from the Maastrichtian-Danian boundary interval at Ouled Haddou, northern Morocco	ALCHERINGA			English	Article						dinoflagellate cysts; taxonomy; biostratigraphy; Maastrichtian-Danian boundary; Ouled Haddou; northern Morocco	CRETACEOUS-TERTIARY BOUNDARY; NEW-ZEALAND; WOODSIDE CREEK; EASTERN RIF; BIOSTRATIGRAPHY; MARLBOROUGH; TRANSITION; SPAIN; GENUS; RIVER	Seven new dinoflagellate cyst species and subspecies, previously figured under open nomenclature, from Maastrichtian and Danian deposits of Ouled Haddou (eastern external Rif Chain) in northern Morocco are formally described, and their stratigraphic ranges are clarified. Conosphaeridium lifum sp.nov. and Kenleyia chabaka sp.nov. have fibrous and reticulate wall surfaces, respectively. Oligosphaeridium saghirum sp.nov. is a small cyst with funnel-shaped distal process extremities. Spiniferella cornuta subsp. kacira subsp. nov. and Fibrocysta brevispinosa sp. nov. are distinguishable by their very short processes. Riculacysta chaouka sp. nov. is characterized by its perforate spinose ectophragm. Andalusiella bacita sp. nov. is a small and spindle-shaped cyst with only a single antapical horn.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Rabat 10106, Morocco; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Toufiq, Abdelkabir] Univ Chouaib Doukkali, Fac Sci, Lab Geosci & Environm Tech, El Jadida 24000, Morocco	Mohammed V University in Rabat; Ghent University; Chouaib Doukkali University of El Jadida	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma; stephen.louwye@ugent.be; toufiq_a@yahoo.fr	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Slimani, Hamid/0000-0001-6392-1913	National Centre of Scientific and Technical Research (CNRST) (research unit URAC 46); University Mohammed V-Agdal [SVT11/09]	National Centre of Scientific and Technical Research (CNRST) (research unit URAC 46); University Mohammed V-Agdal	We thank Mrs Sabine Van Cauwenberghe (Palaeontology Research Unit, University of Gent, Belgium) for the palynological preparation of the studied samples. The first author acknowledges support from National Centre of Scientific and Technical Research (CNRST) (research unit URAC 46) and the University Mohammed V-Agdal (Project SVT11/09). Dr S. McLoughlin (Honorary Editor) and two anonymous journal reviewers, are kindly thanked for their constructive reviews and critical comments that improved the original manuscript.	ANGALA R., 1985, B SOC GEOLOGIQUE FRA, V8, P747; [Anonymous], 1831, SYMBOLAE PHYS SEU IC; [Anonymous], 1976, SCI GEOLOGIQUES B M; [Anonymous], COMPTES RENDUS SEANC; [Anonymous], SCI GEOLOGIQUES B; [Anonymous], 1885, HG BRONNS KLASSEN OR; Arambourg C., 1935, Bulletin de la Societe Geologique de France Ser 5, V5, P413; Arambourg C., 1952, Service Geologique au Maroc, Notes et Memoires, V92, P1; ARAMBOURG C., 1950, COMPTES RENDUS SOC S, V16, P70; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; Benson D.G. 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J	Sarkar, S				Sarkar, Samir			A new species of <i>Muratodinium</i> (Cookson & Eisenack) Drugg from the Subathu Formation (Lutetian) of Lesser Himalaya, India and its biostratigraphic significance	HIMALAYAN GEOLOGY			English	Article						Dinoflagellate; Muratodinium subathuensis; Index fossil; Subathu Formation (Lutetian); Lesser Himalaya	DINOFLAGELLATE; NORTH	A new organic-walled dinoflagellate cyst species Muratodinium subathuensis spoor has been erected from the Subathu Formation (Lutetian) of the Lesser Himalaya, India. It has been observed that this species is associated with near shore estuarine environment and restricted only to the Lutetian sediments of the Subathu Formation. Its significance as a biostratigraphic marker for the Eocene strata in the Lesser Himalaya is discussed.	Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Sarkar, S (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	sarkarsamir@rediffmail.com						Alberti G., 1961, Palaeontographica, V116, P1; [Anonymous], HIMAL GEOL; [Anonymous], PALAEOBOTANIST; Bagi H., 1992, THESIS PUNJAB U CHAN; BHATIA SB, 2005, SPECIAL PUBLICATION, V2, P105; BHATIA SB, 1993, SEM HIM GEOL GEOPH W, P59; Chen-quan, 1980, SOME NEW GENERA OLIG, P1; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; Davey R.J., 1970, B BR MUS NAT HIS G, V18, P333; Drugg W.S., 1970, N AM PAL CONV CHIC G, P809; Eisenack A., 1960, Neues Jahrb. Geol. P.-M., P511; Farr E.R., 1979, REGNUM VEGETABILE, V100, P1896; Fritsch F.E., 1935, Structure and Reproduction of Algae, V1, P791; Haeckel E., 1894, SYST PHYLOG PROTISTE, P1; Jain K.P., 1981, Journal of the Palaeontological Society of India, V26, P6; Khanna A.K., 1985, GEOSCI J, V6, P105; Khanna A.K., 1979, HIMAL GEOL, V9, P255; Lentin JK., 1993, AM ASS STRATIGRAPHIC, V28, P856; Mathur K., 1963, SCI CULTURE, V29, P250; MATHUR KAWAL, 1964, SCI CULT, V30, P607; Mathur N.S., 2000, WADIA I HIMALAYAN GE; Mathur N.S., 1978, RECENT RES GEOLOGY, V5, P96; MATHUR YK, 1986, REV PALAEOBOT PALYNO, V47, P193, DOI 10.1016/0034-6667(86)90013-8; Medlicott H.B., 1964, MEN GEOL IND, V3, P1; Morzadec-Kerfoum M, 1980, 5 INT PAL C CAMBR UK, P270; MOSHKOVITZ S, 1993, MICROPALEONTOLOGY, V39, P167, DOI 10.2307/1485838; Pal D., 2000, HIMAL GEOL, V21, P133; Pascher A., 1914, FLAGELLATEN ALGENBER, V32, P132; Reid P.C., 1974, Nova Hedwigia, V25, P579; Rossignol M., 1962, 2 SEDIMENTS PLEISTOC, V4, P121; SALUJHA SK, 1969, J PALAEONTOLOGICAL S, V12, P25; SARKAR S, 1988, Palaeontographica Abteilung B Palaeophytologie, V209, P29; Sarkar S., 2000, J PALAEONTOLOGICAL S, V45, P37; Sarkar S., 1997, J PETROL GEOL, V6, P99; Sarkar Samir, 2000, Himalayan Geology, V21, P167; Singh H.P., 1992, GEOPHYTOLOGY, V22, P181; Singh H.P., 1987, PALEOBOTANIST, V35, P249; Singh H.P., 1987, PALEOBOTANIST, V35, P204; Singh H.P., 1978, HIMAL GEOL, V8, P33; Singh Y. R., 2007, MICROPALAEONTOLOGY A, P131; Stover L.E., 1978, Analyses of Pre-Pleistocene Organic-Walled Dinoflagellates, V15; WALL D, 1969, J PHYCOL, V5, P140, DOI 10.1111/j.1529-8817.1969.tb02595.x; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1	43	0	0	0	4	WADIA INST HIMALAYAN GEOLOGY	DEHRA DUN	33 GENERAL MAHADEO SINGH RD, DEHRA DUN, 248 001, INDIA	0971-8966			HIMAL GEOL	Himal. Geol.		2012	33	2					173	179						7	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	990IW					2025-03-11	WOS:000307625200008
J	Gonçalves, AA; Gagnon, GA				Goncalves, Alex Augusto; Gagnon, Graham A.			Recent Technologies for Ballast Water Treatment	OZONE-SCIENCE & ENGINEERING			English	Article						IMO; International Marine Organization (IMO); Ballast water; Bioinvasions; Treatment; disinfection	CRUMB RUBBER FILTRATION; DIAPAUSING EGGS; DINOFLAGELLATE CYSTS; OZONE TREATMENT; GREAT-LAKES; SHIPS; RISK; BIOCIDES; EXCHANGE; EFFICACY	Concern about ballast-mediated bioinvasions into freshwater, estuarine and marine habitats is not limited to biodiversity per se but extends to its broader socio-economic impacts on agriculture, forests, fisheries, aquaculture, and other human activities dependent on the stability of living resources in a particular ecosystem. As a result, invasive species pose almost incalculable economic, socio-cultural and human health security risks. The importance of biological invasions was brought into greater focus as several devastating introductions in many countries occurred and given the limitations of the IMO (International Marine Organization) Guidelines. Consequently the International Convention for the Control and Management of Ships' Ballast Water and Sediments was prepared and was adopted in a Diplomatic Conference in 2004. This Convention aimed to prevent, minimize and ultimately eliminate the risks to the environment, human health, property and resources arising from the transfer of harmful aquatic organisms and pathogens via ships' ballast waters. This article describes recent ballast water treatment studies from scientific and academic community since the last IMO Convention in 2004, and the treatment that received basic and final approval by IMO. We examined different methods available on scientific media to treat ballast water (lab-scale and field-scale tests) and we concluded that a standardization of ballast water treatment still to be done to ensure the IMO Standard.	[Goncalves, Alex Augusto] Fed Univ Semi Arid UFERSA, Dept Anim Sci, BR-59625900 Mossoro, RN, Brazil; [Gagnon, Graham A.] Dalhousie Univ, Ctr Water Resources Studies, Halifax, NS B3J 1Z1, Canada	Universidade Federal Rural do Semi-Arido (UFERSA); Dalhousie University	Gonçalves, AA (通讯作者)，Fed Univ Semi Arid UFERSA, Dept Anim Sci, Av Francisco Mota 572, BR-59625900 Mossoro, RN, Brazil.	alaugo@gmail.com	Gagnon, Graham/J-3891-2019	Gagnon, Graham/0000-0001-5925-2294	Foreign Affairs and International Trade Canada (DFAIT)	Foreign Affairs and International Trade Canada (DFAIT)	The present study was carried out with the support of Foreign Affairs and International Trade Canada (DFAIT), which are also acknowledged.	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Eng.		2012	34	3					174	195		10.1080/01919512.2012.663708	http://dx.doi.org/10.1080/01919512.2012.663708			22	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	950SL					2025-03-11	WOS:000304669100006
J	Verhoeven, K; Louwye, S				Verhoeven, Koen; Louwye, Stephen			<i>Selenopemphix islandensis</i> sp nov.: a new organic-walled dinoflagellate cyst from the Lower Pliocene Tjornes beds, northern Iceland	PALYNOLOGY			English	Article						Pliocene; dinoflagellate cysts; taxonomy; Selenopemphix; Tjornes; Iceland; Bering Strait	PLEISTOCENE SEDIMENTS; MIOCENE; PALEOECOLOGY; STRATIGRAPHY; ASSEMBLAGES; ZONATION; BELGIUM; MIDDLE	A new protoperidiniacean dinoflagellate cyst species recorded from the Lower Pliocene Serripes Zone of the Tjornes beds in northern Iceland is formally described and its palaeoecological preferences are evaluated. Selenopemphix islandensis sp. nov. is a thin-walled cyst with strong polar compression and a reniform outline in apical view. The wide cingular margins are dorsally ornamented with processes of varying morphology and ventrally with large fan-shaped processes. A distinct size difference between the dorsal and ventral cingular processes is a major diagnostic characteristic of this species. A differential diagnosis for Selenopemphix islandensis sp. nov. is presented. Within the Tjornes section, Selenopemphix islandensis sp. nov. is restricted to the uppermost Serripes Zone of the Tjornes beds. The base of this zone corresponds to the invasion of cold-water molluscs of Pacific affinity through the Bering Strait into the northern Atlantic. The sudden appearance of Selenopemphix islandensis sp. nov. from this level can possibly be related to this northern migration through the Bering Strait, and suggest a Pacific origin. The new species is not recorded in the underlying Lower Pliocene Tapes Zone and Mactra Zone of the Tjornes beds, and is also absent in the superjacent Pleistocene Breidavik Group. Selenopemphix islandensis sp. nov. has a first and last appearance in the Tjornes region at c. 4.5 Ma and 4.2 Ma, respectively. Palaeoecological studies on molluscs, ostracods, plants and oxygen isotopes indicate an average summer temperature of 5-10 degrees C for the Serripes Zone, which is comparable to the present-day situation in northern Iceland.	[Verhoeven, Koen; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Ghent University	Verhoeven, K (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	koen.verhoeven@ugent.be	Verhoeven, Koen/IZP-9609-2023; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313				Akhmetiev M.A., 1978, ACAD SCI USSR SOVIET, V316; AKHMETIEV MA, 1975, P USSR ACAD SCI GEOL, V7, P100; [Anonymous], 1894, SYSTEMATISCHE PHYLOG; [Anonymous], 1914, BER DTSCH BOT GES, DOI DOI 10.1111/J.1438-8677.1914.TB07573.X; [Anonymous], 1885, HG BRONNS KLASSEN OR; ARONSON JL, 1975, EARTH PLANET SC LETT, V28, P83, DOI 10.1016/0012-821X(75)90077-1; Balech E., 1988, Publ. Espec. Inst. Esp. 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J	Soliman, A; Coric, S; Head, MJ; Piller, WE; El Beialy, SY				Soliman, Ali; Coric, Stjepan; Head, Martin J.; Piller, Werner E.; El Beialy, Salah Y.			Lower and Middle Miocene biostratigraphy, Gulf of Suez, Egypt based on dinoflagellate cysts and calcareous nannofossils	PALYNOLOGY			English	Article						dinoflagellate cysts; calcareous nannofossils; Miocene; Gulf of Suez; Egypt	DINOCYST STRATIGRAPHY; BOREHOLE; BASIN; RIFT; CHRONOLOGY; OLIGOCENE; DEPOSITS; EVENTS	This is the first detailed stratigraphic correlation of Lower and Middle Miocene deposits in the Gulf of Suez, Egypt using dinoflagellate cysts. The correlation is based on 273 ditch-cutting samples from five onshore boreholes located along the southwestern margin of the Gulf of Suez. The interval studied is represented by the Nukhul, Rudeis and Kareem formations of the Gharandal Group, and the lower part of the Belayim Formation of the Ras Malaab Group. These Miocene deposits unconformably overlie the Lower or lower Middle Eocene. The dinoflagellate cyst record is more diverse than previously reported and many taxa are documented for the first time in Egypt. Five biozones are established and tied to a chronostratigraphic framework by calibration to calcareous nannofossils (NN biozones) obtained from the same set of samples: (1) Lingulodinium machaerophorum Assemblage Biozone (GOS1), Aquitanian through mid-Burdigalian; (2) Exochosphaeridium insigne Taxon-range Biozone (GOS2), lower through mid-Burdigalian; (3) Apteodinium spiridoides Interval Biozone (GOS3), mid-Burdigalian through lower Langhian; (4) Cleistosphaeridium placacanthum Interval Biozone (GOS4), upper Burdigalian, Langhian, and lower Serravallian?); and (5) Polysphaeridium zoharyi Assemblage Biozone (GOS5), upper Langhian and Serravallian? Comparison with other Miocene biozonations from the Mediterranean, Central Paratethys, North Atlantic region, and eastern USA indicate that the highest occurrences of Apteodinium spiridoides, Cordosphaeridium cantharellus, Distatodinium paradoxum, Exochosphaeridium insigne and Cleistosphaeridium placacanthum, and the lowest occurrences of Exochosphaeridium insigne and Sumatradinium soucouyantiae are important datums, whereas the lowest occurrences of Hystrichosphaeropsis obscura, Labyrinthodinium truncatum, and Operculodinium? borgerholtense provide useful supporting age control.	[Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci Geol & Palaeontol, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Coric, Stjepan] Geol Survey Austria, Sedimentary Geol Sect, A-1030 Vienna, Austria; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [El Beialy, Salah Y.] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University; Brock University; Egyptian Knowledge Bank (EKB); Mansoura University	Soliman, A (通讯作者)，Graz Univ, Inst Earth Sci Geol & Palaeontol, Heinrichstr 26, A-8010 Graz, Austria.	ali.soliman@uni-graz.at	Beialy, Salah/AAD-7329-2020; Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607; Piller, Werner E./0000-0003-2808-4720	OAD; Austrian Exchange Services; Ministry of Higher Education, Egypt; Palynological Association AASP; OAW, the Austrian Academy of Sciences; Natural Sciences and Engineering Research Council of Canada	OAD; Austrian Exchange Services; Ministry of Higher Education, Egypt(Ministry of Higher Education & Scientific Research (MHESR)); Palynological Association AASP; OAW, the Austrian Academy of Sciences; Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	The presented data are based partly on the first author's Ph.D. thesis. AS thanks OAD, the Austrian Exchange Services, and the Ministry of Higher Education, Egypt for providing financial support. Partial funding was provided by The Palynological Association AASP, and OAW, the Austrian Academy of Sciences. MJH acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. Our appreciation goes to M. Faris (Tanta University, Egypt) for providing samples of the Kareem-30 borehole, and the Egyptian General Petroleum Corporation for kindly providing other borehole samples and releasing basic data. We are grateful to K. Dybkjaer (Geological Survey of Denmark and Greenland, Copenhagen) and J.B. Riding (British Geological Survey, Nottingham) for their helpful reviews of the MS.	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J	Willumsen, PS				Willumsen, Pi Suhr			Three new species of dinoflagellate cyst from Cretaceous-Paleogene (K-Pg) boundary sections at mid-Waipara River and Fairfield Quarry, South Island, New Zealand	PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Cretaceous-Paleogene boundary transition; stratigraphy; biostratigraphy; South Island; New Zealand	TERTIARY BOUNDARY; PALEOENVIRONMENTAL CHANGES; NORTH CANTERBURY; TRANSITION; BIOSTRATIGRAPHY; MARLBOROUGH; IRIDIUM; IMPACT; EOCENE; MARGIN	A palynological investigation of marine uppermost Maastrichtian to lower Paleocene strata in two New Zealand sections, mid-Waipara River and Fairfield Quarry, revealed well-preserved dinoflagellate cyst assemblages including three new dinoflagellate cyst species. A formal description of the new dinoflagellate cyst species are presented here. Furthermore a variation of Carpatella cornuta, named C. aff. cornuta is discussed. In the mid-Waipara River section the ranges of the new species Adnatosphaeridium regulatum sp. nov., Alterbidinium mcmillanii sp. nov. and Canningia fairfieldensis sp. nov. are calibrated directly with other microfossil groups including foraminifera, radiolarian and terrestrially derived spores and pollen. The last occurrence of Adnatosphaeridium regulatum sp. nov. is within the lowermost Danian foraminiferal zone P alpha and this event is recorded in sections located in several New Zealand sedimentary basins. Alterbidinium mcmillanii sp. nov. has a very restricted range within the latest Maastrichtian to basal Danian with its last occurrence within foraminferal zone P0. Canningia fairfieldensis sp. nov. has so far only been recorded in lower Danian strata and occurs within the foraminiferal zones P alpha to P1c and radiolarian zones RP1? RP2. A morphological variation of Carpatella cornuta named Carpatella aff. cornuta is only observed in a very narrow interval across the Cretaceous-Paleogene (K-Pg) boundary in the mid-Waipara River section. Based on comparison with other New Zealand K-Pg boundary sections, A. mcmillanii sp. nov. and C. fairfieldensis sp. nov. seem to have a palaeoenvironmental affinity for shallow marine to inner neritic depositional environments.	Lund Univ, Dept Geol, SE-22362 Lund, Sweden	Lund University	Willumsen, PS (通讯作者)，Lund Univ, Dept Geol, Solvegatan 12, SE-22362 Lund, Sweden.	pi.willumsen@geol.lu.se			New Zealand Marsden Fund; Danish Carlsberg Foundation [2008_ 01_ 0404]; Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI)	New Zealand Marsden Fund(Royal Society of New ZealandMarsden Fund (NZ)); Danish Carlsberg Foundation(Carlsberg Foundation); Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI)	This palynological study was part of a multidisciplinary research programme supported by the New Zealand Marsden Fund and lead by Chris Hollis, Geological and Nuclear Sciences, New Zealand (GNS). The author acknowledges a personal grant from the Danish Carlsberg Foundation (Grant No. 2008_ 01_ 0404) and financial support from Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI). Graeme J. Wilson and Ian Raine (GNS) are acknowledged for sharing their extensive knowledge of Mesozoic-Cainozoic palynology. Simon McMillan is thanked for his assistance when the K-Pg boundary transition in Fairfield Quarry was sampled. Chris Hollis, Jerry Dickens, Brad Field, Percy Strong and Poul Schioler are thanked for assisting in the sampling of the mid-Waipara section. Margaret Collinson is thanked for collecting the high-resolution sample suite across the K-Pg boundary transition in the mid-Waipara River section.	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Surv. Rec, V20, P8; Wilson GJ, 1996, 9639 I GEOL NUCL SCI, P1; WILSON GRAEME J., 1967, N Z J BOT, V5, P223	65	11	12	0	5	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2012	36			1	SI		48	62		10.1080/01916122.2011.642260	http://dx.doi.org/10.1080/01916122.2011.642260			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	947VL					2025-03-11	WOS:000304460700004
J	Oboh-Ikuenobe, FE; Spencer, MK; Campbell, CE; Haselwander, RD				Oboh-Ikuenobe, Francisca E.; Spencer, Marissa K.; Campbell, Carl E.; Haselwander, Robert D.			A portrait of Late Maastrichtian and Paleocene palynoflora and paleoenvironment in the northern Mississippi Embayment, southeastern Missouri	PALYNOLOGY			English	Article						Late Maastrichtian-Paleocene; northern Mississippi Embayment; palynology; palynofacies; southeastern Missouri	CRETACEOUS-TERTIARY BOUNDARY; OLIGOCENE DINOFLAGELLATE CYSTS; CALCAREOUS NANNOFOSSIL; GEOLOGIC HISTORY; EOCENE; STRATIGRAPHY; BIOSTRATIGRAPHY; PALYNOFACIES; EXTINCTION; SEDIMENTS	Upper Cretaceous and lower Paleogene sedimentary rocks in southeastern Missouri record the northwest extension of the Mississippi Embayment, yet very little information exists about them due to rarity of outcrops and borehole material. This has hindered a clearer understanding of the depositional conditions before and after the terminal Cretaceous impact event. Access to freshly excavated sediments of the Owl Creek, Clayton and Porters Creek formations and to material from several US Geological Survey boreholes has provided a wealth of data to study this time interval in the area. In this study, detailed palynomorph and palynofacies data have been used to infer palynostratigraphy and paleovegetation. Characteristics of lithology, ichnofossils, invertebrate fossils, foraminifera and well logs have provided the framework for reconstructing the depositional history. Palynomorphs indicate Late Maastrichtian, Danian and Thanetian-Selandian ages for the Owl Creek, Clayton and Porters Creek formations, respectively. Although the Cretaceous-Paleogene (K-Pg) boundary itself is marked by an unconformity, the basal part of the overlying Clayton Formation was apparently deposited as a single megatsunamite following the Chicxulub impact event. Palynofloras suggest mixed coastal and inland subtropical forest vegetation dominated by angiosperm taxa, although abundant records of gymnosperm pollen production occurred at various times during the deposition of the Porters Creek. While terrestrially derived organic components dominate the four palynofacies assemblages (A-D) identified by cluster analysis, lithologic, ichnofacies, macrofossil and dinoflagellate cysts suggest that assemblages C and D, which are characterized by higher percentages of amorphous organic matter, represent more distal marine depositional environments.	[Oboh-Ikuenobe, Francisca E.; Spencer, Marissa K.; Haselwander, Robert D.] Missouri Univ Sci & Technol, Dept Geol & Geophys, Rolla, MO 65409 USA; [Campbell, Carl E.] St Louis Community Coll Meramec, St Louis, MO 63122 USA	University of Missouri System; Missouri University of Science & Technology	Oboh-Ikuenobe, FE (通讯作者)，Missouri Univ Sci & Technol, Dept Geol & Geophys, 129 McNutt Hall, Rolla, MO 65409 USA.	ikuenobe@mst.edu		Oboh-Ikuenobe, Francisca/0000-0002-2223-9691				[Anonymous], GEOLOGICAL SOC AM SP; Batten D., 1996, Palynology: principles and applications, P1011; Benton MJ, 2004, ATLAS LIFE EARTH, P214; Bercovici A, 2009, CRETACEOUS RES, V30, P632, DOI 10.1016/j.cretres.2008.12.007; BOULTER M C, 1982, Palynology, V6, P55; 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, 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; Campbell CE, 2007, GEOL SOC AM SPEC PAP, V437, P189, DOI 10.1130/2008.2437(11); Davis J.C., 2015, Statistics and data analysis in Geology, V3rd; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome R. 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J	Slimani, H; Louwye, S				Slimani, Hamid; Louwye, Stephen			New junior synonyms of the Late Cretaceous dinoflagellate cysts <i>Membranigonyaulax wilsonii</i> Slimani 1994 and <i>Turnhosphaera hypoflata</i> (Yun 1981) Slimani 1994	PALYNOLOGY			English	Article						dinoflagellate cysts; synonymy; taxonomy; Membranigonyaulax wilsonii; Turnhosphaera hypoflata; Late Cretaceous	BIOSTRATIGRAPHY	The Late Cretaceous organic-walled dinoflagellate cyst species Microdinium? sincfalensis Louwye 1997 and Invertocysta flandriensis Louwye 1997 are considered to be junior synonyms of Membranigonyaulax wilsonii Slimani 1994 and Turnhosphaera hypoflata (Yun 1981) Slimani 1994, respectively.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Rabat 10106, Morocco; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Mohammed V University in Rabat; Ghent University	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Slimani, Hamid/0000-0001-6392-1913; Louwye, Stephen/0000-0003-4814-4313	University Mohammed V-Agdal [SVT 11/09]; National Center of Scientific Research (CNRST), Morocco [URAC46]	University Mohammed V-Agdal; National Center of Scientific Research (CNRST), Morocco	The authors thank the Research Unit Palaeontology, Ghent University, Belgium for technical support and the University Mohammed V-Agdal (project SVT 11/09) and the National Center of Scientific Research (CNRST) (URAC46), Morocco for financial support. The constructive comments by James B. Riding, Claus Heilmann-Clausen and an anonymous reviewer improved the manuscript considerably; their remarks are much appreciated.	[Anonymous], 1997, ANN SOC GEOLOGIQUE B; Butschli O., 1885, Klassen und Ordnungen des Thier-Reichs, Wissenschaftlich Dargestellt in Wort und Bild, P865; COOKSON I C, 1982, Palaeontographica Abteilung B Palaeophytologie, V184, P23; COOKSON ISABEL C., 1960, MICROPALEONTOLOGY, V6, P1, DOI 10.2307/1484313; EDWARDS LE, 1984, DEEP SEA DRILLING PR, V81, P581; Fensome R.A., 1993, Micropaleontology Press Special Paper; Kirsch K.-H., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V22, P1; LINDEMANN E., 1928, NAT RLICHEN PFLANZEN, P3; Marheinecke Uwe, 1992, Palaeontographica Abteilung B Palaeophytologie, V227, P1; Norvick M.S., 1976, BUR MIN RES GEOL GEO, V151, P21; PASCHER A, 1914, DTSCH BOT GESELL BER, V36, P136; Schioler P, 1997, MAR MICROPALEONTOL, V31, P65, DOI 10.1016/S0377-8398(96)00058-8; Slimani H, 2011, NETH J GEOSCI, V90, P129; Slimani Hamid, 1994, Memoires pour Servir a l'Explication des Cartes Geologiques et Minieres de la Belgique, V37, P1; Slimani Hamid, 2001, Geologica et Palaeontologica, V35, P161; Slimani Hamid, 2000, Memoirs of the Geological Survey of Belgium, V46, P1; TAYLOR FJR, 1980, BIOSYSTEMS, V13, P65, DOI 10.1016/0303-2647(80)90006-4; Wilson G.J., 1971, P 2 PLANKT C ROM, V2, P1259; Wilson GJ., 1974, THESIS U NOTTINGHAM; YUN H-S, 1981, Palaeontographica Abteilung B Palaeophytologie, V177, P1	20	2	2	0	2	TAYLOR & FRANCIS INC	PHILADELPHIA	325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA	0191-6122			PALYNOLOGY	Palynology		2012	36	1					110	115		10.1080/01916122.2012.662179	http://dx.doi.org/10.1080/01916122.2012.662179			6	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	947VC					2025-03-11	WOS:000304459500007
J	Garzon, S; Warny, S; Bart, PJ				Garzon, Sandra; Warny, Sophie; Bart, Philip J.			A palynological and sequence-stratigraphic study of Santonian-Maastrichtian strata from the Upper Magdalena Valley basin in central Colombia	PALYNOLOGY			English	Article						Campanian; dinoflagellate cysts; Maastrichtian; pollen; Santonian; sequence stratigraphy; spores	NORTHERN SOUTH-AMERICA; DINOFLAGELLATE CYSTS; SEA; FRAMEWORK; VENEZUELA; ECUADOR	This paper presents a sequence-stratigraphic interpretation from the palynological analysis and lithologic data of two outcrop sections on the NE flank of the Upper Magdalena Valley (UMV) basin primarily comprising the Santonian-Lower Maastrichtian interval. Important stratal horizons are identified in the northeastern part of the UMV basin and ages assigned to them. A cyclic pattern of palynomorph distribution was recognized in both sections and tied to the different stages of the stratigraphic chart. Spikes in abundance of spores accompanied by pollen characterize the lowstand systems tracts and are replaced by the occurrence of euryhaline dinoflagellate cysts (ceratioids and/or gymnodinioids) during the subsequent transgressive phase. Maximum flooding surfaces (MFS) are recognized by a sudden increase in open marine palynomorphs (peridinioids and/or gonyaulacoids) and the scarcity of terrestrial representatives. As sea level starts to fall, the gradual decrease in open marine dinoflagellates along with the occurrence of euryhaline dinoflagellate cysts and terrestrial representatives corresponds to highstand systems tracts. The sequence-stratigraphic interpretation from palynological analysis was correlated to the global sea-level curve allowing the identification of the Santonian-Campanian and Campanian-Maastrichtian boundaries. System tracts from supercycles ZC-3, ZC-4 and TA-1 were recognized from the palynological data.	[Garzon, Sandra; Warny, Sophie; Bart, Philip J.] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Garzon, Sandra; Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Garzon, Sandra] Smithsonian Trop Res Inst, Panama City, Panama	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; Smithsonian Institution; Smithsonian Tropical Research Institute	Garzon, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.	sgarzo1@tigers.lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	Museum of Natural Science and the Department of Geology and Geophysics CENEX Laboratory at Louisiana State University (Baton Rouge, LA); Smithsonian Tropical Research Institute in Panama; Colombian Petroleum Institute	Museum of Natural Science and the Department of Geology and Geophysics CENEX Laboratory at Louisiana State University (Baton Rouge, LA); Smithsonian Tropical Research Institute in Panama(Smithsonian InstitutionSmithsonian Tropical Research Institute); Colombian Petroleum Institute	The authors are grateful to Dr David Pocknall and two anonymous reviewers for their in-depth critique of the manuscript, which resulted in a much-improved paper. S. Garzon would like to thank the Museum of Natural Science and the Department of Geology and Geophysics CENEX Laboratory at Louisiana State University (Baton Rouge, LA), the Smithsonian Tropical Research Institute in Panama and the Colombian Petroleum Institute for their financial and logistical support during her masters thesis research project. The authors also thank Dr Carlos Jaramillo, Carlos Santos and Manuel Paez for their collaboration with this project.	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J	Quattrocchio, ME; Martínez, MA; Asensio, MA; Cornou, ME; Olivera, DE				Quattrocchio, Mirta E.; Martinez, Marcelo A.; Asensio, Marcos A.; Elina Cornou, M.; Olivera, Daniela E.			PALYNOLOGY OF EL FOYEL GROUP (PALEOGENE), NIRIHUAU BASIN, ARGENTINA	REVISTA BRASILEIRA DE PALEONTOLOGIA			English	Article						Paleogene; Palynology; El Foyel Group; Nirihuau Basin; Argentina	DINOFLAGELLATE CYSTS; SEDIMENTS; PROVINCE; MIOCENE; NORTH	This work aims to analyze the paleovegetation, paleoclimates and paleoceanography of the Paleogene of the Rio Foyel section (El Foyel Group), Nirihuau Basin, Argentina. It comprises Troncoso, Salto del Macho and Rio Foyel formations. Sporomorph analysis reflects a regional forest dominated by Nothofagaceae, Myrtaceae, Podocarpaceae and Palmae, developed under a temperate to warm-temperate and humid climate. In the studied section, the relation between terrestrial/marine palynomorphs is considered. In the Troncoso Formation, terrigenous palynomorphs dominate over marine elements. The recurrent presence of gymnosperm pollen with Araucariaceae indicates temperate and humid conditions. The Salto del Macho Formation shows a retraction of the gymnosperm forest, associated with the dominance of Nothofagus. forest, indicating a temperate and humid condition. In the Rio Foyel Formation, the sporomorphs indicate the presence of a temperate to warm-humid forest with subordinate open areas and a remarkable input from the coastal environment. In the same formation, the palynological characteristics, which indicate upward shallowing, allow the identification of parasequences. The bounding surfaces of parasequences are defined as surfaces of flooding which represent a relative sea level rise (marine flooding surfaces). The Rio Foyel Formation shows an upward shallowing sequence, indicated by the decrease in abundance and diversity of dinocysts. Different marine flooding surfaces were detected, associated with the diversity and abundance of dinocyst. A comparison of these spore-pollen assemblages with others from Patagonia, using multivariate statistic techniques, yields strong similarities between the Troncoso Formation and the Sloggett Formation (late Eocene to ?early Oligocene); and between Salto del Macho and Rio Foyel formations with Loreto formation (late Eocene-Oligocene) and San Julian Formation in cabo Curioso area (Oligocene).	[Quattrocchio, Mirta E.; Martinez, Marcelo A.] Univ Nacl Sur, Dept Geol, Inst Geol Sur, CONICET, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Asensio, Marcos A.] TECPETROL, 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)	Quattrocchio, ME (通讯作者)，Univ Nacl Sur, Dept Geol, Inst Geol Sur, CONICET, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	mquattro@criba.edu.ar; martinez@criba.edu.ar; marcos.asensio@tecpetrol.com; elina.cornou@uns.edu.ar; danielaolivera@yahoo.com.ar	Cornou, María/Q-5430-2019	Martinez, Marcelo/0000-0003-0538-4739	Agencia Nacional de Promocion Cientifica y Tecnologica; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Secretaria de Ciencia y Tecnologia (SECyT) of the Universidad Nacional del Sur	Agencia Nacional de Promocion Cientifica y Tecnologica(ANPCyTSpanish Government); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Secretaria de Ciencia y Tecnologia (SECyT) of the Universidad Nacional del Sur(Secretaria de Ciencia y Tecnologia (SECYT))	This research was supported by funds from Agencia Nacional de Promocion Cientifica y Tecnologica, Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET) and Secretaria de Ciencia y Tecnologia (SECyT) of the Universidad Nacional del Sur. In particular, we thank the Administracion de Parques Nacionales for permitting access to the outcrops. The authors wish to thank W. Volkheimer as well as C. Jaramillo, M.C. Zamaloa and two anonymous referees for reviewing this manuscript and offering very valuable comments and advice.	Abbink O.A., 1998, LAB PALAEOBOT PALYNO, V8, P1; [Anonymous], REV ASOCIACION GEOLO; Anzotegui L.M., 2006, THESIS U NACL NORDES; ARCHANGELSKY S, 1973, Ameghiniana, V10, P339; ARCHANGELSKY S, 1976, Ameghiniana, V13, P169; ARCHANGELSKY S, 1974, Ameghiniana, V11, P217; Archangelsky S., 1986, Ameghiniana, V23, P35; Archangelsky S., 1972, Revista del Museo de la Plata, seccion Paleontologia, P65; ASENSIO M., 2005, 16 C GEOL ARG LA PLA, V3, P271; Asensio M., 2008, 7 C EXPL DES HIDR MA, V7, P565; Asensio Marcos A, 2010, Rev. Asoc. Geol. 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JAN-APR	2012	15	1					67	84		10.4072/rbp.2012.1.06	http://dx.doi.org/10.4072/rbp.2012.1.06			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	944TA		Bronze			2025-03-11	WOS:000304225500006
J	De Schutter, PJ; Wijnker, E				De Schutter, Pieter J.; Wijnker, Erik			Large <i>Centrophorus</i> (Chondrichthyes, Squaliformes) of the Belgian Neogene continental shelf.	GEOLOGICA BELGICA			English	Article						Centrophoridae; Pliocene; Kattendijk Formation; Deurganckdok; Belgium; North Sea Basin	DINOFLAGELLATE CYST; NORTHERN BELGIUM; CENTROSCYMNUS-COELOLEPIS; REPRODUCTIVE-BIOLOGY; SHARK FAUNA; PLIOCENE; LAMNIFORMES; MIOCENE	A number of isolated teeth of gulper sharks (genus Centrophorus Muller & Henle, 1837) have been recovered from Neogene sands in the Antwerp area, marking the first occurrence of the genus Centrophorus in the fossil record of Belgium and the North Sea Basin. The precise stratigraphic origin of these teeth could not be established, but the taphonomic condition strongly suggests a Late Miocene or Early Pliocene age, although reworking from older Miocene strata cannot be excluded. These teeth are remarkable for the presence of serrated cutting edges of both upper and lower teeth as well as their large size. The teeth, that measure up to 1 cm, are the largest fossil Centrophorus reported in literature. The subtle differences between the teeth of different Centrophorus species and the paucity of comparative extant material prohibit specific attribution, but the teeth pertain to individuals that equalled the largest extant species. The occurrence of these large Centrophorus in the Belgian deposits is remarkable as Centrophorus usually prefers deeper waters.	[Wijnker, Erik] Wageningen Univ, Genet Lab, NL-6700 AH Wageningen, Netherlands	Wageningen University & Research	De Schutter, PJ (通讯作者)，Averbeekstr 23-1-02, B-1745 Opwijk, Belgium.	somniosus@skynet.be; Erik.Wijnker@wur.nl	Wijnker, Erik/H-4816-2011	De Schutter, Pieter/0000-0002-0477-7824				Adnet S, 2001, LETHAIA, V34, P234; Adnet S., 2006, PALAEO ICHTHYOLOGICA, V10; Adnet S, 2008, CRETACEOUS RES, V29, P711, DOI 10.1016/j.cretres.2008.01.014; [Anonymous], 1818, Journal of the Academy of Natural Sciences of Philadelphia, V1, P359; [Anonymous], 1984, FAO FISHERIES SYNOPS; [Anonymous], 1913, MEMOIRS MUSEUM COMP; Barthelt D., 1991, Muenchner Geowissenschaftliche Abhandlungen Reihe A Geologie und Palaeontologie, V19, P195; Bass A. J., 1976, 45 OC RES I; Bigelow H. 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Belg.		2012	15	1-2					26	35						10	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	941JF					2025-03-11	WOS:000303958800004
J	Lang, I; Kaczmarska, I				Lang, Imke; Kaczmarska, Irena			Morphological and molecular identity of diatom cells retrieved from ship ballast tanks destined for Vancouver, Canada	NOVA HEDWIGIA			English	Article						diatoms; trans-Pacific ship ballast; Pseudo-nitzschia pungens cf. var. aveirensis; hybrid; anoxia; non-native biota	COSCINODISCUS-WAILESII; DINOFLAGELLATE CYSTS; PCR; PHYTOPLANKTON; MARINE; WATER; BACILLARIOPHYTA; DIVERSITY; BAY; INTRODUCTIONS	Nine diatom phylotypes were recovered from trans-Pacific crossing ship ballast water tanks (25 day duration Trans-Pacific Voyage 2) and from associated ports (ballast water source in Osaka, Japan and destination in Vancouver, Canada). Diatoms were characterised morphologically (SEM) and genetically (ITS and rbeL DNA fragments) using one intact cell or a clonal chain of cells as a DNA source. Concurrently we monitored the tank physico-chemical environment (temperature, chl a, oxygen, and mineral nutrient concentrations) daily to provide an environmental context for the diatoms that persisted throughout the crossing. Most diatoms perished in ballast tank waters (probably from hypoxia, darkness and pathogens) but a few persisted several days into the voyage and could have been a part of de-ballasted water inocula in the destination port of Vancouver had the voyage been shorter and ballast tank environment more hospitable. New diatoms were taken up onboard with oceanic water during mid-ocean ballast water exchange (including species tolerant of coastal environments, such as Chaetoceros peruvianus) and some of these also persisted for several clays. Taxa recovered from ballast tanks include diatoms considered non-native to other coastal Canadian waters (e.g.. Atlantic coast, such as Coscinodiscus wailesii, Odontella sinensis and Thalassiosira punctigera) and potentially toxigenic species (Pseudo-nitzschia pungens var. aveirensis). Our results illustrate limitations of the benefits of using mid-ocean exchange as a sole means of ballast water management.	[Lang, Imke; Kaczmarska, Irena] Mt Allison Univ, Dept Biol, Sackville, NB E4L 1G7, Canada	Mount Allison University	Lang, I (通讯作者)，Cyano Biofuels GmbH, Magnusstr 11, D-12489 Berlin, Germany.	imke.lang@cyano-biofuels.com		Lang, Imke/0000-0002-5402-461X	Natural Science and Engineering Research Council of Canada (NSERC)	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We thank the sampling team of the Canadian Aquatic Invasive Species Research Network (CAISN) for sample collection on the cargo ship crossing the North Pacific Ocean and in Vancouver Harbour, J. L. Martin in the Bay of Fundy and K. Pauley in Bedford Basin. We thank M. B. J. Moniz, M. L. MacGillivary and M. Kinney for unpublished ITS and rbcL sequences and C. Leger for clone CL-270. J. M. Ehrman provided expert assistance with SEM, figure preparation and help with other electronic media. We also thank the shipping company for making the sampling on their vessel possible. We acknowledge funding from the Natural Science and Engineering Research Council of Canada (NSERC) for CAISN.	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J	Bringué, M; Rochon, A				Bringue, Manuel; Rochon, Andre			Late Holocene paleoceanography and climate variability over the Mackenzie Slope (Beaufort Sea, Canadian Arctic)	MARINE GEOLOGY			English	Article						Arctic; palynology; dinoflagellate cysts; Mackenzie Slope; climate variability	GREAT SALINITY ANOMALIES; NORTHERN NORTH-ATLANTIC; DINOFLAGELLATE CYSTS; SURFACE CONDITIONS; ORGANIC-CARBON; BARENTS SEA; HYDROGRAPHIC CONDITIONS; MARINE-SEDIMENTS; VICTORIA ISLAND; LATE QUATERNARY	Late Holocene paleoceanography and climate variability of the Southeastern Beaufort Sea (Canadian Arctic) have been investigated on the basis of sedimentary cores collected over the Mackenzie Slope. Piston, trigger and box cores were sampled at station 803 in 2004 aboard the CCGS Amundsen at 218 m water depth. The chronology of the piston core is constrained by 4 AMS-C-14 dates, as the sedimentation rate in the box core is assessed from Pb-210 data. We obtain a continuous composite sequence covering the last 4600 years, with a sedimentation rate of similar to 140 cm.kyr(-1). Transfer functions (modern analogue technique) based on dinoflagellate cyst (dinocyst) assemblages were used to reconstruct the evolution of sea-surface conditions over the time period covered by the cores. Palynological data reveal that dinocyst assemblages are dominated by Operculodinium centrocarpum sensu lato (mean of 43.3%) throughout the core, with the accompanying taxa Brigantedinium spp. (19.6%), Islandinium minutum (15.6%) and cysts of Pentapharsodinium dalei (13.7%). Four zones have been established on the basis of dinocyst relative abundances. Dinocyst assemblage zone 1 (D1), from 4600 to 2700 cal years BP, is dominated by O. centrocarpum (mean of 49.0%). In zone D2 (2700-1500 cal years BP), the relative abundances of 0. centrocarpum decrease (34.4%) in favour of the opportunistic, heterotrophic taxa Brigantedinium spp. (28.8%) and cysts of Polykrikos sp. var. arctic/quadratus (2.8%). Dinocyst zone D3 (1500-30 cal years BP or 450-1920 AD) is characterised by the high relative abundance of the peridinioid taxa I. minutum (19.9%). The last zone (D4), spanning from 1920 to 2004 AD, is again dominated by 0. centrocarpum (44.5%), and shows low relative abundances of Brigantedinium spp. and cf. Echinidinium karaense. Quantitative reconstructions of past sea-surface parameters (August sea-surface temperature: SST. August sea-surface salinity: SSS, and duration of sea-ice cover) indicate relatively stable conditions over the last 4.6 kyr, with episodic cooling events (SST of similar to 1.5 degrees C below the modem value of 6 degrees C) that took place between 700 and 1820 AD. We associate the last and the longest of these cooling events (1560-1820 AD) with the Little Ice Age. Reconstructed SSS shows decadal oscillations since 1920 AD that we tentatively associate with the accumulation of freshwater by the Beaufort Gyre and the subsequent Great Salinity Anomalies. Our data suggest that similar salinity anomalies could have occurred ca. 1860 and 1790 AD. Stable isotopic data show a slight increase in delta C-13 values (from similar to-27.1% at the base to similar to-25.8%,, at the top) over the last 4.6 kyr that we associate with the gradual increase in atmospheric CO2 concentration as recorded by Antarctic ice cores. Variations in the delta N-15 profile suggest variations in Pacific water influence from 4600 to similar to 1300 cal years BP, associated with centennial scale shifts of the Arctic Oscillation phases. (C) 2011 Elsevier B.V. All rights reserved.	[Bringue, Manuel; Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada	University of Quebec	Bringué, M (通讯作者)，Univ Victoria, SEOS, Bob Wright Ctr A405, POB 3065 STN CSC, Victoria, BC V8W 3V6, Canada.	mbringue@uvic.ca; andre_rochon@uqar.qc.ca	Bringue, Manuel/KIH-8224-2024	Bringue, Manuel/0000-0003-4460-8344	Natural Sciences and Engineering Research Council of Canada (NSERC); International Polar Year project; Canadian Foundation for Innovation; NSERC PGS-M	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); International Polar Year project; Canadian Foundation for Innovation(Canada Foundation for Innovation); NSERC PGS-M(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work is a contribution to the Canadian Arctic Shelf Exchange Study program (CASES) and was funded by the Natural Sciences and Engineering Research Council of Canada (NSERC), the International Polar Year project, Natural climate variability and forcings in Canadian Arctic and Arctic Ocean - NSERC Special Research Opportunity - International Polar Year and the Canadian Foundation for Innovation. Manuel Bringue was funded through a NSERC PGS-M scholarship. We are grateful to the officers and crew of the CCGS Amundsen who helped during the collection and analyses of the cores, in addition to David B. Scott and Trecia Schell, Dalhousie University; Kate Jarrett and Robbie Bennett, Bedford Institute of Oceanography; Jean-Francois Helie and Bassam Ghaleb, GEOTOP, UQAM; Claude Belzile, Ursule Boyer-Villemaire and Hubert Gagne, Institut des sciences de la mer de Rimouski, UQAR. Many thanks to Jacques Labrie, Francesco Barletta, David Ledu and Gwenaelle Chaillou (ISMER-UQAR) and Michael Whiticar (SEOS, University of Victoria) for their technical support and advice. Finally, we wish to express our gratitude to Guillaume St-Onge (ISMER-UQAR), Fabienne Marret (University of Liverpool) and two anonymous reviewers who helped in improving the manuscript.	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Geol.	JAN 1	2012	291						83	96		10.1016/j.margeo.2011.11.004	http://dx.doi.org/10.1016/j.margeo.2011.11.004			14	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	910GQ					2025-03-11	WOS:000301625600008
C	Linda, D; Louati, A; Chtara, C; Kabadou, A			IOP	Linda, D.; Louati, A.; Chtara, C.; Kabadou, A.			Oxidations of organic matter present in the phosphoric acid 54% by the ozone: characterization of groups carbonyls upstream and downstream of the ozonation	MATERIAUX 2010	IOP Conference Series-Materials Science and Engineering		English	Proceedings Paper	National Conference on MATERIAUX	NOV 04-07, 2010	Mahdia, TUNISIA	Tunisian Mat Res Soc-Tu-MRS				This study was focused on the oxidation of organic matter in phosphoric acid 54% by ozone. In order to understand the mechanisms involved in this process, the identification of this matter upstream and downstream of the ozonation was necessary. For the identification, after an extraction by a mixture (dichloro-methanol), the organic phase was divided into two parts: the residue and the extract:-The residue was studied by infrared spectroscopy Fourier Transform (IR-TF). It contains Kerogene which is a mixture of saturated hydrocarbons with high molecular weights. The absorption bands of the FT-IR showed that the residue contains also quantities of amino that correspond to the remains of dinoflagellate cysts, which are abundant in sediments.-The extract has been the subject of a detailed study by, chromatography on silica column, IR-TF spectroscopy and CG-SM. The passage of this extract on a silica column yielded two fractions (saturated fraction and polar fraction). Both of these fractions were analyzed by CG-SM. The yield of the reduction of the organic matter content in the phosphoric acid 54% could not exceed 29%. Therefore, we can conclude that the reduction in the rate of organic matter remains limited by the fact that some compounds are inert towards ozone.	[Linda, D.; Kabadou, A.] Univ Sfax, Lab Sci Mat & Environm, Fac Sci, Sfax 3038, Tunisia; [Louati, A.] Univ Sfax, Lab 3E, Sfax, Tunisia; [Chtara, C.] Grp Chim Tunisien, Lab Rech & Dev, Gabes, Tunisia	Universite de Sfax; Faculty of Sciences Sfax; Ecole Nationale dIngenieurs de Sfax (ENIS); Universite de Sfax; Faculty of Sciences Sfax	Linda, D (通讯作者)，Univ Sfax, Lab Sci Mat & Environm, Fac Sci, Sfax 3038, Tunisia.	ahlemkabadou@yahoo.fr						Ahmed H, 2007, SEP PURIF TECHNOL, V55, P212, DOI 10.1016/j.seppur.2006.12.014; [Anonymous], 2000, UZDATNIANIE WODY PRO; Baban A, 2003, DYES PIGMENTS, V58, P93, DOI 10.1016/S0143-7208(03)00047-0; Beltrán FJ, 2002, APPL CATAL B-ENVIRON, V39, P221, DOI 10.1016/S0926-3373(02)00102-9; Beltrán FJ, 1999, WATER RES, V33, P723, DOI 10.1016/S0043-1354(98)00239-5; Blinova O, 2007, J ALLOY COMPD, V444, P486, DOI 10.1016/j.jallcom.2007.02.117; Deng ZH, 2009, J ALLOY COMPD, V484, P619, DOI 10.1016/j.jallcom.2009.05.001; Dunn K., 1985, PHOSPHORUS POTASSIUM, V139, P34; Hsu YC, 2001, AICHE J, V47, P169, DOI 10.1002/aic.690470116; Huang C. P., 1993, Waste Management, V13, P361, DOI 10.1016/0956-053X(93)90070-D; J Bizot, 1967, B SOC CHIM FR, V1, P151; Jochimsen JC, 1997, WATER SCI TECHNOL, V35, P337, DOI 10.1016/S0273-1223(97)00043-7; Kazuo N, 1997, INFRARED RAMAN SPE B, V59; Kotz J.C., 1991, USES PHOSPHATE CONTA; Kowal A., 1997, OCZYSZCZANIE WODY; Skoromvarov J.I, 1988, J RADIOANAL NUCL CH, V229, P455	16	0	0	0	4	IOP PUBLISHING LTD	BRISTOL	DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND	1757-8981			IOP CONF SER-MAT SCI			2012	28								012045	10.1088/1757-899X/28/1/012045	http://dx.doi.org/10.1088/1757-899X/28/1/012045			10	Materials Science, Multidisciplinary; Physics, Condensed Matter	Conference Proceedings Citation Index - Science (CPCI-S)	Materials Science; Physics	BZD65					2025-03-11	WOS:000301182700045
J	Zonneveld, KAF; Chen, L; Elshanawany, R; Fischer, HW; Hoins, M; Ibrahim, MI; Pittauerova, D; Versteegh, GJM				Zonneveld, Karin A. F.; Chen, Liang; Elshanawany, Rehab; Fischer, Helmut W.; Hoins, Mirja; Ibrahim, Mohammed I.; Pittauerova, Daniela; Versteegh, Gerard J. M.			The use of dinoflagellate cysts to separate human-induced from natural variability in the trophic state of the Po River discharge plume over the last two centuries	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Eutrophication; High temporal resolution; Po River; Mediterranean Sea	WESTERN ADRIATIC SEA; ENVIRONMENTAL-FACTORS; TOKYO-BAY; INCREASED EUTROPHICATION; LINGULODINIUM-POLYEDRUM; SPATIAL-DISTRIBUTION; SURFACE SEDIMENTS; COASTAL WATERS; ORGANIC-MATTER; YOKOHAMA-PORT	To obtain insight into the natural and/or human-induced changes in the trophic state of the distal portion of the Po River discharge plume over the last two centuries, high temporal resolution dinoflagellate cyst records were established at three sites. Cyst production rates appear to reflect the natural variability in the river's discharge, whereas cyst associations reflect the trophic state of the upper waters, which in turn can be related to agricultural development. The increased abundances of Lingulodinium machaerophorum and Stelladinium stellatum found as early as 1890 and 1920 correspond to the beginning of the industrial revolution in Italy and the first chemical production and dispersion of ammonia throughout Europe. After 1955, the increased abundances of these species and of Polykrikos schwartzii, Brigantedinium spp. and Pentapharsodinium dalei correspond to agriculturally induced alterations of the hypertrophic conditions. A slight improvement in water quality can be observed from 1987 onward. (C) 2011 Elsevier Ltd. All rights reserved.	[Zonneveld, Karin A. F.; Chen, Liang; Elshanawany, Rehab; Hoins, Mirja; Versteegh, Gerard J. M.] Univ Bremen, MARUM Fachbereich Geowissensch 5, D-28334 Bremen, Germany; [Fischer, Helmut W.; Pittauerova, Daniela] Univ Bremen, Inst Environm Phys, D-28359 Bremen, Germany; [Elshanawany, Rehab; Ibrahim, Mohammed I.] Univ Alexandria, Fac Sci, Alexandria, Egypt	University of Bremen; University of Bremen; Egyptian Knowledge Bank (EKB); Alexandria University	Zonneveld, KAF (通讯作者)，Univ Bremen, MARUM Fachbereich Geowissensch 5, Leobener Str, D-28334 Bremen, Germany.	zonnev@uni-bremen.de	Ibrahim, Mohammed/IUQ-7100-2023; Fischer, Helmut/K-6207-2012; Ransby, Daniela/G-8854-2014; Versteegh, Gerard J.M./H-2119-2011	Fischer, Helmut/0000-0002-0593-5564; Ransby, Daniela/0000-0002-3643-333X; Ibrahim, Mohamed Ismail Abdou/0000-0002-5782-0435; Versteegh, Gerard J.M./0000-0002-9320-3776	Deutscher Akademischer Austausch Dienst (DAAD); DFG; MARUM Research Centrum	Deutscher Akademischer Austausch Dienst (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD)); DFG(German Research Foundation (DFG)); MARUM Research Centrum	We thank the Deutscher Akademischer Austausch Dienst (DAAD), the DFG-funded International Graduate College EURO-PROX and the MARUM Research Centrum for providing the scholarships that allowed Rehab Elshanawany to perform a portion of this research at Bremen University, Germany. The DFG is also acknowledged for funding the position of Liang Chen as part of the NSF/EuroMarc MOCCHA project.	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J	Barski, M				Barski, Marcin			Dinoflagellate cysts from neptunian dykes in the Middle Jurassic of Poland - A stratigraphical approach	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						neptunian dykes; dinoflagellate cysts; Middle-Upper Jurassic	SEA; SUCCESSION; DINOCYSTS; DEPOSITS; FAUNA; AGE	Dinoflagellate cysts are of use in determining the age of allochthonous sediments within host rocks. Due to the high durability of the cyst walls they are able to persist in difficult environmental and synsedimentary conditions. This case study focuses on palynological analysis of neptunian dykes cutting through Middle Jurassic clays with siderite concretions exposed in three sites in Central Poland. Within the fissures, intense mixing of palynodebris from the host rock with the infilling sediments took place. Palynological analysis of the internal sediments from the fissure infillings revealed well-preserved mixed assemblages of Middle and Late Jurassic taxa enabling the age of the process to be constrained. The analysis of the infillings of neptunian dykes is of particular importance as sometimes this provides the only proof of eroded sediments, and the fissure systems are usually evidence of regional extensional tectonic activities. (C) 2011 Elsevier B.V. All rights reserved.	Univ Warsaw, Fac Geol, Inst Geol, PL-02089 Warsaw, Poland	Polish Geological Institute - National Research Institute; University of Warsaw	Barski, M (通讯作者)，Univ Warsaw, Fac Geol, Inst Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	marbar@uw.edu.pl		Barski, Marcin/0000-0002-4102-3538				Aubrecht Roman, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V196, P1; Barski Marcin, 2004, Tomy Jurajskie, V2, P61; Barski M, 2010, GEOL CARPATH, V61, P121, DOI 10.2478/v10096-010-0005-4; Basilone L, 2010, SEDIMENT GEOL, V226, P54, DOI 10.1016/j.sedgeo.2010.02.009; Bertok C, 2009, SEDIMENTOLOGY, V56, P1016, DOI 10.1111/j.1365-3091.2008.01015.x; CASTELLARIN A, 1982, GUIDA GEOLOGIA SUDAL, P23; Deflandre G., 1938, STATION ZOOLOGIQUE W, V13, P147; Edwards LE, 2003, PALAIOS, V18, P275, DOI 10.1669/0883-1351(2003)018<0275:IDTDFT>2.0.CO;2; FAUCONNIER D, 1997, BULL CENT RECH ELF E, V17, P225; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Flugel E., 2004, MICROFACIES CARBONAT, DOI [10.1007/978-3-662-08726-8, DOI 10.1007/978-3-662-08726-8]; Gohn GS, 2009, GEOL SOC AM SPEC PAP, V458, P587, DOI 10.1130/2009.2458(26); Iijima Y., 2004, J. Geol. Soc. Japan, V110, P497; Jaramillo CA, 1999, PALAEOGEOGR PALAEOCL, V145, P259, DOI 10.1016/S0031-0182(98)00126-6; JENKYNS HC, 1991, J GEOL SOC LONDON, V148, P245, DOI 10.1144/gsjgs.148.2.0245; MAO S, 1995, REV PALAEOBOT PALYNO, V86, P235, DOI 10.1016/0034-6667(94)00138-A; Matyja B.A., 2006, FIELD TRIP GUIDEBOOK, P154; Matyja B.A., 1991, 3 INT S JUR STRAT PO, P81; Matyja B.A., 2003, TOMY JURAJSKIE, V1, P3; Matyja BA, 1996, GEORES FORUM, V1&2, P333; MATYJA BA, 2003, TOMY JURAJSKIE, V1, P53; Matyja Bronislaw Andrzej, 2000, Acta Geologica Polonica, V50, P191; Matyja BA, 2009, GEOL Q, V53, P49; POULSEN N.E., 1990, DANMARKS GEOLOGISK C, V10, P1; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; Poulsen Niels E., 1998, Acta Geologica Polonica, V48, P237; Poulsen Niels E., 1991, Palynology, V15, P211; 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 James B., 2002, Palynology, V26, P5, DOI 10.2113/0260005; Sano H, 2004, FACIES, V50, P133, DOI 10.1007/s10347-004-0002-0; Sarjeant W.A.S., 1982, American Association of Stratigraphic Palynologists Contributions Series, V9, P1; SZULCZEWSKI M, 1973, Acta Geologica Polonica, V23, P15; Torricelli Stefano, 2001, Palynology, V25, P29, DOI 10.2113/0250029; Traverse A., 1992, GEOPHYTOLOGY, V22, P65; Traverse A., 2007, Paleopalynology, VSecond; Velledits F, 2003, FACIES, V48, P23, DOI 10.1007/BF02667528; Wall GRT, 2004, GEOL MAG, V141, P471, DOI 10.1017/S0016756804009185; Whiteside DI, 2008, GEOL MAG, V145, P105, DOI 10.1017/S0016756807003925; WINTERER EL, 1994, SEDIMENTOLOGY, V41, P1109, DOI 10.1111/j.1365-3091.1994.tb01444.x	41	13	16	0	3	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	JAN 1	2012	169						38	47		10.1016/j.revpalbo.2011.10.009	http://dx.doi.org/10.1016/j.revpalbo.2011.10.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	889KN					2025-03-11	WOS:000300072700005
J	Ghasemi-Nejad, E; Sabbaghiyan, H; Mosaddegh, H				Ghasemi-Nejad, Ebrahim; Sabbaghiyan, Hossein; Mosaddegh, Hossein			Palaeobiogeographic implications of Late Bajocian-Late Callovian (Middle Jurassic) dinoflagellate cysts from the Central Alborz Mountains, northern Iran	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						Middle Jurassic; Dinoflagellate cysts; Palaeobiogeography; Biocorrelation; Northern Iran; Northwest Europe	EURASIA; MARGIN; BLOCK; EAST	The Dalichai Formation with an age of Late Bajocian-Late Callovian was sampled in Central Alborz Mountains of northern Iran and studied for palynological, palaeobiogeographical and palynocorrelation purposes. Palynological studies revealed diverse and well-preserved dinoflagellate cyst assemblages and lead to identification of three zones i.e., Cribroperidinium crispum (Late Bajocian), Dichadogonyoulax sellwoodii (Bathonian to Early Callovian) and Ctenidodinium continuum (Early to Middle Callovian) Zones. Subzone a of the D. sellwoodii Zone (Early to Middle Bathonian) was also differentiated. This biozonation corresponds to those recognised in Northwest Europe. Furthermore, the ammonoid families recorded including Phylloceratidae, Oppeliidae, Reineckeiidae, Perisphinctidae, Haploceratidae, Parkinsoniidae and Sphaeroceratidae, which confirm the Late Bajocian to Late Callovian age, are quite similar to those of Northwest Europe and the northwestern Tethys. The close similarities of the dinoflagellate cyst assemblages and ammonite fauna of northern Iran with those of Northwest Europe and the northwestern Tethys during the Middle Jurassic indicate direct but episodic marine connection and faunal exchange between the two areas. (C) 2011 Elsevier Ltd. All rights reserved.	[Ghasemi-Nejad, Ebrahim; Sabbaghiyan, Hossein] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran; [Mosaddegh, Hossein] Dameghan Univ Basic Sci, Dept Geol, Dameghan, Iran	University of Tehran	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran.	eghasemi@khayam.ut.ac.ir	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068	University of Tehran	University of Tehran(University of Tehran)	The authors are greatly indebted to Dr. K. Seyed-Emami of the College of Engineering of the University of Tehran, who identified the ammonites recorded, reviewed the first draft of this paper and made comments that improved the quality of the article. Dr. N. Poulsen of the Geological Survey of Denmark and Greenland is especially thanked for his review and many useful comments on the manuscript and Dr. F. T. Fursich of the Universitat Erlangen-Nurnberg, Germany and an anonymous reviewer are thanked for reviewing the manuscript and for their useful comments that improved the quality of the paper. This project was funded by the Vice Chancellor for Research of the University of Tehran.	Alavi M, 1997, GEOL SOC AM BULL, V109, P1563, DOI 10.1130/0016-7606(1997)109<1563:TTAARO>2.3.CO;2; [Anonymous], GEOLOGICAL SOC LONDO; Davies E.H., 1983, Arctic Canada. Geol. Surv. Can. Bull., V359, P59; Dercourt J., 1993, ATLAS TETHYS PALEOEN; Dercourt J., 2000, Atlas Peri-Tethys. Palaeogeographical maps, P268; ENAY R, 1993, ATLAS TETHYS PALAEOE, P1; Fürsich FT, 2009, GEOL SOC SPEC PUBL, V312, P189, DOI 10.1144/SP312.9; Golonka J, 2004, TECTONOPHYSICS, V381, P235, DOI 10.1016/j.tecto.2002.06.004; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hedberg H.D., 1976, International stratigraphic guide: a guide to stratigraphic classification, terminology, and procedure; Lentin J. 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J	Durantou, L; Rochon, A; Ledu, D; Massé, G; Schmidt, S; Babin, M				Durantou, L.; Rochon, A.; Ledu, D.; Masse, G.; Schmidt, S.; Babin, M.			Quantitative reconstruction of sea-surface conditions over the last ∼ 150 yr in the Beaufort Sea based on dinoflagellate cyst assemblages: the role of large-scale atmospheric circulation patterns	BIOGEOSCIENCES			English	Article							RECENT MARINE-SEDIMENTS; ARCTIC-OCEAN; NORTH-ATLANTIC; FRESH-WATER; MACKENZIE DELTA; HYDROGRAPHIC CONDITIONS; POLLEN DISTRIBUTION; LATE QUATERNARY; CANADIAN SHELF; CLIMATE-CHANGE	Dinoflagellate cyst (dinocyst) assemblages have been widely used over the Arctic Ocean to reconstruct sea-surface parameters on a quantitative basis. Such reconstructions provide insights into the role of anthropogenic vs natural forcings in the actual climatic trend. Here, we present the palynological analysis of a dated 36 cm-long core collected from the Mackenzie Trough in the Canadian Beaufort Sea. Dinocyst assemblages were used to quantitatively reconstruct the evolution of sea-surface conditions (temperature, salinity, sea ice) and freshwater palynomorphs fluxes were used as local paleo-river discharge indicators over the last similar to 150 yr. Dinocyst assemblages are dominated by autotrophic taxa (68 to 96 %). Cyst of Pentapharsodinium dalei is the dominant species throughout most of the core, except at the top where the assemblages are dominated by Operculodinium centrocarpum. Quantitative reconstructions of sea-surface parameters display a series of relatively warm, lower sea ice and saline episodes in surface waters, alternately with relatively cool and low salinity episodes. Variations of dinocyst fluxes and reconstructed sea-surface conditions may be closely linked to large scale atmospheric circulation patterns such as the Pacific Decadal Oscillation (PDO) and to a lesser degree, the Arctic Oscillation (AO). Positive phases of the PDO correspond to increases of dinocyst fluxes, warmer and saltier surface waters, which we associate with upwelling events of warm and relatively saline water from Pacific origin. Freshwater palynomorph fluxes increased in three phases from AD 1857 until reaching maximum values in AD 1991, suggesting that the Mackenzie River discharge followed the same trend when its discharge peaked between AD 1989 and AD 1992. The PDO mode seems to dominate the climatic variations at multi-annual to decadal timescales in the western Canadian Arctic and Beaufort Sea areas.	[Durantou, L.; Rochon, A.] Univ Quebec, Inst Sci Mer ISMER, Rimouski, PQ G5L 3A1, Canada; [Ledu, D.; Masse, G.] LOCEAN Inst Pierre Simon Laplace, UMR7159, F-75252 Paris, France; [Schmidt, S.] Univ Bordeaux, EPOC, UMR5805, F-33400 Talence, France; [Babin, M.] Univ Laval, Takuvik Joint Lab, Quebec City, PQ, Canada	University of Quebec; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Laval University	Durantou, L (通讯作者)，Univ Quebec, Inst Sci Mer ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	lise.durantou@uqar.qc.ca	Ledu, David/X-4166-2019; Schmidt, Sabine/G-1193-2013	Babin, Marcel/0000-0001-9233-2253; Ledu, David/0000-0001-5313-7068; Schmidt, Sabine/0000-0002-5985-9747	Natural Science and Engineering Research Council of Canada (NSERC); Institut des sciences de la mer (ISMER); ERC [203441]; European Research Council (ERC) [203441] Funding Source: European Research Council (ERC)	Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Institut des sciences de la mer (ISMER); ERC(European Research Council (ERC)); European Research Council (ERC)(European Research Council (ERC))	This work was funded by the Natural Science and Engineering Research Council of Canada (NSERC) through a Discovery Grant to Andre Rochon, by the Institut des sciences de la mer (ISMER) and both the MALINA and ICEPROXY (ERC Stg 203441) projects. We wish to thank the officers and crew of the CCGS Amundsen for their help during the sampling campaign. We also thank the following people from ISMER: Etienne Faubert, Thomas Richerol, Guillaume Saint-Onge, Marc-Andre Cormier and Jacques Labrie; Yves Gratton and Pascal Guillot (Quebec Ocean) and from GEOTOP: Anne de Vernal, Taoufik Radi, Sophie Bonnet, Maryse Henry, Hans Asnong, Michele Garneau for their help and assistance throughout the duration of this work. This is a contribution to the Malina Program.	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J	Ribeiro, S; Moros, M; Ellegaard, M; Kuijpers, A				Ribeiro, Sofia; Moros, Matthias; Ellegaard, Marianne; Kuijpers, Antoon			Climate variability in West Greenland during the past 1500 years: evidence from a high-resolution marine palynological record from Disko Bay	BOREAS			English	Article							WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; HOLOCENE NORTH-ATLANTIC; ENVIRONMENTAL-CHANGE; SOUTH GREENLAND; IGALIKU-FJORD; OCEAN CIRCULATION; MID-HOLOCENE; SEDIMENTS; BUGT	Here we document late-Holocene climate variability in West Greenland as inferred from a marine sediment record from the outer Disko Bay. Organic-walled dinoflagellate cysts and other palynomorphs were used to reconstruct environmental changes in the area through the last c. 1500 years at 30-40 years resolution. Sea ice cover and primary productivity were identified as the two main factors driving dinoflagellate cyst community changes through time. Our data provide evidence for an opposite climate trend in West Greenland relative to the NE Atlantic region from c. AD 500 to 1050. For the same period, sea-surface temperatures in Disko Bay are out-of-phase with Greenland ice-core reconstructed temperatures and marine proxy data from South and East Greenland. This is probably governed by an NAO-type pattern, which results in warmer sea-surface conditions with less extensive sea ice in the area for the later part of the Dark Ages cold period (c. AD 500 to 750) and cooler conditions with extensive sea ice inferred for the first part of the Medieval Climate Anomaly (MCA) (c. AD 750 to 1050). After c. AD 1050, the marine climate in Disko Bay becomes in-phase with trends described for the NE Atlantic, reflected in the warmer interval for the remainder of the MCA (c. AD 1050-1250), followed by cooling towards the onset of the Little Ice Age at c. AD 1400. The inferred scenario of climate deterioration and extensive sea ice is concomitant with the collapse of the Norse Western Settlement in Greenland at c. AD 1350.	[Ribeiro, Sofia; Ellegaard, Marianne] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-1353 Copenhagen K, Denmark; [Moros, Matthias] Bjerknes Ctr Climate Res, N-5007 Bergen, Norway; [Moros, Matthias] Leibniz Inst Balt Sea Res, D-18119 Rostock, Germany; [Kuijpers, Antoon] Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark	University of Copenhagen; Bjerknes Centre for Climate Research; Leibniz Institut fur Ostseeforschung Warnemunde; Geological Survey Of Denmark & Greenland	Ribeiro, S (通讯作者)，Univ Copenhagen, Dept Biol, Marine Biol Sect, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	sribeiro@bio.ku.dk; matthias.moros@io-warnemuende.de; me@bio.ku.dk; aku@geus.dk	Ribeiro, Sofia/AAZ-2782-2021; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018	Ribeiro, Sofia/0000-0003-0672-9161	German DFG [MO 1422/2-1]; 'NEWGREEN' project; 'NORCLIM' initiative [120]; TROPOLINK (The Danish Council for Independent Research, Nature and Universe) [09-069833/FNU]; Portuguese Foundation for Science and Technology [SFRH/BD/30847/2006]; German Research Council; Fundação para a Ciência e a Tecnologia [SFRH/BD/30847/2006] Funding Source: FCT	German DFG(German Research Foundation (DFG)); 'NEWGREEN' project; 'NORCLIM' initiative; TROPOLINK (The Danish Council for Independent Research, Nature and Universe); Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); German Research Council(German Research Foundation (DFG)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	This study was funded by the German DFG MO 1422/2-1, the 'NEWGREEN' project, which was a Danish contribution to the International Polar Year (no. 120) 'NORCLIM' initiative, and TROPOLINK (The Danish Council for Independent Research, Nature and Universe Grant no. 09-069833/FNU). Sofia Ribeiro was supported by a Ph.D. scholarship from the Portuguese Foundation for Science and Technology (SFRH/BD/30847/2006). Core 343310 was collected during a cruise funded by the German Research Council. We thank the captain and crew of RV 'Maria S. Merian' for their assistance during core acquisition. Gavin Simpson, Steve Juggins and Nicolas van Nieuwenhove are thanked for their suggestions during preliminary data analyses, and Bo Vinther for clarifications regarding the Greenland ice-core temperature reconstructions. Kerstin Perner kindly prepared the map figure. We would like to thank Marit-Solveig Seidenkrantz for commenting on the manuscript. We also thank Jens Matthiessen and John T. Andrews for their helpful and thorough reviews.	Andersen O. G. N., 1981, MEDDELELSER GRONLAND, V5; Andersen O. G. 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J	Zumaque, J; Eynaud, F; Zaragosi, S; Marret, F; Matsuzaki, KM; Kissel, C; Roche, DM; Malaizé, B; Michel, E; Billy, I; Richter, T; Palis, E				Zumaque, J.; Eynaud, F.; Zaragosi, S.; Marret, F.; Matsuzaki, K. M.; Kissel, C.; Roche, D. M.; Malaize, B.; Michel, E.; Billy, I.; Richter, T.; Palis, E.			An ocean-ice coupled response during the last glacial: a view from a marine isotopic stage 3 record south of the Faeroe Shetland Gateway	CLIMATE OF THE PAST			English	Article							NORTHERN NORTH-ATLANTIC; NORWEGIAN SEA OVERFLOW; ABRUPT CLIMATE-CHANGE; DINOFLAGELLATE CYSTS; HEINRICH LAYERS; THERMOHALINE CIRCULATION; SURFACE CONDITIONS; ROCKALL TROUGH; FLEUVE MANCHE; ARCTIC-OCEAN	The rapid climatic variability characterising the Marine Isotopic Stage (MIS) 3 (similar to 60-30 cal ka BP) provides key issues to understand the atmosphere-ocean-cryosphere dynamics. Here we investigate the response of sea-surface paleoenvironments to the MIS3 climatic variability through the study of a high resolution oceanic sedimentological archive (core MD99-2281, 60 degrees 21' N; 09 degrees 27' W; 1197m water depth), retrieved during the MD114-IMAGES (International Marine Global Change Study) cruise from the southern part of the Faeroe Bank. This sector was under the proximal influence of European ice sheets (Fennoscandian Ice Sheet to the East, British Irish Ice Sheet to the South) during the last glacial and thus probably responded to the MIS3 pulsed climatic changes. We conducted a multi-proxy analysis of core MD99-2281, including magnetic properties, x-ray fluorescence measurements, characterisation of the coarse (> 150 mu m) lithic fraction (grain concentration) and the analysis of selected biogenic proxies (assemblages and stable isotope ratio of calcareous planktonic foraminifera, dinoflagellate cyst - e.g. dinocyst - assemblages). Results presented here are focussed on the dinocyst response, this proxy providing the reconstruction of past sea-surface hydrological conditions, qualitatively as well as quantitatively (e. g. transfer function sensu lato). Our study documents a very coherent and sensitive oceanic response to the MIS3 rapid climatic variability: strong fluctuations, matching those of stadial/interstadial climatic oscillations as depicted by Greenland ice cores, are recorded in the MD99-2281 archive. Proxies of terrigeneous and detritical material suggest increases in continental advection during Greenland Stadials (including Heinrich events), the latter corresponding also to southward migrations of polar waters. At the opposite, milder sea-surface conditions seem to develop during Greenland Interstadials. After 30 ka, reconstructed paleohydrological conditions evidence strong shifts in SST: this increasing variability seems consistent with the hypothesised coalescence of the British and Fennoscandian ice sheets at that time, which could have directly influenced sea-surface environments in the vicinity of core MD99-2281.	[Zumaque, J.; Eynaud, F.; Zaragosi, S.; Matsuzaki, K. M.; Malaize, B.; Billy, I.; Palis, E.] Univ Bordeaux 1, EPOC Environm & Paleoenvironm Ocean, UMR5805, F-33405 Talence, France; [Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Kissel, C.; Roche, D. M.; Michel, E.] UVSQ, CNRS, CEA, LSCE,INSU,UMR8212, F-91191 Gif S S Yvette, France; [Roche, D. M.] Vrije Univ Amsterdam, NL-1081 HV Amsterdam, Netherlands; [Richter, T.] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Texel, Netherlands	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; University of Liverpool; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; CEA; Vrije Universiteit Amsterdam; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ)	Eynaud, F (通讯作者)，Univ Bordeaux 1, EPOC Environm & Paleoenvironm Ocean, UMR5805, F-33405 Talence, France.	f.eynaud@epoc.u-bordeaux1.fr	ZARAGOSI, Sébastien/JXL-2488-2024; Catherine, Kissel/AAH-1647-2019; Matsuzaki, Kenji/L-9468-2013; Roche, Didier M./C-9875-2010	Michel, Elisabeth/0000-0001-7810-8888; Matsuzaki, Kenji/0000-0001-8918-9249; Roche, Didier M./0000-0001-6272-9428	ARTEMIS 14C Accelerator Mass Spectrometry French project; French Atomic Energy Commission; CNRS; CNRS-INSU	ARTEMIS 14C Accelerator Mass Spectrometry French project; French Atomic Energy Commission(CEA); CNRS(Centre National de la Recherche Scientifique (CNRS)); CNRS-INSU(Centre National de la Recherche Scientifique (CNRS))	The authors are grateful to IPEV, the captain and the crew of the Marion-Dufresne and the scientific team of the GINNA cruise (Labeyrie et al., 1999). We wish to thank Y. Balut for his assistance at sea. J. St Paul, O. Ther, M.-H. Castera and M. Georget provided invaluable technical assistance. We acknowledge financial support by the ARTEMIS <SUP>14</SUP>C Accelerator Mass Spectrometry French project. Part of the analyses conducted on MD99-2281 was supported by the French INSU (Institut National des Sciences de l'Univers) program LEFE/EVE (Les enveloppes fluides et l'environnement/Evolution et variabilite du climat a l'echelle globale) "RISCC: Role des Ice-Shelves dans le Changement Climatique". The magnetic analyses at LSCE were made with the help of Camille Wandres from laboratory funds from the French Atomic Energy Commission and from the CNRS. This is an U.M.R./EPOC 5805 (Universite Bordeaux I - C.N.R.S.) contribution. The publication of this article is financed by CNRS-INSU.	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J	Bakrac, K; Koch, G; Sremac, J				Bakrac, Koraljka; Koch, Georg; Sremac, Jasenka			Middle and Late Miocene palynological biozonation of the south-western part of Central Paratethys (Croatia)	GEOLOGIA CROATICA			English	Article						palynology; Miocene; biozonation; dinoflagellate; Paratethys; Mediterranean	SEA-LEVEL CHANGES; DINOFLAGELLATE CYST; PANNONIAN BASIN; CENTRAL-EUROPE; LAKE PANNON; EVOLUTION; PALEOGEOGRAPHY; STRATIGRAPHY; SALINITY; NORTH	Middle and Late Miocene palynological biozonation of the south-western parts of Central Paratethys (Croatia) is presented based on organic-walled phytoplankton. Nine characteristic palynozones of regional palynostratigraphic range are recognized, e.g. Early Badenian (Langhian) Cribroperidinium tenuitabulatum (Cte), Badenian (Late Langhian - Earliest Serravallian) Unipontidinium aquaeductum (Uaq), Late Badenian (Early Serravallian) Cleistosphaeridium placacanthum (Cpl), Sarmatian (Middle and Late Serravallian) Polysphaeridium zoharyi - Lingulodinium machaerophorum (Pzo-Lma), early Early Pannonian s.l. Mecsekia ultima - Spiniferites bentorii pannonicus (Mul-Spa), middle Early Pannonian s.l. Spiniferites bentorii oblongus (Sob), late Early Pannonian s.l. Pontiadinium pecsvaradensis (Ppe), early Late Pannonian s.l. Spiniferites validus (Sva), and late Late Pannonian s.l. Galeacysta etrusca (Get). As inferred from the regional palynostratigraphic correlation, the signals of two transgressions after the isolation of Paratethys during the Sarmatian are recognised: the first one in the late Early Pannonian, when Mediterranean dinoflagellates migrated into the Pannonian Basin, and the second one in the Late Pannonian, when endemic Paratethyan taxa migrated into the Mediterranean.	[Bakrac, Koraljka; Koch, Georg] Croatian Geol Survey, HR-10000 Zagreb, Croatia; [Sremac, Jasenka] Univ Zagreb, Fac Sci, Dept Geol, HR-10000 Zagreb, Croatia	Croatian Geological Survey; University of Zagreb	Bakrac, K (通讯作者)，Croatian Geol Survey, Sachsova 2, HR-10000 Zagreb, Croatia.	kbakrac@hgi.cgs.hr	Sremac, Jasenka/J-9364-2014; Bakrac, Koraljka/G-1085-2012	Bakrac, Koraljka/0000-0002-2520-411X; Sremac, Jasenka/0000-0002-4736-7497	Croatian Geological Survey, Department of Geology; Ministry of Science, Education and Sports [181-1811096-1093, 119-1951293-1162]	Croatian Geological Survey, Department of Geology; Ministry of Science, Education and Sports(Ministry of Science, Education and Sports, Republic of Croatia)	The present investigation is part of the basic investigation supported by the Croatian Geological Survey, Department of Geology, and Ministry of Science, Education and Sports Projects no. 181-1811096-1093: "Basic Geological Map of the Republic of Croatia 1:50 000", and no. 119-1951293-1162: "Evidence of Biotic and Abiotic Changes in Palaeoenvironments".	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B	Ogg, JG; Hinnov, LA; Huang, C		Gradstein, FM; Ogg, JG; Schmitz, MD; Ogg, GM		Ogg, J. G.; Hinnov, L. A.; Huang, C.			Jurassic	GEOLOGIC TIME SCALE 2012, VOLS 1 & 2			English	Article; Book Chapter							CARBON-ISOTOPE STRATIGRAPHY; BOUNDARY STRATOTYPE SECTION; TRIASSIC MASS EXTINCTION; OCEANIC ANOXIC EVENT; ATLANTIC MAGMATIC PROVINCE; SEA-LEVEL CHANGES; CALCAREOUS NANNOFOSSIL BIOSTRATIGRAPHY; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; MARL-LIMESTONE ALTERNATIONS; ORBITALLY FORCED CLIMATE	Ammonites exploded in diversity after the end-Triassic near-extinction of their precursor taxa and have been the main tool for global correlation for nearly two centuries. The Pangea super-continent split during mid-Jurassic into Laurasia and Gondwana separated by a Tethys-Atlantic seaway. Late Jurassic organic-rich shales would later provide nearly half of our oil-gas source rocks. Dinosaurs dominated the land surface, and their cousins took to the air.	[Ogg, J. 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J	Barski, M; Matyja, BA; Segit, T; Wierzbowski, A				Barski, Marcin; Matyja, Bronislaw Andrzej; Segit, Tomasz; Wierzbowski, Andrzej			Early to Late Bajocian age of the "black flysch" (Szlachtowa Fm.) deposits: implications for the history and geological structure of the Pieniny Klippen Belt, Carpathians	GEOLOGICAL QUARTERLY			English	Article						Pieniny Klippen Belt; "black flysch"; stratigraphy; dinoflagellate cyst; palaeogeography; Magura Basin	DINOFLAGELLATE CYSTS; BIOSTRATIGRAPHY; GERMANY	The "black flysch" deposits (Szlachtowa Formation at Podubocze near Czorsztyn in Poland), attributed so far to the Pieniny Klippen Basin successions, and at Haluszowa in Poland as well as at Kamienka in Eastern Slovakia, attributed to the Grajcarek Succession of the Magura Basin, have yielded rich dinoflagellate cyst assemblages consisting of forms both redeposited (from Upper Triassic to Aalenian) and indigenous (Lower Bajocian to Upper Bajocian). An Early to Late Bajocian age of the deposits investigated is thus indicated, and this along with other stratigraphical, sedimentological and tectonic data indicates that all the deposits in question represent the early stages of development of the Magura Basin. The formation of "black flysch" deposits was possibly related to the Early Bajocian uplift of the Czorsztyn Ridge which resulted from the opening of the Magura Ocean. The occurrence of the deposits of the Magura Basin below the overthrusted deposits of the Klippen Basin (Czorsztyn Unit) in the area of study results in a marked change in the structural interpretation of the Pieniny Klippen Belt.	[Barski, Marcin; Matyja, Bronislaw Andrzej; Segit, Tomasz; Wierzbowski, Andrzej] Univ Warsaw, Inst Geol, PL-02089 Warsaw, Poland; [Wierzbowski, Andrzej] Polish Geol Inst, Natl Res Inst, PL-00975 Warsaw, Poland	Polish Geological Institute - National Research Institute; University of Warsaw; Polish Geological Institute - National Research Institute	Barski, M (通讯作者)，Univ Warsaw, Inst Geol, Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	marbar@uw.edu.pl; matyja@uw.edu.pl; t.segit@uw.edu.pl; andrzej.wierzbowski@uw.edu.pl		Segit, Tomasz/0000-0003-2952-6332; Barski, Marcin/0000-0002-4102-3538	Institute of Geology of the Faculty of Geology, University of Warsaw	Institute of Geology of the Faculty of Geology, University of Warsaw	The study has been supported by the Institute of Geology of the Faculty of Geology, University of Warsaw. The authors are grateful to the reviewers, N. Oszczypko, K. Pestchevitskaya and D. Plasienka, for their valuable comments. Admittance to protected areas of the Pieniny National Park is gratefully acknowledged.	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Q.		2012	56	3					391	410		10.7306/gq.1030	http://dx.doi.org/10.7306/gq.1030			20	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	012PY		Bronze			2025-03-11	WOS:000309250200001
J	Coats, DW; Bachvaroff, TR; Delwiche, CF				Coats, D. Wayne; Bachvaroff, Tsvetan R.; Delwiche, Charles F.			Revision of the Family Duboscquellidae with Description of Euduboscquella crenulata n. gen., n. sp (Dinoflagellata, Syndinea), an Intracellular Parasite of the Ciliate Favella panamensis Kofoid & Campbell, 1929	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Dinoflagellate; parasitism; sexuality; taxonomy; tintinnid	REPRODUCTION	Recent recognition that tintinnids are infected by dinophycean as well as syndinean parasites prompts taxonomic revision of dinoflagellate species that parasitize these ciliates. Long overlooked features of the type species Duboscquella tintinnicola are used to emend the genus and family Duboscquellidae, resulting in both taxa being moved from the Syndinea to the Dinophyceae. Syndinean species previously classified as Duboscquella are relocated to Euduboscquella n. gen., with Euduboscquella crenulata n. sp. as the type. As an endoparasitic species, E. crenulata shares with its congeners processes associated with intracellular development and sporogenesis, but differs from closely related species in nuclear and cortical morphology of the trophont, including a distinctively grooved shield (episome) that imparts a crenulated appearance in optical section. In addition, E. crenulata produces three morphologically distinct spore types, two of which undergo syngamy to form a uninucleate zygote. The zygote undergoes successive division to produce four daughter cells of unequal size, but that resemble the nonmating spore type.	[Coats, D. Wayne; Bachvaroff, Tsvetan R.] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA; [Delwiche, Charles F.] Univ Maryland, College Pk, MD 20742 USA	Smithsonian Institution; Smithsonian Environmental Research Center; University System of Maryland; University of Maryland College Park	Coats, DW (通讯作者)，Smithsonian Environm Res Ctr, POB 28, Edgewater, MD 21037 USA.	coatsw@si.edu	; Delwiche, Charles Francis/C-6549-2008	Bachvaroff, Tsvetan/0000-0003-3800-9214; Coats, D Wayne/0000-0002-0636-189X; Delwiche, Charles Francis/0000-0001-7854-8584	National Science Foundation;  [EF-06299624]	National Science Foundation(National Science Foundation (NSF)); 	This work was funded in part by a National Science Foundation, Assembling the Tree of Life grant to C. F. D, D. W. C., and colleagues (EF-06299624). We are greatly indebted to Dr. Sabine Agatha, Fachbereich Organismische Biologie, Universitat Salzburg, for advice on tintinnid taxonomy.	Cachon J., 1964, Annales des Sciences Naturelles (12), V6, P1; Cachon J., 1987, The Biology of Dinoflagellates, P571; Chatton E, 1936, CR HEBD ACAD SCI, V203, P573; Chatton E., 1920, Archives de Zoologie Experimentale Paris, V59; Chatton E., 1952, TRAITE ZOOL, P309; Coats DW, 2010, J EUKARYOT MICROBIOL, V57, P468, DOI 10.1111/j.1550-7408.2010.00504.x; COATS DW, 1988, J PROTOZOOL, V35, P607, DOI 10.1111/j.1550-7408.1988.tb04159.x; COATS DW, 1982, MAR BIOL, V67, P71, DOI 10.1007/BF00397096; Duboscq O, 1910, CR HEBD ACAD SCI, V151, P340; Fensome R.A., 1993, Micropaleontology Press Special Paper; Handy SM, 2009, J PHYCOL, V45, P1163, DOI 10.1111/j.1529-8817.2009.00738.x; Kim SY, 2010, J EUKARYOT MICROBIOL, V57, P460, DOI 10.1111/j.1550-7408.2010.00500.x; Kofoid C.A., 1939, Bulletin o fthe Museum of Comparative Zoology, Harvard, V84, P1; KOFOID CHARLES A., 1929, UNIV CALIF PUBL ZOOL, V34, P1; Laackmann Hans, 1906, Zoologischer Anzeiger Leipzig, V30; Laackmann Hans, 1908, Wissenschaftliche Meeresuntersuchungen Kiel N F, V10; Lohmann H., 1908, Wissenschaftliche Meeresuntersuchungen Kiel N F, V10; Montagnes D.J.J., 1993, Handbook of Methods in Aquatic Microbial Ecology, P229; MORGAN DR, 1995, ANN MO BOT GARD, V82, P208	19	29	33	2	23	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	1066-5234			J EUKARYOT MICROBIOL	J. Eukaryot. Microbiol.	JAN-FEB	2012	59	1					1	11		10.1111/j.1550-7408.2011.00588.x	http://dx.doi.org/10.1111/j.1550-7408.2011.00588.x			11	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	872ZN	22221918				2025-03-11	WOS:000298850200001
J	Clausen, OR; Sliwinska, KK; Goledowski, B				Clausen, O. R.; Sliwinska, K. K.; Goledowski, B.			Oligocene climate changes controlling forced regression in the eastern North Sea	MARINE AND PETROLEUM GEOLOGY			English	Article						Incisions; Forced regression; Dinocysts; Oi2 cooling; Rupelian	GENETIC STRATIGRAPHIC SEQUENCES; DINOFLAGELLATE CYSTS; CENTRAL GRABEN; LEVEL CHANGES; BASIN ANALYSIS; MIOCENE; DENMARK; DELTA; TOPOGRAPHY; TRANSITION	In this paper we investigate the Early Oligocene (Rupelian) high-angle clinoform complex from the western part of the Norwegian-Danish Basin. The study consists of an integrated analysis of 3D seismics, petrophysical well logs and micropaleontological data. A series of erosional features and geometry of prograding units, e.g. the high-angle clinoform complex, interpreted as a forced regressive unit, is identified. The proposed depositional model accounts for lithological variations, climate-induced sea-level fluctuation and depositional environment. The characteristic high-angle clinoform complex has been estimated to be of Late Rupelian age. Paleoenvironmental reconstruction of the unit (based on dinocyst analysis) suggests that the deposition of the succession took place in submarine conditions. Presence of a cold-water dinoflagellate Svalbardella within the unit containing high-angle clinoforms suggests that the unit was deposited during one of the Oligocene glacial maxima (the most probably the Oi2 cooling event). (C) 2011 Elsevier Ltd. All rights reserved.	[Clausen, O. R.; Sliwinska, K. K.; Goledowski, B.] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark	Aarhus University	Clausen, OR (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	ole.r.clausen@geo.au.dk	Clausen, Ole/A-5290-2012; Sliwinska, Kasia K./G-9097-2018	Sliwinska, Kasia K./0000-0001-5488-8832; Clausen, Ole Rono/0000-0002-6825-9065	Aarhus University (Denmark); Fur Museum (Denmark); Faculty of Science and Technology, Aarhus University; DONG Norway	Aarhus University (Denmark); Fur Museum (Denmark); Faculty of Science and Technology, Aarhus University; DONG Norway	K.K. Sliwinska thanks Claus Heilmann-Clausen (AU), Karen Dybkjaer (GEUS) and acknowledges financial support for her PhD project from Aarhus University (Denmark) and Fur Museum (Denmark). The Faculty of Science and Technology, Aarhus University and DONG Norway is thanked for financial support of B. Goledowski's PhD project and access to the datasets. Seismic Micro Technologies is thanked for giving access to the KINGDOM Suite. GEUS and DONG Energy A/S are thanked for giving access to the seismic and well data used in this study. Lone Davidsen (AU) is thanked for improving the language of the manuscript. Henrik Nohr-Hansen (GEUS) is acknowledged for his valuable comments. Nicolas Christie-Blick and a second anonymous reviewer are thanked for their insightful and constructive comments and suggestions which substantially improved the structure of the manuscript.	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Pet. Geol.	JAN	2012	29	1					1	14		10.1016/j.marpetgeo.2011.10.002	http://dx.doi.org/10.1016/j.marpetgeo.2011.10.002			14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	863ZE					2025-03-11	WOS:000298206000001
J	Edwards, LE				Edwards, Lucy E.			Dinocyst taphonomy, impact craters, cyst ghosts and the Paleocene-Eocene thermal maximum (PETM)	PALYNOLOGY			English	Article						dinoflagellates; taphonomy; preservation; Paleocene; Eocene; Chesapeake Bay impact; PETM	WALLED DINOFLAGELLATE CYSTS; COMET IMPACT; NEW-JERSEY; PRESERVATION; CARBON; DISSOCIATION; ASSEMBLAGES; INFERENCES; VOLCANISM; MAGNETITE	Dinocysts recovered from sediments related to the Chesapeake Bay impact structure in Virginia and the earliest Eocene suboxic environment in Maryland show strange and intriguing details of preservation. Features such as curled processes, opaque debris, breakage, microborings and cyst ghosts, among others, invite speculation about catastrophic depositional processes, rapid burial and biological and chemical decay. Selected specimens from seven cores taken in the coastal plain of Virginia and Maryland show abnormal preservation features in various combinations that merit illustration, description, discussion and further study. Although the depositional environments described are extreme, many of the features discussed are known from, or could be found in, other environments. These environments will show both similarities to and differences from the extreme environments here.	US Geol Survey, Reston, VA USA	United States Department of the Interior; United States Geological Survey	Edwards, LE (通讯作者)，US Geol Survey, 926A Natl Ctr, Reston, VA USA.	leedward@usgs.gov						Aubry MP, 2007, EPISODES, V30, P271, DOI 10.18814/epiiugs/2007/v30i4/003; BEHRENSMEYER AK, 1985, PALEOBIOLOGY, V11, P105; Bice KL, 2002, PALEOCEANOGRAPHY, V17, DOI 10.1029/2001PA000678; Bralower TJ, 1997, GEOLOGY, V25, P963, DOI 10.1130/0091-7613(1997)025<0963:HRROTL>2.3.CO;2; BUDD DA, 1980, J SEDIMENT PETROL, V50, P881; CANFIELD DE, 1987, GEOCHIM COSMOCHIM AC, V51, P645, DOI 10.1016/0016-7037(87)90076-7; Clark WB, 1901, MARYLAND GEOLOGICAL; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; de Leeuw JW, 2006, PLANT ECOL, V182, P209, DOI 10.1007/s11258-005-9027-x; Deflandre G., 1938, TRAVAUX STATION ZOOL, V13, P147; Dickens GR, 1997, GEOLOGY, V25, P259, DOI 10.1130/0091-7613(1997)025<0259:ABOGIT>2.3.CO;2; DICKENS GR, 1995, PALEOCEANOGRAPHY, V10, P965, DOI 10.1029/95PA02087; Edwards LE, 2009, GEOL SOC AM SPEC PAP, V458, P51, DOI 10.1130/2009.2458(03); Edwards L.E., 2005, Studies of the Chesapeake Bay Impact Structure-The USGS-NASA Langley Corehole, Hampton, Virginia, and Related Coreholes and Geophysical Surveys, pH1; Edwards LE, 2003, PALAIOS, V18, P275, DOI 10.1669/0883-1351(2003)018<0275:IDTDFT>2.0.CO;2; Edwards LE, 1982, WR821 USGS; Edwards LE, 2010, GEOL SOC AM SPEC PAP, V465, P319, DOI 10.1130/2010.2465(19); Efremov I.A., 1940, PAN AM GEOL, V74, P81; ELSIK WILLIAM C., 1966, MICROPALEONTOLOGY [NEW YORK], V12, P515, DOI 10.2307/1484797; Fensome R.A., 1993, Micropaleontology Press Special Paper; Fensome RA, 2004, AASP CONTRIBUTIONS S; Finster KW, 2009, ANTON LEEUW INT J G, V96, P515, DOI 10.1007/s10482-009-9367-y; Frederiksen NO., 2005, Studies of the Chesapeake Bay Impact Structure-The USGS-Langley Corehole, Hampton, Virginia and Related 28 Coreholes and Geophysical Surveys, V1st, pD1; Gibson TG, 2000, SEDIMENT GEOL, V134, P65, DOI 10.1016/S0037-0738(00)00014-2; Gohn GS, 2008, SCIENCE, V320, P1740, DOI 10.1126/science.1158708; Harris AD, 2010, PALEOCEANOGRAPHY, V25, DOI 10.1029/2009PA001800; HART G F, 1986, Palynology, V10, P1; HAVINGA A. 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J	Riding, JB; Pound, MJ; Hill, TCB; Stukins, S; Feist-Burkhardt, S				Riding, James B.; Pound, Matthew J.; Hill, Thomas C. B.; Stukins, Stephen; Feist-Burkhardt, Susanne			The John Williams Index of Palaeopalynology	PALYNOLOGY			English	Article						card indexes; databases; literature; palaeopalynology	FOSSIL; PALYNODATA; MORGENROTH; ENGLAND; BASIN; EMEND; GENUS	The John Williams Index of Palaeopalynology (JWIP) is the result of the lifetime's work of Dr John E. Williams. Housed at the Department of Palaeontology of The Natural History Museum (NHM) in London, the JWIP is publically available and provides probably the most comprehensive fully cross-referenced catalogue on palaeopalynology in the world. It has 23,350 references to fossil palynomorph genera or species as of February 2012. Since its inception in 1971, every publication in the collection referring to a fossil palynomorph genus or species has been critiqued by John E. Williams. Each item is given an accession number and appropriately referenced within the JWIP using index cards which are sorted alphabetically. Once added to the main reference subindex, further entries are completed for four themed subindexes. The first three of these are sets of cards on the three major palynomorph groups (acritarchs/dinoflagellate cysts, chitinozoa and pollen/spores), 26 stratigraphical intervals and 17 geographical areas. The fourth themed subindex is where each palynomorph taxon has a card (or cards) listing all the records of that species in the literature within six categories (acritarchs, dinoflagellate cysts, chitinozoa, fungal spores, pollen/spores and miscellaneous). Due to the sustained and meticulous recording of data since 1971, users can therefore search the database by major palynomorph group, species, age and/or geographical region. The comprehensive and cross-referenced nature of the JWIP means that researchers can readily identify key publications on, for example, specific palynomorph types over a particular interval in a prescribed area. The JWIP is currently entirely analogue, but the NHM is currently evaluating potential strategies for digitisation.	[Riding, James B.] British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England; [Pound, Matthew J.] Northumbria Univ, Sch Built & Nat Environm, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England; [Hill, Thomas C. B.; Stukins, Stephen] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Feist-Burkhardt, Susanne] SFB Geol Consulting & Serv, D-64372 Ober Ramstadt, Germany	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Northumbria University; Natural History Museum London	Riding, JB (通讯作者)，British Geol Survey, Ctr Environm Sci, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009; Stukins, Stephen/B-8396-2013	Stukins, Stephen/0000-0003-3551-8283; Hill, Thomas/0000-0001-6538-4939; Feist-Burkhardt, Susanne/0000-0001-6019-6242; Pound, Matthew/0000-0001-8029-9548	NERC [bgs05002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Alpern B, 1970, C C U LIEGE, V55, P81; Alroy J, 2003, PALEOBIOLOGY, V29, P26, DOI 10.1666/0094-8373(2003)029<0026:GDWYRM>2.0.CO;2; Alroy J., 2012, PALEOBIOLOGY DATABAS; [Anonymous], 1978, ANALYSES PREPLEISTOC; [Anonymous], PALYNOLOGY PRINCIPLE; [Anonymous], LPP CONTRIBUTIONS SE; Artzner D, 1979, SYSTEMATIC ILLUSTRAT; Deflandre G, 1966, FICHIER MICROPALEONT, P2876; Deflandre G, 1965, FICHIER MICROPALEONT, P2522; Eaton GL, 2001, NEUES JAHRB GEOL P-A, V219, P171, DOI 10.1127/njgpa/219/2001/171; Eisenack A, 1967, KATALOG FOSSILEN DIN, VI; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Fensome R. 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C	Orlova, TY		Lutaenko, KA		Orlova, Tatiana Yu.			Resting stages of planktonic microalgae in recent marine sediments from the east coast of Russia with special emphasis on toxic species	PROCEEDINGS OF THE RUSSIA-CHINA BILATERAL SYMPOSIUM ON MARINE ECOSYSTEMS UNDER THE GLOBAL CHANGE IN THE NORTHWESTERN PACIFIC			English	Proceedings Paper	Russia-China Bilateral Symposium on Marine Ecosystems under the Global Change in the Northwestern Pacific	OCT 08-09, 2012	A V Zhirmunsky Inst Marine Biol, Vladivostok, RUSSIA	Far Eastern Branch Russian Acad Sci, A V Zhirmunsky Inst Marine Biol, Chinese Acad Sci, Inst Oceanol	A V Zhirmunsky Inst Marine Biol		DINOFLAGELLATE CYSTS		Russian Acad Sci, Far Eastern Branch, AV Zhirmunsky Inst Marine Biol, Vladivostok 690059, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Orlova, TY (通讯作者)，Russian Acad Sci, Far Eastern Branch, AV Zhirmunsky Inst Marine Biol, Vladivostok 690059, Russia.		Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967				ANDERSON DM, 1982, LIMNOL OCEANOGR, V27, P757, DOI 10.4319/lo.1982.27.4.0757; 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; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; Konovalova G. V., 1999, Russian Journal of Marine Biology, V25, P295; Matsuoka K., 1989, P461; MATSUOKA K, 1994, BOT MAR, V37, P495, DOI 10.1515/botm.1994.37.6.495; Orlova T., 1998, HARMFUL ALGAE, P86; Orlova TY, 2008, BOT MAR, V51, P297, DOI 10.1515/BOT.2008.035; Qi Yu-Zao, 1996, Asian Marine Biology, V13, P87; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	11	0	0	0	2	A V ZHIRMUNSKY INST MARINE BIOLOGY	VLADIVOSTOK	FAR EASTERN BRANCH RUSSIAN ACAD SCIENCES, PAL CHEVSKOGO, 17, VLADIVOSTOK, 690059, RUSSIA			978-5-8044-1327-0				2012							41	43						3	Marine & Freshwater Biology	Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	BA2IV					2025-03-11	WOS:000333442800010
J	Band-Schmidt, CJ; Bustillos-Guzmán, JJ; López-Cortés, DJ; Núñez-Vázquez, E; Hernández-Sandoval, FE				Band-Schmidt, Christine J.; Bustillos-Guzman, Jose J.; Lopez-Cortes, David J.; Nunez-Vazquez, Erick; Hernandez-Sandoval, Francisco E.			The actual state of the study of harmful algal blooms in Mexico	HIDROBIOLOGICA			Spanish	Article						Harmful algal blooms; Mexico; monitoring; publications; toxins	GULF-OF-CALIFORNIA; SHELLFISH POISONING TOXINS; VESSEL BALLAST WATER; DINOFLAGELLATE GYMNODINIUM-CATENATUM; LIQUID-CHROMATOGRAPHIC DETERMINATION; CHATTONELLA-MARINA RAPHIDOPHYCEAE; PARALYTIC SHELLFISH; RED-TIDE; BAHIA-CONCEPCION; QUANTITATIVE-DETERMINATION	This review presents an analysis of the state of knowledge of harmful algae studies in the marine environment in Mexico, in order to evaluate how we can optimize the available resources to study these events, identify unattended issues, and propose improvements in monitoring and/or research programs that could help to further understand the complexity of Harmful Algal Blooms (HAB) in our coasts. An exhaustive bibliographic revision, from 1940 to 2011, was done consulting specialized data analyses, conference meetings, specialized books and manuals. The number of researchers and institutions involved in HAB studies has increased significantly during the last decades, which is reflected in the number and quality of publications. However most of the existing HAB reports are based on sporadic sampling and short-term research programs. Monitoring programs and research activities have focused only in a few HAB species; many toxic and harmful microalgal species have not been considered. To date, there is no laboratory with the capacity and techniques to analyze all the phycotoxins detected in Mexican coasts. Also, many research areas have not been attended adequately in Mexico such as cyst studies, allelophaty, exotic species, effect of climate change, use of molecular tools and teledetection, socioeconomic analyses, and mitigation strategies among others. This review shows that there has been a significantly improvement in the study of HAB in Mexico. However studies are still addressed under an individual and disperse way and lack coordination. Greater achievements would be obtained if we concentrate and coordinate the efforts of researchers and institutions in order to optimize the available resources for HAB studies.	[Band-Schmidt, Christine J.] Inst Politecn Nacl, Ctr Interdisciplinario Ciencias Marinas, La Paz 23096, Bcs, Mexico; [Bustillos-Guzman, Jose J.; Lopez-Cortes, David J.; Nunez-Vazquez, Erick; Hernandez-Sandoval, Francisco E.] Ctr Invest Biol Noroeste, La Paz 23090, Bcs, Mexico; [Nunez-Vazquez, Erick] Invest Conservac & Desarrollo, La Paz 23080, Bcs, Mexico	Instituto Politecnico Nacional - Mexico; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Telefonica SA	Band-Schmidt, CJ (通讯作者)，Inst Politecn Nacl, Ctr Interdisciplinario Ciencias Marinas, Av Inst Politecn Nacl S-N, La Paz 23096, Bcs, Mexico.	cbands@ipn.mx		Band-Schmidt, Christine Johanna/0000-0002-8251-9820; Nunez Vazquez, Erick Julian/0000-0003-1257-731X				AGUIRREGOMEZ R, 1999, GEOFISICA INT, V38, P63; AHMED MS, 1995, BBA-GEN SUBJECTS, V1243, P509; Ake-Castillo J.A., 2010, Harmful Algae News, V41, P16; Ake-Castillo J.A., 2009, HARMFUL ALGAE NEWS, V40, P6; Aldeco J, 2009, CIENC MAR, V35, P333, DOI 10.7773/cm.v35i4.1551; ALMAZANBECERRIL A, 2000, THESIS U NACL AUTONO; ALMAZANBECERRIL.A, 2009, 3 TALL FLOR ALG NOC; Alonso-Rodríguez R, 2004, HARMFUL ALGAE, V3, P163, DOI 10.1016/j.hal.2003.10.002; Alonso-Rodríguez R, 2003, AQUACULTURE, V219, P317, DOI 10.1016/S0044-8486(02)00509-4; Alonso-Rodriguez R., 2008, CATALOGO MICROALGAS; Alonso-Rodriguez R., 2004, El fitoplancton en la camaronicultura y larvicultura: importancia de un buen manejo; ALONSORODRIGUEZ R, 2004, 13 REUN NAC SOC MEX, P54; Altamirano RC, 2008, TOXIN REV, V27, P27, DOI 10.1080/15569540701883437; Alvarez-Góngora C, 2006, MAR POLLUT BULL, V52, P48, DOI 10.1016/j.marpolbul.2005.08.006; ALVAREZBORREGO J, 2008, INTRO IDENTIFICACION, P61; ALVAREZGONGORA C, 2005, AVANCE PERSPECTIVA, V24, P33; ALVAREZGONGORA C, 2009, 3 TALL FLOR ALG NOC; Amandi MF, 2002, J CHROMATOGR A, V976, P329, DOI 10.1016/S0021-9673(02)00946-9; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; Anderson DM, 2010, OCEANOGRAPHY, V23, P72, DOI 10.5670/oceanog.2010.25; [Anonymous], 2003, MANUAL HARMFUL MARIN; [Anonymous], 1996, Harmful and Toxic Algal; [Anonymous], 1998, 388802005 RIVM; [Anonymous], 2006, ACTA BOT MEX, DOI DOI 10.21829/ABM74.2006.1008; [Anonymous], 2004, HARMFUL ALGAE; [Anonymous], 1995, MANUAL HARMFUL MARIN; [Anonymous], 2005, Rev. 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J	Rhodes, L; Smith, K; Selwood, A; McNabb, P; Molenaar, S; Munday, R; Wilkinson, C; Hallegraeff, G				Rhodes, L.; Smith, K.; Selwood, A.; McNabb, P.; Molenaar, S.; Munday, R.; Wilkinson, C.; Hallegraeff, G.			Production of pinnatoxins E, F and G by scrippsielloid dinoflagellates isolated from Franklin Harbour, South Australia	NEW ZEALAND JOURNAL OF MARINE AND FRESHWATER RESEARCH			English	Article						Peridiniales; scrippsielloid; pinnatoxin; toxicity; LC-MS; South Australia		A pinnatoxin producing dinoflagellate was isolated in cyst form from sediments from Franklin Harbour, South Australia, December 2009. One isolate (CAWD180) produced pinnatoxin G, E, F and A (87, 10, 41 and 1.3 pg/cell respectively; liquid chromatograph-mass spectrometer, LC-MS, analysis) and another (CAWD183) produced pinnatoxin G only (13 pg/cell). Australian strains were identical to pinnatoxin E and F producers isolated from Northland, New Zealand (2008), based on large subunit (LSU) rDNA and ITS spacer region sequence data. Cysts were capable of division and produced more toxin per cell than the excysted motile form. Crude extracts of mass cultures were tested for toxicity in mice by intraperitoneal (i.p.) injection, gavage and voluntary consumption, and toxicity ratios were 1.0: 1.8: 4.5 (CAWD180) and 1.0: 2.9: 7.8 (CAWD183). This is similar to the ratios for New Zealand isolates, but differs from other cyclic imines for which oral toxicity can be 10-1000-fold less than i.p. administration.	[Rhodes, L.; Smith, K.; Selwood, A.; McNabb, P.; Molenaar, S.] Cawthron Inst, Nelson, New Zealand; [Munday, R.] AgResearch, Hamilton, New Zealand; [Wilkinson, C.] Lincoln Marine Sci Ctr, Port Lincoln, SA, Australia; [Hallegraeff, G.] Univ Tasmania, Inst Marine & Antarctic Studies, Hobart, Tas, Australia	Cawthron Institute; AgResearch - New Zealand; University of Tasmania	Rhodes, L (通讯作者)，Cawthron Inst, Nelson, New Zealand.	Lesley.Rhodes@cawthron.org.nz	Selwood, Andrew/AAP-7550-2020; McNabb, Paul/LKN-9195-2024; Hallegraeff, Gustaaf/C-8351-2013	Hallegraeff, Gustaaf/0000-0001-8464-7343; Selwood, Andrew/0000-0003-1399-8028	NZ Foundation for RST [CAW0703]	NZ Foundation for RST	Thanks for technical help to Janet Adamson (mass cultures) and Roel van Ginkel (LC-MS analyses). The study was funded by NZ Foundation for RST, Contract CAW0703.	Hall T. A., NUCL ACIDS S SER, V41, P95; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; KELLER MD, 1987, J PHYCOL, V23, P633; McNabb P, 2008, RESULTS ANAL BREVETO; Munday Rex, 2008, P581; Nunn GB, 1996, J MOL EVOL, V42, P211, DOI 10.1007/BF02198847; OECD, 2006, OECD GUID TEST CHEM; Rhodes L, 2010, HARMFUL ALGAE, V9, P384, DOI 10.1016/j.hal.2010.01.008; Rhodes L., 2010, Harmful Algae 2008, P151; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Selwood AI, 2010, J AGR FOOD CHEM, V58, P6532, DOI 10.1021/jf100267a	11	34	35	1	15	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0028-8330	1175-8805		NEW ZEAL J MAR FRESH	N. Z. J. Mar. Freshw. Res.	DEC	2011	45	4					703	709		10.1080/00288330.2011.586041	http://dx.doi.org/10.1080/00288330.2011.586041			7	Fisheries; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries; Marine & Freshwater Biology; Oceanography	880RM					2025-03-11	WOS:000299424600011
J	Crespo, BG; Keafer, BA; Ralston, DK; Lind, H; Farber, D; Anderson, DM				Crespo, Bibiana G.; Keafer, Bruce A.; Ralston, David K.; Lind, Henry; Farber, Dawson; Anderson, Donald M.			Dynamics of <i>Alexandrium fundyense</i> blooms and shellfish toxicity in the Nauset Marsh System of Cape Cod (Massachusetts, USA)	HARMFUL ALGAE			English	Article						Paralytic shellfish poisoning; Alexandrium fundyense; Dinoflagellate cysts; Bloom dynamics; Retention mechanism; Nauset Marsh System	DINOFLAGELLATE GONYAULAX-TAMARENSIS; PHYSICAL-BIOLOGICAL MODEL; RED TIDE DINOFLAGELLATE; CYST FORMATION; WESTERN GULF; POPULATION-DYNAMICS; RESTING CYSTS; MAINE; DINOPHYCEAE; BAY	Paralytic Shellfish Poisoning (PSP) toxins are annually recurrent along the Massachusetts coastline (USA), which includes many small embayments and salt ponds. Among these is the Nauset Marsh System (NMS), which has a long history of PSP toxicity. Little is known, however, about the bloom dynamics of the causative organism Alexandrium fundyense within that economically and socially important system. The overall goal of this work was to characterize the distribution and dynamics of A. fundyense blooms within the NMS and adjacent coastal waters by documenting the distribution and abundance of resting cysts and vegetative cells. Cysts were found predominantly in three drowned kettle holes or salt ponds at the distal ends of the NMS - Salt Pond, Mill Pond, and Town Cove. The central region of the NMS had a much lower concentration of cysts. Two types of A. fundyense blooms were observed. One originated entirely within the estuary, seeded by cysts in the three seedbeds. These blooms developed independently of each other and of the A. fundyense population observed in adjacent coastal waters outside the NMS. The temporal development of the blooms was different in the three salt ponds, with initiation differing by as much as 30 days. These differences do not appear to reflect the initial cyst abundances in these locations, and may simply result from higher cell retention and higher nutrient concentrations in Mill Pond, the first site to bloom. Germination of cysts accounted for a small percentage of the peak cell densities in the ponds, so population size was influenced more by the factors affecting growth than by cyst abundance. Subsurface cell aggregation (surface avoidance) limited advection of the vegetative A. fundyense cells out of the salt ponds through the shallow inlet channels. Thus, the upper reaches of the NMS are at the greatest risk for PSP since the highest cyst abundances and cell concentrations were found there. After these localized blooms in the salt ponds peaked and declined, a second, late season bloom occurred within the central portions of the NMS. The timing of this second bloom relative to those within the salt ponds and the coastal circulation patterns at that time strongly suggest that those cells originated from a regional A. fundyense bloom in the Gulf of Maine, delivered to the central marsh from coastal waters outside the NMS through Nauset Inlet. These results will guide policy decisions about water quality as well as shellfish monitoring and utilization within the NMS and highlight the potential for "surgical" closures of shellfish during PSP events, leaving some areas open for harvesting while others are closed. (C) 2011 Elsevier B.V. All rights reserved.	[Crespo, Bibiana G.; Keafer, Bruce A.; Ralston, David K.; Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Lind, Henry] Town Eastham Dept Nat Resources, Eastham, MA 02642 USA; [Farber, Dawson] Town Orleans Shellfish & Harbormaster Dept, Orleans, MA 02653 USA	Woods Hole Oceanographic Institution	Crespo, BG (通讯作者)，Inst Ciences Mar ICM CSIC, Passeig Maritim Barceloneta 37-49, Barcelona 08003, Spain.	bibiana@icm.csic.es			NOAA [NA06OAR4170021]; NPS [H238015504]; Woods Hole Center for Oceans and Human Health through NSF [OCE-0911031, OCE-0430724]; NIEHS [1P50-ES01274201]; Xunta de Galicia; Woods Hole Oceanographic Institution; Division Of Ocean Sciences; Directorate For Geosciences [0911031, 1128041] Funding Source: National Science Foundation	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); NPS; Woods Hole Center for Oceans and Human Health through NSF; NIEHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); Xunta de Galicia(Xunta de Galicia); Woods Hole Oceanographic Institution; Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We especially thank Mike Conner and staff from the Town of Eastham and staff from the Town of Orleans for small boat operations and collection of shellfish. Mike Hickey/Terry O'Neill from the Massachusetts Division of Marine Fisheries (MA DMF) for providing the shellfish toxicity data, Megan Tyrell for her support in permitting the work within the Cape Cod National Seashore (CACO), Jim Manning (National Oceanograhic and Atmospheric Administration Northeast Fisheries Center) for providing the drifter data, and the crew of the R/V Tioga. We also thank the staff and students from the Anderson Laboratory in WHO] who assisted with the collection and analysis of many cell and cyst samples, especially to K. Norton, J. Selwyn, N. Ishimaru, and B. Conroy. This work was supported by NOAA Grant NA06OAR4170021, NPS Grant H238015504 and by the Woods Hole Center for Oceans and Human Health through NSF Grants OCE-0911031 and OCE-0430724 and NIEHS Grant 1P50-ES01274201. B.G.C. was supported by a Xunta de Galicia Angeles Alvarino fellowship and the Stanley W. 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J	Yang, I; Beszteri, S; Tillmann, U; Cembella, A; John, U				Yang, Ines; Beszteri, Sara; Tillmann, Urban; Cembella, Allan; John, Uwe			Growth- and nutrient-dependent gene expression in the toxigenic marine dinoflagellate <i>Alexandrium minutum</i>	HARMFUL ALGAE			English	Article						Alexandrium minutum; Growth stage; Nutrients; Gene expression	DIFFERENT NITROGEN-SOURCES; TOXIC DINOFLAGELLATE; CHLOROPHYLL FLUORESCENCE; PHYTOPLANKTON BLOOMS; CARBONIC-ANHYDRASE; CYST PRODUCTION; CELL-CYCLE; DINOPHYCEAE; PHOSPHORUS; TAMARENSE	The toxigenic marine dinoflagellate Alexandrium minutum forms toxic blooms causing paralytic shellfish poisoning (PSP), primarily in coastal waters, throughout the world. We examined effects on physiology and gene expression patterns associated with growth and nutrient starvation in a toxic strain of A. minutum. Bloom-relevant factors, including growth rate, intracellular toxin content, allelochemical activity and nutrient status were investigated in A. minutum cultures grown under different environmental regimes. Allelochemical activity of A. minutum cultures, quantified with a cryptomonad Rhodomonas bioassay, increased with age but was independent of nutrient status. The phenotypic data were integrated and compared with gene expression in cell samples taken at selected points along the growth curve. We observed 489 genes consistently differentially expressed between exponentially growing and growth-limited cultures. The expression pattern of stationary-phase cultures was characterized by conspicuous down-regulation of translation-associated genes, up-regulation of sequences involved in intracellular signalling and some indications of increased activity of selfish genetic elements such as transposons. Treatment-specific patterns included five genes regulated in parallel in all nutrient-limited cultures. The conspicuous decrease in photosynthetic: performance identified in N-starved cultures was paralleled by down-regulation of chloroplast-associated genes. The particular gene expression patterns we identified as specifically linked with exponential growth, cessation of growth or nutrient limitation may be suitable biomarkers for indicating the beginning of growth limitation in field- or mesocosm studies. (C) 2011 Elsevier B.V. All rights reserved.	[Yang, Ines; Beszteri, Sara; Tillmann, Urban; Cembella, Allan; John, Uwe] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Yang, I (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Burgermeister Smidt Str 20, D-27568 Bremerhaven, Germany.	Ines.Yang@gmx.net	Yang, Ines/D-6904-2012; John, Uwe/S-3009-2016	Yang, Ines/0000-0002-3812-2690; John, Uwe/0000-0002-1297-4086	EU [GOCE-CT2004-511154]; Marine Genomics [GOCE-CT-2004-505403]; Alfred Wegener Institute, Helmholtz Foundation initiative in Earth and Environment	EU(European Union (EU)); Marine Genomics; Alfred Wegener Institute, Helmholtz Foundation initiative in Earth and Environment	Thanks to Christiane Lorenzen for help with the nutrient measurements and to Annegret Muller and Bernd Krock for help with the PSP toxin measurements. This study was financed by EU-project ESTTAL (GOCE-CT2004-511154), Marine Genomics (GOCE-CT-2004-505403) and the PACES research program of the Alfred Wegener Institute as part of the Helmholtz Foundation initiative in Earth and Environment.[SS]	Anderson CR, 2008, J GEOPHYS RES-OCEANS, V113, DOI 10.1029/2007JC004321; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; Anderson Donald M., 1992, Molecular Marine Biology and Biotechnology, V1, P89; [Anonymous], HARMFUL ALGAE 2002; Bachvaroff TR, 2008, PLOS ONE, V3, DOI 10.1371/journal.pone.0002929; BERMANFRANK I, 1994, LIMNOL OCEANOGR, V39, P1822, DOI 10.4319/lo.1994.39.8.1822; Beszteri S., HARMFUL ALGAE UNPUB; BLANCO J, 1995, J PLANKTON RES, V17, P165, DOI 10.1093/plankt/17.1.165; Bravo I, 2008, HARMFUL ALGAE, V7, P515, DOI 10.1016/j.hal.2007.11.005; Calbet A, 2003, MAR ECOL PROG SER, V259, P303, DOI 10.3354/meps259303; Cembella A, 2006, ECOL STU AN, V189, P215, DOI 10.1007/978-3-540-32210-8_17; 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J	Garg, R; Prasad, V; Thakur, B; Singh, IB; Khowaja-Ateequzzaman				Garg, Rahul; Prasad, Vandana; Thakur, Biswajeet; Singh, Indra Bir; Khowaja-Ateequzzaman			DINOFLAGELLATE CYSTS FROM THE NAREDI FORMATION, SOUTHWESTERN KUTCH, INDIA: IMPLICATION ON AGE AND PALAEOENVIRONMENT	JOURNAL OF THE PALAEONTOLOGICAL SOCIETY OF INDIA			English	Article						Dinoflagellate cysts; Palaeocene-early Eocene; Naredi Formation; Kutch Basin	DECCAN FLOOD BASALTS; LATE PALEOCENE; VASTAN LIGNITE; EOCENE; VOLCANISM; BOUNDARY; TRANSITION; BASIN	The lower part of the early Palaeogene deposits in the Kutch Basin, immediately overlying the Deccan Traps is generally developed as a muddy succession with lignite and rare fossils. Its age has been mostly speculative, based essentially on the age-diagnostic larger foraminiferal fauna in the carbonate horizons present several metres to tens of metres above the base. This muddy succession, named as the Naredi Formation ("Sub-Nummulitic and Gypseous Shale") has been broadly assigned an age of early Eocene or Palaeocene- early Eocene, which has been debated mainly due to the poor record of datable planktic microfossils or lack of age-diagnostic fossils with chronological significance. In the present study, dinoflagellate cyst assemblages including age-diagnostic taxa at several levels from the basal part of the Naredi Formation are recovered. Occurrence of Muratodinium fimbriatum, Heterolaucacysta granulata, Operculodinium severinii and Ginginodinium palaeocenicum in the basal part indicates an age not older than late Thanetian/Sparnacian (similar to 55 Ma, now early Ypresian). Presence of rich Kenleyia complex including LAD of Kenleyia lophophora and K. nuda just below the Venericardia bed indicates Sparnacian/basal Ypresian age (55 similar to 54 Ma). Occurrence of Glaphyrocysta exuberans above this shell coquina also demonstrates early Ypresian age younger than similar to 54Ma. Muratodinium fimbriatum extends up to the base of Assilina Limestone bed in the upper part of the succession. Thus, in terms of traditional European stages, the lower part of the Naredi Formation is assigned the early Ypresian age, broadly corresponding to Ilerdian, representing a time span of similar to 55:54 Ma.	[Garg, Rahul; Singh, Indra Bir] Univ Lucknow, Dept Geol, Lucknow 226007, Uttar Pradesh, India; [Prasad, Vandana; Thakur, Biswajeet; Khowaja-Ateequzzaman] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Lucknow University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Garg, R (通讯作者)，Univ Lucknow, Dept Geol, Lucknow 226007, Uttar Pradesh, India.	rahulbsip@gmail.com	PRASAD, VANDANA/KUF-4093-2024					[Anonymous], PALAEONTOGRAPHICA A; [Anonymous], 2000, Palaeobot; [Anonymous], 1996, Palynology: principles and applications; Aubry MP, 2007, EPISODES, V30, P271, DOI 10.18814/epiiugs/2007/v30i4/003; AUBRY MP, 2003, CAUSES CONSEQUENCES, V369, P551; Biswas S.K., 1992, Journal of the Palaeontological Society of India, V37, P1; Biswas S.K., 1973, B OIL NAT GAS COMM, V10, P37; Biswas S.K., 1965, Bull. Geol. Min. Met Soc, V15, P1; Biswas S.K., 1972, Quart. Jour Geol. 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J	Streng, M; Esper, O; Wollenburg, J				Streng, Michael; Esper, Oliver; Wollenburg, Jutta			Calcareous dinoflagellate cysts from the Pleistocene (Marine Isotope Stage 31) of the Ross Sea, Antarctica	ANTARCTIC SCIENCE			English	Article						Cape Roberts project; Caracomia; cyst ultrastructure; foraminifera; palaeoenvironment; Thoracosphaera	OCEAN	Following a report of supposed fragments of calcareous dinoflagellate cysts from a Pleistocene drill core (CRP-1) recovered in the Ross Sea, Antarctica, sediments of the same core were re-investigated for their microfossil content. Besides common foraminifera and other microfossils, rare complete cysts of calcareous dinoflagellates were found. All cysts belong to the species Caracomia arctica (Gilbert & Clark, 1983) Streng, Hildebrand-Habel & Willems, 2002, a taxon characteristic of late Neogene high latitude, coldwater environments. Two morphotypes can be distinguished, C. arctica f. arctica and C. arctica f. rossensis, of which the latter is described as a new form. The presence of C. arctica strengthens diatom-based palaeoenvironmental reconstructions of periodical sea ice-free conditions at the time of deposition. Accordingly, cysts of C. arctica are interpreted as resting cysts that allow survival during harsh intervals of the high latitude environment. Previously reported calcareous dinoflagellates cyst fragments from these sediments are re-interpreted as test fragments of bilamellar foraminifera, which represent the most common group of foraminifers in the sediments.	[Streng, Michael] Uppsala Univ, Dept Earth Sci, Palaeobiol Programme, S-75236 Uppsala, Sweden; [Esper, Oliver; Wollenburg, Jutta] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Uppsala University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Streng, M (通讯作者)，Uppsala Univ, Dept Earth Sci, Palaeobiol Programme, Villavagen 16, S-75236 Uppsala, Sweden.	michael.streng@geo.uu.se		Streng, Michael/0000-0001-7790-0478; Wollenburg, Jutta/0000-0002-8169-8310; Esper, Oliver/0000-0002-4342-3471	Swedish Research Council (Vetenskapsradet)	Swedish Research Council (Vetenskapsradet)(Swedish Research Council)	Funding by the Swedish Research Council (Vetenskapsradet) to MS is acknowledged. Gary Wife (Uppsala) helped with SEM photography of the uncoated specimen. We thank S. Meier (Kiel), an anonymous reviewer, and the editor for their critical comments and efforts on an earlier version of the manuscript.	[Anonymous], 1998, TERRA ANTART; [Anonymous], TERRA ANTARTICA; [Anonymous], TERRA ANTARTICA; [Anonymous], 1998, TERRA ANTARCT; [Anonymous], 1978, DEEP SEA DRILL PROJ; [Anonymous], TERRA ANTARTICA; [Anonymous], T P PALAEONTOLOGICAL; [Anonymous], 8422 GEOL SURV CAN; Bellemo S., 1974, Bulletin geol Instn Univ Uppsala (NS), V4, P117; Davey F.J., 2001, EOS T AM GEOPHYS UN, V82, P585, DOI [10.1029/01EO00339, DOI 10.1029/01E000339]; Elbrächter M, 2008, TAXON, V57, P1289, DOI 10.1002/tax.574019; Fensome R.A., 1993, Micropaleontology Press Special Paper; FUTTERER DK, 1984, INITIAL REP DEEP SEA, V74, P533; GILBERT MW, 1983, MAR MICROPALEONTOL, V7, P385, DOI 10.1016/0377-8398(83)90017-8; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Hildebrand-Habel T, 2003, PALAEOGEOGR PALAEOCL, V197, P293, DOI 10.1016/S0031-0182(03)00470-X; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; Loeblich A.R., 1988, FORAMINIFERAL GENERA, DOI DOI 10.1007/978-1-4899-5760-3; Scherer RP, 2008, GEOPHYS RES LETT, V35, DOI 10.1029/2007GL032254; Sen Gupta BK, 1999, MODERN FORAMINIFERA, P7; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Streng M, 2002, J PALEONTOL, V76, P397, DOI 10.1666/0022-3360(2002)076<0397:ROTGSK>2.0.CO;2; Streng M, 2009, REV PALAEOBOT PALYNO, V153, P225, DOI 10.1016/j.revpalbo.2008.08.004; Streng Michael, 2004, Journal of Nannoplankton Research, V26, P13; TOWE KENNETH M., 1967, JPALEONTOL, V41, P742; Versteegh GJM, 2009, PALAEONTOLOGY, V52, P343, DOI 10.1111/j.1475-4983.2009.00854.x; Vink A, 2004, MAR MICROPALEONTOL, V50, P43, DOI 10.1016/S0377-8398(03)00067-7; Zonneveld Karin A. F., 2005, Palaeontologische Zeitschrift, V79, P61	28	3	4	0	23	CAMBRIDGE UNIV PRESS	NEW YORK	32 AVENUE OF THE AMERICAS, NEW YORK, NY 10013-2473 USA	0954-1020	1365-2079		ANTARCT SCI	Antarct. Sci.	DEC	2011	23	6					597	604		10.1017/S0954102011000605	http://dx.doi.org/10.1017/S0954102011000605			8	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	865BQ					2025-03-11	WOS:000298286200010
J	Polovodova, I; Nordberg, K; Filipsson, HL				Polovodova, I.; Nordberg, K.; Filipsson, H. L.			The benthic foraminiferal record of the Medieval Warm Period and the recent warming in the Gullmar Fjord, Swedish west coast	MARINE MICROPALEONTOLOGY			English	Article						Medieval Warm Period; Recent warming; Positive NAO; Benthic foraminifera; Nonionella iridea	NORTH-ATLANTIC OSCILLATION; OXYGEN CONCENTRATIONS; CONTINENTAL-SHELF; BATHYMETRIC DISTRIBUTION; TEMPERATURE VARIABILITY; TEMPORAL VARIABILITY; SURFACE TEMPERATURES; DINOFLAGELLATE CYSTS; CLIMATE VARIATIONS; RESERVOIR AGES	A high-resolution study of benthic foraminiferal assemblages was performed on a ca. eight metre long sediment core from Gullmar Fjord on the west coast of Sweden. The results of Pb-210- and AMS C-14-datings show that the record includes the two warmest climatic episodes of the last 1500 years: the Medieval Warm Period (MWP) and the recent warming of the 20th century. Both periods are known to be anomalously warm and associated with positive NAO winter indices. Benthic foraminiferal successions of both periods are compared in order to find faunal similarities and common denominators corresponding to past climate changes. During the MWP, Adercotryma glomerata, Cassidulina laevigata and Nonionella iridea dominated the assemblages. Judging from dominance of species sensitive to hypoxia and the highest faunal diversity for the last ca. 2400 years, the foraminiferal record of the MWP suggests an absence of severe low oxygen events. At the same time, faunas and delta C-13 values both point to high primary productivity and/or increased input of terrestrial organic carbon into the fjord system during the Medieval Warm Period. Comparison of the MWP and recent warming revealed different trends in the faunal record. The thin-shelled foraminifer N. iridea was characteristic of the MWP, but became absent during the second half of the 20th century. The recent Skagerrak-Kattegat fauna was rare or absent during the MWP but established in Gullmar Fjord at the end of the Little Ice Age or in the early 1900s. Also, there are striking differences in the faunal diversity and absolute abundances of foraminifera between both periods. Changes in primary productivity, higher precipitation resulting in intensified land runoff, different oxygen regimes or even changes in the fjord's trophic status are discussed as possible causes of these faunal differences. (C) 2011 Elsevier B.V. All rights reserved.	[Polovodova, I.; Nordberg, K.] Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden; [Filipsson, H. L.] Lund Univ, Dept Earth & Ecosyst Sci, Div Geol, SE-22362 Lund, Sweden	University of Gothenburg; Lund University	Polovodova, I (通讯作者)，Univ Gothenburg, Dept Earth Sci, POB 460, SE-40530 Gothenburg, Sweden.	irina.polovodova@gvc.gu.se	Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Nordberg, Kjell/0000-0003-0085-4607; Polovodova Asteman, Irina/0000-0001-7300-5548	Lamm Foundation; Department of Earth Sciences (University of Gothenburg); Swedish Research Council [VR 621-2007-4369, VR 621-2005-4265]	Lamm Foundation; Department of Earth Sciences (University of Gothenburg); Swedish Research Council(Swedish Research Council)	Authors would like to thank the crew of the R/V Arne Tiselius and R/V Skagerrak for their assistance during sampling; Sofia Andersson and Asli Oflaz for their help with foraminiferal analysis; David Cornell (University of Gothenburg, Sweden) for his assistance with SEM images; Amanda Hicks (Editors Ink) and Timothy Gallagher (University of Gothenburg) for linguistic improvements; Kennet Lundin (Museum of Natural History, Gothenburg) and Anders Waren (Swedish Museum of Natural History, Stockholm) for providing the mollusc shells for reservoir age determinations; the editor Frans Jorissen and two anonymous reviewers for their valuable comments, which significantly improved the manuscript; the Lamm Foundation and Swedish Research Council for the financial support to KN (VR 621-2007-4369) and HLF (VR 621-2005-4265), the Department of Earth Sciences (University of Gothenburg) for a postdoc scholarship to IP and also the PALEOSTUDIES and EUROPROX program (University of Bremen, Germany), which covered the costs for stable oxygen and carbon isotope analyses.	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J	Zegarra, M; Helenes, J				Zegarra, Monica; Helenes, Javier			Changes in Miocene through Pleistocene dinoflagellates from the Eastern Equatorial Pacific (ODP Site 1039), in relation to primary productivity	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate; Neogene; Productivity; Paleoceanography; Pacific Ocean; ODP Site 1039	SURFACE SEDIMENTS; DEEP-SEA; TROPICAL PACIFIC; LATE PLIOCENE; CYSTS; ATLANTIC; NORTHERN; PRESERVATION; NEOGENE; BIOSTRATIGRAPHY	Palynological data from offshore Costa Rica, allow us to investigate the relationship between dinoflagellate cyst assemblages and changes in regional oceanic primary productivity. From Miocene to Pleistocene, productivity at ODP Site 1039 was influenced by tectonic drift, as Site 1039 approached the continent, from the Equator to its current position at similar to 10 degrees N. In addition, dinoflagellate abundance is modulated by regional productivity events, which modified primary productivity, as also indicated by available data on calcareous nannofossils, diatoms, TOC, and CaCO3 content. Five palynomorph intervals are defined. The early-late Miocene one, dominated by Batiacasphaera, represents relatively stable, productive oceanic conditions before the closure of the Indonesian and Panama Seaways. The late Miocene decrease in palynomorph recovery is related to the Carbonate Crash Event. The high abundance and diversity of the assemblages at the end of the late Miocene to early Pliocene indicate increased productivity related to the Global Biogenic Bloom. and a change in dominance from Batiacasphaera to Impagidinium to Nematosphaeropsis. The low abundance of the late Pliocene interval is related to El Nino-like conditions, and there is another change related to the disappearance of Batiacasphaera and dominance of Impagidinium, Nematosphaeropsis, and Operculodinium. The abundant Pleistocene assemblages represent increased marine productivity, and a high influx of continental palynomorphs and bissacate pollen, associated with the proximity of the Costa Rica Dome. Pleistocene dinoflagellates are characterized by Spiniferites and Selenopemphix, together with rare Impagidinium and Nematosphaeropsis. (C) 2011 Elsevier B.V. All rights reserved.	[Zegarra, Monica; Helenes, Javier] CICESE, Dept Geol, Mexico City, DF, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Helenes, J (通讯作者)，CICESE, Dept Geol, Mexico City, DF, Mexico.	jhelenes@cicese.mx	Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879	CONACYT [84274]; CICESE	CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); CICESE	The authors thank CONACYT (project 84274) and CICESE for financial support. We also thank the Ocean Drilling Program for providing the samples used here. The authors thank J. Contreras, J.C. Herguera, and J.G. Flores for their valuable comments, and to E. Collins and M. Duarte for their help in the palynological processing of the samples. We also acknowledge ideas and suggestions made by Lucy Edwards and Stephen Louwye who reviewed and improved the manuscript.	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J	Reñé, A; Satta, CT; Garcés, E; Massana, R; Zapata, M; Anglès, S; Camp, J				Rene, Albert; Satta, Cecilia Teodora; Garces, Esther; Massana, Ramon; Zapata, Manuel; Angles, Silvia; Camp, Jordi			<i>Gymnodinium litoralis</i> sp nov (Dinophyceae), a newly identified bloom-forming dinoflagellate from the NW Mediterranean Sea	HARMFUL ALGAE			English	Article						Cyst; Gymnodinium; HAB; LSU; Mediterranean Sea; Pigments	COMB. NOV; RECENT SEDIMENTS; COASTAL WATERS; LSU RDNA; PHYLOGENETIC ANALYSES; MICRORETICULATE CYST; MOLECULAR PHYLOGENY; POLYKRIKOS-KOFOIDII; ELECTRON-MICROSCOPY; PIGMENT COMPOSITION	Recurrent high-biomass blooms of a gymnodinioid species have been periodically recorded at different sites in the NW Mediterranean Sea (Catalan and Sardinian coast), causing intense discolorations of the water. In this study, several strains of the causative organism were isolated and subsequently studied with respect to the morphology of the vegetative cells and different life cycle stages, pigments profile, and molecular phylogeny. Based on phylogenetic analyses, the strains were placed within the Gymnodinium sensu strict clade. The species possessed a horseshoe-shaped apical groove running anticlockwise around the apex and the major accessory pigment was identified as peridinin. These characteristics place the organism within the Gymnodinium genus, as defined today, although some other characteristics, such as vesicular chambers in the nuclear envelope and a nuclear fibrous connective were not observed. Morphologically, the isolates highly resemble Gyrodinium vorax (Biecheler) but major differences with the latter suggest that they comprise a new species, Gymnodinium litoralis sp. nov. The resting cyst of this species is described herein from field samples of the Catalan and Sardinian coast; pellicle cysts were observed in field samples and also in cultures. This species recurrently produces high biomass blooms (>10(6) cell L-1) in summer along several beaches and coastal lagoons in the NW Mediterranean Sea (L'Estartit, La Muga River mouth, and Corru S'Ittiri). Knowledge about its geographic distribution is limited, since the precise identification of G. litoralis from the field or fixed samples can be difficult. Therefore we expect that molecular studies will reveal a much wider distribution of the species. (C) 2011 Elsevier B.V. All rights reserved.	[Rene, Albert; Garces, Esther; Massana, Ramon; Angles, Silvia; Camp, Jordi] Inst Ciencies Mar CSIC, Barcelona 08003, Spain; [Satta, Cecilia Teodora] Univ Sassari, Dipartimento Sci Bot Ecol & Geol, I-07100 Sassari, Italy; [Zapata, Manuel] Inst Invest Marinas CSIC, Vigo 36208, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); University of Sassari; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM)	Reñé, A (通讯作者)，Inst Ciencies Mar CSIC, Pg Maritim de la Barceloneta 37-49, Barcelona 08003, Spain.	albertrene@icm.csic.es	Satta, Cecilia Teodora/AAF-6417-2020; Massana, Ramon/F-4205-2016; Rene, Albert/D-4560-2012; Angles, Silvia/B-9469-2011; Garces, Esther/C-5701-2011	Camp, Jordi/0000-0002-5202-9783; Massana, Ramon/0000-0001-9172-5418; SATTA, Cecilia Teodora/0000-0003-0130-9432; Rene, Albert/0000-0002-0488-3539; Angles, Silvia/0000-0003-0529-7504; Garces, Esther/0000-0002-2712-501X	Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya); CSIC	Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya); CSIC	Financial support was provided by the Agencia Catalana de l'Aigua (Department de Medi Ambient, Generalitat de Catalunya) and the CSIC through the contract "Pla de vigilancia de fitoplancton nociu i toxic a la Costa Catalana". 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J	Chen, L; Zonneveld, KAF; Versteegh, GJM				Chen, Liang; Zonneveld, Karin A. F.; Versteegh, Gerard J. M.			Short term climate variability during "Roman Classical Period" in the eastern Mediterranean	QUATERNARY SCIENCE REVIEWS			English	Article						Climate; Roman Classical Period; Dinoflagellate cysts; North Atlantic Oscillation	WALLED DINOFLAGELLATE CYSTS; NORTH-ATLANTIC OSCILLATION; RADIOCARBON AGE CALIBRATION; SEA-SURFACE CONDITIONS; WESTERN ADRIATIC SEA; SAHARAN DUST; SELECTIVE PRESERVATION; LAST DEGLACIATION; COSMIC-RAYS; SEDIMENTS	To obtain insight into character and potential forcing of short-term climatic and oceanographic variability in the southern Italian region during the "Roman Classical Period" (60 BC-AD 200), climatic and environmental reconstructions based on a dinoflagelate cyst record from a well dated site in the Gulf of Taranto located at the distal end of the Po-river discharge plume have been established with high temporal resolution. Short-term fluctuations in accumulation rates of the Adriatic Surface Water species Lingulodinium machaerophorum, the freshwater algae Concentricystes and species resistant to aerobic degradation indicate that fluctuations in the trophic state of the upper waters are related to river discharge of northern and eastern Italian rivers which in turn are strongly related to precipitation in Italy. The dinoflagellate cyst association indicates that local sea surface temperatures which in this region are strongly linked to local air temperatures were slightly higher than today. We reconstruct that sea surface temperatures have been relatively high and stable between 60 BC-AD 90 and show a decreasing trend after AD 90. Fluctuations in temperature and river discharge rates have a strong cyclic character with main cyclicities of 7-8 and 11 years. We argue that these cycles are related to variations of the North Atlantic Oscillation climate mode. A strong correlation is observed with global variation in Delta C-14 anomalies suggesting that solar variability might be one of the major forcings of the regional climate. Apart from cyclic climate variability we observed a good correlation between non-cyclic temperature drops and global volcanic activity indicating that the latter forms an additional major forcing factor of the southern Italian climate during the Roman Classical Period. (C) 2011 Elsevier Ltd. All rights reserved.	[Chen, Liang; Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; [Zonneveld, Karin A. F.; Versteegh, Gerard J. M.] Univ Bremen, MARUM, D-28359 Bremen, Germany	University of Bremen; University of Bremen	Chen, L (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330440, D-28334 Bremen, Germany.	lichen@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	ESF (European Science Foundation)	ESF (European Science Foundation)(European Science Foundation (ESF))	The study is funded by ESF (European Science Foundation) MOCCHA project (Multidisciplinary study of continental/ocean climate dynamics using high-resolution records from the eastern Mediterranean). We thank all the group members in Historical Geology and Palaeontology, Bremen University for the laboratory help and fruitful discussions. We thank Anna-Lena Grauel, Stefano M. Bernasconi and the AMS <SUP>14</SUP>C Dating Laboratory at ETH Zurich for preparing, measuring and calibrating the AMS <SUP>14</SUP>C-dates. We further would like to thank Arne Leider (MARUM Bremen), Marie-Louise Goudeau (Utrecht University) and Anna-Lena Grauel (ETH Zurich) for the core sub-sampling. Authors are grateful to Captains, Crew and Colleagues onboard RV Pelagia during the MOCCHA- Project Cruise (October-November 2008) under the coordination of Gert J. De Lange (Utrecht University). We wish to thank Prof. Jose Carrion (Editor), Prof. Rex Harland and an anonymous reviewer for their constructive comments on an earlier version of the manuscript.	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J	Lenz, OK; Wilde, V; Riegel, W				Lenz, Olaf K.; Wilde, Volker; Riegel, Walter			Short-term fluctuations in vegetation and phytoplankton during the Middle Eocene greenhouse climate: a 640-kyr record from the Messel oil shale (Germany)	INTERNATIONAL JOURNAL OF EARTH SCIENCES			English	Article						Middle Eocene; Maar lake; Palynology; Climate variability; Milankovitch cycles; Multivariate statistics; Time series analysis	THERMAL MAXIMUM; PALAEOCENE/EOCENE BOUNDARY; DINOFLAGELLATE CYSTS; WAVELET TRANSFORM; FLORAL CHANGE; GULF-COAST; PALEOCENE; BASIN; PALYNOLOGY; POLLEN	The Palaeogene was the most recent greenhouse period on Earth. Especially for the Late Palaeocene and Early Eocene, several superimposed short-term hyperthermal events have been described, including extremes such as the Palaeocene-Eocene Thermal Maximum. Major faunal and floral turnovers in the marine and terrestrial realms were recorded in association with these events. High-resolution palynological analysis of the early Middle Eocene maar lake sediments at Messel, near Darmstadt, Germany, provides an insight into the dynamics of a climax vegetation during the Middle Eocene greenhouse climate in a time span without significant climatic excursions. Numerical techniques like detrended correspondence analysis and wavelet analysis have been applied to recognize cyclic fluctuations and long-term trends in the vegetation through a time interval of approximately 640 kyr. Based on the numerical zoning of the pollen diagram, three phases in the development of the vegetation may be distinguished. Throughout these phases, the climax vegetation did not change substantially in qualitative composition, but a trend towards noticeably less humid conditions probably in combination with a drop of the water level in the lake may be recognized. A shift in algal population from the freshwater dinoflagellate cyst Messelodinium thielepfeifferae to a dominance of Botryococcus in the uppermost part of the core is interpreted as a response to changes in acidity and nutrient availability within the lake. Time series analyses of pollen assemblages show that variations in the Milankovitch range of eccentricity, obliquity and precession can be distinguished. In addition, fluctuations in the sub-Milankovitch range are indicated. This demonstrates that floral changes during steady depositional conditions in the Middle Eocene of Messel were controlled by orbital forcing.	[Lenz, Olaf K.] Tech Univ Darmstadt, Inst Angew Geowissensch, D-64287 Darmstadt, Germany; [Wilde, Volker; Riegel, Walter] Senckenberg Forschungsinstitut & Naturmuseum, Sekt Palaobotan, D-60325 Frankfurt, Germany; [Riegel, Walter] Univ Gottingen, Geowissensch Zentrum, D-37077 Gottingen, Germany	Technical University of Darmstadt; Leibniz Association; Senckenberg Gesellschaft fur Naturforschung (SGN); University of Gottingen	Lenz, OK (通讯作者)，Tech Univ Darmstadt, Inst Angew Geowissensch, Schnittspahnstr 9, D-64287 Darmstadt, Germany.	lenz@geo.tu-darmstadt.de; volker.wilde@senckenberg.de; wriegel@gwdg.de			Deutsche Forschungsgemeinschaft [DFG-Wi 1676/6]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	Our research has been carried out as part of a project financed by the Deutsche Forschungsgemeinschaft under the grant DFG-Wi 1676/6 including the post-doctoral appointment of the first author. This generous support is gratefully acknowledged. The authors also acknowledge the assistance of Dr. M. Felder and Dr. F.-J. Harms in getting access to the core and the lithologic information and the invaluable help of Karin Schmidt and Petra Held in sampling and sample preparation.	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J. Earth Sci.	NOV	2011	100	8					1851	1874		10.1007/s00531-010-0609-z	http://dx.doi.org/10.1007/s00531-010-0609-z			24	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	870EQ		Green Published, hybrid			2025-03-11	WOS:000298652300005
J	Pienkowski, AJ; Mudie, PJ; England, JH; Smith, JN; Furze, MFA				Pienkowski, Anna J.; Mudie, Peta J.; England, John H.; Smith, John N.; Furze, Mark F. A.			Late Holocene environmental conditions in Coronation Gulf, southwestern Canadian Arctic Archipelago: evidence from dinoflagellate cysts, other non-pollen palynomorphs, and pollen	JOURNAL OF QUATERNARY SCIENCE			English	Article						sea-ice; environmental change; Northwest Passage; Little Ice Age; decadal scale	NORTHERNMOST BAFFIN-BAY; RECENT MARINE-SEDIMENTS; SEA-SURFACE CONDITIONS; PALAEOCEANOGRAPHIC CHANGES; SPATIAL-DISTRIBUTION; NORTHWEST PASSAGE; VICTORIA ISLAND; ICE-SHEET; CLIMATE; FORAMINIFERA	Boxcore 99LSSL-001 (68.0958 degrees N, 114.1868 degrees W; 211 m water depth) from Coronation Gulf represents the first decadal-scale marine palynology and late Holocene sediment record for the southwestern part of the Northwest Passage. The record was studied for organic-walled microfossils (dinoflagellate cysts, non-pollen palynomorphs), pollen, terrestrial spores, and sediment characteristics. Pb-210, Cs-137, and three accelerator mass spectrometry C-14 dates constrain the chronology. Three prominent palaeoenvironmental zones were identified. During the interval AD 1470-1680 (Zone I), the climate was warmer and wetter than at present, and environmental conditions were more favourable to biological activity and northward boreal forest migration, with reduced sea-ice and a longer open-water (growing) season. The interval AD 1680-1940 (Zone II) records sea-ice increase, and generally cool, polar conditions during the Little Ice Age. During AD 1940-2000 (Zone III), organic microfossils indicate an extended open-water season and decreased sea-ice, with suggested amelioration surpassing that of Zone I. Although more marine studies are needed to place this record into an appropriate context, the succession from ameliorated (Zone I) to cooler, sea-ice influenced conditions (Zone II) and finally to 20th-century warming (Zone III) corresponds well with several terrestrial climatic records from the neighbouring mainland and Victoria Island, and with lower-resolution marine records to the west. Copyright (C) 2011 John Wiley & Sons, Ltd.	[Pienkowski, Anna J.; England, John H.] Univ Alberta, Dept Earth & Atmospher Sci, Edmonton, AB, Canada; [Mudie, Peta J.] Geol Survey Canada Atlantic, Dartmouth, NS, Canada; [Smith, John N.] Bedford Inst Oceanog, Dept Fisheries & Oceans, Dartmouth, NS, Canada; [Furze, Mark F. A.] Grant MacEwan Univ, Earth & Planetary Sci Div, Dept Phys Sci, Edmonton, AB, Canada	University of Alberta; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography; Fisheries & Oceans Canada	Pienkowski, AJ (通讯作者)，Bangor Univ, Sch Ocean Sci, Menai Bridge, Anglesey, Wales.	a.pienkowski@bangor.ac.uk	Pieńkowski, Anna/AAL-1312-2020; Smith, John/Y-2316-2019; Pienkowski, Anna/J-9339-2013	Furze, Mark/0000-0003-4636-6182; Pienkowski, Anna/0000-0002-3606-7130	NSERC Northern Chair	NSERC Northern Chair	Grateful thanks are extended to Jane Eert (Institute of Ocean Science), for obtaining the boxcore on the Swedish-led Tundra Northwest 99 expedition of the CCGS Louis S. St-Laurent through the Northwest Passage. We also appreciate the help of Owen Brown and William LeBlanc (GSCA) in providing grain size and carbon analyses. PJM acknowledges the technical support of S. Blasco's ArcticNet Geohazards Program, and the GSCA Climate Change Program 1999-2004. AJP thanks C. Schweger and H. Friebe (University of Alberta) for the use of the palynology lab and help with sample processing, as well as O. Catuneanu (University of Alberta) for use of microscope facilities. Funding from the NSERC Northern Chair Program (awarded to JE) enabled radiocarbon dating for this project. We thank Jens Matthiessen and one anonymous reviewer whose comments greatly improved the manuscript. We also thank Antony Long for editorial handling of our manuscript.	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NOV	2011	26	8					839	853		10.1002/jqs.1503	http://dx.doi.org/10.1002/jqs.1503			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	857VY					2025-03-11	WOS:000297752600008
J	Slimani, H; Louwye, S; Dusar, M; Lagrou, D				Slimani, H.; Louwye, S.; Dusar, M.; Lagrou, D.			Connecting the Chalk Group of the Campine Basin to the dinoflagellate cyst biostratigraphy of the Campanian to Danian in borehole Meer (northern Belgium)	NETHERLANDS JOURNAL OF GEOSCIENCES-GEOLOGIE EN MIJNBOUW			English	Article						Upper Cretaceous; Danian; organic-walled dinoflagellate cysts; biostratigraphy; lithostratigraphy; southern North Sea Basin; correlation	CRETACEOUS-TERTIARY BOUNDARY; MAASTRICHTIAN TYPE AREA; STRATIGRAPHY; DEPOSITS; BUNDE	A palynological study of the Chalk Group (Campanian-Danian) in the Meer borehole (northern Belgium), which penetrated the thickest succession known in the Campine Basin, has revealed diverse, well-preserved organic-walled dinoflagellate cyst assemblages. The succession contains numerous chronostratigraphically significant dinocyst events, which are based mainly on the highest consistent occurrences of index species. At least 35 bio-events have enabled a subdivision into nine intervals, at stage or substage level, within the Campanian to Danian interval, as based on comparison with coeval assemblages elsewhere in northwest Europe, inclusive of stratotypes of stages and stage boundaries. Bio-events allow correlation of the section studied with the Campanian Exochosphaeridium? masureae, Areoligera coronata and Samlandia may zones, the Maastrichtian Pervosphaeridium tubuloaculeatum, Deflandrea galeata and Hystrichostrogylon coninckii zones, and the Danian Damassadinium californicum Zone. In addition, a correlation with other zonal schemes for the southern North Sea Basin and with conventional northwest European belemnite zones is presented. Comparisons with Boreal and Tethyan realms confirm that most bio-events may also be useful for interregional and global correlation. The Campanian-Danian dinocyst biostratigraphy of the Meer borehole is put alongside geophysical well logs and an ecozonation, in order to check the validity of lithostratigraphical correlations across the Campine Basin. This first, detailed correlation attempt shows that sensitivities to facies change associated with differences in accommodation space and sediment supply appear to be at the base of slight, yet consistent, shifts between the local lithological succession and the standard lithostratigraphical scheme of the Maastricht type area.	[Slimani, H.] Univ Mohammed V Agdal, Lab Geol & Remote Sensing, Rabat 10106, Morocco; [Louwye, S.] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Dusar, M.] Geol Survey Belgium, Royal Belgian Inst Nat Sci, B-1000 Brussels, Belgium; [Lagrou, D.] Flemish Inst Technol Res VITO, B-2400 Mol, Belgium	Mohammed V University in Rabat; Ghent University; Royal Belgian Institute of Natural Sciences; VITO	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Lab Geol & Remote Sensing, URAC 46,Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Slimani, Hamid/0000-0001-6392-1913	University Mohammed V-Agdal [SVT 11/09]; CNRST [URAC46]	University Mohammed V-Agdal(Mohammed First University of OujdaMohammed V University in Rabat); CNRST	The authors are indebted to Mrs Sabine Van Cauwenberghe (Research Unit Palaeontology, University of Gent, Belgium) for palynological preparation of the samples studied and to the staff of the Earth Science Department (Scientific Institute, University Mohammed V-Agdat, Morocco) for technical support. They thank the University Mohammed V-Agdal (Project SVT 11/09) and CNRST (URAC46) for financial support. The Subcommission on Cretaceous Stratigraphy, headed by Johan Yans (FUNDP Namur), of the Belgian National Commission on Stratigraphy stimulated the discussion of the lithostratigraphical scale and its biostratigraphical significance and in this way initiated the present study. The Natural Resources Service of the Land and Soil protection, Subsoil, Natural Resources Division (ALBON) of the Ministry of the Flemish Community is acknowledged for allowing the mapping of the Cretaceous in Flanders (northern Belgium). The manuscript greatly benefitted from critical and constructive comments by Henk Brinkhuis, Ian Harding and Norbert Keutgen, who are thanked for their co-operation. The present study could not have been possible without the pioneering work of P.J. (Sjeuf) Felder and W.M. Felder. 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J. Geosci.	NOV	2011	90	2-3					129	164						36	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	855LC					2025-03-11	WOS:000297564900006
J	Slimani, H; Louwye, S				Slimani, Hamid; Louwye, Stephen			New dinoflagellate cyst species of the <i>Microdinium</i> and <i>Phanerodinium</i> Complexes (Evitt) from the Upper Cretaceous-Lower Paleogene Chalk Group in the Meer borehole, northern Belgium	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; taxonomy; Campanian-Danian; biostratigraphy; northern Belgium	BIOSTRATIGRAPHY; NETHERLANDS	A high-resolution palynological study of the Campanian to Danian Chalk Group from the Meer borehole in northern Belgium has revealed the presence of four new smaller organic-walled dinoflagellate cyst species previously left in open nomenclature, within rich, diverse and well-preserved assemblages. A formal description of the new species, an emendation of Phanerodinium fourmarieri Lejeune-Carpentier based on a comparison of well preserved specimens with the type material, and as a result a re-assessment of the stratigraphic occurrences of each of these species are provided. Druggidium discretum sp. nov. is characterized by a finely spongeous wall surface and a discreet indication of tabulation, while Druggidium meerensis sp. nov. is suturocavate with a granulate, vermiculate to rarely pseudoreticulate ornamentation. Gillinia denticulate sp. nov. is distinguishable by its high and denticulate crests. Phanerodinium belgicum sp. nov. has a microgranulate to vermiculate surface wall and membranous crests. We retain Phanerodinium fourmarieri in the genus Phanerodinium, and reject the transfer of the species to the genus Druggidium by Lejeune-Carpentier and Sarjeant, as we demonstrate that the ventral surface of the species is untabulated and that the anterior intercalary plates are lacking. Both features are characteristic of every Phanerodinium species. (C) 2011 Elsevier B.V. All rights reserved.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, Rabat 10106, Morocco; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	Mohammed V University in Rabat; Ghent University	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, URAC 46,Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	Slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Slimani, Hamid/0000-0001-6392-1913; Louwye, Stephen/0000-0003-4814-4313	University Mohammed V-Agdal [SVT 11/09]; "Centre National de la Recherche Scientifique et Technique" (CNRST), Morocco [URAC46]	University Mohammed V-Agdal; "Centre National de la Recherche Scientifique et Technique" (CNRST), Morocco(Centre National de la Recherche Scientifique (CNRS))	We thank Michiel Dusar (Geological survey of Belgium) for kindly providing the samples from the studied section of the Meer borehole and Sabine Van Cauwenberghe (Research Unit Palaeontology, University of Gent, Belgium) for the palynological preparation of these samples. This study was carried in the framework of two research projects: SVT 11/09 of the University Mohammed V-Agdal and URAC46 of "Centre National de la Recherche Scientifique et Technique" (CNRST), Morocco. 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Palaeobot. Palynology	NOV	2011	168	1					41	50		10.1016/j.revpalbo.2011.09.009	http://dx.doi.org/10.1016/j.revpalbo.2011.09.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	853VG					2025-03-11	WOS:000297453200005
J	Baula, IU; Azanza, RV; Fukuyo, Y; Siringan, FP				Baula, Iris U.; Azanza, Rhodora V.; Fukuyo, Yasuwo; Siringan, Fernando P.			Dinoflagellate cyst composition, abundance and horizontal distribution in Bolinao, Pangasinan, Northern Philippines	HARMFUL ALGAE			English	Article						Dinoflagellate cyst; Northern Philippines; Harmful microalgae; Alexandrium minutum; Mariculture	ALEXANDRIUM-MINUTUM; SURFACE SEDIMENTS; PROTOCERATIUM-RETICULATUM; LINGULODINIUM-POLYEDRUM; RESTING CYSTS; WEST-COAST; MANILA BAY; TOKYO-BAY; HARBOR; BLOOM	This paper constitutes the first cyst record of a eutrophic tropical mariculture area with harmful algal blooms since 2002 and provides contribution to the global record on dinoflagellate cysts, specifically from Northern part of Southeast Asia. Surface sediment samples from 54 stations in October 2006 and 5 stations from 2004 to 2006 Bolinao, Pangasinan were processed palynologically and by fluorescent techniques. Exploratory data analysis using Two-Way Indicator Species Analysis (TWINSPAN) to identify major patterns of distribution and Canonical Correspondence Analysis (CCA) ordinated stations and species along sediment and environmental variables have been done to determine spatial variations in community structure. Thirty-six cyst types have been identified which include the toxic species, Alexandrium minutum. Species richness and diversity correlated with silt, mud, carbonates and depth but have been observed to be generally low in the area (p < 0.05). Multivariate analysis shows that sediment grain size, nutrients and water depth are important variables related to cyst distribution. Two accumulation points that can be source and sinks of blooms have been identified. The decrease in species richness and diversity of dinoflagellate cysts from 2005 to 2006 has been attributed to intensive mussel farming. Heterotrophs have dominated during the northeast and southwest monsoon seasons while autotrophs which included A. minutum, have dominated during tradewinds. Results indicate that the cysts accumulation points could possibly seed blooms particularly during the tradewinds season and thus should be monitored effectively to prevent negative public health impacts. (C) 2011 Elsevier B.V. All rights reserved.	[Baula, Iris U.; Azanza, Rhodora V.; Siringan, Fernando P.] Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines; [Baula, Iris U.] Natl Univ Singapore, Trop Marine Sci Inst, Singapore 119227, Singapore; [Fukuyo, Yasuwo] Univ Tokyo, Asian Nat Environm Sci Ctr, Bunkyo Ku, Tokyo 1138657, Japan	University of the Philippines System; University of the Philippines Diliman; National University of Singapore; University of Tokyo	Baula, IU (通讯作者)，Univ Philippines, Inst Marine Sci, Quezon City 1101, Philippines.	irisbaula@gmail.com	Azanza, Rhodora/HGU-5811-2022		Department of Science and Technology - Philippine Council for Aquatic and Marine Research and Development (DOST-PCAMRD); Commission on Higher Education (CHED), University of the Philippines (UP); Japan Society for the Promotion of Science - Ocean Research Institute	Department of Science and Technology - Philippine Council for Aquatic and Marine Research and Development (DOST-PCAMRD)(Department of Science & Technology (DOST), Philippines); Commission on Higher Education (CHED), University of the Philippines (UP)(Commission on Higher Education (CHED), Philippines); Japan Society for the Promotion of Science - Ocean Research Institute	The authors would like to thank the Department of Science and Technology - Philippine Council for Aquatic and Marine Research and Development (DOST-PCAMRD), Commission on Higher Education (CHED), University of the Philippines (UP) and "Dinoflagellate Cyst Mapping" Training Through Research Project of Japan Society for the Promotion of Science - Ocean Research Institute Harmful Algal Bloom Program (JSPS ORI HAB). 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L, 1996, HARMFUL TOXIC ALGAL, P189; Villanoy CL, 2006, HARMFUL ALGAE, V5, P156, DOI 10.1016/j.hal.2005.07.001; WALL D, 1977, MAR MICROPALEONTOL, V2, P121, DOI 10.1016/0377-8398(77)90008-1; Wang ZH, 2004, PHYCOL RES, V52, P387, DOI 10.1111/j.1440-183.2004.00356.x; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1; Yap LG, 2004, MAR POLLUT BULL, V49, P819, DOI 10.1016/j.marpolbul.2004.06.030; Yentsch C.M., 1979, P127; Yoshida M, 2000, FISHERIES SCI, V66, P177, DOI 10.1046/j.1444-2906.2000.00029.x	63	28	33	0	24	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	NOV	2011	11						33	44		10.1016/j.hal.2011.07.002	http://dx.doi.org/10.1016/j.hal.2011.07.002			12	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	859JL					2025-03-11	WOS:000297872600004
J	Horner, RA; Greengrove, CL; Davies-Vollum, KS; Gawel, JE; Postel, JR; Cox, AM				Horner, R. A.; Greengrove, C. L.; Davies-Vollum, K. S.; Gawel, J. E.; Postel, J. R.; Cox, A. M.			Spatial distribution of benthic cysts of <i>Alexandrium catenella</i> in surface sediments of Puget Sound, Washington, USA	HARMFUL ALGAE			English	Article						Alexandrium; Dinoflagellate cysts; Harmful algae; Sediments	RESTING CYSTS; DINOFLAGELLATE CYSTS; FUNDYENSE POPULATIONS; GULF; DINOPHYCEAE; ACCUMULATION; CIRCULATION; ENCYSTMENT; DYNAMICS; GEORGIA	Alexandrium catenella cyst distribution and abundance in the surface sediments throughout Puget Sound, Washington, were mapped for the first time in 2005. Cyst density varied from 0 to >12,000 cysts cm(-3) surface sediment, with Quartermaster Harbor having the highest concentration of cysts. A higher resolution 2006 spatial survey of surface sediment cysts in two central Puget Sound bays, Quartermaster Harbor and Dyes Inlet, found cyst distribution to be patchy. Surface sediment properties were also determined for all samples. Given the diverse hydrographic conditions associated with the different basins in Puget Sound, no correlation was found between cyst abundance and grain size or total organic content (TOC) for the large scale Puget Sound wide survey, but cyst abundance was positively correlated with finer grained and higher TOC sediments within bays from the higher resolution survey. Sediment metal concentrations were also determined and cyst abundance was positively correlated only with Cd concentration. These results are consistent with previous studies in other locations. (C) 2011 Elsevier B.V. All rights reserved.	[Horner, R. A.; Postel, J. R.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Greengrove, C. L.; Davies-Vollum, K. S.; Gawel, J. E.] Univ Washington, Environm Sci IAS, Tacoma, WA 98402 USA; [Cox, A. M.] SW Fisheries Sci Ctr, La Jolla, CA 92037 USA	University of Washington; University of Washington Seattle; University of Washington; University of Washington Tacoma; National Oceanic Atmospheric Admin (NOAA) - USA	Horner, RA (通讯作者)，Univ Washington, Sch Oceanog, Box 357940, Seattle, WA 98195 USA.	rita@ocean.washington.edu		Gawel, James/0000-0002-1595-3678	National Oceanic and Atmospheric Administration [NA04NOS4780273]	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA)	This paper is a result of research funded by the National Oceanic and Atmospheric Administration Coastal Ocean Program under award #NA04NOS4780273 to the University of Washington. It is ECOHAB contribution # 619. We thank R. McQuin and N. Milonas, the crew of the R/V Barnes for logistical support during the cruises, M. Holmes for allowing us to participate in student cruises on the R/V Thompson and showing us how to use the piston corer, D. Shull for advice on cyst counting and <SUP>210</SUP>Pb analyses, C. Nittrouer for the use of his lab to run the <SUP>210</SUP>Pb analyses, J. Coyle for help with the maps, and UW Tacoma undergraduate students Kyle Sorensen, Simone Hoffer, Jeff Hubert, Jonathan Neville, Katherine Tran, Alex Abrahamson, Suzanne Wagner and Bruce Hazen for help with sampling during the cruises and running laboratory analyses. F. Cox and J. Borchert of the Washington Department of Health kindly provided the shellfish toxin data. 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J	Gu, HF				Gu, Haifeng			Morphology, phylogenetic position, and ecophysiology of <i>Alexandrium ostenfeldii</i> (Dinophyceae) from the Bohai Sea, China	JOURNAL OF SYSTEMATICS AND EVOLUTION			English	Article						Alexandrium ostenfeldii; Bohai Sea; China; cyst; growth; toxicity	RESTING CYSTS; DINOFLAGELLATE; GERMINATION; EXCYSTMENT; BLOOM; ENCYSTMENT; TAMARENSE; TOXICITY; TOXIN; LIGHT	Alexandrium ostenfeldii is a potentially toxic dinoflagellate that often occurs in coastal areas at high latitudes. Here we report the presence of A. ostenfeldii in the Bohai Sea, China, for the first time. The vegetative cells of A. ostenfeldii are characterized by a narrow first apical plate and a large ventral pore located on the anterior right side. Partial large subunit sequence comparison revealed that the Chinese strain differs from the Finnish strains at only three positions, and from A. peruvianum of Spain at five positions. Maximum parsimony analysis revealed that A. ostenfeldii from China and Finland and A. peruvianum from Spain grouped together. They were the nearest sister group to a clade with A. ostenfeldii from New Zealand, Europe, and North America. In culture, growth did not occur at temperatures below 9 degrees C and occurred at salinities between 7 and 27 psu. It took 10-20 days for newly formed cysts to mature at 20 degrees C. Lower temperature delayed germination, but the germination rate exceeded 90% at temperatures from 12 to 24 degrees C. No germination occurred below 9 degrees C after 1 month of incubation. The Chinese strain of A. ostenfeldii produced neither spirolides nor paralytic shellfish poisoning toxins.	State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources	Gu, HF (通讯作者)，State Ocean Adm, Inst Oceanog 3, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	Gu, Haifeng/ADN-4528-2022	Gu, Haifeng/0000-0002-2350-9171	National Scientific-Basic Special Fund [2009FY210400]; Public Science and Technology Research Funds Projects of Ocean [200905004-3]	National Scientific-Basic Special Fund; Public Science and Technology Research Funds Projects of Ocean	I thank Dr. Katrin ERLER at the University of Jena (Jena, Germany) for the spirolide shellfish toxin analysis, Dr. Na WANG at Xiamen University for the PSP toxin analysis, and Dr. Anke KREMP for critically reading the manuscript. I am indebted to two anonymous reviewers for constructive suggestions to improve the manuscript. This project was supported by the National Scientific-Basic Special Fund (Grant No. 2009FY210400) and the Public Science and Technology Research Funds Projects of Ocean (Grant No. 200905004-3).	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J	Calado, AJ				Calado, Antonio Jose			On the identity of the freshwater dinoflagellate <i>Glenodinium edax</i>, with a discussion on the genera <i>Tyrannodinium</i> and <i>Katodinium</i>, and the description of <i>Opisthoaulax</i> gen. nov.	PHYCOLOGIA			English	Article						Dinophyceae; Freshwater; Glenodinium edax; Katodinium; Opisthoaulax gen. nov.; Taxonomy; Tyrannodinium	AMPHIDINIUM DINOPHYCEAE; FLAGELLAR APPARATUS; LAKE TOVEL; ULTRASTRUCTURE; PHYLOGENY	Within the context of the preparation of a flora for the identification of freshwater dinoflagellates, the identity of Glenodinium edax and the affinities of a group of phagotrophic species with a conspicuous eyespot not associated with plastids (eyespot type C) currently classified in Katodinium were re-evaluated. The original description and illustrations of the phagotrophic G. edax suggest affinity with the Pfiesteriaceae. Whereas the tabulation currently associated with G. edax is based on a probable misidentification, the similarity to Tyrannodinium berolinense suggests that the two names can be regarded as synonyms and T. edax comb. nov. is proposed. As presented in modern floras, Katodinium is artificially defined on the basis of the position of the cingulum at or below the posterior third of the cell, and includes widely different forms. The presence of an eyespot of type C in the phagotrophic Katodinium vorticella and related species combines with a general cell morphology reminiscent of Esoptrodinium gemma and the formation of Tovellia-like cysts to mark this group of species as belonging to the Tovelliaceae. The type species of Katodinium, K. nieuportense, is morphologically quite different from these species and does not display tovelliacean characters. None of the known genera of Tovelliaceae matches the characters of K. vorticella and its close relatives. Opisthoaulax gen. nov. is described and new combinations are proposed for K. vorticella and six other species.	[Calado, Antonio Jose] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Calado, Antonio Jose] Univ Aveiro, GeoBioTec Res Unit, P-3810193 Aveiro, Portugal	Universidade de Aveiro; Universidade de Aveiro	Calado, AJ (通讯作者)，Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal.	acalado@ua.pt	Calado, Antonio Jose/D-6263-2015	Calado, Antonio Jose/0000-0002-9711-0593				[Anonymous], REGNUM VEG; BOURRELLY P, 1968, Protistologica, V4, P5; Calado AJ, 1997, PHYCOLOGIA, V36, P47, DOI 10.2216/i0031-8884-36-1-47.1; Calado AJ, 2006, J PHYCOL, V42, P434, DOI 10.1111/j.1529-8817.2006.00195.x; Calado AJ, 2005, PHYCOLOGIA, V44, P112, DOI 10.2216/0031-8884(2005)44[112:OTFDPI]2.0.CO;2; Calado AJ, 1998, J PHYCOL, V34, P536, DOI 10.1046/j.1529-8817.1998.340536.x; Calado AJ, 2009, J PHYCOL, V45, P1195, DOI 10.1111/j.1529-8817.2009.00735.x; Christen H. 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Math., V1915, P260	57	25	28	1	17	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0031-8884	2330-2968		PHYCOLOGIA	Phycologia	NOV	2011	50	6					641	649		10.2216/11-21.1	http://dx.doi.org/10.2216/11-21.1			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	850OJ					2025-03-11	WOS:000297204700008
J	Boere, AC; Damsté, JSS; Rijpstra, WIC; Volkman, JK; Coolen, MJL				Boere, Arjan C.; Damste, Jaap S. Sinninghe; Rijpstra, W. Irene C.; Volkman, John K.; Coolen, Marco J. L.			Source-specific variability in post-depositional DNA preservation with potential implications for DNA based paleoecological records	ORGANIC GEOCHEMISTRY			English	Article							GREEN SULFUR BACTERIA; EXTRACELLULAR DNA; ELLIS FJORD; PLASMID DNA; BLACK-SEA; POLARELLA-GLACIALIS; COMMUNITY PATTERNS; DEGRADATION RATES; EARLY DIAGENESIS; VESTFOLD HILLS	Recent studies have shown that genotyping preserved plankton DNA in marine and lacustrine sediment records using ancient DNA methods is a promising approach for refining paleoenvironmental information. However, the extent to which the preservation of fossil plankton DNA differs between species is poorly understood. Using a continuous 2700 year sediment record from Watts Basin in Ellis Fjord (Antarctica), we compared the level of preservation of fossil DNA derived from important plankton members with varying cellular architecture. The amount of preserved small subunit ribosomal DNA (SSU rDNA; ca. 500 base pair fragments) of dinoflagellates (as extracellular DNA rather than as preserved cysts) that could be amplified by way of PCR declined up to five orders of magnitude with increasing sediment depth and age. In contrast, the amount of similar-sized, PCR-amplifiable, diatom SSU rDNA (predominantly from a cyst-forming Chaetoceros sp.) declined only up to tenfold over 2700 years of deposition. No obvious decline in copy numbers with increasing sediment age was observed for similar-sized SSU rDNA of past chemocline-associated photosynthetic green sulfur bacteria (GSB), which do not have a protective resting stage. In good agreement with the quantitative data, the extent of post-depositional natural degradation to fragments too small to serve as a template for the quantitative PCR assays was greatest for dinoflagellates and lowest for GSB. An increase in the ratio between GSB-derived DNA and intact carotenoids with sediment depth implies that short GSB DNA fragments were better preserved than intact carotenoids and provide a more accurate view into paleoproductivity and the sediment flux of GSB in Watts Basin. We discuss the possible causes behind the variation in the level of DNA preservation among the plankton groups investigated, as well as consequences for the use of using fossil DNA records in paleoecology studies. Published by Elsevier Ltd.	[Boere, Arjan C.; Damste, Jaap S. Sinninghe; Rijpstra, W. Irene C.; Coolen, Marco J. L.] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, NL-1790 AB Den Burg, Netherlands; [Volkman, John K.] CSIRO Marine & Atmospher Res & Wealth Oceans Flag, Hobart, Tas 7001, Australia	Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Commonwealth Scientific & Industrial Research Organisation (CSIRO)	Coolen, MJL (通讯作者)，Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA.	mcoolen@whoi.edu	Volkman, John/A-6592-2008; Sinninghe Damste, Jaap/F-6128-2011; Coolen, Marco/B-8263-2015	Sinninghe Damste, Jaap/0000-0002-8683-1854; Coolen, Marco/0000-0002-0417-920X	Australian Antarctic Science Advisory Committee (ASAC) [1166]; Netherlands Organization for Scientific Research (NWO) [851.20.020, 851.20.006]; NSF-OCE [0825020]; Directorate For Geosciences; Division Of Ocean Sciences [0825020] Funding Source: National Science Foundation	Australian Antarctic Science Advisory Committee (ASAC); Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); NSF-OCE(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO)); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We thank C. Wuchter, P. Thompson and crew of the Australian Antarctic Division for assistance during sampling, and F. Sangiorgi and an anonymous reviewer for useful comments. Funding for the collection of sediment and water samples (by M.J.L.C. and C.W.) was provided by the Australian Antarctic Science Advisory Committee (ASAC Grant 1166 to J.K.V.). The work was further supported by grants from the Netherlands Organization for Scientific Research (NWO; Netherlands Antarctic Research Proposals 851.20.020 to M.J.L.C. and 851.20.006 to J.S.S.D), as well as NSF-OCE Grant 0825020 to M.J.L.C.	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Geochem.	NOV	2011	42	10					1216	1225		10.1016/j.orggeochem.2011.08.005	http://dx.doi.org/10.1016/j.orggeochem.2011.08.005			10	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	860CT					2025-03-11	WOS:000297926100006
J	Lundholm, N; Ribeiro, S; Andersen, TJ; Koch, T; Godhe, A; Ekelund, F; Ellegaard, M				Lundholm, Nina; Ribeiro, Sofia; Andersen, Thorbjorn J.; Koch, Trine; Godhe, Anna; Ekelund, Flemming; Ellegaard, Marianne			Buried alive - germination of up to a century-old marine protist resting stages	PHYCOLOGIA			English	Article							LIVING DINOFLAGELLATE CYSTS; KOLJO-FJORD; VERTICAL-DISTRIBUTION; SCRIPPSIELLA-HANGOEI; ALEXANDRIUM SPP.; DINOPHYCEAE; EXCYSTMENT; ENCYSTMENT; SEDIMENTS; DIATOM	We report on the survival and germination of up to a century-old marine protist resting stages naturally preserved in sediments from Koljo Fjord on the west coast of Sweden. This work has focused on germination of dinoflagellate cysts, but diatom resting stages were also observed. We record the longest known survival of dormant dinoflagellate cells. We individually isolated more than 1200 cysts of the three most abundant dinoflagellate taxa: Pentapharsodinium dalei, Lingulodinium polyedrum and Scrippsiella spp. Germination success decreased with core depth, and all successful germinations took place within the first 2 wk of incubation. Pentapharsodinium dalei had the highest germination success rate, with a maximum of up to 80% in 28-yr-old sediment, and could successfully germinate from core sediments dated to 1920 +/- 12. Scrippsiella spp. cysts with cell contents occurred down to c. 90-yr-old sediment and could germinate from down to ca. 40-yr-old sediments, with a maximum germination rate of 50-60% in recent sediments. Cysts of L. polyedrum germinated frequently down to 20 yr and rarely to c. 80 yr, with a maximum of 20-50% germination success in recent sediments. Cyst isolation under cooled conditions rather than at room temperature resulted in a significantly higher germination success in P. dalei, while no effect was observed for L. polyedrum. The time elapsed since slicing of the core affected survival of L. polyedrum cysts negatively, most likely due to the effect of oxygen. The long-term survival potential of benthic resting stages that we report here has important implications, as viable resting stages accumulated in bottom sediments can be transported back to the water column by, for example, bioturbation and human-mediated sediment dredging. Hence, the sediment may to a higher degree than previously considered play a role as seed bank. This is important in a changing climate and might have particularly severe impacts in the case of harmful species.	[Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, DK-1307 Copenhagen K, Denmark; [Ribeiro, Sofia; Koch, Trine; Ellegaard, Marianne] Univ Copenhagen, Dept Biol, Marine Biol Sect, DK-1353 Copenhagen K, Denmark; [Andersen, Thorbjorn J.] Univ Copenhagen, Dept Geog & Geol, DK-1350 Copenhagen K, Denmark; [Godhe, Anna] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden; [Ekelund, Flemming] Univ Copenhagen, Dept Biol, Sect Terr Ecol, DK-1353 Copenhagen K, Denmark	University of Copenhagen; University of Copenhagen; University of Copenhagen; University of Gothenburg; University of Copenhagen	Lundholm, N (通讯作者)，Univ Copenhagen, Nat Hist Museum Denmark, Solvgade 83S, DK-1307 Copenhagen K, Denmark.	nlundholm@snm.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Ekelund, Flemming/M-1731-2014; Lundholm, Nina/AAY-6249-2020; Ellegaard, Marianne/H-6748-2014; Lundholm, Nina/A-4856-2013; Ribeiro, Sofia/G-9213-2018; Andersen, Thorbjorn Joest/N-7560-2014	Ellegaard, Marianne/0000-0002-6032-3376; Lundholm, Nina/0000-0002-2035-1997; Ribeiro, Sofia/0000-0003-0672-9161; Andersen, Thorbjorn Joest/0000-0001-5032-9945	Portuguese Foundation for Science and Technology [SFRH/BD/30847/2006]; Danish Research Council [2111-04-0011]; Fundação para a Ciência e a Tecnologia [SFRH/BD/30847/2006] Funding Source: FCT	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); Danish Research Council(Det Frie Forskningsrad (DFF)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	We thank Jens Sogaard, Dennis Moller and Aage Vestergaard, Hvidovre Hospital, Rontgen Dep., for X-raying the cores, and Jeanet Iversen, Jon Sommer Nagel and Anne Eskildsen for help with the experiments. Goteborg University Marine Research Centre is thanked for sponsoring fieldwork in Koljo Fjord (grant to A.G.). S.R. was supported by a PhD grant from the Portuguese Foundation for Science and Technology (SFRH/BD/30847/2006). This study was part of Danish Research Council project 2111-04-0011.	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J	Hopson, P				Hopson, Peter			The geological history of the Isle of Wight: an overview of the 'diamond in Britain's geological crown'	PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION			English	Article						Isle of Wight; Geological history; Landscape development; Lithostratigraphy; Deep geology; Structure; Jurassic; Cretaceous; Palaeogene; Quaternary	ANGLO-PARIS BASIN; DINOFLAGELLATE CYST BIOSTRATIGRAPHY; FORMATION WEALDEN GROUP; SOUTHERN ENGLAND; SEA-LEVEL; SEISMIC EXPRESSION; HAMPSHIRE BASIN; ENGLISH CHALK; WESSEX BASIN; INVERSION	The geology of the Isle of Wight has attracted-both the amateur and professional geologist alike for well over two centuries. It presents a cornucopia of things geological and offers a window into the fascinating story of the geological history and landscape development of southern England, as well as an important teaching resource for all levels of study from primary education through to academic research. This paper provides a geological framework and a summary of the history of research as context for the papers in this issue. Inevitably, it can only offer a precis of the huge amount of information available, but it is hoped will also give added impetus to further investigation of the literature or, indeed, new research. The island offers a field workshop for topics such as lithostratigraphy, sequence stratigraphy, tectonics and climate change; studies that are becoming ever more international in their influence. There are 15 Sites of Special Scientific Interest designated because of their geological importance and a number of these are internationally significant. After a brief discussion on the concealed geology, this paper concentrates on an outline of the near-surface geology on the coast and inland, and introduces a different view on the structure of the Cretaceous and Palaeogene strata. The enigmatic Quaternary deposits are discussed particularly with reference to the development of the Solent River, human occupation and climate change. (C) 2011 Natural Environment Research Council. Published by Elsevier Ltd on behalf of The Geologists' Association. All rights reserved.	British Geol Survey, Sir Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Hopson, P (通讯作者)，British Geol Survey, Sir Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	pmhop@bgs.ac.uk			NERC [bgs05001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], QUATERNARY W GRAMPIA; [Anonymous], 1996, ENGLISH PALAEOLITHIC; [Anonymous], 2006, The Geology of England and Wales; [Anonymous], 1904, MEMOIR GEOLOGICAL SU; [Anonymous], GUIDE NATURAL HIST I; [Anonymous], TERTIARY RES; Antoine P, 2003, J QUATERNARY SCI, V18, P227, DOI 10.1002/jqs.762; BARNARD T, 1948, P GEOLOGISTS ASS, V59, P229; Bates M.R., 2009, QUATERNARY SOLENT BA; Beamish D, 2011, P GEOLOGIST ASSOC, V122, P800, DOI 10.1016/j.pgeola.2010.12.004; Beamish D, 2011, P GEOLOGIST ASSOC, V122, P787, DOI 10.1016/j.pgeola.2010.12.003; BLAKE JF, 1892, P GEOLOGISTS ASS, V12, P145; Booth KA, 2011, P GEOLOGIST ASSOC, V122, P938, DOI 10.1016/j.pgeola.2011.01.004; BRANNON G, 1848, PICTURES ISLE WIGHT; BRANNON G, 1848, VECTIS SCENERY BEING; Briant RM, 2006, J QUATERNARY SCI, V21, P507, DOI 10.1002/jqs.1035; Bridgland D, 2004, J QUATERNARY SCI, V19, P203, DOI 10.1002/jqs.819; Bridgland D.R., 1995, The Quaternary of Lower Reaches of the Thames, P35; Bridgland D.R., 1994, QUATERNARY THAMES; Bridgland DR, 2010, J QUATERNARY SCI, V25, P433, DOI 10.1002/jqs.1383; BRIDGLAND DR, 2001, PALAEOLITHIC ARCHAEO, P16; Bristow C. 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Geol. Assoc.	NOV	2011	122	5			SI		745	763		10.1016/j.pgeola.2011.09.007	http://dx.doi.org/10.1016/j.pgeola.2011.09.007			19	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	867MX		Green Accepted			2025-03-11	WOS:000298459600001
J	Wilkinson, IP				Wilkinson, Ian P.			Pithonellid blooms in the Chalk of the Isle of Wight and their biostratigraphical potential	PROCEEDINGS OF THE GEOLOGISTS ASSOCIATION			English	Article						Pithonellids; Late Cretaceous; Stratigraphy; Isle of Wight	CALCAREOUS DINOFLAGELLATE CYSTS; PALEOECOLOGY; STRATIGRAPHY	Five pithonellid blooms recognised in the Chalk Group of the Isle of Wight are correlated via foraminiferal biostratigraphy to regional and global events. Blooms were recognised in the Holywell Nodular Chalk to basal New Pit Chalk formations (foraminiferal zones BGS7 to BGS9); M. guerangeri to Mytiloides standard (macrofaunal zones); middle Lewes Chalk (questionably foraminifera Zone BGS12; S. plena standard macrofaunal Zone); basal Seaford Chalk (BGS14: base M. coranguinum standard macrofaunal Zone); lower Newhaven Chalk (base BGS18; base U. socialis standard macrofaunal Zone); and uppermost Newhaven to basal Culver formations (BGS19-20; O. pilula to low G. quadrata standard macrofaunal zones). The blooms appear to be coeval with oceanographic change and the general trend towards an increase in the proportion of planktonic taxa may suggest upwelling and/or dysaerobic bottom waters. (C) 2011 Published by Elsevier Ltd on behalf of The Geologists' Association.	British Geol Survey, Nottingham NG12 5GG, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Wilkinson, IP (通讯作者)，British Geol Survey, Nottingham NG12 5GG, England.	ipw@bgs.ac.uk			NERC [bgs05001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		ADAMS T. D., 1967, MICROPALEONTOLOGY [NEW YORK, V13, P55, DOI 10.2307/1484805; Aguilera-Franco Noemi, 2003, Revista Mexicana de Ciencias Geologicas, V20, P202; BANNER F T, 1972, Micropaleontology (New York), V18, P278, DOI 10.2307/1485008; BEIN A, 1976, Micropaleontology (New York), V22, P83, DOI 10.2307/1485322; Bertle RJ, 2005, CRETACEOUS RES, V26, P882, DOI 10.1016/j.cretres.2005.06.001; Bignot G., 1964, Revue de Micropaleontologie, V7, P138; BISHOP BA, 1972, J SEDIMENT PETROL, V42, P270; COLOM GUILLERMO, 1955, MICROPALEONTOLOGY, V1, P109, DOI 10.2307/1484163; CURRY D, 1975, PHILOS T R SOC A, V279, P155, DOI 10.1098/rsta.1975.0048; Dias-Brito D, 2000, CRETACEOUS RES, V21, P315, DOI 10.1006/cres.2000.0196; Dufaure Ph., 1959, Revue de Micropaleontologie, V2, P99; FENSOME R. A., 1993, MICROPALEONTOLOGY SP, V7; Futterer D., 1976, Neues Jb Geol Paleont Abh, V151, P119; Futterer D.K., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P533; Gale AS, 2000, J GEOL SOC LONDON, V157, P745, DOI 10.1144/jgs.157.4.745; Hart M.B., 2005, Journal of Iberian Geology, V31, P311; HART MB, 1991, PROC USSHER, V7, P413; JARVIS I, 1988, Cretaceous Research, V9, P3, DOI 10.1016/0195-6671(88)90003-1; Kaufmann FJ, 1865, URWELT SCHWEIZ, P194; Kennedy W. J., 1969, Proceedings of the Geological Association, V80, P459; Kennedy W.J., 1987, B CTR RECHERCHE ELF, V11, P91; Keupp H., 1987, Facies, V16, P37, DOI 10.1007/BF02536748; MARSZALEK DS, 1975, J SEDIMENT PETROL, V45, P266; MASTERS B A, 1978, Micropaleontology (New York), V24, P210, DOI 10.2307/1485249; Mortimore R.N., 2001, CONSERVATION REV SER, V23; Niebuhr B, 2005, GEOL MAG, V142, P31, DOI 10.1017/S0016756804009999; Oakman C.D., 1998, PETROLEUM GEOLOGY N, P294; Olszewska-Nejbert D, 2004, GEOL Q, V48, P159; PFLAUMANN U, 1978, INITIAL REPORTS DEEP, V41, P817; Robaszynski F, 2005, CRETACEOUS RES, V26, P157, DOI 10.1016/j.cretres.2004.10.003; Robaszynski Francis, 1993, Revue de Paleobiologie, V12, P351; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Tappan H., 1980, PALAEOBIOLOGY PLANT; Tew B. H., 2000, Gulf Coast Association of Geological Societies Transactions, V50, P157; Thomas H. D., 1932, J PALEONTOL, V6, P100; Villain J.-M., 1977, PALAEONTOGR ABT A, V159, P139; Villain J.-M., 1981, CRETACEOUS RES, V2, P435; Vogler J., 1941, PALAEONTOGRAPHICA, V4, P246; Wendler J, 2002, GEOL SOC AM SPEC PAP, V356, P265; Wendler J, 2002, CRETACEOUS RES, V23, P213, DOI 10.1006/cres.2002.0311; Willems H., 1992, Zeitschrift fuer Geologische Wissenschaften, V20, P155	41	11	11	0	1	ELSEVIER SCI LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, OXON, ENGLAND	0016-7878			P GEOLOGIST ASSOC	Proc. Geol. Assoc.	NOV	2011	122	5			SI		862	867		10.1016/j.pgeola.2011.09.001	http://dx.doi.org/10.1016/j.pgeola.2011.09.001			6	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	867MX		Green Accepted			2025-03-11	WOS:000298459600011
J	Silva, MSD; Anil, AC; D'Costa, PM				Silva, Maria Shamina D'; Anil, Arga Chandrashekar; D'Costa, Priya Mallika			An overview of dinoflagellate cysts in recent sediments along the west coast of India	INDIAN JOURNAL OF GEO-MARINE SCIENCES			English	Article						dinoflagellate cysts; heterotrophic; harmful; sediment texture; west coast of India	HARMFUL ALGAL BLOOMS; RECENT MARINE-SEDIMENTS; POPULATION-DYNAMICS; TOKYO-BAY; EUTROPHICATION; PHYTOPLANKTON; ENVIRONMENT; SCRIPPSIELLA; VARIABILITY; DINOPHYCEAE	Distribution and abundance of dinoflagellate cysts in recent sediments along the west coast of India (26 coastal stations and 3 ports) is presented. A total of 47 different types of cysts and a maximum abundance of 1076 cysts g(-1) dry sediment were recorded. Highest cyst abundance was recorded at coastal station Mangalore (801 cysts g dry sediment) and Kochi port (1076 cysts g-1 dry sediment). Lowest cyst abundance was observed at coastal stations from Kochi to Trivandrum. This difference may be attributed to the composition of sediment, since sandy stations had lower abundance and diversity of cysts. Heterotrophic dinoflagellate cysts, mainly Protoperidinium species, were the most diversified, predominating at most of the stations sampled. Cysts of potential Harmtul Algal Bloom (HAB) species capable of forming blooms were also detected in the sediment. Effect of the environmental settings of the study area such as upwelling, South West monsoon and anthropogenic pressures on the dynamics of these HAB species in Indian waters needs to be elucidated.	[Silva, Maria Shamina D'; Anil, Arga Chandrashekar; D'Costa, Priya Mallika] CSIR, 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)，CSIR, Natl Inst Oceanog, Panaji 403004, Goa, India.	acanil@nio.org			National Institute of Oceanography; Directorate General of Shipping, Government of India; Council of Scientific and Industrial Research (CSIR)	National Institute of Oceanography; Directorate General of Shipping, Government of India(Ministry of Shipping, Government of IndiaDirectorate General of Shipping (DGS), Government of India); Council of Scientific and Industrial Research (CSIR)(Council of Scientific & Industrial Research (CSIR) - India)	Authours are grateful to Dr. S. R. Shetye, Director, National Institute of Oceanography for his support and encouragement. We acknowledge Dr. Fukuyo and his team for help in identifying some of the 14 dinoflagellate cysts. Present was study carried out as part of Ballast Water Management Programme, India and funded by the Directorate General of Shipping, Government of India. M.S.D and P.M.D. acknowledges the Council of Scientific and Industrial Research (CSIR) for providing Senior Research Fellowship (SRF). This is a NIO contribution (5059).	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Geo-Mar. Sci.	OCT	2011	40	5					697	709						13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	868LW					2025-03-11	WOS:000298525800014
J	Msaky, ES				Msaky, Emma Samwel			Middle Jurassic - earliest Late Cretaceous palynofloras, coastal Tanzania Part Two	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			English	Article						Coastal Tanzania; dinoflagellate cysts; spores; pollen grains; systematics; biostratigraphy; palynofacies; Jurassic; Cretaceous	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; ELATER-BEARING POLLEN; BAYU-UNDAN FIELD; SEQUENCE STRATIGRAPHY; TIMOR SEA; SOUTHERN ALPS; PALYNOLOGY; STRATA; ASSEMBLAGES; PALEOENVIRONMENTS	This Part Two of the current monograph (MSAKY 2011) completes the systematic palaeontology and discusses the biostratigraphic and palaeogeographic significance of the palynofloras together with the results of palynofacies analyses. In the systematic section, two new species are established: Pseudoceratium redactum and Sentusidinium tanzaniensis. Six informal, stratigraphically successive, dinoflagellate assemblages are distinguished, as follows: Assemblage I (Bajocian-Bathonian); Assemblage II (Callovian); Assemblage III (Oxfordian); Assemblage IV (Kimmeridgian-Tithonian); Assemblage V (Berriasian-Barremian); and Assemblage VI (Aptian-Cenomanian). Coastal Tanzania appears referable to the Austral dinoflagellate realm due to the presence of, inter alia, Browned ramosa, Komewuia glabra, Wanaea clathrata, and Wanaea digitata. Some minor biostratigraphic anomalies are noted, including the introduction of Glossodinium dimorphum; this is datable as early Oxfordian in Tanzania whereas in Australasia the species appears earlier (in the Callovian). A few noteworthy quantitative phenomena are evident; for instance, the abundance of Lithodinia jurassica in the vicinity of the Callovian Oxfordian boundary and the marked increase of Wanaea spp. in the Oxfordian, specifically in the Ruvu Basin of the northern coastal belt. These events are of chronostratigraphic significance and could be applicable to regional correlation. Middle Late Jurassic assemblages show a conspicuous degree of cosmopolitanism, and include some species previously considered to be restricted to certain regions in the low and high latitudes. The Early Cretaceous (Berriasian-Barremian) assemblages show close affinity to the Tethyan Realm. The latest Early Cretaceous (Albian) to earliest Late Cretaceous (Cenomanian) strata are allied to the Albian Cenomanian Elaterates province. The presence of claret-bearing pollen in offshore and onshore sections of Tanzania indicates that the Elaterates had a wider geographic distribution than previously reported: i.e., extending beyond the northern part of the African and South American continents. The lower part of the Kipatimu Formation, which contains Assemblage IV, yielded Komewuia glabra, Broomea ramosa, and Rigaudella aemula and their presence precludes the Early Cretaceous age previously ascribed to this part of the formation. Likewise the Makonde and Mikindani Beds have yielded typically Early Cretaceous pollen grains including Classopollis braziliensis, Retitricolpites vulgaris, and Elaterocolpites castelainii. The Jurassic/Cretaceous boundary is coincident with the upper limit of Assemblage IV, based on the last appearances of, in particular, Komewuia glabra and Rigaudella aemula. Within the Kipatimu Formation (as represented in wells SS-5 and SS-7), the systemic boundary appears conformable. But elsewhere in the coastal belt, the boundary is clearly unconformable. On the basis of palynostratigraphic data, significant biostratigraphic events, such as introductions and exits of certain dinoflagellate species commonly match sequence boundaries. From palynofacies analyses and palynostratigraphic data, the Kipatimu Formation is dominated by phytoclasts indicating high terrestrial inputs during its deposition. Abundance of black wood (of high buoyancy) in the majority of samples implies high energy settings and abundance of brown wood (less buoyant) is an indication of a sudden terrestrial input into the marine system. The organic composition of sedimentary rocks is an important means whereby the depositional history of the enclosing sediments can be understood. Different environmental settings clearly influence the character of palynofacies. For example, abundant chorate cysts (e.g., Systematophora spp.) in samples from the upper sections of SS-5 suggest open marine settings. Therefore, palynofacies analyses can be viewed as providing useful pointers to interpreting the environmental circumstances in which the rocks, in this case the Kipatimu Formation, were deposited.	Tanzania Petr Dev Corp, Dar Es Salaam, Tanzania		Msaky, ES (通讯作者)，Tanzania Petr Dev Corp, BWM Tower A,POB 2774, Dar Es Salaam, Tanzania.	emma.msaky@uqconnect.edu.au						Abubakar MB, 2006, J AFR EARTH SCI, V45, P347, DOI 10.1016/j.jafrearsci.2006.03.008; Aitken W.G., 1961, Geological Survey of Tanganyika Bulletin, V31, P1; [Anonymous], PALAEONTOLOGY; [Anonymous], 1985, P YORKSHIRE GE; [Anonymous], 2007, Paleopalynology, DOI DOI 10.1007/978-1; [Anonymous], GEOLOGICAL SURVEY CA; [Anonymous], Neues Jahrbuch fur Geologie und Palaontologie, Monatshefte, V3, P137; [Anonymous], 1996, Palynology: principles and applications; Arai M, 2000, CRETACEOUS RES, V21, P351, DOI 10.1006/cres.2000.0211; Arkell W. 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OCT	2011	286	4-6					101	209						109	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	857LB					2025-03-11	WOS:000297718900001
J	Akhmet'ev, MA				Akhmet'ev, M. A.			Problems of Paleogene stratigraphy and paleogeography in the middle latitudes of Eurasia	RUSSIAN GEOLOGY AND GEOPHYSICS			English	Article						Paleogene; Paleocene; Eocene; Oligocene; climate; meridional and latitudinal communication systems of straits; Azolla beds; dinoflagellates; prasinophytes; diatoms; radiolarians; large and small benthonic and planktonic foraminifera; spores and pollen; plant megafossils; West Siberian Plate; Turan Plate; Turgai strait	DEPOSITS	The present-day notions of the Paleogene history, paleogeography, and paleobiogeography of Central Asia middle latitudes are based on studies carried by A.L. Yanshin in the second quarter of the 20th century. Here, main phases in the geologic history of the West Siberian and Turan Plates and Turgai depression are considered. In the Paleocene and Eocene, these regions were key links of a continuous meridional marine communication system connecting the Tethys and Arctic Oceans. Before the emergence of the latitudinal Alpine-Himalayan orogenic belt, the Tethys and its marginal seas formed a united shelf area. The closest linkage of the water bodies and biota exchange between them existed in the Thanetian and in the first half of the Ypresian. There was intense heat transfer from tropical to higher latitudes through the entire system of epeiric seas and straits. From the end of the Paleocene, this system was supplemented and complicated by latitudinal straits that ensured the connection of the seas of the Northern Peri-Tethys with the Northern Sea basin and the Atlantic. The combination of two sea systems determined the climatic history of this region from the Paleocene till the Late Eocene. The Arctic Basin influenced mainly the structure of cold-water benthos, and the Tethys, the composition of planktonic biota in the photic zone. During the Bartonian and Priabonian, in the last phase of marine sedimentation, the West Siberian epeiric sea was completely isolated from the Arctic Basin and connected only with the Turan sea through the Turgai strait. The Azolla beds accumulated during the low stand of the World Ocean in desalted surface waters and in disoxic bottom waters inhabited by depauperated benthos. At the Eocene/Oligocene boundary, the drainage of the Tavda-Chegan sea was followed by the formation of an N-S-directed river network in the vast areas of West Siberia, Turgai, and the northern cis-Aral region. The climate was unstable, moderately warm to subtropical, with variable humidity. The formation of the Turgai ecotype of mesophytic conifer-broadleaved flora was completed by the end of the Early Oligocene. (C) 2011, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.	Russian Acad Sci, Inst Geol, Moscow 119017, Russia	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences	Akhmet'ev, MA (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevskii Per 7, Moscow 119017, Russia.	akhmetiev@ginras.ru			Russian Academy of Sciences; Russian Foundation for Basic Research [11-05-00431];  [16.740.11.0050]	Russian Academy of Sciences(Russian Academy of Sciences); Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); 	This work was supported by State Contract no. 16.740.11.0050, the program "Biosphere Origin and Evolution" of the Russian Academy of Sciences, and the Russian Foundation for Basic Research, project no. 11-05-00431.	Akhmet'ev M. A., 2008, ORIGIN EVOLUTION BIO, P509; Akhmet'ev MA, 2004, STRATIGR GEO CORREL+, V12, P58; Akhmet'ev MA, 2001, STRATIGR GEO CORREL+, V9, P373; Akhmetev M.A., 2001, Stratigrafiya Geologicheskaya Korrelyatsiya, V9, P65; Akhmetev M.A., 2006, Stratigrafiya Geologicheskaya Korrelyatsiya, V14, P54; AKHMETIEV MA, 2002, SPECIAL VOLUME DEDIC, P275; Akhmetiev MA, 2010, B GEOSCI, V85, P77, DOI 10.3140/bull.geosci.1145; [Anonymous], 2002, ALBUM LITHOPALEOGEOG; [Anonymous], 2010, STRATIGR GEO CORREL+; [Anonymous], 1975, PALEOGENE SYSTEM; [Anonymous], 1956, INT WORKSH DEV UN ST; Antipov MP, 2011, RUSS GEOL GEOPHYS+, V52, P1092, DOI 10.1016/j.rgg.2011.09.005; Ashurov A.A., 1978, PALEOGENE NUMMULITES; BACKMAN J, 2006, P INT OC DRILL PROGR, V302; BENIAMOVSKI VN, 2002, OTDEL GEOLOGII, V77, P28; Beniamovskii V.N., 1995, IZV VYSSH UCHEBN ZAV, P2; Bugrova E.M, 1997, LIF EV EARTH P 1 INT, P24; Bugrova E.M., 2011, NEW DATA PALEOGENE E; Davidzon P.M., 1982, STRATIGRAPHY PALEOGE; Edwards L.E, 1992, US GEOLOGICAL SURV B, P1; Formozova L.N, 1949, OTD GEOL, V24, P48; GORDON WA, 1973, J GEOL, V81, P269, DOI 10.1086/627870; Hollis CJ, 2005, PALAEOGEOGR PALAEOCL, V215, P313, DOI 10.1016/j.palaeo.2004.09.011; Koren' T.N., 2009, REGIONAL GEOLOGY MET, P16; Korobkov A.I, 1965, THESIS VSEGEI; Kothe A., 1988, Geologisches Jahrbuch B, V71, P3; Krasheninnikov V.A., 2007, STRATIGRAPHY PALEOGE; Kul'kova I.A, 1994, MIKROFITOFOSSILII DE, P98; Kuz'mina OB, 2003, GEOL GEOFIZ, V44, P348; Likharev B, 1956, STRATIGRAPHIC DICT U; Lipman R.Kh, 1965, BIOSTRATIGRAFICHESKI, V115, P69; LOYAL RS, 1990, NEWSL STRATIGR, V21, P157; Makulbekov N.M, 1972, EOCENE FLORA W KAZAK; Martynov V.A, 1973, MARINE CONTINENTAL P, P45; Mirza K., 2006, ANCIENT LIFE MODERN, P233; NAIDIN DP, 2007, STRAITS NO HEMISPHER, P60; ORESHKINA TV, 1998, URALS BASIC PROBLEMS, P183; PARRISH JT, 1982, PALAEOGEOGR PALAEOCL, V40, P31; Rostovtsev N.N, 1955, COLLECTION PAPERS, P3; Sarma A, 2006, ANCIENT LIFE MODERN, P119; SAXENA R K, 1983, Geophytology, V13, P202; Scotese C.R., 2002, PALEOMAP Project; Shatskii S.B, 1969, T SNIIGGIMS, V94, P150; Shatskii S.B, 1984, ENV LIFE BOUNDARIES, P9; Shatsky S.B., 1978, PALEOGEN NEOGEN SIBI, P3; Tsirel'son B.S., 1996, GEOLOGIC BIOTIC EV 1, P183; Vakhrushev G.V, 1940, UCHENYE ZAPISKI SARA, V15, p[1, 48]; Van A.V, 1984, ENV LIFE BOUNDARIES, P63; VASILEVA O. 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KOPTYUGA, 3, NOVOSIBIRSK, 630090, RUSSIA	1068-7971	1878-030X		RUSS GEOL GEOPHYS+	Russ. Geol. Geophys.	OCT	2011	52	10					1075	1091		10.1016/j.rgg.2011.09.004	http://dx.doi.org/10.1016/j.rgg.2011.09.004			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	844MG					2025-03-11	WOS:000296750700004
J	Bolch, CJS; Subramanian, TA; Green, DH				Bolch, Christopher J. S.; Subramanian, Thaila A.; Green, David H.			THE TOXIC DINOFLAGELLATE <i>GYMNODINIUM CATENATUM</i> (DINOPHYCEAE) REQUIRES MARINE BACTERIA FOR GROWTH	JOURNAL OF PHYCOLOGY			English	Article						antibiotic; axenic; bacteria; culture; dinoflagellate; growth; Gymnodinium catenatum; interaction; stimulation	PARALYTIC SHELLFISH TOXIN; ALEXANDRIUM-TAMARENSE; IRON UPTAKE; RED-TIDE; PHYTOPLANKTON; CULTURES; ALGAE; PURIFICATION; DIVERSITY; SAXITOXIN	Interactions with the bacterial community are increasingly considered to have a significant influence on marine phytoplankton populations. Here we used a simplified dinoflagellate-bacterium experimental culture model to conclusively demonstrate that the toxic dinoflagellate Gymnodinium catenatum H. W. Graham requires growth-stimulatory marine bacteria for postgermination survival and growth, from the point of resting cyst germination through to vegetative growth at bloom concentrations (10(3) cells mL(-1)). Cysts of G. catenatum were germinated and grown in unibacterial coculture with antibiotic-resistant or antibiotic-sensitive Marinobacter sp. DG879 or Brachybacterium sp., and with mixtures of these two bacteria. Addition of antibiotics to cultures grown with antibiotic-sensitive strains of bacteria resulted in death of the dinoflagellate culture, whereas cultures grown with antibiotic-resistant bacteria survived antibiotic addition and continued to grow beyond the 21 d experiment. Removal of either bacterial type from mixed-bacterial dinoflagellate cultures (using an antibiotic) resulted in cessation of dinoflagellate growth until bacterial concentration recovered to preaddition concentrations, suggesting that the bacterial growth factors are used for dinoflagellate growth or are labile. Examination of published reports of axenic dinoflagellate culture indicate that a requirement for bacteria is not universal among dinoflagellates, but rather that species may vary in their relative reliance on, and relationship with, the bacterial community. The experimental model approach described here solves a number of inherent and logical problems plaguing studies of algal-bacterium interactions and provides a flexible and tractable tool that can be extended to examine bacterial interactions with other phytoplankton species.	[Bolch, Christopher J. S.; Subramanian, Thaila A.] Univ Tasmania, Natl Ctr Marine Conservat & Resource Sustainabil, Australian Maritime Coll, Launceston, Tas 7250, Australia; [Green, David H.] Scottish Assoc Marine Sci, Scottish Marine Inst, Oban PA37 1QA, Argyll, Scotland	University of Tasmania; Australian Maritime College; University of the Highlands & Islands	Bolch, CJS (通讯作者)，Univ Tasmania, Natl Ctr Marine Conservat & Resource Sustainabil, Australian Maritime Coll, Locked Bag 1370, Launceston, Tas 7250, Australia.	chris.bolch@utas.edu.au	Bolch, Christopher/J-7619-2014; Green, David/E-2533-2012	Green, David/0000-0001-7499-6021	University of Tasmania (UTAS) [B0015641]; UTAS Rising Stars [B0017413]; Scottish Association for Marine Science (Oban, UK); NERC [dml010007] Funding Source: UKRI	University of Tasmania (UTAS); UTAS Rising Stars; Scottish Association for Marine Science (Oban, UK); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was supported by the University of Tasmania (UTAS) Institutional Research Grants Scheme (grant B0015641), and UTAS Rising Stars (grant B0017413) awarded to author C. J. S. B., and in-kind support from the Scottish Association for Marine Science (Oban, UK) during a sabbatical visit by C. J. S. B. to D. H. G. (Aug. 2010 to Jan. 2011). We also thank Ms. Masako Matsumoto (University of Tasmania, Launceston) for assisting T. A. S. with PCR amplification and 16S rDNA sequencing of bacteria.	Alavi M, 2001, ENVIRON MICROBIOL, V3, P380, DOI 10.1046/j.1462-2920.2001.00207.x; ALLNUTT FCT, 1987, PLANT PHYSIOL, V85, P751, DOI 10.1104/pp.85.3.751; Amin SA, 2009, P NATL ACAD SCI USA, V106, P17071, DOI 10.1073/pnas.0905512106; Andrews JM, 2001, J ANTIMICROB CHEMOTH, V48, P5, DOI 10.1093/jac/48.suppl_1.5; Ausubel F.M., 1999, Short Protocols in Molecular Biology, V4th ed., p2; BAUER AW, 1966, AM J CLIN PATHOL, V45, P493; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; Bolch C.J., 1993, Journal of Marine Environmental Engineering: 1993, P23; Bolch C. J. 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OCT	2011	47	5					1009	1022		10.1111/j.1529-8817.2011.01043.x	http://dx.doi.org/10.1111/j.1529-8817.2011.01043.x			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	836CD	27020182				2025-03-11	WOS:000296084800006
J	Chambouvet, A; Alves-de-Souza, C; Cueff, V; Marie, D; Karpov, S; Guillou, L				Chambouvet, Aurelie; Alves-de-Souza, Catharina; Cueff, Valerie; Marie, Dominique; Karpov, Sergey; Guillou, Laure			Interplay Between the Parasite <i>Amoebophrya</i> sp (Alveolata) and the Cyst Formation of the Red Tide Dinoflagellate <i>Scrippsiella trochoidea</i>	PROTIST			English	Article						Amoebophrya; dinoflagellate; parasite; resting cyst; sexual reproduction	LIFE-CYCLE; ENDOPARASITIC DINOFLAGELLATE; ALEXANDRIUM DINOPHYCEAE; PHYLOGENETIC POSITION; GENUS ICHTHYODINIUM; CHESAPEAKE BAY; RESTING CYSTS; INFECTION; MORPHOLOGY; POPULATION	Syndiniales (Alveolata) are marine parasites of a wide range of hosts, from unicellular organisms to Metazoa. Many Syndiniales obligatorily kill their hosts to accomplish their life cycle. This is the case for Amoebophrya spp. infecting dinoflagellates. However, several dinoflagellate species known to be infected by these parasites produce diploid resting cysts as part of their life history. These resting cysts may survive several seasons in the sediment before germinating. How these parasites survive during the dormancy of their host remained an open question. We successfully established infections by Amoebophrya sp. in the red tide dinoflagellate Scrippsiella trochoidea. This host strain was homothallic and able to continuously produce typical calcified cysts covered by calcareous spines. Presence of the parasite significantly speeded up the host cyst production, and cysts produced were the only cells to resist infections. However, some of them were clearly infected, probably earlier in their formation. After 10 months, cysts produced in presence of the parasite were able to germinate and new infective cycles of the parasite were rapidly observed. Thus, a very novel relationship for protists is demonstrated, one in which parasite and host simultaneously enter dormancy, emerging months later to propagate both species. (C) 2011 Elsevier GmbH. All rights reserved.	[Chambouvet, Aurelie; Alves-de-Souza, Catharina; Cueff, Valerie; Marie, Dominique; Karpov, Sergey; Guillou, Laure] Univ Paris 06, F-29680 Roscoff, France; [Chambouvet, Aurelie; Alves-de-Souza, Catharina; Cueff, Valerie; Marie, Dominique; Karpov, Sergey; Guillou, Laure] CNRS, Stn Biol Roscoff, UMR 7144, F-29680 Roscoff, France; [Alves-de-Souza, Catharina] Univ Austral Chile, Inst Biol Marina, Valdivia, Chile	Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Sorbonne Universite; Universidad Austral de Chile	Guillou, L (通讯作者)，Univ Paris 06, Pl Georges Teissier, F-29680 Roscoff, France.	lguillou@sb-roscoff.fr	Alves-de-Souza, Catharina/G-3286-2014; Cueff, Valerie/AAW-9258-2021; Karpov, Sergey/H-3271-2013	Karpov, Sergey/0000-0002-1509-1908; Chambouvet, Aurelie/0000-0003-3932-0098; Alves-de-Souza, Catharina/0000-0001-9577-8090; Guillou, Laure/0000-0003-1032-7958; Cueff-Gauchard, Valerie/0000-0001-6969-642X	French ANR Aquaparadox and Paralex; CNRS	French ANR Aquaparadox and Paralex(Agence Nationale de la Recherche (ANR)); CNRS(Centre National de la Recherche Scientifique (CNRS))	We thank D. W. Coats for insightful discussion and comments on a draft of this manuscript, Mohamed Laabir and Benjamin Genovesi-Giunti for their help in cyst isolation and germination, Fabien Jouenne for his help with photography and the "Service Mer et Observation" of the Roscoff Biological Station for sampling. This work was financially supported by the French ANR Aquaparadox and Paralex, and by the CNRS (SK grant as associated professor).	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J	Guiot, J; de Vernal, A				Guiot, Joel; de Vernal, Anne			QSR Correspondence "Is spatial autocorrelation introducing biases in the apparent accuracy of palaeoclimatic reconstructions?" Reply to Telford and Birks	QUATERNARY SCIENCE REVIEWS			English	Editorial Material							DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE CONDITIONS; NORTHERN-HEMISPHERE; HIGH-LATITUDES; ENVIRONMENTS; TRACERS; CLIMATE; MIDDLE; PROXY		[Guiot, Joel] CEREGE, UMR 6635, CNRS, F-13545 Aix En Provence 04, France; [Guiot, Joel] Aix Marseille Univ, F-13545 Aix En Provence 04, France; [de Vernal, Anne] Univ Quebec, GEOTOP UQAM, Montreal, PQ H3C 3P8, Canada	Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Aix-Marseille Universite; University of Quebec; University of Quebec Montreal	Guiot, J (通讯作者)，CEREGE, UMR 6635, CNRS, Europole Arbois BP80, F-13545 Aix En Provence 04, France.	guiot@cerege.fr	Guiot, Joel/G-7818-2011; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Guiot, Joel/0000-0001-7345-4466				[Anonymous], 2010, PAGES News; Bonnet S, 2010, MAR MICROPALEONTOL, V74, P59, DOI 10.1016/j.marmicro.2009.12.001; Crosta X, 2007, DEV MARINE GEOL, V1, P327, DOI 10.1016/S1572-5480(07)01013-5; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; de Vernal A, 2007, DEV MARINE GEOL, V1, P371, DOI 10.1016/S1572-5480(07)01014-7; Draper NR., 1966, APPL REGRESSION ANAL, V1, P407; Elshanawany R, 2010, PALYNOLOGY, V34, P233, DOI 10.1080/01916121003711665; Giraudeau J, 2007, DEV MARINE GEOL, V1, P409, DOI 10.1016/S1572-5480(07)01015-9; Grosfjeld K, 2009, NORW J GEOL, V89, P121; Guiot J, 2009, CLIM PAST, V5, P571, DOI 10.5194/cp-5-571-2009; Guiot J, 2011, QUATERNARY SCI REV, V30, P1965, DOI 10.1016/j.quascirev.2011.04.022; Guiot J, 2007, DEV MARINE GEOL, V1, P523, DOI 10.1016/S1572-5480(07)01018-4; Holzwarth U, 2007, MAR MICROPALEONTOL, V64, P91, DOI 10.1016/j.marmicro.2007.04.001; Kucera M, 2007, DEV MARINE GEOL, V1, P213, DOI 10.1016/S1572-5480(07)01011-1; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Radi T, 2008, MAR MICROPALEONTOL, V68, P84, DOI 10.1016/j.marmicro.2008.01.012; Rochon A., 1999, SPECIAL CONTRIBUTION, V35; Shin HH, 2011, ESTUAR COAST, V34, P712, DOI 10.1007/s12237-011-9373-y; Telford RJ, 2011, QUATERNARY SCI REV, V30, P3210, DOI 10.1016/j.quascirev.2011.07.019; Telford RJ, 2009, QUATERNARY SCI REV, V28, P1309, DOI 10.1016/j.quascirev.2008.12.020; Telford RJ, 2006, QUATERNARY SCI REV, V25, P1375, DOI 10.1016/j.quascirev.2006.02.012; Telford RJ, 2005, QUATERNARY SCI REV, V24, P2173, DOI 10.1016/j.quascirev.2005.05.001	24	17	17	0	7	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0277-3791			QUATERNARY SCI REV	Quat. Sci. Rev.	OCT	2011	30	21-22					3214	3216		10.1016/j.quascirev.2011.07.023	http://dx.doi.org/10.1016/j.quascirev.2011.07.023			3	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	830NK					2025-03-11	WOS:000295663500026
J	Riding, JB; Kyffin-Hughes, JE				Riding, James B.; Kyffin-Hughes, Jane E.			A direct comparison of three palynological preparation techniques	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynomorphs; preparation techniques; Upper Jurassic (Oxfordian); United Kingdom (Scotland)	DINOFLAGELLATE CYSTS; STAFFIN BAY; MIDDLE; PRESERVATION; SEDIMENTS	Two samples of palynomorph-rich Upper Jurassic (Lower Oxfordian) mudstone from western Scotland were quantitatively prepared using the traditional hydrochloric and hydrofluoric acid based palynological preparation technique and two non-acid procedures. The latter are protocols using sodium hexametaphosphate [(NaPO3)(6)] and hydrogen peroxide (H2O2). These non-acid techniques have previously been validated only in terms of the absolute numbers of palynomorphs extracted. By contrast, this study aimed to assess the numbers of palynomorphs extracted in terms of absolute numbers of the individual taxa present to test for any taxonomic biases. The (NaPO3)(6) method proved around 50% as efficient as acid digestion in terms of absolute numbers of palynomorphs extracted. It produced clean residues, which are eminently suitable for most palynological studies. The majority of the taxa present were recovered in representative relative proportions, and no taxonomic biases were noted. The absolute numbers of most taxa decrease in a stepwise fashion from acid digestion via the (NaPO3)(6) procedure to the H2O2 method. However, the concentrations of bisaccate pollen were apparently relatively unaffected by the three methods used. Similarly, the Meiourogonyaulax caytonensis group appears to be unusually resistant to oxidation damage by H2O2. It is considered that the (NaPO3)(6) preparation method is an eminently viable alternative to acid digestion, especially in remote operational settings such as rigsites. The H2O2 technique proved to be significantly less effective, at approximately 10% of the extraction level of add digestion which appears to be largely due to oxidation. Hydrogen peroxide is an aggressive oxidant. Therefore the (NaPO3)(6) technique is deemed to be both safer and more effective than the H2O2 method. (C) 2011 Published by Elsevier B.V.	[Riding, James B.; Kyffin-Hughes, Jane E.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; jeky@bgs.ac.uk			British Geological Survey Laboratory; NERC [bgs04003] Funding Source: UKRI	British Geological Survey Laboratory; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution was supported by the British Geological Survey Laboratory Maintenance and Development of Capability Project. Mr Graeme Dagg helped with the production of the Plates. The authors thank Stewart G. Molyneux and Michael H. Stephenson for their very helpful reviews of the manuscript. The authors publish with the permission of the Executive Director, British Geological Survey (NERC).	BENNINGHOFF W. 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Palaeobot. Palynology	OCT	2011	167	3-4					212	221		10.1016/j.revpalbo.2011.07.008	http://dx.doi.org/10.1016/j.revpalbo.2011.07.008			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	859MI		Green Accepted			2025-03-11	WOS:000297880100004
J	Leighton, AD; Hart, MB; Smart, CW				Leighton, Andrew D.; Hart, Malcolm B.; Smart, Christopher W.			A preliminary investigation into calcareous dinoflagellate cysts and problematic microfossils from an expanded Cretaceous/Paleogene boundary section at Kulstirenden, Stevns Klint, Denmark	CRETACEOUS RESEARCH			English	Article						Calcareous dinoflagellate cysts; K/Pg boundary; Fish clay; Stevns Klint; Bolboforma	SOUTH ATLANTIC-OCEAN; K-T BOUNDARY; TERTIARY BOUNDARY; PALEOGENE BOUNDARY; MAASTRICHTIAN CHALK; MASS EXTINCTION; STABLE-ISOTOPE; K/T BOUNDARY; IMPACT; BIOSTRATIGRAPHY	Located to the north of the Stevns Klint Peninsula (Denmark), Kulstirenden shows the transition from Cretaceous chalks to Danian carbonates across the Cretaceous - Paleogene (K/Pg) boundary. The K/Pg boundary at Kulstirenden is represented by the Fiskeler Member (Fish Clay), a streaked marl interval with a smectite rich, red oxidised layer at its base marking the boundary. The Fiskeler Member is important as it includes the iridium concentration linked to the bolide impact which may have caused the end-Cretaceous mass extinction and is at its maximum thickness at Kulstirenden (c.45 cm). Calcareous dinoflagellate cysts (Calciodinelloideae) have been investigated from within the fine fraction (45-125 mu m) at Kulstirenden in order to understand the ecological implications of these enigmatic microfossils. Several species were found within the Fiskeler Member, including Orthopithonella collaris Wendler et al. (2001, Rev. Palaeobot. Palynol. 115, 69-77). This species is of particular interest as it demonstrates reduced paratabulation and may indicate a transgressive period immediately after the K/Pg boundary event. O. collaris has been described as a morphotype formed under post-K/Pg environmental conditions and is, therefore, described as a "disaster" taxon that marks the K/Pg boundary at Stevns Klint The distribution of this taxon is more extensive than previously documented, disappearing as carbonate sedimentation returned in the Cerithium Limestone Member of the Danian. Several calcareous microfossil specimens that were found cannot be associated with the dinoflagellates and display Bolboforma-like features. While the origins of Bolboforma are enigmatic, the current finding expands their stratigraphic range and suggests an appearance of this group of organisms found at Stevns Klint may give an insight into the inception of this group into the earliest Danian. (C) 2011 Elsevier Ltd. All rights reserved.	[Leighton, Andrew D.; Hart, Malcolm B.; Smart, Christopher W.] Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England	University of Plymouth	Leighton, AD (通讯作者)，Univ Plymouth, Sch Geog Earth & Environm Sci, Plymouth PL4 8AA, Devon, England.	andrew.leighton@plymouth.ac.uk	Hart, Malcolm/KMD-8444-2024	Smart, Christopher/0000-0001-6329-4139				ALVAREZ LW, 1980, SCIENCE, V208, P1095, DOI 10.1126/science.208.4448.1095; Anderskouv K, 2007, SEDIMENT GEOL, V200, P57, DOI 10.1016/j.sedgeo.2007.03.005; Bauluz B, 2000, EARTH PLANET SC LETT, V182, P127, DOI 10.1016/S0012-821X(00)00245-4; Bernaola G, 2007, PALAEOGEOGR PALAEOCL, V255, P132, DOI 10.1016/j.palaeo.2007.02.045; Bjerager M, 2007, PALAEOGEOGR PALAEOCL, V250, P184, DOI 10.1016/j.palaeo.2007.03.008; Bown P, 2005, GEOLOGY, V33, P653, DOI 10.1130/G21566.1; Brasier M.D., 1980, MICROFOSSILS, P162; Brinkhuis H, 1998, PALAEOGEOGR PALAEOCL, V141, P67, DOI 10.1016/S0031-0182(98)00004-2; Fensome R.A., 1993, CLASSIFICATION LIVIN, V7; Frei R, 2002, EARTH PLANET SC LETT, V203, P691, DOI 10.1016/S0012-821X(02)00865-8; Gardin S, 2002, PALAEOGEOGR PALAEOCL, V178, P211, DOI 10.1016/S0031-0182(01)00397-2; Gardin S, 1998, B SOC GEOL FR, V169, P709; Håkansson E, 1999, PALAEOGEOGR PALAEOCL, V154, P67, DOI 10.1016/S0031-0182(99)00087-5; Hart M.B., 2011, SEPM SPECIAL PUBLICA, V100; Hart MB, 2005, PALAEOGEOGR PALAEOCL, V224, P6, DOI 10.1016/j.palaeo.2005.03.029; Hart MB, 2004, J GEOL SOC LONDON, V161, P885, DOI 10.1144/0016-764903-071; Heinberg C, 2005, B GEOL SOC DENMARK, V52, P81; 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; Keller G, 2008, CRETACEOUS RES, V29, P754, DOI 10.1016/j.cretres.2008.05.030; Kienel U., 1994, BERLINER GEOWISSENSC, V12, P87; Kohring Rolf, 2005, Palaeontologische Zeitschrift, V79, P79; Rasmussen JA, 2005, B GEOL SOC DENMARK, V52, P113; SCHMITZ B, 1988, GEOLOGY, V16, P1068, DOI 10.1130/0091-7613(1988)016<1068:OOMIWD>2.3.CO;2; SCHMITZ B, 1992, PALAEOGEOGR PALAEOCL, V96, P233, DOI 10.1016/0031-0182(92)90104-D; Schulte P, 2006, SEDIMENT GEOL, V184, P77, DOI 10.1016/j.sedgeo.2005.09.021; Schulte P, 2010, SCIENCE, V327, P1214, DOI 10.1126/science.1177265; Sepúlveda J, 2009, SCIENCE, V326, P129, DOI 10.1126/science.1176233; Smit J, 1999, ANNU REV EARTH PL SC, V27, P75, DOI 10.1146/annurev.earth.27.1.75; Spezzaferri S, 2004, J MICROPALAEONTOL, V23, P139, DOI 10.1144/jm.23.2.139; Spiegler Dorothee, 2005, Palaeontologische Zeitschrift, V79, P167; Spiegler Dorothee, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P35; SURLYK F., 1997, SEPM SPECIAL PUBLICA, V56, P293; Surlyk F, 2006, B GEOL SOC DENMARK, V54, P1; Tantawy AAAM, 2003, MAR MICROPALEONTOL, V47, P323, DOI 10.1016/S0377-8398(02)00135-4; Wendler J, 2004, REV PALAEOBOT PALYNO, V129, P133, DOI 10.1016/j.revpalbo.2003.12.011; Wendler J, 2002, GEOL SOC AM SPEC PAP, V356, P265; 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	40	5	5	0	15	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	OCT	2011	32	5					606	617		10.1016/j.cretres.2011.05.011	http://dx.doi.org/10.1016/j.cretres.2011.05.011			12	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	813UT					2025-03-11	WOS:000294396400005
J	Laabir, M; Jauzein, C; Genovesi, B; Masseret, E; Grzebyk, D; Cecchi, P; Vaquer, A; Perrin, Y; Collos, Y				Laabir, Mohamed; Jauzein, Cecile; Genovesi, Benjamin; Masseret, Estelle; Grzebyk, Daniel; Cecchi, Philippe; Vaquer, Andre; Perrin, Yvon; Collos, Yves			Influence of temperature, salinity and irradiance on the growth and cell yield of the harmful red tide dinoflagellate <i>Alexandrium catenella</i> colonizing Mediterranean waters	JOURNAL OF PLANKTON RESEARCH			English	Article						Alexandrium catenella; toxic blooms; Thau lagoon; growth; cell yield; temperature; irradiance; salinity	TOXIC DINOFLAGELLATE; ALGAL BLOOMS; THAU LAGOON; COMPLEX DINOPHYCEAE; NUTRITIONAL FACTORS; COASTAL WATERS; CYST FORMATION; TAMARENSE; MINUTUM; CULTURES	In a laboratory study, we determined the influence of temperature, salinity and irradiance on the growth of the paralytic shellfish poisoning (PSP) toxin producer Alexandrium catenella, which can form toxic blooms in the Thau lagoon (western Mediterranean Sea). The strain studied, ACT03, was grown in an artificial seawater medium. The influence of temperature and that of salinity were analysed using 48 different combinations of 6 salinities (10-40 psu) and 8 temperatures (9-30 degrees C) under saturating irradiance (100 mu mol photons m(-2) s(-1)). ACT03 appeared to be an euryhaline strain that can survive at salinities as low as 10 psu and can grow at salinities up to 40 psu. This strain can grow between 15 and 30 degrees C. The highest growth rates (>0.4 day(-1)) were observed between 35 and 40 psu and 15 and 27 degrees C. The influence of irradiance on growth and cell pigment content was tested between 10 and 260 mu mol photons m(-2) s(-1) at 20 degrees C and 38 psu. The results revealed both a low compensation irradiance and that light saturation was reached at 90 mu mol photons m(-2) s(-1). Temperature had the greatest influence on growth. The ecophysiological characteristics reported here are consistent with the environmental conditions encountered in the Thau lagoon. A. catenella exhibited important adaptive capacities over the large range of tested physical factors. This flexibility helps us to explain its ability to bloom seasonally on the Mediterranean coast, where the physico-chemical environmental conditions are characterized by high seasonal variations.	[Laabir, Mohamed; Masseret, Estelle; Grzebyk, Daniel; Vaquer, Andre; Perrin, Yvon; Collos, Yves] Univ Montpellier 2, CNRS, IRD, IFREMER,UMR 5119,UM2,UM1, F-34095 Montpellier, France; [Jauzein, Cecile] Univ Texas, Inst Marine Sci, Port Aransas, TX 78373 USA; [Genovesi, Benjamin] Univ Montpellier 2, Inst Sci Evolut, CNRS, IRD,UMR 5554,UM2, F-34095 Montpellier 05, France; [Cecchi, Philippe] IRD UMR G EAU, F-34196 Montpellier, France	Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; Ifremer; University of Texas System; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; CNRS - Institute of Ecology & Environment (INEE); Institut de Recherche pour le Developpement (IRD)	Laabir, M (通讯作者)，Univ Montpellier 2, CNRS, IRD, IFREMER,UMR 5119,UM2,UM1, CC 093, F-34095 Montpellier, France.	mohamed.laabir@univ-montp2.fr	Grzebyk, Daniel/A-9286-2009	Grzebyk, Daniel/0000-0002-1130-7724; Jauzein, Cecile/0000-0001-6291-6821	Agence Nationale de la Recherche [ANR-05-BLAN-0219, ANR-06-BLAN-0397]; Ifremer; Agence Nationale de la Recherche (ANR) [ANR-06-BLAN-0397, ANR-05-BLAN-0219] Funding Source: Agence Nationale de la Recherche (ANR)	Agence Nationale de la Recherche(Agence Nationale de la Recherche (ANR)); Ifremer; Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	This research was supported by grants from the Agence Nationale de la Recherche (ANR-05-BLAN-0219 XPressFlorAland ANR-06-BLAN-0397 GenoSynTox). Additional support was received through the ALCAT program of Ifremer. Thanks to Caroline Solal for helping in laboratory experiments. The anonymous reviewers are thanked for their valuable comments that helped us to greatly improve the manuscript.	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Plankton Res.	OCT	2011	33	10					1550	1563		10.1093/plankt/fbr050	http://dx.doi.org/10.1093/plankt/fbr050			14	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	815UA		Bronze			2025-03-11	WOS:000294554000008
J	Craveiro, SC; Calado, AJ; Daugbjerg, N; Hansen, G; Moestrup, O				Craveiro, Sandra C.; Calado, Antonio J.; Daugbjerg, Niels; Hansen, Gert; Moestrup, Ojvind			Ultrastructure and LSU rDNA-based Phylogeny of <i>Peridinium lomnickii</i> and Description of <i>Chimonodinium</i> gen. nov (Dinophyceae)	PROTIST			English	Article						Chimonodinium; Dinophyceae; LSU rDNA; Peridinium lomnickii; phylogeny; Scrippsiella trochoidea; ultrastructure	FRESH-WATER; MARINE DINOFLAGELLATE; FLAGELLAR APPARATUS; ELECTRON-MICROSCOPY; SPECIAL EMPHASIS; FINE-STRUCTURE; LIFE-CYCLE; TAXONOMY; EVOLUTION; SEQUENCES	Several populations of Peridinium lomnickii were examined by SEM and serial section TEM. Comparison with typical Peridinium, Peridiniopsis, Palatinus and Scrippsiella species revealed significant structural differences, congruent with phylogenetic hypotheses derived from partial LSU rDNA sequences. Chimonodinium gen. nov. is described as a new genus of peridinioids, characterized by the Kofoidian plate formula Po, cp, x, 4', 3a, 7 '', 6c, 5 s, 5''', 2 '''', the absence of pyrenoids, the presence of a microtubular basket with four or five overlapping rows of microtubules associated with a small peduncle, a pusular system with well-defined pusular tubes connected to the flagellar canals, and the production of non-calcareous cysts. Serial section examination of Scrippsiella trochoidea, here taken to represent typical Scrippsiella characters, revealed no peduncle and no associated microtubular strands. The molecular phylogeny placed C. lomnickii comb. nov. as a sister group to a clade composed of Thoracosphaera and the pfiesteriaceans. Whereas the lack of information on fine structure of the swimming stage of Thoracosphaera leaves its affinities unexplained, C. lomnickii shares with the pfiesteriaceans the presence of a microtubular basket and the unusual connection between two plates on the left side of the sulcus, involving extra-cytoplasmic fibres. (C) 2011 Elsevier GmbH. All rights reserved.	[Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, GeoBioSci GeoTechnol & GeoEngn GeoBioTec Res Unit, P-3810193 Aveiro, Portugal; [Craveiro, Sandra C.; Calado, Antonio J.] Univ Aveiro, Dept Biol, P-3810193 Aveiro, Portugal; [Daugbjerg, Niels; Hansen, Gert; Moestrup, Ojvind] Univ Copenhagen, Sect Evolut & Ecol Aquat Organisms, Dept Biol, DK-1353 Copenhagen K, Denmark	Universidade de Aveiro; Universidade de Aveiro; University of Copenhagen	Calado, AJ (通讯作者)，Univ Aveiro, GeoBioSci GeoTechnol & GeoEngn GeoBioTec Res Unit, P-3810193 Aveiro, Portugal.	acalado@ua.pt	Calado, Antonio Jose/D-6263-2015; Daugbjerg, Niels/D-3521-2014; Hansen, Gert/P-3328-2014; Calado, Sandra Carla/A-6791-2016	Calado, Antonio Jose/0000-0002-9711-0593; Daugbjerg, Niels/0000-0002-0397-3073; Hansen, Gert/0000-0002-5751-8316; Moestrup, Ojvind/0000-0003-0965-8645; Calado, Sandra Carla/0000-0002-2738-7626	POCI, Portugal [SFRH/BD/16794/2004]; European Commission's (FP 6) Integrated Infrastructure Initiative; Carlsberg Foundation; Fundação para a Ciência e a Tecnologia [SFRH/BD/16794/2004] Funding Source: FCT	POCI, Portugal; European Commission's (FP 6) Integrated Infrastructure Initiative(European Union (EU)); Carlsberg Foundation(Carlsberg Foundation); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	SCC was supported by a Ph.D. fellowship from the financing program POCI, Portugal (SFRH/BD/16794/2004) and by a grant from the European Commission's (FP 6) Integrated Infrastructure Initiative programme SYNTHESYS (DK-TAF) during July-September 2008. ND thanks the Carlsberg Foundation for equipment grants. The Scrippsiella trochoidea culture was established during the project "Changes in community structure and microevolution in marine protists" and was kindly provided by Nina Lundholm and Marianne Ellegaard. Henrik Levinsen provided the sample collected in Greenland and Karin Lindberg established the culture originating from cysts collected in Sweden.	[Anonymous], 2004, Modeltest v2; Baldauf SL, 2008, J SYST EVOL, V46, P263, DOI 10.3724/SP.J.1002.2008.08008; BALECH E, 1959, BIOL BULL-US, V116, P195, DOI 10.2307/1539204; Balech E., 1988, Publ. Espec. Inst. Esp. Oceanogr., V1, P1; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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J	Casas-Monroy, O; Roy, S; Rochon, A				Casas-Monroy, Oscar; Roy, Suzanne; Rochon, Andre			Ballast sediment-mediated transport of non-indigenous species of dinoflagellates on the East Coast of Canada	AQUATIC INVASIONS			English	Article						invasive species; dinoflagellates; cyst introductions; ballast tank; sediment; ballast water exchange; harmful algae	EEMIAN HYDROGRAPHIC CONDITIONS; RESTING STAGES; BIOLOGICAL INVASIONS; CYST ASSEMBLAGES; BLOOM EVENTS; BALTIC SEA; SHIPS; WATER; DINOPHYCEAE; PHYTOPLANKTON	The presence and abundance of non-indigenous, and/or harmful or toxic dinoflagellate species in ballast sediments is examined for 65 cargo ships visiting ports on the East coast of Canada, as part of the Canadian Aquatic Invasive Species Network (CAISN). Ships visiting several ports in the provinces of Quebec, New Brunswick and Nova Scotia were sampled during three summers (2007, 2008, 2009). These ships included general cargo, bulk carriers and oil tankers, and they represented two major categories: ships undergoing continental and trans-oceanic voyages. Our results show that potentially viable dinoflagellate cysts are present in ballast sediments of all the categories of ships arriving to the East coast of Canada. The concentrations of all types of dinoflagellate cysts are higher in continental ships without ballast water exchange (BWE) than in ships with BWE, including trans-oceanic ships, which presented lower risk of introduction of non-indigenous species (NIS) of dinoflagellates. We identified 14 non-indigenous dinoflagellate cyst species not yet reported from Canadian coasts, including 4 potentially harmful/toxic species, representing a possibility of new introductions. These introductions of toxic NIS could represent a problem for marine Canadian ecosystems, with potentially disastrous effects on fish communities, aquaculture and human health. This potential risk may be facilitated with climate change.	[Casas-Monroy, Oscar; Roy, Suzanne; Rochon, Andre] Univ Quebec, Inst Sci, Rimouski, PQ G5L 3A1, Canada	University of Quebec	Casas-Monroy, O (通讯作者)，Univ Quebec, Inst Sci, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	oscargabriel.casas-monroy@uqar.qc.ca; suzanne_roy@uqar.qc.ca; andre_rochon@uqar.qc.ca			Natural Sciences and Engineering Research Council of Canada (NSERC); Fisheries and Oceans Canada (DFO); Canadian Aquatic Invasive Species Network (CAISN); Institut des Sciences de la Mer de Rimouski (ISMER) of the Universite du Quebec a Rimouski	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fisheries and Oceans Canada (DFO); Canadian Aquatic Invasive Species Network (CAISN); Institut des Sciences de la Mer de Rimouski (ISMER) of the Universite du Quebec a Rimouski	The authors gratefully acknowledge the Natural Sciences and Engineering Research Council of Canada (NSERC), Fisheries and Oceans Canada (DFO), the Canadian Aquatic Invasive Species Network (CAISN) and the Institut des Sciences de la Mer de Rimouski (ISMER) of the Universite du Quebec a Rimouski for financial support. We thank specially Nathalie Simard, Andrea Weise and Dr. Chris McKindsey (DFO), for help during sampling and for discussion. Also, we thank Transport Canada, shipping agents in different ports, captains, ship officers and crews of the vessels sampled. Finally, we thank all the persons involved in the East Coast Sampling Teams and Jean-Guy Nistad for help with the production of maps. Special thanks to reviewers and the editor for their constructive and insightful comments.	Anderson M.J., 2008, PRIMER E PLYMOUTH; [Anonymous], 2004, INT CONVENTION CONTR; [Anonymous], REPROD BIOL INVERTEB; [Anonymous], 1983, Chin. J. Oceanol. 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Invasions	SEP	2011	6	3					231	248		10.3391/ai.2011.6.3.01	http://dx.doi.org/10.3391/ai.2011.6.3.01			18	Ecology; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	972LA		gold, Green Submitted			2025-03-11	WOS:000306277400001
J	Suto, I; Watanabe, M; Jordan, RW				Suto, Itsuki; Watanabe, Mahito; Jordan, Richard W.			Taxonomy of the fossil marine diatom resting spore genus <i>Odontotropis</i>	DIATOM RESEARCH			English	Article						Odontotropis: fossil diatoms; resting spores; IODP Expedition 302; Arctic Coring Expedition; ACEX	GENERA DICLADIA EHRENBERG; CHAETOCEROS-PSEUDOCURVISETUS; PLANKTONIC DIATOM; SYNDENDRIUM EHRENBERG; LIRADISCUS GREVILLE; NORTH PACIFIC; ASSEMBLAGES; SUTO; NOV	This article describes the taxonomy of Odontotropis Grunow including nine taxa with two new species (O. circularis Wise, O. danicus Debes ex Hustedt, O. carinata Grunow, O. arctica Suto sp. nov., O. reticulata Suto sp. nov., O. cristata Grunow, O. galeonis Hanna, O. hyalina Witt and O. birostrata Pantocsek) mostly from Arctic core materials (Integrated Ocean Drilling Program, IODP Expedition 302), in addition to a synonymy list, light and scanning electron microscopy observations and several key references for each taxon. This genus is characterized by having a strongly vaulted frustule, a boat-shaped or circular outline with a sharp carina around the margin and a long history from the Cretaceous to the middle Eocene. The resting spores of Odontotropis may have had a similar ecological strategy to that of dinoflagellate cysts rather than Chaetoceros resting spores. The Odontotropis resting spore extinction occurred before the Eocene/Oligocene Event of Suto which was characterized by a Chaetoceros resting spore explosive diversification, an increase in abundance, and a decrease in valve size. These changes indicate that coastal conditions became unstable, whereby there was a regular seasonal environmental change involving the depletion and sporadic supply of nutrients, conditions more favorable to Chaetoceros resting spores than to dinoflagellate cysts.	[Suto, Itsuki] Nagoya Univ, Dept Earth & Planetary Sci, Grad Sch Environm Studies, Chikusa Ku, Nagoya, Aichi 4648601, Japan; [Watanabe, Mahito] Natl Inst Adv Ind Sci & Technol, Inst Geol & Geoinformat, Geol Survey Japan, Tsukuba, Ibaraki 3058567, Japan; [Jordan, Richard W.] Yamagata Univ, Dept Earth & Environm Sci, Fac Sci, Yamagata 9908560, Japan	Nagoya University; National Institute of Advanced Industrial Science & Technology (AIST); Yamagata University	Suto, I (通讯作者)，Nagoya Univ, Dept Earth & Planetary Sci, Grad Sch Environm Studies, Chikusa Ku, Furo Cho, Nagoya, Aichi 4648601, Japan.	suto.itsuki@a.mbox.nagoya-u.ac.jp	Watanabe, Mahito/N-2494-2018	Jordan, Richard/0000-0002-8997-7349	JSPS [20740299]; Grants-in-Aid for Scientific Research [20740299] Funding Source: KAKEN	JSPS(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We thank the co-chief scientists Jan Backman (Stockholm University) and Kathryn Moran (University of Rhode Island), and the scientific party of IODP Leg 302 ACEX as well as the captain and crew who provided the opportunity for us to sample the sediments on board the R/V Oden. We wish to thank Kota Katsuki (Kochi University), Nalan Koc and Catherine E. Stickley (Norwegian Polar Institute) for invaluable discussions. Special thanks are given to Kozo Takahashi (Kyushu University) and Jonaotaro Onodera (JAMSTEC) who provided sieved samples and gave numerous suggestions. We also thank Yoshihiro Tanimura (National Science Museum, Tokyo), who kindly curated the type specimens described in this paper. We are grateful to Elisabeth Fourtanier (California Academy of Science) and Patrick Kociolek (University of Colorado) for providing valuable discussion and copies of some old papers. This research used samples and data provided by the Integrated Ocean Drilling Program (IODP). This work was partially supported by JSPS Grant-in-Aid for Young Scientists (B) Project No. 20740299.	[Anonymous], Die Kieselalgen Deutschlands, sterreichs und der Schweiz; [Anonymous], 1999, DIATOM RES; Backman J, 2005, SCI DRILL, V1, P12, DOI 10.5194/sd-1-12-2005; Barron J. 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Atlas; WISE F.C., 1956, J QUEKETT MICROSCOPI, V4, P310; Witt O.N., 1886, Verhandlungen der Russisch-kaiserlichen Mineralogischen Gesellschaft zu St. Petersburg Zapiski imperatorskago c. peterburgskago minerulogicheskugo Obshchestv, Series II, V2, P137; YANAGISAWA Y., 1998, J GEOL SOC JPN, V104, P395, DOI DOI 10.5575/GEOSOC.104.395	59	3	4	0	9	TAYLOR & FRANCIS LTD	ABINGDON	2-4 PARK SQUARE, MILTON PARK, ABINGDON OR14 4RN, OXON, ENGLAND	0269-249X	2159-8347		DIATOM RES	Diatom Res.	SEP-DEC	2011	26	3-4					255	272		10.1080/0269249X.2011.591047	http://dx.doi.org/10.1080/0269249X.2011.591047			18	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	881PX					2025-03-11	WOS:000299499700001
J	Barreda, V; Encinas, A; Hinojosa, LF				Barreda, Viviana; Encinas, Alfonso; Felipe Hinojosa, Luis			Pollen and spores of the Navidad Formation, Neogene from Chile	REVISTA CHILENA DE HISTORIA NATURAL			Spanish	Article						Chile; Neogene; palynology; South America	SOUTHERN SOUTH-AMERICA; MIOCENE; FORESTS	Palynological assemblages recovered from the Navidad Formation in outcrops of the Cordillera de la Costa, central Chile, are dominated by wood remains, cuticles, spores and pollen grains and fresh water algae (continental elements) with scarce dinoflagellate cysts, acritarchs, foraminiferal linnings marine palynomorphs) indicating that these assemblages would have been accumulated in a marine environment. Spore-pollen assemblages indicate a forest vegetation with the co-existence of Gondwanan (Podocarpaceae, Araucariaceae, Nothofagaceae) and neotropical (Sapotaceae, Malphigiaceae, Arecaceae, Chloranthaceae, Tiliaceae/Bombacaceae) taxa -Mixed Paleoflora- supporting previous assumptions based on the macroflora. On the forest margins, patches of sclerophyllous formations with Anacardiaceae and Fabaceae as prevailing components may have also established. Xerophitic and halophytic shrubby-herbaceous elements (Chenopodiaceae, Calyceraceae) may have developed in sandy soils and costal salt marshes. Endemic components such as Calyceraceae and Asteraceae (Barnadesioideae) were recorded for the first time in Chile. This flora would have developed under warm and humid climatic conditions. The spore-pollen assemblages support a Neogene age for the Navidad Formation.	[Barreda, Viviana] Museo Argentino Ciencias Nat Bernardino Rivadavia, Div Paleobot, Buenos Aires, DF, Argentina; [Encinas, Alfonso] Univ Concepcion, Dept Ciencias Tierra, Concepcion, Chile; [Felipe Hinojosa, Luis] Univ Chile, Dept Ciencias Ecol, Santiago, Chile	Museo Argentino de Ciencias Naturales Bernardino Rivadavia (MACN); Universidad de Concepcion; Universidad de Chile	Barreda, V (通讯作者)，Museo Argentino Ciencias Nat Bernardino Rivadavia, Div Paleobot, A Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina.	vbarreda@macn.gov.ar	Hinojosa, Luis Felipe/J-7557-2017	Hinojosa, Luis Felipe/0000-0001-5646-649X; Barreda, Viviana Dora/0000-0002-1560-1277				[Anonymous], 1846, APPENDIX DARWIN C GE; [Anonymous], 1979, B MUSEO NACL HIST NA; [Anonymous], 1991, B MUSEO NACL HIST NA; Barreda V, 2008, DEV QUATER SCI, V11, P343, DOI 10.1016/S1571-0866(07)10016-6; Barreda Viviana D., 1996, Ameghiniana, V33, P35; Cecioni G., 1978, Publicacion Ocasional, V25, P3; Darwin Charles., 1846, Geological Observations on South America; Encinas A, 2008, J S AM EARTH SCI, V25, P157, DOI 10.1016/j.jsames.2007.07.001; Encinas A, 2006, REV GEOL CHILE, V33, P339; Feldmann RM, 2005, J CRUSTACEAN BIOL, V25, P427, DOI 10.1651/C-2547; Finger KL, 2007, PALAIOS, V22, P3, DOI 10.2110/palo.2005.p05-081r; FRASSINETTI D, 1984, B MUSEO NACL HIST NA, V40, P107; Graham A., 1996, COMPOSITAE SYSTEMATI, V1, P123; Hinojosa LF, 2006, J BIOGEOGR, V33, P331, DOI 10.1111/j.1365-2699.2005.01350.x; Hinojosa LF, 2005, PALAEOGEOGR PALAEOCL, V217, P1, DOI 10.1016/j.palaeo.2004.11.013; Hinojosa LF, 2005, REV GEOL CHILE, V32, P95; Jacobs BF, 1999, ANN MO BOT GARD, V86, P590, DOI 10.2307/2666186; Macphail M, 2006, PALAEOGEOGR PALAEOCL, V240, P602, DOI 10.1016/j.palaeo.2006.03.010; Mancini, 2007, AMEGHINIANA, V11, P173, DOI DOI 10.13140/2.1.2832.7366; MARTINEZ PARDO R, 1979, C GEOLOGICO CHILENO, V2, P77; Nielsen SN, 2005, J PALEONTOL, V79, P1120, DOI 10.1666/0022-3360(2005)079[1120:CSAASG]2.0.CO;2; Olivero EB., 1998, REV ASOC GEOL ARGENT, V53, P504; Osorio R., 1978, J FACULTY SCI HOKKAI J FACULTY SCI HOKKAI, V4, P57; PALAZZESI L, 2010, REV PALAEOBOT PALYNO, V155, P83; Palazzesi L, 2009, REV PALAEOBOT PALYNO, V155, P83, DOI 10.1016/j.revpalbo.2009.03.001; PHILIPPI RA, 1887, FOSILES CUARTARIOS T; SUAREZ M.E., 2006, Cainozoic Research, V4, P3; TANAI T, 1983, J FS HOKKAIDO U 4, V21, P505; Troncoso A, 2006, AMEGHINIANA, V43, P171; Troncoso A., 1993, B MUSEO NACL HIST NA, V44, P47; Truswell EM, 2009, AUST SYST BOT, V22, P57, DOI 10.1071/SB08046; Villagran C, 1997, REV CHIL HIST NAT, V70, P241; Villagran C., 2005, Regionalizacion Biogeografica en Iberoamerica y topicos fines, P551; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29	34	9	9	1	8	SOC BIOLGIA CHILE	SANTIAGO	CASILLA 16164, SANTIAGO 9, CHILE	0716-078X	0717-6317		REV CHIL HIST NAT	Rev. Chil. Hist. Nat.	SEP	2011	84	3					341	355		10.4067/S0716-078X2011000300003	http://dx.doi.org/10.4067/S0716-078X2011000300003			15	Biodiversity Conservation; Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Biodiversity & Conservation; Environmental Sciences & Ecology	868HS		Green Published, Green Submitted, gold			2025-03-11	WOS:000298514900003
J	Ji, LM; Meng, FW; Yan, K; Song, ZG				Ji, Liming; Meng, Fanwei; Yan, Kui; Song, Zhiguang			The dinoflagellate cyst <i>Subtilisphaera</i> from the Eocene of the Qaidam Basin, northwest China, and its implications for hydrocarbon exploration	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Subtilisphaera; Dinosterane; source rock; Xiaganchaigou Formation; Qaidam Basin	LACUSTRINE SOURCE ROCKS; MOUNT BRUCE SUPERGROUP; VENA-DEL-GESSO; MOLECULAR FOSSILS; PALEOENVIRONMENTAL CHANGE; 4-METHYL STERANES; SEDIMENTS; ORIGIN; BIOMARKERS; RECONSTRUCTION	Although an abundance of 4-methyl-sterane and dinosterane thought to derive from dinoflagellates, has been detected in the Palaeogene source rocks and crude oils in the Qaidam Basin, China, no unequivocal dinoflagellate cysts have been found previously in Cretaceous-Palaeogene terrestrial deposits in this basin, including the Xiaganchaigou Formation. This study reports on a new discovery using detailed analysis of a dinoflagellate cyst assemblage, composed solely of Subtilisphaera, from the Xiaganchaigou Formation on the north margin of the Qaidam Basin. The biomarkers 4-methylsterane and dinosterane in the corresponding fossil-bearing beds have also been detected, further validating the dependability of dinoflagellate cysts. These fossils provide direct evidence of the dinoflagellate contribution to Palaeogene crude oil in the Qaidam Basin and fill a long-existing gap in oil-source correlation. (C) 2011 Elsevier B.V. All rights reserved.	[Ji, Liming] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resource Res, Lanzhou 730000, Peoples R China; [Ji, Liming] Univ Texas Austin, Jackson Sch Geosci, Bur Econ Geol, Austin, TX 78713 USA; [Ji, Liming; Song, Zhiguang] Chinese Acad Sci, Guangzhou Inst Geochem, State Key Lab Organ Geochem, Guangzhou 510640, Guangdong, Peoples R China; [Meng, Fanwei; Yan, Kui] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China	Chinese Academy of Sciences; Institute of Geology & Geophysics, CAS; University of Texas System; University of Texas Austin; Chinese Academy of Sciences; Guangzhou Institute of Geochemistry, CAS; Chinese Academy of Sciences	Ji, LM (通讯作者)，Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resource Res, Lanzhou 730000, Peoples R China.	jiliming1998@hotmail.com	Ji, Liming/B-2573-2013	yan, kui/0000-0002-4205-2437	National Natural Science Foundation of China [40973033]; State Key Laboratory of Organic Geochemistry [OGL-200917]; China Scholarship Council [2007106304]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); State Key Laboratory of Organic Geochemistry(Chinese Academy of Sciences); China Scholarship Council(China Scholarship Council)	This work was financially supported by the fund of the National Natural Science Foundation of China (No. 40973033), the Earmarked Fund of the State Key Laboratory of Organic Geochemistry (No. OGL-200917) and the fund of the China Scholarship Council (No. 2007106304). The authors are grateful to Xu Jinli, senior engineer at the Geology Science Academy of the Shengli Oilfield, for his help in the analysis and identification of algae fossils. Publication authorized by the Director, Bureau of Economic Geology.	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Palaeobot. Palynology	SEP	2011	167	1-2					40	50		10.1016/j.revpalbo.2011.07.005	http://dx.doi.org/10.1016/j.revpalbo.2011.07.005			11	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	843SK					2025-03-11	WOS:000296692700005
J	Smith, KF; Rhodes, LL; Suda, S; Selwood, AI				Smith, Kirsty F.; Rhodes, Lesley L.; Suda, Shoichiro; Selwood, Andrew I.			A dinoflagellate producer of pinnatoxin G, isolated from sub-tropical Japanese waters	HARMFUL ALGAE			English	Article						Pinnatoxin G; Dinoflagellate; Peridiniales; Japan; Australasia	SHELLFISH POISON; DINOPHYCEAE	A thecate dinoflagellate (Peridiniales, Dinophyceae) was cultured from individual non-calcareous cysts, isolated from surface sediment samples collected in Okinawa, Japan. Two isolates (CAWD188 and CAWD190) from two different sampling sites, each cultured from an individual cyst, produced ca. 11.9 and 15 pg cell(-1) pinnatoxin G, respectively, as determined by liquid chromatography-mass spectrometric (LC-MS). No other pinnatoxins were detected. The motile cells and cysts appeared morphologically identical to those of pinnatoxins E and F producers isolated from New Zealand waters and pinnatoxins E, F, and G producers isolated from Australian waters. Motile and cysts cells measured an average of 25 mu m long x 21.3 mu m wide and 29 mu m long x 25.5 mu m wide, respectively. Analysis of the large subunit ribosomal DNA sequence data showed two well supported strains with slight differences between the Japanese and the Australasian isolates. (C) 2011 Elsevier B.V. All rights reserved.	[Smith, Kirsty F.; Rhodes, Lesley L.; Selwood, Andrew I.] Cawthron Inst, Nelson 7042, New Zealand; [Suda, Shoichiro] Univ Ryukyus, Fac Sci, Okinawa 9030213, Japan	Cawthron Institute; University of the Ryukyus	Smith, KF (通讯作者)，Cawthron Inst, 98 Halifax St E,Private Bag 2, Nelson 7042, New Zealand.	Kirsty.Smith@cawthron.org.nz	Selwood, Andrew/AAP-7550-2020; Suda, Shoichiro/ABA-9738-2020	Selwood, Andrew/0000-0003-1399-8028	New Zealand Ministry of Science and Innovation [CAW0703]	New Zealand Ministry of Science and Innovation	Thanks to Prof. T. Yasumoto for his support. Thanks also to D. Hoperoft (Manawatu Microscopy and Imaging Centre, Massey University) for scanning electron microscopy, Prof. G. Hallegraeff (University of Tasmania) for his taxonomic expertise, and J. Adamson and K. Ponikla (Cawthron Institute) for technical support. The work was supported by funding from the New Zealand Ministry of Science and Innovation, contract CAW0703.[SS]	Chou T, 1996, TETRAHEDRON LETT, V37, P4027, DOI 10.1016/0040-4039(96)00753-8; Chou T, 1996, TETRAHEDRON LETT, V37, P4023, DOI 10.1016/0040-4039(96)00752-6; Excoffier L, 2005, EVOL BIOINFORM, V1, P47, DOI 10.1177/117693430500100003; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Hall TA., 1999, NUCL ACIDS S SERIES, V41, P95, DOI [DOI 10.1021/BK-1999-0734.CH008, DOI 10.14344/IOC.ML.11.1]; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; KELLER MD, 1987, J PHYCOL, V23, P633; Litaker RW, 2007, J PHYCOL, V43, P344, DOI 10.1111/j.1529-8817.2007.00320.x; McNabb P., 2008, 1453 CAWTHR; Munday Rex, 2008, P581; Nézan E, 2011, CRYPTOGAMIE ALGOL, V32, P3, DOI 10.7872/crya.v32.iss1.2011.003; Nunn GB, 1996, J MOL EVOL, V42, P211, DOI 10.1007/BF02198847; Nylander J.A. A., 2004, PROGRAM DISTRIBUTED; Rhodes L, 2011, NEW ZEAL J MAR FRESH, V45, P703, DOI 10.1080/00288330.2011.586041; Rhodes L, 2010, HARMFUL ALGAE, V9, P384, DOI 10.1016/j.hal.2010.01.008; Rhodes L., 2010, 14 HARMF ALG C CRET, P183; Rhodes L., 2010, Harmful Algae 2008, P151; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Selwood AI, 2010, J AGR FOOD CHEM, V58, P6532, DOI 10.1021/jf100267a; Takada N, 2001, TETRAHEDRON LETT, V42, P3491, DOI 10.1016/S0040-4039(01)00480-4; Tamura K, 2011, MOL BIOL EVOL, V28, P2731, DOI 10.1093/molbev/msr121; UEMURA D, 1995, J AM CHEM SOC, V117, P1155, DOI 10.1021/ja00108a043; White TJ., 1990, PCR protocols: A guide to methods and applications, V18, P315, DOI [10.1016/b978-0-12-372180-8.50042-1, DOI 10.1016/B978-0-12-372180-8.50042-1, 10.1016/B978-0-12-372180-8.50042-1]	23	40	42	1	24	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	SEP	2011	10	6					702	705		10.1016/j.hal.2011.05.006	http://dx.doi.org/10.1016/j.hal.2011.05.006			4	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	836LH					2025-03-11	WOS:000296112700017
J	Bienfang, PK; Molina, J; DeFelice, SV; Decarlo, EH				Bienfang, P. K.; Molina, J.; DeFelice, S. V.; Decarlo, E. H.			Evaluation of <i>Gambierdiscus</i> survival after exposure to ballast water	HARMFUL ALGAE			English	Article						Ballast water; Ciguatera; Gambierdiscus; Invasive species; Shipping	PROPAGULE PRESSURE; CIGUATERA; DINOPHYCEAE; ORGANISMS; TOXICITY; PACIFIC	The dinoflagellate Gambierdiscus was exposed to ballast water from a trans-oceanic vessel, and maintained at a variety of temperatures in the dark to determine if viability would be maintained. Logarithmically growing Gambierdiscus inocula were admixed (1:6, vol:vol) with ballast water, maintained in the dark at 22.6 degrees C, 24.6 degrees C, 26.8 degrees C and 29.0 degrees C and assessed for numerical abundance over six days. Calculated growth rates from the biomass time series showed no indication that ballast water negatively impacted Gambierdiscus viability; accompanying microscopic inspections supported this conclusion. Filtration of large volumes of collected ballast water failed to show the presence of any Gambierdiscus cells contained therein. Recovery and microscopic examination of the experimental inocula after 10 weeks in the dark, failed to show cyst development at any temperature regime. This examination of ballast water showed no evidence of cytotoxicity to Gambierdiscus spp. (C) 2011 Elsevier B.V. All rights reserved.	[Bienfang, P. K.; DeFelice, S. V.] Univ Hawaii, Sch Ocean & Earth Sci & Technol, Ctr Oceans & Human Hlth, Pacific Res Ctr Marine Biomed, Honolulu, HI 96822 USA; [Molina, J.] Univ Hawaii, Global Environm Studies Program, Honolulu, HI 96822 USA; [Decarlo, E. H.] Univ Hawaii, Dept Oceanog, Honolulu, HI 96822 USA	University of Hawaii System; University of Hawaii System; University of Hawaii System	Bienfang, PK (通讯作者)，Univ Hawaii, Sch Ocean & Earth Sci & Technol, Ctr Oceans & Human Hlth, Pacific Res Ctr Marine Biomed, Honolulu, HI 96822 USA.	bienfang@soest.hawaii.edu			National Institute of Environmental Health Sciences [P50ES012740]; National Science Foundation [OCE04-32479, OCE09-11000, OCE08-52301]; Division Of Ocean Sciences; Directorate For Geosciences [0852301] Funding Source: National Science Foundation	National Institute of Environmental Health Sciences(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); National Science Foundation(National Science Foundation (NSF)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This research was made possible through the Centers for Oceans and Human Health (COHH) program of the National Institute of Environmental Health Sciences (P50ES012740) and National Science Foundation grants OCE04-32479, OCE09-11000, and OCE08-52301. The content is solely the responsibility of the authors and does not necessarily represent the official view of the National Institute of Environmental Health Sciences, the National Institutes of Health, or the National Science Foundation. We thank Mr. G. North and the Matson personnel U. Idema, J. Sullivan, R. Thomas, and R. Lamb) for their cooperation in coordinating the collection of ballast water from the M/V vessel Maunalei.[SS]	Aligizaki K, 2008, J BIOL RES-THESSALON, V9, P75; Bagnis Raymond, 1994, Memoirs of the Queensland Museum, V34, P455; Bailey SA, 2003, LIMNOL OCEANOGR, V48, P1701, DOI 10.4319/lo.2003.48.4.1701; Bienfang P.K., 2008, OCEANS HUMAN HLTH RI, P257; BOMBER JW, 1988, J EXP MAR BIOL ECOL, V115, P53, DOI 10.1016/0022-0981(88)90189-X; CARLTON JT, 1985, OCEANOGR MAR BIOL, V23, P313; Chinain M, 2010, TOXICON, V56, P739, DOI 10.1016/j.toxicon.2009.06.013; Choi KH, 2009, OCEAN SCI J, V44, P221, DOI DOI 10.1007/S12601-009-0021-4; Colautti RI, 2006, BIOL INVASIONS, V8, P1023, DOI 10.1007/s10530-005-3735-y; DECARLO EH, 1998, WINT C PLASM SPECTR, V23, P82; Dickey RW, 2010, TOXICON, V56, P123, DOI 10.1016/j.toxicon.2009.09.008; DURANDCLEMENT M, 1986, TOXICON, V24, P1153, DOI 10.1016/0041-0101(86)90141-8; FRAGA S, 2010, 14 C INT SOC STUD HA; Guillard R.R.L., 1984, P391; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Holmes MJ, 1998, J PHYCOL, V34, P661, DOI 10.1046/j.1529-8817.1998.340661.x; Keller M.D., 1985, P113; Lehane L, 2000, INT J FOOD MICROBIOL, V61, P91, DOI 10.1016/S0168-1605(00)00382-2; Levings CD, 2004, CAN J FISH AQUAT SCI, V61, P1, DOI 10.1139/F03-135; LEWIS RJ, 1986, SOC SCI MED, V23, P983; Lu SH, 2004, HYDROBIOLOGIA, V512, P231, DOI 10.1023/B:HYDR.0000020331.75003.18; McCarthy Heather P., 2000, Biological Invasions, V2, P321, DOI 10.1023/A:1011418432256; MORTON SL, 1990, TOXIC MARINE PHYTOPLANKTON, P201; Roeder K, 2010, TOXICON, V56, P731, DOI 10.1016/j.toxicon.2009.07.039; RUFF TA, 1989, LANCET, V1, P201; Spencer Khalil J., 1995, Pacific Science, V49, P492; STEIDINGER KA, 1984, DINOFLAGELLATES, P210; Verling E, 2005, P ROY SOC B-BIOL SCI, V272, P1249, DOI 10.1098/rspb.2005.3090; YASUMOTO T, 1977, B JPN SOC SCI FISH, V43, P1015	29	2	3	2	24	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	SEP	2011	10	6					759	762		10.1016/j.hal.2011.06.007	http://dx.doi.org/10.1016/j.hal.2011.06.007			4	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	836LH					2025-03-11	WOS:000296112700025
J	Medhioub, W; Sechet, V; Truquet, P; Bardouil, M; Amzil, Z; Lassus, P; Soudant, P				Medhioub, Walid; Sechet, Veronique; Truquet, Philippe; Bardouil, Michele; Amzil, Zouher; Lassus, Patrick; Soudant, Philippe			<i>Alexandrium ostenfeldii</i> growth and spirolide production in batch culture and photobioreactor	HARMFUL ALGAE			English	Article						Alexandrium ostenfeldii; Batch; Growth; Photobioreactor; Spirolide production	TOXIC DINOFLAGELLATE; GONYAULAX-EXCAVATA; CYST FORMATION; DINOPHYCEAE; SHELLFISH; TAMARENSE; TEMPERATURES; SALINITY; PROFILE; LIGHT	Growth and spirolide production of the toxic dinoflagellate Alexandrium ostenfeldii (Danish strain CCMP1773) were studied in batch culture and a photobioreactor (continuous cultures). First, batch cultures were grown in 450 mL flasks without aeration and under varying conditions of temperature (16 and 22 degrees C) and culture medium (L1, f/2 and L1 with addition of soil extract). Second, cultures were grown at 16 degrees C in 8 L aerated flat-bottomed vessels using L1 with soil extract as culture medium. Finally, continuous cultures in a photobioreactor were conducted at 18 degrees C in L1 with soil extract; pH was maintained at 8.5 and continuous stirring was applied. This study showed that A. ostenfeldii growth was significantly affected by temperature. At the end of the exponential phase, maximum cell concentration and cell diameter were significantly higher at 16 degrees C than at 22 C. In batch culture, maximum spirolide quota per cell (approx. 5 pg SPX 13-desMeC eq cell(-1)) was detected during lag phase for all conditions used. Spirolide quota per cell was negatively and significantly correlated to cell concentration according to the following equation: y = 4013.9x(-0.858). Temperature and culture medium affected the spirolide profile which was characterized by the dominance of 13,19-didesMeC (29-46%), followed by SPX-D (21-28%), 13-desMeC (21-23%), and 13-desMeD (17-21%). Stable growth of A. ostenfeldii was maintained in a photobioreactor over two months, with maximum cell concentration of 7 x 10(4) cells mL(-1). As in batch culture, maximum spirolide cell quota was found in lag phase and then decreased significantly throughout the exponential phase. Spirolide cell quota was negatively and significantly correlated to cell concentration according to the equation: y = 12,858x(-0.8986). In photobioreactor, spirolide profile was characterized by higher proportion of 13,19-didesMeC (60-87%) and lower proportions of SPX-D (3-12%) and 13-desMeD (1.6-10%) as compared to batch culture. (C) 2011 Elsevier B.V. All rights reserved.	[Medhioub, Walid; Soudant, Philippe] Univ Bretagne Occidentale, IUEM, LEMAR UMR 6539, F-29280 Plouzane, France; [Medhioub, Walid; Sechet, Veronique; Truquet, Philippe; Bardouil, Michele; Amzil, Zouher; Lassus, Patrick] IFREMER, Lab Phycotoxines, F-44311 Nantes 3, France; [Medhioub, Walid] INSTM, Lab Aquaculture, Monastir 5000, Tunisia	Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Ifremer; Institut de Recherche pour le Developpement (IRD); Ifremer; Institut National des Sciences et Technologies de la Mer	Soudant, P (通讯作者)，Univ Bretagne Occidentale, IUEM, LEMAR UMR 6539, Pl Nicolas Copern,Technopole Brest Iroise, F-29280 Plouzane, France.	Walid.Medhioub@ifremer.fr; Veronique.Sechet@ifremer.fr; Philippe.Truquet@ifremer.fr; Michele.Bardouil@ifremer.fr; Zouher.Amzil@ifremer.fr; Patrick.Lassus@ifremer.fr; Philippe.Soudant@univ-brest.fr		Soudant, Philippe/0000-0003-3090-5612; Medhioub, Walid/0000-0003-1491-5917; sechet, veronique/0000-0002-7085-3215	Tunisian National Institute of Marine Science and Technologies (INSTM); French Research Institute for Exploitation of the Sea (IFREMER)	Tunisian National Institute of Marine Science and Technologies (INSTM); French Research Institute for Exploitation of the Sea (IFREMER)	This work was supported by the convention framework between the Tunisian National Institute of Marine Science and Technologies (INSTM) and the French Research Institute for Exploitation of the Sea (IFREMER). Sincere thanks are due to A. Volety for English corrections.[SS]	Aasen J, 2005, CHEM RES TOXICOL, V18, P509, DOI 10.1021/tx049706n; Amzil Z, 2007, MAR DRUGS, V5, P168, DOI 10.3390/md504168; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], HARMFUL ALGAL BLOOMS; Beuzenberg V., 2007, 6 INT C MOLL SHELLF; Botana Luis M., 2008, P149; BOYER GL, 1987, MAR BIOL, V96, P123, DOI 10.1007/BF00394845; Cembella A. 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J	Larsson, LM; Dybkjær, K; Rasmussen, ES; Piasecki, S; Utescher, T; Vajda, V				Larsson, Linda M.; Dybkjaer, Karen; Rasmussen, Erik S.; Piasecki, Stefan; Utescher, Torsten; Vajda, Vivi			Miocene climate evolution of northern Europe: A palynological investigation from Denmark	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Palaeoenvironment; Pollen; Climate change; Miocene; Mid-Miocene Climatic Optimum Denmark	EARLY-MIDDLE MIOCENE; NORTHWESTERN GERMANY; UPPERMOST OLIGOCENE; PANNONIAN BASIN; LATROBE VALLEY; SEA BASIN; VEGETATION; STRATIGRAPHY; JYLLAND; POLLEN	A palynological investigation has been conducted on Lower-Upper Miocene sediments from Jylland, Denmark, corresponding to the time interval of about 19 to 8 Ma. The sediments, derived from the Sdr. Vium drill core, were deposited in marine to marginal-marine environments, as shown by the relatively high abundance of dinoflagellate cysts in all samples. Nevertheless, rich and diverse pollen assemblages occur throughout the succession and the palynological analysis reveals that coastal areas of the study area were during the Miocene dominated by Taxodium swamp forests that also hosted terrestrial angiosperms such as Nyssa, Betula, Alms and elements of the Myricaceae. Further inland, a mixed deciduous-evergreen forest prevailed. In areas with better drained soils, or on elevated areas, gymnospermous conifer forests prevailed including taxa such as Pinus, Sequoia and Sciadopitys. Overall, the climate in the study area was warm temperate during major parts of the Miocene with mean annual temperatures between 15.5 and 20 degrees C. By employing the Coexistence Approach combined with the method of allocating taxa into standardized climatic groups, four different climatic Miocene events are detected within the studied succession correlated to the coeval climate record of northwestern Europe. The oldest event is a cooling during the earlier Burdigalian, at approximately 19 Ma, coinciding with the MBi-1 oxygen isotope excursion. At ca. 18.5 Ma (in mid-Burdigalian) a warming phase is reconstructed, characterized by the highest precipitation rates observed in the sedimentary succession. A warming trend, starting in the latest Burdigalian, corresponds to the globally recognized Middle Miocene Climatic Optimum (MMCO) while a longer-term late Neogene cooling was initiated in the mid Serravallian, about 13 Ma. (C) 2011 Elsevier B.V. All rights reserved.	[Larsson, Linda M.; Vajda, Vivi] Lund Univ, Dept Earth & Ecosyst Sci, S-22362 Lund, Sweden; [Dybkjaer, Karen; Rasmussen, Erik S.] Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark; [Piasecki, Stefan] Univ Copenhagen, Dept Geog & Geol, DK-1350 Copenhagen K, Denmark; [Utescher, Torsten] Univ Bonn, Steinmann Inst, D-53115 Bonn, Germany	Lund University; Geological Survey Of Denmark & Greenland; University of Copenhagen; University of Bonn	Vajda, V (通讯作者)，Lund Univ, Dept Earth & Ecosyst Sci, Solvegatan 12, S-22362 Lund, Sweden.	vivi.vajda@geol.lu.se	Dybkjær, Karen/G-5223-2018; Vajda, Vivi/N-7693-2018	Vajda, Vivi/0000-0003-2987-5559	Royal Swedish Academy of Sciences through Knut and Alice Wallenbergs Foundation; German Science Foundation [Mo 412/240-1]	Royal Swedish Academy of Sciences through Knut and Alice Wallenbergs Foundation; German Science Foundation(German Research Foundation (DFG))	Stefan Solberg (GEUS) is acknowledged for his professional drafting contributions, improving the figures of this paper. Thomas Persson (LU) is acknowledged for assistance with the Tilia-computer program. We are grateful to D. Ivanov (Sofia) for his support in taxonomical questions. V. Vajda acknowledges the financial support provided by the Royal Swedish Academy of Sciences through Knut and Alice Wallenbergs Foundation. T. Utescher acknowledges the financial support provided by the German Science Foundation (Mo 412/240-1). This study is a contribution to the NECLIME (Neogene climate evolution of Eurasia) network.	Abreu V.S., 1998, Mesozoic and Cenozoic Sequence Stratigraphy of European Basins, V60, P245; [Anonymous], AUSTR COAL GEOLOGY; Ashraf A. R., 1996, Palaeontographica Abteilung B Palaeophytologie, V241, P1; Ashraf A. R., 1995, Palaeontographica Abteilung B Palaeophytologie, V235, P61; Bruch AA, 2007, PALAEOGEOGR PALAEOCL, V253, P1, DOI 10.1016/j.palaeo.2007.03.030; Christensen E. 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Paleoclimatol. Paleoecol.	SEP 1	2011	309	3-4					161	175		10.1016/j.palaeo.2011.05.003	http://dx.doi.org/10.1016/j.palaeo.2011.05.003			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	822TM					2025-03-11	WOS:000295072500002
J	Harding, IC; Smith, GA; Riding, JB; Wimbledon, WAP				Harding, Ian C.; Smith, Giles A.; Riding, James B.; Wimbledon, William A. P.			Inter-regional correlation of Jurassic/Cretaceous boundary strata based on the Tithonian-Valanginian dinoflagellate cyst biostratigraphy of the Volga Basin, western Russia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Latest Jurassic; Early Cretaceous; dinoflagellate cysts; biostratigraphy; correlation; western Russia	JURASSIC-CRETACEOUS BOUNDARY; CALCAREOUS NANNOFOSSILS; MIDDLE; TETHYAN; STRATIGRAPHY; PALYNOLOGY; STAGE; AREA; PALYNOMORPHS; SEQUENCES	Correlation of Jurassic/Cretaceous boundary successions in the Boreal Realm based on ammonite biostratigraphy is problematical due to faunal provincialism. This paper investigates the marine palynology of the Tithonian to Valanginian strata at Gorodishche and Kashpir in western Russia, documenting the ranges of >100 dinoflagellate cyst species used to compile a detailed Tithonian-Valanginian palynostratigraphy for the Volga Basin. Datums of key taxa are used to define ages for unreliably dated strata in the Russian successions by comparison with ranges calibrated to ammonite zones in Boreal northwest Europe. The appearance of Gochteodinia villosa indicates a correlation between the bases of the Late Tithonian Epivirgatites nikitini (ammonite) Zone of the Volga Basin and the Galbanites kerberus Zone of northwest Europe. A dinoflagellate cyst interval zonation, comprising five zones and seven subzones is defined for the Volga Basin. There are notable differences between Tithonian and Berriasian dinoflagellate cyst floras in the Volga Basin and northwest Europe. but Valanginian dinoflagellate cyst assemblages throughout the Northern Hemisphere demonstrate a much more cosmopolitan composition. (C) 2011 Elsevier B.V. All rights reserved.	[Harding, Ian C.] Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England; [Smith, Giles A.; Wimbledon, William A. 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Palynology	SEP	2011	167	1-2					82	116		10.1016/j.revpalbo.2011.07.002	http://dx.doi.org/10.1016/j.revpalbo.2011.07.002			35	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	843SK		Green Accepted			2025-03-11	WOS:000296692700007
J	Valentine, A; Johnson, ALA; Leng, MJ; Sloane, HJ; Balson, PS				Valentine, Annemarie; Johnson, Andrew L. A.; Leng, Melanie J.; Sloane, Hilary J.; Balson, Peter S.			Isotopic evidence of cool winter conditions in the mid-Piacenzian (Pliocene) of the southern North Sea Basin	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palaeoclimate; Pliocene; Mid-Piacenzian; Sclerochronology; Oxygen isotopes; Bivalves	DINOFLAGELLATE CYST STRATIGRAPHY; CLIMATE; SEASONALITY; RECORDS; RECONSTRUCTION; PALEOECOLOGY; DELTA-O-18; PROFILES; PATTERNS; GROWTH	Oxygen isotope thermometry of Aequipecten opercularis and Atrina fragilis bivalves (which demonstrate all-year growth), provides quantitative evidence of cool-temperate winter conditions (below 10 degrees C) during deposition of the mid-Piacenzian Oorderen Sands and time-equivalent strata in the southern North Sea Basin (SNSB). Isotopic summer temperatures (seafloor) are within or only marginally above, the cool-temperate range (upper limit 20 degrees C). The occurrence of warm-temperate dinoflagellate cysts alongside (and presumably contemporaneous with) the bivalves, indicates the development of a correspondingly warm surface layer in summer (encystment allowing the dinoflagellates to survive cool winter conditions).This evidence of greater surface seasonality than now is consistent with greater global warmth and a reduction in the vigour of the Gulf Stream/North Atlantic Drift (GS/NAD), leading to a reduced supply of winter heat. This reduction in GS/NAD strength may be linked to breaching of the emerging Isthmus of Panama. (C) 2011 Elsevier B.V. All rights reserved.	[Valentine, Annemarie; Johnson, Andrew L. A.] Univ Derby, Sch Sci, Derby DE22 1GB, England; [Leng, Melanie J.; Sloane, Hilary J.] British Geol Survey, NERC Isotope Geosci Lab, Nottingham NG12 5GG, England	University of Derby; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Valentine, A (通讯作者)，Univ Derby, Sch Sci, Kedleston Rd, Derby DE22 1GB, England.	A.Valentine@derby.ac.uk	; Johnson, Andrew/ABC-1334-2021	Leng, Melanie/0000-0003-1115-5166; Sloane, Hilary/0000-0001-7965-5429; Johnson, Andrew/0000-0001-5727-1889	University Funding Initiative [BUFI S157]; University of Derby; NERC [nigl010001, bgs05009] Funding Source: UKRI	University Funding Initiative; University of Derby; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We are very grateful to Robert Marquet, Etienne Steurbaut and Frank Wesselingh for donating specimens from the Museum des Sciences naturelles, Brussels, and Naturalis Museum, Leiden, for analysis; to the NERC Isotope Geosciences Facilities Steering Committee for granting analytical services (IP-1108-0509. IP-1155-1109); to the British Geological Survey, University Funding Initiative for financial support to AV (BUFI S157); to the Alexander von Humboldt Foundation for support of a sabbatical stay at the University of Mainz by ALAJ; and to the Research-Inspired Curriculum Fund of the University of Derby for provision of travel funds to AV and ALAJ. Steve Hodson and Steve Taylor (University of Derby) provided a professional service in design of figures and in photography, respectively.	Broecker WS, 1997, SCIENCE, V278, P1582, DOI 10.1126/science.278.5343.1582; Buchardt B, 2003, PALAEOGEOGR PALAEOCL, V189, P71, DOI 10.1016/S0031-0182(02)00594-1; Carter J.G., 1990, SKELETAL BIOMINERALI, V2, P1; *CONCH SOC GREAT B, 2008, ENC BRIT MOLL ATR FR; De Schepper S, 2009, PALEOCEANOGRAPHY, V24, DOI 10.1029/2008PA001725; De Schepper S, 2009, GEOL MAG, V146, P92, DOI 10.1017/S0016756808005438; Denny M W., 2008, How the ocean works: An introduction to oceanography; DICKSON JAD, 1966, J SEDIMENT PETROL, V36, P491; Dowsett HJ, 2007, DEEP-TIME PERSPECTIVES ON CLIMATE CHANGE: MARRYING THE SIGNAL FROM COMPUTER MODELS AND BIOLOGICAL PROXIES, P459; Dowsett H. 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Paleoclimatol. Paleoecol.	AUG 15	2011	309	1-2			SI		9	16		10.1016/j.palaeo.2011.05.015	http://dx.doi.org/10.1016/j.palaeo.2011.05.015			8	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	810RF					2025-03-11	WOS:000294144100002
J	De Schepper, S; Fischer, EI; Groeneveld, J; Head, MJ; Matthiessen, J				De Schepper, Stijn; Fischer, Eva I.; Groeneveld, Jeroen; Head, Martin J.; Matthiessen, Jens			Deciphering the palaeoecology of Late Pliocene and Early Pleistocene dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinocyst; Transfer function; Palaeoecology; North Atlantic; Mg/Ca geochemistry; Quaternary	SEA-SURFACE TEMPERATURE; EASTERN NORTH-ATLANTIC; QUATERNARY SYSTEM/PERIOD; FORMAL RATIFICATION; VERTICAL MIGRATION; HIGH-LATITUDES; SINGA SECTION; UPPER MIOCENE; MID-PLIOCENE; LONG-TERM	In an attempt to document the palaeoecological affinities of individual extant and extinct dinoflagellate cysts, Late Pliocene and Early Pleistocene dinoflagellate cyst assemblages have been compared with geochemical data from the same samples. Mg/Ca ratios of Globigerina bulloides were measured to estimate the spring-summer sea-surface temperatures from four North Atlantic IODP/DSDP sites. Currently, our Pliocene-Pleistocene database contains 204 dinoflagellate cyst samples calibrated to geochemical data. This palaeo-database is compared with modern North Atlantic and global datasets. The focus lies in the quantitative relationship between Mg/Ca-based (i.e. spring-summer) sea-surface temperatures (SSTMg/Ca) and dinoflagellate cyst distributions. In general, extant species are shown to have comparable spring-summer SST ranges in the past (SSTMg/Ca) and today (SST from World Ocean Atlas 2005. Locarnini et al., 2006). demonstrating that our new approach is valid for inferring spring-summer SST ranges for extinct species. For example. Habibacysta tectata represents SSTMg/Ca values between 10 and 15 degrees C when it exceeds 30% of the assemblage, and Invertocysta lacrymosa exceeds 15% when SSTMg/Ca values are between 18.6 and 23.5 degrees C. However, comparing Pliocene and Pleistocene SSTMg/Ca, values with present day summer values for the extant Impagidinium pallidum suggests a greater tolerance of higher temperatures in the past. This species occupies more than 5% of the assemblage at SSTMg/Ca values of 11.6-17.9 degrees C in the Pliocene and Pleistocene, whereas present day summer SSTs are around - 1.7 to 6.9 degrees C. This observation questions the value of Impagidinium pallidum as reliable indicator of cold waters in older deposits, and may explain its bipolar distribution. (C) 2011 Elsevier B.V. All rights reserved.	[De Schepper, Stijn] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Fischer, Eva I.; Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Groeneveld, Jeroen; Matthiessen, Jens] Alfred Wegener Inst, D-27568 Bremerhaven, Germany	University of Bremen; Brock University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	De Schepper, S (通讯作者)，Univ Bergen, Dept Earth Sci, POB 7803, N-5020 Bergen, Norway.	smad2@cantab.net	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914; Matthiessen, Jens/0000-0002-6952-2494	Deutsche Forschungsgemeinschaft (DFG) International Graduate College EUROPROX; DFG [SCHE 1665/2-1, 1665/2-2, MA 3913/2-1]; Natural Sciences and Engineering Research Council (Canada) Discovery	Deutsche Forschungsgemeinschaft (DFG) International Graduate College EUROPROX(German Research Foundation (DFG)); DFG(German Research Foundation (DFG)); Natural Sciences and Engineering Research Council (Canada) Discovery(Natural Sciences and Engineering Research Council of Canada (NSERC))	IODP is thanked for providing samples. Laboratory assistance by S. Van Cauwenberghe, M. Zwick and S. Forke is greatly appreciated. P.M. Langebroek kindly helped with the plotting of figures. D. Heslop is thanked for assistance with the statistics. Funding to SDS from the Deutsche Forschungsgemeinschaft (DFG) International Graduate College EUROPROX allowed the initiation of this work. Further funding to SDS (DFG grant SCHE 1665/2-1, 1665/2-2) and JM (DFG grant MA 3913/2-1), and a Natural Sciences and Engineering Research Council (Canada) Discovery Grant to MJH are gratefully acknowledged. T. Radi and one anonymous reviewer improved the manuscript with their constructive comments.	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Assoc. Strat. Palynologists Contribution Series, V17, P169	103	50	51	1	14	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	AUG 15	2011	309	1-2			SI		17	32		10.1016/j.palaeo.2011.04.020	http://dx.doi.org/10.1016/j.palaeo.2011.04.020			16	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	810RF					2025-03-11	WOS:000294144100003
J	Verhoeven, K; Louwye, S; Eiríksson, J; De Schepper, S				Verhoeven, Koen; Louwye, Stephen; Eiriksson, Jon; De Schepper, Stijn			A new age model for the Pliocene-Pleistocene Tjornes section on Iceland: Its implication for the timing of North Atlantic-Pacific palaeoceanographic pathways	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pliocene; Dinoflagellate cysts; Tjornes; Iceland; Biostratigraphy; Age model; Bering Strait	DINOFLAGELLATE CYST; ARCTIC-OCEAN; SEDIMENTS; MIOCENE; CIRCULATION; QUATERNARY; PLIOPLEISTOCENE; STRATIGRAPHY; ZONATION; BELGIUM	The Plio-Pleistocene outcrops of the Tjornes peninsula in northern Iceland present a unique section in which near-shore and terrestrial deposits alternate with lava flows. This section plays an important role in the correlation of climate signals from around the North Atlantic, but a solid age model has not been available for the entire sequence due to problematic K/Ar dating and incompletely recorded palaeomagnetic signal. A palynological analysis with dinoflagellate cysts of 68 samples from the homes beds and twenty samples from the younger Breidavik Group was carried out in order to establish an age model for the Tjornes section, independent of the available K/Ar ages. The dinoflagellate cyst record of the Tjornes beds consists mainly of Pliocene taxa and indicates most probably a post-Miocene age for the Tapes and Mactra Zones of the Mimes beds. Both Operculodinium tegillatum and Batiacasphaera minuta, which have a highest occurrence near the top of the Zanclean at c. 3.8 Ma. were present in the section up to the middle of the Serripes Zone. Reticulatosphaera actinocoronata. with a highest occurrence around 4.4 Ma, was recorded in situ at the base of the Serripes Zone. This suggests that the entire Serripes Zone was deposited between c. 4.0 and 4.5 Ma. Further, the normal polarities below and above the Skeifa lavas in the Serripes Zone were consequently linked to the Nunivak and Cochiti Subchron respectively. The entire Tjornes beds were likely deposited in the Early Pliocene. before c. 4.0 Ma. The Breidavik Group is deposited much later in the Quaternary, from just before the Olduvai Subchron at c. 2.2 Ma. The Gilbert/Gauss transition is located between the Tjornes beds and the Hoskuldsvik lavas and the Gauss/Matuyama transition between the Furuvik and Horgi Formations. The exact position of both reversals is not preserved because two appreciable hiatuses of c. 600 kyr up to maximally 900 kyr occur at these locations. According to the new age model, the major invasion of Pacific molluscs at the base of the Serripes Zone took place before 3.8 Ma. In combination with the palaeopolarity data, this event can be placed in the Nunivak Subchron at c. 4.5 Ma. The invasion is likely a result of the northward flow of Pacific waters through the Bering Strait to the North Atlantic. which may have been caused by the shoaling of the Central American seaway between 4.7 and 4.2 Ma (Sarnthein et al., 2009). (C) 2011 Elsevier B.V. All rights reserved.	[Verhoeven, Koen; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Eiriksson, Jon] Univ Iceland, Inst Earth Sci, IS-101 Reykjavik, Iceland; [De Schepper, Stijn] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	Ghent University; University of Iceland; University of Bremen	Verhoeven, K (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	Koen.Verhoeven@UGent.be	Verhoeven, Koen/IZP-9609-2023; Louwye, Stephen/D-3856-2012; Eiriksson, Jon/J-4262-2014; De Schepper, Stijn/A-2836-2011	Louwye, Stephen/0000-0003-4814-4313; Eiriksson, Jon/0000-0001-5598-2417; De Schepper, Stijn/0000-0002-6934-0914	Deutsche Forschungsgemeinschaft [SCHE 1665/2-1, SCHE 1665/2-2]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	This study was carried out in the framework of the assistantship of IN in the Research Unit of Palaeontology at Ghent University. Stimulating discussions with Karen Luise Knudsen, Andy Johnson, Morton Smelror and Thomas Verleye are much appreciated. Fridgeir Grimsson is kindly thanked for providing test samples of the Tjornes section. Margret Hallsdottir and the library staff of the Icelandic Institute of Natural History are thanked for their kind assistance in preparing the field campaign. Martin Head and Jens Mattiessen are kindly thanked for their meticulous review of the manuscript and their constructive and stimulating comments. The linguistic remarks by Achilles Gautier are much appreciated. SDS acknowledges funding from the Deutsche Forschungsgemeinschaft (DFG grants SCHE 1665/2-1 and 2-2).	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Paleoclimatol. Paleoecol.	AUG 15	2011	309	1-2			SI		33	52		10.1016/j.palaeo.2011.04.001	http://dx.doi.org/10.1016/j.palaeo.2011.04.001			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	810RF					2025-03-11	WOS:000294144100004
J	Long, PE; Zalasiewicz, JA				Long, Peter E.; Zalasiewicz, Jan A.			The molluscan fauna of the Coralline Crag (Pliocene, Zanclean) at Raydon Hall, Suffolk, UK: Palaeoecological significance reassessed	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Molluscs; Pliocene; Coralline Crag; Ecology; Environment; Taphonomy	SOUTHERN NORTH-SEA; DINOFLAGELLATE CYST STRATIGRAPHY; ARCTICA-ISLANDICA; EARLY PLEISTOCENE; BASIN; PALEOGEOGRAPHY; BELGIUM; CLIMATE	This study assesses the environmental implications of a quantitative study of the unusually well preserved molluscan fauna of over 200 species (about 47% extinct) from six samples from both the Ramsholt and Sudbourne Members of the Coralline Crag Formation at a British Geological Survey borehole at Raydon Hall, near Orford, Suffolk, UK. It reveals a shallow shelf fauna locally transported from a variety of habitats dominated by infaunal species (Spisula, Turritella, Abra, Amyclina) from relatively fine sediments, plus epifauna (especially Heteranomia) possibly in part originating from nearby bryozoan communities as well as dead bivalve shells. There was a small but consistent component of deeper water elements, such as Limopsis, and a lack of strictly littoral species. Overall, a water depth of about 50 m is suggested, with bottom temperatures at times perhaps warmer than the present southern North Sea (but not as high as the modern Mediterranean), and a more oceanic setting. This is in contrast to inferences from previous nineteenth century studies of Coralline Crag molluscs, which viewed it as largely Mediterranean in character, but understated the regular presence of boreal forms such as Arctic. Current interpretations still have to account for the coexistence of some Lusitanian or Mediterranean molluscan taxa alongside the cooler water elements. (C) 2011 Elsevier B.V. All rights reserved.	[Long, Peter E.] Univ Leicester, Dept Biol, Leicester LE1 7RH, Leics, England; [Long, Peter E.] Univ Leicester, Dept Adult Educ, Leicester LE1 7RH, Leics, England; [Zalasiewicz, Jan A.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England	University of Leicester; University of Leicester; University of Leicester	Zalasiewicz, JA (通讯作者)，242 Astill Lodge Rd, Leicester LE4 1EF, Leics, England.	pel2@le.ac.uk						Aartsen J. J., 1984, BASTERIA S, P1; ALMON WD, 1988, PALAIOS, V3, P259; ALTENA C. O. 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S., 1931, P1; WYATT HV, 1961, J ANIM ECOL, V30, P283, DOI 10.2307/2299	105	16	18	0	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	AUG 15	2011	309	1-2			SI		53	72		10.1016/j.palaeo.2011.05.039	http://dx.doi.org/10.1016/j.palaeo.2011.05.039			20	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	810RF					2025-03-11	WOS:000294144100005
J	Salzmann, U; Riding, JB; Nelson, AE; Smellie, JL				Salzmann, Ulrich; Riding, James B.; Nelson, Anna E.; Smellie, John L.			How likely was a green Antarctic Peninsula during warm Pliocene interglacials? A critical reassessment based on new palynofloras from James Ross Island	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Pliocene; Antarctica; Vegetation; Pollen; Dinoflagellate; Neogene; Antarctic Peninsula	GLACIOEUSTATIC SEDIMENTARY CYCLES; CAPE-ROBERTS PROJECT; VICTORIA LAND BASIN; SIRIUS GROUP; ICE-SHEET; LATE NEOGENE; TRANSANTARCTIC MOUNTAINS; GLACIAL HISTORY; PALYNOLOGY; CLIMATE	The question of whether Pliocene climate was warm enough to support a substantial vegetation cover on Antarctica is of great significance to the ongoing and controversial debate on the stability or dynamism of Antarctic ice sheets during warm periods with high atmospheric greenhouse gas concentrations. Here we present a systematic palynological comparison of pollen and dinoflagellate cyst assemblages from Early Pliocene diamictites and underlying late Cretaceous sediments collected from James Ross Island, northern Antarctic Peninsula. The diamictites are dated using a combination of 40Ar/39Ar and Sr-87/Sr-86 isotope ages on interbedded lavas and pristine bivalves. Well preserved pectinid shells and cheilostome bryozoans suggest that the palynomorph-bearing sediments were probably deposited during warmer Pliocene interglacials and later amalgamated into a diamictite formed by a major ice advance during cold glacial cycle. The palynological analyses presented herein do not identify any in-situ pollen and spores which indicate the presence of a substantial vegetation cover. Our study suggests a local (i.e. James Ross Island) provenance for most of the diamictites, whilst sediments from the western coast might have been delivered by ice sheets from the Antarctic Peninsula. Whilst the acritarch Leiosphaeridia might imply the presence of sea-ice and near-modern climate conditions during the Late Neogene, the presence of the dinoflagellate cyst Bitectatodinium tepikiense at one location suggests that sea surface temperatures might have been substantially warmer during some interglacials. The absence of in-situ pollen and spores in the James Ross Island diamictites cannot be taken as proof of non-existence of vegetation. However, the combined palynological and geological evidence presented in this paper makes the presence of a substantial Pliocene vegetation cover on James Ross Island unlikely and supports previous reconstructions of a permanent ice sheet on the Antarctic Peninsula throughout the Late Neogene. (C) 2011 Elsevier B.V. All rights reserved.	[Salzmann, Ulrich] Northumbria Univ, Sch Built & Nat Environment, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England; [Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England; [Nelson, Anna E.] British Antarctic Survey, Cambridge CB3 0ET, England; [Smellie, John L.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England	Northumbria University; 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 Leicester	Salzmann, U (通讯作者)，Northumbria Univ, Sch Built & Nat Environment, Ellison Bldg, Newcastle Upon Tyne NE1 8ST, Tyne & Wear, England.	ulrich.salzmann@northumbria.ac.uk; j.riding@bgs.ac.uk; annaelizabethlaloe@googlemail.com; jls55@le.ac.uk	Salzmann, Ulrich/H-9929-2017	Salzmann, Ulrich/0000-0001-5598-5327	Natural Environment Research Council (NERC); NERC [bgs010024, bas0100026] Funding Source: UKRI	Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was financed by the Natural Environment Research Council (NERC) and was part of the British Antarctic Survey's GEACEP Programme (2005-2009; ISODYN Project), which investigated the greenhouse to ice-house climate change throughout the Neogene. This paper also contributes to the SCAR ACE (Antarctic Climate Evolution) programme. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	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Paleoclimatol. Paleoecol.	AUG 15	2011	309	1-2			SI		73	82		10.1016/j.palaeo.2011.01.028	http://dx.doi.org/10.1016/j.palaeo.2011.01.028			10	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	810RF					2025-03-11	WOS:000294144100006
J	Heinrich, S; Zonneveld, KAF; Bickert, T; Willems, H				Heinrich, Sonja; Zonneveld, Karin A. F.; Bickert, Torsten; Willems, Helmut			The Benguela upwelling related to the Miocene cooling events and the development of the Antarctic Circumpolar Current: Evidence from calcareous dinoflagellate cysts	PALEOCEANOGRAPHY			English	Article							SOUTH-ATLANTIC-OCEAN; ATMOSPHERIC CARBON-DIOXIDE; UPPER WATER COLUMN; SURFACE SEDIMENTS; EQUATORIAL ATLANTIC; MIDDLE MIOCENE; ODP SITE-1085; AGULHAS RETROFLECTION; QUATERNARY EASTERN; THERMOCLINE WATER	Sediment samples from ODP Site 1085 were investigated in order to obtain more information on the initiation and development of the Benguela upwelling system during the middle and upper Miocene. In particular, our intent was to establish the causes of the upwelling as well as the response of the upwelling regime to the development of the Antarctic Circumpolar Current. Based on changes in the calcareous dinoflagellate cyst association, we found an initial increase of the dinoflagellate cyst productivity, probably related to the initiation of upwelling about 11.8 Ma ago. Two distinct increases in cyst productivity in conjunction with temperature decreases of the upper water masses reflect upwelling pulses off Namibia and occur at the end of the Miocene cooling events Mi5 (about 11.5 Ma) and Mi6 (about 10.5 Ma). Both cooling events are associated with an ice volume increase in Antarctica and are thought to have led to an increase in southeasterly winds, possibly causing these two upwelling pulses. We demonstrate a decrease in dinoflagellate cyst productivity and enhanced terrigenous input via the Orange River after the Mi5 event. At about 11.1 Ma, the dinoflagellate cyst productivity increases again. The polar cyst species Caracomia arctica occurs here for the first time. This implies an influence of subantarctic mode water and therefore a change in the quality of the upwelling water which allowed the Benguela upwelling to develop into modern conditions. From about 10.4 Ma, C. arctica forms a permanent part of the association, pointing to an establishment of the upwelling regime.	[Heinrich, Sonja; Zonneveld, Karin A. F.; Willems, Helmut] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Bickert, Torsten] Marum Ctr Marine Environm Sci, D-28359 Bremen, Germany	University of Bremen; University of Bremen	Heinrich, S (通讯作者)，Univ Bremen, Dept Geosci FB5, D-28359 Bremen, Germany.	sonja.heinrich@uni-bremen.de		Heinrich, Sonja/0000-0001-7536-0017	Deutsche Forschungs Gemeinschaft International Graduate College	Deutsche Forschungs Gemeinschaft International Graduate College	Thanks are given to Petra Witte for her help with the SEM analyses. We thank Lieselotte Diester-Haass for providing data on the carbon and coarse fraction of the sediments from ODP Site 1085, as well as foraminiferal accumulation rates. Thanks to Thomas Westerhold for making available the data for the age model. We thank Kara Bogus for improving the language. We gratefully acknowledge thoughtful comments from Christopher Charles, one anonymous editor, and two anonymous reviewers. This work was funded through the Deutsche Forschungs Gemeinschaft International Graduate College "Proxies in Earth History" program.	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F., 2005, Palaeontologische Zeitschrift, V79, P61	78	33	34	0	15	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA	0883-8305			PALEOCEANOGRAPHY	Paleoceanography	AUG 3	2011	26								PA3209	10.1029/2010PA002065	http://dx.doi.org/10.1029/2010PA002065			11	Geosciences, Multidisciplinary; Oceanography; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography; Paleontology	804GJ		Bronze			2025-03-11	WOS:000293642000002
J	Svobodová, M; Svábenická, L; Skupien, P; Hradecká, L				Svobodova, Marcela; Svabenicka, Lilian; Skupien, Petr; Hradecka, Lenka			Biostratigraphy and paleoecology of the Lower Cretaceous sediments in the Outer Western Carpathians (Silesian Unit, Czech Republic)	GEOLOGICA CARPATHICA			English	Article						Lower Cretaceous; Outer Western Carpathians; Czech Republic; Silesian Unit; paleoecology; biostratigraphy; microfossils	PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYST; STRATIGRAPHY; FRANCE; BASIN	Almost black shale filling fissures in the Stramberk Limestone belonging to the Silesian Unit, Outer Western Carpathians contain prolific and poorly to moderately well preserved spores, pollen, organic-walled dinoflagellate cysts, foraminifers, and calcareous nannofossils. A detailed micropaleontological analysis of the proved stratigraphical interval from the Valanginian to the Albian indicated sedimentary conditions of brackish, restricted marine, shallow-marine and neritic sedimentation. Moreover, it drew attention to occasional influence from the Boreal province in the depositional area of the NW part of Tethys, especially during the Early Valanginian and Hauterivian, as supported by the presence of high-latitude nannofossils and organic-walled dinoflagellate cysts. Terrestrial miospores form a significant component of palynoassemblages and give evidence of continent proximity in the Valanginian-Barremian interval. Samples were acquired from isolated fissure fills in the Stramberk Limestone and, therefore, they do not represent a continuous section.	[Svobodova, Marcela] Inst Geol AS CR, VVI, Prague 16500 6, Czech Republic; [Svabenicka, Lilian; Hradecka, Lenka] Czech Geol Survey, Prague 11821 1, Czech Republic; [Skupien, Petr] VSB Tech Univ Ostrava, Inst Geol Engn, Ostrava 70833, Czech Republic	Czech Academy of Sciences; Institute of Geology of the Czech Academy of Sciences; Czech Geological Survey; Technical University of Ostrava	Svobodová, M (通讯作者)，Inst Geol AS CR, VVI, Rozvojova 269, Prague 16500 6, Czech Republic.	msvobodova@gli.cas.cz; lilian.svabenicka@geology.cz; petr.skupien@vsb.cz; lenka.hradecka@geology.cz	Svobodova, Marcela/I-8793-2014; Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X	Grant Agency of the Czech Republic [205/01/1582]; Institute of Geology AS CR; VSB-TU Ostrava [AV0Z30130516]; Czech Geological Survey [MZP 0002579801];  [MSM 6198910019]	Grant Agency of the Czech Republic(Grant Agency of the Czech RepublicNorwegian Agency for Development Cooperation - NORAD); Institute of Geology AS CR(Czech Academy of Sciences); VSB-TU Ostrava; Czech Geological Survey; 	This study was a contribution to the Grant Project No. 205/01/1582, supported by the Grant Agency of the Czech Republic and the research programmes of the Institute of Geology AS CR, v.v.i., AV0Z30130516, of the VSB-TU Ostrava, MSM 6198910019, and of the Czech Geological Survey, MZP 0002579801. The authors thank Ing. A. Langrova, Ing. Z. Korbelova, Institute of Geology AS CR,v.v.i., for CAM-ECA photomicrographs (palynomorphs) and Ing. Gabasova, Czech Geological Survey (foraminifera). Suggestions and fruitful comments of the reviewers Prof. I. Premoli Silva, Prof. A. Wierzbowski and an anonymous reviewer who helped us improve the manuscript. We thank Ing. L. Stasek, Ing. V. Stocek and Ing. J. Monsport (Kotouc Stramberk Ltd.) for the possibility to collect samples in the Kotouc Quarry.	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Carpath.	AUG	2011	62	4					309	332		10.2478/v10096-011-0024-9	http://dx.doi.org/10.2478/v10096-011-0024-9			24	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	817GU		gold			2025-03-11	WOS:000294660100002
J	Hofmann, CC; Mohamed, O; Egger, H				Hofmann, Christa-Ch.; Mohamed, Omar; Egger, Hans			A new terrestrial palynoflora from the Palaeocene/Eocene boundary in the northwestern Tethyan realm (St. Pankraz, Austria)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Palaeocene/Eocene-boundary; dinoflagellates; calcareous nannoplankton; pollen and spores; Eastern Alps	EOCENE THERMAL MAXIMUM; LATE PALEOCENE; POLLEN MORPHOLOGY; SEA-LEVEL; CARBON; VEGETATION; CLIMATE; OCEAN; CLASSIFICATION; EXTINCTION	Inner neritic many claystone of the South-Helvetic thrust unit (Eastern Alps) at St. Pankraz (Salzburg, Austria) yields high percentages of the dinoflagellate genus Apectodinium including the species Apectodinium augustum. The range of this species is almost exclusively restricted to the negative carbon isotope excursion (CIE) at the base of the Eocene. The associated terrestrial palynoflora consists of common Normapolles s.I. and post-Normapolles types with accessory mesothermal and megathermal families such as Anacardiaceae, Arecaceae, Euphorbiaceae s.I., Hamamelidaceae. Icacinaceae, Malvaceae (subfamilies of Helicteroideae, Sterculoideae, Tiloideae), Rutaceae, Sapotaceae and Schizaeales. This composition is similar to the Upper Thanetian palynological record of the same sedimentary succession. It suggests a warm and humid climate in the northwestern Tethyan realm during the Late Thanetian and Early Ypresian. Three new taxa probably have their lowermost occurrence in the basal Eocene. However, neither a major floral change nor the establishment of fully tropical conditions are indicated for the Palaeocene-Eocene transition. (C) 2011 Elsevier B.V. All rights reserved.	[Hofmann, Christa-Ch.] Univ Vienna, Dept Palaeontol, Vienna, Austria; [Mohamed, Omar] Graz Univ, Inst Earth Sci Geol & Palaeontol, A-8010 Graz, Austria; [Mohamed, Omar] Menia Univ, Fac Sci, Dept Geol, El Minia, Egypt; [Egger, Hans] Geol Survey Austria, A-1030 Vienna, Austria	University of Vienna; University of Graz; Egyptian Knowledge Bank (EKB); Minia University	Hofmann, CC (通讯作者)，Univ Vienna, Dept Palaeontol, Althanstr 14, Vienna, Austria.	christa.hofmann@univie.ac.at; omaraosman@yahoo.com; hans.egger@geologie.ac.at						[Anonymous], LATE PALAEOCENE EARL; [Anonymous], MICROPALAEONTOLOGICA; Aubry MP, 2007, EPISODES, V30, P271, DOI 10.18814/epiiugs/2007/v30i4/003; BOGNER J, ZITTELIANA A, V47, P133; Collinson M.E., 2003, Causes and Consequences of Globally Warm Climates in the Early Paleogene, V369, P333; Collinson ME, 2009, GRANA, V48, P38, DOI 10.1080/00173130802707980; Crouch EM, 2003, PALAEOGEOGR PALAEOCL, V194, P387, DOI 10.1016/S0031-0182(03)00334-1; Crouch EM, 2001, GEOLOGY, V29, P315, DOI 10.1130/0091-7613(2001)029<0315:GDEAWT>2.0.CO;2; Crouch Erica M., 2003, Geological Society of America Special Paper, V369, P113; Denk T, 2006, GRANA, V45, P195, DOI 10.1080/00173130600873901; Denk T, 2009, INT J PLANT SCI, V170, P926, DOI 10.1086/600134; Dickens GR, 2004, NATURE, V429, P513, DOI 10.1038/429513a; DICKENS GR, 1995, PALEOCEANOGRAPHY, V10, P965, DOI 10.1029/95PA02087; Domingo L, 2009, EARTH PLANET SC LETT, V281, P226, DOI 10.1016/j.epsl.2009.02.025; DRAXLER I, 2007, JB GEOLOGISCHE BUNDE, V147, P367; Egger H, 2000, B SOC GEOL FR, V171, P207, DOI 10.2113/171.2.207; Egger H, 2009, GEOL ACTA, V7, P215, DOI 10.1344/105.000000266; EGGER H, 1997, JB GEOLOGISCHEN BUND, V140, P29; Fensome R.A., 2008, DINOFLAJ2, Version 1; FRIIS EM, 2003, INT J PLANT SC S, V164, P210; Gibbs SJ, 2006, SCIENCE, V314, P1770, DOI 10.1126/science.1133902; Gingerich PD, 2006, TRENDS ECOL EVOL, V21, P246, DOI 10.1016/j.tree.2006.03.006; Harrington GJ, 2007, J GEOL SOC LONDON, V164, P323, DOI 10.1144/0016-76492006-027; Heilmann-Clausen C, 2000, GFF, V122, P69, DOI 10.1080/11035890001221069; HEILMANNCLAUSEN C, 1997, 13 DANM GRONL UND; Hofmann Christa-Charlotte, 2001, Palaeontographica Abteilung B Palaeophytologie, V259, P47; Jaramillo C, 2010, SCIENCE, V330, P957, DOI 10.1126/science.1193833; KEDVES M, 1968, Pollen et Spores, V10, P117; KEDVES M, 1968, POLLEN SPORES, V10, P385; Kedves M., 1982, PALAEONTOGR ABT B, V182, P87; KEDVES M, 1996, PLANT CELL BIOL DEV, V7, P37; KEDVES M, 1960, POLLEN SPORES, V2, P101; KEDVES M, 1961, POLLEN SPORES, V3, P89; KEDVES M, 1969, PALYNOLOGICAL STUDIE; KEDVES M, 1969, POLLEN SPORES, V12, P83; Kedves M., 1996, PLANT CELL BIOL DEV, V7, P13; Kent DV, 2003, EARTH PLANET SC LETT, V211, P13, DOI 10.1016/S0012-821X(03)00188-2; Kopp RE, 2007, PALEOCEANOGRAPHY, V22, DOI 10.1029/2007PA001473; Kottek M, 2006, METEOROL Z, V15, P259, DOI 10.1127/0941-2948/2006/0130; Krutzsch W., 1961, Berichte Geologische Gesellschaft, V5, P290; Krutzsch W., 1977, PALAEONTOGR ABT B, V163, P1; KRUTZSCH W, 1962, ATLAS MITTEL JUNGTER, V1; Kurtz AC, 2003, PALEOCEANOGRAPHY, V18, DOI 10.1029/2003PA000908; Kvacek J, 2004, REV PALAEOBOT PALYNO, V128, P323, DOI 10.1016/S0034-6667(03)00154-4; Kvacek Z, 2010, B GEOSCI, V85, P63, DOI 10.3140/bull.geosci.1146; Lippert PC, 2007, PALEOCEANOGRAPHY, V22, DOI 10.1029/2007PA001471; LU GY, 1993, MAR MICROPALEONTOL, V21, P101, DOI 10.1016/0377-8398(93)90012-M; Luterbacher H., 2000, NEWSL INT SUBCOMM PA, V9, P13; Manchester SR, 1999, ANN MO BOT GARD, V86, P472, DOI 10.2307/2666183; Manchester SR, 2009, J SYST EVOL, V47, P1, DOI 10.1111/j.1759-6831.2009.00001.x; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; NILSSON S, 1986, WORLD POLLEN SPORE F, V14; Nowicke JW, 1999, REV PALAEOBOT PALYNO, V105, P1, DOI 10.1016/S0034-6667(98)00069-4; Panchuk K, 2008, GEOLOGY, V36, P315, DOI 10.1130/G24474A.1; Raffi I, 2009, MAR MICROPALEONTOL, V70, P201, DOI 10.1016/j.marmicro.2008.12.005; Röhl U, 2007, GEOCHEM GEOPHY GEOSY, V8, DOI 10.1029/2007GC001784; Rogl F., 1983, Ann. 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Palaeobot. Palynology	AUG	2011	166	3-4					295	310		10.1016/j.revpalbo.2011.06.003	http://dx.doi.org/10.1016/j.revpalbo.2011.06.003			16	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	815NI					2025-03-11	WOS:000294531900009
J	Tomaru, Y; Takao, Y; Suzuki, H; Nagumo, T; Koike, K; Nagasaki, K				Tomaru, Yuji; Takao, Yoshitake; Suzuki, Hidekazu; Nagumo, Tamotsu; Koike, Kanae; Nagasaki, Keizo			Isolation and Characterization of a Single-Stranded DNA Virus Infecting <i>Chaetoceros lorenzianus</i> Grunow	APPLIED AND ENVIRONMENTAL MICROBIOLOGY			English	Article							DINOFLAGELLATE HETEROCAPSA-CIRCULARISQUAMA; RESTING SPORE FORMATION; GROWTH-CYCLE; BLOOM; BAY	Diatoms are one of the most significant primary producers in the ocean, and the importance of viruses as a potential source of mortality for diatoms has recently been recognized. Thus far, eight different diatom viruses infecting the genera Rhizosolenia and Chaetoceros have been isolated and characterized to different extents. We report the isolation of a novel diatom virus (ClorDNAV), which causes the lysis of the bloom-forming species Chaetoceros lorenzianus, and show its physiological, morphological, and genomic characteristics. The free virion was estimated to be similar to 34 nm in diameter. The arrangement of virus particles appearing in cross-section was basically a random aggregation in the nucleus. Occasionally, distinctive formations such as a ring-like array composed of 9 or 10 spherical virions or a centipede-like array composed of rod-shaped particles were also observed. The latent period and the burst size were estimated to be <48 h and 2.2 x 10(4) infectious units per host cell, respectively. ClorDNAV harbors a covalently closed circular single-stranded DNA (ssDNA) genome (5,813 nucleotides [nt]) that includes a partially double-stranded DNA region (979 nt). At least three major open reading frames were identified; one showed a high similarity to putative replicase-related proteins of the other ssDNA diatom viruses, Chaetoceros salsugineum DNA virus (previously reported as CsNIV) and Chaetoceros tenuissimus DNA virus. ClorDNAV is the third member of the closed circular ssDNA diatom virus group, the genus Bacilladnavirus.	[Tomaru, Yuji; Nagasaki, Keizo] Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, Hiroshima 7390452, Japan; [Takao, Yoshitake] Fukui Prefectural Univ, Dept Marine Biosci, Fukui 9170003, Japan; [Suzuki, Hidekazu] Tokyo Univ Marine Sci & Technol, Dept Ocean Sci, Minato Ku, Tokyo 1088477, Japan; [Nagumo, Tamotsu] Nippon Dent Univ Tokyo, Dept Biol, Chiyoda Ku, Tokyo 1029159, Japan; [Koike, Kanae] Hiroshima Univ, Ctr Gene Sci, Transmiss Elect Microscopy Serv, Hiroshima 7398527, Japan	Japan Fisheries Research & Education Agency (FRA); Fukui Prefectural University; Tokyo University of Marine Science & Technology; Nippon Dental University; Hiroshima University	Tomaru, Y (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Fisheries Res Agcy, 2-17-5 Maruishi, Hiroshima 7390452, Japan.	tomaruy@affrc.go.jp	SUZUKI, Hidekazu/O-1906-2014	Takao, Yoshitake/0000-0002-0741-7445	Ministry of Education, Science, and Culture of Japan [22688016]; Grants-in-Aid for Scientific Research [22688016] Funding Source: KAKEN	Ministry of Education, Science, and Culture of Japan(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	This study was partially supported by a Grant-in-Aid for Young Scientists (A), no. 22688016, from the Ministry of Education, Science, and Culture of Japan.	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Environ. Microbiol.	AUG	2011	77	15					5285	5293		10.1128/AEM.00202-11	http://dx.doi.org/10.1128/AEM.00202-11			9	Biotechnology & Applied Microbiology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Biotechnology & Applied Microbiology; Microbiology	798PW	21666026	Green Published			2025-03-11	WOS:000293224500026
J	Aleksandrova, GN; Shcherbinina, EA				Aleksandrova, G. N.; Shcherbinina, E. A.			Stratigraphy and paleoenvironmental interpretation of the Paleocene-Eocene transition in the Eastern Crimea	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						biostratigraphy; Paleocene-Eocene Thermal Maximum; dinocysts; nannoplankton; Eastern Crimea	DINOFLAGELLATE CYSTS; THERMAL MAXIMUM; BIOSTRATIGRAPHY; LATITUDES; SECTION; EVENT	The study of nannofossils and dinoflagelate cysts from the Paleocene-Eocene transition in the Nasypnoe section, Eastern Crimea identified the bed corresponding to the global event referred as the Paleocene-Eocene Thermal Maximum (PETM). The assemblages of both groups of microphytoplankton display significant changes including the appearance of Rhomboaster spp., Discoaster anartios and D. araneus nannofossils and Apectodinium augustum and Wilsonidium pechoricum dinocysts featured for this event and major variations in the ratio of taxa resulted in domination of eutrophic and warm-water species. The paleoecological interpretation of nannofossil and dinocyst distribution suggests a drastic sea-level fall preceded the PETM and occurrence of two transgressive episodes during it.	[Aleksandrova, G. N.; Shcherbinina, E. A.] Russian Acad Sci, Inst Geol, Moscow V71, Russia	Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences	Aleksandrova, GN (通讯作者)，Russian Acad Sci, Inst Geol, Moscow V71, Russia.	dinoflag@mail.ru	Galina, Aleksandrova/AAW-8215-2020		Russian Foundation for Basic Research [09-05-00872]; Presidium RAS [24]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Presidium RAS(Russian Academy of Sciences)	The work was supported by the Russian Foundation for Basic Research, project no. 09-05-00872, and by the Program of Presidium RAS no. 24.	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AUG	2011	19	4					424	449		10.1134/S0869593811040022	http://dx.doi.org/10.1134/S0869593811040022			26	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	802WY					2025-03-11	WOS:000293542900004
J	Peyrot, D; Barroso-Barcenilla, F; Barrón, E; Comas-Rengifo, MJ				Peyrot, Daniel; Barroso-Barcenilla, Fernando; Barron, Eduardo; Jose Comas-Rengifo, Maria			Palaeoenvironmental analysis of Cenomanian-Turonian dinocyst assemblages from the Castilian Platform (Northern-Central Spain)	CRETACEOUS RESEARCH			English	Article						Castilian Platform; Cenomanian-Turonian Boundary event (CTBE); Dinocyst assemblages; Upper Cenomanian; Lower Turonian; Palaeoecology; Palynology; Spain	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; SEA-LEVEL CHANGES; VOCONTIAN BASIN; BOUNDARY EVENT; WESTERN INTERIOR; NORTHWEST EUROPE; IBERIAN TROUGH; ATLANTIC; PALYNOFACIES; STRATIGRAPHY	The palynological assemblages from three Cenomanian-Turonian sections from the Castilian Platform are described. The 49 levels analysed yielded a well-diversified palynological content including dinoflagellate cysts, acritarchs, prasinophytes and miospores. The comparison of the terrestrial and marine assemblages from these three sections reveals significant differences that are mainly related to their relative palaeogeographical locations. The quantitative study performed on dinocyst assemblages suggests an association interpreted as inner neritic including Xenascus ceratioides, Cribroperidinium exilicristatum, Canningia reticulata and Kallosphaeridium? ringnesiorum. On the contrary, the group inferred to show outer neritic preferences is integrated by Palaeohystrichophora infusorioides, Spiniferites spp., Odontochitina spp., Trichodinium castanea and Impletosphaeridium polytrichum. In the Castilian Platform, the Cenomanian-Turonian Boundary Event (CUBE) may be manifested by a higher proportion of Cyclonephelium spp. in the distal dinocyst assemblages. (C) 2011 Elsevier Ltd. All rights reserved.	[Peyrot, Daniel; Barroso-Barcenilla, Fernando; Jose Comas-Rengifo, Maria] Fac Ciencias Geol, Inst Geol UCM CSIC, Dept Paleontol, Madrid 28040, Spain; [Barroso-Barcenilla, Fernando] Univ Alcala de Henares, Grp Invest Ibercreta, Alcala De Henares 28871, Spain; [Barron, Eduardo] Inst Geol & Minero Espana IGME, Madrid 28003, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); Universidad de Alcala	Peyrot, D (通讯作者)，Fac Ciencias Geol, Inst Geol UCM CSIC, Dept Paleontol, Jose Antonio Novais 2, Madrid 28040, Spain.	danip@geo.ucm.es	peyrot, Daniel/AAI-6091-2020; Barrón, Eduardo/L-4726-2014; Comas-Rengifo, Maria Jose/H-8373-2015; Barroso-Barcenilla, Fernando/M-5578-2014	Comas Rengifo, Maria Jose/0000-0002-3529-8439; Comas-Rengifo, Maria Jose/0000-0002-6593-3798; Barroso-Barcenilla, Fernando/0000-0002-7938-7230; peyrot, Daniel/0000-0002-3897-6733; Barron, Eduardo/0000-0003-4979-1117	Ministerio de Ciencia e Innovacion [GR910431 (BSCH-UCM), CGL2008-03112/BTE, CGL2009-12008]; Junta de Castilla-La Mancha (Spain) [PAI08-0204-1312, PEII11-0237-7926]; Basler Stiftung fur biologische Forschung (Switzerland)	Ministerio de Ciencia e Innovacion(Ministry of Science and Innovation, Spain (MICINN)Instituto de Salud Carlos IIISpanish Government); Junta de Castilla-La Mancha (Spain); Basler Stiftung fur biologische Forschung (Switzerland)	We thank Paul Dodsworth and Martin A. 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Zevenboom Daan, 1994, Giornale di Geologia (Bologna), V56, P155	144	37	41	0	6	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	AUG	2011	32	4					504	526		10.1016/j.cretres.2011.03.006	http://dx.doi.org/10.1016/j.cretres.2011.03.006			23	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	790JE					2025-03-11	WOS:000292583500010
J	Skupien, P; Smarzová, A				Skupien, Petr; Smarzova, Alexandra			Palynological and geochemical response to environmental changes in the Lower Cretaceous in the Outer Western Carpathians; a record from the Silesian unit, Czech Republic	CRETACEOUS RESEARCH			English	Article						Silesian unit; Lower Cretaceous; Palynology; Dinoflagellate cysts; C-isotopes	CARBON-ISOTOPE EVENT; FRANCE	Rich dinoflagellate cyst assemblages recorded from the Vendryne Formation, Tesin Limestone, and Hradiste Formation of the Silesian unit, Czech Republic are presented. The results of a qualitative and quantitative study of dinoflagellate cysts are presented and discussed. Age-assessment of the sediments based on 86 species suggests a Late Tithonian to Early Berriasian age for the Vendryne Formation and a Late Berriasian (Otopeta Ammonite Zone) to the basal part of the Late Valanginian (Verrucosum Ammonite Zone) age for the Tesin Limestone. Pelitic flyschoid sediments of the Hradiste Formation belong to the Late Valanginian - Early Hauterivian age. Quantitative palynological study and carbon isotope analysis were applied to understand the change from the grey clays to dark grey clays sedimentation. The dinoflagellate cyst assemblages show deposition in a shallow-sea environment. An increasing amount of sporomorphs towards the overlying layers (they are the most abundant in the Hradiste Formation) shows a growing supply of terrestrial material at the same time. The values of delta C-13 increased significantly from a level of 0.43 or 0.75-1.81 parts per thousand in the Late Valanginian. This change probably indicates an increase in organic matter storage and perturbation of the carbon cycle connected with the dark grey clays sedimentation. (C) 2011 Elsevier Ltd. All rights reserved.	[Skupien, Petr; Smarzova, Alexandra] VSB Tech Univ, Inst Geol Engn, Ostrava 70833, Czech Republic	Technical University of Ostrava	Skupien, P (通讯作者)，VSB Tech Univ, Inst Geol Engn, 17 Listopadu 15, Ostrava 70833, Czech Republic.	petr.skupien@vsb.cz	Skupien, Petr/G-8767-2019	Skupien, Petr/0000-0001-9158-466X	 [MSM 61989100 19]		The research was supported by grant MSM 61989100 19 DeCOx processes. We would like to thank David Batten, Gregory Price, Malcolm B. Hart and the anonymous reviewers for reading the manuscript; their critical remarks significantly improved the manuscript.	[Anonymous], TUBINGER MIKROPALAON; [Anonymous], 1996, Palynology: principles and applications; DUCHENE RJJ, 1996, CAHIERS MICROPALEONT, V1, P5; Durr G., 1988, TUBINGER MIKROPALAON, V5, P159; ek Z., 1972, RADA HORNICKO GEOLOG, V17, P97; Eliasˇ M., 2003, TECHNICKE UNIVERZITY, V49, P7; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FISCHER SH, 2003, THESIS SWISS FEDERAL; Gröcke DR, 2005, EARTH PLANET SC LETT, V240, P495, DOI 10.1016/j.epsl.2005.09.001; HANZLIKOVA E, 1964, VESTNIK USTREDNIHO U, V39, P387; Leereveld H, 1997, CRETACEOUS RES, V18, P385, DOI 10.1006/cres.1997.0070; Leereveld H., 1995, LPP CONTRIBUTION SER, V2; LINI A, 1992, TERRA NOVA, V4, P374, DOI 10.1111/j.1365-3121.1992.tb00826.x; Mencik E., 1983, GEOLOGY MORAVSKOSLEZ; MICHALIK J, 1995, GEOL CARPATH, V46, P161; Michalik J., 1994, MITTEILUNGEN O STERR, V86, P101; Michalík J, 2008, CRETACEOUS RES, V29, P871, DOI 10.1016/j.cretres.2008.05.005; Misik M., 1992, ZAPAD KARPATY G, V16, P47; MONTEIL E, 1993, B CENT RECH EXPL, V17, P249; Monteil E., 1992, Revue de Paleobiologie, V11, P299; MONTEIL E, 1991, B CENT RECH EXPL, V15, P461; PICHA EJ, 2006, AAPG MEMOIR, V84, P49; Skupien P, 2002, GEOL CARPATH, V53, P179; Skupien P, 1997, SBOR VED PRACI VYS S, P34; SKUPIEN P, 2003, MONOGRAFIE TECHNICKE, V8, P15; Skupien Petr, 1999, Vestnik Ceskeho Geologickeho Ustavu, V74, P1; Skupien Petr, 2004, Slovak Geological Magazine, V10, P203; VASICEK Z, 2002, TETHYAN BOREAL CRETA, P115; Vasicek Z., 1972, ROZPRAVY USTREDNIHO, V38; WILPSHAAR M, 1994, REV PALAEOBOT PALYNO, V84, P121, DOI 10.1016/0034-6667(94)90046-9	30	26	26	0	7	ACADEMIC PRESS LTD- ELSEVIER SCIENCE LTD	LONDON	24-28 OVAL RD, LONDON NW1 7DX, ENGLAND	0195-6671	1095-998X		CRETACEOUS RES	Cretac. Res.	AUG	2011	32	4					538	551		10.1016/j.cretres.2011.04.001	http://dx.doi.org/10.1016/j.cretres.2011.04.001			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	790JE					2025-03-11	WOS:000292583500012
J	Erdner, DL; Richlen, M; McCauley, LAR; Anderson, DM				Erdner, Deana L.; Richlen, Mindy; McCauley, Linda A. R.; Anderson, Donald M.			Diversity and Dynamics of a Widespread Bloom of the Toxic Dinoflagellate <i>Alexandrium fundyense</i>	PLOS ONE			English	Article							DIATOM DITYLUM-BRIGHTWELLII; POPULATION GENETIC-STRUCTURE; MICROSATELLITE MARKERS; GONYAULAX-TAMARENSIS; CYST FORMATION; SPRING BLOOM; BACILLARIOPHYCEAE; SOFTWARE; DIFFERENTIATION; DINOPHYCEAE	Historically, cosmopolitan phytoplankton species were presumed to represent largely unstructured populations. However, the recent development of molecular tools to examine genetic diversity have revealed differences in phytoplankton taxa across geographic scales and provided insight into the physiology and ecology of blooms. Here we describe the genetic analysis of an extensive bloom of the toxic dinoflagellate Alexandrium fundyense that occurred in the Gulf of Maine in 2005. This bloom was notable for its intensity and duration, covering hundreds of kilometers and persisting for almost two months. Genotypic analyses based on microsatellite marker data indicate that the open waters of the northeastern U.S. harbor a single regional population of A. fundyense comprising two genetically distinct sub-populations. These subpopulations were characteristic of early-and late-bloom samples and were derived from the northern and southern areas of the bloom, respectively. The temporal changes observed during this study provide clear evidence of succession during a continuous bloom and show that selection can act on the timescale of weeks to significantly alter the representation of genotypes within a population. The effects of selection on population composition and turnover would be magnified if sexual reproduction were likewise influenced by environmental conditions. We hypothesize that the combined effects of differential growth and reproduction rates serves to reduce gene flow between the sub-populations, reinforcing population structure while maintaining the diversity of the overall regional population.	[Erdner, Deana L.] Univ Texas Marine Sci Inst, Port Aransas, TX USA; [Richlen, Mindy; McCauley, Linda A. R.; Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	Woods Hole Oceanographic Institution	Erdner, DL (通讯作者)，Univ Texas Marine Sci Inst, Port Aransas, TX USA.	derdner@mail.utexas.edu	Erdner, Deana/C-4981-2008	Erdner, Deana/0000-0002-1736-8835	National Institute of Environmental Health Sciences [1-P50-ES012742]; National Science Foundation through the Woods Hole Center for Oceans and Human Health [OCE-0430724]; NOAA [NA06NOS4780245]; Directorate For Geosciences; Division Of Ocean Sciences [0911031] Funding Source: National Science Foundation	National Institute of Environmental Health Sciences(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); National Science Foundation through the Woods Hole Center for Oceans and Human Health; NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work was supported by the National Institute of Environmental Health Sciences (1-P50-ES012742 to DMA and DLE), by the National Science Foundation through the Woods Hole Center for Oceans and Human Health (OCE-0430724), and by the ECOHAB program (NOAA Grant NA06NOS4780245). This is contribution number 660 from the ECOHAB program. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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J	McCarthy, FMG; Mertens, KN; Ellegaard, M; Sherman, K; Pospelova, V; Ribeiro, S; Blasco, S; Vercauteren, D				McCarthy, Francine M. G.; Mertens, Kenneth Neil; Ellegaard, Marianne; Sherman, Keith; Pospelova, Vera; Ribeiro, Sofia; Blasco, Stephan; Vercauteren, Dries			Resting cysts of freshwater dinoflagellates in southeastern Georgian Bay (Lake Huron) as proxies of cultural eutrophication	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Freshwater dinoflagellate cysts; Peridinium; Cyst-theca relationships; Cultural eutrophication; Great Lakes; Paleolimnology	PERIDINIUM-WILLEI; CRAWFORD LAKE; LONG-TERM; POPULATION-DYNAMICS; ONTARIO; PHYTOPLANKTON; DINOPHYCEAE; TEMPERATURE; INDICATORS; SEDIMENTS	Resting cysts attributed to the freshwater dinoflagellate genus Peridinium were found in surface sediments from Severn Sound, southeastern Georgian Bay (lake Huron, Laurentian Great Lakes of North America). Two distinct cyst morphotypes were present and they were assigned to Peridinium wisconsinense Eddy, 1930 and Peridinium willei Huitfeldt-Kaas, 1900 by establishing cyst-theca relationships through germinations and single-cell LSU rDNA analysis on an excysted cell of Peridinium willei. Sediments recovered from deep, sheltered portions of Severn Sound and restricted basins like Honey Harbour contained between similar to 750 and 8500 cysts/cm(3). However, winnowing by bottom currents and high concentrations of dissolved oxygen adversely impact the dinoflagellate cyst record on the lakebed, and cyst concentrations in easily remobilized muds on bathymetric highs were <100 cysts/cm(3). Down-core changes in the relative abundances of these two cyst morphotypes were attributed primarily to cultural eutrophication related to land-use changes around Severn Sound over the last six centuries. Cysts of Peridinium willei, a cosmopolitan dinoflagellate species that occurs in a broad range of temperature, pH and nutrient conditions, comprise 60-74% of the cysts identified in Ambrosia (ragweed)-rich sediments in the upper 20 cm of a gravity core taken from Honey Harbour. Euro-Canadian settlement and land-clearing that began in the Midland-Penetanguishene region around AD. 1840 are evident in the increase in Ambrosia (ragweed), Gramineae (grasses) and other herbs (non-arboreal pollen) that mark the base of the Ambrosia zone (pollen zone 4) as well as an overall increase in terrigenous flux. In addition to siltation, this terrigenous flux increased the availability of limiting nutrients to the previously oligotrophic waters of Severn Sound, leading to increased cyst flux in Honey Harbour peaking at nearly 3000 cysts/cm(2)/y in A.D. 1966, an order of magnitude higher than cyst fluxes prior to the Euro-Canadian Ambrosia zone. Peridinium wisconsinense was the more common dinoflagellate cyst species in Honey Harbour prior to Euro-Canadian settlement, when cyst flux was an order of magnitude lower. This is consistent with the restriction of this species to relatively warm, oligotrophic to mesotrophic lakes in North America. An earlier increase in P. willei at the expense of P. wisconsinense in the core from Honey Harbour within pollen zone 3 d (similar to 700 to similar to 150 yBP) is attributed to earlier land-clearing by the Wendat ("Huron"), who practiced agriculture in the Penetanguishene peninsula between similar to AD. 1450-1650. The cysts of these freshwater dinoflagellates thus appear to be sensitive to cultural eutrophication. Crown Copyright (C) 2011 Published by Elsevier B.V. All rights reserved.	[McCarthy, Francine M. G.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Mertens, Kenneth Neil] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Ellegaard, Marianne; Ribeiro, Sofia] Univ Copenhagen, Fac Sci, Dept Biol, Aquat Biol Sect, DK-1353 Copenhagen K, Denmark; [Sherman, Keith] Severn Sound Environm Assoc, Midland, ON L4R 3S9, Canada; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada; [Blasco, Stephan] Geol Survey Canada Atlantic, Dartmouth, NS, Canada; [Vercauteren, Dries] Univ Ghent, Lab Gen Biochem & Phys Pharm, B-9000 Ghent, Belgium	Brock University; Ghent University; University of Copenhagen; University of Victoria; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Ghent University	McCarthy, FMG (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	fmccarthy@brocku.ca	Mertens, Kenneth/AAO-9566-2020; Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014; Mertens, Kenneth/C-3386-2015	Ribeiro, Sofia/0000-0003-0672-9161; Ellegaard, Marianne/0000-0002-6032-3376; Mertens, Kenneth/0000-0003-2005-9483; Pospelova, Vera/0000-0003-4049-8133	NSERC	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC))	The samples were collected as part of a research program by the Geological Survey of Canada-Atlantic, headed by Steve Blasco, together with the Midland Remedial Action Plan coordinated by Keith Sherman. We gratefully acknowledge the insights of Geoff Norris, Jock McAndrews, and Martin Head, the field assistance of Mike MacKinnon, Bob Harmes, and Darren Keyes, assistance with drafting figures from Mike Lozon, and the laboratory assistance of Brock University students Andrea Krueger, Heather Gregg, Adam Sarvis, Josh Shaw, and Kara McLachlan. This research was partly supported by NSERC grants to Francine McCarthy and Vera Pospelova. Kenneth Neil Mertens is a Postdoctoral fellow of FWO Belgium. The comments of reviewers Andre Rochon and Karin Zonneveld resulted in a much stronger final product.	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Palaeobot. Palynology	JUL	2011	166	1-2					46	62		10.1016/j.revpalbo.2011.04.008	http://dx.doi.org/10.1016/j.revpalbo.2011.04.008			17	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	799WR					2025-03-11	WOS:000293317400005
J	Msaky, ES				Msaky, Emma Samwel			Middle Jurassic - earliest Late Cretaceous palynofloras, coastal Tanzania Part One	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			English	Article						Coastal Tanzania; dinoflagellate cysts; systematics; Middle Jurassic; Cretaceous	BAYU-UNDAN FIELD; DINOFLAGELLATE CYST; TIMOR SEA; STRATIGRAPHIC PALYNOLOGY; SEQUENCE STRATIGRAPHY; SEDIMENTARY BASINS; EROMANGA BASIN; STRATA; BIOSTRATIGRAPHY; PALYNOMORPHS	This two-part palynostratigraphic study of Mesozoic successions in hydrocarbon-prospective Tanzanian coastal basins utilizes cores, ditch cuttings, and outcrop samples. These contain rich and diverse dinoflagellate suites ranging in age from Middle Jurassic (Bajocian) to earliest late Cretaceous (Cenomanian). Spores and pollen grains are also recorded, but these are, with some exceptions, subordinate to the dinoflagellate components. In the systematic section of the current Part One, one new dinoflagellate cyst genus, Kipatimudinium, is formally described and seven new species are established: Amphorulla ruvuense, Dichadogonyaulax mandawaense, Egmontodinium annaiae, Hystrichodinium playfordii, Kipatimudinium foliatum (type species), Limbodinium patulum, and Yalkalpodinium africanum. The subsequent Part Two of this monograph will conclude the systematic palaeontology and assess the chronological and stratigraphic-correlative significance of the palynofloras, as well as their palaeogeographic implications. A palynofacies study will also be included in Part Two.	Tanzania Petr Dev Corp, BWM Tower A,Azikiwe Jamhuri St,POB 2774, Dar Es Salaam, Tanzania		Msaky, ES (通讯作者)，Tanzania Petr Dev Corp, BWM Tower A,Azikiwe Jamhuri St,POB 2774, Dar Es Salaam, Tanzania.	emma.msaky@uqconnect.edu.au			Tanzania Petroleum Development Corporation (TPDC)	Tanzania Petroleum Development Corporation (TPDC)	The Management of the Tanzania Petroleum Development Corporation (TPDC) is thanked for providing material and financial support and The University of Queensland, School of Earth Sciences, for provision of research facilities and administrative assistance.	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Abt. B-Palaophytol.	JUL	2011	286	1-3					1	99						99	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	797UA					2025-03-11	WOS:000293154400001
J	Shin, HH; Yoon, YH; Kim, YO; Matsuoka, K				Shin, Hyeon Ho; Yoon, Yang Ho; Kim, Young-Ok; Matsuoka, Kazumi			Dinoflagellate Cysts in Surface Sediments from Southern Coast of Korea	ESTUARIES AND COASTS			English	Article						Dinoflagellate cyst; Salinity level; Eutrophication; Heterotrophic cyst; Gamak Bay	SPATIAL-DISTRIBUTION; TOKYO-BAY; COCHLODINIUM-POLYKRIKOIDES; HYDROGRAPHIC CONDITIONS; MARINE-SEDIMENTS; YOKOHAMA-PORT; SEA; INDICATORS; EUTROPHICATION; ASSEMBLAGES	To investigate the distributions of dinoflagellate cysts in relation to environmental conditions from southern coast of Korea, surface sediment samples collected from 11 stations in Gamak Bay, Yeoja Bay and the offshore area of Yeoja Bay were analyzed. Dinoflagellate cyst assemblages observed in the study area included many species commonly reported from other temperate regions. Among them, Polykrikos cysts were dominant, together with Brigantedinium spp. and Spiniferites spp. Based on cluster analysis, dinoflagellate cyst assemblages were divided into two main groups; group I, located in Yeoja Bay and group II, located in Gamak Bay and the offshore area of Yeoja Bay. Principal component analysis identified differences in salinity levels as the main environmental factors affecting the distributional characteristics of dinoflagellate cyst assemblages in the study area. Gamak Bay is a typical eutrophied area as result of extensive human activities around the bay, and heterotrophic cysts, including Polykrikos cysts, are remarkably abundant and likely to be a useful indicator for eutrophication in Gamak Bay.	[Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Shin, Hyeon Ho; Kim, Young-Ok] Korea Ocean Res & Dev Inst, Geoje 656830, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Yeosu 550749, South Korea	Nagasaki University; Korea Institute of Ocean Science & Technology (KIOST); Chonnam National University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp	KIM, YOUNG JIN/E-9374-2011	Shin, Hyeon Ho/0000-0002-9711-6717; Yoon, Yang Ho/0000-0001-8529-9512	Korean Ocean Research and Development Institute [PE98582]	Korean Ocean Research and Development Institute	We thank Dr. K. Mizushima and all members of the Laboratory of the Coastal Environmental Sciences, Nagasaki University for their kind help with the cyst analysis, and also wish to express our gratitude to the reviewers for their critical comments, which helped to improve the manuscript. 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J	Haberkorn, H; Hégaret, H; Marie, D; Lambert, C; Soudant, P				Haberkorn, Hansy; Hegaret, Helene; Marie, Dominique; Lambert, Christophe; Soudant, Philippe			Flow cytometric measurements of cellular responses in a toxic dinoflagellate, <i>Alexandrium minutum</i>, upon exposure to thermal, chemical and mechanical stresses	HARMFUL ALGAE			English	Article						Alexandrium minutum; Cysts; Flow cytometry	CYST FORMATION; LIFE-HISTORY; RESTING CYSTS; GUT PASSAGE; DINOPHYCEAE; PHYTOPLANKTON; GROWTH; CYCLE; GONYAULACALES; ENCYSTMENT	The purpose of the present study was to provide a flow-cytometric (FCM) approach evaluating Alexandrium minutum cellular responses to mechanical, thermal and chemical stresses. Coupling SYBR-Green I and SYTOX-Green staining, FCM analysis and sorting, and microscopic observations permitted identification and characterization of five cellular states/forms of A. minutum: (1) vegetative cells, (2) pellicle cysts, (3) degraded cells, (4) empty theca, and (5) dead cells. Storage on ice resulted in the transformation of a portion of vegetative cells into dead cells, pellicle cysts, and "degraded" cells: however, centrifugation resulted mostly in pellicle cysts and a few degraded cells. After these thermal and mechanical treatments, control and stressed cultures were monitored for 14 days. Stressed A. minutum cultures appeared to grow at the same rates as control cultures during the first seven days. During the last week of monitoring, however, cell densities of stressed cultures reached their stationary phase earlier than control cultures, suggesting incomplete recovery. Additional experiment assessing kinetics of excystment indicated that it can occur less than 9 h following mechanical stress (centrifugation) and that 75% of the culture can excyst within 24 h. Upon 30 min of exposure to chemical stressors (saponine and H2O2), only vegetative cells, pellicle cysts, and dead cells were detected. For both chemicals, encystment was dose-dependent. Counts of pellicle cysts increased with increasing saponine or H2O2 concentration. Pellicle cysts were the most-predominant cell type at chemical treatments above 0.05 g L-1 saponine and above 0.015% H2O2. Occurrence of dead cells appeared to follow an all-or-none response as dead-cell percentage increased from 3% at 0.015% H2O2 to 81% at 0.03% H2O2 without pellicle cyst formation. Overall, encystment-excystment of A. minutum upon changes of environmental conditions can occur very rapidly but can be monitored using FCM and SYBR-Green I staining. (C) 2011 Elsevier B.V. All rights reserved.	[Haberkorn, Hansy; Hegaret, Helene; Lambert, Christophe; Soudant, Philippe] Univ Bretagne Occidentale, Lab Sci Environm Marin, Inst Univ Europeen Mer, F-29280 Plouzane, France; [Marie, Dominique] Univ Paris 06, F-29680 Roscoff, France; [Marie, Dominique] CNRS, UMR7144, Stn Biol Roscoff, F-29680 Roscoff, France	Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); Ifremer; Institut de Recherche pour le Developpement (IRD); Sorbonne Universite; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE)	Soudant, P (通讯作者)，Univ Bretagne Occidentale, Lab Sci Environm Marin, Inst Univ Europeen Mer, Pl Copern, F-29280 Plouzane, France.	soudant@univ-brest.fr	; Hegaret, Helene/B-7206-2008	Lambert, Christophe/0000-0002-5885-467X; Hegaret, Helene/0000-0003-4639-9013; Soudant, Philippe/0000-0003-3090-5612	National Research Agency (ANR) [06SEST23]; Brittany Region	National Research Agency (ANR)(Agence Nationale de la Recherche (ANR)); Brittany Region(Region Bretagne)	Sincere thanks are due to Gary H. Wikfors for English corrections. 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J	Rao, DVS; Stewart, JE				Rao, D. V. Subba; Stewart, James E.			A preliminary study of the formation of a third category of cysts by a toxigenic dinoflagellate, <i>Alexandrium fundyense</i> in response to elevated concentrations of ammonium chloride	HARMFUL ALGAE			English	Article						Alexandrium fundyense; Cysts; Iron; Toxins	GONYAULAX-TAMARENSIS; LIFE-CYCLE; RED TIDE; MARINE MICROALGAE; RESTING CYSTS; IRON; DINOPHYCEAE; NITROGEN; ENCYSTMENT; DIATOM	Exposure of exponentially growing cells of a toxigenic dinoflagellate strain, Alexandrium fundyense, to ammonium chloride concentrations comparable to levels of ammonia observed in Bay of Fundy waters induced formation in a few days of large numbers of double-walled, circular cysts (termed forced cysts). The A. fundyense forced cysts were distinctly different from the asexual pellicle cysts, and the sexual resting cysts (hypnocysts) described by Anderson and Wall (1978). The circular shape of these forced cysts and their relatively rapid formation suggest that they were not products of fusion while their resistance to adverse conditions and, when returned to optimal conditions, their subsequent rapid germination to form viable cultures within 14 days, point to an important long-term survival role in response to rapidly changing nutritional and environmental circumstances as well as in the waxing and waning of local toxic dinoflagellate blooms. The relative ease of producing the forced cysts and their fairly rapid germination suggest that these cysts could be suitable vehicles for investigations of the physiology and biochemistry of encystment and excystment in the species producing them. Chemical analyses of forced cysts harvested from cultures of this A. fundyense strain showed large variabilities in selected storage products: iron ranged from 0.03 pg to 17.40 pg Fe/cyst corresponding to 0.04-61.25% of the cyst dry weight; nitrogen levels ranged from 109 pg to 3183 pg/cyst and phosphorus ranged from 0.55 pg to 5.70 pg/cyst. Total paralytic shellfish poisons for these A. fundyense cysts consisted of the same toxins apparent in the vegetative cells, i.e. C1C2 toxins, GTX 2/3, saxitoxin and neosaxitoxin, and ranged from 4.4 fmol to 333 fmol/fg cyst dry wt. (C) 2011 Elsevier B.V. All rights reserved.	[Rao, D. V. Subba; Stewart, James E.] Bedford Inst Oceanog, Ecosyst Res Div, Dept Fisheries & Oceans, Dartmouth, NS B2Y 4A2, Canada	Fisheries & Oceans Canada; Bedford Institute of Oceanography	Rao, DVS (通讯作者)，Bedford Inst Oceanog, Ecosyst Res Div, Dept Fisheries & Oceans, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	seshu35@gmail.com; stewartje@mar.dfo-mpo.gc.ca						Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1985, J EXP MAR BIOL ECOL, V86, P1, DOI 10.1016/0022-0981(85)90039-5; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; Anderson Donald M., 1998, NATO ASI Series Series G Ecological Sciences, V41, P29; ANDERSON MA, 1982, LIMNOL OCEANOGR, V27, P789, DOI 10.4319/lo.1982.27.5.0789; [Anonymous], 1996, HARMFUL TOXIC ALGAL; Blackburn S., 2005, Algal Culturing Techniques, P399; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; DALE B, 1978, OCEANUS, V21, P41; DOUCETTE GJ, 1991, MAR BIOL, V110, P165, DOI 10.1007/BF01313701; DOUCETTE GJ, 1989, J PHYCOL, V25, P721, DOI 10.1111/j.0022-3646.1989.00721.x; Ellegaard M, 2002, J PHYCOL, V38, P775, DOI 10.1046/j.1529-8817.2002.01062.x; Figueroa RI, 2008, HARMFUL ALGAE, V7, P653, DOI 10.1016/j.hal.2008.02.005; FUDGE H, 1977, MAR BIOL, V39, P381, DOI 10.1007/BF00391941; Furnas Miles, 2002, P221; Genovesi B, 2009, J PLANKTON RES, V31, P1209, DOI 10.1093/plankt/fbp066; Guillard R. 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L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Hargrave BT, 1997, WATER AIR SOIL POLL, V99, P641, DOI 10.1007/BF02406903; HARRISON PJ, 1980, J PHYCOL, V16, P28, DOI 10.1111/j.1529-8817.1980.tb00724.x; Henriques AO, 2007, ANNU REV MICROBIOL, V61, P555, DOI 10.1146/annurev.micro.61.080706.093224; HIROAKI T, 2006, UMI NO KENKYU, V15, P165; Holmes P.R., 1985, Asian Marine Biology, V2, P1; Jensen MO, 1997, EUR J PHYCOL, V32, P9, DOI 10.1080/09541449710001719325; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Laycock Maurice V., 1995, Journal of Marine Biotechnology, V3, P121; Laycock Maurice V., 1994, Natural Toxins, V2, P175, DOI 10.1002/nt.2620020405; LORING DH, 1992, EARTH-SCI REV, V32, P235, DOI 10.1016/0012-8252(92)90001-A; Lourenço SO, 2004, EUR J PHYCOL, V39, P17, DOI 10.1080/0967026032000157156; Martin JL, 2005, DEEP-SEA RES PT II, V52, P2569, DOI 10.1016/j.dsr2.2005.06.010; Montresor M., 2006, Algal cultures, analogues of blooms and applications, Volume 1, P91; Nagai S, 2009, PHYCOLOGIA, V48, P177, DOI 10.2216/08-43.1; Naito K, 2008, PHYCOL RES, V56, P58, DOI 10.1111/j.1440-1835.2008.00485.x; Nicholson WL, 2000, MICROBIOL MOL BIOL R, V64, P548, DOI 10.1128/MMBR.64.3.548-572.2000; Poulton NJ, 2005, DEEP-SEA RES PT II, V52, P2501, DOI 10.1016/j.dsr2.2005.06.029; Probert I, 2002, CRYPTOGAMIE ALGOL, V23, P343; Shikata T, 2008, J OCEANOGR, V64, P355, DOI 10.1007/s10872-008-0028-y; Strain PM, 2002, ATMOS OCEAN, V40, P45, DOI 10.3137/ao.400103; Sugie K, 2008, J PLANKTON RES, V30, P1245, DOI 10.1093/plankt/fbn080; WEGNER HG, 2006, CAN J BOT, V84, P400; WONG JTY, 1994, J MAR BIOL ASSOC UK, V74, P467, DOI 10.1017/S0025315400039515; 2005, ANAL STANDARD METHOD	43	4	4	1	23	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	JUL	2011	10	5					512	520		10.1016/j.hal.2011.04.001	http://dx.doi.org/10.1016/j.hal.2011.04.001			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	785MO					2025-03-11	WOS:000292233300012
J	Genovesi, L; de Vernal, A; Thibodeau, B; Hillaire-Marcel, C; Mucci, A; Gilbert, D				Genovesi, Linda; de Vernal, Anne; Thibodeau, Benoit; Hillaire-Marcel, Claude; Mucci, Alfonso; Gilbert, Denis			Recent changes in bottom water oxygenation and temperature in the Gulf of St. Lawrence: Micropaleontological and geochemical evidence	LIMNOLOGY AND OCEANOGRAPHY			English	Article							BENTHIC FORAMINIFERS; ISOTOPIC COMPOSITION; SEA; EUTROPHICATION; ESTUARY; RATES; RESPIRATION; SEDIMENTS; SLOPE; SHELF	Micropaleontological and geochemical analyses of a sediment core collected in the Laurentian Trough of the Gulf of St. Lawrence were carried out to reconstruct temporal variations in pelagic productivity and benthic environmental conditions. Dinoflagellate cyst assemblages reveal relatively stable pelagic productivity over the last two centuries. Similarly, geochemical (organic C, C-org : N) and isotopic (delta C-13(org), delta N-15) data reveal that organic matter fluxes to the seafloor have been relatively constant over the same period. In contrast, significant changes are recorded in the benthic foraminifer assemblages. A sediment surface peak in the abundance of Cassidulina laevigata and Brizalina subaenariensis is consistent with the recent record of oxygen depletion in the bottom water. A decrease in the relative abundance of Nonionellina labradorica, concomitant with a relatively higher occurrence of Oridorsalis umbonatus in the upper part of the core, reflects a significant warming of the bottom water. Changes in bottom-water properties are further constrained by a negative trend of the delta O-18 in Bulimina exilis carbonate shells over the last century, corresponding to a warming of about 2 degrees C. These results strongly suggest that the recent oxygen depletion in the bottom waters of the Gulf of St. Lawrence is due to changes in water masses that have led to increased bottom-water temperatures and, to some extent, a resultant increase in organic matter respiration rates.	[Genovesi, Linda; de Vernal, Anne; Thibodeau, Benoit; Hillaire-Marcel, Claude] Univ Quebec, Ctr Rech Geochim & Geodynam GEOTOP, Montreal, PQ, Canada; [Mucci, Alfonso] McGill Univ, Ctr Rech Geochim & Geodynam GEOTOP, Montreal, PQ, Canada; [Gilbert, Denis] Fisheries & Oceans Canada, Inst Maurice Lamontagne, Mont Joli, PQ, Canada	University of Quebec; University of Quebec Montreal; Fisheries & Oceans Canada	de Vernal, A (通讯作者)，Univ Quebec, Ctr Rech Geochim & Geodynam GEOTOP, Succursale Ctr Ville, Montreal, PQ, Canada.	devernal.anne@uqam.ca	Gilbert, Denis/A-3067-2010; Thibodeau, Benoit/B-5629-2008; Hillaire-Marcel, Claude/H-1441-2012; Hillaire-Marcel, Claude/C-9153-2013; de Vernal, Anne/D-5602-2013	Hillaire-Marcel, Claude/0000-0002-3733-4632; de Vernal, Anne/0000-0001-5656-724X; Gilbert, Denis/0000-0002-9554-9594; Thibodeau, Benoit/0000-0003-0422-2308; Mucci, Alfonso/0000-0001-9155-6319	NSERC; Fonds Quebecois de la Recherche sur la Nature et les Technologies	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds Quebecois de la Recherche sur la Nature et les Technologies(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT))	Thanks to Guy Bilodeau, Maryse Henry, Bassam Ghaleb, Jean-Francois Helie, Julie Leduc, and Christelle Not (Centre de recherche en geochimie et geodynamique [GEOTOP]) for their help with the sediment analyses. This study is a contribution to a strategic project of the Natural Sciences and Engineering Research Council of Canada (NSERC) entitled "Deep-water hypoxia and the sensitivity of the Lower St. Lawrence Estuary to Environmental change.'' Financial support from NSERC through scholarships, ship time allocation, and Discovery grants and from the Fonds Quebecois de la Recherche sur la Nature et les Technologies (infrastructure award to GEOTOP) is also acknowledged. We are grateful to the anonymous reviewers of the journal for their constructive comments.	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J	Li, JG; Riding, JB; Cheng, JH; He, CQ				Li, Jianguo; Riding, James B.; Cheng, Jinhui; He, Chengquan			Latest Jurassic-earliest Cretaceous (Tithonian-Berriasian) dinoflagellate cysts from the Yanshiping Group of the northern Qinghai-Xizang Plateau (Tibet), western China	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; biostratigraphy; palaeogeography; Latest Jurassic-earliest Cretaceous; Qinghai-Xizang Plateau; western China	EMENDATION; REVISION; COOKSON	Dinoflagellate cysts from the Xiali, Suowa and Xueshan formations (Yanshiping Group) of the Tanggula Mountains, Qinghai-Xizang Plateau, western China were studied. The palynofloras are sparse and poorly-preserved due to high levels of thermal maturation relating to intense tectonic activity. These formations are interpreted as being of Tithonian to Berriasian (latest Jurassic to earliest Cretaceous) age based on key markers such as Amphorula delicata, Amphorula metaelliptica, ?Batioladinium sp., ?Glossodinium dimorphum, Gochteodinia sp., Gonyaulacysta sp. cf. G. dualis, ?Muderongia sp. and ?Scriniodinium crystallinum. The Jurassic-Cretaceous transition probably lies within the upper Suowa Formation. This sparse and low diversity assemblage cannot be easily compared with other floras of the same age. However Amphorula is relatively common, and this indicates a connection with the western Tethyan Realm. No endemic Austral or high latitude taxa were encountered. The sizes of the dinoflagellate cysts are markedly smaller than their respective type material. This phenomenon is interpreted as being a result of the loss of volatile components during intense thermal maturation. The dinoflagellate cyst biostratigraphy herein indicates that the narrowing and the closure of the meso-Tethys in western China occurred during the Tithonian and Berriasian. (C) 2011 Elsevier B.V. All rights reserved.	[Li, Jianguo; Cheng, Jinhui] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Peoples R China; [Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	Chinese Academy of Sciences; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Li, JG (通讯作者)，Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, 39 E Beijing Rd, Nanjing 210008, Peoples R China.	jgli@nigpas.ac.cn; jbri@bgs.ac.uk; jinhuicheng@139.com		cheng, jin hui/0000-0002-3560-3667	Chinese Academy of Sciences [KZCX2-YW-QN112]; State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) [20092105, 063115]; Natural Science Foundation of China [40872013]; NERC [bgs010024] Funding Source: UKRI	Chinese Academy of Sciences(Chinese Academy of Sciences); State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS)(Chinese Academy of Sciences); Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research was funded by the Knowledge Innovation Program of the Chinese Academy of Sciences (grant number KZCX2-YW-QN112), State Key Laboratory of Palaeobiology and Stratigraphy (Nanjing Institute of Geology and Palaeontology, CAS) (No. 20092105 and No. 063115) and Natural Science Foundation of China (40872013). We are indebted to Miss He Culling (NIGPCAS) for technical help. This contribution was completed under the Individual Merit project awarded to James B. Riding entitled Global Jurassic dinoflagellate cyst palaeobiology and its applications. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC). The authors are grateful to Professor Zhou Zhiyan for his help with the study, and to Dr John Backhouse (University of Western Australia) and an anonymous reviewer for their constructive reviews.	[Anonymous], 9210 GEOL SURV CAN; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1996, Palynology: principles and applications; Bai S., 1989, GEOL REV, V35, P529; BGMRX (Bureau of Geology Mineral Resources of the Xizang Autonomous Region), 1993, GEOL MEM MIN GEOL MI, P707; Bint A.N., 1994, The Sedimentary Basins of Western Australia. 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Palaeobot. Palynology	JUL	2011	166	1-2					38	45		10.1016/j.revpalbo.2011.04.007	http://dx.doi.org/10.1016/j.revpalbo.2011.04.007			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	799WR		Green Accepted			2025-03-11	WOS:000293317400004
J	Klais, R; Tamminen, T; Kremp, A; Spilling, K; Olli, K				Klais, Riina; Tamminen, Timo; Kremp, Anke; Spilling, Kristian; Olli, Kalle			Decadal-Scale Changes of Dinoflagellates and Diatoms in the Anomalous Baltic Sea Spring Bloom	PLOS ONE			English	Article							ALEXANDRIUM-FUNDYENSE; SCRIPPSIELLA-HANGOEI; GROWTH STRATEGIES; GULF; GERMINATION; PATTERNS; CYSTS; LIFE; SEDIMENTATION; EVOLUTIONARY	The algal spring bloom in the Baltic Sea represents an anomaly from the winter-spring bloom patterns worldwide in terms of frequent and recurring dominance of dinoflagellates over diatoms. Analysis of approximately 3500 spring bloom samples from the Baltic Sea monitoring programs revealed (i) that within the major basins the proportion of dinoflagellates varied from 0.1 (Kattegat) to.0.8 (central Baltic Proper), and (ii) substantial shifts (e. g. from 0.2 to 0.6 in the Gulf of Finland) in the dinoflagellate proportion over four decades. During a recent decade (1995-2004) the proportion of dinoflagellates increased relative to diatoms mostly in the northernmost basins (Gulf of Bothnia, from 0.1 to 0.4) and in the Gulf of Finland, (0.4 to 0.6) which are typically ice-covered areas. We hypothesize that in coastal areas a specific sequence of seasonal events, involving wintertime mixing and resuspension of benthic cysts, followed by proliferation in stratified thin layers under melting ice, favors successful seeding and accumulation of dense dinoflagellate populations over diatoms. This head-start of dinoflagellates by the onset of the spring bloom is decisive for successful competition with the faster growing diatoms. Massive cyst formation and spreading of cyst beds fuel the expanding and ever larger dinoflagellate blooms in the relatively shallow coastal waters. Shifts in the dominant spring bloom algal groups can have significant effects on major elemental fluxes and functioning of the Baltic Sea ecosystem, but also in the vast shelves and estuaries at high latitudes, where ice-associated cold-water dinoflagellates successfully compete with diatoms.	[Klais, Riina; Olli, Kalle] Univ Tartu, Inst Ecol & Earth Sci, EE-50090 Tartu, Estonia; [Tamminen, Timo; Kremp, Anke; Spilling, Kristian] Ctr Marine Res, Finnish Environm Inst, Helsinki, Finland	University of Tartu; Tartu University Institute of Ecology & Earth Sciences; Finnish Environment Institute	Klais, R (通讯作者)，Univ Tartu, Inst Ecol & Earth Sci, Ulikooli 18, EE-50090 Tartu, Estonia.	riina.klais@ut.ee	Kremp, Anke/I-8139-2013; Klais, Riina/G-6123-2010; Olli, Kalle/G-5389-2010; Spilling, Kristian/L-7932-2014	Spilling, Kristian/0000-0002-8390-8270; Klais-Peets, Riina/0000-0003-2895-1273	Estonian Science Foundation [7787]; Academy of Finland [128987]; 6th FP project THRESHOLDS [GOCE-003900]; Academy of Finland (AKA) [128987] Funding Source: Academy of Finland (AKA)	Estonian Science Foundation(Estonian Research Council); Academy of Finland(Research Council of Finland); 6th FP project THRESHOLDS; Academy of Finland (AKA)(Research Council of Finland)	This study was supported by the Estonian Science Foundation (grant 7787), the Academy of Finland (grant 128987), and the 6th FP project THRESHOLDS (GOCE-003900). The Estonian Science Foundation (http://www.etf.ee/index.php?page=3&) supported Riina Klais with a personal stipend supplement. The Academy of Finland (http://www.aka.fi/eng)supported financially Anke Kremp and Kristian Spilling. The large-scale phytoplankton dataset collection and harmonization was conducted within the EU 6th FP project THRESHOLDS. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	Alheit J, 2005, ICES J MAR SCI, V62, P1205, DOI 10.1016/j.icesjms.2005.04.024; ANDERSON JT, 1981, CAN J BOT, V59, P1793, DOI 10.1139/b81-240; [Anonymous], MAR ECOL PROG SER; [Anonymous], PHYTOPLANKTON ECOLOG; [Anonymous], 2001, R-News, DOI DOI 10.1159/000323281; [Anonymous], CANADIAN J FISHERIES; [Anonymous], 1979, Balt. Mar. Biol. 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J	Molina, E; Alegret, L; Apellaniz, E; Bernaola, G; Caballero, F; Dinarès-Turell, J; Hardenbol, J; Heilmann-Clausen, C; Larrasoaña, JC; Luterbacher, H; Monechi, S; Ortiz, S; Orue-Etxebarria, X; Payros, A; Pujalte, V; Rodríguez-Tovar, FJ; Tori, F; Tosquella, J; Uchman, A				Molina, Eustoquio; Alegret, Laia; Apellaniz, Estibaliz; Bernaola, Gilen; Caballero, Fernando; Dinares-Turell, Jaume; Hardenbol, Jan; Heilmann-Clausen, Claus; Larrasoana, Juan C.; Luterbacher, Hanspeter; Monechi, Simonetta; Ortiz, Silvia; Orue-Etxebarria, Xabier; Payros, Aitor; Pujalte, Victoriano; Rodriguez-Tovar, Francisco J.; Tori, Flavia; Tosquella, Josep; Uchman, Alfred			The Global Stratotype Section and Point (GSSP) for the base of the Lutetian Stage at the Gorrondatxe section, Spain	EPISODES			English	Article							DINOFLAGELLATE CYST BIOSTRATIGRAPHY; CALCAREOUS-NANNOPLANKTON; BETIC CORDILLERA; BASQUE COUNTRY; EOCENE; MIDDLE; STRATIGRAPHY; PALEOGENE; NANNOFOSSIL; BOUNDARY	The GSSP for the base of the Lutetian Stage (early/middle Eocene boundary) is defined at 167.85 metres in the Gorrondatxe sea-cliff section (NW of Bilbao city, Basque Country, northern Spain; 43 degrees 22'46.47 '' N, 3 degrees 00'51.61 '' W). This dark manly level coincides with the lowest occurrence of the calcareous nannofossil Blackites inflatus (CP12a/b boundary), is in the middle of polarity Chron C21r, and has been interpreted as the maximum-flooding surface of a depositional sequence that may be global in extent. The GSSP age is approximately 800 kyr (39 precession cycles) younger than the beginning of polarity Chron C21r, or similar to 47.8 Ma in the GTS04 time scale. The proposal was approved by the International Subcommission on Paleogene Stratigraphy in February 2010, approved by the International Commission of Stratigraphy in January 2011, and ratified by the International Union of Geological Sciences in April 2011.	[Molina, Eustoquio; Alegret, Laia; Ortiz, Silvia] Univ Zaragoza, Dept Ciencias Tierra, E-50009 Zaragoza, Spain; [Apellaniz, Estibaliz; Bernaola, Gilen; Caballero, Fernando; Orue-Etxebarria, Xabier; Payros, Aitor; Pujalte, Victoriano] Univ Basque Country, Dept Estratig & Paleontol, E-48080 Bilbao, Spain; [Dinares-Turell, Jaume] Ist Nazl Geofis & Vulcanol, Lab Paleomagnetismo, I-00143 Rome, Italy; [Hardenbol, Jan] Chronostratigraphy Inc, Global Sequence, Houston, TX 77079 USA; [Heilmann-Clausen, Claus] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Larrasoana, Juan C.] Inst Geol & Minero Espana, Unidad Zaragoza, E-50006 Zaragoza, Spain; [Luterbacher, Hanspeter] Seminario Conciliar, Museo Geol, E-08007 Barcelona, Spain; [Monechi, Simonetta; Tori, Flavia] Univ Florence, Dipartimento Sci Terra, I-50121 Florence, Italy; [Ortiz, Silvia] UCL, Dept Earth Sci, London WC1E 6BT, England; [Rodriguez-Tovar, Francisco J.] Univ Granada, Dept Estratig & Paleontol, E-18002 Granada, Spain; [Tosquella, Josep] Univ Huelva, Dept Geodinam & Paleontol, E-21071 Huelva, Spain; [Uchman, Alfred] Jagiellonian Univ, Inst Geol Sci, PL-30063 Krakow, Poland	University of Zaragoza; University of Basque Country; Istituto Nazionale Geofisica e Vulcanologia (INGV); Aarhus University; University of Florence; University of London; University College London; University of Granada; Universidad de Huelva; Jagiellonian University	Molina, E (通讯作者)，Univ Zaragoza, Dept Ciencias Tierra, E-50009 Zaragoza, Spain.	emolina@unizar.es	Payros, Aitor/Z-2150-2019; monechi, simonetta/AAN-6148-2020; Angrill, Josep/AAH-3086-2020; Bernaola, Gilen/AAA-6959-2019; Heilmann-Clausen, Claus/A-4848-2012; Rodríguez-Tovar, Francisco/AAA-9041-2020; Larrasoana, Juan/O-1350-2013; Ortiz, Silvia/AAA-4174-2019; Tosquella Angrill, Josep/I-2690-2018; /B-4320-2008; /B-5420-2008; Dinares-Turell, Jaume/G-2852-2011	Uchman, Alfred/0000-0002-0591-777X; Tosquella Angrill, Josep/0000-0001-7951-0561; Pujalte, Victoriano/0000-0003-1074-6132; Ortiz, Silvia/0000-0002-3027-7970; /0000-0001-5660-1428; BERNAOLA BILBAO, GILEN/0000-0003-1095-0854; Larrasoana, Juan Cruz/0000-0003-4568-631X; /0000-0002-8801-9544; Rodriguez-Tovar, Francisco/0000-0002-1400-2715; Dinares-Turell, Jaume/0000-0002-5546-2291; Payros, Aitor/0000-0001-9549-4119	Ministry of Science and Innovation of Spain; Town Council of Getxo; Basque Government	Ministry of Science and Innovation of Spain(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); Town Council of Getxo; Basque Government(Basque Government)	We would like to thank all people that collaborated in the long process of defining the base of the Lutetian. We greatly acknowledge those members of the Ypresian/Lutetian Working Group that could not attend the final Workshop in Getxo 2009, who actively participated studying the Gorrondatxe section and could not vote, but agree with the proposal. Furthermore, we are grateful to Stan Finney, Jim Ogg, Isabella Premoli Silva, Birger Schmitz, Paul Pearson, Hellen Coxall and Bridget Wade for constructive comments and suggestions, which improved the original proposal. Financial support was mainly provided by different projects of the Ministry of Science and Innovation of Spain, the Town Council of Getxo and the Basque Government.	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J	Goryacheva, AA				Goryacheva, A. A.			Palynostratigraphy of the Lower-Middle Jurassic Deposits, Borehole Section Vostok 4 (Southeast of West Siberia)	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						spores; pollen; dinoflagellate cysts; palynology; stratigraphy; Jurassic; West Siberia		This work presents the results of palynological investigation of the Vostok 4 borehole section situated in the Azharma region of the Ob-Irtysh facies area, where drilling has penetrated through the Urmanskaya, Ilansk, Peshkovskaya, and Tyumen formations. Six palynoassemblages are distinguished in the section based on the analyzed distribution of spores, pollen of terrestrial plants, and microphytoplankton. According to their succession, the section is subdivided into biostratigraphic units ranked as beds with palynomorphs. Comparative analysis and correlation with the Siberian palynostratigraphic standard scale of the Lower-Middle Jurassic, where succession of palynoassemblages is coordinated with ammonite zones, substantiate the Pliensbachian Bajocian age of the deposits studied. Diverse microphytoplankton (dinoflagellate cysts, acritarchs, prasinophytes, zignematacean and colonial algae) occurs throughout the section. The facies environment of sedimentation is reconstructed based on quantitative proportions of microphytoplankton taxa.	Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Goryacheva, AA (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk, Russia.	GoryachevaAA@ipgg.nsc.ru	Anna, Goryacheva/T-5116-2017	Anna, Goryacheva/0000-0002-9012-7376	Russian Foundation for Basic Research [09-05-00210]; RAS [25]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); RAS(Russian Academy of SciencesRegione Sardegna)	The work was supported by the Russian Foundation for Basic Research, project no. 09-05-00210, and by the RAS program no. 25.	[Anonymous], PALYNOLOGY PRINCIPLE; BATTEN D.J., 1996, PALYNOLOGY PRINCIPLE, V1, P205; Batten DJ., 1996, Palynology: principles and applications, P191; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; GLUSHKO NK, 1994, PALINOLOGICHESKIE KR, P37; GLUSHKO NK, 1988, USKORENIE POISKOV NE, P3; GLUSHKO NK, 1987, BIOSTRATIGRAFIYA MEZ, P12; GORYACHEVA AA, 2006, 7 EUR PAL PAL C PRAG, P50; GORYACHEVA AA, 2009, MAT VSER SOV 200 LET, P29; GORYACHEVA AA, 2008, GEOL GEOFIZ, V49, P205; GORYACHEVA AA, 2005, MAT 11 VSER PAL K PA, P57; Gurari F.G., 2005, Geological Structure and Hydrocarbon Potential of the Lower-Middle Jurassic in the West Siberian Province; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; ILINA VI, 1999, AKTUALNYE PROBLEMY P, P125; ILINA VI, 2003, PROBLEMY STRATIGRAFI, P49; ILINA VI, 1985, PALINOLOGIYA YURY SI; ILINA VI, 1997, BIOSTRATIGRAFIYA NEF, P86; KABANOVA VM, 1997, BIOSTR MIKR FAN EVR, P231; Kontorovich A.E., 1995, Geologiya i Geofizika, V36, P110; KOSTESHA ON, 1994, PALINOLOGICHESKIE KR, P71; KOSTESHA ON, 1991, GEOLOGIYA NEFTEGAZON, P55; MARKOVA LG, 1983, NOVYE DANNYE STRATIG, P41; MYASNIKOVA GP, 2003, PROBLEMY STRATIGRAFI, P68; Nikitenko B.L., 2000, STRATIGRAFIYA NEFTEG; PURTOVA SI, 1989, BIOSTRATIGRAFIYA OSA, P30; ROVNINA LV, 1994, PALINOLOGIYA STRATIG, P69; ROVNINA LV, 2002, METODICHESKIE ASPEKT, P219; ROVNINA LV, 1994, PALINOLOGICHESKIE KR, P52; ROVNINA LV, 2003, PROBLEMY STRATIGRAFI, P85; SHURYGIN BN, 1995, GEOL GEOFIZ, V36, P34; *SNIIGGIMS, 2004, 6 MEZHV STRAT SOV RA; Strother P.K., 1996, Palynology: Principles and Applications, Volume, V1, P81, DOI DOI 10.1016/0034-6667(95)00117-4; Vakhrameev V.A., 1988, Jurassic and Cretaceous Floras and Climates of the Earth; VAKULENKO LG, 2010, GEOL GEOFIZ, V51, P425	34	6	6	0	1	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	0869-5938			STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	JUN	2011	19	3					268	288		10.1134/S086959381103004X	http://dx.doi.org/10.1134/S086959381103004X			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	802WO					2025-03-11	WOS:000293541900002
J	Rundic, L; Ganic, M; Knezevic, S; Soliman, A				Rundic, Ljupko; Ganic, Meri; Knezevic, Slobodan; Soliman, Ali			Upper Miocene Pannonian sediments from Belgrade (Serbia): new evidence and paleoenvironmental considerations	GEOLOGICA CARPATHICA			English	Article						Late Miocene; Lake Pannon; Belgrade; sublittoral environment; endemism	LAKE PANNON; CENTRAL PARATETHYS; EASTERN PARATETHYS; MARGINAL MARINE; STYRIAN BASIN; FAUNA; PALEOGEOGRAPHY; INDICATORS; EVOLUTION; EVENTS	The Late Miocene sublittoral marls of the Pannonian Stage (the long-lived Lake Pannon) were studied. From neotectonic point of view, the investigated area represents a natural border between two different morphostructural domains: the Pannonian Basin to the north and the Peri-Pannonian Realm to the south. More than 20 mollusc and 34 ostracod species were identified which indicate the upper part of the Lower Pannonian and the lower part of the Middle Pannonian ("Serbian") predominantly. The identified dinoflagellate cyst assemblage (21 taxa) hinders assignment of the studied samples to a Pannonian substage but supports the high endemism of the Pannonian flora. The lithostratigraphical, paleontological, and paleoecological analyses indicate a mesohaline (8-16 parts per thousand), sublittoral (<90 m deep) environment of the early Lake Pannon. The estimated stratigraphic range for the investigated deposits is 9.8-11.4 Ma.	[Rundic, Ljupko; Ganic, Meri; Knezevic, Slobodan] Univ Belgrade, Dept Geol, Fac Min & Geol, Belgrade 11000, Serbia; [Soliman, Ali] Graz Univ, Inst Earth Sci Geol & Paleontol, A-8010 Graz, Austria	University of Belgrade; University of Graz	Rundic, L (通讯作者)，Univ Belgrade, Dept Geol, Fac Min & Geol, Kamenicka 6, Belgrade 11000, Serbia.	rundic@rgf.bg.ac.rs; merig@rgf.bg.ac.rs; knezevic.slobodan@gmail.com; ali.soliman@uni-graz.at	Soliman, Ali/R-1583-2018	Soliman, Ali/0000-0001-7366-4607; Rundic, LJupko/0000-0002-1598-9603	Ministry of Science and Technological Development, Republic of Serbia [176015]; Austrian Academy of Sciences; FWF-Project [P 21414-B16]	Ministry of Science and Technological Development, Republic of Serbia(Ministry of Education, Science & Technological Development, Serbia); Austrian Academy of Sciences; FWF-Project(Austrian Science Fund (FWF))	The Ministry of Science and Technological Development, Republic of Serbia (Project No. 176015) supported the study. AS wishes to thank the Austrian Academy of Sciences and FWF-Project No. P 21414-B16 for financial support. We are deeply grateful to Tadeusz Peryt (Polish Geological Institute, Warszawa), Martin Gross (Landesmuseum Joanneum, Graz) as well as three unknown reviewers who gave helpful remarks and critical comments on the manuscript.	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JUN	2011	62	3					267	278		10.2478/v10096-011-0021-z	http://dx.doi.org/10.2478/v10096-011-0021-z			12	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	793GH		gold			2025-03-11	WOS:000292807900006
J	Penaud, A; Eynaud, F; Sánchez-Goñi, M; Malaizé, B; Turon, JL; Rossignol, L				Penaud, A.; Eynaud, F.; Sanchez-Goni, M.; Malaize, B.; Turon, J. L.; Rossignol, L.			Contrasting sea-surface responses between the western Mediterranean Sea and eastern subtropical latitudes of the North Atlantic during abrupt climatic events of MIS 3	MARINE MICROPALEONTOLOGY			English	Article						Dinocysts; SST and SSS quantification; Dansgaard-Oeschger; Greenland and Heinrich stadials; Alboran Sea; Iberian margin	DINOFLAGELLATE CYST ASSEMBLAGES; MILLENNIAL-SCALE VARIABILITY; DEEP-WATER TEMPERATURE; HIGH-RESOLUTION RECORD; LAST 50,000 YR; ALBORAN-SEA; PLANKTONIC-FORAMINIFERA; DANSGAARD-OESCHGER; HEINRICH EVENTS; IBERIAN MARGIN	Dinoflagellate cyst (dinocyst) analysis was conducted on two cores from the SW Iberian margin and central Alboran Sea from which high quality records of Marine Isotope Stage 3 have been previously derived. Our aim in this study is to compare the dinocyst signature between 50 and 25 ka BP with existing datasets of foraminiferal and geochemical proxies related to hydrological parameters. Quantitative reconstructions of sea-surface temperatures (SSTs) and salinities (SSS) based on dinocysts are performed for the first time in this area. The results are compared to SSTs derived from planktonic foraminifera and alkenone measurements, and to SSS calculated from planktonic delta O-18 and foraminiferal SST. Significant oscillations related to Dansgaard-Oeschger cycles are recorded in both cores. Dinocyst-derived hydrological parameters exhibit synchronous fluctuations and similar values to those derived from the other methods, in particular when considering quantitative reconstructions for February based on foraminifera and dinocysts. Our study shows that the influence of subpolar waters was felt during each Greenland Stadial (GS) off Portugal, and that the amplification of the Heinrich Stadial cooling in the Alboran Sea was related to the penetration of subpolar waters through the Strait of Gibraltar. During Greenland Interstadials (GI), we provide evidence for the occurrence of warm and nutrient-rich sea-surface waters in the Alboran Sea, probably due to gyre-induced upwelling. Finally, the difference between August and February dinocyst SST estimates suggests higher seasonal contrasts during GS compared to Cl at the two core sites. Additionally, precession appears to have an imprint on dinocyst-derived long-term seasonality record. However, this observation needs to be confirmed by longer records. (c) 2011 Elsevier B.V. All rights reserved.	[Penaud, A.; Eynaud, F.; Malaize, B.; Turon, J. L.; Rossignol, L.] Univ Bordeaux 1, UMR EPOC 5805, F-33405 Talence, France; [Penaud, A.] IUEM UBO, UMR Domaines Ocean 6538, F-29280 Plouzane, France; [Sanchez-Goni, M.] EPHE, UMR EPOC 5805, F-33405 Talence, France	Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Universite PSL; Ecole Pratique des Hautes Etudes (EPHE); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Penaud, A (通讯作者)，Univ Bordeaux 1, UMR EPOC 5805, F-33405 Talence, France.	aurelie.penaud@univ-brest.fr	Sanchez Goñi, Maria Fernanda/R-3699-2019; Penaud, Aurelie/F-2485-2011	Penaud, Aurelie/0000-0003-3578-4549; Sanchez Goni, Maria Fernanda/0000-0001-8238-7488; Bruno, Malaize/0000-0002-5571-9990; Eynaud, Frederique/0000-0003-1283-7425	French CNRS	French CNRS(Centre National de la Recherche Scientifique (CNRS))	Thanks to the French polar institute IPEV (Institut Paul Emile Victor), the captain and the crew of the Marion Dufresne and the scientific team of the 1995 IMAGES cruise. We wish to thank Mr. Y. Balut for his assistance at sea and M. Castera and O. Ther for invaluable technical assistance at the laboratory. We gratefully acknowledge the reviewers, whose comments have enabled us to greatly improve this manuscript. We thank W. Fletcher for improving the English language of the manuscript. This study was supported by the French CNRS and contributes to the EuroCLIMATE project RESOLuTION.	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JUN	2011	80	1-2					1	17		10.1016/j.marmicro.2011.03.002	http://dx.doi.org/10.1016/j.marmicro.2011.03.002			17	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	793YB		Green Submitted			2025-03-11	WOS:000292858700001
J	Aydin, H; Matsuoka, K; Minareci, E				Aydin, Hilal; Matsuoka, Kazumi; Minareci, Ersin			Distribution of dinoflagellate cysts in recent sediments from Izmir Bay (Aegean Sea, Eastern Mediterranean)	MARINE MICROPALEONTOLOGY			English	Article						Aegean Sea; Alexandrium minutum; Dinoflagellate cyst; Toxic species	RECENT MARINE-SEDIMENTS; SP-NOV DINOPHYCEAE; GYMNODINIUM-CATENATUM; SURFACE SEDIMENTS; COASTAL WATERS; RESTING CYSTS; ASSEMBLAGES; BLACK; EUTROPHICATION; POLLUTION	To determine the species composition, abundance and horizontal distribution of dinoflagellate cysts in recent marine sediments, samples were collected at 13 stations in Izmir Bay, Aegean Sea. At least thirty-six dinoflagellate cyst types were identified, with the assemblages mainly dominated by Lingulodinium machaerophorum, Polykrikos kofoidii, Operculodinium centrocarpum, Gymnodinium cf. nolleri and Quinquecuspis concreta. Total cyst concentrations ranged from 41 to 3292 cystsg(-1) dry weight sediment. The majority of the cysts occurred in the inner and middle parts of the bay, where higher cyst concentrations were observed. According to the One Way Anova test, the difference between stations was significant statistically (p < 0.05). Two of the dinoflagellate cyst species have not been recorded previously as cysts or motile stages in Aegean marine waters; Gymnodinium cf. nolleri and Oblea acanthocysta. Alexandrium minutum and Alexandrium offine type cyst were observed at almost all stations although the cyst type of the Alexandrium catenella/tamarense complex was only found in the outer bay. These findings indicate potential seedbeds for initiation of future blooms and outbreaks of potentially toxic species in Izmir Bay. (c) 2011 Elsevier B.V. All rights reserved.	[Aydin, Hilal; Minareci, Ersin] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey; [Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8528521, Japan	Celal Bayar University; Nagasaki University	Minareci, E (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, Campus Muradiye, TR-45140 Manisa, Turkey.	ersinminareci@hotmail.com			Matsumae International Foundation, Japan	Matsumae International Foundation, Japan	The research was supported by funding from Matsumae International Foundation, Japan. Thanks to Institute for East China Sea Research Laboratory, Nagasaki University, Japan. Many thanks to Dr. Koichiro Mizushima, Dr. Hisae Kawami and Dr. Hyeon Hon Shin for their kind help.	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Micropaleontol.	JUN	2011	80	1-2					44	52		10.1016/j.marmicro.2011.03.004	http://dx.doi.org/10.1016/j.marmicro.2011.03.004			9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	793YB					2025-03-11	WOS:000292858700003
J	Carney, KJ; Delany, JE; Sawant, S; Mesbahi, E				Carney, K. J.; Delany, J. E.; Sawant, S.; Mesbahi, E.			The effects of prolonged darkness on temperate and tropical marine phytoplankton, and their implications for ballast water risk management	MARINE POLLUTION BULLETIN			English	Article						Phytoplankton; Dark incubation; Ballast water; Risk assessment	MICROCYSTIS-AERUGINOSA; DINOFLAGELLATE CYSTS; SURVIVAL STRATEGIES; MEDITERRANEAN SEA; MIDOCEAN EXCHANGE; DIATOM MORTALITY; DOMOIC ACID; BALTIC SEA; TRANSPORT; BLOOM	Phytoplankton assemblages from tropical (Goa) and temperate (UK) locations were exposed to a 28 day dark period, followed by a period of re-exposure to light. During this time phytoplankton survival and changes in nutrient concentrations were mapped. The tropical plankton water samples showed high nutrient levels after the dark period which were utilised by cells during the re-exposure period. UK experiments looked at the effect of three different water types on population recovery after the 28 day dark period, and differences due to seasonal effects. The population growth observed during the re-exposure period in the tropical population was comparable to that of the temperate population. Water type affected recovery and of the three tested media fresh seawater promoted the highest levels of growth. Seasonality had a significant influence on species survival. Understanding the effects of all these factors can aid the development of effective risk assessments in ballast water management. (C) 2011 Elsevier Ltd. All rights reserved.	[Carney, K. J.; Delany, J. 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J	Pestchevitskaya, E; Lebedeva, N; Ryabokon, A				Pestchevitskaya, Ekaterina; Lebedeva, Natalia; Ryabokon, Alyona			Uppermost Jurassic and lowermost Cretaceous dinocyst successions of Siberia, the Subarctic Urals and Russian Platform and their interregional correlation	GEOLOGICA CARPATHICA			English	Article						Upper Jurassic; Lower Cretaceous; Russia; bioevents; interregional correlation; dinoflagellate cysts	BIOSTRATIGRAPHY; BOUNDARY; SECTION; BASIN; MICROFORAMINIFERA; STRATIGRAPHY; PENINSULA; TETHYAN	Uppermost Jurassic and lowermost Cretaceous dinocyst successions calibrated against ammonite and foraminiferal zones were studied in five sections from North Siberia, the Subarctic Urals and the Russian Platform. Together with analysis of published palynological material on additional contemporaneous sections from the Russian Platform, our research provides a reliable regional correlation. The obtained biostratigraphic results are compared to palynological data from different regions of Europe, America, Australia and Antarctica using the method of first/last appearances of selected key species and evolutionary trends of dinocyst floras. Four correlative levels are defined in the middle parts of the Volgian and Berriasian and near their tops providing interregional correlation of dinocyst successions. These levels range within 1-1.5 ammonite zones as the first/last appearances of some key species have minor stratigraphic shifts in different sections that may be related to migration processes or to a different understanding of the stratigraphic position of ammonite zones.	[Pestchevitskaya, Ekaterina; Lebedeva, Natalia; Ryabokon, Alyona] Inst Petr Geol & Geophys SB RAS, Novosibirsk 630090, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Pestchevitskaya, E (通讯作者)，Inst Petr Geol & Geophys SB RAS, Av Ak Koptyug 3, Novosibirsk 630090, Russia.	PeschevickayaEB@ipgg.nsc.ru; LebedevaNK@ipgg.nsc.ru	Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303; Pestchevitskaya, Ekaterina/0000-0001-8174-0737	RFBR [09-05-00210]; Presidium of RAS [21, 25]	RFBR(Russian Foundation for Basic Research (RFBR)); Presidium of RAS(Russian Academy of Sciences)	We are grateful to Dr. J. Michalik, Dr. M. Smelror, Dr. P. Skupien, Dr. J. Clough and Dr. R. Blodgett for valuable criticism and useful suggestions. RFBR Grants 09-05-00210 and Grants by Presidium of RAS No. 21, 25.	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J	Solignac, S; Seidenkrantz, MS; Jessen, C; Kuijpers, A; Gunvald, AK; Olsen, J				Solignac, Sandrine; Seidenkrantz, Marit-Solveig; Jessen, Catherine; Kuijpers, Antoon; Gunvald, Anja K.; Olsen, Jesper			Late-Holocene sea-surface conditions offshore Newfoundland based on dinoflagellate cysts	HOLOCENE			English	Article						dinoflagellate cysts; Holocene; Labrador Current; Newfoundland; sea-ice; sea-surface conditions	CANADIAN ARCTIC ARCHIPELAGO; NORTH-ATLANTIC OSCILLATION; NORTHERNMOST BAFFIN-BAY; LABRADOR SEA; ICE COVER; HIGH-LATITUDES; CLIMATE; GREENLAND; VARIABILITY; SEDIMENTS	Dinoflagellate cysts and XRF core scanning data from two marine sediment cores from embayments north (Bonavista Bay) and south (Placentia Bay) of Newfoundland show significant changes in ocean and atmospheric conditions of the SW Labrador Sea region during the last 5700 years. Fresh and cold conditions, probably accompanied by seasonal sea ice, prevailed both north and south of Newfoundland from c. 5.7 to 4.0 cal. kyr BP. This may be linked to intensified Labrador Current export of cold meltwater and/or sea ice from the Arctic, presumably related to warmer conditions in the northernmost latitudes and the prevalence of strong (north)westerly winds. After c. 4.0 cal. kyr BP, sea-surface conditions warmed up and sea ice decreased northeast of Newfoundland, but conditions were still cold south of Newfoundland. This suggests a decrease in Arctic meltwater export and westerly wind strength. After 2.9-2.5 cal. kyr BP, only minor changes in sea-surface conditions affected the study sites. Sea-surface temperatures increased and sea ice decreased at both sites, which may be related to a more meridional atmospheric circulation pattern associated with the general Northern Hemisphere neoglacial cooling. In Placentia Bay the warmest part of the record corresponds to the Roman Warm Period, while the warmest part of the records in Bonavista Bay notably corresponds to the Dark Ages.	[Seidenkrantz, Marit-Solveig] Aarhus Univ, Dept Earth Sci, Ctr Climate Studies, DK-8000 Aarhus C, Denmark	Aarhus University	Seidenkrantz, MS (通讯作者)，Aarhus Univ, Dept Earth Sci, Ctr Climate Studies, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	mss@geo.au.dk	Jessen, Catherine/HDN-2985-2022; Seidenkrantz, Marit-Solveig/A-3451-2012; Olsen, Jesper/F-1656-2013	Solignac, Sandrine/0000-0003-3373-6922; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969; Olsen, Jesper/0000-0002-4445-5520	Kommisionen for Videnskabelige Undersogelser i Gronland; Danish Council for Independent Research (Nature and Universe) [09-069833/FNU]; EU [243908]; Danish Council for Independent Research [272-06-0604/FNU]	Kommisionen for Videnskabelige Undersogelser i Gronland; Danish Council for Independent Research (Nature and Universe)(Det Frie Forskningsrad (DFF)); EU(European Union (EU)); Danish Council for Independent Research(Det Frie Forskningsrad (DFF))	This study is a contribution to the Danish IPY 'NEWGREEN' project funded by 'Kommisionen for Videnskabelige Undersogelser i Gronland','TROPOLINK' funded by The Danish Council for Independent Research (Nature and Universe project no. 09-069833/FNU) and 'Past4Future' (EU FP7 project no. 243908). 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J	Bouchard, JN; Purdie, DA				Bouchard, Josee Nina; Purdie, Duncan A.			Temporal variation of caspase 3-like protein activity in cultures of the harmful dinoflagellates <i>Karenia brevis</i> and <i>Karenia mikimotoi</i>	JOURNAL OF PLANKTON RESEARCH			English	Article						caspase 3-like protein activity; cell death; harmful dinoflagellate; Karenia spp.	PROGRAMMED CELL-DEATH; RED TIDE DINOFLAGELLATE; HEAT-STRESS; PHYTOPLANKTON; APOPTOSIS; METACASPASES; INDUCTION; GROWTH; PHOTOSYNTHESIS; CYANOBACTERIUM	To better understand the role of caspase-like proteins in the cellular activities of harmful dinoflagellates, cultures of Karenia brevis and Karenia mikimotoi were monitored over a 56-day period. The cellular abundance, maximum photochemical efficiency of photosystem II (F-v/F-m), percentage of dead cells (revealed by SYTOX-labelling of nuclei of cells with a compromised membrane) and the variation in caspase 3-like protein activity were monitored every 7 days. During the cultures' late decline phase, DNA degradation was also confirmed in Karenia cells using a terminal deoxynucletidyl transferase-mediated dUTP nick end labelling assay. Karenia brevis reached its maximal cellular abundance after 3 weeks then declined to its lowest value on Day 56. In cells of K. brevis the caspase 3-like activity likely served some housekeeping functions as demonstrated by the constitutive level of activity observed throughout the whole experiment (similar to 3000-6664 RFU/h/mg protein). The increase in activity which occurred on Days 21 and 28 (similar to 38 000 RFU/h/mg protein on Day 28) coincided with the appearance cyst-like structures in the cultures and suggests a role in the encystment progression of K. brevis. For K. mikimotoi, the highest cellular abundance was reached on Day 42 after which it declined to reach its lowest value, along with the highest percentage of dead cells, on Day 56. The caspase 3-like protein activity (<1300 RFU/h/mg protein) was elevated at the beginning of the experiment (on Days 0, 7 and 14) and just before the decline in cellular abundance (on Days 35 and 42) and likely played some housekeeping functions as well as a role in the death of the cells. This study demonstrates the involvement of caspase 3-like protein activity in a variety of processes in cells of the harmful algae K. brevis and K. mikimotoi.	[Bouchard, Josee Nina; Purdie, Duncan A.] Univ Southampton, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	NERC National Oceanography Centre; University of Southampton	Bouchard, JN (通讯作者)，Univ Southampton, Natl Oceanog Ctr, Waterfront Campus,European Way, Southampton SO14 3ZH, Hants, England.	josee_bouchard@yahoo.com		Purdie, Duncan/0000-0001-6672-1722	Fonds quebecois de la recherche sur la nature et les technologies (FQRNT); NOCS	Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); NOCS	This work was supported by a postdoctoral fellowship awarded to J.N.B. by the Fonds quebecois de la recherche sur la nature et les technologies (FQRNT). Consumable costs were provided by a NOCS Interface Fund to D. A. P and Dr P. Townsend.	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Plankton Res.	JUN	2011	33	6					961	972		10.1093/plankt/fbq158	http://dx.doi.org/10.1093/plankt/fbq158			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	761JO		Green Submitted, Bronze			2025-03-11	WOS:000290394300011
J	Price, AM; Pospelova, V				Price, Andrea M.; Pospelova, Vera			High-resolution sediment trap study of organic-walled dinoflagellate cyst production and biogenic silica flux in Saanich Inlet (BC, Canada)	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Saanich Inlet; Sediment trap; Phytoplankton; Biogenic silica; Palynomorphs; Tintinnid loricae	BRITISH-COLUMBIAN FJORDS; BENGUELA UPWELLING SYSTEM; RECENT MARINE-SEDIMENTS; NEW-ENGLAND USA; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; SURFACE SEDIMENTS; ARABIAN SEA; ASSEMBLAGES	Dinoflagellate cyst fluxes and assemblage composition were investigated from November 2007 to February 2010 in Patricia Bay, Saanich Inlet (BC, Canada). Samples were collected using a sediment trap deployed at similar to 97 m water depth. The sampling interval ranged from 0.5 to 19.5 days, allowing for a high-resolution study of dinoflagellate cyst production in relation to measured environmental parameters. Ninety-six samples were collected and a total of 42 dinoflagellate cyst taxa were identified. The dinoflagellate cyst flux was very high and ranged from similar to 149,000 to similar to 2,400,000 cysts m(-2) day(-1), with an average of similar to 777,000 cysts m(-2) day(-1). Seasonal and interannual variation in cyst assemblage was recorded. It reflects changes in environmental parameters such as sea-surface temperature, sea-surface salinity, solar insolation, river discharge, and biogenic silica flux. Fluxes of cysts produced by autotrophic dinoflagellates, particularly Spiniferites spp. and Spiniferites bentorii, were greatest during winter. Spring dinoflagellate cyst assemblages were dominated by Brigantedinium spp. and Quinquecuspis concreta. In summer the assemblages were characterized by an increase of cysts produced by heterotrophic dinoflagellates, in particular by Echinidinium delicatum, E. cf. delicatum, Votadinium spinosum and cysts of Protoperidinium minutum. Multivariate statistical analysis performed on the data supports the observed seasonal trends, where winter taxa are associated with low sea-surface temperatures, low salinity, and high Cowichan River discharge, whereas summer taxa are associated with warmer sea-surface temperatures, higher solar insolation and increased biogenic silica flux. The cyst assemblage from nearby surface sediment was shown to be very similar to an annual average sediment trap assemblage. (c) 2011 Elsevier B.V. All rights reserved.	[Price, Andrea M.; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, OEASB, Victoria, BC V8W 3V6, Canada	University of Victoria	Price, AM (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, OEASB, PO A405,Box 3065 STN CSC, Victoria, BC V8W 3V6, Canada.	pricea@uvic.ca; vpospe@uvic.ca		Price, Andrea/0000-0002-5359-053X; Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	Funding was provided by the Natural Sciences and Engineering Research Council of Canada (NSERC). We would like to thank Dr. Jim Gower for providing data from buoy 46134, Edward Wiebe (University of Victoria) for providing atmospheric parameters collected at Deep Cove Elementary School, and Maureen Soon (University of British Columbia) for biogenic silica analysis. The VENUS team and Jonathan Rose (University of Victoria) played a crucial role in deploying and maintaining the sediment trap, as well as retrieval of the samples. We also thank Drs. Richard Jordan, Kenneth Mertens and an anonymous reviewer for their constructive comments.	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Micropaleontol.	JUN	2011	80	1-2					18	43		10.1016/j.marmicro.2011.03.003	http://dx.doi.org/10.1016/j.marmicro.2011.03.003			26	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	793YB					2025-03-11	WOS:000292858700002
J	Houben, AJP; Bijl, PK; Guerstein, GR; Sluijs, A; Brinkhuis, H				Houben, Alexander J. P.; Bijl, Peter K.; Raquel Guerstein, G.; Sluijs, Appy; Brinkhuis, Henk			<i>Malvinia escutiana</i>, a new biostratigraphically important Oligocene dinoflagellate cyst from the Southern Ocean	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cysts; peridinioid; Eocene; Oligocene; Southern Ocean; Antarctic glaciation	EOCENE-OLIGOCENE; MIDDLE EOCENE; CLIMATE; SEDIMENTS; GLACIATION; TRANSITION; TERTIARY; DIATOMS	The Eocene-Oligocene Transition (EOT. similar to 34 Ma) represents the culmination of Eocene cooling by the initiation of large-scale Antarctic glaciation. Recognition and correlation of the EOT in Southern Ocean sedimentary successions have been difficult as a result of the general lack of well-calibrated biostratigraphic markers. Here we describe an unusual hypnozygotic organic walled dinoflagellate cyst (dinocyst) that originated in the Southern Ocean in conjunction with the onset of major Antarctic glaciation as reflected by 'oxygen isotope event 1' (Oi-1). We restudied samples from Deep Sea Drilling Program (DSDP) Site 511 using Light Microscopy and Scanning Electron Microscopy and found that a taxon previously known as Formal constitutes a new protoperidinioid dinocyst genus and species that we name Malvinia escutiana. Published and re-evaluated data from other Southern Ocean sites show that M. escutiana did not occur before the Oi-1 (33.7 Ma), emphasizing its potential as a useful biostratigraphic marker for this key interval in the Southern Ocean's Cenozoic climate history. (C) 2011 Elsevier B.V. All rights reserved.	[Houben, Alexander J. P.; Bijl, Peter K.; Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Raquel Guerstein, G.] Univ Nacl Sur, Inst Geol Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	Utrecht University; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Houben, AJP (通讯作者)，Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	A.J.P.Houben@uu.nl	Brinkhuis, Henk/B-4223-2009; Sluijs, Appy/B-3726-2009	Sluijs, Appy/0000-0003-2382-0215; Guerstein, G. Raquel/0000-0003-1623-1084; Houben, Alexander/0000-0002-9497-1048; Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012	Statoil; Netherlands Organisation for Scientific Research (NWO); LPP Foundation; Utrecht University; European Research Council under the European Community [259627]; US National Science Foundation (NSF)	Statoil; Netherlands Organisation for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); LPP Foundation; Utrecht University; European Research Council under the European Community(European Research Council (ERC)); US National Science Foundation (NSF)(National Science Foundation (NSF))	The authors thank Statoil (A.J.P.H.), the Netherlands Organisation for Scientific Research (NWO), the LPP Foundation and Utrecht University (P.K.B.) for funding. The research leading to these results has received funding from the European Research Council under the European Community's Seventh Framework Program (FP7/2007-2013)/ERC Grant agreement no. 259627 to A.S. This study used samples provided by the Deep Sea Drilling Project (DSDP). DSDP was sponsored by the US National Science Foundation (NSF). We thank Natasja Welters, Leonard Bik and Jan van Tongeren for technical support. Steven M. Bohaty, Rob Fensome and Andres Boltovskoy are thanked for helpful suggestions. We are grateful to Jorg Pross for his constructive review, which significantly improved this manuscript.	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Palaeobot. Palynology	JUN	2011	165	3-4					175	182		10.1016/j.revpalbo.2011.03.002	http://dx.doi.org/10.1016/j.revpalbo.2011.03.002			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	780ZE		Green Published			2025-03-11	WOS:000291899600004
J	Sliwinska, KK; Heilmann-Clausen, C				Sliwinska, Katarzyna K.; Heilmann-Clausen, Claus			Early Oligocene cooling reflected by the dinoflagellate cyst <i>Svalbardella cooksoniae</i>	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cysts; Eastern North Sea; Early Oligocene; Oila cooling event; Paleoclimate; Sea level change; Svalbardella cooksoniae; Areosphaeridium diktyoplokum	NORTH-SEA BASIN; NEW-JERSEY; EOCENE; SEQUENCE; STRATIGRAPHY; BIOSTRATIGRAPHY; CALIBRATION; STRATOTYPE; ANTARCTICA; TRANSITION	The early Oligocene interval in several boreholes from the eastern North Sea and Denmark has been studied for dinoflagellate cysts. The cold water dinoflagellate cyst Svalbardella cooksoniae was recorded in a narrow lowermost Oligocene interval in all offshore sections. A critical evaluation of previous records of Svalbardella cooksoniae reveals that it is present in the same narrow interval of Chron 12r, close to the NP21/NP22 boundary in many high and mid latitude Northern Hemisphere sections, ranging from the Greenland Sea in the north to Italy in the south. The Svalbardella cooksoniae interval is closely associated with the LO of the dinoflagellate cyst Areosphaeridium diktyoplokum. The age of the Svalbardella cooksoniae event indicates that it is synchronous with the Oi1a oxygen isotope maximum of Pekar and Miller (1996) and Pekar et al. (2002). In the Danish land area the Svalbardella cooksoniae interval and hence the Oi1a event is shown to coincide with an unconformity. A regional comparison shows that synchronous unconformities are present also in Belgium and New Jersey. A slightly older regional unconformity occurring on both sides of the North Atlantic coincides with the Oi1 oxygen isotope maximum of Pekar and Miller (1996). The finding of a sedimentary package separated by two successive regional unconformities is interpreted to reflect a significant, temporary eustatic sea level rise, and hence a melting phase on the East Antarctic ice sheet between the Oi1 and Oi1a glacioeustatic sea level falls. The paleogeographic distribution and lower frequency of Svalbardella during the earliest Oligocene Oi1a event, as compared with the mid Oligocene Oi2b Svalbardella spp. event, suggest that the Oi1a glacial episode was less severe than the Oi2b glaciation. This is in agreement with recent ice volume estimates for the two events. (C) 2011 Elsevier B.V. All rights reserved.	[Sliwinska, Katarzyna K.; Heilmann-Clausen, Claus] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark	Aarhus University	Sliwinska, KK (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	kasia.sliwinska@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; Sliwinska, Kasia K./G-9097-2018	Sliwinska, Kasia K./0000-0001-5488-8832	Aarhus University (Denmark); Fur Museum (Denmark)	Aarhus University (Denmark); Fur Museum (Denmark)	Kirsten Rosendal, Department of Earth Sciences (Aarhus University), prepared the samples and Bartosz Goledowski, Department of Earth Sciences (Aarhus University), made an outline for Fig. 1B. Katarzyna K. Sliwinska acknowledges financial support for her PhD project from the Aarhus University (Denmark) and Fur Museum (Denmark). The Norwegian Petroleum Directorate (NPD) is acknowledged for placing palynological preparations from the 11/10-1 well at our disposal. The first author thanks Mikkel Jurgens for inspiring discussions and criticism of the first version of the manuscript. Robert Knox (British Geological Survey) and a second anonymous reviewer are thanked for their thoughtful and constructive suggestions and corrections which substantially improved the manuscript	BARTEK LR, 1991, J GEOPHYS RES-SOLID, V96, P6753, DOI 10.1029/90JB02528; 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; Bohaty SM, 2003, GEOLOGY, V31, P1017, DOI 10.1130/G19800.1; BRINKHUIS H, 1993, MAR MICROPALEONTOL, V22, P131, DOI 10.1016/0377-8398(93)90007-K; Coccioni R, 2008, GEOL SOC AM BULL, V120, P487, DOI 10.1130/B25988.1; Danielsen M, 1997, MAR PETROL GEOL, V14, P931, DOI 10.1016/S0264-8172(97)00043-3; De Coninck J., 1999, B SOC BELG GEOL, V105, P171; De Man E, 2004, NETH J GEOSCI, V83, P193, DOI 10.1017/S0016774600020266; DeConto RM, 2003, NATURE, V421, P245, DOI 10.1038/nature01290; DeConto RM, 2008, NATURE, V455, P652, DOI 10.1038/nature07337; Eidvin T, 2007, NORW J GEOL, V87, P75; Eldrett JS, 2009, MAR MICROPALEONTOL, V73, P226, DOI 10.1016/j.marmicro.2009.10.004; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Firth John V., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P203; Gedl P, 2004, GEOL SOC SPEC PUBL, V230, P309, DOI 10.1144/GSL.SP.2004.230.01.16; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; HEAD JM, 1989, P OC DRILL PROGR SCI, P515; Heilmann-Clausen C, 1995, DANMARKS GEOLOGI KRI, P69; Heilmann-Clausen C., 2017, Naturen i Danmark: Geologien, V3rd, P181; HEILMANNCLAUSEN C, 1992, FINAL BIOSTRATIGRAPH, P1; Huuse M, 2001, MAR GEOL, V177, P243, DOI 10.1016/S0025-3227(01)00168-2; Huuse M, 2001, BASIN RES, V13, P17, DOI 10.1046/j.1365-2117.2001.00123.x; HYLAND E, 2009, SPECIAL PAPER GEOLOG, P303; Kothe A., 1990, Geologisches Jahrbuch Reihe A, P3; KOTHE A, 2003, DINOZYSTEN ZONIERUNG, V22, P895; Lagrou D, 2004, NETH J GEOSCI, V83, P209, DOI 10.1017/S001677460002028X; Lavier LL, 2001, MAR GEOL, V178, P63, DOI 10.1016/S0025-3227(01)00175-X; Lund J.J., 2002, NO EUROPEAN CENOZOIC, P83; Luterbacher HP., 2004, GEOLOGIC TIME SCALE, P384; MANUM S., 1960, NYTT MAG BOT, V8, P17; Manum S.B., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P611, DOI 10.2973/odp.proc.sr.104.176.1989; MANUM SB, 1976, DINOCYSTS TERTIARY N, P897; Martinsen O.J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European Basins, P91; Nielsen SB, 2009, J GEODYN, V47, P72, DOI 10.1016/j.jog.2008.09.001; Pälike H, 2006, SCIENCE, V314, P1894, DOI 10.1126/science.1133822; Pagani M, 2005, SCIENCE, V309, P600, DOI 10.1126/science.1110063; Pearson PN, 2009, NATURE, V461, P1110, DOI 10.1038/nature08447; Pekar S, 1996, GEOLOGY, V24, P567, DOI 10.1130/0091-7613(1996)024<0567:NJOISO>2.3.CO;2; Pekar SF, 2002, GEOLOGY, V30, P903, DOI 10.1130/0091-7613(2002)030<0903:CBEEFB>2.0.CO;2; Pekar SF, 2001, GEOLOGY, V29, P55, DOI 10.1130/0091-7613(2001)029<0055:ETSRTE>2.0.CO;2; Pekar SF, 2000, SEDIMENT GEOL, V134, P93, DOI 10.1016/S0037-0738(00)00015-4; Pekar SF, 2008, PALAEOGEOGR PALAEOCL, V260, P41, DOI 10.1016/j.palaeo.2007.08.019; Pollard D, 2005, GLOBAL PLANET CHANGE, V45, P9, DOI 10.1016/j.gloplacha.2004.09.011; Pross J, 2010, REV PALAEOBOT PALYNO, V158, P213, DOI 10.1016/j.revpalbo.2009.09.002; Schioler P, 2005, J MICROPALAEONTOL, V24, P1, DOI 10.1144/jm.24.1.1; Sliwinska KK, 2010, MAR PETROL GEOL, V27, P1424, DOI 10.1016/j.marpetgeo.2010.03.008; SLIWINSKA KK, 2011, EGU GEN ASS 2011 GEO, P13; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; STEURBAUT E, 1986, MEDEDELINGEN WERKGRO, V23, P49; Thomsen E., 1995, 19 AARH U GEOL I, P1; Van Mourik C.A., 2005, Stratigraphy, V2, P13; Van Simaeys S, 2005, REV PALAEOBOT PALYNO, V134, P105, DOI 10.1016/j.revpalbo.2004.12.003; Van Simaeys S, 2005, GEOLOGY, V33, P709, DOI 10.1130/G21634.1; Vandenberghe Noel, 2003, P419; WILLIAMS GL, 2004, 189 SCI RES ODP LEG; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	58	14	15	0	9	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAY 15	2011	305	1-4					138	149		10.1016/j.palaeo.2011.02.027	http://dx.doi.org/10.1016/j.palaeo.2011.02.027			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	773EY					2025-03-11	WOS:000291291000012
J	Kumar, A				Kumar, Arun			Acid-resistant Cretaceous thecamoebian tests from the Arabian Peninsula: a suggestion for study of agglutinated rhizopods in palynological slides	JOURNAL OF MICROPALAEONTOLOGY			English	Article						thecamoebians; Cretaceous; Arabian Peninsula; Palynology	VASE-SHAPED MICROFOSSILS; ARCELLACEANS THECAMOEBIANS; NOVA-SCOTIA; CHUAR GROUP; AMEBAS; ASSEMBLAGES; PALEOECOLOGY; FORAMINIFERA; INDICATORS; ISLAND	Rare specimens of Centropyxis aculeata (Ehrenberg, 1832), cf. Difflugia oblonga (Ehrenberg, 1832), Amphitrema flavum (Archer, 1869) and an unidentified spherical form (similar to a protozoan 'cyst' in van Hengstum et al., 2007) were observed in the palynological preparations of cutting samples from a drill-hole in southern Saudi Arabia. These thecamoebians were found in Cretaceous formations in association with typical Cretaceous spore, pollen and dinoflagellate cysts. Since the youngest rock formation in this drill-hole is of Cretaceous age, contamination due to caving from post-Cretaceous sediments is thus ruled out. Although the oldest record of thecamoebians comes from Neoproterozoic strata, their pre-Holocene occurrences are rare and patchy. Since many thecamoebian tests are autogenous and are made of acid-resistant proteinaceous material, they occur in the palynological preparations of fossil sediments. It is suggested that careful observation and search for thecamoebians in palynological slides could potentially lead to new discoveries of these microfossils from Phanerozoic sediments from all over the world. J. Micropalaeontol. 30(1): 1-5, May 2011.	King Fahd Univ Petr & Minerals, Res Inst, Ctr Petr & Minerals, Dhahran 31261, Saudi Arabia	King Fahd University of Petroleum & Minerals	Kumar, A (通讯作者)，King Fahd Univ Petr & Minerals, Res Inst, Ctr Petr & Minerals, Dhahran 31261, Saudi Arabia.	arunkumarlko@hotmail.com						Al-Husseini M, 2008, GEOARABIA, V13, P89; Al-Husseini M, 2008, GEOARABIA, V13, P11; [Anonymous], 9 QUAT RES ASS; BEYENS L, 1990, POLAR BIOL, V10, P431, DOI 10.1007/BF00233691; Bradley W.H., 1931, US GEOLOGICAL SURVEY, V168, P1; Charman DJ, 2002, J QUATERNARY SCI, V17, P387, DOI 10.1002/jqs.703; Dalby AP, 2000, J FORAMIN RES, V30, P135, DOI 10.2113/0300135; Farooqui A., 2010, Earth Science India, V3, P146; Farooqui A, 2007, CURR SCI INDIA, V92, P992; Foissner W, 2001, EUR J PROTISTOL, V37, P167, DOI 10.1078/0932-4739-00012; FRENGUELLI G., 1933, B SOC GEOL ITAL, V52, P33; Kovary J., 1956, Foldtani Kozlony, V86, P266; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; KUMAR A, 2000, ENV MICROPALEONTOLOG, P257; MEDIOLI FS, 1990, NATO ADV SCI I C-MAT, V327, P813; MEDIOLI FS, 1990, NATO ADV SCI I C-MAT, V327, P793; Pande AC, 2004, J GEOL SOC INDIA, V63, P665; Patterson RT, 2000, J FORAMIN RES, V30, P310, DOI 10.2113/0300310; Patterson RT, 2000, T GEOBIOL, V15, P257; Patterson RT, 2002, PALAEOGEOGR PALAEOCL, V180, P225, DOI 10.1016/S0031-0182(01)00430-8; POINAR GO, 1993, SCIENCE, V259, P222, DOI 10.1126/science.259.5092.222; Porter SM, 2000, PALEOBIOLOGY, V26, P360, DOI 10.1666/0094-8373(2000)026<0360:TAITNE>2.0.CO;2; Porter SM, 2003, J PALEONTOL, V77, P409, DOI 10.1666/0022-3360(2003)077<0409:VMFTNC>2.0.CO;2; Roe HM, 2002, J QUATERNARY SCI, V17, P411, DOI 10.1002/jqs.704; Schiller Wolfgang, 1997, Courier Forschungsinstitut Senckenberg, V201, P385; Schiller Wolfgang, 1998, Geologische Abhandlungen Hessen, V104, P173; Schmidt AR, 2004, PALAEONTOLOGY, V47, P185, DOI 10.1111/j.0031-0239.2004.00368.x; Schónborn W, 1999, J EUKARYOT MICROBIOL, V46, P571, DOI 10.1111/j.1550-7408.1999.tb05133.x; Scott DB, 2003, MICROPALEONTOLOGY, V49, P109, DOI 10.2113/49.2.109; SRIVASTAVA SC, 1998, GEOPHYTOLOGY, V26, P75; van Hengstum PJ, 2007, J FORAMIN RES, V37, P300, DOI 10.2113/gsjfr.37.4.300; VASICEK M., 1957, SBORNIK NARADNIHO B, V13, P333; Waggoner Benjamin M., 1996, Paleobios, V17, P20; Waggoner Benjamin M., 1996, Paleobios, V17, P17; WIGHTMAN WG, 1994, PALAEOGEOGR PALAEOCL, V106, P187, DOI 10.1016/0031-0182(94)90010-8; WIGHTMAN WG, 1992, GEOL SOC AM ANN M, V24; Wolf Monika, 1995, Palaeontologische Zeitschrift, V69, P1; Woodland WA, 1998, HOLOCENE, V8, P261, DOI 10.1191/095968398667004497	38	11	11	0	5	COPERNICUS GESELLSCHAFT MBH	GOTTINGEN	BAHNHOFSALLEE 1E, GOTTINGEN, 37081, GERMANY	0262-821X	2041-4978		J MICROPALAEONTOL	J. Micropalaentol.	MAY	2011	30		1				1	5		10.1144/0262-821X10-018	http://dx.doi.org/10.1144/0262-821X10-018			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	767HT		hybrid			2025-03-11	WOS:000290847000001
J	Riboulleau, A; Tribovillard, N; Baudin, F; Bout-Roumazeilles, V; Lyons, TW				Riboulleau, Armelle; Tribovillard, Nicolas; Baudin, Francois; Bout-Roumazeilles, Viviane; Lyons, Timothy W.			Unexpectedly low organic matter content in Cariaco Basin sediments during the Younger Dryas: Origin and implications	COMPTES RENDUS GEOSCIENCE			English	Article						Cariaco Basin; Upwelling; Diatoms; Dinoflagellates; Geochemistry; Organic matter	INTERTROPICAL CONVERGENCE ZONE; RAPID CLIMATE CHANGES; LAST DEGLACIATION; DINOFLAGELLATE CYSTS; TROPICAL ATLANTIC; C-14 CALIBRATION; VENEZUELA; PRODUCTIVITY; CYCLE; PHYTOPLANKTON	The Cariaco Basin (offshore Venezuela), the second largest anoxic basin after the Black Sea, knew intense upwelling activity and maximum primary production during the Younger Dryas (12.9-11.5 ka cal. BP). Relatively low total organic carbon (TOC) contents are, however, observed in the sediment deposited during this interval. Previous studies have attributed these low TOC values to dilution by inorganic phases during a time of high sediment accumulation rate. The present study demonstrates that the low TOC values result primarily from a relatively reduced flux of organic matter (OM) to the sediment and minor dilution by carbonate. Excellent preservation of the OM during this interval excludes OM degradation as a cause for low TOC values. Consistent with palynological observation and biomarker analyses, the lower relative flux of OM to the sediment is related to changes in the primary producers, with a significant decrease in the contribution of organic-walled organisms during the Younger Dryas. These results, that highlight the need of caution when using TOC values as paleoproductivity or paleoenvironmental indicator, underline the important role of organic-walled primary producers in the organic enrichment of sediments. (C) 2011 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.	[Riboulleau, Armelle; Tribovillard, Nicolas; Bout-Roumazeilles, Viviane] Univ Lille 1, FRE CNRS Geosyst 3298, F-59655 Villeneuve Dascq, France; [Baudin, Francois] Univ Paris 06, UPMC, F-75252 Paris 05, France; [Baudin, Francois] CNRS, UMR iSTeP 7193, F-75252 Paris 05, France; [Lyons, Timothy W.] Univ Calif Riverside, Dept Earth Sci, Riverside, CA 92521 USA	Universite de Lille; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of California System; University of California Riverside	Riboulleau, A (通讯作者)，Univ Lille 1, FRE CNRS Geosyst 3298, Batiment SN5, F-59655 Villeneuve Dascq, France.	armelle.riboulleau@univ-lille1.fr; nicolas.tribovillard@univ-lille1.fr; francois.baudin@upmc.fr; viviane.bout@univ-lille1.fr; timothyl@ucr.edu	Tribovillard, Nicolas/B-6185-2009; Riboulleau, Armelle/G-4719-2012; Lyons, Timothy/ADT-8795-2022; Baudin, Francois/ITU-7485-2023; BOUT-ROUMAZEILLES, Viviane/AAD-5259-2019	Riboulleau, Armelle/0000-0002-2717-8330; Baudin, Francois/0000-0003-3180-459X; Tribovillard, Nicolas/0000-0003-3493-5579; Bout-Roumazeilles, Viviane/0000-0001-6917-818X	"Enfouissement organique dans le Bassin de Cariaco : controles climatique et diagenetique"	"Enfouissement organique dans le Bassin de Cariaco : controles climatique et diagenetique"	We wish to thank the ODP program for providing sediment samples from core 1002 as well as the IMAGES program and crew of the R/V Marion Dufresne. Financial support for this study was provided by the project "Enfouissement organique dans le Bassin de Cariaco : controles climatique et diagenetique" through the French national EVE-CYBER-LEFE program (INSU-CNRS). Larry Peterson is greatly acknowledged for providing MAR data from core PL07-39PC. J.R. Disnar, P. Martinez and A.-Y. Huc are acknowledged for their constructive comments on the manuscript.	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R. Geosci.	MAY	2011	343	5					351	359		10.1016/j.crte.2011.04.001	http://dx.doi.org/10.1016/j.crte.2011.04.001			9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	783EF		Green Submitted			2025-03-11	WOS:000292063600004
J	Wang, ZH; Mu, DH; Li, YF; Cao, Y; Zhang, YJ				Wang, Zhao-Hui; Mu, De-Hai; Li, You-fu; Cao, Yu; Zhang, Yu-Juan			Recent eutrophication and human disturbance in Daya Bay, the South China Sea: Dinoflagellate cyst and geochemical evidence	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						cyst; biogenic silica; organic carbon; total nitrogen; eutrophication; nuclear power station	NEW-BEDFORD HARBOR; RESTING CYSTS; SEDIMENTARY RECORD; MASSACHUSETTS USA; APPONAGANSETT BAY; PB-210; PRESERVATION; DINOPHYCEAE; INDICATORS; ESTUARIES	Recent trends in eutrophication and human disturbance were evaluated using dinoflagellate resting cysts and geochemical parameters. Analyses were performed on three sediment cores from Daya Bay, South China Sea covering the past hundred years. Changes in cyst assemblages as well as geochemical parameters including biogenic silica (BSi), organic carbon (OC) and total nitrogen (TN) reflected environmental change in the area. The clear increase in overall cyst concentration and the prominence of Scrippsiella cysts suggested an increase in cultural eutrophication which began in the 1970s and become evident since 1985. Large fluctuation in cyst assemblages and BSi in the upper 22 cm signaled the influence of construction and operation of nuclear power stations on phytoplankton community and environments, with an increase in the early stage of construction, a rapid decline in the late stage of construction and early operation, and then a sharp increase thereafter. High Alexandrium cyst abundance in shallowest sediments was consistent with high PSP levels and PSP events in the area, and the persistent toxicity suggests recurrent seeding from the rich cyst bed in these surface sediments. (C) 2011 Elsevier Ltd. All rights reserved.	[Wang, Zhao-Hui; Li, You-fu; Cao, Yu; Zhang, Yu-Juan] Jinan Univ, Inst Hydrobiol, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China; [Wang, Zhao-Hui] Minist Educ, Engn Res Ctr Trop & Subtrop Aquat Ecol Engn, Guangzhou 510632, Guangdong, Peoples R China; [Mu, De-Hai] Guangdong Prov Key Lab Emergency Test Dangerous C, Guangzhou 510070, Guangdong, Peoples R China	Jinan University; Chinese Academy of Sciences	Wang, ZH (通讯作者)，Jinan Univ, Inst Hydrobiol, Coll Life Sci & Technol, Guangzhou 510632, Guangdong, Peoples R China.	twzh@jnu.edu.cn			National Natural Science Foundation of China [40773063, 40873065, U0633006]	National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	The authors gratefully acknowledge Dr. Kevin G. Sellner of Chesapeake Research Consortium, Inc. USA for reviewing the manuscript. This research was financially supported by National Natural Science Foundation of China (40773063, 40873065, U0633006).	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Coast. Shelf Sci.	MAY 1	2011	92	3					403	414		10.1016/j.ecss.2011.01.015	http://dx.doi.org/10.1016/j.ecss.2011.01.015			12	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	770WP					2025-03-11	WOS:000291119500011
J	Barke, J; Abels, HA; Sangiorgi, F; Greenwood, DR; Sweet, AR; Donders, T; Reichart, GJ; Lotter, AF; Brinkhuis, H				Barke, Judith; Abels, Hemmo A.; Sangiorgi, Francesca; Greenwood, David R.; Sweet, Arthur R.; Donders, Timme; Reichart, Gert-Jan; Lotter, Andre F.; Brinkhuis, Henk			Orbitally forced <i>Azolla</i> blooms and Middle Eocene Arctic hydrology: Clues from palynology	GEOLOGY			English	Article							RESPONSES	The high abundances and cyclic distribution of remains of the freshwater fern Azolla in early-Middle Eocene sediments from the Arctic Ocean have previously been related to episodic surface-water freshening, which was speculated to be orbitally modulated. Our integrated palynological and cyclostratigraphical analysis of the recovered Azolla interval in Integrated Ocean Drilling Program (IODP) core 302-M0004A-11X resulted in the recognition of two clear periodicities: a dominant similar to 1.2 m cyclicity, which we relate to changes in obliquity (similar to 40 k.y.), and a weaker similar to 0.7 m cyclicity, which we link to precession (similar to 21 k.y.). Cycles in the abundances of Azolla, cysts of freshwater-tolerant dinoflagellates, and swamp-vegetation pollen show covariability in the obliquity domain. This strong correlation suggests periods of enhanced rainfall and runoff during Azolla blooms, presumably linked to increased local summer temperatures during obliquity maxima. Larix and bisaccate conifer pollen covary at the precession frequency, with peak occurrences corresponding to precession minima, possibly as a result of enhanced continental runoff from a more remote source area and a stronger seasonal contrast. Following the sudden demise of Azolla ca. 48.1 Ma, runoff (cycles) continued to influence the central Arctic at decreased intensity. This and a concomitant decline in swamp-vegetation pollen suggest edaphically drier conditions on land and decreased runoff into the Arctic Ocean, causing salinity changes, which might have been fatal for Azolla. Moreover, a sea-level rise, inferred from overall decreasing total terrestrial palynomorph concentrations, possibly facilitated oceanic connections.	[Barke, Judith; Sangiorgi, Francesca; Lotter, Andre F.; Brinkhuis, Henk] Univ Utrecht, Fac Sci, Dept Biol, Inst Environm Biol, NL-3584 CD Utrecht, Netherlands; [Abels, Hemmo A.] Univ Utrecht, Fac Geosci, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands; [Greenwood, David R.] Brandon Univ, Dept Biol, Brandon, MB R7A 6A9, Canada; [Sweet, Arthur R.] Geol Survey Canada, Calgary, AB T2L 2E7, Canada; [Donders, Timme] Geol Survey Netherlands, TNO, NL-3508 TA Utrecht, Netherlands; [Reichart, Gert-Jan] Univ Utrecht, Dept Earth Sci, Fac Geosci, NL-3508 TA Utrecht, Netherlands; [Reichart, Gert-Jan] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany	Utrecht University; Utrecht University; Brandon University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Netherlands Organization Applied Science Research; Utrecht University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Barke, J (通讯作者)，Univ Utrecht, Fac Sci, Dept Biol, Inst Environm Biol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.		Donders, Timme/J-5044-2012; Brinkhuis, Henk/B-4223-2009; Lotter, Andre F./C-3477-2008; Reichart, Gert-Jan/N-6308-2018; Greenwood, David/C-2758-2008	Lotter, Andre F./0000-0002-2954-8809; Reichart, Gert-Jan/0000-0002-7256-2243; Greenwood, David/0000-0002-8569-9695; Abels, Hemmo/0000-0001-7648-3369; Donders, Timme/0000-0003-4698-3463; Brinkhuis, Henk/0000-0003-0253-6610; Sangiorgi, Francesca/0000-0003-4233-6154	Darwin Center for Biogeosciences [DW-2009-5006]; Statoil; Natural Sciences and Engineering Research Council of Canada	Darwin Center for Biogeosciences; Statoil; Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	We thank L. Bik, N. Welters, and J. van Tongeren for their great support, and C. Greenwood, J. H. A. van Konijnenburg-van Cittert, and H. Visscher for pollen analytical assistance. We also thank J. van der Burgh and M. E. Collinson for discussions on the ecology of Azolla, and F. J. Hilgen and L. J. Lourens for discussions on spectral analysis. Jerry Dickens and two anonymous reviewers are also acknowledged. This research used samples and data provided by the Integrated Ocean Drilling Program. This is publication DW-2009-5006 of the Darwin Center for Biogeosciences, which partially funded this project. We thank Statoil for their financial support. Greenwood's research is supported by the Natural Sciences and Engineering Research Council of Canada.	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J	Alvarez, G; Uribe, E; Díaz, R; Braun, M; Mariño, C; Blanco, J				Alvarez, Gonzalo; Uribe, Eduardo; Diaz, Rosario; Braun, Mauricio; Marino, Carmen; Blanco, Juan			Bloom of the Yessotoxin producing dinoflagellate <i>Protoceratium reticulatum</i> (Dinophyceae) in Northern Chile	JOURNAL OF SEA RESEARCH			English	Article						Protoceratium Reticulatum; Yessotoxin; Harmful Algal Blooms; Upwelling; Bahia Mejillones; Chile	HARMFUL ALGAL BLOOMS; LIQUID-CHROMATOGRAPHY; GONYAULAX-SPINIFERA; DIATOM BLOOM; SHELLFISH; BAY; PROFILE; IDENTIFICATION; PECTENOTOXINS; VARIABILITY	In summer 2007, a dinoflagellate preliminarily identified as Protoceratium reticulatum bloomed in Bahia Mejillones, northern Chile. Phytoplankton samples were analyzed in detail by light and scanning electron microscopy revealing the presence of resting cyst and motile cells of P. reticulatum. Oceanographic and phytoplankton data suggest that the bloom was initiated offshore by motile cells and germinated cysts during an upwelling pulse. These cells were advected into the bay when upwelling relaxed and grew without any relevant competitor. Phytoplankton net samples were found to contain yessotoxin as the only toxin in an estimated proportion of 0.2 and 0.4 pg cell(-1), thus confirming that P. reticulatum is a source of yessotoxin in northern Chilean waters and consequently that it poses a risk for human health and mollusk exploitation in the area. (C) 2011 Elsevier B.V. All rights reserved.	[Alvarez, Gonzalo; Marino, Carmen; Blanco, Juan] Ctr Invest Marinas Xunta de Galicia, Vilanova De Arousa 36620, Pontevedra, Spain; [Alvarez, Gonzalo; Uribe, Eduardo; Diaz, Rosario] Univ Catolica Norte, Fac Ciencias Mar, Dept Acuicultura, Coquimbo, Chile; [Braun, Mauricio] Inst Fomento Pesquero, Div Invest Pesquera, Valparaiso, Chile	Universidad Catolica del Norte; Instituto de Fomento Pesquero (Valparaiso)	Alvarez, G (通讯作者)，Ctr Invest Marinas Xunta de Galicia, Apto 13, Vilanova De Arousa 36620, Pontevedra, Spain.	galvarez@cimacoron.org	Uribe, Eduardo/D-1590-2012; Alvarez, Gonzalo/W-1262-2017; Blanco, Juan/A-8000-2008	Alvarez Vergara, Gonzalo/0000-0001-5812-1559; Blanco, Juan/0000-0003-2123-7747	FONDEF-CHILE [DOI 1056]; Conselleria do Mar, Xunta de Galicia, Spain [FIP 2007-20]; Universidad Catolica del Norte, Chile [FIP 2007-20]; Asociacion de Productores de Ostion y Ostras de Chile (APOOCH); MAEC-AECI	FONDEF-CHILE(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDEF); Conselleria do Mar, Xunta de Galicia, Spain(Xunta de Galicia); Universidad Catolica del Norte, Chile; Asociacion de Productores de Ostion y Ostras de Chile (APOOCH); MAEC-AECI	This research was funded by the projects DOI 1056 (FONDEF-CHILE) and FIP 2007-20 developed within the framework of a cooperation agreement between the Conselleria do Mar, Xunta de Galicia, Spain, and the Universidad Catolica del Norte, Chile. We would like to thank to Dr. Santiago Fraga by his valuable comments. We would also like to thank Ines Pasten and Paulo Avalos, for their technical assistance. We also acknowledge the Asociacion de Productores de Ostion y Ostras de Chile (APOOCH) for their support. We are grateful to Jesus Mendez and Ines Pazos by its technical assistance in SEM. Gonzalo Alvarez was funded by a MAEC-AECI grant.	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Sea Res.	MAY	2011	65	4					427	434		10.1016/j.seares.2011.03.008	http://dx.doi.org/10.1016/j.seares.2011.03.008			8	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	781DT					2025-03-11	WOS:000291911500005
J	Ribeiro, S; Berge, T; Lundholm, N; Andersen, TJ; Abrantes, F; Ellegaard, M				Ribeiro, Sofia; Berge, Terje; Lundholm, Nina; Andersen, Thorbjorn J.; Abrantes, Fatima; Ellegaard, Marianne			Phytoplankton growth after a century of dormancy illuminates past resilience to catastrophic darkness	NATURE COMMUNICATIONS			English	Article							MASS EXTINCTION; DINOFLAGELLATE CYSTS; SURVIVAL; VIABILITY; SEDIMENTS; IMPACT; SEA; DINOPHYCEAE; GERMINATION; RECOVERY	Photosynthesis evolved in the oceans more than 3 billion years ago and has persisted throughout all major extinction events in Earth's history. The most recent of such events is linked to an abrupt collapse of primary production due to darkness following the Chicxulub asteroid impact 65.5 million years ago. Coastal phytoplankton groups (particularly dinoflagellates and diatoms) appear to have been resilient to this biotic crisis, but the reason for their high survival rates is still unknown. Here we show that the growth performance of dinoflagellate cells germinated from resting stages is unaffected by up to a century of dormancy. Our results clearly indicate that phytoplankton resting stages can endure periods of darkness far exceeding those estimated for the Cretaceous-Paleogene extinction and may effectively aid the rapid resurgence of primary production in coastal areas after events of prolonged photosynthesis shut-down.	[Ribeiro, Sofia; Berge, Terje; Ellegaard, Marianne] Univ Copenhagen, Fac Sci, Dept Biol, Marine Biol Sect, DK-1353 Cph K, Denmark; [Ribeiro, Sofia; Abrantes, Fatima] LNEG, Unidade Geol Marinha, P-2720866 Amadora, Portugal; [Ribeiro, Sofia] Univ Lisbon, Ctr Oceanog, Fac Ciencias, P-1749016 Lisbon, Portugal; [Lundholm, Nina] Univ Copenhagen, Nat Hist Museum Denmark, DK-1307 Cph K, Denmark; [Andersen, Thorbjorn J.] Univ Copenhagen, Dept Geog & Geol, DK-1350 Cph K, Denmark	University of Copenhagen; Laboratorio Nacional de Energia e Geologia IP (LNEG); Universidade de Lisboa; University of Copenhagen; University of Copenhagen	Ribeiro, S (通讯作者)，Univ Copenhagen, Fac Sci, Dept Biol, Marine Biol Sect, Oster Farimagsgade 2D, DK-1353 Cph K, Denmark.	sribeiro@bio.ku.dk	Ribeiro, Sofia/AAZ-2782-2021; Lundholm, Nina/AAY-6249-2020; Abrantes, Fatima/N-7253-2019; Ellegaard, Marianne/H-6748-2014; Ribeiro, Sofia/G-9213-2018; Andersen, Thorbjorn Joest/N-7560-2014; Lundholm, Nina/A-4856-2013; Abrantes, Fatima/B-5985-2013	Ellegaard, Marianne/0000-0002-6032-3376; Ribeiro, Sofia/0000-0003-0672-9161; Andersen, Thorbjorn Joest/0000-0001-5032-9945; Lundholm, Nina/0000-0002-2035-1997; Berge, Terje/0009-0003-3916-8927; Abrantes, Fatima/0000-0002-9110-0212	Portuguese Foundation for Science and Technology [SFRH/BD/30847/2006]; University of Copenhagen; Danish Research Council; Fundação para a Ciência e a Tecnologia [SFRH/BD/30847/2006] Funding Source: FCT	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); University of Copenhagen; Danish Research Council(Det Frie Forskningsrad (DFF)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	This study was funded by the Danish Research Council through the project: 'Changes in Community Structure and Microevolution in Marine Protists'. S. R. and T. B. hold doctoral grants from the Portuguese Foundation for Science and Technology (SFRH/BD/30847/2006) and University of Copenhagen, respectively. We thank T. Gilbert, G. Simpson, T. Fenchel, P. Cermeno and P.J. Hansen for comments and suggestions, P. Frandsen for laboratory assistance, and A.-M. Nyby for the cyst SEM micrograph. The sediment core was kindly X-rayed at Hvidovre Hospital by J. Sogaard, D. Moller and A. Vestergaard.	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Commun.	MAY	2011	2								311	10.1038/ncomms1314	http://dx.doi.org/10.1038/ncomms1314			7	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	819CI	21587228	hybrid, Green Published			2025-03-11	WOS:000294802600016
J	Patterson, RT; Swindles, GT; Roe, HM; Kumar, A; Prokoph, A				Patterson, R. Timothy; Swindles, Graeme T.; Roe, Helen M.; Kumar, Arun; Prokoph, Andreas			Dinoflagellate cyst-based reconstructions of mid to late Holocene winter sea-surface temperature and productivity from an anoxic fjord in the NE Pacific Ocean	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	24th Pacific Climate Workshop (PACLIM)	APR 19-22, 2009	Pacific Grove, CA				RADIOCARBON AGE CALIBRATION; BELIZE INLET COMPLEX; ODP LEG 169S; BRITISH-COLUMBIA; VANCOUVER-ISLAND; EFFINGHAM INLET; NORTH-ATLANTIC; SAANICH INLET; DECADAL OSCILLATION; FISH PRODUCTION	Published contemporary dinoflagellate distributional data from the NE Pacific margin and estuarine environments (n = 136) were re-analyzed using Canonical Correspondence Analysis (CCA) and partial Canonical Correspondence Analysis (pCCA). These analyses illustrated the dominant controls of winter temperature and productivity on the distribution of dinoflagellate cysts in this region. Dinoflagellate cyst-based predictive models for winter temperature and productivity were developed from the contemporary distributional data using the modern analogue technique and applied to subfossil data from two mid to late Holocene (similar to 5500 calendar years before present present) cores; RJL99B03 and TUL99B11, collected from Effingham Inlet, a 15 km long anoxic fiord located on the southwest coast of Vancouver Island that directly opens to the Pacific Ocean through Barkley Sound. Sedimentation within these basins largely comprises annually deposited laminated couplets, each made up of a winter deposited terrigenous layer and spring to fall deposited diatomaceous layer. The Effingham Inlet dinoflagellate cyst record provides evidence of a mid-Holocene gradual decline in winter SST, ending with the initiation of neoglacial advances in the region by similar to 3500 cal BP. A reconstructed Late Holocene increase in winter SST was initiated by a weakening of the California Current, which would have resulted in a warmer central gyre and more El Nino-like conditions. (C) 2010 Elsevier Ltd and INQUA. All rights reserved.	[Patterson, R. Timothy; Prokoph, Andreas] Carleton Univ, Ottawa Carleton Geosci Ctr, Ottawa, ON K1S 5B6, Canada; [Patterson, R. Timothy; Prokoph, Andreas] Carleton Univ, Dept Earth Sci, Ottawa, ON K1S 5B6, Canada; [Swindles, Graeme T.] Univ Leeds, Sch Geog, Leeds LS2 9JT, W Yorkshire, England; [Roe, Helen M.] Queens Univ Belfast, Sch Geog Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland; [Kumar, Arun] King Fahd Univ Petr & Minerals, Ctr Petr, Dhahran 31261, Saudi Arabia; [Kumar, Arun] King Fahd Univ Petr & Minerals, Minerals Res Inst, Dhahran 31261, Saudi Arabia; [Prokoph, Andreas] SPEEDSTAT, Ottawa, ON K1G 5J5, Canada	Carleton University; University of Ottawa; Carleton University; University of Leeds; Queens University Belfast; King Fahd University of Petroleum & Minerals; King Fahd University of Petroleum & Minerals	Patterson, RT (通讯作者)，Carleton Univ, Ottawa Carleton Geosci Ctr, 1125 Colonel Dr, Ottawa, ON K1S 5B6, Canada.	tpatters@earthsci.carleton.ca	Swindles, Graeme/AAU-4321-2020	Swindles, Graeme/0000-0001-8039-1790				Anderson L, 2005, QUATERNARY RES, V64, P21, DOI 10.1016/j.yqres.2005.03.005; 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Int.	APR 15	2011	235						13	25		10.1016/j.quaint.2010.06.016	http://dx.doi.org/10.1016/j.quaint.2010.06.016			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	742HR					2025-03-11	WOS:000288932800003
J	Pawlowski, J; Christen, R; Lecroq, B; Bachar, D; Shahbazkia, HR; Amaral-Zettler, L; Guillou, L				Pawlowski, Jan; Christen, Richard; Lecroq, Beatrice; Bachar, Dipankar; Shahbazkia, Hamid Reza; Amaral-Zettler, Linda; Guillou, Laure			Eukaryotic Richness in the Abyss: Insights from Pyrotag Sequencing	PLOS ONE			English	Article							DEEP-SEA; MICROBIAL EUKARYOTES; COLD-SEEP; DIVERSITY; DNA; BIODIVERSITY; PHYLOGENY; BIOSPHERE; CLASSIFICATION; COMMUNITY	Background: The deep sea floor is considered one of the most diverse ecosystems on Earth. Recent environmental DNA surveys based on clone libraries of rRNA genes confirm this observation and reveal a high diversity of eukaryotes present in deep-sea sediment samples. However, environmental clone-library surveys yield only a modest number of sequences with which to evaluate the diversity of abyssal eukaryotes. Methodology/Principal Findings: Here, we examined the richness of eukaryotic DNA in deep Arctic and Southern Ocean samples using massively parallel sequencing of the 18S ribosomal RNA (rRNA) V9 hypervariable region. In very small volumes of sediments, ranging from 0.35 to 0.7 g, we recovered up to 7,499 unique sequences per sample. By clustering sequences having up to 3 differences, we observed from 942 to 1756 Operational Taxonomic Units (OTUs) per sample. Taxonomic analyses of these OTUs showed that DNA of all major groups of eukaryotes is represented at the deep-sea floor. The dinoflagellates, cercozoans, ciliates, and euglenozoans predominate, contributing to 17%, 16%, 10%, and 8% of all assigned OTUs, respectively. Interestingly, many sequences represent photosynthetic taxa or are similar to those reported from the environmental surveys of surface waters. Moreover, each sample contained from 31 to 71 different metazoan OTUs despite the small sample volume collected. This indicates that a significant faction of the eukaryotic DNA sequences likely do not belong to living organisms, but represent either free, extracellular DNA or remains and resting stages of planktonic species. Conclusions/Significance: In view of our study, the deep-sea floor appears as a global DNA repository, which preserves genetic information about organisms living in the sediment, as well as in the water column above it. This information can be used for future monitoring of past and present environmental changes.	[Pawlowski, Jan] Univ Geneva, Dept Genet & Evolut, Geneva, Switzerland; [Christen, Richard; Bachar, Dipankar] Univ Nice, Lab Biol Virtuelle, UMR 6543, Nice, France; [Lecroq, Beatrice] Japan Agcy Marine Earth Sci & Technol, Yokosuka, Kanagawa 2370061, Japan; [Shahbazkia, Hamid Reza] Univ Algarve, Dept Engn Elect & Informat, Faro, Portugal; [Amaral-Zettler, Linda] Josephine Bay Paul Ctr Comparat Mol Biol & Evolut, Marine Biol Lab, Woods Hole, MA USA; [Guillou, Laure] Stn Biol Roscoff, UMR 7144, Roscoff, France	University of Geneva; Universite Cote d'Azur; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); Universidade do Algarve; Marine Biological Laboratory - Woods Hole; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE)	Pawlowski, J (通讯作者)，Univ Geneva, Dept Genet & Evolut, Geneva, Switzerland.	Jan.Pawlowski@unige.ch	Pawlowski, Jan/AAO-3306-2021		French ANR Aquaparadox; ANR DeepOases; Swiss National Science Foundation [31003A-125372]; WM Keck foundation; Grants-in-Aid for Scientific Research [10F00202] Funding Source: KAKEN	French ANR Aquaparadox(Agence Nationale de la Recherche (ANR)); ANR DeepOases(Agence Nationale de la Recherche (ANR)); Swiss National Science Foundation(Swiss National Science Foundation (SNSF)); WM Keck foundation(W.M. Keck Foundation); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	This work was financially supported by the French ANR Aquaparadox (RC) and ANR DeepOases (LG), and the Swiss National Science Foundation grant 31003A-125372 (JP). Pyrosequencing was provided by the International Census of Marine Microbes (ICoMM) with financial support from a WM Keck foundation award to the Marine Biological Laboratory at Woods Hole. The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.	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J	Alaug, AS				Alaug, Abdulwahab S.			Source rocks evaluation, hydrocarbon generation and palynofacies study of late cretaceous succession at 16/G-1 offshore well in Qamar Basin, eastern Yemen	ARABIAN JOURNAL OF GEOSCIENCES			English	Article						Source rocks; Maturation; Hydrocarbon generation; Palynofacies; Mukalla; Dabut; Qamar Basin; Yemen	DEPOSITIONAL-ENVIRONMENTS	Subsurface Late Cretaceous succession has been recovered from 16/G-1, an offshore exploratory well that located in the Qamar Basin, eastern Republic of Yemen. This paper deals with the study of source rocks, maturation, hydrocarbon evaluation, and palynofacies of the Late Cretaceous Mukalla and Dabut Formations of the Mahra Group. These two formations consist of an intercalation of argillaceous, carbonates, siltstones, sandstones and coal layers. The sedimentary organic matter as amorphous organic matter, phytoclasts and palynomorphs are investigated and identified under transmitted light microscope. Spores, pollen, dinoflagellates, algae, fungi, and acritarchs in addition to foraminiferal lining test have been also identified. The optical and organic geochemical studies were used to evaluate the source rock, maturation and its hydrocarbons potentiality. The thermal alteration index, vitrinite reflectance, rock-eval pyrolysis, and palynofacies were also used. The upward increase in the relative abundance of marine versus terrestrial input reflects a major marine transgression and retregration cycles from Campanian to Maastrichtian stages. The Mukalla and Dabut Formations are late immature to mature stages with kerogen types II and III. The hydrocarbons generation potentiality of two formations is oil and wet gas prone indicators.	Taiz Univ, Fac Sci Appl, Dept Geol, Taizi 6803, Yemen	Taiz University	Alaug, AS (通讯作者)，Taiz Univ, Fac Sci Appl, Dept Geol, Taizi 6803, Yemen.	wahabalaug@yahoo.com						Al-Ameri TK, 1999, CRETACEOUS RES, V20, P359, DOI 10.1006/cres.1999.0157; Al-Ameri TK, 1997, CRETACEOUS RES, V18, P789, DOI 10.1006/cres.1997.0087; Al-Ameri TK, 2001, CRETACEOUS RES, V22, P735, DOI 10.1006/cres.2001.0288; [Anonymous], 1984, Pollen/spore color 'standard'; BARNARD PC, 1976, 4 INT PAL C; Batten D., 1996, Palynology: principles and applications, P1011; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Beydoun Z.R., 1998, INT UNION GEOLOGICAL, VIII, P245; Beydoun Z.R., 1966, US GEOLOGICAL SURV H, V560-H, P1; Beydoun Z.R., 1968, Lexique Stratigraphique International III, P1; Beydoun ZR, 1964, MIN RESOUR B S, V5, P1; Birse ACR, 1997, MAR PETROL GEOL, V14, P675, DOI 10.1016/S0264-8172(96)00043-8; Bordenave M. L., 1993, APPL PETROLEUM GEOCH, P425; Bosellini A, 2001, J AFR EARTH SCI, V32, P403, DOI 10.1016/S0899-5362(01)90105-8; Bosence DWJ, 1997, MAR PETROL GEOL, V14, P611, DOI 10.1016/S0264-8172(97)00039-1; BOTT WF, 1992, J PETROL GEOL, V15, P211, DOI 10.1111/j.1747-5457.1992.tb00963.x; Brannan J, 1997, MAR PETROL GEOL, V14, P701, DOI 10.1016/S0264-8172(96)00048-7; Brooks J., 1981, ORGANIC MATURATION S, P360; COLLIN A, 2010, MEDEDLINGEN RIJKS GE, V45, P39; ESPITALIE J, 1977, REV I FR PETROL, V32, P23, DOI 10.2516/ogst:1977002; Espitalie J., 1984, Analytical pyrolysis - Techniques and applications, P276; Espitalie J., 1985, Thermal modelling in sedimentary basins, P475; Hunt JM., 1996, PETROLEUM GEOCHEMIST; KILLOPS SD, 1993, INTRO ORGANIC GEOCHE, P265; KILLOPS SD, 1995, INTRO ORGANIC GEOCHE, P393; LANGFORD FF, 1990, AAPG BULL, V74, P799; Peters K.E., 1994, PETROLEUM SYSTEM SOU, P93, DOI DOI 10.1306/M60585C5; Peters K.E., 2005, The biomarker guide: biomarkers and isotopes in the environment and human history, V1; PETERS KE, 1986, AAPG BULL, V70, P318; Sharland P.R., 2001, GEO ARABIA SPECIAL P, V2; Smith P. M. R., 1983, Geological Society Special Publications, V12, P289, DOI [10.1144/GSL.SP.1983.012.01.29, DOI 10.1144/GSL.SP.1983.012.01.29]; Staplin FL., 1969, B CANADIAN PETROL GE, V17, P47; THOMPSON CL, 1986, INT J COAL GEOL, V6, P229, DOI 10.1016/0166-5162(86)90003-0; Tissot B. P., 1984, 2nd ed. Berlin: Springer; TISSOT BP, 1987, AAPG BULL, V71, P1445; Tyson RV., 1995, SEDIMENTARY ORGANIC, P615, DOI [DOI 10.1007/978-94-011-0739-6, 10.1007/978-94-011-0739-6]; Wetzel R, 1948, IRAQI PETROLEU UNPUB	37	23	23	0	8	SPRINGER HEIDELBERG	HEIDELBERG	TIERGARTENSTRASSE 17, D-69121 HEIDELBERG, GERMANY	1866-7511	1866-7538		ARAB J GEOSCI	Arab. J. Geosci.	APR	2011	4	3-4					551	566		10.1007/s12517-010-0182-6	http://dx.doi.org/10.1007/s12517-010-0182-6			16	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	743EO					2025-03-11	WOS:000289000500019
J	Abubakar, MB; Luterbacher, HP; Ashraf, AR; Ziedner, R; Maigari, AS				Abubakar, M. B.; Luterbacher, H. P.; Ashraf, A. R.; Ziedner, R.; Maigari, A. S.			Late Cretaceous palynostratigraphy in the Gongola Basin (Upper Benue Trough, Nigeria)	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Biostratigraphy; Cretaceous sequences; Gongola Basin; Spores; Pollen; Dinoflagellates	ELATER-BEARING POLLEN	Palynostratigraphic study that utilizes mainly spores and pollen was done on the Cretaceous sequences of the well Nasara-1 of the Gongola Basin of the Upper Benue Trough, Nigeria. The recovered spores and pollen in the well made the identification of five palynological zones possible: Droseridites senonicus (Coniacian-Santonian), Cretacaeiporites scabratus (Turonian), Triorites africaensis (Upper Cenomanian), Afropollis jardinus (Lower-Middle Cenomanian) and Elateroplicites africaensis-Elaterosporites klaszii-Elaterosporites protensus (Upper Albian). These zones are similar and correlatable to other Cretaceous palynologic zones in the West Africa and northern South American basins. (C) 2011 Elsevier Ltd. All rights reserved.	[Abubakar, M. B.; Maigari, A. S.] Abubakar Tafawa Balewa Univ, Geol Programme, Bauchi, Nigeria; [Luterbacher, H. P.; Ashraf, A. R.; Ziedner, R.] Univ Tubingen, Inst Geowissensch, D-72076 Tubingen, Germany	Eberhard Karls University of Tubingen	Abubakar, MB (通讯作者)，Abubakar Tafawa Balewa Univ, Geol Programme, PMB 0248, Bauchi, Nigeria.	ambello2002@yahoo.com			German Academic Exchange Service (DAAD)	German Academic Exchange Service (DAAD)(Deutscher Akademischer Austausch Dienst (DAAD))	The German Academic Exchange Service (DAAD) is thankfully acknowledged for providing financial support to the first author that made this work possible. We thank the Institut fur Geowissenschaften, Universitat Tubingen, Germany for providing the research facilities. Chevron Petroleum Nigeria Limited is also thankfully acknowledged for inviting us to participate in the well-site sample collection and for allowing us to work independently on the samples. The review comments of Dr. Ali Ahmed Eisawi, Al Neelain University, Sudan, Dr. Holger Gebhardt and another anonymous reviewer have greatly improved the manuscript and we say thank you.	Abubakar MB, 2008, J PETROL GEOL, V31, P387, DOI 10.1111/j.1747-5457.2008.00428.x; Abubakar MB, 2006, J AFR EARTH SCI, V45, P347, DOI 10.1016/j.jafrearsci.2006.03.008; [Anonymous], 2007, Paleopalynology; BENKHELIL J, 1989, J AFR EARTH SCI, V8, P251, DOI 10.1016/S0899-5362(89)80028-4; BENKHELIL J, 1982, GEOL MAG, V112, P155; BRENNER G J, 1968, Pollen et Spores, V10, P341; BURDEN ET, 1989, AASP CONTR SERIES, V21; Dike EFC., 1993, JOUR MIN GEOL, V29, P77; DIKE EFC, 2002, NIG MIN GEOSCI SOC; Dino R, 1999, REV PALAEOBOT PALYNO, V105, P201, DOI 10.1016/S0034-6667(98)00076-1; du Chene R.E.J., 1979, Revue de Micropaleontologie, V21, P123; GUIRAUD M, 1990, J AFR EARTH SCI, V10, P341, DOI 10.1016/0899-5362(90)90065-M; GUIRAUD R, 1992, TECTONOPHYSICS, V213, P153, DOI 10.1016/0040-1951(92)90256-6; HERNGREEN G F W, 1981, Pollen et Spores, V23, P441; Herngreen G.F.W., 1973, POLLEN SPORE, V15, P514; Herngreen G.F. W., 1975, Medelingen Rijks Geologische Dienst, Nieuwe Serie, V26, P39; HERNGREEN GFW, 1990, REV PALAEOBOT PALYNO, V66, P345, DOI 10.1016/0034-6667(90)90046-L; Kaska H.V., 1989, PALYNOLOGY, V13, P79, DOI [10.1080/01916122.1989.9989356, DOI 10.1080/01916122.1989.9989356]; Lawal O., 1986, Review de Micro. Pal, V29, P61; LAWAL O, 1982, THESIS U NICE; Obaje Nuhu George, 1994, Tuebinger Mikropalaeontologische Mitteilungen, V11, P1; PETTERS S W, 1982, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V179, P1; Schrank E., 1995, BERLINER GEOWISSENSC, V177, P1; Thusu B., 1985, Journal of Micropalaeontology, V4, P131; Zaborski P, 1997, B CENT RECH EXPL, V21, P153; Zaborski P.M., 2003, Africa Geoscience Review, V10, P13; Zaborski P.M., 2000, J. Min. Geol., V36, P153	27	14	17	2	4	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	1464-343X			J AFR EARTH SCI	J. Afr. Earth Sci.	APR	2011	60	1-2					19	27		10.1016/j.jafrearsci.2011.01.007	http://dx.doi.org/10.1016/j.jafrearsci.2011.01.007			9	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	744VT					2025-03-11	WOS:000289124000003
J	Ki, JS; Park, MH; Han, MS				Ki, Jang-Seu; Park, Myung-Hwan; Han, Myung-Soo			DISCRIMINATIVE POWER OF NUCLEAR rDNA SEQUENCES FOR THE DNA TAXONOMY OF THE DINOFLAGELLATE GENUS <i>PERIDINIUM</i> (DINOPHYCEAE)	JOURNAL OF PHYCOLOGY			English	Article						dinoflagellate; DNA taxonomy; molecular divergence; Peridinium; phylogeny; rDNA	WATER RED TIDE; SUBUNIT RIBOSOMAL-RNA; COCHLODINIUM-POLYKRIKOIDES; DIATOM ENDOSYMBIONTS; PHYLOGENY; RESERVOIR; CINCTUM; GROWTH; BLOOM	The genus Peridinium Ehrenb. comprises a group of highly diversified dinoflagellates. Their morphological taxonomy has been established over the last century. Here, we examined relationships within the genus Peridinium, including Peridinium bipes F. Stein sensu lato, based on a molecular phylogeny derived from nuclear rDNA sequences. Extensive rDNA analyses of nine selected Peridinium species showed that intraspecies genetic variation was considerably low, but interspecies genetic divergence was high (> 1.5% dissimilarity in the nearly complete 18S sequence; > 4.4% in the 28S rDNA D1/D2). The 18S and 28S rDNA Bayesian tree topologies showed that Peridinium species grouped according to their taxonomic positions and certain morphological characters (e.g., epithecal plate formula). Of these groups, the quinquecorne group (plate formula of 3', 2a, 7 ') diverged first, followed by the umbonatum group (4', 2a, 7 ') and polonicum group (4', 1a, 7 '). Peridinium species with a plate formula of 4', 3a, 7 ' diverged last. Thus, 18S and 28S rDNA D1/D2 sequences are informative about relationships among Peridinium species. Statistical analyses revealed that the 28S rDNA D1/D2 region had a significantly higher genetic divergence than the 18S rDNA region, suggesting that the former as DNA markers may be more suitable for sequence-based delimitation of Peridinium. The rDNA sequences had sufficient discriminative power to separate P. bipes f. occultaum (Er. Lindem.) M. Lefevre and P. bipes f. globosum Er. Lindem. into two distinct species, even though these taxa are morphologically only marginally discriminated by spines on antapical plates and the shape of red bodies during the generation of cysts. Our results suggest that 28S rDNA can be used for all Peridinium species to make species-level taxonomic distinctions, allowing improved taxonomic classification of Peridinium.	[Ki, Jang-Seu] Sangmyung Univ, Coll Convergence, Dept Green Life Sci, Seoul 110743, South Korea; [Park, Myung-Hwan] Hanyang Univ, Grad Sch, Dept Environm Sci, Seoul 133791, South Korea; [Han, Myung-Soo] Hanyang Univ, Dept Life Sci, Coll Nat Sci, Seoul 133791, South Korea	Sangmyung University; Hanyang University; Hanyang University	Ki, JS (通讯作者)，Sangmyung Univ, Coll Convergence, Dept Green Life Sci, Seoul 110743, South Korea.	kijs@smu.ac.kr; hanms@hanyanga.c.kr			Ministry of Land, Transportation and Maritime Affairs, Republic of Korea	Ministry of Land, Transportation and Maritime Affairs, Republic of Korea(Ministry of Land, Transport and Maritime Affairs (MLTM), Republic of Korea)	This work was supported by both the Marine and Extreme Genome Research Center Program and a grant program (Development of Marine-bioenergy) funded by the Ministry of Land, Transportation and Maritime Affairs, Republic of Korea.	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Phycol.	APR	2011	47	2					426	435		10.1111/j.1529-8817.2010.00950.x	http://dx.doi.org/10.1111/j.1529-8817.2010.00950.x			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	745JW	27021873				2025-03-11	WOS:000289162700020
J	Van Nieuwenhove, N; Bauch, HA; Eynaud, F; Kandiano, E; Cortijo, E; Turon, JL				Van Nieuwenhove, Nicolas; Bauch, Henning A.; Eynaud, Frederique; Kandiano, Evguenia; Cortijo, Elsa; Turon, Jean-Louis			Evidence for delayed poleward expansion of North Atlantic surface waters during the last interglacial (MIS 5e)	QUATERNARY SCIENCE REVIEWS			English	Article						Last Interglacial; MIS 5e; Dinoflagellate cysts; North Atlantic; Nordic seas	DINOFLAGELLATE CYST ASSEMBLAGES; SEA-SURFACE; NORWEGIAN SEA; NORDIC SEAS; LATE-QUATERNARY; ICE-SHEET; OCEAN CIRCULATION; RAPID CHANGES; MARINE; CLIMATE	The Last Interglacial (Marine Isotopic Stage or MIS 5e) surface ocean heat flux from the Rockall Basin (NE Atlantic) towards the Arctic Ocean was reconstructed by analysing dinoflagellate cyst (dinocyst) assemblages in four sediment cores. Together with records of stable isotopes and ice-rafted detritus, the assemblage data reflect the northward retreat of ice(berg)-laden waters and the gradual development towards interglacial conditions at the transition from the Saalian deglaciation (Termination II) into MIS 5e. At the Rockall Basin, this onset of the Last Interglacial is soon followed by the appearance of the thermophilic dinocyst species Spiniferites mirabilis, with relative abundances higher than those observed at present in the area. North of the Iceland-Scotland Ridge, however, S. mirabilis only appears in significant numbers during late MIS 5e, between similar to 118 and 116.5 ka. Hence, fully marine Last Interglacial conditions with most intense Atlantic surface water influence occurred during late MIS 5e in the Nordic seas, and consequently also farther north in the Arctic Ocean, and at times when northern hemisphere summer insolation was already significantly decreased. The stratigraphic position of this Late Interglacial optimum is supported by planktic foraminifers and contrasts with the timing of the early Holocene climatic optimum in this area. We interpret the delayed northward expansion of Atlantic waters towards the polar latitudes as a result of the Saalian ice sheet deglaciation and its specific impact on the subsequent water mass evolution in this region. (C) 2011 Elsevier Ltd. All rights reserved.	[Van Nieuwenhove, Nicolas; Bauch, Henning A.; Kandiano, Evguenia] Leibniz Inst Marine Sci IFM GEOMAR, D-24148 Kiel, Germany; [Bauch, Henning A.] Mainz Acad Sci Humanities & Literature, D-55131 Mainz, Germany; [Eynaud, Frederique; Turon, Jean-Louis] Univ Bordeaux 1, Lab Environm & Paleoenvironm Ocean EPOC, UMR CNRS, F-33405 Talence, France; [Cortijo, Elsa] Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France	Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); Universite Paris Saclay	Van Nieuwenhove, N (通讯作者)，Leibniz Inst Marine Sci IFM GEOMAR, Wischhofstr 1-3, D-24148 Kiel, Germany.	nvannieuwenhove@ifm-geomar.de	Van Nieuwenhove, Nicolas/IAQ-1532-2023	Eynaud, Frederique/0000-0003-1283-7425; Kandiano, Evgenia/0000-0003-1783-9999; Van Nieuwenhove, Nicolas/0000-0001-6369-2751	Deutsche Forschungsgemeinschaft [BA1367/6, NI1248/1]	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	We acknowledge the IMAGES programme, Mr. Y. Balut, the captain, and crew of the RV Marion Dufresne (IPEV) and the RV Meteor for their assistance at sea. We are grateful to Jens Matthiessen for his assistance with the palynomorph taxonomy, T. Rasmussen for providing the IRD data and S. Wastegard for the ash layer data from core MD95-2009. We thank N. Andersen and the team from the Leibniz Laboratory for Radiometric Dating and Stable Isotope Research (Kiel University) for their support in the isotope analyses, as well as O. Ther and M.-H. Castera (EPOC laboratory) for preparing palynological samples from cores MD95-2004 and MD95-2009. The manuscript benefited from the appreciated comments and suggestions made by 3 anonymous reviewers. NVN was financed by the Deutsche Forschungsgemeinschaft" (projects BA1367/6, NI1248/1).	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Sci. Rev.	APR	2011	30	7-8					934	946		10.1016/j.quascirev.2011.01.013	http://dx.doi.org/10.1016/j.quascirev.2011.01.013			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	744XQ					2025-03-11	WOS:000289128900014
J	Gnibidenko, ZN; Volkova, VS; Kuz'mina, OB; Dolya, ZA; Khazina, IV; Levicheva, AV				Gnibidenko, Z. N.; Volkova, V. S.; Kuz'mina, O. B.; Dolya, Zh. A.; Khazina, I. V.; Levicheva, A. V.			Stratigraphic, paleomagnetic, and palynological data on the Paleogene-Neogene continental sediments of southwestern West Siberia	RUSSIAN GEOLOGY AND GEOPHYSICS			English	Article						Oligocene; Neogene; paleomagnetic and pollen zones; Om' basin; West Siberia		The paper presents magnetostratigraphic data on Paleogene-Neogene continental sediments stripped by borehole 8 at the southern periphery of the Om' basin, in the Ishim-Irtysh interfluve, on the border with northern Kazakhstan. Pollen assemblages and zones have been distinguished, and a paleomagnetic section of borehole 8 has been compiled. The section consists of 11 magnetozones, which are associated with pollen zones and paleocarpological data. The absence of some paleomagnetic and pollen zones from the section suggests that the geological record is incomplete, because the formations in the studied sediments are partly eroded. A dinoflagellate community was first recorded in Upper Oligocene-Lower Miocene sediments at the periphery of the Om' basin. The composition and ecologic characteristics of this community cannot give an unambiguous answer to the question whether seawater could penetrate southwestern Siberia through the Turgai Sea. The composition of pollen and spores from the Lower Oligocene sediments (Novomikhailovka Formation) and from the Chilikty Formation (northern Kazakhstan) is similar and reflects the development of Turgai flora in a huge territory. Later, in the second half of the Miocene, broad-leaved/coniferous forests were replaced by small-leaved ones. In the late Miocene, the latter were replaced by forest steppes with some arid flora. (C) 2011, V.S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B.V. All rights reserved.	[Gnibidenko, Z. N.; Volkova, V. S.; Kuz'mina, O. B.; Khazina, I. V.; Levicheva, A. V.] Russian Acad Sci, AA Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia; [Dolya, Zh. A.] Omsk Prospecting Expedit, Omsk 644103, Russia	Russian Academy of Sciences; Siberian Branch of the Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics	Gnibidenko, ZN (通讯作者)，Russian Acad Sci, AA Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akad Koptyuga 3, Novosibirsk 630090, Russia.	gnibidenkozn@ipgg.nsc.ru	Kuzmina, Olga/I-9547-2018		Russian Foundation for Basic Research [08-05-00344, 07-05-00582, 02-05-64787]; Russian Academy of Sciences [15]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Russian Academy of Sciences(Russian Academy of Sciences)	The study was supported by the Russian Foundation for Basic Research (grant nos. 08-05-00344, 07-05-00582, 02-05-64787) and the Russian Academy of Sciences (program no. 15 Biospheric Evolution).	[Anonymous], 1995, Publ. Society for Sedimentary Geology. III. Cenozoic Era; Babushkin A.E., 2001, UNIFIED REGIONAL STR; Batten DJ, 1999, PALAEOGEOGR PALAEOCL, V153, P161, DOI 10.1016/S0031-0182(99)00103-0; BOITSOVA EP, 1961, GEOLOGY TURGAI TROUG, P45; DARGEVICH VA, 1969, GEOLOGY PLACERS SO W, P32; Gnibidenko ZN, 2007, RUSS GEOL GEOPHYS+, V48, P337, DOI 10.1016/j.rgg.2006.03.002; GNIBIDENKO ZN, 2006, IZD SO RAN FILIAL GE; Grichuk V. P., 1948, POLLEN SPORES ANAL I; HE C, 1980, INT PALYNOLOGICAL C, P5; KASHIRTSEV VA, 2008, NEFTEKHIMIYA, V4, P271; Kulkova IA, 1997, GEOL GEOFIZ, V38, P581; Kuz'mina OB, 2004, DOKL EARTH SCI, V394, P14; KUZMINA OB, 2008, STRATIGRAFIYA GEOLOG, V16, P87; KUZMINA OB, 2009, RUSSIAN GEOLOGY GEOP, V12, P159; KUZMINA OB, 2001, GEOL GEOFIZ, V4, P135; Nikitin V.P., 2006, PALEOCARPOLOGY STRAT; Panova L.A., 1990, PRACTICAL PALYNOSTRA; Volkova VS, 2002, GEOL GEOFIZ, V43, P1017; VOLKOVA VS, 2008, RUSSIAN GEOLOGY GEOP, V49, P325; VOLKOVA VS, 2002, P X ALL RUSS PALYNOL, P45; 1986, GUIDELINES PREPARATI	21	11	12	2	7	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1068-7971			RUSS GEOL GEOPHYS+	Russ. Geol. Geophys.	APR	2011	52	4					466	473		10.1016/j.rgg.2011.03.009	http://dx.doi.org/10.1016/j.rgg.2011.03.009			8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	738OB					2025-03-11	WOS:000288648100009
J	Montagnes, DJS; Lowe, CD; Martin, L; Watts, PC; Downes-Tettmar, N; Yang, Z; Roberts, EC; Davidson, K				Montagnes, David J. S.; Lowe, Chris D.; Martin, Laura; Watts, Phillip C.; Downes-Tettmar, Naomi; Yang, Zhou; Roberts, Emily C.; Davidson, Keith			<i>Oxyrrhis marina</i> growth, sex and reproduction	JOURNAL OF PLANKTON RESEARCH			English	Article						model organism; dinoflagellate; protozoa; life history; Oxyrrhis	PREDATOR-PREY INTERACTIONS; ISOCHRYSIS-GALBANA; CELL-CYCLE; PRIMITIVE DINOFLAGELLATE; MICROZOOPLANKTON; NITROGEN; CARBON; DIGESTION; RESPONSES; PROTISTS	We examine the literature on Oxyrrhis marina cell and life cycles, population growth and production. We then provide an overview of what is known regarding aspects of O. marina growth, indicate where information is needed and suggest ways in which this species can and cannot be used as a general model, in this respect. Little is known about the O. marina life cycle; it is even unknown if cells are haploid, diploid or polyploid, although there is one report that sex occurs by homothallic isogamy. There is considerable information on the cell cycle, which we briefly review and provide a guide to the literature for details. We briefly discuss and provide guidance to information on: (i) population cell size distributions; (ii) cannibalism; (iii) our first report of "mini-cells" in cultures (similar to 8 mu m) and their possible role in the life cycle; (iv) cysts, and their possible role in the life and cell cycles; (v) biotic influences on growth, such as food type and abundance, assimilation efficiency, prey stiochiometry, strain differences, population growth and starvation and nutritional shifts; (vi) abiotic factors that affect growth, such as temperature, salinity, pH, light and turbulence. We then reflect on the consequences of interactions between the above factors and review data on population growth of O. marina in the field and laboratory. Finally, we evaluate the use of O. marina as a model organism to examine cell and life cycles and ecological processes. Throughout the paper, we suggest areas that need evaluation.	[Montagnes, David J. S.; Lowe, Chris D.; Martin, Laura; Watts, Phillip C.; Downes-Tettmar, Naomi] Univ Liverpool, Sch Biol Sci, Biosci Bldg, Liverpool L69 7ZB, Merseyside, England; [Yang, Zhou] Nanjing Normal Univ, Sch Biol Sci, Jiangsu Prov Key Lab Biodivers & Biotechnol, Nanjing 210046, Peoples R China; [Roberts, Emily C.] Swansea Univ, Swansea SA2 8PP, W Glam, Wales; [Davidson, Keith] Scottish Assoc Marine Sci, Oban PA37 1QA, Argyll, Scotland	University of Liverpool; Nanjing Normal University; Swansea University; University of the Highlands & Islands	Montagnes, DJS (通讯作者)，Univ Liverpool, Sch Biol Sci, Biosci Bldg, Liverpool L69 7ZB, Merseyside, England.	dmontag@liv.ac.uk	Lowe, Chris/D-1852-2010; Davidson, Keith/A-5474-2013; Watts, Phill/G-7257-2011; Yang, Zhou/H-3407-2011	Davidson, Keith/0000-0001-9269-3227; Watts, Phillip/0000-0001-7755-187X	UK NERC [NE/F005237/1]; National Natural Science Foundation of China [30970500]; SAMS/NERC Oceans [2025]; NERC [NE/C519438/1, NE/G010374/1]; NERC [NE/F005237/1, dml010003] Funding Source: UKRI	UK NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC)); SAMS/NERC Oceans; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was, in part, supported by: a UK NERC grant (NE/F005237/1) awarded to P. C. W., C. D. L. and D.J.S.M.; a Project of International Cooperation and Exchanges from the National Natural Science Foundation of China (30970500) awarded to Y.Z.; SAMS/NERC Oceans 2025 programme awarded to K. D. and NERC grants NE/C519438/1 and NE/G010374/1 awarded to E.C.R.	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Plankton Res.	APR	2011	33	4					615	627		10.1093/plankt/fbq111	http://dx.doi.org/10.1093/plankt/fbq111			13	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	733MW		Green Submitted, Bronze			2025-03-11	WOS:000288267800007
J	Bahi, MM; Tsaloglou, MN; Mowlem, M; Morgan, H				Bahi, M. M.; Tsaloglou, M. -N.; Mowlem, M.; Morgan, H.			Electroporation and lysis of marine microalga <i>Karenia brevis</i> for RNA extraction and amplification	JOURNAL OF THE ROYAL SOCIETY INTERFACE			English	Article						electroporation; dielectrophoresis; Karenia brevis; RNA extraction; RNA amplification; dinoflagellate cysts	CELL-LYSIS; SAMPLE PREPARATION; DIELECTROPHORESIS; DEVICE; CHIP; FLOW; DNA; QUANTIFICATION; PURIFICATION; MANIPULATION	We describe here a simple device for dielectrophoretic concentration of marine microalga Karenia brevis nonmotile cells, followed by electric field-mediated lysis for RNA extraction. The lysate was purified using magnetic beads and pure RNA extracted. RNA quality was assessed off-chip by nucleic acid sequence-based amplification and the optimum conditions for lysis were determined. This procedure will form part of an integrated microfluidic system that is being developed with sub-systems for performing cell concentration and lysis, RNA extraction/purification and real-time quantitative RNA detection. The integrated system and its components could be used for a large range of applications including in situ harmful algal bloom detection, transcriptomics and point-of-care diagnostics.	[Bahi, M. M.; Tsaloglou, M. -N.; Mowlem, M.] Natl Oceanog Ctr, Sensors Dev Grp, Southampton SO14 3ZH, Hants, England; [Tsaloglou, M. -N.; Morgan, H.] Univ Southampton, Sch Elect & Comp Sci, Southampton SO17 1BJ, Hants, England	NERC National Oceanography Centre; University of Southampton	Tsaloglou, MN (通讯作者)，Natl Oceanog Ctr, Sensors Dev Grp, Southampton SO14 3ZH, Hants, England.	m.tsaloglou@soton.ac.uk	; Tsaloglou, Maria-Nefeli/G-4306-2016	Morgan, Hywel/0000-0003-4850-5676; Tsaloglou, Maria-Nefeli/0000-0001-6380-2404; Mowlem, Matthew/0000-0001-7613-6121	EU [224306]; NOCS/NERC; NERC [noc010003, noc010013] Funding Source: UKRI	EU(European Union (EU)); NOCS/NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	M.N.T. developed the experimental protocols and cultured the microalgae. M.M.B. performed all on-chip lyses and nanodrop spectrophotometric quantification. M.N.T. extracted and purified the RNA and carried out all NASBA assays. M.M.B. acquired microscopy images. M.N.T. and M.M.B. analysed the data. M.C.M., M.N.T. and H.M. supervised the work and wrote the paper. M.C.M. and H.M. secured funding. The authors would like to acknowledge funding support by EU FP7 LABONFOIL grant project 224306 and a NOCS/NERC studentship for M.M.B. Also thanks to Nicolas Green for the electroporation chip, to Layla Hazeem of the Purdie laboratory for the initial culture of K. brevis and to Bethan Jones for help with the identification of temporary cysts.	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R. Soc. Interface	APR	2011	8	57					601	608		10.1098/rsif.2010.0445	http://dx.doi.org/10.1098/rsif.2010.0445			8	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	725NV	21084344	Green Published			2025-03-11	WOS:000287653100015
J	Kohn, M; Steinke, S; Baumann, KH; Donner, B; Meggers, H; Zonneveld, KAF				Kohn, Marion; Steinke, Stephan; Baumann, Karl-Heinz; Donner, Barbara; Meggers, Helge; Zonneveld, Karin A. F.			Stable oxygen isotopes from the calcareous-walled dinoflagellate <i>Thoracosphaera heimii</i> as a proxy for changes in mixed layer temperatures off NW Africa during the last 45,000 yr	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Calcareous-walled dinoflagellate cyst; Stable oxygen isotopes; Upwelling; Palaeotemperature; Deep-chlorophyll maximum; NW Africa	RADIOCARBON AGE CALIBRATION; PLANKTONIC-FORAMINIFERA; NORTHWEST AFRICA; EQUATORIAL ATLANTIC; SURFACE SEDIMENTS; CAPE BLANC; TROPICAL ATLANTIC; UPWELLING AREAS; PARTICLE-FLUX; POTENTIAL USE	The present study is the first study on the stable oxygen isotope composition of the photosynthetic calcareous-walled dinoflagellate species Thoracosphaera heimii off NW Africa during the last 45,000 yr. T. heimii based temperature estimates of sediment core GeoB 8507-3 were compared with those obtained from the stable oxygen isotopes of the planktic foraminifera Globigerina bulloides and Globigerinoides ruber (pink), and the Mg/Ca ratio of G. ruber (pink). We show that the isotopic composition of T. heimii and the temperature estimates based on the equation for inorganically precipitated calcite provide comparable results to those obtained from G. ruber (pink) isotopes and Mg/Ca ratios with exception of the Early. Holocene and the Younger Dryas. The recently proposed palaeotemperature equation of Zonneveld et al. (2007), however, provides unrealistic temperature reconstructions that are about 16 degrees C lower than those based on planktic foraminifera. Thus, this equation needs to be revised. The difference between T. heimii and G. bulloides isotopic and temperature reconstructions can be ascribed to differences in the ecology of both species, especially with regard to their depth habitat and/or seasonal production in the research area. All temperature proxies suggest comparable conditions during the last glacial and Holocene. Small differences between the reconstructed temperature values of T. heimii and the other proxies can be explained by differences in seasonal production of the individual species. The relatively low temperatures recorded by T. heimii at about 15,000 to 8,000 yr BP are interpreted to reflect an increase in duration and/or intensity of the upwelling in the vicinity of the core site in comparison to the last glacial, with an abrupt and strong decrease of upwelling intensity and/or duration during the Early Holocene and the Younger Dryas. (C) 2011 Elsevier B.V. All rights reserved.	[Kohn, Marion] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	University of Bremen; University of Bremen	Kohn, M (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, POB 330440, D-28334 Bremen, Germany.	mkohn@uni-bremen.de			DFG-Research Center/Excellence Cluster "The Ocean in the Earth System"	DFG-Research Center/Excellence Cluster "The Ocean in the Earth System"(German Research Foundation (DFG))	Thanks are given to Monika Segl (MARUM, University of Bremen) for carrying out the stable isotope measurements. Jan Meyer, Sven Forke and Carola Ott are acknowledged for their support in the laboratory. Inka Meyer and Aglaia Nagel are thanked for foraminifera picking. Thanks to Till Hanebuth for providing the lithological column. Sebastian Meier, Pout Schioler and Annemiek Vink provided constructive remarks on a previous version of this manuscript as well as Finn Surlyk for the editorial handling. 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Paleoclimatol. Paleoecol.	MAR 15	2011	302	3-4					311	322		10.1016/j.palaeo.2011.01.019	http://dx.doi.org/10.1016/j.palaeo.2011.01.019			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	751ZU					2025-03-11	WOS:000289657700014
J	Verleye, TJ; Pospelova, V; Mertens, KN; Louwye, S				Verleye, Thomas J.; Pospelova, Vera; Mertens, Kenneth N.; Louwye, Stephen			The geographical distribution and (palaeo)ecology of <i>Selenopemphix undulata</i> sp nov., a new late Quaternary dinoflagellate cyst from the Pacific Ocean	MARINE MICROPALEONTOLOGY			English	Article						Selenopemphix undulata sp nov.; Dinoflagellate cysts; Pacific Ocean; Late Quaternary; (palaeo)ecology	CALIFORNIA CURRENT SYSTEM; SEA-SURFACE CONDITIONS; SANTA-BARBARA BASIN; RECENT MARINE-SEDIMENTS; NORTHERN NORTH-ATLANTIC; PERU-CHILE UNDERCURRENT; 42 DEGREES N; INDIAN-OCEAN; HYDROGRAPHIC SECTION; SOUTHEAST PACIFIC	Detailed palynological studies in the northeast (NE) Pacific, Strait of Georgia (BC, Canada), southeast (SE) Pacific and northwest Pacific (Dongdo Bay, South Korea) resulted in the recognition of the new dinoflagellate cyst species Selenopemphix undulata sp. nov. This species is restricted to cool temperate to sub-polar climate zones, where it is found in highest relative abundances in highly productive non-to reduced upwelling regions with an annual mean sea-surface temperature (aSST) below 16 degrees C and an annual mean sea-surface salinity (aSSS) between 20 and 35 psu. Those observations are in agreement with the late Quaternary fossil records from Santa Barbara Basin (ODP 893: 34 degrees N) and offshore Chile (ODP 1233: 41 degrees S), where this species thrived during the last glacial. This period was characterised by high nutrient availability and the absence of species favouring upwelling conditions. The indirect dependence of S. undulata sp. nov. abundances on nutrient availability during reduced or non-upwelling periods is expressed by the synchronous fluctuations with diatom abundances, since the distribution and growth rates of the latter are directly related with the availability of macronutrients in the surface waters. (c) 2010 Elsevier B.V. All rights reserved.	[Verleye, Thomas J.; Mertens, Kenneth N.; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada	Ghent University; University of Victoria	Verleye, TJ (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8 WE13, B-9000 Ghent, Belgium.	thomas.verleye@ugent.be	Mertens, Kenneth/AAO-9566-2020; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Pospelova, Vera/0000-0003-4049-8133; Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483	Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT); Natural Sciences and Engineering Research Council of Canada (NSERC)	Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)(Institute for the Promotion of Innovation by Science and Technology in Flanders (IWT)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	Thanks to Maryse Henry (GEOTOP-UQAM) for providing us the MODIS productivity data of the East Pacific core-top sites. Surface sample material is provided by Oregon State University (OSU), Integrated Ocean Drilling Program (IODP), Scripps Institution of Oceanography (SIO), U.S. Geological Survey (USGSMP) and Woods Hole Oceanographic Institution (WHOI). M. A. Godoi Millan is thanked for providing additional surface sample material. M. J. Head and one anonymous reviewer are acknowledged, since their suggestions considerably improved the manuscript. Financial support to T.J. Verleye was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT). This work was partially funded by the Natural Sciences and Engineering Research Council of Canada (NSERC) through grant to V. Pospelova. K.N. Mertens is a Postdoctoral fellow of FWO Belgium.	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Brasil, V17, P361; Verleye TJ, 2010, PALAEOGEOGR PALAEOCL, V298, P319, DOI 10.1016/j.palaeo.2010.10.006; Verleye TJ, 2010, QUATERNARY SCI REV, V29, P1025, DOI 10.1016/j.quascirev.2010.01.009; Verleye TJ, 2009, PALYNOLOGY, V33, P77; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; WOOSTER WS, 1961, J MAR RES, V19, P97; Wyrtki K., 1963, Bulletin of the Scripps Institute of Oceanography, V8, P313; Yamamato M, 2007, QUATERNARY SCI REV, V26, P405, DOI 10.1016/j.quascirev.2006.07.014; ZONNEVELD, 2001, OCEANOGRAPHY, V48, P25; Zonneveld KAF, 1997, REV PALAEOBOT PALYNO, V97, P319, DOI 10.1016/S0034-6667(97)00002-X; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	132	31	32	1	15	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0377-8398			MAR MICROPALEONTOL	Mar. Micropaleontol.	MAR	2011	78	3-4					65	83		10.1016/j.marmicro.2010.10.001	http://dx.doi.org/10.1016/j.marmicro.2010.10.001			19	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	733WZ					2025-03-11	WOS:000288296500001
J	Morgenroth, P; Rahardjo, AT; Maryunani, KA				Morgenroth, Peter; Rahardjo, Antonius T.; Maryunani, K. Anwar			Dinoflagellate cysts from two Oligocene surface sections on Java Island, Indonesia	PALAEONTOGRAPHICA ABTEILUNG B-PALAOPHYTOLOGIE			English	Article						dinoflagellate cysts; Apteodinium; Spiniferites; Oligocene; Indonesia	ACRITARCHS; HYSTRICHOSPHERES; PROPOSALS	As part of a study on the stratigraphic distribution of dinoflagellate cysts in the Tertiary of Indonesia, two Oligocene surface sections in West Java have been investigated: The type section of the Batuasih Formation located near Cibadak and a section close to Padalarang. The Batuasih Formation represents a transgressional marine sequence consisting mainly of claystones deposited after the continental Eocene/Oligocene Bajah Formation. This sequence is overlain by limestones of the Rajamandala Formation. Foraminifera found by the authors and studies made on nannoplankton date the Batuasih section as Early Upper to Late Early Oligocene. Dinoflagellate cysts are abundant in phosphatic nodules, but are heavily affected by thermal metamorphism, past overheating of the section, in the claystones and sandstones. The Padalarang section consists of claystones with few thin sandstone intercalations in the upper part. Foraminifera are indicative of planktonic zones P20-P21, i.e. Early Upper to Late Early Oligocene. Dinoflagellate cysts are common and seem to indicate that this section, although within the P20-P21 zones, may represent a slightly younger interval than that exposed at Batuasih. Twenty-six dinoflagellate species have been found in both sections including three new species. Our investigations have resulted in the identification of several stratigraphic markers for the Oligocene strata in the region.	[Rahardjo, Antonius T.; Maryunani, K. Anwar] Inst Technol Bandung, Dept Geol, Bandung 40132, Indonesia	Institute Technology of Bandung	Morgenroth, P (通讯作者)，Trienendorfer Str 100, D-58300 Wetter, Germany.	pawmorg@yahoo.com; tjipto@gc.itb.ac.id; anwar@gc.itb.ac.id			LEMBAGA ILMU PENGETAHUAN INDONESIA (Indonesian Institute of Sciences), Jakarta	LEMBAGA ILMU PENGETAHUAN INDONESIA (Indonesian Institute of Sciences), Jakarta	Peter Morgenroth would like to thank LEMBAGA ILMU PENGETAHUAN INDONESIA (Indonesian Institute of Sciences), Jakarta, which has initially supported this study.	AGELOPOULOS J, 1967, THESIS TUBINGEN; [Anonymous], P IND PETR ASS 17 AN; ARTZNER DG, 1978, CAN J BOT, V56, P1381, DOI 10.1139/b78-158; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BIFFI U, 1983, MICROPALEONTOLOGY, V29, P126, DOI 10.2307/1485563; Blow W.H., 1979, The Cenozoic Globigerinidae, VI-III, P1; BOLLI H. 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L., 1955, MICROPALEONTOLOGY, V1, P261, DOI 10.2307/1484455; PASTIELS ANDRE, 1948, MEM MUS ROY HIST NAT BELGIQUE, V109, P1; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; ROSSIGNOL MARTINE, 1962, POLLEN SPORES, V4, P121; SAMUEL L, 1973, GEOLOGIC MAP S UNPUB; Sarjeant W. A. 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Abt. B-Palaophytol.	MAR	2011	284	4-6					125	157		10.1127/palb/284/2011/125	http://dx.doi.org/10.1127/palb/284/2011/125			33	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	732LH					2025-03-11	WOS:000288186100002
J	Genovesi, B; Shin-Grzebyk, MS; Grzebyk, D; Laabir, M; Gagnaire, PA; Vaquer, A; Pastoureaud, A; Lasserre, B; Collos, Y; Berrebi, P; Masseret, E				Genovesi, Benjamin; Shin-Grzebyk, Mi-Sun; Grzebyk, Daniel; Laabir, Mohamed; Gagnaire, Pierre-Alexandre; Vaquer, Andre; Pastoureaud, Annie; Lasserre, Bernard; Collos, Yves; Berrebi, Patrick; Masseret, Estelle			Assessment of cryptic species diversity within blooms and cyst bank of the <i>Alexandrium tamarense</i> complex (Dinophyceae) in a Mediterranean lagoon facilitated by semi-multiplex PCR	JOURNAL OF PLANKTON RESEARCH			English	Article						Alexandrium catenella; Alexandrium tamarense; PSP; ITS; Thau lagoon	RED-TIDE; TOXIC DINOFLAGELLATE; LEBOUR BALECH; GOLFO-NUEVO; CATENELLA; POPULATIONS; SEQUENCE; IDENTIFICATION; HARMFUL; GENE	The occurrence of Alexandrium catenella related to paralytic shellfish poisoning (PSP) in the French Mediterranean Thau lagoon has been known since 1998. Blooms are recurrent and usually occur each year in spring and/or autumn. Taxonomic diversity of resting cysts and vegetative cells has been studied through morphological examination and molecular typing of 558 clonal strains sampled in 2004 and 2007. Sequencing the nuclear rRNA fragment, including ITS1, the 5.8S rRNA gene, ITS2, and the D1/D2 28S rRNA genes, enabled two species to be determined, A. catenella and A. tamarense, which are difficult to distinguish morphologically (cryptic species). In order to carry out extensive and accurate molecular determinations, an original semi-multiplex PCR method, using new ribotype-specific primers targeting the 18S-28S rRNA ITS region, has been developed. The relative abundance of each species was then established in seawater in 2007 and in the sediment collected in 2004. The co-occurrence of A. catenella (Group IV), which is known as the main species responsible for toxic PSP events since 1998 and of A. tamarense (Group III) (non-toxic) that was not formally recognized by microscopic observation since 1995, was examined for several months.	[Genovesi, Benjamin; Shin-Grzebyk, Mi-Sun; Grzebyk, Daniel; Laabir, Mohamed; Vaquer, Andre; Lasserre, Bernard; Collos, Yves; Masseret, Estelle] Univ Montpellier 2, UMR 5119, CNRS IFREMER IRD UM2, Equipe Efflorescences Tox & Diversite Algale, F-34095 Montpellier 05, France; [Genovesi, Benjamin; Gagnaire, Pierre-Alexandre; Berrebi, Patrick] Univ Montpellier 2, UMR 5554, CNRS IRD UM2, Inst Sci Evolut, F-34095 Montpellier 05, France; [Pastoureaud, Annie] IFREMER, Lab Environm Ressources LR, F-34203 Sete, France	Universite de Montpellier; Ifremer; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; CNRS - Institute of Ecology & Environment (INEE); Ifremer	Genovesi, B (通讯作者)，Univ Montpellier 2, UMR 5119, CNRS IFREMER IRD UM2, Equipe Efflorescences Tox & Diversite Algale, CC093,Pl E Bataillon, F-34095 Montpellier 05, France.	benjamin.genovesi@gmail.com	Gagnaire, Pierre-Alexandre/S-2352-2019; Grzebyk, Daniel/A-9286-2009	Grzebyk, Daniel/0000-0002-1130-7724	French National Programme "Ecosphere Continentale Cotiere [EC2CO-PNEC]; Agence Nationale de la Recherche [ANR-06-BLAN-0397 GenoSynTox]	French National Programme "Ecosphere Continentale Cotiere; Agence Nationale de la Recherche(Agence Nationale de la Recherche (ANR))	This study was supported by grants from the French National Programme "Ecosphere Continentale & Cotiere (EC2CO-PNEC) and from the Agence Nationale de la Recherche (ANR-06-BLAN-0397 GenoSynTox). The monitoring survey and field sampling was allowed by the ALCAT programme of IFREMER. We thank Jeremy Beguin and Boram Lee (the latter in the frame of a CNRS researcher exchange project with South Korea) for help in the ribotyping of monoclonal cultures. We have a thought for Patrick Gentien (Ifremer DYNECO-Brest), we will miss his valuable support. We thank the assistance of two anonymous reviewers who contributed to improving this manuscript.	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Plankton Res.	MAR	2011	33	3					405	414		10.1093/plankt/fbq127	http://dx.doi.org/10.1093/plankt/fbq127			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	717EG		Bronze, Green Submitted			2025-03-11	WOS:000287025500005
J	Andresen, CS; McCarthy, DJ; Dylmer, CV; Seidenkrantz, MS; Kuijpers, A; Lloyd, JM				Andresen, Camilla S.; McCarthy, David J.; Dylmer, Christian Valdemar; Seidenkrantz, Marit-Solveig; Kuijpers, Antoon; Lloyd, Jerry M.			Interaction between subsurface ocean waters and calving of the Jakobshavn Isbrae during the late Holocene	HOLOCENE			English	Article						dinoflagellate; foraminifera; iceberg calving; Jakobshavn Isbrae; late-Holocene climate variability; West Greenland Current	GREENLAND ICE-SHEET; DINOFLAGELLATE CYST ASSEMBLAGES; MODERN BENTHIC FORAMINIFERA; NORTH-ATLANTIC CLIMATE; DISKO-BUGT; WEST GREENLAND; ENVIRONMENTAL VARIABILITY; SOUTHERN GREENLAND; SHELF SEDIMENTS; MID-HOLOCENE	A marine sediment core from Vaigat in Disko Bugt, West Greenland, has been analysed in terms of lithology, dinoflagellate cysts and foraminifera in order to evaluate the influence of oceanographic variability on West Greenland glacier stability. The data show that during the past 5200 years the Atlantic foraminiferal abundance in the subsurface waters of the West Greenland Current (WGC) episodically increased, indicating periods of increases in the inflow of subsurface warm Atlantic water at 2000-1500 cal. yr BP and 1300 cal. yr BP as well as periods of less pronounced increased bottom-water temperatures around 4700-4000 cal. yr BP, 3100-2800, 2600, 1000-800, 500-400, and at 200 cal. yr. The sedimentological and dinoflagellate cyst data indicate that these episodes with enhanced advection of Irminger Sea-derived waters are accompanied by increased iceberg rafting, which we link to increased iceberg calving in relation to destabilization of the Jakobshavn Isbrae. The long-term trend in the data documents the end of a late-Holocene Thermal Maximum between 5200 and 4300 cal. yr BP and a final onset of the Neoglaciation at 3500 cal. yr BP. Increased responses of the iceberg rafting after 3500 cal. yr BP, reflects a westward/seaward advance of the glacier margin in relation to onset of Neoglaciation and a development of the glacier into a floating tongue after 2000 cal. yr BP. A comparison of our record with a record from the eastern North Atlantic indicates that a NAO-like anomaly pattern between subsurface waters in West Greenland and atmospheric temperature in the Eastern North Atlantic may have been operating during most of the late Holocene. However, during the past 1000 years the NAO signal may have weakened as some other mode of climate variability overprints the anti-phase climate signal in this region.	[Andresen, Camilla S.; Kuijpers, Antoon] Geol Survey Denmark & Greenland GEUS, Dept Marine Geol & Glaciol, DK-1350 Copenhagen K, Denmark; [McCarthy, David J.; Lloyd, Jerry M.] Univ Durham, Durham DH1 3HP, England; [Dylmer, Christian Valdemar; Seidenkrantz, Marit-Solveig] Aarhus Univ, DK-8000 Aarhus C, Denmark	Geological Survey Of Denmark & Greenland; Durham University; Aarhus University	Andresen, CS (通讯作者)，Geol Survey Denmark & Greenland GEUS, Dept Marine Geol & Glaciol, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	csa@geus.dk	Andresen, Camilla/G-2718-2013; Seidenkrantz, Marit-Solveig/A-3451-2012	Andresen, Camilla S./0000-0002-5249-1812; Seidenkrantz, Marit-Solveig/0000-0002-1973-5969	Danish Council for Independent Research \ Nature and Universe [09-064954/FNU, 09-069833/FNU]; Commission for Scientific Research on Greenland (KVUG); EU [243908]; Durham University; GEUS [DA06-139G]; Bureau of Mineral Resources in Nuuk; NunaOil, Greenland	Danish Council for Independent Research \ Nature and Universe(Det Frie Forskningsrad (DFF)); Commission for Scientific Research on Greenland (KVUG); EU(European Union (EU)); Durham University; GEUS(General Electric); Bureau of Mineral Resources in Nuuk; NunaOil, Greenland	This project has been supported by the Danish Council for Independent Research vertical bar Nature and Universe in a grant to C. S. Andresen (Grant no. 09-064954/FNU), the IPY 'NEWGREEN' project funded by the Commission for Scientific Research on Greenland (KVUG), 'TROPOLINK' funded by The Danish Council for Independent Research vertical bar Nature and Universe (Grant no. 09-069833/FNU) and Past4Future (EU FP7 project no. 243908). D.J. McCarthy acknowledges funding provided by a Durham University Doctoral Research Fellowship. Core DA06-139G was collected in 2006 during a cruise of RV Dana funded by GEUS, the Bureau of Mineral Resources in Nuuk, and NunaOil, Greenland. We thank master and crew for their engagement during the work at sea, and John Boserup (GEUS) for assisting with sediment coring. We are also grateful to Peter H. Kristensen, Kirsten Rosendal and Elly Lykkegaard Hein (Aarhus University) for laboratory treatment of samples for dinoflagellate cyst analysis and to Sandrine Solignac (Aarhus University), for help in the identification of dinocyst species.	Andersen O.G. 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Weidick A, 2007, GEOL SURV DEN GREENL, P7; Willemse NW, 2003, QUATERNARY RES, V59, P322, DOI 10.1016/S0033-5894(03)00037-1; Willemse NW, 1999, GEOLOGY, V27, P580, DOI 10.1130/0091-7613(1999)027<0580:HCSTVF>2.3.CO;2; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	84	52	55	0	9	SAGE PUBLICATIONS LTD	LONDON	1 OLIVERS YARD, 55 CITY ROAD, LONDON EC1Y 1SP, ENGLAND	0959-6836	1477-0911		HOLOCENE	Holocene	MAR	2011	21	2					211	224		10.1177/0959683610378877	http://dx.doi.org/10.1177/0959683610378877			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	725MI		Green Accepted			2025-03-11	WOS:000287648400001
J	Gu, HF; Luo, ZH; Wang, Y; Lan, DZ				Gu, Hai-Feng; Luo, Zhao-He; Wang, Yan; Lan, Dong-Zhao			Diversity, distribution, and new phylogenetic information of calcareous dinoflagellates from the China Sea	JOURNAL OF SYSTEMATICS AND EVOLUTION			English	Article						calcareous dinoflagellates; Calciodinellum; China Sea; Leonella; Posoniella; Scrippsiella	SP-NOV DINOPHYCEAE; SURFACE SEDIMENTS; SCRIPPSIELLA DINOPHYCEAE; MARINE DINOFLAGELLATE; CYSTS; PERIDINIALES; TEMPERATURE; STRATEGIES; MORPHOLOGY; SOUTH	Calcareous dinoflagellates have been recorded from subarctic to tropical areas, inhabiting both neritic and oceanic regions. In the present study we analyse 12 sediment samples from the China Sea to establish the existence of calcareous dinoflagellates in this area. A total of 11 calcareous dinoflagellate species were recorded, among them, three genera (Calciodinellum, Leonella, Posoniella) and seven species (Calciodinellum albatrosianum, C. levantinum, C. operosum, Leonella granifera, Posoniella tricarinelloides, Scrippsiella irregularis, and S. regalis) were reported from the China Sea for the first time. Cysts of S. irregularis and S. precaria are identical, with a mesoepicystal archeopyle, representing the loss of 2-4' and 1-3a paraplates; however, their thecal plates vary slightly and differ from each other in 78 positions of the internal transcribed spacer sequence. Scrippsiella trochoidea is dominant in coastal areas, whereas Calciodinellum albatrosianum is the most abundant offshore. Scrippsiella irregularis is distributed widely along the coast of China, whereas S. precaria is recorded only in northern China. Leonella granifera is the second most abundant species offshore, comprising 15-40% of the cyst assemblage.	[Gu, Hai-Feng; Luo, Zhao-He; Lan, Dong-Zhao] Third Inst Oceanog, Xiamen 361005, Peoples R China; [Wang, Yan] Jinan Univ, Coll Life Sci & Technol, Res Ctr Harmful Algae & Aquat Environm, Guangzhou 510632, Guangdong, Peoples R China	Third Institute of Oceanography, Ministry of Natural Resources; Jinan University	Gu, HF (通讯作者)，Third Inst Oceanog, Xiamen 361005, Peoples R China.	haifenggu@yahoo.com	Luo, Zhaohe/ITT-7163-2023; Gu, Haifeng/ADN-4528-2022	Luo, Zhaohe/0000-0001-8662-2414; Gu, Haifeng/0000-0002-2350-9171	National Basic Research Program of China (973 Program) [2010CB428702]; National Scientific-Basic Special Fund [2009FY210400]; National Natural Science Foundation of China [30670156]	National Basic Research Program of China (973 Program)(National Basic Research Program of China); National Scientific-Basic Special Fund; National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	We thank Dr. K.J.S. METER for helpful discussion and Dr. Walker O. SMITH for improvement of the English. Dr. Rui WU is thanked for collecting sediment samples in the South China Sea. This project was supported by the National Basic Research Program of China (973 Program, 2010CB428702), National Scientific-Basic Special Fund (2009FY210400), and the National Natural Science Foundation of China (30670156).	[Anonymous], 1999, Use of Proxies in Paleoceanography: Examples from the South Atlantic; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; Bison KM, 2009, MAR MICROPALEONTOL, V73, P49, DOI 10.1016/j.marmicro.2009.06.008; [蔡榕硕 CAI Rong-shuo], 2009, [台湾海峡, Journal of Oceanography in Taiwan Strait], V28, P559; Cao Qi-Yuan, 2002, Oceanologia et Limnologia Sinica, V33, P600; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; Elbrächter M, 2008, TAXON, V57, P1289, DOI 10.1002/tax.574019; Evitt W.R., 1967, STANFORD U PUBIS GEO, V10, P1; Fensome R. 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F., 2005, Palaeontologische Zeitschrift, V79, P61	36	9	11	3	26	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	1674-4918	1759-6831		J SYST EVOL	J. Syst. Evol.	MAR	2011	49	2					126	137		10.1111/j.1759-6831.2010.00110.x	http://dx.doi.org/10.1111/j.1759-6831.2010.00110.x			12	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	750GO					2025-03-11	WOS:000289534100005
J	Harding, IC; Charles, AJ; Marshall, JEA; Pälike, H; Roberts, AP; Wilson, PA; Jarvis, E; Thorne, R; Morris, E; Moremon, R; Pearce, RB; Akbari, S				Harding, Ian C.; Charles, Adam J.; Marshall, John E. A.; Paelike, Heiko; Roberts, Andrew P.; Wilson, Paul A.; Jarvis, Edward; Thorne, Robert; Morris, Emily; Moremon, Rebecca; Pearce, Richard B.; Akbari, Shir			Sea-level and salinity fluctuations during the Paleocene-Eocene thermal maximum in Arctic Spitsbergen	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						abrupt/rapid climate change; PETM; paleoecology; sedimentology; Spitsbergen; Arctic	CARBON-ISOTOPE EXCURSION; DINOFLAGELLATE CYSTS; METHANE HYDRATE; BIGHORN BASIN; OCEAN; CLIMATE; MARINE; CLAY; TEMPERATURE; TRANSITION	Palaeoenvironmental manifestations of the Paleocene-Eocene thermal maximum (PETM; similar to 56 Ma) are relatively well documented in low- to mid-latitude settings and at high southern latitudes, but no documented high northern latitude sites record the entire hyperthermal event. We present high-resolution multi-proxy records from a PETM succession on Spitsbergen in the high Arctic (palaeolatitude similar to 75 degrees N). By comparing our results with those from Integrated Ocean Drilling Program Site 302-4A, we document regional palaeoenvironmental variations in the expression of the PETM, with evidence for major differences in basin-margin vegetation and water column oxygen depletion. Sedimentological, palynological and geochemical data demonstrate a pre-PETM sea level rise in Spitsbergen before the -4 parts per thousand delta C-13(TOC) excursion, which culminated in maximum flooding during the peak of the event. The appearance of the dinofiagellate cyst Apectodinium before the onset of the carbon isotope excursion (CIE) corroborates that environmental change in the Arctic had begun prior to the CIE. Sedimentological and palynological evidence indicate that elevated terrestrial runoff resulted in water column stratification, providing further evidence for an intensification of the hydrological cycle during the PETM. (C) 2010 Elsevier B.V. All rights reserved.	[Harding, Ian C.; Charles, Adam J.; Marshall, John E. 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Sci. Lett.	FEB 15	2011	303	1-2					97	107		10.1016/j.epsl.2010.12.043	http://dx.doi.org/10.1016/j.epsl.2010.12.043			11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	738JT					2025-03-11	WOS:000288636800009
J	Bijl, PK; Pross, J; Warnaar, J; Stickley, CE; Huber, M; Guerstein, R; Houben, AJP; Sluijs, A; Visscher, H; Brinkhuis, H				Bijl, Peter K.; Pross, Joerg; Warnaar, Jeroen; Stickley, Catherine E.; Huber, Matthew; Guerstein, Raquel; Houben, Alexander J. P.; Sluijs, Appy; Visscher, Henk; Brinkhuis, Henk			Environmental forcings of Paleogene Southern Ocean dinoflagellate biogeography	PALEOCEANOGRAPHY			English	Article							MIDDLE EOCENE; KERGUELEN PLATEAU; SEA-LEVEL; OLIGOCENE; CLIMATE; ANTARCTICA; HISTORY; PACIFIC; CARBON; CYSTS	Despite warm polar climates and low meridional temperature gradients, a number of different high-latitude plankton assemblages were, to varying extents, dominated by endemic species during most of the Paleogene. To better understand the evolution of Paleogene plankton endemism in the high southern latitudes, we investigate the spatiotemporal distribution of the fossil remains of dinoflagellates, i.e., organic-walled cysts (dinocysts), and their response to changes in regional sea surface temperature (SST). We show that Paleocene and early Eocene (similar to 65-50 Ma) Southern Ocean dinocyst assemblages were largely cosmopolitan in nature but that a distinct switch from cosmopolitan-dominated to endemic-dominated assemblages (the so-called "transantarctic flora") occurred around the early-middle Eocene boundary (similar to 50 Ma). The spatial distribution and relative abundance patterns of this transantarctic flora correspond well with surface water circulation patterns as reconstructed through general circulation model experiments throughout the Eocene. We quantitatively compare dinocyst assemblages with previously published TEX86-based SST reconstructions through the early and middle Eocene from a key locality in the southwest Pacific Ocean, ODP Leg 189 Site 1172 on the East Tasman Plateau. We conclude that the middle Eocene onset of the proliferation of the transantarctic flora is not linearly correlated with regional SST records and that only after the transantarctic flora became fully established later in the middle Eocene, possibly triggered by large-scale changes in surface-ocean nutrient availability, were abundances of endemic dinocysts modulated by regional SST variations.	[Bijl, Peter K.; Warnaar, Jeroen; Houben, Alexander J. P.; Sluijs, Appy; Visscher, Henk; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Fac Sci, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Guerstein, Raquel] Univ Nacl Sur, Dept Geol, INGEOSUR, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Huber, Matthew] Purdue Univ, W Lafayette, IN 47906 USA; [Pross, Joerg] Goethe Univ Frankfurt, Inst Geosci, Paleoenvironm Dynam Grp, D-60438 Frankfurt, Germany; [Stickley, Catherine E.] Univ Tromso, Dept Geol, N-9037 Tromso, Norway; [Stickley, Catherine E.] Norwegian Polar Inst,Polar Environm Ctr, Tromso, Norway	Utrecht University; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Purdue University System; Purdue University; Goethe University Frankfurt; UiT The Arctic University of Tromso; Norwegian Polar Institute	Bijl, PK (通讯作者)，Univ Utrecht, Inst Environm Biol, Fac Sci, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	p.k.bijl@uu.nl	Brinkhuis, Henk/B-4223-2009; Sluijs, Appy/B-3726-2009; Huber, Matthew/A-7677-2008	Sluijs, Appy/0000-0003-2382-0215; Visscher, Henk/0000-0002-9276-0220; Brinkhuis, Henk/0000-0003-0253-6610; Houben, Alexander/0000-0002-9497-1048; Bijl, Peter/0000-0002-1710-4012; Huber, Matthew/0000-0002-2771-9977; Guerstein, G. Raquel/0000-0003-1623-1084	U.S. National Science Foundation; LPP foundation; Biodiversity and Climate Research Center of the Hessian initiative for scientific and economic excellence (LOEWE); Netherlands Organization for Scientific Research [863.07.001]; Statoil	U.S. National Science Foundation(National Science Foundation (NSF)); LPP foundation; Biodiversity and Climate Research Center of the Hessian initiative for scientific and economic excellence (LOEWE); Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO)); Statoil	This research used samples and data provided by the Deep Sea Drilling Project (DSDP) and the Ocean Drilling Program (ODP). DSDP and ODP were sponsored by the U.S. National Science Foundation (ODP was also sponsored by other participating countries) under the management of Joint Oceanographic Institutions (JOI) Inc. The Shipboard Scientific Party of IODP Expedition Leg 318 is thanked for providing data. This project was funded by the LPP foundation to P. K. Bijl. J. Pross acknowledges support by the Biodiversity and Climate Research Center of the Hessian initiative for scientific and economic excellence (LOEWE). C. E. Stickley acknowledges the Research Council of Norway. R. Guerstein acknowledges the Agencia Nacional de Promocion Cientifica y Tecnologica-PICT 26057. A. Sluijs thanks the Netherlands Organization for Scientific Research (Veni grant 863.07.001). M. Huber acknowledges continuing support from NSF 0927946-ATM and NSF PC2C 0902882-OCE. M. Huber also is grateful to the New Zealand GNS Science for providing an excellent work environment while he was visiting. A. J. P. Houben and H. Brinkhuis are grateful to Statoil for financial support. We thank Giuseppe Cortese, Erica Crouch (both GNS Science, New Zealand), Oliver Heiri (Utrecht University), and Martin Pearce (Statoil) for constructive discussions. We thank Jan van Tongeren and Natasja Welters for technical support. Constructive reviews by Philip Sexton and an anonymous reviewer greatly improved an earlier version of the manuscript.	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J	Harland, R; Nordberg, K				Harland, Rex; Nordberg, Kjell			The identification, occurrence and importance of microreticulate dinoflagellate cysts in the latest Holocene sediments of the Skagerrak and Kattegat, west coast of Sweden	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Gymnodinium nolleri; Holocene; Subatlantic; Kattegat; Skagerrak; west coast Sweden	SP-NOV DINOPHYCEAE; GYMNODINIUM-CATENATUM; RESTING CYSTS; RECORD; BLOOMS; FJORD	Microreticulate dinoflagellate cysts are a major component of latest Holocene (Subatlantic) sediments from the Skagerrak and Kattegat, off the west coast of Sweden. They first appear about 4000 years BP, become more prominent from 2000 years BP to about 300 years BP, before they decline to their present minor occurrence in modern sediments. In particular they occur in at least two major pulses and one minor pulse, where their numbers exceed 5000 cysts per gram of sediment, seemingly correlating to times toward the end of the Roman Warm Period, to between the Roman and Medieval warm periods, and with the Little Ice Age. The minor pulse occurs within the Medieval Warm Period. Originally thought to be assignable to the species Gymnodinium catenatum Graham 1943 these cysts were interpreted as an indication of warmer waters, warmer climates and significant changes within the hydrology of the region. Opinion amongst palynologists and phycologists now favour assignment of these cysts to Gymnodinium nolleri Ellegaard and Moestrup 1999, based mainly upon their dimensions; this cautions against earlier environmental interpretations. Further study of microreticulate cysts from core material recovered in the Kattegat and Skagerrak (Gullmar Fjord) supports the identification of these cysts as G. nolleri and emphasises an environmental interpretation that does not solely depend upon possible temperature change but that other factors may be involved. This study also emphasises the importance of these microreticulate cysts to the biostratigraphy of the Subatlantic in offshore west coast Sweden. (C) 2010 Elsevier B.V. All rights reserved.	[Harland, Rex; Nordberg, Kjell] Univ Gothenburg, Dept Earth Sci, S-40530 Gothenburg, Sweden	University of Gothenburg	Harland, R (通讯作者)，Univ Gothenburg, Dept Earth Sci, POB 460, S-40530 Gothenburg, Sweden.	rex.harland@ntlworld.com; kjno@gvc.gu.se		Nordberg, Kjell/0000-0003-0085-4607	Swedish Research Council [VR 621-2007-4369]; Lamm Foundation; Goteborg University Marine Research Centre	Swedish Research Council(Swedish Research Council); Lamm Foundation; Goteborg University Marine Research Centre	The authors would like to thank MB Stratigraphy Ltd for their careful processing of the material from Core 9004 and supplying the detailed description of their methodology. In particular we would also like to acknowledge helpful discussions, and the supplying of literature, with Drs Christopher J S Bolch, at the University of Tasmania and Dr Marianne Ellegaard, at the University of Copenhagen. Dr Christopher J S Bolch kindly read an earlier draft of this contribution. Dr Jim Riding, at the British Geological Survey, Keyworth, kindly made available his digital photomicrography equipment to the senior author. This work is financed through the Swedish Research Council (VR 621-2007-4369), Lamm Foundation and the Goteborg University Marine Research Centre (GMF). The manuscript has benefited from the careful and constructive reviews of an anonymous referee and Dr Karin Zonneveld, at the University of Bremen, for which we are most grateful.	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Palaeobot. Palynology	FEB	2011	164	1-2					84	92		10.1016/j.revpalbo.2010.11.009	http://dx.doi.org/10.1016/j.revpalbo.2010.11.009			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	736EA					2025-03-11	WOS:000288472200007
J	El Beialy, S; El-Soughier, M; Mohsen, SA; El Atfy, H				El Beialy, Salah; El-Soughier, Maher; Mohsen, Sayed Abdel; El Atfy, Haytham			Palynostratigraphy and paleoenvironmental significance of the Cretaceous succession in the Gebel Rissu-1 well, north Western Desert, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Palynostratigraphy; Cretaceous; Pollen; Spores; Egypt	ANGIOSPERM POLLEN; DAKHLA OASIS; OIL-FIELD; PALYNOLOGY; STRATIGRAPHY; PALYNOMORPHS; SEDIMENTS; AREA; SEQUENCES; SPORES	Palynological investigation of the Cretaceous Abu Roash, Bahariya, Kharita, Alamein, Alam El Bueib and Betty formations, encountered in the Gebel Rissu-1 well, north Western Desert, Egypt yielded 27 species of pteridophytic spores, 24 of gymnosperm pollen, 25 of angiosperm pollen and 11 of dinoflagellate cysts in addition to some acritarchs, foraminiferal test linings and freshwater algae. This enabled us to recognize five miospore biozones arranged from youngest to oldest as: Classopollis brasiliensis-Afropollis cf. kahramanensis-Dichastopollenites ghazalataensis Assemblage Zone (Late Cenomanian); Elaterosporites klaszii-Sofrepites legouxae-Afropollis jardinus Assemblage Zone (Middle/Late Albian-Early Cenomanian); Pennipollis peroreticulatus-Duplexisporites generalis-Tricolpates Assemblage Zone (Early Aptian-Early Albian); Tucanopollis crisopolensis-Afropollis sp. Assemblage Zone (Barremian) and Appendicisporites cf. tricornitatus-Ephedripites spp. Assemblage Zone (Late Neocomian). The Early Cretaceous Kharita, Alam El Bueib and the Betty formations encountered in the Gebel Rissu-1 well are interpreted to indicate oxic proximal and distal shelf deposits, characterized by type III/IV. V kerogen, which is gas prone but having little potential to produce hydrocarbons. The Upper Cretaceous Abu Roash and Bahariya formations are characterized by a distal suboxic-anoxic and marginal dysoxic-anoxic environment, and their kerogen type III/II indicates gas/oil prone nature. The Bahariya and Kharita Albian-Cenomanian sediments in the present study witnessed the onset of a semi-arid to arid climate, with local or seasonal humid conditions, based on the continuous high abundance of the elaterates pollen and Afropollis-producing plants that inhabited the paleotropical humid coastal plains. (C) 2010 Elsevier Ltd. All rights reserved.	[El Beialy, Salah; El Atfy, Haytham] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [El-Soughier, Maher; Mohsen, Sayed Abdel] S Valley Univ, Fac Sci, Dept Geol, Aswan, Egypt	Egyptian Knowledge Bank (EKB); Mansoura University; Egyptian Knowledge Bank (EKB); Aswan University; South Valley University Egypt	El Beialy, S (通讯作者)，Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt.	syelbeialy@mans.edu.eg	Beialy, Salah/AAD-7329-2020; Atfy, Haytham/AAT-2276-2021	El Atfy, Haytham/0000-0003-1618-7220				ABDELMALIK WM, 1981, ABHANDLUNGEN, V162, P244; *AMOCO, 1969, WELL LOG GEB RISS 1; [Anonymous], Western Europe Oil and Gas Insights; [Anonymous], 1980, PALEOBIOLOGY PLANT P; Awad M.Z., 1994, Berliner geowissenschaftlische Abhandlungen A, V161, P1; BARAKAT MG, 1980, B CAIRO U, V49, P457; Batten D.J., 1985, Journal of Micropalaeontology, V4, P151; Boltenhagen E., 1980, Memoires de la Section des Sciences, V7, P11; Brenner G. 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J	Figueroa, RI; Vazquez, JA; Massanet, A; Murado, MA; Bravo, I				Isabel Figueroa, Rosa; Antonio Vazquez, Jose; Massanet, Ana; Anxo Murado, Miguel; Bravo, Isabel			INTERACTIVE EFFECTS OF SALINITY AND TEMPERATURE ON PLANOZYGOTE AND CYST FORMATION OF <i>ALEXANDRIUM MINUTUM</i> (DINOPHYCEAE) IN CULTURE	JOURNAL OF PHYCOLOGY			English	Article						Alexandrium minutum; encystment; planozygotes; response surface methodology; salinity; sexuality; temperature	DINOFLAGELLATE GONYAULAX-TAMARENSIS; LACTIC-ACID BACTERIA; HARMFUL ALGAL BLOOMS; SEXUAL REPRODUCTION; TOXIC DINOFLAGELLATE; LIFE-CYCLE; GYMNODINIUM-CATENATUM; PERIDINIUM-CINCTUM; RESTING CYST; ENCYSTMENT	1. Low P/N ratios seem to induce gamete expression because the percentage of planozygotes recorded in the absence of added phosphate (-P) was significantly higher than that obtained in the absence of added nitrogen (-N), or when the concentrations of both nitrogen and phosphate were 20 times lower (N/20 + P/20). 2. Salinity (S) and temperature (T) strongly affected both planozygote and cyst formation, as sexuality in the population increased significantly as salinity decreased and temperatures increased. S, T combinations that resulted in no significant cyst formation were, however, favorable for vegetative growth, ruling out the possibility of negative effects on cell physiology. 3. The initial cell density is thought to be important for sexual cyst formation by determining the chances of gamete contact. However, the inoculum concentrations tested did not explain either planozygote formation or the appearance of resting cysts.	[Isabel Figueroa, Rosa] Inst Ciences Mar ICM CSIC, Barcelona 08003, Spain; [Antonio Vazquez, Jose; Anxo Murado, Miguel] Inst Invest Marinas Vigo CSIC, Grp Reciclado & Valorizac Mat Residuales, Vigo 36208, Spain; [Massanet, Ana; Bravo, Isabel] Inst Espanol Oceanog, Vigo 36200, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Instituto de Investigaciones Marinas (IIM); Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，Inst Ciences Mar ICM CSIC, Passeig Maritim Barceloneta 37-49, Barcelona 08003, Spain.	Rosa.Figueroa@limnol.lu.se	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Vazquez Alvarez, Jose Antonio/K-5938-2014	Bravo, Isabel/0000-0003-3764-745X; Figueroa, Rosa/0000-0001-9944-7993; , Ana Massanet/0000-0003-4253-779X; Vazquez Alvarez, Jose Antonio/0000-0002-1122-4726	Spanish Ministry of Education and Science [I3P]	Spanish Ministry of Education and Science(Spanish Government)	We thank I. Ramilo, A. Fernandez-Villamarin, and P. Rial for technical assistance. R. I. Figueroa was supported by a I3P postdoctoral grant from the Spanish Ministry of Education and Science.	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Phycol.	FEB	2011	47	1					13	24		10.1111/j.1529-8817.2010.00937.x	http://dx.doi.org/10.1111/j.1529-8817.2010.00937.x			12	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	723FT	27021706	Green Submitted			2025-03-11	WOS:000287492700003
J	Akkiraz, MS; Akgün, F; Örçen, S				Akkiraz, Mehmet Serkan; Akgun, Funda; Orcen, Sefer			Stratigraphy and palaeoenvironment of the Lower-"middle" Oligocene units in the northern part of the Western Taurides (Incesu area, Isparta, Turkey)	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						Turkey; Western Taurides; Oligocene; Palynology; Foraminifera; Biostratigraphy; Palaeoenvironment	SW TURKEY; BASIN; EVOLUTION; MICROCODIUM; PALYNOLOGY; PALEOECOLOGY; MOLASSE; POLLEN; EOCENE; ANGLE	This study describes the stratigraphic and palaeoenvironmental significance of the Lower-"middle" Oligocene sediments based on the fauna from the Delikarkasi Formation and the microflora from the Incesu Formation of the Incesu area (northern part of the western Taurides, Isparta province, Turkey). In the area, the Oligocene sediments show a regressive succession, which begins with the limestones of the Delikarkasi Formation indicating marine conditions followed by conglomerates, sandstones and coaly mud-stones of alluvial and fluvial (shallow marine-continental) origin. A well preserved foraminiferal assemblage including Nummulites intermedius, Nummulites vascus and Halkyardia maxima proves an Early Oligocene age for the Delikarkasi Formation. Due to palynological markers such as Boehlensipollis hohli, Slowakipollis hippophaeoides, Dicolpopollis kockelii, Magnolipollis neogenicus ssp. minor, Plicapollis pseudoexcelsus, Caryapollenites simplex and Intratriporopollenites instructus the Incesu Formation, which concordantly rests on the Delikarkasi Formation, may be assigned to the Early-"middle" Oligocene. From the palynomorph assemblage, three zones have been recognised according to abundance of species. Zone 1 is characterized by predominance of C. simplex and Momipites punctatus and rarely presence of tricolpate and tricolporate pollen. Zone 2 consists mainly of Inaperturopollenites dubius, Leiotriletes maxoides ssp. maximus, Verrucatosporites favus, Verrucatosporites alien us and infrequently marine dinoflagellate cysts. Zone 3 is characterized by a high percentage of ferns such as Echinatisporis? chattensis and Polypodiaceoisporites saxonicus. The presence of marine dinoflagellate cysts like Apectodinium sp. and Cleistosphaeridium sp., back-mangrove elements such as Acrostichum aureum and lepidocaryoid palms (e.g. Longapertites discord is, Longapertites punctatus and Longapertites psilatus) in the sediments of the Incesu Formation imply coastal or near-coastal conditions. Terrestrial palynomorphs in more inland settings were transported by running water towards the sea. Conifers are represented by poorly preserved and rare pollen grains of Pityosporites, Cathayapollis and Piceapollis which may have been transported by wind. In this study, the terrestrial climate of the Incesu Formation is also discussed on the basis of the Coexistence Approach method. The climate was warm at the coast (over 20 degrees C), as evidenced by A. aureum and lepidocaryoid palms, whereas there was a mean annual temperature of 17.2-17.4 degrees C must be assumed for the upland environment(s). (C) 2010 Elsevier Ltd. All rights reserved.	[Akkiraz, Mehmet Serkan] Dumlupinar Univ, Dept Geol Engn, TR-43270 Kutahya, Turkey; [Akgun, Funda] Dokuz Eylul Univ, Dept Geol Engn, TR-35160 Izmir, Turkey; [Orcen, Sefer] Yuzuncu Yil Univ, Dept Geol Engn, Van, Turkey	Dumlupinar University; Dokuz Eylul University; Yuzuncu Yil University	Akkiraz, MS (通讯作者)，Dumlupinar Univ, Dept Geol Engn, TR-43270 Kutahya, Turkey.	serkanakkiraz@dpu.edu.tr; funda.akgun@deu.edu.tr; sorcen@yyu.edu.tr	akkiraz, mehmet/ADP-2366-2022; Akgün, Funda/AAC-2859-2020	Akgun, Funda/0000-0002-6028-6704	Scientific and Technical Research Council of Turkey (TUBITAK) [101Y133]; Dokuz Eylul University Graduate School of Natural and Applied Sciences [02KB.FEN.046]	Scientific and Technical Research Council of Turkey (TUBITAK)(Turkiye Bilimsel ve Teknolojik Arastirma Kurumu (TUBITAK)); Dokuz Eylul University Graduate School of Natural and Applied Sciences(Dokuz Eylul University)	This study was supported by a research grant from the Scientific and Technical Research Council of Turkey (TUBITAK Grant Code 101Y133) and the Dokuz Eylul University Graduate School of Natural and Applied Sciences (Project Number: 02KB.FEN.046). The assistance of Ramazan San, Aykut Saygili, Yilmaz Ruzgr, Gokhan Cicek and Kutay Ersal are appreciated who took part in the field works. I would also like to thank Ercan Ozcan, Fuzuli Yagmurlu, Torsten Utescher, Volker Wilde and associate editor, Boris Natalin, for their reviews. Comments and useful criticism of these people helped improving an earlier version of this manuscript considerably.	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J	Ferrow, E; Vajda, V; Koch, CB; Peucker-Ehrenbrink, B; Willumsen, PS				Ferrow, Embaie; Vajda, Vivi; Koch, Christian Bender; Peucker-Ehrenbrink, Bernhard; Willumsen, Pi Suhr			Multiproxy analysis of a new terrestrial and a marine Cretaceous-Paleogene (K-Pg) boundary site from New Zealand	GEOCHIMICA ET COSMOCHIMICA ACTA			English	Article							MID-WAIPARA RIVER; X-RAY-DIFFRACTION; TERTIARY BOUNDARY; WOODSIDE-CREEK; PALEOENVIRONMENTAL CHANGES; MOSSBAUER-SPECTROSCOPY; ELEMENT CONCENTRATIONS; DINOFLAGELLATE CYST; CHICXULUB IMPACT; NORTH CANTERBURY	An integrated study of palynology, Mossbauer spectroscopy, mineralogy and osmium isotopes has led to the detection of the first K-Pg boundary clay layer in a Southern Hemisphere terrestrial setting. The K-Pg boundary layer was independently identified at centimetre resolution by all the above mentioned methods at the marine K-Pg boundary site of mid-Waipara and the terrestrial site of Compressor Creek (Greymouth coal field), New Zealand. Mossbauer spectroscopy shows an anomaly of Fe-containing particles in both K-Pg boundary sections: jarosite at mid-Waipara and goethite at Compressor Creek. This anomaly coincides with a turnover in vegetation indicated by an interval dominated by fern spores and extinction of key pollen species in both sections. In addition to the terrestrial floristic changes, the mid-Waipara section reveals a turnover in the dinoflagellate assemblages and the appearance of global earliest Danian index species. Geochemical data reveal relatively small iridium enrichments in the boundary layers of 321 pg/g at mid-Waipara and 176 pg/g at Compressor Creek. Unradiogenic Os-187/Os-188 values of the boundary clay reveal the presence of a significant extraterrestrial component. We interpret the accumulation of Fe nano-phases at the boundary as originating from both the impactor and the crystalline basement target rock. The goethite and jarosite are interpreted as secondary phases formed by weathering and diagenesis. The primary phases were probably controlled by the initial composition of the vapor plume and condensation kinetics rather than condensation thermodynamics. This investigation indicates that identification of Fe in nano-phases by Mossbauer spectroscopy is an accurate and cost-effective method for identifying impact event horizons and it efficiently complements widely used biostratigraphic and geochemical methods. (C) 2010 Elsevier Ltd. All rights reserved.	[Ferrow, Embaie; Vajda, Vivi; Willumsen, Pi Suhr] Lund Univ, Dept Earth & Ecosyst Sci, S-22362 Lund, Sweden; [Vajda, Vivi] Univ Copenhagen, Dept Basic Sci & Environm, DK-1871 Frederiksberg C, Denmark; [Peucker-Ehrenbrink, Bernhard] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA	Lund University; University of Copenhagen; Woods Hole Oceanographic Institution	Vajda, V (通讯作者)，Lund Univ, Dept Earth & Ecosyst Sci, Solvegatan 12, S-22362 Lund, Sweden.	vivi.vajda@geol.lu.se	Vajda, Vivi/N-7693-2018; Koch, Christian Bender/C-7070-2013	Vajda, Vivi/0000-0003-2987-5559; Peucker-Ehrenbrink, Bernhard/0000-0002-3819-992X; Koch, Christian Bender/0000-0002-7496-297X	NSF; Swedish Royal Academy of Sciences through the Knut & Alice Wallenbergs Foundation; Crafoord Foundation; Carlsberg Foundation [2008_01_0404]; Centre for Studies of Carbon Cycle and Climate interactions (LUCCI), Lund University	NSF(National Science Foundation (NSF)); Swedish Royal Academy of Sciences through the Knut & Alice Wallenbergs Foundation; Crafoord Foundation; Carlsberg Foundation(Carlsberg Foundation); Centre for Studies of Carbon Cycle and Climate interactions (LUCCI), Lund University	We thank the reviewers David Kring (LPI) and Peter Schulte (Erlangen University) and associate editor Uwe Reimold for their constructive criticism and comments that significantly improved this paper. We thank Rob Boyd and Solid Minerals for giving us access to their property, Ian Raine for assistance in the field, and John Simes and Christopher Hollis for providing samples from mid-Waipara. Tracy Atwood and Jerzy Blusztajn helped with the PGE and Os isotope analyses that were carried out in the NSF-supported WHOI ICPMS Facility. E. Ferrow acknowledges the support rendered by Berhane Habtemariam, the general manager of Enamco, during the final review of the paper. V. Vajda acknowledges the financial support provided by the Swedish Royal Academy of Sciences through the Knut & Alice Wallenbergs Foundation and from the Crafoord Foundation. P.S. Willumsen acknowledges financial support from the Carlsberg Foundation No. 2008_01_0404 and from the Centre for Studies of Carbon Cycle and Climate interactions (LUCCI), Lund University.	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J	Bosboom, RE; Dupont-Nivet, G; Houben, AJP; Brinkhuis, H; Villa, G; Mandic, O; Stoica, M; Zachariasse, WJ; Guo, ZJ; Li, CX; Krijgsman, W				Bosboom, Roderic E.; Dupont-Nivet, Guillaume; Houben, Alexander J. P.; Brinkhuis, Henk; Villa, Giuliana; Mandic, Oleg; Stoica, Marius; Zachariasse, Willem Jan; Guo, ZhaoJie; Li, ChuanXin; Krijgsman, Wout			Late Eocene sea retreat from the Tarim Basin (west China) and concomitant Asian paleoenvironmental change	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Tarim Basin; Paratethys; Paleoenvironment; Biostratigraphy; Eocene	OLIGOCENE DINOFLAGELLATE CYSTS; NORTHERN TIBETAN PLATEAU; NORTHEASTERN TIBET; TIAN-SHAN; CLIMATE; TRANSITION; UPLIFT; EVOLUTION; MONSOON; RECORDS	The Paleogene sediments of the southwest Tarim Basin along the West Kunlun Shan in western China include the remnants of the easternmost extent of a large epicontinental sea. This shallow sea once extended across the Eurasian continent before it retreated westward and eventually separated as the Paratethys Sea. Climate modeling results suggest that this sea retreat is an equally important forcing mechanism as the Tibetan plateau uplift in the aridification of the Asian continental interior and the intensification of the Asian monsoon system. The age and paleogeography of the retreat are poorly constrained, hindering the understanding of its cause and paleoenvironmental impacts. This study reports litho- and biostratigraphic results from two sections recording the last major regression out of the Tarim Basin that is expressed by a regional transition from marine clastics and limestones to continental red-beds. Rich micro- and macrofossil assemblages, including benthic foraminifera, ostracods, bivalves, calcareous nannofossils and organic walled dinoflagellate cysts (dinocysts), indicate a shallow, proximal and marine environment. Strong similarity to assemblages known from Central Asia and Europe confirms that surface-ocean connections extended across Eurasia from the Tarim Basin to the western Tethys during the latest Eocene. Moreover, the recovered fossil associations date the last marine sediments as earliest Priabonian in age (similar to 37 Ma: overlap between dinoflagellate Mps Interval Zone and calcareous nannofossil Zone CP 14). The retreat of the sea from the Tarim Basin is time-equivalent with the sea level lowstand at the Bartonian-Priabonian boundary but pre-dates both the Oligocene-Miocene regional uplift of the Pamir mountains and Kunlun Shan and the major eustatic sea-level falls of the Eocene-Oligocene Transition (similar to 34 Ma) and mid-Oligocene (similar to 30 Ma), which are usually held responsible for the sea retreat. Furthermore, a concomitant and significant aridification step occurs at similar to 36.6 Ma (top of chron C17n.1n) as recorded by regional sedimentary records of the Xining Basin along the northeastern Tibetan Plateau, suggesting that the Tarim Sea served as a significant moisture contributor for the Asian interior. (c) 2010 Elsevier B.V. All rights reserved.	[Bosboom, Roderic E.; Dupont-Nivet, Guillaume; Krijgsman, Wout] Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, NL-3584 CD Utrecht, Netherlands; [Dupont-Nivet, Guillaume; Guo, ZhaoJie; Li, ChuanXin] Peking Univ, Minist Educ, Key Lab Orogen Belts & Crustal Evolut, Beijing 100871, Peoples R China; [Dupont-Nivet, Guillaume] Univ Rennes 1, UMR 6118, F-35042 Rennes, France; [Houben, Alexander J. P.; Brinkhuis, Henk] Univ Utrecht, Fac Sci, Inst Environm Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Villa, Giuliana] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy; [Mandic, Oleg] Nat Hist Museum Vienna, Geol Palaeontol Dept, A-1010 Vienna, Austria; [Stoica, Marius] Univ Bucharest, Fac Geol & Geophys, Dept Geol & Paleontol, Bucharest 010041, Romania; [Zachariasse, Willem Jan] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; Peking University; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Rennes; Utrecht University; University of Parma; University of Bucharest; Utrecht University	Bosboom, RE (通讯作者)，Univ Utrecht, Fac Geosci, Paleomagnet Lab Ft Hoofddijk, Budapestlaan 17, NL-3584 CD Utrecht, Netherlands.	R.E.Bosboom@geo.uu.nl	Stoica, Marius/N-4941-2018; Dupont-Nivet, Guillaume/HII-9066-2022; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610; Krijgsman, Wout/0000-0002-1472-1074; Mandic, Oleg/0000-0003-1955-7514; Stoica, Marius/0000-0003-0126-4270; Dupont-Nivet, Guillaume/0000-0001-9905-9739; Houben, Alexander/0000-0002-9497-1048	Molengraaff Fund; Netherlands Organization for Scientific Research (NWO); Statoil	Molengraaff Fund; Netherlands Organization for Scientific Research (NWO)(Netherlands Organization for Scientific Research (NWO)); Statoil	The authors would like to thank Jan van Tongeren for his laboratory assistance and Cor Langereis for his valuable advice and field assistance. This research would not have been possible without funding from the Molengraaff Fund, the Netherlands Organization for Scientific Research (NWO) and Statoil.	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JAN 15	2011	299	3-4					385	398		10.1016/j.palaeo.2010.11.019	http://dx.doi.org/10.1016/j.palaeo.2010.11.019			14	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	717PA					2025-03-11	WOS:000287058700001
S	Tantawy, AA		Keller, G; Adatte, T		Tantawy, Abdel Aziz			CALCAREOUS NANNOFOSSILS ACROSS THE CRETACEOUS-TERTIARY BOUNDARY AT BRAZOS, TEXAS, USA: EXTINCTION AND SURVIVORSHIP, BIOSTRATIGRAPHY, AND PALEOECOLOGY	END-CRETACEOUS MASS EXTINCTION AND THE CHICXULUB IMPACT IN TEXAS	Society for Sedimentary Geology Special Publication		English	Article; Book Chapter						Nannofossils; KT Extinction; Survivorship; Paleoecology; Biostratigraphy; Brazos River; Texas	K-T BOUNDARY; CHICXULUB IMPACT; MASS EXTINCTION; ENVIRONMENTAL-CHANGES; PALEOGENE BOUNDARY; K/T BOUNDARY; ATLANTIC; STRATIGRAPHY; RIVER; PALEOENVIRONMENT	Brazos River sections from Falls County, Texas, U.S.A., provide an excellent opportunity for studying the Cretaceous Tertiary (KT) transition in an expanded sedimentary record that also contains a sandstone complex with Chicxulub impact spherules at the base, which have previously been interpreted as evidence of an impact-generated tsunami at the KT boundary. This study quantifies the calcareous nannofossil assemblages to determine the environmental and ecological changes across the KT transition in a new core Mullinax-3 and three Cottonmouth Creek outcrops. Abundance and diversity of calcareous nannofossils provide evidence of the changing environmental conditions and reveal a sequence of vanishing species, survivors, and the subsequent recovery across the KT boundary. Cretaceous assemblages are dominated by high abundance of dissolution-resistant M. decussate reflecting periods of high-stress environmental conditions prior to the KT boundary. Most Cretaceous taxa disappeared well above the sandstone complex and at the level synchronous with the mass extinction of planktic foraminifera. In addition, a progressive decline in the calcareous nannofossils is recorded in the uppermost Maastrichtian similar to 25 cm above the sandstone complex and 12 cm below the KT boundary. The KT boundary is marked by an important decrease in absolute abundance of calcareous nannofossils, the blooms of the dinoflagellate cysts of Thoracosphaera operculata and the opportunistic survivor Braarudosphaera bigelowd, and the appearance of new Paleocene taxa. These micropaleontological data confirm that the Chicxulub impact predated the KT boundary, consistent with earlier observations in northeastern Mexico and the Chicxulub crater core Yaxcopoil-1. Correlation of selected nannofossil taxa from the Brazos sections with those from various onshore marine and deep-sea sections provides insights into their paleoenvironmental and paleoecological affinities.	S Valley Univ, Aswan Fac Sci, Dept Geol, Aswan 81528, Egypt	Egyptian Knowledge Bank (EKB); South Valley University Egypt; Aswan University	Tantawy, AA (通讯作者)，S Valley Univ, Aswan Fac Sci, Dept Geol, Aswan 81528, Egypt.	aatantawy@yahoo.com						ADATTE T., 1996, CRETACEOUS TERTIARY, P197; 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], CREATACEOUS TERTARY; [Anonymous], J GEOL SOC LOND, DOI DOI 10.1017/S0016756812001069; [Anonymous], P ODP SCI RES; Arenillas I, 2000, MICROPALEONTOLOGY, V46, P31; BARRERA E, 1994, GEOL SOC AM BULL, V106, P1254, DOI 10.1130/0016-7606(1994)106<1254:PATCTB>2.3.CO;2; BARRERA E, 1994, GEOLOGY, V22, P877, DOI 10.1130/0091-7613(1994)022<0877:GECPTC>2.3.CO;2; BERGER WH, 1979, NATURWISSENSCHAFTEN, V66, P46, DOI 10.1007/BF00369357; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Bernaola G, 2007, PALAEOGEOGR PALAEOCL, V255, P132, DOI 10.1016/j.palaeo.2007.02.045; BOURGEOIS J, 1988, SCIENCE, V241, P567, DOI 10.1126/science.241.4865.567; Bukry D., 1973, Initial Rep Deep Sea Drilling Project, V21, P885; Bukry D., 1974, The Black Sea-Geology, Chemistry and Biology, V20, P353; Burnett J.A., 1998, P132; Caron M., 1985, P17; Cepek P., 1969, Transactions of the Gulf Coast Association of Geological Societies, V19, P323; COURTILLOT V, 1986, EARTH PLANET SC LETT, V80, P361, DOI 10.1016/0012-821X(86)90118-4; DOEVEN PH, 1983, GEOLOGICAL SURVEY CA, V356; ERBA E, 1992, PALAEOGEOGR PALAEOCL, V93, P47, DOI 10.1016/0031-0182(92)90183-6; Erba Elisabetta, 1995, Proceedings of the Ocean Drilling Program Scientific Results, V144, P141; ESHET Y, 1992, MAR MICROPALEONTOL, V18, P199, DOI 10.1016/0377-8398(92)90013-A; Eshet Y, 1996, MAR MICROPALEONTOL, V29, P37, DOI 10.1016/0377-8398(96)00006-0; FARIS M., 1995, GEOLOGICAL SURVEY EG, V20, P585; Gale A., 2006, Proceedings of the Geologists' Association, V117, P1; Gardin S, 2002, PALAEOGEOGR PALAEOCL, V178, P211, DOI 10.1016/S0031-0182(01)00397-2; Gardin S, 1998, B SOC GEOL FR, V169, P709; GIRGIS MH, 1989, BR MICROPAL, P327; Hallam A, 1999, EARTH-SCI REV, V48, P217, DOI 10.1016/S0012-8252(99)00055-0; HANSEN T, 1987, Cretaceous Research, V8, P229, DOI 10.1016/0195-6671(87)90023-1; HANSEN TA, 1993, PALEOBIOLOGY, V19, P251, DOI 10.1017/S0094837300015906; HAY WILLIAM W., 1967, J PALEONTOL, V41, P1505; Henriksson Anders S., 1998, Studia Geologica Salmanticensia, V33, P17; Herrle JO, 2003, TERRA NOVA, V15, P14, DOI 10.1046/j.1365-3121.2003.00448.x; Heymann D, 1998, GEOCHIM COSMOCHIM AC, V62, P173, DOI 10.1016/S0016-7037(97)00330-X; HILDEBRAND AR, 1991, GEOLOGY, V19, P867, DOI 10.1130/0091-7613(1991)019<0867:CCAPCT>2.3.CO;2; Hill M.E. 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S	Levac, E; Lewis, CFM; Miller, AAL		Rashid, H; Polyak, L; MosleyThompson, E		Levac, Elisabeth; Lewis, C. F. M.; Miller, A. A. L.			The Impact of the Final Lake Agassiz Flood Recorded in Northeast Newfoundland and Northern Scotian Shelves Based on Century-Scale Palynological Data	ABRUPT CLIMATE CHANGE: MECHANISMS, PATTERNS, AND IMPACTS	Geophysical Monograph Book Series		English	Article; Book Chapter							SEA-SURFACE CONDITIONS; CATASTROPHIC DRAINAGE; DINOFLAGELLATE CYSTS; CONTINENTAL-MARGIN; LABRADOR SEA; ST-LAWRENCE; NOVA-SCOTIA; COLD EVENT; HOLOCENE; POLLEN	Two high-resolution century-scale palynological records from the eastern Canadian margin were analyzed to estimate the impact of Lake Agassiz's final drainage at circa 8.3 ka on sea surface conditions and to track the path of the meltwater plume. Core HU87033-19 from Notre Dame Channel on Northeast Newfoundland Shelf contains four distinct detrital carbonate (DC) beds, known to be sediment transported from Hudson Strait and Hudson Bay, and one layer is coeval with the drainage of Lake Agassiz. Within that DC layer, significant changes in dinoflagellate cyst assemblages indicate lower sea surface temperatures and salinity. The drop in salinity is a doublet, suggesting two episodes of meltwater drainage. Core HU84011-12, from St. Anne's Basin, on the northern Scotian Shelf contains similar changes in dinoflagellate cyst assemblages at the time of the drainage, indicating sea surface cooling accompanied by a slight decrease in salinity. The impact of the meltwater was greater in the Notre Dame Channel This suggests that most of the meltwater from the final drainages of Lake Agassiz flowed south over the Labrador and Northeast Newfoundland shelves and was not dispersed directly into the Labrador Sea. Instead, it was possibly dispersed into the slope water system and subsequently into the North Atlantic after flowing initially over the continental shelf. This is the first paper describing paleoecological data indicating the presence of the Agassiz meltwater along the eastern Canadian margin.	[Levac, Elisabeth] Bishops Univ, Coll 2600, Sherbrooke, PQ J1M 1Z7, Canada; [Lewis, C. F. M.] Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Miller, A. A. 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B	Bohaty, SM; Kulhanek, DK; Wise, SW; Jemison, K; Warny, S; Sjunneskog, C		Anderson, JB; Wellner, JS		Bohaty, Steven M.; Kulhanek, Denise K.; Wise, Sherwood W., Jr.; Jemison, Kelly; Warny, Sophie; Sjunneskog, Charlotte			Age Assessment of Eocene-Pliocene Drill Cores Recovered During the SHALDRIL II Expedition, Antarctic Peninsula	TECTONIC, CLIMATIC, AND CRYOSPHERIC EVOLUTION OF THE ANTARCTIC PENINSULA	American Geophysical Union Special Publications		English	Article; Book Chapter							SHEET GROUNDING EVENTS; ICE-SHEET; DIATOM BIOSTRATIGRAPHY; SEA-ICE; KERGUELEN PLATEAU; SORSDAL FORMATION; FALKLAND PLATEAU; ATLANTIC SECTOR; PROJECT LEG-71; VESTFOLD HILLS	Pre-Quaternary strata were recovered from four sites on the continental shelf of the eastern Antarctic Peninsula during the SHALDRIL II cruise, NBP0602A (March-April 2006). Fully marine shelf sediments characterize these short cores and contain a mixture of opaline, carbonate-walled, and organic-walled microfossils, suitable for both biostratigraphic and paleoenvironmental studies. Here we compile biostratigraphic information and provide age assessments for the Eocene-Pliocene intervals of these cores, based primarily on diatom biostratigraphy with additional constraints from calcareous nannofossil and dinoflagellate cyst biostratigraphy and strontium isotope dating. The Eocene and Oligocene diatom floras are illustrated in nine figures. A late Eocene age (similar to 37-34 Ma) is assigned to strata recovered in Hole 3C, and a late Oligocene age (similar to 28.4-23.3 Ma) is determined for strata recovered in Hole 12A. Middle Miocene (similar to 12.8-11.7 Ma) and early Pliocene (similar to 5.1-4.3 Ma) ages are assigned to the sequence recovered in holes 5C and 5D, and an early Pliocene age (similar to 5.1-3.8 Ma) is interpreted for cores recovered in holes 6C and 6D. These ages provide chronostratigraphic ground truthing for the thick sequences of Paleogene and Neogene strata present on the northwestern edge of the James Ross Basin and on the northeastern side of the Joinville Plateau, as interpreted from a network of seismic stratigraphic survey lines in the drilling areas. Although representing a coarse-resolution sampling of the complete sedimentary package, the well-constrained ages for these cores also allow for the broad reconstruction of marine and terrestrial paleoenvironments in the Antarctic Peninsula for the late Eocene-to-early Pliocene time interval.	[Bohaty, Steven M.] Univ Calif Santa Cruz, Earth & Planetary Sci Dept, Santa Cruz, CA 95064 USA; [Kulhanek, Denise K.; Wise, Sherwood W., Jr.; Jemison, Kelly] Florida State Univ, Dept Earth Ocean & Atmospher Sci, Tallahassee, FL 32306 USA; [Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Sjunneskog, Charlotte] Florida State Univ, Antarctic Res Facil, Tallahassee, FL 32306 USA	University of California System; University of California Santa Cruz; State University System of Florida; Florida State University; Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; State University System of Florida; Florida State University	Bohaty, SM (通讯作者)，Univ Southampton, Natl Oceanog Ctr, Sch Ocean & Earth Sci, European Way, Southampton SO14 3ZH, Hants, England.	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L., 2004, P OCEAN DRILL PROGRA, V189; Williams M, 2010, PALAEOGEOGR PALAEOCL, V292, P306, DOI 10.1016/j.palaeo.2010.04.003; Wilson GS, 2002, GEOLOGY, V30, P1043, DOI 10.1130/0091-7613(2002)030<1043:ICCOTO>2.0.CO;2; Wilson GS., 2000, Terra Antartica, V7, P647; Winter D, 2012, GLOBAL PLANET CHANGE, V96-97, P59, DOI 10.1016/j.gloplacha.2010.04.004; WINTER D, 2002, P OCEAN DRILL PROGRA, V178; Winter D.M., 1997, The Antarctic Region: Geological Evolution and Processes, P985; WISE SW, 1983, INITIAL REP DEEP SEA, V71, P481; Zielinski U, 2002, MAR MICROPALEONTOL, V45, P225, DOI 10.1016/S0377-8398(02)00031-2; Zielinski U, 2002, MAR MICROPALEONTOL, V46, P127, DOI 10.1016/S0377-8398(02)00042-7	115	17	18	0	1	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA			978-0-87590-734-5	AM GEOPHYS UNION SP			2011	63						63	113		10.1029/2010SP001049	http://dx.doi.org/10.1029/2010SP001049	10.1029/SP063		51	Geology	Book Citation Index– Science (BKCI-S)	Geology	BYW62					2025-03-11	WOS:000300647100005
B	Warny, S; Askin, R		Anderson, JB; Wellner, JS		Warny, Sophie; Askin, Rosemary			Last Remnants of Cenozoic Vegetation and Organic-Walled Phytoplankton in the Antarctic Peninsula's Icehouse World	TECTONIC, CLIMATIC, AND CRYOSPHERIC EVOLUTION OF THE ANTARCTIC PENINSULA	American Geophysical Union Special Publications		English	Article; Book Chapter							SHEET GROUNDING EVENTS; MA; PALYNOMORPHS; PALYNOLOGY; OLIGOCENE; ISLANDS; SEA	A late Oligocene, a middle Miocene, and two adjacent Pliocene sections were sampled off the coast of the Antarctic Peninsula in shelf sediments on the Joinville Plateau, Weddell Sea. Drilling was conducted from the research vessel icebreaker Nathaniel B. Palmer during the 2006 SHALDRIL campaign. The drill holes recovered sediment cores that each span a short interval of time because of extensive sea ice constraints during drilling. Despite this limitation, the palynomorphs extracted from these sediments help constrain the region's past environmental conditions during three periods of the "icehouse" world and confirm that tundra vegetation persisted in the Antarctic Peninsula up to at least 12.8 Ma. The terrestrial palynological data reflect southern beech and conifer-dominated woodlands and tundra during the Oligocene, with reduction to pockets of tundra with probably stunted beech and podocarp conifers by the middle Miocene. During both the Oligocene and the Miocene, the phytoplankton were dominated by small sea ice-tolerant opportunistic species taking advantage of the migration of most dinoflagellate cysts to more hospitable parts of the ocean. By the Pliocene, only limited pockets of vegetation may have existed.	[Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University	Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	Directorate For Geosciences; Office of Polar Programs (OPP) [1048343] Funding Source: National Science Foundation	Directorate For Geosciences; Office of Polar Programs (OPP)(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))		Anderson JB, 2011, P NATL ACAD SCI USA, V108, P11356, DOI 10.1073/pnas.1014885108; [Anonymous], 2008, TERRA ANTARTICA, V15, P113; ASKIN R A, 1981, Antarctic Journal of the United States, V16, P11; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R A., 2000, Terra Antarctica, V7, P493; Askin R.A., 1997, The Antarctic Region: Geological Evolution Proceedings, P993; Askin R A., 1983, Antarctic Earth Science, P295; ASKIN RA, 1982, GEOLOGY, V10, P547, DOI 10.1130/0091-7613(1982)10<547:GIORPA>2.0.CO;2; Bart PJ, 2007, MAR GEOL, V236, P1, DOI 10.1016/j.margeo.2006.09.008; Bart P.J., 1995, GEOLOGY SEISMIC STRA, V68, P75; Bart PJ, 2005, J GEOPHYS RES-EARTH, V110, DOI 10.1029/2004JF000254; Bart PJ, 2000, EARTH PLANET SC LETT, V182, P259, DOI 10.1016/S0012-821X(00)00257-0; BIRKENMAJER K, 1996, B POL ACAD SCI-EARTH, V44, P157; Bohaty SM, 2011, AM GEOPHYS UNION SP, V63, P63, DOI 10.1029/2010SP001049; Dingle RV, 1998, J GEOL SOC LONDON, V155, P433, DOI 10.1144/gsjgs.155.3.0433; Duane AM, 1996, REV PALAEOBOT PALYNO, V91, P241, DOI 10.1016/0034-6667(95)00094-1; Grey K, 2003, GEOLOGY, V31, P459, DOI 10.1130/0091-7613(2003)031<0459:NBDSEO>2.0.CO;2; Lewis AR, 2008, P NATL ACAD SCI USA, V105, P10676, DOI 10.1073/pnas.0802501105; MAO S, 1995, REV PALAEOBOT PALYNO, V86, P235, DOI 10.1016/0034-6667(94)00138-A; Marchant D., 2009, 1 ANT CLIM EV S ANT; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Raine J.I., 2001, TERRA ANTARTICA, V7, P389; Raine J.I., 1998, Terra Antarctica, V5, P539; Smith RT, 2011, AM GEOPHYS UNION SP, V63, P51, DOI 10.1029/2010SP000980; Thorn VC, 2009, REV PALAEOBOT PALYNO, V156, P436, DOI 10.1016/j.revpalbo.2009.04.009; Troedson AL, 2002, J SEDIMENT RES, V72, P510, DOI 10.1306/110601720510; Warny S., 2007, ANTARCTICA KEYSTONE, DOI [10.3133/of2007-1047.srp079, DOI 10.3133/OF2007-1047.SRP079]; Warny S, 2006, PALYNOLOGY, V30, P151; Warny S, 2011, AM GEOPHYS UNION SP, V63, P193, DOI 10.1029/2010SP000965; Warny S, 2009, GEOLOGY, V37, P955, DOI 10.1130/G30139A.1; Wellner JS, 2011, AM GEOPHYS UNION SP, V63, P131, DOI 10.1029/2010SP001047; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zhou CM, 2007, GEOL J, V42, P229, DOI 10.1002/gj.1062	34	18	23	0	3	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA			978-0-87590-734-5	AM GEOPHYS UNION SP			2011	63						167	192		10.1029/2010SP000996	http://dx.doi.org/10.1029/2010SP000996	10.1029/SP063		26	Geology	Book Citation Index– Science (BKCI-S)	Geology	BYW62					2025-03-11	WOS:000300647100009
B	Warny, S; Askin, R		Anderson, JB; Wellner, JS		Warny, Sophie; Askin, Rosemary			Vegetation and Organic-Walled Phytoplankton at the End of the Antarctic Greenhouse World: Latest Eocene Cooling Events	TECTONIC, CLIMATIC, AND CRYOSPHERIC EVOLUTION OF THE ANTARCTIC PENINSULA	American Geophysical Union Special Publications		English	Article; Book Chapter							SEYMOUR ISLAND; PALYNOMORPHS; GLACIATION; CARBON; SEA	The NBP0602A-3C SHALDRIL section collected in the Weddell Sea recovered a key stratigraphic interval that captured the response of plants and organic-walled phytoplankton during the first marked increase in delta O-18 followed by the large reduction in atmospheric CO2 in the late Eocene around 36 Ma. Well-preserved palynomorphs recovered from in situ shelf sediments provide evidence of a cooling event followed by a marked sea level drop around 36 Ma. Terrestrial palynomorphs indicate that at the time of deposition, southern beech-dominated and conifer forest vegetation was abundant but with lower diversity and signifying colder climates than for most of the La Meseta Formation on Seymour Island. The marine palynomorph assemblage is dominated by Vozzhennikovia apertura. This low-diversity, high-dominance dinoflagellate cyst assemblage is also a sign of deteriorating conditions. Particularly notable is the marked increase in the uppermost Eocene samples of reworked dinoflagellates and acritarchs of Cretaceous age. This suggests significant erosion and redeposition of nearby Campanian-Maastrichtian sections during a marked drop in sea level. Based on the biostratigraphy and a single isotopic date, it is likely that the cooling and subsequent lowering of sea level can be correlated to the brief spike in delta O-18-enriched values shown by the Zachos et al. (2001) curve in the Priabonian. According to Zachos et al. (2008), this event occurs at a time when lowest carbon dioxide atmospheric concentrations were between 600 and 980 ppmv, giving us some perspectives as to what could be expected when the current CO2 atmospheric concentration is at least doubled.	[Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University	Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	Office of Polar Programs (OPP); Directorate For Geosciences [1048343] Funding Source: National Science Foundation	Office of Polar Programs (OPP); Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))		Anderson J.B., 1999, ANTARCTIC MARINE GEO; ANDERSON JB, 2006, EOS T AGU, V87, P402, DOI DOI 10.1029/2006EO390003; Anderson JB, 2011, P NATL ACAD SCI USA, V108, P11356, DOI 10.1073/pnas.1014885108; [Anonymous], 2001, TERRA ANTARTICA; [Anonymous], 2001, Terra Antartica, V8, P615; Askin R.A., 1988, Geological Society of America Memoir, V169, P131; Askin R A., 2000, Terra Antarctica, V7, P493; Askin R.A., 1997, The Antarctic Region: Geological Evolution Proceedings, P993; Askin RA, 1999, J PALEONTOL, V73, P373, DOI 10.1017/S0022336000027888; ASKIN RA, 1982, GEOLOGY, V10, P547, DOI 10.1130/0091-7613(1982)10<547:GIORPA>2.0.CO;2; Bohaty SM, 2011, AM GEOPHYS UNION SP, V63, P63, DOI 10.1029/2010SP001049; Brinkhuis H., 2003, P OCEAN DRILL PROGRA, V189; Brown C.A., 2008, Palynological Techniques, VSecond; Chen B., 2000, THESIS OHIO STATE U; COCOZZA CD, 1992, ANTARCT SCI, V4, P355, DOI 10.1017/S0954102092000506; DeConto RM, 2003, NATURE, V421, P245, DOI 10.1038/nature01290; Diester-Haass L., 2003, GREENHOUSE ICEHOUSE, P397; Francis JE, 2009, DEV EARTH ENV SCI, V8, P309, DOI 10.1016/S1571-9197(08)00008-6; Francis J.E., 2008, ANTARCTICA KEYSTONE, P19, DOI DOI 10.3133/OF2007-1047; HALL SA, 1977, NATURE, V267, P239, DOI 10.1038/267239a0; Hannah M. 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L., 2003, P OCEAN DRILL PROGRA, V189; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321; WRENN JH, 1982, SCIENCE, V216, P187, DOI 10.1126/science.216.4542.187; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588	38	21	30	0	3	AMER GEOPHYSICAL UNION	WASHINGTON	2000 FLORIDA AVE NW, WASHINGTON, DC 20009 USA			978-0-87590-734-5	AM GEOPHYS UNION SP			2011	63						193	210		10.1029/2010SP000965	http://dx.doi.org/10.1029/2010SP000965	10.1029/SP063		18	Geology	Book Citation Index– Science (BKCI-S)	Geology	BYW62					2025-03-11	WOS:000300647100010
J	Gedl, P; Peryt, D				Gedl, Przemyslaw; Peryt, Danuta			DINOFLAGELLATE CYST, PALYNOFACIES AND FORAMINIFERAL RECORDS OF ENVIRONMENTAL CHANGES RELATED TO THE LATE BADENIAN (MIDDLE MIOCENE) TRANSGRESSION AT KUDRYNTSI (WESTERN UKRAINE)	ANNALES SOCIETATIS GEOLOGORUM POLONIAE			English	Article						palaeoenvironment; dinoflagellate cysts; foraminifers; Upper Badenian; Middle Miocene; Paratethys; Carpathian Foredeep	CENTRAL PARATETHYS; SALINITY CRISIS; SEDIMENTS; DEPOSITS; NORTH; PRESERVATION; ASSEMBLAGES; MARINE; BASIN; SEA	Qualitative and quantitative characteristics of the palynological content of the Upper Badenian strata at Kudryntsi (western Ukraine) indicate that this succession was deposited in variable environments. The basal siliciclastic series Shows a very low content of palynological organic matter and palynofacies, which indicate a restricted environment and/or unfavourable conditions for the palynomorph preservation. The presence of dinoflagellate cysts (and composition of their assemblages) in the upper part of organodetrital limestones and the overlying rhodoid limestones indicates a typical shelf environment. Taxonomically variable dinoflagellate cyst assemblages from particular samples reflect gradual environmental changes from environments of slightly increased salinity of seawater (strata overlying the siliciclastic series) to open marine, more remote environments during deposition of the upper part of the section examined. The gradual deepening of the sea and decrease of salinity is supported also by the succession of foraminiferal assemblages, which undergo gradual changes from Elphidium spp. assemblages, through Miliolidae assemblage, Lobatula lobatula assemblage, Neoconorbina spp. assemblage to Cibicidoides assemblage. The Late Badenian foraminiferal assemblage from Kudryntsi contains two species common for the Sarmatian, i.e. Elphidium reginum and Elphidium koberi, the latter species known so far from the Sarmatian.	[Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland; [Peryt, Danuta] Polish Acad Sci, Inst Paleobiol, PL-00818 Warsaw, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences; Institute of Paleobiology 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; d.peryt@twarda.pan.pl	Peryt, Danuta/F-9988-2019	Peryt, Danuta/0000-0002-5821-1084	Ministry of Science and Higher Education [UKRAINA/193/2006]	Ministry of Science and Higher Education	We would like to thank Barbara Slodkowska for reading the manuscript and critical remarks. Special thanks are due to Mathias Harzhauser for his helpful comments and inspiring suggestions. The research was undertaken as a research project No. UKRAINA/193/2006 of the Ministry of Science and Higher Education carried out at the AGH University of Science and Technology and the Polish Geological Institute - National Research Institute and was financed from the scientific fund of 2007-2010. We thank Zofia Dubicka for the field assistance.	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Pol.		2011	81	3					331	349						19	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	884IW					2025-03-11	WOS:000299699100007
J	Azar, D; Dejax, J; Masure, E				Azar, Dany; Dejax, Jean; Masure, Edwige			Palynological Analysis of Amber-Bearing Clay from the Lower Cretaceous of Central Lebanon	ACTA GEOLOGICA SINICA-ENGLISH EDITION			English	Article						amber; palynology; Lower Cretaceous; Lebanon	MOUNT HERMON; POLLEN	An amber-bearing lignitic layer of sandy clay from the Lower Cretaceous of Central Lebanon (Mderej-Hammana) yielded a well-preserved, moderately variegated palynoflora, which origin is mixed between land plants and marine microflora. Its detailed analysis led to fulfill its inventory, to propose a paleoenvironmental reconstruction, and to draw the paleoclimate which prevailed over the region: an estuarian area under a rather humid, temperate climate; a variety of ferns grew near the shore-side and in the inward land. A tiny piece of amber containing angiospermous pollen grains of stratigraphical interest allows a precise dating. The marine microflora, poorly diversified, includes chitinous foraminifer linings and dinoflagellate cysts, among which Early Aptian guide taxa are present; their occurrence slightly narrows the stratigraphical range indicated by some palynological taxa which are related to land plants.	[Dejax, Jean] Museum Natl Hist Nat, UMR CNRS 7207, CR2P, Dept Hist Terre, F-75231 Paris 05, France; [Azar, Dany] Lebanese Univ, Fac Sci 2, Dept Nat Sci, Fanar Matn, Lebanon; [Masure, Edwige] Univ Paris 06, UMR CNRS 7207, CR2P, F-75005 Paris, France	Museum National d'Histoire Naturelle (MNHN); Sorbonne Universite; Lebanese University; Sorbonne Universite	Dejax, J (通讯作者)，Museum Natl Hist Nat, UMR CNRS 7207, CR2P, Dept Hist Terre, CP 38,57 Rue Cuvier, F-75231 Paris 05, France.	dejax@mnhn.fr	Azar, Dany/AAF-7387-2020		Lebanese University	Lebanese University(Lebanese University)	We thank the unknown reviewers for their helpful remarks on an older version of the manuscript. This paper is a contribution to the scientific project "The Study of the Fossil Insects in Lebanon and their Outcrops: Geology of the Outcrops - Historical and Biodiversity Evolution" and to the team project : "Biodiversity: Origin, Structure, Evolution and Geology" financed by the Lebanese University to the first author (DA).	BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; Brenner Gilbert J., 1992, Palynology, V16, P137; Brenner GJ, 1974, GEOLOGICAL SURVEY, V59, P1; Conway BH, 1996, CRETACEOUS RES, V17, P197, DOI 10.1006/cres.1996.0015; CONWAY BH, 1991, J AFR EARTH SCI, V13, P499, DOI 10.1016/0899-5362(91)90112-C; DAVEY R J, 1974, Palaeontology (Oxford), V17, P623; DEAK MH, 1964, B SOC GEOLOGIQUE HON, V94, P96; Dettmann M.E., 1963, Proc. R. Soc. Vic., V77, P1; Dubertret L., 1947, Bull. Soc. Geol. Fr, V5, P3; Dubertret L., 1975, NOTES M MOIRES MOYEN, V23, P345; Duxbury S., 1980, Palaeontographica Abteilung B Palaeophytologie, V173, P107; FENSOME RA, 2004, CONTRIBUTIONS SERIES, P909; Ferry Serge, 2007, Carnets de Geologie, P38; GOCHT H., 1959, PAL ONTOLOGISCHE Z, V33, P50; Herngreen GF., 1996, Palynology: Principles and Applications, V3, P1157; Ibrahim Mohamed I. A., 2002, Palynology, V26, P107, DOI 10.2113/0260107; Masure E., 1998, GEOLOGIE MEDITERRANE, V25, P263; MROUEH M, 1996, 8 ALL RUSS PAL C PAL, P91; Nohr-Hansen Henrik, 1993, Gronlands Geologiske Undersogelse Bulletin, V166, P1; PENNY J H J, 1991, Palaeontographica Abteilung B Palaeophytologie, V222, P31; POTONIE R., 1954, GEOL JAHRB, V69, P111; POTONTE R, 1970, BIEH GEOL JB, V87, P222; Schrank E, 2002, PALAEONTOLOGY, V45, P33, DOI 10.1111/1475-4983.00226; Smirnova SB, 2010, PALEONTOL J+, V44, P95, DOI 10.1134/S0031030110010132; SMIRNOVA SB, 1980, VOL RES 26 C GEOL IN, P183; SMIRNOVA SB, 1978, GEOLOGY MINERAL RESO, P83; SMIRNOVA SB, 1982, MOBIL ZONES SEDIMENT, P76; SRIVASTAVA SK, 1984, CAHIERS MICROPALEONT, V2, P3; WALLEY C.D., 1997, Lebanese Scientic Re-search Reports, V1, P81; WALLEY CD, 1983, GEOL RUNDSCH, V72, P377, DOI 10.1007/BF01765915; Williams G.L., 1985, P847; Zavialova NE, 2010, PALEONTOL J+, V44, P1353, DOI 10.1134/S0031030110100126	32	23	24	0	3	WILEY-BLACKWELL	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	1000-9515			ACTA GEOL SIN-ENGL	Acta Geol. Sin.-Engl. Ed.		2011	85	4					942	949		10.1111/j.1755-6724.2011.00497.x	http://dx.doi.org/10.1111/j.1755-6724.2011.00497.x			8	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	815JE					2025-03-11	WOS:000294521100020
J	Mohamed, ZA; Al-Shehri, AM				Mohamed, Zakaria A.; Al-Shehri, Abdulrahman M.			Occurrence and germination of dinoflagellate cysts in surface sediments from the Red Sea off the coasts of Saudi Arabia	OCEANOLOGIA			English	Article						Cyst; Dinoflagellates; Red Sea; Saudi Arabia; Toxic species	ALEXANDRIUM-CATENELLA DINOPHYCEAE; RECENT MARINE-SEDIMENTS; SHIPS BALLAST WATER; RESTING CYSTS; ONAGAWA BAY; WEST-COAST; BLOOM; SCRIPPSIELLA; DYNAMICS; ASSEMBLAGES	The distribution and abundance of dinoflagellate cyst assemblages were investigated in surface sediments from south-western Red sea coasts of Saudi Arabia at six sites during March 2010. A total of 19 taxa of dinoflagellate cysts were identified from all sites. The sampling sites showed a similar cyst assemblage, but they differed in total cyst abundance (3 to 4083 cysts g(-1) dry weight). Cyst abundance was strongly correlated with sediment characteristics, the highest numbers being recorded in sediments with large contents of organic carbon, silt and clay. Cyst assemblages were dominated by cysts of potentially toxic species, including Cochlodinium polykrikos, Prorocentrum minimum, Dinophysis acuminata, Alexandrium catenella and Scrippsiella trochoidea. Most cysts germinated successfully at different rates at 15 and 25 degrees C. This study suggests that surface sediments from all Saudi Red Sea coasts should be monitored for the presence of dinoffagellate cysts to give ample warning of the presence and abundance of toxic species in a. given area.	[Mohamed, Zakaria A.] Sohag Univ, Fac Sci, Dept Bot, Sohag 82524, Egypt; [Al-Shehri, Abdulrahman M.] King Khalid Univ, Coll Sci, Dept Biol, Abha 9019, Saudi Arabia	Egyptian Knowledge Bank (EKB); Sohag University; King Khalid University	Mohamed, ZA (通讯作者)，Sohag Univ, Fac Sci, Dept Bot, Sohag 82524, Egypt.	mzakaria_99@yahoo.com	AlShehri, Dhafer/B-5950-2015	Al-Shehri, Dhafer/0000-0002-7032-5199				Alves-De-Souza C, 2008, BOT MAR, V51, P399, DOI 10.1515/BOT.2008.052; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Dale B., 1983, P69; DALE B, 1978, Palynology, V2, P187; DALE B., 1994, CARBON CYCLING GLOBA, P521; de Vernal A, 2007, DEV MARINE GEOL, V1, P371, DOI 10.1016/S1572-5480(07)01014-7; El Wakeel S.K., 1957, J CONS INT EXPLOR ME, V22, P180, DOI 10.1093/icesjms/22.2.180; Fahnenstiel G, 2009, INT VER THEOR ANGEW, V30, P1035; FENSOME RA, 2004, SCOTIAN MARGIN PALYA; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; Folk R. 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J	Villac, MC; Kaczmarska, I				Villac, Maria Celia; Kaczmarska, Irena			Estimating propagule pressure and viability of diatoms detected in ballast tank sediments of ships arriving at Canadian ports	MARINE ECOLOGY PROGRESS SERIES			English	Article						Diatoms; Biological invasion; Ballast sediment; Propagule pressure; Phytoplankton viability	DINOFLAGELLATE CYSTS; BIOLOGICAL INVASIONS; MIDOCEAN EXCHANGE; GREAT-LAKES; CELL-DEATH; WATER; MARINE; PHYTOPLANKTON; TRANSPORT; COAST	This research uses the concept of propagule pressure (number of individuals introduced and number of introduction attempts) to investigate human-mediated bioinvasion patterns. We quantified diatoms in the sediments of ballast tanks of commercial ships arriving on both Canadian coasts during 2007 to 2009. Diatom cell concentrations varied from non-detected to 10(5) cells g(-1) wet weight (10(11) cells per tank). Although the lowest values were often found in tanks that underwent ballast water exchange, the highest concentrations (10(9) to 10(11) cells per tank) were detected in all voyage categories: transoceanic with ballast exchange (TOE), and intra-coastal with exchange (ICE) and without exchange (ICU). For the west coast, 36% of tanks carried detectable quantities of diatoms and there was no statistical difference between ship categories. For the east coast, 60% of tanks contained diatoms; ICU represented a bioinvasion pattern based on more frequent events with consistently lower cell concentrations, whereas ICE and TOE corresponded to less frequent events, though more variable in cell concentrations. Diversity reached 40 taxa per tank, including resting stages and cells that were supposedly growing vegetatively. New records may lead to introduction hypotheses that ought not to be accepted uncritically. Cell viability was tested using the vital stain fluorescein diacetate; parallel counts of protoplasm integrity and chlorophyll autofluorescence revealed that all 3 indicators gave results within the same order of magnitude. Inoculation of 0.2 to 0.5 ml of the slurry into culture media led to the growth of diatoms, even of taxa not initially detected. Within 7 d, cultured assemblages reached cell concentrations equivalent to 1.8 to 4.4 doublings of the original inoculation.	[Villac, Maria Celia; Kaczmarska, Irena] Mt Allison Univ, Dept Biol, Sackville, NB E4L 1G7, Canada	Mount Allison University	Villac, MC (通讯作者)，Mt Allison Univ, Dept Biol, 63B York St, Sackville, NB E4L 1G7, Canada.	celiavillac@gmail.com			Canadian Aquatic Invasive Species Network; Natural Sciences and Engineering Research Council of Canada	Canadian Aquatic Invasive Species Network; Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This research was supported by the Canadian Aquatic Invasive Species Network and the Natural Sciences and Engineering Research Council of Canada. We thank all individuals that were part of CAISN sampling teams on the west and east coasts, J. Ehrman for electron microscopy expertise, E. Briski for providing total sediment estimates for tanks and ships sampled, B. V. Lo for sharing unpublished material about shipping traffic and ballast water operations at Canadian ports, and 3 anonymous reviewers for good suggestions and constructive criticism. Participation of the shipping companies was greatly appreciated.	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Ecol.-Prog. Ser.		2011	425						47	U367		10.3354/meps08999	http://dx.doi.org/10.3354/meps08999			19	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	735GG		Bronze			2025-03-11	WOS:000288400800004
J	Holdgate, GR; Wagstaff, B; Gallagher, SJ				Holdgate, G. R.; Wagstaff, B.; Gallagher, S. J.			Did Port Phillip Bay nearly dry up between 2800 and 1000 cal. yr BP? Bay floor channelling evidence, seismic and core dating	AUSTRALIAN JOURNAL OF EARTH SCIENCES			English	Article						Port Phillip; marine geology; channels; Quaternary; Holocene	DINOFLAGELLATE CYST DISTRIBUTION; SEA-LEVEL CHANGE; DEPOSITIONAL-ENVIRONMENTS; NORTHWESTERN VICTORIA; EASTERN AUSTRALIA; LAKE TYRRELL; HOLOCENE; RECORD	Imagery of meandering river-like channel features up to 5 m deep and 100 m wide on the floor of Port Phillip Bay have been revealed by recent multibeam surveys. They are in water depths to -22 m below the present bay water level. This young channelling overlies older infilled Pleistocene-early Holocene channels considered to be cut by the Yarra and Werribee rivers during the last glacial or previous low stand minima 10 000 cal. yr BP and infilled during the Holocene transgression. Vibrocoring data indicate the young channels incise shelly mud. Twelve 14C shell dates in vibrocores from bay floor to 3.5 m are in two unitsa lower unit range between 2880 cal. yr BP at 0.7 m to 9491 cal. yr BP at 3.5 m, and an upper unit 0.5 to 0.7 m thick 869 cal. yr BP forming the present bay floor. Seismic and vibrocore evidence suggests the post-869 cal. yr BP upper unit also covers the base of the young channels. This evidence implies that Port Phillip dried out to -22 m between 2800 and 1000 cal. yr BP at a time of stable present day sea-levels. The most likely cause is a sand blockage to the Port Phillip Bay channel entrances, coupled with high evaporation rates. Palynological and foraminiferal evidence suggests variable salinities occurred immediately prior to the sedimentary hiatus, with restoration of marine conditions after. The results have wide implications on Port Phillip's water balance, salinity, pre-European climatic events and Aboriginal occupation.	[Holdgate, G. R.; Wagstaff, B.; Gallagher, S. J.] Univ Melbourne, Sch Earth Sci, Parkville, Vic 3010, Australia	University of Melbourne	Holdgate, GR (通讯作者)，Univ Melbourne, Sch Earth Sci, Parkville, Vic 3010, Australia.	grh@unimelb.edu.au	Gallagher, Stephen/AFL-9448-2022	Gallagher, Stephen/0000-0002-5593-2740				Ahmad R, 1996, GEOLOGY, V24, P619, DOI 10.1130/0091-7613(1996)024<0619:LHMAAP>2.3.CO;2; AITKEN DL, 1996, P ROYAL SOC VICT, V105, P67; [Anonymous], 1966, Memoirs of Museum Victoria, DOI DOI 10.24199/J.MMV.1966.27.03; Beardsell D., 1999, YARRA NATURAL TREASU; Beasley A.W., 1966, MEMOIRS NATL MUSEUM, V27, P69, DOI 10.24199/j.mmv.1966.27.04; BEASLEY AW, 1969, MEMOIRS NATL MUSEUM, V29, P1; BEASLEY AW, 1971, VICTORIAN NAT, V88, P291; BOWLER JM, 1981, HYDROBIOLOGIA, V82, P431, DOI DOI 10.1007/BF00048730; Brown R., 1814, A Voyage to Terra Australis, V2; BUCKLEY RW, 1987, 87815 MAR LAB PORT M; Clark I.D., 1990, Monash Publications in Geography, V37; Coulson A., 1935, Proceedings of the Royal Society of Victoria, V48, P1; COX HL, 1864, BATHYMETRIC NAVIGATI; *DCNR, 1995, NOT MUD ISL MAR RES; Dodson JR, 2001, HOLOCENE, V11, P673, DOI 10.1191/09596830195690; Duncan BD, 1994, FERNS ALLIED PLANTS; FELS MH, 2011, ABORIGINAL IN PRESS, V22; GILL E D, 1985, Proceedings of the Royal Society of Victoria, V97, P95; GILL E D, 1971, Proceedings of the Royal Society of Victoria, V84, P71; Gill E. 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Earth Sci.		2011	58	2					157	175	PII 933983498	10.1080/08120099.2011.546429	http://dx.doi.org/10.1080/08120099.2011.546429			19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	726GZ					2025-03-11	WOS:000287709500002
J	Attaran-Fariman, G; Khodami, S; Bolch, CJS				Attaran-Fariman, G.; Khodami, S.; Bolch, C. J. S.			The cyst-motile stage relationship of three <i>Protoperidinium</i> species from south-east coast of Iran	IRANIAN JOURNAL OF FISHERIES SCIENCES			English	Article						Phytoplankton; Protoperidinium; Taxonomy; Cyst; Germinated cell; Sediment; Chabahar bay; Iran	SP-NOV DINOPHYCEAE; DINOFLAGELLATE GYMNODINIUM-CATENATUM; RECENT MARINE-SEDIMENTS; RESTING CYSTS; TASMANIA; DARKNESS; GROWTH; BERGH; BAY	Resting cyst and motile thecate cell stages of three heterotrophic Protoperidinium oblongum, Protoperidinium sp and Protoperidinium claudicans were assessed. Cysts were isolated from sediment collected from southeast coast of Iran. Individual live cysts were incubated under optimal conditions for germination. Results showed that Protoperidinium oblongum cysts were pentagonal smooth walled and three cysts of this species were identified from Iranian sediment. The germinated cell of P. oblongum was colourless and elongated pentagonal in shape. P. claudican theca cell has a pointed antapical horn with a four sided apical plate. Protoperidinium sp. had dark brown pentagonal cyst. Its germinated cell differed from other Protoperidinium species. Two divergent distally antapical horns formed 90 between the horn and Posterio-lateral of main body edge, thus, comprising a unique species in the Protoperidinium genus. This kind of antapical horn has not been previously reported among Protoperidinium spp.	[Attaran-Fariman, G.] Chabahar Maritime Univ, Fac Marine Sci, Chabahar, Iran; [Khodami, S.] Iranian Fisheries Res Org, Tehran, Iran; [Bolch, C. J. S.] Univ Tasmania, Sch Aquaculture, Launceston, Tas 7250, Australia	University of Tasmania	Attaran-Fariman, G (通讯作者)，Chabahar Maritime Univ, Fac Marine Sci, Chabahar, Iran.	Gilan.Attaran@gmail.com	Attaran Fariman, Gilan/ABC-4059-2021; Bolch, Christopher/J-7619-2014; khodami, sharareh/K-9419-2018	khodami, sharareh/0000-0003-0846-8604				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; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P572, DOI 10.2216/07-02.1; Attaran-Fariman G, 2007, PHYCOLOGIA, V46, P644, DOI 10.2216/07-05.1; BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P543, DOI 10.1080/00288330.1987.9516258; Balech E, 1988, DINOFLAGELADOS ATLAN; BINDER BJ, 1987, J PHYCOL, V23, P99; Bisby F., 2007, Species 2000 ITIS Catalogue of Life: 2007 Annual Checklist Taxonomic Classification. 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J. Fish. Sci.	JAN	2011	10	1					1	12						12	Fisheries	Science Citation Index Expanded (SCI-EXPANDED)	Fisheries	721AK					2025-03-11	WOS:000287323600001
J	Odin, GS				Odin, Gilles Serge			Gilianelles: Late Cretaceous microproblematica from Europe and Central America	PALAEONTOLOGY			English	Article						Gilianelles; microproblematica; Upper Cretaceous; evolution; taxonomy; biological crisis	CAMPANIAN-MAASTRICHTIAN BOUNDARY; STRATOTYPE; FRANCE; CHALK	During the last two decades, a range of microfossils have been collected from strata of Late Cretaceous (Coniacian-Maastrichtian) age. The name gilianelles has been coined to accommodate these microproblematica. On the basis of many thousands of specimens, typical features of this group have now been assessed. Distinctive traits are calcareous unilocular, basically axially symmetrical test, in the size range 80-200 mu m, with a single-layered wall of radially arranged crystals, 15 mu m thick, the outer surface with a crochet-like nanostructure, a small-sized aperture (one tenth of test diameter), situated on the upper surface in vivo. Secondary criteria include modification of axial test symmetry into radial or bilateral symmetry, development of expansions, either spiny or laminar and presence of longitudinal and latitudinal ornament. To date, 60 taxa have been described from northern Spain to northern Germany and from Central America. Evolutionary patterns of gilianelles are diverse, with both short- and long-ranging forms, some of which comprise lineages that were affected by a marked crisis dated at about 73 Ma. This event is here illustrated by the tribe Coraliellini, of which a key taxon, Coraliella cognatio, is described as new. Previous interpretations of Gilianelles as dinoflagellate cysts are discussed and rejected.	Univ Paris 06, Dept Geol Sedimentaire, F-75252 Paris 05, France	Sorbonne Universite	Odin, GS (通讯作者)，Univ Paris 06, Dept Geol Sedimentaire, 4 Pl Jussieu,Case 119, F-75252 Paris 05, France.	gilles.odin@upmc.fr						Alegret L, 2005, GEOLOGY, V33, P721, DOI 10.1130/G21573.1; Bison KM, 2004, J MICROPALAEONTOL, V23, P127, DOI 10.1144/jm.23.2.127; Hildebrand-Habel Tania, 1997, Courier Forschungsinstitut Senckenberg, V201, P177; KEUPP H, 1984, Palaeontologische Zeitschrift, V58, P9; KEUPP H, 1979, B CTR RECHERCHE EXPL, V3, P641; Keupp Helmut, 1995, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V196, P221; Odin G.S., 2001, Development in Paleontology and Stratigraphy, V19, P881; Odin GS, 2008, CR PALEVOL, V7, P195, DOI 10.1016/j.crpv.2008.03.004; Odin GS, 2007, CR PALEVOL, V6, P181, DOI 10.1016/j.crpv.2006.10.001; Odin Gilles Serge, 2009, Revue de Paleobiologie, V28, P175; Odin GS, 2009, CR PALEVOL, V8, P39, DOI 10.1016/j.crpv.2008.09.005; Odin Gilles Serge, 2008, Carnets de Geologie, P1; Odin Gilles Serge, 2006, Carnets de Geologie, P1; Odin GS, 2003, CR GEOSCI, V335, P239, DOI 10.1016/S1631-0713(03)00032-4; Oding Gilles Serge, 2008, Revista Espanola de Micropaleontologia, V40, P115; Smit J., 1996, Geological Society of America Special Paper, V307, P151, DOI DOI 10.1130/0-8137-2307-8.151; Streng M, 2004, J PALEONTOL, V78, P456, DOI 10.1666/0022-3360(2004)078<0456:APCOAT>2.0.CO;2; Versteegh GJM, 2009, PALAEONTOLOGY, V52, P343, DOI 10.1111/j.1475-4983.2009.00854.x; Willems H., 1990, Senckenbergiana Lethaea, V70, P239; WILLEMS H, 1994, REV PALAEOBOT PALYNO, V84, P57, DOI 10.1016/0034-6667(94)90041-8; Williams Graham L., 1998, AASP Contributions Series, V34, P1	21	5	5	1	1	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0031-0239	1475-4983		PALAEONTOLOGY	Paleontology	JAN	2011	54		1				133	144		10.1111/j.1475-4983.2010.01012.x	http://dx.doi.org/10.1111/j.1475-4983.2010.01012.x			12	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	706HW					2025-03-11	WOS:000286210000007
J	Juretic, H; Dobrovic, S; Ruzinski, N; Lovric, J; Pecarevic, M; Mikus, J; Crncevic, M; Marcelja, EJ; Rajcic, MM; Sirac, S; Cooper, WJ; Grewell, D; van Leeuwen, J				Juretic, Hrvoje; Dobrovic, Slaven; Ruzinski, Nikola; Lovric, Josip; Pecarevic, Marijana; Mikus, Josip; Crncevic, Marija; Marcelja, Esme-Johanna; Rajcic, Marija Marijanovic; Sirac, Sinisa; Cooper, William J.; Grewell, David; (Hans) van Leeuwen, J.			Pilot Studies of Ozonation for Inactivation of Artemia salina Nauplii in Ballast Water	OZONE-SCIENCE & ENGINEERING			English	Article						Ozone; Total Residual Oxidants (TRO); Artemia salina Nauplii Inactivation; Ballast Water	BROMIDE-CONTAINING WATERS; DINOFLAGELLATE CYSTS; NATURAL-POPULATIONS; HYPOBROMOUS ACID; TREATMENT SYSTEM; MARINE PLANKTON; SHIPS; BROMATE; MICROORGANISMS; DEOXYGENATION	A pilot-plant study was conducted in the Republic of Croatia to determine the applicability of ozonation for inactivation of non-indigenous species and to provide necessary information regarding use of ozone as a ballast water treatment option. Nauplii of the brine shrimp Artemia salina were used as model organisms to investigate the efficacy of ozonation at three different ozone dosages (2.4, 3.7 and 10.9 mg L-1). Mortality of Artemia nauplii at 98.6%, was achieved after 3 h of exposure in ozone-treated water with the highest ozone dosage. Our results indicated that ozonation is a promising treatment for controlling non-indigenous and potentially invasive species; however, to draw more general conclusions, several species with higher level of resistance to ozone are required and will be studied in the future.	[Juretic, Hrvoje; Dobrovic, Slaven; Ruzinski, Nikola] Univ Zagreb, Dept Energy Power Engn & Environm, Fac Mech Engn & Naval Architecture, Zagreb 10000, Croatia; [Lovric, Josip; Pecarevic, Marijana; Mikus, Josip; Crncevic, Marija; Marcelja, Esme-Johanna] Univ Dubrovnik, Dept Aquaculture, Dubrovnik 20000, Croatia; [Rajcic, Marija Marijanovic; Sirac, Sinisa] Cent Water Management Lab, Zagreb 10000, Croatia; [Cooper, William J.] Univ Calif Irvine, Urban Water Res Ctr, Dept Civil & Environm Engn, Irvine, CA 92697 USA; [Grewell, David; (Hans) van Leeuwen, J.] Iowa State Univ, Dept Agr & Biosyst Engn, Ames, IA 50011 USA; [Grewell, David; (Hans) van Leeuwen, J.] Iowa State Univ, Dept Civil Construct & Environm Engn, Ames, IA 50011 USA; [(Hans) van Leeuwen, J.] Iowa State Univ, Dept Food Sci & Human Nutr, Ames, IA 50011 USA	University of Zagreb; University of Zagreb Faculty of Mechanical Engineering & Naval Architecture; University of Dubrovnik; University of California System; University of California Irvine; Iowa State University; Iowa State University; Iowa State University	Juretic, H (通讯作者)，Univ Zagreb, Dept Energy Power Engn & Environm, Fac Mech Engn & Naval Architecture, Zagreb 1000, Croatia.	hrvoje.juretic@fsb.hr	Dobrovic, Slaven/ISA-6507-2023; Cooper, William/D-4502-2011	Juretic, Hrvoje/0000-0002-1511-4073; Pecarevic, Marijana/0000-0003-4665-2103; , Marija/0000-0003-2455-4772	Ministry of Science, Education and Sports of the Republic of Croatia [120-1253092-3021]; Fulbright IIE Student Fellowship	Ministry of Science, Education and Sports of the Republic of Croatia(Ministry of Science, Education and Sports, Republic of Croatia); Fulbright IIE Student Fellowship	The financial support of the Ministry of Science, Education and Sports of the Republic of Croatia (project number 120-1253092-3021) and a Fulbright IIE Student Fellowship (HJ) are appreciated. This is contribution 55 from the University of California, Irvine, Urban Water Research Center.	*APHA, 1995, STAND METH EX WAT WA, pV1; Bai XY, 2005, PLASMA CHEM PLASMA P, V25, P41, DOI 10.1007/s11090-004-8834-5; Bax N, 2003, MAR POLICY, V27, P313, DOI 10.1016/S0308-597X(03)00041-1; CARLTON JT, 1995, CGD1195, P213; Dobbs FC, 2005, ENVIRON SCI TECHNOL, V39, p259A, DOI 10.1021/es053300v; Driedger A, 2001, WATER RES, V35, P2950, DOI 10.1016/S0043-1354(00)00577-7; Echigo S, 2006, WATER SCI TECHNOL, V53, P235, DOI 10.2166/wst.2006.358; Gavand MR, 2007, MAR POLLUT BULL, V54, P1777, DOI 10.1016/j.marpolbul.2007.07.012; Gollasch S, 2006, HELGOLAND MAR RES, V60, P84, DOI 10.1007/s10152-006-0022-y; Gregg MD, 2007, HARMFUL ALGAE, V6, P567, DOI 10.1016/j.hal.2006.08.009; HAAG WR, 1983, ENVIRON SCI TECHNOL, V17, P261, DOI 10.1021/es00111a004; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Herwig RP, 2006, MAR ECOL PROG SER, V324, P37, DOI 10.3354/meps324037; Holm ER, 2008, MAR POLLUT BULL, V56, P1201, DOI 10.1016/j.marpolbul.2008.02.007; Hunt CD, 2005, ENVIRON SCI TECHNOL, V39, p321A, DOI 10.1021/es0533141; *LLOYDS REG, 2008, BALL WAT TREATM TECH, P32; McCarthy Heather P., 2000, Biological Invasions, V2, P321, DOI 10.1023/A:1011418432256; MCCARTHY SA, 1994, APPL ENVIRON MICROB, V60, P2597, DOI 10.1128/AEM.60.7.2597-2601.1994; McCollin T, 2007, MAR POLLUT BULL, V54, P1170, DOI 10.1016/j.marpolbul.2007.04.013; *NAT RES COUNC, 1996, STEMM TID CONTR INTR, pR13; Oemcke D, 2004, OZONE-SCI ENG, V26, P389, DOI 10.1080/01919510490482241; Oemcke DJ, 2005, WATER RES, V39, P5119, DOI 10.1016/j.watres.2005.09.024; Perrins JC, 2006, MAR POLLUT BULL, V52, P1023, DOI 10.1016/j.marpolbul.2006.01.007; Pimentel D, 2000, BIOSCIENCE, V50, P53, DOI 10.1641/0006-3568(2000)050[0053:EAECON]2.3.CO;2; Rigby GR, 1999, MAR ECOL PROG SER, V191, P289, DOI 10.3354/meps191289; Ruiz GM, 2000, NATURE, V408, P49, DOI 10.1038/35040695; Sano LL, 2005, MAR POLLUT BULL, V50, P1050, DOI 10.1016/j.marpolbul.2005.04.008; SONG R, 1996, ACS S SERIES; Sutherland TF, 2001, MAR ECOL PROG SER, V210, P139, DOI 10.3354/meps210139; Tamburri MN, 2002, BIOL CONSERV, V103, P331, DOI 10.1016/S0006-3207(01)00144-6; Tang ZJ, 2006, MAR ENVIRON RES, V61, P410, DOI 10.1016/j.marenvres.2005.06.003; VINOGRADOV ME, 1995, OKEANOLOGIYA+, V35, P569; VOIGT M, 2004, GLOBALLAST MONOGRAPH, V15, P321; von Gunten U, 2003, WATER RES, V37, P1469, DOI 10.1016/S0043-1354(02)00458-X; VONGUNTEN U, 1994, ENVIRON SCI TECHNOL, V28, P1234, DOI 10.1021/es00056a009; Waite TD, 2003, MAR ECOL PROG SER, V258, P51, DOI 10.3354/meps258051; Westerhoff P, 2004, WATER RES, V38, P1502, DOI 10.1016/j.watres.2003.12.014; Wonham MJ, 2001, MAR ECOL PROG SER, V215, P1, DOI 10.3354/meps215001; Wonham MJ, 2000, MAR BIOL, V136, P1111, DOI 10.1007/s002270000303	39	9	9	1	19	TAYLOR & FRANCIS INC	PHILADELPHIA	325 CHESTNUT ST, SUITE 800, PHILADELPHIA, PA 19106 USA	0191-9512			OZONE-SCI ENG	Ozone-Sci. Eng.		2011	33	1					3	13	PII 932775804	10.1080/01919512.2011.536501	http://dx.doi.org/10.1080/01919512.2011.536501			11	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	719GA					2025-03-11	WOS:000287188400002
J	Qin, JA; Taylor, D; Atahan, P; Zhang, XR; Wu, GX; Dodson, J; Zheng, HB; Itzstein-Davey, F				Qin, Jungan; Taylor, David; Atahan, Pia; Zhang, Xinrong; Wu, Guoxuan; Dodson, John; Zheng, Hongbo; Itzstein-Davey, Freea			Neolithic agriculture, freshwater resources and rapid environmental changes on the lower Yangtze, China	QUATERNARY RESEARCH			English	Article						Holocene; Environmental change; Food security; Phytolith; Pollen; Rice; Sea level	RADIOCARBON AGE CALIBRATION; SEA-LEVEL HIGHSTAND; RIVER DELTA; POLLEN DISTRIBUTION; RICE DOMESTICATION; SEDIMENT STORAGE; EASTERN CHINA; HOLOCENE; CLIMATE; RECORD	Analyses of sedimentary evidence in the form of spores, pollen, freshwater algae, dinoflagellate cysts, phytoliths and charcoal from AMS C-14-dated, Holocene-aged sequences provide an excellent opportunity to examine the responses of Neolithic agriculturalists in the lower Yangtze to changing environments. Evidence from two sites close to the southern margin of the Yangtze delta and separated by what is now Hangzhou Bay attests the critical importance to early attempts at food production of access to freshwater resources. More readily, if episodically, available freshwater resources during the early to mid-Holocene on the Hangjiahu plain may have encouraged an early reliance on rice-based agriculture, which in turn facilitated the accumulation of agricultural surpluses and cultural diversification. Cultural change was relatively attenuated and human population pressures possibly lower on the Ningshao plain, seemingly because of much more profound environmental impacts of variations in local hydrological conditions, and because predominantly saline conditions, associated with rising relative sea level, hampered the early development of irrigated agriculture. The evidence, although largely dating to the early and middle parts of the Holocene, provides a timely warning of the complexity of vulnerability to climate change-induced processes of agriculture, and indeed human activities more generally, on megadeltas in Asia. (C) 2010 University of Washington. Published by Elsevier Inc. All rights reserved.	[Qin, Jungan; Taylor, David; Itzstein-Davey, Freea] Trinity Coll Dublin, Sch Nat Sci, Dublin, Ireland; [Qin, Jungan; Wu, Guoxuan] Tongji Univ, Sch Ocean & Earth Sci, Shanghai 200092, Peoples R China; [Atahan, Pia; Dodson, John] Australian Nucl Sci & Technol Org, Inst Environm Res, Sydney, NSW, Australia; [Zhang, Xinrong] Jilin Univ, Coll Earth Sci, Changchun 130023, Peoples R China; [Zheng, Hongbo] Nanjing Univ, Sch Earth Sci & Engn, Nanjing 210008, Peoples R China	Trinity College Dublin; Tongji University; Australian Nuclear Science & Technology Organisation; Jilin University; Nanjing University	Qin, JA (通讯作者)，Trinity Coll Dublin, Sch Nat Sci, Dublin, Ireland.	qinjungan@gmail.com	Zhang, Xinrong/KFS-6736-2024; Zheng, Hongbo/LNP-2343-2024; Atahan, Pia/D-8670-2012; Taylor, David/ISS-5752-2023	Taylor, David/0000-0002-6098-5636	Irish Research Council for Science, Engineering and Technology (IRCSET); Ministry of Education of China; NSFC [40676033, 40830107, 40702027]; Shanghai Government [05XD14015]	Irish Research Council for Science, Engineering and Technology (IRCSET)(Irish Research Council for Science, Engineering and Technology); Ministry of Education of China(Ministry of Education, China); NSFC(National Natural Science Foundation of China (NSFC)); Shanghai Government	Financial support from the Irish Research Council for Science, Engineering and Technology (IRCSET) and the Ministry of Education of China for the research that underpins this paper is gratefully acknowledged. Hongbo Zheng was supported by grants from the NSFC (40676033 and 40830107) and Shanghai Government (05XD14015). Xinrong Zhang was supported by grants from the NSFC (40702027). Special thanks are extended to Wei-Ming Wang, Nanjing Institute of Geology and Palaeontology, Xueqing Hong and Baocheng Zhao, East China Normal University and Dr. Xiangtong Huang and Shifan Xu, Tongji University, for their assistance. The authors are also extremely grateful to members of the coring teams from Ningbo University and Zhejiang Engineering Investigation Institute who helped with the collection of sediment cores, and to the three anonymous reviewers for their highly constructive comments on an earlier version of this manuscript.	*ADM CULT HER SHAN, 1985, ARCHAEOLOGY, P584; An ZS, 2000, QUATERNARY SCI REV, V19, P743, DOI 10.1016/S0277-3791(99)00031-1; [Anonymous], 2007, CLIMATIC CHANGE 2007, DOI 10.2134/jeq2008.0015br; [Anonymous], 1990, Modern Quaternary Research in Southeast Asia; [Anonymous], 1980, VEGETATION CHINA; [Anonymous], 1992, TILIA SOFTWARE; Atahan P, 2008, QUATERNARY SCI REV, V27, P556, DOI 10.1016/j.quascirev.2007.11.003; Barnes GinaL., 1993, China, Korea and Japan : the rise of civilization in East Asia; Bellwood P, 2005, First farmers: the origins of agricultural societies; Bozarth S.R., 1992, PHYTOLITH SYSTEMATIC, P193, DOI [10.1007/978-1-4899-1155-1_10, DOI 10.1007/978-1-4899-1155-1_10]; Cai B Q, 2001, J XIAMEN U ARTS SOCI, P126; Cai Y.L., 2001, J. 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Res.	JAN	2011	75	1					55	65		10.1016/j.yqres.2010.07.014	http://dx.doi.org/10.1016/j.yqres.2010.07.014			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Arts &amp; Humanities Citation Index (A&amp;HCI)	Physical Geography; Geology	713FR					2025-03-11	WOS:000286720900007
J	Willumsen, PS				Willumsen, Pi Suhr			Maastrichtian to Paleocene dinocysts from the Clarence Valley, South Island, New Zealand	ALCHERINGA			English	Article						New Zealand; Maastrichtian; Paleocene; Cretaceous-Paleogene boundary; dinoflagellates; stratigraphy; correlation; new species; taxonomy	CRETACEOUS-TERTIARY BOUNDARY; DINOFLAGELLATE CYST; SEYMOUR-ISLAND; PALEOENVIRONMENTAL CHANGES; SOUTHEASTERN MARLBOROUGH; CALCAREOUS NANNOFOSSIL; FLAXBOURNE RIVER; BIOSTRATIGRAPHY; TRANSITION; PALEOGENE	A palynological study of uppermost Maastrichtian to lower Paleocene marine strata from two stratigraphic sections in the Clarence Valley, Marlborough, New Zealand, revealed diverse organic-walled dinoflagellate cyst (dinocyst) assemblages. One hundred and twelve samples were investigated and 86 dinocyst species were identified, from the two sections studied: Branch and Mead streams. Nine new species are described herein: Cerodinium nielsii, Impagidinium agremon, I. cavea, I. crouchiae, I. hannahii, Lejeunecysta kammae, Pyxidinopsis epakros, P. everriculum and P. meadensis. Stratigraphic correlations are achieved using nine new index species and eight cyst acme intervals, named A to H, integrated with foraminiferal datums and the radiolarian zonation for the South Pacific. The first occurrence of Carpatella septata combined with a high relative abundance of Diconidinium martianum characterizes the interval directly below the Cretaceous-Paleogene (K-Pg) boundary or uppermost part of the Manumiella druggii Zone. Based on the results from both sections, the earliest Paleocene Trithyrodinium evittii Zone is subdivided into the following intervals: Senoniasphaera inornata, Carpatella cornuta, Cassidium fragile and Cerodinium striatum subzones. The following dinocyst species first appear at or near the top of the T. evittii Zone: Alterbidinium pentaradiatum, Glaphyrocysta perforata, Habibacysta sp. cf. H. tectata, Kallosphaeridium brevibarbatum, Lejeunecysta kammae, Pyxidinopsis sp. cf. P. waipawaensis, Spiniferella cornuta and Tectatodinium meandriforme. The boundary between the T. evittii and the overlying Palaeocystodinium golzowense Zone was recorded only in the Mead Stream section where it is dated to ca 64.0 Ma. A high relative abundance of Isabelidinium cingulatum succeeded by the first occurrence of Isabelidinium bakeri, Deflandrea foveolata and D. delineata characterizes the lower to middle part of the early Paleocene P. golzowense Zone. The last consistent occurrence of P. pyrophorum is recorded within the upper part of radiolarian Zone RP3 corresponding to the middle part of the early Paleocene calcareous nannoplankton Zone NP3 (Early Teurian) or ca 63.7 Ma. The K-Pg boundary is not characterized by a mass extinction of dinoflagellates in the New Zealand sections. Instead, there is a marked change in cyst associations directly above the boundary and several new species appear in the lowermost Paleocene. Several typical latest Maastrichtian taxa have their last occurrences within the lowermost Paleocene corresponding to an interval of ca 0.5-0.7 Myrs after the K-Pg boundary.	Lund Univ, Dept Earth & Ecosyst Sci, Div Geol, S-22362 Lund, Sweden	Lund University	Willumsen, PS (通讯作者)，Lund Univ, Dept Earth & Ecosyst Sci, Div Geol, Solvegatan 12, S-22362 Lund, Sweden.	Pi.Willumsen@geol.lu.se			New Zealand Marsden Fund; Danish Research Agency, Ministry of Sciences; Danish Carlsberg Fund [2008_01_0404]	New Zealand Marsden Fund(Royal Society of New ZealandMarsden Fund (NZ)); Danish Research Agency, Ministry of Sciences; Danish Carlsberg Fund	This palynological study was conducted as part of a multidisciplinary research program funded by the New Zealand Marsden Fund. The Danish Research Agency, Ministry of Sciences, is thanked for their financial support during my doctoral studies in New Zealand. The author acknowledges a personal grant no. 2008_01_0404 from the Danish Carlsberg Fund. Dr. Graeme J. Wilson and Dr. Steve McLoughlin are thanked for help with manuscripts. Roger Tremain (GNS) and Erica Vry are thanked for technical assistance in the GNS laboratory. Dr. Vivi Vajda is thanked for her helpful comments on an early version of this manuscript. Detailed and helpful comments from the two reviewers Dr. Graham Williams and Dr. Jim Riding are acknowledged. Steve McLoughlin is also thanked for his editoral assistance.	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J	Smith, BC; Persson, A; Selander, E; Wikfors, GH; Alix, J				Smith, Barry C.; Persson, Agneta; Selander, Erik; Wikfors, Gary H.; Alix, Jennifer			Toxin profile change in vegetative cells and pellicle cysts of <i>Alexandrium fundyense</i> after gut passage in the eastern oyster <i>Crassostrea virginica</i>	AQUATIC BIOLOGY			English	Article						Alexandrium fundyense; Crassostrea virginica; Dinoflagellate; Toxin; PST; Pellicle cyst	PARALYTIC SHELLFISH POISON; PSP TOXINS; OSTENFELDII DINOPHYCEAE; TREATMENT OPTIONS; ACTIVATED CARBON; DRINKING-WATER; HARMFUL ALGAE; HIROSHIMA BAY; DINOFLAGELLATE; SAXITOXIN	Vegetative cells and pellicle cysts of the toxic dinoflagellate Alexandrium fundyense Balech were fed to the eastern oyster Crassostrea virginica Gmelin under controlled conditions. Para lytic shellfish toxins (PSTs) were measured in vegetative cells and pellicle cysts prior to feeding and directly after passage through the oyster alimentary canal and defecation as intact cells. Oysters fed with vegetative cells and those fed with pellicle cysts accumulated toxins. One experimental treatment tested for direct uptake of toxins from the water (oysters and A. fundyense cells were separated by a screen); PSTs were not accumulated from the water by the oysters. There were no significant changes in total, per-cell toxicity after passage through the oyster alimentary canal, suggesting limited transfer of toxins from intact cells to the oysters. However, there were statistically significant changes in the toxin composition of cells following gut passage. Vegetative cells and pellicle cysts from feces had increased amounts of saxitoxin (STX) and decreased amounts of gonyautoxin 4 (GTX4) per cell, compared to amounts prior to gut passage. Following gut passage, pellicle cysts showed better survival in the feces than vegetative cells, which is consistent with the view of pellicle-cyst formation as a successful survival strategy against adverse conditions.	[Smith, Barry C.; Persson, Agneta; Wikfors, Gary H.; Alix, Jennifer] Natl Marine Fisheries Serv, Milford Lab, NE Fisheries Sci Ctr, NOAA, Milford, CT 06460 USA; [Selander, Erik] Univ Gothenburg, Sven Loven Ctr Marine Res, S-45034 Fiskebackskil, Sweden	National Oceanic Atmospheric Admin (NOAA) - USA; University of Gothenburg	Smith, BC (通讯作者)，Natl Marine Fisheries Serv, Milford Lab, NE Fisheries Sci Ctr, NOAA, Milford, CT 06460 USA.	barry.smith@noaa.gov		Selander, Erik/0000-0002-2579-0841; Persson, Agneta/0000-0003-0202-6514	Langmanska kulturfonden; Oscar and Lili Lamms Foundation for Scientific Research	Langmanska kulturfonden; Oscar and Lili Lamms Foundation for Scientific Research	We thank an anonymous reviewer and P. G. Beninger for helpful comments. This experiment was performed with a travel grant from Langmanska kulturfonden and a research grant from Oscar and Lili Lamms Foundation for Scientific Research to A. P. Mention of trade names does not imply endorsement.	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Biol.		2011	13	2					193	201		10.3354/ab00362	http://dx.doi.org/10.3354/ab00362			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	816TB		Bronze			2025-03-11	WOS:000294623900009
J	Mayali, X; Franks, PJS; Burton, RS				Mayali, Xavier; Franks, Peter J. S.; Burton, Ronald S.			Temporal attachment dynamics by distinct bacterial taxa during a dinoflagellate bloom	AQUATIC MICROBIAL ECOLOGY			English	Article						Algal-bacterial interactions; Bloom dynamics; Parasitism; Phycosphere; Roseobacter; Bacteroidetes; Dinoflagellate	IN-SITU HYBRIDIZATION; PHYTOPLANKTON COLONIZATION; BACTERIVOROUS PROTOZOA; ALEXANDRIUM-FUNDYENSE; FUNCTIONAL DIVERSITY; POPULATION-DYNAMICS; MICROBIAL COMMUNITY; MARINE-BACTERIA; CYST FORMATION; DIATOM BLOOM	Limited quantitative information exists on the physical interaction between specific taxa of heterotrophic bacteria and phytoplankton in pelagic aquatic environments. Using catalyzed reporter deposition fluorescence in situ hybridization (CARD-FISH), we quantified bacterial attachment to the cells of the dinoflagellate Lingulodinium polyedrum in 39 surface samples collected during a natural bloom in summer 2005 off the coast of La Jolla, California, USA. Using a ribosomal RNA based tunable array with Luminex (R) bead technology, we also quantified the relative abundances of 11 particle-associated bacterial taxa during this time, including 8 members of the Bacteroidetes division. Bacterial colonization of dinoflagellate cells was generally low (mean < 2 bacteria alga(-1)) but increased during the days preceding bloom decline events. This indicates that physical associations, and thus potentially physiological interactions among bacteria and dinoflagellates, changed over the course of the algal bloom cycle. The 11 detected bacterial taxa exhibited diverse patterns of colonization over time, suggesting that they mediated different types of interactions with the dinoflagellates. Some bacterial types were only detected during the early bloom phase, others peaked in abundance during peaks in algal numbers, and still others peaked following bloom decline events. Our data linking the temporal succession of different bacterial colonizers to algal bloom dynamics exemplify the idea that microscale, species-specific interactions between bacteria and protists can result in large-scale ecosystem level changes that can impact phytoplankton community structure in the coastal ocean.	[Mayali, Xavier] Lawrence Livermore Natl Lab, Livermore, CA 94550 USA; [Franks, Peter J. S.; Burton, Ronald S.] Univ Calif San Diego, Scripps Inst Oceanog, La Jolla, CA 92093 USA	United States Department of Energy (DOE); Lawrence Livermore National Laboratory; University of California System; University of California San Diego; Scripps Institution of Oceanography	Mayali, X (通讯作者)，Lawrence Livermore Natl Lab, 7000 East Ave, Livermore, CA 94550 USA.	mayali1@llnl.gov	Mayali, Xavier/JBJ-2272-2023; Burton, Ronald/F-7694-2010	Mayali, Xavier/0000-0002-2170-0773; Burton, Ronald/0000-0002-6995-5329	Southern California Coastal Ocean Observing System; NOAA/ECOHAB; NSF; US Department of Energy by Lawrence Livermore National Laboratory [DE-AC52-07NA27344]	Southern California Coastal Ocean Observing System; NOAA/ECOHAB(National Oceanic Atmospheric Admin (NOAA) - USA); NSF(National Science Foundation (NSF)); US Department of Energy by Lawrence Livermore National Laboratory(United States Department of Energy (DOE))	We are grateful to F. Malfatti for assistance in field sampling, F. Azam for advice and input to the manuscript, R. Mueller and F. Lauro for insightful discussions, and 3 anonymous reviewers for useful comments. We are indebted to J. McGowan and M. Carter for the chlorophyll data collected through the Scripps Pier Chlorophyll Program, which is funded through the Southern California Coastal Ocean Observing System. This work was funded by a NOAA/ECOHAB grant to P.J.S.F. and F. Azam and an NSF grant to R.S.B. This work was performed under the auspices of the US Department of Energy by Lawrence Livermore National Laboratory under Contract DE-AC52-07NA27344.	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Microb. Ecol.		2011	63	2					111	122		10.3354/ame01483	http://dx.doi.org/10.3354/ame01483			12	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	750WA		Bronze			2025-03-11	WOS:000289577600002
J	Lundgren, V; Granéli, E				Lundgren, Veronica; Graneli, Edna			Influence of altered light conditions and grazers on <i>Scrippsiella trochoidea</i> (Dinophyceae) cyst formation	AQUATIC MICROBIAL ECOLOGY			English	Article						Scrippsiella trochoidea; Cyst formation; Light intensity; Grazer density; Temporary cysts	DINOFLAGELLATE ALEXANDRIUM-OSTENFELDII; PHAEOCYSTIS-GLOBOSA PRYMNESIOPHYCEAE; COPEPOD ACARTIA-TONSA; EGG-PRODUCTION; LIFE-HISTORY; GONYAULAX-TAMARENSIS; TOXIN PRODUCTION; MARINE COPEPODS; TEMPERATURE; GROWTH	We investigated whether or not the presence of copepods and different light conditions induced cyst formation in dinoflagellates. Scrippsiella trochoidea was exposed to Acartia tonsa directly and indirectly (grazer filtrate), in high light and low light conditions. The ingestion, faecal production and egg production of A. tonsa were compared between diets of S. trochoidea vegetative cells and temporary cysts. We found no effect of direct or indirect exposure to A. tonsa on S. trochoidea cyst formation in either high light or low light conditions. Controls and A. tonsa treatments kept in light displayed around 20% temporary cysts, whereas controls and A. tonsa treatments in low light were shown to have 50 to 80% temporary cysts. Thus, low light conditions had a strong effect on temporary cyst formation. No hypnocysts were observed in any experiment, which is probably related to the longer incubation times needed for their observation. Feeding on diets dominated by temporary cysts compared to vegetative cells decreased ingestion by a factor of 2.7, while faecal and egg production decreased by a factor of 2.2 and 2.9, respectively, suggesting that induction of temporary cysts in response to A. tonsa could be a survival strategy. However, S. trochoidea does not possess any grazer-induced defence in terms of temporary cyst formation, as it did not produce temporary cysts when exposed to A. tonsa. Rather, induction of temporary cysts seems to be controlled by decreased light intensity, which is a favorable trait for this species when driven to water depths where light is scarce.	[Lundgren, Veronica; Graneli, Edna] Linnaeus Univ, Sch Nat Sci, Kalmar, Sweden	Linnaeus University	Lundgren, V (通讯作者)，Linnaeus Univ, Sch Nat Sci, Kalmar, Sweden.	veronica.lundgren@lnu.se	Graneli, Edna/F-5936-2015		Linnaeus University	Linnaeus University	We thank the staff at the Sven Loven Centre for Marine Sciences, Gothenburg University, for supplying copepods. We are grateful to M. Clement at the Swedish Museum of Natural History for copepod identification. Four anonymous reviewers are thanked for valuable and constructive criticisms on an earlier version of the manuscript. We extend gratitude to the Linnaeus University for financial support.	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Microb. Ecol.		2011	63	3					231	243		10.3354/ame01497	http://dx.doi.org/10.3354/ame01497			13	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	769ZS		Bronze			2025-03-11	WOS:000291057400003
J	Penaud, A; Eynaud, F; Voelker, A; Kageyama, M; Marret, F; Turon, JL; Blamart, D; Mulder, T; Rossignol, L				Penaud, A.; Eynaud, F.; Voelker, A.; Kageyama, M.; Marret, F.; Turon, J. L.; Blamart, D.; Mulder, T.; Rossignol, L.			Assessment of sea surface temperature changes in the Gulf of Cadiz during the last 30 ka: implications for glacial changes in the regional hydrography	BIOGEOSCIENCES			English	Article							NORTHERN NORTH-ATLANTIC; DINOFLAGELLATE CYST ASSEMBLAGES; RECENT MARINE-SEDIMENTS; PLANKTONIC-FORAMINIFERA; AZORES FRONT; MEDITERRANEAN SEA; HEINRICH EVENTS; IBERIAN MARGIN; PALEOCEANOGRAPHIC CONDITIONS; GLOBAL DISTRIBUTION	New dinocyst analyses were conducted on core MD99-2339 retrieved from the central Gulf of Cadiz. Dinocyst and foraminiferal assemblages from this core are combined with existing data off SW Portugal and NW Morocco to investigate past hydrological and primary productivity regimes in the subtropical NE Atlantic Ocean over the last 30 ka. Our results have revealed highest upwelling intensity during Heinrich Stadial 1 (HS 1) and the Younger Dryas and weaker upwelling cells during the Last Glacial Maximum (LGM) and HS 2, off the SW Iberian and NW Moroccan margins. Similar assemblages between the Gulf of Cadiz and the NW Moroccan margin, and distinct species off Portugal, were observed during the cold climatic extremes that punctuated the last 30 ka. This pattern has been linked to the occurrence of a hydrological structure between SW Iberia and Cadiz during the last glacial period, perhaps similar to the modern Azores Front. This front was probably responsible locally for heterotrophic dinocysts found in the Gulf of Cadiz during the last glacial period, even if this sector is not conductive to upwelling phenomena by Ekman transport. Regional reconstructions of paleo-sea-surface temperatures (SSTs) using dinocyst and foraminiferal transfer functions, as well as alkenones, are also discussed and depict coherent scenarios over the last 30 ka. Seasonal reconstructions of LGM SSTs obtained with this multi-proxy panel are discussed jointly with model outputs in order to contribute to ongoing efforts in model-data comparison.	[Penaud, A.] IUEM UBO, Domaines Ocean UMR6538, F-29280 Plouzane, France; [Penaud, A.; Eynaud, F.; Turon, J. L.; Mulder, T.; Rossignol, L.] Univ Bordeaux 1, EPOC UMR5805, F-33405 Talence, France; [Voelker, A.] LNEG, Unidade Geol Marinha, P-2610143 Zambujal, Amadora, Portugal; [Kageyama, M.; Blamart, D.] Ctr Etud Saclay, LSCE, F-91191 Gif Sur Yvette, France; [Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Laboratorio Nacional de Energia e Geologia IP (LNEG); Universite Paris Saclay; University of Liverpool	Penaud, A (通讯作者)，IUEM UBO, Domaines Ocean UMR6538, F-29280 Plouzane, France.	aurelie.penaud@univ-brest.fr	; Voelker, Antje/C-5427-2012; Penaud, Aurelie/F-2485-2011; Kageyama, Masa/F-2389-2010	Eynaud, Frederique/0000-0003-1283-7425; Voelker, Antje/0000-0001-6465-6023; Penaud, Aurelie/0000-0003-3578-4549; Marret-Davies, Fabienne/0000-0003-4244-0437; Kageyama, Masa/0000-0003-0822-5880	FCT; French CNRS; ANR; CNRS-INSU	FCT(Fundacao para a Ciencia e a Tecnologia (FCT)); French CNRS(Centre National de la Recherche Scientifique (CNRS)); ANR(Agence Nationale de la Recherche (ANR)); CNRS-INSU(Centre National de la Recherche Scientifique (CNRS))	Thanks to IPEV, the captain and the crew of the Marion Dufresne and the scientific team of the PRIVILEGE and IMAGES-GINNA cruises. We wish to thank Mr. Y. Balut for his assistance at sea and M. Castera, M. Georget and O. Ther for invaluable technical assistance at the laboratory. We gratefully acknowledge the reviewers, in particular Michael Rogerson whose comments permit to greatly improve this manuscript. A. V. acknowledges funding support from FCT through the MOWFADRI project. Part of this study was supported by the French CNRS and the ANR IDEGLACE.The publication of this article is financed by CNRS-INSU.	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J	Mertens, KN; Dale, B; Ellegaard, M; Jansson, IM; Godhe, A; Kremp, A; Louwye, S				Mertens, Kenneth Neil; Dale, Barrie; Ellegaard, Marianne; Jansson, Ida-Maria; Godhe, Anna; Kremp, Anke; Louwye, Stephen			Process length variation in cysts of the dinoflagellate <i>Protoceratium reticulatum</i>, from surface sediments of the Baltic-Kattegat-Skagerrak estuarine system: a regional salinity proxy	BOREAS			English	Article							LAST 2000 YEARS; LATE-HOLOCENE; GYMNODINIUM CATENATUM; NORTH-ATLANTIC; SEA; MORPHOLOGY; BLACK; EUTROPHICATION; ASSEMBLAGES; VARIABILITY	Results are presented from a regional comparison of average process length variation in cysts of Protoceratium reticulatum and Lingulodinium polyedrum, extracted from surface sediments in the Skagerrak-Kattegat-Baltic estuarine system, with the environmental variables of seawater temperature and salinity. Although too few cysts of Lingulodinium polyedrum were recovered from the sediments to make reliable correlations, cysts of Protoceratium reticulatum were well represented, and average process length was correlated significantly with both salinity and temperature. Owing to dominant summer surface production, and regional covariation between salinity and density, we propose the use of the significant correlation with summer sea surface salinity (SSSsummer) by the equation SSSsummer=3.16 x average process length -0.84 (R2=0.8). Application of this equation down-core in Limfjord (northern Denmark) shows its usefulness as a regional palaeosalinity proxy.	[Mertens, Kenneth Neil; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Dale, Barrie] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [Ellegaard, Marianne] Univ Copenhagen, Dept Biol, Fac Sci, DK-1353 Copenhagen K, Denmark; [Jansson, Ida-Maria] Univ Toronto, Ctr Earth Sci, Dept Geol, Toronto, ON M5S 3B1, Canada; [Godhe, Anna] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden; [Kremp, Anke] Finnish Environm Inst, Ctr Marine Res, Helsinki 00251, Finland	Ghent University; University of Oslo; University of Copenhagen; University of Toronto; University of Gothenburg; Finnish Environment Institute	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	Kenneth.Mertens@ugent.be; barrie.dale@geo.uio.no; me@bio.ku.dk; jansson@geology.utoronto.ca; anna.godhe@marecol.gu.se; anke.Kremp@ymparisto.fi; stephen.louwye@ugent.be	Kremp, Anke/I-8139-2013; Mertens, Kenneth/AAO-9566-2020; Ellegaard, Marianne/H-6748-2014; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Ellegaard, Marianne/0000-0002-6032-3376; Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483				Aasen J, 2005, TOXICON, V45, P265, DOI 10.1016/j.toxicon.2004.10.012; [Anonymous], THESIS U OSLO; Antonov J., 2006, NOAA ATLAS NESDIS 62, P182; Antonov J.I., 2006, WORLD OCEAN ATLAS 20, V2; Bendle J, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2004PA001025; Blanz T, 2005, GEOCHIM COSMOCHIM AC, V69, P3589, DOI 10.1016/j.gca.2005.02.026; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Bollmann J, 2009, EARTH PLANET SC LETT, V284, P320, DOI 10.1016/j.epsl.2009.05.003; BRAARUD T, 1976, SARSIA, P41; BRAARUD T, 1974, SARSIA, P63; Braarud T., 1939, Hvalradets Skrifter Oslo, V19, P1; 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WALL D., 1967, PALAEONTOLOGY, V10, P95; WANG L, 1995, PALEOCEANOGRAPHY, V10, P749, DOI 10.1029/95PA00577	74	52	53	0	25	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0300-9483	1502-3885		BOREAS	Boreas		2011	40	2					242	255		10.1111/j.1502-3885.2010.00193.x	http://dx.doi.org/10.1111/j.1502-3885.2010.00193.x			14	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	739YY					2025-03-11	WOS:000288759400003
J	Wang, ZH; Ramsdell, JS				Wang, Zhihong; Ramsdell, John S.			Analysis of Interactions of Brevetoxin-B and Human Serum Albumin by Liquid Chromatography/Mass Spectrometry	CHEMICAL RESEARCH IN TOXICOLOGY			English	Article							NUCLEOPHILIC TARGET; KARENIA-BREVIS; MARINE AEROSOL; HUMAN EXPOSURE; PROTEIN; CYSTEINE; ADDUCTS; BINDING; PLASMA; BLOOD	Brevetoxins are neurotoxins produced by marine dinoflagellates, primarily Karenia brevis, and can cause intoxication and even mortality of marine species, affect human health through the consumption of brevetoxin-contaminated shellfish, and effect respiratory irritation through aerosol exposure at coastal areas. Brevetoxin-A and brevetoxin-B, the major brevetoxins produced in algae, are metabolized to a series of amino acid and peptide-related derivatives in shellfish through the reactions of the amino acid residue cysteine with an alpha,beta-unsaturated aldehyde group. In this paper, covalent interactions between brevetoxin and proteins were investigated using brevetoxin-B and human serum albumin (HSA) as a model. It is demonstrated that both noncovalent and covalent interactions can occur between brevetoxin-B and HSA with in vitro experiments. Covalent adducts of brevetoxin-B and HSA were generated under physiological conditions and reduced with sodium borohydride based on the reaction conditions of single amino acid residues with brevetoxin-B. LC/MS analysis of toxin-treated HSA recognized the formation of the intact protein adducts with primarily one and two toxin molecules attached to one HSA molecule. HSA treated with/without brevetoxin-B was digested with trypsin, trypsin following chymotrypsin, and Pronase, respectively, for LC/MS analysis of adduction sites. Brevetoxin-B was found to react primarily with Cys(34) and His(3) and with His and Lys at other sites of HSA with variable reactivity and with Lys in general the least reactive.	[Wang, Zhihong; Ramsdell, John S.] NOAA, Marine Biotoxins Program, Ctr Coastal Environm Hlth & Biomol Res, Natl Ocean Serv, Charleston, SC 29412 USA	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA	Ramsdell, JS (通讯作者)，NOAA, Marine Biotoxins Program, Ctr Coastal Environm Hlth & Biomol Res, Natl Ocean Serv, 219 Ft Johnson Rd, Charleston, SC 29412 USA.	John.ramsdell@noaa.gov						Aldini G, 2005, J MASS SPECTROM, V40, P946, DOI 10.1002/jms.872; Aldini G, 2008, CHEM RES TOXICOL, V21, P824, DOI 10.1021/tx700349r; Bolgar MS, 1996, ANAL CHEM, V68, P2325, DOI 10.1021/ac9601021; Bossart GD, 1998, TOXICOL PATHOL, V26, P276, DOI 10.1177/019262339802600214; Brunmark P, 1997, CHEM RES TOXICOL, V10, P880, DOI 10.1021/tx9700782; Cheng YS, 2005, ENVIRON HEALTH PERSP, V113, P638, DOI 10.1289/ehp.7496; Cohn JA, 1996, ARCH BIOCHEM BIOPHYS, V328, P158, DOI 10.1006/abbi.1996.0156; Crabb JW, 2002, PROTEIN SCI, V11, P831, DOI 10.1110/ps.4400102; da Silveira VC, 2009, J INORG BIOCHEM, V103, P1331, DOI 10.1016/j.jinorgbio.2009.05.015; Dalle-Donne I, 2007, FREE RADICAL BIO MED, V42, P583, DOI 10.1016/j.freeradbiomed.2006.11.026; Damsten MC, 2007, DRUG METAB DISPOS, V35, P1408, DOI 10.1124/dmd.106.014233; Dechraoui MYB, 2007, TOXICON, V50, P825, DOI 10.1016/j.toxicon.2007.06.013; Fasano M, 2005, IUBMB LIFE, V57, P787, DOI 10.1080/15216540500404093; Fenaille F, 2003, J AM SOC MASS SPECTR, V14, P215, DOI 10.1016/S1044-0305(02)00911-X; Flewelling LJ, 2005, NATURE, V435, P755, DOI 10.1038/nature435755a; FRIGUET B, 1994, J BIOL CHEM, V269, P21639; Harris R, 1996, ANALYST, V121, P913, DOI 10.1039/an9962100913; Hinton M, 2008, MAR ECOL PROG SER, V356, P251, DOI 10.3354/meps07267; Kinter M., 2000, PROTEIN SEQUENCING I, P161; Landsberg JH, 2009, HARMFUL ALGAE, V8, P598, DOI 10.1016/j.hal.2008.11.010; LIN YY, 1981, J AM CHEM SOC, V103, P6773, DOI 10.1021/ja00412a053; Noort D, 1999, CHEM RES TOXICOL, V12, P715, DOI 10.1021/tx9900369; Pierce RH, 2005, HARMFUL ALGAE, V4, P965, DOI 10.1016/j.hal.2004.11.004; Plakas SM, 2004, TOXICON, V44, P677, DOI 10.1016/j.toxicon.2004.07.027; Plakas SM, 2010, TOXICON, V56, P137, DOI 10.1016/j.toxicon.2009.11.007; Pournamdari M, 2009, ANAL CHIM ACTA, V633, P216, DOI 10.1016/j.aca.2008.11.070; Radwan FFY, 2005, TOXICOL SCI, V85, P839, DOI 10.1093/toxsci/kfi138; Ramsdell John S., 2008, P519; Requena JR, 1997, BIOCHEM J, V322, P317, DOI 10.1042/bj3220317; Roth PB, 2007, TOXICON, V50, P1175, DOI 10.1016/j.toxicon.2007.08.003; Selwood AI, 2008, CHEM RES TOXICOL, V21, P944, DOI 10.1021/tx700441w; SHIMIZU Y, 1986, J AM CHEM SOC, V108, P514, DOI 10.1021/ja00263a031; Skipper PL, 1996, CHEM RES TOXICOL, V9, P918, DOI 10.1021/tx960028h; Starkenmann C, 2003, J AGR FOOD CHEM, V51, P7146, DOI 10.1021/jf0304268; Szapacs ME, 2006, BIOCHEMISTRY-US, V45, P10521, DOI 10.1021/bi060535q; SZWEDA LI, 1993, J BIOL CHEM, V268, P3342; Törnqvist M, 2002, J CHROMATOGR B, V778, P279, DOI 10.1016/S1570-0232(02)00172-1; UCHIDA K, 1992, P NATL ACAD SCI USA, V89, P4544, DOI 10.1073/pnas.89.10.4544; Walsh CJ, 2010, AQUAT TOXICOL, V97, P293, DOI 10.1016/j.aquatox.2009.12.014; Walsh CJ, 2009, TOXICON, V53, P135, DOI 10.1016/j.toxicon.2008.10.024; Wang ZH, 2004, TOXICON, V43, P455, DOI 10.1016/j.toxicon.2004.02.017; Woofter R, 2003, ENVIRON HEALTH PERSP, V111, P1595, DOI 10.1289/ehp.6166; Woofter RT, 2007, TOXICON, V49, P1010, DOI 10.1016/j.toxicon.2007.01.011; Woofter RT, 2005, ENVIRON HEALTH PERSP, V113, P1491, DOI 10.1289/ehp.8010; Woofter RT, 2005, ENVIRON HEALTH PERSP, V113, P11, DOI 10.1289/ehp.7274	45	22	24	2	32	AMER CHEMICAL SOC	WASHINGTON	1155 16TH ST, NW, WASHINGTON, DC 20036 USA	0893-228X	1520-5010		CHEM RES TOXICOL	Chem. Res. Toxicol.	JAN	2011	24	1					54	64		10.1021/tx1002854	http://dx.doi.org/10.1021/tx1002854			11	Chemistry, Medicinal; Chemistry, Multidisciplinary; Toxicology	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy; Chemistry; Toxicology	705LO	21142195				2025-03-11	WOS:000286130100007
J	Sluijs, A; Bijl, PK; Schouten, S; Röhl, U; Reichart, GJ; Brinkhuis, H				Sluijs, A.; Bijl, P. K.; Schouten, S.; Roehl, U.; Reichart, G. -J.; Brinkhuis, H.			Southern ocean warming, sea level and hydrological change during the Paleocene-Eocene thermal maximum	CLIMATE OF THE PAST			English	Article							CARBON-ISOTOPE EXCURSION; DINOFLAGELLATE CYSTS; SURFACE TEMPERATURES; SOUTHWEST PACIFIC; MEMBRANE-LIPIDS; METHANE HYDRATE; ORGANIC-MATTER; GLOBAL CARBON; BIGHORN BASIN; ARCTIC-OCEAN	A brief (similar to 150 kyr) period of widespread global average surface warming marks the transition between the Paleocene and Eocene epochs, similar to 56 million years ago. This so-called "Paleocene-Eocene thermal maximum" (PETM) is associated with the massive injection of C-13-depleted carbon, reflected in a negative carbon isotope excursion (CIE). Biotic responses include a global abundance peak (acme) of the subtropical dinoflagellate Apectodinium. Here we identify the PETM in a marine sedimentary sequence deposited on the East Tasman Plateau at Ocean Drilling Program (ODP) Site 1172 and show, based on the organic paleothermometer TEX86, that southwest Pacific sea surface temperatures increased from similar to 26 degrees C to similar to 33 degrees C during the PETM. Such temperatures before, during and after the PETM are >10 degrees C warmer than predicted by paleoclimate model simulations for this latitude. In part, this discrepancy may be explained by potential seasonal biases in the TEX86 proxy in polar oceans. Additionally, the data suggest that not only Arctic, but also Antarctic temperatures may be underestimated in simulations of ancient greenhouse climates by current generation fully coupled climate models. An early influx of abundant Apectodinium confirms that environmental change preceded the CIE on a global scale. Organic dinoflagellate cyst assemblages suggest a local decrease in the amount of river run off reaching the core site during the PETM, possibly in concert with eustatic rise. Moreover, the assemblages suggest changes in seasonality of the regional hydrological system and storm activity. Finally, significant variation in dinoflagellate cyst assemblages during the PETM indicates that southwest Pacific climates varied significantly over time scales of 10(3)-10(4) years during this event, a finding comparable to similar studies of PETM successions from the New Jersey Shelf.	[Sluijs, A.; Bijl, P. K.; Brinkhuis, H.] Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Schouten, S.] Royal Netherlands Inst Sea Res NIOZ, Dept Marine Organ Biogeochem, Den Burg, Texel, Netherlands; [Roehl, U.] Univ Bremen, Marum Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Reichart, G. -J.] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bremen; Utrecht University	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Lab Palaeobot & Palynol, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	A.Sluijs@uu.nl	Brinkhuis, Henk/B-4223-2009; Schouten, Stefan/P-4380-2016; Rohl, Ursula/G-5986-2011; Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018	Brinkhuis, Henk/0000-0003-0253-6610; Rohl, Ursula/0000-0001-9469-7053; Sluijs, Appy/0000-0003-2382-0215; Bijl, Peter/0000-0002-1710-4012; Reichart, Gert-Jan/0000-0002-7256-2243	Netherlands Organisation for Scientific Research [863.07.001]; NWO-Vici grant; Deutsche Forschungsgemeinschaft (DFG); LPP Foundation; European Research Council under the European Community [259627]	Netherlands Organisation for Scientific Research(Netherlands Organization for Scientific Research (NWO)); NWO-Vici grant(Netherlands Organization for Scientific Research (NWO)); Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); LPP Foundation; European Research Council under the European Community(European Research Council (ERC))	This research used samples and data provided by the Ocean Drilling Program (ODP). Funding for this research was provided by the Netherlands Organisation for Scientific Research to AS (NWO-Veni grant 863.07.001) and SS (NWO-Vici grant), by the Deutsche Forschungsgemeinschaft (DFG) to UR, and by the LPP Foundation to PKB. AS acknowledges the European Research Council under the European Community's Seventh Framework Program for ERC Starting Grant 259627. We thank Dorian Abbot, Jerry Dickens, and Chris Hollis for constructive reviews, Thorsten Kiefer for editorial handling, and Arnold van Dijk, Jan van Tongeren, Natasja Welters (Utrecht University) and Ellen Hopmans and Jort Ossebaar (Royal NIOZ) for technical support.	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Past.		2011	7	1					47	61		10.5194/cp-7-47-2011	http://dx.doi.org/10.5194/cp-7-47-2011			15	Geosciences, Multidisciplinary; Meteorology & Atmospheric Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Meteorology & Atmospheric Sciences	743CC		Green Submitted, Green Published, gold			2025-03-11	WOS:000288992700005
J	Villanueva-Amadoz, U; Sender, LM; Diez, JB; Ferrer, J; Pons, D				Villanueva-Amadoz, Uxue; Miguel Sender, Luis; Bienvenido Diez, Jose; Ferrer, Javier; Pons, Denise			Palynological studies of the boundary marls unit (Albian-Cenomanian) from northeastern Spain. Paleophytogeographical implications	GEODIVERSITAS			English	Article						Palynology; Lower Cretaceous; Albian-Cenomanian boundary; paleophytogeography	CRETACEOUS ANGIOSPERM POLLEN; ELATER-BEARING POLLEN; WESTERN DESERT; WELL; PALYNOSTRATIGRAPHY; ULTRASTRUCTURE; STRATIGRAPHY; EVOLUTION; SEDIMENTS; BRAZIL	Detailed records of spore-pollen assemblages from four sites located in the Aliaga and Oliete Sub-basins provide new insights into the palaeoclimatic and palaeogeographic settings during the Albian-Cenomanian transition in the Maestrazgo Basin (northeastern Spain). Palynological taxa such as Afropollis jardinus Doyle, Jardine & Doerenkamp, 1982, Elaterosporites klaszii (Jardine & Magloire) Jardine, 1967, Equisetosporites ambiguus (Hedlund 1966) Singh, 1983, Gabonisporis pseudoreticulatus Boltenhagen, 1967, Senectotetradites varireticulatus Dettmann, 1973, Stellatopollis barghoornii Doyle, 1975, and the dinoflagellate cyst Cyclonephelium chabaca Below, 1981 indicate a latest Albian age for this unit. Abundance of Gondwanan elements such as Afropollis Doyle, Jardine & Doerenkainp, 1982, Elaterosporites Jardine, 1967 and Stellatopollis Doyle, 1975 indicates a northward extension of the paleogeographic distributions of those taxa during this time. Comparison between the studied microflora of the Iberian Range and microfloras from Tethyan and Gondwanan realms allows better understanding of the Tethyan paleogeographic setting.	[Villanueva-Amadoz, Uxue] Univ Nacl Autonoma Mexico, Dept Paleontol, Inst Geol, Mexico City 04510, DF, Mexico; [Miguel Sender, Luis; Ferrer, Javier] Univ Zaragoza, Dept Ciencias Tierra Paleontol, SP-50009 Zaragoza, Spain; [Bienvenido Diez, Jose] Univ Vigo, Dept Geociencias Marinas & Ordenac Terr, SP-36200 Vigo, Pontevedra, Spain; [Pons, Denise] Univ Paris 06, UMR 7207, Ctr Rech Paleobiodivers & Paleoenvironm CR2P, Museum Natl Hist Nat, F-75231 Paris 05, France	Universidad Nacional Autonoma de Mexico; University of Zaragoza; Universidade de Vigo; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Museum National d'Histoire Naturelle (MNHN)	Villanueva-Amadoz, U (通讯作者)，Univ Nacl Autonoma Mexico, Dept Paleontol, Inst Geol, Ciudad Univ, Mexico City 04510, DF, Mexico.	uxuevillanueva@yahoo.es; lmsender@unizar.es; jbdiez@uvigo.es; joferrer@unizar.es; dpons@snv.jussieu.fr	Sender, Luis/HJB-3337-2022; Villanueva-Amadoz, Uxue/G-9899-2015; Diez, Jose B./L-1004-2014	Sender, Luis Miguel/0000-0002-7279-049X; Villanueva Amadoz, Uxue/0000-0002-5189-5911; Diez, Jose B./0000-0001-5739-7270	Spanish Project [CGL2008-00809/BTE]; Mexican Project [CONACYT 104515]; Gobierno de Navarra; Caja de Ahorros de la Inmaculada (CM); Aragon Government	Spanish Project(Spanish Government); Mexican Project; Gobierno de Navarra(Spanish Government); Caja de Ahorros de la Inmaculada (CM); Aragon Government(Gobierno de Aragon)	This study was supported by the Spanish Project CGL2008-00809/BTE, Mexican Project CONACYT 104515 and a fellowship award to U.V.A. funded by the Gobierno de Navarra. The authors thank the Caja de Ahorros de la Inmaculada (CM) for research travel grants and the Aragon Government for field grants. The authors also wish to express their gratitude to the Paleobotanist Group of Centre de Recherche en Paleobiodiversite et Paleoenvironnements for providing logistic assistance and access to optical microscopy equipment (UMR 7207-UPMC-CNRS-MNHN) and Suso Mendez from the CACTI (University of Vigo) for his help in getting the electron microscopic images. We are also grateful to James A. Doyle and David J. Batten for suggestions and substantial improvements in the manuscript.	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J	De Schutter, PJ				De Schutter, Pieter J.			<i>CARCHARIAS VORAX</i> (LE HON, 1871) (CHONDRICHTHYES, LAMNIFORMES), FROM THE MIOCENE OF BELGIUM: REDESCRIPTION AND DESIGNATION OF A NEOTYPE AND PARANEOTYPE	GEOLOGICA BELGICA			English	Article						Elasmobranchii; Odontaspididae; cuspidatus; sandtiger shark; Antwerpen Sands Member; North Sea Basin	NORTH-SEA BASIN; DINOFLAGELLATE CYST; MIDDLE; PALEOENVIRONMENT; STRATIGRAPHY; NEOGENE; SHARKS	Carcharias vorax (Le Hon, 1871) is poorly defined with one single tooth only. The holotype could not be found in the Type Collection of the IRScNB (Brussels) and recognition of the holotype is impossible based on the poor drawing in Le Hon (1871). A neotype and paraneotype are designated for the lost holotype. A temporary outcrop at a construction site southeast of the city of Antwerp is chosen as type locality. The basal part of the Middle Miocene Antwerpen Sands Member is selected as type horizon. An artificial tooth set is constructed and illustrated, confirming the attribution of this species to the genus Carcharias. Carcharias vorax (Le Hon, 1871) appears to be closely related to Carcharias cuspidatus (Agassiz, 1843) and seems to have a restricted geographical and temporal distribution, focused on the North Sea Basin only during the Burdigalian-Tortonian interval. The disappearance of Carcharias vorax during the Late Miocene is discussed. A maximum total body length of approximately 280 cm is estimated for this Miocene shark species.			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Belg.		2011	14	3-4					175	191						17	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	850GF					2025-03-11	WOS:000297182400005
S	Mudie, PJ; Leroy, SAG; Marret, F; Gerasimenko, NP; Kholeif, SEA; Sapelko, T; Filipova-Marinova, M		Buynevich, IV; YankoHombach, V; Gilbert, AS; Martin, RE		Mudie, P. J.; Leroy, S. A. G.; Marret, F.; Gerasimenko, N. P.; Kholeif, S. E. A.; Sapelko, T.; Filipova-Marinova, M.			Nonpollen palynomorphs: Indicators of salinity and environmental change in the Caspian-Black Sea-Mediterranean corridor	GEOLOGY AND GEOARCHAEOLOGY OF THE BLACK SEA REGION: BEYOND THE FLOOD HYPOTHESIS	Geological Society of America Special Papers		English	Article; Book Chapter							NON-POLLEN PALYNOMORPHS; DINOFLAGELLATE CYST ASSEMBLAGES; ST-ERTH BEDS; AEGEAN SEA; PALYNOLOGICAL EVIDENCE; LATE PLEISTOCENE; RECENT SEDIMENTS; ORGANIC-MATTER; HOLOCENE; LAKE	Previous palynological studies of the Caspian-Black Sea-Mediterranean corridor primarily focused on pollen and spores for paleoecological and chronostratigraphic studies. Until recently, there has been less emphasis on the nonpollen palynomorphs, such as dinoflagellate cysts, algal and fungal spores, and animal remains. New studies of nonpollen palynomorphs in land-locked seas, estuaries, and lakes reported here indicate that they are important markers of salinity, nutrient loading, and human activity, including ballast discharge, farming, and soil erosion. We describe the nonoxidative laboratory processing methods necessary to extract nonpollen palynomorphs from marine-and brackish-water sediment samples. We list 48 nonpollen palynomorphs taxa from 37 surface sediments (including the past millennium) for cores along the salinity gradient from <16% off the Danube Delta to >39% in the Aegean, Mediterranean, and Red Seas, for two Crimean saline lakes, the Caspian and Aral Seas, and for lakes in Iran and Kazakhstan. The main nonpollen palynomorphs taxa are illustrated and listed systematically to provide a baseline for future collaborative studies among Black Sea corridor palynologists. We outline the biological affinities of some nonpollen palynomorphs and discuss the initial results of the study in terms of what nonpollen palynomorphs may reveal about the history of the salinity in the Black Sea corridor and the impact of humans on soil erosion, plankton production, and harmful algal blooms.	[Mudie, P. J.] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Leroy, S. A. G.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Marret, F.] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Gerasimenko, N. P.] Natl Taras Shevchenko Univ Kyiv, Earth Sci & Geomorphol Dept, Kiev, Ukraine; [Kholeif, S. E. A.] Natl Inst Oceanog & Fisheries Egypt, Alexandria, Egypt; [Sapelko, T.] Russian Acad Sci, Inst Limnol, St Petersburg 196105, Russia; [Filipova-Marinova, M.] Museum Nat Hist, Varna 9000, Bulgaria	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Brunel University; University of Liverpool; Ministry of Education & Science of Ukraine; Taras Shevchenko National University of Kyiv; Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF); Russian Academy of Sciences; St. Petersburg Federal Research Center of the Russian Academy of Sciences; St. Petersburg Scientific Centre of the Russian Academy of Sciences; St. Petersburg Scientific Centre Institute of Limnology	Mudie, PJ (通讯作者)，Geol Survey Canada Atlantic, Box 1006, Dartmouth, NS B2Y 4A2, Canada.	mudiep@ns.sympatico.ca; suzanne.leroy@brunel.ac.uk; marret@liv.ca.uk; geras@gu.kiev.ua; Suzan_Kholeif@yahoo.com; tsapelko@mail.ru; marianafilipova@yahoo.com	Leroy, Suzanne/D-3996-2009; Gerasimenko, Natalia/I-1427-2018; Sapelko, Tatyana/K-2575-2018	Gerasimenko, Natalia/0000-0001-9278-5770; Filipova-Marinova, Mariana/0000-0002-0786-9476; Marret-Davies, Fabienne/0000-0003-4244-0437				AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; Aksu AE, 1999, MAR GEOL, V153, P303, DOI 10.1016/S0025-3227(98)00077-2; ALADIN NV, 1992, HYDROBIOLOGIA, V237, P67, DOI 10.1007/BF00016032; [Anonymous], OCEANOGR MAR BIOL AN; Atanassova J, 2005, HOLOCENE, V15, P576, DOI 10.1191/0959683605hl832rp; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Batten D.J., 1996, Palynology: principles and applications, P205; Berard-Therriault L., 1999, SCIENCES, V128, P387; Beyens Louis, 2001, Developments in Paleoenvironmental Research, V3, P121; Brenner W.W., 2001, BALTICA, V14, P40; Brenner Wolfram W., 2006, Meyniana, V58, P33; Brenner WW, 2005, PALAEOGEOGR PALAEOCL, V220, P227, DOI 10.1016/j.palaeo.2004.12.010; Bryant V.M., 1983, ADV ARCHAEOL METH TH, V6, P191, DOI DOI 10.1016/B978-0-12-003106-1.50010-9; Bryant VM, 1998, AM ASS STRATIGRAPHIC, V33; Chmura GL, 2006, REV PALAEOBOT PALYNO, V141, P103, DOI 10.1016/j.revpalbo.2006.03.019; CHRISTOPHER R A, 1976, Micropaleontology (New York), V22, P143, DOI 10.2307/1485396; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dawes C. 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B	Nagai, S; Yoshida, G; Tarutani, K		Casalegno, S		Nagai, Satoshi; Yoshida, Goro; Tarutani, Kenji			Change in Species Composition and Distribution of Algae in the Coastal Waters of Western Japan	GLOBAL WARMING IMPACTS - CASE STUDIES ON THE ECONOMY, HUMAN HEALTH, AND ON URBAN AND NATURAL ENVIRONMENTS			English	Article; Book Chapter							SETO-INLAND-SEA; DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; HIROSHIMA-BAY; NORTH PACIFIC; GONYAULAX-TAMARENSIS; RESTING CYSTS; DINOPHYCEAE; TAMIYAVANICHII; COHORTICULA; PHENOLOGY		[Nagai, Satoshi] Natl Res Inst Fisheries & Environm Inland Sea, Res Ctr Environm Conservat, Fisheries Res Agcy, Hatsukaichi, Hiroshima, Japan; [Yoshida, Goro; Tarutani, Kenji] Natl Res Inst Fisheries & Environm Inland Sea, Coastal Fisheries & Environm Div, Fisheries Res Agcy, Hatsukaichi, Hiroshima, Japan	Japan Fisheries Research & Education Agency (FRA); Japan Fisheries Research & Education Agency (FRA)	Nagai, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Res Ctr Environm Conservat, Fisheries Res Agcy, Hatsukaichi, Hiroshima, Japan.		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J	Grímsson, F; Zetter, R; Baal, C				Grimsson, Frigeir; Zetter, Reinhard; Baal, Christian			Combined LM and SEM study of the Middle Miocene (Sarmatian) palynoflora from the Lavanttal Basin, Austria: Part I. Bryophyta, Lycopodiophyta, Pteridophyta, Ginkgophyta, and Gnetophyta	GRANA			English	Article						Cainozoic; Carinthia; fossils; Northern Hemisphere; palynomorphs; phosphoritic nodules; pollen; spores	EASTERN ALPS; NONMARINE DIATOMS; VEGETATION; POLLEN; EOCENE; LAKE; BACILLARIOPHYCEAE; STRATIGRAPHY; CALIBRATION; ASSEMBLAGE	Preliminary studies of the palynoflora from the Lavanttal Basin show a relatively rich assemblage of pollen and spores. The palynoflora comprises at least 17 different kinds of spores, representing the Bryophyta (Sphagnum), Lycopodiophyta (Lycopodium, Selaginella), and the Pteridophyta (Dryopteris, Osmunda, Pteris), about 20 different pollen types of conifers assignable to Cupressaceae and Pinaceae, and 130-160 different kinds of angiosperm pollen. In this study, we describe all spores together with pollen from two seed plants, i.e. Ginkgo (Ginkgophyta) and Ephedra (Gnetophyta). The fossil spores and pollen grains are preserved in phosphoritic nodules. Absence of palynomorphs characteristic of marine settings and presence of numerous freshwater algae (diatoms, dinoflagellates, and different green algae) indicate freshwater environments. This is also supported by sedimentological observations suggestive of wetland surroundings, characterised by lakes, swamps, streams, rivers and floodplain areas. The taxa reported here all seem to represent part of azonal vegetation with plants growing in swamps, on hummocks, along border of lakes or streams, on levees, or on sandy patches of floodplains. Preliminary results suggest that the vegetation thrived under a relatively warm and humid climate.	[Grimsson, Frigeir; Zetter, Reinhard; Baal, Christian] Univ Vienna, Dept Palaeontol, A-1090 Vienna, Austria	University of Vienna	Grímsson, F (通讯作者)，Univ Vienna, Dept Palaeontol, Althanstr 14,UZA 2, A-1090 Vienna, Austria.	fridgeir.grimsson@univie.ac.at	Grimsson, Fridgeir/A-9943-2012	Zetter, Reinhard/0000-0002-0220-6921; Grimsson, Fridgeir/0000-0002-1874-6412	FWF (Austrian Science Foundation) [M 1181-B17]	FWF (Austrian Science Foundation)(Austrian Science Fund (FWF))	The authors wish to thank the FWF (Austrian Science Foundation) for granting FG with a Lise-Meitner-grant (project number M 1181-B17) that made this study possible. They are also grateful to Christa-Charlotte Hofmann, Hugh Rice, and Thomas Denk for reading over and improving the manuscript. 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J	Tobin, ED; Horner, RA				Tobin, Elizabeth D.; Horner, Rita A.			Germination characteristics of <i>Alexandrium catenella</i> cysts from surface sediments in Quartermaster Harbor, Puget Sound, Washington, USA	HARMFUL ALGAE			English	Article						Alexandrium catenella; Dinoflagellate; Cyst; Puget sound; Germination; Mandatory dormancy	GENETIC-MARKERS; RESTING CYSTS; DINOPHYCEAE; IDENTIFICATION; EXCYSTMENT	The dinoflagellate Alexandrium catenella causes frequent outbreaks of paralytic shellfish toxins (PSTs) in Puget Sound, Washington; however, little is known about its basic biology and ecology. Most of what is known is inferred mainly from shellfish toxin records and recent work on cyst distribution and germination potential. We report on a year-long study of cyst dormancy and germination potential based on experiments using surface sediment collected from a shallow embayment, Quartermaster Harbor, in Puget Sound. Cyst abundance in Quartermaster Harbor was 1550-1750 cysts cm(-3) when sediment was collected in mid-October 2006. Germination experiments set up monthly had germination occur in all months when cysts were provided with adequate growth supporting conditions. Germination rates were highest in May and June when 100% germination occurred within 2 days. Longer incubation periods observed for the first two months of the study (November and December) may indicate a mandatory dormancy period of up to 5 months if the majority of cysts were deposited in the sediments following a late summer bloom that apparently occurred in Quartermaster Harbor in 2006 as indicated by Washington State Department of Health's toxin records. The data provide no evidence of an endogenous clock restricting germination to a specific annual timeframe for these shallow water cysts. This contrasts with the presence of a circannual endogenous clock, for deep water cysts of A. fundyense in the Gulf of Maine. The significance of these results is that germination of the A. catenella Puget Sound population appears to be primarily regulated by physiological requirements. However, once physiological requirements are met cysts can germinate rapidly, often within 24 h, when provided with adequate environmental conditions. (C) 2010 Elsevier B.V. All rights reserved.	[Tobin, Elizabeth D.; Horner, Rita A.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA	University of Washington; University of Washington Seattle	Tobin, ED (通讯作者)，Univ Washington, Sch Oceanog, Box 357940, Seattle, WA 98195 USA.	etobin@u.washington.edu			National Oceanic and Atmospheric Administration (NOAA) [NA04NOS4780273]; NOM Washington State Sea Grant [NA040AR170032]	National Oceanic and Atmospheric Administration (NOAA)(National Oceanic Atmospheric Admin (NOAA) - USA); NOM Washington State Sea Grant	This paper was partially funded by the National Oceanic and Atmospheric Administration (NOAA) Coastal Ocean Program under award #NA04NOS4780273 and by the NOM Washington State Sea Grant #NA040AR170032 to the University of Washington. This is ECOHAB contribution #321. We thank the captain and crew of the R.V. Clifford, A. Barnes, R. McQuin, and N. Milonas, members of the scientific party, C. Greengrove, J. Postel, T. Bjorkman, UW students, K. Holtermann, and M. Ewert-Sarmiento, for help with sediment collection. We would also like to thank E. Lessard and D. 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Copenhagen: International Society for the Study of Harmful Algae and Intergovernmental Oceanographic Commission of UNESCO, P196; Figueroa RI, 2006, J PHYCOL, V42, P1028, DOI 10.1111/j.1529-8817.2006.00262.x; Joyce LB, 2006, AFR J MAR SCI, V28, P295, DOI 10.2989/18142320609504165; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; NISHITANI L, 1984, AQUACULTURE, V39, P317, DOI 10.1016/0044-8486(84)90274-6; 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; SCHOLIN CA, 1994, J PHYCOL, V30, P744, DOI 10.1111/j.0022-3646.1994.00744.x; SCHOLIN CA, 1993, DEV MAR BIO, V3, P95; TAYLOR FJR, 1984, ACS SYM SER, V262, P77; Trainer VL, 2003, J SHELLFISH RES, V22, P213; YAMAGUCHI M, 1995, PHYCOLOGIA, V34, P207, DOI 10.2216/i0031-8884-34-3-207.1	24	14	19	2	24	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JAN	2011	10	2					216	223		10.1016/j.hal.2010.10.002	http://dx.doi.org/10.1016/j.hal.2010.10.002			8	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	714XP					2025-03-11	WOS:000286845300012
C	de Vernal, A; Rochon, A		StOnge, G; VeigaPires, C; Solignac, S		de Vernal, Anne; Rochon, Andre			Dinocysts as tracers of sea-surface conditions and sea-ice cover in polar and subpolar environments	IODP-CANADA SUMMER SCHOOL ON OCEAN AND CLIMATE CHANGES IN POLAR AND SUBPOLAR ENVIRONMENTS	IOP Conference Series-Earth and Environmental Science		English	Proceedings Paper	IODP-Canada Summer School on Ocean and Climate Changes in Polar and Subpolar Environments	JUN 27-JUL 12, 2010	CANADA	Integrated Ocean Drilling Program, European Consortium Ocean Drilling Program, Canadian Consortium Ocean Drilling, Network Univ Quebec, Univ Quebec Montreal, Geochemistry & Geodynam Res Ctr, UQAM, Univ Quebec Rimouski, Inst Sci Mer Rimouski, Univ Quebec, Univ Avant Garde, Inst Natl Rech Sci, Geol Survey Canada			DINOFLAGELLATE CYST ASSEMBLAGES; LATE QUATERNARY; NORTHERN-HEMISPHERE; HIGH-LATITUDES; ATLANTIC; HOLOCENE; OCEAN; RECONSTRUCTION; PRODUCTIVITY; MICROFOSSILS	Dinoflagellates are unicellular protists that produce a cyst (dinocyst) as part of their life cycle. The cyst wall of many species is composed of highly resistant organic matter. Dinocysts are thus routinely recovered in marine sediments and occur in high number along the continental margins of the world oceans notably in high latitude environments. They are widely used as proxy indicators of marine conditions and provide valuable information on the natural variability of climate, which in turn helps understanding and assessing the potential threat posed by the actual global warming. Here we present a brief outline of their biology, ecology and distribution in Arctic and subarctic areas. We also provide a few examples of paleoenvironmental reconstructions and briefly discuss on the significance of these results.	[de Vernal, Anne] Univ Quebec, GEOTOP, POB 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada; [Rochon, Andre] Univ Quebec, ISMER, GEOTOP, Rimouski, PQ G5L 3A1, Canada	University of Quebec; University of Quebec Montreal; University of Quebec	de Vernal, A (通讯作者)，Univ Quebec, GEOTOP, POB 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	devernal.anne@uqam.ca	de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X				Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; [Anonymous], CANOCO REFERENCE MAN; [Anonymous], NEOGENE QUATERNARY D; Bonnet S, 2010, MAR MICROPALEONTOL, V74, P59, DOI 10.1016/j.marmicro.2009.12.001; 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, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; de Vernal A, 2007, ENCY QUATERNARY SCI, P1653; de Vernal A, 2006, GLOBAL PLANET CHANGE, V54, P263, DOI 10.1016/j.gloplacha.2006.06.023; de Vernal A, 2008, GEOPHYS MONOGR SER, V180, P27, DOI 10.1029/180GM04; Fensome R.A., 1993, Micropaleontology Press Special Paper; Guiot J, 2007, DEV MARINE GEOL, V1, P523, DOI 10.1016/S1572-5480(07)01018-4; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Kokinos JP, 1998, ORG GEOCHEM, V28, P265, DOI 10.1016/S0146-6380(97)00134-4; Ledu D, 2010, PALEOCEANOGRAPHY, V25, DOI 10.1029/2009PA001817; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Marret F, 2001, CAN J EARTH SCI, V38, P373, DOI 10.1139/e00-092; Marret F, 2001, J QUATERNARY SCI, V16, P739, DOI 10.1002/jqs.648; Matthiessen J, 2001, GLOBAL PLANET CHANGE, V31, P65, DOI 10.1016/S0921-8181(01)00113-8; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; McKay JL, 2008, CAN J EARTH SCI, V45, P1377, DOI 10.1139/E08-046; Radi T, 2008, MAR MICROPALEONTOL, V68, P84, DOI 10.1016/j.marmicro.2008.01.012; REID PC, 1975, NEW PHYTOL, V75, P589, DOI 10.1111/j.1469-8137.1975.tb01425.x; Rochon A., 1999, American Association of Stratigraphic Palynologists Contributions Series, V35, P1, DOI DOI 10.1016/0377-8398(94)00016-G; Solignac S, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001175	26	9	10	0	3	IOP PUBLISHING LTD	BRISTOL	DIRAC HOUSE, TEMPLE BACK, BRISTOL BS1 6BE, ENGLAND	1755-1307			IOP C SER EARTH ENV	IOP Conf. Ser. Earth Envir. Sci.		2011	14								012007	10.1088/1755-1315/14/1/012007	http://dx.doi.org/10.1088/1755-1315/14/1/012007			12	Geosciences, Multidisciplinary; Oceanography; Paleontology	Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Oceanography; Paleontology	BHX76		Bronze			2025-03-11	WOS:000326961700007
J	von Dassow, P; Montresor, M				von Dassow, Peter; Montresor, Marina			Unveiling the mysteries of phytoplankton life cycles: patterns and opportunities behind complexity	JOURNAL OF PLANKTON RESEARCH			English	Article						phytoplankton; genomics; life cycle; evolution	PROGRAMMED CELL-DEATH; DIATOM THALASSIOSIRA-WEISSFLOGII; MARINE PLANKTONIC DIATOM; SEXUAL REPRODUCTION; PUNGENS BACILLARIOPHYCEAE; POPULATION-DYNAMICS; EMILIANIA-HUXLEYI; OXIDATIVE STRESS; RESTING CYSTS; DINOFLAGELLATE	Life cycles of phytoplankton species have been selected over a long evolutionary history and represent a key element for our understanding of their ecology and natural history and for improving our comprehension of ocean functioning. A species can alternate in its life cycle between four distinct major phases: growth, sex, quiescence and cell death. This implies that the population of a phytoplankton species found in any particular water sample will contain cells that undergo different fates, have strong differentiation in physiology and have different functional roles even if they are genetically identical. The factors regulating transitions among the different phases are still largely unknown but have direct impacts on the ecological distribution of species and on their biogeochemical function. Focused research efforts in recent years have begun to reveal emerging patterns in the variability of phytoplankton life cycle traits. This research has relied both on careful observations in culture and at sea and on making use of new genomics- and transcriptomics-based tools. The study of phytoplankton in the context of their life cycle characteristics opens up new opportunities to address fundamental questions about the physiology and cell biology of these important organisms and creates a new evolutionary and ecological framework for defining phytoplankton functional groups.	[von Dassow, Peter] Pontificia Univ Catolica Chile, Fac Ciencias Biol, Dept Ecol, Santiago, Chile; [Montresor, Marina] Stn Zool Anton Dohrn, I-80121 Naples, Italy	Pontificia Universidad Catolica de Chile; Stazione Zoologica Anton Dohrn	von Dassow, P (通讯作者)，Pontificia Univ Catolica Chile, Fac Ciencias Biol, Dept Ecol, Ave Bernardo OHiggins 340, Santiago, Chile.	pvondassow@bio.puc.cl	von Dassow, Peter/JXW-7856-2024	Montresor, Marina/0000-0002-2475-1787; von Dassow, Peter/0000-0002-1858-1953				Amato A, 2005, J PHYCOL, V41, P542, DOI 10.1111/j.1529-8817.2005.00080.x; Amato A, 2007, PROTIST, V158, P193, DOI 10.1016/j.protis.2006.10.001; [Anonymous], 2007, EVOLUTION PRIMARY PR; [Anonymous], 2002, PHYTOPLANKTON PRODUC; Armbrust EV, 1999, APPL ENVIRON MICROB, V65, P3121; Bell G, 2005, J EVOLUTION BIOL, V18, P722, DOI 10.1111/j.1420-9101.2004.00830.x; Bidle KD, 2008, EUKARYOT CELL, V7, P223, DOI 10.1128/EC.00296-07; Bidle KD, 2004, NAT REV MICROBIOL, V2, P643, DOI 10.1038/nrmicro956; Brodie Juliet., 2007, Unravelling the Algae: The past, Present, and Future of Algal Systematics; Brosnahan ML, 2010, DEEP-SEA RES PT II, V57, P175, DOI 10.1016/j.dsr2.2009.09.005; CANTER HM, 1979, NEW PHYTOL, V82, P187, DOI 10.1111/j.1469-8137.1979.tb07574.x; Casteleyn G, 2009, MAR BIOL, V156, P1149, DOI 10.1007/s00227-009-1157-6; Chepurnov VA, 2004, INT REV CYTOL, V237, P91; Chepurnov VA, 2008, BIOESSAYS, V30, P692, DOI 10.1002/bies.20773; Chepurnov VA, 2006, J PHYCOL, V42, P845, DOI 10.1111/j.1529-8817.2006.00244.x; Coelho SM, 2007, GENE, V406, P152, DOI 10.1016/j.gene.2007.07.025; CRAWFORD RM, 1995, LIMNOL OCEANOGR, V40, P200, DOI 10.4319/lo.1995.40.1.0200; Cros L, 2002, THESIS U BARCELONA; D'Alelio D, 2010, LIMNOL OCEANOGR, V55, P106, DOI 10.4319/lo.2010.55.1.0106; Derelle E, 2006, P NATL ACAD SCI USA, V103, P11647, DOI 10.1073/pnas.0604795103; Ejercito M, 2003, J EUKARYOT MICROBIOL, V50, P427, DOI 10.1111/j.1550-7408.2003.tb00268.x; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Frada M, 2008, P NATL ACAD SCI USA, V105, P15944, DOI 10.1073/pnas.0807707105; Franklin DJ, 2006, EUR J PHYCOL, V41, P1, DOI 10.1080/09670260500505433; Fukuda Y, 2006, EUR J PROTISTOL, V42, P209, DOI 10.1016/j.ejop.2006.05.003; Graham L.E., 2000, Algae; Grimsley N, 2010, MOL BIOL EVOL, V27, P47, DOI 10.1093/molbev/msp203; Haag CR, 2007, GENETICS, V176, P1663, DOI 10.1534/genetics.107.073080; Hadany L, 2009, AM NAT, V174, pS71, DOI 10.1086/599086; Holtermann KE, 2010, J PHYCOL, V46, P41, DOI 10.1111/j.1529-8817.2009.00792.x; Honda D, 2007, PROTIST, V158, P77, DOI 10.1016/j.protis.2006.08.004; Houdan A, 2005, MAR ECOL PROG SER, V292, P139, DOI 10.3354/meps292139; Houdan A, 2006, AQUAT MICROB ECOL, V44, P291, DOI 10.3354/ame044291; Figueroa RI, 2006, J PHYCOL, V42, P1028, DOI 10.1111/j.1529-8817.2006.00262.x; Figueroa RI, 2010, DEEP-SEA RES PT II, V57, P190, DOI 10.1016/j.dsr2.2009.09.016; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Jones SE, 2010, P NATL ACAD SCI USA, V107, P5881, DOI 10.1073/pnas.0912765107; Kobayashi T, 2005, FEBS J, V272, P5378, DOI 10.1111/j.1742-4658.2005.04936.x; Koester JA, 2010, BMC EVOL BIOL, V10, DOI 10.1186/1471-2148-10-1; Kooistra Wiebe H. 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Plankton Res.	JAN	2011	33	1					3	12		10.1093/plankt/fbq137	http://dx.doi.org/10.1093/plankt/fbq137			10	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	689SG		Bronze			2025-03-11	WOS:000284948600002
J	Kotthoff, U; Koutsodendris, A; Pross, J; Schmiedl, G; Bornemann, A; Kaul, C; Marino, G; Peyron, O; Schiebel, R				Kotthoff, Ulrich; Koutsodendris, Andreas; Pross, Joerg; Schmiedl, Gerhard; Bornemann, Andre; Kaul, Christian; Marino, Gianluca; Peyron, Odile; Schiebel, Ralf			Impact of Lateglacial cold events on the northern Aegean region reconstructed from marine and terrestrial proxy data	JOURNAL OF QUATERNARY SCIENCE			English	Article						land-sea correlation; temperature changes; Heinrich event 1; Younger Dryas; Lateglacial; eastern Mediterranean	LAST DEGLACIATION; MEDITERRANEAN SEA; BLACK-SEA; CLIMATIC OSCILLATIONS; PLANKTIC FORAMINIFERA; DINOFLAGELLATE CYSTS; HOLOCENE CLIMATE; ATLANTIC REGION; WESTERN-EUROPE; SAPROPEL S1	Marine palynomorph data paired with other indicators of sea-surface hydrography (planktic foraminiferal assemblages and oxygen isotopes) were used to decipher the impact of cold events on the northern Aegean region during the last glacial to interglacial transition. The data, which were derived from marine sediment cores GeoTu SL152 and GeoTu SL148, point to a strong impact of the Heinrich 1 and Younger Dryas cold events on surface-water conditions in the northern Aegean Sea. Shifts in marine palynomorph assemblages correlate with changes in terrestrial vegetation and climate (i.e. precipitation and temperature reconstructions based on pollen assemblages) in the northern borderlands of the Aegean Sea. The climate responses of the Aegean region to Heinrich event 1 (H1, ca. 17.5 to ca. 15.7 cal ka BP) and Younger Dryas (ca. 12.6 to ca. 11.7 cal ka BP) events appear similar in magnitude (with mean annual temperatures between similar to 6 and 10 degrees C and mean annual precipitation between similar to 300 and similar to 450 mm). However, the annual temperature decline during the H1 relative to the preceding already cold conditions was minor (<3 degrees C). The transition from the relatively warm and humid local equivalent of the Allerod interstadial to the Younger Dryas, on the other hand, witnessed an annual temperature decline of 6 C and an annual precipitation decrease of 300 mm, the latter occurring abruptly within only ca. 150 a. The return to warmer conditions in the northern Aegean region after the Younger Dryas was completed at ca. 11.6 cal ka BP. Copyright (C) 2011 John Wiley & Sons, Ltd.	[Kotthoff, Ulrich; Schmiedl, Gerhard] Univ Hamburg, Geol Palaeontol Inst, D-20146 Hamburg, Germany; [Kotthoff, Ulrich; Koutsodendris, Andreas; Pross, Joerg] Goethe Univ Frankfurt, Paleoenvironm Dynam Grp, Inst Geosci, Frankfurt, Germany; [Bornemann, Andre; Kaul, Christian] Univ Leipzig, Inst Geol & Geophys, Leipzig, Germany; [Marino, Gianluca] Univ Autonoma Barcelona, ICTA, Bellaterra, Cerdanyola Vall, Spain; [Peyron, Odile] Univ Franche Comte, Lab Chronoenvironm, UMR UFC CNRS USC INRA 6249, F-25030 Besancon, France; [Schiebel, Ralf] Univ Southampton, Natl Oceanog Ctr, Southampton, Hants, England; [Schiebel, Ralf] Univ Angers, Lab Bioindicateurs Actuels & Fossiles, Angers, France	University of Hamburg; Goethe University Frankfurt; Leipzig University; Autonomous University of Barcelona; Universite de Franche-Comte; INRAE; NERC National Oceanography Centre; University of Southampton; Universite d'Angers	Kotthoff, U (通讯作者)，Univ Hamburg, Geol Palaeontol Inst, Bundesstr 55, D-20146 Hamburg, Germany.	ulrich.kotthoff@uni-hamburg.de	Marino, Gianluca/AAN-3969-2020; Bornemann, André/N-7239-2019; Schmiedl, Gerhard/E-6644-2017; Koutsodendris, Andreas/G-8966-2013	Schmiedl, Gerhard/0000-0002-2177-6858; Koutsodendris, Andreas/0000-0003-4236-7508; Bornemann, Andre/0000-0003-4341-2366; Schiebel, Ralf/0000-0002-6252-7647; Marino, Gianluca/0000-0001-9795-5337	German Research Foundation [651/6-1]; State of Hesse; French CNRS	German Research Foundation(German Research Foundation (DFG)); State of Hesse; French CNRS(Centre National de la Recherche Scientifique (CNRS))	Discussions with K.-C. Emeis, W. Ehrmann, U. C. Muller,). Fiebig and B. van de Schootbrugge are gratefully acknowledged, as are helpful comments and suggestions by two anonymous reviewers. We thank the crew, the scientific party and chief scientist C. Hemleben of RV Meteor cruise M51/3. The Greek authorities are thanked for allowing research to be carried out in their territorial waters. This study was supported by the German Research Foundation (grant Pr 651/6-1) and the BiK-F/LOEWE research funding program of the State of Hesse, and furthermore by the French CNRS through the LAMA ANR research project.	AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; Bahr A, 2008, GEOCHEM GEOPHY GEOSY, V9, DOI 10.1029/2007GC001683; Barker S, 2009, NATURE, V457, P1097, DOI 10.1038/nature07770; Be A.W. 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Quat. Sci.	JAN	2011	26	1					86	96		10.1002/jqs.1430	http://dx.doi.org/10.1002/jqs.1430			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	718LW					2025-03-11	WOS:000287124100010
J	Suikkanen, S; Hakanen, P; Spilling, K; Kremp, A				Suikkanen, Sanna; Hakanen, Paivi; Spilling, Kristian; Kremp, Anke			Allelopathic effects of Baltic Sea spring bloom dinoflagellates on co-occurring phytoplankton	MARINE ECOLOGY PROGRESS SERIES			English	Article						Allelopathy; Baltic Sea; Spring bloom; Dinoflagellate; Biecheleria baltica; Gymnodinium corollarium; Scrippsiella hangoei; Diatom	RED-TIDE DINOFLAGELLATE; HARMFUL ALGAL BLOOMS; SCRIPPSIELLA-HANGOEI; KARENIA-BREVIS; PERIDINIUM-ACICULIFERUM; SKELETONEMA-COSTATUM; CYST FORMATION; OKADAIC ACID; HIGH PH; ALEXANDRIUM	Dinoflagellate-dominated spring blooms are globally uncommon, but they regularly occur and are even increasing in the Baltic Sea, varying interannually in importance with diatom-dominated blooms. The success of dinoflagellates in the spring phytoplankton community has remained poorly understood, as they are expected to be inferior competitors due to their low growth rates and nutrient uptake capacities under nutrient-replete spring conditions. To prevail in the phytoplankton community, dinoflagellates must either be favored by specific environmental settings or possess adaptations, such as allelopathy, to compensate for their competitive disadvantage. Using batch cultures, we studied the allelopathic effects of 3 dominant vernal dinoflagellates-Biecheleria baltica, Gymnodinium corollarium and Scrippsiella hangoei-on 5 typical spring bloom diatoms and 1 cryptophyte. We also tested the effects of the dinoflagellates on each other. Three of the 5 diatoms-Melosira arctica, Skeletonema marinoi and Thalassiosira baltica-were significantly inhibited by cell-free filtrates or live cells of all dinoflagellates. Chaetoceros cf. wighamii and Diatoma tenuis were suppressed by G. corollarium, and D. tenuis was also suppressed by live cells of S. hangoei. In contrast, the cryptophyte Rhodomonas sp. was stimulated by all dinoflagellate species. The effects of dinoflagellate filtrates on other dinoflagellate species were mostly positive, but co-culturing tended to inhibit the growth of the respective target dinoflagellates. As some of the major players of the diatom spring bloom can be suppressed by co-occurring dinoflagellates in culture, we conclude that allelopathy may be one mechanism by which vernal dinoflagellates frequently outcompete diatoms and form intense spring blooms.	[Suikkanen, Sanna; Hakanen, Paivi; Spilling, Kristian; Kremp, Anke] Ctr Marine Res, Finnish Environm Inst, Helsinki 00251, Finland	Finnish Environment Institute	Suikkanen, S (通讯作者)，Ctr Marine Res, Finnish Environm Inst, Helsinki 00251, Finland.	sanna.suikkanen@ymparisto.fi	Kremp, Anke/I-8139-2013; Spilling, Kristian/L-7932-2014	Suikkanen, Sanna/0000-0002-0768-8149; Spilling, Kristian/0000-0002-8390-8270	Academy of Finland [111336]; Walter & Andree de Nottbeck Foundation; Academy of Finland (AKA) [111336] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Walter & Andree de Nottbeck Foundation; Academy of Finland (AKA)(Research Council of Finland)	This work was supported by grants from the Academy of Finland (S.S., K.S., A.K.; grant 111336) and Walter & Andree de Nottbeck Foundation (P.H.).	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Ecol.-Prog. Ser.		2011	439						45	55		10.3354/meps09356	http://dx.doi.org/10.3354/meps09356			11	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	835WR		Bronze			2025-03-11	WOS:000296068200004
J	Chen, BZ; Irwin, AJ; Finkel, ZV				Chen, Bingzhang; Irwin, Andrew J.; Finkel, Zoe V.			Biogeographic distribution of diversity and size-structure of organic-walled dinoflagellate cysts	MARINE ECOLOGY PROGRESS SERIES			English	Article						Dinoflagellate cysts; Biogeography; Diversity; Size	SURFACE SEDIMENTS; CELL-SIZE; MARINE-PHYTOPLANKTON; ALGAL BLOOMS; OCEAN; SEA; PATTERNS; TEMPERATURE; GROWTH; ISLANDINIUM	Global biogeographic patterns and environmental correlates of diversity and size structure of extant marine organic dinoflagellate cysts were determined. Dinoflagellate cyst diversity, like that of many other terrestrial and marine groups, is lowest at the poles and higher at lower latitudes. Temperature is responsible for much of the positive correlation between dinoflagellate cyst diversity and latitude. In contrast, the most obvious correlate with the median size of dinoflagellate cysts is the depth of the water column, especially in warm-water regions, perhaps due to changes in mixing regime and the advantages associated with the lower sinking rates and lower nutrient requirements of smaller species in offshore waters. The unique biogeographic pattern in dinoflagellate cyst diversity may reflect the unique physiological features of dinoflagellates: preference for warm, stable water columns, slower inherent growth rates, and their ability to act as mixotrophs or heterotrophs. Dinoflagellates tend to be 'gleaners', slow-growers adapted to oligotrophic conditions and less sensitive to inorganic nutrient supply, as compared to inorganic resource 'opportunists' with high growth rates, such as diatoms. These ecophysiological differences between dinoflagellates and other functional groups, such as diatoms and coccolithophores, may account for the major differences in the biogeographic and latitudinal diversity gradients between these groups.	[Irwin, Andrew J.] Mt Allison Univ, Dept Math & Comp Sci, Sackville, NB E4L 1A6, Canada; [Chen, Bingzhang; Finkel, Zoe V.] Mt Allison Univ, Environm Sci Program, Sackville, NB E4L 1A7, Canada	Mount Allison University; Mount Allison University	Chen, BZ (通讯作者)，Xiamen Univ, State Key Lab Marine Environm Sci, Xiamen 361005, Fujian, Peoples R China.	zfinkel@mta.ca	Irwin, Andrew/B-2245-2008; Chen, Bingzhang/AAH-6784-2020; Finkel, Zoe/B-9626-2008	Irwin, Andrew/0000-0001-7784-2319; Chen, Bingzhang/0000-0002-1573-7473; Finkel, Zoe/0000-0003-4212-3917	NSERC; ACENET Post-Doctoral Fellowship	NSERC(Natural Sciences and Engineering Research Council of Canada (NSERC)); ACENET Post-Doctoral Fellowship	We thank J. Sebbo and D. Blanchette for their contributions to this work. This work was supported by NSERC Discovery (Z.V.F and A.J.I) and a ACENET Post-Doctoral Fellowship Award (B.C.).	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Ecol.-Prog. Ser.		2011	425						35	U348		10.3354/meps08985	http://dx.doi.org/10.3354/meps08985			19	Ecology; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Oceanography	735GG		Bronze			2025-03-11	WOS:000288400800003
S	Davidson, K; Tett, P; Gowen, R		Hester, RE; Harrison, RM		Davidson, Keith; Tett, Paul; Gowen, Richard			Harmful Algal Blooms	MARINE POLLUTION AND HUMAN HEALTH	Issues in Environmental Science and Technology Series		English	Article; Book Chapter							NITZSCHIA-SERIATA BACILLARIOPHYCEAE; DOMOIC ACID PRODUCTION; PHAEOCYSTIS-POUCHETII; RED TIDE; COCHLODINIUM-POLYKRIKOIDES; GYMNODINIUM-CATENATUM; DINOFLAGELLATE CYSTS; PHYTOPLANKTON BLOOMS; GYRODINIUM-AUREOLUM; TOXIC PROPERTIES	Phytoplankton are free-floating plants found inmarine and freshwaters that through their photosynthetic growth form the base of the aquatic food chain. A small subset of the phytoplankton may be harmful to human health or to human use of the ecosystem. The species that cause harm are now widely referred to as 'Harmful Algae' with the term 'Harmful Algal Bloom' (HAB) commonly being used to describe their occurrence and effects. In terms of human health, the most important consequence is the production, by some species, of biotoxins. Typically, biotoxin-producing phytoplankton species exist at relatively low densities (c. few hundred or thousand of cells per litre) with the toxins becoming concentrated in the flesh of organisms (particularly bivalve molluscs) that filter feed on phytoplankton. In most cases, there are no adverse effects to these primary consumers, but this concentrating mechanism creates a risk to health if the shellfish are consumed by humans. In this review, we provide an overview of the mechanisms through which marine phytoplankton may cause harm to humans in terms of heath, and the negative effects on the use of ecosystem services. Subsequently, we consider HAB issues in the area we are most familiar with: UK coastal waters. Finally, the methodologies used to safeguard human health from HAB-generated syndromes are discussed.	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Sci. Technol. Ser.		2011	33						95	127				10.1039/9781849732871		33	Environmental Sciences; Public, Environmental & Occupational Health	Book Citation Index– Science (BKCI-S)	Environmental Sciences & Ecology; Public, Environmental & Occupational Health	BIE28		Green Published, Green Submitted			2025-03-11	WOS:000327872500005
J	Peyrot, D				Peyrot, Daniel			Late Cretaceous (Late Cenomanian-Early Turonian) dinoflagellate cysts from the Castilian Platform, northern Spain	PALYNOLOGY			English	Article						Cenomanian; Turonian; dinoflagellate cysts; Castillian Platform; Cenomanian-Turonian Boundary Event (CTBE)	BOUNDARY EVENT; SOUTHERN ENGLAND; WESTERN; STRATIGRAPHY; FRANCE; DINOCYST; DISTRIBUTIONS; ASSOCIATIONS; ACRITARCHS; SECTIONS	The biostratigraphical ranges, geographical distribution and taxonomy of 45 dinoflagellate cyst species are described based on the analysis of 99 samples from the Upper Cenomanian-Lower Turonian outcrop sections of Puentedey, Fuentetoba, Condemios and Tamajon in northern Spain. A specific rank for Coronifera hebospina (formerly Coronifera oceanica subsp. hebospina) and the new combination Exochosphaeridium majus are proposed. The generic assignment of Implestosphaeridium? clavulum and Implestosphaeridium? polytrichum are questioned. Early Turonian range tops for Coronifera albertii, Cyclonephelium vannophorum and Palaeohystrichophora palaeoinfusa are confirmed.	UCM CSIC, Dept UEI Paleontol, Madrid 28040, Spain	Complutense University of Madrid	Peyrot, D (通讯作者)，UCM CSIC, Dept UEI Paleontol, Jose Antonio Novais 2, Madrid 28040, Spain.	danip@geo.ucm.es	peyrot, Daniel/AAI-6091-2020	peyrot, Daniel/0000-0002-3897-6733	Spanish Ministerio de Educacion y Ciencia [GR58/08-B (BSCH-UCM), CGL2005-01765/BTE, CGL2008-03112/BTE]; Basler Stiftung fur biologische Forschung (Switzerland); Universidad Complutense de Madrid, Spain; Instituto Geologico y Minero de Espana	Spanish Ministerio de Educacion y Ciencia(Spanish Government); Basler Stiftung fur biologische Forschung (Switzerland); Universidad Complutense de Madrid, Spain; Instituto Geologico y Minero de Espana	This article was funded by projects GR58/08-B (BSCH-UCM), CGL2005-01765/BTE and CGL2008-03112/BTE of the Spanish Ministerio de Educacion y Ciencia and the Basler Stiftung fur biologische Forschung (Switzerland). Maria Jose Comas Rengifo (Universidad Complutense de Madrid, Spain) and Eduardo Barron (Instituto Geologico y Minero de Espana) are thanked for their continuous support. Much of the systematic section was prepared during meetings at the Bedford Institute of Oceanography (Geological Survey of Canada, Dartmouth, Nova Scotia, Canada) and Saint Mary's University (Halifax, Nova Scotia, Canada). The author expresses his gratitude to R. Andrew MacRae, Robert A. Fensome and Graham L. Williams who gave insightful advice on dinoflagellate cyst taxonomy, and who checked and commented on early versions of the manuscript. Thanks are also owed to Susanne Feist-Burkhardt of the Natural History Museum (London, UK), who provided access to the dinoflagellate cysts voucher collection, and to Paul Dodsworth (Stratasolve Ltd.), Henrik Nohr-Hansen (Geological Survey of Denmark and Greenland) and James B. Riding (British Geological Survey), who notably improved the original content of the paper.	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J	Borges, MEN; Riding, JB; Fernandes, P; Pereira, Z				Borges, Marisa E. N.; Riding, James B.; Fernandes, Paulo; Pereira, Zelia			The Jurassic (Pliensbachian to Kimmeridgian) palynology of the Algarve Basin and the Carrapateira outlier, southern Portugal	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						biostratigraphy; palynology; Jurassic; Algarve Basin; Carrapateira outlier; Portugal	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; COASTAL DEPOSITS; MIDDLE; STRATIGRAPHY; BOUNDARY; RECORDS; WESTERN; BOREAL; FRANCE	The palynology of the Jurassic (Upper Pliensbachian to Lower Kimmeridgian) fill of the Algarve Basin and the Carrapateira outlier, southern Portugal was investigated. Samples were collected from Armacao Nova Bay, Mareta Beach, Cilheta Beach and the Carrapateira outlier. At Armacao Nova Bay the Upper Pliensbachian-Lower Toarcian succession proved barren, or yielded sparse, non age-diagnostic palynomorphs. Dinoflagellate cysts are confined to the Upper Bajocian to Upper Callovian sedimentary rocks exposed at Mareta and Cilheta beaches and the Lower Kimmeridgian strata of the Carrapateira outlier. At Mareta Beach, the Upper Bajocian, Bathonian and Callovian produced relatively low to moderate diversity dinoflagellate cyst assemblages. Several key bioevents confirm the Bathonian and Callovian ages of the succession; no age-significant Late Bajocian bioevents were noted. The Upper Callovian of Cilheta Beach yielded moderately diverse dinoflagellate cyst associations dominated by Ctenidodinium spp. Key Late Callovian bioevents confirm the age of this succession. Many familiar marker forms known from northwest Europe were not encountered. No typically Arctic forms were recovered throughout the Upper Bajocian to Callovian of this part of the Algarve Basin. It is clear that there was no significant Late Bajocian to Late Callovian dinoflagellate cyst provincialism within southern and northern Europe and adjacent regions. The Carrapateira outlier yielded a moderately diverse Early Kimmeridgian dinoflagellate cyst flora. The Early Kimmeridgian age assessment based on corals and foraminifera is confirmed. Amphorula and Histiophora are present; these are typical of the Late Jurassic of the Tethyan Realm, and their presence is consistent with Late Jurassic provincialism within Europe. The relatively low diversity nature of these late Bajocian to Early Kimmeridgian dinoflagellate cyst floras is probably mainly due to the relatively deep water, partially enclosed depositional setting. The partially enclosed nature of this part of the Algarve Basin and the Carrapateira outlier seems to have prevented the free migration of dinoflagellates between southern Portugal and elsewhere in Europe. (C) 2011 Natural Environment Research Council. Published by Elsevier BV. All rights reserved.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England; [Borges, Marisa E. N.; Pereira, Zelia] LNEG LGM, P-4465965 Sao Mamede de Infesta, Portugal; [Borges, Marisa E. N.; Fernandes, Paulo] Univ Algarve, CIMA, P-8005139 Faro, Portugal	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Laboratorio Nacional de Energia e Geologia IP (LNEG); Universidade do Algarve	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England.	marisa.borges@ineti.pt; jbri@bgs.ac.uk; pfernandes@ualg.pt; zelia.pereira@ineti.pt	Pereira, Zelia/B-2740-2017; Fernandes, Paulo/J-6577-2014	Pereira, Zelia/0000-0003-3056-6219; Fernandes, Paulo/0000-0003-4888-0230	Portuguese Foundation for Science and Technology [SFRH/BD/40428/2007]; NERC [bgs05004] Funding Source: UKRI; Fundação para a Ciência e a Tecnologia [SFRH/BD/40428/2007] Funding Source: FCT	Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	The input of Marisa E.N. Borges represents a part of her PhD scholarship from the Portuguese Foundation for Science and Technology (number SFRH/BD/40428/2007). The contribution of James B. Riding was completed under the BGS Individual Merit project entitled Global Jurassic dinoflagellate cyst palaeobiology and its applications. James B. Riding publishes with the approval of the Executive Director, British Geological Survey (NERC).	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Palaeobot. Palynology	JAN	2011	163	3-4					190	204		10.1016/j.revpalbo.2010.09.006	http://dx.doi.org/10.1016/j.revpalbo.2010.09.006			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	712SF					2025-03-11	WOS:000286685800002
J	Riding, JB; Quattrocchio, ME; Martínez, MA				Riding, James B.; Quattrocchio, Mirta E.; Martinez, Marcelo A.			Mid Jurassic (Late Callovian) dinoflagellate cysts from the Lotena Formation of the Neuquen Basin, Argentina and their palaeogeographical significance	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Lotena Formation; Mid Jurassic; dinoflagellate cysts; biostratigraphy; palaeogeography; Argentina	BAYU-UNDAN FIELD; TIMOR SEA; SEQUENCE STRATIGRAPHY; ANTARCTIC PENINSULA; PALYNOLOGY; STRATA; PALEOENVIRONMENTS; BIOSTRATIGRAPHY; PALYNOMORPHS; AMERICA	The Lotena Formation from two localities, Plain Leufu and Portada Covunco, in the Neuquen Basin of west-central Argentina was studied palynologically. The material examined produced moderately diverse Late Callovian dinoflagellate cyst assemblages. This age assignment is consistent with ammonite evidence. The dinoflagellate cyst floras are reminiscent of the Middle Jurassic associations of northwest Europe and surrounding areas. Marine palynomorphs typical of Australasia and the Arctic are absent. The similarity with Europe is strongly suggestive of an open marine connection between western Tethys and the Neuquen Basin during the Late Callovian. This is interpreted as being via the Hispanic Corridor, with the palynofloras being passively dispersed to the southwest by the circum-Tropical Marine Current. Earlier studies indicate that this trans-Pangean equatorial seaway first began to allow biotic interchange during the Mid Jurassic and this study proves that this open marine connection was established by the Late Callovian. The similarities between the dinoflagellate cyst assemblages of Europe and the Neuquen Basin are consistent with the distribution of other marine fossils and the existence of geographically continuous marine facies belts. (C) 2011 Natural Environment Research Council. Published by Elsevier BV. All rights reserved.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England; [Quattrocchio, Mirta E.; Martinez, Marcelo A.] Univ Nacl Sur, Dept Geol, CONICET, RA-8000 Bahia Blanca, Buenos Aires, Argentina	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk; mquattro@criba.edu.ar; martinez@criba.edu.ar		Martinez, Marcelo/0000-0003-0538-4739	NERC [bgs05004] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Aberhan M, 2001, PALAEOGEOGR PALAEOCL, V165, P375, DOI 10.1016/S0031-0182(00)00172-3; AGER DV, 1981, J GEOL SOC LONDON, V138, P159, DOI 10.1144/gsjgs.138.2.0159; [Anonymous], JURASSIC CIRCUM PACI; [Anonymous], 1992, ARCTIC GEOLOGY PETRO; [Anonymous], 7 C GEOL ARG NEUQ AC; Berger J.-P., 1986, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V172, P331; Boomer I, 1996, PALAEOGEOGR PALAEOCL, V121, P53, DOI 10.1016/0031-0182(95)00049-6; Brideaux W.W., 1976, GEOLOGICAL SURVEY CA, V259; Bush ABG, 1997, SCIENCE, V275, P807, DOI 10.1126/science.275.5301.807; Conway B.H., 1990, GEOLOGICAL SURVEY IS, V82; Davey R.J., 1987, GEOLOGICAL SURVEY PA, V13; Davies E.H., 1983, GEOLOGICAL SURVEY CA, V359; Dorhofer G, 1980, LIFE SCI MISCELLANEO; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Garg R., 1988, Palaeobotanist (Lucknow), V36, P254; Garg Rahul, 2003, Journal of the Palaeontological Society of India, V48, P41; Groeber P., 1953, GEOGRAFIA REPUBLICA, V2, P143; HALLAM A, 1983, PALAEOGEOGR PALAEOCL, V43, P181, DOI 10.1016/0031-0182(83)90010-X; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Helby R., 1988, Memoir of the Association of Australasian Palaeontologists, V5, P125; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Howell JA, 2005, GEOL SOC SPEC PUBL, V252, P1, DOI 10.1144/GSL.SP.2005.252.01.01; Ibrahim MIA, 2002, NEUES JAHRB GEOL P-A, V224, P255; Irurralde-Vinent M.A., 2003, AAPG MEMOIR, V79, P75; Iturralde-Vinent MA, 2006, INT GEOL REV, V48, P791, DOI 10.2747/0020-6814.48.9.791; Jain K.P., 1986, Palaeobotanist (Lucknow), V35, P73; JIANG Q, 1992, REV PALAEOBOT PALYNO, V74, P77, DOI 10.1016/0034-6667(92)90139-8; JOHNSON C D, 1973, Bulletin of Canadian Petroleum Geology, V21, P178; Legarreta L., 1999, Servicio Geologico Minero Argentino, Anales, V29, P399; LONGSHAW SK, 1983, J GEOL SOC LONDON, V140, P945, DOI 10.1144/gsjgs.140.6.0945; Mantle DJ, 2009, PALAEONTOGR ABT B, V280, P87, DOI 10.1127/palb/280/2009/87; Mantle DJ, 2009, PALAEONTOGR ABT B, V280, P1; Mantle DJ, 2005, REV PALAEOBOT PALYNO, V135, P245, DOI 10.1016/j.revpalbo.2005.05.004; Martínez MA, 2004, AMEGHINIANA, V41, P485; MARTINEZ MA, 2003, 12 SIMP ARG PAL PAL, P16; Mpodozis Constantino, 2008, Rev. 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Palaeobot. Palynology	JAN	2011	163	3-4					227	236		10.1016/j.revpalbo.2010.10.009	http://dx.doi.org/10.1016/j.revpalbo.2010.10.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	712SF		Green Published, Green Accepted			2025-03-11	WOS:000286685800004
J	Zinssmeister, C; Soehner, S; Facher, E; Kirsch, M; Meier, KJS; Gottschling, M				Zinssmeister, Carmen; Soehner, Sylvia; Facher, Eva; Kirsch, Monika; Meier, K. J. Sebastian; Gottschling, Marc			Catch me if you can: the taxonomic identity of <i>Scrippsiella trochoidea</i> (F.STEIN) A.R.LOEBL. (Thoracosphaeraceae, Dinophyceae)	SYSTEMATICS AND BIODIVERSITY			English	Article						calcareous dinoflagellates; coccoid stage; cryptic speciation; distribution; epitypification; morphology; Peridiniales; phylogeny; thecate cell	DINOFLAGELLATE RESTING CYSTS; MULTIPLE SEQUENCE ALIGNMENT; MARINE DINOFLAGELLATE; MIXED MODELS; KIEL BIGHT; BALTIC SEA; CALCIODINELLOIDEAE; SEDIMENTS; GERMINATION; MORPHOLOGY	The species concept is challenged for the unicellular dinophytes, exhibiting both high intraspecific variability (in terms of morphology) and cryptic speciation (as inferred from molecular data). As one of the most abundant species assigned to calcareous dinophytes (Thoracosphaeraceae, Dinophyceae), Scrippsiella trochoidea is cosmopolitan in distribution, but its taxonomic identity is presently unclear. We collected, isolated and cultivated Scrippsiella trochoidea (strain GeoB*185) from the type locality in the Kiel Fjord (Baltic Sea, Germany). We barcoded the species of the Thoracosphaeraceae based on ITS sequences (including 22 new sequences) and investigated the morphology of strain GeoB*185 by using light, fluorescence and electron microscopy. Numerous distinct lineages that had previously been determined as Scrippsiella trochoidea constituted a species complex rather than a single species. This species complex subsequently comprised three primary clades, for which the strain GeoB*185 was assigned to one of them. We designate an epitype for Scrippsiella trochoidea, which has been prepared from the culture collected in the Kiel Fjord. The unambiguous links between a scientific species name, its protologue, genetic characterization and spatial distribution bear particular importance for character-poor, unicellular organisms such as the dinophytes.	[Zinssmeister, Carmen; Soehner, Sylvia; Facher, Eva; Gottschling, Marc] Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, D-80638 Munich, Germany; [Zinssmeister, Carmen; Soehner, Sylvia] Free Univ Berlin, Fachbereich Geol Wissensch, Fachrichtung Palaontol, D-12249 Berlin, Germany; [Kirsch, Monika] Univ Bremen, Fachbereich Geowissensch, Fachrichtung Hist Geol Palaontol, D-28359 Bremen, Germany; [Meier, K. J. Sebastian] Univ Kiel, Inst Geowissensch, D-24118 Kiel, Germany	University of Munich; Free University of Berlin; University of Bremen; University of Kiel	Gottschling, M (通讯作者)，Univ Munich, GeoBioctr, Dept Biol Systemat Bot & Mykol, Menzinger Str 67, D-80638 Munich, Germany.	gottschling@biologie.uni-muenchen.de	Gottschling, Marc/K-2186-2014; Meier, K. J. Sebastian/H-7914-2014	Meier, K. J. Sebastian/0000-0002-3918-4092	Deutsche Forschungsgemeinschaft [KE 322/36, RI 1738/5, WI 725/25]; Munchener Universitatsgesellschaft	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Munchener Universitatsgesellschaft	We thank Julia Daum, Patricia Silva Flores and Martina Rom-Roeske (all Munich) for their key assistance during the cultivation of the strains. Mona Hoppenrath (Bremerhaven) and Michael Schweikert (Stuttgart) gave valuable advice regarding methodology. We further thank two anonymous reviewers, who helped to improve our manuscript. Anne Beck (Berlin) and Adrienne Jochum (Frankfurt) kindly provided editorial insights in reviewing this manuscript. Financial support by the Deutsche Forschungsgemeinschaft (grants KE 322/36, RI 1738/5, and WI 725/25) and the Munchener Universitatsgesellschaft is gratefully acknowledged here.	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J	Guerstein, GR; Daners, G				Raquel Guerstein, G.; Daners, Gloria			PALEOGENE DISTRIBUTION OF <i>ENNEADOCYSTA</i> (DINOFLAGELLATA) IN THE SOUTHWESTERN ATLANTIC OCEAN: PALEOCEANOGRAPHIC IMPLICATIONS.	AMEGHINIANA			Spanish	Article						Dinoflagellate cysts; Circum-Antarctic endemic flora; Eocene; Southwest Atlantic Ocean; Oceanic paleocirculation	SPORE POLLEN BIOSTRATIGRAPHY; COLORADO BASIN; SEA-LEVEL; ANTARCTICA; MIDDLE; MARGIN; CYSTS; CIRCULATION; GREENHOUSE; RECORD	PALEOGENE DISTRIBUTION OF ENNEADOCYSTA (DINOFLAGELLATA) IN THE SOUTHWESTERN ATLANTIC OCEAN: PALEOCEANOGRAPHIC IMPLICATIONS. The study of Middle to Late Eocene dinoflagellate cyst assemblages from subtropical Southwest Atlantic basins shows the presence of species of Enneadocysta, including E. dictyostila (Menendez) Stover and Williams emend. Fensome et al., E. brevistila Fensome et al. and E. multicornuta (Eaton) Stover and Williams. The species Enneadocysta dictyostila has been widely recorded in middle Paleogene sections from Southern Hemisphere high latitudes. High representativity of Enneadocysta spp., along with other components of the Southern Ocean endemic dinoflagellate flora, have been observed in samples from Colorado Basin (similar to 38 degrees S), Argentina and Punta del Este Basin (similar to 36 degrees S), Uruguay. Previous research in the Tasman area has related the presence of these endemic taxa at mid-latitudes to the formation of a strong clockwise subpolar gyre ("cold trap") favoured by the continental blockage of the Tasman Gateway. In this paper we propose that the observed dinoflagellate cyst distribution in the Southwest Atlantic basins can be explained by a similar dynamical mechanism operating close to the present Weddell Gyre. The blockage of the Tasman Gateway and a partially open Drake Passage both contributed to the formation of a strong western-intensified clockwise gyre that may have transported the endemic flora components, mainly represented by Enneadocysta spp., from the Antarctic continent northward along the Southwest Atlantic Shelf during the Middle - Late Eocene.	[Raquel Guerstein, G.] Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, Inst Geol Sur, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Daners, Gloria] Fac Ciencias, Dept Evoluc Cuencas, Montevideo 11400, Uruguay	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Universidad de la Republica, Uruguay	Guerstein, GR (通讯作者)，Univ Nacl Sur, Dept Geol, Consejo Nacl Invest Cient & Tecn, Inst Geol Sur, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	raquel.guerstein@uns.edu.ar; glo@fcien.edu.uy						[Anonymous], 1971, P 2 PLANKT C; Antunes R.L., 2004, B GEOCIENCIAS PETROB, V12, P421; ARCHANGELSKY S, 1969, Ameghiniana, V6, P181; Archangelsky S., 1997, PEJERREY X 1 OFFSHOR; BASOV IA, 1983, INITIAL REP DEEP SEA, V71, P445; Berggren W.A., 1995, GEOCHRONOLOGY TIME S, V54, P129, DOI 10.2110/pec.95.04.0129; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; CLOWES C D, 1985, Palynology, V9, P27; COCOZZA CD, 1992, ANTARCT SCI, V4, P355, DOI 10.1017/S0954102092000506; Cookson I.C., 1967, Proceeding of the Royal Society of Victoria, V80, P131; COOKSON ISABEL C., 1967, MICROPALEONTOLOGY [NEW YORK], V13, P204, DOI 10.2307/1484671; Cranwell L.M, 1964, Grana Palynol., V5, P397; CRANWELL LM, 1960, NATURE, V186, P700, DOI 10.1038/186700a0; Daners G., 2004, 4 C UR GEOL 2 REUN G; Daners G., 2004, CUENCAS SEDIMENTARIA, P37; Exon NF, 2004, Proceeding of the Ocean Drilling Program, Scientific Results, V189, P1, DOI 10.2973/odp.proc.sr.189.101.2004; FASOLA A, 1969, Ameghiniana, V6, P3; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Fensome R.A., 1993, CLASSIFICATION FOSSI; Fensome R.A., 2008, American Association of Stratigraphic Palynologists, Data Series; Fensome RA, 2006, MICROPALEONTOLOGY, V52, P385, DOI 10.2113/gsmicropal.52.5.385; Ferreira E.P., 2004, THESIS UFR; Franke D, 2007, MAR GEOL, V244, P46, DOI 10.1016/j.margeo.2007.06.009; Franke D, 2006, GEOPHYS J INT, V165, P850, DOI [10.1111/j.1365-246X.2006.02907.x, 10.1111/j.1365-246X.2006.02907.X]; Fryklund R., 1996, GEOLOGIA RECURSOS NA, V8, P135; GAMERRO J C, 1981, Revista Espanola de Micropaleontologia, V13, P119; Ghidella M.E., 2006, AN MAGN MARG ARG REU; GOODMAN DK, 1983, INITIAL REP DEEP SEA, V71, P859; Gradstein F., 2004, A Geological Time Scale; Guerstein GR, 2008, J MICROPALAEONTOL, V27, P75, DOI 10.1144/jm.27.1.75; Guerstein G.R., 2002, Revista Espanola de Micropaleontologia, V354, P105; Guerstein G.R., 2003, AMEGHINIANA S, V40, p87R; Guerstein G. 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J	Versteegh, GJM; Zonneveld, KAF; de Lange, GJ				Versteegh, Gerard J. M.; Zonneveld, Karin A. F.; de Lange, Gert J.			Selective aerobic and anaerobic degradation of lipids and palynomorphs in the Eastern Mediterranean since the onset of sapropel S1 deposition	MARINE GEOLOGY			English	Article						organic geochemistry; palynology; organic matter; kerogen; selective preservation; S1 sapropel; lipid; kerogen; pollen; dinoflagellate cyst	WALLED DINOFLAGELLATE CYSTS; ORGANIC-MATTER PRESERVATION; MADEIRA ABYSSAL-PLAIN; CONTINENTAL-MARGIN SEDIMENTS; REDOX-SENSITIVE ELEMENTS; OXYGEN EXPOSURE TIME; MARINE-SEDIMENTS; EMILIANIA-HUXLEYI; EARLY DIAGENESIS; SEA SEDIMENTS	Selective degradation of organic matter in sediments is important for reconstructing past environments and understanding the carbon cycle. Here, we report on compositional changes between and within lipid classes and kerogen types (represented by palynomorph groups) in relation to the organic matter flux to the sea floor and oxidation state of the sediments since the early Holocene for central Eastern Mediterranean site ABC26. This includes the initially oxic but nowadays anoxic presapropelic interval, the still unoxidised lower part of the organic rich S1 sapropel, its postdepositionally oxidised and nowadays organic-poor upper part as well as the overlying postsapropelic sediments which have always been oxic. A general similar to 2.3 times increase in terrestrial and marine input during sapropel formation is estimated on the basis of the total organic carbon (TOC), pollen, spore, dinoflagellate cyst, n-alkane, n-alkanol and n-alkanoic acid concentration changes in the unoxidised part of the sapropel. The long-chain alkenones, 1,15 diols and keto-ols, loliolides and sterols indicate that some plankton groups, notably dinoflagellates, may have increased much more. Apart from the terrestrial and surface water contributions to the sedimentary organic matter, anomalous distributions and preservation of some C-23-C-27 alkanes, alkanols and alkanoic acids have been observed, which are interpreted as a contribution by organisms living in situ. Comparison of the unoxidised S1 sapropel with the overlying oxidised sapropel and the organic matter concentration profiles in the oxidised postsapropelic sediments demonstrates strong and highly selective aerobic degradation of lipids and palynomorphs. There seems to be a fundamental difference in degradation kinetics between lipids and pollen which may be possibly related with the absence of sorptive preservation as a protective mechanism for palynomorph degradation. The n-alkanes, Impagidinium, and Nematosphaeropsis are clearly more resistant than TOC. The n-alkanols and n-carboxylic acids are about equally resistant whereas the pollen, all other dinoflagellate cysts and other lipids appear to degrade considerably faster, which questions the practice of normalising to TOC without taking diagenesis into account. Selective degradation also modifies the relative distributions within lipid classes, whereby the longer-chain alkanes, alcohols and fatty acids disappear faster than their shorter-chain equivalents. Accordingly, interpretation of lipid and palynomorph assemblages in terms of pre- or syndepositional environmental change should be done carefully when proper knowledge of the postdepositional preservation history is absent. Two lipid-based preservation proxies are tested the diol-keto-ol oxidation index based on the 1,15C(30) diol and keto-ols (DOXI) and the alcohol preservation index (API) whereby the former seems to be the most promising. (C) 2010 Elsevier B.V. All rights reserved.	[Versteegh, Gerard J. M.] Univ Bremen, MARUM, D-28359 Bremen, Germany; [Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; [de Lange, Gert J.] Fac Earth Sci, Dept Geochem, NL-3584 CD Utrecht, Netherlands	University of Bremen; University of Bremen	Versteegh, GJM (通讯作者)，Univ Bremen, MARUM, Leobenerstr, D-28359 Bremen, Germany.	versteegh@uni-bremen.de	De Lange, Gert/B-9639-2014; Versteegh, Gerard J.M./H-2119-2011	De Lange, Gert/0000-0002-9420-3022; Versteegh, Gerard J.M./0000-0002-9320-3776	German Science Foundation (DFG) [VE486/2-1]; Dutch Science Foundation; EU	German Science Foundation (DFG)(German Research Foundation (DFG)); Dutch Science Foundation(Netherlands Organization for Scientific Research (NWO)); EU(European Union (EU))	We thank Royal NIOZ, Netherlands for analytical support. We also thank Richard Seifert, Hamburg University, for inspiring and constructive discussions during the final stage of manuscript preparation. The study was financially supported by the German Science Foundation (DFG) through a grant to GJMV (VE486/2-1). Financial support to GJdL came from the Dutch Science Foundation (Pass2) and EU (SAP) grants.	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Geol.	DEC 15	2010	278	1-4					177	192		10.1016/j.margeo.2010.10.007	http://dx.doi.org/10.1016/j.margeo.2010.10.007			16	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	705JT					2025-03-11	WOS:000286125400013
J	Verleye, TJ; Louwye, S				Verleye, Thomas J.; Louwye, Stephen			Recent geographical distribution of organic-walled dinoflagellate cysts in the southeast Pacific (25-53°S) and their relation to the prevailing hydrographical conditions	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinoflagellate cysts; Southeast Pacific; Quantitative reconstruction; Upwelling; Nutrient availability	SEA-SURFACE CONDITIONS; NORTHERN NORTH-ATLANTIC; MAJOR GLACIATION CYCLES; RECENT MARINE-SEDIMENTS; ABRUPT CLIMATE-CHANGE; HIGH-LATITUDE; OCEAN; TEMPERATURE; SALINITY; HOLOCENE	Forty-eight surface sediment samples from the southeast (SE) Pacific (25-53 degrees S) are investigated for the determination of the spatial distribution of organic-walled dinoflagellate cysts along the western South American continental margin. Fifty-five different taxa are recorded and reflect oceanic or coastal assemblages. The oceanic assemblages are characterised by low cyst concentrations and the dominance of autotrophs, while the coastal assemblages generally contain a higher number of cysts, which are mainly produced by heterotrophic species. Highest cyst concentrations are observed in the active upwelling system offshore Concepcion (35-37 degrees S). Brigantedinium spp., Echinidinium aculeatum, Echinidinium granulatum/delicatum and cysts of Protoperidinium americanum dominate assemblages related to upwelling. Echinidinium aculeatum appears to be the best indicator for the presence of all year round active upwelling cells. Other protoperidinioid cysts may also occur in high relative abundances in coastal regions outside active upwelling systems, if the availability of nutrients, co-responsible for the presence/absence of their main food sources such as diatoms and other protists, is sufficient. The importance of nutrient availability as a determining environmental variable influencing cyst signals on a regional scale (SE Pacific) is demonstrated through statistical analyses of the data. Because of the importance of nutrients, uncertainties about the outcomes of quantitative sea-surface temperature (SST) reconstructions (Modern Analogue Technique) based on dinoflagellate cysts may arise, since no interaction between different hydrographical variables is considered in this approach. The combination of the SE Pacific surface sample dataset with other published cyst data from the Southern Hemisphere resulted in a database which includes 350 samples: the 'SH350 database'. This database is used to test the accuracy of the quantitative reconstructions by calculating and comparing the estimated versus observed values for each site. An attempt to perform quantitative SST reconstructions on the last 25 cal ka of site ODP1233 (41 degrees S; 74 degrees 27'W) is made and again stresses the importance of other environmental variables such as nutrient availability in determining the dinoflagellate cyst assemblages. (C) 2010 Elsevier B.V. All rights reserved.	[Verleye, Thomas J.; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, B-9000 Ghent, Belgium	Ghent University	Verleye, TJ (通讯作者)，Univ Ghent, Res Unit Palaeontol, Dept Geol & Soil Sci, Krijgslaan 281 S8-WE13, B-9000 Ghent, Belgium.	thomas.verleye@ugent.be	Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313	Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)	Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT)(Institute for the Promotion of Innovation by Science and Technology in Flanders (IWT))	The authors thank V. Pospelova for help with the statistical treatment of the data. F. Marret is acknowledged for providing the scripts to run the MAT with the R software 2.7.0. The fruitful discussions with V. Pospelova are appreciated. We kindly acknowledge M. A. Godoi Millan who provided five surface samples from near the Strait of Magellan. Other samples were provided by the International Ocean Drilling Program (IODP) and Oregon State University (OSU). A. Gautier is acknowledged for the grammatical and stylistic corrections. Thanks also to the two anonymous reviewers, whose suggestions considerably improved the manuscript. Financial support to the first author was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (IWT).	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Paleoclimatol. Paleoecol.	DEC 15	2010	298	3-4					319	340		10.1016/j.palaeo.2010.10.006	http://dx.doi.org/10.1016/j.palaeo.2010.10.006			22	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	709AC					2025-03-11	WOS:000286406400014
J	Mikkelsen, DM; Witkowski, A				Mikkelsen, Ditte Marie; Witkowski, Anzdrej			Melting sea ice for taxonomic analysis: a comparison of four melting procedures	POLAR RESEARCH			English	Article						Buffer; diatoms; direct melt; flagellates; osmotic stress; sea ice	BALTIC SEA; SALINITIES	The influence of four melting procedures on the taxonomic composition of the sea-ice algal community in Kobbefjord, south-west Greenland, was investigated in April 2008. Direct melting (at 4 and 20 degrees C) was compared with melting in buffering seawater (with salinities of 10 and 30). The sea-ice algal community consisted of diatoms, cysts and several flagellate groups. Direct melting at 20 degrees C differed significantly from one or more of the other melting procedures regarding the flagellate groups chrysophytes, chlorophytes, dinoflagellates and unidentified flagellates, whereas diatom, cyst and cryptophyte abundance was similar, regardless of the melting procedure. Apart from chrysophytes, the three other melting procedures (direct melting at 4 degrees C and buffered in seawater with salinities of 10 and 30) were not statistically different. It is recommended that direct melting at 20 degrees C is avoided, whereas the three slow melting procedures are all comparable. This will enable the future comparison of data from a wide geographic and historical range, thereby increasing our knowledge of sympagic algal communities.	[Mikkelsen, Ditte Marie] Greenland Inst Nat Resources, Nuuk 3900, Greenland; [Witkowski, Anzdrej] Univ Szczecin, PL-71475 Szczecin, Poland	Greenland Institute of Natural Resources; University of Szczecin	Mikkelsen, DM (通讯作者)，Greenland Inst Nat Resources, POB 570, Nuuk 3900, Greenland.	dittemikkelsen@gmail.com		Witkowski, Andrzej/0000-0003-1714-218X	Danish Energy Agency	Danish Energy Agency	This project received funding from the Danish Energy Agency as part of the climate support programme to the Arctic. The work is a contribution to the Zackenberg Basic and Nuuk Basic programmes in Greenland.	COX GFN, 1983, J GLACIOL, V29, P306, DOI 10.3189/S0022143000008364; GARRISON DL, 1986, POLAR BIOL, V6, P237, DOI 10.1007/BF00443401; Grasshoff K., 1999, METHODS SEAWATER ANA, DOI 10.1002/9783527613984; Haecky P, 1999, AQUAT MICROB ECOL, V20, P107, DOI 10.3354/ame020107; Ikavalko J, 1998, POLAR BIOL, V19, P323, DOI 10.1007/s003000050253; Kirst G.O., 1989, Annual Review of Plant Physiology and Plant Molecular Biology, V40, P21, DOI [DOI 10.1146/ANNUREV.PP.41.060190.000321, 10.1146/annurev.pp.41.060190.000321]; Medlin L.K., 1990, POLAR MARINE DIATOMS, P1; Mikkelsen DM, 2008, MAR ECOL PROG SER, V368, P65, DOI 10.3354/meps07627; Ryan KG, 2004, POLAR BIOL, V27, P679, DOI 10.1007/s00300-004-0636-y; Stoecker DK, 1997, J PHYCOL, V33, P585, DOI 10.1111/j.0022-3646.1997.00585.x; Utermohl H, 1958, LIMNOLOGIE, V9, P1; Von Quillfeldt CH, 1996, THESIS U TROMSO	12	17	19	1	15	WILEY-BLACKWELL PUBLISHING, INC	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0800-0395			POLAR RES	Polar Res.	DEC	2010	29	3					451	454		10.1111/j.1751-8369.2010.00162.x	http://dx.doi.org/10.1111/j.1751-8369.2010.00162.x			4	Ecology; Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Oceanography	699TF		hybrid			2025-03-11	WOS:000285685000019
J	Rossi, S; Fiorillo, I				Rossi, Sergio; Fiorillo, Ida			Biochemical features of a <i>Protoceratium reticulatum</i> red tide in Chipana Bay (Northern Chile) in summer conditions	SCIENTIA MARINA			English	Article						Protoceratium reticulatum; red tide; available food; dinoflagellate; fatty acids; upwelling system	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; FATTY-ACID-COMPOSITION; HARMFUL ALGAL BLOOMS; EL-LOA RIVER; TROPHIC MARKERS; UPWELLING SITE; PHYTOPLANKTON; FOOD; BIOMARKERS; COMMUNITY	Protoceratium reticulatum is considered a potential toxic dinoflagellate. This paper describes a high-frequency monitoring study performed at Chipana Bay (northern Chile), sampling over 48 hours in a near-bottom shallow coastal area to quantify the biochemical features of a red tide dominated by this microscopic algae. This area belongs to the Humboldt Current upwelling system, and is considered highly productive for artisanal fisheries. Total chlorophyll a, total lipids, particulate organic carbon and nitrogen, fatty acids and major phytoplankton group concentration (i.e. dinoflagellates, diatoms, ciliates and cysts) were studied in 7-hour intervals in February 2007. Our results indicate a high concentration of potential available food in the form of lipids ranging from 50 to 300 mu g L-1 for benthic suspension feeders, i.e. bivalves. The dominance of P. reticulation (60-80% of the total cell concentration per litre, ranging from 55x10(3) to 384x10(3) cells L-1) can be considered as a possible interference for harvesting in this productive area, although the toxicity of this algae was not proved in the present study. The main dinoflagellate fatty acid markers [18:0, 18:4(n-3), 20:5(n-3), and 22:6(n-3)] showed high proportions (%) during the short time cycle and in at least two cases [the 18:4 (n-3) and 22:6 (n-3) fatty acids] a highly significant relationship with dinoflagellate concentration (cells L-1). The topographical and benthic structure (mainly kelp forest) of the zone helps to retain particles and nutrients that may in part explain the high productivity and food availability, but the presence of recurrent red tides in this coastal area-if they prove to be toxic-is argued to be a major problem for local fisheries.	[Rossi, Sergio] Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Cerdanyola Del Valles 08193, Spain; [Fiorillo, Ida] CSIC, Inst Ciencias Mar, E-08003 Barcelona, Spain	Autonomous University of Barcelona; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Rossi, S (通讯作者)，Univ Autonoma Barcelona, Inst Ciencia & Tecnol Ambientals, Campus Cn UAB S-N, Cerdanyola Del Valles 08193, Spain.	Sergio.Rossi@uab.cat	rossi, sergio/I-3725-2014	Rossi, Sergio/0000-0003-4402-3418	EU [511071]; Beatriu de Pinos [2006 BP-B1 00069]; Ramon y Cajal [RyC-2007-01327]	EU(European Union (EU)); Beatriu de Pinos; Ramon y Cajal(Spanish Government)	We are grateful to Mario Villegas (Requiescat in Pacem), Daniel Carstensen and Juergen Laudien for field support in Chipana and to Enrique Isla, Elisabet Sane and "el Perra" for logistics. Phytoplankton groups were identified with the help of Claudio Fuentes-Grunewald and the fatty acid analysis was carried out by Mireia Farres. We are also grateful for the comments of two anonymous reviews that greatly improved the final version of the manuscript. This study was funded by the EU Project CENSOR (Climate Variability and El Nino Southern Oscillation: Implications for Natural Resources and Management, contract 511071). SR was co-financed by a Beatriu de Pinos Contract (2006 BP-B1 00069) and by a Ramon y Cajal Contract (RyC-2007-01327).	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Mar.	DEC	2010	74	4					633	642		10.3989/scimar.2010.74n4633	http://dx.doi.org/10.3989/scimar.2010.74n4633			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	699OF		Green Submitted, gold			2025-03-11	WOS:000285672000002
J	Kohn, M; Zonneveld, KAF				Kohn, Marion; Zonneveld, Karin A. F.			Calcification depth and spatial distribution of <i>Thoracosphaera heimii</i> cysts Implications for palaeoceanographic reconstructions	DEEP-SEA RESEARCH PART I-OCEANOGRAPHIC RESEARCH PAPERS			English	Article						Calcareous walled dinoflagellates; Calcification depth; Deep chlorophyll maximum; Geographical distribution; NW Africa; Tanzania	CALCAREOUS DINOFLAGELLATE CYSTS; DIEL VERTICAL MIGRATION; SEA-SURFACE TEMPERATURE; EQUATORIAL ATLANTIC; QUATERNARY EASTERN; TROPICAL ATLANTIC; NORTHWEST AFRICA; UPWELLING AREAS; SOMALI CURRENT; POTENTIAL USE	For the optimal use in palaeoceanographic studies of the stable oxygen isotopic signal and elemental composition of the calcareous photosynthetic dinoflagellate Thoracosphaera helm it is essential to gain detailed information about its calcification depth and spatial distribution We therefore studied the vertical and horizontal distribution patterns of T heimii in the upper water column (0-200 m) along three transects an Inshore-offshore gradient off Cape Blanc (CB) a south-north transect from CB to the Portuguese coast and a north-south transect off Tanzania We compared concentrations of living cysts (cells with cell content) with chlorophyll-a salinity and temperature measurements at the sampling depth In order to explore the seasonal variability in cyst production three transect off CB were sampled at three different times of the year Living T heimii cysts were found in the upper 160 m of the water column with highest concentrations in the photic zone indicating that the calcification of T heimii occurs in the upper part of the water column Maximal abundances of living cysts were found relatively often in or just above the deep chlorophyll maximum (DCM) the depth of which varies regionally from about 20-40 m off CB to about 80 m off Tanzania and along the transect from CB to the Portuguese Coast However there was no significant correlation at the 95% confidence level between the cyst concentrations and temperature salinity and chlorophyll-a concentrations at the sampling depths observed In both the Atlantic and Indian Oceans the highest abundances of T heimii were observed in regions where the upper water masses contained relatively low nutrient concentrations that are Influenced only sporadically or not at all by enhanced photic zone mixing related to the presence of upwelling cells or river outflow plumes at or close to the sampling sites The seasonal production of cysts by T heimii appears to be negatively related to the presence of upwelling filaments across the sampling sites Our study suggests that turbulence of the upper water masses is a major environmental factor influencing T heimii production (C) 2010 Elsevier Ltd All rights reserved	[Kohn, Marion] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28334 Bremen, Germany; Univ Bremen, Fac Geosci, D-28334 Bremen, Germany	University of Bremen; University of Bremen	Kohn, M (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, POB 330440, D-28334 Bremen, Germany.				DFG-Research Center/Excellence Cluster	DFG-Research Center/Excellence Cluster(German Research Foundation (DFG))	Thanks are given to Monika Kodrans-Nsiah the crew of P 344-1 and the crew of MSM4/4B Furthermore we thank Ilham Bouimetarhan and the crew of M75-2 as well as the EUROPROX cruise participants of P366-1 and P366-2 for recovering water samples The manuscript benefitted from helpful comments from MARUM working group A9 We also thank all members of the working group Historical Geology and Palaeontology especially Kara Bogus for their general assistance and openness to discussions Michael P Bacon Andrew J Gooday Sebastian Meier and an anonymous reviewer provided constructive comments that improved the manuscript The images and data used in this study were acquired using the GES-DISC Interactive Online Visualization and Analysis Infrastructure (Giovanni) as part of the NASA s Goddard Earth Sciences (GES) Data and Information Services Center (DISC) This research was funded through DFG-Research Center/Excellence Cluster 'The Ocean in the Earth System	ANDERSON DM, 1985, MAR ECOL PROG SER, V25, P39, DOI 10.3354/meps025039; [Anonymous], PRELIMINARY SURVEY H; [Anonymous], 2001, TANZANIAN COASTAL MA; Barton ED, 1998, PROG OCEANOGR, V41, P455, DOI 10.1016/S0079-6611(98)00023-8; BRYCESON I, 1977, ECOLOGICAL STUDY PHY; Clark CO, 2003, J CLIMATE, V16, P548, DOI 10.1175/1520-0442(2003)016<0548:IVOTRB>2.0.CO;2; Coelho HS, 2002, J MARINE SYST, V32, P153, DOI 10.1016/S0924-7963(02)00032-5; GABRIC AJ, 1993, J GEOPHYS RES-OCEANS, V98, P4697, DOI 10.1029/92JC01714; GUERRA AH, 1997, INT J REMOTE SENS, V18, P2539; Gussone N, 2004, EARTH PLANET SC LETT, V227, P201, DOI 10.1016/j.epsl.2004.09.004; Gussone N, 2010, EARTH PLANET SC LETT, V289, P180, DOI 10.1016/j.epsl.2009.11.006; Hagen E, 2001, OCEANOL ACTA, V24, pS113; HAGEN E, 1984, BEITRAGE MEERESKUNDE, V51, P5; 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; Huthnance JM, 2002, J MARINE SYST, V32, P107, DOI 10.1016/S0924-7963(02)00034-9; INOUYE I, 1983, S AFR J BOT, V2, P63, DOI 10.1016/S0022-4618(16)30147-4; Kamykowski D, 1998, J PLANKTON RES, V20, P1781, DOI 10.1093/plankt/20.9.1781; Karwath B, 2000, INT J EARTH SCI, V88, P668, DOI 10.1007/s005310050296; Karwath B, 2000, MAR MICROPALEONTOL, V39, P43, DOI 10.1016/S0377-8398(00)00013-X; KARWATH B, 2000, ECOLOGICAL STUDIES L; Kitheka JU, 1996, J SEA RES, V35, P257, DOI 10.1016/S1385-1101(96)90753-4; KOHN M, 2009, THESIS U BREMEN; KRONKAMP J, 1997, TOPICAL STUDIES OCEA, V44, P1195; Kuroyanagi A, 2008, MAR MICROPALEONTOL, V68, P236, DOI 10.1016/j.marmicro.2008.04.004; LIEBERMAN OS, 1994, J PHYCOL, V30, P964, DOI 10.1111/j.0022-3646.1994.00964.x; Lugomela C, 2002, HYDROBIOLOGIA, V477, P1, DOI 10.1023/A:1021017125376; Lugomela C, 2001, J PLANKTON RES, V23, P1121, DOI 10.1093/plankt/23.10.1121; MCCLANAHAN TR, 1988, MAR ECOL PROG SER, V44, P191, DOI 10.3354/meps044191; Meggers H, 2002, DEEP-SEA RES PT II, V49, P3631, DOI 10.1016/S0967-0645(02)00103-0; MITTELSTAEDT E, 1991, PROG OCEANOGR, V26, P307, DOI 10.1016/0079-6611(91)90011-A; MITTELSTAEDT E, 1983, PROG OCEANOGR, V12, P307, DOI 10.1016/0079-6611(83)90012-5; MORGANS JFC, 1962, NATURE, V193, P86, DOI 10.1038/193086a0; Newell B.S., 1959, COLONIAL OFFICE FI 2, V12, P18; NYKJAER L, 1994, J GEOPHYS RES-OCEANS, V99, P14197, DOI 10.1029/94JC00814; PATZOLD J, METEOR BERICHT UNPUB; Paula J, 1998, J PLANKTON RES, V20, P2165, DOI 10.1093/plankt/20.11.2165; Peliz AJ, 1999, INT J REMOTE SENS, V20, P1363, DOI 10.1080/014311699212786; Pérez FF, 2001, DEEP-SEA RES PT I, V48, P1519, DOI 10.1016/S0967-0637(00)00101-1; Pollard RT, 1996, PROG OCEANOGR, V37, P167, DOI 10.1016/S0079-6611(96)00008-0; QASIM SZ, 1982, DEEP-SEA RES, V29, P1041, DOI 10.1016/0198-0149(82)90027-9; RICHTER D, 2010, THESIS U BREMEN BREM; Richter D, 2007, MAR MICROPALEONTOL, V63, P201, DOI 10.1016/j.marmicro.2006.12.002; SARNTHEIN M, 1981, NATURE, V293, P193, DOI 10.1038/293193a0; SARNTHEIN M, 1982, GEOLOGY NW AFRICAN C; Schonfeld J, 1997, MAR MICROPALEONTOL, V29, P211, DOI 10.1016/S0377-8398(96)00050-3; SCHOTT F, 1990, DEEP-SEA RES, V37, P1825, DOI 10.1016/0198-0149(90)90080-F; SCHOTT F, 1983, PROG OCEANOGR, V12, P357, DOI 10.1016/0079-6611(83)90014-9; Schott FA, 2002, GEOPHYS RES LETT, V29, DOI 10.1029/2002GL014786; SMITH SI, 1991, US JGOFS ARABIAN SEA; Smyth TJ, 2001, PROG OCEANOGR, V51, P269, DOI 10.1016/S0079-6611(01)00070-2; Steinke S, 2005, GEOCHEM GEOPHY GEOSY, V6, DOI 10.1029/2005GC000926; SWALLOW JC, 1991, J GEOPHYS RES-OCEANS, V96, P22245, DOI 10.1029/91JC01942; ter Braak C.J. 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Part I-Oceanogr. Res. Pap.	DEC	2010	57	12					1543	1560		10.1016/j.dsr.2010.09.004	http://dx.doi.org/10.1016/j.dsr.2010.09.004			18	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	696HI					2025-03-11	WOS:000285432100003
J	Dyck, S; Tremblay, LB; de Vernal, A				Dyck, Sarah; Tremblay, L. Bruno; de Vernal, Anne			Arctic sea-ice cover from the early Holocene: the role of atmospheric circulation patterns	QUATERNARY SCIENCE REVIEWS			English	Article							NORTH-ATLANTIC OSCILLATION; WINTER CLIMATE; SURFACE; VARIABILITY; TRENDS; OCEAN; RECORD; SIMULATION; FREQUENCY; DYNAMICS	Proxy evidence suggests that a mean atmospheric state, reminiscent of the positive phase of the North Atlantic/Arctic Oscillation (NAO), persisted throughout the early Holocene and resulted in a dipole pattern in sea-ice concentration between the north-eastern and north-western North Atlantic. A dynamic thermodynamic coupled sea-ice-ocean model is used to simulate the sea-ice concentration and thickness in the Arctic during the early Holocene. It is forced with winds, ocean currents and surface air temperatures (SAT) from recent years with a positive phase of the NAO in conjunction with altered long and shortwave radiation and surface air/ocean temperatures. The simulation reproduces an east/west dipole in sea-ice cover of the Arctic and is compatible with reconstructed sea-ice conditions in the Chukchi Sea (inferred from dinoflagellate cyst analysis of ocean sediment cores). Sensitivity studies were performed to investigate the individual effects of radiation, ocean forcing, SAT and winds on sea-ice cover. Results show that in the East Siberian Sea, SAT is the dominant forcing for changes in sea-ice thickness, whereas winds and SAT are the dominant factors in sea-ice concentration anomalies. In the Barents Sea, sea-ice anomalies are influenced by air and sea surface temperatures, and ocean currents. (C) 2010 Elsevier Ltd. All rights reserved.	[Dyck, Sarah; Tremblay, L. Bruno] McGill Univ, Montreal, PQ H3A 2K6, Canada; [de Vernal, Anne] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; University of Quebec Montreal	Dyck, S (通讯作者)，McGill Univ, 805 Sherbrooke St W, Montreal, PQ H3A 2K6, Canada.	sarah.dyck@ec.gc.ca	Tremblay, Bruno/I-4497-2012; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X	National Science and Engineering Research Council of Canada [OPP-0230325]; Arctic Science Program [ARC-05-20496]; Canadian Foundation of Climate and Atmospheric Sciences (Polar Climate Stability Network); Les Fonds de Recherche sur la Nature et les Technologies	National Science and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Arctic Science Program; Canadian Foundation of Climate and Atmospheric Sciences (Polar Climate Stability Network); Les Fonds de Recherche sur la Nature et les Technologies	The authors would like to acknowledge the financial support provided by the National Science and Engineering Research Council of Canada Discovery Grant program, grant OPP-0230325, the Arctic Science Program, grant ARC-05-20496, the Canadian Foundation of Climate and Atmospheric Sciences (Polar Climate Stability Network) and les Fonds de Recherche sur la Nature et les Technologies. We would also like to thank Allegra LeGrande for sharing her data from the GISS ModelER. Finally we thank the anonymous reviewers for their invaluable examination of this manuscript.	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Sci. Rev.	DEC	2010	29	25-26			SI		3457	3467		10.1016/j.quascirev.2010.05.008	http://dx.doi.org/10.1016/j.quascirev.2010.05.008			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	686VK					2025-03-11	WOS:000284724400009
J	Ledu, D; Rochon, A; de Vernal, A; St-Onge, G				Ledu, David; Rochon, Andre; de Vernal, Anne; St-Onge, Guillaume			Holocene paleoceanography of the northwest passage, Canadian Arctic Archipelago	QUATERNARY SCIENCE REVIEWS			English	Article							SEA-SURFACE CONDITIONS; LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYST ASSEMBLAGES; INNUITIAN ICE-SHEET; PALEOMAGNETIC SECULAR VARIATION; NORTHERNMOST BAFFIN-BAY; VARVED LAKE-SEDIMENTS; CLIMATE VARIABILITY; ELLESMERE-ISLAND; OCEAN CIRCULATION	A series of cores (box and piston) were collected at 2 key locations in Lancaster Sound (cores 2004-804-009 BC and PC) and Barrow Strait (cores 2005-804-004 BC and PC) in the Canadian Arctic Archipelago to document the evolution of sea-surface conditions in the main axis of the Northwest Passage during the Holocene time period. Reconstruction of sea-surface parameters (summer temperature and salinity, duration of sea-ice cover) were estimated based on transfer functions using dinoflagellate cyst assemblages as proxy indicators. The chronology of these cores is based on calibrated AMS-C-14 dates, Pb-210 analyses, and correlations between paleomagnetic secular variations of the geomagnetic field and a predicted spherical harmonic model of the geomagnetic field (CALS7 K.2). Our age models for both cores indicate that 009 PC spans the last 11,100 cal BP, while 004 PC encompasses the last 10,800 cal BP. Calculated sedimentation rates are in the range of 43-140 cm/kyr for core 009 PC and 15-118 cm/kyr for core 004 PC, allowing for a millennial time scale resolution in each core. Our results indicate relatively harsh conditions in Lancaster Sound between 10,800 and 9000 cal BP (summer temperatures 2 degrees C cooler than at present), which we associate with the presence of active ice-streams in northernmost Baffin Bay and a weak West Greenland Current. This is followed by a warming trend (up to 3 degrees C higher than present) that took place between (similar to)8500 and 5500 cal BP, which we associate with the Holocene thermal maximum and to a large scale atmospheric pattern such as the Arctic Oscillation operating at the millennial time scale. This is concomitant with an increase in the relative abundance of phototrophic dinoflagellate cyst taxa. A gradual cooling of sea-surface temperature and increased sea-ice follow this from 5500 cal BP until the modern period. In Barrow Strait, harsh sea-surface conditions prevailed from 11,100 to 5500 cal BP, with summer temperatures as low as 4 degrees C cooler than at present. The warming trend occurred later in this region (between 5500 and (similar to)1000 cal BP), after which a gradual cooling is observed until the modern period. The apparent shift, or opposite warming trends, between Lancaster Sound and Barrow Strait after 5500 cal BP could be the result of a change in atmospheric circulation patterns related to a possible shift in the AO mode (from AO(+) to AO(-)). Comparison of ice core delta O-18 record from Devon Island ice cap and the reconstructed sea-surface temperature from core 009 PC suggests a strong atmospheric-oceanic coupling throughout the Holocene in this area. (C) 2010 Elsevier Ltd. All rights reserved.	[Ledu, David; Rochon, Andre; St-Onge, Guillaume] ISMER UQAR, Rimouski, PQ G5L 3A1, Canada; [Ledu, David; Rochon, Andre; St-Onge, Guillaume] GEOTOP, Rimouski, PQ G5L 3A1, Canada; [de Vernal, Anne] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; Universite du Quebec a Rimouski; University of Quebec; University of Quebec Montreal	Ledu, D (通讯作者)，ISMER UQAR, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	david.ledu@uqar.qc.ca; andre_rochon@uqar.qc.ca; devernal.anne@uqam.ca; guillaume_st-onge@uqar.qc	St-Onge, Guillaume/E-4828-2014; Ledu, David/X-4166-2019; de Vernal, Anne/D-5602-2013	St-Onge, Guillaume/0000-0001-6958-4217; de Vernal, Anne/0000-0001-5656-724X; Ledu, David/0000-0001-5313-7068	Arctic Net Network of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC); Canadian Foundation for Climate and Atmospheric Science (CFCAS)	Arctic Net Network of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Canadian Foundation for Climate and Atmospheric Science (CFCAS)	This work was funded by the Arctic Net Network of Centres of Excellence and the Natural Science and Engineering Research Council of Canada (NSERC). This is a contribution to the Arctic Net project 1.6, the Polar Climate Stability Network (PCSN) supported by the Canadian Foundation for Climate and Atmospheric Science (CFCAS), and the NSERC-IPY project "International Polar Year: Natural climate variability and forcings in Canadian Arctic and Arctic Ocean - Special Research Opportunity - International Polar Year".	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Sci. Rev.	DEC	2010	29	25-26			SI		3468	3488		10.1016/j.quascirev.2010.06.018	http://dx.doi.org/10.1016/j.quascirev.2010.06.018			21	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	686VK					2025-03-11	WOS:000284724400010
J	Kim, SY; Scourse, J; Marret, F; Lim, DI				Kim, So-Young; Scourse, James; Marret, Fabienne; Lim, Dhong-Il			A 26,000-year integrated record of marine and terrestrial environmental change off Gabon, west equatorial Africa	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Ogooue; Monsoon; Last Glacial Maximum; Holocene; Pollen; Dinoflagellate cysts	WALLED DINOFLAGELLATE CYSTS; LAST DEGLACIATION; LATE QUATERNARY; CLIMATE CHANGES; RAIN-FOREST; TROPICAL ATLANTIC; LATE-HOLOCENE; SEDIMENTS; POLLEN; BP	Dinoflagellate cysts, pollen and charred cuticle fragments from two sediment cores (giant piston Calypso core MD03-2708 and giant gravity Casq core MD03-2708CQ) collected off the Ogooue River mouth, Gabon (01 degrees 10.33'S-08 degrees 19.01'E, 920 m water depth) have been analysed to identify the direction and timing of marine-terrestrial environmental changes over western equatorial Africa during the last 26,000 yr. Changes in the proxy records indicate that both terrestrial and oceanic domains off Gabon were impacted synchronously by significant climate changes during the last glacial-interglacial transition and Holocene. Leading into, and during, the Last Glacial Maximum (LGM), heterotrophic dinoflagellate cysts and Ca X-ray fluorescence intensity suggest nutrient enrichment off the river mouth, while pollen records indicate expansions of open forest, savannah woodland, and the Afromontane forest in the catchment area. From the deglaciation to mid-Holocene, however, a marked decrease in Brigantedinium spp. as well as in Poaceae. Cyperaceae and Podocarpus pollen reflects a reduction in nutrient supply to the coastal ocean in parallel with a reduction in grassland, herbaceous communities and Afromontane forest within the catchment. A sharp decline or even disappearance of heterotrophic species during this period is almost contemporaneous with an appearance of Operculodinium aguinawense, reflecting enhanced river influence in the study area. A marked increase of Rhizophora (mangrove) pollen during this transition also indicates eustatic sea-level rise after the LGM which forced a major expansion of the mangrove ecosystem across the gradually submerging shelf. The combination during the late Holocene of a reoccurrence of heterotrophic dinoflagellate cysts with increased Poaceae, Cyperaceae and Podocarpus pollen indicates enhanced nutrient supply to the ocean concordant with a shift to cooler/drier conditions over the Gabon basin. This appears to be linked to a deterioration of the monsoon system induced by the low sea-surface temperatures in the tropical Atlantic Ocean in association with decreased summer insolation. (C) 2010 Elsevier B.V. All rights reserved.	[Kim, So-Young; Lim, Dhong-Il] Korea Ocean Res & Dev Inst, S Sea Res Inst, Jangmok Myun 656830, Geoje, South Korea; [Kim, So-Young; Scourse, James; Marret, Fabienne] Bangor Univ, Coll Nat Sci, Sch Ocean Sci, Menai Bridge LL59 5AB, Gwynedd, Wales; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 3BX, Merseyside, England	Korea Institute of Ocean Science & Technology (KIOST); Bangor University; University of Liverpool	Kim, SY (通讯作者)，Korea Ocean Res & Dev Inst, S Sea Res Inst, 391 Jangmok Ri, Jangmok Myun 656830, Geoje, South Korea.	kimsy@kordi.re.kr	Lim, Dhongil/ACH-3964-2022; Kim, So-Young/JFS-7698-2023	Marret-Davies, Fabienne/0000-0003-4244-0437; Lim, Dhongil/0000-0002-0832-2907	Korea Ocean Research and Development Institute [PE98443]; National Institute for International Education Development; NERC [NRCF010001, bosc01001] Funding Source: UKRI	Korea Ocean Research and Development Institute; National Institute for International Education Development; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This work was supported by the Korea Ocean Research and Development Institute research program under grant no. PE98443 and the Korean Government Overseas Scholarship program of the National Institute for International Education Development. We thank the UK Natural Environment Research Council for Radiocarbon Allocation 1162.1005. We are grateful to the editor Prof. Thierry Correge and two anonymous reviewers for constructive comments which considerably strengthened the manuscript.	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Paleoclimatol. Paleoecol.	NOV 10	2010	297	2					428	438		10.1016/j.palaeo.2010.08.026	http://dx.doi.org/10.1016/j.palaeo.2010.08.026			11	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	681SY					2025-03-11	WOS:000284340500015
J	Figueroa, RI; Garcés, E; Camp, J				Isabel Figueroa, Rosa; Garces, Esther; Camp, Jordi			Reproductive plasticity and local adaptation in the host-parasite system formed by the toxic <i>Alexandrium minutum</i> and the dinoflagellate parasite <i>Parvilucifera sinerae</i>	HARMFUL ALGAE			English	Article						Alexandrium minutum; Cyst formation; Dinoflagellates; Local adaptation; Parvilucifera; Plastic response; Sexuality	SEXUAL REPRODUCTION; DINOPHYCEAE; COEVOLUTION; COMPATIBILITY; AVAILABILITY; POPULATIONS; STRATEGIES; EVOLUTION; INFECTION; FREQUENCY	A parasite threat stimulates adaptive shifts in the life-history strategy (sexual recombination rate) of the toxic bloom-forming dinoflagellate Alexandrium minutum Halim. This microalgae divides asexually when clonal but can also form mobile zygotes (planozygotes) when compatible clones are crossed. Planozygotes usually form resistant dormant stages (resting cysts) although they can also divide. In this study, asexual and sexual cultures were infected with the parasite Parvilucifera sinerae (Perkinsozoa) and the resulting clones classified as susceptible (S), low susceptible (LS), or resistant (R) to the infection. R and LS clones were never of Mediterranean origin, pointing to local adaptation of the parasite. (S x S) crosses were infected faster than either of the parental clones growing asexually. By contrast, (S x R) crosses were resistant to the parasite and produced no resting cysts, even when planozygotes were formed. Therefore, in infected cultures, the planozygotes mainly divided instead of encysting, thus increasing the rate at which recombinant progeny formed. This strategy against infection seems to combine the benefits of quickly producing asexual offspring and increasing recombination. As the susceptibility of the crosses was dependent on parental sexual compatibility, and cultures established by the division of (R x S) planozygotes (F1 offspring) also formed R or LS cultures, resistance may be regulated by several genes or through maternal effects. (C) 2010 Elsevier B.V. All rights reserved.	[Isabel Figueroa, Rosa; Garces, Esther; Camp, Jordi] CSIC, ICM, E-08003 Barcelona, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Figueroa, RI (通讯作者)，CSIC, ICM, Pg Maritim Barceloneta 37-49, E-08003 Barcelona, Spain.	figueroa@icm.csic.es	Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011	Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X; Camp, Jordi/0000-0002-5202-9783	PARAL [CTM2009-08399]; CSIC; Spanish Ministry of Science and Innovation;  [I3P]	PARAL; CSIC; Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); 	The authors thank the Spanish Institute of Oceanography (Vigo) for kindly lending us the Alexandrium minutum strains. This study was supported by the Spanish funded project PARAL (CTM2009-08399). The work of R.I. Figueroa and E. Garces was supported by a postdoctoral grant I3P and a Ramon y Cajal award respectively, from the CSIC and the Spanish Ministry of Science and Innovation. 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J	Cucchiari, E; Pistocchi, R; Pezzolesi, L; Penna, A; Battocchi, C; Cerino, F; Totti, C				Cucchiari, Emellina; Pistocchi, Rossella; Pezzolesi, Laura; Penna, Antonella; Battocchi, Cecilia; Cerino, Federica; Totti, Cecilia			Resting cysts of <i>Fibrocapsa japonica</i> (Raphidophyceae) from coastal sediments of the northern Adriatic Sea (Mediterranean Sea)	HARMFUL ALGAE			English	Article						Adriatic Sea; Cyst; Fibrocapsa japonica; ITS-5.8S rDNA; Raphidophyceae; Resting stages	SETO INLAND SEA; RED TIDE FLAGELLATE; CHATTONELLA-MARINA RAPHIDOPHYCEAE; GONYAULAX-TAMARENSIS; TOXIC DINOFLAGELLATE; ALGAL BLOOMS; LIFE-CYCLE; DINOPHYCEAE; GERMINATION; SEXUALITY	Fibrocapsa japonica resting cysts were detected in coastal sediments of the Marche region (northern Adriatic Sea, Italy), where summer blooms regularly occur. Sampling was carried out along 18 transects (2 stations each) during May-June 2007. The identification and counting of raphidophyte cysts were carried out under the inverted microscope and molecular analyses were applied to sediment samples to confirm species-specific identification. Raphidophyte cysts were recorded in almost all stations with maximum abundance of 9 +/- 5 and 12 +/- 3 cysts g(-1) dw for cysts of F. japonica and undetermined Raphidophyceae, respectively. Cyst formation was induced in F. japonica monoclonal cultures under different conditions: shadow-optimal temperature and dark-low temperature treatment; both experiments were performed at two salinity values (30 and 35). Cyst formation (preliminary cysts) was observed in both experiments, although with different encystment rates. However, only a further permanence in the dark at 15 degrees C in microplates led to the formation of mature cysts, probably supported by the possibility to adhere to solid surfaces. Before pre-cyst formation, vegetative cells showed a cytoplasmatic "brown body". (C) 2010 Elsevier B.V. All rights reserved.	[Cucchiari, Emellina; Cerino, Federica; Totti, Cecilia] Univ Politecn Marche, Dipartimento Sci Mare, I-60131 Ancona, Italy; [Pistocchi, Rossella; Pezzolesi, Laura] Univ Bologna, Ctr Interdipartimentale Ric Sci Ambientali, I-48100 Ravenna, Italy; [Penna, Antonella; Battocchi, Cecilia] Univ Urbino, Sez Biol Ambientale, Dipartimento Sci Biomol, I-61100 Pesaro, Italy	Marche Polytechnic University; University of Bologna; University of Urbino	Totti, C (通讯作者)，Univ Politecn Marche, Dipartimento Sci Mare, I-60131 Ancona, Italy.	c.totti@univpm.it	Pezzolesi, Laura/ABD-7677-2020; TOTTI, Cecilia Maria/A-9178-2016	PISTOCCHI, ROSSELLA/0000-0003-1304-6270; Cerino, Federica/0000-0002-9191-9957; TOTTI, Cecilia Maria/0000-0002-1532-6009; PEZZOLESI, LAURA/0000-0002-6260-2715	Ordinary Scientific Research funds of University	Ordinary Scientific Research funds of University	Authors are grateful to Franca Guerrini and Tiziana Romagnoli for laboratory support. 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J	Coats, DW; Kim, S; Bachvaroff, TR; Handy, SM; Delwiche, CF				Coats, D. Wayne; Kim, Sunju; Bachvaroff, Tsvetan R.; Handy, Sara M.; Delwiche, Charles F.			<i>Tintinnophagus acutus</i> n. g., n. sp. (Phylum Dinoflagellata), an Ectoparasite of the Ciliate <i>Tintinnopsis cylindrica</i> Daday 1887, and Its Relationship to <i>Duboscquodinium collini</i> Grasse 1952	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Ciliate; dinoflagellate; parasite; taxonomy; tintinnids	SP-NOV DINOPHYCEAE; LAKE TOVEL; PARASITE; FISH; GEN.; DUBOSCQUELLA; REPRODUCTION; PHYLOGENY; OCELLATUM; LETHAL	The dinoflagellate Tintinnophagus acutus n. g., n. sp., an ectoparasite of the ciliate Tintinnopsis cylindrica Daday, superficially resembles Duboscquodinium collini Grasse, a parasite of Eutintinnus fraknoii Daday. Dinospores of T. acutus are small transparent cells having a sharply pointed episome, conspicuous eyespot, posteriorly positioned nucleus with condensed chromosomes, and rigid form that may be supported by delicate thecal plates. Dinospores attach to the host via a feeding tube, losing their flagella, sulcus, and girdle to become spherical or ovoid cells. The trophont of T. acutus feeds on the host for several days, increasing dramatically in size before undergoing sporogenesis. Successive generations of daughter sporocytes are encompassed in an outer membrane or cyst wall, a feature not evident in trophonts. Tintinnophagus acutus differs from D. collini in host species, absence of a second membrane surrounding pre-sporogenic stages, and failure to differentiate into a gonocyte and a trophocyte at the first sporogenic division. Phylogenetic analyses based on small subunit (SSU) ribosomal DNA (rDNA) sequences placed T. acutus and D. collini in the class Dinophyceae, with T. acutus aligned loosely with Pfiesteria piscicida and related species, including Amyloodinium ocellatum, a parasite of fish, and Paulsenella vonstoschii, a parasite of diatoms. Dubosquodinium collini nested in a clade composed of several Scrippsiella species and Peridinium polonicum. Tree construction using longer rDNA sequences (i.e. SSU through partial large subunit) strengthened the placement of T. acutus and D. collini within the Dinophyceae.	[Coats, D. Wayne; Kim, Sunju; Bachvaroff, Tsvetan R.] Smithsonian Environm Res Ctr, POB 28, Edgewater, MD 21037 USA; [Handy, Sara M.; Delwiche, Charles F.] Univ Maryland, College Pk, MD 20742 USA	Smithsonian Institution; Smithsonian Environmental Research Center; University System of Maryland; University of Maryland College Park	Kim, S (通讯作者)，Smithsonian Environm Res Ctr, POB 28, Edgewater, MD 21037 USA.	kimsu@si.edu	Kim, Sunju/IXN-3072-2023; Handy, Sara/C-6195-2008; Delwiche, Charles Francis/C-6549-2008	Bachvaroff, Tsvetan/0000-0003-3800-9214; Delwiche, Charles Francis/0000-0001-7854-8584; Coats, D Wayne/0000-0002-0636-189X; Handy, Sara/0000-0003-3861-4609	National Science Foundation [EF-06299624, OCE-8911316]	National Science Foundation(National Science Foundation (NSF))	This work was funded in part by a National Science Foundation, Assembling the Tree of Life grant to C. F. D, D. W. C., and colleagues (EF-06299624) and a NSF Biological Oceanography award OCE-8911316 to D. W. C. Support on a Smithsonian Post-doctoral Fellowship enabled Sunju Kim to participate in the project. Collection and processing of sample in Villefranche-sur-Mer were made possible through the hospitality of Dr. John R. Dolan, Laboratoire d'Oceanographie de Villefranche Station Zoologique, and by logistic support from the ANR-BIODIVERSITE project AQUAPARADOX. We are greatly indebted to Dr. Sabine Agatha, Fachbereich Organismische Biologie, Universitat Salzburg for advice on tintinnid taxonomy and to Lois Reid for illustrations.	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J	Riding, JB; Mantle, DJ; Backhouse, J				Riding, James B.; Mantle, Daniel J.; Backhouse, John			A review of the chronostratigraphical ages of Middle Triassic to Late Jurassic dinoflagellate cyst biozones of the North West Shelf of Australia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						biostratigraphy; chronostratigraphy; dinoflagellate cysts; Mesozoic; North West Shelf; Australia	EARLIEST CRETACEOUS STRATA; BAYU-UNDAN FIELD; NEW-ZEALAND; TIMOR SEA; STRATIGRAPHIC PALYNOLOGY; SEQUENCE STRATIGRAPHY; EROMANGA BASIN; BAJOCIAN; BIOSTRATIGRAPHY; ASSEMBLAGES	The chronostratigraphical ages of the 20 dinoflagellate cyst zones and one dinoflagellate cyst assemblage for the Middle Triassic (Ladinian) to the Jurassic-Cretaceous transition of the North West Shelf of Australia are comprehensively reviewed. Evidence from macro- and micropalaeontology, palynology and strontium isotopes made available after the establishment of these biozones in the 1980s has been used to reassess the ages of this important zonal scheme and to calibrate it to the international stratigraphical stages. The Shublikodinium Superzone is renamed herein as the Rhaetogonyaulax Superzone, and based on conodont evidence is determined to span the Ladinian to Early Sinemurian. This is significantly shorter in duration than was originally envisaged (Late Anisian to Late Pliensbachian). The Luehndea Assemblage is a low diversity dinoflagellate cyst association which marks a eustatic rise; it is subdivided into two subzones. It is of latest Pliensbachian to Early Toarcian age, based largely on palynological evidence. The Bajocian to earliest Oxfordian Pareodinia ceratophora Superzone represents the inception of a continuous Mesozoic-Cenozoic dinoflagellate cyst record in Australia. It comprises seven zones, which are considered to be slightly older than originally interpreted. The overlying Pyxidiella Superzone is characterised by diverse dinoflagellate cyst associations. It is Early Oxfordian to Kimmeridgian in age, and comprises three zones. The bases of the Wanaea spectabilis and Wanaea clathrata zones are reinterpreted as being slightly older than originally proposed. The superjacent Fromea cylindrica Superzone is Tithonian to earliest Valanginian and modified ages are indicated for four of the nine zones. This unit is dominated by endemic dinoflagellate cysts, reflecting a global trend towards provincialism at this time due to a regressive eustatic regime. (C) 2010 NERC and Geoscience Australia. Published by Elsevier B.V. All rights reserved.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England; [Mantle, Daniel J.] Geosci Australia, Canberra, ACT 2601, Australia; [Backhouse, John] Univ Western Australia, Sch Earth & Environm, Crawley, WA 6009, Australia	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; Geoscience Australia; University of Western Australia	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England.	jbri@bgs.ac.uk			Virtual Centre of Economic Micropalaeontology and Palynology (VCEMP); BGS Individual Merit project 'Global Jurassic dinoflagellate cyst palaeobiology and its applications'; NERC [bgs010024] Funding Source: UKRI	Virtual Centre of Economic Micropalaeontology and Palynology (VCEMP); BGS Individual Merit project 'Global Jurassic dinoflagellate cyst palaeobiology and its applications'; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution is part of a joint British Geological Survey (BGS) and Geoscience Australia (GA) research programme under the auspices of the Virtual Centre of Economic Micropalaeontology and Palynology (VCEMP). It was produced as part of the BGS Individual Merit project of James B. Riding entitled 'Global Jurassic dinoflagellate cyst palaeobiology and its applications.' The authors are grateful to Dr Clinton B. Foster (GA) for enthusiastically facilitating and promoting this research. The manuscript greatly benefited from rigorous discussions on all aspects of Triassic-Jurassic dinoflagellate cyst biostratigraphy with Robin Helby and Natalie Sinclair; they are both warmly acknowledged. The authors thank the four internal reviewers from BGS and GA, and two anonymous referees for their perceptive comments on initial drafts of the manuscript. Bianca Reese and Veronika Galinec (GA) are acknowledged for drafting the figures. James B. Riding and Daniel J. Mantle publish with the permission of the Executive Director, British Geological Survey (NERC) and the Chief Executive Officer, Geoscience Australia respectively.	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Palaeobot. Palynology	NOV	2010	162	4					543	575		10.1016/j.revpalbo.2010.07.008	http://dx.doi.org/10.1016/j.revpalbo.2010.07.008			35	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	694UL		Green Accepted			2025-03-11	WOS:000285324400001
J	Mudie, PJ; Marret, F; Rochon, A; Aksu, AE				Mudie, Peta J.; Marret, Fabienne; Rochon, Andre; Aksu, Ali E.			Non-pollen palynomorphs in the Black Sea corridor	VEGETATION HISTORY AND ARCHAEOBOTANY			English	Article						Non-pollen palynomorphs; Shales; Black Sea; Pleistocene; Holocene	WALLED DINOFLAGELLATE CYSTS; ST-ERTH BEDS; FLAGELLAR APPARATUS; LATE PLEISTOCENE; HOLOCENE; WATER; MARMARA; ALGAE; PLIOCENE; SPORES	There have been few studies of non-pollen palynomorphs (NPP) in Holocene brackish water environments. The Black Sea is one of the world's largest and deepest bodies of stable brackish water and a natural laboratory for study of marine carbon cycling to anoxic sediments. The main NPP in the modern sediments of this brackish water sea are dinoflagellate cysts (dinocysts), acritarchs (mainly the prasinophytes Cymatiosphaera, Micrhystridium, Sigmopollis and Pseudoschizaea) and diverse fungal remains. Other NPP include colonial algae, tintinnids, copepod and cladoceran egg covers, testate amoebae and microforaminiferal linings. These NPP assemblages are similar to those in the marginal marine environment of the Pliocene St. Erth Beds (England), but have more abundant NPP, and virtually lack scolecodonts. In the Black Sea corridor, modern assemblages from areas with salinity > 22aEuro degrees have higher percentages of microforaminiferal linings and fewer prasinophytes, colonial algae and fungal spores. Prasinophytes dominate only in mid-Holocene sediments, during a 2000 years interval of sea level transgression and sapropel deposition. Early Holocene sediments have lower dinocyst diversity, increased fresh-brackish water colonial algae (Pediastrum spp. and Botryococcus braunii), zygnemataceous spores and desmids (including Zygnema, Cosmarium), ostracod linings and fewer foraminiferal linings. These assemblages are similar to those in the Baltic Sea where the annual salinity is about 6-8aEuro degrees.	[Mudie, Peta J.] Nat Resources Canada, Geol Survey Canada Atlantic, Dartmouth, NS B3H 1S3, Canada; [Marret, Fabienne] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Rochon, Andre] Univ Quebec, Rimouski, PQ GL5 3A1, Canada; [Mudie, Peta J.; Aksu, Ali E.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF, Canada	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Liverpool; University of Quebec; Memorial University Newfoundland	Mudie, PJ (通讯作者)，Nat Resources Canada, Geol Survey Canada Atlantic, 1 Challenger Dr, Dartmouth, NS B3H 1S3, Canada.	pmudie@nrcan.gc.ca; f.marret@liv.ac.uk; andre_rochon@uqar.qc.ca; aaksu@mun.ca		Marret-Davies, Fabienne/0000-0003-4244-0437				Aksu AE, 2002, MAR GEOL, V190, P119, DOI 10.1016/S0025-3227(02)00345-6; Aysel Veysel, 2008, Journal of the Black Sea Mediterranean Environment, V14, P53; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Beyens L., 2001, TRACKING ENV CHANGE, V3, P121; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; CHRISTOPHER R A, 1976, Micropaleontology (New York), V22, P143, DOI 10.2307/1485396; de la Rue SR, 2007, INT J COAL GEOL, V71, P72, DOI 10.1016/j.coal.2006.06.003; DE VERNAL A, 1989, CAN J EARTH SCI, V26, P2450, DOI 10.1139/e89-209; Degens E, 1974, The Black Sea - Geology, Chemistry and Biology, P396; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; Fensome R.A., 1990, ACRITARCHS FOSSIL PR, P1; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Filipova-Marinova M., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P453, DOI [10.1007/978-1-4020-5302-319, DOI 10.1007/978-1-4020-5302-319, 10.1007/978-1- 4020-5302-3_19, DOI 10.1007/978-1-4020-5302-3_19]; Graham L.E., 2000, Algae; Guy-Ohlson D., 1996, Palynology: Principles and Applications, V1, P181; HAYWW, 1995, GEOLOGY, V40, P21; HEAD MJ, 1993, J PALEONTOL, V67, P1; Head MJ, 2006, J PALEONTOL, V80, P1, DOI 10.1666/0022-3360(2006)080[0001:TCOTCD]2.0.CO;2; Head MJ, 2003, J PALEONTOL, V77, P1, DOI 10.1666/0022-3360(2003)077<0001:NSODCA>2.0.CO;2; HEAD MJ, 1992, MICROPALEONTOLOGY, V38, P237, DOI 10.2307/1485790; HISCOTT RN, 2007, QUATERN INT, V167, P9; INOUYE I, 1990, J PHYCOL, V26, P329, DOI 10.1111/j.0022-3646.1990.00329.x; KALGUTKAR RM, 2000, CONTRIBUTION SERIES, V39; Kholeif SEA, 2009, PALYNOLOGY, V33, P1, DOI 10.2113/gspalynol.33.1.1; KONZALOVA M, 2002, ZPRAVY GEOLOGICKYCH, P209; Kunz-Pirrung Martina, 1998, Berichte zur Polarforschung, V281, P1; Marret F, 2004, REV PALAEOBOT PALYNO, V129, P1, DOI 10.1016/j.revpalbo.2003.10.002; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Marret F., 1993, PALYNOSCIENCES, V2, P267; Marret F, 2009, QUATERN INT, V197, P72, DOI 10.1016/j.quaint.2007.01.010; Matthiessen J, 2000, INT J EARTH SCI, V89, P470, DOI 10.1007/s005310000127; Matthiessen Jens, 1996, Senckenbergiana Maritima, V27, P33; Mee Laurence D., 2005, Oceanography, V18, P100; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; Morzadec-Kerfourn MT, 2005, QUATERN INT, V133, P137, DOI 10.1016/j.quaint.2004.10.006; Mudie PJ, 2007, QUATERN INT, V167, P73, DOI 10.1016/j.quaint.2006.11.009; Mudie Peta J., 2006, Transactions of the Royal Society of South Africa, V61, P139; Mudie PJ, 2004, REV PALAEOBOT PALYNO, V128, P143, DOI 10.1016/S0034-6667(03)00117-9; Mudie PJ, 2002, MAR GEOL, V190, P203, DOI 10.1016/S0025-3227(02)00348-1; MUDIE PJ, GEOLOGY GEO IN PRESS, pCH7; MUHSIN TM, 1987, CAN J BOT, V65, P1137, DOI 10.1139/b87-159; Murray J.W., 2007, BLACK SEA FLOOD QUES, P1, DOI DOI 10.1007/978-1-4020-5302-3_1; Nicholls KH, 1997, FRESHWATER BIOL, V38, P419, DOI 10.1046/j.1365-2427.1997.00247.x; PALS JP, 1980, REV PALAEOBOT PALYNO, V30, P371, DOI 10.1016/0034-6667(80)90020-2; PARKE M, 1978, J MAR BIOL ASSOC UK, V58, P239, DOI 10.1017/S0025315400024528; PLAYFORD G, 2003, CONTRIBUTIONS SERIES, V41; REID PC, 1978, J MAR BIOL ASSOC UK, V58, P551, DOI 10.1017/S0025315400041205; REID PC, 1981, REV PALAEOBOT PALYNO, V34, P251, DOI 10.1016/0034-6667(81)90043-9; Rossignol M., 1964, Revue de Micropaleontologie, V7, P83; Strother P.K., 1996, Palynology: Principles and Applications, Volume, V1, P81, DOI DOI 10.1016/0034-6667(95)00117-4; TAKAHASHI KIYOSHI, 1964, TRANS PROC PALAENTOL SOC JAP NEW SER, V54, P201; Tissot B.P., 1978, PETROLEUM FORMATION, DOI DOI 10.1007/978-3-642-96446-6; Tolun L, 2002, MAR GEOL, V190, P47, DOI 10.1016/S0025-3227(02)00342-0; Tomas C.R., 1993, Marine Phytoplankton. 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Hist. Archaeobot.	NOV	2010	19	5-6					531	544		10.1007/s00334-010-0268-9	http://dx.doi.org/10.1007/s00334-010-0268-9			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	684ZF					2025-03-11	WOS:000284593100012
J	Krepakevich, A; Pospelova, V				Krepakevich, Alanna; Pospelova, Vera			Tracing the influence of sewage discharge on coastal bays of Southern Vancouver Island (BC, Canada) using sedimentary records of phytoplankton	CONTINENTAL SHELF RESEARCH			English	Article						Eutrophication; Dinoflagellate cysts; Toxic species; Sewage; Estuaries; British Columbia	WALLED DINOFLAGELLATE CYSTS; SEA-SURFACE CONDITIONS; DE-FUCA STRAIT; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; BRITISH-COLUMBIA; LATE QUATERNARY; BIOGENIC OPAL; PUGET-SOUND; TOKYO-BAY	The impact of sewage and stormwater effluents on phytoplankton is investigated by comparing organic-walled dinoflagellate cyst abundance and diversity from 38 surface sediment samples flanking southern Vancouver Island Site locations include those directly adjacent to wastewater outfall at Clover and Macaulay Points and Saanich Peninsula as well as from a variety of near-shore environments with differing tidal flow influences Excellently preserved dinoflagellate cyst assemblages have been recovered and 36 cyst taxa were identified Local assemblages are characterized by a high relative proportion (average 56%) of cysts produced by heterotrophic dinoflagellates which is typical for regions of high primary production Relative proportional increases of cysts from heterotrophic species with particular Increases of Polykrikos kofoidn/schwartzu and Dubridinium species known to reflect areas affected by eutrophication occur directly adjacent to all three sewage outfalls as well as in the more stagnant waters of Esquimalt and Victoria Harbours and at the mouth of Cadboro Bay Further effects of an anthropogenic effluent can be seen in the relatively higher concentrations of organic carbon and the diatom production proxy biogenic opal Results from this study clearly indicate a much larger impact zone than predicted by a sewage effluent plume model or trends found in monitored benthic biota and sediment chemistry that evidence primary outfall affects <800 m eastward of Macaulay Point and about 200 m eastward of the Clover Point Enhanced production of cysts from potentially toxic Alexandrium species is also observed near locations of sewage outfalls (C) 2010 Elsevier Ltd All rights reserved	[Krepakevich, Alanna; Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada	University of Victoria	Krepakevich, A (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, Bob Wright Ctr A405,POB 3065 STN CSC, Victoria, BC V8W 3V6, Canada.			Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We thank Captain Brown and crew of the MSV Strickland for facilitating two very successful cruises the UBC Inorganic Geochemical Laboratory for biogenic opal and inorganic carbon analysis Kim Picard of NRCan and the Bedford Institute of Oceanography Sedimentary Laboratory for grain size analysis and Peter Chandler of the Institute of Ocean Sciences for providing current results from the CRD Mooring Program The Natural Sciences and Engineering Research Council of Canada (NSERC) provided funding for this work	Anderson DM, 2008, HARMFUL ALGAE, V8, P39, DOI 10.1016/j.hal.2008.08.017; Bouimetarhan I, 2009, MAR MICROPALEONTOL, V71, P113, DOI 10.1016/j.marmicro.2009.02.001; BOYER TP, 2002, 50 NOAA ATL NESDIS; CHANDLER P, 2001, POSTDISCHARGE MARINE; Chandler P, 1997, SUMMARY CRD MOORING; Chapman PM, 2006, MAR POLLUT BULL, V52, P719, DOI 10.1016/j.marpolbul.2006.03.006; Conkright M., 2002, NUTRIENTS; *CRD ENV SERV DEP, 2007, SAAN PEN LIQ WAST MA; *CRD ENV SERV DEP, 2000, COR AR LIQ WAST MAN; *CRD MAR PROGR, 2008, CRD STORMW QUAL ANN; *CRD MAR PROGR, 2008, MAC CLOV POINT WAST; *CRD MAR PROGR, 2008, SAAN PEN TREATM PLAN; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Ellegaard M, 2006, ESTUAR COAST SHELF S, V68, P567, DOI 10.1016/j.ecss.2006.03.013; Fensome R.A., 1993, CLASSIFICATION FOSSI; FOREMAN MGG, 1995, J GEOPHYS RES-OCEANS, V100, P721, DOI 10.1029/94JC02721; González C, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2008PA001602; Harland R, 2006, SCI TOTAL ENVIRON, V355, P204, DOI 10.1016/j.scitotenv.2005.02.030; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2002, J MICROPALAEONTOL, V21, P169, DOI 10.1144/jm.21.2.169; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hodgins D. 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Shelf Res.	OCT 31	2010	30	18					1924	1940		10.1016/j.csr.2010.09.002	http://dx.doi.org/10.1016/j.csr.2010.09.002			17	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	682GZ					2025-03-11	WOS:000284390700002
J	Heldt, M; Lehmann, J; Willems, H				Heldt, M.; Lehmann, J.; Willems, H.			Calcareous dinoflagellate cysts from the Aptian/Albian boundary interval of northern Germany: Abundance patterns related to orbital forcing?	NEWSLETTERS ON STRATIGRAPHY			English	Article						Aptian; Albian; Calcareous dinoflagellate cysts; Lower Saxony Basin; North Germany	LOWER SAXONY BASIN; NW GERMANY; CRETACEOUS SEDIMENTS; CLIMATIC-CHANGE; EVOLUTION; SEA; NANNOFOSSILS; PALEOCLIMATE; ENGLAND; MARGIN	Boreal Aptian-Albian marine sediments of the Hannover region (northern Germany) mainly consist of dark to medium grey claystones, which were deposited in the central part of the Lower Saxony Basin. Calcareous dinoflagellate cyst samples of the Vohrum clay pit, east of Hannover, yield a diverse flora of latest Aptian-earliest Albian (H jacobi/L. schrammeni ammonite zones). A total of 24 different morphotypes with radial and oblique wall structures has been observed. Among these, eight undescribed species have been identified. The associations of all samples are dominated by two typical Boreal Aptian-Albian morphotypes with radial wall structures: Praecalcigonellum polymorphum and Echinodinella erinacea, which together constitute around 75% of all specimens encountered. All other morphotypes are scarce, except those of the phylogenetically closely related species Pirumella multistrata forma multistrata and Pirumella cf. heirtzleri, which together constitute another 16% of the assemblage. The dominance of Boreal forms is in accordance with a cool global climatic phase, which has been suggested by independent evidence for the Aptian/Albian boundary interval. Praecalcigonellum polymorphum and Echinodinella erinacea are alternately abundant within the succession; each of this species rhythmically reaches abundance peaks/minima every 2.5 m intervals. These rhythms remind of bedding rhythms from time-equivalent outcrops and cores of the Hannover region, which have been related to eccentricity cycles of the Milankovitch frequency band.	[Heldt, M.] Fed Inst Geosci & Nat Resources, D-30655 Hannover, Germany; [Lehmann, J.; Willems, H.] Univ Bremen, D-28334 Bremen, Germany	University of Bremen	Heldt, M (通讯作者)，Fed Inst Geosci & Nat Resources, Stilleweg 2, D-30655 Hannover, Germany.	Matthias.Heldt@bgr.de	Lehmann, Jens/A-6516-2009	Lehmann, Jens/0000-0001-6580-6644	European Community	European Community	This research received support from the SYNTHESIS Project, financied by the European Community Research Infrastructure Action under the FP7 Integrating Activities Programme.	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J	Soták, J				Sotak, Jan			Paleoenvironmental changes across the Eocene-Oligocene boundary: insights from the Central-Carpathian Paleogene Basin	GEOLOGICA CARPATHICA			English	Article						Paratethys; Central Western Carpathians; Terminal Eocene Event; platform drowning; climatic cooling; productivity changes; estuarine circulation; anoxia; eutrophication; semi-isolation	COOL-WATER CARBONATE; FORE-ARC BASIN; WESTERN CARPATHIANS; FORAMINIFERAL BIOSTRATIGRAPHY; PALEOCLIMATIC INTERPRETATION; PALEOGEOGRAPHIC SIGNIFICANCE; PLANKTONIC-FORAMINIFERA; DINOFLAGELLATE CYSTS; MICROFACIES ANALYSIS; EVOLUTIONARY TRENDS	The sedimentary sequence of the Central-Carpathian Paleogene Basin provides proxy records of climatic changes related to cooling events at the Eocene/Oligocene boundary (TEE). In this basin, climatic deterioration is inferred from the demise of the carbonate platform and oligotrophic benthic biota in the SBZ19 and from the last species of warm-water planktonic foraminifers in the El 4 Zone. Upper Eocene formations already indicate warm-temperate to cool-temperate productivity and nutrient-enriched conditions (Bryozoan Marls, Globigerina Marls). Rapid cooling during the earliest Oligocene (Oi-1 event) led to a temperature drop (similar to 11 degrees C), humidity, fresh water influx and continental runoff, water mass stratification, bottom water anoxia, eutrofication, estuarine circulation and upwelling, carbonate depletion, sapropelitic and biosiliceous deposition, H2S intoxication and mass faunal mortality, and also other characteristics of Black Sea-type basins. Tectonoeustatic events with the interference of TA 4.4 sea-level fall and the Pyrenean phase caused basin isolation at the beginning of the Paratethys. The Early Oligocene. stage of Paratethyan isolation is indicated by a stagnant regime, low tide influence, endemic fauna development, widespread anoxia and precipitation of manganese deposits. The episodic rise in the sea-level, less humid conditions and renewed circulation is marked by calcareous productivity, nannoplankton blooms and the appearance of planktic pteropods and re-oxygenation. Paleogeographic differentiation of the Carpatho-Pannonian Paleogene basins resulted from plate-tectonic reorganization during the Alpine orogenesis.	Slovak Acad Sci, Inst Geol, Banska Bystrica 97411, Slovakia	Slovak Academy of Sciences	Soták, J (通讯作者)，Slovak Acad Sci, Inst Geol, Dumbierska 1, Banska Bystrica 97411, Slovakia.	sotak@savbb.sk	Soták, Ján/AAC-7053-2019	Sotak, Jan/0000-0003-0095-5299	Scientific Grant Agency of the Ministry of Education of the Slovak Republic; Slovak Academy of Sciences (VEGA) [2/0140/09]	Scientific Grant Agency of the Ministry of Education of the Slovak Republic; Slovak Academy of Sciences (VEGA)(Vedecka grantova agentura MSVVaS SR a SAV (VEGA))	The author wishes to thank to Przemyslaw Gedl, Andras Nagymarosy and Diego Puglisi for their valuable comments and improvements in earlier drafts of the manuscript. This research was supportedby the Scientific Grant Agency of the Ministry of Education of the Slovak Republic and the Slovak Academy of Sciences (VEGA Grant 2/0140/09).	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Carpath.	OCT	2010	61	5					393	418		10.2478/v10096-010-0024-1	http://dx.doi.org/10.2478/v10096-010-0024-1			26	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	679XJ		gold			2025-03-11	WOS:000284193800004
J	D'Errico, M; Di Staso, A				D'Errico, Marco; Di Staso, Angelida			Stratigraphic revision of the Cenozoic deposits of the Lungro-Verbicaro Unit (Northern Calabria): new data for the reconstruction of tectonic evolution of the southern Apennines	ITALIAN JOURNAL OF GEOSCIENCES			English	Article						Stratigraphy; calcareous nannofossils; dinoflagellate cysts; Cenozoic; Lungro-Verbicaro Unit; Northern Calabria		Field and biostratigraphic data from Cenozoic metasedimentary succession ("breccia a selce", Colle Trodo and "Scisti del Fiume Lao" Formations) of Lungro-Verbicaro Unit are reported. The "Scisti del Fiume Lao" Formation, formerly included in the ophiolite-bearing Frido Unit, defined at the Calabria-Lucania border area, is interpreted as the stratigraphic uppermost part of the above Cenozoic succession. Therefore, the occurrence of nannofossil assemblage not older than late Aquitanian, represents the minimum age constrain both to the deformation and to the HP/LT metamorphic event affecting the Lungro-Verbicaro Unit. This age is in agreement with the Burdigalian radiometric age recognized in metavolcanic and metapelitic rocks of Lungro-Verbicaro Unit.	[D'Errico, Marco; Di Staso, Angelida] Univ Naples Federico 2, Dipartimento Sci Terra, I-80138 Naples, Italy	University of Naples Federico II	Di Staso, A (通讯作者)，Univ Naples Federico 2, Dipartimento Sci Terra, Largo San Marcellino 10, I-80138 Naples, Italy.	distaso@unina.it	Di Staso, Angelida/C-6878-2008; D'Errico, Marco/B-5733-2013		Italian Ministry of University	Italian Ministry of University(Ministry of Education, Universities and Research (MIUR))	Financial support from the Italian Ministry of University (PRINT 2006, Resp. G. Bonardi).	Amidio-Morelli L., 1976, Memorie della Societa Italiana, V17, P1; [Anonymous], 1975, BOLLETTINO SOC GEOLO; [Anonymous], B SOC GEOLOGICA ITAL; BIGI G, 1991, QUADERNI RICERCA SCI, V114; BONARDI G, 1993, CR ACAD SCI II, V317, P955; Bonardi G., 1976, Mem. Soc. Geol. It, V17; Bonardi G., 1988, Memorie della Societa Geologica Italiana, V41, P17; BOUSQUET JC, 1969, CR HEBD ACAD SCI, V264, P204; Damiani A. V., 1970, B SOC GEOL ITAL, V89, P65; De Capoa P, 2003, COUR FOR SEKENBG, V244, P105; DERRICO M, 2004, THESIS U NAPOLI FEDE, P182; Grandjacquet C., 1962, Geologica Romana, V1, P297; Iannace A, 2007, J GEOL SOC LONDON, V164, P1165, DOI 10.1144/0016-76492007-017; Iannace A, 2005, CR GEOSCI, V337, P1541, DOI 10.1016/j.crte.2005.09.003; Iannace Alessandro, 1995, Rivista Italiana di Paleontologia e Stratigrafia, V101, P301; *INT COMM STRAT, 2004, INT STRAT CHART; Martini E., 1971, Proceeding of the 2nd International Conference of Planktonic Microfossils in Roma, P739, DOI DOI 10.1002/IROH.19720570511; OKADA H, 1980, MAR MICROPALEONTOL, V5, P321, DOI 10.1016/0377-8398(80)90016-X; PATACCA E, 2004, MEMORIE DESCRITTIVE, V63, P20; Patacca E., 1992, MEM SCI GEOL, V43, P297; PERRONE V, 1973, Rivista Italiana di Paleontologia e Stratigrafia, V79, P157; Perrone V, 1996, CR ACAD SCI II A, V322, P877; QUITZOW HW, 1935, GES WISS GOTTINGEN 4, V1, P83; Selli R., 1957, Giornale di Geologia, V26, P1; VALLARIO A, 1967, MEM SOC GEOL ITAL, V86, P233	25	4	5	0	2	SOC GEOLOGICA ITALIANA	ROME	UNIV DEGLI STUDI LA SAPIENZA, DIPART SCI DELLA TERRA, PIAZZALE ALDO MORO 5, ROME, I-00185, ITALY	2038-1719			ITAL J GEOSCI	Ital. J. Geosci.	OCT	2010	129	3					450	456		10.3301/IJG.2010.14	http://dx.doi.org/10.3301/IJG.2010.14			7	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	708MR					2025-03-11	WOS:000286366400008
J	Stutz, S; Borel, CM; Fontana, SL; del Puerto, L; Inda, H; García-Rodriguez, F; Tonello, MS				Stutz, Silvina; Marcela Borel, C.; Fontana, Sonia L.; del Puerto, Laura; Inda, Hugo; Garcia-Rodriguez, Felipe; Tonello, Marcela S.			Late Holocene climate and environment of the SE Pampa grasslands, Argentina, inferred from biological indicators in shallow, freshwater Lake Nahuel Ruca	JOURNAL OF PALEOLIMNOLOGY			English	Article						Holocene; Multi-proxy analysis; Paleolimnology; Pampa grasslands; Shallow lake	BUENOS-AIRES PROVINCE; LATE PLEISTOCENE; PALEOLIMNOLOGICAL EVIDENCE; PHYTOLITH ASSEMBLAGES; ALLUVIAL SEQUENCES; VEGETATION HISTORY; EVOLUTION; SEDIMENTS; COAST; ACRITARCHS	We analyzed pollen, non-pollen palynomorphs (NPPs), calcareous microfossils, plant macrofossils, diatoms, chrysophyte cysts, opal phytoliths and organic matter content in a 123-cm sediment sequence from Nahuel Ruca Lake, a shallow, freshwater system in the southeastern Pampa grasslands, Argentina. Three stages in the lake evolution were identified. Before 3,680 cal year BP, only pollen, NPPs (dinoflagellate cysts and acritarchs) and ostracods were recovered, suggesting brackish/saline conditions in the lake and nearby areas. Freshwater conditions are, however, indicated by Myriophyllum, Pediastrum and Zygnemataceae. The brackish/saline conditions could have been caused by marine influence during a Holocene sea level high stand that affected the area ca. 6,000 year BP. Between 3,680 and 390 cal year BP, macrophyte pollen and plant macrofossils indicate increasingly freshwater conditions in the lake and the adjacent area. Diatom and ostracod assemblages, however, suggest brackish and oligotrophic conditions, giving way to freshwater and meso-eutrophic conditions toward the end of this period. The relationship between submersed macrophytes (Myriophyllum, Potamogeton, Ceratophyllum, Chara) and planktonic algae (Chlorophyta and diatoms), suggests a shift in the lake from a clear to a turbid state. This turbid state is more evident after 390 cal year BP. High values of Pediastrum, Scenedesmus and diatoms (Cyclotella meneghiniana, Aulacoseira granulata, A. muzzanensis) observed during this stage could have reduced light penetration, with consequent loss of submersed plants. Pollen and plant macrofossils in the uppermost 20 cm indicate a shallow, freshwater lake similar to present, though an increase in brackish/freshwater diatoms suggests an increase in salinity, perhaps related to periodic droughts. Opal phytoliths yield a regional paleoclimatic reconstruction that agrees closely with inferences made using pollen, mammals and sediment characteristics.	[Stutz, Silvina; Tonello, Marcela S.] Univ Nacl Mar del Plata, FCEyN, Lab Paleoecol & Palinol, RA-7600 Mar Del Plata, Argentina; [Marcela Borel, C.] Univ Nacl Sur, Dept Geol, INGEOSUR, Lab Palinol, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Fontana, Sonia L.] Univ Gottingen, Dept Palynol & Climate Dynam, D-37073 Gottingen, Germany; [Fontana, Sonia L.] Uppsala Univ, EBC, Dept Evolutionary Funct Genom, S-75236 Uppsala, Sweden; Univ Republica, Fac Ciencias, Montevideo 11400, Uruguay; [Stutz, Silvina; Marcela Borel, C.] Consejo Nacl Invest Cient & Tecn, RA-1033 Buenos Aires, DF, Argentina	National University of Mar del Plata; National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); University of Gottingen; Uppsala University; Universidad de la Republica, Uruguay; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Stutz, S (通讯作者)，Univ Nacl Mar del Plata, FCEyN, Lab Paleoecol & Palinol, Funes 3250, RA-7600 Mar Del Plata, Argentina.	smstutz@mdp.edu.ar; maborel@criba.edu.ar; sonia.fontana@biologie.uni-goettingen.de; felipe.garciarodriguez@gmail.com	Fontana, Sonia/N-2263-2014	Inda, Hugo/0000-0003-1955-7821; del Puerto, Laura/0000-0003-2003-9263; Fontana, Sonia/0000-0001-8238-4172; Borel, C. Marcela/0000-0001-5772-4534; Tonello, Marcela Sandra/0000-0002-4134-3814	(NSF)-Arizona AMS Facility; ANPCyT [32345]; UNMdP [EXA 384/07]	(NSF)-Arizona AMS Facility(National Science Foundation (NSF)); ANPCyT(ANPCyT); UNMdP	We thank P. Urrutia for giving us permission to work on his property, and A. Gonzalez, M. Hernandez, I. Vilanova for their support during coring activities. F. I. Isla kindly lent us the vibracorer and T. Giesecke provided valuable comments on an early version of the manuscript. We thank the (NSF)-Arizona AMS Facility and T. Jull for financial support for dating. We thank Mark Brenner and two anonymous reviewers for helpful comments. Mark Brenner kindly corrected the English. Financial support was provided by PICT No. 32345 (ANPCyT) and EXA 384/07 (UNMdP).	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PACT, V50, P399; Vilanova I, 2006, J QUATERNARY SCI, V21, P227, DOI 10.1002/jqs.953; VILLALBA R, 2005, SERIES ADV GLOBAL CH, V23; Violante R.A., 2001, Rev. De. la Asoc. oN. Geol. ogica Argent., V56, P51; Violante R.A., 1992, REV ASOC GEOL ARGENT, V47, P201; Whatley R., 1997, Revista Espanola de Micropaleontologia, V29, P5; Zárate M, 2000, HOLOCENE, V10, P481, DOI 10.1191/095968300669846317	65	40	45	1	17	SPRINGER	DORDRECHT	VAN GODEWIJCKSTRAAT 30, 3311 GZ DORDRECHT, NETHERLANDS	0921-2728	1573-0417		J PALEOLIMNOL	J. Paleolimn.	OCT	2010	44	3					761	775		10.1007/s10933-010-9450-4	http://dx.doi.org/10.1007/s10933-010-9450-4			15	Environmental Sciences; Geosciences, Multidisciplinary; Limnology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology; Marine & Freshwater Biology	652AY		Green Published, hybrid			2025-03-11	WOS:000281973500002
J	Shin, HH; Matsuoka, K; Yoon, YH; Kim, YO				Shin, Hyeon Ho; Matsuoka, Kazumi; Yoon, Yang Ho; Kim, Young-Ok			Response of dinoflagellate cyst assemblages to salinity changes in Yeoja Bay, Korea	MARINE MICROPALEONTOLOGY			English	Article						dinoflagellate cysts; ellipsoidal Alexandrium cyst; salinity; Tsushima Warm Current; Yeoja Bay	COCHLODINIUM-POLYKRIKOIDES; SURFACE SEDIMENTS; ALEXANDRIUM-TAMARENSE; BRITISH-COLUMBIA; VANCOUVER-ISLAND; TOKYO-BAY; INDICATORS; WATER; SEA; EUTROPHICATION	To investigate dinoflagellate cysts as indicators of salinity or eutrophication and to document the historical occurrence of ellipsoidal Alexandrium cysts in the Korean coastal areas we studied a sediment core from Yeoja Bay The analyzed dinoflagellate cysts Include over 30 taxa commonly reported from other temperate regions Cluster analysis based on dinoflagellate cyst assemblages indicated two main time intervals from the mid-1990s to 2006 (Zone II) and from the early 1900s to early 1990s (Zone I) The total cyst concentration Increased sharply in Zone IT to reach approximately five times the level in Zone I The salinity in Yeoja Bay increased after 1995 (from 28 to 31 psu) possibly due to a stronger intrusion of the Tsushima Warm Current The increase in salinity coincided with increases in the abundance of Brigantedinium spp and Selenopemphix nephroides In addition ellipsoidal Alexandrium cysts have occurred since the 1980s and increased in abundance since the mid-1990s when a paralytic shellfish poisoning outbreak and increases in ellipsoidal Alexandrium cysts were recorded in several Korean and Japanese coastal areas This suggests that ellipsoidal Alexandrium cysts may have been carried to the Korean coast, including Yeoja Bay by the current system possibly the Tsushima Warm Current, and that the current system may influence the growth of Alexandrium cysts (C) 2010 Elsevier BV All rights reserved	[Shin, Hyeon Ho; Kim, Young-Ok] Korea Ocean Res & Dev Inst, Geoje 656830, South Korea; [Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Yeosu 550749, South Korea; [Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan	Korea Institute of Ocean Science & Technology (KIOST); Chonnam National University; Nagasaki University	Shin, HH (通讯作者)，Korea Ocean Res & Dev Inst, Geoje 656830, South Korea.		KIM, YOUNG JIN/E-9374-2011	Yoon, Yang Ho/0000-0001-8529-9512; Shin, Hyeon Ho/0000-0002-9711-6717	Korea Ocean Research and Development Institute [PE98521]; Nagasaki University	Korea Ocean Research and Development Institute; Nagasaki University	We thank all members of the Laboratory of Coastal Environmental Sciences Nagasaki University for their help with cyst analysis and also wish to express our gratitude to the reviewers for their critical comments which helped to improve the manuscript This work was supported by a grant from the Korea Ocean Research and Development Institute (PE98521) and by the Nagasaki University Major Research Project "Restoration of Marine Environment and Resources in East Asia	ASAKAWA M, 1995, TOXICON, V33, P691, DOI 10.1016/0041-0101(94)00177-A; Asakawa M., 1995, J FOOD HYG SOC JPN, V34, P50; Chang D.-S., 1987, Bulletin of the Korean Fisheries Society, V20, P293; Cho ES, 2001, BOT MAR, V44, P57, DOI 10.1515/BOT.2001.008; CHO HJ, 2000, THESIS NAGASAKI U, P112; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; FUKUYO Y, 1985, B MAR SCI, V37, P529; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; Hallett R.I., 1999, THESIS U WESTMINSTER, P109; 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; Head M.J., 1996, Palynology: Principles and Applications, P1197; Hue H.K., 2000, KOREAN J ENV BIOL, V18, P227; Hwang DW, 2005, MAR CHEM, V96, P61, DOI 10.1016/j.marchem.2004.11.002; Irwin A, 2003, HARMFUL ALGAE, V2, P61, DOI 10.1016/S1568-9883(02)00084-7; Jeter H.W., 2000, TERRA AQUA, V78, P21; Kim CJ, 2007, HARMFUL ALGAE, V6, P104, DOI 10.1016/j.hal.2006.07.004; KIM DI, 2003, THESIS KYUSHU U, P154; Kim H G., 1997, Recent Red Tides in Korean coastal Waters, P237; KIM HG, 1999, INITIATION COCHLODIN, P119; Kim HG, 1998, COCHLIDINIUM POLYKRI, P227; Kim Hyung Chul, 2001, Journal of the Korean Fisheries Society, V34, P445; Kim So-Young, 2003, Journal of the Korean Fisheries Society, V36, P290; Kong GS, 2007, J ASIAN EARTH SCI, V29, P84, DOI 10.1016/j.jseaes.2006.01.004; Kumar A, 2002, PALAEOGEOGR PALAEOCL, V180, P187, DOI 10.1016/S0031-0182(01)00428-X; Kwon C. 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Micropaleontol.	OCT	2010	77	1-2					15	24		10.1016/j.marmicro.2010.07.001	http://dx.doi.org/10.1016/j.marmicro.2010.07.001			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	683AB					2025-03-11	WOS:000284443000002
J	Godhe, A; Härnström, K				Godhe, Anna; Harnstrom, Karolina			Linking the planktonic and benthic habitat: genetic structure of the marine diatom <i>Skeletonema marinoi</i>	MOLECULAR ECOLOGY			English	Article						Bacillariophyceae; diatom; microsatellites; plankton; resting stage; Skeletonema marinoi	DINOFLAGELLATE ALEXANDRIUM-TAMARENSE; SWEDISH WEST-COAST; GULLMAR FJORD; POPULATION-GENETICS; MICROSATELLITE ANALYSIS; DITYLUM-BRIGHTWELLII; BLOOM DEVELOPMENT; SEPARATED CLONES; RESTING STAGES; SPRING BLOOM	Dormant life stages are important strategies for many aquatic organisms. The formation of resting stages will provide a refuge from unfavourable conditions in the water column, and their successive accumulation in the benthos will constitute a genetic reservoir for future planktonic populations. We have determined the genetic structure of a common bloom-forming diatom, Skeletonema marinoi, in the sediment and the plankton during spring, summer and autumn two subsequent years (2007-2009) in Gullmar Fjord on the Swedish west coast. Eight polymorphic microsatellite loci were used to assess the level of genetic differentiation and the respective gene diversity of the two different habitats. We also determined the degree of genetic differentiation between the seed banks inside the fjord and the open sea. The results indicate that Gullmar Fjord has one dominant endogenous population of S. marinoi, which is genetically differentiated from the open sea population. The fjord population is encountered in the plankton and in the sediment. Shifts from the dominant population can happen, and in our study, two genetically differentiated plankton populations, displaying reduced genetic diversity, occurred in September 2007 and 2008. Based on our results, we suggest that sill fjords maintain local long-lived and well-adapted protist populations, which continuously shift between the planktonic and benthic habitats. Intermittently, short-lived and mainly asexually reproducing populations can replace the dominant population in the water column, without influencing the genetic structure of the benthic seed bank.	[Godhe, Anna; Harnstrom, Karolina] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden	University of Gothenburg	Godhe, A (通讯作者)，Univ Gothenburg, Dept Marine Ecol, Box 461, SE-40530 Gothenburg, Sweden.	anna.godhe@marecol.gu.se			Formas [2006-1892]; Sida [SWE-2004-129]; University of Gothenburg Marine Research Centre (GMF)	Formas(Swedish Research Council Formas); Sida; University of Gothenburg Marine Research Centre (GMF)	We are thankful to Jenny Egardt and Lovisa Jansson for their assistance in the laboratory, to Stefan Agrenius (Department of Marine Ecology, University of Gothenburg) for providing the sediment samples from Kattegat and Skagerrak and to Professor Kerstin Johannesson (same Department) for commenting on an early version of the manuscript. Two anonymous reviewers are acknowledged for their constructive comments. The fragment analysis was performed at RSKC, University Hospital MAS. The DNA sequencing was carried out at Genomics Core Facility, The Sahlgrenska Academy, University of Gothenburg, by Dr Elham Rekabdar. This work was supported by grants from Formas (2006-1892), Sida (SWE-2004-129), University of Gothenburg Marine Research Centre (GMF), C.F. Lundstroms Stiftelse, Stiftelsen Oscar och Lilli Lamms Minne, Magnus Bergvalls Stiftelse, Lars Hiertas Minnesfond.	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Ecol.	OCT	2010	19	20					4478	4490		10.1111/j.1365-294X.2010.04841.x	http://dx.doi.org/10.1111/j.1365-294X.2010.04841.x			13	Biochemistry & Molecular Biology; Ecology; Evolutionary Biology	Science Citation Index Expanded (SCI-EXPANDED)	Biochemistry & Molecular Biology; Environmental Sciences & Ecology; Evolutionary Biology	660JD	20875064				2025-03-11	WOS:000282635700011
J	Grunert, P; Soliman, A; Coric, S; Scholger, R; Harzhauser, M; Piller, WE				Grunert, Patrick; Soliman, Ali; Coric, Stjepan; Scholger, Robert; Harzhauser, Mathias; Piller, Werner E.			Stratigraphic re-evaluation of the stratotype for the regional Ottnangian stage (Central Paratethys, middle Burdigalian)	NEWSLETTERS ON STRATIGRAPHY			English	Article						Central Paratethys; Ottnangian; stratotype; biostratigraphy; magnetostratigraphy	LOWER MIOCENE; OLIGOCENE; BIOSTRATIGRAPHY; TERTIARY	The Ottnangian stage represents the middle Burdigalian (c. 18.1-17.2 Ma) within the regional stratigraphic concept for the Central Paratethys. The section Ottnang-Schanze in the North Alpine Foreland Basin of Upper Austria has been defined as its stratotype by Rogl et al. (1973). We present an updated stratigraphic evaluation of the section based on biostratigraphy of foraminifers, dinoflagellate cysts and calcareous nannoplankton as well as magnetostratigraphy. In agreement with earlier studies, assemblages of benthic foraminifers (co-occurrence of Amphicoryna ottnangensis and Sigmoilopsis ottnangensis, mass-occurrences of Lenticulina inornata) document a late early Ottnangian age. Dinoflagellate cyst Exochosphaeridium insigne is recorded for the first time in the early Ottnangian and its occurrence together with Apteodinium spiridoides, Cordosphaeridium cantharellus and Glaphyrocysta reticulosa s. l. extends the regional dinoflagellate zone Ein from the middle to the early Ottnangian. On a global scale, the revealed marker species indicate zone D17a (middle-late Burdigalian). Calcareous nannoplankton assemblages with the very rare occurrence of Sphenolithus cf. belemnos and S. aff. heteromorphus show remarkable affinities to Mediterranean nannoplankton zone MNN3b. Together with the frequent occurrence of Helicosphaera ampliaperta and the absence of Triquetrorhabdulus carinatus an assignment to standard nannoplankton zone NN3 (early-middle Burdigalian) is indicated. Magnetostratigraphy revealed an inverse polarisation for the outcrop. In combination with the biostratigraphic age constraints and the present correlation of the Ottnangian to the Bur3 sea-level cycle the section belongs to polarity chron C5Dr.2r. For the first time, an absolute age between 17.95-18.056 Ma for the stratotype can be inferred.	[Grunert, Patrick; Soliman, Ali; Piller, Werner E.] Graz Univ, Inst Earth Sci, A-8010 Graz, Austria; [Coric, Stjepan] Geol Survey Austria, A-1030 Vienna, Austria; [Scholger, Robert] Univ Leoben, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria; [Harzhauser, Mathias] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1014 Vienna, Austria	University of Graz; University of Leoben	Grunert, P (通讯作者)，Graz Univ, Inst Earth Sci, Heinrichstr 26, A-8010 Graz, Austria.	patrick.grunert@uni-graz.at	Soliman, Ali/R-1583-2018	Harzhauser, Mathias/0000-0002-4471-6655; Piller, Werner E./0000-0003-2808-4720; Scholger, Robert/0000-0002-5412-3167; Soliman, Ali/0000-0001-7366-4607; Grunert, Patrick/0000-0002-3633-8674	Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	The authors would like to thank Sorin Filipsecu (University of Cluj), Ralph Hinsch (Rohol-Aufsuchungs AG, Vienna), Bettina Reichenbacher (University of Munich) and Fred Rogl (Natural History Museum Vienna) for comments and discussions. Franz Topka (Natural History Museum Vienna) is thanked for assistance with the field-work. Karl Stingl (Graz) performed paleomagnetic sampling. Peter Pohn (Wolfsegg) kindly provided access to the outcrop. This study was financially supported by the Commission for the Paleontological and Stratigraphical Research of Austria (Austrian Academy of Sciences) and benefited from the cooperation between the universities of Graz and Leoben within UZAG-framework. This paper contributes to the FWF-project 21,414-B16.	Aberer F., 1958, MITTEILUNGEN GEOLOGI, V50, P23; [Anonymous], [No title captured]; [Anonymous], CHRONOSTRATIGRAPHIE; [Anonymous], CHRONOSTRATIGRAPHIE; Association of Stratigraphic Palynologists, DAT SER ASS STRAT PA; Berger J.P., 1996, Neues Jahrbuch Geol. 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OCT	2010	44	1					1	16		10.1127/0078-0421/2010/0001	http://dx.doi.org/10.1127/0078-0421/2010/0001			16	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	704AX					2025-03-11	WOS:000286024600001
J	Lebedeva, NK				Lebedeva, N. K.			Palynofacies in Upper Cretaceous Sediments of Northern Siberia	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						palynomorphs; Upper Cretaceous; biofacies; northern Siberia	DINOFLAGELLATE CYSTS; WESTERN INTERIOR; BOUNDARY; BIOSTRATIGRAPHY; STRATIGRAPHY; DEPOSITS; SECTION; REGION; MIDDLE; BASIN	Different palynomorph groups (spores and pollen of terrestrial plants, dinoflagellate cysts, prasinophytes, acritarchs, Zygnemataceae algae, and others) have been thoroughly studied to define major patterns in their distribution depending on the impact of different environmental factors and to establish their paleoecological characteristics. The comparative analysis of palynomorph assemblages from coeval Cenomanian-Coniacian sediments of the Ust'-Yenisei area, Berezovskaya 23k, Yuzhno-Russkaya 113, Leningradskaya-1 boreholes and Santonian-Campanian sequences of the Ust'-Yenisei, Khatanga and Polar Urals regions reveals transgressive-regressive cycles, which are best evident in coastal sections and smoothed in their marine counterparts. The biofacies and compositions of palynomorphs form the regular succession from the periphery toward central parts of the West Siberian basin. The facies successions in Santonian-Campanian sections of the eastern and western parts of the basin are inconsistent with each other, which may be explained by influence of both the West Siberian and Russian seas on sedimentation in its western areas.	Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia	Russian Academy of Sciences; Trofimuk Institute of Petroleum Geology & Geophysics; Siberian Branch of the Russian Academy of Sciences	Lebedeva, NK (通讯作者)，Russian Acad Sci, Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Pr Akademika Koptyuga 3, Novosibirsk 630090, Russia.	lebedevank@ipgg.nsc.ru	Natalia, Lebedeva/T-6040-2017	Natalia, Lebedeva/0000-0002-7192-8303	Russian Foundation for Basic Research [09-05-00210]; Earth Sciences Branch of the Russian Academy of Sciences [15, 17]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Earth Sciences Branch of the Russian Academy of Sciences(Russian Academy of Sciences)	The study was supported by the Russian Foundation for Basic Research (project no. 09-05-00210) and the Earth Sciences Branch of the Russian Academy of Sciences (Programs 15 and 17).	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Geol. Correl.	OCT	2010	18	5					532	549		10.1134/S0869593810050059	http://dx.doi.org/10.1134/S0869593810050059			18	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	662QO					2025-03-11	WOS:000282826600005
J	Louwye, S; De Schepper, S				Louwye, Stephen; De Schepper, Stijn			The Miocene-Pliocene hiatus in the southern North Sea Basin (northern Belgium) revealed by dinoflagellate cysts	GEOLOGICAL MAGAZINE			English	Article						dinoflagellate cysts; palynology; Miocene; Pliocene; North Sea Basin	DIEST FORMATION; MID-PLIOCENE; STRATIGRAPHY; LEVEL; PALEOECOLOGY; PLEISTOCENE; ACRITARCHS; TAXA	A palynological analysis with marine palynomorphs (dinoflagellate cysts, acritarchs, green algae) and terrestrial palynomorphs (pollen and spores) of the Kasterlee and Poederlee formations provides new insights in the depositional history at the southern border of the North Sea basin (northern Belgium) around the Miocene-Pliocene transition. Dinoflagellate cyst stratigraphy constrains the age of the Kasterlee Formation in the Oud-Turnhout borehole between 7.5 and 5.32 Ma. The upper boundary of the formation can be correlated with sequence boundary Me2 at 5.73 Ma of Hardenbol and co-workers, which further constrains its age to the time interval 7.5-5.73 Ma. The palynomorph assemblages reflect a near-coast depositional environment. Where present, the Kasterlee Formation thus terminates the Miocene series in northern Belgium. The overall shallow nature of the latest Miocene deposits is related to a sea-level lowering caused by the onset of globally cooling conditions. For the first time, palynology is applied to estimate the age of the Poederlee Formation, suggesting it was deposited during the Mid-Pliocene warm period. Dinoflagellate cysts and sequence stratigraphy together constrain the age of the unit between 3.21 and 2.76 Ma, and possibly even between 3.21 and 3.15 Ma. The Poederlee Formation was deposited in neritic environments, which shoaled in the upper part of the unit as a consequence of the decreasing availability of accommodation space. We demonstrate that the magnitude of the hiatus between the Miocene and Pliocene series varies strongly at the southern boundary of the North Sea Basin, and lasts in the Antwerp area c. 3.2 million years and c. 2.52 million years in the Campine area.	[Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, Ghent, Belgium; [De Schepper, Stijn] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany	Ghent University; University of Bremen	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, Ghent, Belgium.	stephen.louwye@ugent.be	Louwye, Stephen/D-3856-2012; De Schepper, Stijn/A-2836-2011	Louwye, Stephen/0000-0003-4814-4313; De Schepper, Stijn/0000-0002-6934-0914	Deutsche Forschungsgemeinschaft; MARUM	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); MARUM	S. Van Cauwenberghe kindly helped with the palynological preparations. The stimulating discussions on Neogene stratigraphy with P. Laga (Geological Survey of Belgium) and with S. Geets are much appreciated. SDS appreciates funding from the Deutsche Forschungsgemeinschaft (International Graduate College 'Proxies in Earth History', EUROPROX, University of Bremen) and MARUM (G. Wefer). The samples of the Oud-Turnhout borehole were kindly made available by the Geological Survey of Belgium, and their co-operation is much appreciated. The constructive reviews by L. Edwards and an anonymous reviewer are much appreciated and improved the manuscript considerably.	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Mag.	SEP	2010	147	5					760	776		10.1017/S0016756810000191	http://dx.doi.org/10.1017/S0016756810000191			17	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	644JS		Green Published			2025-03-11	WOS:000281372700011
J	Matsuoka, K; Mizuno, A; Iwataki, M; Takano, Y; Toshifumi, Y; Yoon, YH; Lee, JB				Matsuoka, Kazumi; Mizuno, Akane; Iwataki, Mitsunori; Takano, Yoshihito; Yamatogi, Toshifumi; Yoon, Yang Ho; Lee, Joon-Baek			Seed populations of a harmful unarmored dinoflagellate <i>Cochlodinium polykrikoides</i> Margalef in the East China Sea	HARMFUL ALGAE			English	Article						Seed population; East China Sea; Harmful dinoflagellate; Cochlodinium polykrikoides; Cochlodinium fuvescens ecology	DINOPHYCEAE; GYMNODINIALES; CIRCULATION	An unarmored dinoflagellate Cochlodinium polykrikoides has formed red tides responsible for fish mass mortalities especially in coastal areas of western Japan and southern Korea almost every summer to autumn. In laboratory culture, the optimum temperature for growth of the species is ca. 27 degrees C. Since the species cannot survive in water of temperatures of less than 10 degrees C, it was considered to over-winter in some certain regions as a motile form or resting cyst, and expand its distribution after the temperature increases to a level tolerable for growth. To determine the over-wintering regions and migration pattern of C. polykrikoides, occurrences of the motile cells were surveyed in the coastal and offshore areas of western Kyushu, Japan and south coast of the Korean Peninsula from April 2006 to August 2008. Cells of C. polykrikoides were found at 14 sites during the investigated period. Motile cells occurred throughout the year in Usuka Bay, Hirado of West Japan. From offshore regions of the Goto Islands and off Shin-Nagasaki Fishing Port, motile cells of C. polykrikoides were first detected from late May, and continuously occurred until February in Nama Bay of the Kami-Goto Islands. This first appearance was before red tides of C. polykrikoides reported at coastal areas in western Kyushu. In Korea, this species was first observed in May and disappeared after October in 2007. These occurrence patterns imply that Usuka Bay in Hirado is one of the over-wintering regions in western Kyushu, and also this species is possibly transported into the northern part of the East China Sea by the Tsushima Warm Current every year. (c) 2010 Elsevier B.V. All rights reserved.	[Matsuoka, Kazumi; Iwataki, Mitsunori; Takano, Yoshihito] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Mizuno, Akane] Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan; [Yamatogi, Toshifumi] Nagasaki Prefectural Inst Fisheries, Nagasaki 8512213, Japan; [Yoon, Yang Ho] Chonnam Natl Univ, Coll Fisheries & Ocean Sci, Dundeok Dong 550479, Yeosu, South Korea; [Lee, Joon-Baek] Cheju Natl Univ, Coll Ocean Sci, Cheju 690756, South Korea	Nagasaki University; Nagasaki University; Chonnam National University; Jeju National University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp	Iwataki, Mitsunori/H-9640-2019	Iwataki, Mitsunori/0000-0002-5844-2800; Yoon, Yang Ho/0000-0001-8529-9512	A Japanese, Korean and Chinese joint study for harmful algal blooms in the East China Sea	A Japanese, Korean and Chinese joint study for harmful algal blooms in the East China Sea	We are grateful to Captain H. Yoshimura of T/V Nagasaki-Maru and crews, Captain H. Kanehara of T/V Kakuyo-Maru and crews in Nagasaki Univrsity, Ms R. Kida, and Dr. N. Takagi of Nagasaki Prefectural Institute of Fisheries for their kind support to collect plankton samples. This work was supported by Special Coordination Funds for Promotion Science and Technology "A Japanese, Korean and Chinese joint study for harmful algal blooms in the East China Sea".[TS]	FUJII M, 1961, SUIRO YOHO, V67, P58; ICHIKAWA H, 2007, MONTHLY KAIYO, V29, P521; Isobe A, 2008, J OCEANOGR, V64, P569, DOI 10.1007/s10872-008-0048-7; Iwataki M, 2008, HARMFUL ALGAE, V7, P271, DOI 10.1016/j.hal.2007.12.003; Iwataki M, 2007, PHYCOL RES, V55, P231, DOI 10.1111/j.1440-1835.2007.00466.x; *KAG PERF FISH EXP, 1982, COCHL SP, V78, P50; *KAG PREF FISH EXP, 1984, RED TID KAG BAY; *KAG PREF FISH EXP, 1995, RED TID CAUS ORG KAG; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kim Chang-Hoon, 2009, Bulletin of Plankton Society of Japan, V56, P31; Kim DI, 2004, J PLANKTON RES, V26, P61, DOI 10.1093/plankt/fbh001; KIM DI, 2005, MONTHLY KAIYO, V37, P40; Kim HG, 2006, ECOL STU AN, V189, P327, DOI 10.1007/978-3-540-32210-8_25; Kim Hak Gyoon, 1999, Bulletin of National Fisheries Research and Development Institute, V57, P119; Kondo M., 1985, Bull Seikai Region Fish Res Lab, V62, P19; Lie HJ, 2002, FISH OCEANOGR, V11, P318, DOI 10.1046/j.1365-2419.2002.00215.x; Matsuoka K, 2008, HARMFUL ALGAE, V7, P261, DOI 10.1016/j.hal.2007.12.002; Matsuoka Kazumi, 2004, Bulletin of Plankton Society of Japan, V51, P38; Miyahara K., 2004, B PLANKTON SOC JPN, V52, P11; Nagai Satoshi, 2009, Bulletin of Plankton Society of Japan, V56, P47; NAGAYI S, 2009, MOL ECOL, DOI DOI 10.111/J.1365-294X.2009.04193.X; NISHIMURA S, 1981, EARTHS OCEAN LIFE CH; NISHITANI G, 2008, DNA TAKEI, V16, P140; SAKAMOTO S, 2008, 5 INT S TARG HAB SPE; YAMATOGI T, JPN J PHYCOL; Yamatogi Toshifumi, 2005, Japanese Journal of Phycology, V53, P229; Yamatogi Toshifumi, 2005, Bulletin of Plankton Society of Japan, V52, P4; Yuki K., 1989, P451	28	32	35	1	11	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	SEP	2010	9	6					548	556		10.1016/j.hal.2010.04.003	http://dx.doi.org/10.1016/j.hal.2010.04.003			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	652JC					2025-03-11	WOS:000281999300003
J	Limoges, A; Kielt, JF; Radi, T; Ruíz-Fernandez, AC; de Vernal, A				Limoges, Audrey; Kielt, Jean-Francois; Radi, Taoufik; Carolina Ruiz-Fernandez, Ana; de Vernal, Anne			Dinoflagellate cyst distribution in surface sediments along the south-western Mexican coast (14.76° N to 24.75°N)	MARINE MICROPALEONTOLOGY			English	Article						Mexico; Cysts; Environmental parameters; Upwelling; Primary productivity	GULF-OF-CALIFORNIA; ORGANIC-WALLED MICROFOSSILS; OCEANIC PRIMARY PRODUCTION; EASTERN TROPICAL PACIFIC; NORTHERN NORTH-ATLANTIC; MARINE-SEDIMENTS; GYMNODINIUM-CATENATUM; RED TIDE; UPWELLING SYSTEM; HIGH-LATITUDES	In this study, we explore the relationship between the modern assemblages of organic-walled dinoflagellate cysts and sea-surface conditions (temperature, salinity, primary productivity) and water depth and distance to the coast. Statistical treatments were performed on 95 surface sediment samples from sites located along the south-western Mexican coast (14.76 degrees N to 24.75 degrees N). Redundancy analysis (RDA) illustrates that the principal parameters correlated with the regional cyst distribution are the distance to the coast and the productivity in the upper water column, which is closely related to upwelling intensity. Empirical observations coupled with RDA provide insight into the spatial coverage of some cyst taxa produced by dinoflagellate species potentially responsible for harmful algal blooms along the coast They also allow the recognition of four zones of assemblages, which are linked to the upwelling intensity and the productivity and characterize La Paz Bay, the south-western Mexican margin (from 15.95 degrees N to 23.11 degrees N), the northern part of the Gulf of Tehuantepec and the southern part of the Gulf of Tehuantepec. (C) 2010 Elsevier B.V. All rights reserved.	[Limoges, Audrey; Kielt, Jean-Francois; Radi, Taoufik; de Vernal, Anne] GEOTOP UQAM, Succ Ctr ville, Montreal, PQ H3C 3P8, Canada; [Carolina Ruiz-Fernandez, Ana] Univ Nacl Autonoma Mexico, Mazatlan 82000, Sinaloa, Mexico	University of Quebec; University of Quebec Montreal; Universidad Nacional Autonoma de Mexico	Limoges, A (通讯作者)，GEOTOP UQAM, Succ Ctr ville, CP 8888, Montreal, PQ H3C 3P8, Canada.	limoges.audrey@courrier.uqam.ca	Ruiz-Fernández, Ana Carolina/ABG-6985-2020; de Vernal, Anne/D-5602-2013	Limoges, Audrey/0000-0002-4587-3417; RUIZ-FERNANDEZ, ANA CAROLINA/0000-0002-2515-1249; de Vernal, Anne/0000-0001-5656-724X	Natural Science and Engineering Council (NSERC) of Canada; Government of Quebec within the framework of the Groupe de travail Quebec-Mexique (GTQM)	Natural Science and Engineering Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Government of Quebec within the framework of the Groupe de travail Quebec-Mexique (GTQM)	This study was possible through the financial support of The Natural Science and Engineering Council (NSERC) of Canada and the government of Quebec within the framework of the Groupe de travail Quebec-Mexique (GTQM). Thanks are due to the crew of the El PUMA which helped to collect sediment samples during the oceanographic campaign TEHUA V. We want to thank Maryse Henry for providing the environmental data from moDIS and CZCS programs. We appreciated the constructive review comments of Javier Helenes and an anonymous reviewer who helped to improve the final version of the manuscript.	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Micropaleontol.	SEP	2010	76	3-4					104	123		10.1016/j.marmicro.2010.06.003	http://dx.doi.org/10.1016/j.marmicro.2010.06.003			20	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	658DE					2025-03-11	WOS:000282469400005
J	Sliwinska, KK; Clausen, OR; Heilmann-Clausen, C				Sliwinska, K. K.; Clausen, O. R.; Heilmann-Clausen, C.			A mid-Oligocene cooling (0i-2b) reflected in the dinoflagellate record and in depositional sequence architecture. An integrated study from the eastern North Sea Basin	MARINE AND PETROLEUM GEOLOGY			English	Article						3D seismics; Dinoflagellates; Oi-2b cooling event; Oligocene; Rupelian/Chattian boundary; Sequence stratigraphy	CYST BIOSTRATIGRAPHY; STRATIGRAPHY; CALIBRATION; MORPHOLOGY; EOCENE	Integrated micropaleontological (dinoflagellate and foraminifera) and 3D seismic studies of Oligocene surfaces were carried out in the eastern North Sea in order to investigate the influence of the climate on the evolution of depositional geometries and surface morphologies. Age-indicative dinoflagellates allowed a correlation of the succession with the global time scale and thereby with published oxygen isotope curves. Temperature-indicative dinoflagellate taxa furthermore allowed to infer paleoclimatic changes during the mid-Oligocene. One of the surfaces studied on 3D seismic datasets shows features such as low-angle landward directed onlaps, incised valleys and pockmarks, indicating a prominent, relative sea-level fall. The cold-water dinoflagellate Svalbardella was recorded immediately above this surface. The coincidence of a cold-water indicator with this distinctive sequence boundary shows that deposition of this sequence was controlled by climatically induced sea-level changes, and that 3D seismic analysis combined with high-resolution dinoflagellate analysis substantially improves the understanding of the depositional history and processes within the North Sea Basin. The Svalbardella event represents the Oi-2b glaciation and coincides with the onshore NW European Rupelian/Chattian boundary. (C) 2010 Elsevier Ltd. All rights reserved.	[Sliwinska, K. K.; Clausen, O. R.; Heilmann-Clausen, C.] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark	Aarhus University	Sliwinska, KK (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	kasia.sliwinska@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; Clausen, Ole/A-5290-2012; Sliwinska, Kasia K./G-9097-2018	Clausen, Ole Rono/0000-0002-6825-9065; Sliwinska, Kasia K./0000-0001-5488-8832	Aarhus University (Denmark); Fur Museum (Denmark)	Aarhus University (Denmark); Fur Museum (Denmark)	Soren Bo Andersen (Aarhus University, Denmark) is thanked for here leads to two major conclusions preparing the plate with dinoflagellate photographs. Bartosz Goledowski (Aarhus University, Denmark) is thanked for preparing the map of the study area. Katarzyna K. Sliwinska acknowledges financial support for her PhD project from Aarhus University (Denmark) and Fur Museum (Denmark). Reviewers are thanked for their constructive suggestions and comments that had improved the manuscript.	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Pet. Geol.	AUG	2010	27	7					1424	1430		10.1016/j.marpetgeo.2010.03.008	http://dx.doi.org/10.1016/j.marpetgeo.2010.03.008			7	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	638ZH					2025-03-11	WOS:000280940000009
J	Shin, HH; Mizushima, K; Oh, SJ; Park, JS; Noh, IH; Iwataki, M; Matsuoka, K; Yoon, YH				Shin, Hyeon Ho; Mizushima, Koichiro; Oh, Seok Jin; Park, Jong Sick; Noh, Il Hyeon; Iwataki, Mitsunori; Matsuoka, Kazumi; Yoon, Yang Ho			Reconstruction of historical nutrient levels in Korean and Japanese coastal areas based on dinoflagellate cyst assemblages	MARINE POLLUTION BULLETIN			English	Article						Dinoflagellate cyst; Heterotrophic cyst; Lingulodinium machaerophorum; Nutrient level; Gamak Bay; Ariake Bay	SURFACE SEDIMENTS; TOKYO-BAY; YOKOHAMA-PORT; LATE HOLOCENE; EUTROPHICATION; INDICATORS; MASSACHUSETTS; DISTRIBUTIONS; TEMPERATURE; POLLUTION	Dinoflagellate cysts acquired from sediment cores were analyzed in order to reconstruct historical nutrient levels in Gamak Bay, Korea and Ariake Bay, Japan. Dinoflagellate cyst assemblages in Gamak Bay were characterized by high proportions of heterotrophic cysts such as Brigantedinium spp., Protoperidinium americanum and Polykrikos cysts, which suggested that nutrients levels may have already been high before 1970s, and then increased further to the hypertrophic conditions of the 1990s. In contrast, dinoflagellate cyst assemblages in Ariake Bay were characterized by high relative abundances of Lingulodinium machaerophorum and Spiniferites spp., which suggested that nutrient levels in Ariake Bay had increased gradually since the mid 1960s, and may have been significantly enhanced by the mid 1980s. Dinoflagellate cyst assemblages reflecting environmental changes in the two bays are contrasting, perhaps due to different nutrient enrichment mechanisms. This suggests that the indicators of nutrient levels encoded in dinoflagellate cyst assemblages may exhibit site-specific information. (C) 2010 Elsevier Ltd. All rights reserved.	[Shin, Hyeon Ho; Park, Jong Sick; Noh, Il Hyeon; Yoon, Yang Ho] Chonnam Natl Univ, Fac Marine Technol, Yeosu 550749, South Korea; [Shin, Hyeon Ho] KORDI, S Sea Inst, Coastal Ecol Proc Res Div, Geoje 656830, South Korea; [Iwataki, Mitsunori; Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Mizushima, Koichiro] Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; [Oh, Seok Jin] Pukyong Natl Univ, Korea Interuniv Inst Ocean Sci, Pusan 608737, South Korea	Chonnam National University; Korea Institute of Ocean Science & Technology (KIOST); Nagasaki University; Japan Fisheries Research & Education Agency (FRA); Pukyong National University	Yoon, YH (通讯作者)，Chonnam Natl Univ, Fac Marine Technol, Mipyeongro 386, Yeosu 550749, South Korea.	yoonyh@chonnam.ac.kr	; Iwataki, Mitsunori/H-9640-2019	Yoon, Yang Ho/0000-0001-8529-9512; Oh, Seok Jin/0000-0002-2572-5150; Iwataki, Mitsunori/0000-0002-5844-2800; Shin, Hyeon Ho/0000-0002-9711-6717	Grants-in-Aid for Scientific Research [22580202] Funding Source: KAKEN	Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))		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, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; Ghaffar A, 2008, ELECT J ENV AGR FOOD, V7, P3065; Hallett R.I, 1996, 9 INT PAL C HOUST TX, P59; Holzwarth U, 2007, MAR MICROPALEONTOL, V64, P91, DOI 10.1016/j.marmicro.2007.04.001; Howarth RW, 2002, ESTUARIES, V25, P656, DOI 10.1007/BF02804898; Kim H.-G., 1990, Bulletin of the Korean Fisheries Society, V23, P468; KIM HJ, 2005, J KOREAN SOC OCEANOG, V10, P196; Kim Jeong-Bae, 2006, 한국해양환경•에너지학회지, V9, P216; Kim YS, 2007, CHEMOSPHERE, V67, P456, DOI 10.1016/j.chemosphere.2006.09.063; Koo Bon Joo, 2004, Ocean and Polar Research, V26, P11; Lee G.-H., 1992, B KOREAN FISH TECHNO, V28, P117; LEE J-B, 1991, Journal of the Korean Society of Oceanography, V26, P304; LEE K-H, 1990, Journal of the Korean Fisheries Society, V23, P25; Lee M.H., 1999, Algae, V14, P255; LEE YG, 2006, NATURAL ENV IND GAMA, P247; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Lopes CB, 2007, ESTUAR COAST SHELF S, V71, P480, DOI 10.1016/j.ecss.2006.09.015; 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; Matsuoka K, 2003, J PLANKTON RES, V25, P1461, DOI 10.1093/plankt/fbg111; 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, 2004, B COAST OCEANOG, V42, P55; Mertens KN, 2009, MAR MICROPALEONTOL, V70, P54, DOI 10.1016/j.marmicro.2008.10.004; *NFRDI, 1998, RED TID KOR, P292; Park Gi-Hong, 2004, Journal of the Korean Fisheries Society, V37, P202; Park Jong Sick, 2003, Journal of the Korean Fisheries Society, V36, P151; Pospelova V, 2005, MAR ECOL PROG SER, V292, P23, DOI 10.3354/meps292023; Pospelova V, 2002, SCI TOTAL ENVIRON, V298, P81, DOI 10.1016/S0048-9697(02)00195-X; Pospelova V, 2008, MAR MICROPALEONTOL, V68, P21, DOI 10.1016/j.marmicro.2008.01.008; Rochon A, 2004, REV PALAEOBOT PALYNO, V128, P1, DOI 10.1016/S0034-6667(03)00109-X; Saetre MML, 1997, MAR ENVIRON RES, V44, P167, DOI 10.1016/S0141-1136(96)00109-2; Sangiorgi F, 2004, ESTUAR COAST SHELF S, V60, P69, DOI 10.1016/j.ecss.2003.12.001; SHIM JH, 1980, J OCEANOLOGICAL SOC, V15, P89; SHIMATSU Y, 2003, NIPPON SUISAN GAKK, V69, P439; Shin Hyeon Ho, 2007, Ocean Science Journal, V42, P31; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; SMAYDA TJ, 1990, TOXIC MARINE PHYTOPLANKTON, P29; Taylor FJR, 1987, BOT MONOGR, V21, P785; Teague WJ, 2003, CONT SHELF RES, V23, P63, DOI 10.1016/S0278-4343(02)00150-4; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; Tsutsumi Hiroaki, 2006, Plankton & Benthos Research, V1, P3; Vilanova I, 2008, REV PALAEOBOT PALYNO, V152, P11, DOI 10.1016/j.revpalbo.2008.03.006; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; Yokouchi K, 2005, UMI SORA, V80, P141; 노일현, 2006, 한국해양환경•에너지학회지, V9, P1; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6; Zonneveld KAF, 2007, MAR GEOL, V237, P109, DOI 10.1016/j.margeo.2006.10.023	52	32	37	0	9	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	2010	60	8					1243	1258		10.1016/j.marpolbul.2010.03.019	http://dx.doi.org/10.1016/j.marpolbul.2010.03.019			16	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	645PC	20382400				2025-03-11	WOS:000281474000024
J	Barrón, E; Ureta, S; Goy, A; Lassaletta, L				Barron, Eduardo; Ureta, Soledad; Goy, Antonio; Lassaletta, Luis			Palynology of the Toarcian-Aalenian Global Boundary Stratotype Section and Point (GSSP) at Fuentelsaz (Lower-Middle Jurassic, Iberian Range, Spain)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Toarcian-Aalenian stratotype; palynology; biostratigraphy; environmental conditions; palaeoecology	LUSITANIAN BASIN; NORTHERN SPAIN; GYMNOSPERMS; EVENTS; FRANCE; CYCLES; EXINE; FIELD	The Fuentelsaz Section is located in the Castilian Branch of the Iberian Range (Guadalajara, Spain). Its exceptional Lower-Middle Jurassic transition outcrops led to its designation as the Global Boundary Stratotype Section and Point for the base of the Aalenian. The sediments of the Toarcian-Aalenian transition at Fuentelsaz are composed of marls with interbedded limestones in rhythmic alternation. Marls are dominant in the Toarcian and the Opalinum Zone up to the middle part of the Comptum Subzone. In the remaining Comptum Subzone, marly materials are scarce and limestones predominate. Sedimentation at Fuentelsaz took place over an extensive marine epeiric carbonate platform that was well connected with the open sea. In the Fuentelsaz Section, a total of 43 palynomorph taxa were recorded: 23 spore taxa, 13 pollen taxa, 4 acritarchs, 2 prasinophytes and 1 dinoflagellate cyst. The studied sediment samples were always dominated by terrestrial allochthonous miospores. In general, miospore assemblages are biased due to the transport of pollen from land or islands to the continental platform. Spheripollenites, Classopollis or indeed both pollens numerically dominate the assemblages. Other miospores appear in low numbers. Aquatic palynomorphs are also scarce; Micrhystridium lymensis is the most common. Five palynological assemblages (PA) were distinguished: PA1, PA2 and PA3 are Toarcian in age, PA4 is located at the boundary between the Toarcian and the Aalenian and PAS. This latter palynological assemblage which is lower Aalenian in age shows a strong reduction in palynomorph diversity and preservation in the Comptum Subzone. Palaeoecological analysis of the palynomorphs indicated the presence of calm, oligotrophic sea water. The palaeofloral communities of gymnosperms and vascular cryptogams which grew in subtropical arid conditions were poorly diversified. (C) 2010 Elsevier B.V. All rights reserved.	[Barron, Eduardo] IGME, Madrid 28003, Spain; [Ureta, Soledad; Goy, Antonio] Fac Ciencias Geol, Dept & UEI Paleontol UCM CSIC, Madrid 28040, Spain; [Lassaletta, Luis] Univ Complutense Madrid, Fac Ciencias Biol, Dept Interuniv Ecol, E-28040 Madrid, Spain; [Lassaletta, Luis] Univ Alcala, Dept Ecol, Alcala De Henares 28871, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); Complutense University of Madrid; Universidad de Alcala	Barrón, E (通讯作者)，IGME, Rios Rosas 23, Madrid 28003, Spain.	e.barron@igme.es	Barrón, Eduardo/L-4726-2014; Lassaletta, Luis/D-3894-2009	Goy, Antonio/0000-0002-2331-9765; Lassaletta, Luis/0000-0001-9428-2149; Barron, Eduardo/0000-0003-4979-1117	Spanish Ministry of Science and Innovation [CGL2005-0474/BTE, CGL2008-03112/BTE]; UCM-CCMM [910431]; Triassic/Jurassic times [467/506]	Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government); UCM-CCMM; Triassic/Jurassic times	This research work was financed by projects CGL2005-0474/BTE and CGL2008-03112/BTE from the Spanish Ministry of Science and Innovation, and 910431 from the UCM-CCMM. We wish to thank Peggy Tan (Journal Manager) as well as the anonymous referees who provided useful criticisms and valuable suggestions. We also thank Javier Castrillo and Daniel Peyrot for their help and kindness. This paper is a contribution to the International Geological Correlation Program Project 467/506 (Triassic/Jurassic times). Adrian Burton and Otto Kalin are thanked for their assistance with the English manuscript.	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Palynology	AUG	2010	162	1					11	28		10.1016/j.revpalbo.2010.04.003	http://dx.doi.org/10.1016/j.revpalbo.2010.04.003			18	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	642CN		Green Accepted			2025-03-11	WOS:000281181100002
J	Soulet, G; Delaygue, G; Vallet-Coulomb, C; Böttcher, ME; Sonzogni, C; Lericolais, G; Bard, E				Soulet, G.; Delaygue, G.; Vallet-Coulomb, C.; Boettcher, M. E.; Sonzogni, C.; Lericolais, G.; Bard, E.			Glacial hydrologic conditions in the Black Sea reconstructed using geochemical pore water profiles	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Black Sea; interstitial water; salinity; water isotopes; advection/diffusion modelling; deglaciation	ANAEROBIC METHANE OXIDATION; OXYGEN ISOTOPIC COMPOSITION; LATE QUATERNARY CORES; DINOFLAGELLATE CYSTS; MARMARA SEA; INTERGLACIAL TRANSITION; MEDITERRANEAN SEA; LAST; SHELF; CONSTRAINTS	Chloride and delta(18)O compositions of interstitial water extracted from a long sediment core retrieved from the NW coast of the Black Sea allowed us to constrain the main hydrologic changes of the Back Sea during the Late Pleistocene and Holocene. Prior to its reconnection with the Mediterranean Sea (through the Marmara Sea) at approximately 9000 calendar yr before present (9 ka cal BP), the Black Sea has evolved as a fresh to brackish water lake. At the time of reconnection, hydrologic changes were drastic. Bottom water salinities changed from a few psu (practical salinity unit) to similar to 22 psu. Since solutes in the interstitial water column within sediments are advected and diffused the measured concentrations do not reflect those of past bottom waters. In order to reconstruct these former concentrations, we used an advection/diffusion model. Different scenarios of bottom water chloride and delta(18)O variations were accounted for in this model in order to simulate "present day" vertical profiles for concentrations of interstitial water in order to compare them to measured ones. The comparison suggests that the glacial Black Sea was a homogeneous freshwater lake (with a delta(18)O of similar to - 10 parts per thousand M. and a salinity of similar to 1 psu). Modem hydrologic conditions would only have been reached at similar to 2 ka cal BP, concomitant with the onset of coccolith-rich thin layers that characterize modern basin sediments. Such delayed salinization (over similar to 7000 yr) in the basin may have been due to higher precipitation during the early Holocene. We also simulated the impact of a catastrophic reconnection and a smoother reconnection. Both salinity scenarios lead to undistinguishable modelled "present day" profiles, indicating that the precise impact of the last reconnection was lost due to the advection/diffusion processes. (C) 2010 Elsevier B.V. All rights reserved.	[Soulet, G.; Delaygue, G.; Vallet-Coulomb, C.; Sonzogni, C.; Bard, E.] Univ Paul Cezanne Aix Marseille III, CNRS, CEREGE, UMR6635,Coll France, F-13545 Aix En Provence 04, France; [Boettcher, M. E.] Max Planck Inst Marine Microbiol, D-28359 Bremen, Germany; [Lericolais, G.] IFREMER, Ctr Brest, F-29280 Plouzane, France	Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Aix-Marseille Universite; Max Planck Society; Ifremer	Soulet, G (通讯作者)，Univ Paul Cezanne Aix Marseille III, CNRS, CEREGE, UMR6635,Coll France, BP 80, F-13545 Aix En Provence 04, France.	soulet@cerege.fr	Böttcher, Michael/A-6746-2013; Sonzogni, Corinne/AAG-5816-2019; Bard, Edouard/G-7717-2014; Lericolais, Gilles/AAX-1662-2021; Soulet, Guillaume/K-1961-2015	Soulet, Guillaume/0000-0003-2941-6440; Vallet-Coulomb, Christine/0000-0001-5898-1516; Lericolais, Gilles/0000-0002-8159-9187; Bottcher, Michael Ernst/0000-0002-8877-0303	European Commission [EVK3-CT-2002-00090]; Max Plank Society; CNRS; IFREMER; College de France; Gary Corner Foundation for Science and Education; European Community; CNRS-INSU	European Commission(European Union (EU)European Commission Joint Research Centre); Max Plank Society(Max Planck Society); CNRS(Centre National de la Recherche Scientifique (CNRS)); IFREMER; College de France; Gary Corner Foundation for Science and Education; European Community; CNRS-INSU(Centre National de la Recherche Scientifique (CNRS))	Our paper is a contribution to the ASSEMBLAGE project funded by the European Commission (EVK3-CT-2002-00090). We thank the crew of the research vessel Marion Dufresne for assistance during the ASSEMBLAGE 1 cruise. We also thank G. Leduc, Y. Ternois, and F. Ebersbach for on board pore water sampling. We are also grateful to N. cagatay for lending the sediment squeezer. We thank P. Henry for useful discussions and the three anonymous reviewers for their constructive comments. M.E. Bottcher wishes to thank A. Schipper and the Max Plank Society for technical and financial support, respectively. We are grateful to CNRS, IFREMER and College de France for providing salarial support to G. Soulet. Paleoclimate work at CEREGE is supported by grants from the Gary Corner Foundation for Science and Education, the European Community (Project Past4Future), the CNRS-INSU (BLACKMED project) and the College de France.	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Sci. Lett.	JUL 15	2010	296	1-2					57	66		10.1016/j.epsl.2010.04.045	http://dx.doi.org/10.1016/j.epsl.2010.04.045			10	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	625OW		Green Published			2025-03-11	WOS:000279905800006
J	Sánchez, A; Pavlishina, P; Godoy, E; Hervé, F; Fanning, CM				Sanchez, Alejandro; Pavlishina, Polina; Godoy, Estanislao; Herve, Francisco; Mark Fanning, C.			On the presence of Upper Paleocene rocks in the foreland succession at Cabo Nariz, Tierra del Fuego, Chile: geology and new palynological and U-Pb data	ANDEAN GEOLOGY			English	Article						Dinoflagellate cysts; K-T; Stratigraphy; U-Pb detrital zircon ages; Tierra del Fuego; Chile	ANDES; STRATIGRAPHY; BASIN	On the west coast of Tierra del Fuego, south of Cabo Nariz, in Chile, Upper Cretaceous to Paleocene sedimentary successions of the Magallanes foreland basin crop out. The presence of dinoflagellate cysts, as well as radiometric U-Pb SHRIMP dating of detrital zircons, indicate that this succession ranges from the Campanian to Thanetian (Late Paleocene) in age. The base of the exposed sedimentary succession comprises siltstones of external platform facies (Cerro Cuchilla Formation), which are thrust over the Cabo Nariz Beds. The latter formation is divided into two members: a lower siltstone-dominated turbidite facies member and an upper member of sandstone-dominated turbidites, with sandstone and conglomerate channel facies. The presence of dinocysts in the Cerro Cuchilla Formation suggests a late Campanian to early Danian age. The fossil content in the Cabo Nariz Beds indicate a Selandian (Middle Paleocene) depositional age in accordance with the detrital zircon ages which provide a maximum possible Campanian age (76.5 +/- 0.7 Ma), and very close to the Thanetian (Late Paleocene) (57.6 +/- 1 Ma) depositional ages for the lower and upper member, respectively. The sedimentary succession of Cabo Nariz Beds, is interpreted as a north-northwest prograding submarine fan of middle to Late Paleocene age. It is considered to represent the deposition of detritus derived from an uplifting orogen located to the south. The detrital zircon age spectra suggest that there was a period of low intensity of magmatic activity in the source area around the K-T boundary.	[Sanchez, Alejandro; Herve, Francisco] Univ Chile, Dept Geol, Santiago, Chile; [Pavlishina, Polina] Sofia Univ St Kl Ohridski, Dept Geol & Palaeontol, Sofia 1504, Bulgaria; [Godoy, Estanislao] Serv Nacl Geol & Mineria, Santiago, Chile; [Mark Fanning, C.] Australian Natl Univ, Res Sch Earth Sci, Canberra, ACT 0200, Australia	Universidad de Chile; University of Sofia; Australian National University	Sánchez, A (通讯作者)，Univ Chile, Dept Geol, Casilla 13518,Correo 21, Santiago, Chile.	alsanche@cec.uchile.cl; polina@gea.uni-sofia.bg; egodyster@gmail.com; fherve@cec.uchile.cl; mark.fanning@anu.edu.au	Fanning, C./I-6449-2016; Sánchez, Lorenzo/AAG-8049-2021; Herve, Francisco/HDO-6628-2022; Pavlishina, Polina/AAL-5710-2021	Pavlishina, Polina/0000-0002-1172-9142	FONDECYT [1010412, 1050431]	FONDECYT(Comision Nacional de Investigacion Cientifica y Tecnologica (CONICYT)CONICYT FONDECYT)	We thank L. Rojas from Empresa Nacional del Petroleo (ENAP) for access to unpublished ENAP reports and A. Carpinelli (ENAP) for logistic support. M. Fuentealba assistance in the field, as well as geologic discussions, and friendship was very important during fieldwork. We also thank Mr. S. Maldonado, the Ea. Miguelito owner, for his support in the field in critical moments. Comments by S. Palma (Universidad de Concepcion), C. Mpodozis (Sipetrol, presently at Antofagasta Minerals) and specially J. Le Roux (Universidad de Chile) were useful to improve the manuscript. The project was financed by FONDECYT grants 1010412 and 1050431.	ALVAREZMARRON J, 1993, AAPG BULL, V77, P1904; [Anonymous], 1996, Palynology: principles and applications; Biddle K., 1986, Assoc. 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J	Louwye, S; Marquet, R; Bosselaers, M; Lambert, O				Louwye, Stephen; Marquet, Robert; Bosselaers, Mark; Lambert, Olivier			STRATIGRAPHY OF AN EARLY-MIDDLE MIOCENE SEQUENCE NEAR ANTWERP IN NORTHERN BELGIUM (SOUTHERN NORTH SEA BASIN)	GEOLOGICA BELGICA			English	Article						Antwerpen Sands; Mollusca; Odontoceti; Mysticeti; Pinnipedia; dinoflagellate cysts	ODONTOCETI; CETACEA; BIOSTRATIGRAPHY; SYSTEMATICS; MAMMALIA; WHALES; FOSSIL	The lithostratigraphy and biostratigraphy of a temporary outcrop in the Antwerp area is described The deposits can be attributed to the Kiel Sands and the Antwerpen Sands members, both belonging to the Lower and Middle Miocene Berchem Formation Invertebrate and vertebrate macrofossils are abundantly present The molluscan fauna compares well to former findings in the Antwerpen Sands Member It can be concluded that the studied sequence is continuously present in the Antwerp area, and thickens in a northward direction The study of the marine mammal fauna shows that curhinodelphinids are the most common fossil odontocete (toothed-bearing cetaceans) in the Antwerpen Sands Member, associated here with kentriodontine, physeteroid, squalodontid mysticete (baleen whales) and pinniped (seals) fragmentary remains Both the molluscan fauna and the organic-walled palynomorphs indicate for the Antwerpen Sands Member deposition in a neritic, energetic environment which shallowed upwards The dinoflagellate cysts indicate that the Antwerpen Sande Member was deposited during late Burdigalian to Langhian times	[Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Marquet, Robert] Royal Belgian Inst Nat Sci, Dept Palaeontol, B-1000 Brussels, Belgium; [Lambert, Olivier] Inst Royal Sci Nat Belgique, Dept Paleontol, B-1000 Brussels, Belgium	Ghent University; Royal Belgian Institute of Natural Sciences	Louwye, S (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.		Lambert, Olivier/AEN-2469-2022; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Lambert, Olivier/0000-0003-0740-5791	Belgian Federal Science Policy Office [MO/36/016]	Belgian Federal Science Policy Office(Belgian Federal Science Policy Office)	The assistance of S Vancauwenberghe during the palynological maceration is much appreciated J Herman (Belgian Geologica Survey, RBINS) kindly informed us about the Posthofbrug outcrop The assistance of P De Schutter and L Dufraign in the field is much appreciated The work of O L at the IRSNB was financially supported by the Research Project MO/36/016 of the Belgian Federal Science Policy Office The constructive remarks by the reviewers Stun de Schepper and Dirk Munsterman considerably improved the manuscript	Abel O., 1905, Memoires du Musee royal d'histoire naturelle de Belgique, V3, P1; Abel O., 1901, M M MUS R HIST NAT B, V1, P1; Abel O., 1902, MEM MUS R HIST NAT B, V2, P99, DOI 10.5962/bhl.title.16053; [Anonymous], 1869, MEMOIRES LACADEMIE R; Brinkhuis H, 1996, GEOL MIJNBOUW, V75, P193; BROCCHI G., 1814, Conchiologia fossile subapennina, con osservazioni geologiche sugli Apennini e sul suolo adiacente, V2; Chevalier J. 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J	El Beialy, SY; Head, MJ; El Atfy, HS				El Beialy, Salah Y.; Head, Martin J.; El Atfy, Haytham S.			PALYNOLOGY OF THE MID-CRETACEOUS MALHA AND GALALA FORMATIONS, GEBEL EL MINSHERA, NORTH SINAI, EGYPT	PALAIOS			English	Article							ELATER-BEARING POLLEN; WESTERN-DESERT; ORGANIC FACIES; PALYNOSTRATIGRAPHY; PALYNOFACIES; PALYNOMORPHS; WELL; SEDIMENTS; BASIN	Palynological investigations of the mid-Cretaceous, delta-influenced Malha Formation and superjacent transgressive Galala Formation exposed at Gebel El Minshera, north Sinai, Egypt, have yielded a sparse but biostratigraphically useful record of spores, pollen, and rare dinoflagellate cysts. A representative of the pollen genus Tricolporites, recovered 18 m above the base of the Malha Formation, is post-Aptian in age. An interval comprising the upper Malha Formation and lower Galala Formation is dated as middle Albian/middle Cenomanian based on the occurrence of Elaterosporites klaszii at the base and Afropollis jardinus at the top. A palynoflora from the upper Malha Formation, which includes ephedroids as well as Elaterosporites, has affinities with the Albian-Cenomanian Elaterates Province. The presence of palynomorphs associated with active fluvio-deltaic settings supports a proximal deltaic environment for the deposition of the Malha Formation, with the superjacent Galala Formation representing a subsequent marine flooding of the delta. A distinctive monospecific assemblage of the dinoflagellate cyst Subtilisphaera senegalensis in the upper part (Cenomanian) of the Galala Formation reflects an ecologically stressed, marginal-marine environment. This assemblage constitutes the first record of the mid-Cretaceous Subtilisphaera ecozone in Egypt and indeed east of Morocco, and in deposits as young as Cenomanian. The Malha and lowermost Galala Formations are characterized by type III-VI kerogen, which is gas prone but having little potential to produce hydrocarbons. Spore-pollen color indicates thermal maturity at the transitional to over-mature level, which is anomalously high when compared with equivalent deposits in the region.	[El Beialy, Salah Y.; El Atfy, Haytham S.] Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	Egyptian Knowledge Bank (EKB); Mansoura University; Brock University	El Beialy, SY (通讯作者)，Mansoura Univ, Fac Sci, Dept Geol, Mansoura 35516, Egypt.	syelbeialy@mans.edu.eg	Beialy, Salah/AAD-7329-2020; Atfy, Haytham/AAT-2276-2021	El Atfy, Haytham/0000-0003-1618-7220	Arab Fund Fellowships Program, Kuwait; Natural Sciences and Engineering Research Council of Canada	Arab Fund Fellowships Program, Kuwait(Arab Fund for Economic & Social Development); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	The first author is indebted to the Arab Fund Fellowships Program, Kuwait, for financial support through a Distinguished Scholar Award that allowed a one-year research stay at Brock University from September 2006. This study would not have been possible without such support and generosity. M.J.H. acknowledges support from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. We are grateful to David T. Pocknall, an anonymous reviewer, and the Associate Editor for their careful and constructive comments on the manuscript.	Abd-Elshafy E, 2010, CRETACEOUS RES, V31, P291, DOI 10.1016/j.cretres.2009.11.003; Abdallah AM, 1965, 25 MIN IND GEOL SURV; ABDALLAH AM, 1965, 27 MIN IND GEOL SURV; AbdelKireem MR, 1996, J AFR EARTH SCI, V22, P93, DOI 10.1016/0899-5362(95)00125-5; Abdou H.F., 1966, B FS, V7, P335; Aboul Ela N. 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J	Penaud, A; Eynaud, F; Turon, JL; Blamart, D; Rossignol, L; Marret, F; Lopez-Martinez, C; Grimalt, JO; Malaizé, B; Charlier, K				Penaud, A.; Eynaud, F.; Turon, J. L.; Blamart, D.; Rossignol, L.; Marret, F.; Lopez-Martinez, C.; Grimalt, J. O.; Malaize, B.; Charlier, K.			Contrasting paleoceanographic conditions off Morocco during Heinrich events (1 and 2) and the Last Glacial Maximum	QUATERNARY SCIENCE REVIEWS			English	Article							SEA-SURFACE CONDITIONS; WALLED DINOFLAGELLATE CYST; NORTHERN NORTH-ATLANTIC; RECENT MARINE-SEDIMENTS; HIGH-RESOLUTION RECORD; PLANKTONIC-FORAMINIFERA; BENTHIC FORAMINIFERA; NW-AFRICA; CLIMATIC VARIABILITY; CANARY-ISLANDS	Past hydrological and primary productivity regimes, on the basis of dinocyst and foraminiferal fossil assemblages as well as on stable isotopes (O, C) and alkenones, were investigated over the last 30 ka at upwelling site MD04-2805 CQ off Morocco. The results show highest upwelling intensity during Heinrich event (HE) 1, time-coeval with a distinct plateau of heavy planktonic delta C-13 values, high concentrations of Pinus pollen and heterotrophic dinocysts, caused by an increased northern wind regime. In addition, we also present regional reconstructions of paleo-sea-surface temperatures (SSTs) using three different proxy tools: dinocyst and foraminiferal transfer functions as well as alkenones (U-37(k') - SST). The reconstructed SSTs depict coherent scenarios as modulated by the typical Northern Hemisphere climatic fluctuations. Furthermore, specific occurrences of the dinocyst Spiniferites lazus and of the foraminifer Turborotalita quinqueloba are noted for HE 2, HE 1, and the Younger Dryas, whereas in the Alboran Sea and in peri-Iberian waters these cold events were accompanied by the dinocyst Bitectatodinium tepikiense and the subpolar foraminifer Neogloboquadrina pachyderma s., both implying a marked southward shift in the planktonic population in response to the migration of polar water masses. This very pronounced demarcation between the planktonic communities better seems to attest the presence of a distinct hydrological structure in proximity of the strait of Gibraltar which separated at that time African (north of Morocco) from European (southern Iberia) water masses. (C) 2010 Elsevier Ltd. All rights reserved.	[Penaud, A.; Eynaud, F.; Turon, J. L.; Rossignol, L.; Lopez-Martinez, C.; Malaize, B.; Charlier, K.] EPOC, CNRS, UMR 5805, F-33405 Talence, France; [Penaud, A.; Eynaud, F.; Turon, J. L.; Rossignol, L.; Malaize, B.; Charlier, K.] Univ Bordeaux, EPOC, UMR 5805, F-33405 Talence, France; [Blamart, D.] Ctr Etud Saclay, LSCE, F-91191 Gif Sur Yvette, France; [Marret, F.] Univ Liverpool, Sch Environm Sci, Liverpool L69 7ZT, Merseyside, England; [Lopez-Martinez, C.; Grimalt, J. O.] Spanish Natl Res Council IIQAB CSIC, Chem & Environm Res Inst Barcelona, Dept Environm Chem, Barcelona 08034, Spain	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; University of Liverpool; Consejo Superior de Investigaciones Cientificas (CSIC)	Penaud, A (通讯作者)，EPOC, CNRS, UMR 5805, F-33405 Talence, France.	a.penaud@epoc.u-bordeaux1.fr	Lopez-Martinez, Carlos/J-7446-2012; Penaud, Aurelie/F-2485-2011; Grimalt, Joan/E-2073-2011	Lopez-Martinez, Carlos/0000-0002-1366-9446; Penaud, Aurelie/0000-0003-3578-4549; Bruno, Malaize/0000-0002-5571-9990; Eynaud, Frederique/0000-0003-1283-7425; Grimalt, Joan/0000-0002-7391-5768; Marret-Davies, Fabienne/0000-0003-4244-0437	French CNRS	French CNRS(Centre National de la Recherche Scientifique (CNRS))	Thanks to IPEV, the captain and the crew of the Marion Dufresne and the scientific team of the PRIVILEGE cruise. We wish to thank Mr. Y. Balut for his assistance at sea and M. Castera, and O. Ther for invaluable technical assistance at the laboratory. We gratefully acknowledge the reviewers, whose comments permit to greatly improve this manuscript. Part of this study was supported by the French CNRS. This is CNRS/UMR 5805-EPOC contribution No ...	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J	Torricelli, S; Knezaurek, G				Torricelli, Stefano; Knezaurek, Gabriella			NEW BIOSTRATIGRAPHIC DATA FROM THE REITANO FLYSCH <i>AUCT</i>. (SICILY, ITALY): A KEY TO A REVISED STRATIGRAPHY OF THE SICILIDE UNITS	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						Biostratigraphy; organic-walled dinoflagellate cysts; calcareous nannofossils; turbidites; volcano-arenites; Rupelian; Sicily; Italy	BASIN; SEDIMENTATION; EVOLUTION; ONSET	The study of palynomorphs and calcareous nannofossils recovered front the volcano-at clinic succession outcropping at Troma and Cerami (Sicily) documents Rupelian assemblages comparable to those published for the Tusa Tuffite This new evidence, combined with petrographic, geochemical and sedimentological affinities documented in the literature, eventually proves the genetic relationships between these units Accordingly, the new name Troma-Tusa Formation is proposed to include all these Rupehan volcano-sedimentary units and to replace inappropriate names formerly used The Troma-Tusa Formation conformably lies on a mixed siliciclastic-carbonate turbidite succession, lacking volcanic detritus, reported in the literature with different names (Polizzi Formation, Vacolori Shales, Troma-Tusa Flysch) and different ages (ranging from Eocene to Early Miocene) Palynomorphs and nannofossils recovered from Its uppermost part. Indicate an earliest Oligocene age The denomination Polizzi POT mat on is recommended (cm this unit that includes also the Varicoloured Shales (Eocene-basal Oligocene) The appearance of conglomerates and volcano-arenites in the basal portion of the Troma-Tusa Formation, immediately above the top of the Polizzi Formation, marks a sudden reorganization of the Rupehan depositional systems related to the rise and erosion of a volcanic belt Apparently, no biostratigraphically detectable hiatus is associated to this boundary Differences in the composition of sandstones, sedimentary features and relationships with the substratum do exist between the 'Internal' Reitano Flysch, outcropping in the type-area on the northern slope of the Nebrodi Mountains, and the volcano-arenitic successions of Cerami and Troma, reported by some authors as 'external' Reitano Flysch These differences are widely documented in the literature, where the 'Internal' Reitano Flysch is shown to lack volcanic detritus and to rest unconformably on the deformed Monte Soro Flysch Since the definition of the Troma-Tusa Formation now includes the external outcrops (Cerami, Troma, Ancipa Lake), the adjectives 'internal' and 'external' become disused, and the name Reliant) Flysch is restricted to the successions lacking volcanic detritus exposed in the type-area of Reitano, Pettineo, Caronia and Capizzi. Palynomorphs and nannofossils recovered from the Pettineo section, suggest a Rupehan age also fin the Reitano Flysch	[Torricelli, Stefano; Knezaurek, Gabriella] Ent Explorat & Prod, I-20097 San Donato Milanese, Italy		Torricelli, S (通讯作者)，Ent Explorat & Prod, Via Emilia 1, I-20097 San Donato Milanese, Italy.							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JUL	2010	116	2					201	221		10.13130/2039-4942/5951	http://dx.doi.org/10.13130/2039-4942/5951			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	627QH					2025-03-11	WOS:000280054600005
J	Torricelli, S				Torricelli, Stefano			<i>PSEUDORHOMBODINIUM CINGULOINDENTATUM</i> GEN. N. SP N. (DINOFLAGELLATA): A NEW ORGANIC-WALLED DINOFLAGELLATE CYST FROM THE UPPER EOCENE OF SICILY, ITALY	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						Organic-walled dinoflagellate cysts; new taxon; taxonomy; Upper Eocene; Sicily; Italy		The organic-walled dinoflagellate cyst Pseudorhombodinium cinguloindentatum gen n sp n is formally described from the Upper Eocene of Sicily, Italy It consists of a brown coloured, circumcavate wetzelielloid cyst with mat ked V-shaped cingular indentations in the pericvst The proposed generic name refers to similarities existing in the overall morphology with the genus Rhombodinium Gocht However, substantial differences in archeopyle styling, in the disposition of antapical horns, and in the amount of cingular indentation, advocate the erection of the new genus Pseudorhombodinium	Ent Explorat & Prod, I-20097 San Donato Milanese, Italy		Torricelli, S (通讯作者)，Ent Explorat & Prod, Via Emilia 1, I-20097 San Donato Milanese, Italy.							Bello M., 2000, MEM SOC GEOL ITAL, V55, P61; BUJAK JP, 1979, RHOMBODIMUM GOCHTODI, V25, P308; EVITT WR, 1985, AM ASS STRAT PALYNOL, V1; Fensome R.A., 1993, Micropaleontology Press Special Paper; FENSOME RA, 2004, AM ASS STRAT PALYNOL, V42; Fensome RA, 2009, J SYST PALAEONTOL, V7, P1, DOI 10.1017/S1477201908002538; Gocht H., 1955, Neues Jahrbuch fuer Geologie und Palaeontologie B, V2, P84; LENTIN JK, 1989, REV PALAEOBOT PALYNO, V58, P215, DOI 10.1016/0034-6667(89)90087-0; MICHOUX D, 1988, Palynology, V12, P11; TONTEETH S, 2010, RIV ITAL PALEONTOL S, V116, P201; WILLIAMS GL, 2004, P ODP SCI RES LEG, V189	11	1	1	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.	JUL	2010	116	2					261	265		10.13130/2039-4942/5950	http://dx.doi.org/10.13130/2039-4942/5950			5	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	627QH					2025-03-11	WOS:000280054600009
J	Ledu, D; Rochon, A; de Vernal, A; Barletta, F; St-Onge, G				Ledu, David; Rochon, Andre; de Vernal, Anne; Barletta, Francesco; St-Onge, Guillaume			Holocene sea ice history and climate variability along the main axis of the Northwest Passage, Canadian Arctic	PALEOCEANOGRAPHY			English	Article							PALEOMAGNETIC SECULAR VARIATION; SOUTHWESTERN VICTORIA ISLAND; WHALE BALAENA-MYSTICETUS; VARVED LAKE-SEDIMENTS; SURFACE CONDITIONS; DINOFLAGELLATE CYSTS; OSCILLATION SIGNATURE; HIGH-LATITUDES; BAFFIN-ISLAND; RIVER RUNOFF	[1] Palynological, geochemical, and physical records were used to document Holocene paleoceanographic changes in marine sediment core from Dease Strait in the western part of the main axis of the Northwest Passage (core 2005-804-006 PC latitude 68 degrees 59.552'N, longitude 106 degrees 34.413'W). Quantitative estimates of past sea surface conditions were inferred from the modern analog technique applied to dinoflagellate cyst assemblages. The chronology of core 2005-804-006 PC is based on a combined use of the paleomagnetic secular variation records and the CALS7K.2 time-varying spherical harmonic model of the geomagnetic field. The age-depth model indicates that the core spans the last similar to 7700 cal years B. P., with a sedimentation rate of 61 cm ka(-1). The reconstructed sea surface parameters were compared with those from Barrow Strait and Lancaster Sound (cores 2005-804-004 PC and 2004-804-009 PC, respectively), which allowed us to draw a millennial-scale Holocene sea ice history along the main axis of the Northwest Passage (MANWP). Overall, our data are in good agreement with previous studies based on bowhead whale remains. However, dinoflagellate sea surface based reconstructions suggest several new features. The presence of dinoflagellate cysts in the three cores for most of the Holocene indicates that the MANWP was partially ice-free over the last 10,000 years. This suggests that the recent warming observed in the MANWP could be part of the natural climate variability at the millennial time scale, whereas anthropogenic forcing could have accelerated the warming over the past decades. We associate Holocene climate variability in the MANWP with a large-scale atmospheric pattern, such as the Arctic Oscillation, which may have operated since the early Holocene. In addition to a large-scale pattern, more local conditions such as coastal current, tidal effects, or ice cap proximity may have played a role on the regional sea ice cover. These findings highlight the need to further develop regional investigations in the Arctic to provide realistic boundary conditions for climatic simulations.	[Ledu, David; Rochon, Andre; Barletta, Francesco; St-Onge, Guillaume] UQAR, ISMER, Rimouski, PQ G5L 3A1, Canada; [Ledu, David; Rochon, Andre; de Vernal, Anne; Barletta, Francesco; St-Onge, Guillaume] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada	University of Quebec; Universite du Quebec a Rimouski; University of Quebec; University of Quebec Montreal	Ledu, D (通讯作者)，UQAR, ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	david.ledu@uqar.qc.ca; andre_rochon@uqar.qc.ca; devernal.anne@uqam.ca; francesco.barletta@uqar.qc.ca; guillaume_st-onge@uqar.qc.ca	Ledu, David/X-4166-2019; St-Onge, Guillaume/E-4828-2014; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Ledu, David/0000-0001-5313-7068; St-Onge, Guillaume/0000-0001-6958-4217	ArcticNet Network of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC)	ArcticNet Network of Centres of Excellence; Natural Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was funded by the ArcticNet Network of Centres of Excellence and the Natural Science and Engineering Research Council of Canada (NSERC). This is a contribution to the ArcticNet project 1.6 (The Opening NW Passage: Resources, Navigation, Sovereignty & Security), the Polar Climate Stability Network supported by the Canadian Foundation for Climate and Atmospheric Science, and the NSERC-IPY project "Natural climate variability and forcings in Canadian Arctic and Arctic Ocean." We wish to thank the officers and crew of the CCGS Amundsen for their help and support during sampling. We also wish to express our gratitude to the following people who helped during the collection and analysis of the samples: Robbie Bennett, Bedford Institute of Oceanography; Trecia Schell, Dalhousie University; Sylvain Leblanc, Pierre Simard, and Guillaume Auclair, UQAR. Thanks are due to Bassam Ghaleb and Jean-Francois Helie (GEOTOP) for geochemical and isotope analyses. We also wish to thank Monika Korte for the CALS7K.2 inclination data at the sites of cores 006, 004, and 009 PC. Finally, we are grateful to the two anonymous reviewers for their comments, which helped to improve the manuscript.	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J	Luzar-Oberiter, B; Hochuli, PA; Babic, L; Glumac, B; Tibljas, D				Luzar-Oberiter, Borna; Hochuli, Peter A.; Babic, Ljubomir; Glumac, Bosiljka; Tibljas, Darko			Climatic cycles recorded in the Middle Eocene hemipelagites from a Dinaric foreland basin of Istria (Croatia)	GEOLOGICA CARPATHICA			English	Article						Eocene; Dinarides; Croatia; climate; cycles; hemipelagites	CYCLICITY; FORAMINIFERA; SUCCESSION; DIAGENESIS; SEDIMENTS; SIGNALS	Middle Eocene hemipelagic marls from the Pazin-Trieste Basin, a foreland basin of the Croatian Dinarides, display repetitive alternations of two types of marls with different resistance to weathering. This study focuses on the chemical composition, stable isotopes, and palynomorph content of these marls in order to better understand the nature of their cyclic deposition and to identify possible paleoenvironmental drivers responsible for their formation. The less resistant marls (LRM) have consistently lower carbonate content, lower delta O-18 and delta C-13 values, and more abundant dinoflagellate cysts than the more resistant marls (MRM). We interpret these differences between the two marl types to be a result of climatic variations, likely related to Milankovitch oscillations. Periods with wetter climate, associated with increased continental runoff, detrital and nutrient influx produced the LRM. Higher nutrient supply sparked higher dinoflagellate productivity during these times, while reduced salinity and stratification of the water column may have hampered the productivity of calcareous nannoplankton and/or planktonic foraminifera. In contrast, the MRM formed during dryer periods which favoured higher carbonate accumulation rates. This study provides new in about the sedimentary record of short-scale climate variations reflected in wet-dry cycles during an overall warm, greenhouse Earth.	[Luzar-Oberiter, Borna; Babic, Ljubomir] Univ Zagreb, Fac Sci, Inst Geol & Palaeontol, Zagreb 10000, Croatia; [Hochuli, Peter A.] Univ Zurich, Palaontol Inst, CH-8006 Zurich, Switzerland; [Glumac, Bosiljka] Smith Coll, Dept Geosci, Northampton, MA 01063 USA; [Tibljas, Darko] Univ Zagreb, Fac Sci, Inst Mineral & Petrol, Zagreb 10000, Croatia	University of Zagreb; University of Zurich; Smith College; University of Zagreb	Luzar-Oberiter, B (通讯作者)，Univ Zagreb, Fac Sci, Inst Geol & Palaeontol, Horvatovac 102A, Zagreb 10000, Croatia.	bluzar@geol.pmf.hr	Lužar-Oberiter, Borna/J-8410-2012	Luzar-Oberiter, Borna/0000-0001-9408-8071	Croatian Ministry of Science, Education and Sports [119-1191155-1159]	Croatian Ministry of Science, Education and Sports(Ministry of Science, Education and Sports, Republic of Croatia)	This work was funded by the Croatian Ministry of Science, Education and Sports project 119-1191155-1159 "Evolutionary Changes of the Dinarides from Subduction to Modern Adriatic Beaches". We sincerely thank Robert Koscal for helping prepare the figures. Stable isotope analyses were performed at the Stable Isotope Laboratory of Prof. Stephen Burns at the University of Massachusetts at Amherst, USA. Element concentrations were determined by ICP-MS at Actlab Laboratories, Canada.	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Carpath.	JUN	2010	61	3					193	200		10.2478/v10096-010-0010-7	http://dx.doi.org/10.2478/v10096-010-0010-7			8	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	632KN		Green Submitted, gold, Green Published			2025-03-11	WOS:000280422700002
J	Park, MG; Kim, M				Park, Myung Gil; Kim, Miran			PREY SPECIFICITY AND FEEDING OF THE THECATE MIXOTROPHIC DINOFLAGELLATE <i>FRAGILIDIUM DUPLOCAMPANAEFORME</i>	JOURNAL OF PHYCOLOGY			English	Article						allelopathy; Dinophysis; ecdysis; engulfment; Fragilidium duplocampanaeforme; mixotrophy; prey specificity	RED-TIDE; GRAZING RESPONSES; GROWTH; DINOPHYCEAE; LIGHT; MECHANISMS; MEXICANUM; PREDATOR	In summer to autumn of 2008, a recently described thecate mixotrophic dinoflagellate, Fragilidium duplocampanaeforme Nezan et Chomerat, occurred in Masan Bay, Korea, where it frequently contained bright-orange fluorescent inclusions. Using cultures of F. duplocampanaeforme isolated from Masan Bay, we investigated feeding, digestion, and prey specificity of this mixotroph. F. duplocampanaeforme fed exclusively on Dinophysis spp. when offered a variety of prey including dinoflagellates, a raphidophyte, a cryptophyte, a ciliate, and diatoms separately. In addition, F. duplocampanaeforme had allelopathic effects on other organisms, including cell immobilization/motility decrease (in Dinophysis acuminata, D. caudata, D. fortii, D. infundibulus, Gonyaulax polygramma, Heterocapsa triquetra, and Prorocentrum triestinum), breaking of cell chains (in Cochlodinium polykrikoides), cell death (in Prorocentrum minimum), and temporary cyst formation (in Scrippsiella trochoidea). F. duplocampanaeforme engulfed whole Dinophysis cells through the sulcus. About 1 h after ingestion, F. duplocampanaeforme became immobile and shed all thecal plates. The ecdysal cyst persisted for similar to 7 h, during which the ingested prey was gradually digested. These observations suggest that F. duplocampanaeforme may play an important role in the Dinophysis population dynamics in the field.	[Park, Myung Gil; Kim, Miran] Chonnam Natl Univ, Dept Oceanog, LOHABE, Kwangju 500757, South Korea	Chonnam National University	Park, MG (通讯作者)，Chonnam Natl Univ, Dept Oceanog, LOHABE, Kwangju 500757, South Korea.	mpark@chonnam.ac.kr	Kim, Miran/P-5739-2014	Kim, Miran/0000-0002-1958-3125	Korean Government [2009-0066796]	Korean Government(Korean Government)	This work was supported by National Research Foundation of Korea Grant funded by the Korean Government (2009-0066796) to M. G. P. We thank D. Wayne Coats (SERC) who provided valuable comments on the early version of the manuscript.	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Phycol.	JUN	2010	46	3					424	432		10.1111/j.1529-8817.2010.00824.x	http://dx.doi.org/10.1111/j.1529-8817.2010.00824.x			9	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	611MR		Bronze			2025-03-11	WOS:000278820000002
J	Pospelova, V; Kim, SJ				Pospelova, Vera; Kim, Sung-Jae			Dinoflagellate cysts in recent estuarine sediments from aquaculture sites of southern South Korea	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Cochlodinium polykrikoides; Aquaculture.; Eutrophication; Geochemistry; Buk Bay; Dongdo Bay; Gosung Bay; Harmful algal blooms (HAB's); South Korea	SURFACE SEDIMENTS; SPATIAL-DISTRIBUTION; RESTING CYSTS; TOKYO-BAY; COCHLODINIUM-POLYKRIKOIDES; MARINE-SEDIMENTS; LATE QUATERNARY; COASTAL WATERS; NORTH-ATLANTIC; YOKOHAMA-PORT	Assemblages of organic-walled dinoflagellate cysts collected from 23 surface sediment samples distributed in shallow estuarine waters along the southern South Korean coast show high abundance and diversity. A total of 47 cyst types, representing 27 genera of three orders, were identified and distribution maps of the most common taxa have been produced. The cyst assemblages were dominated by Spiniferites (Gonyaulax cf. spinifera), Brigantedinium spp. (Protoperidinium spp.), and Dubridinium spp. (Diplopsalis spp.). Total cyst concentration varies from 1000 to 8900 cysts per gram of dry sediment, with the highest values observed in the most southern sites of the Marine Fish Ranching Ground (MFRG) of Dongdo Bay, near Saryang Island, and the Outer part of Buk Bay. The Inner Buk Bay and the south-western sites of the MFRG were recognized to be subjected to eutrophication, as indicated by the elevated proportional increase in cysts of heterotrophic species of the genera Dubridinium, Polykrikos and Protoperidinium. Cysts of HAB's causing ichthyotoxic Cochlodinium polykrikoides were not found in Buk Bay, and were otherwise found in most of the studied sites in low proportions, except in Gosung Bay where it comprised up to 41% of the cyst assemblage. This is in agreement with previously observed blooms of C polykrikoides in Gosung Bay. (C) 2010 Elsevier B.V. All rights reserved.	[Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada; [Kim, Sung-Jae] Gyeongsang Natl Univ, Dept Marine Environm Engn, Tongyeong 650160, Gyeongnam, South Korea; [Kim, Sung-Jae] Gyeongsang Natl Univ, Inst Marine Ind, Coll Marine Sci, Tongyeong 650160, Gyeongnam, South Korea	University of Victoria; Gyeongsang National University; Gyeongsang National University	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, OEASB A405,POB 3065,STN CSC, Victoria, BC V8W 3V6, Canada.	vpospe@uvic.ca	Kim, Sung/AAV-4875-2021	Pospelova, Vera/0000-0003-4049-8133	Natural Sciences and Engineering Research Council of Canada (NSERC)	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	We are grateful to Dr. Choong-Jae Kim and Dr. Hee-Mock Oh for helpful comments on the initial identification of cysts of Cochlodinium polykrikoides. We particularly thank Maryse Henry (GEOTOP, UQAM) for providing us access to the environmental data. Financial support for this research was provided to VP by the Natural Sciences and Engineering Research Council of Canada (NSERC).	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Micropaleontol.	JUN	2010	76	1-2					37	51		10.1016/j.marmicro.2010.04.003	http://dx.doi.org/10.1016/j.marmicro.2010.04.003			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	621KV					2025-03-11	WOS:000279578400004
J	Matsubara, T; Kurita, H; Matsuo, H				Matsubara, Takashi; Kurita, Hiroshi; Matsuo, Hiroshi			Eocene Mollusca from the Tainohata Formation in Kobe City, southwest Japan	PALEONTOLOGICAL RESEARCH			English	Article						Eocene; geologic age; Mollusca; paleoecology; Tainohata Formation; taxonomy; temporal parallelism	PALEOGENE; PREFECTURE; AGE	The Tertiary Tainohata Formation of the Kobe Group has yielded 10 species of Gastropoda and 19 species of Bivalvia. The formation is of late Middle Eocene age on the basis of the dinoflagellate cyst assemblage and radiometric data. The occurrences of the genera Trinacria, Vicarya, and Sulcobuccinum strongly support an Eocene age for the Tainohata Formation. The molluscan fauna shows high endemism at the species level, whereas it is characterized by Tethyan-Indo-West Pacific genera. Two indigenous molluscan assemblages, Potamides-Cyclina and Corbicula, were discriminated. The composition of these assemblages compares with those of the Neogene intertidal assemblages in embayments. This fact indicates that "temporal parallelism" in the shallow embayment assemblages can be traced back to the late Middle Eocene age in the Japanese Islands. The following 10 new species are proposed herein: Potamides huzitai sp. nov., Cerithideopsilla hondai sp. nov., Crepidula tainohataensis sp. nov., Cantharus (s.l.) andoi sp. nov., Barbatia nodai sp. nov., Trinacria nipponica sp. nov., Trapezium (Neotrapezium) kobe sp. nov., Tellina (Gastranopsis?) sumaensis sp. nov., Corbicula (Corbicula) uejii sp. nov., and Pitar ozakii sp. nov.	[Matsubara, Takashi] Museum Nat & Human Act, Div Nat Hist, Hyogo Ku, Yayoigaoka, Sanda 6691546, Japan; [Kurita, Hiroshi] Niigata Univ, Fac Sci, Dept Geol, Niigata 9502181, Japan; [Matsuo, Hiroshi] Kobe Fujiwaradai Elementary Sch, Kita Ku, Kobe, Hyogo 6691546, Japan	Niigata University	Matsubara, T (通讯作者)，Museum Nat & Human Act, Div Nat Hist, Hyogo Ku, 6 Chome, Yayoigaoka, Sanda 6691546, Japan.	matsu@nat-museum.sanda.hyogo.jp	Kurita, Hiroshi/KIC-0968-2024		Japan Society for the Promotion of Sciences [12740293]; Grants-in-Aid for Scientific Research [12740293] Funding Source: KAKEN	Japan Society for the Promotion of Sciences(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We would like to express our appreciation to Yasuo Kondo (Kochi University, Kochi) and an anonymous reviewer for their critically reading the manuscript and providing valuable comments. We are also indebted to Takenori Sasaki (University of Tokyo, Tokyo), Rei Nakashima (Geological Survey of Japan, Tsukuba), Jun Nemoto (Tohoku University, Sendai), Naoko Kato (formerly of Akashi City Cultural Museum, Akashi), and Katsuki Ito (Kobe) for their kind help in the examination of specimens. We are grateful to Tokio Miyazu (Kobe) for his cooperation in collecting specimens. Thanks are also extended to the following persons for their help in accessing some references: Tomoki Kase (National Museum of Nature and Science, Tokyo); Yukito Kurihara (Mie University, Tsu); Kazutaka Amano (Joetsu University of Education, Joetsu); Tamiko Nasu (formerly of Kyoto University, Kyoto); Yoko Otani and Kenji Ohara (Nishinomiya Shell Museum, Nishinomiya); and K. Victoria Brown (Natural History Museum of Los Angeles County, Los Angeles). This study was supported by a Grant-in-Aid for Scientific Research from the Japan Society for the Promotion of Sciences (no. 12740293) to T. M.	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J	Dybkjær, K; Piasecki, S				Dybkjaer, Karen; Piasecki, Stefan			Neogene dinocyst zonation for the eastern North Sea Basin, Denmark	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Miocene; Pliocene; biostratigraphy; palynology; dinoflagellates; North Sea Basin; Denmark	DINOFLAGELLATE CYST STRATIGRAPHY; OLIGOCENE-LOWER MIOCENE; STRONTIUM ISOTOPE STRATIGRAPHY; LOOK-UP TABLE; SEQUENCE STRATIGRAPHY; UPPERMOST OLIGOCENE; CALCAREOUS NANNOPLANKTON; RESEARCH BOREHOLE; JYLLAND; MARGIN	A dinocyst zonation for the Neogene succession in the eastern part of the North Sea Basin (Denmark) is presented. The zonation is based on an extensive database comprising data from more than fifty onshore and offshore boreholes and about twenty five outcrops. Most of the nineteen dinocyst zones described and defined herein, are new. The zonation is correlated with previously published dinocyst zonations within the North Sea Basin, in the North Atlantic and with the revised Northwest European zonation. The presented zonation gives a detailed subdivision of the Oligocene-Miocene transition, of the Lower Miocene, and of the Upper Miocene and Pliocene successions. The previous zonation of the onshore Danish Middle Miocene is reconsidered and partly redefined. The zonation is correlated with other biostratigraphic subdivisions of the Neogene succession in the Danish region in addition to litho- and sequence stratigraphy. The dinocyst zonation and the foraminifer zonation of the Danish Miocene (based upon analysis of the same boreholes) were independently calibrated with the established nannoplankton zonation. This correlation revealed a mismatch generally corresponding to one nannoplankton zone. Absolute ages of the new dinocyst zones are proposed based on correlation from the studied succession within the North Sea Basin with the international zonations and stratigraphic schemes. In addition, parts of the succession have been dated by strontium isotope analysis of mollusc shells. Inconsistencies due to first and last occurrences of some dinocyst species in previous studies and the present study, especially within the Lower Miocene, implied that new Sr-isotope datings from mollusc shells from the cored Sdr. Vium borehole and other localities in this study would be invaluable. Indeed, this method allowed the previous last occurrence of Cordosphaeridium cantharellus (one of the zonal index fossils) dated as between 17.95 My and 19.5 My in previous studies, to be assigned a new dating of 18.4 My. The timespan of the zones range from 2.6 My for the Amiculospharea umbraculum Zone to 0.4 My for the Achomosphaera andalousiensis Zone. Neogene biostratigraphy in the North Sea Basin has been problematic due to the periodically limited connection between the North Sea Basin and the North Atlantic Ocean, especially with respect to stratigraphy based on foraminifers and calcareous nannoplankton. Many of the stratigraphically most important taxa, e.g. those defining stratigraphic boundaries in type sections, have not been found within the North Sea Basin. This problem seems to be solved by correlation based on the new dinocyst stratigraphy, because stratigraphically significant taxa do occur in the North Sea deposits, even in marginal marine settings. (C) 2010 Elsevier B.V. All rights reserved.	[Dybkjaer, Karen; Piasecki, Stefan] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Dybkjær, K (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	kd@geus.dk	Dybkjær, Karen/G-5223-2018					[Anonymous], 1988, Geol. 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Palaeobot. Palynology	JUN	2010	161	1-2					1	29		10.1016/j.revpalbo.2010.02.005	http://dx.doi.org/10.1016/j.revpalbo.2010.02.005			29	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	621GH					2025-03-11	WOS:000279563300001
J	Ghasemi-Nejad, E; Ardakani, EP; Ruffell, A				Ghasemi-Nejad, Ebrahim; Ardakani, Elahe Poureslami; Ruffell, Alastair			Palaeoclimate change recorded in Upper Cretaceous (Albian-Cenomanian) Kazhdumi Formation Borehole SPECTRAL Gamma-Ray Logs, South Pars Gas field, Persian Gulf	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palaeoclimate change; Gamma-ray spectroscopy; Element mobility; Cretaceous; Kazhdumi Formation; South Pars Gas field (Iran)	DINOFLAGELLATE CYSTS; CLAY MINERALOGY; CARBONATES	Th/U and Th/K data from spectral gamma-ray logs obtained from outcrop successions have been used as a rapid and inexpensive proxy for determining possible episodes of humid-arid palaeoclimate change. Such outcrop-based measurements have never been tested using spectral gamma-ray data obtained from wireline logs in subsurface boreholes. Th/K and Th/U ratios have traditionally been used to decipher sequence stratigraphic patterns, at outcrop and in borehole. The possible influence of palaeoclimate on such ratio changes has yet to be proven, especially from borehole data. In this work, we compare borehole-derived Th/K (and to a lesser extent Th/U) to palaeoenvironmental changes inferred from palynology and deduce that both sea level and changing hinterland weathering regimes caused discrete fluctuations observed in the spectral gamma-ray logs. This is the first time such subsurface information has been used in this way. Interpretation of wireline logs in terms of palaeoclimate as well as sea level may now be considered, and the use of such logs in palaeoclimate reconstruction is strengthened. (C) 2010 Elsevier B.V. All rights reserved.	[Ghasemi-Nejad, Ebrahim] Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran; [Ardakani, Elahe Poureslami] Univ Alberta, Dept Phys, Edmonton, AB T6G 2G7, Canada; [Ruffell, Alastair] Queens Univ, Sch Geog Archaeol & Palaeoecol, Belfast BT7 1NN, Antrim, North Ireland	University of Tehran; University of Alberta; Queens University Belfast	Ghasemi-Nejad, E (通讯作者)，Univ Tehran, Fac Sci, Dept Geol, Tehran, Iran.	eghasemi@khayam.ut.ac.ir; epoureslami@hotmail.com; a.ruffell@qub.ac.uk	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ruffell, Alastair/0000-0001-6072-501X; Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068	University Of Tehran	University Of Tehran(University of Tehran)	The authors EG-N and EPA wish to thank the research directorate of the South Pars Oil and Gas Company of Iran and the National Iranian Oil Company (NIOC) for the provision of samples. The Vice Chancellor for research (University Of Tehran) provided financial support for this project. We are grateful to M. Rajabi for his helpful comments and A. Kadkhodaie for his cooperation. We also thank Professor David Batten for his extensive comments on previous versions of this work, as well as the great efforts of both reviewers and editors of this manuscript.	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Paleoclimatol. Paleoecol.	MAY 15	2010	291	3-4					338	347		10.1016/j.palaeo.2010.03.005	http://dx.doi.org/10.1016/j.palaeo.2010.03.005			10	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	611AI					2025-03-11	WOS:000278782400014
J	Holzwarth, U; Meggers, H; Esper, O; Kuhlmann, H; Freudenthal, T; Hensen, C; Zonneveld, KAF				Holzwarth, Ulrike; Meggers, Helge; Esper, Oliver; Kuhlmann, Holger; Freudenthal, Tim; Hensen, Christian; Zonneveld, Karin A. F.			NW African climate variations during the last 47,000 years: Evidence from organic-walled dinoflagellate cysts	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Northwest Africa; Dinoflagellate cysts; Fluvial input; Sea-level; Productivity; Upwelling	SEA-SURFACE CONDITIONS; NORTH CANARY BASIN; UPWELLING INTENSITY; OCEAN PRODUCTIVITY; GYMNODINIUM-CATENATUM; TROPICAL ATLANTIC; LATE QUATERNARY; HIGH-LATITUDES; GLACIAL OCEAN; PARTICLE-FLUX	NW African climate shows orbital and millennial-scale variations, which are tightly connected to changes in marine productivity. We present an organic-walled dinoflagellate cyst (dinocyst) record from a sediment core off Cape Yubi at about 27 degrees N in the Canary Basin covering the time period from 47 to 3 ka before present (BP). The dinocyst record reflects differences in upwelling intensity and seasonality as well as the influence of fluvial input. Sea-level changes play an important role for the upwelling pattern and productivity signals at the core site. Within the studied time interval, four main phases were distinguished. (1) From 45 to 24 ka BP, when sea-level was mostly about 75 m lower than today, high relative abundances of cysts of heterotrophic taxa point to enhanced upwelling activity, especially during Heinrich Events, while relatively low dinocyst accumulation rates indicate that filament activity at the core location was strongly reduced. (2) At sea-level lowstand during the LGM to H1, dinocyst accumulation rates suggest that local filament formation was even more inhibited. (3) From the early Holocene to about 8 ka BP, extraordinary high accumulation rates of most dinocyst species, especially of Lingulodinium machaerophorum, suggest that nutrient supply via fluvial input increased and rising sea-level promoted filament formation. At the same time, the upwelling season prolongated. (4) A relative increase in cysts of photoautotrophic taxa from about 8 ka BP onwards indicates more stratified conditions while fluvial input decreased. Our study shows that productivity records can be very sensitive to regional features. From the dinocyst data we infer that marine surface productivity off Cape Yubi during glacial times was within the scale of modern times but extremely enhanced during deglaciation. (C) 2010 Elsevier B.V. All rights reserved.	[Holzwarth, Ulrike; Kuhlmann, Holger; Freudenthal, Tim] Univ Bremen, Ctr Marine Environm Sci MARUM, D-28359 Bremen, Germany; [Meggers, Helge; Zonneveld, Karin A. F.] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Esper, Oliver] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; [Hensen, Christian] Leibniz Inst Meereswissensch IFM GEOMAR, D-24148 Kiel, Germany	University of Bremen; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel	Holzwarth, U (通讯作者)，Univ Bremen, Ctr Marine Environm Sci MARUM, Leobener Str, D-28359 Bremen, Germany.	holzwarth@uni-bremen.de	Hensen, Christian/B-8161-2014	Kuhlmann, Holger/0000-0001-8932-7031; Esper, Oliver/0000-0002-4342-3471	DFG	DFG(German Research Foundation (DFG))	We thank C. Harnach for sample processing. S. de Schepper, K. Mertens and J.-B. Stuut are acknowledged for useful discussions. We are grateful to W.R. Peltier and R. Drummond for help with the local sea-level prediction. F. Marret, an anonymous Reviewer and the Editor of the Journal provided constructive comments. All data presented in this study are available through the database PANGAEA (www.pangaea.de; http://doi.pangaea.de/10.1594/PANGAEA.726630). This work was funded through the DFG Research Center/Excellence Cluster "The Ocean in the Earth System".	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Paleoclimatol. Paleoecol.	MAY 15	2010	291	3-4					443	455		10.1016/j.palaeo.2010.03.013	http://dx.doi.org/10.1016/j.palaeo.2010.03.013			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	611AI					2025-03-11	WOS:000278782400022
J	Fernández-Marrón, MT; Gil, J; Gil-Cid, MD; Fonollá-Ocete, JF				Teresa Fernandez-Marron, Maria; Gil, Javier; Dolores Gil-Cid, Maria; Fernando Fonolla-Ocete, Jose			Precisions to the depositional stacking pattern of Cenomanian-Turonian sequences in the Iberian Range (Somolinos outcrop, Spain) from a palynological study	GEOBIOS			French	Article						Palynology; Late Cenomanian-Mid Turonian; 3rd order depositional pattern; Somolinos outcrop; Iberian Basin; Spain	TROUGH; CYCLES	The Somolinos outcrop was widely studied in detailed correlations, stratigraphical architecture and high frequency sequence analysis of Central System and Iberian range successions. A rich assemblage of echinoids, ammonites, bivalves and bryozoans was described; conversely, the palynological study of the Late Cretaceous levels from Somolinos has never been performed up to now. A palynological study of two intervals within a monotonous alternation of grey marls and nodular limestone succession in the Somolinos section was carried out. The two intervals sampled are located in two correlative sequences of Late Cenomanian-Early Turonian and mid Turonian ages, respectively. Both sequences are separated by a sequence boundary, but its location and age in the stratigraphic record differs depending on the authors and the Basin considered. A rich palynofacies with abundant dinoflagellate cysts, pteridophyte spores, conifer pollens and breviary angiosperm grains of the normapolles group is described; besides, inner linings of acid resistant microforaminiferal tests were also found. The analysis of the palynological diagrams clearly indicates that the upper interval corresponds to open sea neritic sediments, deposited in more distal sedimentary environments than those of the lower interval, which were deposited in more proximal environments. This evolution of sedimentary environments represents a major sedimentary change in the general shallowing upwards trend of the late Albian-mid Turonian 2nd order succession, revealing a major facies belt retrogradation of the sequence containing the upper interval. This retrogradational event allows to accurately place the sequence boundary and to improve the arrangement of the low frequency (3rd order) depositional stacking pattern of the Early-mid Turonian in the Iberian Basin and other European and Tethyan basins. (C) 2010 Elsevier Masson SAS. All rights reserved.	[Teresa Fernandez-Marron, Maria; Dolores Gil-Cid, Maria; Fernando Fonolla-Ocete, Jose] Univ Complutense, Fac Ciencias Geol, Dept UEI Paleontol, E-28040 Madrid, Spain; [Teresa Fernandez-Marron, Maria; Dolores Gil-Cid, Maria; Fernando Fonolla-Ocete, Jose] UCM, CSIC, Inst Geol Econ, Madrid 28040, Spain; [Gil, Javier] Univ Alcala, Dept Geol, IBERCRETA UAH Res Team CCTE 2007 R23, Madrid 28871, Spain	Complutense University of Madrid; Complutense University of Madrid; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC-UCM - Instituto de Geologia Economica (IGE); Universidad de Alcala	Fernández-Marrón, MT (通讯作者)，Univ Complutense, Fac Ciencias Geol, Dept UEI Paleontol, C J Antonio Novais 2, E-28040 Madrid, Spain.	emarron@geo.ucm.es	Gil Gil, Javier/E-5856-2012	Gil Gil, Javier/0000-0002-7298-8113				Barroso-Barcenilla F, 2007, GEOBIOS-LYON, V40, P455, DOI 10.1016/j.geobios.2008.02.003; Barroso-Barcenilla F, 2009, NEWSL STRATIGR, V43, P139, DOI 10.1127/0078-0421/2009/0043-0139; BERTHOU P.-Y., 1982, CUADERNOS GEOLOG A I, V8, P761; CALDERON S, 1874, REV U MADRID, V97, P34; CARENAS B, 1989, CRETACEOUS W TETHYS, P15; Castel C., 1881, B COMISION MAPA GEOL, V8, P157; Cech Stanislav, 2005, Bulletin of Geosciences, V80, P321; FLOQUET M., 1991, M MOIRES G OLOGIQUES, V14, P1; Floquet M., 1998, MESOZOIC CENOZOIC SE, V60, P343; Floquet M., 1982, CRET CICO ESPA A, P387; Garcia A, 1996, SEDIMENT GEOL, V103, P175, DOI 10.1016/0037-0738(95)00109-3; Garcia A., 2004, GEOLOGIA ESPANA, P510; Garcia-Hidalgo JF, 2007, SEDIMENTOLOGY, V54, P1245, DOI 10.1111/j.1365-3091.2007.00880.x; GARCIAHIDALGO JF, 2003, J IBER GEOL, V29, P55; Gil J, 2006, SEDIMENT GEOL, V191, P191, DOI 10.1016/j.sedgeo.2006.03.023; GIL J., 1996, ESTUDIOS GEOL GICOS, V52, P37; Gil J., 2006, Z DTSCH GESELLSCHAFT, V157, P667; GIL J., 2004, REV SOC GEOL GICA ES, V17, P249; Gradstein F., 2004, A Geological Time Scale; GRAFE KU, 1998, SEPM SPECIAL PUBLICA, V60, P333; GROOT JOHAN J., 1962, COMMUNICACOES SERV GEOL PORT, V46, P133; Haq BU, 2005, GEOARABIA, V10, P127; Haq BU., 1988, SEA LEVEL CHANGES IN, V42, P71, DOI DOI 10.2110/PEC.88.01.0071; Hardenbol J., 1998, Mesozoic and Cenozoic sequence stratigraphy of European basins, V60, P3, DOI 10.2110/pec.98.02.0003 cs; Hardenbol J., 1998, MESOZOIC CENOZOIC SE, P329, DOI 10.2110/pec.98.02.0329; HERNGREEN G F W, 1980, Revista Espanola de Micropaleontologia, V12, P23; Herngreen GFW., 1996, PALYNOLOGY PRINCIPLE, V3, P1157; KEDVES M, 1979, Boletim da Sociedade Geologica de Portugal, V21, P203; KEDVES M, 1994, PLANT CELL BIOL DEV, V5, P29; KEDVES M, 1993, PLANT CELL BIOL DEV, V4, P22; Lister J.K., 1988, PALAEONTOGRAPHICA SE, V210, P9; lvarez Ramis C., 1980, Boletn De La Real Sociedad Espaola De Historia Natural, V78, P205; 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; Méon H, 2004, B SOC GEOL FR, V175, P579, DOI 10.2113/175.6.579; RAMIS CA, 1996, REV ESP MICROPALEONT, V28, P101; RAMIS CA, 1994, PLANT CELL BIOL DEV, V5, P42; RAMIS CA, 1994, REV ESP MICROPALEONT, V36, P5; ROBASZYNSKI F, 1993, B CENT RECH EXPL, V17, P395; Robaszynski F., 1990, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V14, P213; Robaszynski F., 1998, SEPM Special Publications, V60, P363, DOI [10.2110/pec.98.02.0363, DOI 10.2110/PEC.98.02.0363]; Schroeder E., 1930, PUBLICACIONES EXTRAN, V4, P294; SEGURA M, 1993, AAPG BULL, P283; SEGURA M., 1989, GEOBIOS-LYON, V22, P161; SEGURA M., 1996, GEOGACETA, V20, P54; Segura M., 2002, GEOLOGY SPAIN, P288; Segura M., 2004, Geogaceta, V36, P103; SEGURA M, 1999, CRETACICO ZONA INTER, P129; Sole de Porta N., 1978, PALINOLOGIA, P435; VERNEUIL C, 1853, B SOC GEOLOGIQUE FRN, V2, P1; Wiedmann J., 1964, Estudios Geologicos Instituto de Investigaciones Geologicas Lucas Mallada, V20, P107	51	3	5	0	4	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	ISSY-LES-MOULINEAUX	65 RUE CAMILLE DESMOULINS, CS50083, 92442 ISSY-LES-MOULINEAUX, FRANCE	0016-6995	1777-5728		GEOBIOS-LYON	Geobios	MAY-JUN	2010	43	3					305	315		10.1016/j.geobios.2009.10.007	http://dx.doi.org/10.1016/j.geobios.2009.10.007			11	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	615WR					2025-03-11	WOS:000279169300003
J	Kholeif, SE; Ibrahim, MI				Kholeif, Suzan El Hasanein; Ibrahim, Mohamed Ismail			Palynofacies Analysis of Inner Continental Shelf and Middle Slope Sediments offshore Egypt, South-eastern Mediterranean	GEOBIOS			English	Article						Dinoflagellate cysts; Palynofacies; Phytoclasts; Sedimentary organic matter; South-eastern Mediterranean; Nile Delta	WALLED DINOFLAGELLATE CYSTS; ORGANIC-MATTER; HYDROLOGICAL CHANGES; SAPROPEL FORMATION; HOLOCENE SAPROPEL; AFRICAN MONSOON; AEGEAN SEA; CLIMATE; INTERRUPTION; VARIABILITY	Marine palynological studies of Quaternary sediments usually focus on dinoflagellate and pollen assemblages for palcoceanographic and paleohydrographic interpretations of past events. This paper focuses on the use of palynofacies analysis for paleohydrological reconstructions of deltaic and deep sea environments to evaluate transport of organic matter to the ocean. These palynodebris data are used to interpret palaeoenvironmental and paleohydrographic changes in two marine cores from the continental shelf (core-1, 27 m water depth) and middle slope (core-2, 1030 m) offshore Egypt, south-eastern Mediterranean Sea, during the latest Pleistocene and the Holocene. The relative abundances of various types of sedimentary organic matter such as phytoclasts, zooclasts, amorphous organic matter and palynomorphs are related to paleohydrographic changes of the overlying water column. Based on the total palynodebris and organic carbon content, sediments of the inner continental shelf core are characteristic of a prodelta environment proximal to a fluvio-deltaic source and moderately distal oxic environments with enhanced structured organic matter preservation potential. In contrast, the palynodebris of the middle slope core show that the basal sediments (105-140 cm depth) indicate suboxic to dysoxic bottom water conditions, followed by anoxic-suboxic bottom water conditions for the interval from 30-85 cm, which represents the SI Sapropel. The top sediments of core-2 (0-25 cm) were deposited under oxic bottom water conditions, suggesting good ventilation in the water column. A quantitative approach was also used for interpreting the Holocene sea-level changes, based on the correlation between phytoclast and organic matter abundances. Sedimentation rate in the continental shelf is varied, being relatively very low (6.7 cm/kyr) in the basal part and increased upward to be 20 cm/kyr (depth 115-120 cm). In the upper Gray clayey silt layer the sedimentation rate was high (about 40-45 cm/kyr) due to the high discharge from El Manzala Lagoon and Damietta Nile branch. In the middle slope depth the sedimentation rate was relatively low and uniform, around 14 cm/kyr. (C) 2010 Elsevier Masson SAS. All rights reserved.	[Kholeif, Suzan El Hasanein] NIOF, Alexandria, Egypt; [Ibrahim, Mohamed Ismail] Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria 21511, Egypt	Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF); Egyptian Knowledge Bank (EKB); Alexandria University	Kholeif, SE (通讯作者)，NIOF, Alexandria, Egypt.	suzan_kholeif@yahoo.com	Ibrahim, Mohammed/IUQ-7100-2023	Ibrahim, Mohamed Ismail Abdou/0000-0002-5782-0435				Abrajano T, 2002, MAR GEOL, V190, P151, DOI 10.1016/S0025-3227(02)00346-8; 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; [Anonymous], 1974, FOSSIL LIVING DINOFL; BARTZOKAS A, 1991, RIV METEOROLOGIA AER, V51, P47; Batten D., 1996, Palynology: principles and applications, P1011; BATTEN D J, 1973, Palaeontology (Oxford), V16, P1; BATTEN D.J., 1975, P GEOL ASS, V85, P433; Batten D.J., 1983, PETROLEUM GEOCHEMIST, P275; Batten D.J., 1982, J. 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J	Rhodes, L; Smith, K; Selwood, A; McNabb, P; van Ginkel, R; Holland, P; Munday, R				Rhodes, L.; Smith, K.; Selwood, A.; McNabb, P.; van Ginkel, R.; Holland, P.; Munday, R.			Production of pinnatoxins by a peridinoid dinoflagellate isolated from Northland, New Zealand	HARMFUL ALGAE			English	Article						LC-MS; New Zealand; Peridiniales; Pinnatoxin; Rangaunu Harbour; Toxicity	SHELLFISH POISON; DINOPHYCEAE	A peridinoid dinoflagellate was newly identified as the producer of pinnatoxins E (0-3.7 pg cell(-1)) and F (0.3-20.1 pg cell(-1)), as determined by LC-MS analysis of extracts of eight strains of the organism. The cyst-forming, thecate dinoflagellate was isolated from surface sediments associated with eel grass beds and mangroves in Rangaunu Harbour, Northland, New Zealand. Extracts of mass cultures of the dinoflagellate were tested for toxicity in mice by intraperitoneal injection, gavage and voluntary consumption. The LD50 values were 1.33, 2.33 and 5.95 mg/kg respectively. (C) 2010 Elsevier B.V. All rights reserved.	[Rhodes, L.; Smith, K.; Selwood, A.; McNabb, P.; van Ginkel, R.; Holland, P.] Cawthron Inst, Nelson 7042, New Zealand; [Munday, R.] AgResearch, Hamilton, New Zealand	Cawthron Institute; AgResearch - New Zealand	Rhodes, L (通讯作者)，Cawthron Inst, 98 Halifax St E, Nelson 7042, New Zealand.	Lesley.Rhodes@cawthron.org.nz	Selwood, Andrew/AAP-7550-2020; McNabb, Paul/LKN-9195-2024	Selwood, Andrew/0000-0003-1399-8028	NZ Foundation [CAW0703]; NZ Food Safety Authority	NZ Foundation; NZ Food Safety Authority	Particular thanks to S. Waitai and members of his whanau for sampling and barge time in Rangaunu Harbour. Thanks to P. Harris (Sanford Ltd.), R. Sabritzski (Northland biotoxin sampling officer), D.-J. McCoubrey (Aquaculture NZ), G.M. Hallegraeff, M. de Salas (UTas), D. Hoperoft (Manawatu Microscopy and Imaging Centre, Massey Univ.), and J. Adamson, A. Immers and D. Clement (Cawthron), who supported the study in different ways. Funded by NZ Foundation for RST, Contract CAW0703 and a NZ Food Safety Authority contract.[SS]	[Anonymous], REV MARINE BIOTOXIN; BINDER BJ, 1987, J PHYCOL, V23, P99; Chou T, 1996, TETRAHEDRON LETT, V37, P4027, DOI 10.1016/0040-4039(96)00753-8; Chou T, 1996, TETRAHEDRON LETT, V37, P4023, DOI 10.1016/0040-4039(96)00752-6; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; GUILLARD RRL, 1993, PHYCOLOGIA, V32, P234, DOI 10.2216/i0031-8884-32-3-234.1; Huelsenbeck JP, 2001, BIOINFORMATICS, V17, P754, DOI 10.1093/bioinformatics/17.8.754; KELLER MD, 1987, J PHYCOL, V23, P633; LOEBLICH AR, 1968, LIPIDS, V3, P5, DOI 10.1007/BF02530961; McNabb P., 2008, 1453 CAWTHR; Munday R, 2006, AFR J MAR SCI, V28, P447, DOI 10.2989/18142320609504195; Munday Rex, 2008, P581; Nunn GB, 1996, J MOL EVOL, V42, P211, DOI 10.1007/BF02198847; Nylander J.A. A., 2004, PROGRAM DISTRIBUTED; OECD, 2006, OECD GUID TEST CHEM; Parrow Matthew, 2002, Harmful Algae, V1, P5, DOI 10.1016/S1568-9883(02)00009-4; RHODES L, 1996, P 6 NZ MAR BIOT SCI; RHODES L, P 13 INT C IN PRESS; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; SELWOOD AI, J AGR FOOD CHEM; Takada N, 2001, TETRAHEDRON LETT, V42, P3491, DOI 10.1016/S0040-4039(01)00480-4; THOMAS A, 1998, CATHRON I CULTURE CO; UEMURA D, 1995, J AM CHEM SOC, V117, P1155, DOI 10.1021/ja00108a043	24	79	85	1	20	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	MAY	2010	9	4					384	389		10.1016/j.hal.2010.01.008	http://dx.doi.org/10.1016/j.hal.2010.01.008			6	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	598GM					2025-03-11	WOS:000277823100005
J	Hattenrath, TK; Anderson, DM; Gobler, CJ				Hattenrath, Theresa K.; Anderson, Donald M.; Gobler, Christopher J.			The influence of anthropogenic nitrogen loading and meteorological conditions on the dynamics and toxicity of <i>Alexandrium fundyense</i> blooms in a New York (USA) estuary	HARMFUL ALGAE			English	Article						Alexandrium; Anthropogenic nitrogen loading; delta N-15; Toxin; Climate	HARMFUL ALGAL BLOOMS; PHYSICAL-BIOLOGICAL MODEL; RED TIDE DINOFLAGELLATE; GONYAULAX-TAMARENSIS; WESTERN GULF; AUREOCOCCUS-ANOPHAGEFFERENS; PHYTOPLANKTON COMMUNITIES; UNITED-STATES; NEW-ENGLAND; MAINE	The goal of this two-year study was to explore the role of nutrients and climatic conditions in promoting reoccurring Alexandrium fundyense blooms in the Northport-Huntington Bay complex, NY, USA. A bloom in 2007 was short and small (3 weeks, 10(3) cells L-1 maximal density) compared to 2008 when the A. fundyense bloom, which persisted for 6 weeks, achieved cell densities >10(6) cells L-1 and water column saxitoxin concentrations >2.4 x 10(4) pmol STX eq. L-1. During the 2008 bloom, both deployed mussels (used as indicator species) and wild soft shell clams became highly toxic (1400 and 600 mu g STX eq./100 g shellfish tissue, respectively) resulting in the closure of shellfish beds. The densities of benthic A. fundyense cysts at the onset of this bloom were four orders of magnitude lower than levels needed to account for observed cell densities, indicating in situ growth of vegetative cells was responsible for elevated bloom densities. Experimental enrichment of bloom water with nitrogenous compounds, particularly ammonium, significantly increased A. fundyense densities and particulate saxitoxin concentrations relative to unamended control treatments. The delta N-15 signatures (12-23 parts per thousand) of particulate organic matter (POM) during blooms were similar to those of sewage (10-30 parts per thousand) and both toxin and A. fundyense densities were significantly correlated with POM delta N-15 (p < 0.001). These findings suggest A. fundyense growth was supported by a source of wastewater such as the sewage treatment plant which discharges into Northport Harbor. Warmer than average atmospheric temperatures in the late winter and spring of 2008 and a cooler May contributed to an extended period of water column temperatures optimal for A. fundyense growth (12-20 degrees C), and thus may have also contributed toward the larger and longer bloom in 2008. Together this evidence suggests sewage-derived N loading and above average spring temperatures can promote intense and toxic A. fundyense blooms in estuaries. (C) 2010 Elsevier B.V. All rights reserved.	[Hattenrath, Theresa K.; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY 11968 USA; [Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	State University of New York (SUNY) System; Stony Brook University; Woods Hole Oceanographic Institution	Gobler, CJ (通讯作者)，SUNY Stony Brook, Sch Marine & Atmospher Sci, Southampton, NY 11968 USA.	christopher.gobler@sunysb.edu	Gobler, Christopher/JOZ-2924-2023		EPA's Long Island Sound Study, New York Sea; New York State Department of Environmental Conservation; NOAA [NA060AR4170021 (R/B-177)]	EPA's Long Island Sound Study, New York Sea; New York State Department of Environmental Conservation; NOAA(National Oceanic Atmospheric Admin (NOAA) - USA)	We gratefully acknowledge F. Koch, A. Marcoval, J. Goleski, A. Burson, M. Harke, T. Davis, S. Angles, C. Wall, Y.Z. Tang, C. Lehmann and R. Hattenrath for their assistance in the field and with sample processing. We would also like to thank B. Keafer, K. Norton and D. Kulis for assistance with the oligonucleotide method, cyst sampling methodologies as well as HPLC analysis of saxitoxin samples. This work was supported by a grant from EPA's Long Island Sound Study, New York Sea Grant, and the New York State Department of Environmental Conservation (to CJG) and from the NOAA Sea Grant Program (Grant No. NA060AR4170021 (R/B-177)) to DMA.[SS]	Anderson D.M., 2003, Monographs on Oceanographic Methodology, V11, P165; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2467, DOI 10.1016/j.dsr2.2005.06.015; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1990, TOXICON, V28, P885, DOI 10.1016/0041-0101(90)90018-3; Anderson DM, 2005, LIMNOL OCEANOGR, V50, P328, DOI 10.4319/lo.2005.50.1.0328; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; ANDERSON DM, 1994, MAR BIOL, V120, P467, DOI 10.1007/BF00680222; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 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, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; ANDERSON DM, 2000, 200111 WHOI; Anderson DM, 2008, HARMFUL ALGAE, V8, P39, DOI 10.1016/j.hal.2008.08.017; Anderson Donald M., 1994, Scientific American, V271, P52; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BIANCHI TS, 2007, BIGEOCHEMISTRY ESTUA; Bricelj V. 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J	Ji, LM; Yan, K; Meng, FW; Zhao, M				Ji, Li-ming; Yan, Kui; Meng, Fan-wei; Zhao, Min			The oleaginous <i>Botryococcus</i> from the Triassic Yanchang Formation in Ordos Basin, Northwestern China: Morphology and its paleoenvironmental significance	JOURNAL OF ASIAN EARTH SCIENCES			English	Article						Ordos Basin; Triassic; Yanchang Formation; Hydrocarbon source rocks; Botryococcus; Paleoenvironment	GLOEOCAPSOMORPHA-PRISCA; DINOFLAGELLATE CYSTS; ARCTIC-OCEAN; BRAUNII; ALGA; HYDROCARBONS; LAKE; INDICATORS; VENEZUELA; SEDIMENTS	High abundance but rather low diversity algal fossils were found in the hydrocarbon source rocks of the Ch 7-2-Ch 7-3 section, Triassic Yanchang Formation in the Xifeng area of southwest Ordos Basin, which are mainly composed of prolific Leiosphaeridia and Botryococcus. Botryococcus colonies are of various forms; the majority is nubbly, with some of cluster and cotton shape. The nubbly colonies appear globular, cordiform, ternate petal, obtuse triangle, chrysanthemum shape and so on. Most Botryococcus are saffron or brown and are frequently covered with clay under transmission microscope, and shows strong yellow and light brown under fluorescence microscope. Botryococcus could live in freshwater and brackish water. The Botryococcus colonies that lived in fresh water are small with small single cells arranged radially, with undulant or indented edges. The Botryococcus colonies that lived in brackish water are bigger, with larger single cells arranged irregularly, with slippery contours. The most of Botryococcus are discovered from the organic-rich argillaceous sediment with abundant pyrites in the semi- and deep-lake facies, and shows they were preserved in low-energy reducing environments. Taphonomic characteristics of various microfossils and the present of Pediastrum in the phytoplankton flora indicate that they are in situ or near burial. The lake area of the Ordos Basin was gradually expanding and reaching its most extensive flood surface in the Ch 7 of Yanchang Formation interval during the Middle and Late Triassic, with warm climate, plentiful rainfall, and luxuriant vegetation, as determined by the environmental analysis with Botryococcus in Xifeng area. The presence of two ecological types of Botryococcus indicates that the salinity of lake water was fluctuating in the Ch 7 interval. The occurrence of symbiotic acritarchs and geochemical salinity indices show that the Ordos Lake was a typical fresh-water lake, which was gradually desalted, and its salinity fluctuation was narrow during the Mid-Later Triassic. The ecological type of the palynological flora discovered from the Ch 7 to Ch 8 in Xifeng area is similar to that from the Fuxian Lake, with abundant Botryococcus in the Yungui Plateau of China. These findings imply that the Ordos Basin was in a lower-latitude area of temperate to subtropical climate during the Middle and Late Triassic. (C) 2009 Elsevier Ltd. All rights reserved.	[Ji, Li-ming; Zhao, Min] Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Lanzhou 730000, Gansu Province, Peoples R China; [Yan, Kui; Meng, Fan-wei] Chinese Acad Sci, Nanjing Inst Geol & Palaeontol, State Key Lab Palaeobiol & Stratig, Nanjing 210008, Jiangsu Prov, Peoples R China; [Zhao, Min] Chinese Acad Sci, Grad Sch, Beijing 100069, Peoples R China	Chinese Academy of Sciences; Institute of Geology & Geophysics, CAS; Chinese Academy of Sciences; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Ji, LM (通讯作者)，Chinese Acad Sci, Inst Geol & Geophys, Key Lab Petr Resources Res, Lanzhou 730000, Gansu Province, Peoples R China.	Jiliming1998@hotmail.com	Ji, Liming/B-2573-2013; Zhao, Min/JGM-3156-2023	yan, kui/0000-0002-4205-2437	Chinese Academy of Sciences [CAS2002-404-01]; State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology [073105]	Chinese Academy of Sciences(Chinese Academy of Sciences); State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology	We thank Xu Jinli, the senior engineer of Geology Science Academy of the Shengli Oilfield for identifying algae fossils and Li Jianfeng, the senior engineer of the Prospecting and Development Academy of Changqing Oilfield Company for collecting samples. Financial support from the following institutions is acknowledged: The Chinese Academy of Sciences (Grant No. CAS2002-404-01) and State Key Laboratory of Palaeobiology and Stratigraphy, Nanjing Institute of Geology and Palaeontology (Grant No. 073105). We thank Dr. Gabriel Yedid of the Nanjing Institute of Geology and Palaeontology for editing and proofreading the English manuscript.	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Asian Earth Sci.	MAY 1	2010	38	5					175	185		10.1016/j.jseaes.2009.12.010	http://dx.doi.org/10.1016/j.jseaes.2009.12.010			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	599OV					2025-03-11	WOS:000277923900001
J	Pearce, MA				Pearce, Martin A.			New organic-walled dinoflagellate cysts from the Cenomanian to Maastrichtian of the Trunch borehole, UK	JOURNAL OF MICROPALAEONTOLOGY			English	Article						new species & genera; Trunch borehole; dinoflagellate cysts; taxonomy; Upper Cretaceous	SEA; BIOSTRATIGRAPHY; NETHERLANDS; ZONATION; GENERA; CHALK	A high-resolution palynological study of Cenomanian to Maastrichtian chalks from the Trunch borehole (southeastern UK) has revealed twelve new species and one new subspecies of organic-walled dinoflagellate cysts: Alterbidinium ioannidesii sp. nov., Cassiculosphaeridia alta sp. nov., Chatangiella eminens sp. nov., Cordosphaeridium catherineae sp. nov., Eatonicysta exilis sp. nov., Eatonieysta? mutabilireta sp. nov., Hystrichostrogylon robustum, sp. nov., Membranilarnacia wilsonii sp. nov., Nelsoniella incomposita sp. nov., Odontochitina diducta sp. nov., Spiniferites jarvisii sp. nov., Spiniferites multispinulus sp. nov. and Spiniferites ramosus aquilus subsp. nov. Two new genera, Dimidium gen. nov. and Whitecliffia gen. nov. are described to necessitate the new combinations (with a former name in parentheses) of Dimidium striatum twit et comb. nov. (Pterodinium? striatum) and Whitecliffia spinosa gen. et comb. nov. (Thalassiphord? spinosa). J. Micropalaeontol. 29(1): 51-72. May 2010.	Statoil ASA Sandsliveien 90, N-5254 Bergen, Norway	Equinor	Pearce, MA (通讯作者)，Statoil ASA Sandsliveien 90, N-5254 Bergen, Norway.	mpear@statoil.com		Pearce, Martin/0000-0001-7856-1076	Statoil ASA, Norway	Statoil ASA, Norway	The author would like to thank the British Geological Survey for access to the Trunch borehole material and to Malcolm Jones (Palynological laboratory Service) for preparing the palynoloeical slides. Sincere thanks go to Roger Davey, Pool Schioler and F. John Gregory for a detailed and critical review that improved an earlier draft. Funding from Statoil ASA, Norway is gratefully acknowledged.	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MAY	2010	29		1				51	72		10.1144/jm.29.1.51	http://dx.doi.org/10.1144/jm.29.1.51			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	614BN		hybrid			2025-03-11	WOS:000279030100005
J	Pospelova, V; Esenkulova, S; Johannessen, SC; O'Brien, MC; Macdonald, RW				Pospelova, Vera; Esenkulova, Svetlana; Johannessen, Sophia C.; O'Brien, Mary C.; Macdonald, Robie W.			Organic-walled dinoflagellate cyst production, composition and flux from 1996 to 1998 in the central Strait of Georgia (BC, Canada): A sediment trap study	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Sediment trap; Strait of Georgia; El Nino; Coastal and estuarine systems; Phytoplankton; Dinoflagellates; Biogenic silica	SEA-SURFACE CONDITIONS; RECENT MARINE-SEDIMENTS; JUAN-DE-FUCA; BRITISH-COLUMBIA; ENVIRONMENTAL-FACTORS; SPATIAL-DISTRIBUTION; ESTUARINE SEDIMENTS; NORTH-ATLANTIC; PACIFIC-OCEAN; PRESERVATION	Bi-weekly fluxes of dinoflagellate cysts and assemblage composition were recorded from March 1996 to January 1999 in the central part of the Strait of Georgia (BC, Canada). The study period captured the 1997-98 El Nino event, which was characterized locally by increased Fraser River discharge resulting from earlier than usual snowmelt in 1997 and warmer sea-surface temperatures in 1998. Thirty dinoflagellate cyst taxa were identified in the sediment trap samples. The dinoflagellate cyst flux varied from similar to 600 to 336,200 cysts m(-2) day(-1), with an average of 20,000 cysts m(-2) day(-1). In general, dinoflagellate cyst flux and species composition reflected seasonal variation of water conditions in the Strait of Georgia. Throughout the study period, assemblages were dominated by cysts produced by heterotrophic dinoflagellates, such as Protoperidineaceae (Brigantedinium spp., Quinquecuspis concreta, and Protoperidinium americanum). The greatest abundance of cysts of the potentially toxic Alexandrium spp. was recorded in the spring of 1996. Our results demonstrate that cysts produced by heterotrophic dinoflagellates peak in June each year, during or following diatom blooms, as indicated by biogenic silica flux. Cysts produced by autotrophic taxa were most abundant during August-September. The total annual dinoflagellate cyst flux was lower in 1997 and 1998 than in 1996, mostly due to the bloom of Alexandrium spp. in 1996. Warmer sea-surface temperature and the early spring of 1998 had a positive effect on the production of both autotrophic and heterotrophic dinoflagellates as reflected in the cyst fluxes. Cyst assemblages from sediment trap samples were consistent with a cyst assemblage recovered from a core sample at the same site. (C) 2010 Elsevier B.V. All rights reserved.	[Pospelova, Vera; Esenkulova, Svetlana] Univ Victoria, Sch Earth & Ocean Sci, Bob Wright Ctr A405, Victoria, BC V8W 3V6, Canada; [Johannessen, Sophia C.; O'Brien, Mary C.; Macdonald, Robie W.] Inst Ocean Sci, Dept Fisheries & Oceans, Sidney, BC V8L 4B2, Canada	University of Victoria; Fisheries & Oceans Canada	Pospelova, V (通讯作者)，Univ Victoria, Sch Earth & Ocean Sci, Bob Wright Ctr A405, Victoria, BC V8W 3V6, Canada.	vpospe@uvic.ca	Macdonald, Robie/A-7896-2012	Esenkulova, Svetlana/0000-0003-3611-1944; Pospelova, Vera/0000-0003-4049-8133; Macdonald, Robie/0000-0002-1141-8520	Natural Sciences and Engineering Research Council of Canada (NSERC); ESSRF (Environmental Sciences Strategic Research Fund); Ecosystem Research Initiative (ERI) of the Department of Fisheries and Oceans	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); ESSRF (Environmental Sciences Strategic Research Fund); Ecosystem Research Initiative (ERI) of the Department of Fisheries and Oceans	Financial assistance was provided by the Natural Sciences and Engineering Research Council of Canada (NSERC) through Discovery and Shiptime grants to Dr. Vera Pospelova. Sediment trap collections and analyses were supported by the ESSRF (Environmental Sciences Strategic Research Fund) and Ecosystem Research Initiative (ERI) of the Department of Fisheries and Oceans. Special thanks are due to Dr. Jim Gower for sharing his data on monthly averaged values of sea surface temperature from buoy 46146. Additional thanks to Dr. Mike Foreman and Dr. John Morrison for help with obtaining data on Fraser river flow. Captain Brown and the crew of the marine sciences vessel John Strickland are thanked for their assistance during the sediment core sampling cruise. Thoughtful reviews of the manuscript by Drs. F. Marret and E. Thomas are sincerely appreciated.	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MAY	2010	75	1-4					17	37		10.1016/j.marmicro.2010.02.003	http://dx.doi.org/10.1016/j.marmicro.2010.02.003			21	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	609AS					2025-03-11	WOS:000278627800002
J	Pendea, IF; Costopoulos, A; Nielsen, C; Chmura, GL				Pendea, Ionel Florin; Costopoulos, Andre; Nielsen, Colin; Chmura, Gail Lois			A new shoreline displacement model for the last 7 ka from eastern James Bay, Canada	QUATERNARY RESEARCH			English	Article						Glacio-isostatic rebound; Relative sea level change; Chronosequence; Dinoflagellate cysts; Pollen; Tidal marsh; Isolation stratigraphy	RADIOCARBON AGE CALIBRATION; CAL KYR BP; HUDSON-BAY; NORTHWEST-TERRITORIES; SEA; ISOSTASY; QUEBEC; EARTH	The shoreline displacement history of the eastern James Bay lowlands in the last 7 ka has been investigated by means of AMS radiocarbon dating of sediments cored from wetlands. We present twelve radiocarbon dates on macrofossils from six sites spread along a gradient of increasing land age and elevation. Palynomorph analysis (pollen, spores, and dinoflagellate cysts) was used to define the isolation stratigraphy. During the last 7 ka the shoreline elevation has regressed at a decreasing rate. The rate of shoreline emergence was initially rapid (6.5 m/ 100 yr) between 6850 and 6400 cal yr BP then slowed down to 1.4-2 m/ 100 yr during the late Holocene. Examination of previous relative sea level data based upon mollusc shells reveals high levels of uncertainty that mask potential temporal variability. (C) 2010 University of Washington. Published by Elsevier Inc. All rights reserved.	[Pendea, Ionel Florin; Chmura, Gail Lois] McGill Univ, Dept Geog, Montreal, PQ H3A 2K6, Canada; [Pendea, Ionel Florin; Chmura, Gail Lois] Global Environm & Climate Change Ctr GEC3, Montreal, PQ H3A 2K6, Canada; [Costopoulos, Andre; Nielsen, Colin] McGill Univ, Dept Anthropol, Montreal, PQ H3A 2T7, Canada	McGill University; McGill University	Pendea, IF (通讯作者)，McGill Univ, Dept Geog, 805 Sherbrooke St W, Montreal, PQ H3A 2K6, Canada.	ionel.pendea@mail.mcgill.ca	Chmura, Gail/LNI-4648-2024	Chmura, Gail/0000-0001-7163-3903	Social Sciences and Humanities Research Council; Natural Sciences and Engineering Research Council of Canada.	Social Sciences and Humanities Research Council(Social Sciences & Humanities Research Council of Canada (SSHRC)); Natural Sciences and Engineering Research Council of Canada.(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This work is part of the European Science Foundation EUROCORES Program BOREAS and is supported by funds from the Social Sciences and Humanities Research Council and the Natural Sciences and Engineering Research Council of Canada. We thank the people of the Wemindji Cree First Nation, in particular Fred Asquabanes-kum and the Stewart family for their help and guidance during the field work. We also thank Jesse Sayles, Eby Heller, and Tom Heller for their most valuable help during the sampling campaign. In addition, we are indebted to our laboratory assistants-A. De Young, L Murchison, Z. Hudda, F. Syed, Y. Li, K. Yu, and N. Okere. We thank two anonymous reviewers for comments that helped us improve this paper.	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Res.	MAY	2010	73	3					474	484		10.1016/j.yqres.2010.02.001	http://dx.doi.org/10.1016/j.yqres.2010.02.001			11	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	594SH					2025-03-11	WOS:000277557200006
J	Wang, ZH; Xu, H; Zhan, Q; Saito, Y; He, ZF; Xie, JL; Li, X; Dong, YH				Wang, Zhanghua; Xu, Hao; Zhan, Qing; Saito, Yoshiki; He, Zhongfa; Xie, Jianlei; Li, Xiao; Dong, Yonghong			Lithological and palynological evidence of late Quaternary depositional environments in the subaqueous Yangtze delta, China	QUATERNARY RESEARCH			English	Article						Depositional system; Sedimentation rate; Sea-level fluctuation; East Asia monsoon	SEA-LEVEL RECORD; RIVER DELTA; SEDIMENTARY FACIES; LATE PLEISTOCENE; ASIAN MONSOON; HOLOCENE; POLLEN; VEGETATION; EVOLUTION; CLIMATE	AMS C-14 ages of post-glacial core sediments from the subaqueous Yangtze delta, along with sedimentary structures and distributions of grain size, pollen spores, and dinoflagellate cysts, show an estuarine depositional system from 13 to 8.4 cal ka BP and a deltaic system from 5.9 cal ka BP to the present. The estuarine system consists of intertidal to subtidal flat, estuarine, and estuarine-front facies, characterized by sand-mud couplets and a high sedimentation rate. The deltaic system includes nearshore shelf and prodelta mud featured by lower sedimentation rate, markedly fewer coastal wetland herbaceous pollens, and more dinoflagellate cysts. We explain the extremely high sedimentation rate during 9.2-8.4 cal ka BP at the study site as a result of rapid sea-level rise, high sediment load due to the unstable monsoonal climate, and subaqueous decrease of elevation from inner to outer estuary. A depositional hiatus occurred during 8.2-5.9 cal ka BP, the transition from estuarine to deltaic system, caused possibly by a shortage of sediment supply resulting from delta initiation in paleo-incised Yangtze valley and strong tidal or storm-related reworking in offshore areas. The subsequent development of deltaic system at the study site indicates accelerated progradation of Yangtze delta post-5.9 cal ka BP. (C) 2009 University of Washington. Published by Elsevier Inc. All rights reserved.	[Wang, Zhanghua] E China Normal Univ, State Key Lab Estuarine & Coastal Sci, Shanghai 200062, Peoples R China; [Saito, Yoshiki] AIST, Geol Survey Japan, Tsukuba, Ibaraki 3058597, Japan; [He, Zhongfa; Xie, Jianlei; Li, Xiao] Shanghai Geol Survey, Shanghai 200072, Peoples R China; [Xu, Hao; Zhan, Qing; Dong, Yonghong] E China Normal Univ, Dept Geog, Shanghai 200062, Peoples R China	East China Normal University; National Institute of Advanced Industrial Science & Technology (AIST); East China Normal University	Wang, ZH (通讯作者)，E China Normal Univ, State Key Lab Estuarine & Coastal Sci, Shanghai 200062, Peoples R China.	zhwang@geo.ecnu.edu.cn	Saito, Yoshiki/O-9087-2019; zhan, qingfeng/E-5019-2010	Wang, Zhanghua/0000-0003-1374-8328; SAITO, Yoshiki/0000-0003-3212-6356	Ministry of Science and Technology of China [SKLEC-2008KYYW02]; Chinese "111" Programme [B08022]; Asia-Pacific Network plan [ARCP2008-08CMY]; Asia-Africa Science Platform Program "Mega-Delta Watching in Asia"; Japan Society for the Promotion of Science; Laboratory of Marine Ecosystem and Biogeochemistry, State Oceanic Administration, China [LMEB200708]	Ministry of Science and Technology of China(Ministry of Science and Technology, China); Chinese "111" Programme(Ministry of Education, China - 111 Project); Asia-Pacific Network plan; Asia-Africa Science Platform Program "Mega-Delta Watching in Asia"; Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Laboratory of Marine Ecosystem and Biogeochemistry, State Oceanic Administration, China	Authors are grateful to Dr. Qin J. who identified carefully the pollen spores and dinoflagellate cysts, and two professional editors from ELSS, Inc. who edited kindly the manuscript. This work was supported by grants from the Ministry of Science and Technology of China (Grant No. SKLEC-2008KYYW02), the Chinese "111" Programme (Grant no. B08022), Asia-Pacific Network plan (Grant No. ARCP2008-08CMY), Asia-Africa Science Platform Program "Mega-Delta Watching in Asia", Japan Society for the Promotion of Science, and the open research program of Laboratory of Marine Ecosystem and Biogeochemistry, State Oceanic Administration, China (Grant No. LMEB200708).	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Res.	MAY	2010	73	3					550	562		10.1016/j.yqres.2009.11.001	http://dx.doi.org/10.1016/j.yqres.2009.11.001			13	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	594SH					2025-03-11	WOS:000277557200013
J	Leroy, SAG; Albay, M				Leroy, Suzanne A. G.; Albay, Meric			Palynomorphs of brackish and marine species in cores from the freshwater Lake Sapanca, NW Turkey	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Lake Sapanca; palaeogeography; palynomorphs; lake sediment; Black Sea; Sakarya Strait; fish translocation; dinocysts	DINOFLAGELLATE CYSTS; MARMARA; SEA; DISPERSAL; BLACK; PHYTOPLANKTON; ASSEMBLAGES; SEDIMENTS; HOLOCENE; QUALITY	Lake Sapanca, which is located on the Sakarya-Sapanca-Izmit corridor in NW Turkey, is a freshwater lake with numerous fish farms in its catchment. Palynological analyses including non-pollen palynomorphs of a short (38.5 cm) and a longer sediment core (586 cm), taken in the centre of the lake and dated in previous investigations, revealed the presence of brackish and marine palynomorphs. The longer sediment sequence shows the occurrence of Brigantedinium sp., lmpagidinium caspienense and Spituferites cruciformis from the base of the core at c. AD 580 years up to 300 cm depth at shortly after c. AD 910. A similar assemblage, but this time with the additional presence of dinoflagellate thecae and the acritarch, Radiosperma corbiferum, was found in the recent core, especially from AD 1986 until the present. Past connections between the Gulf of lzmit and the Black Sea, via the River Sakarya and Lake Sapanca, could be the origin of these two microfossil assemblages. Accidental re-introduction via fish translocation since the Roman times may have been a additional mechanism. The consequences of the survival of brackish and marine forms in a freshwater lake are discussed in terms of wider euryhalinity than has been suggested for those still poorly known organisms. (C) 2010 Elsevier B.V. All rights reserved.	[Leroy, Suzanne A. G.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Albay, Meric] Istanbul Univ, Fac Fisheries, Dept Inland Waters, TR-34470 Istanbul, Turkey	Brunel University; Istanbul University	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England.	suzanne.leroy@brunel.ac.uk	Leroy, Suzanne/D-3996-2009; , merbay/AAB-9694-2020		European Union, EC [EVG1-CT-2002-00069]	European Union, EC(European Union (EU)European Commission Joint Research Centre)	This study was funded by the European Union as part of the EC Project RELIEF (EVG1-CT-2002-00069). This is a contribution to IGCP 521 "Black Sea-Mediterranean Corridor during the last 30 ky: sea level change and human adaptation", working group 2 on Palynology. The authors are grateful to F. Marret (Liverpool University) for the confirmation of the identifications.	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Palaeobot. Palynology	MAY	2010	160	3-4					181	188		10.1016/j.revpalbo.2010.02.011	http://dx.doi.org/10.1016/j.revpalbo.2010.02.011			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	603NV		Green Submitted			2025-03-11	WOS:000278216200010
J	Crouch, EM; Mildenhall, DC; Neil, HL				Crouch, E. M.; Mildenhall, D. C.; Neil, H. L.			Distribution of organic-walled marine and terrestrial palynomorphs in surface sediments, offshore eastern New Zealand	MARINE GEOLOGY			English	Article						dinoflagellate cysts; pollen; surface sediments; New Zealand; Chatham Rise; Subtropical Front	DINOFLAGELLATE CYST DISTRIBUTION; NORTHERN NORTH-ATLANTIC; SUBTROPICAL CONVERGENCE REGION; SOUTHWEST PACIFIC-OCEAN; POLLEN DISTRIBUTION; DEEP-SEA; PHYTOPLANKTON ASSEMBLAGES; NORTHEASTERN AUSTRALIA; CONTINENTAL-MARGIN; SOUTHERN-OCEAN	Organic-walled dinoflagellate cyst (dinocyst) and terrestrial spore/pollen assemblages are analysed from 38 modern surface sediments offshore eastern New Zealand, from 33 to 54 S, water depths of 79 to 4680 m, and spanning the prominent Chatham Rise. The most diverse, abundant and best preserved marine and terrestrial assemblages are observed on the northern flank of Chatham Rise, coincident with the Subtropical Front region being an area of enhanced biological activity and primary productivity. Dinocyst assemblages are dominated by the gonyaulacoid (autotrophic) taxa Impagidinium, Nematospheropsis labyrinthus, Oper-culodinium centrocarpum, Spiniferites and peridinioid (heterotrophic) Brigantedinium. Taxa with preferences for cooler (e.g.. Selenopemphix antarctica) and warmer (e.g.. Impagidinium strialatum) water masses are identified in distribution records and canonical correspondence analysis. Of the nine environmental parameters measured, dinocyst assemblages were strongly correlated to sea-surface temperature (February) and chlorophyll a (autumn). Terrestrial spores and pollen dominate palynomorph assemblages in many sites, and primarily reflect the presence of lowland podocarp-broadleaf forest of onshore eastern New Zealand. Spores and bisaccate pollen dominate assemblages, with angiosperm pollen comprising up to 10% in the Chatham Rise area. Pollen from plants restricted to northern regions has been transported south via subtropical surface currents. This pilot study shows that palynomorph assemblages offshore New Zealand, including the high terrigenous input margin of eastern North Island, can provide suitable proxy records for characterisation of coeval marine and terrestrial changes through time. (C) 2009 Elsevier B.V. All rights reserved.	[Crouch, E. M.; Mildenhall, D. C.] GNS Sci, Lower Hutt 5040, New Zealand; [Neil, H. 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Geol.	APR 15	2010	270	1-4			SI		235	256		10.1016/j.margeo.2009.11.004	http://dx.doi.org/10.1016/j.margeo.2009.11.004			22	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	576IF					2025-03-11	WOS:000276137100018
J	Barski, M; Bojanowski, M				Barski, Marcin; Bojanowski, Maciej			Organic-walled dinoflagellate cysts as a tool to recognize carbonate concretions: an example from Oligocene flysch deposits of the Western Carpathians	GEOLOGICA CARPATHICA			English	Article						Oligocene; Western Carpathians; biostratigraphy; concretions; organic-walled dinoflagellate cysts	EOCENE	Carbonate concretions found within the Krosno shales (Polish Outer Carpathians) have formerly been interpreted as limestone exotics. Both the concretions and the host shales yield well preserved organic-walled dinoflagellate cysts. The dinoflagellate cyst assemblages provide valuable age-diagnostic information: they indicate a mid-Oligocene age and prove the concretionary origin of the carbonates. Detailed analysis of relative abundance, biodiversity and paleoecology of the dinoflagellates from concretions provides additional information on the sedimentary environment and the model of concretion formation.	[Barski, Marcin; Bojanowski, Maciej] Univ Warsaw, Inst Geol, PL-02089 Warsaw, Poland	Polish Geological Institute - National Research Institute; University of Warsaw	Barski, M (通讯作者)，Univ Warsaw, Inst Geol, Al Zwirki & Wigury 93, PL-02089 Warsaw, Poland.	marbar@uw.edu.pl; mcbojan@uw.edu.pl	Bojanowski, Maciej/H-1352-2012	Barski, Marcin/0000-0002-4102-3538; Bojanowski, Maciej/0000-0002-4735-1938				Bojanowski M., 2001, MINERAL SOC POL SPEC, V18, P15; 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; BURTAN J, 1984, B I GEOL, V346, P146; Dzulynski S., 1958, ANN SOC GEOL POL, V28, P205; Gedl P., 2000, Studia Geologica Polonica, V117, P69; GEDL P, 1999, PRZEGL GEOL, V47, P394; Gradstein FM, 2012, GEOLOGIC TIME SCALE 2012, VOLS 1 & 2, P1, DOI 10.1016/B978-0-444-59425-9.00001-9; Haczewski G., 1989, ANN SOC GEOL POL, V59, P435; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; JURKIEWICZ H, 1959, ACTA GEOL POL, V9, P17; KOSZARSKI L, 1985, CARPATHO BALKAN GEOL, V3, P16; Kothe A., 1990, GEOLOGISCHES JB A, V118, P1; KOZIKOWSKI H, 1956, B I GEOL, V110, P1; MASTELLA L, 1998, GEOL Q, V42, P173; MOCHNACKA K, 1972, ANN SOC GEOL POL, V42, P229; Narebski W., 1956, ROCZNIK POLSKIEGO TO, V26, P29; Poulsen N.E., 1990, Danmarks Geologiske Undersogelse Serie C, V10, P1; Powell A.J., 1992, P155; Pross Joerg, 2005, Palaeontologische Zeitschrift, V79, P53; SLACZKA A, 1962, GEOL Q, V4, P662; SLACZKA A, 1961, ANN SOC GEOL POL, V31, P129; Sluijs A, 2005, EARTH-SCI REV, V68, P281, DOI 10.1016/j.earscirev.2004.06.001; VANCOUVERING JA, 1981, PALAEOGEOGR PALAEOCL, V36, P321, DOI 10.1016/0031-0182(81)90111-5; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; Wilpshaar M, 1996, J GEOL SOC LONDON, V153, P553, DOI 10.1144/gsjgs.153.4.0553	26	17	17	0	7	SLOVAK ACAD SCIENCES GEOLOGICAL  INST	BRATISLAVA	DUBRAVSKA CESTA 9, BRATISLAVA, 840 05, SLOVAKIA	1335-0552	1336-8052		GEOL CARPATH	Geol. Carpath.	APR	2010	61	2					121	128		10.2478/v10096-010-0005-4	http://dx.doi.org/10.2478/v10096-010-0005-4			8	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	596RX		gold			2025-03-11	WOS:000277704100003
J	Grunert, P; Soliman, A; Harzhauser, M; Müllegger, S; Piller, WE; Roetzel, R; Rögl, F				Grunert, Patrick; Soliman, Ali; Harzhauser, Mathias; Muellegger, Stefan; Piller, Werner E.; Roetzel, Reinhard; Roegl, Fred			Upwelling conditions in the Early Miocene Central Paratethys Sea	GEOLOGICA CARPATHICA			English	Article						Early Miocene; Central Paratethys; upwelling; foraminifers; dinoflagellates; stable isotopes	DINOFLAGELLATE CYST DISTRIBUTION; EEMIAN HYDROGRAPHIC CONDITIONS; LIVE BENTHIC FORAMINIFERA; ISOTOPIC COMPOSITION; PLANKTONIC-FORAMINIFERA; GLOBIGERINA-BULLOIDES; MARINE-SEDIMENTS; STABLE-ISOTOPES; CARBON ISOTOPES; BALTIC SEA	Evidence for regional upwelling conditions in the Central Paratethys Sea is presented for mid-Burdigalian (early Ottnangian) times. The oceanographic phenomenon is detected in clay-diatomite successions along the steep escarpment of the Bohemian Massif in the eastern North Alpine Foreland Basin. Interpretations are based on a multi-proxy data-set including published sedimentological and paleontological data, newly performed stable isotope measurements (delta O-18, delta C-13) of foraminifers and bulk sediment samples, and analyses of dinoflagellate cyst assemblages. The revealed stable isotope values of planktonic foraminifers point to upwelling: low delta C-13 values indicate strong mixing of surface waters with rising nutrient-rich waters, high delta O-18 values reflect cool sea surface temperatures (SST). Temperature calculations give SSTs ranging from 10-14 degrees C. Cool SSTs and high productivity are additionally supported by bulk sediment analyses. Assemblages of dinoflagellate cysts indicate a distal-shelf environment with nutrient-rich waters. Westerly winds and tidal currents are discussed as potential driving forces behind the local upwelling event. As mid-Burdigalian geography favoured strong current patterns in the Central Paratethys as documented in the sedimentary record from the Rhone Basin to Hungary upwelling might have been a more common phenomenon in this epicontinental sea than currently known.	[Grunert, Patrick; Soliman, Ali; Muellegger, Stefan; Piller, Werner E.] Graz Univ, Inst Earth Sci Geol & Paleontol, A-8010 Graz, Austria; [Harzhauser, Mathias; Roegl, Fred] Nat Hist Museum Vienna, Geol Paleontol Dept, A-1014 Vienna, Austria; [Roetzel, Reinhard] Geol Survey Austria, A-1030 Vienna, Austria	University of Graz	Grunert, P (通讯作者)，Graz Univ, Inst Earth Sci Geol & Paleontol, Heinrichstr 26, A-8010 Graz, Austria.	patrick.grunert@uni-graz.at; ali.soliman@uni-graz.at; mathias.harzhauser@nhm-wien.ac.at; stefan.muellegger@uni-graz.at; werner.piller@uni-graz.at; reinhard.roetzel@geologie.ac.at; fred.roegl@nhm-wien.ac.at	Soliman, Ali/R-1583-2018	Piller, Werner E./0000-0003-2808-4720; Soliman, Ali/0000-0001-7366-4607; Harzhauser, Mathias/0000-0002-4471-6655; Grunert, Patrick/0000-0002-3633-8674	Commission for the Palaeontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	Commission for the Palaeontological and Stratigraphical Research of Austria (Austrian Academy of Sciences)	We want to thank Albrecht Leis (Johanneum Research, Graz) for carrying out part of the isotopic measurements. We are grateful to Fabrizio Lirer (Istitutio per l'Ambiente Marino Costiero, Naples, Italy), Michal Kovac (University of Bratislava, Slovakia), Andrea Kern (University of Vienna), Andreas Kroh and Oleg Mandic (both Natural History Museum Vienna) for many helpful discussions. Martin Head (Brock University, St. Catharines, Canada) and Lilian Svabenicka (Czech Geological Survey, Prague) are thanked for constructive comments which helped to improve the paper. Franz Topka (Natural History Museum Vienna) is thanked for assisting with the fieldwork. Financial support for this study was provided by the Commission for the Palaeontological and Stratigraphical Research of Austria (Austrian Academy of Sciences).	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Carpath.	APR	2010	61	2					129	145		10.2478/v10096-010-0006-3	http://dx.doi.org/10.2478/v10096-010-0006-3			17	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	596RX		gold			2025-03-11	WOS:000277704100004
J	Kholeif, SEA				Kholeif, Suzan E. A.			Holocene paleoenvironmental change in inner continental shelf sediments, Southeastern Mediterranean, Egypt	JOURNAL OF AFRICAN EARTH SCIENCES			English	Article						Dinoflagellate cyst; Palynomorph; Southeastern Mediterranean; Nile Delta; Holocene	WALLED DINOFLAGELLATE CYSTS; LEVANTINE BASIN; NILE CONE; SEA; EVOLUTION; CIRCULATION; PRESERVATION; ASSEMBLAGES	The palynology of marine sediments from CS Core taken on the inner continental shelf offshore Nile Delta, Southeastern Mediterranean, has been used to reconstruct the regional paleoenvironment during the past 5380 yr BP. This includes detailing the relative abundances of dinoflagellate cysts, acritarchs, prasinophytes and other algal spores, microforaminiferal linings, crustacean eggs, and fungal hyphae. The composition and ecological interpretation of the dinoflagellate cyst assemblages, acritarchs and other nonpollen palynomorphs is discussed. Concentrations of dinoflagellate cysts range from 5926 to 416 specimens per gram of sediment, and the most common taxa were Lingulodinium machaeropho rum, Operculodinium centrocarpum, Operculodinium israelianum, Polysphaeridium zoharyi, Spirnferites ramosus, Spiniferites mirabilis, Echinidinium transparantum and Protoperidinum nudum. The assemblages are like those on the Tunisian Shelf, but with more protoperidinioid cysts. It is concluded that the shelf sediments were deposited under suboxic bottom water conditions. A high nutrient supply to the area during the deposition of the CS Core sediments is evidenced by the strong significant correlation (R-values) between the nutrient-demanding species, L. machaerophorum and P. zoharyi, toxic species, total phosphorous percent (TP%) and total organic carbon percent (TOC%). These data suggest that Nile discharge from the Damietta Channel increased during the past 5830 yr BP and was accompanied by increases in fresh or brackish water algae and fungal hyphae. (C) 2009 Elsevier Ltd. All rights reserved.	NIOF, Alexandria, Egypt	Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF)	Kholeif, SEA (通讯作者)，NIOF, Alexandria, Egypt.	suzan_kholeif@yahoo.com						AKSU AE, 1995, MAR MICROPALEONTOL, V25, P1, DOI 10.1016/0377-8398(94)00026-J; BARTZOKAS A, 1991, J RIV METEOROLOGIA A, V51, P47; BETHOUX JP, 1989, DEEP-SEA RES, V36, P769, DOI 10.1016/0198-0149(89)90150-7; BIRKS H.J.B., 1980, QUATERNARY PALAEOECO; Boulter M. 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Afr. Earth Sci.	APR	2010	57	1-2					143	153		10.1016/j.jafrearsci.2009.08.001	http://dx.doi.org/10.1016/j.jafrearsci.2009.08.001			11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	576BV					2025-03-11	WOS:000276119600011
J	Hallegraeff, GM				Hallegraeff, Gustaaf M.			OCEAN CLIMATE CHANGE, PHYTOPLANKTON COMMUNITY RESPONSES, AND HARMFUL ALGAL BLOOMS: A FORMIDABLE PREDICTIVE CHALLENGE	JOURNAL OF PHYCOLOGY			English	Review						adaptation; algal blooms; climate change; continuous plankton recorder; ENSO; NAO; ocean acidification; range expansion	NORTH-ATLANTIC OSCILLATION; DINOFLAGELLATE CYSTS; RED TIDES; GYMNODINIUM-CATENATUM; SEDIMENTARY RECORD; POSITIVE FEEDBACK; ATMOSPHERIC CO2; FUTURE; PLANKTON; PACIFIC	Prediction of the impact of global climate change on marine HABs is fraught with difficulties. However, we can learn important lessons from the fossil record of dinoflagellate cysts; long-term monitoring programs, such as the Continuous Plankton Recorder surveys; and short-term phytoplankton community responses to El Nino Southern Oscillation (ENSO) and North Atlantic Oscillation (NAO) episodes. Increasing temperature, enhanced surface stratification, alteration of ocean currents, intensification or weakening of local nutrient upwelling, stimulation of photosynthesis by elevated CO2, reduced calcification through ocean acidification ("the other CO2 problem"), and heavy precipitation and storm events causing changes in land runoff and micronutrient availability may all produce contradictory species- or even strain-specific responses. Complex factor interactions exist, and simulated ecophysiological laboratory experiments rarely allow for sufficient acclimation and rarely take into account physiological plasticity and genetic strain diversity. We can expect: (i) range expansion of warm-water species at the expense of cold-water species, which are driven poleward; (ii) species-specific changes in the abundance and seasonal window of growth of HAB taxa; (iii) earlier timing of peak production of some phytoplankton; and (iv) secondary effects for marine food webs, notably when individual zooplankton and fish grazers are differentially impacted ("match-mismatch") by climate change. Some species of harmful algae (e.g., toxic dinoflagellates benefitting from land runoff and/or water column stratification, tropical benthic dinoflagellates responding to increased water temperatures and coral reef disturbance) may become more successful, while others may diminish in areas currently impacted. Our limited understanding of marine ecosystem responses to multifactorial physicochemical climate drivers as well as our poor knowledge of the potential of marine microalgae to adapt genetically and phenotypically to the unprecedented pace of current climate change are emphasized. The greatest problems for human society will be caused by being unprepared for significant range expansions or the increase of algal biotoxin problems in currently poorly monitored areas, thus calling for increased vigilance in seafood-biotoxin and HAB monitoring programs. Changes in phytoplankton communities provide a sensitive early warning for climate-driven perturbations to marine ecosystems.	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Phycol.	APR	2010	46	2					220	235		10.1111/j.1529-8817.2010.00815.x	http://dx.doi.org/10.1111/j.1529-8817.2010.00815.x			16	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	577LZ					2025-03-11	WOS:000276226100001
J	Bonnet, S; de Vernal, A; Hillaire-Marcel, C; Radi, T; Husum, K				Bonnet, Sophie; de Vernal, Anne; Hillaire-Marcel, Claude; Radi, Taoufik; Husum, Katrine			Variability of sea-surface temperature and sea-ice cover in the Fram Strait over the last two millennia	MARINE MICROPALEONTOLOGY			English	Article						Holocene; Nordic Seas; Fram Strait; Sea-surface conditions; Dinocyst	WALLED DINOFLAGELLATE CYSTS; ARTIFICIAL NEURAL-NETWORKS; NORWEGIAN-GREENLAND SEA; NORTHERN NORTH-ATLANTIC; NORDIC SEAS; HOLOCENE CLIMATE; LIVING COMMUNITIES; HIGH-LATITUDES; CAL KYR; WATER	A sediment core located on the West Spitzbergen margin in the Fram Strait (78 degrees 54.931'N, 6 degrees 46.005'E, water depth: 1497 m) was analyzed for its dinocyst content in order to reconstruct hydroclimatic variations of the last 2500 years. The relative abundance of dinocyst taxa and principal component analysis show a major transition at about 300 cal. years BP. It is characterized by the disappearance of thermophilic taxa Spiniferites mirabilis-hyperacanthus and Impagidinium sphaericum and the increase of polar-subpolar taxa Impagidinium pallidum and Pentapharsodinium dalei. Sea-surface temperature (SST) estimates suggest warmer conditions than present (anomaly similar to+2 degrees C) averaging at 7 degrees C in summer until 300 cal. years BP, although cooling pulses are recorded around 1700. 1500, 1200 and 800 cal. years BR The last 300 years were marked by a cooling from 7.6 to 3.5 degrees C and sea-ice cover increasing up to 7 months/yr. The results demonstrate that the Fram Strait area is sensitive to hydroclimatic variations, notably with respect to sea-ice and SSTs, which are linked to the relative strength of northward flow of North Atlantic waters to the East and southward outflow of cold and fresh waters from the Arctic Ocean. Based on our data, the warmest part of our record around 1320 cal. years BP is the only interval of the last 2500 years that provides a possible analogue for the modern post-AD 2000 interval, which is characterized by sea-ice free conditions. (C) 2009 Elsevier B.V. All rights reserved.	[Bonnet, Sophie; de Vernal, Anne; Hillaire-Marcel, Claude; Radi, Taoufik] Univ Quebec, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Montreal, PQ H3C 3P8, Canada; [Husum, Katrine] Univ Tromso, Dept Geol, N-9037 Tromso, Norway	University of Quebec; University of Quebec Montreal; UiT The Arctic University of Tromso	Bonnet, S (通讯作者)，Univ Quebec, Ctr Rech Geochim Isotop & Geochronol GEOTOP, Case Postale 8888,Succursale Ctr Ville, Montreal, PQ H3C 3P8, Canada.	s.bonnet@wanadoo.fr; devernal.anne@uqam.ca; hillaire-marcel.claude@uqam.ca; radi.taoufik@courrier.uqam.ca; katrine.husum@uit.no	Hillaire-Marcel, Claude/H-1441-2012; Husum, Katrine/HGD-4711-2022; Hillaire-Marcel, Claude/C-9153-2013; de Vernal, Anne/D-5602-2013	Hillaire-Marcel, Claude/0000-0002-3733-4632; Husum, Katrine/0000-0003-1380-5900; de Vernal, Anne/0000-0001-5656-724X	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT); Natural Sciences and Engineering Research Council of Canada (NSERC); University of Tromso; Research Council of Norway	Canadian Foundation for Climate and Atmospheric Sciences (CFCAS); Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); University of Tromso; Research Council of Norway(Research Council of Norway)	This study is a contribution to the Polar Climate Stability Network (PCSN) supported by the Canadian Foundation for Climate and Atmospheric Sciences (CFCAS). Additional support was provided by the Fonds Quebecois de la Recherche sur la Nature et les Technologies (FQRNT) and the Natural Sciences and Engineering Research Council of Canada (NSERC). It is also a contribution to the WARMPAST (Arctic Ocean Warming in the Past) project in the context of the International Polar Year (IPY no.36) supported by the University of Tromso and the Research Council of Norway. Thanks are also due to Maryse Henry (GEOTOP) for her help in the laboratory, Bassam Ghaleb (GEOTOP) for Lead-210 and Cesium-137 measurements and Robert Spielhagen for providing two AMS Carbon-14 dates. We appreciate constructive comments and suggestions from both reviewers: Jens Matthiessen and Marit-Solveig Seidenkrantz. 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Micropaleontol.	APR	2010	74	3-4					59	74		10.1016/j.marmicro.2009.12.001	http://dx.doi.org/10.1016/j.marmicro.2009.12.001			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	581PR					2025-03-11	WOS:000276536900001
J	Smayda, TJ; Trainer, VL				Smayda, T. J.; Trainer, V. L.			Dinoflagellate blooms in upwelling systems: Seeding, variability, and contrasts with diatom bloom behaviour	PROGRESS IN OCEANOGRAPHY			English	Review							SHORT-TERM VARIABILITY; HARMFUL ALGAL BLOOMS; MARINE PLANKTONIC DIATOM; GYMNODINIUM-CATENATUM; RED TIDE; RESTING SPORES; ANCHOR STATION; CHAETOCEROS-PSEUDOCURVISETUS; ENVIRONMENTAL-CONTROL; PHYTOPLANKTON BLOOMS	The influence of diatom bloom behaviour, dinoflagellate life cycles, propagule type and upwelling bloom cycles on the seeding of dinoflagellate blooms in eastern boundary current upwelling systems is evaluated. Winter-spring diatom bloom behaviour is contrasted with upwelling bloom behaviour because their phenology impacts dinoflagellate blooms. The winter-spring diatom bloom is usually sustained, whereas the classical upwelling diatom bloom occurs as a series of separate, recurrent mini-blooms intercalated by upwelling-relaxation periods, during which dinoflagellates often bloom. Four sequential wind-regulated phases characterize upwelling cycles, with each phase having different effects on diatom and dinoflagellate bloom behaviour: bloom "spin up", bloom maximum, bloom "spin down", and upwelling relaxation. The spin up - bloom maximum is the period of heightened diatom growth; the spin down - upwelling-relaxation phases are the periods when dinoflagellates often bloom. The duration, intensity and ratio of the upwelling and relaxation periods making up upwelling cycles determine the potential for dinoflagellate blooms to develop within a given upwelling cycle and prior to the subsequent "spin up" of upwelling that favours diatom blooms. Upwelling diatoms and meroplanktonic dinoflagellates have three types of propagules available to seed blooms: vegetative cells, resting cells and resting cysts. However, most upwelling dinoflagellates are holoplanktonic, which indicates that the capacity to form resting cysts is not an absolute requirement for growth and survival in upwelling systems. The long-term (decadal) gaps in bloom behaviour of Gymnodinium catenatum and Lingulodinium polyedrum, and the unpredictable bloom behaviour of dinoflagellates generally, are examined from the perspective of seeding strategies. Mismatches between observed and expected in situ bloom behaviour and resting cyst dynamics are common among upwelling dinoflagellates. This disassociation suggests unrecognized upwelling system factors that fall within the physical-chemical-biological domain are more important than life cycle in selecting dinoflagellates species having the survival-seeding strategies and ecophysiological adaptations required for growth in physically robust upwelling systems. It is conjectured that diatom life cycles, as a group, are geared towards exploiting seeding opportunities, whereas dinoflagellates have evolved life-cycle behaviour more attuned to survival. The role of ecological dormancy and ecological release from bloom inhibition underlying dinoflagellate bloom irregularity is considered. The expectation that the dinoflagellate species selected to bloom from among the common upwelling flora would be the same in all eastern boundary upwelling systems is not realized. (C) 2010 Elsevier Ltd. All rights reserved.	[Smayda, T. J.] Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA; [Trainer, V. L.] NOAA, NW Fisheries Sci Ctr, Seattle, WA 98112 USA	University of Rhode Island; National Oceanic Atmospheric Admin (NOAA) - USA	Smayda, TJ (通讯作者)，Univ Rhode Isl, Grad Sch Oceanog, Kingston, RI 02881 USA.	tsmayda@gso.uri.edu	Trainer, Vera/AAE-9306-2022	, Vera/0009-0005-9585-6753	EPA [R83-2443]; STAR research	EPA(United States Environmental Protection Agency); STAR research	This analysis was aided by the EPA's Science to Achieve Results (STAR) Program, supported by EPA Grant No. R83-2443 awarded to Dr. Smayda. STAR is managed by the EPA's Office of Research and Development (ORD), National Center for Environmental Research and Quality Assurance (NCERQA). STAR research supports the Agency's mission to safeguard human health and the environment. The comments of two anonymous reviewers were very helpful in revising the original draft.	Allen W E, 1933, Science, V78, P12, DOI 10.1126/science.78.2010.12; Allen W. 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Oceanogr.	APR-MAY	2010	85	1-2			SI		92	107		10.1016/j.pocean.2010.02.006	http://dx.doi.org/10.1016/j.pocean.2010.02.006			16	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	608UZ					2025-03-11	WOS:000278612800006
J	Verleye, TJ; Louwye, S				Verleye, Thomas J.; Louwye, Stephen			Late Quaternary environmental changes and latitudinal shifts of the Antarctic Circumpolar Current as recorded by dinoflagellate cysts from offshore Chile (41°S)	QUATERNARY SCIENCE REVIEWS			English	Article							SEA-SURFACE CONDITIONS; ATLANTIC THERMOHALINE CIRCULATION; NORTHERN NORTH-ATLANTIC; SOUTHERN-OCEAN; RAINFALL VARIABILITY; MARINE-SEDIMENTS; CLIMATE HISTORY; RESTING CYSTS; ASSEMBLAGES; SALINITY	The late Quaternary organic-walled dinoflagellate cyst record of Site 1233 (41 degrees S, offshore Chile) was studied with a similar to 200 year resolution spanning the last 25,000 years The study provides the first continuous record of sub-recent and recent dinoflagellate cysts in the Southeast (SE) Pacific. Major changes in the composition of the cyst association, cyst concentration and morphology of Operculodinium centrocatpum reflect changes in sea surface temperature (SST), sea surface salinity (SSS), palaeoproductivity and upwelling intensity. These changes can be associated with latitudinal shifts of the circumpolar frontal systems. The high cyst concentration, high Brigantedinium spp abundances, low species diversity and the occurrence of certain cold water species are supportive for a 7-10 degrees equatorward shift of the Antarctic Circumpolar Current (ACC) during the coldest phase of the List Glacial Maximum (LGM) between 25 and 211 cal ka BP Deglacial warming initiated at similar to 18.6 cal ka BP Termination 1(18 6-11.1 cal ka BP) is interrupted by an unstable period of extreme seasonality, rather than a cooling event, between 14.4 and 13 2 cal ka BP, synchronous with the Antarctic Cold Reversal (ACR). The Holocene Maximum is observed between 11 6 and 98 cal ka BP and is typified by the most southward position of the northern margin of the ACC A cooling phase occurred during the early Holocene (until similar to 7 cal ka BP) and during the last similar to 0 8 ka. Our data indicates that the SE Pacific (41 degrees S) climate has been influenced over the whole record by changes in the Southern Hemisphere (SH) high-latitudes, while during the mid to late Holocene, also a tropical forcing mechanism was involved, including the El Nino Southern Oscillation and the variable Hadley cell intensity Furthermore, this study showed a relationship between the variable morphology of the spines/processes of O. centrocarpum and the combined variation of sea surface salinity and temperature (SSS/SST-ratio). (C) 2010 Elsevier Ltd All rights reserved	[Verleye, Thomas J.; Louwye, Stephen] Univ Ghent, Dept Soil Sci & Geol, Res Unit Palaeontol, B-9000 Ghent, Belgium	Ghent University	Verleye, TJ (通讯作者)，Univ Ghent, Dept Soil Sci & Geol, Res Unit Palaeontol, Krijgslaan 281,S8-WE13, B-9000 Ghent, Belgium.		Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313	Institute for the Encouragement of Innovation through Science and Technology in Flanders (WIT)	Institute for the Encouragement of Innovation through Science and Technology in Flanders (WIT)	T. Blunier, X. Boes, J Kaiser, A. Koutavas, F Lamy and L Thompson are thanked for providing data and for the instructive discussions. The interesting discussions with V. Pospelova and IC. Mertens are greatly acknowledged We are grateful to H. Bauch, and two anonymous reviewers for the critical remarks and suggestions which greatly improved the manuscript. Financial support to the first author was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders (WIT). Samples for this study were kindly provided by the Ocean Drilling Program (ODP).	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Sci. Rev.	APR	2010	29	7-8					1025	1039		10.1016/j.quascirev.2010.01.009	http://dx.doi.org/10.1016/j.quascirev.2010.01.009			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	584JY					2025-03-11	WOS:000276749200015
J	Vasil'eva, ON; Musatov, VA				Vasil'eva, O. N.; Musatov, V. A.			Paleogene biostratigraphy of the North Caspian region based on dinocysts and nannofossils from the Novouzensk borehole. Article 2: Biotic events and paleoecological settings	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Paleocene; Eocene; North Caspian region; dinocysts; nannoplankton; biotic events; rhythms; paleoecology	OLIGOCENE DINOFLAGELLATE CYSTS; SEA-LEVEL CHANGE; PALEOCENE; EOCENE; ENGLAND	The relatively complete late Danian-initial Lutetian succession of biotic events, which are suitable to serve as biostratigraphic reference levels for interregional correlations are defined in the section of the Novouzensk reference borehole based on dinocyst and nannoplankton assemblages. The analysis of palynological and nannofossil assemblages allows dynamics of basin development and sea-level fluctuations to be traced. Three major stages reflecting different sedimentation regimes are established in the borehole section: (1) Danian with terrigenous-carbonate sedimentation regime corresponding to the Algai and Tsyganovka formations; (2) Selandian-Thanetian (initial Eocene included) characterized largely by siliceous-terrigenous sediments of the Syzran, Novouzensk, and, partly, Bostandyk formations; (3) Ypresian-Lutetian with the carbonate-terrigenous sedimentation regime corresponding to the upper part of the Ypresian Bostandyk and Lutetian Kopterek formations. The composition of dinoflagellate and nannoplankton assemblages characterizes the North Caspian basin as an internal largely shallow sea with a changeable temperature regime. The paleoecological analysis of phytocoenoses made it possible to define basin fluctuations comparable with third-order rhythms. Four Danian rhythms definable in the Algai and Tsyganovka formations indicate conditions of an open warm-water basin. Dynamics of the step-wise shoaling of the basin was characteristic of the Selandian-early Thanetian ages with subsequent restoration of the marine regime in the late Thanetian. The Syzran Formation corresponds to two Selandian rhythms, which were formed in shallower settings of the restricted sea basin. Four Thanetian rhythms are established in the Novouzensk Formation. The early Thanetian basin was characterized by the shallowest disturbed marine conditions, which were followed by the restored normal marine regime in the late Thanetian. Six Ypresian rhythms correspond to the Bostandyk Formation (Yp-0, Yp-1, Yp-5-Yp-8) reflecting transition from initial Ypresian coastal (Yp-0, Yp-1) to normal marine conditions during the Yp-5 rhythm. The early (Yp-2-Yp-4) and late (Yp-9-Yp-10) Ypresian corresponded to the sedimentation break. Most abundant and diverse microbiotic assemblages characteristic of the Yp-7 rhythm are correlative with the EECO event. The marly Kopterek Formation corresponding to the early Lutetian rhythm (Lu-1) is characterized by diverse thermophilic biota.	[Vasil'eva, O. N.] Russian Acad Sci, Ural Branch, Inst Geol & Geochem, Ekaterinburg 620219, Russia; [Musatov, V. A.] Nizhne Volzhskii Res Inst Geol & Geophys, Saratov, Russia	Russian Academy of Sciences	Vasil'eva, ON (通讯作者)，Russian Acad Sci, Ural Branch, Inst Geol & Geochem, Pochtovyi Per 7, Ekaterinburg 620219, Russia.	vasilyeva@igg.uran.ru; vmusatov@nvniigg.san.ru	Васильева, Ольга/B-6221-2018		Russian Foundation for Basic Research [06-05-64780]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government)	This work was supported by the Russian Foundation for Basic Research, project no. 06-05-64780.	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N., 2008, LITOSFERA, P18; VASILEVA ON, STRATIGR GE IN PRESS; VASILEVA ON, 2008, LITOSFERA, P121; Wall D., 1977, MAR MICROPALEONTOL, V30, P319; WILLIAMS GL, 2004, 189 SCI RES ODP LEG; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412	49	2	2	0	7	PLEIADES PUBLISHING INC	MOSCOW	PLEIADES PUBLISHING INC, MOSCOW, 00000, RUSSIA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	APR	2010	18	2					179	199		10.1134/S0869593810020061	http://dx.doi.org/10.1134/S0869593810020061			21	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	587XB					2025-03-11	WOS:000277028300006
J	Tang, XH; Yu, RC; Zhang, QC; Wang, YF; Yan, T; Zhou, MJ				Tang Xianghai; Yu Rencheng; Zhang Qingchun; Wang Yunfeng; Yan Tian; Zhou Mingjiang			Molecular phylogenetic analysis of dinoflagellate Scrippsiella trochoidea isolated from the East Asian waters	CHINESE JOURNAL OF OCEANOLOGY AND LIMNOLOGY			English	Article						Scrippsiella trochoidea; phylogeny; rDNA; molecular systematics	SOUTH CHINA SEA; SPECIES COMPLEX DINOPHYCEAE; ALEXANDRIUM DINOPHYCEAE; POPULATION-DYNAMICS; RECENT SEDIMENTS; NORTHEAST JAPAN; RIBOSOMAL DNA; ONAGAWA BAY; DAYA BAY; CYSTS	Previous studies found intraspecific diversity in Scrippsiella trochoidea A. R. Loeblich III, a widely distributed calcareous cyst-producing dinoflagellate. In this study, three strains (ST-1, ST-D6 and ST-K) of S. trochoidea isolated from the East Asian waters were studied, together with other geographical strains, to resolve their phylogenetic relationships. For the three East Asian isolates, two highly diverse regions of nuclear-encoded ribosomal DNA (rDNA), the 5.8S rDNA and its flanking internal transcribed spacers 1 and 2, and the 5' portion of the large-subunit rDNA (encompassing the "D1" and "D2" domains) were sequenced. Homologous sequences from other geographical isolates were selected from the GenBank database and the phylogenetic relationships were inferred from the molecular data of these strains. Strains of S. trochoidea were found to cluster into three major clades (STR1, STR2 and STR3), as reported in previous studies. Two of the three strains ST-1 and ST-K, were grouped in clade STR2, the other strain, ST-D6, belonged to clade STR3. The intraspecific diversity of S. trochoidea in East Asian waters makes it necessary to carry out phylogenetic investigations in combination with data of biogeography, population dynamics, and life cycle on the ecophysiology of a region.	[Tang Xianghai; Yu Rencheng; Zhang Qingchun; Wang Yunfeng; Yan Tian; Zhou Mingjiang] Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China; [Tang Xianghai; Zhang Qingchun] Chinese Acad Sci, Grad Sch, Beijing 100039, Peoples R China	Chinese Academy of Sciences; Institute of Oceanology, CAS; Chinese Academy of Sciences; University of Chinese Academy of Sciences, CAS	Yu, RC (通讯作者)，Chinese Acad Sci, Inst Oceanol, Key Lab Marine Ecol & Environm Sci, Qingdao 266071, Peoples R China.	rcyu@ms.qdio.ac.cn	Yu, Rencheng/J-4450-2017	Yu, Rencheng/0000-0001-6430-9224	Chinese Academy of Sciences [KZCX2-YW-208]; National Natural Science Foundation of China [40676072]	Chinese Academy of Sciences(Chinese Academy of Sciences); National Natural Science Foundation of China(National Natural Science Foundation of China (NSFC))	Supported by the Knowledge Innovation Program of Chinese Academy of Sciences (No. KZCX2-YW-208) and National Natural Science Foundation of China (No. 40676072)	Adachi M, 1996, J PHYCOL, V32, P424, DOI 10.1111/j.0022-3646.1996.00424.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; Gottschling M, 2005, MOL PHYLOGENET EVOL, V36, P444, DOI 10.1016/j.ympev.2005.03.036; Gottschling M, 2005, EUR J PHYCOL, V40, P207, DOI 10.1080/09670260500109046; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; ISHIKAWA A, 1994, MAR BIOL, V119, P39, DOI 10.1007/BF00350104; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; John U, 2003, MOL BIOL EVOL, V20, P1015, DOI 10.1093/molbev/msg105; Kim E, 2004, MICROB ECOL, V48, P521, DOI 10.1007/s00248-004-0219-z; Lilly EL, 2007, J PHYCOL, V43, P1329, DOI 10.1111/j.1529-8817.2007.00420.x; Logares R, 2007, MICROB ECOL, V53, P549, DOI 10.1007/s00248-006-9088-y; Montresor M, 2003, PHYCOLOGIA, V42, P56, DOI 10.2216/i0031-8884-42-1-56.1; Park J.S., 1989, P37; Qi YZ, 2004, HYDROBIOLOGIA, V512, P209, DOI 10.1023/B:HYDR.0000020329.06666.8c; SAKO Y, 1990, TOXIC MARINE PHYTOPLANKTON, P320; 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; Wang SF, 2008, HYDROBIOLOGIA, V596, P79, DOI 10.1007/s10750-007-9059-4; Wang Y, 2008, HARMFUL ALGAE, V7, P65, DOI 10.1016/j.hal.2007.05.005; Wang ZH, 2004, PHYCOL RES, V52, P387, DOI 10.1111/j.1440-183.2004.00356.x; Wang ZH, 2004, PHYCOL RES, V52, P396, DOI 10.1111/j.1440-1835.2004.tb00348.x; Wang ZH, 2004, MAR ECOL-P S Z N I, V25, P289, DOI 10.1111/j.1439-0485.2004.00035.x; Wang ZH, 2007, J PLANKTON RES, V29, P209, DOI 10.1093/plankt/fbm008; Wang ZH, 2006, J MARINE SYST, V62, P85, DOI 10.1016/j.jmarsys.2006.04.008; White TJ., 1990, PCR PROTOCOLS GUIDE, P315; [徐宁 Xu Ning], 2004, [海洋环境科学, Marine Environmental Science], V23, P36	27	5	6	4	17	SCIENCE PRESS	BEIJING	16 DONGHUANGCHENGGEN NORTH ST, BEIJING, 100717, PEOPLES R CHINA	0254-4059	1993-5005		CHIN J OCEANOL LIMN	Chin. J. Oceanol. Limnol.	MAR	2010	28	2					323	328		10.1007/s00343-010-9288-7	http://dx.doi.org/10.1007/s00343-010-9288-7			6	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	571UN					2025-03-11	WOS:000275781400018
J	Feist-Burkhardt, S; Pross, J				Feist-Burkhardt, Susanne; Pross, Joerg			Dinoflagellate cyst biostratigraphy of the Opalinuston Formation (Middle Jurassic) in the Aalenian type area in southwest Germany and north Switzerland	LETHAIA			English	Article						Aalenian; biostratigraphy; dinoflagellate cysts; Germany; Jurassic; Switzerland; Toarcian	SEDIMENTS; BAJOCIAN	In order to provide a detailed dinoflagellate cyst stratigraphy of the Lower Aalenian Opalinuston Formation from the Aalenian type area, 68 samples from four boreholes and one outcrop section were analysed. The sample localities are Hausen an der Fils and Wittnau in southwest Germany, Weiach in north Switzerland and Mont Russelin in the Swiss Jura Mountains. Dinoflagellate cyst assemblages were recovered from the Late Toarcian Aalensis Zone to the Late Aalenian Murchisonae Zone. The samples yielded rich, well-preserved and diverse assemblages with 51 dinoflagellate cyst taxa identified in total. The dinoflagellate cyst distribution data obtained from this study allow a high-resolution biostratigraphical subdivision of the lowermost Middle Jurassic Opalinuston Formation into four palynostratigraphical units. First and last occurrences, acmes and consistent presence of the species Batiacasphaera sp. A, Evansia cf. granochagrinata, Kallosphaeridium praussii, Nannoceratopsis triangulata, Phallocysta? frommernensis and Wallodinium laganum were selected as the criteria for defining these units. The obtained high-resolution palynostratigraphical scheme provides a basis for establishing and further refining early Middle Jurassic biostratigraphy in the Boreal and Tethyan realms.	[Feist-Burkhardt, Susanne] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Pross, Joerg] Goethe Univ Frankfurt, Palaeoenvironm Dynam Grp, Inst Geosci, D-60438 Frankfurt, Germany	Natural History Museum London; Goethe University Frankfurt	Feist-Burkhardt, S (通讯作者)，Nat Hist Museum, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.	s.feist-burkhardt@nhm.ac.uk; joerg.pross@em.uni-frankfurt.de	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242				[Anonymous], 2008, GEOLOGY CENTRAL EURO, DOI DOI 10.1144/CEV2P; [Anonymous], 1992, ARCTIC GEOLOGY PETRO; 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; BLASI HR, 1987, ECLOGAE GEOL HELV, V80, P415; Bloos G, 2005, NEWSL STRATIGR, V41, P263, DOI 10.1127/0078-0421/2005/0041-0263; BUJAK JP, 1977, STRATIGRAPHIC MICROP, P321; Burkhalter RM, 1996, ECLOGAE GEOL HELV, V89, P875; Burkhalter RM, 1997, ECLOGAE GEOL HELV, V90, P269; BUTLER N, 2005, RECENT DEV APPL BIOS, P43; Cresta S, 2001, EPISODES, V24, P166; DAVIES E H, 1985, Palynology, V9, P105; de Vains G., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P451; DIETL G., 1977, STUTTGARTER BEITRA B, V25, P1; DIETL G, 1977, STUTTGARTER BEITRA B, V30, P1; Engel T., 1908, Geognostischer Wegweiser durch Wurttemberg, V3rd; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Feist-Burkhardt S, 1999, BULL CENT RECH ELF E, V22, P103; Feist-Burkhardt S, 2001, NEUES JAHRB GEOL P-A, V219, P33, DOI 10.1127/njgpa/219/2001/33; Feist-Burkhardt Susanne, 1995, Palynology, V19, P211; FEISTBURKHARDT S, 1990, B CENT RECH EXPL, V14, P611; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Geyer O. F., 1984, SAMMLUNG GEOLOGISCHE, V67; Geyer OF, 1986, GEOLOGIE BADEN WURTT; GORIN GE, 1990, REV PALAEOBOT PALYNO, V65, P349, DOI 10.1016/0034-6667(90)90085-W; Goy A., 1996, INF GEOL LANDESAMT B, V8, P43; Helby R., 2004, Updated Jurassic and Early Cretaceous dinocyst zonation NWS Australia; Helby R.J., 1987, MEM ASS AUSTRALAS PA, V4, P1; Klocker P., 1967, Bericht der Naturforschenden Gesellschaft zu Freiburg i Br, V57, P69; Klocker P., 1966, Bericht der Naturforschenden Gesellschaft zu Freiburg i Br, V56, P209; Koppelhus Eva B., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P723; Koppelhus Eva B., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P777; Koppelhus Eva Bundgaard, 1994, Palynology, V18, P139; MacRae RA, 1996, CAN J BOT, V74, P1687, DOI 10.1139/b96-205; Matter A., 1988, GEOLOGISCHE BERICHTE, V6, P1; Ogg JG., 2004, A geologic time scale 2004, P307; Ohmert W., 1994, Miscellanea Servizio Geologico Nazionale, V5, P33; OPPEL A., 1862, PALAEONTOLOGISCHE MI, V1, P127; Palliani RB, 1997, B CENT RECH EXPL, V21, P107; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; PRAUSS M, 1989, Palaeontographica Abteilung B Palaeophytologie, V214, P1; Prauss M., 1987, Neues Jahrbuch fuer Geologie und Palaeontologie Abhandlungen, V176, P129; PRAUSS M, 1991, GEOL SOC LOND SPEC P, V58, P335; QUATTROCCHIO ME, 1990, REV PALAEOBOT PALYNO, V65, P319, DOI 10.1016/0034-6667(90)90082-T; Quenstedt F.A, 1886, Die Ammoniten des Schwabischen Jura. 2. 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Verlag & Lithographie der Expedition des Werkes Unsere Zeit; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]	77	20	21	0	17	WILEY	HOBOKEN	111 RIVER ST, HOBOKEN 07030-5774, NJ USA	0024-1164	1502-3931		LETHAIA	Lethaia	MAR	2010	43	1					10	31		10.1111/j.1502-3931.2009.00170.x	http://dx.doi.org/10.1111/j.1502-3931.2009.00170.x			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	548VW					2025-03-11	WOS:000273998200002
J	Esper, O; Gersonde, R; Kadagies, N				Esper, Oliver; Gersonde, Rainer; Kadagies, Nicole			Diatom distribution in southeastern Pacific surface sediments and their relationship to modern environmental variables	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Diatoms; Marine sediments; Amundsen Sea; Bellingshausen Sea; Antarctic Circumpolar Current; Canonical redundancy analysis	SOUTHERN-OCEAN SEDIMENTS; SEASONAL SEA-ICE; BELLINGSHAUSEN SEA; BRANSFIELD STRAIT; DINOFLAGELLATE CYSTS; ANTARCTIC WATERS; BIOGENIC SILICA; INDIAN SECTOR; AMUNDSEN SEA; ROSS SEA	The quantitative analysis of diatom assemblages preserved in 52 samples from the Bellingshausen and the Amundsen Seas provides the first comprehensive view on the distribution of diatoms in surface sediments of the eastern and central Pacific sector of the Southern Ocean. On a latitudinal transect along 120 degrees W, diatom valve accumulation rates (AR) reach maximum values (8-10 x 10(8) valves m(-2) yr(-1)) in a zone extending over ca. 900 km between the Antarctic Polar Front and the maximum average winter sea ice extent and exceed those ARs obtained from an eastern transect along 90 degrees W by one order of magnitude. Lowest diatom concentrations (1-3 x 10(6) valves g(-1)) were encountered in sediments of the Sea Ice Zone, affected by winter and summer sea ice. The accumulation rate pattern of the most abundant diatom Fragilariopsis kerguelensis (>50% abundance in 47 samples) mirrors the pattern of the total diatom valve AR and the biogenic silica (BSi) AR, making F. kerguelensis the major contributor to the BSi preserved at the sea floor. Relative abundances of diatom species and species groups were statistically compared with a selection of environmental variables, such as the mean summer sea surface temperature and salinity, mean annual surface nutrient concentration (nitrate, phosphate, silicon), mean annual water column stratification, mixed layer depth in summer, and mean summer and winter sea ice concentrations. Polynomial canonical redundancy analysis (RDA) revealed the biogeographic distribution of diatom species had the strongest relationship with summer sea surface temperature (SSST) out of the nine tested environmental variables. This relationship accounted for 69.6% of the total variance of the diatom distribution, with 29.7% explained by the first gradient (significantly correlated to SSST with r(2) = 0.941) and 15.6% explained by the second gradient (correlated to both summer and winter sea ice and silicon concentration). Azpeitia tabularis, Hemidiscus cuneiformis and Roperia tesselata were associated with warmer water conditions (>4 degrees C), whereas Fragilariopsis curta, F. separanda, F. rhombica and Thalassiosira gracilis were correlated with cold SSST (<1.5 degrees C). Under the second gradient relationship, Actinocyclus actinochilus and F. curta were the most important diatoms representative of the diatom distribution in relation to the observed mean summer and winter sea ice concentrations. Confirming these environmental relationships is crucial for the development of reference data sets used in quantitative estimations of palaeoclimatic and palaeoceanographic conditions with statistical methods. This new data set represents the first modernised treatment of diatom remains from the SE Pacific Ocean and generally supports the use of a circum-polar database for the determination of summer SST, sea ice and potentially biogenic silica distribution of the Southern Ocean back into the Late Quaternary. (C) 2010 Elsevier B.V. All rights reserved.	[Esper, Oliver; Gersonde, Rainer; Kadagies, Nicole] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Esper, O (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Columbusstr, D-27568 Bremerhaven, Germany.	Oliver.Esper@awi.de		Esper, Oliver/0000-0002-4342-3471	German Israel Foundation (GIF); DFG-Research Center/Cluster of Excellence "The Ocean in the Earth System" in Bremen, Germany	German Israel Foundation (GIF)(German-Israeli Foundation for Scientific Research and Development); DFG-Research Center/Cluster of Excellence "The Ocean in the Earth System" in Bremen, Germany(German Research Foundation (DFG))	The authors are grateful to the anonymous reviewers for constructive reviews and comments on the manuscript We thank R. Crawford, G. Cortese and CL De La Rocha for useful comments and a fruitful discussion. We acknowledge the technical assistance of U. Bock and R. Cordelair. This study was supported by grants from the German Israel Foundation (GIF) and the DFG-Research Center/Cluster of Excellence "The Ocean in the Earth System" in Bremen, Germany.	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Paleoclimatol. Paleoecol.	MAR 1	2010	287	1-4					1	27		10.1016/j.palaeo.2009.12.006	http://dx.doi.org/10.1016/j.palaeo.2009.12.006			27	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	576WH					2025-03-11	WOS:000276180100001
J	Geraga, M; Ioakim, C; Lykousis, V; Tsaila-Monopolis, S; Mylona, G				Geraga, M.; Ioakim, Chr.; Lykousis, V.; Tsaila-Monopolis, St; Mylona, G.			The high-resolution palaeoclimatic and palaeoceanographic history of the last 24,000 years in the central Aegean Sea, Greece	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Late Quaternary; Eastern Mediterranean; Climatic variability; Planktonic foraminifera; Pollen; Dinoflagellate	DINOFLAGELLATE CYST ASSEMBLAGES; MILLENNIAL-SCALE; MEDITERRANEAN SEA; ATMOSPHERIC CIRCULATION; PLANKTONIC-FORAMINIFERA; CLIMATIC VARIABILITY; SURFACE TEMPERATURE; SAPROPEL FORMATION; ORGANIC-MATTER; COASTAL-PLAIN	The palaeoclimatic and palaeoceanographic history of the N. Skyros Basin, central Aegean Sea, was studied based on the planktonic foraminifera and the stable isotopes obtained from the sediments of a sediment core selected in this area. The data were further supported by pollen and dinoflagellate cyst data. The data correspond to a mean sampling interval of about 170 yrs and cover the last 24,000 yrs. The variations in almost all of the records showed synchronicity, suggesting the occurrence of a series of climatic changes. The most pronounced climatic changes during the last glacial and late glacial periods are as follows: (i) a brief relatively warm and humid event at 19.5 kyr, (ii) two cold spells, at 17 ka and 15.8 ka, (iii) the climatic oscillation during the GI-1 event, and (iv) the development of the Younger Dryas (GS-1) event in two phases. During the Holocene epoch, five brief cold and/or arid phases occurred, at around 10.5 ka, 8.2 ka, 7 ka to 6 ka, 5.0 ka and 3.0 ka. The most warm and humid Holocene events correspond to the time of the deposition of the two sapropel sublayers: S1a and S1b. Almost all of these brief climatic changes are coeval with equivalent changes in high northern latitude areas and with changes in the intensity of the Siberian High, suggesting a climatic link between the studied area and the high-latitude areas. The prevalence of Holocene arid events, which coincide with equivalent events recorded in North-Eastern Africa and the Middle East, suggests a climatic link between the eastern and south-eastern regions of the Mediterranean Sea. (C) 2010 Elsevier B.V. All rights reserved.	[Geraga, M.; Mylona, G.] Univ Patras, Dept Geol, Lab Marine Geol & Phys Oceanog, Patras 26504, Greece; [Lykousis, V.] Hellen Ctr Marine Res, Inst Oceanog, Anavyssos 19013, Greece; [Tsaila-Monopolis, St] Univ Patras, Dept Geol, Lab Paleontol, Patras 26504, Greece	University of Patras; Hellenic Centre for Marine Research; University of Patras	Geraga, M (通讯作者)，Univ Patras, Dept Geol, Lab Marine Geol & Phys Oceanog, Patras 26504, Greece.	mgeraga@upatras.gr	GERAGA, MARIA/AGJ-4293-2022	Geraga, Maria/0000-0002-6861-2789				Aksu AE, 2008, MAR GEOL, V252, P174, DOI 10.1016/j.margeo.2008.04.004; AKSU AE, 1995, PALAEOGEOGR PALAEOCL, V116, P71, DOI 10.1016/0031-0182(94)00092-M; Alley RB, 1997, GEOLOGY, V25, P483, DOI 10.1130/0091-7613(1997)025<0483:HCIAPW>2.3.CO;2; Asioli A, 2001, QUATERNARY SCI REV, V20, P1201, DOI 10.1016/S0277-3791(00)00147-5; Bar-Matthews M, 1999, EARTH PLANET SC LETT, V166, P85, DOI 10.1016/S0012-821X(98)00275-1; Bartov Y, 2003, GEOLOGY, V31, P439, DOI 10.1130/0091-7613(2003)031<0439:CAEITE>2.0.CO;2; 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Zachariasse Zachariasse Zachariasse Zachariasse Zachariasse Zachariasse Zachariasse Zachariasse W.J. W.J. W.J. W.J. W.J. W.J. W.J. W.J., P 5 HELL S OC FISH P 5 HELL S OC FISH, P391; Zervakis V, 2000, J GEOPHYS RES-OCEANS, V105, P26103, DOI 10.1029/2000JC900131; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	64	72	72	1	15	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	MAR 1	2010	287	1-4					101	115		10.1016/j.palaeo.2010.01.023	http://dx.doi.org/10.1016/j.palaeo.2010.01.023			15	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	576WH					2025-03-11	WOS:000276180100008
J	Collinson, ME; Barke, J; van der Burgh, J; van Konijnenburg-van Cittert, JHA; Heilmann-Clausen, C; Howard, LE; Brinkhuis, H				Collinson, Margaret E.; Barke, Judith; van der Burgh, Johan; van Konijnenburg-van Cittert, Johanna H. A.; Heilmann-Clausen, Claus; Howard, Lauren E.; Brinkhuis, Henk			Did a single species of Eocene <i>Azolla</i> spread from the Arctic Basin to the southern North Sea?	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Arctic Ocean; North Sea Basin; Denmark; Azolla; Eocene; megaspores; microspore massulae; Palynology; ultrastructure	BIOSTRATIGRAPHY; ULTRASTRUCTURE; SALVINIACEAE; MICROFOSSILS; MORPHOLOGY; PALEOCENE; GREENLAND; REVISION; BIOMASS; RECORD	Recent Arctic drilling has revealed that the freshwater surface-floating heterosporous fern Azolla arctica Collinson et al. (Azollaceae, Salviniales) bloomed and reproduced in the Arctic Ocean on a massive scale during the early Middle Eocene. These blooms have been suggested to have been capable of significant drawdown of atmospheric CO(2) paving the way to Cenozoic climatic cooling. Sites of similar age across the Arctic and Nordic Seas also contain Azolla fossils suggestive of an area much larger than the Arctic Ocean being affected by Azolla blooms, as far south as Denmark. Here we investigate the Danish occurrences known from the Lillebaelt Clay Formation, transitional Ypresian/Lutetian in age (latest Early Eocene to earliest Middle Eocene). The Lillebaelt Clay is a marine deposit rich in diverse organic-walled dinoflagellate cysts yet conspicuously characterized by abundant co-occurring and interconnected fully mature Azolla megaspores and microspore massulae. Perhaps surprisingly, we find that multiple morphological and ultrastructural characters distinguish the Danish Azolla species from Azolla arctica and it is here described as Azolla jutlandica sp. nov. Therefore, contrary to expectations given the overlapping age of these assemblages, it appears that not a single Azolla species has spread from the Arctic to the Southern North Sea either through freshwater spills from the Arctic Ocean or as a result of rapid spread due to highly invasive biology. Apparently Northern Hemisphere middle and high latitude conditions near the termination of a period known as the Early Eocene Climatic Optimum (EECO) were suitable for proliferation of two different Azolla species, one in the Arctic Ocean and one in the southern North Sea. (C) 2009 Elsevier B.V. All rights reserved.	[Collinson, Margaret E.] Royal Holloway Univ London, Dept Earth Sci, Egham TW20 0EX, Surrey, England; [Barke, Judith; van der Burgh, Johan; van Konijnenburg-van Cittert, Johanna H. A.; Brinkhuis, Henk] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [van Konijnenburg-van Cittert, Johanna H. A.] Natl Museum Nat Hist, NL-2300 RA Leiden, Netherlands; [Heilmann-Clausen, Claus] Aarhus Univ, Inst Geol, DK-8000 Aarhus C, Denmark; [Howard, Lauren E.] Nat Hist Museum, Dept Mineral, EMMA Unit, London SW7 5BD, England	University of London; Royal Holloway University London; Utrecht University; Aarhus University; Natural History Museum London	Collinson, ME (通讯作者)，Royal Holloway Univ London, Dept Earth Sci, Egham TW20 0EX, Surrey, England.	m.collinson@es.rhul.ac.uk	Heilmann-Clausen, Claus/A-4848-2012; Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610	Darwin Centre; Utrecht; Statoil Hydro	Darwin Centre; Utrecht; Statoil Hydro	We would like to thank R. van der Ham for access to specialist literature; T. Brain in Kings College London for embedding and sectioning the specimens illustrated by TEM and for his extensive support for both TEM and SEM work during this study; BJ. van Heuven in Leiden and J. van Tongeren in Utrecht for technical support for the SEM work. The samples and accompanying data for Azolla arctica (Collinson et al., 2009) with which A. jutlandica sp nov is compared in detail, were provided by the Integrated Ocean Drilling Program (IODP). We thank the Darwin Centre, Utrecht and Statoil Hydro for their financial support.	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Palaeobot. Palynology	MAR	2010	159	3-4					152	165		10.1016/j.revpalbo.2009.12.001	http://dx.doi.org/10.1016/j.revpalbo.2009.12.001			14	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	570OU					2025-03-11	WOS:000275688400002
J	Londeix, L; Herreyre, Y; Turon, JL; Fletcher, W				Londeix, Laurent; Herreyre, Yannick; Turon, Jean-Louis; Fletcher, William			Last glacial to Holocene hydrology of the Marmara Sea inferred from a dinoflagellate cyst record (vol 158, pg 52, 2009)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Correction									[Londeix, Laurent; Herreyre, Yannick; Turon, Jean-Louis; Fletcher, William] Univ Bordeaux 1, CNRS, UMR EPOC 5805, F-33405 Talence, France; [Fletcher, William] Goethe Univ Frankfurt, Inst Geowissensch, Frankfurt, Germany	Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Goethe University Frankfurt	Londeix, L (通讯作者)，Univ Bordeaux 1, CNRS, UMR EPOC 5805, Ave Fac, F-33405 Talence, France.	l.londeix@epoc.u-bordeaux1.fr						Londeix L, 2009, REV PALAEOBOT PALYNO, V158, P52, DOI 10.1016/j.revpalbo.2009.07.004	1	1	1	0	2	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0034-6667			REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	MAR	2010	159	3-4					204	204		10.1016/j.revpalbo.2009.12.004	http://dx.doi.org/10.1016/j.revpalbo.2009.12.004			1	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	570OU		Bronze			2025-03-11	WOS:000275688400007
J	Farooqui, A; Ray, JG; Farooqui, SA; Tiwari, RK; Khan, ZA				Farooqui, Anjum; Ray, J. G.; Farooqui, S. A.; Tiwari, R. K.; Khan, Z. A.			Tropical rainforest vegetation, climate and sea level during the Pleistocene in Kerala, India	QUATERNARY INTERNATIONAL			English	Article							SOUTHEASTERN ARABIAN SEA; TOBA ERUPTION; VOLCANIC ASH; QUATERNARY; POLLEN; RECORD; SEDIMENT; DEPOSITS; TEPHRA; BASIN	The southwestern Ghats region of the Indian Peninsula is unique for its extant endemic rainforest flora supported by high rainfall throughout the year. The record of tropical rainforest corresponding to the dynamic series of Pleistocene interglacial/glacial cycles is poorly known from peninsular India. This communication discusses the palynological study of organic matter (OM) deposits (>40 ka BP) in two well sections (Chaganachery, Kerala) from the Indian Peninsula (west coast). A rich archive of tropical rainforest pollen/spores and marine dinoflagellate cysts indicates anoxic fluvio-marine/estuarine depositional environments during warmer climates with an intensified Asian monsoon. The geochemical fingerprinting of glass shards indicates the presence of Youngest Toba ash of similar to 74 ka from northern Sumatra, and therefore establishes a time-controlled stratigraphy. Thus, the depositional time period of the OM is related to the sea level highstand of Marine Isotopic Stage 5.1 (similar to 80 ka) which was the host to the YTT shards. The Late Quaternary pollen/spores diversity suggests that the modern climatic conditions in the southwestern Ghats have facilitated the conservation of moist evergreen rainforest and dry/moist deciduous forest. The pollen grains show its lineage with the extant flora and some of the fossil pollen recorded during the mesic Tertiary period from the Indian peninsula. Thus, it appears that the tropical rainforest survived here as 'Plant Refugia' in xeric (glacial) Quaternary periods, perhaps as riparian vegetation, and was rejuvenated during the Holocene as modern extant flora. (C) 2009 Elsevier Ltd and INQUA. All rights reserved.	[Farooqui, Anjum] Birbal Sahni Inst Paleobot, Lucknow 226001, Uttar Pradesh, India; [Ray, J. G.] St Berchmans Coll, Dept Bot, Chaganacherry, Kerala, India; [Farooqui, S. A.; Khan, Z. A.] Directorate Geol & Min, Lucknow, Uttar Pradesh, India; [Tiwari, R. K.] Geol Survey India, Lucknow, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); Geological Survey India	Farooqui, A (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226001, Uttar Pradesh, India.	afarooqui_2000@yahoo.com	Khan, Zahoor/R-5965-2019; Ray, Joseph/E-7320-2010	Ray, Joseph/0000-0001-5045-050X				Acharyya SK, 2000, ENVIRON GEOL, V39, P1127, DOI 10.1007/s002540000107; ACHARYYA SK, 1993, QUATERNARY RES, V40, P10, DOI 10.1006/qres.1993.1051; [Anonymous], 1968, A Revised Survey of the Forest Types of India; ARINUSHKIN EV, 1978, GUIDE SOIL CHEM ANAL; Axelrod D.I., 1979, Occasional Papers of the California Academy of Sciences, V132, P1; Barboni D, 2003, J VEG SCI, V14, P551, DOI 10.1111/j.1654-1103.2003.tb02182.x; Barboni D, 2001, REV PALAEOBOT PALYNO, V114, P239, DOI 10.1016/S0034-6667(01)00057-4; BEDDOESTEPHENS B, 1983, CONTRIB MINERAL PETR, V83, P278, DOI 10.1007/BF00371196; Bera S.K., 1997, PALEOBOTANIST, V46, P191; Bera S.K., 2000, Jour. 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Int.	FEB 23	2010	213	1-2					2	11		10.1016/j.quaint.2009.09.024	http://dx.doi.org/10.1016/j.quaint.2009.09.024			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	569CE					2025-03-11	WOS:000275572900002
J	Emeis, KC; Finney, BP; Ganeshram, R; Gutiérrez, D; Poulsen, B; Struck, U				Emeis, Kay-Christian; Finney, Bruce P.; Ganeshram, Raja; Gutierrez, Dimitri; Poulsen, Bo; Struck, Ulrich			被撤回的出版物: Impacts of past climate variability on marine ecosystems: Lessons from sediment records (Retracted Article)	JOURNAL OF MARINE SYSTEMS			English	Article; Proceedings Paper; Retracted Publication	Workshop on the Impact of Climate Variability on Marine Ecosystems	SEP 04-08, 2006	Alexander VonHuboldy Univ, Museum Nat Hist, Berlin, GERMANY		Alexander VonHuboldy Univ, Museum Nat Hist	Proxy; Upwelling; Nitrogen isotopes; Fish scales; Paleo climate; Humboldt Current; Benguela Current	FISH SCALES; SELECTIVE PRESERVATION; DINOFLAGELLATE CYSTS; UPWELLING SYSTEM; CARBON FLUX; HOLOCENE; NORTHERN; SEA; FISHERIES; SARDINE	Sediment records and historical accounts are the only source of information on marine ecosystem status and variability at higher trophic levels before scientific observations began. Most reconstructions of paleoenvironments and higher ecosystem levels are based on measurable proxies in these sedimentary archives, ideally those that are directly and robustly related to environmental or biological variables of interest. Depositional characteristics place some constraints on the types of environments where proxy-based investigations into the dynamics of higher levels of marine ecosystems can be done and many proxy methods have large error ranges. But although sedimentary proxy records are often plagued by dating uncertainties and although proxies for higher ecosystem levels are scarce, the few studies performed in lakes and coastal upwelling environments have already yielded some fascinating insights into spatial and temporal scales of ecosystem variability in the past. Most available records are low-pass filtered with a bias to longer-term changes, which limits the window of detection to (interannual)-decades to centuries or even longer. Available data suggest pervasive bottom-up control of marine ecosystems in response to relatively subtle changes in external forcing, which telescopes into very high variability on higher trophic levels. Many paleo-curves suggest cyclicities or thresholds, which point to either cyclic external drivers or non-linear reactions. In particular, response of higher trophic levels to changes at the base of ecosystems appears to be highly nonlinear and shows variations of several orders of magnitude, as exemplified by fish stocks in several areas (Baltic Sea, North Sea, upwelling systems, lakes in Canada) from historical records, observations and sediment archives. (C) 2009 Elsevier B.V. All rights reserved.	[Emeis, Kay-Christian] Univ Hamburg, Inst Biageochem & Meereschem, D-20146 Hamburg, Germany; [Finney, Bruce P.] Idaho State Univ, Dept Biol Sci, Pocatello, ID 83209 USA; [Ganeshram, Raja] Univ Edinburgh, Sch Geosci, Grant Inst Geol, Edinburgh EH9 3JW, Midlothian, Scotland; [Gutierrez, Dimitri] Inst Mar Peru, Esquina, Chucuito, Peru; [Poulsen, Bo] Roskilde Univ, DK-4000 Roskilde, Denmark; [Struck, Ulrich] Museum Nat Kunde, D-10115 Berlin, Germany	University of Hamburg; Idaho State University; University of Edinburgh; Instituto del Mar del Peru; Roskilde University; Leibniz Institut fur Evolutions und Biodiversitatsforschung	Emeis, KC (通讯作者)，Univ Hamburg, Inst Biageochem & Meereschem, Bundesstr 55, D-20146 Hamburg, Germany.	kay.emeis@zmaw.de	Ganeshram, Raja S/JPX-5314-2023	Poulsen, Bo/0000-0002-6759-2341; Emeis, Kay-Christian/0000-0003-0459-913X				Alheit J, 2004, PROG OCEANOGR, V60, P201, DOI 10.1016/j.pocean.2004.02.006; Alheit J, 2010, J MARINE SYST, V79, P267, DOI 10.1016/j.jmarsys.2008.11.029; 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Mar. Syst.	FEB 10	2010	79	3-4			SI		333	342		10.1016/j.jmarsys.2008.12.012	http://dx.doi.org/10.1016/j.jmarsys.2008.12.012			10	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Geology; Marine & Freshwater Biology; Oceanography	536OD		Bronze			2025-03-11	WOS:000273052800011
J	Caissie, BE; Brigham-Grette, J; Lawrence, KT; Herbert, TD; Cook, MS				Caissie, Beth E.; Brigham-Grette, Julie; Lawrence, Kira T.; Herbert, Timothy D.; Cook, Mea S.			Last Glacial Maximum to Holocene sea surface conditions at Umnak Plateau, Bering Sea, as inferred from diatom, alkenone, and stable isotope records	PALEOCEANOGRAPHY			English	Review							DINOFLAGELLATE CYST ASSEMBLAGES; NORTH PACIFIC-OCEAN; OKHOTSK SEA; BIOMARKER APPROACH; LATE PLEISTOCENE; AGE CALIBRATION; CLIMATE-CHANGE; DATA-BASE; DEEP-SEA; ICE	The Bering Sea gateway between the Pacific and Arctic oceans impacts global climate when glacial-interglacial shifts in shore line position and ice coverage change regional albedo. Previous work has shown that during the last glacial termination and into the Holocene, sea level rises and sea ice coverage diminishes from perennial to absent. Yet, existing work has not quantified sea ice duration or sea surface temperatures (SST) during this transition. Here we combine diatom assemblages with the first alkenone record from the Bering Sea to provide a semiquantitative record of sea ice duration, SST, and productivity change since the Last Glacial Maximum (LGM). During the LGM, diatom assemblages indicate that sea ice covered the southeastern Bering Sea perennially. At 15.1 cal ka B. P., the diatom assemblage shifts to one more characteristic of seasonal sea ice and alkenones occur in the sediments in low concentrations. Deglaciation is characterized by laminated intervals with highly productive and diverse diatom assemblages and inferred high coccolithophorid production. At 11.3 cal ka B. P. the diatom assemblage shifts from one dominated by sea ice species to one dominated by a warmer water, North Pacific species. Simultaneously, the SST increases by 3 degrees C and the southeastern Bering Sea becomes ice-free year-round. Productivity and temperature proxies are positively correlated with independently dated records from elsewhere in the Bering Sea, the Sea of Okhotsk, and the North Pacific, indicating that productivity and SST changes are coeval across the region.	[Caissie, Beth E.; Brigham-Grette, Julie] Univ Massachusetts, Dept Geosci, Amherst, MA 01301 USA; [Cook, Mea S.] Williams Coll, Dept Geosci, Williamstown, MA 01267 USA; [Herbert, Timothy D.] Brown Univ, Dept Geol Sci, Providence, RI 02912 USA; [Lawrence, Kira T.] Lafayette Coll, Dept Geol & Environm Geosci, Easton, PA 18042 USA	University of Massachusetts System; University of Massachusetts Amherst; Williams College; Brown University; Lafayette College	Caissie, BE (通讯作者)，Univ Massachusetts, Dept Geosci, 233 Morrill Sci Ctr,611 N Pleasant St, Amherst, MA 01301 USA.	bethc@geo.umass.edu	Caissie, Beth/F-3463-2013	Cook, Mea/0000-0003-3786-6353; Caissie, Beth/0000-0001-9587-1842	National Science Foundation; Office of Polar Programs Arctic Natural Sciences; ATM Paleoclimate [OPP-0002643]	National Science Foundation(National Science Foundation (NSF)); Office of Polar Programs Arctic Natural Sciences; ATM Paleoclimate(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We thank John Barron (USGS) and Connie Sancetta for taxonomic assistance; Mark Leckie (UMass), Rob DeConto (UMass), Gerald Dickens, Eleanor Maddison, and one anonymous reviewer for constructive criticism of the manuscript; and Peter Schweitzer (USGS) for assistance with the Query Ice tool. We would also like to thank the officers and crew of the USCGC Healy WAGB-20 for their support during core collection. This work was supported by a grant to J. B. G. from the National Science Foundation, Office of Polar Programs Arctic Natural Sciences, and ATM Paleoclimate OPP-0002643.	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J	Cavalier-Smith, T				Cavalier-Smith, Thomas			Origin of the cell nucleus, mitosis and sex: roles of intracellular coevolution	BIOLOGY DIRECT			English	Article							POLO-LIKE KINASE; BACTERIAL-DNA SEGREGATION; HORIZONTAL GENE-TRANSFER; MESSENGER-RNA DECAY; CENTRIOLE DUPLICATION; DINOFLAGELLATE CHROMOSOMES; TRYPANOSOMA-BRUCEI; PROTEIN-KINASES; EVOLUTIONARY RELATIONSHIPS; PHYLOGENETIC ANALYSIS	Background: The transition from prokaryotes to eukaryotes was the most radical change in cell organisation since life began, with the largest ever burst of gene duplication and novelty. According to the coevolutionary theory of eukaryote origins, the fundamental innovations were the concerted origins of the endomembrane system and cytoskeleton, subsequently recruited to form the cell nucleus and coevolving mitotic apparatus, with numerous genetic eukaryotic novelties inevitable consequences of this compartmentation and novel DNA segregation mechanism. Physical and mutational mechanisms of origin of the nucleus are seldom considered beyond the longstanding assumption that it involved wrapping pre-existing endomembranes around chromatin. Discussions on the origin of sex typically overlook its association with protozoan entry into dormant walled cysts and the likely simultaneous coevolutionary, not sequential, origin of mitosis and meiosis. Results: I elucidate nuclear and mitotic coevolution, explaining the origins of dicer and small centromeric RNAs for positionally controlling centromeric heterochromatin, and how 27 major features of the cell nucleus evolved in four logical stages, making both mechanisms and selective advantages explicit: two initial stages (origin of 30 nm chromatin fibres, enabling DNA compaction; and firmer attachment of endomembranes to heterochromatin) protected DNA and nascent RNA from shearing by novel molecular motors mediating vesicle transport, division, and cytoplasmic motility. Then octagonal nuclear pore complexes (NPCs) arguably evolved from COPII coated vesicle proteins trapped in clumps by Ran GTPase-mediated cisternal fusion that generated the fenestrated nuclear envelope, preventing lethal complete cisternal fusion, and allowing passive protein and RNA exchange. Finally, plugging NPC lumens by an FG-nucleoporin meshwork and adopting karyopherins for nucleocytoplasmic exchange conferred compartmentation advantages. These successive changes took place in naked growing cells, probably as indirect consequences of the origin of phagotrophy. The first eukaryote had 1-2 cilia and also walled resting cysts; I outline how encystation may have promoted the origin of meiotic sex. I also explain why many alternative ideas are inadequate. Conclusion: Nuclear pore complexes are evolutionary chimaeras of endomembrane-and mitosis-related chromatin-associated proteins. The keys to understanding eukaryogenesis are a proper phylogenetic context and understanding organelle coevolution: how innovations in one cell component caused repercussions on others. Reviewers: This article was reviewed by Anthony Poole, Gaspar Jekely and Eugene Koonin.	Univ Oxford, Dept Zool, Oxford OX1 3PS, England	University of Oxford	Cavalier-Smith, T (通讯作者)，Univ Oxford, Dept Zool, S Parks Rd, Oxford OX1 3PS, England.	tom.cavalier-smith@zoo.ox.ac.uk			NERC	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	I thank NERC for grant and fellowship support.	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Direct	FEB 4	2010	5								7	10.1186/1745-6150-5-7	http://dx.doi.org/10.1186/1745-6150-5-7			78	Biology	Science Citation Index Expanded (SCI-EXPANDED)	Life Sciences & Biomedicine - Other Topics	568HU	20132544	gold, Green Published			2025-03-11	WOS:000275514000001
J	Uzar, S; Aydin, H; Minareci, E				Uzar, Serdar; Aydin, Hilal; Minareci, Ersin			Dinoflagellate cyst assemblages in the surface sediments from Izmir bay, Aegean sea, Eastern Mediterranean	SCIENTIFIC RESEARCH AND ESSAYS			English	Article						Dinoflagellate cysts; cyst assemblage; cyst morphology; Izmir Bay; surface sediments	RECENT MARINE-SEDIMENTS; EUTROPHICATION; NUTRIENT; INDICATORS; MARMARA; COAST	The present study was conducted on dinoflagellate cyst assemblages from Izmir Bay, Aegean Sea subject to high human impact. Sediment cores were taken from twelve stations. Twenty-eight dinoflagellate cyst types, representing nine genera, were identified. The most common cysts were those of Lingulodinium machaerophorum, Polykrikos kofoidii, Quinquecuspis concreta and Dubridinium caperatum. Potentially toxic species were widely distributed in the study area. This finding is also important to know the seed-bank areas in the Bay of Izmir.	[Uzar, Serdar; Aydin, Hilal; Minareci, Ersin] Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey	Celal Bayar University	Minareci, E (通讯作者)，Celal Bayar Univ, Fac Sci & Arts, Dept Biol, TR-45140 Manisa, Turkey.	ersinminareci@gmail.com	UZAR, SERDAR/G-9956-2014	UZAR, SERDAR/0000-0002-9477-7413	Scientific Investigation Project to Coordinate of Celal Bayar University [FEF 2008-004]	Scientific Investigation Project to Coordinate of Celal Bayar University(Celal Bayar University)	The author thanks to Scientific Investigation Project to Coordinate of Celal Bayar University (Project No. FEF 2008-004) for financial support. This study contains a part of Master dissertation prepared by Serdar Uzar in Celal Bayar University.	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Res. Essays	FEB 4	2010	5	3					285	295						11	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	565DN					2025-03-11	WOS:000275269500004
J	Bravo, I; Figueroa, RI; Garcés, E; Fraga, S; Massanet, A				Bravo, Isabel; Figueroa, Rosa Isabel; Garces, Esther; Fraga, Santiago; Massanet, Ana			The intricacies of dinoflagellate pellicle cysts: The example of <i>Alexandrium minutum</i> cysts from a bloom-recurrent area (Bay of Baiona, NW Spain)	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium minutum; Ecdysal cysts; Galician rias; Pellicle cysts; Spain; Temporary cysts	RED-TIDE DINOFLAGELLATE; GYMNODINIUM-CATENATUM DINOPHYCEAE; GONYAULAX-POLYEDRA STEIN; OYSTER CRASSOSTREA-GIGAS; LIFE-CYCLE; TOXIC DINOFLAGELLATE; TAYLORI DINOPHYCEAE; SEXUAL REPRODUCTION; HETEROCAPSA-CIRCULARISQUAMA; LINGULODINIUM-POLYEDRUM	The terms "temporary", "pellicle", and "ecdysal" cyst have been employed arbitrarily in the literature of the dinoflagellate life cycle to describe a non-motile and single-layered-wall stage with no mandatory dormancy period, of asexual or sexual origin. These three terms have been used more or less synonymously, but more specific definitions, taking into account morphological and physiological aspects and their roles in dinoflagellate population dynamics, are still needed. To clarify the current terminology, we examine and discuss the usages and foundations of those terms, The background for this discussion is Provided by a comparison of the morphology and germination times of three different types of Alexandrium minutum cysts collected during a seasonal bloom in the Bay of Baiona (NW Spain). The double-walled cysts were similar to the resting cysts reported for this species, but other, thin-walled and thecate cysts were also observed. These latter cyst types needed between 1 and 17 days to germinate and were therefore considered as short-term cysts, in contrast to the 1.5-month dormancy period of resting (hypnozygotic) cysts. Our results showed that the temporal distribution of these short-term cysts during the bloom period followed a pattern very similar to that of vegetative cells. However, resting cysts were only detected at the end of the bloom. In the context of our present knowledge regarding the dormancy and quiescence of dinoflagellate cysts, "temporary" is a very misleading and uncertain term and must be rejected. The term "ecdysal" has been used in reference to thin-walled cysts when ecdysis has been proven; however, ecdysis is not unique to this type of cysts as thick-walled zygotic cysts can be formed thorough ecdysis of a thecate planozygote. In conclusion, based on our current understanding of cysts, the term "pellicle" more appropriately describes single-layered-wall stages. (C) 2009 Elsevier Ltd. All rights reserved.	[Bravo, Isabel; Fraga, Santiago; Massanet, Ana] Ctr Oceanog Vigo, Inst Espanol Oceanog, E-36390 Vigo, Spain; [Figueroa, Rosa Isabel; Garces, Esther] CSIC, Dept Biol Marina & Oceanog, Inst Ciencies Mar, E-08003 Barcelona, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Bravo, I (通讯作者)，Ctr Oceanog Vigo, Inst Espanol Oceanog, Subida Radio Faro 50, E-36390 Vigo, Spain.	isabel.bravo@vi.ieo.es	Fraga, Santiago/AAA-3760-2020; Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011; Fraga, Santiago/C-8641-2012	, Ana Massanet/0000-0003-4253-779X; Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X; Bravo, Isabel/0000-0003-3764-745X; Fraga, Santiago/0000-0003-3917-9960	Spanish Ministry of Education and Science; EU [GOCE-CT-2005-003875]	Spanish Ministry of Education and Science(Spanish Government); EU(European Union (EU))	The authors thank I. Ramilo, A. Fernandez-Villamarin, and P. Rial for their assistance in phytoplankton and trap sampling. We also thank Puerto Deportivo de Baiona for permission to place the trap and taking samples from the marina, and D. Anderson and an anonymous reviewer who helped us to clarify the distinction between the different cyst types. The work of E. Garces was supported by the Ramon y Cajal contract of the Spanish Ministry of Education and Science. R.I. Figueroa's work was supported by a postdoctoral I3P contract of the Spanish Ministry of Education and Science. Financial support was provided by EU Project SEED (GOCE-CT-2005-003875).	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					166	174		10.1016/j.dsr2.2009.09.003	http://dx.doi.org/10.1016/j.dsr2.2009.09.003			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900003
J	Brosnahan, ML; Kulis, DM; Solow, AR; Erdner, DL; Percy, L; Lewis, J; Anderson, DM				Brosnahan, Michael L.; Kulis, David M.; Solow, Andrew R.; Erdner, Deana L.; Percy, Linda; Lewis, Jane; Anderson, Donald M.			Outbreeding lethality between toxic Group I and nontoxic Group III <i>Alexandrium tamarense</i> spp. isolates: Predominance of heterotypic encystment and implications for mating interactions and biogeography	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Dinoflagellates; Hybridization; Biogeography; Harmful algal blooms; Genotypes; UK; Northern Ireland; Belfast Lough	DINOFLAGELLATE GONYAULAX-TAMARENSIS; CYST FORMATION; SEXUAL REPRODUCTION; GENETIC-MARKERS; RESTING CYSTS; DINOPHYCEAE; IDENTIFICATION; PACIFIC; STRAIN; EXCYSTMENT	We report the zygotic encystment of geographically dispersed isolates in the dinoflagellate species complex Alexandrium tamarense, in particular, successful mating of toxic Group I and nontoxic Group III isolates. However, hypnozygotes produced in Group I/III co-cultures complete no more than three divisions after germinating. Previous reports have Suggested a mate recognition mechanism whereby hypnozygotes produced in co-cultures could arise from either homotypic (inbred) or heterotypic (outbred) gamete pairs. To determine the extent to which each occurs, a nested PCR assay was developed to determine parentage of individual hypnozygotes. The vast majority of hypnozygotes from pairwise Group I/III co-cultures were outbred, so that inviability was a result of hybridization, not inbreeding. These findings support the assertion that complete speciation underlies the phylogenetic structure of the Alexandrium tamarense species complex. Additionally, the ribosomal DNA (rDNA) copy numbers of both hybrid and single ribotype hypnozygotes were reduced substantially from those of haploid motile cells. The destruction of rDNA loci may be crucial for the successful mating of genetically distant conjugants and appears integral to the process of encystment. The inviability of Group I/III hybrids is important for public health because the presence of hybrid cysts may indicate ongoing displacement of a nontoxic population by a toxic one (or vice versa). Hybrid inviability also suggests a bloom control strategy whereby persistent, toxic Group I blooms could be mitigated by introduction of nontoxic Group III cells. The potential for hybridization in nature was investigated by applying the nested PCR assay to hypnozygotes from Belfast Lough, Northern Ireland, a region where Group I and M populations co-occur. Two hybrid cysts were identified in 14 successful assays, demonstrating that Group I and III populations do interbreed in that region. However, an analysis of mating data collected over an 18-year period indicated a leaky pre-mating barrier between ribosomal species (including Groups I and III). Whether the observed selectivity inhibits hybridization in nature is dependent on its mechanism. If the point of selectivity is the induction of gametogenesis, dissimilar ribotypes could interbreed freely, promoting displacement in cases where hybridization is lethal. If instead, selectivity occurs during the adhesion of gamete pairs, it could enable stable coexistence of A. tamarense species. In either case, hybrid inviability may impose a significant obstacle to range expansion. The nested PCR assay developed here is a valuable tool for investigation of interspecies hybridization and its consequences for the global biogeography of these important organisms. (C) 2009 Elsevier Ltd. All rights reserved.	[Brosnahan, Michael L.; Kulis, David M.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Solow, Andrew R.] Woods Hole Oceanog Inst, Marine Policy Ctr, Woods Hole, MA 02543 USA; [Erdner, Deana L.] Univ Texas Austin, Dept Marine Sci, Inst Marine Sci, Port Aransas, TX 78373 USA; [Percy, Linda; Lewis, Jane] Univ Westminster, Sch Biosci, London W1W 6UW, England	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; University of Texas System; University of Texas Austin; University of Westminster	Brosnahan, ML (通讯作者)，Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA.	mbrosnahan@whoi.edu	; Erdner, Deana/C-4981-2008	Brosnahan, Michael/0000-0002-2620-7638; Erdner, Deana/0000-0002-1736-8835	NSF [OCE-0402707, OCE-9808173, OCE-0430724]; NIEHS [P50ES012742-0]; NOAA [NA06-NOS4780245]; EU [GOCE-CT-2005-003875]; US Environmental Protection Agency [FP-91688601]; Directorate For Geosciences; Division Of Ocean Sciences [0911031] Funding Source: National Science Foundation	NSF(National Science Foundation (NSF)); NIEHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); EU(European Union (EU)); US Environmental Protection Agency(United States Environmental Protection Agency); Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	We thank K. Norton, B. Keafer, J. Kleindinst and other members of the Anderson laboratory for technical support, and are also grateful to S. Bickel and R. Sloboda at Dartmouth College (Hanover, NH) for hosting MLB during completion of the laser catapult experiments. We also thank a large number of colleagues who shared their Alexandrium cultures for these experiments. Work by MLB, DLE, and DMA was supported by NSF Grant nos. OCE-0402707 and OCE-9808173 and by the Woods Hole Center for Oceans and Human Health through NSF Grant no. OCE-0430724 and NIEHS Grant no. P50ES012742-0. Research support has also been provided through NOAA Grant no. NA06-NOS4780245, an EU SEED Grant no. GOCE-CT-2005-003875 (JL, LP), and a STAR graduate fellowship to MLB (FP-91688601) from the US Environmental Protection Agency. The EPA has not formally reviewed this publication, and the EPA does not endorse any of the products mentioned in it. The views expressed are solely those of the authors. This is ECOHAB Contribution no. 309.	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J	Figueroa, RI; Rengefors, K; Bravo, I; Bensch, S				Isabel Figueroa, Rosa; Rengefors, Karin; Bravo, Isabel; Bensch, Staffan			From homothally to heterothally: Mating preferences and genetic variation within clones of the dinoflagellate <i>Gymnodinium catenatum</i>	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Dinophyceae; Encystment; Gymnodinium catenatum; AFLPs; Sexual compatibility; Life cycle; Mating; Intraclonal genetic variation	LIFE-CYCLE; GONYAULAX-TAMARENSIS; SEXUAL REPRODUCTION; DINOPHYCEAE; AFLP; DNA; RAPD; EVOLUTION; MUTATION; STRAINS	The chain-forming dinoflagellate Gymnodinium catenatum Graham is responsible for outbreaks of paralytic shellfish poisoning (PSP), a human health threat in coastal waters. Sexuality in this species is of great importance in its bloom dynamics, and has been shown to be very complex but lacks an explanation. For this reason, we tested if unreported homothallic behavior and rapid genetic changes may clarify the sexual system of this alga. To achieve this objective, 12 clonal strains collected from the Spanish coast were analyzed for the presence of sexual reproduction. Mating affinity results, self-compatibility studies, and genetic fingerprinting (amplified fragment length polymorphism, AFLP) analysis on clonal strains, showed three facts not previously described for this species: (i) That there is a continuous mating system within G. catenatum, with either self-compatible strains (homothallic), or strains that needed to be outcrossed (heterothallic), and with a range of differences in cyst production among the crosses. (ii) There was intraclonal genetic variation, i.e. genetic variation within an asexual lineage. Moreover, the variability among homothallic clones was smaller than among the heterothallic ones. (iii) Sibling strains (the two strains established by the germination of one cyst) increased their intra- and inter-sexual compatibility with time. To summarize, we have found that G. catenatum's sexual system is much more complex than previously described, including complex homothallic/heterothallic behaviors. Additionally, high rates of genetic variability may arise in clonal strains, although explanations for the mechanisms responsible are still lacking. (C) 2009 Elsevier Ltd. All rights reserved.	[Isabel Figueroa, Rosa] CSIC, CMIMA, Inst Ciencies Mar, Dept Biol Marina & Oceanog,ICM, E-08003 Barcelona, Spain; [Rengefors, Karin] Lund Univ, Limnol Div, Dept Ecol, S-22362 Lund, Sweden; [Bravo, Isabel] CO Vigo, IEO, Vigo 36280, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Lund University; Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，CSIC, CMIMA, Inst Ciencies Mar, Dept Biol Marina & Oceanog,ICM, P Maritim de la Barceloneta 37-43, E-08003 Barcelona, Spain.	figueroa@icm.csic.es	Bravo, Isabel/D-3147-2012; Rengefors, Karin/K-5873-2019; Figueroa, Rosa/M-7598-2015	Bravo, Isabel/0000-0003-3764-745X; Rengefors, Karin/0000-0001-6297-9734; Figueroa, Rosa/0000-0001-9944-7993; Bensch, Staffan/0000-0002-0082-0899	Swedish Research Council; SEED [GOCE-CT-2005-003875]	Swedish Research Council(Swedish Research Council); SEED	We thank M. Svensson and A. Fernandez-Villamarin for technical assistance. We also thank J. Galindo for his help with the statistical analysis. The research was supported by an I3P postdoctoral grant for training of research staff to R.I.F., by the Swedish Research Council (VR) to K.R., and by the SEED project (GOCE-CT-2005-003875). We are grateful to several reviewers who helped improve earlier versions of this manuscript.	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					190	198		10.1016/j.dsr2.2009.09.016	http://dx.doi.org/10.1016/j.dsr2.2009.09.016			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900005
J	Anglès, S; Jordi, A; Garcés, E; Basterretxea, G; Palanques, A				Angles, Silvia; Jordi, Antoni; Garces, Esther; Basterretxea, Gotzon; Palanques, Albert			<i>Alexandrium minutum</i> resting cyst distribution dynamics in a confined site	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium minutum; Mediterranean Sea; Resting cyst; Resuspension; Sediment dynamics; Seiche	LIVING DINOFLAGELLATE CYSTS; RECENT SEDIMENTS; SURFACE SEDIMENTS; RESUSPENSION EVENTS; BLOOM; MODEL; GULF; RECRUITMENT; AFRICA; AREAS	The life cycle of the toxic dinoflagellate Alexandrium minutum consists of an asexual stage, characterized by motile vegetative cells, and a sexual stage, a resting cyst that once formed remains dormant in the sediment. Insight into the factors that determine the distribution and abundance of resting cysts is essential to understanding the dynamics of the vegetative phase. In investigations carried out between January 2005 and January 2008 in Arenys de Mar harbor (northwestern Mediterranean Sea), the spatial and temporal distribution patterns of A. minutum resting cysts and of the sediments were studied during different bloom stages of the vegetative population. Maximum cyst abundance was recorded mainly in the innermost part of the harbor while the lowest abundance always occurred near the harbor entrance, consistent with the distribution of silt-clay sediment fractions. The tendency of cysts in sediments to increase after bloom periods was clearly associated with new cyst formation, while cyst abundance decreased during non-bloom periods. Exceptions to this trend were observed in stations dominated by the deposition of coarse sediments. High correlation between the presence of cysts and clays during non-bloom periods indicates that cysts behave as passive sediment particles and are influenced by the same hydrodynamic processes as clays. In Arenys de Mar, the main physical forcing affecting sediment resuspension is the seiche, which was studied using in situ measurements and numerical models to interpret the observed distribution patterns. During non-bloom periods, cyst losses were smaller when the seiche was more active and at the station where the seiche-induced current was larger. Thus, seiche-forced resuspension appears to reduce cyst losses by reallocating cysts back to the sediment surface such that their burial in the sediment is avoided. The observed vertical profiles of the cysts were consistent with this process. (C) 2009 Elsevier Ltd. All rights reserved.	[Angles, Silvia; Garces, Esther; Palanques, Albert] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Jordi, Antoni] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA; [Jordi, Antoni; Basterretxea, Gotzon] UIB CSIC, IMEDEA, Esporles 07190, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); State University of New York (SUNY) System; Stony Brook University; Universitat de les Illes Balears; Consejo Superior de Investigaciones Cientificas (CSIC); ATTITUS Educacao	Anglès, S (通讯作者)，CSIC, Inst Ciencies Mar, Pg Maritim Barceloneta 37-49, E-08003 Barcelona, Spain.	sangles@icm.cat	Palanques, Albert/C-2661-2013; Basterretxea, Gotzon/D-2314-2011; Garces, Esther/C-5701-2011; Jordi, Antoni/C-3935-2008; Angles, Silvia/B-9469-2011	Garces, Esther/0000-0002-2712-501X; Jordi, Antoni/0000-0003-2637-8389; Basterretxea, Gotzon/0000-0001-7466-1360; Palanques, Albert/0000-0003-2544-2342; Angles, Silvia/0000-0003-0529-7504	EC [GOCE-CT-2005-003875]; Spanish Ministry of Science and Innovation	EC(European Union (EU)European Commission Joint Research Centre); Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government)	The authors thank N. Sampedro and A. Rene for data from the toxic phytoplankton monitoring program, and S. de Diago and N. Maestro for the sediment analysis. B. Casas, K. Van Lenning, and X. Novell provided valuable help with the fieldwork. We also are grateful to Creu Roja, Club Nautic, and Cofradia de Pescadors St Telm of Arenys de Mar harbor. This study was financed by the EC-funded Research Project SEED (GOCE-CT-2005-003875). The work of A. Jordi and E. Garces was supported by a postdoctoral grant and a Ramon y Cajal award, respectively, both from the Spanish Ministry of Science and Innovation.	Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; Andersen P., 2003, Manual on harmful marine microalgae. 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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					210	221		10.1016/j.dsr2.2009.09.002	http://dx.doi.org/10.1016/j.dsr2.2009.09.002			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR		Green Submitted			2025-03-11	WOS:000275943900007
J	Bravo, I; Fraga, S; Figueroa, RI; Pazos, Y; Massanet, A; Ramilo, I				Bravo, Isabel; Fraga, Santiago; Isabel Figueroa, Rosa; Pazos, Yolanda; Massanet, Ana; Ramilo, Isabel			Bloom dynamics and life cycle strategies of two toxic dinoflagellates in a coastal upwelling system (NW Iberian Peninsula)	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Phytoplankton; Population dynamics; Red tides; Paralytic shellflsh poisoning; Spain; Galician rias	GYMNODINIUM-CATENATUM DINOPHYCEAE; ALEXANDRIUM-MINUTUM DINOPHYCEAE; POLEWARD CURRENT; RIAS-BAIXAS; RED TIDES; CYSTS; SPAIN; CATENELLA; CULTURE; GROWTH	A study of Gymnodinium catenatum and Alexandrium minutum blooms on the Galician coast was conducted from 2005 to 2007 in order to increase knowledge of the mechanisms governing recurrent blooms of these species. Considerable differences in their bloom dynamics were observed. G. catenatum blooms occurred in autumn and winter, following the pattern previously reported in the literature: they began off-shore and were advected to the Galician rias when a relaxation of the coastal upwelling occurred. On the other hand, A. minutum blooms developed inside embayments in spring and summer during the upwelling season and were associated with water stability and stratification. Both the vegetative population and the cyst distribution of A. minutum were related to less saline water from freshwater river outputs, which support a saline-gradient relationship postulated herein for this species. Dinoflagellates may produce both long-term double-walled cysts (resting) and short-term pellicle cysts. Resting cyst deposition and distribution in sediments showed that seeding occurred during the blooms of both species. However, the relationship between the cyst distribution in the sediments in Baiona Bay and the intensity and occurrence of C. catenatum blooms, suggests that the latter are not directly related to resting cyst germination. Moreover, the results presented in the present study point to other difference between the two species, such as the detection of pellicle cysts only for A. minutum. Finally, we discuss how the life cycle strategies of these two species may help to explain the different mechanisms of bloom formation reported herein. (C) 2009 Elsevier Ltd. All rights reserved.	[Bravo, Isabel; Fraga, Santiago; Massanet, Ana; Ramilo, Isabel] Ctr Oceanog Vigo, Inst Espanol Oceanog, E-36390 Vigo, Spain; [Isabel Figueroa, Rosa] CSIC, CMIMA, Dept Biol Marina & Oceanog, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Pazos, Yolanda] Inst Tecnolox Control Medio Marino Galicia, Vilaxoan, Pontevedra, Spain	Spanish Institute of Oceanography; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Bravo, I (通讯作者)，Ctr Oceanog Vigo, Inst Espanol Oceanog, Subida Radio Faro 50, E-36390 Vigo, Spain.	isabel.bravo@vi.ieo.es	Bravo, Isabel/D-3147-2012; Fraga, Santiago/AAA-3760-2020; Figueroa, Rosa/M-7598-2015; Fraga, Santiago/C-8641-2012	Figueroa, Rosa/0000-0001-9944-7993; Fraga, Santiago/0000-0003-3917-9960; Bravo, Isabel/0000-0003-3764-745X; , Ana Massanet/0000-0003-4253-779X	EU [GOCE-CT-2005-003875]	EU(European Union (EU))	The authors thank A. Fernandez-Villamarin and P. Rial for their assistance in phytoplankton sampling and for their technical assistance in sediment processing and culture maintenance. We express our gratitude to the Confraria de Baiona for lending the ship and its Patron Maior Suso for their support on sampling cruises. We also want to Antonio Liebanas for its helpful attitude and Puerto Deportivo de Baiona for permission to place the trap and taking samples from the marina. Financial support was provided by EU Project SEED (GOCE-CT-2005-003875).	ALVAREZSALGADO XA, 1993, J GEOPHYS RES-OCEANS, V98, P14447, DOI 10.1029/93JC00458; ANDERSON DM, 1988, J PHYCOL, V24, P255; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; [Anonymous], COASTAL UPWELLING SE; [Anonymous], 1996, HARMFUL TOXIC ALGAL; BAKUN A, 1973, NHFSSSRS693 NOAA; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Basterretxea G, 2005, ESTUAR COAST SHELF S, V62, P1, DOI 10.1016/j.ecss.2004.07.008; Blackburn SI, 2001, PHYCOLOGIA, V40, P78, DOI 10.2216/i0031-8884-40-1-78.1; BLANCO J, 1990, Scientia Marina, V54, P287; BLANCO J, 1985, TOXIC DINOFLAGELLATE, P8; BOLCH CJ, 1991, PHYCOLOGIA, V30, P215, DOI 10.2216/i0031-8884-30-2-215.1; Bolli L, 2007, BIOGEOSCIENCES, V4, P559, DOI 10.5194/bg-4-559-2007; BRAVO I, 1994, J PLANKTON RES, V16, P513, DOI 10.1093/plankt/16.5.513; Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; Bravo I, 2008, HARMFUL ALGAE, V7, P515, DOI 10.1016/j.hal.2007.11.005; Bravo I, 2006, EUR J PHYCOL, V41, P293, DOI 10.1080/09670260600810360; Bravo I, 2010, DEEP-SEA RES PT II, V57, P166, DOI 10.1016/j.dsr2.2009.09.003; CANNON JA, 1990, TOXIC MARINE PHYTOPLANKTON, P110; Castro CG, 1997, J MAR RES, V55, P321, DOI 10.1357/0022240973224436; Crespo BG, 2007, HARMFUL ALGAE, V6, P686, DOI 10.1016/j.hal.2007.02.007; Crespo BG, 2006, HARMFUL ALGAE, V5, P770, DOI 10.1016/j.hal.2006.03.006; Erard-Le Denn E., 1997, EFFLORESCENCES TOXIQ, V13, P52; FIGUEIRAS FG, 1991, J PLANKTON RES, V13, P589, DOI 10.1093/plankt/13.3.589; Figueiras FG, 2002, HYDROBIOLOGIA, V484, P121, DOI 10.1023/A:1021309222459; Figueroa RI, 2006, J PHYCOL, V42, P67, DOI 10.1111/j.1529-8817.2006.00181.x; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Figueroa RI, 2005, J PHYCOL, V41, P370, DOI 10.1111/j.1529-8817.2005.04150.x; Figueroa RI, 2008, AQUAT MICROB ECOL, V52, P13, DOI 10.3354/ame01206; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; FRAGA S, 1988, ESTUAR COAST SHELF S, V27, P349, DOI 10.1016/0272-7714(88)90093-5; Fraga S., 1989, P281; FRAGA S, 1984, ICES SPAT M CAUS DYN; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Garcés E, 2004, J PLANKTON RES, V26, P637, DOI 10.1093/plankt/fbh065; Garcés E, 2002, J PLANKTON RES, V24, P681, DOI 10.1093/plankt/24.7.681; Giacobbe MG, 1996, ESTUAR COAST SHELF S, V42, P539, DOI 10.1006/ecss.1996.0035; Kudela Raphael, 2005, Oceanography, V18, P184; Laabir M, 2007, AQUAT LIVING RESOUR, V20, P51, DOI 10.1051/alr:2007015; Lav'in A., 1991, Informes T'ecnicos del Instituto Espa~nol de Oceanograf'ia, V91, P1; LINDAHL O, 1986, COMM M; Maguer JF, 2004, LIMNOL OCEANOGR, V49, P1108, DOI 10.4319/lo.2004.49.4.1108; MARGALEF M, 1956, INVESTIGACIONES PESQ, V5, P113; Margalef R., 1978, OECOL AQUATICA, V3, P97; Sordo I, 2001, ESTUAR COAST SHELF S, V53, P787, DOI 10.1006/ecss.2000.0788; STEIDINGER KA, 1981, BIOSCIENCE, V31, P814, DOI 10.2307/1308678; TILSTONE GH, 1994, MAR ECOL PROG SER, V112, P241, DOI 10.3354/meps112241; Varela M., 1992, Boletin del Instituto Espanol de Oceanografia, V8, P57; Vila M, 2005, HARMFUL ALGAE, V4, P673, DOI 10.1016/j.hal.2004.07.006; Walker L.M., 1984, P19; Yamamoto T, 2002, HARMFUL ALGAE, V1, P301, DOI 10.1016/S1568-9883(02)00029-X	51	63	70	2	27	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.	FEB	2010	57	3-4					222	234		10.1016/j.dsr2.2009.09.004	http://dx.doi.org/10.1016/j.dsr2.2009.09.004			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900008
J	Olli, K; Trunov, K				Olli, Kalle; Trunov, Karolin			Abundance and distribution of vernal bloom dinoflagellate cysts in the Gulf of Finland and Gulf of Riga (the Baltic Sea)	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Dinoflagellates; Spring bloom; Cyst formation; Sediments; Woloszynskia; Pendiniella	PERIDINIELLA-CATENATA DINOPHYCEAE; SCRIPPSIELLA-HANGOEI DINOPHYCEAE; SPRING-BLOOM; VERTICAL MIGRATION; PHYTOPLANKTON; POPULATIONS; GERMINATION; ENCYSTMENT; MORPHOLOGY; DYNAMICS	In the northern Baltic Sea, brackish water dinoflagellates Peridiniella catenata, Woloszynskia spp. and Scrippsiella hangoei form a major part of the spring bloom biomass, comparable to, or even exceeding the biomass of diatoms. The life cycle of these dinoflagellates involves a relatively short period of vegetative growth in early spring (2-3 months), followed by encystment during the first part of May, and a resting period in the form of benthic cysts. The bloom intensity of the Woloszynskia/Scrippsiella complex in the Baltic Sea is spatially variable, with peak abundances in the central and eastern Gulf of Finland, while the species are rare in the Gulf of Riga. During a field survey in late May 2004, we investigated the abundance and distribution of benthic cysts of P. catenata and Woloszynskia spp. ill surface (5 cm) sediments around the Estonian coast. The broad distribution patterns of benthic cysts reflected the overall knowledge of basin-wide planktonic phase distribution of the species. On a finer scale, sediment properties (percent of clay, organic matter content) demarked the accumulation regions of the cysts. Woloszynskia cyst abundances in the surface 5 cm sediment were Lip to 3.2 x 10(6) cysts cm(-2) and Peridiniella cyst abundances were approximately an order of magnitude less, up to 0.3 x 10(6) cysts cm(-2). (C) 2009 Elsevier Ltd. All rights reserved.	[Olli, Kalle; Trunov, Karolin] Univ Tartu, Inst Ecol & Earth Sci, EE-51005 Tartu, Estonia	University of Tartu; Tartu University Institute of Ecology & Earth Sciences	Olli, K (通讯作者)，Univ Tartu, Inst Ecol & Earth Sci, Lai 40, EE-51005 Tartu, Estonia.	kalle.olli@ut.ee	Olli, Kalle/G-5389-2010		EC [GOCE-CT-2005-003875]; Estonian Science Foundation (ETF ) [6470, 7787]	EC(European Union (EU)European Commission Joint Research Centre); Estonian Science Foundation (ETF )(Estonian Research Council)	This study was supported by the EC-funded Research Project SEED (GOCE-CT-2005-003875) and the Estonian Science Foundation (ETF 6470, 7787). We are thankful to the Institute of Aquatic Ecology (University of Latvia), Estonian Marine Institute (Tartu University) and Finnish Environment Institute, for providing the quantitative phytoplankton data. The comments of two anonymous reviewers improved the manuscript.	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					235	242		10.1016/j.dsr2.2009.09.009	http://dx.doi.org/10.1016/j.dsr2.2009.09.009			8	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900009
J	Rubino, F; Belmonte, M; Caroppo, C; Giacobbe, M				Rubino, Fernando; Belmonte, Manuela; Caroppo, Carmela; Giacobbe, Mariagrazia			Dinoflagellate cysts from surface sediments of Syracuse Bay (Western Ionian Sea, Mediterranean)	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Plankton; Resting stages; Dinoflagellates; Toxic species; Mediterranean Sea; Syracuse Bay	DINOPHYCEAE; PLANKTON; BLOOMS; WATERS; GULF	The occurrence and abundance of dinoflagellate cysts were investigated for the first time at an Ionian locality along the south-eastern coast of Sicily, subject to spring-summer harmful algal events. Thirty-four cyst morphotypes were recognized belonging to 24 taxa identified at least at the genus level. Cyst abundance in surface sediments ranged from 43 to 828 cysts g(-1) dry weight, with the highest numbers recorded at the most restricted station. Germination experiments allowed confirmation of species identification determined by cyst analysis and provided clonal Cultures of Alexandrium minutum and Gymnodinium nolleri, two of the bloom-forming species in the area. This represents the first record of G. nolleri for the Mediterranean Sea. (C) 2009 Elsevier Ltd. All rights reserved.	[Rubino, Fernando; Belmonte, Manuela; Caroppo, Carmela] CNR, Ist Ambiente Marino Costiero, I-74100 Taranto, Italy; [Giacobbe, Mariagrazia] CNR, Ist Ambiente Marino Costiero, I-98122 Messina, Italy	Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR)	Rubino, F (通讯作者)，CNR, Ist Ambiente Marino Costiero, Talossog A Cerruti,Via Roma 3, I-74100 Taranto, Italy.	rubino@iamc.cnr.it	Rubino, Fernando/GOP-0332-2022; Caroppo, Carmela/AAW-6575-2020; Belmonte, Marisol/AAG-9759-2019	CAROPPO, CARMELA/0000-0002-8316-4195; Rubino, Fernando/0000-0003-2552-2510	European Commission [GOCE-CT-2005-003875]	European Commission(European Union (EU)European Commission Joint Research Centre)	We thank Dr. R.I. Figueroa and S. Fraga (IEO Vigo, Spain) for their assistance in identifying Gymnodinium nolleri; A. Rabito and S. Di Grande (DAP, ARPA Syracuse, Italy) for their help with sampling; S. Borzi, A. Marini and F. Azzaro (IAMC-CNR of Messina, Italy) for technical assistance and nutrient data, respectively. This study was funded by the European Commission, SEED Project no.GOCE-CT-2005-003875.	AMINOT A, 1983, MANUEL ANAL CHIMIQUE, P365; Belmonte G, 1995, OLSEN INT S, P53; Blackburn S., 2005, Algal Culturing Techniques, P399; 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; Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; Dale B., 1983, P69; Ellegaard M, 1998, PHYCOLOGIA, V37, P369, DOI 10.2216/i0031-8884-37-5-369.1; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Figueroa RI, 2006, J PHYCOL, V42, P350, DOI 10.1111/j.1529-8817.2006.00191.x; GIACOBBE MG, 2006, P 5 INT C MOLL SHELL, P206; Guillard R. R. L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; 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; Morquecho L, 2004, BOT MAR, V47, P313, DOI 10.1515/BOT.2004.037; Moscatello S, 2004, SCI MAR, V68, P85, DOI 10.3989/scimar.2004.68s185; Ribeiro S, 2008, MAR MICROPALEONTOL, V68, P156, DOI 10.1016/j.marmicro.2008.01.013; Rubino F, 2009, J MARINE SYST, V78, P536, DOI 10.1016/j.jmarsys.2008.12.023; Sonneman JA, 1997, BOT MAR, V40, P149, DOI 10.1515/botm.1997.40.1-6.149; Stock CA, 2007, CONT SHELF RES, V27, P2486, DOI 10.1016/j.csr.2007.06.008; Strickland J.D.H., 1972, B FISH RES BOARD CAN, V157, P310, DOI DOI 10.1002/IROH.19700550118; Vila M, 2005, HARMFUL ALGAE, V4, P673, DOI 10.1016/j.hal.2004.07.006	22	37	39	2	14	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.	FEB	2010	57	3-4					243	247		10.1016/j.dsr2.2009.09.011	http://dx.doi.org/10.1016/j.dsr2.2009.09.011			5	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900010
J	Satta, CT; Anglès, S; Garcés, E; Lugliè, A; Padedda, BM; Sechi, N				Satta, Cecilia Teodora; Angles, Silvia; Garces, Esther; Luglie, Antonella; Padedda, Bachisio Mario; Sechi, Nicola			Dinoflagellate cysts in recent sediments from two semi-enclosed areas of the Western Mediterranean Sea subject to high human impact	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium minutum; Alexandrium catenella/tamarense complex; Dinoflagellate cysts; Diversity; Mediterranean Sea; Human impact	RECENT MARINE-SEDIMENTS; ALEXANDRIUM-MINUTUM; RESTING CYSTS; COASTAL SEDIMENTS; LIFE-HISTORY; DINOPHYCEAE; SCRIPPSIELLA; GULF; PLANKTON; WATERS	Studies were conducted on dinoflagellate cyst assemblages from two semi-enclosed areas of the Western Mediterranean Sea subject to high human impact, Arenys de Mar harbor and the Gulf of Olbia. Sediment cores were taken from seven stations (December 2006 and August 2007) in Arenys and from eight (October 2006) and ten (May 2007) stations in Olbia. Of the 42 morphotypes found in the sediments collected at the two sites, 27 were identified at the species level, representing 10 genera. The most common cysts were those of Scrippsiella trochoidea, Scrippsiella sp. 2, Gymnodiniales type 1, and Scrippsiella precaria. A number of the morphotypes had not been previously described in the literature. Total cyst abundances varied substantially between the two surveys, with an increased total density in Arenys and a decrease in Olbia. However, at the latter site, a higher abundance of cysts was recorded at more confined sampling stations. Calcareous Peridiniales, belonging to the genus Scrippsiella, dominated the cyst assemblages of both sites, while at some stations higher numbers of Gymnodiniales (Olbia) and Gonyaulacales (Arenys) were determined. Cysts of the toxic species Alexandrium minutum and A. catenella/tamarense were also detected. A. minutum was present at both sites whereas A. catenella/tamarense was found only in Olbia. Peridinium quinquecorne was recovered in the sediments of both sites. In Olbia, cysts of this species were present at high densities and were detected even in deep sediments. Species such as Pentapharsodinium cf. tyrrhenicum, Scrippsiella crystallina, S. lachrymosa, S. precaria, S. trochoidea, Protoperidinium avellanum, P. claudicans, P. compressum, P. conicum, P. cf. minutum, P. oblongum, P pentagonum, P. subinerme, and Zygabikodinium lenticulatum were not detected as motile stages in the study areas. The results of this study, the first on dinoflagellate cyst assemblages at these two sites, further our knowledge of cyst diversity and confirm the importance of embayments and hydrographically confined areas as reservoirs for planktonic dinoflagellates. (C) 2009 Elsevier Ltd. All rights reserved.	[Satta, Cecilia Teodora; Luglie, Antonella; Padedda, Bachisio Mario; Sechi, Nicola] Univ Sassari, Dipartimento Sci Bot Ecol & Geol, I-07100 Sassari, Italy; [Angles, Silvia; Garces, Esther] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain	University of Sassari; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM)	Satta, CT (通讯作者)，Univ Sassari, Dipartimento Sci Bot Ecol & Geol, Via Piandanna 4, I-07100 Sassari, Italy.	ctsatta@uniss.it	Satta, Cecilia Teodora/AAF-6417-2020; Angles, Silvia/B-9469-2011; Luglie, Antonella/M-4321-2015; Garces, Esther/C-5701-2011	Angles, Silvia/0000-0003-0529-7504; Luglie, Antonella/0000-0001-6382-4208; Padedda, Bachisio Mario/0000-0002-0988-5613; SATTA, Cecilia Teodora/0000-0003-0130-9432; Garces, Esther/0000-0002-2712-501X	EU [GOCE-CT-2005-003875]; Spanish Ministry of Science and Innovation	EU(European Union (EU)); Spanish Ministry of Science and Innovation(Ministry of Science and Innovation, Spain (MICINN)Spanish Government)	The authors thank K. Van Lenning, X. Novell, and the personnel at the Creu Roja of Arenys de Mar for their help with the fieldwork; I. Bravo, M. Montresor, and J. Lewis for their kind and useful suggestions; and J.M. Fortuno for his technical help during SEM analyses. This study was financed by the EU-funded Research Project SEED (GOCE-CT-2005-003875). E. Garces work is supported by a Ramon y Cajal contract from the Spanish Ministry of Science and Innovation.	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					256	267		10.1016/j.dsr2.2009.09.013	http://dx.doi.org/10.1016/j.dsr2.2009.09.013			12	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR		Green Submitted			2025-03-11	WOS:000275943900012
J	Erdner, DL; Percy, L; Keafer, B; Lewis, J; Anderson, DM				Erdner, D. L.; Percy, L.; Keafer, B.; Lewis, J.; Anderson, D. M.			A quantitative real-time PCR assay for the identification and enumeration of <i>Alexandrium</i> cysts in marine sediments	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Quantitative PCR; Ribosomal; Toxic dinoflagellate; Saxitoxins; Algal blooms; Red tides	LIVING DINOFLAGELLATE CYSTS; HARMFUL ALGAL BLOOMS; FUNDYENSE BLOOMS; UNITED-STATES; GULF; QUANTIFICATION; TAMARENSE; MAINE; DNA; DINOPHYCEAE	Harmful algal blooms (HABs) are a global problem that affects both human and ecosystem health. One of the most serious and widespread HAB poisoning syndromes is paralytic shellfish poisoning, commonly caused by Alexandrium spp. dinoflagellates. Like many toxic dinoflagellates, Alexandrium produces resistant resting cysts as part of its life cycle. These cysts play a key role in bloom initiation and decline, as well as dispersal and colonization of new areas. Information on cyst numbers and identity is essential for understanding and predicting blooms, yet comprehensive cyst surveys are extremely time- and labor-intensive. Here we describe the development and validation of a quantitative real-time PCR (qPCR) technique for the enumeration of cysts of A. tamarense of the toxic North American/Group I ribotype. The method uses a cloned fragment of the large subunit ribosomal RNA gene as a standard for cyst quantification, with an experimentally determined conversion factor of 28,402 +/- 6152 LSU ribosomal gene copies per cyst. Tests of DNA extraction and PCR efficiency show that mechanical breakage is required for adequate cyst lysis, and that it was necessary to dilute Our DNA extracts 50-fold in order to abolish PCR inhibition from compounds co-extracted from the sediment. The resulting assay shows a linear response over 6 orders of magnitude and can reliably quantify >= 10 cysts/cm(3) sediment. For method validation, 129 natural sediment samples were split and analyzed in parallel, using both the qPCR and primulin-staining techniques. Overall, there is a significant correlation (p < 0.001) between the cyst abundances determined by the two methods, although the qPCR counts tend to be lower than the primulin values. This underestimation is less Pronounced in those samples collected from the top 1 cm of sediment, and more pronounced in those derived from the next 1-3 cm of the core. These differences may be due to the condition of the cysts in the different layers, as the top I cm contains more recent cysts while those in the next 1-3 cm may have been in the sediments for many years. Comparison of the cyst densities obtained by both methods shows that a majority (56.6%) of the values are within a two-fold range of each other and almost all of the samples (96.9%) are within an order of magnitude. Thus, the qPCR method described here represents a promising alternative to primulin-staining for the identification and enumeration of cysts. The qPCR method has a higher throughput, enabling the extraction and assay of 24 samples in the time required to process and count 8-10 samples by primulin-staining. Both methods require prior expertise, either in taxonomy or molecular biology. Fewer person-hours per sample are required for qPCR, but primulin-staining has lower reagent costs. The qPCR method might be more desirable for large-scale cyst mapping, where large numbers of samples are generated and a higher sample analysis rate is necessary. While the qPCR and primulin-staining methods generate similar data, the choice of counting method may be most influenced by the practical issue of the different relative costs of labor and materials between the two methods. (C) 2009 Elsevier Ltd. All rights reserved.	[Erdner, D. L.] Univ Texas, Inst Marine Sci, Port Aransas, TX 78373 USA; [Percy, L.; Lewis, J.] Univ Westminster, Sch Biosci, London W1W 6UW, England; [Keafer, B.; Anderson, D. M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA	University of Texas System; University of Westminster; Woods Hole Oceanographic Institution	Erdner, DL (通讯作者)，Univ Texas, Inst Marine Sci, 750 Channel View Dr, Port Aransas, TX 78373 USA.	derdner@mail.utexas.edu	Erdner, Deana/C-4981-2008	Erdner, Deana/0000-0002-1736-8835	NSF [OCE-0402707, OCE-0430724]; NOAA [NA04-NOS4780274]; NIEHS [1P50-ES01274201]; EU [GOCE-CT-2005-003875]	NSF(National Science Foundation (NSF)); NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); NIEHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); EU(European Union (EU))	We thank the scientists and crew of the R/V Cape Hatteras for their assistance with sample collection, particularly C. Pilskaln, J. Brown, K. Norton, and J. Lawrence and colleagues. We also thank E. Harrison and L. McCauley for processing and counting numerous cyst samples. This work was supported by NSF GrantOCE-0402707 (DLE, DMA), NOAA ECOHAB GrantNA04-NOS4780274 (DMA, BAK), NSF/NIEHS Centers for Oceans and Human Health NSF GrantOCE-0430724 and NIEHS Grant1P50-ES01274201 (DMA, DLE) and EU SEED GrantGOCE-CT-2005-003875 (JL, LP).	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					279	287		10.1016/j.dsr2.2009.09.006	http://dx.doi.org/10.1016/j.dsr2.2009.09.006			9	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR	20368759	Green Accepted			2025-03-11	WOS:000275943900014
J	Penna, A; Battocchi, C; Garcés, E; Anglès, S; Cucchiari, E; Totti, C; Kremp, A; Satta, C; Giacobbe, MG; Bravo, I; Bastianini, M				Penna, Antonella; Battocchi, Cecilia; Garces, Esther; Angles, Silvia; Cucchiari, Emellina; Totti, Cecilia; Kremp, Anke; Satta, Cecilia; Giacobbe, Maria Grazia; Bravo, Isabel; Bastianini, Mauro			Detection of microalgal resting cysts in European coastal sediments using a PCR-based assay	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						HAB species; Mediterranean Sea; PCR; Ribosomal genes; Resting stages; Sediments	REAL-TIME PCR; GYMNODINIUM-CATENATUM; ALEXANDRIUM-MINUTUM; SCRIPPSIELLA-HANGOEI; DINOFLAGELLATE CYSTS; MEDITERRANEAN SEA; RIBOSOMAL DNA; DINOPHYCEAE; IDENTIFICATION; QUANTIFICATION	A PCR-based assay was developed and applied to sediment and sediment trap samples for the detection of different cysts belonging to dinoflagellates and raphidophytes in European coastal areas. Oligonucleotide primers were designed based on the ITS-5.8S and LSU ribosomal gene sequences. The specificity and sensitivity of the PCR assay were assessed using genomic DNA from clonal cultures, plasmid copy number of cloned target sequences, as well as from sediment samples. Qualitative PCR determinations of different cysts in sediment and sediment trap samples were compared to taxonomic examinations by light microscopy. This molecular methodology permitted a fast and specific detection of target cysts in sediment samples. We also detected dinoflagellate and raphidophyte cysts at concentrations not detectable by microscopic methods or that are difficult to identify. The results given by molecular and microscopic methods were comparable. However, higher values of positive detection for target cysts were obtained by PCR than with microscopy. Some taxa were detected in 100% of the samples using PCR, while others were only found in 10% of the samples. The data obtained in this study showed that the PCR-based method is a valid tool for cyst identification in marine sediments. (C) 2009 Elsevier Ltd. All rights reserved.	[Penna, Antonella; Battocchi, Cecilia] Univ Urbino, Dept Biomol Sci, I-61100 Pesaro, Italy; [Garces, Esther; Angles, Silvia] CSIC, Inst Ciencies Mar, E-08003 Barcelona, Spain; [Cucchiari, Emellina; Totti, Cecilia] Univ Politecn Marche, Dipartimento Sci Mare, I-60131 Ancona, Italy; [Kremp, Anke] Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland; [Satta, Cecilia] Univ Sassari, Dip Bot & Ecol Vegetale, I-07100 Sassari, Italy; [Giacobbe, Maria Grazia] CNR, Ist Ambiente Marino Costiero, I-98122 Messina, Italy; [Bravo, Isabel] Inst Espanol Oceanog, Vigo 36200, Spain; [Bastianini, Mauro] CNR ISMAR, Ist Sci Marine, I-30122 Venice, Italy	University of Urbino; Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Marche Polytechnic University; University of Helsinki; University of Sassari; Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); Spanish Institute of Oceanography; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR)	Penna, A (通讯作者)，Univ Urbino, Dept Biomol Sci, Viale Trieste 296, I-61100 Pesaro, Italy.	antonella.penna@uniurb.it	Satta, Cecilia Teodora/AAF-6417-2020; Kremp, Anke/I-8139-2013; Bravo, Isabel/D-3147-2012; Garces, Esther/C-5701-2011; CNR, Ismar/P-1247-2014; TOTTI, Cecilia Maria/A-9178-2016; Angles, Silvia/B-9469-2011	Bravo, Isabel/0000-0003-3764-745X; Garces, Esther/0000-0002-2712-501X; CNR, Ismar/0000-0001-5351-1486; TOTTI, Cecilia Maria/0000-0002-1532-6009; Bastianini, Mauro/0000-0001-6758-4192; Angles, Silvia/0000-0003-0529-7504; SATTA, Cecilia Teodora/0000-0003-0130-9432	EU [GOCE-CT-2005-003875]; Spanish Ministry of Science and Education	EU(European Union (EU)); Spanish Ministry of Science and Education(Spanish Government)	We thank S. Casabianca and A. Casabianca for molecular analysis assistance and suggestions; S. Fraga for culture strains; S. Capellacci for technical assistance. Thanks to the two anonymous reviewers who made an effort in improving the paper. This Study was financed by the EU funded Research Project SEED (GOCE-CT-2005-003875). E. Garces was sustained by a Ramon y Cajal contract from the Spanish Ministry of Science and Education.	ADACHI M, 1994, J PHYCOL, V30, P857, DOI 10.1111/j.0022-3646.1994.00857.x; ALTSCHUL SF, 1990, J MOL BIOL, V215, P403, DOI 10.1016/S0022-2836(05)80360-2; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; Andersen P., 2003, Manual on harmful marine microalgae. 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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					288	300		10.1016/j.dsr2.2009.09.010	http://dx.doi.org/10.1016/j.dsr2.2009.09.010			13	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900015
J	Figueroa, RI; Garcés, E; Bravo, I				Isabel Figueroa, Rosa; Garces, E.; Bravo, I.			The use of flow cytometry for species identification and life-cycle studies in dinoflagellates	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Alexandrium; DNA content; Flow cytometry; Karlodinium; Sexuality	DNA-CONTENT; CYST FORMATION; SCRIPPSIELLA-HANGOEI; RESTING CYSTS; CELL-CYCLE; DINOPHYCEAE; BLOOM; POPULATIONS; SEXUALITY; DIATOM	The difficulties encountered in attempts to differentiate between dinoflagellate species of the genera Alexandrium and Karlodinium using morphological characteristics are well-known. For this reason, species of these genera were analyzed by flow cytometry to determine whether haploid DNA content served as a valid criterion for species identification. The DNA content of species often confused with each other due to their overlapping size and geographical Occurrence, such as Alexandrium ostenfeldii and the complexes Alexandrium catenella, Alexandrium tamarense, Alexandrium minutum and Alexandrium tamutum, and Karlodinium veneficum and Karlodinium armiger were analyzed. These species differed greatly in DNA content, which provided a means of distinguishing among them. The only cases of DNA overlap involved A. ostenfeldii with Alexandrium peruvianum, and A. catenella with A. tamarense, two groups not yet clearly established either morphologically or genetically. Variability in intraspecies DNA content was observed only in the species K. veneficum. Significant differences between the two A. tamarense strains analyzed were not detected, and the haploid DNA content (63 pg cell(-1)) was very different from the one reported previously for this species (103.5 pg cell(-1)), suggesting cryptic speciation within this group. Flow-cytometric analysis of field samples identified K. veneficum as the causative species of a bloom, suggesting this method as a tool to readily identify species responsible for natural blooms. Additionally, after clonal cultures had been established, cytometric analyses Corroborated the variability in the haploid DNA content of this species, (C) 2009 Elsevier Ltd. All rights reserved.	[Isabel Figueroa, Rosa; Garces, E.] CSIC, Inst Ciencies Mar, ICM, E-08003 Barcelona, Spain; [Bravo, I.] Inst Oceanog Vigo, Vigo 36200, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，CSIC, Inst Ciencies Mar, ICM, E-08003 Barcelona, Spain.	figueroa@icm.csic.es	Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011	Bravo, Isabel/0000-0003-3764-745X; Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X	EU [GOCE-CT-2005-003875]; Spanish Ministry of Education and Science	EU(European Union (EU)); Spanish Ministry of Education and Science(Spanish Government)	This research was funded by the EU Project SEED (GOCE-CT-2005-003875). R.I. Figueroa work is Supported by a I3P postdoctoral contract and E. Garces work is supported by a Ramon y Cajal grant, both from the Spanish Ministry of Education and Science. The A. ostenfeldii strain was kindly provided by Dr. L. Percy; M. Fernandez-Tejedor kindly provided samples of Karlodinium natural population; Dr. M. G. Giacobbe provided the strains CNRATAC2 and CNRAT4, and N. Sampedro the Alexandrium andersoni strain. The remaining strains belong to the culture collection of the Centro Oceanografico de Vigo and were kindly provided by S. Fraga.	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Part II-Top. Stud. Oceanogr.	FEB	2010	57	3-4					301	307		10.1016/j.dsr2.2009.09.008	http://dx.doi.org/10.1016/j.dsr2.2009.09.008			7	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	573VR					2025-03-11	WOS:000275943900016
J	Flaim, G; Rott, E; Frassanito, R; Guella, G; Obertegger, U				Flaim, Giovanna; Rott, Eugen; Frassanito, Rita; Guella, Graziano; Obertegger, Ulrike			Eco-fingerprinting of the dinoflagellate Borghiella dodgei: experimental evidence of a specific environmental niche	HYDROBIOLOGIA			English	Article; Proceedings Paper	15th Workshop of the International-Association-of-Phytoplankton-Taxonomy-and-Ecology	NOV 23-30, 2008	Golan Heights, ISRAEL	Int Assoc Phytoplankton Taxon & Ecol		Borghiella; Mycosporine-like amino acids; Cold stenothermic; Encystment; Organic requirement; Life cycle	LAKE TOVEL; AMINO-ACIDS; LIFE-CYCLE; PERIDINIUM-CINCTUM; GROWTH-RATES; COMB. NOV; TEMPERATURE; PHYTOPLANKTON; ENCYSTMENT; NITROGEN	In Lake Tovel, an oligotrophic and weakly stratified lake, the dinoflagellate Borghiella dodgei Moestrup, Hansen et Daugbjerg, showed a peculiar spatial-temporal pattern with highest abundances in the bottom of the shallow side bay (4 m) along with remarkable abundance variations from year to year. We investigated B. dodgei's growth in laboratory cultures and related results to their implication for bloom formation. B. dodgei was cultivated under different temperature, nutrient and light conditions. Growth rates, cell biovolume, cyst formation and pigment and mycosporine-like amino acids (MAAs) concentrations were determined. Experiments showed that this alga (i) had higher growth rates at low temperatures (< 7A degrees C) and high irradiance levels (similar to 250 mu mol m(-2) s(-1)), (ii) produced higher yields with organic supplements such as peptone, (iii) did not grow in the dark even with organic supplements, (iv) survived for long periods without a light source, (v) synthesised MAAs, (vi) showed an increase in cell volume with nutrient shortage and increasing temperatures (> 7A degrees C) and (vii) had high encystment rates with temperatures > 7A degrees C. These laboratory fingerprints allowed us to construct a theoretical model defining the species' niche. Borghiella needed a mixture of low temperatures, high irradiance levels and sufficient quantities of dissolved organic nitrogen to form blooms. Such a strict combination was probably a transient situation and occurred in oligotrophic Lake Tovel only in early summers followed by heavy spring rains.	[Flaim, Giovanna; Obertegger, Ulrike] IASMA Res & Innovat Ctr, Fdn Edmund Mach, Environm & Nat Resources Area, Michele Alladige, TN, Italy; [Rott, Eugen] Univ Innsbruck, Inst Bot, WG Hydrobot, A-6020 Innsbruck, Austria; [Frassanito, Rita; Guella, Graziano] Univ Trent, Dept Phys, I-38123 Povo, TN, Italy	Fondazione Edmund Mach; University of Innsbruck; University of Trento	Flaim, G (通讯作者)，IASMA Res & Innovat Ctr, Fdn Edmund Mach, Environm & Nat Resources Area, Via Mach 2-38010 S, Michele Alladige, TN, Italy.	giovanna.flaim@iasma.it	Rott, Eugen/J-4768-2012; Flaim, Giovanna/AAD-5013-2020; Guella, Graziano/A-6283-2010; Flaim, Giovanna/C-7622-2016; Obertegger, Ulrike/A-8254-2010	Guella, Graziano/0000-0002-1799-0819; Flaim, Giovanna/0000-0002-1753-5605; Obertegger, Ulrike/0000-0002-4057-9366				Alster A, 2006, FRESHWATER BIOL, V51, P1219, DOI 10.1111/j.1365-2427.2006.01543.x; Andersen RA, 1997, J PHYCOL, V33, P1, DOI 10.1111/j.0022-3646.1997.00001.x; [Anonymous], HDB MICROALGAL CULTU; [Anonymous], 1981, ESP RIC; 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Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	541UX					2025-03-11	WOS:000273447500009
J	Zonneveld, KAF; Susek, E; Fischer, G				Zonneveld, Karin A. F.; Susek, Ewa; Fischer, Gerhard			SEASONAL VARIABILITY OF THE ORGANIC-WALLED DINOFLAGELLATE CYST PRODUCTION IN THE COASTAL UPWELLING REGION OFF CAPE BLANC (MAURITANIA): A FIVE-YEAR SURVEY	JOURNAL OF PHYCOLOGY			English	Article						cysts; Dinophyta; ecology; seasonal production; sediment trap; taphonomy	ZOOPLANKTON FECAL PELLETS; SURFACE SEDIMENTS; GRAZING RATES; WEST-COAST; POLYKRIKOS-KOFOIDII; PARTICLE-FLUX; MARINE SNOW; RED-TIDE; PROTOPERIDINIUM; PHYTOPLANKTON	A 5-year sediment trap survey in the upwelling area off Cape Blanc (NW Africa) provides information on the seasonal and annual resting cyst production of dinoflagellates, their sinking characteristics and preservation potential. Strong annual variation in cyst production characterizes the region. Cyst production of generally all investigated species, including Alexandrium pseudogonyaulax (Biecheler) T. Horig. ex T. Kita et Fukuyo (cyst genus Impagidinium) and Gonyaulax spinifera (Clap. et J. Lachm.) Diesing (cyst genus Nematosphaeropsis) was enhanced with increasing upper water nutrient and trace-element concentrations. Cyst production of Lingulodinium polyedrum (F. Stein) J. D. Dodge was the highest at the transition between upwelling and upwelling-relaxation. Cyst production of Protoperidinium americanum (Gran et Braarud) Balech, Protoperidinium monospinum (Paulsen) K. A. F. Zonn. et B. Dale, and Protoperidinium stellatum (D. Wall) Balech, and heterotrophic dinoflagellates forming Brigantedinium spp. and Echinidinium aculeatum Zonn., increased most pronouncedly during upwelling episodes. Production of Protoperidinium conicum (Gran) Balech and Protoperidinium pentagonum (Gran) Balech cysts and total diatom valves were related, providing evidence of a predator-prey relationship. The export cyst-flux of E. aculeatum, P. americanum, P. monospinum, and P. stellatum was strongly linked to the flux of total diatom valves and CaCO3, whereas the export production of Echinidinium granulatum Zonn. and Protoperidinium subinerme (Paulsen) A. R. Loebl. correlated with total organic carbon, suggesting potential consumption of diatoms, prymnesiophytes, and organic matter, respectively. Sinking velocities were at least 274 m . d(-1), which is in range of the diatom- and coccolith-based phytoplankton aggregates and "slower" fecal pellets. Species-selective degradation did not occur in the water column, but on the ocean floor.	[Zonneveld, Karin A. F.; Susek, Ewa; Fischer, Gerhard] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	University of Bremen	Zonneveld, KAF (通讯作者)，Univ Bremen, Fachbereich Geowissensch 5, Postfach 330440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de			Deutsche Forschungsgemeinschaft; Cluster of Excellence at the MARUM	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Cluster of Excellence at the MARUM	This research is funded by the Deutsche Forschungsgemeinschaft as a part of European Graduate College "Proxies in Earth History" EUROPROX, Bremen University, and by the Cluster of Excellence at the MARUM. We thank two anonymous reviewers, Prof. Rex Harland, and the associate editor Michelle Wood for their constructive remarks.	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Phycol.	FEB	2010	46	1					202	215		10.1111/j.1529-8817.2009.00799.x	http://dx.doi.org/10.1111/j.1529-8817.2009.00799.x			14	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	546PN					2025-03-11	WOS:000273822800021
J	Holzwarth, U; Esper, O; Zonneveld, KAF				Holzwarth, Ulrike; Esper, Oliver; Zonneveld, Karin A. F.			Organic-walled dinoflagellate cysts as indicators of oceanographic conditions and terrigenous input in the NW African upwelling region	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						organic-walled dinocysts; accumulation rates; aeolian dust; river discharge; upwelling; Cape Ghir; Cape Yubi; Cape Blanc	SEA-SURFACE CONDITIONS; CANARY ISLAND REGION; GYMNODINIUM-CATENATUM; EASTERN BOUNDARY; NORTHWEST AFRICA; INTERANNUAL VARIABILITY; PRODUCTIVITY GRADIENT; MARINE-PHYTOPLANKTON; SPATIAL-DISTRIBUTION; POLYKRIKOS-KOFOIDII	In order to examine the spatial distribution of organic-walled dinoflagellate cysts (dinocysts) in recent sediments related to environmental conditions in the water column, thirty-two surface sediment samples from the NW African upwelling region (20-32 degrees N) were investigated. Relative abundances of the dinocyst species show distinct regional differences allowing the separation of four hydrographic regimes. (1) In the area off Cape Ghir, which is characterized by most seasonal upwelling and river discharge, Lingulodinium machaerophorum strongly dominates the associations which are additionally characterized by cysts of Gymnodinium nolleri, cysts of Polykrikos kofoidii and cysts of Polykrikos schwartzii. (2) Off Cape Yubi, a region with increasing perennial upwelling, L. machaerophorum, Brigantedinium spp., species of the genus Impagidinium and cysts of Protoperidinium stellatum occur in highest relative abundances. (3) In coastal samples between Cape Ghir and Cape Yubi, Gymnodinium catenatum, species of the genus Impagidinium, Nematosphaeropsis labyrinthus, Operculodinium centrocarpum, cysts of P. stellatum and Selenopemphix nephroides determine the species composition. (4) Off Cape Blanc, where upwelling prevails perennially, and at offshore sites, heterotrophic dinocyst species show highest relative abundances. A Redundancy Analysis reveals fluvial mud, sea-surface temperature and the depth of the mixed layer in boreal spring (spring) as the most important parameters relating to the dinocyst species association. Dinocyst accumulation rates were calculated for a subset of samples using well-constrained sedimentation rates. Highest accumulation rates with up to almost 80,000 cysts cm(-2) ka(-1) were found off Cape Ghir and Cape Yubi reflecting their eutrophic upwelling filaments. A Redundancy Analysis gives evidence that primary productivity and the input of fluvial mud are mostly related to the dinocyst association. By means of accumulation rate data, quantitative cyst production of individual species can be considered independently from the rest of the association, allowing autecological interpretations. We show that a combined interpretation of relative abundances and accumulation rates of dinocysts can lead to a better understanding of the productivity conditions off NW Africa. (C) 2009 Elsevier B.V. All rights reserved.	[Holzwarth, Ulrike; Zonneveld, Karin A. F.] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [Esper, Oliver] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Holzwarth, U (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28334 Bremen, Germany.	holzwarth@uni-bremen.de		Esper, Oliver/0000-0002-4342-3471	Deutsche Forschungsgemeinschaft; University of Bremen	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); University of Bremen	Michael Marhold is acknowledged for his support in the laboratory. We thank Martin Head for accurate revision of an earlier version of this article. Three anonymous reviewers also contributed constructive and useful comments. This work was funded through the Deutsche Forschungsgemeinschaft as part of the Research Center/Excellence Cluster "The Ocean in the Earth System" of the University of Bremen.	[Anonymous], OCEANOGR MAR BIOL AN; [Anonymous], COASTAL UPWELLING B; [Anonymous], CANOCO; Barton E., 1998, The Sea: The Global Coastal Ocean. 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Palaeobot. Palynology	FEB	2010	159	1-2					35	55		10.1016/j.revpalbo.2009.10.005	http://dx.doi.org/10.1016/j.revpalbo.2009.10.005			21	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	564VK					2025-03-11	WOS:000275245800003
J	Bottein, MYD; Fuquay, JM; Munday, R; Selwood, AI; van Ginkel, R; Miles, CO; Loader, JI; Wilkins, AL; Ramsdell, JS				Bottein, Marie-Yasmine Dechraoui; Fuquay, Jennifer Maucher; Munday, Rex; Selwood, Andrew I.; van Ginkel, Roel; Miles, Christopher O.; Loader, Jared I.; Wilkins, Alistair L.; Ramsdell, John S.			Bioassay methods for detection of <i>N</i>-palmitoylbrevetoxin-B2 (BTX-B4)	TOXICON			English	Article						Brevetoxin; BTX-B2; N-palmitoylbrevetoxin-B2 (BTX-B4); Bioassay; Metabolism; Fatty acid conjugate; Neurotoxic shellfish poisoning	OYSTER CRASSOSTREA-VIRGINICA; RED-TIDE DINOFLAGELLATE; SENSITIVE SODIUM-CHANNELS; PTYCHODISCUS-BREVIS; NEW-ZEALAND; BREVETOXIN METABOLISM; CONTROLLED EXPOSURES; GREENSHELL MUSSELS; KARENIA-BREVIS; GYMNODINIUM	Brevetoxins (BTXs) are a class of cyclic polyether toxins produced by the dinoflagellate Karenia brevis. These substances are subject to extensive conjugative metabolism in shellfish. BTX-B forms a conjugate with cysteine and is oxidized and reduced to yield BTXB2, which is further modified by fatty acid addition via cysteine amide linkage to give biologically active brevetoxin metabolites. In this study, we evaluated the commonly used in vitro (ELISA, radioimmunoassay, receptor binding assay and N2A cytotoxicity assay) and in vivo mouse brevetoxin bioassays for the detection of the brevetoxin fatty acid conjugate N-palmitoylBTX-B2, and compared the results to those for dihydroBTX-B and BTX-B2. The receptor binding assay for N-palmitoylBTX-B2 showed comparable sensitivity to that for dihydroBTX-B, and an 11-fold higher sensitivity than for BTX-B2. Although the ELISA showed similarly high sensitivity to dihydroBTX-B and BTX-B2, with EC50 values of ca. 0.26 ng/ml, it was 23 times less sensitive to N-palmitoylBTX-B2. On the other hand, the N2A cytotoxicity assay was highly sensitive to N-palmitoylBTX-B2, with an EC50 of 0.15 ng/ml, but was 12- and 40-fold less sensitive to dihydroBTX-B and BTX-B2, respectively. The relative sensitivity of the N2A cytotoxicity assay for each of these metabolites paralleled that of the mouse bioassay (relative LD50 values 1:20:30 for N-palmitoylBTX-B2:dihydroBTX-B:BTX-B2). We conclude that the most sensitive bioassay for dihydroBTX-B and BTX-B2 is the ELISA, whereas the N2A cytotoxicity assay is most sensitive for N-palmitoylBTX-B2. Published by Elsevier Ltd.	[Bottein, Marie-Yasmine Dechraoui; Fuquay, Jennifer Maucher; Ramsdell, John S.] NOAA, Marine Biotoxins Program, Ctr Coastal Environm Hlth & Biomol Res, Natl Ocean Serv, Charleston, SC 29412 USA; [Munday, Rex; Miles, Christopher O.; Loader, Jared I.] Ruakura Agr Res Ctr, Hamilton, New Zealand; [Selwood, Andrew I.; van Ginkel, Roel] Cawthron Inst, Nelson, New Zealand; [Miles, Christopher O.; Wilkins, Alistair L.] Natl Vet Inst, N-0106 Oslo, Norway; [Wilkins, Alistair L.] Univ Waikato, Dept Chem, Hamilton 3240, New Zealand	National Oceanic Atmospheric Admin (NOAA) - USA; National Ocean Service, NOAA; AgResearch - New Zealand; Cawthron Institute; Norwegian Veterinary Institute; University of Waikato	Ramsdell, JS (通讯作者)，NOAA, Marine Biotoxins Program, Ctr Coastal Environm Hlth & Biomol Res, Natl Ocean Serv, Charleston, SC 29412 USA.	john.ramsdell@noaa.gov	Selwood, Andrew/AAP-7550-2020; Bottein, Marie-Yasmine/J-8851-2018	Dechraoui Bottein, Marie-Yasmine/0000-0002-6468-7222; Selwood, Andrew/0000-0003-1399-8028	New Zealand Foundation [AGRX0402]; Marie Curie International Incoming Fellowship [FP7/2007-2013, 221117]	New Zealand Foundation(New Zealand Foundation for Research, Science and Technology); Marie Curie International Incoming Fellowship(European Union (EU))	We thank M. Poli (U.S. Army Medical Research Institute of Infectious Diseases, FT Detrick. Washington D.C) for supplying anti-BTX antibodies, P. Gread (University of Waikato Spectrometry Facility) for obtaining HR-MS spectra, and A.D. Hawkes (AgResearch) for accurate weighing of the products. This work was supported in part by a New Zealand Foundation for Science and Technology Post-doctoral Fellowship (Contract AGRX0402) (to J.I.L.) and a Marie Curie International Incoming Fellowship within the 7th European Community Framework Programme (FP7/2007-2013) under grant agreement No. 221117 (to C.O.M.).	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J	van Soelen, EE; Lammertsma, EI; Cremer, H; Donders, TH; Sangiorgi, F; Brooks, GR; Larson, RA; Damsté, JSS; Wagner-Cremer, F; Reichart, GJ				van Soelen, E. E.; Lammertsma, E. I.; Cremer, H.; Donders, T. H.; Sangiorgi, F.; Brooks, G. R.; Larson, R. A.; Damste, J. S. Sinninghe; Wagner-Cremer, F.; Reichart, G. J.			Late Holocene sea-level rise in Tampa Bay: Integrated reconstruction using biomarkers, pollen, organic-walled dinoflagellate cysts, and diatoms	ESTUARINE COASTAL AND SHELF SCIENCE			English	Article						Palaeoenvironments; Holocene; Estuaries; Sea-level changes; Florida	VEGETATION HISTORY; CONTINENTAL-SHELF; CENTRAL FLORIDA; ALKENONE; SOUTH; CALIBRATION; RECORD; DIOLS; OCEAN	A suite of organic geochemical, micropaleontological and palynological proxies was applied to sediments from Southwest Florida, to study the Holocene environmental changes associated with sea-level rise. Sediments were recovered from Hillsborough Bay, part of Tampa Bay, and studied using biomarkers, pollen, organic-walled dinoflagellate cysts and diatoms. Analyses show that the site flooded around 7.5 ka as a consequence of Holocene transgression, progressively turning a fresh/brackish marl-marsh into a shallow, restricted marine environment. Immediately after the marine transgression started, limited water circulation and high amounts of runoff caused stratification of the water column. A shift in dinocysts and diatom assemblages to more marine species, increasing concentrations of marine biomarkers and a shift in the Diol Index indicate increasing salinity between 7.5 ka and the present, which is likely a consequence of progressing sea-level rise. Reconstructed sea surface temperatures for the past 4 kyrs are between 25 and 26 degrees C, and indicate stable temperatures during the Late Holocene. A sharp increase in sedimentation rate in the top similar to 50 cm of the core is attributed to human impact. The results are in agreement with parallel studies from the area, but this study further refines the environmental reconstructions having the advantage of simultaneously investigating changes in the terrestrial and marine environment. (C) 2009 Elsevier Ltd. All rights reserved.	[van Soelen, E. E.; Damste, J. S. Sinninghe; Reichart, G. J.] Univ Utrecht, Dept Earth Sci Geochem, Fac Geosci, NL-3584 CD Utrecht, Netherlands; [Lammertsma, E. I.; Sangiorgi, F.; Wagner-Cremer, F.] Univ Utrecht, Inst Environm Biol, Fac Sci, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Cremer, H.; Donders, T. H.] Geol Survey Netherlands, NL-3508 TA Utrecht, Netherlands; [Brooks, G. R.; Larson, R. A.] Eckerd Coll, Dept Marine Sci, St Petersburg, FL 33733 USA; [Damste, J. S. Sinninghe] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, NL-1790 AB Den Burg, Netherlands; [Reichart, G. J.] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	Utrecht University; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	van Soelen, EE (通讯作者)，POB 80-021, NL-3508 TA Utrecht, Netherlands.	e.vansoelen@geo.uu.nl	Donders, Timme/J-5044-2012; Reichart, Gert-Jan/N-6308-2018; Sinninghe Damste, Jaap/F-6128-2011; Wagner-Cremer, Friederike/B-4225-2009	Reichart, Gert-Jan/0000-0002-7256-2243; Sinninghe Damste, Jaap/0000-0002-8683-1854; Sangiorgi, Francesca/0000-0003-4233-6154; Wagner-Cremer, Friederike/0000-0002-8119-3558; Donders, Timme/0000-0003-4698-3463	Utrecht University HIPO	Utrecht University HIPO	A Utrecht University HIPO grant to Friederike Wagner-Cremer, Stefan Dekker and Gert-Jan Reichart provided the funding for this research. Gijs Nobbe and Natasja Welters are acknowledged for analytical assistance. Thomas Cronin is thanked for providing C-14 dates for this core. Samples were kindly provided by the USGS.	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Coast. Shelf Sci.	JAN 20	2010	86	2					216	224		10.1016/j.ecss.2009.11.010	http://dx.doi.org/10.1016/j.ecss.2009.11.010			9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	547EE		Green Published			2025-03-11	WOS:000273867900007
J	Gussone, N; Zonneveld, K; Kuhnert, H				Gussone, Nikolaus; Zonneveld, Karin; Kuhnert, Henning			Minor element and Ca isotope composition of calcareous dinoflagellate cysts of cultured <i>Thoracosphaera heimii</i>	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Thoracosphaera heimii; SST proxy; calcium isotopes; Mg/Ca; Sr/Ca; U/Ca; biomineralisation	BENTHIC FORAMINIFERAL MG/CA; SEA-SURFACE TEMPERATURE; UPPER WATER COLUMN; PLANKTONIC-FORAMINIFERA; EQUATORIAL ATLANTIC; EMILIANIA-HUXLEYI; CALCIUM-CARBONATE; LIFE-CYCLE; FRACTIONATION; RATIOS	We investigated the influences of temperature, salinity and pH on the calcium isotope as well as trace and minor element (uranium, strontium, magnesium) to Ca ratios on calcium carbonate cysts of the calcareous dinoflagellate species Thoracosphaera heimii grown in laboratory cultures. The natural habitat of this species is the photic zone (preferentially at the chlorophyll maximum depth) of temperate to tropical oceans, and it is abundant in deep-sea sediments over the entire Cenozoic. In our experiments, temperatures ranged from 12 to 30 degrees C, salinity from 36.5 to 38.8 and pH from 7.9 to 8.4. The delta(44/40) Ca of T. heimii cysts resembles that of other marine calcifiers, including coccolithophores, foraminifers and corals. However, its temperature sensitivity is considerably smaller and statistically insignificant, and T heimii might serve as a recorder of changes in seawater delta Ca-44/40 over geologic time. The Sr/Ca ratios of T heimii cysts show a pronounced temperature sensitivity (0.016 mmol/mol degrees C-1) and have the potential to serve as a palaeo-sea surface temperature proxy. No clear temperature- and pH-dependences were observed for Mg/Ca. U/Ca seems to be influenced by temperature and pH, but the correlations change sign at 23 degrees C and pH 8.2, respectively. (C) 2009 Elsevier B.V. All rights reserved.	[Gussone, Nikolaus] Univ Munster, Inst Mineral, D-48149 Munster, Germany; [Gussone, Nikolaus; Zonneveld, Karin; Kuhnert, Henning] Univ Bremen, D-28359 Bremen, Germany	University of Munster; University of Bremen	Gussone, N (通讯作者)，Univ Munster, Inst Mineral, Corrensstr 24, D-48149 Munster, Germany.	nikolaus.gussone@uni-muenster.de		, Nikolaus/0000-0002-3390-1118; Kuhnert, Henning/0000-0001-5242-4495	Deutsche ForschungsGemeinschaft; International Graduate College;  [GU 1035/2-1]	Deutsche ForschungsGemeinschaft(German Research Foundation (DFG)); International Graduate College; 	We greatly appreciate the constructive and helpful comments of P. DeMenocal and two anonymous reviewers. For support in the laboratory, we would like to thank Heidi Bayer and Jorn Hovelmann. We are grateful to A. Eisenhauer for making the TIMS-facilities in Kiel available for test measurements. This study was supported by the Deutsche ForschungsGemeinschaft as part of the DFG Research Center "The Ocean in the Earth System" (MARUM) and grant GU 1035/2-1 as well as the International Graduate College "EUROPROX."	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Sci. Lett.	JAN 15	2010	289	1-2					180	188		10.1016/j.epsl.2009.11.006	http://dx.doi.org/10.1016/j.epsl.2009.11.006			9	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	551AU					2025-03-11	WOS:000274178000018
J	Riding, JB; Westermann, GEG; Darbyshire, DPF				Riding, James B.; Westermann, Gerd E. G.; Darbyshire, D. P. Fiona			New evidence for the age of the Athol Formation (Middle Jurassic; Bajocian) in the Tusk-1 and Tusk-2 wells, offshore Carnarvon Basin, Western Australia	ALCHERINGA			English	Article						ammonites; palynomorphs; strontium isotope stratigraphy; Middle Jurassic; Bajocian; Laeviuscula Chronozone; Western Australia; taxonomy; biostratigraphy	NEWMARRACARRA LIMESTONE; CHRONOLOGY; AMMONITES	The co-occurrence of ammonites with palynomorphs in the Athol Formation of the Tusk-1 and Tusk-2 wells drilled in the offshore Carnarvon Basin, Western Australia confirms the Early Bajocian (Middle Jurassic) age of the Dissiliodinium caddaense dinoflagellate cyst Oppel Zone. The macrofaunas refine this Early Bajocian age to the early Laeviuscula Chronozone. A belemnite from the Tusk-1 well has a strontium isotope (87Sr/86Sr) ratio consistent with the biostratigraphical age. All the identifiable ammonites belong to Pseudotoites robiginosus (Crick). Pseudotoites is prominent in the Early Bajocian of the Indo-Pacific Realm, being known mainly from onshore Western Australia and the Southern Andes, together with rare occurrences in Irian Jaya (west New Guinea); somewhat surprisingly, it is also rarely present in southern Alaska. The palynofloras studied from the Tusk-1 and Tusk-2 wells contain abundant specimens of the marine dinoflagellate cyst Dissiliodinium caddaense, and are assigned to the Dissiliodinium caddaense Oppel Zone. The Athol Formation is a correlative of the Newmarracarra Limestone of the onshore Perth Basin, Western Australia; the distribution of both these units indicates a marine transgression onto the Australian block during the Early Bajocian.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England; [Westermann, Gerd E. G.] McMaster Univ, Sch Geog & Geol, Hamilton, ON L8S 4M1, Canada; [Darbyshire, D. P. Fiona] NERC, Isotope Geosci Lab, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; McMaster University; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; gwestermann@sympatico.ca; dpfd@nigl.nerc.ac.uk			NERC [bgs04003, nigl010001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], 2008, GNS SCI MISCELLANEOU; [Anonymous], 1987, ASS AUSTRALASIAN PAL; Arkell W.J., 1956, Monograph of the Palaeontographical Society; ARKELL WJ, 1954, PHILOS T ROY SOC B, V237, P547, DOI 10.1098/rstb.1954.0003; BIRCK JL, 1986, CHEM GEOL, V56, P73, DOI 10.1016/0009-2541(86)90111-7; CRICK W, 1894, GEOLOGICAL MAGAZINE, V4, P385; CRICK W, 1894, GEOLOGICAL MAGAZINE, V4, P434; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; Filatoff J., 1975, Palaeontographica Abteilung B Palaeophytologie, V154, P1; Hall R.L., 1980, Palaeontographica Americana, V9, P5; HALL RL, 1989, ALCHERINGA, V13, P1, DOI 10.1080/03115518908619122; Hantzpergue, 1997, BULL CENT RECH ELF E, V17, P1; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; Hillebrandt A., 1992, JURASSIC CIRCUM PACI, P247; KRUIZINGA P, 1926, JB MIJNWEZEN NEDERLA, V4, P11; MASCKE E, 1907, THESIS G AUGUST U GO; McArthur J.M., 2012, GEOLOGIC TIME SCALE, P127, DOI [10.1017/CBO9780511536045.008, DOI 10.1017/CBO9780511536045.008, 10.1016/B978-0-444-59425-9.00007-X, DOI 10.1016/B978-0-444-59425-9.00007-X]; MCARTHUR JM, 1994, TERRA NOVA, V6, P331, DOI 10.1111/j.1365-3121.1994.tb00507.x; PLAYFORD PE, 1990, ALCHERINGA, V14, P310, DOI 10.1080/03115519008619060; Spath L. F., 1939, Journal of the Royal Society of Western Australia, V25, P123; Veizer J, 1999, CHEM GEOL, V161, P59, DOI 10.1016/S0009-2541(99)00081-9; Visser W. A., 1962, Verhandelingen van het Geologisch-Mijnbouwkundig Genootschap voor Nederland en Kolonien, V20, P1; Westermann G. E. G., 1969, Bull. Am. Paleont., V57, P1; Westermann G. E. G., 1964, Palaeontographica, VA124, P33; WESTERMANN G E G, 1970, Bulletins of American Paleontology, V57, P231; Westermann G.E.G., 1979, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V164, P85; WESTERMANN GEG, 1988, PALAEONTOLOGY, V31, P295; [No title captured]	28	8	10	0	2	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0311-5518			ALCHERINGA	Alcheringa		2010	34	1					21	35	PII 917775515	10.1080/03115510903277824	http://dx.doi.org/10.1080/03115510903277824			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	560MN		Green Accepted			2025-03-11	WOS:000274906900003
J	Vajda, V; Raine, JI				Vajda, Vivi; Raine, J. Ian			A palynological investigation of plesiosaur-bearing rocks from the Upper Cretaceous Tahora Formation, Mangahouanga, New Zealand	ALCHERINGA			English	Article						New Zealand; Mangahouanga; Campanian; Maastrichtian; high latitude; palaeoclimate; palynology; plesiosaur; dinosaur	NORTH-ISLAND; SOUTH ISLAND; HAWKES BAY; DINOFLAGELLATE BIOSTRATIGRAPHY; MAUNGATANIWHA SANDSTONE; FAMILY MOSASAURIDAE; MOANASAURUS; BIVALVE; SPORES; RECORD	High-palaeolatitude plesiosaur, mosasaur and, more rarely, dinosaur fossils are well known from the Maungataniwha Sandstone Member of the Tahora Formation in Mangahouanga Stream, Hawkes Bay, New Zealand. A palynological investigation of strata exposed along Mangahouanga Stream and of transported boulders hosting vertebrate fossils reveals well-preserved assemblages dominated by terrestrial pollen and spores but also including marine dinoflagellate cysts in some samples. The palynofacies are strongly dominated by wood fragments including charcoal; one outcrop sample and the sample taken from a boulder hosting plesiosaur vertebrae contain entirely terrestrially derived palynoassemblages, suggesting a freshwater habitat for at least some of the plesiosaurs. The host unit spans the Santonian to lowermost Maastrichtian, while the key pollen taxa Nothofagidites senectus and Tricolpites lilliei, together with the dinocyst Isabelidinium pellucidum and the megaspore Grapnelispora evansii, indicate a late Campanian to early Maastrichtian age for the fossiliferous boulders. The palynoflora indicates a mixed local vegetation dominated by podocarp conifers and angiosperms with a significant tree-fern subcanopy. The presence of taxa with modern temperate distributions, such as Nothofagus (southern beech), Proteaceae and Cyatheaceae (tree-ferns), indicates a mild-temperate climate and lack of severe winter freezing during the latest Cretaceous, providing an ecosystem that most probably made it possible for polar dinosaurs to overwinter in this part of the world.	[Vajda, Vivi] Lund Univ, Div Geol, Dept Earth & Ecosyst Sci, Lund, Sweden; [Raine, J. Ian] GNS Sci, Lower Hutt, New Zealand	Lund University; GNS Science - New Zealand	Vajda, V (通讯作者)，Lund Univ, Div Geol, Dept Earth & Ecosyst Sci, Lund, Sweden.	vivi.vajda@geol.lu.se; i.raine@gns.cri.nz	Raine, James/D-5124-2009; Vajda, Vivi/N-7693-2018	Vajda, Vivi/0000-0003-2987-5559; Raine, James Ian/0000-0001-5294-2102	New Zealand Foundation for Research Science and Technology (FRST); Swedish Research Council (VR) [2007-4509]; Knut and Alice Wallenberg Foundation	New Zealand Foundation for Research Science and Technology (FRST)(New Zealand Foundation for Research, Science and Technology); Swedish Research Council (VR)(Swedish Research Council); Knut and Alice Wallenberg Foundation(Knut & Alice Wallenberg Foundation)	Mrs Joan Wiffen is acknowledged for sharing her knowledge on the Mangahouanga fossil localities and introducing the sampling site to VV. The reviewers Mercedes Pramparo and Mitsuru Arai are gratefully acknowledged for their constructive criticism and comments improving this paper. This research was funded by the New Zealand Foundation for Research Science and Technology (FRST) programme 'Paleontological Collections and Databases' and the Swedish Research Council (VR) grant 2007-4509. VV is a Swedish Royal Academy of Sciences Research Fellow funded through the Knut and Alice Wallenberg Foundation.	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J	Willumsen, PS; Vajda, V				Willumsen, Pi Suhr; Vajda, Vivi			A new early Paleocene dinoflagellate cyst species, Trithyrodinium partridgei: its biostratigraphic significance and palaeoecology	ALCHERINGA			English	Article						Paleocene; palynology; dinoflagellate cyst; miospores; biostratigraphy; palaeoecology; New Zealand	CRETACEOUS-PALEOGENE BOUNDARY; NEW-ZEALAND; TERTIARY BOUNDARY; TRANSITION; EXTINCTION; SPORES	A palynological investigation of lower Paleocene (lower Teurian) marine sediments of the Abbotsford Formation, exposed in the Fairfield Quarry, Dunedin, New Zealand, reveals a well-preserved association of dinoflagellate cysts and miospores. Thirty-six dinoflagellate species representing 26 genera were recorded, including one new peridinioid dinoflagellate species, Trithyrodinium partridgei characterized by a three-layered wall and a distinct brown, foveolate mesophragm. Trithyrodinium partridgei has a narrow range and at Fairfield Quarry co-occurs with typical New Zealand late Danian to Selandian index species such as Glaphyrocysta perforata and Alterbidinium pentaradiatum; hence it may prove an additional useful stratigraphic marker. The terrestrial palynomorph assemblage from samples within the range of Trithyrodinium partridgei includes 36 spore-pollen species dominated by the podocarp pollen Phyllocladidites mawsonii. The presence of Nothofagidites waipawaensis and Tricolpites phillipsii confirms a Paleocene age for the assemblage. The abundance of terrestrial palynomorphs and the composition of the dinocyst assemblages suggest a marine nearshore depositional environment.	[Willumsen, Pi Suhr; Vajda, Vivi] Lund Univ, Div Geol, Dept Earth & Ecosyst Sci, SE-22362 Lund, Sweden	Lund University	Willumsen, PS (通讯作者)，Lund Univ, Div Geol, Dept Earth & Ecosyst Sci, SE-22362 Lund, Sweden.	pi.willumsen@geol.lu.se; vivi.vajda@geol.lu.se	Vajda, Vivi/N-7693-2018	Vajda, Vivi/0000-0003-2987-5559	New Zealand Marsden Fund; Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI); Carlsberg Fundation [2008-01-0404]; LUCCI centre; Swedish Royal Academy of Sciences through the Knut and Alice Wallenberg Foundation	New Zealand Marsden Fund(Royal Society of New ZealandMarsden Fund (NZ)); Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI); Carlsberg Fundation(Carlsberg Foundation); LUCCI centre; Swedish Royal Academy of Sciences through the Knut and Alice Wallenberg Foundation	This palynological study was part of a multidisciplinary research program supported by the New Zealand Marsden Fund and the Lund University Center for Studies of Carbon Cycle and Climate Interactions (LUCCI). Drs Poul Schioler, Hamid Slimani and Ian Raine are thanked for constructive critiques that considerably improved this paper. Dr Graeme J. Wilson (GNS) and Dr Ian Raine (GNS) are acknowledged for sharing their extensive knowledge of Mesozoic-Cenozoic palynology. PSW thanks Dr Alan Partridge for helpful discussions. Dr S. McLoughlin is thanked for his editorial assistance. Roger Tremain (GNS) and Erica Vry are thanked for technical assistance, Dr Simon McMillan for assistance with fieldwork during the senior author's PhD project. PSW acknowledges support from the Carlsberg Fundation (grant no. 2008-01-0404) and LUCCI centre. VV acknowledges support from the Swedish Royal Academy of Sciences through the Knut and Alice Wallenberg Foundation.	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J	López-Rodas, V; González, R; Costas, E				Lopez-Rodas, Victoria; Gonzalez, Raquel; Costas, Eduardo			The ignored stowaways: worldwide dispersion of exotic microalgae species through the biofouling recovering the ships underwater body	ANALES DE LA REAL ACADEMIA NACIONAL DE FARMACIA			English	Article						Adaptation; Biofouling; HABs; Harmful algae; Introduced species; TBT	PRE-SELECTIVE MUTATIONS; DICTYOSPHAERIUM-CHLORELLOIDES CHLOROPHYCEAE; BALLAST WATER; DINOFLAGELLATE CYSTS; PRESELECTIVE MUTATIONS; MICROCYSTIS-AERUGINOSA; COLORECTAL-CANCER; RESISTANT MUTANTS; RAPID ADAPTATION; SENSITIVITY	Invasion by introduced species cause huge environmental damage and economic (estimated in $138 billion in USA). Marine ecosystems are specially affected by introduced species of toxin-producing microalgae. Ships ballast water has been considered the major vector in dispersion of phytoplankton. However, most ships do not use ballast water. Alternatively, we propose that the biofouling recovering the underwater body of ships is the main cause of microalgal dispersion. Antifouling paints (containing tributyltin, TBT or other toxics) are used to coat the bottoms of ships to prevent biofouling. After sampling biofouling recovering the underwater body of ships we demonstrate that numerous coastal, oceanic and toxin-producing microalgae species proliferates attached on bottoms of ships directly on TBT antifouling paint. These microalgae species should be resistant variants because antifouling paints rapidly destroy sensitive wild type microalgae. Consequently, the key to explain microalgae species transport via ships biofouling is know the mechanisms that allow to these species to survive long time attached to antifouling paint. A fluctuation analysis demonstrate that genetic adaptation by rare spontaneous mutation, which occurs by chance prior to antifouling exposure is the mechanism allowing adaptation of microalgae to antifoulig paints and their dispersion in the ships biofouling. Around 3 TBT-resistant mutants per each 10(-4) wild type sensitive cells occurs in microalgal population. This assures a rapid colonization of ships bottoms to travel long-distances.	[Lopez-Rodas, Victoria; Gonzalez, Raquel; Costas, Eduardo] Univ Complutense Madrid, Fac Vet, Dept Genet Prod Anim, E-28040 Madrid, Spain; [Lopez-Rodas, Victoria; Costas, Eduardo] AlgasGen Biotecnol EBT UCM, Madrid 28040, Spain	Complutense University of Madrid	Costas, E (通讯作者)，Univ Complutense Madrid, Fac Vet, Dept Genet Prod Anim, Avda Puerta Hierro S-N, E-28040 Madrid, Spain.	ecostas@vet.ucm.es			Ministerio de Ciencia e Innovacion, Spain [CTM2008-05680-C02-02, CGL2008-00652/BOS]	Ministerio de Ciencia e Innovacion, Spain(Ministry of Science and Innovation, Spain (MICINN)Spanish Government)	Special thanks are given to Carmen Romero by micrographs and Lara de Miguel by technical support. Supported by Grants CTM2008-05680-C02-02 and CGL2008-00652/BOS (Ministerio de Ciencia e Innovacion, Spain).	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Real Acad. Nac. Farm.		2010	76	2					189	208						20	Pharmacology & Pharmacy	Science Citation Index Expanded (SCI-EXPANDED)	Pharmacology & Pharmacy	737SN					2025-03-11	WOS:000288588600001
J	Sachsenhofer, RF; Leitner, B; Linzer, HG; Bechtel, A; Coric, S; Gratzer, R; Reischenbacher, D; Soliman, A				Sachsenhofer, Reinhard F.; Leitner, Birgit; Linzer, Hans-Gert; Bechtel, Achim; Coric, Stjepan; Gratzer, Reinhard; Reischenbacher, Doris; Soliman, Ali			DEPOSITION, EROSION AND HYDROCARBON SOURCE POTENTIAL OF THE OLIGOCENE EGGERDING FORMATION (MOLASSE BASIN, AUSTRIA)	AUSTRIAN JOURNAL OF EARTH SCIENCES			English	Article						Alpine Foreland Basin; Submarine Slide; Source Rock; Palynology; Paratethys	ALPINE FORELAND BASIN; SOURCE ROCKS; DINOFLAGELLATE CYSTS; SEA; SEDIMENTS; MIOCENE; MARINE; EOCENE; BIOSTRATIGRAPHY; NANNOPLANKTON	The Eggerding Formation, typically about 45 m thick, forms part of the deep marine Oligocene succession in the Molasse Basin, which comprises from bottom to top the Schoneck (formerly "Fish Shale"), Dynow ("Bright Marlstone"), Eggerding ("Banded Marl") and Zupfing formations ("Rupelian Marl"). The Eggerding Formation and the lower part of the Zupfing Formation have been studied using core and cuttings samples and a multidisciplinary approach involving core description, geochemistry, palynology and nannopaleontology. The Dynow Formation and the lower part of the Eggerding Formation were deposited during nannoplankton zone NP23 (Martini, 1971). The transition between the Dynow and Eggerding formations is characterized by a gradual decrease in carbonate contents. The Eggerding Formation deposited in near-shore environments contains several sand layers. In contrast, the Eggerding Formation deposited along the northern slope is generally poor in sand. Its lower part consists of dark grey laminated shaly marlstone with white bands rich in coccolithophorides. TOC contents are about 5 %. The upper part of the Eggerding Formation consists of a homogenous sequence of marly shale and includes in average 1.6 % TOC. Oxygen deficient conditions prevailed during deposition of the Eggerding Formation. Marine palynomorphs are present in all samples from the Eggerding Formation, but calcareous nannoplankton is restricted to its lower part. Salinity variations are recorded in rocks of the lower part of the Eggerding Formation. The environment during deposition of its upper part was more stable. Log signatures, which are comparable over tens of kilometres, provide evidence for the lateral continuity of the Eggerding Formation deposited on the upper slope. Slope instabilities are indicated by slumps and extensive submarine slides. Sliding reached a maximum at the transition from the Eggerding to the Zupfing Formation, when locally a succession up to 70 m thick was removed from the northern slope. The slided material was redeposited either on the northern slope or at the base of the slope. The Eggerding Formation is overlain by the Zupfing Formation (NP24), consisting of clay marl up to 450 m thick. Oxygen-depleted conditions continued during deposition of the Zupfing Formation, but only the lowermost few meters of the Zupfing Formation ("Transition Zone") are rich in organic matter (1.5 % TOC). Whereas the lower part of the Eggerding Formation (TOC 1.9-6.0 %; HI up to 600 mg HC/g TOC) holds a very good source potential for oil (and gas), its upper part and the Transition Zone (TOC: similar to 1.5 %; "true" HI 500-600 mg HC/g TOC) are characterized by a good potential. Biomarker data suggest that the latter contributed significantly to the Molasse oils. In contrast, the contribution of the Dynow Formation and the lower Eggerding Formation was minor.	[Sachsenhofer, Reinhard F.; Leitner, Birgit; Bechtel, Achim; Gratzer, Reinhard; Reischenbacher, Doris] Montanuniv, Dept Appl Geosci & Geophys, A-8700 Leoben, Austria; [Linzer, Hans-Gert] Rohol Aufsuchungs AG, A-1015 Vienna, Austria; [Coric, Stjepan] Geol Survey Austria, A-1030 Vienna, Austria; [Soliman, Ali] Karl Franzens Univ Graz, Inst Earth Sci, A-8010 Graz, Austria	University of Graz	Sachsenhofer, RF (通讯作者)，Montanuniv, Dept Appl Geosci & Geophys, Peter Tunner Str 5, A-8700 Leoben, Austria.	reinhard.sachsenhofer@unileoben.ac.at	Sachsenhofer, Reinhard/KFA-6113-2024; Soliman, Ali/R-1583-2018; Bechtel, Achim/A-9885-2011	Sachsenhofer, Reinhard/0000-0002-6616-5583; Soliman, Ali/0000-0001-7366-4607; Gross, Doris/0000-0001-7442-5093; Bechtel, Achim/0000-0002-3937-8209	OAW; FWF [21414]	OAW; FWF(Austrian Science Fund (FWF))	Seismic and borehole data, samples, as well as financial support and a wealth of information were provided by Rohol-Aufsuchung AG (RAG). We also would like to thank employees of RAG including Wolfgang Nachtmann, Alan Reingruber, Andreas Smuk, Werner Tschelaut for their help. Petrel software was provided by Schlumberger free of cost within the frame of a software grant to the University of Leoben. The paper benefited from the UZAG project, a cooperation between Leoben University, Graz University and Technical University Graz. AS wishes to thank OAW and FWF (project no. 21414) for financial support.	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J	Zonneveld, KAF; Versteegh, GJM; Kasten, S; Eglinton, TI; Emeis, KC; Huguet, C; Koch, BP; de Lange, GJ; de Leeuw, JW; Middelburg, JJ; Mollenhauer, G; Prahl, FG; Rethemeyer, J; Wakeham, SG				Zonneveld, K. A. F.; Versteegh, G. J. M.; Kasten, S.; Eglinton, T. I.; Emeis, K. -C.; Huguet, C.; Koch, B. P.; de Lange, G. J.; de Leeuw, J. W.; Middelburg, J. J.; Mollenhauer, G.; Prahl, F. G.; Rethemeyer, J.; Wakeham, S. G.			Selective preservation of organic matter in marine environments; processes and impact on the sedimentary record	BIOGEOSCIENCES			English	Article							DINOFLAGELLATE CYST PRODUCTION; MADEIRA ABYSSAL-PLAIN; RESOLUTION MASS DATA; FULVIC-ACIDS; MOLECULAR CHARACTERIZATION; EQUATORIAL ATLANTIC; SURFACE SEDIMENTS; NITROGEN-FIXATION; OXIC DEGRADATION; BIOMARKER RECORD	The present paper is the result of a workshop sponsored by the DFG Research Center/Cluster of Excellence MARUM 'The Ocean in the Earth System', the International Graduate College EUROPROX, and the Alfred Wegener Institute for Polar and Marine Research. The workshop brought together specialists on organic matter degradation and on proxy-based environmental reconstruction. The paper deals with the main theme of the workshop, understanding the impact of selective degradation/preservation of organic matter (OM) in marine sediments on the interpretation of the fossil record. Special attention is paid to (A) the influence of the molecular composition of OM in relation to the biological and physical depositional environment, including new methods for determining complex organic biomolecules, (B) the impact of selective OM preservation on the interpretation of proxies for marine palaeoceanographic and palaeoclimatic reconstruction, and (C) past marine productivity and selective preservation in sediments. It appears that most of the factors influencing OM preservation have been identified, but many of the mechanisms by which they operate are partly, or even fragmentarily, understood. Some factors have not even been taken carefully into consideration. This incomplete understanding of OM breakdown hampers proper assessment of the present and past carbon cycle as well as the interpretation of OM based proxies and proxies affected by OM breakdown. To arrive at better proxy-based reconstructions 'deformation functions' are needed, taking into account the transport and diagenesis-related molecular and atomic modifications following proxy formation. Some emerging proxies for OM degradation may shed light on such deformation functions. The use of palynomorph concentrations and selective changes in assemblage composition as models for production and preservation of OM may correct for bias due to selective degradation. Such quantitative assessment of OM degradation may lead to more accurate reconstruction of past productivity and bottom water oxygenation. Given the cost and effort associated with programs to recover sediment cores for paleoclimatological studies, as well as with generating proxy records, it would seem wise to develop a detailed sedimentological and diagenetic context for interpretation of these records. With respect to the latter, parallel acquisition of data that inform on the fidelity of the proxy signatures and reveal potential diagenetic biases would be of clear value.	[Zonneveld, K. A. F.; Versteegh, G. J. M.] Fachbereich 5 Geowissensch, D-27412 Bremen, Germany; [Kasten, S.; Koch, B. P.; Mollenhauer, G.; Rethemeyer, J.] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Eglinton, T. I.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Emeis, K. -C.] Univ Hamburg, Zentrum Meeres & Klimaforsch, D-20146 Hamburg, Germany; [Huguet, C.] Univ Washington, Sch Oceanog, Seattle, WA 98195 USA; [Huguet, C.; de Leeuw, J. W.] Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands; [de Lange, G. J.; de Leeuw, J. W.; Middelburg, J. J.] Univ Utrecht, Fac Geosci, NL-3508 TA Utrecht, Netherlands; [de Leeuw, J. W.] Univ Utrecht, Fac Sci, Inst Environm Biol, NL-3508 TA Utrecht, Netherlands; [Middelburg, J. J.] Netherlands Inst Ecol, Ctr Estuarine & Marine Ecol, NL-4400 AC Yerseke, Netherlands; [Prahl, F. G.] Oregon State Univ, Coll Ocean & Atmospher Sci, Corvallis, OR 97331 USA; [Wakeham, S. G.] Skidaway Inst Oceanog, Savannah, GA 31411 USA	University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Woods Hole Oceanographic Institution; University of Hamburg; University of Washington; University of Washington Seattle; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Utrecht University; Utrecht University; Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); Oregon State University; University System of Georgia; University of Georgia; Skidaway Institute of Oceanography	Versteegh, GJM (通讯作者)，Fachbereich 5 Geowissensch, Postfach 330440, D-27412 Bremen, Germany.	versteegh@uni-bremen.de	Huguet, Carme/C-6918-2013; de Leeuw, Jan/F-6471-2011; Mollenhauer, Gesine/AAD-8167-2019; Middelburg, Jack/B-4951-2011; Rethemeyer, Janet/G-4019-2013; De Lange, Gert/B-9639-2014; Versteegh, Gerard J.M./H-2119-2011; Mollenhauer, Gesine/B-5190-2015; Koch, Boris/B-2784-2009	Middelburg, Jack/0000-0003-3601-9072; Rethemeyer, Janet/0000-0001-6698-4186; Emeis, Kay-Christian/0000-0003-0459-913X; Huguet, Carme/0000-0001-8025-2010; Eglinton, Timothy/0000-0001-5060-2155; Kasten, Sabine/0000-0001-7453-5137; De Lange, Gert/0000-0002-9420-3022; Versteegh, Gerard J.M./0000-0002-9320-3776; Mollenhauer, Gesine/0000-0001-5138-564X; Koch, Boris/0000-0002-8453-731X	DFG Research Center/Cluster of Excellence MARUM "The Ocean in the Earth System"; International Graduate College EUROPROX; Alfred Wegener Institute for Polar and Marine Research; German Science Foundation [VE486/2]	DFG Research Center/Cluster of Excellence MARUM "The Ocean in the Earth System"(German Research Foundation (DFG)); International Graduate College EUROPROX; Alfred Wegener Institute for Polar and Marine Research; German Science Foundation(German Research Foundation (DFG))	We thank Stefan Schouten for useful comments on an earlier version of the manuscript. We acknowledge generous financial support by the DFG Research Center/Cluster of Excellence MARUM "The Ocean in the Earth System", the International Graduate College EUROPROX and the Alfred Wegener Institute for Polar and Marine Research enabling the realisation of the "Workshop on Selective Preservation of Organic Matter: Processes and Impact on the Fossil Record" which formed the basis of this paper. GJMV acknowledges support by the German Science Foundation (DFG grant VE486/2).	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Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Geology	561QQ		Green Submitted, gold			2025-03-11	WOS:000274993900007
J	Brown, L; Bresnan, E; Graham, J; Lacaze, JP; Turrell, E; Collins, C				Brown, Lyndsay; Bresnan, Eileen; Graham, Jennifer; Lacaze, Jean-Pierre; Turrell, Elizabeth; Collins, Catherine			Distribution, diversity and toxin composition of the genus <i>Alexandrium</i> (Dinophyceae) in Scottish waters	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						Alexandrium; dinoflagellate cysts; LC-MS/MS; LSU; morphology; paralytic shellfish poisoning; Scottish waters; spirolides; toxin profile	MINUTUM DINOPHYCEAE; TAMARENSE DINOPHYCEAE; OSTENFELDII DINOPHYCEAE; SEQUENCE COMPARISONS; SPECIES BOUNDARIES; EAST-COAST; NORTH-EAST; SHELLFISH; IDENTIFICATION; TOXICITY	Alexandrium is detected throughout Scottish coastal waters on a near annual basis, and corresponding paralytic shellfish poisoning (PSP) toxins are found in Scottish shellfish. Previous studies at selected Scottish sites have shown diversity within the genus Alexandrium. In order to examine the distribution, diversity and toxicity of Alexandrium populations around the Scottish coast, historic cyst and cell data were compiled and cultures established from sediment and water samples. Historic data showed high cell densities of Alexandrium in Shetland, Orkney, the Western Isles and mainland east coast. Low abundances of Alexandrium cysts were observed along the west coast. Four species of Alexandrium (A. tamarense, A. ostenfeldii, A. minutum and A. tamutum) were established in laboratory culture and identified using morphological criteria. Sequencing of LSU rDNA from isolates of A. ostenfeldii, A. minutum and A. tamutum confirmed their identification and showed them to be similar to other European strains. Alexandrium tamarense, identified by morphological criteria, was observed to have a widespread distribution around the coast. Both toxin-and non toxin-producing strains of this species were isolated, suggesting the presence of A. tamarense Groups I and III. Alexandrium ostenfeldii was isolated from the east coast and Shetland Isles and was observed to produce both spirolide and PSP toxins. Alexandrium tamutum was identified from cultures isolated from Shetland and Orkney, the most northerly observation of this species to date. PSP toxins were not detected in isolates of A. minutum from the east coast and Orkney or of A. tamutum under the culture conditions used. This study has highlighted the diversity of Alexandrium in Scottish waters and reveals the requirement for temporal and regional studies on a species level in order to understand the variation in cell densities and PSP toxicity that is observed on an annual and decadal scale.	[Brown, Lyndsay; Bresnan, Eileen; Graham, Jennifer; Lacaze, Jean-Pierre; Turrell, Elizabeth; Collins, Catherine] Marine Lab, Aberdeen AB11 9DB, Scotland		Brown, L (通讯作者)，Marine Lab, 375 Victoria Rd, Aberdeen AB11 9DB, Scotland.	brownl@marlab.ac.uk						Aasen J, 2005, CHEM RES TOXICOL, V18, P509, DOI 10.1021/tx049706n; ALPERMANN T.J., 2008, P 12 INT C HARMF ALG, P51; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 1990, MAR BIOL, V104, P511, DOI 10.1007/BF01314358; [Anonymous], SCOTTISH OCEAN CLIMA; Ayres P.A., 1978, PARALYTIC SHELLFISH; Balech E., 1995, The genus Alexandrium Halim (Dinoflagellata); Beaugrand G, 2002, SCIENCE, V296, P1692, DOI 10.1126/science.1071329; Bresnan E, 2009, J SEA RES, V61, P17, DOI 10.1016/j.seares.2008.05.007; Bresnan E., 2008, P 12 INT C HARM ALG, P76; BRESNAN E, 2005, 0405 FRS; Brown J, 2001, J PLANKTON RES, V23, P105, DOI 10.1093/plankt/23.1.105; CEMBELLA AD, 1999, NAT TOXINS, V8, P1; Collins C, 2009, J PHYCOL, V45, P692, DOI 10.1111/j.1529-8817.2009.00678.x; Edwards M, 2002, MAR ECOL PROG SER, V239, P1, DOI 10.3354/meps239001; Figueroa RI, 2007, J PHYCOL, V43, P1039, DOI 10.1111/j.1529-8817.2007.00393.x; Flynn Kevin J., 2002, Harmful Algae, V1, P147, DOI 10.1016/S1568-9883(02)00028-8; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Gayoso AM, 2006, HARMFUL ALGAE, V5, P233, DOI 10.1016/j.hal.2004.12.010; Gribble KE, 2005, DEEP-SEA RES PT II, V52, P2745, DOI 10.1016/j.dsr2.2005.06.018; Guillard R. 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J. Phycol.		2010	45	4					375	393		10.1080/09670262.2010.495164	http://dx.doi.org/10.1080/09670262.2010.495164			19	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	734XB					2025-03-11	WOS:000288374100004
J	Hoppenrath, M; Yubuki, N; Bachvaroff, TR; Leander, BS				Hoppenrath, Mona; Yubuki, Naoji; Bachvaroff, Tsvetan R.; Leander, Brian S.			Re-classification of <i>Pheopolykrikos hartmannii</i> as <i>Polykrikos</i> (Dinophyceae) based partly on the ultrastructure of complex extrusomes	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						Chloroplast; Dinoflagellate; Peridinin; Polykrikoids; Taeniocyst-nematocyst complex; Ultrastructure	GYMNODINIUM-SENSU-STRICTO; FLAGELLAR APPARATUS; DINOFLAGELLATE POLYKRIKOS; MORPHOLOGY; PHYLOGENY; SCHWARTZII; KOFOIDII; CYST; NOV; SSU	Athecate, pseudocolony-forming dinoflagellates have been classified within two genera of polykrikoids, Polykrikos and Pheopolykrikos, and different views about the boundaries and composition of these genera have been expressed in the literature. The photosynthetic polykrikoid Pheopolykrikos hartmannii, for instance, was originally described within Polykrikos and is now known to branch closely with several Polykrikos species in molecular phylogenetic analyses of ribosomal gene sequences. In this study, we report the first ultrastructural data for this species and demonstrate that Ph. hartmannii has all of the features that characterize the genus Polykrikos, including the synapomorphic "taeniocystnematocyst complex". We also demonstrate that the ultrastructure of the chloroplasts in Ph. hartmannii conforms to the usual peridinin-containing chloroplasts of most photosynthetic dinoflagellates, which improves inferences about the origin(s) and evolution of photosynthesis within the genus. After taking into account all of the ultrastructural data on polykrikoids presented here and in the literature, this species is re-classified to its original status as Polykrikos hartmannii. (C) 2008 Elsevier GmbH. All rights reserved.	[Hoppenrath, Mona; Yubuki, Naoji; Leander, Brian S.] Univ British Columbia, Dept Bot, Vancouver, BC V6T 1Z4, Canada; [Hoppenrath, Mona; Yubuki, Naoji; Leander, Brian S.] Univ British Columbia, Dept Zool, Vancouver, BC V6T 1Z4, Canada; [Bachvaroff, Tsvetan R.] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA	University of British Columbia; University of British Columbia; Smithsonian Institution; Smithsonian Environmental Research Center	Hoppenrath, M (通讯作者)，DZMB, Forschungsinst Senckenberg, Sudstrand 44, D-26382 Wilhelmshaven, Germany.	mhoppenrath@senckenberg.de	Yubuki, Naoji/AAB-7775-2020	Bachvaroff, Tsvetan/0000-0003-3800-9214; Yubuki, Naoji/0009-0000-1688-0725	NSF [EF-0629624]; Tula Foundation (Centre for Microbial Diversity and Evolution); National Science and Engineering Research Council of Canada (NSERC) [283091-04]	NSF(National Science Foundation (NSF)); Tula Foundation (Centre for Microbial Diversity and Evolution); National Science and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC))	This work was supported by a postdoctoral research salary to MH and TRBLife grant (NSF #EF-0629624); a postdoctoral research salary to NY from the Tula Foundation (Centre for Microbial Diversity and Evolution); and operating funds to BSL from the National Science and Engineering Research Council of Canada (NSERC 283091-04); BSL is a fellow of the Canadian Institute for Advanced Research, Program in Integrated Microbial Biodiversity.	BRADBURY PC, 1983, J ULTRA MOL STRUCT R, V85, P24, DOI 10.1016/S0022-5320(83)90113-2; Chatton E., 1952, TRAITE ZOOL, P309; CHATTON EDOUARD, 1933, BULL SOC ZOOL FRANCE, V58, P251; Daugbjerg N, 2000, PHYCOLOGIA, V39, P302, DOI 10.2216/i0031-8884-39-4-302.1; Dodge J.D., 1982, MARINE DINOFLAGELLAT, DOI DOI 10.37543/OCEANIDES.V25I1.79; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; Fensome R.A., 1993, Micropaleontology Press Special Paper; Greuet C., 1987, Botanical Monographs (Oxford), V21, P119; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Hansen G, 2005, PHYCOL RES, V53, P169, DOI 10.1111/j.1440-183.2005.00383.x; Hansen G, 2000, PHYCOLOGIA, V39, P365, DOI 10.2216/i0031-8884-39-5-365.1; Hansen G, 2001, J PHYCOL, V37, P612, DOI 10.1046/j.1529-8817.2001.037004612.x; Hoppenrath M, 2007, PROTIST, V158, P209, DOI 10.1016/j.protis.2006.12.001; Hoppenrath M, 2007, J PHYCOL, V43, P366, DOI 10.1111/j.1529-8817.2007.00319.x; Hoppenrath M, 2009, BMC EVOL BIOL, V9, DOI 10.1186/1471-2148-9-116; HULBURT EM, 1957, BIOL BULL-US, V112, P196, DOI 10.2307/1539198; Kim KY, 2008, PHYCOL RES, V56, P89, DOI 10.1111/j.1440-1835.2008.00489.x; MARTIN G. W., 1929, BOT GAZ, V87, P556, DOI 10.1086/333960; MATSUOKA K, 1986, J PLANKTON RES, V8, P811, DOI 10.1093/plankt/8.4.811; Nagai S, 2002, PHYCOLOGIA, V41, P319, DOI 10.2216/i0031-8884-41-4-319.1; REYNOLDS ES, 1963, J CELL BIOL, V17, P208, DOI 10.1083/jcb.17.1.208; Saldarriaga JF, 2004, EUR J PROTISTOL, V40, P85, DOI 10.1016/j.ejop.2003.11.003; Saldarriaga JF, 2001, J MOL EVOL, V53, P204, DOI 10.1007/s002390010210; Sournia A., 1986, Introduction, Cyanophycees, Dictyophycees, Raphidophycees, P219; TAKAHASHI K, 1985, J RADIO RES LAB, V32, P129; WESTFALL JA, 1983, J CELL SCI, V63, P245; ZIMMERMANN WALTER, 1930, ZEITSCHR BOT, V23, P419	27	36	37	1	23	ELSEVIER GMBH, URBAN & FISCHER VERLAG	JENA	OFFICE JENA, P O BOX 100537, 07705 JENA, GERMANY	0932-4739	1618-0429		EUR J PROTISTOL	Eur. J. Protistol.	JAN	2010	46	1					29	37		10.1016/j.ejop.2009.08.003	http://dx.doi.org/10.1016/j.ejop.2009.08.003			9	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	576XG	19767184				2025-03-11	WOS:000276182800004
S	Howe, JA; Harland, R; Cottier, FR; Brand, T; Willis, KJ; Berge, JR; Grosfjeld, K; Eriksson, A		Howe, JA; Austing, WEN; Forwick, M; Paetzel, M		Howe, John A.; Harland, Rex; Cottier, Finlo R.; Brand, Tim; Willis, Kate J.; Berge, Jorgen R.; Grosfjeld, Kari; Eriksson, Anita			Dinoflagellate cysts as proxies for palaeoceanographic conditions in Arctic fjords	FJORD SYSTEMS AND ARCHIVES	Geological Society Special Publication		English	Article; Book Chapter							VERTICAL MIGRATION; LATE QUATERNARY; ATLANTIC WATER; KOLJO FJORD; WEST-COAST; KONGSFJORDEN; ASSEMBLAGES; ZOOPLANKTON; HYDROGRAPHY; INDICATORS	The potential of using dinoflagellate cysts as proxies for palaeoceanographic conditions and as monitors of the dynamic marine environment of climatically sensitive Arctic fjords was investigated with sediment traps. Dinoflagellate cysts were analysed from three separate deployments in two high Arctic fjords in the Svalbard archipelago. Two deployments in Kongsfjorden on the west coast of Svalbard occurred during 2002 and 2006 2007 and a deployment in Rijpfjorden on the NE coast occurred during 2006-2007. The cyst production displayed peaks of abundance in the spring and late summer with distinct differences in cyst occurrence in different fjords and in different years. The recorded and identified cyst species were consistent both with the hydrography of the fjords and with changes in cyst composition that are comparable to the seasonal shifts in water mass characteristics. The presence of the heterotrophic species Protoperidinium conicum in Kongsfjorden during 2002 is of note and may reflect the availability of a particular food source possibly associated with the strong influx of Atlantic Water. Cysts recovered from Kongsfjorden during 2006-2007 were dominated by Islandinium minutum, an indicator of cold, polar to subpolar conditions. The temperature and salinity characteristics of the ambient hydrography in this period indicated less influence by Atlantic Water than in 2002, and the cyst production was consistent with regional cyst distribution patterns. In Rijpfjorden, cyst assemblages were dominated by Pentapharsodinium dalei, consistent with the fjord being dominated by full Arctic conditions during the mooring deployment and the possible occurrence of stratified water with high productivity during the spring phytoplankton bloom.	[Howe, John A.; Cottier, Finlo R.; Brand, Tim; Willis, Kate J.; Eriksson, Anita] Scottish Assoc Marine Sci, Scottish Marine Inst, Oban PA37 1QA, Argyll, Scotland; [Harland, Rex] Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden; [Willis, Kate J.] Natl Inst Water & Atmospher Res, Christchurch, New Zealand; [Berge, Jorgen R.] Univ Ctr Svalbard, N-9171 Longyearbyen, Norway; [Grosfjeld, Kari] Geol Survey Norway, N-7491 Trondheim, Norway	University of the Highlands & Islands; University of Gothenburg; National Institute of Water & Atmospheric Research (NIWA) - New Zealand; University Centre Svalbard (UNIS); Geological Survey of Norway	Howe, JA (通讯作者)，Scottish Assoc Marine Sci, Scottish Marine Inst, Oban PA37 1QA, Argyll, Scotland.	john.howe@sams.ac.uk	Cottier, Finlo/K-6277-2012; Berge, Jorgen/E-7544-2015	Berge, Jorgen/0000-0003-0900-5679; Cottier, Finlo/0000-0002-3068-1754	NERC [dml010002] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		[Anonymous], OCEAN BIOCOENOSIS SE; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Berge J, 2009, BIOL LETTERS, V5, P69, DOI 10.1098/rsbl.2008.0484; Cottier F, 2005, J GEOPHYS RES-OCEANS, V110, DOI 10.1029/2004JC002757; Cottier FR, 2007, GEOPHYS RES LETT, V34, DOI 10.1029/2007GL029948; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B., 1992, OCEAN BIOCOENOSIS SE, V5, P1; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; Falk-Petersen S, 2008, DEEP-SEA RES PT II, V55, P2275, DOI 10.1016/j.dsr2.2008.05.010; Filipsson HL, 2005, ESTUAR COAST SHELF S, V63, P551, DOI 10.1016/j.ecss.2005.01.001; Gerland S, 2007, ANN GLACIOL-SER, V46, P435, DOI 10.3189/172756407782871215; GRAN HH, 1990, HYDROGRAPHIC BIOL ST, V1; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Grosfjeld K, 2009, NORW J GEOL, V89, P121; Hald M, 2004, QUATERNARY SCI REV, V23, P2075, DOI 10.1016/j.quascirev.2004.08.006; Harland R, 2006, SCI TOTAL ENVIRON, V355, P204, DOI 10.1016/j.scitotenv.2005.02.030; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P107, DOI 10.1016/S0034-6667(03)00115-5; HARLAND R, 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; HONJO S, 1988, DEEP-SEA RES, V35, P1223, DOI 10.1016/0198-0149(88)90078-7; Hop H, 2002, POLAR RES, V21, P167, DOI 10.1111/j.1751-8369.2002.tb00073.x; Hop H, 2006, PROG OCEANOGR, V71, P182, DOI 10.1016/j.pocean.2006.09.007; INDELICATO S R, 1986, Japanese Journal of Phycology, V34, P153; IVANOV IV, 2008, DEEP-SEA RES PT 1, V56, P1; JEONG HJ, 2008, 8 INT C MOD FOSS DIN, V23; Kremp A, 1999, MAR BIOL, V134, P771, DOI 10.1007/s002270050594; Kwasniewski S, 2003, J PLANKTON RES, V25, P1, DOI 10.1093/plankt/25.1.1; MacLachlan SE, 2007, POLAR RES, V26, P160, DOI 10.1111/j.1751-8369.2007.00016.x; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Matthiessen J, 2001, GLOBAL PLANET CHANGE, V31, P65, DOI 10.1016/S0921-8181(01)00113-8; Matthiessen Jens, 2005, Palaeontologische Zeitschrift, V79, P3; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Nilsen F, 2008, CONT SHELF RES, V28, P1838, DOI 10.1016/j.csr.2008.04.015; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Sakshaug E, 2004, ORGANIC CARBON CYCLE IN THE ARCTIC OCEAN, P57; Smayda T.J., 1980, PHYSIOLOGICAL ECOLOG, P493; Solignac S, 2009, NORW J GEOL, V89, P109; Svendsen H, 2002, POLAR RES, V21, P133, DOI 10.1111/j.1751-8369.2002.tb00072.x; Taylor F.J.R., 1987, BOT MONOGR, V21, P399; Willis K, 2006, J MARINE SYST, V61, P39, DOI 10.1016/j.jmarsys.2005.11.013; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zonneveld KAF, 2001, MAR GEOL, V172, P181, DOI 10.1016/S0025-3227(00)00134-1	46	34	35	0	10	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		978-1-86239-312-7	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2010	344						61	74		10.1144/SP344.6	http://dx.doi.org/10.1144/SP344.6			14	Geology; Geosciences, Multidisciplinary	Book Citation Index– Science (BKCI-S)	Geology	BUB84					2025-03-11	WOS:000288751900006
S	Harland, R; Nordberg, K; Filipsson, HL		Howe, JA; Austing, WEN; Forwick, M; Paetzel, M		Harland, Rex; Nordberg, Kjell; Filipsson, Helena L.			A major change in the dinoflagellate cyst flora of Gullmar Fjord, Sweden, at around 1969/1970 and its possible explanation	FJORD SYSTEMS AND ARCHIVES	Geological Society Special Publication		English	Article; Book Chapter							WEST-COAST; BENTHIC FORAMINIFERA; RECENT SEDIMENTS; REGIME SHIFT; KOLJO-FJORD; EUTROPHICATION; PHYTOPLANKTON; PRESERVATION; CLIMATE; RECORD	An ultra high-resolution study of the latest Holocene dinoflagellate cysts from Gullmar Fjord, on the west coast of Sweden, provides evidence for the recognition of at least two major dinoflagellate communities within the fjord over the last 85 years. These communities may result from changes within the North Atlantic Oscillation (NAO) and hydrography of the fjord between the approximate years 1915 and 1999 and/or from the local pollution history. The dinoflagellate cyst populations were compared in detail with hydrographical parameters available from this fjord with its long historical instrumental records. The dinoflagellate cysts fail to demonstrate a convincing ongoing eutrophication for the fjord, although the reduction of Lingulodinium polyedrum partly coincides with the curtailment of activity at a sulphite pulp mill at Munkedal and canning activity at Lysekil, together with a cessation in the influx of untreated sewage from water closets. The significant change in the assemblage composition at about the late 1960s/early 1970s coincides with a change in the NAO from a negative phase to its present-day positive phase. The unravelling of local environmental effects from those associated with regional fluctuations is complex and needs to be approached with caution.	[Harland, Rex; Nordberg, Kjell] Univ Gothenburg, Ctr Earth Sci, S-40530 Gothenburg, Sweden; [Filipsson, Helena L.] Lund Univ, GeoBiosphere Sci Ctr, S-22362 Lund, Sweden	University of Gothenburg; Lund University	Harland, R (通讯作者)，Univ Gothenburg, Ctr Earth Sci, POB 460, S-40530 Gothenburg, Sweden.	rex.harland@ntlworld.com	; Filipsson, Helena/F-7419-2011	Nordberg, Kjell/0000-0003-0085-4607; Filipsson, Helena/0000-0001-7200-8608				Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Arneborg L, 2004, CONT SHELF RES, V24, P443, DOI 10.1016/j.csr.2003.12.005; Beaugrand G, 2004, PROG OCEANOGR, V60, P245, DOI 10.1016/j.pocean.2004.02.018; Beaugrand G, 2002, SCIENCE, V296, P1692, DOI 10.1126/science.1071329; Björk G, 2003, CONT SHELF RES, V23, P1143, DOI 10.1016/S0278-4343(03)00081-5; 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, 2004, NORSK GEOLOGISK TIDS, V65, P97; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; Drinkwater KF, 2006, PROG OCEANOGR, V68, P134, DOI 10.1016/j.pocean.2006.02.011; Erdtman G., 1954, Botaniska Notiser, V2, P103; Filipsson HL, 2010, GEOL SOC SPEC PUBL, V344, P261, DOI 10.1144/SP344.18; Filipsson HL, 2005, ESTUAR COAST SHELF S, V63, P551, DOI 10.1016/j.ecss.2005.01.001; Filipsson HL, 2004, ESTUARIES, V27, P867, DOI 10.1007/BF02912048; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Gustafsson B, 1999, CONT SHELF RES, V19, P1021, DOI 10.1016/S0278-4343(99)00008-4; Harland R, 2006, SCI TOTAL ENVIRON, V355, P204, DOI 10.1016/j.scitotenv.2005.02.030; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; HARLAND R, 1989, J GEOLOGICAL SOC, V146, P954; JONSSON H, 2003, HAVETTID STRATEGI SL, V73, P1; Lindahl O, 1998, ICES J MAR SCI, V55, P723, DOI 10.1006/jmsc.1998.0379; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; Nordberg K, 2001, J SEA RES, V46, P187, DOI 10.1016/S1385-1101(01)00084-3; Nordberg K, 2000, J MARINE SYST, V23, P303, DOI 10.1016/S0924-7963(99)00067-6; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Powell A.J., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V112, P297, DOI 10.2973/odp.proc.sr.112.196.1990; ROSENBERG R, 1976, OIKOS, V27, P414, DOI 10.2307/3543460; Smayda TJ, 2003, J SEA RES, V49, P95, DOI 10.1016/S1385-1101(02)00219-8; Smayda TJ, 2001, J PLANKTON RES, V23, P447, DOI 10.1093/plankt/23.5.447; TRENDSINNUTRIEN.AL, 1996, J SEA RES, V35, P63; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Zonneveld KAF, 1997, MAR MICROPALEONTOL, V29, P393, DOI 10.1016/S0377-8398(96)00032-1	35	7	7	1	3	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		978-1-86239-312-7	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2010	344						75	82		10.1144/SP344.7	http://dx.doi.org/10.1144/SP344.7			8	Geology; Geosciences, Multidisciplinary	Book Citation Index– Science (BKCI-S)	Geology	BUB84					2025-03-11	WOS:000288751900007
S	Filipsson, HL; Nordberg, K		Howe, JA; Austing, WEN; Forwick, M; Paetzel, M		Filipsson, Helena L.; Nordberg, Kjell			Variations in organic carbon flux and stagnation periods during the last 2400 years in a Skagerrak fjord basin, inferred from benthic foraminiferal δ<SUP>13</SUP>C	FJORD SYSTEMS AND ARCHIVES	Geological Society Special Publication		English	Article; Book Chapter							NORTH-ATLANTIC OSCILLATION; DEEP-WATER RENEWAL; GULLMAR FJORD; LATE-HOLOCENE; OXYGEN CONCENTRATIONS; DINOFLAGELLATE CYSTS; CLIMATE-CHANGE; WEST-COAST; SWEDEN; VARIABILITY	A well-dated high-resolution delta C-13 record of the last 2400 a, based on the benthic foraminifer Cassidulina laevigata, is presented for Gullmar Fjord, Sweden. The time interval covers the Roman Warm Period (RWP), the Viking Age/Medieval Warm Period (VA/MWP), the Little Ice Age (LIA) and the most recent warming. There is little variation in the delta C-13 record until the early Viking Age (AD 800), when the delta C-13 signal becomes significantly more negative and continues to decrease throughout the VA/MWP. The delta C-13 signal increases both at the beginning and at the end of the LIA but is marked by more negative values during the larger part of the period. Since about 1970, the delta C-13 values are more negative than the long-term average. This general negativity of the record may result from a higher flux of organic matter, possibly of terrestrial origin due to land-use changes together with moderate changes in stagnation periods since the VA/MWP. In most recent times, the oceanic Suess effect together with increased number of extended stagnation periods are probably the main causes of the shift towards more negative delta C-13 values.	[Filipsson, Helena L.] Univ Bremen, D-28359 Bremen, Germany; [Nordberg, Kjell] Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden	University of Bremen; University of Gothenburg	Filipsson, HL (通讯作者)，Lund Univ, GeoBiosphere Sci Ctr, Solvegatan 12, SE-22362 Lund, Sweden.	Helena.filipsson@geol.lu.se	Filipsson, Helena/F-7419-2011	Filipsson, Helena/0000-0001-7200-8608; Nordberg, Kjell/0000-0003-0085-4607				Alheit J, 1997, FISH OCEANOGR, V6, P130, DOI 10.1046/j.1365-2419.1997.00035.x; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; Arneborg L, 2004, LIMNOL OCEANOGR, V49, P768, DOI 10.4319/lo.2004.49.3.0768; Arneborg L, 2004, CONT SHELF RES, V24, P443, DOI 10.1016/j.csr.2003.12.005; Bradley RS, 2001, SCIENCE, V292, P2011; Bradshaw EG, 2005, HOLOCENE, V15, P1152, DOI 10.1191/0959683605hl887rp; Broecker WS, 2001, SCIENCE, V291, P1497, DOI 10.1126/science.291.5508.1497; Brückner S, 2006, HOLOCENE, V16, P331, DOI 10.1191/0959683605hl931rp; Brückner S, 2008, MAR MICROPALEONTOL, V66, P192, DOI 10.1016/j.marmicro.2007.09.002; DALE B, 2000, ENV MICROPALEONTOLOG, P305; EKMAN FL, 1870, KONGL SVENSKA VETENS, V9, P16; Erlandsson CP, 2006, LIMNOL OCEANOGR, V51, P631, DOI 10.4319/lo.2006.51.1_part_2.0631; Filipsson HL, 2004, ESTUARIES, V27, P867, DOI 10.1007/BF02912048; FILIPSSON HL, 2003, THESIS GOTEBORG U GO; Fontanier C, 2006, MAR MICROPALEONTOL, V58, P159, DOI 10.1016/j.marmicro.2005.09.004; Gil IM, 2006, MAR MICROPALEONTOL, V60, P113, DOI 10.1016/j.marmicro.2006.03.003; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Gruber N, 1999, GLOBAL BIOGEOCHEM CY, V13, P307, DOI 10.1029/1999GB900019; Gustafsson M, 2001, J FORAMIN RES, V31, P2, DOI 10.2113/0310002; Harland R, 2006, SCI TOTAL ENVIRON, V355, P204, DOI 10.1016/j.scitotenv.2005.02.030; Harland R, 2010, GEOL SOC SPEC PUBL, V344, P75, DOI 10.1144/SP344.7; Hebbeln D, 2006, HOLOCENE, V16, P987, DOI 10.1177/0959683606hl989rp; Keeling C.D., 1979, ENVIRON INT, V2, P229, DOI [10.1016/0160-4120(79)90005-9, DOI 10.1016/0160-4120(79)90005-9]; Körtzinger A, 2003, GLOBAL BIOGEOCHEM CY, V17, DOI 10.1029/2001GB001427; Lamb H.H., 1995, Climate, History and the Modern World, VSecond; Lebreiro SM, 2006, HOLOCENE, V16, P1003, DOI 10.1177/0959683606hl990rp; Lindahl O, 2007, SWEDISH NATL REPORT, P41; McCorkle DC, 2008, GEOL SOC SPEC PUBL, V303, P135, DOI 10.1144/SP303.10; McCorkle DC, 1997, DEEP-SEA RES PT I, V44, P983, DOI 10.1016/S0967-0637(97)00004-6; McGregor HV, 2007, SCIENCE, V315, P637, DOI 10.1126/science.1134839; Nordberg K, 2000, J MARINE SYST, V23, P303, DOI 10.1016/S0924-7963(99)00067-6; RAMSEY CB, 2005, BIBLE RADIOCARBON DA, P57; Reimer PJ, 2004, RADIOCARBON, V46, P1029, DOI 10.1017/S0033822200032999; Rodhe J., 1998, The sea, V11, P699; Rohling EJ, 1999, MODERN FORAMINIFERA, P239; RYDBERG L, 1977, 23 GOTEBORG U DEP OC; *SMHI, 1994, VATT SVER 4 VATT VAS; SVANSSON A, 1984, MEDD HAVSFISKELABORA, V297, P1; Thorsen TA, 1995, HOLOCENE, V5, P435, DOI 10.1177/095968369500500406; Wanner H, 2008, QUATERNARY SCI REV, V27, P1791, DOI 10.1016/j.quascirev.2008.06.013; Wefer Gerold., 2002, CLIMATE DEV HIST N A; Zillén L, 2008, EARTH-SCI REV, V91, P77, DOI 10.1016/j.earscirev.2008.10.001	42	17	19	0	3	GEOLOGICAL SOC PUBLISHING HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CTR, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0305-8719		978-1-86239-312-7	GEOL SOC SPEC PUBL	Geol. Soc. Spec. Publ.		2010	344						261	270		10.1144/SP344.18	http://dx.doi.org/10.1144/SP344.18			10	Geology; Geosciences, Multidisciplinary	Book Citation Index– Science (BKCI-S)	Geology	BUB84					2025-03-11	WOS:000288751900019
J	Amo, M; Suzuki, N; Kawamura, H; Yamaguchi, A; Takano, Y; Horiguchi, T				Amo, Miki; Suzuki, Noriyuki; Kawamura, Hiroshi; Yamaguchi, Aika; Takano, Yoshihito; Horiguchi, Takeo			Sterol composition of dinoflagellates: Different abundance and composition in heterotrophic species and resting cysts	GEOCHEMICAL JOURNAL			English	Article						4 alpha-methyl sterol; autotrophic dinoflagellate; heterotrophic dinoflagellate; resting cyst; motile cell	MARINE DINOFLAGELLATE; TRACE STEROLS; DINOPHYCEAE; INVERTEBRATES; BIOMARKER; SEDIMENTS; FOOD	The motile cells of the autotrophic dinoflagellates Peridinium umbonatum var. inaequale, Akashiwo sanguinea, Scrippsiella tinctoria, and Prorocentrum micans commonly contain five major sterols: cholesterol, 4-methylcholestan-3-ol, 4,24-dimethylcholestan-3-ol, dinosterol, and dinostanol. The motile cell of the heterotrophic dinoflagellate Protoperidinium crassipes contains cholesterol, 4,24-dimethylcholestan-3-ol, dinosterol, dinostanol, and 4-tetramethylcholestan-3-ol as major free sterols. The dinosterol concentrations of heterotrophic dinoflagellates are about 4-12 times higher than those of autotrophic species, suggesting that the heterotrophic dinoflagellate is an important source of dinosterol in some sediments. 4-Tetramethylcholestan-3-ol has not been reported in cultured samples of other heterotrophic dinoflagellates. The difference in 4-methyl sterol composition in heterotrophic dinoflagellates may be related to the feeds used during the culture experiment. The resting cyst of P. umbonatum var. inaequale contains 4-methylcholestan-3-ol, 4,24-dimethylcholestan-3-ol, dinosterol, dinostanol, and C-31 Delta(5.22)-sterol as major free sterols. The C-31 Delta(5.22)-sterol has not been reported in cultured samples of motile cells from dinoflagellates. This compound might be produced during the resting stage, and thus may serve as a potential biomarker for the resting cysts of dinoflagellates.	[Amo, Miki; Suzuki, Noriyuki; Kawamura, Hiroshi; Yamaguchi, Aika; Takano, Yoshihito; Horiguchi, Takeo] Hokkaido Univ, Dept Nat Hist Sci, Grad Sch Sci, Kita Ku, Sapporo, Hokkaido 0600810, Japan	Hokkaido University	Amo, M (通讯作者)，Hokkaido Univ, Dept Nat Hist Sci, Grad Sch Sci, Kita Ku, N10 W8, Sapporo, Hokkaido 0600810, Japan.	amo-miki@jogmec.go.jp	Horiguchi, Takeo/D-7612-2012; Suzuki, Noriyuki/B-5694-2012	Suzuki, Noriyuki/0000-0002-8921-2450	Ministry of Education, Culture, Sports, Science and Technology of Japan [17740354]; Grants-in-Aid for Scientific Research [17740354] Funding Source: KAKEN	Ministry of Education, Culture, Sports, Science and Technology of Japan(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We thank Dr. K. Sawada for comments during the course of the study. We are indebted to Dr. Y. Chikaraishi and an anonymous reviewer for their constructive suggestions and helpful proofreading. This study was financially supported in part by Grants-in-Aid for Scientific Research (No. 17740354) and the 21st Century COE Grant for the "Neo-Science of Natural History" program (Leader: Prof. H. Okada) from the Ministry of Education, Culture, Sports, Science and Technology of Japan.	ALAM M, 1979, J ORG CHEM, V44, P4466, DOI 10.1021/jo01338a053; [Anonymous], 1985, SPOROPOLLENIN DINOFL; BOHLIN L, 1981, PHYTOCHEMISTRY, V20, P2397, DOI 10.1016/S0031-9422(00)82674-6; Breteler WCMK, 1999, MAR BIOL, V135, P191, DOI 10.1007/s002270050616; Calderón GJ, 2004, STEROIDS, V69, P93, DOI 10.1016/j.steroids.2003.11.001; Chu FL, 2008, MAR BIOL, V156, P155, DOI 10.1007/s00227-008-1072-2; Evitt W. 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J.		2010	44	3					225	231		10.2343/geochemj.1.0063	http://dx.doi.org/10.2343/geochemj.1.0063			7	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	613JG		gold, Green Published			2025-03-11	WOS:000278974600007
J	Peryt, D; Gedl, P				Peryt, Danuta; Gedl, Przemyslaw			Palaeoenvironmental changes preceding the Middle Miocene Badenian salinity crisis in the northern Polish Carpathian Foredeep Basin (Borkow quarry) inferred from foraminifers and dinoflagellate cysts	GEOLOGICAL QUARTERLY			English	Article						Carpathian Foredeep; Paratethys; foraminifers; dinoflagellates; Badenian; salinity crisis	BENTHIC FORAMINIFERA; ISOTOPIC COMPOSITION; PLANKTONIC-FORAMINIFERA; STABLE-ISOTOPE; VIENNA BASIN; IN-SITU; SEA; PARATETHYS; SEDIMENTS; OXYGENATION	Study of foraminiferal and dinoflagellate cyst assemblages and palynofacies occurring in 2 in-thick marls cropping out beneath a giant gypsum intergrowth unit in the Borkow gypsum quarry in Southern Poland, one of the key Badenian evaporite sections M the Polish Carpathian Foredeep Basin, has shown the presence of 49 species of benthic foraminifers and 11 species of planktonic ones, and 51 dinoflagellate (including 8 redeposited ones). The composition of the foraminiferal fauna and its isotopic signal indicate temperature-stratified, nutrient-rich and thus less-oxygenated marine water. Changes in the relative abundance of epifaunal and infaunal species indicate a clear environmental change during the deposition of the marls. A middle to outer shelf marine, well-ventilated environment with moderate primary productivity existed during the deposition of the bottom part of the marls. Subsequently, infaunal bottom-dwellers became dominant due to a massive increase in food supply to the sea bottom and shallowing of the sea to inner middle shelf depths, and than a decreasing trend of a relative abundance of the infaunal morphogroups is observed until the top of the marls that were deposited in an inner shelf environment with moderate primary productivity. The calculated palacotemperatures for particular foraminifer taxa (Globigerina spp., Cibicidoides and Bulimina elongata) show a slight upsection decrease and a decrease in the temperature differences between the bottom and intermediate water beds. Palynofacies are composed of elements of mixed origin, including terrestrial, marine (mainly dinoflagellate cysts) and elements of uncertain derivation (structureless organic matter). The palynological content of most samples indicates their deposition in an open-marine marine environment, in the stable marine conditions of an open shelf basin with no salinity fluctuations. The sample just below the gypsum contains no dinoflagellate cysts, perhaps due to a drastic change in the photic zone leading to a complete collapse of the dinoflagellate flora. Very rare occurrence of planktonic foraminifers in that sample suggest the shallowing of the basin accompanied by a decrease in the temperature gradient between the upper (warmer) and lower (colder) water beds. A shallow, cold water marine environment is indicated for the topmost foraminiferal assemblage.	[Peryt, Danuta] Polish Acad Sci, Inst Palaeobiol, PL-00818 Warsaw, Poland; [Gedl, Przemyslaw] Polish Acad Sci, Inst Geol Sci, PL-31002 Krakow, Poland	Polish Academy of Sciences; Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences	Peryt, D (通讯作者)，Polish Acad Sci, Inst Palaeobiol, Twarda 51-55, PL-00818 Warsaw, Poland.	d.peryt@twarda.pan.pl; ndgedl@cyf-kr.edu.pl	Peryt, Danuta/F-9988-2019	Peryt, Danuta/0000-0002-5821-1084	Ministry of Science and Higher Education [Ukraina/193/2006]	Ministry of Science and Higher Education	We thank S. Gebka (Saint-Gobain Construction Products Polska) for permission to collect the samples, T. M. Peryt (PGI-NRI) for samples, comments and suggestions, W. Narkiewicz (PGI-NRI) for the XRF analyses, and in particular K. Malkowski (Institute of Palaeobiology) for the isotopic analyses. We also thank A. Becker, M. Gonera, N. Hudackova and P. Kovacova for their comments and suggestions which improved the text. The paper resulted from special grant No. Ukraina/193/2006 (Ministry of Science and Higher Education) to M. Kotarba (Academy of Mining and Metallurgy) and statutory studies of the Institute of Palaeobiology, Polish Academy of Sciences.	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J	Park, TG; Park, YT				Park, Tae-Gyu; Park, Young-Tae			Detection of <i>Cochlodinium polykrikoides</i> and <i>Gymnodinium impudicum</i> (Dinophyceae) in sediment samples from Korea using real-time PCR	HARMFUL ALGAE			English	Article						Cochlodinium polykrikoides; Cyst; Gymnodinium impudicum; Harmful algal blooms; Real-time PCR; Red tide	PFIESTERIA-PISCICIDA DINOPHYCEAE; GONYAULAX-TAMARENSIS; ENVIRONMENTAL-SAMPLES; RAPID DETECTION; RESTING CYSTS; LIFE-CYCLE; DINOFLAGELLATE; QUANTIFICATION; IDENTIFICATION; TEMPERATURE	Recurring blooms of fish killing dinoflagellate Cochlodinium polykrikoides has resulted in large economic losses in fisheries industry in Korea. This species has been monitored in water column samples, but its spatial distribution in sediments is poorly understood. To address this area, geographic distribution of C. polykrikoides and morphologically similar species Gymnodinium impudicum in surface sediments of Korea was investigated using species-specific real-time PCR probes targeting the internal transcribed spacer 2 rRNA gene. PCR-inhibitory substances in sediment samples were removed by dilution of DNA extracts from the field samples for preventing false-negative detection. G. impudicum was widely distributed in sediments from East, South, and Yellow Seas. C. polykrikoides was prevalent in sediments from South Sea whereas it was not detected in sediments from East and Yellow Seas. These results indicate that these dinoflagellates may persist in surface sediment likely in the form of cyst and their "seed beds" may exist in sediments of South Sea where blooms of C. polykrikoides occur annually. (C) 2009 Elsevier B.V. All rights reserved.	[Park, Tae-Gyu; Park, Young-Tae] Natl Fisheries Res & Dev Inst, Marine Ecol Res Div, Pusan 619705, South Korea		Park, YT (通讯作者)，Natl Fisheries Res & Dev Inst, Marine Ecol Res Div, Pusan 619705, South Korea.	ytparknfrdi@gmail.com			NFRDI [RP-2009-ME008]	NFRDI	This work was funded by a grant from NFRDI (RP-2009-ME008).[SS]	ANDERSON DM, 1980, J PHYCOL, V16, P166; 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, 1985, J PHYCOL, V21, P200; BINDER BJ, 1987, J PHYCOL, V23, P99; Bowers HA, 2000, APPL ENVIRON MICROB, V66, P4641, DOI 10.1128/AEM.66.11.4641-4648.2000; Bowers HA, 2006, HARMFUL ALGAE, V5, P342, DOI 10.1016/j.hal.2005.09.005; Coyne KJ, 2006, HARMFUL ALGAE, V5, P363, DOI 10.1016/j.hal.2005.07.008; Cullen DW, 1998, SOIL BIOL BIOCHEM, V30, P983, DOI 10.1016/S0038-0717(98)00001-7; Dale B., 1983, P69; DALE B, 1993, EUR J PHYCOL, V28, P129, DOI 10.1080/09670269300650211; England LS, 1997, SOIL BIOL BIOCHEM, V29, P1521, DOI 10.1016/S0038-0717(97)00013-8; Galluzzi L, 2004, APPL ENVIRON MICROB, V70, P1199, DOI 10.1128/AEM.70.2.1199-1206.2004; GUILLARD RR, 1962, CAN J MICROBIOL, V8, P229, DOI 10.1139/m62-029; Guy RA, 2003, APPL ENVIRON MICROB, V69, P5178, DOI 10.1128/AEM.69.9.5178-5185.2003; Kamikawa R., 2006, Microbes and Environments, V21, P163, DOI 10.1264/jsme2.21.163; Kamikawa R, 2007, HARMFUL ALGAE, V6, P413, DOI 10.1016/j.hal.2006.12.004; Kim CH, 2002, PHYCOLOGIA, V41, P667, DOI 10.2216/i0031-8884-41-6-667.1; Kim CJ, 2007, HARMFUL ALGAE, V6, P104, DOI 10.1016/j.hal.2006.07.004; Kim CS, 1999, J PLANKTON RES, V21, P2105, DOI 10.1093/plankt/21.11.2105; Kim D, 2002, COMP BIOCHEM PHYS C, V132, P415, DOI 10.1016/S1532-0456(02)00093-5; Kremp A, 2006, J PHYCOL, V42, P400, DOI 10.1111/j.1529-8817.2006.00205.x; Lin SJ, 2006, J PLANKTON RES, V28, P667, DOI 10.1093/plankt/fbi150; Litaker RW, 2003, J PHYCOL, V39, P754, DOI 10.1046/j.1529-8817.2003.02112.x; Matsuoka K., 2000, TECHNICAL GUIDE MODE; *NFRDI, 2008, DAT RED TID; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Park TG, 2007, APPL ENVIRON MICROB, V73, P2552, DOI 10.1128/AEM.02389-06; Park TG, 2007, POLAR BIOL, V30, P843, DOI 10.1007/s00300-006-0244-0; Park TG, 2009, HARMFUL ALGAE, V8, P430, DOI 10.1016/j.hal.2008.09.003; Park TG, 2009, PHYCOLOGIA, V48, P32, DOI 10.2216/08-52.1; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Wilson IG, 1997, APPL ENVIRON MICROB, V63, P3741, DOI 10.1128/AEM.63.10.3741-3751.1997	33	22	24	1	17	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883	1878-1470		HARMFUL ALGAE	Harmful Algae	JAN	2010	9	1					59	65		10.1016/j.hal.2009.08.002	http://dx.doi.org/10.1016/j.hal.2009.08.002			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	530OP					2025-03-11	WOS:000272602500007
J	Petersen, HI; Bojesen-Koefoed, JA; Mathiesen, A				Petersen, H. I.; Bojesen-Koefoed, J. A.; Mathiesen, A.			VARIATIONS IN COMPOSITION, PETROLEUM POTENTIAL AND KINETICS OF ORDOVICIAN - MIOCENE TYPE I AND TYPE I-II SOURCE ROCKS (OIL SHALES): IMPLICATIONS FOR HYDROCARBON GENERATION CHARACTERISTICS	JOURNAL OF PETROLEUM GEOLOGY			English	Article						oil shale; Type I kerogen; alginite; source rock; kinetics; modelling	SONG-HONG BASIN; RESISTANT OUTER WALLS; CENOZOIC RIFT-BASINS; MAE-SOT-BASIN; ORGANIC GEOCHEMISTRY; NORTHERN THAILAND; PHENOLIC MOIETIES; THERMAL MATURITY; GAS GENERATION; FRESH-WATER	Lacustrine and marine oil shales with Type I and Type I-II kerogen constitute significant petroleum source rocks around the world. Contrary to common belief, such rocks show considerable compositional variability which influences their hydrocarbon generation characteristics. A global set of 23 Ordovician - Miocene freshwater and brackish water lacustrine and marine oil shales has been studied with regard to their organic composition, petroleum potential and generation kinetics. In addition their petroleum generation characteristics have been modelled. The oil shales can be classified as lacosite, torbanite, tasmanite and kukersite. They are thermally immature. Most of the shales contain > 10 wt% TOC and the highest sulphur contents are recorded in the brackish water and marine oil shales. The kerogen is sapropelic and is principally composed of a complex of algal-derived organic matter in the form of: (i) telalginite (Botryococcus-, Prasinophyte- (Tasmanites ?) or Gloeocapsomorpha-type); (ii) lamalginite (laminated, filamentous or network structure derived from Pediastrum- or Tetraedron-type algae, from dinoflagellate/acritarch cysts or from thin-walled Prasinophyte-type algae); (iii) fluorescing amorphous organic matter (AOM) and (iv) liptodetrinite. High atomic H/C ratios reflect the hydrogen-rich Type I and Type I-II kerogen, and Hydrogen Index values generally > 300 mg HC/g TOC and reaching nearly 800 mg HC/g TOC emphasise the oil-prone nature of the oil shales. The kerogen type and source rock quality appear not to be related to age, depositional environment or oil shale type. Therefore, a unique, global activation energy (E(a)) distribution and frequency factor (A) for these source rocks cannot be expected. The differences in kerogen composition result in considerable variations in E(a)-distributions and A-factors. Generation modelling using custom kinetics and the known subsidence history of the Malay-Cho Thu Basin (Gulf of Thailand/South China Sea), combined with established and hypothetical temperature histories, show that the oil shales decompose at different rates during maturation. At a maximum temperature of similar to 120 degrees C reached during burial, only limited kerogen conversion has taken place. However, oil shales characterised by broader E(a)-distributions with low E(a)-values (and a single approximated A-factor) show increased decomposition rates. Where more deeply buried (maximum temperature similar to 150 degrees C), some of the brackish water and marine oil shales have realised the major part of their generation potential, whereas the freshwater oil shales and other brackish water oil shales are only similar to 30-40% converted. At still higher temperatures between similar to 165 degrees C and 180 degrees C all oil shales reach 90% conversion. Most hydrocarbons from these source rocks will be generated within narrow oil windows (similar to 20-80% kerogen conversion). Although the brackish water and marine oil shales appear to decompose faster than the freshwater oil shales, this suggests that with increasing heatflow the influence of kerogen heterogeneity on modelling of hydrocarbon generation declines. It may thus be critical to understand the organic facies of Type I and Type I-II source rocks, particularly in basins with moderate heatflows and restricted burial depths. Measurement of custom kinetics is recommended, if possible, to increase the accuracy of any computed hydrocarbon generation models.	[Petersen, H. I.; Bojesen-Koefoed, J. A.; Mathiesen, A.] Geol Survey Denmark & Greenland GEUS, DK-1350 Copenhagen K, Denmark	Geological Survey Of Denmark & Greenland	Petersen, HI (通讯作者)，Geol Survey Denmark & Greenland GEUS, Oster Voldgade 10, DK-1350 Copenhagen K, Denmark.	hip@geus.dk	Bojesen-Koefoed, Jørgen/AAH-5501-2020; Petersen, Henrik/ABB-4663-2020; Mathiesen, Anders/H-3115-2018	Bojesen-Koefoed, Jorgen Albert/0000-0001-5647-2769; Mathiesen, Anders/0000-0003-4345-7513; Petersen, Henrik I./0000-0001-6606-7062	Geological Survey of Denmark and Greenland (GEUS)	Geological Survey of Denmark and Greenland (GEUS)	The authors would like to thank C. Araujo (Petrobras, Brazil), A. G. Borrego (INCAR, Spain), O. A. Ehinola (University of Ibadan, Nigeria), N. Sherwood (CSIRO, Australia), Feiyu Wang (China University of Petroleum, China), and F. X. Widiarto (Indonesia) for providing samples. S. Solberg (GEUS) is thanked for drafting the figures. JPG reviewers D. M. Jarvie (IFP, France) and N. V. Lopatin (Geosystems Institute, Russia) are thanked for their comments on an earlier version of the manuscript. The article is published with permission of the Geological Survey of Denmark and Greenland (GEUS).	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Pet. Geol.	JAN	2010	33	1					19	41		10.1111/j.1747-5457.2010.00462.x	http://dx.doi.org/10.1111/j.1747-5457.2010.00462.x			23	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	533PU					2025-03-11	WOS:000272837500002
J	Young, MD; Hannah, MJ				Young, Martin D.; Hannah, Michael J.			Dinoflagellate biostratigraphy of the vertebrate fossil-bearing Maungataniwha Sandstone, northwest Hawke's Bay, New Zealand	NEW ZEALAND JOURNAL OF GEOLOGY AND GEOPHYSICS			English	Article						organic-walled dinoflagellate cysts; dinocysts; Hawke's Bay; cretaceous; marine reptiles; dinosaurs; Maungataniwha Sandstone; concretions	SOUTH ISLAND; PIRIPAUAN	Fossil organic-walled dinoflagellate cysts (dinocysts) have been used to constrain the age of the Maungataniwha Sandstone and associated phosphatic and calcareous concretions from the Mangahouanga Stream, northwest Hawke's Bay, New Zealand. These concretions often contain dinosaur and marine reptile fossils, including the mosasaur Moanasaurus mangahouangae, first discovered within the study area in a calcareous concretion. The Maungataniwha Sandstone contains low to moderately diverse dinocyst assemblages corresponding to the Vozzhennikovia spinulosa - Isabelidinium pellucidum zonal interval (lower to upper Haumurian). Recovered dinocyst assemblages from in situ concretions are similar to those from the surrounding sediments, suggesting that the concretions have grown in place. Calcareous float concretions containing the mosasaur Moanasaurus mangahouangae, as well as the two phosphatic concretions (one of which also contained a mosasaur fossil), are all of a lower Haumurian age. Plesiosaur fossil-bearing calcareous concretions exhibit a range of ages from lower to upper Haumurian (early Campanian to early Maastrichtian), spanning the age range of the Maungataniwha Sandstone section within the study area. The two dinosaur fossil-bearing calcareous concretions can only be dated as no younger than the middle upper Haumurian (early Maastrichtian).	[Young, Martin D.] CSIRO Petr Resources, N Ryde, NSW, Australia; [Hannah, Michael J.] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington, New Zealand	Commonwealth Scientific & Industrial Research Organisation (CSIRO); Victoria University Wellington	Young, MD (通讯作者)，CSIRO Petr Resources, Riverside Corp Pk, N Ryde, NSW, Australia.	martin.young@csiro.au	Hannah, Michael/H-1083-2015	Hannah, Michael/0000-0002-2275-0086				Crampton J, 2000, NEW ZEAL J GEOL GEOP, V43, P309, DOI 10.1080/00288306.2000.9514890; CRAMPTON JS, 1990, NEW ZEAL J GEOL GEOP, V33, P333, DOI 10.1080/00288306.1990.10425691; CRAMPTON JS, 2004, I GEOLOGICAL NUCL SC, V22, P102; Fensome R. A., 2008, AM ASS STRATIGRAPHIC, V1; ISAAC MJ, 1991, NEW ZEAL J GEOL GEOP, V34, P227, DOI 10.1080/00288306.1991.9514460; Lawver L., 1991, Geological evolution of Antarctica, P533; MCKEE JWA, 1998, MISCELLANEOUS PUBLIC, V96; Molnar R.E., 1981, Gondwana Five: Proceeding of the Fifth International Gondwanan Symposium, P91; Molnar RE, 1998, NEW ZEAL J GEOL GEOP, V41, P145, DOI 10.1080/00288306.1998.9514798; Roncaglia L, 1999, CRETACEOUS RES, V20, P271, DOI 10.1006/cres.1999.0153; Schioler P, 1998, MICROPALEONTOLOGY, V44, P313, DOI 10.2307/1486039; Wilson G.J., 1984, Newsletters on Stratigraphy, V13, P104; Wilson GJ, 2005, NEW ZEAL J GEOL GEOP, V48, P377, DOI 10.1080/00288306.2005.9515120; WILSON GJ, 1987, DINOFLAGELLATE BIOST, P8; [No title captured]	15	6	7	0	1	TAYLOR & FRANCIS LTD	ABINGDON	4 PARK SQUARE, MILTON PARK, ABINGDON OX14 4RN, OXON, ENGLAND	0028-8306			NEW ZEAL J GEOL GEOP	N. Z. J. Geol. Geophys.		2010	53	1					81	87	PII 921300497	10.1080/00288301003639742	http://dx.doi.org/10.1080/00288301003639742			7	Geology; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	600WF		Bronze			2025-03-11	WOS:000278018900007
J	Rouis-Zargouni, I; Turon, JL; Londeix, L; Essallami, L; Kallel, N; Sicre, MA				Rouis-Zargouni, Imene; Turon, Jean-Louis; Londeix, Laurent; Essallami, Latifa; Kallel, Nejib; Sicre, Marie-Alexandrine			Environmental and climatic changes in the central Mediterranean Sea (Siculo-Tunisian Strait) during the last 30 ka based on dinoflagellate cyst and planktonic foraminifera assemblages	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Dinocysts; Planktonic foraminifera; Mediterranean region; Heinrich events; Holocene; Presapropelic condition	GLACIAL-INTERGLACIAL TRANSITION; NORTHERN NORTH-ATLANTIC; HIGH-RESOLUTION RECORD; ORGANIC-CARBON; SURFACE TEMPERATURE; HEINRICH EVENTS; SAPROPEL S1; MARINE; SCALE; RECONSTRUCTION	A high resolution micropalaeontological study of the core MID 04-2797 CQ recovered in the Sicilian-Tunisian Strait provides insights into the paleoclimatic history of the Mediterranean Sea at the transition between the western and eastern basin over the last 30 ka. Using the analysis of dinoflagellate cyst and planktonic foraminiferal assemblages, we reconstruct the paleoenvironmental changes that took place in this region. High abundances of cold temperate dinocyst species (Nematosphaeropsis labyrinthus, Spiniferites elongatus, Bitectatodinium tepikiense) and the polar planktonic foraminifera Neogloboquadrina pachyderma (left coiling) reveal three major cooling events synchronous with North Atlantic Henrich events 1 and 2 (H1 and H2) and the European and North Atlantic Younger Dryas event. During the Holocene, the presence of warm dinocyst species (Spiniferites mirabilis and Impagidinium aculeatum) and planktonic foraminifera (Globorotalia inflata and Globigerinoides ruber), reflects a significant increase of sea surface temperatures in the western Mediterranean basin, but a full warming was not recorded until 1500 years after the onset of the Holocene. Moreover, our results show that the Holocene was interrupted by at least four brief cooling events at similar to 9.2 ka, similar to 8 ka, similar to 7 ka and similar to 2.2 ka cal. FIR which may be correlated to climatic events recorded in Greenland ice cores and in the Atlantic Ocean. (C) 2009 Elsevier B.V. All rights reserved.	[Rouis-Zargouni, Imene; Turon, Jean-Louis; Londeix, Laurent] Univ Bordeaux 1, EPOC, UMR 5805, F-33405 Talence, France; [Rouis-Zargouni, Imene; Essallami, Latifa; Kallel, Nejib] Fac Sci Sfax, Lab GEOGLOB, Sfax 3028, Tunisia; [Sicre, Marie-Alexandrine] IPS CNRS INSU CEA UVSQ, Lab Sci Climat & Environm, F-91198 Gif Sur Yvette, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bordeaux; Universite de Sfax; Faculty of Sciences Sfax; CEA; Universite Paris Saclay	Rouis-Zargouni, I (通讯作者)，Univ Bordeaux 1, EPOC, UMR 5805, Ave Fac, F-33405 Talence, France.	imenerouis@ymail.com; Jl.turon@epoc.u-bordeaux.fr; l.londeix@epoc.u-bordeaux.fr; ess_latifa@yahoo.fr; nejib.kallel@fss.rnu.tn; sicre@lsce.cnrs-gif.fr	Marie-Alexandrine, Sicre/AAR-1516-2020	Sicre, Marie-Alexandrine/0000-0002-5015-1400	Centre National de la Recherche Scientifique (CNRS); RV Marion-Dufresne officers and crew; IMAGES; Institut Paul Emile Victor (IPEV); French-Tunisian CMCU (Comite Mixte de Cooperation Universitaire) [05-S-1004]	Centre National de la Recherche Scientifique (CNRS)(Centre National de la Recherche Scientifique (CNRS)); RV Marion-Dufresne officers and crew; IMAGES; Institut Paul Emile Victor (IPEV); French-Tunisian CMCU (Comite Mixte de Cooperation Universitaire)	The authors thank the Institut National des Sciences de l'Univers (INSU) of the Centre National de la Recherche Scientifique (CNRS), the RV Marion-Dufresne officers and crew, the IMAGES program and the Institut Paul Emile Victor (IPEV) for support and Organisation of the coring cruises. We would finally like to thank B. Lecoat for isotope analyses, ARTEMIS for the radiocarbon age measurements and M.H. Castera (UMR-EPOC5805) for preparing the dinocyst samples.I. R-Z. and N.K. gratefully acknowledge the financial support provided by the French-Tunisian CMCU (Comite Mixte de Cooperation Universitaire) joint project 05-S-1004.	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JAN 1	2010	285	1-2					17	29		10.1016/j.palaeo.2009.10.015	http://dx.doi.org/10.1016/j.palaeo.2009.10.015			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	556BZ					2025-03-11	WOS:000274563700002
J	Schrank, E				Schrank, Eckart			Pollen and spores from the Tendaguru Beds, Upper Jurassic and Lower Cretaceous of southeast Tanzania: palynostratigraphical and paleoecological implications	PALYNOLOGY			English	Article						Jurassic; Cretaceous; Tendaguru Beds; Tanzania; pollen; spores; paleoecology	STRATIGRAPHIC PALYNOLOGY; EROMANGA BASIN; DINOFLAGELLATE; ARAUCARIACEAE; EPHEDRA; STRATA; ASSEMBLAGES; QUEENSLAND; DIVERSITY; AUSTRALIA	Two informal sporomorph assemblage zones can be distinguished in the dinosaur-bearing Tendaguru Beds of southeast Tanzanian. The first zone, the Classopollis-Araucariacites-Shanbeipollenites Assemblage Zone, ranges from the Lower to the Upper Saurian Bed, and a mid-Oxfordian to Tithonian age is suggested based on the presence of Shanbeipollenites quadratus. The second zone, the Classopollis-Cicatricosisporites-Ruffordiaspora Assemblage Zone, is restricted in the Trigonia schwarzi Bed, which overlies the Upper Saurian Bed. The combined ranges of Cicatricosisporites hughesii, Ruffordiaspora australiensis and Trilobosporites obsitus would be consistent with a late Berriasian to Hauterivian age of this zone. This is refined further to late Valanginian to Hauterivian on the basis of already existing evidence from fauna and dinoflagellate cysts. From a phytogeographic point of view the Tendaguru locality belongs to the southern Gondwana Trisaccates Province because of the presence of trisaccate podocarpaceous pollen. The quantitative composition of the palynofloras is characterized by the dominance or abundance of pollen produced by the two conifer families Cheirolepidiaceae (Classopollis) and Araucariaceae (mainly Araucariacites). Pollen of Cheirolepidiaceae, typically xerophytic, drought-resistant, thermophilic plants, is dominant throughout the Tendaguru Beds except in parts of the Middle Saurian Bed where pollen of Araucariaceae, a presumably mesic group, becomes most abundant. Classopollis attains the highest degree of dominance in the shallow marine deposits associated with the saurian beds. This may be related to paleoecological and taphonomic factors, namely abundance of Classopollis-producing plants in low-lying coastal environments close to the lagoon-like depositional sites and transportational sorting of sporomorphs leading to a relative enrichment of small and/or anemophilous pollen. The abundance of Araucariacites in the Middle Saurian Bed suggests that araucarians existed in coastal plain environments that were stable enough to allow the growth of large trees. This open araucarian forest, which may have been a source of food for high-browsing dinosaurs, was situated landward of the cheirolepidiacean belt not far from the depositional sites. Pteridophytes and bryophytes were concentrated at moist places and around water bodies. Podocarpaceous conifers producing bisaccate and trisaccate pollen grew in local uplands, while gnetaleans related to Ephedra and Welwitschia may have been present in dry places. The palynological evidence is consistent with a seasonally dry, tropical to sub-tropical paleoclimate. Three new combinations, Equisetosporites certus (Bolkhovitina), Jugella caichiguensis (Volkheimer and Quattrocchio) and Trichotomosulcites microsaccatus (Couper), are proposed, and Jugella semistriata is described as a new species.	Tech Univ Berlin, Inst Angew Geowissensch, D-10623 Berlin, Germany	Technical University of Berlin	Schrank, E (通讯作者)，Tech Univ Berlin, Inst Angew Geowissensch, Sekr EB10,Str 17,Juni 145, D-10623 Berlin, Germany.	e.schrank@tu-berlin.de			German Research Foundation (DFG) [Schr 356/2-4]	German Research Foundation (DFG)(German Research Foundation (DFG))	Thanks are due to Tanzanian officials and to the members of the expedition team 2000, Martin Aberhan, Robert Bussert, Remigius Chami, Oliver Hampe, Wolf-Dieter Heinrich, Saidi Kapilima, Gerhard Maier, Emma Msaky, Benjamin Sames and Stephan Schultka who made fieldwork in the Tendaguru area possible. Special thanks go to Robert Bussert and Benjamin Sames for the two samples from the Namunda Plateau and for relevant information. Help from Mr J. Nissen in operating the SEM and from Ms H. Glowa and Mr M. Thiel in preparing the illustrations is gratefully acknowledged. The careful and constructive reviews by James A. Doyle and Mercedes B. Pramparo as well as palynological information from Wolfgang Volkheimer are greatly appreciated. Field and laboratory work was supported by the German Research Foundation (DFG, Schr 356/2-4).	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J	Slimani, H; Louwye, S; Toufiq, A				Slimani, Hamid; Louwye, Stephen; Toufiq, Abdelkabir			Dinoflagellate cysts from the Cretaceous-Paleogene boundary at Ouled Haddou, southeastern Rif, Morocco: biostratigraphy, paleoenvironments and paleobiogeography	PALYNOLOGY			English	Article						Cretaceous-Paleogene boundary; dinoflagellate cysts; stratigraphy; Ouled Haddou section; southeastern Rif; northern Morocco	SEA-LEVEL CHANGES; TERTIARY BOUNDARY; NEW-ZEALAND; CALCAREOUS NANNOFOSSIL; SEQUENCE STRATIGRAPHY; NORTHERN APENNINES; WOODSIDE CREEK; NEW-JERSEY; SP-NOV.; EL-KEF	A palynological investigation of a section dated by foraminifera, at Ouled Haddou, south-eastern Rifian Corridor, northern Morocco, revealed a rich and well-preserved dinoflagellate cyst assemblage that allowed a palynological separation of Maastrichtian from Danian deposits. The gradual change of the dinoflagellate cyst assemblages and the biostratigraphic resolution attained, suggest that the studied Maastrichtian-Danian section is continuous. The recognition of the latest Maastrichtian and earliest Danian is based on global dinoflagellate cyst events, including the first occurrence of the latest Maastrichtian species Disphaerogena carposphaeropsis, Glaphyrocysta perforata, and Manumiella seelandica, the latest Maastrichtian acme of Manumiella seelandica, and the first occurrence of the earliest Danian markers Carpatella cornuta, Damassadinium californicum, Eisenackia circumtabulata, Membranilarnacia tenella and Senoniasphaera inornata. The Cretaceous Paleogene boundary is placed above the latest Maastrichtian events, mainly immediately above the acme of M. seelandica and below the earliest Danian events, particularly below the first occurrences of C. cornuta and D. californicum. The biostratigraphic interpretations are based on a comparison with calibrated dinoflagellate cyst ranges from several reference sections, mainly in the Northern Hemisphere middle latitudes. The Cretaceous-Paleogene boundary is not marked by a mass extinction of dinoflagellate cyst species, but shows important changes in the relative abundances of different species or groups of morphologically related species. These changes are paleoenvironmentally controlled. The peridinioid assemblage suggests deposition in a subtropical to warm temperate province. One dinoflagellate cyst species, Phelodinium elongatum, is formally described.	[Slimani, Hamid] Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, URAC 46, Rabat 10106, Morocco; [Louwye, Stephen] Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium; [Toufiq, Abdelkabir] Univ Chouaib Doukkali, Fac Sci, Lab Geosci & Environm Tech, El Jadida 24000, Morocco	Mohammed V University in Rabat; Ghent University; Chouaib Doukkali University of El Jadida	Slimani, H (通讯作者)，Univ Mohammed V Agdal, Inst Sci, Lab Geol & Remote Sensing, URAC 46, Ave Ibn Batouta,PB 703, Rabat 10106, Morocco.	slimani@israbat.ac.ma	Slimani, Hamid/AAL-4055-2020; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Slimani, Hamid/0000-0001-6392-1913	URAC 46; Hassan II Academy of Sciences and Technology	URAC 46; Hassan II Academy of Sciences and Technology(Hassan II Academy of Sciences & Technology)	We are indebted to Mrs Sabine Van Cauwenberghe (Research Unit Palaeontology, University of Ghent, Belgium) for the palynological preparation of the samples. Thanks are also given to the staff of the Earth Science Department (Scientific Institute, University Mohammed V-Agdal, Morocco) for providing technical support. James B. Riding (Managing Editor) and the two journal referees, Javier Helenes (C. I. C. E. S. E., Department of Geology, Baja, California, Mexico) and John Firth (IODP-USIO, Texas A&M University, College Station, Texas, USA) are thanked for their useful constructive reviews and critical comments that improved the original manuscript. Collaboration (exchanges of ideas, observation of palynological material of the Elles Section) with Kmar Ben Ismail-Lattrache and Amel M'hamdi (Faculty of Sciences, Tunis, Tunisia), in the context of a Morocco-Tunisian project (88/MT/08), was helpful. We thank URAC 46 and the Hassan II Academy of Sciences and Technology for their financial support.	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J	Jarzen, DM; Klug, C				Jarzen, David M.; Klug, Curtis			A preliminary investigation of a lower to middle Eocene palynoflora from Pine Island, Florida, USA	PALYNOLOGY			English	Article						early Eocene; palynomorphs; angiosperms; phytoplankton	NEOTROPICAL PALEOBOTANY; MIOCENE COMMUNITIES; PANAMA; PALYNOLOGY; POLLEN; MEXICO; ANGIOSPERMS; PALEOCENE; SEDIMENTS; PLIOCENE	A small but diverse assemblage of pollen, spores and marine phytoplankton recovered from a single, lignitic clay sample of the lower to middle Eocene strata from a deep injection well on Pine Island, Florida represents the oldest land flora described from the state. The assemblage contains 17 terrestrial forms and four to five brackish to marine forms of dinoflagellate cysts or algal taxa. Angiosperm pollen forms are comparable to extant taxa including the palms, Bombacacidites (Bombacaceae), Corsinipollenites (Onagraceae), Milfordia (Restioniaceae), Tiliaepollenites (Tiliaceae), and Retitricolporites sp. (Lisianthius Gentianaceae). These suggested affinities point to a mild, warm-temperate to subtropical, probably lowland, environment. No new pollen taxa are described. This is the earliest report of terrestrial vegetation and near marine vegetation of Florida and documents the presence of a Florida landmass during the early Eocene.	[Jarzen, David M.] Univ Florida, Florida Museum Nat Hist, Paleobot & Palynol Lab, Gainesville, FL 32611 USA; [Klug, Curtis] ENTRIX, Ft Myers, FL 33907 USA	State University System of Florida; University of Florida	Jarzen, DM (通讯作者)，Univ Florida, Florida Museum Nat Hist, Paleobot & Palynol Lab, Gainesville, FL 32611 USA.	dmj@flmnh.ufl.edu						[Anonymous], 2008, 20075207 US GEOL SUR; [Anonymous], 2001, FLORIDA GEOLOGICAL S; [Anonymous], 1999, AUSTR RUSHES BIOL ID; Applin E. R., 1945, JOUR PALEONTOL, V19, P129; Applin P. 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J	Iakovleva, AI; Heilmann-Clausen, C				Iakovleva, Alina I.; Heilmann-Clausen, Claus			Eocene dinoflagellate cyst biostratigraphy of research borehole 011-BP, Omsk Region, southwestern Siberia	PALYNOLOGY			English	Article						Eocene; dinoflagellate cysts; biostratigraphy; southwestern Siberia		A shallow marine Eocene section recovered in the cored borehole 011-BP, southwestern Siberia, was analyzed palynologically. Age-diagnostic dinoflagellate cyst events including the first occurrences of Charlesdowniea coleothrypta, Dracodinium politum, Ochetodinium romanum, Samlandia chlamydophora, Areosphaeridium diktyoplokum, Hystrichosphaeropsis costae, Wetzeliella eocaenica and Duosphaeridium nudum are recognized at successive levels in the Upper Lulinvor Formation (498.0-459.0 m), indicating a Middle-latest Ypresian age. A hiatus spanning the Early Lutetian is present at an unconformity at 459.0 m which underlies sediments of the uppermost Lulinvor Formation (459.0-456.0 m), which are referred to the Middle Lutetian based on the presence of Costacysta bucina, Cordosphaeridium cantharellus and Wilsonidium echinosuturatum. The overlying interval from 456.0 m to 265.0 m (Tavda Formation) is referred to the latest Lutetian to Priabonian primarily based on a combination of published paleomagnetic signals and the presence of Rhombodinium draco, Membranosphaeridium aspinatum, Svalbardella sp., Thalassiphora fenestrata, Thalassiphora reticulata, Rhombodinium perforatum and Rhombodinium longimanum. According to the combined dinoflagellate cyst data and normal magnetic polarity in the uppermost part of the Tavda Formation, marine sedimentation was interrupted in southwestern Siberia during the Late Priabonian (similar to 34.8 Ma). The dinoflagellate cyst assemblages are illustrated, the new species Thalassiphora dominiquei is formally described and a neotype for Wetzeliella coronata (Vozzhennikova 1967) Lentin & Williams 1976 is designated. The morphology and taxonomy of several taxa are discussed.	[Heilmann-Clausen, Claus] Aarhus Univ, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Iakovleva, Alina I.] Russian Acad Sci, Inst Geol, Moscow 109017, Russia	Aarhus University; Russian Academy of Sciences; Geological Institute, Russian Academy of Sciences	Heilmann-Clausen, C (通讯作者)，Aarhus Univ, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	claus.heilmann@geo.au.dk	Heilmann-Clausen, Claus/A-4848-2012; IAKOVLEVA, ALINA/ABH-9243-2020		Russian Foundation of Fundamental Research [05-05-64910-a, 06-05-64618, 09-05-00210-a, RFFI NSh-4185.2008.5]; Danish Natural Science Research Council [21-04-0298]	Russian Foundation of Fundamental Research(Russian Foundation for Basic Research (RFBR)); Danish Natural Science Research Council(Danish Natural Science Research Council)	M. A. Akhmetiev and V.N. Benyamovsky (Moscow) are thanked for giving access to the material from the borehole 011-BP. G. Aleksandrova (Moscow) and K. Rosendal (Aarhus) are thanked for the chemical palynological preparations. S. B. Andersen is thanked for technical preparation of the plates. Z.N. Gnibidenko is kindly thanked for helpful discussions about the paleomagnetic data. H. Brinkhuis is thanked for reading an earlier version of manuscript. This study was supported by the Russian Foundation of Fundamental Research (Grant RFFI Nos. 05-05-64910-a, 06-05-64618, and 09-05-00210-a; RFFI NSh-4185.2008.5); a PostDoc. for Alina Iakovleva at the Department of Earth Sciences, Aarhus University was supported by Danish Natural Science Research Council (Grant No. 21-04-0298). Finally we wish to thank A. Kothe and H. Nohr-Hansen for their careful and constructive reviews of the manuscript.	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J	Elshanawany, R; Zonneveld, K; Ibrahim, MI; Kholeif, SEA				Elshanawany, Rehab; Zonneveld, Karin; Ibrahim, Mohamed I.; Kholeif, Suzan E. A.			Distribution patterns of recent organic-walled dinoflagellate cysts in relation to environmental parameters in the Mediterranean Sea	PALYNOLOGY			English	Article						Mediterranean Sea; dinoflagellate cysts; temperature; productivity; preservation; eutrophication	BENGUELA UPWELLING REGION; NORTHERN NORTH-ATLANTIC; RECENT MARINE-SEDIMENTS; SURFACE SEDIMENTS; ADRIATIC SEA; SPATIAL-DISTRIBUTION; SEASONAL OCCURRENCE; WEST-COAST; NILE CONE; ASSEMBLAGES	To determine the relationship between the spatial dinoflagellate cyst distribution and oceanic environmental conditions, 34 surface sediments from the Eastern and Western Mediterranean Sea have been investigated for their dinoflagellate cyst content. Multivariate ordination analyses identified sea-surface temperature, chlorophyll-a, nitrate concentration, salinity, and bottom oxygen concentration as the main factors affecting dinoflagellate cyst distribution in the region. Based on the relative abundance data, two associations can be distinguished that can be linked with major oceanographic settings. (1) An offshore eastern Mediterranean regime where surface sediments are characterized by oligotrophic, warm, saline surface water, and high oxygen bottom water concentrations (Impagidinium species, Nematosphaeropsis labyrinthus, Pyxidinopsis reticulata and Operculodinium israelianum). Based on the absolute abundance, temperature is positively related to the cyst accumulation of Operculodinium israelianum. Temperature does not form a causal factor influencing the accumulation rate of the other species in this association. Impagidinium species and Nematosphaeropsis labyrinthus show a positive relationship between cyst accumulation and nitrate availability in the upper waters. (2) Species of association 2 have highest relative abundances in the Western Mediterranean Sea, Strait of Sicily/NW Ionian Sea, and/or the distal ends of the Po/Nile/ Rhone River plumes. At these stations, surface waters are characterized by (relative to the other regime) higher productivity associated with lower sea-surface temperature, salinity, and lower bottom water oxygen concentrations (Selenopemphix nephroides, Echinidinium spp., Selenopemphix quanta, Quinquecuspis concreta, Brigantedinium spp. and Lingulodinium machaerophorum). Based on both the absolute and relative abundances, Selenopemphix nephroides is suggested to be a suitable indicator to trace changes in the trophic state of the upper waters. The distribution of Lingulodinium machaerophorum is related to the presence of river-influenced surface waters, notably the Nile River. We suggest that this species might form a suitable marker to trace past variations in river discharge, notably from the Nile.	[Elshanawany, Rehab; Zonneveld, Karin] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Ibrahim, Mohamed I.] Univ Alexandria, Fac Sci, Dept Environm Sci, Alexandria, Egypt; [Ibrahim, Mohamed I.] Univ Alexandria, Dept Geol, Alexandria, Egypt; [Kholeif, Suzan E. A.] Natl Inst Oceanog & Fisheries NIOF, Alexandria, Egypt	University of Bremen; Egyptian Knowledge Bank (EKB); Alexandria University; Egyptian Knowledge Bank (EKB); Alexandria University; Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF)	Elshanawany, R (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28359 Bremen, Germany.	s_peaedc@uni-bremen.de	Ibrahim, Mohammed/IUQ-7100-2023	Ibrahim, Mohamed Ismail Abdou/0000-0002-5782-0435	international graduate college EUROPROX; DFG; European society	international graduate college EUROPROX; DFG(German Research Foundation (DFG)); European society	Thanks are given to Deutscher Akademischer Austausch Dienst (DAAD) for providing of the first author to study in Bremen University, Germany. Consumables and travel grants were funded by the international graduate college EUROPROX, DFG, and European society funded projects in the group of Karin Zonneveld. We gratefully acknowledge the Historical Geology and Palaeontology group in Bremen University for providing all laboratory facilities and equipment. We particularly thank the captain and crew of Meteor cruises M40/4, M44/3, and M51/3 for providing the investigated sediment samples. We thank Francesca Sangiorgi and Peta Mudie for the constructive reviews of an earlier version of this manuscript. Analyses and visualizations used in this study were produced with the Giovanni online data system, developed and mainted by NASA GES DISC.	Abu El Ella E. 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J	Ribeiro, S; Lundholm, N; Amorim, A; Ellegaard, M				Ribeiro, Sofia; Lundholm, Nina; Amorim, Ana; Ellegaard, Marianne			<i>Protoperidinium minutum</i> (Dinophyceae) from Portugal: cyst-theca relationship and phylogenetic position on the basis of single-cell SSU and LSU rDNA sequencing	PHYCOLOGIA			English	Article						Cyst-theca relationship; Diplopsaloideae; Dinoflagellate cysts; Echinidinium; Islandinium; LSU; Protoperidiniaceae; Protoperidinium minutum; Single-cell PCR; SSU	HETEROTROPHIC DINOFLAGELLATE GENUS; MOTILE STAGE RELATIONSHIPS; SP-NOV; SEDIMENTS; ATLANTIC; SEA; PERIDINIALES; ASSEMBLAGES; ISLANDINIUM; QUATERNARY	Round brown spiny cysts Lire common elements of Recent and Quaternary dinoflagellate cyst records and are often used to infer past climate conditions. Echinidinium and Islandinium. two cyst-based genera composed of round brown spiny cysts, are believed to have affinities within the Protoperidiniaceae. However, their biological counterparts are still virtually unknown. In this study, we examined the cyst-theca relationship of an Echinidinium-like cyst isolated from recent sediments of the Portuguese coast. The cysts (25-34 mu m) had an intercalary theropylic archeopyle and numerous processes (4-9 mu m) with tapered stems and minutely expanded tips. Germinated cells were identified as Protoperidinium minutum on the basis of theca morphology and tabulation. This taxon has a complicated taxonomic history and most likely represents a complex of species with very similar thecae but different cyst morphologies. To provide a First step in elucidating the phylogeny of P. minutum and its evolutionary relationship among the Protoperidiniaceae, we undertook the first molecular study of this taxon on the basis of small-subunit (SSU) and large-subunit (LSU) ribosomal (r)DNA genetic sequences obtained through single-cell polymerase chain reaction. On the basis of SSU rDNA analysis, P. minutum formed a clade together with the Diplopsaloideae, not grouping together with the other Protoperidinium species. LSU rDNA-based phylogenies indicate R minutum as early divergent within the Protoperidiniaceae. The evolutionary significance of round brown spiny cysts produced by P. minutum-like species and diplopsalids is discussed.	[Ribeiro, Sofia; Lundholm, Nina; Ellegaard, Marianne] Univ Copenhagen, Dept Biol, DK-1353 Copenhagen K, Denmark; [Ribeiro, Sofia; Amorim, Ana] Univ Lisbon, Fac Ciencias, Ctr Oceanog, P-1749016 Lisbon, Portugal; [Ribeiro, Sofia] LNEG, Unidade Geol, P-2721866 Alfragide, Portugal	University of Copenhagen; Universidade de Lisboa; Laboratorio Nacional de Energia e Geologia IP (LNEG)	Ribeiro, S (通讯作者)，Univ Copenhagen, Dept Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	sribeiro@bio.ku.dk	Lundholm, Nina/AAY-6249-2020; Ribeiro, Sofia/AAZ-2782-2021; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014; Lundholm, Nina/A-4856-2013; Amorim, Ana/AAA-2615-2020	Ribeiro, Sofia/0000-0003-0672-9161; Ellegaard, Marianne/0000-0002-6032-3376; Lundholm, Nina/0000-0002-2035-1997; Amorim, Ana/0000-0002-9612-4280	Danish Research Council [PDCT/MAR/60086/2004]; Portuguese Foundation for Science and Technology [SFRH/BD/30847/2006]; Fundação para a Ciência e a Tecnologia [SFRH/BD/30847/2006, PDCT/MAR/60086/2004] Funding Source: FCT	Danish Research Council(Det Frie Forskningsrad (DFF)); Portuguese Foundation for Science and Technology(Fundacao para a Ciencia e a Tecnologia (FCT)); Fundação para a Ciência e a Tecnologia(Fundacao para a Ciencia e a Tecnologia (FCT))	SR is grateful to Marten Flo Jorgensen for advice regarding the molecular work. Paula Campos and Tom Gilbert from Eske Willerslev's Ancient DNA and Evolution Research Group are thanked for facilitating access to the Clean Lab. Gert Hansen helped with recommendations for the SEM and Jells Hoeg kindly operated the Z-drive-equipped microscope. Ojvind Moestrup, Antonio Calado and Yuri Oklodkov are acknowledged for useful comments and for sharing their literature collections. Henning Knudsen and Mikako Sasa kindly translated literature from the Japanese. This work has been partially financed through the project "Changes in community structure and microevolution in marine protists" by the Danish Research Council, and project HABCOL (PDCT/MAR/60086/2004) by the Portuguese Foundation for Science and Technology. SR holds a PhD scholarship from the Portuguese Foundation for Science and Technology (SFRH/BD/30847/2006). Two anonymous reviewers are acknowledged for their comments, which helped to improve the manuscript.	Abe T. H., 1981, PUBLICATIONS SETO MA, V6, P1; Abe T. 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J	Birkenmajer, K; Gedl, P; Worobiec, E				Birkenmajer, Krzysztof; Gedl, Przemyslaw; Worobiec, Elzbieta			Dinoflagellate cyst and spore-pollen spectra from the Lower Oligocene Krabbedalen Formation at Kap Brewster, East Greenland	POLISH POLAR RESEARCH			English	Article						Greenland; Kap Brewster; Early Oligocene; biostratigraphy; palynology; dinoflagellate cyst assemblages	BIOSTRATIGRAPHY; ZONATION; EOCENE	Shallow-marine deposits of the Krabbedalen Formation (Kap Dalton Group) from Kap Brewster, central East Greenland, yielded rich dinoflagellate cyst and pollen-spore assemblages. Previously, this formation yielded also rich mollusc and foraminifer age-diagnostic assemblages. A Lower Oligocene age of the Krabbedalen Formation seems to be supported by the dinoflagellate cyst assemblage analysis, while the pollen-spore assemblages point to a wider stratigraphic age range within Oligocene-Middle Miocene.	[Birkenmajer, Krzysztof; Gedl, Przemyslaw] Inst Nauk Geol PAN, PL-31002 Krakow, Poland; [Worobiec, Elzbieta] Inst Bot PAN, PL-31512 Krakow, Poland	Polish Academy of Sciences; Institute of Geological Sciences of the Polish Academy of Sciences; Polish Academy of Sciences	Birkenmajer, K (通讯作者)，Inst Nauk Geol PAN, Senacka 1, PL-31002 Krakow, Poland.	ndbirken@cyf-kr.edu.pl; ndgedl@cyf-kr.edu.pl; e.worobiec@botany.pl		Worobiec, Elzbieta/0000-0001-5997-9602				[Anonymous], 1996, GRONLANDS GEOLOGISKE; [Anonymous], MUSK OX; [Anonymous], 1996, P ODP SCI RESULTS; [Anonymous], 1980, SP PAP PALAEONTOL; Basinger J F., 1994, Cenozoic plants and climates of the Arctic, P175; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BIRKENMAJER K, 2000, POL POL STUD 27 INT, P153; Birkenmajer K., 1977, RAPP GR NLAND GEOL U, V85, P86, DOI [10.34194/rapggu.v85.7537, DOI 10.34194/RAPGGU.V85.7537]; BIRKENMAJER K, 1972, GRONLANDS GEOLOGISKE, V48, P85; Birkenmajer Krzysztof, 1997, Annales Societatis Geologorum Poloniae, V67, P155; Boulter M.C., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P663, DOI 10.2973/odp.proc.sr.104.192.1989; Boulter M.C., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P289; BOULTER M.C., 1994, CENOZOIC PLANTS CLIM; Boulter M C., 1989, Spec Pap Palaeontol, V42, P1; BRINKHUIS H, 1994, PALAEOGEOGR PALAEOCL, V107, P121, DOI 10.1016/0031-0182(94)90168-6; BRINKHUIS H, 1992, THESIS U UTRECHT; COSTA LI, 1979, INITIAL REPORTS DEEP, V48, P513; DAMASSA SP, 1990, REV PALAEOBOT PALYNO, V65, P331, DOI 10.1016/0034-6667(90)90083-U; 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; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Elsik WC., 1978, P 4 INT PAL C LUCKN, P331; Fensome Robert A., 2004, AASP Contributions Series, V42, P1; Firth John V., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P203; HAQ BU, 1987, SCIENCE, V235, P1156, DOI 10.1126/science.235.4793.1156; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; HASSAN MY, 1953, MEDDELELSER GRONLAND, V111; 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; Heilmann-Clausen C., 1990, Geol. 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J	Gómez, F; Moreira, D; López-García, P				Gomez, Fernando; Moreira, David; Lopez-Garcia, Purificacion			<i>Neoceratium</i> gen. nov., a New Genus for All Marine Species Currently Assigned to <i>Ceratium</i> (Dinophyceae)	PROTIST			English	Article						alveolate evolution; Dinoflagellata; Neoceratium gen. nov.; new combination; resting cyst; SSU rDNA phylogeny	FINE-STRUCTURE; DINOFLAGELLATE; IDENTIFICATION; PROTISTS; PLANKTON; HISTORY; SAMPLES; TREES; PCR	The dinoflagellate genus Ceratium contains marine and freshwater species. Freshwater species possess six cingular plates, thick plates in the concave ventral area and usually develop a third hypothecal horn. The marine Ceratium species (>62 species) possess five cingular plates and thin plates in the concave ventral area; a third hypothecal horn is atypical. Resting cysts, a common feature in the freshwater species, are unreported in marine species. We illustrate for the first time resting cysts in marine Ceratium species (C. furca and C. candelabrum). We obtained small subunit ribosomal RNA gene (SSU rDNA) sequences of 23 Ceratium species (more than one third of the total marine species described so far), with representatives of the four acknowledged subgenera. Phylogenetic analyses including the type species, the freshwater C. hirundinella, showed that the four available sequences of freshwater species formed a strongly supported subclade, very distant from the marine cluster. Our data support the splitting of Ceratium sensu lato into two genera. Ceratium sensu stricto should be reserved for fresh water species possessing six cingular plates (three cingular plates in dorsal view). The new genus name, Neoceratium gen. nov. should be applied to the marine species of Ceratium sensula to that possess five cingular plates (two cingular plates in dorsal view). (C) 2009 Elsevier GmbH. All rights reserved.	[Gomez, Fernando] Univ Paris 06, CNRS, UMR 7621, Observ Oceanol Banyuls Sur Mer, F-66651 Banyuls Sur Mer, France; [Moreira, David; Lopez-Garcia, Purificacion] Univ Paris 11, CNRS, UMR 8079, Unite Ecol Systemat & Evolut, F-91405 Orsay, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Universite Paris Saclay; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); AgroParisTech	Gómez, F (通讯作者)，Univ Paris 06, CNRS, UMR 7621, Observ Oceanol Banyuls Sur Mer, Ave Fontaule,BP 44, F-66651 Banyuls Sur Mer, France.	fernando.gomez@fitoplancton.com	Moreira, David/F-7445-2012; Lopez-Garcia, Purificacion/B-6775-2012; Gomez, Fernando/B-2495-2009	Lopez-Garcia, Purificacion/0000-0002-0927-0651; Gomez, Fernando/0000-0002-5886-3488	Ministerio Espanol de Educacion y Ciencia [2007-0213]; French CNRS; ANR Biodiversity project 'Aquaparadox'	Ministerio Espanol de Educacion y Ciencia(Spanish Government); French CNRS(Centre National de la Recherche Scientifique (CNRS)); ANR Biodiversity project 'Aquaparadox'(Agence Nationale de la Recherche (ANR))	This is a contribution to the project DIVERPLAN-MED supported by a post-doctoral grant to F. G. of the Ministerio Espanol de Educacion y Ciencia #2007-0213. P. L. G. and D. M. acknowledge financial support from the French CNRS and the ANR Biodiversity project 'Aquaparadox'. We thank M. Segura and C. Rojo for C. hirundinella samples and the associated Editor and Reviewers for their comments and suggestions.	[Anonymous], HIDROBIOLOGICA; [Anonymous], 1817, NEUE SCHRIFTEN NATUR; [Anonymous], 1954, PUBL I BIOL APL; [Anonymous], U CALIF PUBL ZOOL; Auinger BM, 2008, APPL ENVIRON MICROB, V74, P2505, DOI 10.1128/AEM.01803-07; BAILEY JW, 1855, SMITHSONIAN CONTR KN, V7, P16; Balech E., 1974, Revista Mus argent Cienc nat Bernardino Rivadavia Inst nac Invest Cienc nac (Hydrobiol), V4, P1; Balech E, 1988, DINOFLAGELADOS ATLAN; Balech E., 1980, An. Centro Cienc. del Mar y Limnol. Univ. Nal. Auton. 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F. J., 1963, CSIRO AUST DIV FISH, V14, P1; Zhang H, 2005, J PHYCOL, V41, P411, DOI 10.1111/j.1529-8817.2005.04168.x	86	46	60	3	35	ELSEVIER GMBH, URBAN & FISCHER VERLAG	JENA	OFFICE JENA, P O BOX 100537, 07705 JENA, GERMANY	1434-4610			PROTIST	Protist	JAN	2010	161	1					35	54		10.1016/j.protis.2009.06.004	http://dx.doi.org/10.1016/j.protis.2009.06.004			20	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	536OS	19665427				2025-03-11	WOS:000273054300003
J	Pross, J; Houben, AJP; van Simaeys, S; Williams, GL; Kotthoff, U; Coccioni, R; Wilpshaar, M; Brinkhuis, H				Pross, Joerg; Houben, Alexander J. P.; van Simaeys, Stefaan; Williams, Graham L.; Kotthoff, Ulrich; Coccioni, Rodolfo; Wilpshaar, Martin; Brinkhuis, Henk			Umbria-Marche revisited: A refined magnetostratigraphic calibration of dinoflagellate cyst events for the Oligocene of the Western Tethys	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Paleogene; Oligocene; biostratigraphy; dinoflagellates; Tethys; Italy	NORTH-SEA BASIN; TIME-SCALE; PELAGIC SEQUENCE; MIDDLE EOCENE; BIOSTRATIGRAPHY; TRANSITION; STRATIGRAPHY; GREENHOUSE; PALEOGENE; SEDIMENTS	In order to contribute to the improvement of biostratigraphic age control for the Oligocene of the Western Tethys, we have carried out a high-resolution study of dinoflagellate cysts from three outcrop sections in the Umbria-Marche Basin of Central Italy. All three sections investigated (Contessa Barbetti Road, Monte Cagnero and Pieve d'Accinelli) have magnetostratigraphic age control, thus allowing us to firmly tie the identified dinoflagellate cyst bioevents to the global geomagnetic polarity timescale. The Oligocene succession of the Umbria-Marche Basin is marked by recurrent acmes of Chiropteridium spp., Lingulodinium machaerophorum and Deflandrea spp. that can be correlated between the sections studied. These acmes originate from long-distance transport from near-shore environments into the pelagic setting represented by the sections studied, probably triggered by eustatic sea-level variations. Four formal dinoflagellate cyst zones of Wilpshaar et al. (1996; journal of the Geological Society, London 153. 553-561). viz the Hpu, Clo, Dbi, and Ebu zones are revised. Furthermore we propose two new subzones for the Dbi zone. The new taxon Oligokolpoma galeottii is formally described. (C) 2009 Elsevier B.V. All rights reserved.	[Pross, Joerg; Kotthoff, Ulrich] Goethe Univ Frankfurt, Paleoenvironm Dynam Grp, Inst Geosci, D-60438 Frankfurt, Germany; [Houben, Alexander J. P.; Brinkhuis, Henk] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [van Simaeys, Stefaan] Mobil Cepu Ltd, Exxon Mobil Explorat, Wisma GKBI, Jl Jend, Jakarta 10210, Indonesia; [Williams, Graham L.] Geol Survey Canada, Atlantic Geosci Ctr, Dartmouth, NS B2Y 4A2, Canada; [Coccioni, Rodolfo] Univ Urbino, Dipartimento Sci Uomo Ambiente & Nat, I-61029 Urbino, Italy; [Wilpshaar, Martin] Wintershall Noordzee BASF Grp, NL-2280 CA Rijswijk, Netherlands	Goethe University Frankfurt; Utrecht University; Exxon Mobil Corporation; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; University of Urbino; BASF	Pross, J (通讯作者)，Goethe Univ Frankfurt, Paleoenvironm Dynam Grp, Inst Geosci, Altenhoferallee 1, D-60438 Frankfurt, Germany.	joerg.pross@em.uni-frankfurt.de	Brinkhuis, Henk/B-4223-2009	Brinkhuis, Henk/0000-0003-0253-6610; Houben, Alexander/0000-0002-9497-1048; COCCIONI, Rodolfo/0000-0003-2333-4030	German Research Foundation; State of Hesse	German Research Foundation(German Research Foundation (DFG)); State of Hesse	N. Welters and J. van Tongeren are thanked for the palynological processing of the MCA and PAC samples. Suggestions by D.J. Shillington are gratefully acknowledged. Two anonymous referees provided thoughtful reviews of an earlier version of the manuscript. JP acknowledges support through the German Research Foundation and the funding program "LOEWE - Landes-Offensive zur Entwicklung Wissenschaftlich-okonomischer Exzellenz" of the State of Hesse. This is publication no. 34 of the GEOPCAP Section (DiSUAN) of Urbino University.	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Palaeobot. Palynology	JAN	2010	158	3-4					213	235		10.1016/j.revpalbo.2009.09.002	http://dx.doi.org/10.1016/j.revpalbo.2009.09.002			23	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	549VW					2025-03-11	WOS:000274083400001
J	Riding, JB; Kyffin-Hughes, JE				Riding, James B.; Kyffin-Hughes, Jane E.			The use of pre-treatments in palynological processing	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						palynomorph preparation techniques; pre-treatment; sodium hexametaphosphate; Carboniferous; United Kingdom (Scotland)	DINOFLAGELLATE CYSTS; SEDIMENTS	A sample of palynomorph-rich Upper Carboniferous mudstone from Scotland was separately pre-treated overnight with acetone, two detergent solutions, formic acid, household bleach (two methods), methylated spirits and white spirit prior to palynological preparation using sodium hexametaphosphate [(NaPO3)(6)]. The aim of this study was to identify effective methods of pre-treatment that would increase palynomorph yields using the (NaPO3)(6) method. Pre-treatment generally increased the mass of sample that was broken down by the (NaPO3)(6) technique. Detergent one (carpet cleaner), formic acid, household bleach and white spirit allowed the disaggregation of more rock than without any pre-treatment. However, formic acid produced a lower concentration of Carboniferous miospores than with no pre-treatment. Pre-treatment with acetone, detergent two (industrial detergent) and methylated spirits actually decreased the weight of rock that was disaggregated with (NaPO3)(6). Despite this, all these three pre-treatments improved the palynomorph yield as compared to with no pre-treatment. Moreover, all the pre-treatments except formic acid improved palynomorph productivity. The effectiveness of pre-treatments was demonstrated by the increased absolute numbers of indigenous palynomorphs extracted. However, the concentrations of miospores per gram of rock are more significant. Acetone, both detergent solutions, methylated spirit and white spirit significantly improved the amounts of palynomorph extracted. Household bleach was found to lighten and selectively destroy relatively delicate palynomorphs; this reagent should be used with caution, and only with robust material. In the subsample soaked overnight in 5% bleach solution, all the exotic Lycopodium spores added were destroyed. By contrast in the subsample treated with 2.5% bleach solution for 6 h, a small proportion of the exotic Lycopodium spores survived. This study indicates that the (NaPO3)(6) method using either detergent or white spirit as a pre-treatment is highly effective at extracting palynomorphs from clay-rich lithotypes. However the concentration of palynomorphs obtained is generally lower than those from mineral acid digestions. (C) 2009 Natural Environment Research Council Published by Elsevier B.V. All rights reserved.	[Riding, James B.; Kyffin-Hughes, Jane E.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk; jeky@bgs.ac.uk			British Geological Survey (BGS) Laboratory Maintenance and Development of Capability; NERC [bgs04003] Funding Source: UKRI	British Geological Survey (BGS) Laboratory Maintenance and Development of Capability; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This contribution was funded by the British Geological Survey (BGS) Laboratory Maintenance and Development of Capability Project managed by Shaun Reeder (BGS, Nottingham). The authors thank Fabienne Marret-Davies, Kenneth N. Mertens, Stewart G. Molyneux and Michael H. Stephenson for their perceptive reviews of the manuscript. 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Palaeobot. Palynology	JAN	2010	158	3-4					281	290		10.1016/j.revpalbo.2009.09.009	http://dx.doi.org/10.1016/j.revpalbo.2009.09.009			10	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	549VW		Green Accepted			2025-03-11	WOS:000274083400007
J	Brittain, JM; Higgs, KT; Riding, JB				Brittain, Jennifer M.; Higgs, Kenneth T.; Riding, James B.			The palynology of the Pabay Shale Formation (Lower Jurassic) of SW Raasay, northern Scotland	SCOTTISH JOURNAL OF GEOLOGY			English	Article							LOWER LIAS GROUP; INNER HEBRIDES; STAFFIN BAY; AREA; PALYNOMORPHS; RADIATION; SEQUENCE; BOREHOLE	A thermally-mature palynomorph assemblage containing significant proportions of the characteristic dinoflagellate cyst Liasidium variabile Drugg 1978 was recovered from the Lower Jurassic Pabay Shale Formation of SW Raasay. This is the first record of this biostratigraphically important species from the Jurassic of onshore Scotland. Liasidium variabile is a zonal index for the Late Sinemurian in NW Europe, and this occurrence allows a correlation to the Oxynotum Zone of this substage. This is the first evidence for this chronozone on Raasay. Furthermore, the presence of morphotypes A and B of Liasidium variabile indicates a probable correlation to the Oxynotum Subzone of the Oxynotum Zone. This interpretation is not consistent with a hiatus within the Upper Sinemurian succession on Raasay.	[Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England; [Brittain, Jennifer M.; Higgs, Kenneth T.] Natl Univ Ireland Univ Coll Cork, Dept Geog, Cork, Ireland	UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University College Cork	Riding, JB (通讯作者)，British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England.	jbri@bgs.ac.uk			NERC [bgs05001] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Ainsworth N.R., 1989, Northwest European Micropaleontology and Palynology, P1; Ainsworth N.R., 1987, Petroleum Geology of North West Europe, P611; [Anonymous], 1980, Special Papers; [Anonymous], 1980, Special Report; [Anonymous], 1985, SPOROPOLLENIN DINOFL; [Anonymous], 1996, Palynology: principles and applications; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; Berridge N.G., 1999, MEMOIR BRIT GEOLOGIC, V127, P1; BRADSHAW MJ, 1982, SCOT J GEOL, V18, P131, DOI 10.1144/sjg18020131; BRENNER W., 1986, Neues Jahrbuch fur Geologie und Paleontologie Abhandlungen, V173, P131; Bujak J.P., 1983, AM ASS STRATIGRAPHIE, V13, P1; Cox B.M., 2002, British Middle Jurassic Stratigraphy (No. 26); Drugg W.S., 1978, Palaeontographica Abteilung B Palaeophytologie, V168, P61; DYBKJAER K., 1988, DANMARKS GEOLOGISKE, V21, P1; Dybkjaer K., 1991, DANMARKS GEOLOGISK A, V30, P1; FAUCONNIER D, 1995, REV PALAEOBOT PALYNO, V87, P15, DOI 10.1016/0034-6667(94)00142-7; FAUCONNIER D, 1997, BULL CENT RECH ELF E, V17, P225; Feist-Burkhardt S., 1992, Cahiers de Micropaleontologie Nouvelle Serie, V7, P141; Feist-Burkhardt Susanne, 1994, Revue de Paleobiologie, V13, P313; Feist-Burkhardt S, 2009, NEUES JAHRB GEOL P-A, V254, P293, DOI 10.1127/0077-7749/2009/0019; Fensome R.A., 1996, Palynology: principles and applications, V1, P107; Fensome RA, 1996, PALEOBIOLOGY, V22, P329, DOI 10.1017/S0094837300016316; Fensome Robert A., 1995, Eisenack Catalog of Fossil Dinoflagellates New Series, V3, P1463; GAUNT GD, 1980, I GEOLOGICAL SCI REP, P1; Getty T.A., 1973, University of Kansas Paleontological Contributions, V63, P1; Hesselbo SP, 1998, SCOT J GEOL, V34, P23, DOI 10.1144/sjg34010023; Howarth M.K., 1956, P YORKS GEOL SOC, V30, P353; Lee G.W., 1920, MEMOIR GEOLOGICAL SU; Lund JJ, 2002, COUR FOR SEKENBG, V241, P69; MELLERE D, 1996, SPECIAL PUBLICATION, V117, P49; MOLDOVANU M, 1987, ANALE U BUCURESTI, P67; Morbey S.J., 1978, CONTINENTAL SHELF I, V100, P47; Morbey S.J., 1978, Palinologia numero extraordinario, V1, P355; Morton N, 1999, SCOT J GEOL, V35, P119, DOI 10.1144/sjg35020119; Morton N, 1995, FIELD GEOLOGY OF THE BRITISH JURASSIC, P209; Morton N, 1999, SCOT J GEOL, V35, P85, DOI 10.1144/sjg35010085; Morton N., 1965, Scottish Journal of Geology, V1, P189; Morton N., 1976, SCOTLAND J GEOLOGY, V12, P23, DOI [DOI 10.1144/SJG12010023, 10.1144/sjg12010023]; MORTON N, 1992, SPECIAL PUBLICATIONS, V62, P97; Oates M.J., 1978, Proceedings of the Yorkshire Geological Society, V42, P143; PAGE KN, 1992, NEWSL STRATIGR, V27, P129; Palliani RB, 2000, P YORKS GEOL SOC, V53, P1, DOI 10.1144/pygs.53.1.1; PARTINGTON MA, 1993, PETROLEUM GEOLOGY OF NORTHWEST EUROPE: PROCEEDINGS OF THE 4TH CONFERENCE, P371, DOI 10.1144/0040371; POULSEN N.E., 1996, American Association of Stratigraphic Palynologists, Contribution Series, V31, P1; Poulsen Niels E., 2003, Geological Survey of Denmark and Greenland Bulletin, V1, P115; RAUSCHER R, 1990, REV PALAEOBOT PALYNO, V62, P107, DOI 10.1016/0034-6667(90)90020-J; RICHEY JE, 1961, BRIT REGIONAL GEOLOG; 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., 1992, WH92307R BRIT GEOL S; Riding James B., 1999, Palynology, V23, P15; Riding James B., 1991, Palynology, V15, P115; Riding JB, 1997, SCOT J GEOL, V33, P59, DOI 10.1144/sjg33010059; RIDING JB, 1992, SCOT J GEOL, V28, P155, DOI 10.1144/sjg28020155; Riding JB, 2003, P YORKS GEOL SOC, V54, P223, DOI 10.1144/pygs.54.4.223; RIDING JB, 1985, NEWSL STRATIGR, V14, P96; RUEDAGAXIOLA J, 1999, GEOL S AM S, P229; SELLWOOD B W, 1972, Palaeontology (Oxford), V15, P125; Simms M.J., 2004, British Lower Jurassic stratigraphy, V30; van de Schootbrugge B, 2007, PALAEOGEOGR PALAEOCL, V244, P126, DOI 10.1016/j.palaeo.2006.06.026; van de Schootbrugge B, 2005, PALEOBIOLOGY, V31, P73, DOI 10.1666/0094-8373(2005)031<0073:EJCCAT>2.0.CO;2; WEISS M, 1986, NEUES JB GEOLOGIE PA, P317; WILLIAMS GL, 2001, GEOLOGY CONTINENTAL, V2, P89; Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; WOOLLAM R, 1983, I GEOLOGICAL SCI REP, P1	66	8	9	0	16	GEOLOGICAL SOC PUBL HOUSE	BATH	UNIT 7, BRASSMILL ENTERPRISE CENTRE, BRASSMILL LANE, BATH BA1 3JN, AVON, ENGLAND	0036-9276			SCOT J GEOL	Scott. J. Geol.		2010	46		1				67	75		10.1144/0036-9276/01-391	http://dx.doi.org/10.1144/0036-9276/01-391			9	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	606MF		Green Accepted			2025-03-11	WOS:000278428400008
J	Kodrans-Nsiah, M; März, C; Harding, IC; Kasten, S; Zonneveld, KAF				Kodrans-Nsiah, Monika; Maerz, Christian; Harding, Ian C.; Kasten, Sabine; Zonneveld, Karin A. F.			Are the Kimmeridge Clay deposits affected by "burn-down" events? Palynological and geochemical studies on a 1 metre long section from the Upper Kimmeridge Clay Formation (Dorset, UK)	SEDIMENTARY GEOLOGY			English	Review						Kimmeridge Clay (Dorset, UK); Preservation; Productivity; Oxidation; Palynology; Trace metals	ORGANIC-MATTER PRESERVATION; OXYGEN EXPOSURE TIME; TRACE-METALS; RICH SEDIMENTS; WATER COLUMN; DEEP-SEA; POSTDEPOSITIONAL OXIDATION; PALEOPRODUCTIVITY PROXIES; SEQUENCE STRATIGRAPHY; SELECTIVE DEGRADATION	Two independent analytical approaches, pallynology and inorganic geochemistry, were applied to identify potential oxygen "bum-down" events in the Late Jurassic Kimmeridge Clay Formation (KCF). The KCF interval of the rotunda ammonite zone, spanning 121.82-122.72 m depth was sampled from the Swanworth Quarry 1 borehole (Dorset UK) at 2.5-5.0 cm resolution. Samples were analysed for total organic carbon (TOC), concentrations of elements that are known to be productivity- and/or nutrient-related (e.g. Cu, P), detrital (e.g. Al, Ti, Zr) and redox-sensitive/ sulphide-forming (eg. V, Mo, Fe, Mn, S), and palynofacies components including analysis of organic-walled dinoflagellate cysts (dinocysts) on a species level. The TOC contents generally exceed 2 wt.%, with a maximum of 8.8 wt.% at 122.37 cm depth and elevated values in the central part of the investigated interval. This interval of relatively higher TOC values correlates well with the maximum recovery of marine palynomorphs and low Al values, suggesting that the TOC is primarily of marine organic matter (OM). Changes in V/Al, Mo/Al, Fe/Al, Mn/AI and S patterns at 122.37 m depth mark a shift from anoxic conditions in the lower part of the studied interval to more oxic conditions in its upper part. Such a shift could explain the relatively high TOC and marine palynomorph concentrations in the lower part of the studied interval as a result of better preservation, and the subsequent decrease as an effect of a post-depositional "bum-down", i.e. OM oxidation. As the amount of marine palynomorphs and TOC content diminishes from the middle part of the section upwards, species-specific changes in dinocyst assemblages can be observed. In particular, concentrations of Circulodinium spp., Cyclonephelium spp., Sirmiodinium grossi, Senoniasphaera jurassica and Systematophora spp. decrease rapidly in comparison to other species, such as Glossodinium dimorphum and Cribroperidinium sp. 1, which may suggest selective degradation of dinocysts due to oxidation. We suggest that post-depositional oxygenation of bottom and pore waters within the sediment was most probably the cause for decreasing TOC values and reduced recovery of marine palynomorphs towards the top of the studied interval in comparison to high TOC and marine palynomorph values in the central part of the studied interval due to anoxic conditions. (C) 2009 Elsevier B.V. All rights reserved.	[Kodrans-Nsiah, Monika; Maerz, Christian; Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; [Harding, Ian C.] Univ Southampton, Natl Oceanog Ctr, Sch Earth & Ocean Sci, Southampton SO14 3ZH, Hants, England; [Kasten, Sabine] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	University of Bremen; NERC National Oceanography Centre; University of Southampton; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Kodrans-Nsiah, M (通讯作者)，Univ Szczecin, Geosci Fac, Mickiewicza 18, PL-70383 Szczecin, Poland.	monika.kodrans-nsiah@univ.szczecin.pl	Harding, Ian/K-3320-2012	Harding, Ian/0000-0003-4281-0581; Kasten, Sabine/0000-0001-7453-5137; , Christian/0000-0003-2558-4711	DFG [EUROPROX]	DFG(German Research Foundation (DFG))	We thank John E. A. Marshall for helpful comments on the initial manuscript. This study was supported by DFG grant EUROPROX. The samples were provided by BGS in Keyworth.	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Geol.	DEC 15	2009	222	3-4					301	313		10.1016/j.sedgeo.2009.09.015	http://dx.doi.org/10.1016/j.sedgeo.2009.09.015			13	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	530BV					2025-03-11	WOS:000272564800009
J	Wu, CH				Wu, Chau H.			Palytoxin: Membrane mechanisms of action	TOXICON			English	Review						Palytoxin; Cation channel; Na,K-ATPase; Na+,K+-adenosine triphosphatase; Na,K-pump; P-type ATPase; Ciguatera; Ouabain	NA,K-ATPASE ALPHA-SUBUNIT; CYSTEINE-SCANNING MUTAGENESIS; VASCULAR SMOOTH-MUSCLE; GROWTH-FACTOR RECEPTOR; MAMMALIAN SODIUM-PUMP; INDUCED NA+ INFLUX; TRANSMEMBRANE SEGMENT; PUTATIVE PALYTOXIN; TUMOR PROMOTER; PALYTHOA-CARIBAEORUM	Palytoxin is a marine toxin originally isolated from the zoantharians of the genus Palythoa, but now is found in marine organisms ranging from dinoflagellates to fishes. With a MW of 2680, it is one of the largest nonpolymeric natural products ever found. Its complex structure has been elucidated and total synthesis has been achieved. With an LD50 Of 25 ng/kg for rabbits (the most sensitive species), it is one of the most lethal marine toxins. It binds to the Na,K-ATPase specifically with a K-D of 20 pM. It has a unique action on the Na,K-ATPase, converting the pump into an ion channel and resulting in K+ efflux, Na+ influx and membrane depolarization. As a result palytoxin causes a wide spectrum of secondary pharmacological actions. By acting like a key to unlock the internal structure of the Na,K-ATPase, palytoxin holds promise as a useful tool for investigation of the pump molecule. (C) 2009 Elsevier Ltd. All rights reserved.			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J	Prauss, ML				Prauss, Michael L.			The K/Pg boundary at Brazos-River, Texas, USA - An approach by marine palynology	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						Cretaceous; Palaeogene; Impact; Palynology; Dinocysts	CRETACEOUS-TERTIARY BOUNDARY; K-T-BOUNDARY; SEA-LEVEL FLUCTUATIONS; DINOFLAGELLATE CYSTS; MASS EXTINCTION; CHICXULUB IMPACT; ENVIRONMENTAL-CHANGES; SPECIES SURVIVORSHIP; CONTIGUOUS STRATA; WESTERN INTERIOR	Two cores and one outcrop section from the Cretaceous/Palaeogen (K/Pg) boundary interval at the Brazos-River area, Texas, USA, have been high resolution sampled and analysed fully quantitatively by marine palynology. The results have been compared and integrated with data from micropalaeontology, sedimentology and isotope-geochemistry from the same sections. Within all three sections, the K/Pg boundary, defined as the base of the PO foraminifera zone and the onset of a negative carbon isotope anomaly, closely corresponds to the appearance of lowermost Danian organic-walled dinocysts. Based on various palynological proxies as well as on sedimentologic features, a sequence stratigraphic subdivision of the sections is proposed. From a synopsis of all three sections, a long term, punctuated drop of relative sea-level is indicated, starting at about the top of the Upper Cretaceous CF2 foraminifera zone and reaching a minimum within the upper P1a zone of the Lower Palaeogene. This is followed by a prominent transgression starting within the P1a/P1b boundary interval. The "event deposit" (ED), a siliciclastic unit located well below the base of the PO foraminifera zone in the present sections, most probably represents a combination of both episodic relative sea-level fall and lag deposit due to initial transgression. It is preceded by significant fluctuations of climatic boundary conditions, with cool climates correlating to heavier delta C-13 values and increased p/g ratio of dinocysts, suggestive of higher marine primary productivity. Across the K/Pg boundary, a prominent increase and spike of the warm-temperate waters dinocysts fraction is documented, represented mainly by Trithyrodinium evittii, which is accompanied by climatic warming and an episodic relative sea-level rise. Thus, prominent paleo-environmental changes and sea-level fluctuations precede and coincide with the K/Pg boundary proper. These data are inconsistent with a single "catastrophic" impact as the cause for the K/Pg boundary event, but suggest relative longer term environmental stress as finally leading to End-Cretaceous crisis of the biosphere. Between the ED and the K/Pg boundary proper, the gradual increase to peak abundance in trilete spores demonstrates a significant time lag between these two horizons. According to the distinct distribution of this peak abundance, it cannot be excluded that an impact/tsunami event is related to the lower portion of the ED. In contrast, no significant changes within most palynologic proxies are documented across the yellow clay layer below the ED documented within one of the sections and recently suggested as the original Chicxulub impact ejecta horizon. This questions the impact origin of this horizon or, at least, suggests only little consequences of this event on the ecosystem. (C) 2009 Elsevier B.V. All rights reserved.	Free Univ Berlin, Inst Geol Sci, Sect Palaeontol, D-12249 Berlin, Germany	Free University of Berlin	Prauss, ML (通讯作者)，Free Univ Berlin, Inst Geol Sci, Sect Palaeontol, Malteser Str 74-100,Bldg D, D-12249 Berlin, Germany.	mprauss@zedat.fu-berlin.de			Deutsche Forschungsgemeinschaft, DFG [Pr 288/3-1]	Deutsche Forschungsgemeinschaft, DFG(German Research Foundation (DFG))	Sample material for the core KT-1 has been provided by Wolfgang Stinnesbeck, Heidelberg University, Germany. The samples for core Mullinax-I and the outcrop sections CMA-CMB have been provided by Gerta Keller, Princeton University, U.S.A., who also did a stratigraphic analyses on planktonic foraminifera for core MullinaxI and outcrop CMA-CMB, as well as valuable stratigraphical reanalysis of planktonic foraminifera for core KT-1. The data from geochernical analyses have been provided by Doris Stilben and research group, Karlsruhe University, and Sigal Abramovich, Ben Gurion University, Negev Beer Sheva, Israel. Mazeration of sediments and initial examination of palynomorphs for the core KT-1 have been facilitated by Volker Mosbrugger and research group, Tijbingen University, Germany. Mazeration of sediments for core Mullinax-1 and outcrop CMA-CMB have been done at the Museum of Natural History, Berlin. The critical and constructive suggestions by Paul Schioler and two anonymous reviewers are greatly acknowledged. The project has been supported by a research grant of the Deutsche Forschungsgemeinschaft, DFG, grant number Pr 288/3-1.	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Wood G.D., 1996, PALYNOLOGY PRINCIPLE, V1, P29; Yancey T.E., 1996, GULF COAST ASS GEOLO, V46, P433; ZACHOS JC, 1989, NATURE, V337, P61, DOI 10.1038/337061a0; [No title captured]	108	20	22	1	23	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0031-0182	1872-616X		PALAEOGEOGR PALAEOCL	Paleogeogr. Paleoclimatol. Paleoecol.	DEC 10	2009	283	3-4					195	215		10.1016/j.palaeo.2009.09.024	http://dx.doi.org/10.1016/j.palaeo.2009.09.024			21	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	524DT					2025-03-11	WOS:000272124700009
J	Kobanova, GI				Kobanova, G. I.			Morphology and Life Cycle of <i>Gymnodinium baicalense</i> Ant. (Dinophyceae) from Lake Baikal	CONTEMPORARY PROBLEMS OF ECOLOGY			English	Article						Gymnodinium baicalense; living material; dinoflagellates; photomicrographs; sexual reproduction; resting cysts; congener relations		Living populations of Gymnodinium baicalense Ant. from Lake Baikal were studied. It has been shown that G. baicalense var. minor Ant. is a life stage of G. baicalense, whose species size is smaller than it is given in the diagnosis. Morphology of the living vegetative cells of G. baicalense is close to that of G. wigrense Wolosz. These species share ecological features. The vegetative cells form endogenous resting cysts. The sexual reproduction takes place in the period of the mass development of the species. The author believes that it is a relict species, which formed in the Ice age.	Irkutsk State Univ, Res Inst Biol, Irkutsk 664003, Russia	Irkutsk State University	Kobanova, GI (通讯作者)，Irkutsk State Univ, Res Inst Biol, Ul Lenina 3, Irkutsk 664003, Russia.	kobanov@iszf.irk.ru			Development of Scientific Potential of the Higher School [2.1.1/1359]	Development of Scientific Potential of the Higher School	The work is completed with the financial support of the analytical departmental target program "Development of Scientific Potential of the Higher School (2009-2010)," project no. 2.1.1/1359.	ANTIPOVA NL, 1955, DOKL AKAD NAUK SSSR+, V103, P325; DAVIDOVICH NA, 2007, MORPHOLOGY CELL BIOL, P5; DREBES G, BOT MONOGRAPHS, V13, P250; IZMESTJEVA LR, 1988, LONG RANGE PROJECTIO, P97; KISELEV IA, 1954, PYRROPHYTE ALGAE; KOBANOVA GI, 2007, P INT C LEMA ST PET, P121; KOZHOVA O M, 1977, Gidrobiologicheskii Zhurnal, V13, P77; MATVIENKO OM, 1977, PYRROPHYTA; MIKHEEVA TM, 1999, ALGAE FLORA BELARUS; Popovskaya G. I, 1987, MARINE FRESHWATER PL, P107; Sedova T. V, 1996, KARYOLOGY ALGAE; SEDOVA TV, 1977, FUNDAMENTALS CYTOLOG; SHUKANOV AS, 2009, ALGOLOGY MYCOLOGY; SIGEE DC, 1986, ADV BOT RES, V12, P205, DOI 10.1016/S0065-2296(08)60195-0; STARMACH K, 1974, CHRYPTOPHYCEA KRYPTO; STEIDINGER KA, 1980, FREE LIVING DINOFLAG, P407; TANICHEV AI, 1995, ATLAS GUIDE PELAGOBI, P151	17	2	2	1	7	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	1995-4255			CONTEMP PROBL ECOL	Contemp. Probl. Ecol.	DEC	2009	2	6					581	585		10.1134/S1995425509060150	http://dx.doi.org/10.1134/S1995425509060150			5	Ecology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology	538JP					2025-03-11	WOS:000273180700015
J	Coolen, MJL; Shtereva, G				Coolen, Marco J. L.; Shtereva, Galina			Vertical distribution of metabolically active eukaryotes in the water column and sediments of the Black Sea	FEMS MICROBIOLOGY ECOLOGY			English	Article						Black Sea; suboxic; sulfidic; 18S rRNA gene transcripts; DGGE; active eukaryotes	CALANUS-EUXINUS; MICROBIAL EUKARYOTES; DEEP-SEA; DINOFLAGELLATE CYSTS; OIKOPLEURA-DIOICA; DIVERSITY; RNA; GRADIENT; BASIN; DNA	Recent DNA-based phylogenetic studies have reported high eukaryotal diversities in a wide range of settings including samples obtained from anoxic environments. However, parallel RNA-based surveys are required in order to verify whether the species detected are in fact metabolically active in such extreme environments. The Black Sea is the World's largest anoxic basin but remains undersampled with respect to molecular eukaryotic diversity studies. Here, we report the distribution of active eukaryotes (18S rRNA-based survey) along a vertical nutrient and redox gradient in the water column and surface sediments of the Black Sea. A wide variety of eukaryotes were active in suboxic deep waters. Notably, certain species were active but escaped detection during a parallel 18S rDNA survey. The 18S rDNA survey from surface sediments yielded taxa of pelagic origin but none of these were identified from the water column at the time of sampling. Our data also indicate that gene transcripts do not always provide unequivocal proof that active microorganisms are indigenous to a specific position in an environmental gradient, because certain zoo- and phytoplankton species were still viable with detectable 18S rRNA in up to 300-year-old sulfidic sediments that underlie similar to 830 in of sulfidic waters.	[Coolen, Marco J. L.] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA; [Shtereva, Galina] Bulgarian Acad Sci, Inst Oceanol, Varna, Bulgaria	Woods Hole Oceanographic Institution; Bulgarian Academy of Sciences	Coolen, MJL (通讯作者)，Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, 360 Woods Hole Rd, Woods Hole, MA 02543 USA.	mcoolen@whoi.edu	Coolen, Marco/B-8263-2015	Coolen, Marco/0000-0002-0417-920X	US National Science Foundation [OCE 0602423]; WHOI's Access to the Sea program; Andrew W. Mellon Foundation	US National Science Foundation(National Science Foundation (NSF)); WHOI's Access to the Sea program; Andrew W. Mellon Foundation	We would especially like to thank Ognyana Hristova and Tatyana Nikolova, IOBAS, for the analysis of the water column chemistry and Dr Cornelia Wuchter, Dr Angela Dickens, Alan Gagnon, Daniel Montlucon, Chris Ward (WHOI), and the R/V Akademik staff, in particular Delcho Solakov, for their extensive organizational and participatory help with the cruise. We thank Dr Timothy Eglinton (WHOI) and two anonymous reviewers for suggestions to improve the manuscript. We are grateful for the financial support from the US National Science Foundation grant OCE 0602423, as well as funding from WHOI's Access to the Sea program, and a grant from the Andrew W. Mellon Foundation Endowed Fund for Innovative Research.	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Ecol.	DEC	2009	70	3					525	539		10.1111/j.1574-6941.2009.00756.x	http://dx.doi.org/10.1111/j.1574-6941.2009.00756.x			15	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	527EE	19732144	Bronze			2025-03-11	WOS:000272348800018
J	Eldrett, JS; Harding, IC				Eldrett, James S.; Harding, Ian C.			Palynological analyses of Eocene to Oligocene sediments from DSDP Site 338, Outer Voring Plateau	MARINE MICROPALEONTOLOGY			English	Article						palynology; Eocene-Oligocene; Voring Plateau; Norwegian-Greenland Sea; palaeoenvironment	DINOFLAGELLATE CYST STRATIGRAPHY; ANTARCTIC GLACIATION; ATMOSPHERIC CO2; NORWEGIAN SEA; ARCTIC-OCEAN; GREENLAND; PALEOGENE; NORTH; TRANSITION; BASIN	Against the background of the profound global climatic shift from greenhouse to icehouse conditions during the Eocene-Oligocene transition, major geographic and oceanographic changes were taking place in the Norwegian-Greenland Sea region. The Voring Plateau was a prominent structural feature which influenced the evolution of water mass circulation in the Nordic seas, and we present detailed palaeoenvironmental reconstructions of this structure. New palynological results suggest that shallow water inner-neritic environments were developed across parts of the Voring Plateau during early Eocene times, with terrestrial and brackish water palynomorphs indicating that both basement highs to the north, and the crestal part of the Voring Escarpment, may have been emergent. A transition from marginal-marine to open marine conditions occurred around 44 Ma ago, with the complete subsidence of the Voting Plateau below sea level, facilitating inter-basinal surface water circulation and promoted a significant increase in photic zone fertility. Carbon sequestration associated with such enhanced productivity in the late Eocene Nordic seas may have contributed to declining Cenozoic atmospheric carbon dioxide levels, thence to declining global temperatures and the development of limited Northern Hemisphere continental ice on Greenland in the latest Eocene. (C) 2009 Elsevier B.V. All rights reserved.	[Eldrett, James S.] Shell UK Ltd, Aberdeen AB12 3FY, Scotland; [Harding, Ian C.] Univ Southampton, Southampton Oceanog Ctr, Sch Ocean & Earth Sci, Southampton SO14 3ZH, Hants, England	Royal Dutch Shell; University of Southampton; NERC National Oceanography Centre	Eldrett, JS (通讯作者)，Shell UK Ltd, 1 Altens Farm Rd, Aberdeen AB12 3FY, Scotland.	james.eldrett@shell.com; ich@noc.soton.ac.uk	Harding, Ian/K-3320-2012	Eldrett, James/0000-0001-5196-3112; Harding, Ian/0000-0003-4281-0581	U.S. National Science Foundation (NSF); American Association of Stratigraphic Palynologists (AASP); The Geological Society of London; The Micropalaeontological Society (TMS); Natural Environment Research Council (NERC)	U.S. National Science Foundation (NSF)(National Science Foundation (NSF)); American Association of Stratigraphic Palynologists (AASP); The Geological Society of London; The Micropalaeontological Society (TMS); Natural Environment Research Council (NERC)(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	This research used samples provided by the Ocean Drilling Program (ODP). ODP was sponsored by the U.S. National Science Foundation (NSF) and participating countries under management of joint Oceanographic Institutions (JOI), Inc.. We also thank S. Akbari for palynological processing and to the manuscript reviewers Prof Henk Brinkuis (Utrecht University) and Prof Claus Heilmann-Clausen for their helpful suggestions, which have greatly improved the final manuscript.We also thank the American Association of Stratigraphic Palynologists (AASP), The Geological Society of London, The Micropalaeontological Society (TMS) and the Natural Environment Research Council (NERC) for funding this research.	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Micropaleontol.	DEC	2009	73	3-4					226	240		10.1016/j.marmicro.2009.10.004	http://dx.doi.org/10.1016/j.marmicro.2009.10.004			15	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	530EW					2025-03-11	WOS:000272572800008
J	Wood, AM				Wood, Adrian M.			The phylogeny and palaeozoogeography of cold-water species of ostracod (Crustacea) from the Pre-Ludhamian Stage (late Pliocene-early Pleistocene), Red Crag Formation, East Anglia, England; with reference to the earliest arrival of Pacific species	PALEONTOLOGICAL RESEARCH			English	Review						Ostracoda (Crustacea); palaeozoogeography; phylogeny; Pliocene; transoceanic dispersal	SEA-LEVEL CHANGES; DINOFLAGELLATE CYST; MARINE OSTRACODA; NORTH; JAPAN; MA; ASSEMBLAGES; DISPERSAL; DEPOSITS; POLLEN	The Pliocene Epoch represents a significant period in the palaeozoogeography of North Atlantic, Arctic and northern Pacific podocopid ostracods. A climate crash during Marine Isotope Stage (MIS) G6 (c. 2.74 Ma) resulted in the extinction of early-mid Pliocene thermophilic ostracods and the subsequent emergence of oligothermal assemblages during the late Pliocene. During the numerous cold stages of the late Pliocene-early Pleistocene Arctic ostracod species were able to disperse southwards into the mid-latitudes of the North Atlantic. The Pre-Ludhamian Stage of the Red Crag Formation, Suffolk, England spans one such episode (c. 2.7-2.41 Ma) and thus offers new insight into the vagility of shallow marine ostracods as they responded to glacio-eustatic and isostatic changes. Five podocopid ostracods are described from the Sizewell Member (Pre-Ludhamian Stage) of the Red Crag Formation and new information regarding their phylogeny and palaeozoogeography is presented. Four of the species are new to science, Microcytherura gelida sp. nov., Thaerocythere liebaui sp. nov., Thaerocythere russus sp. nov. and Pectocythere hollowayae sp. nov., while the fifth, Neomonoceratina tsurugasakensis (Tabuki), is reexamined and reassigned. The comparative morphology of Pectocythere Hanai and Kotoracythere Ishizaki is reviewed and a morphological continuum recognized between phenotypic end-members. Pectocythere hollowayae sp. nov. forms part of a distinctive morphological group comprising Arctic and northern Pacific species: P. ishizakii Irizuki and Yamada, Pectocythere? sp. cf. P.? dentarticulata (Smith) sensu Swain and Gilby, Kotoracythere sp. Irizuki, P. janae Brouwers and P. parkerae Swain and Gilby. Although lacking a distinctive caudal process, Paijenborchella tsurugasakensis Tabuki is reassigned to Neontonoceratina sensu Zhao and Whatley. Neontonoceratina tsurugasakensis displays some minor polymorphism over an enormous geo-temporal range that extends from the early Miocene of the northwestern Pacific to the late Pliocene-early Pleistocene of the southern North Sea Basin. Despite its lack of pelagic larvae N. tsurugasakensis was capable of transoceanic dispersal, evidenced by its occurrence in the early Pliocene (c.4.90-4.81 Ma), Oosterhout Formation, Western Netherlands Basin, alongside other pan-Arctic and North Pacific ostracod taxa. Mechanisms of dispersal remain unclear but could involve passive transport on Fucus brown algae, aided by the Transpolar Drift. Further agents of dispersion could include fish and birds. The viability of water birds as vectors of invertebrate dispersal is given further credence by the discovery of Phoebastria anglica (Lydekker), a fossil albatross, in the Pliocene crags of East Anglia.	Coventry Univ, Dept Geog, Coventry CV1 5FB, W Midlands, England	Coventry University	Wood, AM (通讯作者)，Coventry Univ, Dept Geog, Priory St, Coventry CV1 5FB, W Midlands, England.	a.wood@coventry.ac.uk						[Anonymous], 1878, T ZOOLOGICAL SOC LON; [Anonymous], 1996, P ODP SCI RESULTS; [Anonymous], DAWN QUATERNARY; Baird W., 1850, Annals and Magazine of Natural History, V10, P56; BALSON P, 1999, GEOLOGICAL CONSERVAT, V15, P291; Balson P.S., 1993, Proceedings of the Geologists' Association, V104, P59, DOI DOI 10.1016/S0016-7878(08)80155-1; Bartoli G, 2005, EARTH PLANET SC LETT, V237, P33, DOI 10.1016/j.epsl.2005.06.020; BECK RB, 1972, GEOL MAG, V109, P137, DOI 10.1017/S0016756800039522; BEETS CJ, 1992, CALIBRATION CENOZOIC; BENSON R.H., 1972, SMITHSONIAN CONTRIBU, V12; Benton M. 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Res.	DEC	2009	13	4					345	366		10.2517/1342-8144-13.4.345	http://dx.doi.org/10.2517/1342-8144-13.4.345			22	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	542SG					2025-03-11	WOS:000273514800005
J	Kawami, H; van Wezel, R; Koeman, RP; Matsuoka, K				Kawami, Hisae; van Wezel, Rene; Koeman, Reinoud P. T.; Matsuoka, Kazumi			<i>Protoperidinium tricingulatum</i> sp nov (Dinophyceae), a new motile form of a round, brown, and spiny dinoflagellate cyst	PHYCOLOGICAL RESEARCH			English	Article						cyst; Echinidinium; heterotrophic dinoflagellate; Islandinium; Protoperidinium tricingulatum sp; nov	SURFACE SEDIMENTS; ULTRASTRUCTURE; PERIDINIALES; PRODUCTIVITY; INDICATORS; OCEAN; GULF	P>A small, broadly ovoidal and heterotrophic dinoflagellate containing round, brownish, and spiny cyst was found in the water column of Huibertsplaat in the Wadden Sea off the coast of the Netherlands. This dinoflagellate had these conspicuous morphological characters: a five-sided first apical plate (1'), only three cingular plates, and an extremely small first antapical plate. Based on these morphological features, Protoperidinium tricingulatum Kawami, vanWezel, Koeman et Matsuoka is described as a new species. The flagellar pore of P. tricingulatum is covered with a small fin, which rises from the left side of the right sulcal plate to the large V-shaped posterior sulcal plate. This feature suggests that P. tricingulatum is assigned to the Abe's Monovela Group. The cyst stage of P. tricingulatum was positively linked to the vegetative stage by comparison of the ribosomal 5.8S rDNA, internal transcribed spacers (ITS1 and ITS2). Living cysts of P. tricingulatum are round, brownish, and covered with many slender spines bearing capitate or cauliforate distal ends. The cyst also possesses a theropylic archeopyle formed by a slit corresponding to parasutures between three apical and two apical intercaraly plates. These morphological characters indicate that this species is morphologically related to two dinoflagellate cyst-genera Islandinium and Echinidinium.	[Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Kawami, Hisae] Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan; [van Wezel, Rene; Koeman, Reinoud P. T.] Ecol Res & Consultancy, Koeman & Bijkerk Bv, Haren, Netherlands	Nagasaki University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp			Science of Japan Society for the Promotion of Science [18340166]; Grants-in-Aid for Scientific Research [18340166] Funding Source: KAKEN	Science of Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	Samples were taken during the research project Framework of Water Monitoring funded by the Dutch Directorate-General for Public Works and Water Management. The authors thank Bert Wetsteyn for permission to use the data. We also thank Dr L. M. Liao for constructive comments on the manuscript. This work was partly supported by a Grant-in-Aid for the Science of Japan Society for the Promotion of Science (Re: 18340166).	Abe T. 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Res.	DEC	2009	57	4					259	267		10.1111/j.1440-1835.2009.00545.x	http://dx.doi.org/10.1111/j.1440-1835.2009.00545.x			9	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	529QW					2025-03-11	WOS:000272533300002
J	Leroy, SAG; Boyraz, S; Gürbüz, A				Leroy, Suzanne A. G.; Boyraz, Sonay; Gurbuz, Alper			High-resolution palynological analysis in Lake Sapanca as a tool to detect recent earthquakes on the North Anatolian Fault	QUATERNARY SCIENCE REVIEWS			English	Article							1999 IZMIT EARTHQUAKE; NW TURKEY; DINOFLAGELLATE CYSTS; BRITISH-COLUMBIA; MUDURNU VALLEY; WATER-QUALITY; POLLEN DATA; SEDIMENTS; KOCAELI; SEA	High-resolution palynological analysis of a 38-cm long core collected from Lake Sapanca, northwest Turkey, reveals large earthquakes that occurred during the second half of the 20th century along the North Anatolian Fault Zone. Four events have disturbed the lacustrine sedimentary sequence. Three of the four events are historical earthquakes in 1999 in Izmit, 1967 in Mudurnu and 1957 in Abant. These events are recorded in the core by turbiditic deposits and reworked sediment and by low overall palynomorph concentrations but high values of thick-exined pollen, fern spores and fungal spores. Palynomorphs in the event beds have been grouped based on their associations in modern moss, river and lake samples. The inferred mechanisms of transport and sources for the palynomorphs are: 1- lake sediment displaced by slump, 2- collapsed shoreline sediment owing to seiche, waves and sudden lake level changes, 3- subsidence of deltas and 4- river-transported soil and sediment from upland areas. The 1999 Izmit earthquake is only weakly recorded by palynomorphs, probably due to recent engineering control on the rivers. The 1967 Mudurnu earthquake had the strongest effect on the lake, introducing successive packages of sediment to the centre of the lake from underwater slopes, the lakeshore and rivers. (C) 2009 Elsevier Ltd. All rights reserved.	[Leroy, Suzanne A. G.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, West London, England; [Boyraz, Sonay; Gurbuz, Alper] Ankara Univ, Muhendisl Fak, Jeol Muhendisligi Bolumu, TR-06100 Ankara, Turkey	Brunel University; Ankara University	Leroy, SAG (通讯作者)，Brunel Univ, Inst Environm, Uxbridge UB8 3PH, West London, England.	suzanne.leroy@brunel.ac.uk	Leroy, Suzanne/D-3996-2009	GURBUZ, ALPER/0000-0002-8448-9629	European Union [EVG1-CT-2002-00069]; IGCP [490]; ICSU Dark Nature; INQUA TERPRO	European Union(European Union (EU)); IGCP; ICSU Dark Nature; INQUA TERPRO	We are grateful to Fatih Uysal (Ankara University) and Sebastien Bertrand (Brunel University) for help in collecting the modern samples and for providing the data on the region. We collected the short cores with the support M. Albay of the Faculty of Fisheries of Istanbul University. The core chronology is based on data from E. McGee (University College Dublin, Ireland) and was established with the help of P. Werner and M. Schwab (Brunel University). Multiproxy analysis of the Kayak cores was done by a group of researchers and students from Brunel University. The study was funded by the European Union as part of the EC Project RELIEF (EVG1-CT-2002-00069). M. Turner (Brunel University), John Clague (Simon Fraser University) and Oliver Korup (Swiss Federal Research Institutes) helped improved the English of the manuscript. This paper is a contribution to IGCP Project 490, the ICSU Dark Nature project and the INQUA TERPRO Commission.	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J	Marino, G; Rohling, EJ; Sangiorgi, F; Hayes, A; Casford, JL; Lotter, AF; Kucera, M; Brinkhuis, H				Marino, Gianluca; Rohling, Eelco J.; Sangiorgi, Francesca; Hayes, Angela; Casford, James L.; Lotter, Andre F.; Kucera, Michal; Brinkhuis, Henk			Early and middle Holocene in the Aegean Sea: interplay between high and low latitude climate variability	QUATERNARY SCIENCE REVIEWS			English	Review							LAST GLACIAL MAXIMUM; DINOFLAGELLATE CYST ASSEMBLAGES; EASTERN MEDITERRANEAN SAPROPEL; GREENLAND ICE CORES; HIGH-RESOLUTION RECORD; WEST-AFRICAN MONSOON; NORTH-ATLANTIC; SOREQ CAVE; INDIAN MONSOON; OXYGEN-ISOTOPE	Changes in the orbital parameters, solar output, and ocean circulation are widely considered as main drivers of the Holocene climate. Yet, the interaction between these forcings and the role that they play to produce the pattern of changes observed in different domains of the climate system remain debated. Here, we present new early to middle Holocene season-specific sea surface temperature (SST) and delta(18)O(seawater) results, based on organic-walled dinoflagellate cyst and planktonic foraminiferal data from two sediment cores located in the central (SL21) and south-eastern (LC21) Aegean Sea (eastern Mediterranean). Today, this region is affected by high to mid latitude climate in winter and tropical/subtropical climate in summer. The reconstructed delta(18)O(seawater) from LC21 displays a marked (similar to 1.3%) negative shift between 10.7 and 9.7 ka BP, which represents the regional expression of the orbitally driven African monsoon intensification and attendant freshwater flooding into the eastern Mediterranean. A virtually contemporaneous shift, of the same sign and magnitude, is apparent in the delta(18)O(speleothem) record from Soreq Cave (Northern Israel), an important part of which may therefore reflect a change in the isotopic composition of the moisture source region (Aegean and Levantine Seas). Our SST reconstructions show that Aegean winter SSTs decreased in concert with intensifications of the Siberian High, as reflected in the GISP2 nss [K(+)] record. Specifically, three distinct sea surface cooling events at 10.5, 9.5-9.03 and 8.8-7.8 ka BP in the central Aegean Sea match increases in GISP2 nss [K(+)]. These events also coincide with dry interludes in Indian monsoon, hinting at large (hemispheric) scale teleconnections (luring the early Holocene on centennial timescales. A prominent short-lived (similar to 150 years) cooling event in core SL21 - centred on 8.2 ka BP - is coeval to the '8.2 ka BP event' in the Greenland delta(18)O(ice), which is commonly linked to a melt-water related perturbation of the Atlantic Meridional Overturning Circulation and associated ocean heat transport. By deciphering the phasing between a recently published record of reduced overflow from the Nordic Seas into the northern North Atlantic, the Greenland delta(18)O(ice) '8.2 ka BP event' anomaly, and the short-lived cooling in SL21, we demonstrate severe far-field impacts of this North Atlantic event in the Aegean Sea. The Aegean is isolated from the North Atlantic oceanic circulation, so that signal transmission must have been of an atmospheric nature. (C) 2009 Elsevier Ltd. All rights reserved.	[Marino, Gianluca; Sangiorgi, Francesca; Lotter, Andre F.; Brinkhuis, Henk] Univ Utrecht, Fac Sci, Inst Environm Biol, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Marino, Gianluca] CNR, Inst Coastal Marine Environm IAMC, I-80133 Naples, Italy; [Rohling, Eelco J.] Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England; [Hayes, Angela] Univ Limerick, Mary Immaculate Coll, Dept Geog, Limerick, Ireland; [Casford, James L.] Univ Durham, Durham, England; [Kucera, Michal] Univ Tubingen, Inst Geowissensch, DE-72076 Tubingen, Germany	Utrecht University; Consiglio Nazionale delle Ricerche (CNR); L'Istituto per l'Ambiente Marino Costiero (IAMC-CNR); NERC National Oceanography Centre; University of Limerick; Mary Immaculate College - University Limerick; Durham University; Eberhard Karls University of Tubingen	Marino, G (通讯作者)，Univ Autonoma Barcelona, ICTA, Edifici Cn,Campus UAB, Bellaterra 08193, Cerdanyola Vall, Spain.	gianluca.marino@uab.cat	Brinkhuis, Henk/B-4223-2009; Casford, James/A-6984-2008; Marino, Gianluca/AAN-3969-2020; Kucera, Michal/B-9277-2009; rohling, eelco/B-9736-2008; Lotter, Andre F./C-3477-2008	Kucera, Michal/0000-0002-7817-9018; Marino, Gianluca/0000-0001-9795-5337; Casford, James/0000-0001-6789-4932; Brinkhuis, Henk/0000-0003-0253-6610; rohling, eelco/0000-0001-5349-2158; Lotter, Andre F./0000-0002-2954-8809; Sangiorgi, Francesca/0000-0003-4233-6154	Department of Biology, Utrecht University; Institute for Coastal Marine Environment, National Research Council (IAMC-CNR) in Naples, Italy; NERC [NER/B/S/2002/00268, NER/T/S/2002/00453, NE/D001846/1]; NERC [NE/E015905/1, bosc01001, NE/D001846/1] Funding Source: UKRI	Department of Biology, Utrecht University; Institute for Coastal Marine Environment, National Research Council (IAMC-CNR) in Naples, Italy; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC)); NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	G.M. was supported by the Department of Biology, Utrecht University and Institute for Coastal Marine Environment, National Research Council (IAMC-CNR) in Naples, Italy. E.J.R. acknowledges financial support from NERC projects NER/B/S/2002/00268, NER/T/S/2002/00453, and NE/D001846/1. Sune Rasmussen provided correlation points to transfer the GISP2 records on the GICC05 timescale. Kikki Kleiven and Dominik Fleitmann have made available to us their data for core MD03-2665 and Qunf Cave, respectively Suggestions by Hans Renssen, Walter Finsinger, Oliver Heiri, Bruno D'Argenio, and by three anonymous reviewers were critical for the improvement of the manuscript. We kindly thank Natasja Welters for technical support during palynological processing. This study contributes to the Marine Science and Engineering Doctorate, Federico II University, Naples, Italy.	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Sci. Rev.	DEC	2009	28	27-28					3246	3262		10.1016/j.quascirev.2009.08.011	http://dx.doi.org/10.1016/j.quascirev.2009.08.011			17	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	538PF					2025-03-11	WOS:000273195700016
J	Londeix, L; Herreyre, Y; Turon, JL; Fletcher, W				Londeix, Laurent; Herreyre, Yannick; Turon, Jean-Louis; Fletcher, William			Last Glacial to Holocene hydrology of the Marmara Sea inferred from a dinoflagellate cyst record	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Review						organic-walled dinoflagellate cysts; late Quaternary; palaeohydrology; Marmara Sea; Black Sea connection; Fennoscandian Ice Sheet deglaciation; M1 sapropel; Heinrich Event 1.	NORTHERN NORTH-ATLANTIC; LATE QUATERNARY CORES; BLACK-SEA; ICE-SHEET; SURFACE SEDIMENTS; OXYGEN-ISOTOPE; AEGEAN SEA; POSTGLACIAL TRANSGRESSION; HYDROGRAPHIC CONDITIONS; BENTHIC FORAMINIFERA	The history of the connection between the Mediterranean and Black seas since the Last Glacial Maximum (LGM) is documented through the study of an organic-walled dinoflagellate cysts (dinocysts) record at high temporal resolution from the Marmara Sea (MD01-2430 core). Late Glacial dinocyst assemblages indicate that the Marmara Sea was a mildly brackish (caspibrackish) lake with mean annual sea-surface salinities (SSS) around 7-14 psu which probably experienced low seasonal contrasts in SSS; winter and summer sea-surface temperature (SST) were probably around 3-5 and 10-13 degrees C, respectively. This climatic and hydrological context remained effectively unchanged up to 20.5 cal. ka BP. Prior to the end of the LGM, a clear warming preceding a strong meltwater influx has been observed for the first time in the Marmara Sea as early as similar to 20.5 cal. ka BP. The meltwater episode presents a two-step history: 1) a weak phase (similar to 20.0 to 18.1 cal. ka BP) which corresponds to a possible melting of hinterland permafrost; and 2) a strong phase with important meltwater inflow originating from melting of the Fennoscandian Ice Sheet and arriving via the Black Sea. Occuring from similar to 18.1 to 15.9 cal. ka BP, the second phase implies that Black Sea sea-level temporarily exceeded the Bosphorus sill at that time (ca Heinrich Event 1). The introduction of meltwater into the Marmara Sea caused very high seasonal contrasts in Marmara Sea surface-water salinity and temperature. During the Bolling/Allerod, the Marmara Sea was again a caspibrackish lake experiencing relatively cold conditions (with low seasonal contrast in SST) and enhanced moisture as recorded on the continent. Inflowing Mediterranean waters filled the Marmara Sea bottom-waters ca 12.2 cal. ka BP (approximatively the beginning of the Younger Dryas), then reached the sea-surface at similar to 11.7 cal. ka BP. Younger Dryas SSTs were colder than during the Bolling/Allerod, with a likely enhancement of seasonal SST contrasts. At the beginning of the Holocene, SSTs may have been slightly cooler than today, with minimum SSS ranging from 13 to 17.5 psu (maximum 27 psu) and likely with high seasonality in both SST and SSS (possibly up to 19 degrees C and 17 psu). During the deposition of the Holocene sapropel M1, the Marmara Sea experienced enhanced primary productivity and dysoxic/anoxic conditions in the benthic zone. Dinocyst assemblages from the M1 time interval do not provide evidence of an enhanced outflow from the Black Sea. Following the connection of the Mediterranean to the Black Sea (similar to 9 cal. ka BP), several distinct climatic and hydrological phases occurred, including a short cooling (similar to 7.5 to 5.8 cal. ka BP; possibly linked to a strengthening of the Siberian High [Kotthoff, U., Pross,J., Muller, U.C., Peyron, C., Schmiedl, G., Schulz, H., Bordon, A., 2008. Climate dynamics in the borderlands of the Aegean Sea during formation of sapropel S1 deduced from a marine pollen record. Quaternary Science Reviews, 27: 832-845.]), a thermal optimum (similar to 5.8 to 4.7 cal. ka BP), and the installation of the modern hydrological system (similar to 4.7 cal. ka BP). The timing of this sequence appears close to that recorded in the Black Sea, supporting the idea that the two basins would have operated in tandem. (C) 2009 Elsevier B.V. All rights reserved.	[Londeix, Laurent; Herreyre, Yannick; Turon, Jean-Louis; Fletcher, William] Univ Bordeaux 1, CNRS, UMR 5805, EPOC, F-33405 Talence, France; [Fletcher, William] Goethe Univ Frankfurt, Inst Geowissensch, Frankfurt, Germany	Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Goethe University Frankfurt	Londeix, L (通讯作者)，Univ Bordeaux 1, CNRS, UMR 5805, EPOC, Ave Fac, F-33405 Talence, France.	l.londeix@epoc.u-bordeaux1.fr		Fletcher, William/0000-0001-8918-0690				Aksu AE, 1999, MAR GEOL, V153, P275, DOI 10.1016/S0025-3227(98)00078-4; Aksu AE, 2002, MAR GEOL, V190, P61, DOI 10.1016/S0025-3227(02)00343-2; 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, 2002, GSA TODAY        MAY, P4; ALAVI SN, 1988, MAR MICROPALEONTOL, V13, P213, DOI 10.1016/0377-8398(88)90004-7; Alley RB, 2005, QUATERNARY SCI REV, V24, P1123, DOI 10.1016/j.quascirev.2004.12.004; 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Palynology	DEC	2009	158	1-2					52	71		10.1016/j.revpalbo.2009.07.004	http://dx.doi.org/10.1016/j.revpalbo.2009.07.004			20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	536SS					2025-03-11	WOS:000273064700005
J	Rossi, M; Mosca, P; Polino, R; Rogledi, S; Biffi, U				Rossi, Massimo; Mosca, Pietro; Polino, Riccardo; Rogledi, Sergio; Biffi, Ulderico			NEW OUTCROP AND SUBSURFACE DATA IN THE TERTIARY PIEDMONT BASIN (NW-ITALY): UNCONFORMITY-BOUNDED STRATIGRAPHIC UNITS AND THEIR RELATIONSHIPS WITH BASIN-MODIFICATION PHASES	RIVISTA ITALIANA DI PALEONTOLOGIA E STRATIGRAFIA			English	Article						Alps-Apennines junction; seismic stratigraphy; sequence stratigraphy; field geology; palynology	DINOFLAGELLATE CYSTS; CASTAGNOLA FM.; SOUTHERN ALPS; MIOCENE; PLIOCENE; COMPLEX; RECORD	This paper deals with the regional stratigraphy around the Alps-Apennines junction during late Eocene-Mioccne. The basin-fill architecture and its relation to changes in structural style were deciphered through the integration of subsurface and outcrop data on the basis of seismic- and sequence-stratigraphy principles, respectively. During late Eocene-Oligocene, the study area hosted a mosaic of partially interconnected sub-basins, and the Torino Hill area marked the junction towards the western apex of the Southern Alps foredeep (Gonfolite Basin). Since the latest Oligocene, the uplift of the north-verging Monferrato arc provided the separation from the adjacent Gonfolite Basin and the Tertiary Piedmont Basin behaved as a larger and more regularly subsiding thrust-top basin. The upper Eocene-Miocene successions record a long-term, major transgressive-regressive cycle, consisting of seven large-scale unconformity-bounded stratigraphic units, whose stacking pattern was controlled by changes in the rate of tectonic subsidence and whose boundaries were generated by basin-modification phases. During the Oligocene-lower Miocene deepening-upward sequence set, the marginal marine systems show a marked diachronism associated with the SW-ward change of coastal onlap, punctuated by drowning-platform unconformities generated in relation to basinward tilting and high-angle syn-sedimentary faults. The maximum transgression coincides with the late Burdigalian tectonic space creation phase, when a basinwide, highly efficient turbidite system was deposited. The middle-upper Miocene progradation, punctuated by forced regression pulses, was driven by the inversion and uplift of the southern basin margin, so that a northward shift and progressive narrowing of the turbidite depocentre occurred.	[Rossi, Massimo; Biffi, Ulderico] Eni E&P Div, Geosci Tech Serv, I-20097 San Donato Milanese, MI, Italy; [Mosca, Pietro; Polino, Riccardo] CNR, Inst Geosci & Earth Resources, I-10125 Turin, Italy; [Rogledi, Sergio] Eni E&P Div, So Europe Explorat, I-20097 San Donato Milanese, MI, Italy	Eni SpA; Consiglio Nazionale delle Ricerche (CNR); Istituto di Geoscienze e Georisorse (IGG-CNR); Eni SpA	Rossi, M (通讯作者)，Eni E&P Div, Geosci Tech Serv, Via Emilia 1, I-20097 San Donato Milanese, MI, Italy.	massimo.rossi@eni.it; p.mosca@csg.to.cnr.it; polinori@gmail.com; sergio.rogledi@eni.it; ulderico.biffi@eni.it		MOSCA, PIETRO/0000-0002-7517-5353; rossi, massimo/0000-0002-0342-8120				[Anonymous], 1964, ATTI ACCADEMIA LINCE; Barbieri C, 2003, INT J EARTH SCI, V92, P758, DOI 10.1007/s00531-003-0351-x; Baruffini L., 1994, SUBMAR FANS TURBID S, P9; Bersezio R., 2005, GEOACTA-BOLOGNA, V4, P83; Bicchi Erica, 2006, Bollettino della Societa Paleontologica Italiana, V45, P171; BIFFI U, 1988, Bollettino della Societa Paleontologica Italiana, V27, P163; BIFFI U, 1995, PROGETTO RICERCA DES; Brinkhuis H., 1992, Neogene and Quaternary Dinoflagellate Cysts and Acritarchs, P219; Bukry D., 1975, Initial Rep Deep Sea Drilling Project, V32, P677, DOI 10.2973/dsdp.proc.32.124.1975; Bukry D., 1973, Initial Reports DSDP, V15, P685, DOI DOI 10.2973/DSDP.PROC.15.116.1973; Carrapa B, 2001, SEDIMENT GEOL, V139, P217, DOI 10.1016/S0037-0738(00)00167-6; CAVANNA E, 1989, ATTI TIC SCI TERRA, V32; Cazzola C., 1992, Atti Tic.Sc.Terra, V33, P177; CAZZOLA C, 1985, SUBMARINE FANS RELAT, P179; Cazzola C., 1981, 2 IAS REG M, P8; CITA MB, 1960, REND SCI FIS MAT NAT, V29, P360; CLARI P, 1995, TERRA NOVA, V7, P144, DOI 10.1111/j.1365-3121.1995.tb00683.x; Corradini D., 1988, Bulletin du Centre de Recherches Exploration-Production Elf-Aquitaine, V12, P221; D'Atri A., 1990, MEM SOC GEOL ITAL, V45, P723; Dalla Stefano, 1993, Paleontologia i Evolucio, V24-25, P341; DATRI A, 1995, B MUS REG SCI NAT TO, V13, P345; Dela Pierre F, 2002, SEDIMENT GEOL, V152, P289, DOI 10.1016/S0037-0738(02)00097-0; DELAPIERRE F, 2002, SISTEMA ALPINO APPEN, P116; deVerteuil L, 1996, MICROPALEONTOLOGY, V42, P1; Di Giulio A., 1991, Atti Tic. 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DEC	2009	115	3					305	335		10.13130/2039-4942/6386	http://dx.doi.org/10.13130/2039-4942/6386			31	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	539BE					2025-03-11	WOS:000273227600003
J	Náñez, C; Quattrocchio, ME; Ruiz, L				Nanez, Carolina; Quattrocchio, Mirta E.; Ruiz, Liliana			PALYNOLOGY AND MICROPALEONTOLOGY OF THE SAN JULIAN AND MONTE LEON FORMATIONS (OLIGOCENE - EARLY MIOCENE), CABO CURIOSO SUBSURFACE, SANTA CRUZ PROVINCE, ARGENTINA	AMEGHINIANA			Spanish	Article						Palynomorphs; Foraminifera; San Julian Formation; Monte Leon Formation; Oligocene-early Miocene; Austral Basin; Argentina	PALEOGENE-EARLY NEOGENE; PATAGONIA; FORAMINIFERA; EVOLUTION; HISTORY	PALYNOLOGY AND MICROPALEONTOLOGY OF THE SAN JULIAN AND MONTE LEON FORMATIONS (OLIGOCENE - EARLY MIOCENE), CABO CURIOS SUBSURFACE, SANTA CRUZ PROVINCE, ARGENTINA. The CC-3 and CC-4 boreholes drilled a Cenozoic sedimentary column integrated by the Monte Le On and San Julian formations, similar to that cropping out in the Gran Bajo de San Julian. The palynology and micropaleontology of both boreholes are analyzed, particularly focused on the "basal muddy section" of the San Julian Formation. The palynomorphs of this section are of continental origin, reflecting a regional forest dominated by Nothofagaceae, Myrtaceae, Podocarpaceae and Palmae, developed under a temperate to warm-temperate and humid climate. The palynomorphs from the carbonaceous claystones of the upper part of this section, dominated by Poaceae, some Podocarpaceae and the presence of fresh-water algae, mainly reflect the local vegetation associated with fresh to brackish-water swamps. The foraminifera, recovered from only two horizons from the middle part of the "basal muddy section", scarce and poorly preserved, suggest a marginal marine paleoenvironment, and resemble those described from the Gran Bajo Member of the San Julian Formation; the occurrence of Boltovskoyella patagonica Malumian and Masiuk, suggests affinity with the assemblage of the late middle Eocene Man Aike Formation as well, but specimens are rare and tentatively identified. An Oligocene age and a paralic paleoenvironment is estimated for the "basal muddy section" in the CC-3 and CC-4 boreholes. The upper section of the San Julian Formation (late Oligocene) yielded an inner shelf foraminiferal assemblage, similar to that described for the Meseta Chica Member of this Formation. The foraminiferal assemblage from the base of the overlying Monte Leon Formation (early Miocene), mainly composed of agglutinated species, and the presence of dinoflagellate cysts suggest more open marine conditions, probably a middle to outer shelf setting, reflecting the transgressive character of this Formation. The abrupt change and dissimilitude between the foraminiferal assemblages of the San Julian and Monte Leon formations suggest an unconformable relationship between these two units.	[Nanez, Carolina] Serv Geol Minero Argentino, RA-1107 Buenos Aires, DF, Argentina; [Nanez, Carolina; Quattrocchio, Mirta E.] Consejo Nacl Invest Cient & Tecn, Buenos Aires, DF, Argentina; [Quattrocchio, Mirta E.; Ruiz, Liliana] Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Náñez, C (通讯作者)，Serv Geol Minero Argentino, Benjamin Lavaisse 1194, RA-1107 Buenos Aires, DF, Argentina.	carolina.nanez@yahoo.com; mquattro@criba.edu.ar	Ruiz, Liliana/GVT-1079-2022					[Anonymous], 1938, Boletin de Informaciones Petroleras; ARCHANGELSKY S, 1973, Ameghiniana, V10, P339; ARCHANGELSKY S, 1976, Ameghiniana, V13, P169; ARCHANGELSKY S, 1974, Ameghiniana, V11, P217; Archangelsky S., 1986, Ameghiniana, V23, P35; Archangelsky S., 1972, Revista del Museo de la Plata, seccion Paleontologia, P65; ASENSIO M, 2005, 16 C GEOL ARG SAN SA, V3, P271; BAEZ A M, 1990, Ameghiniana, V27, P83; Barreda V, 2000, AMEGHINIANA, V37, P103; Barreda V, 2000, AMEGHINIANA, V37, P3; BARREDA VD, 2004, 7 INT ORG PAL C; BARREDA VD, 2002, REL 15 C GEOL ARG CA, V2, P545; Barreda V, 2007, BOT REV, V73, P31, DOI 10.1663/0006-8101(2007)73[31:PVTDTP]2.0.CO;2; Barreda V, 2009, REV PALAEOBOT PALYNO, V154, P22, DOI 10.1016/j.revpalbo.2008.11.005; Barreda Viviana D., 1997, Ameghiniana, V34, P283; Barreda Viviana D., 1996, Ameghiniana, V33, P35; BARTELS A, 1996, GEOLOGIC AFRIQUE ATL, P351; BARTELS A, 1979, AMEGHINIANA, V14, P233; Becker D, 1964, AMEGHINIANA, V3, P319; Bertels A., 1975, Revista Esp Micropaleont, V7, P429; Bertels A., 1970, Revta Asoc. geol. argent., V25, P495; Bertels A., 1980, 2 C ARG PAL BIOESTR, V2, P213; Blow W.H., 1979, CAINOZOIC GLOBIGERIN; Boltovskoy E., 1976, Foraminifera, V2, P171; Cabrera AL., 1976, ENCICLOPEDIA ARGENTI, V2nd, P1; CABRERA OR, 1982, EXPLORACION CARBOMFE; Caramés A, 2004, AMEGHINIANA, V41, P461; CARAMES A, 2000, SUBSECRETARIA MINERI, V33, P33; Carrizo R., 1990, 2 S TERC CHIL ACT, V1, P29; Casadío S, 2001, AMEGHINIANA, V38, P321; Cesari S.N., 2006, 9 C PAL BIOESTR CORD, P34; Codignotto J.O., 1981, Rev. 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J	Beard, KC; Dawson, MR				Beard, K. Christopher; Dawson, Mary R.			EARLY WASATCHIAN MAMMALS OF THE RED HOT LOCAL FAUNA, UPPERMOST TUSCAHOMA FORMATION, LAUDERDALE COUNTY, MISSISSIPPI	ANNALS OF CARNEGIE MUSEUM			English	Review						biostratigraphy; Eocene; mammals; paleobiogeography; Paleocene; Wasatchian	PALEOCENE-EOCENE BOUNDARY; EARLIEST EOCENE; BIGHORN BASIN; LAND MAMMALS; CARBON; DISPERSAL; PANTOLESTIDAE; INSECTIVORA; TRANSITION; LIPOTYPHLA	Fossil mammals comprising the early (and perhaps earliest) Wasatchian Red Hot local fauna from the Gulf Coastal Plain of Mississippi are described. As currently understood, the fauna consists of 33 species of mammals, including the following new taxa: Mimoperadectes sowasheensis, new species, Apatemys pygmaeus, new species; Palaeosinopa aestuarium, new species; Naranius americanus, new species; Colpocherus mississippiensis, new genus and species; Diacocherus dockeryi, new species; Wyonycteris primitivus, new species; Choctawius foxi, new genus and species; Haplomylus meridionalis, new species; Ectocion nanabeensis, new species; Miacis igniculus, new species; Eogale parydros, new genus and species; Viverriscus omnivorus, new genus and species; Paramys dispar, new species; Corbarimys? nomadus, new species; and Franimys? actites, new species. New combinations proposed here include Plagioctenodon dormaalensis (Quinet, 1964), Plagioctenodon rosei (Gingerich, 1987), Choctawius mckennai (Szalay, 1969), and Paramys wutui (Tong and Dawson, 1995). The Red Hot local fauna derives from an estuarine sand unit that also yields fossil spores, pollen, dinoflagellate cysts, fishes, and snakes. The fauna is taphonomically biased against the preservation of mammals having medium to large body mass. The Red Hot local fauna provides a rare opportunity to gauge the significance of biotic provincialism within North America near the Paleocene-Eocene boundary, a time of dynamic climate change. Faunal endemism with respect to the Rocky Mountain Interior of North America is high at the species level, consistent with evidence for substantive differences in the physical environment and flora. Several lines of evidence, including mammalian biostratigraphy, sequence stratigraphy, and dinoflagellate zonation, suggest that the Red Hot local fauna correlates with earliest Wasatchian (Wa-M) faunas from the Bighorn Basin of Wyoming. Latitudinal shifts in taxon ranges coincident with global warming provide an alternative explanation for seemingly transient episodes of phyletic dwarfing among mammals during the PETM in the Bighorn Basin.	[Beard, K. Christopher; Dawson, Mary R.] Sect Vertebrate Paleontol, Pittsburgh, PA 15213 USA		Beard, KC (通讯作者)，Sect Vertebrate Paleontol, 4400 Forbes Ave, Pittsburgh, PA 15213 USA.	beardc@carnegiemnh.org; dawsonm@carnegiemnh.org	Beard, K./AAQ-4438-2021	Beard, K. Christopher/0000-0002-6279-9837				[Anonymous], 1984, BULL CARNEG MUS NAT; [Anonymous], 1980, MARSUPIAUX TERTIAIRE; [Anonymous], SPECIAL PUBLICATION; BADGLEY C, 1990, GEOL SOC AM SPEC PAP, V243, P153; Beard KC, 2008, P NATL ACAD SCI USA, V105, P3815, DOI 10.1073/pnas.0710180105; Beard K. 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NOV 15	2009	78	3					193	243		10.2992/007.078.0301	http://dx.doi.org/10.2992/007.078.0301			51	Paleontology; Zoology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology; Zoology	531BI					2025-03-11	WOS:000272637300001
J	Kim, SY; Moon, CH; Cho, HJ; Lim, DI				Kim, So-Young; Moon, Chang-Ho; Cho, Hyun-Jin; Lim, Dhong-Il			Dinoflagellate Cysts in Coastal Sediments as Indicators of Eutrophication: A Case of Gwangyang Bay, South Sea of Korea	ESTUARIES AND COASTS			English	Article						Eutrophication; Dinoflagellate cysts; Diatoms; Coastal zone; Gwangyang Bay sediments	CHESAPEAKE BAY; SURFACE SEDIMENTS; GROWTH; PHYTOPLANKTON; PRODUCTIVITY; IRRADIANCE; SILICA	Diatom densities in the surface water and dinoflagellate cysts in bottom sediments of Gwangyang Bay were studied to determine changes in the phytoplankton community structure in response to anthropogenic eutrophication and to assess the use of dinoflagellate cysts as indicators of coastal eutrophication. Our results show that, in nutrient-enriched environments, diatoms are particularly benefited from the nutrients supplied and, as a consequence, heterotrophic dinoflagellates that feed on the diatoms can be more abundant than autotrophic dinoflagellates. In short-core sediment records, a marked shift in autotrophic-heterotrophic dinoflagellate cyst compositions occurred at a depth of approximately 9-10 cm corresponding to the timing of the 1970s industrialization around Gwangyang Bay. This tentatively indicates that diatom and dinoflagellate communities here have undergone a considerable change mainly due to increased nutrient loadings from both domestic sewage effluent and industrial pollution. Our study suggests a possible potential use of dinoflagellate cysts in providing retrospective information on the long-term effects of coastal eutrophication.	[Kim, So-Young; Lim, Dhong-Il] Korea Ocean Res & Dev Inst, Environm Sci Lab, Geoje 656830, Gyeongnam, South Korea; [Moon, Chang-Ho] Pukyong Natl Univ, Dept Oceanog, Pusan 608737, South Korea; [Cho, Hyun-Jin] Mokpo Coast Guard, Pollut Response Dept, Mokpo 530350, Jeollanamdo, South Korea	Korea Institute of Ocean Science & Technology (KIOST); Pukyong National University	Kim, SY (通讯作者)，Korea Ocean Res & Dev Inst, Environm Sci Lab, Geoje 656830, Gyeongnam, South Korea.	kimsy@kordi.re.kr	Kim, So-Young/JFS-7698-2023; Lim, Dhongil/ACH-3964-2022	Lim, Dhongil/0000-0002-0832-2907	Korea Ocean Research and Development Institute [PE98314]	Korea Ocean Research and Development Institute	We thank the anonymous reviewers for their useful suggestions to improve the quality of the manuscript and for correcting the English. This study was supported by the Korea Ocean Research and Development Institute research program under grant no. PE98314.	Andrén E, 1999, ESTUAR COAST SHELF S, V48, P665, DOI 10.1006/ecss.1999.0480; BOYNTON WR, 1995, ESTUARIES, V18, P285, DOI 10.2307/1352640; CHAN AT, 1978, J PHYCOL, V14, P396, DOI 10.1111/j.1529-8817.1978.tb02458.x; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; Colman SM, 2003, GEOLOGY, V31, P71, DOI 10.1130/0091-7613(2003)031<0071:AICISA>2.0.CO;2; CONLEY DJ, 1993, MAR ECOL PROG SER, V101, P179, DOI 10.3354/meps101179; DALE B., 1994, CARBON CYCLING GLOBA, P521; Dale B, 2009, J SEA RES, V61, P103, DOI 10.1016/j.seares.2008.06.007; Diaz RJ, 2001, J ENVIRON QUAL, V30, P275, DOI 10.2134/jeq2001.302275x; FALKOWSKI PG, 1985, LIMNOL OCEANOGR, V30, P311, DOI 10.4319/lo.1985.30.2.0311; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; *HYDR OFF KOR, 1986, 256 HYDR OFF KOR; Hyun S., 2003, Sea: J. Korea Soc. Oceanography, V8, P380; *KOR OC RES DEV I, 2003, 3080015384 BSPS KOR; LANGDON C, 1987, J PLANKTON RES, V9, P459, DOI 10.1093/plankt/9.3.459; LEE JB, 1991, J OCEANOLOGICAL SOC, V4, P304; LEE YS, 2007, J KOREAN SOC OCEANOG, V12, P1; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; Malone TC, 1996, ESTUARIES, V19, P371, DOI 10.2307/1352457; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Shim J.H., 1984, Journal of the Oceanological Society of Korea, V19, P172; TANG EPY, 1995, J PLANKTON RES, V17, P1325, DOI 10.1093/plankt/17.6.1325; Taylor F.J.R., 1987, General group characteristics; special features of interest; short history of dinoflagellate study; Tiselius P, 1996, J PLANKTON RES, V18, P133, DOI 10.1093/plankt/18.2.133; TURNER RE, 1994, NATURE, V368, P619, DOI 10.1038/368619a0; Wall D., 1977, MAR MICROPALEONTOL, V30, P319	27	23	25	1	19	SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013 USA	1559-2723	1559-2731		ESTUAR COAST	Estuaries Coasts	NOV	2009	32	6					1225	1233		10.1007/s12237-009-9212-6	http://dx.doi.org/10.1007/s12237-009-9212-6			9	Environmental Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology	514MJ					2025-03-11	WOS:000271398600016
J	Gómez, F; Moreira, D; López-García, P				Gomez, Fernando; Moreira, David; Lopez-Garcia, Purificacion			Life cycle and molecular phylogeny of the dinoflagellates <i>Chytriodinium</i> and <i>Dissodinium</i>, ectoparasites of copepod eggs	EUROPEAN JOURNAL OF PROTISTOLOGY			English	Article						Alveolata; Blastodiniales; Gymnodinium; Parasitic dinophyceae; SSU rDNA	NOV; ULTRASTRUCTURE; DINOPHYCEAE; REDEFINITION; PSEUDOLUNULA; SEQUENCES; SPEC; GEN	The dinoflagellates Chytriodinium affine, C. roseum and Dissodinium pseudolunula are ectoparasites of crustacean eggs. Here, we present new observations regarding their life cycle based on coastal plankton samples and incubations and analyze their molecular phylogeny using the small subunit ribosomal RNA gene (SSU rDNA) as a marker. In contrast to the typical stages already documented for its life cycle, we observed that D. pseudolunula dinospores may exceptionally differentiate inside a globular cyst. Despite its parasitic life style, the cysts and dinospores of D. pseudolunula contain chlorophyll a. We obtained the first SSU rDNA sequences for the genera Chytriodinium (the type C roseum and C affine) and Dissodinium (D. pseudolunula). Classical taxonomical schemes have ascribed these genera to the order Blastodiniales. However, our SSU rDNA-based phylogenetic analysis shows that these ectoparasites form a clade in the Gymnodinium sensu stricto group, unarmored dinokaryotic dinoflagellates of the order Gymnodiniales. They branch in a subgroup composed of warnowiids, polykrikoids, the type of Gymnodinium, G. fuscum and G. aureolum. Although Chytriodinium and Dissodinium appear to be relatives based on SSU rDNA phylogeny, feeding and host specificity, their life cycles are substantially different. Based on these data we consider that the type of life cycle is a poor criterion for classification at the family level. We suggest that the morphology of the infective cell is probably the most reliable phenotypic characteristic to determine the systematic position of parasitic dinoflagellates. (C) 2009 Elsevier GmbH. All rights reserved.	[Gomez, Fernando] Univ Paris 06, CNRS, INSU UMR 7621, Observ Oceanol Banyuls Mer, F-66651 Banyuls Sur Mer, France; [Moreira, David; Lopez-Garcia, Purificacion] Univ Paris 11, CNRS, UMR 8079, Unite Ecol Systemat & Evolut, F-91405 Orsay, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - Institute of Ecology & Environment (INEE); Universite Paris Saclay; AgroParisTech	Gómez, F (通讯作者)，Univ Paris 06, CNRS, INSU UMR 7621, Observ Oceanol Banyuls Mer, Ave Fontaule,BP 44, F-66651 Banyuls Sur Mer, France.	fernando.gomez@fitoplancton.com	Moreira, David/F-7445-2012; Gomez, Fernando/B-2495-2009; Lopez-Garcia, Purificacion/B-6775-2012	Gomez, Fernando/0000-0002-5886-3488; Lopez-Garcia, Purificacion/0000-0002-0927-0651	Ministerio Espanol de Educacion y Ciencia [2007-0213]; French CNRS; ANR	Ministerio Espanol de Educacion y Ciencia(Spanish Government); French CNRS(Centre National de la Recherche Scientifique (CNRS)); ANR(Agence Nationale de la Recherche (ANR))	This is a contribution to the project DIVERPLANMED supported by a post-doctoral grant to F.G. of the Ministerio Espanol de Educacion y Ciencia #2007-0213. P.L.G. and D.M. acknowledge financial support from the French CNRS and the ANR Biodiversity project 'Aquaparadox'. We thank I. Salter for assistance with the English edition.	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A., 1993, CLASSIFICATION LIVIN; Georg H., 1858, Mem Inst Natn Genev, DOI 10.5962/bhl.title.29753; Gomez Fernando, 2005, Acta Botanica Croatica, V64, P129; Gómez F, 2009, J EUKARYOT MICROBIOL, V56, P440, DOI 10.1111/j.1550-7408.2009.00420.x; Gonnert R., 1936, Zeitschrift fuer Parasitenkunde, V9, P140, DOI 10.1007/BF02120308; Hansen G, 2001, J PHYCOL, V37, P612, DOI 10.1046/j.1529-8817.2001.037004612.x; Hansen G, 2007, PHYCOL RES, V55, P25, DOI 10.1111/j.1440-1835.2006.00442.x; Hoppenrath M, 2007, PROTIST, V158, P209, DOI 10.1016/j.protis.2006.12.001; Hoppenrath M, 2007, J PHYCOL, V43, P366, DOI 10.1111/j.1529-8817.2007.00319.x; Jobb G, 2004, BMC EVOL BIOL, V4, DOI 10.1186/1471-2148-4-18; Jorgensen MF, 2004, J PHYCOL, V40, P351, DOI 10.1111/j.1529-8817.2004.03131.x; Kim KY, 2008, PHYCOL RES, V56, P89, DOI 10.1111/j.1440-1835.2008.00489.x; Kühn SF, 2005, PROTIST, V156, P393, DOI 10.1016/j.protis.2005.09.002; Lartillot N, 2004, MOL BIOL EVOL, V21, P1095, DOI 10.1093/molbev/msh112; Loeblich III A. R., 1982, Synopsis and Classification of Living Organisms, P101; Mauchline J, 1998, ADV MAR BIOL, V33, P1; PHILIPPE H, 1993, NUCLEIC ACIDS RES, V21, P5264, DOI 10.1093/nar/21.22.5264; SAITOU N, 1987, MOL BIOL EVOL, V4, P406, DOI 10.1093/oxfordjournals.molbev.a040454; Saldarriaga JF, 2001, J MOL EVOL, V53, P204, DOI 10.1007/s002390010210; Skovgaard A, 2007, J PHYCOL, V43, P553, DOI 10.1111/j.1529-8817.2007.00338.x; Stoecker DK, 1999, J EUKARYOT MICROBIOL, V46, P397, DOI 10.1111/j.1550-7408.1999.tb04619.x; TAYLOR FJR, 1987, BIOL DINOFLAGELLATES, P723	38	35	39	1	18	ELSEVIER GMBH	MUNICH	HACKERBRUCKE 6, 80335 MUNICH, GERMANY	0932-4739	1618-0429		EUR J PROTISTOL	Eur. J. Protistol.	NOV	2009	45	4					260	270		10.1016/j.ejop.2009.05.004	http://dx.doi.org/10.1016/j.ejop.2009.05.004			11	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	540YY	19589664				2025-03-11	WOS:000273378700002
J	Rubino, F; Saracino, OD; Moscatello, S; Belmonte, G				Rubino, F.; Saracino, O. D.; Moscatello, S.; Belmonte, G.			An integrated water/sediment approach to study plankton (a case study in the southern Adriatic Sea)	JOURNAL OF MARINE SYSTEMS			English	Article						Resting stages; Cyst bank; Plankton; South Adriatic	VERTICAL-DISTRIBUTION; RESTING EGGS; SEDIMENTS	In marine coastal areas many planktonic species produce resting stages (cysts) that sink to the bottom. Integrated sampling from both the water column (to collect active stages). and sediments (to collect cysts), could be useful to achieve more complete information about plankton composition. In the framework of the "INTERREG II Albania-Italy Project" an oceanographic survey was carried out aboard the r/v "Italica" from 20 to 31 October 2000. The survey interested the northern Albanian coast (Gulf of Drin) and the northern Apulian coast (Gulf of Manfredonia) on the opposite sides of the South Adriatic Sea. The plankton was collected from 14 stations. A total of 188 categories were recognized in plankton samples. Among those categories, 130 species were recognized (87 of phytoplankton, 43 of microzooplankton), and only 53 (40.8%) resulted common to both the Adriatic sides. A total of 69 cyst morphotypes were recognized in sediment samples; 38 of them were classified at the level of species. A statistical analysis of the microzooplankton species abundance showed a segregation of the two areas better than that obtained with the phytoplankton. Cyst distribution in the sediments showed a good gulf-segregation too. In addition, they allowed us to find complementary information, particularly for dinoflagellates. The most abundant species in the water column were not equally dominant as resting stages in the sediments. Sediment sampling allowed further information about the composition of the plankton communities, and suggested us to search for a new method to enhance the yield of less abundant cysts. (C) 2009 Elsevier B.V. All rights reserved.	[Rubino, F.; Saracino, O. D.] Talassograf A Cerruti CNR, Inst Coastal Marine Environm, I-74100 Taranto, Italy; [Moscatello, S.; Belmonte, G.] Univ Salento, Dept Biol & Environm Sci & Technol, I-73100 Lecce, Italy	University of Salento	Rubino, F (通讯作者)，Talassograf A Cerruti CNR, Inst Coastal Marine Environm, Via Roma 3, I-74100 Taranto, Italy.	rubino@iamc.cnr.it	Rubino, Fernando/GOP-0332-2022; BELMONTE, GENUARIO/AAG-4029-2020	Rubino, Fernando/0000-0003-2552-2510				Andersen P., 2003, Manual on harmful marine microalgae. Monographs on oceanographic methodology, P99; Belmonte G., 1999, Biologia Marina Mediterranea, V6, P172; 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; Clarke K R., 1994, An approach to statistical analysis and interpretation; CLARKE KR, 1993, AUST J ECOL, V18, P117, DOI 10.1111/j.1442-9993.1993.tb00438.x; Dale B., 1983, P69; Fonda-Umani S., 1992, Atti V Congresso SITE, P221; Gacic M., 1996, Dynamics of Mediterranean Straits and Channels, P117; GIANGRANDE A, 1994, OCEANOGR MAR BIOL, V32, P305; Giordani P, 2002, J MARINE SYST, V33, P365, DOI 10.1016/S0924-7963(02)00067-2; Krsinic F, 2006, SCI MAR, V70, P77, DOI 10.3989/scimar.2006.70n177; Krsinic F, 1998, J PLANKTON RES, V20, P1033, DOI 10.1093/plankt/20.6.1033; MARCUS NH, 1994, LIMNOL OCEANOGR, V39, P154, DOI 10.4319/lo.1994.39.1.0154; Moscatello S, 2004, SCI MAR, V68, P85, DOI 10.3989/scimar.2004.68s185; ORLIC M, 1992, OCEANOL ACTA, V15, P109; Rubino F, 2000, MAR ECOL-P S Z N I, V21, P263, DOI 10.1046/j.1439-0485.2000.00725.x; Rubino F., 1998, BIOL MAR MEDIT, V5, P253; Rubino F, 2002, MAR ECOL-P S Z N I, V23, P329, DOI 10.1111/j.1439-0485.2002.tb00031.x; Saracino OD, 2006, NOVA HEDWIGIA, V83, P253, DOI 10.1127/0029-5035/2006/0083-0253; Siokou-Frangou I, 2005, CONT SHELF RES, V25, P2597, DOI 10.1016/j.csr.2005.08.024; Stoecker DK, 1996, AQUAT MICROB ECOL, V10, P273, DOI 10.3354/ame010273; VILICIC D, 1995, MAR BIOL, V123, P619, DOI 10.1007/BF00349240; YACOBI YZ, 1995, J MARINE SYST, V6, P179, DOI 10.1016/0924-7963(94)00028-A; Zore-Armanda M., 1968, Stud. Rev. Gen. Fish. Counc. Mediterr, V34, P1	26	21	21	2	13	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	0924-7963			J MARINE SYST	J. Mar. Syst.	NOV	2009	78	4			SI		536	546		10.1016/j.jmarsys.2008.12.023	http://dx.doi.org/10.1016/j.jmarsys.2008.12.023			11	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	522FU					2025-03-11	WOS:000271984100007
J	Zonneveld, KAF; Chen, L; Möbius, J; Mahmoud, MS				Zonneveld, Karin A. F.; Chen, Liang; Moebius, Juergen; Mahmoud, Magdy S.			Environmental significance of dinoflagellate cysts from the proximal part of the Po-river discharge plume (off southern Italy, Eastern Mediterranean)	JOURNAL OF SEA RESEARCH			English	Review						Eastern Mediterranean; Dinoflagellate Cysts; Eutrophication; River Discharge	SEA-SURFACE CONDITIONS; WESTERN ADRIATIC SEA; NORTHERN NORTH-ATLANTIC; IONIAN SEA; RECENT SEDIMENTS; COASTAL WATERS; SPATIAL-DISTRIBUTION; PHYTOPLANKTON BLOOM; SEASONAL OCCURRENCE; PARTICULATE MATTER	To determine the relationship between region specific dinoflagellate cyst distribution in the Po-river discharge area and oceanic environmental conditions, surface sediments of 48 sites in the middle and distal part of the discharge plume area have been studied. Establishing such a relationship is a prerequisite to create reconstructions of the eutrophication history as well as the palaeoclimatic and palaeoceanography history of the area. Literature based information about the sedimentation rates based on Pb-210 dating methods are available for 18 sites. This enables the calculation of cyst accumulation rates of individual cyst species which reflect their cyst production. Correlation of the accumulation rates of individual species with environmental parameters of the upper waters allows us to adapt and refine the ecological characteristics of a selection of cyst species. This latter is trivial since the current concepts on the ecological significance of dinoflagellate cyst have to be revised as a result of the current developments in the dinoflagellate research field. These developments have elucidated that a considerable part of the relative abundance datasets that form the basis for the present day ecological concepts of dinoflagellate cysts might have suffered from so called "closed sum effects" and have been overprinted by early diagenetic processes. The dinoflagellate cyst association reflects both upper and bottom water circulation. Based on the relative abundance data four associations can be distinguished that are characteristic for the major oceanographic settings in the region. (1) River discharge association. This association consists of Echinidinium spp., Lejeunecysta sabrina, Lingulodinium machaerophorum, Polykrikos kofoidii, Polykrikos schwarzii, cysts of Protoperidinium stellatum, Selenopemphix quanta and reworked cysts. These species have high relative abundances in sites where bottom waters are low in oxygen and upper waters are influenced by river discharge waters that are characterized by high productivity and relative low salinity. (2) Warm water association. This association consists of Spiniferites mirabilis, Spiniferites pachydemus, Spiniferites ramosus and Spiniferites spp. which have their highest relative abundances in the sites at the plume margin that are characterized by relative warm upper waters and intermediate chlorophyll-a concentrations. (3) Oxygenated bottom water group. Species of this group; Impagidinium aculeatum, Impagidinium patulum, Impagidinium sphaericum, Operculodinium centrocarpum and Operculodinium israelianum have their highest relative abundances at sites where bottom waters are formed by well ventilated Adriatic Deep Water or Eastern Mediterranean Deep Water. (4) Golfo di Taranto group consisting of round brown cysts produced by Protoperidinium species (grouped as Brigantedinium spp,). The variation in accumulation rates can be related to gradiental changes in the trophic state of the surface waters linked to river outflow. Most species show a positive relationship between cyst production and nutrient/trace element availability in upper waters. No negative correlation between cyst production and nutrient/trace element availability could be documented. Production of Brigantidinium spp., Echinidinium spp., L. sabrina. L. machaerophorum, P. kofoidii/schwarzii, Spiniferites spp., S. mirabilis and S. quanta shows the most pronounced increase with increasing nutrient/trace element availability. These species can be considered as valuable indicators for reconstructing changes in the trophic state of the upper waters within the Po-river area in palaeo-environmental studies. (C) 2009 Elsevier B.V. All rights reserved.	[Zonneveld, Karin A. F.; Chen, Liang] Fachbereich 5 Geowissensch, D-28334 Bremen, Germany; [Moebius, Juergen] Inst Biogeochem & Meereschem, D-20146 Hamburg, Germany; [Mahmoud, Magdy S.] Assiut Univ, Fac Sci, Dept Geol, Assiut 71516, Egypt	University of Bremen; Egyptian Knowledge Bank (EKB); Assiut University	Zonneveld, KAF (通讯作者)，Fachbereich 5 Geowissensch, Postfach 330440, D-28334 Bremen, Germany.	zonnev@uni-bremen.de	Mahmoud, Magdy/ABD-1262-2020		German Science foundation (DFG)	German Science foundation (DFG)(German Research Foundation (DFG))	We thank the captain Schneider and the R.V. POSEIDON crew members for the professional and kind help of collecting the samples during the CAPPUCINCI cruise. This study has been carried out in the German Science foundation (DFG) sponsored International Graduate college EUROPROX and ISF project MOCCHA through financing of the shiptime and the position of Liang Chen. The Humbold Foundation is thanked for making a stay of Magdy Mahmoud in July-September at the University of Bremen possible. We thank the two reviewers and the editor for their constructive remarks that improved the paper.	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NOV	2009	62	4					189	213		10.1016/j.seares.2009.02.003	http://dx.doi.org/10.1016/j.seares.2009.02.003			25	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	539KE					2025-03-11	WOS:000273252000001
J	Feist-Burkhardt, S				Feist-Burkhardt, Susanne			Palynology of the Sinemurian/Pliensbachian boundary (Lower Jurassic) in the Wutach area, SW Germany: dinoflagellate cyst systematics, biostratigraphy and heterotrophic character of <i>Liasidium variabile</i>	NEUES JAHRBUCH FUR GEOLOGIE UND PALAONTOLOGIE-ABHANDLUNGEN			English	Review						Jurassic; Sinemurian; Pliensbachian; dinoflagellate cysts; systematics; biostratigraphy; trophic mode; Liasidium; heterotroph	STRATOTYPE SECTION; POINT GSSP; STRATIGRAPHY; ASSEMBLAGES; YORKSHIRE; BOREHOLE; TOARCIAN; STRATA; BASE	A palynological study of the outcrop section at Aselfingen, Wutach area, SW Germany, has yielded well-preserved and relatively diverse dinoflagellate cyst assemblages from sediments of Late Sinemurian and Early Pliensbachian age. The encountered dinoflagellate cyst taxa are documented and their morphology, systematics and stratigraphical ranges are discussed. The precise correlation of the samples to chronozones and subzones and the continuous record of dinoflagellate cysts from all sampled beds in this section allow a high-resolution palynostratigraphical characterisation of the Sinemurian/Pliensbachian boundary. This was not possible in the recently ratified Global Boundary Stratigraphic Section and Point (GSSP) for the base of the Pliensbachian stage in Yorkshire, UK, because it was found to be devoid of dinoflagellate cysts. The study yielded new information on the stratigraphical ranges of some widely used index taxa such as Liasidium variabile, Mancodinium semitabulatum and Valvaeodinium armatum. The discovery of weakly fluorescing, brown-pigmented specimens of Liasidium variabile, together with evidence from previous studies, leads to the interpretation that these cysts may have been formed by a heterotrophic dinoflagellate.	Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England	Natural History Museum London	Feist-Burkhardt, S (通讯作者)，Nat Hist Museum, Dept Palaeontol, Cromwell Rd, London SW7 5BD, England.	S.Feist-Burkhardt@nhm.ac.uk	Feist-Burkhardt, Susanne/B-1522-2009	Feist-Burkhardt, Susanne/0000-0001-6019-6242	Deutsche Forschungsgemeinschaft (DFG); CHITOLIE (Geotechniques Research and NHM)	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG)); CHITOLIE (Geotechniques Research and NHM)	I would like to thank C. MEISTER (Museum d'Histoire Naturelle, Geneva) and J. BLAU (Rosbach- Rodheim, Germany) for initiating this project, their help in sampling the section and advice on Early Jurassic ammonite biostratigraphy. Many thanks also go to the other members of the German Subcommission of Jurassic Stratigraphy for dis cussions, and especially to R. SCHLATTER (Naturkundemuseum Leipzig) for guiding the fieldtrip at Aselfingen. I am grateful to J. E. WILLIAMS (NHM) for access to his library and reference system, and to him and T. L. POTTER (NHM) for valuable advice and their help with editing the English text. N. POULSEN (Copenhagen) and C. MEISTER (Geneva) are thanked for their constructive reviews. Samples were processed in the palynology laboratory at Darmstadt University of Technology thanks to funds provided by Deutsche Forschungsgemeinschaft (DFG) and by J. CHITOLIE (Geotechniques Research and NHM).	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Jahrb. Geol. Palaontol.-Abh.	NOV	2009	254	3					293	313		10.1127/0077-7749/2009/0019	http://dx.doi.org/10.1127/0077-7749/2009/0019			21	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	539PS					2025-03-11	WOS:000273269500003
J	Mertens, KN; Verhoeven, K; Verleye, T; Louwye, S; Amorim, A; Ribeiro, S; Deaf, AS; Harding, IC; De Schepper, S; González, C; Kodrans-Nsiah, M; De Vernal, A; Henry, M; Radi, T; Dybkjaer, K; Poulsen, NE; Feist-Burkhardt, S; Chitolie, J; Heilmann-Clausen, C; Londeix, L; Turon, JL; Marret, F; Matthiessen, J; McCarthy, FMG; Prasad, V; Pospelova, V; Hughes, JEK; Riding, JB; Rochon, A; Sangiorgi, F; Welters, N; Sinclair, N; Thun, C; Soliman, A; Van Nieuwenhove, N; Vink, A; Young, M				Mertens, Kenneth Neil; Verhoeven, Koen; Verleye, Thomas; Louwye, Stephen; Amorim, Ana; Ribeiro, Sofia; Deaf, Amr S.; Harding, Ian C.; De Schepper, Stijn; Gonzalez, Catalina; Kodrans-Nsiah, Monika; De Vernal, Anne; Henry, Maryse; Radi, Taoufik; Dybkjaer, Karen; Poulsen, Niels E.; Feist-Burkhardt, Susanne; Chitolie, Jonah; Heilmann-Clausen, Claus; Londeix, Laurent; Turon, Jean-Louis; Marret, Fabienne; Matthiessen, Jens; McCarthy, Francine M. G.; Prasad, Vandana; Pospelova, Vera; Hughes, Jane E. Kyffin; Riding, James B.; Rochon, Andre; Sangiorgi, Francesca; Welters, Natasja; Sinclair, Natalie; Thun, Christian; Soliman, Ali; Van Nieuwenhove, Nicolas; Vink, Annemiek; Young, Martin			Determining the absolute abundance of dinoflagellate cysts in recent marine sediments: The <i>Lycopodium</i> marker-grain method put to the test	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate cyst; concentration; Lycopodium clavatum tablets; spike; inter-laboratory calibration	SURFACE SEDIMENTS; PRESERVATION; MICROFOSSIL; ASSEMBLAGES; SAMPLE	Absolute abundances (concentrations) of dinoflagellate cysts are often determined through the addition of Lycopodium clavatum marker-grains as a spike to a sample before palynological processing. An inter-laboratory calibration exercise was set up in order to test the comparability of results obtained in different laboratories, each using its own preparation method. Each of the 23 laboratories received the same amount of homogenized splits of four Quaternary sediment samples. The samples originate from different localities and consisted of a variety of lithologies. Dinoflagellate cysts were extracted and counted, and relative and absolute abundances were calculated. The relative abundances proved to be fairly reproducible, notwithstanding a need for taxonomic calibration. By contrast, excessive loss of Lycopodium spores during sample preparation resulted in non-reproducibility of absolute abundances. Use of oxidation, KOH, warm acids, acetolysis, mesh sizes larger than 15 mu m and long ultrasonication (>1 min) must be avoided to determine reproducible absolute abundances. The results of this work therefore indicate that the dinoflagellate cyst worker should make a choice between using the proposed standard method which circumvents critical steps, adding Lycopodium tablets at the end of the preparation and using an alternative method. (C) 2009 Elsevier B.V. All rights reserved.	[Mertens, Kenneth Neil; Verhoeven, Koen; Verleye, Thomas; Louwye, Stephen] Res Unit Palaeontol, B-9000 Ghent, Belgium; [Amorim, Ana; Ribeiro, Sofia] Univ Lisbon, Inst Oceanografia, Fac Ciencias, P-1749016 Lisbon, Portugal; [Deaf, Amr S.; Harding, Ian C.] Univ Southampton, Sch Ocean & Earth Sci, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England; [De Schepper, Stijn; Gonzalez, Catalina; Kodrans-Nsiah, Monika] Univ Bremen, Dept Geosci, D-28334 Bremen, Germany; [De Vernal, Anne; Henry, Maryse; Radi, Taoufik] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Dybkjaer, Karen; Poulsen, Niels E.] Geol Survey Denmark & Greenland, DK-1350 Copenhagen K, Denmark; [Feist-Burkhardt, Susanne; Chitolie, Jonah] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Heilmann-Clausen, Claus] Aarhus Univ, Inst Geol, DK-8000 Aarhus C, Denmark; [Londeix, Laurent; Turon, Jean-Louis] Univ Bordeaux 1, CNRS, UMR 5805, OEPOC1, F-33405 Talence, France; [Marret, Fabienne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Matthiessen, Jens] Alfred Wegener Inst Polar & Marine Res, D-27515 Bremerhaven, Germany; [McCarthy, Francine M. G.] Brock Univ, St Catharines, ON L2S 3A1, Canada; [Prasad, Vandana] Birbal Sahni Inst Paleobot, Micropaleontol Lab, Lucknow 226007, Uttar Pradesh, India; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3V6, Canada; [Hughes, Jane E. Kyffin; Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Keyworth NG12 5GG, Notts, England; [Rochon, Andre] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada; [Sangiorgi, Francesca; Welters, Natasja] Univ Utrecht, Inst Environm Biol, Fac Sci, Lab Palaeobot & Palynol, NL-3584 CD Utrecht, Netherlands; [Sinclair, Natalie; Thun, Christian] Geosci Australia, Canberra, ACT 2601, Australia; [Soliman, Ali] Karl Franzens Univ Graz, Inst Earth Sci, A-8010 Graz, Austria; [Van Nieuwenhove, Nicolas] Leibniz Inst Marine Sci, IFM, GEOMAR, D-24148 Kiel, Germany; [Vink, Annemiek] Fed Inst Geosci & Nat Resources, D-30655 Hannover, Germany; [Young, Martin] CSIRO Petr, N Ryde, NSW 2113, Australia; [Sinclair, Natalie] Australian Natl Univ, Res Sch Earth Sci, Acton, ACT 0200, Australia; [Soliman, Ali] Tanta Univ, Dept Geol, Fac Sci, Tanta 31527, Egypt	Universidade de Lisboa; NERC National Oceanography Centre; University of Southampton; University of Bremen; University of Quebec; University of Quebec Montreal; Geological Survey Of Denmark & Greenland; Natural History Museum London; Aarhus University; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Liverpool; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Brock University; Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP); University of Victoria; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Quebec; Utrecht University; Geoscience Australia; University of Graz; Helmholtz Association; GEOMAR Helmholtz Center for Ocean Research Kiel; Commonwealth Scientific & Industrial Research Organisation (CSIRO); Australian National University; Egyptian Knowledge Bank (EKB); Tanta University	Mertens, KN (通讯作者)，Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	Kenneth.Mertens@ugent.be	Arango, Catalina/D-2308-2011; Feist-Burkhardt, Susanne/B-1522-2009; Ribeiro, Sofia/AAZ-2782-2021; Verhoeven, Koen/IZP-9609-2023; Deaf, Amr/AAF-6269-2020; Mertens, Kenneth/AAO-9566-2020; PRASAD, VANDANA/KUF-4093-2024; Heilmann-Clausen, Claus/A-4848-2012; Van Nieuwenhove, Nicolas/IAQ-1532-2023; Dybkjær, Karen/G-5223-2018; Harding, Ian/K-3320-2012; Soliman, Ali/R-1583-2018; Amorim, Ana/AAA-2615-2020; de Vernal, Anne/D-5602-2013; De Schepper, Stijn/A-2836-2011; Ribeiro, Sofia/G-9213-2018; Vink, Annemiek/GXG-6435-2022; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Amorim, Ana/0000-0002-9612-4280; Marret-Davies, Fabienne/0000-0003-4244-0437; Gonzalez Arango, Catalina/0000-0003-1709-4405; Van Nieuwenhove, Nicolas/0000-0001-6369-2751; Deaf, Amr/0000-0002-5073-7911; Matthiessen, Jens/0000-0002-6952-2494; de Vernal, Anne/0000-0001-5656-724X; Sangiorgi, Francesca/0000-0003-4233-6154; De Schepper, Stijn/0000-0002-6934-0914; Harding, Ian/0000-0003-4281-0581; Feist-Burkhardt, Susanne/0000-0001-6019-6242; Pospelova, Vera/0000-0003-4049-8133; Soliman, Ali/0000-0001-7366-4607; Ribeiro, Sofia/0000-0003-0672-9161; Vink, Annemiek/0000-0002-5178-9721; Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483	NERC [bgs05009, bgs04003] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		BENNINGHOFF W. S., 1962, POLLEN ET SPORES, V4, P332; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; De Vernal A., 1996, CAHIERS GEOTOP, V3; DESEZAR YB, 1994, AM ASS STRATIGRAPHIC, V27, P12; DEVERNAL A, 1987, POLLEN SPORES, V19, P291; Fensome R. 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Palaeobot. Palynology	NOV	2009	157	3-4					238	252		10.1016/j.revpalbo.2009.05.004	http://dx.doi.org/10.1016/j.revpalbo.2009.05.004			15	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	534OI		Green Accepted			2025-03-11	WOS:000272906600005
J	De Schepper, S; Head, MJ; Groeneveld, J				De Schepper, Stijn; Head, Martin J.; Groeneveld, Jeroen			North Atlantic Current variability through marine isotope stage M2 (circa 3.3 Ma) during the mid-Pliocene	PALEOCEANOGRAPHY			English	Article							SEA-SURFACE CONDITIONS; DINOFLAGELLATE CYST ASSEMBLAGES; CONTINENTAL-MARGIN; NORDIC SEAS; THERMOHALINE CIRCULATION; PLANKTONIC-FORAMINIFERA; HEMISPHERE GLACIATIONS; GLOBIGERINA-BULLOIDES; OCEAN; PLEISTOCENE	The mid-Pliocene was an episode of prolonged global warmth and strong North Atlantic thermohaline circulation, interrupted briefly at circa 3.30 Ma by a global cooling event corresponding to marine isotope stage (MIS) M2. Paleoceanographic changes in the eastern North Atlantic have been reconstructed between circa 3.35 and 3.24 Ma at Deep Sea Drilling Project Site 610 and Integrated Ocean Drilling Program Site 1308. Mg/Ca ratios and delta O-18 from Globigerina bulloides are used to reconstruct the temperature and relative salinity of surface waters, and dinoflagellate cyst assemblages are used to assess variability in the North Atlantic Current (NAC). Our sea surface temperature data indicate warm waters at both sites before and after MIS M2 but a cooling of similar to 2-3 degrees C during MIS M2. A dinoflagellate cyst assemblage overturn marked by a decline in Operculodinium centrocarpum reflects a southward shift or slowdown of the NAC between circa 3.330 and 3.283 Ma, reducing northward heat transport 23-35 ka before the global ice volume maximum of MIS M2. This will have established conditions that ultimately allowed the Greenland ice sheet to expand, leading to the global cooling event at MIS M2. Comparison with an ice-rafted debris record excludes fresh water input via icebergs in the northeast Atlantic as a cause of NAC decline. The mechanism causing the temporary disruption of the NAC may be related to a brief reopening of the Panamanian Gateway at about this time.	[De Schepper, Stijn] Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Groeneveld, Jeroen] Univ Bremen, MARUM, D-28334 Bremen, Germany	University of Bremen; Brock University; University of Bremen	De Schepper, S (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330 440, D-28334 Bremen, Germany.	sdeschepper@uni-bremen.de; mjhead@brocku.ca; jeroen.groeneveld@awi.de	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914	Gates Cambridge Trust; Dudley Stamp Memorial Trust (Royal Society); Philip Lake Fund (Department of Geography, University of Cambridge); Deutsche Forschungsgemeinschaft; Natural Sciences and Engineering Research Council of Canada; MARUM Fellowship	Gates Cambridge Trust; Dudley Stamp Memorial Trust (Royal Society)(Royal Society); Philip Lake Fund (Department of Geography, University of Cambridge)(University of Cambridge); Deutsche Forschungsgemeinschaft(German Research Foundation (DFG)); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR); MARUM Fellowship	This contribution is based partly on the doctoral research of S. D. S., who is grateful to the Gates Cambridge Trust for the award of a Gates Cambridge Scholarship (University of Cambridge) and additional funding from the Dudley Stamp Memorial Trust (Royal Society) and Philip Lake Fund (Department of Geography, University of Cambridge). S. D. S. also appreciates funding from the Deutsche Forschungsgemeinschaft (International Graduate College "Proxies in Earth History,'' EUROPROX, University of Bremen) and MARUM (G. Wefer). M.J.H. acknowledges support from a Natural Sciences and Engineering Research Council of Canada discovery grant. J.G. is grateful for a MARUM Fellowship, funded through the DFG Research Center/Excellence Cluster program "The Ocean in the Earth System.'' G. Bartoli and H. Kleiven kindly shared their raw data. Thanks are extended to M. Hall, P. Ferretti, L. de Abreu, and J. Rolfe (University of Cambridge), M. Segl (University of Bremen), and S. Vancauwenberghe (Ghent University) for technical assistance. Comments by F. Eynaud and H. Dowsett on an earlier version of the manuscript and by J. Matthiessen, an anonymous reviewer, and G. Dickens on a more recent version are gratefully acknowledged. IODP is thanked for providing the samples.	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J	Klein, G; Kaczmarska, I; Ehrman, JM				Klein, Georgia; Kaczmarska, Irena; Ehrman, James M.			The diatom <i>Chaetoceros</i> in ships' ballast waters - survivorship of stowaways	ACTA BOTANICA CROATICA			English	Article	20th International Diatom Symposium	SEP 07-13, 2008	Dubrovnik, CROATIA	Croatian Botan Soc, Univ Zagreb, Fac Sci, Algol Grp		Diatom; Chaetoceros; phytoplankton; non-indigenous species; ballast water; resting stage; spore; ultrastructure	RESTING SPORES; DINOFLAGELLATE CYSTS; SEDIMENTS; TRANSPORT; SURVIVAL; BACILLARIOPHYCEAE; GERMINATION; COAST; SEA; BAY	Ship ballast water discharged by vessels into the receiving port is recognised today as all important vector for the spread of non-indigenous species and facilitates the introduction of potential invasive species. Here, we report on 18 species (of about 30 identified), both vegetative cells and spores, of the diatom genus Chaetoceros Ehrenberg found in ballast water collected from ships arriving at Canadian ports on the West Coast (WC), East Coast (EC) and the Great Lakes (GL). We found live, vegetative Chaetoceros cells (one of the most abundant taxa) in 49% of the 57 ballast water samples. The highest density of viable spores enumerated in our counts was 414 cells L(-1). In 62% of 52 samples examined Using scanning electron microscopy (SEM), Chaetoceros spores were found, though fewer live, identifiable spores were found Using light microscopy. Three reportedly harmful species, C. convolutus, C. danicus, C. debilis were encountered in WC samples, and additionally, C. cf. hispidus, a species not yet reported from Canada. C. ceratosporus and C. cf. subsecundus, to date reported only from the EC of the USA, now have been transported to the port of Vancouver, British Columbia. Our findings contribute to the assessment of the effectiveness of ballast water treatment via water exchange, and serve to evaluate the diversity of diatom vegetative cells and spores transported in ballast water tanks.	[Klein, Georgia; Kaczmarska, Irena] Mt Allison Univ, Dept Biol, Sackville, NB E4L 1G7, Canada; [Ehrman, James M.] Mt Allison Univ, Digital Microscopy Facil, Sackville, NB E4L 1G7, Canada	Mount Allison University; Mount Allison University	Klein, G (通讯作者)，Mt Allison Univ, Dept Biol, Sackville, NB E4L 1G7, Canada.	gklein@mta.ca						Anil AC, 2007, J EXP MAR BIOL ECOL, V343, P37, DOI 10.1016/j.jembe.2006.11.006; BATES SS, 2006, CANADIAN TECHNICAL R, V2668, P1; BERARDTHERRIAUL.L, 1999, GUIDE IDENTIFICATION; Bolch CJS, 2007, HARMFUL ALGAE, V6, P465, DOI 10.1016/j.hal.2006.12.008; Breen E, 2008, ESTUAR COAST, V31, P728, DOI 10.1007/s12237-008-9068-1; Carlton JT, 1996, ECOLOGY, V77, P1653, DOI 10.2307/2265767; Cleve-Euler A., 1951, DIATOMEEN SCHWEDEN F; Cupp E.E., 1943, MARINE PLANKTON DIAT; Drebes G., 1974, MARINES PHYTOPLANKTO; Edlund MB, 2000, CAN J FISH AQUAT SCI, V57, P610, DOI 10.1139/cjfas-57-3-610; GARRISON D L, 1981, Journal of Plankton Research, V3, P137, DOI 10.1093/plankt/3.1.137; 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, 1990, P 4 INT C TOX MAR PH; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; HASLE R, 1997, IDENTIFYING MARINE D, P3; HOLLIBAUGH JT, 1981, J PHYCOL, V17, P1; Horner RA, 1997, LIMNOL OCEANOGR, V42, P1076, DOI 10.4319/lo.1997.42.5_part_2.1076; Hustedt F., 1962, L RABENHORSTS KRYPTO; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; Jokela A, 2008, FRESHWATER BIOL, V53, P1845, DOI 10.1111/j.1365-2427.2008.02009.x; Kaczmarska I, 2005, HARMFUL ALGAE, V4, P1, DOI 10.1016/j.hal.2003.07.001; Kuwata A, 1999, MAR BIOL, V134, P471, DOI 10.1007/s002270050563; MARTIN JL, 2006, CANADIAN TECHNICAL R, V2629; MARTIN JL, 2001, CANADIAN TECHNICAL R, V2349; McQuoid MR, 2002, EUR J PHYCOL, V37, P191, DOI 10.1017/S0967026202003670; 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; Pertola S, 2006, MAR POLLUT BULL, V52, P900, DOI 10.1016/j.marpolbul.2005.11.028; Peterson TD, 1999, BOT MAR, V42, P253, DOI 10.1515/BOT.1999.029; PITCHER GC, 1990, ESTUAR COAST SHELF S, V31, P283, DOI 10.1016/0272-7714(90)90105-Z; Proschkina-Lavrenko A. 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OCT	2009	68	2					325	338						14	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	514MX					2025-03-11	WOS:000271400100013
J	Falk-Petersen, S; Haug, T; Hop, H; Nilssen, KT; Wold, A				Falk-Petersen, Stig; Haug, Tore; Hop, Haakon; Nilssen, Kjell T.; Wold, Anette			Transfer of lipids from plankton to blubber of harp and hooded seals off East Greenland	DEEP-SEA RESEARCH PART II-TOPICAL STUDIES IN OCEANOGRAPHY			English	Article						Lipids; Fatty acids; Stable isotopes; Harp seal; Hooded seal; East Greenland Sea	MARGINAL ICE-ZONE; CYSTOPHORA-CRISTATA; PHOCA-GROENLANDICA; FOOD-WEB; TROPHIC RELATIONSHIPS; STABLE-ISOTOPES; BARENTS SEA; FATTY-ACIDS; DIVING BEHAVIOR; FEEDING-HABITS	Sub-Arctic marine ecosystems are some of the most productive ecosystems in the world's oceans. The capacity of herbivorous zooplankton, such as Calanus, to biosynthesize and store large amounts of lipids during the short and intense spring bloom is a fundamental adaptation which facilitates the large production in these ecosystems. These energy-rich lipids are rapidly transferred through the food chain to Arctic seals. The fatty acids and stable isotopes from harp seal (Phoca groenlandica) and hooded seal (Cystophora cristata) off East Greenland as well as their potential prey, were analysed. The results were used to describe the lipid dynamics and energy transfer in parts of the East Greenland ecosystem. Even if the two seal species showed considerable overlap in diet and occurred at relatively similar trophic levels, the fatty acid profiles indicated that the bases of the food chains of harp and hooded seals were different. The fatty acids of harp seals originate from diatom-based food chain, whereas the fatty acids of hooded seals originate from dinoflagellate and the prymnesiophyte Phaeocystis pouchetii-based food chain. Stable isotope analyses showed that both species are true carnivores on the top of their food chains, with hooded seal being slightly higher on the food chain than harp seal. (C) 2008 Elsevier Ltd. All rights reserved.	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F., 1988, CANOCO REFERENCE MAN; WELCH HE, 1992, ARCTIC, V45, P343	55	38	43	1	50	PERGAMON-ELSEVIER SCIENCE LTD	OXFORD	THE BOULEVARD, LANGFORD LANE, KIDLINGTON, OXFORD OX5 1GB, ENGLAND	0967-0645	1879-0100		DEEP-SEA RES PT II	Deep-Sea Res. Part II-Top. Stud. Oceanogr.	OCT	2009	56	21-22					2080	2086		10.1016/j.dsr2.2008.11.020	http://dx.doi.org/10.1016/j.dsr2.2008.11.020			7	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	511CL					2025-03-11	WOS:000271141400018
J	Warny, S; Askin, RA; Hannah, MJ; Mohr, BAR; Raine, JI; Harwood, DM; Florindo, F; Levy, R; Acton, G; Atkins, C; Bassett, K; Berg, M; Bibby, T; Blair, S; Blank, L; Browne, G; Del Carlo, P; Dooley, J; Drew, S; Dunbar, G; Field, B; Fielding, C; Frank, T; Frisch-Gleason, R; Grelle, T; Handwerger, D; Hoffmann, S; Hubbard, J; Huffman, L; Ishman, S; Johnson, K; Jovane, L; Konfirst, M; Krissek, L; Kuhn, G; Lacy, L; Lehmann, R; Magens, D; Mankoff, K; Millan, C; Nielsen, S; Olney, M; Panter, K; Passchier, S; Patterson, T; Paulsen, T; Pekar, S; Persico, D; Petrushak, S; Pierdominici, S; Pound, K; Reed, J; Reichelt, L; Riesselman, C; Sandroni, S; Schmitt, D; di Clemente, GS; Speece, M; Strada, E; Szymcek, P; Talarico, F; Taviani, M; Tuzzi, E; Williams, R; Wonik, T				Warny, Sophie; Askin, Rosemary A.; Hannah, Michael J.; Mohr, Barbara A. R.; Raine, J. Ian; Harwood, David M.; Florindo, Fabio; Levy, Richard (Rich); Acton, Gary; Atkins, Clifford (Cliff); Bassett, Kari; Berg, Megan; Bibby, Theodore (Ted); Blair, Stacie; Blank, Leslie; Browne, Gregory (Greg); Del Carlo, Paola; Dooley, Julia; Drew, Scott; Dunbar, Gavin; Field, Bradley (Brad); Fielding, Christopher (Chris); Frank, Tracy; Frisch-Gleason, Robin; Grelle, Thomas; Handwerger, David (Dave); Hoffmann, Stefan; Hubbard, Joanna; Huffman, Louise; Ishman, Scott; Johnson, Katherine (Katie); Jovane, Luigi; Konfirst, Matthew (Matt); Krissek, Lawrence (Larry); Kuhn, Gerhard (Gerd); Lacy, Laura; Lehmann, Rainer; Magens, Diana; Mankoff, Kenneth (Ken); Millan, Cristina; Nielsen, Simon; Olney, Matthew (Matt); Panter, Kurt; Passchier, Sandra; Patterson, Taylor; Paulsen, Timothy (Tim); Pekar, Stephen (Steve); Persico, Davide; Petrushak, Steven (Steve); Pierdominici, Simona; Pound, Katherine (Kate); Reed, Joshua (Josh); Reichelt, Lucia (Lucy); Riesselman, Christina; Sandroni, Sonia; Schmitt, Douglas (Doug); di Clemente, Graziano Scotto; Speece, Marvin (Marv); Strada, Eleonora; Szymcek, Phillip (Phill); Talarico, Franco; Taviani, Marco; Tuzzi, Eva; Williams, Robert (Bob); Wonik, Thomas		SMS Sci Team	Palynomorphs from a sediment core reveal a sudden remarkably warm Antarctica during the middle Miocene	GEOLOGY			English	Article							DINOFLAGELLATE CYST DISTRIBUTION; NORTH-SEA BASIN; CLIMATE; PLIOCENE; STRATIGRAPHY; VEGETATION; GREENLAND; OLIGOCENE; TRANSECT; BELGIUM	An exceptional triple palynological signal (unusually high abundance of marine, freshwater, and terrestrial palynomorphs) recovered from a core collected during the 2007 ANDRILL (Antarctic geologic drilling program) campaign in the Ross Sea, Antarctica, provides constraints for the Middle Miocene Climatic Optimum. Compared to elsewhere in the core, this signal comprises a 2000-fold increase in two species of dinoflagellate cysts, a synchronous five-fold increase in freshwater algae, and up to an 80-fold increase in terrestrial pollen, including a proliferation of woody plants. Together, these shifts in the palynological assemblages ca. 15.7 Ma ago represent a relatively short period of time during which Antarctica became abruptly much warmer. Land temperatures reached 10 degrees C (January mean), estimated annual sea-surface temperatures ranged from 0 to 11.5 degrees C, and increased freshwater input lowered the salinity during a short period of sea-ice reduction.	[Warny, Sophie; Askin, Rosemary A.] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie; Askin, Rosemary A.] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA; [Hannah, Michael J.] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Antarctic Res Ctr, Wellington, New Zealand; [Mohr, Barbara A. R.] Museum Nat Hist, D-10115 Berlin, Germany; [Raine, J. Ian; Levy, Richard (Rich); Browne, Gregory (Greg); Field, Bradley (Brad)] GNS Sci, Lower Hutt, New Zealand; [Harwood, David M.; Fielding, Christopher (Chris); Frank, Tracy; Tuzzi, Eva] Univ Nebraska, Dept Geosci, Lincoln, NE 68588 USA; [Harwood, David M.; Huffman, Louise; Lacy, Laura; Reed, Joshua (Josh)] Univ Nebraska, ANDRILL Sci Management Off, Lincoln, NE 68588 USA; [Florindo, Fabio] Ist Nazl Geofis & Vulcanol, I-00143 Rome, Italy; [Acton, Gary] Univ Calif Davis, Dept Geol, Davis, CA 95616 USA; [Atkins, Clifford (Cliff)] Victoria Univ Wellington, Sch Geog Environm & Earth Sci, Wellington 6005, New Zealand; [Bassett, Kari] Univ Canterbury, Dept Geol Sci, Christchurch, New Zealand; [Bibby, Theodore (Ted); Blair, Stacie; Petrushak, Steven (Steve)] Florida State Univ, Dept Geol Sci, Tallahassee, FL 32306 USA; [Blank, Leslie] Raytheon Polar Serv, Centennial, CO USA; [Del Carlo, Paola] Ist Nazl Geofis & Vulcanol, Sezione Pisa, I-56126 Pisa, Italy; [Drew, Scott; Krissek, Lawrence (Larry); Millan, Cristina] Ohio State Univ, Sch Earth Sci, Columbus, OH 43210 USA; [Dunbar, Gavin] Victoria Univ Wellington, Antarctic Res Ctr, Wellington 6005, New Zealand; [Grelle, Thomas; Wonik, Thomas] LIAG, Hannover, Germany; Victoria Univ Wellington, Sch Earth Sci, Wellington 4007, New Zealand; [Hoffmann, Stefan] Univ Gottingen, Dept Sedimentol & Environm Geol, D-37077 Gottingen, Germany; [Ishman, Scott] SO Illinois Univ Carbondale, Dept Geol, Carbondale, IL 62901 USA; [Johnson, Katherine (Katie)] Geomarine Res, Auckland 1072, New Zealand; [Jovane, Luigi] Univ Calif Davis, Paleomagnet Lab, Dept Geol, Davis, CA 95616 USA; [Konfirst, Matthew (Matt)] No Illinois Univ, Dept Geol & Environm Geosci, De Kalb, IL 60115 USA; [Kuhn, Gerhard (Gerd); Magens, Diana] Alfred Wegener Inst, Dept Marine Geophys, D-27515 Bremerhaven, Germany; [Mankoff, Kenneth (Ken)] NASA GISS, New York, NY 10025 USA; [Nielsen, Simon] Japan Agcy Marine Earth Sci & Technol, Ctr Deep Earth Explorat, Yokohama, Kanagawa 2360001, Japan; [Olney, Matthew (Matt)] Univ S Florida, Dept Geol, Tampa, FL 33620 USA; [Panter, Kurt] Bowling Green State Univ, Earth & Environm Stud, Bowling Green, OH 43403 USA; [Passchier, Sandra] Montclair State Univ, Earth & Environm Stud, Montclair, NJ 07043 USA; [Patterson, Taylor; Speece, Marvin (Marv)] Montana Tech Univ Montana, Dept Geophys Engn, Butte, MT 59701 USA; [Paulsen, Timothy (Tim)] Univ Wisconsin Oshkosh, Dept Geol, Oshkosh, WI 54901 USA; [Pekar, Stephen (Steve)] Queens Coll, Sch Earth & Environm Sci, Flushing, NY 11367 USA; [Persico, Davide] Univ Parma, Dipartimento Sci Terra, I-43100 Parma, Italy; [Pierdominici, Simona] Ist Nazl Geofis & Vulcanol, I-00143 Rome, Italy; [Pound, Katherine (Kate)] St Cloud State Univ, Dept Earth & Atmospher Sci, St Cloud, MN 56301 USA; [Reichelt, Lucia (Lucy)] Alfred Wegener Inst, D-27568 Bremerhaven, Germany; [Riesselman, Christina] Stanford Univ, Geol & Environm Sci, Stanford, CA 94305 USA; [Sandroni, Sonia] Sez Sci Terra Siena, Museo Nazl Antartide, I-53100 Siena, Italy; [Schmitt, Douglas (Doug)] Univ Alberta, Inst Geophys Res, Dept Phys, Edmonton, AB T6G 2G7, Canada; [di Clemente, Graziano Scotto; Talarico, Franco] Secondary Sch Luigi Stefanini, I-31100 Treviso, Italy; [Strada, Eleonora] Univ Siena, Dipartimento Sci Terra, I-53100 Siena, Italy; [Taviani, Marco] CNR, ISMAR Bologna, I-40129 Bologna, Italy	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University; Victoria University Wellington; GNS Science - New Zealand; University of Nebraska System; University of Nebraska Lincoln; University of Nebraska System; University of Nebraska Lincoln; Istituto Nazionale Geofisica e Vulcanologia (INGV); University of California System; University of California Davis; Victoria University Wellington; University of Canterbury; State University System of Florida; Florida State University; Istituto Nazionale Geofisica e Vulcanologia (INGV); University System of Ohio; Ohio State University; Victoria University Wellington; Leibniz Institut fur Angewandte Geophysik (LIAG); Victoria University Wellington; University of Gottingen; Southern Illinois University System; Southern Illinois University; University of California System; University of California Davis; Northern Illinois University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; National Aeronautics & Space Administration (NASA); NASA Goddard Space Flight Center; Goddard Institute for Space Studies; Japan Agency for Marine-Earth Science & Technology (JAMSTEC); State University System of Florida; University of South Florida; University System of Ohio; Bowling Green State University; Montclair State University; University of Montana System; University of Montana; University of Wisconsin System; University of Wisconsin Oshkosh; City University of New York (CUNY) System; Queens College NY (CUNY); University of Parma; Istituto Nazionale Geofisica e Vulcanologia (INGV); Minnesota State Colleges & Universities; Saint Cloud State University; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Stanford University; University of Alberta; University of Siena; Consiglio Nazionale delle Ricerche (CNR); Istituto di Scienze Marine (ISMAR-CNR)	Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E235 Howe Russell, Baton Rouge, LA 70803 USA.	swarny@lsu.edu; askin@bresnan.net; Michael.hannah@vuw.ac.nz; Barbara.mohr@museum.hu-berlin.de; I.Raine@gns.cri.nz; dharwood1@unl.edu; florindo@ingv.it; r.levy@gns.cri.nz; gdacton@ucdavis.edu; cliff.atkins@vuw.ac.nz; kari.bassett@canterbury.ac.nz; meganberg@mac.com; tcb03c@fsu.edu; blair@quartz.gly.fsu.edu; G.Browne@gns.cri.nz; delcarlo@pi.ingv.it; dooleyj@christina.k12.de.us; drew.37@osu.edu; gavin.dunbar@vuw.ac.nz; brad.field@gns.cri.nz; cfielding2@unl.edu; tfrank2@unl.edu; gleason@aaps.k12.mi.us; t.grelle@liag-hannover.de; dave@xmission.com; s.hoffmann@geo.uni-goettingen.de; hubbard_joanna@asdk12.org; lhuffman@andrill.org; sishman@siu.edu; k.johnson@geomarine.org.nz; jovane@geology.ucdavis.edu; mk@mattkonfirst.com; krissek@mps.ohio-state.edu; gerhard.kuhn@awi.de; llacy2@unl.edu; rainer.lehmann@gmx.net; Diana.Magens@awi.de; mankoff@giss.nasa.gov; millan.2@osu.edu; simon.n@jamstec.go.jp; cyclingolney@yahoo.co.uk; kpanter@bgsu.edu; passchiers@mail.montclair.edu; paulsen@uwosh.edu; stephen.pekar@qc.cuny.edu; davide.persico@unipr.it; gneissguy2000@yahoo.com; pierdominici@ingv.it; kspound@stcloudstate.edu; jareed@andrill.org; lreichelt@gmx.de; criessel@stanford.edu; sandroni@unisi.it; doug@phys.ualberta.ca; grscott@tin.it; mspeece@mtech.edu; strada2@unisi.it; pszymcek@gmail.com; talarico@unisi.it; marco.taviani@bo.ismar.cnr.it; evatuzzi@libero.it; bbermk@xtra.co.nz; Thomas.wonik@liag-hannover.de	Taviani, Marco/AAF-2168-2020; Sandroni, Sonia/C-7188-2008; Riesselman, Christina/H-5037-2012; Jovane, Luigi/AAH-5438-2020; Raine, James/D-5124-2009; Warny, Sophie/A-8226-2013; Del Carlo, Paola/AAH-1725-2019; Passchier, Sandra/AAQ-2243-2021; Pierdominici, Simona/JAC-4185-2023; Hannah, Michael/H-1083-2015; Florindo, Fabio/F-4119-2010; Passchier, Sandra/B-1993-2008	Pierdominici, Simona/0000-0002-5368-4536; Hannah, Michael/0000-0002-2275-0086; Florindo, Fabio/0000-0002-6058-9748; Passchier, Sandra/0000-0001-7204-7025; Warny, Sophie/0000-0002-3451-040X; Raine, James Ian/0000-0001-5294-2102	U. S. Antarctic Program; Raytheon Polar Services Corporation; Antarctica New Zealand; U. S. National Science Foundation; New Zealand Foundation for Research Science and Technology; Italian Antarctic Research Program; German Science Foundation; Alfred Wegener Institute	U. S. Antarctic Program; Raytheon Polar Services Corporation; Antarctica New Zealand; U. S. National Science Foundation(National Science Foundation (NSF)); New Zealand Foundation for Research Science and Technology(New Zealand Foundation for Research, Science and Technology); Italian Antarctic Research Program; German Science Foundation(German Research Foundation (DFG)); Alfred Wegener Institute	The ANDRILL (Antarctic geologic drilling) Program is a multinational collaboration between the Antarctic programs of Germany, Italy, New Zealand, and the United States. Antarctica New Zealand is the project operator and has developed the drilling system in collaboration with Alex Pyne at Victoria University of Wellington and Webster Drilling and Exploration. The U. S. Antarctic Program and Raytheon Polar Services Corporation supported the science team at McMurdo Station, while Antarctica New Zealand supported the drilling team at Scott Base. Scientific studies are jointly supported by the U. S. National Science Foundation, New Zealand Foundation for Research Science and Technology, the Italian Antarctic Research Program, the German Science Foundation, and the Alfred Wegener Institute. We are grateful to Vanessa Bowman and Rex Harland for their careful review of the manuscript.	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J	Genovesi, B; Laabir, M; Masseret, E; Collos, Y; Vaquer, A; Grzebyk, D				Genovesi, Benjamin; Laabir, Mohamed; Masseret, Estelle; Collos, Yves; Vaquer, Andre; Grzebyk, Daniel			Dormancy and germination features in resting cysts of <i>Alexandrium tamarense</i> species complex (Dinophyceae) can facilitate bloom formation in a shallow lagoon (Thau, southern France)	JOURNAL OF PLANKTON RESEARCH			English	Article							DINOFLAGELLATE GONYAULAX-TAMARENSIS; SCRIPPSIELLA-TROCHOIDEA DINOPHYCEAE; LAWRENCE ESTUARY CANADA; SETO INLAND SEA; TOXIC DINOFLAGELLATE; CATENELLA DINOPHYCEAE; PLANKTONIC DIATOMS; COASTAL WATERS; HIROSHIMA BAY; SEED BANK	This study investigated the dormancy length, germination patterns and cyst progeny fate of Alexandrium catenella and A. tamarense found in Thau lagoon, France. In laboratory-produced cysts, the dormancy period was estimated to be less than 2 weeks. A vernalization period was not required prior to germination. However, after 1 month of dark-storage at 6 degrees C, excystment was obtained 2-3 days from re-exposure to favourable conditions thereby suggesting that germination was sychronized. Germination patterns and germling cell viability in laboratory-produced cysts were similar to those exhibited in natural cysts. The following conditions optimized germination: temperature between 14 and 26 degrees C, salinity between 30 and 38 psu and light exposure for >1 h at 100 mu moles photons m(-2)s(-1). Similar conditions prevailed at the commencement of and during Alexandrium blooms in Thau lagoon, suggesting that cysts may germinate shortly after being recruited from sediment re-suspensions. Accordingly, cyst bank germinations contribute to the initial seeding of blooms, and subsequently germinations of newly formed cysts can help to maintain blooms.In cyst banks, the high germination capabilities seem, however, to be counter-balanced by the low viability of cyst progeny, as estimated from the realized seeding ratio. This ratio is proposed as a means of quantifying the potential for cyst banks to regenerate planktonic populations.	[Genovesi, Benjamin; Laabir, Mohamed; Masseret, Estelle; Collos, Yves; Vaquer, Andre; Grzebyk, Daniel] Univ Montpellier 2, Lab Ecosyst Lagunaires, UMR 5119, CNRS IFREMER IRD UM2, F-34095 Montpellier 05, France	Ifremer; Universite de Montpellier	Genovesi, B (通讯作者)，Univ Montpellier 2, Lab Ecosyst Lagunaires, UMR 5119, CNRS IFREMER IRD UM2, Pl Eugene Bataillon, F-34095 Montpellier 05, France.	benjamin.genovesi@gmail.com	Grzebyk, Daniel/A-9286-2009	Grzebyk, Daniel/0000-0002-1130-7724	Programme National d'Envirnnement Cotier (PNEC-France); Agence Nationale de la Recherche [ANR-05-BLAN-0219]; GenoSynTox [ANR-06-BLAN-0397]; Agence Nationale de la Recherche (ANR) [ANR-06-BLAN-0397, ANR-05-BLAN-0219] Funding Source: Agence Nationale de la Recherche (ANR)	Programme National d'Envirnnement Cotier (PNEC-France); Agence Nationale de la Recherche(Agence Nationale de la Recherche (ANR)); GenoSynTox; Agence Nationale de la Recherche (ANR)(Agence Nationale de la Recherche (ANR))	This study has been conducted with the support of the Region Languedoc-Roussillon through a Ph.D. fellowship granted to B.G., and with financial support from the Programme National d'Envirnnement Cotier (PNEC-France). The French funding agency Agence Nationale de la Recherche provided support to D.G. through the grants XpressFlorAl (ANR-05-BLAN-0219) and GenoSynTox (ANR-06-BLAN-0397)	ABADIE E, 1999, CONTAMINATION ETANG; ANDERSON DM, 1980, J PHYCOL, V16, P166; ANDERSON DM, 1987, LIMNOL OCEANOGR, V32, P340, DOI 10.4319/lo.1987.32.2.0340; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2856, DOI 10.1016/j.dsr2.2005.09.004; Anderson DM, 2005, DEEP-SEA RES PT II, V52, P2522, DOI 10.1016/j.dsr2.2005.06.014; ANDERSON DM, 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], P 12 INT C HARMF ALG; [Anonymous], 1997, ADV MAR BIOL; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; Band-Schmidt CJ, 2003, BOT MAR, V46, P44, DOI 10.1515/BOT.2003.007; Béchemin C, 1999, AQUAT MICROB ECOL, V20, P157, DOI 10.3354/ame020157; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; Blanco J, 1986, OCEANOGRAPHY WASHING, V3, P181; CANON J, 1993, TOXIC PHYTOPLANKTON, P103; CHAPMAN DV, 1982, J PHYCOL, V18, P121, DOI 10.1111/j.0022-3646.1982.00121.x; Collos Y, 2009, J SEA RES, V61, P68, DOI 10.1016/j.seares.2008.05.008; DALE B, 1978, SCIENCE, V201, P1223, DOI 10.1126/science.201.4362.1223; Dedieu K, 2007, ESTUAR COAST SHELF S, V72, P393, DOI 10.1016/j.ecss.2006.11.010; Denis L, 1996, CR ACAD SCI III-VIE, V319, P529; Fauchot J, 2005, J PHYCOL, V41, P263, DOI 10.1111/j.1529-8817.2005.03092.x; Fauchot J, 2008, HARMFUL ALGAE, V7, P214, DOI 10.1016/j.hal.2007.08.002; Figueroa RI, 2005, PHYCOLOGIA, V44, P658, DOI 10.2216/0031-8884(2005)44[658:EONFAD]2.0.CO;2; Genovesi B, 2007, HARMFUL ALGAE, V6, P837, DOI 10.1016/j.hal.2007.04.007; Genovesi B., 2008, Harmful Algae News, V37, P1; Genovesi-Giunti B, 2006, VIE MILIEU, V56, P327; Giacobbe MG, 1999, J PHYCOL, V35, P331, DOI 10.1046/j.1529-8817.1999.3520331.x; Grzebyk D, 2003, J PLANKTON RES, V25, P1185, DOI 10.1093/plankt/fbg088; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; HARRISON PJ, 1980, J PHYCOL, V16, P28, DOI 10.1111/j.1529-8817.1980.tb00724.x; Ishikawa A, 2007, HARMFUL ALGAE, V6, P301, DOI 10.1016/j.hal.2006.04.005; Itakura S, 2001, PHYCOLOGIA, V40, P263, DOI 10.2216/i0031-8884-40-3-263.1; Itakura S, 1997, MAR BIOL, V128, P497, DOI 10.1007/s002270050116; Joyce LB, 2006, AFR J MAR SCI, V28, P295, DOI 10.2989/18142320609504165; Kim YO, 2002, AQUAT MICROB ECOL, V29, P279, DOI 10.3354/ame029279; Kirn SL, 2005, DEEP-SEA RES PT II, V52, P2543, DOI 10.1016/j.dsr2.2005.06.009; Kremp A, 2001, MAR ECOL PROG SER, V216, P57, DOI 10.3354/meps216057; LAABIR M, 2004, P 12 INT C HARMF ALG, P26; LAANIA N, 2008, 13 INT C HARMF ALG 3; Lewis J, 1999, J PLANKTON RES, V21, P343, DOI 10.1093/plankt/21.2.343; Lilly EL, 2002, J PLANKTON RES, V24, P443, DOI 10.1093/plankt/24.5.443; LIRDWITAYAPRASIT T, 1990, J PHYCOL, V26, P299, DOI 10.1111/j.0022-3646.1990.00299.x; Masseret E, 2009, APPL ENVIRON MICROB, V75, P2037, DOI 10.1128/AEM.01686-08; Masson MarilynA., 2001, Lithic Technology, V26, P29; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; Metzger E, 2007, ESTUAR COAST SHELF S, V72, P406, DOI 10.1016/j.ecss.2006.11.011; MILLET B, 1992, LIMNOL OCEANOGR, V37, P140, DOI 10.4319/lo.1992.37.1.0140; Mizushima K, 2004, PHYCOL RES, V52, P408, DOI 10.1111/j.1440-183.2004.00358.x; 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; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Plante-Cuny MR, 1998, OCEANOL ACTA, V21, P819, DOI 10.1016/S0399-1784(99)80009-7; 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; Ståhl-Delbanco A, 2002, LIMNOL OCEANOGR, V47, P1836, DOI 10.4319/lo.2002.47.6.1836; TOURNIER H, 1982, REV TRAV I PECHES, V45, P283; TURPIN DH, 1978, J PHYCOL, V14, P235, DOI 10.1111/j.1529-8817.1978.tb02454.x; Wyatt T, 1997, J PLANKTON RES, V19, P551, DOI 10.1093/plankt/19.5.551; YOSHIMATSU S, 1984, Bulletin of Plankton Society of Japan, V31, P107; YOSHIMATSU S, 1981, Bulletin of Plankton Society of Japan, V28, P131	60	58	65	2	41	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	OCT	2009	31	10					1209	1224		10.1093/plankt/fbp066	http://dx.doi.org/10.1093/plankt/fbp066			16	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	500AQ					2025-03-11	WOS:000270269800008
J	Bison, KM; Versteegh, GJM; Orszag-Sperber, F; Rouchy, JM; Willems, H				Bison, Katarzyna-Maria; Versteegh, Gerard J. M.; Orszag-Sperber, Fabienne; Rouchy, Jean Marie; Willems, Helmut			Palaeoenvironmental changes of the early Pliocene (Zanclean) in the eastern Mediterranean Pissouri Basin (Cyprus) evidenced from calcareous dinoflagellate cyst assemblages	MARINE MICROPALEONTOLOGY			English	Article						Messinian Salinity Crisis; calcareous dinoflagellates; eastern Mediterranean; early Pliocene (Zanclean); Pissouri Basin (Cyprus)	MESSINIAN SALINITY CRISIS; SOUTH ATLANTIC-OCEAN; LATE MIOCENE CLIMATE; SURFACE SEDIMENTS; ISOTOPE COMPOSITION; POTENTIAL USE; EVOLUTION; SEA; DINOPHYCEAE; BOUNDARY	The first similar to 100 ka of the earliest Pliocene (Zanclean) sediments of the eastern Mediterranean Pissouri Basin on Cyprus have been investigated on calcareous dinoflagellate cyst assemblages. These assemblages reflect the return, in three phases, to the open oceanic conditions following the Messinian Salinity Crisis (MSC) 5.33 Ma ago. The lowermost phase (dominated by Leonella granifera cysts) indicates substantial land-derived nutrient supply and low salinities. This confirms earlier observations of enhanced continental water runoff during the earliest Pliocene in the eastern Mediterranean basin. The second phase (dominated by Caracomia stella and Calciodinellum albatrosianum cysts) indicates a change to warmer, meso- to oligotrophic waters. The third phase marks the first appearance and still continuing dominance of Thoracosphaera heimii in the region. In addition, the endemic eastern Mediterranean species, Lebessphaera urania, peaks within this upper interval. It probably survived the Salinity Crisis in the Mediterranean. The assemblage reflects the establishment of typical open marine, well stratified and oligotrophic surface conditions similar but not yet identical to the situation in the Mediterranean Sea today. This study points out a discrepancy between the fast refilling scenario (similar to 1-2 ka) in the Pissouri Basin and a long time (similar to 100 ka) environmental reorganisation in the surface waters as indicated by the calcareous dinoflagellate cysts. The onset of the Pliocene is also marked by the first appearance of Calciodinellum elongatum and Calciodinellum levantinum, which must have migrated from the Atlantic Ocean. (C) 2009 Elsevier B.V. All rights reserved.	[Bison, Katarzyna-Maria; Willems, Helmut] Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; [Versteegh, Gerard J. M.] Univ Bremen, MARUM Zentrum Marine Umweltwissensch, D-28334 Bremen, Germany; [Orszag-Sperber, Fabienne] Univ Paris 11, Dept Sci Terre, F-91405 Orsay, France; [Rouchy, Jean Marie] Museum Natl Hist Nat, F-75005 Paris, France	University of Bremen; University of Bremen; Universite Paris Saclay; Museum National d'Histoire Naturelle (MNHN)	Bison, KM (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330440, D-28334 Bremen, Germany.	kbison@uni-bremen.de	Versteegh, Gerard J.M./H-2119-2011	Versteegh, Gerard J.M./0000-0002-9320-3776	German Research Foundation [WI-725/19-1/2]	German Research Foundation(German Research Foundation (DFG))	The authors thank two anonymous reviewers for critical reading of the manuscript and for helpful suggestions. Financial support by the German Research Foundation (Project WI-725/19-1/2) is gratefully acknowledged.	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F., 2005, Palaeontologische Zeitschrift, V79, P61	91	6	7	0	9	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0377-8398	1872-6186		MAR MICROPALEONTOL	Mar. Micropaleontol.	OCT	2009	73	1-2					49	56		10.1016/j.marmicro.2009.06.008	http://dx.doi.org/10.1016/j.marmicro.2009.06.008			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	514BR					2025-03-11	WOS:000271369000005
J	Flores-Trujillo, JG; Helenes, J; Herguera, JC; Orellana-Cepeda, E				Flores-Trujillo, Juan G.; Helenes, Javier; Carlos Herguera, Juan; Orellana-Cepeda, Elizabeth			Palynological record (1483-1994) of <i>Gymnodinium catenatum</i> in Pescadero Basin, southern Gulf of California, Mexico	MARINE MICROPALEONTOLOGY			English	Article						Dinoflagellate cysts; Gymnodinium catenatum; Laminated sediments; Gulf of California; Sea surface temperature	SEA-SURFACE TEMPERATURE; SP-NOV DINOPHYCEAE; RED TIDE; DINOFLAGELLATE CYSTS; PACIFIC COAST; BAHIA CONCEPCION; SEDIMENTS; NORTH; VARIABILITY; GRAHAM	This paper presents the stratigraphic record of Gymnodinium catenatum during the last similar to 500 years, in Pescadero Basin. southern Gulf of California. Our aim is to help clarify the relation between abundances of cysts of G. catenatum and regional changes in the sea surface temperature and nutrient availability at a decadal scale. The record was obtained from core samples of laminated sediments dated with C-14, representing conditions in thearea from 1483 to 1967 (PCM99-74C-5) and from 1907 to 1994 (PCM00-61C-4). Samples were treated with normal palynological processing, without oxidation, and using Lycopodium spores for quantification. The palynological assemblages observed contain varied and abundant terrestrial and marine components. However, we focus on the abundance of G. catenatum, due to its toxicity and the resulting impact in the area. This species is currently common in the area, and according to our results has been present there since - 1483. Cysts of G. catenatum are generally abundant in the 20th century, with maximum concentrations observed from 1888 to 1920, and from 1945 to 1965, but they show a steady decrease in the latter part of the century (1965-1994). Before 1830, abundances of G. catenatum were low because of increased upwelling conditions, probably related to a higher variability of the winter sea surface temperatures in the area. Both our data in the 20th century and the actual reports in the area, indicate a close relation with sea surface temperature. From 1907 to 1994 cyst abundances seem to increase during cool La Nina conditions in the area, and decrease during warmer El Nino events. They also show an evident decrease in cyst abundance from 1970 to 1994, while the sea surface temperature in the area increased during the same period. This inverse relation is also indicated by the low abundances of G. catenatum observed during red tide events, combined with high sea surface temperatures in Mazatlan. Additionally, our results do not show any relation of G. catenatum blooms and anthropogenic activity in the area. (C) 2009 Elsevier B.V. All rights reserved.	[Flores-Trujillo, Juan G.] CICESE, Dept Geol, Mexico City, DF, Mexico; [Carlos Herguera, Juan] CICESE, Dept Ecol, Mexico City, DF, Mexico; [Orellana-Cepeda, Elizabeth] UABC, Dept Ecol, Mexico City, 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	Helenes, J (通讯作者)，Km 107 Carretera Tijuana Ensenada, Ensenada, Baja California, Mexico.	jflores@cicese.mx; jhelenes@cicese.mx; herguera@cicese.mx; orellana@uabc.mx	Helenes, Javier/J-5033-2016; Herguera, Juan Carlos/B-7812-2016	Helenes, Javier/0000-0002-0135-1879; Herguera, Juan Carlos/0000-0001-8335-2607	CONACYT; CICESE [33415-T]	CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT)); CICESE	The authors thank CONACYT and CICESE for their financial support to project 33415-T and to the first author J-G Flores-Trujillo throughout his Ph. D. studies. T Cavazos provided access to the rainfall database, N. Perez-Morga helped in the use of statistical software, and E. Collins helped in the processing of samples.	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Micropaleontol.	OCT	2009	73	1-2					80	89		10.1016/j.marmicro.2009.06.009	http://dx.doi.org/10.1016/j.marmicro.2009.06.009			10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	514BR					2025-03-11	WOS:000271369000009
J	Penaud, A; Eynaud, F; Turon, JL; Zaragosi, S; Malaizé, B; Toucanne, S; Bourillet, JF				Penaud, A.; Eynaud, F.; Turon, J. L.; Zaragosi, S.; Malaize, B.; Toucanne, S.; Bourillet, J. F.			What forced the collapse of European ice sheets during the last two glacial periods (150 ka BP and 18 ka cal BP)? Palynological evidence	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						Dinoflagellate cysts; European ice sheets; Celtic-Armorican margin; MIS 2 and MIS 6; Terminations I and II	DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; SEA-SURFACE CONDITIONS; ARMORICAN MARGIN BAY; HEINRICH EVENTS; PENULTIMATE DEGLACIATION; OVERTURNING CIRCULATION; CLIMATE VARIABILITY; ICEBERG DISCHARGES; ISOTOPE RECORDS	We present a new marine palynological record from the temperate North-eastern Atlantic (core MD03-2692, Celtic-Armorican margin) in the area of influence of the 'Fleuve Manche' paleoriver during glacial times. The runoff of this paleoriver was connected to the glacial history of European ice sheets (including the British Irish Ice Sheet-BIIS). Our study conducted on dinoflagellate cysts assemblages over the last 200 ka, associated with quantification of palynological remains reflecting continental influence (pre-Quaternary dinocysts and micro-algae Pediastrum spp. coenobia), yields detailed insights into the sea-surface paleoenvironments of this sector. More specifically, mechanisms responsible for the origin of unusual deposits of laminated sequences found at the end of Marine Isotope Stage (MIS) 2 and within mid-MIS 6 are here constrained. We provide evidence of genetic similarities between fluvial discharges occurring before and during times of deposition of the laminated deposits. Our study clarifies the causes of the collapse of European glaciated systems. At the end of MIS 2, prior to the deposition of the laminated deposits, plenioceanic influence characterized by high concentrations of Quaternary dinocysts prevailed, and a dinocyst species tracing the penetration of the warm North Atlantic Drift into the Bay of Biscay is recorded. However, this scenario did not recur prior to the deposition of laminated sediments of mid-MIS 6. In addition, contrary to the laminated deposits found at the end of MIS 2 and directly associated with Termination I, MIS 6 laminae appeared 20 ka earlier than Termination II. Our work shows that, during the penultimate glacial stage, the collapse of mid-latitudes ice sheets around 170 ka B.P. may have immediately followed the MIS 6.5 warming phase. Then, the most important melting event around 150 ka B.P. may be linked to a peak in insolation at 65 degrees N, though less important than those during MIS 6.5 and Termination II. (C) 2009 Elsevier B.V. All rights reserved.	[Penaud, A.; Eynaud, F.; Turon, J. L.; Zaragosi, S.; Malaize, B.; Toucanne, S.] Univ Bordeaux 1, CNRS, EPOC, UMR 5805, F-33405 Talence, France; [Bourillet, J. F.] IFREMER, Dept Geosci Marines, Lab Environm Sedimentaires, F-29280 Plouzane, France	Centre National de la Recherche Scientifique (CNRS); Universite de Bordeaux; CNRS - National Institute for Earth Sciences & Astronomy (INSU); Ifremer	Penaud, A (通讯作者)，Univ Bordeaux 1, CNRS, EPOC, UMR 5805, Ave Facultes, F-33405 Talence, France.	a.penaud@epoc.u-bordeaux1.fr	ZARAGOSI, Sébastien/JXL-2488-2024; Toucanne, Samuel/H-3437-2011; Bourillet, Jean-Francois/O-9761-2017; Penaud, Aurelie/F-2485-2011	Zaragosi, Sebastien/0000-0002-1456-8129; BOURILLET, Jean-Francois/0000-0002-6982-592X; Bruno, Malaize/0000-0002-5571-9990; Eynaud, Frederique/0000-0003-1283-7425; Toucanne, Samuel/0000-0002-4858-8953; Penaud, Aurelie/0000-0003-3578-4549				ALLEY RB, 1994, PALEOCEANOGRAPHY, V9, P503, DOI 10.1029/94PA01008; Auffret G, 2000, OCEANOL ACTA, V23, P109, DOI 10.1016/S0399-1784(00)00116-X; Ayalon A, 2002, GEOLOGY, V30, P303, DOI 10.1130/0091-7613(2002)030<0303:CCDMOI>2.0.CO;2; Ballantyne CK, 2008, QUATERNARY SCI REV, V27, P185, DOI 10.1016/j.quascirev.2007.10.019; Bard E, 2000, SCIENCE, V289, P1321, DOI 10.1126/science.289.5483.1321; Bard E, 2002, EARTH PLANET SC LETT, V202, P481, DOI 10.1016/S0012-821X(02)00788-4; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; BOND G, 1993, NATURE, V365, P143, DOI 10.1038/365143a0; BOND GC, 1995, SCIENCE, V267, P1005, DOI 10.1126/science.267.5200.1005; Bourillet JF, 2003, J QUATERNARY SCI, V18, P261, DOI 10.1002/jqs.757; BOURILLET JF, 2003, RAPPORTS CAMPAGNE ME; Broecker WS, 1990, PALEOCEANOGRAPHY, V5, P469, DOI 10.1029/PA005i004p00469; Buoncristiani JF, 2004, SEDIMENT GEOL, V165, P253, DOI 10.1016/j.sedgeo.2003.11.007; CHEDDADI R, 1995, PALEOCEANOGRAPHY, V10, P291, DOI 10.1029/94PA02672; *CLIMAP PROJ MEMB, 1981, GEOL SOC AM MAP CHAR, V56; Cottet-Puinel M, 2004, QUATERNARY SCI REV, V23, P449, DOI 10.1016/S0277-3791(03)00123-9; de Abreu L, 2003, MAR GEOL, V196, P1, DOI 10.1016/S0025-3227(03)00046-X; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; de Vernal A, 2006, QUATERNARY SCI REV, V25, P2820, DOI 10.1016/j.quascirev.2006.06.006; de Vernal A, 1999, CAHIERS GEOTOP, V3, P16; DUPLESSY JC, 1985, NATURE, V316, P500, DOI 10.1038/316500a0; Ehlers J., 2004, DEV QUATERNARY SCI, V2; Elliot M, 1998, PALEOCEANOGRAPHY, V13, P433, DOI 10.1029/98PA01792; Elliot M, 2001, EARTH PLANET SC LETT, V194, P151, DOI 10.1016/S0012-821X(01)00561-1; Esat TM, 1999, SCIENCE, V283, P197, DOI 10.1126/science.283.5399.197; Everest JD, 2006, GEOGR ANN A, V88A, P9, DOI 10.1111/j.0435-3676.2006.00279.x; Eynaud F, 2004, REV PALAEOBOT PALYNO, V128, P55, DOI 10.1016/S0034-6667(03)00112-X; Eynaud F, 2007, GEOCHEM GEOPHY GEOSY, V8, DOI 10.1029/2006GC001496; Eynaud F, 2000, MAR MICROPALEONTOL, V40, P9, DOI 10.1016/S0377-8398(99)00045-6; Eynaud F., 1999, KYSTES DINOFLAGELLES; Fensome R. 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OCT 1	2009	281	1-2					66	78		10.1016/j.palaeo.2009.07.012	http://dx.doi.org/10.1016/j.palaeo.2009.07.012			13	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	513YY		Green Published			2025-03-11	WOS:000271361400006
J	Naidina, OD				Naidina, O. D.			Environmental changes in the eastern shelf of the Laptev Sea in the late-glacial time	STRATIGRAPHY AND GEOLOGICAL CORRELATION			English	Article						Laptev Sea eastern shelf; Late Pleistocene; paleoenvironment; climate; pollen; organic-walled phytoplankton	ARCTIC-OCEAN; CLIMATE; SEDIMENTS	Data on the interaction of the land-sea system have been obtained based on complex palynological analysis (pollen and spores of terrestrial plants and cysts of dinoflagellates and green algae) and the SEM analysis of sediments from boreholes drilled on the Laptev Sea's eastern shelf and dated by the radiocarbon method. The spore and pollen ensemble revealed for the first time in late-glacial sediments of the boreholes indicates that warming which started within the time interval 15.6-10.7 ka ago was accompanied by short-term cooling events. Sedge and herb phytocoenosis predominated in the vegetation cover of East Arctic Siberia during the cooling. The climate warming favored the distribution of shrub birch tundra. The results of the analysis of organic-walled phytoplankton and the low value of the AH criterion indicate cold-water conditions with a longstanding ice sheet at sea. After the interval that ended 10.7 ka ago, thermophilic species of dinocysts appeared on the outer shelf, and the AH-criterion value increased, which suggests an active inflow of relatively warm North-Atlantic water to the shelf. Based on the comparison of the obtained results, an inference has been made about frequent changes of the climate in the region and the environment in the eastern part of the Laptev Sea during the deglaciation epoch.	Russian Acad Sci, Inst Geol, Moscow 119017, Russia	Geological Institute, Russian Academy of Sciences; Russian Academy of Sciences	Naidina, OD (通讯作者)，Russian Acad Sci, Inst Geol, Pyzhevskii 7, Moscow 119017, Russia.	naidina@ilran.ru			Otto Schmidt Russian-German Laboratory for Polar and Marine Research Fellowship Program	Otto Schmidt Russian-German Laboratory for Polar and Marine Research Fellowship Program	This work was supported by the Otto Schmidt Russian-German Laboratory for Polar and Marine Research Fellowship Program.	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N., 1999, Kriosfera Zemli, V3, P79; ROMANOVSKII NN, 2000, POLARFORSCHUNG, V68, P237; RUDDIMAN WF, 1981, PALAEOGEOGR PALAEOCL, V35, P145; RUDENKO OV, 2005, PALYNOLOGY THEORY PR, P223; RUDENKO OV, 2002, CLIMATE DRIVERS N, P95; SCHIRRMEISTER L, 2006, PROBLEM CORRELATION, P83; SERGEENKO AI, 2007, OTECHESTVENNAYA GEOL, V5, P35; SHEVCHENKO VP, 2004, ORGANIC CARBON CYCLE, P45; STRELETSKAYA ID, 2004, KRIOSFERA ZEMLI, V7, P53; Svendsen JI, 2004, QUATERNARY SCI REV, V23, P1229, DOI 10.1016/j.quascirev.2003.12.008; Velichko A.A., 1973, The Natural Process in Pleistocene, P256; VELICHKO AA, 2002, WAYS EVOLUTIONARY GE	56	2	2	0	4	PLEIADES PUBLISHING INC	MOSCOW	PLEIADES PUBLISHING INC, MOSCOW, 00000, RUSSIA	0869-5938	1555-6263		STRATIGR GEO CORREL+	Stratigr. Geol. Correl.	OCT	2009	17	5					544	557		10.1134/S0869593809050062	http://dx.doi.org/10.1134/S0869593809050062			14	Geology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Paleontology	504XL					2025-03-11	WOS:000270651300006
J	Li, YZ; He, RY; McGillicuddy, DJ; Anderson, DM; Keafer, BA				Li, Yizhen; He, Ruoying; McGillicuddy, Dennis J., Jr.; Anderson, Donald M.; Keafer, Bruce A.			Investigation of the 2006 <i>Alexandrium fundyense</i> bloom in the Gulf of Maine: In-situ observations and numerical modeling	CONTINENTAL SHELF RESEARCH			English	Article						Harmful algal bloom; Coastal circulation; Gulf of Maine; Bio-physical interaction	FLORIDA SHELF CIRCULATION; PHYSICAL-BIOLOGICAL MODEL; TEMPERATURE BUDGET; COASTAL CURRENT; WESTERN GULF; DINOFLAGELLATE; MECHANISMS; TRANSITION; SURFACE	In-situ observations and a coupled bio-physical model were used to study the germination, initiation, and development of the Gulf of Maine (GOM) Alexandrium fundyense bloom in 2006 Hydrographic measurements and comparisons with GOM climatology indicate that 2006 was a year with normal coastal water temperature. salinity. current and river runoff conditions. A. fundyense cyst abundance in bottom sediments preceding the 2006 bloom was at a moderate level compared to other recent annual cyst survey data We used the coupled bio-physical model to hindcast coastal circulation and A fundyense cell concentrations. Field data including water temperature. salinity, velocity time series and Surface A fundyense cell concentration maps were applied to gauge the model's fidelity The coupled model is capable of reproducing the hydrodynamics and the temporal and spatial distributions of A fundyense cell concentration reasonably well. Model hindcast solutions were further used to diagnose physical and biological factors controlling the bloom dynamics Surface wind fields modulated the bloom's horizontal and vertical distribution. The initial cyst distribution was found to be the dominant factor affecting the severity and the interannual variability of the A. fundyense bloom Initial cyst abundance for the 2006 bloom was about 50% of that prior to the 2005 bloom As the result, the time-averaged gulf-wide cell concentration in 2006 was also only about 60% of that in 2005 In addition, weaker alongshore currents and episodic upwelling-favorable winds in 2006 reduced the spatial extent of the bloom as compared with 2005. (C) 2009 Elsevier Ltd All rights reserved	[Li, Yizhen; He, Ruoying] N Carolina State Univ, Dept Maine Earth & Atmospher Sci, Raleigh, NC 27695 USA; [McGillicuddy, Dennis J., Jr.] Woods Hole Oceanog Inst, Dept Appl Ocean Phys & Engn, Woods Hole, MA USA; [Anderson, Donald M.; Keafer, Bruce A.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA USA	North Carolina State University; Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution	He, RY (通讯作者)，N Carolina State Univ, Dept Maine Earth & Atmospher Sci, 2800 Faucette Dr, Raleigh, NC 27695 USA.		He, Ruoying/C-5598-2015; Li, Yizhen/O-3869-2015	He, Ruoying/0000-0001-6158-2292; McGillicuddy, Dennis/0000-0002-1437-2425; Li, Yizhen/0000-0001-6565-1339	NOAA [NA06NOS4780245]; NSF [OCE-0430724, DMS-0417769]; NIEHS [1P50-ES01274201]; ECOHAB [NA04-NOS4780274]; Directorate For Geosciences; Division Of Ocean Sciences [0911031] Funding Source: National Science Foundation	NOAA(National Oceanic Atmospheric Admin (NOAA) - USA); NSF(National Science Foundation (NSF)); NIEHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); ECOHAB; Directorate For Geosciences; Division Of Ocean Sciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	The authors thank technical and logistical support provided by K. Norton, O. Kosnyreva, V. Kosnyreva, K. Smith, J. Manning and L. Anderson. Thanks to the captain, crews and Support personnel of the R/V Oceanus S. Libby. M. Mickelson, and others associated with the Massachusetts Water Resources Authority monitoring program for Massachusetts Bay provided many valuable observations and helpful discussions. We thank Dr. B. Petrie for providing the Gulf of Maine nutrient climatology used in the simulations. Thanks also to NOAA NCEP, LISGS, and GoMOOS for providing data products online. Research support was provided by the GOMTOX program through NOAA Grant NA06NOS4780245. DJM and DMA were also supported by NSF Grants OCE-0430724, DMS-0417769 and NIEHS Grant 1P50-ES01274201 (Woods Hole Center for Oceans and Human Health). Cyst abundance data is provided through the ECOHAB grant NOAA ECOHAB Grant NA04-NOS4780274 to DMA. This is ECOHAB contribution number 311.	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Shelf Res.	SEP 30	2009	29	17					2069	2082		10.1016/j.csr.2009.07.012	http://dx.doi.org/10.1016/j.csr.2009.07.012			14	Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Oceanography	518LQ	28979059	Green Accepted			2025-03-11	WOS:000271694200002
J	Warnaar, J; Bijl, PK; Huber, M; Sloan, L; Brinkhuis, H; Röhl, U; Sriver, R; Visscher, H				Warnaar, Jeroen; Bijl, Peter K.; Huber, Matthew; Sloan, Lisa; Brinkhuis, Henk; Roehl, Ursula; Sriver, Ryan; Visscher, Henk			Orbitally forced climate changes in the Tasman sector during the Middle Eocene	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Southern Ocean; Middle Eocene; Orbital forcing; Model-data comparison; Organic-walled dinoflagellate cysts; General circulation model	CARBON-DIOXIDE CONCENTRATIONS; ICE-SHEET; GREENHOUSE; INDICATORS; SEDIMENTS; RESPONSES; PACIFIC; MIOCENE; FLORAS; CYSTS	The influence of orbital precession on early Paleogene climate and ocean circulation patterns in the southeast Pacific region is investigated by combining environmental analyses of cyclic Middle Eocene sediments and palynomorph records recovered from ODP Hole 1172A on the East Tasman Plateau with climate model simulations. Integration of results indicates that in the marine realm, direct effects of precessional forcing are not pronounced, although increased precipitation/runoff could have enhanced dinoflagellate cyst production. On the southeast Australian continent, the most pronounced effects of precessional forcing were fluctuations in summer precipitation and temperature on the Antarctic Margin. These fluctuations resulted in vegetational changes, most notably in the distribution of Nothofagus (subgenus Brassospora). The climate model results suggest significant fluctuations in sea ice in the Ross Sea, notably during Austral summers. This is consistent with the influx of Antarctic heterotrophic dinoflagellates in the early part of the studied record. The data demonstrate a strong precessionally driven climate variability and thus support the concept that precessional forcing could have played a role in early Antarctic glaciation via changes in runoff and/or precipitation. (c) 2009 Elsevier B.V. All rights reserved.	[Warnaar, Jeroen; Bijl, Peter K.; Brinkhuis, Henk; Visscher, Henk] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Huber, Matthew; Sriver, Ryan] Purdue Univ, W Lafayette, IN 47907 USA; [Sloan, Lisa] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95064 USA; [Roehl, Ursula] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany	Utrecht University; Purdue University System; Purdue University; University of California System; University of California Santa Cruz; University of Bremen	Bijl, PK (通讯作者)，Univ Utrecht, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	p.k.bijl@uu.nl; huberm@purdue.edu; lsloan@es.ucsc.edu; uroehl@marum.de	Brinkhuis, Henk/B-4223-2009; Rohl, Ursula/G-5986-2011; Huber, Matthew/A-7677-2008	Rohl, Ursula/0000-0001-9469-7053; Huber, Matthew/0000-0002-2771-9977; Visscher, Henk/0000-0002-9276-0220; Brinkhuis, Henk/0000-0003-0253-6610; Bijl, Peter/0000-0002-1710-4012	U.S. National Science Foundation (NSF); Oceanographic Institutions (JOI) Inc; Netherlands Council for Earth and Life Sciences; Deutsche Forschungsgemeinschaft (DFG)	U.S. National Science Foundation (NSF)(National Science Foundation (NSF)); Oceanographic Institutions (JOI) Inc; Netherlands Council for Earth and Life Sciences; Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	This research used samples provided by the Ocean Drilling Program (ODP). ODP was sponsored by the U.S. National Science Foundation (NSF) and participating countries under management of joint Oceanographic Institutions (JOI) Inc. Funding for this research was provided by the Netherlands Council for Earth and Life Sciences (ALW-NWO) to JW and the Deutsche Forschungsgemeinschaft (DFG) to U. Rohll. We are particularly grateful to the lab technicians Natasja Welters and Jan van Tongeren at the Laboratory of palaeobotany and palynology of Utrecht University for their help with processing the palynological samples. We kindly acknowledge John Cann and an anonymous reviewer for the constructive criticism and suggestions.	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Paleoclimatol. Paleoecol.	SEP 15	2009	280	3-4					361	370		10.1016/j.palaeo.2009.06.023	http://dx.doi.org/10.1016/j.palaeo.2009.06.023			10	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	496QQ					2025-03-11	WOS:000269990700007
J	Servais, T; Munnecke, A; Versteegh, GJM				Servais, Thomas; Munnecke, Axel; Versteegh, Gerard J. M.			Silurian calcispheres (Calcitarcha) of Gotland (Sweden): Comparisons with calcareous dinoflagellates	COMPTES RENDUS PALEVOL			English	Article						Calcitarcha; Calcispheres; Calcareous dinoflagellates; Silurian; Gotland	MOLECULAR EVIDENCE; MICROFOSSILS; CLASSIFICATION; LIMESTONES; PHYLOGENY	Scanning electron microscope examinations of polished and etched surfaces of sediments from the Silurian carbonate platform of Gotland, Sweden, revealed the presence of numerous, morphologically diverse "calcispheres" (Calcitarcha). Some of these spherical calcareous microfossils display wall structures that are surprisingly similar to those of calcareous dinoflagellate cysts. In analogy to the interpretation of the biological affinities of Palaeozoic acritarchs as cysts of organisms that might have been the ancestors of organic-walled dinoflagellates, the Calcitarcha from Gotland can be compared and may possibly be related to organisms that may have been the ancestors of calcareous cyst-producing dinoflagellates that so far have not been observed before the Late Jurassic. To cite this article: T. Servais et al., C. R. Palevol 8 (2009). (C) 2009 Academie des sciences. Published by Elsevier Masson SAS. All rights reserved.	[Servais, Thomas; Versteegh, Gerard J. M.] Univ Lille 1, CNRS Geosyst, UMR 8157, F-59655 Villeneuve Dascq, France; [Servais, Thomas; Munnecke, Axel] Univ Erlangen Nurnberg, GeoZentrum Nordbayern, Fachgrp Palaoumwelt, D-91054 Erlangen, Germany; [Versteegh, Gerard J. M.] Univ Bremen, MARUM, D-28359 Bremen, Germany	Universite de Lille; University of Erlangen Nuremberg; University of Bremen	Servais, T (通讯作者)，Univ Lille 1, CNRS Geosyst, UMR 8157, Cite Sci,Batiment SN5, F-59655 Villeneuve Dascq, France.	thomas.servais@univ-lille1.fr; axel.munnecke@gzn.uni-erlangen.de; versteegh@uni-bremen.de	Servais, Thomas/S-8045-2019; Munnecke, Axel/G-3698-2010; Versteegh, Gerard J.M./H-2119-2011; Servais, Thomas/I-2115-2018	Versteegh, Gerard J.M./0000-0002-9320-3776; Munnecke, Axel/0000-0002-6898-1082; Servais, Thomas/0000-0002-4089-7874	Deutsche Forschungsgemeinschaft (DFG) [Scha 355/8]	Deutsche Forschungsgemeinschaft (DFG)(German Research Foundation (DFG))	We are grateful to a number of colleagues who discussed with us calcareous dinoflagellate morphology: Tania Hildebrandt-Habel (University of Oslo), Michael Streng (University of Uppsala), Jens Wendler and Karin Zonneveld (Universitat Bremen). We thank Daniel Vachard (Villeneuve d'Ascq) for information and literature about calcispheres and Reed Wicander (Mount Pleasant, MI) for discussing with us an earlier version of the manuscript. Frank Chanier (USTL) is acknowledged for providing Cretaceous samples with calcareous dinoflagellates from New Zealand. We are grateful to the two reviewers (of which one remained anonymous) and in particular to Rob Fensome (Dartmouth, Nova Scotia) for his very detailed review of the manuscript and the numerous suggestions that improved the final version. TS benefited from support of the Alexander von Humboldt-Foundation (Bonn, Germany). The study was supported by the Deutsche Forschungsgemeinschaft (DFG grant Scha 355/8). GJMV benefited from a position as invited professor at the USTL (Lille). This paper is a contribution to IGCP project n degrees 503 "Ordovician Palaeogeography and Palaeoclimate".	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R. Palevol	SEP	2009	8	6					527	534		10.1016/j.crpv.2009.04.002	http://dx.doi.org/10.1016/j.crpv.2009.04.002			8	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	491SK					2025-03-11	WOS:000269599600002
J	Murik, O; Kaplan, A				Murik, Omer; Kaplan, Aaron			Paradoxically, prior acquisition of antioxidant activity enhances oxidative stress-induced cell death	ENVIRONMENTAL MICROBIOLOGY			English	Article							CHLAMYDOMONAS-REINHARDTII; ASCORBATE PEROXIDASE; PERIDINIUM-GATUNENSE; ARABIDOPSIS-THALIANA; GENE-EXPRESSION; PLANTS; DINOFLAGELLATE; PHOTOSYNTHESIS; METACASPASES; METABOLISM	P>Oxidative stress has been implicated in the induction of programmed cell death in a wide variety of organisms. Acquiring antioxidant capacity is thought to enhance the viability of cells challenged by a subsequent oxidative stress. Counter-intuitively, we show that in two phytoplankton species, Chlamydomonas reinhardtii and Peridinium gatunense, representing the green and red plastid lineages, oxidative stress induced cell death in cultures that already possessed high antioxidant activity but not in cells that exhibited low activity. Cell death of low antioxidant possessing cultures was markedly enhanced by the addition of dehydroascorbate, a product of ascorbate peroxidase (APX), but not of ascorbate or reduced glutathione, and was preceded by increased metacaspase expression and activity. These data suggested that the level of APX and its products, strongly upregulated by oxidative stress, serves as a possible surveillance signal, reporting that the cells already experienced an earlier oxidative stress. Our data presents a novel role of APX in antioxidant activity and response to oxidative stress in photosynthetic microorganisms. Elimination of cysts production by phytoplankton cells that were already damaged by oxidative stress (indicated by the rise in oxidized proteins) as the inoculum for the following year's population may be the evolutionary trigger for this phenomenon.	[Murik, Omer; Kaplan, Aaron] Hebrew Univ Jerusalem, Dept Plant & Environm Sci, IL-91904 Jerusalem, Israel	Hebrew University of Jerusalem	Kaplan, A (通讯作者)，Hebrew Univ Jerusalem, Dept Plant & Environm Sci, IL-91904 Jerusalem, Israel.	aaronka@vms.huji.ac.il	Murik, Omer/O-7894-2019; Kaplan, Aaron/GLN-5655-2022	Kaplan, Aaron/0000-0002-0815-5731	Israeli Science Foundation (ISF); German-Israeli Science Foundation (GIF)	Israeli Science Foundation (ISF)(Israel Science Foundation); German-Israeli Science Foundation (GIF)(German-Israeli Foundation for Scientific Research and Development)	We thank Dr Arthur Grossman, Carnegie Institution Stanford, for making the Chlamydomonas microarray accessible for this study and for many helpful discussions. This study was supported by the Israeli Science Foundation (ISF) and the German-Israeli Science Foundation (GIF).	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Microbiol.	SEP	2009	11	9					2301	2309		10.1111/j.1462-2920.2009.01957.x	http://dx.doi.org/10.1111/j.1462-2920.2009.01957.x			9	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	490WV	19508337				2025-03-11	WOS:000269539700012
J	Pearce, MA; Jarvis, I; Tocher, BA				Pearce, Martin A.; Jarvis, Ian; Tocher, Bruce A.			The Cenomanian-Turonian boundary event, OAE2 and palaeoenvironmental change in epicontinental seas: New insights from the dinocyst and geochemical records	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Review						Cenomanian; Turonian; Chalk; Dinoflagellate cysts; Chemostratigraphy; OAE2; Anoxia	OCEANIC ANOXIC EVENT; CARBON-ISOTOPE STRATIGRAPHY; CALCAREOUS DINOFLAGELLATE CYSTS; GLASSY FORAMINIFERAL CALCITE; ORBITAL TIME-SCALE; ORGANIC-CARBON; WESTERN INTERIOR; LEVEL CHANGES; MG/CA RATIO; PLANKTONIC-FORAMINIFERA	Organic-walled dinoflagellate cyst (dinocyst) and geochemical records across the Cenomanian-Turonian boundary (CTB) are presented for the NW European reference section at Eastbourne, England. Dinocyst and nannofossil fertility indexes indicate that an upwelling-driven productivity pulse accompanied a eustatic sea-level fall that preceded, by at least 40 kyr, the global rise in delta C-13 values that marks the onset of Oceanic Anoxic Event 2 (OAE2) and the deposition of black shales in the deep ocean. A marine productivity collapse in the latest Cenomanian is evidenced by the falling absolute and relative abundance of peridinioid dinocysts, believed to be the product of heterotrophic dinoflagellates. This biotic change accompanied transgression and sharply rising sea-surface temperatures, following an Atlantic-wide episode of short-lived cooling. Geochemical tracers provide evidence of Caribbean-Colombian plateau volcanism. The increase in water depth caused by the latest Cenomanian transgression resulted in less eutrophic waters in epicontinental seas, where CTB biotic turnover was driven largely by water-mass changes rather than oxygen depletion. The species richness/absolute abundance ratio of dinocysts is proposed as a water-mass stability proxy. (C) 2009 Elsevier B.V. All rights reserved.	[Jarvis, Ian] Kingston Univ London, Sch Geog Geol & Environm, Ctr Earth & Environm Sci Res, Kingston upon Thames KT1 2EE, Surrey, England; [Pearce, Martin A.; Tocher, Bruce A.] StatoilHydro, N-5254 Bergen, Norway	Kingston University; Equinor	Jarvis, I (通讯作者)，Kingston Univ London, Sch Geog Geol & Environm, Ctr Earth & Environm Sci Res, Penrhyn Rd, Kingston upon Thames KT1 2EE, Surrey, England.	i.jarvis@kingston.ac.uk	Jarvis, Ian/A-1637-2008	Jarvis, Ian/0000-0003-3184-3097; Pearce, Martin/0000-0001-7856-1076	Kingston University London (UK); StatoilHydro (Norway)	Kingston University London (UK); StatoilHydro (Norway)	Our thanks to Henk Brinkhuis and Poul Schioler for critical reviews that improved an earlier draft of the manuscript. Funding for this work from Kingston University London (UK) and StatoilHydro (Norway) is gratefully acknowledged. Chris Paul supplied carbon and oxygen isotope data for the Gun Gardens section; new isotope data were provided by Greg Carson. Catherine Stickley (University of Tromso) assisted with sampling in the field.	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J	Moestrup, O; Lindberg, K; Daugbjerg, N				Moestrup, Ojvind; Lindberg, Karin; Daugbjerg, Niels			Studies on woloszynskioid dinoflagellates IV: The genus <i>Biecheleria</i> gen. nov.	PHYCOLOGICAL RESEARCH			English	Article						Baldinia; Biecheleria; Borghiella; Borghiellaceae; freshwater dinoflagellates; molecular phylogeny; ultrastructure	LAKE TOVEL; COMB. NOV; ULTRASTRUCTURE; DINOPHYCEAE; PHYLOGENY	P>The well known freshwater dinoflagellate Woloszynskia pseudopalustris is transferred to the new genus Biecheleria, based on the very unusual structure of the eyespot (comprising a stack of cisternae), the apical apparatus of a single elongate amphiesma vesicle, the structure of the resting cyst, and molecular data. Biecheleria is phylogenetically related to Symbiodinium and Polarella of the family Suessiaceae. This family, which extends back to the Jurassic, is redefined with the eyespot (Type E sensu Moestrup and Daugbjerg) and apical apparatus as diagnostic features, unknown elsewhere in the dinoflagellates. Biecheleria also comprises the brackish water species Biecheleria baltica sp. nov. (presently identified as Woloszynskia halophila) and the marine species Biecheleria natalensis (syn. Gymnodinium natalense). Gymnodinium halophilum described in 1952 by B. Biecheler but apparently not subsequently refound, is transferred to Biecheleria. The Suessiaceae further includes the marine species Protodinium simplex, described by Lohmann in 1908 but shortly afterwards (1921) transferred to Gymnodinium by Kofoid and Swezy and subsequently known as Gymnodinium simplex. It only distantly related to Gymnodinium. A new family, the Borghiellaceae, is proposed for the sister group to the Suessiaceae, based on eyespot structure (Type B of Moestrup and Daugbjerg), the morphology of the apical apparatus (if present), and molecular data. It presently comprises the genera Baldinia and Borghiella. Cells of Biecheleria pseudopalustris and B. baltica contain a microtubular strand (msp) associated with vesicles containing opaque material. Such structures are known in other dinoflagellates to serve as a peduncle, indicating that the two species may be mixotrophic.	[Moestrup, Ojvind; Lindberg, Karin; Daugbjerg, Niels] Univ Copenhagen, Phycol Lab, Inst Biol, DK-1353 Copenhagen K, Denmark	University of Copenhagen	Moestrup, O (通讯作者)，Univ Copenhagen, Phycol Lab, Inst Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	moestrup@bio.ku.dk	Daugbjerg, Niels/D-3521-2014	Daugbjerg, Niels/0000-0002-0397-3073; Moestrup, Ojvind/0000-0003-0965-8645	Villum Kann Rasmussen Foundation	Villum Kann Rasmussen Foundation(Villum Fonden)	We thank A. Calado for figures 6 and 7, Lisbeth Haukrogh and Lis Munk Frederiksen for assisting with sectioning of the material for TEM, and Kirsten Olrik for providing information about Lake Vejlese. Mona Hoppenrath and Marina Montresor provided very constructive comments on the manuscript. Christian Hogel kindly assisted with the Latin diagnoses. This article is part of the project 'Biodiversity and phylogeny of dinoflagellates' supported by the Villum Kann Rasmussen Foundation.	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J	Moestrup, O; Lindberg, K; Daugbjerg, N				Moestrup, Ojvind; Lindberg, Karin; Daugbjerg, Niels			Studies on woloszynskioid dinoflagellates V. Ultrastructure of <i>Biecheleriopsis</i> gen. nov., with description of <i>Biecheleriopsis adriatica</i> sp nov.	PHYCOLOGICAL RESEARCH			English	Article						dinoflagellates; phylogeny; phytoplankton; taxonomy; ultrastructure; woloszynskioids	FLAGELLAR APPARATUS; LAKE TOVEL; COMB. NOV; DINOPHYCEAE; PHYLOGENY; POLYKRIKOS; LIGHT	P>An isolate of the very small marine dinoflagellate Biecheleriopsis adriatica gen. et sp. nov. (12-15 mu m long) has been examined by light, scanning and transmission electron microscopy, combined with partial sequencing of nuclear-encoded large subunit rRNA. Biecheleriopsis is a genus of thin-walled dinoflagellates, related to Biecheleria and the taxonomic group of Polarella, Protodinium and Symbiodinium, the latter comprising mainly symbionts of marine invertebrates. The mixotrophic Biecheleriopsis adriatica is characterized by: (i) a special type of apical furrow apparatus; (ii) an eyespot of Type E sensu Moestrup and Daugbjerg; (iii) an unusual type of pyrenoid; and (iv) a spiny resting cyst. Thin sections showed the presence a fibrous connection between the flagellar apparatus and a finger-like extension of the nucleus ('rhizoplast'). It forms a physical connection between the flagella and the nucleus. This unusual structure has previously been considered to characterize the 'true' gymnodinioids, represented by Gymnodinium sensu Daugbjerg et al. and related forms. However, the apical furrow apparatus and the nuclear envelope of Biecheleriopsis are woloszynskioid rather than gymnodinioid. The related genus Biecheleria lacks a rhizoplast, and it also lacks a 51-base pair fragment of domain D2 of the large subunit rRNA, which is present in other woloszynskioids. A physical connection between the flagellar apparatus and the nucleus mediated by a fibrous structure is known in other groups of protists, for example, the 'rhizoplast' of many heterokont flagellates, some green algal flagellates, etc. The phylogenetic significance of a rhizoplast in two groups of dinoflagellates that are only distantly related is presently difficult to assess.	[Moestrup, Ojvind; Lindberg, Karin; Daugbjerg, Niels] Univ Copenhagen, Phycol Lab, Inst Biol, DK-1353 Copenhagen K, Denmark	University of Copenhagen	Moestrup, O (通讯作者)，Univ Copenhagen, Phycol Lab, Inst Biol, Oster Farimagsgade 2D, DK-1353 Copenhagen K, Denmark.	moestrup@bio.ku.dk	Daugbjerg, Niels/D-3521-2014	Daugbjerg, Niels/0000-0002-0397-3073	Villum Kann Rasmussen Foundation	Villum Kann Rasmussen Foundation(Villum Fonden)	We thank Patrick Gentien and Evelyne Erard-Le Denn for supplying the strain of Biecheleriopsis adriatica from IFREMER, and Lisbeth Haukrogh for assisting with sectioning of the material for TEM. ND thanks Charlotte Hansen for help with the automated sequencing. We thank Stuart Sym for translating the diagnosis into Latin. This article is part of the project 'Biodiversity and phylogeny of dinoflagellates' supported financially by Villum Kann Rasmussen Foundation.	[Anonymous], 2004, Modeltest v2; Biecheler B., 1952, Bull. Biol. Fr. 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J	Moczydlowska, M; Willman, S				Moczydlowska, Malgorzata; Willman, Sebastian			Ultrastructure of cell walls in ancient microfossils as a proxy to their biological affinities	PRECAMBRIAN RESEARCH			English	Review						Ultrastructure; Cell wall; Acritarcha; Microfossils; Affinities; Ediacaran	OFFICER-BASIN; ACANTHOMORPHIC ACRITARCHS; EDIACARAN MICROBIOTA; MOLECULAR FOSSILS; WESTERN-AUSTRALIA; PILBARA CRATON; ANIMAL EMBRYOS; BILLION YEARS; OUTER WALLS; RESISTANT	Bacteria and protoctists dominated the biosphere in the Archean and Proterozoic, their affinities being deduced by studies of their comparative morphology, palaeoecology, biogeochemistry, and wall ultrastructure. However, exact phylogenetic relationships are uncertain for most such microfossils. Because of the limitations imposed by the simple morphology and small dimensions of such microorganisms and their little known biochemistry, new techniques in microscopy, tomography and spectroscopy are applied to examine individual microfossils at the highest attainable spatial resolution. TEM/SEM studies of the wall ultrastructure of sphaero- and acanthomorphic acritarchs have revealed complex, single to multilayered walls, having a unique texture in sub-layers and an occasionally preserved trilaminar sheath structure (TLS) of the external layer. A variety of optical characteristics, the electron density and texture of fabrics of discrete layers, and the properties of biopolymers may indicate the polyphyletic affiliations of such microfossils and/or the preservation of various stages (vegetative, resting) in their life cycle. Primarily, wall ultrastructure allows discrimination between fossilized prokaryotic and eukaryotic cells. Composite wall ultrastructure provides evidence that some Proterozoic and Cambrian leiosphaerids are of algal affinities (but not, per se, that they are referable to "Leiosphaeridia"). Certain Cambrian specimens represent chlorophyceaens, having the multilayered composite wall with TLS structure known from vegetative and resting cells in modern genera of the Chlorococcales and Volvocales. The wall ultrastructure of the studied Cambrian and Proterozoic acanthomorphs resembles the resting cysts of green microalgae, but there is no evidence to suggest a close relationship of these taxa, to dinoflagellates. It is apparent that although there is no single and direct method to recognize the precise phylogenetic relations of such microfossils, ultrastructural studies of their preserved cell walls and encompassing sheaths, combined with biochemical analyses and other advanced methods, may further elucidate their affinities to the modern biota. (C) 2009 Elsevier B.V. All rights reserved.	[Moczydlowska, Malgorzata; Willman, Sebastian] Uppsala Univ, Dept Earth Sci, SE-75236 Uppsala, Sweden	Uppsala University	Moczydlowska, M (通讯作者)，Uppsala Univ, Dept Earth Sci, Villavagen 16, SE-75236 Uppsala, Sweden.	Malgo.Vidal@pal.uu.se	Willman, Sebastian/IUP-9870-2023	Willman, Sebastian/0000-0002-1434-7131	Swedish Research Council (VR) [621-2004-5316]	Swedish Research Council (VR)(Swedish Research Council)	We acknowledge funding by the Swedish Research Council (VR) through research grant no. 621-2004-5316 to M. Moczydlowska. This contribution has been inspired by Bill Schopf, the Organizer of the World Summit on Ancient Microscopic Fossils, 2008 at University of California, Los Angeles, who also provided excellent facilities for the meeting and stimulated many discussions among colleagues. Caroline van Mourik kindly donated the dinocyst specimens for the studies, which are continued as a part of our collaborative project.	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SEP	2009	173	1-4			SI		27	38		10.1016/j.precamres.2009.02.006	http://dx.doi.org/10.1016/j.precamres.2009.02.006			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	487SY					2025-03-11	WOS:000269297400005
J	Bouimetarhan, I; Dupont, L; Schefuss, E; Mollenhauer, G; Mulitza, S; Zonneveld, K				Bouimetarhan, Ilham; Dupont, Lydie; Schefuss, Enno; Mollenhauer, Gesine; Mulitza, Stefan; Zonneveld, Karin			Palynological evidence for climatic and oceanic variability off NW Africa during the late Holocene	QUATERNARY RESEARCH			English	Article						Palaeoceanography; Palaeoenvironment; Pollen; Organic-walled dinoflagellate cyst; Senegal River; Mud-belt	WALLED DINOFLAGELLATE CYSTS; MARINE-SEDIMENTS; DISTRIBUTION PATTERNS; SURFACE SEDIMENTS; CANARY-ISLANDS; WEST-AFRICA; POLLEN; VEGETATION; PRESERVATION; CIRCULATION	Pollen and organic-walled dinoflagellate cyst assemblages from core GeoB 9503-5 retrieved from the mud-belt (similar to 50 m water depth) off the Senegal River mouth have been analyzed to reconstruct short-term palaeoceanographic and palaeoenvironmental changes in subtropical NW Africa during the time interval from ca. 4200 to 1200 cal yr BP. Our study emphasizes significant coeval changes in continental and oceanic environments in and off Senegal and shows that initial dry conditions were followed by a strong and rapid increase in humidity between ca. 2900 and 2500 cal yr BP. After ca. 2500 cal yr BP, the environment slowly became drier again as indicated by slight increases in Sahelian savannah and desert elements in the pollen record. Around ca. 2200 cal yr BP, this relatively dry period ended with periodic pulses of high terrigenous contributions and strong fluctuations in fern spore and river plume dinoflagellate cyst percentages as well as in the fluxes of pollen, dinoflagellate cysts, fresh-water algae and plant cuticles, suggesting "episodic flash flood" events of the Senegal River. The driest phase developed after about 2100 cal yr BR (C) 2009 University of Washington. Published by Elsevier Inc. All rights reserved.	[Bouimetarhan, Ilham; Mollenhauer, Gesine; Zonneveld, Karin] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Bouimetarhan, Ilham; Dupont, Lydie; Schefuss, Enno; Mulitza, Stefan; Zonneveld, Karin] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany; [Mollenhauer, Gesine] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany	University of Bremen; University of Bremen; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Bouimetarhan, I (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28359 Bremen, Germany.	bouimetarhan@uni-bremen.de	Bouimetarhan, Ilham/D-2388-2011; Mollenhauer, Gesine/AAD-8167-2019; Mollenhauer, Gesine/B-5190-2015; Schefuss, Enno/A-7101-2015; Mulitza, Stefan/G-5357-2011	Bouimetarhan, Ilham/0000-0003-3369-3811; Mollenhauer, Gesine/0000-0001-5138-564X; Dupont, Lydie/0000-0001-9531-6793; Schefuss, Enno/0000-0002-5960-930X; Mulitza, Stefan/0000-0002-3842-1447	Deutsche Forschungsgemeinschaft	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	This work was funded through the Deutsche Forschungsgemeinschaft as part of the DFG-Research Center/Excellence cluster "The Ocean in the Earth System" (MARUM) at the University of Bremen. Thanks to the captain and crew of the R/V Meteor for the logistic and technical assistance. Thanks to M. Segl for help with isotope analyses and to S. Forke for his assistance with palynological processing. The manuscript benefitted from helpful comments by M. Kolling and J. Groeneveld. Thanks to Jean-Pierre Cazet for helping with the fresh water algae determination and Anne-Marie Lezine for valuable discussion. We express our gratitude to Fabienne Marret, Sander van der Kaars, and Editor Wyatt Oswald, for constructive comments and for detailed reviews of an earlier version of this manuscript.	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Res.	SEP	2009	72	2					188	197		10.1016/j.yqres.2009.05.003	http://dx.doi.org/10.1016/j.yqres.2009.05.003			10	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology	486UA					2025-03-11	WOS:000269223500004
J	Thorn, VC; Riding, JB; Francis, JE				Thorn, Vanessa C.; Riding, James B.; Francis, Jane E.			The Late Cretaceous dinoflagellate cyst <i>Manumiella</i> - Biostratigraphy, systematics, and palaeoecological signals in Antarctica	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Late Cretaceous; Maastrichtian; dinoflagellate cysts; Manumiella; Seymour Island; Antarctic Peninsula	LOPEZ-DE-BERTODANO; SEA-LEVEL CHANGES; SEYMOUR-ISLAND; TERTIARY BOUNDARY; CAPE LAMB; STRATIGRAPHY; SEDIMENTOLOGY; MARLBOROUGH; PALYNOLOGY; CHRONOLOGY	This study of the Maastrichtian (latest Cretaceous, 71-65 Ma) species of Manumiella Bujak and Davies 1983 in the James Ross Basin, Antarctic Peninsula is focussed on the biostratigraphical and palaeoecological significance of this peridinioid dinoflagellate cyst genus, in particular with reference to oceanic changes associated with the Cretaceous/Tertiary (KT) boundary. New palynological analyses throughout the upper part of the latest Maastrichtian Lopez de Bertodano Formation on Seymour Island has resulted in the emendation of Manumiella to include the presence of a mesophragm, and the formal description of Manumiella bertodano sp. nov. A morphological continuum exists between species of Manumiella, but the apparent biostratigraphical significance of the end-member morphologies emphasises the need for consistent and distinct species concepts. Consequently, a new botanical key has been devised based on the morphological features of Manumiella bertodano sp. nov., Manumiella conorata [Stover, L.E., 1973. Palaeocene and Eocene species of Deflandrea (Dinophyceae) in Victorian coastal and offshore basins, Australia. In: Glover J.E., Playford, G. (Eds.), Mesozoic and Cainozoic Palynology: Essays in Honour of Isabel Cookson. Geological Society of Australia, Special Publication vol. 4,167-188.] Bujak and Davies 1983, Manumiella druggii [Stover, LE., 1973. Palaeocene and Eocene species of Deflandrea (Dinophyceae) in Victorian coastal and offshore basins, Australia. In: Glover, J.E., Playford, G. (Eds.), Mesozoic and Cainozoic Palynology: Essays in Honour of Isabel Cookson. Geological Society of Australia, Special Publication vol. 4,167-188.] Bujak and Davies 1983, Manumiella seelandica (Lange, D., 1969. Mikroplankton aus dem Fischton von Stevns-KIint auf Seeland. Beitrage zur Meereskunde, 24-25, 110-121.) Bujak and Davies emend. Firth 1987 and Manumiella seymourensis Askin 1999. Manumiella druggii and Manumiella seelandica are retained as separate species. The key has been successfully tested on the well-preserved dinoflagellate cyst assemblages from the uppermost Lopez de Bertodano Formation on Seymour Island, resulting in a clear biostratigraphy based on an existing preliminary scheme. Manumiella seymourensis is prominent in the lowermost part of the succession, and the uppermost part of the range of this species overlaps with that of Manumiella bertodano sp. nov. The latter species ranges into the latest Maastrichtian, where it co-occurs with Manumiella conorata and Manumiella seelandica. Manumiella druggii is confined to the uppermost part of the succession examined. Abundance spikes of Manumiella immediately prior to the KT boundary in this succession have also been recognised globally, and may be related to short-term regressions and/or ocean cooling before the KT event. (C) 2009 Published by Elsevier B.V.	[Thorn, Vanessa C.; Francis, Jane E.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Riding, James B.] British Geol Survey, Kingsley Dunham Ctr, Nottingham NG12 5GG, England	University of Leeds; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey	Thorn, VC (通讯作者)，Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England.	vcbowman@googlemail.com		Bowman, Vanessa/0000-0002-4887-3949	Natural Environment Research Council Antarctic [NE/C506399/1]; NERC [bgs05002] Funding Source: UKRI	Natural Environment Research Council Antarctic; NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	The authors acknowledge funding from the Natural Environment Research Council Antarctic Funding Initiative Grant NE/C506399/1 entitled 'Terminal Cretaceous climate change and biotic response in Antarctica'. We thank the British Antarctic Survey and H.M.S. Endurance for support in the field, and the Transantarctic Association and Antarctic Science Bursary for additional funding. Support for palynological processing came from the Climate Change research programme of the British Geological Survey. J.B. Riding publishes with the permission of the Executive Director, British Geological Survey (NERC). We thank other members of the project for discussion and/or support in the field including J.A. Crame, C.S.M. Day, P. Frost, A.M. Haywood, S. Hunter, J.M. Marshall, D. Pirrie, M. Preistman and R. Raiswell. This contribution was considerably improved by the incisive comments of R.A. Askin and an anonymous reviewer.	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J	Cusick, KD; Boyer, GL; Wilhelm, SW; Sayler, GS				Cusick, Kathleen D.; Boyer, Gregoby L.; Wilhelm, Steven W.; Sayler, Gary S.			Transcriptional Profiling of <i>Saccharomyces cerevisiae</i> Upon Exposure to Saxitoxin	ENVIRONMENTAL SCIENCE & TECHNOLOGY			English	Article							MOLECULAR CHARACTERIZATION; SULFUR ASSIMILATION; COPPER; IRON; YEAST; GENES; EXPRESSION; IDENTIFICATION; HOMEOSTASIS; METABOLISM	Saxitoxin is a potent neurotoxin produced by several species of dinoflagellates and cyanobacteria. The molecular target of saxitoxin in higher eukaryotes is the voltage-gated sodium channel; however, its target in lower eukaryotic organisms remains unknown. The goal of this study was to obtain the transcriptional fingerprint of the model lower eukaryote Saccharomyces cerevisiae upon exposure to saxitoxin to identify potential genes suitable for biomarker development Microarray analyses identified multiple genes associated with copper and iron homeostasis and sulfur metabolism as significantly differentially expressed upon exposure to saxitoxin; these results were verified with quantitative reverse-transcriptase PCR (qRT-PCR). Additionally, the qRT-PCR assays were used to generate expression profiles in a subset of the differentially regulated genes across multiple exposure times and concentrations, the results of which demonstrated that overall, genes tended to respond in a consistent manner to the toxin. In general, the genes encoding the metallothioneins CUP1 and CRS5 were induced following exposure to saxitoxin, while those encoding the ferric/cupric reductase FRE1 and the copper uptake transporter CTR1 were repressed. The gene encoding the multicopper ferroxidase FET3, part of the high-affinity iron uptake system, was also induced in all treatments, along with the STR3 gene, which codes for the cystathionine beta-lyase found in the methionine biosynthetic pathway.	[Cusick, Kathleen D.; Wilhelm, Steven W.; Sayler, Gary S.] Univ Tennessee, Ctr Environm Biotechnol, Knoxville, TN 37966 USA; [Cusick, Kathleen D.; Sayler, Gary S.] Univ Tennessee, Dept Microbiol, Knoxville, TN 37966 USA; [Boyer, Gregoby L.] SUNY Coll Environm Sci & Forestry, Dept Chem, Syracuse, NY 13210 USA; [Sayler, Gary S.] Univ Tennessee, Dept Ecol & Evolutionary Biol, Knoxville, TN 37966 USA	University of Tennessee System; University of Tennessee Knoxville; University of Tennessee System; University of Tennessee Knoxville; State University of New York (SUNY) System; State University of New York (SUNY) College of Environmental Science & Forestry; University of Tennessee System; University of Tennessee Knoxville	Sayler, GS (通讯作者)，Univ Tennessee, Ctr Environm Biotechnol, 676 Dabney Hall, Knoxville, TN 37966 USA.	sayler@utk.edu	Cusick, Kathleen/AAZ-4174-2020; Wilhelm, Steven/B-8963-2008	Wilhelm, Steven/0000-0001-6283-8077; Boyer, Gregory/0000-0003-4490-5461; Cusick, Kathleen/0000-0001-7224-3472	NASA [NNX07AT76H]	NASA(National Aeronautics & Space Administration (NASA))	Julia Stair Gouffon at the Affymetrix Core Facility, UT Knoxville, performed the sample preparation, hybridization, and scanning in the microarray experiments. Jim Fleming provided the ArrayStat program. Research funded by a NASA Graduate Student Research Fellowship NNX07AT76H to KDC.	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Sci. Technol.	AUG 1	2009	43	15					6039	6045		10.1021/es900581q	http://dx.doi.org/10.1021/es900581q			7	Engineering, Environmental; Environmental Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Engineering; Environmental Sciences & Ecology	476XR	19731715				2025-03-11	WOS:000268480600076
J	Triantaphyllou, MV; Antonarakou, A; Kouli, K; Dimiza, M; Kontakiotis, G; Papanikolaou, MD; Ziveri, P; Mortyn, PG; Lianou, V; Lykousis, V; Dermitzakis, MD				Triantaphyllou, M. V.; Antonarakou, A.; Kouli, K.; Dimiza, M.; Kontakiotis, G.; Papanikolaou, M. D.; Ziveri, P.; Mortyn, P. G.; Lianou, V.; Lykousis, V.; Dermitzakis, M. D.			Late Glacial-Holocene ecostratigraphy of the south-eastern Aegean Sea, based on plankton and pollen assemblages	GEO-MARINE LETTERS			English	Article							CENTRAL MEDITERRANEAN SEA; TERM CLIMATE CHANGES; LATE QUATERNARY; LATE PLEISTOCENE; SURFACE-WATER; SAPROPEL S1; PALEOENVIRONMENTAL CHANGES; TEMPERATURE-VARIATIONS; CARBONATE DIAGENESIS; DINOFLAGELLATE CYSTS	Quantitative analyses of coccolithophores, planktonic foraminifers, dinoflagellate cysts and pollen assemblages were carried out on shallow (NS-14) and deeper (NS-40) sediment cores from the south-eastern Aegean Sea. Nine coccolithophore (ACE 1-9) and nine planktonic foraminifer (APFE 1-9) ecozones, correlated with dinoflagellate cyst evidence, have been defined for the last 14.5 cal. ka. Additionally, eight pollen assemblage zones (PAZ 1-8) have been recognised and correlated with the plankton ecozones. Although generally consistent with existing schemes for the central and eastern Mediterranean, the established high-resolution ecostratigraphy has led to an expanded palaeoecological reconstruction of the Late Glacial-Holocene archive in the south-eastern Aegean Sea, defining two warm and humid phases at 9.3-8.6 and 7.6-6.4 cal. ka b.p., associated with the deposition of the early Holocene sapropel S1, and a third one between 5.2 and 4.2 cal. ka b.p. The high sedimentation rates which characterise the study area enabled the detection of even minor and brief climatic events in the Aegean Sea during S1 deposition times.	[Triantaphyllou, M. V.; Antonarakou, A.; Kouli, K.; Dimiza, M.; Kontakiotis, G.; Lianou, V.; Dermitzakis, M. D.] Univ Athens, Dept Hist Geol Paleontol, Fac Geol & Geoenvironm, Athens 15784, Greece; [Papanikolaou, M. D.] Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; [Ziveri, P.] Vrije Univ Amsterdam, FALW, Dept Paleoclimatol & Geomorphol, NL-1081 HV Amsterdam, Netherlands; [Ziveri, P.; Mortyn, P. G.] Autonomous Univ Barcelona, ICTA, Bellaterra 08193, Spain; [Lykousis, V.] Hellen Ctr Marine Res, Inst Oceanog, Anavyssos 19013, Greece	National & Kapodistrian University of Athens; University of Cambridge; Vrije Universiteit Amsterdam; Autonomous University of Barcelona; Hellenic Centre for Marine Research	Triantaphyllou, MV (通讯作者)，Univ Athens, Dept Hist Geol Paleontol, Fac Geol & Geoenvironm, Athens 15784, Greece.	mtriant@geol.uoa.gr	; Mortyn, P. Graham/I-3860-2015; Triantaphyllou, Maria/AAL-7877-2021; Dimiza, Margarita/A-6857-2015; Kouli, Katerina/M-8243-2013; Ziveri, Patrizia/I-3856-2015	Papanikolaou, Maria/0009-0005-4380-7917; Mortyn, P. Graham/0000-0002-9473-4309; Antonarakou, Assimina/0000-0001-8901-8423; Triantaphyllou, Maria/0000-0001-7508-7508; Dimiza, Margarita/0000-0002-9809-1902; Kouli, Katerina/0000-0003-1656-1091; Kontakiotis, George/0000-0001-9371-6726; Ziveri, Patrizia/0000-0002-5576-0301	Pythagoras I project (EU and Greek Ministry of Education, EPEAEK II); European Science Foundation (ESF) [ERAS-CT-2003-980409]	Pythagoras I project (EU and Greek Ministry of Education, EPEAEK II); European Science Foundation (ESF)(European Science Foundation (ESF)Estonian Research Council)	We acknowledge financial support from the Pythagoras I project (EU and Greek Ministry of Education, EPEAEK II) and partial support from the European Science Foundation (ESF) under the EUROCORES Programme EuroCLIMATE, through contract no. ERAS-CT-2003-980409 of the European Commission, DG Research, FP6. Critical comments by two anonymous referees and the journal editors have proved essential in improving the manuscript.	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Lett.	AUG	2009	29	4					249	267		10.1007/s00367-009-0139-5	http://dx.doi.org/10.1007/s00367-009-0139-5			19	Geosciences, Multidisciplinary; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Oceanography	472AV					2025-03-11	WOS:000268102400004
J	Sundström, AM; Kremp, A; Daugbjerg, N; Moestrup, O; Ellegaard, M; Hansen, R; Hajdu, S				Sundstrom, Annica M.; Kremp, Anke; Daugbjerg, Niels; Moestrup, Ojvind; Ellegaard, Marianne; Hansen, Regina; Hajdu, Susanna			<i>GYMNODINIUM COROLLARIUM</i> SP NOV (DINOPHYCEAE)-A NEW COLD-WATER DINOFLAGELLATE RESPONSIBLE FOR CYST SEDIMENTATION EVENTS IN THE BALTIC SEA	JOURNAL OF PHYCOLOGY			English	Article						Baltic Sea; dinoflagellate cysts; Gymnodinium; LSU rDNA; spring bloom; taxonomy	SCRIPPSIELLA-HANGOEI DINOPHYCEAE; RIBOSOMAL-RNA; SPRING-BLOOM; COMB. NOV; PHYLOGENETIC ANALYSIS; ELECTRON-MICROSCOPY; FUSCUM DINOPHYCEAE; AUSTRALIAN WATERS; RDNA SEQUENCES; ULTRASTRUCTURE	A naked dinoflagellate with a unique arrangement of chloroplasts in the center of the cell was isolated from the northern Baltic proper during a spring dinoflagellate bloom (March 2005). Morphological, ultrastructural, and molecular analyses revealed this dinoflagellate to be undescribed and belonging to the genus Gymnodinium F. Stein. Gymnodinium corollarium A. M. Sundstrom, Kremp et Daugbjerg sp. nov. possesses features typical of Gymnodinium sensu stricto, such as nuclear chambers and an apical groove running in a counterclockwise direction around the apex. Phylogenetic analyses based on partial nuclear-encoded LSU rDNA sequences place the species in close proximity to G. aureolum, but significant genetic distance, together with distinct morphological features, such as the position of chloroplasts, clearly justifies separation from this species. Temperature and salinity experiments revealed a preference of G. corollarium for low salinities and temperatures, confirming it to be a cold-water species well adapted to the brackish water conditions in the Baltic Sea. At nitrogen-deplete conditions, G. corollarium cultures produced small, slightly oval cysts resembling a previously unidentified cyst type commonly found in sediment trap samples collected from the northern and central open Baltic Sea. Based on LSU rDNA comparison, these cysts were assigned to G. corollarium. The cysts have been observed in many parts of the Baltic Sea, indicating the ecologic versatility of the species and its importance for the Baltic ecosystem.	[Sundstrom, Annica M.; Hajdu, Susanna] Stockholm Univ, Dept Syst Ecol, SE-10691 Stockholm, Sweden; [Kremp, Anke] Finnish Environm Inst, Helsinki 00251, Finland; [Kremp, Anke] Univ Helsinki, Tvarminne Zool Stn, FI-10900 Hango, Finland; [Daugbjerg, Niels; Moestrup, Ojvind; Ellegaard, Marianne] Univ Copenhagen, Phycol Lab, Dept Biol, DK-1353 Copenhagen K, Denmark; [Hansen, Regina] Leibniz Inst Balt Sea Res Warnemunde, D-18119 Rostock, Germany	Stockholm University; Finnish Environment Institute; University of Helsinki; University of Copenhagen; Leibniz Institut fur Ostseeforschung Warnemunde	Sundström, AM (通讯作者)，Stockholm Univ, Dept Syst Ecol, SE-10691 Stockholm, Sweden.	annica@ecology.su.se	Kremp, Anke/I-8139-2013; Ellegaard, Marianne/H-6748-2014; Daugbjerg, Niels/D-3521-2014	Ellegaard, Marianne/0000-0002-6032-3376; Moestrup, Ojvind/0000-0003-0965-8645; Daugbjerg, Niels/0000-0002-0397-3073	Academy of Finland [111336-]; Academy of Finland (AKA) [111336] Funding Source: Academy of Finland (AKA)	Academy of Finland(Research Council of Finland); Academy of Finland (AKA)(Research Council of Finland)	Laboratory facilities were provided by the Tvarminne Zoological Station (University of Helsinki), the Department of Systems Ecology (Stockholm University), and the Phycology laboratory (University of Copenhagen). We thank Helena Hoglander and Antonella Penna for discussion and Sanna Eirtovaara for assistance with the molecular work. Dr. Reijo Pitkaranta (Department of Classical Languages, University of Helsinki) kindly translated the species diagnosis into Latin. This work was funded by the Walter and Andree de Nottbeck Foundation (A. Sundstrom), SYNTHESYS (http://www.synthesys.info/), which is financed by European Community Research Infrastructure Action under the FP6 "Structuring the European Research Area" Programme (A. Sundstrom), and the Academy of Finland grant 111336 (A. Kremp).	[Anonymous], OPHELIA S; [Anonymous], ACTA BOT FENN; AUTIO R, 1990, ECOLOGICAL PLANKTON; Biecheler B., 1939, Bulletin de la Societe Zoologique de France, V64, P12; Biecheler B., 1952, Bull. Biol. Fr. 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Phylogenetic Analysis Using Parsimony (and Other Methods); Tang YZ, 2008, J EUKARYOT MICROBIOL, V55, P91, DOI 10.1111/j.1550-7408.2008.00305.x; THOMPSON JD, 1994, NUCLEIC ACIDS RES, V22, P4673, DOI 10.1093/nar/22.22.4673; Thomsen HA., 1992, Plankton i Indre Danske Farvande. En Analyse Af Forekomsten Af Alger Og Heterotrofe Protister (Ekskl. Ciliater) i Kattegat; Wasmund N, 2003, ICES J MAR SCI, V60, P177, DOI 10.1016/S1054-3139(02)00280-1; Wasmund N, 1998, J PLANKTON RES, V20, P1099, DOI 10.1093/plankt/20.6.1099; WEDEMAYER GJ, 1982, J PHYCOL, V18, P13, DOI 10.1111/j.1529-8817.1982.tb03152.x; WILCOX LW, 1984, J PHYCOL, V20, P236, DOI 10.1111/j.0022-3646.1984.00236.x; WILCOX LW, 1982, J PHYCOL, V18, P18	67	47	47	1	27	WILEY-BLACKWELL PUBLISHING, INC	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	0022-3646			J PHYCOL	J. Phycol.	AUG	2009	45	4					938	952		10.1111/j.1529-8817.2009.00712.x	http://dx.doi.org/10.1111/j.1529-8817.2009.00712.x			15	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	488TF	27034225				2025-03-11	WOS:000269372300019
J	Pitcher, GC; Joyce, LB				Pitcher, Grant C.; Joyce, Linda B.			Dinoflagellate cyst production on the southern Namaqua shelf of the Benguela upwelling system	JOURNAL OF PLANKTON RESEARCH			English	Article							SURFACE SEDIMENTS; WEST-COAST; RED TIDE; BAY; SCRIPPSIELLA; AFRICA; BLOOMS; EUTROPHICATION; LINGULODINIUM; DINOPHYCEAE	To study dinoflagellate cyst production in the southern Benguela, a sediment trap was deployed for a period of 3.5 years at a single station located downstream of the Cape Columbine upwelling cell on the southern Namaqua shelf. The cyst assemblage of surface sediments below the trap was also investigated. Twenty-nine different cyst types were recorded of which 25 were from the sediment trap, and 22 from the surface sediments. The flux of cysts followed a clear seasonal trend with an initial peak in spring followed by a major peak in autumn; with a mean flux for the entire period of deployment of 1.4 x 10(6) cysts m(-2) day(-1). Of the cysts recovered from the trap, those of heterotrophic dinoflagellates were six times more abundant than those of autotrophic dinoflagellates. The study also revealed the presence of cysts of species previously unrecorded in the plankton of the southern Benguela, specifically the toxic dinoflagellate Lingulodinium polyedrum.	[Pitcher, Grant C.; Joyce, Linda B.] Marine & Coastal Management, ZA-8012 Cape Town, Cape Town, South Africa; [Joyce, Linda B.] Univ Cape Town, Dept Oceanog, ZA-7701 Cape Town, South Africa	University of Cape Town; University of Cape Town	Pitcher, GC (通讯作者)，Marine & Coastal Management, Private Bag X2, ZA-8012 Cape Town, Cape Town, South Africa.	gpitcher@deat.gov.za						ANDERSON DM, 1984, ACS SYM SER, V262, P125; ANDERSON DM, 1985, LIMNOL OCEANOGR, V30, P1000, DOI 10.4319/lo.1985.30.5.1000; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; Bockelmann FD, 2007, LIMNOL OCEANOGR, V52, P2582, DOI 10.4319/lo.2007.52.6.2582; CEMBELLA A D, 1988, Journal of Shellfish Research, V7, P597; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; Dale B., 1983, P69; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DODGE JD, 1991, NEW PHYTOL, V118, P593, DOI 10.1111/j.1469-8137.1991.tb01000.x; Fawcett A, 2007, MAR ECOL PROG SER, V348, P19, DOI 10.3354/meps07027; Fujii R, 2006, J PLANKTON RES, V28, P131, DOI 10.1093/plankt/fbi106; Godhe A, 2001, J PLANKTON RES, V23, P923, DOI 10.1093/plankt/23.9.923; GRINDLEY J R, 1970, Fisheries Bulletin South Africa, V6, P36; GRINDLEY J R, 1968, South African Journal of Science, V64, P420; Harland R, 1999, MAR MICROPALEONTOL, V37, P77, DOI 10.1016/S0377-8398(99)00016-X; Hasle G.R., 1978, PHYTOPLANKTON MANUAL, P88; Head M.J., 1996, Palynology: Principles and Applications, P1197; HEANEY SI, 1983, BRIT PHYCOL J, V18, P47, DOI 10.1080/00071618300650061; HEISKANEN AS, 1993, MAR BIOL, V116, P161, DOI 10.1007/BF00350743; Horstman DA., 1981, FISHERIES B S AFRICA, V15, P71; Ishikawa A, 1996, MAR ECOL PROG SER, V140, P169, DOI 10.3354/meps140169; Joyce LB, 2006, AFR J MAR SCI, V28, P295, DOI 10.2989/18142320609504165; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; Joyce LB, 2004, ESTUAR COAST SHELF S, V59, P1, DOI 10.1016/j.ecss.2003.07.001; Kim YO, 2000, MAR ECOL PROG SER, V204, P111, DOI 10.3354/meps204111; 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; KROCK B, 2008, P 12 INT C HARMF ALG; LEWIS J, 1988, J MAR BIOL ASSOC UK, V68, P701, DOI 10.1017/S0025315400028812; Matsuoka K., 2003, Monographs on Oceanographic Methodology, V11, P563; Matsuoka K, 1999, SCI TOTAL ENVIRON, V231, P17, DOI 10.1016/S0048-9697(99)00087-X; Matsuoka K, 2009, REV PALAEOBOT PALYNO, V154, P79, DOI 10.1016/j.revpalbo.2008.12.013; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; Mitchell-Innes BA, 2000, S AFR J MARINE SCI, V22, P273, DOI 10.2989/025776100784125762; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Nehring S., 1993, INTERDISCIPLINARY DI, P454; NELSON G, 1983, PROG OCEANOGR, V12, P333, DOI 10.1016/0079-6611(83)90013-7; Paz B, 2004, TOXICON, V44, P251, DOI 10.1016/j.toxicon.2004.05.021; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; Pitcher G., 1995, P657; Pitcher GC, 2000, S AFR J MARINE SCI, V22, P255, DOI 10.2989/025776100784125681; Pitcher GC, 1998, MAR ECOL PROG SER, V172, P253, DOI 10.3354/meps172253; Pitcher GC, 2006, LAR MAR ECOSYST, V14, P125; Pitcher GC, 2006, LIMNOL OCEANOGR, V51, P2660, DOI 10.4319/lo.2006.51.6.2660; Sapeika N., 1948, South African Medical Journal, V22, P337; Satake Masayuki, 1997, Natural Toxins, V5, P164; SHANNON LV, 1985, OCEANOGR MAR BIOL, V23, P105; SMAYDA TJ, PROG OCEANOGR UNPUB; 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; Wendler I, 2002, MAR MICROPALEONTOL, V46, P1, DOI 10.1016/S0377-8398(02)00049-X; Zohary T, 1998, LIMNOL OCEANOGR, V43, P175, DOI 10.4319/lo.1998.43.2.0175; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1	54	36	37	1	9	OXFORD UNIV PRESS	OXFORD	GREAT CLARENDON ST, OXFORD OX2 6DP, ENGLAND	0142-7873	1464-3774		J PLANKTON RES	J. Plankton Res.	AUG	2009	31	8					865	875		10.1093/plankt/fbp040	http://dx.doi.org/10.1093/plankt/fbp040			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	469II		Bronze			2025-03-11	WOS:000267889300007
J	Coolen, MJL; Saenz, JP; Giosan, L; Trowbridge, NY; Dimitrov, P; Dimitrov, D; Eglinton, TI				Coolen, Marco J. L.; Saenz, James P.; Giosan, Liviu; Trowbridge, Nan Y.; Dimitrov, Petko; Dimitrov, Dimitar; Eglinton, Timothy I.			DNA and lipid molecular stratigraphic records of haptophyte succession in the Black Sea during the Holocene	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Black Sea; Holocene; ancient DNA; fossil DNA; paleogenetics; alkenones; Emliania huxleyi; Isochrysis	LONG-CHAIN ALKENONES; ORGANIC-CARBON ACCUMULATION; GREEN SULFUR BACTERIA; MARMARA SEA; PALYNOLOGICAL EVIDENCE; DINOFLAGELLATE CYSTS; EXTRACELLULAR DNA; MEDITERRANEAN SEA; LATE PLEISTOCENE; AGE CALIBRATION	Previous studies suggest that the coccolithophorid haptophyte Emiliania huxleyi entered the Black Sea similar to 3400 yrs ago and since then a coccolith ooze defined as Unit I has developed. Unit I sediments contain long-chain alkenones derived from E huxleyi whereas the alkenone distribution of the deeper coccolith-free sapropel (Unit II) is rather unusual. Alkenone-derived past sea surface temperature (SST) estimates suggest a large difference between Unit II and Unit I, which is likely a result of unusual biological precursors of the alkenones in Unit II. Here, we report a high-resolution stratigraphic analysis of ancient haptophyte DNA to establish the Holocene succession of haptophytes as sources of the alkenones in the Black Sea. Haptophytes related to brackish Isochrysis spp. were the initial sources of alkenones, and appeared immediately after the onset of sapropel deposition (similar to 7550 yrs before present [a BP]). As salinity increased, Isochrysis-related haptophytes were slowly replaced by a complex suite of huxleyi strains as sources of alkenones. Our paleogenetic data showed that E. huxleyi colonized the Black Sea shortly after the onset of sapropel deposition, similar to 4000 yrs earlier than previously recognized based on their preserved coccoliths. E. huxleyi strains were the most likely source of the previously reported abundant and unusual C-36 di-unsaturated "Black Sea alkenone". Strong haptophyte species and strain-specific effects were observed on the level of unsaturation of alkenones which resulted in spurious alkenone-derived SST estimates before 5250 a BP. In contrast, from similar to 5250 a BP onwards a relatively stable haptophyte assemblage dominated by a different suite of E. huxleyi strains yielded robust alkenone-SST values and indicated a gradual cooling from 19 degrees C to similar to 15 degrees C at the top of the record (similar to 450 a BP). Published by Elsevier B.V.	[Coolen, Marco J. L.; Saenz, James P.; Trowbridge, Nan Y.; Eglinton, Timothy I.] Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA; [Giosan, Liviu] Woods Hole Oceanog Inst, Dept Geol & Geophys, Woods Hole, MA 02543 USA; [Dimitrov, Petko; Dimitrov, Dimitar] Bulgarian Acad Sci, Inst Oceanol, Marine Geol & Archaeol Dept, Varna 9000, Bulgaria	Woods Hole Oceanographic Institution; Woods Hole Oceanographic Institution; Bulgarian Academy of Sciences	Coolen, MJL (通讯作者)，Woods Hole Oceanog Inst, Marine Chem & Geochem Dept, Woods Hole, MA 02543 USA.	mcoolen@whoi.edu	Saenz, James/E-9218-2011; Giosan, Liviu/F-1809-2010; Coolen, Marco/B-8263-2015; Dimitrov, Petko/T-6909-2019; Dimitrov, Dimitar Petkov/B-7374-2017	Saenz, James/0000-0001-8901-4377; Eglinton, Timothy/0000-0001-5060-2155; Coolen, Marco/0000-0002-0417-920X; Dimitrov, Petko/0000-0003-2280-2058; Dimitrov, Dimitar Petkov/0000-0001-8402-9529	US National Science Foundation [OCE 0602423]; WHOI's Access to the Sea program; Andrew W. Mellon Foundation Endowed Fund for Innovative Research	US National Science Foundation(National Science Foundation (NSF)); WHOI's Access to the Sea program; Andrew W. Mellon Foundation Endowed Fund for Innovative Research	We would like to thank Al Gagnon, Daniel Montlucon, Drs. Cornelia Wuchter and Angela Dickens (WHOI) as well as the R/V Akademik crew and IOBAS researchers, and in particular Delcho Solakov, for their extensive organizational and participatory help with the cruise, and Carl G. Johnson (WHOI) for the extensive TOC measurements. In addition, we would like to thank two anonymous and dedicated reviewers for their suggestions to improve the manuscript. We are grateful for the financial support from US National Science Foundation grant OCE 0602423, as well as funding from WHOI's Access to the Sea program, and a grant from the Andrew W. Mellon Foundation Endowed Fund for Innovative Research.	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Sci. Lett.	JUL 15	2009	284	3-4					610	621		10.1016/j.epsl.2009.05.029	http://dx.doi.org/10.1016/j.epsl.2009.05.029			12	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	487NY					2025-03-11	WOS:000269282700034
J	Melinte-Dobrinescu, MC; Suc, JP; Clauzon, G; Popescu, SM; Armijo, R; Meyer, B; Biltekin, D; Çagatay, MN; Ucarkus, G; Jouannic, G; Fauquette, S; Çakir, Z				Melinte-Dobrinescu, Mihaela Carmen; Suc, Jean-Pierre; Clauzon, Georges; Popescu, Speranta-Maria; Armijo, Rolando; Meyer, Bertrand; Biltekin, Demet; Cagatay, M. Namik; Ucarkus, Guelsen; Jouannic, Gwenael; Fauquette, Severine; Cakir, Ziyadin			The Messinian Salinity Crisis in the Dardanelles region: Chronostratigraphic constraints	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Calcareous nannoplankton; Chronostratigraphy; Messinian Salinity Crisis; Palaeogeography; NE Aegean region	NORTH ANATOLIAN FAULT; LAST 2000 YEARS; LATE MIOCENE; WESTWARD PROPAGATION; WESTERN GULF; DACIC BASIN; BLACK-SEA; PARATETHYS; DEPOSITS; FRANCE	An intense controversy on chronostratigraphy of upper Miocene-lower Pliocene deposits and the Messinian Salinity Crisis in the Dardanelles area led to a systematic investigation of calcareous nannoplankton content of 10 key-sections representative of the most relevant regional Kirazli and Alcitepe formations. Our study shows clearly that the Kirazli Formation deposits predate the Messinian Salinity Crisis while those of the Alcitepe Formation postdate this outstanding event, which severely impacted the region as widely known around the Mediterranean Basin. Fluvial canyon cutting or gap in sedimentation linked to the peak of the Messinian Salinity Crisis separates the two formations. Detailed palaeoenvironmental investigations (based on the fluctuation and distribution pattern of dinoflagellate cysts, pollen grains and calcareous nannoplankton) allow us to reconstruct the regional palaeogeography before, during and after the Messinian Salinity Crisis. The gathered data do not indicate any marine corridor between the Eastern Mediterranean Sea and Eastern Paratethys through the Marmara Sea region at the time of the Messinian Salinity Crisis. (C) 2009 Elsevier B.V. All rights reserved.	[Suc, Jean-Pierre; Popescu, Speranta-Maria] CNRS, UMR 5125, Lab PaleoEnvironm & PaleobioSphere, F-75700 Paris, France; [Suc, Jean-Pierre; Popescu, Speranta-Maria] Univ Lyon 1, F-69622 Villeurbanne, France; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, GEOECOMAR, RO-024053 Bucharest, Romania; [Clauzon, Georges] Univ Paul Cezanne, CNRS, UMR 6635, CEREGE, F-13545 Aix En Provence, France; [Armijo, Rolando] CNRS, Inst Phys Globe, Lab Tecton, UMR 7154, F-75252 Paris, France; [Meyer, Bertrand; Jouannic, Gwenael] Univ Paris 06, ISTeP, UMR 7193, F-75252 Paris 05, France; [Biltekin, Demet; Cagatay, M. Namik; Ucarkus, Guelsen; Cakir, Ziyadin] Istanbul Tech Univ, Sch Mines, TR-34469 Istanbul, Turkey; [Biltekin, Demet; Cagatay, M. Namik; Ucarkus, Guelsen; Cakir, Ziyadin] Eurasia Inst Earth Sci, TR-34469 Istanbul, Turkey; [Fauquette, Severine] Univ Montpellier 2, Equipe Paleoenvironm & Paleoclimats, CNRS, Inst Sci Evolut,UMR 5554, F-34095 Montpellier 05, France	Centre National de la Recherche Scientifique (CNRS); Universite Claude Bernard Lyon 1; National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Aix-Marseille Universite; Universite PSL; College de France; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite Paris Cite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Istanbul Technical University; Istanbul Technical University; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD); Universite de Montpellier; CNRS - Institute of Ecology & Environment (INEE)	Suc, JP (通讯作者)，CNRS, UMR 5125, Lab PaleoEnvironm & PaleobioSphere, F-75700 Paris, France.	melinte@geoecomar.ro; jean-pierre.suc@univ-lyon1.fr; clauzon@cerege.fr; speranta.popescu@univ-lyon1.fr; armijo@ipgp.jussieu.fr; bertrand.meyer@upmc.fr; biltekin@itu.edu.tr; cagatay@itu.edu.tr; ucarkus1@itu.edu.tr; gwenael.jouannic@gmail.com; severine.fauquette@univ-montp2.fr; ziyadin.cakir@itu.edu.tr	Cagatay, M./S-6736-2016; Armijo, Rolando/P-5123-2019; Mihaela, mihaela/AAF-5894-2021; Ucarkus, Gulsen/HTT-3956-2023; Meyer, Bertrand/E-6903-2011; Fauquette, Severine/M-3686-2019; Cakir, Ziyadin/C-3594-2008; Jouannic, Gwenael/ABG-7687-2020; Biltekin, Demet/AAB-3460-2020	Fauquette, Severine/0000-0003-0516-7734; Popescu, Speranta- Maria/0000-0001-5345-395X; Melinte-Dobrinescu, Mihaela Carmen/0000-0003-4716-6844; Cakir, Ziyadin/0000-0003-3050-5619; Armijo, Rolando/0000-0002-8258-2862; Jouannic, Gwenael/0000-0003-3399-389X; Biltekin, Demet/0000-0003-2976-0321	Romanian National Programme of Research, Development and Innovation [144/2007, 364/2007]; ISEM [2009-029]	Romanian National Programme of Research, Development and Innovation; ISEM	This research started within the frame of the CNRS-INSU ECLIPSE II Programme and was mostly developed thanks to the ANR EGEO Project. One of us (D. Biltekin) was granted by the French Embassy in Turkey for her PhD thesis. This paper is a contribution to the Projects IDEI of the Romanian National Programme of Research, Development and Innovation (Projects No. 144/2007 CNCSIS Code 816 and 364/2007, CNCSIS Code 815 - M.C. Melinte-Dobrinescu). We are indebted to Marie-Pierre Aubry, who reviewed this paper and made valuable suggestions and comments, which significantly increase the chronostratigraphic and ecostratigraphic inferences of the manuscript. We also appreciate the improvements suggested by an anonymous referee. The English language was improved by Oliver Bazely. This paper is the ISEM contribution no 2009-029.	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Paleoclimatol. Paleoecol.	JUL 15	2009	278	1-4					24	39		10.1016/j.palaeo.2009.04.009	http://dx.doi.org/10.1016/j.palaeo.2009.04.009			16	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	468SW					2025-03-11	WOS:000267842500002
J	Morquecho, L; Góngora-González, DT; Okolodkov, YB				Morquecho, Lourdes; Gongora-Gonzalez, Diana T.; Okolodkov, Yuri B.			CYST-THECA RELATIONSHIPS OF GONYAULACALES AND PERIDINIALES (DINOPHYCEAE) FROM BAHIA CONCEPCION, GULF OF CALIFORNIA	ACTA BOTANICA MEXICANA			English	Article						cyst-theca relationships; dinoflagellates; Gonyaulacales; Gulf of California; Mexican Pacific; Peridiniales	DINOFLAGELLATE RESTING CYSTS; RECENT SEDIMENTS; BALTIC SEA; GYMNODINIUM-CATENATUM; COASTAL WATERS; COMB-NOV; MORPHOLOGY; TEMPERATURE; PLANKTON; MEXICO	Based on samples obtained in 2000-2002 from a 1-cm layer of surface sediment at two sites in Bahia Concepcion in the Gulf of California, cyst-theca relationships were defined from cyst germination assays for Gonyaulax spinifera (= Spiniferites mirabilis), Protoce-ratium globosum, Preperidinium meunieri (= Dubridinium caperatum), Protoperidinium denticulatum (= Brigantedinium irregulare), and Protoperidinium cf. thorianum. All the taxa are illustrated with photomicrographs and descriptions of the resting and vegetative stages are given, including synonymy, size variation, distribution in Mexico, and global distribution, when known. As a result of cyst germination assays, the previously unknown cyst-theca relationship of P. globosum was described. We also confirmed the presence of the vegetative stage of P. denticulatum in the Gulf of California and heterospory in G. spinifera from Bahia Concepcion. Cultures of G. spinifera and P. globosum were successfully established.	[Morquecho, Lourdes; Gongora-Gonzalez, Diana T.] Ctr Invest Biol Noroeste, La Paz 23090, Baja California, Mexico; [Okolodkov, Yuri B.] Univ Veracruzana, Ctr Ecol & Pesquerias, Boca Del Rio 94290, Veracruz, Mexico	Telefonica SA; CIBNOR - Centro de Investigaciones Biologicas del Noroeste; Universidad Veracruzana	Morquecho, L (通讯作者)，Ctr Invest Biol Noroeste, Mar Bermejo 195,Colonia Playa Palo Santa Rita, La Paz 23090, Baja California, Mexico.	lamorquecho@cibnor.mx; yurikolodkov@yahoo.com	Morquecho, Lourdes/JPY-0626-2023	Morquecho, Lourdes/0000-0003-2963-8836	Consejo Nacional de Ciencia y Tecnologia of Mexico (CONACYT) [R33598-B]	Consejo Nacional de Ciencia y Tecnologia of Mexico (CONACYT)(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	We appreciate the field and laboratory work of Than Murrillo, Francisco Hemandez, and Felipe Zapata. Malte Elbrachter at Deutsches Zentrum fur Marine Biodiversitatsforschung, Forschungsinstitut Senkenberg, Germany and Martin J. Head from Brock University, St. Catharines, Ontario, Canada provided important suggestions to improve the manuscript, as did the anonymous reviewers. Marcia M. Gowing at the University of California at Santa Cruz kindly improved the text. Boris Okolodkov assisted in preparing a map of sampling sites. This survey was supported by Consejo Nacional de Ciencia y Tecnologia of Mexico (CONACYT grant R33598-B).	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Bot. Mex.	JUL	2009	88						9	29						21	Plant Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences	469JQ					2025-03-11	WOS:000267894300002
J	Mulholland, MR; Morse, RE; Boneillo, GE; Bernhardt, PW; Filippino, KC; Procise, LA; Blanco-Garcia, JL; Marshall, HG; Egerton, TA; Hunley, WS; Moore, KA; Berry, DL; Gobler, CJ				Mulholland, Margaret R.; Morse, Ryan E.; Boneillo, George E.; Bernhardt, Peter W.; Filippino, Katherine C.; Procise, Leo A.; Blanco-Garcia, Jose L.; Marshall, Harold G.; Egerton, Todd A.; Hunley, William S.; Moore, Kenneth A.; Berry, Dianna L.; Gobler, Christopher J.			Understanding Causes and Impacts of the Dinoflagellate, <i>Cochlodinium polykrikoides</i>, Blooms in the Chesapeake Bay	ESTUARIES AND COASTS			English	Article						Cochlodinium polykrikoides; Nitrogen uptake; Chesapeake Bay; Fish mortality	NITROGEN; GYMNODINIALES; DINOPHYCEAE; MORTALITY; CYSTS; PRODUCTIVITY; MIXOTROPHY; SALINITY; DYNAMICS; REGIONS	During August and September 2007, the lower Chesapeake Bay and its tributaries experienced a massive bloom of Cochlodinium polykrikoides Margalef (> 10(4) cells per milliliter) that persisted for over a month, was extremely patchy, and at times penetrated into the Atlantic Ocean. The onset of the bloom coincided with a period of intense rainfall and stormwater runoff after a protracted summer drought period. Genetic evidence showed this species to be distinct from many Asian strains but similar to other North American strains. Populations dominated by C. polykrikoides took up a variety of nitrogenous compounds to support their growth and were able to mobilize additional sources of organic nutrients through peptide hydrolysis. Bioassays determined that C. polykrikoides exerted a lethal affect on juvenile fish and shellfish, causing 100% mortality of juvenile fish (Cyprinodon variegates) in less than 24 h and 20% mortality in juvenile American oysters (similar to 21 mm; Crassostrea virginica) within 72 h.	[Mulholland, Margaret R.; Morse, Ryan E.; Boneillo, George E.; Bernhardt, Peter W.; Filippino, Katherine C.; Procise, Leo A.; Blanco-Garcia, Jose L.] Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, 4600 Elkhorn Ave, Norfolk, VA 23529 USA; [Marshall, Harold G.; Egerton, Todd A.] Old Dominion Univ, Dept Biol Sci, Norfolk, VA 23529 USA; [Hunley, William S.] Hampton Rd Sanitat Dist, Virginia Beach, VA USA; [Moore, Kenneth A.] Coll William & Mary, Sch Marine Sci, Virginia Inst Marine Sci, Gloucester Point, VA 23062 USA; [Berry, Dianna L.; Gobler, Christopher J.] SUNY Stony Brook, Sch Marine & Atmospher Sci, Stony Brook, NY 11794 USA	Old Dominion University; Old Dominion University; William & Mary; Virginia Institute of Marine Science; State University of New York (SUNY) System; Stony Brook University	Mulholland, MR (通讯作者)，Old Dominion Univ, Dept Ocean Earth & Atmospher Sci, 4600 Elkhorn Ave, Norfolk, VA 23529 USA.	mmulholl@odu.edu	Gobler, Christopher/JOZ-2924-2023; Mulholland, Margaret/E-8480-2011; Morse, Ryan/ITT-9676-2023	Morse, Ryan/0000-0002-0854-2723; Egerton, Todd/0000-0002-0341-7915	National Oceanic and Atmospheric Administration; Center for Sponsored Coastal Ocean Research Event Response Program; DATAFLOW; Virginia Environmental Endowment to MRM	National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); Center for Sponsored Coastal Ocean Research Event Response Program; DATAFLOW; Virginia Environmental Endowment to MRM	Funding was provided by the National Oceanic and Atmospheric Administration, Center for Sponsored Coastal Ocean Research Event Response Program. We thank the Hampton Roads Sanitation District and Virginia Department of Environmental Quality for supporting DATAFLOW mapping and shallow-water continuous monitoring efforts. This work was also funded through grants from the Virginia Environmental Endowment to MRM.	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J	Kremp, A; Rengefors, K; Montresor, M				Kremp, Anke; Rengefors, Karin; Montresor, Marina			Species-specific encystment patterns in three Baltic cold-water dinoflagellates: The role of multiple cues in resting cyst formation	LIMNOLOGY AND OCEANOGRAPHY			English	Article							ALEXANDRIUM-TAMARENSE DINOPHYCEAE; LIFE-CYCLE; SCRIPPSIELLA-HANGOEI; TOXIC DINOFLAGELLATE; POPULATION-DYNAMICS; GROWTH; PHYTOPLANKTON; TEMPERATURE; PHOSPHORUS; ZOOPLANKTON	The relationships among cellular nutrient status, environmental conditions (temperature and nutrient availability), and cyst production were studied in batch cultures of three cold-water dinoflagellates (Scrippsiella hangoei, Gymnodinium corollarium, and Woloszynskia halophila) isolated from the Baltic Sea. We tested the effect of increasing temperature while providing nutrient-replete conditions as well as the effect of ambient nutrient (N, P) deficiency. The results revealed different encystment cues and patterns in the three species. While depletion of ambient nitrogen and subsequent internal N stress were the primary factors behind cyst production of G. corollarium, higher temperature led to substantial encystment of S. hangoei and W. halophila without a direct link to cellular nutrient physiology. In W. halophila, N limitation induced a transition of the population to small cells presumably representing gametes, but this process was not followed by cyst formation. Phosphorus stress was not directly linked to cyst formation in any of the species. Our data indicate that both reliable token cues (such as temperature) and ultimate causes (for example, nutrient depletion) for encystment are likely involved in the cyst-formation process. Such duality might provide an explanation for multiple triggers inducing encystment in laboratory settings and the lack of evidence for a direct relationship between nutrient depletion and cyst formation in the field.	[Kremp, Anke] Univ Helsinki, Tvarminne Zool Stn, Hango, Finland; [Rengefors, Karin] Lund Univ, Dept Ecol, S-22362 Lund, Sweden; [Montresor, Marina] Stn Zool Anton Dohrn, Naples, Italy	University of Helsinki; Lund University; Stazione Zoologica Anton Dohrn	Kremp, A (通讯作者)，Finnish Environm Inst, Ctr Marine Res, Helsinki, Finland.	anke.kremp@ymparisto.fi	Kremp, Anke/I-8139-2013; Rengefors, Karin/K-5873-2019	Montresor, Marina/0000-0002-2475-1787; Rengefors, Karin/0000-0001-6297-9734	European Commission [SEED GOCE-CT-2005-003875]; Academy of Finland [111336]	European Commission(European Union (EU)European Commission Joint Research Centre); Academy of Finland(Research Council of Finland)	We thank the staff of the Tvarminne Zoological Station, particularly Elina Salminen, Mervi Sjoblom, and Ulla Sjolund, for support in the laboratory. G. Versteegh and one anonymous reviewer are thanked for their valuable comments on the manuscript. This work was supported by grants from the European Commission (SEED GOCE-CT-2005-003875) and the Academy of Finland (grant 111336).	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Oceanogr.	JUL	2009	54	4					1125	1138		10.4319/lo.2009.54.4.1125	http://dx.doi.org/10.4319/lo.2009.54.4.1125			14	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	474ZZ		Bronze			2025-03-11	WOS:000268325100009
J	Smith, BC; Persson, A; Wikfors, GH				Smith, Barry C.; Persson, Agneta; Wikfors, Gary H.			A particle separator used to concentrate Dinoflagellate cysts from sediment	LIMNOLOGY AND OCEANOGRAPHY-METHODS			English	Article							RESTING CYSTS	A device has been developed to separate and collect large numbers of dinoflagellate cysts from sediment samples of several liters volume. The apparatus consists of a 152.5 x 44.5 x 38-cm fiberglass tank with a 20-mu m screen inserted diagonally across the long dimension, creating an inclined plane as the bottom of a settling tank. A peristaltic pump delivers resuspended bottom material to the top of the deep end of the tank. The particles settle according to mass and friction as the water moves to a drain near the top center of the shallow end of the screen. The desired particles can be vacuumed from specific areas of the screen and further refined with a final sieving step. More than 16 L marine mud were processed in this apparatus at one time. In a reference sediment sample collected from beneath New Haven Harbor (Connecticut, USA), cyst recovery was 25% for living cysts. The sediment in the uppermost part of the sorter had approximately 376 times more cysts/mL than the sediment originally added. The cyst fraction (particles 20-100 mu m) contained ten times more cysts in the uppermost part of the sorter than at the middle or lower ends. Cysts within the cyst-rich zone of the separator settled differently depending upon species, size, and morphology.	[Smith, Barry C.; Persson, Agneta; Wikfors, Gary H.] Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Smith, BC (通讯作者)，Natl Ocean & Atmospher Adm, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA.	barry.smith@noaa.gov						AMORIM A, 2001, THESIS U LISSABON; ANDERSON DM, 1983, MAR BIOL, V76, P179, DOI 10.1007/BF00392734; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; Capriulo GM, 2002, HYDROBIOLOGIA, V475, P263, DOI 10.1023/A:1020387325081; Conover S. A. MacM., 1956, Bulletin of the Bingham Oceanographic Collection, V15, P62; Dale B., 1983, P69; DORIN M, 1994, T1785A BECKM INSTR I; Erard-Le Denn Evelyne, 1995, P725; Hallegraeff G. M., 2004, Manual on Harmful Marine Microalgae; Landsberg JH, 2002, REV FISH SCI, V10, P113, DOI 10.1080/20026491051695; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Rings A, 2004, LIMNOL OCEANOGR-METH, V2, P25, DOI 10.4319/lom.2004.2.25; Smith BC, 2004, J APPL PHYCOL, V16, P401, DOI 10.1023/B:JAPH.0000047951.72497.53	15	6	6	1	2	AMER SOC LIMNOLOGY OCEANOGRAPHY	WACO	5400 BOSQUE BLVD, STE 680, WACO, TX 76710-4446 USA	1541-5856			LIMNOL OCEANOGR-METH	Limnol. Oceanogr. Meth.	JUL	2009	7						521	526		10.4319/lom.2009.7.521	http://dx.doi.org/10.4319/lom.2009.7.521			6	Limnology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology; Oceanography	481UY					2025-03-11	WOS:000268838700006
J	Harper, JDI; Thuet, J; Lechtreck, KF; Hardham, AR				Harper, John D. I.; Thuet, Jacques; Lechtreck, Karl F.; Hardham, Adrienne R.			Proteins related to green algal striated fiber assemblin are present in stramenopiles and alveolates	PROTOPLASMA			English	Article						Assemblin; Alveolates; Flagellar apparatus; Phytophthora; Oomycetes; Striated fiber; Stramenopiles; Thalassiosira	MICROTUBULE-ASSOCIATED FIBERS; SEGMENTED COILED-COIL; PHYTOPHTHORA-CINNAMOMI; FLAGELLAR APPARATUS; 2-NM FILAMENTS; SF-ASSEMBLIN; PREDICTION; CENTRIN; SPORES; FORMS	In green algae, striated fiber assemblin (SFA) is the major protein of the striated microtubule-associated fibers that are structural elements in the flagellar basal apparatus. Using Basic Local Alignment Search Tool (BLAST) searches of recently established databases, SFA-like sequences were detected in the genomes not only of green algal species but also of a range of other protists. These included species in two alveolate subgroups, the ciliates (Tetrahymena thermophila, Paramecium tetraurelia) and the dinoflagellates (Perkinsus marinus), and two stramenopile subgroups, the oomycetes (Phytophthora sojae, Phytophthora ramorum, Phytophthora infestans) and the diatoms (Thalassiosira pseudonana, Phaeodactylum tricornutum). Together with earlier identification of SFA-like sequences in the apicomplexans, these results indicate that homologs of SFA are present across the alveolates and stramenopiles. Antibodies raised against SFA from the green alga, Spermatozopsis similis, react in immunofluorescence assays with the two basal bodies and an anteriorly directed striated fiber in the flagellar apparatus of biflagellate Phytophthora zoospores.	[Harper, John D. I.; Thuet, Jacques; Hardham, Adrienne R.] Australian Natl Univ, Plant Cell Biol Grp, Sch Biol, Canberra, ACT 0200, Australia; [Harper, John D. I.] New S Wales Dept Primary Ind, EH Graham Ctr Agr Innovat, Wagga Wagga, NSW 2678, Australia; [Harper, John D. I.] Charles Sturt Univ, EH Graham Ctr Agr Innovat, Wagga Wagga, NSW 2678, Australia; [Lechtreck, Karl F.] Univ Massachusetts, Sch Med, Dept Cell Biol, Worcester, MA 01655 USA	Australian National University; Department of Primary Industries & Regional Development NSW; Charles Sturt University; University of Massachusetts System; University of Massachusetts Worcester	Hardham, AR (通讯作者)，Australian Natl Univ, Plant Cell Biol Grp, Sch Biol, GPO Box 4, Canberra, ACT 0200, Australia.	Adrienne.hardham@anu.edu.au	Hardham, Adrienne/C-9674-2009	Lechtreck, Karl/0000-0002-6219-6470; Harper, John/0000-0002-0262-5632	Charles Sturt University	Charles Sturt University	We thank Dr. Frank Gubler for providing the image in Fig. 1e. This work was partially funded by a special studies program and a multidisciplinary grant from Charles Sturt University to JDIH.	ALLEN RD, 1967, J PROTOZOOL, V14, P553, DOI 10.1111/j.1550-7408.1967.tb02042.x; [Anonymous], MOL CELL BIOL FILAME; BARON AT, 1992, BIOL CELL, V76, P383, DOI 10.1016/0248-4900(92)90442-4; HARDHAM AR, 1987, PROTOPLASMA, V137, P109, DOI 10.1007/BF01281146; HARPER JDI, 1995, PROTOPLASMA, V188, P225, DOI 10.1007/BF01280374; HOLBERTON D, 1988, J MOL BIOL, V204, P789, DOI 10.1016/0022-2836(88)90370-1; Joiner KA, 2002, J CELL BIOL, V157, P557, DOI 10.1083/jcb.200112144; LECHTRECK KF, 1991, J CELL BIOL, V115, P705, DOI 10.1083/jcb.115.3.705; Lechtreck KF, 1998, CELL MOTIL CYTOSKEL, V41, P289, DOI 10.1002/(SICI)1097-0169(1998)41:4<289::AID-CM2>3.0.CO;2-1; Lechtreck KF, 2003, MOL BIOCHEM PARASIT, V128, P95, DOI 10.1016/S0166-6851(03)00038-0; Lupas A, 1996, METHOD ENZYMOL, V266, P513; Patterson David J., 1992, P13; Pollastri G, 2005, BIOINFORMATICS, V21, P1719, DOI 10.1093/bioinformatics/bti203; Robold AV, 2005, CURR GENET, V47, P307, DOI 10.1007/s00294-004-0559-8; Saldarriaga JF, 2003, INT J SYST EVOL MICR, V53, P355, DOI 10.1099/ijs.0.02328-0; SPERLING L, 1991, DEV BIOL, V148, P205, DOI 10.1016/0012-1606(91)90330-6; Van de Peer Y, 1997, J MOL EVOL, V45, P619, DOI 10.1007/PL00006266; VandePeer Y, 1996, J MOL EVOL, V42, P201, DOI 10.1007/BF02198846; WEBER K, 1993, J CELL BIOL, V121, P837, DOI 10.1083/jcb.121.4.837	19	10	12	1	11	SPRINGER WIEN	WIEN	SACHSENPLATZ 4-6, PO BOX 89, A-1201 WIEN, AUSTRIA	0033-183X	1615-6102		PROTOPLASMA	Protoplasma	JUL	2009	236	1-4					97	101		10.1007/s00709-009-0041-z	http://dx.doi.org/10.1007/s00709-009-0041-z			5	Plant Sciences; Cell Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Cell Biology	471PL	19333716				2025-03-11	WOS:000268070400012
J	Orlova, TY; Morozova, TV				Orlova, T. Yu.; Morozova, T. V.			Resting stages of microalgae in recent marine sediments of Peter the Great Bay, Sea of Japan	RUSSIAN JOURNAL OF MARINE BIOLOGY			English	Article						Dinoflagellate cysts; resting stage; spores; resting cells; microalgae; Peter the Great Bay; Sea of Japan	MODERN DINOFLAGELLATE CYSTS; TOKYO-BAY; RED-TIDE; GONYAULAX-EXCAVATA; COASTAL SEDIMENTS; YOKOHAMA-PORT; EAST-COAST; NORTH-SEA; EUTROPHICATION; RAPHIDOPHYCEAE	Data on the qualitative and quantitative composition of resting stages of planktonic microalgae in recent marine sediments of Peter the Great Bay (Sea of Japan) over the period 2000-2007 are presented. A total of sixty one morphological forms of resting stages represented by dinoflagellate and raphidophyte cysts and diatom spores and resting cells were recorded in the sediment samples. This study revealed cysts of the potentially toxic species Alexandrium tamarense, A. cf. minutum, Alexandrium sp., Gymnodinium catenatum (PSP toxin producers), and Protoceratium reticulatum (yessotoxin producer); resting cells of Pseudo-nitzschia sp. (potential producer of domoic acid); and cysts of bloom-forming species Cochlodinium cf. polykrikoides and Heterosigma cf. akashiwo.	[Orlova, T. Yu.; Morozova, T. V.] Russian Acad Sci, Far E Div, AV Zhirmunsky Inst Marine Biol, Vladivostok 690041, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Orlova, TY (通讯作者)，Russian Acad Sci, Far E Div, AV Zhirmunsky Inst Marine Biol, Vladivostok 690041, Russia.	torlova06@mail.ru	Morozova, Tatiana/G-4468-2018; Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967	Russian Foundation for Basic Research [06-04-48649, 08-04-01422]; RAS; Far East Division of RAS [06-III-A-06-167, 06-I-II-11-034, 06-I-II-16-057, 09-III-A-06-213, 09-I-II-15-03, 09-I-II-23-01, 09-I-II23-12]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); RAS(Russian Academy of SciencesRegione Sardegna); Far East Division of RAS	This investigation was supported by grants from the Russian Foundation for Basic Research (no. 06-04-48649 and 08-04-01422), Far East Division of the RAS and Russian Foundation for Basic Research (no. 09-04-98570-r_vostok_a), and Far East Division of RAS (nos. 06-III-A-06-167, 06-I-II-11-034, 06-I-II-16-057, 09-III-A-06-213, 09-I-II-15-03, 09-I-II-23-01 and 09-I-II23- 12); partial support was provided under the World Ocean Federal Program for 2008-2012, federal contract no. 01.420.1.2.0003 of November 7, 2008.	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V., 1995, Biologiya Morya (Vladivostok), V21, P403; SUTRE MML, 1997, MAR ENVIRON RES, V44, P167; Thorsen TA, 1997, HOLOCENE, V7, P433, DOI 10.1177/095968369700700406; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	54	26	28	1	22	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1063-0740	1608-3377		RUSS J MAR BIOL+	Russ. J. Mar. Biol.	JUL	2009	35	4					313	322		10.1134/S1063074009040063	http://dx.doi.org/10.1134/S1063074009040063			10	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	495XR					2025-03-11	WOS:000269929400006
J	Rose, KD; Rana, RS; Sahni, A; Kumar, K; Singh, L; Smith, T				Rose, Kenneth D.; Rana, Rajendra S.; Sahni, Ashok; Kumar, Kishor; Singh, Lachham; Smith, Thierry			First tillodont from India: Additional evidence for an early Eocene faunal connection between Europe and India?	ACTA PALAEONTOLOGICA POLONICA			English	Article							VASTAN LIGNITE MINE; WESTERN INDIA; MIDDLE EOCENE; MAMMALIA; PAKISTAN; GUJARAT; AGE	Vastan Lignite Mine in southeastern Gujarat, India, produces the oldest known Cenozoic land-mammals and the only early Eocene continental vertebrate fauna known from India (e.g., Bajpai et al. 2005; Rana et al. 2005, 2008; Rose et al. 2006, 1008, 2009; Smith et al. 2007; Rage et al. 2008). The fauna comes from the Cambay Shale Formation and has been dated as middle Ypresian (similar to 52 Ma, early Cuisian) based on a common nummulitid foraminiferan from about 15 m above the vertebrate-producing layer (Sahni et al. 2006; Rana et al. 2008). However, a recent study of dinoflagellate cysts from the section suggests that the deposits may be as old as 54-55 Ma (Garg et al. 2008). Although some elements of the fauna, such as anthracobunids and lagomorphs, have Asian affinities, a surprising number of taxa among the snakes, bats, insectivores, primates, rodents, and artiodactyls appear to be most closely related to early Eocene European or North American taxa. This may simply reflect the poor state of knowledge of contemporary south Asian vertebrate faunas; alternatively, it might be evidence of previously unsuspected early Eocene faunal exchange between Europe and southwest Asia. We report here two teeth of a tillodont from Vastan Mine, which constitute the first record of the mammalian order Tillodontia known from India. Despite the much greater generic diversity of tillodonts in Asia than elsewhere, the Vastan tillodont shows clear affinities with Euramerican esthonychines.	[Rose, Kenneth D.] Johns Hopkins Univ, Sch Med, Ctr Funct Anat & Evolut, Baltimore, MD 21205 USA; [Rana, Rajendra S.; Singh, Lachham] HNB Garhwal Univ, Dept Geol, Srinagar 246175, Uttarakhand, India; [Sahni, Ashok] Panjab Univ, Dept Geol, Sector 14, Chandigarh 160014, India; [Kumar, Kishor] Wadia Inst Himalayan Geol, Dehra Dun 248001, Uttarakhand, India; [Smith, Thierry] Royal Belgian Inst Nat Sci, Dept Paleontol, B-1000 Brussels, Belgium	Johns Hopkins University; Hemwati Nandan Bahuguna Garhwal University; Panjab University; Department of Science & Technology (India); Wadia Institute of Himalayan Geology (WIHG); Royal Belgian Institute of Natural Sciences	Rose, KD (通讯作者)，Johns Hopkins Univ, Sch Med, Ctr Funct Anat & Evolut, 1830 E Monument St, Baltimore, MD 21205 USA.	kdrose@jhmi.edu; Rajendra.Rana1@gmail.com; ashok.sahni@gmail.com; kumark@wihg.res.in; rawat.lachham@yahoo.com; Thierry.Smith@naturalsciences.be	KUMAR, Kishor/H-7232-2013	Smith, Thierry/0000-0002-1795-2564				[Anonymous], 1997, Classification of Mammals Above the Species Level; Bajpai Sunil, 2005, Journal of the Palaeontological Society of India, V50, P101; Baudry Mylene, 1992, Bulletin du Museum National d'Histoire Naturelle Section C Sciences de la Terre Paleontologie Geologie Mineralogie, V14, P205; Chow M.-C., 1996, AM MUS NOVIT, V3171, P1; Garg Rahul, 2008, Journal of the Palaeontological Society of India, V53, P99; Gazin C.L., 1953, SMITHSONIAN MISCELLA, V121, P1; GINGERICH P D, 1979, Contributions from the Museum of Paleontology University of Michigan, V25, P125; Gingerich P.D., 2001, EOCENE BIODIVERSITY, P251, DOI 10.1007/978-1-4615-1271-4_10; Gingerich P.D., 1989, University of Michigan Papers on Paleontology, V28, P1; Gingerich PD, 2003, J VERTEBR PALEONTOL, V23, P643, DOI 10.1671/2409; Gunnell Gregg F., 2008, Contributions from the Museum of Paleontology University of Michigan, V32, P1; Huang Xue-Shi, 2003, Vertebrata Palasiatica, V41, P131; Huang Xue-Shi, 1999, Vertebrata Palasiatica, V37, P96; Lucas S.G., 1981, Mitteilungen der Bayerischen Staatssammlung fuer Palaeontologie und Historische Geologie, V21, P89; Lucas S.G., 2004, Bulletin of the New Mexico Museum of Natural History and Science, V26, P45; LUCAS S. G., 1998, EVOLUTION TERTIARY M, V1, P268; LUCAS SG, 1993, MAMMAL PHYLOGENY : PLACENTALS, P182; MINCHEN C, 1979, VERTEBRAT PALASIATIC, V17, P37; Miyata Kazunori, 1998, Paleontological Research, V2, P53; Nel A, 1999, CR ACAD SCI II A, V329, P65, DOI 10.1016/S1251-8050(99)80229-8; Rage JC, 2008, ACTA PALAEONTOL POL, V53, P391, DOI 10.4202/app.2008.0303; Rana R.S., 2005, Journal of the Palaeontological Society of India, V50, P93; Rana RS, 2008, ACTA PALAEONTOL POL, V53, P1, DOI 10.4202/app.2008.0101; Rose K., 2006, The Beginning of the Age of Mammals, DOI DOI 10.56021/9780801884726; Rose K.D., 1981, University of Michigan Papers in Paleontology, V26, P1; Rose KD, 2006, J VERTEBR PALEONTOL, V26, P219, DOI 10.1671/0272-4634(2006)26[219:EEYCVA]2.0.CO;2; Rose KD, 2008, P ROY SOC B-BIOL SCI, V275, P1203, DOI 10.1098/rspb.2007.1661; Rose KD, 2009, J HUM EVOL, V56, P366, DOI 10.1016/j.jhevol.2009.01.008; Sahni A., 2006, INDIAN J PET GEOL, V15, P1, DOI DOI 10.4202/APP.2008.0101; Smith T, 2007, NATURWISSENSCHAFTEN, V94, P1003, DOI 10.1007/s00114-007-0280-9; STUCKY R K, 1983, Annals of Carnegie Museum, V52, P375; Ting Suyin, 1989, Vertebrata Palasiatica, V27, P77; Tong Y., 2006, PALAEONTOL SINICA, V28, P1; Tong Yong-Sheng, 2003, Vertebrata Palasiatica, V41, P55; Wang Yuan-Qing, 2004, Vertebrata Palasiatica, V42, P13	35	26	28	0	4	INST PALEOBIOLOGII PAN	WARSAW	UL TWARDA 51/55, 00-818 WARSAW, POLAND	0567-7920	1732-2421		ACTA PALAEONTOL POL	Acta Palaeontol. Pol.	JUN	2009	54	2					351	355		10.4202/app.2008.0067	http://dx.doi.org/10.4202/app.2008.0067			5	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	466PA		Green Submitted, gold			2025-03-11	WOS:000267673300013
J	Boere, AC; Abbas, B; Rijpstra, WIC; Versteegh, GJM; Volkman, JK; Damsté, JSS; Coolen, MJL				Boere, A. C.; Abbas, B.; Rijpstra, W. I. C.; Versteegh, G. J. M.; Volkman, J. K.; Damste, J. S. Sinninghe; Coolen, M. J. L.			Late-Holocene succession of dinoflagellates in an Antarctic fjord using a multi-proxy approach: paleoenvironmental genomics, lipid biomarkers and palynomorphs	GEOBIOLOGY			English	Article							ACE LAKE ANTARCTICA; ELLIS FJORD; VESTFOLD HILLS; ROSS SEA; FAST-ICE; STEROL COMPOSITION; PHYTOPLANKTON SUCCESSION; MARINE DINOFLAGELLATE; POLARELLA-GLACIALIS; SURFACE SEDIMENTS	Recent work has shown that paleoenvironmental genomics, i.e. the application of genomic tools to analyze preserved DNA in sedimentary records, is a promising approach to reconstruct the diversity of past planktonic communities. This provides information about past ecological and environmental changes. A major advantage of this approach is that individual species, including those that did not leave other characteristic markers, can be identified. In this study, we determined which dinoflagellate marker (i.e. 18S rDNA, dinosterol or dinocysts) provided the most detailed information about the late-Holocene succession of dinoflagellates in an Antarctic Fjord (Ellis Fjord, Vestfold Hills). The preserved rDNA revealed two intervals in the 2750-year-old sediment record. The dinoflagellate diversity was the highest until similar to 1850 cal yr BP and included phylotypes related to known dinosterol producers. A lower concentration of dinosterol in sediments <1850 cal yr BP coincided with a community shift towards a predominance of the autotrophic sea-ice dinoflagellate Polarella glacialis, which is not a source of dinosterol. Remarkably, cultures of P. glacialis are known to produce other diagnostic sterols, but these were not recovered here. In addition, conspicuous resting cysts of P. glacialis were not preserved in the analyzed sediments. Overall, dinocysts were rare and the paleoenvironmental genomics approach revealed the highest diversity of dinoflagellates in Ellis Fjord, and was the only approach that recorded a shift in dinoflagellate composition at similar to 1850 cal yr BP indicative of a colder climate with more extensive ice cover-this timing coincides with a period of changing climate reported for this region.	[Boere, A. C.; Abbas, B.; Rijpstra, W. I. C.; Damste, J. S. Sinninghe; Coolen, M. J. L.] NIOZ, Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, Den Burg, Netherlands; [Versteegh, G. J. M.] Univ Bremen, Dept Organ Geochem, Bremen, Germany; [Volkman, J. K.] CSIRO Marine & Atmospher Res, Hobart, Tas, Australia; [Coolen, M. J. L.] Woods Hole Oceanog Inst, Dept Marine Chem & Geochem, Woods Hole, MA 02543 USA	Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bremen; Commonwealth Scientific & Industrial Research Organisation (CSIRO); Woods Hole Oceanographic Institution	Boere, AC (通讯作者)，NIOZ, Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, Den Burg, Netherlands.	arjan.boere@nioz.nl	Volkman, John/A-6592-2008; Sinninghe Damste, Jaap/F-6128-2011; Versteegh, Gerard J.M./H-2119-2011; Coolen, Marco/B-8263-2015	Sinninghe Damste, Jaap/0000-0002-8683-1854; Versteegh, Gerard J.M./0000-0002-9320-3776; Coolen, Marco/0000-0002-0417-920X	Australian Antarctic Science Advisory Committee [1166]; Netherlands Organization for Scientific Research [851.20.006, 813.03.001, 863.04.020]; German Science Foundation [VE486/3-1]	Australian Antarctic Science Advisory Committee; Netherlands Organization for Scientific Research(Netherlands Organization for Scientific Research (NWO)); German Science Foundation(German Research Foundation (DFG))	We thank Dr Cornelia Wuchter, Peter Thompson and the crew of Australian Antarctic Division for help with obtaining the samples and core, and Anna Noordeloos for providing cultures of A. minutum and Scrippsiella sp. used to develop the dinoflagellate- specific primers. Two anonymous reviewers are thanked for helpful comments on an earlier version of the manuscript. This work was supported by grants from the Australian Antarctic Science Advisory Committee (1166 to J. K. V.), the Netherlands Organization for Scientific Research (NWO; 851.20.006 to J. S. S. D.; NWO grant 813.03.001 and NWO-VENI grant 863.04.020 to M. J. L. C.) and the German Science Foundation (DFG grant VE486/3-1) to GJMV.	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J	Spatharis, S; Dolapsakis, NP; Economou-Amilli, A; Tsirtsis, G; Danielidis, DB				Spatharis, Sofie; Dolapsakis, Nicolas P.; Economou-Amilli, Athena; Tsirtsis, George; Danielidis, Daniel B.			Dynamics of potentially harmful microalgae in a confined Mediterranean Gulf-Assessing the risk of bloom formation	HARMFUL ALGAE			English	Article						Abundance-occupancy; Heterocapsa; Karlodinium; Scrippsiella; Toxic microalgae	ALGAL BLOOMS; DOMOIC ACID; PHYTOPLANKTON; EUTROPHICATION; DINOPHYCEAE; CALIFORNIA; CERATIUM; SEA	The population dynamics of potentially harmful microalgae was investigated in the semi-enclosed shallow Gulf of Kalloni, Greece (Aegean Sea, Eastern Mediterranean), during a 2-year period from August 2004 to March 2006. A total of 21 potentially harmful microalgae (bloom-forming and/or toxic) were identified including 3 diatoms and 18 dinoflagellates. The densities of each species were analyzed in time and space and in relation to environmental parameters. Some species such as Alexandrium insuetum, Heterocapsa circularisquama, Karlodinium veneficum, Scrippsiella trochoidea, and Ceratium spp. developed high cell concentrations, particularly during a Pseudo-nitzschia calliantha winter bloom. Other species such as Dinophysis caudata, Ostreopsis ovata, Prorocentrurn minimum, and Protoperidinium crassipes were rare or appeared in small numbers. Densities of the most abundant species were closely associated with freshwater nutrient-rich inputs during winter, being negatively correlated with temperature and salinity and positively correlated with nitrogen. The spatial distribution of the abundant species exhibited a marked increase towards the inner part of the gulf, close to the main freshwater inputs, whereas some species were mainly concentrated in the dilute surface layer (1 m depth). Examination of the abundance-occupancy relationship revealed that the species more prone to bloom are those with wide spatial distribution and frequent presence throughout the year such as the diatom P. calliantha. Although blooms of cyst-forming species are rarer, an increased risk can be foreseen under favorable resource supply and environmental conditions during winter. (C) 2009 Elsevier B.V. All rights reserved.	[Spatharis, Sofie; Tsirtsis, George] Univ Aegean, Dept Marine Sci, Mitilini 81100, Greece; [Dolapsakis, Nicolas P.; Economou-Amilli, Athena; Danielidis, Daniel B.] Univ Athens, Fac Biol, Dept Systemat & Ecol, Athens 15784, Greece	University of Aegean; National & Kapodistrian University of Athens	Spatharis, S (通讯作者)，Univ Aegean, Dept Marine Sci, Univ Hill, Mitilini 81100, Greece.	spathari@marine.aegean.gr	Spatharis, Sofie/I-9193-2019; Danielidis, Daniel/D-3907-2009	Tsirtsis, George/0000-0002-2485-2684; ECONOMOU-AMILLI, Athena/0000-0002-5615-1372				Anderson D.M., 1985, P219; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; [Anonymous], J RECHERCHE OCEANOGR; Baric A, 2003, SCI MAR, V67, P129, DOI 10.3989/scimar.2003.67n2129; BURKHOLDER JM, 2008, ECOLOGY HARMFUL ALGA, P53; Cembella Allan D., 2005, Oceanography, V18, P158; Collos Y, 2004, J PHYCOL, V40, P96, DOI 10.1046/j.1529-8817.2004.03034.x; Dolapsakis NP, 2008, J BIOL RES-THESSALON, V9, P89; Feyzioglu Ali Muzaffer, 2006, Turkish Journal of Botany, V30, P375; Figueiras FG, 2006, ECOL STU AN, V189, P127, DOI 10.1007/978-3-540-32210-8_10; Gárate-Lizárraga I, 2008, ACTA BOT MEX, V83, P33, DOI 10.21829/abm83.2008.1059; Gaston KJ, 2000, J APPL ECOL, V37, P39, DOI 10.1046/j.1365-2664.2000.00485.x; Gaston KJ, 1996, OIKOS, V76, P211, DOI 10.2307/3546192; Glibert Patricia M., 2002, Harmful Algae, V1, P215, DOI 10.1016/S1568-9883(02)00013-6; Graneli E., 2006, Ecology of Harmful Algae; Guillard R.R. 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J	Ghasemi-Nejad, E; Head, MJ; Naderi, M				Ghasemi-Nejad, Ebrahim; Head, Martin J.; Naderi, Mehrangiz			Palynology and petroleum potential of the Kazhdumi Formation (Cretaceous: Albian-Cenomanian) in the South Pars field, northern Persian Gulf	MARINE AND PETROLEUM GEOLOGY			English	Article						Palynology; Palynofacies; Geochemical analyses; Petroleum potential; Kazhdumi Formation; Persian Gulf	BELT	The Kazhdumi Formation of the Bangestan Group is a well-known source rock that has produced abundant oil in most petroleum fields in the Zagros Basin, which stretches from northwest to southwest Iran over hundreds of kilometres. The formation reaches a thickness of 230 m at the type section in northwest Zagros but thins out to 40-50 m in wells studied from the South Pars giant petroleum field, where it comprises mainly grey shales with occasional intercalations of marls and sandstones. South Pars, best known as the Iranian part of the world's largest non-associated gas field, contains small quantities of oil above and below the Kazhdumi Formation. Palynology has been used to assess the age and palaeoenvironment of the Kazhdumi Formation and to evaluate its petroleum potential. A total of 68 ditch cutting samples recovered from five wells, of which four are oil-prone, have been analyzed. An age between late Albian and Cenomanian is established for the formation based on dinoflagellate cyst biostratigraphy, and four palynofacies types have been recognized using the relative proportions of terrestrial elements, marine palynomorphs and amorphous organic matter (AOM). The ratio of terrestrial to marine elements is high in most samples, indicating a nearshore sedimentary environment. Twenty-two samples from the four oil-prone wells were also selected for geochemical analysis using Rock-Eval pyrolysis. Results show that the Kazhdumi Formation at South Pars, in contrast to the Zagros Basin, is gas-prone (predominantly type III kerogen), thermally immature, and poor in terms of hydrocarbon generation. It could not have produced the oil in those oil-prone wells studied. (C) 2008 Elsevier Ltd. All rights reserved.	[Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Ghasemi-Nejad, Ebrahim; Naderi, Mehrangiz] Univ Tehran, Fac Sci, Dept Geol, Tehran 14174, Iran	Brock University; University of Tehran	Head, MJ (通讯作者)，Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada.	eghasemi@khayam.ut.ac.ir; mjhead@brocku.ca	Ghasemi-Nejad, Ebrahim/AAF-6087-2020	Ghasemi-Nejad, Ebrahim/0000-0002-4421-5068	South Pars Oil and Gas Company of Iran; University of Tehran; Natural Sciences and Engineering Research Council of Canada	South Pars Oil and Gas Company of Iran; University of Tehran(University of Tehran); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	The authors wish to thank the research directorate of the South Pars Oil and Gas Company of Iran and the Vice Chancellor for Research of the University of Tehran for financial support. We are grateful to the National Iranian Oil Company (NIOC) for the provision of samples. MJH acknowledges funding from a Natural Sciences and Engineering Research Council of Canada discovery grant. S.Y. El Beialy (Mansoura University, Egypt) is thanked for many useful discussions. M. Lozon of Brock University kindly assisted with drafting. We are grateful to D.J. Batten (University of Manchester) and J.B. Riding (British Geological Survey, Keyworth) for their helpful reviews.	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Pet. Geol.	JUN	2009	26	6					805	816		10.1016/j.marpetgeo.2008.05.005	http://dx.doi.org/10.1016/j.marpetgeo.2008.05.005			12	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	457CQ					2025-03-11	WOS:000266903600006
J	Helenes, J; Carreño, AL; Carrillo, RM				Helenes, J.; Carreno, A. L.; Carrillo, R. M.			Middle to late Miocene chronostratigraphy and development of the northern Gulf of California	MARINE MICROPALEONTOLOGY			English	Review						Gulf of California; middle Miocene; dinoflagellates; calcareous nannofossils	DINOFLAGELLATE CYST GENUS; COLORADO RIVER DELTA; BAJA-CALIFORNIA; NEOGENE STRATIGRAPHY; NORTHWESTERN MEXICO; SALTON TROUGH; MARIA-MADRE; EXTENSION; VOLCANISM; PLIOCENE	Geologic models locate Baja California next to mainland Mexico during the Oligocene and propose opening of the Gulf of California during Miocene times. Outcrop information in the northern part of the Gulf indicates late Miocene marine sedimentation on a continental platform. However, the earliest marine sediments in the region are present in basins sampled by oil exploratory wells in the area, which drilled as much as 5591 m of marine sands to silty clays. Stratigraphic and paleontological data in these wells indicate almost continuous marine sedimentation from middle Miocene times, in maximum water depths of approximately 200 m. The presence of the dinoflagellates Cribroperidinium tenuitabutatum, Diphyes latiusculum and Spiniferites pseudofurcatus, together with the nannofossil Cyclicargolithus floridanus in samples from some of these wells, indicates marine deposition during middle Miocene times in the Tiburon, Consag and Wagner basins in the northern Gulf of California. Our data indicate that in the middle Miocene, a marine proto-gulf basin was formed in the central part of the proto-gulf, probably related to Basin and Range extension. Published data indicate that during late Miocene times, the proto-gulf extended from southeastern California and southern Arizona, to central Baja California and Isla Tiburon. Finally. by Pliocene times, marine sedimentation within the Gulf reached the modern distribution. (C) 2009 Elsevier B.V. All rights reserved.	[Helenes, J.; Carrillo, R. M.] CICESE, Dept Geol, Ensenada 22860, Baja California, Mexico; [Carreno, A. L.] Univ Nacl Autonoma Mexico, Inst Geol, CU, Mexico City 04510, DF, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; Universidad Nacional Autonoma de Mexico	Helenes, J (通讯作者)，CICESE, Dept Geol, Km 107 Carretera Tijuana, Ensenada 22860, Baja California, Mexico.	jhelenes@cicese.mx; anacar@geologia.unam.mx	Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879	PAPIIT [IN116308]	PAPIIT(Programa de Apoyo a Proyectos de Investigacion e Innovacion Tecnologica (PAPIIT))	Thanks to Petroleos Mexicanos Exploracion y Produccion for their financial support during this study, for making available samples and data for the analyses and for the permission to publish these results. 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JUN	2009	72	1-2					10	25		10.1016/j.marmicro.2009.02.003	http://dx.doi.org/10.1016/j.marmicro.2009.02.003			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	464OT					2025-03-11	WOS:000267515500002
J	Kobayashi, J				Kobayashi, Jun'ichi			Chemistry and biology of Okinawan marine natural products	PURE AND APPLIED CHEMISTRY			English	Article; Proceedings Paper	IUPAC International Conference on Biodiversity and Natural Products	JUL 13-18, 2008	Charlottetown, CANADA			marine natural products; tunicates; dinoflagellates; sponges; alkaloids; polyketides; terpenoids	SESQUITERPENOID QUINONES; THEONEZOLIDE-A; EUDISTOMIN-D; SPONGE; MACROLIDE; AMPHIDINOLACTONE; STEREOCHEMISTRY; MOIETY	Marine macro- and micro-organisms collected in Okinawa are good sources of compounds with intriguing structures and interesting biological activities. Synthetic hybrid molecules of caffeine and eudistomin D from tunicates Eudistoma sp. were found to show better potency as adenosine receptor ligands than caffeine, and one of them exhibits potent activity for adenosine receptors tested, especially for A(3) subtype. Potent cytotoxic polyene macrolides from a tunicate Cystodytes sp. were found to be potent osteoclast inhibitors and to inhibit vacuolar type H+-ATPase (V-ATPase) of both mammalian and yeast cells. Amphidinolactones A and B are new macrolides from a dinoflagellate Amphidinium sp., and a potent cytotoxic macrolide from another strain was found to target actin cytoskeleton. Theonezolide A, a long-chain polyketide from a sponge Theonella sp., induces a drastic shape change in platelets by reorganization of microtubules. The stereochemistry of many chiral centers in theonezolide A was elucidated by spectral data and chemical means. Metachromins L-Q are new sesquiterpenoid quinones with an amino acid residue, while nakijiquinones E and F were the first dimeric sesquiterpenoid quinones possessing a 3-aminobenzoate moiety. Halichonadin E is the first hetero-dimeric sesquiterpenoid with eudesmane and aromadendrane skeletons linked through a urea fragment isolated from a sponge Halichondria sp. Pyrinadine A and nakinadine A are novel bis-pyridine alkaloids from sponges, while nagelamides are new bromopyrrole alkaloids from a sponge Agelas sp. Here, the structures and bioactivities of these interesting marine natural products will be described.	Hokkaido Univ, Grad Sch Pharmaceut Sci, Sapporo, Hokkaido 0600812, Japan	Hokkaido University	Kobayashi, J (通讯作者)，Hokkaido Univ, Grad Sch Pharmaceut Sci, Sapporo, Hokkaido 0600812, Japan.		Kobayashi, Jun'ichi/A-4253-2012					Araki A, 2008, ORG LETT, V10, P2099, DOI 10.1021/ol8003904; Ishiyama H, 2008, J NAT PROD, V71, P1301, DOI 10.1021/np800164s; Ishiyama H, 2008, BIOORGAN MED CHEM, V16, P3825, DOI 10.1016/j.bmc.2008.01.041; Kariya Y, 2006, TETRAHEDRON LETT, V47, P997, DOI 10.1016/j.tetlet.2005.11.163; Kazami S, 2006, BIOSCI BIOTECH BIOCH, V70, P1364, DOI 10.1271/bbb.50644; Kobayashi J, 1998, HETEROCYCLES, V49, P39, DOI 10.3987/COM-97-S6-1; KOBAYASHI J, 1993, J AM CHEM SOC, V115, P6661, DOI 10.1021/ja00068a024; Kobayashi J, 2008, J ANTIBIOT, V61, P271, DOI 10.1038/ja.2008.39; Kobayashi J, 2007, J NAT PROD, V70, P451, DOI 10.1021/np0605844; KONDO K, 1994, TETRAHEDRON, V50, P8355, DOI 10.1016/S0040-4020(01)85558-7; Kozawa S, 2008, J NAT PROD, V71, P445, DOI 10.1021/np0703139; Kubota T, 2007, TETRAHEDRON LETT, V48, P4983, DOI 10.1016/j.tetlet.2007.05.121; Mitsui-Saito M, 2002, THROMB RES, V108, P133, DOI 10.1016/S0049-3848(02)00355-9; Ohshita K, 2007, BIOORGAN MED CHEM, V15, P3235, DOI 10.1016/j.bmc.2007.02.043; Rho MC, 1996, CAN J PHYSIOL PHARM, V74, P193, DOI 10.1139/cjpp-74-2-193; Sato M, 1998, TETRAHEDRON, V54, P4819, DOI 10.1016/S0040-4020(98)00190-2; Takahashi Y, 2008, BIOORGAN MED CHEM, V16, P7561, DOI 10.1016/j.bmc.2008.07.028; Takahashi Y, 2007, TETRAHEDRON, V63, P8770, DOI 10.1016/j.tet.2007.06.031; Takahashi Y, 2007, J ANTIBIOT, V60, P376, DOI 10.1038/ja.2007.51; Takahashi Y, 2007, HETEROCYCLES, V72, P567; Takahashi Y, 2009, BIOORGAN MED CHEM, V17, P2185, DOI 10.1016/j.bmc.2008.10.080; Usui T, 2004, CHEM BIOL, V11, P1269, DOI 10.1016/j.chembiol.2004.07.014	22	14	15	1	33	WALTER DE GRUYTER GMBH	BERLIN	GENTHINER STRASSE 13, D-10785 BERLIN, GERMANY	0033-4545	1365-3075		PURE APPL CHEM	Pure Appl. Chem.	JUN	2009	81	6					1009	1018		10.1351/PAC-CON-08-08-22	http://dx.doi.org/10.1351/PAC-CON-08-08-22			10	Chemistry, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Chemistry	455NM		Bronze			2025-03-11	WOS:000266767700003
J	Zhao, Y; Morzadec-Kerfourn, MT				Zhao, YunYun; Morzadec-Kerfourn, Marie-Therese			DINOFLAGELLATE CYSTS AND QUATERNARY PALEOENVIRONMENT IN THE IZU-BONIN REGION, NORTH-WEST PACIFIC (ODP Leg 125, site 782A and Leg 126, site 791B)	QUATERNAIRE			French	Article						North-west Pacific ocean; Izu-Bonin region; deep sea sediments; ODP leg 125 and 126; dinoflagellate cysts; Quaternary	SEA-SURFACE CONDITIONS; SOUTH CHINA SEA; ADJACENT SEAS; TIMESCALE; SEDIMENTS; OCEAN	DINOFLAGELLATE CYSTS AND QUATERNARY PALEOENVIRONMENT IN THE IZU-BONIN REGION, NORTH-WEST PACIFIC (ODP Leg 125, site 782A and Leg 126, site 791 B) Fifty species of dinoflagellate cysts, among them two new species, have been identified in oceanic sediments of the Izu-Bonin region, south of Japan. All these species have a paleoenvironmental significance. The Quaternary climatic oscillation and environment evolution in the NW Pacific have been demonstrated by the variation of dinoflagellate cyst assemblages and the contents pollen grains in the arc sediments of the Izu-Bonin region. The variation of species ratios: temperate-warm to temperate-cold dinoflagellate cysts reveals the cyclic temperature changes of sea surface waters. The data are used to reconstruct the climatic evolution since 1,79 Ma ago. The results of the present study and a consideration of relevant sedimentological factors allow us to draw the following conclusions concerning the environment of the Izu-Bonin region. It appears that the carbonate concentration in sediments was higher in the temperate-cold than in the temperate-warm phases. In comparison with the ridge of outer arc, the axial region of the inner arc rift is characterized by greater proportion of volcaniclastic materials as well as a higher sedimentation rate and the palynological contents by high percentages of coniferous pollen. These particularity suggest a possible effect of the volcanic activity on the palynological contents in the intra-arc basin since I Ma ago. Thus the axial region of the inner arc has maintained outside of the influence of warm current Kuroshio since 0.46 Ma ago; this is reflected by the very high abundance of Impagidinium patulum to Impagidinium aculeatum.				yzhaowelling@hotmail.com; marie-therese.morzadec@wanadoo.fr						ALI JR, 1992, P OCEAN DRILLING PRO, V125, P547; An Z., 1990, QUATERN INT, V7-8, P91, DOI [10.1016/1040-6182(90)90042-3., DOI 10.1016/1040-6182(90)90042-3]; An ZS, 2000, QUATERNARY SCI REV, V19, P171, DOI 10.1016/S0277-3791(99)00060-8; [Anonymous], NEOGENE QUATERNARY D; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; Ciampo G., 1992, Proceedings of the Ocean Drilling Program Scientific Results, V125, P15, DOI 10.2973/odp.proc.sr.125.141.1992; DALE B, 1996, PALYNOLOGY PRINCIPES, V3; De Vernal A, 1997, GEOBIOS-LYON, V30, P905, DOI 10.1016/S0016-6995(97)80215-X; DEVERNAL A, 1992, NEOGENE QUATERNARY D, P209; Farrell JW, 1989, PALEOCEANOGRAPHY, V4, P447, DOI 10.1029/PA004i004p00447; FENG WK, 1986, MARINE GEOLOGY QUATE, V6, P9; FRYER P, 1992, P OCEAN DRILLING PRO, V125; FRYER P, 1992, P OCEAN DRILLING PRO, V125, P5; Fryer P., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V125; Fujioka K, 1992, P OCEAN DRILLING PRO, V126, P23; HARLAND R, 1983, PALAEONTOLOGY, V26, P321; Heslop D, 2000, EARTH PLANET SC LETT, V184, P125, DOI 10.1016/S0012-821X(00)00324-1; JARVIS J, 1984, INITIAL REPORTS DEEP, V85, P407; 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., 1985, NATURAL SCI B, V25, P21; Matsuoka K., 1992, NEOGENE QUATERNARY D, P33; Matsuoka K., 1987, Bull. 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Palynologists Contribution Series, V17, P169; ZHAO SC, 1994, CANCER GENE THER, V1, P27; ZHAO Y, 1992, ACTA MICROPALAEONTOL, V9, P29; ZHAO Y, 1993, THESIS U RENNES; Zhao Y.Y., 1992, Revue de Micropaleontologie, V35, P77; ZHOU K, 1984, SCI GEOL SINICA, V2, P165; ZONNEVELD K, 1996, LAB PALEOBOTANY PALY, V3	43	4	4	0	0	ASSOC FRANCE ETUD QUATERNAIRE	PARIS	MAISON DE LA GEOLOGIE, 79, RUE CLAUDE BERN, PARIS, F-75005, FRANCE	1142-2904			QUATERNAIRE	Quaternaire	JUN	2009	20	2					195	213						19	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	484NB					2025-03-11	WOS:000269051100006
J	Donders, TH; Weijers, JWH; Munsterman, DK; Hoeve, MLKV; Buckles, LK; Pancost, RD; Schouten, S; Damsté, JSS; Brinkhuis, H				Donders, T. H.; Weijers, J. W. H.; Munsterman, D. K.; Hoeve, M. L. Kloosterboer-van; Buckles, L. K.; Pancost, R. D.; Schouten, S.; Damste, J. S. Sinninghe; Brinkhuis, H.			Strong climate coupling of terrestrial and marine environments in the Miocene of northwest Europe	EARTH AND PLANETARY SCIENCE LETTERS			English	Article						Miocene; land-sea coupling; GDGT lipids; pollen; dinoflagellates; sea level	IONIZATION-MASS-SPECTROMETRY; ATMOSPHERIC CARBON-DIOXIDE; TETRAETHER MEMBRANE-LIPIDS; GLOBAL SEA-LEVEL; MIDDLE MIOCENE; DINOFLAGELLATE CYSTS; RIFT SYSTEM; NW-EUROPE; EVOLUTION; OLIGOCENE	A palynological and organic geochemical record from a shallow marine paleoenvironmental setting in SE Netherlands documents the coupled marine and terrestrial climate evolution from the late Burdigalian (similar to 17 Ma) through the early Zanclean (similar to 4.5 Ma). Proxy climate records show several coeval variations in both relative sea surface (deduced from percent cool dinocysts) and terrestrial (subtropical vs. cool temperate pollen) temperature indices. The terrestrial climatic trend is confirmed by a quantitative reconstruction of annual mean air temperature based on the distribution of fossil branched glycerol dialkyl glycerol tetraethers, showing a cooling from similar to 27 degrees C to similar to 14 degrees C between 17 and 5 Ma punctuated by short-term variations. Decreases in sea surface temperature broadly correlate to inferred third-order sea level variations and correspond to isotope glacial events Mi-3 through Mi-7. An additional strong SST decrease occurs around similar to 8.4 Ma, coincident with a strong reduction and regional disappearance of subtropical pollen types. This cooling phase seems associated with lowered sea levels, but it has not yet been described from the deep sea delta(18)O record. (c) 2009 Elsevier B.V. All rights reserved.	[Donders, T. H.; Munsterman, D. K.] TNO B&O, Geol Survey Netherlands, NL-3508 TA Utrecht, Netherlands; [Donders, T. H.; Hoeve, M. L. Kloosterboer-van; Brinkhuis, H.] Univ Utrecht, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Weijers, J. W. H.; Schouten, S.; Damste, J. S. Sinninghe] NIOZ Royal Netherlands Inst Sea Res, Dept Marine Organ Biogeochem, NL-1790 AB Den Burg, Netherlands; [Buckles, L. K.; Pancost, R. D.] Univ Bristol, Sch Chem, Organ Geochem Unit, Bristol Biogeochem Res Ctr, Bristol BS8 1TS, Avon, England; [Hoeve, M. L. Kloosterboer-van] Goois Lyceum, NL-1401 RT Bussum, Netherlands	Netherlands Organization Applied Science Research; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bristol	Donders, TH (通讯作者)，TNO B&O, Geol Survey Netherlands, POB 80015, NL-3508 TA Utrecht, Netherlands.	timme.donders@tno.nl	Donders, Timme/J-5044-2012; Brinkhuis, Henk/B-4223-2009; Schouten, Stefan/P-4380-2016; Sinninghe Damste, Jaap/F-6128-2011	Brinkhuis, Henk/0000-0003-0253-6610; Pancost, Richard/0000-0003-0298-4026; Donders, Timme/0000-0003-4698-3463; Sinninghe Damste, Jaap/0000-0002-8683-1854	Netherlands Research School of Sedimentary Geology (NSG) [20090202]	Netherlands Research School of Sedimentary Geology (NSG)	The authors thank Natasha Welters (UU) for the palynological sample processing, Hopmans (NIOZ) for the analytical assistance with the HPLC/MS equipment, and Francesca Sangiorgi, Lucas Lourens and Appy Sluijs (LIU) for their helpful comments and discussion. The comments and suggestions from the editor and two anonymous reviewers significantly improved the manuscript. This paper is Netherlands Research School of Sedimentary Geology (NSG) publication no. 20090202.	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Sci. Lett.	MAY 15	2009	281	3-4					215	225		10.1016/j.epsl.2009.02.034	http://dx.doi.org/10.1016/j.epsl.2009.02.034			11	Geochemistry & Geophysics	Science Citation Index Expanded (SCI-EXPANDED)	Geochemistry & Geophysics	456SQ					2025-03-11	WOS:000266869000008
J	Bouimetarhan, I; Marret, F; Dupont, L; Zonneveld, K				Bouimetarhan, Ilham; Marret, Fabienne; Dupont, Lydie; Zonneveld, Karin			Dinoflagellate cyst distribution in marine surface sediments off West Africa (17-6°N) in relation to sea-surface conditions, freshwater input and seasonal coastal upwelling	MARINE MICROPALEONTOLOGY			English	Article						Organic-walled dinoflagellate cysts; West Africa; Marine surface sediments; Sea-surface conditions; Upwelling; River discharge	NORTHWESTERN INDIAN-OCEAN; HYDROGRAPHIC CONDITIONS; ESTUARINE SEDIMENTS; NW AFRICA; VARIABILITY; ATLANTIC; PRESERVATION; IMPACT; RECORD; BAY	An organic-walled dinoflagellate cyst analysis was carried out on 53 surface sediment samples from West Africa (17-6 degrees N) to obtain insight in the relationship between their spatial distribution and hydrological conditions in the upper water column as well as marine productivity in the study area. Multivariate analysis of the dinoflagellate cyst relative abundances and environmental parameters of the water column shows that sea-surface temperature, salinity, marine productivity and bottom water oxygen are the factors that relate significantly to the distribution patterns of individual species in the region. The composition of cyst assemblages and dinoflagellate cyst concentrations allows the identification of four hydrographic regimes; 1) the northern regime between 17 and 14 degrees N characterized by high productivity associated with seasonal coastal upwelling, 2) the southern regime between 12 and 6 degrees N associated with high-nutrient waters influenced by river discharge 3) the intermediate regime between 14 and 12 degrees N influenced mainly by seasonal coastal upwelling additionally associated with fluvial input of terrestrial nutrients and 4) the offshore regime characterized by low chlorophyll-a concentrations in upper waters and high bottom water oxygen concentrations. Our data show that cysts of Polykrikos kofoidii, Selenopemphix quanta, Dubridinium spp., Echinidinium species, cysts of Protoperidinium monospinum and Spiniferites pachydermus are the best proxies to reconstruct the boundary between the NE trade winds and the monsoon winds in the subtropical eastern Atlantic Ocean. The association of Bitectatodinium spongium, Lejeunecysta oliva, Quinquecuspis concreta, Selenopemphix nephroides, Trinovantedinium applanatum can be used to reconstruct past river outflow variations within this region. (C) 2009 Elsevier B.V. All rights reserved.	[Bouimetarhan, Ilham; Zonneveld, Karin] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Marret, Fabienne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Bouimetarhan, Ilham; Dupont, Lydie; Zonneveld, Karin] Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany	University of Bremen; University of Liverpool; University of Bremen	Bouimetarhan, I (通讯作者)，Univ Bremen, Dept Geosci, Klagenfurter Str, D-28359 Bremen, Germany.	bouimetarhan@uni-bremen.de	Bouimetarhan, Ilham/D-2388-2011	Dupont, Lydie/0000-0001-9531-6793; Marret-Davies, Fabienne/0000-0003-4244-0437; Bouimetarhan, Ilham/0000-0003-3369-3811	Deutsche Forschungsgemeinschaft	Deutsche Forschungsgemeinschaft(German Research Foundation (DFG))	The authors thank the captain and crew of R/V Meteor cruise M65-1 for the logistic and technical assistance to recover the investigated sediment samples. The manuscript benefitted from helpful comments by M. Kolling, J. Groenveld and C. Gonzalez. Thanks to Sven Forke for his assistance with palynological processing. This work is funded through the Deutsche Forschungsgemeinschaft as part of the DFG-Research Centre / Excellence cluster MARUM-The Ocean in the Earth System" of the University of Bremen. We express our gratitude to Lucy Edwards and one anonymous reviewer for constructive comments and for detailed reviews of an earlier version of this manuscript.	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Micropaleontol.	MAY	2009	71	3-4					113	130		10.1016/j.marmicro.2009.02.001	http://dx.doi.org/10.1016/j.marmicro.2009.02.001			18	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	452ZD					2025-03-11	WOS:000266578800002
J	Mantle, DJ				Mantle, Daniel Jack			Palynology, sequence stratigraphy, and palaeoenvironments of Middle to Upper Jurassic strata, Bayu-Undan Field, Timor Sea region Part Two	PALAEONTOGRAPHICA ABTEILUNG B-PALAOPHYTOLOGIE			English	Review						Dinoflagellate cysts; acritarchs; systematic palynology; biostratigraphy; palynofacies; sequence stratigraphy; palaeoenvironments; Timor Sea; Elang Formation; Jurassic	DINOFLAGELLATE CYSTS; PALYNOFACIES ANALYSIS; ORGANIC-MATTER; ADJACENT SEAS; BIOSTRATIGRAPHY; SEDIMENTS; NORTH; BASIN; PALYNOSTRATIGRAPHY; STEPHANELYTRON	This second part of a detailed palynological study of 230 core and sidewall core samples from the uppermost Plover, Elang, and lower Frigate formations, Bayu-Undan Field, Timor Sea, concludes the dinoflagellate (Rigaudella to Woodinia), acritarch, and prasinophyte phycomata taxonomy, and examines the biostratigraphy, sequence stratigraphy, and palaeoenvironments from this stratigraphic interval. The palynomorph assemblages, detailed systematically herein, comprise 55 dinoflagellate species and 17 acritarch and prasinophyte phycomata groupings. Of these, the following six dinoflagellate cyst species are newly instituted: Ampulladinium aiax, Batiacasphaera macbethiae, Cauca bayuiana, Ellipsoidictyum fenestellum, Leberidocysta? strigosa, and Yalkalpodinium playfordii. A further species Is not formally named due to a lack of adequately preserved specimens. The palynostratigraphic sequence has previously been assessed as latest Bathonian to early Oxfordian in age, based mainly on correlations with European dinoflagellate assemblages dated by ammonite faunas. Ten subzones (TB1 through 5 and M through 5) are informally proposed, collectively encompassing the Ternia balmei and Voodooia tabulata dinoflagellate cyst Interval Zones. The subzones are defined variously on first and last appearance datums, first and last common occurrences, and species acmes. The acme events are coincident with marine flooding surfaces and enable precise correlation across the Bayu-Undan Field. The Elang Formation - the prime focus of this study - is divided into three third-order sequences, each comprising a lowstand, transgressive, and highstand systems tract. These tracts and their delimiting stratal horizons or flooding surfaces possess distinctive palynomorph or palynodebris assemblages. Qualitative and quantitative variations of these assemblages correlate very closely with gamma-ray log profiles and can consistently be placed within a sequence stratigraphic framework across the Bayu-Undan Field. Palynofacies analyses provide additional means to distinguish among the systems tracts; viz., microphytoplankton diversity increases through transgressive systems tracts to a peak diversity at the maximum flooding surface; atypically brown wood frequencies may also peak at maximum flooding surfaces; and black debris frequencies increase higher in the highstand systems tracts. Palaeoenvironmental interpretations based primarily on palynological assemblages (especially microphytoplankton groupings and palynodebris distribution) enable identification of depositional settings in non-cored intervals. For instance, the occurrences of Ternia balmei, the Meiourogonyaulax group, the Ctenidodinium group, and the Rigaudella group represent an approximate gradation from very nearshore to offshore environments or possibly an increase in salinities from euryhaline to stenohaline conditions.	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J	Nagai, S; Nishitani, G; Takano, Y; Yoshida, M; Takayama, H				Nagai, Satoshi; Nishitani, Goh; Takano, Yoshihito; Yoshida, Makoto; Takayama, Haruyoshi			Encystment and excystment under laboratory conditions of the nontoxic dinoflagellate <i>Alexandrium fraterculus</i> (Dinophyceae) isolated from the Seto Inland Sea, Japan	PHYCOLOGIA			English	Article						Alexandrium fraterculus; Dinoflagellate; Encystment; Excystment; Life history; Planomeiocyte; Planozygote	SP-NOV DINOPHYCEAE; RDNA SEQUENCE DATA; GONYAULAX-TAMARENSIS; GENUS ALEXANDRIUM; SEXUAL REPRODUCTION; COASTAL WATERS; LIFE-HISTORY; NEW-ZEALAND; CYSTS; MORPHOLOGY	The sexuality (i.e. encystment and excystment) of the nontoxic dinoflagellate Alexandrium fraterculus, 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 in 25-60 min after the conjugation started and produced a planozygote with one transverse and two longitudinal flagella, then a cyst was formed. Cysts were round or elliptical. The cyst size was 37.5-50.0 mu m in diameter. The surface of cysts was smooth, and there was no paratabulation. Encystment through sexual reproduction was observed in two of 28 pairs, which included seven self-crossings, by use of seven nonaxenic clonal strains. No planozygote formation or encystment was found in any of the self-crossings, indicating that this species is heterothallic. Successful excystment was observed when the cysts, which had been preserved at 10 degrees C in the dark for 3 mo, were incubated under light conditions at 25 degrees C, thus showing that this species has a similar life cycle as reported in A. tamarensel catenella tamiyavanichii.	[Nagai, Satoshi; Nishitani, Goh] Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; [Takano, Yoshihito] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8528521, Japan; [Yoshida, Makoto] Saga Univ, Ariake Sea Res Project, Saga 8408520, Japan	Japan Fisheries Research & Education Agency (FRA); Nagasaki University; Saga University	Nagai, S (通讯作者)，Natl Res Inst Fisheries & Environm Inland Sea, Maruishi 2-17-5, Hiroshima 7390452, Japan.	snagai@affrc.go.jp	Nagai, Satoshi/HOA-8686-2023	Nagai, Satoshi/0000-0001-7510-0063	Fisheies Research Agency of Japan	Fisheies Research Agency of Japan	We thank Mr N. Hata, Mie Prefecture Fisheries Research Institute, for providing us with natural seawater samples containing Alexandrium fraterculus. Dr T. Kamiyama (National Research Institute of Fisheries and Environment of Inland Sea, Fisheries Research Agency of Japan) and Dr S. Itakura (Fisheries Agency of Japan) are also thanked for their useful suggestions and encouragement during this study. This work was supported in part by a grant from the Fisheies Research Agency of Japan.	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J	Figueroa, RI; Bravo, I; Fraga, S; Garcés, E; Llaveria, G				Figueroa, Rosa Isabel; Bravo, Isabel; Fraga, Santiago; Garces, Esther; Llaveria, Gisela			The Life History and Cell Cycle of <i>Kryptoperidinium foliaceum</i>, A Dinoflagellate with Two Eukaryotic Nuclei	PROTIST			English	Article						Kryptoperidinium foliaceum; binucleate; cell cycle; cysts; dinoflagellate; endosymbiont; life history; sexual reproduction	SP-NOV DINOPHYCEAE; GONYAULAX-TAMARENSIS; TERTIARY ENDOSYMBIOSIS; PERIDINIUM FOLIACEUM; DIATOM ENDOSYMBIONT; SEXUAL REPRODUCTION; EVOLUTION; GERMINATION; KLEPTOPLASTIDY; REPLACEMENT	Kryptoperidinium foliaceum is a binucleate dinoflagellate that contains an endosymbiont nucleus of diatom origin. However, it is unknown whether the binucleate condition is permanent or not and how the diatom nucleus behaves during the life history processes. In this sense, it is also unknown if there is a sexual cycle or a resting stage during the life history of this species, two key aspects necessary to understand the life history strategy of this dinoflagellate. To answer these questions, life history and cell cycle studies were performed with the following results: (i) Kryptoperidinium foliaceum has a sexual cycle and in the dinoflagellate strains studied, the binucleate condition is permanent. Sexuality in the host was confirmed by the presence of fusing gamete pairs and planozygotes in clonal cultures (revealing homothallism), but signs of meiosis in the endosymbiont were not observed. The endosymbiont nucleus likely fuses first, because fusing gamete pairs were found to have two dinoflagellate nuclei but only one endosymbiont nucleus. After complete gamete fusion, the planozygotes had apparently normal endosymbiont and dinoflagellate nuclei. (ii) Asexual division studies using flow cytometry showed that the S phase in the endosymbiont (diatom) nucleus starts 6 - 8h later than in the host nucleus, but there was no evidence of mitosis in the former. (iii) Sexual and asexual cysts were formed in culture. Neither cysts from natural samples nor those formed in culture exhibited a dormancy period before germination. (C) 2009 Elsevier GmbH. All rights reserved.	[Figueroa, Rosa Isabel; Garces, Esther; Llaveria, Gisela] CSIC, Inst Ciencies Mar, CMIMA, Dept Biol Marina & Oceanog, E-08003 Barcelona, Spain; [Bravo, Isabel; Fraga, Santiago] Ctr Oceanog Vigo, Inst Espanol Oceanog, E-36390 Vigo, Spain	Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centro Mediterraneo de Investigaciones Marinas y Ambientales (CMIMA); CSIC - Instituto de Ciencias del Mar (ICM); Spanish Institute of Oceanography	Figueroa, RI (通讯作者)，CSIC, Inst Ciencies Mar, CMIMA, Dept Biol Marina & Oceanog, P Maritim de la Barceloneta 37-49, E-08003 Barcelona, Spain.	figueroa@icm.csic.es	Fraga, Santiago/AAA-3760-2020; Bravo, Isabel/D-3147-2012; Figueroa, Rosa/M-7598-2015; Garces, Esther/C-5701-2011; Fraga, Santiago/C-8641-2012	Figueroa, Rosa/0000-0001-9944-7993; Garces, Esther/0000-0002-2712-501X; Fraga, Santiago/0000-0003-3917-9960; Bravo, Isabel/0000-0003-3764-745X				ANDERSON DM, 1980, J PHYCOL, V16, P166; Anderson DM, 2006, LIMNOL OCEANOGR, V51, P860, DOI 10.4319/lo.2006.51.2.0860; Anderson DM, 1997, LIMNOL OCEANOGR, V42, P1009, DOI 10.4319/lo.1997.42.5_part_2.1009; ANDERSON DM, 1978, J PHYCOL, V14, P224, DOI 10.1111/j.1529-8817.1978.tb02452.x; ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1970, ORIGIN EUKARYOTIC CE; Bell G., 1982, The Masterpiece of Nature: The Evolution and Genetics of Sexuality, DOI 10.4324/9780429322884; BERNSTEIN H, 1983, BIOSCIENCE, V33, P326, DOI 10.2307/1309320; Bhattacharya D, 2007, BIOESSAYS, V29, P1239, DOI 10.1002/bies.20671; Biecheler B., 1952, Bull. 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J	Rochon, A; Lewis, J; Ellegaard, M; Harding, IC				Rochon, Andre; Lewis, Jane; Ellegaard, Marianne; Harding, Ian C.			The <i>Gonyaulax spinifera</i> (Dinophyceae) "complex": Perpetuating the paradox?	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						culture; cyst; cyst-theca relationship; dinoflagellate; excystment; gene expression; Gonyaulax spinifera; motile; Nematosphaeropsis labyrinthus; Spiniferites ramosus	DINOFLAGELLATE CYST ASSEMBLAGES; THECA RELATIONSHIP; LATE QUATERNARY; MORPHOLOGY; SEA; SALINITY; NORTHERN; REGION; NOV	Specimens of dinoflagellate cysts referable to the cyst-species Spiniferites ramosus (Ehrenberg 1838) Mantell 1854 and Nematosphaeropsis labyrinthus (Ostenfeld 1903) Reid 1974 have been produced in the same crossed-strain of Gonyaulax spinifera-type (Claparede and Lachmann 1857) Diesing 1866 motile cells during a routine encystment experiment. Detailed observations were made and are reported on the process of encystment, which follows a similar pattern to that already described for Lingulodinium polyedrum. Both cyst types displayed a wide range of morphological variations with respect to process length and/or trabecular development. The cysts morphology vary between "typical" S. ramosus specimens with well developed trifurcate processes with bifurcated distal ends, to specimens with abnormally developed or incomplete processes, specimens with partially developed trabecular network, to typical N. labyrinthus specimens with a complete network of trabecula joining the distal ends of the processes. The cysts were produced in salinities of 25 and 30 psu at 12 degrees C. Experiments in other salinities (15, 20, 35 and 40 psu) only produced cysts of S. ramosus-type. We suggest that the particular salinity conditions (25 and 30 psu) used in our experience probably triggered the expression of a particular phenotype. (C) 2009 Elsevier B.V. All rights reserved.	[Rochon, Andre; Lewis, Jane; Ellegaard, Marianne] Univ Westminster, Sch Biosci, London W1W 6UW, England; [Harding, Ian C.] Univ Southampton, Sch Ocean & Earth Sci, Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England	University of Westminster; University of Southampton; NERC National Oceanography Centre	Rochon, A (通讯作者)，Univ Quebec, Inst Sci Mer Rimouski ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	andre_rochon@uqar.qc.ca	Harding, Ian/K-3320-2012; Ellegaard, Marianne/H-6748-2014	Harding, Ian/0000-0003-4281-0581; Ellegaard, Marianne/0000-0002-6032-3376	NERC [GR3/10803]	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))	We wish to thank Alex Simpson (Orkney Harbour Authority) for collecting the surface sediment samples. We are grateful to Fabienne Marret for providing the slide from core MD99-2271. This work was funded by NERC Grant No. GR3/10803 awarded to J. Lewis and Ian Harding. The authors wish to thank Cecile Devigne, Karine Lemarchand, Suzanne Roy (ISMER-UQAR), Laurent Londeix (University of Bordeaux 1) and Marc Shulman (University of Toronto) for valuable discussions during the preparation of the manuscript, Dr. Barbara Cressey for help with the SEM and Mr. Barry Marsh for assistance with production of SEM micrographs. We acknowledge two anonymous reviewers for their thorough review, which helped improve the manuscript.	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Palaeobot. Palynology	MAY	2009	155	1-2					52	60		10.1016/j.revpalbo.2008.12.017	http://dx.doi.org/10.1016/j.revpalbo.2008.12.017			9	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	447JH					2025-03-11	WOS:000266186900006
J	McCauley, LAR; Erdner, DL; Nagai, S; Richlen, ML; Anderson, DM				McCauley, Linda A. R.; Erdner, Deana L.; Nagai, Satoshi; Richlen, Mindy L.; Anderson, Donald M.			BIOGEOGRAPHIC ANALYSIS OF THE GLOBALLY DISTRIBUTED HARMFUL ALGAL BLOOM SPECIES <i>ALEXANDRIUM MINUTUM</i> (DINOPHYCEAE) BASED ON rRNA GENE SEQUENCES AND MICROSATELLITE MARKERS	JOURNAL OF PHYCOLOGY			English	Article						A; lusitanicum; A; minutum; biogeography; genotype; harmful algal blooms; LSU rRNA; microsatellites; phylogeny	COASTAL WATERS; TAMARENSE DINOPHYCEAE; DINOFLAGELLATE CYSTS; COMPLEX DINOPHYCEAE; TOXIN PRODUCTION; MUTATION-RATES; NEW-ZEALAND; RED TIDE; PHYLOGENY; DNA	The toxic dinoflagellate Alexandrium minutum Halim is one of three species that comprise the "minutum" species complex. This complex is notable due to its role in the etiology of paralytic shellfish poisoning (PSP). Recent increases in PSP incidence and the geographic expansion of toxin-producing Alexandrium dinoflagellates have prompted the intensive examination of genetic relationships among globally distributed strains to address questions regarding their present distribution and reasons for their apparent increase. The biogeography of A. minutum was studied using large subunit ribosomal DNA gene (LSU rRNA) and internal transcribed spacer (ITS) sequences and genotypic data from 12 microsatellite loci. rRNA gene and ITS sequencing data distinguished between two clades, herein termed the "Global" and the "Pacific"; however, little to no resolution was seen within each clade. Genotypic data from 12 microsatellite loci provided additional information regarding genetic relationships within the Global clade, but it was not possible to amplify DNA from the Pacific clade using these markers. With the exception of isolates from Italy and Spain, strains generally clustered according to origin, revealing geographic structuring within the Global clade. Additionally, no evidence supported the separation of A. lusitanicum and A. minutum as different species. With the use of microsatellites, it is now possible to initiate studies on the origin, history, and genetic heterogeneity of A. minutum that were not previously possible using only rRNA gene sequence data. This study demonstrates the power of combining a marker with intermediate resolution (rRNA sequences) with finer-scale markers (microsatellites) to examine intraspecies variability among globally distributed isolates and represents the first effort to employ this technique in A. minutum.	[McCauley, Linda A. R.; Richlen, Mindy L.; Anderson, Donald M.] Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA; [Nagai, Satoshi] Natl Res Inst Fisheries & Environm Inland Sea, Hiroshima 7390452, Japan; [Erdner, Deana L.] Univ Texas Richardson, Inst Marine Sci, Port Aransas, TX 78373 USA	Woods Hole Oceanographic Institution; Japan Fisheries Research & Education Agency (FRA); University of Texas System; University of Texas Dallas	Anderson, DM (通讯作者)，Woods Hole Oceanog Inst, Woods Hole, MA 02543 USA.	danderson@whoi.edu	Nagai, Satoshi/HOA-8686-2023; Erdner, Deana/C-4981-2008	Nagai, Satoshi/0000-0001-7510-0063; Erdner, Deana/0000-0002-1736-8835	NSF [OCE-0402707, OCE-0430724]; EU-US Scientific Initiative on Harmful Algal Blooms; NSF; NIEHS [1 P50 ES012742]; Division Of Ocean Sciences; Directorate For Geosciences [0911031] Funding Source: National Science Foundation	NSF(National Science Foundation (NSF)); EU-US Scientific Initiative on Harmful Algal Blooms; NSF(National Science Foundation (NSF)); NIEHS(United States Department of Health & Human ServicesNational Institutes of Health (NIH) - USANIH National Institute of Environmental Health Sciences (NIEHS)); Division Of Ocean Sciences; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	This work would not have been possible without the generous contributions of cultures by researchers from many countries. We would also like to acknowledge Judy Kleindinst for her assistance with the figures, Katie Libera for her help with the manuscript, and David Kulis for maintaining all cultures used in this study. Funding was provided by NSF Grant OCE-0402707 through the EU-US Scientific Initiative on Harmful Algal Blooms, and NSF grant OCE-0430724 and NIEHS grant 1 P50 ES012742 through the Centers for Oceans and Human Health program.	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J	Persson, A; Smith, BC				Persson, Agneta; Smith, Barry C.			CONSUMPTION OF <i>SCRIPPSIELLA LACHRYMOSA</i> RESTING CYSTS BY THE EASTERN OYSTER (<i>CRASSOSTREA VIRGINICA</i>)	JOURNAL OF SHELLFISH RESEARCH			English	Article						Scrippsiella lachrymose; Crassostrea virginica; dinoflagellate; cyst; oyster; grazing	CALCAREOUS DINOFLAGELLATE CYSTS; POPULATION-DYNAMICS; MARINE-SEDIMENTS; HARMFUL ALGAE; DINOPHYCEAE; TROCHOIDEA; AUSTRALIA; PASSAGE; EVENTS; GUT	Scrippsiella spp. resting cysts, unlike many other dinoflagellate cysts. Possess an outer layer of calcite beneath which is a thin sporopollenin wall. This feature may affect cyst survival through the digestive tract of benthic organisms, when they consume the cysts. The extent of digestibility is related to the degree to which grazing by benthic organisms could influence a benthic cyst population. To test consumption and digestion of a representative Scrippsiella cyst by one benthic grazer, the eastern oyster (Crassostrea virginica) was fed culture-produced resting cysts or the dinoflagellate Scrippsiella lachrymosa under controlled conditions. Cyst recovery from no-oyster, control containers was 97%; therefore, digestive destruction of cysts could be quantified as the difference between cysts added to experimental containers containing oysters and the number of intact cysts recovered after a period of oyster feeding. In each treatment, 18% of the cysts were destroyed after being ingested at a cell density of 43.4 cysts/mL and 11% were digested at a higher cell density (263,2 cysts/mL). Cysts were observed to become rounded and turn yellow after first losing the outer, calcareous wall as a first step in digestion. In fecal-pellet samples, contents from broken cysts could be found as well as intact cysts and rounded yellow cysts. Viability of ingested cysts was not evaluated, but it seems that Scrippsiella cysts are relatively resistant to digestion by oysters.	[Persson, Agneta; Smith, Barry C.] NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA; [Persson, Agneta] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden	National Oceanic Atmospheric Admin (NOAA) - USA; University of Gothenburg	Smith, BC (通讯作者)，NOAA, Natl Marine Fisheries Serv, NE Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT 06460 USA.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514				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; [Anonymous], 1998, PHYSL ECOLOGY HARMFU; BINDER BJ, 1990, J PHYCOL, V26, P289, DOI 10.1111/j.0022-3646.1990.00289.x; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Dale B., 1983, P69; Dale B., 1979, P443; GALTSTOFF PS, 1964, FISHERY B FISH WILDL, V64; Hégaret H, 2008, MAR ECOL PROG SER, V361, P169, DOI 10.3354/meps07375; Hégaret H, 2007, J SHELLFISH RES, V26, P549, DOI 10.2983/0730-8000(2007)26[549:DFROFS]2.0.CO;2; 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, 2003, MAR ECOL PROG SER, V263, P65, DOI 10.3354/meps263065; LEWIS J, 1991, BOT MAR, V34, P91, DOI 10.1515/botm.1991.34.2.91; 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; Lewis J., 2001, lifehab life histories of microalgal species causing harmful blooms, P49; Montresor M, 2003, J EXP MAR BIOL ECOL, V287, P209, DOI 10.1016/S0022-0981(02)00549-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, 1996, INT REV GES HYDROBIO, V81, P513, DOI 10.1002/iroh.19960810404; Olli K, 2002, J PHYCOL, V38, P145, DOI 10.1046/j.1529-8817.2002.01113.x; Persson A, 2003, HARMFUL ALGAE, V2, P43, DOI 10.1016/S1568-9883(03)00003-9; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; PERSSON A, 2008, MALACOLOGIA IN PRESS, V20; Persson A, 2006, HARMFUL ALGAE, V5, P678, DOI 10.1016/j.hal.2006.02.004; Pringsheim E. 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J	Mantle, DJ				Mantle, Daniel Jack			Palynology, sequence stratigraphy, and palaeoenvironments of Middle to Upper Jurassic strata, Bayu-Undan Field, Timor Sea region Part One	PALAEONTOGRAPHICA ABTEILUNG B-PALAEOPHYTOLOGIE PALAEOBOTANY-PALAEOPHYTOLOGY			English	Review						Spores; pollen grains; dinoflagellate cysts; systematic palynology; Timor Sea; Elang Formation; Jurassic	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; EARLIEST CRETACEOUS STRATA; EROMANGA BASIN; MICROPLANKTON; PALYNOMORPHS; ASSEMBLAGES; QUEENSLAND; AUSTRALIA; DINOCYSTS; BOREHOLE	Detailed palynological analysis of 230 core and sidewall core samples from the uppermost Plover, Elang, and lower Frigate formations, Bayu-Undan Field, Timor Sea, reveals the presence of diverse and moderately well preserved palynomorph assemblages (predominantly dinoflagellate cysts, together with acritarchs, spores, and pollen grains) that facilitate biostratigraphic, sequence stratigraphic, and palaeoenvironmental interpretations. This report comprises two parts: Part One: spore, pollen, and dinoflagellate (Microdinium through Voodooia) taxonomy. Part Two: dinoflagellate (Rigaudella through Woodinia), acritarch, and prasinophyte phycomata taxonomy; biostratigraphy; sequence stratigraphy; and palaeoenvironmental synthesis. The palynomorphs detailed systematically in this first part comprise 96 spore and pollen species and 32 dinoflagellate species. Of these, the following four dinoflagellate cyst species are newly instituted: Broomea fusticula, Meiourogonyaulax baculata, Paragonyaulacysta? feneseptata, and P. helbyi. A further four species are not formally named due to a lack of adequately preserved specimens. One genus, Broomea COOKSON & EISENACK (1958), is formally emended. The palynostratigraphic sequence has previously been assessed as latest Bathonian to early Oxfordian in age, based mainly on correlations with European dinoflagellate assemblages dated by ammonite faunas.	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Micropalaeontology, V4, P440; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]; [No title captured]	372	10	10	0	5	E SCHWEIZERBARTSCHE VERLAGSBUCHHANDLUNG	STUTTGART	NAEGELE U OBERMILLER, SCIENCE PUBLISHERS, JOHANNESSTRASSE 3A, D 70176 STUTTGART, GERMANY	2194-900X	2509-839X		PALAEONTOGR ABT B	Palaeontogr. Abt. B-Palaophytol.	APR	2009	280	1-3					1	U29						115	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	426GR					2025-03-11	WOS:000264696500001
J	Sluijs, A; Brinkhuis, H; Williams, GL; Fensome, RA				Sluijs, Appy; Brinkhuis, Henk; Williams, Graham L.; Fensome, Rob A.			Taxonomic revision of some Cretaceous-Cenozoic spiny organic-walled peridiniacean dinoflagellate cysts	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						organic-walled dinoflagellate cysts; (dinocysts); Spinidinium; Vozzhennikovia; peridiniaceans; taxonomy; Eocene; Southern Ocean	BIOSTRATIGRAPHY	In the marginal marine Eocene sediments recovered on Ocean Drilling Program Leg 189, offshore Tasmania. the dominant peridiniacean dinoflagellate cysts in many samples are spiny forms with generally steno-isodeltaform 2a plates assigned to Spinidinium, Vozzhennikovia and allied genera. Many of the species are endemic Antarctic taxa. Based on new observations we propose taxonomic revisions on the basis of the distribution of the ornamentation and the shape of the second anterior intercalary (2a) plate, as well as the nature of archeopyle formation. which always involves the 2a plate. We regard Magallanesium and Volkheimeridium to be taxonomic junior synonyms of Spinidinium. We erect the genus Moria and the species Moria zachosii, Spinidinium schellenbergii, Vozzhennikovia stickleyae and Vozzhennikovia roehliae. We also propose a new morphological term, "proximosutural". The refinement of these taxonomic concepts and the addition of new taxa will enable spiny peridinaiacean dinocysts to be more effectively used in biostratigraphic and paleoenvironmental interpretations. (C) 2008 Elsevier B.V. All rights reserved.	[Sluijs, Appy; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Williams, Graham L.; Fensome, Rob A.] Geol Survey Canada Atlantic, Bedford Inst Oceanog, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada	Utrecht University; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Bedford Institute of Oceanography	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	A.Sluijs@uu.nl	Brinkhuis, Henk/B-4223-2009; Sluijs, Appy/B-3726-2009	Sluijs, Appy/0000-0003-2382-0215; Brinkhuis, Henk/0000-0003-0253-6610	Utrecht Center of Biogeology; LPP Foundation; Utrecht University; Netherlands Organisation; NWO;  [VENI grant 863.07.001]	Utrecht Center of Biogeology; LPP Foundation; Utrecht University; Netherlands Organisation(Netherlands Organization for Scientific Research (NWO)); NWO(Netherlands Organization for Scientific Research (NWO)); 	This research used samples and/or data provided by the Ocean Drilling Program (ODP). Appy Sluijs thanks the Utrecht Center of Biogeology, the LPP Foundation, Utrecht University and the Netherlands Organisation for Scientific Research (NWO; VENI grant # 863.07.001) for funding. Appy Sluijs and Henk Brinkhuis thank NWO for their continued support of the ODP. We thank Erica Crouch, Geoff Eaton, Raquel Guerstein, Jorg Pross and Graeme Wilson for their discussions and Ian Harding for a constructive review of an earlier version of this paper.	[Anonymous], CONTRIBUTIONS SERIES; [Anonymous], 1980, Special Papers in Palaeontology; [Anonymous], 1978, GEOLOGICAL SCI; [Anonymous], 1885, HG BRONNS KLASSEN OR; AURISANO RW, 1984, J PALEONTOL, V58, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BENSON DG, 1976, TULANE STUD GEOL, V12, P1; BRINKHUIS H, 2003, P OC DRILL PROGR SCI; CHENGLONG S, 1999, TAIWANIA, V44, P155; Cookson I. 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ODP, V189, P1, DOI DOI 10.2973/ODP.PROC.SR.189.111.2004; Stickley CE, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2004PA001022; STOVER LE, 1974, GEOLOGICAL SOC AUSTR, V4, P167; STOVER LE, 1987, CONTRIBUTIONS SERIES, V18; Stover Lewis E., 1994, Bulletin de la Societe Belge de Geologie, V102, P5; Sverdlove M.S., 1974, Geoscience Man, V9, P53; VOZZHENNIKOVA TF, 1967, ISKOPAEMYE PERIDINEI, V347, P121; WARNAAR J, 2006, LAB PALAEOBOTANY PAL, V22; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; WILSON GJ, 1984, NEW ZEAL J BOT, V22, P549, DOI 10.1080/0028825X.1984.10425289; WILSON GJ, 1988, NZ GEOLOGICAL SURVEY, V5796; WILSON GRAEME J., 1967, NZ J BOT, V5, P57; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321	72	27	27	0	6	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0034-6667	1879-0615		REV PALAEOBOT PALYNO	Rev. Palaeobot. Palynology	APR	2009	154	1-4					34	53		10.1016/j.revpalbo.2008.11.006	http://dx.doi.org/10.1016/j.revpalbo.2008.11.006			20	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	435OS					2025-03-11	WOS:000265353800004
J	Matsuoka, K; Kawami, H; Nagai, S; Iwataki, M; Takayama, H				Matsuoka, Kazumi; Kawami, Hisae; Nagai, Satoshi; Iwataki, Mitsunori; Takayama, Haruyoshi			Re-examination of cyst-motile relationships of <i>Polykrikos kofoidii</i> Chatton and <i>Polykrikos schwartzii</i> Butschli (Gymnodiniales, Dinophyceae)	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						dinoflagellate; cyst-motile relationship; Polykrikos kofoidii; Polykrikos schwartzii; phylogenetic analysis	DINOFLAGELLATE RESTING CYSTS; NORTH-SEA BASIN; RECENT SEDIMENTS; HYDROGRAPHIC CONDITIONS; COASTAL WATERS; ASSEMBLAGES; MORPHOLOGY; BAY; PHYLOGENY; BELGIUM	We have re-examined the cyst-motile relationships of two Polykrikos species; P. schwartzii and P. kofoidii (Dinophyceae), based on the literature, incubation experiments, and molecular phylogenetic analysis. The longitudinal furrows on the hypocone of P. kofoidii differentiate it from P. schwartzii. Differences in surface ornamentations on the cysts of P. schwartzii and P. kofoidii were considered as important morphological features to differentiate these two species. Many researchers accepted that the cyst of P. schwartzii was characterized by reticulate ornaments and P kofoidii by separate, rod-like processes. However, encystment/excystment experiments carried out in previous studies clarified that the P. kofoidii cyst has coarse reticulate ornaments, not rod-like processes. Further subsequent observations on these relationships have indicated that rod-like processes develop not on cysts of P kofoidii but on cysts of P. schwartzii. In combination with morphological observations, phylogenetic analyses of the small subunit and large subunit rDNA sequences, directly collected from vegetative cells and living cysts of P. kofoidii and P. schwartzii confirmed these findings on the cyst motile relationships and thus the criteria for the identification of cysts required revision. Furthermore morphologically intermediate forms, which sometimes occur, are identical to the cysts of P. schwartzii based on the molecular data of a single cell PCR technique for living cysts. (C) 2008 Elsevier B.V. All rights reserved.	[Matsuoka, Kazumi; Iwataki, Mitsunori] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8512213, Japan; [Kawami, Hisae] Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan; [Nagai, Satoshi] Fisheries Res Agcy, Natl Res Inst Fisheries & Environm Inland Sea, Harmful Algal Bloom Div, Hiroshima 7390452, Japan	Nagasaki University; Nagasaki University; Japan Fisheries Research & Education Agency (FRA)	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, 1551-7 Taira Machi, Nagasaki 8512213, Japan.	kazu-mtk@nagasaki-u.ac.jp	Nagai, Satoshi/HOA-8686-2023; Iwataki, Mitsunori/H-9640-2019	Iwataki, Mitsunori/0000-0002-5844-2800; Nagai, Satoshi/0000-0001-7510-0063	 [Re: 18340166]		The authors much appreciate Dr. Rex Harland, who gave critical and useful comments for improving the manuscript. This work was partly supported by Grant-in-Aid (Re: 18340166) for Science of Japan Society for the Promotion of Science.	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Palaeobot. Palynology	APR	2009	154	1-4					79	90		10.1016/j.revpalbo.2008.12.013	http://dx.doi.org/10.1016/j.revpalbo.2008.12.013			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	435OS					2025-03-11	WOS:000265353800007
J	Marret, F; Mudie, P; Aksu, A; Hiscott, RN				Marret, Fabienne; Mudie, Peta; Aksu, Ali; Hiscott, Richard N.			A Holocene dinocyst record of a two-step transformation of the Neoeuxinian brackish water lake into the Black Sea	QUATERNARY INTERNATIONAL			English	Article; Proceedings Paper	3rd IGCP 521-INQUA Plenary Meeting	AUG 20-28, 2006	Odessa I I Mechnikov Natl Univ, Odessa, UKRAINE		Odessa I I Mechnikov Natl Univ		MICRORETICULATE DINOFLAGELLATE CYSTS; GYMNODINIUM-CATENATUM; RECENT SEDIMENTS; MARMARA SEA; TOKYO-BAY; ASSEMBLAGES; EUTROPHICATION; DINOPHYCEAE; INDICATORS; RESOLUTION	An exceptionally high-resolution and species-rich dinoflagellate cyst record from core M02-45 collected from the southwestern Black Sea shelf provides strong evidence of a gradual reconnection between the Black (BS) and Mediterranean (MS) seas at the beginning of the Holocene. Two main assemblages, one dominated by brackish species, Spiniferites cruciformis and Pyxidinopsis psilata, and freshwater algae, and a subsequent one, characterised by euryhaline species (Lingulodinium machaerophorum, Brigantedinium spp., Protoperidinium ponticum), document a progressive change in sea-surface conditions from low saline (similar to 7-12 psu) to present-day conditions. A first major pulse of marine waters is recorded at around 8.46 ka BP, with a maximum of L. machaerophorum. The occurrence of this species from the bottom of the core, dated at 9.3 ka BP, supports the hypothesis that water levels were already high on the southwestern shelf by that time. Fully present-day conditions are recorded at around 5.6 ka BP, when brackish species and morphotypes of S. belerius, S. bentorii and L. machaerophorum disappeared. Arrivals of Mediterranean species (Operculodinium centrocarpum and S. mirabilis) are observed simultaneously in the southwest and southeast region of the BS at around 7 ka BP. Despite a different protocol for palynomorph preparation and presentation of data, previous studies from the northern shelf also document the arrival of euryhaline species at 7 ka BP, and marine influence prior to that time. The history of harmful algal blooms (HABs) shows a correlation with warmer mid-Holocene temperatures, followed by a succession of introductions possibly associated with early Greek exploration, then merchant shipping. (c) 2007 Elsevier Ltd and INQUA. All rights reserved.	[Marret, Fabienne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Mudie, Peta] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Aksu, Ali; Hiscott, Richard N.] Mem Univ Newfoundland, Dept Earth Sci, St John, NF A1B 3X5, Canada	University of Liverpool; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Memorial University Newfoundland	Marret, F (通讯作者)，Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk; pmudie@nrcan.gc.ca; aaksu@esd.mun.ca; rickh@esd.mun.ca		Marret-Davies, Fabienne/0000-0003-4244-0437				Aksu AE, 2002, MAR GEOL, V190, P119, DOI 10.1016/S0025-3227(02)00345-6; AKSU AE, 2002, GSA TODAY, V12; Aktan Y., 2005, Harmful Algae News, V28, P6; Amorim A, 2006, AFR J MAR SCI, V28, P193, DOI 10.2989/18142320609504146; Amorim A, 2001, PHYCOLOGIA, V40, P572, DOI 10.2216/i0031-8884-40-6-572.1; [Anonymous], 2006, Advances in Phycological Studies Festschrift in Honour of Prof. Dobrina Temniskova-Topalova; ATANASSOVA ID, 1995, ENVIRON POLLUT, V87, P17, DOI 10.1016/S0269-7491(99)80003-7; Atanassova J, 2005, HOLOCENE, V15, P576, DOI 10.1191/0959683605hl832rp; Atanassova J., 1992, Proceedings of the Institute of Oceanology (Varna), V1, P97; BODEANU N, 1993, DEV MAR BIO, V3, P203; Bolch CJS, 2002, J PLANKTON RES, V24, P565, DOI 10.1093/plankt/24.6.565; Bravo I, 1999, SCI MAR, V63, P45, DOI 10.3989/scimar.1999.63n145; Cordova CE, 2005, HOLOCENE, V15, P263, DOI 10.1191/0959683605hl791rp; 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., 1996, PALYNOLOGY PRINCIPLE, P1249; Daskalov GM, 2002, MAR ECOL PROG SER, V225, P53, DOI 10.3354/meps225053; DILORIO D, 1999, J GEOPHYS RES, V104, P3091; Eker-Develi E, 2003, J MARINE SYST, V39, P203, DOI 10.1016/S0924-7963(03)00031-9; Ellegaard M, 1999, PHYCOLOGIA, V38, P289, DOI 10.2216/i0031-8884-38-4-289.1; Faegri K., 1989, J BIOGEOGR, V4th; Fensome RA., 1993, MICROPALEONTOLOGY, V7; Filipova-Marinova M., 2003, Aspects of Palynology and Palaeoecology, P213; Filipova-Marinova M., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P453, DOI [10.1007/978-1-4020-5302-319, DOI 10.1007/978-1-4020-5302-319, 10.1007/978-1- 4020-5302-3_19, DOI 10.1007/978-1-4020-5302-3_19]; Filipova-Marinova Mariana, 2002, Phytologia Balcanica, V8, P133; Glebov A.Y., 2007, The Black Sea Flood Question: Changes in Coastline, Climate, and Human Settlement, P731; Gömez F, 2004, HYDROBIOLOGIA, V517, P43, DOI 10.1023/B:HYDR.0000027336.05452.07; GRIMM E, 1991, TILIA 2 00 PROGRAM; GRIMM EC, 1987, COMPUT GEOSCI, V13, P13, DOI 10.1016/0098-3004(87)90022-7; Head M.J., 1996, Palynology: Principles and Applications, P1197; Head MJ, 2006, J PALEONTOL, V80, P1, DOI 10.1666/0022-3360(2006)080[0001:TCOTCD]2.0.CO;2; Hiscott RN, 2002, MAR GEOL, V190, P261, DOI 10.1016/S0025-3227(02)00350-X; HISCOTT RN, 2006, INT C SED FUK JAP; HISCOTT RN, QUATERNARY IN PRESS; Hiscott RN., 2007, The Black Sea Flood question: Changes in coastline, climate, and human settlement, P89, DOI DOI 10.1007/978-1-4020-5302-3_5; Hopkins Jennifer A., 2002, Palynology, V26, P167, DOI 10.2113/0260167; Jones G. 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MAR 15	2009	197						72	86		10.1016/j.quaint.2007.01.010	http://dx.doi.org/10.1016/j.quaint.2007.01.010			15	Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Physical Geography; Geology	426FV					2025-03-11	WOS:000264694300009
J	Peña-Manjarrez, JL; Gaxiola-Castro, G; Helenes-Escamilla, J				Pena-Manjarrez, J. L.; Gaxiola-Castro, G.; Helenes-Escamilla, J.			Environmental factors influencing the variability of <i>Lingulodinium polyedrum</i>? and <i>Scrippsiella trochoidea</i> (Dinophyceae) cyst production	CIENCIAS MARINAS			English	Article						Baja California; cysts; dinoflagellates; Lingulodinium; Scrippsiella	WALLED DINOFLAGELLATE CYSTS; BENGUELA UPWELLING SYSTEM; GULF-OF-CALIFORNIA; TODOS-SANTOS BAY; SURFACE SEDIMENTS; BAJA-CALIFORNIA; GONYAULAX-TAMARENSIS; POPULATION-DYNAMICS; MEXICO; TEMPERATURE	This study analyzes the temporal variability of the abundance of Lingulodinium polyedrum and Scrippsiella trochoidea resting cysts in surface sediments, as well as the temporary cysts and vegetative cells of L. polyedrum in the upper water column of Todos Santos Bay (Baja California, Mexico). Samples were collected monthly from January 2002 to June 2005 at four sites. Multidimensional scaling analysis and analysis of similarities revealed that resting cysts are distributed heterogeneously according to the sedimentary environment. Surface water temperature, inorganic dissolved phosphate, and the abundance of temporary cysts were the main factors influencing the abundance of L, polyedrum resting cysts, while the variability of temporary cysts was explained by the abundance of planktonic cells. Scrippsiella trochoidea resting cysts showed no statistical relationship with the environmental factors considered. Local runoff during the rainy season and sewage from the city of Ensenada contribute to the eutrophication of the bay. This is an important factor for future blooms since inorganic dissolved nitrate + nitrite and daylight hours during the spring-summer season are not limiting factors for dinoflagellate growth. After the dinoflagellate blooms, there was massive cyst production of both species, and the new cysts settled oil the surface sediments. Surface water temperatures between 17 degrees C and 22.5 degrees C during spring-summer appear to trigger excystment in these species.	[Pena-Manjarrez, J. L.] Ctr Estudios Tecnol Mar Ensenada, Direcc Gen Educ Ciencia & Tecnol Mar, Ensenada, Baja California, Mexico; [Pena-Manjarrez, J. L.; Gaxiola-Castro, G.] CICESE, Dept Oceanog Biol, Div Oceanol, Ensenada, Baja California, Mexico; [Helenes-Escamilla, J.] CICESE, Dept Geol, Div Ciencias Tierra, Ensenada, Baja California, Mexico	CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada; CICESE - Centro de Investigacion Cientifica y de Educacion Superior de Ensenada	Peña-Manjarrez, JL (通讯作者)，Ctr Estudios Tecnol Mar Ensenada, Direcc Gen Educ Ciencia & Tecnol Mar, Km 6-5 Carretera Ensenada Tijuana, Ensenada, Baja California, Mexico.	jopema@cicese.mx	Helenes, Javier/J-5033-2016	Helenes, Javier/0000-0002-0135-1879	Coordinacion Sectorial de Desarrollo Acadomico; SEMARNAT; CONACYT	Coordinacion Sectorial de Desarrollo Acadomico; SEMARNAT; CONACYT(Consejo Nacional de Ciencia y Tecnologia (CONACyT))	We gratefully acknowledge financial support from the Coordinacion Sectorial de Desarrollo Acadomico (COSDAQ and the Direccion General de Educacion en Ciencia y Tecnologia del Mar (DGECyTM) through project 910.06-P. Field and laboratory work was partially funded by SEMARNAT through project 2004-COI-62. The first author acknowledges receipt of a scholarship from CONACYT and SEMARNAT. We thank P Chagoya-Loli, L Lafarga-Cosio and M Ortega (CETMAR, Ensenada), V Acosta-Chamorro (SEMAR), and Z Mij angos-Alqui sires (DGECyTM) for their help in the field and laboratory work. We also thank two anonymous reviewers and H Maske for their comments and recommendations to the final version of this work, as well as JM Dominguez and F Ponce for the figures.	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Mar.	MAR	2009	35	1					1	14						14	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	438XI					2025-03-11	WOS:000265589100001
J	Scafati, L; Melendi, DL; Volkheimer, W				Scafati, L.; Melendi, D. L.; Volkheimer, W.			A Danian subtropical lacustrine palynobiota from South America (Bororo Formation, San Jorge Basin, Patagonia - Argentina)	GEOLOGICA ACTA			English	Article						Paleogene; Patagonia; Palynology; Aquatic palynomorphs; Paleoenvironment	TIERRA-DEL-FUEGO; TERTIARY SEDIMENTS; POLLEN GRAINS; NETHERLANDS; SPORES; ZYGNEMATACEAE; PALEOECOLOGY; BOTRYOCOCCUS; PALYNOLOGY; ALGAE	New results on a lacustrine Danian palynological association in extra-andean northern Patagonia (lower member of the Cerro Bororo Formation, San Jorge Basin, Chubut province, Argentina) are presented. This is a contribution to the largely unexplored field of Paleogene freshwater environments. The palynobiota includes representatives of the kingdoms Protoctista and Plantae. Twelve of the aquatic species are Protoctista. From the nine Chlorophyta form-species, four correspond to Botryococcaceae, one to Coelastraceae and four to Zygnemataceae (Gelasinicysta, Schizosporis, Ovoidites, and Pseudoschizaea). The remaining forms are dinoflagellate cysts (Peridinium and dinocyst indet.) and prasinophyceans (Leiosphaeridia). Plants are represented by spores and pollen of Bryophytes (Sphagnaceae and Ricciaceae), Pteridophytes (Salviniaceae), and Angiosperms (Arecaceae, Araceae and Sparganiaceae/Typhaceae, the latter representing macrophytes living in or near the swampy areas). Other palynomorph groups closely related with biotopes of permanent moisture are dominated by spores of the families Selaginellaceae, Lycopodiaceae, Cyatheaceae, Schizaeaceae, Polypodiaceae and Psilotaceae. The palynological assemblage reflects a freshwater lacustrine environment that developed in a marine coastal zone nearby brackish coastal swamps. Based on the composition of the palynoflora including palm pollen and other thermophilous taxa, humid, warm climatic conditions are inferred for the area of deposition.	[Scafati, L.; Melendi, D. L.] Museo Argentino Ciencias Nat B Rivadavis CONICET, Div Paleobot, Buenos Aires, DF, Argentina; [Volkheimer, W.] IANIGLA CCT Mendoza CONICET, Unid Paleopalinol, RA-5500 Mendoza, 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 Nacional Cuyo Mendoza	Scafati, L (通讯作者)，Museo Argentino Ciencias Nat B Rivadavis CONICET, Div Paleobot, A Gallardo 470,C1405DJR, Buenos Aires, DF, Argentina.	lscafati@macn.gov.ar; volkheim@lab.cricyt.edu.ar			CONICET [5222]	CONICET(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET))	We wish to acknowledge CONICET for economic support ( PIP 5222). IANIGLA/CRICYT-Mendoza and the Museo Argentino de Ciencias Naturales "B. Rivadavia" (MACNINICN), Buenos Aires provided laboratory and SEM facilities. We thank Helga Smekal (Asociacion Paleontologica Bariloche) for helping during fieldwork, and Dr. Vivi Vajda and Lic. Paula Narvez is acknowledged for the very helpful corrections of the manuscript.	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Acta	MAR-JUN	2009	7	1-2					35	61		10.1344/105.000000270	http://dx.doi.org/10.1344/105.000000270			27	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	415AI					2025-03-11	WOS:000263906300003
J	Tripathi, SKM; Kumar, M; Srivastava, D				Tripathi, S. K. M.; Kumar, M.; Srivastava, D.			Palynology of Lower Palaeogene (Thanetian-Ypresian) coastal deposits from the Barmer Basin (Akli Formation, Western Rajasthan, India): Palaeoenvironmental and palaeoclimatic implications	GEOLOGICA ACTA			English	Article						Mangrove pollen; Nypa; Thanetian-Ypresian; India	SEDIMENTARY ORGANIC-MATTER; ENVIRONMENTS; TASMANIA	The 32-m thick sedimentary succession of the Paleocene-Eocene Akli Formation (Barmer basin, Rajasthan, India), which is exposed in an open-cast lignite mine, interbed several lignite seams that alternate with fossiliferous carbonaceous clays, green clays and widespread siderite bands and chert nodules. The palynofloral assemblages consist of spore, pollen and marine dinoflagellate cysts that indicate a Thanetian to Ypresian age. The assemblage is dominated by angiospermic pollen and specimens showing affinity with the mangrove Palm Nypa are also very abundant. The Nypa-like pollen specimens exhibit a wide range of morphological variation, some of the recorded morphotypes being restricted to this Indian basin. Preponderance of these pollen taxa indicates that the sediments were deposited in a coastal swamp surrounded by thick, Nypa-dominated mangrove vegetation. The dispersed organic matter separated from macerated residues indicates the dominance of anoxic conditions throughout the succession, although a gradual transition to oxic conditions is recorded in the upper part.	[Tripathi, S. K. M.; Kumar, M.; Srivastava, D.] Birbal Sahni Inst Paleobot, Lucknow 226007, Uttar Pradesh, India	Department of Science & Technology (India); Birbal Sahni Institute of Palaeobotany (BSIP)	Tripathi, SKM (通讯作者)，Birbal Sahni Inst Paleobot, 53 Univ Rd, Lucknow 226007, Uttar Pradesh, India.	skmtripathi@yahoo.com; madhavbsip@yahoo.com; divya_t20@yahoo.co.in						Ambwani AK., 1996, PALEOBOTANIST, V43, P139; Batten D.J., 1996, Palynology: Principles and Applications, P1065; Bombardiere L, 1998, SEDIMENTOLOGY, V45, P771, DOI 10.1046/j.1365-3091.1998.00177.x; BOSE MN, 1952, J SCI IND RES B PH S, V11, P85; Chaloner W.G., 1968, EVOLUTION ENV, P125; DEMAISON GJ, 1980, AAPG BULL, V64, P1179; FREDERIKSEN NO, 1985, AM ASS STRATIGRAPHIC, V15, P1; Frederiksen Norman O., 1994, Palynology, V18, P91; Habib D., 1994, PALYNOLOGY SEDIMENTA, P311, DOI DOI 10.1017/CBO9780511524875; JAIN K P, 1973, Geophytology, V3, P150; Kar, 1996, PALEOBOTANIST, V45, P71; Kar R. K., 2001, Palaeontographica Abteilung B Palaeophytologie, V256, P123; KAR R K, 1986, Pollen et Spores, V28, P177; Kar R.K., 1995, PALEOBOTANIST, V42, P380; KAR RK, 1978, PALAEOBOTANIST, V34; Kar RK., 1992, PALAEOBOTANIST, V40, P336; KAR RK, 1985, PALAEOBOTANIST, V34; LUKOSE NG, 1974, PALEOBOTANIST, V21, P285; Mandal J., 1986, PALEOBOTANIST, V35, P196; Masran Th.C., 1981, ORGANIC MATURATION F, P145; Morley R. J., 2000, ORIGIN EVOLUTION TRO; Muller J., 1979, P 4 INT PALYNOLOGICA, V1, P568; Muller J., 1964, Ancient Pacific Floras, P33; MULLER JAN, 1968, MICROPALEONTOLOGY [NY], V14, P1, DOI 10.2307/1484763; Naskar P., 1978, PALEOBOTANIST, V25, P314; PARRISH JT, 1982, PALAEOGEOGR PALAEOCL, V40, P67, DOI 10.1016/0031-0182(82)90085-2; Pittet B, 1997, SEDIMENTOLOGY, V44, P915, DOI 10.1046/j.1365-3091.1997.d01-58.x; Pole MS, 1998, AUST J EARTH SCI, V45, P979, DOI 10.1080/08120099808728452; Pole MS, 1996, REV PALAEOBOT PALYNO, V92, P55, DOI 10.1016/0034-6667(95)00099-2; RAO A. R., 1952, PROC NATL INST SCI INDIA, V18, P595; RAO AR, 1950, P NATL I SCI, V18, P595; Roy AB., 2002, Geology of Rajasthan (Northwest India) precambrian to recent; Sah SCD., 1974, PALAEOBOTANIST, V21, P163; Sahni A., 2004, Second Association of Petroleum Geologists Conference and Exhibition, Madhya Pradesh, V2426, P1; Saxena R.K., 1981, PALEOBOTANIST, V27, P300; Saxena R. K., 1980, PALEOBOTANIST, V26, P279; SAXENA RK, 1988, P S PAL IND LIM SUBD, P68; Scafati L, 2009, GEOL ACTA, V7, P35, DOI 10.1344/105.000000270; SINGH A, 1991, REV PALAEOBOT PALYNO, V67, P205, DOI 10.1016/0034-6667(91)90043-3; Singh R.Y., 1988, PALAEOCENE INDIA, P51; Singh RY., 1977, Palaeobot, V23, P189; Sinha-Roy S, 1998, Geology of Rajasthan; SISODIA M.S., 2000, NAFTA, V51, P309; Tripathi S., 1995, PALAEOBOTANIST, V43, P45; Tripathi S., 1993, J PALAEOSCI, V42, P61; Tripathi S K M, 1984, SPECIAL PUBLICATION, P316; Tripathi SKM., 1997, PALAEOBOTANIST, V46, P168; Tripathi SKM., 2003, PALEOBOTANIST, V52, P87; Venkatachal B.S., 1986, PALEOBOTANIST, V42, P106; VENKATACHALA B.S., 1968, Palaeobotanist, V17, P157, DOI DOI 10.54991/JOP.1968.792	50	48	53	0	7	UNIV BARCELONA	BARCELONA	INST CIENCIES TERRA JAUME ALMERA-CSIC, LLUIS SOLE I SABARIS S-N, BARCELONA, E-08028, SPAIN	1695-6133	1696-5728		GEOL ACTA	Geol. Acta	MAR-JUN	2009	7	1-2					147	160		10.1344/105.000000275	http://dx.doi.org/10.1344/105.000000275			14	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	415AI					2025-03-11	WOS:000263906300009
J	Fensome, RA; Williams, GL; MacRae, RA				Fensome, Robert A.; Williams, Graham L.; MacRae, R. Andrew			LATE CRETACEOUS AND CENOZOIC FOSSIL DINOFLAGELLATES AND OTHER PALYNOMORPHS FROM THE SCOTIAN MARGIN, OFFSHORE EASTERN CANADA	JOURNAL OF SYSTEMATIC PALAEONTOLOGY			English	Review						dinoflagellate cysts; Scotian Margin; dinocysts; spores; pollen; taxonomy; biostratigraphy	CYST; PALYNOLOGY; MIOCENE; BIOSTRATIGRAPHY; STRATIGRAPHY; ASSEMBLAGES; TAXONOMY; PLIOCENE; GENERA; EMEND	Palynomorphs, especially dinoflagellate cysts (dinocysts), have been at the forefront of research carried out on Mesozoic-Cenozoic sediments on the Scotian Margin over the last 30-40 years: this research has been driven by the need to develop a stratigraphical framework to better understand the region's petroleum systems. To support the compilation of a detailed event stratigraphical scheme for the Late Cretaceous to Cenozoic of the margin, emphasising dinocysts but with information from other fossil groups and non-biostratigraphical data, there is a need to formalise the dinocyst taxonomy. In this paper, we fulfill this need by illustrating and, where appropriate, describing and discussing taxa used in our event biostratigraphical scheme. The following taxa (dinocysts except where indicated) are new: Areoligera, circumsenonensis, Axiodinium, Axiodinium prearticulatum, Cordosphaeridium delimurum, Glaphyracysto extensa, Hafniasphaera delicata, Impletosphaeridium capitatum, Mendicodinium robustum (validation of previously proposed name), Minisphaeridium, Oligokolpoma, Oligokolpoma tubulus, Palaeocystodinium obesum, Palaeocystodinium teespinosum, Palaeohystrichophora palaeoinfusa, Pentadinium sabulum, Pervosphaeridium granaciculare, Talladinium, Wetzeliella caviarticulata and Cingutriletes tyriskos (a trilete spore). The following are newly proposed combinations (with a former name in parentheses): Cerebrocysta waipawaensis (Pyxidinopsis waipawaensis), Cerodinium glabrum (Cerodinium speciosum subsp. globrum), Dinopterygium alatum (Xiphophoridium alatum), Kleithriasphaeridium cooksonioe (Florentinia cooksoniae), Kleithriasphaeridium perforatum (Florentinia perforata), Minisphaeridium latirictum (Hystrichosphaeridium latirictum), Nyktericysta tripenta (Balmula tripenta), Pentadinium granulatum (Pentodinium loticinctum subsp. granulatum) Talladinium? clathratum (Charlesdowniea clathrata) and Talladinium wulagenense (Chorlesdowniea wulagenensis). Emendations of the following taxa are proposed: Apectodinium, Dinopterygium, Distatodinium, Glaphyrocysta, Hafniasphaera, Isabelidinium, Kleithriasphaeridium, Manumiella, Nyktericysta, Palaeocystodinium, Rhombodinium, Wetzeliella and Wetzeliella articulata. Material from the Kiowa Formation of Kansas supports our concept of Dinopterygium. We review several morphological terms already in the literature and introduce the following new ones: mesotabular, obtabular, contabular, penicontabular, epeliform, equi-epeliform and lati-epeliform.	[Fensome, Robert A.; Williams, Graham L.] Nat Resources Canada, Geol Survey Canada Atlantic, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [MacRae, R. Andrew] St Marys Univ, Halifax, NS B3H 3C3, Canada	Bedford Institute of Oceanography; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Saint Marys University - Canada	Fensome, RA (通讯作者)，Nat Resources Canada, Geol Survey Canada Atlantic, Bedford Inst Oceanog, POB 1006, Dartmouth, NS B2Y 4A2, Canada.	rfensome@nrcan.gc.ca						Alberti G., 1959, Mitteilungen aus dem Geologischen Staatsinstitut in Hamburg, V28, P93; Alberti G., 1961, Palaeontographica, V116, P1; Anderson RY., 1960, STATE BUREAU MINES M, V6, P1; [Anonymous], PALAEONTOLOGY; [Anonymous], PALAEONTOGRAPHICA A; [Anonymous], NOVA HEDWIGIA; [Anonymous], 1963, ATLAS MITTEL JUNGTER; [Anonymous], 1970, U KANSAS PALEONTOLOG; [Anonymous], 1979, 4 INT PAL C LUCKN 19; [Anonymous], PALAEOBOTANIST; [Anonymous], 1985, SPOROPOLLENIN DINOFL; Ashraf A.R., 1979, Palaeontographica Abteilung B Palaeophytologie, V169, P122; BACKHOUSE J, 1988, GEOLOGICAL SURVEY W, P135; BALTES N, 1969, 1 INT C PLANKT MICR, V1, P26; BARSS MS, 1979, GEOLOGICAL SURVEY CA, V78; BELOW R, 1982, Palaeontographica Abteilung B Palaeophytologie, V182, P1; BELOW R, 1981, Palaeontographica Abteilung B Palaeophytologie, V176, P1; BELOW R, 1987, Palaeontographica Abteilung B Palaeophytologie, V205, P1; BENEDEK P N, 1981, Palaeontographica Abteilung B Palaeophytologie, V180, P39; BENEDEK P.N., 1972, PALAEONTOGRAPHICA B, V137, P1; BENEDEK PN, 1982, ABHANDLUNGEN, V162, P265; Benson D.G. 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Syst. Palaeontol.	MAR	2009	7	1					1	79		10.1017/S1477201908002538	http://dx.doi.org/10.1017/S1477201908002538			79	Evolutionary Biology; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Evolutionary Biology; Paleontology	418IW					2025-03-11	WOS:000264142900001
J	Boucsein, B; Stein, R				Boucsein, Bettina; Stein, Ruediger			Black shale formation in the late Paleocene/early Eocene Arctic Ocean and paleoenvironmental conditions: New results from a detailed organic petrological study	MARINE AND PETROLEUM GEOLOGY			English	Article						Arctic Ocean; Lomonosov Ridge; Organic carbon; Maceral analysis; Paleogene; Paleoenvironmental reconstruction	CONTINENTAL-MARGIN; CARBON-SOURCE; SOURCE-ROCK; SEDIMENTS; SEA; MATTER; LAPTEV; INDICATORS; ATLANTIC; BEAUFORT	The study of particulate organic matter (OM) in Arctic Ocean sediments from the late Cretaceous to the Eocene (IODP Expedition 302) has revealed detailed information about the aquatic/marine OM fluxes, biological sources, preservation and export of terrestrial material. Here, we present detailed data from maceral analysis, vitrinite reflectance measurements and organic geochemistry. During the Campanian/Paleocene, fluxes of land-derived OM are indicated by reworked and oxidized macerals (vitrinite, inertinite) and terrigenous liptinite (cutinite, sporinite). In the early Eocene, drastic environmental changes are indicated by peaks in aquatic OM (up to 40-45%, lamalginite, telalginite, liptodetrinite, dinoflagellate cysts) and amorphous OM (up to 50% bituminite). These events of increased aquatic OM flux, similar to conditions favoring black shale deposition, correlate with the global delta C-13 events 'Paleocene/Eocene Thermal Maximum' (PETM) and 'Elmo event'. Freshwater discharge and proximity of the source area are documented by freshwater algae material (Pediastrum, Botryococcus) and immature land-plant material (corphuminite, textinite). We consider that erosion of coal-bearing sediments during transgression time lead to humic acids release as a source for bituminite deposited in the early Eocene black shales. (c) 2008 Elsevier Ltd. All rights reserved.	[Boucsein, Bettina] Alfred Wegener Inst Polar & Marine Res, Res Unit Potsdam, D-14473 Potsdam, Germany; [Stein, Ruediger] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research	Boucsein, B (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Res Unit Potsdam, Telegrafenberg A43, D-14473 Potsdam, Germany.	bettina.boucsein@awi.de		Stein, Ruediger/0000-0002-4453-9564	German Research Foundation (DFG) [BO 2911/1-1-2]	German Research Foundation (DFG)(German Research Foundation (DFG))	This research used samples and data provided by the Integrated Ocean Drilling Program (IODP) and was funded by the German Research Foundation (DFG) (Grant BO 2911/1-1-2). Tom Wagner and one anonymous reviewer are gratefully acknowledged for their comments on an earlier draft of the manuscript. We thank Ralf Littke for numerous and helpful discussion of the petrographical data and Bernard Coakley for checking the English. I would also like to thank Henriette Kampe and Gerhard Berger for technical assistance. All data are available in doi:10.1594/PANGAEA.690523.	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J	Masure, E; Vrielynck, B				Masure, E.; Vrielynck, B.			Late Albian dinoflagellate cyst paleobiogeography as indicator of asymmetric sea surface temperature gradient on both hemispheres with southern high latitudes warmer than northern ones	MARINE MICROPALEONTOLOGY			English	Article						Late Albian; dinoflagellate cysts; northern hemisphere; southern hemisphere; thermal gradient; climate	CALCAREOUS NANNOFOSSIL BIOGEOGRAPHY; DRILLING PROJECT LEG-79; CRETACEOUS CLIMATE; ADJACENT SEAS; BRITISH-ISLES; OCEAN; SEDIMENTS; ATLANTIC; RECORD; PRESERVATION	Late Albian temperature sensitive dinoflagellate cysts are characterized in order to better understand mid-Cretaceous sea surface temperature gradients. Distribution maps of thirty-seven species recovered from one hundred fifty outcrops and deep sea drilling holes (ODP, DSDP) Sites located from low and high paleolatitudes over the two hemispheres (75 degrees N-70 degrees S) are encountered. Fifty years of published data available in eighty-seven articles have been considered and synthesized using a database coupled with a Geographical Information System (GIS). The continuous and disjoint biogeographic patterns of dinocyst species along latitudes define seven climatic belts, four in the northern hemisphere (high, mid-high, mid-low, low latitude belts) and three in the southern hemisphere (low, mid-low, mid-high latitude belts). Dinocysts restricted along latitudes are temperature sensitive species. Limit ranges of temperature sensitive dinocysts of mid-low and mid-high latitude belts reveal mixing belts, located at 40-45 degrees N and 50 degrees-70 degrees S. They represent major palaeofrontal systems as paleosubtropical fronts with strongly mixed water column. The northern frontal system (40-45 degrees N) was located as in the modem ocean. The large southern frontal system (50 degrees S-70 degrees S) was 10 degrees-20 degrees poleward to Antarctica. Semi-quantitative temperature range limits for mid-Cretaceous dinoflagellates and SST gradients in the two hemispheres are suggested by setting dinocyst climatic belts against estimated delta(18)O temperature curve from fish teeth. A paleoecological classification is suggested. Latitudinal distribution of extant temperature sensitive dinoflagellate cysts follows the asymmetric modern temperature gradient. Asymmetric latitudinal ranges of Late Albian dinocyst species of mid-low latitude belts restricted between 45 degrees N and 70 degrees S demonstrate asymmetric temperature gradients with southern high latitudes being warmer than northern high latitudes. (C) 2008 Elsevier B.V. All rights reserved.	[Masure, E.] Univ Paris 06, CNRS, UMR 5143, F-75005 Paris, France; [Vrielynck, B.] Univ Paris 06, CNRS, UMR 7072, F-75005 Paris, France	Centre National de la Recherche Scientifique (CNRS); Sorbonne Universite; Sorbonne Universite; Centre National de la Recherche Scientifique (CNRS)	Masure, E (通讯作者)，Univ Paris 06, CNRS, UMR 5143, Case 104,4 Pl Jussieu, F-75005 Paris, France.	edwige.masure@upmc.fr; bruno.vrielynck@upmc.fr			CEPGE (Centre Parisien en Geologie); UMR-CNRS 5143 "Paleobiodiversite et Paleoenvironnements"	CEPGE (Centre Parisien en Geologie); UMR-CNRS 5143 "Paleobiodiversite et Paleoenvironnements"	This work was carried out with support from CEPGE (Centre Parisien en Geologie) and the UMR-CNRS 5143 "Paleobiodiversite et Paleoenvironnements".	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J	Anthonissen, ED				Anthonissen, Erik D.			A new Pliocene biostratigraphy for the northeastern North Atlantic	NEWSLETTERS ON STRATIGRAPHY			English	Review						North Sea; Norwegian Sea; Foraminifera; dinoflagellate cysts; Pliocene; calibrations	NORWEGIAN CONTINENTAL-SHELF; DINOFLAGELLATE CYSTS; FORAMINIFERAL BIOSTRATIGRAPHY; UTSIRA FORMATION; ROCKALL PLATEAU; VIKING GRABEN; UPPER MIOCENE; MID-PLIOCENE; SEA; STRATIGRAPHY	This study has aimed to integrate and improve upon the existing marine biostratigraphic schemes pertaining to the Lower to mid-Pliocene (ca. 5.3-2.4 Ma) in the northeastern North Atlantic ('Nordic Atlantic') region. This has been achieved through: the updating of age calibrations for key microfossil bioevents, identification of new events, and integration of new biostratigraphic data from a foraminiferal analysis of cored wells and outcrops in the North Sea region. At these high latitudes, where standard zonal markers are often absent, integration of microfossil groups significantly improves temporal resolution. A new multi-group microfossil zonation is presented comprising 7 Nordic Pliocene (NP) Zones. Zonal duration ranges from 300,000 to 600,000 years. A total of 51 bioevents (28 foraminifers and bolboforms; 17 dinoflagellate cysts and acritarchs; 6 marine diatoms) facilitates zonal identification throughout the Nordic Atlantic region. Via correlations to the bio-magnetostratigraphy and oxygen isotope records of Ocean Drilling Program and Deep Sea Drilling Project Sites, the ages of shallower North Sea deposits have been better constrained. The Early to Mid-Pliocene is biostratigraphically characteristic in being the last time a significant influx of a temperate to subtropical planktonic foraminiferal fauna and dinoflagellate flora was present at such high latitudes in the Nordic and North Seas.	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J	Candel, MS; Borromei, AM; Martínez, MA; Gordillo, S; Quattrocchio, M; Rabassa, J				Soledad Candel, Maria; Maria Borromei, Ana; Martinez, Marcelo A.; Gordillo, Sandra; Quattrocchio, Mirta; Rabassa, Jorge			Middle-Late Holocene palynology and marine mollusks from Archipielago Cormoranes area, Beagle Channel, southern Tierra del Fuego, Argentina	PALAEOGEOGRAPHY PALAEOCLIMATOLOGY PALAEOECOLOGY			English	Article						Palynology; Marine mollusks; Paleoenvironment; Holocene transgression; Beagle Channel	DINOFLAGELLATE CYST ASSEMBLAGES; LATE QUATERNARY; HYDROGRAPHIC CONDITIONS; SURFACE SEDIMENTS; MAGELLAN; CLIMATE; INDICATORS; AMERICA; OCEAN; COAST	The palynology and marine mollusks of a marine sequence from Rio Ovando (54 degrees 51' S, 68 degrees 35' W), Archipielago Cormoranes, Beagle Channel, has been studied in order to reconstruct paleoenvironmental conditions during the Middle-Late Holocene. The dinoflagellate cyst assemblages from Rio Ovando sequence reflect fjord (estuarine) environments close to terrestrial ice field, affected by glacier meltwater discharge, and characterized by short-term oscillations of sea-surface water parameters. The base of the section, which is dated at about ca. 4160 C-14 yr B.P. (4736 cal yr B.P.) (Palynological Subzone RO-2c), is characterized by a high species diversity of dinocyst and mollusks, and it is immediately followed by an interval (Palynological Subzone RO-2b) characterized by the presence of the Echinidinium-Islandinium complex and the monospecific Mytilus mollusk assemblage. This subzone registers an inverse correlation between Nothofagus dombeyi type and Echinidinium-Islandinium complex concentration values during ca. 4160 C-14 yr B.P. (4736 cal yr B.P.)-4064 C-14 yr B.P. (4540 cal yr B.P.), suggesting a variable climatic condition, probably related to Neoglacial episodes occurred in the southern Patagonia Andes during this interval. The pollen assemblages permit direct correlations with the onshore palynostratigraphy from southern of Tierra del Fuego. The high percentages of Nothofagus dombeyi type recorded throughout most of the profile strongly suggest the presence of a closed forest, confirming the existence of a variable, cool and wet climate for the Archipielago Cormoranes area during the Middle-Late Holocene. (C) 2008 Elsevier B.V. All rights reserved.	[Soledad Candel, Maria; Maria Borromei, Ana; Martinez, Marcelo A.; Quattrocchio, Mirta] Univ Nacl Sur, CONICET, Dept Geol, INGEOSUR, RA-8000 Bahia Blanca, Buenos Aires, Argentina; [Gordillo, Sandra] Univ Nacl Cordoba, CONICET, CIPAL, RA-5000 Cordoba, Argentina; [Rabassa, Jorge] Consejo Nacl Invest Cient & Tecn, CADIC, Lab Geol Cuaternario, Ushuaia, Tierra Fuego, Argentina	Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE); National University of Cordoba; Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET); Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)	Candel, MS (通讯作者)，Univ Nacl Sur, CONICET, Dept Geol, INGEOSUR, San Juan 670,B8000ICN, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	scandel@uns.edu.ar; borromei@criba.edu.ar; martinez@criba.edu.ar; sgordillo@efn.uncor.edu; mquattro@criba.edu.ar; jrabassa@cadic.gov.ar		Martinez, Marcelo/0000-0003-0538-4739; Gordillo, Sandra/0000-0002-3937-4865	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas) [PIP 02787/02]; Agencia Nacional para la Promocion de la Ciencia y Tecnologia (PICT-Redes) [2002-00067]	CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Agencia Nacional para la Promocion de la Ciencia y Tecnologia (PICT-Redes)(ANPCyT)	The first author M.S. Candel thanks Dr. Anne de Vernal and Dr. Taoufik Radi from the Centre de recherche en geochimie et geodynamique (GEOTOP-UQAM, Universite du Quebec Montreal) for their help in the systematic identifications of dinoflagellate cyst of Tierra del Fuego. We are also grateful to Dr. Andrea Coronato (CADIC, Centro Austral de Investigaciones Cientificas, Ushuaia, Tierra del Fuego) for field assistance and contributing resources in the field work. This study was supported by CONICET (Consejo Nacional de Investigaciones Cientificas y Tecnologicas; PIP 02787/02) and the Agencia Nacional para la Promocion de la Ciencia y Tecnologia (PICT-Redes 2002-00067), both being Argentine federal government institutions. The study on mollusks is part of a broader project focused on the Quaternary molluscan faunas from southern South America, between CADIC (Laboratorio de Geologia del Cuaternario) and the Centro de Investigaciones Paleobiologicas (CIPAL), Universidad Nacional de Cordoba. The technical assistance of the staff of the Laboratorio de Microscopia Electronica y Microanalisis de la Universidad Nacional de San Luis is greatly appreciated.	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Paleoclimatol. Paleoecol.	MAR 1	2009	273	1-2					111	122		10.1016/j.palaeo.2008.12.009	http://dx.doi.org/10.1016/j.palaeo.2008.12.009			12	Geography, Physical; Geosciences, Multidisciplinary; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Physical Geography; Geology; Paleontology	424RI		Green Published			2025-03-11	WOS:000264584600011
J	Versteegh, GJM; Servais, T; Streng, M; Munnecke, A; Vachard, D				Versteegh, Gerard J. M.; Servais, Thomas; Streng, Michael; Munnecke, Axel; Vachard, Daniel			A DISCUSSION AND PROPOSAL CONCERNING THE USE OF THE TERM CALCISPHERES	PALAEONTOLOGY			English	Article						calcareous microfossil; calcisphere; Calcitarcha; Nomenclature; pithonelloid; gilianelloid	CALCAREOUS DINOFLAGELLATE CYSTS; CAMPANIAN-MAASTRICHTIAN BOUNDARY; GILIANELLES MICROPROBLEMATICA; INCERTAE-SEDIS; GERMANY; STRATOTYPE; ACRITARCHS; GOTLAND; FRANCE; FOSSIL	The terminology and grouping of spherical, calcareous microfossils of unknown biological affinity, usually referred to as calcispheres, are diffuse. The term calcispheres is inconsistently used, the morphological and taxonomical concepts are mostly ill-defined and a formal definition is lacking. To resolve this issue, we propose, in analogy with the erection of the Acritarcha for organic microfossils of unknown origin, a new group called Calcitarcha, including all calcareous microfossils with a central cavity for which the biological affinities remain unknown.	[Versteegh, Gerard J. M.; Servais, Thomas; Vachard, Daniel] Univ Sci & Technol Lille, UMR 8157, CNRS Geosyst, F-59655 Villeneuve Dascq, France; [Versteegh, Gerard J. M.] Univ Bremen, Fachbereich 5, D-28334 Bremen, Germany; [Streng, Michael] Uppsala Univ, Dept Earth Sci Palaeobiol, S-75236 Uppsala, Sweden; [Munnecke, Axel] Univ Erlangen Nurnberg, GeoZentrum Nordbayern, Fachgrp Palaoumwelt, D-91054 Erlangen, Germany	Universite de Lille; University of Bremen; Uppsala University; University of Erlangen Nuremberg	Versteegh, GJM (通讯作者)，Univ Sci & Technol Lille, UMR 8157, CNRS Geosyst, Bat SN5, F-59655 Villeneuve Dascq, France.	Versteegh@uni-bremen.de; thomas.servais@univ-lille1.fr; michael.streng@geo.uu.se; axel.munnecke@pal.uni-erlangen.de; daniel.vachard@univ-lille1.fr	Munnecke, Axel/G-3698-2010; Servais, Thomas/S-8045-2019; Servais, Thomas/I-2115-2018; Versteegh, Gerard J.M./H-2119-2011	Servais, Thomas/0000-0002-4089-7874; Versteegh, Gerard J.M./0000-0002-9320-3776; Munnecke, Axel/0000-0002-6898-1082	USTL; Alexander von Humboldt Foundation	USTL; Alexander von Humboldt Foundation(Alexander von Humboldt Foundation)	We thank Katarzyna Bison (Bremen University) for scanning and providing the microphotographs of Tetratropis and P. cardiiformis. Jeremy Young (NHM London) and Malte ElbrAchter (AWI Sylt) and an anonymous reviewer are thanked for helpful suggestions. Financial support for GJMV by the USTL, (Lille) and the Alexander von Humboldt Foundation (Bonn) to AM and TS is gratefully acknowledged.	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J	Kamikawa, R; Nishimura, H; Sako, Y				Kamikawa, Ryoma; Nishimura, Hiroshi; Sako, Yoshihiko			Analysis of the mitochondrial genome, transcripts, and electron transport activity in the dinoflagellate <i>Alexandrium catenella</i> (Gonyaulacales, Dinophyceae)	PHYCOLOGICAL RESEARCH			English	Article						Alexandrium; dinoflagellate; electron transporter; mitochondria; rRNA fragmentation	TOXIC DINOFLAGELLATE; MESSENGER-RNAS; GENES; ORGANIZATION; OXIDASE; COMPLEX; SYSTEM; CYSTS	The mitochondrial (mt) genomes of dinoflagellates are not completely sequenced due to frequent recombination events resulting in a shortage of information about the dinoflagellate mt genome. To obtain a large amount of information, we characterized 14 polymerase chain reaction (PCR) fragments of more than 27 kb of the mt genome of the toxic dinoflagellate Alexandrium catenella Whedon et Kofoid (Balech) using the cob and cox1 genes, the only identified functional mt genes of A. catenella excluding rRNA fragments. The mt PCR clones encode multiple copies of cytochrome b (cob) and cytochrome c oxidase subunit 1 (cox1) bearing several types of 5' or 3' sequences, and two rRNA fragments showing sequence similarity with a large subunit (LSU) rRNA D fragment and LSU RNA2 of apicomplexa. Each mt PCR clone showed different gene arrangements and intergenic sequences suggesting multiple contexts in the mt genome of A. catenella and frequent homologous recombinations. Reverse transcription PCR analysis suggested some types of the multiple copies of cob and cox1 genes are likely non-transcriptional. Further, A. catenella mt mRNAs lacked in-frame termination codons and a canonical initiation codon, excluding an 'atg' codon in cob mRNA. However, we successfully detected the activity of the electron transport proteins suggesting mt translation requires no canonical initiation and termination codons.	[Kamikawa, Ryoma; Nishimura, Hiroshi; Sako, Yoshihiko] Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Lab Marine Microbiol, Kyoto 6068502, Japan	Kyoto University	Kamikawa, R (通讯作者)，Kyoto Univ, Grad Sch Agr, Div Appl Biosci, Lab Marine Microbiol, Kyoto 6068502, Japan.	kami_88@kais.kyoto-u.ac.jp			Japan Society for the Promotion of Science for Young Scientists [1803336, 1906369]	Japan Society for the Promotion of Science for Young Scientists(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science)	We thank S. Yoshimatsu, Akashiwo Research Institute of Kagawa Prefecture, for providing the strain of A. catenella; and T. Amano, Kyoto University, for providing critical comments on this manuscript. R.K and H.N. are research fellows supported by the Japan Society for the Promotion of Science for Young Scientists (no. 1803336 and no. 1906369).	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Res.	MAR	2009	57	1					1	11		10.1111/j.1440-1835.2008.00511.x	http://dx.doi.org/10.1111/j.1440-1835.2008.00511.x			11	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	407JQ					2025-03-11	WOS:000263359800001
J	Selina, MS; Orlova, TY				Selina, M. S.; Orlova, T. Yu.			Morphological peculiarities of <i>Fragilidium mexicanum</i> Balech, 1988 (Dinophyta) from the Far-Eastern Seas of Russia	RUSSIAN JOURNAL OF MARINE BIOLOGY			English	Article						dinoflagellates; morphology; Fragilidium mexicanum; Fragilidium subglobosum; Fragilidium cysts; Sea of Japan; Sea of Okhotsk	DINOFLAGELLATE; CYSTS; COAST	The vegetative cells of Fragilidium mexicanum Balech are recorded from the Far Eastern seas of Russia (Sea of Japan and Sea of Okhotsk) for the first time. Morphological study of both cultured and wild cells of F. mexicanum showed that the shape of the cell and the first (1aEuro(3)) and second (2aEuro(3)) precingular plates, the direction of the slot in plate 1aEuro(3), and the shape of the anterior sulcul plate (S.a.) vary greatly. These features bear similarity to those of F. mexicanum, as well as a closely related species, F. subglobosum. The most conservative characters distinguishing the two species are the shape and size of the first and seventh postcingular plates and the shape of the posterior sulcal plate.	[Selina, M. S.; Orlova, T. Yu.] Russian Acad Sci, Far E Div, Inst Marine Biol, Vladivostok 690041, Russia	Russian Academy of Sciences; National Scientific Center of Marine Biology, Far East Branch of the Russian Academy of Sciences	Selina, MS (通讯作者)，Russian Acad Sci, Far E Div, Inst Marine Biol, Vladivostok 690041, Russia.		Selina, Marina/AAM-6847-2021; Orlova, Tatiana/AAU-8448-2020	Orlova, Tatiana/0000-0002-5246-6967	Russian Foundation for Basic Research [0804-01422]; Russian Academy of Sciences Far East Division DVO-1 [06-1-P16-057]; DVO-3 [06-III-A-06-167]	Russian Foundation for Basic Research(Russian Foundation for Basic Research (RFBR)Spanish Government); Russian Academy of Sciences Far East Division DVO-1(Russian Academy of Sciences); DVO-3	The present research was partially financed by the Russian Foundation for Basic Research (grant no. 0804-01422), and the Russian Academy of Sciences Far East Division DVO-1 (no. 06-1-P16-057) and DVO-3 (nos. 06-III-A-06-167).	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., 1988, Anales Del Instituto De Biologia Serie Zoologia, V58, P479; Cembella AD, 2000, PHYCOLOGIA, V39, P67, DOI 10.2216/i0031-8884-39-1-67.1; Dodge J.D., 1982, P1; Drebes G., 1974, MARINES PHYTOPLANKTO; Fensome R. A., 1993, Micropaleontology, Special Publication; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Gu HF, 2007, ACTA PHYTOTAXON SIN, V45, P828, DOI 10.1360/aps07001; Jeong HJ, 1997, MAR ECOL PROG SER, V151, P299, DOI 10.3354/meps151299; Kim Keun-Yong, 2002, Algae, V17, P11; KONOVALOVA GV, 1988, DINOFLAGELLATY DINOP; Loeblich A.R., 1970, P N AM PAL CONV CHIC, P867; LOEBLICH ALFRED R. III, 1965, TAXON, V14, P15, DOI 10.2307/1216704; LOEBLICH AR, 1980, TAXON, V29, pE321; Loeblich III A. R., 1982, Synopsis and Classification of Living Organisms, P101; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; OWEN KC, 1985, J COASTAL RES, V1, P263; Sournia A., 1986, P1; STEIDINGER KA, 1975, ENVIRON LETT, V9, P129, DOI 10.1080/00139307509435842; Steidinger Karen A., 1995, P387; STOSCH H A, 1969, Helgolaender Wissenschaftliche Meeresuntersuchungen, V19, P569, DOI 10.1007/BF01608816; 1997, ILLUSTRATED GUIDE MA	23	8	9	2	5	MAIK NAUKA/INTERPERIODICA/SPRINGER	NEW YORK	233 SPRING ST, NEW YORK, NY 10013-1578 USA	1063-0740			RUSS J MAR BIOL +	Russ. J. Mar. Biol.	MAR	2009	35	2					151	155		10.1134/S1063074009020060	http://dx.doi.org/10.1134/S1063074009020060			5	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	444DT					2025-03-11	WOS:000265961400006
J	Blanco, EP; Lewis, J; Aldridge, J				Blanco, Eva Perez; Lewis, Jane; Aldridge, John			The germination characteristics of <i>Alexandrium minutum</i> (Dinophyceae), a toxic dinoflagellate from the Fal estuary (UK)	HARMFUL ALGAE			English	Article						Alexandrium; Cysts; Dinoflagellate; Excystment; Germination	GONYAULAX-TAMARENSIS; RESTING CYSTS; LIFE-CYCLE; SCRIPPSIELLA; EXCYSTMENT	The germination characteristics of Alexandrium minutum cysts from the Fal estuary were studied at different conditions of temperature (4-24 degrees C) and salinity (15-35 parts per thousand) and in the dark and low light intensity (2 mu mol(-2) s(-1)). Sediment sub-samples were directly cultured and processed at the end of the experiment for counts of non-germinated cysts. A decrease in the number of cysts was interpreted as germination that was calculated by comparison of the number of cysts over time with that of initial counts. The 50% germination time (time at which 50% of the total initial number of cysts had germinated) was calculated for each condition. A minutum did not germinate in the dark but it germinated under all other conditions studied. Highest germination occurred at salinities of 30 psu and 35 psu and temperatures from 8 degrees C to 24 degrees C (germination rate-expressed as the inverse of the 50% germination time: 1.1-1.2). Lowest germination occurred at 15 psu and 4 degrees C and 24 degrees C (germination rate: 3.9-3.8). However, little variation in germination rates occurred across the conditions studied. As these conditions represent those likely in the estuary it is probable that A. minutum cysts on the surface of the sediments represent a constant source of cells to the water column and sediment disturbance (revealing buried cysts) could rapidly inoculate the water column with vegetative cells. This data was used to develop a model for Alexandrium germination from coastal sediments. (C) 2008 Elsevier B.V. All rights reserved.	[Blanco, Eva Perez; Lewis, Jane] Univ Westminster, Sch Biosci, London W1W 6UW, England; [Aldridge, John] CEFAS Lowestoft Lab, Lowestoft NR33 0HT, Suffolk, England	University of Westminster; Centre for Environment Fisheries & Aquaculture Science	Blanco, EP (通讯作者)，196 Rue Commandant Drogou, F-29200 Brest, France.	evaperezi@gmail.com	Aldridge, John/IWE-0253-2023		MAFF	MAFF(Ministry of Agriculture Forestry & Fisheries - Japan)	This work was carried out in collaboration with CEFAS as part of a Research Contract with MAFF. We are grateful to Linda Percy and Wendy Higman for their assistance with sediment sampling in the Fal estuary.[SS]	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, 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, 1982, ESTUAR COAST SHELF S, V14, P447, DOI 10.1016/S0272-7714(82)80014-0; [Anonymous], 1997, ADV MAR BIOL; BINDER BJ, 1987, J PHYCOL, V23, P99; BLACKBURN SI, 1989, J PHYCOL, V25, P577, DOI 10.1111/j.1529-8817.1989.tb00264.x; BLANCO EP, 2005, THESIS U WESTMINSTER, P137; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; CANNON JA, 1993, DEV MAR BIO, V3, P103; *CFRD, 1999, TOX ALG WORK GROUP M; Dale B., 1983, P69; Hallegraeff GM, 1998, MAR FRESHWATER RES, V49, P415, DOI 10.1071/MF97264; Kremp A, 2000, J PLANKTON RES, V22, P1311, DOI 10.1093/plankt/22.7.1311; LEWIS J, 2002, LIFEHAB LIFE HIST MI, P49; Matrai P, 2005, DEEP-SEA RES PT II, V52, P2560, DOI 10.1016/j.dsr2.2005.06.013; MONTRESOR M, 2005, ALGAL CULTURES ANALO, P91; Nuzzo L, 1999, J PLANKTON RES, V21, P2009, DOI 10.1093/plankt/21.10.2009; PARK HD, 1993, J PHYCOL, V29, P435, DOI 10.1111/j.1529-8817.1993.tb00144.x; PERCY L, 2006, THESIS U WESTMINSTER, P375; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; PROBERT IP, 1999, THESIS U WESTMINSTER, P245; Taylor F.J. R., 1987, The biology of dinoflagellates, P399; *UKDMAP, 1998, ATL SEAS BRIT ISL UK	26	17	19	0	20	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1568-9883			HARMFUL ALGAE	Harmful Algae	FEB	2009	8	3					518	522		10.1016/j.hal.2008.10.008	http://dx.doi.org/10.1016/j.hal.2008.10.008			5	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	409LF					2025-03-11	WOS:000263506500015
J	Streng, M; Banasová, M; Rehaková, D; Willems, H				Streng, Michael; Banasova, Mariana; Rehakova, Daniela; Willems, Helmut			An exceptional flora of calcareous dinoflagellates from the middle Miocene of the Vienna Basin, SW Slovakia	REVIEW OF PALAEOBOTANY AND PALYNOLOGY			English	Article						Thoracosphaeraceae; Dinoflagellata; taxonomy; morphology; Vienna Basin; Badenian; Slovakia	SOUTH ATLANTIC-OCEAN; RIO-GRANDE RISE; DSDP SITE 357; SCRIPPSIELLA-TROCHOIDEA; CYSTS; SEA; DINOPHYCEAE; CALCIODINELLOIDEAE; RECONSTRUCTION; PERIDINIALES	Novel and diverse associations of calcareous dinoflagellate cysts have been discovered in Late Badenian (late Middle Miocene) coastal marine sediments within the Vienna Basin. Samples derive from a clay pit near Devinska Nova Ves, a borough of Bratislava, Slovakia, in which the Late Badenian lectotype section is exposed. Seventeen different taxa, many of them new and of abnormal morphology, have been distinguished and assigned to ten genera. The following seven taxa are newly introduced from the Devinska Nova Ves clay pit: four genera comprising five new species. i.e., Calciconus irregularis, Juergenella remanei, Cylindratus borzae, Posoniella pustulata, Posoniella campestris, one new varietas, i.e., Calcicarpinum perfectum var. poratum, and one new forma, i.e., Caracomia arctica forma duplicata. In addition, the following new combinations have been made: Posoniella tricarinelloides (Versteegh), Juergenella ansata (Hildebrand-Habel and Willems), and Juergenella granulata (Kohring). The genus Melodomuncula Versteegh is emended based on a new interpretation of its tabulation, and the genus Pirumella Bolli is emended because the concept used for the genus is not in accordance with the original description. (c) 2008 Elsevier B.V. All rights reserved.	[Streng, Michael] Uppsala Univ, Inst Geovetenskaper Paleobiol, S-75236 Uppsala, Sweden; [Banasova, Mariana; Rehakova, Daniela] Comenius Univ, Fac Nat Sci, Dept Geol & Paleontol, Bratislava 84212, Slovakia; [Willems, Helmut] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany	Uppsala University; Comenius University Bratislava; University of Bremen	Streng, M (通讯作者)，Uppsala Univ, Inst Geovetenskaper Paleobiol, Villavagen 16, S-75236 Uppsala, Sweden.	michael.streng@geo.uu.se	Reháková, Daniela/AAA-8694-2020	Rehakova, Daniela/0000-0002-3569-9179	Slovak Research and Development Agency [APVV-51-011-305, APVV-0280-07]	Slovak Research and Development Agency(Slovak Research and Development Agency)	We thank H. Mai, N. Kniebel (both Bremen) and I. Holick (Bratislava) for their assistance with the SEM and photographic work. Linguistic corrections by A. C. Daley and G. E. Budd (both Uppsala) are much appreciated. Funding from the Slovak Research and Development Agency (grants APVV-51-011-305 and APVV-0280-07) to support this work is greatly acknowledged. The manuscript benefited from suggestions of two anonymous reviewers.	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J	Williams, M; Haywood, AM; Harper, EM; Johnson, ALA; Knowles, T; Leng, MJ; Lunt, DJ; Okamura, B; Taylor, PD; Zalasiewicz, J				Williams, Mark; Haywood, Alan M.; Harper, Elizabeth M.; Johnson, Andrew L. A.; Knowles, Tanya; Leng, Melanie J.; Lunt, Daniel J.; Okamura, Beth; Taylor, Paul D.; Zalasiewicz, Jan			Pliocene climate and seasonality in North Atlantic shelf seas	PHILOSOPHICAL TRANSACTIONS OF THE ROYAL SOCIETY A-MATHEMATICAL PHYSICAL AND ENGINEERING SCIENCES			English	Article						Pliocene; shelf seas; bryozoans; bivalves; seasonality	MIDDLE PLIOCENE; ISOTOPE FRACTIONATION; CHEILOSTOME BRYOZOANS; SURFACE TEMPERATURES; DINOFLAGELLATE CYST; ARCTICA-ISLANDICA; ZOOID SIZE; MARINE; RECORDS; RECONSTRUCTION	This paper reviews North Atlantic shelf seas palaeoclimate during the interval 4 3 Ma, prior to and incorporating the 'Mid-Pliocene warm period' (ca 3.29 2.97 Ma). Fossil assemblages and stable isotope data demonstrate northwards extension of subtropical faunas along the coast of the Carolinas Virginia (Yorktown and Duplin Formations) relative to the present day, suggesting a more vigorous Florida Current, with reduced seasonality and warm water extending north of Cape Hatteras (reconstructed annual range for Virginia 12 30 degrees C). This interpretation supports conceptual models of increased meridional heat transport for the Pliocene. Sea temperatures for Florida (Lower Pinecrest Beds) were similar to or slightly cooler than (summers 25 27 degrees C) today, and were probably influenced by seasonal upwelling of cold deep water. Reduced seasonality is also apparent in the Coralline Crag Formation of the southern North Sea, with ostracods suggesting winter sea temperatures of 10 degrees C (modern 4 degrees C). However, estimates from Pliocene bivalves (3.6 16.6 degrees C) are similar to or cooler than the present day. This 'mixed' signal is problematic given warmer seas in the Carolinas Virginia, and climate model and oceanographic data that show warmer seas in the 'Mid-Pliocene' eastern North Atlantic. This may be because the Coralline Crag Formation was deposited prior to peak Mid-Pliocene warmth.	[Williams, Mark; Zalasiewicz, Jan] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England; [Haywood, Alan M.] Univ Leeds, Sch Earth & Environm, Leeds LS2 9JT, W Yorkshire, England; [Harper, Elizabeth M.] Univ Cambridge, Dept Earth Sci, Cambridge CB2 3EQ, England; [Johnson, Andrew L. A.] Univ Derby, Sch Sci, Derby DE22 1GB, England; [Knowles, Tanya; Okamura, Beth] Nat Hist Museum, Dept Zool, London SW7 5BD, England; [Taylor, Paul D.] Nat Hist Museum, Dept Palaeontol, London SW7 5BD, England; [Leng, Melanie J.] British Geol Survey, NERC, Isotope Geosci Lab, Nottingham NG12 5GG, England; [Lunt, Daniel J.] Univ Bristol, Sch Geog Sci, Bristol BS8 1SS, Avon, England	University of Leicester; University of Leeds; University of Cambridge; University of Derby; Natural History Museum London; Natural History Museum London; UK Research & Innovation (UKRI); Natural Environment Research Council (NERC); NERC British Geological Survey; University of Bristol	Williams, M (通讯作者)，Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England.	mri@le.ac.uk	Harper, Elizabeth/B-3890-2008; Johnson, Andrew/ABC-1334-2021; Lunt, Daniel/G-9451-2011; Williams, Mark/B-7590-2009	Johnson, Andrew/0000-0001-5727-1889; Leng, Melanie/0000-0003-1115-5166; Lunt, Daniel/0000-0003-3585-6928; Taylor, Paul/0000-0002-3127-080X; Williams, Mark/0000-0002-7987-6069	NERC [nigl010001, bgs04003] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		ALLMON WD, 1996, EVOLUTION ENV TROPIC, P217; Balson P.S., 1993, Proceedings of the Geologists' Association, V104, P59, DOI DOI 10.1016/S0016-7878(08)80155-1; BALSON PS, 1983, J GEOL SOC LONDON, V140, P377, DOI 10.1144/gsjgs.140.3.0377; BERGGREN WA, 1973, NATURE, V243, P391, DOI 10.1038/243391a0; Bigg GR, 2000, J GEOPHYS RES-OCEANS, V105, P8527, DOI 10.1029/2000JC900005; Blow W. 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Ocean Drill. Program, V138, P73, DOI [DOI 10.2973/ODP.PROC.SR.138.106.1995, 10.2973/odp.proc.sr.138.106.1995.]; Swertz OC, 1999, ENVIRON MANAGE, V23, P527, DOI 10.1007/s002679900207; Ward L.W., 1991, GEOLOGY CAROLINAS, P274; WARD LW, 2004, GEOLOGY NATL CAPITAL, P264; WILKINSON I P, 1980, Proceedings of the Geologists' Association, V91, P291; WILLARD DA, 1993, GEOLOGY, V21, P679, DOI 10.1130/0091-7613(1993)021<0679:TAMROC>2.3.CO;2; Witbaard R, 2003, J SEA RES, V50, P11, DOI 10.1016/S1385-1101(03)00039-X; WOOD AM, 1993, QUATERNARY SCI REV, V12, P747, DOI 10.1016/0277-3791(93)90015-E; Zachos J, 2001, SCIENCE, V292, P686, DOI 10.1126/science.1059412; ZACHOS JC, 1994, PALEOCEANOGRAPHY, V9, P353, DOI 10.1029/93PA03266	78	64	77	0	23	ROYAL SOC	LONDON	6-9 CARLTON HOUSE TERRACE, LONDON SW1Y 5AG, ENGLAND	1364-503X	1471-2962		PHILOS T R SOC A	Philos. Trans. R. Soc. A-Math. Phys. Eng. Sci.	JAN 13	2009	367	1886					85	108		10.1098/rsta.2008.0224	http://dx.doi.org/10.1098/rsta.2008.0224			24	Multidisciplinary Sciences	Science Citation Index Expanded (SCI-EXPANDED)	Science & Technology - Other Topics	375YW	18852093	Green Submitted			2025-03-11	WOS:000261150700006
J	Mertens, KN; Ribeiro, S; Bouimetarhan, I; Caner, H; Nebout, NC; Dale, B; De Vernal, A; Ellegaard, M; Filipova, M; Godhe, A; Goubert, E; Grosfjeld, K; Holzwarth, U; Kotthoff, U; Leroy, SAG; Londeix, L; Marret, F; Matsuoka, K; Mudie, PJ; Naudts, L; Peña-Manjarrez, JL; Persson, A; Popescu, SM; Pospelova, V; Sangiorgi, F; van der Meer, MTJ; Vink, A; Zonneveld, KAF; Vercauteren, D; Vlassenbroeck, J; Louwye, S				Mertens, Kenneth N.; Ribeiro, Sofia; Bouimetarhan, Ilham; Caner, Hulya; Nebout, Nathalie Combourieu; Dale, Barrie; De Vernal, Anne; Ellegaard, Marianne; Filipova, Mariana; Godhe, Anna; Goubert, Evelyne; Grosfjeld, Kari; Holzwarth, Ulrike; Kotthoff, Ulrich; Leroy, Suzanne A. G.; Londeix, Laurent; Marret, Fabienne; Matsuoka, Kazumi; Mudie, Peta J.; Naudts, Lieven; Luis Pena-Manjarrez, Jose; Persson, Agneta; Popescu, Speranta-Maria; Pospelova, Vera; Sangiorgi, Francesca; van der Meer, Marcel T. J.; Vink, Annemiek; Zonneveld, Karin A. F.; Vercauteren, Dries; Vlassenbroeck, Jelle; Louwye, Stephen			Process length variation in cysts of a dinoflagellate, <i>Lingulodinium machaerophorum</i>, in surface sediments: Investigating its potential as salinity proxy	MARINE MICROPALEONTOLOGY			English	Article						Lingulodinium machaerophorum; Processes; Lingulodinium polyedrum; Biometry; Palaeosalinity; Dinoflagellate cysts	LAST 2000 YEARS; RED TIDE; EMILIANIA-HUXLEYI; MARINE-SEDIMENTS; NORTH-ATLANTIC; RESTING CYSTS; NW AFRICA; SEA; HOLOCENE; EASTERN	A biometrical analysis of the dinoflagellate cyst Lingulodinium machaerophorum [Deflandre, G., Cookson, I.C., 1955. Fossil microplankton from Australia late Mesozoic and Tertiary sediments. Australian journal of Marine and Freshwater Research 6: 242-313.] Wall, 1967 in 144 globally distributed surface sediment samples revealed that the average process length is related to summer salinity and temperature at a water depth of 30 m by the equation (salinity/temperature) = (0.078*average process length + 0.534) with R-2=0.69. This relationship can be used to reconstruct palaeosalinities, albeit with caution. The particular ecological window can be associated with known distributions of the corresponding motile stage Lingulodinium polyedrum (Stein) Dodge, 1989. Confocal laser microscopy showed that the average process length is positively related to the average distance between process bases (R-2=0.78), and negatively related to the number of processes (R-2=0.65). These results document the existence of two end members in cyst formation: one with many short, densely distributed processes and one with a few, long, widely spaced processes. which can be respectively related to low and high salinity/temperature ratios. Obstruction during formation of the Cysts Causes anomalous distributions of the processes. From a biological perspective, processes function to facilitate sinking of the cysts through clustering. (c) 2008 Elsevier B.V. All rights reserved.	[Mertens, Kenneth N.; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Ribeiro, Sofia; Ellegaard, Marianne] Univ Copenhagen, Fac Sci, Dept Biol, Aquat Biol Sect, DK-1353 Copenhagen K, Denmark; [Bouimetarhan, Ilham; Holzwarth, Ulrike] Univ Bremen, Ctr Marine Environm Sci Marum, D-28334 Bremen, Germany; [Caner, Hulya] Istanbul Univ, Inst Marine Sci & Management, TR-34470 Vefa, Turkey; [Nebout, Nathalie Combourieu] CEA, Domaine CNRS, UVSQ, UMR,IPSL,LSCE, F-91198 Gif Sur Yvette, France; [Dale, Barrie] Univ Oslo, Dept Geosci, N-0316 Oslo, Norway; [De Vernal, Anne] Univ Quebec, GEOTOP, Montreal, PQ H3C 3P8, Canada; [Filipova, Mariana] Museum Nat Hist, Varna 9000, Bulgaria; [Persson, Agneta] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden; [Goubert, Evelyne] Univ Bretagne Sud, Lab STICC, Univ Europeenne Bretagne, F-56000 Vannes, France; [Grosfjeld, Kari] Geol Survey Norway, N-7491 Trondheim, Norway; [Kotthoff, Ulrich] Goethe Univ Frankfurt, Inst Geosci, D-60438 Frankfurt M, Germany; [Leroy, Suzanne A. G.] Brunel Univ, Inst Environm, Uxbridge UB8 3PH, Middx, England; [Londeix, Laurent] Univ Bordeaux 1, EPOC, UMR 5805, F-33405 Talence, France; [Marret, Fabienne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Matsuoka, Kazumi] Inst E China Sea Res ECSER, Nagasaki 8528521, Japan; [Mudie, Peta J.] Geol Survey Canada Atlantic, Dartmouth, NS B2Y 4A2, Canada; [Naudts, Lieven] Univ Ghent, RCMG, B-9000 Ghent, Belgium; [Luis Pena-Manjarrez, Jose] Ctr Estudios Tecnol Mar, Ensenada, Baja California, Mexico; [Popescu, Speranta-Maria] Univ Lyon 1, CNRD, UMR 5125, Lab PaleoEnvironm & PaleobioSphere, F-69622 Villeurbanne, France; [Pospelova, Vera] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 3P6, Canada; [Sangiorgi, Francesca] Univ Utrecht, Lab Palaeobot & Palynol, Inst Environm Biol, Utrecht, Netherlands; [van der Meer, Marcel T. J.] NIOZ Royal Netherlands Inst Sea Res, NL-1790 AB Den Burg, Netherlands; [Vink, Annemiek] Fed Inst Geosci & Nat Resources, D-30655 Hannover, Germany; [Zonneveld, Karin A. F.] Univ Bremen, Fachbereich Geowissensch 5, D-28334 Bremen, Germany; [Vercauteren, Dries] Univ Ghent, Lab Gen Biochem & Phys Pharm, B-9000 Ghent, Belgium; [Vlassenbroeck, Jelle] Univ Ghent, UGCT, B-9000 Ghent, Belgium; [Ribeiro, Sofia] Univ Lisbon, Fac Ciencias, Inst Oceanog, P-1749016 Lisbon, Portugal; [Ribeiro, Sofia] LNEG, Dept Geol Marinha, P-2721866 Zambujal, Alfragide, Portugal; [Godhe, Anna] Univ Gothenburg, Dept Marine Ecol, SE-40530 Gothenburg, Sweden	Ghent University; University of Copenhagen; University of Bremen; Istanbul University; Centre National de la Recherche Scientifique (CNRS); Universite Paris Saclay; CEA; Universite Paris Cite; University of Oslo; University of Quebec; University of Quebec Montreal; University of Gothenburg; Universite de Bretagne Occidentale; Geological Survey of Norway; Goethe University Frankfurt; Brunel University; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Liverpool; Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Ghent University; Universite Claude Bernard Lyon 1; University of Victoria; Utrecht University; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); University of Bremen; Ghent University; Ghent University; Universidade de Lisboa; Laboratorio Nacional de Energia e Geologia IP (LNEG); University of Gothenburg	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281 S8, B-9000 Ghent, Belgium.	Kenneth.Mertens@ugent.be	Leroy, Suzanne/D-3996-2009; Mertens, Kenneth/AAO-9566-2020; Caner, Hulya/AAG-5807-2019; Ribeiro, Sofia/AAZ-2782-2021; Bouimetarhan, Ilham/D-2388-2011; Vink, Annemiek/GXG-6435-2022; Ribeiro, Sofia/G-9213-2018; Ellegaard, Marianne/H-6748-2014; de Vernal, Anne/D-5602-2013; van der Meer, Marcel/L-3450-2013; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Sangiorgi, Francesca/0000-0003-4233-6154; Bouimetarhan, Ilham/0000-0003-3369-3811; Vink, Annemiek/0000-0002-5178-9721; Ribeiro, Sofia/0000-0003-0672-9161; CANER, HULYA/0000-0001-6197-2813; Ellegaard, Marianne/0000-0002-6032-3376; Pospelova, Vera/0000-0003-4049-8133; de Vernal, Anne/0000-0001-5656-724X; Persson, Agneta/0000-0003-0202-6514; van der Meer, Marcel/0000-0001-6454-1752; Popescu, Speranta- Maria/0000-0001-5345-395X; Louwye, Stephen/0000-0003-4814-4313; Marret-Davies, Fabienne/0000-0003-4244-0437; Mertens, Kenneth/0000-0003-2005-9483; Combourieu-Nebout, Nathalie/0000-0002-3604-5986				[Anonymous], TRACEURS PALYNOLOGIQ; 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Micropaleontol.	JAN 10	2009	70	1-2					54	69		10.1016/j.marmicro.2008.10.004	http://dx.doi.org/10.1016/j.marmicro.2008.10.004			16	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	405HR		Green Submitted			2025-03-11	WOS:000263214300005
J	Persson, A; Smith, BC				Persson, Agneta; Smith, Barry C.			Grazing on a natural assemblage of ciliate and dinoflagellate cysts by the eastern oyster <i>Crassostrea virginica</i>	AQUATIC BIOLOGY			English	Article						Dinoflagellate; Cyst; Crassostrea virginica; Oyster; Grazing; Digesting	RESTING CYSTS; SCRIPPSIELLA-LACHRYMOSA; GLOBAL DIVERSITY; SEDIMENTS; GULF; GERMINATION; CILIOPHORA; MORPHOLOGY; DYNAMICS; PROTOZOA	A natural dinoflagellate- and ciliate-cyst community from anoxic sediment collected from New Haven, Long Island Sound, was concentrated with a particle sorter and fed to oysters Crassostrea virginica. The total number of cysts and the species composition of cysts in beakers containing live oysters were measured before and after feeding by the oysters. The oysters significantly reduced the numbers of both dinoflagellate and ciliate cysts. Both empty cyst walls and filled (live) cysts were consumed. The oysters decreased the number of total cysts to less than half compared to control beakers containing empty oyster shells. Results from the experiment show that natural assemblages of cysts in sediment are degraded by the feeding activities of oysters. If toxic cysts were present in natural sediments resuspended from the bottom, digestion of resting cysts could lead to toxin accumulation in oysters. There was no major shift in species composition of cysts; cysts known as fossilizable were destroyed, as well as cysts not known to be very resistant or preservable.	[Persson, Agneta; Smith, Barry C.] Natl Marine Fisheries Serv, NOAA, NE Fisheries Sci Ctr, Milford Lab, Milford, CT 06460 USA	National Oceanic Atmospheric Admin (NOAA) - USA	Smith, BC (通讯作者)，Natl Marine Fisheries Serv, NOAA, NE Fisheries Sci Ctr, Milford Lab, 212 Rogers Ave, Milford, CT 06460 USA.	barry.smith@noaa.gov		Persson, Agneta/0000-0003-0202-6514	National Research Council Research Associateship; National Oceanic and Atmospheric Administration; National Marine Fisheries Service laboratory in Milford, Connecticut	National Research Council Research Associateship; National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); National Marine Fisheries Service laboratory in Milford, Connecticut	This research was performed while A.P. held a National Research Council Research Associateship Award at the National Oceanic and Atmospheric Administration, National Marine Fisheries Service laboratory in Milford, Connecticut. We are very grateful to G. H. Wikfors for comments on the manuscript; to J. Alix for laboratory assistance; to M. S. Dixon, NOAA Diving Program, for diving for mud; to Capt. R. Alix and the RV 'Victor Loosanoff; and to K. Rivara, Noank, Connecticut Aquaculture facility. Mention of trade names does not imply endorsement.	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Biol.		2009	6	1-3					227	233		10.3354/ab00129	http://dx.doi.org/10.3354/ab00129			7	Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Marine & Freshwater Biology	491FF		Bronze			2025-03-11	WOS:000269562400024
J	Tillmann, U; Hansen, PJ				Tillmann, Urban; Hansen, Per Juel			Allelopathic effects of <i>Alexandrium tamarense</i> on other algae: evidence from mixed growth experiments	AQUATIC MICROBIAL ECOLOGY			English	Article						Alexandrium; PST; Paralytic shellfish toxin; Allelopathy; Growth; Algae; pH	DINOFLAGELLATE ALEXANDRIUM; FAVELLA-TARAIKAENSIS; PHYTOPLANKTON; OSTENFELDII	The effect of 2 strains (Alex2 and Alex5) of the marine red tide dinoflagellate Alexandrium tamarense on 10 other planktonic algal target species common in temperate waters was studied in mixed growth experiments under nutrient-rich conditions. In a comparative approach, the 2 strains of A. tamarense, similar in their cellular paralytic shellfish toxin (PST) content, were selected because of their fundamentally different lytic potencies. The Alex2 strain clearly affected all target algae while the Alex5 strain had no negative effect on the growth of any of the target species during the study period, even though cell concentrations of Alex5 became very high (2 x 10(4) cells ml(-1)). As both strains contained comparable amounts of PST, this confirmed previous suggestions that so far unidentified compounds are causing the negative effects on other algae. Sensitivity of the tested algae to Alex2 differed considerably. The growth of some species was affected at very low Alex2 cell concentrations (< 10(2) cells ml(-1)), while the growth of other algae was not affected until cell concentrations exceeded 10(3) cells ml(-1). While a complete dieoff was the ultimate fate for almost all target species when grown in mixed culture with Alex2, Scrippsiella trochoidea formed temporary cysts, the number of which remained constant during the course of the experiment. The pH in the mixed cultures increased as the cultures grew dense. This had a substantial effect on Alex5 in the mixed cultures, in which Alex5 eventually died off because the target species have a higher tolerance to high pH. pH values did not determine the outcome of the experiments with Alex2 because the adverse effects of Alex2 on the growth of the other algae was evident before pH values became too high. Lytic extracellular compounds, which are produced by the large majority of A. tamarense strains tested so far, clearly have the potential to benefit this dinoflagellate by reducing competitor growth rates.	[Tillmann, Urban] Alfred Wegener Inst Polar & Marine Res, D-27570 Bremerhaven, Germany; [Hansen, Per Juel] Univ Copenhagen, Marine Biol Lab, DK-3000 Helsingor, Denmark	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Copenhagen	Tillmann, U (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Handelshafen 12, D-27570 Bremerhaven, Germany.	urban.tillmann@awi.de	Hansen, Per Juel/E-9969-2011	Hansen, Per Juel/0000-0003-0228-9621				Adolf JE, 2007, HARMFUL ALGAE, V6, P400, DOI 10.1016/j.hal.2006.12.003; ALPERMANN T, J PHYCOL IN PRESS; Alpermann TJ, 2009, MOL ECOL, V18, P2122, DOI 10.1111/j.1365-294X.2009.04165.x; Cembella AD, 2002, HARMFUL ALGAE, V1, P313, DOI 10.1016/S1568-9883(02)00048-3; Cembella AD, 2003, PHYCOLOGIA, V42, P420, DOI 10.2216/i0031-8884-42-4-420.1; DAHL E, 1989, NOVEL PHYTOPLANKTON, P383; Fistarol GO, 2004, ENVIRON MICROBIOL, V6, P791, DOI 10.1111/j.1462-2920.2004.00609.x; Fistarol GO, 2004, AQUAT MICROB ECOL, V35, P45, DOI 10.3354/ame035045; Fulco VK, 2007, J MAR BIOL ASSOC UK, V87, P1085, DOI 10.1017/S002531540705374X; Granéli E, 2006, ECOL STU AN, V189, P189, DOI 10.1007/978-3-540-32210-8_15; HANSEN PJ, 1992, J PHYCOL, V28, P597, DOI 10.1111/j.0022-3646.1992.00597.x; Hansen PJ, 2002, AQUAT MICROB ECOL, V28, P279, DOI 10.3354/ame028279; HANSEN PJ, 1989, MAR ECOL PROG SER, V53, P105, DOI 10.3354/meps053105; Jeong HJ, 2005, AQUAT MICROB ECOL, V40, P133, DOI 10.3354/ame040133; Kamiyama T, 2006, MAR ECOL PROG SER, V317, P57, DOI 10.3354/meps317057; KELLER MD, 1987, J PHYCOL, V23, P633; Legrand C, 2003, PHYCOLOGIA, V42, P406, DOI 10.2216/i0031-8884-42-4-406.1; Mortensen A.M., 1985, P165; Schmidt LE, 2001, MAR ECOL PROG SER, V216, P67, DOI 10.3354/meps216067; Shimizu Y, 1996, ANNU REV MICROBIOL, V50, P431, DOI 10.1146/annurev.micro.50.1.431; Skovgaard A, 2003, LIMNOL OCEANOGR, V48, P1161, DOI 10.4319/lo.2003.48.3.1161; SYKES PF, 1987, MAR BIOL, V94, P19, DOI 10.1007/BF00392895; Tillmann U, 2003, AQUAT MICROB ECOL, V32, P73, DOI 10.3354/ame032073; Tillmann U, 2002, MAR ECOL PROG SER, V230, P47, DOI 10.3354/meps230047; Tillmann U., 2008, Proceedings of the 12. International conference on harmful algae. International society for the study of harmful algae and intergovernmental oceanographic commission of UNESCO, P12; Tillmann U, 2008, HARMFUL ALGAE, V7, P52, DOI 10.1016/j.hal.2007.05.009; Tillmann U, 2007, J PLANKTON RES, V29, P527, DOI 10.1093/plankt/fbm034; Tillmann U, 2009, HARMFUL ALGAE, V8, P759, DOI 10.1016/j.hal.2009.03.005; Toth GB, 2004, P ROY SOC B-BIOL SCI, V271, P733, DOI 10.1098/rspb.2003.2654; TURNER JT, 1998, PHYSL ECOLOGY HARMFU, P453; ULITZUR S, 1973, BIOCHIM BIOPHYS ACTA, V298, P673, DOI 10.1016/0005-2736(73)90083-7	31	69	72	1	28	INTER-RESEARCH	OLDENDORF LUHE	NORDBUNTE 23, D-21385 OLDENDORF LUHE, GERMANY	0948-3055	1616-1564		AQUAT MICROB ECOL	Aquat. Microb. Ecol.		2009	57	1					101	112		10.3354/ame01329	http://dx.doi.org/10.3354/ame01329			12	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	509YZ		Bronze			2025-03-11	WOS:000271056500009
J	Portune, KJ; Coyne, KJ; Hutchins, DA; Handy, SM; Cary, SC				Portune, Kevin J.; Coyne, Kathryn J.; Hutchins, David A.; Handy, Sara M.; Cary, S. Craig			Quantitative real-time PCR for detecting germination of <i>Heterosigma akashiwo</i> and <i>Chattonella subsalsa</i> cysts from Delaware's Inland Bays, USA	AQUATIC MICROBIAL ECOLOGY			English	Article						Raphidophytes; Cyst germination; Quantitative real-time PCR; Heterosigma akashiwo; Chattonella subsalsa	RED-TIDE FLAGELLATE; OLISTHODISCUS-LUTEUS CHRYSOPHYCEAE; LIFE-CYCLE; RAPHIDOPHYCEAE; DINOFLAGELLATE; ANTIQUA; JAPAN; SEA; DNA; DYNAMICS	Cyst germination of strains of the harmful algal species Heterosigma akashiwo and Chattonella subsalsa (Raphidophyceae) from Delaware's (USA) Inland Bays was studied both in the field and laboratory during the spring and early summer seasons. Quantitative real-time PCR was employed for detection and quantification of cells in natural sediments and of germinated vegetative cells in the water column. Temperature, salinity, and dissolved nutrient concentrations were examined in field mesocosm experiments to identify physicochemical factors associated with germination, while the effects of temperature and light on germination were examined in laboratory experiments. We detected and monitored a wide range of cyst abundances of H. akashiwo (from 164 to 2820 cysts cm 3 wet sediment) and C. subsalsa cysts (from 2 to 135 Cysts cm(-3) wet sediment) in environmental sediments. Germinated H. akashiwo cells were detected in situ after temperatures reached 15 degrees C. However, in laboratory studies, H. akashiwo germination occurred at even lower temperatures (10 degrees C), which was considerably lower than typical germination temperatures from similar Japanese strains. In contrast, a temperature of 20 degrees C stimulated C. subsalsa germination in both field and laboratory studies, although germination still occurred at low temperatures (10 degrees C). The presence or absence of light did not affect the germination of C. subsalsa. The low quantities of detected vegetative cells from cyst germination for both H. akashiwo and C. subsalsa suggest the inoculation of a small number of vegetative cells into the water column during the spring and early summer months.	[Portune, Kevin J.; Coyne, Kathryn J.; Hutchins, David A.; Handy, Sara M.; Cary, S. Craig] Univ Delaware, Coll Marine & Earth Studies, Lewes, DE 19958 USA	University of Delaware	Cary, SC (通讯作者)，Univ Waikato, Dept Biol Sci, Private Bag 3105, Hamilton, New Zealand.	caryc@udel.edu	Portune, Kevin/L-3943-2017; Handy, Sara/C-6195-2008; Hutchins, David/D-3301-2013	Cary, Stephen/0000-0002-2876-2387; Portune, Kevin/0000-0002-3428-8044; Coyne, Kathryn/0000-0001-8846-531X; Hutchins, David/0000-0002-6637-756X; Handy, Sara/0000-0003-3861-4609	USA EPA-ECOHAB STAR Grant [8310401]; Center for the Inland Bays Grant [EPA 99399-008-2]; Delaware EPSCoR graduate research fellowship	USA EPA-ECOHAB STAR Grant(United States Environmental Protection Agency); Center for the Inland Bays Grant; Delaware EPSCoR graduate research fellowship	We acknowledge USA EPA-ECOHAB STAR Grant 8310401 (to D.A.H., S.C.C., and K.J.C.), Center for the Inland Bays Grant EPA 99399-008-2 (to S.C.C. and K.J.P.), and a Delaware EPSCoR graduate research fellowship to K.J.P. Thanks to G. Luther, D. Miller, E. Whereat, J. Scudlark, Y. Zhang, M. Warner, T. Moore, R. Dale, E. Demir, and the DE Phytoplankton Monitoring Group for assistance with experimental design, data collection and analysis, or interpretation of results. Thanks to M. Chofsky and B. Winkler for extensive use of their docks for field sampling.	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Microb. Ecol.		2009	55	3					229	239		10.3354/ame01292	http://dx.doi.org/10.3354/ame01292			11	Ecology; Marine & Freshwater Biology; Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Marine & Freshwater Biology; Microbiology	470HP		Bronze			2025-03-11	WOS:000267966100003
J	Gooday, AJ; Jorissen, F; Levin, LA; Middelburg, JJ; Naqvi, SWA; Rabalais, NN; Scranton, M; Zhang, J				Gooday, A. J.; Jorissen, F.; Levin, L. A.; Middelburg, J. J.; Naqvi, S. W. A.; Rabalais, N. N.; Scranton, M.; Zhang, J.			Historical records of coastal eutrophication-induced hypoxia	BIOGEOSCIENCES			English	Review							SEA BENTHIC FORAMINIFERA; GULF-OF-MEXICO; WALLED DINOFLAGELLATE CYSTS; OXYGEN MINIMUM ZONE; SANTA-BARBARA BASIN; ORGANIC-CARBON FLUX; CENTRAL BALTIC SEA; LONG-TERM CHANGES; CHESAPEAKE BAY; MISSISSIPPI RIVER	Under certain conditions, sediment cores from coastal settings subject to hypoxia can yield records of environmental changes over time scales ranging from decades to millennia, sometimes with a resolution of as little as a few years. A variety of biological and geochemical indicators (proxies) derived from such cores have been used to reconstruct the development of eutrophication and hypoxic conditions over time. Those based on (1) the preserved remains of benthic organisms (mainly foraminiferans and ostracods), (2) sedimentary features (e.g. laminations) and (3) sediment chemistry and mineralogy (e.g. presence of sulphides and redox-sensitive trace elements) reflect conditions at or close to the seafloor. Those based on (4) the preserved remains of planktonic organisms (mainly diatoms and dinoflagellates), (5) pigments and lipid biomarkers derived from prokaryotes and eukaryotes and (6) organic C, N and their stable isotope ratios reflect conditions in the water column. However, the interpretation of these indicators is not straightforward. A central difficulty concerns the fact that hypoxia is strongly correlated with, and often induced by, organic enrichment caused by eutrophication, making it difficult to separate the effects of these phenomena in sediment records. The problem is compounded by the enhanced preservation in anoxic and hypoxic sediments of organic microfossils and biomarkers indicating eutrophication. The use of hypoxia-specific proxies, such as the trace metals molybdenum and rhenium and the bacterial biomarker isorenieratene, together with multi-proxy approaches, may provide a way forward. All proxies of bottom-water hypoxia are basically qualitative; their quantification presents a major challenge to which there is currently no satisfactory solution. Finally, it is important to separate the effects of natural ecosystem variability from anthropogenic effects. Despite these problems, in the absence of historical data for dissolved oxygen concentrations, the analysis of sediment cores can provide plausible reconstructions of the temporal development of human-induced hypoxia, and associated eutrophication, in vulnerable coastal environments.	[Gooday, A. J.] Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England; [Jorissen, F.] BIAF, EA 2644, UPRES, Lab Recent & Fossil Bioindicators, F-49045 Angers, France; [Jorissen, F.] LEBIM, Ile Dyeu, France; [Levin, L. A.] Univ Calif San Diego, Scripps Inst Oceanog, Integrat Oceanog Div, La Jolla, CA 92093 USA; [Middelburg, J. J.] Ctr Estuarine & Marine Ecol, NIOO KNAW, NL-4400 AC Yerseke, Netherlands; [Middelburg, J. J.] Univ Utrecht, Fac Geosci, NL-3508 TA Utrecht, Netherlands; [Naqvi, S. W. A.] Natl Inst Oceanog, Panaji 403004, Goa, India; [Rabalais, N. N.] Louisiana Univ Marine Consortium, Chauvin, LA 70344 USA; [Scranton, M.] SUNY Stony Brook, Sch Marine & Atmospher Sci SoMAS, Stony Brook, NY 11794 USA; [Zhang, J.] E China Normal Univ, State Key Lab Estuarine & Coastal Res, Shanghai 200062, Peoples R China	NERC National Oceanography Centre; Universite d'Angers; University of California System; University of California San Diego; Scripps Institution of Oceanography; Royal Netherlands Academy of Arts & Sciences; Netherlands Institute of Ecology (NIOO-KNAW); Utrecht University; Council of Scientific & Industrial Research (CSIR) - India; CSIR - National Institute of Oceanography (NIO); State University of New York (SUNY) System; Stony Brook University; East China Normal University	Gooday, AJ (通讯作者)，Natl Oceanog Ctr, Southampton SO14 3ZH, Hants, England.	ang@noc.soton.ac.uk	Levin, Lisa/KFQ-2165-2024; Gooday, Andrew/ABB-4267-2020; Rabalais, Nancy/GQA-6087-2022; Jorissen, Frans/D-2392-2009; Naqvi, Syed Wasif Ali/ACJ-3163-2022; Middelburg, Jack/B-4951-2011	Levin, Lisa/0000-0002-2858-8622; Middelburg, Jack/0000-0003-3601-9072; Jorissen, Frans/0000-0002-9325-6085; Rabalais, Nancy N./0000-0002-1514-837X	NERC [soc010009] Funding Source: UKRI	NERC(UK Research & Innovation (UKRI)Natural Environment Research Council (NERC))		Adelson JM, 2001, GEOCHIM COSMOCHIM AC, V65, P237, DOI 10.1016/S0016-7037(00)00539-1; Agnihotri R, 2008, HOLOCENE, V18, P755, DOI 10.1177/0959683608091795; ALTABET MA, 1994, GLOBAL BIOGEOCHEM CY, V8, P103, DOI 10.1029/93GB03396; ALVE E, 1990, NATO ADV SCI I C-MAT, V327, P661; Alve E, 1995, MAR MICROPALEONTOL, V25, P269, DOI 10.1016/0377-8398(95)00026-7; ALVE E, 1995, J FORAMIN RES, V25, P190, DOI 10.2113/gsjfr.25.3.190; Alve E., 1991, Holocene, V1, P243, DOI 10.1177/095968369100100306; Alve E, 2003, ESTUAR COAST SHELF S, V57, P501, DOI 10.1016/S0272-7714(02)00383-9; Alve E., 2000, Environmental Micropaleontology, P323; ALVE E, 2006, FORAMS 2006, V29, P520; Andrén E, 1999, HOLOCENE, V9, P25, DOI 10.1191/095968399676523977; Andrén E, 1999, ESTUAR COAST SHELF S, V48, P665, DOI 10.1006/ecss.1999.0480; Arnaboldi M, 2007, PALAEOGEOGR PALAEOCL, V249, P425, DOI 10.1016/j.palaeo.2007.02.016; BARMAWIDJAJA DM, 1995, MAR GEOL, V122, P367, DOI 10.1016/0025-3227(94)00121-Z; Behl R.J., 1995, PROC ODP, V146, P295; Behl RJ, 1996, NATURE, V379, P243, DOI 10.1038/379243a0; Bennion H, 1996, ENVIRON SCI TECHNOL, V30, P2004, DOI 10.1021/es9508030; BERNER RA, 1984, GEOCHIM COSMOCHIM AC, V48, P605, DOI 10.1016/0016-7037(84)90089-9; Bernhard JM, 1999, MODERN FORAMINIFERA, P201; Bernhard JM, 2000, MICROPALEONTOLOGY, V46, P38; Bianchi TS, 2000, LIMNOL OCEANOGR, V45, P716, DOI 10.4319/lo.2000.45.3.0716; Bianchi TS, 2000, J EXP MAR BIOL ECOL, V251, P161, DOI 10.1016/S0022-0981(00)00212-4; Black DE, 2007, PALEOCEANOGRAPHY, V22, DOI 10.1029/2007PA001427; Blackwelder P, 1996, QUATERN INT, V31, P19, DOI 10.1016/1040-6182(95)00018-E; Blazejak A, 2005, APPL ENVIRON MICROB, V71, P1553, DOI 10.1128/AEM.71.3.1553-1561.2005; Boesch DF, 2002, ESTUARIES, V25, P886, DOI 10.1007/BF02804914; Boomer I, 2002, QUATERNARY ENVIRONMENTAL MICROPALAEONTOLOGY, P115; Brandes JA, 2002, GLOBAL BIOGEOCHEM CY, V16, DOI 10.1029/2001GB001856; Brandes JA, 1998, LIMNOL OCEANOGR, V43, P1680, DOI 10.4319/lo.1998.43.7.1680; Bratton JF, 2003, GEOCHIM COSMOCHIM AC, V67, P3385, DOI 10.1016/S0016-7037(03)00131-5; Brhret J.-G., 1991, Geol. 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J	Sluijs, A; Brinkhuis, H				Sluijs, A.; Brinkhuis, H.			A dynamic climate and ecosystem state during the Paleocene-Eocene Thermal Maximum: inferences from dinoflagellate cyst assemblages on the New Jersey Shelf	BIOGEOSCIENCES			English	Article							CARBON-ISOTOPE EXCURSION; NEW-ZEALAND; BIGHORN BASIN; SEA-LEVEL; OCEAN; MARINE; RECORD; BOUNDARY; SECTION; METHANE	Late Paleocene and Early Eocene climates and ecosystems underwent significant change during several transient global warming phases, associated with rapidly increasing atmospheric carbon concentrations, of which the Paleocene-Eocene Thermal Maximum (PETM; similar to 55.5 Ma) is best studied. While biotic response to the PETM as a whole (similar to 170 kyrs) has been relatively well documented, variations during the PETM have been neglected. Here we present organic dinoflagellate cyst (dinocyst) distribution patterns across two stratigraphically expanded PETM sections from the New Jersey Shelf, Bass River and Wilson Lake. Many previously studied sites show a uniform abundance of the thermophilic and presumably heterotrophic taxon Apectodinium that spans the entire carbon isotope excursion (CIE) of the PETM. In contrast, the New Jersey sections show large variations in abundances of many taxa. during the PETM, including the new species Florentinia reichartii that we formally propose. We infer paleoecological preferences of taxa that show temporal abundance peaks, both qualitative and absolute quantitative, from empirical as well as statistical information, i.e., principle (PCA) and canonical correspondence analyses (CCA). In the CCAs, we combine the dinocyst data with previously published environmental proxy data from these locations, such as TEX86 paleothermometry, magnetic susceptibility and sedimentary size fraction. The combined information supports previous inferences that sea level rose during the PETM, but also indicates a (regional) increase in fresh-water runoff that started similar to 10 kyr after the onset of the CIE, and perhaps precession-paced cycles in sea surface productivity. The highly variable dinocyst assemblages of the PETM contrast with rather stable Upper Paleocene assemblages, which suggests that carbon input caused a dynamic climate state, at least regionally.	[Sluijs, A.; Brinkhuis, H.] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	Utrecht University	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	a.sluijs@uu.nl	Brinkhuis, Henk/B-4223-2009; Sluijs, Appy/B-3726-2009	Brinkhuis, Henk/0000-0003-0253-6610; Sluijs, Appy/0000-0003-2382-0215	Netherlands Organisation for Scientific Research [863.07.001]; Utrecht Biogeology Center; LPP Foundation	Netherlands Organisation for Scientific Research(Netherlands Organization for Scientific Research (NWO)); Utrecht Biogeology Center; LPP Foundation	This research used samples and data provided by the Ocean Drilling Program (ODP; now Integrated Ocean Drilling Program: IODP). Funding for this research was provided by the Netherlands Organisation for Scientific Research to AS (NWO-VENI grant #863.07.001), the Utrecht Biogeology Center and the LPP Foundation. We thank Jim Browning, Ken Miller (both Rutgers University), John Firth and Gar Esmay (both IODP) for help regarding the logistics around sampling the Bass River section, and Samantha Gibbs (NOC, Southampton), Ellen Thomas (Yale) and James Zachos (UC Santa Cruz) for providing samples from the Wilson Lake section. We thank Jim Riding and two anonymous reviewers for their comments, which significantly improved the paper. We thank Andy Lotter (Utrecht University) for advice regarding PCA and CCA analyses and Urbino Summer School in Paleoclimatology (USSP) instructors and students and Peter Lippert (UC Santa Cruz) for discussions. Leonard Bik, Jan van Tongeren and Natasja Welters are thanked for technical support.	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J	Mertens, KN; González, C; Delusina, I; Louwye, S				Mertens, Kenneth Neil; Gonzalez, Catalina; Delusina, Irina; Louwye, Stephen			30 000 years of productivity and salinity variations in the late Quaternary Cariaco Basin revealed by dinoflagellate cysts	BOREAS			English	Article							INTERTROPICAL CONVERGENCE ZONE; GLOBIGERINOIDES-RUBER WHITE; RAPID CLIMATE CHANGES; SOUTH CHINA SEA; TROPICAL ATLANTIC; ORGANIC-MATTER; LAKE VALENCIA; VEGETATION RESPONSE; HOLOCENE; VARIABILITY	Dinoflagellate cysts and other palynomorphs were studied from ODP Hole 1002C in the Cariaco Basin over the past 30 000 years. The assemblage shifts between a dominance of heterotrophic dinoflagellate cysts (mainly Brigantedinium spp., Lejeunecysta spp., Selenopemphix nephroides and Stelladinium reidii) and autotrophic dinoflagellate cysts (mainly Spiniferites ramosus, Lingulodinium machaerophorum and Operculodinium centrocarpum). These assemblage shifts are associated with stronger upwelling during stadials and stronger river influx during interstadials. Increases in productivity caused by enhanced upwelling are coupled to improved preservation and vice versa. More stratified water is indicated by higher abundances of L. machaerophorum and succeeds Heinrich events. The average process length of L. machaerophorum can be used to track changes in salinity, since this shows a similar pattern as the delta 18O(SW) (paired Mg/Ca -delta 18O) reconstruction. During the last glacial, conditions were more saline than during the current interglacial. On a millennial scale, changes in salinity are opposite to open ocean salinities and the hydrological proxies, which can be explained by a modulation of the signal by stratification, isolation of the Basin or advection of freshwater masses. These results highlight both generalities and particularities of the palaeoecological record of this tropical semi-enclosed basin.	[Mertens, Kenneth Neil; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Gonzalez, Catalina] Univ Bremen, Dept Geosci, D-28359 Bremen, Germany; [Delusina, Irina] Univ Calif Davis, Dept Geol, Davis, CA 95616 USA	Ghent University; University of Bremen; University of California System; University of California Davis	Mertens, KN (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8, B-9000 Ghent, Belgium.	Kenneth.Mertens@ugent.be; cataruga@yahoo.com; delusina@geology.ucdavis.edu; stephen.louwye@ugent.be	Arango, Catalina/D-2308-2011; Mertens, Kenneth/AAO-9566-2020; Louwye, Stephen/D-3856-2012; Mertens, Kenneth/C-3386-2015	Louwye, Stephen/0000-0003-4814-4313; Mertens, Kenneth/0000-0003-2005-9483; Gonzalez Arango, Catalina/0000-0003-1709-4405	Ghent University (BOF)	Ghent University (BOF)(Ghent University)	We thank Walter Hale, from the IODP repository in Bremen, for his kind help in sampling Hole 1002C and the IODP in general. Larry Peterson, Joseph Werne, Kristina Dahl, Hui-Ling Lin and Gerald Haug are gratefully thanked for supplying data. Martha McConnell is acknowledged for discussions on delta 18O<INF>SW</INF> variation in the Cariaco Basin. This analysis is part of the PhD programme of the first author, funded by Ghent University (BOF). Fabienne Marret and one anonymous reviewer are kindly thanked for detailed reviews leading to significant improvements to the manuscript.	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J	Tardio, M; Ellegaard, M; Lundholm, N; Sangiorgi, F; Di Giuseppe, G				Tardio, Massimiliano; Ellegaard, Marianne; Lundholm, Nina; Sangiorgi, Francesca; Di Giuseppe, Graziano			A hypocystal archeopyle in a freshwater dinoflagellate from the Peridinium umbonatum group (Dinophyceae) from Lake Nero di Cornisello, South Eastern Alps, Italy	EUROPEAN JOURNAL OF PHYCOLOGY			English	Article						cyst; dinoflagellate; hypocystal archeopyle; lakes; Peridinium inconspicuum; Peridinium umbonatum; South Eastern Alps	SEXUAL REPRODUCTION; CYST FORMATION; PHYLOGENY; STEIN	This study presents the first record of a living dinoflagellate cyst with a hypocystal, antapical archeopyle. It is also the first detailed account of the archeopyle of a living freshwater cyst from the genus Peridinium. The cysts were isolated from sediment traps deployed in Lake Nero di Cornisello, a low-alkalinity high mountain lake of the Adamello mountain range (2233 m above sea level, South Eastern Alps, Italy). The archeopyle is large, clearly hypocystal, polygonal, and slightly peanut-shaped. The species producing this cyst belongs to the Peridinium umbonatum group and is described based on scanning electron microscopy and light microscopy. Partial sequences of SSU rDNA were obtained and compared with previously published sequences from the P. umbonatum group. The taxonomic position of the species is discussed.	[Tardio, Massimiliano] Museo Tridentino Sci Nat, Limnol & Phycol Sect, I-38100 Trento, Italy; [Ellegaard, Marianne; Lundholm, Nina] Univ Copenhagen, Dept Biol, Sect Phycol, DK-1168 Copenhagen, Denmark; [Sangiorgi, Francesca] Univ Utrecht, Palaeobot & Palynol Lab, Inst Environm Biol, Fac Sci, NL-3508 TC Utrecht, Netherlands; [Di Giuseppe, Graziano] Univ Pisa, Dept Biol, I-56126 Pisa, Italy	University of Copenhagen; Utrecht University; University of Pisa	Tardio, M (通讯作者)，Museo Tridentino Sci Nat, Limnol & Phycol Sect, I-38100 Trento, Italy.	tardio@mtsn.tn.it	Lundholm, Nina/AAY-6249-2020; Ellegaard, Marianne/H-6748-2014; Lundholm, Nina/A-4856-2013	Di Giuseppe, Graziano/0000-0002-9999-7650; Ellegaard, Marianne/0000-0002-6032-3376; Sangiorgi, Francesca/0000-0003-4233-6154; Lundholm, Nina/0000-0002-2035-1997	European Commission's; European-funded (FP 6); Danish Agency for Science Technology and Innovation [2111-04-0011]	European Commission's(European Union (EU)European Commission Joint Research Centre); European-funded (FP 6)(European Union (EU)); Danish Agency for Science Technology and Innovation	The work for this paper was carried out towards the PhD thesis of MT at the University of Pisa (Italy; Doctoral Study Programme in Evolutionary Biology -Protistology). We are grateful to the Autonomous Province of Trento for funding the OLOAMBIENT project; we thank the MTSN research fellows, who assisted us during field work, the Department of Phycology of the Biological Institute of the University of Copenhagen research fellows who assisted us in the laboratory studies, Henk Brinkhuis and Andre ' Lotter of the Laboratory of Palaeobotany and Palynology of the Institute of Environmental Biology of the University of Utrecht and SYNTHESYS (DK-TAF) project, financed by the European Commission's framework programmes through a grant from the European-funded (FP 6) Integrated Infrastructure Initiative SYNTHESYS(DK-TAF). NL was funded by grant number 2111-04-0011 from the Danish Agency for Science Technology and Innovation.	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J. Phycol.		2009	44	2					241	250	PII 911034352	10.1080/09670260802588442	http://dx.doi.org/10.1080/09670260802588442			10	Plant Sciences; Marine & Freshwater Biology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Marine & Freshwater Biology	444JG					2025-03-11	WOS:000265976200011
C	Dupont, LM		Kneller, B; Martinsen, OJ; McCaffrey, B		Dupont, Lydie M.			THE CONGO DEEP-SEA FAN AS AN ARCHIVE OF QUATERNARY CHANGE IN AFRICA AND THE EASTERN TROPICAL SOUTH ATLANTIC (A REVIEW)	EXTERNAL CONTROLS ON DEEP-WATER DEPOSITIONAL SYSTEMS	Society for Sedimentary Geology Special Publication		English	Proceedings Paper	SEPM-GSL Joint Research Conference	MAR 27-29, 2006	London, ENGLAND	Soc Sedimentary Geology		Congo deep-sea fan; paleoclimate; African monsoon; Quaternary	WEST EQUATORIAL AFRICA; ODP SITE 1075; SURFACE SEDIMENTS; CLIMATE CHANGES; ORGANIC-MATTER; MARINE; POLLEN; RIVER; CIRCULATION; PLEISTOCENE	A wide variety of proxies has been applied to study the terrestrial input in the Congo deep-sea fan area, the composition of its overlying waters, and the land ocean interactions of the past 1 to 2 million years. These proxies include stable isotopes of foraminifers, total organic carbon (TOC), alkenone-derived sea-surface temperatures (SST), biomarker content and compound-specific stable isotopes, element composition, clay minerals, pollen and spores, dinoflagellate cysts, diatom valves, and opal. Not only the sedimentation in the deep-sea fan but also the productivity of the overlying waters is strongly influenced by the Congo River discharge and its fluctuations depending on the strength of the monsoon. SST and marine productivity are further affected by wind- and river-induced upwelling. A direct relation between SST, precipitation in the Congo Basin, vegetation cover, chemical weathering, and runoff could be established for the past 200 thousand years. Increase of mean global ice volume between 1000 and 500 ka suppressed the precession forcing of trade-wind zonality and monsoonal river runoff, leading to a higher production of nonsilica marine organisms compared to diatoms, and increased eolian transport of terrigenous material.	Univ Bremen, MARUM Ctr Marine Environm Sci, D-28359 Bremen, Germany	University of Bremen	Dupont, LM (通讯作者)，Univ Bremen, MARUM Ctr Marine Environm Sci, Leobenerstr, D-28359 Bremen, Germany.	dupont@uni-bremen.de		Dupont, Lydie/0000-0001-9531-6793				[Anonymous], 2004, J BIOGEOGR; BERGER A, 1991, QUATERNARY SCI REV, V10, P297, DOI 10.1016/0277-3791(91)90033-Q; Berger W, 1998, PROC OCEAN DRILL PRO, V175, P561; Berger W.H., 2002, P OCEAN DRILLING PRO, V175, P1, DOI DOI 10.2973/ODP.PROC.SR.175; BONGOPASSI G, 1988, B SOC GEOL FR, V4, P437; Dupont L, 1999, PALAEOECO A, V26, P61; Dupont LM, 2003, QUATERNARY SCI REV, V22, P157, DOI 10.1016/S0277-3791(02)00032-X; Dupont LM, 2001, GEOLOGY, V29, P195, DOI 10.1130/0091-7613(2001)029<0195:MPECIT>2.0.CO;2; Dupont LM, 2007, VEG HIST ARCHAEOBOT, V16, P87, DOI 10.1007/s00334-006-0080-8; EISMA D, 1978, NETH J SEA RES, V12, P255, DOI 10.1016/0077-7579(78)90030-3; EISMA D, 1978, NETH J SEA RES, V12, P382, DOI 10.1016/0077-7579(78)90041-8; Gingele FX, 1998, PALAEOGEOGR PALAEOCL, V138, P17, DOI 10.1016/S0031-0182(97)00121-1; GIRESSE P, 1982, B SOC GEOL FR, V24, P803; GIRESSE P, 1981, MILIEU MARIN RESSOUR, P13; Holtvoeth J, 2003, GEOCHEM GEOPHY GEOSY, V4, DOI 10.1029/2003GC000590; Holtvoeth J, 2001, GEO-MAR LETT, V21, P23; Jahn B, 2005, GEOL SOC SPEC PUBL, V247, P65, DOI 10.1144/GSL.SP.2005.247.01.04; Jahns S, 1996, VEG HIST ARCHAEOBOT, V5, P207, DOI 10.1007/BF00217498; JANSEN JHF, 1984, NETH J SEA RES, V17, P364, DOI 10.1016/0077-7579(84)90056-5; Kim JH, 2003, GEOPHYS RES LETT, V30, DOI 10.1029/2003GL017557; Kutzbach J.E., 1987, Monsoon, P247; Maley J, 1998, REV PALAEOBOT PALYNO, V99, P157, DOI 10.1016/S0034-6667(97)00047-X; Marret F, 2001, J QUATERNARY SCI, V16, P761, DOI 10.1002/jqs.646; Mayaux P, 2004, J BIOGEOGR, V31, P861, DOI 10.1111/j.1365-2699.2004.01073.x; MEEUWIS JM, 1990, S AFR J MARINE SCI, V9, P261; Mollenhauer G, 2005, PALEOCEANOGRAPHY, V20, DOI 10.1029/2004PA001103; Murray R.M., 1998, Proc. 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J	Sánchez, GE; Sarno, D; Montresor, M; Siano, R; Lange, CB				Sanchez, Gloria E.; Sarno, Diana; Montresor, Marina; Siano, Raffaele; Lange, Carina B.			GERMINATION OF RESTING STAGES OF DIATOMS AND DINOFLAGELLATES IN MARINE SEDIMENTS FROM TWO UPWELLING AREAS OF CHILE	GAYANA BOTANICA			Spanish	Article						Diatoms; dinoflagellates; resting stages; cultures; sediments; Chile	NORTHERN BALTIC SEA; FRAGILARIOID DIATOMS; BACILLARIOPHYCEAE; VARIABILITY; SURVIVAL; PRODUCTIVITY; SPORES; WATERS; OXYGEN; EXPORT	With the aim to assess germination of diatom and dinoflagellates resting spores we Cultured under laboratory conditions surface sediments collected in the Mejillones Bay (23 degrees S) and off Concepcion (36 degrees S), Chile. These sediments were cultured in the laboratory with a 12:12 h L/D cycle, light intensity of 140 mu mol m(2) s(-1), at room temperature, and with a salinity of 35.4 units. The main diatom species in the sediments were Skeletonema japonicum and Chaetoceros spores. Dinoflagellate cysts were represented by the genera Diplopsalis, Scrippsiella, and Woloszynskia and the species Protoperidinium avellanum and P. leonis. After 20 days of culturing, germination and growth was recorded for S. japonicum and several of the Chaetoceros species, although their abundance was low. The diatoms with abundant growth were Stauroneis legleri, Pseudostaurosira trainorii, Pseudostaurosira sp. 1, Pseudostaurosira sp. 2, and Navicula pseudoreinhardtii. The dinoflagellate Woloszynskia sp. also germinated and grew abundantly in the culture. This study includes a brief description of the cultured species and some aspects of their ecology. In addition, we discuss the possible causes for low levels of germination in planktonic diatoms, finding low dissolved oxygen concentrations in the bottom waters to be one of the main factors that presumably affected the survival of resting spores in the sediment.	[Sanchez, Gloria E.] Univ Concepcion, Dept Bot, Programa Doctorado Ciencias Biol Menc Bot, Concepcion, Chile; [Sanchez, Gloria E.; Lange, Carina B.] Univ Concepcion, Ctr Invest Oceanog Pacifico Sur Oriental FONDAP C, Concepcion, Chile; [Sarno, Diana; Montresor, Marina; Siano, Raffaele] Stn Zool Anton Dohrn, I-80121 Naples, Italy; [Lange, Carina B.] Univ Concepcion, Dept Oceanog, Concepcion, Chile	Universidad de Concepcion; Universidad de Concepcion; Stazione Zoologica Anton Dohrn; Universidad de Concepcion	Sánchez, GE (通讯作者)，Univ Concepcion, Dept Bot, Programa Doctorado Ciencias Biol Menc Bot, Casilla 160-C, Concepcion, Chile.	glsanchez@udec.cl	Lange, Carina/AHC-2015-2022	Montresor, Marina/0000-0002-2475-1787				Amato A, 2005, J PHYCOL, V41, P542, DOI 10.1111/j.1529-8817.2005.00080.x; Anderson DM., 1995, IOC MAN GUIDES, V33, P229; Anil AC, 2007, J EXP MAR BIOL ECOL, V343, P37, DOI 10.1016/j.jembe.2006.11.006; [Anonymous], 1979, GAYANA BOT; [Anonymous], 1968, GAYANA BOT; [Anonymous], 1987, Invest. 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J	Kouli, K; Triantaphyllou, M; Pavlopoulos, K; Tsourou, T; Karkanas, P; Dermitzakis, MD				Kouli, Katerina; Triantaphyllou, Maria; Pavlopoulos, Kosmas; Tsourou, Theodora; Karkanas, Panagiotis; Dermitzakis, Michael D.			Palynological investigation of Holocene palaeoenvironmental changes in the coastal plain of Marathon (Attica, Greece)	GEOBIOS			English	Article						Pollen analysis; Vegetation history; Palaeoecology; Holocene; Greece	SEA; EVOLUTION; RECORD	The identification of Middle-Late Holocene palaeoenvironmental conditions of the Marathon coastal plain gained great interest in the last decades due to its high environmental and archaeological importance. Palynological analysis of samples from two boreholes and two trenches along a transect in the marshy area of the Marathon coastal plain, enabled the tracing of the vegetation and the main environmental changes for the last similar to 6000 cal BP. Pollen data suggest a human disturbed environment with Pinus, Quercus, Juniperus and Ericaceae, while a general trend towards Mediterranean vegetation patterns is observed during the last similar to 3000 cal BP. Pollen grains from aquatic and hydrophilous plants, dinoflagellate cysts, algal remains and other palynomorphs were used in order to determine the local depositional environment and its evolution through time.. (C) 2008 Elsevier Masson SAS. All rights reserved.	[Kouli, Katerina; Triantaphyllou, Maria; Tsourou, Theodora; Dermitzakis, Michael D.] Univ Athens, Dept Hist Geol Palaeomol, Panepistimiopolis 15784, Greece; [Pavlopoulos, Kosmas] Harokopio Univ, Fac Geog, Athens 17671, Greece; [Karkanas, Panagiotis] Ephoreia Palaeoanthropol Speleol, Athens 11636, Greece	National & Kapodistrian University of Athens; Harokopio University Athens	Kouli, K (通讯作者)，Univ Athens, Dept Hist Geol Palaeomol, Panepistimiopolis 15784, Greece.	akouli@geol.uoa.gr	Pavlopoulos, Kosmas/X-8566-2019; Tsourou, Theodora/AEX-5082-2022; Kouli, Katerina/M-8243-2013; Triantaphyllou, Maria/AAL-7877-2021; Karkanas, Panagiotis/F-7762-2011	Kouli, Katerina/0000-0003-1656-1091; Triantaphyllou, Maria/0000-0001-7508-7508; Karkanas, Panagiotis/0000-0002-7156-671X; PAVLOPOULOS, KOSMAS/0000-0003-4503-9120; Tsourou, Theodora/0000-0001-9427-2661				ALLEN H, 1990, MANS ROLE IN THE SHAPING OF THE EASTERN MEDITERRANEAN LANDSCAPE, P173; Atherden M., 1993, HOLOCENE, V3, P351, DOI [10.1177/095968369300300407, DOI 10.1177/095968369300300407]; BAETEMAN C, 1985, J COASTAL RES, V1, P173; BOTTEMA S, 1990, MANS ROLE IN THE SHAPING OF THE EASTERN MEDITERRANEAN LANDSCAPE, P231; Bottema S., 1990, Franchthi Paralia: The Sediments, Stratigraphy, and Offshore Investigations (Franchthi 6), P117; Bottema S., 1974, PhD thesis; Carrión JS, 1999, REV PALAEOBOT PALYNO, V106, P209, DOI 10.1016/S0034-6667(99)00009-3; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; FOUACHE E, 1999, B CORRESPONDANCE HEL, V35; Grimm E.C., 1992, Program and Abstracts, 8th International Palynological Congress, Aix-en- Provence [France], September 6-12, 1992, P56; Head MJ, 2005, QUATERN INT, V130, P3, DOI 10.1016/j.quaint.2004.04.027; Jahns S, 2003, VEG HIST ARCHAEOBOT, V12, P127, DOI 10.1007/s00334-003-0013-8; Jahns S., 1993, Vegetation History and Archaeobotany, V2, P187, DOI DOI 10.1007/BF00198161; KAMBOUROGLOU E, 1989, THESIS U ATHENS; Kontopoulos N, 2003, QUATERN INT, V111, P75, DOI 10.1016/S1040-6182(03)00016-8; KRAFT JC, 1977, SCIENCE, V195, P941, DOI 10.1126/science.195.4282.941; KRAFT JC, 1975, GEOL SOC AM BULL, V86, P1191, DOI 10.1130/0016-7606(1975)86<1191:LHPOTC>2.0.CO;2; KRAFT JC, 1972, 9 U DEL; Lambeck K, 1996, ANTIQUITY, V70, P588, DOI 10.1017/S0003598X00083733; LAMBECK K, 1995, GEOPHYSICAL J INT, V115, P960; LOZIOS S, 1993, THESIS U ATHENS ATHE; MAROUKIAN H, 1993, GEOLOGICA BALCANICA, V23, P67; Moore P.D., 1994, Pollen Analysis; Mudie PJ, 2001, MAR MICROPALEONTOL, V43, P155, DOI 10.1016/S0377-8398(01)00006-8; PANTELIDOUGOFAS M, 1997, ARCHAEOLOGICAL SOC A, V167; PANTELIDOUGOFAS M, 2005, ARCHAEOLOGICAL SOC A, V235; PANTELIDOUGOFAS M, 1995, ARCHAEOLOGICAL SOC A, V153; PANTELIDOUGOFAS M, 1991, ARCHAEOLOGICAL SOC A, V119; Pavlopoulos K, 2006, J COASTAL RES, V22, P424, DOI 10.2112/03-0145.1; PAVLOPOULOS K, 2003, MEDITERRANEAN WORLD, P453; PETRAKOS B, 1995, ARCHAEOLOGICAL SOC A, V167; PETRUCCI F, 1983, Acta Naturalia de l'Ateneo Parmense, V19, P63; REILLE M, 1992, LAB BOT HIST PALYN S, V1; Scott D.B., 1979, Rivista Italiana di Paleontologia e Stratigrafia, V85, P243; Triantaphyllou MV, 2003, RIV ITAL PALEONTOL S, V109, P539, DOI 10.13130/2039-4942/5522; TURNER J, 1975, REV PALAEOBOT PALYNO, V20, P171, DOI 10.1016/0034-6667(75)90020-2; VAN G, 1983, REV PALAEOBOT PALYNO, V38, P269; van Geel B, 2003, J ARCHAEOL SCI, V30, P873, DOI 10.1016/S0305-4403(02)00265-0; VANANDEL TH, 1984, QUATERNARY RES, V22, P31, DOI 10.1016/0033-5894(84)90004-8; VANGEEL B, 1983, REV PALAEOBOT PALYNO, V38, P269, DOI 10.1016/0034-6667(83)90026-X; VANGEEL B, 1989, REV PALAEOBOT PALYNO, V60, P25, DOI 10.1016/0034-6667(89)90072-9; VANGEEL B, 1981, REV PALAEOBOT PALYNO, V31, P367; WALL D, 1973, Micropaleontology (New York), V19, P18, DOI 10.2307/1484962	43	25	26	0	3	ELSEVIER FRANCE-EDITIONS SCIENTIFIQUES MEDICALES ELSEVIER	ISSY-LES-MOULINEAUX	65 RUE CAMILLE DESMOULINS, CS50083, 92442 ISSY-LES-MOULINEAUX, FRANCE	0016-6995	1777-5728		GEOBIOS-LYON	Geobios	JAN-FEB	2009	42	1					43	51		10.1016/j.geobios.2008.07.004	http://dx.doi.org/10.1016/j.geobios.2008.07.004			9	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	414YK					2025-03-11	WOS:000263900900003
J	De Schutter, P				De Schutter, Pieter			THE PRESENCE OF <i>MEGACHASMA</i> (CHONDRICHTHYES: LAMNIFORMES) IN THE NEOGENE OF BELGIUM, FIRST OCCURRENCE IN EUROPE.	GEOLOGICA BELGICA			English	Article						Megachasmidae; Miocene; Pliocene; Kattendijk Formation; Deurganckdok; North Sea Basin	DINOFLAGELLATE CYST BIOSTRATIGRAPHY; NORTHERN BELGIUM; PLIOCENE; SHARKS; CORRIDOR; ORIGIN	Fossil teeth of the genus Megachasma Taylor, Compagno & Struhsaker, 1983 are recorded for the first time in Europe. Isolated teeth have been recovered from the transgressive layer at the base of the Belgian Pliocene, extending the known paleogeographic range of this genus. These teeth are compared with fossil specimens from Greece, Chile, USA and extant specimens. The Belgian teeth seem to fit well in the gap between the early Miocene teeth from California and those of the extant taxon Megachasma pelagios Taylor, Compagno & Struhsaker, 1983; while the megamouth teeth found in Late Miocene to Early Pliocene sediments worldwide (Chile, North Carolina, Florida, and Greece) appear to be giant versions of modern teeth. Juvenile teeth of modern Megachasma pelagios are illustrated for the first time, showing a distinct ontogenetic variation in the roots and crown surface.			De Schutter, P (通讯作者)，Averbeekstr 23 Bus 1-02, B-1745 Opwijk, Belgium.	pieter.deschutter@skynet.be		De Schutter, Pieter/0000-0002-0477-7824				Adnet S., 2007, Historical Biology, V19, P279, DOI 10.1080/08912960701194461; [Anonymous], B SOC BELGE GEOLOGIE; [Anonymous], 2000, PROFIL; Benson RH, 1991, PALEOCEANOGRAPHY, V6, P165, DOI 10.1029/90PA00756; Bleeker P., 1871, PRELIMINAIRES MEMOIR; Bosselaers Mark, 2004, Geologica Belgica, V7, P27; CAPPETA H, 1991, Palaeontographica Abteilung A Palaeozoologie-Stratigraphie, V218, P49; CAPPETTA H, 2006, FOSSILIUM CATALOGU 1, V142; Cappetta H., 1987, Chondrichthyes II--Mesozoic and Cenozoic Elasmobranchii; Cappetta Henri, 2006, Rivista Piemontese di Storia Naturale, V27, P33; Chandler RE, 2006, PALAEONTOL ELECTRON, V9; Compagno L., 2001, FAO Species Catalogue for Fishery Purposes, V2. Bullhead, mackerel and carpet sharks; Compagno L.J.V., 1984, SHARKS WORLD ANNOTAT, V4, P1; Compagno L.J. V., 1990, NOAA TECH REP NMFS, V90, P357; De Ceuster J., 1987, MEDEDELINGEN WERKGRO, V24, P231; De Meuter F., 1976, Bulletin Belgische Vereniging voor Geologie, V85, P133; De Schepper S, 2004, J PALEONTOL, V78, P625, DOI 10.1666/0022-3360(2004)078<0625:NDCAIS>2.0.CO;2; DEHEINZELIN J, 1955, B SOC BELG GEOL, V64, P463; Esteban Mateu, 1996, Concepts in Sedimentology and Paleontology, V5, P55; GUNNERUS JE, 1765, DET TRONDHIEMSKE SEL, V3, P33; Herman J., 1993, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Biologie, V63, P185; Herman J., 1974, Bulletin Soc belge Geol Palaeont Hydrol, V83, P15; HERMAN J, 1979, Annales de la Societe Geologique de Belgique, V102, P357; HERMAN J, 2007, MEMOIR GEOLOGICAL SU, V54; HSU KJ, 1973, NATURE, V242, P240, DOI 10.1038/242240a0; KEUPP H, 2002, MIOZAN FOSSILIEN NW, V19, P34; Krijgsman W, 1999, NATURE, V400, P652, DOI 10.1038/23231; Laga Pieter, 2001, Geologica Belgica, V4, P135; Landini W., 1977, Palaeontographia Italica, V70, P92; Ledoux J.-C., 1972, Doc. 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Lyon Notes Mem, V52, P133; Leriche M, 1908, CR HEBD ACAD SCI, V146, P875; LERICHE MAURICE, 1926, MEM MUS ROY HIST NAT BELGIQUE, V32, P365; Loget N, 2006, SEDIMENT GEOL, V188, P341, DOI 10.1016/j.sedgeo.2006.03.012; Louwye S, 2000, GEOL MAG, V137, P381, DOI 10.1017/S0016756800004258; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Louwye S, 2002, GEOL J, V37, P55, DOI 10.1002/gj.900; Louwye S., 2007, GEOL J, V43, P75; Mane Ramon, 1996, Batalleria, V6, P19; Marquet Robert, 2004, Bulletin de l'Institut Royal des Sciences Naturelles de Belgique Sciences de la Terre, V74, P205; Marsili S, 2007, NEUES JAHRB GEOL P-A, V244, P247, DOI 10.1127/0077-7749/2007/0244-0247; Marsili S, 2007, GEODIVERSITAS, V29, P229; Marsili S, 2007, ANN PALEONTOL, V93, P27, DOI 10.1016/j.annpal.2007.01.001; Martin AP, 2002, MOL PHYLOGENET EVOL, V23, P205, DOI 10.1016/S1055-7903(02)00001-5; Martín JM, 2001, TERRA NOVA, V13, P418, DOI 10.1046/j.1365-3121.2001.00376.x; NOLF D, 1988, KONINKLIJK BELGISCH; PARCO BA, 2007, CEBU DAILY NEWS 0530; Phillips F.J., 1976, P SOC EC PALEONTOLOG, P137; Purdy RW, 2001, SM C PALEOB, V90, P71; REINECKE T, 2006, PALAEOVERTEBRATA MON, V34; REUTER M, 2007, INT J EARTH SCI, DOI DOI 10.1007/S00532-007-0269-9; Rogl F., 1998, ANN NATURHIST MUS A, V99, P279, DOI DOI 10.2307/41702129; 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]; SHIMADA K, 2006, J PALEONTOLOGY, V63; Shimada K, 2007, J VERTEBR PALEONTOL, V27, P512, DOI 10.1671/0272-4634(2007)27[512:MOFMSL]2.0.CO;2; Shirai Shigeru, 1996, P9, DOI 10.1016/B978-012670950-6/50003-5; Siverson M, 1996, PALAEONTOLOGY, V39, P813; TAYLOR L R, 1983, Proceedings of the California Academy of Sciences, V43, P87; Van Vliet-Lanoe Brigitte, 2002, Geodiversitas, V24, P511; Walsh S., 2006, Historical Biology, V18, P115, DOI [10.1080/08912960600640796, DOI 10.1080/08912960600640796]; WALSH S, 2001, BAHIA INGLESA FORMAT; Walsh SA, 2005, ACTA PALAEONTOL POL, V50, P595; Ward David J., 2001, Central Mediterranean Naturalist, V3, P131; White WT, 2004, RAFFLES B ZOOL, V52, P603; Yabumoto Yoshitaka, 1997, P63	64	11	11	0	8	GEOLOGICA BELGICA	BRUSSELS	JENNER STREET 13, BRUSSELS, BELGIUM	1374-8505	2034-1954		GEOL BELG	Geol. Belg.		2009	12	3-4					179	203						25	Geology	Science Citation Index Expanded (SCI-EXPANDED)	Geology	477OS					2025-03-11	WOS:000268529000005
J	De Schepper, S; Head, MJ; Louwye, S				De Schepper, Stijn; Head, Martin J.; Louwye, Stephen			Pliocene dinoflagellate cyst stratigraphy, palaeoecology and sequence stratigraphy of the Tunnel-Canal Dock, Belgium	GEOLOGICAL MAGAZINE			English	Article						dinoflagellate cyst; palynology; Pliocene; North Sea; sequence stratigraphy	NORTH-SEA BASIN; MIOCENE; PRESERVATION; ASSEMBLAGES; POLLEN; RECONSTRUCTION; PLEISTOCENE; CLIMATE; ONSET; CRAG	Dinoflagellate cysts and sequence stratigraphy are used to date accurately the Tunnel-Canal Dock section, which contains the most complete record of marine Pliocene deposits in the Antwerp harbour area. The Zanclean Kattendijk Formation was deposited between 5.0 and 4.4 Ma during warm-temperate conditions on a shelf influenced by open-marine waters. The overlying Lillo Formation is divided into four members. The lowest is the Luchtbal Sands Member, estimated to have been deposited between 3.71 and 3.21 Ma, under cooler conditions but with an open-water influence. The Oorderen Sands, Kruisschans Sands and Merksem Sands members of the Lillo Formation are considered a single depositional sequence, and biostratigraphically dated between 3.71 and c. 2.6 Ma, with the Oorderen Sands Member no younger than 2.72-2.74 Ma. Warm-temperate conditions had returned, but a cooling event is noted within the Oorderen Sands Member. Shoaling of the depositional environment is also evidenced, with the transgressive Oorderen Sands Member passing upwards into (near-)coastal high-stand deposits of the Kruisschans Sands and Merksem Sands members, as accommodation space decreased. Applying sequence stratigraphy to our section implies that the Kattendijk/Lillo Formation boundary corresponds to the sequence boundary (SB) Za2 (4.04 Ma), the Luchtbal/Oorderen sands boundary to SB Pia1 (3.21 Ma), and the top of the Merksem Sands to SB Pia2 (2.76 Ma). Finally, the Belgian deposits are compared with marine Pliocene deposits of eastern England.	[De Schepper, Stijn] Univ Cambridge, Dept Geog, Cambridge CB2 3EN, England; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Louwye, Stephen] Univ Ghent, Palaeontol Res Unit, B-9000 Ghent, Belgium	University of Cambridge; Brock University; Ghent University	De Schepper, S (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330 440, D-28334 Bremen, Germany.	sdeschepper@uni-bremen.de	De Schepper, Stijn/A-2836-2011; Louwye, Stephen/D-3856-2012	De Schepper, Stijn/0000-0002-6934-0914; Louwye, Stephen/0000-0003-4814-4313				ANDREW R, 1977, NEW PHYTOL, V78, P709, DOI 10.1111/j.1469-8137.1977.tb02175.x; BALSON P, 1999, GEOLOGICAL CONSERVAT, V15, P235; Bartoli G, 2005, EARTH PLANET SC LETT, V237, P33, DOI 10.1016/j.epsl.2005.06.020; Boessenkool KP, 2001, GLOBAL PLANET CHANGE, V30, P33, DOI 10.1016/S0921-8181(01)00075-3; Cameron T., 1992, UK OFFSHORE REGIONAL; COSTA LI, 1979, INITIAL REPORTS DEEP, V48, P513; de Heinzelin de Braucourt J, 1952, B SOC BELGE GEOLOGIE, V61, P106; 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Mag.	JAN	2009	146	1					92	112		10.1017/S0016756808005438	http://dx.doi.org/10.1017/S0016756808005438			21	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	396QL					2025-03-11	WOS:000262606100006
J	Kremp, A; Lindholm, T; Dressler, N; Erler, K; Gerdts, G; Eirtovaara, S; Leskinen, E				Kremp, Anke; Lindholm, Tore; Dressler, Nicole; Erler, Katrin; Gerdts, Gunnar; Eirtovaara, Sanna; Leskinen, Elina			Bloom forming <i>Alexandrium ostenfeldii</i> (Dinophyceae) in shallow waters of the Aland Archipelago, Northern Baltic Sea	HARMFUL ALGAE			English	Article						Alexandrium ostenfeldii; Baltic Sea; Bioluminescent blooms; LSU and ITS rDNA; Morphology; Salinity tolerance; Toxicity	MINUTUM DINOPHYCEAE; SPECIES BOUNDARIES; INORGANIC NITROGEN; TOXIN CONTENT; TAMARENSE; SEQUENCES; GROWTH; BIOGEOGRAPHY; SALINITY; TOXICITY	In the past years, late summer blooms of the bioluminescent dinoflagellate Alexandrium ostenfeldii have become a recurrent phenomenon in coastal waters of the central and Northern Baltic Sea. This paper reports exceptionally high cell concentrations (10(5) to 10(6) cells L-1) of the species found during bioluminescent blooms in 2003 and 2004 in a shallow embayment of the Aland archipelago at the SW coast of Finland. Clonal cultures were established for morphological, molecular, toxicological and ecophysiological investigations to characterize the Finnish populations and compare them to other global A. ostenfeldii isolates. The Finnish isolates exhibited typical morphological features of A. ostenfeldii such as large size, a prominent ventral pore and an orthogonally bent first apical plate. However, unambiguous differentiation from closely related Alexandrium peruvianum was difficult due to considerable variation of sulcal anterior plate shapes. The Finnish strains were genetically distinct from other isolates of the species, but phylogenetic analyses revealed a close relationship to isolates from southern England and an A. peruvianum morphotype from the Spanish Mediterranean. Together these isolates formed a distinct clade which was separated from a clade containing other Northern European, North American and New Zealand populations. Toxin analyses confirmed the presence of the PSP toxins GTX2, GTX3 and STX in both Finnish isolates with GTX3 being the dominant toxin. Total relative PSP toxin contents were moderate, ranging from approximately 6 to 15 fmol cell(-1) at local salinities of 5 and 10 psu, respectively. Spirolides were not detected. Salinity tolerance experiments showed that the Finnish isolates were well adapted to grow at the low salinities of the Baltic Sea. With a salinity range of approximately 6 to 2025 psu, Baltic populations are physiologically distinct from their marine relatives. Vigorous production of different cyst types in the cultures suggest that cysts may play a crucial role in the survival and retainment of A. ostenfeldii populations in the Baltic Sea. (C) 2008 Elsevier B.V. All rights reserved.	[Kremp, Anke] Univ Helsinki, Tvarminne Zool Stn, Hango 10900, Finland; [Lindholm, Tore] Abo Akad Univ, Dept Biol, SF-20500 Turku, Finland; [Dressler, Nicole; Erler, Katrin] Univ Jena, Inst Nutr, Dept Food Chem, D-07743 Jena, Germany; [Gerdts, Gunnar] Alfred Wegener Inst Polar & Marine Res, Biol Anstalt Helgoland, D-27483 Helgoland, Germany; [Eirtovaara, Sanna; Leskinen, Elina] Univ Helsinki, Dept Biol & Environm Sci, FIN-00014 Helsinki, Finland	University of Helsinki; Abo Akademi University; Friedrich Schiller University of Jena; Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; University of Helsinki	Kremp, A (通讯作者)，Finnish Environm Inst, POB 140, Helsinki 00251, Finland.	anke.kremp@environment.fi	Kremp, Anke/I-8139-2013; Gerdts, Gunnar/R-7000-2016	Gerdts, Gunnar/0000-0003-0872-3927	European Commission [GOCE-CT-2005-003875]; Academy of Finland [111336]; Walter and Andree de Nottbeck Foundation; Academy of Finland (AKA) [111336] Funding Source: Academy of Finland (AKA)	European Commission(European Union (EU)European Commission Joint Research Centre); Academy of Finland(Research Council of Finland); Walter and Andree de Nottbeck Foundation; Academy of Finland (AKA)(Research Council of Finland)	We thank Johan Franzen for bringing the bioluminescent blooms at Foglo to our attention. The authors are grateful to Linda Percy and Isabel Bravo for providing cultures of their English and Spanish isolates of A. ostenfeldii and A. peruvianum. Deana Erdner and Donald Anderson allowed us to use an unpublished sequence of their Gulf of Maine isolate. Pekka Kotilainen kindly provided the drawings of the study area. The critical comments of S. Fraga and the assistance of two anonymous reviewers are gratefully acknowledged. 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C	Fahnenstiel, G; Hong, Y; Millie, D; Doblin, M; Johengen, T; Reid, D		Jones, J		Fahnenstiel, G.; Hong, Y.; Millie, D.; Doblin, M.; Johengen, T.; Reid, D.			Marine dinoflagellate cysts in the ballast tank sediments of ships entering the Laurentian Great Lakes	INTERNATIONAL ASSOCIATION OF THEORETICAL AND APPLIED LIMNOLOGY, VOL 30, PT. 7, PROCEEDINGS	International Association of Theoretical and Applied Limnology Proceedings		English	Proceedings Paper	30th Congress of the International-Association-of-Theoretical-and-Applied-Limnology	AUG 12-18, 2007	Montreal, CANADA	Int Assoc Theoret & Appl Limnol		harmful algae; NOBOB; non-indigenous species	WATER; TRANSPORT		[Fahnenstiel, G.] NOAA, GLERL, Lake Michigan Field Stn, 1431 Beach St, Muskegon, MI 49441 USA; [Millie, D.] Univ S Florida, Florida Inst Oceanog, St Petersburg, FL 33701 USA; [Doblin, M.] Univ Technol Sydney, Sydney, NSW 2007, Australia; [Johengen, T.] Univ Michigan, Sch Nat Res & Env, Cooperat Inst Limnol Ecosyst Res, Ann Arbor, MI 48109 USA; [Reid, D.] NOAA, Great Lakes Environm Res Lab, Ann Arbor, MI 48105 USA	National Oceanic Atmospheric Admin (NOAA) - USA; State University System of Florida; University of South Florida; University of Technology Sydney; University of Michigan System; University of Michigan; National Oceanic Atmospheric Admin (NOAA) - USA	Fahnenstiel, G (通讯作者)，NOAA, GLERL, Lake Michigan Field Stn, 1431 Beach St, Muskegon, MI 49441 USA.		Fahnenstiel, Gary/ABD-6133-2020; Doblin, Martina/E-8719-2013		Great Lake Protection Fund; National Oceanic and Atmospheric Administration; U.S. Environmental Protection Agency; U.S. Coast Guard	Great Lake Protection Fund; National Oceanic and Atmospheric Administration(National Oceanic Atmospheric Admin (NOAA) - USA); U.S. Environmental Protection Agency(United States Environmental Protection Agency); U.S. Coast Guard	Thank you to: members of the Great Lakes NOBOB team and ship's captains and crew for their efforts in collecting ballast water samples; Rich Stone for his technical assistance associated with sample collection and analysis; and Cathy Darnell for assistance with manuscript preparation and editing. This work was conducted under the multi-institutional Great Lakes NOBOB Project funded by the Great Lake Protection Fund, the National Oceanic and Atmospheric Administration, the U.S. Environmental Protection Agency, and the U.S. Coast Guard. GLERL publication No. 1504.	BALDWIN RP, 1987, NEW ZEAL J MAR FRESH, V21, P243; Bolch CJS, 1997, PHYCOLOGIA, V36, P472, DOI 10.2216/i0031-8884-36-6-472.1; DALE B, 1983, DINOFLAGELLATE RESTI; DOZIER BJ, 1975, VERHANDLUNG INT VERE, V19, P1524; Duggan IC, 2005, CAN J FISH AQUAT SCI, V62, P2463, DOI 10.1139/F05-160; FUKUYO Y, 1982, CYSTS NAKED DINOFLAG; GUILLARD RR, 1972, J PHYCOL, V8, P10, DOI 10.1111/j.1529-8817.1972.tb03995.x; Hallegraeff GM, 1998, MAR ECOL PROG SER, V168, P297, DOI 10.3354/meps168297; HALLEGRAEFF GM, 1992, J PLANKTON RES, V14, P1067, DOI 10.1093/plankt/14.8.1067; HALLEGRAEFF GM, 1991, MAR POLLUT BULL, V22, P27, DOI 10.1016/0025-326X(91)90441-T; Hamer JP, 2000, MAR POLLUT BULL, V40, P731, DOI 10.1016/S0025-326X(99)00198-8; Hamer JP, 2001, PHYCOLOGIA, V40, P246, DOI 10.2216/i0031-8884-40-3-246.1; Holeck KT, 2004, BIOSCIENCE, V54, P919, DOI 10.1641/0006-3568(2004)054[0919:BTWBIT]2.0.CO;2; MAHONEY JB, 1979, J EXP MAR BIOL ECOL, V37, P213, DOI 10.1016/0022-0981(79)90061-3; MILLS EL, 1993, J GREAT LAKES RES, V19, P1, DOI 10.1016/S0380-1330(93)71197-1; Ricciardi A, 2006, DIVERS DISTRIB, V12, P425, DOI 10.1111/j.1366-9516.2006.00262.x; SICKOGOAD L, 1986, J PHYCOL, V22, P22, DOI 10.1111/j.1529-8817.1986.tb02510.x; Sullivan Barbara E., 2001, Phycological Research, V49, P207, DOI 10.1046/j.1440-1835.2001.00241.x	18	10	12	0	3	E SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG	STUTTGART	JOHANNESTRASSE 3, W-7000 STUTTGART, GERMANY	0368-0770		978-3-510-54078-5	INT VER THEOR ANGEW	Int. Assoc. Theor. Appl. Limnol. Proc.		2009	30		7				1035	+						3	Limnology	Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology	BKR97					2025-03-11	WOS:000269050500012
J	Medeanic, S; Torgan, LC; Clerot, LCP; dos Santos, CB				Medeanic, Svetlana; Torgan, Lezilda Carvalho; Pinheiro Clerot, Luiz Carlos; dos Santos, Cristiane Bahi			Holocene Marine Transgression in the Coastal Plain of Rio Grande do Sul, Brazil: Palynomorph and Diatom Evidence	JOURNAL OF COASTAL RESEARCH			English	Article						Palaeoenvironmental reconstructions; southern Brazil	SOUTHERN PATAGONIA; LEVEL CHANGES; SEDIMENTS; ZYGNEMATACEAE; EASTERN; FOSSIL	Based on sedimentology, geochronology, palynology, and diatom analyses from core silt sediments in Cassino Beach (32 degrees 11'06 '' S and 52 degrees 09'45 '' W), southern Brazil, the Holocene marine transgressive stage was established. The absolute age of one sample is about 4940 +/- 80 years BP. The palynomorphs (pollen and spores of vascular plants, zygospores and colonies of Chlorophyceae, cysts of dinoflagellates and acritarchs, fungal spores, and microforaminifera), silicoflagellates, and diatoms indicate the presence of an inlet bay in the southern part of the coastal plain during the marine transgression. The changes in the taxonomic composition, abundance, and frequency of palynomorphs and diatoms from the samples corresponding to transgression show an oscillatory character of the sea level. The posterior marine regression resulted in sand deposition and dune formation. The results demonstrate the importance of palynomorph and diatom application for the palaeoenvironmental reconstructions in coastal plains.	[Medeanic, Svetlana; Pinheiro Clerot, Luiz Carlos] Univ Fed Rio Grande do Sul, Inst Geociencias, BR-91509900 Porto Alegre, RS, Brazil; [Torgan, Lezilda Carvalho; dos Santos, Cristiane Bahi] Fundacao Zoobot Rio Grande Sul, Museo Ciencias Nat, BR-90690000 Porto Alegre, RS, Brazil	Universidade Federal do Rio Grande do Sul	Medeanic, S (通讯作者)，Univ Fed Rio Grande do Sul, Inst Geociencias, Ave Bento Goncalves 9500, BR-91509900 Porto Alegre, RS, Brazil.	svetlana.medeanic@ufrgs.br	Torgan, Lezilda/AAV-6154-2021; Torgan, Lezilda Carvalho/D-7811-2017	Torgan, Lezilda Carvalho/0000-0001-6787-9441	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) [300005/2007-5, 302926/2004-6]	Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq)(Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPQ))	We thank the Conselho Nacional de Desenvolvimento Cientifico e Tecnologico (CNPq) for grants 300005/2007-5 and 302926/2004-6. We are grateful to Dr. S.R. Dillenburg, who provided the <SUP>14</SUP>C dating, and to Haywood Dail Laughinghouse IV for reviewing the English in the manuscript. We are indebted to two anonymous reviewers for their criticism, suggestions, and corrections which improved this manuscript.	ABREU VS, 1987, C ASS BRAS EST QU 1, P177; Angulo RJ, 1999, MAR GEOL, V159, P323, DOI 10.1016/S0025-3227(98)00204-7; Angulo RJ, 1997, MAR GEOL, V140, P141, DOI 10.1016/S0025-3227(97)00015-7; [Anonymous], IHERINGIA B; [Anonymous], 1996, Diatomeas del Golfo de California; [Anonymous], 2007, Paleopalynology; [Anonymous], SEA LEVEL CHANGES; CLEROT L. C. 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C., 1999, Iheringia, Serie Botanica, V52, P89; TORGAN LC, 2004, J COASTAL RES, V39, P1149; Torgan Lezilda Carvalho, 2001, Iheringia Serie Botanica, V56, P147; Torgan Lezilda Carvalho, 2002, VVolume 15, P459; TRAVERSE A, 1967, Review of Palaeobotany and Palynology, V3, P243, DOI 10.1016/0034-6667(67)90057-7; VANGEEL B, 1976, REV PALAEOBOT PALYNO, V22, P337, DOI 10.1016/0034-6667(76)90029-4; VANGEEL B, 1978, REV PALAEOBOT PALYNO, V25, P377, DOI 10.1016/0034-6667(78)90021-0; VANGEEL B, 1981, REV PALAEOBOT PALYNO, V31, P367; VIEIRA JP, 1988, PLANICIE COSTEIRA RI; Villwock J.A., 1986, QUATERNARY S AM ANTA, P79, DOI [10.1201/9781003079316-5, DOI 10.1201/9781003079316-5]; ZONG Y, 1977, DIATOM RES, V12, P125	53	21	22	0	5	COASTAL EDUCATION & RESEARCH FOUNDATION	COCONUT CREEK	5130 NW 54TH STREET, COCONUT CREEK, FL 33073 USA	0749-0208	1551-5036		J COASTAL RES	J. Coast. Res.	JAN	2009	25	1					224	233		10.2112/07-0935.1	http://dx.doi.org/10.2112/07-0935.1			10	Environmental Sciences; Geography, Physical; Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Environmental Sciences & Ecology; Physical Geography; Geology	397YS					2025-03-11	WOS:000262698900019
J	Gribble, KE; Anderson, DM; Coats, DW				Gribble, Kristin E.; Anderson, Donald M.; Coats, D. Wayne			Sexual and Asexual Processes in <i>Protoperidinium steidingerae</i> Balech (Dinophyceae), with Observations on Life-History Stages of <i>Protoperidinium depressum</i> (Bailey) Balech (Dinophyceae)	JOURNAL OF EUKARYOTIC MICROBIOLOGY			English	Article						Eleutheroschisis; gamete; heterotrophic dinoflagellate; hypnozygote; nuclear cyclosis; planomeiocyte; planozygote	HETEROTROPHIC DINOFLAGELLATE; GRAZING RATES; GROWTH; REPRODUCTION; PHYLOGENY; CYCLE; RDNA	A suite of morphological, histological, and molecular techniques was used to reveal for the first time division, sexuality, mandatory dormancy period of hypnozygotes, and identity of life-history stages of any Protoperidinium spp. In both Protoperidinium steidingerae and Protoperidinium depressum, asexual division occurred by eleutheroschisis within a temporary cyst, yielding two daughter cells. Daughter cells were initially round and one-half to two-thirds the size of parent cells then rapidly increased in size, forming horns before separating. Gamete production and fusion was constitutive in clonal and non-clonal cultures, indicating that both species may be homothallic. Gametes were isogamous, approximately half the size and lacking the pink pigmentation of the vegetative cells, and were never observed to feed. Gamete fusion resulted in a planozygote with two longitudinal flagella. Planozygotes of P. steidingerae formed hypnozygotes. The fate of planozygotes of P. depressum is unknown. Hypnozygotes of P. steidingerae had a mandatory dormancy period of ca. 70 days. Germination resulted in planomeiocytes with two longitudinal flagella. Nuclear cyclosis occurred in the planozygotes of P. depressum, but in the planomeiocytes of P. steidingerae. The plate tabulation and gross morphology of gametes of P. steidingerae and P. depressum differed markedly from those of vegetative cells. Thus, misidentification of morphologically distinct life-history stages and incomplete examination of thecal plate morphology in field specimens has likely led to taxonomic confusion of Protoperidinium spp. in previous studies.	[Gribble, Kristin E.; Anderson, Donald M.] Woods Hole Oceanog Inst, Dept Biol, Woods Hole, MA 02543 USA; [Coats, D. Wayne] Smithsonian Environm Res Ctr, Edgewater, MD 21037 USA	Woods Hole Oceanographic Institution; Smithsonian Institution; Smithsonian Environmental Research Center	Gribble, KE (通讯作者)，Marine Biol Lab, 7 MBL St,Lillie 319, Woods Hole, MA 02543 USA.	kgribble@mbl.edu		Gribble, Kristin/0000-0002-8781-9523; Coats, D Wayne/0000-0002-0636-189X	The Comer Foundation; the Woods Hole Oceanographic Institution Biology Department Education Fund; the Carroll Wilson Award from the MIT Entrepreneurship Society	The Comer Foundation; the Woods Hole Oceanographic Institution Biology Department Education Fund; the Carroll Wilson Award from the MIT Entrepreneurship Society	We thank the Marine Institute of Ireland and Captain Kenneth Houtler of the Woods Hole Oceanographic Institution for sample collection. Thank you to Malte ElbrAchter for assistance with identification of P. steidingerae. Thank you to Matthew Parrow for helpful suggestions for creating chambers for single cell culture using 96-well plates. Thank you to Rebecca Gast and Sonya Dyhrman for microscope and camera use, and to Jane Doucette for assistance with life history diagrams. The Comer Foundation, the Woods Hole Oceanographic Institution Biology Department Education Fund, and the Carroll Wilson Award from the MIT Entrepreneurship Society provided funding for this work.	ANDERSON DM, 1984, J PHYCOL, V20, P418, DOI 10.1111/j.0022-3646.1984.00418.x; [Anonymous], 1981, Studies on the family Peridiniidae. 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L., 1975, CULTURE MARINE INVER, P29, DOI DOI 10.1007/978-1-4615-8714-9_3; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JACOBSON DM, 1993, J PLANKTON RES, V15, P723, DOI 10.1093/plankt/15.7.723; Jeong Hae Jin, 1996, Journal of the Korean Society of Oceanography, V31, P144; JEONG HJ, 1994, MAR ECOL PROG SER, V106, P173, DOI 10.3354/meps106173; Jeong HJ., 1995, INTERACTIONS MICROZO; Kokinos John P., 1995, Palynology, V19, P143; Menden-Deuer S, 2005, AQUAT MICROB ECOL, V41, P145, DOI 10.3354/ame041145; Montagnes D.J.J., 1993, Handbook of Methods in Aquatic Microbial Ecology, P229; Naustvoll LJ, 2000, PHYCOLOGIA, V39, P187, DOI 10.2216/i0031-8884-39-3-187.1; Parrow Matthew, 2002, Harmful Algae, V1, P5, DOI 10.1016/S1568-9883(02)00009-4; Parrow MW, 2004, J PHYCOL, V40, P664, DOI 10.1111/j.1529-8817.2004.03202.x; Pfiester L.A., 1987, BIOL DINOFLAGELLATES, P611; SCHOLIN CA, 1994, J PHYCOL, V30, P999, DOI 10.1111/j.0022-3646.1994.00999.x; Stosch H.A., 1964, Helgolander Wissenschaftliche Meeresuntersuchungen, V10, P140; THOMPSON JD, 1994, NUCLEIC ACIDS RES, V22, P4673, DOI 10.1093/nar/22.22.4673; Von Stosch HA., 1973, Br Phycol J, V8, P105; VONSTOSCH HA, 1972, SOC BOT FR MEMOIRES, P201; WALL D, 1968, Micropaleontology (New York), V14, P265, DOI 10.2307/1484690	33	24	26	1	12	WILEY-BLACKWELL PUBLISHING, INC	MALDEN	COMMERCE PLACE, 350 MAIN ST, MALDEN 02148, MA USA	1066-5234			J EUKARYOT MICROBIOL	J. Eukaryot. Microbiol.	JAN-FEB	2009	56	1					88	103		10.1111/j.1550-7408.2008.00378.x	http://dx.doi.org/10.1111/j.1550-7408.2008.00378.x			16	Microbiology	Science Citation Index Expanded (SCI-EXPANDED)	Microbiology	415QE	19335779				2025-03-11	WOS:000263948600012
J	Bresnan, E; Hay, S; Hughes, SL; Fraser, S; Rasmussen, J; Webster, L; Slesser, G; Dunn, J; Heath, MR				Bresnan, E.; Hay, S.; Hughes, S. L.; Fraser, S.; Rasmussen, J.; Webster, L.; Slesser, G.; Dunn, J.; Heath, M. R.			Seasonal and interannual variation in the phytoplankton community in the north east of Scotland	JOURNAL OF SEA RESEARCH			English	Article; Proceedings Paper	Workshop on Time Series Data Relevant to Eutrophication and Ecological Quality Indicators	SEP 11-14, 2006	Tisvildeleje, DENMARK			Time series; Phytoplankton; Diatoms; Dinoflagellates; Spring bloom; Chaetoceros; Skeletonema	NE ATLANTIC-OCEAN; NARRAGANSETT BAY; CLIMATE-CHANGE; RESTING STAGES; SEA WATER; LONG-TERM; VARIABILITY; PATTERNS; DIATOM; ECOSYSTEMS	In 1997 a monitoring site was established 5 km offshore from Stonehaven (56 degrees 57.8' N, 02 degrees 06.2'W) in the north east of Scotland to examine the effects of physical and chemical parameters on the plankton community in this region. Analysis of the first 10 years of data show that, in common with trends in the NE Atlantic, there was an increasing trend in temperature and salinity at the site. Nutrients were typical of unimpacted waters in this region, with nitrate being the main limiting nutrient over the summer months. The phytoplankton community composition showed strong seasonality with low phytoplankton biomass in the winter, diatoms dominating in spring and early summer and dinoflagellates appearing in mid to late summer. Two different regimes were recognised: from 1997-2000 and 2005-2006, where the chlorophyll concentration peaked in the early part of the year (mid month values ranging from 2.6-4.1 mu l(-1)) and a period from 2001-2004 where chlorophyll mid month values did not exceed 2.5 mu g l(-1). A decreasing trend in the abundance of dinoflagellates, including members of the genus Ceratium, was observed from 2003-2006. In addition, from 1997-2001, the diatom genus Chaetoceros was the dominant species in the spring bloom, but post 2001 Skeletonema spp. became more abundant. The study highlights the variability that exists in time series data and emphasises the need for long term time series to determine the long term trends and impacts of the phytoplankton community on the marine ecosystem. Crown Copyright (C) 2008 Published by Elsevier B.V. All rights reserved.	[Bresnan, E.; Hay, S.; Hughes, S. L.; Fraser, S.; Rasmussen, J.; Webster, L.; Slesser, G.; Dunn, J.; Heath, M. R.] Fisheries Res Serv Marine Lab, Aberdeen AB11 9DB, Scotland		Bresnan, E (通讯作者)，Fisheries Res Serv Marine Lab, 375 Victoria Rd, Aberdeen AB11 9DB, Scotland.	e.bresnan@marlab.ac.uk	Heath, Michael/D-5765-2013; Hughes, Sarah/C-1160-2008; Rasmussen, Jens/P-2956-2019; Rasmussen, Jens/N-2460-2014	Rasmussen, Jens/0000-0002-3139-6365; Heath, Michael/0000-0001-6602-3107				ARAR EJ, 1992, 4450 USEPA; Beaugrand G, 2003, FISH OCEANOGR, V12, P270, DOI 10.1046/j.1365-2419.2003.00248.x; Beaugrand G, 2003, NATURE, V426, P661, DOI 10.1038/nature02164; BENDSCHNEIDER K, 1952, J MAR RES, V11, P87; BERTHELOT MP, 1859, REPERTOIRE CHIMIE AP, P284; Bresnan E., 2003, 1403 FISH RES SERV; BRESNAN E, P 12 HAB C IN PRESS; Clarke K., 2001, Change in Marine Communities, V2; CUSHING DH, 1989, J PLANKTON RES, V11, P1, DOI 10.1093/plankt/11.1.1; Devlin M, 2007, MAR POLLUT BULL, V55, P91, DOI 10.1016/j.marpolbul.2006.09.018; DICKSON RR, 1992, ICES MAR SC, V195, P232; *DIR AGR FISH SCOT, 1969, DIR FISH RES REP 196; *DIR AGR FISH SCOT, 1970, DIR FISH RES REP 196; *DIR AGR FISH SCOT, 1971, DIR FISH RES REP 197; Edwards M, 2006, LIMNOL OCEANOGR, V51, P820, DOI 10.4319/lo.2006.51.2.0820; Edwards M, 2004, NATURE, V430, P881, DOI 10.1038/nature02808; Edwards M, 2002, MAR ECOL PROG SER, V239, P1, DOI 10.3354/meps239001; Edwards M, 2001, ICES J MAR SCI, V58, P39, DOI 10.1006/jmsc.2000.0987; Eilertsen HC, 2000, S AFR J MARINE SCI, V22, P323, DOI 10.2989/025776100784125717; *FISH RES SERV, 2003, FISH RES SERV INT RE; *FISH RES SERV, 2005, FISH RES SERV INT RE; *FISH RES SERV, 2007, FISH RES SERV INT RE; FRASER S, 2006, 0306 FISH RES SERV; FRASER S, 2004, 1204 FISH RES SERV; Heath MR, 2005, ICES J MAR SCI, V62, P847, DOI 10.1016/j.icesjms.2005.01.023; Joint I, 1997, J PLANKTON RES, V19, P937, DOI 10.1093/plankt/19.7.937; Karentz D, 1998, J PLANKTON RES, V20, P145, DOI 10.1093/plankt/20.1.145; KORELOFF F, 1971, 1971C ICES CM, V43; Leterme SC, 2006, MAR ECOL PROG SER, V312, P57, DOI 10.3354/meps312057; Lewis Jane, 1995, P175; Litchman E, 2007, ECOL LETT, V10, P1170, DOI 10.1111/j.1461-0248.2007.01117.x; McQuatters-Gollop A, 2007, MAR ECOL PROG SER, V339, P301, DOI 10.3354/meps339301; McQuoid MR, 2005, MAR ECOL PROG SER, V289, P151, DOI 10.3354/meps289151; McQuoid MR, 1996, J PHYCOL, V32, P889, DOI 10.1111/j.0022-3646.1996.00889.x; MURPHY J, 1958, J MAR BIOL ASSOC UK, V37, P9, DOI 10.1017/S0025315400014776; Reid PC, 2001, FISH RES, V50, P163, DOI 10.1016/S0165-7836(00)00249-6; Richardson AJ, 2004, SCIENCE, V305, P1609, DOI 10.1126/science.1100958; *SCOTT HOM DEP, 1955, FISH RES REP YE END; *SCOTT HOM DEP, 1958, FISH RES REP YE END; *SCOTT HOM DEP, 1957, FISH RES REP YE END; Smayda TJ, 1998, ICES J MAR SCI, V55, P562, DOI 10.1006/jmsc.1998.0385; SPARKS TH, 2006, 167 SCOTT NAT HER CO; Throndsen J., 1978, Preservation and storage, P69, DOI DOI 10.1111/J.0022-3646.1975.00142.X; Tilstone GH, 2000, MAR ECOL PROG SER, V205, P23, DOI 10.3354/meps205023; Tunin-Ley A, 2007, J PHYCOL, V43, P1149, DOI 10.1111/j.1529-8817.2007.00417.x; WEBSTER L, 2007, 1907 FISH RES SERV I; WOOD ED, 1967, J MAR BIOL ASSOC UK, V47, P23, DOI 10.1017/S002531540003352X	47	31	36	2	34	ELSEVIER SCIENCE BV	AMSTERDAM	PO BOX 211, 1000 AE AMSTERDAM, NETHERLANDS	1385-1101			J SEA RES	J. Sea Res.	JAN	2009	61	1-2					17	25		10.1016/j.seares.2008.05.007	http://dx.doi.org/10.1016/j.seares.2008.05.007			9	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology; Oceanography	405BL					2025-03-11	WOS:000263197000003
J	Dale, B				Dale, Barrie			Eutrophication signals in the sedimentary record of dinoflagellate cysts in coastal waters	JOURNAL OF SEA RESEARCH			English	Article; Proceedings Paper	Workshop on Time Series Data Relevant to Eutrophication and Ecological Quality Indicators	SEP 11-14, 2006	Tisvildeleje, DENMARK			Eutrophication; North Sea; Skagerrak; Dinoflagellates; Dinoflagellate cysts; Phytoplankton; Eutrophication signals; NAO; Climate change; Pollution; Fishery collapse; Fjord sediments	SUMMER ALGAL BLOOMS; TOKYO-BAY; GULLMAR FJORD; YOKOHAMA-PORT; WEST-COAST; INDICATORS; PHYTOPLANKTON; ASSEMBLAGES; MASSACHUSETTS; PRESERVATION	A brief review is presented of the current status of eutrophication signals from the sedimentary records of dinoflagellate cysts in coastal waters, particularly of NW Europe. There is a dearth of the multi-decadal time series data from plankton needed to document eutrophication. and the cysts may provide an alternative source of information. Two different eutrophication signals have been described so far from cyst records: 1) from the Oslofjord, comprising a marked increase in total cyst concentrations (interpreted as probably reflecting increased phytoplankton productivity). with Lingulodinium polyedrum cysts accounting for most of the increase (interpreted as a species particularly benefiting from added nutrients from cultural eutrophication in late summer when nutrients otherwise may be limiting); and 2) the heterotroph signal, from several other Norwegian fjords and Tokyo Bay, Japan, involving both cases of increased cyst concentrations and others with no particular increase, but with a marked proportional increase in cysts of heterotrophic species (interpreted as reflecting increased diatoms and possibly other prey for the heterotrophic dinoflagellates and/or more unfavourable conditions for autotrophs, e.g. from shading). These signals should be used critically, and there is a particular need to distinguish between eutrophication signals and climate signals that may be co-occurring at a given time. Work by various authors has generally supported the concept of these cyst-based signals since they were first published, including both further records from cored sediments from other parts of the world and studies relating cyst distributions in surface sediments to gradients of pollution and nutrients from sewage discharge. Recent, unpublished work by Dale and Saetre, linked cyst signals in cored sediments to the timing of collapse of local fisheries at different times within the past fifty years in four fjord systems along the Norwegian Skagerrak coast (supporting earlier postulations by fisheries biologists that eutrophication was a possible cause). They also link these local eutrophication events to regional variation in the NAO, thought to have caused pulses of nutrient loading within the Skagerrak from increased transport of relatively nutrient rich North Sea water into the system. This may represent a major breakthrough in understanding the relationship between climatic variation and coastal eutrophication. Some concluding remarks are added in an attempt to show how these cyst signals: 1) suggest interesting comparisons with the ecological classification of bloom dinoflagellates by Smayda and Reynolds [Smayda, T.J., Reynolds, C.S., 2003. Strategies of marine dinoflagellate survival and some rules of assembly. J. Sea Res. 49, 95-106.]: and 2) have helped to identify important questions regarding the extent to which climate variation influences coastal eutrophication. Addressing these questions represents an urgent challenge to marine science. (C) 2008 Elsevier B.V. All rights reserved.	Univ Oslo, Dept Geosci, N-0316 Oslo, Norway	University of Oslo	Dale, B (通讯作者)，Univ Oslo, Dept Geosci, PB 1047 Blindern, N-0316 Oslo, Norway.	barrie.dale@geo.uio.no						Abrantes F, 2005, QUATERNARY SCI REV, V24, P2477, DOI 10.1016/j.quascirev.2004.04.009; Andersen JH, 2004, MAR POLLUT BULL, V49, P283, DOI 10.1016/j.marpolbul.2004.04.014; Anderson DM, 2002, ESTUARIES, V25, P704, DOI 10.1007/BF02804901; Bennion H, 1996, ENVIRON SCI TECHNOL, V30, P2004, DOI 10.1021/es9508030; Boesch DF, 2001, J ENVIRON QUAL, V30, P303, DOI 10.2134/jeq2001.302303x; Carstensen J, 2005, ESTUAR COAST SHELF S, V62, P595, DOI 10.1016/j.ecss.2004.09.026; Carstensen J, 2007, LIMNOL OCEANOGR, V52, P370, DOI 10.4319/lo.2007.52.1.0370; Clarke A, 2003, MAR POLLUT BULL, V46, P1615, DOI 10.1016/S0025-326X(03)00375-8; Cloern JE, 2001, MAR ECOL PROG SER, V210, P223, DOI 10.3354/meps210223; CONLEY DJ, 1993, MAR ECOL PROG SER, V101, P179, DOI 10.3354/meps101179; COOPER SR, 1995, ECOL APPL, V5, P703, DOI 10.2307/1941979; Dale Amy L., 2002, P259; 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., 1983, P69; Dale B, 2001, SCI TOTAL ENVIRON, V264, P235, DOI 10.1016/S0048-9697(00)00719-1; Dale B, 2001, SCI MAR, V65, P257, DOI 10.3989/scimar.2001.65s2257; Dale B, 1999, ESTUAR COAST SHELF S, V48, P371, DOI 10.1006/ecss.1999.0427; DALE B, 2000, ENV MICROPALEONTOLOG, P305; DALE B., 1994, CARBON CYCLING GLOBA, P521; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; Filipsson HL, 2005, ESTUAR COAST SHELF S, V63, P551, DOI 10.1016/j.ecss.2005.01.001; Godhe A, 2003, AQUAT MICROB ECOL, V32, P185, DOI 10.3354/ame032185; Gundersen N, 1988, THESIS U OSLO, P1; Harland R, 2006, SCI TOTAL ENVIRON, V355, P204, DOI 10.1016/j.scitotenv.2005.02.030; Harland R, 2004, REV PALAEOBOT PALYNO, V128, P119, DOI 10.1016/S0034-6667(03)00116-7; HURRELL JW, 1995, SCIENCE, V269, P676, DOI 10.1126/science.269.5224.676; JOSEFSON AB, 1990, MAR ECOL PROG SER, V66, P117, DOI 10.3354/meps066117; Kowalewska G, 2005, QUATERN INT, V130, P141, DOI 10.1016/j.quaint.2004.04.037; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Lindahl O, 1998, ICES J MAR SCI, V55, P723, DOI 10.1006/jmsc.1998.0379; MARINO G, 2008, THESIS UTRECHT U NET, P1; Matsuoka K., 1989, P461; Matsuoka K, 2003, J PLANKTON RES, V25, P1461, DOI 10.1093/plankt/fbg111; 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; Morzadec-Kerfourn M. 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Sea Res.	JAN	2009	61	1-2					103	113		10.1016/j.seares.2008.06.007	http://dx.doi.org/10.1016/j.seares.2008.06.007			11	Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED); Conference Proceedings Citation Index - Science (CPCI-S)	Marine & Freshwater Biology; Oceanography	405BL					2025-03-11	WOS:000263197000013
J	Matthiessen, J; Brinkhuis, H; Poulsen, N; Smelror, M				Matthiessen, Jens; Brinkhuis, Henk; Poulsen, Niels; Smelror, Morten			Decahedrella martinheadii Manum 1997-a stratigraphically and paleoenvironmentally useful Miocene acritarch of the high northern latitudes	MICROPALEONTOLOGY			English	Review							DINOFLAGELLATE CYSTS; LOMONOSOV RIDGE; SEA; RECORD; HISTORY; SEDIMENTATION; CIRCULATION; GREENLAND; OCEAN; BASIN	The endemic aquatic acritarch Decahedrella martinheodii is confined to the Atlantic sector of the high northern latitudes in the Miocene and has been previously considered as useful for biostratigraphy and palcoenvironmental interpretations in temperate to cold water environments. Stimulated by its recovery in Neogene sediments from the Lomonosov Ridge (Central Arctic Ocean) during IODP Expedition 302, the stratigraphic and biogeographic distribution has been compiled to revise its age range based on the Astronomically Tuned Neogene Time Scale 2004, and to assess its paleoecologic affinities. The biostratigraphic revision reveals that this species is restricted to the late Middle to Late Miocene. The first appearence is inconsistent at the various sites but was probably in sediments younger than 13 Ma, whereas the last appearance is a relatively well-constrained datum in the Norwegian-Greenland Sea at around 6.2 Ma. Decahedrella martinheadii was particularly abundant and had its widest biogeographic distribution in the northwestern North Atlantic Ocean, the Norwegian-Greenland Sea, the Fram Strait and the Central Arctic Ocean in the Late Miocene suggesting that it was adapted to temperate to cold seasonally ice-covered surface waters. This species evolved during the global cooling after the mid-Miocene thermal optimum, and it became extinct when small-scale glaciations developed in the Northern Hemisphere in the latest Miocene. Moreover, fundamental reorganisations of the circulation system and the water mass characteristics may have affected the distribution of this species.	[Matthiessen, Jens] Alfred Wegener Inst Polar & Marine Res, D-27568 Bremerhaven, Germany; [Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [Poulsen, Niels] Geol Survey Denmark & Greenland, DK-1350 Copenhagen, Denmark; [Smelror, Morten] Geol Survey Norway, NO-7040 Trondheim, Norway	Helmholtz Association; Alfred Wegener Institute, Helmholtz Centre for Polar & Marine Research; Utrecht University; Geological Survey Of Denmark & Greenland; Geological Survey of Norway	Matthiessen, J (通讯作者)，Alfred Wegener Inst Polar & Marine Res, Am Alten Hafen 26, D-27568 Bremerhaven, Germany.	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J	Sangiorgi, F; Brinkhuis, H; Damassa, SP				Sangiorgi, Francesca; Brinkhuis, Henk; Damassa, Sarah Pierce			<i>Arcticacysta</i>: A new organic-walled dinoflagellate cyst genus from the early Miocene? of the central Arctic Ocean	MICROPALEONTOLOGY			English	Article							BIOSTRATIGRAPHY; CALIBRATION	The Cenozoic sedimentary record of the central Arctic Ocean recovered during the Arctic Coring Expedition (ACEX) Integrated Ocean Drilling Program (IODP) Expedition 302 contains a new dinoflagellate cyst genus, Arcticacvsta, assignable to the Peridiniales. Two different species are here formally described, Arcticacysta backmanii and A. moram. ae gen. et sp. nov. Both species have a combination archeopyle, formed by the loss of several plates. In A. backmanii the archeopyle involves three apical (2'-4') and three intercalary (la-3a) plates. In A. moraniae the archeopyle is formed by the loss of four apical (1'-4') and three intercalary ( la-3a) plates. The species differ in size and in the wall structure. A. backmanii has a microreticulate wall and is relatively large, whereas A. moraniae is smaller and with spinose wall. Their lowest Occurrence in the ACEX core lies at the base Of Subunit 115 (core M0002A 46X, 113-114 cm, 198.70 meters composite depth, mcd). Morphologically closely related taxa, potentially representing other species of Arcticacysta, have been previOLISly recovered from the late Olieocene and early Miocene sediments of the Norwegian-Greenland Seas.	[Sangiorgi, Francesca; Brinkhuis, Henk] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands	Utrecht University	Sangiorgi, F (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	f.sangiorgi@uu.nl	Brinkhuis, Henk/B-4223-2009	Sangiorgi, Francesca/0000-0003-4233-6154; Brinkhuis, Henk/0000-0003-0253-6610				[Anonymous], 2006, Proceedings IODP, P302, DOI [10.2204/iodp.proc.302.2006, DOI 10.2204/IODP.PROC.302.103.2006, 10.2204/iodp.proc.302.103.2006, DOI 10.2204/IODP.PROC.302.2006]; Backman J, 2004, QUATERNARY SCI REV, V23, P1435, DOI 10.1016/j.quascirev.2003.12.005; BACKMAN J, P IODP, V302; Backman J, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001476; BRIDEAUX WW, 1977, GEOLOGICAL SURVEY CA, V281; Bujak J.P., 1994, Journal of Micropalaeontology, V13, P119; CANDE SC, 1995, J GEOPHYS RES-SOL EA, V100, P6093, DOI 10.1029/94JB03098; Clark DL, 1988, PALEOCEANOGRAPHY, V3, P539, DOI 10.1029/PA003i005p00539; DAMASSA SP, 1990, REV PALAEOBOT PALYNO, V65, P331, DOI 10.1016/0034-6667(90)90083-U; DAMASSA SP, 1998, PALYNOLOGY, V22, P238; DELLAGNESE DJ, 1994, J PALEONTOL, V68, P31, DOI 10.1017/S0022336000025580; Dybkjaer K, 2007, J MICROPALAEONTOL, V26, P1, DOI 10.1144/jm.26.1.1; Eldrett JS, 2004, MAR GEOL, V204, P91, DOI 10.1016/S0025-3227(03)00357-8; Fensome R.A., 1993, Micropaleontology Press Special Paper; Firth John V., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P203; Firth JV, 1998, MAR MICROPALEONTOL, V34, P1, DOI 10.1016/S0377-8398(97)00046-7; 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; Heilmann-Clausen C., 1989, Geol. Jahrb., V111, P1; Kaminski MA, 2005, MICROPALEONTOLOGY, V51, P373, DOI 10.2113/gsmicropal.51.5.373; KAMINSKI MA, 2007, IODP UK NEWSL, V32, P18; 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; Moran K, 2006, NATURE, V441, P601, DOI 10.1038/nature04800; Munsterman DK, 2004, NETH J GEOSCI, V83, P267, DOI 10.1017/S0016774600020369; Poulsen Niels E., 1996, Proceedings of the Ocean Drilling Program Scientific Results, V151, P255; Sangiorgi F, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2007PA001477; Sluijs A, 2008, PALEOCEANOGRAPHY, V23, DOI 10.1029/2008PA001615; Stein R, 2006, GEOPHYS RES LETT, V33, DOI 10.1029/2006GL026776; Van Simaeys S, 2005, REV PALAEOBOT PALYNO, V134, P105, DOI 10.1016/j.revpalbo.2004.12.003; Williams Graham L., 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P99	31	4	4	0	4	MICRO PRESS	FLUSHING	6530 KISSENA BLVD, FLUSHING, NY 11367 USA	0026-2803	1937-2795		MICROPALEONTOLOGY	Micropaleontology		2009	55	2-3					249	258						10	Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Paleontology	453ZM					2025-03-11	WOS:000266651400008
J	Suto, I; Jordan, RW; Watanabe, M				Suto, Itsuki; Jordan, Richard W.; Watanabe, Mahito			Taxonomy of middle Eocene diatom resting spores and their allied taxa from the central Arctic Basin	MICROPALEONTOLOGY			English	Review							MARINE PLANKTONIC DIATOM; GENUS CHAETOCEROS BACILLARIOPHYCEAE; GENERA DICLADIA EHRENBERG; NORWEGIAN SEA; STRATIGRAPHIC SIGNIFICANCE; SYNDENDRIUM EHRENBERG; NORTH PACIFIC; PSEUDOCURVISETUS; BIOSTRATIGRAPHY; OLIGOCENE	In the late summer of 2004, Integrated Ocean Drilling Program (IODP) Expedition 302, also called the Arctic Coring Expedition (ACEX), successfully drilled the First deep boreholes on the Lomonosov Ridge in the central Arctic Ocean. The well preserved fossil diatoms used here are from biosiliceous Unit 2 in Holes 2A and 4A of middle Eocene age. In the lower part of Unit 2, resting spores Occurred abundantly with other fossil diatoms. 25 diatom resting spore taxa and five allied vegetative cell taxa are described in this study of ACEX samples. Moreover I I diatom taxa which did not occur in these sediments are also described for comparison with the Eocene Arctic resting spores. Their biostratigraphic ranges are also indicated. 10 of the resting spore species which occur in the ACEX samples had already appeared during the late Cretaceous while the rest of them appeared in Eocene. 21 of 25 (84%) resting spore taxa became extinct during the middle Eocene to early Oligocene. Most resting spore taxa described in this study do not belong to Chaetoceros resting spores because they lack a single ring of puncta on the hypovalve mantle that characterizes the resting spores of Chaetoceros and became extinct before Oligocene, therefore it is clear that Chaetoceros did not flourish in the middle Eocene in the Arctic Ocean. Other diatoin genera that produced resting spores such as Pierotheca and Pseudopyxilla, might have prospered before the Eocene/Oligoene boundary. although their vegetative cells are unknown so far. Since some Chaetoceros resting spore taxa are reported in this study, most coastal regions experienced regular seasonal environmental change, which benefitted genera such as Pterotheca, Pseudopyxilla and Odontotropis, but also there might have been some patchy coastal upwelling regions with nutrient depletion and sporadic supplies where Chaetoceros may have survived. The abundant dinoflagellate cysts preserved in middle Eocene ACEX cores provide evidence of stable conditions before the Eocene/Oligocene boundary. The resting spore ecology of most resting spore taxa before the Eocene may have been similar to that of dinoflagellate cysts rather than that of Chaetoceros resting spores after the Oligocene.	[Suto, Itsuki] Nagoya Univ, Grad Sch Environm Studies, Dept Earth & Planetary Sci, Nagoya, Aichi 4648601, Japan; [Jordan, Richard W.] Yamagata Univ, Fac Sci, Dept Earth & Environm Sci, Yamagata 9908560, Japan; [Watanabe, Mahito] Natl Inst Adv Ind Sci & Technol, Geol Survey Japan, Inst Geol & Geoinformat, Tsukuba, Ibaraki 3058567, Japan	Nagoya University; Yamagata University; National Institute of Advanced Industrial Science & Technology (AIST)	Suto, I (通讯作者)，Nagoya Univ, Grad Sch Environm Studies, Dept Earth & Planetary Sci, Nagoya, Aichi 4648601, Japan.	suto.itsuki@a.mbox.nagoya-ac.jp; sh081@kdw.kj.yamagata-u.ac.jp; mht.watanabe@aist.go.jp	Watanabe, Mahito/N-2494-2018	Jordan, Richard/0000-0002-8997-7349				ABBOTT W H, 1979, Micropaleontology (New York), V25, P225, DOI 10.2307/1485301; [Anonymous], J QUEKETT MICROSCOPI; [Anonymous], FDN PALEONTOLOGY GUI; [Anonymous], PUBLICATIONS SADO MU; [Anonymous], ANTARCTIC RES SERIES; [Anonymous], 1975, PALAEONTOGRAPHICA AB; [Anonymous], 1884, DENKSCHRIFTEN KAISER; [Anonymous], J PALEONTOLOGICAL SO; [Anonymous], P OCEAN DRILLING PRO; BACKMAN J, 2005, P INTEGRATED OCEAN D, V302; Backman J, 2005, SCI DRILL, V1, P12, DOI 10.5194/sd-1-12-2005; BALDAUF JG, 1987, U S GEOLOGICAL SURVE, V1765; BALDAUF JG, 1985, INIT REPTS DSDP, V81, P439; Barron J. 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J	Ibrahim, MIA; Dilcher, D; Kholeif, S				Ibrahim, Mohamed I. A.; Dilcher, David; Kholeif, Suzan			Palynomorph succession and paleoenvironment in the Upper Cretaceous Abu Gharadig Oil Field, Northwestern Desert, Egypt	MICROPALEONTOLOGY			English	Article							WESTERN-DESERT; PALYNOLOGY; SEDIMENTS; POLLEN; SUDAN; PALYNOSTRATIGRAPHY; STRATIGRAPHY; PLATEAU; BASIN; WELL	An Upper Cretaceous spore-pollen and dinoflagellate zonation in two deep wells (AG-5 and AG-13) of the Abu Gharadig oil field, Northwestern Desert, Egypt is presented. Six pollen and spores zones equivalent to five dinoflagellate and phytoplankton zones are defined for the Cenomanian-Santonian Bahariya and Abu Roash formations. One new pollen species. Integritetradites foveolatus sp. nov., is described from the middle to late Cenomanian strata. The Cenomanian-Turonian boundary is defined for the first time in Egypt using stable carbon and oxygen isotopes (delta C-13 and delta O-18), where a positive carbon excursion is detected in organic rich shale of the basal Abu Roash "F" Member. During the Cenomanian, Egypt was part of the mid-Cretaceous "African-South American" Province (ASA), characterized by dominance of Classopollis, Araucariacites, eleter-bearing and Afropollis pollen assemblage in an arid to semi-arid warm climate. The marine/terrestrial palynomorph ratio increased upward from the Cenomanian to Santonian related to a global sea level rise. The Cenomanian siliciclastics of the Bahariya Formation and the basal Abu Roash G and F members were deposited in a shallow marine, inner shelf environment. The Middle part of the Abu Roash Formation (E member: Turonian) is a shallow water, middle shelf deposit, while the upper part of the Abu Roash Formation (A, B, C and D members: Coniacian-Santonian) are open marine, outer shelf deposits.	[Ibrahim, Mohamed I. A.] Univ Alexandria, Dept Environm Sci, Fac Sci, Alexandria 21511, Egypt; [Dilcher, David] Univ Florida, Florida Museum Nat Hist, Gainesville, FL 32611 USA; [Kholeif, Suzan] Natl Inst Oceanog & Fisheries, Alexandria, Egypt	Egyptian Knowledge Bank (EKB); Alexandria University; State University System of Florida; University of Florida; Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF)	Ibrahim, MIA (通讯作者)，Univ Alexandria, Dept Environm Sci, Fac Sci, Alexandria 21511, Egypt.	mibrah@gmail.com			Fulbright Binational Commission; Florida Museum of Natural History, University of Florida	Fulbright Binational Commission; Florida Museum of Natural History, University of Florida(University of Florida)	We are indebted to the authorities of the Egyptian General Petroleum Corporation EGPC, for providing the samples and well logs for this study. 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J	Solignac, S; Grosfjeld, K; Giraudeau, J; de Vernal, A				Solignac, Sandrine; Grosfjeld, Kari; Giraudeau, Jacques; de Vernal, Anne			Distribution of recent dinocyst assemblages in the western Barents Sea	NORWEGIAN JOURNAL OF GEOLOGY			English	Article							DINOFLAGELLATE CYST ASSEMBLAGES; NORTHERN NORTH-ATLANTIC; SURFACE CONDITIONS; HIGH-LATITUDES; POLAR FRONT; SEDIMENTS; ICE; PHYTOPLANKTON; INDICATORS; COLOR	Dinoflagellate cyst (dinocyst) assemblages were analyzed in 43 surface sediment samples from the Barents Sea. They can be divided into five major assemblage types, the distribution of which can clearly be linked to the overlying water masses. Notably, a very clear distinction between sites influenced by Atlantic water and Arctic water, respectively, is seen in the change in dominance from O. centrocarpum s.l. to I. minutum and is strongly related to sea-surface temperature. More subtle hydrographical features are also recorded in the assemblages, as can be seen from the spatially coherent distribution of the Atlantic assemblages, which allows discrimination between the Norwegian Coastal Current zone, the Norwegian Atlantic Current zone and two regions of modified Norwegian Atlantic Current waters. Here sea-surface temperature does not seem to be the primary parameter controlling the distribution of the assemblages. Multivariate analyses suggest that the assemblages are associated with the stratification and productivity annual cycles. Cysts of P. dalei seem to favour stratified environments, while O. centrocarpum s.l. might be more adapted to unstable conditions. Cysts of P dalei are also associated with early spring stratification and productivity, whereas other species such as S. ramosus are related to late spring/summer productivity and stratification.	[Solignac, Sandrine] Univ Aarhus, Dept Earth Sci, DK-8000 Aarhus C, Denmark; [Solignac, Sandrine; de Vernal, Anne] Univ Quebec, Geotop, Montreal, PQ H3C 3P8, Canada; [Grosfjeld, Kari] Geol Survey Norway, N-7021 Trondheim, Norway; [Giraudeau, Jacques] Univ Bordeaux 1, CNRS, UMR 5805, F-33405 Talence, France	Aarhus University; University of Quebec; University of Quebec Montreal; Geological Survey of Norway; Universite de Bordeaux; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU)	Solignac, S (通讯作者)，Univ Aarhus, Dept Earth Sci, Hoegh Guldbergs Gade 2, DK-8000 Aarhus C, Denmark.	sandrine.solignac@geo.au.dk	Giraudeau, Jacques/AAF-5764-2019; de Vernal, Anne/D-5602-2013	de Vernal, Anne/0000-0001-5656-724X; Solignac, Sandrine/0000-0003-3373-6922; Giraudeau, Jacques/0000-0002-5069-4667	Natural Sciences and Engineering Research Council of Canada (NSERC); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT); Research Council of Norway; French Ministry of Education, Research and Technology	Natural Sciences and Engineering Research Council of Canada (NSERC)(Natural Sciences and Engineering Research Council of Canada (NSERC)); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Research Council of Norway(Research Council of Norway); French Ministry of Education, Research and Technology	The authors would like to thank Jochen Knies, Norwegian Geological Survey (NGU, Trondheim, Norway) for access to the surface samples, and Frederique Eynaud and Fabienne Marret for their helpful comments on the manuscript. This study was supported by the Natural Sciences and Engineering Research Council of Canada (NSERC), the Fonds quebecois de la recherche sur la nature et les technologies (FQRNT) and the Aurora mobility exchange programme, funded by the Research Council of Norway and the French Ministry of Education, Research and Technology	[Anonymous], 2006, NGU REPORT; [Anonymous], 2001, WORLD OC ATL; Antoine D, 1996, GLOBAL BIOGEOCHEM CY, V10, P57, DOI 10.1029/95GB02832; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; de Vernal A., 1999, CAHIERS GEOTOP, V3; Divine DV, 2006, J GEOPHYS RES-OCEANS, V111, DOI 10.1029/2004JC002851; Engelsen O, 2002, J MARINE SYST, V35, P79, DOI 10.1016/S0924-7963(02)00077-5; GAWARKIEWICZ G, 1995, J GEOPHYS RES-OCEANS, V100, P4509, DOI 10.1029/94JC02427; Gloersen P., 1992, ARCTIC ANTARCTIC SEA; HARLAND R, 1982, Palynology, V6, P9; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Kögeler J, 1999, INT J REMOTE SENS, V20, P1303, DOI 10.1080/014311699212740; LOENG H, 1991, POLAR RES, V10, P5, DOI 10.1111/j.1751-8369.1991.tb00630.x; Marret F, 2004, REV PALAEOBOT PALYNO, V128, P35, DOI 10.1016/S0034-6667(03)00111-8; *NSIDC, 2003, ARCT SO OC SEA IC CO; Olsen A, 2003, SARSIA, V88, P379, DOI 10.1080/00364820310003145; Radi T, 2008, MAR MICROPALEONTOL, V68, P84, DOI 10.1016/j.marmicro.2008.01.012; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; Schlitzer R., 2008, OCEAN DATA VIEW; Solignac S, 2008, MAR MICROPALEONTOL, V68, P115, DOI 10.1016/j.marmicro.2008.01.001; Strass VH, 1996, POLAR BIOL, V16, P409; Ter Braak C.J.F, 1998, CANOCO RELEASE 4 REF; TERBRAAK CJF, 1986, ECOLOGY, V67, P1167; Vinje T, 2001, J CLIMATE, V14, P255, DOI 10.1175/1520-0442(2001)014<0255:AATOSI>2.0.CO;2; Vink A., 2003, S ATLANTIC LATE QUAT, P101; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650	29	22	22	0	4	GEOLOGICAL SOC NORWAY	TRONDHEIM	C/O NGU, 7491 TRONDHEIM, NORWAY		1502-5322		NORW J GEOL	Norw. J. Geol.		2009	89	1-2					109	119						11	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	590UQ					2025-03-11	WOS:000277254200012
J	Grosfjeld, K; Harland, R; Howe, J				Grosfjeld, Kari; Harland, Rex; Howe, John			Dinoflagellate cyst assemblages inshore and offshore Svalbard reflecting their modern hydrography and climate	NORWEGIAN JOURNAL OF GEOLOGY			English	Article							WEST SPITSBERGEN CURRENT; SEA-SURFACE CONDITIONS; NORTHERN NORTH-ATLANTIC; BARENTS SEA; WATER; KONGSFJORDEN; FJORD; RECONSTRUCTION; VARIABILITY; INDICATORS	Thirty-six seabed samples from inshore and offshore Svalbard and the northern part of the Barents Sea were collected for dinoflagellate cyst (dinocyst) analysis. Svalbard is an important locality representing the distal influence of an attenuated North Atlantic Current, and crucial to the understanding of the thermohaline circulation in the North Atlantic. The study presents the first modern report of dinoflagellate cysts from this region making use of many recent taxonomic advances. Dinocysts are associated with waters of particular abiotic and biotic properties (temperature, salinity and nutrient content). On the basis of the dinocyst assemblages recovered from the sediments, several surface water types are recognized including those influenced by warm, saline Atlantic Water (AW) and those, where such influence is restricted.	[Grosfjeld, Kari] Geol Survey Norway, N-7021 Trondheim, Norway; [Harland, Rex] Univ Gothenburg, Dept Earth Sci, SE-40530 Gothenburg, Sweden; [Howe, John] Scottish Assoc Marine Sci, Dunstaffnage Marine Lab, Dept Biogeochem & Earth Sci, Oban PA37 1QA, Argyll, Scotland	Geological Survey of Norway; University of Gothenburg; University of the Highlands & Islands	Grosfjeld, K (通讯作者)，Geol Survey Norway, N-7021 Trondheim, Norway.	kari.grosfjeld@ngu.no; rex.harland@ntlworld.com; John.Howe@sams.ac.uk			Norwegian Research Council	Norwegian Research Council(Research Council of Norway)	We acknowledge the Norwegian Research Council through the French/Norwegian collaboration project Aurora for funding, Kari Lise Rorvik for assisting with the collection of the samples on board r\v Heincke, Bente Kjosnes at the Geological Survey of Norway for processing the samples and Martin Head and Anne de Vernal for improving the manuscript by their critical reviewing. 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J. Geol.		2009	89	1-2					121	134						14	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	590UQ					2025-03-11	WOS:000277254200013
J	Rorvik, KL; Grosfjeld, K; Hald, M				Rorvik, Kari-Lise; Grosfjeld, Kari; Hald, Morten			A Late Holocene climate history from the Malangen fjord, North Norway, based on dinoflagellate cysts	NORWEGIAN JOURNAL OF GEOLOGY			English	Article							RADIOCARBON AGE CALIBRATION; SEA-SURFACE CONDITIONS; PHYSICAL OCEANOGRAPHY; SUMMER TEMPERATURES; TIME SCALE; RECORD; SHELF; RECONSTRUCTION; GREENLAND; SEDIMENTS	The Malangen fjord, a high Boreal/low Arctic fjord in northern Norway, reflects Atlantic Water heat flux. Studies of dinoflagellate cyst assemblages, reflecting the fjord surface water masses, have been performed on sediment cores and surface sediment samples in order to reconstruct the Late Holocene climate history. Four dinoflagellate cyst assemblage zones reflect the hydrological changes that took place in the Malangen fjord during the Late Holocene. The periods from c. AD 500 to 790 and c. AD 1500 to 1940, stand out as cold periods. The period from c. AD 790 to 1500 is characterized by warm saline water, whereas the period from AD 1940 to present is characterized by decreasing inflow of warm, saline water.	[Rorvik, Kari-Lise; Hald, Morten] Univ Tromso, Dept Geol, NO-9011 Tromso, Norway; [Grosfjeld, Kari] Geol Survey Norway NGU, NO-7491 Trondheim, Norway	UiT The Arctic University of Tromso; Geological Survey of Norway	Rorvik, KL (通讯作者)，Univ Tromso, Dept Geol, NO-9011 Tromso, Norway.	kari-lise.rorvik@ig.uit.no; kari.grosfjeld@ngu.no; morten.hald@ig.uit.no						ANDREWS JT, 1999, GEOPHYS MONOGRAPH, V2335; Appleby P.G., 1992, URANIUM SERIES DISEQ, P731; APPLEBY PG, 1986, HYDROBIOLOGIA, V143, P21, DOI 10.1007/BF00026640; Appleby PG., 1978, CATENA, V5, P1, DOI [10.1016/S0341-8162(78)80002-2, DOI 10.1016/S0341-8162(78)80002-2]; BRIFFA KR, 1992, CLIM DYNAM, V7, P111, DOI 10.1007/BF00211153; BRIFFA KR, 1990, NATURE, V346, P434, DOI 10.1038/346434a0; Broecker WS, 2001, SCIENCE, V291, P1497, DOI 10.1126/science.291.5508.1497; DANSGAARD W, 1975, NATURE, V255, P24, DOI 10.1038/255024a0; DANSGAARD W, 1969, SCIENCE, V166, P377, DOI 10.1126/science.166.3903.377; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; Eiríksson J, 2006, HOLOCENE, V16, P1017, DOI 10.1177/0959683606hl991rp; FLOHN H, 1984, CLIMATE EUROPE PRESE, P356; Gade H.G., 1986, The Nordic Seas, P183, DOI DOI 10.1007/978-1-4615-8035-5_7; GRONAS S, 1999, CICERONE, V3, P29; HALD M, 1999, SPINOF CRUISE REPORT; HALD M, 2000 YEAR RECO UNPUB; HANSSENBAUER I, 1999, OTTAR, V4, P41; Hass HC, 1996, PALAEOGEOGR PALAEOCL, V123, P121, DOI 10.1016/0031-0182(95)00114-X; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; HOPKINS TS, 1991, EARTH-SCI REV, V30, P175, DOI 10.1016/0012-8252(91)90001-V; Hughen KA, 2004, RADIOCARBON, V46, P1059, DOI 10.1017/S0033822200033002; Husum K, 2004, J FORAMIN RES, V34, P34, DOI 10.2113/0340034; Jennings AE, 1996, HOLOCENE, V6, P179, DOI 10.1177/095968369600600205; KARLEN W, 1988, QUATERNARY SCI REV, V7, P199, DOI 10.1016/0277-3791(88)90006-6; Kirchhefer AJ, 2001, HOLOCENE, V11, P41, DOI 10.1191/095968301670181592; Kristensen DK, 2004, PALEOCEANOGRAPHY, V19, DOI 10.1029/2003PA000960; LABEYRIE L, 1999, IMAGES CRUISE REPORT; Lamb H.H., 1977, Climate, Present, P835; Lamb H. H., 1969, GEN CLIMATOLOGY, V2, P173; LAMB HH, 1979, QUATERNARY RES, V11, P1, DOI 10.1016/0033-5894(79)90067-X; LENTIN JK, 2004, AM ASS STRATIGRAPHIC, V28; MANGERUD J, 1975, QUATERNARY RES, V5, P263, DOI 10.1016/0033-5894(75)90028-9; Marret F, 2004, HOLOCENE, V14, P689, DOI 10.1191/0959683604hl747rp; NESJE A, 1991, QUATERNARY SCI REV, V10, P87, DOI 10.1016/0277-3791(91)90032-P; Normann U, 2001, SEA ENV DATA NO NORW; OGILVIE AEJ, 1984, CLIMATIC CHANGE, V6, P131, DOI 10.1007/BF00144609; Reimer PJ, 2004, RADIOCARBON, V46, P1029, DOI 10.1017/S0033822200032999; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A, 2008, MAR MICROPALEONTOL, V68, P1, DOI 10.1016/j.marmicro.2008.04.001; Rochon Andre, 1999, AASP Contributions Series, V35, P1; ROTHLISBERGER F, 1976, ALPEN, V52, P59; SAELEN OH, 1947, VENGSOYFJORD MALANGE, V70, P1; SCHONWIESE CD, 1979, KLIMASHCWANKUNGEN; STUIVER M, 1993, RADIOCARBON, V35, P215, DOI 10.1017/S0033822200013904; STUIVER M, 1993, RADIOCARBON, V35, P1, DOI 10.1017/S0033822200013874; STUIVER M, 1993, RADIOCARBON, V35, P67, DOI 10.1017/S0033822200013813; THOMPSON LG, 1992, CLIMATE AD 1500, P517; Thomsen E., 1986, Striae, V24, P207; Wassmann P, 1996, J MARINE SYST, V8, P53, DOI 10.1016/0924-7963(95)00037-2	50	6	6	0	2	GEOLOGICAL SOC NORWAY	TRONDHEIM	C/O NGU, 7491 TRONDHEIM, NORWAY		1502-5322		NORW J GEOL	Norw. J. Geol.		2009	89	1-2					135	147						13	Geosciences, Multidisciplinary	Science Citation Index Expanded (SCI-EXPANDED)	Geology	590UQ					2025-03-11	WOS:000277254200014
B	Wood, AM; Wilkinson, IP; Maybury, CA; Whatley, RC		Whittaker, JE; Hart, MB		Wood, Adrian M.; Wilkinson, Ian P.; Maybury, Caroline A.; Whatley, Robin C.			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J	Kholeif, SEA; Mudie, PJ				Kholeif, Suzan E. A.; Mudie, Peta J.			PALYNOLOGICAL RECORDS OF CLIMATE AND OCEANIC CONDITIONS IN THE LATE PLEISTOCENE AND HOLOCENE OF THE NILE CONE, SOUTHEASTERN MEDITERRANEAN, EGYPT	PALYNOLOGY			English	Article						Dinoflagellate cysts; pollen; spores; amorphous organic matter; sapropel S1; Nile Cone; Late Pleistocene; Holocene	LATE QUATERNARY STRATIGRAPHY; LAND-SEA CORRELATION; ORGANIC-MATTER; DINOFLAGELLATE CYSTS; SAPROPEL RECORD; SUMMER MONSOON; POLLEN; EVOLUTION; CORES; FLUCTUATIONS	Variations in palynomorph concentrations and relative abundances, including pollen and spores, organic-walled dinoflagellate cysts, and amorphous organic matter (AOM), were studied in sediment core NC Core 2 from the upper slope (1,030 m water depth) of the Nile Cone, southeastern Mediterranean, Egypt. Each sample represents palynomorph deposition for intervals of around 500-1,000 years, and this study provides the first detailed palynological record for the Nile Cone. The dinoflagellate cyst assemblages and AOM production reflect changes in surface water temperature and river discharge in response to climate forcing as marked by variations in pollen and spore indicators of semi-desert vegetation and tropical Monsoon intensity. The basal sediments (approximately 14,600-9,500 yr before present [BP]) contain high concentrations and relative abundances of Polysphaeridium zoharyi, Polysphaeridium spp., Spiniferites elongatus, and Spiniferites spp. during the transition from postglacial to interglacial conditions. Variations in these taxa and total Impagidinium spp. suggest a gradual temperature increase, interrupted by a pre-Holocene cool interval around 11,000 yr BP. The high African monsoon index for this pre-Holocene time corresponds with pollen evidence of relatively high Nile discharge. The organic-rich S I sapropel sediments, dated as around 9,500-6,270 yr BP, were deposited several thousand years later, during a time of lower Monsoon index, warmer surface water, and increased dinoflagellate cyst production. This was accompanied by moderate Nile flooding and oxygen-deficient or anoxic bottom water on the upper Nile Cone, mainly supporting the increased production and carbon import hypothesis for eastern Mediterranean S1 formation. Dinoflagellate cyst assemblages in the Nile Cone S1 differ from those of the deeper, more northern Levantine and Cretan basins in the near absence of heterotrophic protoperidinioid cysts, despite the uniformly high organic S I carbon content. The prevailing climate during the formation of sapropelic sediments in the southeastern Mediterranean was tropical to subtropical, but was interrupted by an early cooler interval with reduced humidity, as marked by re-appearance of Spiniferites elongatus and increased Ephedra pollen. The carbonate-rich surface layers were probably deposited under warm dry climatic conditions with minimum Nile input, but evidence of oxidation prevents detailed interpretation.	[Mudie, Peta J.] Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada; [Kholeif, Suzan E. A.] NIOF, Alexandria, Egypt	Natural Resources Canada; Lands & Minerals Sector - Natural Resources Canada; Geological Survey of Canada; Egyptian Knowledge Bank (EKB); National Institute of Oceanography & Fisheries (NIOF)	Mudie, PJ (通讯作者)，Geol Survey Canada Atlantic, Nat Resources Canada, Dartmouth, NS B2Y 4A2, Canada.	Suzan_Kholeif@yahoo.com; pmudie@nrcan.gc.ca			National Institute of Oceanography and Fisheries (NIOF), Alexandria, Egypt	National Institute of Oceanography and Fisheries (NIOF), Alexandria, Egypt	The authors gratefully acknowledge Dr. Mona Khalil (National Institute of Oceanography and Fisheries (NIOF), Alexandria, Egypt), for providing the samples and geochernical data. Sincere thanks go to Professor Karin Zonneveld (Bremen University, Germany) and to Dr. Fabienne Marret (University of Liverpool, U.K.), for their help in identification, providing references, and suggestions during the preparation of the manuscript. We also thank four reviewers, particularly Drs. Rex Harland and Suzanne Leroy, for their helpful comments.	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J	Kawami, H; Matsuoka, K				Kawami, Hisae; Matsuoka, Kazumi			A NEW CYST-THECA RELATIONSHIP FOR <i>PROTOPERIDINIUM</i> <i>PARTHENOPES</i> ZINGONE & MONTRESOR 1988 (PERIDINIALES, DINOPHYCEAE)	PALYNOLOGY			English	Article						Cyst-theca relationship; Protoperidinium parthenopes; Protoperidinium americanum; capsulate cyst	WALLED DINOFLAGELLATE CYSTS; RECENT MARINE-SEDIMENTS; SP-NOV DINOPHYCEAE; SURFACE SEDIMENTS; COASTAL WATERS; INDIAN-OCEAN; SEA; DISTRIBUTIONS; AFRICA; NORWAY	Organic-walled resting cysts of Protoperidinium parthenopes Zingone & Montresor 1988 were collected from a sediment trap in Omura Bay, western Japan. The cysts are spherical and pale brown in color. The cyst wall has two layers: a thick endophragm with granulate surface, and a thin periphragm. Three complete and incomplete parasutures appear on the surface of the endocyst. The archeopyle formed on the endocyst is basically saphopylic and compound with some combination of complete and incomplete parasutures. The cyst of Protoperidinium parthenopes closely resembles the cyst of Protoperidinium americanum (Gran & Braarud 1935) Balech 1974, but differs in the shape of the periphragm, the cyst diameter, and in the archeopyle.	[Matsuoka, Kazumi] Nagasaki Univ, Inst E China Sea Res, Nagasaki 8528521, Japan; [Kawami, Hisae] Nagasaki Univ, Grad Sch Sci & Technol, Nagasaki 8528521, Japan	Nagasaki University; Nagasaki University	Matsuoka, K (通讯作者)，Nagasaki Univ, Inst E China Sea Res, Nagasaki 8528521, Japan.	kazu-mtk@nagasaki-u.ac.jp			Japan Society for the Promotion of Science [18340166]; Grants-in-Aid for Scientific Research [18340166] Funding Source: KAKEN	Japan Society for the Promotion of Science(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of Science); Grants-in-Aid for Scientific Research(Ministry of Education, Culture, Sports, Science and Technology, Japan (MEXT)Japan Society for the Promotion of ScienceGrants-in-Aid for Scientific Research (KAKENHI))	We thank I. Kawaguchi for his kind assistance during sample collecting in Omura Bay. We are indebted to M. Iwataki and members of the Laboratory of Coastal Environmental Sciences, Nagasaki University for their advice Rochon,and an anonymous reviewer, for their constructive comments on the manuscript. We dedicate this article to the late Professor John H. Wrenn, a good friend and outstanding scientist. This work is partly supported by a Grant-in-Aid for Science from the Japan Society for the Promotion of Science (Re: 18340166).	[Anonymous], OCEAN BIOCOENOSIS SE; [Anonymous], SPECIAL PUBLICATION; BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Bujak J.P., 1983, AM ASS STRATIGRAPHIE, V13, P1; Cho HJ, 2003, BOT MAR, V46, P332, DOI 10.1515/BOT.2003.030; Cho HJ, 2001, MAR MICROPALEONTOL, V42, P103, DOI 10.1016/S0377-8398(01)00016-0; DALE B, 1976, REV PALAEOBOT PALYNO, V22, P39, DOI 10.1016/0034-6667(76)90010-5; FRITZ L, 1985, J PHYCOL, V21, P662, DOI 10.1111/j.0022-3646.1985.00662.x; Gomez Fernando, 2005, Acta Botanica Croatica, V64, P129; HARLAND R, 1982, PALAEONTOLOGY, V25, P369; Head M.J., 1996, Palynology: Principles and Applications, P1197; Joyce LB, 2005, HARMFUL ALGAE, V4, P309, DOI 10.1016/j.hal.2004.08.001; KIM HS, 1999, THESIS NAGASAKI U JA; Kim Hyeung-Sin, 1998, Bulletin of Plankton Society of Japan, V45, P133; Lewis J., 1987, Journal of Micropalaeontology, V6, P113; Marret F, 2004, HOLOCENE, V14, P689, DOI 10.1191/0959683604hl747rp; Marret F, 1997, MAR MICROPALEONTOL, V29, P367, DOI 10.1016/S0377-8398(96)00049-7; Matsuoka K., 2000, Technical guide for modern dinoflagellate cyst study, P1; Matsuoka K, 1999, E CHINA SEA, P195; Matsuoka K., 1987, Bull. 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Sci., V28, P35; Montresor M, 1998, J PLANKTON RES, V20, P2291, DOI 10.1093/plankt/20.12.2291; Morquecho L, 2003, BOT MAR, V46, P132, DOI 10.1515/BOT.2003.014; Moscatello S, 2004, SCI MAR, V68, P85, DOI 10.3989/scimar.2004.68s185; Nehring S, 1997, BOT MAR, V40, P307, DOI 10.1515/botm.1997.40.1-6.307; Orlova TY, 2004, BOT MAR, V47, P184, DOI 10.1515/BOT.2004.019; Persson A, 2000, BOT MAR, V43, P69, DOI 10.1515/BOT.2000.006; Pospelova V, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001251; REID PC, 1972, THESIS U SHEFFIELD E; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; SARNO D, 1993, HYDROBIOLOGIA, V271, P27, DOI 10.1007/BF00005692; Siano R, 2005, EUR J PHYCOL, V40, P221, DOI 10.1080/09670260500128293; Targarona J, 1999, GRANA, V38, P170; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; Wang ZH, 2004, MAR ECOL-P S Z N I, V25, P289, DOI 10.1111/j.1439-0485.2004.00035.x; Watanabe MM., 2000, NIES COLLECTION LIST; ZINGONE A, 1988, CRYPTOGAMIE ALGOL, V9, P117; ZONNEVELD KA, 1994, PHYCOLOGIA, V33, P359, DOI 10.2216/i0031-8884-33-5-359.1; Zonneveld KAF, 2001, PROG OCEANOGR, V48, P25, DOI 10.1016/S0079-6611(00)00047-1; Zonneveld KAF, 1997, DEEP-SEA RES PT II, V44, P1411, DOI 10.1016/S0967-0645(97)00007-6	39	17	17	0	4	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2009	33		2				11	18		10.1080/01916122.2009.9989680	http://dx.doi.org/10.1080/01916122.2009.9989680			8	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	551JL					2025-03-11	WOS:000274204000003
J	Le Hérissé, A; Dorning, KJ; Mullins, GL; Wicander, R				Le Herisse, Alain; Dorning, Ken J.; Mullins, Gary L.; Wicander, Reed			GLOBAL PATTERNS OF ORGANIC-WALLED PHYTOPLANKTON BIODIVERSITY DURING THE LATE SILURIAN TO EARLIEST DEVONIAN	PALYNOLOGY			English	Review						Acritarchs; organic-walled phytoplankton; biodiversity; marine ecosystems; Late Silurian; earliest Devonian	DINOFLAGELLATE CYSTS; PRASINOPHYCEAN PHYCOMATA; ACRITARCH DISTRIBUTION; BIOLOGICAL AFFINITIES; BAINBRIDGE FORMATION; EXTINCTION EVENT; OCEANIC EPISODES; LATE ORDOVICIAN; LUDLOW SERIES; ACTIVE MARGIN	Numerous environmental factors as well as oceanic circulation patterns and geographic constraints all contribute to the abundance, distribution, and diversity of present-day marine phytoplankton assemblages. These same factors presumably affected the Paleozoic marine phytoplankton, which was dominated by organic-walled acritarchs and prasinophytes. During the Late Silurian (Gorstian, Ludfordian, and Pridoli) and earliest Devonian (Lochkovian), important paleogeographic, paleooceanographic, and geochemical changes were occurring as well as major compositional changes and diversity fluctuations in the marine organic-walled phytoplankton. Innovative morphologies appeared during the Late Silurian, in both low and high latitude assemblages, but with significant quantitative differences. This was followed by a turnover in assemblage composition during the Silurian/Devonian transition, and an initial radiation of new acritarch and prasinophyte taxa in the Early Devonian. Observed changes in total phytoplankton diversity during the Gorstian through earliest Lochkovian are based on organic-walled microphytoplankton data derived from published and unpublished key stratigraphic sections where independent age control has been firmly established. These key sections are from: Missouri and Oklahoma, U.S.A. and western Newfoundland, Canada (Laurentia); Gotland, Sweden, and Podolia, Ukraine (Baltica); the Welsh Basin and Borderland (Avalonia); northern France and northern Spain (Armorica); and Libya in northern Africa, and Argentina and Bolivia, South America (Gondwana). Regional biodiversity changes for the organic-walled microphytoplankton were determined for the warm low latitude areas (Baltica, Laurentia, and Avalonia) and temperate to cool higher latitude areas (northern and southern Gondwana). The Late Silurian-earliest Devonian organic-walled phytoplankton was divided into three major categories to facilitate comparison of compositional fluctuations, both within stratigraphic sections as well as between geographic areas. The three categories, based on overall morphology, are marine chlorophytes and prasinophytes, marine acritarchs, and nonmarine types, including coenobial forms. This triparate grouping is both broad and detailed enough to mark critical changes in both the phytoplankton assemblages, as well as the paleoenvironment. In general, high phytoplankton diversity peaks occurred during the Early and Late Gorstian in the warm low latitude areas, followed by varying fluctuations during the Ludfordian and Pridoli for both the warm low latitude and cool high latitude areas. An initial radiation of new phytoplankton taxa and the appearance of more cosmopolitan assemblages mark the beginning of the Lochkovian.	[Le Herisse, Alain] Univ Brest, Inst Univ Europeen Mer, CNRS, UMR Domaines Ocean 6538, F-29238 Brest 3, France; [Dorning, Ken J.] Pallab Res, Sheffield S6 5DX, S Yorkshire, England; [Mullins, Gary L.] Univ Leicester, Dept Geol, Leicester LE1 7RH, Leics, England; [Wicander, Reed] Cent Michigan Univ, Dept Geol, Mt Pleasant, MI 48859 USA	Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); University of Leicester; Central Michigan University	Le Hérissé, A (通讯作者)，Univ Brest, Inst Univ Europeen Mer, CNRS, UMR Domaines Ocean 6538, Batiment G,6 Ave Le Gorgeu, F-29238 Brest 3, France.	Alain.Le.Herisse@univ-brest.fr; kjdorning@googlemail.com; gary.mullins@fugro-robertson.com; reed.wicander@cmich.edu			Leverhulme Trust Research Interchange [F/00212/F]	Leverhulme Trust Research Interchange(Leverhulme Trust)	Reed Wicander thanks Central Michigan University for granting sabbatical leave to undertake this project. This is a contribution to the phytoPal project funded by the Leverhulme Trust Research Interchange Grant Reference F/00212/F, awarded to Richard J. Aldridge (Department of Geology, University of Leicester, United Kingdom). In addition, we would like to thank Richard J. Aldridge for all his help and support of this project. We also thank Stewart G. Molyneux (British Geological Survey, Nottingham, United Kingdom) and Thomas Servais (Universite des Sciences et Technologies de Lille, France) for critically reviewing, and making useful suggestions for the improvement of this paper.	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J	Warny, S				Warny, Sophie			SPECIES OF THE ACRITARCH GENUS <i>PALAEOSTOMOCYSTIS</i> DEFLANDRE 1937: POTENTIAL INDICATORS OF NERITIC SUBPOLAR TO POLAR ENVIRONMENTS IN ANTARCTICA DURING THE CENOZOIC	PALYNOLOGY			English	Article						Palaeostomocystis; acritarch; palynomorph; Antarctica; glaciation; neritic	DINOFLAGELLATE CYSTS; SEA; SEDIMENTS; TRANSECT; PACIFIC	A palynological analysis was undertaken on 16 samples from seven piston cores collected along two offshore transects near Seymour and James Ross Islands. Diverse assemblages of reworked marine microplankton (including organic-walled dinoflagellate cysts, cymatiosphaerids leiospheres,and other acritarchs) and terrestrial palynomorphs (including pollen and spores) were recovered from glacio-marine sediments' of late Pleistocene age. Among the reworked taxa, four species belonging to the acritarch genus Palaeostomocystis Deflandre 1937 comprise up to 17% of all palynomorphs. Highest abundances were recorded from sites close to the coast. The potential use of Palaeostomocystis as a proxy for early ice-sheet development on the Antarctic margins is evaluated in light of earlier studies. This evaluation suggests that the high abundances of Palaeostomocystis on the Antarctic Peninsula reflect neritic-type environments (shallow waters, bay-like areas, or marginal seas) and sub-polar to polar conditions as exist in the Bering Sea, Greenland margins, and other sub-arctic to arctic areas today.	[Warny, Sophie] Louisiana State Univ, Dept Geol & Geophys, Baton Rouge, LA 70803 USA; [Warny, Sophie] Louisiana State Univ, Museum Nat Sci, Baton Rouge, LA 70803 USA	Louisiana State University System; Louisiana State University; Louisiana State University System; Louisiana State University	Warny, S (通讯作者)，Louisiana State Univ, Dept Geol & Geophys, E-235 Howe Russell Bldg, Baton Rouge, LA 70803 USA.	swarny@lsu.edu	Warny, Sophie/A-8226-2013	Warny, Sophie/0000-0002-3451-040X	National Science Foundation [0533879]; Division Of Polar Programs; Directorate For Geosciences [0533879] Funding Source: National Science Foundation	National Science Foundation(National Science Foundation (NSF)); Division Of Polar Programs; Directorate For Geosciences(National Science Foundation (NSF)NSF - Directorate for Geosciences (GEO))	Thanks are extended to Martin J. Head for his editorial help, and reviewers Mike Hannah and Fabienne Marret for their constructive feedback on the manuscript. This research is funded by the National Science Foundation, SGER grant #0533879. Thanks are extended to Dr. John Anderson,Rice University, for providing samples from his pre-SHALDRIL cruise.	Anderson J., 1992, Recent Progress in Antarctic Earth Sciences, P603; Anderson J.B., 1999, ANTARCTIC MARINE GEO; ANDERSON JB, 2006, EOS T AGU, V87, P402, DOI DOI 10.1029/2006EO390003; [Anonymous], ANTARCTIC RES SERIES; Balech E., 1965, Antarctic Research Series, V5, P107; BARSS MS, 1973, GEOL SURV CAN PAP, V73, P1; Bart P.J., 1995, GEOLOGY SEISMIC STRA, V68, P75; Birkenmajer K., 1989, Origins and Evolution of the Antarctic Biota, P227; Brinkhuis H., 2003, P OCEAN DRILLING PRO, P1, DOI [10.2973/odp.proc.sr.189.106.2003, DOI 10.2973/ODP.PROC.SR.189.106.2003]; BUJAK JP, 1984, MICROPALEONTOLOGY, V30, P180, DOI 10.2307/1485717; DEFLANDRE G., 1937, ANN PALEONTOL, V26, P51; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; FOUCHER JC, 1971, B MUSEE NATL HIST NA, V21; Gray J., 1965, Handbook of paleontological techniques, P530; HALL SA, 1977, NATURE, V267, P239, DOI 10.1038/267239a0; Harland R, 1998, PALAEONTOLOGY, V41, P1093; Ichinomiya M, 2004, AQUAT MICROB ECOL, V37, P305, DOI 10.3354/ame037305; Ivany LC, 2006, GEOLOGY, V34, P377, DOI 10.1130/G22383.1; Macphail M.K., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V188, P1; Mohr B.A.R., 1990, Proceedings of the Ocean Drilling Program Scientific Results, V113, P449, DOI 10.2973/odp.proc.sr.113.207.1990; MUDIE P.J., 1992, NEOGENE QUATERNARY D, P347; Munk P, 2003, J PLANKTON RES, V25, P815, DOI 10.1093/plankt/25.7.815; Pirrie D, 1997, GEOL MAG, V134, P745, DOI 10.1017/S0016756897007796; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Roncaglia L, 2004, GRANA, V43, P81, DOI 10.1080/00173130410018966; *SHALDR STEER COMM, 2003, SHALDRIL NEWSLETTER, V2, P1; SHAOZHI M, 1994, REV PALAEOBOT PALYNO, V86, P235; van Waveren I.M., 1994, Scripta Geologica, V105, P27; Warny S, 2006, PALYNOLOGY, V30, P151; Wrenn J.H., 1988, Geological Society of America Memoir, V169, P321; WRENN JH, 2001, 34 ANN M SAN ANT TEX, P34	31	10	10	0	3	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2009	33		2				43	54		10.1080/01916122.2009.9989682	http://dx.doi.org/10.1080/01916122.2009.9989682			12	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	551JL					2025-03-11	WOS:000274204000005
J	Soliman, A; Head, MJ; Louwye, S				Soliman, Ali; Head, Martin J.; Louwye, Stephen			MORPHOLOGY AND DISTRIBUTION OF THE MIOCENE DINOFLAGELLATE CYST <i>OPERCULODINIUM</i>? <i>BORGERHOLTENSE</i> LOUWYE 2001, EMEND	PALYNOLOGY			English	Article						Operculodinium? borgerholtense; Miocene dinoflagellate cysts; morphology; taxonomy	CENTRAL PARATETHYS; NORTHERN BELGIUM; STRATIGRAPHY	The extinct, organic-walled, proximochorate dinoflagellate cyst Operculodinium? borgerholtense Louwye 2001 was first described from Miocene shallow-marine deposits of northern Belgium, and has since been documented from the Miocene of the eastern North Atlantic, North Sea, Austria, Hungary, and Egypt. Conventional and confocal light microscopy and scanning electron microscopy are used to reveal new details of the archeopyle, wall structure, and ornament. The archeopyle is shown to have well-defined rather than rounded angles, a distinction we consider significant in assigning this species only provisionally to the genus. Operculodinium? borgerholtense was a euryhaline neritic species highly tolerant of environmental stress, a feature consistent with its morphological variability. Present records indicate it tropical-subtropical to temperate paleoclimatic distribution. It ranges from the upper Lower Miocene to tipper Middle Miocene, and promises to be a useful stratigraphic marker particularly in neritic settings where adverse paleoenvironmental factors have excluded other species.	[Soliman, Ali] Karl Franzens Univ Graz, Graz Inst Earth Sci Geol & Palaeontol, A-8010 Graz, Austria; [Soliman, Ali] Tanta Univ, Fac Sci, Dept Geol, Tanta 31527, Egypt; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium	University of Graz; Egyptian Knowledge Bank (EKB); Tanta University; Brock University; Ghent University	Soliman, A (通讯作者)，Karl Franzens Univ Graz, Graz Inst Earth Sci Geol & Palaeontol, Heinrichstr 26, A-8010 Graz, Austria.	ali.soliman@uni-graz.at; mjhead@brocku.ca; Stephen.Louwye@ugent.be	Soliman, Ali/R-1583-2018; Louwye, Stephen/D-3856-2012	Louwye, Stephen/0000-0003-4814-4313; Soliman, Ali/0000-0001-7366-4607	Austrian Exchange Service (OAD); Commission for the Palaeontological; Stratigraphical Research of Austria (Austrian Academy of Science); Natural Sciences and Engineering Research Council of Canada	Austrian Exchange Service (OAD); Commission for the Palaeontological; Stratigraphical Research of Austria (Austrian Academy of Science); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	A.S. thanks the Austrian Exchange Service (OAD) and the Commission for the Palaeontological and Stratigraphical Research of Austria (Austrian Academy of Science) for financial support, and M. Faris (Tanta University) and Salah El Beialy (El Mansoura University) respectively for providing samples from the Kareem-30 and East Shukheir-1 boreholes of the Gulf of Suez. Werner Piller (Karl-Franzens University, Graz) generously made available laboratory and SEM facilities, and provided the Waltersdorf-I samples. S. Mullegger (Karl-Franzens University, Graz) kindly provided the Retznei sample. We are most grateful to Dries Vercauteren (Ghent University) for use of the confocal microscope facility. M.J.H. acknowledges support from a Natural Sciences and Engineering Research Council of Canada discovery grant. It is a pleasure to thank D.K. Munsterman (Netherlands Institute of Applied Geoscience TNO) and S. Piasecki (Geological Survey of Denmark and Greenland) for their helpful reviews of the manuscript.	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J	Verleye, TJ; Mertens, KN; Louwye, S; Arz, HW				Verleye, Thomas J.; Mertens, Kenneth N.; Louwye, Stephen; Arz, Helge W.			HOLOCENE SALINITY CHANGES IN THE SOUTHWESTERN BLACK SEA: A RECONSTRUCTION BASED ON DINOFLAGELLATE CYSTS	PALYNOLOGY			English	Article						Dinoflagellate cysts; salinity changes; Black Sea; Holocene	LATE QUATERNARY; MINOAN ERUPTION; MARMARA SEA; STRATIGRAPHY; VARIABILITY; INDICATORS; MORPHOLOGY; SANTORINI; SEDIMENTS; BOSPORUS	Dinoflagellate cysts were used as a proxy for reconstructing the salinity variations during the Holocene in the southwestern Black Sea. The aim of this study was to determine the timing of the reconnection between the Black and Marmara seas. Core GeoB 7625-2, located 50 km northeast of the mouth of the Sakarya River, was sampled with a 200-year resolution between 7.42 and 0.52 ka BP. The lower part of the core was sampled with varying resolution. A distinct change in the dinoflagellate cyst assemblages from freshwater/brackish water to saltwater was observed between similar to 8.25 and similar to 7.97 ka BP, which is similar to 0.6 ka earlier than observed in other dinoflagellate cyst studies. This discrepancy may indicate the diachronous salinification of the Black Sea. The freshwater to brackish water assemblage is dominated by Pyxidinopsis psilata and Spiniferites cruciformis, while the most important euryhaline species are Lingulodinium machaerophorum and cysts of Pentapharsodinium dalei. The average process length of Lingulodinium machaerophorum was used as a salinity proxy. Both proxies suggest a gradual reconnection between the Black and Marmara seas, and these findings confirm earlier studies. Peridinium ponticum is restricted to the Black Sea; abundance fluctuations of this species were controlled by salinity variations and changes in nutrient concentrations. Earlier studies have demonstrated that the 800 to 500 year cycles observed in the sedimentary record are related to the intensity of the discharge of the Sakarya River, and linked to the North Atlantic Oscillations. Cysts of Pentapharsodinium dalei and Spiniferites spp. fluctuated synchronously with the clay layer frequency. The poor preservation of these forms may indicate shelfal transport during periods of intense river discharge. The variation in relative abundance of heterotrophic species does not correlate with the clay layer frequency, since upwelling and nutrient supply also influenced their abundances. Lingulodinium machaerophorum shows the highest relative abundances during periods with reduced river input.	[Verleye, Thomas J.; Mertens, Kenneth N.; Louwye, Stephen] Univ Ghent, Res Unit Palaeontol, B-9000 Ghent, Belgium; [Arz, Helge W.] Geoforschungszentrum Potsdam, D-14473 Potsdam, Germany	Ghent University; Helmholtz Association; Helmholtz-Center Potsdam GFZ German Research Center for Geosciences	Verleye, TJ (通讯作者)，Univ Ghent, Res Unit Palaeontol, Krijgslaan 281-S8 WE13, B-9000 Ghent, Belgium.	thomas.verleye@ugent.be	Arz, Helge/A-6659-2013; Mertens, Kenneth/AAO-9566-2020; Mertens, Kenneth/C-3386-2015; Louwye, Stephen/D-3856-2012	Arz, Helge Wolfgang/0000-0002-1997-1718; Mertens, Kenneth/0000-0003-2005-9483; Louwye, Stephen/0000-0003-4814-4313	Institute for the Encouragement of Innovation	Institute for the Encouragement of Innovation	Financial support to the first author was provided by the Institute for the Encouragement of Innovation through Science and Technology in Flanders. Fabienne Marret, Jens Matthiessen, and Karin Zonneveld are thanked for stimulating discussions on the morphology of some species. Sharon Schillewaert measured the process lengths of Lingulodinium machaerophorum in a number of samples. Technical assistance by Sabine Vancauwenberghe is acknowledged. The constructive reviews by Barrie Dale (Oslo University) and an anonymous reviewer are much appreciated and greatly improved the manuscript.	Aksu A.E., 2002, GSA Today, V12, P4, DOI DOI 10.1130/1052-5173(2002)012<0004:PH0FTB>2.0.C0;2; Aksu AE, 2002, MAR GEOL, V190, P61, DOI 10.1016/S0025-3227(02)00343-2; [Anonymous], NOVA HEDWIGIA; Bahr A, 2006, EARTH PLANET SC LETT, V241, P863, DOI 10.1016/j.epsl.2005.10.036; BESIKTEPE ST, 1994, PROG OCEANOGR, V34, P285, DOI 10.1016/0079-6611(94)90018-3; Cullen HM, 2000, INT J CLIMATOL, V20, P853, DOI 10.1002/1097-0088(20000630)20:8<853::AID-JOC497>3.0.CO;2-M; DALE B., 1996, PALYNOLOGY PRINCIPLE, P1249; DALE B, 1994, NATO ASI SER, V1, P521; Delaney MP, 2004, J MARINE SYST, V49, P123, DOI 10.1016/j.jmarsys.2003.10.006; Ellegaard M, 2000, REV PALAEOBOT PALYNO, V109, P65, DOI 10.1016/S0034-6667(99)00045-7; Evitt WR, 1963, NATL ACAD SCI P, V49, P158; Felis T, 2004, NATURE, V429, P164, DOI 10.1038/nature02546; Fensome R.A., 2004, AM ASS STRATIGRAPHIC, V42; GUICHARD F, 1993, NATURE, V363, P610, DOI 10.1038/363610a0; HAMMER CU, 1987, NATURE, V328, P517, DOI 10.1038/328517a0; HAY BJ, 1991, DEEP-SEA RES, V38, pS1211; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; JORGENSEN BB, 2003, 031 METEOR CTR MAR E; Kara AB, 2008, J MARINE SYST, V74, P74, DOI 10.1016/j.jmarsys.2007.11.010; Kazmin AS, 2007, J MARINE SYST, V68, P293, DOI 10.1016/j.jmarsys.2007.01.002; Kerey IE, 2004, PALAEOGEOGR PALAEOCL, V204, P277, DOI 10.1016/S0031-0182(03)00731-4; Kouli K, 2001, REV PALAEOBOT PALYNO, V113, P273, DOI 10.1016/S0034-6667(00)00064-6; KRAFT JC, 1971, GEOL SOC AM BULL, V82, P2131, DOI 10.1130/0016-7606(1971)82[2131:SFPAGH]2.0.CO;2; Kwiecien O, 2008, RADIOCARBON, V50, P99, DOI 10.1017/S0033822200043393; Lamy F, 2006, PALEOCEANOGRAPHY, V21, DOI 10.1029/2005PA001184; LATIF ML, 1992, 922 MIDD E TU I MAR; Leroy SAG, 2007, QUATERNARY SCI REV, V26, P3359, DOI 10.1016/j.quascirev.2007.09.012; Lewis Jane, 1997, Oceanography and Marine Biology an Annual Review, V35, P97; Louwye S, 2004, GEOL MAG, V141, P353, DOI 10.1017/S0016756804009136; Marret F, 2004, REV PALAEOBOT PALYNO, V129, P1, DOI 10.1016/j.revpalbo.2003.10.002; Marret F, 2009, QUATERN INT, V197, P72, DOI 10.1016/j.quaint.2007.01.010; 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; MURRAY JW, 1991, BLACK SEA OCEANOGRAP, V351, P1; Ozsoy E, 1997, EARTH-SCI REV, V42, P231, DOI 10.1016/S0012-8252(97)81859-4; OZSOY E, 1995, B I OCEANOGR MONACO, V15, P1; Polat C., 1996, DYNAMICS MEDITERRANE, P167; Polat C. S., 1996, CIESME SCI SERIES, V2, P167; Reid P.C., 1974, Nova Hedwigia, V25, P579; Rochon A, 1999, AM ASS STRATIGRAPHIC, V35; Ross D.A., 1974, The Black Sea - geology, chemistry and biology; American Association of Petroleum Geologists, P183; Ryan WBF, 2003, ANNU REV EARTH PL SC, V31, P525, DOI 10.1146/annurev.earth.31.100901.141249; Ryan WBF, 1997, MAR GEOL, V138, P119, DOI 10.1016/S0025-3227(97)00007-8; Ryan William., 1998, Noah's Flood: The New Scientific Discoveries About the Event that Changed History; Stanev E., 2005, OCEANOGRAPHY, V18, P56, DOI [10.5670/oceanog.2005.42, DOI 10.5670/OCEANOG.2005.42]; Türkes M, 2003, INT J CLIMATOL, V23, P1771, DOI 10.1002/joc.962; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; Wall D., 1973, Geoscience Man, V7, P95; Yanko-Hombach V, 2007, QUATERN INT, V167, P91, DOI 10.1016/j.quaint.2006.08.004; Yu SY, 2007, QUATERNARY RES, V67, P215, DOI 10.1016/j.yqres.2006.12.004	50	43	45	0	10	AMER ASSOC STRATIGRAPHIC PALYNOLOGISTS FOUNDATION	COLLEGE STATION	C/O VAUGHN M BRYANT, JR, PALNOLOGY LABORATORY, TEXAS A & M UNIV, COLLEGE STATION, TX 77843-4352, UNITED STATES	0191-6122			PALYNOLOGY	Palynology		2009	33		1				77	100						24	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	551JJ					2025-03-11	WOS:000274203800003
J	Popescu, SM; Dalesme, F; Jouannic, G; Escarguel, G; Head, MJ; Melinte-Dobrinescu, MC; Süto-Szentai, M; Bakrac, K; Clauzon, G; Suc, JP				Popescu, Speranta-Maria; Dalesme, Florent; Jouannic, Gwenael; Escarguel, Gilles; Head, Martin J.; Melinte-Dobrinescu, Mihaela Carmen; Sueto-Szentai, Maria; Bakrac, Koraljka; Clauzon, Georges; Suc, Jean-Pierre			<i>GALEACYSTA</i> <i>ETRUSCA</i> COMPLEX: DINOFLAGELLATE CYST MARKER OF PARATETHYAN INFLUXES TO THE MEDITERRANEAN SEA BEFORE AND AFTER THE PEAK OF THE MESSINIAN SALINITY CRISIS	PALYNOLOGY			English	Review						Galeacysta etrusca complex; Paratethys-Mediterranean; Messinian; Zanclean; 'Lago Mare'	MIOCENE LAKE PANNON; NORTHERN APENNINES; DACIC BASIN; BLACK-SEA; LAGO-MARE; EASTERN PARATETHYS; PLIOCENE BOUNDARY; EVOLUTION; DEPOSITS; CHRONOLOGY	More than one thousand specimens of a morphological complex including Galeacysta etrusca Corradini & Biffi 1988 from I I Upper Miocene and Lower Pliocene localities of the Paratethyan and Mediterranean realms have been studied using a biometric approach in part relating to the degree of separation between endocyst and ectocyst. Four stable biometric groups have been distinguished statistically, the occurrence or prevalence of which appears closely linked to environmental conditions irrespective of the realm. Group 'a' is related to brackish conditions, group V to marine conditions, group V to freshwater, and group V to high nutrient levels. Based on an accurate chronology provided by calcareous nannoplankton bioevents and recognition of the Messinian Erosional Surface, this Study reveals: (1) the high sensitivity of the Galeacysta etrusca complex for reconstructing paleoenvironments and discriminating phases of connection and isolation of basins (2) the detailed history of this species complex which originated in the Pannonian Basin at ca. 8 Ma before invading the Dacic Basin during the interval 6-5.60 Ma, then migrating into the Mediterranean during high sea-level connections (the 'Lago Mare' events just before and after the peak of the Messinian Salinity Crisis, i.e. at 5.60 Ma and during the interval ca. 5.46-5.278 Ma, respectively), and finally into the Black Sea at ca. 5.13 Ma; (3) an improved paleogeography for the Mediterranean and Paratethyan realms with focus on the location of corridors and the timing of when they were active. Based on field observations and dinoflagellate cyst data, we propose that the reflooding of the Mediterranean Basin by Atlantic waters occurred at ca. 5.46 Ma. about 130 kyr before the Zanclean GSSP (5.332 Ma).	[Popescu, Speranta-Maria] Univ Bretagne Occidentale, Inst Univ Europeen Mer, UMR 6538, F-29280 Plouzane, France; [Dalesme, Florent] Univ Lyon 1, UFR Sci Terre, F-69622 Villeurbanne, France; [Jouannic, Gwenael] Univ Paris 11, UMR 8148, Lab Interact & Dynam Environm Surface, F-91405 Orsay, France; [Suc, Jean-Pierre] Univ Lyon 1, CNRS, PEPS, UMR 5125, F-69622 Villeurbanne, France; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada; [Melinte-Dobrinescu, Mihaela Carmen] Natl Inst Marine Geol & Geoecol, Bucharest 024053, Romania; [Sueto-Szentai, Maria] Nat Hist Collect Komlo, H-7300 Komlo, Hungary; [Bakrac, Koraljka] CGS, HGI, Zagreb 10000, Croatia; [Clauzon, Georges] Univ Paul Cezanne, CNRS, CEREGE, UMR 6635, F-13545 Aix En Provence 04, France	Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite de Bretagne Occidentale; Institut Universitaire Europeen de la Mer (IUEM); Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); CNRS - National Institute for Earth Sciences & Astronomy (INSU); Universite Paris Saclay; Universite Claude Bernard Lyon 1; Centre National de la Recherche Scientifique (CNRS); Brock University; National Institute of Marine Geology & Geoecology of Romania (GeoEcoMar); Universite PSL; College de France; Aix-Marseille Universite; Centre National de la Recherche Scientifique (CNRS); Institut de Recherche pour le Developpement (IRD)	Popescu, SM (通讯作者)，Univ Bretagne Occidentale, Inst Univ Europeen Mer, UMR 6538, 1 Pl Nicolas Copernic, F-29280 Plouzane, France.	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Chemistry and Biology, P364; WELCH BL, 1947, BIOMETRIKA, V34, P28, DOI 10.1093/biomet/34.1-2.28	111	67	67	0	12	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2009	33		2				105	134		10.1080/01916122.2009.9989688	http://dx.doi.org/10.1080/01916122.2009.9989688			30	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	551JL					2025-03-11	WOS:000274204000011
J	Marret, F; Kim, SY				Marret, Fablenne; Kim, So-Young			<i>OPERCULODINIUM AGUINAWENSE</i> SP NOV., A DINOFLAGELLATE CYST FROM THE LATE PLEISTOCENE AND RECENT SEDIMENTS OF THE EAST EQUATORIAL ATLANTIC OCEAN	PALYNOLOGY			English	Article						dinoflagellate cysts; Pleistocene-Holocene; taxonomy; Gulf of Guinea; river discharge	RECENT MARINE-SEDIMENTS; SEA-SURFACE CONDITIONS; COASTAL WATERS; NORTH-ATLANTIC; ADJACENT SEAS; INDIAN-OCEAN; ASSEMBLAGES; RECONSTRUCTION; DISTRIBUTIONS; ENVIRONMENTS	An organic-walled dinoflagellate cyst, Operculodinium aguinawense sp. nov. is described from recent marine sediments in Biafra Bay, Gulf of Guinea, Atlantic Ocean. This species is characterized by a subspheroidal, egg-shaped cyst body with a fibroreticulate surface wall, and flexible to stout processes with wide, fibrous bases and multifurcate terminations. Paratabulation is only expressed by the loss of a single precingular paraplate (3 ''). The distribution of this form in recent marine sediments suggests an affinity for lower salinity conditions (29) and as such, it could be an index of palcosalinity changes. Marine palynomorph records from the Gulf of Guinea document its occurrence from at least the Last Interglacial. Fluctuations in abundance appear to be associated with periods of strengthened monsoon dynamics and river discharge.	[Marret, Fablenne] Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England; [Kim, So-Young] Korea Ocean Res & Dev Inst, S Sea Res Inst, Gyeongsangnam Do 656830, South Korea	University of Liverpool; Korea Institute of Ocean Science & Technology (KIOST)	Marret, F (通讯作者)，Univ Liverpool, Dept Geog, Liverpool L69 7ZT, Merseyside, England.	f.marret@liv.ac.uk	Kim, So-Young/JFS-7698-2023	Marret-Davies, Fabienne/0000-0003-4244-0437				BOLCH CJ, 1990, BOT MAR, V33, P173, DOI 10.1515/botm.1990.33.2.173; Cho HJ, 2003, BOT MAR, V46, P332, DOI 10.1515/BOT.2003.030; Conkright M., 2002, NUTRIENTS; Dale B, 2002, PALAEOGEOGR PALAEOCL, V185, P309, DOI 10.1016/S0031-0182(02)00380-2; 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; Dupont LM, 1996, VEG HIST ARCHAEOBOT, V5, P273; FENSOME R. 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J	Quattrocchio, ME				Quattrocchio, Mirta E.			PALEOGENE DINOFLAGELLATE CYSTS FROM PUNTA PRAT, SOUTHERN CHILE	PALYNOLOGY			English	Article						Paleogene; dinoflagellate cysts; biostratigraphy; Punta Prat; Chile		Paleogene dinoflagellate cysts were recorded from the Chorrillo Chico and Agua Fresca formations at Punta Prat. southern Chile. Due to the presence of Palaeoperidinium pyrophorum, the Chorrillo Chico Formation is no younger than Late Selandian. By comparison with other basins, a Late Danian to Late Selandian age is proposed for the Chorrillo Chico Formation at Punta Prat. The Paleocene-Eocene boundary is characterized by Apectodinium-dominated assemblages in the mid and high latitudes, the Atlantic coast of Isla Grande de Tierra del Fuego in Argentina, and Chile. The absence of this event at Punta Prat suggests a regional hiatus across the Paleocene-Eocene boundary. An Early to Middle Eocene age is assigned to the lower part of the Agua Fresca Formation by comparison with dinoflagellate cyst assemblages from elsewhere in the Southern Hemisphere.	Univ Nacl Sur, Dept Geol, RA-8000 Bahia Blanca, Buenos Aires, Argentina	National University of the South; Instituto de Investigaciones en Ingenieria Electrica (IIIE)	Quattrocchio, ME (通讯作者)，Univ Nacl Sur, Dept Geol, San Juan 670, RA-8000 Bahia Blanca, Buenos Aires, Argentina.	mquattro@criba.edu.ar			Agencia Nacional de Promocion Cientifica y Tecnologica (FONCYT); Consejo Nacional de Investigaciones Cientfficas y Tecnicas (CONICET); Universidad Nacional del Sur, Bahia Blanca, Argentina	Agencia Nacional de Promocion Cientifica y Tecnologica (FONCYT)(ANPCyTFONCyT); Consejo Nacional de Investigaciones Cientfficas y Tecnicas (CONICET)(Consejo Nacional de Investigaciones Cientificas y Tecnicas (CONICET)); Universidad Nacional del Sur, Bahia Blanca, Argentina	This paper is dedicated to Dr William A.S. Sarjeant (1935-2002). It was funded by the Agencia Nacional de Promocion Cientifica y Tecnologica (FONCYT), Consejo Nacional de Investigaciones Cientfficas y Tecnicas (CONICET) and the Secretaria de Ciencia y Tecnica of the Universidad Nacional del Sur, Bahia Blanca, Argentina. Many thanks go to Dr Hamid Slimani for his review of the manuscript and Drs Norberto Malumian and Eduardo Olivero for their valuable comments. Help in sample preparation from Mrs Ngat-Mee Choo of the University of Saskatchewan, Canada is gratefully acknowledged. Drs Claus Heilmann-Clausen and A. James Powell are thanked for their critical comments and constructive advice for improvement of the initial submission.	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J	De Schepper, S; Head, MJ				De Schepper, Stijn; Head, Martin J.			PLIOCENE AND PLEISTOCENE DINOFLAGELLATE CYST AND ACRITARCH ZONATION OF DSDP HOLE 610A, EASTERN NORTH ATLANTIC	PALYNOLOGY			English	Article						organic-walled dinoflagellate cysts; acritarchs; Quaternary; Neogene; North Atlantic; biostratigraphy; taxonomy	ROCKALL PLATEAU; HEMISPHERE GLACIATIONS; SEA BASIN; BIOSTRATIGRAPHY; STRATIGRAPHY; BELGIUM; ENGLAND; OCEAN; PALEOECOLOGY; DEFINITION	A diverse and well-preserved dinoflagellate cyst and acritarch record, comprising 35 genera and 104 species of dinoflagellate cyst and 14 acritarch taxa, is presented for the Lower Pliocene through Middle Pleistocene (4.00-0.53 Ma) of eastern North Atlantic Deep Sea Drilling Project Hole 610A. The Pliocene samples contain twice as many dinoflagellate cyst taxa than the Quaternary samples but far lower cyst concentrations. The disappearance of taxa during the latest Pliocene is likely to have been associated with global cooling. Eight biozones and four subzones are established, representing a level of detail that surpasses earlier studies. The zones are based mostly on highest occurrences, as these are most prevalent in the Pliocene and Lower Pleistocene. The subzones, based on both the acme and highest persistent occurrence of Habibacysta tectata, appear regionally useful within the Lower Pleistocene. The lowest occurrence of Impagidinium cantabrigiense is a potential marker for the uppermost Gelasian Stage (Lower Pleistocene). While this biozonation is intended primarily for use in the eastern North Atlantic, elements will be applicable across the higher-latitude North Atlantic where calcareous microfossil zonations have reduced reliability and resolution. Most of the stratigraphically useful taxa are illustrated, and selected species are described informally.	[De Schepper, Stijn] Univ Bremen, Fachbereich Geowissensch, D-28334 Bremen, Germany; [Head, Martin J.] Brock Univ, Dept Earth Sci, St Catharines, ON L2S 3A1, Canada	University of Bremen; Brock University	De Schepper, S (通讯作者)，Univ Bremen, Fachbereich Geowissensch, Postfach 330 440, D-28334 Bremen, Germany.	sdeschepper@uni-bremen.de; mjhead@brocku.ca	De Schepper, Stijn/A-2836-2011	De Schepper, Stijn/0000-0002-6934-0914	Gates Cambridge Scholarship (University of Cambridge); Royal Society); Philip Lake Fund (Department of Geography, University of Cambridge); MARUM; DFG International Graduate College 'Proxies in Earth History' (EUROPROX); Palynology Oil Company Consortium (Unocal, Phillips, Amoco, Statoil, NorskHydro, and Elf-Aquitaine); Natural Sciences and Engineering Research Council of Canada	Gates Cambridge Scholarship (University of Cambridge)(University of Cambridge); Royal Society)(Royal Society); Philip Lake Fund (Department of Geography, University of Cambridge)(University of Cambridge); MARUM; DFG International Graduate College 'Proxies in Earth History' (EUROPROX)(German Research Foundation (DFG)); Palynology Oil Company Consortium (Unocal, Phillips, Amoco, Statoil, NorskHydro, and Elf-Aquitaine); Natural Sciences and Engineering Research Council of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)CGIAR)	This contribution is based partly on the doctoral research of Stijn De Schepper who is grateful to the Gates Cambridge Trust for the award of a Gates Cambridge Scholarship (University of Cambridge), and additional funding from the Dudley Stamp Memorial Trust (Royal Society), and the Philip Lake Fund (Department of Geography, University of Cambridge). Stijn De Schepper is also grateful for support from MARUM (G. Wefer) and the DFG International Graduate College 'Proxies in Earth History' (EUROPROX) at the University of Bremen. Martin J. Head acknowledges support from the Palynology Oil Company Consortium (Unocal, Phillips, Amoco, Statoil, NorskHydro, and Elf-Aquitaine) for the initial research on Hole 61 OA, and from a Natural Sciences and Engineering Research Council of Canada Discovery Grant. Colleagues at the Palaeontology Research Unit, University of Ghent, are thanked for the the use of the SEM and transmitted light microscopes. We thank the Ocean Drilling Program for providing the samples. Constructivereviews by Dirk Munsterman and Stefan Piasecki are greatly appreciated.	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B., 1976, Initial Rep Deep Sea Drilling Project, V38, P897; Marret F, 2003, REV PALAEOBOT PALYNO, V125, P1, DOI 10.1016/S0034-6667(02)00229-4; MATSUOKA K, 1987, MICROPALEONTOLOGY, V33, P214, DOI 10.2307/1485638; MATSUOKA K, 1983, Palaeontographica Abteilung B Palaeophytologie, V187, P89; McMinn A., 1992, NEOGENE QUATERNARY D, P147; McMinn Andrew, 1994, Palynology, V18, P41; Mudie P.J., 1989, Proceedings of the Ocean Drilling Program Scientific Results, V104, P587, DOI 10.2973/odp.proc.sr.104.174.1989; MUDIE PJ, 1987, INITIAL REP DEEP SEA, V94, P785; PIASECKI S, 1980, Bulletin of the Geological Society of Denmark, V29, P53; Piasecki S, 2003, MAR PETROL GEOL, V20, P1075, DOI 10.1016/S0264-8172(02)00089-2; Piasecki S, 2002, MAR PETROL GEOL, V19, P55, DOI 10.1016/S0264-8172(01)00053-8; Powell A.J., 1992, P155; RUDDIMAN WF, 1987, DEEP SEA DRILLING PR, V94, P351; Salvador A., 1994, Geological Society of America, P1; SHACKLETON NJ, 1984, INITIAL REP DEEP SEA, V81, P599, DOI 10.2973/dsdp.proc.81.116.1984; Smelror Morton, 1999, Proceedings of the Ocean Drilling Program Scientific Results, V162, P83; STOCKMARR J, 1971, Pollen et Spores, V13, P615; TAKAYAMA T, 1987, INITIAL REP DEEP SEA, V94, P651; Udeze CU, 2005, PALAEOGEOGR PALAEOCL, V219, P199, DOI 10.1016/j.palaeo.2004.12.026; Versteegh GJM, 1997, MAR MICROPALEONTOL, V30, P319, DOI 10.1016/S0377-8398(96)00052-7; VERSTEEGH GJM, 1995, THESIS U UTRECHT NET; Vink A, 2000, REV PALAEOBOT PALYNO, V112, P247, DOI 10.1016/S0034-6667(00)00046-4; WALL D, 1966, NATURE, V211, P1025, DOI 10.1038/2111025a0; WEAVER PPE, 1987, INITIAL REP DEEP SEA, V94, P815; Williams G.L., 2004, Proceedings of the Ocean Drilling Program Scientific Results, V189, P1; WILLIAMS GL, 1975, GEOLOGICAL SURVEY CA, V7430, P107; Williams GL., 1977, American Association of Stratigraphic Palynologists Contribution Series A, V5, P14; WILSON GJ, 1973, NEW ZEAL J GEOL GEOP, V16, P345, DOI 10.1080/00288306.1973.10431363; Wrenn J.H., 1986, Amer. Assoc. Strat. Palynologists Contribution Series, V17, P169; Zachos JC, 2008, NATURE, V451, P279, DOI 10.1038/nature06588	72	46	46	0	6	TAYLOR & FRANCIS INC	PHILADELPHIA	530 WALNUT STREET, STE 850, PHILADELPHIA, PA 19106 USA	0191-6122	1558-9188		PALYNOLOGY	Palynology		2009	33		1				179	218						40	Plant Sciences; Paleontology	Science Citation Index Expanded (SCI-EXPANDED)	Plant Sciences; Paleontology	551JJ					2025-03-11	WOS:000274203800010
S	Lami, A; Musazzi, S; Marchetto, A; Buchaca, T; Kernan, M; Jeppesen, E; Guilizzoni, P		Catalan, J; Curtis, CJ; Kernan, M		Lami, Andrea; Musazzi, Simona; Marchetto, Aldo; Buchaca, Teresa; Kernan, Martin; Jeppesen, Erik; Guilizzoni, Piero			Sedimentary pigments in 308 alpine lakes and their relation to environmental gradients	PATTERNS AND FACTORS OF BIOTA DISTRIBUTION IN REMOTE EUROPEAN MOUNTAIN LAKES	Advances in Limnology		English	Article; Book Chapter						carotenoids; canonical analysis; alpine lakes; EMERGE	CHRYSOPHYTE CYST ASSEMBLAGES; FOSSIL PIGMENTS; MOUNTAIN LAKES; WATER-QUALITY; QUANTITATIVE INDICATORS; MODERN DIATOM; CAROTENOIDS; PHYTOPLANKTON; CLIMATE; ALPS	We undertook a comprehensive comparison between the pigment composition of surface sediment samples and contemporary catchment and limnological data deriving from 308 mountain lakes in I I mountain regions (Lake Districts) covering a wide latitudinal and longitudinal gradient across Europe. This paper examines whether photosynthetic algal and bacterial pigments stored in the lake sediment can be used to identify different lake typologies and population dynamics of primary producers. We focus on a multivariate numerical analysis relating the relative abundance of marker pigments of algae, cyanobacteria and phototrophic sulphur bacteria to a set of physical and chemical factors (both natural and anthropogenic) determining the environmental conditions in mountain lakes. Redundancy Analysis (RDA), including partial RDA, of carotenoid assemblages constrained by environmental variables suggests that the main differences between lake districts are caused by geographic position (e.g. longitude), catchment characteristics (e.g. % carbonate rocks) and chemical variables (e.g. Mg, NO3). Other variables such as temperature and phosphorus play a minor role, probably because of the short length of the gradient covered by these cold and mostly oligotrophic lakes. Pigment composition varies primarily in response to catchment geology and pollution (i.e. acidification from long range transport) gradients. Purple sulphur photosynthetic bacteria (okenone) and cyanobacteria (echinenone, canthaxanthin, scytonemin) are replaced by siliceous algae (fucoxanthin and diatoxanthin), cryptophytes (alloxanthin) and dinoflagellates (diadinoxanthin). With respect to site classification, the pigment ordination shows a clear distinction between the more pristine lakes (in the Pyrenees) and the more polluted sites (in the Tatra Mountains and Central Southern Alps) or those with water higher in solute content (the Julian Alps and Greenland).	[Lami, Andrea; Musazzi, Simona; Marchetto, Aldo; Guilizzoni, Piero] CNR, Ist Studio Ecosistemi, Verbania, Italy; [Buchaca, Teresa] Ctr Estudis Avancats Blanes Ceab, CSIC, Blanes, Spain; [Kernan, Martin] UCL, Environm Change Res Ctr, London, England; [Jeppesen, Erik] Natl Environm Res Inst, Dept Freshwater Ecol, Silkeborg, Denmark	Consiglio Nazionale delle Ricerche (CNR); Istituto per lo Studio degli Ecosistemi (ISE-CNR); Consejo Superior de Investigaciones Cientificas (CSIC); CSIC - Centre d'Estudis Avancats de Blanes (CEAB); University of London; University College London; Aarhus University; Danish National Environmental Research Institute	Lami, A (通讯作者)，CNR, Ist Studio Ecosistemi, Verbania, Italy.	a.lami@ise.cnr.it	Lami, Andrea/M-3982-2019; Jeppesen, Erik/O-2667-2019; Marchetto, Aldo/H-3258-2013; Jeppesen, Erik/A-4463-2012; Lami, Andrea/F-1415-2013; Musazzi, Simona/AGR-3253-2022; Buchaca, Teresa/L-1679-2014	Marchetto, Aldo/0000-0002-1033-4114; Jeppesen, Erik/0000-0002-0542-369X; Lami, Andrea/0000-0003-3627-0363; Musazzi, Simona/0000-0001-5549-0084; Buchaca, Teresa/0000-0001-7933-8992				[Anonymous], 1988, J ANAL PURIF; [Anonymous], 1976, CAROTENOIDS, DOI DOI 10.1590/S0101-20612001000200017; [Anonymous], J LIMNOLOGY; Battarbee Richard W., 1999, P85; Battarbee RW, 2002, J PALEOLIMNOL, V28, P1, DOI 10.1023/A:1020342316326; Battarbee RW, 2002, J PALEOLIMNOL, V28, P161, DOI 10.1023/A:1020384204940; BATTARBEE RW, 1995, P SETAC C COP 25 28; BOURCART FE, 1906, LACS ALPINE SUISSES; Brown SR, 1984, SIL Proceedings, V22, P1357, DOI DOI 10.1080/03680770.1983.11897499; Bryce SA, 1996, ENVIRON MANAGE, V20, P297, DOI 10.1007/BF01203839; Buchaca T, 2008, J PALEOLIMNOL, V40, P369, DOI 10.1007/s10933-007-9167-1; Buchaca T, 2007, FRESHWATER BIOL, V52, P1365, DOI 10.1111/j.1365-2427.2007.01774.x; DEMARCHI M, 1913, ATTI SOC ITAL SC NAT, V51, P207; GELETA S, 1994, J ENVIRON QUAL, V23, P36, DOI 10.2134/jeq1994.00472425002300010007x; Goodwin T.W., 1980, The Biochemistry of the Carotenoids, VI, P377; GUILIZZONI P, 1983, HYDROBIOLOGIA, V103, P103, DOI 10.1007/BF00028436; Guilizzoni P, 2006, HYDROBIOLOGIA, V562, P167, DOI 10.1007/s10750-005-1810-0; GUILIZZONI P, 1986, HYDROBIOLOGIA, V143, P321, DOI 10.1007/BF00026677; GUILIZZONI P, 1992, MEM I ITAL IDROBIOL, V50, P61; GUILIZZONI P, 2001, ENCY ENV MICROBIOLOG, V6, P2306; Hodgson DA, 2004, AQUAT MICROB ECOL, V37, P247, DOI 10.3354/ame037247; Jeffrey S.W., 1997, PHYTOPLANKTON PIGMEN, V10, P595; Jenerette GD, 2002, ENVIRON MANAGE, V29, P67, DOI 10.1007/s00267-001-0041-z; Jeppesen E, 2001, TRENDS ECOL EVOL, V16, P191, DOI 10.1016/S0169-5347(01)02100-0; Jeppesen E, 2003, HYDROBIOLOGIA, V491, P321, DOI 10.1023/A:1024488525225; JOHANNESSEN M, 1990, P CEC PALL JUN 20 22; KERNAN M, 2009, FUNDAM APPL LIMNOL A, V62, P3; LAMI A, 2000, J LIMNOL, V59, P119; Leavitt P.R., 2001, TRACKING ENV CHANGE, V3; Leavitt Peter R., 1993, Journal of Paleolimnology, V9, P109, DOI 10.1007/BF00677513; Leavitt PR, 1997, NATURE, V388, P457, DOI 10.1038/41296; LEGENDRE L., 1983, NUMERICAL ECOLOGY; LIAAENJENSEN S, 1979, PURE APPL CHEM, V51, P661, DOI 10.1351/pac197951030661; Livingstone DM, 2001, LIMNOL OCEANOGR, V46, P1220, DOI 10.4319/lo.2001.46.5.1220; Lotter AF, 1998, J PALEOLIMNOL, V19, P443, DOI 10.1023/A:1007994206432; Lotter AF, 1997, J PALEOLIMNOL, V18, P395, DOI 10.1023/A:1007982008956; Lovejoy SB, 1997, J SOIL WATER CONSERV, V52, P18; MANTOURA RFC, 1983, ANAL CHIM ACTA, V151, P297, DOI 10.1016/S0003-2670(00)80092-6; OMERNIK JM, 1991, ENVIRON MANAGE, V15, P281, DOI 10.1007/BF02393860; Omernik JM, 1997, J AM WATER RESOUR AS, V33, P935, DOI 10.1111/j.1752-1688.1997.tb04115.x; Patrick S, 1998, IAHS-AISH P, P403; PETERJOHN WT, 1984, ECOLOGY, V65, P1466, DOI 10.2307/1939127; SANGER JE, 1988, PALAEOGEOGR PALAEOCL, V62, P343, DOI 10.1016/0031-0182(88)90061-2; Shirmohammadi A, 1997, T ASAE, V40, P1563, DOI 10.13031/2013.21420; SUMMER RM, 1990, J ENVIRON QUAL, V9, P421; SWAIN EB, 1985, FRESHWATER BIOL, V15, P53, DOI 10.1111/j.1365-2427.1985.tb00696.x; ter Braak C.J. F., 1988, CANOCO REFERENCE MAN; Vinebrooke RD, 1998, CAN J FISH AQUAT SCI, V55, P668, DOI 10.1139/cjfas-55-3-668; WRIGHT SW, 1991, MAR ECOL PROG SER, V77, P183, DOI 10.3354/meps077183; ZSCHOKKE F, 1894, REV SUISSE ZOOL, V2, P349; ZULLIG H, 1982, SCHWEIZ Z HYDROL, V44, P1, DOI 10.1007/BF02502191	51	19	21	0	11	E SCHWEIZERBART'SCHE VERLAGSBUCHHANDLUNG	STUTTGART	JOHANNESTRASSE 3, W-7000 STUTTGART, GERMANY	1612-166X		978-3-510-47064-8	ADV LIMNOL	Adv. Limnol.		2009	62						247	268				10.1007/978-1-84882-229-0		22	Limnology	Book Citation Index– Science (BKCI-S)	Marine & Freshwater Biology	BMX02					2025-03-11	WOS:000273782900011
J	Egger, H; Koeberl, C; Wagreich, M; Stradner, H				Egger, Hans; Koeberl, Christian; Wagreich, Michael; Stradner, Herbert			The Cretaceous-Paleogene (K/Pg) boundary at Gams, Austria: Nannoplankton stratigraphy and geochemistry of a bathyal northwestern Tethyan setting	STRATIGRAPHY			English	Article							NORTHERN CALCAREOUS ALPS; TRANSITIONAL CLAY LAYER; CHICXULUB IMPACT EVENT; TERTIARY BOUNDARY; EASTERN ALPS; GEODYNAMIC EVOLUTION; NANNOFOSSIL; PALEOCENE; SURVIVORSHIP; EXTINCTION	In the area east of Gains (Styria, Austria), the Cretaceous/Paleogene boundary has been recognized in a newly discovered section, which comprises the upper part of the Cretaceous Nephrolithus frequens Zone (CC26) and the lower part of the Paleocene Markalius inversus Zone (NP1). The 6.5m long section is part of the Nierental Formation of the Gosau Group of the Northern Calcareous Alps. The boundary is characterized by (1) all enrichment of the contents of the siderophile elements It, Co, Ni, and Cr compared to the background and continental crustal values, (2) a sudden decrease of carbon and oxygen isotope Values, (3) a sudden decrease of carbonate content, and (4) an acme of the calcareous dinoflagellate cyst Operculodinella operculata, which is Succeeded by all acme of the small coccolith species Neobiscutum parvulum. The Neobiscutum acme is associated with a positive excursion of delta O-18 indicating a transient cooling of ocean Surface waters due to short-lived changes in the configuration of ocean circulation after the impact.	[Egger, Hans; Stradner, Herbert] Geol Survey Austria, A-1030 Vienna, Austria; [Koeberl, Christian] Univ Vienna, Dept Lithospher Res, A-1090 Vienna, Austria; [Wagreich, Michael] Univ Vienna, Dept Geodynam & Sedimentol, A-1090 Vienna, Austria	University of Vienna; University of Vienna	Egger, H (通讯作者)，Geol Survey Austria, Neulinggasse 38, A-1030 Vienna, Austria.	hans.egger@geologie.ac.at; christian.koeberl@univie.ac.at; michael.wagreich@univie.ac.at	Wagreich, Michael/D-2279-2013	Wagreich, Michael/0000-0002-8828-0857; Koeberl, Christian/0000-0001-5155-7405	Austrian Science Foundation FWF [P18862-N10, AJS308-B17]; IGCP [555]; Austrian Science Fund (FWF) [AJS308, P18862] Funding Source: Austrian Science Fund (FWF)	Austrian Science Foundation FWF(Austrian Science Fund (FWF)); IGCP; Austrian Science Fund (FWF)(Austrian Science Fund (FWF))	The authors are grateful to Marie-Pierre Aubry and Werner E. Piller whose critical and constructive reviews improved this manuscript. Thanks are due to Helga Priewalder for taking the SEM-pictures. Peter Klein for providing total organic carbon values. Sabine Hruby-Nichtenberger for providing carbonate values, Helmut Keupp for information on the wall structures of dinoflagellates and Christoph Spotl for determining stable isotope values. CK is Supported by the Austrian Science Foundation FWF (grant P18862-N10). MW is supported by IGCP 555 and Austrian Science Foundation FWF (grant AJS308-B17)..	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J	Sluijs, A; Brinkhuis, H; Crouch, EM; John, CM; Handley, L; Munsterman, D; Bohaty, SM; Zachos, JC; Reichart, GJ; Schouten, S; Pancost, RD; Damsté, JSS; Welters, NLD; Lotter, AF; Dickens, GR				Sluijs, Appy; Brinkhuis, Henk; Crouch, Erica M.; John, Cedric M.; Handley, Luke; Munsterman, Dirk; Bohaty, Steven M.; Zachos, James C.; Reichart, Gert-Jan; Schouten, Stefan; Pancost, Richard D.; Damste, Jaap S. Sinninghe; Welters, Natasja L. D.; Lotter, Andre F.; Dickens, Gerald R.			Eustatic variations during the Paleocene-Eocene greenhouse world	PALEOCEANOGRAPHY			English	Review							SEA-LEVEL HISTORY; THERMAL MAXIMUM; DINOFLAGELLATE CYSTS; NEW-JERSEY; CONTINENTAL-MARGIN; COASTAL-PLAIN; NEW-ZEALAND; METHANE HYDRATE; LONG-TERM; NORTH	We reconstruct eustatic variations during the latest Paleocene and earliest Eocene (similar to 58-52 Ma). Dinoflagellate cysts, grain size fractions, and organic biomarkers in marine sections at four sites from three continents indicate an increased distance to the coast during the Paleocene-Eocene thermal maximum (PETM). The same trend is recognized in published records from other sites around the world. Together, the data indicate a eustatic rise during the PETM, beginning 20 to 200 ka before the globally recorded negative carbon isotope excursion (CIE) at similar to 55.5 Ma. Although correlations are tentative, we recognize other global transgressions during Chrons C25n and C24n. The latter may be associated with Eocene Thermal Maximum 2 (similar to 53.5 Ma) or the "X''-event (similar to 52 Ma). These results suggest a link between global sea level and "hyperthermal'' intervals, potentially because of the melting of small alpine ice sheets on Antarctica, thermal expansion of seawater, or both. However, the early onset of sea level rise relative to the CIE of the PETM suggests contributions from other mechanisms, perhaps decreasing ocean basin volume, on sea level rise.	[Sluijs, Appy; Brinkhuis, Henk; Welters, Natasja L. D.; Lotter, Andre F.] Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, NL-3584 CD Utrecht, Netherlands; [John, Cedric M.; Bohaty, Steven M.; Zachos, James C.] Univ Calif Santa Cruz, Dept Earth & Planetary Sci, Santa Cruz, CA 95060 USA; [Crouch, Erica M.] GNS Sci, Lower Hutt, New Zealand; [Schouten, Stefan; Damste, Jaap S. Sinninghe] Royal Netherlands Inst Sea Res, Dept Marine Biogeochem & Toxicol, NL-1790 AB Den Burg, Texel, Netherlands; [Dickens, Gerald R.] Rice Univ, Dept Earth Sci, Houston, TX 77005 USA; [Handley, Luke; Pancost, Richard D.] Univ Bristol, Sch Chem, Organ Geochem Unit, Biogeochem Res Ctr, Bristol BS8 1TS, Avon, England; [Munsterman, Dirk] TNO, Natl Geol Survey, Netherlands Inst Appl Geosci, NL-3508 TA Utrecht, Netherlands; [Reichart, Gert-Jan] Univ Utrecht, Dept Earth Sci, NL-3584 CD Utrecht, Netherlands	Utrecht University; University of California System; University of California Santa Cruz; GNS Science - New Zealand; Utrecht University; Royal Netherlands Institute for Sea Research (NIOZ); Rice University; University of Bristol; Netherlands Organization Applied Science Research; Utrecht University	Sluijs, A (通讯作者)，Univ Utrecht, Inst Environm Biol, Palaeobot & Palynol Lab, Budapestlaan 4, NL-3584 CD Utrecht, Netherlands.	a.sluijs@uu.nl	John, Cedric/B-3292-2008; Crouch, Erica/C-2820-2013; Schouten, Stefan/P-4380-2016; Brinkhuis, Henk/B-4223-2009; Dickens, Gerald/G-1222-2011; Sinninghe Damste, Jaap/F-6128-2011; Lotter, Andre F./C-3477-2008; Sluijs, Appy/B-3726-2009; Reichart, Gert-Jan/N-6308-2018; Zachos, James/A-7674-2008	Sinninghe Damste, Jaap/0000-0002-8683-1854; Lotter, Andre F./0000-0002-2954-8809; Sluijs, Appy/0000-0003-2382-0215; Brinkhuis, Henk/0000-0003-0253-6610; Dickens, Gerald/0000-0003-2869-4860; Pancost, Richard/0000-0003-0298-4026; Reichart, Gert-Jan/0000-0002-7256-2243; John, Cedric/0000-0001-9711-1548; Zachos, James/0000-0001-8439-1886	Netherlands Organisation for Scientific Research [863.07.001]; NSF [EAR-0628719]	Netherlands Organisation for Scientific Research(Netherlands Organization for Scientific Research (NWO)); NSF(National Science Foundation (NSF))	This research used samples and/or data provided by the Integrated Ocean Drilling Program (IODP). Appy Sluijs thanks the Utrecht Center of Biogeology, the LPP Foundation, Utrecht University, and the Netherlands Organisation for Scientific Research (NWO; VENI grant 863.07.001) for funding. This research was supported by NSF grant EAR-0628719 to Zachos. Richard Pancost and Luke Handley acknowledge support from the NERC for funding Handley's Ph. D. studentship. Appy Sluijs, Henk Brinkhuis, Dirk Munsterman, Gert-Jan Reichart, Stefan Schouten, Jaap Sinninghe Damste, Natasja Welters, and Andre Lotter thank NWO for their continued support of the IODP. We thank Debbie Thomas and an anonymous reviewer for constructive reviews and James Browning, Ben Cramer, Matt Huber, Luc Lourens, Ken Miller, Dietmar Muller, and Michelle Kominz for discussions.	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J	Richerol, T; Rochon, A; Blasco, S; Scott, DB; Schell, TM; Bennett, RJ				Richerol, Thomas; Rochon, Andre; Blasco, Steve; Scott, Dave B.; Schell, Trecia M.; Bennett, Robbie J.			Distribution of dinoflagellate cysts in surface sediments of the Mackenzie Shelf and Amundsen Gulf, Beaufort Sea (Canada)	JOURNAL OF MARINE SYSTEMS			English	Article						Arctic; Dinoflagellate cysts; Beaufort Sea; Mackenzie Shelf; Amundsen Gulf; Surface sediments; Palynology; Climate; Sea-ice cover; Global warming	HYDROGRAPHIC CONDITIONS; LATE QUATERNARY; PRODUCTIVITY; PHYTOPLANKTON; ASSEMBLAGES; INDICATORS; CHUKCHI; WATER; TRACERS; BUDGET	In order to document long-tern climate cycles and predict future climate trends for the Arctic, we need to look at the geological records to establish the link between historical and pre-historical sea-surface parameters. Dinoflagellate cysts (dinocysts) are used as proxy indicators of sea-surface parameters (temperature, salinity, sea-ice cover, primary productivity) jointly with transfer functions and a modern dinocyst reference database, to reconstruct the evolution of sea-surface conditions at decadal and millennial timescales. Here we present the surface distribution of recent dinocyst assemblages from 34 surface sediment samples collected on the Mackenzie Slope/Amundsen Gulf during the 2004 CASES (Canadian Arctic Shelf Exchange Study) cruise. Dinocyst concentrations in surface sediments are relatively high outside the Mackenzie plume area and increase gradually eastward toward Amundsen Gulf. The cysts of autotrophic dinoflagellates are dominant throughout the study area, while the maximum abundance of heterotrophic taxa is found within the Mackenzie plume. Hierarchical clustering analyses allowed defining two dinocyst assemblages. Assemblage I is located on the Mackenzie Slope and southern Amundsen Gulf, while Assemblage 11 is located within the Cape Bathurst Polynya area in northern Amundsen Gulf. Both assemblages are dominated by Operculodinium centmcarpum, but are distinguished on the basis of the relative abundance of Islandinium minutum, a taxon generally associated with sea ice. I. minutum is found in lower abundance in the Cape Bathurst Polynya. (C) 2007 Elsevier B.V. All rights reserved.	[Richerol, Thomas; Rochon, Andre] UQAR ISMER, Rimouski, PQ G5L 3A1, Canada; [Blasco, Steve; Bennett, Robbie J.] Fisheries & Oceans Canada, Bedford Inst Oceanog, Dartmouth, NS B2Y 4A2, Canada; [Scott, Dave B.; Schell, Trecia M.] Dalhousie Univ, Ctr Environm & Marine Geol, Halifax, NS B3H 3J5, Canada	University of Quebec; Universite du Quebec a Rimouski; Bedford Institute of Oceanography; Fisheries & Oceans Canada; Dalhousie University	Richerol, T (通讯作者)，UQAR ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	thomas.richerol@uqar.qc.ca	RICHEROL, Thomas/G-4598-2017	RICHEROL, Thomas/0000-0001-5295-0022				[Anonymous], ARCTIC OCEAN REGION; [Anonymous], POLAR BIOL; Arrigo KR, 2004, GEOPHYS RES LETT, V31, DOI 10.1029/2003GL018978; Aziz OIA, 2006, J HYDROL, V319, P282, DOI 10.1016/j.jhydrol.2005.06.039; Boessenkool KP, 2001, J QUATERNARY SCI, V16, P661, DOI 10.1002/jqs.654; Carmack EC, 2004, MAR ECOL PROG SER, V277, P37, DOI 10.3354/meps277037; Clarke K.R., 2001, PRIMER V5 USER MANUA; Cremer H, 1998, REP POLAR RES, V260, P1; de Vernal A, 2001, J QUATERNARY SCI, V16, P681, DOI 10.1002/jqs.659; de Vernal A, 2005, QUATERNARY SCI REV, V24, P897, DOI 10.1016/j.quascirev.2004.06.014; de Vernal A., 1991, Canadian Special Publication of Fisheries and Aquatic Sciences, V113, P189; Dumas J, 2005, COLD REG SCI TECHNOL, V42, P41, DOI 10.1016/j.coldregions.2004.12.001; Fensome R.A, 2004, CONTRIBUTION SERIES, V42; GIOVANDO LF, 1981, PACIFIC MARINE SCI R, V81, P198; Grosfjeld K, 2001, J QUATERNARY SCI, V16, P651, DOI 10.1002/jqs.653; Hamel D, 2002, DEEP-SEA RES PT II, V49, P5277, DOI 10.1016/S0967-0645(02)00190-X; Head MJ, 2001, J QUATERNARY SCI, V16, P621, DOI 10.1002/jqs.657; Hill PR, 1996, CAN J EARTH SCI, V33, P1064, DOI 10.1139/e96-081; Hill PR, 2001, SEDIMENTOLOGY, V48, P1047, DOI 10.1046/j.1365-3091.2001.00408.x; HILL PR, 1991, CONT SHELF RES, V11, P821, DOI 10.1016/0278-4343(91)90081-G; Hill V, 2005, DEEP-SEA RES PT II, V52, P3369, DOI 10.1016/j.dsr2.2005.10.010; HILLAIREMARCEL C, 1994, CAN J EARTH SCI, V31, P139, DOI 10.1139/e94-012; Horner R., 1984, The Alaskan Beaufort Sea, P295; HSIAO SIC, 1977, CAN J BOT, V55, P685, DOI 10.1139/b77-083; JACOBSON DM, 1986, J PHYCOL, V22, P249, DOI 10.1111/j.1529-8817.1986.tb00021.x; JACOBSON DM, 1992, J PHYCOL, V28, P69, DOI 10.1111/j.0022-3646.1992.00069.x; Kunz-Pirrung M, 2001, J QUATERNARY SCI, V16, P637, DOI 10.1002/jqs.647; Lewis J., 1990, Proceedings of the Ocean Drilling Program, Scientific Results, V112, P323; MACDONALD RW, 1995, J GEOPHYS RES-OCEANS, V100, P895, DOI 10.1029/94JC02700; Macdonald RW, 1998, MAR GEOL, V144, P255, DOI 10.1016/S0025-3227(97)00106-0; MACNEILL MR, 1975, BEAUFORT SEA TECHNIC, V17, P113; Melling H, 2000, NATO SCI S PRT 2 ENV, V70, P479; Mudie PJ, 2001, J QUATERNARY SCI, V16, P603, DOI 10.1002/jqs.658; *NCDC, 1953, NAT OC ATM ADM NOAA; *NODC WORLD OC ATL, 2001, NAT OC ATM ADM; O'Brien MC, 2006, CONT SHELF RES, V26, P41, DOI 10.1016/j.csr.2005.09.007; PARSONS TR, 1989, POLAR BIOL, V9, P261, DOI 10.1007/BF00263774; PARSONS TR, 1988, POLAR BIOL, V8, P235, DOI 10.1007/BF00443455; Parsons TR., 1984, BIOL OCEANOGRAPHIC P, V2nd; Radi T, 2004, REV PALAEOBOT PALYNO, V128, P169, DOI 10.1016/S0034-6667(03)00118-0; Radi T, 2001, J QUATERNARY SCI, V16, P667, DOI 10.1002/jqs.652; Radi T, 2007, MAR MICROPALEONTOL, V62, P269, DOI 10.1016/j.marmicro.2006.09.002; ROCHON A, 1994, CAN J EARTH SCI, V31, P115, DOI 10.1139/e94-010; Rochon A., 1999, Surface Sediments From the North Atlantic Ocean and Adjacent Seas in Relation to Sea-Surface Parameters, V35; Rothrock DA, 1999, GEOPHYS RES LETT, V26, P3469, DOI 10.1029/1999GL010863; Stein R, 2004, ORGANIC CARBON CYCLE IN THE ARCTIC OCEAN, P169; Stein R., 2004, ORGANIC CARBON CYCLE, DOI [10.1007/978-3-642-18912-8, DOI 10.1007/978-3-642-18912-8, DOI 10.1007/978-3-642-18912-8_4]; VILKS G, 1979, GEOLOGICAL SURVEY CA, V303; Voronina E, 2001, J QUATERNARY SCI, V16, P717, DOI 10.1002/jqs.650; Wang J, 2005, DEEP-SEA RES PT II, V52, P3355, DOI 10.1016/j.dsr2.2005.10.014	50	42	50	0	12	ELSEVIER	AMSTERDAM	RADARWEG 29, 1043 NX AMSTERDAM, NETHERLANDS	0924-7963	1879-1573		J MARINE SYST	J. Mar. Syst.	DEC 1	2008	74	3-4			SI		825	839		10.1016/j.jmarsys.2007.11.003	http://dx.doi.org/10.1016/j.jmarsys.2007.11.003			15	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	385KF					2025-03-11	WOS:000261812400008
J	Rózanska, M; Poulin, M; Gosselin, M				Rozanska, Magdalena; Poulin, Michel; Gosselin, Michel			Protist entrapment in newly formed sea ice in the Coastal Arctic Ocean	JOURNAL OF MARINE SYSTEMS			English	Article						Protist; Entrapment; Newly formed sea ice; Arctic	ANTARCTIC PACK-ICE; GREENLAND SEA; COMMUNITY STRUCTURE; STANDING STOCK; BARENTS SEA; NORTH WATER; WEDDELL SEA; FRAZIL ICE; PHYTOPLANKTON; ALGAE	Protist abundance and taxonomic composition were determined in four development stages of newly formed sea ice (new ice, nilas, young ice and thin first-year ice) and in the underlying surface waters of the Canadian Beaufort Sea from 30 September to 19 November 2003. Pico- and nanoalgae were counted by flow cytometry whereas photosynthetic and heterotrophic protists >= 4 mu m were identified and counted by inverted microscopy. Protists were always present in sea ice and surface water samples throughout the study period. The most abundant protists in sea ice and surface waters were cells <4 mu m. They were less abundant in sea ice (418-3051 x 10(3) cells L(-1)) than in surface waters (1393-5373 x 10(3) cells L(-1)). In contrast, larger protists (>= 4 mu m) were more abundant in sea ice (59-821 x 10(3) cells L(-1)) than in surface waters (22-256 x 10(3) cells L(-1)). These results suggest a selective incorporation of larger cells into sea ice. The >= 4 mu m protist assemblage was composed of a total number of 73 taxa, including 12 centric diatom species, 7 pennate diatoms, 11 dinoflagellates and 16 flagellates. The taxonomic composition in the early stage of ice formation (i.e., new ice) was very similar to that observed in surface waters and was composed of a mixed population of nanoflagellates (Prasinophyceae and Prymnesiophyceae), diatoms (mainly Chaetoceros species) and dinoflagellates. In older stages of sea ice (i.e., young ice and thin first-year ice), the taxonomic composition became markedly different from that of the surface waters. These older ice samples contained relatively fewer Prasinophyceae and more unidentified nanoflagellates than the younger ice. Diatom resting spores and dinoflagellate cysts were generally more abundant in sea ice than in surface waters. However, further studies are needed to determine the importance of this winter survival strategy in Arctic sea ice. This study clearly shows the selective incorporation of large cells (>= 4 mu m) in newly formed sea ice and the change in the taxonomic composition of protists between sea ice and surface waters as the fall season progresses. (C) 2007 Elsevier B.V. All rights reserved.	[Rozanska, Magdalena; Gosselin, Michel] Univ Quebec, ISMER, Rimouski, PQ G5L 3A1, Canada; [Poulin, Michel] Canadian Museum Nat, Div Res, Ottawa, ON K1P 6P4, Canada	University of Quebec	Rózanska, M (通讯作者)，Univ Quebec, ISMER, 310 Allee Ursulines, Rimouski, PQ G5L 3A1, Canada.	magdalena.rozanska@uqar.qc.ca; mpoulin@mus-nature.ca; michel_gosselin@uquar.qc.ca	Gosselin, Michel/B-4477-2014	Gosselin, Michel/0000-0002-1044-0793	Natural Sciences and Engineering Research Council (NSERC) of Canada; Individual and Northern Research Supplement Discovery; Canadian Museum of Nature; CCGS Amundsen; Canada Foundation for Innovation; Fonds quebecois de la recherche sur la nature et les technologies (FQRNT); Institut des sciences de la mer de Rimouski (ISMER); Universite du Quebec a Rimouski	Natural Sciences and Engineering Research Council (NSERC) of Canada(Natural Sciences and Engineering Research Council of Canada (NSERC)); Individual and Northern Research Supplement Discovery; Canadian Museum of Nature; CCGS Amundsen; Canada Foundation for Innovation(Canada Foundation for InnovationCGIARSpanish Government); Fonds quebecois de la recherche sur la nature et les technologies (FQRNT)(Fonds de recherche du Quebec (FRQ)Fonds de recherche du Quebec - Nature et technologies (FRQNT)); Institut des sciences de la mer de Rimouski (ISMER); Universite du Quebec a Rimouski	This project was supported by grants from the Natural Sciences and Engineering Research Council (NSERC) of Canada (Research Network grant to M.P. and M.G.; Discovery grant to M.P.; Individual and Northern Research Supplement Discovery grants to M.G.) and by financial support from the Canadian Museum of Nature to M.P. Partial operating funds for the CCGS Amundsen were provided by the International Joint Ventures Fund of the Canada Foundation for Innovation and the Fonds quebecois de la recherche sur la nature et les technologies (FQRNT). M.R. received post-graduate scholarships from the Institut des sciences de la mer de Rimouski (ISMER) and Universite du Quebec a Rimouski. We sincerely thank the officers and crew of the CCGS Amundsen for their invaluable support during the expedition; Bernard LeBlanc, Christine Michel and Andrea Riedel for assistance in the field and laboratory; Claude Belzile and Sonia Brugel for flow cytometry analyses; Connie Lovejoy and Sylvie Lessard for assistance in some taxonomic identification; and Laure Devine and two anonymous reviewers for their helpful comments. This is a contribution to the research programs of the Canadian Arctic Shelf Exchange Study (CASES), ISMER and Quebec-Ocean.	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Mar. Syst.	DEC 1	2008	74	3-4					887	901		10.1016/j.jmarsys.2007.11.009	http://dx.doi.org/10.1016/j.jmarsys.2007.11.009			15	Geosciences, Multidisciplinary; Marine & Freshwater Biology; Oceanography	Science Citation Index Expanded (SCI-EXPANDED)	Geology; Marine & Freshwater Biology; Oceanography	385KF					2025-03-11	WOS:000261812400011
